Physical Geology 16th Edition by by Charles (Carlos) Plummer – Test Bank

Physical Geology, 16th version, is the latest improvement of a traditional introductory content that has assisted numerous students in understanding fundamental physical geology principles for over 25 years. Students enrolled in introductory physical geology for a science elective, as well as those exploring opportunities in geology, will value the clear writing style and comprehensive coverage in Textual Geology. Extensive illustrations and related photographs work in harmony with the chapter explanations to facilitate a quick grasp of new geological concepts. Multiple chapter study aids and a website further support students in their exploration of physical geology.

Chapter 11 Water on the Ground

1) The quantity of existing water stored in oceans is significantly greater than the amount of ground water.

Answer: FALSE
Subject: Water Resources
Level: 2. Comprehend
Accessibility: Keyboard Navigation
Chapter: 11

2) Groundwater represents a crucial economic asset.

Answer: TRUE
Subject: Water Resources
Level: 2. Comprehend
Accessibility: Keyboard Navigation
Chapter: 11

3) Gravel displays both high porosity and excellent permeability.

Answer: TRUE
Subject: Water Resources
Level: 2. Comprehend
Accessibility: Keyboard Navigation
Chapter: 11

4) The rate of ground water movement typically decreases with depth due to sedimentary rock pores being sealed by increasing cementation and the weight of overlying rock.

Answer: TRUE
Subject: Water Resources
Level: 2. Comprehend
Accessibility: Keyboard Navigation
Chapter: 11

5) The saturated zone lies above the water table.

Answer: FALSE
Subject: Water Resources
Level: 2. Comprehend
Accessibility: Keyboard Navigation
Chapter: 11

6) The capillary fringe varies in thickness depending on the sediment type, being thicker in fine-grained sediments and thinner in coarse-grained sediments.

Answer: TRUE
Subject: Water Resources
Level: 2. Comprehend
Accessibility: Keyboard Navigation
Chapter: 11

7) In comparison to water flow in streams, most ground water moves relatively slowly.

Answer: TRUE
Subject: Water Resources
Level: 2. Comprehend
Accessibility: Keyboard Navigation
Chapter: 11

8) Water in the upper section of the saturated zone tends to descend following the inclination of the water table.

Answer: TRUE
Subject: Water Resources
Level: 2. Comprehend
Accessibility: Keyboard Navigation
Chapter: 11

9) The velocity of groundwater movement is influenced, in part, by the permeability of the sediment through which it travels.

Answer: TRUE
Subject: Water Resources
Level: 2. Comprehend
Accessibility: Keyboard Navigation
Chapter: 11

10) Contrary to popular belief, sandstones and gravels are not the only aquifers available; other rock types can also serve as aquifers.

Answer: FALSE
Subject: Water Resources
Level: 2. Comprehend
Accessibility: Keyboard Navigation
Chapter: 11