. Brigham Young University science bulletin. Biology -- Periodicals. Biological Series, Vol. 18. No. 2 Algae ok Huntington Canyon, Utah. Fie 5 North central portion of the Wasatch Plateau sliowing the Huntington Creek drainage. Left Fork of Huntington Creek is at A, Right Fork of Huntington Creek is at B, Nuck Woodward Canyon is at C, North Hughes Canyon is at D and Candland Mountain is at E. Photographed i-eb. 7, 197Z. Creek The eastern face of the plateau consists of the eastern slopes of the plateau. The San of sharp cUffs of Starpoint sandstone and rough Rafael River drains into the Green
. Brigham Young University science bulletin. Biology -- Periodicals. Biological Series, Vol. 18. No. 2 Algae ok Huntington Canyon, Utah. Fie 5 North central portion of the Wasatch Plateau sliowing the Huntington Creek drainage. Left Fork of Huntington Creek is at A, Right Fork of Huntington Creek is at B, Nuck Woodward Canyon is at C, North Hughes Canyon is at D and Candland Mountain is at E. Photographed i-eb. 7, 197Z. Creek The eastern face of the plateau consists of the eastern slopes of the plateau. The San of sharp cUffs of Starpoint sandstone and rough Rafael River drains into the Green River, which erosion of the uppermost layers of Mancos in turn feeds the Colorado River. Streams of shale. From the mouth of Huntington Canyon, the western slope of the Wasatch Plateau dram Castle Vallev extends eastward toward the San into the San Pitch and Sevier rivers. Rafael River (Fig. 7), which collects the waters Spieker and Billings (1940) described the of Huntington Creek and other drainage waters stratigraphy and thickness of each formation. Please note that these images are extracted from scanned page images that may have been digitally enhanced for readability - coloration and appearance of these illustrations may not perfectly resemble the original Brigham Young University. Provo, Utah : Brigham Young University
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