{"pageNumber":"552","pageRowStart":"13775","pageSize":"25","recordCount":16498,"records":[{"id":43536,"text":"ofr81212 - 1981 - Hydrology of the Winter Haven Chain of Lakes, Polk County, Florida","interactions":[],"lastModifiedDate":"2022-04-18T16:28:41.630956","indexId":"ofr81212","displayToPublicDate":"1994-01-01T00:00:00","publicationYear":"1981","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":"81-212","title":"Hydrology of the Winter Haven Chain of Lakes, Polk County, Florida","docAbstract":"<p>Fourteen interconnected lakes in and around the city of Winter Haven, Polk County, Fla., form the Winter Haven Chain of Lakes. Levels of the lakes during the spring of 1976 were at a record low stage for the 31 years of record. During 1960-76, rainfall had been below average for all but 2 years, and departure from average rainfall totaled 72.34 inches. Fluctuations in stage of Lake Howard, representative of the chain, and of Lake Otis, the nearest isolated lake that has a reasonably long record of stage , were compared with other hydrologic variables. Analyses of lake stage and rainfall records indicate that deficient rainfall has been the key factor in the decline of lake levels in the area. Manipulation of lake levels, pumpage from the lakes and underlying aquifer, and urbanization of the watershed probably have affected the lakes as well, but records are not available to determine the significance of their effects. The surficial aquifer drains to the lakes. Water level in the underlying Floridan aquifer is everywhere lower than in any of the lakes, thus water moves from the lakes and surficial aquifer through the confining clay layer to the Floridan aquifer.&nbsp;</p>","language":"English","publisher":"U.S. Geological Survey","doi":"10.3133/ofr81212","collaboration":"Prepared in cooperation with the Southwest Florida Water Management District, Peace River Basin Board, and the Winter Haven Lake Region Boat Course District","usgsCitation":"Sinclair, W.C., and Reichenbaugh, R.C., 1981, Hydrology of the Winter Haven Chain of Lakes, Polk County, Florida: U.S. Geological Survey Open-File Report 81-212, 1 Plate: 41.96 x 31.37 inches, https://doi.org/10.3133/ofr81212.","productDescription":"1 Plate: 41.96 x 31.37 inches","costCenters":[],"links":[{"id":398944,"rank":2,"type":{"id":17,"text":"Plate"},"url":"https://pubs.usgs.gov/of/1981/0212/plate-1.pdf","linkFileType":{"id":1,"text":"pdf"}},{"id":173659,"rank":0,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/of/1981/0212/report-thumb.jpg"}],"country":"United States","state":"Florida","county":"Polk County","otherGeospatial":"Winter Haven Chain of Lakes","geographicExtents":"{\"type\":\"FeatureCollection\",\"features\":[{\"type\":\"Feature\",\"geometry\":{\"type\":\"Polygon\",\"coordinates\":[[[-81.6578,28.3471],[-81.6576,28.2593],[-81.5574,28.2598],[-81.5245,28.2011],[-81.5247,28.1431],[-81.4556,28.1429],[-81.4558,28.0854],[-81.3749,28.0853],[-81.3465,28.085],[-81.3482,28.08],[-81.3468,28.0754],[-81.347,28.0694],[-81.3486,28.0676],[-81.3538,28.0668],[-81.3553,28.0668],[-81.3604,28.0688],[-81.3646,28.068],[-81.3669,28.0607],[-81.3639,28.0574],[-81.365,28.0546],[-81.3642,28.0463],[-81.3617,28.044],[-81.3623,28.0426],[-81.3629,28.0389],[-81.3666,28.0363],[-81.375,28.0296],[-81.3761,28.0287],[-81.3752,28.0259],[-81.381,28.0201],[-81.38,28.0177],[-81.3765,28.0158],[-81.3797,28.0118],[-81.3828,28.0123],[-81.3867,28.0175],[-81.3923,28.0194],[-81.3947,28.0282],[-81.407,28.029],[-81.4135,28.0361],[-81.417,28.038],[-81.4241,28.0405],[-81.4277,28.0414],[-81.4318,28.0425],[-81.4348,28.0476],[-81.4351,28.0527],[-81.4381,28.0569],[-81.4437,28.0593],[-81.4463,28.0589],[-81.4535,28.0573],[-81.4561,28.0564],[-81.4594,28.0514],[-81.4604,28.0496],[-81.4592,28.0399],[-81.4486,28.0318],[-81.4455,28.0331],[-81.4388,28.033],[-81.4335,28.0218],[-81.4299,28.0213],[-81.4279,28.0185],[-81.4274,28.0175],[-81.4212,28.0031],[-81.4182,27.9998],[-81.4057,28.0027],[-81.3948,28.0057],[-81.3877,28.0037],[-81.3823,27.9953],[-81.3774,27.9873],[-81.3755,27.9799],[-81.369,27.976],[-81.3619,27.9713],[-81.3517,27.9683],[-81.3483,27.9627],[-81.3495,27.9553],[-81.3435,27.9529],[-81.3374,27.95],[-81.3365,27.9444],[-81.3387,27.9403],[-81.3428,27.9418],[-81.3459,27.94],[-81.3435,27.9358],[-81.341,27.9321],[-81.3369,27.9324],[-81.3302,27.9318],[-81.3206,27.9279],[-81.314,27.9231],[-81.3117,27.9143],[-81.3141,27.9056],[-81.3123,27.8973],[-81.3069,27.8893],[-81.3046,27.8805],[-81.3037,27.8745],[-81.3024,27.868],[-81.3015,27.8634],[-81.2919,27.859],[-81.2827,27.8579],[-81.2818,27.8537],[-81.2701,27.8493],[-81.2589,27.8471],[-81.2496,27.8478],[-81.2414,27.8471],[-81.2313,27.8423],[-81.2182,27.8332],[-81.2104,27.8224],[-81.2065,27.8158],[-81.2012,27.8046],[-81.1978,27.7967],[-81.1934,27.7902],[-81.1875,27.7831],[-81.1857,27.7761],[-81.1806,27.7737],[-81.1783,27.7677],[-81.1728,27.7629],[-81.1734,27.7592],[-81.177,27.7575],[-81.1767,27.7515],[-81.1718,27.7458],[-81.1678,27.7411],[-81.1644,27.7369],[-81.1656,27.7314],[-81.1673,27.7268],[-81.1623,27.723],[-81.1542,27.7187],[-81.1487,27.7134],[-81.1475,27.7042],[-81.1483,27.6945],[-81.1457,27.6816],[-81.1435,27.6714],[-81.1365,27.6643],[-81.131,27.6609],[-81.1329,27.6517],[-81.1424,27.6432],[-81.1701,27.6431],[-81.1952,27.6442],[-81.2233,27.6449],[-81.3673,27.6463],[-81.4776,27.6467],[-81.4827,27.6464],[-81.5027,27.6464],[-81.5637,27.6464],[-81.617,27.6463],[-81.6247,27.646],[-81.6334,27.6462],[-81.6493,27.6465],[-81.6626,27.6464],[-81.6873,27.646],[-81.6965,27.6466],[-81.7073,27.646],[-81.7283,27.6459],[-81.7416,27.6462],[-81.7498,27.6464],[-81.8749,27.6458],[-81.8841,27.6464],[-82.0543,27.6465],[-82.0545,27.7266],[-82.0564,27.7542],[-82.0546,27.8781],[-82.0566,27.9273],[-82.0562,28.1716],[-82.1062,28.1716],[-82.1063,28.259],[-82.0562,28.259],[-82.0565,28.3119],[-82.045,28.3186],[-82.0326,28.3211],[-82.0232,28.3242],[-82.0093,28.323],[-81.9985,28.3191],[-81.9915,28.3102],[-81.9864,28.3055],[-81.9792,28.3063],[-81.976,28.3086],[-81.9678,28.3079],[-81.958,28.3082],[-81.9581,28.345],[-81.8578,28.3463],[-81.8579,28.3619],[-81.7907,28.3619],[-81.7911,28.3463],[-81.6578,28.3471]]]},\"properties\":{\"name\":\"Polk\",\"state\":\"FL\"}}]}","noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"4f4e4acce4b07f02db67e75d","contributors":{"authors":[{"text":"Sinclair, William C.","contributorId":14798,"corporation":false,"usgs":true,"family":"Sinclair","given":"William","email":"","middleInitial":"C.","affiliations":[],"preferred":false,"id":228343,"contributorType":{"id":1,"text":"Authors"},"rank":1},{"text":"Reichenbaugh, Ronald C.","contributorId":222163,"corporation":false,"usgs":true,"family":"Reichenbaugh","given":"Ronald","email":"","middleInitial":"C.","affiliations":[],"preferred":false,"id":228342,"contributorType":{"id":1,"text":"Authors"},"rank":2}]}}
,{"id":48679,"text":"ofr81205 - 1981 - Potentiometric surface of the Floridan aquifer in the Northwest Florida Water Management District, May 1980","interactions":[],"lastModifiedDate":"2012-02-02T00:10:44","indexId":"ofr81205","displayToPublicDate":"1994-01-01T00:00:00","publicationYear":"1981","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":"81-205","title":"Potentiometric surface of the Floridan aquifer in the Northwest Florida Water Management District, May 1980","docAbstract":"A May 1980 potentiometric surface map of the Northwest Florida Water Management District depicts water levels in wells tapping the Floridan aquifer prior to summer pumpage. Compared to earlier potentiometric maps of the area, there are no significant differences in the 1980 map that are the result of hydrologic conditions. The addition of numerous new monitor wells in Jackson, Calhoun, Gadsden, and Liberty Counties, however, permitted refinement or better delineation of contours and a separation of water-bearing zones of the Floridan aquifer in the latter two counties. (USGS)","language":"ENGLISH","doi":"10.3133/ofr81205","usgsCitation":"Rosenau, J., and Milner, R., 1981, Potentiometric surface of the Floridan aquifer in the Northwest Florida Water Management District, May 1980: U.S. Geological Survey Open-File Report 81-205, 1 sheet; map 61 x 91 cm. fold. in envelope 25 x 31 cm., https://doi.org/10.3133/ofr81205.","productDescription":"1 sheet; map 61 x 91 cm. fold. in envelope 25 x 31 cm.","costCenters":[],"links":[{"id":171482,"rank":0,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/thumbnails/usgs_thumb.jpg"}],"noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"4f4e4a81e4b07f02db64a1f8","contributors":{"authors":[{"text":"Rosenau, J.C.","contributorId":99192,"corporation":false,"usgs":true,"family":"Rosenau","given":"J.C.","email":"","affiliations":[],"preferred":false,"id":238011,"contributorType":{"id":1,"text":"Authors"},"rank":1},{"text":"Milner, R.S.","contributorId":75614,"corporation":false,"usgs":true,"family":"Milner","given":"R.S.","email":"","affiliations":[],"preferred":false,"id":238010,"contributorType":{"id":1,"text":"Authors"},"rank":2}]}}
