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"talus" Definitions
  1. a slope formed especially by an accumulation of rock debris
  2. rock debris at the base of a cliff
  3. the human tarsal bone that bears the weight of the body and that together with the tibia and fibula forms the ankle joint
  4. the entire ankle

748 Sentences With "talus"

How to use talus in a sentence? Find typical usage patterns (collocations)/phrases/context for "talus" and check conjugation/comparative form for "talus". Mastering all the usages of "talus" from sentence examples published by news publications.

Suzuki said a scan in Barcelona had revealed a partial fracture of the Spaniard's talus bone.
"But leaving a room light on can disrupt sleep," said Kim Filippone, marketing director at Talus.
His left foot was sliced open, and the talus bone that pivots the ankle was later removed.
It's above the timberline, and its only features are grass, tarns, and bald peaks of talus and scree.
Off trail, we scramble up a hillside of loose talus and survey some caves littered with small animal bones.
A man named Eldon Surbeck was out hunting fossils when he found it on a talus slope east of Montrose.
They make their habitats in the talus"—the pile of rocky debris at the base of a slope or cliff—"and they find a mode of circulation almost decoupled from the outside.
Moth aggregations also sustain bears, but these concentration points occur in high-elevation talus slopes, or fields of frost-shattered rock in steep mountains, and some bears don't eat the moths for reasons that scientists don't understand.
The North Face's season sale features cold weather classics like up to $100 off men's and women's down parkas, $30 off fuzzy zip-ups, and $20 off convertible pants, plus accessories like the iconic Talus camping tent for $75 off.
A massive, golem-like stone talus is involved, whoops... No spoilers, except to say that I'm playing again this week, which means I need you to choose a new difficulty modifier for me, so go here and place your vote, or just scroll below!
The Franklin Mountain talus snail, scientific name Sonorella metcalfi, is a species of air-breathing land snail, a terrestrial pulmonate gastropod mollusk in the family Helminthoglyptidae. This species is endemic to the United States. The name "talus snail" refers to the fact that snails in this genus live on and in talus. This species is called "Franklin Mountain talus snail" after the Franklin Mountains in Texas.
The San Xavier talus snail, scientific name Sonorella eremita, is a species of air-breathing land snail, a terrestrial pulmonate gastropod mollusc in the family Helminthoglyptidae. This species is endemic to the United States. The common name "talus snail" refers to the fact that snails in this genus live on and in talus.
Talus Lake is located in Grand Teton National Park, in the U. S. state of Wyoming. Talus Lake is NNE of Rolling Thunder Mountain and is at the head of upper Snowshoe Canyon.
It grows on rocky terrain such as talus and fell fields.
Talus blocks up to in size cover the seafloor around Horizon Guyot.
In medical terminology, "ankle" (without qualifiers) can refer broadly to the region or specifically to the talocrural joint. The main bones of the ankle region are the talus (in the foot), and the tibia and fibula (in the leg). The talocrural joint is a synovial hinge joint that connects the distal ends of the tibia and fibula in the lower limb with the proximal end of the talus. The articulation between the tibia and the talus bears more weight than that between the smaller fibula and the talus.
The preferred habitat of T. feicki is upland caves, cliffs, and talus deposits.
Talus caves are formed by the openings among large boulders that have fallen down into a random heap, often at the bases of cliffs. These unstable deposits are called talus or scree, and may be subject to frequent rockfalls and landslides.
The posterior talocalcaneal ligament (posterior calcaneo-astragaloid ligament) connects the lateral tubercle of the talus with the upper and medial part of the calcaneus; it is a short band, and its fibers radiate from their narrow attachment to the talus.
Talus at the bottom of Mount Yamnuska, Alberta, Canada. Scree is a collection of broken rock fragments at the base of crags, mountain cliffs, volcanoes or valley shoulders that has accumulated through periodic rockfall from adjacent cliff faces. Landforms associated with these materials are often called talus deposits. Talus deposits typically have a concave upwards form, while the maximum inclination corresponds to the angle of repose of the mean debris size.
Talus-Saint-Prix is a commune in the Marne department in north-eastern France.
The top of the talus is marked by a decorative string-course of stone.
The treatment of congenital vertical talus can be broadly classified into conservative and surgical.
Devil island is a recent volcano consisting of two basalt volcano necks, surrounded by extensive talus.
The talus (; Latin for ankleMosby's Medical, Nursing & Allied Health Dictionary, Fourth Edition, Mosby-Year Book Inc., 1994, p. 1526), talus bone, astragalus , or ankle bone is one of the group of foot bones known as the tarsus. The tarsus forms the lower part of the ankle joint.
Endangered and Threatened Wildlife and Plants; Determination of Threatened Status for the Cheat Mountain Salamander and Endangered Status for the Shenandoah Salamander. Federal Register, 54(159), 34464-68. The talus slopes are typically dry, so the Shenandoah salamander is generally found within moist microhabitats scattered throughout the talus environment. Although the dry talus slopes are not optimal, the Shenandoah salamander is excluded from optimal forested areas containing deep, moist soil due to competition with the red-backed salamander.
These caves occur throughout Central Oregon, usually in rim rock areas. Finally, there are a few talus caves. Talus caves are found in cracks and open spaces between boulders along faults and in rock fall area. Some Central Oregon caves are easy to explore, especially the larger lava tubes.
Haypiles tend to be stored under the talus near the talus-meadow interface, although they may be constructed on the talus surface. Males generally store more vegetation than females and adults usually store more than juveniles. Pikas deposit two kinds of fecal droppings: Hard, brown, round pellets and pellets that are soft black shiny strings that form in the caecum. Caecal pellets have more energy value than stored plant food and the pika may consume them directly or store them for later.
Rock glacier with multiple flow lobes, Chugach Mountains, Alaska. Rock glaciers are distinctive geomorphological landforms, consisting either of angular rock debris frozen in interstitial ice, former "true" glaciers overlain by a layer of talus, or something in-between. Rock glaciers may extend outward and downslope from talus cones, glaciers or terminal moraines of glaciers. There are two types of rock glaciers: periglacial glaciers (or talus-derived glaciers), and glacial rock glaciers, such as the Timpanogos Glacier in Utah, which are often found where glaciers once existed.
The snail occurs in various outcrops of rock from the bottom of the gorge to the ridgetops. Rock outcrops that are one meter or more in height appear to be potential habitat, as long as there are cracks and crevices that are at least one meter deep. The snail appears to prefer rock talus, but is also found in cliffline areas that contain deep, dark crevices. When the two habitats coincide (rock talus and cliffline), then Triodopsis platysayoides is more often found in the talus.
Algific means "cold producing" while "talus slope" refers to a collection of talus or broken rock which rests near the surface it detached from. A related term is maderate cliff, which is an algific slope lacking talus. They were first described in the early 1980s.Driftless Area National Wildlife Refuge Comprehensive Conservation Plan, United States Fish and Wildlife Service, Retrieved July 24, 2007 (This is very good source, but can take a long time to download) These ecosystems can only exist in regions displaying karst topography.
It transmits the entire weight of the body from the lower legs to the foot.Platzer (2004), p 216 The talus has joints with the two bones of the lower leg, the tibia and thinner fibula. These leg bones have two prominences (the lateral and medial malleoli) that articulate with the talus. At the foot end, within the tarsus, the talus articulates with the calcaneus (heel bone) below, and with the curved navicular bone in front; together, these foot articulations form the ball-and-socket-shaped talocalcaneonavicular joint.
Physaria arctica grows in sand and gravel from calcareous bedrock, river bars and terraces, cliff ledges, scree and talus slopes.
Unlike the flexible flat foot that is commonly encountered in young children, congenital vertical talus is characterized by presence of a very rigid foot deformity. The foot deformity in congenital vertical talus consists of various components, namely a prominent calcaneus caused by the ankle equines or planter flexion, a convex and rounded sole of the foot caused by prominence of the head of the talus, and a dorsiflexion and abduction of the forefoot and midfoot on the hindfoot. It gets its name from the foot's resemblance to the bottom of a rocking chair. There are two subcategories of congenital vertical talus namely idiopathic or isolated type and non-idiopathic type which may be seen in association with arthrogryposis multiplex congenital, genetic syndromes and other neuromuscular disorders.
Allegheny woodrats prefer rocky outcrops associated with mountain ridges such as cliffs, caves, talus slopes, and even mines. This is mostly true for Pennsylvania and Maryland. In Virginia and West Virginia, woodrats are found on ridges, but also on side slopes in caves and talus (boulders and breakdown) fields. The surrounding forest is usually deciduous.
The talus is an architectural feature of some late medieval castles, especially prevalent in crusader constructions. It consists of a battered (sloping) face at the base of a fortified wall. The slope acts as an effective defensive measure in two ways. First, conventional siege equipment is less effective against a wall with a talus.
The os trigonum or accessory talus represents a failure of fusion of the lateral tubercle of the posterior process of the talus bone. Is estimated to be present in 7–25% of adults. It can be mistaken for an avulsion fracture of lateral tubercle of talus (Shepherd fracture) or a fracture of the Stieda process. In most cases, Os Trigonum will go unnoticed, but with some ankle injuries it can get trapped between the heel and ankle bones which irritates the surrounding structures, leading to Os Trigonum Syndrome.
Algific talus slopes are found mainly on north-facing slopes of ridges and canyons and are characterized by crumbly, heavily fissured, and porous exposed bedrock, with an overburden of talus remaining in situ from where it detached from its underlying bedrock; it may also display scree, which is talus finding its narrowest angle of repose down-canyon. This is a "unique system involving ridgetop sinkholes and subterranean ice caves; this system also supports Maderate Cliffs." The valleys in which they occur tend to be very steep, and often have dense forest cover.
Scaling ladders may be unable to reach the top of the walls and are also more easily broken due to the bending stresses caused by the angle they are forced to adopt. Siege towers cannot approach closer than the base of the talus, and their gangplank may be unable to cover the horizontal span of the talus, rendering them useless. Furthermore, defenders are able to drop rocks over the walls, which will shatter on the talus, spraying a hail of shrapnel into any attackers massed at the base of the wall.
A few other caves exist in the system. These are mostly surface tubes, though a couple are shelters or talus caves.
Extensive talus deposits have accumulated around the rock's base. The surrounding soil is primarily the sticky, eroded remnants of volcaniclastic breccia.
Descriptions of the talus (ankle bone) in 2011 have helped to strengthen support for the strepsirrhine status of Azibius and Algeripithecus, which would indicate that the evolutionary history of lemurs and their kin is rooted in Africa. Azibius trerki is the only named species, although a few teeth and a talus (ankle bone) of a larger, unnamed species (cf.
Less frequent patients with arthrogryposis may develop congenital vertical talus also known as rocker bottom foot. Similarly, congenital vertical talus is classically managed by serial casting according to the reversed Ponseti method. Resistant or recurrent cases may be offered an extensive soft tissue release. However this is fraught with risk of foot stiffness and pain on the long term.
The accumulated rock detritus at Ice Mountain's base forms a talus that is thick in some places. It creates a refrigeration effect. As cold air sinks into the talus pile during the cooler months it forms masses of ice and ice vents inside it. The ice vents are in a section about in length along Ice Mountain's southern flank.
The inner walls are slumped in places, forming a pile of talus along the western base. The interior floor is otherwise relatively featureless.
Obsidian debris (talus), Obsidian Dome, California. In geology, debris usually applies to the remains of geological activity including landslides, volcanic explosions, avalanches, mudflows or Glacial lake outburst floods (Jökulhlaups) and moraine, lahars, and lava eruptions. Geological debris sometimes moves in a stream called a debris flow. When it accumulates at the base of hillsides, it can be called "talus" or "scree".
Cote became chairman and CEO of SecureWorks in February 2002 and led the company through an acquisition by Dell in February 2011. Prior to joining SecureWorks, Cote held executive positions with Talus Solutions,. Cote joined Talus from MSI Solutions, a web application development and systems integration company where he was chief operating officer. Cote's early career included international assignments with KPMG.
The talus then moves laterally, shearing off the lateral malleolus or, more commonly, breaking the fibula superior to the tibiofibular syndesmosis. If the tibia is carried anteriorly, the posterior margin of the distal end of the tibia is also sheared off by the talus. A fractured fibula in addition to detaching the medial malleolus will tear the tibiofibular syndesmosis.Moore and Agur.
The species is scattered throughout forested areas where it margins prefer closed vegetation. It grows on limestone, sandstone, basalt, granite, gypsum, porphyry, and talus.
It is common in all habitats within the El Muerto Island: rocks and rubble of talus slopes, scrub, hill ridges, and the intertidal zone.
NanoRoute is an Integrated Circuit routing tool built into Cadence Encounter. Similar software includes Synopsys IC Compiler's ZRoute, and Magma Design Automation's Talus Router.
The term scree comes from the Old Norse term for landslide, skriða, while the term talus is a French word meaning a slope or embankment.
Most of the sediments however are transported upslope; those which do end up at the bottom of the seamount form talus deposits around Horizon Guyot.
In summer, the cooler talus-covered slopes power an air exchange with sinkholes atop the ridge, with warm air entering the sinkhole to an ice cave. The air is cooled and vented on the algific slope. In winter, the airflow is reversed. Cool or cold air is drawn through the algific talus into the ice cave, with flowing water or atmospheric humidity being turned to ice.
An anthropometric study of 1197 North American adult Caucasian males (mean age 35.5 years) found that a man's foot length was 26.3 cm with a standard deviation of 1.2 cm. The foot can be subdivided into the hindfoot, the midfoot, and the forefoot: The hindfoot is composed of the talus (or ankle bone) and the calcaneus (or heel bone). The two long bones of the lower leg, the tibia and fibula, are connected to the top of the talus to form the ankle. Connected to the talus at the subtalar joint, the calcaneus, the largest bone of the foot, is cushioned underneath by a layer of fat.
The ankle joint consists of the talus resting within the mortise created by the tibia and fibula as previously described. Since the talus is wider anteriorly (in the front) than posteriorly (at the back), as the front of the foot is raised (dorsiflexed) reducing the angle between the foot and lower leg to less than 90°, then the mortise is confronted with an increasingly wider talus. The force is heightened when the foot is simultaneously forced into external rotation (turned outward). This chain of events may occur when the front of a hockey player's skate strikes the boards and the foot is forced outward.
The talus apparently derives from the fusion of three separate bones in the feet of primitive amphibians; the tibiale, articulating with tibia, the intermedium, between the bases of the tibia and fibula, and the fourth centrale, lying in the mid-part of the tarsus. These bones are still partially separate in modern amphibians, which therefore do not have a true talus. The talus forms a considerably more flexible joint in mammals than it does in reptiles. This reaches its greatest extent in artiodactyls, where the distal surface of the bone has a smooth keel to allow greater freedom of movement of the foot, and thus increase running speed.
Typical habitat is in chert or shale talus at the edge of chaparral or within chaparral gaps. As its flowers would suggest, it is hummingbird pollinated.
The refuge protects diverse habitat types, including northern hardwood-conifer, hemlock-hardwood, and spruce-fir forests and woodlands, oldfields, scrub-shrub habitat, and rock ledges with talus.
Silene seelyi. Flora of North America.Silene seelyi. Washington Burke Museum. This plant grows on cliffs. It can be found in shady crevices on steep slopes and talus.
It can be found on Grandfather Mountain, Hanging Rock, and Roan Mountain.Solidago spithamaea. The Nature Conservancy. It grows on rocky peaks, cliffs, and slopes covered in talus.
Its range is allopatric with that of the Chinese red pika. It is a rock-dwelling pika which usually inhabits talus deposits (collection of broken rock pieces at the base of cliffs, volcanoes, or valley shoulders, accumulated due to periodic rockfall from adjacent cliff faces) and takes shelter in large boulders. It is typically found at moderate elevations of less than from sea level, despite the availability of the talus environment.
Talus cones on the north shore of Isfjorden, Svalbard, Norway. Talus cones are accumulations of coarse hillslope debris at the foot of the slopes producing the material. Ferguson Slide is an active landslide in the Merced River canyon on California State Highway 140, a primary access road to Yosemite National Park. Soil, regolith, and rock move downslope under the force of gravity via creep, slides, flows, topples, and falls.
Fritillaria falcata is a species of fritillary known by the common name talus fritillary. It is endemic to California, known only from 5 counties south and east of San Francisco Bay (Monterey, San Benito, Stanislaus, Alameda and Santa Clara).Biota of North America Program It grows in the Coast Ranges at elevations of 300–1200 m, mostly on serpentine talus. It is sometimes considered a subspecies of Fritillaria atropurpurea.
It is native to California, southern Nevada, and Arizona, where it can be found in many types of habitat, from mountain talus to coastal bluffs to desert scrub.
These teeth are three times larger than those of A. trerki. A larger right talus has also been found, and is assumed to belong to this new species.
USDA Forest Service, Rocky Mountain Region. Blooming occurs in June and July. This plant grows on steep slopes, talus, and the sandy areas at the bases of cliffs.
Pronation of the foot also causes the calcaneus to jam under the talus. The calcaneum cannot rotate and stays in varus. The cavus increases as outlined in step 2.
As a result, the Shenandoah salamander, which has a higher tolerance for dry conditions, is restricted to the talus slope environments in which the red-backed salamander cannot survive.
Collomia larsenii is a species of flowering plant in the phlox family known by the common name talus collomia. It is native to the Olympic Mountains of Washington and the Cascade Range from Washington to northern California, where it grows in high exposed mountainside talus. It is a perennial herb forming a clump in the volcanic rocks. The branching stem is covered in fleshy, glandular, hairy leaves, each divided into many lobes.
Bandiagara Escarpment in Mali. Scarp retreat is a geological process through which the location of an escarpment changes over time. Typically the cliff is undermined, rocks fall and form a talus slope, the talus is chemically or mechanically weathered and then removed through water or wind erosion, and the process of undermining resumes. Scarps may retreat for tens of kilometers in this way over relatively short geological time spans, even in arid locations.
There are over 300 algific talus slopes but some are in poor condition. Anything disrupting the air flow through sinkholes and out the vents can affect the habitat. In the past, the impacts of logging, grazing, road building, quarries, agricultural runoff, and sinkhole filling reduced the number of algific talus slopes. Today, these habitats are still threatened by logging, grazing, agricultural runoff, and sinkhole filling activities and invasive species like garlic mustard.
The surface of the growing pile of about a of lava crumbled continually, forming enormous banks of talus. When Lassen Peak formed it looked much like the nearby Chaos Crags domes do today, with steep sides covered by angular rock talus. Lassen Peak's shape was significantly altered by glacial erosion from 25,000 to 18,000 years ago during the Wisconsin glaciation. At least one of Lassen's glaciers extended as far as from the volcano itself.
The area lacks trees, and comprises steep cliffs, talus slopes, and meadows filled with wildflowers. The volcano can be hiked and has been noted for its trails by local mountaineers.
Cladonia amaurocraea is found in boreal forests, where it typically grows on talus deposits between boulders and on rocky ground. In North America, it is widespread throughout Canada and Alaska.
Footballer's Ankle is a pinching or impingement of the ligaments or tendons of the ankle between the bones, particularly the talus and tibia. This results in pain, inflammation and swelling.
Proplatyarthrus was named and a talus bone described by Florentino Ameghino in 1905.Ameghino, 1905, p.59 It was assigned to Megalonychidae by Carroll in 1988.R. L. Carroll. 1988.
The sandy soil overlies talus, and the often steep canyon slopes are easily eroded. The habitat is dry and relatively warm native grassland with some shrubs.Mirabilis macfarlanei. The Nature Conservancy.
Both of the sexes claim their talus using scent-markings and vocalizations. While they can defend territories in pairs, males are more known to defend their territory from intruders than females.
The resort is southeast of Yosemite Village, at an elevation of , and occupies a central position in the Yosemite Valley. It lies on a talus cone of debris from old rockfalls.
The plant is endemic to the Klamath Mountains of far northern California and southern Oregon. It grows in mountain habitats, including alpine talus and subalpine coniferous forest, often on serpentine soils.
Throughout his teenage years he sang for several local bands, such as Talus and Koo-Dot-N-Boo-Jang, most of which played half original songs and half Black Sabbath songs.
The Talus Atlantic 85 DO-DO launch carriage is a Drive On - Drive Off Lifeboat launch and recovery carriage currently used by the RNLI to launch its Atlantic class inshore lifeboats.
There are up to seven kiva depressions around the spring. Remnants of wall alignments below the rim on the talus represent possible terrace farming.Winter, Joseph. (1976). Hovenweep 1975 Archeological Report no.
Strepsirrhines also possess distinctive features in their tarsus (ankle bones) that differentiate them from haplorhines, such as a sloping talo-fibular facet (the face where the talus bone and fibula meet) and a difference in the location of the position of the flexor fibularis tendon on the talus. These differences give strepsirrhines the ability to make more complex rotations of the ankle and indicate that their feet are habitually inverted, or turned inward, an adaptation for grasping vertical supports.
All of the outer towers were rectangular in shape. The second curtain wall has a gate near the inner keep with a high brick arch enclosed by a geometric border, the alfiz, which is a classic Moorish design feature. The inner curtain wall has several towers and a talus as well. It has centered cylindrical towers on each side and smaller turrets between them, while the talus is constructed all the way down to the moat.
The Driftless Area National Wildlife Refuge was established in 1989 to protect native flora and fauna, including endangered and threatened species such as the Iowa Pleistocene snail. The refuge conserves the algific talus slope habitat and other local habitat such as cold, moist sinkholes. Other glacial relict snails occur on the refuge, including the Midwest Pleistocene vertigo (Vertigo hubrichti). Rare plants include the northern blue monkshood (Aconitum noveboracense), which thrives in the same cool talus habitat as the snail.
Epilobium clavatum is a species of flowering plant in the evening primrose family known by the common names talus willowherb and clavatefruit willowherb. It is native to western North America from Alaska to northern California to Colorado, where it grows in rocky high mountain habitat such as talus. It is a clumping perennial herb forming bristly mounds up to about 20 centimeters high and spreading outward via tough stolons. The oval-shaped leaves are 1 to 3 centimeters long.
The talus is the second largest of the tarsal bones; it is also one of the bones in the human body with the highest percentage of its surface area covered by articular cartilage. It is also unusual in that it has a retrograde blood supply, i.e. arterial blood enters the bone at the distal end. In humans, no muscles attach to the talus, unlike most bones, and its position therefore depends on the position of the neighbouring bones.
Diplacus whitneyi is endemic to the southern Sierra Nevada of California, such as below the Mount Whitney area. It grows in bare and disturbed habitat, such as exposed talus slopes and roadsides.
This formation in places can be found cropping out at sea bottom. The depositional environment is thought to be talus and open marine basin. Biostratigraphic data indicate a Tertiary age.Clemente, 2013, p.
Hot, dry upper slopes, cool, moist ravines, and mineral-rich ledges of basalt talus produce a combination of microclimate ecosystems on the mountain that support plant and animal species uncommon in greater Massachusetts.
Most scientists regard the bauxites of the Mediterranean province as talus and proluvial deposits having formed from the products of the erosion of the lateritic and subsequently having undergone the process of bauxitization.
Formerly lumped with Cryptogramma acrostichoides, C. cascadensis was described as a distinct species by Ed Alverson in 1989. The type specimen was collected growing on talus below Chair Peak, northwest of Snoqualmie Pass.
Calamagrostis purpurascens grows in dry mountainous zones, from high up on the foothills to close to the snow-line, often taking root in gaps in the talus, where few other plants can grow.
Hot, dry upper slopes, cool, moist ravines, and mineral-rich ledges of basalt talus produce a combination of microclimate ecosystems on the mountain that support plant and animal species uncommon in greater Massachusetts.
It can grow in dry, marginal habitat, such as roadsides, dry meadows, and talus. Thus it can be used for rock gardens, providing bright bunches of yellow when few other plants are blooming.
The dominant, largest, and most obvious tree species are Metrosideros angustifolia, Brabejum stellatifolium, Cassine schinoides, Apodytes dimidiata, Cunonia capensis, Ilex mitis, Kiggelaria africana, Rapanea melanophloeos, Olinia ventosa, and Podocarpus elongatus. Western Cape Talus forests naturally undergo periodic disturbance, flooding in the case of riverine forests, and rock-slides in the case of scree forests. Swift regeneration immediately follows. The natural cycle of disturbance of the surrounding fynbos vegetation is fire-driven, but this has little effect on the sheltered talus forests.
The refuge currently consists of scattered tracts in northeast Iowa ranging from a few acres to a few hundred acres. Land acquisition from willing sellers is ongoing. Restoration of forest or prairie habitat is conducted on the land surrounding algific talus slopes and provides habitat for a variety of wildlife including white-tailed deer, wild turkeys, bald eagles, American woodcock, woodpeckers and a variety of songbirds. States, counties, and private organizations like The Nature Conservancy also help protect algific talus slopes.
Pilsbry (1948) reported that Novisuccinea chittenangoensis was found "on a sloping weedy talus near the foot of the falls." The only sloping weedy talus is on the east side of the Falls. This area is adjacent to and between the vegetated ledge at the base of the Falls where Novisuccinea chittenangoensis now occurs and the spring-fed watercress beds previously reported to be Novisuccinea chittenangoensis habitat. Presence of Novisuccinea chittenangoensis has not been verified on the west side of the Falls.
The Shenandoah salamander species is believed to have originated in the Appalachians of eastern North America, though the historical abundance of this species is unknown. Currently, Shenandoah salamanders are exclusively found on the north-facing talus slopes of three mountains within the Shenandoah National Park in Virginia: Hawksbill, The Pinnacles, and Stony Man (see range map). Each of the three talus slopes houses an isolated salamander population residing at approximately 3,000 feet above sea level.U. S. Fish and Wildlife Service (1989).
When the foot is on the ground, the muscle helps to balance the leg and talus on the other tarsal bones so that the leg is kept vertical even when walking on uneven ground.
Talus is an unincorporated community in Inyo County, California. It is located on the Southern Pacific Railroad north-northwest of Coso Junction, at an elevation of 3730 feet (1137 m). It was incorporated in 1847.
The medial talocalcaneal ligament (internal calcaneo-astragaloid ligament) connects the medial tubercle of the back of the talus with the back of the sustentaculum tali. Its fibers blend with those of the plantar calcaneonavicular ligament.
Adjacent family territory centres are generally separated by , but can be as close as . Like other pika species, it is a generalist herbivore, and stores vegetation in the form of hayplies (piles of grass, legumes, or other herbaceous plants that serve as animal fodder). However, unlike most other pikas, it does not feed in open meadows, but in an area of within from the talus-vegetation edge. They have wide home ranges and can find sufficient food, as the vegetation on the talus is widely dispersed.
The masonry walls are made of sandstone cobbles collected from the talus slope. The second segment and a major defensive feature is the eastern moat. The wide moat separated the mesa from the open plateau along with a strong wall incorporated on the northeastern face completing a ribbon of defense against access from the plateau approach. The third segment and second room block of Crumbled House is about to the south of the castle on a steep talus slope, stepping down about in five or six terraces.
Halme was divorced from his wife Katja Talus. He had a Schutzstaffel tattoo on his calf. On July 4, 2003, a handgun was fired inside Halme's apartment. No one was injured, but the gun was unlicensed.
The Pecos has around 150 miles of streams holding rainbow trout, brown trout, and cutthroat trout. The scenery ranges from 100-foot waterfalls and crumbled talus slopes to dramatic cliff rocks, towering peaks, and wildflower meadows.
It was published by Black Star Crime books. Two years later, he published a sequel, Close Enemies. In 2014, Edwards published the hybrid low fantasy detective novel Talus and the Frozen King under his own name.
Draba globosa. NatureServe. This species grows in mountain habitat such as talus and mountain meadows. It is largely an alpine climate species, growing at elevations above 9,000 feet. It can also be found in subalpine areas.
It is native to western North America from British Columbia to Montana to California, where it grows in the cracks and crevices of mountain talus slopes, especially in moist subalpine areas on volcanic or granite rocks.
Seattle, WA: Mountaineers Books, 2008. Oval Peak has a small rock glacier on its slopes.SummitPost - Oval Peak Retrieved 1 June 2015. Climbing Oval Peak can be difficult due to the amount of talus on its slopes.
The inner walls have slumped around much of the circumference, forming an irregular ring of talus about the interior floor. There are some low ridges near the midpoint and in the eastern half of the floor.
The seeds are winged. Blooming occurs in July and August, and possibly September. This plant is limited to the alpine climates of the high San Juan Mountains. It grows on white volcanic ash and sandstone talus.
Lewisia disepala is endemic to the Sierra Nevada of California, where it is known from several sites high in the mountains. It grows in rocky mountain habitat such as talus and open beds of bare gravel.
The Shenandoah salamander species is threatened by competition by the aggressive red-backed salamander, which restricts the Shenandoah salamander to dry, sub-optimal talus environments and prevents Shenandoah salamander populations from expanding into heavily forested areas. Furthermore, the talus habitat of the Shenandoah salamander is in a state of disintegration due to erosion. Eventually, this weathering will result in soil formation and a subsequent increase in moisture, thus making the talus environment suitable for red-backed salamander invasion and increasing the possibility of extinction of the Shenandoah salamander species Both laboratory and field experiments have provided evidence of the red-backed salamander’s aggressive, territorial behavior toward the Shenandoah salamander. The two species compete for large cover objects that provide cool temperatures and high moisture levels, but the territoriality of P. cinereus results in competitive exclusion of the Shenandoah salamander from moist soil environments.
Puddicombe Falls is a high talus ribbon cascade waterfall found on Stoney Creek in Hamilton, Ontario, Canada. Nearby attractions include Bruce Trail, Puddicombe Farms, Dofasco 2000 Trail, Battlefield House Museum, Devil's Punch Bowl, Erland Lee House Museum.
The plant is native to much of western North America from the Arctic northwestern Canada and Alaska to California and New Mexico. It grows in meadows and talus on high mountain slopes and other open rocky habitat.
The formation overtops the Miocene Tagpochau rocks with an angular unconformity. Talus, marsh sediments and limestones such as the Mariana Limestone are common across the surface, resulting from deposition and mass-wasting during the Pleistocene and Holocene.
The snail has a limited range in two isolated mountain ranges, but it is a common species within this range. The snail lives in open rocky mountain habitat and is only found in accumulations of limestone talus.
Federal Register, Vol. 43, Number 128. Triodopsis platysayoides specimens are typically observed within 1 meter of a rock feature. They can be found in cool, moist, deep fissures in shale, sandstone and limestone outcrops, and in talus.
Blooming occurs in June through August. This plant grows in sagebrush and alpine ecosystems. It grows in dry, rocky mountain habitat such as talus slopes. In Nevada it grows in limber pine and pinyon-juniper woodland habitat.
Oil, Gas and Energy Law is a peer-reviewed academic journal covering all aspects of law pertaining to oil, gas, and energy in general. It publishes short comments, scholarly articles, opinion pieces, and book reviews. The journal was established in 2003 and is published by Maris BV.Publishing, Maris B.V. The founding editor-in-chief was Thomas W. Walde (University of Dundee). The current editors-in-chief are Kim Talus (Tulane University Law School)Kim Talus Joins Tulane as McCulloch Chair in Energy Law, Anas F. Alhajji (Energy Economist)Dr.
Romer-Parsons 1977, pp 205-208 In reptiles and mammals, there are normally just two proximal tarsals, the calcaneus (equivalent to the amphibian fibulare) and the talus (probably derived from a fusion of multiple bones). In mammals, including humans, the talus forms a hinge joint with the tibia, a feature especially well developed in the artiodactyls. The calcaneus is also modified, forming a heel for the attachment of the Achilles tendon. Neither of these adaptations is found in reptiles, which have a relatively simple structure to both bones.
Algific talus slopes along Howard Creek at Driftless Area National Wildlife Refuge, May 2018 Iowa Pleistocene Snail, Discus macclintocki Portions of Iowa, Wisconsin, Minnesota and Illinois contain unusual geology. The karst region, referred to as the "Driftless Area", escaped the last glaciers leaving the Paleozoic-age bedrock subject to erosion. In addition to the curious topography of steep slopes and cliffs, there are unique habitats. Certain slopes, usually north facing, are covered with a talus layer that allows ice- cooled air to exit from underground cracks and fissures.
The Caddo Mountain salamander (Plethodon caddoensis) is a species of salamander in the family Plethodontidae endemic to Arkansas in the south- central United States, and only known from the Caddo Mountains, a part of the Ouachita Mountains. The Caddo Mountain salamander has been found to be abundant in or near talus slopes and other rocky habitats, particularly on north-facing slopes covered by mature, mesic forests. It can also be found in secondary growth, mixed deciduous forests. During dry, hot conditions, these salamanders withdraw into underground retreats under shaded talus or in abandoned mines.
The interosseous talocalcaneal ligament forms the chief bond of union between the talus and calcaneus. It is a portion of the united capsules of the talocalcaneonavicular and the talocalcaneal joints, and consists of two partially united layers of fibers, one belonging to the former and the other to the latter joint. It is attached, above, to the groove between the articular facets of the under surface of the talus; below, to a corresponding depression on the upper surface of the calcaneus. It is very thick and strong, being at least 2.5 cm.
Penstemon digitalis (foxglove beard-tongue,Dickinson, T.; Metsger, D.; Bull, J.; & Dickinson, R. (2004). ROM Field Guide to Wildflowers of Ontario. Toronto: Royal Ontario Museum, p. 332. foxglove beardtongue, talus slope penstemon, or white beardtongue Newcomb, L. (1977).
The Western Pennsylvania Council was formed through the merger of five regional councils: Keystone, Girl Scouts of Beaver and Lawrence Counties, Girl Scouts of Penn Lakes Council, Girl Scouts of Talus Rock Council and Girl Scouts-Trillium Council.
Retrieved July 26, 2011.Highest Mountain Peaks in Arizona. Mountainzone.com. Retrieved July 26, 2011. It grows in alpine tundra habitat in the volcanic talus of the mountain slopes, an area with little vegetation located above the tree line.
Calflora taxon report, University of California: Hulsea vestita (pumice alpinegold) . accessed 2.2.2013Biota of North America Program 2014 county distribution map The plant can generally be found on the talus of mountain slopes, often in soils of volcanic origin.
Other geographic features of the wilderness include steep talus slopes, rock outcrops, and alpine meadows.Willamette National Forest - Mount Jefferson Wilderness Several lakes are situated within the wilderness area, including Marion Lake, Duffy Lake, Santiam Lake and Wasco Lake.
Cerastium sventenii is a species of flowering plant in the family Caryophyllaceae. It is endemic to the Canary Islands. It grows in moist talus in forested habitat. It is threatened by introduced grazing herbivores and non-native plants.
The loose material along the inner walls has slid down to form a ring of talus around the base, leaving walls that slope straight down with no terraces. There is a small crater along the northern rim top.
The holotype was collected on May 24, 1975 from talus accumulation of igneous rock on the east side of the east branch of Maple Canyon. It is deposited at the Academy of Natural Sciences of Drexel University ANSP 340726.
As a result, it is one of the most challenging climbs among Colorado's fourteeners. All routes involve at least class 3 scrambling on loose talus, and poor route-finding can expose the climber to more difficult and dangerous terrain.
Mutations in this gene have been associated with Wilms' tumor and congenital vertical talus (also known as "rocker-bottom foot" deformity or congenital convex pes valgus) and/or a foot deformity resembling that seen in Charcot-Marie-Tooth disease.
A fractured talar body often has a displacement that is best visualised using CT imaging. In case a talus fracture is accompanied by a dislocation, restoration of articular and axial alignment is necessary to optimize ankle and hindfoot function.
The dam, a weir, was merely 43 ft. tall, almost two-thirds of which were built below the riverbed. Subsequently, the dam only raised the river ten feet. Modifications to the dam's downstream talus were done between 1923-1924.
The holotype was collected on April 11, 1975 from limestone talus on the north-facing wall of a canyon indenting the East side of Goat Mountain. It is deposited at the Academy of Natural Sciences of Drexel University ANSP 340724.
The plant is native to the Modoc Plateau in the northeastern corner of California and adjacent sections of Nevada and Oregon. It grows at elevations of , in subalpine coniferous forest, Northern Sierra juniper woodlands, and talus of alpine fell-field habitats.
