{"pageNumber":"5185","pageRowStart":"129600","pageSize":"25","recordCount":184563,"records":[{"id":26628,"text":"wri834065 - 1983 - Backwater and discharge at highway crossings with multiple bridges in Louisiana and Mississippi","interactions":[],"lastModifiedDate":"2012-02-02T00:08:23","indexId":"wri834065","displayToPublicDate":"1994-01-01T00:00:00","publicationYear":"1983","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":"83-4065","title":"Backwater and discharge at highway crossings with multiple bridges in Louisiana and Mississippi","docAbstract":"Data were collected for nine floods in Mississippi and Louisiana at eight stream crossings having two to six separate bridge openings. Discharge through each bridge, water surface profiles, valley cross sections, and bridge geometry were measured. The multiple openings were divided into equivalent single-opening cases by apportioning interior embankments in direct proportion to the area of openings on either side. Using existing procedures for computer discharge, the bias in computed discharge was 2 percent with a root mean square error of 18 percent. Backwater was computed by two current U.S. Geological Survey methods that use the average flow path in the friction loss term for the approach. One method gave a root mean square error of 0.34 ft. with a bias of -0.25 ft., suggesting that the method underestimates backwater. The other method gave a root mean square error of 0.39 ft with a bias of -0.03 ft. The results indicate that the method developed for single-opening highway crossings can be applied to the multiple bridge crossings. (USGS)","language":"ENGLISH","publisher":"U.S. Geological Survey,","doi":"10.3133/wri834065","usgsCitation":"Colson, B., and Schneider, V., 1983, Backwater and discharge at highway crossings with multiple bridges in Louisiana and Mississippi: U.S. Geological Survey Water-Resources Investigations Report 83-4065, vii, 46 p. :ill. ;28 cm., https://doi.org/10.3133/wri834065.","productDescription":"vii, 46 p. :ill. ;28 cm.","costCenters":[],"links":[{"id":121509,"rank":0,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/wri/1983/4065/report-thumb.jpg"},{"id":55500,"rank":300,"type":{"id":11,"text":"Document"},"url":"https://pubs.usgs.gov/wri/1983/4065/report.pdf","linkFileType":{"id":1,"text":"pdf"}}],"noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"4f4e4a82e4b07f02db64ad91","contributors":{"authors":[{"text":"Colson, B.E.","contributorId":71546,"corporation":false,"usgs":true,"family":"Colson","given":"B.E.","email":"","affiliations":[],"preferred":false,"id":196737,"contributorType":{"id":1,"text":"Authors"},"rank":1},{"text":"Schneider, V.R.","contributorId":75129,"corporation":false,"usgs":true,"family":"Schneider","given":"V.R.","email":"","affiliations":[],"preferred":false,"id":196738,"contributorType":{"id":1,"text":"Authors"},"rank":2}]}}
,{"id":27562,"text":"wri834213 - 1983 - Sediment transport in the Tanana River near Fairbanks, Alaska, 1982","interactions":[],"lastModifiedDate":"2012-02-02T00:08:42","indexId":"wri834213","displayToPublicDate":"1994-01-01T00:00:00","publicationYear":"1983","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":"83-4213","title":"Sediment transport in the Tanana River near Fairbanks, Alaska, 1982","docAbstract":"Suspended-sediment and bedload-transport rates for the Tanana River near Fairbanks can be related to water discharge, and annual sediment loads can be computed using these relations. For a site at Fairbanks the annual loads in 1982 were 26.1 million metric tons of suspended sediment and 227,000 metric tons of bedload. Data collected at five other sites within a 40-kilometer reach of the river indicate similar suspended-sediment-transport relations but bedload-transport relations varied from site to site. For all sites bedload is about 1 percent of suspended-sediment load. Particle-size distribution of suspended sediment is similar at all six sites. Median particle size is generally in the silt range; only occasionally is it in the very fine sand range. Median particle size of bedload ranged from the gravel range to the medium sand range at four of the six sampling sites. At the farthest downstream site, Byers Island, and the farthest upstream site, above Chena River Floodway, median particle size of bedload was always in the sand range. (USGS)","language":"ENGLISH","publisher":"U.S. Geological Survey, Water Resources Division,","doi":"10.3133/wri834213","usgsCitation":"Harrold, P., and Burrows, R., 1983, Sediment transport in the Tanana River near Fairbanks, Alaska, 1982: U.S. Geological Survey Water-Resources Investigations Report 83-4213, v, 60 p. :ill., maps ;28 cm., https://doi.org/10.3133/wri834213.","productDescription":"v, 60 p. :ill., maps ;28 cm.","costCenters":[],"links":[{"id":110163,"rank":700,"type":{"id":15,"text":"Index