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    National Parks Assignment

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    honored as a World Heritage site." These Volcanoes are a National Park System because even if man tried to touch this land‚ it would all be melted by the burning lava. It isn’t possible for man to ruin the nature of these volcanoes. There is no need for protection because nature acts on its own creating these lava flows. Besides for the lava‚ the park includes the hawaiian culture‚ animals and foods that grow on the Islands. People believe the reason it is kept protected and is an importance to america

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    Notes on Natural Disasters

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    Energy Source of Natural Hazards Disasters occur where and when the earth’s natural processes concentrate energy and then release it‚ killing and causing destruction. Four energy sources make the earth an active body: 1) the Earth’s internal energy; 2) solar energy; 3)gravity; 4)the impact of extraterrestrial bodies The interior of the Earth holds a tremendous store of heat released primarily from the ongoing decay of radioactive elements. Earth’s internal energy flows unceasingly toward the

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    The lava flows from the Galapagos chain‚ while similar to the Hawaiian‚ do not form a line which is unusual in most volcanic hotspots. When people normally think of a volcano‚ the image is of a Composite or Stratovolcano. Composite volcanos have a conical shape built up by layers of hardened lava‚ pumice and volcanic ash. Composite volcanos typically have steep sides and their eruptions‚ while they

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    moor‚ among others. Sill: A tabular sheet intrusion where magma has intruded between older layers of sedimentary rock‚ beds of volcanic lava or tuff‚ or even along the direction of foliation in metamorphic rock. Good examples are the Salisbury crags in Edinburgh‚ which are formed by a sill partially exposed by the ice age. Dyke: Similar to a sill‚ except the lava has intruded along cracks and faults in one particular rock type. It cuts across layers‚ or through one layer or an unlayered rock‚ rather

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    Exam 2 Geo 1301

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    Devils Tower‚ a famous landmark/landform of the western Great Plains is? - A volcanic deposit‚ largely the remnants of a volcanic conduit 17. Which of the following volcanoes is most likely to contain pillow lava? -Deep-sea volcano 18. What is the international scientific term for a lava flow with a rough surface? -aa 19. The most common type of rock produced in Iceland are? -Mafic 20. The most abundant gas emitted by volcanoes are? -Water vapor (H2O) 21. A common rock composed largely

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    It has had 33 eruptions and in most of the eruptions‚ an earthquake has preceded the eruption. The most famous eruptions occurred in 1950 and 1984. On June 1‚ 1950‚ lava erupted from a 20 km long fissure along the middle portion of the rift zone. The lava

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    Explosive Diamond Cinder Cone‚ Washington County Shield Volcano Very gentle slopes; convex upward (shaped like a warrior’s shield) Large over 10s of kms across fluid lava flows (basalt) Quiet Cedar Hill‚ Box Elder County Strato Volcano Gentle lower slopes‚ but steep upper slopes; concave upward Large 1-10 km in diameter numerous layers of lava and pyroclastics Explosive Mount Belknap‚ Tushar Mountains‚ Paiute County Active Volcanoes A volcano will be classified as an active volcano if at the

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    Success in life

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    first time in around 9‚400 years on Friday 2nd May. The volcano is a caldera which is situated above a subduction zone where the Pacific Ocean plate is consumed beneath the South American continental crust. The volcano is composed of viscous rhyolitic lavas and pyroclastics and is typical of the magmas rising through the young fold mountains of the Andes. The eruption is said to have been triggered by a string of earthquakes that occurred on 30th April. Here is a diagram showing how Chaitén is located

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    explosive volcanic eruptions‚ producing fragmentary pyroclastic material or ash.  Basaltic Lava. Igneous Bedrock formed approximately 342 to 400 million years ago in the Carboniferous and Devonian Periods. Local environment previously dominated by eruptions of silica-poor magma. Eruptions of silica-poor magma. These rocks were formed from mobile magma‚ poor in silica. It rose to the surface and erupted as fluid lava from shallow-sided volcanoes and fissures. These eruptions are associated with the spreading

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    activity is due to magma from a hot spot nearby. The magma fills up in a reservoir two kilometers below the surface until a certain point at which it either explodes out the top‚ or it moves laterally forming dikes. These dikes‚ filled with solidified lava‚ shift leading to mountain deformation. There was almost a half-meter of displacement from the 1983 dike injection. The greatest earthquake recorded in Hawaiian history occurred on November 29‚ 1975. The displacement‚ which was between three and

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