The purpose of this investigation is to provide information about the ground-water resources in Benson and Pierce Counties that is sufficient for planning the safe and intelligent development of water supplies for irrigation, domestic, stock, industrial, and municipal purposes. The investigation is part of a statewide program to determine the location and extent of ground-water aquifers; to evaluate the occurrence and movement of ground water within the aquifers, including sources of recharge and discharge; to determine potential yields to wells developed in the aquifers; and to determine the chemical quality of ground water.
Benson and Pierce Counties cover an area of 2,512 square miles in north-central North Dakota. This study, which began in July 1967 and was completed in June 1971, was made cooperatively by the U.S. Geological Survey, the North Dakota State Water Commission, the North Dakota Geological Survey, and the Benson and Pierce Counties Water Management Districts. This interim report presents only the major conclusions of the study.
","language":"English","publisher":"U.S. Geological Survey","doi":"10.3133/ha476","usgsCitation":"Randich, P., 1972, Ground-water resources of Benson and Pierce Counties, north-central North Dakota: U.S. Geological Survey Hydrologic Atlas 476, 43.0 x 34.5 inches, https://doi.org/10.3133/ha476.","productDescription":"43.0 x 34.5 inches","costCenters":[{"id":478,"text":"North Dakota Water Science Center","active":true,"usgs":true},{"id":34685,"text":"Dakota Water Science Center","active":true,"usgs":true}],"links":[{"id":186110,"rank":0,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/thumbnails/usgs_thumb.jpg"},{"id":89322,"rank":400,"type":{"id":17,"text":"Plate"},"url":"https://pubs.usgs.gov/ha/476/plate-1.pdf","linkFileType":{"id":1,"text":"pdf"}}],"scale":"26720","country":"United States","state":"North Dakota","county":"Benson County, Pierce County","geographicExtents":"{\"type\":\"FeatureCollection\",\"features\":[{\"type\":\"Feature\",\"geometry\":{\"type\":\"Polygon\",\"coordinates\":[[[-98.5254,47.9159],[-98.5261,47.8478],[-98.5463,47.8481],[-98.9586,47.8477],[-99.092,47.8478],[-99.1419,47.8478],[-99.1816,47.8477],[-99.2974,47.8479],[-99.8141,47.8477],[-100.0694,47.8469],[-100.1987,47.8477],[-100.1972,48.0213],[-100.2384,48.0218],[-100.2376,48.3699],[-100.2777,48.3704],[-100.2771,48.543],[-100.1457,48.5437],[-99.9367,48.5425],[-99.9068,48.5424],[-99.8904,48.5423],[-99.885,48.5423],[-99.7556,48.5435],[-99.6249,48.5432],[-99.4942,48.5433],[-99.4942,48.457],[-99.4935,48.3688],[-99.2029,48.3697],[-99.2033,48.2811],[-99.203,48.259],[-99.2032,48.2511],[-99.2023,48.1949],[-99.201,48.157],[-99.1977,48.1538],[-99.1924,48.1505],[-99.1836,48.1486],[-99.1762,48.1462],[-99.1708,48.1452],[-99.1668,48.1447],[-99.1621,48.1415],[-99.154,48.1386],[-99.1371,48.1408],[-99.133,48.1389],[-99.1311,48.1356],[-99.1298,48.1324],[-99.1292,48.1301],[-99.1272,48.1278],[-99.1206,48.1217],[-99.1187,48.1134],[-99.1175,48.1069],[-99.0735,48.1065],[-99.0713,48.053],[-99.0711,48.0341],[-99.0706,48.0235],[-99.0625,48.0234],[-99.0531,48.0238],[-99.0509,48.0311],[-99.0446,48.0398],[-99.0377,48.0457],[-99.0289,48.0484],[-99.0213,48.052],[-99.0126,48.0519],[-99.0018,48.0504],[-99.0012,48.0458],[-99.0034,48.0398],[-99.0028,48.0352],[-99.0015,48.032],[-99.0017,48.0255],[-99.0024,48.0237],[-98.9945,48.0149],[-98.9877,48.018],[-98.9843,48.0166],[-98.9892,48.0125],[-98.9934,48.0047],[-98.9983,47.996],[-98.9943,47.9932],[-98.9916,47.9941],[-98.9787,47.9986],[-98.9678,48.0021],[-98.9569,48.0038],[-98.9536,48.0038],[-98.9475,48.0037],[-98.932,48.0004],[-98.9232,48.0012],[-98.9157,48.0052],[-98.9183,48.0099],[-98.9208,48.0173],[-98.918,48.0205],[-98.9079,48.0227],[-98.8998,48.0207],[-98.9005,48.0193],[-98.8973,48.011],[-98.894,48.0087],[-98.8906,48.0096],[-98.8865,48.0141],[-98.8808,48.0228],[-98.8894,48.033],[-98.8885,48.0386],[-98.8845,48.0385],[-98.8799,48.0352],[-98.8752,48.0324],[-98.8657,48.0355],[-98.8568,48.0391],[-98.852,48.0414],[-98.8513,48.0418],[-98.8439,48.0422],[-98.8356,48.0476],[-98.8328,48.0503],[-98.828,48.0554],[-98.8238,48.0608],[-98.8217,48.0631],[-98.8116,48.0611],[-98.8016,48.0583],[-98.7975,48.0582],[-98.7955,48.0573],[-98.7989,48.0545],[-98.7996,48.0541],[-98.8031,48.0509],[-98.8025,48.0481],[-98.796,48.0388],[-98.7861,48.0277],[-98.7864,48.0175],[-98.786,48.006],[-98.7801,48.0018],[-98.7747,48.0008],[-98.77,48.0017],[-98.7711,48.0081],[-98.7704,48.0118],[-98.767,48.0118],[-98.7637,48.0089],[-98.7624,48.0066],[-98.7639,48.0016],[-98.7619,47.9997],[-98.7566,47.996],[-98.7553,47.9946],[-98.754,47.9913],[-98.7576,47.9849],[-98.7801,47.976],[-98.7877,47.9682],[-98.7933,47.9623],[-98.7988,47.9587],[-98.7995,47.9555],[-98.7982,47.9527],[-98.7956,47.9508],[-98.7929,47.9508],[-98.7881,47.9517],[-98.7764,47.9626],[-98.7702,47.9666],[-98.76,47.9707],[-98.7477,47.9742],[-98.7423,47.9755],[-98.7361,47.981],[-98.7311,47.9883],[-98.7276,47.9933],[-98.7208,47.9969],[-98.7146,47.9996],[-98.7071,48.0027],[-98.699,48.004],[-98.6841,48.0047],[-98.674,48.0023],[-98.6681,47.9981],[-98.6656,47.9916],[-98.6666,47.9778],[-98.6641,47.9727],[-98.659,47.9629],[-98.6524,47.9559],[-98.6418,47.9484],[-98.6278,47.9418],[-98.6273,47.9358],[-98.6362,47.9322],[-98.633,47.9248],[-98.6272,47.9183],[-98.6246,47.915],[-98.6198,47.9177],[-98.6056,47.918],[-98.5914,47.9178],[-98.5881,47.9154],[-98.5254,47.9159]]]},\"properties\":{\"name\":\"Benson\",\"state\":\"ND\"}}]}","noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"4f4e4a9ae4b07f02db65d9dc","contributors":{"authors":[{"text":"Randich, P.G.","contributorId":69953,"corporation":false,"usgs":true,"family":"Randich","given":"P.G.","affiliations":[],"preferred":false,"id":277585,"contributorType":{"id":1,"text":"Authors"},"rank":1}]}} ,{"id":68058,"text":"ha434 - 1972 - Analog simulation of water-level declines in the Sparta sand, Mississippi embayment","interactions":[],"lastModifiedDate":"2022-08-22T20:17:21.838054","indexId":"ha434","displayToPublicDate":"1994-01-01T00:00:00","publicationYear":"1972","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":"434","title":"Analog simulation of water-level declines in the Sparta sand, Mississippi embayment","docAbstract":"No abstract available.
