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Highway one at the base of a scree slope of Krossanesfjall (mountain) between Höfn and Djupivogur in the Eastern Fjord region of Iceland.

"Scree is a collection of broken rock fragments at the base of crags, mountain cliffs, volcanoes or valley shoulders that has accumulated through periodic rockfall from adjacent cliff faces."
"Scree formation is commonly attributed to the formation of ice within mountain rock slopes. During the day, water can flow in joints and discontinuities in the rock wall. If the temperature drops sufficiently, for example with the onset of evening, this water may freeze. Since water expands by 9% when it freezes, it can generate large forces that either creates new cracks or wedges blocks into an unstable position."http://en.wikipedia.org/wiki/Scree

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Additional Photos by Trevor Moffiet (trevormoffiet) Gold Star Critiquer/Gold Note Writer [C: 213 W: 2 N: 578] (3110)
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