,{"id":43598,"text":"ofr81638 - 1981 - Hydrologic sections through Lee County and adjacent areas of Hendry and Collier counties, Florida","interactions":[],"lastModifiedDate":"2024-01-22T20:45:50.878254","indexId":"ofr81638","displayToPublicDate":"1994-01-01T00:00:00","publicationYear":"1981","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":"81-638","title":"Hydrologic sections through Lee County and adjacent areas of Hendry and Collier counties, Florida","docAbstract":"<p>Most of the freshwater underlying Lee, western Hendry, and northern Collier Counties (fig. 1) occurs within the uppermost 400 feet of sediments which comprise the marine terrace sands, Fort Thompson Formation, Caloosahatchee Formation, Tamiami Formation, and part of the Hawthorn Formation. Although all these sediments contain water, they may be divided into those which yield water to wells (aquifers) and those which yield little to no water to wells (confining beds.) The aquifers are composed of permeable materials including sand, sandstone, limestone, or combinations of these sediments. The confining beds of of low permeability and usually consists of fine-grained materials, such as clay or marl or mixtures of these sediments with sand, sandstone, or limestone. Thus, limestone usually yields water to wells, whereas marly limestone does not.&nbsp;</p>","language":"English","publisher":"U.S. Geological Survey","doi":"10.3133/ofr81638","collaboration":"Prepared in cooperation with Lee County and Hendry County","usgsCitation":"Boggess, D.H., Missimer, T., and O’Donnell, T., 1981, Hydrologic sections through Lee County and adjacent areas of Hendry and Collier counties, Florida: U.S. Geological Survey Open-File Report 81-638, Report: 1 p.; 1 Plate: 35.55 x 27.68 inches, https://doi.org/10.3133/ofr81638.","productDescription":"Report: 1 p.; 1 Plate: 35.55 x 27.68 inches","costCenters":[],"links":[{"id":424699,"rank":3,"type":{"id":17,"text":"Plate"},"url":"https://pubs.usgs.gov/of/1981/0638/plate-1.pdf","linkFileType":{"id":1,"text":"pdf"}},{"id":424698,"rank":2,"type":{"id":11,"text":"Document"},"url":"https://pubs.usgs.gov/of/1981/0638/report.pdf","linkFileType":{"id":1,"text":"pdf"}},{"id":168654,"rank":1,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/of/1981/0638/report-thumb.jpg"}],"country":"United States","state":"Florida","county":"Collier County, Lee County, Hendry County","geographicExtents":"{\n  \"type\": \"FeatureCollection\",\n  \"features\": [\n    {\n      \"type\": \"Feature\",\n      \"properties\": {},\n      \"geometry\": {\n        \"coordinates\": [\n          [\n            [\n              -82.24575298889263,\n              26.722892747714823\n            ],\n            [\n              -82.24575298889263,\n              26.312469462605932\n            ],\n            [\n              -81.33114117248604,\n              26.312469462605932\n            ],\n            [\n              -81.33114117248604,\n              26.722892747714823\n            ],\n            [\n              -82.24575298889263,\n              26.722892747714823\n            ]\n          ]\n        ],\n        \"type\": \"Polygon\"\n      }\n    }\n  ]\n}","noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"4f4e4a18e4b07f02db60537b","contributors":{"authors":[{"text":"Boggess, Durward H.","contributorId":28650,"corporation":false,"usgs":true,"family":"Boggess","given":"Durward","email":"","middleInitial":"H.","affiliations":[],"preferred":false,"id":228438,"contributorType":{"id":1,"text":"Authors"},"rank":1},{"text":"Missimer, T.M.","contributorId":41839,"corporation":false,"usgs":true,"family":"Missimer","given":"T.M.","email":"","affiliations":[],"preferred":false,"id":228439,"contributorType":{"id":1,"text":"Authors"},"rank":2},{"text":"O’Donnell, T.H.","contributorId":69970,"corporation":false,"usgs":true,"family":"O’Donnell","given":"T.H.","email":"","affiliations":[],"preferred":false,"id":228440,"contributorType":{"id":1,"text":"Authors"},"rank":3}]}}
,{"id":46588,"text":"ofr801288 - 1981 - Generalized thickness of the Floridan aquifer, Southwest Florida Water Management District","interactions":[],"lastModifiedDate":"2022-04-21T20:33:51.041678","indexId":"ofr801288","displayToPublicDate":"1994-01-01T00:00:00","publicationYear":"1981","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":"80-1288","title":"Generalized thickness of the Floridan aquifer, Southwest Florida Water Management District","docAbstract":"<p>This map report presents the thickness of the Floridan aquifer in the Southwest Florida Water Management District. The Floridan aquifer ranges in thickness from 600 feet in the northern part of the District to 2,400 feet in the southern part. It is composed chiefly of limestone and dolomite beds that range in age from early Miocene to middle Eocene. For this investigation, the formations considered to be part of the Floridan aquifer are: Lake City and Avon Park Limestones of middle Eocene age; Ocala Limestone of late Eocene age; Suwannee Limestone of Oligocene age; and permeable parts of the Tampa Limestone and Hawthorn Formation of Miocene age that are in hydrologic contact with the rest of the aquifer.&nbsp;</p>","language":"English","publisher":"U.S. Geological Survey","doi":"10.3133/ofr801288","collaboration":"Prepared in cooperation with Southwest Florida Water Management District","usgsCitation":"Wolansky, R., and Garbade, J., 1981, Generalized thickness of the Floridan aquifer, Southwest Florida Water Management District: U.S. Geological Survey Open-File Report 80-1288, 1 Plate: 27.93 x 36.71 inches, https://doi.org/10.3133/ofr801288.","productDescription":"1 Plate: 27.93 x 36.71 inches","costCenters":[],"links":[{"id":399451,"rank":2,"type":{"id":17,"text":"Plate"},"url":"https://pubs.usgs.gov/of/1980/1288/plate-1.pdf","linkFileType":{"id":1,"text":"pdf"}},{"id":173737,"rank":0,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/of/1980/1288/report.thumb.jpg"}],"country":"United States","state":"Florida","otherGeospatial":"Southwest Florida","geographicExtents":"{\n  \"type\": \"FeatureCollection\",\n  \"features\": [\n    {\n      \"type\": \"Feature\",\n      \"properties\": {},\n      \"geometry\": {\n        \"type\": \"Polygon\",\n        \"coordinates\": [\n          [\n            [\n              -83.07861328125,\n              26.931865156388916\n            ],\n            [\n              -81.243896484375,\n              26.931865156388916\n            ],\n            [\n              -81.243896484375,\n              29.458731185355344\n            ],\n            [\n              -83.07861328125,\n              29.458731185355344\n            ],\n            [\n              -83.07861328125,\n              26.931865156388916\n            ]\n          ]\n        ]\n      }\n    }\n  ]\n}","noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"4f4e4b24e4b07f02db6aec3b","contributors":{"authors":[{"text":"Wolansky, R. M.","contributorId":89163,"corporation":false,"usgs":true,"family":"Wolansky","given":"R. M.","affiliations":[],"preferred":false,"id":233622,"contributorType":{"id":1,"text":"Authors"},"rank":1},{"text":"Garbade, J.M.","contributorId":13683,"corporation":false,"usgs":true,"family":"Garbade","given":"J.M.","email":"","affiliations":[],"preferred":false,"id":233621,"contributorType":{"id":1,"text":"Authors"},"rank":2}]}}
,{"id":29704,"text":"wri8132 - 1981 - Streamflow characteristics of the Hudson Bay and Upper Missouri River Basins, Montana, through 1979","interactions":[],"lastModifiedDate":"2020-11-04T18:17:07.269475","indexId":"wri8132","displayToPublicDate":"1994-01-01T00:00:00","publicationYear":"1981","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":"81-32","title":"Streamflow characteristics of the Hudson Bay and Upper Missouri River Basins, Montana, through 1979","docAbstract":"<p><span>Statistical summaries of streamflow data for selected gaging stations </span><span>are presented in this report to aid in appraising the hydrology of the Hud</span><span>son Bay and upper Missouri River basins in Montana. Streamflow records are </span><span>presented for 122 gaging stations for the period of record of each station. </span><span>Streamflow-record collection in the Missouri River basin began in 1890 at </span><span>Fort Benton, Montana. </span></p><p><span>For each streamflow-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, average discharge, and extremes of discharge. These data are followed by tables of monthly and annual mean discharge, flood-frequency data, low-flow and high-flow frequency data, and flow-duration information. </span></p>","language":"English","publisher":"U.S. Geological Survey","doi":"10.3133/wri8132","collaboration":"Prepared in cooperation with the Montana Department of Natural Resources and Conservation","usgsCitation":"Shields, R.R., and White, M.K., 1981, Streamflow characteristics of the Hudson Bay and Upper Missouri River Basins, Montana, through 1979: U.S. Geological Survey Water-Resources Investigations Report 81-32, iii, 144 p., https://doi.org/10.3133/wri8132.","productDescription":"iii, 144 p.","costCenters":[],"links":[{"id":380163,"rank":2,"type":{"id":11,"text":"Document"},"url":"https://pubs.usgs.gov/wri/1981/0032/report.pdf","linkFileType":{"id":1,"text":"pdf"}},{"id":159518,"rank":0,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/wri/1981/0032/report-thumb.jpg"}],"country":"United 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Ronald R.","contributorId":64655,"corporation":false,"usgs":true,"family":"Shields","given":"Ronald","email":"","middleInitial":"R.","affiliations":[],"preferred":false,"id":201979,"contributorType":{"id":1,"text":"Authors"},"rank":1},{"text":"White, Melvin K. mwhite@usgs.gov","contributorId":1563,"corporation":false,"usgs":true,"family":"White","given":"Melvin","email":"mwhite@usgs.gov","middleInitial":"K.","affiliations":[],"preferred":true,"id":201978,"contributorType":{"id":1,"text":"Authors"},"rank":2}]}}
,{"id":53613,"text":"wri81690 - 1981 - Availability and Quality of Water from Underground Coal Mines in Johnson and Martin Counties, Kentucky","interactions":[],"lastModifiedDate":"2012-02-10T00:10:11","indexId":"wri81690","displayToPublicDate":"1994-01-01T00:00:00","publicationYear":"1981","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":"81-690","title":"Availability and Quality of Water from Underground Coal Mines in Johnson and Martin Counties, Kentucky","docAbstract":"This report provides water users with detailed information on the location, quantity, and quality of water available from underground coal mines in the Breathitt Formation of Pennsylvanian age in part of eastern Kentucky. The principal coal seams mined are the Van Lear in Johnson County and the Alma in Martin County. Coal mines that contained water were located by field inventory and coal-mine maps.\r\n\r\nThe principal factors that affect the occurrence of water in coal mines are the size of the recharge area overlying the mine, the intensity and duration of precipitation, and the altitude of the mine relative to that of the nearest perennial stream.\r\n\r\nTen above-drainage mines (that is, mines at higher elevations than that of the nearest perennial stream) are considered potential sources of water. Discharge from these mines ranged from 12 to 1,700 gallons per minute. The highest sustained discharge from a mine ranged from 750 to 1,200 gallons per minute.\r\n\r\nThe water in coal mines is part of the hydrologic system and varies seasonally with precipitation. Annual discharge from most above-drainage mines ranged from 3 to 10 percent of annual precipitation on the 1and-surface area above the mine.