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Water levels and artesian pressure in observation wells in the United States, 1941, Part 5, Northwestern States

Water Resources Division, U.S. Geological Survey

1942, Water Supply Paper 940

Surface water supply of the United States, 1940, Part VIII, Western Gulf of Mexico basins

Water Resources Division, U.S. Geological Survey

1942, Water Supply Paper 898

Ground-water conditions in the vicinity of Portsmouth, New Hampshire, Febuary 9, 1942

M.L. Brashears Jr.

1942, Open-File Report 50-56

Notes on the possibilities of domestic water supplies in the area to be irrigated from the Heart Mountain Canal; Ground water conditions in the area of the Heart Mountain Division of the Shoshone Irrigation Project, Wyoming

William G. Pierce

1942, Open-File Report 42-29

Water levels and artesian pressure in observation wells in the United States, 1940, Part 3, North-Central States

Water Resources Division, U.S. Geological Survey

1942, Water Supply Paper 908

Surface water supply of the United States, 1941 : Part 10, The Great Basin

Water Resources Division, U.S. Geological Survey

1942, Water Supply Paper 930

Surface water supply of the United States, 1940, Part I, North Atlantic slope basins

Water Resources Division, U.S. Geological Survey

1942, Water Supply Paper 891

Water utilization in tributaries of the Rogue River

Water Resources Division, U.S. Geological Survey

1942, Open-File Report 42-10

Mineral production of Alaska in 1941

Water Resources Division, U.S. Geological Survey

1942, Open-File Report 42-24

Topographic and geologic map of the Kokomo-Robinson area, Summit County, Colorado

Water Resources Division, U.S. Geological Survey

1942, Open-File Report 42-16

Water levels and artesian pressure in observation wells in the United States, 1940, Part 1, Northeastern States

Water Resources Division, U.S. Geological Survey

1942, Water Supply Paper 906

Surface water supply of the United States, 1941 : Part 12, North Pacific drainage basins

Water Resources Division, U.S. Geological Survey

1942, Water Supply Paper 932

Surface water supply of the United States, 1941 : Part 14, Pacific slope basins in Oregon and lower Columbia River basin

Water Resources Division, U.S. Geological Survey

1942, Water Supply Paper 934

Water supply of the Dakota sandstone in the Ellendale-Jamestown area, North Dakota, with reference to changes between 1923 and 1938

Leland Keith Wenzel, H. H. Sand

1942, Water Supply Paper 889-A

The Dakota sandstone underlies most of North Dakota and South Dakota and considerable parts of nearby States. In most of the area that it occupies it is covered with thick deposits of younger formations, chiefly shale, that confine the water in the sandstone under considerable pressure. Where the topography is...

Methods for determining permeability of water-bearing materials, with special reference to discharging-well methods, with a section on direct laboratory methods and bibliography on permeability and laminar flow

Leland Keith Wenzel, Vinton Crews Fishel

1942, Water Supply Paper 887

Nickel-copper deposit at Snipe Bay, Baranof Island, Alaska

Water Resources Division, U.S. Geological Survey

1942, Open-File Report 42-28

Surface water supply of the United States, 1940, Part VI, Missouri River basin

Water Resources Division, U.S. Geological Survey

1942, Water Supply Paper 896

Andersonville bauxite district, Georgia

Water Resources Division, U.S. Geological Survey

1942, Open-File Report 42-12

Spirit leveling in Illinois, 1896-1942. Part 1, Southern Illinois

Water Resources Division, U.S. Geological Survey

1942, Bulletin 930-A

Floods of March 1938 in southern California

H.C. Troxell

1942, Water Supply Paper 844

Industrial quality of public water supplies in Georgia, 1940

William L. Lamar

1942, Water Supply Paper 912

Monthly evapo‐transpiration losses from natural drainage‐basin

Walter B. Langbein

1942, Eos, Transactions, American Geophysical Union (23) 604-614

With limited restrictions the hydrologic cycle in a given area may be expressed essentially as follows: P = (R + E + ΔFm) in which P represents the precipitation during a given period, R that portion which has reached or will reach the stream‐channel either through surface or subsurface paths,...

Recharge to ground‐water from floods in a typical desert wash, Pinal County, Arizona

H. M. Babcock, E. M. Cushing

1942, Eos, Transactions, American Geophysical Union (23) 49-56

Queen Creek, considered in this paper, is a typical large desert wash. It rises in the Pinal Mountains near the mining town of Superior and enters the outwash‐plain at Black Point about three miles north of Florence Junction (see Fig. 1). Thence it passes over the desert in a southwesterly...

Recharge and discharge of the ground‐water reservoirs on the High Plains in Texas

W. L. Broadhurst

1942, Eos, Transactions, American Geophysical Union (23) 9-15

The High Plains in Texas occupy an area of about 35,000 square miles extending from the northern boundary of the Panhandle southward about 300 miles, and from the New Mexico line eastward an average distance of about 120 miles to a boundary which in most places is sharply defined by...

Recharge, movement, and discharge in the Edwards Limestone Reservoir, Texas

A.N. Sayre, R.R. Bennett

1942, Eos, Transactions, American Geophysical Union (23) 19-27

The Edwards limestone of Lower Cretaceous age is the principal water‐bearing formation in a belt 5 to 25 miles wide that extends from Austin southwest to San Antonio and thence west through Uvalde and Del Rio to Comstock, a distance of about 250 miles (see Fig. 1). Throughout this belt...