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No abstract available.

","language":"English","publisher":"U.S. Geological Survey","doi":"10.3133/pp1214","usgsCitation":"Bateman, P.C., and Sawka, W.N., 1981, Raymond quadrangle, Madera and Mariposa counties, California— Analytic data: U.S. Geological Survey Professional Paper 1214, iii, 16 p., https://doi.org/10.3133/pp1214.","productDescription":"iii, 16 p.","costCenters":[],"links":[{"id":389991,"rank":3,"type":{"id":36,"text":"NGMDB Index Page"},"url":"https://ngmdb.usgs.gov/Prodesc/proddesc_74458.htm"},{"id":32287,"rank":300,"type":{"id":11,"text":"Document"},"url":"https://pubs.usgs.gov/pp/1214/report.pdf","linkFileType":{"id":1,"text":"pdf"}},{"id":121484,"rank":0,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/pp/1214/report-thumb.jpg"}],"country":"United States","state":"California","county":"Madera County, Mariposa County","otherGeospatial":"Raymond quadrangle","geographicExtents":"{\n \"type\": \"FeatureCollection\",\n \"features\": [\n {\n \"type\": \"Feature\",\n \"properties\": {},\n \"geometry\": {\n \"type\": \"Polygon\",\n \"coordinates\": [\n [\n [\n -120.0,\n 37\n ],\n [\n -119.75,\n 37\n ],\n [\n -119.75,\n 37.25\n ],\n [\n -120.0,\n 37.25\n ],\n [\n -120.0,\n 37\n ]\n ]\n ]\n }\n }\n ]\n}","noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"4f4e4a7fe4b07f02db6486fb","contributors":{"authors":[{"text":"Bateman, Paul Charles","contributorId":54586,"corporation":false,"usgs":true,"family":"Bateman","given":"Paul","email":"","middleInitial":"Charles","affiliations":[],"preferred":false,"id":151480,"contributorType":{"id":1,"text":"Authors"},"rank":1},{"text":"Sawka, Wayne N.","contributorId":40592,"corporation":false,"usgs":true,"family":"Sawka","given":"Wayne","email":"","middleInitial":"N.","affiliations":[],"preferred":false,"id":151479,"contributorType":{"id":1,"text":"Authors"},"rank":2}]}} ,{"id":43055,"text":"ofr81776 - 1981 - Preliminary maps showing interpretation of Landsat imagery of the Ugashik and Karluk quadrangles, Alaska","interactions":[],"lastModifiedDate":"2012-02-02T00:11:08","indexId":"ofr81776","displayToPublicDate":"1994-01-01T00:00:00","publicationYear":"1981","noYear":false,"publicationType":{"id":18,"text":"Report"},"publicationSubtype":{"id":5,"text":"USGS Numbered Series"},"seriesTitle":{"id":330,"text":"Open-File Report","code":"OFR","onlineIssn":"2331-1258","printIssn":"0196-1497","active":true,"publicationSubtype":{"id":5}},"seriesNumber":"81-776","title":"Preliminary maps showing interpretation of Landsat imagery of the Ugashik and Karluk quadrangles, Alaska","language":"ENGLISH","doi":"10.3133/ofr81776","usgsCitation":"Le Compte, J.R., 1981, Preliminary maps showing interpretation of Landsat imagery of the Ugashik and Karluk quadrangles, Alaska: U.S. Geological Survey Open-File Report 81-776, 2 maps ;45 x 95 cm., https://doi.org/10.3133/ofr81776.","productDescription":"2 maps ;45 x 95 cm.","costCenters":[],"links":[{"id":108176,"rank":700,"type":{"id":15,"text":"Index Page"},"url":"https://ngmdb.usgs.gov/Prodesc/proddesc_12162.htm","linkFileType":{"id":5,"text":"html"},"description":"12162"},{"id":175644,"rank":0,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/thumbnails/usgs_thumb.jpg"},{"id":20184,"rank":400,"type":{"id":17,"text":"Plate"},"url":"https://pubs.usgs.gov/of/1981/0776/plate-1.pdf","linkFileType":{"id":1,"text":"pdf"}},{"id":20185,"rank":401,"type":{"id":17,"text":"Plate"},"url":"https://pubs.usgs.gov/of/1981/0776/plate-2.pdf","linkFileType":{"id":1,"text":"pdf"}}],"noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"4f4e4aafe4b07f02db66ce81","contributors":{"authors":[{"text":"Le Compte, James R.","contributorId":23913,"corporation":false,"usgs":true,"family":"Le Compte","given":"James","email":"","middleInitial":"R.","affiliations":[],"preferred":false,"id":227650,"contributorType":{"id":1,"text":"Authors"},"rank":1}]}} ,{"id":8759,"text":"ofr811125 - 1981 - Hydrologic and morphologic changes in channels of the Platte River basin: A historical perspective","interactions":[],"lastModifiedDate":"2022-08-31T19:15:57.552529","indexId":"ofr811125","displayToPublicDate":"1994-01-01T00:00:00","publicationYear":"1981","noYear":false,"publicationType":{"id":18,"text":"Report"},"publicationSubtype":{"id":5,"text":"USGS Numbered Series"},"seriesTitle":{"id":330,"text":"Open-File Report","code":"OFR","onlineIssn":"2331-1258","printIssn":"0196-1497","active":true,"publicationSubtype":{"id":5}},"seriesNumber":"81-1125","title":"Hydrologic and morphologic changes in channels of the Platte River basin: A historical perspective","docAbstract":"

The channels of the Platte River and its major tributaries, the South Platte and North Platte Rivers in Colorado, Wyoming, and Nebraska, have undergone major changes in hydrologic regime and morphology since 1860. These changes are attributed here to agricultural, municipal, and industrial water use.

Although water-resource development varied temporally throughout the basin, the history of development along the Platte River and tributaries followed four stages: (1) Construction of small, crude ditches to irrigate flood plains; (2) construction of larger canals to irrigate bench lands; (3) construction of reservoirs to store snowmelt runoff; and (4) accelerated development of ground-water resources. Despite differences in rates of development, diversion and storage of water for irrigation, municipal, and industrial use have changed streamflow patterns throughout the basin. At some stations, significant changes in flood peaks, annual mean discharges, and shapes of flow-duration curves have been recorded.

