Ch4and5ReviewJeopardyGame
... What is a plate boundary called where one plate slides under another? ...
... What is a plate boundary called where one plate slides under another? ...
Plate Tectonics, Layers, and Continental Drift Mini
... 10. Geologist learn about the Earth’s interior by using sound waves. 11. Oceanic crust near the mid-ocean ridge is younger than oceanic crust farther away from the ridge. 12. Earth’s plates slip past each other at a transform boundary. 13. Continental crust is made of rock called granite. C. Fill-in ...
... 10. Geologist learn about the Earth’s interior by using sound waves. 11. Oceanic crust near the mid-ocean ridge is younger than oceanic crust farther away from the ridge. 12. Earth’s plates slip past each other at a transform boundary. 13. Continental crust is made of rock called granite. C. Fill-in ...
Volcano formation dbq
... landform. Unlike mountains, volcanoes can erupt causing lava and gasses to be expelled from deep inside the earth. As a result, volcanoes act as windows to the interior of the earth. Volcanoes are not randomly distributed over the Earth's surface. Most are concentrated on the edges of continents. Mo ...
... landform. Unlike mountains, volcanoes can erupt causing lava and gasses to be expelled from deep inside the earth. As a result, volcanoes act as windows to the interior of the earth. Volcanoes are not randomly distributed over the Earth's surface. Most are concentrated on the edges of continents. Mo ...
Core Case Study: Environmental Effects of Gold Mining
... Concept 14-4A All nonrenewable mineral resources exist in finite amounts, and as we get closer to depleting any mineral resource, the environmental impacts of extracting it generally become more harmful. Concept 14-4B An increase in the price of a scarce mineral resource can lead to increased su ...
... Concept 14-4A All nonrenewable mineral resources exist in finite amounts, and as we get closer to depleting any mineral resource, the environmental impacts of extracting it generally become more harmful. Concept 14-4B An increase in the price of a scarce mineral resource can lead to increased su ...
Convergent boundary
... plates pull slowly apart and magma effuses upward through the gap. Volcanoes are not generally found at strike-slip zones, where two plates slide laterally past each other. “Hot spot” volcanoes may form where plumes of lava rise from deep within the mantle to the Earth’s crust far from any plate mar ...
... plates pull slowly apart and magma effuses upward through the gap. Volcanoes are not generally found at strike-slip zones, where two plates slide laterally past each other. “Hot spot” volcanoes may form where plumes of lava rise from deep within the mantle to the Earth’s crust far from any plate mar ...
RESTLESS EARTH
... asthenosphere. These are pieces of a jigsaw puzzle. continental drift : A theory that continents can drift apart from one another and have done so in the past. It also explained why fossils of the same plant and animal species are found on both sides of the Atlantic Ocean. Ancient species could not ...
... asthenosphere. These are pieces of a jigsaw puzzle. continental drift : A theory that continents can drift apart from one another and have done so in the past. It also explained why fossils of the same plant and animal species are found on both sides of the Atlantic Ocean. Ancient species could not ...
PHS 111 Test 1 Review Answers Chapters 20-22
... Glacial deposits are characteristically: well sorted and well rounded; composed of unsorted, angular rock fragments; asymmetrical rock debris. The most powerful agent of erosion is: stream flow; glacial action; action from waves and ocean currents. Glacial striations are caused by: rocks embedded in ...
... Glacial deposits are characteristically: well sorted and well rounded; composed of unsorted, angular rock fragments; asymmetrical rock debris. The most powerful agent of erosion is: stream flow; glacial action; action from waves and ocean currents. Glacial striations are caused by: rocks embedded in ...
Ultramafic Rocks
... – Can not be the source of basaltic magmas by melting • Lherzolitic type – Mainly lherzolite , minor pyroxenite – May yield basaltic magmas by partial melting ...
... – Can not be the source of basaltic magmas by melting • Lherzolitic type – Mainly lherzolite , minor pyroxenite – May yield basaltic magmas by partial melting ...
Chapter 6 - Cloudfront.net
... can drift apart and have done so in the past • Alfred Wegener – created the continental drift theory ...
... can drift apart and have done so in the past • Alfred Wegener – created the continental drift theory ...
Katey Lesneski 5/16/10 ARCH0330 Final Project Consequences of
... Apart from remarks about the general ambiance, many sources note the beginnings of environmental impacts. In a letter, Horace Walpole proclaims that he has grown tired of the recent weather, as "it parches the leaves [and] makes the turf crisp" [Cunningham]. In Suffolk, Sir John Cullum wrote a detai ...
