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| | Pequop |
 | | Bryozoans, echinoid spines, small gastropods, fusulinids, crinoid fragments are relatively abundant in the Pequop (Bissell, 1964). |
 | | The middle 1,095 feet is composed of olive-gray, pink, and brown aphanitic dolomite, sandy and calcareous dolomite, orthoquartzite, and thick bedded to massive algal limestone. |
 | | The upper member is 497 feet of gray to blue-gray or brown micritic limestone, sandy and calcareous dolomite, dolomitic limestone, and skeletal limestone with mollusks, algae, fusulinids, and crinoids (Bissell, 1964). |
| www.westerncordillera.com /pequop.htm (1336 words) |
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