No abstract available.
","language":"English","publisher":"U.S. Geological Survey","doi":"10.3133/ofr69296","collaboration":"Prepared in cooperation with Texas Water Development Board and Soil Conservation Service","usgsCitation":"Water Resources Division, U.S. Geological Survey, 1969, Compilation of hydrologic data, Honey Creek, Trinity River basin, Texas, 1966: U.S. Geological Survey Open-File Report 69-296, v, 125 p., https://doi.org/10.3133/ofr69296.","productDescription":"v, 125 p.","onlineOnly":"N","additionalOnlineFiles":"N","costCenters":[{"id":583,"text":"Texas Water Science Center","active":true,"usgs":true}],"links":[{"id":393359,"rank":2,"type":{"id":11,"text":"Document"},"url":"https://pubs.usgs.gov/of/1969/0296/report.pdf","linkFileType":{"id":1,"text":"pdf"}},{"id":184387,"rank":0,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/of/1969/0296/report-thumb.jpg"}],"country":"United States","state":"Texas","otherGeospatial":"Honey Creek","noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"4f4e4b1de4b07f02db6a9c97","contributors":{"authors":[{"text":"Water Resources Division, U.S. Geological Survey","contributorId":128075,"corporation":true,"usgs":false,"organization":"Water Resources Division, U.S. Geological Survey","id":532421,"contributorType":{"id":1,"text":"Authors"},"rank":1}]}} ,{"id":3796,"text":"cir630 - 1969 - Hydrogeologic information on the Glorieta Sandstone and the Ogallala Formation in the Oklahoma Panhandle and adjoining areas as related to underground waste disposal","interactions":[],"lastModifiedDate":"2022-09-02T21:59:54.813067","indexId":"cir630","displayToPublicDate":"1994-01-01T00:00:00","publicationYear":"1969","noYear":false,"publicationType":{"id":18,"text":"Report"},"publicationSubtype":{"id":5,"text":"USGS Numbered Series"},"seriesTitle":{"id":307,"text":"Circular","code":"CIR","onlineIssn":"2330-5703","printIssn":"1067-084X","active":true,"publicationSubtype":{"id":5}},"seriesNumber":"630","title":"Hydrogeologic information on the Glorieta Sandstone and the Ogallala Formation in the Oklahoma Panhandle and adjoining areas as related to underground waste disposal","docAbstract":"The Oklahoma Panhandle and adjacent areas in Texas, Kansas, Colorado, and New Mexico have prospered because of the development of supplies of fresh water and of oil and gas. The Ogallala and, in places, Cretaceous rocks produce fresh water for irrigation, public supply, and domestic and stock use through approximately 9,000 irrigation and public supply wells and a large but undetermined number of other wells. Disposal of oil-field brine and other wastes into the Glorieta Sandstone is of concern to many local residents because of the possibility of pollution of the overlying fresh-water aquifers, particularly the Ogallala Formation. Permits for 147 disposal wells into the Glorieta have been issued in this area. This report summarizes the data on geology, hydrology, and water development currently available to the U.S. Geological Survey. Geologic information indicates that, in the report area, the Glorieta Sandstone lies at depths ranging from about 500 to 1,600 feet below the base of the Ogallala Fox, nation. The rocks between those two formations are of relatively impermeable types, but solution and removal of salt has resulted in collapse of the rocks in some places. Collapse and fracturing of the rocks could result in increased vertical permeability. This might result in movement of brine under hydrostatic head from the Glorieta Sandstone into overlying fresh-water aquifers, in places where an upward hydraulic gradient exists or is created by an increase in pressure within the Glorieta. Abandoned or inadequately sealed boreholes also are possible conduits for such fluids. The mixing of water in the fresh-water aquifers with brines injected into the Glorieta is not known to have occurred anywhere in the report area, but the information available is not adequate to show positively whether or not this may have occurred locally. Much additional information on the stratigraphy and hydrology--particularly, data on the potentiometric surface of water in the Glorieta--needs to be collected and analyzed before conclusions can be drawn regarding the possibility of vertical movement of oil-field brines from the Glorieta to fresh-water aquifers above.
","language":"English","publisher":"U.S. Geological Survey","publisherLocation":"Washington, D.C.","doi":"10.3133/cir630","usgsCitation":"Irwin, J.H., and Morton, R.B., 1969, Hydrogeologic information on the Glorieta Sandstone and the Ogallala Formation in the Oklahoma Panhandle and adjoining areas as related to underground waste disposal: U.S. Geological Survey Circular 630, Report: iii, 26 p.; 4 Plates: 41.62 x 21.27 inches or smaller, https://doi.org/10.3133/cir630.","productDescription":"Report: iii, 26 p.; 4 Plates: 41.62 x 21.27 inches or smaller","numberOfPages":"34","onlineOnly":"N","additionalOnlineFiles":"N","costCenters":[],"links":[{"id":311912,"rank":304,"type":{"id":17,"text":"Plate"},"url":"https://pubs.usgs.gov/circ/1969/0630/plate-4.pdf","text":"Plate 4","linkFileType":{"id":1,"text":"pdf"}},{"id":406196,"rank":7,"type":{"id":36,"text":"NGMDB Index Page"},"url":"https://ngmdb.usgs.gov/Prodesc/proddesc_23973.htm","linkFileType":{"id":5,"text":"html"}},{"id":311911,"rank":303,"type":{"id":17,"text":"Plate"},"url":"https://pubs.usgs.gov/circ/1969/0630/plate-3.pdf","text":"Plate 3","linkFileType":{"id":1,"text":"pdf"}},{"id":30866,"rank":300,"type":{"id":11,"text":"Document"},"url":"https://pubs.usgs.gov/circ/1969/0630/report.pdf","linkFileType":{"id":1,"text":"pdf"}},{"id":311910,"rank":302,"type":{"id":17,"text":"Plate"},"url":"https://pubs.usgs.gov/circ/1969/0630/plate-2.pdf","text":"Plate 2","linkFileType":{"id":1,"text":"pdf"}},{"id":124418,"rank":0,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/circ/1969/0630/report-thumb.jpg"},{"id":311909,"rank":301,"type":{"id":17,"text":"Plate"},"url":"https://pubs.usgs.gov/circ/1969/0630/plate-1.pdf","text":"Plate 1","linkFileType":{"id":1,"text":"pdf"}}],"country":"United States","state":"Colorado, Kansas, New Mexico, Oklahoma, Texas","geographicExtents":"{\n \"type\": \"FeatureCollection\",\n \"features\": [\n {\n \"type\": \"Feature\",\n \"properties\": {},\n \"geometry\": {\n \"type\": \"Polygon\",\n \"coordinates\": [\n [\n [\n -104.388,\n 35.242\n ],\n [\n -104.388,\n 38.25\n ],\n [\n -99.25,\n 38.25\n ],\n [\n -99.25,\n 35.242\n ],\n [\n -104.388,\n 35.242\n ]\n ]\n ]\n }\n }\n ]\n}","noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"4f4e4a4ee4b07f02db627989","contributors":{"authors":[{"text":"Irwin, James Haskell","contributorId":56633,"corporation":false,"usgs":true,"family":"Irwin","given":"James","email":"","middleInitial":"Haskell","affiliations":[],"preferred":false,"id":147617,"contributorType":{"id":1,"text":"Authors"},"rank":1},{"text":"Morton, Robert B.","contributorId":50899,"corporation":false,"usgs":true,"family":"Morton","given":"Robert","email":"","middleInitial":"B.","affiliations":[],"preferred":false,"id":147616,"contributorType":{"id":1,"text":"Authors"},"rank":2}]}} ,{"id":3097,"text":"wsp1957 - 1969 - Quality of surface waters of the United States, 1964, Parts 7 and 8, lower Mississippi River basin and western Gulf of Mexico basins","interactions":[],"lastModifiedDate":"2012-02-02T00:05:33","indexId":"wsp1957","displayToPublicDate":"1994-01-01T00:00:00","publicationYear":"1969","noYear":false,"publicationType":{"id":18,"text":"Report"},"publicationSubtype":{"id":5,"text":"USGS Numbered Series"},"seriesTitle":{"id":341,"text":"Water Supply Paper","code":"WSP","active":false,"publicationSubtype":{"id":5}},"seriesNumber":"1957","title":"Quality of surface waters of the United States, 1964, Parts 7 and 8, lower Mississippi River basin and western Gulf of Mexico basins","language":"ENGLISH","publisher":"U.S. Govt. 