The Cenomanian-Turonian formations of central Israel constitute a highly permeable dolomite and limestone aquifer. In this area it is on the west limb of an anticlinorium that trends north-northeast, and it contains water under artesian pressure. A graph of water temperatures and well depths suggests that there is a very small vertical temperature gradient in local segments of the aquifer. The small gradient is believed to result from a large vertical component of flow that tends to equalize the vertical temperature distribution. On a regional scale the apparent horizontal temperature distribution indicates a westward increase with increasing depth of the aquifer, suggesting a manifestation of the regional geothermal gradient. The westward increase in temperature also implies that the lateral component of flow may be in the normal range for artesian carbonate-rock aquifers whose pores consist mainly of solution cavities. Locally, pumping appears to have affected the temperature distribution by modifying the natural flow pattern. In parts of the most intensively developed area, the aquifer is hydraulically connected with overlying coastal-plain deposits, and some cooler water has been induced to move into the aquifer from this source. At three other areas, pumping has resulted in an apparent horizontal shift of the isotherms on a temperature-distribution map. The data suggest that the spatial distribution of temperature may be used to determine some of the flow characteristics of carbonate-rock aquifers.
","language":"English","publisher":"Geological Society of America","doi":"10.1130/0016-7606(1964)75[209:ROTDTG]2.0.CO;2","usgsCitation":"Schneider, R., 1964, Relation of temperature distribution to ground-water movement in carbonate rocks of central Israel: Geological Society of America Bulletin, v. 75, no. 3, p. 209-216, https://doi.org/10.1130/0016-7606(1964)75[209:ROTDTG]2.0.CO;2.","productDescription":"8 p.","startPage":"209","endPage":"216","costCenters":[],"links":[{"id":386224,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/thumbnails/outside_thumb.jpg"}],"country":"Israel","geographicExtents":"{\n \"type\": \"FeatureCollection\",\n \"features\": [\n {\n \"type\": \"Feature\",\n \"properties\": {},\n \"geometry\": {\n \"type\": \"Polygon\",\n \"coordinates\": [\n [\n [\n 35.57373046875,\n 33.284619968887675\n ],\n [\n 35.430908203125,\n 33.100745405144245\n ],\n [\n 35.13427734375,\n 33.100745405144245\n ],\n [\n 34.1455078125,\n 31.372399104880525\n ],\n [\n 34.9365234375,\n 29.458731185355344\n ],\n [\n 35.595703125,\n 32.13840869677249\n ],\n [\n 35.57373046875,\n 33.284619968887675\n ]\n ]\n ]\n }\n }\n ]\n}","volume":"75","issue":"3","noUsgsAuthors":false,"publicationStatus":"PW","contributors":{"authors":[{"text":"Schneider, Robert","contributorId":102460,"corporation":false,"usgs":true,"family":"Schneider","given":"Robert","email":"","affiliations":[],"preferred":false,"id":817001,"contributorType":{"id":1,"text":"Authors"},"rank":1}]}} ,{"id":70010471,"text":"70010471 - 1964 - Tritium-hydrologic research: Some results of the U.S. Geological Survey Research Program","interactions":[],"lastModifiedDate":"2026-02-13T16:21:12.862036","indexId":"70010471","displayToPublicDate":"1964-02-02T00:00:00","publicationYear":"1964","noYear":false,"publicationType":{"id":2,"text":"Article"},"publicationSubtype":{"id":10,"text":"Journal Article"},"seriesTitle":{"id":3338,"text":"Science","active":true,"publicationSubtype":{"id":10}},"title":"Tritium-hydrologic research: Some results of the U.S. Geological Survey Research Program","docAbstract":"In general tritium is of limited usefulness as a tool in hydrologic studies because the tritium content of ground water, as a result of radioactive decay, becomes too low to be detectable after about 50 years. Nevertheless, a unique study was made of the hydrologic cycle of small stream basins in Wisconsin and New Jersey on the basis of measurements relative to the peak of tritium fallout in the spring of 1958. The continental and the coastal basins received approximately the same tritium fallout. Approximately 30 percent went into ground-water storage, the remainder being exported as runoff and evapotranspiration. The mean residence time for ground-water recharge for the two basins was 45 and 30 days, respectively.","language":"English","publisher":"American Association for the Advancement of Science.","doi":"10.1126/science.143.3608.804","issn":"00368075","usgsCitation":"Carlston, C., 1964, Tritium-hydrologic research: Some results of the U.S. Geological Survey Research Program: Science, v. 143, no. 3608, p. 804-806, https://doi.org/10.1126/science.143.3608.804.","productDescription":"3 p.","startPage":"804","endPage":"806","costCenters":[],"links":[{"id":219076,"rank":1,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/thumbnails/outside_thumb.jpg"}],"country":"United States","state":"New Jersey, Wisconsin","geographicExtents":"{\n \"type\": \"FeatureCollection\",\n \"features\": [\n {\n \"type\": \"Feature\",\n \"properties\": {},\n \"geometry\": {\n \"coordinates\": [\n [\n [\n -92.65443024683039,\n 47.18686471532902\n ],\n [\n -92.92337344008368,\n 44.76948314682184\n ],\n [\n -91.54422384565291,\n 43.91380985726313\n ],\n [\n -90.40331265602809,\n 42.36186629934298\n ],\n [\n -87.66640475516137,\n 42.473317234890345\n ],\n [\n -86.69378362897187,\n 45.09478563580936\n ],\n [\n -87.76789223463291,\n 45.99366780802788\n ],\n [\n -89.9402097973789,\n 46.41028342019218\n ],\n [\n -89.94150082434655,\n 47.33914537549116\n ],\n [\n -92.65443024683039,\n 47.18686471532902\n ]\n ]\n ],\n \"type\": \"Polygon\"\n }\n },\n {\n \"type\": \"Feature\",\n \"properties\": {},\n \"geometry\": {\n \"coordinates\": [\n [\n [\n -75.03044920156037,\n 41.368918438639554\n ],\n [\n -75.21217801383332,\n 40.6314679025723\n ],\n [\n -74.81474599562263,\n 40.24767874671271\n ],\n [\n -75.6121640073091,\n 39.468177148463866\n ],\n [\n -74.80122580215662,\n 38.82749379603797\n ],\n [\n -74.0060957836949,\n 40.04453424272181\n ],\n [\n -73.96363933005574,\n 41.368918438639554\n ],\n [\n -75.03044920156037,\n 41.368918438639554\n ]\n ]\n ],\n \"type\": \"Polygon\"\n }\n }\n ]\n}","volume":"143","issue":"3608","noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"505bb875e4b08c986b327884","contributors":{"authors":[{"text":"Carlston, C.W.","contributorId":26062,"corporation":false,"usgs":true,"family":"Carlston","given":"C.W.","affiliations":[],"preferred":false,"id":358994,"contributorType":{"id":1,"text":"Authors"},"rank":1}]}} ,{"id":1479,"text":"1479 - 1964 - Letters received by the United States Geological Survey, 1879-1901","interactions":[],"lastModifiedDate":"2014-07-11T16:49:40","indexId":"1479","displayToPublicDate":"1964-01-01T16:48:00","publicationYear":"1964","noYear":false,"publicationType":{"id":18,"text":"Report"},"publicationSubtype":{"id":6,"text":"USGS Unnumbered Series"},"title":"Letters received by the United States Geological Survey, 1879-1901","docAbstract":"No abstract available.","largerWorkType":{"id":18,"text":"Report"},"largerWorkTitle":"National