Refer to Figure 6.23 to describe the strike and dip of the limestone layer

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Answer 1

Textbook Question

Chapter 6, Problem 1LR

Refer to Figure 6.23 to describe the strike and dip of the limestone layer

Chapter 6, Problem 1LR, Refer to Figure 6.23 to describe the strike and dip of the limestone layer

Expert Solution & Answer

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 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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Exercise Ten / Geologic Time 177 d. Based on the ages of the rock layers in outcrop 1, identify an unconformity. Remember that an unconformity is a break in the rock record. Draw a wavy line on the figure to represent the unconformity. Ginkgo Period Ginkgo Lepidodendron Dimetrodon Period Tyrannosaurus Calamites Inoceramus Period Lepidodendron Rhodocrinites Archimedes Eurypterus Period Sharks Period Phacops Agnostus Outcrop 1 Period Period Ichthyosaurus Period Sharks Ceratites Period Paleolimulus A Figure 10.17 Sequences of sedimentary rock layers to accompany Question 7. 10.8 Numerical Dating with Radioactivity ■ Explain the principle of radiometric dating, including half-life, parent isotope, and daughter product. Radioactivity has provided a reliable means for calculating the numerical (absolute) age of rocks, a procedure called radiometric dating. Radioactive isotopes, such as uranium-238, emit particles from their nuclei that we call radiation. Ultimately, the process of decay…

Answer 2

Textbook Question

Chapter 6, Problem 1LR

Refer to Figure 6.23 to describe the strike and dip of the limestone layer

Chapter 6, Problem 1LR, Refer to Figure 6.23 to describe the strike and dip of the limestone layer

Expert Solution & Answer

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 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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01:09

Answer 3

Textbook Question

Chapter 6, Problem 1LR

Refer to Figure 6.23 to describe the strike and dip of the limestone layer

Chapter 6, Problem 1LR, Refer to Figure 6.23 to describe the strike and dip of the limestone layer

Expert Solution & Answer

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 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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01:09

Answer 4

Textbook Question

Chapter 6, Problem 1LR

Refer to Figure 6.23 to describe the strike and dip of the limestone layer

Chapter 6, Problem 1LR, Refer to Figure 6.23 to describe the strike and dip of the limestone layer

Expert Solution & Answer

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 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 5

Textbook Question

Answer 6

Textbook Question

Answer 7

Expert Solution & Answer

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 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 8

Expert Solution & Answer

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 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 9

Expert Solution & Answer

Answer 10

Expert Solution & Answer

Answer 11

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 12

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 13

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 14

Ch. 6.1 - Define rock deformation in your own words.Ch. 6.1 - Prob. 2A Ch. 6.1 - Prob. 3A Ch. 6.1 - In Figure 6.2, describe the type of deformation...Ch. 6.1 - Prob. 5A Ch. 6.2 - Prob. 1A Ch. 6.2 - Prob. 2A Ch. 6.3 - Prob. 1A Ch. 6.3 - Prob. 2A Ch. 6.3 - Prob. 3A

Refer to Figure 6.23 to describe the strike and dip of the limestone layer

Answer to Problem 1LR

Explanation of Solution

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