Page"},"url":"https://ngmdb.usgs.gov/Prodesc/proddesc_35856.htm","linkFileType":{"id":5,"text":"html"},"description":"35856"},{"id":122629,"rank":0,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/thumbnails/wri_83_4213.jpg"},{"id":13748,"rank":100,"type":{"id":15,"text":"Index Page"},"url":"https://pubs.usgs.gov/wri/wri83-4213/","linkFileType":{"id":5,"text":"html"}},{"id":56418,"rank":400,"type":{"id":17,"text":"Plate"},"url":"https://pubs.usgs.gov/wri/1983/4213/plate-1.pdf","linkFileType":{"id":1,"text":"pdf"}},{"id":56419,"rank":401,"type":{"id":17,"text":"Plate"},"url":"https://pubs.usgs.gov/wri/1983/4213/plate-2.pdf","linkFileType":{"id":1,"text":"pdf"}}],"noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"4f4e4a0be4b07f02db5fbecc","contributors":{"authors":[{"text":"Harrold, P.E.","contributorId":89935,"corporation":false,"usgs":true,"family":"Harrold","given":"P.E.","email":"","affiliations":[],"preferred":false,"id":198329,"contributorType":{"id":1,"text":"Authors"},"rank":1},{"text":"Burrows, R.L.","contributorId":19977,"corporation":false,"usgs":true,"family":"Burrows","given":"R.L.","email":"","affiliations":[],"preferred":false,"id":198328,"contributorType":{"id":1,"text":"Authors"},"rank":2}]}}
,{"id":26575,"text":"wri834076 - 1983 - Numerical simulation of the alluvium and terrace aquifer along the North Canadian River from Canton Lake to Lake Overholser, central Oklahoma","interactions":[],"lastModifiedDate":"2012-02-02T00:08:28","indexId":"wri834076","displayToPublicDate":"1994-01-01T00:00:00","publicationYear":"1983","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":"83-4076","title":"Numerical simulation of the alluvium and terrace aquifer along the North Canadian River from Canton Lake to Lake Overholser, central Oklahoma","docAbstract":"Alluvium and terrace deposits of Quaternary age, which cover an area of about 400 square miles along the North Canadian River between Canton Lake and Lake Overholser, locally yield as much as 500 gallons per minute to wells. The deposits are as much as 100 feet thick and consist of clay, silt, sand, and gravel, with sand-sized material dominating. The underlying bedrock is Permian sandstone and shale. The amount of water stored in the aquifer during 1980 was estimated to be 4.00 x 1010 cubic feet.\r\nA digital model was used to estimate the ability of the aquifer to continue to supply water for irrigation, industry, and domestic use. A block-centered, finite-difference model with 1 mile node spacing was used to project the amount and distribution of water in the aquifer in the future. The model was calibrated using the aquifer discharge to the North Canadian River and the difference between computed and measured heads. The model was calibrated using recharge rate of 1 inch per year, a horizontal hydraulic conductivity of 4.5 x 10 -4 feet per second and a specific yield of 0.16.\r\n\r\nModel simulations using the 1979 pumping rate, a projected pumping rate (based on expected increases in water use), and double the projected increase in pumping rate were made to 1993. With the 1979 pumping rate, the volume of water in storage in 1993 is 3.88 x 10 10 cubic feet and ground-water discharge to the North Canadian River is 10.9 cubic feet per second. With the projected pumping increase, the volume of water in storage is 3.81 x 1010 cubic feet and ground-water discharge to the stream is 6.91 cubic feet per second. At double the projected increase in pumping rate, the volume of water in storage is\r\n3.74 x 1010 cubic feet and the ground-water discharge is 2.93 cubic feet per second.","language":"ENGLISH","publisher":"U.S. Geological Survey, Water Resources Division,","doi":"10.3133/wri834076","usgsCitation":"Christenson, S.C., 1983, Numerical simulation of the alluvium and terrace aquifer along the North Canadian River from Canton Lake to Lake Overholser, central Oklahoma: U.S. Geological Survey Water-Resources Investigations Report 83-4076, v, 41 p. :ill., maps ;28 cm., https://doi.org/10.3133/wri834076.","productDescription":"v, 41 p. :ill., maps ;28 cm.","costCenters":[],"links":[{"id":110160,"rank":700,"type":{"id":15,"text":"Index Page"},"url":"https://ngmdb.usgs.gov/Prodesc/proddesc_35707.htm","linkFileType":{"id":5,"text":"html"},"description":"35707"},{"id":126886,"rank":0,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/wri/1983/4076/report-thumb.jpg"},{"id":55439,"rank":402,"type":{"id":17,"text":"Plate"},"url":"https://pubs.usgs.gov/wri/1983/4076/plate-03.pdf","linkFileType":{"id":1,"text":"pdf"}},{"id":55440,"rank":403,"type":{"id":17,"text":"Plate"},"url":"https://pubs.usgs.gov/wri/1983/4076/plate-04.pdf","linkFileType":{"id":1,"text":"pdf"}},{"id":55441,"rank":404,"type":{"id":17,"text":"Plate"},"url":"https://pubs.usgs.gov/wri/1983/4076/plate-05.pdf","linkFileType":{"id":1,"text":"pdf"}},{"id":55442,"rank":405,"type":{"id":17,"text":"Plate"},"url":"https://pubs.usgs.gov/wri/1983/4076/plate-06.pdf","linkFileType":{"id":1,"text":"pdf"}},{"id":55443,"rank":406,"type":{"id":17,"text":"