Archives microfilm publications","largerWorkSubtype":{"id":6,"text":"USGS Unnumbered Series"},"language":"English","publisher":"National Archives and Records Service","publisherLocation":"Washington, D.C.","doi":"10.3133/1479","usgsCitation":"Water Resources Division, U.S. Geological Survey, 1964, Letters received by the United States Geological Survey, 1879-1901, 118 microfilm reels, https://doi.org/10.3133/1479.","productDescription":"118 microfilm reels","temporalStart":"1878-12-31","temporalEnd":"1901-12-31","costCenters":[],"links":[{"id":289830,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/thumbnails/usgs_thumb.jpg"}],"noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"53c0ec80e4b065ccca5fe427","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":527855,"contributorType":{"id":1,"text":"Authors"},"rank":1}]}} ,{"id":878,"text":"878 - 1964 - Water resources data for Virginia","interactions":[],"lastModifiedDate":"2014-08-05T16:13:40","indexId":"878","displayToPublicDate":"1964-01-01T16:12:07","publicationYear":"1964","noYear":false,"publicationType":{"id":18,"text":"Report"},"publicationSubtype":{"id":6,"text":"USGS Unnumbered Series"},"title":"Water resources data for Virginia","docAbstract":"No abstract available.","language":"English","publisher":"Water Resources Division, U.S. Geological Survey","publisherLocation":"Richmond, VA","doi":"10.3133/878","issn":"0276-1319","collaboration":"Prepared in cooperation with the State of Virginia and other agencies.","usgsCitation":"Water Resources Division, U.S. Geological Survey, 1964, Water resources data for Virginia, https://doi.org/10.3133/878.","costCenters":[],"links":[{"id":291736,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/thumbnails/usgs_thumb.jpg"}],"country":"United States","state":"Virginia","geographicExtents":"{ \"type\": \"FeatureCollection\", \"features\": [ { \"type\": \"Feature\", \"properties\": {}, \"geometry\": { \"type\": \"Polygon\", \"coordinates\": [ [ [ -83.6754,36.5408 ], [ -83.6754,39.466 ], [ -75.2422,39.466 ], [ -75.2422,36.5408 ], [ -83.6754,36.5408 ] ] ] } } ] }","noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"53e1eff2e4b0fe532be2df6c","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":527797,"contributorType":{"id":1,"text":"Authors"},"rank":1}]}} ,{"id":836,"text":"836 - 1964 - Water resources data for Arizona","interactions":[],"lastModifiedDate":"2014-08-05T15:21:02","indexId":"836","displayToPublicDate":"1964-01-01T15:19:53","publicationYear":"1964","noYear":false,"publicationType":{"id":18,"text":"Report"},"publicationSubtype":{"id":6,"text":"USGS Unnumbered Series"},"title":"Water resources data for Arizona","docAbstract":"No abstract available.","language":"English","publisher":"U.S. Geological Survey","publisherLocation":"Tucson, AZ","doi":"10.3133/836","collaboration":"Prepared in cooperation with the State of Arizona and other agencies.","usgsCitation":"Water Resources Division, U.S. Geological Survey, 1964, Water resources data for Arizona, https://doi.org/10.3133/836.","costCenters":[],"links":[{"id":291729,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/thumbnails/usgs_thumb.jpg"}],"country":"United States","state":"Arizona","geographicExtents":"{ \"type\": \"FeatureCollection\", \"features\": [ { \"type\": \"Feature\", \"properties\": {}, \"geometry\": { \"type\": \"Polygon\", \"coordinates\": [ [ [ -114.82,31.33 ], [ -114.82,37.0 ], [ -109.05,37.0 ], [ -109.05,31.33 ], [ -114.82,31.33 ] ] ] } } ] }","noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"53e1efe1e4b0fe532be2dea9","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":527755,"contributorType":{"id":1,"text":"Authors"},"rank":1}]}} ,{"id":70095523,"text":"70095523 - 1964 - Sedimentology: general introduction and definitions : fluvial sediment and channel morphology","interactions":[],"lastModifiedDate":"2014-03-25T10:35:32","indexId":"70095523","displayToPublicDate":"1964-01-01T13:52:00","publicationYear":"1964","noYear":false,"publicationType":{"id":18,"text":"Report"},"publicationSubtype":{"id":6,"text":"USGS Unnumbered Series"},"seriesTitle":{"id":375,"text":"Open-File Report","active":false,"publicationSubtype":{"id":6}},"title":"Sedimentology: general introduction and definitions : fluvial sediment and channel morphology","docAbstract":"Sedimentology, the study of sedimentary rocks and the \nprocesses by which they are formed, includes and is related \nto a large number of phenomena. Sedimentology includes the \nfive fundamental processes defined by the term sediaentation \n--weathering, erosion, transportation, deposition and \ndiagenesis. \nSedimentology shares with geomorphology the study of \nthe surface features of the earth. Sedimentology also \nshares with hydrology the study of river.--channels. River \nchannels are formed in part or in total as a result of \nflowing water and sediment transport, commonly called the \n\"work of the rivers.\" \nThis survey of published literature was made to aid in \narriving at definitions which would be acceptable to, and \nrepresentative of, a majority of professional personnel \nactively engaged in laboratory and field investigations \nrelated to the \"work of the river.\" The definitions in this \nlist are intended to explain the terms used in studies of \nfluvial sediment and channel morphology. No set of \ndefinitions can expect universal acceptance, however, i t is \nhoped that this compilation will be considered a summary \nand synthesis of present and past usage and that it will \nserve as a starting point for future usage. \nMultiple references are cited from textbooks, glossaries and dictionaries, scientific journals and u.s. Government \npublications. To obtain a mutual understanding and enhance \nprecision, many of the proposed definitions are a composite \nof those selected from papers or reports covering research \nstudies and field investigations. \n\nA draft of this glossary has been reviewed by a group of \ninterested personnel. The results of this review have been \ncarefully considered and the originally-suggested definitions \nhave been revised accordingly, resulting in the present \ncompilation. \nR. G. Wolff, with the help of Mrs. v. Blatcher, carried \nout the literature search and compilation of terms and the \nreview results. Paul c. Benedict approved or composed the \ndefinitions as presented in this report.","language":"English","publisher":"U.S. Geological Survey, Water Resources Division","publisherLocation":"Washington, DC","doi":"10.3133/70095523","usgsCitation":"Wolff, R.G., and Benedict, P., 1964, Sedimentology: general introduction and definitions : fluvial sediment and channel morphology: Open-File Report, iii, 132 p., https://doi.org/10.3133/70095523.","productDescription":"iii, 132 p.","additionalOnlineFiles":"N","costCenters":[],"links":[{"id":283310,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/thumbnails/70095523.jpg"},{"id":284835,"type":{"id":11,"text":"Document"},"url":"https://pubs.usgs.gov/unnumbered/70095523/report.pdf"}],"noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"5355955fe4b0120853e8c1d4","contributors":{"authors":[{"text":"Wolff, Roger