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Within the image power lines (B) can be seen
travelling straight across the landscape, taking only a few sudden
and sharp changes in direction. Power line corridors are also identified
by their colour, which is typically pink (non-vegetated areas) or
yellow (grassed areas), therefore distinguishable from a road system,
which are usually bluish in tone. Steep sided stream valleys (C) can be identified in the image by the shadows that they cast, each of which creates an impression of a profile view of the valley. The low sun angle experienced at the time the image was taken, November, has helped to highlight such topographic variations and is therefore a useful aid to assist the identification of certain geologic features. A further geological structure that can be identified
is the series of obvious concentric ovals, located towards the centre
of the satellite image (surrounded by black arrows). Folding
of the underlying sedimentary rocks is the most likely reason for
the formation of this feature.
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Last up-dated 7 August, 2002