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Volcanoes and Igneous Activity Earth
Volcanoes and Igneous Activity Earth

... (smaller bodies are termed stocks) – Frequently form the cores of mountains ...
Volcanoes are classified as active or inactive
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Hazards Chapter 3a
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... destruction machines that we often make them out to be: (1) volcanoes frequently give us warning of their actions (2) many volcanoes are located in rural uninhabited places (3) if the eruption produces lava flows rather than poisonous gas or flaming particulates, it is more possible to evacuate and ...
chapter 4 volcanoes
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... Volcanoes are classified as active or inactive. Inactive volcanoes are older and have usually erupted many times. A volcano is described as active if it is currently erupting or expected to erupt eventually. Eruption Stage A volcanic eruption occurs when lava, gasses, and other subterranean matter c ...
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... https://www.youtube.com/watch?v=GTXG-ahu120 Mount Nyiragongo, Democratic Republic of Congo The world's most dramatic example of a lava flow through a major town. 17 January 2002 Nyiragongo is part of the East African Rift Valley, an area of many faults where the plates are being stretched as they mo ...
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... _____ 33. One of the most important warning signs of a volcanic eruption is a. a change in earthquake activity around the volcano. b. a change in air pressure around the volcano. c. a change in animal behavior around the volcano. d. increased steepness of the volcanic cone. 34. What are three causes ...
Volcanoes
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... • The composition of the subducted plate determines the composition of the lava – Subducted continental crust may melt and produce rhyolite lava – Subducted oceanic crust may melt and produce basalt or andesite lava – Subduction of sediments derived from the top of the subducted slab may produce a v ...
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Axial Seamount



Axial Seamount (also Coaxial Seamount or Axial Volcano) is a seamount and submarine volcano located on the Juan de Fuca Ridge, approximately 480 km (298 mi) west of Cannon Beach, Oregon. Standing 1,100 m (3,609 ft) high, Axial Seamount is the youngest volcano and current eruptive center of the Cobb-Eickelberg Seamount chain. Located at the center of both a geological hotspot and a mid-ocean ridge, the seamount is geologically complex, and its origins are still poorly understood. Axial Seamount is set on a long, low-lying plateau, with two large rift zones trending 50 km (31 mi) to the northeast and southwest of its center. The volcano features an unusual rectangular caldera, and its flanks are pockmarked by fissures, vents, sheet flows, and pit craters up to 100 m (328 ft) deep; its geology is further complicated by its intersection with several smaller seamounts surrounding it.Axial Seamount was first detected in the 1970s by satellite altimetry, and mapped and explored by Pisces IV, DSV Alvin, and others through the 1980s. A large package of sensors was dropped on the seamount through 1992, and the New Millennium Observatory was established on its flanks in 1996. Axial Seamount received significant scientific attention following the seismic detection of a submarine eruption at the volcano in January 1998, the first time a submarine eruption had been detected and followed in situ. Subsequent cruises and analysis showed that the volcano had generated lava flows up to 13 m (43 ft) thick, and the total eruptive volume was found to be 18,000–76,000 km3 (4,300–18,200 cu mi). Axial Seamount erupted again in April 2011, producing a mile-wide lava flow and fulfilling a 16-year cycle that had been predicted in 2006.
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