G.","contributorId":19580,"corporation":false,"usgs":true,"family":"Wolff","given":"Roger","email":"","middleInitial":"G.","affiliations":[],"preferred":false,"id":491227,"contributorType":{"id":1,"text":"Authors"},"rank":1},{"text":"Benedict, Paul C.","contributorId":72293,"corporation":false,"usgs":true,"family":"Benedict","given":"Paul C.","affiliations":[],"preferred":false,"id":491228,"contributorType":{"id":1,"text":"Authors"},"rank":2}]}} ,{"id":70221132,"text":"70221132 - 1964 - Hydrologic factors pertinent to ground‐water contamination","interactions":[],"lastModifiedDate":"2021-06-04T12:04:08.414151","indexId":"70221132","displayToPublicDate":"1964-01-01T13:47:53","publicationYear":"1964","noYear":false,"publicationType":{"id":2,"text":"Article"},"publicationSubtype":{"id":10,"text":"Journal Article"},"seriesTitle":{"id":3825,"text":"Groundwater","active":true,"publicationSubtype":{"id":10}},"title":"Hydrologic factors pertinent to ground‐water contamination","docAbstract":"Predictions of where and how a fluid waste may travel from disposal site to the water table require detailed information on the physical characteristics, location, and extent of all pervious and impervious materials in the unsaturated zone. Principles concerning the flow system in the unsaturated zone indicate the importance of choice of disposal technique in predicting the time required for the fluid waste to traverse the distance to the water table. With appropriate data on the location, extent, and physical properties of water‐bearing materials and on the boundaries of the saturated zone flow system, it is possible to analyze the relative merits of a variety of waste disposal techniques and to describe the probable consequences of each. Environments of consolidated rocks, such as granites, sandstones, and limestones, pose problems in addition to those related to unconsolidated or granular porous media in defining the fluid‐flow regimes that involve joint patterns, fracture patterns, solutional openings, and the rock structure. The consequences of ground‐water contamination can be just as damaging to water users as the pollution of surface streams. In fact it can be argued that the consequences are far more damaging because they persist over much longer periods of time after the contaminating source has been eliminated. It would appear prudent, therefore, to guard against contamination of the ground‐water resource in the first instance, rather than to engage in long expensive rehabilitation measures after the damage has been done. In 1960 Graham Walton presented data concerning contamination, by sewage or other man‐made wastes, of surface and underground waters. The circumstances attending the reported incidents of contamination, especially those involving ground‐water supplies, have aided materially in the choice of a few principles and ideas that will identify the role of some significant hydrologic factors in the underground movement of fluid wastes. Walton's discussion of ground‐water contamination refers often to physical settings into which fluid wastes are discharged at or near the land surface into cesspools, tile‐drain fields, and holding ponds. Furthermore, most reported instances of ground‐water contamination have taken place in relatively humid.
","language":"English","publisher":"NGWA The Groundwater Association","doi":"10.1111/j.1745-6584.1964.tb01739.x","usgsCitation":"Brown, R., 1964, Hydrologic factors pertinent to ground‐water contamination: Groundwater, v. 2, no. 1, p. 5-12, https://doi.org/10.1111/j.1745-6584.1964.tb01739.x.","productDescription":"8 p.","startPage":"5","endPage":"12","costCenters":[],"links":[{"id":386191,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/thumbnails/outside_thumb.jpg"}],"volume":"2","issue":"1","noUsgsAuthors":false,"publicationDate":"2006-07-06","publicationStatus":"PW","contributors":{"authors":[{"text":"Brown, R.","contributorId":101419,"corporation":false,"usgs":true,"family":"Brown","given":"R.","affiliations":[],"preferred":false,"id":816940,"contributorType":{"id":1,"text":"Authors"},"rank":1}]}} ,{"id":70221133,"text":"70221133 - 1964 - Hydrologic factors pertinent to ground‐water contamination","interactions":[],"lastModifiedDate":"2021-06-02T18:50:54.556763","indexId":"70221133","displayToPublicDate":"1964-01-01T13:47:53","publicationYear":"1964","noYear":false,"publicationType":{"id":2,"text":"Article"},"publicationSubtype":{"id":10,"text":"Journal Article"},"seriesTitle":{"id":3825,"text":"Groundwater","active":true,"publicationSubtype":{"id":10}},"title":"Hydrologic factors pertinent to ground‐water contamination","docAbstract":"Predictions of where and how a fluid waste may travel from disposal site to the water table require detailed information on the physical characteristics, location, and extent of all pervious and impervious materials in the unsaturated zone. Principles concerning the flow system in the unsaturated zone indicate the importance of choice of disposal technique in predicting the time required for the fluid waste to traverse the distance to the water table. With appropriate data on the location, extent, and physical properties of water‐bearing materials and on the boundaries of the saturated zone flow system, it is possible to analyze the relative merits of a variety of waste disposal techniques and to describe the probable consequences of each. Environments of consolidated rocks, such as granites, sandstones, and limestones, pose problems in addition to those related to unconsolidated or granular porous media in defining the fluid‐flow regimes that involve joint patterns, fracture patterns, solutional openings, and the rock structure. The consequences of ground‐water contamination can be just as damaging to water users as the pollution of surface streams. In fact it can be argued that the consequences are far more damaging because they persist over much longer periods of time after the contaminating source has been eliminated. It would appear prudent, therefore, to guard against contamination of the ground‐water resource in the first instance, rather than to engage in long expensive rehabilitation measures after the damage has been done. In 1960 Graham Walton presented data concerning contamination, by sewage or other man‐made wastes, of surface and underground waters. The circumstances attending the reported incidents of contamination, especially those involving ground‐water supplies, have aided materially in the choice of a few principles and ideas that will identify the role of some significant hydrologic factors in the underground movement of fluid wastes. Walton's discussion of ground‐water contamination refers often to physical settings into which fluid wastes are discharged at or near the land surface into cesspools, tile‐drain fields, and holding ponds. Furthermore, most reported instances of ground‐water contamination have taken place in relatively humid.
