Platinum-group elements in sedimentary environments in the conterminous United States
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Geology topics
Source-linked reports with geographic coverage including Conterminous United States.
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This CD-ROM contains a digital version of the Geologic Map of the Conterminous United States compiled by Philip B. King and Helen M. Beikman of the U.S. Geological Survey. It excludes Alaska and Hawaii. The map was originally published in 1974 at a scale of 1:2,500,000. Although the digitized map can be displayed at different scales, the geology is not intended to be used at any scale larger than 1:2,500,000. The CD-ROM also contains the text and figures from Professional Paper 901 by the same authors. It describes the historical background of the map, details of the compilation process, and limitations to interpretation. The digital version of the text can be searched for key words and phrases. For DOS users, the CD-ROM contains a menu-driven operating system and MAPPER display software, a user-friendly map display package. Both raster image and vector versions of the geologic map can be displayed. The raster version is at 1-km resolution in the original Albers Equal Area projection. The vector version is stored unprojected in decimal degrees. Other thematic layers include cities, counties, States, and major roads. The geologic map is provided in the following additional formats: - Arc/INFO 6.1.1 Export - Digital Line Graph (DLG) Optional - Drawing Exchange File (DXF) - Map Overlay Statistical System (MOSS)
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Samples of soils or other regoliths, taken at a depth of approximately 20 cm form locations about 80 km apart, throughout the conterminous United States, were analyzed for their content of elements. In this manner, 1,318 sampling sites were chosen, and the results of the sample analyses for 50 elements were plotted on maps. The arithmetic and geometric mean, the geometric deviation, and a histogram showing frequencies of analytical values are given for 47 elements. The lower concentrations of some elements (notable, aluminum, barium, calcium, magnesium, potassium, sodium, and strontium) in most samples of surficial materials from the Eastern United States, and the greater abundance of heavy metals in the same materials of the Western United States, indicates a regional geochemical pattern of the largest scale. The low concentrations of many elements in soils characterize the Atlantic Coastal Plain. Souls of the Pacific Northwest generally have high concentrations of aluminum, cobalt, iron, scandium, and vanadium, but are low in boron. Soils of the Rocky Mountain region tend to have high concentrations of copper, lead, and zinc. High mercury concentrations in surficial materials are characteristic of Gulf Coast sampling sites and the Atlantic coast sites of Connecticut, Massachusetts, and Maine. At the State level, Florida has the most striking geochemical pattern by having soils that are low in concentrations of most elements considered in this study. Some smaller patterns of element abundance can be noted, but the degree of confidence in the validity of these patterns decreases as the patterns become less extensive.
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