The sand-and-gravel aquifer in southern Okaloosa and Walton Counties, northwest Florida, extends from land surface to depth of 50 to 150 feet. Intervening layers of clay generally separate the aquifer into an unconfined surficial zone, composed principally of fine to medium sand, and a lower confined zone, consisting of variable amounts of medium to coarse sand and gravel. Well yields of 50 to 500 gallons per minute are possible in most of the area, and yields of 500 to 1,000 gallons per minute can be developed in parts of southwestern Okaloosa County.
","language":"English","publisher":"U.S. Geological Survey","doi":"10.3133/wri824110","usgsCitation":"Hayes, L.R., and Barr, D.E., 1982, Hydrology of the sand-and-gravel aquifer, southern Okaloosa and Walton Counties, northwest Florida: U.S. Geological Survey Water-Resources Investigations Report 82-4110, vi, 49 p., https://doi.org/10.3133/wri824110.","productDescription":"vi, 49 p.","costCenters":[],"links":[{"id":158870,"rank":0,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/wri/1982/4110/report-thumb.jpg"},{"id":56467,"rank":300,"type":{"id":11,"text":"Document"},"url":"https://pubs.usgs.gov/wri/1982/4110/report.pdf","linkFileType":{"id":1,"text":"pdf"}},{"id":396266,"rank":3,"type":{"id":36,"text":"NGMDB Index Page"},"url":"https://ngmdb.usgs.gov/Prodesc/proddesc_35617.htm"}],"country":"United States","state":"Florida","county":"Okaloosa County, Walton County","geographicExtents":"{\n \"type\": \"FeatureCollection\",\n \"features\": [\n {\n \"type\": \"Feature\",\n \"properties\": {},\n \"geometry\": {\n \"type\": \"Polygon\",\n \"coordinates\": [\n [\n [\n -86.70135498046875,\n 30.379983796443767\n ],\n [\n -86.19873046875,\n 30.379983796443767\n ],\n [\n -86.19873046875,\n 30.590637026892917\n ],\n [\n -86.70135498046875,\n 30.590637026892917\n ],\n [\n -86.70135498046875,\n 30.379983796443767\n ]\n ]\n ]\n }\n }\n ]\n}","noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"4f4e4a0ce4b07f02db5fc79d","contributors":{"authors":[{"text":"Hayes, L. R.","contributorId":50931,"corporation":false,"usgs":true,"family":"Hayes","given":"L.","email":"","middleInitial":"R.","affiliations":[],"preferred":false,"id":198387,"contributorType":{"id":1,"text":"Authors"},"rank":1},{"text":"Barr, D. E.","contributorId":55469,"corporation":false,"usgs":true,"family":"Barr","given":"D.","email":"","middleInitial":"E.","affiliations":[],"preferred":false,"id":198388,"contributorType":{"id":1,"text":"Authors"},"rank":2}]}} ,{"id":26400,"text":"wri8245 - 1982 - Delineation and hydrologic effects of a gasoline leak at Stovepipe Wells Hotel, Death Valley National Monument, California","interactions":[],"lastModifiedDate":"2019-08-05T11:21:19","indexId":"wri8245","displayToPublicDate":"1994-01-01T00:00:00","publicationYear":"1982","noYear":false,"publicationType":{"id":18,"text":"Report"},"publicationSubtype":{"id":5,"text":"USGS Numbered Series"},"seriesTitle":{"id":342,"text":"Water-Resources Investigations Report","code":"WRI","active":false,"publicationSubtype":{"id":5}},"seriesNumber":"82-45","title":"Delineation and hydrologic effects of a gasoline leak at Stovepipe Wells Hotel, Death Valley National Monument, California","docAbstract":"Ground water is the only local source of water available to the Stovepipe Wells Hotel facilities of the Death Valley National Monument, California. A leak in a service station storage tank caused the formation of a gasoline layer overlying the water table, creating the potential for contamination of the water supply. The maximum horizontal extent of the gasoline layer was mathematically estimated to be 1,300 feet downgradient from the leaky gasoline tank. Exploratory drilling detected the gasoline layer between 900 and 1,400 feet downgradient and between 50 and 150 feet upgradient from the source. Traces of the soluble components of gasoline were also found in the aquifer 150 feet upgradient, and 250 feet distant from the source perpendicular to the direction of ground-water movement. The gasoline spill is not likely to have an effect on the supply wells located 0.4 mile south of the leak source, which is nearly perpendicular to the direction of ground-water movement and the primary direction of gasoline movement in the area. No effect on phreatophytes 2 miles downgradient from the layer is likely, but the potential effects of gasoline vapors within the unsaturated zone on local xerophytes are not known. (USGS)","language":"English","publisher":"U.S. Geological Survey","publisherLocation":"Reston, VA","doi":"10.3133/wri8245","usgsCitation":"Buono, A., and Packard, E.M., 1982, Delineation and hydrologic effects of a gasoline leak at Stovepipe Wells Hotel, Death Valley National Monument, California: U.S. Geological Survey Water-Resources Investigations Report 82-45, iv, 23 p. , https://doi.org/10.3133/wri8245.","productDescription":"iv, 23 p. ","costCenters":[],"links":[{"id":157879,"rank":0,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/wri/1982/0045/report-thumb.jpg"},{"id":366241,"rank":2,"type":{"id":11,"text":"Document"},"url":"https://pubs.usgs.gov/wri/1982/0045/report.pdf","linkFileType":{"id":1,"text":"pdf"}}],"country":"United States","state":"California","otherGeospatial":"Death Valley National Monument","geographicExtents":"{\n \"type\": \"FeatureCollection\",\n \"features\": [\n {\n \"type\": \"Feature\",\n \"properties\": {},\n \"geometry\": {\n \"type\": \"Polygon\",\n \"coordinates\": [\n [\n [\n -117.14996337890625,\n 36.605055259475584\n ],\n [\n -117.14275360107422,\n 36.605055259475584\n ],\n [\n -117.14275360107422,\n 36.60774238525424\n ],\n [\n -117.14996337890625,\n 36.60774238525424\n ],\n [\n -117.14996337890625,\n 36.605055259475584\n ]\n ]\n ]\n }\n }\n ]\n}","noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"4f4e4abae4b07f02db671cbe","contributors":{"authors":[{"text":"Buono, A.","contributorId":61034,"corporation":false,"usgs":true,"family":"Buono","given":"A.","email":"","affiliations":[],"preferred":false,"id":196323,"contributorType":{"id":1,"text":"Authors"},"rank":1},{"text":"Packard, Elaine M.","contributorId":99593,"corporation":false,"usgs":true,"family":"Packard","given":"Elaine","email":"","middleInitial":"M.","affiliations":[],"preferred":false,"id":196324,"contributorType":{"id":1,"text":"Authors"},"rank":2}]}} ,{"id":27657,"text":"wri824019 - 1982 - Model modifications for simulation of flow through stratified rocks in eastern Ohio","interactions":[],"lastModifiedDate":"2012-02-02T00:08:37","indexId":"wri824019","displayToPublicDate":"1994-01-01T00:00:00","publicationYear":"1982","noYear":false,"publicationType":{"id":18,"text":"Report"},"publicationSubtype":{"id":5,"text":"USGS Numbered Series"},"seriesTitle":{"id":342,"text":"Water-Resources Investigations Report","code":"WRI","active":false,"publicationSubtype":{"id":5}},"seriesNumber":"82-4019","title":"Model modifications for simulation of flow through stratified rocks in eastern Ohio","docAbstract":"A quasi three-dimensional groundwater flow model is being used as part of a study to determine impacts of coal-strip mining on local hydrologic systems. Modifications to the model were necessary to simulate local hydrologic conditions properly. Perched water tables required that the method of calculating vertical flow rate be changed. A head-dependent spring-discharge function and a head-dependent stream aquifer-interchange function were added to the program. Modifications were also made to allow recharge from precipitation to any layer. The modified program, data deck instructions, and sample input and output are presented. (USGS)","language":"ENGLISH","publisher":"U.S. Geological Survey,","doi":"10.3133/wri824019","usgsCitation":"Helgesen, J.O., Razem, A., and Larson, S.P., 1982, Model modifications for simulation of flow through stratified rocks in eastern Ohio: U.S. Geological Survey Water-Resources Investigations Report 82-4019, iv, 113 p. :ill. ;28 cm., https://doi.org/10.3133/wri824019.","productDescription":"iv, 113 p. :ill. ;28 cm.","costCenters":[],"links":[{"id":122914,"rank":0,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/wri/1982/4019/report-thumb.jpg"},{"id":56512,"rank":300,"type":{"id":11,"text":"Document"},"url":"https://pubs.usgs.gov/wri/1982/4019/report.pdf","linkFileType":{"id":1,"text":"pdf"}}],"noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"4f4e4b05e4b07f02db699a2f","contributors":{"authors":[{"text":"Helgesen, J. O.","contributorId":62600,"corporation":false,"usgs":true,"family":"Helgesen","given":"J.","email":"","middleInitial":"O.","affiliations":[],"preferred":false,"id":198482,"contributorType":{"id":1,"text":"Authors"},"rank":1},{"text":"Razem, A. C.","contributorId":34924,"corporation":false,"usgs":true,"family":"Razem","given":"A. C.","affiliations":[],"preferred":false,"id":198481,"contributorType":{"id":1,"text":"Authors"},"rank":2},{"text":"Larson, S. P.","contributorId":34903,"corporation":false,"usgs":true,"family":"Larson","given":"S.","email":"","middleInitial":"P.","affiliations":[],"preferred":false,"id":198480,"contributorType":{"id":1,"text":"Authors"},"rank":3}]}} ,{"id":27457,"text":"wri8244 - 1982 - Preliminary evaluation of the ground-water-flow system in the Twin Cities Metropolitan area, Minnesota","interactions":[],"lastModifiedDate":"2018-03-12T11:43:11","indexId":"wri8244","displayToPublicDate":"1994-01-01T00:00:00","publicationYear":"1982","noYear":false,"publicationType":{"id":18,"text":"Report"},"publicationSubtype":{"id":5,"text":"USGS Numbered Series"},"seriesTitle":{"id":342,"text":"Water-Resources Investigations Report","code":"WRI","active":false,"publicationSubtype":{"id":5}},"seriesNumber":"82-44","title":"Preliminary evaluation of the ground-water-flow system in the Twin Cities Metropolitan area, Minnesota","docAbstract":"A preliminary quasi-three-dimensional finite-difference ground-water-flow model of the seven-county Twin Cities Metropolitan area was constructed and used to evaluate parameter sensitivity and adequacy of available data. Fourteen geologic units that underlie the study area were grouped into nine hydr,bgeologic units and were incorporated into a five-layer model. The layers in the simulation model include the Mount SimonHinckley, Ironton-Galesville, Prairie du Chien-Jordan, and St. Peter aquifers, and the drift.
\nSensitivity analyses were made for 19 parameter and boundary-condition specifications. Model results are -most sensitive to recharge and withdrawal rates and to hydrogeologic variations related to drift-filled bedrock valleys. Analyses of available data and results of steady-state simulations indicate that critical data needs for improving the simulation model include spatial and temporal variations in ground-water withdrawals and potentiometric levels, and hydraulic properties of drift filling or partly filling bedrock valleys.
\nAreal distribution of calcium, sodium, sulfate, and chloride concentrations were analyzed to provide information on the hydrologic and geochemical relationships between aquifers. Ground water is generally of the calcium magnesium bicarbonate type. Concentration of dissolved solids in water from the Jordan Sandstone and Mount Simon-Hinckley aquifer generally decreases from southwest to northeast across the study area. This decrease probably reflects differences in the quality of recharge water and geochemical processes within the aquifers, such as ion exchange.
