General geology and ground-water resources of the island of Maui, Hawaii
Harold T. Stearns, Gordon Andrew Macdonald
1942, Bulletin 7
Maui, the second largest island in the Hawaiian group, is 48 miles long, 26 miles wide, and covers 728 square miles. The principal town is Wailuku. Sugar cane and pineapples are the principal crops. Water is used chiefly for irrigating cane. The purpose of the investigation was to study the...
Geologic structure and occurrence of gas in part of southwestern New York. Part 1, Structure and gas possibilities of the Oriskany sandstone in Steuben, Yates, and parts of the adjacent counties
W. H. Bradley, J. F. Pepper
1941, Bulletin 899-A
The area covered by this report is in southwestern New York and includes a little more than 3,000 square miles in Steuben and Yates counties and parts of the six adjacent counties. This area has been mapped to determine the structural attitude of the exposed rocks, so as to aid...
Subsurface geology and oil and gas resources of Osage County, Oklahoma. Part 9, Townships 23 and 24 north, range 7 east
N. W. Bass, W. R. Dillard, L. E. Kennedy, H. B. Goodrich
1941, Bulletin 900-I
No abstract available....
Subsurface geology and oil and gas resources of Osage County, Oklahoma. Part 8, Parts of township 20 north, ranges 9 and 10 east, and township 21 north, ranges 8 and 9 east and all of township 21 north, range 10 east
C. T. Kirk, W. R. Dillard, Otto Leatherock, H. D. Jenkins
1941, Bulletin 900-H
The area whose subsurface geology and oil and gas resources are described in this report lies along the southern border of Osage County, Okla., and includes parts of T. 20 N., Rs. 9 and 10 E., and of T. 21 N., Rs. 8 and 9 E., and all of T....
Subsurface geology and oil and gas resources of Osage County, Oklahoma. Part 7, Townships 20 and 21 north, ranges 11 and 12 east
W.R. Dillar, N. W. Bass, C. T. Kirk
1941, Bulletin 900-G
No abstract available....
Pre-Cambrian geology and mineral resources of the Delaware Water Gap and Easton quadrangles, New Jersey and Pennsylvania
William Shirley Bayley
1941, Bulletin 920
No abstract available....
Surface water supply of the United States, 1939, Part II, South Atlantic slope and eastern Gulf of Mexico basins
Water Resources Division, U.S. Geological Survey
1941, Water Supply Paper 872
Geology of the Moreno Valley, New Mexico
L.L. Ray, J.F. Smith Jr.
1941, Geological Society of America Bulletin (52) 177-210
The Moreno Valley, located along the complex eastern boundary between the Sangre de Cristo Mountains and the Great Plains, is structurally a broad, northwardplunging syncline, disrupted by smaller folds and faults. This major synclinal structure is the result of the Laramide disturbance. Deformation, however, has continued possibly into the Quaternary....
Depth of active solution by ground‐waters in the Pecos Valley, New Mexico
Arthur M. Morgan
1941, Eos, Transactions, American Geophysical Union (22) 779-783
The Pecos River Drainage‐Basin is underlain by a thick series of Permian rocks consisting largely of limestone, gypsum (or anhydrite), and halite. The beds have a regional eastward or southeastward dip of 40 to 80 feet to the mile and successively younger beds are exposed at the surface from west...
Factors influencing runoff during the flood of December, 1937, in northern California
W.G. Boyt
1941, Eos, Transactions, American Geophysical Union (22) 124-129
Engineers and hydrologists engaged on flood‐problems throughout much of the United States east of the Rocky Mountains must deal to a considerable extent with wide‐spread storms covering thousands of square miles. The gradations of meteorologic conditions as regard both area and time are relatively homogeneous during such storm‐events and are...
Magnetic studies by the Geophysical Section of the United States Geological Survey
F.W. Lee
1941, Eos, Transactions, American Geophysical Union (22) 460-462
Continued progress has been made in magnetic surveys over large sectional areas by G. R. MacCarthy. Beginning in Florida south of the Okeefenokee Swamp, magnetic traverses were measured and continued through the southern part of Georgia. The most northerly traverses crossed regions where they contacted the crystallines near the surface...
Contamination of Lake Wewoka and fresh-water sands by disposal of oil-well brines near Wewoka, Seminole County, Oklahoma
Stuart L. Schoff, Robert H. Dott, Cecil Gordon Lalicker
1941, Open-File Report 41-32
This report deals with ground-water conditions in an area about 5 miles wide from east to west and 8 miles long from north to south, in Tps. 8 and 9 N., Rs. 7 and 8 E., in Seminole County, Oklahoma, including the town of Wewoka and Lake Wewoka. The possible...