Changes in streamflow patterns are manifested by changes in appearance of channels of the Platte River. Prior to water development in the 19th century, the Platte was a wide (-2 kilometers), shallow (1.8 to 2.4 meters) river characterized by bankfull spring flows and low summer flows. Although timber generally was scarce in the valley, the Platte channels contained hundreds of small, timbered islands. Since development, the channels have changed radically. Comparing surveyor's maps (General Land Office), drawn during the 1860's, with six sets of aerial photographs, taken between 1938 and 1979, for six 5-kilometer reaches of the river shows that the channels have narrowed considerably above the confluence with the Loup River. The width of the channels in 1979 ranged from 8 to 50 percent of the channel width in 1860. Below the confluence with the Loup River, the width of the river in 1979 was about 92 percent of the channel width in 1860. Above the confluence with the Loup River, width reduction has occurred by progressive encroachment of vegetation and consequent vertical and horizontal accretion on sand bars in the channel. Vegetative encroachment on sand bars has occurred because (1) the present hydrologic regime provides more favorable conditions for germination and growth on sand bars, and (2) since development of the basin, flood peaks are no longer capable of scouring vegetation from the sand bars. Overbank flows evidently have become more common, probably because channel narrowing and vegetative encroachment have increased the hydraulic roughness of the channels. Moreover, the magnitude of low flows has increased and the days of no flows has decreased giving the channels a more perennial character.

","language":"English","publisher":"U.S. Geological Survey","doi":"10.3133/ofr811125","usgsCitation":"Eschner, T., Hadley, R.F., and Crowley, K., 1981, Hydrologic and morphologic changes in channels of the Platte River basin: A historical perspective: U.S. Geological Survey Open-File Report 81-1125, v, 57 p., https://doi.org/10.3133/ofr811125.","productDescription":"v, 57 p.","costCenters":[],"links":[{"id":406027,"rank":2,"type":{"id":11,"text":"Document"},"url":"https://pubs.usgs.gov/of/1981/1125/report.pdf","linkFileType":{"id":1,"text":"pdf"}},{"id":141947,"rank":0,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/of/1981/1125/report-thumb.jpg"}],"country":"United States","state":"Colorado, Nebraska, Wyoming","otherGeospatial":"Platte River basin","geographicExtents":"{\n \"type\": \"FeatureCollection\",\n \"features\": [\n {\n \"type\": \"Feature\",\n \"properties\": {},\n \"geometry\": {\n \"type\": \"Polygon\",\n \"coordinates\": [\n [\n [\n -108.67675781249999,\n 39.57182223734374\n ],\n [\n -95.9326171875,\n 39.57182223734374\n ],\n [\n -95.9326171875,\n 43.99281450048989\n ],\n [\n -108.67675781249999,\n 43.99281450048989\n ],\n [\n -108.67675781249999,\n 39.57182223734374\n ]\n ]\n ]\n }\n }\n ]\n}","noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"4f4e4a29e4b07f02db6117ba","contributors":{"authors":[{"text":"Eschner, T.R.","contributorId":45700,"corporation":false,"usgs":true,"family":"Eschner","given":"T.R.","email":"","affiliations":[],"preferred":false,"id":158281,"contributorType":{"id":1,"text":"Authors"},"rank":1},{"text":"Hadley, R. F.","contributorId":27028,"corporation":false,"usgs":true,"family":"Hadley","given":"R.","middleInitial":"F.","affiliations":[],"preferred":false,"id":158280,"contributorType":{"id":1,"text":"Authors"},"rank":2},{"text":"Crowley, K.D.","contributorId":86769,"corporation":false,"usgs":true,"family":"Crowley","given":"K.D.","email":"","affiliations":[],"preferred":false,"id":158282,"contributorType":{"id":1,"text":"Authors"},"rank":3}]}} ,{"id":65632,"text":"i1335 - 1981 - Controlled photomosaic of the Phaethontis Northeast Quadrangle of Mars","interactions":[],"lastModifiedDate":"2012-02-02T00:13:10","indexId":"i1335","displayToPublicDate":"1994-01-01T00:00:00","publicationYear":"1981","noYear":false,"publicationType":{"id":18,"text":"Report"},"publicationSubtype":{"id":5,"text":"USGS Numbered Series"},"seriesTitle":{"id":320,"text":"IMAP","code":"I","active":false,"publicationSubtype":{"id":5}},"seriesNumber":"1335","subseriesTitle":"NONE","title":"Controlled photomosaic of the Phaethontis Northeast Quadrangle of Mars","language":"ENGLISH","doi":"10.3133/i1335","usgsCitation":"Water Resources Division, U.S. Geological Survey, 1981, Controlled photomosaic of the Phaethontis Northeast Quadrangle of Mars: U.S. Geological Survey IMAP 1335, 1 map ;52 x 58 cm., https://doi.org/10.3133/i1335.","productDescription":"1 map ;52 x 58 cm.","costCenters":[],"links":[{"id":190232,"rank":0,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/thumbnails/usgs_thumb.jpg"},{"id":260780,"rank":900,"type":{"id":17,"text":"Plate"},"url":"https://pubs.usgs.gov/imap/1335/plate-1.pdf"}],"scale":"2000000","noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"4f4e4adce4b07f02db6866a0","contributors":{"authors":[{"text":"Water Resources Division, U.S. Geological Survey","contributorId":128075,"corporation":true,"usgs":false,"organization":"Water Resources Division, U.S. Geological Survey","id":534020,"contributorType":{"id":1,"text":"Authors"},"rank":1}]}} ,{"id":61105,"text":"mf857 - 1981 - Continental margin stratigraphy along the U.S. Geological Survey seismic line 5; Long Island Platform and western Georges Bank Basin","interactions":[],"lastModifiedDate":"2025-05-16T18:17:40.127248","indexId":"mf857","displayToPublicDate":"1994-01-01T00:00:00","publicationYear":"1981","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":"857","title":"Continental margin stratigraphy along the U.S. Geological Survey seismic line 5; Long Island Platform and western Georges Bank Basin","docAbstract":"

No abstract available.

