File:Late Fall in the Adirondack Mountains.jpg
Summary
In this image the mountains are brown and farmed valleys are gold. Straight valleys, many containing dark-coloured rivers or lakes, cross the dome north-east to south-west like long scratch marks. Though the valleys resemble the striations of <a href="//commons.wikimedia.org/wiki/Glacier" title="Glacier">glaciers</a> on a rock, they formed along faults. Veins of green evergreen forest are visible throughout the mountains now that the leaves of the surrounding <a href="//commons.wikimedia.org/wiki/Category:Deciduous_forests" title="Category:Deciduous forests">deciduous forest</a> are gone. Water drains down and around the dome into the valleys that surround it. Lower elevation land around the Adirondack Dome is light green or gold.
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File history
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Date/Time | Thumbnail | Dimensions | User | Comment | |
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current | 00:03, 5 January 2017 | 4,800 × 6,200 (6.11 MB) | 127.0.0.1 (talk) | In this image the mountains are brown and farmed valleys are gold. Straight valleys, many containing dark-coloured rivers or lakes, cross the dome north-east to south-west like long scratch marks. Though the valleys resemble the striations of <a href="//commons.wikimedia.org/wiki/Glacier" title="Glacier">glaciers</a> on a rock, they formed along faults. Veins of green evergreen forest are visible throughout the mountains now that the leaves of the surrounding <a href="//commons.wikimedia.org/wiki/Category:Deciduous_forests" title="Category:Deciduous forests">deciduous forest</a> are gone. Water drains down and around the dome into the valleys that surround it. Lower elevation land around the Adirondack Dome is light green or gold. |
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