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| | Geology of the Ashcroft Area (Site not responding. Last check: 2007-10-26) |
 | | Colorados major north-south trending ranges, including the Sangre de Cristo, Wet, Sawatch, Ten Mile, Gore, Park, Front, and Mosquito mountains rose in great blocks, cracking and shifting along their margins. |
 | | Mineralized with lead, iron, copper, zinc, silver, and traces of gold, these dikes, sills and stocks also metamorphosed the Paleozoic sediments with which they came in contact. |
 | | Mineralized material pushed along faults and "leeched" into the sediments; particularly the lower Carboniferous (310-350 million years old) Leadville Limestone. |
| www.aspenhistory.org /geology.html (326 words) |
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