95 Sentences With "splays" | Random Sentence Generator

Overhead light splays dramatic shadows across the gallery floor producing ghostly doubles.

In the center, a massive tangle of rocks and dead branches splays.

He really kind of splays himself emotionally, and I stay on him.

Their blood splays out in a red-tinted mist with a cinematic arc.

They end as high-contrast splays of sound, ranging from melodic solo statements to coordinated wallops.

The dying pigeon's flaps grow weaker as the raven splays its guts across the concrete platform.

After walking up a twisting staircase, the gym splays out through what is essentially a wide hallway.

Lexy Anderson splays open her Japanese tunic to reveal an American-style gown, an homage to her mixed heritage.

It splays onto the sidewalk, massive, yielding (though quite durable), its color vibrant against the concrete building behind it.

But with the Popular Photos feature, Facebook splays out more images for users to scroll through after the original.

The arc of women-led sitcoms splays out from Lucy Ricardo in an apron to Abbi and Ilana high, running around New York.

Then, when Nick throws Cheryl on his bed, he splays her out like a broken doll, again turning her from person to living sex toy.

The chief judge, sitting in the middle, splays his right arm across the bench like a piece of wet laundry and fiddles with his fingers.

He splays his legs on the release for no reason, like he's auditioning for a Jump Man commercial instead of trying to knock down an open shot.

There are echoes, too, of Trish Brown's gravity-defying dances with ropes and harnesses — especially when Ms. Bauer climbs a huge charred tree and splays her body horizontally.

He splays his long limbs in front of the chair and folds his arms against his torso—extraordinarily fit by any standard, but especially for a man who turned 73 in September.

The way he splays himself wide after scoring a goal, like a earth-bound wing suit, is a perfect fit to Da Vinci's Vitruvian Man—the platonic ideal of form and arrested motion.

Every vein in the marble splays in the right pattern, every tile is lined up to a fare-thee-well, every fold in every drape — floor-to-ceiling plaster-hued cashmere — is perfect.

The bracket is inserted through holes drilled into the sheets of plywood, and owing to the varied placement of the holes relative to the panels' center of gravity, the wood splays as it sags, forming an irregular 12-pointed star.

There's also a poster from the London Underground in 1986, depicting a rare example of womanspreading: A female punk with a rainbow mohawk splays her legs on a bus seat while an elderly gentleman stands and waits for a chance to sit.

In the trilogy, there is also a landscape crop of three very similar-looking male models, two of which are wearing what look like chainlink skirts, while a third splays on the floor of a gray set, donning a tailored coat of the same color.

Just check it out as your dude rolls up wearing bunny ears (for some reason), splays out some balls on the floor to trip the wrestlers, swings a bucket in a dude's face, and then brings the match to an end with a Santa-assisted frog splash.

" A zigzagging, finger-tapping guitar pattern splays into a mesh of chords with a hint of Hendrix, behind a breathy, androgynous vocal that doesn't mince words: "I might be a soft-spoken person/But I'm aware of the power I have/So move out of my way.

Advertise on Hyperallergic with Nectar Ads Packed with verdant splays of moss and fern, dark clumps of rock and soil, and tumbling surges of water, the large-scale landscapes in Claire Sherman's New Pangaea at DC Moore Gallery, convey, in their shadowy overgrowth, the sense that something is hidden.

Star Wars novels have traditionally been resistant to books that play with form, but Older splays out his narrative across a number of timelines: the main thrust of the story is set two years after the Battle of Endor, and bounces between Han and Lando's stories from a decade prior (bracketing Solo), as they hunt after and acquire a mysterious package from a villain named Fryzen Gor, whose own origins play out twenty years before the main story.

In the undercroft itself the walls are impregnably thick, the windows narrow, with wide splays.

The DST splays within the area of the restraining bend, with several distinct active fault segments recognised.

The splays on both sides display (inferior copies of) statues of the apostles, with one standing on a chained devil. The tympanum shows Christ enthroned, sitting under a baldachin and flanked by the four Evangelists, each with his own attribute.

