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Falls at mouth of Fall Creek in northwestern part of Burnet quadrangle, the falls go over Ellenburger limestone which is covered with travertine deposited by the stream. San Saba County, Texas. 1912. Plate 7 in U.S. Geological Survey. Folio 183. 1912.
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Ranch in sec. 14, T.21 N., R. 10 W. Washington. Circa 1899. Plate 6-B in U.S. Geological Survey, Professional paper 7. 1902.
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Evergreen Post Office. Washington. Circa 1899. Plate 6-A in U.S. Geological Survey, Professional paper 7. 1902.
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Divide between Queets and Queniult Rivers. Washington. Circa 1899. Plate 3-B in U.S. Geological Survey, Professional paper 7. 1902.
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Moraines of Emmons Glacier in the valley of White River and Inter Fork, Emmons Glacier is visible upstream to left of area 22. Baker Point is the prominent snow-covered ridge at top left. Numbered points indicate the approximate locations of areas studied (extents from braided stream next to forest in center foreground to left curve of stream in the middle ground). Mount Rainer National Park, Pierce County, Washington. July 18, 1959. Published as figure 9 in U. S. Geological Survey. Professional paper 387-A. 1961.
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Valley of East Tennessee bear Jonesboro, looking southeast. This valley is composed of many rounded hills, characteristic of Knox dolomite, with red clay soil and some chert. The summits rise in general to elevations of 1,700 to 1,800 feet and are remnants of an ancient plain that extends to the foot Cherokee Mountain, in the background. This mountain rises abruptly about 1,000 feet above the limestone hills. Beyond, a peak of Buffalo Mountain and the high dome of Unaka Mountain are visible. Washington County, Tennessee. 1907. Figure 16 in U.S. Geological Survey. Folio 151. 1907.
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Petroliferous Moenkopi strata in eastern part of Circe Cliffs: Garfield County, Utah. 1921. Plate 31-A in U.S. Geological Survey. Professional paper 164. 1931.
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Glen Canyon west of Kane Creek; monuments and buttes of hard sandstone (Entrada, Summerville, and Morrison formations) on a broad bench formed by erosion of weak strata (Carmel formation) overlying hard sandstone (Navajo). Kane County, Utah. 1921. Plate 22-A, in U.S. Geological Survey. Professional paper 164. 1931.
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Streamflow in the Colorado River is heavily influenced by high-elevation snowpack. Warming temperatures in spring can reduce snow-fed flows, with serious implications for the water supplies that support communities and wildlife. While it is already well-known that precipitation has a significant influence on river flow, recent observations suggest that temperature and the amount of water in soil may also influence streamflow. In the face of a changing climate, it is important that resource managers understand how factors such as changing temperatures and precipitation will affect this vital water source. To address this need, researchers are examining records of streamflow, temperature, soil moisture, and precipitation...
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Form a panorama of Big Horn Hot Spring, Thermopolis; looking east across Big Horn River and the terraces of travertine to the "Red Beds' which are inclined southward on the flank of a sharp anticline whose apex lies to the left. From this anticline 18,600,000 gallons of sulphur water issues every 24 hours, having a temperature of 135 degrees F, and carrying calcium carbonate and other mineral matter in solution. In the distance in order from left to right, are the older Chugwater red beds, the Alcova marine limestone, gypsum and shale of the upper part of the Chugwater, the marine Sundance formation, (the basal sandstone is absent here), the Morrison formation and the sandstone correlated with the lower sandstone...
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Detail of the Bishop conglomerate on the south side of Little Mountain; the larger boulders are a little more than 1 foot across. Sweetwater County, Wyoming. 1930. Plate 39-B, U.S.Geological Survey Professional paper 185-I. 1936.
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Section of Illinoian till temporarily exposed in bed of Detroit River near Stony Island during excavation of Livingstone Channel, this till is very stony compared with the Wisconsin till shown in Stose 961, Wayne County, Michigan. 1916. Plate 5 in U.S. Geological Survey. Folio 205. 1917.
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Album caption: Quartzite at north side of Stony Island, 4 miles northeast of Waterloo, showing glacially smooth surface. Waterloo quadrangle, Dodge County, Wisconsin. October 17, 1903. Plate 8-B in U.S. Geological Survey. Professional paper 106. 1918.
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Typical weathered surface of Bighorn limestone, shows projecting reticulations due to silica. The space represented is about 4 x 5 feet. Sheridan County, Wyoming. August 1897. Plate 11-B in U.S. Geological Survey. Professional paper 51. 1906.
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Conglomeratic sandstone regarded by the writer as the base of the Cloverly formation south of Hyattville, resting on the carbonaceous shale, which separates it from the Morrison. Big Horn County, Wyoming. 1922. Plate 34-C in U.S. Geological Survey. Professional paper 149. 1927.
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This dataset provides maps of biomass carbon (C) in gC/m2 of coastal herbaceous wetlands at a resolution of 30 m across the conterminous United States (CONUS) for 2015.
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Late basalt flow resting on a conglomerate of basalt and other boulders: on road from Toquerville to La Verkin, Washington County, Utah. 1919. Plate 13-B in U.S. Geological Survey. Professional paper 129. 1922.
