(a)
The average yearly rate at which the ice in the centre of the glacier advanced.
(a)
Answer to Problem 1GST
Explanation of Solution
Given info:
Number of years taken for the movement is
Explanation:
The expression for calculating the average yearly rate at which the glacier advanced in the centre,
Substitute
(b)
The speed at which the glacier advances per day in the centre.
(b)
Answer to Problem 1GST
Explanation of Solution
Given info:
We found from above that the annual rate of movement of the glacier in the centre is
Explanation:
The expression for calculating the speed at which the glacier advances in the centre per day,
Substitute
(c)
The average rate at which the ice along the sides of the glacier moved forward.
(c)
Answer to Problem 1GST
Explanation of Solution
Given info:
Number of years taken for the movement is
Explanation:
The expression for calculating the average rate at which the glacier advanced along the sides,
Substitute
(d)
The reason for the difference in the rate of movement of the glacial ice in the centre and along the sides.
(d)
Answer to Problem 1GST
The frictional drags causes the glacial ice to flow at a slower rate along the sides whereas the central part is devoid of friction and can move at a faster rate.
Explanation of Solution
During the movement of glacial ice, the movement occurs both internally and externally. The frictional drag affects the external motion of the ice and it is more along the sides and bottom of the glacier.
The central part of the glacier escapes from the friction. This causes the central part of the glacial ice to advance forward at a faster rate than those along the sides, thus bringing difference in the rate of movement in the centre and along the sides of the glacier.
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Chapter 18 Solutions
Earth: An Introduction to Physical Geology (12th Edition)
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- Provide examples to illustrate the effects of glacier and ice sheet melting on climate globally and regionally. Use words to illustrate any feedback mechanisms between melting ice sheets and the climate.arrow_forwardUse diagrams and word explanations to show how excess heat from the tropics is transferred to higher latitudes (discuss cells and ciruclations) . Additionally, show how the broadening of the Hadley Cell, caused by rising greenhouse gases, could affect surface climate in subtropical and mid-latitude regions.arrow_forwardExplain why the Earth is in not in radiative equilibriumarrow_forward
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