","language":"English","publisher":"Wiley Blackwell","doi":"10.1111/j.1745-6584.1964.tb01739.x","usgsCitation":"Brown, R., 1964, Hydrologic factors pertinent to ground‐water contamination: Groundwater, v. 2, no. 1, p. 5-12, https://doi.org/10.1111/j.1745-6584.1964.tb01739.x.","productDescription":"8 p.","startPage":"5","endPage":"12","costCenters":[],"links":[{"id":386147,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/thumbnails/outside_thumb.jpg"}],"volume":"2","issue":"1","noUsgsAuthors":false,"publicationDate":"2006-07-06","publicationStatus":"PW","contributors":{"authors":[{"text":"Brown, R.","contributorId":101419,"corporation":false,"usgs":true,"family":"Brown","given":"R.","affiliations":[],"preferred":false,"id":816821,"contributorType":{"id":1,"text":"Authors"},"rank":1}]}} ,{"id":37483,"text":"37483 - 1964 - Waterfowl status report, 1964","interactions":[],"lastModifiedDate":"2014-07-15T13:33:00","indexId":"37483","displayToPublicDate":"1964-01-01T13:31:20","publicationYear":"1964","noYear":false,"publicationType":{"id":18,"text":"Report"},"publicationSubtype":{"id":1,"text":"Federal Government Series"},"seriesTitle":{"id":83,"text":"Special Scientific Report - Wildlife","active":false,"publicationSubtype":{"id":1}},"seriesNumber":"86","title":"Waterfowl status report, 1964","docAbstract":"No abstract available.","language":"English","publisher":"U.S. Fish and Wildlife Service","publisherLocation":"Washington, D.C.","usgsCitation":"Hansen, H., 1964, Waterfowl status report, 1964: Special Scientific Report - Wildlife 86, ii, 142 p.","productDescription":"ii, 142 p.","numberOfPages":"144","costCenters":[],"links":[{"id":290141,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/thumbnails/outside_thumb.jpg"}],"noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"53c64debe4b0001bd51477da","contributors":{"authors":[{"text":"Hansen, Henry A.","contributorId":15533,"corporation":false,"usgs":true,"family":"Hansen","given":"Henry A.","affiliations":[],"preferred":false,"id":218149,"contributorType":{"id":1,"text":"Authors"},"rank":1}]}} ,{"id":846,"text":"846 - 1964 - Water resources data for Indiana","interactions":[],"lastModifiedDate":"2014-08-05T13:21:31","indexId":"846","displayToPublicDate":"1964-01-01T13:20:04","publicationYear":"1964","noYear":false,"publicationType":{"id":18,"text":"Report"},"publicationSubtype":{"id":6,"text":"USGS Unnumbered Series"},"title":"Water resources data for Indiana","docAbstract":"No abstract available.","language":"English","publisher":"U.S. Department of the Interior","publisherLocation":"Indianapolis, IN","doi":"10.3133/846","issn":"0364-4340","collaboration":"Prepared in cooperation with the State of Indiana and other State and Federal agencies.","usgsCitation":"Water Resources Division, U.S. Geological Survey, 1964, Water resources data for Indiana, https://doi.org/10.3133/846.","costCenters":[],"links":[{"id":291702,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/thumbnails/usgs_thumb.jpg"}],"country":"United States","state":"Indiana","geographicExtents":"{ \"type\": \"FeatureCollection\", \"features\": [ { \"type\": \"Feature\", \"properties\": {}, \"geometry\": { \"type\": \"Polygon\", \"coordinates\": [ [ [ -88.0979,37.7717 ], [ -88.0979,41.7607 ], [ -84.7847,41.7607 ], [ -84.7847,37.7717 ], [ -88.0979,37.7717 ] ] ] } } ] }","noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"53e1efe4e4b0fe532be2dec4","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":527765,"contributorType":{"id":1,"text":"Authors"},"rank":1}]}} ,{"id":25139,"text":"25139 - 1964 - Annual and accrued mineral production, royalty income, and related statistics","interactions":[],"lastModifiedDate":"2014-07-14T13:14:26","indexId":"25139","displayToPublicDate":"1964-01-01T13:13:17","publicationYear":"1964","noYear":false,"publicationType":{"id":18,"text":"Report"},"publicationSubtype":{"id":6,"text":"USGS Unnumbered Series"},"title":"Annual and accrued mineral production, royalty income, and related statistics","docAbstract":"No abstract available.","language":"English","publisher":"U.S. Geological Survey","publisherLocation":"Washington, D.C.","doi":"10.3133/25139","usgsCitation":"Water Resources Division, U.S. Geological Survey, 1964, Annual and accrued mineral production, royalty income, and related statistics, https://doi.org/10.3133/25139.","costCenters":[],"links":[{"id":289915,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/thumbnails/usgs_thumb.jpg"}],"noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"53c4fbece4b0b58d96eeb54d","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":529180,"contributorType":{"id":1,"text":"Authors"},"rank":1}]}} ,{"id":849,"text":"849 - 1964 - Water resources data for Kentucky","interactions":[],"lastModifiedDate":"2014-08-05T13:04:37","indexId":"849","displayToPublicDate":"1964-01-01T13:03:30","publicationYear":"1964","noYear":false,"publicationType":{"id":18,"text":"Report"},"publicationSubtype":{"id":6,"text":"USGS Unnumbered Series"},"title":"Water resources data for Kentucky","docAbstract":"No abstract available.","language":"English","publisher":"U.S. Department of the Interior","publisherLocation":"Louisville, KY","doi":"10.3133/849","issn":"0364-4081","collaboration":"Prepared in cooperation with the Commonwealth of Kentucky, University of Kentucky, Kentucky Geological Survey, and with other state and federal agencies.","usgsCitation":"Water Resources Division, U.S. Geological Survey, 1964, Water resources data for Kentucky, https://doi.org/10.3133/849.","costCenters":[],"links":[{"id":291698,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/thumbnails/usgs_thumb.jpg"}],"country":"United States","state":"Kentucky","geographicExtents":"{ \"type\": \"FeatureCollection\", \"features\": [ { \"type\": \"Feature\", \"properties\": {}, \"geometry\": { \"type\": \"Polygon\", \"coordinates\": [ [ [ -89.5693,36.4972 ], [ -89.5693,39.1475 ], [ -81.965,39.1475 ], [ -81.965,36.4972 ], [ -89.5693,36.4972 ] ] ] } } ] }","noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"53e1efe5e4b0fe532be2decd","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":527768,"contributorType":{"id":1,"text":"Authors"},"rank":1}]}} ,{"id":855,"text":"855 - 1964 - Water resources data for Michigan","interactions":[],"lastModifiedDate":"2014-08-05T12:44:09","indexId":"855","displayToPublicDate":"1964-01-01T12:42:38","publicationYear":"1964","noYear":false,"publicationType":{"id":18,"text":"Report"},"publicationSubtype":{"id":6,"text":"USGS Unnumbered Series"},"title":"Water resources data for Michigan","docAbstract":"No abstract available.","language":"English","publisher":"U.S. Department of the Interior","publisherLocation":"Lansing, MI","doi":"10.3133/855","issn":"0364-4375","collaboration":"Prepared in cooperation with the State of Michigan and other agencies.","usgsCitation":"Water Resources Division, U.S. Geological Survey, 1964, Water resources data for Michigan, https://doi.org/10.3133/855.","costCenters":[],"links":[{"id":291689,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/thumbnails/usgs_thumb.jpg"}],"country":"United States","state":"Michigan","geographicExtents":"{ \"type\": \"FeatureCollection\", \"features\": [ { \"type\": \"Feature\", \"properties\": {}, \"geometry\": { \"type\": \"Polygon\", \"coordinates\": [ [ [ -90.42,41.7 ], [ -90.42,48.2 ], [ -82.41,48.2 ], [ -82.41,41.7 ], [ -90.42,41.7 ] ] ] } } ] }","noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"53e1efe8e4b0fe532be2deee","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":527774,"contributorType":{"id":1,"text":"Authors"},"rank":1}]}} ,{"id":856,"text":"856 - 1964 - Water resources data for Minnesota","interactions":[],"lastModifiedDate":"2014-08-05T12:40:50","indexId":"856","displayToPublicDate":"1964-01-01T12:39:39","publicationYear":"1964","noYear":false,"publicationType":{"id":18,"text":"Report"},"publicationSubtype":{"id":6,"text":"USGS Unnumbered Series"},"title":"Water resources data for Minnesota","docAbstract":"No abstract available.","language":"English","publisher":"U.S. Geological Survey","publisherLocation":"St. Paul, MN","doi":"10.3133/856","issn":"0364-4383","usgsCitation":"Water Resources Division, U.S. Geological Survey, 1964, Water resources data for Minnesota, https://doi.org/10.3133/856.","costCenters":[],"links":[{"id":291688,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/thumbnails/usgs_thumb.jpg"}],"country":"United States","state":"Minnesota","geographicExtents":"{ \"type\": \"FeatureCollection\", \"features\": [ { \"type\": \"Feature\", \"properties\": {}, \"geometry\": { \"type\": \"Polygon\", \"coordinates\": [ [ [ -97.24,43.5 ], [ -97.24,49.38 ], [ -89.49,49.38 ], [ -89.49,43.5 ], [ -97.24,43.5 ] ] ] } } ] }","noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"53e1efe8e4b0fe532be2def3","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":527775,"contributorType":{"id":1,"text":"Authors"},"rank":1}]}} ,{"id":70263594,"text":"wdrCA642 - 1964 - Surface water records of California, 1964; Volume 2: Northern Great Basin and Central Valley","interactions":[],"lastModifiedDate":"2025-02-14T15:32:39.182988","indexId":"wdrCA642","displayToPublicDate":"1964-01-01T10:32:13","publicationYear":"1964","noYear":false,"publicationType":{"id":18,"text":"Report"},"publicationSubtype":{"id":5,"text":"USGS Numbered Series"},"seriesTitle":{"id":340,"text":"Water Data Report","code":"WDR","active":false,"publicationSubtype":{"id":5}},"seriesNumber":"CA-64-2","title":"Surface water records of California, 1964; Volume 2: Northern Great Basin and Central Valley","docAbstract":"The surface-water records for the 1964 water year for gaging stations, partial-record stations, and miscellaneous sites within the State of California are given in this report. For convenience there are also included records for a few pertinent gaging stations in bordering States. The records were collected and computed by the Water Resources Division of the U.S. Geological Survey, under the direction of Walter Hofmann, district engineer, Surface Water Branch.
Through September 30, 1960, the records of discharge and stage of streams and contents and stage of lakes or reservoirs were published in an annual series of U.S. Geological Survey water-supply papers entitled \"Surface Water Supply of the United States.\" Since 1951 there have been 20 volumes in the series; each volume covered an area whose boundaries coincided with those of certain natural drainage areas. The records in California were contained in parts 9, 10, and 11 of that series.
Beginning with the 1961 water year, streamflow records and related data are being released by the Geological Survey in annual reports on a State-boundary basis. Distribution of these basic data reports is limited and primarily for local needs. The records later will be published in Geological Survey water-supply papers at 5-year intervals. These 5-year water-supply papers will show daily discharge and will be compiled on the same geographical areas previously used for the annual series; however, some of the 14 parts of conterminous United States will be further subdivided.
","language":"English","publisher":"U.S. Geological Survey","doi":"10.3133/wdrCA642","collaboration":"Prepared in cooperation with the State of California and with other agencies","usgsCitation":"Water Resources Division, U.S. Geological Survey, 1964, Surface water records of California, 1964; Volume 2: Northern Great Basin and Central Valley: U.S. Geological Survey Water Data Report CA-64-2, xiv, 499-991 p., https://doi.org/10.3133/wdrCA642.","productDescription":"xiv, 499-991 p.","costCenters":[],"links":[{"id":482103,"rank":2,"type":{"id":11,"text":"Document"},"url":"https://pubs.usgs.gov/wdr/1964/ca-64-2/report.pdf","linkFileType":{"id":1,"text":"pdf"}},{"id":482102,"rank":1,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/wdr/1964/ca-64-2/report-thumb.jpg"}],"country":"United States","state":"California","otherGeospatial":"Central Valley, Northern Great 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","language":"English","publisher":"Connecticut Water Resources Commission","collaboration":"Prepared in cooperation with the Connecticut Water Resources Commission","usgsCitation":"Cushman, R., Baker, J.A., and Meikle, R.L., 1964, Records and logs of selected wells and test borings and chemical analyses of water in north-central Connecticut: Connecticut Water Resources Bulletin 4, Report: 27 p.; 1 Figure.","productDescription":"Report: 27 p.; 1 Figure","costCenters":[],"links":[{"id":404007,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/thumbnails/outside_thumb.jpg"}],"country":"United States","state":"Connecticut","geographicExtents":"{\n \"type\": \"FeatureCollection\",\n \"features\": [\n {\n \"type\": \"Feature\",\n \"properties\": {},\n \"geometry\": {\n \"type\": \"Polygon\",\n \"coordinates\": [\n [\n [\n -73.08929443359375,\n 41.38608229923676\n ],\n [\n -72.344970703125,\n 41.38608229923676\n ],\n [\n -72.344970703125,\n 42.042153895364\n ],\n [\n -73.08929443359375,\n 42.042153895364\n ],\n [\n -73.08929443359375,\n 41.38608229923676\n ]\n ]\n ]\n }\n }\n ]\n}","noUsgsAuthors":false,"publicationStatus":"PW","contributors":{"authors":[{"text":"Cushman, R.V.","contributorId":28220,"corporation":false,"usgs":true,"family":"Cushman","given":"R.V.","email":"","affiliations":[],"preferred":false,"id":846914,"contributorType":{"id":1,"text":"Authors"},"rank":1},{"text":"Baker, John A.","contributorId":90815,"corporation":false,"usgs":true,"family":"Baker","given":"John","email":"","middleInitial":"A.","affiliations":[],"preferred":false,"id":846915,"contributorType":{"id":1,"text":"Authors"},"rank":2},{"text":"Meikle, Robert L.","contributorId":100397,"corporation":false,"usgs":true,"family":"Meikle","given":"Robert","email":"","middleInitial":"L.","affiliations":[],"preferred":false,"id":846916,"contributorType":{"id":1,"text":"Authors"},"rank":3}]}} ,{"id":1003311,"text":"1003311 - 1964 - Toxicological effects of herbicides on the fish environment Part 2","interactions":[],"lastModifiedDate":"2012-02-02T00:11:25","indexId":"1003311","displayToPublicDate":"1964-01-01T00:00:00","publicationYear":"1964","noYear":false,"publicationType":{"id":2,"text":"Article"},"publicationSubtype":{"id":10,"text":"Journal Article"},"seriesTitle":{"id":3727,"text":"Water and Sewage Works","active":true,"publicationSubtype":{"id":10}},"title":"Toxicological effects of herbicides on the fish environment Part 2","docAbstract":"Abstract has not been submitted","largerWorkType":{"id":2,"text":"Article"},"largerWorkTitle":"Water and Sewage Works","largerWorkSubtype":{"id":10,"text":"Journal Article"},"language":"English","usgsCitation":"Walker, C., 1964, Toxicological effects of herbicides on the