","language":"English","publisher":"U.S. Geological Survey","doi":"10.3133/ha434","usgsCitation":"Reed, J., 1972, Analog simulation of water-level declines in the Sparta sand, Mississippi embayment: U.S. Geological Survey Hydrologic Atlas 434, 1 Plate: 32.00 × 34.00 inches, https://doi.org/10.3133/ha434.","productDescription":"1 Plate: 32.00 × 34.00 inches","costCenters":[],"links":[{"id":186109,"rank":0,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/thumbnails/usgs_thumb.jpg"},{"id":405405,"rank":3,"type":{"id":36,"text":"NGMDB Index Page"},"url":"https://ngmdb.usgs.gov/Prodesc/proddesc_15819.htm","linkFileType":{"id":5,"text":"html"}},{"id":89321,"rank":400,"type":{"id":17,"text":"Plate"},"url":"https://pubs.usgs.gov/ha/434/plate-1.pdf","linkFileType":{"id":1,"text":"pdf"}}],"scale":"2500000","country":"United States","state":"Arkansas, Louisiana, Mississippi, Missouri, Tennessee","otherGeospatial":"Mississippi embayment","geographicExtents":"{\n \"type\": \"FeatureCollection\",\n \"features\": [\n {\n \"type\": \"Feature\",\n \"properties\": {},\n \"geometry\": {\n \"type\": \"Polygon\",\n \"coordinates\": [\n [\n [\n -93.667,\n 31\n ],\n [\n -88.50,\n 31\n ],\n [\n -88.50,\n 37\n ],\n [\n -93.667,\n 37\n ],\n [\n -93.667,\n 31\n ]\n ]\n ]\n }\n }\n ]\n}","noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"4f4e4ad5e4b07f02db683a6d","contributors":{"authors":[{"text":"Reed, J.E.","contributorId":41801,"corporation":false,"usgs":true,"family":"Reed","given":"J.E.","email":"","affiliations":[],"preferred":false,"id":277584,"contributorType":{"id":1,"text":"Authors"},"rank":1}]}} ,{"id":14599,"text":"ofr72218 - 1972 - Clay deposits of the Connecticut River Valley, Connecticut: a special problem in land management","interactions":[],"lastModifiedDate":"2018-05-08T11:08:04","indexId":"ofr72218","displayToPublicDate":"1994-01-01T00:00:00","publicationYear":"1972","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":"72-218","title":"Clay deposits of the Connecticut River Valley, Connecticut: a special problem in land management","docAbstract":"When man first settled the United States, two natural features favored settlement; flat land that was easy to build on and to farm, and a nearby river that could act as a source of water, transportation, and power. The Connecticut River Valley from Middletown, Ct. north past the Connecticut-Massachusetts state line satisfied these two needs, and was favored by many early Americans in New England. This area remains an area of rapid urbanization, partly because of the broad flat lowlands.
The subdued topography of this area is due in large part to deposition of fine-grained materials into glacial Lake Hitchcock. This lake was formed during the Wisconsinan age when southward drainage in the Triassic valley of Connecticut was dammed by glacial drift in the area of Rocky Hill, Connecticut. Lake Hitchcock grew to and beyond St. Johnsbury, Vt. with much of the lake being filled with cyclical lake-bottom deposits during the 2,290 to 2,350 years of its life.
Aside from the relative flatness inherent in the deposition of fine-grained lake-bottom deposits, these deposits present very few characteristics that are favorable for urbanization. Favorable characteristics are possible sources of clay for manufacturing and possible sources for waste storage sites. Unfavorable characteristics include low water yields resulting in poor urban water-supply sources, and very low flows in streams during dry periods; low percolation rates resulting In drainage and septic problems; and low or uneven bearing strength which create problems in construction.
Fine-grained lake-bottom deposits have been mapped for six quadrangles in the Connecticut Valley lowlands; the quadrangles of Windsor Locks, Broad Brook, Hartford North, Manchester, Hartford South, and Glastonbury (all located in Connecticut). All the maps were prepared from existing information including well and test hole data on file at the Water Resources Division in Hartford, surficial geologic quadrangle maps, and bedrock contour maps. The maps also reflect geologic interpretations of the history of glacial Lake Hitchcock.
The Hartford North maps were prepared as test maps to determine if the project was feasible. They were prepared using the previously described information plus additional subsurface data obtained from engineering firms and the State Highway Department.
During preparation of the maps, an arcuate-shaped, ice-contact deposit composed of coarse sand and gravel was delineated in the Broad Brook and Windsor Locks quadrangles. This feature marks the location of a zone of stagnant ice In front of and marginal to active ice to the north.
Two types of maps were prepared for the area in study; Thickness of the Principal Clay Deposit, and Thickness of Material Overlying the Principal Clay Deposit. The term \"principal clay deposit\" refers to the fine-grained lake-bottom deposits of Glacial Lake Hitchcock. These maps define the distribution of the deposit, and show the thickness of the deposit in 50 foot intervals and the thickness of the material overlying the deposit In 20 foot intervals. The maps indicate that much of the area is underlain with substantial thicknesses of finegrained lake-bottom deposits (50 feet thick or greater), and that much of the deposit is within 20 feet of the surface.
