McKnight's Physical Geography: A Landscape Appreciation (12th Edition)
12th Edition
ISBN: 9780134195421
Author: Darrel Hess, Dennis G. Tasa
Publisher: PEARSON
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Question
Chapter 20, Problem 1LC
To determine
The ways by which ocean shoreline-shaping processes are different from those shaping lakeshores.
Expert Solution & Answer
Answer to Problem 1LC
Landform development along ocean shorelines is different from that along lakeshores because short range of tides along lakeshore, difference in fluctuations of lakes and sea and difference in favorable environment for the formation of coral reefs.
Explanation of Solution
Landform development of ocean and lakes is affected by the motion of water and wind. Oceanic water is an agent of erosion and form rocky cliffs and headlands. Wind affects the landforms by depositing sand along shoreline. However, the landform development of lakeshore is different from ocean shoreline because range of tide is small along lakeshore, lake-level fluctuations are different from sea-level fluctuations and the development of coral reefs are formed place in tropical and subtropical oceans, not lakes.
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Students have asked these similar questions
44) In periglacial environments, the layer of ground that thaws every summer and freezes every winter is called
A) frost layer
B) permafrost
C) active layer
D) discontinuous permafrost
Use the attached piezometer map to make your own, clean version of the map, and indicate the elevation of the water table at all piezometer locations.
Draw equipotential lines (lines of equal water table elevation) using regular intervals – creating a contoured map of the water table.
Determine the direction of groundwater flow based on the horizontal gradient. Label the areas of recharge and discharge directly on your map.
Flow lines: Draw flow lines on your water table map. The lines should be at right angles to the equipotential lines and extend from the recharge area to the discharge area.
Hydraulic Gradient, Specific Discharge (Darcy Flux), Average Linear Velocity:
Using your water table map, estimate an average hydraulic gradient between two locations, call them locations A and B, one at the eastern-most and a second at the western-most extent of your dataset (note the north arrow on the map).
Calculate the specific discharge, q, between the two locations. For this calculation…
Calculate all the values of table 1:
Q in (L/day)
Q out (L/day)
Residence time (days)
Please show all steps
Chapter 20 Solutions
McKnight's Physical Geography: A Landscape Appreciation (12th Edition)
Ch. 20 - Prob. 1LCCh. 20 - Prob. 2LCCh. 20 - Prob. 3LCCh. 20 - Prob. 4LCCh. 20 - Prob. 5LCCh. 20 - Prob. 6LCCh. 20 - Prob. 7LCCh. 20 - Prob. 8LCCh. 20 - Prob. 9LCCh. 20 - Prob. 10LC
Ch. 20 - Prob. 11LCCh. 20 - Prob. 12LCCh. 20 - Prob. 1KTCCh. 20 - Prob. 2KTCCh. 20 - Prob. 3KTCCh. 20 - Prob. 4KTCCh. 20 - Prob. 5KTCCh. 20 - Prob. 6KTCCh. 20 - Prob. 7KTCCh. 20 - Prob. 8KTCCh. 20 - Prob. 9KTCCh. 20 - Prob. 10KTCCh. 20 - Prob. 11KTCCh. 20 - Prob. 12KTCCh. 20 - Prob. 13KTCCh. 20 - Prob. 14KTCCh. 20 - Prob. 15KTCCh. 20 - Prob. 16KTCCh. 20 - Prob. 17KTCCh. 20 - Prob. 18KTCCh. 20 - Prob. 19KTCCh. 20 - Prob. 20KTCCh. 20 - Prob. 21KTCCh. 20 - Prob. 22KTCCh. 20 - Prob. 23KTCCh. 20 - Prob. 1SQCh. 20 - Prob. 2SQCh. 20 - Prob. 3SQCh. 20 - Prob. 4SQCh. 20 - Prob. 5SQCh. 20 - Prob. 6SQCh. 20 - Prob. 1ECh. 20 - Prob. 2ECh. 20 - Prob. 3E
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