","language":"English","publisher":"U.S. Geological Survey","publisherLocation":"St. Paul, MN","doi":"10.3133/wri8244","collaboration":"Prepared in cooperation with the Metropolitan Council of the Twin Cities, Minnesota Department of Natural Resources, Minnesota Geological Survey","usgsCitation":"Guswa, J.H., Siegel, D., and Gillies, D.C., 1982, Preliminary evaluation of the ground-water-flow system in the Twin Cities Metropolitan area, Minnesota: U.S. Geological Survey Water-Resources Investigations Report 82-44, v, 65 p., https://doi.org/10.3133/wri8244.","productDescription":"v, 65 p.","onlineOnly":"N","additionalOnlineFiles":"N","costCenters":[{"id":392,"text":"Minnesota Water Science Center","active":true,"usgs":true}],"links":[{"id":157946,"rank":0,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/wri/1982/0044/report-thumb.jpg"},{"id":95634,"rank":300,"type":{"id":11,"text":"Document"},"url":"https://pubs.usgs.gov/wri/1982/0044/report.pdf","size":"7263","linkFileType":{"id":1,"text":"pdf"}}],"country":"United States","state":"Minnesota","otherGeospatial":"Twin Cites Metropolitan area","geographicExtents":"{\"type\":\"FeatureCollection\",\"features\":[{\"type\":\"Feature\",\"geometry\":{\"type\":\"Polygon\",\"coordinates\":[[[-93.5093,45.4163],[-93.1289,45.4153],[-93.0186,45.4131],[-93.0188,45.2984],[-92.7894,45.297],[-92.7439,45.2963],[-92.7516,45.2935],[-92.7551,45.2927],[-92.7583,45.2904],[-92.7597,45.2872],[-92.7604,45.2845],[-92.7591,45.2794],[-92.7559,45.2739],[-92.7527,45.2694],[-92.7515,45.2657],[-92.7526,45.2626],[-92.7535,45.2584],[-92.7561,45.2541],[-92.7575,45.2502],[-92.7569,45.2443],[-92.7557,45.2397],[-92.7553,45.2356],[-92.7538,45.2305],[-92.7536,45.2276],[-92.7521,45.2236],[-92.752,45.2196],[-92.7527,45.2168],[-92.7546,45.2136],[-92.7573,45.2107],[-92.7603,45.2065],[-92.7619,45.2041],[-92.7632,45.2009],[-92.7637,45.1972],[-92.764,45.1895],[-92.7629,45.1853],[-92.7557,45.178],[-92.7522,45.1759],[-92.7493,45.173],[-92.748,45.1698],[-92.7472,45.1634],[-92.7483,45.1597],[-92.7475,45.1551],[-92.7473,45.1515],[-92.7484,45.1483],[-92.749,45.1419],[-92.7484,45.1373],[-92.7441,45.1264],[-92.7415,45.1172],[-92.7422,45.1135],[-92.7446,45.11],[-92.7467,45.1076],[-92.7513,45.1045],[-92.7591,45.0999],[-92.7624,45.0972],[-92.7803,45.0849],[-92.7847,45.083],[-92.7885,45.0806],[-92.7917,45.0791],[-92.795,45.0772],[-92.7982,45.0746],[-92.8001,45.0723],[-92.8019,45.0647],[-92.8016,45.0597],[-92.8005,45.0567],[-92.7984,45.0531],[-92.7952,45.0499],[-92.7926,45.0481],[-92.7881,45.0453],[-92.7837,45.0421],[-92.7745,45.0373],[-92.7707,45.0344],[-92.7683,45.0325],[-92.7645,45.0265],[-92.7639,45.0237],[-92.7639,45.0196],[-92.7682,45.0005],[-92.7694,44.9909],[-92.7686,44.9796],[-92.7646,44.9711],[-92.7547,44.9571],[-92.7527,44.9527],[-92.7523,44.9481],[-92.753,44.9369],[-92.7534,44.9237],[-92.7547,44.9159],[-92.7569,44.9105],[-92.7606,44.9068],[-92.7645,44.9046],[-92.767,44.9039],[-92.7707,44.9023],[-92.7729,44.901],[-92.775,44.8982],[-92.7738,44.8933],[-92.7689,44.8848],[-92.7632,44.8759],[-92.7628,44.8716],[-92.763,44.8671],[-92.7644,44.8622],[-92.7682,44.8554],[-92.7683,44.853],[-92.7671,44.8494],[-92.7652,44.8462],[-92.7646,44.8423],[-92.7644,44.8382],[-92.766,44.8308],[-92.7679,44.8265],[-92.7719,44.8211],[-92.7751,44.8161],[-92.7784,44.8125],[-92.7801,44.8095],[-92.781,44.8056],[-92.7823,44.8029],[-92.783,44.7966],[-92.7858,44.7893],[-92.7909,44.7842],[-92.7993,44.7765],[-92.802,44.7729],[-92.8046,44.7683],[-92.8059,44.7624],[-92.8073,44.7524],[-92.8061,44.7483],[-92.8054,44.7473],[-92.8022,44.7446],[-92.7901,44.7381],[-92.7805,44.7344],[-92.7722,44.7317],[-92.7658,44.7289],[-92.7569,44.7234],[-92.7536,44.7226],[-92.7471,44.7204],[-92.7415,44.7192],[-92.7339,44.7157],[-92.737,44.658],[-92.7386,44.6329],[-92.7957,44.6305],[-92.7915,44.5452],[-92.9165,44.5449],[-92.9179,44.5221],[-92.9218,44.518],[-92.9282,44.5158],[-92.9321,44.513],[-92.941,44.5149],[-92.9449,44.5131],[-92.9494,44.5104],[-92.9584,44.514],[-92.9634,44.5177],[-92.975,44.5159],[-92.9827,44.5173],[-92.991,44.5215],[-93.0057,44.5197],[-93.0121,44.5175],[-93.0166,44.5166],[-93.0275,44.5198],[-93.0301,44.5148],[-93.0346,44.5148],[-93.039,44.5171],[-93.0406,44.4729],[-93.2826,44.473],[-93.2798,44.546],[-93.5259,44.5466],[-93.9091,44.5446],[-93.9117,44.5492],[-93.9078,44.5528],[-93.9027,44.5524],[-93.9008,44.5492],[-93.8956,44.5483],[-93.8937,44.5515],[-93.8963,44.5561],[-93.9008,44.5606],[-93.8996,44.5647],[-93.8957,44.5675],[-93.8958,44.5711],[-93.8996,44.5743],[-93.8958,44.5775],[-93.8939,44.5807],[-93.8959,44.5871],[-93.8991,44.5903],[-93.8908,44.5962],[-93.8857,44.5967],[-93.8838,44.6012],[-93.878,44.6013],[-93.878,44.6077],[-93.8716,44.6063],[-93.8658,44.6063],[-93.8569,44.6168],[-93.8563,44.6218],[-93.8505,44.6219],[-93.8447,44.6201],[-93.8422,44.6233],[-93.8358,44.6242],[-93.8319,44.6251],[-93.8217,44.6297],[-93.8031,44.6366],[-93.7999,44.6361],[-93.7967,44.6343],[-93.7935,44.6311],[-93.7883,44.632],[-93.78,44.6362],[-93.7768,44.6385],[-93.7729,44.6366],[-93.7723,44.6325],[-93.7691,44.6312],[-93.7665,44.6362],[-93.7685,44.6417],[-93.7686,44.675],[-93.8887,44.6756],[-93.8902,44.7185],[-94.0104,44.719],[-94.0085,44.8947],[-94.0136,44.8951],[-94.0117,44.9796],[-93.7692,44.9789],[-93.7702,45.0734],[-93.7663,45.077],[-93.7631,45.0839],[-93.7534,45.0853],[-93.7399,45.0894],[-93.7341,45.0922],[-93.7322,45.0963],[-93.7257,45.1022],[-93.7225,45.11],[-93.72,45.1205],[-93.7155,45.1269],[-93.7019,45.1374],[-93.6852,45.1489],[-93.6793,45.1525],[-93.6716,45.1562],[-93.6574,45.1585],[-93.6554,45.1599],[-93.6529,45.1631],[-93.6503,45.169],[-93.6516,45.1841],[-93.6549,45.1905],[-93.6555,45.1969],[-93.6562,45.201],[-93.6471,45.2079],[-93.6387,45.2074],[-93.6361,45.206],[-93.6329,45.2056],[-93.6258,45.2092],[-93.6167,45.2115],[-93.6096,45.2111],[-93.6031,45.2111],[-93.5967,45.2134],[-93.5857,45.2189],[-93.5792,45.2189],[-93.5734,45.2202],[-93.5676,45.2225],[-93.5617,45.2289],[-93.554,45.2298],[-93.5462,45.2289],[-93.5371,45.2294],[-93.5332,45.2317],[-93.5197,45.2417],[-93.5158,45.2458],[-93.5138,45.2454],[-93.5093,45.4163]]]},\"properties\":{\"name\":\"Anoka\",\"state\":\"MN\"}}]}","noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"4f4e4ac9e4b07f02db67c39c","contributors":{"authors":[{"text":"Guswa, John H.","contributorId":97881,"corporation":false,"usgs":true,"family":"Guswa","given":"John","email":"","middleInitial":"H.","affiliations":[],"preferred":false,"id":198151,"contributorType":{"id":1,"text":"Authors"},"rank":1},{"text":"Siegel, Donald I.","contributorId":97499,"corporation":false,"usgs":true,"family":"Siegel","given":"Donald I.","affiliations":[],"preferred":false,"id":198150,"contributorType":{"id":1,"text":"Authors"},"rank":2},{"text":"Gillies, Daniel C.","contributorId":39824,"corporation":false,"usgs":true,"family":"Gillies","given":"Daniel","email":"","middleInitial":"C.","affiliations":[],"preferred":false,"id":198149,"contributorType":{"id":1,"text":"Authors"},"rank":3}]}} ,{"id":25667,"text":"wri8250 - 1982 - Methodology for hydrologic evaluation of a potential surface mine: Loblolly Branch basin, Tuscaloosa County, Alabama","interactions":[],"lastModifiedDate":"2020-11-05T21:33:26.214436","indexId":"wri8250","displayToPublicDate":"1994-01-01T00:00:00","publicationYear":"1982","noYear":false,"publicationType":{"id":18,"text":"Report"},"publicationSubtype":{"id":5,"text":"USGS Numbered Series"},"seriesTitle":{"id":342,"text":"Water-Resources Investigations Report","code":"WRI","active":false,"publicationSubtype":{"id":5}},"seriesNumber":"82-50","title":"Methodology for hydrologic evaluation of a potential surface mine: Loblolly Branch basin, Tuscaloosa County, Alabama","docAbstract":"Methodology for evaluating premining hydrology and postmining effects of mining and reclamation on the hydrology of an area is presented for a potential mine-permit area of 1,680 acres in the Warrior Coal Field, northwestern Alabama.
Information is included on climate, geology, soil-water relations, vegetation, surface water, ground water, and quality of water. Estimation techniques are used to develop data for reconstructed topography, soil-water relations, vegetation cover, peak flows, flow volumes, soil losses, and sediment yields.
Streamflow response of the basin is described by the variable-source-area concept; nearly all water moving from slopes flows through coarse-textured soils and unconsolidated sand and gravel deposits that are underlain by an impermeable clay zone. The resultant peak discharges per unit area are small to moderate, and there is very little erosion of slopes or channels. Susceptibility of the soils to compaction by heavy machines and the effects of compaction on soil-water relations are demonstrated.
Regression and empirical methods for evaluating streamflow characteristics are compared. Estimates of peak discharges made with four methods are divergent, particularly for recurrence intervals of 2, 5, and 10 years; divergence is less for 25-, 50-, and 100-year discharges.
The Universal Soil Loss Equation (USLE) and sediment-delivery ratios are used to estimate sediment yields for various land and cover conditions from premining until 20 years after reclamation would begin. A premining estimate of sediment yield made with the Universal Soil Loss Equation and a sediment-delivery ratio is about 2.5 times larger than an estimate made with the sediment rating curve-flow duration method.
