The continental slope, continental rise and continental shelf and shelf break among the given points in the diagram.

Question

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Answer 1

Question

Chapter 13, Problem 1GST

a)

To determine

The continental slope, continental rise and continental shelf and shelf break among the given points in the diagram.

a)

Expert Solution

Answer to Problem 1GST

Therefore,

Point-B: Continental shelf
Point-D: Continental shelf break
Point-A: Continental slope
Point-C: Continental rise.

Explanation of Solution

The major features accompanying these margins are as follows:

Continental shelf: It is the gentle sloped submerged surface which extends from the shoreline to the deep ocean basin. It is composed of continental crust. The average inclination of the shelf is about one-tenth of a degree. Its width greatly varies from ocean to ocean.

Continental slope: The seaward edge of the continental edge is known as continental slope. It the boundary between the continental crust and oceanic crust and is relatively steep with an average of 5 degrees.

Continental rise: The extension of continental slope with the thick accumulation of sediment down the slope is known as continental rise. The deep sea fans produced by the canyons merge together to form a continuous wedge shape at the base of the slope. This is termed as continental rise.

b)

To determine

The comparison of the size of continental shelf of surrounding Florida to the surrounding size of Florida peninsula.

b)

Expert Solution

Answer to Problem 1GST

The size of continental shelf of surrounding Florida is larger when compared to the surrounding size of Florida peninsula.

Explanation of Solution

Continental shelf is the gentle sloped submerged surface which extends from the shoreline to the deep ocean basin. It is composed of continental crust. The average inclination of the shelf is about one-tenth of a degree. Its width greatly varies from ocean to ocean.

From the accompanying map, it can be observed that the size of the Florida is much smaller when compared with the size of the continental shelf surrounding it. The presence of the major part of Florida much below the sea level also proves the same.

c)

To determine

The reason for the absence of deep-ocean trenches on the given map.

c)

Expert Solution

Answer to Problem 1GST

The given map has no convergent boundaries present and hence there are no deep-ocean trenches.

Explanation of Solution

Deep-ocean trenches are the long, narrow deep trenches located at the deepest parts of the ocean.

These are the prominent features of the convergent plate boundaries. These are formed when he slabs of oceanic slab subducts under the other plate boundary, and plunge into the mantle. It results in the volcanic activity due to the energy released by the scrap of the plate.

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1. Complete the block diagram in Figure 6.20 by drawing a left-lateral fault on Part B. 2. Draw arrows on both sides of the fault in Figure 6.20B to illustrate the relative motion of each block.

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Complete Figure 6.18 by illustrating an eroded reverse fault on Part B. Place arrows on both sides of the fault to illustrate relative motion.

Answer 2

Question

Chapter 13, Problem 1GST

a)

To determine

The continental slope, continental rise and continental shelf and shelf break among the given points in the diagram.

a)

Expert Solution

Answer to Problem 1GST

Therefore,

Point-B: Continental shelf
Point-D: Continental shelf break
Point-A: Continental slope
Point-C: Continental rise.

Explanation of Solution

The major features accompanying these margins are as follows:

Continental shelf: It is the gentle sloped submerged surface which extends from the shoreline to the deep ocean basin. It is composed of continental crust. The average inclination of the shelf is about one-tenth of a degree. Its width greatly varies from ocean to ocean.

Continental slope: The seaward edge of the continental edge is known as continental slope. It the boundary between the continental crust and oceanic crust and is relatively steep with an average of 5 degrees.

Continental rise: The extension of continental slope with the thick accumulation of sediment down the slope is known as continental rise. The deep sea fans produced by the canyons merge together to form a continuous wedge shape at the base of the slope. This is termed as continental rise.

b)

To determine

The comparison of the size of continental shelf of surrounding Florida to the surrounding size of Florida peninsula.

b)

Expert Solution

Answer to Problem 1GST

The size of continental shelf of surrounding Florida is larger when compared to the surrounding size of Florida peninsula.

Explanation of Solution

Continental shelf is the gentle sloped submerged surface which extends from the shoreline to the deep ocean basin. It is composed of continental crust. The average inclination of the shelf is about one-tenth of a degree. Its width greatly varies from ocean to ocean.

