44 Sentences With "lava bed" | Random Sentence Generator

You just stare at the waterfall or grassland or mossy lava bed.

Now a team of researchers think they've found it, buried beneath a lava bed in Laos.

Onlookers gather at the foot of the lava bed, as a lava shoots molten rock into the air, in the Leilani Estates near Pahoa.

"What used to be the bay is now all lava bed, new land, almost a mile out into the ocean," the civil defense spokesman said.

The Round Barn and Jenkins Family Visitor Center has an interesting gift shop and small museum, open daily from 9 to 5 (51955 Lava Bed Road, Diamond, 888-493-2420).

It recalls the early Mesoamerican site of the pyramid of Cuicuilco, with 64 hulking wedges of concrete circling the basin of an ancient, craggy lava bed now wild with plants.

The cinder cone that produced the Big Lava Bed rises above a forest, which covers part of the extensive lava flow it produced. One of Indian Heaven's vents produced a large effusive eruption about 9,000 years ago, forming the Big Lava Bed, which consisted of basaltic lava. With an area of and a volume of , the Big Lava Bed mostly consists of unvegetated basalt. It moved to the south down the Little White Salmon River drainage, which it filled for of its length.

A band may represent a specific mode of deposition: river silt, beach sand, coal swamp, sand dune, lava bed, etc.

The Ibkilwit Lava Bed is a lava bed on Nunivak Island in the U.S. state of Alaska. It is located at , one mile (1.6 km) east of Karon Lake and twelve miles (19 km) north of Cape Mendenhall. Ibkilwit is an Eskimo term that was recorded in 1949. Variations include Ebcyeet, Ibkhikhyit, and Ibxixyit.

The Big Lava Bed, located in the Gifford Pinchot National Forest in the southwestern area of the State of Washington, originated from a 500-foot-deep crater in the northern center of the bed. The Big Lava Bed is the youngest feature of the Indian Heaven volcanic field. The 0.9-cubic kilometer lava flow erupted from the cinder cone about 8200 years ago. The lava flow traveled 13 km from the source crater.

The geology of the district is transitional with Deccan trap rocks (lava bed) predominating, displaying characteristic step-like hills and ridges. These have been eroded through in places, exposing older Puranic and Aryan sediments.

Mount Adams was last active about 1,000 years ago and has created few eruptions during the past several thousand years, resulting in several major lava flows, the most notable being the A. G. Aiken Lava Bed, the Muddy Fork Lava Flows, and the Takh Takh Lava Flow. One of the most recent flows issued from South Butte created the long by wide A.G. Aiken Lava Bed. Thermal anomalies (hot spots) and gas emissions (including hydrogen sulfide) have occurred especially on the summit plateau since the Great Slide of 1921.

Goose Lake formed when the Big Lava Bed dammed up a nearby stream. The blocked stream formed the lake. On the southeast side of the lake, there is a ghostly stand of dead trees rising from the water.

Hell's Half Acre Lava Field, Idaho, United States of America. Reykjanes Peninsula, Iceland. Degassing Holuhraun lava field with fountaining at crater Baugur, Iceland, Sept. 2014 A lava field, also called a lava plain or lava bed, is a large expanse of nearly flat-lying lava flows.

Inside the ecological reserve stands the Sculptural Space. It is a big round natural solidified lava bed surrounded by many white triangular prisms that seem to radiate from its center, a bit like a sunflower. There are many big and colorful metallic sculptures made by contemporary artists surrounding this area, hence its name.

Derrick Cave is a classic lava tube structure. It was created by lava flowing downhill from a volcanic vent located north of the cave. Lava from the vent also created Devils Garden, a lava bed southwest of the cave. Most of the lava deposited around the Devils Garden area was delivered through the Derrick Cave lava tube.

It is composed almost entirely of unvegetated barren lava. Kipukas (vegetated oases on the lava bed) harbor remnant native plants among the dominant non-native trees. Compared to this ecotype's historical extent on Maui, less than 2% was left as of 2010. Plant life cycles here are keyed to a very severe and prolonged dry season and variable wet season.

The lake is a popular spot for brook, brown and coastal cutthroat trout fishing. Goose Lake Campground offers a concrete boat ramp for launching small boats, kayaks and canoes. The campground also offers activities such as camping, hiking, and berry picking. Nearby places include the Big Lava Bed, south of the campground; a trail takes hikers through a landscape dotted by pine forest and basalt lava formations.

