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Bench at base of Book Cliffs east of Thompsons (Thompson Spring). Grand County, Utah. 1906. Plate 2-A in U.S. Geological Survey. Bulletin 371. 1909.
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This collection of maps shows vegetation cover types that are either Dominant or Common (see project documentation for full methodology in mapping). Sparse cover types are not shown here. All patches have a dominant cover type, but not all have a Common type. Vegetation features were mapped by National Park Service staff; ground-truthing and editing of vegetation data was done by project staff, as was mapping of bare areas and channel features. Associated layers of river channels, reaches, and bottomland kilometers are included for reference.
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An Earth erosion column in a semi-arid country ordinary earth becomes almost as enduring as solid rock. These columns are 30 feet high and are protected by caps from the rain. Grand County, Utah. 1907. Plate 50-C in U.S. Geological Survey. Bulletin 707. 1922.
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This set of maps shows relative habitat quality for bat watering. Component layers (distance to water, vegetation cover types, open flight areas) are included, as are complementary layers of channel boundaries, reaches, and bottomland kilometers.
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Dry screening at the C.F.I. mine. Another view similar to No.418. The cleaned ore is measured with pails and piled on a platform as shown at the right. Thence team and wagon haul it to Floy for shipment on the D. & R.G. Railroad for shipment East. La Sal and Moab quadrangles, Grand County, Utah. May, 25, 1918.
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Album caption and index card: Canyons of Green River. Dellenbaugh Butte, near the mouth of San Rafael. Labyrinth Canyon. Grand and Emery Counties, Utah. ca. 1871. (Stereoscopic view) (Photo same as J.K. Hillers no. 585, hjk00585)
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As viewed from a boat. High cliffs on right are Wingate Sandstone capped by Kayenta Formation and underlain by slopes of Chinle and Moenkopi Formations.
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Album caption and index card: Canyons of Green River. Tump-in-kon-tu-weap. Labyrinth Canyon. Grand and Emery Counties, Utah. ca. 1871. (Stereoscopic view) (Photo similar to J.K. Hillers no. 736, hjk00736)
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Wingate sandstone and underlying softer Chinle shale exposed at Big Hole on the Colorado River 8 miles east of Cisco, note the extensive horizontal softer beds in the Wingate sandstone and the cross-bedding within the thicker sandstone beds. sec. 8 T. 21 S., R. 23 E. Grand County, Utah. October 1927. Plate 6-B, in U.S. Geological Survey. Professional paper 183. 1936. Plate 9-A, in U.S. Geological Survey. Bulletin 863, 1935.
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Ballards mine, north of Thompsons. Grand County, Utah.n.d. Plate 9-A in U.S. Geological Survey. Bulletin 371. 1909.
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A model of natural recovery potential is presented along with component layers (overbank flow, abundance of native and non-native cover types) and assigned values, plus associated layers of bottomland boundaries, and the river channel at low flow (2010).
This is a habitat suitablilty map and component layers estimating bat watering habitat on the Colorado River bottomland in Utah during high flow conditions. The model combines the presence of prefered slow water channel types (backwaters, isolated pools and tributary mouths), with cover types amenable to bat overflights and drinking 'on-the-wing'. See Open File Report, Rasmussen and Shafroth, Colorado River Conservation Planning for geoprocessing details. For more detailed information, please visit this project's ScienceBase landing page at https://doi.org/10.5066/P927I36K, or the final report for this project at https://www.coloradomesa.edu/water-center/documents/rasmussen_shaftroth_2016_watercenter_cmu.pdf.
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Shinnville - Camp of the Green River Mining Co., at the C.F.I. mine, southeast of Green River, a temporary habitation in the bleak and inhospitable region. The 4-mule team shown is employed continuously supplying the camp with water, the necessary supply of which must be hauled up hill from a spring 6 miles distant. La Sal and Moab quadrangles, Grand County, Utah. May 25, 1918.
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Indefinite contact between the Kayenta formation and the overlying Navajo sandstone, on the west bank of the Colorado River at the mouth of (now Negro Bill) Creek, in sec. 19, T. 25 S., R. 22 E. Grand County, Utah. 1926. Plate 8-C, in U.S. Geological Survey. Professional paper 183. 1936.


map background search result map search result map Indefinite contact between the Kayenta formation and the overlying Navajo sandstone. Grand County, Utah. 1926. Wingate sandstone and underlying softer Chinle shale exposed at Big Hole on the Colorado River 8 miles east of Cisco. Grand County, Utah. October 1927. Trinalcove, Labyrinth Canyon. Grand and Emery Counties, Utah. circa 1871. River view in Labyrinth Canyon. Grand and Emery Counties, Utah. circa 1871. Tump-in-kon-tu-weap, Labyrinth Canyon. Grand and Emery Counties, Utah. circa 1871. Tump-in-kon-tu-weap, Labyrinth Canyon. Grand and Emery Counties, Utah. circa 1871. Dellenbaugh Butte, near the mouth of San Rafael.  Grand and Emery Counties, Utah. circa 1871. Bat Watering Model and Component Layers Estimated Recovery Potential for Colorado River Bottomland Riparian Habitats Vegetation Mapping of Dominant and Common Cover Types WMR 012 - Thompson Magnesium Well. Grand County, Utah. 1942. Bat Watering Model and Component Layers Estimated Recovery Potential for Colorado River Bottomland Riparian Habitats Vegetation Mapping of Dominant and Common Cover Types Indefinite contact between the Kayenta formation and the overlying Navajo sandstone. Grand County, Utah. 1926. Wingate sandstone and underlying softer Chinle shale exposed at Big Hole on the Colorado River 8 miles east of Cisco. Grand County, Utah. October 1927. WMR 012 - Thompson Magnesium Well. Grand County, Utah. 1942. Trinalcove, Labyrinth Canyon. Grand and Emery Counties, Utah. circa 1871. River view in Labyrinth Canyon. Grand and Emery Counties, Utah. circa 1871. Tump-in-kon-tu-weap, Labyrinth Canyon. Grand and Emery Counties, Utah. circa 1871. Tump-in-kon-tu-weap, Labyrinth Canyon. Grand and Emery Counties, Utah. circa 1871. Dellenbaugh Butte, near the mouth of San Rafael.  Grand and Emery Counties, Utah. circa 1871.