The maps included in this report can be used for land-use planning. Uses include location of favorable sites for specific uses such as landfills, utility corridors, heavy construction, etc; location of problem areas for specific land uses; identification of possible problems for specific areas; design and construction cost estimates; and prospecting for exploitable clay deposits. It Is suggested that, for effective planning, these maps be used together or in conjunction with other maps such as maps showing surface materials, depth to bedrock, depth to water table, and flood prone areas.
","language":"English","publisher":"U.S. Geological Survey","doi":"10.3133/ofr72218","usgsCitation":"Langer, W.H., 1972, Clay deposits of the Connecticut River Valley, Connecticut: a special problem in land management: U.S. Geological Survey Open-File Report 72-218, Report: vii, 39 leaves; 13 Plates: 22.43 x 30.27 inches or smaller, https://doi.org/10.3133/ofr72218.","productDescription":"Report: vii, 39 leaves; 13 Plates: 22.43 x 30.27 inches or smaller","costCenters":[],"links":[{"id":354002,"rank":15,"type":{"id":17,"text":"Plate"},"url":"https://pubs.usgs.gov/of/1972/0218/plate-13.pdf","linkFileType":{"id":1,"text":"pdf"}},{"id":354001,"rank":14,"type":{"id":17,"text":"Plate"},"url":"https://pubs.usgs.gov/of/1972/0218/plate-12.pdf","linkFileType":{"id":1,"text":"pdf"}},{"id":353997,"rank":10,"type":{"id":17,"text":"Plate"},"url":"https://pubs.usgs.gov/of/1972/0218/plate-8.pdf","linkFileType":{"id":1,"text":"pdf"}},{"id":353989,"rank":2,"type":{"id":11,"text":"Document"},"url":"https://pubs.usgs.gov/of/1972/0218/report.pdf","linkFileType":{"id":1,"text":"pdf"}},{"id":353995,"rank":8,"type":{"id":17,"text":"Plate"},"url":"https://pubs.usgs.gov/of/1972/0218/plate-6.pdf","linkFileType":{"id":1,"text":"pdf"}},{"id":353998,"rank":11,"type":{"id":17,"text":"Plate"},"url":"https://pubs.usgs.gov/of/1972/0218/plate-9.pdf","linkFileType":{"id":1,"text":"pdf"}},{"id":353990,"rank":3,"type":{"id":17,"text":"Plate"},"url":"https://pubs.usgs.gov/of/1972/0218/plate-1.pdf","linkFileType":{"id":1,"text":"pdf"}},{"id":353991,"rank":4,"type":{"id":17,"text":"Plate"},"url":"https://pubs.usgs.gov/of/1972/0218/plate-2.pdf","linkFileType":{"id":1,"text":"pdf"}},{"id":353992,"rank":5,"type":{"id":17,"text":"Plate"},"url":"https://pubs.usgs.gov/of/1972/0218/plate-3.pdf","linkFileType":{"id":1,"text":"pdf"}},{"id":353993,"rank":6,"type":{"id":17,"text":"Plate"},"url":"https://pubs.usgs.gov/of/1972/0218/plate-4.pdf","linkFileType":{"id":1,"text":"pdf"}},{"id":353994,"rank":7,"type":{"id":17,"text":"Plate"},"url":"https://pubs.usgs.gov/of/1972/0218/plate-5.pdf","linkFileType":{"id":1,"text":"pdf"}},{"id":353996,"rank":9,"type":{"id":17,"text":"Plate"},"url":"https://pubs.usgs.gov/of/1972/0218/plate-7.pdf","linkFileType":{"id":1,"text":"pdf"}},{"id":353999,"rank":12,"type":{"id":17,"text":"Plate"},"url":"https://pubs.usgs.gov/of/1972/0218/plate-10.pdf","linkFileType":{"id":1,"text":"pdf"}},{"id":354000,"rank":13,"type":{"id":17,"text":"Plate"},"url":"https://pubs.usgs.gov/of/1972/0218/plate-11.pdf","linkFileType":{"id":1,"text":"pdf"}},{"id":148239,"rank":0,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/of/1972/0218/report-thumb.jpg"}],"scale":"24000","country":"United States","state":"Connecticut","otherGeospatial":"Connecticut River Valley","geographicExtents":"{\n \"type\": \"FeatureCollection\",\n \"features\": [\n {\n \"type\": \"Feature\",\n \"properties\": {},\n \"geometry\": {\n \"type\": \"Polygon\",\n \"coordinates\": [\n [\n [\n -72.75,\n 41.625\n ],\n [\n -72.5,\n 41.625\n ],\n [\n -72.5,\n 42\n ],\n [\n -72.75,\n 42\n ],\n [\n -72.75,\n 41.625\n ]\n ]\n ]\n }\n }\n ]\n}","noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"4f4e4abbe4b07f02db672b5f","contributors":{"authors":[{"text":"Langer, William H. blanger@usgs.gov","contributorId":1241,"corporation":false,"usgs":true,"family":"Langer","given":"William","email":"blanger@usgs.gov","middleInitial":"H.","affiliations":[{"id":387,"text":"Mineral Resources Program","active":true,"usgs":true}],"preferred":false,"id":169716,"contributorType":{"id":1,"text":"Authors"},"rank":1}]}} ,{"id":68042,"text":"ha421 - 1972 - Availability and quality of ground water in the Ashland quadrangle, Jackson County, Oregon","interactions":[],"lastModifiedDate":"2017-02-03T13:27:05","indexId":"ha421","displayToPublicDate":"1994-01-01T00:00:00","publicationYear":"1972","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":"421","title":"Availability and quality of ground water in the Ashland quadrangle, Jackson County, Oregon","language":"ENGLISH","doi":"10.3133/ha421","usgsCitation":"Robison, J.H., 1972, Availability and quality of ground water in the Ashland quadrangle, Jackson County, Oregon: U.S. Geological Survey Hydrologic Atlas 421, 1 map., https://doi.org/10.3133/ha421.","productDescription":"1 map.","costCenters":[{"id":518,"text":"Oregon Water Science Center","active":true,"usgs":true}],"links":[{"id":187737,"rank":0,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/thumbnails/usgs_thumb.jpg"},{"id":89295,"rank":400,"type":{"id":17,"text":"Plate"},"url":"https://pubs.usgs.gov/ha/421/plate-1.pdf","linkFileType":{"id":1,"text":"pdf"}}],"scale":"62500","geographicExtents":"{ \"type\": \"FeatureCollection\", \"features\": [ { \"type\": \"Feature\", \"properties\": {}, \"geometry\": { \"type\": \"Polygon\", \"coordinates\": [ [ [ -122.75,42 ], [ -122.75,42.25 ], [ -122.5,42.25 ], [ -122.5,42 ], [ -122.75,42 ] ] ] } } ] }","noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"4f4e4aa9e4b07f02db667f40","contributors":{"authors":[{"text":"Robison, J. H.","contributorId":60183,"corporation":false,"usgs":true,"family":"Robison","given":"J.","email":"","middleInitial":"H.","affiliations":[],"preferred":false,"id":277554,"contributorType":{"id":1,"text":"Authors"},"rank":1}]}} ,{"id":48096,"text":"ofr72462 - 1972 - A summary view of water supply and demand in the San Francisco Bay Region, California","interactions":[],"lastModifiedDate":"2014-05-29T07:35:21","indexId":"ofr72462","displayToPublicDate":"1994-01-01T00:00:00","publicationYear":"1972","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":"72-462","title":"A summary view of water supply and demand in the San Francisco Bay Region, California","docAbstract":"This report presents a summary view of the water-supply situation in the nine counties that comprise the San Francisco Bay region, California, and thereby provides water data, based on 1970 conditions, that are needed for regional planning. For the purpose of this study the nine-county region has been divided into 15 subregions on the basis of hydrologic and economic considerations. Firm water supply is tabulated for each subregion by source--ground water, surface water, and imported water. Water demand in 1970 is tabulated for each subregion by type of use or demand--public supply, rural self-supply, irrigation, self-supplied industrial water and thermoelectric power generation.