"Even-toed but uneven in length: the digits of artiodactyls." Zoology 112, no. 4 (2009): 270-278. The moose hoof splays under load, increasing surface area, which limits sinking of the moose foot into soft ground or snow, and which increases efficiency when swimming.

The more southeasterly branch of the Wellington Fault is known as the Mohaka fault. The fault splays to the north, onto the Waimana Fault, which itself branches into the Waiotahi and Waioeka Faults, the main segment of the Mohaka Fault eventually passes into the Whakatane Fault.

This was formed in the deep crust and mantle. The two different rock zones are separated by the Finch-Langdon fault zone. It consists of seven segments of faults, subsidiary faults and splays. The fault is a transform fault with a corner at the spreading ridge.

The environment during time of deposition was semi-arid, but with seasonal rain and flooding due to the presence of crevasse splays in the mudstone layers. A lack of well developed channel sandstones provides evidence for more lacustrine areas in the more northerly occurring outcrops of the biozone.

The chancel walls were raised and a new roof constructed in 1642. The north aisle was rebuilt in 1884–5, and the west tower in 1890, and other works done in 1912 and 1921. The chancel, c. 1150, has a modern east window with internal splays of the 15th century.

Overbank deposits are fine-grained and accumulate vertically. The disturbance of adjacent environments during flooding events leads to deposits containing terrestrial organic debris such as plant matter, and the intervening dry periods allow subaerial bioturbation by roots and burrowing animals. Notable sub-environments within the floodplain include natural levees and crevasse splays.

Stained glass window made by James Powell and Sons There are windows of various dates, and others were removed during the frequent extensions and alterations. The east window of the chancel was altered during the 17th and 20th centuries, but has 13th-century origins in the form of chamfered vertical sections with moulded splays.

The suburb of Molonglo is split by an east-west direction fault that splays off the Winslade Fault. This fault is marked by quartz. The south side has been thrown down, and the north side elevated. This fault crosses the Molonglo River at the point where it goes in a tight bend from east to north west.

The chancel was restyled in the 15th century, and has many niches for saints in the window splays. The church suffered damage during the Reformation and the Civil War and was much altered in succeeding centuries.Taken from 'A photographic and historical guide to the Parish Churches of East Suffolk' compiled by Adrian S. Pye. 27 January 2009.

The interior room is approximately by , a size that befits more an oratory or a small chapel than a church. It is dimly lit, with only a tiny round-headed window in the east wall, opposite the entrance door. The window splays more widely towards the inside of the wall. The doorway is 1.67 m (5.5 ft) high.

The south wall also has a bricked-up doorway, which may have been a Saxon-era entrance. Overall, though, the building is low, broad and sturdy—a "vigorous, down-to- earth and practical work" which was characteristic of Norman builders. The king-post roof is likely to be original. High in the nave walls are two small windows with modest splays.

The Los Angeles basin is still active tectonically and the region continues to experience earthquakes as a result. Due to the number of faults and fault splays, seismic activity is not concentrated in one particular area. The cities that are overlain by the Newport–Inglewood and Whittier fault zones have a higher probability of experiencing seismic activity. The region experiences earthquakes that are mostly mild (magnitude ≤2.25).

These volcanic rocks are distributed along splays of the Sorong Fault system. The formation and propagation of the Halmahera arc is a consequence of the clockwise rotation of the Philippine Sea plate as the southern edge moved across the northern Australian margin and impinged on the east Eurasian margin. The ages of initiation of volcanism and subduction track the developing plate boundary as subduction propagated northwards.

Coppins Crossing in 2020 The suburb of Denman Prospect is split by an east–west direction fault that splays off the Winslade Fault just to the west of the suburb. This fault is marked by quartz. The south side of the fault has been thrown down, and the north side elevated. The north-east heading Winslade Fault itself cuts off the northern tip of the suburb.

The degree of channel amalgamation and palaeosol development corresponds with sediment discharge rates: More confined meandering channels and extensive palaeosol developments are associated with lower discharge rates rather than amalgamated braided channel systems.Wanke, 2000, p.43 The channel geometries and the low degree of amalgamation in the Lower Omingonde Formation indicate an overall meandering river system. Sandy mudstones were generated during crevasse splays and associated flood stages.