\r\n\r\nEight below-drainage mines are considered potential sources of water. Two were test-pumped at rates of 560 to 620 gallons per minute for as long as 6 hours. After test pumping the Warfield Mining No. 1 mine during September 1977 and March 1978, the recovery (or recharge) rates were significantly different. In September, the recharge rate was about 1,150 gallons per minute, but in March the recharge rate was 103,500 gallons per minute. This difference reflects the seasonal variations in the amount of water available to the ground-water system. Estimates of water stored in below-drainage mines ranged from 22 to 1,462 million gallons. This storage represents a safety factor sufficient to provide water through periods of limited recharge to the mine.\r\n\r\nMost mine water is of the calcium magnesium sulfate type. In general, water from below-drainage mines had lower concentrations of dissolved constituents and higher pH than water from mines above drainage. The hardness of water ranged from soft to very hard and pH ranged -from 3.1 to 8.0 units. Dissolved iron ranged from 0.01 to 64 milligrams per liter. Phenol concentrations in water from eight coal mines ranged from 0 to 5 micrograms per liter.\r\n\r\nThere seems to be a significant difference in the chemical quality of water from above- and below-drainage mines. The concentration of most constituents was lower in water from below-drainage mines than it was from above-drainage mines.\r\n\r\nThe better quality water from below-drainage mines may reflect (1) lower mineralization resulting from less atmospheric oxygen available to react with pyrite or, (2) the result of sampling only the upper zones of water in below-drainage mines where the water has been diluted by less mineralized surface water or inflow or recharge.","language":"ENGLISH","publisher":"Geological Survey (U.S.)","doi":"10.3133/wri81690","collaboration":"Prepared in cooperation with the Kentucky Geological Survey and the University of Kentucky","usgsCitation":"Mull, D.S., Cordivio1a, S., and Risser, D.W., 1981, Availability and Quality of Water from Underground Coal Mines in Johnson and Martin Counties, Kentucky (WRI/OFR 81-690): U.S. Geological Survey Water-Resources Investigations Report 81-690, viii, 55 p.; Plates, https://doi.org/10.3133/wri81690.","productDescription":"viii, 55 p.; Plates","costCenters":[{"id":595,"text":"U.S. Geological Survey","active":false,"usgs":true}],"links":[{"id":124648,"rank":0,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/of/1981/0690/report-thumb.jpg"},{"id":91361,"rank":300,"type":{"id":11,"text":"Document"},"url":"https://pubs.usgs.gov/of/1981/0690/report.pdf","linkFileType":{"id":1,"text":"pdf"}}],"scale":"48000","geographicExtents":"{ \"type\": \"FeatureCollection\", \"features\": [ { \"type\": \"Feature\", \"properties\": {}, \"geometry\": { \"type\": \"Polygon\", \"coordinates\": [ [ [ -83,37.666666666666664 ], [ -83,38 ], [ -82.58333333333333,38 ], [ -82.58333333333333,37.666666666666664 ], [ -83,37.666666666666664 ] ] ] } } ] }","edition":"WRI/OFR 81-690","noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"4f4e4a85e4b07f02db64d4be","contributors":{"authors":[{"text":"Mull, D. S.","contributorId":43331,"corporation":false,"usgs":true,"family":"Mull","given":"D.","email":"","middleInitial":"S.","affiliations":[],"preferred":false,"id":247913,"contributorType":{"id":1,"text":"Authors"},"rank":1},{"text":"Cordivio1a, Steven","contributorId":26357,"corporation":false,"usgs":true,"family":"Cordivio1a","given":"Steven","email":"","affiliations":[],"preferred":false,"id":247912,"contributorType":{"id":1,"text":"Authors"},"rank":2},{"text":"Risser, Dennis W. 0000-0001-9597-5406 dwrisser@usgs.gov","orcid":"https://orcid.org/0000-0001-9597-5406","contributorId":898,"corporation":false,"usgs":true,"family":"Risser","given":"Dennis","email":"dwrisser@usgs.gov","middleInitial":"W.","affiliations":[{"id":532,"text":"Pennsylvania Water Science Center","active":true,"usgs":true}],"preferred":true,"id":247911,"contributorType":{"id":1,"text":"Authors"},"rank":3}]}}
,{"id":47186,"text":"ofr801283 - 1981 - Floods of September 16, 1975 in the Tallaboa Valley, Puerto Rico","interactions":[],"lastModifiedDate":"2018-12-19T08:49:28","indexId":"ofr801283","displayToPublicDate":"1994-01-01T00:00:00","publicationYear":"1981","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":"80-1283","title":"Floods of September 16, 1975 in the Tallaboa Valley, Puerto Rico","docAbstract":"<p>This report provides a record of the flood of September 16, 1975, and associated hydrologic data. These data can be used in making rational decisions in formulating effective flood-plain regulations that would minimize flood problems in the Tallaboa Valley.</p><p>The Tallaboa Valley (fig. 1) lies on the southwestern coast of Puerto Rico about 12 km (7.5 mi) west of the city of Ponce. The climate is semiarid with a mean annual precipitation of about 1,020 mm (40 in). It is a relatively small valley which until the late fifties was dedicated mainly to the product ion of sugarcane. Since then, the economy started changing from agriculture to industry. At present the lower part of the valley is completely industrialized. The upper part of the valley is used for agriculture--mostly as pastureland. The reach from Highway 132 downstream to the new Highway 2 is mainly agricultural with a few scattered communities. The lower part of the valley that includes the area from the Highway 2 bridge to the mouth is covered with heavy industry concerned with the refinement of oil, and associated industries.</p><p>The continuous growth of industry and consequently of the urban area of Peñuelas has encouraged growth onto the<br>flood plain. The study area is subject to flooding by the Rio Tallaboa and the Rio Guayanes, its main tributary. The Rio Guayanes is the- cause of flooding in the urban area of Penuelas, encompassing the reach from the northern edge of town downstream to Highway 132 where it joins the Rio Tallaboa.</p><p>Data are generally referred to in SI (International System) units followed&nbsp;by corresponding inch-pound units in parentheses. The SI units.may be converted to inch-pound units by multiplying the units given by the factors shown.&nbsp;</p>","language":"English","publisher":"U.S. Geological Survey","doi":"10.3133/ofr801283","usgsCitation":"Johnson, K.G., 1981, Floods of September 16, 1975 in the Tallaboa Valley, Puerto Rico (WRI/OFR): U.S. Geological Survey Open-File Report 80-1283, 5 Plates: 17.00 x 22.00 inches, https://doi.org/10.3133/ofr801283.","productDescription":"5 Plates: 17.00 x 22.00 inches","costCenters":[],"links":[{"id":360545,"rank":2,"type":{"id":17,"text":"Plate"},"url":"https://pubs.usgs.gov/of/1980/1283/plate-1.pdf","linkFileType":{"id":1,"text":"pdf"}},{"id":360546,"rank":3,"type":{"id":17,"text":"Plate"},"url":"https://pubs.usgs.gov/of/1980/1283/plate-2.pdf","linkFileType":{"id":1,"text":"pdf"}},{"id":360547,"rank":4,"type":{"id":17,"text":"Plate"},"url":"https://pubs.usgs.gov/of/1980/1283/plate-3.pdf","linkFileType":{"id":1,"text":"pdf"}},{"id":135211,"rank":0,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/of/1980/1283/report-thumb.jpg"},{"id":360548,"rank":5,"type":{"id":17,"text":"Plate"},"url":"https://pubs.usgs.gov/of/1980/1283/plate-4.pdf","linkFileType":{"id":1,"text":"pdf"}},{"id":360549,"rank":6,"type":{"id":17,"text":"Plate"},"url":"https://pubs.usgs.gov/of/1980/1283/plate-5.pdf","linkFileType":{"id":1,"text":"pdf"}}],"state":"Puerto Rico","otherGeospatial":"Tallaboa Valley","geographicExtents":"{\n  \"type\": \"FeatureCollection\",\n  \"features\": [\n    {\n      \"type\": \"Feature\",\n      \"properties\": {},\n      \"geometry\": {\n        \"type\": \"Polygon\",\n        \"coordinates\": [\n          [\n            [\n              -66.7690658569336,\n              17.96567026450932\n            ],\n            [\n              -66.67808532714842,\n              17.96567026450932\n            ],\n            [\n              -66.67808532714842,\n              18.116160664342022\n            ],\n            [\n              -66.7690658569336,\n              18.116160664342022\n            ],\n            [\n              -66.7690658569336,\n              17.96567026450932\n            ]\n          ]\n        ]\n      }\n    }\n  ]\n}","edition":"WRI/OFR","noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"4f4e49d8e4b07f02db5df88c","contributors":{"authors":[{"text":"Johnson, Karl G.","contributorId":7680,"corporation":false,"usgs":true,"family":"Johnson","given":"Karl","email":"","middleInitial":"G.","affiliations":[],"preferred":false,"id":234791,"contributorType":{"id":1,"text":"Authors"},"rank":1}]}}
,{"id":43691,"text":"ofr81908 - 1981 - Hydrologic maps of Ogallala Aquifer, west-central Kansas","interactions":[],"lastModifiedDate":"2012-02-02T00:10:10","indexId":"ofr81908","displayToPublicDate":"1994-01-01T00:00:00","publicationYear":"1981","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":"81-908","title":"Hydrologic maps of Ogallala Aquifer, west-central Kansas","language":"ENGLISH","doi":"10.3133/ofr81908","usgsCitation":"Dunlap, L.E., and Spinazola, J.M., 1981, Hydrologic maps of Ogallala Aquifer, west-central Kansas: U.S. Geological Survey Open-File Report 81-908, 4 maps ;61 x 126 cm., https://doi.org/10.3133/ofr81908.","productDescription":"4 maps ;61 x 126 cm.","costCenters":[],"links":[{"id":161804,"rank":0,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/thumbnails/usgs_thumb.jpg"},{"id":20211,"rank":400,"type":{"id":17,"text":"Plate"},"url":"https://pubs.usgs.gov/of/1981/0908/plate-1.pdf","linkFileType":{"id":1,"text":"pdf"}},{"id":20212,"rank":401,"type":{"id":17,"text":"Plate"},"url":"https://pubs.usgs.gov/of/1981/0908/plate-2.pdf","linkFileType":{"id":1,"text":"pdf"}},{"id":20213,"rank":402,"type":{"id":17,"text":"Plate"},"url":"https://pubs.usgs.gov/of/1981/0908/plate-3.pdf","linkFileType":{"id":1,"text":"pdf"}},{"id":20214,"rank":403,"type":{"id":17,"text":"Plate"},"url":"https://pubs.usgs.gov/of/1981/0908/plate-4.pdf","linkFileType":{"id":1,"text":"pdf"}}],"noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"4f4e4a1ae4b07f02db606797","contributors":{"authors":[{"text":"Dunlap, Lloyd E.","contributorId":92261,"corporation":false,"usgs":true,"family":"Dunlap","given":"Lloyd","email":"","middleInitial":"E.","affiliations":[],"preferred":false,"id":228564,"contributorType":{"id":1,"text":"Authors"},"rank":1},{"text":"Spinazola, Joseph M.","contributorId":102044,"corporation":false,"usgs":true,"family":"Spinazola","given":"Joseph","email":"","middleInitial":"M.","affiliations":[],"preferred":false,"id":228565,"contributorType":{"id":1,"text":"Authors"},"rank":2}]}}