\nThe San Francisco Bay region is dependent to a large degree on imported water. Under 1970 conditions of development, the firm water supply is 2.2 million acre-feet per year; of that quantity, almost 1 million acre-feet per year is imported water. The water demand in 1970 was 1.9 million acre-feet, about half of which was consumed. Under 1970 conditions of water development and use, a series of dry years would probably necessitate some curtailment of irrigation activities in four of the subregions, where the bulk of the demands i for irrigation water. Under those same conditions there is generally ample water for municipal and industrial use throughout the region, except in eastern Marin County where the firm municipal supple does not exceed the 1970 demand for municipal and industrial water.
\nAlthough the firm water supply of the San Francisco Bay region, including imported water, is generally adequate to meet present needs, supplemental supply will be required to meet increased demand in the future. The expansion of existing surface-water facilities and the construction of new surface-water projects, now considered feasible, could provide a combined firm supplemental yield of slightly more than 1 million acre-feet per year, almost three-fourths of which would be available for import by those subregions that might experience a water deficient in the future. However, any supplemental water that might be developed by such alternative methods as desalination of brackish or salt water, weather modification, and various conservation measure, will correspondingly reduce requirement for supplemental water from the more conventional sources.
\nThe aspect of water quality is not discussed in this paper. Because of the present availability of imported water of good or acceptable quality, water quality, as it affects the supply, is not a serious problem at this time, except perhaps in local areas adjacent to San Francisco Bay and in the Sacramento-San Joaquin Delta. In those areas ground water has been degraded by salinity intrusion. Although the prediction of future trends in population, land use, and water demand is beyond the scope of this report, there is not doubt that vigilance and careful planning will be required to prevent serious future deterioration of the quality of the water supply.
","language":"English","publisher":"U.S. Geological Survey","publisherLocation":"Menlo Park, CA","doi":"10.3133/ofr72462","collaboration":"Prepared in cooperation with the U.S. Department of Housing and Urban Development","usgsCitation":"Rantz, S.E., 1972, A summary view of water supply and demand in the San Francisco Bay Region, California: U.S. Geological Survey Open-File Report 72-462, iv, 41 p., https://doi.org/10.3133/ofr72462.","productDescription":"iv, 41 p.","numberOfPages":"44","costCenters":[],"links":[{"id":287754,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/thumbnails/usgs_thumb.jpg"},{"id":287753,"type":{"id":11,"text":"Document"},"url":"https://pubs.usgs.gov/of/1972/0462/report.pdf"}],"country":"United States","state":"California","otherGeospatial":"San Francisco Bay","geographicExtents":"{ \"type\": \"FeatureCollection\", \"features\": [ { \"type\": \"Feature\", \"properties\": {}, \"geometry\": { \"type\": \"Polygon\", \"coordinates\": [ [ [ -124.0,37.0 ], [ -124.0,39.0 ], [ -121.0,39.0 ], [ -121.0,37.0 ], [ -124.0,37.0 ] ] ] } } ] }","noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"4f4e4b17e4b07f02db6a5f0d","contributors":{"authors":[{"text":"Rantz, Saul E.","contributorId":46010,"corporation":false,"usgs":true,"family":"Rantz","given":"Saul","email":"","middleInitial":"E.","affiliations":[],"preferred":false,"id":236802,"contributorType":{"id":1,"text":"Authors"},"rank":1}]}} ,{"id":48011,"text":"ofr7238 - 1972 - Water temperatures of California streams, central coastal subregion","interactions":[],"lastModifiedDate":"2012-02-02T00:10:03","indexId":"ofr7238","displayToPublicDate":"1994-01-01T00:00:00","publicationYear":"1972","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":"72-38","title":"Water temperatures of California streams, central coastal subregion","language":"ENGLISH","doi":"10.3133/ofr7238","usgsCitation":"Blodgett, J.C., 1972, Water temperatures of California streams, central coastal subregion: U.S. Geological Survey Open-File Report 72-38, 80 p. ill., maps ; 27 cm., https://doi.org/10.3133/ofr7238.","productDescription":"80 p. ill., maps ; 27 cm.","costCenters":[],"links":[{"id":161654,"rank":0,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/thumbnails/usgs_thumb.jpg"}],"noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"4f4e49f4e4b07f02db5efe3f","contributors":{"authors":[{"text":"Blodgett, J. C.","contributorId":32154,"corporation":false,"usgs":true,"family":"Blodgett","given":"J.","email":"","middleInitial":"C.","affiliations":[],"preferred":false,"id":236671,"contributorType":{"id":1,"text":"Authors"},"rank":1}]}} ,{"id":37634,"text":"tp67 - 1972 - Effects of water hardness on the toxicity of several organic and inorganic herbicides to fish","interactions":[],"lastModifiedDate":"2012-02-02T00:10:01","indexId":"tp67","displayToPublicDate":"1994-01-01T00:00:00","publicationYear":"1972","noYear":false,"publicationType":{"id":18,"text":"Report"},"publicationSubtype":{"id":1,"text":"Federal Government Series"},"seriesTitle":{"id":89,"text":"Technical Paper","active":false,"publicationSubtype":{"id":1}},"seriesNumber":"67","title":"Effects of water hardness on the toxicity of several organic and inorganic herbicides to fish","language":"ENGLISH","publisher":"U.S. Fish and Wildlife Service","usgsCitation":"Inglis, A., and Davis, E.L., 1972, Effects of water hardness on the toxicity of several organic and inorganic herbicides to fish: Technical Paper 67, 22 p. : ill. ; 26 cm.","productDescription":"22 p. : ill. ; 26 cm.","costCenters":[],"links":[{"id":161643,"rank":0,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/thumbnails/outside_thumb.jpg"}],"noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"4f4e4a26e4b07f02db60fbdc","contributors":{"authors":[{"text":"Inglis, Anthony","contributorId":41867,"corporation":false,"usgs":true,"family":"Inglis","given":"Anthony","email":"","affiliations":[],"preferred":false,"id":218374,"contributorType":{"id":1,"text":"Authors"},"rank":1},{"text":"Davis, Edward L.","contributorId":96735,"corporation":false,"usgs":true,"family":"Davis","given":"Edward","email":"","middleInitial":"L.","affiliations":[],"preferred":false,"id":218375,"contributorType":{"id":1,"text":"Authors"},"rank":2}]}} ,{"id":1382,"text":"wsp1532G - 1972 - Hydrology and effects of conservation structures, Willow Creek basin, Valley County, Montana, 1954-68","interactions":[],"lastModifiedDate":"2012-02-02T00:05:13","indexId":"wsp1532G","displayToPublicDate":"1994-01-01T00:00:00","publicationYear":"1972","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":"1532","chapter":"G","title":"Hydrology and effects of conservation structures, Willow Creek basin, Valley County, Montana, 1954-68","language":"ENGLISH","publisher":"U.S. Govt. 