The resulting deposition can create graded deposits similar to those found in Bouma sequences. In some cases crevasse splays can cause a river to abandon its old river channel, a process known as avulsion.Boggs, S. Jr., 2012, Principles of Sedimentation and Stratigraphy: New Jersey, Prentice Hall, 218 p. Breaches that form a crevasse splay deposits occur most commonly on the outside banks of meanders where the water has the highest energy.

There are, inside, a nice set of disc-shaped steles. The jewel is the famous Romanesque portal, the most complete and most beautiful of Lauragais. It is a "portal Toulouse" without eardrum but with multiple arches, corresponding to projections of splays and columns housed in the projections • The Ruins of the Chapel of the Rosary (15th) located above the village near the castle. • The Church of St. John Baptist de Tresmèzes.

This fault zone is the most notable feature within the basin that is a single strand with local (fault) splays. The fault zone is also marked by low hills, scarps, and ten anticlinal folds in a right-stepping en echelon pattern. It is located in the southwest portion of the basin and is a strike-slip margin. There are several oil fields that run parallel to this fault.

The junction between the Hope fault and the Alpine Fault is complex. The Kelly Fault forms a major splay of the Hope Fault from just west of Harper Pass; it splays again to the west into the Newton and Hura faults. From repeat GPS surveying on the region near Arthur's Pass, the Kelly Fault marks a sharp reduction in velocities to the northwest of the Kelly and Hura faults.

The frills of ceratopsians are incredibly diverse. They may have been used for protective purposes as the frill sometimes splays over the neck. However, some say that the frill would have provided little protection from other large dinosaurs such as Tyrannosaurus. Other possible functions include intraspecific communication for mating purposes or as a visual display of territorial protection, as seen in many common day organisms such as red-breasted robins.

1350, partly restored and of two cinquefoiled lights with tracery in a segmental pointed head, under a chamfered label; the western window is Victorian, except the internal splays and hollow chamfered rear arch, which are of the 15th century. Between the windows is a Victorian doorway. There is no chancel arch, but between the chancel and the nave is a chamfered and moulded beam, probably of the 15th century.The Monuments of North West Essex.

The east window is an example of a single Early English lancet with very wide splays and shafts in the inner arch. The main roof timbers, both in the Nave and Chancel, date from the sixteenth century, whilst the ceiling above the sanctuary is panelled and its bosses and carvings picked out in gilt and colour. The font is octagonal in shape. The bowl is modern and it stands on a very much older shaft.

The parapets are of the stepped Irish type (now much restored) but probably datable to c. 1395, the year in which a Papal relaxation was given to those who visited Kildare and gave alms for the conservation of the church. The interior treatment is plain, the window splays are not moulded, but the rear-arches, which are, spring from shafts with moulded capitals. These shafts are short and terminate in small curved tails.

Part of the school grounds. The 46-acre school campus is in two halves. The North site, separated by a public lane, has modern buildings set behind its largely administrative 17th century rebuilding of Thorpe manor house (with Georgian front elevation). The South site centers on the grand early 19th-century convent built in the grounds of Thorpe manor house, built in yellow brick featuring a two-storey splay sided bay with sash windows in splays and French windows.

Great Hall, Bradfield House, Devon, looking toward the north gable wall showing the arms of King James I and a crudely executed wall-painting of two soldiers. The Walrond arms can be seen painted on the window splays to the rightPevsner, p.199 The door in the back wall leads to the "Spanish Room" via the internal porch. The door to the right leads to the "Oriel Room" The Parlour or "Spanish Room", Bradfield House, Uffculme, Devon.

Late Triassic (220 Ma) The Quebrada del Barro Formation formed within a rift basin during a period of renewed fracturing. It encompasses of red sandstones, fine conglomerates, and diamictites. Early hypotheses on the depositional environment proposed that the sediments formed in an alluvial fan or braided river system, while a newer proposal outlines how four different facies within the formation can be used to reconstruct a meandering semiarid floodplain deposited by mudflows and discharging in heterolithic terminal splays.