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Off.,","doi":"10.3133/wsp1957","usgsCitation":"Water Resources Division, U.S. Geological Survey, 1969, Quality of surface waters of the United States, 1964, Parts 7 and 8, lower Mississippi River basin and western Gulf of Mexico basins: U.S. Geological Survey Water Supply Paper 1957, xii, 602 p. ;23 cm., https://doi.org/10.3133/wsp1957.","productDescription":"xii, 602 p. ;23 cm.","costCenters":[],"links":[{"id":139086,"rank":0,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/wsp/1957/report-thumb.jpg"},{"id":30009,"rank":300,"type":{"id":11,"text":"Document"},"url":"https://pubs.usgs.gov/wsp/1957/report.pdf","linkFileType":{"id":1,"text":"pdf"}}],"noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"4f4e4a8be4b07f02db651a5f","contributors":{"authors":[{"text":"Water Resources Division, U.S. Geological Survey","contributorId":128075,"corporation":true,"usgs":false,"organization":"Water Resources Division, U.S. Geological Survey","id":528074,"contributorType":{"id":1,"text":"Authors"},"rank":1}]}} ,{"id":53421,"text":"ofr69328 - 1969 - Geology, hydrology, and water quality in the Fresno area, California","interactions":[],"lastModifiedDate":"2024-08-01T13:34:45.292576","indexId":"ofr69328","displayToPublicDate":"1994-01-01T00:00:00","publicationYear":"1969","noYear":false,"publicationType":{"id":18,"text":"Report"},"publicationSubtype":{"id":5,"text":"USGS Numbered Series"},"seriesTitle":{"id":330,"text":"Open-File Report","code":"OFR","onlineIssn":"2331-1258","printIssn":"0196-1497","active":true,"publicationSubtype":{"id":5}},"seriesNumber":"69-328","title":"Geology, hydrology, and water quality in the Fresno area, California","docAbstract":"The Fresno area comprises about 1.400 square miles lying west of the foothills of the Sierra Nevada and east of the trough of the San Joaquin Valley. The rainfall averages less than 10 inches per year causing agricultural development to depend mainly on surface-water deliveries and ground-water pumpage. Surface-water deliveries and ground-water pumpage, however, vary considerably from year to year. For example, in agricultural year 1958 (April 1, 1958-March 31, 1959) surface-water deliveries were about 1,340,000 acre-feet and agricultural ground-water pumpage was about 1,740,000 acre-feet, but in agricultural year 1960 deliveries were only about 560,000 acre-feet and pumpage was about 2,520,000 acre-feet.
Alluvial fans are the dominant geomorphic features in the area. Small alluvial fans have been formed near the foothills by the deposits from the numerous intermittent streams that lie both north and south of the Kings River. Thicker and much more extensive alluvial fans have been formed under most of the area by deposits from the San Joaquin and Kings Rivers.
Geologic units in the area consist of consolidated rocks and unconsolidated deposits. In turn, consolidated rocks consist of basement complex of pre-Tertiary age and marine and continental sedimentary rocks of Cretaceous and Tertiary age. Unconsolidated deposits are of both Tertiary and Quaternary age. Most of the geologic units dip gently southwestward approximately paralleling the back slope of the Sierra Nevada. Although some of these geologic units are faulted, especially in the deep subsurface, faulting has not affected the occurrence and movement of fresh ground water.
The basement complex crops out along the eastern border of the area and yields only small amounts of water to wells; the marine and continental sedimentary rocks do not crop out in the area and do not yield any water to wells.
The unconsolidated deposits are divided into an older series of Tertiary and Quaternary age, and a younger series of Quaternary age. The continental deposits of Tertiary and Quaternary age crop out beneath the extreme southeastern part of the area and yield small amounts of water to wells, and the deposits of Quaternary age crop out over most of the area and yield more than 90 percent of the water pumped from wells.
The deposits of Quaternary age in turn are divided into older alluvium, lacustrine and marsh deposits, younger alluvium, flood-basin deposits. and sand dunes.
The older alluvium is by far the most important aquifer in the Fresno area. It consists of intercalated lenses of clay, silt, silty and sandy clay, clayey and silty sand, sand, gravel, cobbles, and boulders, and in general it is fine grained near the trough of the valley and beneath the alluvial fans of intermittent streams.
In the older alluvium, yields to wells range from less than 20 gpm (gallons per minute) to more than 3,000 gpm.
The lacustrine and marsh deposits occur only in the subsurface in the western part of the area. Consisting mostly of silt and clay, they are virtually impermeable and thus restrict the vertical movement of water. These deposits from oldest to youngest are designated the E-clay, the C-clay, and the A-clay. The E-clay is the thickest and most extensive of all the lacustrine and marsh deposits.
Because the clays tend to confine ground water in the Fresno area, five water bodies are recognized. These are the unconfined water body, the shallow water body, the confined water body below the A-clay, the confined water body below the C-clay, and the confined water body below the E-clay. The unconfined water body underlies most of the Fresno area. The shallow and confined water bodies underlie parts of the extreme western part of the area. There, heads in successively underlying water bodies are less than those in overlying water bodies, indicating that some ground water moves slowly downward through the clays.
From agricultural years 1957 to 1962, outflow in the area exceeded inflow. As a result, for this period, the Fresno area had a net deficit of about 2,890,000 acre-feet. This deficit was made up for mostly by a decline in ground water stored.
Water levels in all water bodies have been declining over the years, yet when streamflow and canal deliveries are large they show a general rise.
The general movement of ground water in the Fresno area is toward the southwest, although pumping depressions near Fresno and near the western part of the area, cause ground water to move northward, southward, and westward toward them.
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A1-A425, https://doi.org/10.3133/pp650A.","productDescription":"p. 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Chapter A, to be published later in the year, will present a summary of significant results of work done during fiscal year 1969, together with lists of investigations in progress, reports published, cooperating agencies, and Geological Survey offices.