,{"id":28152,"text":"wri80107 - 1981 - Hydrologic effects of proposed changes in management practices, Winnebago Pool, Wisconsin","interactions":[],"lastModifiedDate":"2015-10-20T14:39:25","indexId":"wri80107","displayToPublicDate":"1994-01-01T00:00:00","publicationYear":"1981","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":"80-107","title":"Hydrologic effects of proposed changes in management practices, Winnebago Pool, Wisconsin","docAbstract":"<p>Various changes in the management practices for the Winnebago pool have been proposed. The objectives of the proposed changes are protecting wetlands adjacent to the lakes in the pool and assuring adequate flow in the Fox River downstream from Lake Winnebago. Three proposed operation plans for the Winnebago pool were studied to determine the effects on lake stage and discharge. A digital reservoir model simulated daily lake stage and discharge from the Winnebago pool.</p>\n<p>Inflow for this simulation was computed from daily discharge, recorded at Rapide Croche Dam, and daily stage, recorded at Oshkosh. This computed inflow is net inflow, combining the effects of streamflow, precipitation, evaporation, and net ground-water inflow.</p>\n<p>The model was adapted to simulate operation of the Winnebago pool according to each of the proposed plans. Because the important features of each operation plan were expressed in terms of stages to be attained at certain dates, simulated discharge was adjusted daily to keep simulated lake stage close to that specified in the plan.</p>\n<p>The simulated lake stage for each of the proposed plans exceeded the allowable maximum in some years. However, the simulated stage exceeded the allowable maximum less frequently and for shorter periods than did the observed stage.</p>\n<p>For the 61 years simulated (water years 1918-78), the simulated 7-day, 10- year low flow ((57,10) at Rapide Croche Dam was 1,000 ft^/s compared with 900 ft^/s for the observed record. The 7-day, 2-year low flow (Qy 2) was 1,500 ft^/s (simulated) versus 1,600 ft3/s (observed).</p>\n<p>The model predicted that executing the proposed operation plan would result in monthly Q7 JQ for August and September of 1,100 ft-Vs. This is no change for August and a 12-percent increase for September.</p>\n<p>In addition, the study illustrated that the discharge from the Winnebago pool could be managed to guarantee that the discharge in the Fox River downstream would not fall below a specified discharge up to 1,500 ft^/s. In most years this would have no effect on the stage of the pool. In a few years there would be a conflict between releasing water from the pool to maintain the desired discharge and maintaining water levels above the required minimum stage. The frequency of this possible conflict varies with the level of discharge desired in the Fox River from 1 year in 60 for a discharge of 1,100 ft^/s to about 1 year in 15 for a discharge of 1,500 ft^/s.</p>","language":"English","publisher":"U.S. Geological Survey","doi":"10.3133/wri80107","collaboration":"Prepared in cooperation with Wisconsin Department of Natural Resources, Fox Valley Water Quality Planning Agency","usgsCitation":"Krug, W.R., 1981, Hydrologic effects of proposed changes in management practices, Winnebago Pool, Wisconsin: U.S. Geological Survey Water-Resources Investigations Report 80-107, iv, 19 p., https://doi.org/10.3133/wri80107.","productDescription":"iv, 19 p.","numberOfPages":"25","onlineOnly":"N","additionalOnlineFiles":"N","costCenters":[{"id":677,"text":"Wisconsin Water Science Center","active":true,"usgs":true}],"links":[{"id":158637,"rank":0,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/wri/1980/0107/report-thumb.jpg"},{"id":56982,"rank":300,"type":{"id":11,"text":"Document"},"url":"https://pubs.usgs.gov/wri/1980/0107/report.pdf","linkFileType":{"id":1,"text":"pdf"}}],"country":"United States","state":"Wisconsin","otherGeospatial":"Fox River, Lake Butte des Morts, Lake Poygan, Lake Winneconne, Lake Winnebago","geographicExtents":"{\n  \"type\": \"FeatureCollection\",\n  \"features\": [\n    {\n      \"type\": \"Feature\",\n      \"properties\": {},\n      \"geometry\": {\n        \"type\": \"Polygon\",\n        \"coordinates\": [\n          [\n            [\n              -90.2911376953125,\n              42.867912483915305\n            ],\n            [\n              -90.2911376953125,\n              44.70770622183535\n            ],\n            [\n              -87.57202148437499,\n              44.70770622183535\n            ],\n            [\n              -87.57202148437499,\n              42.867912483915305\n            ],\n            [\n              -90.2911376953125,\n              42.867912483915305\n            ]\n          ]\n        ]\n      }\n    }\n  ]\n}","noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"4f4e4a1be4b07f02db606f7d","contributors":{"authors":[{"text":"Krug, William R.","contributorId":53381,"corporation":false,"usgs":true,"family":"Krug","given":"William","email":"","middleInitial":"R.","affiliations":[],"preferred":false,"id":199306,"contributorType":{"id":1,"text":"Authors"},"rank":1}]}}
,{"id":56902,"text":"wdrUT801 - 1981 - Water resources data for Utah, water year 1980","interactions":[],"lastModifiedDate":"2025-02-20T14:59:13.016642","indexId":"wdrUT801","displayToPublicDate":"1994-01-01T00:00:00","publicationYear":"1981","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":"UT-80-1","title":"Water resources data for Utah, water year 1980","docAbstract":"<p>Water resources data for the 1980 water year for Utah 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 ground water. This report contains discharge records for 294 gaging stations; stage and contents for 22 lakes and reservoirs; water quality for 64 hydrologic stations, 194 partial-record stations, and 323 wells; and water levels for 36 observation wells. Additional water data were collected at various sites, not involved in the systematic data collection program, and are published as miscellaneous measurements. These data represent that part of the National Water Data System collected by the U.S. Geological Survey and cooperating State and Federal agencies in Utah.</p>","language":"English","publisher":"U.S. Geological Survey","doi":"10.3133/wdrUT801","collaboration":"Prepared in cooperation with the State of Utah and with other agencies","usgsCitation":"Water Resources Division, U.S. Geological Survey, 1981, Water resources data for Utah, water year 1980: U.S. Geological Survey Water Data Report UT-80-1, xv, 684 p., https://doi.org/10.3133/wdrUT801.","productDescription":"xv, 684 p.","costCenters":[{"id":610,"text":"Utah Water Science 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,{"id":43688,"text":"ofr81494 - 1981 - Hydrologic description of Lake Jackson, Sebring, Florida","interactions":[],"lastModifiedDate":"2022-04-18T23:20:19.771099","indexId":"ofr81494","displayToPublicDate":"1994-01-01T00:00:00","publicationYear":"1981","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":"81-494","title":"Hydrologic description of Lake Jackson, Sebring, Florida","docAbstract":"<p>No abstract available.</p>","language":"English","publisher":"U.S. Geological Survey","doi":"10.3133/ofr81494","usgsCitation":"Hammett, K., 1981, Hydrologic description of Lake Jackson, Sebring, Florida: U.S. Geological Survey Open-File Report 81-494, 1 Plate: 38.51 x 29.02 inches, https://doi.org/10.3133/ofr81494.","productDescription":"1 Plate: 38.51 x 29.02 inches","costCenters":[],"links":[{"id":399061,"rank":3,"type":{"id":17,"text":"Plate"},"url":"https://pubs.usgs.gov/of/1981/0494/plate-1.pdf","linkFileType":{"id":1,"text":"pdf"}},{"id":397145,"rank":2,"type":{"id":36,"text":"NGMDB Index Page"},"url":"https://ngmdb.usgs.gov/Prodesc/proddesc_12052.htm"},{"id":161801,"rank":0,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/of/1981/0494/report-thumb.jpg"}],"country":"United States","state":"Florida","city":"Sebring","otherGeospatial":"Lake Jackson","geographicExtents":"{\n  \"type\": \"FeatureCollection\",\n  \"features\": [\n    {\n      \"type\": \"Feature\",\n      \"properties\": {},\n      \"geometry\": {\n        \"type\": \"Polygon\",\n        \"coordinates\": [\n          [\n            [\n              -81.53778076171874,\n              27.358351545806766\n            ],\n            [\n              -81.38397216796875,\n              27.358351545806766\n            ],\n            [\n              -81.38397216796875,\n              27.577677346218785\n            ],\n            [\n              -81.53778076171874,\n              27.577677346218785\n            ],\n            [\n              -81.53778076171874,\n              27.358351545806766\n            ]\n          ]\n        ]\n      }\n    }\n  ]\n}","noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"4f4e4ae2e4b07f02db688d20","contributors":{"authors":[{"text":"Hammett, K.M.","contributorId":59006,"corporation":false,"usgs":true,"family":"Hammett","given":"K.M.","email":"","affiliations":[],"preferred":false,"id":228560,"contributorType":{"id":1,"text":"Authors"},"rank":1}]}}
