ISBN-13
978-1259916823
Physical Geology, 16th model, is the newest refinement of a standard introductory textual content material that has helped quite a few faculty college students research elementary bodily geology concepts for over 25 years. Faculty college students taking introductory bodily geology to fulfill a science elective, along with these contemplating a career in geology, will admire the accessible writing kind and depth of safety in Physical Geology. An entire bunch of rigorously rendered illustrations and accompanying pictures correlate utterly with the chapter descriptions to help readers shortly grasp new geologic concepts. Fairly a number of chapter finding out devices and an web website further assist faculty college students of their look at of bodily geology.
Chapter 11 Flooring Water
1) The amount of current water saved in oceans is many events bigger than the amount of flooring water.
Reply: FALSE
Matter: Water Sources
Bloom’s: 2. Understand
Accessibility: Keyboard Navigation
Chapter: 11
2) Groundwater is a major monetary helpful useful resource.
Reply: TRUE
Matter: Water Sources
Bloom’s: 2. Understand
Accessibility: Keyboard Navigation
Chapter: 11
3) Gravel has every extreme porosity and wonderful permeability.
Reply: TRUE
Matter: Water Sources
Bloom’s: 2. Understand
Accessibility: Keyboard Navigation
Chapter: 11
4) The velocity of flooring water motion tends to decrease with depth because of sedimentary rock pores are usually closed by rising portions of cement and the burden of the overlying rock.
Reply: TRUE
Matter: Water Sources
Bloom’s: 2. Understand
Accessibility: Keyboard Navigation
Chapter: 11
5) The saturated zone overlies the water desk.
Reply: FALSE
Matter: Water Sources
Bloom’s: 2. Understand
Accessibility: Keyboard Navigation
Chapter: 11
6) The capillary fringe is thicker in optimistic-grained sediments and thinner in coarse-grained sediments.
Reply: TRUE
Matter: Water Sources
Bloom’s: 2. Understand
Accessibility: Keyboard Navigation
Chapter: 11
7) As compared with the motion of water in streams, most flooring water strikes comparatively slowly.
Reply: TRUE
Matter: Water Sources
Bloom’s: 2. Understand
Accessibility: Keyboard Navigation
Chapter: 11
8) Water inside the increased part of the saturated zone tends to maneuver downward following the slope of the water desk.
Reply: TRUE
Matter: Water Sources
Bloom’s: 2. Understand
Accessibility: Keyboard Navigation
Chapter: 11
9) How briskly groundwater flows depends upon, partly, on the permeability of the sediment by which it passes.
Reply: TRUE
Matter: Water Sources
Bloom’s: 2. Understand
Accessibility: Keyboard Navigation
Chapter: 11
10) Sandstones and gravels make the one aquifers; no totally different rocks are useful.
Reply: FALSE
Matter: Water Sources
Bloom’s: 2. Understand
Accessibility: Keyboard Navigation
Chapter: 11
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