","largerWorkType":{"id":18,"text":"Report"},"largerWorkTitle":"Geological Survey research 1969","largerWorkSubtype":{"id":5,"text":"USGS Numbered Series"},"language":"English","publisher":"U.S. Government Printing Office","publisherLocation":"Washington, D.C.","doi":"10.3133/pp650C","usgsCitation":"Water Resources Division, U.S. Geological Survey, 1969, Geological Survey research 1969, Chapter C: U.S. Geological Survey Professional Paper 650, iv, 247 p., https://doi.org/10.3133/pp650C.","productDescription":"iv, 247 p.","numberOfPages":"254","costCenters":[{"id":610,"text":"Utah Water Science Center","active":true,"usgs":true}],"links":[{"id":67410,"rank":2,"type":{"id":11,"text":"Document"},"url":"https://pubs.usgs.gov/pp/0650c/report.pdf","linkFileType":{"id":1,"text":"pdf"}},{"id":123061,"rank":1,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/pp/0650c/report-thumb.jpg"}],"noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"4f4e4adfe4b07f02db6877bf","contributors":{"authors":[{"text":"Water Resources Division, U.S. Geological Survey","contributorId":128075,"corporation":true,"usgs":false,"organization":"Water Resources Division, U.S. Geological Survey","id":529923,"contributorType":{"id":1,"text":"Authors"},"rank":1}]}} ,{"id":4719,"text":"twri03A11 - 1969 - Measurement of discharge by the moving-boat method","interactions":[],"lastModifiedDate":"2012-02-02T00:05:32","indexId":"twri03A11","displayToPublicDate":"1994-01-01T00:00:00","publicationYear":"1969","noYear":false,"publicationType":{"id":18,"text":"Report"},"publicationSubtype":{"id":5,"text":"USGS Numbered Series"},"seriesTitle":{"id":336,"text":"Techniques of Water-Resources Investigations","code":"TWRI","active":false,"publicationSubtype":{"id":5}},"seriesNumber":"03-A11","title":"Measurement of discharge by the moving-boat method","docAbstract":"This chapter describes the procedures for measuring discharge in large streams by the moving-boat technique. During the traverse of a boat across a stream, a sonic sounder records the geometry of the cross section, and a continuously operating current meter senses the combined stream and boat velocities. These data are converted to discharge for the cross section quickly, efficiently, and inexpensively. Measurements obtained by the moving-boat technique compare within 5 percent of measurements obtained by conventional means. Field and office procedures applicable to this method are outlined. Theory of technique is developed and equipment required is described. Selection and preparation of the cross section is detailed. A complete facsimile example of computation of a moving-boat measurement is given, and the determination and application of adjustment factors are described.","language":"ENGLISH","publisher":"U.S. Govt. Print. Off.,","doi":"10.3133/twri03A11","issn":"0565-596X","usgsCitation":"Smoot, G.F., and Novak, C.E., 1969, Measurement of discharge by the moving-boat method: U.S. Geological Survey Techniques of Water-Resources Investigations 03-A11, vi, 22 p. :ill. ;26 cm. Reprinted in 1977., https://doi.org/10.3133/twri03A11.","productDescription":"vi, 22 p. :ill. ;26 cm. Reprinted in 1977.","costCenters":[],"links":[{"id":139085,"rank":0,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/thumbnails/usgs_thumb.jpg"},{"id":347,"rank":100,"type":{"id":15,"text":"Index Page"},"url":"https://pubs.usgs.gov/twri/twri3-a11/","linkFileType":{"id":5,"text":"html"}}],"noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"4f4e4a28e4b07f02db611030","contributors":{"authors":[{"text":"Smoot, George F.","contributorId":34116,"corporation":false,"usgs":true,"family":"Smoot","given":"George","email":"","middleInitial":"F.","affiliations":[],"preferred":false,"id":149674,"contributorType":{"id":1,"text":"Authors"},"rank":1},{"text":"Novak, Charles E.","contributorId":76723,"corporation":false,"usgs":true,"family":"Novak","given":"Charles","email":"","middleInitial":"E.","affiliations":[],"preferred":false,"id":149675,"contributorType":{"id":1,"text":"Authors"},"rank":2}]}} ,{"id":3078,"text":"wsp1901 - 1969 - Surface water supply of the United States, 1961-65: Part 1. North Atlantic slope basins: Volume 1. Basins from Maine to Connecticut","interactions":[],"lastModifiedDate":"2022-11-02T19:31:35.448472","indexId":"wsp1901","displayToPublicDate":"1994-01-01T00:00:00","publicationYear":"1969","noYear":false,"publicationType":{"id":18,"text":"Report"},"publicationSubtype":{"id":5,"text":"USGS Numbered Series"},"seriesTitle":{"id":341,"text":"Water Supply Paper","code":"WSP","active":false,"publicationSubtype":{"id":5}},"seriesNumber":"1901","title":"Surface water supply of the United States, 1961-65: Part 1. North Atlantic slope basins: Volume 1. Basins from Maine to Connecticut","docAbstract":"No abstract available.
","language":"English","publisher":"U.S. Geological Survey","doi":"10.3133/wsp1901","usgsCitation":"Water Resources Division, U.S. Geological Survey, 1969, Surface water supply of the United States, 1961-65: Part 1. North Atlantic slope basins: Volume 1. Basins from Maine to Connecticut: U.S. Geological Survey Water Supply Paper 1901, Report: xi, 1027 p.; 1 Plate: 25.00 × 35.00 inches, https://doi.org/10.3133/wsp1901.","productDescription":"Report: xi, 1027 p.; 1 Plate: 25.00 × 35.00 inches","costCenters":[],"links":[{"id":139416,"rank":0,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/wsp/1901/report-thumb.jpg"},{"id":29950,"rank":400,"type":{"id":17,"text":"Plate"},"url":"https://pubs.usgs.gov/wsp/1901/plate-1.pdf","linkFileType":{"id":1,"text":"pdf"}},{"id":29951,"rank":300,"type":{"id":11,"text":"Document"},"url":"https://pubs.usgs.gov/wsp/1901/report.pdf","linkFileType":{"id":1,"text":"pdf"}},{"id":409074,"rank":4,"type":{"id":36,"text":"NGMDB Index Page"},"url":"https://ngmdb.usgs.gov/Prodesc/proddesc_25126.htm","linkFileType":{"id":5,"text":"html"}}],"country":"United States","state":"Connecticut, Maine, Massachusetts, New Hampshire, Rhode Island, Vermont","geographicExtents":"{\n \"type\": \"FeatureCollection\",\n \"features\": [\n {\n \"type\": \"Feature\",\n \"properties\": {},\n \"geometry\": {\n \"coordinates\": [\n [\n [\n -66.30105327026975,\n 47.52171404918724\n ],\n [\n -73.42461764114435,\n 47.52171404918724\n ],\n [\n -73.42461764114435,\n 41.240450495549254\n ],\n [\n -66.30105327026975,\n 41.240450495549254\n ],\n [\n -66.30105327026975,\n 47.52171404918724\n ]\n ]\n ],\n \"type\": \"Polygon\"\n }\n }\n ]\n}","noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"4f4e4af8e4b07f02db6942ac","contributors":{"authors":[{"text":"Water Resources Division, U.S. Geological Survey","contributorId":128075,"corporation":true,"usgs":false,"organization":"Water Resources Division, U.S. Geological Survey","id":528059,"contributorType":{"id":1,"text":"Authors"},"rank":1}]}} ,{"id":4686,"text":"twri05C1 - 1969 - Laboratory theory and methods for sediment analysis","interactions":[],"lastModifiedDate":"2012-02-02T00:05:31","indexId":"twri05C1","displayToPublicDate":"1994-01-01T00:00:00","publicationYear":"1969","noYear":false,"publicationType":{"id":18,"text":"Report"},"publicationSubtype":{"id":5,"text":"USGS Numbered Series"},"seriesTitle":{"id":336,"text":"Techniques of Water-Resources Investigations","code":"TWRI","active":false,"publicationSubtype":{"id":5}},"seriesNumber":"05-C1","title":"Laboratory theory and methods for sediment analysis","docAbstract":"The diverse character of fluvial sediments makes the choice of laboratory analysis somewhat arbitrary and the pressing of sediment samples difficult. This report presents some theories and methods used by the Water Resources Division for analysis of fluvial sediments to determine the concentration of suspended-sediment samples and the particle-size distribution of both suspended-sediment and bed-material samples. Other analyses related to these determinations may include particle shape, mineral content, and specific gravity, the organic matter and dissolved solids of samples, and the specific weight of soils.\r\nThe merits and techniques of both the evaporation and filtration methods for concentration analysis are discussed. Methods used for particle-size analysis of suspended-sediment samples may include the sieve pipet, the VA tube-pipet, or the BW tube-VA tube depending on the equipment available, the concentration and approximate size of sediment in the sample, and the settling medium used. The choice of method for most bed-material samples is usually limited to procedures suitable for sand or to some type of visual analysis for large sizes.\r\nSeveral tested forms are presented to help insure a well-ordered system in the laboratory to handle the samples, to help determine the kind of analysis required for each, to conduct the required processes, and to assist in the required computations. Use of the manual should further 'standardize' methods of fluvial sediment analysis among the many laboratories and thereby help to achieve uniformity and precision of the data.","language":"ENGLISH","publisher":"U.S. G.P.O. :For sale by Superintendent of Documents,","doi":"10.3133/twri05C1","issn":"0565-596X","usgsCitation":"Guy, H., 1969, Laboratory theory and methods for sediment analysis: U.S. Geological Survey Techniques of Water-Resources Investigations 05-C1, vi, 58 p. :ill. ;26 cm. Reprinted in 1977., https://doi.org/10.3133/twri05C1.","productDescription":"vi, 58 p. :ill. ;26 cm. Reprinted in 1977.","costCenters":[],"links":[{"id":139162,"rank":0,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/thumbnails/usgs_thumb.jpg"},{"id":246,"rank":100,"type":{"id":15,"text":"Index Page"},"url":"https://pubs.usgs.gov/twri/twri5c1/","linkFileType":{"id":5,"text":"html"}}],"noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"4f4e4828e4b07f02db4e5e1e","contributors":{"authors":[{"text":"Guy, Harold P.","contributorId":6434,"corporation":false,"usgs":true,"family":"Guy","given":"Harold P.","affiliations":[],"preferred":false,"id":149623,"contributorType":{"id":1,"text":"Authors"},"rank":1}]}} ,{"id":13757,"text":"ofr69304 - 1969 - Oil shale in the Green River Formation","interactions":[],"lastModifiedDate":"2012-02-02T00:06:42","indexId":"ofr69304","displayToPublicDate":"1994-01-01T00:00:00","publicationYear":"1969","noYear":false,"publicationType":{"id":18,"text":"Report"},"publicationSubtype":{"id":5,"text":"USGS Numbered Series"},"seriesTitle":{"id":330,"text":"Open-File Report","code":"OFR","onlineIssn":"2331-1258","printIssn":"0196-1497","active":true,"publicationSubtype":{"id":5}},"seriesNumber":"69-304","title":"Oil shale in the Green River Formation","language":"ENGLISH","publisher":"U.S. Geological Survey],","doi":"10.3133/ofr69304","usgsCitation":"Water Resources Division, U.S. Geological Survey, 1969, Oil shale in the Green River Formation: U.S. Geological Survey Open-File Report 69-304, 13 p. ill. (some folded), maps (some folded) ;29 cm., https://doi.org/10.3133/ofr69304.","productDescription":"13 p. ill. (some folded), maps (some folded) ;29 cm.","costCenters":[],"links":[{"id":145483,"rank":0,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/thumbnails/usgs_thumb.jpg"}],"noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"4f4e4af4e4b07f02db691d2c","contributors":{"authors":[{"text":"Water Resources Division, U.S. Geological Survey","contributorId":128075,"corporation":true,"usgs":false,"organization":"Water Resources Division, U.S. Geological Survey","id":528954,"contributorType":{"id":1,"text":"Authors"},"rank":1}]}} ,{"id":64040,"text":"gp656 - 1969 - Aeromagnetic map of Beach Hill and vicinity, New Hampshire and Vermont","interactions":[],"lastModifiedDate":"2025-06-20T17:30:04.673343","indexId":"gp656","displayToPublicDate":"1994-01-01T00:00:00","publicationYear":"1969","noYear":false,"publicationType":{"id":18,"text":"Report"},"publicationSubtype":{"id":5,"text":"USGS Numbered Series"},"seriesTitle":{"id":317,"text":"Geophysical Investigations Map","code":"GP","active":false,"publicationSubtype":{"id":5}},"seriesNumber":"656","title":"Aeromagnetic map of Beach Hill and vicinity, New Hampshire and Vermont","docAbstract":"No abstract available.
