A geologic life history of a sedimentary rock.

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Answer 1

Question

Chapter 7, Problem 1GST

To determine

To develop: A geologic life history of a sedimentary rock.

Expert Solution & Answer

Answer to Problem 1GST

Erosion or weathering, transportation, and deposition are the three geologic processes that control the formation of a sedimentary rock.

Explanation of Solution

A huge mass of igneous rock is exposed to the surface of the Earth as a result of upliftment. The uplifted rock fragmented into smaller particles due to weathering. The silicate minerals present in the rock will convert the ferromagnesian minerals into clays and dissolved silica and they are transported downstream.

The rocks, which are enriched in quartz minerals, will release quartz grains as a result of chemical weathering and they are carried downstream. The mechanical weathering processes, such as frost wedging and sheeting, also act to increase the surface area of the rock for further weathering.

If the deposition of materials that constitute the parent rock occurs close to its source, then there is a possibility to find the arkose sandstone, which is composed of feldspathic grains and quartz in a cemented matrix. If the materials are deposited far from its source, then the quartz sandstone that is composed of rounded, weathered, sorted grains of quartz cemented with silica or iron oxide can be identified.

Depending on the environment of deposition of sand grains, the characteristics of sandstone will vary. The method and medium by which the rock is transported can be determined with the help of cross-bedding and ripple marks present on the rock. In a far distant from the source, there is a possibility for the occurrence of shale and mudstones, which are composed of lithified clay that formed during the initial stages of chemical weathering.

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1. Calculate the elevation of the water table at each well location and write the approximate elevation on the line next to each well. Next, use a colored pencil to draw smooth 10-foot contours that show the shape of the water table. (Start with the 1160-foot contour.) Use a pencil of a different color to draw arrows on the map to indicate the direction of the slope of the water table. a. Toward which direction (downward) does the water table slope? b. Referring to the site of the proposed water well, at approximately what depth below the surface should the proposed well intersect the water table? 2. Assume that a dye was put into well A on May 10, 2017, and detected in well B on May 25, 2018. What was the rate of groundwater movement between the two wells, in centimeters per day? (Hint: Convert feet to centimeters.)Velocity:_____________centimeters per day

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Answer 2

Question

Chapter 7, Problem 1GST

To determine

To develop: A geologic life history of a sedimentary rock.

Expert Solution & Answer

Answer to Problem 1GST

Erosion or weathering, transportation, and deposition are the three geologic processes that control the formation of a sedimentary rock.

Explanation of Solution

A huge mass of igneous rock is exposed to the surface of the Earth as a result of upliftment. The uplifted rock fragmented into smaller particles due to weathering. The silicate minerals present in the rock will convert the ferromagnesian minerals into clays and dissolved silica and they are transported downstream.

The rocks, which are enriched in quartz minerals, will release quartz grains as a result of chemical weathering and they are carried downstream. The mechanical weathering processes, such as frost wedging and sheeting, also act to increase the surface area of the rock for further weathering.

If the deposition of materials that constitute the parent rock occurs close to its source, then there is a possibility to find the arkose sandstone, which is composed of feldspathic grains and quartz in a cemented matrix. If the materials are deposited far from its source, then the quartz sandstone that is composed of rounded, weathered, sorted grains of quartz cemented with silica or iron oxide can be identified.

Depending on the environment of deposition of sand grains, the characteristics of sandstone will vary. The method and medium by which the rock is transported can be determined with the help of cross-bedding and ripple marks present on the rock. In a far distant from the source, there is a possibility for the occurrence of shale and mudstones, which are composed of lithified clay that formed during the initial stages of chemical weathering.

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Answer 3

Question

Chapter 7, Problem 1GST

To determine

To develop: A geologic life history of a sedimentary rock.

Expert Solution & Answer

Answer to Problem 1GST

Erosion or weathering, transportation, and deposition are the three geologic processes that control the formation of a sedimentary rock.

Explanation of Solution

A huge mass of igneous rock is exposed to the surface of the Earth as a result of upliftment. The uplifted rock fragmented into smaller particles due to weathering. The silicate minerals present in the rock will convert the ferromagnesian minerals into clays and dissolved silica and they are transported downstream.

The rocks, which are enriched in quartz minerals, will release quartz grains as a result of chemical weathering and they are carried downstream. The mechanical weathering processes, such as frost wedging and sheeting, also act to increase the surface area of the rock for further weathering.

If the deposition of materials that constitute the parent rock occurs close to its source, then there is a possibility to find the arkose sandstone, which is composed of feldspathic grains and quartz in a cemented matrix. If the materials are deposited far from its source, then the quartz sandstone that is composed of rounded, weathered, sorted grains of quartz cemented with silica or iron oxide can be identified.

Depending on the environment of deposition of sand grains, the characteristics of sandstone will vary. The method and medium by which the rock is transported can be determined with the help of cross-bedding and ripple marks present on the rock. In a far distant from the source, there is a possibility for the occurrence of shale and mudstones, which are composed of lithified clay that formed during the initial stages of chemical weathering.

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Answer 4

Question

Chapter 7, Problem 1GST

To determine

To develop: A geologic life history of a sedimentary rock.

Expert Solution & Answer

Answer to Problem 1GST

Erosion or weathering, transportation, and deposition are the three geologic processes that control the formation of a sedimentary rock.

Explanation of Solution

A huge mass of igneous rock is exposed to the surface of the Earth as a result of upliftment. The uplifted rock fragmented into smaller particles due to weathering. The silicate minerals present in the rock will convert the ferromagnesian minerals into clays and dissolved silica and they are transported downstream.

The rocks, which are enriched in quartz minerals, will release quartz grains as a result of chemical weathering and they are carried downstream. The mechanical weathering processes, such as frost wedging and sheeting, also act to increase the surface area of the rock for further weathering.