Research and data needs are discussed regarding: (1) An improved understanding of the hydrology of small, very ,permeable, upland basins; (2) alternative methods for estimating streamflow and sediment yield of such basins; (3) field evaluation of permeability and erodibility of soils on reclaimed areas; and (4) better understanding of ground-water hydrology and geochemistry of the coal-bearing Pottsville Formation before and after mining.
","language":"English","publisher":"U.S. Geological Survey","doi":"10.3133/wri8250","usgsCitation":"Shown, L.M., Frickel, D., Miller, R., and Branson, F., 1982, Methodology for hydrologic evaluation of a potential surface mine: Loblolly Branch basin, Tuscaloosa County, Alabama: U.S. Geological Survey Water-Resources Investigations Report 82-50, vii, 93 p., https://doi.org/10.3133/wri8250.","productDescription":"vii, 93 p.","costCenters":[],"links":[{"id":380219,"rank":2,"type":{"id":11,"text":"Document"},"url":"https://pubs.usgs.gov/wri/1982/0050/report.pdf","linkFileType":{"id":1,"text":"pdf"}},{"id":157622,"rank":0,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/wri/1982/0050/report-thumb.jpg"}],"country":"United States","state":"Alabama","county":"Tuscaloosa County","otherGeospatial":"Loblolly Branch basin","geographicExtents":"{\n \"type\": \"FeatureCollection\",\n \"features\": [\n {\n \"type\": \"Feature\",\n \"properties\": {},\n \"geometry\": {\n \"type\": \"Polygon\",\n \"coordinates\": [\n [\n [\n -87.5,\n 33.33333333\n ],\n [\n -87.41666667,\n 33.33333333\n ],\n [\n -87.41666667,\n 33.45\n ],\n [\n -87.5,\n 33.45\n ],\n [\n -87.5,\n 33.33333333\n ]\n ]\n ]\n }\n }\n ]\n}","noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"4f4e4a51e4b07f02db629fab","contributors":{"authors":[{"text":"Shown, Lynn M.","contributorId":7326,"corporation":false,"usgs":true,"family":"Shown","given":"Lynn","email":"","middleInitial":"M.","affiliations":[],"preferred":false,"id":194575,"contributorType":{"id":1,"text":"Authors"},"rank":1},{"text":"Frickel, D. G.","contributorId":11213,"corporation":false,"usgs":true,"family":"Frickel","given":"D. G.","affiliations":[],"preferred":false,"id":194576,"contributorType":{"id":1,"text":"Authors"},"rank":2},{"text":"Miller, R.F.","contributorId":83882,"corporation":false,"usgs":true,"family":"Miller","given":"R.F.","email":"","affiliations":[],"preferred":false,"id":194578,"contributorType":{"id":1,"text":"Authors"},"rank":3},{"text":"Branson, F.A.","contributorId":31430,"corporation":false,"usgs":true,"family":"Branson","given":"F.A.","affiliations":[],"preferred":false,"id":194577,"contributorType":{"id":1,"text":"Authors"},"rank":4}]}} ,{"id":43567,"text":"ofr81536 - 1982 - Hydrology of Lake Tohopekaliga, Osceola County, Florida","interactions":[],"lastModifiedDate":"2022-04-18T16:23:05.159371","indexId":"ofr81536","displayToPublicDate":"1994-01-01T00:00:00","publicationYear":"1982","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":"81-536","title":"Hydrology of Lake Tohopekaliga, Osceola County, Florida","docAbstract":"No abstract available.
","language":"English","publisher":"U.S. Geological Survey","doi":"10.3133/ofr81536","collaboration":"Prepared in cooperation with the South Florida Water Management District","usgsCitation":"Phelps, G.G., 1982, Hydrology of Lake Tohopekaliga, Osceola County, Florida: U.S. Geological Survey Open-File Report 81-536, 2 Plates: 38.54 x 28.43 inches and 38.46 x 27.83 inches, https://doi.org/10.3133/ofr81536.","productDescription":"2 Plates: 38.54 x 28.43 inches and 38.46 x 27.83 inches","costCenters":[],"links":[{"id":398942,"rank":3,"type":{"id":17,"text":"Plate"},"url":"https://pubs.usgs.gov/of/1981/0536/plate-1.pdf","linkFileType":{"id":1,"text":"pdf"}},{"id":398941,"rank":2,"type":{"id":17,"text":"Plate"},"url":"https://pubs.usgs.gov/of/1981/0536/plate-2.pdf","linkFileType":{"id":1,"text":"pdf"}},{"id":167847,"rank":0,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/of/1981/0536/report-thumb.jpg"}],"country":"United States","state":"Florida","county":"Osceola County","otherGeospatial":"Lake Tohopekaliga","geographicExtents":"{\n \"type\": \"FeatureCollection\",\n \"features\": [\n {\n \"type\": \"Feature\",\n \"properties\": {},\n \"geometry\": {\n \"type\": \"Polygon\",\n \"coordinates\": [\n [\n [\n -81.43890380859375,\n 28.132549863716783\n ],\n [\n -81.31118774414062,\n 28.132549863716783\n ],\n [\n -81.31118774414062,\n 28.311635046750613\n ],\n [\n -81.43890380859375,\n 28.311635046750613\n ],\n [\n -81.43890380859375,\n 28.132549863716783\n ]\n ]\n ]\n }\n }\n ]\n}","noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"4f4e4a17e4b07f02db604893","contributors":{"authors":[{"text":"Phelps, G. G.","contributorId":82346,"corporation":false,"usgs":true,"family":"Phelps","given":"G.","email":"","middleInitial":"G.","affiliations":[],"preferred":false,"id":228397,"contributorType":{"id":1,"text":"Authors"},"rank":1}]}} ,{"id":30344,"text":"wri8234 - 1982 - Water-quality characteristics of Everglades National Park, 1959-77, with reference to the effects of water management","interactions":[],"lastModifiedDate":"2019-08-05T12:06:39","indexId":"wri8234","displayToPublicDate":"1994-01-01T00:00:00","publicationYear":"1982","noYear":false,"publicationType":{"id":18,"text":"Report"},"publicationSubtype":{"id":5,"text":"USGS Numbered Series"},"seriesTitle":{"id":342,"text":"Water-Resources Investigations Report","code":"WRI","active":false,"publicationSubtype":{"id":5}},"seriesNumber":"82-34","title":"Water-quality characteristics of Everglades National Park, 1959-77, with reference to the effects of water management","docAbstract":"The U.S. Geological Survey has collected water-quality data in the Everglades National Park since 1959. Major ions, macronutrients, trace elements, and pesticides are the primary chemical groups analyzed. The period of record and frequency of sampling vary for each chemical group, with the longest record for the major ions and the shortest for the macronutrients. Within the park there are three major drainageways: Big Cypress Swamp, Shark River Slough, and Taylor Slough. Each drainageway exhibits unique hydrologic conditions, yet there is a high degree of homogeneity in water-quality characteristics among these areas. Seasonal changes in major-ion, trace-element, and macronutrient concentrations are marked in the shallow marsh. Concentrations generally increase in the dry season due to evapotranspiration, changes in chemical equilibria, and precipitation. Water-management practices in south Florida have changed the water quality in the Shark River Slough. Most major-ion, dissolved-solid, and iron concentrations and color levels have steadily increased since 1963. The water quality in the other two drainageways has not changed since sampling began. Chlorinated-hydrocarbon insecticide residues in bottom material were found in low concentration at every sampling station in the park. (USGS)","language":"English","publisher":"U.S. Geological Survey","publisherLocation":"Reston, VA","doi":"10.3133/wri8234","usgsCitation":"Waller, B.G., 1982, Water-quality characteristics of Everglades National Park, 1959-77, with reference to the effects of water management: U.S. Geological Survey Water-Resources Investigations Report 82-34, vi, 51 p. , https://doi.org/10.3133/wri8234.","productDescription":"vi, 51 p. ","costCenters":[],"links":[{"id":366265,"rank":2,"type":{"id":11,"text":"Document"},"url":"https://pubs.usgs.gov/wri/1982/0034/report.pdf","linkFileType":{"id":1,"text":"pdf"}},{"id":159310,"rank":0,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/wri/1982/0034/report-thumb.jpg"}],"country":"United States","state":"Florida","otherGeospatial":"Everglades National Park","geographicExtents":"{\n \"type\": \"FeatureCollection\",\n \"features\": [\n {\n \"type\": \"Feature\",\n \"properties\": {},\n \"geometry\": {\n \"type\": \"Polygon\",\n \"coordinates\": [\n [\n [\n -81.15600585937499,\n 25.13533901613099\n ],\n [\n -80.48583984375,\n 25.13533901613099\n ],\n [\n -80.48583984375,\n 25.517657429994035\n ],\n [\n -81.15600585937499,\n 25.517657429994035\n ],\n [\n -81.15600585937499,\n 25.13533901613099\n ]\n ]\n ]\n }\n }\n ]\n}","noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"4f4e4a9ae4b07f02db65d9f0","contributors":{"authors":[{"text":"Waller, Bradley G.","contributorId":83492,"corporation":false,"usgs":true,"family":"Waller","given":"Bradley","email":"","middleInitial":"G.","affiliations":[],"preferred":false,"id":203093,"contributorType":{"id":1,"text":"Authors"},"rank":1}]}} ,{"id":30351,"text":"wri8182 - 1982 - Streamflow characteristics of the upper Columbia River basin, Montana, through 1979","interactions":[],"lastModifiedDate":"2020-12-28T18:00:28.071514","indexId":"wri8182","displayToPublicDate":"1994-01-01T00:00:00","publicationYear":"1982","noYear":false,"publicationType":{"id":18,"text":"Report"},"publicationSubtype":{"id":5,"text":"USGS Numbered Series"},"seriesTitle":{"id":342,"text":"Water-Resources Investigations Report","code":"WRI","active":false,"publicationSubtype":{"id":5}},"seriesNumber":"81-82","title":"Streamflow characteristics of the upper Columbia River basin, Montana, through 1979","docAbstract":"Statistical summaries of streamflow data for selected stream-gaging sites presented in this report aid in appraising the hydrology of the upper Columbia River basin in Montana. Streamflow records are provided for 54 gaging stations for the period of record. Streamflow records for five gaging stations were compiled into separate periods related to changes in regulation after data collection commenced. The entire period of record, the period before regulation, and the period after regulation are presented for comparison. For each gaging station selected for this report, a brief description is given for station location, drainage area, period of record, revisions of previously published records, type and history of gages, regulation and diversions, and extremes of discharge. These data are followed by tables of monthly and annual flow statistics, flood-frequency data, low-flow and high-flow frequency data, and flow-duration information. 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\"}}]}","noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"4f4e4b15e4b07f02db6a4eb0","contributors":{"authors":[{"text":"Waltemeyer, Scott D.","contributorId":101709,"corporation":false,"usgs":true,"family":"Waltemeyer","given":"Scott","email":"","middleInitial":"D.","affiliations":[],"preferred":false,"id":203102,"contributorType":{"id":1,"text":"Authors"},"rank":1},{"text":"Shields, Ronald R.","contributorId":64655,"corporation":false,"usgs":true,"family":"Shields","given":"Ronald","email":"","middleInitial":"R.","affiliations":[],"preferred":false,"id":203101,"contributorType":{"id":1,"text":"Authors"},"rank":2}]}} ,{"id":38574,"text":"pp1242 - 1982 - Perennial-streamflow characteristics related to channel geometry and sediment in Missouri River basin","interactions":[],"lastModifiedDate":"2022-10-26T19:27:54.095277","indexId":"pp1242","displayToPublicDate":"1994-01-01T00:00:00","publicationYear":"1982","noYear":false,"publicationType":{"id":18,"text":"Report"},"publicationSubtype":{"id":5,"text":"USGS Numbered Series"},"seriesTitle":{"id":331,"text":"Professional Paper","code":"PP","onlineIssn":"2330-7102","printIssn":"1044-9612","active":true,"publicationSubtype":{"id":5}},"seriesNumber":"1242","title":"Perennial-streamflow characteristics related to channel geometry and sediment in Missouri River basin","docAbstract":"Geometry, channel-sediment, and discharge data were collected and compiled from 252 streamflow-gaging stations in the Missouri River basin. The sites represent the complete ranges of hydrologic and geologic conditions found in the basin. The data were analyzed by computer to yield equations relating various discharge characteristics to variables of channel geometry and bed and bank material. The equations provide discharge as the dependent variable for the purpose of making estimates of discharge characteristics at ungaged sites. Results show that channel width is best related to variables of discharge, but that reduction of standard errors can be achieved by considering channel-sediment properties, channel gradient, and discharge variability. The channel-material variables do not exert uniform effects on width-discharge relations and, therefore, are considered as sediment-data groups, or stream types, rather than as terms in multiple power-function equations. Relative to streamflow, narrowest channels occur when streams of steady discharge transport sufficient silt and clay to form stable, cohesive banks but have a small tractive load of sand and coarser sizes. Stable channels also are associated with high channel gradients, which cause high channel roughness and bed and bank armouring by coarse particle sizes. The widest, most unstable channels are found with streams that apparently transport of large tractive load of sand sizes. The downstream rates of change of width with discharge reflect these trends, suggesting that a given bed-material load necessitates a minimum width over which the tractive material can be moved.
