{"pageNumber":"358","pageRowStart":"8925","pageSize":"25","recordCount":11004,"records":[{"id":6449,"text":"pp1222 - 1982 - Upper Cretaceous subsurface stratigraphy and structure of coastal Georgia and South Carolina","interactions":[],"lastModifiedDate":"2012-02-02T00:06:03","indexId":"pp1222","displayToPublicDate":"1994-01-01T00:00:00","publicationYear":"1982","noYear":false,"publicationType":{"id":18,"text":"Report"},"publicationSubtype":{"id":5,"text":"USGS Numbered Series"},"seriesTitle":{"id":331,"text":"Professional Paper","code":"PP","onlineIssn":"2330-7102","printIssn":"1044-9612","active":true,"publicationSubtype":{"id":5}},"seriesNumber":"1222","title":"Upper Cretaceous subsurface stratigraphy and structure of coastal Georgia and South Carolina","docAbstract":"Upper Cretaceous subsurface stratigraphy and structure of coastal Georgia and South Carolina is based on the study of 24 wells along two transects, one extending across the seaward-dipping sedimentary basin termed the 'Southeast Georgia Embayment' northeastward to the crest of the Cape Fear Arch, and the other alined east-west, parallel to the basin axis and including the COST GE-l well on the Outer Continental Shelf. A new biostratigraphic analysis, using calcareous nannofossils, of the Fripp Island, S.C., well and reinterpretations of the Clubhouse Crossroads corehole 1, South Carolina, and other wells in South Carolina, Georgia, and northernmost Florida have made possible the comparison and reevaluation of stratigraphic interpretations of the region made by G. S. Gohn and others in 1978 and 1980 and by P. M. Brown and others in 1979. The present study indicates that within the Upper Cretaceous section the stratigraphic units formerly assigned a Cenomanian (Eaglefordian and Woodbinian) age are Coniacian (Austinian) and Turonian (Eaglefordian) in age. A previously described hiatus encompassing Coniacian and Turonian time is not present. More likely, a hiatus is probably present in the upper Turonian, and major gaps in the record are present within the Cenomanian and between the Upper Cretaceous and the pre-Cretaceous basement. \r\n\r\nAfter an erosional episode in Cenomanian time that affected the section beneath eastern Georgia and South Carolina, Upper Cretaceous marine clastic and carbonate rocks were deposited on a regionally subsiding margin that extended to the present Blake Escarpment. In contrast, during Cenozoic time, especially in the Eocene, subsidence and sedimentation rates were uneven across the margin. A thick progradational sequence of carbonate rocks accumulated in the Southeast Georgia Embayment and also built the present Continental Shelf, whereas farther offshore a much thinner layer of sediments was deposited on the Blake Plateau. \r\n\r\nThere is no general agreement on the exact placement of the Cenomanian-Turonian boundary in Europe or the United States Western Interior, and the widespread Sciponoceras gracile ammonite zone represents an interval of equivocal age between accepted Cenomanian and Turonian strata. The extinction of the foraminifer genus Rotalipora took place within the Sciporwceras gracile zone; it is used here to identify the Cenomanian-Turonian boundary. \r\n\r\nPollen zone IV (Complexiopollis-Atlantopollis assemblage zone) is an important and widespread biostratigraphic unit characterized by a distinctive spore and pollen flora. It is consistently associated with lower Turonian calcareous nannofossils on the Atlantic continental margin; these nannofossil assemblages are also present in pollen zone IV, in strata that encompass the Sciponoceras gracile zone and the lower part of the Mytiloides labiatus zone in the Gulf Coastal Plain at Dallas, Tex.","language":"ENGLISH","publisher":"U.S. G.P.O.,","doi":"10.3133/pp1222","usgsCitation":"Valentine, P.C., 1982, Upper Cretaceous subsurface stratigraphy and structure of coastal Georgia and South Carolina: U.S. Geological Survey Professional Paper 1222, 33 p., https://doi.org/10.3133/pp1222.","productDescription":"33 p.","costCenters":[],"links":[{"id":125091,"rank":0,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/pp/1222/report-thumb.jpg"},{"id":33868,"rank":300,"type":{"id":11,"text":"Document"},"url":"https://pubs.usgs.gov/pp/1222/report.pdf","linkFileType":{"id":1,"text":"pdf"}}],"noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"4f4e4a23e4b07f02db60d354","contributors":{"authors":[{"text":"Valentine, Page C. 0000-0002-0485-6266 pvalentine@usgs.gov","orcid":"https://orcid.org/0000-0002-0485-6266","contributorId":1947,"corporation":false,"usgs":true,"family":"Valentine","given":"Page","email":"pvalentine@usgs.gov","middleInitial":"C.","affiliations":[{"id":678,"text":"Woods Hole Coastal and Marine Science Center","active":true,"usgs":true}],"preferred":true,"id":152740,"contributorType":{"id":1,"text":"Authors"},"rank":1}]}}
,{"id":40934,"text":"ofr82565 - 1982 - Potentiometric-surface map of water in the Eagle Sandstone and equivalent units in the northern Great Plains area of Montana","interactions":[],"lastModifiedDate":"2022-09-27T20:51:53.126062","indexId":"ofr82565","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":"82-565","title":"Potentiometric-surface map of water in the Eagle Sandstone and equivalent units in the northern Great Plains area of Montana","docAbstract":"<p>The potentiometric surface of water in the Upper Cretaceous Eagle Sandstone and equivalent units (Virgelle Sandstone and Telegraph Creek Formation) is shown on a base map at a scale of 1:1,000,000. The map is one of a series of maps produced as part of a regional study of aquifers of Cenozoic and Mesozoic age in the northern Great plains of Montana. The contour interval is 200 feet. The map shows that the directions of regional ground-water movement is from west to east except in the extreme northwestern corner where the movement is from east to west. Water is discharged from the Eagle Sandstone to the Missouri River south of the Bearpaw Mountains. In the area north of the Bearpaw Mountains, depressurization from gas production may account for the decline in the potentiometric surface. The average discharge from 115 wells is about 23 gallons per minute and the specific capacity of 85 wells averages 1.4 gallons per minute per foot of drawdown.</p>","language":"English","publisher":"U.S. Geological Survey","doi":"10.3133/ofr82565","usgsCitation":"Levings, G., 1982, Potentiometric-surface map of water in the Eagle Sandstone and equivalent units in the northern Great Plains area of Montana: U.S. Geological Survey Open-File Report 82-565, 1 Plate: 40.81 × 22.83 inches, https://doi.org/10.3133/ofr82565.","productDescription":"1 Plate: 40.81 × 22.83 inches","costCenters":[],"links":[{"id":78824,"rank":400,"type":{"id":17,"text":"Plate"},"url":"https://pubs.usgs.gov/of/1982/0565/plate-1.pdf","linkFileType":{"id":1,"text":"pdf"}},{"id":407484,"rank":3,"type":{"id":36,"text":"NGMDB Index Page"},"url":"https://ngmdb.usgs.gov/Prodesc/proddesc_75643.htm","linkFileType":{"id":5,"text":"html"}},{"id":171535,"rank":0,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/thumbnails/usgs_thumb.jpg"}],"country":"United States","state":"Montana","geographicExtents":"{\n  \"type\": \"FeatureCollection\",\n  \"features\": [\n    {\n      \"type\": \"Feature\",\n      \"properties\": {},\n      \"geometry\": {\n        \"type\": \"Polygon\",\n        \"coordinates\": [\n          [\n            [\n              -112.5,\n              45\n            ],\n            [\n              -104.0417,\n              45\n            ],\n            [\n              -104.0417,\n              49\n            ],\n            [\n              -112.5,\n              49\n            ],\n            [\n              -112.5,\n              45\n            ]\n          ]\n        ]\n      }\n    }\n  ]\n}","noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"4f4e4afde4b07f02db696b88","contributors":{"authors":[{"text":"Levings, Gary W.","contributorId":106889,"corporation":false,"usgs":true,"family":"Levings","given":"Gary W.","affiliations":[],"preferred":false,"id":224205,"contributorType":{"id":1,"text":"Authors"},"rank":1}]}}
,{"id":11677,"text":"ofr82755 - 1982 - Water resources of Rockland Basin, southeastern Idaho","interactions":[],"lastModifiedDate":"2023-02-07T20:36:58.317284","indexId":"ofr82755","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":"82-755","title":"Water resources of Rockland Basin, southeastern Idaho","docAbstract":"<p>Rockland basin comprises about 320 sq mi of the Snake River drainage in southeastern Idaho. Mountain ranges bordering the basin are composed predominantly of limestone and are complexly faulted. Major aquifers include Holocene alluvium, Quaternary-Tertiary volcanic rocks, and Tertiary sedimentary rocks. Groundwater occurs under water table conditions except where it is locally confined. Groundwater discharges to springs in the Deep Creek Mountains and maintains perennial streamflow. Near the mouth of Rock Creek, groundwater movement is northward toward the Snake River. Underflow is estimated to be 51,000 acre-ft/yr. </p><p>Total water yield available to Rockland basin is estimated to be 5.0 in. (85,000 acre-ft) of the estimated 17.3 in. of annual precipitation. Evapotranspiration ranges from 9.9 to 17 in./yr, depending, in part, on altitude of the land surface. </p><p>An estimated 12,000 acre-ft of surface water and 3,500 acre-ft of groundwater are used annually for irrigation. Less than 100 acre-ft of water is used for public supply, domestic, and stock supplies. East Fork Rock Creek supplies the most surface water for irrigation of agricultural lands. </p><p>At the present (1980) state of groundwater development in Rockland basin, streams and aquifers are hydraulically connected. Pumping of groundwater in increased quantities from wells near streams will affect groundwater movement and may diminish streamflow. There are no long-term regional water table declines at present. Continued water level monitoring of selected wells may aid in documenting effects of future management practices on the groundwater system.&nbsp;</p>","language":"English","publisher":"U.S. Geological Survey","doi":"10.3133/ofr82755","usgsCitation":"Williams, R.P., and Young, H., 1982, Water resources of Rockland Basin, southeastern Idaho: U.S. Geological Survey Open-File Report 82-755, v, 68 p., https://doi.org/10.3133/ofr82755.","productDescription":"v, 68 p.","costCenters":[],"links":[{"id":39550,"rank":2,"type":{"id":11,"text":"Document"},"url":"https://pubs.usgs.gov/of/1982/0755/report.pdf","linkFileType":{"id":1,"text":"pdf"}},{"id":145557,"rank":1,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/of/1982/0755/report-thumb.jpg"},{"id":412824,"rank":3,"type":{"id":36,"text":"NGMDB Index Page"},"url":"https://ngmdb.usgs.gov/Prodesc/proddesc_75649.htm"}],"country":"United States","state":"idaho","otherGeospatial":"Rockland Basin","geographicExtents":"{\n  \"type\": \"FeatureCollection\",\n  \"features\": [\n    {\n      \"type\": \"Feature\",\n      \"properties\": {},\n      \"geometry\": {\n        \"coordinates\": [\n          [\n            [\n              -113.00005230365849,\n              42.727096308338844\n            ],\n            [\n              -113.00005230365849,\n              42.31807748978014\n            ],\n            [\n              -112.73189310111351,\n              42.31807748978014\n            ],\n            [\n              -112.73189310111351,\n              42.727096308338844\n            ],\n            [\n              -113.00005230365849,\n              42.727096308338844\n            ]\n          ]\n        ],\n        \"type\": \"Polygon\"\n      }\n    }\n  ]\n}","noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"4f4e4a9ae4b07f02db65da57","contributors":{"authors":[{"text":"Williams, Rhea P.","contributorId":87114,"corporation":false,"usgs":true,"family":"Williams","given":"Rhea","email":"","middleInitial":"P.","affiliations":[],"preferred":false,"id":163557,"contributorType":{"id":1,"text":"Authors"},"rank":1},{"text":"Young, H.W.","contributorId":68278,"corporation":false,"usgs":true,"family":"Young","given":"H.W.","email":"","affiliations":[],"preferred":false,"id":163556,"contributorType":{"id":1,"text":"Authors"},"rank":2}]}}