","language":"English","publisher":"U.S. Geological Survey","publisherLocation":"Reston, VA","doi":"10.3133/mf857","usgsCitation":"Valentine, P.C., 1981, Continental margin stratigraphy along the U.S. Geological Survey seismic line 5; Long Island Platform and western Georges Bank Basin: U.S. Geological Survey Miscellaneous Field Studies Map 857, 2 Plates: 30.84 x 43.09 inches and 37.95 x 43.26 inches, https://doi.org/10.3133/mf857.","productDescription":"2 Plates: 30.84 x 43.09 inches and 37.95 x 43.26 inches","costCenters":[],"links":[{"id":182592,"rank":1,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/mf/0857/report-thumb.jpg"},{"id":364242,"rank":2,"type":{"id":17,"text":"Plate"},"url":"https://pubs.usgs.gov/mf/0857/plate-1.pdf","linkFileType":{"id":1,"text":"pdf"}},{"id":364243,"rank":3,"type":{"id":17,"text":"Plate"},"url":"https://pubs.usgs.gov/mf/0857/plate-2.pdf","linkFileType":{"id":1,"text":"pdf"}},{"id":486099,"rank":4,"type":{"id":36,"text":"NGMDB Index Page"},"url":"https://ngmdb.usgs.gov/Prodesc/proddesc_4037.htm","linkFileType":{"id":5,"text":"html"}}],"country":"United States","otherGeospatial":"Long Island Platform and western Georges Bank Basin","geographicExtents":"{ \"type\": \"FeatureCollection\", \"features\": [ { \"type\": \"Feature\", \"properties\": {}, \"geometry\": { \"type\": \"Polygon\", \"coordinates\": [ [ [ -72,39.5 ], [ -72,41.5 ], [ -68,41.5 ], [ -68,39.5 ], [ -72,39.5 ] ] ] } } ] }","noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"4f4e4b04e4b07f02db69909a","contributors":{"authors":[{"text":"Valentine, P. 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S.","contributorId":48937,"corporation":false,"usgs":true,"family":"Harwood","given":"D.","email":"","middleInitial":"S.","affiliations":[],"preferred":false,"id":274083,"contributorType":{"id":1,"text":"Authors"},"rank":1},{"text":"Helley, E. J.","contributorId":76330,"corporation":false,"usgs":true,"family":"Helley","given":"E.","email":"","middleInitial":"J.","affiliations":[],"preferred":false,"id":274084,"contributorType":{"id":1,"text":"Authors"},"rank":2},{"text":"Doukas, M.P.","contributorId":28615,"corporation":false,"usgs":true,"family":"Doukas","given":"M.P.","email":"","affiliations":[],"preferred":false,"id":274082,"contributorType":{"id":1,"text":"Authors"},"rank":3}]}} ,{"id":8479,"text":"ofr811329 - 1981 - Coal exploratory holes drilled in 1980 in the Birney 1 degree x 2 degrees quadrangle, Powder River and Big Horn Counties, Montana","interactions":[],"lastModifiedDate":"2012-02-02T00:06:14","indexId":"ofr811329","displayToPublicDate":"1994-01-01T00:00:00","publicationYear":"1981","noYear":false,"publicationType":{"id":18,"text":"Report"},"publicationSubtype":{"id":5,"text":"USGS Numbered Series"},"seriesTitle":{"id":330,"text":"Open-File Report","code":"OFR","onlineIssn":"2331-1258","printIssn":"0196-1497","active":true,"publicationSubtype":{"id":5}},"seriesNumber":"81-1329","title":"Coal exploratory holes drilled in 1980 in the Birney 1 degree x 2 degrees quadrangle, Powder River and Big Horn Counties, Montana","language":"ENGLISH","publisher":"U.S. Geological Survey,","doi":"10.3133/ofr811329","usgsCitation":"Culbertson, W., 1981, Coal exploratory holes drilled in 1980 in the Birney 1 degree x 2 degrees quadrangle, Powder River and Big Horn Counties, Montana: U.S. Geological Survey Open-File Report 81-1329, 54 p. ill. ;28 cm., https://doi.org/10.3133/ofr811329.","productDescription":"54 p. ill. ;28 cm.","costCenters":[],"links":[{"id":141617,"rank":0,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/of/1981/1329/report-thumb.jpg"},{"id":36045,"rank":400,"type":{"id":17,"text":"Plate"},"url":"https://pubs.usgs.gov/of/1981/1329/plate-1.pdf","linkFileType":{"id":1,"text":"pdf"}},{"id":36046,"rank":300,"type":{"id":11,"text":"Document"},"url":"https://pubs.usgs.gov/of/1981/1329/report.pdf","linkFileType":{"id":1,"text":"pdf"}}],"noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"4f4e49d5e4b07f02db5dda52","contributors":{"authors":[{"text":"Culbertson, W.C.","contributorId":28979,"corporation":false,"usgs":true,"family":"Culbertson","given":"W.C.","email":"","affiliations":[],"preferred":false,"id":157785,"contributorType":{"id":1,"text":"Authors"},"rank":1}]}} ,{"id":5896,"text":"pp1223 - 1981 - Seismic intensities of earthquakes of conterminous United States– Their prediction and interpretation","interactions":[],"lastModifiedDate":"2021-12-09T21:28:54.020938","indexId":"pp1223","displayToPublicDate":"1994-01-01T00:00:00","publicationYear":"1981","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":"1223","title":"Seismic intensities of earthquakes of conterminous United States– Their prediction and interpretation","docAbstract":"

No abstract available.