From the accompanying map, it can be observed that the size of the Florida is much smaller when compared with the size of the continental shelf surrounding it. The presence of the major part of Florida much below the sea level also proves the same.

c)

To determine

The reason for the absence of deep-ocean trenches on the given map.

c)

Expert Solution

Answer to Problem 1GST

The given map has no convergent boundaries present and hence there are no deep-ocean trenches.

Explanation of Solution

Deep-ocean trenches are the long, narrow deep trenches located at the deepest parts of the ocean.

These are the prominent features of the convergent plate boundaries. These are formed when he slabs of oceanic slab subducts under the other plate boundary, and plunge into the mantle. It results in the volcanic activity due to the energy released by the scrap of the plate.

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Subscribe now to access step-by-step solutions to millions of textbook problems written by subject matter experts!

Answer 3

Question

Chapter 13, Problem 1GST

a)

To determine

The continental slope, continental rise and continental shelf and shelf break among the given points in the diagram.

a)

Expert Solution

Answer to Problem 1GST

Therefore,

Point-B: Continental shelf
Point-D: Continental shelf break
Point-A: Continental slope
Point-C: Continental rise.

Explanation of Solution

The major features accompanying these margins are as follows:

Continental shelf: It is the gentle sloped submerged surface which extends from the shoreline to the deep ocean basin. It is composed of continental crust. The average inclination of the shelf is about one-tenth of a degree. Its width greatly varies from ocean to ocean.

Continental slope: The seaward edge of the continental edge is known as continental slope. It the boundary between the continental crust and oceanic crust and is relatively steep with an average of 5 degrees.

Continental rise: The extension of continental slope with the thick accumulation of sediment down the slope is known as continental rise. The deep sea fans produced by the canyons merge together to form a continuous wedge shape at the base of the slope. This is termed as continental rise.

b)

To determine

The comparison of the size of continental shelf of surrounding Florida to the surrounding size of Florida peninsula.

b)

Expert Solution

Answer to Problem 1GST

The size of continental shelf of surrounding Florida is larger when compared to the surrounding size of Florida peninsula.

Explanation of Solution

Continental shelf is the gentle sloped submerged surface which extends from the shoreline to the deep ocean basin. It is composed of continental crust. The average inclination of the shelf is about one-tenth of a degree. Its width greatly varies from ocean to ocean.

From the accompanying map, it can be observed that the size of the Florida is much smaller when compared with the size of the continental shelf surrounding it. The presence of the major part of Florida much below the sea level also proves the same.

c)

To determine

The reason for the absence of deep-ocean trenches on the given map.

c)

Expert Solution

Answer to Problem 1GST

The given map has no convergent boundaries present and hence there are no deep-ocean trenches.

Explanation of Solution

Deep-ocean trenches are the long, narrow deep trenches located at the deepest parts of the ocean.

These are the prominent features of the convergent plate boundaries. These are formed when he slabs of oceanic slab subducts under the other plate boundary, and plunge into the mantle. It results in the volcanic activity due to the energy released by the scrap of the plate.

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Subscribe now to access step-by-step solutions to millions of textbook problems written by subject matter experts!

Answer 4

Question

Chapter 13, Problem 1GST

a)

To determine

The continental slope, continental rise and continental shelf and shelf break among the given points in the diagram.

a)

Expert Solution

Answer to Problem 1GST

Therefore,

Point-B: Continental shelf
Point-D: Continental shelf break
Point-A: Continental slope
Point-C: Continental rise.

Explanation of Solution

The major features accompanying these margins are as follows:

Continental shelf: It is the gentle sloped submerged surface which extends from the shoreline to the deep ocean basin. It is composed of continental crust. The average inclination of the shelf is about one-tenth of a degree. Its width greatly varies from ocean to ocean.

Continental slope: The seaward edge of the continental edge is known as continental slope. It the boundary between the continental crust and oceanic crust and is relatively steep with an average of 5 degrees.

Continental rise: The extension of continental slope with the thick accumulation of sediment down the slope is known as continental rise. The deep sea fans produced by the canyons merge together to form a continuous wedge shape at the base of the slope. This is termed as continental rise.

b)

To determine

The comparison of the size of continental shelf of surrounding Florida to the surrounding size of Florida peninsula.

b)

Expert Solution

Answer to Problem 1GST

The size of continental shelf of surrounding Florida is larger when compared to the surrounding size of Florida peninsula.