","language":"English","publisher":"U.S. Geological Survey","doi":"10.3133/pp1242","usgsCitation":"Osterkamp, W.R., and Hedman, E.R., 1982, Perennial-streamflow characteristics related to channel geometry and sediment in Missouri River basin: U.S. Geological Survey Professional Paper 1242, 37 p., https://doi.org/10.3133/pp1242.","productDescription":"37 p.","costCenters":[],"links":[{"id":408768,"rank":3,"type":{"id":36,"text":"NGMDB Index Page"},"url":"https://ngmdb.usgs.gov/Prodesc/proddesc_74500.htm","linkFileType":{"id":5,"text":"html"}},{"id":65350,"rank":300,"type":{"id":11,"text":"Document"},"url":"https://pubs.usgs.gov/pp/1242/report.pdf","linkFileType":{"id":1,"text":"pdf"}},{"id":123419,"rank":0,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/pp/1242/report-thumb.jpg"}],"country":"United States","otherGeospatial":"Missouri River basin","geographicExtents":"{\n \"type\": \"FeatureCollection\",\n \"features\": [\n {\n \"type\": \"Feature\",\n \"properties\": {},\n \"geometry\": {\n \"coordinates\": [\n [\n [\n -114,\n 49\n ],\n [\n -114,\n 37\n ],\n [\n -80,\n 37\n ],\n [\n -80,\n 49\n ],\n [\n -114,\n 49\n ]\n ]\n ],\n \"type\": \"Polygon\"\n }\n }\n ]\n}","noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"4f4e4ae0e4b07f02db687e36","contributors":{"authors":[{"text":"Osterkamp, W. R.","contributorId":46044,"corporation":false,"usgs":true,"family":"Osterkamp","given":"W.","email":"","middleInitial":"R.","affiliations":[],"preferred":false,"id":220090,"contributorType":{"id":1,"text":"Authors"},"rank":1},{"text":"Hedman, E. R.","contributorId":71527,"corporation":false,"usgs":true,"family":"Hedman","given":"E.","email":"","middleInitial":"R.","affiliations":[],"preferred":false,"id":220091,"contributorType":{"id":1,"text":"Authors"},"rank":2}]}} ,{"id":36476,"text":"fwsobs82_59 - 1982 - Proceedings of the conference on coastal erosion and wetland modification in Louisiana: causes, consequences, and options","interactions":[],"lastModifiedDate":"2018-01-30T12:45:31","indexId":"fwsobs82_59","displayToPublicDate":"1994-01-01T00:00:00","publicationYear":"1982","noYear":false,"publicationType":{"id":18,"text":"Report"},"publicationSubtype":{"id":1,"text":"Federal Government Series"},"seriesTitle":{"id":20,"text":"FWS/OBS","active":false,"publicationSubtype":{"id":1}},"seriesNumber":"82/59","title":"Proceedings of the conference on coastal erosion and wetland modification in Louisiana: causes, consequences, and options","docAbstract":"This volume contains 16 papers and panel discussions from a conference held in Baton Rouge, La., 5-6 October 1981. The presentations consider the causes and consequences of coastal erosion and wetland modification in Louisiana and the mitigative options available to slow or reverse the rapid rate of coastal land loss. Detailed habitat mapping studies have allowed accurate estimates of coastal habitat change and land loss through 1978. Projections from these rates of change indicate an annual rate of land loss in coastal Louisiana in the early 1980's of approximately 130 km2/yr (50 m2/yr).
The projected effects of wetland modification on the bountiful living resources of coastal Louisiana (fisheries, fur and hide bearers and waterfowl) are major because of the close dependence of these resources on estuarine wetlands. These changes and others related to flood protection, transportation and ownership of mineral resources are projected to have extensive social and economic consequences.
Options proposed to slow coastal land loss include major and minor diversion of the Mississippi River, barrier island and shoreline restoration protection, hydrological management of wetlands and more restrictive permitting of dredging activities.
","language":"English","publisher":"U.S. Fish and Wildlife Service, Biological Services Program","publisherLocation":"Washington, D.C.","usgsCitation":"1982, Proceedings of the conference on coastal erosion and wetland modification in Louisiana: causes, consequences, and options: FWS/OBS 82/59, viii, 256 p.","productDescription":"viii, 256 p.","numberOfPages":"265","costCenters":[],"links":[{"id":289595,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/thumbnails/outside_thumb.jpg"},{"id":289594,"type":{"id":11,"text":"Document"},"url":"https://pubs.usgs.gov/fwsobs/1982/0059/report.pdf"}],"country":"United States","state":"Louisiana","geographicExtents":"{ \"type\": \"FeatureCollection\", \"features\": [ { \"type\": \"Feature\", \"properties\": {}, \"geometry\": { \"type\": \"Polygon\", \"coordinates\": [ [ [ -94.0434,28.9254 ], [ -94.0434,33.0195 ], [ -88.8162,33.0195 ], [ -88.8162,28.9254 ], [ -94.0434,28.9254 ] ] ] } } ] }","noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"4f4e4a9ee4b07f02db660489","contributors":{"editors":[{"text":"Boesch, Donald F.","contributorId":23599,"corporation":false,"usgs":true,"family":"Boesch","given":"Donald","email":"","middleInitial":"F.","affiliations":[],"preferred":false,"id":504035,"contributorType":{"id":2,"text":"Editors"},"rank":1}]}} ,{"id":43040,"text":"ofr82120 - 1982 - Semiannual water-table and potentiometric surface for two water-yielding zones in the surficial aquifer, 1975-79, Naples area, Florida","interactions":[],"lastModifiedDate":"2022-04-15T17:45:10.428533","indexId":"ofr82120","displayToPublicDate":"1994-01-01T00:00:00","publicationYear":"1982","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":"82-120","title":"Semiannual water-table and potentiometric surface for two water-yielding zones in the surficial aquifer, 1975-79, Naples area, Florida","docAbstract":"Potable ground water in the Naples area along the coastal ridge of western Collier County, Florida, is available from two principal sources-the water-table zone and the pumped zone, both within the surficial aquifer. The primary source of public supply is from the pumped zone, locally known as the Coastal Ridge aquifer. Water levels in wells in the pumped zone respond rapidly to pumpage and usually indicate a cone of depression in most of the highly urbanized Naples area. The cone of depression caused by pumpage has created significant water-level differences between the water-table zone and pumped zone. Water-level differences in the two zones from 1975 to 1979 frequently exceed 10 feet. The maps have been drawn to be representative of hydrologic conditions in both zones for the wet and dry seasons from 1975-79.
","language":"English","publisher":"U.S. Geological Survey","doi":"10.3133/ofr82120","collaboration":"Prepared in cooperation with Collier County","usgsCitation":"Buchmiller, R., 1982, Semiannual water-table and potentiometric surface for two water-yielding zones in the surficial aquifer, 1975-79, Naples area, Florida: U.S. Geological Survey Open-File Report 82-120, 2 Plates: 36.64 x 25.00 inches and 37.02 x 25.10 inches, https://doi.org/10.3133/ofr82120.","productDescription":"2 Plates: 36.64 x 25.00 inches and 37.02 x 25.10 inches","costCenters":[],"links":[{"id":398846,"rank":4,"type":{"id":17,"text":"Plate"},"url":"https://pubs.usgs.gov/of/1982/0120/plate-1.pdf","linkFileType":{"id":1,"text":"pdf"}},{"id":398845,"rank":3,"type":{"id":17,"text":"Plate"},"url":"https://pubs.usgs.gov/of/1982/0120/plate-2.pdf","linkFileType":{"id":1,"text":"pdf"}},{"id":397220,"rank":2,"type":{"id":36,"text":"NGMDB Index Page"},"url":"https://ngmdb.usgs.gov/Prodesc/proddesc_13663.htm"},{"id":176195,"rank":0,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/of/1982/0120/report-thumb.jpg"}],"country":"United States","state":"Florida","city":"Naples","geographicExtents":"{\n \"type\": \"FeatureCollection\",\n \"features\": [\n {\n \"type\": \"Feature\",\n \"properties\": {},\n \"geometry\": {\n \"type\": \"Polygon\",\n \"coordinates\": [\n [\n [\n -81.815185546875,\n 25.975329851614575\n ],\n [\n -81.57623291015625,\n 25.975329851614575\n ],\n [\n -81.57623291015625,\n 26.305726417424278\n ],\n [\n -81.815185546875,\n 26.305726417424278\n ],\n [\n -81.815185546875,\n 25.975329851614575\n ]\n ]\n ]\n }\n }\n ]\n}","noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"4f4e49e2e4b07f02db5e4d24","contributors":{"authors":[{"text":"Buchmiller, R.C.","contributorId":59458,"corporation":false,"usgs":true,"family":"Buchmiller","given":"R.C.","email":"","affiliations":[],"preferred":false,"id":227623,"contributorType":{"id":1,"text":"Authors"},"rank":1}]}} ,{"id":24985,"text":"pp1275 - 1982 - Geological Survey research 1981","interactions":[],"lastModifiedDate":"2025-01-07T19:40:11.539183","indexId":"pp1275","displayToPublicDate":"1994-01-01T00:00:00","publicationYear":"1982","noYear":false,"publicationType":{"id":18,"text":"Report"},"publicationSubtype":{"id":5,"text":"USGS Numbered Series"},"seriesTitle":{"id":331,"text":"Professional Paper","code":"PP","onlineIssn":"2330-7102","printIssn":"1044-9612","active":true,"publicationSubtype":{"id":5}},"seriesNumber":"1275","title":"Geological Survey research 1981","docAbstract":"This U.S. Geological Survey activities report includes a summary of 1981 fiscal year scientific and economic results accompanied by a list of geologic, hydrologic, and cartographic investigations in progress. The summary of results includes: (1) Mineral, (2) Water resources, (3) Engineering geology and hydrology, (4) Regional geology, (5) Principles and processes, (6) Laboratory and field methods, (7) Topographic surveys and mapping, (8) Management of resources on public lands, (9) Land information and analysis, and (10) Investigations in other countries. Also included are lists of investigations in progress.