Raccoon photographed in the Delta National Wildlife Refuge in Louisiana Delta NWR supports a wide variety of wildlife species. Tens of thousands of wintering waterfowl take advantage of the rich food resources found in the delta. Large numbers of other bird species can be found on the refuge, with numbers peaking during the spring and fall migrations. Large numbers of wading birds nest on the refuge, and thousands of shorebirds can be found on tidal mudflats and deltaic splays.

Tertiary volcanic and sedimentary rocks, and Quaternary glacial deposits, developed over the older rocks. The Lake Clark (Alaska) fault, or a splay, probably lies within of the Pebble deposits and possibly much closer. The Lake Clark fault is a major right-lateral strike-slip crustal feature, considered to be a westward expression of the Castle Mountain fault. The actual ground trace of the fault and its splays are unknown in the Pebble area, due to extensive ground cover.

F Shed is the retail market's newest permanent structure, debuting in April 2013. It replaced what was previously a sequence of tents deployed ad hoc over pavement during appropriate times of the year. There is room for 75 stalls in F Shed, which runs the same length of 270 feet as the market's older structures, but splays wider than some of them at 80 feet. F Shed was built for $1.5 million paid from the authority's reserves, without borrowing.

This fault splays off from the Altyn Tagh Fault at the southwestern end of the Altyn Tagh mountains and runs along the edge of the Altyn Tagh range. It is a dominantly sinistral strike-slip structure, with some subsidiary thrusting. It is thought to extend northeastward from the end of the Altyn Tagh based on effects on drainage and bedrock ridges suggesting a linkage with the Cherchen Fault. It may have formed part of the ATF at an early stage in its development.

In low sun-angle photography additional scarps and splays can be observed. The erosion/sedimentation patterns and the path of drainages such as Canyon Creek may have been influenced by movement along the fault, and topographic ridges are offset. Finally ductile folding, vegetation and landform variations have also been recognized on the Meers fault. In some rock formations faulting has mainly led to warping, instead of brittle displacements and in several sites evidence of faulting appears to be concealed by floodplain sedimentation.

The light fittings on the pilasters and proscenium splays are designed as angular vase elements. A number of these wall panels are fixed over the shuttered openings to the outside. These as well as the decorative grille running the length of the ceiling in the auditorium were incorporated as a way of ensuring air circulation and cooling in summer and were closed in winter. The whole auditorium features a complex and pleasing original paint scheme and elements of decorative plaster.

While round portholes are the most common, square ones are also found. In front of the facade is a court that usually splays out, creating an area where rituals possibly took place. The court is usually outlined by large stone walls, sometimes over a meter high, which enclose the court. It is in this area that Bronze and Iron Age pottery has been found - which helped date these sites -, along with human remains, bronze tools and silver, gold and semi-precious stone ornaments.

Rivers in the Sundarbans are meeting places of salt water and freshwater. Thus, it is a region of transition between the freshwater of the rivers originating from the Ganges and the saline water of the Bay of Bengal. The Sundarbans along the Bay of Bengal has evolved over the millennia through natural deposition of upstream sediments accompanied by intertidal segregation. The physiography is dominated by deltaic formations that include innumerable drainage lines associated with surface and subaqueous levees, splays and tidal flats.

The northeastern section of the fault zone shows increasing interaction with WNW-ESE trending structures within the eastern Kunlun Shan and the Qilian Mountains. The estimated displacement rate decreases along the northern section, suggesting that some of the displacement is transferred onto thrust structures along the south side of the Qaidam Basin. Northeast of the Qilian Mountains, a series of five or more splays of the ATF have been identified, with active slip constrained to the post-Cretaceous to pre middle Miocene time interval.

The cross stands at the junction of Romsey Road (the A3057 road) and Church Road in the centre of King's Somborne. It is in Portland stone, consisting of a tapering, lozenge-shaped shaft with short arms moulded close to the top. It sits on a three-tiered plinth of stone blocks which itself sits on a narrow coved plinth which splays upwards from the bottom to provide a seat at the foot of the cross. The plinth rests on base of three shallow stone steps.