Plate"},"url":"https://pubs.usgs.gov/wri/1983/4076/plate-07.pdf","linkFileType":{"id":1,"text":"pdf"}},{"id":55444,"rank":407,"type":{"id":17,"text":"Plate"},"url":"https://pubs.usgs.gov/wri/1983/4076/plate-08.pdf","linkFileType":{"id":1,"text":"pdf"}},{"id":55445,"rank":408,"type":{"id":17,"text":"Plate"},"url":"https://pubs.usgs.gov/wri/1983/4076/plate-09.pdf","linkFileType":{"id":1,"text":"pdf"}},{"id":55446,"rank":409,"type":{"id":17,"text":"Plate"},"url":"https://pubs.usgs.gov/wri/1983/4076/plate-10.pdf","linkFileType":{"id":1,"text":"pdf"}},{"id":55447,"rank":410,"type":{"id":17,"text":"Plate"},"url":"https://pubs.usgs.gov/wri/1983/4076/plate-11.pdf","linkFileType":{"id":1,"text":"pdf"}},{"id":55448,"rank":411,"type":{"id":17,"text":"Plate"},"url":"https://pubs.usgs.gov/wri/1983/4076/plate-12.pdf","linkFileType":{"id":1,"text":"pdf"}},{"id":55449,"rank":412,"type":{"id":17,"text":"Plate"},"url":"https://pubs.usgs.gov/wri/1983/4076/plate-13.pdf","linkFileType":{"id":1,"text":"pdf"}},{"id":55450,"rank":300,"type":{"id":11,"text":"Document"},"url":"https://pubs.usgs.gov/wri/1983/4076/report.pdf","linkFileType":{"id":1,"text":"pdf"}},{"id":55437,"rank":400,"type":{"id":17,"text":"Plate"},"url":"https://pubs.usgs.gov/wri/1983/4076/plate-01.pdf","linkFileType":{"id":1,"text":"pdf"}},{"id":55438,"rank":401,"type":{"id":17,"text":"Plate"},"url":"https://pubs.usgs.gov/wri/1983/4076/plate-02.pdf","linkFileType":{"id":1,"text":"pdf"}}],"noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"4f4e4afce4b07f02db696831","contributors":{"authors":[{"text":"Christenson, S. C.","contributorId":98320,"corporation":false,"usgs":true,"family":"Christenson","given":"S.","email":"","middleInitial":"C.","affiliations":[],"preferred":false,"id":196644,"contributorType":{"id":1,"text":"Authors"},"rank":1}]}}
,{"id":4239,"text":"cir892 - 1983 - Assessment of low-temperature geothermal resources of the United States; 1982","interactions":[],"lastModifiedDate":"2018-10-22T20:03:36","indexId":"cir892","displayToPublicDate":"1994-01-01T00:00:00","publicationYear":"1983","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":"892","title":"Assessment of low-temperature geothermal resources of the United States; 1982","language":"ENGLISH","publisher":"U.S. Geological Survey,","doi":"10.3133/cir892","usgsCitation":"1983, Assessment of low-temperature geothermal resources of the United States; 1982: U.S. Geological Survey Circular 892, v, 73 p. :ill. ;27 cm., https://doi.org/10.3133/cir892.","productDescription":"v, 73 p. :ill. ;27 cm.","costCenters":[],"links":[{"id":31353,"rank":300,"type":{"id":11,"text":"Document"},"url":"https://pubs.usgs.gov/circ/1983/0892/report.pdf","linkFileType":{"id":1,"text":"pdf"}},{"id":117903,"rank":0,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/circ/1983/0892/report-thumb.jpg"}],"noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"4f4e4abae4b07f02db671f22","contributors":{"editors":[{"text":"Reed, Marshall J.","contributorId":81479,"corporation":false,"usgs":true,"family":"Reed","given":"Marshall J.","affiliations":[],"preferred":false,"id":749350,"contributorType":{"id":2,"text":"Editors"},"rank":1}]}}
,{"id":28002,"text":"wri834170 - 1983 - Reconnaissance of surface-water resources in the Togiak River basin, southwestern Alaska, 1980 and 1982","interactions":[],"lastModifiedDate":"2012-02-02T00:08:40","indexId":"wri834170","displayToPublicDate":"1994-01-01T00:00:00","publicationYear":"1983","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":"83-4170","title":"Reconnaissance of surface-water resources in the Togiak River basin, southwestern Alaska, 1980 and 1982","docAbstract":"Data collected during August and September 1980 and March 1982 describe hydrologic characteristics of the Togiak River and its tributaries. Surface waters are generally cold and clear, have significant wilderness recreation values, and provide outstanding salmon habitat. Late summer unit runoff ranged from 2.3 to 8.1 cubic feet per second per square mile. Stream width increased with discharge from about 20 feet on the tributaries to more than 300 feet on the Togiak River near its mouth. Mean depth increased with discharge downstream direction from about 1 to more than 4 feet. Mean velocity ranged between 1 and 4 feet per second and bore little relation to discharge. Late winter unit discharge for sites having little or no upstream lake storage was about 0.5 cubic foot per second per square mile. For the remaining sites, values ranged from 0.8 to 1.4 cubic feet per second per square mile. Unit runoff of maximum evident floods ranged from 12.9 to 50 cubic feet per second per square mile. Field measurements of water temperature, dissolved oxygen, pH, alkalinity and specific conductance indicated that water quality seems much the same throughout the basin and is influenced by the major lakes. Benthic invertebrates indicate a reasonably diverse fauna with midge larvae representing