A few other caves exist in the system. They are mostly very small talus caves along the collapse trench walls. One other, Woolhiser Cave, appears to be a rather large surface tube and is offset from the main lava tubes.
It grows in calcareous soils. The plants grow in meadows and on talus slopes. The land is flat to sloping. The worst threat to this species is probably motorized recreation in the habitat, such as off-road vehicles and snowmobiles.
Eriogonum ursinum is a species of wild buckwheat known by the common names Bear Valley buckwheat and talus buckwheat. It is endemic to northern California where it is found on mountains from the northern Sierra Nevada to the southern Klamath Mountains.
While in the Russian wasteland, Talus has a secret that is so terrible that it will cost him his life if he shares it. The secret is so terrible that he must share it with those who will help him protect the knowledge that will one day save all of humanity. His two brothers, who are both hermit monks, are the ones he has decided to share his secret with. Time is short, and no man could fully prepare themselves with the revelation that this secret holds, a secret Talus’ two brothers will discover: that they are already dead.
The talus bone or ankle bone is connected superiorly to the two bones of the lower leg, the tibia and fibula, to form the ankle joint or talocrural joint; inferiorly, at the subtalar joint, to the calcaneus or heel bone. Together, the talus and calcaneus form the hindfoot.Podiatry Channel, Anatomy of the foot and ankle The five irregular bones of the midfoot—the cuboid, navicular, and three cuneiform bones—form the arches of the foot which serves as a shock absorber. The midfoot is connected to the hind- and forefoot by muscles and the plantar fascia.
The talus bone of the ankle joint connects the leg to the foot. The head of talus looks forward and medialward; its anterior articular or navicular surface is large, oval, and convex. Its inferior surface has two facets, which are best seen in the fresh condition.Gray's Anatomy (1918) The medial, situated in front of the middle calcaneal facet, is convex, triangular, or semi-oval in shape, and rests on the plantar calcaneonavicular ligament; the lateral, named the anterior calcaneal articular surface, is somewhat flattened, and articulates with the facet on the upper surface of the anterior part of the calcaneus.
Fractures to the lower leg are also rare but 20% of injuries are to the foot and ankle. Fractures of the talus bone are rare in other sports but account for 2% of snowboard injuries – a lateral process talus fracture is sometimes called "snowboarder's ankle" by medical staff. This particular injury results in persistent lateral pain in the affected ankle yet is difficult to spot in a plain X-ray image. It may be misdiagnosed as just a sprain, with possibly serious consequences as not treating the fracture can result in serious long-term damage to the ankle.
The Achilles tendon is inserted into a roughened area on its superior side, the cuboid bone articulates with its anterior side, and on its superior side are three articular surfaces for the articulation with the talus bone. Between these superior articulations and the equivalents on the talus is the tarsal sinus (a canal occupied by the interosseous talocalcaneal ligament). At the upper and forepart of the medial surface of the calcaneus, below the middle talar facet, there is a horizontal eminence, the talar shelf (also sustentaculum tali), which gives attachment to the plantar calcaneonavicular (spring) ligament, tibiocalcaneal ligament, and medial talocalcaneal ligament. This eminence is concave above, and articulates with the middle calcaneal articular surface of the talus; below, it is grooved for the tendon of the flexor hallucis longus; its anterior margin gives attachment to the plantar calcaneonavicular ligament, and its medial margin to a part of the deltoid ligament of the ankle-joint.
Among other smaller trailheads which provide on-street parking and access directly or via connecting trails to the park trail system are the following: # Newcastle Crosstown Trail Trailhead at SE 85th St near 146th Pl SE in Newcastle # Cul de sac at end of 161st Ave SE south of SE Cougar Mountain Way in Bellevue # Indian Trail/Licorice Fern Trail crossing of SE Licorice Way above 169th Ave SE on the south side of the park # Ring Road Trailhead located in the private area above Wilderness Creek Trail # Bear Ridge Trailhead on SR900 1 mile south of Newport Way with overflow area just south of creek culvert. # Big Tree Ridge Trailhead on Newport Way NW 1/2 mile NW of SR-900 Renton-Issaquah Road SE (pullover parking). # Talus Neighborhood: The Bridges neighborhood in SW corner (Talus Bridge Trail) and Shangri-la Way at center west (Surprise Creek Trail) # Harvey Manning Park at Talus. Restrooms, water fountains, play equipment.
It is endemic to California, where it is known only from the Kings-Kern Divide in the Sierra Nevada, a series of high mountain peaks near the intersection of Tulare, Fresno, and Inyo Counties. It grows in weathered rocky habitat such as talus.
Hot, dry upper slopes, cool, moist ravines, and mineral-rich ledges of basalt talus produce a combination of microclimate ecosystems on the mountain that support plant and animal species uncommon in greater Connecticut. Ragged Mountain is also an important raptor migration path.
Leaves are gray-green, some forming a rosette at the base, others attached to the stem. Heads are small but numerous, yellow. The species is found in tundra and on talus slopes.Flora of North America, Artemisia furcata M. Bieberstein, Fl. Taur.-Caucas.
The posterior talofibular ligament, runs almost horizontally from the malleolar fossa of the lateral malleolus of the fibula to a prominent tubercle on the posterior surface of the talus immediately lateral to the groove for the tendon of the flexor hallucis longus.
The small interior floor is located in the middle of this ring of talus. The interior is free of impacts of note. This crater lies near the center of the Mendel-Rydberg Basin, a 630 km wide impact basin of Nectarian age.
Narrow ravines crowded with hemlock block sunlight, creating damp, cooler growing conditions with associated cooler climate plant species. Talus slopes are especially rich in nutrients and support a number of calcium-loving plants uncommon in eastern Connecticut.The Traprock Wilderness Recovery Strategy . Cited Dec.
It often weathers to prominent scarps without talus. For the most part, Middle Cretaceous rocks include thick sandstone, although some marine rocks are present to the north and Jordan. A combined sequence of of limestone and dolomite spans the Cretaceous into the Paleogene.
Most of its known locations are in the George Washington National Forest. Its natural habitats are temperate forests, talus, and high elevations. It is threatened by habitat loss and climate change. While it is a rare species, it is abundant in small localities.
On the bone's inferior side, three articular surfaces serve for the articulation with the calcaneus, and several variously developed articular surfaces exist for the articulation with ligaments. For descriptive purposes the talus bone is divided into three sections, neck, body, and head.
Northern red-backed voles are commonly found in northern shrub vegetation or open taiga forests. They also inhabit tundra. Northern red- backed voles are abundant on early successional sites as well as in mature forests. They occasionally inhabit rock fields and talus slopes.
Lespedeza frutescens, commonly known as shrubby lespedeza, is a species of herbaceous plant in the legume family. It is native to eastern North America, where it is found on cliffs, balds, or ledges, forests, ridges or ledges, talus and rocky slopes, woodlands.
Alpine plants usually occur in communities spaced between barren talus slopes. Cushion-shaped Diapensia lapponica usually grows in communities in the windiest areas, and in less exposed sites sedge, heath, snowbank, and alpine bog communities can be found.Slack and Bell, pp. 69–78.
Butternut is found most frequently in coves, on stream benches and terraces, on slopes, in the talus of rock ledges, and on other sites with good drainage. It is found up to an elevation of in the Virginias – much higher altitudes than black walnut.
The Ili pika inhabits talus slopes at high elevations, usually from about 2,800 to 4,100 meters. This species constructs haypiles and is a generalized herbivore. It primarily feeds on grasses and herbs. Almost nothing is known about the ecology or behavior of the species.
This improvement was necessary to house the inshore lifeboat. The new Talus MB-H T99 tractor which was supplied to improve the launch equipment for the lifeboats was then housed in the old inshore lifeboat house, which also had to be enlarged and altered.
The Beebe vent field is located in the very near vicinity of the spreading center, which has been described as an ultraslow ridge at a rate of to per year. The area is primarily basalt, with metal-sulfide mounds and talus sourced from hydrothermal activity.
Spray Falls is a waterfall in the Mount Rainier National Park in Pierce County, Washington. The falls are fed by Spray Creek, which is a tributary of the Puyallup River. The falls drop about into a talus slope in a vailed horsetail form about wide.
In human anatomy, the subtalar joint, also known as the talocalcaneal joint, is a joint of the foot. It occurs at the meeting point of the talus and the calcaneus. The joint is classed structurally as a synovial joint, and functionally as a plane joint.
Merope was a daughter of King Oenopion, who was a legendary ruler of Chios and son of Princess Ariadne. He was said to have brought winemaking to the island. Her mother was Helike. She was a sister to Melas, Talus, Euanthes, Salagus and Athamas.
Specifically, it prefers dry basalt talus scree overlying clay soils. It associates with the low sagebrush community, and specific associates include Artemisia arbuscula, Poa secunda, Elymus elymoides, Arenaria aculeata, Phlox spp., Erigeron linearis, etc. The fire ecology is unknown for members of this genus.
Podistera nevadensis is endemic to California, where it is known only from the highest peaks of the Sierra Nevada, the White and Inyo Mountains, and the San Bernardino Mountains. It is a plant of alpine climates above the tree line, growing in gravel and talus.
The dorsal talonavicular ligament is a broad, thin band, which connects the neck of the talus to the dorsal surface of the navicular bone; it is covered by the Extensor tendons. The plantar calcaneonavicular supplies the place of a plantar ligament for this joint.
Luzula orestera, with the common name Sierra woodrush, is a species of flowering plant in the rush family. It is endemic to the High Sierra Nevada of California, where it grows in fellfields, talus, and other habitat in regions of subalpine and alpine climates.
The western paintbrush occurs in areas above and below the treeline. It is found in dry places, favoring rocky soils and talus slopes. It has thin, lanceolate leaves (with occasionally lobed upper leaves) borne on woody stems. The bracts are pale yellow to nearly white.
The medial arch is higher than the lateral longitudinal arch. It is made up by the calcaneus, the talus, the navicular, the three cuneiforms (medial, intermediate, and lateral), and the first, second, and third metatarsals. Its summit is at the superior articular surface of the talus, and its two extremities or piers, on which it rests in standing, are the tuberosity on the plantar surface of the calcaneus posteriorly and the heads of the first, second, and third metatarsal bones anteriorly. The chief characteristic of this arch is its elasticity, due to its height and to the number of small joints between its component parts.
They are mainly elsewhere in Iowa, but also in southeastern Minnesota, southwestern Wisconsin and northwestern Illinois. In winter and early spring comparatively warm air rises from the elaborate system of sinkholes, causing cold moist air to be drawn into the north-facing talus slopes and sent through fissures into ice caves, where it turns to ice on the walls of the cave. In summer and fall, the system is reversed, with cool moist air venting to the talus slopes, creating a unique ecosystem. The only road into the preserve is closed on both the north and south sides of the preserve as of June 7, 2013.
Griffiths was a prolific poet who published widely in Britain and the United States. In later years he lived in Seaham, County Durham, and ran Amra Press, which published his poetry and books of local studies. Griffiths' books of poetry from other publishers include Rousseau and the Wicked (Invisible Books, London, 1996), Etruscan Reader 5 (with Tom Raworth and Tom Leonard) (Etruscan Books, Buckfastleigh, 1997), Nomad Sense (Talus Editions, London, 1998), A Book of Spilt Cities (Etruscan Books, 1999), Ushabtis (Talus, 2001) and Durham and other sequences (West House Books, 2002). A substantial collection of his work was also published in Future Exiles (Paladin 1992).
Talus slopes on Bare Mountain The ridge of the Holyoke Range was formed 200 million years ago during the late Triassic and early Jurassic periods and is composed of traprock, also known as basalt, an extrusive volcanic rock. Basalt is a dark colored rock, but the iron within it weathers to a rusty brown when exposed to the air, lending the ledges a distinct reddish appearance. Basalt frequently breaks into octagonal and pentagonal columns, creating a unique "postpile" appearance. Huge slopes made of fractured basalt talus are visible beneath many of the ledges; they are particularly visible along the Metacomet-Monadnock Trail on Bare Mountain.
The Shawangunk Conglomerate is very hard and resistant to weathering; whereas the underlying shale erodes relatively easily. Thus, the quartz conglomerate forms cliffs and talus slopes, particularly along the eastern margin of the ridge. The entire ridge was glaciated during the last Wisconsin glaciation, which scoured the ridges, left pockets of till, and dumped talus (blocks of rock) off the east side of the ridge. On top of the ridge, the soils are generally thin, highly acidic, low in nutrients, and droughty, but in depressions and other areas where water is trapped by the bedrock or till, there are interspersed lakes and wetland areas.
The project construction will be in two distinct construction projects. Phase 1: Will remove the existing talus material and install cable drapery to minimize additional rock fall. Work will begin in spring 2015. Phase 2: Will construct a 750-foot rockshed structure on the same alignment.
Packera werneriifolia, known by the common names alpine rock butterweed and hoary groundsel, is a species of flowering plant in the aster family. It is native to the western United States in the Sierra Nevada mountain habitat in subalpine and alpine climates, including forests and barren talus.
Felsenmeers only form on slopes of 25° or lower. A steeper angle results in transport of the blocks due to gravity. This creates a talus slope, rather than a felsenmeer.Dahl, R. (1966) Block fields, weathering pits and tor-like forms in the Narvik Mountains, Nordland, Norway.
Flora of North America. This plant grows in high mountain habitat types, mainly in alpine climates, and sometimes in the subalpine zone. It grows in rocky talus and tundra habitat, most commonly in the latter. It grows in areas where snow persists most of the year.
Other shrubs on the mountain include mountain whitethorn, buckwheat, and mountain gooseberry. Wildflower species include Galium parishii, San Gabriel alumroot, gray monardella, pumice alpinegold, Parry's pussypaws, Nuttall's sandwort, and caulanthus. There are also Ross's sedge and rockcress. Oreonana vestita, a type of mountainparsley, is adapted to talus.
The angular rock fragments gather at the foot of the slope to form a talus slope (or scree slope). The splitting of rocks along the joints into blocks is called block disintegration. The blocks of rocks that are detached are of various shapes depending on rock structure.
Gastrotheca pacchamama is a terrestrial species occurring in puna grasslands at an elevation of about asl. The type series was found under rocks. Some males were calling during the day from moss-covered talus. Gastrotheca pacchamama is a poorly known species occurring in an isolated area.
The first documented and reported case in Japan involved a baby girl exhibiting microcephaly, severe edema, and other symptoms. In her case she had a condition known as congenital vertical talus or rocker-feet. The foot is abnormally shaped in a convex position. She survived 134 days.
Dice were originally made from the talus of hoofed animals, leading to the nickname "bones" for dice. Colloquially known as "knucklebones", these are approximately tetrahedral. Modern Mongolians still use such bones as shagai for games and fortune- telling, with each piece relating to a symbolic meaning.
On Steens Mountain in Oregon it has been observed among western juniper (Juniperus occidentalis), curlleaf mountain-mahogany (Cercocarpus ledifolius), and quaking aspen (Populus tremuloides). In the Tendoy Mountains of Montana it is associated with big sagebrush (Artemisia tridentata) and Indian ricegrass (Oryzopsis hymenoides) on limestone talus.
Hot, dry upper slopes, cool, moist ravines, and mineral-rich ledges of basalt talus produce a combination of microclimate ecosystems on the mountain that support plant and animal species uncommon in greater Connecticut. (See Metacomet Ridge for more information on the geology and ecosystem of Beacon Hill).
Superficial deposits refer to geological deposits typically of Quaternary age (less than 2.6 million years old). These geologically recent unconsolidated sediments may include stream channel and floodplain deposits, beach sands, talus gravels and glacial drift and moraine. All pre-Quaternary deposits are referred to as bedrock.
This species grows in a number of habitat types, especially in alpine environments. It can be found in talus, on cliffs and ledges, fellfields, tundra, and meadows. It grows in a wide variety of heath ecosystems. The soils may be dry to moist, calcareous, and acidic.
Lower Sanatorium Falls is a talus classic cascade waterfall found near the Chedoke Civic Golf Course in Hamilton, Ontario, Canada. Nearby attractions include the Bruce Trail, Dundas Valley Conservation Area, Mountview Falls, Tiffany Falls Conservation Area, Iroquoia Heights Conservation Area, Chedoke Radial Trail, Chedoke Civic Golf Course.
The only known Parvinatator fossil was located in an unknown horizon from the Sulfur Mountain Formation in a talus deposit, so its exact geological age is unknown. Best estimates place the fossil somewhere between the Olenekian and Ladinian age around 251-235 mya.Motani, R. (1999). Phylogeny of the Ichthyopterygia.
S Glacier is in North Cascades National Park in the U.S. state of Washington, on the east slopes of Hurry-up Peak. S Glacier is disconnected in several spots. The uppermost sections terminate in icefalls, while the lower section ends in talus. Total descent of the glacier is from .
South of the fault on the west coast is breccia interbedded with the basalts. The breccia matrix is mud, and the stones consist of basalt, dolerite, and gabbro. The southern end of Bauer Bay has a talus of breccia 140 m thick. On top is greywacke and chert.
Fifty Road Cascade is a talus ribbon cascade waterfall found at the Vinemount Conservation Area in Stoney Creek, Hamilton, Ontario, Canada. Nearby attractions include the Bruce Trail, Puddicombe Farms, Puddicombe Falls, Dofasco 2000 Trail, Battlefield House Museum, Devil's Punch Bowl, Devil's Punch Bowl Conservation Area, Erland Lee House Museum.
Grand Cascade is a talus ribbon cascade waterfall found on private property (with permission to access) in Stoney Creek, Hamilton, Ontario, Canada. Nearby attractions include the Bruce Trail, Puddicombe Farms, Dofasco 2000 Trail, Battlefield House Museum, Devil's Punch Bowl, Devil's Punch Bowl Conservation Area, Erland Lee House Museum.
A talus of crushed shells of murex shells (correctly, specimens of Bolinus brandaris and Hexaplex trunculus) along the western slope can still be seen. This artificial mound (100 m. long and 50 m. high) was formed by the accumulation of refuse from the purple dye factories of Phoenician times.
Plagiomnium cuspidatum, also known as toothed plagiomnium moss and woodsy thyme-moss, is a species of thyme-moss found in North America, Africa and Asia. It grows in wet meadows, forested rich peatlands, wet forests, fire- dependent woodlands, mesic hardwood forests, and cliff/talus at low to moderate elevations.
The tractor, a Talus four wheel drive hydrostatic mode TW24H (registration No. K313 ENT) cost the sum of £147,000. To launch, the new tractor would propel the lifeboat on its carriage trailer, reversing down to the beach on the concrete slipway and pull it back up on retrieval.
Chondroblastoma shows a predilection towards the male sex, with a ratio of male to female patients of 2:1. The most commonly affected site is the femur, followed by the humerus and tibia. Less commonly affected sites include the talus and calcaneus of the foot and flat bones.
The southeastern flank of the main Tocorpuri volcano shows evidence of a sector collapse. On its west side lies a rhyolite lava dome called Cerro La Torta. Its steep sides are surrounded with talus and its top surface has flow structures. The complex is located at about 30 km.
Each head has 65–110 blue, lavender, or white ray florets surrounding numerous yellow disc florets. The species grows on cliffs, talus, gravel, and dry tundra.Flora of North America, Erigeron porsildii G. L. Nesom & D. F. Murray, 2004. Porsild’s Arctic fleabane Nesom, Guy L. & Murray, David Fletcher 2004.
The Barbapapa series of books by Annette Tison and Talus Taylor was published in France in the 1970s. They feature the shapeshifting pink blob Barbapapa and his numerous colorful children. The Mr. Men series of 40-some books by English author and illustrated Roger Hargreaves started in 1971.
Nemophila heterophylla is a species of flowering plant in the borage family known by the common name small baby blue eyes. It is native to South east UK and California north of the Transverse Ranges. It grows in many types of habitat, from valley chaparral to mountain talus.
The granodiorite has been altered to create talus, and there are few outcrops, which only occur at stream bottoms and rarely at cliffs that have not been covered with talus. Lava flows, likely produced during the Pleistocene epoch, were deposited in the Lewis River canyon to the west of the Silver Star Mountain and in the Wind River canyon to the east. Silver Star Mountain consists of late Eocene epoch to Oligocene epoch rock, particularly calc-alkaline volcaniclastic sediment. These rock formations were intruded on the mountain's eastern side by the Silver Star intrusion, a deep stock of granodiorite and quartz diorite that also formed small deposits of copper in the area.
The short story is prefaced by an excerpt from an article about Professor J. Howard Erlenmeyer, who claims to have solved the mystery of the Easter Island statues, saying they were beyond doubt religious artifacts. On the continent Mu, in the province of Lac, a governor is about to be elected. Robar, Clevum and Dolph are three campaign workers trying to get Talus elected, but every time they have an idea to counter the smear campaign from incumbent governor Vortus, their boss Oric claims Talus is so noble that he won't allow it. Finally they decide to distribute stone statue caricatures (huge noses and bat ears) of Vortus to the polling places at election day.
Williams Island was formed about 9,100 years ago when sea levels began to rise at the start of the Holocene. The island's geological structure consists of an upper platform of calcarenite laying over on "a U-shaped ridge of pink granite, dark coloured porphyritic granite gneiss with intrusions by large, dark dolerite dykes." The open end of the "U" aligns with the island's northern coast. The U-shaped ridge is visible as an "encircling wall of steep cliffs and talus slopes" over which the "calcarenite platform starts as a talus slope of fractured rock and scree or as low cliffs and overhangs" thickens into "a thick layer of soil" covering most of the island.
At the base of these cliffs (on the western side of the Notch Road, Vermont Route 108), there is a honeycomb network of talus caves. There are cliffs on the eastern side of the Notch Road as well. These two sets of facing cliffs are separated by at their base.
The dome is located on the northwestern side of Cerro del Azufre. It is constructed from three lobes with diameters of . The flanks of the dome are steep and talus and lava blocks lie at its feet. Cerro Chanka has a SiO2 content of 66% and is of calc-alkaline origin.
View of Fajana de Franceses, in the island of La Palma, Spain. A fajã () is a Portuguese-language term of obscure origin designating supratidal talus- platform geology constructed from landslides or lava flows, that are relatively common coastal features, occurring on the toe of cliffs.G. Lameiras et al. (2009), p.
A minimally-invasive surgical intervention involving a small implant is also available. The implant is inserted into the sinus tarsi and prevents the calcaneus and talus from sliding relative to each other. This prevents the sinus tarsi from collapsing and thus prevents the external symptom of the fallen arch from occurring.
The anterior talocalcaneal ligament (anterior calcaneo-astragaloid ligament or anterior interosseous ligament) is a ligament in the foot. The anterior talocalcaneal ligament extends from the front and lateral surface of the neck of the talus to the sinus tarsi of the calcaneus. It forms the posterior boundary of the talocalcaneonavicular joint.
The Capitan Reef also found a stable foundation on the reef debris and talus that rested on its slopes, and this foundation allowed the reef to grow outward. In some locations, nutrients and minerals were so abundant that the Capitan Reef grew out almost 50 km from the starting point.
Gyldén and Saunder lie to the west and east, respectively. The rim of Horrocks is somewhat irregular and polygonal, particularly with an outward protrusion on the eastern rim. It has a small outer rampart. The inner wall is slumped, particularly along the northwest where it forms a heap of talus.
Vinemount West Falls is a talus ribbon cascade waterfall found on CN property near the unincorporated settlement of Vinemount in Stoney Creek, Hamilton, Ontario, Canada. Nearby attractions include the Bruce Trail, Vinemount Conservation Area, Dofasco 2000 Trail, Battlefield House Museum, Devil's Punch Bowl, Devil's Punch Bowl Conservation Area, Erland Lee House.
It is endemic to the eastern San Francisco Bay Area of California. It is known only from Mount Diablo and Mount Hamilton, both in the Diablo Range. Its habitat is mostly rocky chaparral slopes and talus. Although it is rare, most occurrences are in remote mountainous locales that are relatively safe from disturbance.
Judging from the properties of its talus, Azibius was probably an arboreal quadruped, capable of leaping and climbing in trees, very similar to living cheirogaleid lemurs. Based on what can be inferred from the maxillary remains, Azibius is thought to have had large eyes and extra vibrissae, which suggests it was nocturnal.
The gulf experiences an average of three cyclones each year that are thought to transport sediments in a clockwise direction along the Gulf's coast.Harris, P.T., Heap, A., 2009. Cyclone-induced net sediment transport pathway on the continental shelf of tropical Australia inferred from reef talus deposits. Continental Shelf Research 29, 2011-2019.
He was shut down, and the team announced he would not be available for the playoffs and would have surgery to repair the problem. Kemp suffered an articular talar injury requiring microfracture surgery to his talus bone. He appeared in only 73 games in 2013, due to his various injuries. He hit .
There are two summits, with the true summit rising on the north. The volcanic features include piles of monzogranite and basalt talus on the mountain's steep slopes. The hill is composed of aphanitic alkaline olivine basalt, with phenocrysts of olivine. Xenoliths of lherzolite are abundant and more rarely of White Tank monzogranite.
The towers on the corners of the walls are rectangular. The surviving wall is machicolated. This coupled with the talus served as a formidable defence. The battlements on the walls have been constructed as both ornament and as defensive fortifications, so they have been built with crests that jut out from the walls.
These types of fused bones are called atavistic, e.g., the coracoid process of the scapula, which has been fused in humans, but is separate in four-legged animals. ostrigonum (posterior tubercle of talus ) is another example for atavistic epiphysis. # Aberrant epiphysis: These epiphyses are deviations from the norm and are not always present.
Gymnocarpium dryopteris has small, delicate fronds up to 40 cm (16 inches) long, with ternately- compound pinnae (leaves). Fronds occur singly. On the underside of matured pinnae the naked sori can be found (the Latin generic name gymnocarpium means "with naked fruit"). The species grows in coniferous woodlands and on shale talus slopes.
Talus slopes beneath cliffs accumulate minerals that support alkaline-loving plant species uncommon in surrounding acidic southern New England. Extensive cliffs provide ideal habitat and important migration corridors for raptor species.Raymo, Chet and Raymo, Maureen E. Written in Stone: A Geologic History of the Northeastern United States. Globe Pequot, Chester, Connecticut, 1989.
Any other populations have been extirpated or determined to belong to other species. This plant grows in open talus and rock ledges between stands of Ponderosa pine and Douglas-fir. The soil is sandy and rocky and low in nutrients, and few other plants grow in it. The plant does not tolerate shade.
Forks of the Credit Provincial Park, located in Caledon, Ontario, Canada, is part of the Ontario Parks system and is part of the Niagara Escarpment biosphere. The park is on the Bruce Trail. The Credit River runs through the park. Other notable features of the park include a kettle lake and talus slope.
It is bounded on the northern and western sides by densely forested hills. Thick forests are relieved by smooth meadows and deep valleys as the terrain slopes from north to south. Cliffs, talus, and caves provide refuge for several animals. The two forested rectangles are formed of the Tadoba and Andhari ranges.
The neck of talus is directed anteromedially, and comprises the constricted portion of the bone between the body and the oval head. Its upper and medial surfaces are rough, for the attachment of ligaments; its lateral surface is concave and is continuous below with the deep groove for the interosseous talocalcaneal ligament.
Talus slopes beneath cliffs accumulate minerals that support alkaline-loving plant species uncommon in surrounding acidic southern New England. Extensive cliffs provide ideal habitat and important migration corridors for raptor species.Raymo, Chet and Raymo, Maureen E. Written in Stone: A Geologic History of the Northeastern United States. Globe Pequot, Chester, Connecticut, 1989.
196, 200. The removal of the talus and the damage to the castle stonework in the 16th century had put excessive pressure on the supporting motte, causing a recurrence of the 14th century subsidence.Cooper, p.200. Sir Basil Mott, a leading Victorian engineer, installed concrete underpinnings to stabilise the structure beneath the gatehouse.
Lower Hopkins Cascade is a 6 metre high talus classic cascade waterfall found in the Borer's Falls Conservation Area in Flamborough, Hamilton, Ontario, Canada. Nearby attractions include Rock Chapel Golf Course, Smokey Hollow Resource Management Area, Spencer Gorge / Webster's Falls Conservation Area, Borer's Falls, Little Rock Chapel Falls, Royal Botanical Gardens, Dundurn Castle.
The plantar calcaneonavicular ligamentous complex is a broad and thick band with three constituent ligaments that connect the anterior margin of the sustentaculum tali of the calcaneus to the plantar surface of the navicular. Its individual components are the superomedial, intermedial (medioplantar) and lateral (inferoplantar) ligaments, which fan out and attach to the navicular bone at three separate locations. This ligamentous complex not only serves to connect the calcaneus and navicular, but supports the head of the talus, forming part of the articular cavity in which it is received. It helps to maintain the medial longitudinal arch of the foot, and by providing support to the head of the talus, bears most of the body weight in a normally functioning foot.
The indications for the operation in general are as follow: # patients with primary or posttraumatic osteoarthritis with relatively low functional demand; # patients with severe ankle rheumatoid arthritis but not severe osteoporosis of the ankle; # patients suitable for arthrodesis but rejecting it. The general contraindications are: # varus or valgus deformity greater than 15 degrees, severe bony erosion, severe talus subluxation; # substantial osteoporosis or osteonecrosis particularly affecting the talus; # previous or current infections of the foot; # vascular disease or severe neurologic disorders; # previous arthrodesis of the ipsilateral hip or knee or severe deformities of these joints. Other potential contraindications such as capsuloligamentous instability and hindfoot or forefoot deformities affecting correct posture, are not considered relevant if resolved before or during this surgery.
Layia discoidea is a local serpentine endemic where it is known only from the Diablo Range in southern San Benito County and far western Fresno County. The known distribution of the species is the New Idria serpentine mass (BLM Clear Creek Management Area) and nearby Laguna Mountain, Hepsedam Peak, and Panther Peak serpentine masses. Layia discoidea is regarded as a strict serpentine endemic with several populations known (as of 2017) to occur on greywacke and chert outcrop and talus at the edge of the New Idria Serpentine Mass near Condon Peak, Sampson Peak, and Idria Reservoir. Typical habitat of the species is serpentine rock outcrop, serpentine talus, and serpentine stream terraces where it grows in full sun with little to no competition from other plant species.
The mountain from the south side consists of mostly talus with small rocky outcroppings, often compared with mountains in the Colorado Rockies. The northeast side is much different, with a steep rocky summit sheltering the small Entiat Glacier. Most climbers will climb Maude, Seven Fingered Jack, and sometimes Mount Fernow in the same trip.
The erosive relief of the middle part of the mountains occupies absolute altitudes in a range of 1700 up to 3000 m. Gorges and narrow valleys up to 700 m. deep with steep slopes are most typical here. The relief of the given chord is notable for intensive by slope processes: talus, downfalls and rockfalls.
East Glover Falls is a talus ribbon cascade waterfall found in Hamilton, Ontario, Canada. Nearby attractions include Bruce Trail, Glover’s Falls, Mount Albion Conservation Area, Felker's Falls, Felker's Falls Conservation Area, King's Forest Golf Course, Mohawk Sports park, Glendale Golf Course, Dofasco 2000 Trail, Battlefield House Museum, Devil's Punch Bowl, Devil's Punch Bowl Conservation Area.
Sedum oreganum is a species of succulent plant of the genus Sedum. It grows along the Pacific Coast of North America from Alaska to far northern California. The plant, known by the common name Oregon stonecrop, grows in many types of rocky habitat, including coastal bluffs and cliffs and the talus of higher inland mountains.
The terrain in this zone is dominated by ice, snow, rock, and glaciers. Glacier-related features like cirques, talus, alpine lakes and moraine are common. Climate is a major barrier to life; the growing season is extremely short. Mean average temperature usually ranges from to , and even in summer the average temperature does not exceed .
The sides of Mount Conner are also blanketed by scree (talus) and its top is blanketed by colluvium. The base of Mount Conner is surrounded by alluvium.Young, DN, N Duncan, A Camacho, PA Ferenczi, and TLA Madigan (2002a) Ayers Rock, SG 52-8 map, 1:250 000 Geological Series (Second Edition), Northern Territory Geological Survey.
Marie Morisawa was part of the geomorphology revolution in the 1950s and 1960s. This work involves measuring both slopes and stream channels and understanding the relationship they have on larger scale impacts. Marie worked on talus slopes in the Rocky Mountains doing research involving geomorphology. Morisawa was also one of the founders of environmental geomorphology.
The etymology is doubtful, although some sources suggest it may be from Old English side "hillside, talus, slope" (related to Old Norse siða, of similar meaning), but nothing is confirmed. The first element is uncertain. However, another source claims a completely different etymology, that it was named after "Scissett Wood", itself named after a woman.
The east side has shade and water, the west has high walls. The rock formations provide for spectacular pinnacles that attract rock climbers. The park features unusual talus caves that house at least 13 species of bats. Pinnacles is most often visited in spring or fall because of the intense heat during the summer.
All inner canyon descents are strenuous and require Class 3 climbing and basic route finding skills. Steep talus, impassable ledges, and lack of cover are some of the challenges hikers are faced with. Poison ivy also grows abundantly in the draws and on the canyon floor. Long sleeves and hiking boots are strongly recommended.
The cross stratification of the layers were formed in s shallow bottomed lake where it drops into deeper water. The slope reflects the change from the shallows into deeper water. Are like this were used as rock shelters by Native Americans and early pioneers. Along the valley escarpment, talus rocks have fallen into the valley.
Raymo, Chet and Raymo, Maureen E. (1989). Written in Stone: A Geologic History of the Northeastern United States. Chester, Connecticut: Globe Pequot. Hot, dry upper slopes, cool, moist ravines, and mineral-rich ledges of basalt talus produce a combination of microclimate ecosystems on the mountain that support plant and animal species uncommon in greater Connecticut.
Hot, dry upper slopes, cool, moist ravines, and mineral-rich ledges of basalt talus produce a combination of microclimate ecosystems on the mountain that support plant and animal species uncommon in greater Connecticut. Trimountain is also an important raptor migration path. (See Metacomet Ridge for more information on the geology and ecosystem of Trimountain).
Raymo, Chet and Raymo, Maureen E. (1989). Written in Stone: A Geologic History of the Northeastern United States. Chester, Connecticut: Globe Pequot. Hot, dry upper slopes, cool, moist ravines, and mineral-rich ledges of basalt talus produce a combination of microclimate ecosystems on the mountain that support plant and animal species uncommon in greater Connecticut.
Hot, dry upper slopes, cool, moist ravines, and mineral-rich ledges of basalt talus produce a combination of microclimate ecosystems on the mountain that support plant and animal species uncommon in greater Connecticut. Short Mountain is also a raptor migration path. (See Metacomet Ridge for more information on the geology and ecosystem of Short Mountain).
In general, these snakes are not aggressive. They tend to rely heavily on their camouflage, and will often not strike or even rattle their tails unless physically harassed. They spend most of their lives in rocky outcroppings and talus slopes, from which they are named. Man-made road cuts are often a favorite place.
Hot, dry upper slopes, cool, moist ravines, and mineral-rich ledges of basalt talus produce a combination of microclimate ecosystems on the mountain that support plant and animal species uncommon in greater Connecticut. Bradley Mountain is an important raptor migration path. (See Metacomet Ridge for more information on the geology and ecosystem of Bradley Mountain).
Based on the cranium, this species had an external brain surface much like that of gibbons and cercopithecoid monkeys. The wrist of this species has been described as monkey-like. This species has a talus in which the trochlear surface is highly curved and deeply grooved. The foot of this species possessed a transverse arch.
Lower Fruitland Falls is a talus ribbon cascade waterfall found on CN property in Stoney Creek, Hamilton, Ontario, Canada. Named after the road that lies just north of it, Fruitland Road. Nearby attractions include the Bruce Trail, Dofasco 2000 Trail, Battlefield House Museum, Devil's Punch Bowl, Devil's Punch Bowl Conservation Area, Erland Lee House Museum.
Unlike Alpine pikas, which live in a family group, Hoffmann's pikas are typically asocial. They rarely interact, unless they are in pairs. These pairs will claim territory together and share a hay-storage, which they store together. They are very territorial of their claimed talus, or sloping rock formation, especially against those of the same sex.
Hot, dry upper slopes, cool, moist ravines, and mineral- rich ledges of basalt talus produce a combination of microclimate ecosystems on the mountain that support plant and animal species uncommon in greater Connecticut. Manitook Mountain is also an important raptor migration path. (See Metacomet Ridge for more information on the geology and ecosystem of Manitook Mountain).