,{"id":40899,"text":"ofr82562 - 1982 - Potentiometric-surface map of water in the Judith River Formation in the northern Great Plains area of Montana","interactions":[],"lastModifiedDate":"2022-09-27T20:57:58.601919","indexId":"ofr82562","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":"82-562","title":"Potentiometric-surface map of water in the Judith River Formation in the northern Great Plains area of Montana","docAbstract":"<p>The potentiometric surface of the Judith River Formation is mapped at a scale of 1:1,000,000. The map is one of a series produced as part of a regional study of aquifers of Cenozoic and Mesozoic age in the northern Great Plains of Montana. The contour interval is 200 feet. Water in the Judith River Formation occurs under water-table and artesian conditions. The direction of regional ground-water movement is from west to east. Water is discharged from the Judith River Formation to the Milk River from near Havre, Montana, to Malta and to the Missouri River south of the Bearpaw and Little Rocky Mountains. The average discharge from 236 wells is about 10 gallons per minute, and the specific capacity of 186 wells averages 0.66 gallon per minute per foot of drawdown.</p>","language":"English","publisher":"U.S. Geological Survey","doi":"10.3133/ofr82562","usgsCitation":"Levings, G., 1982, Potentiometric-surface map of water in the Judith River Formation in the northern Great Plains area of Montana: U.S. Geological Survey Open-File Report 82-562, 1 Plate: 40.47 × 23.06 inches, https://doi.org/10.3133/ofr82562.","productDescription":"1 Plate: 40.47 × 23.06 inches","costCenters":[],"links":[{"id":407485,"rank":3,"type":{"id":36,"text":"NGMDB Index Page"},"url":"https://ngmdb.usgs.gov/Prodesc/proddesc_75640.htm","linkFileType":{"id":5,"text":"html"}},{"id":78781,"rank":400,"type":{"id":17,"text":"Plate"},"url":"https://pubs.usgs.gov/of/1982/0562/plate-1.pdf","linkFileType":{"id":1,"text":"pdf"}},{"id":172091,"rank":0,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/thumbnails/usgs_thumb.jpg"}],"country":"United States","state":"Montana","geographicExtents":"{\n  \"type\": \"FeatureCollection\",\n  \"features\": [\n    {\n      \"type\": \"Feature\",\n      \"properties\": {},\n      \"geometry\": {\n        \"type\": \"Polygon\",\n        \"coordinates\": [\n          [\n            [\n              -111,\n              45\n            ],\n            [\n              -104.0418,\n              45\n            ],\n            [\n              -104.0418,\n              49\n            ],\n            [\n              -111,\n              49\n            ],\n            [\n              -111,\n              45\n            ]\n          ]\n        ]\n      }\n    }\n  ]\n}","noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"4f4e4ae4e4b07f02db68a2f5","contributors":{"authors":[{"text":"Levings, Gary W.","contributorId":106889,"corporation":false,"usgs":true,"family":"Levings","given":"Gary W.","affiliations":[],"preferred":false,"id":224137,"contributorType":{"id":1,"text":"Authors"},"rank":1}]}}
,{"id":42103,"text":"ofr82275 - 1982 - Altitude and configuration of the predevelopment water table in the High Plains regional aquifer, northwestern Oklahoma","interactions":[],"lastModifiedDate":"2018-11-05T11:29:05","indexId":"ofr82275","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":"82-275","title":"Altitude and configuration of the predevelopment water table in the High Plains regional aquifer, northwestern Oklahoma","docAbstract":"<p>The High Plains aquifer in Oklahoma is part of a region~l aquifer<br>system extending from South Dakota on the north through Wyoming, Colorado,<br>Nebraska, Kansas, and Oklahoma to Texas and New Mexico o~ the south.<br>(index map). The principal aquifer, the Ogallala F?rmat1on of :ert1ary<br>age, is hydraulically connected with other unconsolidated ~eposits, .<br>principally of Quaternary age. Alluvium and terrace dep?sits htdrau]ically<br>connected with the Ogallala are included in the High Pla1ns.aqu1fer in<br>Oklahoma. Parts of the underlying bedrock also are hydraul 1cally connected<br>with the Ogallala. The High Plai ns aquifer in Oklahoma has been<br>removed by erosion on the west exposing underlying rocks of Cretaceous<br>age and on the east exposing rocks of Permian age.</p>","language":"English","publisher":"U.S. Geological Survey","doi":"10.3133/ofr82275","usgsCitation":"Havens, J., 1982, Altitude and configuration of the predevelopment water table in the High Plains regional aquifer, northwestern Oklahoma: U.S. Geological Survey Open-File Report 82-275, 2 Sheets: 24.53 x 35.82 inches and 46.58 x 16.85 inches, https://doi.org/10.3133/ofr82275.","productDescription":"2 Sheets: 24.53 x 35.82 inches and 46.58 x 16.85 inches","costCenters":[],"links":[{"id":359167,"rank":2,"type":{"id":17,"text":"Plate"},"url":"https://pubs.usgs.gov/of/1982/0275/plate-2.pdf","linkFileType":{"id":1,"text":"pdf"}},{"id":359168,"rank":3,"type":{"id":17,"text":"Plate"},"url":"https://pubs.usgs.gov/of/1982/0275/plate-1.pdf","linkFileType":{"id":1,"text":"pdf"}},{"id":176699,"rank":0,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/of/1982/0275/report-thumb.jpg"}],"country":"United States","state":"Oklahoma","geographicExtents":"{\"type\":\"FeatureCollection\",\"features\":[{\"type\":\"Feature\",\"geometry\":{\"type\":\"Polygon\",\"coordinates\":[[[-100.9441,36.9988],[-100.6337,36.9986],[-100.1079,36.9983],[-100.0902,36.9983],[-100.0024,36.9985],[-100.0009,36.9985],[-99.5399,36.9998],[-99.4516,37],[-99.4423,36.9923],[-99.4371,36.9874],[-99.4364,36.9783],[-99.43,36.962],[-99.4253,36.9498],[-99.4132,36.9353],[-99.4051,36.929],[-99.397,36.9217],[-99.3947,36.9159],[-99.3935,36.91],[-99.3865,36.9055],[-99.3697,36.8815],[-99.3536,36.8711],[-99.3346,36.8657],[-99.3236,36.8599],[-99.3144,36.8608],[-99.3138,36.8594],[-99.3138,36.8572],[-99.3167,36.8549],[-99.3184,36.8535],[-99.3201,36.8508],[-99.3207,36.8485],[-99.3207,36.8435],[-99.3114,36.8291],[-99.2999,36.815],[-99.2958,36.8096],[-99.2878,36.806],[-99.2797,36.8019],[-99.2751,36.8001],[-99.2687,36.7938],[-99.2578,36.7893],[-99.2394,36.7898],[-99.2314,36.7898],[-99.2193,36.7875],[-99.209,36.7916],[-99.2038,36.7916],[-99.1911,36.7899],[-99.1705,36.7876],[-99.1572,36.7854],[-99.1475,36.7795],[-99.1377,36.7727],[-99.1302,36.7654],[-99.1239,36.7596],[-99.1147,36.7559],[-99.1089,36.7559],[-99.1043,36.7519],[-99.1032,36.7491],[-99.0968,36.7396],[-99.094,36.7328],[-99.0842,36.7242],[-99.0785,36.7201],[-99.0658,36.7161],[-99.0555,36.7047],[-99.0486,36.6984],[-99.0486,36.6893],[-99.0428,36.6775],[-99.0279,36.663],[-99.025,36.654],[-99.0222,36.6454],[-99.0141,36.639],[-99.0032,36.629],[-98.9918,36.6181],[-98.9729,36.6027],[-98.9593,36.5992],[-98.9604,36.507],[-98.9611,36.4779],[-98.9606,36.247],[-98.9562,36.2469],[-98.9565,36.1587],[-99.382,36.1645],[-99.3806,36.0719],[-99.3809,36.017],[-99.3808,35.8991],[-99.374,35.8991],[-99.3736,35.8111],[-99.3763,35.67],[-99.3751,35.5497],[-99.3751,35.5488],[-99.3627,35.5489],[-99.3631,35.508],[-99.5755,35.5085],[-99.576,35.42],[-100.0009,35.4223],[-100.0014,35.4558],[-100.0011,35.6197],[-100.001,35.64],[-100.0015,35.8008],[-100.0015,35.8782],[-100.0015,35.9478],[-100.002,36.0539],[-100.0025,36.1891],[-100.003,36.3134],[-100.0031,36.3348],[-100.0038,36.4998],[-100.1458,36.4998],[-100.3204,36.4999],[-100.5459,36.4994],[-100.7022,36.5],[-100.8939,36.4998],[-100.9524,36.4998],[-101.0908,36.5003],[-101.6255,36.5025],[-101.87,36.5034],[-102.1618,36.5004],[-103.0007,36.5013],[-103.0007,36.5905],[-103.0007,36.6732],[-103.0007,36.7643],[-103.0008,36.9341],[-103.0009,36.999],[-102.7973,36.9988],[-102.7859,36.9988],[-102.7808,36.9986],[-102.7016,36.9958],[-102.6943,36.9957],[-102.6757,36.9956],[-102.5627,36.9962],[-102.5372,36.9963],[-102.5034,36.9963],[-102.4775,36.9963],[-102.4577,36.9961],[-102.3931,36.9955],[-102.351,36.9951],[-102.3247,36.9948],[-102.0423,36.9922],[-102.0417,36.9922],[-102.0281,36.9925],[-101.9881,36.9925],[-101.918,36.9929],[-101.5552,36.9951],[-101.544,36.9952],[-101.2679,36.9967],[-101.0671,36.9978],[-100.9536,36.9988],[-100.9441,36.9988]]]},\"properties\":{\"name\":\"Beaver\",\"state\":\"OK\"}}]}","noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"4f4e4adce4b07f02db686999","contributors":{"authors":[{"text":"Havens, John S.","contributorId":13949,"corporation":false,"usgs":true,"family":"Havens","given":"John S.","affiliations":[],"preferred":false,"id":225943,"contributorType":{"id":1,"text":"Authors"},"rank":1}]}}
,{"id":46897,"text":"ofr82552 - 1982 - Geohydrology of the preglacial Genesee Valley, Monroe County, New York","interactions":[],"lastModifiedDate":"2021-09-07T18:32:27.017525","indexId":"ofr82552","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":"82-552","title":"Geohydrology of the preglacial Genesee Valley, Monroe County, New York","docAbstract":"This report is last in a series of 11 map sets depicting geohydrologic conditions in selected aquifers in upstate New York. Geohydrologic data are compiled on five maps at 1:24,000 scale. Together the maps provide a comprehensive overview of a buried glacio-fluvial aquifer in Monroe County. The maps include surficial geology, geologic sections, bedrock topography, water-infiltration potential of soil zone, potentiometric surface altitude, and land use. The buried-valley deposits consist of ice-contact sand and gravel, till, and glaciolacustrine sand, silt, and clay. The sand and gravel have relatively high permeabilities whereas the till, silt, and clay deposits have relatively low permeabilities. Water-table conditions prevail in unconfined sand and gravel, whereas artesian conditions prevail in the northern part of the system within sand and gravel confined by silty deposits. Recharge occurs principally over the southern part of the aquifer, due to permeable land-surface conditions. Ground-water movement is towards the Irondequoit Bay and Lake Ontario, where discharge occurs. Several communities have wells capable of producing several hundred gallons per minute from the aquifer. The use of land overlying the aquifer is predominantly residential with lesser amounts of industrial uses. (USGS)","language":"English","publisher":"U.S. Geological Survey","doi":"10.3133/ofr82552","usgsCitation":"Waller, R.M., Holecek, T.J., Stelz, W., and Belli, J.L., 1982, Geohydrology of the preglacial Genesee Valley, Monroe County, New York: U.S. Geological Survey Open-File Report 82-552, 5 Plates: 28.49 × 36.65 or smaller, https://doi.org/10.3133/ofr82552.","productDescription":"5 Plates: 28.49 × 36.65 or smaller","costCenters":[],"links":[{"id":172002,"rank":0,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/thumbnails/usgs_thumb.jpg"},{"id":83789,"rank":404,"type":{"id":17,"text":"Plate"},"url":"https://pubs.usgs.gov/of/1982/0552/plate-5.pdf","linkFileType":{"id":1,"text":"pdf"}},{"id":83788,"rank":403,"type":{"id":17,"text":"Plate"},"url":"https://pubs.usgs.gov/of/1982/0552/plate-4.pdf","linkFileType":{"id":1,"text":"pdf"}},{"id":388906,"rank":7,"type":{"id":36,"text":"NGMDB Index