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earthquakes and volcanoes - Didattica Orizzonte Scuola
earthquakes and volcanoes - Didattica Orizzonte Scuola

... Earth’s crust is the layer of rock closest to the Earth’s surface. The crust is divided into a number of blocks of rock, called plates, that cover the planet. An earthquake is a sudden, violent shaking in Earth’s crust. It happens when two of these plates, under great pressure, move past each other ...
Chapter 4 Mt. St. Helens: A Case Study
Chapter 4 Mt. St. Helens: A Case Study

... velocities  decreased  and  they  turned  into  mudflows,  i.e.,  in  a  volcanic  setting,  a  lahar  composed mostly of material finer grained than about 0.06 mm (e.g., of a mixture of sand, silt,  and clay between about 20% to 80% will be silt sized or smaller).    Slumping and flowage of water‐s ...
(2006), Decreasing magmatic footprints of individual volcanoes in a
(2006), Decreasing magmatic footprints of individual volcanoes in a

... Southwestern Nevada Volcanic Field (not including known or inferred buried volcanoes). Pliocene volcanoes (magenta) include Thirsty Mountain (TM), Pliocene Crater Flat (PCF), and Buckboard Mesa (BM). Pleistocene volcanoes (red) include Makani (MC), Black Cone (BC), Red Cone (RC), SW and NE Little Co ...
Volcanoes - LessonSnips
Volcanoes - LessonSnips

... the magma chamber. Steam causes explosions that blow the rocks apart. The crater widens. Eventually it can fill with water to form a lake. Crater Lake in Oregon is a famous caldera-formed lake. Eventually the lava will form a mountain. This can happen on land or underwater. The islands of Hawaii wer ...
Diverging Plate Boundaries
Diverging Plate Boundaries

... 5. How far is the sea-floor spreading each year at the Mid-Atlantic Ridge? Tectonic Processes at the Mid-Ocean Ridge 1. The tectonic processes at diverging plate boundaries are less violent than at other types of boundaries. Read page 94 in your textbook and list the three reasons for this. ...
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Thehazardspresentedhavethegreatestimpactonthepoorestpeople

... Californian scientist commented of the L’Aquila earthquake ‘an earthquake of this magnitude in California wouldn’t have killed a single person’. The major reason L’Aquila was lethal was because of the collapse of old medieval buildings and more modern buildings with poor workmanship and poor land-us ...
Plate Tectonics
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... Constructive plate boundaries Constructive plate boundaries are caused when two plates move away from each other (diverge). When they move apart from each other a ‘gap’ is created. The gap is filled with hot, molten lava that solidifies when it reaches the surface (meeting either the sea or air). L ...
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Volcanism - MsMonroesScience

...  ________________________________________________________________________  It includes _____________________________________, two volcanoes in Italy.  Its general outlines correspond to the _________________________________ ________________________________________  At divergent plate boundaries ...
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Volcanism - FacultyWeb Support Center

... Chp 4: Volcanism VIII. Distinguishing Flows from Sills in Cross-section Chilled Margin – The solidified outer edge of a lava flow or an intrusive body such as a sill. As a lava flow flows across the surface of the earth, the first to solidify is the “margin that touches the relatively cold ground. ...
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... oceans constantly move at rates of centimeters per year in response to movements in the mantle. Major geological events, such as earthquakes, volcanic eruptions, and mountain building result from these plate motions. ...
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PlateTectwebquest

... massive eruptions have occurred during the past several thousand years, e.g., Mt. Mazama in Oregon, whose remains make up Crater Lake National Park. And once every few hundred thousand years, a truly gigantic eruption occurs, producing deposits such as California's Bishop Tuff and having profound lo ...
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... What landforms are found at different plate boundaries? • Both fold mountains and ocean trenches result from plates moving together. If both landforms occur in the same area, they are found in association with subduction. • If fold mountains occur by themselves, they are in areas where collision i ...
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... 11. An area of volcanic activity far from a tectonic plate boundary is called a(n) a. Mantle plume b. Island arc c. Cone d. Hot spot 12. The Hawaiian Islands are in the middle of a large tectonic plate with many volcanoes. The volcanoes are the direct result of the tectonic plate a. Applying great p ...
Magma - Cloudfront.net
Magma - Cloudfront.net

... 2. Mid-Ocean Ridges – tectonic plates are moving away from each other a. Occur along lithospheric plates. b. Site of where there is the greatest amount of magma that comes to the surface. c. The interconnected mid-ocean ridges that circle the earth form a major zone of volcanic activity. d. As plat ...
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- Hope`s Institutional Research Archive (HIRA)