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Off.,","doi":"10.3133/wsp1532G","usgsCitation":"Frickel, D.G., 1972, Hydrology and effects of conservation structures, Willow Creek basin, Valley County, Montana, 1954-68: U.S. Geological Survey Water Supply Paper 1532, iv, G1-G34 p. :illus. ;24 cm., https://doi.org/10.3133/wsp1532G.","productDescription":"iv, G1-G34 p. :illus. ;24 cm.","costCenters":[],"links":[{"id":137365,"rank":0,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/wsp/1532g/report-thumb.jpg"},{"id":26485,"rank":300,"type":{"id":11,"text":"Document"},"url":"https://pubs.usgs.gov/wsp/1532g/report.pdf","linkFileType":{"id":1,"text":"pdf"}}],"noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"4f4e4a18e4b07f02db60516a","contributors":{"authors":[{"text":"Frickel, Donald G.","contributorId":23524,"corporation":false,"usgs":true,"family":"Frickel","given":"Donald","email":"","middleInitial":"G.","affiliations":[],"preferred":false,"id":143669,"contributorType":{"id":1,"text":"Authors"},"rank":1}]}} ,{"id":56760,"text":"wdrKY712 - 1972 - Water resources data for Kentucky, water year 1971; Part 2, Water quality records","interactions":[],"lastModifiedDate":"2012-02-02T00:11:48","indexId":"wdrKY712","displayToPublicDate":"1994-01-01T00:00:00","publicationYear":"1972","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":"KY-71-2","title":"Water resources data for Kentucky, water year 1971; Part 2, Water quality records","language":"ENGLISH","doi":"10.3133/wdrKY712","usgsCitation":"Water Resources Division, U.S. Geological Survey, 1972, Water resources data for Kentucky, water year 1971; Part 2, Water quality records: U.S. Geological Survey Water Data Report KY-71-2, 148 p., https://doi.org/10.3133/wdrKY712.","productDescription":"148 p.","costCenters":[],"links":[{"id":175278,"rank":0,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/thumbnails/usgs_thumb.jpg"}],"noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"4f4e4a82e4b07f02db64acd3","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":532876,"contributorType":{"id":1,"text":"Authors"},"rank":1}]}} ,{"id":56723,"text":"wdrWY711 - 1972 - Water resources data for Wyoming, water year 1971, part 1, surface water records","interactions":[],"lastModifiedDate":"2025-02-21T14:49:50.077247","indexId":"wdrWY711","displayToPublicDate":"1994-01-01T00:00:00","publicationYear":"1972","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":"WY-71-1","title":"Water resources data for Wyoming, water year 1971, part 1, surface water records","docAbstract":"Surface-water records for the 1971 water year for Wyoming, including records of streamflow or reservoir storage at gaging stations, partial-record stations, and miscellaneous sites, are given in this report. The locations of the gaging stations and partial-record stations are shown in figures 1 and 2. Records for a few pertinent gaging stations in bordering States also are included. The records were collected and computed by the Water Resources Division of the U.S. Geological Survey under the direction of Robert L. Cushman, district chief. These data represent that portion of the National Water Data System collected by the U.S. Geological Survey and cooperating State and Federal agencies in Wyoming.
Through September 30, 1960, the records of discharge and stage of streams and canals, 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.\"
Beginning with the 1961 water year, surface-water records have been released by the Geological Survey in annual reports on a State-boundary basis. Distribution of these reports is limited; they are designed primarily for rapid release of data shortly after the end of the water year to meet local needs. Records of discharge and reservoir storage for 1961-65 have been published in a Geological Survey water-supply paper series entitled \"Surface Water Supply of the United States 1961-65.\" Records of discharge and reservoir storage for 1966-70 also will be published in a Geological Survey water-supply paper series entitled \"Surface Water Supply of the United States 1966-70.\"
","language":"English","publisher":"U.S. Geological Survey","doi":"10.3133/wdrWY711","collaboration":"Prepared in cooperation with the State of Wyoming and with other agencies","usgsCitation":"Water Resources Division, U.S. Geological Survey, 1972, Water resources data for Wyoming, water year 1971, part 1, surface water records: U.S. Geological Survey Water Data Report WY-71-1, x, 262 p., https://doi.org/10.3133/wdrWY711.","productDescription":"x, 262 p.","costCenters":[],"links":[{"id":482270,"rank":2,"type":{"id":11,"text":"Document"},"url":"https://pubs.usgs.gov/wdr/1971/wy-71-1/report.pdf","linkFileType":{"id":1,"text":"pdf"}},{"id":180867,"rank":1,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/wdr/1971/wy-71-1/report-thumb.jpg"}],"country":"United 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\"}}]}","noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"4f4e4aa8e4b07f02db66755c","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":527852,"contributorType":{"id":1,"text":"Authors"},"rank":1}]}} ,{"id":48145,"text":"ofr73119 - 1972 - Generalized subsurface geology of the water-bearing deposits, northern San Joaquin Valley, California","interactions":[],"lastModifiedDate":"2022-01-11T21:22:31.788721","indexId":"ofr73119","displayToPublicDate":"1994-01-01T00:00:00","publicationYear":"1972","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":"73-119","title":"Generalized subsurface geology of the water-bearing deposits, northern San Joaquin Valley, California","docAbstract":"The study area includes about 5,000 square miles of the northern part of the San Joaquin Valley, a broad structural trough drained by the San Joaquin River. Fresh ground water is mostly in unconsolidated deposits derived from the Coast Ranges on the west and the Sierra Nevada on the east.. The interfingering of Coast Range and Sierran alluvium, together with the variability and lenticularity of each, causes variation in the hydrologic properties both vertically and horizontally in San Joaquin Valley deposits. A persistent confining stratum, the Corcoran Clay Member of the Tulare Formation, can be correlated through most of the study area. Informally, the deposits above the clay are termed the upper units the clay is termed the confining clay stratums and the deposits from the bottom of the clay to the base of fresh water, where known, are termed the lower unit. The upper unit is composed of beds, lenses, and tongues of gravel, sand, and clay ranging in thickness from about 100 feet