These variations likely coincided with the presence of small "sub- environments" commonly found between rivers like splays, ponds or creeks. After being deposited in their final resting places the carcasses were torn apart, had their bones trampled and chewed by scavengers. These processes left the abrasion and toothmarks seen on the bones preserved at H97-02. Chemical reactions between the decaying dinosaur flesh and floodwaters caused iron to precipitate out of the water and formed the ironstone concretions commonly found in the mudrock hosting the mega-bonebed.

The roll mouldings of the arch are held in the beaks of these "fearsome", "wide- eyed horrors". Such "beakhead" decoration is a little-understood feature of Late Norman architecture: in churches, it may have been used to capture the congregation's interest or to inspire fear and awe. The moulding has two orders (recessed jambs which together form a chamfered opening): in contrast to the lavishly decorated outer order, the inner order is plain. Some Norman windows survive: these are large, round-arched and chamfered with deep splays.

Overpronation Those who overpronate tend to push off almost completely from the big toe and second toe. As a result, the shock from the foot’s impact doesn’t spread evenly throughout the foot and the ankle has trouble stabilizing the rest of the body. Additionally, an unnatural angle forms between the foot and ankle and the foot splays out abnormally. It is common even for people who pronate normally to have some angle between the foot and the ankle, but not to the extent seen in those who overpronate.

The Cimitarra Fault splays from the Palestina Fault in a northeasterly direction on the eastern border of the Central Ranges of the Colombian Andes, passes north of Barrancabermeja,Paris et al., 2000b and possibly connects to the Bucaramanga-Santa Marta Fault in the northeast.Plancha 5-06, 2015 The fault displaces Jurassic to Cretaceous volcanic rocks, Mesozoic igneous rocks, a Tertiary erosion surface in the Central Ranges, and late Quaternary sediments. Portions of the fault are pre-Pliocene in age, since it is locally covered by undeformed Pliocene sediments.

Figurative scenes predominated, but representations of foliage were sometimes painted in awkward locations such as sloping walls. Few of these decorative images survive, but at St Margaret's Church some painted vines are visible in one of the window splays. The "very delicate painting" is on the inside of one of the windows in the chancel's south wall, which was inserted in the mid-13th century. The present west gallery was erected in 1899 as a replacement for the original, installed in 1723 but removed during Slater and Carpenter's renovations of 1870.

The Marlborough Fault System consists of four main dominantly strike-slip fault strands, which together carry almost all of the displacement associated with the plate boundary. Other smaller faults form as splays of these main faults or accommodate deformation of the crust between them, such as the Newton and Hura Faults at the western end of the Hope Fault and the Jordan Thrust that formed the Seaward Kaikoura Range. The dextral strike-slip across this zone has also involved clockwise rotation of the intervening fault blocks of about 20° since the early Pliocene.

Firstly, the median parietal bar (the bone bar between the frill openings) at mid-length splays out to the rear like a fan and its rear edge is not notched or embayed. Secondly, the upper surface of the bar is, at the midline, hollowed out by a symmetrical depression. It is this hollow in the form of an inverted tear that occasioned the specific name as it resembled the single eye of a cyclops, thus the allusion with Polyphemus. The authors assumed it formed the base of a horn-like epiparietal.

The domination of sandstone in the Lystrosaurus Assemblage Zone shows that the climate at the time had become more arid, where rainfall was unpredictable and the shallow, braided rivers would seasonally dry up. When the rivers flowed again after the rains, due to being shallow, they would frequently flood their banks, hence the presence of crevasse-splays. Conglomerates are also found in eastern outcrops, which are indicative of erosion occurring due to die-offs of plant ecosystems. There is in addition a notable gap in coal deposits at this time as a result.

The columns are accentuated at the springing line of the splays with two rows of rectangular moulding forming decorative capitals and with plinths at their base. The current paint scheme distinguishes various components of the exterior using pale yellow as a base colour detailed with a teal blue, terracotta orange and red. Having originally incorporated a lookout, the Innisfail Water Tower still has views over the region. Within the central tower, a half-turn stair with equal flights, constructed of concrete with a tubular metal handrail and balustrade, provides access to the tank.

