{"pageNumber":"1619","pageRowStart":"40450","pageSize":"25","recordCount":46644,"records":[{"id":10761,"text":"ofr82865 - 1982 - An evaluation of Idaho stream-gaging networks","interactions":[],"lastModifiedDate":"2012-02-02T00:06:24","indexId":"ofr82865","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":"82-865","title":"An evaluation of Idaho stream-gaging networks","docAbstract":"Network Analysis for Regional Information (NARI) and the Cost-Effectiveness Procedure were tested by applying them to stream-gaging networks in Idaho. NARI was used to determine network design strategies that would maximize the value of additional data. Value of data was measured as the decrease in the probable true standards error of regional regression equations. NARI indicated that no significant decrease in regression error can be achieved by the collection of additional data and that better models should be sought. No major modifications to NARI are necessary to make it widely applicable. The Cost-Effectiveness Procedure was used to determine optimal network operation strategies. It showed network uncertainty can be reduced when six- or one-visit per year minimum constraints are in force. Sensitivity to various cost factors was examined. Attempts to model networks that included sites for collection of groundwater and water-quality data were unsuccessful. (USGS)","language":"ENGLISH","publisher":"U.S. Geological Survey,","doi":"10.3133/ofr82865","usgsCitation":"Quillian, E., and Harenberg, W., 1982, An evaluation of Idaho stream-gaging networks: U.S. Geological Survey Open-File Report 82-865, 61 p., ill. ;28 cm., https://doi.org/10.3133/ofr82865.","productDescription":"61 p., ill. ;28 cm.","costCenters":[],"links":[{"id":143385,"rank":0,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/of/1982/0865/report-thumb.jpg"},{"id":38570,"rank":300,"type":{"id":11,"text":"Document"},"url":"https://pubs.usgs.gov/of/1982/0865/report.pdf","linkFileType":{"id":1,"text":"pdf"}}],"noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"4f4e4afbe4b07f02db696054","contributors":{"authors":[{"text":"Quillian, E.W.","contributorId":38561,"corporation":false,"usgs":true,"family":"Quillian","given":"E.W.","email":"","affiliations":[],"preferred":false,"id":161915,"contributorType":{"id":1,"text":"Authors"},"rank":1},{"text":"Harenberg, W. A.","contributorId":78743,"corporation":false,"usgs":true,"family":"Harenberg","given":"W. A.","affiliations":[],"preferred":false,"id":161916,"contributorType":{"id":1,"text":"Authors"},"rank":2}]}}
,{"id":10756,"text":"ofr82105 - 1982 - Hydrology of potential mining areas in the Warrior coal field, Alabama","interactions":[],"lastModifiedDate":"2012-02-02T00:06:23","indexId":"ofr82105","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":"82-105","title":"Hydrology of potential mining areas in the Warrior coal field, Alabama","docAbstract":"Hydrologic data for four small basins and for numerous other sites in the Warrior coal field are used to define the potential impact of surface mining on water resources. Bear and Blue Creek basins are underlain predominantly by relatively impermeable consolidated rocks in the Pottsville Formation. Turkey and Yellow Creek basins are underlain predominantly by permeable unconsolidated rocks in the Coker Formation. \r\n\r\nWell yields from the Pottsville Formation generally range from 0 to 5 gallons per minute and those from the Coker Formation generally range from 5 to 100 gallons per minute. With the exception of locally objectional concentrations of dissolved iron and manganese, ground water in the basins is suitable for most uses. \r\n\r\nStreamflow distribution reflects seasonal precipitation. Storm runoff is characterized by concentrated peakflows of short duration that rapidly recede to low flow. Streams draining basins underlain mainly by the Pottsville Formation frequently go dry, whereas those draining basins underlain chiefly by the Coker Formation have well-sustained low flows.\r\n\r\nSurface water is generally acidic and low in dissolved solids. Water in streams draining basins underlain chiefly by the Pottsville Formation is slightly more mineralized and less acidic than water in streams draining areas underlain chiefly by the Coker Formation. Climatic, physiographic, hydrologic, and land-use data are analyzed by regressions to derive relations for estimating water quality in streams draining mined and unmined areas. \r\n\r\nThe impacts of mining on the hydrologic systems are identified as increased erosion and sedimentation, baseflow augmentation, decline in groundwater levels, and degradation of water quality. \r\n\r\nA digital model was calibrated to simulate streamflow for Bear, Blue, and Yellow Creeks under unmined conditions. The model, when calibrated and verified under mined and unmined conditions, can be coupled with developed water-quality relationships. This will permit a general examination of .surface-water characteristics (quantity and quality), and estimation of hydrologic impacts that will result from surface mining.","language":"ENGLISH","publisher":"U.S. Geological Survey,","doi":"10.3133/ofr82105","usgsCitation":"Puente, C., and Newton, J., 1982, Hydrology of potential mining areas in the Warrior coal field, Alabama: U.S. Geological Survey Open-File Report 82-105, 117 p., 10 over-size sheets, ill., maps ;28 cm., https://doi.org/10.3133/ofr82105.","productDescription":"117 p., 10 over-size sheets, ill., maps ;28 cm.","costCenters":[],"links":[{"id":112942,"rank":410,"type":{"id":17,"text":"Plate"},"url":"https://pubs.usgs.gov/of/1982/0105/plate-figure_02.pdf","size":"2786","linkFileType":{"id":1,"text":"pdf"}},{"id":112943,"rank":411,"type":{"id":17,"text":"Plate"},"url":"https://pubs.usgs.gov/of/1982/0105/plate-figure_03.pdf","size":"3319","linkFileType":{"id":1,"text":"pdf"}},{"id":112944,"rank":412,"type":{"id":17,"text":"Plate"},"url":"https://pubs.usgs.gov/of/1982/0105/plate-figure_07.pdf","size":"507","linkFileType":{"id":1,"text":"pdf"}},{"id":112945,"rank":413,"type":{"id":17,"text":"Plate"},"url":"https://pubs.usgs.gov/of/1982/0105/plate-figure_16.pdf","size":"645","linkFileType":{"id":1,"text":"pdf"}},{"id":112946,"rank":414,"type":{"id":17,"text":"Plate"},"url":"https://pubs.usgs.gov/of/1982/0105/plate-figure_17.pdf","size":"485","linkFileType":{"id":1,"text":"pdf"}},{"id":112947,"rank":415,"type":{"id":17,"text":"Plate"},"url":"https://pubs.usgs.gov/of/1982/0105/plate-figure_18.pdf","size":"263","linkFileType":{"id":1,"text":"pdf"}},{"id":112948,"rank":416,"type":{"id":17,"text":"Plate"},"url":"https://pubs.usgs.gov/of/1982/0105/plate-figure_20.pdf","size":"2434","linkFileType":{"id":1,"text":"pdf"}},{"id":112949,"rank":417,"type":{"id":17,"text":"Plate"},"url":"https://pubs.usgs.gov/of/1982/0105/plate-figure_21.pdf","size":"3675","linkFileType":{"id":1,"text":"pdf"}},{"id":112950,"rank":418,"type":{"id":17,"text":"Plate"},"url":"https://pubs.usgs.gov/of/1982/0105/plate-figure_22.pdf","size":"2647","linkFileType":{"id":1,"text":"pdf"}},{"id":143601,"rank":0,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/of/1982/0105/report-thumb.jpg"},{"id":38562,"rank":300,"type":{"id":11,"text":"Document"},"url":"https://pubs.usgs.gov/of/1982/0105/report.pdf","linkFileType":{"id":1,"text":"pdf"}}],"noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"4f4e4a0ee4b07f02db5fdaff","contributors":{"authors":[{"text":"Puente, Celso","contributorId":36140,"corporation":false,"usgs":true,"family":"Puente","given":"Celso","email":"","affiliations":[],"preferred":false,"id":161909,"contributorType":{"id":1,"text":"Authors"},"rank":1},{"text":"Newton, J.G.","contributorId":71552,"corporation":false,"usgs":true,"family":"Newton","given":"J.G.","email":"","affiliations":[],"preferred":false,"id":161910,"contributorType":{"id":1,"text":"Authors"},"rank":2}]}}
