Chapter 8 - Plate Tectonics - Quiz Questions (#1- #6)
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Back - Answer |
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Q1-1: Who was Alfred Wegener? |
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A1-1: German climatologist who wrote 1915 book, Origins of the Continents and Oceans, and hypothesized that Earth's continents were once connected as a large supercontinent called Pangaea. |
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Q1-2: Alfred Wegener thought that all continents were once connected. Explain three (3) observations that led to this belief. |
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A1-2: (1) Eastern US coal beds match southern Europe coal beds; (2) South America plant fossils match plant fossils in Africa, India, Australia, & Australia; (3) Reptile fossils in South America match with ones in Africa; (4) Early mammal fossils in South America match those in Africa; (5) North American mountain ranges match those in Africa & South America; (6) Warm, dry climate evidence in Antarctica |
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Q1-3: Why did scientists reject Wegener’s idea of continental drift? |
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A1-3: Wegener could not identify a force strong enough to push continents. |
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Q1-4: The development of the theory of plate tectonics is a good example of the application of the scientific process. a. How did Wegener follow this process? b. When scientists rejected continental drift, were they using the scientific process? Why or why not? |
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A1-4: (a) He made observations and then stated a hypothesis; (b) Yes, since they could not prove his hypothesis, they had to conclude that it was not correct. |
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Q1-5: List the animal fossils found on each continent based on the graphics on page 160. |
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A1-5: North America - none; South America - Cynognathus, Mesosaurus, and Lystrosaurus; Europe - none; Africa - Cynognathus, Lystrosaurus, Mesosaurus; Asia - Lystrosaurus; Australia - none; Antarctica - Lystrosaurus |
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Q1-6: A long time ago, glaciers covered parts of some of the continents. Why aren’t glaciers on these continents today? |
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A1-6: The continents have moved more towards the equator. |
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Q2-1: Explain
why magnetic patterns are important evidence for plate tectonics. |
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A2-1: Parallel patterns of magnetic stripes occur in rocks on either side of mid-ocean ridges. New rock appears at the center of the ridge. This helps to prove sea floor spreading |
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Q2-2: How were mid-ocean ridges discovered? |
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A2-2: Harry Hess, a geophysicist and naval officer discovered them while mapping the ocean floor. |
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Q2-3: What was Harry Hess’ hypothesis regarding the ocean floor and how it was made? |
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A2-3: That new sea floor is made at the mid-ocean ridges. Newer rock is less dense. The older rock far away from the ridge is more dense and so sinks back into the mantle at subduction trenches, pulling the plate behind it. |
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Q2-4: What two discoveries supported Hess’ hypothesis? |
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A2-4: (1) matching magnetic patterns on either side of mid-ocean ridges; and, (2) younger rock in the center and older rock farther away from the ridge. |
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Q2-5: What is the study of lithospheric plates called? |
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A2-5: Plate tectonics |
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Q2-6: Over what surface do lithospheric plates move? |
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A2-6: aesthenosphere |
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Q2-7: Name the two types of lithospheric plates & describe them. |
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A2-7: granitic continental plates and basaltic oceanic plates |
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Q2-8: What
are some questions that are answered by tectonic plates? |
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A2-8: This theory helps explain earthquakes and volcanoes |
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Q2-9: What is the source of energy that drives the movement of plates? |
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A2-9: Heat from the core of the Earth |
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Q2-10: Do lithospheric plates move quickly or slowly? Explain. |
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A2-10: Slowly -- about as fast as a fingernail grows |
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Q2-11: Describe the process of subduction in your own words. What causes it to happen? |
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A2-11: Heavier, denser plates sink into mantle and slide under less dense and lighter plates (usually continental) |
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Q2-12: Name an island chain formed by a mantle plume hot spot. Describe the process of how it forms. |
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A2-12: Hawaiian Islands. Mantle plume stays in one place and as ocean plate moves northwest across it, magma squirts up through plate to create a new lava island. |
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Q2-13: What effect is the mid-Atlantic ridge having on the country of Iceland? |
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A2-13: It is splitting it apart. A rift is appearing in the middle of the country. It is the cause of Iceland's geothermal activity. |
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Q2-14: When Pangaea broke apart it is thought it divided into two continents. What were they called and what do the names mean? |
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A2-14: Laurasia split into Laurentia (North America) and Eurasia; Gondwana - named by Eduard Suess after a region in eastern India. |
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Q3-1: What are the three types of plate boundaries and what does each do in relation to other plate boundaries? |
