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True or False.Numbers number 10 and 11.

True or False.Numbers number 10 and 11.

Applications and Investigations in Earth Science (9th Edition)
Applications and Investigations in Earth Science (9th Edition)
9th Edition
ISBN:9780134746241
Author:Edward J. Tarbuck, Frederick K. Lutgens, Dennis G. Tasa
Publisher:Edward J. Tarbuck, Frederick K. Lutgens, Dennis G. Tasa
Chapter1: The Study Of Minerals
Section: Chapter Questions
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True or False.Numbers number 10 and 11.
TOPIC VIDEO PRESENTATION: Using your viewing device, access from your flash drive the video presentation titled M5 U3 EXPLAIN VC. A corresponding PowerPoint Presentation titled M5 U3 EXPLAIN PP is provided for further study. After studying the provided resources, answer the succeeding WRITTEN WORK NO. 3 | Part 1 (11 points) | Second Grading. An answer sheet is provided at the end of this module. Explain Alternate Response: Shade letter A if the statement is correct. Otherwise, shade letter E. 1. "Plate" is synonymous to "continent". 2. All plates are presently moving in the same direction. 3. Continents drift through the ocean and oceanic currents are responsible for continental drift. 4. Plate tectonic processes cause sea-level to move up and down. 5. The age of ocean lithosphere decreases as an ocean ridge is approached. 6. The Earth is expanding; seafloor is created but never destroyed. 7. The entire seafloor is the same age 8. The oceanic ridge systems are the longest mountain ranges on Earth. 9. The oldest rocks on Earth are found in ocean basins. 10. The seafloor is flat or bowl-shaped and the deepest portion is in the middle. 11. The seafloor is the same age as the continents. at can happen to rocks when they are exposed to stress? Stress is the force applied to an object. In geology, stress is the force per unit area that is ced on a rock. The figure below shows three types of stresses acting on materials. How Rocks Respond to Differential Stress pe of tress TENSION (Tension causes stretching) SHEAR (Shear distorts rock) COMPRESSION (Compression causes shortening) shallow opthe ocks rittle cture At shallow depths shortening occurs by brittle deformation along faults where one rock mass is thrust over another. At shallow depths tensional stresses cause rocks to fracture and pull apart. At shallow depths shear stress causes offsets in crustal blocks along faults. deeper ustal pths ocks pr by Gle flow At deeper crustal levels where temperatures are high, shear stress distorts rock masses by ductile flow, At deeper crustal levels ntures are At deeper crustal levels where temperatures are ft forces
Transcribed Image Text:TOPIC VIDEO PRESENTATION: Using your viewing device, access from your flash drive the video presentation titled M5 U3 EXPLAIN VC. A corresponding PowerPoint Presentation titled M5 U3 EXPLAIN PP is provided for further study. After studying the provided resources, answer the succeeding WRITTEN WORK NO. 3 | Part 1 (11 points) | Second Grading. An answer sheet is provided at the end of this module. Explain Alternate Response: Shade letter A if the statement is correct. Otherwise, shade letter E. 1. "Plate" is synonymous to "continent". 2. All plates are presently moving in the same direction. 3. Continents drift through the ocean and oceanic currents are responsible for continental drift. 4. Plate tectonic processes cause sea-level to move up and down. 5. The age of ocean lithosphere decreases as an ocean ridge is approached. 6. The Earth is expanding; seafloor is created but never destroyed. 7. The entire seafloor is the same age 8. The oceanic ridge systems are the longest mountain ranges on Earth. 9. The oldest rocks on Earth are found in ocean basins. 10. The seafloor is flat or bowl-shaped and the deepest portion is in the middle. 11. The seafloor is the same age as the continents. at can happen to rocks when they are exposed to stress? Stress is the force applied to an object. In geology, stress is the force per unit area that is ced on a rock. The figure below shows three types of stresses acting on materials. How Rocks Respond to Differential Stress pe of tress TENSION (Tension causes stretching) SHEAR (Shear distorts rock) COMPRESSION (Compression causes shortening) shallow opthe ocks rittle cture At shallow depths shortening occurs by brittle deformation along faults where one rock mass is thrust over another. At shallow depths tensional stresses cause rocks to fracture and pull apart. At shallow depths shear stress causes offsets in crustal blocks along faults. deeper ustal pths ocks pr by Gle flow At deeper crustal levels where temperatures are high, shear stress distorts rock masses by ductile flow, At deeper crustal levels ntures are At deeper crustal levels where temperatures are ft forces
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