stratovolcano oor Noorweegse Nynorsk

stratovolcano

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(geology) A tall conical volcano, composed of layers (or strata) of hardened lava, tephra and ash.

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stratovulkan

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tall, conical volcano built up by many layers (strata) of hardened lava
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They range in shape from shield volcanoes with broad, shallow slopes formed from predominantly effusive eruptions of relatively fluid basaltic lava flows, to steeply-sided stratovolcanoes (also known as composite volcanoes) made of alternating layers of ash and more viscous lava flows typical of intermediate and felsic lavas.
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The town is located between the volcanic Melandiz Mountains, which include the Mount Hasan stratovolcano near the city of Aksaray to the north, and the Niğde Massif to the south-southeast.
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The 3,718 m (12,198 ft) summit of Teide itself, and its sister stratovolcano Pico Viejo (3,134 m (10,282 ft)), are both situated in the eruptions[edit]
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The 3,718 m (12,198 ft) summit of Teide itself, and its sister stratovolcano Pico Viejo (3,134 m (10,282 ft)), are both situated in the the caldera and are derived from eruptions later than this prehistoric explosion.
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Osorno Volcano is a 2,652-metre (8,701 ft) tall conical stratovolcano lying between Osorno Province and Llanquihue Province, in Los Lagos Region of Chile.
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Stratovolcanoes or composite volcanoes are tall conical mountains composed of lava flows and other ejecta in alternate layers, the strata that give rise to the name. Stratovolcanoes are also known as composite volcanoes, created from several structures during different kinds of eruptions.
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Acotango is the central and highest of a group of stratovolcanoes straddling the border of Bolivia and Chile.
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Unlike shield volcanoes, stratovolcanoes are characterized by a steep profile and periodic, explosive eruptions and quiet eruptions.
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Mount Ruapehu, or just Ruapehu, is an active stratovolcano at the southern end of the Taupo Volcanic Zone in New Zealand.
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A stratovolcano, also known as a composite volcano,[1] is a tall, conical volcano built up by many layers (strata) of hardened lava, tephra, pumice, and volcanic ash.
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Because siliceous magmas are so viscous, they tend to trap volatiles (gases) that are present, which cause the magma to erupt catastrophically, eventually forming stratovolcanoes.
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Lava domes are one of the principal structural features of many stratovolcanoes worldwide.
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A stratovolcano, also known as a composite volcano,[1] is a conical volcano built up by many layers (strata) of hardened lava, tephra, pumice, and volcanic ash.
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A stratovolcano, also known as a composite volcano,[1] is a conical volcano built up by many layers (strata) of hardened lava, tephra, pumice, and volcanic ash.
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A view of the stratovolcano of Pico at sunset Historical eruptions of Pico have occurred from vents on its flanks rather than the summit crater.
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The magma forming stratovolcanoes rises when water trapped both in hydrated minerals and in the porous basalt rock of the upper oceanic crust is released into mantle rock of the asthenosphere above the sinking oceanic slab.
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Unlike shield volcanoes, stratovolcanoes have a steep slope and periodic, explosive eruptions.
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Mount Erciyes (Turkish: Erciyes Dağı; derived from the ancient Greek name Argaeos; Latinized as Argaeus by the ancient Romans) is a massive stratovolcano located 25 km (16 mi) to the south of Kayseri in Turkey.
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A stratovolcano, also known as a composite volcano,[1] is a conical volcano built up by many layers (strata) of hardened lava, tephra, pumice and ash.
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When the magma nears the top surface, it pools in a magma chamber within the crust below the stratovolcano.
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The island is a basaltic andesite stratovolcano, and the latest crater, about 152 metres (500 ft) across and 61 metres (200 ft) deep, formed explosively some time between 1968 and 1984.
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stratovolcano, also known as a composite volcano,[1] is a tall, conical volcano built up by many layers (strata) of hardened lava, tephra, pumice, and volcanic ash.
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The stratovolcano rises to a height of 985 metres (3,232 ft) and is the highest point on the island.
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The 3,718 m (12,198 ft) summit of Teide itself, and its sister stratovolcano Pico Viejo (3,134 m (10,282 ft)), are both situated in the northern half of the caldera and are derived from eruptions Potential eruptionsEdit
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The 3,718 m (12,198 ft) summit of Teide itself, and its sister stratovolcano Pico Viejo (3,134 m (10,282 ft)), are both situated in the northern half of the caldera and are derived from eruptions later than this prehistoric explosion.
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