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Publication Extents

Not all publications have extents, not all extents are completely accurate
Availability of ground water in the Blackstone River area Rhode Island and Massachusetts
Herbert E. Johnston, David C. Dickerman
1974, Water-Resources Investigations Report 74-4
The Blackstone River study area covers 83 square miles of northern Rhode Island and 5 square miles of adjacent Massachusetts (fig. 1). It includes parts of the Blackstone, Moshassuck, and Tenmile River basins, and a coastal area that drains to the brackish Seekonk and Providence Rivers. In Rhode Island, all...
Availability of ground water in the Branch River basin; Providence County, Rhode Island
H.E. Johnston, D.C. Dickerman
1974, Water-Resources Investigations Report 74-18
Stratified glacial drift consisting largely of sand and gravel constitutes the only aquifer capable of supporting continuous yields of 100 gpm (6.3 1/s) or more to individual wells. The aquifer covers about a third of the 79 mi 2 (205 km2) study area, occurring mainly in stream valleys that are...
Mineral resources of Antarctica
Nancy A. Wright, Paul L. Williams, editor(s)
1974, Circular 705
Although the existence of mineral deposits in Antarctica is highly probable, the chances of finding them are quite small. Minerals have been found there in great variety but only as occurrences. Manganese nodules, water (as ice), geothermal energy, coal, petroleum, and natural gas are potential resources that could perhaps be...
A water-quality reconnaissance of Big Bear Lake, San Bernardino County, California, 1972-1973
George A. Irwin, Michael Lemons
1974, Water-Resources Investigations Report 74-3
A water-quality reconnaissance study of the Big Bear Lake area in southern California was made by the U.S. Geological Survey from April 1972 through April 1973. The primary purpose of the study was to measure the concentration and distribution of selected primary nutrients, organic carbon, dissolved oxygen, phytoplankton, and water...
Water resources of the Crow River watershed, south-central Minnesota
Gerald F. Lindholm, D.F. Farrell, John O. Helgesen
1974, Hydrologic Atlas 528
The Crow River watershed, an area of about 2,760 square miles, is covered entirely by glacial deposits. A topographically high, east-west-trending end moraine divides most of the watershed into two drainage areas of approximately equal size. The North Fork Crow River drains a mixture of glacial outwash and till deposits,...