","language":"English","publisher":"U.S. Geological Survey","publisherLocation":"Washington, D.C.","doi":"10.3133/pp1275","usgsCitation":"Water Resources Division, U.S. Geological Survey, 1982, Geological Survey research 1981: U.S. Geological Survey Professional Paper 1275, ix, 402 p., https://doi.org/10.3133/pp1275.","productDescription":"ix, 402 p.","numberOfPages":"412","costCenters":[{"id":114,"text":"Alaska Science Center","active":true,"usgs":true}],"links":[{"id":403863,"rank":3,"type":{"id":36,"text":"NGMDB Index Page"},"url":"https://ngmdb.usgs.gov/Prodesc/proddesc_93011.htm","text":"Paleomagnetic correlations of Proterozoic rocks","linkFileType":{"id":5,"text":"html"}},{"id":53970,"rank":2,"type":{"id":11,"text":"Document"},"url":"https://pubs.usgs.gov/pp/1275/report.pdf","linkFileType":{"id":1,"text":"pdf"}},{"id":118863,"rank":1,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/pp/1275/report-thumb.jpg"},{"id":465800,"rank":4,"type":{"id":36,"text":"NGMDB Index Page"},"url":"https://ngmdb.usgs.gov/Prodesc/proddesc_93013.htm","text":"The mafic \"Chickwolnepy complex\""}],"noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"4f4e4adee4b07f02db6876d8","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":529146,"contributorType":{"id":1,"text":"Authors"},"rank":1}]}} ,{"id":29035,"text":"wri824004 - 1982 - Reconnaissance of ground-water quality, eastern Snake River basin, Idaho","interactions":[],"lastModifiedDate":"2012-02-02T00:08:44","indexId":"wri824004","displayToPublicDate":"1994-01-01T00:00:00","publicationYear":"1982","noYear":false,"publicationType":{"id":18,"text":"Report"},"publicationSubtype":{"id":5,"text":"USGS Numbered Series"},"seriesTitle":{"id":342,"text":"Water-Resources Investigations Report","code":"WRI","active":false,"publicationSubtype":{"id":5}},"seriesNumber":"82-4004","title":"Reconnaissance of ground-water quality, eastern Snake River basin, Idaho","docAbstract":"Water-quality, geologic, and hydrologic data were collected for 165 wells in the eastern Snake River basin, Idaho. Water-quality characteristics analyzed include specific conductance, pH, water temperature, major dissolved cations and anions, and coliform bacteria. Ground water from aquifers in all rock units is generally composed of calcium, magnesium, and bicarbonate type and contains carbonate ions. Changes in area trends of ground-water composition probably are most directly related to variability in aquifer composition and proximity to varying sources of recharge, especially those related to man 's land- and water-use activities. In the uplands subareas, median values for selected ground-water characteristics from current analyses are 2000 mg/l hardness; 7.6, pH; 200 mg/l alkalinity; 13C; 0.2 mg/l fluoride; 15 mg/l silica; 0.51 mg/l nitrite (as nitrogen); less than 1 colony per 100 milliliters of water coliform bacteria; 0.02 mg/l phosphorus (total); and 25 mg/l hardness; 7.7, pH; 180 mg/l alkalinity; 11C; 0.4 mg/l fluoride; 26 mg/l silica; 1.2 mg/l nitrite plus nitrate; less than 1 colony per 100 milliliters of water coliform bacteria; 0.01 amg/l phosphorus; and 283 mg/l dissolved solids. Ground-water quality in most of the study area meets recommended standards or criteria for most uses. (USGS)","language":"ENGLISH","publisher":"U.S. Geological Survey,","doi":"10.3133/wri824004","usgsCitation":"Parliman, D., 1982, Reconnaissance of ground-water quality, eastern Snake River basin, Idaho: U.S. Geological Survey Water-Resources Investigations Report 82-4004, vii, 100 p. :ill., maps ;28 cm., https://doi.org/10.3133/wri824004.","productDescription":"vii, 100 p. :ill., maps ;28 cm.","costCenters":[],"links":[{"id":158893,"rank":0,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/wri/1982/4004/report-thumb.jpg"},{"id":57898,"rank":400,"type":{"id":17,"text":"Plate"},"url":"https://pubs.usgs.gov/wri/1982/4004/plate-1.pdf","linkFileType":{"id":1,"text":"pdf"}},{"id":57899,"rank":401,"type":{"id":17,"text":"Plate"},"url":"https://pubs.usgs.gov/wri/1982/4004/plate-2.pdf","linkFileType":{"id":1,"text":"pdf"}},{"id":57900,"rank":402,"type":{"id":17,"text":"Plate"},"url":"https://pubs.usgs.gov/wri/1982/4004/plate-3.pdf","linkFileType":{"id":1,"text":"pdf"}},{"id":57901,"rank":403,"type":{"id":17,"text":"Plate"},"url":"https://pubs.usgs.gov/wri/1982/4004/plate-4.pdf","linkFileType":{"id":1,"text":"pdf"}},{"id":57902,"rank":300,"type":{"id":11,"text":"Document"},"url":"https://pubs.usgs.gov/wri/1982/4004/report.pdf","linkFileType":{"id":1,"text":"pdf"}}],"noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"4f4e4a63e4b07f02db636fdf","contributors":{"authors":[{"text":"Parliman, D. J.","contributorId":64220,"corporation":false,"usgs":true,"family":"Parliman","given":"D. J.","affiliations":[],"preferred":false,"id":200831,"contributorType":{"id":1,"text":"Authors"},"rank":1}]}} ,{"id":28639,"text":"wri8137 - 1982 - Hydrology of the Prairie Dog Creek drainage basin, Rosebud and Big Horn Counties, Montana","interactions":[],"lastModifiedDate":"2020-11-04T18:01:01.580789","indexId":"wri8137","displayToPublicDate":"1994-01-01T00:00:00","publicationYear":"1982","noYear":false,"publicationType":{"id":18,"text":"Report"},"publicationSubtype":{"id":5,"text":"USGS Numbered Series"},"seriesTitle":{"id":342,"text":"Water-Resources Investigations Report","code":"WRI","active":false,"publicationSubtype":{"id":5}},"seriesNumber":"81-37","title":"Hydrology of the Prairie Dog Creek drainage basin, Rosebud and Big Horn Counties, Montana","docAbstract":"The Prairie Dog Creek drainage basin in southeastern Montana was investigated during 1978-79 to assess the surface-water and ground-water resources and the quality of water in an area having coal-mining potential. The area, a 24.2-square-mile basin, is located 30 miles southwest of Ash-land, Montana. The principal mineable coal is the 40-to 60-foot-thick Wall and lower Wall coal beds near the middle part of the Tongue River Member of the Fort Union Formation (Paleocene age). Other possibly mineable intervals are the Canyon coal bed lying 200 to 250 feet above the Wall, and the Brewster-Arnold coal bed lying about 220 feet below the base of the Wall coal beds.
The hydrologic regime in the basin is composed of Prairie Dog Creek and sandstone, coal, clinker, and alluvium aquifers. Prairie Dog Creek, which originates from springs and seeps issuing from coal and sandstone layers, maintained perennial flow in its upstream and middle reaches during 1978 and 1979. In its downstream reach, the flow decreased consistently until the channel near the mouth had only standing water or was dry. The dissolved-solids concentration of streamflow during periods of high flow (1 cubic foot per second or more) in the spring months ranged from 700 to about 1,000 milligrams per liter and during periods of lesser flow (0.5 cubic foot per second or less) in the summer ranged from about 1,300 to 1,600 milligrams per liter.
Forty-two cased observation wells were used to obtain data on aquifer characteristics and quality of water. Relatively clean (free of silt or mud) sandstone beds have transmissivities of about 15 feet squared per day; the water was a magnesium sulfate or sodium sulfate type and dissolved-solids concentrations ranged from about 2,170 to 3,260 milligrams per liter. The Wall coal aquifer has transmissivities ranging from 2.5 to 65 feet squared per day; the water was a sodium sulfate type and dissolved-solids concentrations ranged from 1,820 to 4,190 milligrams per liter. The Brewster-Arnold coal aquifer has transmissivities similar to those of the Wall coal but the water was a sodium bicarbonate type; the water contained an excessive concentration of fluoride (more than 10 milligrams per liter) and had a very high sodium-adsorption ratio (more than 60).
The alluvial aquifer in the Prairie Dog Creek valley has transmissivities ranging from about 1,000 to 5,000 feet squared per day in the middle reaches and as much as 9,200 feet squared per day near the mouth of the creek. The water quality changed from a magnesium sulfate type in the middle reaches to a sodium sulfate type near the mouth. The dissolved-solids concentration decreased from about 1,700 milligrams per liter in the middle reaches to about 1,100 milligrams per liter near the mouth as inflow of water from clinker and alluvial deposits beneath terraces diluted the alluvial water.
","language":"English","publisher":"U.S. Geological Survey","doi":"10.3133/wri8137","collaboration":"Report prepared on behalf of the U.S. Bureau of Land Management","usgsCitation":"McClymonds, N.E., 1982, Hydrology of the Prairie Dog Creek drainage basin, Rosebud and Big Horn Counties, Montana: U.S. Geological Survey Water-Resources Investigations Report 81-37, vii, 64 p., https://doi.org/10.3133/wri8137.","productDescription":"vii, 64 p.","costCenters":[],"links":[{"id":158797,"rank":0,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/wri/1981/0037/report-thumb.jpg"},{"id":380150,"rank":2,"type":{"id":11,"text":"Document"},"url":"https://pubs.usgs.gov/wri/1981/0037/report.pdf","linkFileType":{"id":1,"text":"pdf"}}],"country":"United States","state":"Montana","county":"Big Horn County, Rosebud County","geographicExtents":"{\n \"type\": \"FeatureCollection\",\n \"features\": [\n {\n \"type\": \"Feature\",\n \"properties\": {},\n \"geometry\": {\n \"type\": \"Polygon\",\n \"coordinates\": [\n [\n [\n -107.86376953125,\n 44.99588261816546\n ],\n [\n -106.512451171875,\n 44.99588261816546\n ],\n [\n -106.512451171875,\n 45.99314540468519\n ],\n [\n -107.86376953125,\n 45.99314540468519\n ],\n [\n -107.86376953125,\n 44.99588261816546\n ]\n ]\n ]\n }\n }\n ]\n}","noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"4f4e4ac9e4b07f02db67ca4c","contributors":{"authors":[{"text":"McClymonds, N. E.","contributorId":94653,"corporation":false,"usgs":true,"family":"McClymonds","given":"N.","email":"","middleInitial":"E.","affiliations":[],"preferred":false,"id":200158,"contributorType":{"id":1,"text":"Authors"},"rank":1}]}} ,{"id":48793,"text":"ofr8250 - 1982 - Methodology for Hydrologic Evaluation of a Potential Surface Mine: Loblolly Branch Basin, Tuscaloosa County, Alabama","interactions":[],"lastModifiedDate":"2012-02-02T00:10:22","indexId":"ofr8250","displayToPublicDate":"1994-01-01T00:00:00","publicationYear":"1982","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":"82-50","title":"Methodology for Hydrologic Evaluation of a Potential Surface Mine: Loblolly Branch Basin, Tuscaloosa County, Alabama","language":"ENGLISH","publisher":"Geological Survey (U.S.)","doi":"10.3133/ofr8250","usgsCitation":"Shown, L.M., Frickel, D., Miller, R., and Branson, F., 1982, Methodology for Hydrologic Evaluation of a Potential Surface Mine: Loblolly Branch Basin, Tuscaloosa County, Alabama (WRI/OFR 82-50): U.S. Geological Survey Open-File Report 82-50, vii, 93 p., https://doi.org/10.3133/ofr8250.","productDescription":"vii, 93 p.","costCenters":[{"id":595,"text":"U.S. Geological Survey","active":false,"usgs":true}],"links":[{"id":169624,"rank":0,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/thumbnails/usgs_thumb.jpg"}],"edition":"WRI/OFR 82-50","noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"4f4e4a51e4b07f02db629fa5","contributors":{"authors":[{"text":"Shown, Lynn M.","contributorId":7326,"corporation":false,"usgs":true,"family":"Shown","given":"Lynn","email":"","middleInitial":"M.","affiliations":[],"preferred":false,"id":238266,"contributorType":{"id":1,"text":"Authors"},"rank":1},{"text":"Frickel, D. G.","contributorId":11213,"corporation":false,"usgs":true,"family":"Frickel","given":"D. G.","affiliations":[],"preferred":false,"id":238267,"contributorType":{"id":1,"text":"Authors"},"rank":2},{"text":"Miller, R.F.","contributorId":83882,"corporation":false,"usgs":true,"family":"Miller","given":"R.F.","email":"","affiliations":[],"preferred":false,"id":238269,"contributorType":{"id":1,"text":"Authors"},"rank":3},{"text":"Branson, F.A.","contributorId":31430,"corporation":false,"usgs":true,"family":"Branson","given":"F.A.","affiliations":[],"preferred":false,"id":238268,"contributorType":{"id":1,"text":"Authors"},"rank":4}]}} ,{"id":47139,"text":"ofr801282 - 1982 - Flood of September 16, 1975 in the Guayanilla Valley, Puerto Rico","interactions":[],"lastModifiedDate":"2023-06-05T19:50:10.602004","indexId":"ofr801282","displayToPublicDate":"1994-01-01T00:00:00","publicationYear":"1982","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":"80-1282","title":"Flood of September 16, 1975 in the Guayanilla Valley, Puerto Rico","docAbstract":"This report provides hydrologic and hydraulic information related to the flood of September 16, 1975 in the Guayanilla Valley. The information presented is a compilation of data recovered by the U.S. Geological Survey, and information provided by the residents in the study area.