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F.","contributorId":40593,"corporation":false,"usgs":true,"family":"Evernden","given":"J. F.","affiliations":[],"preferred":false,"id":151763,"contributorType":{"id":1,"text":"Authors"},"rank":1},{"text":"Kohler, W.M.","contributorId":62999,"corporation":false,"usgs":true,"family":"Kohler","given":"W.M.","email":"","affiliations":[],"preferred":false,"id":151764,"contributorType":{"id":1,"text":"Authors"},"rank":2},{"text":"Clow, Gary D. 0000-0002-2262-3853 clow@usgs.gov","orcid":"https://orcid.org/0000-0002-2262-3853","contributorId":2066,"corporation":false,"usgs":true,"family":"Clow","given":"Gary","email":"clow@usgs.gov","middleInitial":"D.","affiliations":[{"id":318,"text":"Geosciences and Environmental Change Science Center","active":true,"usgs":true}],"preferred":true,"id":151762,"contributorType":{"id":1,"text":"Authors"},"rank":3}]}} ,{"id":65848,"text":"i1295 - 1981 - Shaded relief map of the Coprates Northwest Quadrangle of Mars","interactions":[],"lastModifiedDate":"2012-02-02T00:13:17","indexId":"i1295","displayToPublicDate":"1994-01-01T00:00:00","publicationYear":"1981","noYear":false,"publicationType":{"id":18,"text":"Report"},"publicationSubtype":{"id":5,"text":"USGS Numbered Series"},"seriesTitle":{"id":320,"text":"IMAP","code":"I","active":false,"publicationSubtype":{"id":5}},"seriesNumber":"1295","subseriesTitle":"NONE","title":"Shaded relief map of the Coprates Northwest Quadrangle of Mars","language":"ENGLISH","doi":"10.3133/i1295","usgsCitation":"Water Resources Division, U.S. Geological Survey, 1981, Shaded relief map of the Coprates Northwest Quadrangle of Mars: U.S. Geological Survey IMAP 1295, 1 remote-sensing image :col. ;30 x 60 cm. on sheet 86 x 67 cm. folded in envelope 30 x 24 cm., https://doi.org/10.3133/i1295.","productDescription":"1 remote-sensing image :col. ;30 x 60 cm. on sheet 86 x 67 cm. folded in envelope 30 x 24 cm.","costCenters":[],"links":[{"id":190179,"rank":0,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/thumbnails/usgs_thumb.jpg"},{"id":101202,"rank":400,"type":{"id":17,"text":"Plate"},"url":"https://pubs.usgs.gov/imap/1295/plate-1.pdf","size":"8324","linkFileType":{"id":1,"text":"pdf"}}],"scale":"2000000","noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"4f4e49fbe4b07f02db5f473a","contributors":{"authors":[{"text":"Water Resources Division, U.S. Geological Survey","contributorId":128075,"corporation":true,"usgs":false,"organization":"Water Resources Division, U.S. Geological Survey","id":534203,"contributorType":{"id":1,"text":"Authors"},"rank":1}]}} ,{"id":5847,"text":"pp1205 - 1981 - The Accotink Schist, Lake Barcroft Metasandstone, and Popes Head Formation— Keys to an understanding of the tectonic evolution of the northern Virginia Piedmont","interactions":[],"lastModifiedDate":"2021-09-14T19:06:43.500379","indexId":"pp1205","displayToPublicDate":"1994-01-01T00:00:00","publicationYear":"1981","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":"1205","title":"The Accotink Schist, Lake Barcroft Metasandstone, and Popes Head Formation— Keys to an understanding of the tectonic evolution of the northern Virginia Piedmont","docAbstract":"The newly named Accotink Schist and Lake Barcroft Metasandstone of the Eastern Fairfax sequence are the structurally lowest metamorphic rocks in the northernmost Piedmont of Virginia. The Accotink consists of beds of pelitic schist that have thin basal intervals containing graded, very fine grained metasiltstone, as well as interbeds of metasandstone like that in the overlying Lake Barcroft Metasandstone. The unit is characterized by the Bouma turbidite sequences Te and Tde and can be assigned to turbidite facies D and E. The thickness of the Accotink is not known because its base is not exposed. \r\n\r\nThe Accotink Schist grades up into the Lake Barcroft Metasandstone, which consists of two types of metasandstone. Type I metaarenite is quartzofeldspathic granofels which forms thick sequences of amalgamated beds that can best be described as belonging to the Bouma turbidite sequence Ta and to turbidite facies B 2 . Type II metagraywacke of the Lake Barcroft Metasandstone consists of micaceous metagraywacke in thin to medium beds, which can be described as belonging to the Buoma turbidite sequences Tabe and (or) Tae and to turbidite facies C. The Lake Barcroft Metasandstone appears to be about 400 m thick. It and the Accotink Schist are thought to represent a coarsening-upward sequence of an outer submarine-fan association of rocks. \r\n\r\nThe Eastern Fairfax sequence is overlain by the Sykesville Formation. We believe that this contact is a movement surface upon which the Sykesville was emplaced by subaqueous sliding. The Sykesville contains isoclinally folded fragments, thought to be rip-ups, of Accotink and Lake Barcroft rocks. The Eastern Fairfax sequence is intruded by rocks of the Occoquan Granite batholith, which contains pendants of isoclinally folded schist and metagraywacke. Mter intrusion, the metasedimentary and plutonic rocks were folded together. Gamet and chlorite porphyroblasts within the Eastern Fairfax sequence appear to be related to the emplacement of the batholith. The minimum age of the Eastern Fairfax sequence is that of the Occoquan Granite batholith, currently thought to be about 560 m.y. The sequence, then, is considered to be of Early Cambrian age or older. The Accotink Schist and Lake Barcroft Metasandstone have some lithic similarity to the Loch Raven Schist and Oella Formation of Crowley (1976) of the Baltimore area, but a correlation is very uncertain at this time. \r\n\r\nThe newly named Popes Head Formation overlies all other metasedimentary and transported meta-igneous rocks in northernmost Virginia west ofthe Occoquan Granite batholith and is intruded by the batholith. The Popes Head consists of a lower Old Mill Branch Metasiltstone Member and an upper Station Hills Phyllite Member. The Old Mill Branch consists largely of alternating coarser and finer grained strata that are mostly fine- to very fine grained, mineralogically quite mature graded metasiltstone, which can be described as belonging to Bouma turbidite sequence Tbde and (or) Tde, more rarely Tcde. The metasiltstone contains interbedded intervals in which both felsic and mafic metatuff contain pristine euhedral crystals of igneous minerals. We believe that the metatuff represents ash-fall deposits. The Old Mill Branch appears to be about 730 m thick. \r\n\r\nThe Old Mill Branch grades up into the Station Hills Phyllite Member, which consists of thin- to medium-bedded pelitic phyllite and smaller amounts of very fine grained metasiltstone. The metasiltstone beds are graded, and many phyllite beds appear to have basal in- tervals containing graded, very fine grained metasiltstone. These beds can be described as belonging to Bouma turbidite sequence Tde. The Station Hills has intervals containing chlorite-rich phyllite, which probably represents mafic metatuff. No felsic metatuff has been recognized. The top of the Station Hills is not known, neither therefore, is its thickness. This unit appears to have a maximum thickness of about 300 m in northern","language":"English","publisher":"U.S. Geological Survey","doi":"10.3133/pp1205","usgsCitation":"Drake, A., and Lyttle, P.T., 1981, The Accotink Schist, Lake Barcroft Metasandstone, and Popes Head Formation— Keys to an understanding of the tectonic evolution of the northern Virginia Piedmont: U.S. Geological Survey Professional Paper 1205, Report: iv, 16 p.; 12.50 × 26.00 inches, https://doi.org/10.3133/pp1205.","productDescription":"Report: iv, 16 p.; 12.50 × 26.00 inches","costCenters":[],"links":[{"id":104571,"rank":3,"type":{"id":36,"text":"NGMDB Index Page"},"url":"https://ngmdb.usgs.gov/Prodesc/proddesc_4752.htm","linkFileType":{"id":5,"text":"html"},"description":"4752"},{"id":32626,"rank":301,"type":{"id":11,"text":"Document"},"url":"https://pubs.usgs.gov/pp/1205/report.pdf","linkFileType":{"id":1,"text":"pdf"}},{"id":32625,"rank":401,"type":{"id":17,"text":"Plate"},"url":"https://pubs.usgs.gov/pp/1205/plate-1.pdf","linkFileType":{"id":1,"text":"pdf"}},{"id":121841,"rank":0,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/pp/1205/report-thumb.jpg"}],"country":"United States","state":"Virginia","geographicExtents":"{\n \"type\": \"FeatureCollection\",\n \"features\": [\n {\n \"type\": \"Feature\",\n \"properties\": {},\n \"geometry\": {\n \"type\": \"Polygon\",\n \"coordinates\": [\n [\n [\n -77.46185302734375,\n 38.494443887725055\n ],\n [\n -77.069091796875,\n 38.494443887725055\n ],\n [\n -77.069091796875,\n 38.97862765746913\n ],\n [\n -77.46185302734375,\n 38.97862765746913\n ],\n [\n -77.46185302734375,\n 38.494443887725055\n ]\n ]\n ]\n }\n }\n ]\n}","noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"4f4e4ad5e4b07f02db683669","contributors":{"authors":[{"text":"Drake, Avery Ala","contributorId":65460,"corporation":false,"usgs":true,"family":"Drake","given":"Avery Ala","affiliations":[],"preferred":false,"id":151676,"contributorType":{"id":1,"text":"Authors"},"rank":1},{"text":"Lyttle, Peter T. plyttle@usgs.gov","contributorId":293,"corporation":false,"usgs":true,"family":"Lyttle","given":"Peter","email":"plyttle@usgs.gov","middleInitial":"T.","affiliations":[],"preferred":true,"id":151675,"contributorType":{"id":1,"text":"Authors"},"rank":2}]}} ,{"id":5649,"text":"pp1141 - 1981 - Research in the Geysers-Clear Lake geothermal area, Northern California","interactions":[{"subject":{"id":22152,"text":"ofr80988 - 1980 - Seismicity of the Geysers-Clear Lake region, California","indexId":"ofr80988","publicationYear":"1980","noYear":false,"title":"Seismicity of the Geysers-Clear Lake region, California"},"predicate":"SUPERSEDED_BY","object":{"id":5649,"text":"pp1141 - 1981 - Research in the Geysers-Clear Lake geothermal area, Northern California","indexId":"pp1141","publicationYear":"1981","noYear":false,"title":"Research in the Geysers-Clear Lake geothermal area, Northern California"},"id":1}],"lastModifiedDate":"2024-11-18T18:45:00.711422","indexId":"pp1141","displayToPublicDate":"1994-01-01T00:00:00","publicationYear":"1981","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":"1141","title":"Research in the Geysers-Clear Lake geothermal area, Northern California","docAbstract":"