,{"id":10755,"text":"ofr81540 - 1982 - Assessment of hydrologic conditions in potential coal-lease tracts in the Warrior coal field, Alabama","interactions":[],"lastModifiedDate":"2012-02-02T00:06:23","indexId":"ofr81540","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":"81-540","title":"Assessment of hydrologic conditions in potential coal-lease tracts in the Warrior coal field, Alabama","docAbstract":"Assessing the hydrology of potential Federal coal-lease tracts, because of their dissemination and limited data, requires some predictive capability. Four tracts assessed were located in the outcrop of three coal groups and of other relatively impermeable rocks in the Pottsville Formation. Physical settings of the tracts and most other areas in the Warrior coal field are similar. This results in similar ground-water and surface-water characteristics, in similar impacts resulting from surface coal mining, and in maximizing the transfer-ability of data. Assessments of the tracts reflected the small storage of water in underlying rocks and corresponding low yields to wells and to the base flow of streams. Ground water and surface water in undisturbed areas are generally of good quality. Some subbasins in the tracts have already been impacted by mining. Estimates of streamflow characteristics and the availability and quality of ground water in the tracts were made using available methodology , or assessments based on local and regional data. Estimates of the degree mineralization of surface-water were made using methodology developed from other coal hydrology work. Climatic, physiographic, hydrologic, and land-use data were analyzed by regressions to derive relations for assessing water quality in streams draining mined and unmined areas. In this approach, an equation was derived to estimate specific conductance. Additional equations, based on relations between specific conductance and other constituents, allow estimates of mine drainage indicators such as hardness, dissolved solids, and sulfate. Hydrologic assessments of the tracts, based on limited verification data, proved to be reasonably accurate. (USGS)","language":"ENGLISH","publisher":"U.S. Geological Survey,","doi":"10.3133/ofr81540","usgsCitation":"Puente, C., Newton, J., and Bingham, R.H., 1982, Assessment of hydrologic conditions in potential coal-lease tracts in the Warrior coal field, Alabama: U.S. Geological Survey Open-File Report 81-540, v, 47 p. :ill., maps ;28 cm., https://doi.org/10.3133/ofr81540.","productDescription":"v, 47 p. :ill., maps ;28 cm.","costCenters":[],"links":[{"id":143600,"rank":0,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/of/1981/0540/report-thumb.jpg"},{"id":38560,"rank":400,"type":{"id":17,"text":"Plate"},"url":"https://pubs.usgs.gov/of/1981/0540/plate-1.pdf","linkFileType":{"id":1,"text":"pdf"}},{"id":38561,"rank":300,"type":{"id":11,"text":"Document"},"url":"https://pubs.usgs.gov/of/1981/0540/report.pdf","linkFileType":{"id":1,"text":"pdf"}}],"noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"4f4e4abae4b07f02db671f72","contributors":{"authors":[{"text":"Puente, Celso","contributorId":36140,"corporation":false,"usgs":true,"family":"Puente","given":"Celso","email":"","affiliations":[],"preferred":false,"id":161907,"contributorType":{"id":1,"text":"Authors"},"rank":1},{"text":"Newton, John F.","contributorId":13985,"corporation":false,"usgs":true,"family":"Newton","given":"John F.","affiliations":[],"preferred":false,"id":161906,"contributorType":{"id":1,"text":"Authors"},"rank":2},{"text":"Bingham, Roy H.","contributorId":56632,"corporation":false,"usgs":true,"family":"Bingham","given":"Roy","email":"","middleInitial":"H.","affiliations":[],"preferred":false,"id":161908,"contributorType":{"id":1,"text":"Authors"},"rank":3}]}}
,{"id":10630,"text":"ofr82504 - 1982 - Quality of runoff from small watersheds in the Twin Cities metropolitan area, Minnesota: Hydrologic data for 1980","interactions":[],"lastModifiedDate":"2018-03-19T10:48:45","indexId":"ofr82504","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":"82-504","title":"Quality of runoff from small watersheds in the Twin Cities metropolitan area, Minnesota: Hydrologic data for 1980","docAbstract":"<p>An intensive study of nonpoint-source runoff was conducted in the Twin Cities metropolitan area in Minnesota during 1980. The purpose of the study was to determine the relationships between land use, watershed characteristics, and the quantity, quality, and timing of runoff.</p>\n<p>Discharge and water-quality data were collected at 19 sites located in 6 rural and 4 urban watersheds. Basin characteristics and land use were determined for each watershed. Recording instruments provided continuous discharge records at 17 sites and continuous rainfall records at 12 sites. Automatic samplers were used at 12 sites. Water-quality samples were collected at 15- to 60-minute intervals during periods of increased runoff. Samples were collected periodically during low flow. Primary emphasis was placed on analysis of samples for suspended solids, nutrients, and oxygen-demanding constituents. Secondary emphasis was placed on analysis for chloride, metals, bacteria, pesticides, and PCB's. Wetfall and dryfall precipitation-quality data were collected at six sites.</p>\n<p>Discharge and water-quality data were used to calculate storm and daily loads of chemical oxygen demand, total suspended solids, ammonia plus organic nitrogen, nitrite plus nitrate-nitrogen, total phosphorus, chloride, and lead.</p>\n<p>All data collected during the study are documented in tables that contain watershed characteristics and land use, daily and unit values for discharge and rainfall, rainfall characteristics, water-quality data for runoff and precipitation, results of laboratory settling tests, results of quality-assurance tests, dally loads, and storm loads.</p>","language":"English","publisher":"U.S. Geological Survey","publisherLocation":"St. Paul, MN","doi":"10.3133/ofr82504","collaboration":"Prepared in cooperation with the Metropolitan Council of the Twin Cities","usgsCitation":"Payne, G.A., Ayers, M.A., and Brown, R.G., 1982, Quality of runoff from small watersheds in the Twin Cities metropolitan area, Minnesota: Hydrologic data for 1980: U.S. Geological Survey Open-File Report 82-504, iv, 289 p., https://doi.org/10.3133/ofr82504.","productDescription":"iv, 289 p.","onlineOnly":"N","additionalOnlineFiles":"N","costCenters":[{"id":392,"text":"Minnesota Water Science Center","active":true,"usgs":true}],"links":[{"id":142533,"rank":0,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/of/1982/0504/report-thumb.jpg"},{"id":38464,"rank":300,"type":{"id":11,"text":"Document"},"url":"https://pubs.usgs.gov/of/1982/0504/report.pdf","linkFileType":{"id":1,"text":"pdf"}}],"country":"United States","state":"Minnesota","otherGeospatial":"Twin Cities 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\"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,{"id":48764,"text":"ofr82300F - 1982 - Preliminary geomagnetic data, College Observatory, Fairbanks, Alaska: June 1982","interactions":[],"lastModifiedDate":"2024-05-03T21:17:36.105011","indexId":"ofr82300F","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":"82-300","chapter":"F","title":"Preliminary geomagnetic data, College Observatory, Fairbanks, Alaska: June 1982","docAbstract":"<p>The preliminary geomagnetic data included here is made available to scientific personnel and organizations, as part of a cooperative effort and on a data exchange basis because of the early need by some users. To avoid delay, all of the data is copied from original forms processed at the observatory; therefore it should be regarded as preliminary.</p>","language":"English","publisher":"U.S. Geological Survey","doi":"10.3133/ofr82300F","usgsCitation":"Townshend, J.B., Papp, J., Sauter, E., Torrence, L., and Cunningham, T., 1982, Preliminary geomagnetic data, College Observatory, Fairbanks, Alaska: June 1982: U.S. Geological Survey Open-File Report 82-300, 25 p., https://doi.org/10.3133/ofr82300F.","productDescription":"25 p.","costCenters":[],"links":[{"id":428365,"rank":2,"type":{"id":11,"text":"Document"},"url":"https://pubs.usgs.gov/of/1982/0300-f/report.pdf","linkFileType":{"id":1,"text":"pdf"}},{"id":162578,"rank":1,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/of/1982/0300-f/report-thumb.jpg"}],"country":"United States","state":"Alaska","city":"Fairbanks","otherGeospatial":"College Observatory","geographicExtents":"{\n  \"type\": \"FeatureCollection\",\n  \"features\": [\n    {\n      \"type\": \"Feature\",\n      \"properties\": {},\n      \"geometry\": {\n        \"coordinates\": [\n          [\n            [\n              -147.9716829972995,\n              64.92275521538983\n            ],\n            [\n              -147.9716829972995,\n              64.77266196148724\n            ],\n            [\n              -147.4142995458633,\n              64.77266196148724\n            ],\n            [\n              -147.4142995458633,\n              64.92275521538983\n            ],\n            [\n              -147.9716829972995,\n              64.92275521538983\n            ]\n          ]\n        ],\n        \"type\": \"Polygon\"\n      }\n    }\n  ]\n}","noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"4f4e4abde4b07f02db673bac","contributors":{"authors":[{"text":"Townshend, John B.","contributorId":70383,"corporation":false,"usgs":true,"family":"Townshend","given":"John","email":"","middleInitial":"B.","affiliations":[],"preferred":false,"id":238184,"contributorType":{"id":1,"text":"Authors"},"rank":1},{"text":"Papp, J.E.","contributorId":95057,"corporation":false,"usgs":true,"family":"Papp","given":"J.E.","email":"","affiliations":[],"preferred":false,"id":238187,"contributorType":{"id":1,"text":"Authors"},"rank":2},{"text":"Sauter, E.A.","contributorId":51738,"corporation":false,"usgs":true,"family":"Sauter","given":"E.A.","email":"","affiliations":[],"preferred":false,"id":238185,"contributorType":{"id":1,"text":"Authors"},"rank":3},{"text":"Torrence, L.Y.","contributorId":62587,"corporation":false,"usgs":true,"family":"Torrence","given":"L.Y.","email":"","affiliations":[],"preferred":false,"id":238186,"contributorType":{"id":1,"text":"Authors"},"rank":4},{"text":"Cunningham, T.K.","contributorId":103270,"corporation":false,"usgs":true,"family":"Cunningham","given":"T.K.","email":"","affiliations":[],"preferred":false,"id":900123,"contributorType":{"id":1,"text":"Authors"},"rank":5}]}}