The Hula pull-apart basin lies to the north of the Sea of Galilee basin and is formed between several short fault segments. The currently active part of the basin is relatively narrow. The Hula Western Border Fault defines the western side of the basin and splays to the north into several faults, including the Roum fault and the Yammouneh fault. The Hula Eastern Border Fault continues northwards from the northeastern part of the Sea of Galilee, forming the eastern edge of the basin and linking eventually to the Rachaya fault.

The San Andreas Fault (SAF) spans nearly the length of California, where much of its length the fault is clearly identifiable, especially from San Francisco to near Cajon Pass. There, the fault splays into several branches. Several unusual characteristics are displayed further to the southeast in the area of the San Gorgonio Pass. There are no lateral stream offsets (that are associated with strike-slip faulting) near the pass like there are along other segments (one researcher indicated that thrust faulting was the dominant type of fault displacement at the pass).

The first floor loggia consists of three arched bays with rendered balustrade, separated by pilasters supporting deep cornices on either side of a raised central rounded pediment surmounted by a shield. Sash windows open onto the loggia, with a door at the eastern end. The rear of the building has metal framed hopper windows with a two-storeyed, skillion roofed amenities addition on the western side, and a single-storeyed carport/loading area with roller doors beside. Internally, the central foyer splays open off a short hall and has a shop at the rear.

The great fresco of the Madonna and Child Enthroned with Saints Augustine, Francis, Anthony of Padua and a Holy Monk above the altar, with a lunette that shows the God the Father Blessing, is enclosed by a white marble frame with rich golden decorations. There are two arched windows on the two adjacent walls with splays decorated with grotesques. The first wall is decorated by the fresco of the Assumption of the Virgin Mary while last section is covered by the funeral monument of Giovanni Basso (†1483). That was created around 1485 by the workshop of Andrea Bregno.

In the rostral direction, the midbrain noticeably splays laterally. Sectioning of the midbrain is usually performed axially, at one of two levels – that of the superior colliculi, or that of the inferior colliculi. One common technique for remembering the structures of the midbrain involves visualizing these cross-sections (especially at the level of the superior colliculi) as the upside-down face of a bear, with the cerebral peduncles forming the ears, the cerebral aqueduct the mouth, and the tectum the chin; prominent features of the tegmentum form the eyes and certain sculptural shadows of the face.

The 20mm/yr dextral (right lateral) strike slip Sagaing Fault detaches the Burma microplate from the Sunda plate. The arc-parallel fault spans over 1400 km in a north-south direction, remarkably linear for the central 700 km (at 17°N to 23°N latitude) and forms a slight arc shape swinging N10°E and N170°E direction at the north and south ends of the fault respectively. Northward, the Sagaing fault terminates at the Jade Mine belt (~ 24.5°N) and splays into a 200 km width compressive horsetail structure. Southward, it is connected to the active Andaman spreading rift.

Located on the top of a hill in Mourilyan Road on the east side of the Johnstone River, the Innisfail Water Tower is a prominent feature on the skyline, its stylistic influences strongly reflecting the Art Deco character of a number of other buildings in Innisfail. Surrounded by palm trees and a low masonry fence with iron railing, the reinforced concrete structure comprises a circular tank supported on a central cylindrical tower and eight rectangular section columns. The tank wall is embellished with a continuous parapet moulding and recessed panels. Beneath the tank, arched reinforced concrete splays span between the columns.

The small chapel is hexagonal with a sexpartite ribbed vault and the entrance is protected by an elegant marble parapet which is decorated by garlands, ribbons and patenas. The fresco decoration was painted by a helper of Pinturicchio, stylistically close to Melozzo da Forli. The side walls are articulated by painted Corinthian pilasters decorated with candelabra, flowers and garlands on a yellow background, resting on a fake monochrome pedestal. The ribs and the splays of the two arched windows were decorated with grotesques but only the right-hand window is preserved (the other was later walled up).

