Ground-water development in the high plains of Colorado, with a section on chemical quality of the ground water
Arnold J. Boettcher, Robert Brennan
1966, Water Supply Paper 1819-I
The High Plains of Colorado includes all or part of 11 counties and has an area of about 9,500 square miles. The land surface slopes eastward and in most areas is gently rolling owing to erosion by ephemeral streams. The Ogallala Formation, of Pliocene age, is the principal aquifer. In...
Gunpowder Falls, Maryland : uses of a water resource today and tomorrow
Deric O’Bryan, Russell Lonnie McAvoy
1966, Water Supply Paper 1815
Hydrology of Cornfield Wash area and effects of land-treatment practices, Sandoval County, New Mexico, 1951-60
D. E. Burkham
1966, Water Supply Paper 1831
The collection of runoff and sediment data was the primary objective of the 10-year (1951-60) study in the Cornfield Wash basin, which has an area of 21.3 square miles. However, reconnaissance investigations also were made of (1) precipitation; (2) the effects of reservoirs on runoff, erosion, and sediment yield; (3)...
Hydrologic reconnaissance of Point Reyes National Seashore area, California
R. H. Dale, S. E. Rantz
1966, Open-File Report 66-22
This report summarizes the results of a hydrologic reconnaissance of the Point Reyes National Seashore area, the primary purpose of which was to appraise potential sources of water supply at park sites where visitor accommodations are proposed. Point Reyes National Seashore is a peninsular area on the California coast about...
Ground-Water Geology and Hydrology of the Kern River Alluvial-Fan Area, California
R. H. Dale, James J. French, G. V. Gordon
1966, Open-File Report 66-21
The Kern River alluvial fan is the southernmost major alluvial fan built by the streams which drain the west side of the Sierra Nevada. The climate is semiarid with rainfall near 5 inches per year. Agricultural development within the area uses over half the 700,000 acre-feet per year flow of...
Prospects for obtaining a water supply in the Fall River entrance area of Rocky Mountain National Park, Colorado, November 9, 1964
Donald L. Coffin, Edward J. Jenkins
1966, Open-File Report 66-15
Pesticides in the Boise River basin
G. L. Bodhaine
1966, Open-File Report 66-8
No abstract available....
Hydrochemical facies and ground-water flow patterns in northern part of Atlantic Coastal Plain
William Back
1966, Professional Paper 498-A
The part of the Atlantic Coastal Plain that extends from New Jersey through Virginia was selected as a suitable field model in which to study the relationships between geology, hydrology, and chemical character of ground water. The ground-water flow pattern is the principal hydrologic control on the chemical character of...
Water resources in the Everglades
William J. Schneider
1966, Photogrammetric Engineering and Remote Sensing (32) 958-965
Aerial photography is playing an important role in the evaluation of the water resources of the almost-inaccessible 1,400 square miles of Everglades in southern Florida. Color, infrared, and panchromatic photographs show salient features that permit evaluation of the overall water resources picture. The fresh water-salt water interface, drainage...
Water and the Everglades
William J. Schneider
1966, Natural History (75) 32-41
This fundamental element, whether profuse or scarce, rules the life and character of Florida's great park. But water, like living space, is a resource that civilization demands in ever increasing quantities. Examined here are the economics of water use by Florida's east coast cities and its effects on Everglades ecology....
Magnitude and frequency of Iowa floods, part one
Harlan H. Schwob
1966, Iowa Highway Research Board Bulletin 28
No abstract available....
Magnitude and frequency of Iowa floods, Part two
Harlan H. Schwob
1966, Iowa Highway Research Board Bulletin 28
Flood records for regular and partial-record gaging stations are contained in the following pages. Each listing contains the station number and name, descriptive paragraphs pertaining to the station, and a listing of the flood peaks available through the 1965 water year. Peaks above a base as well as annual peaks...
Surface water records of Nepal: Supplement no. 1
Nepal Hydrological Survey Department.
1966, Book
No Abstract available....
Selected flow characteristics of streams in the Willamette River Basin, Oregon
C. H. Swift III
1966, Report
Flow-duration, annual low-flow, and annual high-flow tables through September 30, 1963, are given in this report for 110 stream-gaging stations in the Willamette and Sandy River basins. These tables summarize the basic data needed to define the streamflow characteristics at the gaging stations. The content of each of the three...
