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50 vertical feet above a creek. The lower edge of this quite planar hillside is locally defined by a much steeper escarpment which drops down to a cold stream. During the September fieldwork, this creek could only crossed with dry feet in a few locations. The escarpment is an obvious linear feature that was easily recognized during the helicopter flight into the hot springs (Figures 2). The relief on the escarpment rapidly diminishes downstream (SW) of the thermal springs and gradually diminishes upstream (NE) over a distance of 1⁄2 mile. The total length of this escarpment is about 0.6 miles and for reasons to be discussed later it appears to be the most important geologic feature controlling the location of the geothermal system. Most likely this escarpment represents vertical displacement along a recently active fault, although no evidence was obtained to prove this hypothesis. In several nonvolcanic areas in the world such as the Basin and Range province in Nevada and Utah as well as in Turkey, there is a close association between many geothermal systems and recently active faults or fault zones. Figure 2. View of escarpment looking to the southwest. 3.1.3 Bedrock Geology All of the area is covered by tundra and willows. Hand drilling showed impenetrable rock to be present everywhere at depths of 1 to 3 feet below the ground surface. The only actual outcroppings of bedrock are two small areas located about 350 ft east of the hot pool at the base of the escarpment on the north side of the cold stream (Figure 3). These are overlain by tens of feet of alluvium exposed on the face of the escarpment. No attempt was made to try to map or define units within this complex as bedrock outcrops occur in less than 1% of the area. A small percentage of the area consists of flat outcroppings of frost shattered rock generally broken into blocks less than a foot in diameter. In places there is also pattern ground (polygonal shaped), presumably due to annual freeze-thaw cycles and production of ice wedges. The bedrock in the vicinity of the thermal springs consist of either high grade metamorphic rocks intruded by abundant granitic material or are migmatites, mixed rock consisting of high temperature metamorphic rocks which have partially melted (Figure 4). In either case the overall chemical composition of these crystalline rocks is similar to granitic rocks. 4PDF Image | US Department of Energy Tribal Energy Program
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