For instance, there is a small walled window with late Gothic splays. Until the French Revolution in 1794 (when revolutionary troops conquered the Trier region), it was an agricultural estate owned by the St. Matthias Benedictine monastery, which still exists today. As part of the secularisation of these years, the estate was auctioned off in 1805 to the credit of the French state and acquired by Nicholas Valdenaire, who had come to the nearby town of Saarburg as a French soldier in 1801 and married there. Valdenaire extended the estate and enlarged the Roscheider Hof buildings with extensive renovations.

A parapet was added to the nave and aisle roofs, the north wall of the chancel was pulled down to enlarge the building, the east walls were rebuilt, the church building faced with flint and a vestry added to the north side. This vestry was further enlarged about the turn of the 20th century. A proposal in 1893 to build an organ at the south side of the chancel was abandoned when three Norman windows were uncovered, still showing decoration on the splays. The T.C.Lewis Company was commissioned to build a three manual organ which was completed in 1900.

The south aisle dates from the early 14th century. At the western end is the Lady chapel with a small altar table, which is used for quiet prayer and contemplation. Behind the altar table is the east window; this has two lights with pointed trefoil heads and a diamond-shaped quatrefoil light at the top; the interior splays of the window have shallow cinquefoil-headed niches. On the south wall, to the right of the altar are the aumbry, behind a wooden door in a square stone opening, and a triangle-headed piscina; these both date from the construction of the aisle in the early 14th century.

Careful inspection reveals the two faces of the completed fiador knot, where the four strands emerge, are not identical. One has the appearance of a crown knot surrounding the emerging strands and is somewhat resistant to spreading when they are pulled apart. By comparison, the strands emerging from the other face of the knot are not nearly as well-contained and if pulled apart, the fiador knot easily distorts and splays. Depending on how the fiador knot is tied, these distinct faces can be positioned differently with respect to the side of the knot with the two loops and the side with a single loop and the two free ends.

These multiple trunks commonly will grow together to form a large combined mass at the base and split into individual trunk at greater heights. If they are individual trunks at breast height then the individual trunks can be measured separately and treated as individual single trunk trees. If they have grown together at breast height then a measurement of their combined girth should be made at that height the number of trunks incorporated into the girth measurement listed. If the tree splays outward dramatically at breast height, then the girth should be measured at the narrowest point between breast height and the ground and that height noted.

The building includes much Roman material salvaged from the surrounding ruins of Verulamium, including Roman brick used in the splays of the nave windows. Early in the 12th century a north aisle and then a south aisle were added, linked with the nave by arcades of plain round-headed arches cut in the latter's north and south walls, leaving sections of Saxon wall as piers. The arcades do not match: the earlier north arcade has three bays spaced irregularly; the later south arcade was built with four bays. The round-headed Norman window at the east end of the north aisle may also be 12th-century.

The faults at Chalamant and Le Rouchou de la Forêt are brecciated and cataclastic. The latter is a major fault, it even cuts off tectonic units (like the oceanic Sarrazac Massif from the Upper Gneiss Unit); it can be traced to Sarrazac in the south, in the north it splays out. Some of the higher ridges are mantled by Tertiary alterites, which consist mainly of Pliocene fluvial gravels (tongues near La Lande de Beauplat, La Lande de Perrières, La Petite Lande and Le Pierrefiche) and colluvium. The colluvium underlies the gravel tongues and probably dates back to the Eocene, but was later reworked during the Pleistocene (ice ages).

Manual for Streets has updated geometric guidelines for low trafficked residential streets, examines the effect of the environment on road user behaviour, and draws on practice in other countries. Research undertaken by TRL provides the evidence base upon which the revised geometric guidelines in the Manual for Streets are based, including link widths, forward visibility, visibility splays and junction spacing.Department for Transport: Policy, guidance and research – Sustainable travel – Manual for Streets Manual for Streets applies in England and Wales and is national guidance, not a policy document. The Scottish Government commissioned WSP Group, Phil Jones Associates and Edaw to produce Designing Streets, a version of Manual for Streets for application in Scotland and was published in 2010.