","language":"English","publisher":"U.S. Geological Survey","doi":"10.3133/gp656","usgsCitation":"Water Resources Division, U.S. Geological Survey, 1969, Aeromagnetic map of Beach Hill and vicinity, New Hampshire and Vermont: U.S. Geological Survey Geophysical Investigations Map 656, 1 Plate: 18.75 x 27.67 inches, https://doi.org/10.3133/gp656.","productDescription":"1 Plate: 18.75 x 27.67 inches","costCenters":[],"links":[{"id":491044,"rank":4,"type":{"id":36,"text":"NGMDB Index Page"},"url":"https://ngmdb.usgs.gov/Prodesc/proddesc_6023.htm","linkFileType":{"id":5,"text":"html"}},{"id":250478,"rank":3,"type":{"id":17,"text":"Plate"},"url":"https://pubs.usgs.gov/gp/0656/plate-1.pdf","linkFileType":{"id":1,"text":"pdf"}},{"id":253969,"rank":1,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/gp/0656/report-thumb.jpg"},{"id":250477,"rank":2,"type":{"id":11,"text":"Document"},"url":"https://pubs.usgs.gov/gp/0656/report.pdf","linkFileType":{"id":1,"text":"pdf"}}],"scale":"62500","country":"United States","state":"New Hampshire, Vermont","otherGeospatial":"Beach Hill and vicinity","geographicExtents":"{\n \"type\": \"FeatureCollection\",\n \"features\": [\n {\n \"type\": \"Feature\",\n \"properties\": {},\n \"geometry\": {\n \"type\": \"Polygon\",\n \"coordinates\": [\n [\n [\n -71.3333,\n 44.4167\n ],\n [\n -71.3333,\n 44.75\n ],\n [\n -71.5944,\n 44.75\n ],\n [\n -71.5944,\n 44.4167\n ],\n [\n -71.3333,\n 44.4167\n ]\n ]\n ]\n }\n }\n ]\n}","noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"4f4e4b00e4b07f02db698373","contributors":{"authors":[{"text":"Water Resources Division, U.S. Geological Survey","contributorId":128075,"corporation":true,"usgs":false,"organization":"Water Resources Division, U.S. Geological Survey","id":533509,"contributorType":{"id":1,"text":"Authors"},"rank":1}]}} ,{"id":3084,"text":"wsp1917 - 1969 - Surface water supply of the United States 1961-65: Part 6, Missouri River basin: Volume 2. Missouri River basin from Williston, North Dakota to Sioux City, Iowa","interactions":[],"lastModifiedDate":"2022-11-02T19:00:54.010678","indexId":"wsp1917","displayToPublicDate":"1994-01-01T00:00:00","publicationYear":"1969","noYear":false,"publicationType":{"id":18,"text":"Report"},"publicationSubtype":{"id":5,"text":"USGS Numbered Series"},"seriesTitle":{"id":341,"text":"Water Supply Paper","code":"WSP","active":false,"publicationSubtype":{"id":5}},"seriesNumber":"1917","title":"Surface water supply of the United States 1961-65: Part 6, Missouri River basin: Volume 2. Missouri River basin from Williston, North Dakota to Sioux City, Iowa","docAbstract":"No abstract available.
","language":"English","publisher":"U.S. Geological Survey","doi":"10.3133/wsp1917","usgsCitation":"Water Resources Division, U.S. Geological Survey, 1969, Surface water supply of the United States 1961-65: Part 6, Missouri River basin: Volume 2. Missouri River basin from Williston, North Dakota to Sioux City, Iowa: U.S. Geological Survey Water Supply Paper 1917, Report: viii, 560 p.; 1 Plate: 23.00 × 22.50 inches, https://doi.org/10.3133/wsp1917.","productDescription":"Report: viii, 560 p.; 1 Plate: 23.00 × 22.50 inches","costCenters":[],"links":[{"id":409071,"rank":4,"type":{"id":36,"text":"NGMDB Index Page"},"url":"https://ngmdb.usgs.gov/Prodesc/proddesc_25141.htm","linkFileType":{"id":5,"text":"html"}},{"id":29962,"rank":300,"type":{"id":11,"text":"Document"},"url":"https://pubs.usgs.gov/wsp/1917/report.pdf","linkFileType":{"id":1,"text":"pdf"}},{"id":29961,"rank":400,"type":{"id":17,"text":"Plate"},"url":"https://pubs.usgs.gov/wsp/1917/plate-1.pdf","linkFileType":{"id":1,"text":"pdf"}},{"id":138628,"rank":0,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/wsp/1917/report-thumb.jpg"}],"country":"United States","state":"Iowa, Nebraska, North Dakota, South Dakota","otherGeospatial":"Missouri River basin","geographicExtents":"{\n \"type\": \"FeatureCollection\",\n \"features\": [\n {\n \"type\": \"Feature\",\n \"properties\": {},\n \"geometry\": {\n \"coordinates\": [\n [\n [\n -103.78678268521452,\n 48.142391817720835\n ],\n [\n -103.78678268521452,\n 42.48788765617516\n ],\n [\n -96.32676997197834,\n 42.48788765617516\n ],\n [\n -96.32676997197834,\n 48.142391817720835\n ],\n [\n -103.78678268521452,\n 48.142391817720835\n ]\n ]\n ],\n \"type\": \"Polygon\"\n }\n }\n ]\n}","noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"4f4e4a4ee4b07f02db6282aa","contributors":{"authors":[{"text":"Water Resources Division, U.S. Geological Survey","contributorId":128075,"corporation":true,"usgs":false,"organization":"Water Resources Division, U.S. Geological Survey","id":528065,"contributorType":{"id":1,"text":"Authors"},"rank":1}]}} ,{"id":1690,"text":"wsp1898A - 1969 - Stage-discharge characteristics of a Weir in a sand-channel stream","interactions":[],"lastModifiedDate":"2012-02-02T00:05:14","indexId":"wsp1898A","displayToPublicDate":"1994-01-01T00:00:00","publicationYear":"1969","noYear":false,"publicationType":{"id":18,"text":"Report"},"publicationSubtype":{"id":5,"text":"USGS Numbered Series"},"seriesTitle":{"id":341,"text":"Water Supply Paper","code":"WSP","active":false,"publicationSubtype":{"id":5}},"seriesNumber":"1898","chapter":"A","title":"Stage-discharge characteristics of a Weir in a sand-channel stream","docAbstract":"A unique relation between water-surface elevation and water discharge usually does not exist for sand-channel streams. The relation is affected by changes in bed roughness and changes in bed elevation because of scour and fill. An artificial control on a sand-channel stream must control both the resistance to flow and the bed elevation in order to stabilize the relation between water-surface elevation and water discharge. \r\n\r\nThe weir (control structure) in the Rio Grande conveyance channel near Bernardo, N. Mex., was designed on the basis of a model study and field data (Harris and Richardson, 1964). About 72 percent of the measurements used to define the base relation between water-surface elevation and water discharge falls within plus or minus 5 percent of the mean relation for the prototype. The stage-discharge relation is not affected by backwater for values of submergence less than 90 percent. There is no consistent relation between the ratio of measured discharge to rated discharge and submergence for values of submergence greater than 90 percent. \r\n\r\nThe control does not restrict the channel capacity to less than the stated design capacity of 2,000 cubic feet per second. When the control is drowned out, or ineffective, the relation of water-surface elevation to water discharge is virtually the same as that prior to construction of the control for discharges greater than 1,500 cubic feet per second. When the control is not drowned out--that is, free-fall conditions exist--the water-surface elevation for a discharge of 2,000 cubic feet per second is greater than the minimum elevation, but is less than the maximum elevation that occurred at that discharge prior to construction. \r\n\r\nThe model study was only partially successful in predicting the operating characteristics of the prototype. Some of the differences between prototype operation and model predictions may exist because the prototype was not built exactly as