in the north to 500 feet at the south end of the study area. A distinctive white clay, at or near the base of the upper unit, can be traced across the center of the valley. The confining clay stratum is the greenish to bluish gray lacustrine Corcoran Clay Member of the Tulare Formation; it ranges from 0 to 130 feet in thickness. No attempt to delineate the top and bottom of the Tulare Formation was made because of the thickness and similarity of deposits overlying and underlying the Corcoran. The lower unit is lithologically similar to the upper unit and ranges in thickness, where the base of fresh water has been mapped, from 90 to more than 1,400 feet.","language":"English","publisher":"U.S. Geological Survey","doi":"10.3133/ofr73119","usgsCitation":"Hotchkiss, W.R., 1972, Generalized subsurface geology of the water-bearing deposits, northern San Joaquin Valley, California: U.S. Geological Survey Open-File Report 73-119, iv, 18 p., https://doi.org/10.3133/ofr73119.","productDescription":"iv, 18 p.","costCenters":[],"links":[{"id":84851,"rank":300,"type":{"id":11,"text":"Document"},"url":"https://pubs.usgs.gov/of/1973/0119/report.pdf","linkFileType":{"id":1,"text":"pdf"}},{"id":162303,"rank":0,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/of/1973/0119/report-thumb.jpg"},{"id":394221,"rank":3,"type":{"id":36,"text":"NGMDB Index Page"},"url":"https://ngmdb.usgs.gov/Prodesc/proddesc_52127.htm"}],"country":"United States","state":"California","otherGeospatial":"northern San Joaquin Valley","geographicExtents":"{\n \"type\": \"FeatureCollection\",\n \"features\": [\n {\n \"type\": \"Feature\",\n \"properties\": {},\n \"geometry\": {\n \"type\": \"Polygon\",\n \"coordinates\": [\n [\n [\n -121.6083,\n 36.75\n ],\n [\n -120.1056,\n 36.75\n ],\n [\n -120.1056,\n 37.8711\n ],\n [\n -121.6083,\n 37.8711\n ],\n [\n -121.6083,\n 36.75\n ]\n ]\n ]\n }\n }\n ]\n}","noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"4f4e4b24e4b07f02db6aec64","contributors":{"authors":[{"text":"Hotchkiss, W. R.","contributorId":61820,"corporation":false,"usgs":true,"family":"Hotchkiss","given":"W.","email":"","middleInitial":"R.","affiliations":[],"preferred":false,"id":236870,"contributorType":{"id":1,"text":"Authors"},"rank":1}]}} ,{"id":68273,"text":"ha389 - 1972 - Ground water in Polk County, Nebraska","interactions":[],"lastModifiedDate":"2012-02-10T00:11:16","indexId":"ha389","displayToPublicDate":"1994-01-01T00:00:00","publicationYear":"1972","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":"389","title":"Ground water in Polk County, Nebraska","language":"ENGLISH","doi":"10.3133/ha389","usgsCitation":"Keech, C.F., 1972, Ground water in Polk County, Nebraska: U.S. Geological Survey Hydrologic Atlas 389, 1 map :col. ;on sheet 98 x 120 cm., https://doi.org/10.3133/ha389.","productDescription":"1 map :col. ;on sheet 98 x 120 cm.","costCenters":[],"links":[{"id":188557,"rank":0,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/thumbnails/usgs_thumb.jpg"},{"id":89679,"rank":400,"type":{"id":17,"text":"Plate"},"url":"https://pubs.usgs.gov/ha/389/plate-1.pdf","linkFileType":{"id":1,"text":"pdf"}}],"scale":"25000","geographicExtents":"{ \"type\": \"FeatureCollection\", \"features\": [ { \"type\": \"Feature\", \"properties\": {}, \"geometry\": { \"type\": \"Polygon\", \"coordinates\": [ [ [ -97.75,41 ], [ -97.75,41.416666666666664 ], [ -97.5,41.416666666666664 ], [ -97.5,41 ], [ -97.75,41 ] ] ] } } ] }","noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"4f4e4ab0e4b07f02db66daba","contributors":{"authors":[{"text":"Keech, Charles Franklin","contributorId":44123,"corporation":false,"usgs":true,"family":"Keech","given":"Charles","email":"","middleInitial":"Franklin","affiliations":[],"preferred":false,"id":277948,"contributorType":{"id":1,"text":"Authors"},"rank":1}]}} ,{"id":1786,"text":"wsp1999I - 1972 - Water for cranberry culture in the Cranmoor area of central Wisconsin","interactions":[],"lastModifiedDate":"2015-10-02T13:26:50","indexId":"wsp1999I","displayToPublicDate":"1994-01-01T00:00:00","publicationYear":"1972","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":"1999","chapter":"I","title":"Water for cranberry culture in the Cranmoor area of central Wisconsin","docAbstract":"The Cranmoor area of central Wisconsin is the principal cranberry producing area of the State. Cranberries are grown in only about 2.5 square miles of an 80-square-mile marsh and swamp in the Cranberry Creek basin. Cranberry growers have built reservoirs and ditches throughout 25 square miles of marsh for better management of the area's natural water supply. Additional water is diverted into the basin to supplement the cranberry needs. In the 1966-67 hydrologic budget for Cranberry Creek basin, annual inputs were 27.8 inches of precipitation, 3.8 inches of surface-water diversion into the basin, and 1.1 inches decrease in stored water. Annual outputs were. 20.8 inches of evapotranspiration, 11.7 inches of runoff, and 0.2 inch of groundwater outflow. During the 1966-67 period, precipitation averaged about 3 inches per year below normal. The water used for cranberry culture is almost exclusively surface water. Efficient management of the basin's water supply, plus intermittent diversions of about 100 cubic feet per second from outside the basin, provide cranberry growers with a sufficient quantity of water. Although the quantity of surface water is adequate, the pH (generally 5.7-6.7) is slightly high for optimum use. Dissolved oxygen is slightly low, generally between 4 and 10 milligrams per liter. The water is soft; iron and manganese contents vary seasonally, being high in winter and summer and low in spring. Additional supplies of surface water can be obtained by increasing diversions from outside the basin and by increasing reservoir capacity within the basin. Ground water, although not presently used for cranberries, is available in the central, southern, and eastern parts of the basin, where the thickness of the saturated alluvium exceeds 50 feet. Well yields in these areas might be as much as 1,000 gpm (gallons per minute). Additionally, well yields of as much as 1,000 gpm may be expected from saturated alluvium southeast of Cranberry Creek basin. Where saturated alluvium is less than 50 feet thick, in the northern and western parts of the basin, well yields generally are less than 50 gpm. Ground water is also available from sandstone in the western part of the basin. Where the sandstone is thickest (about 60 ft.), well yields may be as much as 200 gpm. The quality of ground water is similar to that of surface water. The pH of water from the shallow alluvium ranges between 6.0 and 6,6; the pH of water from the deep alluvium is about 7.0. Ground water is soft to moderately hard, 22 to 88 milligrams per liter, and contains excessive amounts of iron and manganese.