The Meers fault is the only fault on Oklahoma which has generated a rupture on the surface, resulting in about of vertical offset over a long distance. It is possible that the fault rupture was limited by geological structures that occur at the northwestern end of the Meers fault where it splays out. The possibility that faulting continued for another along its northwestern end is equivocal with some evidence indicating that recent faulting was limited to Comanche County; research published in 2019 indicates that the northwestern segment did not move during the 1,200 BP earthquake but was active in the 3,400–2,900 BP event. The underground rupture on the other hand might reach a length of .

The arches forms three lunettes: in the larger one is a representation of the Holy Trinity with two Angels, flanked by St. Joseph and the Holy Virgin. The Father sits on a Gothic throne with Crucifix on his knees and Christ on his side, surmounted by a dove. In the two smaller lunettes, directly over the portal, are portrayed the Bishop leading the Veronese people and St. Peter of Verona leading the friars, with the white-black banner of the Dominicans. The five splays of the Gothic arch are decorated with six chronological scenes of Jesus' life: the Annunciation, the Birth, the Adoration of the Magi, the Path towards the Calvary, the Crucifixion and the Resurrection.

The kneeling queen Maria of Aragon western portal of the Jerónimos Monastery in Belém By January 1517 he and an assistant were at work as master contractors at the western portal of the Jerónimos Monastery in Belém. This was probably his first assignment in Portugal. When he arrived, the supporting corbels had already been decorated in Late Gothic style with small angels holding the coat-of-arms and, at the side of the king, an armillary sphere and, at the side of the queen, three blooming twigs. He filled the splays on each side of the portal with statues, among them king Manuel I and his second wife Maria of Aragón, both kneeling in a niche under a lavishly decorated baldachin.

26; pp167-183 Primarily the strata exist as fault-bounded slices within splays of, and to the southeast of, the main Church Stretton fault system. The Uriconian rocks comprise both intermediate to acidic and basic (bimodal) volcanic suites that reflect largely intraplate origins for the complex although some subduction signatures have been identified. Further work has led to suggest that the locality of this kind of volcanism is related to marginal basin volcanicity (behind the main arc) influenced by trans-tension brought about by oblique subduction.Pharaoh, T.C., Gibbons, W., Precambrian Rocks in England and Wales south of the Menai Straight Fault System, 1987 A Revised Correlation of the Precambrian Rocks in the British Isles The Neoproterozoic sediments were deposited on Avalonia in various strike-slip faulted basins and they comprise predominantly volcaniclastic and siliciclastic sediments.

In this are visible windows and a pointed front door with splays of the old medieval structure; A large hall divided by two pointed arches with the central column; The private chapel where you can admire a beautiful wooden tabernacle of the first decade of '600, with Corinthian columns that mark prospectively space. Outside the chapel, a portal giving access to the bastion, where the remains of a perimeter wall are visible. The second floor, reached by an outside stone staircase Billiemi, architect Matteo Carnalivari, comprises: the ballroom, classic example of fifteenth-century room with coffered wooden ceiling, fireplace adorned with the emblem of La Grua and large windows with leaning seats and from the sleeping area, composed of frescoed rooms, where you can admire a beautiful eighteenth-century decorated door that characterizes the alcove. A small circular staircase leads to the kitchen, while another adjoining rooms on the upper floors.

Strong aeromagnetic anomalies in the Strait that curve from Victoria to Discovery Bay (west of Port Townsend) led to early speculation that the LRF, and the eastern limit of the Crescent Formation, ran down Discovery Bay and the west side of Puget Sound, following the edge of a relict continental margin just as the Tofino Fault follows the present margin.;. This alignment through Discovery Bay is what calls the "Cenozoic truncation scar". More recent interpretations of marine seismic reflection studies align the Goldstream arm of the LRF with the Southern Whidbey Island Fault (SWIF), with splays branching towards Discovery Bay.. Discovery of Crescent Formation basalt in an exploration well on Whidbey Island (just east of Port Townsend) has led some writers to locate this extension of the LRF onto the southern part of Whidbey Island, just where the SWIF is found.. While the eastern contact of the Crescent Formation is believed to not extend east Whidbey Island, and may double-back westward under Seattle,. active faulting on the SWIF extends southeast to where it connects with the Rattlesnake Mountain Fault Zone.