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<p>in the zone of accumulation is greater than loss due to melting or ablation.</p>

<p><big> History </big></p>
<p>During the <a href="page.php?w=Last_Glacial_Maximum">Last Glacial Maximum</a> (LGM), the Northern hemisphere began its modern ice-age. Most of what is now <a href="page.php?w=Canada">Canada</a> and northern portions of the <a href="page.php?w=United_States">United States</a> were covered in ice sheets or mountain driven glaciers during the last stage of the <a href="page.php?w=Pleistocene_Epoch">Pleistocene Epoch</a>. In the last 400,000 years</p><p>
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