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A3-1: (a) Convergent - coming together; (b) Divergent - separating; (c) Transform - sliding past each other |
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Q3-2: What
kind of boundary is a mid-ocean ridge? |
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A3-2: Divergent boundary |
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Q3-3: What
is pillow lava and where is it found? |
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A3-3: Round-type lava flows created under water. Water cools the surface of lava and hot lava underneath causes the surface to balloon out |
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Q3-4: What
is a place (on land) where divergent boundaries can be found? Give an
example
of a divergent boundary on land. |
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A3-4: African rift boundary and the Red Sea |
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Q3-5: What happens when ocean plates come together? What landform does this event create? |
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A3-5: One subducts under the other and a trench is formed |
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Q3-6: What two (2) features of a plate determine whether a plate will subduct under another plate? |
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A3-6: The age of the plate and whether it is made of granite or basalt |
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Q3-7: Which
is more buoyant, a continental plate or oceanic plate? |
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A3-7: Continental plate |
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Q3-8: What happens when two continental plates collide? Give an example of continents colliding today. |
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A3-8: Land crumples and forms mountains (Himalayan Mountains) |
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Q3-9: Why are transform faults harder to find than divergent and convergent boundaries? |
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A3-9: They leave few clues to show their location and they don't occur in a single straight line. |
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Q3-10: What are three clues to finding transform faults? |
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A3-10: (1) offsets; (2) earthquakes; (3) small valleys or ponds |
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Q4-1: What does the term -- metamorphism -- mean? |
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A4-1: To change the form of something |
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Q4-2: What two things can cause metamorphic rock formation? |
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A4-2: Heat and pressure |
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Q4-3: What is contact metamorphism? |
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A4-3: When rocks come into contact with magma without much pressure being involved |
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Q4-4: Look at the rock images on page 175. Which image is most likely to be a metamorphic rock? Explain your answer. |
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A4-4: Sample A -- wavy lines indicate high pressure |
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Q4-5: Metamorphic rocks are commonly formed at what kind of plate boundary? |
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A4-5: convergent plate boundaries |
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Q4-6: In which location would you be most likely to find a metamorphic rock? |
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A4-6: On a mountain |
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Q4-7: At what type of boundary can limestone be metamorphosed into marble? |
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A4-7: At a convergent plate boundary |
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Q4-8: a. Formed from particles of sand & soil; b. Formed after a volcano erupts; c. Formed at a subduction zone |
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A4-8: (a) sedimentary; (b) igneous; (c) metamorphic |
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Q5-1: Means “all land” & is the name for the great landmass that existed 245 million years ago. |
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A5-1: Pangaea |
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Q5-2: Idea that the continents move aorund on Earth’s surface. |
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A5-2: continental drift |
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Q5-3: The study of Earth’s lithospheric plates. |
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A5-3: plate tectonics |
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Q5-4: Layer of Earth made of granite. |
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A5-4: continental plates |
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Q5-5: The sinking process that completes the lower mantle convection cell. |
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A5-5: subduction |
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Q5-6: What moves over the aesthenosphere? |
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A5-6: lithospheric plates |
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Q5-7: Undersea features where new ocean floor is created. |
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A5-7: mid-ocean ridges |
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Q5-8: Idea that Hess proposed. |
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A5-8: sea-floor spreading |
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Q5-9: Thin layer made of basalt. |
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A5-9: oceanic plates |
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Q5-10: Rises to the surface & may create a volcano. |
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A5-10: mantle plume |
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Q5-11: Type of boundary where mountains form. |
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A5-11: convergent boundary |
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Q5-12: Type of boundary where mid-ocean ridges form. |
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A5-12: divergent boundary |
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Q5-13: Type of boundary where earthquakes & offsetting occur. |
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A5-13: transform boundary |
