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lightweight, brittle, and has a conchoidal fracture. The largest “deposits” of gilsonite in the world are in the Uinta Basin of northeastern Utah, USA. Gilsonite occurs there as vertical NW-SE trending dikes (veins) intruded within the Eocene-aged Uinta
Formation. The source of the hydrocarbons is organic-rich beds in the underlying Green River Formation (Eocene) and Wasatch Formation (Paleocene).
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Gilsonite is not readily combustible and is not a fuel, but it does have economic value. Gilsonite is mined in northeastern Utah and processed and is used in numerous products and applications (e.g., see: www.geospectra.net/kite/gilsonite/gilson.htm).
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essentially identical to the basalt pahoehoe lava flows of
Kilauea Volcano at the Hawaii Hotspot. These gilsonite pahoehoe paralavas reportedly weathered relatively quickly, but this specimen was collected fresh.
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Locality: gilsonite paralava flow in the Wolf Den Fire area, southwest of the historic town of Dragon, southeastern Uintah County, northeastern Utah, USA
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Gilsonite pahoehoe paralava from the uppermost
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Gilsonite pahoehoe paralava (summer 2012; southwest of Dragon, Utah, USA) 2.jpg
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526:11 March 2016
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