Page"},"url":"https://ngmdb.usgs.gov/Prodesc/proddesc_45788.htm"},{"id":83787,"rank":402,"type":{"id":17,"text":"Plate"},"url":"https://pubs.usgs.gov/of/1982/0552/plate-3.pdf","linkFileType":{"id":1,"text":"pdf"}},{"id":83786,"rank":401,"type":{"id":17,"text":"Plate"},"url":"https://pubs.usgs.gov/of/1982/0552/plate-2.pdf","linkFileType":{"id":1,"text":"pdf"}},{"id":83785,"rank":400,"type":{"id":17,"text":"Plate"},"url":"https://pubs.usgs.gov/of/1982/0552/plate-1.pdf","linkFileType":{"id":1,"text":"pdf"}}],"country":"United States","state":"New York","county":"Monroe County","otherGeospatial":"East Rochester-Irondequoit Bay Area","geographicExtents":"{\n  \"type\": \"FeatureCollection\",\n  \"features\": [\n    {\n      \"type\": \"Feature\",\n      \"properties\": {},\n      \"geometry\": {\n        \"type\": \"Polygon\",\n        \"coordinates\": [\n          [\n            [\n              -77.4580,\n              43.2500\n            ],\n            [\n              -77.5500,\n              43.2500\n            ],\n            [\n              -77.5500,\n              43.0830\n            ],\n            [\n              -77.4580,\n              43.0830\n            ],\n            [\n              -77.4580,\n              43.2500\n            ]\n          ]\n        ]\n      }\n    }\n  ]\n}","noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"4f4e4b1ae4b07f02db6a884b","contributors":{"authors":[{"text":"Waller, Roger Milton","contributorId":22320,"corporation":false,"usgs":true,"family":"Waller","given":"Roger","email":"","middleInitial":"Milton","affiliations":[],"preferred":false,"id":234276,"contributorType":{"id":1,"text":"Authors"},"rank":1},{"text":"Holecek, T. J.","contributorId":51362,"corporation":false,"usgs":true,"family":"Holecek","given":"T.","email":"","middleInitial":"J.","affiliations":[],"preferred":false,"id":234278,"contributorType":{"id":1,"text":"Authors"},"rank":2},{"text":"Stelz, W. B.","contributorId":43811,"corporation":false,"usgs":true,"family":"Stelz","given":"W.","middleInitial":"B.","affiliations":[],"preferred":false,"id":234277,"contributorType":{"id":1,"text":"Authors"},"rank":3},{"text":"Belli, J. L.","contributorId":83561,"corporation":false,"usgs":true,"family":"Belli","given":"J.","email":"","middleInitial":"L.","affiliations":[],"preferred":false,"id":234279,"contributorType":{"id":1,"text":"Authors"},"rank":4}]}}
,{"id":29895,"text":"wri8211 - 1982 - Nitrate-nitrogen concentrations in ground water from three selected areas in Kansas","interactions":[],"lastModifiedDate":"2017-10-03T10:11:08","indexId":"wri8211","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":"82-11","title":"Nitrate-nitrogen concentrations in ground water from three selected areas in Kansas","docAbstract":"<p>Nitrate-nitrogen data collected during 1976-79 from 333 wells in western, central, and eastern Kansas were summarized and statistically analyzed on the basis of area, aquifer, and well depth. Concentrations exceeding 10 milligrams per liter occurred generally in wells less than 100 feet in depth, indicating that nitrate-nitrogen concentrations in ground water greater than 10 milligrams per liter commonly are derived from nitrogen sources at or near the land surface, although soluble nitrogen may be derived from fine-grained sediments in some aquifers.</p><p>Water from shales in central and eastern Kansas and from limestone in eastern Kansas exhibited the highest median concentrations and highest incidence of concentrations above 10 milligrams per liter. Water from 10 percent of the wells in unconsolidated Quaternary deposits in western Kansas and almost 30 percent of the wells in eastern Kansas had nitrate-nitrogen concentrations that exceeded 10 milligrams per liter. Shallow wells in shales, limestones, and unconsolidated Quaternary deposits are highly susceptible to nitrate contamination. Water from unconsolidated Tertiary deposits produced a low incidence of nitrate-nitrogen concentrations greater than 10 milligrams per liter, indicating minimal nitrate contamination from sources at or near the land surface. Sandstones in all areas exhibited the lowest median and lowest incidence of nitratenitrogen concentrations above 10 milligrams per liter.</p>","language":"English","publisher":"U.S. Geological Survey","doi":"10.3133/wri8211","usgsCitation":"Spruill, T.B., 1982, Nitrate-nitrogen concentrations in ground water from three selected areas in Kansas: U.S. Geological Survey Water-Resources Investigations Report 82-11, 32 p., https://doi.org/10.3133/wri8211.","productDescription":"32 p.","numberOfPages":"35","costCenters":[{"id":353,"text":"Kansas Water Science Center","active":false,"usgs":true}],"links":[{"id":159472,"rank":0,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/wri/1982/0011/report-thumb.jpg"},{"id":346292,"rank":2,"type":{"id":11,"text":"Document"},"url":"https://pubs.usgs.gov/wri/1982/0011/report.pdf","linkFileType":{"id":1,"text":"pdf"}}],"country":"United 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,{"id":59050,"text":"mf1475D - 1982 - Mineral resource potential map of the Vermilion Cliffs-Paria Canyon instant study area, Coconino County, Arizona, and Kane County, Utah","interactions":[],"lastModifiedDate":"2015-10-20T13:09:32","indexId":"mf1475D","displayToPublicDate":"1994-01-01T00:00:00","publicationYear":"1982","noYear":false,"publicationType":{"id":18,"text":"Report"},"publicationSubtype":{"id":5,"text":"USGS Numbered Series"},"seriesTitle":{"id":325,"text":"Miscellaneous Field Studies Map","code":"MF","active":false,"publicationSubtype":{"id":5}},"seriesNumber":"1475","chapter":"D","title":"Mineral resource potential map of the Vermilion Cliffs-Paria Canyon instant study area, Coconino County, Arizona, and Kane County, Utah","docAbstract":"<p>In general, the mineral potential of the study area is low; in the past the area has yielded only several hundred tons of uranium ore, and there have been a number of unsuccessful efforts to produce gold.</p>\n<p>The generally small uraniferous deposits are in the Chinle Formation, mostly in the basal Shinarump Member, and mostly on the east side of the Paria Plateau. To the south and west, around the plateau, the Shinarump host rock pinches out or is present in only a few places, and the same relationships are likely below the plateau, where the host rocks are deeply buried, from 1,500 to 3,000 ft below the surface. These factors suggest the total uranium-copper-vanadium-silver potential to be very low.</p>\n<p>Gold and mercury occur in very low concentrations in the clayey units of the Petrified Forest Member of the Chinle. Gold concentrations are 40 ppb and less, and the gold is present in very fine particles; recovery is very difficult. Overall, the mercury concentrations are so low that no realistic mineral resource potential can be estimated.</p>\n<p>Nonmetallic mineral materials of possible value include limestone, flagstone, clay, and gravel, but they are of only local interest. No oil or gas resources are known in the study area. Coal resources within the area are nonexistent, but the Dakota Sandstone does contain coaly beds a few miles to the north.</p>\n<p>Water is perhaps the most significant resource needed in the study area. A number of perennial springs support the few local ranchers and tourist facilities. Some ground water would be available below the plateau, but drilling depths would be more than 2,000 ft (600-700 m).</p>","language":"English","publisher":"U.S. Geological Survey","doi":"10.3133/mf1475D","usgsCitation":"Bush, A., and Lane, M., 1982, Mineral resource potential map of the Vermilion Cliffs-Paria Canyon instant study area, Coconino County, Arizona, and Kane County, Utah: U.S. Geological Survey Miscellaneous Field Studies Map 1475, Report: 11 p.; Plate: 46.25 x 38.48 inches, https://doi.org/10.3133/mf1475D.","productDescription":"Report: 11 p.; Plate: 46.25 x 38.48 inches","onlineOnly":"N","additionalOnlineFiles":"N","costCenters":[],"links":[{"id":183527,"rank":0,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/thumbnails/mf1475D.jpg"},{"id":310159,"rank":1,"type":{"id":11,"text":"Document"},"url":"https://pubs.usgs.gov/mf/1475-D/report.pdf","text":"Report","linkFileType":{"id":1,"text":"pdf"}},{"id":310160,"rank":2,"type":{"id":17,"text":"Plate"},"url":"https://pubs.usgs.gov/mf/1475-D/plate-1.pdf","text":"Plate","linkFileType":{"id":1,"text":"pdf"}}],"country":"United States","state":"Arizona","county":"Coconino County, Kane County","geographicExtents":"{ \"type\": \"FeatureCollection\", \"features\": [ { \"type\": \"Feature\", \"properties\": {}, \"geometry\": { \"type\": \"Polygon\", \"coordinates\": [ [ [ -112.25,36.75 ], [ -112.25,37 ], [ -111.75,37 ], [ -111.75,36.75 ], [ -112.25,36.75 ] ] ] } } ] }","noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"4f4e4a61e4b07f02db6357d1","contributors":{"authors":[{"text":"Bush, Alfred L.","contributorId":48977,"corporation":false,"usgs":true,"family":"Bush","given":"Alfred L.","affiliations":[],"preferred":false,"id":261327,"contributorType":{"id":1,"text":"Authors"},"rank":1},{"text":"Lane, Michael","contributorId":39756,"corporation":false,"usgs":true,"family":"Lane","given":"Michael","affiliations":[],"preferred":false,"id":261326,"contributorType":{"id":1,"text":"Authors"},"rank":2}]}}
,{"id":4156,"text":"cir855 - 1982 - The Alaska Mineral Resource Assessment Program: Guide to information about the geology and mineral resources of the Ketchikan and Prince Rupert quadrangles, southeastern Alaska","interactions":[],"lastModifiedDate":"2021-11-18T20:54:59.200928","indexId":"cir855","displayToPublicDate":"1994-01-01T00:00:00","publicationYear":"1982","noYear":false,"publicationType":{"id":18,"text":"Report"},"publicationSubtype":{"id":5,"text":"USGS Numbered Series"},"seriesTitle":{"id":307,"text":"Circular","code":"CIR","onlineIssn":"2330-5703","printIssn":"1067-084X","active":true,"publicationSubtype":{"id":5}},"seriesNumber":"855","title":"The Alaska Mineral Resource Assessment Program: Guide to information about the geology and mineral resources of the Ketchikan and Prince Rupert quadrangles, southeastern Alaska","docAbstract":"The Ketchikan and Prince Rupert 1-degree by 2-degree quadrangles, which encompass about 16,000 km2 at the south tip of southeastern Alaska, have been investigated by integrated field and laboratory studies in the disciplines of geology, geochemistry, geophysics, and Landsat data interpretation to determine their mineral-resource potential. Mineral deposits in the study area have been mined or prospected intermittently since about 1900, and production of small tonnages of ores containing gold, silver, copper, lead, zinc, and tungsten has been recorded. Extensive exploration and development currently (1981) is underway at a molybdenum prospect about 65 km east of Ketchikan. Our mineral-resource assessment indicates that the area contains potentially significant amounts of those metallic commodities, as well as of molybdenum, iron, antimony, and barite. The results of these studies have been published in a folio of maps accompanied by descriptive texts, diagrams, tables, and pertinent references. The present report serves as a guide to these investigations, provides relevant background information, and integrates the component maps and reports. It also describes revisions to the geology based on studies completed since the folio was published and includes a list of specific and general references on the geology and mineral deposits of the study area.","language":"English","publisher":"U.S. Geological Survey","doi":"10.3133/cir855","usgsCitation":"Berg, H., 1982, The Alaska Mineral Resource Assessment Program: Guide to information about the geology and mineral resources of the Ketchikan and Prince Rupert quadrangles, southeastern Alaska: U.S. Geological Survey Circular 855, iii, 24 p., https://doi.org/10.3133/cir855.","productDescription":"iii, 24 p.","costCenters":[],"links":[{"id":391884,"rank":3,"type":{"id":36,"text":"NGMDB Index Page"},"url":"https://ngmdb.usgs.gov/Prodesc/proddesc_23951.htm"},{"id":139234,"rank":0,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/circ/1982/0855/report-thumb.jpg"},{"id":31265,"rank":300,"type":{"id":11,"text":"Document"},"url":"https://pubs.usgs.gov/circ/1982/0855/report.pdf","linkFileType":{"id":1,"text":"pdf"}}],"country":"United States","state":"Alaska","otherGeospatial":"Ketchikan and Prince Rupert quadrangles","geographicExtents":"{\n  \"type\": \"FeatureCollection\",\n  \"features\": [\n    {\n      \"type\": \"Feature\",\n      \"properties\": {},\n      \"geometry\": {\n        \"type\": \"Polygon\",\n        \"coordinates\": [\n          [\n            [\n              -132,\n              54.717\n            ],\n            [\n              -130,\n              54.717\n            ],\n            [\n              -130,\n              56\n            ],\n            [\n              -132,\n              56\n            ],\n            [\n              -132,\n              54.717\n            ]\n          ]\n        ]\n      }\n    }\n  ]\n}","noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"4f4e4ad5e4b07f02db6835c1","contributors":{"authors":[{"text":"Berg, Henry C.","contributorId":73176,"corporation":false,"usgs":true,"family":"Berg","given":"Henry C.","affiliations":[],"preferred":false,"id":148308,"contributorType":{"id":1,"text":"Authors"},"rank":1}]}}