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Q5-14: Feature created when one lithospheric plate subducts under another. |
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A5-14: trench |
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Q5-15: Type of rock created when sedimentary rocks are exposed to intense heat and pressure. |
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A5-15: metamorphic rock |
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Q5-16: How do fossils support the idea of continental drift? |
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A5-16: Fossils are records of plants and animals that lived on continents in the past. Their age and distribution indicate continents that at one time were next to each other. |
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Q5-17: Where would you find the oldest and youngest rocks on the sea floor? |
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A5-17: Oldest - furtherest away from the ridge; Youngest - closest to the ridge |
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Q5-18: List the 3 types of plate boundaries. California’s San Andreas Fault represents which type of boundary? |
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A5-18: Convergent, divergent, transform; transform |
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Q6-1: The idea that continents move around on Earth's surface. |
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A6-1: continental drift |
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Q6-2: An ancient, huge landmass composed of earlier forms of today's continents; an ancient supercontinent. |
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A6-2: Pangaea |
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Q6-3: Theory explaining how plates on the Earth's surface move. |
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A6-3: plate tectonics |
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Q6-4: Published Origins of Continents and Oceans in 1915 to explain continental drift. |
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A6-4: Alfred Wegener |
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Q6-5: A long chain of undersea mountains |
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A6-5: mid-ocean ridge |
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Q6-6: The remains or impression of a living thing of a former geologic age, preserved in stone |
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A6-6: fossil |
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Q6-7: Hypothesis that new sea floor is created at mid-ocean ridges. |
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A6-7: sea floor spreading |
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Q6-8: Large pieces of Earth's lithosphere that move over the aethenosphere. |
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A6-8: lithospheric plate |
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Q6-9: Thin, dense lithospheric plates that are made of basalt and form the ocean floor. |
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A6-9: oceanic plate |
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Q6-10: Thick, less-dense lithospheric plates that are made of granite and form the continents. |
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A6-10: continental plate |
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Q6-11: A process that involves a lithospheric plate sinking into the mantle and pulling the plate behind it. |
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A6-11: subduction |
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Q6-12: Heated lower mantle rock that rises toward the lithosphere because it is less dense than surrounding mantle rock. |
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A6-12: mantle plume |
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Q6-13: A lithospheric plate boundary where two plates move apart. |
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A6-13: divergent boundary |
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Q6-14: A lithospheric plate boundary where two plates come together. |
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A6-14: convergent boundary |
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Q6-15: A lithospheric plate boundary where two plates slide by each other. |
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A6-15: transform boundary |
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Q6-16: A divergent boundary that forms on land. |
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A6-16: rift valley |
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Q6-17: A valley in the ocean created where one lithospheric plate subducts under another. |
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A6-17: trench |
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Q6-18: Evidence of a transform fault where the movement of the fault will break or "offset" the feature.... as in a zigzag creek. |
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A6-18: offsetting |
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Q6-19: A scientist who studies how lithospheric plates move and change shape. |
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A6-19: geodynamacist |
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Q6-20: A rock formed from another kind of rock due to heat and pressure. |
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A6-20: metamorphic rock |
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Q6-21: When magma comes in contact with another type of rock, causing a change in structure due to high heat. |
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A6-21: contact metamorphism |
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Q6-22: Rocks that are made of sediments. |
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A6-22: sedimentary rock |
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Q6-23: Rocks that are formed from magma or lava. |
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A6-23: igneous rock |
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Q6-24: A Cluster of tar pits in the urban heart of Los Angeles, CA. Asphalt or tar (brea in Spanish) has seeped up from the ground in this area for tens of thousands of years. The tar is often covered with water. Animals that came to drink the water fell in, sank in the tar, died, and were preserved. |
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A6-24: La Brea tar pits |
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Q6-25: Latin name for sabre-toothed cat. |
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A6-25: Smilodon Californicus |