Floods of June 24-25, 1966 in southwest-central North Dakota
Orlo A. Crosby
1966, Report
A severe thunderstorm accompanied by much hail swept through southwest-central North Dakota on the afternoon of June 24. Rainfall of up to 13 inches caused floods higher than any previously known in the area. The isohyetal map (fig. 1) indicates the extent and magnitude of the storm. This map was...
Insecticide contaminations in wetland habitats and their effects on fish- eating birds
James O. Keith
1966, Journal of Applied Ecology (3) 71-85
An unusual mortality of fish-eating birds occurred at the Tule Lake National Wildlife Refuge in California between 1960 and 1962. Over 1100 dead birds of ten species were found during that period. Investigations of the mortality indicated that birds died as a result of their exposure to toxaphene, which was...
Hydration of natural glass and formation of perlite
I. Friedman, R.L. Smith, W.D. Long
1966, Geological Society of America Bulletin (77) 323-328
The hydration rate of rhyolitic glass has been determined at temperatures ranging from 5° C to 100° C. The relationship between the depth of hydration, x, and time, t is x2 = kt; k varies from 0.4 μ2/103 years at 5° C to 104 μ2/103 years at 100° C; k is independent of the...
Tropical lakes, copropel, and oil shale
W.H. Bradley
1966, GSA Bulletin (77) 1333-1337
During a long-continued study of the lacustrine beds of the Eocene Green River Formation, I have tried to interpret past events from observation of present-day processes. After a search of some 40 years, four lakes have been found that are producing a kind of organic ooze judged to be a...
Pesticide residues in the ecosystem
E. H. Dustman, Lucille F. Stickel
S. Breth, editor(s)
1966, Book chapter, Pesticides and their effects on soils and water
Pesticide residues have become a component of nearly all living organisms. Nearly all California birds and fish collected in a 1963 pesticide survey contained residues. Discovery of DDT and metabolites in Antarctic animals in 1964 pushed the distribution of pesticides to the remotest portions of the globe. Exchange of pesticides...
Development of permeability and storage in the tertiary limestones of the southeastern states, USA
H. E. LeGrand, V. T. Stringfield
1966, International Association of Scientific Hydrology - Bulletin (11) 61-73
Permeability and storage characteristics in the Tertiary limestone system of southern United States have developed progressively but non-uniformly as circulation of water and solution in the limestone have changed during the geologic and hydrologic history.The limestone formations, predominantly of Eocene age and subordinated of Oligocene and Miocene age, are widespread...
Deep layer of sediments in Alpine Lake in the tropical mid-Pacific
A.H. Woodcock, M. Rubin, R.A. Duce
1966, Science (154) 647-648
Sediments from a unique high-altitude lake on Hawaii indicate ash falls and other airborne and waterborne materials for a period estimated to extend into the Pleistocene....
Use of analog model to predict streamflow depletion, big and little Blue River basin, Nebraska
P. A. Emery
1966, Groundwater (4) 13-19
The States of Nebraska and Kansas are negotiating a compact for apportionment of the waters of the Big and Little Blue Rivers. So that the negotiating officials could allocate the water equitably, the amount of streamflow depletion caused by ground‐water withdrawals upgradient from the State line needed to be determined. At the request of the Nebraska officials, the U. S. Geological Survey...
Ground-water levels and trends May-July 1966 (Abstracted from U. S. Geological Survey “Water Resources Review”)
Faith N. Payne
1966, Groundwater (4) 55-55
No abstract available. ...
Frequency distribution of dissolved solids in ground water
G.H. Davis
1966, Groundwater (4) 5-12
The frequency distribution of dissolved‐solids content of ground waters in geologically and climatologically homogeneous terrane units commonly approximates a log‐normal distribution. A graphic logarithmic transformation is de‐scribed which permits rapid calculation of approximate values for the mean, standard deviation, and coefficient of variation. Statistical parameters calculated by this method show good agreement with known physical conditions in the terranes studied and are...
The effect of climate on drainage density and streamflow
C.W. Carlston
1966, International Association of Scientific Hydrology - Bulletin (11) 62-69
Sir Charles Cotton (1964) has pointed out that in an earlier paper (Carlston, 1963) which related drainage density to hydrology, there was insufficient emphasis on the role of climate in its effect on drainage density. Re-examination of the relation of drainage density to base flow in the 15 basins originally...