,{"id":10620,"text":"ofr82397 - 1982 - MRNIDX - Marine Data Index: Database Description, Operation, Retrieval, and Display","interactions":[],"lastModifiedDate":"2012-02-02T00:06:21","indexId":"ofr82397","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":"82-397","title":"MRNIDX - Marine Data Index: Database Description, Operation, Retrieval, and Display","docAbstract":"A database referencing the location and content of data stored on magnetic medium was designed to assist in the indexing of time-series and spatially dependent marine geophysical data collected or processed by the U. S. Geological Survey. The database was designed and created for input to the Geologic Retrieval and Synopsis Program (GRASP) to allow selective retrievals of information pertaining to location of data, data format, cruise, geographical bounds and collection dates of data. This information is then used to locate the stored data for administrative purposes or further processing. \r\n\r\nDatabase utilization is divided into three distinct operations. The first is the inventorying of the data and the updating of the database, the second is the retrieval of information from the database, and the third is the graphic display of the geographical boundaries to which the retrieved information pertains.","language":"ENGLISH","publisher":"Geological Survey (U.S.)","doi":"10.3133/ofr82397","usgsCitation":"Paskevich, V.F., 1982, MRNIDX - Marine Data Index: Database Description, Operation, Retrieval, and Display: U.S. Geological Survey Open-File Report 82-397, iii, 57 p., https://doi.org/10.3133/ofr82397.","productDescription":"iii, 57 p.","costCenters":[{"id":680,"text":"Woods Hole Science Center","active":false,"usgs":true}],"links":[{"id":142487,"rank":0,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/of/1982/0397/report-thumb.jpg"},{"id":9764,"rank":100,"type":{"id":15,"text":"Index Page"},"url":"https://woodshole.er.usgs.gov/pubs/of1982_397/","linkFileType":{"id":5,"text":"html"}},{"id":38452,"rank":300,"type":{"id":11,"text":"Document"},"url":"https://pubs.usgs.gov/of/1982/0397/report.pdf","linkFileType":{"id":1,"text":"pdf"}}],"noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"4f4e4a7fe4b07f02db648d9c","contributors":{"authors":[{"text":"Paskevich, Valerie F.","contributorId":81907,"corporation":false,"usgs":true,"family":"Paskevich","given":"Valerie","email":"","middleInitial":"F.","affiliations":[],"preferred":false,"id":161694,"contributorType":{"id":1,"text":"Authors"},"rank":1}]}}
,{"id":48770,"text":"ofr82300L - 1982 - Preliminary geomagnetic data, College Observatory, Fairbanks, Alaska, December 1982","interactions":[],"lastModifiedDate":"2012-02-02T00:10:06","indexId":"ofr82300L","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":"82-300","chapter":"L","title":"Preliminary geomagnetic data, College Observatory, Fairbanks, Alaska, December 1982","language":"ENGLISH","doi":"10.3133/ofr82300L","usgsCitation":"Townshend, J., Papp, J., Sauter, E., and Torrence, L., 1982, Preliminary geomagnetic data, College Observatory, Fairbanks, Alaska, December 1982: U.S. Geological Survey Open-File Report 82-300, 25 p.; 12 v. : ill. ; 28 cm., https://doi.org/10.3133/ofr82300L.","productDescription":"25 p.; 12 v. : ill. ; 28 cm.","costCenters":[],"links":[{"id":162847,"rank":0,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/of/1982/0300l/report-thumb.jpg"},{"id":85567,"rank":300,"type":{"id":11,"text":"Document"},"url":"https://pubs.usgs.gov/of/1982/0300l/report.pdf","linkFileType":{"id":1,"text":"pdf"}}],"noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"4f4e4abde4b07f02db673de9","contributors":{"authors":[{"text":"Townshend, J.B.","contributorId":30623,"corporation":false,"usgs":true,"family":"Townshend","given":"J.B.","email":"","affiliations":[],"preferred":false,"id":238208,"contributorType":{"id":1,"text":"Authors"},"rank":1},{"text":"Papp, J.E.","contributorId":95057,"corporation":false,"usgs":true,"family":"Papp","given":"J.E.","email":"","affiliations":[],"preferred":false,"id":238211,"contributorType":{"id":1,"text":"Authors"},"rank":2},{"text":"Sauter, E.A.","contributorId":51738,"corporation":false,"usgs":true,"family":"Sauter","given":"E.A.","email":"","affiliations":[],"preferred":false,"id":238209,"contributorType":{"id":1,"text":"Authors"},"rank":3},{"text":"Torrence, L.Y.","contributorId":62587,"corporation":false,"usgs":true,"family":"Torrence","given":"L.Y.","email":"","affiliations":[],"preferred":false,"id":238210,"contributorType":{"id":1,"text":"Authors"},"rank":4}]}}
,{"id":48773,"text":"ofr82462 - 1982 - Geochemical and geostatistical evaluation, Arkansas Canyon Planning Unit, Fremont and Custer Counties, Colorado","interactions":[],"lastModifiedDate":"2022-10-04T19:33:19.166239","indexId":"ofr82462","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":"82-462","title":"Geochemical and geostatistical evaluation, Arkansas Canyon Planning Unit, Fremont and Custer Counties, Colorado","docAbstract":"A mineral assessment of the Arkansas Canyon Planning Unit was undertaken by Barringer Resources Inc., under the terms of contract YA-553-CTO-100 with the Bureau of Land Management, Colorado State Office. The study was based on a geochemical-geostatistical survey in which 700 stream sediment samples were collected and analyzed for 25 elements. Geochemical results were interpreted by statistical processing which included factor, discriminant, multiple regression and characteristic analysis. \r\n\r\nThe major deposit types evaluated were massive sulfide-base metal, sedimentary and magmatic uranium, thorium vein, magmatic segregation, and carbonatite related deposits. Results of the single element data and multivariate geostatistical analysis indicate that limited potential exists for base metal mineralization near the Horseshoe, El Plomo, and Green Mountain Mines. Thirty areas are considered to be anomalous with regard to one or more of the geochemical parameters evaluated during this study. The evaluation of carbonatite related mineralization was restricted due to the lack of geochemical data specific to this environment.","language":"English","publisher":"U.S. Geological Survey","doi":"10.3133/ofr82462","usgsCitation":"Weiland, E.F., Connors, R.A., Robinson, M.L., Lindemann, J.W., and Meyer, W.T., 1982, Geochemical and geostatistical evaluation, Arkansas Canyon Planning Unit, Fremont and Custer Counties, Colorado: U.S. Geological Survey Open-File Report 82-462, Report: iv, 108 p.; 30 Plates: 50.75 × 32.56 inches or smaller, https://doi.org/10.3133/ofr82462.","productDescription":"Report: iv, 108 p.; 30 Plates: 50.75 × 32.56 inches or smaller","costCenters":[],"links":[{"id":407876,"rank":33,"type":{"id":36,"text":"NGMDB Index 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States","state":"Colorado","county":"Custer County, Fremont County","otherGeospatial":"Arkansas Canyon Planning Unit","geographicExtents":"{\n  \"type\": \"FeatureCollection\",\n  \"features\": [\n    {\n      \"type\": \"Feature\",\n      \"properties\": {},\n      \"geometry\": {\n        \"type\": \"Polygon\",\n        \"coordinates\": [\n          [\n            [\n              -105.715,\n              38.225\n            ],\n            [\n              -105.302,\n              38.225\n            ],\n            [\n              -105.302,\n              38.487\n            ],\n            [\n              -105.715,\n              38.487\n            ],\n            [\n              -105.715,\n              38.225\n            ]\n          ]\n        ]\n      }\n    }\n  ]\n}","noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"4f4e4b24e4b07f02db6ae732","contributors":{"authors":[{"text":"Weiland, E. F.","contributorId":43403,"corporation":false,"usgs":true,"family":"Weiland","given":"E.","email":"","middleInitial":"F.","affiliations":[],"preferred":false,"id":238219,"contributorType":{"id":1,"text":"Authors"},"rank":1},{"text":"Connors, R. A.","contributorId":24347,"corporation":false,"usgs":true,"family":"Connors","given":"R.","email":"","middleInitial":"A.","affiliations":[],"preferred":false,"id":238217,"contributorType":{"id":1,"text":"Authors"},"rank":2},{"text":"Robinson, M. L.","contributorId":108157,"corporation":false,"usgs":true,"family":"Robinson","given":"M.","email":"","middleInitial":"L.","affiliations":[],"preferred":false,"id":238221,"contributorType":{"id":1,"text":"Authors"},"rank":3},{"text":"Lindemann, J. W.","contributorId":70756,"corporation":false,"usgs":true,"family":"Lindemann","given":"J.","email":"","middleInitial":"W.","affiliations":[],"preferred":false,"id":238220,"contributorType":{"id":1,"text":"Authors"},"rank":4},{"text":"Meyer, W. T.","contributorId":24825,"corporation":false,"usgs":true,"family":"Meyer","given":"W.","email":"","middleInitial":"T.","affiliations":[],"preferred":false,"id":238218,"contributorType":{"id":1,"text":"Authors"},"rank":5}]}}