fish environment Part 2: Water and Sewage Works, v. 111, no. 4, p. 173-175.","productDescription":"pp. 173-175","startPage":"173","endPage":"175","numberOfPages":"3","costCenters":[{"id":606,"text":"Upper Midwest Environmental Sciences Center","active":true,"usgs":true}],"links":[{"id":179527,"rank":0,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/thumbnails/outside_thumb.jpg"}],"volume":"111","issue":"4","noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"4f4e4a4ee4b07f02db627f14","contributors":{"authors":[{"text":"Walker, C.R.","contributorId":69097,"corporation":false,"usgs":true,"family":"Walker","given":"C.R.","email":"","affiliations":[],"preferred":false,"id":313097,"contributorType":{"id":1,"text":"Authors"},"rank":1}]}} ,{"id":1000486,"text":"1000486 - 1964 - Bottom sediments of Saginaw Bay, Michigan","interactions":[],"lastModifiedDate":"2013-02-12T08:07:19","indexId":"1000486","displayToPublicDate":"1964-01-01T00:00:00","publicationYear":"1964","noYear":false,"publicationType":{"id":2,"text":"Article"},"publicationSubtype":{"id":10,"text":"Journal Article"},"seriesTitle":{"id":2450,"text":"Journal of Sedimentary Petrology","active":true,"publicationSubtype":{"id":10}},"title":"Bottom sediments of Saginaw Bay, Michigan","docAbstract":"Saginaw Bay is a southwest extension of Lake Huron on the east shore of the Southern Peninsula of Michigan. It is a shallow-water derivative of the Pleistocene Lake Saginaw. Sixty-one bottom samples were collected on a semigrid pattern and analyzed physically. Findings were treated statistically. Sediments range in size from large pebbles to clay. Medium- to fine-grained clear quartz sand is common to all parts of the bay. Currents and wave action are primarily responsible for both median diameter and sorting distribution patterns. Only a very general correlation can be established between depth and median diameter. Heavy minerals occur in abundance locally and show an affinity to shallow-water areas subject to prevailing currents. Shape also locally determines heavy mineral concentrations. Only general conclusions can be established from roundness and sphericity and acid-soluble content. Increased organic content is correlative with quiet water environments. The shallow-water, heterogeneous nature of Saginaw Bay is not conducive to the recognition of sedimentary criteria suitable for correlations in other than a local environment.","largerWorkType":{"id":2,"text":"Article"},"largerWorkTitle":"Journal of Sedimentary Petrology","largerWorkSubtype":{"id":10,"text":"Journal Article"},"language":"English","publisher":"SEPM Society for Sedimentary Geology","publisherLocation":"Tulsa, OK","doi":"10.1306/74D71000-2B21-11D7-8648000102C1865D","collaboration":"Out-of-print","usgsCitation":"Wood, L.E., 1964, Bottom sediments of Saginaw Bay, Michigan: Journal of Sedimentary Petrology, v. 34, no. 1, p. 173-184, https://doi.org/10.1306/74D71000-2B21-11D7-8648000102C1865D.","productDescription":"12 p.","startPage":"173","endPage":"184","numberOfPages":"12","costCenters":[{"id":324,"text":"Great Lakes Science Center","active":true,"usgs":true}],"links":[{"id":131764,"rank":0,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/thumbnails/outside_thumb.jpg"},{"id":267262,"type":{"id":10,"text":"Digital Object Identifier"},"url":"https://dx.doi.org/10.1306/74D71000-2B21-11D7-8648000102C1865D"}],"volume":"34","issue":"1","noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"4f4e4a0ce4b07f02db5fcdf1","contributors":{"authors":[{"text":"Wood, Leonard E.","contributorId":73157,"corporation":false,"usgs":true,"family":"Wood","given":"Leonard","email":"","middleInitial":"E.","affiliations":[],"preferred":false,"id":308612,"contributorType":{"id":1,"text":"Authors"},"rank":1}]}} ,{"id":1000315,"text":"1000315 - 1964 - Age and growth of the round whitefish in Lake Michigan","interactions":[],"lastModifiedDate":"2013-02-04T11:32:48","indexId":"1000315","displayToPublicDate":"1964-01-01T00:00:00","publicationYear":"1964","noYear":false,"publicationType":{"id":2,"text":"Article"},"publicationSubtype":{"id":10,"text":"Journal Article"},"seriesTitle":{"id":3624,"text":"Transactions of the American Fisheries Society","active":true,"publicationSubtype":{"id":10}},"title":"Age and growth of the round whitefish in Lake Michigan","docAbstract":"The round whitefish, though rarely abundant, is widely distributed in northern waters. It is one of the least studied of the coregonines; the present report is but the second for Great Lakes waters. Commercial production in Lake Michigan has been tightly confined to the northern portion. The period 1924-30 showed the best production: 200,000 to 359,000 pounds. Since 1956, production has been around 10,000 pounds or less. The present age and growth study is based on 208 fish collected by gill net in December 1951. The relation between total length in inches (L) and the weight in ounces (W) is described by the equation log W = -2.7232 + 3.2940 log L. Age-group III made up 66.3 percent, and age-group IV, 20.6 percent of the sample; age-groups V, VI, and VII combined contributed only 5.9 percent. The average length for all fish in the sample was 14.5 inches. Growth was calculated from a previously published linear body-scale relation with an intercept of 1.1 inches on the axis of fish length. The increments of calculated length declined steadily from a maximum of 4.6 inches the first year to 1.0 inch the eighth. A 3-year-old Lake Michigan fish (12.3 inches) is as long as a 5-year-old Lake Superior fish, and an 8-year-old Lake Michigan fish (18.9 inches) is 0.9 inch longer than the oldest (12 years) from Lake Superior. The smallest mature males and females were in the length intervals 12.0-12.4 inches and 13.0-13.4 inches, respectively. All males over 1.4 inches and all females over 14.9 inches were mature. The youngest mature males were in age-group II; 36 percent of II-group males but none of the females were mature. All fish older than age-group III were mature.","largerWorkType":{"id":2,"text":"Article"},"largerWorkTitle":"Transactions of the American Fisheries Society","largerWorkSubtype":{"id":10,"text":"Journal Article"},"language":"English","publisher":"Taylor & Francis","publisherLocation":"London, UK","doi":"10.1577/1548-8659(1964)93[46:AAGOTR]2.0.CO;2","collaboration":"Out-of-print","usgsCitation":"Mraz, D., 1964, Age and growth of the round whitefish in Lake Michigan: Transactions of the American Fisheries Society, v. 93, no. 1, p. 46-52, https://doi.org/10.1577/1548-8659(1964)93[46:AAGOTR]2.0.CO;2.","productDescription":"7 p.","startPage":"46","endPage":"52","costCenters":[{"id":324,"text":"Great Lakes Science Center","active":true,"usgs":true}],"links":[{"id":266922,"type":{"id":10,"text":"Digital Object Identifier"},"url":"https://dx.doi.org/10.1577/1548-8659(1964)93[46:AAGOTR]2.0.CO;2"},{"id":132989,"rank":0,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/thumbnails/outside_thumb.jpg"}],"volume":"93","issue":"1","noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"4f4e4ae4e4b07f02db689b6b","contributors":{"authors":[{"text":"Mraz, Donald","contributorId":21502,"corporation":false,"usgs":true,"family":"Mraz","given":"Donald","email":"","affiliations":[],"preferred":false,"id":308378,"contributorType":{"id":1,"text":"Authors"},"rank":1}]}} ,{"id":2354,"text":"wsp1654 - 1964 - Ground water for irrigation in