Rock Cycle Interactive Activity
... While completing this section, you will transform one rock into another rock type by using the various processes from the rock cycle. As you complete each step, paste the cut out processes into the empty box to complete the transformation indicated. Note: Only paste the processes the screen indicate ...
... While completing this section, you will transform one rock into another rock type by using the various processes from the rock cycle. As you complete each step, paste the cut out processes into the empty box to complete the transformation indicated. Note: Only paste the processes the screen indicate ...
ExamView - FINAL-Exam-zeroth-version.tst
... Seafloor spreading at mid-ocean ridge. Comparing the ages of continental rocks with those of oceanic rocks. ...
... Seafloor spreading at mid-ocean ridge. Comparing the ages of continental rocks with those of oceanic rocks. ...
PLATE TECTONICS
... First thought to be the result of a permanently magnetized core. However, it has been shown that when any substance is heated above 500 degrees C it looses its permanent magnetism. Earth is a Dynamo - Outer core is a fluid consisting largely of iron, so it is an excellent conductor. Electromagnetic ...
... First thought to be the result of a permanently magnetized core. However, it has been shown that when any substance is heated above 500 degrees C it looses its permanent magnetism. Earth is a Dynamo - Outer core is a fluid consisting largely of iron, so it is an excellent conductor. Electromagnetic ...
Earth`s Internal Structure
... composed of less-dense grantic rock, is strongly deformed and includes the planet’s oldest rocks (billions of years in age). Oceanic crust is only about 8km thick, is composed of denser volcanic rock called basalt and is comparatively undeformed by folding and is geologically young (less than 200 mi ...
... composed of less-dense grantic rock, is strongly deformed and includes the planet’s oldest rocks (billions of years in age). Oceanic crust is only about 8km thick, is composed of denser volcanic rock called basalt and is comparatively undeformed by folding and is geologically young (less than 200 mi ...
CRCT Review Guide
... 103. About how deep have we been able to go into the Earth? 104. Name two differences between the mantle and the core. 105. How is continental crust different from oceanic crust? 106. What happens when ocean crust and continental crust collide? 107. What does the Theory of Continental Drift explain? ...
... 103. About how deep have we been able to go into the Earth? 104. Name two differences between the mantle and the core. 105. How is continental crust different from oceanic crust? 106. What happens when ocean crust and continental crust collide? 107. What does the Theory of Continental Drift explain? ...
Ocean Features PPT
... sediments originating mostly from the continents, usually lying at the foot of the continental rise • Flattest areas on the planet • Not tectonically active ...
... sediments originating mostly from the continents, usually lying at the foot of the continental rise • Flattest areas on the planet • Not tectonically active ...
Rock Cycle Teacher Notes
... 1. EXTRUSIVE (VOLCANIC): Cooled at the surface --Quick cooling leads to small crystals --Extrusive rocks also include glassy and frothy textures, formed when lava is ejected into the air and quickly cooled 2. INTRUSIVE (PLUTONIC): Cooled underground Slow cooling leads to Large Crystals Mineral Compo ...
... 1. EXTRUSIVE (VOLCANIC): Cooled at the surface --Quick cooling leads to small crystals --Extrusive rocks also include glassy and frothy textures, formed when lava is ejected into the air and quickly cooled 2. INTRUSIVE (PLUTONIC): Cooled underground Slow cooling leads to Large Crystals Mineral Compo ...
Chapter 11 Study GuideName: Section 11.1 – Rock Deformation
... _____________________________________________________________________________________ _____________________________________________________________________________________ 5. What are the two ways rocks permanently deform? _____________________________________________________________________________ ...
... _____________________________________________________________________________________ _____________________________________________________________________________________ 5. What are the two ways rocks permanently deform? _____________________________________________________________________________ ...
GEOL_106_lecture_03_..
... located beneath the Big Island of Hawaii (the active volcanoes) at the south eastern end of the Hawaiian Ridge. Many other hot spots are known, most in the ocean basins. Where hot spots occur beneath continental lithosphere, large volumes of rhyolite are produced (See figure 4.11 in your text). Hot ...
... located beneath the Big Island of Hawaii (the active volcanoes) at the south eastern end of the Hawaiian Ridge. Many other hot spots are known, most in the ocean basins. Where hot spots occur beneath continental lithosphere, large volumes of rhyolite are produced (See figure 4.11 in your text). Hot ...
Powerpoint Presentation Physical Geology, 10/e
... Features of the Sea Floor • Passive continental margins have a continental shelf, continental slope, and continental rise descending to the abyssal plain • Active continental margins have continental shelves and slopes, but the slope extends down into a deep oceanic trench • A mid-oceanic ridge sys ...