,{"id":10613,"text":"ofr811011 - 1982 - Ground-water quality in east-central Idaho valleys","interactions":[],"lastModifiedDate":"2012-02-02T00:06:21","indexId":"ofr811011","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":"81-1011","title":"Ground-water quality in east-central Idaho valleys","docAbstract":"From May through November 1978, water quality, geologic, and hydrologic data were collected for 108 wells in the Lemhi, Pahsimeroi, Salman River (Stanley to Salmon), Big Lost River, and Little Lost River valleys in east-central Idaho. Data were assembled to define, on a reconnaissance level, water-quality conditions in major aquifers and to develop an understanding of factors that affected conditions in 1978 and could affect future ground-water quality. Water-quality characteristics determined include specific conductance, pH, water temperature, major dissolved cations, major dissolved anions, and coliform bacteria. Concentrations of hardness, nitrite plus nitrate, coliform bacteria, dissolved solids, sulfate, chloride, fluoride , iron, calcium, magnesium, sodium, potassium or bicarbonate exceed public drinking water regulation limits or were anomalously high in some water samples. Highly mineralized ground water probably is due to the natural composition of the aquifers and not to surface contamination. Concentrations of coliform bacteria that exceed public drinking water limits and anomalously high dissolved nitrite-plus-nitrite concentrations are from 15- to 20-year old irrigation wells in heavily irrigated or more densely populated areas of the valleys. Ground-water quality and quantity in most of the study area are sufficient to meet current (1978) population and economic demands. Ground water in all valleys is characterized by significant concentrations of calcium, magnesium, and bicarbonate plus carbonate ions. Variations in the general trend of ground-water composition (especially in the Lemhi Valley) probably are most directly related to variability in aquifer lithology and proximity of sampling site to source of recharge. (USGS)","language":"ENGLISH","publisher":"U.S. Geological Survey,","doi":"10.3133/ofr811011","usgsCitation":"Parliman, D., 1982, Ground-water quality in east-central Idaho valleys: U.S. Geological Survey Open-File Report 81-1011, 62 p., 3 over-size sheets, ill., maps ;35 cm., https://doi.org/10.3133/ofr811011.","productDescription":"62 p., 3 over-size sheets, ill., maps ;35 cm.","costCenters":[],"links":[{"id":142548,"rank":0,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/of/1981/1011/report-thumb.jpg"},{"id":38446,"rank":400,"type":{"id":17,"text":"Plate"},"url":"https://pubs.usgs.gov/of/1981/1011/plate-1.pdf","linkFileType":{"id":1,"text":"pdf"}},{"id":38447,"rank":401,"type":{"id":17,"text":"Plate"},"url":"https://pubs.usgs.gov/of/1981/1011/plate-2.pdf","linkFileType":{"id":1,"text":"pdf"}},{"id":38448,"rank":402,"type":{"id":17,"text":"Plate"},"url":"https://pubs.usgs.gov/of/1981/1011/plate-3.pdf","linkFileType":{"id":1,"text":"pdf"}},{"id":38449,"rank":300,"type":{"id":11,"text":"Document"},"url":"https://pubs.usgs.gov/of/1981/1011/report.pdf","linkFileType":{"id":1,"text":"pdf"}}],"noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"4f4e4aa8e4b07f02db667390","contributors":{"authors":[{"text":"Parliman, D. J.","contributorId":64220,"corporation":false,"usgs":true,"family":"Parliman","given":"D. J.","affiliations":[],"preferred":false,"id":161682,"contributorType":{"id":1,"text":"Authors"},"rank":1}]}}
,{"id":11247,"text":"ofr82701 - 1982 - Preliminary results of gravity investigations at Yucca Mountain and vicinity, southern Nye County, Nevada","interactions":[],"lastModifiedDate":"2024-06-03T17:15:28.48172","indexId":"ofr82701","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":"82-701","title":"Preliminary results of gravity investigations at Yucca Mountain and vicinity, southern Nye County, Nevada","docAbstract":"<p>Exploration for a high-level-nuclear-waste-repository site in the Yucca Mountain area, Nev., resulted in the addition of 423 new gravity stations during the past 2 years to the 934 existing stations to form the data base of this study. About 100 surface-rock samples, three borehole gamma-gamma logs, and one borehole gravity study provide excellent density control. A linear increase in density of 0.26 g/cm3 per km is indicated in the thick tuff sequences. This steady increase of density within the tuff sequences makes the density contrast across the basal contact of the tuff the only strong source of gravity fluctuations. Isostatic and 2.0-g/cm3 Bouguer corrections were applied to the observed gravity values to remove deep-crust-related regional gradients and topographic effects, respectively. The resulting residual-gravity plot shows significant gravity anomalies that correlate closely with the structures inferred from drill-hole and surface geologic studies.</p><p>Gravity highs over the three Paleozoic rock outcrops within the study area--Bare Mountain, the Calico Hills, and the Striped Hills--served as reference points for the gravity models. The Bare Mountain gravity high, which peaks at 48 mGal, connects with a larger gravity high over the Funeral Mountains to the south; together, these highs may result from a continuous block of mildly metamorphosed Precambrian and Paleozoic rocks stretching from the east edge of Death Valley to Bare Mountain. The Calico Hills gravity high appears more likely to originate from a northeast-trending remanent topographic high of buried Paleozoic rocks rather than from an isolated structural dome. This buried ridge may extend southwestward beneath Busted Butte, 5 km southeast of the proposed repository, where 2 1/2- and 3dimensional modeling indicates that the pre-Cenozoic rocks may be less than 1,000 m deep.</p><p>At least 3,000 m of tuff fills a large steep-sided depression in the prevolcanic rocks beneath Yucca Mountain and Crater Flat. The gravity low and thick tuff section probably lie within a large collapse area comprising the Crater Flat-Timber Mountain-Silent Canyon caldera complexes. Gravity lows in Crater Flat itself are thought to coincide with the source areas of the Prow Pass Member, the Bullfrog Member, and the unnamed member of the Crater Flat Tuff. Southward extension of the broad gravity low associated with Crater Flat into the Amargosa Desert is evidence for sector graben-type collapse segments related to Timber Mountain caldera and superimposed on the other structures within Crater Flat.</p>","language":"English","publisher":"U.S. Geological Survey","doi":"10.3133/ofr82701","usgsCitation":"Snyder, D., and Carr, W.J., 1982, Preliminary results of gravity investigations at Yucca Mountain and vicinity, southern Nye County, Nevada: U.S. Geological Survey Open-File Report 82-701, iv, 36 p., https://doi.org/10.3133/ofr82701.","productDescription":"iv, 36 p.","costCenters":[],"links":[{"id":429467,"rank":3,"type":{"id":11,"text":"Document"},"url":"https://pubs.usgs.gov/of/1982/0701/report.pdf","linkFileType":{"id":1,"text":"pdf"}},{"id":39042,"rank":2,"type":{"id":17,"text":"Plate"},"url":"https://pubs.usgs.gov/of/1982/0701/plate-1.pdf","linkFileType":{"id":1,"text":"pdf"}},{"id":143712,"rank":1,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/of/1982/0701/report-thumb.jpg"}],"country":"United States","state":"Nevada","county":"Nye County","otherGeospatial":"Yucca Mountain","geographicExtents":"{\n  \"type\": \"FeatureCollection\",\n  \"features\": [\n    {\n      \"type\": \"Feature\",\n      \"properties\": {},\n      \"geometry\": {\n        \"coordinates\": [\n          [\n            [\n              -116.54199992341728,\n              36.969218668834756\n            ],\n            [\n              -116.54199992341728,\n              36.7955322232273\n            ],\n            [\n              -116.33873566687758,\n              36.7955322232273\n            ],\n            [\n              -116.33873566687758,\n              36.969218668834756\n            ],\n            [\n              -116.54199992341728,\n              36.969218668834756\n            ]\n          ]\n        ],\n        \"type\": \"Polygon\"\n      }\n    }\n  ]\n}","noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"4f4e4aade4b07f02db66b2f8","contributors":{"authors":[{"text":"Snyder, D.B.","contributorId":99141,"corporation":false,"usgs":true,"family":"Snyder","given":"D.B.","email":"","affiliations":[],"preferred":false,"id":162801,"contributorType":{"id":1,"text":"Authors"},"rank":1},{"text":"Carr, W. James","contributorId":16014,"corporation":false,"usgs":true,"family":"Carr","given":"W.","email":"","middleInitial":"James","affiliations":[],"preferred":false,"id":162800,"contributorType":{"id":1,"text":"Authors"},"rank":2}]}}