The airport grounds permit fly-in camping. The Santiam Junction vicinity is listed by the National Register of Historic Places as the site of the Oregon Pacific Railroad Linear Historic District, which consists of roughly of the old railroad grade between Idanha and the line's Cascade Range summit. Geologically, much of the area is a lava bed created during a period of volcanic activity around 1000 B.C.

The main route was Damascus to Baghdad but local troubles and commercial opportunities often involved variations. After the Druze Revolt of 1925 a new route was required around the troubled area, Beirut-Haifa-Jerusalem-Dead Sea-Amman and Rutbah. This involved five-mile long stretches of lava bed which was very destructive of the cars. A better route of 650 miles was found of Beirut-Homs-Palmyra-Rutbah-Baghdad.

The area is home to 806 people and the Nisga'a Memorial Lava Bed Provincial Park. Gitlax̱t'aamiks is located overlooking a lava flow that erupted in the 18th century. The source for this lava flow was the Tseax Cone. In front of the Nisga'a Elementary Secondary School stands the Unity Totem Pole which, raised in 1977, was the first totem pole raised in the Nass Valley since the late 19th century.

Administratively, Hwadae is divided into one ŭp and 20 ri. The southern region is relatively flat, while the inland north is rugged, with mountains of approximately 1,000 meters. The Musudan-ri missile base is located on the coast near its namesake cape, which forms the northern end of the East Korea Bay. In April 2002, Paleolithic fossils of approximately 300,000 years age were reported to have been excavated from a lava bed in Hwadae.

Since its construction, constant emissions of heat and caustic gases have transformed much of the rock into clays (mostly kaolinite), iron oxides, sulfur-rich compounds and quartz. The present eruptive cone above was constructed sometime between 40,000 to 10,000 years ago. Since that time the volcano has erupted at least ten times, generally from above . One of the more recent flows issued from South Butte and created the long by wide A.G. Aiken Lava Bed.

Lava once flowed from the numerous volcanic cones that rise above the plateau, consisting mainly of overlapping shield volcanoes, spatter cones, and cinder cones, which averages in elevation. The wilderness' highest point is Lemei Rock (5,927 ft), whose crater now contains Lake Wapiki. Other prominent volcanic peaks include Bird Mountain, Sawtooth Mountain, Gifford Peak, East Crater, and Red Mountain. Big Lava Bed is the result of the most recent volcanic activity about 8,200 years ago.

Goose Lake, in the U.S. state of Washington, is located within the Gifford Pinchot National Forest. Travel to Goose Lake is by dirt road, along Forest Road 60, also called the Carson Guler Road, typically free of snow by late June. Fed by several streams, Goose Lake was dammed by a lava flow from Big Lava Bed, directly to the south. The lake is 58 acres in size and includes a boat launch and campground with 18 primitive campsites.

The Bosque de Tlalpan, also called the Parque Nacional Bosque de Pedregal, is fully surrounded by urban area, just south of the Anillo Periférico and between the highways heading to Cuernavaca and to Picacho-Ajusco. The Bosque de Tlalpan is filled with pines, oyamel fir, cedars, oaks and eucalyptus trees, which grow on a solidified lava bed. Wildlife includes eagles, falcons, squirrels and the Mexican mouse opossum. It has been open to the public since 1968.

2), 2014, removed 63 hectares from the Nisga'a Memorial Lava Bed Park to accommodate a pipeline to one of the proposed LNG facilities. Also, the Container Trucking Act, which created the office of the British Columbia Container Trucking Commissioner, was adopted as a result of the negotiations in the previous session's response to the Port of Vancouver strike. The Canadian Pacific Railway (Stone and Timber) Settlement Act extinguished all of Canadian Pacific Limited's stone and timber reservations in exchange for $19 million.

The southern half became the Columbia National Forest. The name was changed in 1949 to honor the first Chief of the Forest, Gifford Pinchot. In 1964, the lands around Mount Adams were set aside as a wilderness. Adams is home to the oldest building on the Gifford Pinchot National Forest, the Gotchen Creek Guard Station just south of the A. G. Aiken Lava Bed. Built in 1909, it served as the administrative headquarters of the Mount Adams District until 1916.

Lodgepole pine, alder, and other pioneer plants struggle to grow, seen sparsely growing between and amid towering rock piles, caves, and strange lava formations. Access into the interior of the lava bed is difficult, since there are no roads or trails crossing the lava field. Explorers who wish to venture deep within the lava flow are advised to choose their route carefully. Compasses are not always reliable, since local magnetic influences affect their magnetic performance in the vast expanse of rock.