,{"id":43687,"text":"ofr81131 - 1981 - Hydrologic description of Lake Hancock, Polk County, Florida","interactions":[],"lastModifiedDate":"2022-04-18T22:09:07.628369","indexId":"ofr81131","displayToPublicDate":"1994-01-01T00:00:00","publicationYear":"1981","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":"81-131","title":"Hydrologic description of Lake Hancock, Polk County, Florida","docAbstract":"<p>Available data were evaluated to document hydrologic conditions in the Lake Hancock basin. Bathymetric data indicate that Lake Hancock is very shallow, having a maximum depth of about 3 feet. The lake bottom is covered by a layer of organic material that may be more than 5 feet thick near the center of the lake. Lake Hancock 's stage fluctuates within 0.5 foot of average stage about 40 percent of the time. Lake outflow is through an operable control. There are many days with no outflow in some years. A water-budget analysis of the lake indicates that substantial lake stage declines in 1968 and 1975 followed successive years of deficient precipitation and were primarily the result of a net loss of water from the lake to the ground-water system. During a period in 1971-72 when lake stage remained relatively stable, the ground-water system contributed a significant volume of water to the lake. Water-quality data indicate that Lake Hancock is in a eutrophic state. The eutrophication process appears to have been accelerated through the addition of nutrients from inflow of wastewater effluent from secondary treatment plants.&nbsp;</p>","language":"English","publisher":"U.S. Geological Survey","doi":"10.3133/ofr81131","collaboration":"Prepared in cooperation with Southwest Florida Water Management District","usgsCitation":"Hammett, K., Snell, L., and Joyner, B.F., 1981, Hydrologic description of Lake Hancock, Polk County, Florida: U.S. Geological Survey Open-File Report 81-131, 1 Plate: 41.76 x 32.92 inches, https://doi.org/10.3133/ofr81131.","productDescription":"1 Plate: 41.76 x 32.92 inches","costCenters":[],"links":[{"id":399016,"rank":2,"type":{"id":17,"text":"Plate"},"url":"https://pubs.usgs.gov/of/1981/0131/plate-1.pdf","linkFileType":{"id":1,"text":"pdf"}},{"id":161800,"rank":0,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/of/1981/0131/report-thumb.jpg"}],"country":"United States","state":"Florida","county":"Polk County","otherGeospatial":"Lake 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,{"id":46212,"text":"ofr81530 - 1981 - Maps Showing Ground-Water Conditions in the San Simon Wash Area, Papago Indian Reservation, Arizona - 1979","interactions":[],"lastModifiedDate":"2012-02-10T00:10:10","indexId":"ofr81530","displayToPublicDate":"1994-01-01T00:00:00","publicationYear":"1981","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":"81-530","title":"Maps Showing Ground-Water Conditions in the San Simon Wash Area, Papago Indian Reservation, Arizona - 1979","docAbstract":"INTRODUCTION\r\n\r\nThe San Simon Wash area includes about 2,300 mi2 in the Papago Indian Reservation in south-central Arizona and is characterized by low mountains separated by broad alluvial basins. Most of the basins and mountains trend north and slightly northwest. The basins are underlain by a thick sequence of basin-fill deposits. The mountains are composed of crystalline and consolidated sedimentary rocks, and thin alluvial deposits are present in the narrow mountain valleys and on pediments.\r\n\r\nThe climate is semiarid, and the precipitation pattern is characterized by two distinct types of storms--local summer thunderstorms and regional winter storms. In most of the area the average annual precipitation ranges from 5 to 10 in.; in the Baboquivari Mountains, however, the average annual precipitation is 20 in. (Sellers and Hill, 1974, p. 7). Owing to the small amount of precipitation and the abundant sunshine, the evaporation rate is about 8 to 10 times the average rainfall (Heindl and others, 1962). Storm runoff occurs mainly as sheetflow and floods of short duration. Although some runoff is diverted to catchment tanks for use by livestock, runoff is not known to be diverted for irrigation or public-supply uses.\r\n\r\nGround-water development has been slight compared with that in many areas in Arizona. In 1979 about 2,700 acre-ft of ground water was withdrawn, of which 2,200 acre-ft was used for irrigation at Papago Farms, and 500 acre-ft was used for public and livestock supplies.\r\n\r\nThe hydrologic data on which these maps are based are available, for the most part, in computer-printout form and may be consulted at the Arizona Department of Water Resources, 99 East Virginia, Phoenix, and at U.S. Geological Survey offices in: Federal Building, 301 West Congress Street, Tucson, and Valley Center, Suite 1880, Phoenix. Material from which copies can be made at private expense is available at the Tucson and Phoenix offices of the U.S. Geological Survey.","language":"ENGLISH","publisher":"Geological Survey (U.S.)","doi":"10.3133/ofr81530","collaboration":"Prepared in cooperation with the U.S. Bureau of Indian Affairs and the Arizona Department of Water Resources","usgsCitation":"Hollet, K.J., 1981, Maps Showing Ground-Water Conditions in the San Simon Wash Area, Papago Indian Reservation, Arizona - 1979: U.S. Geological Survey Open-File Report 81-530, 2 Maps, https://doi.org/10.3133/ofr81530.","productDescription":"2 Maps","costCenters":[{"id":595,"text":"U.S. Geological Survey","active":false,"usgs":true}],"links":[{"id":172007,"rank":0,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/thumbnails/usgs_thumb.jpg"},{"id":83178,"rank":400,"type":{"id":17,"text":"Plate"},"url":"https://pubs.usgs.gov/of/1981/0530/plate-1.pdf","linkFileType":{"id":1,"text":"pdf"}},{"id":83179,"rank":401,"type":{"id":17,"text":"Plate"},"url":"https://pubs.usgs.gov/of/1981/0530/plate-2.pdf","linkFileType":{"id":1,"text":"pdf"}}],"scale":"250000","geographicExtents":"{ \"type\": \"FeatureCollection\", \"features\": [ { \"type\": \"Feature\", \"properties\": {}, \"geometry\": { \"type\": \"Polygon\", \"coordinates\": [ [ [ -112.75,31.5 ], [ -112.75,32.583333333333336 ], [ -111.5,32.583333333333336 ], [ -111.5,31.5 ], [ -112.75,31.5 ] ] ] } } ] }","noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"4f4e4a81e4b07f02db64a2a3","contributors":{"authors":[{"text":"Hollet, Kenneth J.","contributorId":104971,"corporation":false,"usgs":true,"family":"Hollet","given":"Kenneth","email":"","middleInitial":"J.","affiliations":[],"preferred":false,"id":232845,"contributorType":{"id":1,"text":"Authors"},"rank":1}]}}
,{"id":12259,"text":"ofr811186 - 1981 - Reconnaissance of the ground-water resources of Kings and Queens counties, New York","interactions":[],"lastModifiedDate":"2012-02-02T00:06:41","indexId":"ofr811186","displayToPublicDate":"1994-01-01T00:00:00","publicationYear":"1981","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":"81-1186","title":"Reconnaissance of the ground-water resources of Kings and Queens counties, New York","docAbstract":"Western Long Island 's ground-water resources are being considered for redevelopment as a supplemental source of public water supply. The ground-water reservoir in Kings and Queens Counties had supplied an average of more than 120 million gallons per day for industrial and public water supply from 1904 to 1947. However, deterioration of groundwater quality from induced encroachment of salty ground-water caused the total cessation of pumping for public supply in Kings County in 1947 and in western Queens County in 1974. This investigation was designed to make a preliminary evaluation of the present groundwater quality and to review hydrologic information pertinent to the formulation of an appropriate development plan. Detailed hydrogeologic mapping was done to define the geometry of the ground-water system. The history of ground-water development and the consequent responses of ground-water levels and quantity were summarized. A well network was established to monitor ground-water levels and ground-water quality in Kings and Queens Counties. The distribution of chloride and nitrate in ground-water was used to identify contamination from salt-water intrusion and surface sources. A limited source of potable ground-water is available in the Magothy-Jameco and Lloyd aquifers; however, an accurate estimate of the quantity of water available or a draft rate suitable for maintaining a useable ground-water quality is undetermined. (USGS)","language":"ENGLISH","publisher":"U.S. Geological Survey,","doi":"10.3133/ofr811186","usgsCitation":"Buxton, H., Soren, J., Posner, A., and Shernoff, P., 1981, Reconnaissance of the ground-water resources of Kings and Queens counties, New York: U.S. Geological Survey Open-File Report 81-1186, 64 p., ill., maps ;28 cm., https://doi.org/10.3133/ofr811186.","productDescription":"64 p., ill., maps ;28 cm.","costCenters":[],"links":[{"id":145567,"rank":0,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/of/1981/1186/report-thumb.jpg"},{"id":40423,"rank":300,"type":{"id":11,"text":"Document"},"url":"https://pubs.usgs.gov/of/1981/1186/report.pdf","linkFileType":{"id":1,"text":"pdf"}}],"noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"4f4e4ac9e4b07f02db67c497","contributors":{"authors":[{"text":"Buxton, H. T.","contributorId":67873,"corporation":false,"usgs":true,"family":"Buxton","given":"H. T.","affiliations":[],"preferred":false,"id":165675,"contributorType":{"id":1,"text":"Authors"},"rank":1},{"text":"Soren, Julian","contributorId":54184,"corporation":false,"usgs":true,"family":"Soren","given":"Julian","email":"","affiliations":[],"preferred":false,"id":165674,"contributorType":{"id":1,"text":"Authors"},"rank":2},{"text":"Posner, Alex","contributorId":18376,"corporation":false,"usgs":true,"family":"Posner","given":"Alex","email":"","affiliations":[],"preferred":false,"id":165672,"contributorType":{"id":1,"text":"Authors"},"rank":3},{"text":"Shernoff, P. K.","contributorId":22779,"corporation":false,"usgs":true,"family":"Shernoff","given":"P. K.","affiliations":[],"preferred":false,"id":165673,"contributorType":{"id":1,"text":"Authors"},"rank":4}]}}