The type specimen of Ohmdenosaurus consists of a tibia and a talus bone (astragalus). The tibia is approximately long with an estimated femur length of at least . This yields an estimated total body length of , which is relatively small for a sauropod. A re-evaluation of Ohmdenosaurus' size suggests a body length of and a weight of .
This plant grows in the transition between desert scrub and grassland. In the Santa Rita Mountains it grows on limestone talus and in Mexico it has been found on granite. Other plants in the habitat include Eysenhardtia, Erythrina, Cercidium floridum, Tecoma, Agave schottii, Heteropogon, Fouquieria, Calliandra, Opuntia spp., Krameria, Janusia gracilis, Agave palmeri and Hibiscus coulteri.
The flowers are pale blue and appear in May through July. This species grows in rocky, sandy habitat, such as sandstone outcrops and talus slopes. The rare plant faces a number of threats, including petroleum exploration, off-road vehicle use, sand and gravel mining, road maintenance, poaching, pesticides, livestock grazing and trampling, introduced species of plants, and climate change.
The argument for strepsirrhine affinities was strengthened in 2011 when Marivaux et al. published an interpretation of recently discovered talus bones found at Gour Lazib, which they claimed were more similar to those of living strepsirrhines and extinct adapiforms, not simians. The tali morphology also differed radically from those of plesiadapiforms, confirming that azibiids are true primates.
In mountains with predominantly crystalline rock the heads of the valleys are generally very wet, sometimes boggy and often support lush alpine meadows, whilst those made of limestone are usually dry and covered in talus or gravel. Where there has been ice age glaciation, the valley bottoms are modified by moraines and mountain lakes are common.
Iowa Pleistocene snail Northern monkshood The Driftless Area contains more than half of the world's algific talus slopes, a type of small, isolated ecosystem. These refugia create cool summer and fall microclimates which host species usually found further north. They contain at least one endangered species, the Iowa Pleistocene Snail, and a threatened plant, the Northern monkshood.
Shimada Seamount is a seamount in the Pacific Ocean located southwest of Baja California Sur in Mexico. It is a shallow seamount, reaching a depth of below sea level and is a regular single-peaked mountain with a westerly spur and little relief otherwise. A platform lies at a depth of . Talus deposits surround the seamount at its base.
The Azufrera stage edifice was subject to the most alteration; especially in the summit area and between the Angulo and Azufrera summits lie sulfur rich talus deposits. The central part of the complex is heavily altered by fumarole activity. Hydrothermal alteration may be driven by the formation of a deep magma reservoir and resulting hydrothermal circulation in overlying rocks.
Open sites are the majority on both sides of the river. The majority of sites, mostly Navajo camps, feature lithic garbage or ceramics, or both. Talus sites are rarely recorded. Most of the cultural remains found are chipped stone tools (lithic materials), including projectile points, scrapers, drills, knives, choppers, and ground stone tools and manos (grinders).
Penstemon tracyi is a rare species of penstemon known by the common names Trinity penstemon and Tracy's beardtongue. The plant is endemic to Trinity County, California, where it is known from fewer than 10 occurrences in the Trinity Alps, of the Klamath Mountains. It grows in exposed rocky outcrops and barren talus in the high mountains.
Piper Sandy Grieve of the Black Watch, who had fought against the South African Boers as part of the Highland Brigade, in the Battle of Magersfontein in 1899 and been wounded through the cheeks, played the South Africans out. The survivors spent the night at Talus Boise and next day withdrew to Happy Valley south of Longueval.
The talocalcaneonavicular joint is a ball and socket joint: the rounded head of the talus being received into the concavity formed by the posterior surface of the navicular, the anterior articular surface of the calcaneus, and the upper surface of the plantar calcaneonavicular ligament. There are two ligaments in this joint: the articular capsule and the dorsal talonavicular.
He stars in the 2018 film Con Man, an independent film about the life of Barry Minkow, the famous con man. Hamill plays Minkow's father, Robert Minkow. Hamill appears in second season of historical fiction drama series Knightfall, premiered in 2019. His role is Master Talus, a veteran Templar who trains the initiates at the Chartres Temple.
Private landowners are perhaps the most significant stewards of remaining algific talus slopes. The Fish and Wildlife Service contacts land owners whose properties have these habitats and offers assistance in managing them. The Refuge is managed from McGregor, Iowa, where tours can be arranged. Fishing and White-tailed deer hunting are permitted in a small number of units.
Hot, dry upper slopes, cool, moist ravines, and mineral-rich ledges of basalt talus produce a combination of microclimate ecosystems on the mountain that support plant and animal species uncommon in greater Massachusetts. East Mountain is also an important raptor migration path. (See Metacomet Ridge for more information on the geology and ecosystem of East Mountain).
Hot, dry upper slopes, cool, moist ravines, and mineral- rich ledges of basalt talus produce a combination of microclimate ecosystems on the mountain that support plant and animal species uncommon in greater Massachusetts. Provin Mountain is also an important raptor migration path. (See Metacomet Ridge for more information on the geology and ecosystem of Provin Mountain).
Hot, dry upper slopes, cool, moist ravines, and mineral-rich ledges of basalt talus produce a combination of microclimate ecosystems on the mountain that support plant and animal species uncommon in greater Connecticut. West Suffield Mountain is also an important raptor migration path. (See Metacomet Ridge for more information on the geology and ecosystem of West Suffield Mountain).
Talus MB-H is a continuous track launch tractor which was specifically designed for the Royal National Lifeboat Institution (RNLI), to launch and recover lifeboats from beach-launched lifeboat stations. The tractor was built by Clayton Engineering Limited in Knighton, Powys.OS Explorer Map 201 - Knighton and Presteigne Tref-y-clawdd a Dyffryn Elan, Author: Ordnance Survey. Publisher: Ordnance Survey.
The species occurs in areas of moist talus and rocky substrates in redwood or Douglas fir forests. It is typically encountered among moss-covered rocks or under bark and other forest litter, usually avoiding very wet areas. The Del Norte salamander is locally abundant in suitable habitat. It is threatened by habitat loss caused by logging.
The Mount Lyell salamander (Hydromantes platycephalus) is a species of salamander in the family Plethodontidae. It is endemic to the Sierra Nevada mountains of California, United States. It is found in a range of microhabitats, such as rock exposures, talus and rock fissures, and under rocks or in caves or crevices. Its altitudinal range is above sea level.
A steep talus cascade is also found at the foot of the falls. Rainy Lake's outlet stream eventually flows into the Stehekin River. The drainage area of Rainy Lake Falls is very small, but its sources allow it to retain water all year long, with best flows from May through August. It is located alongside the North Cascades Highway.
Prior to starting Nomis Solutions, Phillips was Chief Technology Officer of Manugistics. He also was founder and CEO for Talus Solutions, which was acquired by Manugistics in 2000 and CEO of Decision Focus Incorporated (DFI), a management consulting company. He was elected to the 2014 class of Fellows of the Institute for Operations Research and the Management Sciences.
Hot, dry upper slopes, cool, moist ravines, and mineral-rich ledges of basalt talus produce a combination of microclimate ecosystems on the mountain that support plant and animal species uncommon in greater Connecticut. Pistapaug Mountain is also an important raptor migration path. (See Metacomet Ridge for more information on the geology and ecosystem of Pistapaug Mountain).
Hot, dry upper slopes, cool, moist ravines, and mineral-rich ledges of basalt talus produce a combination of microclimate ecosystems on the mountain that support plant and animal species uncommon in greater Connecticut. Hatchett Hill is also an important raptor migration path. (See Metacomet Ridge for more information on the geology and ecosystem of Hatchett Hill).
Hot, dry upper slopes, cool, moist ravines, and mineral-rich ledges of basalt talus produce a combination of microclimate ecosystems on the mountain that support plant and animal species uncommon in greater Connecticut. Pinnacle Rock is also an important raptor migration path. (See Metacomet Ridge for more information on the geology and ecosystem of Pinnacle Rock).
The Sapphires contain three large National Forest roadless areas, in addition to the officially protected Welcome Creek Wilderness. The northernmost, about 77,000 acres in size, is centered on Quigg Peak, el. 8419 ft. This area is characterized by thousands of acres of sliderock or talus slopes, and extensive Douglas-fir and lodgepole pine forests rising to open, glaciated ridges.
Hot, dry upper slopes, cool, moist ravines, and mineral-rich ledges of basalt talus produce a combination of microclimate ecosystems on the mountain that support plant and animal species uncommon in greater Connecticut. Fowler Mountain is also an important raptor migration path. (See Metacomet Ridge for more information on the geology and ecosystem of Fowler Mountain).
Hot, dry upper slopes, cool, moist ravines, and mineral-rich ledges of basalt talus produce a combination of microclimate ecosystems on the mountain that support plant and animal species uncommon in greater Connecticut. Lamentation Mountain is also an important raptor migration path. (See Metacomet Ridge for more information on the geology and ecosystem of Lamentation Mountain).
There are two small ponds in the notch, the Carter Lakes, as well as a large boulder field named The Ramparts. The ponds drain south through the talus barrier formed by The Ramparts. The height of land is to the north. To the north, the notch drains via Nineteenmile Brook, which flows into the Peabody River.
Lower Little Falls is an 8.2 metre high talus ribbon cascade waterfall found in Ancaster, Hamilton, Ontario, Canada. Nearby attractions include the Bruce Trail, Tiffany Falls Conservation Area, Tiffany Falls, Dundas Valley Conservation Area, Hermitage ruins, Griffin House, Fieldcote Memorial Park & Museum, Royal Botanical Gardens, Dundurn Castle, Crooks Hollow Conservation Area, Christie Lake Conservation Area, Iroquoia Heights Conservation Area.
Koenigia davisiae is native to the western United States from Washington, Oregon, and central and northern California (northern Coast Ranges and northern Sierra Nevada). There are also isolated populations in central Idaho. It grows in high mountain habitat, such as talus and fellfields.Biota of North America Program 2014 county distribution mapCalflora taxon report, University of California, Aconogonon davisiae (W.
A view of Mount Agassiz from the west, near Bishop Pass, showing a talus slope and several chutes, August 2007. In 1879, Lilbourne Winchell named it Agassiz Needle for Harvard University professor of zoology and geology Louis Agassiz. Later, the USGS recognized it by its current name. The peak is named after Swiss-American scientist Louis Agassiz.
These findings showed that archaeocetes were more terrestrial than previously thought, and that the special construction of the talus (ankle bone) with a double-rolled joint surface, previously thought to be unique to even-toed ungulates, were also in early cetaceans. The mesonychids, another type of ungulate, did not show this special construction of the talus, and thus was concluded to not have the same ancestors as cetaceans.alt=A hippo splashes in the water The oldest cetaceans date back to the early Eocene (53 million years ago), whereas the oldest known hippopotamus dates back only to the Miocene (15 million years ago). Some doubts have arisen regarding the relationship between the two, as there is a 40-million-year gap between their first appearances in the fossil record.
China is home to the Ochotona gaoligongensis, Gaoligong Pika, where it lives in a meadow-like habitat. Its locality includes, Gaoligong Mountains, located northwest of the Yunnan Province, China, where their name derives. Pikas primarily live in habitats which consist of leaves and grass. They are usually found in mountain terrains at high altitudes and in talus slopes and rock boulders.
The Alaska marmots live in polar habitats including the terrestrial tundra and mountain biomes. They are located at elevations of about to . They are often found in boulder fields, rock slides and outcrops, terminal moraines, and Talus slopes in Alpine tundra with herbaceous forage. They are often found on mountain slopes surrounding lakes, and are found less commonly away from a lake.
Lonesome Lake, on the south side of the mountain, is a popular hiking destination and is the location of the Appalachian Mountain Club-maintained Lonesome Lake Hut. The Appalachian Trail passes Lonesome Lake but does not cross the summit of Cannon. The base of the cliff face can be approached via an ambiguous path up the right side of the talus field.
Polemonium eximium, the skypilot or showy sky pilot, is a perennial plant in the phlox family (Polemoniaceae) that grows at high altitudes (mostly above ).Sierra Nevada Wildflowers, Elizabeth Horn, Mountain Press Publishing Co., , 1998, p. 126 It is endemic to the Sierra Nevada in California where it grows in the talus of the high mountain slopes.Sierra Nevada Wildflowers, Karen Wiese, 2nd ed.
The Northcutt-Carter Route of Hallett Peak is recognized in the historic climbing text Fifty Classic Climbs of North America.Stewart M. Green Rock Climbing Colorado, Chockstone, Falcon, Helena, MO, 1995; . Non- technical climbers may reach the summit of Hallett Peak by hiking up the Flattop Mountain Trail to its highpoint, then walking south along the ridgeline and ascending the peak over talus piles.
Colchuck Glacier is in the Stuart Range immediately north of Colchuck Peak and Dragontail Peak, in the U.S. state of Washington. Colchuck Glacier is within the Alpine Lakes Wilderness of Wenatchee National Forest. The glacier is approximately in length, in width at its widest and descends from , where it terminates on barren rock and talus. Below the glacier lies Colchuck Lake.
The river has three waterfalls along its stretch. The first is the Kicking Horse Cascade, a long talus cascade which occurs just below the first highway crossing of the river below Wapta Lake. The second is the Natural Bridge Falls near Field. The final and largest is Wapta Falls, one of the largest waterfalls in Canada in both volume and width.
Flora of North America. There are about 7 to 10 known occurrences of this plant on the high slopes of the Tushar Mountains of central Utah, mostly within the Fishlake National Forest. It occurs on Mt. Belknap and Gold Mountain, and probably other peaks. It grows on barren talus on windy, exposed mountain slopes in alpine tundra habitat above the tree line.
Its northwestern slope is composed from karstified limestone cliffs in which numerous fossiliferous fissures and caves were found. Approximately 48 meter (157 ft) of this slope are covered by complex talus fan. At this place extensive excavations were made by paleonthologist Rudolf Musil and his colleagues in 1956–1968 which yielded rich paleothological material, including Homotherium moravicumM. Anton et al.
The standard ascent route for West Spanish Peak starts at Cordova Pass, a high pass () to the west of the peak. It follows a trail for about to treeline. From there, there's a rough path on talus (scree) up the southwest ridge of the peak for an additional .Mike Garratt and Bob Martin, Colorado's High Thirteeners, Third Edition, Johnson Books, Boulder, Colorado, .
In 2011, Marivaux et al. published an interpretation of recently discovered talus bones found at Gour Lazib, which they claimed were more similar to those of living strepsirrhines and extinct adapiforms, not simians, thus reinforcing the strepsirrhine status favored by Tabuce et al. two years earlier. The tali morphology also differed radically from those of plesiadapiforms, confirming that azibiids are true primates.
Most have since been filled in with andesite lava, pyroclastic flows, and talus from lava domes. Shastina, by comparison, has a fully intact summit crater indicating Shastina developed after the last ice age. Shastina has been built by mostly pyroxene andesite lava flows. Some 9,500 years ago, these flows reached about south and north of the area now occupied by nearby Black Butte.
There are several routes up the mountain, which take 5–6 hours, rising in elevation. Running for round-trip, Old Snowy can be scrambled or climbed using glaciers, although a trail exists. From the summit, mountaineers can see Mount St. Helens and Mount Rainier in the distance. Because this area has a lot of loose talus and rock, an avalanche hazard exists.
Little information on this wallflower species relationship with pollinators exists. Andrew Moldenke studied a population of Erysimum capitatum var. perenne in Subalpine Talus Fell Scree of the Timberland Hall Area ( elevation). He observed 13 species of flower visitors, although over 80% of the visits to the flowers were performed by two ant species, Formica lasioides and one from the Formica fusca group.
A smaller square building, known as the Talus Unit, with a McElmo style floor plan lies just west of Chetro Ketl. The Kiva G complex was constructed using McElmo type masonry, and ceramic evidence uncovered from refuse found in Chetro Ketl indicates a significant McElmo presence. Much of the masonry found in North Block F also appears to be McElmo style.
Scree Cove is a cove on the southwest side of the island. It was mapped by FIDS from surveys and air photos in 1948–59, and named for the very prominent scree or talus slopes along the southern shore of the cove. Mount Kershaw sits on the northeast end of the island, above Kosiba Wall and the former Jones Ice Shelf.
32 and comprises a thick interval of dark grey clayey rocks, interbedded with the clastics of the Santos and Juréia Formations. Within this formation, the Ilhabela Member includes the turbiditic sandstones occurring along the section. The sedimentary environment is thought to be marine talus to open basin. Biostratigraphic data from palynomorphs, calcareous nanofossils and planktonic foraminifera indicate a Late Cretaceous age (Cenomanian-Maastrichtian).
1770) and a pair of paintings based on Milton's Allegro and Penseroso, commissioned by Benjamin Bates (1774). In the 1770s Mortimer was associated with more masculine, and criminal, presentation of the male form after a period of more effete images. His painting Sir Arthegal, the Knight of Justice, with Talus, the Iron Man is used as an example of this style.
Penstemon heterodoxus is a species of penstemon known by the common name Sierra beardtongue. It is native to California and western Nevada where it grows in several of the mountain ranges from the Klamath Mountains to the Sierra Nevada - and the slopes and plateaus to the east. It grows in subalpine and alpine climates in mountain forests, meadows and talus.
Since 2003, a section of the river is protected in the Goulais River Provincial Park. It is a waterway park consisting of a strip of land along both shores of the river. Some of its features includes shoreline wetlands, falls, a lake section, and stretches through talus slopes and bedrock resembling rock gardens. It is home to a self-sustaining brook trout population.
Former Flag used from 1977-1992 With the exception of coastal plains, talus slopes and alluvial fans, most of Pohnpei Island, a high island, is ruggedly mountainous, lush and verdant, with the highest peak at . Its rainforest is dense and rich; extensive mangrove swamps line much of the low shore. The island is roughly circular in outline, its coast surrounded by coral reef.
3D CT image of Trevor's disease of the ankle and talus. This disorder is rare, and is characterised by an asymmetrical limb deformity due to localized overgrowth of cartilage, histologically resembling osteochondroma. It is believed to affect the limb bud in early fetal life. The condition occurs mostly in the ankle or knee region and it is always confined to a single limb.
South slopes of Šator are grassy, in spring covered with carpets of flowers. On the opposite, north side are steep cliffs and scree slopes (also: talus piles) and karst depression with lot of dwarf pine. Šator and area around the mountain were enormous pastures for thousands of cattle, which were driven from as far as Dalmatia, but are now almost depopulated.
Across their entire range, dusky grasswrens adhere to the same habitat type: rocky ranges and outcrops, often preferring tumbled talus or scree, and with areas of thick, long-unburnt spinifex grasses in the genus Triodia. They are not known to use sandplain habitat adjacent to rocky areas which may be one factor giving rise to the patchiness of their occurrence across Central Australia.
On coasts and isolated mountains the tree line is often much lower than in corresponding altitudes inland and in larger, more complex mountain systems, because strong winds reduce tree growth. In addition the lack of suitable soil, such as along talus slopes or exposed rock formations, prevents trees from gaining an adequate foothold and exposes them to drought and sun.
The western red-backed salamander is found from southwestern Oregon to southwestern British Columbia. Within that geographic range, the salamander is found from the western slopes of the Cascade Mountains to the Pacific Coast. The western red-backed salamander has been found on Vancouver Island. A variety of habitats are inhabited by the salamander, including temperate forests, rocky talus slopes, and riparian areas.
Copper Lake Falls is a waterfall about upstream from Malachite Falls. Its three tiers total about in height, and its tallest drop is . The two lower drops probably disappear into the talus they cascade over during lower stream flows, but the upper tier flows over rock hard enough to sustain it all year. The falls flows best from April to July.
Upper Copper Falls is the first of the three Copper Falls along Copper Creek. Well downstream from the much larger Malachite Falls and Copper Lake Falls, the segmented falls is about high, and quite photogenic. One segment of the falls probably dries up during lower stream flows, as it most probably cascades over talus. The falls' best flows are perennial.
Saltonstall Mountain rises steeply above the surrounding landscape, with a high point of (est.) . It is roughly long by wide and shaped like a hunting bow. The mountain lies within the towns of Branford, North Branford, and East Haven, Connecticut. Its western side is steepest, with vertical ledges and talus slopes, while its eastern side is lower and punctuated by hilly rises.
The lateral talocalcaneal ligament (external calcaneo-astragaloid ligament) is a ligament in the ankle. It is a short, strong fasciculus, passing from the lateral surface of the talus, immediately beneath its fibular facet to the lateral surface of the calcaneus. It is placed in front of, but on a deeper plane than, the calcaneofibular ligament, with the fibers of which it is parallel.
Yarmouth, Maine: DeLorme. Considered particularly scenic is Black Pond, located on the northwest side of the mountain. Cliffs and talus slopes plunge into the pond from the ridgeline. Other bodies of water on the mountain include the developed Besek Lake on the east side of the mountain, and the lower end of the Mount Higby Reservoir on the north side.
Catlow Rim in Oregon A stone stripe, also called a lava stringer, is an elongated concentration of mostly talus-like basalt rock found along a hillside or the base of a cliff. Many stringers occur without cliffs. A stringer is identified by its lack of vegetative cover. They typically occur in north central Oregon and develop at 900 to 1,100 meter elevations.
The common rock rat (Zyzomys argurus) is a species of rodent in the family Muridae. It is found only in Australia, where it lives in the rocky areas of woodlands, grasslands and low open forests, particularly on the talus, or scree, of cliff slopes.Larson, Matthes, and Kelly. Cliff ecology: pattern and process in cliff ecosystems. Cambridge University Press, 2000. page 159.
They reside often in high mountains, in the sub-alpine and alpine biome. They also are found in low foothills and forested regions, but to a much smaller extent. They build nesting burrows in the rocks of talus slopes, and rock covered scree. They often fill in rock fissures with excrement mixed with plant debris to form an insulated wall.
A deep portion of the muscle is rarely inserted into the talus, or a tendinous slip may pass to the head of the first metatarsal bone or the base of the first phalanx of the great toe. The tibiofascialis anterior, a small muscle from the lower part of the tibia to the transverse or cruciate crural ligaments or deep fascia.
Under the NatureServe conservation status system, A. viridimontanum is considered globally vulnerable (G3). It is considered imperiled (S2) in Vermont and vulnerable (S3) in Quebec; it has not yet been classified in Maine. Conservation of A. viridimontanum is primarily limited by its restricted habitat on serpentine cliffs and talus slopes. However, these sites are also of little value to humans.
Haystack rocks are blocks of basalt ripped from the entablature of the Columbia River Basalt Group by glacial ice of the Okanogan ice lobe. Preferential weathering along the joints of the entablature results in piles of talus, which together with the weathered erratics, that from a distance look like black haystacks. Some haystack rocks, e.g. Yeager Rock, are the size of large houses.
Külliki Saldre was born in the small town of Kehtna, in Rapla County in 1952, where she graduated from secondary school. Her older sister is performance artist Krista Tool and her younger brother is philosopher and translator Andrus Tool.Index Scriptorum Estoniae Isakodus Juhani talus Karuse külas Läänemaal 2005. a. suvel : Külliki Saldre, ema Leida, õde Krista, tütar Maarja Retrieved 23 December 2016.Kodukolle.
2004 In the southern Tusas Mountains, it fills narrow paleovalleys eroded in basement quartzite. Further south, the rock grades from heterogeneous breccia to a poorly sorted conglomerate. The breccia is interpreted as regolith and talus, while the conglomerate is interpreted as a high-energy stream deposit. The distinctive red color is found penetrating joints in the underlying quartzite to depths of several meters.
In an attempt to retrieve Batch SW6, the Dominators unleash B.I.O.N., an advanced android with all the powers of the Legionnaires. The unit instead engages the adult Legion at their headquarters on the planet Talus. B.I.O.N. is eventually defeated, and Brainiac 5 discovers that it was created using the Computo matrix.Brainiac 5 created Computo in Adventure Comics #340 (January 1966).
This tendon lies in a groove which crosses the posterior surface of the lower end of the tibia, between the medial and lateral tubercles of the posterior surface of the talus, and the under surface of the sustentaculum tali of the calcaneus; in the sole of the foot it runs forward between the two heads of the flexor hallucis brevis, and is inserted into the base of the last phalanx of the great toe. The grooves on the talus and calcaneus, which contain the tendon of the muscle, are converted by tendinous fibers into distinct canals, lined by a mucous sheath. As the tendon passes forward in the sole of the foot, it is situated above, and crosses from the lateral to the medial side of the tendon of the flexor digitorum longus, to which it is connected by a fibrous slip.
The Cardenas Basalt is about thick and is typically divided into lower and upper units. The lower unit ranges in thickness from and forms low, talus covered slopes. It consists of complexly interbedded, thin, and discontinuous beds of basalt, hyaloclastite, and sandstone. Within the lower part of the Cardenas Basalt, the basaltic lavas are highly fractured and weather into rubble that is about in diameter.
The Bureau of Reclamation worked quickly to restore the project in 15 days. In 1918, the Colorado River's meandering damaged part of the Reservation levee and it was repaired slowly with unskilled labor because of World War I's troop demands. The Laguna Diversion Dam weathered the floods but its downstream talus at its toe was extended between 1923 and 1924 to help better protect it.
As a result, runoff has eroded gullies on local slopes and increased removal of soil. However, there are talus slopes with heights up to , which cover a large amount of the granodiorite deposit. Small cirque-like basins, likely carved out by small glaciers, occur in a few of the larger canyons, with depressions up to in depth. These often host tarn lakes, and some support snowdrifts.
From Ueno's performance notes, KenUeno.com His Talus is, in a manner of speaking, a biography of a traumatic event in the life of its soloist, violist Wendy Richman, who shattered her ankle in a ten-foot fall.From Ueno's performance notes, KenUeno.com He is keenly interested in the process of exploring unique, in some sense irreproducible, sonic events linked to the performers for which his music is written.
Potentilla pseudosericea is a species of cinquefoil known by the common names silky cinquefoil and Mono cinquefoil. It is native to the Sierra Nevada of California and mountain ranges just to the east, where its distribution extends into Nevada. It grows in rocky mountainous habitat. It is a small plant forming mats or tufts in rock cracks and talus, its short stem growing from a caudex.
Potentilla morefieldii is a species of cinquefoil known by the common name Morefield's cinquefoil. It is endemic to eastern California, where it is known from just a few occurrences in the White Mountains. It grows in rocky habitat such as talus in alpine climates. This cinquefoil was considered part of the Potentilla drummondii complex until 1992, when it was separated and elevated to species status.
Delphinium purpusii is a rare species of larkspur known by the common names Kern County larkspur and rose-flowered larkspur. It is endemic to California where it is known only from Kern and Tulare Counties in the region where the Sierra Nevada meets the Mojave Desert. It grows on rocky cliffs and talus. This wildflower reaches between one half and one meter in height.
The northern part of the range features rugged Bell and Limekiln Canyons, which contain 700' high cliff faces, ledges, talus, caves and rock walls. A free- standing rock wall, Wedding Ring Rock, is of special geological interest. Indian pictographs are found in some caves. Excellent mule deer habitat is provided by the range's typical habitats of grassland, sagebrush, and ridges forested with lodgepole pine and Douglas-fir.
The gracile body of the heel bone and the robust malleolus (the bony prominence on each side of the ankle) are quite apelike, with less efficient force transfer between the heel bone and the talus, and apelike mobility at the midfoot. A. sediba is most similar to the condition seen in gorillas, and the foot may have been functionally equivalent to that of A. africanus.
Jacobsville Sandstone varies from horizontal to gently inclined and paleocurrents point toward the Lake Superior basin. The Jacobsville Formation outcrops significantly throughout the Upper Peninsula, with lesser exposures in Ontario and Wisconsin. Cliffs of the sandstone tend to have blocky talus that supports little vegetation. Jacobsville Sandstone, rising only a few feet above lake level, is the oldest formation exposed in Pictured Rocks National Lakeshore.
Septarian calcite concretions and calcite geodes are numerous, and the shale forms the less steep canyon walls covered by talus slopes. A prominent band of jointed white sandstone about thick marks the middle of this formation. Lavender, gray and white shales lie below this sandstone, while an orange shale lies between this sandstone and the Trujillo Formation above. The Quartermaster and Tecovas Formations make up Capital Peak.
Narrow ravines crowded with hemlock block sunlight, creating damp, cooler growing conditions with associated cooler climate plant species. Talus slopes are especially rich in nutrients and support a number of calcium-loving plants uncommon in eastern Connecticut. Because the trap rock ridges generate such varied terrain, they are the home of several plant and animal species that are state-listed or globally rare.The Traprock Wilderness Recovery Strategy .
Biota of North America Program 2014 state-level distribution map It grows in mountain talus habitats in subalpine to alpine climates. Artemisia michauxiana is a rhizomatous perennial herb with green, lemon- scented foliage. The plant grows up to 100 cm (40 inches) tall with several erect branches. The leaves are divided into many narrow segments which are hairless or lightly hairy and bear yellowish resin glands.
It came from a talus slope or pile of rock fragments at the base of Mount Celsius, encased in a pale red sandstone. The fossil's origin on the mountain has not been identified. There are four formations preserved at Mt. Celsius, all belonging to the larger Celsius Bjerg Group. Since the skull cannot be traced to any one of these formations, its exact age is uncertain.
Narrow ravines crowded with hemlock block sunlight, creating damp, cooler growing conditions with associated cooler climate plant species. Talus slopes are especially rich in nutrients and support a number of calcium-loving plants uncommon in eastern Connecticut. Because the trap rock ridges generate such varied terrain, they are the home of several plant and animal species that are state-listed or globally rare.The Traprock Wilderness Recovery Strategy .
Hulsea algida is a species of flowering plant in the daisy family, known by the common name Pacific hulsea or alpine gold. Hulsea algida is native to California, Oregon, Nevada, Idaho, Montana, and Wyoming.Biota of North America Program 2014 county distribution map Within California, it grows in the Sierra Nevada and in the White Mountains. It grows between in elevation, in alpine and subalpine talus habitats.
The current lifeboat station was built in 1994 to replace a smaller older one on the same site. The new station gave cover for the first time to the boat and Talus MB-H tractor. Incorporated into the design there is a public viewing platform. The station has showers and toilet facilities for the crew and a heated store for their foul weather suits.
Falls can also result from undercutting by running water as well as by waves. They usually occur at very steep slopes such as a cliff face. The rock material may be loosened by earthquakes, rain, plant-root wedging and expanding ice, among other things. The accumulation of rock material that has fallen and resides at the base of the structure is known as talus.
Morro Chascoso and Pabelloncita Loma are cone shaped domes with blocky slopes with talus and central depressions. The much smaller Cerro Guichi ( high and long) may be an exposed intrusion, considering that it lacks any indication of surface flow. The two southernmost domes of the southern group have similar shapes to Chascoso and Pabelloncita. However the second southernmost dome is accompanied with an andesitic lava flow.
The first recorded ascent was in 1890 by Joseph N. LeConte, Hubert P. Dyer, Fred S. Pheby, and C. B. Lakeman. They called it University Peak. They scrambled the talus of Gould's south ridge, and climbed the more solid rock of its summit block. This route, by way of the Kearsarge Pass Trail from the Onion Valley trailhead, remains the easiest and most accessible approach.
12,253 The bluff has similar geology to the rest of the range, and a similar form with cliffs, and talus (a mixture of scree and soil) slopes. Due to its prominence and isolation, views from the top cover a large portion of Northern Tasmania.Forestry Commission of Tasmania, p.9 In the right conditions Mount Strzelecki on Flinders Island, approximately distant, can be seen from the peak.
In a Russian wasteland two hermits, Pavel and Gustov have heard a horrible secret. As the two sit by a fire one night they are visited by Talus, a man with a secret to share with the two. He shares a secret so terrible that he must share it with those who will help him protect the knowledge that will one day save all of humanity.
Firsov is a lunar impact crater on the far side of the Moon. It is located to due south of the crater Lobachevskiy, and to the northwest of Abul Wáfa. The circular rim of this crater has a small outward bulge along the southern edge, and smaller bulges along the western side. The inner walls have slumped to form talus piles along the base.
Nordin-Frankel 2001, pp 229-30 The talonavicular and calcaneocuboid joints (i.e. between the talus and navicular bones, and the calcaneus and cuboid bones) form the so-called transverse tarsal joint or Chopart's joint. It has two axes of motion. Inversion and eversion occur about a longitudinal axis oriented 15 degrees upward from the horizontal plane and 9 degrees medially from the longitudinal axis of the foot.
The National Park service has noted several designated trails, advising visitors to bring adequate safe water supplies on some trails. The Main Loop Trail is long and loops through archeological areas, including the Big Kiva, Tyuonyi, Talus House, and Long House. It will take between 45 minutes to one hour. There are some optional ladders to allow access to the cavates (small human-carved alcoves).
One site of archaeological interest in the canyon is Tyuonyi (Que-weh-nee) pueblo and nearby building sites, such as Long House. Tyuonyi is a circular pueblo site that once stood one to three stories tall. Long House is adjacent to Tyounyi, built along and supported by the walls of the canyon. A reconstructed Talus House is also found along the Main Loop Trail.
Northern monkshood The threatened Northern Wild Monkshood, belonging to the buttercup family, grows on 114 algific talus slopes and similar cool moist habitats in Iowa, Wisconsin, Ohio and New York. The majority of the sites are in Iowa. The purple hood-shaped flower, an adaptation for bumble bee pollination, was listed as threatened in 1978. Its options for recovery are similar to the snail.
The species occurs in damp talus slopes and rockslides of limestone in young forests dominated by Pinus densiflora and Quercus mongolica, mostly under small stones. Although the species is considered locally common, and reasonably widespread (as of 2006, it was known from more than 20 sites), it has not been well studied in the field. Thus, its natural history, population dynamics, and reproductive behavior remain unknown.
After millions of years of erosion and glaciation, the vertical fin-like form of the Nohku Crags was exposed. Erosion continues to reshape the Crags, as evidenced by the extensive talus field at its base. Today the mountain is a barren, almost treeless form, virtually devoid of vegetation. During the day, pika and mountain goats may be seen and heard on the steep slopes.
It grows on hot, dry talus slopes originating from the Green River Formation, a geological formation. It is unusual in a genus of plants that generally grow in moist habitats. There are few other plants in its arid habitat but other species may include Astragalus lutosus, Mentzelia argillosa, and Festuca dasyclada. There are 18 occurrences of this plant for an estimated total of less than 200,000 individuals.
Biostratigraphic data indicate a Late Cretaceous age (Cenomanian- Maastrichtian). ;Itajaí-Açu Formation The Itajaí-Açu Formation is thick and comprises a thick interval of dark grey clayey rocks, interbedded with the clastics of the Santos and Juréia Formations. Within this formation, the Ilhabela Member includes the turbiditic sandstones occurring along the section. The sedimentary environment is thought to be marine talus to open basin.
The Mátra can be divided into several readily distinguishable parts. The highest point of the Western Mátra is Muzsla (805 m). The Central Mátra consists of the plateau of Mátrabérc (Mátra ridge) and the groups of the volcanic cones of Galya-tető (964 m) and Kékes (1014 m). Steep, rugged slopes, screes, talus slopes and slides alternate with one another, covered with closed beech forests.
C. patruela is found in eastern North America from Minnesota to Massachusetts and Georgia to QuebecEnvironment Canada. 2016. Recovery Strategy for the Northern Barrens Tiger Beetle (Cicindela patruela) in Canada [Proposed], Species at Risk Act Recovery Strategy Series, Environment Canada, Ottawa, vi + 27 p. where it lives in grained sand or sandstone, talus deposits and various forests which have oak trees, or lichen and moss grounds.
Rocky country, including rocky hillsides and canyons, talus slopes and rock ledges. In southern California, these snakes have sometimes been found in chaparral or cactus country, but usually never stray far from the rocks that provide its usual shelter. Not exclusively a rock dweller, they have also been observed emerging from mammal burrows at dusk. The species has been found at elevations of more than .
The ridge tail salamander (Pseudoeurycea obesa) , also known as ridge-tailed salamander is a species of salamander in the family Plethodontidae. It is endemic to Oaxaca, Mexico, and only known from the area of its type locality. Its natural habitat is cloud forest. It is only known from a total of five individuals that were found under small rocks and schist slabs in roadside talus.
