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WHAT HAPPENS WHEN PIECES OF THE CRUST ARE FORCED TOGETHER ?
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Extension and injection of mantle material into crust Extension and injection of mantle material into crust
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Extension and injection of mantle material into crust Extension and injection of mantle material into crust Crustal Compression
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Extension and injection of mantle material into crust Extension and injection of mantle material into crust Crustal Compression Consideration of Conservation of Mass: Mass leaving Mantle Injected to Crust. Mass leaving Mantle Injected to Crust. Unless Crustal material is returned mantle in equal volume the Earth will grow larger and larger, but also “hollower” and “hollower”. ?
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CRUSTAL COMPRESSION
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Crustal Thickening
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CRUSTAL COMPRESSION Crustal Thickening
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CRUSTAL COMPRESSION Crustal Thickening Crustal Faulting
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Denser Crust to Mantle. Crustal Convergence and Compression. Heat Heat and Pressure
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CRUSTAL ROCKS Block 1 Block 2 Two Origins of Crustal Rocks: 1)Continental Crust – Lower density as “floated” to outside of Earth. 2)Oceanic Crust – Higher density as origin deeper in the mantle. Continental Crust Continental Crust Oceanic Crust
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CONVERGENT BOUNDARIES Two types of crustal rocks, thus three possible types of convergence: 1. Oceanic vs. Continental: e.g. Western South America
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CONVERGENT BOUNDARIES Two types of crustal rocks, thus three possible types of convergence: 1. Oceanic vs. Continental: e.g. Western South America 2. Oceanic vs. Oceanic: e.g. Japanese Islands
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CONVERGENT BOUNDARIES Two types of crustal rocks, thus three possible types of convergence: 1. Oceanic vs. Continental: e.g. Western South America 2. Oceanic vs. Oceanic: e.g. Japanese Islands 3. Continental vs. Continental: e.g. Himalayas
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1. GENERAL SETTING
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WESTERN SOUTH AMERICA Pacific OceanAtlantic OceanSouth America
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WESTERN SOUTH AMERICA Pacific OceanAtlantic OceanSouth America Mid- Atlantic Ridge
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WESTERN SOUTH AMERICA Pacific OceanAtlantic OceanSouth America Mid- Atlantic Ridge
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WESTERN SOUTH AMERICA Pacific OceanAtlantic OceanSouth America South American Plate African Plate Mid- Atlantic Ridge
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WESTERN SOUTH AMERICA Pacific OceanAtlantic OceanSouth America South American Plate African Plate Mid- Atlantic Ridge
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WESTERN SOUTH AMERICA Pacific OceanAtlantic OceanSouth America South American Plate Mid- Atlantic Ridge East Pacific Rise African Plate
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WESTERN SOUTH AMERICA Pacific OceanAtlantic OceanSouth America South American Plate Mid- Atlantic Ridge East Pacific Rise Nazca Plate Nazca Plate Pacific Plate African Plate
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WESTERN SOUTH AMERICA Pacific OceanAtlantic OceanSouth America South American Plate Mid- Atlantic Ridge East Pacific Rise Nazca Plate Nazca Plate Pacific Plate African Plate
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WESTERN SOUTH AMERICA Pacific OceanAtlantic OceanSouth America South American Plate Mid- Atlantic Ridge East Pacific Rise Nazca Plate Nazca Plate Pacific Plate African Plate CONVERGENCE AND CRUSTAL COMPRESSION
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WESTERN SOUTH AMERICA Pacific OceanAtlantic OceanSouth America Nazca Plate South American Plate African Plate Pacific Plate East Pacific Rise Mid- Atlantic Ridge Crustal Thickening
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WESTERN SOUTH AMERICA Pacific OceanAtlantic OceanSouth America Nazca Plate South American Plate African Plate Pacific Plate East Pacific Rise Mid- Atlantic Ridge Mato Grosso Brazilian Highlands Guiana Highlands Compressional Faulting
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WESTERN SOUTH AMERICA Pacific OceanAtlantic OceanSouth America Nazca Plate South American Plate African Plate Pacific Plate East Pacific Rise Mid- Atlantic Ridge Mato Grosso Brazilian Highlands Guiana Highlands More dense oceanic crust Sub-ducted beneath South America
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WESTERN SOUTH AMERICA Pacific OceanAtlantic OceanSouth America Nazca Plate South American Plate African Plate Pacific Plate East Pacific Rise Mid- Atlantic Ridge Mato Grosso Brazilian Highlands Guiana Highlands Deep ocean trench
