DQuestion 31 Which of these features are not found at convergent plate boundaries? O subduction zones island arcs mid ocean ridges O venches D Question 32 When viewed from above (map view) the row of volcanoes produced at a subduction zone is ar shaped because The descending plate is curved The descending plate is going down at an angle The edges of the descending plate are moving faster than its middie O The middle of the descending plate is moving faster than its edges
DQuestion 31 Which of these features are not found at convergent plate boundaries? O subduction zones island arcs mid ocean ridges O venches D Question 32 When viewed from above (map view) the row of volcanoes produced at a subduction zone is ar shaped because The descending plate is curved The descending plate is going down at an angle The edges of the descending plate are moving faster than its middie O The middle of the descending plate is moving faster than its edges
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
Problem 1LR
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![204 PM Fri Feb 12
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D Question 31
1 pts
Which of these features are not found at convergent plate boundaries?
subduction zones
sland arcs
mid-ocean ridges
trenches
D Question 32
1 pts
When viewed from above (map view) the row of volcanoes produced at a subduction zone is arc-
shaped because
The descending plate is curved
The descending plate is going down at an angle
The edges of the descending piate are moving faster than its middie
The middle of the descending plate is moving fester than its edges
D Question 33
1 pts
When both plates at a convergent boundary have continental crust neither slab is subducted
because
Continental crust is too strong to be subducted
Continental crust has too much sediment to be subducted
Continental crust is too light to be subducted
Continental crust contains too much water to be subducted](/v2/_next/image?url=https%3A%2F%2Fcontent.bartleby.com%2Fqna-images%2Fquestion%2Fe30979ef-1ccc-4f1e-a522-5b3af4acddad%2F47031aa7-0eaa-480d-a62a-cd3d579ca775%2F6d8zfr2n_processed.jpeg&w=3840&q=75)
Transcribed Image Text:204 PM Fri Feb 12
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D Question 31
1 pts
Which of these features are not found at convergent plate boundaries?
subduction zones
sland arcs
mid-ocean ridges
trenches
D Question 32
1 pts
When viewed from above (map view) the row of volcanoes produced at a subduction zone is arc-
shaped because
The descending plate is curved
The descending plate is going down at an angle
The edges of the descending piate are moving faster than its middie
The middle of the descending plate is moving fester than its edges
D Question 33
1 pts
When both plates at a convergent boundary have continental crust neither slab is subducted
because
Continental crust is too strong to be subducted
Continental crust has too much sediment to be subducted
Continental crust is too light to be subducted
Continental crust contains too much water to be subducted
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