Indian Heaven features both polygenetic and monogenetic volcanic activity; many of its volcanoes have only erupted once before coming extinct, while others have erupted several times. Approximately 50 eruptive centers lie within the Indian Heaven field, which also has approximately 40 lava flows. The field's eruptive output totals , with sporadic activity taking place for the past 700,000 years. The last volcanic activity in the field produced a large cinder cone, Big Lava Bed, as well as a voluminous lava and scoria flows about 9,000 years ago.

The rest of the crew wake just as Starbug plunges into the lava bed of the planet they were heading for. Before Starbug can burn up, it then ends up in an ocean created by the Mayflower. With Starbug damaged, the crew board the Mayflower and find several hundred vials of diverse viruses including positive ones that bestow luck on the infected for a time. Kochanski, after infecting herself for a short while, manages to find more luck virus as well as other vials that will come in handy.

Only one obvious flow appears on the south slopes of Adams, the A. G. Aiken Lava Bed. Other smaller flows exist in various locations around the mountain as well. The many other vents and volcanoes encompassed by the Mount Adams field include Glaciate Butte and Red Butte on the north, King Mountain, Meadow Butte, Quigley Butte, and Smith Butte on the south, with others interspersed throughout. Located a few miles north of Adams is Goat Rocks Wilderness and the heavily eroded ruins of a stratovolcano that is much older than Adams.

One of the longest trails on the Gifford Pinchot, Boundary Trail #1, has its eastern terminus in the Midway High Lakes area at Council Lake. Other trails in the area include the Council Bluff Trail #117, Green Mountain Trail #110, and East Canyon Trail #265. Several long trails pass through the Morrison Creek area on the south side of the mountain. The Snipes Mountain Trail #11 follows the eastern edge of the A. G. Aiken Lava Bed from the lower end for 6 miles to the Round the Mountain Trail.

Walking back to the forest through "Nomansland" - the lethal interface-area between land and sea - Gren is waylaid by a "morel", a sentient fungus which attaches itself to his head and forms a symbiotic relationship. After a power-struggle, Gren leaves the tribe with his girlfriend Poyly, also taken over by the morel. On their travels, they meet Yattmur of the Herder tribe, who live in caves in a congealed lava bed. At the "Skirt of the black mouth", an unknown creature with Siren-like capabilities almost leads them to their deaths.

The area near the cave entrance is dominated by Western juniper and Ponderosa pine with big sagebrush, bitterbrush, mountain mahogany, rabbitbrush, and a variety of desert grasses as the main ground cover. Common grasses in this area include Idaho fescue, bunch grass, and bluebunch wheatgrass."Devil's Garden Lava Bed Wilderness Study Area", Oregon Wilderness Environmental Impact Statement (Volume 2), Bureau of land Management, Department of Interior, Portland, Oregon, April 1985, p. 6-7. Townsend’s big-eared batsAnimals common in the forest around the cave include mule deer, pronghorn, coyotes, bobcats, cougar, and American black bear.

Detail of the Nili Patera dune field lying on a bed of solidified lava Location of Nili Patera Nili Patera is a dune field on Mars. It is located on top of a lava bed, at the site of an ancient volcano, the Nili Patera caldera of Syrtis Major, near the Martian equator, and it is one of the most active dune fields of Mars. Its location coordinates on Mars are 8.7° N latitude, 67.3° E longitude. It is being actively studied by the HiRISE camera, on board the Mars Reconnaissance Orbiter, at the rate of one image every six weeks.

For winter recreation, there are a number of Washington state sno-parks on the south side that are popular with snowmobilers and cross-country skiers. There are three sno-parks on Mount Adams south slope: Snow King, Pineside, and Smith Butte Sno-parks. The south side of the mountain, especially the A.G. Aiken Lava Bed, is especially popular with snowmobilers and skiers. The Mount Adams Recreation Highway (FR 80) is plowed all the way to Pineside and Snow King Sno-parks at about elevation for most of the year, as long as there is enough money in the Forest Service's winter budget.

Now known as the Columbia Plateau, this great lava bed of flood basalt covers much of Oregon, Washington and even parts of Idaho. Northern California's Modoc Plateau is a thinner basaltic flow which some geologists associate with the Columbia Plateau, but there are technical objections to this. The High Cascades took shape as a distinct mountain belt as a result of this upheaval and the bending of the thick blanket of volcanic rocks. During the next 10 million years, a series of new basaltic volcanic cones similar to the shield volcanoes now found in Hawaii were built.

