shield volcano oor Noorse Bokmål
shield volcano
en
(geology) A large volcano, with shallow-sloping sides and a flattened dome, formed of successive eruptions of free-flowing lava; a lava dome
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skjoldvulkan
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type of volcano usually built almost entirely of fluid lava flows
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Cinder cones are commonly found on the flanks of shield volcanoes, stratovolcanoes, and calderas.
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Molokaʻi developed from two distinct shield volcanoes known as East Molokaʻi and the much smaller West Molokaʻi.
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The huge shield volcano Olympus Mons lies off the main bulge, at the western edge of the province.
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This rifting gave rise to large alkaline basalt shield volcanoes beginning about 30–31 million years ago.
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Ionian shield volcanoes or tholi are named after mythological figures associated with fire or with the nymph Io.
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Mount Hampton is a shield volcano with a circular ice-filled crater occupying much of the summit area.
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The island is the largest shield volcano in the South Pacific with recent eruptions in the early 1900s.
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Small shield volcanoes use the term tholus or the plural tholi, e.g. Inachus Tholus.
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The island is the result of repeated sequences of shield volcano construction followed by caldera collapse.
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The highest peak in the Sahara is Emi Koussi, a shield volcano in the Tibesti range of northern Chad.
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A lunar dome is a type of shield volcano that is found on the surface of the Earth's Moon.
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The volcano itself has eroded, but the dark types of rock on Saltstein are remnants of the defunct shield volcano.
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These mountains resemble small shield volcanoes, with steep slopes (6–7°) near a small, central caldera and shallow slopes along their margins.
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It stretches from northeast to southwest along the center of the peninsula and is made up of volcanoes, mostly shield volcanoes and stratovolcanoes.
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For example, geologists have identified nearly 100 cinder cones on the flanks of Mauna Kea, a shield volcano located on the island of Hawaii.
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The following table lists those positive topographic structures (mountains, plateaus, shield volcanoes, and layered plains) that have been given names by the International Astronomical Union.
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Finally, as in the case of Mauna Kea, the eruptions of a shield volcano become more explosive, producing cone-shaped heaps of volcanic cinders that dot the volcano.
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Other shield volcanoes with much shallower slopes are inferred from the morphology of several of Io's volcanoes, where thin flows radiate out from a central patera, such as at Ra Patera.
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It is a massive, mainly snow-covered shield volcano which is the highest and most imposing of the five volcanic mountains that comprise the Executive Committee Range of Marie Byrd Land.
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It was discovered, on the basis of data from Mars Global Surveyor, to be a low-relief shield volcano, but was formerly believed to be a plain, and was then known as Syrtis Major Planitia.
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The island is a shield volcano, although it is not known if it is still active, and it has been categorized as either Holocene or historic, based on date samples ranging from 0.1 to 0.35 million years ago.
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The Piton de la Fournaise, a shield volcano on the eastern end of Réunion Island, rises more than 2,631 m (8,632 ft) above sea level and is sometimes called a sister to Hawaiian volcanoes because of the similarity of climate and volcanic nature.
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Unlike similar features on Earth and Mars, these depressions generally do not lie at the peak of shield volcanoes and are normally larger, with an average diameter of 41 km (25 mi), the largest being Loki Patera at 202 km (126 mi).
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The most likely origin for the plains is through volcanic processes; their linear vent geometry, resembling terrestrial shield volcanoes, and distinct topographic margins suggest that the erupted liquid was very viscous, possibly a supercooled water/ammonia solution, with solid ice volcanism also a possibility.
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About 3800 years ago the shield volcano Ketildyngja was formed about 25 km south-east of Mývatn, and from it a huge lava flow, the Older Laxá-lava, spread over the southern part of the district, plunged down the Laxárdalur valley and flowed almost to the sea.
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40 sinne gevind in 11 ms. Hulle kom uit baie bronne en word nie nagegaan nie.