the Snake River Basin in Idaho","interactions":[],"lastModifiedDate":"2023-03-24T18:32:01.922661","indexId":"wsp1654","displayToPublicDate":"1964-01-01T00:00:00","publicationYear":"1964","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":"1654","title":"Ground water for irrigation in the Snake River Basin in Idaho","docAbstract":"The Snake River basin, in southern Idaho, upstream from the mouth of the Powder River in Oregon, includes more than 50 percent of the land area and 65 percent of the total population of the State. More than 2.5 million acres of land is irrigated ; irrigation agriculture and industry allied with agriculture are the basis of the economy of the basin. Most of the easily developed sources of surface water are fully utilized, and few storage sites remain where water could be made available to irrigate lands under present economic conditions. Because surface-water supplies have be come more difficult to obtain, use of ground water has increased greatly. At the present time (1959), about 600,000 acres of land is irrigated with ground water. Ground-water development has been concentrated in areas where large amounts of water are available beneath or adjacent to tracts of arable land and where the depth to water is not excessive under the current economy. Under these criteria, many of the most favorable areas already have been developed; however, tremendous volumes of water are still available for development. In some places, water occurs at depths considered near or beyond the limit for economic recovery, whereas in some other places, water is reasonably close to the surface but no arable land is available in the vicinity. In other parts of the basin large tracts of arable land are without available water supply. Thus the chief tasks in development of the ground-water resources include not only locating and evaluating ground-water supplies but also the planning necessary to bring the water to the land. Irrigation began in the 1860's ; at the present time more than 10 million acre feet of surface water, some of which is recirculated water, is diverted annually for irrigation of more than 2.5 million acres. Diversion of this large quantity of water has had a marked effect on the ground-water regimen. In some areas, the water table has risen more than 100 feet and the discharge of some springs has more than doubled. Large-scale development of ground water began after World War II, and it is estimated that in 1959 about 1,500,000 acre-feet of ground water was pumped for irrigation of the 600,000 acres irrigated wholly with ground water in addition to a substantial amount of ground water pumped to supplement surface-water supplies. Ground water is also the principal source of supply for municipal, industrial, and domestic use. The water regimen in the Snake River basin is greatly influenced by the geology. The rocks forming the mountains are largely consolidated rocks of low permeability; however, a fairly deep and porous subsoil has formed on them by decay and disintegration of the parent rock. Broad intermontane valleys and basins are partly filled with alluvial sand and gravel. The subsoil and alluvial materials are utilized very little as a source of water supply but are important as seasonal ground-water reservoirs because they store water during periods of high rainfall and snowmelt. Discharge from these reservoirs maintains stream flow during periods of surface runoff. Because these aquifers are fairly thin, they drain rapidly and are considerably depleted at the end of each dry cycle. The plain and plateau areas and tributary valleys, on the other hand, are underlain chiefly by rocks of high permeability and porosity. These rocks, mostly basaltic lava flows and alluvial materials, constitute a reservoir which fluctuates only slightly from season to season. Large amounts' of water are withdrawn from them for irrigation and other uses, and discharge from the Snake Plain aquifer is an important part of the total flow of the Snake River downstream from Hagerman Valley. The ultimate source of ground water in the basin is precipitation on the basin. In the mountainous areas, aquifers mostly are recharged directly by precipitation.
","language":"English","publisher":"U.S. Geological Survey","doi":"10.3133/wsp1654","usgsCitation":"Mundorff, M.J., Crosthwaite, E., and Kilburn, C., 1964, Ground water for irrigation in the Snake River Basin in Idaho: U.S. Geological Survey Water Supply Paper 1654, vii, 224 p., https://doi.org/10.3133/wsp1654.","productDescription":"vii, 224 p.","costCenters":[],"links":[{"id":414716,"rank":3,"type":{"id":36,"text":"NGMDB Index Page"},"url":"https://ngmdb.usgs.gov/Prodesc/proddesc_24846.htm","linkFileType":{"id":5,"text":"html"}},{"id":28283,"rank":2,"type":{"id":11,"text":"Document"},"url":"https://pubs.usgs.gov/wsp/1654/report.pdf","linkFileType":{"id":1,"text":"pdf"}},{"id":137782,"rank":1,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/wsp/1654/report-thumb.jpg"}],"country":"United States","state":"Idaho","otherGeospatial":"Snake River basin","geographicExtents":"{\n \"type\": \"FeatureCollection\",\n \"features\": [\n {\n \"type\": \"Feature\",\n \"properties\": {},\n \"geometry\": {\n \"coordinates\": [\n [\n [\n -111.048,\n 45.217\n ],\n [\n -117.213,\n 45.217\n ],\n [\n -117.213,\n 42\n ],\n [\n -111.048,\n 42\n ],\n [\n -111.048,\n 45.217\n ]\n ]\n ],\n \"type\": \"Polygon\"\n }\n }\n ]\n}","noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"4f4e4ab0e4b07f02db66dc28","contributors":{"authors":[{"text":"Mundorff, Maurice John","contributorId":41404,"corporation":false,"usgs":true,"family":"Mundorff","given":"Maurice","email":"","middleInitial":"John","affiliations":[],"preferred":false,"id":145067,"contributorType":{"id":1,"text":"Authors"},"rank":1},{"text":"Crosthwaite, E. G.","contributorId":83098,"corporation":false,"usgs":true,"family":"Crosthwaite","given":"E. G.","affiliations":[],"preferred":false,"id":145068,"contributorType":{"id":1,"text":"Authors"},"rank":2},{"text":"Kilburn, Chabot","contributorId":83499,"corporation":false,"usgs":true,"family":"Kilburn","given":"Chabot","email":"","affiliations":[],"preferred":false,"id":145069,"contributorType":{"id":1,"text":"Authors"},"rank":3}]}} ,{"id":1001811,"text":"1001811 - 1964 - Numbered nasal discs for waterfowl","interactions":[],"lastModifiedDate":"2025-02-05T16:56:06.547022","indexId":"1001811","displayToPublicDate":"1964-01-01T00:00:00","publicationYear":"1964","noYear":false,"publicationType":{"id":2,"text":"Article"},"publicationSubtype":{"id":10,"text":"Journal Article"},"seriesTitle":{"id":2508,"text":"Journal of Wildlife Management","active":true,"publicationSubtype":{"id":10}},"title":"Numbered nasal discs for waterfowl","docAbstract":"Numbered nasal discs were successfully used in studies requiring large numbers of individually marked waterfowl. The procedure for constructing these discs is outlined. Blue-winged teal (Anas discors) with 5/8-inch discs, and canvasback (Aythya valisineria) and redhead (A. americana) with 3/4-inch discs can be individually identified up to 50 and 80 yards, respectively, with a gunstock-mounted, 20-power spotting scope. The particular value of these markers is their durability, the number of combinations possible, and the apparent absence of behavioral or mortality influence among such species as the blue-winged teal.
