plate tectonic study guide
... --new oceanic crust 21. Tell me everything you know about sea-floor spreading (divergent boundary). --sea-floor spreading occurs at the mid-ocean ridge. New oceanic crust is formed at the mid-ocean ridge and the old crust is pushed to the sides. The old oceanic crust continues to get more dense as i ...
... --new oceanic crust 21. Tell me everything you know about sea-floor spreading (divergent boundary). --sea-floor spreading occurs at the mid-ocean ridge. New oceanic crust is formed at the mid-ocean ridge and the old crust is pushed to the sides. The old oceanic crust continues to get more dense as i ...
ES Practice quiz part 2 sect 3
... D. The following diagram shows how island arcs form. Label the type(s) of crust (include the word “crust” in each answer), and trench. Then, answer the questions that follow. Magma ...
... D. The following diagram shows how island arcs form. Label the type(s) of crust (include the word “crust” in each answer), and trench. Then, answer the questions that follow. Magma ...
Title Page Photo “Come forth into the light of things, —William Wordsworth
... Internal and External Geomorphic Processes • Relief is the difference between the highest and the lowest points of a place. E.g. saying that the distance btw Mt. Everest and the Mariana ...
... Internal and External Geomorphic Processes • Relief is the difference between the highest and the lowest points of a place. E.g. saying that the distance btw Mt. Everest and the Mariana ...
Differentiation of the Earth
... Before the formation of the Moon’s oldest known rocks, 4.47 billion years ago ...
... Before the formation of the Moon’s oldest known rocks, 4.47 billion years ago ...
Astro ch 20
... Continental drift: Entire Earth’s surface is covered with crustal plates, which can move independently ...
... Continental drift: Entire Earth’s surface is covered with crustal plates, which can move independently ...
How Earthquakes Happen
... surface beneath the instrument. From the data expressed in seismograms, scientists can determine the time, the epicenter, the focal depth, and the type of faulting of an earthquake and can estimate how much energy was released. The size of an earthquake is indicated by a number called its magnitude. ...
... surface beneath the instrument. From the data expressed in seismograms, scientists can determine the time, the epicenter, the focal depth, and the type of faulting of an earthquake and can estimate how much energy was released. The size of an earthquake is indicated by a number called its magnitude. ...
8.4 Plate Movement and Continental Growth
... A thick layer of sediments accumulates on the bottom of the planetary ocean. These sediments consist of dead organisms, debris carried from the surface of the continents by major rivers, or loose material carried by air currents from continents (dust particles, volcanic ashes, etc.) This material wi ...
... A thick layer of sediments accumulates on the bottom of the planetary ocean. These sediments consist of dead organisms, debris carried from the surface of the continents by major rivers, or loose material carried by air currents from continents (dust particles, volcanic ashes, etc.) This material wi ...
Plate Tectonics Vocabulary Words
... against each other, forming a mountain chain. If they are of unequal density, one plate usually sinks beneath the other in a subduction zone. The western coast of South America and the Himalayan Mountains are convergent plate boundaries. • Convergent plate boundaries form where lithospheric plates c ...
... against each other, forming a mountain chain. If they are of unequal density, one plate usually sinks beneath the other in a subduction zone. The western coast of South America and the Himalayan Mountains are convergent plate boundaries. • Convergent plate boundaries form where lithospheric plates c ...
Plate Tectonics Chapter 10
... 1. Continental-Oceanic= subduction 2. Continental-Continental= uplift 3. Oceanic-Oceanic= deep-ocean trench/island arc ...
... 1. Continental-Oceanic= subduction 2. Continental-Continental= uplift 3. Oceanic-Oceanic= deep-ocean trench/island arc ...
This is another Regents Review Packet to help you.
... 6. Why do trees and other plants help keep soil from eroding away? 7. The MOVEMENT of weathered material is called E____________. 8. The 4 methods of erosion are: 9. When running water has a greater gradient (slope) and discharge (volume), what happens to its velocity (speed)? ...
... 6. Why do trees and other plants help keep soil from eroding away? 7. The MOVEMENT of weathered material is called E____________. 8. The 4 methods of erosion are: 9. When running water has a greater gradient (slope) and discharge (volume), what happens to its velocity (speed)? ...