Talus MB-764 is a four-wheel drive launch tractor which was specifically designed for the RNLI, to launch and recover inflatable inshore lifeboats from beach and shorebased launched lifeboat stations. The Tractor is produced by the British company of Clayton Engineering Limited who are based in Knighton, Powys.OS Explorer Map 201 - Knighton and Presteigne Tref-y-clawdd a Dyffryn Elan, Author: Ordnance Survey. Publisher: Ordnance Survey.
It may anchor in rock cracks and crevices in talus. It is limited to a small area in southern Washington and northern Oregon, where it can be found in the Columbia River Gorge and the Klickitat River canyon. Threats to the species include poaching, road maintenance, herbicides, quarrying, logging, and recreational activity. This species is named after Almeta Hodge Barrett, who discovered it sometime prior to 1886.
Talus MB-4H is a four-wheel-drive launch tractor which was specifically designed for the RNLI, to launch and recover inshore lifeboats from beach launched lifeboat stations. The Tractor is produced by the British company of Clayton Engineering Limited who are based in Knighton, Powys.OS Explorer Map 201 - Knighton and Presteigne Tref-y-clawdd a Dyffryn Elan, Author: Ordnance Survey. Publisher: Ordnance Survey.
His wife, a Twilight fan, told him he should audition for New Moon, believing he was perfect for the part. They have a son named Somak, for whom his mentor, actor Raoul Trujillo, is the godfather. Somak means "beautiful one" in Quechua, an indigenous language from Bolivia, Ecuador and Peru. In June 2012 the couple had their second child: a son named Talus Alexander Meraz.
The park is bordered on the north by the Lakemont neighborhood in the city of Bellevue and on the northeast by the city of Issaquah. The park is bounded on the east by the 260-acre Talus Open Space. State Route 900 forms the southeastern border. Neighboring Squak Mountain looms to the southeast and the farms of May Creek valley lie to the south.
Lower extremity of tibia seen from the front Lower extremity of tibia seen from the back The distal end of the tibia is much smaller than the proximal end and presents five surfaces; it is prolonged downward on its medial side as a strong pyramidal process, the medial malleolus. The lower extremity of the tibia together with the fibula and talus forms the ankle joint.
The Canyon rim with its steep tributaries is composed of hard, white, grainy Pottsville sandstone. This forms the outcrops and cliffs along the rim which often break off to form talus fields that gradually slide down the forest slopes and pile up at the river bottom. Numerous caves have been formed by water in the Greenbrier Limestone of the lower strata of the Canyon walls.
The episode focuses on Dr. Rodney McKay, who has been infected with a disease known as "Second Childhood", which is considered the Pegasus equivalent of rapid-onset Alzheimer's disease, where he quickly reverts to a childlike state. The only way for the team to save him is to send him to a shrine on the planet of Talus, which has since turned into a Wraith outpost.
Stellaria borealis is a species of flowering plant in the family Caryophyllaceae known by the common name boreal starwort. It has a circumboreal distribution, occurring throughout northern areas of the Northern Hemisphere. It occurs in many types of moist and wet habitat, including marshes, riverbanks, lakesides, floodplains, talus, ditches, and moist spots in forests and woodlands. It is quite variable in appearance, especially across subspecies.
Barbapapa is a 1970 children's picture book by the French-American couple Annette Tison and Talus Taylor, who lived in Paris, France. Barbapapa is both the title character and the name of his "species". The book was the first of a series of children's books originally written in French and later translated into over 30 languages. Barbe à papa – literally "Daddy's beard" – is French for cotton candy or candy floss.
The inspiration for Barbapapa came by chance in the Luxembourg Garden in Paris one day in May 1970. While walking in the park with Annette Tison, Talus Taylor thought he heard a child ask his parents for something called "Baa baa baa baa". Not speaking French, he asked Tison what the words meant. She explained that the child was asking for a treat called Barbe à papa (cotton candy).
Two distinct ridges lead to its summit: Ridge of the Caps and Castle Ridge. The mountain is surrounded by the three dramatic glacial cirques of Jefferson Ravine, Castle Ravine, and the Great Gulf. Finally, Monticello Lawn is a large expanse of alpine sedge and rush near the otherwise talus-covered summit cone. When viewed from the Mount Washington Auto Road, Jefferson features an arrow-shaped bald patch pointing to its summit.
Mineral Hill () is a round-topped hill, high, with ice-free, talus-covered slopes, standing west of Trepassey Bay on Tabarin Peninsula, Antarctica. It was probably first seen by the Swedish Antarctic Expedition under Otto Nordenskiöld, 1901–04. The hill was first charted by the Falkland Islands Dependencies Survey in 1946, who so named it because small quantities of reddish mineral in the rock gave the surfaces a conspicuous color.
Hackelia sharsmithii is a species of flowering plant in the borage family known by the common name Sharsmith's stickseed. It is native to the Sierra Nevada of California, where its range extends along ridges surrounding the intersection of Inyo County and Fresno and Tulare Counties, including Mount Whitney. It is a plant of rocky habitat, such as talus. It is a hairy perennial herb up to about 30 centimeters tall.
The natural habitat of Western Cape Talus is usually within catchment areas, and they thus perform an important function in regulating the water-systems and preventing erosion. They are also host to many scenic hiking trails and have value as a source of medicinal plants. In addition, several species (such as Clivia mirabilis and Cryptocarya angustifolia) are endemic to these forests and occur nowhere else in the world.Rourke, J.P. 2002.
It is still currently under study. The type skull of T. perrini has not been located, but the vomer figured by Merriam in 1905 did not differ from the vomer of T. alexandrae. In 1993, another species named Thalattosarus borealis was found in a talus slope near Wapiti Lake, British Columbia, in the Sulphur Mountain Formation. The environment, similar to the discovery of T. alexandrae, was also marine shale, and marl.
Madroño 57(4) 213-19. The plant is apparently adapted to a fellfield habitat made up of unstable talus, as evidenced by its long rhizome and adventitious roots which may not be anchored to any stable surface. As rocks tumble, the root may break, and pieces of the root can generate new plants through cloning. Despite its being limited to a small area, the plant is common locally.
Hyundai Genesis Coupe concept Hyundai Genesis Coupe In 2002, Eric was recruited as a senior designer to Hyundai Kia Automotive Group in Irvine, California. At Hyundai, under Design Chief Joel Piaskowski, Eric lead the exterior design of the Hyundai Genesis Coupe Concept unveiled at the 2007 LA Auto Show, the Production 2010 Hyundai Genesis Coupe, the HCD-9 Talus Concept, the 2007 Hyundai Elantra and KCD-1 Slice Concept.
The Lake Catherine Quarry is a prehistoric stone quarry in Hot Spring County, Arkansas. The site was used as a source of black novaculite, a relatively rare form of chert. Evidence of Native American quarrying activity at the site includes quarry pits, spoil piles, and a scattered talus slope of rejected materials. The site is untainted by historic quarrying, providing a potentially significant window into prehistoric quarrying methods.
The estimation of stature is only possible if there are complete long bones available There are two different techniques that can be used when estimating stature: anatomical and mathematical methods. The anatomical methods use all elements of the skeleton that contribute to height. These elements include the femur and tibia, the vertebral body heights, including the first sacral segment, talus and calcaneus, and the basion-bregma measurement of the skull.
Tophet Bastion () is a conspicuous ice-capped rock wall, 1 nautical mile (1.9 km) long, with an apron of talus. It stands 1 nautical mile (1.9 km) east of Saunders Point on the south coast of Coronation Island in the South Orkney Islands. Roughly surveyed in 1933 by DI personnel. The name, which is biblical, was applied by the Falkland Islands Dependencies Survey (FIDS) following their survey of 1948–49.
The geology of the Massanutten Mountains is dominated by Silurian Massanutten Sandstone, a lateral equivalent of the Tuscarora Formation in the Appalachian Mountains to the west, overlying the Ordovician Martinsburg Formation. Erosion of the Martinsburg shale in some areas of the mountain caused the sandstone to break and slide to form talus slopes. The Massanutten Sandstone is folded in a synclinorium, and it outcrops at the ridge tops.Frye, Keith.
Viola pinetorum is a species of violet known by the common names goosefoot violet, goosefoot yellow violet, gray-leaved violet, or mountain yellow violet. It is endemic to California, where it grows in mountain ranges throughout the state. It occurs in various types of mountain habitat, including forests and talus. This herb grows from a tough taproot and produces an erect or decumbent stem up to about 22 centimeters long.
Reynolds Mountain () is located in the Lewis Range, Glacier National Park in the U.S. state of Montana. Reynolds Mountain is situated along the Continental Divide and is easily seen from Logan Pass by looking due south from the pass. Hidden Lake is located below Reynolds Mountain to the west. Reynolds is a class 2(3) climb via the southwestern talus slope route that allows many people to easily climb the peak.
Muhlenbergia richardsonis grows in a number of habitat types including talus and meadows in alpine mountain environments, wet alkaline and saline soils, desert arroyos, chaparral, forests and woodlands. It is a species of botanical interest for being an alpine plant utilizing C4 carbon fixation, reported at higher altitudes than any other C4 plant in North America.Sage, R. F. & T. L. Sage. (2002). Microsite characteristics of Muhlenbergia richardsonis (Trin.) Rydb.
The Ledges are a rock outcropping that provides a westward view across the valley's wooded areas. Talus caves are located among the boulders in the forest around the Ledges. The park has many trails, most notably the Towpath Trail, which follows a former stretch of the Ohio and Erie Canal and is popular for hiking, bicycling, and running. Skiing and sled-riding are available during the winter at Kendall Hills.
Pleistocene glaciers further accelerated this process and the larger ones transported the resulting talus and till from valley floors. Numerous vertical joint planes controlled where and how fast erosion took place. Most of these long, linear and very deep cracks trend northeast or northwest and form parallel, often regularly spaced sets. They were created by uplift-associated pressure release and by the unloading of overlying rock via erosion.
Many of the slopes are still very active due to numerous shatter belts within the highly jointed bedrock resulting in the predominantly scree-covered terrain. Although valley glaciations would have been extensive in the Late Pleistocene, most evidence of this has been severely modified due to fluvial erosion and talus deposition. The ski area consists of approximately 80% of this scree with the remaining cover being alpine vegetation.
Erigeron evermannii is a North American species of flowering plants in the daisy family known by the common name Evermann's fleabane. Erigeron evermannii is native to the western United States. It is native to central Idaho and has also been found in western Montana.Biota of North America Program 2014 county distribution map It grows at high elevations in the mountains, on steep slopes, talus outcrops, and ridges, sometime alongside whitebark pine.
It forms the striking summits of the Mieminger and Wetterstein Mountains, not least the Sonnenspitze, Igelskopf and Zugspitze. Because Wetterstein limestone contains few plant nutrients, its scree and talus slopes are largely unvegetated and this tends to characterise the scene above the tree line. A feature of Wetterstein limestone is silver-containing lead and zinc ore. These were mined at Silberleithe and in the rest of the Mieminger Mountains.
Much of the area was covered by glaciers about 500,000 years ago, while parts of the Driftless Area were unglaciated. The algific talus slope habitat that harbors the snail is a landscape cooled by air and water emerging from masses of subterranean ice. The ground temperature rarely exceeds 50 °F even in summer. Here the snail feeds on leaf litter from trees (mainly birch, maple and dogwood) and shrubs.
Raymo, Chet and Raymo, Maureen E. Written in Stone: A Geologic History of the Northeastern United States. Globe Pequot, Chester, Connecticut, 1989. Hot, dry upper slopes, cool, moist ravines, and mineral-rich ledges of basalt talus produce a combination of microclimate ecosystems on the mountain that support plant and animal species uncommon in greater Massachusetts. (The Metacomet Ridge article has more information on the geology and ecosystem of Mount Holyoke).
The North Branch of the Susquehanna River and the Lackawanna River flow through this valley. Large-scale coal mining and its accompanying industry and railroads have long been abandoned. Unlike the southern and middle anthracite fields, the anthracite valley has been recently glaciated repeatedly. This action has left many talus slopes at the base of Moosic Mountains, and the soils often contain large boulders that make excavation difficult.
On the summit of a basalt outcrop is the almost rectangular complex which measures 150 meters on its long north-to-south axis, and 105 meters in width. The walls are protected by numerous round towers and a lethal array of embrasured loopholes (shooting ports). At the south and east is a second highly fortified wall. To the west and north is a massive talus with its own system of tunnels.
Apart from the autapomorphy, a unique combination of, in themselves not unique, traits was also demonstrated. The bottom surface of the shinbone was, in its transverse width, about 1.5 times as wide as the longitudinal distance (measured from front to rear). In dinosaurs in general, the lower front of the shinbone is covered by the talus bone. A ridge on the front surface demarcates the upper limit of this area.
Conrad Glacier is located in the Goat Rocks region of the U.S. state of Washington. Situated on the north side of Gilbert Peak, the glacier flows north-northeast from an elevation of to barren rocks and talus. A proglacial lake at , lies where the glacier once terminated. Between 1970 and 2004, Conrad Glacier lost more than in thickness in some places and split into several separate bodies of ice.
Acid mine drainage drastically alters the acidity (pH values of 2 - 3) and chemistry of groundwater and streams, and may endanger plant and animal populations downstream of mining areas. Activities similar to acid mine drainage, but on a much lower scale, are also found in natural conditions such as the rocky beds of glaciers, in soil and talus, on stone monuments and buildings and in the deep subsurface.
The bowl-shaped depression on the volcano's northeastern flank, called a cirque, was eroded by a glacier that extended out from the dome. By 18,000 years ago, Lassen Peak started to form a mound-shaped dacite lava dome, pushing its way through Tehama's destroyed northern flank. As the lava dome grew it shattered overlaying rock, which formed a blanket of angular talus around the emerging steep-sided volcano.
The house is known popularly as "The Flintstone House", from The Flintstones, a Hanna-Barbera Productions animated cartoon series of the early 1960s about a Stone Age family. It is also known as the Dome House, the Gumby House, the Worm Casting House, the Bubble House, and "The Barbapapa House", from Barbapapa, a character and series of books created by Annette Tison and Talus Taylor in the 1970s.
A large variety of wildlife is found in the wildlife sanctuary. Some precipitous hills have cliffs; have large rock blocks and talus at the base. This unique feature provides shelter to various animals like vultures, reptiles and small mammals. Carnivores are the tiger, leopard, dhole, hyena, jackal and fox, and the herbivores include chital, sambar, nilgai, four-horned antelope, langur and wild boar, and primates: langur and rhesus macaque.
Naviculectomy or simply navicular excision represents a form of mid-tarsal resection arthroplasty. It may be necessary to associate naviculectomy with limited soft tissue releases to address the remaining components of the deformity. Naviculectomy has been practiced on ambulatory and non-ambulatory (non-walkers) patients. Naviculectomy is usually reserved for children with resistant or complicated forms of congenital vertical talus such as neglected, previously operated and recurrent cases.
Careful examination of the thick 'stems' fails to resemble that of the flowers. German scholar Eugen Petersen (1837–1919) proposed that the figures were holding knucklebones (talus bones from goats or sheep used to play the game of jacks) in their left hand and roses in the right hand; Hampe argues that the stele depicts only knucklebones, not flowers.De Ruyt, Franz. (1952). Roland Hampe, Die Stele aus Pharsalos im Louvre.
During WW II the steep east side was used by the German alpine troops for training. It is still possible to see at least one of the campsites used by them on the west side of the road. Earlier, until the 70s, paths of their mules could still be seen in the huge talus slope on the east side. The path is still there, but it is now made by sheep.
In medieval castles, they were often crenellated. In later artillery forts, parapets tend to be higher and thicker. They could be provided with embrasures for the fort's guns to fire through, and a banquette or fire-step so that defending infantry could shoot over the top. The top of the parapet often slopes towards the enemy to enable the defenders to shoot downwards; this incline is called the superior talus.
A moraine would be an easily identified DDA as would an esker. Although scree (talus) is generally easily identified and mapped, these deposits may be modified by ice, avalanches or downlope movement to create essentially new landforms. Many small slope failures and landslides can give the appearance of moraines or protalus ramparts on slopes. After mapping as a DDA, further investigation might draw light on the origin of the feature.
This ecoregion is abundant with varying types of mammals, fish, and birds. Many dominant animal species, such as the bighorn sheep and hoary marmot, have adapted to the terrain of the region. The talus slopes provide burrowing shelters for the hoary marmot, and the bighorn sheep have adapted to climb the steep slopes in order to find shelter from predators (National Park Service). Top carnivorous predators include coyotes, wolves, and cougars.
Piute Creek is a long stream in northern Yosemite National Park, in Tuolumne County, California. It is a major tributary of the Tuolumne River, draining a rugged and remote area of the Sierra Nevada. The creek begins at an unnamed lake near Burro Pass and Matterhorn Peak, flowing west then southwest into Slide Canyon. Here, it briefly flows underground through a fallen talus pile known as "The Slide".
Sisters of Mary Falls is a talus ribbon cascade waterfall found on private property, (private with permission to access), in Ancaster, Hamilton, Ontario, Canada. Nearby attractions include the Bruce Trail, Dundas Valley Conservation Area, Hermitage ruins, Old Mill Restaurant, Griffin House, Fieldcote Memorial Park & Museum, Royal Botanical Gardens, Dundurn Castle, Crooks Hollow Conservation Area, Canterbury Falls, Christie Lake Conservation Area, Tiffany Falls, Tiffany Falls Conservation Area, Iroquoia Heights Conservation Area.
236 in the Harcourt version. The novel evolved from a verse play that Warren began writing in 1936 entitled Proud Flesh. One of the characters in Proud Flesh was named Willie Talos, in reference to the brutal character Talus in Edmund Spenser's late 16th century epic poem The Faerie Queene.See All the King's Men, published 1946 Harcourt, Brace and Co., and 1953, by Random House, publisher of the Modern Library.
Smelowskia americana is a species of Smelowskia known by the common names alpine smelowskia, Siberian smelowskia, and American false candytuft. Native to mountain ranges of western North America including the Olympic Mountains and Cascade Range of Washington and the Rocky Mountains of British Columbia and Alberta south to Colorado, it occurs on rocky outcrops and talus at subalpine and alpine elevations, i.e., from , and blooms from late May until early September.
A phylogenetic analysis in 2016 focusing on the new neovenatorid Gualicho found that Australovenator and other megaraptorids were either allosauroids or basal coelurosaurs as opposed to being tyrannosauroids. The ankles of Australovenator and Fukuiraptor are similar to the Australian talus bone known as NMVP 150070 that had previously been identified as belonging to Allosaurus sp., and this bone likely represents Australovenator or a close relative of it. Alternatively, this bone could belong to an abelisaur.
This is a local community, found mainly on Carboniferous limestone in England and Wales. It is an early coloniser of limestone screes and slopes, but is only able to persist if the talus if especially coarse or if there is limited grazing, both conditions which inhibit invasion by scrub and woodland species. This community was first described in Britain by Shimwell, who assigned it to the Gymnocarpietum robertianae (Kuhn 1937), previously described from Germany.
As the plug dome grew, massive sheets of broken lava crumbled as talus down its sides. Numerous Peléan pyroclastic flows accompanied these cooler avalanches, forming a fragmental cone and an overall slope of 12 to 15 degrees. Some of the glacial ice was melted by the eruptions, forming a small lake against Brohm Ridge's southern arm. The volcanic sandstones seen today atop Brohm Ridge were created by ash settling in this lake.
Potentilla cristae is a rare species of cinquefoil known by the common name crested cinquefoil. It is endemic to the Klamath Mountains of far northern California, where it is known from a few occurrences in the subalpine and alpine climates of the high mountain ridges. It grows in talus and moist rocky or gravelly serpentine soils. This is a low, matted plant producing a clump of hairy, glandular herbage up to about 20 centimeters tall.
Needle Rock Natural Area is located at the western edge of the West Elk Mountains of Colorado. The surrounding terrain is characterized by laccolithic mountains flanked by precipitous cliffs, extensive talus aprons, forested mesas, canyons, and spacious, well-watered intermontane basins. Needle Rock is an intrusive plug of monzonite porphyryNoe, D. C., and Alexander T. Klink. “OF-15-06 Geologic Map of the Crawford Quadrangle, Delta and Montrose Counties, Colorado.” Geologic, 1:24,000.
Long Mountain, like much of the Metacomet Ridge, is composed of basalt, also called traprock, a volcanic rock. The mountain formed near the end of the Triassic Period with the rifting apart of the North American continent from Africa and Eurasia. Lava welled up from the rift and solidified into sheets of strata hundreds of feet thick. Subsequent faulting and earthquake activity tilted the strata, creating the steep ridge and talus slopes of Long Mountain.
Many exposed granitic outcroppings, talus slopes, and boulder fields limit the amount of vegetation that grows here. The herbaceous plants need to flower and produce their seeds quickly during the short, frost-free period of summer. Flora includes cushion plants, grasses, willows, and sedges. The macrolichen flora in the Sierra Nevada alpine zone is not well developed as compared to neighboring alpine zones in the Rocky Mountains and mountains of the Pacific Northwest.
Streptanthus oliganthus is an uncommon species of flowering plant in the mustard family known by the common name Masonic Mountain jewelflower. It is native to western Nevada and eastern California, where it grows in the rocky hills east of the central Sierra Nevada. Its habitat includes forest, woodland, sagebrush, and mountain talus. It is a rhizomatous perennial herb producing a hairless, waxy, usually unbranched stem up to about 40 or 50 centimeters in maximum height.
It is no more than by in size, containing about 150 rectangular rooms and sixteen round kivas. The lower house is built from dark sandstone rocks collected from the talus slope to the west. Based on ceramic and architectural criteria, the great house was occupied between 1150 and 1250, and the compound between 1250 and 1300. Crumbled House's rock masonry style and keyhole shaped kivas suggest a relation to Mesa Verde masonry traditions.
Cortinarius talimultiformis is a species of fungus in the large mushroom genus Cortinarius (subgenus Phlegmacium). Found in North and Central Europe, as well as the East Black Sea Region's mountains (Turkey), it was described as new to science in 2014. It grows on the ground in hemiboreal to boreal, mesic coniferous forests containing spruce and fir. The specific epithet talimultiformis refers to the similar features it shares with species C. multiformis and C. talus.
Timpanogos Glacier is a rock-covered mass found on a long, north-facing slope, and usually has patches of snow the entire year. Although an above ground cirque glacier was present before the Dust Bowl Drought of the 1930s, no glacial ice is visible today. However, in 1994, a large crevasse opened up, revealing that there still is a glacier buried beneath the talus. Flowing water can occasionally be heard beneath the rocks.
This popular trail travels 28 miles (45 kilometers) through the park connecting Eagle River and Girdwood as it traverses the Chugach Mountains. It affords incredible views and wildlife viewing opportunities. Even along the first view miles, hikers often see hoary marmots (Marmota caligata) and Arctic ground squirrels (Urocitellus parryii), and occasionally mountain goats (Oreamnos americanus) or Dall sheep (Ovis dalli). Hoary marmots live in alpine meadows, often adjacent to boulders or talus.
This plant grows in high-elevation habitat in the mountains of southwestern Colorado. It can be found in a number of habitat types in montane, subalpine and alpine climates, including fellfields, talus, meadows, ridges, passes, rock outcrops, and disturbed areas. Species associated with the plant include Abies lasiocarpa, Agrostis thurberiana, Anemone multifida, Draba nivalis var. exigua, Eritrichium aretioides, Festuca thurberi, Oreoxis alpina, Pinus ponderosa, Polemonium viscosum, Rydbergia grandiflora, Trifolium dasyphyllum, Trifolium nanum, and Valeriana capitata.
Of particular note is the large, well-defined columnar basalt formation on the southwest side of Peter's Rock. Hot, dry upper slopes, cool, moist ravines, and mineral-rich ledges of basalt talus produce a combination of microclimate ecosystems on the mountain that support plant and animal species uncommon in greater Connecticut. Peter's Rock is also an important raptor migration path. (See Metacomet Ridge for more information on the geology and ecosystem of Peter's Rock).
The major habitats are coniferous forests, moors, rock and talus slopes, plus glacial moraines. The biological richness is further influenced by the different aspects of the faces, by the geology, and by the influence of man on the lower and middle slopes where forest clearance has created open grassland. The native forest habitats are essential for the survival of many species, with the key conifer species including larch, pine, stone pine and red pine.
Phacelia procera is a species of phacelia known by the common name tall phacelia. It is native to the northwestern United States as far south as the Sierra Nevada, where it grows in mountainous habitat, such as forests, meadows, and talus. It is a perennial herb producing an erect stem from a taproot, reaching a maximum height around two meters. It is hairy in texture, some of the hairs black and glandular.
Narrow ravines crowded with eastern hemlock block sunlight, creating damp, cooler growing conditions with associated cooler climate plant species. Talus slopes are especially rich in nutrients and support a number of calcium-loving plants uncommon in eastern Connecticut. Because the ridge generates such varied terrain, it is the home of several plant and animal species that are state-listed or globally rare. Sleeping Giant is also an important seasonal raptor migration path.
Campanula scabrella is a species of bellflower known by the common name rough bellflower. It is native to the mountains of the western United States, where it grows in talus and other rocky alpine habitat. This is a tough perennial herb growing in a clump from a woody rhizome and rarely exceeding 5 centimeters in height. The stiff leaves are linear to narrowly oval in shape and about 3 centimeters long, borne on winged petioles.
The site is a rock shelter well up on the western side of Bishop's Cap, an outlier of the Organ Mountains. It lies about 450 ft below the summit according to Brattstrom (1964); this would make its elevation about 1500 m. It was originally excavated by the Los Angeles County Museum (LACM) c. 1929 (LACMVP site number 1010). Specimens collected from talus, fill, or other areas are labeled 1010 Dump or 1010D.
Buttes form by weathering and erosion when hard caprock overlies a layer of less resistant rock that is eventually worn away. The harder rock on top of the butte resists erosion. The caprock provides protection for the less resistant rock below from wind abrasion which leaves it standing isolated. As the top is further eroded by abrasion and weathering, the excess material that falls off adds to the scree or talus slope around the base.
The walls were supported by square pillars, spaced roughly apart, linked by a row of arches for support. These were buried underneath a talus, and they supported the main wall, which had a number of arrow slits in it. A second arcade supported a crenellated parapet, where defenders could stand. A large ditch was dug in front of the walls, and in places this could be flooded with water to form a moat if needed.
Erigeron trifidus is a Canadian species of flowering plant in the daisy family known by the common name Alberta fleabane. It is native to the provinces of Alberta and British Columbia in western Canada.Biota of North America Program 2014 county distribution map Erigeron trifidus grows on talus and scree slopes in alpine zones at high elevations. It is a small perennial herb rarely more than 10 centimeters (4 inches) tall, producing a branching underground caudex.
Carex albonigra is a species of sedge known by the common name black and white sedge. It is native to western North America from Alaska and most of western Canada to California to New Mexico, where it grows in mainly dry, rocky high mountain habitat such as talus. This sedge forms a dense clump 10 to 30 centimeters in height with narrow gray-green leaves. The inflorescence is a headlike cluster of overlapping spikes.
This snail is limited to patches of algific talus slope habitat. It is a relict species from the last ice age. Much of its remaining habitat is located on the Driftless Area National Wildlife Refuge in Iowa. Known from fossil evidence about 400,000 years old, it is one of many glacial relict species that remain in the Driftless Area, a glacier-eroded plateau that now makes up parts of Iowa, Illinois, Minnesota, and Wisconsin.
When torn, it can result in a flatfoot deformity, and impair mobility. The dorsal or superomedial component of the ligament presents a fibrocartilaginous facet, lined by the synovial membrane, upon which a portion of the head of the talus rests. Its plantar surface, consisting of the intermedial and lateral ligaments, is supported by the tendon of the tibialis posterior; its medial border is blended with the forepart of the deltoid ligament of the ankle-joint.
The end moraines in the Constance depression were formed along the edge of the ice during the Constance stage (see above). In the area of the old town of Constance, we find a moraine surrounded by Lake deposits. The section of the moraine in Kreuzlingen, however, is surrounded predominantly by Pleistocene talus. Sections of the end moraine are found further north east and south east, in the area of the Bodanrück and Seerücken, respectively.
Around 43,000 acres of roadless country centered on 5,980' Mt. Bushnell, south of Thompson Falls, provides good habitat for deer, elk, and mountain lion. This area is/was densely forested with lodgepole pine generated from the Great Fire of 1910. Thirty miles of trails provide good hiking opportunities in this roadless area. Talus slopes, grassy parks in the highest reaches, and boggy creek bottoms characterize the landscape here in addition to the forests.
Silene suksdorfii is a species of flowering plant in the family Caryophyllaceae known by the common names Suksdorf's silene, Suksdorf's catchfly and Cascade alpine campion. It is native to the Pacific Northwest of the United States, where it occurs from Washington and Idaho to northern California. It is mainly an alpine species, growing in the talus of high mountain slopes. It can also be found below the tree line in forested subalpine habitat.
Smelowskia ovalis is a species of flowering plant in the mustard family known by the common name alpine false candytuft. It is native to western North America from British Columbia to northern California, occurring mostly in the Cascade Range. It is a plant of alpine climates, growing in high mountain habitat such as talus and fellfields. It is clumpy in shape, producing several hairy stems growing erect to a maximum height around 18 centimeters.
Oeneis melissa, the Melissa Arctic, is a species of butterfly in the family Nymphalidae. It has a Holarctic distribution, ranging from Siberia and the North American Arctic from Alaska east to Baffin Island and Labrador. Isolated populations are found from the Rocky Mountains south to northern New Mexico and in the White Mountains of New Hampshire. The habitat consists of tundra, talus slopes, rocky summits and saddles and frost-heaved clear cuts.
The , which is launched using a Talus MB-4H launch tractor aboard a Do-Do carriage, can operate in Force 7 winds (Force 6 at night), has a top speed of and a range of 2½ hours at maximum speed. Adjacent lifeboats are at Minehead Lifeboat Station to the west, and Weston- super-Mare Lifeboat Station to the north. If a larger all weather lifeboat is needed in the area it can be summoned from .
The Multnomah Falls Lodge and the surrounding footpaths at the falls were added to the National Register of Historic Places in 1981. Contemporarily, the state of Oregon maintains a switchback trail that ascends to a talus slope above the falls, and descends to an observation deck that overlooks the falls' edge. The falls attract over two million visitors each year, making it the most-visited natural recreation site in the U.S. Pacific Northwest.
A species endemic to California, it inhabits shaded, moss-covered talus slopes in old-growth mixed evergreen and montane fir forests of the Klamath Mountain Range. It was discovered in 2001, and is currently known from a few locations near the confluence of the Klamath and Scott Rivers, hence its common name Scott Bar salamander. Its range is only 20 km (13 mi) at its greatest dimension. Known elevations extend from above sea level.
The lake is located in a narrow valley, with Chair Peak to the east and Kaleetan Peak to the west, and is usually accessible by late June. It is known for its clear water and beautiful blue-green color. A short scramble up the talus slope on the north end of the lake leads to Melakwa Pass, where views of Gem Lake, Glacier Peak, and the North Cascades are visible on clear days.
Bayshore Blufflands State Natural Area is a Wisconsin Department of Natural Resources-designated State Natural Area of significant note for its grand scenery, unusual geology, rare plant and animal species. Containing more than of the Niagara Escarpment, the Bayshore Blufflands is an ecologically complex site with a diversity of plant communities both above and below the escarpment and a series of seeps and springs at the base of the bluff's talus slopes.
Liberal Arts, Nagasaki Univ. (Nat. Sci.), 14, 43-57 (in Japanese with English abstract). These strata are intruded by sheets of Mio-Pliocene porphyritic hornblende diorite, and are fringed by recent coral outcrops and surface talus deposits. Kuba and Taisho are volcanic in origin, with Kuba comprising "pyroxene andesite, lava, volcanic bombs, pumice, limestone, and other rocky material" and Taisho is thought to be consist of "andesite, tuff breccia, and tuffaceous sandstone".
Hot, dry upper slopes, cool, moist ravines, and mineral-rich ledges of basalt talus produce a combination of microclimate ecosystems on the mountain that support plant and animal species uncommon in greater Connecticut. Farmington Mountain is also an important raptor migration path. (See Metacomet Ridge for more information on the geology and ecosystem of Farmington Mountain).Raymo, Chet and Raymo, Maureen E. Written in Stone: A Geologic History of the Northeastern United States.
Hot, dry upper slopes, cool, moist ravines, and mineral-rich ledges of basalt talus produce a combination of microclimate ecosystems on the mountain that support plant and animal species uncommon in greater Connecticut. Rattlesnake Mountain is also an important raptor migration path. (See Metacomet Ridge for more information on the geology and ecosystem of Rattlesnake Mountain).Raymo, Chet and Maureen E. Written in Stone: A Geologic History of the Northeastern United States.
Narrow ravines support eastern hemlock that block sunlight, creating damp, cooler growing conditions with associated cooler climate plant species. These hemlocks have suffered from infestation by the hemlock woolly adelgid. Talus slopes are especially rich in nutrients and support a number of calcium-loving plants uncommon in eastern Connecticut. Because the ridge generates such varied terrain, it is the home of several plant and animal species that are state- listed or globally rare.
Bushy-tailed woodrats occupy a wide range of habitats, from boreal forests to deserts. Their preferred habitat is in and around rocky places, so they are often found along cliffs, canyons, talus slopes, and open rocky fields. They readily adapt to abandoned buildings and mines. They can be found from sea level up to 14,000 feet (4300 m), but they become increasingly restricted to higher elevations toward the southern end of their range.
The seamount is about high and reaches a depth of below sea level. On the seafloor, it occupies a surface of , making it much larger than other Pacific seamounts, and is surrounded by a shallow moat on the northern and southeastern side. The outer slopes of the seamount have a step-like appearance and feature radial grabens formed presumably by subsidence. At their foot, sediments descending from the seamount have formed talus deposits.
Mountain Lake Virginia lakeviewMountain Lake has been referred to as "The Silver Gem of the Alleghenies". Many modes of formation have been suggested for the lake. Among the possibilities are the blocking of a stream by talus or slide-rock, a glacial cirque, a depression formed volcanic activity or the result of a meteoric impact. Recent studies have shown that a stream flowing from the Mountain Lake basin was blocked creating a lake.
The lifeboat station is built on the promenade in Rhyl. The building contains the All-Weather Lifeboat, Inshore Lifeboat, Talus tractor, and Softrac used for Search and Rescue operations off the coast in Rhyl. The station also has a short concrete slipway that leads down to the beach. Each boat is kept on a carriage attached to a tractor which propels it down to the water and brings it back after use.
In 1994 while searching through museum boxes labelled 'Cercopithecoids' containing fossil fragments, Ronald J. Clarke identified several that were unmistakably hominin. He spotted four left foot bones (the talus, navicular, medial cuneiform and first metatarsal) that were most likely from the same individual. These fragments came from the Silberberg Grotto, a large cavern within the Sterkfontein cave system. They were described as belonging to the genus Australopithecus, and catalogued as Stw 573.
The sandstone forming the bluffs has a tendency to fracture into blocks, creating unusual boulder formations. The concave shape of the top of Lookout Mountain also drains rainwater through fissures into the underlying limestone, forming miles of caves in the area. The canyon is more than deep, ranging in elevation from to over ; the park's peak elevation is . The bottom of Cloudland canyon contains a slope of rock talus, which are sandstone and shale fragments.
Botanical Gazette 62(2): 145–146 description and commentary in English Amsinckia carinata was believed to be extinct until 1984, when it was rediscovered. It occurs in the Malheur River Valley in eastern Oregon, where it grows on slopes of talus and gravel. It grows alongside the more common Amsinckia tessellata, which replaces it at lower elevations and in less pristine habitat. There are six populations, in less than 12 square miles (30.7 km2) of territory.
Sedum stenopetalum is a species of flowering plant in the family Crassulaceae known by the common name wormleaf stonecrop, or golden constellation. It is native to western North America from British Columbia and Alberta to northern California to Wyoming. It can be found in many types of rocky habitat, such as cliffs, talus, and steep ridges. It is a succulent plant producing mats or clumps of lance-shaped, linear, or three-lobed leaves each under 2 centimeters long.