recommended on the basis of the model study. In general, the prototype has operated somewhat better than the model predicted.","language":"ENGLISH","publisher":"U. S. Govt. Print. Off.,","doi":"10.3133/wsp1898A","usgsCitation":"Gonzalez, D.D., Scott, C., and Culbertson, J.K., 1969, Stage-discharge characteristics of a Weir in a sand-channel stream: U.S. Geological Survey Water Supply Paper 1898, iii, 29 p., https://doi.org/10.3133/wsp1898A.","productDescription":"iii, 29 p.","costCenters":[],"links":[{"id":137040,"rank":0,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/wsp/1898a/report-thumb.jpg"},{"id":26775,"rank":300,"type":{"id":11,"text":"Document"},"url":"https://pubs.usgs.gov/wsp/1898a/report.pdf","linkFileType":{"id":1,"text":"pdf"}}],"noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"4f4e478fe4b07f02db48a1b7","contributors":{"authors":[{"text":"Gonzalez, Don D.","contributorId":49774,"corporation":false,"usgs":true,"family":"Gonzalez","given":"Don","email":"","middleInitial":"D.","affiliations":[],"preferred":false,"id":143978,"contributorType":{"id":1,"text":"Authors"},"rank":1},{"text":"Scott, C.H.","contributorId":101634,"corporation":false,"usgs":true,"family":"Scott","given":"C.H.","email":"","affiliations":[],"preferred":false,"id":143979,"contributorType":{"id":1,"text":"Authors"},"rank":2},{"text":"Culbertson, James K.","contributorId":31371,"corporation":false,"usgs":true,"family":"Culbertson","given":"James","email":"","middleInitial":"K.","affiliations":[],"preferred":false,"id":143977,"contributorType":{"id":1,"text":"Authors"},"rank":3}]}} ,{"id":3208,"text":"wsp1591E - 1969 - Sediment movement in an area of suburban highway construction, Scott Run Basin, Fairfax County Virginia, 1961-64","interactions":[],"lastModifiedDate":"2012-02-02T00:05:25","indexId":"wsp1591E","displayToPublicDate":"1994-01-01T00:00:00","publicationYear":"1969","noYear":false,"publicationType":{"id":18,"text":"Report"},"publicationSubtype":{"id":5,"text":"USGS Numbered Series"},"seriesTitle":{"id":341,"text":"Water Supply Paper","code":"WSP","active":false,"publicationSubtype":{"id":5}},"seriesNumber":"1591","chapter":"E","title":"Sediment movement in an area of suburban highway construction, Scott Run Basin, Fairfax County Virginia, 1961-64","language":"ENGLISH","publisher":"U.S. Govt. Print. Off.,","doi":"10.3133/wsp1591E","usgsCitation":"Vice, R., Guy, H., and Ferguson, G., 1969, Sediment movement in an area of suburban highway construction, Scott Run Basin, Fairfax County Virginia, 1961-64: U.S. Geological Survey Water Supply Paper 1591, 1 v. (issued as seperate chapters) :ill. ;24 cm. ;41 p., https://doi.org/10.3133/wsp1591E.","productDescription":"1 v. (issued as seperate chapters) :ill. ;24 cm. ;41 p.","costCenters":[],"links":[{"id":138135,"rank":0,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/wsp/1591e/report-thumb.jpg"},{"id":30198,"rank":300,"type":{"id":11,"text":"Document"},"url":"https://pubs.usgs.gov/wsp/1591e/report.pdf","linkFileType":{"id":1,"text":"pdf"}}],"noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"4f4e4a0be4b07f02db5fc007","contributors":{"authors":[{"text":"Vice, R.B.","contributorId":58258,"corporation":false,"usgs":true,"family":"Vice","given":"R.B.","email":"","affiliations":[],"preferred":false,"id":146433,"contributorType":{"id":1,"text":"Authors"},"rank":1},{"text":"Guy, H.P.","contributorId":73571,"corporation":false,"usgs":true,"family":"Guy","given":"H.P.","email":"","affiliations":[],"preferred":false,"id":146435,"contributorType":{"id":1,"text":"Authors"},"rank":2},{"text":"Ferguson, G.E.","contributorId":62575,"corporation":false,"usgs":true,"family":"Ferguson","given":"G.E.","email":"","affiliations":[],"preferred":false,"id":146434,"contributorType":{"id":1,"text":"Authors"},"rank":3}]}} ,{"id":3085,"text":"wsp1920 - 1969 - Surface water supply of the United States, 1961-65, Part 7. Lower Mississippi River basin, Volume 1. Lower Mississippi River basin except Arkansas River basin","interactions":[],"lastModifiedDate":"2021-12-03T20:14:45.804805","indexId":"wsp1920","displayToPublicDate":"1994-01-01T00:00:00","publicationYear":"1969","noYear":false,"publicationType":{"id":18,"text":"Report"},"publicationSubtype":{"id":5,"text":"USGS Numbered Series"},"seriesTitle":{"id":341,"text":"Water Supply Paper","code":"WSP","active":false,"publicationSubtype":{"id":5}},"seriesNumber":"1920","title":"Surface water supply of the United States, 1961-65, Part 7. Lower Mississippi River basin, Volume 1. Lower Mississippi River basin except Arkansas River basin","docAbstract":"No abstract available.
","language":"English","publisher":"U.S. Geological Survey","doi":"10.3133/wsp1920","usgsCitation":"Water Resources Division, U.S. Geological Survey, 1969, Surface water supply of the United States, 1961-65, Part 7. Lower Mississippi River basin, Volume 1. Lower Mississippi River basin except Arkansas River basin: U.S. Geological Survey Water Supply Paper 1920, 1103 p., https://doi.org/10.3133/wsp1920.","productDescription":"1103 p.","costCenters":[],"links":[{"id":29963,"rank":300,"type":{"id":11,"text":"Document"},"url":"https://pubs.usgs.gov/wsp/1920/report.pdf","linkFileType":{"id":1,"text":"pdf"}},{"id":138629,"rank":0,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/wsp/1920/report-thumb.jpg"},{"id":392462,"rank":3,"type":{"id":36,"text":"NGMDB Index Page"},"url":"https://ngmdb.usgs.gov/Prodesc/proddesc_25144.htm"}],"country":"United States","state":"Arkansas, Illinois, Kansas, Kentucky, Louisiana, Mississippi, Missouri, Oklahoma, Tennessee, Texas","otherGeospatial":"lower Mississippi River basin","geographicExtents":"{\n \"type\": \"FeatureCollection\",\n \"features\": [\n {\n \"type\": \"Feature\",\n \"properties\": {},\n \"geometry\": {\n \"type\": \"Polygon\",\n \"coordinates\": [\n [\n [\n -103,\n 29\n ],\n [\n -88.293,\n 29\n ],\n [\n -88.293,\n 38.694\n ],\n [\n -103,\n 38.694\n ],\n [\n -103,\n 29\n ]\n ]\n ]\n }\n }\n ]\n}","noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"4f4e4af5e4b07f02db692938","contributors":{"authors":[{"text":"Water Resources Division, U.S. Geological Survey","contributorId":128075,"corporation":true,"usgs":false,"organization":"Water Resources Division, U.S. Geological Survey","id":528066,"contributorType":{"id":1,"text":"Authors"},"rank":1}]}} ,{"id":3478,"text":"cir601A - 1969 - Water for the cities - The outlook","interactions":[],"lastModifiedDate":"2018-04-02T10:19:55","indexId":"cir601A","displayToPublicDate":"1994-01-01T00:00:00","publicationYear":"1969","noYear":false,"publicationType":{"id":18,"text":"Report"},"publicationSubtype":{"id":5,"text":"USGS Numbered Series"},"seriesTitle":{"id":307,"text":"Circular","code":"CIR","onlineIssn":"2330-5703","printIssn":"1067-084X","active":true,"publicationSubtype":{"id":5}},"seriesNumber":"601","chapter":"A","title":"Water for the cities - The outlook","docAbstract":"Except perhaps for the arid Southwest, water resources are generally sufficient to meet the needs of cities for the foreseeable future. Cities will continue to expand and additional rural areas will be converted to urban and suburban complexes. Demands for urban water will continue to rise and this will place a heavy strain on existing systems.
