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Additional info for Bull Creek (Anthropological papers University of Utah)

Sample text

The implications of both radiocarbon samples have been discussed (see Chronology above). Other Sites Tested Sites 42Wn959 and 970 occurred a few meters north of the point where Bull Creek was diverted a few years ago into Dry Valley Wash. They were essentially circular, crater-like patterns of stones 3 to 4 m in diameter on low elevations. The stones were absent from the center of the circular arrangement. These were sampled by driving a trench from outside the distribution of stones through the center to the other edge of the circle.

5 to 23 cm over a 20-year period (Jeppson et al. 1968). Seasonal variability in precipitation is also important in the Bull Creek area. Precipitation in southeastern Utah is marked by a summer maximum associated with thunderstorms. These storms are the result of weather patterns that originate in the Gulf of Mexico. There is a secondary storm peak in October and a minor winter frontal maximum, originating in the Pacific, around December (Jeppson et al. 1968:25). The table below lists the total precipitation (converted from inches) for given months of the year in the Bull Creek area (taken from Jeppson et al.

Hunt during an ecological study of the Bull Creek drainage system. S. Department of Interior permits 76-UT-055 and 77-UT-081, and Bureau of Land Management permits 76-UT-053, as amended, and 77-UT-080. The cooperation of these agencies was appreciated. A portion of the costs of the study was supported by NSF Grant No. BNS-73-05506-A01; without these funds the work would not have been accomplished. Valuable explanation and interpretation of geological and morphological phenomena were provided by Charles B.

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Bull Creek (Anthropological papers University of Utah) by Jesse David Jennings

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