It typically rages in the spring and early summer while shrinking to a trickle by late summer to mid-autumn.Yosemite News - Pywiack Cascade The water of the Pywiack Cascade slides down a steep angle of solid granite, for a total of about . A small waterfall lies directly below the main drop. Below that, the creek continues over jumbled talus for less than a quarter of a mile (0.4 km) before it plunges over another large waterfall.
The calcaneum, which contacts the fibula, is almost unanimously considered to be identical to the fibulare. The other proximal tarsal, the astragalus (or talus), is likely a mass formed by the fusion of the intermedium, tibiale, and the fourth (and possible also the third) centrale. Some lepospondyls, such as the reptile-like microsaur Tuditanus, also may have evolved these modifications. The ankle of Westlothiana, as well as that of most other "reptiliomorphs", is intermediate between these two conditions.
But if they were not back in their mountain fastness by sunrise, they would be denied access and would become mere mortals. On one occasion, what with dancing and pleasure, the faterelle had not noticed the approach of dawn. Scrambling up the Vettore, their goatlike feet crushed the rock to fragments. They reached the safety of their grotto just before dawn, but the long slope of talus is still pointed out as the Path of the Fata.
42, No. 3 (August 2010) , pp. 250-259 The island is steeper to the northern side than the southern side, and slightly north of the center of the island is a steep-walled caldera surrounding a lake. The crater is about 4,000 feet in diameter, with its lake's surface lying only about 60 m above sea level. In all areas surrounding the crater, the island is characterized by steep sea-cliffs, talus slopes, and small, boulder-filled beaches.
A trimalleolar fracture is a fracture of the ankle that involves the lateral malleolus, the medial malleolus, and the distal posterior aspect of the tibia, which can be termed the posterior malleolus. The trauma is sometimes accompanied by ligament damage and dislocation. The three aforementioned parts of bone articulate with the talus bone of the foot. Strictly speaking, there are only two malleoli (medial and lateral), but the term trimalleolar is used nevertheless and as such is a misnomer.
Talus, p. 37. However, with the rising threat from Nazi Germany, and the ineffectiveness of the League of Nations, this policy eventually lost credibility. By 1937, Labour had jettisoned its pacifist position and came to support rearmament and oppose Neville Chamberlain's policy of appeasement. In 1938, Attlee opposed the Munich Agreement, in which Chamberlain negotiated with Hitler to give Germany the German-speaking parts of Czechoslovakia, the Sudetenland: > We all feel relief that war has not come this time.
1\. The calcaneal internal rotation (adduction) and plantar flexion is the key deformity. The foot is adducted and plantar-flexed at the subtalar joint, and the goal is to abduct the foot and dorsiflex it. In order to achieve correction of the clubfoot, the calcaneus should be allowed to rotate freely under the talus bone, which also is free to rotate in the ankle mortise. The correction takes place through the normal arc of the subtalar joint.
The cast must incorporate the toes right up to the tips but not squeeze the toes or obliterate the transverse arch. The cast is molded to contour around the heel while abducting the forefoot against counter pressure on the lateral aspect of the head of the talus. The knee is flexed to 90° for the long leg component of the cast. The parents can soak these casts for 30–45 minutes prior to removal with a plaster knife.
Most nonserpentine soils have a ratio far greater than 1 (more calcium and much less magnesium). The extreme chemical characteristics of serpentine soils give rise to uniquely adapted and rare serpentine endemic plant species such as C. benitensis. Like Camissonia benitensis, the previously ranked strict serpentine endemic Layia discoidea also has several populations that occur on greywacke and chert outcrops and talus around the New Idria Serpentine Mass. Additionally, the strict serpentine endemic Quercus durata var.
Saxifragopsis is a monotypic genus of flowering plants in the saxifrage family containing the single species Saxifragopsis fragarioides, which is known by the common name strawberry saxifrage. This plant is sometimes included in genus Saxifraga.Flora of North America It is native to the northwestern United States, where it is mostly limited to the Klamath Mountains of southern Oregon and northern California, with some disjunct occurrences known from Washington. It grows in rocky mountain habitat, such as talus.
Eastern red cedar, a dry-loving species, clings to the barren edges of cliffs. Backslope plant communities tend to be more similar to the adjacent Berkshire plateau containing species common to the northern hardwood and oak-hickory forest forest types. Eastern hemlock crowds narrow ravines, blocking sunlight and creating damp, cooler growing conditions with associated cooler climate plant species. Talus slopes are especially rich in nutrients and support a number of calcium-loving plants uncommon in Massachusetts.
19th-century "rusticators" traveled by railroad and after the turn of the century float plane fly-in service became popular for anglers. Guests can spare themselves the arduous ten mile hike in from U.S. Route 201 via the access road built by the owner of Bulldog Camps in 2005. Various species dwell among the surrounding cliffs and talus slopes, including peregrine falcons, bald eagles and common loons. The region also has a large moose and bear population.
Cymopterus cinerarius is a species of flowering plant in the carrot family known by the common name gray springparsley. This small plant is native to the US states of California and Nevada, where it grows on the rocky talus of the Sierra Nevada. This plant has a short stem and lies against the ground or draped over rocky debris. Its distinctive leaves are only a few centimeters long and dissected into segments of a few millimeters in length.
Lomatium shevockii is a rare species of flowering plant in the carrot family known by the common name Owens Peak desertparsley, or Owens Peak lomatium. It is endemic to Kern County, California, where it is known from only two occurrences at Owens Peak, one of the highest points of the Sierra Nevada. It is a plant of the talus and wooded slopes of the high mountains. This species was discovered in 1984 and first described to science in 1988.
The Venus Throw was the highest roll in the Ancient Roman gambling game of tali (knucklebones). The game was played with four 4-sided rectangular dice numbered I, III, IV and VI, usually made from sheep's or goat's knucklebones. In a Venus Throw, each talus landed on a different side, yielding as a score of 14. A gambler would either throw the tali from his or her hand, or from a small box, (called a fritillus).
Erigeron tweedyi is a North American species of flowering plant in the daisy family known by the common name Tweedy's fleabane. It is native to the northern Rocky Mountains in the US states of Montana, Idaho, and Wyoming.Biota of North America Program 2014 county distribution map Erigeron tweedyi grows on talus and rocky slopes at high elevations. It is a perennial herb up to 20 centimeters (8 inches) tall, producing a taproot and a branching underground caudex.
Traprock was harvested from talus slopes of the Metacomet Ridge to build house foundations; copper ore was discovered at the base of Peak Mountain in northern Connecticut and was mined by prisoners incarcerated at Old Newgate Prison located there.Connecticut Commission on Culture and Tourism. Retrieved December 22, 2007. With the advent of industrialization in the 19th century, riverways beneath the Metacomet Ridge were dammed to provide power as the labor force expanded in nearby cities and towns.
Metcalfe, R. P., Geol. Soc. London, 1993, 74, 495–509. The glacier is composed of a variety of depositional features such as talus cones, snow-avalanche fans, snow-bridges, and dead ice mounds, and erosional features like pyramidal and conical peaks, serrated ridge crests, glacial troughs, smooth rock walls, crags and tails, waterfalls, rock basins, gullies and glacial lakes. All along the Gangotri glacier, several longitudinal and transverse crevasses are formed along which ice blocks have broken down.
Differential erosion and weathering of the exposed rock created the Pinnacles that are seen today. The rock formations are andesite and rhyolite, forming a dropped fault block embedded in the Gabilan Range. Large-scale earth movement also created the talus caves that can be found in the park. Deep, narrow gorges and shear fractures were transformed into caves by large chunks of rock falling from above and wedging into the cracks, leaving an open area below.
The salamander inhabits a variety of moist microhabitats and is found along shady, cool streams or seepages in wet, rocky areas and in forests, talus slopes, and moss-covered outcrops, often under rocks, logs, moss, and leaf-litter. This salamander generally prefers moister microhabitats than sympatric species such as Ensatina or the Western Red-backed Salamander. Dunn's salamander is not considered threatened because of its relatively wide range and not being sensitive to habitat modification (logging).
The solidifying, spreading lava could then generate rockfalls and form a voluminous talus apron into the Squamish valley. As the lava dome spreads, it would periodically undergo gravitational collapse to generate dense pyroclastic flows into the Squamish and Cheakamus valleys. Ash elutriated from the pyroclastic flows would form plumes up to high, again dropping ash onto Pemberton and Whistler and causing disruptions to local air traffic. Infrequently, the lava dome might produce small explosions, ash plumes and pyroclastic flows.
The formation contains a basal limestone conglomerate overlain by evenly bedded red or gray limestones (more accurately, limy mudstones) and calcareous shales. It is a lenticular, channel-fill deposit which is some wide and thick at maximum. Most collections are from the talus slope. Stable oxygen and isotope data (Poulson in Fiorillo, 2000) indicate that the Beartooth Butte Formation was deposited in an estuarine environment, with the Cottonwood Canyon section being slightly less saline than the type section.
The ramparts follow the contours of the rocky plateau where the Château de Vitré and the urban nucleus developing around the Church of Notre-Dame are built. The construction of the ramparts was made according to the defensive strengths and constraints of the relief. The town is located on a plateau with very deep valleys. To the north flows the river Vilaine where there was a pond, swamps and a very high talus of 30 meters.
Blocky andesite lava then flowed from St. Helens' summit crater down the volcano's southeast flank. Later, pyroclastic flows raced down over the andesite lava and into the Kalama River valley. It ended with the emplacement of a dacite dome several hundred feet (~200 m) high at the volcano's summit, which filled and overtopped an explosion crater already at the summit. Large parts of the dome's sides broke away and mantled parts of the volcano's cone with talus.
Ice Mountain is a mountain ridge and algific talus slope that is part of a preserve near the community of North River Mills in Hampshire County, West Virginia, United States. It was designated a National Natural Landmark in 2012. Ice Mountain is protected by The Nature Conservancy and open for visits by small groups of hikers. It is nicknamed "Nature's Ice Box" and "Nature's Refrigerator" owing to its ice vents that release cool air all year long.
Cool air is expelled from the ice in the warmer months. Vent air temperatures vary throughout the year, but the mean annual temperature can be as low as 2 °C (35 °F). Within the area of ice vents there are approximately 60 different pockets and the cold air escapes through more than 150 small openings in the talus. The cool air affects surrounding air and soil around creating an area of boreal species and plant growth.
Sârbu, p. 19 Gomoiu published steadily, and also lectured at the Medical Students' Society and the Surgical Society. Topics included meningoencephalitis, cerebral atrophy, facial nerve paralysis, fibrous tissue neoplasm, lipoma, the anatomy of the endothelium, corneal transplantation, skin grafting, dental implants, hysterectomy, various types of cysts and "rare tumors", and talus bone expulsion. These works were taken up in Eraclie Sterian's magazine, Spitalul, of which Gomoiu was co-editor,Riga & Călin, p. 378 or published as brochures.
Mordru and Glorith travel to Legion Headquarters on the planet Talus, and reach the team's Time Beacon. They use it to summon the Infinite Man, who is the living embodiment of the space-time continuum. Mordru and Glorith immediately attack, allowing them to absorb all of the Infinite Man's energies and dissolve him into nothingness. Meanwhile, on Baaldur, Rokk cannot escape the castle, but is able to flee into the Infinite Library, the archive of all chronal knowledge.
The Cardenas Basalt, also known as either the Cardenas Lava or Cardenas Lavas, is a rock formation that outcrops over an area of about 310 km2 (120 mi2) in the eastern Grand Canyon, Coconino County, Arizona. The lower part of the Cardenas Basalt forms granular talus slopes. Its upper part forms nearly continuous low cliffs that are parallel to the general course of the Colorado River. The most complete, readily accessible, and easily studied exposure of the Cardenas Basalt lies in Basalt Canyon.
This pass, probably one of the many constructed by the CPR in an effort to attract tourists, led along what is now called Fossil Ridge. Walcott recognised the talus material which lay across the trail as the Stephen Formation, and noticed interesting fossils. This find is often considered to be the first discovery of the Burgess Shale 'proper'. He spent several more days collecting on Fossil Ridge before returning to Mount Stephen to bolster his collections from the Trilobite Beds.
Ann G. Harris, et al., The Geology of National Parks,(Dubuque, Iowa: Kendall-Hunt, 2004) Olivine basalts were extruded from a N. 70° E. trending rift zone, oriented along the current Afono and Masefay bays of Tutuila, in the Pliocene or earliest Pleistocene. The Masefau dike complex and talus breccias are remnants of this rifting. Development of the Taputapu, Pago, Alofau, and Olomoana shield domes followed long parallel fissures followed, but when the Pago and Alofau summits collapsed, calderas were formed.
Talus Taylor (1933 – 19 February 2015) was a writer of children's literature, best known for being the co-creator with his wife Annette Tison of the Barbapapa series. Taylor was born in 1933 in San Francisco. He was a biology teacher and the companion of Annette Tison, the co-creator of the famous Barbapapa series; initially published as an album in 1970, before becoming a cartoon and a magazine in 1976. Taylor died in 2015 in Paris at the age of 82.
In humans, the calcaneus is the largest of the tarsal bones and the largest bone of the foot. The talus bone, calcaneus, and navicular bone are considered the proximal row of tarsal bones. In the calcaneus, several important structures can be distinguished:Platzer (2004), p 216 The half of the bone closest to the heel is the calcaneal tuberosity. On its lower edge on either side are its lateral and medial processes (serving as the origins of the abductor hallucis and abductor digiti minimi).
This causes trees to be stunted in the shallow soils. Despite this, forest cover is extensive, with Douglas-fir, lodgepole pine, and spruce common, while the highest slopes are home to vast stands of pure limber pine intermixed with small parks, a habitat type found more commonly far to the south. Other features of the Rubies include free-standing rock walls, caves, cliffs, and talus. Wildlife includes a few elk, a large mule deer herd and excellent blue grouse habitat.
The approach trail to Cannon cliff can be found by walking along the bike path on the western (southbound) side of I-93. Climbers park and sign in at a trailhead lot just south of Profile Lake. After about of narrow, climber- maintained trails through the woods, climbers must cross a long section of talus. Steep unofficial descent trails back to the trailhead can be found on both the north and south ends of the cliff, above Whitney-Gilman and Lakeside, respectively.
The geographical area has a rough terrain, making it difficult to access other than on foot. Remains of Maltese rubble walls and water canals, built over a hundred years ago, are taken as primarily evidence that until recent human activity took place for agricultural purposes. Some stretches of land were used as a quarry, but other than that the area was not altered by man-made intervention. Huge rocks, some the size of small houses, pile over each other forming deep talus 'caves'.
Ice Cave at Bixby State Preserve Bixby State Preserve is a nature reserve located in southwestern Clayton County, Iowa, in the midwestern United States. It is located north of Edgewood. It is operated by the Iowa Department of Natural Resources as one of the Iowa state preserves. Bixby State Preserve is one of the few places in the world to contain algific talus slopes and consequently has an ecosystem encountered in only a few other sites, all in the Driftless Area.
We say we want to see put on the statute book something which will make our people citizens of the world before they are citizens of this country".Talus, Your Alternative Government (London: Eyre and Spottiswoode, 1945), p. 17. During a debate on defence in Commons a year later, Attlee said "We are told (in the White Paper) that there is danger against which we have to guard ourselves. We do not think you can do it by national defence.
6, 2008 and is adjacent to the east side of Lassen Volcanic National Park. Although the park (which includes its own Lassen Volcanic Wilderness area) is surrounded by Lassen National Forest, it is managed separately by the National Park Service, whereas the U.S. Forest Service manages the wilderness. Elevations range from to . The terrain is a volcanic plateau with 75% covered by water and conifer forests and the remainder being barren rock such as cliff faces, talus slopes and cinder cones.
Crumbled House is a fortification type structure that utilizes the natural defenses around a tabletop mesa. The site has two room blocks and three major segments that begin at the top of the mesa, and descend the talus west slope and the plateau east slope via the use of stairways. The mesa top segment formed a triangular upper block. There were massive circular towers at each tip of the triangular structure; high stone walls followed the edges of the mesa.
Paul Accola (born 20 February 1967 in Davos) is a Swiss former Alpine skier. He came in first in the overall World Cup in 1992, and won a total of four medals at the Winter Olympics and World Championships in the combined event. By the end of his career, he won seven world cup victories and was on the podium 26 times, the last time being in 2000. In 2002 Accola suffered a serious ankle injury, breaking both of his talus bones.
In a small slope area there are 60 small holes and openings at the base of a rock talus whose vents blow air year round. As a result, high elevation boreal plants group around the cold air vents, where ice can be seen well into May. The effects of gradually warming temperatures are already noticeable on Ice Mountain, and ice around the vents is disappearing earlier in the year. This could adversely impact the boreal plants found in this system.
South of the Trout Creek Mountains is the Kings River Valley, which separates the Bilk Creek Mountains on the west from the Montana Mountains on the east. The terrain in the Trout Creek Mountains varies from broad, flat basins and rolling ridges to high rock escarpments cut by deep canyons. The canyons have steep walls with loose talus slopes at the bottoms. There are meadows around springs in the mountains, although most streams in the range do not flow year-round.
Penstemon newberryi is a species of penstemon known by the common name mountain pride or Newberry's penstemon. It is native to the mountains of northern California, Oregon, and Nevada, where it grows in rocky habitat, often at high elevation, such as talus. It is a bushy, mat-forming subshrub growing up to 30 centimeters tall. The leaves are mostly basal on the plant, oblong or oval and toothed, measuring 1 to 4 centimeters in length, with a few smaller pairs along the stem.
This is a relatively recent impact compared to most of the craters on the far side, and the rim is still well- formed with little erosion. It is old enough, however, that its albedo matches its surroundings and it lacks a ray system. The inner wall has slumped in places and formed piles of talus along the south. The interior floor has two lines of low ridges that begin in the southeast and curve up to the northwestern inner wall.
The game events were originally set following the destruction of the Death Star in Episode IV: A New Hope, but before the beginning of The Empire Strikes Back. Even though the battle of Hoth has been included this does not change the timeline. Some parts of the game include past "missions" to before the destruction of the Death Star. The game launched with 10 planets: Tatooine, Naboo, Corellia, Talus, Rori, Dantooine, Lok, Yavin 4, the forest moon of Endor, and Dathomir.
Lomatium martindalei is a species of flowering plant in the carrot family known by the common names Cascade desertparsley and coast range lomatium. It is native to the west coast of North America, from Vancouver Island south to the Klamath Mountains of far northern California. It can be found in a number of coastal and inland habitats, from coastal plains to high mountain talus and meadows. This is a perennial herb growing 15 to 40 centimeters tall from a carrot-like taproot.
The columnar basalt was likely formed by cooled eruptions of Mount Rainier, which is a stratovolcano. Near the base, it crashes onto a rock ledge and fans out towards the left bank, before dropping again vertically onto a pile of talus and cascading downwards. It is located in a steep canyon on the southwest face of Mount Rainier. Pearl Creek drains to another glacial stream, Pyramid Creek, which parallels then flows into Kautz Creek and finally into the Nisqually River.
Basalt frequently breaks into octagonal and pentagonal columns, creating a unique "postpile" appearance. Extensive slopes made of fractured basalt talus are visible at the base of many of the cliffs along the Metacomet Ridge. The basalt floods of lava that now form much of the Metacomet Ridge took place over a span of 20 million years. Erosion and deposition occurring between the eruptions deposited layers of sediment between the lava flows which eventually lithified into sedimentary rock layers within the basalt.
Eliot Glacier is a glacier on the northeastern slopes of Mount Hood in the U.S. state of Oregon. Researchers have reported that Eliot Glacier covered an area of in 2004 but had retreated since 1901, though that decline was less than all but one other glacier on Mount Hood. The glacier's situation on a northeast slope, its higher altitude accumulation zone close to the summit of Mount Hood and its high level of talus debris may explain its slower retreat.
Snowshoe Canyon is located in Grand Teton National Park, in the U. S. state of Wyoming. The canyon was formed by glaciers which retreated at the end of the last glacial maximum approximately 15,000 years ago, leaving behind a U-shaped valley. Snowshoe Canyon splits into an upper and lower canyon. The source of the upper canyon is near Talus Lake () while the south canyon is situated between Rolling Thunder Mountain to the north and Raynolds, Traverse and Bivouac Peaks to the south ().
Ahern Glacier is in Glacier National Park in the U.S. state of Montana. The glacier was named after George Patrick Ahern. Ahern Glacier is situated on a ridge between Ipasha Peak to the north and Ahern Peak to the south at an elevation between and above sea level, immediately east of the Continental Divide. Meltwater from the glacier feeds Ahern Glacier Falls, a waterfall which descends an estimated in one sheer drop to a talus slope below en route to Helen Lake.
Talus slope on Bare Mountain Bare Mountain, like much of the Metacomet Ridge, is composed of basalt, also called traprock, a volcanic rock. The lava from which the mountain is formed was erupted in the early Jurassic Period when North America was rifting apart from Africa and Eurasia. The lava welled up from the rift and solidified into sheets of strata hundreds of feet thick. Subsequent faulting and earthquake activity tilted the strata, creating the dramatic cliffs and ridges of Bare Mountain.
Novisuccinea chittenangoensis were found on vegetation up to 92 cm above the ground and at 1/3 the maximum sunlight intensities of the sympatric Succinea sp. B. Vegetation is quite sparse on the west side of the Falls, and the only snails that have been observed there are Succinea sp. B. In drier talus adjacent to the mossy areas are various plant species, such as eastern skunk cabbage Symplocarpus foetidus and Angelica atropurpurea, upon which Succinea sp. B has also been found.
The anterior ligament of the lateral malleolus (anterior tibiofibular ligament or anterior inferior ligament) is a flat, trapezoidal band of fibers, broader below than above, which extends obliquely downward and lateralward between the adjacent margins of the tibia and fibula, on the front aspect of the syndesmosis. It is in relation, in front, with the fibularis tertius, the aponeurosis of the leg, and the integument; behind, with the interosseous ligament; and lies in contact with the cartilage covering the talus.
Backslope plant communities tend to be similar to the adjacent upland plateaus and nearby Berkshires, containing species common to the northern hardwood and oak-hickory forest ecosystem types. Eastern hemlock crowds narrow ravines, blocking sunlight and creating damp, cooler growing conditions with associated cooler climate plant species. Talus slopes are especially rich in nutrients and support a number of calcium-loving plants uncommon in the region. Miles of cliffs make ideal raptor habitat, and the range is an important seasonal raptor migration corridor.
Later in the summer there is more travel on talus (scree) and more danger from rockfall. An alternative in snow-free conditions is to hike up to the saddle between the peak and Hagerman Peak. From that point there are climbers' trails which proceed on the opposite (west) side of the ridge to the summit. A different and much less used route climbs the west side of Snowmass Mountain from Geneva Lake, which is accessed from the North Fork of the Crystal River.
Juncus parryi is a species of rush known by the common name Parry's rush. It is native to western North America from British Columbia and Alberta to California to Colorado, where it grows in moist and dry spots in mountain habitat, including rocky talus and other areas in the subalpine and alpine climate. This is a rhizomatous perennial herb producing a dense clump of stems up to about 30 centimeters tall. There are short, thready leaves around the stem bases.
He was later found to be an asthmatic patient. Another, local Papua New Guinean, from Tari in the Southern Highlands Province, died in 2007 a few meters south of the Christopher Donnan plaque. Local sources revealed that the deceased was unaware of the warning and was wearing only his sporting suit, T-shirt and Dunlop shoes. He was covered by debris and fallen rock fragments, forming a talus at the base of the southern tip of the Christopher Donnan section.
Claytonia umbellata is a species of wildflower in the purslane family known by the common name Great Basin springbeauty. It is native to the Great Basin of the United States, where it grows mainly in subalpine coniferous forests, often on north-facing exposed slopes in the talus. It is a perennial herb growing from a tuberous root up to 5 centimeters wide and a thin taproot. Most of the stem develops underground, as do the petioles of the most basal leaves.
The tractor when tethered to a lifeboat carriage has the capability of towing and pulling such carriages at a top speed of up to . In addition to its original design intent, the tractor has the advantages of having a varied performance range and can be used for hauling, winching and heavy recovery operations either on dry land or in flood conditions. There are 30 Talus MB-H machines in the RNLI fleet in the United Kingdom and Republic of Ireland.
Lewisia longipetala is a rare species of flowering plant in the family Montiaceae known by the common names long-petalled lewisia and Truckee lewisia. It is endemic to the Sierra Nevada of California, where it is known from less than 20 locations in areas not far from Lake Tahoe. It grows in subalpine and alpine climates in moist areas in rocky habitat, such as talus that retains patches of snow year-round. Most specimens grow on north-facing slopes with little surrounding vegetation.
The Pleistocene glaciation has excavated cirques and U shaped valleys in the western and northern side of Azufre and Gordo above . It has left talus and moraines on the upper flanks of the volcano as well as exposing hydrothermally altered areas, chiefly on the western side of the range. Among these are separate moraines on the southwestern slope of Azufre and Quevar and till. Surface exposure dating indicates that these moraines developed during lake highstands in the Salar de Uyuni.
With the series' renewal, two new main cast members were announced. Mark Hamill was cast as Talus, an old Templar veteran of the Crusades who lived through a decade of captivity in the Middle East, and now tasked with training younger knights. One of his ex-students is Landry, once a master himself but forced to start over after breaking his vows in the first season. Tom Forbes was cast as Prince Louis, the violent and unpredictable son of King Philip.
This summit dome is capped off by a summit crater at an altitude of , and four additional craters occur northeast of the summit at altitudes of . Northwest of the summit, a dacitic lava dome is the source of a high talus slope. The summit area is surrounded by an inwards-dropping scarp that opens to the northwest and whose southern margin is buried by lava flows. Pyroclastic flows crop out beneath lava flows in the northwestern segment of the volcano, within the scarp.
The Cumberland Narrows (or simply "The Narrows") is a water gap in western Maryland in the United States, just west of Cumberland. Wills Creek cuts through the central ridge of the Wills Mountain Anticline at a low elevation here between Wills Mountain to the north and Haystack Mountain to the south. Cliffs and talus of the two mountains' Tuscarora quartzite caprock are prominent within the Narrows. A prominent rocky outcropping at the south end of Wills Mountain in the Cumberland Narrows is known as Lover's Leap.
The lower part of this formation consists of complexly interbedded, thin, and discontinuous beds of basalt, hyaloclastite, and sandstone that form low, talus-covered slopes. The upper unit of the Cardenas Basalt consists of cliff- forming basaltic and andesitic lava flows that are interbedded with beds of breccia, sandstone, and lapillite. No fossils have been found in the Cardenas Basalt. The Cardenas Basalt was formed by the subaerial eruption of basaltic and andesitic magma in wet coastal environments such as river deltas or tidal flats.
The Gaoligong Pika can be found at an elevation of about in the rocky and talus habitat of Mount Gaoligong. Primarily, due to this type of habitat of the Gaoligong pikas, there is a limited amount of information about their group. Within the family Ochotonidae however, there is a total of 24 species of pikas found also in China, generally in steppe and alpine environments. However, Ochotonids were once also found in a range of other locations, such as Asia, Europe, North America and northern Africa.
Carpal bones were missing, as in other titanosaurs. Finger bones and claws were also completely absentin most other titanosaurs, these bones were still present though extremely reduced in size. In the foot, the talus bone was strongly reduced as in other titanosaurs, while the calcaneus was probably completely absent in Opisthocoelicaudia. In contrast to the manus, the foot showed well developed digits and claws. The phalangeal formula, which states the number of phalanges (digit bones) beginning with the innermost digit, is 2-2-2-1-0.
Koonalda Cave is a cave in the Australian state of South Australia, on the Nullarbor Plain in the locality of Nullarbor. It is notable as an archeological site."Koonalda Cave", Encyclopædia Britannica"Koonalda Cave" Australia Thru Time. Retrieved 2014-3-17. I.D. Lewis described the cave in 1976 as: > Large doline 60m in diam. and 25m deep; talus slope to two main large > passages connected by a high window; total length of cave 1200m; three lakes > at -80m; narrow airspace beyond third lake leads to 45m diam.
The Outer Defences comprise artillery fortifications, and were built in their present form in the 18th century, although some parts, including the French Spur at the east end, date back to the regency of Mary of Guise in the 1550s.Fawcett, p.66 The French Spur was originally an ear-shaped bastion known as an orillon, and contained gun emplacements which protected the main spur. This projecting spur was fronted by an earth ramp called a talus, and was entered via a drawbridge over a ditch.
The west edge of the Mt. Tom ridge is a sharp escarpment of cliffs and talus slopes. This feature gives rise to the common name traprock, which is derived from the Swedish word for step. The Metacomet-Monadnock Trail follows the top edge of this escarpment, and has views toward the west. Away from the edge of the escarpment, the topography near the top of the main ridge is a landscape of small outcrops and ledges alternating with hollows, which sometimes hide vernal pools.
Micranthes tolmiei is a species of flowering plant known by the common name Tolmie's saxifrage, or Tolmie's alpine saxifrage. It is native to western North America from Alaska to Montana to California, where it grows in rocky mountain habitat types, especially in alpine climates, such as talus and fellfields. It is a small perennial herb growing in mats of creeping stems lined with thick, fleshy leaves each up to 1.5 centimeters long. The inflorescence arises on a stout, erect peduncle with a few stubby bracts midway up.
There is no concrete measurement of the exact of the landmass, however, the Alaska Department of Fish and Game has a management area which encompasses the landmass as well as lands that are not usually considered part of a peninsula. The land which better fits the definition is roughly 10 miles long, running from near Thumb Cove and Talus Bay to Cape Resurrection at its southern extremity. Slightly less than half of the land on the Resurrection Peninsula is part of the Chugach National Forest's southern terminus.
A common cause of anterior impingement is a bone spur on anklebone (talus) or the shinbone (tibia). Repeated kicking actions can cause the anklebone to hit the bottom of the shinbone, which can lead to a lump of bone (or bone spur) developing. This bone spur may then begin to impact on the soft tissue at the front of the ankle, causing inflammation and swelling. The condition is most common in athletes who repeatedly bend the ankle upward (dorsiflexion), such as footballers, hence the name.
The lavas show no evidence of ponding in crustal magma chambers, suggesting that the large volatile content of the magma was sufficient to quickly transport it through the crust. Magma temperatures have been estimated at higher than . The cones are constructed by reddish lapilli and lava bombs up to wide with subordinate amounts of ash-like material, concentrated in the talus deposits that have been formed by erosion at the basis of the cones. Arenite of sedimentary origin and dacite are found as xenoliths.
The anterior talofibular ligament is a ligament in the ankle. It passes from the anterior margin of the fibular malleolus, anteriorly and laterally, to the talus bone, in front of its lateral articular facet. It is one of the lateral ligaments of the ankle and prevents the foot from sliding forward in relation to the shin. It is the most commonly injured ligament in a sprained ankle—from an inversion injury—and will allow a positive anterior drawer test of the ankle if completely torn.
From Games, Gods and Gambling by F. N. David: :In ancient times there were games played using astragali, or Talus bone. The Pottery of ancient Greece was evidence to show that there was a circle drawn on the floor and the astragali were tossed into this circle, much like playing marbles. In Egypt, excavators of tombs found a game they called "Hounds and Jackals", which closely resembles the modern game "Snakes and Ladders". It seems that this is the early stages of the creation of dice.
Precipitation would frequently trigger lahars and these would continuously create problems in the Squamish and Cheakamus river valleys. If the lava dome continues to grow, it would eventually rise above the crater rim. The lava would be cooling and expanding then may produce landslides to create a massive zone of blocky talus in the Squamish river valley. While the dome of lava grows, it would frequently subside to create large pyroclastic flows that would again travel down the adjacent Squamish and Cheakamus river valleys.
Douka, K. 2011. An Upper Palaeolithic shell scraper from Ksar Akil (Lebanon). Journal of Archaeological Science 38 (2):429-437Kuhn, Steven L., Stiner, Mary C., Reese, David S., Güleç, Erksin., Ornaments of the earliest Upper Paleolithic: New insights from the Levant, Edited by Henry C. Harpending, PNAS, June 5th 2001 The site was rescued from burial under the sludge of gravel-making machines in 1964 by the Department of Antiquities, although is mostly unrecognizable due to quarrying operations with its talus buried under tons of soil.
Marmot on left The yellow-bellied marmot lives in southwestern Canada and western United States, including the Rocky Mountains and the Sierra Nevada. Northwards, its range extends into the southern British Columbia and goes eastwards up to the montane and basin regions of Wyoming, eastern Montana, Colorado, and southern Alberta. Southwards, its range extends into northern New Mexico. It inhabits steppes, meadows, talus fields, and other open habitats, sometimes on the edge of deciduous or coniferous forests, and found from as low as to over of elevation.
The snail lives on rocky mountain slopes, taking shelter in talus and rockslides. During the dry conditions common in its habitat, the snail seals its shell aperture to solid rock to avoid desiccation. The rock should be rich in calcium carbonate, which the snail uses to form its shell. It is associated with local plant species such as saguaro cactus (Carnegiea gigantea), yellow paloverde (Parkinsonia microphylla), brittlebush (Encelia farinosa), foxtail brome (Bromus madritensis), Natal grass (Melinis repens), creosote bush (Larrea tridentata), and Coulter's lupine (Lupinus sparsiflorus).
The collared pika within the talus sites where it resides and stores up food caches The estimated population density is roughly around 6.4 to 7.2 individuals per hectare. In various regions of the Yukon, the range is around one to four pikas per hectare. Both collared pikas and American pikas are commonly believed to be philopatric species. In addition, research data have shown that young collared pikas rarely disperse over 300 m away from their original den, and adults hardly ever leave an established territory.
Tretower Castle, as engraved around 1800, showing an impression of its earlier and fullest extent The castle is roughly triangular in plan, with the motte and keep assemblage occupying the western corner. The 12th century shell-keep is an irregular enclosure with a gate-tower on the line of approach from the bailey. In the centre of the shell stands the tall cylindrical 13th century keep. The keep is of three storeys, with an original entrance at first floor level, above a strong, slanted batter or talus.
The No. 2 mine was established on the southern side of the river, east of the works. This mine was to provide most of the oil shale for the working life of Newnes. The main works site was established in a sweeping bend on the south bank of the Wolgan River and extending up the adjacent talus hillside. These works consisted of retorts, various distillation areas, oil storage tanks and washers, plant for the refining of the various finished products, a power station, workshops, etc.
Hot, dry upper slopes, cool, moist ravines, and mineral-rich ledges of basalt talus produce a combination of microclimate ecosystems on the mountain that support plant and animal species uncommon in greater Connecticut. Examples rare plant and animal species (protected by the state of Connecticut) that live on Saltonstall Mountain include the eastern box turtle, red-shouldered hawk, and violet wood sorrel. Saltonstall Mountain is also an important raptor migration path. (See Metacomet Ridge for more information on the geology and ecosystem of Saltonstall Mountain).
Such clonal stands of Linnaea can be long-persisting, in some places remaining extant even if seed is not produced or if seedling germination or establishment does not occur. The species was presumably common in areas south of its present range during times of Pleistocene ("Ice Age") glaciations, and its clone-forming perennial growth habit has allowed it to survive the subsequent millennia locally within this former range in various high- elevation or otherwise cool and moist habitats, including algific talus slopes with persisting underground periglacial ice.
Around the late 19th and early 20th centuries, North River Mills residents would celebrate Independence Day and other occasions as late as September by digging up ice from the talus for the making of ice cream and lemonade. The mountain had through generations been owned by the Deaver family, the last of which was Mrs. Virginia Pugh. On September 22, 1962 Hampshire County farmer Otis Baker purchased the Ice Mountain and an adjacent for $23,000 at a public auction at the Hampshire County Courthouse in Romney.
On April 13, 1946, Maria Spencer traveled to the Bahamas to begin her work in Andros, conducting strati-graphic testing on the land. This testing was done at a location off of the eastern shore, approximately 7 miles inland. This location was picked specifically due to the lack of influence from the talus deposits that were built out from the reef, as well as minimal movement from the reef front’s tectonic waves. This included possible slumping of the land and movement in the layers of the earth.