the largest percentage of all organisms found at most sites. (USGS)","language":"ENGLISH","publisher":"U.S. Geological Survey,","doi":"10.3133/wri834170","usgsCitation":"Kernodle, D., Squires, R., and Childers, J., 1983, Reconnaissance of surface-water resources in the Togiak River basin, southwestern Alaska, 1980 and 1982: U.S. Geological Survey Water-Resources Investigations Report 83-4170, iv, 28 p. :ill., maps ;28 cm., https://doi.org/10.3133/wri834170.","productDescription":"iv, 28 p. :ill., maps ;28 cm.","costCenters":[],"links":[{"id":158678,"rank":0,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/wri/1983/4170/report-thumb.jpg"},{"id":56829,"rank":300,"type":{"id":11,"text":"Document"},"url":"https://pubs.usgs.gov/wri/1983/4170/report.pdf","linkFileType":{"id":1,"text":"pdf"}}],"noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"4f4e4a4ae4b07f02db624e40","contributors":{"authors":[{"text":"Kernodle, D.R.","contributorId":26691,"corporation":false,"usgs":true,"family":"Kernodle","given":"D.R.","email":"","affiliations":[],"preferred":false,"id":199048,"contributorType":{"id":1,"text":"Authors"},"rank":1},{"text":"Squires, R.R.","contributorId":85227,"corporation":false,"usgs":true,"family":"Squires","given":"R.R.","email":"","affiliations":[],"preferred":false,"id":199050,"contributorType":{"id":1,"text":"Authors"},"rank":2},{"text":"Childers, J.M.","contributorId":41455,"corporation":false,"usgs":true,"family":"Childers","given":"J.M.","email":"","affiliations":[],"preferred":false,"id":199049,"contributorType":{"id":1,"text":"Authors"},"rank":3}]}}
,{"id":27998,"text":"wri834007 - 1983 - Application of remote-sensing techniques to hydrologic studies in selected coal-mined areas of southeastern Kansas","interactions":[],"lastModifiedDate":"2022-01-10T20:04:36.318938","indexId":"wri834007","displayToPublicDate":"1994-01-01T00:00:00","publicationYear":"1983","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":"83-4007","title":"Application of remote-sensing techniques to hydrologic studies in selected coal-mined areas of southeastern Kansas","docAbstract":"<p>Disturbances resulting from intensive coal mining in the Cherry Creek basin of southeastern Kansas were investigated using color and color-infrared aerial photography in conjunction with water-quality data from simultaneously acquired samples. Imagery was used to identify the type and extent of vegetative cover on strip-mined lands and the extent and success of reclamation practices. Drainage patterns, point sources of acid mine drainage, and recharge areas for underground mines were located for onsite inspection. Comparison of these interpretations with water-quality data illustrated differences between the eastern and western parts of the Cherry Creek basin. Contamination in the eastern part is due largely to circulation of water from unreclaimed strip mines and collapse features through the network of underground mines and subsequent discharge of acidic drainage through seeps. Contamination in the western part is primarily caused by runoff and seepage from strip-mined lands in which surfaces have frequently been graded and limed but are generally devoid of mature stands of soil-anchoring vegetation. The successful use of aerial photography in the study of Cherry Creek basin indicates the potential of using remote-sensing techniques in studies of other coal-mined regions.&nbsp;</p>","language":"English","publisher":"U.S. Geological Survey","doi":"10.3133/wri834007","usgsCitation":"Kenny, J.F., and McCauley, J.R., 1983, Application of remote-sensing techniques to hydrologic studies in selected coal-mined areas of southeastern Kansas: U.S. Geological Survey Water-Resources Investigations Report 83-4007, Report: iv, 33 p.; 1 Plate: 16.01 × 18.60 inches, https://doi.org/10.3133/wri834007.","productDescription":"Report: iv, 33 p.; 1 Plate: 16.01 × 18.60 inches","costCenters":[],"links":[{"id":56824,"rank":400,"type":{"id":17,"text":"Plate"},"url":"https://pubs.usgs.gov/wri/1983/4007/plate-1.pdf","linkFileType":{"id":1,"text":"pdf"}},{"id":394124,"rank":4,"type":{"id":36,"text":"NGMDB Index Page"},"url":"https://ngmdb.usgs.gov/Prodesc/proddesc_35653.htm"},{"id":56825,"rank":300,"type":{"id":11,"text":"Document"},"url":"https://pubs.usgs.gov/wri/1983/4007/report.pdf","linkFileType":{"id":1,"text":"pdf"}},{"id":123358,"rank":0,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/wri/1983/4007/report-thumb.jpg"}],"country":"United States","state":"Kansas","geographicExtents":"{\n  \"type\": \"FeatureCollection\",\n  \"features\": [\n    {\n      \"type\": \"Feature\",\n      \"properties\": {},\n      \"geometry\": {\n        \"type\": \"Polygon\",\n        \"coordinates\": [\n          [\n            [\n              -94.9720,\n              37.158\n            ],\n            [\n              -94.5730,\n              37.158\n            ],\n            [\n              -94.5730,\n              