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<a accesskey="3" href="page.php?w=hydrothermal_circulation&amp;p=2">3.Next</a>
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<p><b>Hydrothermal circulation</b> in its most general sense is the circulation of hot water (<a href="page.php?w=Ancient_Greek">Ancient Greek</a> ????, water, and ???u?, heat ). Hydrothermal circulation occurs most often in the vicinity of sources of heat within the Earth's <a href="page.php?w=Crust_%28geology%29">crust</a>. In general, this occurs near <a href="page.php?w=volcanic">volcanic</a> activity, but can occur in the shallow to mid crust along deeply penetrating fault irregularities or in the deep crust related to the intrusion of <a href="page.php?w=granite">granite</a>,</p><p>
<a accesskey="3" href="page.php?w=hydrothermal_circulation&amp;p=2">3.Next</a>
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