The inferior articular surface is quadrilateral, and smooth for articulation with the talus. It is concave from before backward, broader in front than behind, and traversed from before backward by a slight elevation, separating two depressions. It is continuous with that on the medial malleolus. The anterior surface of the lower extremity is smooth and rounded above, and covered by the tendons of the Extensor muscles; its lower margin presents a rough transverse depression for the attachment of the articular capsule of the ankle-joint.
Keller blames herself for not catching the disease sooner, but refuses to give up even as McKay has only a few days left to live. Ronon Dex proposes an alternative: a shrine on the planet Talus that grants those afflicted with the Second Childhood a single day of mental clarity, followed by a quick death. Jeannie overrules Keller's wishes and asks that McKay be brought to the planet. Despite the fact that the planet has become a Wraith stronghold, Richard Woolsey reluctantly approves the mission.
Astragalectomy, sometimes called a talectomy, is a surgical operation for removal of the talus bone (astragalus) for stabilization of the ankle. Historically, an astragalectomy was used in cases of severe ankle trauma and congenial talipes equinovarus (clubfoot). It is no longer a common operation, but is still used in cases of a deformed calcaneus, foot paralysis following poliomyelitis, and rigid clubfoot deformities that are secondary to spina bifida or arthrogryposis (AMC). The surgery is also performed in severe cases of pulverized or infected open fractures.
He considered his next trip, in 1917, to have "practically exhausted" the quarry, with 1300 kg of material being collected that year. He returned to take additional collections, mainly from talus material, in 1919, 1921, and 1924, amassing a total of 65,000 fossil specimens over 30,000 slabs. During these years, he made further preliminary descriptions of the less glamorous sponges and algae. He photographed and clearly intended to describe many further taxa, many of which sat alone with their photograph in a Smithsonian drawer for decades after Walcott's death.e.g.
The Silver Star Mountain area consists of an eroded plateau, largely made up of lava, with an average relief of about and reaching a local maximum elevation of . Unlike the rest of the western Cascade backcountry, it has a ridge-like appearance, creating a striking skyline similar to mountains further north in the Cascade Range. The area lacks trees and comprises steep cliffs, talus slopes, and meadows filled with wildflowers. The locale drains into the Washougal River and the Lewis River's South Fork, which flow to the south and west respectively.
From there Pemon Indians Cecilio and Feliciano joined them and it took four days to traverse right to the col between Tramen and Ilu Tepui where the Indians left them. On the 24 November they left their tent at dawn and climbed the steep vegetated talus slope to the first steep step. A difficult move up a steep vegetated corner led to a belay ledge below the plateau. They crossed the half-mile rock platform, leaving stone cairns and upturned pitcher plants every few metres to mark the route in case the swirling cloud descended.
The Dubuque region is relatively far south for the white pine to thrive. White Pine Hollow, part of the Driftless Area, is a patch of north-facing algific talus slope land, a subset of dolomite karstland with many sinkholes, caverns, and other sharp changes in elevation. The conifer population may have established itself here at a time when the climate of Iowa was colder than it is today, and this grove could be a relict of what was once a much larger population. White Pine Hollow contains over 625 species of plants.
Erigeron algidus is a species of flowering plant in the daisy family known by the common name stalked fleabane. Erigeron algidus is native to the High Sierra and nearby peaks in eastern California and western Nevada.Biota of north America Program 2014 county distribution map It is a resident of alpine plant communities such as talus slopes.Calflora taxon report, University of California, Erigeron algidus Jepson stalked fleabane Erigeron algidus a daisy-like perennial with a basal clump of narrow fuzzy leaves and erect, naked stems to 30 centimeters (1 foot) in height.
Navajo boy at T-shaped door The Pueblo III Period (AD 1150 to AD 1350) was the third period, also called the "Great Pueblo period" when Ancestral Puebloans lived in large cliff-dwelling, multi-storied pueblo, or cliff-side talus house communities. By the end of the period, the ancient people of the Four Corners region migrated south into larger, centralized pueblos in central and southern Arizona and New Mexico. The Pueblo III Period (Pecos Classification) is roughly the same as the "Great Pueblo Period" and "Classic Pueblo Period" (AD 1100 to AD 1300).
The Hunstanton lifeboat station was officially opened in June 1979 with D 181 performing its first service in July 1979, saving two people from a rubber dinghy. In April 1980 another D-class ILB D 126 was sent to the station. With the re-opening of the station being a resounding success the RNLI agreed that the station would be sent a new Atlantic-class 21 ILB together with a new drive-on drive-of trailer and a new Talus MB-4H amphibious tractor to launch the ILB.
Crac des Chevaliers: the south face of the inner ward with its steep glacis. Glacis, also called talus, were incorporated into medieval fortifications to strengthen the walls against undermining, to hamper escalades and so that missiles dropped from the battlements would ricochet off the glacis into attacking forces. Towards the end of the medieval period some castles were modified to make them defensible against cannons. Glacis consisting of earthen slopes faced with stones were placed in front of the curtain walls and bastions (towers) to absorb the impact of cannon shots or to deflect them.
The new species of Bathychaunax was found at depths between 1320m and 1760 m. Furthermore, in 2015 an article was published indicating that new specemins from the genus Chaunacops were found off the coasts of Australia and New Caledonia. In addition, it was found that the Chaunacops coloratus are also often found near "manganese-encrusted volcanic talus slopes". The fish were observed to often have one of their pectoral fins in sediment and another one on a rock in order to make it seem as though they were wedged between two substrates.
They have inactive vents similar in profile to Posidon with a talus (scree) deposit separating them from the central vent field, though they have not been as actively explored. It is hypothesized from the ages of samples collected that hot fluid flow migrated from the south to the north where Posidon currently resides. Strontium, carbon, and oxygen isotope data and radiocarbon ages document at least 30,000 years of hydrothermal activity driven by serpentinization reactions at Lost City, making Lost City older than all known black smoker vents by at least two orders of magnitude.
Slopes evolve by parallel retreat when rock strength remains constant and basal debris, like talus, is continuously removed. These conditions are often met in areas where hard horizontal rock layers of basalt or hard sedimentary rock overlie softer rocks. Slopes tend to cease to evolve by parallel retreat once overlying hard layers covering softer rock have been fully eroded. As rock strength is related to weathering and weathering to climate in the case a slope retreat over large distances or over long time- spans retreat is unlikely to remain fully parallel.
Along with playing soccer and football, he studied medicine at the University of Gothenburg and graduated in 1966. He served his Residency in General Surgery in Kungalvs Hospital and his Orthopaedic Residency in Sahlgren University Hospital from 1967-1974 and became specialist in General Surgery 1972 and in Orthopaedic Surgery 1974. In 1974, Dr. Peterson defended his thesis: Fracture of the Neck of the Talus, An Experimental and Clinical Study. In 1980, Dr. Peterson was approved associate professor of Orthopaedic Surgery at the University of Goteborg and in 2000, appointed professor of Orthopaedic Surgery.
Components of a scarp where the caprock slopes back from the rim, as is common Aerial view of retreating scarp in Namibia. A scarp is a line of cliffs that has usually been formed by faulting or erosion. If it is protected by a strong caprock, or if it contains vertical fractures, it may retain its steep profile as it retreats. Scarps in dry climates typically have a near-vertical upper face, that may account for 10% - 75% of the total height, with a talus-covered sloping rampart forming the lower section.
Delphinium polycladon is a species of larkspur known by the common name mountain marsh larkspur. It is native to the High Sierra Nevada and the White and Inyo Mountains of eastern California and far western Nevada, where it grows in wet sites in the talus. It is a perennial herb producing one or more erect stems which easily exceed a meter in height but often remain dwarfed in high-elevation, exposed habitat with thin soils.Flora of North America The leaves are small and mostly located near the base of the plant.
The rim of the caldera lies at a depth of about . Parasitic cones occur around the caldera, and a cone is also found within the inner caldera and appears to be about high resurgent dome; additional cones can be found on the caldera floor which is covered by sediments. On Mussel Ridge, a ridge located within the caldera and close to its southwestern margin, seafloor observations have found cemented volcanic ash, dispersed rocks, mud, pillow lavas, pillow tube lavas, and talus. Another about high cone is situated between the Monowai cone and the caldera.
In the human body, the tarsus is a cluster of seven articulating bones in each foot situated between the lower end of the tibia and the fibula of the lower leg and the metatarsus. It is made up of the midfoot (cuboid, medial, intermediate, and lateral cuneiform, and navicular) and hindfoot (talus and calcaneus). The tarsus articulates with the bones of the metatarsus, which in turn articulate with the proximal phalanges of the toes. The joint between the tibia and fibula above and the tarsus below is referred to as the ankle joint.
The Mosier Mounds Complex (Smithsonian trinomial: 35WS274), also known locally as the Mosier Battlements, is an archaeological site near Mosier, Oregon, United States. This collection of stone walls, pits, and mounds amid a basalt talus slope is the largest and most complex of a number of similar Native American sites in the southern Columbia Plateau. The site predates the arrival of Europeans and probably the local ascendance of Chinookan peoples, but has resisted more precise dating or cultural affiliation.. The site was added to the National Register of Historic Places in 2003..
The Gettysburg Formation and other formations of the Newark Supergroup were deposited in the Gettysburg Basin, just one of many Triassic rift basins existing on the east coast of North and South America, which formed as plate tectonics pulled apart Pangaea into the continents we see today. The conglomerates within the formation were most likely alluvial fan or mudflow deposits, or possibly talus, eroding directly from the Precambrian and early Paleozoic rocks to the north and south. The sandstones and shales were most likely deposited in the flooded rift valley as deltas.
Polemonium chartaceum is a rare species of flowering plant in the phlox family known by the common names Mason's Jacob's-ladder and Mason's sky pilot. It is native to California, where it has a disjunct distribution. It occurs in the Klamath Mountains as well as the ranges east of the Sierra Nevada, including the White Mountains, where its distribution extends just into Nevada.Nevada Natural Heritage Program Rare Plant Fact Sheet It is a plant of high elevations, growing in exposed, rocky mountain slope habitat such as talus and alpine fellfields.
Polemonium pulcherrimum is a species of flowering plant in the phlox family known by several common names, including beautiful Jacob's-ladder, showy Jacob's-ladder, and skunk-leaved polemonium. It is native to western North America from Alaska and Yukon to Arizona and New Mexico, where it can be found in many types of mountain habitat, including alpine talus at high elevations. It is a common and widespread wildflower in several regions. It is a perennial herb producing a clump of several erect stem approaching a maximum height of 30 centimeters.
Specifically, it is important to bring the ankle to neutral, the heel into neutral, the midfoot aligned with the hindfoot (navicula aligned with the talus, and the cuboid aligned with the calcaneus). Once these joints can be aligned, thin wires are usually placed across these joints to hold them in the corrected position. These wires are temporary and left out through the skin for removal after 3–4 weeks. Once the joints are aligned, tendons (typically the Achilles, posterior tibialis, and flexor halluces longus) are repaired at an appropriate length.
The peak is formed from sandstones of the Brownstones Formation and the overlying Plateau Beds Formation of the Old Red Sandstone laid down during the Devonian period. In accord with a regional trend, the beds dips southwards into the South Wales Coalfield basin. A notable feature of the hill is the prominent ridge of Fan Fechan (the 'little peak') which parallels the main ridge below it to the east. It is largely composed of broken Old Red Sandstone and has been interpreted as either a glacial moraine or as a pro-talus rampart.
The Oddfellows is long and has a beam of and with the engine raised a draught of just .Lifeboat Specifications retrieved 18 March 2013 The propulsion is provided by two Yamaha inversion-proof four- stroke petrol engines. The motors are capable of pushing the lifeboat through the water at speeds in excess of . The lifeboat is launched with a crew of four aboard and uses a Do-Do (drive on - drive off) trolley pushed directly into the sea by a Talus MB-4H amphibious tractor via the station slipway.
At Lost Creek Lake, the lava attained its maximum thickness of and thinned to about to the north of Medford. Andesite lava cap Since the Olson eruption, the Rogue River has eroded 90 percent of the solidified lava. Though the andesite prevented much erosion to the caps of the Table Rocks, the andesite-capped cliffs eroded from the side as the softer sedimentary units of the Payne Cliffs Formation gave way. This erosion created expansive talus fields which surround the plateaus on all sides, creating slopes capable of supporting abundant plant and animal life.
Backslope plant communities tend to be more similar to the adjacent Berkshire plateau containing species common to the northern hardwood and oak-hickory forest forest types. Eastern hemlock crowds narrow ravines, blocking sunlight and creating damp, cooler growing conditions with associated cooler climate plant species. Talus slopes are especially rich in nutrients and support a number of calcium-loving plants uncommon in Massachusetts. Because the traprock ridges generate such varied terrain, they are the home of several plant and animal species that are state-listed or globally rare.
Further study determined that the remains represented a new dinosaur genus which was intermediate between early bipedal sauropodomorphs and the later giant quadruped sauropods, adding to the list of transitional sauropodomorphs from Argentina and South Africa, and further clarifying their diversification. A distinctive feature of this dinosaur is the cross-shaped astragalus or talus bone in its ankle. The generic name is derived from the Sesotho word sefapano, meaning ‘cross’ and the Greek word saurus, meaning 'lizard'. The specific name refers to Zastron, the type locality, where the specimen was discovered.
Eastern hemlock crowds narrow ravines, blocking sunlight and creating damp, cooler growing conditions with associated cooler climate plant species. Talus slopes are especially rich in nutrients and support a number of calcium-loving plants uncommon in the region. Miles of high cliffs make ideal raptor habitat, and the Metacomet Ridge is a seasonal raptor migration corridor. Ram's-head lady's slipperBecause the topography of the ridge offers such varied terrain, many species reach the northern or southern limit of their range on the Metacomet Ridge; others are considered rare nationally or globally.
Silene grayi is a species of flowering plant in the family Caryophyllaceae known by the common name Gray's catchfly. It is native to the mountains of Oregon and northern California, including the Klamath Mountains, where it grows in chaparral, mountain forests, and the talus of high slopes in alpine climates. It has been observed to occur in a plant association with oceanspray (Holodiscus microphyllus), littleleaf silverback (Luina hypoleuca), and Gray's bedstraw (Galium grayanum).USFS. Establishment record for Manzanita Creek Research Natural Area within the Shasta-Trinity National Forests, Trinity Co., California.
Upland sinkholes contribute to the air flow regime and are an important component of a unique system called an algific talus slopes, meaning a cold producing rocky slope. Even on a midsummer day when the outside air temperature is 90 °F (32 °C), ground temperatures on these slopes range from 42 °F (6 °C) to about 55 °F (13 °C). Although the slopes will freeze in winter, the temperatures are moderated. These slopes remain cool throughout the year and are home to rare species of plants and animals.
USGS, North Park-Medicine Bow Mountains Project: Task 3: Neogene landscape evolution Beginning two million years ago, glaciers began carving the jagged peaks of the Never Summer Mountains. Successive waves of glaciation continued to reshape the mountains until the Pinedale Glaciation ended twelve-thousand years ago.Harris, Ann G., Esther Tuttle and Sherwood D. Tuttle, Geology of National Parks, Kendall/Hunt Publishing Company, 6th ed., 2003, The peaks are enormous weathered masses of granitic rock heavily covered with green and orange lichens surrounded on all sides by large fields of talus shed from the original peaks.
Five short nature trails cross the park area: the Ed Foote Trail, Lookout Trail, Otter Creek Trail, River Trail, and Talus Trail. Visitors to the canyon can climb 372 steps that lead to the "Lookout" located on the wall of the gorge. The observation platform situated above the tracks provides a panoramic view of the canyon. The Algoma Central Railway offers tours trains to canyon in the summer, fall and winter months; during late September and October for the changing colors and in December, January and February for the "snow train".
In June, Drury was set to compete in Providence, Rhode Island at the USA Gymnastics Championships, the final Olympic selection event. Having won the previous two selection events, Drury was considered the favorite to earn herself a return trip to Rio in August. However, during a training session the day before the individual event was to start, Drury sustained an injury to her right foot. Initially believing it to be a bruise, an MRI later confirmed a fracture in her talus bone, forcing her to withdraw from the competition.
During the ensuing long period of dormancy, the Cheekye River cut a deep valley into the cone's western flank that was later filled with a glacier. After reaching its maximum extent the Cheekye Glacier along with part of the area's ice sheet were covered with volcanic ash and fragmented debris from Garibaldi. This period of growth began with the eruption of the Atwell Peak plug dome from a ridge surrounded by the several thousand foot ice sheet. As the plug dome rose, massive sheets of broken lava crumbled as talus down its sides.
Talus slopes are especially rich in nutrients and support a number of calcium-loving plants uncommon in Massachusetts. Because the traprock ridges generate such varied terrain, they are the home of several plant and animal species that are state-listed or globally rare,A thorough study of the Metacomet Ridge environment and its species can be found within a report commissioned by the National Park Service as part of its New England National Scenic Trail Study such as the timber rattlesnake. The Holyoke Range is also an important seasonal raptor migration path.
Symptoms of an ankle fracture can be similar to those of ankle sprains (pain), though typically they are often more severe by comparison. It is exceedingly rare for the ankle joint to dislocate in the presence of ligamentous injury alone. However, in the setting of an ankle fracture the talus can become unstable and subluxate or dislocate. Patients may notice ecchymosis ("black and blue" coloraction from bleeding under the skin), or there may be an abnormal position, alignment, gross instability, or lack of normal motion secondary to pain.
Aspect plays a role as well; the treeline often occurs at higher elevations on warmer equator-facing slopes. Because the alpine zone is present only on mountains, much of the landscape is rugged and broken, with rocky, snowcapped peaks, cliffs, and talus slopes, but also contains areas of gently rolling to almost flat topography. Averaging over many locations and local microclimates, the treeline rises when moving 1 degree south from 70 to 50°N, and per degree from 50 to 30°N. Between 30°N and 20°S, the treeline is roughly constant, between .
The navicular bone in humans is one of the tarsal bones, found in the foot. Its name derives from the human bone's resemblance to a small boat, caused by the strongly concave proximal articular surface. The term navicular bone or hand navicular bone was formerly used for the scaphoid bone, one of the carpal bones of the wrist. The navicular bone in humans is located on the medial side of the foot, and articulates proximally with the talus, distally with the three cuneiform bones, and laterally with the cuboid.
The park's talus caves provide roosting and breeding habitat for the bats. In the 1990s, a student biologist, Olivia Messinger, did a census of bees at Pinnacles. She found that the park has more bees per unit area than known anywhere else on earth, around 400 species. Most of these bees are solitary bees, not living in colonies like European honeybees, and most live for only three to four weeks, and since flowers bloom here throughout the growing season, many niches are available for all the bee species.
Other trails include lush wildflower-accented views along flat stream beds, trails that bring one into beautiful caves, and trails that involve high vistas of the Pinnacle formations. The park is popular with advanced rock climbers due to the many difficult and challenging climbs. The caves at Pinnacles are talus caves, formed when steep, narrow canyons were filled with boulders, leaving passages between the larger rocks. Bear Gulch Cave on the east side of the park and Balconies Cave on the west side are seasonally open to visitors.
A lava dome, Lassen Peak has a volume of making it the largest lava dome on Earth. The volcano arose from the destroyed northern flank of now-collapsed Mount Tehama about 27,000 years ago, from a series of eruptions over the course of a few years. The mountain has been significantly eroded by glaciers over the last 25,000 years, and is now covered in talus deposits. On May 22, 1915, a powerful explosive eruption at Lassen Peak devastated nearby areas, and spread volcanic ash as far as to the east.
Piles of talus and rockfall were created by retreating alpine glaciers. In the high mountains, the major rivers have their headwaters in alpine glacially carved cirques. During the Orting, followed by the Stuck, the Salmon Springs, and the Fraser glaciations, the vast continental Cordilleran Ice Sheet descended from Alaska south through British Columbia to the Olympics. The ice split into the Juan de Fuca and Puget ice lobes, as they encountered the resistant Olympic Mountains, carving out the current waterways and advanced as far south as present day Olympia.
Invasive insect species in the Shenandoah National Park, namely the gypsy moth (Lymantria dispar dispar) and the hemlock woolly adelgid (Adelges tsugae), also threaten the survival of the Shenandoah salamander. Gypsy moth larvae feed on tree leaves, resulting in widespread defoliation and tree mortality. This loss of overstory dramatically alters the Shenandoah salamander habitat, reducing the ground moisture and potentially altering the Shenandoah salamander’s ability to catch prey. Hemlock woolly adelgids are a major cause of hemlock tree mortality within Shenandoah National Park, contributing to overstory loss and talus slope habitat dehydration.
There is an unusual diversity of vegetation on the ridge, containing species typically found north of this region alongside species typically found to the south or restricted to the Coastal Plain. The results is an area where many regionally rare plants are found at or near the limits of their ranges. Other rare species found in the area are those adapted to the harsh conditions on the ridge. Upland communities include chestnut oak and mixed-oak forest, pine barrens including dwarf pine ridges, hemlock-northern hardwood forest, and cliff and talus slope and cave communities.
Satellite image of the Apocalypse Peaks The Apocalypse Peaks () are a group of peaks with a highest point of , standing east of Willett Range and between Barwick Valley and Balham Valley, in Victoria Land, Antarctica. The peaks were so named by the Victoria University of Wellington Antarctic Expedition (VUWAE) (1958–59) because the peaks are cut by talus slopes which gives them the appearance of the "Riders of the Apocalypse." The peaks lie on the Pennell Coast, a portion of Antarctica lying between Cape Williams and Cape Adare.
Erigeron miser is a species of flowering plant in the daisy family known by the common names starved daisy or starved fleabane. It is endemic to California, where it is known only from the northern High Sierra Nevada.Calflora taxon report, University of California, Erigeron miser A. Gray, starved daisy, starved fleabane Biota of North America Program 2014 county distribution map Erigeron miser grows in rock crevices in coniferous forests and talus. It is a perennial herb producing several decumbent or erect stems up to about 25 centimeters (10 inches) long from a woody caudex.
While the mountains of the United Kingdom are not very tall, they contain much formerly glaciated terrain with steep cliffs, talus slopes, high peaks and cirque basins, and generally experience a sub-Arctic climate at relatively low altitudes. Snow and high winds, sometimes in excess of , are possible any month of the year. Rescue operations in these conditions require personnel with specialised mountaineering training and equipment. The Royal Air Force mountain rescue teams are credited with some of the earliest development of mountain rescue techniques and teams in the United Kingdom and overseas.
That day, Kaptzevich and Kleist rendezvoused with Blücher at Vertus, Olsufiev marched west to Champaubert, Sacken reached La Ferté-sous-Jouarre and Yorck was at Château-Thierry. According to Karl Freiherr von Müffling of Blücher's staff, the Army of Silesia counted 57,000 men, including Sacken's 20,000, Yorck's 18,000 and Kaptzevich, Olsufiev and Kleist with a combined 19,000. Marmont's cavalry advance guard appeared at Talus-Saint-Prix on the Petit Morin River. Because the horsemen soon withdrew, Blücher's chief of staff August Neidhardt von Gneisenau believed they represented no danger.
Le Reclus Abbey (; ) was a Cistercian monastery in the present Talus-Saint- Prix near Sézanne in the arrondissement of Épernay, Marne, France. It was in the diocese of Troyes. It was founded by Bernard of Clairvaux in around the hermitage of Blessed Hugh the Hermit (Hugues le Reclus, Hugo reclusus), from whom the abbey took its name. Hugh had at first retired from the world to an arid place in the parish of Saint-Prix known as Fons Balimi around 1128–1130, before being joined by a few companions.
Os trigonum on x-ray Though irregular in shape, the talus can be subdivided into three parts. Facing anteriorly, the head carries the articulate surface of the navicular bone, and the neck, the roughened area between the body and the head, has small vascular channels. The body features several prominent articulate surfaces: On its superior side is the trochlea tali, which is semi- cylindrical,Lee F. Rogers (1992) Radiology of skeletal trauma - Volume 2 p.1463 and it is flanked by the articulate facets for the two malleoli.
The design was conceived by Clayton Engineering Limited, who worked closely with the RNLI to produce this very efficient launch system. The carriage works in conjunction with the range of Talus tractors which are used to deploy the Atlantic 85 inshore lifeboats. There are three versions of this carriage which include a standard carriage and the option of a hydraulic power pack so that the angle of the launch can be changed to suit the conditions. The carriage’s launch platform has a main bed which elevates through 10° to achieve this feature.
The mainstay of management of congenital vertical talus is serial manipulative casting also known as the reversed Ponseti technique. This technique involves gradual step-wise correction of the deformity usually on weekly basis. In the event there is residual deformity or incomplete correction at the end of the serial castings, the orthopedic surgeon may resort to a minimally invasive surgery at the talo-navicular joint to achieve full correction. The results of the serial manipulative casting technique or reversed Ponseti technique are satisfactory especially if started shortly after birth.
Naviculectomy may be indicated in the above resistant case of congenital vertical talus on the condition that a plantigrade foot is considered unlikely by the conservative serial casting methods. And on the condition that extensive soft tissue release is not expected to yield an satisfactory clinical and functional result. Generally, naviculectomy is a more tissue-friendly procedure in contrast to the more aggressive classic and extensive peri-talar soft tissue releases. The clinical and radiologic results of naviculectomy are satisfactory on the short term, and long term follow-up.
An eastern small-footed myotis at Grayson Highlands State Park in Virginia There is little published information about the spring and summer roosting locations of eastern small- footed bats. The first study into the summer roosting habits was only done in 2011 so information is scarce. This study discovered that these bats most commonly use ground level rock roosts in talus slopes, rock fields and vertical cliff faces for their summer roosts. On average they change their roosts every 1.1 days, males travel about 41 meters between consecutive roosts and females around 67 meters.
Mount Tom, , is a steep, rugged traprock mountain peak on the west bank of the Connecticut River 4.5 miles (7 km) northwest of downtown Holyoke, Massachusetts. The mountain is the southernmost and highest peak of the Mount Tom Range and the highest traprock peak of the long Metacomet Ridge. A popular outdoor recreation resource, the mountain is known for its continuous line of cliffs and talus slopes visible from the south and west, its dramatic rise over the surrounding Connecticut River Valley, and its rare plant communities and microclimate ecosystems.The Metacomet-Monadnock Trail Guide.
The Dinétah region is marked by high mesas and deep canyons that drain to the San Juan River. The canyons of the area are composed of irregular layers of sandstone, marked by multiple benches and talus slopes. Elevations average approximately 5,000 to 6,500 feet, with a few mountain peaks rising to more than 14,000 feet. The traditional boundary of the land is demarcated by four mountains: Blanca Peak (Sis Naajinį́), to the east, Mount Taylor (Tsoodzil), to the south, the San Francisco Peaks (Dook'o'ooshį́į́), to the west, and Hesperus Peak, (Dibé Nitsaa), to the north.
Palaeolithic deposits, up to thick, underlie the middle Holocene layers, around thick and contain Middle and Late Neolithic pottery. Locally derived rock blocks up to in size rest on the talus slope in front of, and below, the entrance, indicating that there was originally an overhang that later collapsed. Deposits of human occupation contain numerous bones and stone tools, rounded out of size-exogenous pebbles and abundant charcoal detritus which is related to fireplaces. About fifty discovered pottery shards are evidence for occupation of the cave during the Neolithic/Iron Age transition.
Sphaeromeria cana (recently proposed name Artemisia albicans) is a species of flowering plant in the aster family known by the common name gray chickensage. It is native to the western United States, where it is known from the Sierra Nevada, the adjacent desert ranges of eastern California and Nevada, and Steens Mountain of Oregon. It grows in dry, rocky mountain habitat, such as cracks and crevices, including the talus above the tree line. This is an aromatic subshrub with numerous erect branches growing up to 30 to 60 centimeters tall.
Generally, the surgical procedure involves making an anterolateral incision, stripping the ligaments from both malleoli and the calcaneus so that the foot can be displaced posteriorly. The talus is then resected, and the foot is placed so that the lateral malleolus rests opposite the calcaneocuboid joint, and the medial malleolus lies just above and behind the navicular bone. The foot is held in place with a surgical pin or with Kirschner wire. After the operation, the patient wears an above- knee cast for six weeks, followed by a below-knee cast for eighteen weeks.
Roberts Creek State Preserve is located in rural Clayton County, Iowa, in Wagner Township, near St. Olaf, Iowa, and a few miles north of Elkader, Iowa. Roberts Creek is a tributary of the Turkey River. The Preserve contains algific talus slopes, a rare ecosystem unique to the Driftless Area and hosts a threatened wildflower. The preserve is not open to the public, in that it is a rare ecosystem that contains a threatened species, Aconitum noveboracense, also known as Northern Blue Monkshood or Northern Wild Monkshood, a saxifrage, (a buttercup).
The ruminants, ancestors of the Cervidae, are believed to have evolved from Diacodexis, the earliest known artiodactyl (even-toed ungulate), 50–55 Mya in the Eocene. Diacodexis, nearly the size of a rabbit, featured the talus bone characteristic of all modern even-toed ungulates. This ancestor and its relatives occurred throughout North America and Eurasia, but were on the decline by at least 46 Mya. Analysis of a nearly complete skeleton of Diacodexis discovered in 1982 gave rise to speculation that this ancestor could be closer to the non-ruminants than the ruminants.
A number of ditches near Silver Star Mountain known as the Indian Pits can be seen on one of the trails, which is known as the Indian Pits Trail #180E. These ditches also occur in other parts of the Columbia River Gorge area. Archaeologists debate the purpose of these pits, though three prominent hypotheses have emerged. One states that the pits were built by Native Americans to seek spiritual visions, while another claims that the pits served as blinds for hunting mountain sheep and goats fleeing cougars or wolves down local talus slopes or other hunters in brush below.
The older volcanics of Laguna del Maule have been disproportionately eroded by glacial action. Slopes around Laguna del Maule lake are covered by colluvium including talus. Besides Laguna del Maule, other lakes in the field are Laguna Cari Launa on the Chilean side in the northeastern sector of the field, and Laguna Fea in the south at elevation and Laguna Negra lake both on the Argentine side. The Laguna Sin Salida ("lake without exit"; so named because it lacks a river running out of it) is in the northeastern sector of the volcanic field and it formed within a glacial cirque.
Emerald Lake and the Timpanogos Glacier from the summit of Mount Timpanogos, September 2014 The glacier is situated on the north slope of Mount Timpanogos (). The best evidence indicates that the Timpanogos Glacier was once a "true" glacier with crevasses present in the early 20th century, but that the surface portion was lost during the dust bowl drought of the 1930s and reduced to a permanent snowfield. The glacier is considered to be a rock glacier, since the remaining ice is buried in the talus. However, in 1994 the rocks parted, revealing a crevasse or meltwater channel in the buried ice.
This is due to two primary factors: the Cinema encompasses a greater elevation range, and receives more precipitation, due to its location on the east slopes of the Cascades, which provides alpine and subalpine environments. Fauna includes deer, elk, black bears, coyotes, badgers, many types of rodents, jackrabbits and rabbits, cougars, bobcats, porcupines, Reptiles and amphibians. Endangered endemic fauna includes the Larch Mountain salamander (Plethodon larselli), a rare, lungless amphibian that lives on steep talus slopes. Golden and bald eagles are permanent fixtures, as well as hawks, herons, sandhill cranes, and many migratory birds that move along the Pacific flyway.
A couloir may be a seam, scar, or fissure, or vertical crevasse in an otherwise solid mountain mass. Though often hemmed in by sheer cliff walls, couloirs may also be less well-defined, and often simply a line of broken talus or scree ascending the mountainside and bordered by trees or other natural features. Couloirs are especially significant in winter months when they may be filled in with snow or ice, and become much more noticeable than in warmer months when most of the snow and ice may recede. These physical features make the use of couloirs popular for both mountaineering and skiing.
In prison, Sarrazin wrote her first novels, L'Astragale and La Cavale, which were published after her release in 1964 (the astragale of the title is the French word for the talus bone, which both she and the main character of her novel broke on their escapes from jail). Astragale was translated in English at that same time. Their success allowed the married couple to settle in Montpellier where she wrote her third story, La Traversière. The novel also performed well, but she died shortly afterwards from complications during kidney surgery; she was only 29 years old.
The valleys of North Branch Bowman Creek and South Branch Bowman Creek are the only places in the Sweet Valley quadrangle where this type of surficial geology occurs. Part of the creek's valley also has surficial geology of bedrock consisting of sandstone and shale, which occurs on the valley walls and part of the valley floor. Most of the rest of the surficial geology along the creek consists of a till known as Wisconsinan Till, but there are wetlands and peat bogs as well. A talus deposit with sandstone boulders is located in the vicinity of North Branch Bowman Creek.
Earl H. Morris conducted an excavation of this open talus site in Animas Valley in 1938-1939. It was the first site where dwellings had been found of the early Basketmakers with actual house structures, one of which he describes as follows: > A site for the dwelling was secured by digging a drift into the steep > hillside and piling the excavated earth and stone out in front until a > terrace large enough to accommodate the projected house had been provided. > The floor area was scooped out to shallow saucer shape—in this case 9 m. in > diameter—and coated with mud.
Less fragmentary remains discovered between 2003 and 2009 demonstrated a close relationship between Azibius and Algeripithecus. Descriptions of the talus (ankle bone) in 2011 have helped to strengthen support for the strepsirrhine status of Azibius and Algeripithecus, which would indicate that the evolutionary history of lemurs and their kin is rooted in Africa. Likewise, if azibiids are simians, it would support the hypothesis that simians originated in Africa instead of Asia. Azibiids were small-bodied primates, with Algeripithecus minutus weighing between , Azibius trerki weighing approximately , and an unnamed species of Azibius being notably larger, weighing an estimated .
Adapidae is a family of extinct primates that primarily radiated during the Eocene epoch between about 55 and 34 million years ago. Adapid systematics and evolutionary relationships are controversial, but there is fairly good evidence from the postcranial skeleton (everything but the skull, or cranium) that adapids were stem strepsirrhines (members of the group including the living lemurs, lorises, and bushbabies). In particular, the anatomy of the adapid wrist and ankle (e.g., position of the groove for the flexor fibularis tendon on the talus, the presence of a sloping talo-fibular facet) show derived similarities with those of living strepsirrhines.
Today, along the summits of the Watchungs, talus slope environs as well as globally rare trap rock glade/outcrop communities and their unique species have become threatened by development. As a response, efforts to conserve the unique landscapes of the Watchungs have been undertaken. The largest of the conservation efforts so far is High Mountain Park Preserve, which at sets aside one of the largest tracts of wilderness in the New Jersey Piedmont. The park is known to contain at least one globally imperiled plant, Torrey's mountain mint (Pycnanthemum torrei), as well as three other plants endangered within New Jersey.
Abrupt vertical cliffs with visible talus slopes and frequent viewpoints are common throughout. Views are generally to the west on Provin Mountain, East Mountain, and the Mount Tom ranges; and to the north on the Holyoke Range. The Connecticut River cuts through the ridgeline between the Mount Tom and Holyoke ranges in Holyoke, Massachusetts, and the Westfield River separates Provin Mountain from East Mountain in Westfield. Historic features along the trail include the Horse Caves on Mount Norwottuck, the ruins of the 19th-century hotel Eyrie House on Mount Nonotuck, and the refurbished Mount Holyoke Summit House on Mount Holyoke.
The Mark O. Hatfield Wilderness is a wilderness area located on the northern side of Mount Hood in the northwestern Cascades of the U.S. state of Oregon, near the Columbia River Gorge and within Mount Hood National Forest. Prior to Wilderness designation it was known as the Columbia Gorge Recreation Area. The slopes of the Wilderness rise steeply to a slightly uneven plateau and on to mountain peaks, talus slopes, and lakes with elevations ranging from approximately near the river to on Mount Defiance. The main waterways in the Wilderness are Herman Creek, Eagle Creek, and Tanner Creek.
Lithoautotrophic microbial consortia are responsible for the phenomenon known as acid mine drainage, whereby energy-rich pyrite present in mine tailing heaps and in exposed rock faces is metabolized to form sulfites, which form potentially corrosive sulfuric acid when dissolved in water and exposed to aerial oxygen. Acid mine drainage drastically alters the acidity and chemistry of groundwater and streams, and may endanger plant and animal populations. Activity similar to acid mine drainage, but on a much lower scale, is also found in natural conditions such as the rocky beds of glaciers, in soil and talus, and in the deep subsurface.