The Geysers-Clear Lake area is one of two places in the world where major vapor-dominated hydrothermal reservoirs are commercially exploited for electric power production. Because energy can be extracted more efficiently from steam than from hot water, vapor-dominated systems are preferable for electric power generation, although most geothermal electric power facilities tap water-dominated systems. The Geysers- Clear Lake geothermal system has therefore been of great interest to the geothermal industry.

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D.","contributorId":87551,"corporation":false,"usgs":true,"family":"Rowley","given":"P.","email":"","middleInitial":"D.","affiliations":[],"preferred":false,"id":264342,"contributorType":{"id":1,"text":"Authors"},"rank":1},{"text":"Cunningham, C. G.","contributorId":76741,"corporation":false,"usgs":true,"family":"Cunningham","given":"C.","middleInitial":"G.","affiliations":[],"preferred":false,"id":264341,"contributorType":{"id":1,"text":"Authors"},"rank":2},{"text":"Kaplan, A.M.","contributorId":69234,"corporation":false,"usgs":true,"family":"Kaplan","given":"A.M.","email":"","affiliations":[],"preferred":false,"id":264340,"contributorType":{"id":1,"text":"Authors"},"rank":3}]}} ,{"id":9696,"text":"ofr81140 - 1981 - Fluoride concentrations in water from four principal coastal plain aquifer systems, South Carolina","interactions":[],"lastModifiedDate":"2022-03-14T16:24:46.592512","indexId":"ofr81140","displayToPublicDate":"1994-01-01T00:00:00","publicationYear":"1981","noYear":false,"publicationType":{"id":18,"text":"Report"},"publicationSubtype":{"id":5,"text":"USGS Numbered Series"},"seriesTitle":{"id":330,"text":"Open-File Report","code":"OFR","onlineIssn":"2331-1258","printIssn":"0196-1497","active":true,"publicationSubtype":{"id":5}},"seriesNumber":"81-140","title":"Fluoride concentrations in water from four principal coastal plain aquifer systems, South Carolina","docAbstract":"

Ample supplies of ground water are available throughout most of the Coastal Plain of South Carolina, but in many places the fluoride concentrations far exceed (as high as 5.8 mg/L, milligrams per liter) the MCL (maximum concentration limit) established for drinking water by the EPA (U.S. Environmental Protection Agency) and SCDHEC (South Carolina Department of Health and Environmental Control).

Fluoridation of drinking water for the prevention of dental caries is a well known practice in many parts of the country. Low concentrations of fluoride have an apparent beneficial effect whereas high concentrations may cause dental fluorosis (mottled teeth enamel) in young children. The recommended concentration of fluoride, as established by EPA (1975) in South Carolina ranges from 1.4 to about 2.4 mg/L depending on the daily air temperature (tables 1 and 2). A lower fluoride concentration in drinking water is considered optimum in areas of high air temperature because generally more water is consumed by individuals in these areas. The total fluoride intake in a warm area where the concentration is low, therefore, will be approximately the same as in a cooler area where the concentration is higher. However, it has been established by SCDHEC that the MCL for fluoride in public drinking water in the coastal areas will be 1.6 mg/L (R. Lewis Shaw, written commun., 1976).