,{"id":10102,"text":"ofr82386 - 1982 - Programs for filing and plotting U-Pb isotope data for concordia diagrams, using an HP-9830 computer and HP-9862 plotter","interactions":[],"lastModifiedDate":"2012-02-02T00:06:32","indexId":"ofr82386","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":"82-386","title":"Programs for filing and plotting U-Pb isotope data for concordia diagrams, using an HP-9830 computer and HP-9862 plotter","language":"ENGLISH","publisher":"U.S. Geological Survey,","doi":"10.3133/ofr82386","usgsCitation":"Ludwig, K., 1982, Programs for filing and plotting U-Pb isotope data for concordia diagrams, using an HP-9830 computer and HP-9862 plotter: U.S. Geological Survey Open-File Report 82-386, 23 p., 28 cm., https://doi.org/10.3133/ofr82386.","productDescription":"23 p., 28 cm.","costCenters":[],"links":[{"id":143907,"rank":0,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/of/1982/0386/report-thumb.jpg"},{"id":37951,"rank":300,"type":{"id":11,"text":"Document"},"url":"https://pubs.usgs.gov/of/1982/0386/report.pdf","linkFileType":{"id":1,"text":"pdf"}}],"noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"4f4e4a9be4b07f02db65e049","contributors":{"authors":[{"text":"Ludwig, K.R.","contributorId":97112,"corporation":false,"usgs":true,"family":"Ludwig","given":"K.R.","email":"","affiliations":[{"id":218,"text":"Denver Federal Center","active":false,"usgs":true}],"preferred":false,"id":160822,"contributorType":{"id":1,"text":"Authors"},"rank":1}]}}
,{"id":57244,"text":"wdrWV811 - 1982 - Water resources data, West Virginia, water year 1981","interactions":[],"lastModifiedDate":"2025-02-26T20:01:48.171181","indexId":"wdrWV811","displayToPublicDate":"1994-01-01T00:00:00","publicationYear":"1982","noYear":false,"publicationType":{"id":18,"text":"Report"},"publicationSubtype":{"id":5,"text":"USGS Numbered Series"},"seriesTitle":{"id":340,"text":"Water Data Report","code":"WDR","active":false,"publicationSubtype":{"id":5}},"seriesNumber":"WV-81-1","title":"Water resources data, West Virginia, water year 1981","docAbstract":"<p>Water resources data for the 1981 water year for West Virginia consist of records of stage, discharge, and water quality of streams and springs; stage and contents of lakes and reservoirs; and water levels in wells. This report contains discharge records for 120 gaging stations; stage only records for 8 gaging stations; stage and contents for 8 lakes and reservoirs; contents for 1 reservoir; change in contents for 1 reservoir; water quality for 103 gaging stations; and water levels for 35 observation wells. Also included are 2 crest-stage partial-record stations, and 1 low-flow partial record station. Additional water data were collected at various sites, not part of the systematic data collections program, and are published as miscellaneous measurements and analyses. These data represent that part of the National Water Data System operated by the U.S. Geological Survey and cooperating State and Federal Agencies in West Virginia. </p>","language":"English","publisher":"U.S. Geological Survey","doi":"10.3133/wdrWV811","collaboration":"Prepared in cooperation with the State of West Virginia and other agencies","usgsCitation":"Water Resources Division, U.S. Geological Survey, 1982, Water resources data, West Virginia, water year 1981: U.S. Geological Survey Water Data Report WV-81-1, viii, 505 p., https://doi.org/10.3133/wdrWV811.","productDescription":"viii, 505 p.","costCenters":[],"links":[{"id":482450,"rank":2,"type":{"id":11,"text":"Document"},"url":"https://pubs.usgs.gov/wdr/1981/wv-81-1/report.pdf","linkFileType":{"id":1,"text":"pdf"}},{"id":184205,"rank":1,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/thumbnails/usgs_thumb.jpg"}],"country":"United States","state":"West 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Virginia\",\"nation\":\"USA  \"}}]}","noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"4f4e4a08e4b07f02db5fa5b9","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":533045,"contributorType":{"id":1,"text":"Authors"},"rank":1}]}}
,{"id":56874,"text":"wdrME811 - 1982 - Water resources data for Maine, water year 1981","interactions":[],"lastModifiedDate":"2025-08-19T14:30:23.307869","indexId":"wdrME811","displayToPublicDate":"1994-01-01T00:00:00","publicationYear":"1982","noYear":false,"publicationType":{"id":18,"text":"Report"},"publicationSubtype":{"id":5,"text":"USGS Numbered Series"},"seriesTitle":{"id":340,"text":"Water Data Report","code":"WDR","active":false,"publicationSubtype":{"id":5}},"seriesNumber":"ME-81-1","title":"Water resources data for Maine, water year 1981","docAbstract":"<p>Water resources data for the 1981 water year for Maine consist of records of stage, discharge, and water quality of streams; stage and contents of lakes and reservoirs; and water levels and water quality of wells. This report contains discharge records for 66 gaging stations; stage only for 2 gaging stations; contents for 17 lakes and reservoirs; water quality for 19 gaging stations and 8 wells; and water levels for 24 observation wells. Additional water data were collected at various sites, not part of the systematic data collection program, and are published as miscellaneous measurements. These data represent that part of the National Water Data System operated by the U.S. Geological Survey and cooperating State and Federal agencies.</p>","language":"English","publisher":"U.S. Geological Survey","doi":"10.3133/wdrME811","collaboration":"Prepared in cooperation with the State of Maine and with other agencies","usgsCitation":"Water Resources Division, U.S. Geological Survey, 1982, Water resources data for Maine, water year 1981: U.S. Geological Survey Water Data Report ME-81-1, vii, 212 p., https://doi.org/10.3133/wdrME811.","productDescription":"vii, 212 p.","costCenters":[],"links":[{"id":184415,"rank":1,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/wdr/1981/me-81-1/report-thumb.jpg"},{"id":494306,"rank":2,"type":{"id":11,"text":"Document"},"url":"https://pubs.usgs.gov/wdr/1981/me-81-1/report.pdf","linkFileType":{"id":1,"text":"pdf"}}],"country":"United 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,{"id":25600,"text":"wri824076 - 1982 - Hydrologic-information needs for oil-shale development, northwestern Colorado","interactions":[],"lastModifiedDate":"2012-02-02T00:08:28","indexId":"wri824076","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":"82-4076","title":"Hydrologic-information needs for oil-shale development, northwestern Colorado","docAbstract":"Hydrologic information is not adequate for proper development of the large oil-shale reserves of Piceance basin in northwestern Colorado. Exploratory drilling and aquifer testing are needed to define the hydrologic system, to provide wells for aquifer testing, to design mine-drainage techniques, and to explore for additional water supplies. Sampling networks are needed to supply hydrologic data on the quantity and quality of surface water, ground water, and springs. A detailed sampling network is proposed for the White River basin because of expected impacts related to water supplies and waste disposal. Emissions from oil-shale retorts to the atmosphere need additional study because of possible resulting corrosion problems and the destruction of fisheries. Studies of the leachate materials and the stability of disposed retorted shale piles are needed to insure that these materials will not cause problems. Hazards related to in-situ retorts, and the wastes related to oil-shale development in general also need further investigation. (USGS)","language":"ENGLISH","publisher":"U.S. Geological Survey,","doi":"10.3133/wri824076","usgsCitation":"Taylor, O., 1982, Hydrologic-information needs for oil-shale development, northwestern Colorado: U.S. Geological Survey Water-Resources Investigations Report 82-4076, ix, 101 p. :ill., maps ;28 cm., https://doi.org/10.3133/wri824076.","productDescription":"ix, 101 p. :ill., maps ;28 cm.","costCenters":[],"links":[{"id":123458,"rank":0,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/wri/1982/4076/report-thumb.jpg"},{"id":54344,"rank":300,"type":{"id":11,"text":"Document"},"url":"https://pubs.usgs.gov/wri/1982/4076/report.pdf","linkFileType":{"id":1,"text":"pdf"}}],"noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"4f4e4aa7e4b07f02db66710d","contributors":{"authors":[{"text":"Taylor, O.J.","contributorId":71584,"corporation":false,"usgs":true,"family":"Taylor","given":"O.J.","email":"","affiliations":[],"preferred":false,"id":194363,"contributorType":{"id":1,"text":"Authors"},"rank":1}]}}