37.333\n            ],\n            [\n              -94.9720,\n              37.333\n            ],\n            [\n              -94.9720,\n              37.158\n            ]\n          ]\n        ]\n      }\n    }\n  ]\n}","noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"4f4e4ac6e4b07f02db67a8ad","contributors":{"authors":[{"text":"Kenny, J. F.","contributorId":100378,"corporation":false,"usgs":true,"family":"Kenny","given":"J.","email":"","middleInitial":"F.","affiliations":[],"preferred":false,"id":199040,"contributorType":{"id":1,"text":"Authors"},"rank":1},{"text":"McCauley, J. R.","contributorId":97533,"corporation":false,"usgs":true,"family":"McCauley","given":"J.","email":"","middleInitial":"R.","affiliations":[],"preferred":false,"id":199039,"contributorType":{"id":1,"text":"Authors"},"rank":2}]}}
,{"id":66923,"text":"i1455 - 1983 - Geologic map of the Guthrie Quadrangle, Graham and Greenlee counties, Arizona","interactions":[],"lastModifiedDate":"2012-02-10T00:11:14","indexId":"i1455","displayToPublicDate":"1994-01-01T00:00:00","publicationYear":"1983","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":"1455","subseriesTitle":"NONE","title":"Geologic map of the Guthrie Quadrangle, Graham and Greenlee counties, Arizona","language":"ENGLISH","doi":"10.3133/i1455","usgsCitation":"Richter, D., Houser, B.B., and Damon, P., 1983, Geologic map of the Guthrie Quadrangle, Graham and Greenlee counties, Arizona: U.S. Geological Survey IMAP 1455, 1 map :col. ;58 x 49 cm. on sheet 85 x 109 cm. folded in envelope 30 x 24 cm., https://doi.org/10.3133/i1455.","productDescription":"1 map :col. ;58 x 49 cm. on sheet 85 x 109 cm. folded in envelope 30 x 24 cm.","costCenters":[],"links":[{"id":106761,"rank":700,"type":{"id":15,"text":"Index Page"},"url":"https://ngmdb.usgs.gov/Prodesc/proddesc_9249.htm","linkFileType":{"id":5,"text":"html"},"description":"9249"},{"id":189100,"rank":0,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/thumbnails/usgs_thumb.jpg"}],"scale":"48000","geographicExtents":"{ \"type\": \"FeatureCollection\", \"features\": [ { \"type\": \"Feature\", \"properties\": {}, \"geometry\": { \"type\": \"Polygon\", \"coordinates\": [ [ [ -109.5,32.75 ], [ -109.5,33 ], [ -109.25,33 ], [ -109.25,32.75 ], [ -109.5,32.75 ] ] ] } } ] }","noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"4f4e4a61e4b07f02db635bf2","contributors":{"authors":[{"text":"Richter, D.H.","contributorId":43325,"corporation":false,"usgs":true,"family":"Richter","given":"D.H.","email":"","affiliations":[{"id":595,"text":"U.S. Geological Survey","active":false,"usgs":true}],"preferred":false,"id":275294,"contributorType":{"id":1,"text":"Authors"},"rank":1},{"text":"Houser, B. B.","contributorId":46092,"corporation":false,"usgs":true,"family":"Houser","given":"B.","email":"","middleInitial":"B.","affiliations":[],"preferred":false,"id":275295,"contributorType":{"id":1,"text":"Authors"},"rank":2},{"text":"Damon, P.E.","contributorId":89610,"corporation":false,"usgs":true,"family":"Damon","given":"P.E.","email":"","affiliations":[],"preferred":false,"id":275296,"contributorType":{"id":1,"text":"Authors"},"rank":3}]}}
,{"id":27631,"text":"wri834123 - 1983 - Estimating 1980 ground-water pumpage for irrigation on the High Plains in parts of Colorado, Kansas, Nebraska, New Mexico, Oklahoma, South Dakota, Texas, and Wyoming","interactions":[],"lastModifiedDate":"2017-09-20T16:58:30","indexId":"wri834123","displayToPublicDate":"1994-01-01T00:00:00","publicationYear":"1983","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":"83-4123","title":"Estimating 1980 ground-water pumpage for irrigation on the High Plains in parts of Colorado, Kansas, Nebraska, New Mexico, Oklahoma, South Dakota, Texas, and Wyoming","docAbstract":"Current ground-water use is required for the High Plains Regional Aquifer-System Analysis. In response to this need, a sampling approach was developed to estimate water pumped for irrigation on the High Plains during 1980. Pumpage was computed by combining application estimates with mapped irrigated-acreage information. Irrigation application (inches of water applied) was measured at 480 sites in 15 counties in the High Plains during the 1980 growing season. The relationship between calculated Blaney-Criddle irrigation demand and measured application was used to estimate application for unsampled areas of the High Plains. Application estimates multiplied by irrigated-acreate estimates, compiled from Landsat-satellite imagery, yielded the volume of ground water pumped for irrigation. The estimate of ground water pumped for irrigation in the High Plains during 1980 and 18,902,000 acre-feet for 13 ,715,000 irrigated areas. The sampled application data were evaluated for significant trends. The application was greater for crops requiring more water such as corn and hay and less for crops such as sorghum, grain, and cotton. The data showed greater application for