\nCities have always faced water problems. This has largely been the result of 'crisis planning' or apathy. Immediate needs and minimum cost have been the governing criteria in solving water problems, as cities developed local supplies unilaterally and only at scales to meet local foreseeable demands. Most city water problems, however, have not been the result of shortages of sources of water but rather the result of overtaxed collection, storage, and distribution systems. This is verified by the experience of the Northeast during the recent prolonged drought.
\nRapid expansion of urban areas, particularly in the large metropolitan complexes of the United States, is placing urban political entities in ever closer juxtaposition to each other. The large demand for water for each entity is resulting in competition for available sources and is rapidly reaching critical proportions. Increasing awareness of the role of water in our society further complicates this competition. Pollution abatement, recreation, wildlife conservation, and aesthetics are demands now recognized by both rural and urban areas. Future development of water resources must consider regional demands and resources. Only in this way can our reasonably abundant water resources meet the severe demands imposed by our rapidly expanding urban areas.
","language":"English","publisher":"U.S. Geological Survey","publisherLocation":"Washington, D.C.","doi":"10.3133/cir601A","usgsCitation":"Schneider, W.J., and Spieker, A.M., 1969, Water for the cities - The outlook: U.S. Geological Survey Circular 601, v, 6 p., https://doi.org/10.3133/cir601A.","productDescription":"v, 6 p.","onlineOnly":"N","additionalOnlineFiles":"N","costCenters":[{"id":392,"text":"Minnesota Water Science Center","active":true,"usgs":true},{"id":478,"text":"North Dakota Water Science Center","active":true,"usgs":true},{"id":532,"text":"Pennsylvania Water Science Center","active":true,"usgs":true},{"id":34685,"text":"Dakota Water Science Center","active":true,"usgs":true}],"links":[{"id":30489,"rank":300,"type":{"id":11,"text":"Document"},"url":"https://pubs.usgs.gov/circ/1969/0601a/report.pdf","linkFileType":{"id":1,"text":"pdf"}},{"id":123019,"rank":0,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/circ/1969/0601a/report-thumb.jpg"}],"noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"4f4e49dfe4b07f02db5e3d24","contributors":{"authors":[{"text":"Schneider, William Joseph","contributorId":104466,"corporation":false,"usgs":true,"family":"Schneider","given":"William","email":"","middleInitial":"Joseph","affiliations":[],"preferred":false,"id":147000,"contributorType":{"id":1,"text":"Authors"},"rank":1},{"text":"Spieker, Andrew Maute","contributorId":78716,"corporation":false,"usgs":true,"family":"Spieker","given":"Andrew","email":"","middleInitial":"Maute","affiliations":[],"preferred":false,"id":146999,"contributorType":{"id":1,"text":"Authors"},"rank":2}]}} ,{"id":3149,"text":"wsp1967 - 1969 - Quality of surface waters for irrigation, Western states, 1965","interactions":[],"lastModifiedDate":"2012-02-02T00:05:27","indexId":"wsp1967","displayToPublicDate":"1994-01-01T00:00:00","publicationYear":"1969","noYear":false,"publicationType":{"id":18,"text":"Report"},"publicationSubtype":{"id":5,"text":"USGS Numbered Series"},"seriesTitle":{"id":341,"text":"Water Supply Paper","code":"WSP","active":false,"publicationSubtype":{"id":5}},"seriesNumber":"1967","title":"Quality of surface waters for irrigation, Western states, 1965","language":"ENGLISH","publisher":"U.S. Govt. Print. Off.,","doi":"10.3133/wsp1967","usgsCitation":"Water Resources Division, U.S. Geological Survey, 1969, Quality of surface waters for irrigation, Western states, 1965: U.S. Geological Survey Water Supply Paper 1967, viii, 148 p., https://doi.org/10.3133/wsp1967.","productDescription":"viii, 148 p.","costCenters":[],"links":[{"id":138882,"rank":0,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/wsp/1967/report-thumb.jpg"},{"id":30097,"rank":300,"type":{"id":11,"text":"Document"},"url":"https://pubs.usgs.gov/wsp/1967/report.pdf","linkFileType":{"id":1,"text":"pdf"}}],"noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"4f4e4a8ee4b07f02db6549f3","contributors":{"authors":[{"text":"Water Resources Division, U.S. Geological Survey","contributorId":128075,"corporation":true,"usgs":false,"organization":"Water Resources Division, U.S. Geological Survey","id":528107,"contributorType":{"id":1,"text":"Authors"},"rank":1}]}} ,{"id":3086,"text":"wsp1921 - 1969 - Surface water supply of the United States 1961-65: Part 7. Lower Mississippi River basin: Volume 2, Arkansas River basin","interactions":[],"lastModifiedDate":"2022-12-09T21:09:10.501404","indexId":"wsp1921","displayToPublicDate":"1994-01-01T00:00:00","publicationYear":"1969","noYear":false,"publicationType":{"id":18,"text":"Report"},"publicationSubtype":{"id":5,"text":"USGS Numbered Series"},"seriesTitle":{"id":341,"text":"Water Supply Paper","code":"WSP","active":false,"publicationSubtype":{"id":5}},"seriesNumber":"1921","title":"Surface water supply of the United States 1961-65: Part 7. Lower Mississippi River basin: Volume 2, Arkansas River basin","docAbstract":"No abstract available.
","language":"English","publisher":"U.S. Geological Survey","doi":"10.3133/wsp1921","usgsCitation":"Water Resources Division, U.S. Geological Survey, 1969, Surface water supply of the United States 1961-65: Part 7. Lower Mississippi River basin: Volume 2, Arkansas River basin: U.S. Geological Survey Water Supply Paper 1921, 878 p., https://doi.org/10.3133/wsp1921.","productDescription":"878 p.","costCenters":[],"links":[{"id":29964,"rank":1,"type":{"id":11,"text":"Document"},"url":"https://pubs.usgs.gov/wsp/1921/report.pdf","linkFileType":{"id":1,"text":"pdf"}},{"id":410234,"rank":3,"type":{"id":36,"text":"NGMDB Index Page"},"url":"https://ngmdb.usgs.gov/Prodesc/proddesc_25145.htm","linkFileType":{"id":5,"text":"html"}},{"id":138630,"rank":0,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/wsp/1921/report-thumb.jpg"}],"country":"United States","otherGeospatial":"Arkansas River basin","geographicExtents":"{\n \"type\": \"FeatureCollection\",\n \"features\": [\n {\n \"type\": \"Feature\",\n \"properties\": {},\n \"geometry\": {\n \"coordinates\": [\n [\n [\n -106.6,\n 39.367\n ],\n [\n -106.6,\n 34\n ],\n [\n -91.35,\n 34\n ],\n [\n -91.35,\n 39.367\n ],\n [\n -106.6,\n 39.367\n ]\n ]\n ],\n \"type\": \"Polygon\"\n }\n }\n ]\n}","noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"4f4e4b00e4b07f02db6980a3","contributors":{"authors":[{"text":"Water Resources Division, U.S. Geological Survey","contributorId":128075,"corporation":true,"usgs":false,"organization":"Water Resources Division, U.S. Geological Survey","id":528067,"contributorType":{"id":1,"text":"Authors"},"rank":1}]}} ,{"id":63818,"text":"gp645 - 1969 - Aeromagnetic map of the Tariffville quadrangle and parts of the Avon and Southwick quadrangles, Connecticut and Massachusetts","interactions":[],"lastModifiedDate":"2025-06-18T20:22:59.518066","indexId":"gp645","displayToPublicDate":"1994-01-01T00:00:00","publicationYear":"1969","noYear":false,"publicationType":{"id":18,"text":"Report"},"publicationSubtype":{"id":5,"text":"USGS Numbered Series"},"seriesTitle":{"id":317,"text":"Geophysical Investigations Map","code":"GP","active":false,"publicationSubtype":{"id":5}},"seriesNumber":"645","title":"Aeromagnetic map of the Tariffville quadrangle and parts of the Avon and Southwick quadrangles, Connecticut and Massachusetts","docAbstract":"No abstract available.