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152035,33.350925],[-79.158429,33.332811],[-79.162332,33.327246],[-79.180318,33.254141],[-79.180563,33.237955],[-79.172394,33.206577],[-79.18787,33.173712],[-79.195631,33.166016],[-79.215453,33.155569],[-79.238262,33.137055],[-79.24609,33.124865],[-79.290754,33.110051]]]},\"properties\":{\"name\":\"South Carolina\",\"nation\":\"USA \"}}]}","noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"4f4e49d6e4b07f02db5de68c","contributors":{"authors":[{"text":"Johnson, Phillip W.","contributorId":27422,"corporation":false,"usgs":true,"family":"Johnson","given":"Phillip","email":"","middleInitial":"W.","affiliations":[],"preferred":false,"id":160144,"contributorType":{"id":1,"text":"Authors"},"rank":1},{"text":"Rhett, James M.","contributorId":60217,"corporation":false,"usgs":true,"family":"Rhett","given":"James M.","affiliations":[],"preferred":false,"id":160145,"contributorType":{"id":1,"text":"Authors"},"rank":2}]}} ,{"id":8411,"text":"ofr811097 - 1981 - Geochemical analyses and summaries of shale from Kentucky","interactions":[],"lastModifiedDate":"2012-02-02T00:06:12","indexId":"ofr811097","displayToPublicDate":"1994-01-01T00:00:00","publicationYear":"1981","noYear":false,"publicationType":{"id":18,"text":"Report"},"publicationSubtype":{"id":5,"text":"USGS Numbered Series"},"seriesTitle":{"id":330,"text":"Open-File Report","code":"OFR","onlineIssn":"2331-1258","printIssn":"0196-1497","active":true,"publicationSubtype":{"id":5}},"seriesNumber":"81-1097","title":"Geochemical analyses and summaries of shale from Kentucky","language":"ENGLISH","publisher":"U.S. Geological Survey,","doi":"10.3133/ofr811097","usgsCitation":"Connor, J.J., 1981, Geochemical analyses and summaries of shale from Kentucky: U.S. Geological Survey Open-File Report 81-1097, ii, 116 p. ill. ;28 cm., https://doi.org/10.3133/ofr811097.","productDescription":"ii, 116 p. ill. ;28 cm.","costCenters":[],"links":[{"id":141956,"rank":0,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/of/1981/1097/report-thumb.jpg"},{"id":35978,"rank":300,"type":{"id":11,"text":"Document"},"url":"https://pubs.usgs.gov/of/1981/1097/report.pdf","linkFileType":{"id":1,"text":"pdf"}}],"noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"4f4e4b24e4b07f02db6ae92c","contributors":{"authors":[{"text":"Connor, Jon J.","contributorId":21948,"corporation":false,"usgs":true,"family":"Connor","given":"Jon","email":"","middleInitial":"J.","affiliations":[],"preferred":false,"id":157669,"contributorType":{"id":1,"text":"Authors"},"rank":1}]}} ,{"id":5890,"text":"pp1188 - 1981 - Geology and origin of the Chilean nitrate deposits","interactions":[],"lastModifiedDate":"2012-02-02T00:05:49","indexId":"pp1188","displayToPublicDate":"1994-01-01T00:00:00","publicationYear":"1981","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":"1188","title":"Geology and origin of the Chilean nitrate deposits","language":"ENGLISH","publisher":"U.S. G.P.O. :\r\nfor sale by the Supt. of Docs., GPO,","doi":"10.3133/pp1188","usgsCitation":"Ericksen, G.E., 1981, Geology and origin of the Chilean nitrate deposits: U.S. Geological Survey Professional Paper 1188, 37 p., https://doi.org/10.3133/pp1188.","productDescription":"37 p.","costCenters":[],"links":[{"id":117379,"rank":0,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/pp/1188/report-thumb.jpg"},{"id":32731,"rank":300,"type":{"id":11,"text":"Document"},"url":"https://pubs.usgs.gov/pp/1188/report.pdf","linkFileType":{"id":1,"text":"pdf"}}],"noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"4f4e4ad7e4b07f02db684379","contributors":{"authors":[{"text":"Ericksen, George Edward","contributorId":38537,"corporation":false,"usgs":true,"family":"Ericksen","given":"George","email":"","middleInitial":"Edward","affiliations":[],"preferred":false,"id":151753,"contributorType":{"id":1,"text":"Authors"},"rank":1}]}} ,{"id":43100,"text":"ofr811106 - 1981 - Ground-water levels in selected well fields and in west-central Florida, May 1981","interactions":[],"lastModifiedDate":"2012-02-02T00:05:03","indexId":"ofr811106","displayToPublicDate":"1994-01-01T00:00:00","publicationYear":"1981","noYear":false,"publicationType":{"id":18,"text":"Report"},"publicationSubtype":{"id":5,"text":"USGS Numbered Series"},"seriesTitle":{"id":330,"text":"Open-File Report","code":"OFR","onlineIssn":"2331-1258","printIssn":"0196-1497","active":true,"publicationSubtype":{"id":5}},"seriesNumber":"81-1106","title":"Ground-water levels in selected well fields and in west-central Florida, May 1981","docAbstract":"The water table in the surficial aquifer and the potentiometric surface of the Floridan aquifer in a 1,200-square-mile area in west-central Florida are mapped semi-annually by the U.S. Geological Survey. Maps are based on water levels measured in wells each May to coincide with seasonal low levels and each September to coincide with seasonal high levels. The mapped area shows 14 well fields that supplied 200.7 million gallons to municipalities on May 18, 1981. The water is withdrawn from the Floridan aquifer, the major aquifer in Florida. The effect of localized withdrawal on ground water is shown on the maps as depressions in both the potentiometric and water-table surfaces. Water levels were lower in May 1981 than in May and September 1980. Annual change of water levels ranged from decreases of 19 feet at Sun City well field to less than 1 foot at Eldridge-Wilde well field. (USGS)","language":"ENGLISH","doi":"10.3133/ofr811106","usgsCitation":"Yobbi, D.K., and Woodham, W.M., 1981, Ground-water levels in selected well fields and in west-central Florida, May 1981: U.S. Geological Survey Open-File Report 81-1106, 32 maps ;on 2 sheets 103 x 75 cm., https://doi.org/10.3133/ofr811106.","productDescription":"32 maps ;on 2 sheets 103 x 75 cm.","costCenters":[],"links":[{"id":135666,"rank":0,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/thumbnails/usgs_thumb.jpg"},{"id":80913,"rank":400,"type":{"id":17,"text":"Plate"},"url":"https://pubs.usgs.gov/of/1981/1106/plate-1.pdf","linkFileType":{"id":1,"text":"pdf"}},{"id":80914,"rank":401,"type":{"id":17,"text":"Plate"},"url":"https://pubs.usgs.gov/of/1981/1106/plate-2.pdf","linkFileType":{"id":1,"text":"pdf"}}],"noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"4f4e4aa8e4b07f02db667605","contributors":{"authors":[{"text":"Yobbi, D. K.","contributorId":56622,"corporation":false,"usgs":true,"family":"Yobbi","given":"D.","email":"","middleInitial":"K.","affiliations":[],"preferred":false,"id":227720,"contributorType":{"id":1,"text":"Authors"},"rank":1},{"text":"Woodham, W. M.","contributorId":72356,"corporation":false,"usgs":true,"family":"Woodham","given":"W.","email":"","middleInitial":"M.","affiliations":[],"preferred":false,"id":227721,"contributorType":{"id":1,"text":"Authors"},"rank":2}]}} ,{"id":8406,"text":"ofr801214 - 1981 - Techniques for estimating magnitude and frequency of floods for Wisconsin streams","interactions":[],"lastModifiedDate":"2015-10-20T09:07:20","indexId":"ofr801214","displayToPublicDate":"1994-01-01T00:00:00","publicationYear":"1981","noYear":false,"publicationType":{"id":18,"text":"Report"},"publicationSubtype":{"id":5,"text":"USGS Numbered Series"},"seriesTitle":{"id":330,"text":"Open-File Report","code":"OFR","onlineIssn":"2331-1258","printIssn":"0196-1497","active":true,"publicationSubtype":{"id":5}},"seriesNumber":"80-1214","title":"Techniques for estimating magnitude and frequency of floods for Wisconsin streams","docAbstract":"

This report provides improved methods for estimating the magnitude and frequency of floods for Wisconsin streams. Proper design of hydraulic structures and adequate flood-plain management depend on this information. Multiple-regression techniques were used to develop equations for estimating flood frequencies at ungaged sites.

\n

The State is divided into five areas and has equations developed for each area. These areas are based on areal factors determined from previous studies and physical basin characteristics. Significant characteristics in the equations are soil permeability, drainage area, slope, storage, forest cover, snowfall, precipitation intensity, and mean annual precipitation. Standard errors of estimate for the regression equations ranged from 23 to 38 percent.

\n

Annual flood peaks, basin characteristics, and flood-frequency values are presented in this report. Data from 184 gaging stations were used in the regression analysis, of which 20 had rainfall-runoff data collected. Long-term synthetic peaks were generated from the rainfall-runoff data and were weighted with the observed peak data to improve the flood-frequency distributions.

\n

A method to estimate flood-frequency values for regulated streams was developed by discharge-drainage area relationships. Graphs for the major regulated streams are presented in the report.