,{"id":22129,"text":"ofr8160 - 1981 - Sample mine-site permit application (hydrologic assessment)","interactions":[],"lastModifiedDate":"2017-06-27T11:17:49","indexId":"ofr8160","displayToPublicDate":"1994-01-01T00:00:00","publicationYear":"1981","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":"81-60","title":"Sample mine-site permit application (hydrologic assessment)","docAbstract":"<p>Hydrologic data are presented that may be useful in the permitapplication procedure required under current Office of Surface Mining regulations. The material is presented in a format which may serve as a guide for subsequent permit applications. Data on the quality and quantity of surface water and ground water for the mine plan, adjacent, and general areas are presented. The data are presented in three general categories: measured and estimated current conditions, estimated annual variations, and predicted effects of mining and reclamation. Current surface-water, ground-water, and biological conditions are the easiest to define. Seasonal variations in surface-water flow can be estimated with some confidence, but seasonal variations in surface-water quality, biological quality, and ground-water levels and quality are difficult to estimate with the insufficient field data available. The effects of mining and reclamation cannot be predicted through the use of the scant data collected and current predictive tools.</p>","language":"English","publisher":"U.S. Geological Survey","doi":"10.3133/ofr8160","issn":"0094-9140","usgsCitation":"Herb, W.J., Brown, D., Carswell, L., and Lietman, P., 1981, Sample mine-site permit application (hydrologic assessment): U.S. Geological Survey Open-File Report 81-60, 57 p. ill., charts, maps ;28 cm., https://doi.org/10.3133/ofr8160.","productDescription":"57 p. ill., charts, maps ;28 cm.","costCenters":[{"id":532,"text":"Pennsylvania Water Science Center","active":true,"usgs":true}],"links":[{"id":154960,"rank":0,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/of/1981/0060/report-thumb.jpg"},{"id":51578,"rank":300,"type":{"id":11,"text":"Document"},"url":"https://pubs.usgs.gov/of/1981/0060/report.pdf","linkFileType":{"id":1,"text":"pdf"}}],"noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"4f4e4aaee4b07f02db66c845","contributors":{"authors":[{"text":"Herb, William J.","contributorId":79454,"corporation":false,"usgs":true,"family":"Herb","given":"William","email":"","middleInitial":"J.","affiliations":[],"preferred":false,"id":187239,"contributorType":{"id":1,"text":"Authors"},"rank":1},{"text":"Brown, D.M.","contributorId":80657,"corporation":false,"usgs":true,"family":"Brown","given":"D.M.","affiliations":[],"preferred":false,"id":187240,"contributorType":{"id":1,"text":"Authors"},"rank":2},{"text":"Carswell, L.D.","contributorId":6435,"corporation":false,"usgs":true,"family":"Carswell","given":"L.D.","email":"","affiliations":[],"preferred":false,"id":187237,"contributorType":{"id":1,"text":"Authors"},"rank":3},{"text":"Lietman, P. L.","contributorId":63040,"corporation":false,"usgs":true,"family":"Lietman","given":"P. L.","affiliations":[],"preferred":false,"id":187238,"contributorType":{"id":1,"text":"Authors"},"rank":4}]}}
,{"id":23739,"text":"ofr81535 - 1981 - Hydrology of the Ferron sandstone aquifer and effects of proposed surface-coal mining in Castle Valley, Utah","interactions":[{"subject":{"id":23739,"text":"ofr81535 - 1981 - Hydrology of the Ferron sandstone aquifer and effects of proposed surface-coal mining in Castle Valley, Utah","indexId":"ofr81535","publicationYear":"1981","noYear":false,"title":"Hydrology of the Ferron sandstone aquifer and effects of proposed surface-coal mining in Castle Valley, Utah"},"predicate":"SUPERSEDED_BY","object":{"id":3192,"text":"wsp2195 - 1983 - Hydrology of the Ferron Sandstone aquifer and effects of proposed surface-coal mining in Castle Valley, Utah, with a section on stratigraphy and a section on leaching of overburden","indexId":"wsp2195","publicationYear":"1983","noYear":false,"title":"Hydrology of the Ferron Sandstone aquifer and effects of proposed surface-coal mining in Castle Valley, Utah, with a section on stratigraphy and a section on leaching of overburden"},"id":1}],"supersededBy":{"id":3192,"text":"wsp2195 - 1983 - Hydrology of the Ferron Sandstone aquifer and effects of proposed surface-coal mining in Castle Valley, Utah, with a section on stratigraphy and a section on leaching of overburden","indexId":"wsp2195","publicationYear":"1983","noYear":false,"title":"Hydrology of the Ferron Sandstone aquifer and effects of proposed surface-coal mining in Castle Valley, Utah, with a section on stratigraphy and a section on leaching of overburden"},"lastModifiedDate":"2025-09-11T16:21:35.852856","indexId":"ofr81535","displayToPublicDate":"1994-01-01T00:00:00","publicationYear":"1981","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":"81-535","title":"Hydrology of the Ferron sandstone aquifer and effects of proposed surface-coal mining in Castle Valley, Utah","docAbstract":"<p>No abstract available.</p>","language":"English","publisher":"U.S. Geological Survey","doi":"10.3133/ofr81535","issn":"0094-9140","collaboration":"Prepared in cooperation with the U.S. Bureau of Land Management","usgsCitation":"Lines, G.C., and Morrissey, D.J., 1981, Hydrology of the Ferron sandstone aquifer and effects of proposed surface-coal mining in Castle Valley, Utah: U.S. Geological Survey Open-File Report 81-535, 94 p., https://doi.org/10.3133/ofr81535.","productDescription":"94 p.","costCenters":[],"links":[{"id":495331,"rank":2,"type":{"id":11,"text":"Document"},"url":"https://pubs.usgs.gov/of/1981/0535/report.pdf","linkFileType":{"id":1,"text":"pdf"}},{"id":156804,"rank":1,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/of/1981/0535/report-thumb.jpg"}],"country":"United States","state":"Utah","city":"Castle 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Gregory C.","contributorId":50502,"corporation":false,"usgs":true,"family":"Lines","given":"Gregory","email":"","middleInitial":"C.","affiliations":[],"preferred":false,"id":190628,"contributorType":{"id":1,"text":"Authors"},"rank":1},{"text":"Morrissey, Daniel J.","contributorId":89875,"corporation":false,"usgs":true,"family":"Morrissey","given":"Daniel","email":"","middleInitial":"J.","affiliations":[],"preferred":false,"id":190629,"contributorType":{"id":1,"text":"Authors"},"rank":2}]}}
,{"id":8969,"text":"ofr80422 - 1981 - Model of the ground-water flow system of the Gordo and Eutaw aquifers in west-central Alabama","interactions":[],"lastModifiedDate":"2025-09-15T15:48:19.995794","indexId":"ofr80422","displayToPublicDate":"1994-01-01T00:00:00","publicationYear":"1981","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":"80-422","title":"Model of the ground-water flow system of the Gordo and Eutaw aquifers in west-central Alabama","docAbstract":"<p>Hydrologic conditions for a two-aquifer system consisting of the Gordo and Eutaw aquifers of Cretaceous age in west-central Alabama were simulated using a three-dimensional finite difference digital model. The model was calibrated to observed heads in the aquifers using a least squares method for obtaining the values for hydraulic parameters which provided the best fit to 28 calibration points in the model. The standard error of estimate for computed heads in the model is 3.46 feet.</p><p>Data collected during the period of 1900 to 1970 indicate that the modeled aquifer system is in a steady-state condition. The results of steady-state model simulations show that about 56 percent of the discharge from the system is by upward vertical leakage through confining beds to rivers, about 18 percent is to unregulated flowing wells, 10 percent is to pumped wells, and 16 percent is to boundaries. The areal distribution of water in the aquifer containing chloride concentrations greater than 1,000 mg/L appears to be related to flow patterns in the system.</p><p>Areas of greatest head loss in the system are those where there is natural discharge and pumpage. More than 80 percent of the head loss in the system can be attributed to natural discharge by upward leakage through the confining beds.</p>","language":"English","publisher":"U.S. Geological Survey","doi":"10.3133/ofr80422","collaboration":"Prepared by the United States Geological Survey in cooperation with Geological Survey of Alabama","usgsCitation":"Gardner, R.A., 1981, Model of the ground-water flow system of the Gordo and Eutaw aquifers in west-central Alabama: U.S. Geological Survey Open-File Report 80-422, Report: 30 p.; 23 Figures: 7.61 x 10.38 inches or smaller, https://doi.org/10.3133/ofr80422.","productDescription":"Report: 30 p.; 23 Figures: 7.61 x 10.38 inches or smaller","costCenters":[],"links":[{"id":495502,"rank":24,"type":{"id":29,"text":"Figure"},"url":"https://pubs.usgs.gov/of/1980/0422/figure-24.pdf","text":"Figure 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,{"id":31091,"text":"ofr81628 - 1981 - Hydrologic data for urban studies in the Austin, Texas, metropolitan area, 1979","interactions":[],"lastModifiedDate":"2025-09-11T16:18:31.221766","indexId":"ofr81628","displayToPublicDate":"1994-01-01T00:00:00","publicationYear":"1981","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":"81-628","title":"Hydrologic data for urban studies in the Austin, Texas, metropolitan area, 1979","docAbstract":"<p>Hydrologic investigations of urban watersheds in Texas were begun by theU.S. Geological Survey in 1954. Studies are now in progress in Austin, Houston, and San Antonio. Studies have been completed in the Dallas and Fort Worth areas.</p><p>The Geological Survey, in cooperation with the Texas Department of Water Resources, began hydrologic studies in the Austin urban area in 1954. In cooperation with the city of Austin, the program was expanded in 1975 to include additional streamflow and rainfall gaging stations, and the collection of surface water-quality data. In 1978, the program was expanded to include a ground-water resources study of the South Austin metropolitan area in the Balcones fault zone.</p>","language":"English","publisher":"U.S. Geological Survey","doi":"10.3133/ofr81628","usgsCitation":"Slade, R., Dorsey, M., Gordon, J., Mitchell, R., and Gaylord, J., 1981, Hydrologic data for urban studies in the Austin, Texas, metropolitan area, 1979: U.S. Geological Survey Open-File Report 81-628, 281 p., https://doi.org/10.3133/ofr81628.","productDescription":"281 p.","onlineOnly":"N","additionalOnlineFiles":"N","costCenters":[{"id":583,"text":"Texas Water Science Center","active":true,"usgs":true}],"links":[{"id":495330,"rank":2,"type":{"id":11,"text":"Document"},"url":"https://pubs.usgs.gov/of/1981/0628/report.pdf","linkFileType":{"id":1,"text":"pdf"}},{"id":160830,"rank":1,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/of/1981/0628/report-thumb.jpg"}],"country":"United States","state":"Texas","city":"Austin","geographicExtents":"{\n  \"type\": \"FeatureCollection\",\n  \"features\": [\n    {\n      \"type\": \"Feature\",\n      \"properties\": {},\n      \"geometry\": {\n        \"type\": \"Polygon\",\n        \"coordinates\": [\n          [\n            [\n              -98.09280395507812,\n              29.991812888666043\n            ],\n            [\n              -97.38006591796874,\n              29.991812888666043\n            ],\n            [\n              -97.38006591796874,\n              30.615459280672667\n            ],\n            [\n              -98.09280395507812,\n              30.615459280672667\n            ],\n            [\n              -98.09280395507812,\n              29.991812888666043\n            ]\n          ]\n        ]\n      }\n    }\n  ]\n}","noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"4f4e4a1ce4b07f02db607f18","contributors":{"authors":[{"text":"Slade, R.M.","contributorId":84364,"corporation":false,"usgs":true,"family":"Slade","given":"R.M.","affiliations":[],"preferred":false,"id":204939,"contributorType":{"id":1,"text":"Authors"},"rank":1},{"text":"Dorsey, M.E.","contributorId":73997,"corporation":false,"usgs":true,"family":"Dorsey","given":"M.E.","email":"","affiliations":[],"preferred":false,"id":204938,"contributorType":{"id":1,"text":"Authors"},"rank":2},{"text":"Gordon, J.D.","contributorId":26684,"corporation":false,"usgs":true,"family":"Gordon","given":"J.D.","email":"","affiliations":[],"preferred":false,"id":204936,"contributorType":{"id":1,"text":"Authors"},"rank":3},{"text":"Mitchell, R.N.","contributorId":94301,"corporation":false,"usgs":true,"family":"Mitchell","given":"R.N.","email":"","affiliations":[],"preferred":false,"id":204940,"contributorType":{"id":1,"text":"Authors"},"rank":4},{"text":"Gaylord, J.L.","contributorId":46520,"corporation":false,"usgs":true,"family":"Gaylord","given":"J.L.","email":"","affiliations":[],"preferred":false,"id":204937,"contributorType":{"id":1,"text":"Authors"},"rank":5}]}}