Happy Isles is located where the slope of the Merced River changes from the much steeper upper main stem to the essentially flat Valley floor. At Happy Isles, the river gradient is approximately 2%. The gradient of the Merced River at Happy Isles is steeper than in the Valley floor, and the channel of the river is cut into erosion-resistant granitic boulders and talus materials, compared to channel deposits of sands and gravel present on the Valley floor. The steeper gradient and composition of streambed materials together impede meandering patterns from developing in this area.
Favourable geology and climate are the principal causal mechanisms of rockfall, factors that include intact condition of the rock mass, discontinuities within the rockmass, weathering susceptibility, ground and surface water, freeze-thaw, root- wedging, and external stresses. A tree may be blown by the wind, and this causes a pressure at the root level and this loosens rocks and can trigger a fall. The pieces of rock collect at the bottom creating a talus or scree. Rocks falling from the cliff may dislodge other rocks and serve to create another mass wasting process, for example an avalanche.
Claytonia megarhiza is a species of wildflower in the family Montiaceae known by the common names fell-fields claytonia and alpine springbeauty. It is native to western North America from northwestern Canada to New Mexico, where it grows in rock crevices and talus habitats in subalpine and alpine climates. The species is known from summits and slopes of North America's highest mountains including the Redstone Mountains of the Canadian Northwest Territories, disjunct south to the central and southern Rocky Mountains reaching a southern limit in the Sangre de Cristo Mountains. The specific epithet megarhiza is Greek for "large roots".
Alternately, the Elsay Lake Trail takes one to the East of Mount Seymour, across several rock slides, then up a large talus slope (bear right to the low point of the ridge) to join the other trail on the south shoulder of the mountain. The route to Vicar Lakes, Mount Bishop and the Indian Arm Trail heads left shortly after the ridge starts to rise to Mount Elsay. The Peak is flanked by Mount Bishop and Elsay Lake on the North, with Mount Seymour and Runner Peak to the South. This is rough backcountry and should be approached only with caution and experience.
Additional uplift occurred when major faults developed to the east, especially the creation of Owens Valley from Basin and Range-associated extensional forces. Uplift of the Sierra accelerated again about two million years ago during the Pleistocene. The uplifting and increased erosion exposed granitic rocks in the area to surface pressures, resulting in exfoliation (responsible for the rounded shape of the many domes in the park) and mass wasting following the numerous fracture joint planes (cracks; especially vertical ones) in the now solidified plutons. Pleistocene glaciers further accelerated this process and the larger ones transported the resulting talus and till from valley floors.
The second is tibiofibular overlap, the horizontal distance between the medial border of the fibula and the lateral border of the anterior tibial prominence, with less than 10 mm being abnormal. The final measurement is the medial clear space, the distance between the lateral aspect of the medial malleolus and the medial border of the talus at the level of the talar dome, with a measurement greater than 4 mm being abnormal. Loss of any of these normal anatomic spaces can indirectly reflect ligamentous injury or occult fracture, and can be followed by MRI or CT.
The boathouse was abandoned in 1932, and the all-weather lifeboat was withdrawn, leaving the nearest stations at Fishguard and New Quay. The subsequent popularity of this area, with increased leisure incidents and accidents, led to the decision to construct a new station on the present site; this opened in 1971.Poppit Sands Information Board In 1987 a new boathouse, built for the new C-class lifeboat, was officially opened. Then in 1998 a new double boathouse was completed for a B-class and D-class lifeboats, for the Talus MB-4H launching vehicle, and it also provided improved crew facilities.
Rhodiola integrifolia is a species of flowering plant in the stonecrop family known by the common names ledge stonecrop, western roseroot, and king's crown. It is native to north-easternmost Russia, including Kamchatka, and western North America, where it grows in mountainous habitat in subalpine and alpine climates, including meadows, cliffs, and talus. It is a perennial herb producing a stout stem from a fleshy, branching caudex, reaching a maximum height near 30 centimeters. The fleshy leaves are alternately arranged on the stem, widely lance-shaped to oval and pointed, flat but upcurved toward the tip, reaching 2.5 centimeters long.
A green tuffbreccia composed of pumice fragments, feldspar crystals and minor debris is recognizable in several areas.Report on Preliminary Geology and Geochemistry of the Ilga Claim group Retrieved on 2007-10-11 Smooth northern flanks of the Ilgachuz Range are remnants of the original shield volcano The Dome Forming Assemblages include most of the rhyolite domes, related flows and the Ilgachuz Comendite. The northerly domes are subcircular talus mounds of plate sized pieces of light to dark grey, slightly porphyritic, flowbanded rhyolite with minor obsidian. Massive to banded chalcedony blobs and veinlets are related with these domes.
The Inn valley is an example of a valley carved by glaciers during the ice ages with a typical terraced structure caused by erosion. Eroded rocks from the most recent ice age lie at the bottom of the valley while the top of the valley consists of erosion from earlier ice ages. Glacial valleys have characteristically steep walls (reliefs); valleys with lower reliefs and talus slopes are remnants of glacial troughs or previously infilled valleys.Gerrard, (1990), 132 Moraines, piles of rock picked up during the movement of the glacier, accumulate at edges, centre and the terminus of glaciers.
Whenever eruptions took place in the presence of ice, lava was chilled by glaciers, creating glassy talus deposits. Sometimes, the lava coursed into areas previously carved by glaciers like at Sentinel Rock, filling canyons with volcanic rock. Moraines occur up to from the rim of Mazama's caldera, and there are glacial striations visible at several sites in the area. When the climactic eruption occurred, the climate was warm and dry, and the most recent period of glacial advance ceased about 27,000 years ago, so by the time Mazama collapsed, ice was likely only present at higher elevations.
However, subsequent analyses have cast doubt on this assessment, instead proposing that the two preserved proximal tarsals are the fibulare and intermedium, and that Limnoscelis possessed an unfused tibiale along with these elements. The absence of the tibiale has been attributed either to poor preservation (possibly due to being cartilaginous), or to being displaced and misidentified as one of the distal tarsals. This differs from other diadectomorphs in the family Diadectidae, which possessed an astragalus consisting of a fused tibiale, intermedium, and proximal centrale, similar (and possibly homologous) to the astragalus or talus bone found in amniotes.
They are commonly in diameter, but specimens as large as have been observed. There is less variety in their composition at any one volcanic centre than in the case of the lithic blocks, and their composition indicates the type of magma being erupted. Agglomerates are typically found near volcanic vents and within volcanic conduits, where they may be associated with pyroclastic or intrusive volcanic breccias. Older (pre-1970) publications, particularly in Scotland, referred to any coarse-grained volcaniclastic rock as 'agglomerate', which led to debris flow deposits, talus deposits and other types of breccia being mistaken for vents.
Recovery of the widely scattered remains of the victims was extremely challenging due to the difficult terrain at the crash site. At the base of the almost perpendicular cliff where the aircraft hit, movement was hindered by a wide talus of weathered, fragmented rock and large boulders, all piled loosely on a steep slope. Mountaineers doing the recovery work also had to be constantly wary of rock falls that might be triggered by the activities of those above them on the cliff face. Cold weather and occasional snow also played a role in impeding recovery efforts.
On 7 July Prince Wrede received intelligence of the Convention of Paris, and at the same time, directions to move towards the Loire. On 8 July Lieutenant General Czernitscheff fell in with the French between Talus-Saint-Prix and Montmirail; and drove them across the Morin, towards the Seine. Previously to the arrival of the IV (Bavarian) Corps at Château-Thierry; the French garrison had abandoned the place, leaving behind it several pieces of artillery, with ammunition. On 10 July, the Bavarian Army took up a position between the Seine and the Marne; and Prince Wrede's Headquarters were at La Ferté-sous-Jouarre.
The inferior transverse ligament of the tibiofibular syndesmosis is a connective tissue structure in the lower leg that lies in front of the posterior ligament. It is a strong, thick band, of yellowish fibers which passes transversely across the back of the ankle joint, from the lateral malleolus to the posterior border of the articular surface of the tibia, almost as far as its malleolar process. This ligament projects below the margin of the bones, and forms part of the articulating surface for the talus. It is not included in Terminologia Anatomica, but it still appears in some anatomy textbooks.
A collared pika in Hatcher Pass, Alaska Collared pika colonies are mainly found in the mountain regions and they typically inhabit rock slides near areas of vegetation and fields of meadows. Due to these talus sites, the species’ range distribution is broken into several condensed areas. Their homes have a range of about 30 m in diameter with caches and dens distancing from 30 to 70 m. The way organisms respond to climate change can be a distinct and peculiar characteristic, so patterns between closely related species, such as the collared pika and the American pika, are important.
Collared pikas generally mate with their nearest neighbors and are believed to be facultatively monogamous, but they have also been predicted to participate in polygynandry and reproduce with multiple partners, because males often travel to territories of several females during the spring before mating season begins. The males receive the females around the end of spring. However, the pinnacle of the mating season arises in May and early June. Collared pikas, both male and female, are reproductively developed at one year of age and give birth to two or three young each year in their nests within the talus.
The north-west section of the walls was protected by a talus and the sides of the motte were scarped to increase their angle, all producing a small but powerful fortification. Further work followed between 1268 and 1277, which added two large towers, a turning-bridge for the gatehouse and further protection to the north-west walls. On Gilbert's death, the castle passed to his widow Joan and around this time it was referred to as Castrum Rubeum, Latin for "the Red Castle", probably after the colour of the Red sandstone defences. Gilbert's son, also named Gilbert, inherited the property in 1307.
Roughly 27,000 years ago (older data gave an age of 18,000 years), Lassen Peak started to form as a dacite lava dome quickly pushed its way through Tehama's destroyed north-eastern flank. As the lava dome pushed its way up, it shattered overlaying rock, which formed a blanket of talus around the emerging volcano. Lassen rose and reached its present height in a relatively short time, probably in as little as a few years. Lassen Peak has also been partially eroded by Ice Age glaciers, at least one of which extended as much as from the volcano itself.
The deposits also contain large amounts of quartz, especially pyroxene-rimmed quartz crystals, with sparse appearance of olivine and calcic-plagioclase xenocrysts. At dome E, the penultimate dome to be produced, non-bedded deposits with fine, granular pieces to blocks with lengths of up to occur, and many of the larger blocks have internal fractures. Domes D, C, and A have compositions that are extremely similar to dome F; dome B, too, is similar, but also has pumice deposits and mafic inclusions. At dome E and dome D, there are also talus blocks as large as in length.
A red-figure pottery (terracotta) lekythos in Kerch style, depicting a nymph and satyr playing at knucklebones, with two Eros figures (standing near Aphrodite) offering laurel wreaths of victory to the nymph and to a youth, c. 350 BC The talus bones of hooved animals (also known as astragali) are found in archaeological excavations related to the period starting from 5000 B.C. much more frequently than other bones. Astragalus, being almost symmetric, has only four sides on which it may rest and is an early example of the game of chance. Knucklebones are believed to be an early precursor of the dice.
The scenic attractiveness of the Park, in particular, has attracted growing numbers of visitors from all parts of the world, with tourism operators now offering excursions through, and into, the Park. Numerous hiking trails intrude into the park from the Dempster corridor (a 1-km strip alongside the highway exempt from the park). Along this strip is an interpretive centre, open in summer, which provides visitors with necessary resources for accessing the backcountry and interpretive programs for understanding it, as well as several car camping sites. There are three designated backcountry campgrounds: Grizzly, Divide, and Talus Lakes.
The treatment of pilon fractures depends on the extent of the injury. This includes the involvement of other bones such as the fibula and the talus, involvement of soft tissue, and the fracture pattern. Treatment strategies and fixation methods used include internal and external fixation, as well as staged approaches, with the aim of reducing the fracture, reconstructing the involved bones and restoration of articular surface congruence, with minimal insult to soft tissues. Appropriate wound management is important to reduce the high rate of infectious complications and secondary wound healing problems associated with open pilon fractures.
The Denis Julien Inscription is an incised carving on a rock face in a side canyon of the Green River north of Canyonlands National Park in southwestern Grand County, Utah, United States. The site is about to the east of the Green River in Hell Roaring Canyon, at the top of a talus slope. The inscription was left by trapper Denis Julien in 1836, when he was one of the few Europeans in southern Utah. The panel reads: > D. Julien > 1836 > 3 mai A boat with a mast is depicted to the right of the lettering, with a bird-like object below.
Tool marks on the ceiling and pillars clearly illustrate that the modifications served dual purposes, to providing a living space and to facilitate the removal of rock which was discarded down a talus slope. The floor is covered with soil, a mix of ash from fires, fine sand, silt, and locally fragmented rock to a depth of approximately which lies in seven distinct horizontal stratigraphic layers. Completely open to the north and south, construction has left the shelter entirely protected from rainfall. The rock shelter features prehistoric paintings of fish, including the Barramundi, wallabies, crocodiles, people and spiritual figures.
The creek's steep catchment area of 3.3 km2, with headwaters at the 1720 m elevation, 300 m southeast of the summit of Brunswick Mountain. Diorite cliffs flank the course of the creek, between the 900m and 1200 m elevation, with the rocks of the basin part of the Gambier Group. Much of the creek's course is a bedrock canyon, with talus and rockslide debris notable in its upper course, especially on the south side. Prior to the washout of 1981, there had been no debris fan on the waterfront, afterwards the resulting debris fan was 14,100 sq m.
It can generally be separated from A. pedatum by the shape of the ultimate segments (the smallest divisions of the leaf), and by its habitat on thin, exposed serpentine soils rather than in rich woodlands. It more closely resembles A. aleuticum; however, the stalks of the ultimate segments and the false indusia are longer and the spores larger. Due to its limited distribution and similarity to other Adiantum species within its range, little is known of its ecology. It thrives on sunny, disturbed areas where ultramafic rock is covered with thin soil, such as road cuts, talus slopes, and asbestos mines.
The type specimen of A. viridimontanum was collected from a talus slope at the old asbestos mine on Belvidere Mountain on August 28, 1985. The sequencing of several chloroplast DNA loci has revealed that the A. viridimontanum chloroplast genome most closely resembles that of A. aleuticum, suggesting that A. aleuticum was the maternal parent of A. viridimontanum. In 2015, Christopher Fraser-Jenkins treated it as a subspecies of a broadly defined A. pedatum as A. pedatum subsp. viridimontanum, arguing that the morphological similarity among members of the complex should outweigh the biological species concept in defining the boundaries of the species.
However, the species has also been observed at lower elevation rocky sites. During the spring, summer, and autumn they predominantly roost at emergent rock-outcrops such as cliffs, bluffs, shale barrens, and talus slopes, but also man-made structures, including buildings, joints between segments of cement guard rails, turnpike tunnels, road-cuts, and rip-rap covered dams. The largest populations of Myotis leibii have been found in New York, Pennsylvania, West Virginia and Virginia. (red list) The total count of individuals across all known hibernacula is only 3,000, with roughly 60% of the total number from just two sites in New York.
With a global uprising in process and the Presidential Palace in London in resistance hands, U.P. officials convince Pinnacle Command to order his troops to surrender, on the condition that they are allowed to return to Elia and prevent it for being completely conquered. Earth is named a United Planets protectorate, and the U.P. Council names Jacques the planet's acting president. Pinnacle Command is taken to Weber's World to stand trial for crimes against humanity. At Legion headquarters on Talus, Bounty tries to apprehend Sade and secure the billion-credit bounty on her head, but Sade critically injuries her in a shootout.
Talus cones produced by mass wasting, north shore of Isfjord, Svalbard, Norway. Mass wasting is the geomorphic process by which surface material move downslope typically as a mass, largely under the force of gravity As rivers flow down steeply sloping mountains, deep channel incision occurs as the river's flow wears away the underlying rock. Large channel incision progressively decreases the amount of gravitational force needed for a slope failure event to occur, eventually resulting in mass wasting. Removal of large amounts of surface mass in this fashion will induce an isostatic response resulting in uplift until equilibrium is reached.
From the south it is an almost perfect cone, and with fresh snow covering the peak, it is a sight admired by many tourists. The summit is easily climbed from Sjodalen valley either from Hindsæter Mountain Lodge, which is the longer route, or from the Russa/Sjoa confluence. Both ways the route will start in low birch forest and gradually enter long talus slopes and plains with many snow patches in the summer. In the winter, the summit is easily reached, but one should be very wary about the proximity of the northern wall, falling 500 m into Nautgarden.
Flowers in an alpine meadow at Copper Mountain, Colorado Alpine tundra is a complex of high-elevation meadows, fell (barren) fields, and talus or scree (rock) slopes above treeline. Depending on latitude, treeline occurs between in the United States, and in Canada. Grasses and sedges dominate the meadow communities, and fens (a type of wet meadow) and willows exist in wet soils. Vegetation in the alpine zone is similar to that in the Arctic: 47% of the plant species in the alpine zone of the Beartooth Mountains in Wyoming and Montana are also found in the Arctic.
The Argo then reached the island of Crete, guarded by the bronze man, Talos (Talus). Talos had one vein which went from his neck to his ankle, bound shut by a single bronze nail. According to Apollodorus, Talos was slain either when Medea drove him mad with drugs, deceived him that she would make him immortal by removing the nail, or was killed by Poeas's arrow (Apollodorus 1.140). In the Argonautica, Medea hypnotized him from the Argo, driving him mad so that he dislodged the nail, ichor flowed from the wound, and he bled to death (Argonautica 4.1638).
Glacial drift deposited by this glacier covers almost all of the region, but none is found on Tumtum Mountain itself, and the mountain shows no evidence of glacial erosion, so it must be younger than this last regional glaciation. Geologists estimate its age at around 70,000 years. The rock of Tumtum Mountain is a very fine-grained light buff to gray dacite, with silica content of 68%, fairly typical and similar to that found in the lava domes of Mount St. Helens. The volcanic cone of Tumtum Mountain consists of talus and fragments of this dacite surrounding the lava dome itself.
Until 1975, no Canadian museum had its own collection of Burgess Shale fossils. With the work of the GSC and its associates, the shale was rising to prominence, and in 1975 the Royal Ontario Museum (ROM) obtained permission from the National Parks authority, Parks Canada, to collect fossils from talus material in order to develop its own display. Parks Canada would redirect other museums' requests for material to the ROM, so the 1975 collection team gathered ample specimens to meet the anticipated teaching and display requirements. As well as 7750 specimens, this expedition yielded evidence that further fossil outcrops existed up-slope, and in 1981 a five- year reconnaissance program begun.
Its weakest part (i.e., the part most liable to yield from overpressure) is the joint between the talus and navicular, but this portion is braced by the plantar calcaneonavicular ligament a.k.a. spring ligament, which is elastic and is thus able to quickly restore the arch to its original condition when the disturbing force is removed. The ligament is strengthened medially by blending with the deltoid ligament of the ankle joint, and is supported inferiorly by the tendon of the Tibialis posterior, which is spread out in a fanshaped insertion and prevents undue tension of the ligament or such an amount of stretching as would permanently elongate it.
Talus at the bottom of Mount Yamnuska, Alberta, Canada The region of Turkestan is present in central Asia between the Gobi Desert and the Caspian Sea, and comprises Xinjiang, Kazakhstan, Kyrgyzstan, Tajikistan, Turkmenistan, and Uzbekistan. The Turkestan red pika is found in the mountains in western Xinjiang in China, and sporadically in the central Asian mountains such as the Pamir Mountains in Tajikistan, and the Tien Shan Mountains in southeastern Uzbekistan, Kyrgyzstan, and southeastern Kazakhstan. It is also probably found in northern Afghanistan. It is considered to be commonly found in the Iskanderkul Lake area of Tajikistan, and the Great Alma-Ata Lake area in Kazakhstan.
Both males and females have been observed to mark corners of stones mostly located near the center of their home territory, from April to December, by rubbing their neck glands against them. The female's fecundity is low, as with other pikas inhabiting talus piles, and the size of litters decreases as the elevation increases. A.F. Potapkina observed a seasonal increase in the number of offspring per litter. On average, the female of the western Altai Mountains produces two litters, while in the northwestern Altai and the western Sayan Mountains she produces 2.7 litters—with 10% producing up to three litters in the latter case.
Following the film's release, there were initial plans for a sequel with Johnson to return as Mathayus and go up against a new villain, Sargon, but these plans eventually fell through and the project was shelved. A direct-to-video prequel, The Scorpion King 2: Rise of a Warrior, was released in 2008 with Michael Copon as Mathayus and Randy Couture as Sargon. A sequel, The Scorpion King 3: Battle for Redemption, was released in 2012 with Victor Webster as Mathayus and Billy Zane as the villain, King Talus. The fourth film in the franchise, The Scorpion King 4: Quest for Power, was released in 2015.
Angel Falls (; Pemon language: Kerepakupai Meru meaning "waterfall of the deepest place", or Parakupá Vená, meaning "the fall from the highest point") is a waterfall in Venezuela. It is the world's highest uninterrupted waterfall, with a height of and a plunge of . The waterfall drops over the edge of the Auyán-tepui mountain in the Canaima National Park (Spanish: Parque Nacional Canaima), a UNESCO World Heritage site in the Gran Sabana region of Bolívar State. The height figure, , mostly consists of the main plunge but also includes about of sloped cascade and rapids below the drop and a high plunge downstream of the talus rapids.
Often, every joint in a patient with arthrogryposis is affected; in 84% all limbs are involved, in 11% only the legs, and in 4% only the arms are involved. Every joint in the body, when affected, displays typical signs and symptoms: for example, the shoulder (internal rotation); wrist (volar and ulnar); hand (fingers in fixed flexion and thumb in palm); hip (flexed, abducted and externally rotated, frequently dislocated); elbow (extension and pronation) and foot clubfoot and less commonly congenital vertical talus . Range of motion can be different between joints because of the different deviations. Some types of arthrogryposis like amyoplasia have a symmetrical joint/limb involvement, with normal sensations.
The New Preston CDP includes the entire northwestern quadrant of the town of Washington, including the villages of New Preston and Marbledale, as well as Mount Bushnell and Meeker Swamp. The CDP has a total area of , of which are land and , or 6.47%, are water. The dominant geographic feature of New Preston is Lake Waramaug, which is situated just north of the New Preston village center and is the headwaters of the East Aspetuck River, which runs through the village center and over New Preston Falls. The terrain is characterized by steep hills and narrow valleys, with a preponderance of talus slopes and ledge rock.
Arabidopsis lyrata is found largely in subarctic or subalpine environments with thin soils, such as rock faces, eskers and talus slopes, or exposed coastal zones. Individual plants may form solitary rosettes, and are able to reproduce asexually through clonal patches. Lastly, Arabidopsis does not survive in agro-ecosystems in which weeds are rampant; it performs best under low competition and therefore has a life cycle that depends on germination, growth, and the setting of seeds in a very short amount of time before other species of plants can prevent light access. Arabidopsis lyrata has a circumpolar distribution, meaning it is found across northern and central Europe, Asia, and North America.
The hill is formed from a succession of mudstones and siltstones laid down by turbidity currents during the Ordovician Period. The main ridge is developed in rocks of the Ceiswyn Formation assigned to the Ogwen Group and dating from around 457 to 454 million years ago. A near vertical cleavage is developed in the steeply southeasterly dipping strata.British Geological Survey 1:50,000 map sheet 149 Cader Idris & accompanying memoirBGS ‘Geology of Britain’ viewer Talus slopes (scree) lie beneath the main cliff, the massive landslip of part of which some time after the last ice age blocked the valley and is responsible for the presence of Tal-y-llyn Lake.
Huge slopes made of fractured basalt talus are visible beneath many of the ledges; they are particularly noticeable beneath Mount Tom, Whiting Peak, and Deadtop along the Mount Tom State Reservation park road, or along Metacomet-Monadnock Trail on the summit crest gazing down. The basalt ridges are the product of several massive lava flows hundreds of feet deep that welled up in faults created by the rifting apart of North America from Eurasia and Africa. These basalt floods of lava happened over a period of 20 million years. Erosion occurring between the eruptions deposited deep layers of sediment between the lava flows, which eventually lithified into sedimentary rock.
Bridal Veil Falls, with Luna Island to the left The Bridal Veil Falls is the smallest of the three waterfalls that make up Niagara Falls. It is located on the American side (in New York State); Luna Island separates it from the American Falls and Goat Island separates it from the Horseshoe Falls. The Bridal Veil Falls faces to the northwest and has a crest wide. Luna Island being very small, the Bridal Veil is similar in appearance to the American Falls, starting with a vertical fall of , followed by the water violently descending the talus boulders to the Maid of the Mist pool below.
A hiking destination popular among local college students, Bare Mountain offers a 270° vista over the surrounding valleys to the north and south, and a bird's eye view across Mount Norwottuck and the eastern peaks of the Holyoke Range. Also visible from the top are the Round Mountain quarry and the campuses of the University of Massachusetts Amherst and Hampshire College to the north and Westover Joint Air Reserve Base to the south. A prime example of a basalt talus slope is located on the east side of the mountain, along the Metacomet- Monadnock Trail. The next peak to its west is called Mount Hitchcock.
The human navicular is not a commonly broken bone but it breaks due two reasons. The first mechanism is a stress fracture which happens commonly in athletes and the other mechanism is a high energy trauma. The navicular bone is a keystone of the foot: it is part of the coxa pedis and articulates with the talus, first, second and third cuneiform, cuboid and calcaneus. It plays an important role in the biomechanics of the foot helping in inversion, eversion and motion; it is a structural link between midfoot and forefoot and it is part of the longitudinal and transverse arch of the foot.
In this area, however, the cave ceiling lowers to a point where it falls in level with the surface, preventing access to the deposit beneath. In the area north-east of the main chamber, the deposit expands into a low laying ante-chamber of unknown extent due to the sand filling it. By the end of the 2011 field season about 19.5 m² of interior cave has been dug during the Blombos Cave excavations. Blombos Cave's outer talus forms a gently sloping platform of about 23 m² that extends 4–5 meters southwards, before the terrain abruptly drops down towards the shoreline that lies some 34.5 meters below the cave entrance.
The only sites in Wisconsin are "the Western Coulee and Ridges Ecological Landscape in western Grant County and are within a few miles of the Mississippi River".Agific Talus Slopes , Wisconsin Department of Natural Resources, Retrieved July 24, 2007Western Coulee and Ridges Ecological Landscape , Wisconsin Department of Natural Resources, Retrieved July 24, 2007 The great majority of the protected sites are closed to the general public, and in fact, are notably undocumented on the net, in order to keep them out of the eye of those who would vandalize them. One place that can be visited, however, is Bixby State Preserve, in southwestern Clayton County, Iowa.
Osasuna hit back for stunning win; ESPN Soccernet, 11 May 2011 His injury was not as serious as initially expected though.El susto de Nelson se queda en luxación del astrágalo (Nelson scare just a talus bone dislocation); Marca, 12 May 2011 (in Spanish) Nélson spent the first part of 2011–12, with Betis again in the top level, recovering from his condition. On 4 December 2011, in one of his first bench appearances, he was caught on camera talking to his previous team Osasuna's assistant manager Alfredo, leading to rumours that he was filtering his team's lineup to the opposition, which was denied by both parties.
The front line was close to the bottom of the forward (south-facing) slope of a valley between the Maricourt and Montauban ridges and the German front line was further up the slope. Maricourt Ridge declines to the east into the Hardecourt valley which contains the woods of Bois d'en Haut and Bois Favière. Beyond Montauban on the crest of the ridge lies Caterpillar Valley, beyond which are the Ginchy–Pozières ridges. A valley containing Carnoy divides into a northern branch with a pre-war light railway known as Railway Valley with a long tree plantation known as Talus Boisé along the eastern slope.
The way was cleared for the left-hand battalion, which ran up Train Alley and overran the machine-gun nest. The advance of the brigade continued, reached Glatz Redoubt at and gained touch with the 89th Brigade. The 90th Brigade had assembled west of Maricourt at and at the two leading battalions advanced in lines of companies, each company making lines of half-platoons which advanced in files, with the third battalion following closely. The battalions moved forward east of Talus Boisé which was sheltered by Railway Valley and further on, the infantry were protected by a smoke screen along Dublin Trench, raised by the leading brigades.
Rising 150-200 feet (45-60 m) above the low terrace of Green Bay, the steep carbonate cliffs and outcrops support numerous rare land snails including the cherrystone drop snail (Hendersonia occulta), a state-threatened species. Aspen, sugar maple, red oak, hemlock, and white cedar grow out of the talus affording complete shade to the escarpment maintaining the cool and damp conditions, which support a lush growth of mosses. The unique site conditions also support such uncommon species as climbing fumitory, mountain maple, bulbet fern, common polypody, and fragile fern. Above the escarpment is a dry- mesic forest of red and white pine with red oak.
Beacon Hill, open to hiking, picnicking, snowshoeing, bird watching, and other passive pursuits, is isolated from the surrounding suburban areas of Branford and East Haven by salt marsh, riverway, and other wetlands. The hill is steep, with talus slopes in several locations, and offers scenic vistas of Long Island Sound and protected salt marsh from a number of outlooks. Several hiking trails cross the property, most notably the Branford Trail, which loops around the circumference of the town of Branford, passing through a number of scenic conservation areas. Short Beach, also a Branford Land Trust property, lies 1 mile (1.6 km) to the south of Beacon Hill along the Branford Trail.
Talus MB-H tractor The previous station was located from the launching point, with its consequential launch taking on average 12–15 minutes depending on traffic conditions. Local residents around the existing lifeboat station complained of shaking every time a launch was undertaken. Llandudno was scheduled to gain a new Shannon class lifeboat in 2015, but the existing lifeboat station was too small to house it. In previous years, a number of attempts had been made to relocate the lifeboat station without success, due to planning complaints raised by local hoteliers who do not want a lifeboat station interrupting the view in front of their hotel.
Flora of North America, Calochortus persistens Calochortus persistens grows at about nine sites scattered on the Gunsight- Humbug Ridge in Siskiyou County, California, and in one population of just a few individuals on Bald Mountain near Ashland in Jackson County, Oregon.USFWS. (2007). Species Assessment and Listing Priority Assignment FormCalflora taxon report, University of California @ Berkeley, Calochortus persistens Ownbey Siskiyou mariposa lily Calochortus persistens grows on rocky slopes in acidic soils and talus. This is a perennial herb producing an unbranching stem around 10 centimeters tall. There is generally one basal leaf about 20 centimeters long which persists in flowering, and one smaller leaf higher up on the stem.
Replica Roman astragali Astragali used for gaming in Mongolia Astragalomancy, also known as astragyromancy, is a form of divination that uses dice specially marked with letters or numbers. Originally, as with dice games, the "dice" were knucklebones or other small bones of quadrupeds. Marked astragali (talus bones) of sheep and goats are common at Mediterranean and Near Eastern archaeological sites, particularly at funeral and religious locations. For example, marked astragali have been found near the altar of Aphrodite Ourania in Athens, Greece, suggesting astragalomancy was performed near the altar after about 500 BC. Also known as cleromancy, the practice of contacting divine truth via random castings of dice or bones stretches back before recorded history.
Isfjord, Svalbard, Norway, showing angle of repose for coarse sediment The angle of repose is sometimes used in the design of equipment for the processing of particulate solids. For example, it may be used to design an appropriate hopper or silo to store the material, or to size a conveyor belt for transporting the material. It can also be used in determining whether or not a slope (of a stockpile, or uncompacted gravel bank, for example) will likely collapse; the talus slope is derived from angle of repose and represents the steepest slope a pile of granular material will take. This angle of repose is also crucial in correctly calculating stability in vessels.
Mount Kineo, with 700-foot (200 m) cliffs rising straight up from Moosehead Lake, has attracted visitors for centuries, from early American Indians (Red Paint People), to later tribes seeking its rhyolite to make stone tools, Penobscots and Norridgewocks, the Abenaki bands who battled here with their enemy the Mohawks, to 19th-century "rusticators" traveling by railroad and steamboat and today's hotel guests. Various species dwell among its cliffs and talus slopes, including peregrine falcons and rare plants. The Moosehead region includes the headwaters of the Kennebec, the West Branch of the Penobscot, the Piscataquis, the Pleasant, and the Saint John rivers. Henry David Thoreau and other 19th-century visitors remarked on the beauty of the area.
This is achieved by placing the index finger of the operator on the medial malleolus to stabilize the leg and levering on the thumb placed on the lateral aspect head of the talus while abducting the forefoot in supination. Forcible attempts at correcting the heel varus by abducting the forefoot while applying counter pressure at the calcaneocuboid joint prevents the calcaneus from abducting and therefore everting. 2\. Foot cavus increases when the forefoot is pronated. If cavus is present, the first step in the manipulation process is to supinate the forefoot by gently lifting the dropped first metatarsal to correct the cavus. Once the cavus is corrected, the forefoot can be abducted as outlined in step 1. 3\.
Continuous areas and narrow filaments of light-gray ejecta extend from the crater across the dark mare surface through 270°, but are entirely absent in the southern 90° sector. Within the crater, dark material occurs on the southern crater wall while the remaining walls are bright. This crater probably resulted from the impact of a projectile traveling from south to north along an oblique trajectory. Its pattern of ejecta distribution is similar to that of small craters produced by the impact of missiles along oblique trajectories at the White Sands Missile Range, NM. Some observers postulate that the dark material is a talus deposit of mare material that has fallen into the crater.
Over time the overhangs fall into the pit and the crater fills with talus from the collapsing sides and roof. A middle- aged pit crater is cylindrical but its rim will continue to collapse, resulting in the crater's expanding outward until it resembles a funnel or drain—narrower at the bottom than the top. While pit craters and calderas form through similar processes, the former term is usually reserved for smaller features of a mile or less in diameter. The term "pit crater" was coined by C. Wilkes in 1845 to describe craters along Hawaii's East Rift Zone.Wilkes, C., 1845. Narrative of the United States Exploring Expedition during the years 1838, 1839, 1840, 1841, and 1842, Vol. 4.
Driftless Area National Wildlife Refuge Comprehensive Conservation Plan, U.S. Fish and Wildlife Service, Retrieved July 23, 2007 Superb site, but Beware, this is a very long PDF document The Driftless Area National Wildlife Refuge was primarily carved out of the Upper Mississippi River National Wildlife and Fish Refuge in order to protect these species and their associated ecosystems. Isolated relic stands of pines and associated northern vegetation are found in some locations where algific talus slopes are present. These trees survive in the cooler Microclimate produced at these locations outside of their current range further north. A particularly noteworthy annual event is the rising of fishflies, a kind of mayfly endemic to the Mississippi valley in the region.
Donaueschingen lies in the Baar basin in the southern Black Forest at the confluence of the Brigach and Breg rivers— the two source tributaries of the Danube— from which the town gets its name. This is today considered the true source of the Danube. Source of the Donaubach in Donaueschingen (historically considered the source of the Danube) An enclosed karst spring on the castle grounds, the source of the "Donaubach", is known as the source of the Danube. The municipal area extends continuously from the granite and gneiss of the Black Forest through the Triassic formations of the Schwarzwald-Baar talus to the Swabian Alb, and exhibits all strata of the southern German cuesta country.
Excavations began during the summer of 1958 on 16 sites. A thesis emerged that prehistoric people living permanently on the highlands south of Glen Canyon and on the Cummings Mesa, farmed the Lower Glen Canyon on a seasonal basis, and gathered raw materials. To prove this thesis of seasonal habitation, criteria such as architectural units, locations of trail systems, occurrence of ceremonial structures, prevalence of burials, and position of natural and cultural strata were investigated. Four types of sites are described in the survey, classified as either open sites situated on rock terraces; talus sites on broken material below cliffs; shelter sites in protected areas under overhanging cliffs; and cliff sites beneath ledges or in caves and canyon walls.
The lavas, intrusive volcanic rocks, and volcanic vents have largely gone unaltered by erosion or other geological processes besides sparse mineralization as a result of volcanic exhalative processes, though there are tiny amounts of specular hematite and malachite in cracks among lava flows. Heavily eroded by glaciers, which no longer exist on Diamond Peak, the mountain has several cirques from glacial erosion, some of which have talus deposits due to Holocene glacial motion. Glaciers also placed both lateral and ground moraines along the lower to middle elevations of the wilderness area, unlayered pebble deposits interbedded with sand and rock. These deposits have very few weathering rinds, corresponding to their production during the late Pleistocene.