","language":"English","publisher":"U.S. Geological Survey","doi":"10.3133/ofr801282","collaboration":"Prepared in cooperation with the Puerto Rico Department of Natural Resources","usgsCitation":"Johnson, K.G., 1982, Flood of September 16, 1975 in the Guayanilla Valley, Puerto Rico: U.S. Geological Survey Open-File Report 80-1282, 1 Plate: 41.41 x 36.37 inches, https://doi.org/10.3133/ofr801282.","productDescription":"1 Plate: 41.41 x 36.37 inches","costCenters":[],"links":[{"id":417763,"rank":2,"type":{"id":17,"text":"Plate"},"url":"https://pubs.usgs.gov/of/1980/1282/plate-1.pdf","linkFileType":{"id":1,"text":"pdf"}},{"id":169378,"rank":1,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/of/1980/1282/report-thumb.jpg"}],"scale":"20000","country":"United States","otherGeospatial":"Puerto Rico","geographicExtents":"{\n \"type\": \"FeatureCollection\",\n \"features\": [\n {\n \"type\": \"Feature\",\n \"properties\": {},\n \"geometry\": {\n \"coordinates\": [\n [\n [\n -67.33054839621207,\n 18.582631166666303\n ],\n [\n -67.33054839621207,\n 17.84788950213283\n ],\n [\n -65.28636165453952,\n 17.84788950213283\n ],\n [\n -65.28636165453952,\n 18.582631166666303\n ],\n [\n -67.33054839621207,\n 18.582631166666303\n ]\n ]\n ],\n \"type\": \"Polygon\"\n }\n }\n ]\n}","noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"4f4e49f2e4b07f02db5eebfc","contributors":{"authors":[{"text":"Johnson, Karl G.","contributorId":7680,"corporation":false,"usgs":true,"family":"Johnson","given":"Karl","email":"","middleInitial":"G.","affiliations":[],"preferred":false,"id":234694,"contributorType":{"id":1,"text":"Authors"},"rank":1}]}} ,{"id":28725,"text":"wri8184 - 1982 - Water-quality and hydrogeologic data for three phosphate industry waste-disposal sites in central Florida, 1979-80","interactions":[],"lastModifiedDate":"2019-12-05T08:35:31","indexId":"wri8184","displayToPublicDate":"1994-01-01T00:00:00","publicationYear":"1982","noYear":false,"publicationType":{"id":18,"text":"Report"},"publicationSubtype":{"id":5,"text":"USGS Numbered Series"},"seriesTitle":{"id":342,"text":"Water-Resources Investigations Report","code":"WRI","active":false,"publicationSubtype":{"id":5}},"seriesNumber":"81-84","title":"Water-quality and hydrogeologic data for three phosphate industry waste-disposal sites in central Florida, 1979-80","docAbstract":"This report is a complilation of geologic, hydrologic, and water-quality data and information on test holes collected in the vicinity of gypsum stack complexes at two phosphate chemical plants and one phosphatic clayey waste disposal pond at a phosphate mine and beneficiation plant in central Florida. The data were collected from September 1979 to October 1980 at thee AMAX Phosphate, Inc., chemical plant, Piney Point; the USS AgriChemicals chemical plant, Bartow; and the International Minerals and Chemical Corporation Clear Springs mine, Bartow. Approximmmtely 5,400 field and laboratory water-quality determinations on water samples were collected from about 78 test holes and 31 surface-water, rainfall, and other sampling sites at phosphate industry beneficiation and chemical plant waste-disposal operations. Maps show locations of sampling sites. (USGS)","language":"English","publisher":"U.S. Geological Survey","publisherLocation":"Reston, VA","doi":"10.3133/wri8184","usgsCitation":"Miller, R.L., and Sutcliffe, H., 1982, Water-quality and hydrogeologic data for three phosphate industry waste-disposal sites in central Florida, 1979-80: U.S. Geological Survey Water-Resources Investigations Report 81-84, vii, 77 p. , https://doi.org/10.3133/wri8184.","productDescription":"vii, 77 p. 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\"}}]}","noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"4f4e49e6e4b07f02db5e7265","contributors":{"authors":[{"text":"Miller, Ronald L.","contributorId":103245,"corporation":false,"usgs":true,"family":"Miller","given":"Ronald","email":"","middleInitial":"L.","affiliations":[],"preferred":false,"id":200296,"contributorType":{"id":1,"text":"Authors"},"rank":1},{"text":"Sutcliffe, Horace Jr.","contributorId":96725,"corporation":false,"usgs":true,"family":"Sutcliffe","given":"Horace","suffix":"Jr.","email":"","affiliations":[],"preferred":false,"id":200295,"contributorType":{"id":1,"text":"Authors"},"rank":2}]}} ,{"id":25462,"text":"wri8223 - 1982 - Effects of a floodwater-retarding structure on the hydrology and ecology of Trout Creek in southwestern Wisconsin","interactions":[],"lastModifiedDate":"2023-12-13T22:19:53.342114","indexId":"wri8223","displayToPublicDate":"1994-01-01T00:00:00","publicationYear":"1982","noYear":false,"publicationType":{"id":18,"text":"Report"},"publicationSubtype":{"id":5,"text":"USGS Numbered Series"},"seriesTitle":{"id":342,"text":"Water-Resources Investigations Report","code":"WRI","active":false,"publicationSubtype":{"id":5}},"seriesNumber":"82-23","title":"Effects of a floodwater-retarding structure on the hydrology and ecology of Trout Creek in southwestern Wisconsin","docAbstract":"The primary effects of a floodwater-retarding structure (FRS) on the streamflow of Trout Creek, Wisconsin, are attenuation of flood peaks and extension of the time base of flood hydrographs. Reduction of flood peaks ranged from 58 to 91 percent during the study period from 1975 to 1979.
\nThere is an inverse relation between sediment concentration and outflow from the FRS during floods. As water went into storage in the flood pool in March 1976, the daily-mean total-sediment concentration in the FRS outflow dropped from 562 to 147 milligrams per liter. Sediment concentration subsequently increased to 809 milligrams per liter as the discharge from the FRS dropped; concentrations remained more than 400 milligrams per liter for several weeks thereafter. Most sediment stored in the flood pool during flood flows is released from the reservoir during subsequent reduced discharge. Sediment trapping efficiency of the FRS was about 7 percent for the 4-year period of the study.
\nThe bankfull capacity of the channel was reduced from 154 cubic feet per second upstream from the flood pool of the FRS to 65 cubic feet per second just downstream from the FRS. This latter discharge corresponds closely to the normal FRS outflow of 58 to 71 cubic feet per second during floods. Mean bankfull depth downstream from the FRS has adjusted to a value 45 percent less than upstream from the structure due to sedimentation of materials transported from the FRS during reduced flows. The hydraulic geometry and relationships between channel geometry and drainage area indicate little effect of the FRS near the mouth of Trout Creek, 2.4 miles downstream from the FRS. The arthropod fauna of Trout Creek is large and diverse. No effects of the FRS on these fauna were observed from April 1975 to October 1979.
\nFrom fall 1975 to winter 1978, the most important factor contributing to increased brown trout egg survival and fry emergence in Trout Creek during a single reproductive season is higher water temperatures in the upper reaches of the stream. The FRS was not found to have any significant effect on trout reproduction during that period.
\nFrom 1960 to 1979, winter floods seem to have had the greatest adverse effect on the survival of brown trout eggs and sac fry. Although construction of the FRS has eliminated some spawning gravels in the flood pool owing to sedimentation, the wild trout have adapted by using spawning grounds above the flood pool more extensively and intensively. The FRS has not blocked the upstream migration of spawning trout, but it has eliminated similar migrations of fish that compete with and prey on the trout. Controlled streamflows downstream from the FRS have had a stabilizing influence on the limited trout reproduction in this region.