,{"id":8877,"text":"ofr81813 - 1981 - Index to active hydrologic data collection sites in Florida, 1980-81","interactions":[{"subject":{"id":15989,"text":"ofr80220 - 1980 - Index to active hydrologic data collection sites in Florida, 1978-79","indexId":"ofr80220","publicationYear":"1980","noYear":false,"title":"Index to active hydrologic data collection sites in Florida, 1978-79"},"predicate":"SUPERSEDED_BY","object":{"id":8877,"text":"ofr81813 - 1981 - Index to active hydrologic data collection sites in Florida, 1980-81","indexId":"ofr81813","publicationYear":"1981","noYear":false,"title":"Index to active hydrologic data collection sites in Florida, 1980-81"},"id":1}],"lastModifiedDate":"2025-12-11T18:33:29.14673","indexId":"ofr81813","displayToPublicDate":"1994-01-01T00:00:00","publicationYear":"1981","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":"81-813","title":"Index to active hydrologic data collection sites in Florida, 1980-81","docAbstract":"<p>This index contains a list of active data-collection sites in Florida operated by the U.S. Geological Survey in cooperation with local, State, and Federal agencies during the period from October 1, 1980 through September 30, 1981. It is an update of \"Index to Active Hydrologic Data Collection Sites in Florida, 1978-79\" by J. D. Simmons, 1980, which was released as U.S. Geological Survey Open-File Report 80-220. 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,{"id":68299,"text":"ha653 - 1981 - Flood of July 1-5, 1978 on the Kickapoo River, southwestern Wisconsin","interactions":[],"lastModifiedDate":"2015-10-05T16:21:59","indexId":"ha653","displayToPublicDate":"1994-01-01T00:00:00","publicationYear":"1981","noYear":false,"publicationType":{"id":18,"text":"Report"},"publicationSubtype":{"id":5,"text":"USGS Numbered Series"},"seriesTitle":{"id":318,"text":"Hydrologic Atlas","code":"HA","active":false,"publicationSubtype":{"id":5}},"seriesNumber":"653","title":"Flood of July 1-5, 1978 on the Kickapoo River, southwestern Wisconsin","docAbstract":"<p>The Kickapoo River valley in southwestern Wisconsin had a devastating flood ($10 million estimated damages) during July 1-5, 1978. The flash flooding was caused by intense storms on June 30 through July 2. Total rainfall accumulation ranged from 5.8 inches near Ontario to 9.5 inches at La Farge. The resulting flood equaled or exceeded the largest ones recorded since the 1850 's and equaled or exceeded the 100-year flood frequency at the U.S. Geological Survey 's streamflow gages at La Farge and Steuben. Elevation and delineation of the flood are shown on photo mosaics developed from black and white aerial photographs. The 100-mile reach from Wauzeka to Wilton is shown. A summary of the storm conditions causing the flood and an analysis of the rainfall totals, as prepared by the Wisconsin Geological and Natural History Survey, are also included. (USGS)</p>","language":"English","publisher":"U.S. Geological Society","doi":"10.3133/ha653","usgsCitation":"Hughes, P.E., Hannuksela, J., and Danchuk, W., 1981, Flood of July 1-5, 1978 on the Kickapoo River, southwestern Wisconsin: U.S. Geological Survey Hydrologic Atlas 653, 6 Sheets: 37.50 x 25.42 inches or smaller, https://doi.org/10.3133/ha653.","productDescription":"6 Sheets: 37.50 x 25.42 inches or smaller","onlineOnly":"N","additionalOnlineFiles":"N","costCenters":[{"id":677,"text":"Wisconsin Water Science 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,{"id":68690,"text":"ha650 - 1981 - Geologic structure, hydrology, and water quality of the Laramie-Fox Hills aquifer in the Denver basin, Colorado","interactions":[],"lastModifiedDate":"2022-08-25T20:15:42.86453","indexId":"ha650","displayToPublicDate":"1994-01-01T00:00:00","publicationYear":"1981","noYear":false,"publicationType":{"id":18,"text":"Report"},"publicationSubtype":{"id":5,"text":"USGS Numbered Series"},"seriesTitle":{"id":318,"text":"Hydrologic Atlas","code":"HA","active":false,"publicationSubtype":{"id":5}},"seriesNumber":"650","title":"Geologic structure, hydrology, and water quality of the Laramie-Fox Hills aquifer in the Denver basin, Colorado","docAbstract":"<p>The Denver ground-water basin underlies a 6,700-square-mile area extending from Greeley in the north to Colorado Springs in the south, and from the Front Range in the west to near Limon in the east.&nbsp; The four major bedrock aquifers that occur in the basin are the Laramie-Fox Hills aquifer (the deepest aquifer), the Arapahoe aquifer, the Denver aquifer, and the Dawson aquifer (the uppermost aquifer).&nbsp; The Laramie-Fox Hills aquifer, which is the subject of this report, underlies the entire area of the basin in east-central Colorado (index map, fig. 1) and is an important source of water for residents in the northern Denver suburban area and in the rural areas of eastern Jefferson, Arapahoe, and Elbert Counties, Adams County, and southern Weld and El Paso Counties.&nbsp; About 90 percent of the estimated 1,700 wells completed in the aquifer supply water to residents and livestock.&nbsp; The remaining wells supply water for commercial and industrial use and limited irrigation of commercial crops.</p>","language":"English","publisher":"U.S. Geological Survey","doi":"10.3133/ha650","usgsCitation":"Robson, S.G., 1981, Geologic structure, hydrology, and water quality of the Laramie-Fox Hills aquifer in the Denver basin, Colorado: U.S. Geological Survey Hydrologic Atlas 650, 3 Plates: 34.74 x 40.63 inches or smaller, https://doi.org/10.3133/ha650.","productDescription":"3 Plates: 34.74 x 40.63 inches or smaller","onlineOnly":"N","additionalOnlineFiles":"N","costCenters":[],"links":[{"id":90408,"rank":400,"type":{"id":17,"text":"Plate"},"url":"https://pubs.usgs.gov/ha/650/plate-1.pdf","linkFileType":{"id":1,"text":"pdf"}},{"id":405625,"rank":5,"type":{"id":36,"text":"NGMDB Index Page"},"url":"https://ngmdb.usgs.gov/Prodesc/proddesc_16050.htm","linkFileType":{"id":5,"text":"html"}},{"id":187920,"rank":0,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/thumbnails/usgs_thumb.jpg"},{"id":90409,"rank":401,"type":{"id":17,"text":"Plate"},"url":"https://pubs.usgs.gov/ha/650/plate-2.pdf","linkFileType":{"id":1,"text":"pdf"}},{"id":90410,"rank":402,"type":{"id":17,"text":"Plate"},"url":"https://pubs.usgs.gov/ha/650/plate-3.pdf","linkFileType":{"id":1,"text":"pdf"}}],"scale":"500000","country":"United States","state":"Colorado","otherGeospatial":"Denver basin","geographicExtents":"{\n  \"type\": \"FeatureCollection\",\n  \"features\": [\n    {\n      \"type\": \"Feature\",\n      \"properties\": {},\n      \"geometry\": {\n        \"type\": \"Polygon\",\n        \"coordinates\": [\n          [\n            [\n              -105.257,\n              38.661\n            ],\n            [\n              -103.603,\n              38.661\n            ],\n            [\n              -103.603,\n              40.425\n            ],\n            [\n              -105.257,\n              40.425\n            ],\n            [\n              -105.257,\n              38.661\n            ]\n          ]\n        ]\n      }\n    }\n  ]\n}","noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"4f4e4ae0e4b07f02db688117","contributors":{"authors":[{"text":"Robson, Stanley G.","contributorId":73187,"corporation":false,"usgs":true,"family":"Robson","given":"Stanley","email":"","middleInitial":"G.","affiliations":[],"preferred":false,"id":278754,"contributorType":{"id":1,"text":"Authors"},"rank":1}]}}
,{"id":7241,"text":"ofr81403 - 1981 - Hydrology of Area 35, Eastern region, Interior coal province, Illinois and Kentucky","interactions":[],"lastModifiedDate":"2012-02-02T00:05:50","indexId":"ofr81403","displayToPublicDate":"1994-01-01T00:00:00","publicationYear":"1981","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":"81-403","title":"Hydrology of Area 35, Eastern region, Interior coal province, Illinois and Kentucky","language":"ENGLISH","publisher":"U.S. Geological Survey,","doi":"10.3133/ofr81403","usgsCitation":"Zuehls, E., Ryan, G., Peart, D., and Fitzgerald, K.K., 1981, Hydrology of Area 35, Eastern region, Interior coal province, Illinois and Kentucky: U.S. Geological Survey Open-File Report 81-403, v, 82 p. :ill. (some col.), maps (some col.) ;28 cm., https://doi.org/10.3133/ofr81403.","productDescription":"v, 82 p. :ill. (some col.), maps (some col.) ;28 cm.","costCenters":[],"links":[{"id":94759,"rank":300,"type":{"id":11,"text":"Document"},"url":"https://pubs.usgs.gov/of/1981/0403/report.pdf","size":"21275","linkFileType":{"id":1,"text":"pdf"}},{"id":139843,"rank":0,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/of/1981/0403/report-thumb.jpg"}],"noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"4f4e4acce4b07f02db67e76b","contributors":{"authors":[{"text":"Zuehls, E.E.","contributorId":19942,"corporation":false,"usgs":true,"family":"Zuehls","given":"E.E.","email":"","affiliations":[],"preferred":false,"id":154874,"contributorType":{"id":1,"text":"Authors"},"rank":1},{"text":"Ryan, G.L.","contributorId":68727,"corporation":false,"usgs":true,"family":"Ryan","given":"G.L.","email":"","affiliations":[],"preferred":false,"id":154877,"contributorType":{"id":1,"text":"Authors"},"rank":2},{"text":"Peart, D.B.","contributorId":45304,"corporation":false,"usgs":true,"family":"Peart","given":"D.B.","email":"","affiliations":[],"preferred":false,"id":154876,"contributorType":{"id":1,"text":"Authors"},"rank":3},{"text":"Fitzgerald, K. K.","contributorId":34501,"corporation":false,"usgs":true,"family":"Fitzgerald","given":"K.","email":"","middleInitial":"K.","affiliations":[],"preferred":false,"id":154875,"contributorType":{"id":1,"text":"Authors"},"rank":4}]}}
