The sedimentary rocks are formed from sediments that are transported by running water to the shallow seas, and over time they undergo processes like compression, compaction, burial, and cementation in the deep crust to form sedimentary rocks.

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Answer 1

Question

Chapter 8, Problem 1LR

Summary Introduction

Introduction:

The sedimentary rocks are formed from sediments that are transported by running water to the shallow seas, and over time they undergo processes like compression, compaction, burial, and cementation in the deep crust to form sedimentary rocks.

Expert Solution & Answer

Answer to Problem 1LR

Correct answer:

The strike in the given limestone layer is 25 ° East. The direction of dip is 180 °, and the angle of dip is 40°.

Explanation of Solution

The method of calculating the strike, angle of dip, and direction of dip includes the measurement of strike and dip present on the rock layers or planar features. The strike in limestone is defined as the compass direction that is relative to north. It is constructed of the line formed by the intersection of a rock layer. The strike of the limestone layer is 25 ° East, the direction of dip is 180 °, and the angle of dip is 40°.

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Answer 2

Question

Chapter 8, Problem 1LR

Summary Introduction

Introduction:

The sedimentary rocks are formed from sediments that are transported by running water to the shallow seas, and over time they undergo processes like compression, compaction, burial, and cementation in the deep crust to form sedimentary rocks.

Expert Solution & Answer

Answer to Problem 1LR

Correct answer:

The strike in the given limestone layer is 25 ° East. The direction of dip is 180 °, and the angle of dip is 40°.

Explanation of Solution

The method of calculating the strike, angle of dip, and direction of dip includes the measurement of strike and dip present on the rock layers or planar features. The strike in limestone is defined as the compass direction that is relative to north. It is constructed of the line formed by the intersection of a rock layer. The strike of the limestone layer is 25 ° East, the direction of dip is 180 °, and the angle of dip is 40°.

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Answer 3

Question

Chapter 8, Problem 1LR

Summary Introduction

Introduction:

The sedimentary rocks are formed from sediments that are transported by running water to the shallow seas, and over time they undergo processes like compression, compaction, burial, and cementation in the deep crust to form sedimentary rocks.

Expert Solution & Answer

Answer to Problem 1LR

Correct answer:

The strike in the given limestone layer is 25 ° East. The direction of dip is 180 °, and the angle of dip is 40°.

Explanation of Solution

The method of calculating the strike, angle of dip, and direction of dip includes the measurement of strike and dip present on the rock layers or planar features. The strike in limestone is defined as the compass direction that is relative to north. It is constructed of the line formed by the intersection of a rock layer. The strike of the limestone layer is 25 ° East, the direction of dip is 180 °, and the angle of dip is 40°.

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Answer 4

Question

Chapter 8, Problem 1LR

Summary Introduction

Introduction:

The sedimentary rocks are formed from sediments that are transported by running water to the shallow seas, and over time they undergo processes like compression, compaction, burial, and cementation in the deep crust to form sedimentary rocks.

Expert Solution & Answer

Answer to Problem 1LR

Correct answer:

The strike in the given limestone layer is 25 ° East. The direction of dip is 180 °, and the angle of dip is 40°.

Explanation of Solution

The method of calculating the strike, angle of dip, and direction of dip includes the measurement of strike and dip present on the rock layers or planar features. The strike in limestone is defined as the compass direction that is relative to north. It is constructed of the line formed by the intersection of a rock layer. The strike of the limestone layer is 25 ° East, the direction of dip is 180 °, and the angle of dip is 40°.

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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 8, Problem 1LR

Summary Introduction

Introduction:

The sedimentary rocks are formed from sediments that are transported by running water to the shallow seas, and over time they undergo processes like compression, compaction, burial, and cementation in the deep crust to form sedimentary rocks.

Expert Solution & Answer

Answer to Problem 1LR

Correct answer:

The strike in the given limestone layer is 25 ° East. The direction of dip is 180 °, and the angle of dip is 40°.

Explanation of Solution

The method of calculating the strike, angle of dip, and direction of dip includes the measurement of strike and dip present on the rock layers or planar features. The strike in limestone is defined as the compass direction that is relative to north. It is constructed of the line formed by the intersection of a rock layer. The strike of the limestone layer is 25 ° East, the direction of dip is 180 °, and the angle of dip is 40°.

Answer 6

Chapter 8, Problem 1LR

Summary Introduction

Introduction:

The sedimentary rocks are formed from sediments that are transported by running water to the shallow seas, and over time they undergo processes like compression, compaction, burial, and cementation in the deep crust to form sedimentary rocks.

Expert Solution & Answer

Answer to Problem 1LR

Correct answer:

The strike in the given limestone layer is 25 ° East. The direction of dip is 180 °, and the angle of dip is 40°.

Explanation of Solution

The method of calculating the strike, angle of dip, and direction of dip includes the measurement of strike and dip present on the rock layers or planar features. The strike in limestone is defined as the compass direction that is relative to north. It is constructed of the line formed by the intersection of a rock layer. The strike of the limestone layer is 25 ° East, the direction of dip is 180 °, and the angle of dip is 40°.

Answer 7

Chapter 8, Problem 1LR

Summary Introduction

Introduction:

The sedimentary rocks are formed from sediments that are transported by running water to the shallow seas, and over time they undergo processes like compression, compaction, burial, and cementation in the deep crust to form sedimentary rocks.

Answer 8

Expert Solution & Answer

Answer to Problem 1LR

Correct answer:

The strike in the given limestone layer is 25 ° East. The direction of dip is 180 °, and the angle of dip is 40°.

Answer 9

Expert Solution & Answer

Answer 10

Expert Solution & Answer

Answer 11

Explanation of Solution

The method of calculating the strike, angle of dip, and direction of dip includes the measurement of strike and dip present on the rock layers or planar features. The strike in limestone is defined as the compass direction that is relative to north. It is constructed of the line formed by the intersection of a rock layer. The strike of the limestone layer is 25 ° East, the direction of dip is 180 °, and the angle of dip is 40°.

Answer 12

Ch. 8.1 - Define rock deformation in your own words.Ch. 8.1 - Prob. 2A Ch. 8.1 - Prob. 3A Ch. 8.1 - Prob. 4A Ch. 8.1 - Prob. 5A Ch. 8.2 - Prob. 1A Ch. 8.2 - Prob. 2A Ch. 8.3 - Prob. 1A Ch. 8.3 - Prob. 2A Ch. 8.3 - Prob. 3A

The sedimentary rocks are formed from sediments that are transported by running water to the shallow seas, and over time they undergo processes like compression, compaction, burial, and cementation in the deep crust to form sedimentary rocks.

Introduction: The sedimentary rocks are formed from sediments that are transported by running water to the shallow seas, and over time they undergo processes like compression, compaction, burial, and cementation in the deep crust to form sedimentary rocks.

Answer to Problem 1LR

Explanation of Solution

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Chapter 8 Solutions

Introduction:

The sedimentary rocks are formed from sediments that are transported by running water to the shallow seas, and over time they undergo processes like compression, compaction, burial, and cementation in the deep crust to form sedimentary rocks.