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Back Owl Creek/Castle Rocks Written in collaboration with Gretchen Hurley
Location and Access Geologically, this site is known as the Castle Rocks Chaos. It is a jumble of volcanic debris representing a unique geologic event which occurred during the Eocene period (Sundell 1982). Both the Owl Creek section and the Castle Rocks are distinguished by high (elevation of 9,000 to 10,900 feet) alpine tundra with windswept slopes and mountainous cliffs scattered with erratic dense patches of conifer, and aspen. The bare rocky soil along lower draws and ridges and sagebrush grasslands along wide creek bottoms enhance this mountain transition area. All tracts border the Washakie Wilderness Area of the Shoshone National Forest. These wild areas are logical extensions of the Washakie Wilderness. Wilderness Qualities Two of the area's streams are important fisheries for rainbow, brook, and Yellowstone cutthroat trout. The area also provides crucial habitat for bighorn sheep, moose and mule deer, crucial winter range and calving grounds for elk, and migration routes for elk and bighorn sheep (WG&F, 1992). Raptors, pronghorn antelope, mountain lions, and black bears use the area, and grizzly bears have been observed nearby. A high priority in this area is the occurrence of the harlequin duck a category two candidate for federal listing (WNDD, 1993). Dwarf shrews and montane vole‑‑two state Priority Species in Need of Special Management‑‑may inhabit Owl Creek's grasslands and conifer forests (Luce 1991; WNDD, 1993). Several rare plant species have been found in the area - Evert's waferparsnip, shoshoea, Rocky Mountain twinpod, yellow spring-beauty, sweet-flowered rock jasmine, and the nuttall townsend-daisy (WNDD,1993). | ||||