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Album caption: Example of parallel, continuous bedding within sandstone of the Thumb Member, Horse Spring Formation. An outcrop in Callville wash, north of Callville Bay, shows undulatory bedding. Photo case on the left is 50 cm square. Lake Mead area. Clark County, Nevada. ca. 1975. Same as black and white figure 9-B in U.S. Geological Survey. Professional paper 1259. 1984.
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Coral, as an indicator of past environments, is especially useful in determining past sea levels. Some types of corals, such as brain coral, must live close to the surface. As the sea level rises with the melting of the ice sheets, the corals must grow upward to survive. If the age of the corals can be determined, the past rate of sea level rise can be estimated. As the ice sheets melted rapidly during the latest ice age, sea levels rose at a rate of 8 feet in 100 years. Page 6, U.S. Geological Survey Circular 1085.
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Indiana Dunes National Lakeshore, Indiana. Storms with high winds and waves create steep narrow beaches, like this one where winter storms are frequent and especially destructive. Page 28 (bottom left), U.S. Geological Survey Circular 1085.
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Wetlands include swamps, bogs, marshes, ponds, and peat lands. Circa 1990. Page 22 (bottom left photo), U.S. Geological Survey Circular 1085.
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Indiana Dunes National Lakeshore, Indiana. The unique environment of the Indiana Dunes supports a large variety of animals, such as opossums. Page 19 (bottom left), U.S. Geological Survey Circular 1085.
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Indiana Dunes National Lakeshore, Indiana. The unique environment of the Indiana Dunes supports a large variety of vegetation, such as the white trillium. Page 18 (left), U.S. Geological Survey Circular 1085.
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Indiana Dunes National Lakeshore, Indiana. The unique environment of the Indiana Dunes supports a large variety of animals, such as turtles. Page 19 (center left), U.S. Geological Survey Circular 1085.
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Indiana Dunes National Lakeshore, Indiana. Fragmentation of park land by urban areas, such this highway, can create islands of natural ecosystems and can disrupt the natural movement of plants and animals. Page 16 (bottom left), U.S. Geological Survey Circular 1085.
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Indiana Dunes National Lakeshore, Indiana. This color infrared aerial photograph shows a major part of the lakeshore. Vegetation is shown in red. Page 13 (top), U.S. Geological Survey Circular 1085.
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Satellite photograph of the earth, Red Sea, Africa, Arabia, Indian and Atlantic Oceans, and wind patterns. 1991. Published on frontispiece in U.S. Geological Survey. Professional paper 560-A.
Categories: Image; Tags: NASA, Photographers, photo color print
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Indiana Dunes National Lakeshore, Indiana. The unique environment of the Indiana Dunes supports a large variety of animals, such as six-lined racerunners (lizard). Page 19 (center right), U.S. Geological Survey Circular 1085.
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Wetlands are an important nesting site for birds. Circa 1990. Page 22 (top photo), U.S. Geological Survey Circular 1085.
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Indiana Dunes National Lakeshore, Indiana. Park ranger helping children. Page VI (top right), U.S. Geological Survey Circular 1085.
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Indiana Dunes National Lakeshore, Indiana. The unique environment of the Indiana Dunes supports a large variety of vegetation, such as the prickly pear cactus. Page 18 (right), U.S. Geological Survey Circular 1085.
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Indiana Dunes National Lakeshore, Indiana. The forest changes as it approaches the shore line. Portion of page VI (center), U.S. Geological Survey Circular 1085.
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Album caption and index card: (40ct). Strata of Supai Group, Grand Canyon. B, Massive sandstone beds of cliff unit of Wescogame Formation (We) are mostly various shades of grayish orange-pink. Channels near base are filled with conglomerate. Manakacha Formation (M) below. Thunder River Trail. Grand Canyon National Park. Coconino County, Arizona. n.d. (Graphics on published photo only). Published as figure MS2-B in U.S. Geological Survey. Professional Paper 1173. 1982. Note: Same photo as med00040_ct.
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Album caption: Forest at Indiana Dune National Lakeshore, Indiana. Published as picture at top left on page VI in the U.S. Geological Survey Circular 1085 (1991).
