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ANSWERS

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Image courtesy of the Canada Centre for Remote Sensing, Natural Resources Canada.

1. How can you tell that the land reaches very high elevations?

It is clear from the image that the area reaches high elevations due to the distinct shadows that are cast on the mountainsides, and is the reason why the image has a 3-dimentional look. In contrast to the calm and smooth appearance of the water body (in squares 1D and 2D for example) the land area is more mottled in tone and is evidently more rugged.

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2. What do you think is the dominant land cover in this area?

As the image is a natural colour image the green colour of the mountains indicates that the dominant land cover is dense forest
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3. Can you identify evidence of mass movement within the mountain range?

Within the forested slopes there is evidence of bare rock surface, these non-vegetated areas are represented by pale pink tones. However, within B4, the rocky outcrops tend to be relatively linear in appearance and as they are orientated up and down the slope, they are clear evidence of landslides. These features are a further indication of the area being composed of steep slopes

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4. On what facing slopes do the majority of the snow patches occur? Why is this?

The snow patches (eg. square C3) are present on the north facing slopes. The main reason for this is aspect. Slopes that face towards the sun (South facing slopes) are exposed to direct insolation. Whereas the slopes that face away from the sun (North facing slopes) are sheltered from the direct solar rays and tend to have relatively cooler slopes. Hence the snow and ice patches will melt sooner on the south facing slopes. Thus the direction the slopes face (or aspect) is the reason for the accumulation of snow.
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5. What sort of shoreline is present in the area?

The jagged shape of the coastline indicates that the shoreline is rocky one as opposed to a sandy one.
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6. What do the white tones around the coastline represent?

The white tones around the shore represent waves breaking on the rocky shoreline, they are particularly noticeable at the top of the image (especially in B1). The reason for this is that this side of the coast is likely to have been considerably more windy and exposed at the time the image was obtained.
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Last up-dated 7 August, 2002