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Subphylum Vertebrata – Early Vertebrates and
Subphylum Vertebrata – Early Vertebrates and

... Major plates of Earth’s crust float on semi-molten upper mantle ...
EarthViewer Questions
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... 20. Name  two  (2)  supercontinents.   ____________________________________________  and  ___________________________________________   21. According  to  the  diagram,  where  is  new  plate  material  formed?   _____________________________________________________ ...
Chapter 3 – Rocks
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Plate Tectonics
Plate Tectonics

... 2. Wegner also noted that fossils from South America and Africa came from the same extinct animal. Both continents back then had the same climate and vegetation, today that is not the case. ...
The district is situated in a complex zone of intrusions on the
The district is situated in a complex zone of intrusions on the

... The district is situatedin a complexzone of intrusionson the boundarybetweentwo contrastingstructural domains. The rocks are composeddominantlyof Mesozoicgranitesand volcanics(Table 2; Figure 5) which are intrudedby a stronglyENE-WSWorientedporphyritic rhyolite dyke swarm. Palaeozoicsedimentaryrocks ...
Name Date
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... 2. divergent boundaries- The place where two plates move apart, or diverge, is called a divergent boundary. Most divergent boundaries occur at the mid-ocean ridge. Sea floor spreading is a result at a divergent boundary along a mid-ocean ridge. When a divergent boundary develops on land, two slabs o ...
Pre-Test: Chapter 7-Plate Tectonics
Pre-Test: Chapter 7-Plate Tectonics

... 3. Evidence for sea-floor spreading has come from a. fossils in South America and Africa. c. ancient climatic conditions. b. magnetic minerals on the ocean floor. d. the breakup of Pangaea. ...
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Plate Tectonics - Canvas by Instructure
Plate Tectonics - Canvas by Instructure

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... Tension builds up when one plate gets stuck as is subducts down into the mantle ...
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Chapter 4 - Igneous Rocks
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... • Incomplete melting of rocks is known as partial melting • Formation of basaltic magmas – Most originate from partial melting of ultramafic rock in the mantle at oceanic ridges – Large outpourings of basaltic magma are common at Earth’s surface ...
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... d. islands of Japan _____ 30. As island arcs become larger, they join to form one landmass, such as the islands that make up the a. Solomon Islands. b. Aleutian Islands. c. Channel Islands. d. islands of Japan. 31. Describe what happens as magma comes to the surface where plates move apart at mid-oc ...
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Study Guide Geology 303, SDSU Spring PEOPLE for TEST 1: 1
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... 36.(3)-mainshock: The largest earthquake in a sequence, preceded by foreshocks and followed by aftershocks. 37.(3)-normal fault: A dip-slip fault in which the upper fault block (hanging wall) has moved downward in response to tensional (pull-apart) stresses. 38.(3)-P (primary)-wave: The first seism ...
Earth Science Text Assignments
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... 35. What is sonar and what does it show about features beneath the ocean? Sonar is a device that bounces sound waves off underwater objects and records echoes of these sound waves. It allows the sea floor to be mapped. 36. Describe Harry Hess’s idea of “sea floor spreading”. At the mid-ocean ridge, ...
Plate Tectonics campus assessment File
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... supercontinent, and slowly drifted apart to their current locations over a long period of time. B. A theory by Alfred Wegener of how the continents were once a supercontinent and drifted to their current locations over a short period of time. C. A theory by Alfred Wegener of how the continents were ...
Thermal state of the lithosphere during Late Heavy Bombardment
Thermal state of the lithosphere during Late Heavy Bombardment

... (Germany) are part of the Central European Cenozoic Igneous Province (CECIP) and one of the seismically most active areas in Central Europe: frequent swarm earthquakes and massive degassing with increasing isotopic mantle signatures indicate subsurface magma migration or magmatic fluid circulation. ...
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Large igneous province



A large igneous province (LIP) is an extremely large accumulation of igneous rocks, including liquid rock (intrusive) or volcanic rock formations (extrusive), when hot magma extrudes from inside the Earth and flows out. The source of many or all LIPs is variously attributed to mantle plumes or to processes associated with plate tectonics. Types of LIPs can include large volcanic provinces (LVP), created through flood basalt and large plutonic provinces (LPP). Eleven distinct flood basalt episodes occurred in the past 250 million years, creating volcanic provinces, which coincided with mass extinctions in prehistoric times. Formation depends on a range of factors, such as continental configuration, latitude, volume, rate, duration of eruption, style and setting (continental vs. oceanic), the preexisting climate state, and the biota resilience to change.
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