","language":"English","publisher":"U.S. Geological Survey","doi":"10.3133/wri8223","collaboration":"Prepared in cooperation wit the Wisconsin Department of Natural Resources","usgsCitation":"Baima, S., Graczyk, D.J., Field, S.J., Wentz, D.A., Hilsenhoff, W.L., Avery, E.L., and Brynildson, O.M., 1982, Effects of a floodwater-retarding structure on the hydrology and ecology of Trout Creek in southwestern Wisconsin: U.S. Geological Survey Water-Resources Investigations Report 82-23, vi, 68 p., https://doi.org/10.3133/wri8223.","productDescription":"vi, 68 p.","numberOfPages":"76","onlineOnly":"N","additionalOnlineFiles":"N","costCenters":[{"id":677,"text":"Wisconsin Water Science Center","active":true,"usgs":true}],"links":[{"id":423548,"rank":3,"type":{"id":36,"text":"NGMDB Index Page"},"url":"https://ngmdb.usgs.gov/Prodesc/proddesc_35522.htm","linkFileType":{"id":5,"text":"html"}},{"id":123564,"rank":1,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/wri/1982/0023/report-thumb.jpg"},{"id":54192,"rank":2,"type":{"id":11,"text":"Document"},"url":"https://pubs.usgs.gov/wri/1982/0023/report.pdf","linkFileType":{"id":1,"text":"pdf"}}],"country":"United States","state":"Wisconsin","otherGeospatial":"Trout Creek","geographicExtents":"{\n \"type\": \"FeatureCollection\",\n \"features\": [\n {\n \"type\": \"Feature\",\n \"properties\": {},\n \"geometry\": {\n \"type\": \"Polygon\",\n \"coordinates\": [\n [\n [\n -90.00720977783203,\n 43.00941729870574\n ],\n [\n -90.00720977783203,\n 43.15760973366244\n ],\n [\n -89.86026763916016,\n 43.15760973366244\n ],\n [\n -89.86026763916016,\n 43.00941729870574\n ],\n [\n -90.00720977783203,\n 43.00941729870574\n ]\n ]\n ]\n }\n }\n ]\n}","noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"4f4e4a4ae4b07f02db624ab3","contributors":{"editors":[{"text":"Wentz, Dennis A. dawentz@usgs.gov","contributorId":1838,"corporation":false,"usgs":true,"family":"Wentz","given":"Dennis","email":"dawentz@usgs.gov","middleInitial":"A.","affiliations":[{"id":595,"text":"U.S. Geological Survey","active":false,"usgs":true}],"preferred":false,"id":890148,"contributorType":{"id":2,"text":"Editors"},"rank":1},{"text":"Graczyk, David J.","contributorId":208789,"corporation":false,"usgs":false,"family":"Graczyk","given":"David","email":"","middleInitial":"J.","affiliations":[],"preferred":false,"id":890149,"contributorType":{"id":2,"text":"Editors"},"rank":2}],"authors":[{"text":"Baima, Steve","contributorId":332431,"corporation":false,"usgs":false,"family":"Baima","given":"Steve","email":"","affiliations":[],"preferred":false,"id":890150,"contributorType":{"id":1,"text":"Authors"},"rank":1},{"text":"Graczyk, David J.","contributorId":208789,"corporation":false,"usgs":false,"family":"Graczyk","given":"David","email":"","middleInitial":"J.","affiliations":[],"preferred":false,"id":890151,"contributorType":{"id":1,"text":"Authors"},"rank":2},{"text":"Field, Stephen J.","contributorId":53800,"corporation":false,"usgs":true,"family":"Field","given":"Stephen","email":"","middleInitial":"J.","affiliations":[],"preferred":false,"id":890152,"contributorType":{"id":1,"text":"Authors"},"rank":3},{"text":"Wentz, Dennis A. dawentz@usgs.gov","contributorId":1838,"corporation":false,"usgs":true,"family":"Wentz","given":"Dennis","email":"dawentz@usgs.gov","middleInitial":"A.","affiliations":[{"id":595,"text":"U.S. Geological Survey","active":false,"usgs":true}],"preferred":false,"id":890153,"contributorType":{"id":1,"text":"Authors"},"rank":4},{"text":"Hilsenhoff, William L.","contributorId":332432,"corporation":false,"usgs":false,"family":"Hilsenhoff","given":"William","email":"","middleInitial":"L.","affiliations":[],"preferred":false,"id":890154,"contributorType":{"id":1,"text":"Authors"},"rank":5},{"text":"Avery, Eddie L.","contributorId":332433,"corporation":false,"usgs":false,"family":"Avery","given":"Eddie","email":"","middleInitial":"L.","affiliations":[],"preferred":false,"id":890155,"contributorType":{"id":1,"text":"Authors"},"rank":6},{"text":"Brynildson, O. M.","contributorId":332434,"corporation":false,"usgs":false,"family":"Brynildson","given":"O.","email":"","middleInitial":"M.","affiliations":[],"preferred":false,"id":890156,"contributorType":{"id":1,"text":"Authors"},"rank":7}]}} ,{"id":10084,"text":"ofr82430 - 1982 - Computer programs for modeling flow and water quality of surface water systems","interactions":[],"lastModifiedDate":"2012-02-02T00:06:31","indexId":"ofr82430","displayToPublicDate":"1994-01-01T00:00:00","publicationYear":"1982","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":"82-430","title":"Computer programs for modeling flow and water quality of surface water systems","docAbstract":"A selection of available computer programs for modeling flow and water quality in surface water systems is described. The models include programs developed as part of the U.S. Geological Survey Water Resources Division hydrologic research activities and others developed by other agencies, universities, and consulting firms. Each model description includes a statement of program use; data requirements; computer costs; availability of documentation and reference material; and a contact person for additional information. The report is intended to assist the researcher by presenting a very brief description of the surface-water models which are readily available for project use. (USGS)","language":"ENGLISH","publisher":"U.S. Geological Survey, Gulf Coast Hydroscience Center,","doi":"10.3133/ofr82430","usgsCitation":"Lorens, J., 1982, Computer programs for modeling flow and water quality of surface water systems: U.S. Geological Survey Open-File Report 82-430, 33 p. ;11 x 28 cm., https://doi.org/10.3133/ofr82430.","productDescription":"33 p. ;11 x 28 cm.","costCenters":[],"links":[{"id":143957,"rank":0,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/of/1982/0430/report-thumb.jpg"},{"id":37937,"rank":300,"type":{"id":11,"text":"Document"},"url":"https://pubs.usgs.gov/of/1982/0430/report.pdf","linkFileType":{"id":1,"text":"pdf"}}],"noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"4f4e4b19e4b07f02db6a76de","contributors":{"authors":[{"text":"Lorens, J.A.","contributorId":15201,"corporation":false,"usgs":true,"family":"Lorens","given":"J.A.","email":"","affiliations":[],"preferred":false,"id":160792,"contributorType":{"id":1,"text":"Authors"},"rank":1}]}} ,{"id":10112,"text":"ofr82334 - 1982 - Procedures for assessment of cumulative impacts of coal mining on the hydrologic balance","interactions":[],"lastModifiedDate":"2012-02-02T00:06:38","indexId":"ofr82334","displayToPublicDate":"1994-01-01T00:00:00","publicationYear":"1982","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":"82-334","title":"Procedures for assessment of cumulative impacts of coal mining on the hydrologic balance","docAbstract":"Techniques were developed to assess the probable cumulative impacts of anticipated surface mining upon the hydrology of and area. An activity profile of cumulative drainage area versus river miles downstream from the surface mining site is constructed that shows major water uses, flood prone areas, and stream classifications. From the summary shown by the activity profile, an impact matrix is used as a checklist for the importance of the impacts under categories such as water supply, flood prone areas, water contact recreation, etc. Based on the categories checked on the impact matrix, a simple, less accurate model or a more comprehensive and accurate one can be used to quantify the impacts. Quantified impacts are then displayed on an impact profile showing the percentage change in a hydrologic characteristic versus distance downstream of the surface mining site. The simple model for quantification considers only dilution from tributary areas during critical periods whereas the comprehensive model routes flows and quality of water continuously through the year and considers, in addition to dilution, instream processes such as settling, biological uptake , and chemical reactions. (USGS)","language":"ENGLISH","publisher":"U.S. Geological Survey,","doi":"10.3133/ofr82334","usgsCitation":"Lumb, A.M., 1982, Procedures for assessment of cumulative impacts of coal mining on the hydrologic balance: U.S. Geological Survey Open-File Report 82-334, vi, 56 p. :ill., maps ;28 cm., https://doi.org/10.3133/ofr82334.","productDescription":"vi, 56 p. :ill., maps ;28 cm.","costCenters":[],"links":[{"id":144590,"rank":0,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/of/1982/0334/report-thumb.jpg"},{"id":37961,"rank":300,"type":{"id":11,"text":"Document"},"url":"https://pubs.usgs.gov/of/1982/0334/report.pdf","linkFileType":{"id":1,"text":"pdf"}}],"noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"4f4e4a82e4b07f02db64abad","contributors":{"authors":[{"text":"Lumb, Alan M.","contributorId":47792,"corporation":false,"usgs":true,"family":"Lumb","given":"Alan","email":"","middleInitial":"M.","affiliations":[],"preferred":false,"id":160835,"contributorType":{"id":1,"text":"Authors"},"rank":1}]}} ,{"id":10429,"text":"ofr82855 - 1982 - Water resources of Borrego Valley and vicinity, California: Phase 1— Definition of geologic and hydrologic characteristics of the basin","interactions":[],"lastModifiedDate":"2021-09-20T21:15:32.447361","indexId":"ofr82855","displayToPublicDate":"1994-01-01T00:00:00","publicationYear":"1982","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":"82-855","title":"Water resources of Borrego Valley and vicinity, California: Phase 1— Definition of geologic and hydrologic characteristics of the basin","docAbstract":"This report is phase 1 of a 3-phase study and includes information needed to build a digital hydrologic model of Borrego Valley. It includes sources and amounts of recharge water to the basin, areas of water withdrawal, total ground water in storage at steady-state conditions (1945), net ground-water depletion, grid network used to determine storage and depletion, total depth of alluvial fill, transmissivity, hydraulic conductivity and specific yield of aquifers, thickness of individual aquifers, and chemical quality of water. (USGS)","language":"English","publisher":"U.S. Geological Survey","doi":"10.3133/ofr82855","usgsCitation":"Moyle, W., 1982, Water resources of Borrego Valley and vicinity, California: Phase 1— Definition of geologic and hydrologic characteristics of the basin: U.S. Geological Survey Open-File Report 82-855, Report: v, 39 p.; 12 Plates: 47.22 × 30.19 inches or smaller, https://doi.org/10.3133/ofr82855.","productDescription":"Report: v, 39 p.; 12 Plates: 47.22 × 30.19 inches or smaller","costCenters":[],"links":[{"id":38297,"rank":411,"type":{"id":17,"text":"Plate"},"url":"https://pubs.usgs.gov/of/1982/0855/plate-12.pdf","linkFileType":{"id":1,"text":"pdf"}},{"id":38296,"rank":410,"type":{"id":17,"text":"Plate"},"url":"https://pubs.usgs.gov/of/1982/0855/plate-11.pdf","linkFileType":{"id":1,"text":"pdf"}},{"id":38295,"rank":409,"type":{"id":17,"text":"Plate"},"url":"https://pubs.usgs.gov/of/1982/0855/plate-10.pdf","linkFileType":{"id":1,"text":"pdf"}},{"id":38294,"rank":408,"type":{"id":17,"text":"Plate"},"url":"https://pubs.usgs.gov/of/1982/0855/plate-09.pdf","linkFileType":{"id":1,"text":"pdf"}},{"id":38293,"rank":407,"type":{"id":17,"text":"Plate"},"url":"https://pubs.usgs.gov/of/1982/0855/plate-08.pdf","linkFileType":{"id":1,"text":"pdf"}},{"id":38292,"rank":406,"type":{"id":17,"text":"Plate"},"url":"https://pubs.usgs.gov/of/1982/0855/plate-07.pdf","linkFileType":{"id":1,"text":"pdf"}},{"id":38291,"rank":405,"type":{"id":17,"text":"Plate"},"url":"https://pubs.usgs.gov/of/1982/0855/plate-06.pdf","linkFileType":{"id":1,"text":"pdf"}},{"id":38290,"rank":404,"type":{"id":17,"text":"Plate"},"url":"https://pubs.usgs.gov/of/1982/0855/plate-05.pdf","linkFileType":{"id":1,"text":"pdf"}},{"id":38289,"rank":403,"type":{"id":17,"text":"Plate"},"url":"https://pubs.usgs.gov/of/1982/0855/plate-04.pdf","linkFileType":{"id":1,"text":"pdf"}},{"id":38288,"rank":402,"type":{"id":17,"text":"Plate"},"url":"https://pubs.usgs.gov/of/1982/0855/plate-03.pdf","linkFileType":{"id":1,"text":"pdf"}},{"id":38287,"rank":401,"type":{"id":17,"text":"Plate"},"url":"https://pubs.usgs.gov/of/1982/0855/plate-02.pdf","linkFileType":{"id":1,"text":"pdf"}},{"id":38298,"rank":300,"type":{"id":11,"text":"Document"},"url":"https://pubs.usgs.gov/of/1982/0855/report.pdf","linkFileType":{"id":1,"text":"pdf"}},{"id":389508,"rank":15,"type":{"id":36,"text":"NGMDB Index Page"},"url":"https://ngmdb.usgs.gov/Prodesc/proddesc_13842.htm"},{"id":38286,"rank":400,"type":{"id":17,"text":"Plate"},"url":"https://pubs.usgs.gov/of/1982/0855/plate-01.pdf","linkFileType":{"id":1,"text":"pdf"}},{"id":145699,"rank":0,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/of/1982/0855/report-thumb.jpg"}],"country":"United States","state":"California","otherGeospatial":"Borrego Valley","geographicExtents":"{\n \"type\": \"FeatureCollection\",\n \"features\": [\n {\n \"type\": \"Feature\",\n \"properties\": {},\n \"geometry\": {\n \"type\": \"Polygon\",\n \"coordinates\": [\n [\n [\n -116.5,\n 33.0750\n ],\n [\n -116.0,\n 33.0750\n ],\n [\n -116.0,\n 33.43373345341701\n ],\n [\n -116.5,\n 33.43373345341701\n ],\n [\n -116.5,\n 33.0750\n ]\n ]\n ]\n }\n }\n ]\n}","noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"4f4e49f4e4b07f02db5f0868","contributors":{"authors":[{"text":"Moyle, W. 