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\"}}]}","noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"4f4e4adbe4b07f02db685c2f","contributors":{"authors":[{"text":"Conger, Duane H.","contributorId":90731,"corporation":false,"usgs":true,"family":"Conger","given":"Duane","email":"","middleInitial":"H.","affiliations":[],"preferred":false,"id":157664,"contributorType":{"id":1,"text":"Authors"},"rank":1}]}} ,{"id":8483,"text":"ofr81639 - 1981 - Low-flow characteristics of streams in the Deschutes River basin, Washington","interactions":[],"lastModifiedDate":"2022-08-15T18:19:42.790664","indexId":"ofr81639","displayToPublicDate":"1994-01-01T00:00:00","publicationYear":"1981","noYear":false,"publicationType":{"id":18,"text":"Report"},"publicationSubtype":{"id":5,"text":"USGS Numbered Series"},"seriesTitle":{"id":330,"text":"Open-File Report","code":"OFR","onlineIssn":"2331-1258","printIssn":"0196-1497","active":true,"publicationSubtype":{"id":5}},"seriesNumber":"81-639","title":"Low-flow characteristics of streams in the Deschutes River basin, Washington","docAbstract":"

The purpose of the study was to determine the magnitude and frequency of low flows of streams in the Deschutes River basin.

The streams in the basin usually have their low flows in August and September. Seven-day low flows were smallest in 1952 when annual rainfall at the Olympia airport was also the least during the 1945-75 period of continuous gaging-station records in the basin.

The magnitude and frequency of seven-day low flows were estimated for 23 streamflow sites, either from frequency analysis of data at long-term stations or from correlation of measured or computed discharges at a stream flow site with data at a long-term station.

Seven-day low flows ranged from no-flow at one tributary of Deschutes River having a drainage area of 1.85 square miles to 98 cubic feet per second for Deschutes River near its mouth, where the drainage was 162 square miles.

Mean monthly flows were determined for two long-term stations and estimated for the months of July to September for the other streamflow sites.

Miscellaneous streamflow measurements made over the years by the U.S. Geological Survey are listed in the Appendix.

","language":"English","publisher":"U.S. Geological Survey","doi":"10.3133/ofr81639","collaboration":"Prepared in cooperation with the State of Washington Department of Fisheries","usgsCitation":"Cummans, J., 1981, Low-flow characteristics of streams in the Deschutes River basin, Washington: U.S. Geological Survey Open-File Report 81-639, iv, 20 p., https://doi.org/10.3133/ofr81639.","productDescription":"iv, 20 p.","costCenters":[],"links":[{"id":405145,"rank":2,"type":{"id":11,"text":"Document"},"url":"https://pubs.usgs.gov/of/1981/0639/report.pdf","linkFileType":{"id":1,"text":"pdf"}},{"id":141641,"rank":0,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/of/1981/0639/report-thumb.jpg"}],"country":"United States","state":"Washington","otherGeospatial":"Deschutes River basin","geographicExtents":"{\n \"type\": \"FeatureCollection\",\n \"features\": [\n {\n \"type\": \"Feature\",\n \"properties\": {},\n \"geometry\": {\n \"type\": \"Polygon\",\n \"coordinates\": [\n [\n [\n -122.9150390625,\n 46.63057868059483\n ],\n [\n -121.904296875,\n 46.63057868059483\n ],\n [\n -121.904296875,\n 47.11499982620772\n ],\n [\n -122.9150390625,\n 47.11499982620772\n ],\n [\n -122.9150390625,\n 46.63057868059483\n ]\n ]\n ]\n }\n }\n ]\n}","noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"4f4e4a7fe4b07f02db6486be","contributors":{"authors":[{"text":"Cummans, J. E.","contributorId":24767,"corporation":false,"usgs":true,"family":"Cummans","given":"J. E.","affiliations":[],"preferred":false,"id":157795,"contributorType":{"id":1,"text":"Authors"},"rank":1}]}} ,{"id":65656,"text":"i1342 - 1981 - Controlled photomosaic of the Oxia Palus Southeast Quadrangle of Mars","interactions":[],"lastModifiedDate":"2012-02-02T00:13:18","indexId":"i1342","displayToPublicDate":"1994-01-01T00:00:00","publicationYear":"1981","noYear":false,"publicationType":{"id":18,"text":"Report"},"publicationSubtype":{"id":5,"text":"USGS Numbered Series"},"seriesTitle":{"id":320,"text":"IMAP","code":"I","active":false,"publicationSubtype":{"id":5}},"seriesNumber":"1342","subseriesTitle":"NONE","title":"Controlled photomosaic of the Oxia Palus Southeast Quadrangle of Mars","language":"ENGLISH","doi":"10.3133/i1342","usgsCitation":"Water Resources Division, U.S. Geological Survey, 1981, Controlled photomosaic of the Oxia Palus Southeast Quadrangle of Mars: U.S. Geological Survey IMAP 1342, 1 map ;41 x 60 cm., https://doi.org/10.3133/i1342.","productDescription":"1 map ;41 x 60 cm.","costCenters":[],"links":[{"id":115003,"rank":300,"type":{"id":11,"text":"Document"},"url":"https://pubs.usgs.gov/imap/1342/report.pdf","size":"31","linkFileType":{"id":1,"text":"pdf"}},{"id":115004,"rank":400,"type":{"id":17,"text":"Plate"},"url":"https://pubs.usgs.gov/imap/1342/plate-1.pdf","size":"7903","linkFileType":{"id":1,"text":"pdf"}},{"id":189762,"rank":0,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/imap/1342/report-thumb.jpg"}],"scale":"2000000","noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"4f4e4adee4b07f02db68752c","contributors":{"authors":[{"text":"Water Resources Division, U.S. Geological Survey","contributorId":128075,"corporation":true,"usgs":false,"organization":"Water Resources Division, U.S. Geological Survey","id":534044,"contributorType":{"id":1,"text":"Authors"},"rank":1}]}} ,{"id":43281,"text":"ofr81976 - 1981 - Geophysical log suite from drill hole No. 10, Mariano Lake-Lake Valley drilling project, McKinley County, New Mexico","interactions":[],"lastModifiedDate":"2012-02-02T00:10:26","indexId":"ofr81976","displayToPublicDate":"1994-01-01T00:00:00","publicationYear":"1981","noYear":false,"publicationType":{"id":18,"text":"Report"},"publicationSubtype":{"id":5,"text":"USGS Numbered Series"},"seriesTitle":{"id":330,"text":"Open-File Report","code":"OFR","onlineIssn":"2331-1258","printIssn":"0196-1497","active":true,"publicationSubtype":{"id":5}},"seriesNumber":"81-976","title":"Geophysical log suite from drill hole No. 10, Mariano Lake-Lake Valley drilling project, McKinley County, New Mexico","language":"ENGLISH","doi":"10.3133/ofr81976","usgsCitation":"Water Resources Division, U.S. Geological Survey, 1981, Geophysical log suite from drill hole No. 10, Mariano Lake-Lake Valley drilling project, McKinley County, New Mexico: U.S. Geological Survey Open-File Report 81-976, 2 well logs ;181 x 31 cm. and 214 x 32 cm. +1 text (7 p. ; 28 cm., https://doi.org/10.3133/ofr81976.","productDescription":"2 well logs ;181 x 31 cm. and 214 x 32 cm. +1 text (7 p. ; 28 cm.","costCenters":[],"links":[{"id":172525,"rank":0,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/of/1981/0976/report-thumb.jpg"},{"id":81061,"rank":300,"type":{"id":11,"text":"Document"},"url":"https://pubs.usgs.gov/of/1981/0976/report.pdf","linkFileType":{"id":1,"text":"pdf"}}],"noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"4f4e4ac8e4b07f02db67c112","contributors":{"authors":[{"text":"Water Resources Division, U.S. Geological Survey","contributorId":128075,"corporation":true,"usgs":false,"organization":"Water Resources Division, U.S. Geological Survey","id":531086,"contributorType":{"id":1,"text":"Authors"},"rank":1}]}} ,{"id":43283,"text":"ofr81969 - 1981 - Geophysical log suite from drill hole No. 4, Mariano Lake-Lake Valley drilling project, McKinley County, New Mexico","interactions":[],"lastModifiedDate":"2018-10-30T13:18:57","indexId":"ofr81969","displayToPublicDate":"1994-01-01T00:00:00","publicationYear":"1981","noYear":false,"publicationType":{"id":18,"text":"Report"},"publicationSubtype":{"id":5,"text":"USGS Numbered Series"},"seriesTitle":{"id":330,"text":"Open-File Report","code":"OFR","onlineIssn":"2331-1258","printIssn":"0196-1497","active":true,"publicationSubtype":{"id":5}},"seriesNumber":"81-969","title":"Geophysical log suite from drill hole No. 4, Mariano Lake-Lake Valley drilling project, McKinley County, New Mexico","docAbstract":"