","largerWorkType":{"id":18,"text":"Report"},"largerWorkTitle":"Contributions to the hydrology of the United States","largerWorkSubtype":{"id":5,"text":"USGS Numbered Series"},"language":"English","publisher":"U.S. Geological Survey","doi":"10.3133/wsp1999I","collaboration":"Prepared in cooperation with University Extension-the University of Wisconsin Geological and Natural History Survey","usgsCitation":"Hamilton, L.J., 1972, Water for cranberry culture in the Cranmoor area of central Wisconsin: U.S. Geological Survey Water Supply Paper 1999, Report: iii, 20 p.; 2 Plates: 34.50 x 24.00 inches and 17.00 x 27.00 inches, https://doi.org/10.3133/wsp1999I.","productDescription":"Report: iii, 20 p.; 2 Plates: 34.50 x 24.00 inches and 17.00 x 27.00 inches","numberOfPages":"26","onlineOnly":"N","additionalOnlineFiles":"Y","costCenters":[{"id":677,"text":"Wisconsin Water Science Center","active":true,"usgs":true}],"links":[{"id":138497,"rank":0,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/wsp/1999i/report-thumb.jpg"},{"id":26922,"rank":401,"type":{"id":17,"text":"Plate"},"url":"https://pubs.usgs.gov/wsp/1999i/plate-2.pdf","linkFileType":{"id":1,"text":"pdf"}},{"id":26923,"rank":300,"type":{"id":11,"text":"Document"},"url":"https://pubs.usgs.gov/wsp/1999i/report.pdf","linkFileType":{"id":1,"text":"pdf"}},{"id":26921,"rank":400,"type":{"id":17,"text":"Plate"},"url":"https://pubs.usgs.gov/wsp/1999i/plate-1.pdf","linkFileType":{"id":1,"text":"pdf"}}],"country":"United States","state":"Wisconsin","city":"Cranmoor","geographicExtents":"{\n \"type\": \"FeatureCollection\",\n \"features\": [\n {\n \"type\": \"Feature\",\n \"properties\": {},\n \"geometry\": {\n \"type\": \"Polygon\",\n \"coordinates\": [\n [\n [\n -90.3131103515625,\n 44.50825885600572\n ],\n [\n -90.450439453125,\n 44.308126684886126\n ],\n [\n -90.3570556640625,\n 44.05601169578525\n ],\n [\n -90.164794921875,\n 44.07969327425713\n ],\n [\n -90.02197265625,\n 44.24126379833979\n ],\n [\n -89.9615478515625,\n 44.296332880058706\n ],\n [\n -89.9176025390625,\n 44.37098696297173\n ],\n [\n -89.945068359375,\n 44.46123053905882\n ],\n [\n -90.0164794921875,\n 44.53175879707938\n ],\n [\n -90.142822265625,\n 44.57873024377564\n ],\n [\n -90.3131103515625,\n 44.50825885600572\n ]\n ]\n ]\n }\n }\n ]\n}","noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"4f4e48d1e4b07f02db547e08","contributors":{"authors":[{"text":"Hamilton, Louis J.","contributorId":53768,"corporation":false,"usgs":true,"family":"Hamilton","given":"Louis","email":"","middleInitial":"J.","affiliations":[],"preferred":false,"id":144154,"contributorType":{"id":1,"text":"Authors"},"rank":1}]}} ,{"id":1385,"text":"wsp1985 - 1972 - Ground-water resources of Orange and Ulster Counties, New York","interactions":[{"subject":{"id":55900,"text":"ofr6997 - 1969 - Ground-water basic data for Orange and Ulster Counties, New York","indexId":"ofr6997","publicationYear":"1969","noYear":false,"title":"Ground-water basic data for Orange and Ulster Counties, New York"},"predicate":"SUPERSEDED_BY","object":{"id":1385,"text":"wsp1985 - 1972 - Ground-water resources of Orange and Ulster Counties, New York","indexId":"wsp1985","publicationYear":"1972","noYear":false,"title":"Ground-water resources of Orange and Ulster Counties, New York"},"id":1}],"lastModifiedDate":"2012-02-02T00:05:13","indexId":"wsp1985","displayToPublicDate":"1994-01-01T00:00:00","publicationYear":"1972","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":"1985","title":"Ground-water resources of Orange and Ulster Counties, New York","language":"ENGLISH","publisher":"U.S. Govt. 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","language":"English","doi":"10.3133/ofr72416","usgsCitation":"Water Resources Division, U.S. Geological Survey, and Lucchitta, B.K., 1972, Preliminary geologic terrain map of Mars: U.S. Geological Survey Open-File Report 72-416, 1 map on 2 sheets, https://doi.org/10.3133/ofr72416.","productDescription":"1 map on 2 sheets","costCenters":[],"links":[{"id":136490,"rank":0,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/thumbnails/usgs_thumb.jpg"}],"scale":"25000000","noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"4f4e4abde4b07f02db673ec5","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":530938,"contributorType":{"id":1,"text":"Authors"},"rank":1},{"text":"Lucchitta, Baerbel K. blucchitta@usgs.gov","contributorId":3649,"corporation":false,"usgs":true,"family":"Lucchitta","given":"Baerbel","email":"blucchitta@usgs.gov","middleInitial":"K.","affiliations":[],"preferred":true,"id":749374,"contributorType":{"id":1,"text":"Authors"},"rank":2}]}} ,{"id":41690,"text":"ofr72386 - 1972 - Aeromagnetic map of parts of the Lovelock, Reno, and Millett 1° by 2° quadrangles, Nevada","interactions":[],"lastModifiedDate":"2021-11-30T20:24:20.293193","indexId":"ofr72386","displayToPublicDate":"1994-01-01T00:00:00","publicationYear":"1972","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":"72-386","title":"Aeromagnetic map of parts of the Lovelock, Reno, and Millett 1° by 2° quadrangles, Nevada","docAbstract":"No abstract available.