Aquilegia longissima, the long-spur columbine, is a rare perennial herb that is native to northern Mexico, Trans-Pecos Texas and southern Arizona. In the original species description by Asa Gray in 1883, Aquilegia longissima is distinguished from the shorter-spurred golden columbine Aquilegia chrysantha based on the extremely long spur over 10 cm long, narrow spatulate petals, and very slender spurs that usually hang straight down. The plants typically flower in the fall after monsoon rains and are found in oak-pine-juniper woodlands in shaded canyons near intermittent streams or on talus slopes. William Trelease hypothesized in 1883 that the most likely pollinator of A. longissima would be the giant sphinx moth, Cocytius antaeus.
Some of the measures taken to counter escalade included the digging of moats (which prevented ladder-bearing soldiers from reaching the base of a wall), the construction of machicolations (which facilitated attacks on enemy soldiers while they climbed), and walls incorporating a talus feature. Badajoz in 1812 Because of the difficulties involved, escalade was usually very costly for the attackers. Two critical factors in determining the success or failure of escalade were the number of ladders and the speed with which they could be arranged. A slow attack gave the defenders too much time to pick off the attackers with arrows, while having too few ladders meant that the number of troops would be insufficient to capture the battlements.
Antennaria soliceps is a rare species of flowering plant in the daisy family known by the common name Charleston Mountain pussytoes. It has been found only on Mount Charleston in Clark County in the southern part of the US state of Nevada.Biota of North America Program 2014 county distribution map Antennaria soliceps is a small plant rarely growing more than 2 inches (5 cm) from the ground, spreading by means of horizontal stems running along the surface of the ground. All known plants discovered to date are female, the species apparently relying exclusively on asexual reproduction. It grows on talus slopes near the tree line in the mountains, 3000–3400 meters (10,000–11,300 feet) above sea level.
Chamaenerion latifolium (formerly Epilobium latifolium, also called Chamerion latifolium) is a species of flowering plant in the evening primrose family known by the English common names dwarf fireweed and river beauty willowherb. It has a circumboreal distribution, appearing throughout the northern regions of the Northern Hemisphere, including subarctic and Arctic areas such as snowmelt-flooded gravel bars and talus, in a wide range of elevations.Flora of the Canadian Arctic Archipelago This is a perennial herb growing in clumps of leaves variable in size, shape, and texture above a woody caudex. The leaves are 1 to 10 centimeters long, lance-shaped to oval, pointed or rounded at the tips, and hairy to hairless and waxy.
Fir Creek, a Bull Run River tributary Columbia River basalts, 10 to 20 million years old, that underlie much of the Bull Run watershed are exposed near the bottoms of steep canyons along the river and its tributaries. In the western half of the watershed, the Rhododendron formation, rich in sediments, overlies the basalt, and later volcanic flows of basalt and andesite overlie both older formations. Areas of thick talus occur in the eastern part of the watershed at elevations higher than above sea level, and north-facing slopes above show evidence of glaciation. Over many centuries, streams in the watershed have carved canyons through the Rhododendron formation to the level of the basalt.
The Niagara Escarpment represents the largest contiguous stretch of primarily forested land in south-central Ontario. The biosphere reserve includes the greatest topographic variability in southern Ontario, with habitats ranging over more than in elevations and including Great Lakes coastlines, cliff edges, talus slopes, wetlands, woodlands, limestone alvar pavements, oak savannahs, conifer swamps and many others. These habitats collectively boast the highest level of species diversity among Canadian biosphere reserves, including more than 300 bird species, 55 mammals, 36 reptiles and amphibians, 90 fish and 100 varieties of special interest flora. The Niagara Escarpment stretches along the entire eastern edge of the Bruce Peninsula, a globally significant area covering at the tip of which lies Bruce Peninsula National Park.
The Allegheny Mountain dusky salamander is one of the known predators of the Chittenango ovate amber snail. Predators may include beetles and sciomyzid fly larvae, many of which specialize in feeding upon snails. Other potential predators may include the northern two-lined salamander (Eurycea bislineata), northern dusky salamander (Desmognathus fuscus), and Allegheny Mountain dusky salamander (Desmognathus ochrophaeus), which are common in the talus and on the ledges, as well as various small mammals or passerine birds such as robins and pigeons, which are often seen in or near the habitat. Although predation does not appear to be a limiting factor at this time, its potential impact on a low or stressed population is unclear.
Huntington Ravine is a glacial cirque on Mount Washington in the White Mountains of New Hampshire. It is named for Joshua H. Huntington, the Principal Assistant to State Geologist Charles H. Hitchcock (1836–1919) for the Geological Survey of New Hampshire. Of the four major cirques on Mount Washington (Tuckerman and Huntington ravines, Oakes Gulf, and the Great Gulf), it has the steepest and highest headwall. Only one hiking trail ascends Huntington Ravine toward Mount Washington's summit; that trail, the Huntington Ravine Trail, crosses a boulder field, ascends a talus fan, and winds steeply up the center of the cirque's headwall, requiring several tricky scrambling moves that may be intimidating for less-experienced (or more acrophobic) hikers.
The Iowa Pleistocene Snail was believed extinct until it was discovered on algific talus slopes in northeast Iowa in 1955. Placed on the Endangered Species List in 1977, Congress created the Driftless Area National Wildlife Refuge in 1989 to protect this species, as well as threatened and some relict species.Driftless Area National Wildlife Refuge, United States Fish and Wildlife Service, Retrieved July 24, 2007 Much of this refuge was carved out of pre-existing protected areas, most notably the Upper Mississippi River National Wildlife and Fish Refuge. The Northern monkshood is a threatened wildflower in the buttercup family (Ranunculaceae) occurring in the Driftless Area as well as in New York State and receives similar protection.
During the 20th century, scientists thought they had identified a new glacier, which they named Milk Creek Glacier, but later studies established that it was an artifact of stagnant ice that had been hidden by debris, and it is no longer considered its own distinct feature. Other geographic features at Jefferson include rock outcrops, steep talus slopes, conifer forests, and alpine meadows. Additionally, a number of rivers drain Mount Jefferson. The northern and northwestern slopes feed the South Fork Breitenbush River, which flows into Detroit Lake, and the eastern side of Detroit Lake also receives water from Whitewater Creek, Russell Creek, and Milk Creek, which flow from the western flank of Mount Jefferson.
Polystichum is a genus of ferns in the family Dryopteridaceae, subfamily Dryopteridoideae, according to the Pteridophyte Phylogeny Group classification of 2016 (PPG I). The genus has about 500 species and has a cosmopolitan distribution. The highest diversity is in eastern Asia, with about 208 species in China alone; the region from Mexico to Brazil has at least 100 additional species; Africa (at least 17 species), North America (at least 18 species), and Europe (at least 5 species) have much lower diversity. Polystichum species are terrestrial or rock-dwelling ferns of warm-temperate and montane-tropical regions (a few species grow in alpine regions). They often are found in disturbed habitat such as road cuts, talus slopes, and stream banks.
Russia currently has the following controlled appellations that correspond to the sorts of grapes: Sibirkovy (Сибирьковый), Tsimlyanski Cherny (Цимлянский чёрный), Plechistik (Плечистик), Narma (Нарма), and Güliabi Dagestanski (Гюляби Дагестанский),J. Robinson "The Oxford Companion to Wine" Third Edition pg 598 Oxford University Press 2006 Krasnostop Zolotovsky (Красностоп Золотовский), Saperavi (Саперави), Platovsky (Платовский), Bastardo Magarachsky (Бастардо Магарачский), Kefesia (Кефесия), Kokur Belyi (Кокур Белый). A Russian wine guide published in 2012 lists 55 wines from 13 wineries, including names such as Fanagoria, Lefkadia, Chateau du Talus, Abrau-Durso, Chateau le Grand Vostock. The market is largely fragmented, and even the market share of leading producers (such as Kuban-Vino or Viktoria TD) is below 3%.
The site is characterized by "extensive alpine tundra, a variety of glacial landforms, glacial lakes and moraines, cirques and talus slopes, patterned ground, and permafrost", and is home to Arikaree Glacier. Habitats include western spruce-fir forest,, lodgepole pine (Pinus contorta) subalpine forest, alpine meadows as well as ponderosa pine (Pinus ponderosa) shrubland. The site is little influenced by human impact and is thus an excellent site to monitor biological, chemical, and physical responses to changes in atmospheric chemistry and climate. The site is administered cooperatively by the U.S. Forest Service and the University of Colorado Boulder's Institute of Arctic and Alpine Research (INSTAAR) for experimental and long-term studies of alpine tundra.
Eucalyptus urnigera is an endemic Tasmanian alpine eucalypt of the sub genus Symphomyrtus and is the dominant eucalypt species at altitudes from on moist but well drained dolerite slopes and talus. It is restricted to the mountains of south eastern Tasmania, the Mount Wellington range, Mount Field and isolated pockets from Tylers Hill near Southport, south of Hobart, north to Alma Tier near Interlaken and Mount Seymour east of Oatlands in central Tasmania and a small population on the eastern side of Maria Island off the east coast. Typically, it is found below the range of E. coccifera (snow gum) and above the mixed and wet sclerophyll forests of the lower slopes although it will grow within both vegetation types.
Erigeron vagus is a high-elevation species of flowering plant in the daisy family known by the common names rambling fleabane. Erigeron vagus is native to the peaks of the western United States where it lives on talus slopes, sometimes above the tree line but other times in open coniferous forests. It has been found in several locations isolated from each other, in eastern California (Sierra Nevada and White Mountains), southern Utah, southern Colorado, northeastern Nevada (Elko County), and northeastern Oregon (Wallowa Mountains).Biota of North America Program 2014 county distribution mapCalflora taxon report, University of California, Erigeron vagus Payson, rambling fleabane Erigeron vagus is a small perennial herb reaching a maximum height of about five centimeters (2 inches), forming a taproot and a branched underground caudex.
The garden is situated on a high ridge south of Mont Blanc, and contains a rockery, alpine pasture, talus slopes, and wetlands. Snow covers the area for 8 to 9 months per year, to a depth of 3-4 metres, disappearing in late June. Plants are identified by a card with family name, gender, species, Italian name, and country of origin. Species include Alnus viridis, Androsace septentrionalis, Arnica montana, Artemisia genipi, Artemisia umbelliformis, Aquilegia alpina, Campanula thyrsoides, Centaurea triumphetti, Eringium burgatii, Eritrichium nanum, Gentiana lutea, Gnaphalium supinum, Leontopodium alpinum, Lilium martagon, Lychnis alpina, Lychnis flos- jovis, Minuartia verna, Nardus stricta, Paeonia officinalis, Peucedanum ostruthium, Potentilla nepalensis, Pulsatilla halleri, Rhododendron ferrugineum, Salix herbacea, Silene elisabethae, Trifolium alpinum, Vaccinium myrtillus, and Veratrum album.
Michael Portnoy's TALUS abstract gambling table, 2007 Portnoy expanded his practice to include choreography, video, installation, sculpture, painting, participatory works and curation. His projects have included Google Office 0.2, a project for the 2010 Taipei Biennial that involved the formation of a think tank called The Improvement League, which operated by improving existing artworks in the Biennial by pruning and hybridizing in a cross between futurology and conceptual horticulture. Portnoy's long-standing investigation of social exchange, and the rules of communication and play, has been conducted through a series of 'abstract gambling' tables for Casino Ilinx (2008) and Filzzungeungewiss (2009); and conversation or inventional games drawing on 17th century universal or taxonomic languages for Fran Spafa Feda (2010); and the game-show format of 27 Gnosis (2012).
As a result, the African origins of crown strepsirhines (including lemurs and lorisoids) is well supported, whereas the African origins of simians has been placed in doubt, possibly giving favor to an Asian origins hypothesis. However, in 2010, Godinot reasserted his view that Algeripithecus was a simian based on its upper molar morphology and hypothesized that this applied to all azibiids, favoring his earlier view that azibiids may be early simians instead of stem lemuriforms. In 2011, Marivaux et al. published an interpretation of recently discovered talus bones of closely related Azibius found at Gour Lazib, which they claimed were more similar to those of living strepsirrhines and extinct adapiforms, not simians, thus reinforcing the strepsirrhine status favored by Tabuce et al.
Flat feet (also called pes planus or fallen arches) is a postural deformity in which the arches of the foot collapse, with the entire sole of the foot coming into complete or near-complete contact with the ground. There is a functional relationship between the structure of the arch of the foot and the biomechanics of the lower leg. The arch provides an elastic, springy connection between the forefoot and the hind foot so that a majority of the forces incurred during weight bearing on the foot can be dissipated before the force reaches the long bones of the leg and thigh. In pes planus, the head of the talus bone is displaced medially and distal from the navicular bone.
The talus, which primarily consists of Middle Stone Age deposit, rock fall and unconsolidated sediments, is stabilized by an area of large, exposed blocks (14 m²). At some stage – and in between the prehistoric occupation of the cave site – these blocks have fallen down from the rock face above, effectively preventing site erosion and allowing sediments to stabilize and accumulate in front of the cave's drip line. Calcium carbonate (CaCO₃) rich ground water seeps in from the cave roof and percolates through the interior sediments, resulting in an alkaline environment with good preservation conditions. The excavated Middle Stone Age deposit in Blombos Cave consists of aeolian (wind-borne) dune sand, blown in through the cave entrance, and roof spall from the cave ceiling.
It represents one of the largest lava domes on Earth, with a height of above its surroundings, and an approximate volume of . Unlike more conventional, conical stratovolcanoes like Mount Shasta or Mount Rainier, Lassen Peak is part of a volcanic center that erupts from different vents, which each remain active for a number of years or decades but often do not erupt from the same vent twice, also known as a monogenetic volcanic field. 2000 years after Lassen's formation, it was surrounded by glaciers which ate away at its spiny protrusions of dacite. Due to glacial erosion from the last local glacial advance, which ceased roughly 15,000 years ago, Lassen's lava dome is now covered in broken rock fragments at the base of crags called talus deposits.
The fern thrives in thin serpentine soils on sunny, disturbed habitats such as roadcuts and talus slopes, in dunite and other ultramafic rocks. Anthropogenic disturbance has removed thicker soils and increased sun exposure in many of these sites; for instance, many of the Quebec stations are in asbestos mines, both abandoned and active. In more natural habitats, frost weathering and erosion may promote rock fall and maintain suitable habitat. A detailed quantitative analysis of habitat preferences has shown that while A. viridimontanum occupies similar habitat to A. aleuticum in northeastern North America (ultramafic ledges, mine dumps, etc.), it also occupies serpentine-influenced northern hardwood forests, where the calcium-rich forest habitats preferred by A. pedatum have been altered by magnesium-rich drainage from ultramafic sites.
The posterior surface is traversed by a shallow groove directed obliquely downward and medialward, continuous with a similar groove on the posterior surface of the talus and serving for the passage of the tendon of the Flexor hallucis longus. The lateral surface presents a triangular rough depression for the attachment of the inferior interosseous ligament connecting it with the fibula; the lower part of this depression is smooth, covered with cartilage in the fresh state, and articulates with the fibula. The surface is bounded by two prominent borders (the anterior and posterior colliculi), continuous above with the interosseous crest; they afford attachment to the anterior and posterior ligaments of the lateral malleolus. The medial surface -- see medial malleolus for details.
The Cumberland Narrows west of Cumberland, Maryland, along Wills Creek, with Haystack Mountain on the left and Wills Mountain on the right. The easy crossing of the rugged Wills Mountain Anticline through this water gap is used by the Western Maryland Scenic Railroad (left), the Old National Road (Alternate U.S. 40) (center, left of the creek), and the CSX Railroad (right). Cumberland is at the eastern entrance to the Cumberland Narrows (or "The Narrows"), a water gap along Wills Creek that crosses the central ridge of the Wills Mountain Anticline at a low elevation between Wills Mountain to the north and Haystack Mountain to the south. Cliffs and talus of the two mountains' Tuscarora quartzite caprock are prominent within the Narrows.
The waterfall and gorge comprise an example of a hanging valley, formed where Taughannock Creek's stream-carved valley meets the deeper glacially carved valley that contains Cayuga Lake. The gorge has continued to retreat westward from Cayuga Lake as easily eroded shale near the fall's base is worn away by the stream, which supports erosion-resistant siltstone and sandstone found in the upper portions of the gorge. Annual freeze and thaw cycles also act upon small faults in the rock, causing large sections to occasionally break away, further expanding the gorge. The gorge supports a "Shale Cliff and Talus" community of plants, including three regionally rare species classified as threatened in New York State: Butterwort (Pinguicula vulgaris), birds-eye primrose (Primula mistassinica) and yellow mountain saxifrage (Saxifraga aizoides).
Snake Pond, a kettle pond along the M&M; Trail on trap rock East Mountain The ridge that forms the spine of the M&M; Trail across Provin Mountain, East Mountain, and the Mount Tom and Holyoke ranges was formed 200 million years ago during the late Triassic and early Jurassic periods and is composed of trap rock, also known as basalt, an extrusive volcanic rock. Basalt is a dark colored rock, but the iron within it weathers to a rusty brown when exposed to the air, lending the ledges a distinct reddish appearance. Basalt frequently breaks into octagonal and pentagonal columns, creating a unique "postpile" appearance. Huge slopes made of fractured basalt talus are visible beneath many of the ledges; they are particularly visible along the Metacomet- Monadnock Trail on Bare Mountain.
On December 7, he was diagnosed with a non-displaced fracture of the posterior talus in his right ankle, an injury requiring surgery and eight to ten weeks of rehabilitation. He returned to action in late March. On November 12, 2016, Hollis-Jefferson scored a then career-high 20 points and tied a career high with 13 rebounds in a 122–104 win over the Phoenix Suns. On December 14, 2017, Hollis-Jefferson scored a career-high 25 points on 10-for-16 shooting in a 111–104 loss to the New York Knicks. He strained his right groin during a 116–91 loss to the Milwaukee Bucks on January 26, returning to action on February 26 against the Chicago Bulls after missing the Nets' previous 11 games.
A paved foot trail leads to Benson Footbridge, a 45-foot (14 m)-long footbridge that allows visitors to cross 105 feet (32 m) above the lower cascade. After a viewpoint of the upper falls, the trail continues to ascend to an elevation of ; it consists of eleven switchbacks which reach a forested talus slope above the falls. The trail then descends to an observation deck (elevation ) overlooking the falls' edge, providing visitors a bird's-eye view of the Columbia Gorge and also of "Little Multnomah", a small cascade slightly upstream from the "upper" falls, which is not visible from ground level. There are a number of trail junctions along the footpaths ascending to the falls' observation deck, which allow access to a trail loop to other nearby waterfalls.
If the first phase succeeded and the attack further west captured Fricourt, XIII Corps was to wheel to the right by pivoting on Favière Wood and Dublin Redoubt. The third phase consisted of an eastwards advance via Bernafay and Trônes woods to the German second position from Falfemont Farm to Guillemont. When the plan was issued in mid-June, the 30th Division dug a new front line trench about closer to the German front line and six communication trenches between Maricourt on the right and Talus Boisé on the left, which was the boundary with the 18th (Eastern) Division. The infantry advance was to be assisted by a heavy artillery barrage which was to fall successively on German defensive lines and a field artillery barrage which was to creep forward.
They eagerly explored the talus and were able to find some more remains including over a dozen flint tools and they described the area as having several beddings of rock falls and breccias. From these discoveries and the fact that Devil's Tower Cave was so close to Forbes' Quarry Cave, where Gibraltar 1, the famous Neanderthal skull, had been found a few years earlier in 1848, they deduced that the cave site had been used by "Prehistoric Man" and that the remains of animal bones and shells were the leftovers of their food. It was clear to them that they had also been cooking these animals, since pieces of burnt bone and charcoal was also found. Between November 1925 and January 1927, the site was further investigated by Dorothy Garrod from Cambridge University at the suggestion of L’Abbe Breuil.
A monograph compact disc of three works for soloist(s) and orchestra, Talus for viola and orchestra, On a Sufficient Condition for the Existence of Most Specific Hypothesis for solo throat-singer and orchestra, and Kaze-no-Oka for biwa, shakuhachi, and orchestra, was released by the Boston Modern Orchestra Project in 2010. Ueno has also written for such ensembles as the So Percussion Group, Bang on a Can All-Stars, San Francisco Contemporary Music Players, Del Sol String Quartet, Prism Quartet, and eighth blackbird. Ueno's compositional approach frequently involves extra- musical modeling, including using images, cultural phenomena, or architecture as the basis for structural decisions, somewhat analogous to the use of architectural proportions in Renaissance music. Kaze-no-Oka, for example, reflects in part the structure of the Japanese architect Fumihiko Maki's like- named project.
Talus cones produced by mass wasting, north shore of Isfjord, Svalbard, Norway. Mass wasting at Palo Duro Canyon, West Texas (2002) A rockfall in Grand Canyon National Park Mass wasting, also known as slope movement or mass movement, is the geomorphic process by which soil, sand, regolith, and rock move downslope typically as a solid, continuous or discontinuous mass, largely under the force of gravity, frequently with characteristics of a flow as in debris flows and mudflows.Britannica Types of mass wasting include creep, slides, flows, topples, and falls, each with its own characteristic features, and taking place over timescales from seconds to hundreds of years. Mass wasting occurs on both terrestrial and submarine slopes, and has been observed on Earth, Mars, Venus, and Jupiter's moon Io. When the gravitational force acting on a slope exceeds its resisting force, slope failure (mass wasting) occurs.
Panoramic view over the park from the Radical Road track Salisbury Crags are a series of cliffs at the top of a subsidiary spur of Arthur's Seat which rise on the west of Holyrood Park. Below the foot of the cliffs is a large and steep talus slope falling to the floor of Holyrood Park with a track known as the Radical Road running in the space between the two. This track was given its name after it was paved in the aftermath of the Radical War of 1820, using the labour of unemployed weavers from the west of Scotland at the suggestion of Walter Scott. On the basis of it simply being the same name, Hugo Arnot derived the name from the first Earl of Salisbury who accompanied Edward III of England on one of his invasions of Scotland.
The valley from an airplane Starting about 2 to 3 million years ago a series of glaciations further modified the area by accelerating mass wasting through ice-wedging, glacial plucking, scouring/abrasion and the release of pressure after the retreat of each glaciation. Severe glaciations formed very large glaciers that tended to strip and transport top soil and talus piles far down glacial valleys, while less- severe glaciations deposited a great deal of glacial till further up in the valleys. At least 4 major glaciations have occurred in the Sierra Nevada; locally called the Sherwin (also called the pre-Tahoe), Tahoe, Tenaya, and Tioga. The Sherwin glaciers were the largest, filling Yosemite and other valleys, while later stages produced much smaller glaciers. The Sherwin may have lasted almost 300 thousand years and ended about 1 million years ago.
Allium parvum is an American species of wild onion known by the common name small onion.Calflora, Taxon Report 222, Allium parvum KelloggUSDA Plants Profile It is native to the western United States where it is a common member of the flora in rocky, dry areas in mountainous areas, especially in talus at elevations of . It is widespread in California, Nevada, Oregon and Idaho, and also reported from western Utah and from extreme southwestern Montana (Ravalli and Beaverhead Counties)Jepson Manual TreatmentFlora of North America v 26 p 271, Allium parvumBONAP (Biota of North America Program) 2014 county distribution map, Allium parvum Allium parvum has a bulb one to two and a half centimeters wide and bears a relatively short scape for an onion species, rarely more than 12 centimeters tall. The two leaves are sickle-shaped.
Since Stargate SG-1 produced 214 episodes, and this episode is the 86th produced from Stargate Atlantis, this makes "The Shrine" the 300th episode produced in the Stargate franchise. When writer Brad Wright was asked to write this episode, he originally came up with two ideas, "The Shrine", and "The Replacements", which was meant to be an episode about where Sheppard's team went missing for six months, and finally returned to see completely different crew in the Atlantis Expedition. However, since the cast change from Amanda Tapping (Samantha Carter) to Robert Picardo (Richard Woolsey) from the beginning of the season, the idea for "The Replacement" was dropped, and Wright went with "The Shrine". The working title of the episode was "The Shrine of Talus", but was changed to "The Shrine", due to clearance issues with releasing the title.
In 1920 the Turkish armies in Eastern Anatolia led by Kazım Karabekir invaded Armenia during the Turkish War of National Liberation and occupied Oltu, a territorial gain which was confirmed in subsequent treaties signed between the Turks and the Soviets. The primary historical sight in Oltu is the castle, which covers the top of a rocky outcrop. Its walls are fortified by large round towers and salients, including an imposing talus at the southwest. A circuit wall once extended from the outcrop to protect a small adjoining settlement. The medieval fortress is the result of two major periods of construction between the 7th and the 11th centuries; major repairs were undertaken by the Turkish Corps of Engineers in 1977. Atop the north tower are the remains of a Georgian hexaconch church in which a fragment of a 7th-century “bilingual” Greek-Armenian inscription was reused in the foundation.
62 Wade Bootes a highly respected Senior Pro was an early adopter of clipless pedals and helped with the move to them. Another criticism of clipless pedals is that they lead to more injuries since the feet can not be readily be freed from the pedals despite their quick release feature. The racer is prevented from either stabilizing his bike by placing one foot on the ground to prevent a crash or brace himself quickly if a crash is inevitable, leading to more frequent and serious crashes involving leg and foot injury. On August 20, 2007 professional BMX racer Bubba Harris completely dislocated ankle at the talus bone in Beijing, China on the official Olympic BMX racing track during the first run of his Time Trial in the "rhythm section", a series of closely but evenly spaced jumps that you use gravity and "body English" to navigate and maintain speed.
While the Horseshoe Falls absorbed the extra flow, the U.S. Army Corps of Engineers studied the riverbed and mechanically bolted and strengthened any faults they found; faults that would, if left untreated, have hastened the retreat of the American Falls. A plan to remove the huge mound of talus deposited in 1954 was abandoned owing to cost, and in November 1969, the temporary dam was dynamited, restoring flow to the American Falls. Even after these undertakings, Luna Island, the small piece of land between the main waterfall and the Bridal Veil, remained off limits to the public for years owing to fears that it was unstable and could collapse into the gorge. Encroachment of urban landscape on the Canadian side Commercial interests have continued to encroach on the land surrounding the state park, including the construction of several tall buildings (most of them hotels) on the Canadian side.
1, G. Pilot ed. Presses de l’École Nationale des Ponts et Chaussées, 1983, p. 133-158Matar, M. et Salençon, J., Bearing capacity of circular shallow foundations, Paris, Foundation Engineering, vol. 1, G. Pilot ed. Presses de l’École Nationale des Ponts et Chaussées, 1983, p. 159-168 or anisotropic soilsSalençon, J. et Tristan-Lopez, A., « Analyse de la stabilité des talus en sols cohérents anisotropes », C.R.Acad.Sc.Paris. t. 290, série Série B, 23 juin 1980, p. 493-496 (lire en ligne)Salençon, J. et Tristan-Lopez, A., « Calcul à la rupture en mécanique des sols: cas des sols cohérents anisotropes », Annales de l'ITBTP, série Sols et fondations, 182, mars-avril, 1983, p. 53-83 (lire en ligne) and also for stability analyses of earth and reinforced soil structures.de Buhan, P. et Salençon, J., « A comprehensive stability analysis of soil nailed structures », European Journal of Mechanics, a, 12, n°3, 1993, p.
Penstemon ,Sunset Western Garden Book, 1995:606–607 the beardtongues, is a large genus of roughly 250 species of flowering plants native mostly to the Nearctic, but with a few species also found in the North American portion of the Neotropics. It is the largest genus of flowering plants endemic to North America. Formerly placed in the family Scrophulariaceae by the Cronquist system, new genetic research has placed it in the vastly expanded family Plantaginaceae. A prominent, often hairy, staminode is the most distinctive feature of this genus, as in this Penstemon rupicola flower Golden-beard Penstemon (Penstemon barbatus) Penstemon bridgesii Bellflower Beardtongue (Penstemon campanulatus) Penstemon confertus Talus Slope Penstemon (Penstemon digitalis) Lowbush Penstemon (Penstemon fruticosus) Davidson's Penstemon (Penstemon davidsonii) Lilac Penstemon (Penstemon gracilis) Hairy Beardtongue (Penstemon hirsutus) Penstemon hirsutus pubescens Pineneedle Beardtongue (Penstemon pinifolius) Littleflower Penstemon (Penstemon procerus) Serrulate Penstemon (Penstemon serrulatus) Prairie-clover (Penstemon speciosus) They have opposite leaves, partly tube-shaped, and two-lipped flowers and seed capsules.
Sign at the boundary of the state-managed Zoar Valley Multiple Use Area The state-managed Zoar Valley Multiple Use Area encompasses a area along an section of the Cattaraugus Creek's Main Branch canyon and a stretch of the smaller South Branch, centered around the confluence of the two streams. The Multiple Use Area is maintained by the New York State Department of Environmental Conservation. In 2007, the state established the Zoar Valley Unique Area, a area which further protects and preserves the entire state-owned length of the gorge's cliffs and bottomlands, in addition to a buffer area along the gorge's upper rim and along several larger side creeks, where sufficient state-owned land is available. The Unique Area contains the majority of the currently known or suspected old-growth forest, all of the riverside floodplain and terrace woodlands, as well as all of the slope, cliff and talus plant communities.
The Commonwealth Commons plan divides the state into five regions, Berkshires, Connecticut River Valley, Central Massachusetts, Southeast Massachusetts, Metropolitan Boston, and Northeast Massachusetts. The Berkshires region includes the Berkshire mountains, from the eastern limit of those mountains to the western boundary of the state. Suggested recommendations and projects for this section include securing protection for the area's major long distance trails (the Appalachian Trail, the Taconic Trails, and the Mahican-Mohawk Trail); creating greenway links between the Taconic Trails and Appalachian Trail; creating new greenway corridors that would link open space parcels within the Berkshires; promoting, protecting, and creating a Housatonic River greenway; creating a bikeway that would run from Connecticut to Vermont and include the Ashuwillticook Rail Trail; and creating and protecting a greenway along the federally designated wild and scenic Westfield River. The Metacomet- Monadnock Trail passing along talus slope The Connecticut River Valley region includes an area from the eastern front of the Berkshires east to western Worcester County.
In 1961, while hunting marmots at a sandstone outcrop on the Anzick family property, about one mile south of Wilsall, Montana, Bill Roy Bray found a stone biface and small human infant bones that were covered with red ocher. In the same area, in May 1968, Ben Hargis and Calvin Sarver of Wilsall, Montana were removing talus from the same outcrop and inadvertently found the partial remains of a one- to two-year-old child associated with some 115 red ocher-covered, stone, bone and antler artifacts that are dated at about 13,000 cal BP.New Radiocarbon Dates for the Clovis Component of the Anzick Site, Park County, Montana in Paleoindian Archaeology- A Hemispheric Perspective. University Press of Florida by Juliet Morrow and Stuart Fiedel, 2006. In another location in the same area, not associated with the Clovis child, the men found a partial skull fragment of a 6- to 8-year-old male child that dated 2,400 years later.
The 1994 recovery plan explained that due to the interspecific competition, the Shenandoah Salamander differs from other listed species. Because of this competition, it would not be advisable to attempt to increase population numbers, transplant individuals, or reduce naturally occurring competitors. Attempts to repopulate the salamander on talus areas between or adjacent to known populations would be unfeasible, costly, and unnecessary. Instead, recovery attempts should focus on minimizing human-related impacts on the Shenandoah and red-backed salamander populations. The actions needed for the recovery of the Shenandoah Salamander included determining the boundaries of occupied habitat and to determine if additional populations exist, monitoring the known salamander populations on a long-term basis, determining and minimizing the impact of human-related factors such as herbicides and air-pollutants on the salamander, investigating aspects of the salamander’s life history, ensuring compatibility of park maintenance and management activities with the salamander populations, and promoting information exchange on the salamander.
The ankle mortise, the fork-like structure of the malleoli, holds these three articulate surfaces in a steady grip, which guarantees the stability of the ankle joint. However, because the trochlea is wider in front than at the back (approximately 5–6 mm) the stability in the joint vary with the position of the foot: with the foot dorsiflexed (toes pulled upward) the ligaments of the joint are kept stretched, which guarantees the stability of the joint; but with the foot plantarflexed (as when standing on the toes) the narrower width of the trochlea causes the stability to decrease.Thieme Atlas of Anatomy (2006), p 406 Behind the trochlea is a posterior process with a medial and a lateral tubercle separated by a groove for the tendon of the flexor hallucis longus. Exceptionally, the lateral of these tubercles forms an independent bone called os trigonum or accessory talus; it may represent the tarsale proximale intermedium.
The flexor retinaculum of foot (laciniate ligament, internal annular ligament) is a strong fibrous band, extending from the bony ankle prominence (malleolus) above, to the margin of the heelbone (calcaneus) below, converting a series of bony grooves in this situation into canals for the passage of the tendons of the flexor muscles and the posterior tibial vessels and tibial nerve into the sole of the foot. It is continuous by its upper border with the deep fascia of the leg, and by its lower border with the plantar aponeurosis and the fibers of origin of the abductor hallucis muscle. Enumerated from the medial side, the four canals which it forms transmit the tendons of the tibialis posterior and flexor digitorum longus muscles; the posterior tibial artery and tibial nerve, which run through a broad space beneath the ligament; and lastly, in a canal formed partly by the talus, the tendon of the flexor hallucis longus. The entrapment of the tibial nerve beneath the laciniate ligament causes tarsal tunnel syndrome, characterized by pain, numbness and tingling of the medial plantar surface of the foot.
At Siccar Point, during the lower Silurian Llandovery epoch around 435 million years ago, thin beds of fine-grained mudstone were laid down gradually deep in the Iapetus Ocean, alternating with thicker layers of hard greywacke formed when torrents swept unsorted sandstone down the continental slope. During the following 65 million years, the ocean closed and the layers of rock were buckled almost vertically, getting forced to the surface as the ocean floor was subducted under the northern continent. Erosion of the exposed edges of layers formed a characteristic shape of ribs of hard greywracke with narrow gaps where mudstone was worn away, and fragments of greywacke lay on the surface as a talus deposit. In the Famennian Late Devonian period around 370 million years ago this was a low-lying tropical area just south of the equator, where rainy season rivers deposited sands and silts rich in iron oxide, then during the dry seasons these were blown about by winds to form easily eroded layers and dunes.
Roman die, found in Leicestershire, England Bone die found at Cantonment Clinch (1823–1834), a fort used in the American Civil War A collection of historical dice from various regions of Asia Knucklebones die, made of steatite Dice have been used since before recorded history, and it is uncertain where they originated. It is theorized that dice developed from the practice of fortune-telling with the talus of hoofed animals, colloquially known as knucklebones. The Egyptian game of senet was played with flat two-sided throwsticks which indicated the number of squares a player could move, and thus functioned as a form of dice. Senet was played before 3000 BC and up to the 2nd century AD. Perhaps the oldest known dice were excavated as part of a backgammon-like game set at the Burnt City, an archeological site in south-eastern Iran, estimated to be from between 2800 and 2500 BC. Bone dice from Skara Brae have been dated to 3100–2400 BC. Excavations from graves at Mohenjo-daro, an Indus Valley civilization settlement, unearthed terracotta dice dating to 2500–1900 BC.Possehl, Gregory. "Meluhha".
Dark grey gritstone was used in the construction to produce a forbidding appearance, although the prison itself was considered healthy and well ventilated.Butler, p.24; Sears, p.180. Clifford's Tower played no part in the formal design of the prison, although the talus, or sloping edge of the motte, was cut away and replaced by a retaining wall to allow more space for the new prison building.Cooper, p.195. The backyard of the Female Prison, concealed from public view by the new wall, was used for hangings from 1868 onwards. The Prison Act, 1877, reformed the English prison system, and York Castle gaol was passed into the control of central government the following year.Cooper, p.196. It was used as the county prison until 1900, when the remaining prisoners were transferred to Wakefield Prison, and from then onwards the facility was used as a military prison instead.Butler, p.24. Architects Robinson and Andrews' original design for the front (l) and interior (r) elevations of the new 1825 York Castle prison gatehouse By the early 19th century, dredging and other improvements to the river Foss had made it possible to import flour into York by river, reducing the economic significance of the castle mills.Butler, p.8.

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