flood-irrigated systems than for sprinkler-irrigation systems. Areas of the High Plains with thin saturated thickness tended to have a smaller average discharge per well, fewer irrigated acres per well, and a predominance of crops requiring less water crops. (USGS).","language":"ENGLISH","publisher":"U.S. Geological Survey,","doi":"10.3133/wri834123","usgsCitation":"Heimes, F., and Luckey, R.R., 1983, Estimating 1980 ground-water pumpage for irrigation on the High Plains in parts of Colorado, Kansas, Nebraska, New Mexico, Oklahoma, South Dakota, Texas, and Wyoming: U.S. Geological Survey Water-Resources Investigations Report 83-4123, iv, 40 p. :ill., maps ;28 cm., https://doi.org/10.3133/wri834123.","productDescription":"iv, 40 p. :ill., maps ;28 cm.","costCenters":[{"id":5050,"text":"WY-MT Water Science Center","active":true,"usgs":true}],"links":[{"id":56497,"rank":300,"type":{"id":11,"text":"Document"},"url":"https://pubs.usgs.gov/wri/1983/4123/report.pdf","linkFileType":{"id":1,"text":"pdf"}},{"id":123364,"rank":0,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/wri/1983/4123/report-thumb.jpg"}],"noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"4f4e4abbe4b07f02db6727f3","contributors":{"authors":[{"text":"Heimes, F.J.","contributorId":60654,"corporation":false,"usgs":true,"family":"Heimes","given":"F.J.","affiliations":[],"preferred":false,"id":198443,"contributorType":{"id":1,"text":"Authors"},"rank":1},{"text":"Luckey, R. R.","contributorId":93055,"corporation":false,"usgs":true,"family":"Luckey","given":"R.","email":"","middleInitial":"R.","affiliations":[],"preferred":false,"id":198444,"contributorType":{"id":1,"text":"Authors"},"rank":2}]}}
,{"id":28428,"text":"wri834221 - 1983 - A method for estimating ground-water return flow to the lower Colorado River in the Yuma area, Arizona and California — Executive summary","interactions":[],"lastModifiedDate":"2022-01-21T19:34:33.304148","indexId":"wri834221","displayToPublicDate":"1994-01-01T00:00:00","publicationYear":"1983","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":"83-4221","title":"A method for estimating ground-water return flow to the lower Colorado River in the Yuma area, Arizona and California — Executive summary","docAbstract":"<p>No abstract available.</p>","language":"English","publisher":"U.S. Geological Survey","doi":"10.3133/wri834221","usgsCitation":"Loeltz, O.J., and Leake, S.A., 1983, A method for estimating ground-water return flow to the lower Colorado River in the Yuma area, Arizona and California — Executive summary: U.S. Geological Survey Water-Resources Investigations Report 83-4221, vi, 13 p., https://doi.org/10.3133/wri834221.","productDescription":"vi, 13 p.","costCenters":[],"links":[{"id":57231,"rank":300,"type":{"id":11,"text":"Document"},"url":"https://pubs.usgs.gov/wri/1983/4221/report.pdf","linkFileType":{"id":1,"text":"pdf"}},{"id":121728,"rank":0,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/wri/1983/4221/report-thumb.jpg"},{"id":394681,"rank":3,"type":{"id":36,"text":"NGMDB Index Page"},"url":"https://ngmdb.usgs.gov/Prodesc/proddesc_35862.htm"}],"country":"United States","state":"Arizona, California","city":"Yuma","otherGeospatial":"Colorado River","geographicExtents":"{\n  \"type\": \"FeatureCollection\",\n  \"features\": [\n    {\n      \"type\": \"Feature\",\n      \"properties\": {},\n      \"geometry\": {\n        \"type\": \"Polygon\",\n        \"coordinates\": [\n          [\n            [\n              -114.7412109375,\n              32.65325087996883\n            ],\n            [\n              -114.4830322265625,\n              32.65325087996883\n            ],\n            [\n              -114.4830322265625,\n              32.82421110161336\n            ],\n            [\n              -114.7412109375,\n              32.82421110161336\n            ],\n            [\n              -114.7412109375,\n              32.65325087996883\n            ]\n          ]\n        ]\n      }\n    }\n  ]\n}","noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"4f4e4b23e4b07f02db6ae0ef","contributors":{"authors":[{"text":"Loeltz, Omar J.","contributorId":86312,"corporation":false,"usgs":true,"family":"Loeltz","given":"Omar","email":"","middleInitial":"J.","affiliations":[],"preferred":false,"id":199779,"contributorType":{"id":1,"text":"Authors"},"rank":1},{"text":"Leake, S. A.","contributorId":52164,"corporation":false,"usgs":true,"family":"Leake","given":"S.","email":"","middleInitial":"A.","affiliations":[],"preferred":false,"id":199778,"contributorType":{"id":1,"text":"Authors"},"rank":2}]}}