,{"id":7245,"text":"ofr81343 - 1981 - Hydrology of area 4, Eastern Coal Province, Pennsylvania, Ohio, and West Virginia","interactions":[],"lastModifiedDate":"2012-02-02T00:05:49","indexId":"ofr81343","displayToPublicDate":"1994-01-01T00:00:00","publicationYear":"1981","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":"81-343","title":"Hydrology of area 4, Eastern Coal Province, Pennsylvania, Ohio, and West Virginia","docAbstract":"Area 4 (one of the 24 hydrologic areas defining the Eastern Coal Province) is located at the northern end of the Eastern Coal Province in eastern Ohio, northern West Virginia, and western Pennsylvania. It is part of the upper Ohio River basin, which includes the Beaver, Mahoning, and Shenango Rivers. The area is underlain by rocks of the Pottsville, Allegheny, Conemaugh, Monongahela Groups (or Formations) and Dunkard Group. Area 4 has a temperate climate with an annual average rainfall of 38 to 42 inches, most of its area is covered by forest. The soils have a high erosion potential where the vegetation cover is removed. In response to Public Law 95-87, 132 sites were added to the existing surface-water data-collection network in area 4. At these added sites, collected data includes discharge, water quality, sediment, and biology. The data are available from computer storage through the National Water Data Exchange (NAWDEX) or the published annual Water Resources Data reports for Ohio, Pennsylvania, and West Virginia. Hydrologic problems related to mining are: (1) Erosion and increased sedimentation, and (2) degradation of water quality. Erosion and sedimentation are associated chiefly with surface mining. Sediment yields increase drastically when vegetation is removed from the highly erosive soils. Degradation of water quality can be caused by acid-mine drainage from underground and surface mining. More than half the acid-mine drainage effluent in area 4 comes from underground mines. The rest seeps from abandoned surface mines. Usually in reclaimed surface mines the overburden is replaced in such a short time after the coal is taken out that oxidation of acid-forming minerals, commonly pyrite or marcasite, is not complete or is neutralized by the buffering action of calcareous minerals in the soils. (USGS)","language":"ENGLISH","publisher":"U.S. Geological Survey,","doi":"10.3133/ofr81343","usgsCitation":"Roth, D.K., Engelke, M.J., and and others, 1981, Hydrology of area 4, Eastern Coal Province, Pennsylvania, Ohio, and West Virginia: U.S. Geological Survey Open-File Report 81-343, v, 62 p. :ill. (some col.), maps (some col.) ;28 cm., https://doi.org/10.3133/ofr81343.","productDescription":"v, 62 p. :ill. (some col.), maps (some col.) ;28 cm.","costCenters":[],"links":[{"id":94761,"rank":300,"type":{"id":11,"text":"Document"},"url":"https://pubs.usgs.gov/of/1981/0343/report.pdf","size":"18771","linkFileType":{"id":1,"text":"pdf"}},{"id":139902,"rank":0,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/of/1981/0343/report-thumb.jpg"}],"noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"4f4e4a13e4b07f02db602088","contributors":{"authors":[{"text":"Roth, Donald K.","contributorId":30977,"corporation":false,"usgs":true,"family":"Roth","given":"Donald","email":"","middleInitial":"K.","affiliations":[],"preferred":false,"id":154887,"contributorType":{"id":1,"text":"Authors"},"rank":1},{"text":"Engelke, Morris J. Jr.","contributorId":100379,"corporation":false,"usgs":true,"family":"Engelke","given":"Morris","suffix":"Jr.","email":"","middleInitial":"J.","affiliations":[],"preferred":false,"id":154888,"contributorType":{"id":1,"text":"Authors"},"rank":2},{"text":"and others","contributorId":127886,"corporation":true,"usgs":false,"organization":"and others","id":528823,"contributorType":{"id":1,"text":"Authors"},"rank":3}]}}
,{"id":7249,"text":"ofr81815 - 1981 - Hydrology of Area 7, Eastern Coal Province, Ohio","interactions":[],"lastModifiedDate":"2012-02-02T00:05:49","indexId":"ofr81815","displayToPublicDate":"1994-01-01T00:00:00","publicationYear":"1981","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":"81-815","title":"Hydrology of Area 7, Eastern Coal Province, Ohio","docAbstract":"The U.S. Geological Survey established 24 study areas in Eastern Appalachian Coal Province to appraise the hydrology and water resources from Alabama to Pennsylvania. Chemical, physical, biological, and streamflow data were collected from 138 synoptic sites in Area 7, eastern Ohio. The data are evaluated and presented in this report. Area 7 lies within the drainage basins of Muskingum Rivers and Duck and Willis Creeks in eastern Ohio. Walhounding, Tuscarawas, and Little Muskingum, and Muskingum Rivers and Wills and Duck Creeks are the major streams draining the study area.\r\n\r\nIn Ohio, surface and subsurface coal mining has altered the environment. In areas where land has been reclaimed, the environmental stress expected to be temporary. Hydrologic problems related to coal mining are erosion and sedimentation which degrade water-quality. Based on available sediment data, suspended sediment concentration were highest in abandoned mine areas, followed by currently mined and reclaimed areas, and lowest in unmined areas.\r\n\r\nLow pH, high specific conductance, high concentrations of iron, sulfate and manganese, increased sediment yields, discoloration of streambeds, limited aquatic vegetation and animal life typify streams draining areas with abandoned mines. In abandoned mine areas, the specific conductance of water ranged from 800 to 2,300 micromhos; pH ranged from 2.8 to 5.8; dissolved-iron concentrations ranged from 1,000 to 85,000 micrograms per liter; dissolved-sulfate concentrations ranged from 14 to 1,200 milligrams per liter and dissolved-manganese concentration commonly exceeded 2,000 micrograms per liter. Red and yellow coloration on the streambeds were precipitates from the hydrolysis of iron, manganese, and sulfate minerals carried into the stream channel by increased sediment erosion from abandoned coal mines. Trace metal concentrations (arsenic, cadmium, chromium, cobalt, copper, lead, mercury, selenium, and zinc) were generally low. Degradation of fish habitat is illustrated by conceptual model of the aquatic biology related to water chemistry.","language":"ENGLISH","publisher":"U.S. Geological Survey,","doi":"10.3133/ofr81815","usgsCitation":"Engelke, M.J., Roth, D., and and others, 1981, Hydrology of Area 7, Eastern Coal Province, Ohio: U.S. Geological Survey Open-File Report 81-815, v, 60 p. :ill. (some col.), maps (some col.) ;28 cm., https://doi.org/10.3133/ofr81815.","productDescription":"v, 60 p. :ill. (some col.), maps (some col.) ;28 cm.","costCenters":[],"links":[{"id":94764,"rank":300,"type":{"id":11,"text":"Document"},"url":"https://pubs.usgs.gov/of/1981/0815/report.pdf","size":"21723","linkFileType":{"id":1,"text":"pdf"}},{"id":139916,"rank":0,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/of/1981/0815/report-thumb.jpg"}],"noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"4f4e4acce4b07f02db67e780","contributors":{"authors":[{"text":"Engelke, Morris J. Jr.","contributorId":100379,"corporation":false,"usgs":true,"family":"Engelke","given":"Morris","suffix":"Jr.","email":"","middleInitial":"J.","affiliations":[],"preferred":false,"id":154898,"contributorType":{"id":1,"text":"Authors"},"rank":1},{"text":"Roth, D.K.","contributorId":60275,"corporation":false,"usgs":true,"family":"Roth","given":"D.K.","email":"","affiliations":[],"preferred":false,"id":154897,"contributorType":{"id":1,"text":"Authors"},"rank":2},{"text":"and others","contributorId":127886,"corporation":true,"usgs":false,"organization":"and others","id":528824,"contributorType":{"id":1,"text":"Authors"},"rank":3}]}}
,{"id":7311,"text":"ofr8175 - 1981 - Methodology for hydrologic evaluation of a potential surface mine, Red Rim Site, Carbon and Sweetwater counties, Wyoming","interactions":[],"lastModifiedDate":"2012-02-02T00:06:03","indexId":"ofr8175","displayToPublicDate":"1994-01-01T00:00:00","publicationYear":"1981","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":"81-75","title":"Methodology for hydrologic evaluation of a potential surface mine, Red Rim Site, Carbon and Sweetwater counties, Wyoming","language":"ENGLISH","publisher":"U.S. Geological Survey,","doi":"10.3133/ofr8175","usgsCitation":"Frickel, D.G., Shown, L., Hadley, R.F., and Miller, R., 1981, Methodology for hydrologic evaluation of a potential surface mine, Red Rim Site, Carbon and Sweetwater counties, Wyoming: U.S. Geological Survey Open-File Report 81-75, vi, 65 p. :ill., maps ;28 cm., https://doi.org/10.3133/ofr8175.","productDescription":"vi, 65 p. :ill., maps ;28 cm.","costCenters":[],"links":[{"id":140618,"rank":0,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/of/1981/0075/report-thumb.jpg"},{"id":34701,"rank":300,"type":{"id":11,"text":"Document"},"url":"https://pubs.usgs.gov/of/1981/0075/report.pdf","linkFileType":{"id":1,"text":"pdf"}}],"noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"4f4e4a51e4b07f02db629fbe","contributors":{"authors":[{"text":"Frickel, Donald G.","contributorId":23524,"corporation":false,"usgs":true,"family":"Frickel","given":"Donald","email":"","middleInitial":"G.","affiliations":[],"preferred":false,"id":155170,"contributorType":{"id":1,"text":"Authors"},"rank":1},{"text":"Shown, L. M.","contributorId":43757,"corporation":false,"usgs":true,"family":"Shown","given":"L. M.","affiliations":[],"preferred":false,"id":155172,"contributorType":{"id":1,"text":"Authors"},"rank":2},{"text":"Hadley, R. F.","contributorId":27028,"corporation":false,"usgs":true,"family":"Hadley","given":"R.","middleInitial":"F.","affiliations":[],"preferred":false,"id":155171,"contributorType":{"id":1,"text":"Authors"},"rank":3},{"text":"Miller, R.F.","contributorId":83882,"corporation":false,"usgs":true,"family":"Miller","given":"R.F.","email":"","affiliations":[],"preferred":false,"id":155173,"contributorType":{"id":1,"text":"Authors"},"rank":4}]}}
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