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R.","affiliations":[],"preferred":false,"id":161376,"contributorType":{"id":1,"text":"Authors"},"rank":1}]}} ,{"id":11537,"text":"ofr811055 - 1982 - Drainage areas of New York streams, by river basins; a stream gazetteer; Part 1, Data compiled as of October 1980","interactions":[],"lastModifiedDate":"2012-02-02T00:06:36","indexId":"ofr811055","displayToPublicDate":"1994-01-01T00:00:00","publicationYear":"1982","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":"81-1055","title":"Drainage areas of New York streams, by river basins; a stream gazetteer; Part 1, Data compiled as of October 1980","docAbstract":"Hydrologic studies concerned with surface water require geographic data of several types, among which are stream length and size of drainage area from which runoff is contributed. This gazetteer presents all drainage-area data on New York streams that were available as of October 1980. The information is grouped by river basin, and each section consists of two lists. The first gives sites alphabetically by stream name and includes the body of water to which the stream is tributary, county in which the site is located, drainage area above the mouth, coordinates of the topographic quadrangle on the State index map , and the Geological Survey site number. The second list presents site information by U.S. Geological Survey site number (downstream order along the main stream) and includes drainage area, distance of measurement site above the mouth, and location by latitude and longitude. Data were compiled from published and unpublished sources, all of which are available for inspection at the U.S. Geological Survey in Albany, N.Y. Also included are updated values on several river basins that have been redelineated and whose drainage areas have been recomputed and retabulated since 1977. (USGS)","language":"ENGLISH","publisher":"U.S. Geological Survey,","doi":"10.3133/ofr811055","usgsCitation":"Wagner, L., 1982, Drainage areas of New York streams, by river basins; a stream gazetteer; Part 1, Data compiled as of October 1980: U.S. Geological Survey Open-File Report 81-1055, 365 p., 1 over-size sheet, maps (1 col.) ;28 cm., https://doi.org/10.3133/ofr811055.","productDescription":"365 p., 1 over-size sheet, maps (1 col.) ;28 cm.","costCenters":[],"links":[{"id":144574,"rank":0,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/of/1981/1055/report-thumb.jpg"},{"id":39399,"rank":400,"type":{"id":17,"text":"Plate"},"url":"https://pubs.usgs.gov/of/1981/1055/plate-1.pdf","linkFileType":{"id":1,"text":"pdf"}},{"id":39400,"rank":300,"type":{"id":11,"text":"Document"},"url":"https://pubs.usgs.gov/of/1981/1055/report.pdf","linkFileType":{"id":1,"text":"pdf"}}],"noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"4f4e4a5ee4b07f02db633c77","contributors":{"authors":[{"text":"Wagner, L.A.","contributorId":12427,"corporation":false,"usgs":true,"family":"Wagner","given":"L.A.","email":"","affiliations":[],"preferred":false,"id":163323,"contributorType":{"id":1,"text":"Authors"},"rank":1}]}} ,{"id":11560,"text":"ofr8291 - 1982 - Selected climatic characteristics of the southeastern Uinta Basin, Utah and Colorado","interactions":[],"lastModifiedDate":"2019-07-10T09:03:39","indexId":"ofr8291","displayToPublicDate":"1994-01-01T00:00:00","publicationYear":"1982","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":"82-91","title":"Selected climatic characteristics of the southeastern Uinta Basin, Utah and Colorado","docAbstract":"The southeastern Uinta Basin in Utah and Colorado contains large reserves of oil shale, the mining of which could affect the area 's water resources. Climatic characteristics of the area, which were evaluated as one phase of a comprehensive hydrologic study, are presented to help provide the means of evaluating the impact of mining on the area 's water resources. Data for precipitation , air temperature, and evaporation obtained by the U.S. Geological Survey from October 1974 to September 1978, and similar short-term data obtained by other Federal agencies at sites in and near the study area, were tabulated and adjusted to a 1941-70 base period. For all sites with incomplete records for 1941-70, the data were adjusted by relating them to concurrent data collected at one or more long-term National Oceanic and Atmospheric Administration sites. Maps were prepared showing areal variance for normal annual precipitation, normal annual air temperature, and normal annual pan evaporation.. The normal annual precipitation ranges from less than 8 inches for altitudes under 5,000 feet to more than 20 inches above 9,000 feet. The normal annual air temperature ranges from 37 to 47 degrees Fahrenheit and varies inversely with altitude and latitude. The normal annual pan evaporation ranges from 42 to 60 inches and varies directly with normal annual air temperature. Although not mapped, it is shown that the normal April 1 water content of the snowpack increases from about 5 inches at 7,000 feet to about 11 inches at 9,000 feet. In addition, the year-to-year and within-year variances of some climatic characteristics are illustrated. The standard error of estimate when relating normal annual precipitation to altitude is 17%, which is equivalent to the standard error when relating the average for 5 years of observed record at a site to the long-term mean at the site. Thus, it appears that additional observation points would not improve areal coverage unless the observation sites were continued for 5 years or longer. (USGS)","language":"English","publisher":"U.S. Geological Survey","publisherLocation":"Reston, VA","doi":"10.3133/ofr8291","usgsCitation":"Waltemeyer, S., 1982, Selected climatic characteristics of the southeastern Uinta Basin, Utah and Colorado: U.S. Geological Survey Open-File Report 82-91, Report: vi, 33 p.; 3 Plates: 22.25 x 27.14 inches or smaller, https://doi.org/10.3133/ofr8291.","productDescription":"Report: vi, 33 p.; 3 Plates: 22.25 x 27.14 inches or smaller","costCenters":[],"links":[{"id":145786,"rank":0,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/of/1982/0091/report-thumb.jpg"},{"id":365406,"rank":2,"type":{"id":11,"text":"Document"},"url":"https://pubs.usgs.gov/of/1982/0091/report.pdf","linkFileType":{"id":1,"text":"pdf"}},{"id":365407,"rank":3,"type":{"id":17,"text":"Plate"},"url":"https://pubs.usgs.gov/of/1982/0091/plate-3.pdf","linkFileType":{"id":1,"text":"pdf"}},{"id":365408,"rank":4,"type":{"id":17,"text":"Plate"},"url":"https://pubs.usgs.gov/of/1982/0091/plate-2.pdf","linkFileType":{"id":1,"text":"pdf"}},{"id":365409,"rank":5,"type":{"id":17,"text":"Plate"},"url":"https://pubs.usgs.gov/of/1982/0091/plate-1.pdf","linkFileType":{"id":1,"text":"pdf"}}],"country":"United States","state":"Colorado, Utah","otherGeospatial":"Uinta Basin","noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"4f4e4a08e4b07f02db5fa2c7","contributors":{"authors":[{"text":"Waltemeyer, S. D.","contributorId":65857,"corporation":false,"usgs":true,"family":"Waltemeyer","given":"S. D.","affiliations":[],"preferred":false,"id":163358,"contributorType":{"id":1,"text":"Authors"},"rank":1}]}} ,{"id":10185,"text":"ofr81916 - 1982 - Hydrologic data for the Potomac Formation in New Castle County, Delaware","interactions":[],"lastModifiedDate":"2017-07-12T11:17:36","indexId":"ofr81916","displayToPublicDate":"1994-01-01T00:00:00","publicationYear":"1982","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":"81-916","title":"Hydrologic data for the Potomac Formation in New Castle County, Delaware","docAbstract":"Hydrologic data for the Potomac Formation in New Castle County, Delaware, consist of records of historical ground-water pumpage, water levels, water quality, and surface-water discharge. This report includes records of 405 wells and hydro-graphs of water levels in 86 wells. Pumpage from 20 well fields is reported. Also included are stream-discharge hydrographs for 6 stations for water years 1979 and 1980 and historical low-flow measurements for 22 stations.
In the analysis of 23 aquifer tests, transmissivity and storage coefficient values for the Potomac Formation range from 454 to 8,480 feet squared per day and 3.8X10-3 to 5.6X10-5, respectively. Vertical hydraulic conductivities of the confining bed range from 0.0083 to 3.2 feet per day.
","language":"English","publisher":"U.S. Geological Survey","doi":"10.3133/ofr81916","usgsCitation":"Martin, M.M., and Denver, J.M., 1982, Hydrologic data for the Potomac Formation in New Castle County, Delaware: U.S. Geological Survey Open-File Report 81-916, ix, 148 p., https://doi.org/10.3133/ofr81916.","productDescription":"ix, 148 p.","numberOfPages":"161","costCenters":[],"links":[{"id":143061,"rank":0,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/of/1981/0916/report-thumb.jpg"},{"id":343702,"rank":2,"type":{"id":11,"text":"Document"},"url":"https://pubs.usgs.gov/of/1981/0916/report.pdf","linkFileType":{"id":1,"text":"pdf"}}],"country":"United States","state":"Delaware","county":"New Castle 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Castle\",\"state\":\"DE\"}}]}","noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"4f4e4ac9e4b07f02db67c6f8","contributors":{"authors":[{"text":"Martin, Mary M.","contributorId":15207,"corporation":false,"usgs":true,"family":"Martin","given":"Mary","email":"","middleInitial":"M.","affiliations":[],"preferred":false,"id":160961,"contributorType":{"id":1,"text":"Authors"},"rank":1},{"text":"Denver, Judith M. jmdenver@usgs.gov","contributorId":140022,"corporation":false,"usgs":true,"family":"Denver","given":"Judith","email":"jmdenver@usgs.gov","middleInitial":"M.","affiliations":[{"id":374,"text":"Maryland Water Science Center","active":true,"usgs":true}],"preferred":false,"id":160962,"contributorType":{"id":1,"text":"Authors"},"rank":2}]}} ,{"id":11678,"text":"ofr82874 - 1982 - Plan for hydrologic study of an area to be surface mined for coal in northwestern Colorado","interactions":[],"lastModifiedDate":"2012-02-02T00:06:39","indexId":"ofr82874","displayToPublicDate":"1994-01-01T00:00:00","publicationYear":"1982","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":"82-874","title":"Plan for hydrologic study of an area to be surface mined for coal in northwestern Colorado","docAbstract":"A data-collection network was established in 1980 in northwestern Colorado in a drainage basin which may be surface mined for coal. This report describes the work plan set up to study the premining hydrology of this area near Steamboat Springs, Routt County, Colorado. The bedrock, alluvial, and surface-water systems as well as the climatic inputs to these systems, are monitored for this study.","language":"ENGLISH","publisher":"U.S. Geological Survey,","doi":"10.3133/ofr82874","usgsCitation":"Williams, R., and Driver, N.E., 1982, Plan for hydrologic study of an area to be surface mined for coal in northwestern Colorado: U.S. Geological Survey Open-File Report 82-874, iv, 23 p. :ill., maps ;28 cm., https://doi.org/10.3133/ofr82874.","productDescription":"iv, 23 p. :ill., maps ;28 cm.","costCenters":[],"links":[{"id":145570,"rank":0,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/of/1982/0874/report-thumb.jpg"},{"id":39551,"rank":300,"type":{"id":11,"text":"Document"},"url":"https://pubs.usgs.gov/of/1982/0874/report.pdf","linkFileType":{"id":1,"text":"pdf"}}],"noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"4f4e4ad6e4b07f02db68432a","contributors":{"authors":[{"text":"Williams, Robert S.","contributorId":55444,"corporation":false,"usgs":true,"family":"Williams","given":"Robert S.","affiliations":[],"preferred":false,"id":163558,"contributorType":{"id":1,"text":"Authors"},"rank":1},{"text":"Driver, Nancy E.","contributorId":67858,"corporation":false,"usgs":true,"family":"Driver","given":"Nancy","email":"","middleInitial":"E.","affiliations":[],"preferred":false,"id":163559,"contributorType":{"id":1,"text":"Authors"},"rank":2}]}} ]}