... The first section, Geological Setting, places S. Miguel in the volcanic and tectonic contexts of the Azores and discusses its position astride the triple junction between the African, North American and Eurasian plates. Miranda et al. provide an overview of the regional tectonic setting based on geo ...
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... Stratovolcano collapse calderas are the most abundant, (~0.1-1 km deep, <~10 km diam.; VEI~4-7), caused by shallow magma chamber withdrawl (eg. Tambora 1815 Indonesia; Pinatubo 1991 Philippines; Azores). Volcanic field calderas (2~30 km diam., VEI~6-7) are caused by collapse with violent explosions ...
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... The Hawaiian archipelago, the most isolated island group of comparable size and topographic diversity on Earth, is about 4,000 kilometers from the nearest continent and 3,200 kilometers from the nearest high-island group (the Marquesas Islands of French Polynesia). The state of Hawaii consists of 1 ...
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... Scenario: You are a prominent Volcanologist and are studying a volcano that is on the verge of an eruption. You are trying to determine which type of volcano it is and whether it will be an explosive of non-explosive eruption. Here are your clues: gentle slopes, high magma volume, basaltic magma, lo ...
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... A. Because the poles are cold B. Because the equator is hot C. The light passing through at the equator illuminates a square meter and at the poles the light passing through is spread over many square meters on the surface. D. The light passing through at the equator illuminates many square meter an ...
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How and Where Volcanoes Form

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Earthquakes, Volcanoes, tsunamis

... surface. Under certain conditions, small amounts of mantle rock can melt, forming liquid magma. The magma rises upward through the crust, erupting at the surface as a volcano. Magma rises because it is less dense than the solid rock around and above it. ...
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... Magma that hardens beneath the surface forms batholiths, dome mountains, dikes and sills, which are eventually exposed by erosion This would be caused by magma that rises through the cracks in the upper crust, but fails to reach the surface ...
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...  Calculate the rate and direction of motion.  Describe features formed by gradual changes such as plate tectonics. Background: Mantle hot spots are areas where magma burns a hole through the crust in the middle of a tectonic plate. Volcanoes form above the hot spot. The interesting thing is that v ...
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Mid-Ocean Ridges que..

... 1. The tectonic processes at diverging plate boundaries are less violent than at other types of boundaries. Suggest three reasons for this. 2. The most common type of volcanic activity in the world occurs at the crest of mid-ocean ridges. These eruptions underwater create unique features and ecologi ...
Chapter 10 Volcanoes and Other Igneous Activity Section 1 The
Chapter 10 Volcanoes and Other Igneous Activity Section 1 The

... material may land near the vent and build a cone-shaped structure. The wind will carry smaller particles great distances. Viscous rhyolitic magmas are highly charged with gases. As the gases expand, pulverized rock and lava fragments are blown from the vent. Pyroclastic material is the name give to ...
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Ring of Fire



The Ring of Fire is an area in the basin of the Pacific Ocean where a large number of earthquakes and volcanic eruptions occur. In a 40,000 km (25,000 mi) horseshoe shape, it is associated with a nearly continuous series of oceanic trenches, volcanic arcs, and volcanic belts and/or plate movements. It has 452 volcanoes and is home to over 75% of the world's active and dormant volcanoes. The Ring of Fire is sometimes called the circum-Pacific belt.About 90% of the world's earthquakes and 81% of the world's largest earthquakes occur along the Ring of Fire. The next most seismically active region (5–6% of earthquakes and 17% of the world's largest earthquakes) is the Alpide belt, which extends from Java to the northern Atlantic Ocean via the Himalayas and southern Europe.All but 3 of the world's 25 largest volcanic eruptions of the last 11,700 years occurred at volcanoes in the Ring of Fire.The Ring of Fire is a direct result of plate tectonics and the movement and collisions of lithospheric plates. The eastern section of the ring is the result of the Nazca Plate and the Cocos Plate being subducted beneath the westward moving South American Plate. The Cocos Plate is being subducted beneath the Caribbean Plate, in Central America. A portion of the Pacific Plate along with the small Juan de Fuca Plate are being subducted beneath the North American Plate. Along the northern portion, the northwestward-moving Pacific plate is being subducted beneath the Aleutian Islands arc. Farther west, the Pacific plate is being subducted along the Kamchatka Peninsula arcs on south past Japan. The southern portion is more complex, with a number of smaller tectonic plates in collision with the Pacific plate from the Mariana Islands, the Philippines, Bougainville, Tonga, and New Zealand; this portion excludes Australia, since it lies in the center of its tectonic plate. Indonesia lies between the Ring of Fire along the northeastern islands adjacent to and including New Guinea and the Alpide belt along the south and west from Sumatra, Java, Bali, Flores, and Timor. The famous and very active San Andreas Fault zone of California is a transform fault which offsets a portion of the East Pacific Rise under southwestern United States and Mexico. The motion of the fault generates numerous small earthquakes, at multiple times a day, most of which are too small to be felt. The active Queen Charlotte Fault on the west coast of the Haida Gwaii, British Columbia, Canada, has generated three large earthquakes during the 20th century: a magnitude 7 event in 1929; a magnitude 8.1 in 1949 (Canada's largest recorded earthquake); and a magnitude 7.4 in 1970.
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