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Looking down San Juan Canyon, at a point 9 miles by stream above Honaker Trail, canyon has been cut in Goodridge formation. San Juan County, Utah. 1921. Plate 3-A in U.S. Geological Survey. Professional paper 132. 1925. Plate 3-B in U.S. Geological Survey. Professional paper 188. 1938. Plate 2-B in U.S. Geological Survey. Water-supply paper 538. 1924.
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View looking northwest from head of Armstrong Canyon, across flat into which upper White Canyon and its tributaries are cut. San Juan County, Utah. 1925. Plate 5-B in U.S. Geological Survey. Professional paper 188. 1938.


map background search result map search result map Waterloo Quartzite , showing dip of beds at the north end of Stony Island, from the north. Wisconsin, 1903. Detail of the Bishop conglomerate on the south side of Little Mountain.  Sweetwater County, Wyoming. 1930. Valley of East Tennessee bear Jonesboro, looking southeast. Washington County, Tennessee. 1907. Form a panorama of Big Horn Hot Spring, Thermopolis. Hot Springs County, Wyoming. 1922. Conglomeratic sandstone, the base of the Cloverly formation south of Hyattville. Big Horn County, Wyoming. 1922. View looking northwest from head of Armstrong Canyon, across flat into which upper White Canyon and its tributaries are cut.  San Juan County, Utah. 1925. Looking down San Juan Canyon, at a point 9 miles by stream above Honaker Trail, canyon has been cut in Goodridge formation. San Juan County, Utah. 1921. Petroliferous Moenkopi strata in eastern part of Circe Cliffs: Garfield County, Utah. 1921. Glen Canyon west of Kane Creek; monuments and buttes of hard sandstone (Entrada, Summerville, and Morrison formations. Kane County, Utah. 1921. Falls at mouth of Fall Creek in northwestern part of Burnet quadrangle. San Saba County, Texas, 1912. Looking down stream north 45 degrees west at Rainbow Bridge. Rainbow Bridge National Monument, Utah. 1921. Late basalt flow resting on a conglomerate of basalt and other boulders: on road from Toquerville to La Verkin. Washington County, Utah. 1919. Evergreen Post Office. Washington.  1899. Ranch in sec. 14, T.21 N., R. 10 W. Washington.  1899. Divide between Queets and Queniult Rivers. Washington.1899. Moraines of Emmons Glacier in the valley of White River and Inter Fork.  Mount Rainer National Park, Pierce County, Washington. 1959. Section of Illinoian till temporarily exposed in bed of Detroit River near Stony Island during excavation of Livingstone Channel. Wayne County, Michigan. 1916. Typical weathered surface of Bighorn limestone, shows projecting reticulations due to silica. Sheridan County, Wyoming. August 1897. Examining the Influence of Temperature and Precipitation on Colorado River Water Resources: Reconstructing the Past to Understand the Future Peak Biomass Carbon in Tidal Herbaceous Wetlands of the Conterminous United States Looking down stream north 45 degrees west at Rainbow Bridge. Rainbow Bridge National Monument, Utah. 1921. Valley of East Tennessee bear Jonesboro, looking southeast. Washington County, Tennessee. 1907. Waterloo Quartzite , showing dip of beds at the north end of Stony Island, from the north. Wisconsin, 1903. Section of Illinoian till temporarily exposed in bed of Detroit River near Stony Island during excavation of Livingstone Channel. Wayne County, Michigan. 1916. Falls at mouth of Fall Creek in northwestern part of Burnet quadrangle. San Saba County, Texas, 1912. Moraines of Emmons Glacier in the valley of White River and Inter Fork.  Mount Rainer National Park, Pierce County, Washington. 1959. Typical weathered surface of Bighorn limestone, shows projecting reticulations due to silica. Sheridan County, Wyoming. August 1897. Form a panorama of Big Horn Hot Spring, Thermopolis. Hot Springs County, Wyoming. 1922. Glen Canyon west of Kane Creek; monuments and buttes of hard sandstone (Entrada, Summerville, and Morrison formations. Kane County, Utah. 1921. Conglomeratic sandstone, the base of the Cloverly formation south of Hyattville. Big Horn County, Wyoming. 1922. Detail of the Bishop conglomerate on the south side of Little Mountain.  Sweetwater County, Wyoming. 1930. View looking northwest from head of Armstrong Canyon, across flat into which upper White Canyon and its tributaries are cut.  San Juan County, Utah. 1925. Looking down San Juan Canyon, at a point 9 miles by stream above Honaker Trail, canyon has been cut in Goodridge formation. San Juan County, Utah. 1921. Petroliferous Moenkopi strata in eastern part of Circe Cliffs: Garfield County, Utah. 1921. Late basalt flow resting on a conglomerate of basalt and other boulders: on road from Toquerville to La Verkin. Washington County, Utah. 1919. Evergreen Post Office. Washington.  1899. Ranch in sec. 14, T.21 N., R. 10 W. Washington.  1899. Examining the Influence of Temperature and Precipitation on Colorado River Water Resources: Reconstructing the Past to Understand the Future Peak Biomass Carbon in Tidal Herbaceous Wetlands of the Conterminous United States