... Features of the Sea Floor • Passive continental margins have a continental shelf, continental slope, and continental rise descending to the abyssal plain • Active continental margins have continental shelves and slopes, but the slope extends down into a deep oceanic trench • A mid-oceanic ridge sys ...
Magma, Igneous Rocks, and Intrusive Activity Earth, 10e
... – Most originate from partial melting of mantle rocks at oceanic ridges – Large outpourings of basaltic magma are common at Earth’s surface. ...
... – Most originate from partial melting of mantle rocks at oceanic ridges – Large outpourings of basaltic magma are common at Earth’s surface. ...
Rock Summary Worksheet Key
... chemical compounds, which means that they are made of two or more elements. For example, the mineral sapphire is made up of aluminum and oxygen. A few minerals such as gold, silver and copper are made of a single element. Minerals are considered to be the building blocks of rocks. Rocks can be a com ...
... chemical compounds, which means that they are made of two or more elements. For example, the mineral sapphire is made up of aluminum and oxygen. A few minerals such as gold, silver and copper are made of a single element. Minerals are considered to be the building blocks of rocks. Rocks can be a com ...
Volcanoes - schmidtsciencepage
... island on the surface. (Ex. Hawaii) • The hot spot is stationary and the plate moves over it. ...
... island on the surface. (Ex. Hawaii) • The hot spot is stationary and the plate moves over it. ...
6-8 Plate Tectonics Activity
... Plate tectonics is the theory that the Earth’s surface (lithosphere) is made up of many plates that move over the Earth’s inner mantle due to convection currents. This theory was developed throughout the 1900s. Alfred Wegener first described it as the continental drift in 1912, but lacked evidence t ...
... Plate tectonics is the theory that the Earth’s surface (lithosphere) is made up of many plates that move over the Earth’s inner mantle due to convection currents. This theory was developed throughout the 1900s. Alfred Wegener first described it as the continental drift in 1912, but lacked evidence t ...
Greenland rocks provide evidence of Earth formation
... elements, caused this material to melt. As a result, 100 to 200 million years after its formation, the Earth must have been made up of an ocean of molten magma, in the center of which a metallic core formed. The ocean gradually cooled. The Earth's crust then appeared, and the process of continental ...
... elements, caused this material to melt. As a result, 100 to 200 million years after its formation, the Earth must have been made up of an ocean of molten magma, in the center of which a metallic core formed. The ocean gradually cooled. The Earth's crust then appeared, and the process of continental ...
Gluep-Honors
... see how it behaves. You can try poking quickly, poking slowly, shaping, pouring, etc. 2. Record your observations, indicating if the substance was more solid-like or liquid-like. ...
... see how it behaves. You can try poking quickly, poking slowly, shaping, pouring, etc. 2. Record your observations, indicating if the substance was more solid-like or liquid-like. ...
Methods and Equipment Used by Marine Geologists
... research began in the North Pacific and North Atlantic Oceans and now extends into both polar regions, the South and Southwest Pacific Islands, off New Zealand, and the Caribbean. In many respects, the present state of knowledge of offshore regions is comparable to what was known of the Western Stat ...
... research began in the North Pacific and North Atlantic Oceans and now extends into both polar regions, the South and Southwest Pacific Islands, off New Zealand, and the Caribbean. In many respects, the present state of knowledge of offshore regions is comparable to what was known of the Western Stat ...
The Earth
... • Has largest satellite (moon) compared to its own diameter; the Moon helps to keep the Earth’s tilt stable. • Abundant water in the atmosphere. • At the right distance from the Sun to have liquid water. • Only planet in the solar system to have open oceans. Because water can dissolve CO2, the Earth ...
... • Has largest satellite (moon) compared to its own diameter; the Moon helps to keep the Earth’s tilt stable. • Abundant water in the atmosphere. • At the right distance from the Sun to have liquid water. • Only planet in the solar system to have open oceans. Because water can dissolve CO2, the Earth ...
green ch9 lesson4
... (sed/o men/tor e) rock, rock that forms from cemented or pressed sediments. ...
... (sed/o men/tor e) rock, rock that forms from cemented or pressed sediments. ...
2003108 - Geological Society of America
... (as inferred from earthquakes by Pardo and Suárez, 1995) are included for reference. Approximate locations of Deep Sea Drilling Project legs 66 (L66), 67 (L67), and 84 (L84) are also indicated. Our geochemical database for the MVB (411 individual samples) concerns a wider area to the East and to the ...
... (as inferred from earthquakes by Pardo and Suárez, 1995) are included for reference. Approximate locations of Deep Sea Drilling Project legs 66 (L66), 67 (L67), and 84 (L84) are also indicated. Our geochemical database for the MVB (411 individual samples) concerns a wider area to the East and to the ...
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.