,{"id":9854,"text":"ofr82849 - 1982 - Lineaments derived from analysis of linear features mapped from Landsat images of the Four Corners region of the Southwestern United States","interactions":[],"lastModifiedDate":"2012-02-02T00:06:16","indexId":"ofr82849","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":"82-849","title":"Lineaments derived from analysis of linear features mapped from Landsat images of the Four Corners region of the Southwestern United States","docAbstract":"Linear features are relatively short, distinct, non-cultural linear elements mappable on Landsat multispectral scanner images (MSS). Most linear features are related to local topographic features, such as cliffs, slope breaks, narrow ridges, and stream valley segments that are interpreted as reflecting directed aspects of local geologic structure including faults, zones of fracturing (joints), and the strike of tilted beds. \r\n\r\n6,050 linear features were mapped on computer-enhanced Landsat MSS images of 11 Landsat scenes covering an area from the Rio Grande rift zone on the east to the Grand Canyon on the west and from the San Juan Mountains, Colorado, on the north to the Mogollon Rim on the south. Computer-aided statistical analysis of the linear feature data revealed 5 statistically important trend intervals: 1.) N. 10W.-N.16E., 2.) N.35-72E., 3.) N.33-59W., 4.) N. 74-83W., and 5.) N.89-9-W. and N. 89-90E. Subsequent analysis of the distribution of the linear features indicated that only the first three trend intervals are of regional geologic significance. Computer-generated maps of the linear features in each important trend interval were prepared, as well as contour maps showing the relative concentrations of linear features in each trend interval. These maps were then analyzed for patterns suggestive of possible regional tectonic lines. \r\n\r\n20 possible tectonic lines, or lineaments, were interpreted from the maps. One lineament is defined by an obvious change in overall linear feature concentrations along a northwest-trending line cutting across northeastern Arizona. Linear features are abundant northeast of the line and relatively scarce to the southwest. The remaining 19 lineaments represent the axes of clusters of parallel linear features elongated in the direction of the linear feature trends. Most of these lineaments mark previously known structural zones controlled by linear features in the Precambrian basement or show newly recognized relationships to geological and/or geophysical patterns that suggest probable influence by buried basement features. The remaining few lineaments are not strongly correlative with geological or geophysical patterns, but on the basis of existing data they cannot be dismissed as being possible expressions of basement features.","language":"ENGLISH","publisher":"U.S. Geological Survey,","doi":"10.3133/ofr82849","usgsCitation":"Knepper, D.H., 1982, Lineaments derived from analysis of linear features mapped from Landsat images of the Four Corners region of the Southwestern United States: U.S. Geological Survey Open-File Report 82-849, 81 p., 1 over-size sheet, ill., maps ;30 cm., https://doi.org/10.3133/ofr82849.","productDescription":"81 p., 1 over-size sheet, ill., maps ;30 cm.","costCenters":[],"links":[{"id":141873,"rank":0,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/of/1982/0849/report-thumb.jpg"},{"id":37635,"rank":400,"type":{"id":17,"text":"Plate"},"url":"https://pubs.usgs.gov/of/1982/0849/plate-1.pdf","linkFileType":{"id":1,"text":"pdf"}},{"id":37636,"rank":300,"type":{"id":11,"text":"Document"},"url":"https://pubs.usgs.gov/of/1982/0849/report.pdf","linkFileType":{"id":1,"text":"pdf"}}],"noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"4f4e4b15e4b07f02db6a50c8","contributors":{"authors":[{"text":"Knepper, Daniel H. dknepper@usgs.gov","contributorId":1242,"corporation":false,"usgs":true,"family":"Knepper","given":"Daniel","email":"dknepper@usgs.gov","middleInitial":"H.","affiliations":[],"preferred":true,"id":160411,"contributorType":{"id":1,"text":"Authors"},"rank":1}]}}
,{"id":56876,"text":"wdrMI811 - 1982 - Water resources data for Michigan, water year 1981","interactions":[],"lastModifiedDate":"2017-08-10T14:56:08","indexId":"wdrMI811","displayToPublicDate":"1994-01-01T00:00:00","publicationYear":"1982","noYear":false,"publicationType":{"id":18,"text":"Report"},"publicationSubtype":{"id":5,"text":"USGS Numbered Series"},"seriesTitle":{"id":340,"text":"Water Data Report","code":"WDR","active":false,"publicationSubtype":{"id":5}},"seriesNumber":"MI-81-1","title":"Water resources data for Michigan, water year 1981","docAbstract":"<p>Water resources data for the 1981 water year for Michigan consist of records of stage, discharge, and water quality of streams; stage, contents, and water quality of lakes and reservoirs; and water levels and water temperature of ground water. This report contains discharge records for 178 gaging stations; stage only records for 4 gaging stations; stage and contents for 5 lakes and reservoirs; water quality for 45 continuous-record stations; and water levels for 53 observation wells. Also included are 85 crest-stage partial-record stations and 59 low-flow partial-record stations. Additional water data were collected at various sites, not part of the systematic data-collection program, and are published as miscellaneous measurements. These data represent that part of the National Water Data System operated by the U.S. Geological Survey and cooperating State and Federal agencies in Michigan.</p>","language":"English","publisher":"U.S. Geological Survey","doi":"10.3133/wdrMI811","usgsCitation":"Water Resources Division, U.S. Geological Survey, 1982, Water resources data for Michigan, water year 1981: U.S. Geological Survey Water Data Report MI-81-1, x, 524 p., https://doi.org/10.3133/wdrMI811.","productDescription":"x, 524 p.","numberOfPages":"540","costCenters":[{"id":382,"text":"Michigan Water Science Center","active":true,"usgs":true}],"links":[{"id":184417,"rank":0,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/wdr/1981/mi-81-1/report-thumb.jpg"},{"id":344738,"rank":2,"type":{"id":11,"text":"Document"},"url":"https://pubs.usgs.gov/wdr/1981/mi-81-1/report.pdf","linkFileType":{"id":1,"text":"pdf"}}],"country":"United 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,{"id":8758,"text":"ofr82436 - 1982 - Hydraulic geometry of the Platte River in south-central Nebraska","interactions":[],"lastModifiedDate":"2020-10-06T21:25:04.529394","indexId":"ofr82436","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":"82-436","title":"Hydraulic geometry of the Platte River in south-central Nebraska","docAbstract":"At-a-station hydraulic-geometry of the Platte River in south-central Nebraska is complex. The range of exponents of simple power-function relations is large, both between different reaches of the river, and among different sections within a given reach. The at-a-station exponents plot in several fields of the b-f-m diagram, suggesting that morphologic and hydraulic changes with increasing discharge vary considerably. Systematic changes in the plotting positions of the exponents with time indicate that in general, the width exponent has decreased, although trends are not readily apparent in the other exponents. Plots of the hydraulic-geometry relations indicate that simple power functions are not the proper model in all instances. For these sections, breaks in the slopes of the hydraulic geometry relations serve to partition the data sets. Power functions fit separately to the partitioned data described the width-, depth-, and velocity-discharge relations more accurately than did a single power function. Plotting positions of the exponents from hydraulic geometry relations of partitioned data sets on b-f-m diagrams indicate that much of the apparent variations of plotting positions of single power functions results because the single power functions compromise both subsets of partitioned data. For several sections, the shape of the channel primarily accounts for the better fit of