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WESTERN SOUTH AMERICA Pacific OceanAtlantic OceanSouth America Nazca Plate South American Plate African Plate Pacific Plate East Pacific Rise Mid- Atlantic Ridge Mato Grosso Brazilian Highlands Guiana Highlands Shallow Earthquakes Deep Earthquakes Heat and pressure cause melting
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WESTERN SOUTH AMERICA Pacific OceanAtlantic OceanSouth America Nazca Plate South American Plate African Plate Pacific Plate East Pacific Rise Mid- Atlantic Ridge Mato Grosso Brazilian Highlands Guiana Highlands Heat and pressure cause melting Ocean sediments Andes
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WESTERN SOUTH AMERICA Pacific OceanAtlantic OceanSouth America Nazca Plate South American Plate African Plate Pacific Plate East Pacific Rise Mid- Atlantic Ridge Mato Grosso Brazilian Highlands Guiana Highlands Heat and pressure cause melting Andes Active Volcanoes
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03.05.b1
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03.09.a1
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2. JAPANESE ISLANDS GENERAL SETTING
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Pacific OceanAsiaSea of Japan JAPANESE ISLANDS
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East Pacific Rise Pacific OceanAsiaSea of Japan JAPANESE ISLANDS
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East Pacific Rise Nazca Plate Pacific Plate Pacific OceanAsiaSea of Japan JAPANESE ISLANDS
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East Pacific Rise Nazca Plate Pacific Plate Pacific OceanAsiaSea of Japan JAPANESE ISLANDS
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East Pacific Rise Nazca Plate Pacific Plate Eurasian Plate Pacific OceanAsiaSea of Japan JAPANESE ISLANDS
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East Pacific Rise Nazca Plate Pacific Plate Eurasian Plate Pacific OceanAsiaSea of Japan JAPANESE ISLANDS
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Eurasia Moved from North Atlantic Mid-ocean Ridge
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East Pacific Rise Nazca Plate Pacific Plate Eurasian Plate Pacific OceanAsiaSea of Japan JAPANESE ISLANDS CONVERGENCE AND CRUSTAL COMPRESSION
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East Pacific Rise Nazca Plate Pacific Plate Eurasian Plate Pacific OceanAsiaSea of Japan The Pacific Plate composed entirely of denser oceanic crust, is subducted beneath the oceanic fringe of the dominantly continental Eurasian Plate. JAPANESE ISLANDS
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East Pacific Rise Nazca Plate Pacific Plate Eurasian Plate Pacific OceanAsiaSea of Japan Ocean trench JAPANESE ISLANDS
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East Pacific Rise Nazca Plate Pacific Plate Eurasian Plate Pacific OceanAsiaSea of Japan Heat and Pressure cause melting JAPANESE ISLANDS
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East Pacific Rise Nazca Plate Pacific Plate Eurasian Plate Pacific OceanAsiaSea of Japan Heat and Pressure cause melting Shallow and deep earthquakes JAPANESE ISLANDS
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East Pacific Rise Nazca Plate Pacific Plate Eurasian Plate Pacific OceanAsiaSea of Japan Mountain building breaking ocean surface as a series of islands or “island arcs”. JAPANESE ISLANDS
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East Pacific Rise Nazca Plate Pacific Plate Eurasian Plate Pacific OceanAsiaSea of Japan Compressional faulting permits “recycled” oceanic crust to rise to the surface, producing active volcanoes. JAPANESE ISLANDS
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Island Arcs Ocean Trenches
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East Pacific Rise Nazca Plate Pacific Plate Eurasian Plate Pacific OceanAsiaSea of Japan As the Pacific plate is subducted it tends to “roll- back” southeastwards, pulling the Japanese Islands further off of Asia. “Push” “Pull” JAPANESE ISLANDS
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East Pacific Rise Nazca Plate Pacific Plate Eurasian Plate Pacific OceanAsiaSea of Japan Motion of Japanese islands away from Asia causes split of crust and “back arc spreading” beneath the sea of Japan. JAPANESE ISLANDS
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03.00.a1e
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Source: R.A. Kerr., 2011 Science, 332, p.911
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Displacement during Earthquake March 2011. Source: Simons et al., 2011 Science Express
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CREDIT: ADAPTED FROM THE EARTHQUAKE RESEARCH COMMITTEE, NATIONAL SEISMIC HAZARD MAPS FOR JAPAN (2010), HEADQUARTERS FOR EARTHQUAKE RESEARCH PROMOTION
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3. HIMALAYA GENERAL SETTING
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250 million years ago Eurasia Indian sub- continent
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EARLY DIVERGENCE AND CRUSTAL EXTENSION AfricaIndia HIMALAYA MOUNTAINS 250 million years ago Africa and India part of the same continental mass, Gondwanaland, also comprised of present day, South Africa, Australia and Antarctica.