,{"id":7457,"text":"ofr821033 - 1982 - Probabilistic estimates of maximum acceleration and velocity in rock in the contiguous United States","interactions":[],"lastModifiedDate":"2012-02-02T00:06:13","indexId":"ofr821033","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":"82-1033","title":"Probabilistic estimates of maximum acceleration and velocity in rock in the contiguous United States","docAbstract":"Maximum horizontal accelerations and velocities caused by earthquakes are mapped for exposure times of 10, 50 and 250 years at the 90-percent probability level of nonexceedance for the contiguous United States. In many areas these new maps differ significantly from the 1976 probabilistic acceleration map by Algermlssen and Perkins because of the increase in detail, resulting from greater emphasis on the geologic basis for seismic source zones. This new emphasis is possible because of extensive data recently acquired on Holocene and Quaternary faulting in the western United States and new interpretations of geologic structures controlling the seismicity pattern in the central and eastern United States. ","language":"ENGLISH","publisher":"U.S. Geological Survey,","doi":"10.3133/ofr821033","usgsCitation":"Algermissen, S.T., Perkins, D.M., Thenhaus, P., Hanson, S., and Bender, B., 1982, Probabilistic estimates of maximum acceleration and velocity in rock in the contiguous United States: U.S. Geological Survey Open-File Report 82-1033, 107 p., ill., maps ;28 cm., https://doi.org/10.3133/ofr821033.","productDescription":"107 p., ill., maps ;28 cm.","costCenters":[],"links":[{"id":142072,"rank":0,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/of/1982/1033/report-thumb.jpg"},{"id":34868,"rank":400,"type":{"id":17,"text":"Plate"},"url":"https://pubs.usgs.gov/of/1982/1033/plate-1.pdf","linkFileType":{"id":1,"text":"pdf"}},{"id":34869,"rank":401,"type":{"id":17,"text":"Plate"},"url":"https://pubs.usgs.gov/of/1982/1033/plate-2.pdf","linkFileType":{"id":1,"text":"pdf"}},{"id":34870,"rank":402,"type":{"id":17,"text":"Plate"},"url":"https://pubs.usgs.gov/of/1982/1033/plate-3.pdf","linkFileType":{"id":1,"text":"pdf"}},{"id":34871,"rank":403,"type":{"id":17,"text":"Plate"},"url":"https://pubs.usgs.gov/of/1982/1033/plate-4.pdf","linkFileType":{"id":1,"text":"pdf"}},{"id":34872,"rank":404,"type":{"id":17,"text":"Plate"},"url":"https://pubs.usgs.gov/of/1982/1033/plate-5.pdf","linkFileType":{"id":1,"text":"pdf"}},{"id":34873,"rank":405,"type":{"id":17,"text":"Plate"},"url":"https://pubs.usgs.gov/of/1982/1033/plate-6.pdf","linkFileType":{"id":1,"text":"pdf"}},{"id":34874,"rank":300,"type":{"id":11,"text":"Document"},"url":"https://pubs.usgs.gov/of/1982/1033/report.pdf","linkFileType":{"id":1,"text":"pdf"}}],"noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"4f4e4a9fe4b07f02db660d58","contributors":{"authors":[{"text":"Algermissen, Sylvester Theodore","contributorId":94300,"corporation":false,"usgs":true,"family":"Algermissen","given":"Sylvester","email":"","middleInitial":"Theodore","affiliations":[],"preferred":false,"id":155704,"contributorType":{"id":1,"text":"Authors"},"rank":1},{"text":"Perkins, D. M.","contributorId":83922,"corporation":false,"usgs":true,"family":"Perkins","given":"D.","email":"","middleInitial":"M.","affiliations":[],"preferred":false,"id":155703,"contributorType":{"id":1,"text":"Authors"},"rank":2},{"text":"Thenhaus, P.C.","contributorId":46089,"corporation":false,"usgs":true,"family":"Thenhaus","given":"P.C.","affiliations":[],"preferred":false,"id":155701,"contributorType":{"id":1,"text":"Authors"},"rank":3},{"text":"Hanson, S.L.","contributorId":47361,"corporation":false,"usgs":true,"family":"Hanson","given":"S.L.","email":"","affiliations":[],"preferred":false,"id":155702,"contributorType":{"id":1,"text":"Authors"},"rank":4},{"text":"Bender, B.L.","contributorId":99976,"corporation":false,"usgs":true,"family":"Bender","given":"B.L.","email":"","affiliations":[],"preferred":false,"id":155705,"contributorType":{"id":1,"text":"Authors"},"rank":5}]}}
,{"id":47320,"text":"ofr81496 - 1982 - Geologic map of the Redwood Creek drainage basin, Humboldt County, California","interactions":[],"lastModifiedDate":"2022-01-07T21:12:18.954209","indexId":"ofr81496","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":"81-496","title":"Geologic map of the Redwood Creek drainage basin, Humboldt County, California","docAbstract":"A 1:62,500-scale geologic map with 14 rock stratigraphic units and an accompanying explanatory text are used to describe the geology of the Redwood Creek drainage basin of northwestern California. A large part of Redwood National Park is located in the downstream part of this actively eroding drainage basin. The bedrock consists primarily of Mesozoic sedimentary and metamorphic rocks. The structurally complex Franciscan assemblage of rocks underlies most of the basin, but rocks of the Klammath Mountain tectonic province occurs in a small eastern part of the basin. Most major boundaries between Mesozoic rock units are north-northwest trending faults parallel to the regional structural trend. Extensive areas of surficial coastal plain sediments, landslide deposits, stream terrace deposits and modern alluvium are also present; these areas help identify loci of vigorous recent erosion. (USGS)","language":"English","publisher":"U.S. Geological Survey","doi":"10.3133/ofr81496","usgsCitation":"Harden, D.R., Kelsey, H., Morrison, S., and Stephens, T., 1982, Geologic map of the Redwood Creek drainage basin, Humboldt County, California: U.S. Geological Survey Open-File Report 81-496, 1 Plate: 32.46 x 56.62 inches, https://doi.org/10.3133/ofr81496.","productDescription":"1 Plate: 32.46 x 56.62 inches","costCenters":[],"links":[{"id":394062,"rank":2,"type":{"id":17,"text":"Plate"},"url":"https://pubs.usgs.gov/of/1981/0496/plate-1.pdf","linkFileType":{"id":1,"text":"pdf"}},{"id":172519,"rank":0,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/of/1981/0496/report-thumb.jpg"}],"scale":"62500","country":"United States","state":"California","county":"Humboldt County","otherGeospatial":"Redwood Creek drainage basin","geographicExtents":"{\n  \"type\": \"FeatureCollection\",\n  \"features\": [\n    {\n      \"type\": \"Feature\",\n      \"properties\": {},\n      \"geometry\": {\n        \"type\": \"Polygon\",\n        \"coordinates\": [\n          [\n            [\n              -124.1667,\n              40.66667\n            ],\n            [\n              -123.6667,\n              40.66667\n            ],\n            [\n              -123.6667,\n              41.41667\n            ],\n            [\n              -124.1667,\n              41.41667\n            ],\n            [\n              -124.1667,\n              40.66667\n            ]\n          ]\n        ]\n      }\n    }\n  ]\n}","noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"4f4e4ae4e4b07f02db689c3c","contributors":{"authors":[{"text":"Harden, Deborah Reid","contributorId":10042,"corporation":false,"usgs":true,"family":"Harden","given":"Deborah","email":"","middleInitial":"Reid","affiliations":[],"preferred":false,"id":235050,"contributorType":{"id":1,"text":"Authors"},"rank":1},{"text":"Kelsey, H.M.","contributorId":84300,"corporation":false,"usgs":true,"family":"Kelsey","given":"H.M.","email":"","affiliations":[],"preferred":false,"id":235053,"contributorType":{"id":1,"text":"Authors"},"rank":2},{"text":"Morrison, S.D.","contributorId":49849,"corporation":false,"usgs":true,"family":"Morrison","given":"S.D.","email":"","affiliations":[],"preferred":false,"id":235052,"contributorType":{"id":1,"text":"Authors"},"rank":3},{"text":"Stephens, T.A.","contributorId":48239,"corporation":false,"usgs":true,"family":"Stephens","given":"T.A.","email":"","affiliations":[],"preferred":false,"id":235051,"contributorType":{"id":1,"text":"Authors"},"rank":4}]}}
,{"id":47274,"text":"ofr82336 - 1982 - Generalized configuration of the top of the limestone unit of the lower part of the surficial aquifer, Duval County, Florida","interactions":[],"lastModifiedDate":"2022-04-28T20:19:14.74335","indexId":"ofr82336","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":"82-336","title":"Generalized configuration of the top of the limestone unit of the lower part of the surficial aquifer, Duval County, Florida","docAbstract":"<p>The top of the limestone unit ranges from about 25 feet above sea level in western Duval County to about 75 feet below sea level locally in the eastern part of the county. The limestone, which is part of the surficial aquifer, is the principal source of water to shallow wells in the county. The unit generally consists of a soft, friable, cavernous, sandy limestone, which ranges from about 5 to 40 feet in thickness. Along the coast and in the southern part of the county, the limestone becomes discontinuous.&nbsp;</p>","language":"English","publisher":"U.S. Geological Survey","doi":"10.3133/ofr82336","collaboration":"Prepared in cooperation with the City of Jacksonville","usgsCitation":"Spechler, R.M., 1982, Generalized configuration of the top of the limestone unit of the lower part of the surficial aquifer, Duval County, Florida: U.S. Geological Survey Open-File Report 82-336, 1 Plate: 34.92 x 28.86 inches, https://doi.org/10.3133/ofr82336.","productDescription":"1 Plate: 34.92 x 28.86 inches","costCenters":[],"links":[{"id":399852,"rank":2,"type":{"id":17,"text":"Plate"},"url":"https://pubs.usgs.gov/of/1982/0336/plate-1.pdf","linkFileType":{"id":1,"text":"pdf"}},{"id":171064,"rank":0,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/of/1982/0336/report-thumb.jpg"}],"country":"United States","state":"Florida","county":"Duval 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,{"id":59546,"text":"mf1415B - 1982 - Geochemical survey of the Cohutta Wilderness and the Hemp Top Roadless Area, northern Georgia and southeastern Tennessee","interactions":[],"lastModifiedDate":"2018-09-14T12:52:09","indexId":"mf1415B","displayToPublicDate":"1994-01-01T00:00:00","publicationYear":"1982","noYear":false,"publicationType":{"id":18,"text":"Report"},"publicationSubtype":{"id":5,"text":"USGS Numbered Series"},"seriesTitle":{"id":325,"text":"Miscellaneous Field Studies Map","code":"MF","active":false,"publicationSubtype":{"id":5}},"seriesNumber":"1415","chapter":"B","title":"Geochemical survey of the Cohutta Wilderness and the Hemp Top Roadless Area, northern Georgia and southeastern Tennessee","docAbstract":"<p>The contiguous Cohutta Wilderness and Hemp Top Roadless Area are in the western part of the Blue Ridge physiographic province of northern Georgia and southeastern Tennessee (fig. 1).