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<a accesskey="3" href="page.php?w=periglaciation&amp;p=2">3.Next</a>
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<p> <a href="page.php?w=Image%3AMelting_pingo_wedge_ice.jpg">thumb</a><b>Periglaciation</b> (adjective: "periglacial", referring to places at the edges of <a href="page.php?w=glacier">glacial</a> areas) describes <a href="page.php?w=Geomorphology">geomorphic</a> processes that result from seasonal thawing and freezing, very often in areas of <a href="page.php?w=permafrost">permafrost</a>. The meltwater may refreeze in ice wedges and other structures. "Periglacial" originally suggested an environment located on the margin of past glaciers. However,</p><p>
<a accesskey="3" href="page.php?w=periglaciation&amp;p=2">3.Next</a>
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