Ciudad Universitaria (University City), Mexico, is the main campus of the National Autonomous University of Mexico (UNAM), located in Coyoacán borough in the southern part of Mexico City. Designed by architects Mario Pani and Enrique del Moral, it encloses the Olympic Stadium, about 40 faculties and institutes, the Cultural Center, an ecological reserve, the Central Library, and a few museums. It was built during the 1950s on an ancient solidified lava bed in Coyoacán called "El Pedregal" to replace the scattered buildings in downtown Mexico City where classes were given. It was completed in 1954 at a cost of approximately $25 million.

Later that day, Sheriff David Ward, accompanied by the Sheriff of Malheur County, Oregon, and the Sheriff of Tillamook County, Oregon, met with Ammon Bundy and Ryan Payne. The meeting occurred in what was described as "one of the most remote spots in Oregon," at a location along Lava Bed Road, approximately from the site of the occupation. In the meeting, which lasted between five and ten minutes, Ward repeated his earlier offer to provide safe passage to the militants to the Harney County line. Bundy rejected the offer, saying he and his confederates would hold out until the federal government had surrendered all of its land holdings to local residents.

The second Strong Angel (SA-II) was also held on a remote lava bed in Hawaii and, in 2004, pursued problems identified by members of the first Strong Angel team who were deployed to conflicts then underway in Afghanistan and Iraq. SA-II eventually incorporated 83 tasks designed to propose answers to problems seen in civil-military integration during those wartime deployments, including such topics as trans-boundary communications, civil-military transportation coordination, sustainable power provisioning, machine-based translation services, and competent cultural awareness. That set of tasks were addressed through the efforts of more than 60 staff on a remote and austere site on the lava beds north of Kailua-Kona, Hawaii and resulted in alterations in tactics, techniques, and procedures regarding international and coalition civil-military operations.

Nisga'a Memorial Lava Bed Provincial Park (Nisga'a: Anhluut'ukwsim Laxmihl Angwinga'asankswhl Nisga'a) is a provincial park in the Nass River valley in northwestern British Columbia, Canada, about 80 kilometres north of Terrace, and near the Nisga'a Villages of Gitlakdamix and Gitwinksihlkw. The park was established by Order in Council on April 29, 1992, expanded in 1995, included in the Nisga'a Treaty in 2000, and is the first park in the province to be jointly managed by the government and a First Nation.BC Parks An interpretive centre in a traditional Nisga'a longhouse informs visitors about the Nisga'a legend that accounts for the lava as well as geological causes. The park has waterfalls, pools, cinder cones, tree moulds, lava tubes, spatter cones, a lava-dammed lake, caves and other features created by lava flows.

It was designed by architects Mario Pani, Armando Franco Rovira, Enrique del Moral, Eugenio Peschard, Ernesto Gómez Gallardo Argüelles, Domingo García Ramos, and others such as Mauricio De Maria y Campos who always showed great interest in participating in the project. Architects De Maria y Campos, Del Moral, and Pani were given the responsibility as directors and coordinators to assign each architect to each selected building or constructions which enclose the Estadio Olímpico Universitario, about 40 schools and institutes, the Cultural Center, an ecological reserve, the Central Library, and a few museums. It was built during the 1950s on an ancient solidified lava bed to replace the scattered buildings in downtown Mexico City, where classes were given. It was completed in 1954, and is almost a separate region within Mexico City, with its own regulations, councils, and police (to some extent), in a more fundamental way than most universities around the world.

Mount Adams along Trail #20 just above Hellroaring Overlook, on the way to Iceberg Lake and Sunrise Camp The Round the Mountain Trail, the Pacific Crest Trail, and the Highline Trail when joined almost completely encircle the mountain, save for a 4-mile section known as "The Gap" on the east side of the Mountain in the Mount Adams Recreation Area. The Round the Mountain Trail extends from the Pacific Crest Trail on the southwest side of the Mount Adams Wilderness, and travels east over the A.G. Aiken Lava Bed before crossing into the Yakama Nation Mount Adams Recreation Area. It then proceeds to pass through Bird Creek Meadows before ending at the western edge of Hellroaring Canyon. Hikers can continue the round the mountain circuit by following Trail #20 to Hellroaring Overlook, then continue following the (now poorly defined) trail to Sunrise Camp, perched between the Mazama and Klickitat Glaciers at 8,000 feet.