Plate Tectonics Review Worksheet
... 1. Continental Drift: A theory proposed by Alfred Wegner that said all continents were once joined 300 million years ago in a single land mass called Pangaea. Over time the continents moved to their present day locations. 2. What are four pieces of evidence for continental drift? Fossils, puzzle fit ...
... 1. Continental Drift: A theory proposed by Alfred Wegner that said all continents were once joined 300 million years ago in a single land mass called Pangaea. Over time the continents moved to their present day locations. 2. What are four pieces of evidence for continental drift? Fossils, puzzle fit ...
CGF3M - mr
... Create and explain diagram(s) showing the TECTONIC PLATES related to your earthquake or volcano’s existence. You may need to create or produce a plate tectonic map of your region to show the forces creating your volcano. These should clearly show which plates are moving to ‘create’ your event. - Pro ...
... Create and explain diagram(s) showing the TECTONIC PLATES related to your earthquake or volcano’s existence. You may need to create or produce a plate tectonic map of your region to show the forces creating your volcano. These should clearly show which plates are moving to ‘create’ your event. - Pro ...
Fault - Cloudfront.net
... Tension – The stress that occurs when forces act to stretch an object. An example of this is when two tectonic plates pull away from each other. ...
... Tension – The stress that occurs when forces act to stretch an object. An example of this is when two tectonic plates pull away from each other. ...
The Theory of Tectonic Plates
... slab pull, and convection. Since mid-ocean ridges have higher oceanic lithosphere, it causes a downhill motion to outside oceanic lithosphere which is called ridge push. A slab pull is a downward pulling motion since oceanic crust is denser than the asthenosphere and the oceanic crust will sink into ...
... slab pull, and convection. Since mid-ocean ridges have higher oceanic lithosphere, it causes a downhill motion to outside oceanic lithosphere which is called ridge push. A slab pull is a downward pulling motion since oceanic crust is denser than the asthenosphere and the oceanic crust will sink into ...
Dynamic Planet Test
... 26. Which of the following would be first to crystallize as magma cools? a. Amphibole b. Pyroxene c. Olivine d. Quartz 27. What is the primary cause of delamination? a. The instability caused by the difference in density of the lithosphere and asthenosphere b. Accretion due to interplate forces c. ...
... 26. Which of the following would be first to crystallize as magma cools? a. Amphibole b. Pyroxene c. Olivine d. Quartz 27. What is the primary cause of delamination? a. The instability caused by the difference in density of the lithosphere and asthenosphere b. Accretion due to interplate forces c. ...
Dynamic Planet Test 1. Label the plates on the map: (1 point each) A
... 26. Which of the following would be first to crystallize as magma cools? a. Amphibole b. Pyroxene c. Olivine d. Quartz 27. What is the primary cause of delamination? a. The instability caused by the difference in density of the lithosphere and asthenosphere b. Accretion due to interplate forces c. ...
... 26. Which of the following would be first to crystallize as magma cools? a. Amphibole b. Pyroxene c. Olivine d. Quartz 27. What is the primary cause of delamination? a. The instability caused by the difference in density of the lithosphere and asthenosphere b. Accretion due to interplate forces c. ...
Plate Boundaries foldable
... falls back down to the core. This movement causes tectonic plates to meet at plate boundaries . ...
... falls back down to the core. This movement causes tectonic plates to meet at plate boundaries . ...
“I Can” – Plate Tectonics Objectives – Learning Target Analysis
... E3.1B Explain the relationship between the rock cycle and plate tectonics theory in regard to the origins of igneous, sedimentary, and metamorphic rocks – section 6.4. E3.2A Describe the interior of the Earth (in terms of crust, mantle, inner and outer cores) and where the magnetic field of the Eart ...
... E3.1B Explain the relationship between the rock cycle and plate tectonics theory in regard to the origins of igneous, sedimentary, and metamorphic rocks – section 6.4. E3.2A Describe the interior of the Earth (in terms of crust, mantle, inner and outer cores) and where the magnetic field of the Eart ...
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.