Explanation of Solution

Continental shelf is the gentle sloped submerged surface which extends from the shoreline to the deep ocean basin. It is composed of continental crust. The average inclination of the shelf is about one-tenth of a degree. Its width greatly varies from ocean to ocean.

From the accompanying map, it can be observed that the size of the Florida is much smaller when compared with the size of the continental shelf surrounding it. The presence of the major part of Florida much below the sea level also proves the same.

c)

To determine

The reason for the absence of deep-ocean trenches on the given map.

c)

Expert Solution

Answer to Problem 1GST

The given map has no convergent boundaries present and hence there are no deep-ocean trenches.

Explanation of Solution

Deep-ocean trenches are the long, narrow deep trenches located at the deepest parts of the ocean.

These are the prominent features of the convergent plate boundaries. These are formed when he slabs of oceanic slab subducts under the other plate boundary, and plunge into the mantle. It results in the volcanic activity due to the energy released by the scrap of the plate.

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Subscribe now to access step-by-step solutions to millions of textbook problems written by subject matter experts!

Answer 5

Chapter 13, Problem 1GST

a)

To determine

The continental slope, continental rise and continental shelf and shelf break among the given points in the diagram.

a)

Expert Solution

Answer to Problem 1GST

Therefore,

Point-B: Continental shelf
Point-D: Continental shelf break
Point-A: Continental slope
Point-C: Continental rise.

Explanation of Solution

The major features accompanying these margins are as follows:

Continental shelf: It is the gentle sloped submerged surface which extends from the shoreline to the deep ocean basin. It is composed of continental crust. The average inclination of the shelf is about one-tenth of a degree. Its width greatly varies from ocean to ocean.

Continental slope: The seaward edge of the continental edge is known as continental slope. It the boundary between the continental crust and oceanic crust and is relatively steep with an average of 5 degrees.

Continental rise: The extension of continental slope with the thick accumulation of sediment down the slope is known as continental rise. The deep sea fans produced by the canyons merge together to form a continuous wedge shape at the base of the slope. This is termed as continental rise.

b)

To determine

The comparison of the size of continental shelf of surrounding Florida to the surrounding size of Florida peninsula.

b)

Expert Solution

Answer to Problem 1GST

The size of continental shelf of surrounding Florida is larger when compared to the surrounding size of Florida peninsula.

Explanation of Solution

Continental shelf is the gentle sloped submerged surface which extends from the shoreline to the deep ocean basin. It is composed of continental crust. The average inclination of the shelf is about one-tenth of a degree. Its width greatly varies from ocean to ocean.

From the accompanying map, it can be observed that the size of the Florida is much smaller when compared with the size of the continental shelf surrounding it. The presence of the major part of Florida much below the sea level also proves the same.

c)

To determine

The reason for the absence of deep-ocean trenches on the given map.

c)

Expert Solution

Answer to Problem 1GST

The given map has no convergent boundaries present and hence there are no deep-ocean trenches.

Explanation of Solution

Deep-ocean trenches are the long, narrow deep trenches located at the deepest parts of the ocean.

These are the prominent features of the convergent plate boundaries. These are formed when he slabs of oceanic slab subducts under the other plate boundary, and plunge into the mantle. It results in the volcanic activity due to the energy released by the scrap of the plate.

Answer 6

Chapter 13, Problem 1GST

a)

To determine

The continental slope, continental rise and continental shelf and shelf break among the given points in the diagram.

a)

Expert Solution

Answer to Problem 1GST

Therefore,

Point-B: Continental shelf
Point-D: Continental shelf break
Point-A: Continental slope
Point-C: Continental rise.

Explanation of Solution

The major features accompanying these margins are as follows:

Continental shelf: It is the gentle sloped submerged surface which extends from the shoreline to the deep ocean basin. It is composed of continental crust. The average inclination of the shelf is about one-tenth of a degree. Its width greatly varies from ocean to ocean.

Continental slope: The seaward edge of the continental edge is known as continental slope. It the boundary between the continental crust and oceanic crust and is relatively steep with an average of 5 degrees.

