Periglacial stone stripes resulting from downslope creep and rock segregation during freezing and thawing of thin soil layer. Glacier-Waterton National Park on the border of Montana, USA and Alberta, Canada.


Periglacial stone stripes resulting from downslope creep and rock segregation during freezing and thawing of thin soil layer. Glacier-Waterton National Park on the border of Montana, USA and Alberta, Canada. Stock Photo - Rights-Managed, Artist: Visuals Unlimited, Code: 861-03347285

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861- Alberta alpine environment alpine tundra Canada Canadian color image day EARTH SCIENCE geology glacial erosion glaciated gravel Marli Miller Montana mountain no people North America outdoors patterned ground periglacial photography rock segregation rock sorting Rocky Mountains segregated rock soil creep solifluction sorted rock temperature effect USA Visuals Unlimited Waterton Lakes National Park

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861-03347285
Rights-Managed
 Artist: Visuals Unlimited
Periglacial stone stripes resulting from downslope creep and rock segregation during freezing and thawing of thin soil layer. Glacier-Waterton National Park on the border of Montana, USA and Alberta, Canada.
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Related keywords:


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