If the deposition of materials that constitute the parent rock occurs close to its source, then there is a possibility to find the arkose sandstone, which is composed of feldspathic grains and quartz in a cemented matrix. If the materials are deposited far from its source, then the quartz sandstone that is composed of rounded, weathered, sorted grains of quartz cemented with silica or iron oxide can be identified.

Depending on the environment of deposition of sand grains, the characteristics of sandstone will vary. The method and medium by which the rock is transported can be determined with the help of cross-bedding and ripple marks present on the rock. In a far distant from the source, there is a possibility for the occurrence of shale and mudstones, which are composed of lithified clay that formed during the initial stages of chemical weathering.

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Answer 5

Chapter 7, Problem 1GST

To determine

To develop: A geologic life history of a sedimentary rock.

Expert Solution & Answer

Answer to Problem 1GST

Erosion or weathering, transportation, and deposition are the three geologic processes that control the formation of a sedimentary rock.

Explanation of Solution

A huge mass of igneous rock is exposed to the surface of the Earth as a result of upliftment. The uplifted rock fragmented into smaller particles due to weathering. The silicate minerals present in the rock will convert the ferromagnesian minerals into clays and dissolved silica and they are transported downstream.

The rocks, which are enriched in quartz minerals, will release quartz grains as a result of chemical weathering and they are carried downstream. The mechanical weathering processes, such as frost wedging and sheeting, also act to increase the surface area of the rock for further weathering.

If the deposition of materials that constitute the parent rock occurs close to its source, then there is a possibility to find the arkose sandstone, which is composed of feldspathic grains and quartz in a cemented matrix. If the materials are deposited far from its source, then the quartz sandstone that is composed of rounded, weathered, sorted grains of quartz cemented with silica or iron oxide can be identified.

Depending on the environment of deposition of sand grains, the characteristics of sandstone will vary. The method and medium by which the rock is transported can be determined with the help of cross-bedding and ripple marks present on the rock. In a far distant from the source, there is a possibility for the occurrence of shale and mudstones, which are composed of lithified clay that formed during the initial stages of chemical weathering.

Answer 6

Chapter 7, Problem 1GST

To determine

To develop: A geologic life history of a sedimentary rock.

Expert Solution & Answer

Answer to Problem 1GST

Erosion or weathering, transportation, and deposition are the three geologic processes that control the formation of a sedimentary rock.

Explanation of Solution

A huge mass of igneous rock is exposed to the surface of the Earth as a result of upliftment. The uplifted rock fragmented into smaller particles due to weathering. The silicate minerals present in the rock will convert the ferromagnesian minerals into clays and dissolved silica and they are transported downstream.

The rocks, which are enriched in quartz minerals, will release quartz grains as a result of chemical weathering and they are carried downstream. The mechanical weathering processes, such as frost wedging and sheeting, also act to increase the surface area of the rock for further weathering.

If the deposition of materials that constitute the parent rock occurs close to its source, then there is a possibility to find the arkose sandstone, which is composed of feldspathic grains and quartz in a cemented matrix. If the materials are deposited far from its source, then the quartz sandstone that is composed of rounded, weathered, sorted grains of quartz cemented with silica or iron oxide can be identified.

Depending on the environment of deposition of sand grains, the characteristics of sandstone will vary. The method and medium by which the rock is transported can be determined with the help of cross-bedding and ripple marks present on the rock. In a far distant from the source, there is a possibility for the occurrence of shale and mudstones, which are composed of lithified clay that formed during the initial stages of chemical weathering.

Answer 7

Chapter 7, Problem 1GST

To determine

To develop: A geologic life history of a sedimentary rock.

Answer 8

Expert Solution & Answer

Answer to Problem 1GST

Erosion or weathering, transportation, and deposition are the three geologic processes that control the formation of a sedimentary rock.

Answer 9

Expert Solution & Answer

Answer 10

Expert Solution & Answer

Answer 11

Explanation of Solution

A huge mass of igneous rock is exposed to the surface of the Earth as a result of upliftment. The uplifted rock fragmented into smaller particles due to weathering. The silicate minerals present in the rock will convert the ferromagnesian minerals into clays and dissolved silica and they are transported downstream.

The rocks, which are enriched in quartz minerals, will release quartz grains as a result of chemical weathering and they are carried downstream. The mechanical weathering processes, such as frost wedging and sheeting, also act to increase the surface area of the rock for further weathering.

If the deposition of materials that constitute the parent rock occurs close to its source, then there is a possibility to find the arkose sandstone, which is composed of feldspathic grains and quartz in a cemented matrix. If the materials are deposited far from its source, then the quartz sandstone that is composed of rounded, weathered, sorted grains of quartz cemented with silica or iron oxide can be identified.

Depending on the environment of deposition of sand grains, the characteristics of sandstone will vary. The method and medium by which the rock is transported can be determined with the help of cross-bedding and ripple marks present on the rock. In a far distant from the source, there is a possibility for the occurrence of shale and mudstones, which are composed of lithified clay that formed during the initial stages of chemical weathering.

Answer 12

Ch. 7.1 - Prob. 1CC Ch. 7.1 - Prob. 2CC Ch. 7.1 - Prob. 3CC Ch. 7.1 - Prob. 4CC Ch. 7.2 - Prob. 1CC Ch. 7.2 - Prob. 2CC Ch. 7.2 - Prob. 3CC Ch. 7.2 - Prob. 4CC Ch. 7.3 - Prob. 1CC Ch. 7.3 - Prob. 2CC

A geologic life history of a sedimentary rock.

To develop: A geologic life history of a sedimentary rock.

Answer to Problem 1GST

Explanation of Solution

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