... Apart from remarks about the general ambiance, many sources note the beginnings of environmental impacts. In a letter, Horace Walpole proclaims that he has grown tired of the recent weather, as "it parches the leaves [and] makes the turf crisp" [Cunningham]. In Suffolk, Sir John Cullum wrote a detai ...
Rocks
... • Texture determined by rate of cooling – Intrusive = cools slowly • Course-grained texture • Ex: granite ...
... • Texture determined by rate of cooling – Intrusive = cools slowly • Course-grained texture • Ex: granite ...
Why do the terrestrial planets have different geological have
... How does the cooling of planets and potatoes vary with size? a) Larger makes it harder for heat from inside to escape b) Larger has a bigger ratio of volume (which needs to cool) to surface area (the surface is where cooling happens) c) Larger takes longer to cool d) All off the th above b ...
... How does the cooling of planets and potatoes vary with size? a) Larger makes it harder for heat from inside to escape b) Larger has a bigger ratio of volume (which needs to cool) to surface area (the surface is where cooling happens) c) Larger takes longer to cool d) All off the th above b ...
Climate-exodus expected in the Middle East and North
... limiting global warming to less than two degrees Celsius, agreed at the recent UN climate summit in often than they do now. Paris, will not be sufficient to prevent this scenario. The temperature during summer in the already very hot Middle East and North Africa will increase more than two times fas ...
... limiting global warming to less than two degrees Celsius, agreed at the recent UN climate summit in often than they do now. Paris, will not be sufficient to prevent this scenario. The temperature during summer in the already very hot Middle East and North Africa will increase more than two times fas ...
Plate Tectonics
... oceanic crust slowly moves away from the ridge, it becomes colder and denser. Exercise 7 What is the proper name for these igneous features? All oceans must start somewhere. They begin when the continental lithosphere becomes pulled apart, this causes it to stretch and get thinner. The surface of th ...
... oceanic crust slowly moves away from the ridge, it becomes colder and denser. Exercise 7 What is the proper name for these igneous features? All oceans must start somewhere. They begin when the continental lithosphere becomes pulled apart, this causes it to stretch and get thinner. The surface of th ...
Sea Floor Spreading NOTES 2016 Key
... 2. Mid-Ocean Ridge: The longest chain of __mountains___ in the world ...
... 2. Mid-Ocean Ridge: The longest chain of __mountains___ in the world ...
Study Guide Answer Key for Plate Tectonics
... 21. What happens when two plates carrying continental crust collide? Mountain ranges are formed because neither crust is dense enough to subduct under the other 22. What happens when a plate carrying continental crust and a plate carrying oceanic crust collide? The denser oceanic crust subducts und ...
... 21. What happens when two plates carrying continental crust collide? Mountain ranges are formed because neither crust is dense enough to subduct under the other 22. What happens when a plate carrying continental crust and a plate carrying oceanic crust collide? The denser oceanic crust subducts und ...
Name: Date: Period: ______
... Earth’s surface. Plate tectonics is the theory that describes how tectonic plates move and shape Earth’s surface. They move in different directions and at different rates relative to one another, and they interact with one another at their boundaries. Types of Plate Boundaries Divergent Boundary: tw ...
... Earth’s surface. Plate tectonics is the theory that describes how tectonic plates move and shape Earth’s surface. They move in different directions and at different rates relative to one another, and they interact with one another at their boundaries. Types of Plate Boundaries Divergent Boundary: tw ...
Slide 1 - MisterSyracuse.com
... Directions: This test is designed to let your teacher know how much information you have learned over the past few weeks, and to allow you to gauge this as well. Remember to think about your notes, and all the examples and demonstrations that we’ve done in class. Read each question carefully and com ...
... Directions: This test is designed to let your teacher know how much information you have learned over the past few weeks, and to allow you to gauge this as well. Remember to think about your notes, and all the examples and demonstrations that we’ve done in class. Read each question carefully and com ...
Tectonic–climatic interaction
Tectonic–climatic interaction is the interrelationship between tectonic processes and the climate system. The tectonic processes in question include orogenesis, volcanism, and erosion, while relevant climatic processes include atmospheric circulation, orographic lift, monsoon circulation and the rain shadow effect. As the geological record of past climate changes over millions of years is sparse and poorly resolved, many questions remain unresolved regarding the nature of tectonic-climate interaction, although it is an area of active research by geologists and palaeoclimatologists.