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AfricaIndia Eurasia Eurasian Plate African Plate HIMALAYA MOUNTAINS 250 million years ago Eurasia (Europe and Asia), part of northern continental landmass including present day North America.
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AfricaIndia Eurasia Eurasian Plate African Plate HIMALAYA MOUNTAINS 250 million years ago Sea of Tethys Tethys Plate
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AfricaIndia Eurasia Eurasian Plate Tethys Plate African Plate HIMALAYA MOUNTAINS 250 million years ago CONVERGENCE (Ocean vs Continent) AND CRUSTAL COMPRESSION
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AfricaIndia Eurasia Eurasian Plate Tethys Plate African Plate HIMALAYA MOUNTAINS 250 million years ago Tethys Ocean crust subducted beneath Eurasian continent
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AfricaIndia Eurasia Eurasian Plate Tethys Plate African Plate HIMALAYA MOUNTAINS 250 million years ago Ocean trench
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AfricaIndia Eurasia Eurasian Plate Tethys Plate African Plate HIMALAYA MOUNTAINS 250 million years ago Melting under Heat and pressure
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AfricaIndia Eurasia Eurasian Plate Tethys Plate African Plate HIMALAYA MOUNTAINS 250 million years ago Earthquakes
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AfricaIndia Eurasia Eurasian Plate Tethys Plate African Plate HIMALAYA MOUNTAINS 250 million years ago Mountain building
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AfricaIndia Eurasia Eurasian Plate Tethys Plate African Plate HIMALAYA MOUNTAINS 250 million years ago Volcanoes
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AfricaIndiaEurasiaSea of Tethys Eurasian Plate Tethys Plate African Plate Indian Ocean Indo-Australian Plate HIMALAYA MOUNTAINS 150 million years ago
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AfricaIndiaEurasiaSea of Tethys Eurasian Plate Tethys Plate African Plate Indian Ocean Indo-Australian Plate HIMALAYA MOUNTAINS 75 million years ago
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AfricaIndiaEurasia Eurasian Plate Tethys Plate African Plate Indian Ocean Indo-Australian Plate Himalaya Mountains HIMALAYA MOUNTAINS Present
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Wilhan and Gaur, 2013. Buildings as weapons of mass destruction.www.sciencemag.org SCIENCE VOL 341 9, p618-619
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03.00.a1d INDUS GANGES INDIA PAKISTAN CHINA BANGLADESH HIMALAYA TIBET PLATEAU
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SICHUAN EARTHQUAKE CHINA, 2008.
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WORLD’S 100 HIGHEST MOUNTAINS RANK ELEVATION (m) Himalaya and Associated Ranges Andes
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03.02.b1 VOLCANOES WHY NO VOLCANOES?
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India Eurasia Eurasian Plate Tethys Plate Indian Ocean Indo-Australian Plate Himalaya Mountains WHAT’S HAPPENING NOW? Present Tibetan Plateau
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India Eurasia Eurasian Plate Tethys Plate Indian Ocean Indo-Australian Plate Himalaya Mountains WHAT’S HAPPENING NOW? Present Tibetan Plateau ?
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GLOBAL DISTRIBUTION OF EARTHQUAKES
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1. Western South America
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GLOBAL DISTRIBUTION OF EARTHQUAKES 2. Japanese Islands
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GLOBAL DISTRIBUTION OF EARTHQUAKES 3. Himalaya
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GLOBAL DISTRIBUTION OF VOLCANOES
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1. Western South America
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GLOBAL DISTRIBUTION OF VOLCANOES 2. Japanese Islands
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GLOBAL DISTRIBUTION OF VOLCANOES 3. Himalaya
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