Geologic structure and occurrence of gas in part of southwestern New York
Wilmot H. Bradley, James F. Pepper, G. B. Richardson
1941, Bulletin 899
The area covered by this report is in southwestern New York and includes a little more than 3,000 square miles in Steuben and Yates counties and parts of the six adjacent counties. This area has been mapped to determine the structural attitude of the exposed rocks, so as to aid...
Transit traverse in Missouri, 1900-1937. Part 6, Northeastern Missouri, 1900-37
John George Staack
1940, Bulletin 916-F
This bulletin, which for convenience is to be published in eight parts, contains the results of all transit traverse* done In Missouri through 1937 by the Geological Survey, United States Department of the Interior, including those heretofore published. (See page X.) Each of the parts deals with one of eight...
Transit traverse in Missouri, 1900-1937. Part 5, Southwestern Missouri, 1900-37
John G. Staack
1940, Bulletin 916-E
This bulletin, which for convenience is to be published in eight parts, contains the results of all transit traverse* done In Missouri through 1937 by the Geological Survey, United States Department of the Interior, including those heretofore published. (See page X.) Each of the parts deals with one of eight...
Transit traverse in Missouri, 1900-1937. Part 4, Northwestern Missouri, 1911-37
John G. Staack
1940, Bulletin 916-D
This bulletin, which for convenience is to be published in eight parts, contains the results of all transit traverse* done In Missouri through 1937 by the Geological Survey, United States Department of the Interior, including those heretofore published. (See page X.) Each of the parts deals with one of eight...
Transit traverse in Missouri, 1900-1937. Part 7, Central Missouri, 1902-37
John George Staack
1940, Bulletin 916-G
This bulletin, which for convenience is to be published in eight parts, contains the results of all transit traverse* done In Missouri through 1937 by the Geological Survey, United States Department of the Interior, including those heretofore published. (See page X.) Each of the parts deals with one of eight...
Transit traverse in Missouri, 1900-1937. Part 8, West-central Missouri, 1906-37
John G. Staack
1940, Bulletin 916-H
This bulletin, which for convenience is to be published in eight parts, contains the results of all transit traverse* done In Missouri through 1937 by the Geological Survey, United States Department of the Interior, including those heretofore published. (See page X.) Each of the parts deals with one of eight...
Transit traverse in Missouri, 1900-1937. Part 3, East-central Missouri, 1903-37
John George Staack
1940, Bulletin 916-C
This bulletin, which for convenience is to be published in eight parts, contains the results of all transit traverse* done In Missouri through 1937 by the Geological Survey, United States Department of the Interior, including those heretofore published. (See page X.) Each of the parts deals with one of eight...
Subsurface geology and oil and gas resources of Osage County, Oklahoma. Part 6, Township 28 north, ranges 10 and 11 east, and township 29 north, ranges 9 to 11 east
H. B. Goodrich, L. E. Kennedy, Otto Leatherock
1940, Bulletin 900-F
No abstract available....
Natural water loss in selected drainage basins
Gordon R. Williams
1940, Water Supply Paper 846
Determinations of areal rainfall, run-off, and water loss, comprising largely evaporation from land surfaces and transpiration by vegetation, are essential in indicating the hydrologic characteristics of river basins. This report is primarily a statistical study that presents the results of computations of annual water loss, or annual rainfall minus annual...
Transit traverse in Missouri, 1900-1937. Part 2, South-central Missouri, 1908-37
John George Staack
1940, Bulletin 916-B
This bulletin, which for convenience is to be published in eight parts, contains the results of all transit traverse* done In Missouri through 1937 by the Geological Survey, United States Department of the Interior, including those heretofore published. (See page X.) Each of the parts deals with one of eight...
Surface water supply of the United States, 1938, Part II, South Atlantic slope and eastern Gulf of Mexico basins
Water Resources Division, U.S. Geological Survey
1940, Water Supply Paper 852
Subsurface geology and oil and gas resources of Osage County, Oklahoma. Part 5, Townships 26 and 27 north, ranges 10 and 11 east
L. E. Kennedy, W. E. Shamblin, Otto Leatherock, N. W. Bass
1940, Bulletin 900-E
No abstract available....
Subsurface geology and oil and gas resources of Osage County, Oklahoma. Part 4, Townships 24 and 25 north, ranges 10 and 11 east
L. E. Kennedy, J. D. McClure, H. D. Jenkins, N. W. Bass
1940, Bulletin 900-D
No abstract available....