","language":"English","publisher":"U.S. Geological Survey","doi":"10.3133/gp645","usgsCitation":"Water Resources Division, U.S. Geological Survey, 1969, Aeromagnetic map of the Tariffville quadrangle and parts of the Avon and Southwick quadrangles, Connecticut and Massachusetts: U.S. Geological Survey Geophysical Investigations Map 645, 1 Plate: 21.23 x 33.95 inches, https://doi.org/10.3133/gp645.","productDescription":"1 Plate: 21.23 x 33.95 inches","costCenters":[],"links":[{"id":490949,"rank":4,"type":{"id":36,"text":"NGMDB Index Page"},"url":"https://ngmdb.usgs.gov/Prodesc/proddesc_6012.htm","linkFileType":{"id":5,"text":"html"}},{"id":253592,"rank":1,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/gp/0645/report-thumb.jpg"},{"id":250053,"rank":3,"type":{"id":17,"text":"Plate"},"url":"https://pubs.usgs.gov/gp/0645/plate-1.pdf","linkFileType":{"id":1,"text":"pdf"}},{"id":250052,"rank":2,"type":{"id":11,"text":"Document"},"url":"https://pubs.usgs.gov/gp/0645/report.pdf","linkFileType":{"id":1,"text":"pdf"}}],"scale":"24000","country":"United States","state":"Connecticut, Massachusetts","otherGeospatial":"Tariffville quadrangle and parts of the Avon and Southwick quadrangles","geographicExtents":"{\n \"type\": \"FeatureCollection\",\n \"features\": [\n {\n \"type\": \"Feature\",\n \"properties\": {},\n \"geometry\": {\n \"coordinates\": [\n [\n [\n -72.875,\n 42\n ],\n [\n -72.875,\n 41.875\n ],\n [\n -72.75,\n 41.875\n ],\n [\n -72.75,\n 42\n ],\n [\n -72.875,\n 42\n ]\n ]\n ],\n \"type\": \"Polygon\"\n }\n }\n ]\n}","noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"4f4e4aeee4b07f02db691108","contributors":{"authors":[{"text":"Water Resources Division, U.S. Geological Survey","contributorId":128075,"corporation":true,"usgs":false,"organization":"Water Resources Division, U.S. Geological Survey","id":533287,"contributorType":{"id":1,"text":"Authors"},"rank":1}]}} ,{"id":63895,"text":"gp684 - 1969 - Aeromagnetic map of the McGregor Lake-Tally Lake area, Flathead and Lincoln Counties, Montana","interactions":[],"lastModifiedDate":"2025-06-23T16:46:37.443541","indexId":"gp684","displayToPublicDate":"1994-01-01T00:00:00","publicationYear":"1969","noYear":false,"publicationType":{"id":18,"text":"Report"},"publicationSubtype":{"id":5,"text":"USGS Numbered Series"},"seriesTitle":{"id":317,"text":"Geophysical Investigations Map","code":"GP","active":false,"publicationSubtype":{"id":5}},"seriesNumber":"684","title":"Aeromagnetic map of the McGregor Lake-Tally Lake area, Flathead and Lincoln Counties, Montana","docAbstract":"No abstract available.
","language":"English","publisher":"U.S. Geological Survey","doi":"10.3133/gp684","usgsCitation":"Water Resources Division, U.S. Geological Survey, 1969, Aeromagnetic map of the McGregor Lake-Tally Lake area, Flathead and Lincoln Counties, Montana: U.S. Geological Survey Geophysical Investigations Map 684, 1 Plate: 29.61 x 38.73 inches, https://doi.org/10.3133/gp684.","productDescription":"1 Plate: 29.61 x 38.73 inches","costCenters":[],"links":[{"id":491112,"rank":4,"type":{"id":36,"text":"NGMDB Index Page"},"url":"https://ngmdb.usgs.gov/Prodesc/proddesc_6050.htm","linkFileType":{"id":5,"text":"html"}},{"id":253664,"rank":1,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/gp/0684/report-thumb.jpg"},{"id":250197,"rank":3,"type":{"id":17,"text":"Plate"},"url":"https://pubs.usgs.gov/gp/0684/plate-1.pdf","linkFileType":{"id":1,"text":"pdf"}},{"id":250196,"rank":2,"type":{"id":11,"text":"Document"},"url":"https://pubs.usgs.gov/gp/0684/report.pdf","linkFileType":{"id":1,"text":"pdf"}}],"scale":"62500","country":"United States","state":"Montana","county":"Flathead County, Lincoln County","otherGeospatial":"McGregor Lake-Tally Lake area","geographicExtents":"{\n \"type\": \"FeatureCollection\",\n \"features\": [\n {\n \"type\": \"Feature\",\n \"properties\": {},\n \"geometry\": {\n \"type\": \"Polygon\",\n \"coordinates\": [\n [\n [\n -115,\n 48.5\n ],\n [\n -115,\n 48\n ],\n [\n -114.425,\n 48\n ],\n [\n -114.425,\n 48.5\n ],\n [\n -115,\n 48.5\n ]\n ]\n ]\n }\n }\n ]\n}","noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"4f4e4af4e4b07f02db691e19","contributors":{"authors":[{"text":"Water Resources Division, U.S. Geological Survey","contributorId":128075,"corporation":true,"usgs":false,"organization":"Water Resources Division, U.S. Geological Survey","id":533364,"contributorType":{"id":1,"text":"Authors"},"rank":1}]}} ,{"id":63886,"text":"gp679 - 1969 - Aeromagnetic map of the Nantasket quadrangle, Suffolk, Norfolk, and Plymouth Counties, Massachusetts","interactions":[],"lastModifiedDate":"2025-06-23T16:24:36.436401","indexId":"gp679","displayToPublicDate":"1994-01-01T00:00:00","publicationYear":"1969","noYear":false,"publicationType":{"id":18,"text":"Report"},"publicationSubtype":{"id":5,"text":"USGS Numbered Series"},"seriesTitle":{"id":317,"text":"Geophysical Investigations Map","code":"GP","active":false,"publicationSubtype":{"id":5}},"seriesNumber":"679","title":"Aeromagnetic map of the Nantasket quadrangle, Suffolk, Norfolk, and Plymouth Counties, Massachusetts","docAbstract":"No abstract available.
