When groundwater is heated below the surface to boiling by hot igneous rocks, it can create a geothermal system where the water becomes superheated, leading to the formation of steam. This steam can accumulate pressure and, if it finds a way to escape, may result in geysers or hot springs. Additionally, the intense heat can alter the surrounding rock and minerals, potentially leading to the formation of geothermal features and deposits. In some cases, the heated water can contribute to the formation of hydrothermal ore deposits.
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