In the fall of 1980, the U.S. Geological Survey contracted with .Longman Drilling Company of Albuquerque, New Mexico to rotary drill and core twelve holes along a north-south line from Mariano Lake to the vicinity of Lake Valley, New Mexico. This report incorporates the logs from drill hole no. 4. Similar reports on holes no. 1, 2, and 3 were released by the U.S. Geological Survey (1981a, b).

The drilling project is funded under a reimbursable interagency agreement between the U.S. Bureau of Indian Affairs (BIA) and the U.S. Geological Survey (USGS). The program was designed by representatives of the BIA, USGS, and the Minerals Department of the Navajo Tribe.

","language":"English","publisher":"U.S. Geological Survey","doi":"10.3133/ofr81969","usgsCitation":"Water Resources Division, U.S. Geological Survey, 1981, Geophysical log suite from drill hole No. 4, Mariano Lake-Lake Valley drilling project, McKinley County, New Mexico: U.S. Geological Survey Open-File Report 81-969, Report: i, 7 p.; 8 Plates: 11.37 x 170.31 inches or smaller, https://doi.org/10.3133/ofr81969.","productDescription":"Report: i, 7 p.; 8 Plates: 11.37 x 170.31 inches or smaller","costCenters":[],"links":[{"id":358960,"rank":4,"type":{"id":17,"text":"Plate"},"url":"https://pubs.usgs.gov/of/1981/0969/plate-2.pdf","linkFileType":{"id":1,"text":"pdf"}},{"id":172527,"rank":0,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/of/1981/0969/report-thumb.jpg"},{"id":358959,"rank":2,"type":{"id":17,"text":"Plate"},"url":"https://pubs.usgs.gov/of/1981/0969/plate-1.pdf","linkFileType":{"id":1,"text":"pdf"}},{"id":81063,"rank":300,"type":{"id":11,"text":"Document"},"url":"https://pubs.usgs.gov/of/1981/0969/report.pdf","linkFileType":{"id":1,"text":"pdf"}},{"id":358961,"rank":5,"type":{"id":17,"text":"Plate"},"url":"https://pubs.usgs.gov/of/1981/0969/plate-3.pdf","linkFileType":{"id":1,"text":"pdf"}},{"id":358962,"rank":6,"type":{"id":17,"text":"Plate"},"url":"https://pubs.usgs.gov/of/1981/0969/plate-4.pdf","linkFileType":{"id":1,"text":"pdf"}},{"id":358963,"rank":7,"type":{"id":17,"text":"Plate"},"url":"https://pubs.usgs.gov/of/1981/0969/plate-5.pdf","linkFileType":{"id":1,"text":"pdf"}},{"id":358964,"rank":8,"type":{"id":17,"text":"Plate"},"url":"https://pubs.usgs.gov/of/1981/0969/plate-6.pdf","linkFileType":{"id":1,"text":"pdf"}},{"id":358965,"rank":9,"type":{"id":17,"text":"Plate"},"url":"https://pubs.usgs.gov/of/1981/0969/plate-7.pdf","linkFileType":{"id":1,"text":"pdf"}},{"id":358966,"rank":10,"type":{"id":17,"text":"Plate"},"url":"https://pubs.usgs.gov/of/1981/0969/plate-8.pdf","linkFileType":{"id":1,"text":"pdf"}}],"country":"United States","state":"New Mexico","county":"McKinley County","noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"4f4e4ac8e4b07f02db67c119","contributors":{"authors":[{"text":"Water Resources Division, U.S. Geological Survey","contributorId":128075,"corporation":true,"usgs":false,"organization":"Water Resources Division, U.S. Geological Survey","id":531088,"contributorType":{"id":1,"text":"Authors"},"rank":1}]}} ,{"id":30553,"text":"wri8113 - 1981 - An observation-well network concept as applied to North Carolina","interactions":[],"lastModifiedDate":"2018-11-08T15:51:38","indexId":"wri8113","displayToPublicDate":"1994-01-01T00:00:00","publicationYear":"1981","noYear":false,"publicationType":{"id":18,"text":"Report"},"publicationSubtype":{"id":5,"text":"USGS Numbered Series"},"seriesTitle":{"id":342,"text":"Water-Resources Investigations Report","code":"WRI","active":false,"publicationSubtype":{"id":5}},"seriesNumber":"81-13","title":"An observation-well network concept as applied to North Carolina","docAbstract":"

A statewide observation-well program is proposed for North Carolina based on four networks of observation wells with different but clearly-defined objectives. These are referred to as the (1) climatic-effects network, (2) terrane-effects network, (3) local-effects network, and (4) areal-effects network.

The characteristics of each network are related to natural and manmade stresses in aquifers, and the areas and hydrogeologic units in North Carolina where these networks are needed are identified.

Formats for collection, processing, and publication of data from these networks are suggested.

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