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Colorado Potential Geothermal Pathways

Published by Flint Geothermal, LLC | Department of Energy | Metadata Last Checked: January 27, 2026 | Last Modified: 2021-08-23T19:35:07Z
This layer contains the weakened basement rocks. Isostatic gravity was utilized to identify structural basin areas, characterized by gravity low values reflecting weakened basement rocks. Together interpreted regional fault zones and basin outlines define geothermal "exploration fairways", where the potential exists for deep, superheated fluid flow in the absence of Pliocene or younger volcanic units.

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