Continental rise: The extension of continental slope with the thick accumulation of sediment down the slope is known as continental rise. The deep sea fans produced by the canyons merge together to form a continuous wedge shape at the base of the slope. This is termed as continental rise.

Answer 7

Chapter 13, Problem 1GST

a)

To determine

The continental slope, continental rise and continental shelf and shelf break among the given points in the diagram.

Answer 8

a)

Expert Solution

Answer to Problem 1GST

Therefore,

Point-B: Continental shelf
Point-D: Continental shelf break
Point-A: Continental slope
Point-C: Continental rise.

Answer 9

a)

Expert Solution

Answer 10

a)

Expert Solution

Answer 11

Expert Solution

Answer 12

Explanation of Solution

The major features accompanying these margins are as follows:

Continental shelf: It is the gentle sloped submerged surface which extends from the shoreline to the deep ocean basin. It is composed of continental crust. The average inclination of the shelf is about one-tenth of a degree. Its width greatly varies from ocean to ocean.

Continental slope: The seaward edge of the continental edge is known as continental slope. It the boundary between the continental crust and oceanic crust and is relatively steep with an average of 5 degrees.

Continental rise: The extension of continental slope with the thick accumulation of sediment down the slope is known as continental rise. The deep sea fans produced by the canyons merge together to form a continuous wedge shape at the base of the slope. This is termed as continental rise.

Answer 13

b)

To determine

The comparison of the size of continental shelf of surrounding Florida to the surrounding size of Florida peninsula.

b)

Expert Solution

Answer to Problem 1GST

The size of continental shelf of surrounding Florida is larger when compared to the surrounding size of Florida peninsula.

Explanation of Solution

Continental shelf is the gentle sloped submerged surface which extends from the shoreline to the deep ocean basin. It is composed of continental crust. The average inclination of the shelf is about one-tenth of a degree. Its width greatly varies from ocean to ocean.

From the accompanying map, it can be observed that the size of the Florida is much smaller when compared with the size of the continental shelf surrounding it. The presence of the major part of Florida much below the sea level also proves the same.

Answer 14

b)

To determine

The comparison of the size of continental shelf of surrounding Florida to the surrounding size of Florida peninsula.

Answer 15

b)

Expert Solution

Answer to Problem 1GST

The size of continental shelf of surrounding Florida is larger when compared to the surrounding size of Florida peninsula.

Answer 16

b)

Expert Solution

Answer 17

b)

Expert Solution

Answer 18

Expert Solution

Answer 19

Explanation of Solution

Continental shelf is the gentle sloped submerged surface which extends from the shoreline to the deep ocean basin. It is composed of continental crust. The average inclination of the shelf is about one-tenth of a degree. Its width greatly varies from ocean to ocean.

From the accompanying map, it can be observed that the size of the Florida is much smaller when compared with the size of the continental shelf surrounding it. The presence of the major part of Florida much below the sea level also proves the same.

Answer 20

c)

To determine

The reason for the absence of deep-ocean trenches on the given map.

c)

Expert Solution

Answer to Problem 1GST

The given map has no convergent boundaries present and hence there are no deep-ocean trenches.

Explanation of Solution

Deep-ocean trenches are the long, narrow deep trenches located at the deepest parts of the ocean.

These are the prominent features of the convergent plate boundaries. These are formed when he slabs of oceanic slab subducts under the other plate boundary, and plunge into the mantle. It results in the volcanic activity due to the energy released by the scrap of the plate.

Answer 21

c)

To determine

The reason for the absence of deep-ocean trenches on the given map.

Answer 22

c)

Expert Solution

Answer to Problem 1GST

The given map has no convergent boundaries present and hence there are no deep-ocean trenches.

Answer 23

c)

Expert Solution

Answer 24

c)

Expert Solution

Answer 25

Expert Solution

Answer 26

Explanation of Solution

Deep-ocean trenches are the long, narrow deep trenches located at the deepest parts of the ocean.

These are the prominent features of the convergent plate boundaries. These are formed when he slabs of oceanic slab subducts under the other plate boundary, and plunge into the mantle. It results in the volcanic activity due to the energy released by the scrap of the plate.