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| | EVAPORITE KARST HAZARDS OF THE LOWER FORK RIVER VALLEY, WEST-CENTRAL COLORADO |
 | | The valley is centered in the Carbondale Collapse Center, a 1,165 km2 structural depression that has collapsed 1,200 meters in response to late Cenozoic plastic flow and dissolution of the evaporite. |
 | | Deeply buried evaporite, under very high overburden pressures, flows towards the river valley where overburden pressures are markedly reduced. |
 | | Exposures of evaporite rock along the valley walls reveal highly contorted fine-grained clastic beds, massive gypsum, and evidence of diapiric piercement. |
| gsa.confex.com /gsa/2002AM/finalprogram/abstract_41192.htm (473 words) |
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