two-power functions to partitioned data than a single power function over the entire range of data. These non-log linear relations may have significance for channel maintenance. (USGS)","language":"English","publisher":"U.S. Geological Survey","publisherLocation":"Reston, VA","doi":"10.3133/ofr82436","usgsCitation":"Eschner, T., 1982, Hydraulic geometry of the Platte River in south-central Nebraska: U.S. Geological Survey Open-File Report 82-436, iv, 59 p., https://doi.org/10.3133/ofr82436.","productDescription":"iv, 59 p.","costCenters":[],"links":[{"id":379137,"rank":2,"type":{"id":11,"text":"Document"},"url":"https://pubs.usgs.gov/of/1982/0436/report.pdf","linkFileType":{"id":1,"text":"pdf"}},{"id":141946,"rank":0,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/of/1982/0436/report-thumb.jpg"}],"country":"United States","state":"Nebraska","geographicExtents":"{\n  \"type\": \"FeatureCollection\",\n  \"features\": [\n    {\n      \"type\": \"Feature\",\n      \"properties\": {},\n      \"geometry\": {\n        \"type\": \"Polygon\",\n        \"coordinates\": [\n          [\n            [\n              -103.699951171875,\n              40.718119379753446\n            ],\n            [\n              -100.4150390625,\n              40.718119379753446\n            ],\n            [\n              -100.4150390625,\n              41.90636538970964\n            ],\n            [\n              -103.699951171875,\n              41.90636538970964\n            ],\n            [\n              -103.699951171875,\n              40.718119379753446\n            ]\n          ]\n        ]\n      }\n    }\n  ]\n}","noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"4f4e4a4ee4b07f02db627e94","contributors":{"authors":[{"text":"Eschner, T.R.","contributorId":45700,"corporation":false,"usgs":true,"family":"Eschner","given":"T.R.","email":"","affiliations":[],"preferred":false,"id":158279,"contributorType":{"id":1,"text":"Authors"},"rank":1}]}}
,{"id":9327,"text":"ofr82511 - 1982 - Water quality of coal deposits and abandoned mines, Saginaw County, Michigan","interactions":[],"lastModifiedDate":"2017-07-12T11:21:42","indexId":"ofr82511","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":"82-511","title":"Water quality of coal deposits and abandoned mines, Saginaw County, Michigan","docAbstract":"<p>Surface water arid;ground water from an area underlain by coal- bearing rocks in the vicinity of St. Charles Michigan, were analyzed to determine the quality characteristics of these water resources and to assess the relation between the two. Data for 15 constituents, including boron, phenol, lithium, strontium and manganese, were in such high concentrations that they could be used to differentiate between water from wells drilled into coal-bearing beds and water from streams not directly associated with coal deposits. </p><p>Ground water from abandoned mines and undisturbed coal-bearing beds is highly mineralized, and contains higher concentrations of trace metals than surface water. Water from the undistrubed coal- bearing beds and abandoned mines is not suitable for domestic, public supply, or agricultural uses. Large amounts of this highly mineralized ground water reaching local streams would have a deleterious effect on surface-water quality.</p>","language":"English","publisher":"U.S. Geological Survey","publisherLocation":"Lansing, MI","doi":"10.3133/ofr82511","usgsCitation":"Handy, A., 1982, Water quality of coal deposits and abandoned mines, Saginaw County, Michigan: U.S. Geological Survey Open-File Report 82-511, v, 35 p, https://doi.org/10.3133/ofr82511.","productDescription":"v, 35 p","numberOfPages":"45","costCenters":[{"id":382,"text":"Michigan Water Science Center","active":true,"usgs":true}],"links":[{"id":343704,"rank":2,"type":{"id":11,"text":"Document"},"url":"https://pubs.usgs.gov/of/1982/0511/report.pdf","linkFileType":{"id":1,"text":"pdf"}},{"id":142369,"rank":0,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/of/1982/0511/report-thumb.jpg"}],"country":"United States","state":"Michigan","county":"Saginaw County","geographicExtents":"{\"type\":\"FeatureCollection\",\"features\":[{\"type\":\"Feature\",\"geometry\":{\"type\":\"Polygon\",\"coordinates\":[[[-84.1702,43.5689],[-84.0521,43.5668],[-84.0524,43.5235],[-83.8188,43.5217],[-83.8186,43.478],[-83.7,43.4787],[-83.7009,43.3941],[-83.6996,43.3317],[-83.6943,43.3252],[-83.694,43.2223],[-83.8154,43.2212],[-83.9318,43.2204],[-83.9294,43.1334],[-84.0519,43.1317],[-84.1687,43.1306],[-84.2874,43.1286],[-84.3684,43.1281],[-84.3698,43.2059],[-84.3701,43.2146],[-84.3717,43.3884],[-84.3718,43.4654],[-84.3713,43.4817],[-84.1719,43.4825],[-84.1702,43.5689]]]},\"properties\":{\"name\":\"Saginaw\",\"state\":\"MI\"}}]}","noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"4f4e4a07e4b07f02db5f99be","contributors":{"authors":[{"text":"Handy, A.H.","contributorId":104493,"corporation":false,"usgs":true,"family":"Handy","given":"A.H.","email":"","affiliations":[],"preferred":false,"id":159486,"contributorType":{"id":1,"text":"Authors"},"rank":1}]}}
,{"id":48794,"text":"ofr82292 - 1982 - Preliminary study of methods for upgrading USGS Antarctic seismological capability","interactions":[],"lastModifiedDate":"2018-07-23T10:26:25","indexId":"ofr82292","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":"82-292","title":"Preliminary study of methods for upgrading USGS Antarctic seismological capability","docAbstract":"<p>The purpose of this study is to evaluate potential methods for obtaining higher quality seismic data from Antarctica. Currently, USGS-sponsored WWSSN stations are located at Scott Base, Sanae Base, and at South Pole Station. Scott and Sanae Stations are located near the coast; data obtained from coastal installations are normally degraded by noise generated by ocean wave action on the coast. Operations at South Pole are rather difficult because of the severe environmental characteristics and the extended logistics which are required to provide supplies and operating personnel to its remote location. Short-period data quality from Pole Station has been moderately high with a short-period magnification of 100K at 1Hz.&nbsp;</p>","language":"English","publisher":"U.S. Geological Survey","doi":"10.3133/ofr82292","usgsCitation":"Holcomb, L.G., 1982, Preliminary study of methods for upgrading USGS Antarctic seismological capability: U.S. Geological Survey Open-File Report 82-292, 43 p., https://doi.org/10.3133/ofr82292.","productDescription":"43 p.","costCenters":[{"id":122,"text":"Albuquerque Seismological Laboratory","active":false,"usgs":true}],"links":[{"id":9710,"rank":300,"type":{"id":11,"text":"Document"},"url":"https://pubs.usgs.gov/of/1982/0292/ofr82-292.pdf","size":"2131","linkFileType":{"id":1,"text":"pdf"}},{"id":169705,"rank":0,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/of/1982/0292/coverthb.jpg"}],"noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"4f4e4b07e4b07f02db69ade2","contributors":{"authors":[{"text":"Holcomb, L. Gary","contributorId":26308,"corporation":false,"usgs":true,"family":"Holcomb","given":"L.","email":"","middleInitial":"Gary","affiliations":[],"preferred":false,"id":238270,"contributorType":{"id":1,"text":"Authors"},"rank":1}]}}
,{"id":56872,"text":"wdrAZ801 - 1982 - Water resources data for Arizona, water year 1980","interactions":[],"lastModifiedDate":"2025-12-11T16:36:22.877871","indexId":"wdrAZ801","displayToPublicDate":"1994-01-01T00:00:00","publicationYear":"1982","noYear":false,"publicationType":{"id":18,"text":"Report"},"publicationSubtype":{"id":5,"text":"USGS Numbered Series"},"seriesTitle":{"id":340,"text":"Water Data Report","code":"WDR","active":false,"publicationSubtype":{"id":5}},"seriesNumber":"AZ-80-1","title":"Water resources data for Arizona, water year 1980","docAbstract":"<p>Water resources data for the 1980 water year for Arizona consist of records of stage, discharge, and water quality of streams; stage, contents, and water quality of lakes and reservoirs; water levels of observation wells; and quality of ground water. This report contains discharge records for 240 gaging stations, annual peaks for 61 crest-stage partial-record stations, and discharge measurements at 14 miscellaneous sites; contents only records for 9 lakes and reservoirs; stage and contents for 1 lake; elevation and discharge for 1 streamflow station; elevation only for 1 stream-flow station; gage height only for I head over a dam; 16 supplementary records, included with gaging-station records, consisting of month end or monthly stage, contents, and evaporation of lakes and reservoirs, diversions, and return flows; water-quality records for 62 continuous-record stations and 9 miscellaneous sites; water levels for 93 observation wells; and water-quality data for water from 741 wells. The data represent that part of the National Water Data System operated by the U.S. Geological Survey and cooperating Federal and State Agencies in Arizona.