Complete 7 pages APA formatted article: The Gravity. When arranged in a stereoscopic fashion, the glacier at the right appears to be at a lower elevation. This is because the image on the left-hand side focuses more on the terminus of the glacier.6.c. The dark stripes on the glacier get their color due to interaction with morainal rubble. These dark stripes indicate that the glacier had come in contact with a moraine while flowing through. This could be because of an advance of the glacier or the accidental fall of any substance from the valley wall, which later mixed with the water formed from the melting ice and eventually took the form of moraines.d. The medial moraine is a ridge formed when two glaciers clashe. Since the crevasses appear at the end of the glacier in high concentration, several damages intersect at the end, forming ice pinnacles.f. The sides show the stratification or the layering of the underlying rocks. In this image, we can see that the cliff’s steep walls come to an abrupt end, suggesting that the glacier was once longer and thicker.h. The Gulf of Alaska. The shoreline on the northeast side is steeply sloping.i. The crevasses are near the delta because the delta is a result of active deposition occurring from damages.j. Figures 17.7 b and 17.8 show sedimentary deposits of a continental glacierb. The Yosemite Valley floor is flat, and the valley is a broadened part of the canyon of the Merced River. The roughly parallel sides rise to 4,000 feet and stop at the cliffs’ foot, which reaches up to another 4,000 feet. The valley narrows considerably at El Capitan and the Cathedral Rocks and is relatively more comprehensive in other places. The head of the valley is marked with the presence of Half Dome. True to its name, it is a rock structure that is smoothly shaped on three sides. However, the side facing the valley is steeply sloping and continues the skyward straight line of the valley’s walls.c. Studies have stated that, about 10 million years ago, a small valley was tilted westward, accelerating the flow of the Merced River and its tributaries. As the river cut deeper through the valley, it widened the valley and gave birth to the valley’s first forests. About 30,000 years ago, the Tioga glaciations further enlarged the valley.d. The Yosemite Valley is 7 miles in length and 1 mile in width. The floor is flat, and the valley is a widened part of the Merced River’s canyon. .
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