&nbsp; All of the study area is in Georgia except an irregular strip of land about 1 mi at its widest on the northern end of the Cohutta Wilderness in Tennessee.&nbsp; The area of the Cohutta Wilderness is 34,650 acres; that of the Hemp Top Roadless Area is 2,800 acres.&nbsp; The areas are in rugged mountainous terrain- a strongly dissected upland ranging in altitude from about 980 to 4,200 ft above sea level.&nbsp; Local altitude differences of 1,450-2,000 ft and slopes steeper than 25° are common.&nbsp; The north end of the Cohutta Wilderness is about 6 mi south of the Ocoee River gorge, 10 mi west-southwest of the major copper-and sulfur-mining district at Ducktown, Tenn., and approximately 22 mi southeast of Cleveland, Tenn., in Bradley County, west of the area shown in figure 1.&nbsp; The eastern, central, and northwestern parts of the wilderness are drained by Jacks River and it tributaries; the southwestern part, by the Conasauga River and its tributaries; and the Hemp Top Roadless Area, by Tumbling Creek and some of its western tributaries.&nbsp; All drainage ultimately goes to the Ocoee River and from these into the Hiwassee River.</p>","language":"English","publisher":"U.S. Geological Survey","doi":"10.3133/mf1415B","usgsCitation":"Gair, J.E., 1982, Geochemical survey of the Cohutta Wilderness and the Hemp Top Roadless Area, northern Georgia and southeastern Tennessee: U.S. Geological Survey Miscellaneous Field Studies Map 1415, 2 Plates: 52.33 x 39.84 inches and 48.70 x 31.49 inches, https://doi.org/10.3133/mf1415B.","productDescription":"2 Plates: 52.33 x 39.84 inches and 48.70 x 31.49 inches","costCenters":[],"links":[{"id":183161,"rank":0,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/mf/1415-B/report-thumb.jpg"},{"id":357341,"rank":2,"type":{"id":17,"text":"Plate"},"url":"https://pubs.usgs.gov/mf/1415-B/plate-1.pdf","linkFileType":{"id":1,"text":"pdf"}},{"id":357342,"rank":3,"type":{"id":17,"text":"Plate"},"url":"https://pubs.usgs.gov/mf/1415-B/plate-2.pdf","linkFileType":{"id":1,"text":"pdf"}}],"scale":"0","country":"United States","state":"Georgia, Tennessee","otherGeospatial":"Cohutta Wilderness, Hemp Top Roadless Area","geographicExtents":"{ \"type\": \"FeatureCollection\", \"features\": [ { \"type\": \"Feature\", \"properties\": {}, \"geometry\": { \"type\": \"Polygon\", \"coordinates\": [ [ [ -84.66666666666667,34.833333333333336 ], [ -84.66666666666667,35.016666666666666 ], [ -84.45083333333334,35.016666666666666 ], [ -84.45083333333334,34.833333333333336 ], [ -84.66666666666667,34.833333333333336 ] ] ] } } ] }","noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"4f4e4b20e4b07f02db6aba72","contributors":{"authors":[{"text":"Gair, Jacob E.","contributorId":18381,"corporation":false,"usgs":true,"family":"Gair","given":"Jacob","email":"","middleInitial":"E.","affiliations":[],"preferred":false,"id":262200,"contributorType":{"id":1,"text":"Authors"},"rank":1}]}}
,{"id":58624,"text":"mf1458C - 1982 - Mineral resource potential map of the Muddy Mountains Wilderness Study Area, Clark County, Nevada","interactions":[],"lastModifiedDate":"2015-10-20T11:21:30","indexId":"mf1458C","displayToPublicDate":"1994-01-01T00:00:00","publicationYear":"1982","noYear":false,"publicationType":{"id":18,"text":"Report"},"publicationSubtype":{"id":5,"text":"USGS Numbered Series"},"seriesTitle":{"id":325,"text":"Miscellaneous Field Studies Map","code":"MF","active":false,"publicationSubtype":{"id":5}},"seriesNumber":"1458","chapter":"C","title":"Mineral resource potential map of the Muddy Mountains Wilderness Study Area, Clark County, Nevada","docAbstract":"<p>The Muddy Mountains Wilderness Study Area (WSA 050-0229), Clark County, Nevada, has a high potential for mineral deposits of calcium borates and lithium. The known and potential mineral deposits are concentrated in the east-central and south-central parts of the study area (see map). Zeolites (in particular clinoptilolite) are present in some tuff beds throughout much of the study area, and this resource potential is probably moderate to high. Stream-sediment sampling suggests that the Muddy Mountains area has little potential for mineral deposits of metals (other than lithium). Clay minerals are mined at one locality in the (!rea (see map). Building stone and silica sand have moderate to low potential in some places. Oil and gas potential within the study area is low, but complete evaluation of its potential is not possible without drilling.</p>","language":"English","publisher":"U.S. Geological Survey","doi":"10.3133/mf1458C","usgsCitation":"Bohannon, R.G., Leszcykowski, A.M., Esparza, L.E., and Rumsey, C.M., 1982, Mineral resource potential map of the Muddy Mountains Wilderness Study Area, Clark County, Nevada: U.S. Geological Survey Miscellaneous Field Studies Map 1458, Report: 11 p.; Plate: 43.58 x 21.94 inches, https://doi.org/10.3133/mf1458C.","productDescription":"Report: 11 p.; Plate: 43.58 x 21.94 inches","onlineOnly":"N","additionalOnlineFiles":"N","costCenters":[],"links":[{"id":184761,"rank":0,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/thumbnails/mf1458C.jpg"},{"id":310132,"rank":1,"type":{"id":11,"text":"Document"},"url":"https://pubs.usgs.gov/mf/1458-C/report.pdf","text":"Report","linkFileType":{"id":1,"text":"pdf"}},{"id":310133,"rank":2,"type":{"id":17,"text":"Plate"},"url":"https://pubs.usgs.gov/mf/1458-C/plate-1.pdf","text":"Plate","linkFileType":{"id":1,"text":"pdf"}}],"country":"United States","state":"Nevada","county":"Clark County","otherGeospatial":"Muddy Mountains Wilderness Study Area","geographicExtents":"{ \"type\": \"FeatureCollection\", \"features\": [ { \"type\": \"Feature\", \"properties\": {}, \"geometry\": { \"type\": \"Polygon\", \"coordinates\": [ [ [ -114.83333333333333,36.25 ], [ -114.83333333333333,36.333333333333336 ], [ -114.58333333333333,36.333333333333336 ], [ -114.58333333333333,36.25 ], [ -114.83333333333333,36.25 ] ] ] } } ] }","noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"4f4e4b23e4b07f02db6adec6","contributors":{"authors":[{"text":"Bohannon, Robert G. rbohannon@usgs.gov","contributorId":2255,"corporation":false,"usgs":true,"family":"Bohannon","given":"Robert","email":"rbohannon@usgs.gov","middleInitial":"G.","affiliations":[],"preferred":true,"id":260120,"contributorType":{"id":1,"text":"Authors"},"rank":1},{"text":"Leszcykowski, Andrew M.","contributorId":78387,"corporation":false,"usgs":true,"family":"Leszcykowski","given":"Andrew","email":"","middleInitial":"M.","affiliations":[],"preferred":false,"id":260122,"contributorType":{"id":1,"text":"Authors"},"rank":2},{"text":"Esparza, Leon E.","contributorId":70112,"corporation":false,"usgs":true,"family":"Esparza","given":"Leon","email":"","middleInitial":"E.","affiliations":[],"preferred":false,"id":260121,"contributorType":{"id":1,"text":"Authors"},"rank":3},{"text":"Rumsey, Clayton M.","contributorId":50514,"corporation":false,"usgs":true,"family":"Rumsey","given":"Clayton","email":"","middleInitial":"M.","affiliations":[],"preferred":false,"id":260119,"contributorType":{"id":1,"text":"Authors"},"rank":4}]}}
,{"id":40150,"text":"ofr821022 - 1982 - Configuration of the water table, March 1980, in the Snake River plain regional aquifer system, Idaho and eastern Oregon","interactions":[],"lastModifiedDate":"2022-09-26T19:51:05.522249","indexId":"ofr821022","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":"82-1022","title":"Configuration of the water table, March 1980, in the Snake River plain regional aquifer system, Idaho and eastern Oregon","docAbstract":"<p>No abstract available.</p>","language":"English","publisher":"U.S. Geological Survey","doi":"10.3133/ofr821022","usgsCitation":"Lindholm, G.F., Garabedian, S., Newton, G.D., and Whitehead, R., 1982, Configuration of the water table, March 1980, in the Snake River plain regional aquifer system, Idaho and eastern Oregon: U.S. Geological Survey Open-File Report 82-1022, 1 Plate: 38.61 × 23.12 inches, https://doi.org/10.3133/ofr821022.","productDescription":"1 Plate: 38.61 × 23.12 inches","costCenters":[],"links":[{"id":176698,"rank":0,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/thumbnails/usgs_thumb.jpg"},{"id":407347,"rank":2,"type":{"id":36,"text":"NGMDB Index Page"},"url":"https://ngmdb.usgs.gov/Prodesc/proddesc_13621.htm","linkFileType":{"id":5,"text":"html"}},{"id":69766,"rank":400,"type":{"id":17,"text":"Plate"},"url":"https://pubs.usgs.gov/of/1982/1022/plate-1.pdf","linkFileType":{"id":1,"text":"pdf"}}],"country":"United States","state":"Idaho, Oregon","otherGeospatial":"Snake River plain regional aquifer system","geographicExtents":"{\n  \"type\": \"FeatureCollection\",\n  \"features\": [\n    {\n      \"type\": \"Feature\",\n      \"properties\": {},\n      \"geometry\": {\n        \"type\": \"Polygon\",\n        \"coordinates\": [\n          [\n            [\n              -117.175,\n              42.3\n            ],\n            [\n              -111.54,\n              42.3\n            ],\n            [\n              -111.54,\n              44.427\n            ],\n            [\n              -117.175,\n              44.427\n            ],\n            [\n              -117.175,\n              42.3\n            ]\n          ]\n        ]\n      }\n    }\n  ]\n}","noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"4f4e4b13e4b07f02db6a3276","contributors":{"authors":[{"text":"Lindholm, G. F.","contributorId":88763,"corporation":false,"usgs":true,"family":"Lindholm","given":"G.","email":"","middleInitial":"F.","affiliations":[],"preferred":false,"id":223048,"contributorType":{"id":1,"text":"Authors"},"rank":1},{"text":"Garabedian, S. P.","contributorId":56657,"corporation":false,"usgs":true,"family":"Garabedian","given":"S. P.","affiliations":[],"preferred":false,"id":223047,"contributorType":{"id":1,"text":"Authors"},"rank":2},{"text":"Newton, G. D.","contributorId":43374,"corporation":false,"usgs":true,"family":"Newton","given":"G.","email":"","middleInitial":"D.","affiliations":[],"preferred":false,"id":223046,"contributorType":{"id":1,"text":"Authors"},"rank":3},{"text":"Whitehead, R.L.","contributorId":34891,"corporation":false,"usgs":true,"family":"Whitehead","given":"R.L.","email":"","affiliations":[],"preferred":false,"id":223045,"contributorType":{"id":1,"text":"Authors"},"rank":4}]}}
,{"id":36629,"text":"fwsobs80_67 - 1982 - A guide for enhancement of fish and wildlife on abandoned mine lands in the eastern United States","interactions":[],"lastModifiedDate":"2012-02-02T00:10:01","indexId":"fwsobs80_67","displayToPublicDate":"1994-01-01T00:00:00","publicationYear":"1982","noYear":false,"publicationType":{"id":18,"text":"Report"},"publicationSubtype":{"id":1,"text":"Federal Government Series"},"seriesTitle":{"id":20,"text":"FWS/OBS","active":false,"publicationSubtype":{"id":1}},"seriesNumber":"80/67","title":"A guide for enhancement of fish and wildlife on abandoned mine lands in the eastern United States","language":"ENGLISH","publisher":"U.S. Fish and Wildlife Service","usgsCitation":"Nawrot, J.R., Woolf, A., and Klimstra, W., 1982, A guide for enhancement of fish and wildlife on abandoned mine lands in the eastern United States: FWS/OBS 80/67, x, 101 p. : ill., 1 map; 28 cm.","productDescription":"x, 101 p. : ill., 1 map; 28 cm.","costCenters":[],"links":[{"id":162174,"rank":0,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/thumbnails/outside_thumb.jpg"}],"noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"4f4e4b24e4b07f02db6ae5d5","contributors":{"authors":[{"text":"Nawrot, Jack R.","contributorId":60283,"corporation":false,"usgs":true,"family":"Nawrot","given":"Jack","email":"","middleInitial":"R.","affiliations":[],"preferred":false,"id":216690,"contributorType":{"id":1,"text":"Authors"},"rank":1},{"text":"Woolf, A.","contributorId":18421,"corporation":false,"usgs":true,"family":"Woolf","given":"A.","affiliations":[],"preferred":false,"id":216688,"contributorType":{"id":1,"text":"Authors"},"rank":2},{"text":"Klimstra, W.D.","contributorId":59084,"corporation":false,"usgs":true,"family":"Klimstra","given":"W.D.","email":"","affiliations":[],"preferred":false,"id":216689,"contributorType":{"id":1,"text":"Authors"},"rank":3}]}}