,{"id":3695,"text":"cir866 - 1983 - Geothermal resources of southern Idaho","interactions":[],"lastModifiedDate":"2012-02-02T00:05:32","indexId":"cir866","displayToPublicDate":"1994-01-01T00:00:00","publicationYear":"1983","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":"866","title":"Geothermal resources of southern Idaho","docAbstract":"The geothermal resource of southern Idaho as assessed by the U.S. Geological Survey in 1978 is large. Most of the known hydrothermal systems in southern Idaho have calculated reservoir temperatures of less than 150?C. Water from many of these systems is valuable for direct heat applications, but is lower than the temperature of interest for commercial generation of electricity at the present time. Most of the known and inferred geothermal resources of southern Idaho underlie the Snake River Plain. However, major uncertainties exist concerning the geology and temperatures beneath the plain. By far the largest hydrothermal system in Idaho is in the Bruneau-Grand View area of the western Snake River Plain with a calculated reservoir temperature of 107?C and an energy of 4.5? 10 20 joules. No evidence of higher temperature water associated with this system has been found. Although the geology of the eastern Snake River Plain suggests that a large thermal anomaly may underlie this area of the plain, direct evidence of high temperatures has not been found. Large volumes of water at temperatures between 90? and 150?C probably exist along the margins of the Snake River Plain and in local areas north and south of the plain. Areas that appear particularly promising for the occurrence of large high-temperature hydrothermal systems are: the area north of the Snake River Plain and west of the Idaho batholith, the Island Park area, segments of the margins of the eastern Snake River Plain, and the Blackfoot lava field.","language":"ENGLISH","publisher":"U.S. Geological Survey,","doi":"10.3133/cir866","usgsCitation":"Mabey, D.R., 1983, Geothermal resources of southern Idaho: U.S. Geological Survey Circular 866, iii, 24 p. :ill., maps ;26 cm., https://doi.org/10.3133/cir866.","productDescription":"iii, 24 p. :ill., maps ;26 cm.","costCenters":[],"links":[{"id":124364,"rank":0,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/circ/1983/0866/report-thumb.jpg"},{"id":30747,"rank":300,"type":{"id":11,"text":"Document"},"url":"https://pubs.usgs.gov/circ/1983/0866/report.pdf","linkFileType":{"id":1,"text":"pdf"}}],"noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"4f4e4ad5e4b07f02db683649","contributors":{"authors":[{"text":"Mabey, Don R.","contributorId":43741,"corporation":false,"usgs":true,"family":"Mabey","given":"Don","email":"","middleInitial":"R.","affiliations":[],"preferred":false,"id":147424,"contributorType":{"id":1,"text":"Authors"},"rank":1}]}}
,{"id":27975,"text":"wri8167 - 1983 - An engineering economic analysis of artificial recharge in a conjunctive irrigation plan in the Columbia Basin Project, Washington","interactions":[],"lastModifiedDate":"2019-08-05T11:41:59","indexId":"wri8167","displayToPublicDate":"1994-01-01T00:00:00","publicationYear":"1983","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":"81-67","title":"An engineering economic analysis of artificial recharge in a conjunctive irrigation plan in the Columbia Basin Project, Washington","docAbstract":"<p>No abstract available.&nbsp;</p>","language":"English","publisher":"U.S. Geological Survey","publisherLocation":"Reston, VA","doi":"10.3133/wri8167","usgsCitation":"Karlinger, M., and Hansen, A.J., 1983, An engineering economic analysis of artificial recharge in a conjunctive irrigation plan in the Columbia Basin Project, Washington: U.S. Geological Survey Water-Resources Investigations Report 81-67, iv, 28 p. , https://doi.org/10.3133/wri8167.","productDescription":"iv, 28 p. ","costCenters":[],"links":[{"id":366257,"rank":2,"type":{"id":11,"text":"Document"},"url":"https://pubs.usgs.gov/wri/1981/0067/report.pdf","linkFileType":{"id":1,"text":"pdf"}},{"id":159024,"rank":0,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/wri/1981/0067/report-thumb.jpg"}],"country":"United States","state":"Washington","otherGeospatial":"Columbia Basin Project","geographicExtents":"{\n  \"type\": \"FeatureCollection\",\n  \"features\": [\n    {\n      \"type\": \"Feature\",\n      \"properties\": {},\n      \"geometry\": {\n        \"type\": \"Polygon\",\n        \"coordinates\": [\n          [\n            [\n              -120.10253906249999,\n              46.15700496290803\n            ],\n            [\n              -117.1142578125,\n              46.15700496290803\n            ],\n            [\n              -117.1142578125,\n              47.945786463687185\n            ],\n            [\n              -120.10253906249999,\n              47.945786463687185\n            ],\n            [\n              -120.10253906249999,\n              46.15700496290803\n            ]\n          ]\n        ]\n      }\n    }\n  ]\n}","noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"4f4e4ad8e4b07f02db684aa0","contributors":{"authors":[{"text":"Karlinger, M.R.","contributorId":95039,"corporation":false,"usgs":true,"family":"Karlinger","given":"M.R.","affiliations":[],"preferred":false,"id":198995,"contributorType":{"id":1,"text":"Authors"},"rank":1},{"text":"Hansen, Arnold J. Jr.","contributorId":84336,"corporation":false,"usgs":true,"family":"Hansen","given":"Arnold","suffix":"Jr.","email":"","middleInitial":"J.","affiliations":[],"preferred":false,"id":198994,"contributorType":{"id":1,"text":"Authors"},"rank":2}]}}