","language":"English","publisher":"U.S. Geological Survey","doi":"10.3133/ofr72386","usgsCitation":"Water Resources Division, U.S. Geological Survey, 1972, Aeromagnetic map of parts of the Lovelock, Reno, and Millett 1° by 2° quadrangles, Nevada: U.S. Geological Survey Open-File Report 72-386, 1 Plate: 52.00 × 42.00 inches, https://doi.org/10.3133/ofr72386.","productDescription":"1 Plate: 52.00 × 42.00 inches","costCenters":[],"links":[{"id":173676,"rank":0,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/thumbnails/usgs_thumb.jpg"},{"id":98585,"rank":400,"type":{"id":17,"text":"Plate"},"url":"https://pubs.usgs.gov/of/1972/0386/plate-1.pdf","linkFileType":{"id":1,"text":"pdf"}},{"id":392265,"rank":3,"type":{"id":36,"text":"NGMDB Index Page"},"url":"https://ngmdb.usgs.gov/Prodesc/proddesc_8718.htm"}],"country":"United States","state":"Nevada","otherGeospatial":"Lovelock, Reno, and Millett 1° by 2° quadrangles","geographicExtents":"{\n \"type\": \"FeatureCollection\",\n \"features\": [\n {\n \"type\": \"Feature\",\n \"properties\": {},\n \"geometry\": {\n \"type\": \"Polygon\",\n \"coordinates\": [\n [\n [\n -120,\n 39.25\n ],\n [\n -116.5,\n 39.25\n ],\n [\n -116.5,\n 41\n ],\n [\n -120,\n 41\n ],\n [\n -120,\n 39.25\n ]\n ]\n ]\n }\n }\n ]\n}","noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"4f4e4afee4b07f02db697560","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":530570,"contributorType":{"id":1,"text":"Authors"},"rank":1}]}} ,{"id":64045,"text":"gp833 - 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1972 - Aeromagnetic map of the Bergland quadrangle and part of the White Pine quadrangle, Ontonagon and Gogebic Counties, Michigan","interactions":[{"subject":{"id":42183,"text":"ofr648 - 1964 - Aeromagnetic map of the Bergland and part of the White Pine quadrangles, Ontonagon and Gogebic Counties, Michigan","indexId":"ofr648","publicationYear":"1964","noYear":false,"title":"Aeromagnetic map of the Bergland and part of the White Pine quadrangles, Ontonagon and Gogebic Counties, Michigan"},"predicate":"SUPERSEDED_BY","object":{"id":63981,"text":"gp829 - 1972 - Aeromagnetic map of the Bergland quadrangle and part of the White Pine quadrangle, Ontonagon and Gogebic Counties, Michigan","indexId":"gp829","publicationYear":"1972","noYear":false,"title":"Aeromagnetic map of the Bergland quadrangle and part of the White Pine quadrangle, Ontonagon and Gogebic Counties, Michigan"},"id":1}],"lastModifiedDate":"2012-02-10T00:10:54","indexId":"gp829","displayToPublicDate":"1994-01-01T00:00:00","publicationYear":"1972","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":"829","title":"Aeromagnetic map of the Bergland quadrangle and part of the White Pine quadrangle, Ontonagon and Gogebic Counties, Michigan","language":"ENGLISH","doi":"10.3133/gp829","usgsCitation":"Water Resources Division, U.S. Geological Survey, 1972, Aeromagnetic map of the Bergland quadrangle and part of the White Pine quadrangle, Ontonagon and Gogebic Counties, Michigan: U.S. Geological Survey Geophysical Investigations Map 829, 1 map on two sheets., https://doi.org/10.3133/gp829.","productDescription":"1 map on two sheets.","costCenters":[],"links":[{"id":250362,"rank":300,"type":{"id":11,"text":"Document"},"url":"https://pubs.usgs.gov/gp/0829/report.pdf","size":"46","linkFileType":{"id":1,"text":"pdf"}},{"id":250363,"rank":400,"type":{"id":17,"text":"Plate"},"url":"https://pubs.usgs.gov/gp/0829/plate-1.pdf","size":"3264","linkFileType":{"id":1,"text":"pdf"}},{"id":253829,"rank":0,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/gp/0829/report-thumb.jpg"}],"scale":"62500","geographicExtents":"{ \"type\": \"FeatureCollection\", \"features\": [ { \"type\": \"Feature\", \"properties\": {}, \"geometry\": { \"type\": \"Polygon\", \"coordinates\": [ [ [ -89.75,46.5 ], [ -89.75,46.833333333333336 ], [ -89.5,46.833333333333336 ], [ -89.5,46.5 ], [ -89.75,46.5 ] ] ] } } ] }","noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"4f4e4afde4b07f02db697141","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":533450,"contributorType":{"id":1,"text":"Authors"},"rank":1}]}} ,{"id":56309,"text":"wdrME711 - 1972 - Water resources data for Maine, water year 1971","interactions":[],"lastModifiedDate":"2025-08-19T13:54:39.325036","indexId":"wdrME711","displayToPublicDate":"1994-01-01T00:00:00","publicationYear":"1972","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":"ME-71-1","title":"Water resources data for Maine, water year 1971","docAbstract":"Water resources data for the 1971 water year for Maine including records of streamflow or reservoir storage at gaging stations, partial-record stations, and miscellaneous sites, records of water-quality data on the chemical and physical characteristics of surface- and ground-water, and records of ground-water levels in index wells are given in this report. Records for a few pertinent gaging stations in bordering States and Provinces are also included. The records were collected and computed by the Water Resources Division of the U.S. Geological Survey under the direction of G. S. Hayes, District Chief. These data represent that portion of the National Water Data System collected by the U.S. Geological Survey and cooperating State and Federal agencies in Maine.
","language":"English","publisher":"U.S. Geological Survey","doi":"10.3133/wdrME711","usgsCitation":"Water Resources Division, U.S. Geological Survey, 1972, Water resources data for Maine, water year 1971: U.S. Geological Survey Water Data Report ME-71-1, vi, 112 p., https://doi.org/10.3133/wdrME711.","productDescription":"vi, 112 p.","costCenters":[],"links":[{"id":181429,"rank":1,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/wdr/1971/me-71-1/report-thumb.jpg"},{"id":494297,"rank":2,"type":{"id":11,"text":"Document"},"url":"https://pubs.usgs.gov/wdr/1971/me-71-1/report.pdf","linkFileType":{"id":1,"text":"pdf"}}],"country":"United 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