","language":"English","publisher":"Wiley","doi":"10.2307/3798783","usgsCitation":"Bartonek, J., and Dane, C., 1964, Numbered nasal discs for waterfowl: Journal of Wildlife Management, v. 28, no. 4, p. 688-692, https://doi.org/10.2307/3798783.","productDescription":"5 p.","startPage":"688","endPage":"692","costCenters":[{"id":480,"text":"Northern Prairie Wildlife Research Center","active":true,"usgs":true}],"links":[{"id":130488,"rank":1,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/thumbnails/outside_thumb.jpg"}],"volume":"28","issue":"4","noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"4f4e4afce4b07f02db696878","contributors":{"authors":[{"text":"Bartonek, James C.","contributorId":38085,"corporation":false,"usgs":true,"family":"Bartonek","given":"James C.","affiliations":[],"preferred":false,"id":311836,"contributorType":{"id":1,"text":"Authors"},"rank":1},{"text":"Dane, C.W.","contributorId":95003,"corporation":false,"usgs":true,"family":"Dane","given":"C.W.","email":"","affiliations":[],"preferred":false,"id":311837,"contributorType":{"id":1,"text":"Authors"},"rank":2}]}} ,{"id":2233,"text":"wsp1779C - 1964 - Chemical quality of surface water in the West Branch Susquehanna River basin, Pennsylvania","interactions":[],"lastModifiedDate":"2023-03-22T18:45:31.751873","indexId":"wsp1779C","displayToPublicDate":"1964-01-01T00:00:00","publicationYear":"1964","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":"1779","chapter":"C","title":"Chemical quality of surface water in the West Branch Susquehanna River basin, Pennsylvania","docAbstract":"The West Branch Susquehanna River is 228 miles long and drains 6,913 square miles of mountainous area in central Pennsylvania. Much of this area is forestcovered wilderness, part of which is reserved as State game land. Wild animals, such as deer, bear, turkey and grouse, are sheltered there, and many streams contain trout and other game fish. This helps to make the region one of the best hunting and fishing areas in Pennsylvania. The Congress has approved Federal funds for the construction of several reservoirs to prevent flooding of the main river and several of its tributaries. Water stored behind the dams will not be withdrawn below a minimum level designated as conservation pools. These pools will be available for recreation. Several headwater streams, such as Clearfield, Moshannon, and at times Sinnemahoning Creek, that carry drainage from coal mines are acid and contain high concentrations of dissolved solids, especially sulfates. These streams acidify the West Branch Susquehanna River downstream as far as Jersey Shore. One of the most influential tributaries affecting the quality of the West Branch Susquehanna River after they merge is Bald Eagle Creek. Bald Eagle Creek enters the main river downstream from Lock Haven which is approximately 100 river miles from the river's source. Because of its alkaline properties, water of Bald Eagle Creek can neutralize acidic water. Many streams draining small areas and several draining large areas such as Pine Creek, Lycoming Creek, and Loyalsock Creek are clear nearly neutral water low in dissolved solids whose pH is about 7.0 most of the time. These streams have a diluting and neutralizing effect on the quality of the West Branch Susquehanna River, so that from Williamsport downstream the river water is rarely acid, and for most of the time it is of good chemical quality.
","language":"English","publisher":"U.S. Geological Survey","doi":"10.3133/wsp1779C","usgsCitation":"McCarren, E.F., 1964, Chemical quality of surface water in the West Branch Susquehanna River basin, Pennsylvania: U.S. Geological Survey Water Supply Paper 1779, Report; iv, 40 p.; 1 Plate: 21.00 x 16.62 inches, https://doi.org/10.3133/wsp1779C.","productDescription":"Report; iv, 40 p.; 1 Plate: 21.00 x 16.62 inches","costCenters":[{"id":532,"text":"Pennsylvania Water Science Center","active":true,"usgs":true}],"links":[{"id":27992,"rank":2,"type":{"id":11,"text":"Document"},"url":"https://pubs.usgs.gov/wsp/1779c/report.pdf","linkFileType":{"id":1,"text":"pdf"}},{"id":414560,"rank":4,"type":{"id":36,"text":"NGMDB Index Page"},"url":"https://ngmdb.usgs.gov/Prodesc/proddesc_24956.htm","linkFileType":{"id":5,"text":"html"}},{"id":27991,"rank":3,"type":{"id":17,"text":"Plate"},"url":"https://pubs.usgs.gov/wsp/1779c/plate-1.pdf","linkFileType":{"id":1,"text":"pdf"}},{"id":137748,"rank":1,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/wsp/1779c/report-thumb.jpg"}],"country":"United States","state":"Pennsylvania","otherGeospatial":"Susquehanna River basin","geographicExtents":"{\n \"type\": \"FeatureCollection\",\n \"features\": [\n {\n \"type\": \"Feature\",\n \"properties\": {},\n \"geometry\": {\n \"coordinates\": [\n [\n [\n -78.667,\n 41.75\n ],\n [\n -78.667,\n 40.583\n ],\n [\n -76.25,\n 40.583\n ],\n [\n -76.25,\n 41.75\n ],\n [\n -78.667,\n 41.75\n ]\n ]\n ],\n \"type\": \"Polygon\"\n }\n }\n ]\n}","noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"4f4e49dfe4b07f02db5e3b11","contributors":{"authors":[{"text":"McCarren, Edward F.","contributorId":106472,"corporation":false,"usgs":true,"family":"McCarren","given":"Edward","email":"","middleInitial":"F.","affiliations":[],"preferred":false,"id":144863,"contributorType":{"id":1,"text":"Authors"},"rank":1}]}} ,{"id":70191371,"text":"70191371 - 1964 - Developing a State Water Plan: A basic water resource data program for Utah","interactions":[],"lastModifiedDate":"2017-10-09T08:52:31","indexId":"70191371","displayToPublicDate":"1964-01-01T00:00:00","publicationYear":"1964","noYear":false,"publicationType":{"id":18,"text":"Report"},"publicationSubtype":{"id":2,"text":"State or Local Government Series"},"seriesTitle":{"id":110,"text":"Cooperative Investigations Report","active":true,"publicationSubtype":{"id":2}},"seriesNumber":"1","title":"Developing a State Water Plan: A basic water resource data program for Utah","docAbstract":"Reliable data on Utah's water resources are essential to development of a State Water plan. While the need for such data was outlined in the report entitles \"Developing a State Water Plan - Utah's water resources, problems, and needs - A challenge\" published by the Utah Water and Power Board and Utah State University in 1963, the discussion was, of necessity, brief. Further definition and scheduling of data collection and related investigations were known to be needed.
The report which follows was prepared by the U.S. Geological Survey as part of that agency's cooperative program with the State of Utah. It outlines, in greater detail, what the Geological Survey feels is an appropriate long-range program of investigations to provide part of the basic data which will be needed during the course of the State's water planning program. Some of these investigations already are underway, and others will be undertaken in the immediate future.