The San Rafael Swell is a large geologic feature located in south-central Utah, United States about 16 miles (26 km) west of Green River. The San Rafael Swell, measuring approximately 75 by 40 miles (121 by 64 km), consists of a giant dome-shaped anticline of sandstone, shale, and limestone that was pushed up during the Paleocene Laramide Orogeny 60–40 million years ago. Since that time, infrequent but powerful flash floods have eroded the sedimentary rocks into numerous valleys, canyons, gorges, mesas, buttes, and badlands.
The swell is part of the Colorado Plateau physiographic region.
By elevation San Rafael Knob is
# 29 out of 187 in Emery County
By prominence San Rafael Knob is
# 55 out of 5677 in the Colorado Plateau # 75 out of 3409 in Utah # 2 out of 187 in Emery County
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