","language":"English","publisher":"U.S. Geological Survey","doi":"10.3133/gp679","usgsCitation":"Water Resources Division, U.S. Geological Survey, 1969, Aeromagnetic map of the Nantasket quadrangle, Suffolk, Norfolk, and Plymouth Counties, Massachusetts: U.S. Geological Survey Geophysical Investigations Map 679, 1 Plate: 20.78 x 31.44 inches, https://doi.org/10.3133/gp679.","productDescription":"1 Plate: 20.78 x 31.44 inches","costCenters":[],"links":[{"id":491108,"rank":4,"type":{"id":36,"text":"NGMDB Index Page"},"url":"https://ngmdb.usgs.gov/Prodesc/proddesc_6046.htm","linkFileType":{"id":5,"text":"html"}},{"id":253655,"rank":1,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/gp/0679/report-thumb.jpg"},{"id":250179,"rank":3,"type":{"id":17,"text":"Plate"},"url":"https://pubs.usgs.gov/gp/0679/plate-1.pdf","linkFileType":{"id":1,"text":"pdf"}},{"id":250178,"rank":2,"type":{"id":11,"text":"Document"},"url":"https://pubs.usgs.gov/gp/0679/report.pdf","linkFileType":{"id":1,"text":"pdf"}}],"scale":"24000","country":"United States","state":"Massachusetts","county":"Norfolk County, Plymouth County, Suffolk County","otherGeospatial":"Nantasket quadrangle","geographicExtents":"{\n \"type\": \"FeatureCollection\",\n \"features\": [\n {\n \"type\": \"Feature\",\n \"properties\": {},\n \"geometry\": {\n \"type\": \"Polygon\",\n \"coordinates\": [\n [\n [\n -70.75,\n 42.25\n ],\n [\n -70.75,\n 42.375\n ],\n [\n -70.875,\n 42.375\n ],\n [\n -70.875,\n 42.25\n ],\n [\n -70.75,\n 42.25\n ]\n ]\n ]\n }\n }\n ]\n}","noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"4f4e4af4e4b07f02db691d14","contributors":{"authors":[{"text":"Water Resources Division, U.S. Geological Survey","contributorId":128075,"corporation":true,"usgs":false,"organization":"Water Resources Division, U.S. Geological Survey","id":533355,"contributorType":{"id":1,"text":"Authors"},"rank":1}]}} ,{"id":63980,"text":"gp663 - 1969 - Aeromagnetic map of the Belchertown quadrangle, Hampshire County, Massachusetts","interactions":[],"lastModifiedDate":"2012-02-10T00:10:54","indexId":"gp663","displayToPublicDate":"1994-01-01T00:00:00","publicationYear":"1969","noYear":false,"publicationType":{"id":18,"text":"Report"},"publicationSubtype":{"id":5,"text":"USGS Numbered Series"},"seriesTitle":{"id":317,"text":"Geophysical Investigations Map","code":"GP","active":false,"publicationSubtype":{"id":5}},"seriesNumber":"663","title":"Aeromagnetic map of the Belchertown quadrangle, Hampshire County, Massachusetts","language":"ENGLISH","doi":"10.3133/gp663","usgsCitation":"Water Resources Division, U.S. Geological Survey, 1969, Aeromagnetic map of the Belchertown quadrangle, Hampshire County, Massachusetts: U.S. Geological Survey Geophysical Investigations Map 663, 1 map., https://doi.org/10.3133/gp663.","productDescription":"1 map.","costCenters":[],"links":[{"id":250360,"rank":300,"type":{"id":11,"text":"Document"},"url":"https://pubs.usgs.gov/gp/0663/report.pdf","size":"27","linkFileType":{"id":1,"text":"pdf"}},{"id":250361,"rank":400,"type":{"id":17,"text":"Plate"},"url":"https://pubs.usgs.gov/gp/0663/plate-1.pdf","size":"2750","linkFileType":{"id":1,"text":"pdf"}},{"id":253828,"rank":0,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/gp/0663/report-thumb.jpg"}],"scale":"24000","geographicExtents":"{ \"type\": \"FeatureCollection\", \"features\": [ { \"type\": \"Feature\", \"properties\": {}, \"geometry\": { \"type\": \"Polygon\", \"coordinates\": [ [ [ -72.5,42.25 ], [ -72.5,42.3675 ], [ -72.36749999999999,42.3675 ], [ -72.36749999999999,42.25 ], [ -72.5,42.25 ] ] ] } } ] }","noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"4f4e4afee4b07f02db697248","contributors":{"authors":[{"text":"Water Resources Division, U.S. Geological Survey","contributorId":128075,"corporation":true,"usgs":false,"organization":"Water Resources Division, U.S. Geological Survey","id":533449,"contributorType":{"id":1,"text":"Authors"},"rank":1}]}} ,{"id":42051,"text":"ofr69290 - 1969 - Aeromagnetic map of Gladstone and vicinity, Delta, Alger, Menominee, and Marquette Counties, Michigan.","interactions":[],"lastModifiedDate":"2012-02-02T00:05:06","indexId":"ofr69290","displayToPublicDate":"1994-01-01T00:00:00","publicationYear":"1969","noYear":false,"publicationType":{"id":18,"text":"Report"},"publicationSubtype":{"id":5,"text":"USGS Numbered Series"},"seriesTitle":{"id":330,"text":"Open-File Report","code":"OFR","onlineIssn":"2331-1258","printIssn":"0196-1497","active":true,"publicationSubtype":{"id":5}},"seriesNumber":"69-290","title":"Aeromagnetic map of Gladstone and vicinity, Delta, Alger, Menominee, and Marquette Counties, Michigan.","language":"ENGLISH","doi":"10.3133/ofr69290","usgsCitation":"Water Resources Division, U.S. Geological Survey, 1969, Aeromagnetic map of Gladstone and vicinity, Delta, Alger, Menominee, and Marquette Counties, Michigan.: U.S. Geological Survey Open-File Report 69-290, 4 maps, https://doi.org/10.3133/ofr69290.","productDescription":"4 maps","costCenters":[],"links":[{"id":136740,"rank":0,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/thumbnails/usgs_thumb.jpg"},{"id":98780,"rank":400,"type":{"id":17,"text":"Plate"},"url":"https://pubs.usgs.gov/of/1969/0290/plate-1.pdf","size":"9267","linkFileType":{"id":1,"text":"pdf"}},{"id":98781,"rank":401,"type":{"id":17,"text":"Plate"},"url":"https://pubs.usgs.gov/of/1969/0290/plate-2.pdf","size":"6286","linkFileType":{"id":1,"text":"pdf"}},{"id":98782,"rank":402,"type":{"id":17,"text":"Plate"},"url":"https://pubs.usgs.gov/of/1969/0290/plate-3.pdf","size":"10402","linkFileType":{"id":1,"text":"pdf"}},{"id":98783,"rank":403,"type":{"id":17,"text":"Plate"},"url":"https://pubs.usgs.gov/of/1969/0290/plate-4.pdf","size":"8397","linkFileType":{"id":1,"text":"pdf"}}],"scale":"62500","noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"4f4e4af4e4b07f02db69218f","contributors":{"authors":[{"text":"Water Resources Division, U.S. Geological Survey","contributorId":128075,"corporation":true,"usgs":false,"organization":"Water Resources Division, U.S. Geological Survey","id":530800,"contributorType":{"id":1,"text":"Authors"},"rank":1}]}} ,{"id":68642,"text":"ha360 - 1969 - Water resources of Wisconsin: Rock-Fox River basin","interactions":[],"lastModifiedDate":"2024-02-28T23:08:39.564696","indexId":"ha360","displayToPublicDate":"1994-01-01T00:00:00","publicationYear":"1969","noYear":false,"publicationType":{"id":18,"text":"Report"},"publicationSubtype":{"id":5,"text":"USGS Numbered Series"},"seriesTitle":{"id":318,"text":"Hydrologic Atlas","code":"HA","active":false,"publicationSubtype":{"id":5}},"seriesNumber":"360","title":"Water resources of Wisconsin: Rock-Fox River basin","docAbstract":"PURPOSE AND SCOPE
\nThe purpose of this report is to describe the physical environment, availability, distribution, characteristics, movement, quality, water problems, and use of water within the Rock-Fox River basin in order to aid in planning future water management within the basin.
\nThis report presents general information on the basin that was derived from data obtained from Federal, State, and local agencies. In addition, new data were collected from areas where available data were scarce. The reader is referred to the section entitled “Agencies Having Additional Information” and to the list of selected references (sheet 4) for sources of more detailed information.
\nThis atlas is one of a series of 12 river-basin studies designed to describe in general terms the water resources of the State. More detailed studies of problem areas will be required in the future as the need for additional information increases.
\nLOCATION AND EXTENT
\nThe Rock-Fox River basin in Wisconsin, covers about 4,750 square miles in the southeastern part of the State. It includes all or parts of the following 13 counties: Columbia, Dane, Dodge, Fond du Lac, Green Lake, Jefferson, Kenosha, Milwaukee, Racine, Rock, Walworth, Washington, and Waukesha. It includes the area drained by the Rock, Fox, and Des Plaines Rivers within the State of Wisconsin.
\nAlthough the basin boundary is the topographic divide, part of the streamflow is derived from ground water that drains from an area similar to, but not having the same boundaries as, the topographic basin. The ground-water basin covers about 4,350 square miles, 400 square miles less than the topographic basin. Most of the reduction in basin area is along the eastern side of the basin.
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No abstract available.
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