,{"id":9953,"text":"ofr82751 - 1982 - Yearly variations in runoff and frequency of dry years for the conterminous United States, 1911-79","interactions":[],"lastModifiedDate":"2016-05-09T09:03:40","indexId":"ofr82751","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":"82-751","title":"Yearly variations in runoff and frequency of dry years for the conterminous United States, 1911-79","docAbstract":"<p>Gaging-station data are presented on variations in annual runoff over the conterminous United States and nearby Canada during the period 1911-79 in tabular and graphic (map) form. These data bring up-to-date and extend backward in time previous reports on streamflow stations by Harbeck and Langbein in 1949 which covered the period 1921-45 and that by Busby in 1963 which covered the period 1931-60. As depicted in Langbein and Slack (1980), these data show that, contained within a rather large seemingly random or sporadic pattern, there appears to be a previously unnoticed degree of similarity in the occurrence of subnormal flows across the country. In each of three regions, viz., West, Center, and East, dry years were concentrated in two sequences, one centered in the 1930 's and the second in the decade from the mid-50 's to the mid-60's. (USGS)</p>","language":"English","publisher":"U.S. Geological Survey","doi":"10.3133/ofr82751","usgsCitation":"Langbein, W.B., and Slack, J.R., 1982, Yearly variations in runoff and frequency of dry years for the conterminous United States, 1911-79: U.S. Geological Survey Open-File Report 82-751, iii, 88 p. ill., maps ;28 cm., https://doi.org/10.3133/ofr82751.","productDescription":"iii, 88 p. ill., maps ;28 cm.","onlineOnly":"N","additionalOnlineFiles":"N","costCenters":[],"links":[{"id":143611,"rank":0,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/of/1982/0751/report-thumb.jpg"},{"id":37727,"rank":300,"type":{"id":11,"text":"Document"},"url":"https://pubs.usgs.gov/of/1982/0751/report.pdf","linkFileType":{"id":1,"text":"pdf"}}],"noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"4f4e49e3e4b07f02db5e5bf3","contributors":{"authors":[{"text":"Langbein, W. B.","contributorId":102053,"corporation":false,"usgs":true,"family":"Langbein","given":"W.","email":"","middleInitial":"B.","affiliations":[],"preferred":false,"id":160564,"contributorType":{"id":1,"text":"Authors"},"rank":1},{"text":"Slack, J. R.","contributorId":40205,"corporation":false,"usgs":true,"family":"Slack","given":"J.","email":"","middleInitial":"R.","affiliations":[],"preferred":false,"id":160563,"contributorType":{"id":1,"text":"Authors"},"rank":2}]}}
,{"id":9354,"text":"ofr811113 - 1982 - Hydrology of Area 24, Eastern Coal Province, Alabama and Georgia","interactions":[],"lastModifiedDate":"2016-12-14T12:01:54","indexId":"ofr811113","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":"81-1113","title":"Hydrology of Area 24, Eastern Coal Province, Alabama and Georgia","language":"ENGLISH","publisher":"U.S. Geological Survey,","doi":"10.3133/ofr811113","usgsCitation":"Harkins, J.R., and and others, 1982, Hydrology of Area 24, Eastern Coal Province, Alabama and Georgia: U.S. Geological Survey Open-File Report 81-1113, v, 81 p. :ill., col. maps ;28 cm., https://doi.org/10.3133/ofr811113.","productDescription":"v, 81 p. :ill., col. 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,{"id":58575,"text":"mf1493A - 1982 - Mineral resource potential map of the Bighorn Mountains Wilderness Study Area (CDCA-217), San Bernardino County, California","interactions":[{"subject":{"id":46460,"text":"ofr82962 - 1982 - Mineral resource potential map of the Bighorn Mountains Wilderness Study Area (CDCA-217), San Bernardino County, California","indexId":"ofr82962","publicationYear":"1982","noYear":false,"title":"Mineral resource potential map of the Bighorn Mountains Wilderness Study Area (CDCA-217), San Bernardino County, California"},"predicate":"SUPERSEDED_BY","object":{"id":58575,"text":"mf1493A - 1982 - Mineral resource potential map of the Bighorn Mountains Wilderness Study Area (CDCA-217), San Bernardino County, California","indexId":"mf1493A","publicationYear":"1982","noYear":false,"chapter":"A","title":"Mineral resource potential map of the Bighorn Mountains Wilderness Study Area (CDCA-217), San Bernardino County, California"},"id":1}],"lastModifiedDate":"2015-10-20T13:14:35","indexId":"mf1493A","displayToPublicDate":"1994-01-01T00:00:00","publicationYear":"1982","noYear":false,"publicationType":{"id":18,"text":"Report"},"publicationSubtype":{"id":5,"text":"USGS Numbered Series"},"seriesTitle":{"id":325,"text":"Miscellaneous Field Studies Map","code":"MF","active":false,"publicationSubtype":{"id":5}},"seriesNumber":"1493","chapter":"A","title":"Mineral resource potential map of the Bighorn Mountains Wilderness Study Area (CDCA-217), San Bernardino County, California","docAbstract":"<p>Geological, geochemical, and geophysical evidence, together with a review of historical mining and prospecting activities, suggests that most of the Bighorn Mountains Wilderness Study Area has low potential for the discovery of all types of mineral and energy resources-including precious and base metals, building stone and aggregate, fossil fuels, radioactive-mineral resources, and geothermal resources. Low-grade mineralization has been documented in one small area near Rattlesnake Canyon, and this area has low to moderate potential for future small-scale exploration and development of precious and base metals. Thorium and uranium enrichment have been documented in two small areas in the eastern part of the wilderness study area; these two areas have low to moderate potential for future small-scale exploration and development of radioactive-mineral resources.</p>","language":"English","publisher":"U.S. Geological Survey","doi":"10.3133/mf1493A","usgsCitation":"Matti, J.C., Cox, B.F., Rodriguez, E.A., Obi, C.M., Powell, R.E., Hinkle, M., Griscom, A., Sabine, C., and Cwick, G.J., 1982, Mineral resource potential map of the Bighorn Mountains Wilderness Study Area (CDCA-217), San Bernardino County, California: U.S. Geological Survey Miscellaneous Field Studies Map 1493, Report: 8 p.; Plate: 45.83 x 38.60 inches, https://doi.org/10.3133/mf1493A.","productDescription":"Report: 8 p.; Plate: 45.83 x 38.60 inches","numberOfPages":"10","onlineOnly":"N","additionalOnlineFiles":"N","costCenters":[],"links":[{"id":181313,"rank":0,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/thumbnails/mf1493A.PNG"},{"id":310170,"rank":2,"type":{"id":17,"text":"Plate"},"url":"https://pubs.usgs.gov/mf/1493-A/plate-1.pdf","text":"Plate"},{"id":310169,"rank":1,"type":{"id":11,"text":"Document"},"url":"https://pubs.usgs.gov/mf/1493-A/report.pdf","text":"Report","linkFileType":{"id":1,"text":"pdf"}}],"country":"United States","state":"California","county":"San Bernardino County","geographicExtents":"{ \"type\": \"FeatureCollection\", \"features\": [ { \"type\": \"Feature\", \"properties\": {}, \"geometry\": { \"type\": \"Polygon\", \"coordinates\": [ [ [ -116.75,34.200833333333335 ], [ -116.75,34.3675 ], [ -116.45083333333334,34.3675 ], [ -116.45083333333334,34.200833333333335 ], [ -116.75,34.200833333333335 ] ] ] } } ] }","noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"4f4e4afde4b07f02db696cef","contributors":{"authors":[{"text":"Matti, Jonathan C. jmatti@usgs.gov","contributorId":3666,"corporation":false,"usgs":true,"family":"Matti","given":"Jonathan","email":"jmatti@usgs.gov","middleInitial":"C.","affiliations":[{"id":312,"text":"Geology, Minerals, Energy, and Geophysics Science Center","active":true,"usgs":true}],"preferred":false,"id":259862,"contributorType":{"id":1,"text":"Authors"},"rank":1},{"text":"Cox, Brett F. bcox@usgs.gov","contributorId":5793,"corporation":false,"usgs":true,"family":"Cox","given":"Brett","email":"bcox@usgs.gov","middleInitial":"F.","affiliations":[],"preferred":true,"id":259863,"contributorType":{"id":1,"text":"Authors"},"rank":2},{"text":"Rodriguez, Eduardo A.","contributorId":83540,"corporation":false,"usgs":true,"family":"Rodriguez","given":"Eduardo","email":"","middleInitial":"A.","affiliations":[],"preferred":false,"id":259864,"contributorType":{"id":1,"text":"Authors"},"rank":3},{"text":"Obi, Curtis M.","contributorId":86829,"corporation":false,"usgs":true,"family":"Obi","given":"Curtis","email":"","middleInitial":"M.","affiliations":[],"preferred":false,"id":259865,"contributorType":{"id":1,"text":"Authors"},"rank":4},{"text":"Powell, Robert E. 0000-0001-7682-1655 rpowell@usgs.gov","orcid":"https://orcid.org/0000-0001-7682-1655","contributorId":4210,"corporation":false,"usgs":true,"family":"Powell","given":"Robert","email":"rpowell@usgs.gov","middleInitial":"E.","affiliations":[{"id":312,"text":"Geology, Minerals, Energy, and Geophysics Science Center","active":true,"usgs":true}],"preferred":true,"id":259866,"contributorType":{"id":1,"text":"Authors"},"rank":5},{"text":"Hinkle, Margaret","contributorId":36918,"corporation":false,"usgs":true,"family":"Hinkle","given":"Margaret","affiliations":[],"preferred":false,"id":259860,"contributorType":{"id":1,"text":"Authors"},"rank":6},{"text":"Griscom, Andrew","contributorId":23520,"corporation":false,"usgs":true,"family":"Griscom","given":"Andrew","email":"","affiliations":[],"preferred":false,"id":259861,"contributorType":{"id":1,"text":"Authors"},"rank":7},{"text":"Sabine, Charles","contributorId":88407,"corporation":false,"usgs":true,"family":"Sabine","given":"Charles","email":"","affiliations":[],"preferred":false,"id":576232,"contributorType":{"id":1,"text":"Authors"},"rank":8},{"text":"Cwick, Gary J.","contributorId":86022,"corporation":false,"usgs":true,"family":"Cwick","given":"Gary","email":"","middleInitial":"J.","affiliations":[],"preferred":false,"id":576233,"contributorType":{"id":1,"text":"Authors"},"rank":9}]}}