</p>","language":"English","publisher":"U.S. Geological Survey","doi":"10.3133/wdrAZ801","collaboration":"Prepared in cooperation with the State of Arizona and with other agencies","usgsCitation":"Water Resources Division, U.S. Geological Survey, 1982, Water resources data for Arizona, water year 1980: U.S. Geological Survey Water Data Report AZ-80-1, xiv, 568 p., https://doi.org/10.3133/wdrAZ801.","productDescription":"xiv, 568 p.","costCenters":[],"links":[{"id":497329,"rank":2,"type":{"id":11,"text":"Document"},"url":"https://pubs.usgs.gov/wdr/1980/az-80-1/report.pdf","linkFileType":{"id":1,"text":"pdf"}},{"id":184413,"rank":1,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/wdr/1980/az-80-1/report-thumb.jpg"}],"country":"United 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,{"id":48796,"text":"ofr82702 - 1982 - A note on transients in the SRO and ASRO long-period data","interactions":[],"lastModifiedDate":"2018-07-17T11:04:14","indexId":"ofr82702","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":"82-702","title":"A note on transients in the SRO and ASRO long-period data","docAbstract":"Data users have occasionally observed pulse-like transients in the long-period waveforms recorded at the Seismic Research Observatories (SRO) and at the Modified High-Gain Long-Period (ASRO) stations. In a recent paper, Dziewonski et al (1981) reported transients associated with earthquake signals record at some SRO stations, and the authors ascribed these transients to an unpredictable nonlinear system response. While some transients in the SRO and ASRO data are indeed generated by a nonlinear response (clipping), others are the result of linear processes. All event-associated transients are predictable in the sense that they are produced by large impulsive body-wave signals.","language":"English","publisher":"U.S. Geological Survey","doi":"10.3133/ofr82702","usgsCitation":"Peterson, J., 1982, A note on transients in the SRO and ASRO long-period data: U.S. Geological Survey Open-File Report 82-702, 20 p., https://doi.org/10.3133/ofr82702.","productDescription":"20 p.","costCenters":[{"id":122,"text":"Albuquerque Seismological Laboratory","active":false,"usgs":true}],"links":[{"id":169707,"rank":0,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/of/1982/0702/coverthb.jpg"},{"id":9712,"rank":2,"type":{"id":11,"text":"Document"},"url":"https://pubs.usgs.gov/of/1982/0702/ofr82-702.pdf","text":"Report","size":"584 kB","linkFileType":{"id":1,"text":"pdf"},"description":"OFR 1982-0702"}],"noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"53cd495ee4b0b290850ef1bd","contributors":{"authors":[{"text":"Peterson, Jon","contributorId":67522,"corporation":false,"usgs":true,"family":"Peterson","given":"Jon","affiliations":[],"preferred":false,"id":238275,"contributorType":{"id":1,"text":"Authors"},"rank":1}]}}
,{"id":9242,"text":"ofr82189 - 1982 - Description of digital aeromagnetic data, U.S. Atlantic continental margin, survey of 1974-76","interactions":[],"lastModifiedDate":"2018-03-05T15:13:49","indexId":"ofr82189","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":"82-189","title":"Description of digital aeromagnetic data, U.S. Atlantic continental margin, survey of 1974-76","language":"ENGLISH","publisher":"U.S. Geological Survey,","doi":"10.3133/ofr82189","usgsCitation":"Grim, M.S., Behrendt, J.C., and Klitgord, K.D., 1982, Description of digital aeromagnetic data, U.S. Atlantic continental margin, survey of 1974-76: U.S. Geological Survey Open-File Report 82-189, 11 p., 1 over-size sheet, maps ;28 cm., https://doi.org/10.3133/ofr82189.","productDescription":"11 p., 1 over-size sheet, maps ;28 cm.","costCenters":[],"links":[{"id":141614,"rank":0,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/of/1982/0189/report-thumb.jpg"},{"id":36889,"rank":400,"type":{"id":17,"text":"Plate"},"url":"https://pubs.usgs.gov/of/1982/0189/plate-1.pdf","linkFileType":{"id":1,"text":"pdf"}},{"id":36890,"rank":300,"type":{"id":11,"text":"Document"},"url":"https://pubs.usgs.gov/of/1982/0189/report.pdf","linkFileType":{"id":1,"text":"pdf"}}],"noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"4f4e4aafe4b07f02db66d275","contributors":{"authors":[{"text":"Grim, M. S.","contributorId":102884,"corporation":false,"usgs":true,"family":"Grim","given":"M.","email":"","middleInitial":"S.","affiliations":[],"preferred":false,"id":159344,"contributorType":{"id":1,"text":"Authors"},"rank":1},{"text":"Behrendt, John C. jbehrendt@usgs.gov","contributorId":25945,"corporation":false,"usgs":true,"family":"Behrendt","given":"John","email":"jbehrendt@usgs.gov","middleInitial":"C.","affiliations":[{"id":213,"text":"Crustal Imaging and Characterization Team","active":false,"usgs":true},{"id":218,"text":"Denver Federal Center","active":false,"usgs":true}],"preferred":false,"id":159342,"contributorType":{"id":1,"text":"Authors"},"rank":2},{"text":"Klitgord, Kim D.","contributorId":82307,"corporation":false,"usgs":true,"family":"Klitgord","given":"Kim","email":"","middleInitial":"D.","affiliations":[{"id":678,"text":"Woods Hole Coastal and Marine Science Center","active":true,"usgs":true}],"preferred":false,"id":159343,"contributorType":{"id":1,"text":"Authors"},"rank":3}]}}
,{"id":48795,"text":"ofr82694 - 1982 - Submersed aquatic vegetation in the tidal Potomac River and Estuary of Maryland, Virginia and the District of Columbia; Hydrologic data report, May, 1978 to November, 1981","interactions":[],"lastModifiedDate":"2012-02-02T00:10:22","indexId":"ofr82694","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":"82-694","title":"Submersed aquatic vegetation in the tidal Potomac River and Estuary of Maryland, Virginia and the District of Columbia; Hydrologic data report, May, 1978 to November, 1981","language":"ENGLISH","doi":"10.3133/ofr82694","usgsCitation":"Paschal, J.E., Miller, D.R., Bartow, N.C., and Carter, V., 1982, Submersed aquatic vegetation in the tidal Potomac River and Estuary of Maryland, Virginia and the District of Columbia; Hydrologic data report, May, 1978 to November, 1981: U.S. Geological Survey Open-File Report 82-694, 220 p., https://doi.org/10.3133/ofr82694.","productDescription":"220 p.","costCenters":[],"links":[{"id":169706,"rank":0,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/of/1982/0694/report-thumb.jpg"},{"id":85626,"rank":300,"type":{"id":11,"text":"Document"},"url":"https://pubs.usgs.gov/of/1982/0694/report.pdf","linkFileType":{"id":1,"text":"pdf"}}],"noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"4f4e4b05e4b07f02db699b89","contributors":{"authors":[{"text":"Paschal, James E. Jr.","contributorId":45768,"corporation":false,"usgs":true,"family":"Paschal","given":"James","suffix":"Jr.","email":"","middleInitial":"E.","affiliations":[],"preferred":false,"id":238272,"contributorType":{"id":1,"text":"Authors"},"rank":1},{"text":"Miller, Darin R.","contributorId":64713,"corporation":false,"usgs":true,"family":"Miller","given":"Darin","email":"","middleInitial":"R.","affiliations":[],"preferred":false,"id":238274,"contributorType":{"id":1,"text":"Authors"},"rank":2},{"text":"Bartow, Nancy C.","contributorId":56203,"corporation":false,"usgs":true,"family":"Bartow","given":"Nancy","email":"","middleInitial":"C.","affiliations":[],"preferred":false,"id":238273,"contributorType":{"id":1,"text":"Authors"},"rank":3},{"text":"Carter, Virginia","contributorId":12018,"corporation":false,"usgs":true,"family":"Carter","given":"Virginia","email":"","affiliations":[],"preferred":false,"id":238271,"contributorType":{"id":1,"text":"Authors"},"rank":4}]}}
,{"id":56877,"text":"wdrSD811 - 1982 - Water resources data for South Dakota, water year 1981","interactions":[],"lastModifiedDate":"2020-10-23T20:40:50.251101","indexId":"wdrSD811","displayToPublicDate":"1994-01-01T00:00:00","publicationYear":"1982","noYear":false,"publicationType":{"id":18,"text":"Report"},"publicationSubtype":{"id":5,"text":"USGS Numbered Series"},"seriesTitle":{"id":340,"text":"Water Data Report","code":"WDR","active":false,"publicationSubtype":{"id":5}},"seriesNumber":"SD-81-1","title":"Water resources data for South Dakota, water year 1981","docAbstract":"<p>No abstract available.&nbsp;</p>","language":"English","publisher":"U.S. Geological Survey","publisherLocation":"Reston, VA","doi":"10.3133/wdrSD811","usgsCitation":"Water Resources Division, U.S. Geological Survey, 1982, Water resources data for South Dakota, water year 1981: U.S. Geological Survey Water Data Report SD-81-1, vii, 357 p., https://doi.org/10.3133/wdrSD811.","productDescription":"vii, 357 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