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Indiana Dunes National Lakeshore, Indiana. The unique environment of the Indiana Dunes supports a large variety of animals, such as raccoons. Page 19 (bottom right), U.S. Geological Survey Circular 1085. 1991


    map background search result map search result map Example of parallel, continuous bedding within sandstone of the Thumb Member, Horse Spring Formation. Clark County, Nevada. 1975. Forest at Indiana Dune National Lakeshore, Porter County, Indiana. 1991. Park ranger helping children. Indiana Dunes National Lakeshore, Porter County, Indiana. 1991. The forest changes as it approaches the shoreline. Indiana Dunes National Lakeshore, Porter County, Indiana. 1991. Wind-blown sand encroaching on the forest. Indiana Dunes National Lakeshore, Porter County, Indiana. 1991. This color infrared aerial photograph shows a major part of the lakeshore. Indiana Dunes National Lakeshore, Indiana. Porter County, Indiana. 1991. Fragmentation of park land by urban areas. Indiana Dunes National Lakeshore, Porter County, Indiana. 1991. The unique environment of the Indiana Dunes supports a large variety of vegetation. Indiana Dunes National Lakeshore, Porter County, Indiana. 1991. The unique environment of the Indiana Dunes. Indiana Dunes National Lakeshore, Porter County, Indiana. 1991. The unique environment of the Indiana Dunes supports a large variety of animals. Indiana Dunes National Lakeshore, Indiana. Porter County, Indiana. 1991. The unique environment of the Indiana Dunes supports a large variety of animals. Indiana Dunes National Lakeshore, Indiana. Porter County, Indiana. 1991 The unique environment of the Indiana Dunes supports a large variety of animals. Indiana Dunes National Lakeshore, Indiana. Porter County, Indiana. 1991. The unique environment of the Indiana Dunes supports a large variety of animals. Indiana Dunes National Lakeshore, Indiana. Porter County, Indiana. 1991. Wetlands are commonly adjacent to dunes. Indiana Dunes National Lakeshore, Indiana. Porter County, Indiana. 1991. Storms with high winds and waves create steep narrow beaches. Indiana Dunes National Lakeshore, Porter County, Indiana. Middle Cliff Member, Supai Group, Thunder River Trail, Grand Canyon National Park, Coconino County, Arizona. 1967. Forest at Indiana Dune National Lakeshore, Porter County, Indiana. 1991. Park ranger helping children. Indiana Dunes National Lakeshore, Porter County, Indiana. 1991. The forest changes as it approaches the shoreline. Indiana Dunes National Lakeshore, Porter County, Indiana. 1991. Wind-blown sand encroaching on the forest. Indiana Dunes National Lakeshore, Porter County, Indiana. 1991. This color infrared aerial photograph shows a major part of the lakeshore. Indiana Dunes National Lakeshore, Indiana. Porter County, Indiana. 1991. Fragmentation of park land by urban areas. Indiana Dunes National Lakeshore, Porter County, Indiana. 1991. The unique environment of the Indiana Dunes supports a large variety of vegetation. Indiana Dunes National Lakeshore, Porter County, Indiana. 1991. The unique environment of the Indiana Dunes. Indiana Dunes National Lakeshore, Porter County, Indiana. 1991. The unique environment of the Indiana Dunes supports a large variety of animals. Indiana Dunes National Lakeshore, Indiana. Porter County, Indiana. 1991. The unique environment of the Indiana Dunes supports a large variety of animals. Indiana Dunes National Lakeshore, Indiana. Porter County, Indiana. 1991 The unique environment of the Indiana Dunes supports a large variety of animals. Indiana Dunes National Lakeshore, Indiana. Porter County, Indiana. 1991. The unique environment of the Indiana Dunes supports a large variety of animals. Indiana Dunes National Lakeshore, Indiana. Porter County, Indiana. 1991. Wetlands are commonly adjacent to dunes. Indiana Dunes National Lakeshore, Indiana. Porter County, Indiana. 1991. Storms with high winds and waves create steep narrow beaches. Indiana Dunes National Lakeshore, Porter County, Indiana. Example of parallel, continuous bedding within sandstone of the Thumb Member, Horse Spring Formation. Clark County, Nevada. 1975. Middle Cliff Member, Supai Group, Thunder River Trail, Grand Canyon National Park, Coconino County, Arizona. 1967.