,{"id":38648,"text":"pp813T - 1982 - Summary appraisals of the nation's ground-water resources – New England region","interactions":[],"lastModifiedDate":"2021-12-14T21:58:30.42222","indexId":"pp813T","displayToPublicDate":"1994-01-01T00:00:00","publicationYear":"1982","noYear":false,"publicationType":{"id":18,"text":"Report"},"publicationSubtype":{"id":5,"text":"USGS Numbered Series"},"seriesTitle":{"id":331,"text":"Professional Paper","code":"PP","onlineIssn":"2330-7102","printIssn":"1044-9612","active":true,"publicationSubtype":{"id":5}},"seriesNumber":"813","chapter":"T","title":"Summary appraisals of the nation's ground-water resources – New England region","docAbstract":"<p>The New England Region has a total area of about 62,400 square miles (160,000 km<sup>2</sup>) and includes the States of Maine and New Hampshire, eastern Vermont, most of Massachusetts and Connecticut, all of Rhode Island, and a small part of southeastern New York. The longest stream is the Connecticut River, which extends from northern Vermont and New Hampshire, through western Massachusetts and central Connecticut, and drains into Long Island Sound. Other major streams are the Penobscot and Kennebec Rivers in Maine, the Androscoggin in Maine and New Hampshire, the Merrimack in New Hampshire and Massachusetts, and the Housatonic in western Massachusetts and Connecticut. Of the smaller streams, some, like the Charles River in the Boston area, are widely known because of their proximity to large population centers.</p>\n<p>Ground water occurs in two types of geologic materials: consolidated rocks and unconsolidated sedimentary rocks. The consolidated rocks underlie the entire region. They include crystalline igneous and metamorphic rocks and consolidated sedimentary rocks-shale, sandstone, and limestone and other carbonate rocks. The most productive unconsolidated rocks are sand and gravel of glacial origin. These deposits occur all over Cape Cod and nearby islands in southeastern Massachusetts and in many valleys throughout the region.</p>\n<p>Ground water is derived from precipitation. It can be intercepted for use by pumping from wells (1) before it discharges to the streams as base flow and (2) before it drains directly into coastal wetlands, bays, Long Island Sound, or the ocean.</p>\n<p>Withdrawals of fresh ground water in 1975 aggregated about 220 billion gallons (830 hm<sup>3</sup>), or about 12 percent of the total freshwater withdrawals (from all sources) of 1,800 billion gallons (6,800 hm<sup>3</sup>). In view of the available ground-water reserves, considerable additional water, for the anticipated continuing increase in population and economic activity, could be developed.</p>","language":"English","publisher":"U.S. Government Printing Office","publisherLocation":"Washington, D.C.","doi":"10.3133/pp813T","usgsCitation":"Sinnott, A., 1982, Summary appraisals of the nation's ground-water resources – New England region: U.S. Geological Survey Professional Paper 813, vi, 23 p., https://doi.org/10.3133/pp813T.","productDescription":"vi, 23 p.","onlineOnly":"N","additionalOnlineFiles":"N","costCenters":[],"links":[{"id":392898,"rank":3,"type":{"id":36,"text":"NGMDB Index Page"},"url":"https://ngmdb.usgs.gov/Prodesc/proddesc_5074.htm"},{"id":65480,"rank":300,"type":{"id":11,"text":"Document"},"url":"https://pubs.usgs.gov/pp/0813t/report.pdf","text":"Report","size":"6.64 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,{"id":30462,"text":"wri8169 - 1982 - Sedimentation in the East Branch Mahoning Creek basin, Clearfield and Jefferson Counties, Pennsylvania, June 1979 to June 1980","interactions":[],"lastModifiedDate":"2017-06-07T12:25:54","indexId":"wri8169","displayToPublicDate":"1994-01-01T00:00:00","publicationYear":"1982","noYear":false,"publicationType":{"id":18,"text":"Report"},"publicationSubtype":{"id":5,"text":"USGS Numbered Series"},"seriesTitle":{"id":342,"text":"Water-Resources Investigations Report","code":"WRI","active":false,"publicationSubtype":{"id":5}},"seriesNumber":"81-69","title":"Sedimentation in the East Branch Mahoning Creek basin, Clearfield and Jefferson Counties, Pennsylvania, June 1979 to June 1980","docAbstract":"<p>Parts of the East Branch Mahoning Creek basin, a forested area of 29.6 square miles in west-central Pennsylvania, are disturbed by farming, surface mining, unpaved haul roads, eroding reclaimed areas, and logging. Streamflow was measured and water samples collected at a site upstream from the mouth from June 1979 to June 1980 during base flow and storm periods to evaluate sediment discharges. An additional site on a tributary draining mostly farmland was sampled from December 1979 to June 1980. Samples were analyzed for suspended sediment, turbidity, and specific conductance. Daily mean suspended-sediment concentrations and discharges were computed.</p>\n<p>From June 1979 to June 1980, 3,570 tons of suspended sediment was transported from the basin. This was an average yield of 121 tons per square mile per year. From December 1979 to June 1980, a tributary draining 2.21 square miles of a predominantly agricultural area discharged 328 tons of sediment which was 12 percent of the sediment load transported from the entire basin.</p>\n<p>Monthly sediment discharges averaged 298 tons ranged from 32 tons in July to 1,250 tons in March. The highest daily mean suspended-sediment concentration was 712 milligrams per liter on June 8, 1980. On that date, 267 tons of sediment was discharged from the basin.</p>","language":"English","publisher":"U.S. Geological Survey","doi":"10.3133/wri8169","collaboration":"Prepared in cooperation with the  Pennsylvania Department of Environmental Resources, Bureau of Mining and Reclamation","usgsCitation":"Wetzel, K.L., 1982, Sedimentation in the East Branch Mahoning Creek basin, Clearfield and Jefferson Counties, Pennsylvania, June 1979 to June 1980: U.S. Geological Survey Water-Resources Investigations Report 81-69, iv, 33 p., https://doi.org/10.3133/wri8169.","productDescription":"iv, 33 p.","onlineOnly":"N","additionalOnlineFiles":"N","costCenters":[{"id":532,"text":"Pennsylvania Water Science Center","active":true,"usgs":true}],"links":[{"id":159817,"rank":0,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/thumbnails/wri8169.jpg"},{"id":318653,"rank":1,"type":{"id":11,"text":"Document"},"url":"https://pubs.usgs.gov/wri/1981/0069/report.pdf"}],"country":"United 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Kim L.","contributorId":104884,"corporation":false,"usgs":true,"family":"Wetzel","given":"Kim","email":"","middleInitial":"L.","affiliations":[],"preferred":false,"id":203294,"contributorType":{"id":1,"text":"Authors"},"rank":1}]}}
,{"id":10619,"text":"ofr811121 - 1982 - Water resources of the Ochlockonee River area, northwest Florida","interactions":[],"lastModifiedDate":"2022-08-31T19:15:04.672539","indexId":"ofr811121","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":"81-1121","title":"Water resources of the Ochlockonee River area, northwest Florida","docAbstract":"<p>The Ochlockonee River area comprises about 1,420 square miles in the panhandle of northwest Florida. In 1975, the population of the area was about 48,000. Water use averaged 11.4 million gallons per day; about half was pumped from wells and half from streams.</p><p>The area receives 57 inches of precipitation per year on the average. Much of this water enters the surficial sand aquifer, seeps to streams, or enters the underlying water-bearing zone of the upper confining unit and the Floridan aquifer.</p><p>The water-bearing zone of the upper confining unit is used for rural domestic supplies and is also important because the water it stores is a source of recharge to the underlying Floridan aquifer.</p><p>The Floridan aquifer underlies all of the Ochlockonee River area and, except for the city of Quincy, is the principal source of municipal water supply. Well yields range from as little as 20 gallons per minute in Gadsden County to as much as 4,500 gallons per minute in Leon County. The transmissivity of the Floridan aquifer ranges from about 170 feet squared per day in the southern part of the area to 5,100 feet squared per day in the northern part. Storage coefficients calculated from two aquifer tests are 2 x 10-4 and 2.6 x 10-4. At Tallahassee, directly east of the Ochlockonee River, transmissivity is as high as 130,000 feet squared per day. The Floridan aquifer is recharged by downward leakage of water from the surficial sand aquifer and from the water-bearing zone of the upper confining unit. The Floridan aquifer is also recharged directly by rainfall in northern Leon County and in southern Georgia where it is near or at land surface. Ground water moves toward the southeast from the potentiometric high in southwestern Gadsden County and south from Leon County toward Wakulla Springs, located about 10 miles south of Tallahassee. The potentiometric surface of the upper part of the Floridan aquifer ranges from about 50 feet higher than that of the middle and lower part of the Floridan aquifer in southwestern Gadsden County to about 10 feet higher near Midway in eastern Gadsden County. The aquifer discharge in the basin area is by wells and by natural discharge through seeps and springs along the Ochlockonee River and at Ochlockonee Bay.</p><p>Water levels in the Floridan aquifer fluctuate in response to seasonal and long-term variations in rainfall. Hydrographs do not show evidence of any long-term water-level declining trend.</p><p>Saline water (more than 1,000 milligrams per liter of dissolved solids) occurs naturally within the Floridan aquifer throughout the Ochlockonee River area at depths ranging from 200 to 600 feet below sea level. The depth below which dissolved solids in water exceed 500 milligrams per liter in the Havana area ranges from 200 to 250 feet below sea level; in the Quincy area, from 400 to 450 feet below; and in the Greensboro area, from 200 to 250 feet below.</p><p>Concentrations of dissolved solids in water pumped from wells tapping the Floridan aquifer in the Ochlockonee River area range from 60 to 1,370 milligrams per liter; chloride from 0 to 630 milligrams per liter; sulfate from 0.0 to 280 milligrams per liter; and fluoride from 0.0 to 1.3 milligrams per liter.</p><p>Streamflow originating in the Ochlockonee River area in Florida averages about 1,000 million gallons per day; minimum discharge during dry periods is about 285 million gallons per day. Stream yields range from 0.90 to 2.62 cubic feet per second per square mile. Quincy Creek, at State Highway 267 at Quincy, the primary source of water for the city of Quincy, yields an average flow of 19 million gallons per day, has a 7-day 10-year low flow of 2.8 million gallons per day, and contains water of acceptable quality. The chemical quality of most streams in the basin is acceptable for most uses. Dissolved-solids concentration is generally less than 135 milligrams per liter; pH ranges from 5.3 to 7.3 units; color from 20 to 90 platinum-cobalt units; and turbidity from 3 to 85 Jackson turbidity units. Variations in chloride concentration in water from the Ochlockonee River (5.2 to 140 milligrams per liter) are influenced by discharge of food processing waste and municipal sewage plant effluent to the river.</p><p>The three large lakes in the basin range from 4,000 to 7,000 acres in surface area. All are now used primarily for recreation. Dissolved-solids concentrations of water from the lakes range from less than 20 to 50 milligrams per liter. A major flood occurred in 1975 when the Ochlockonee River near Havana reached the third highest stage of record and the peak flood at the Sopchoppy River exceeded that for the period of record (11 years in 1975); no significant damage occurred.</p>","language":"English","publisher":"U.S. Geological Survey","doi":"10.3133/ofr811121","collaboration":"Prepared in cooperation with the Northwest Florida Water Management District, Gadsden County and the City of Quincy","usgsCitation":"Pascale, C.A., and Wagner, J.R., 1982, Water resources of the Ochlockonee River area, northwest Florida: U.S. Geological Survey Open-File Report 81-1121, vii, 114 p., https://doi.org/10.3133/ofr811121.","productDescription":"vii, 114 p.","costCenters":[],"links":[{"id":406025,"rank":2,"type":{"id":11,"text":"Document"},"url":"https://pubs.usgs.gov/of/1981/1121/report.pdf","linkFileType":{"id":1,"text":"pdf"}},{"id":142486,"rank":0,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/of/1981/1121/report-thumb.jpg"}],"country":"United States","state":"Florida","otherGeospatial":"Ochlockonee River area","geographicExtents":"{\n  \"type\": \"FeatureCollection\",\n  \"features\": [\n    {\n      \"type\": \"Feature\",\n      \"properties\": {},\n      \"geometry\": {\n        \"type\": \"Polygon\",\n        \"coordinates\": [\n          [\n            [\n              -84.75814819335936,\n              29.846599772557077\n            ],\n            [\n              -84.38735961914062,\n              29.846599772557077\n            ],\n            [\n              -84.38735961914062,\n              30.198552988693212\n            ],\n            [\n              -84.75814819335936,\n              30.198552988693212\n            ],\n            [\n              -84.75814819335936,\n              29.846599772557077\n            ]\n          ]\n        ]\n      }\n    }\n  ]\n}","noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"4f4e49f4e4b07f02db5f0499","contributors":{"authors":[{"text":"Pascale, Charles A.","contributorId":99978,"corporation":false,"usgs":true,"family":"Pascale","given":"Charles","email":"","middleInitial":"A.","affiliations":[],"preferred":false,"id":161693,"contributorType":{"id":1,"text":"Authors"},"rank":1},{"text":"Wagner, Jeffry R.","contributorId":48179,"corporation":false,"usgs":true,"family":"Wagner","given":"Jeffry","email":"","middleInitial":"R.","affiliations":[],"preferred":false,"id":161692,"contributorType":{"id":1,"text":"Authors"},"rank":2}]}}
,{"id":10598,"text":"ofr82825 - 1982 - Geochemical analyses of panned heavy-mineral concentrates, stream sediments and rock samples from the East Yuba and West Yuba Roadless Areas, Plumas and Sierra Counties, California","interactions":[],"lastModifiedDate":"2022-09-22T19:37:31.214682","indexId":"ofr82825","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":"82-825","title":"Geochemical analyses of panned heavy-mineral concentrates, stream sediments and rock samples from the East Yuba and West Yuba Roadless Areas, Plumas and Sierra Counties, California","docAbstract":"<p>No abstract available.</p>","language":"English","publisher":"U.S. Geological Survey","doi":"10.3133/ofr82825","usgsCitation":"Page, S.S., and Bergquist, J.R., 1982, Geochemical analyses of panned heavy-mineral concentrates, stream sediments and rock samples from the East Yuba and West Yuba Roadless Areas, Plumas and Sierra Counties, California: U.S. Geological Survey Open-File Report 82-825, Report: i, 116 p.; 1 Plate: 26.28 × 27.58 inches, https://doi.org/10.3133/ofr82825.","productDescription":"Report: i, 116 p.; 1 Plate: 26.28 × 27.58 inches","costCenters":[],"links":[{"id":38428,"rank":300,"type":{"id":11,"text":"Document"},"url":"https://pubs.usgs.gov/of/1982/0825/report.pdf","linkFileType":{"id":1,"text":"pdf"}},{"id":38427,"rank":400,"type":{"id":17,"text":"Plate"},"url":"https://pubs.usgs.gov/of/1982/0825/plate-1.pdf","linkFileType":{"id":1,"text":"pdf"}},{"id":407238,"rank":4,"type":{"id":36,"text":"NGMDB Index Page"},"url":"https://ngmdb.usgs.gov/Prodesc/proddesc_75654.htm","linkFileType":{"id":5,"text":"html"}},{"id":143027,"rank":0,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/of/1982/0825/report-thumb.jpg"}],"country":"United States","state":"California","county":"Plumas County, Sierra County","otherGeospatial":"East Yuba and West Yuba Roadless Areas","geographicExtents":"{\n  \"type\": \"FeatureCollection\",\n  \"features\": [\n    {\n      \"type\": \"Feature\",\n      \"properties\": {},\n      \"geometry\": {\n        \"type\": \"Polygon\",\n        \"coordinates\": [\n          [\n            [\n              -120.925,\n              39.5417\n            ],\n            [\n              -120.66,\n              39.5417\n            ],\n            [\n              -120.66,\n              39.75\n            ],\n            [\n              -120.925,\n              39.75\n            ],\n            [\n              -120.925,\n              39.5417\n            ]\n          ]\n        ]\n      }\n    }\n  ]\n}","noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"4f4e4b24e4b07f02db6ae911","contributors":{"authors":[{"text":"Page, Susan S.","contributorId":67095,"corporation":false,"usgs":true,"family":"Page","given":"Susan","email":"","middleInitial":"S.","affiliations":[],"preferred":false,"id":161654,"contributorType":{"id":1,"text":"Authors"},"rank":1},{"text":"Bergquist, Joel R.","contributorId":106465,"corporation":false,"usgs":true,"family":"Bergquist","given":"Joel","email":"","middleInitial":"R.","affiliations":[],"preferred":false,"id":161655,"contributorType":{"id":1,"text":"Authors"},"rank":2}]}}
,{"id":59016,"text":"mf1337D - 1982 - Mineral resource potential map of the James River Face Wilderness, Bedford and Rockbridge counties, Virginia","interactions":[],"lastModifiedDate":"2015-10-20T11:06:57","indexId":"mf1337D","displayToPublicDate":"1994-01-01T00:00:00","publicationYear":"1982","noYear":false,"publicationType":{"id":18,"text":"Report"},"publicationSubtype":{"id":5,"text":"USGS Numbered Series"},"seriesTitle":{"id":325,"text":"Miscellaneous Field Studies Map","code":"MF","active":false,"publicationSubtype":{"id":5}},"seriesNumber":"1337","chapter":"D","title":"Mineral resource potential map of the James River Face Wilderness, Bedford and Rockbridge counties, Virginia","docAbstract":"<p>The rocks in the James River Face Wilderness are shales and quartzites that overlie a meta-igneous basement. They are folded into a large southwestward-plunging anticline that is cut off on the east and south by an extensive thrust fault that brings old basement rocks over the younger sedimentary rocks. Geochemical studies of stream sediments, soils, and rocks do not reveal any unusually high metal concentrations, but a large resource of metallurgical-grade quartzite and shale suitable for structural clay products and lightweight aggregate is in the wilderness. Antietam (Erwin) Quartzite has been quarried at three sites in the wilderness as raw material for silicon used in the manufacture of ferrosilicon. Other uses included crushed rock for concrete aggregate, road metal, and railroad ballast, and sand for cement and mortar. Potential uses include ganister for silica brick and specialty sands such as filter and furnace sand. Firing tests on samples of shale from the Harpers (Hampton) Formation show that it could be used for the manufacture of brick and as lightweight aggregate. Of marginal economic interest are heavy-mineral layers in the basal Unicoi (Weverton) Formation.</p>","largerWorkType":{"id":18,"text":"Report"},"largerWorkSubtype":{"id":5,"text":"USGS Numbered Series"},"language":"English","publisher":"U.S. Geological Survey","doi":"10.3133/mf1337D","usgsCitation":"Brown, C.E., and Gazdik, G., 1982, Mineral resource potential map of the James River Face Wilderness, Bedford and Rockbridge counties, Virginia: U.S. Geological Survey Miscellaneous Field Studies Map 1337, Report: 6 p.; 1 Plate: 18.1 x 15.4 inches, https://doi.org/10.3133/mf1337D.","productDescription":"Report: 6 p.; 1 Plate: 18.1 x 15.4 inches","startPage":"1","endPage":"6","numberOfPages":"6","onlineOnly":"N","additionalOnlineFiles":"N","costCenters":[],"links":[{"id":185084,"rank":0,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/thumbnails/MF1337D.JPG"},{"id":310119,"rank":1,"type":{"id":11,"text":"Document"},"url":"https://pubs.usgs.gov/mf/1337-D/report.pdf","text":"Report","linkFileType":{"id":1,"text":"pdf"}},{"id":310120,"rank":2,"type":{"id":17,"text":"Plate"},"url":"https://pubs.usgs.gov/mf/1337-D/plate-1.pdf","text":"Plate","linkFileType":{"id":1,"text":"pdf"}}],"scale":"0","country":"United States","state":"Virginia","county":"Bedford County, Rockbridge County","geographicExtents":"{ \"type\": \"FeatureCollection\", \"features\": [ { \"type\": \"Feature\", \"properties\": {}, \"geometry\": { \"type\": \"Polygon\", \"coordinates\": [ [ [ -79.5,37.534166666666664 ], [ -79.5,37.6175 ], [ -79.36749999999999,37.6175 ], [ -79.36749999999999,37.534166666666664 ], [ -79.5,37.534166666666664 ] ] ] } } ] }","noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"4f4e4b1fe4b07f02db6ab75b","contributors":{"authors":[{"text":"Brown, C. Erwin","contributorId":96261,"corporation":false,"usgs":true,"family":"Brown","given":"C.","email":"","middleInitial":"Erwin","affiliations":[],"preferred":false,"id":261274,"contributorType":{"id":1,"text":"Authors"},"rank":1},{"text":"Gazdik, Gertrude C.","contributorId":76736,"corporation":false,"usgs":true,"family":"Gazdik","given":"Gertrude C.","affiliations":[],"preferred":false,"id":261273,"contributorType":{"id":1,"text":"Authors"},"rank":2}]}}
,{"id":7127,"text":"ofr811115 - 1982 - An evaluation of water-quality monitoring in the Brandywine Creek basin, Pennsylvania, 1973-78","interactions":[],"lastModifiedDate":"2017-06-20T10:02:13","indexId":"ofr811115","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":"81-1115","title":"An evaluation of water-quality monitoring in the Brandywine Creek basin, Pennsylvania, 1973-78","docAbstract":"Data recorded from 1973 through 1978 by monitors on West Branch Brandywine Creek at Modena, East Branch Brandywine Creek below Downingtown, and Brandywine Creek at Chadds Ford were analyzed to evaluate the effectiveness of the monitors in describing water-quality conditions. The data show that the stream at Modena and below Downingtown had periods of low dissolved oxygen, and that the stream below Downingtown had a particularly severe dissolved-oxygen deficiency from May through September 1974. The pH at all three sites exceeded 9.0 at times and the pH below Downingtown occasionally dropped below 6.0. The most critical period in the basin was from March to November when pH was most likely to exceed water-quality standards and dissolved oxygen was most likely to fall below the standards. Without the monitors, the extent and magnitude of these problems would not have been detected.","language":"English","publisher":"U.S. Geological Survey","publisherLocation":"Harrisburg, PA","doi":"10.3133/ofr811115","usgsCitation":"Murphy, J., Ritter, J., Brown, A., and Chiarella, J., 1982, An evaluation of water-quality monitoring in the Brandywine Creek basin, Pennsylvania, 1973-78: U.S. Geological Survey Open-File Report 81-1115, iv, 28 p., https://doi.org/10.3133/ofr811115.","productDescription":"iv, 28 p.","additionalOnlineFiles":"N","costCenters":[{"id":532,"text":"Pennsylvania Water Science Center","active":true,"usgs":true}],"links":[{"id":141561,"rank":0,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/of/1981/1115/report-thumb.jpg"},{"id":277911,"type":{"id":11,"text":"Document"},"url":"https://pubs.usgs.gov/of/1981/1115/report.pdf"}],"country":"United States","state":"Pennsylvania","geographicExtents":"{ \"type\": \"FeatureCollection\", \"features\": [ { \"type\": \"Feature\", \"properties\": {}, \"geometry\": { \"type\": \"Polygon\", \"coordinates\": [ [ [ -76.0000,39.7283 ], [ -76.0000,40.1250 ], [ -75.2563,40.1250 ], [ -75.2563,39.7283 ], [ -76.0000,39.7283 ] ] ] } } ] }","noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"4f4e4ad8e4b07f02db68484c","contributors":{"authors":[{"text":"Murphy, J.J.","contributorId":69144,"corporation":false,"usgs":true,"family":"Murphy","given":"J.J.","email":"","affiliations":[],"preferred":false,"id":154391,"contributorType":{"id":1,"text":"Authors"},"rank":1},{"text":"Ritter, J.R.","contributorId":22350,"corporation":false,"usgs":true,"family":"Ritter","given":"J.R.","email":"","affiliations":[],"preferred":false,"id":154389,"contributorType":{"id":1,"text":"Authors"},"rank":2},{"text":"Brown, A.E.","contributorId":48557,"corporation":false,"usgs":true,"family":"Brown","given":"A.E.","email":"","affiliations":[],"preferred":false,"id":154390,"contributorType":{"id":1,"text":"Authors"},"rank":3},{"text":"Chiarella, J.P.","contributorId":17603,"corporation":false,"usgs":true,"family":"Chiarella","given":"J.P.","email":"","affiliations":[],"preferred":false,"id":154388,"contributorType":{"id":1,"text":"Authors"},"rank":4}]}}
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