,{"id":27762,"text":"wri834033 - 1983 - Ground-water-use trends in the Twin Cities metropolitan area, Minnesota, 1880-1980","interactions":[],"lastModifiedDate":"2018-03-12T12:01:11","indexId":"wri834033","displayToPublicDate":"1994-01-01T00:00:00","publicationYear":"1983","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":"83-4033","title":"Ground-water-use trends in the Twin Cities metropolitan area, Minnesota, 1880-1980","docAbstract":"<p>Detailed ground-water-use information from 1880 to 1980 has been collected and analyzed for the Twin Cities metropolitan area. Interpretation of historic water-use data was required to help water-resource planners and managers assess future trends in water use. Data were also needed for three computer-simulation models of ground-water flow being developed in the Twin Cities area. Methods were developed to collect, evaluate, store, and retrieve information from all local, State, and Federal agencies1 records and publications. A computerized water-use data base was constructed to facilitate generation of statistics on water-use trends and to store and retrieve data for the flow models.</p>\n<p>Ground-water use was analyzed by use category and aquifer and several trends were observed. Eighty percent of ground water currently withdrawn is from wells in the Prairie du Chien-Jordan aquifer. Ground-water use increased from 1880 until the early 1970's, and then declined slightly in the late 1970's. Industrial use in particular declined during the 1970's as a result of conservation that was prompted by increased sewagetreatment and energy costs. The intensity of pumping has decreased within the St. Paul and Minneapolis city limits and increased outside the city limits. The seasonal variability of ground-water use became more pronounced as the percentage of water used for irrigation and air conditioning increased.</p>","language":"English","publisher":"U.S. Geological Survey","publisherLocation":"St. Paul, MN","doi":"10.3133/wri834033","collaboration":"Prepared in cooperation with the Metropolitan Council of the Twin Cities and the Minnesota Department of Natural Resources","usgsCitation":"Horn, M., 1983, Ground-water-use trends in the Twin Cities metropolitan area, Minnesota, 1880-1980: U.S. Geological Survey Water-Resources Investigations Report 83-4033, iv, 37 p., https://doi.org/10.3133/wri834033.","productDescription":"iv, 37 p.","onlineOnly":"N","additionalOnlineFiles":"N","costCenters":[{"id":392,"text":"Minnesota Water Science Center","active":true,"usgs":true}],"links":[{"id":56610,"rank":300,"type":{"id":11,"text":"Document"},"url":"https://pubs.usgs.gov/wri/1983/4033/report.pdf","linkFileType":{"id":1,"text":"pdf"}},{"id":123357,"rank":0,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/wri/1983/4033/report-thumb.jpg"}],"country":"United States","state":"Minneosta","otherGeospatial":"Twin Cities Metropolitan 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{\"name\":\"Anoka\",\"state\":\"MN\"}}]}","noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"4f4e4a96e4b07f02db65a281","contributors":{"authors":[{"text":"Horn, M.A.","contributorId":92223,"corporation":false,"usgs":true,"family":"Horn","given":"M.A.","email":"","affiliations":[],"preferred":false,"id":198655,"contributorType":{"id":1,"text":"Authors"},"rank":1}]}}
,{"id":3733,"text":"cir876 - 1983 - Subsidence from underground mining; environmental analysis and planning considerations","interactions":[],"lastModifiedDate":"2012-02-02T00:05:38","indexId":"cir876","displayToPublicDate":"1994-01-01T00:00:00","publicationYear":"1983","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":"876","title":"Subsidence from underground mining; environmental analysis and planning considerations","docAbstract":"Subsidence, a universal process that occurs in response to the voids created by extracting solids or liquids from beneath the Earth's surface, is controlled by many factors including mining methods, depth of extraction, thickness of deposit, and topography, as well as the in situ properties of the rock mass above the deposit. The impacts of subsidence are potentially severe in terms of damage to surface utility lines and structures, changes in surface-water and ground-water conditions, and effects on vegetation and animals. Although subsidence cannot be eliminated, it can be reduced or controlled in areas where deformation of the ground surface would produce dangerous or costly effects. \r\n\r\nSubsidence prediction is highly developed in Europe where there are comparatively uniform mining conditions and a long history of field measurements. Much of this mining has been carried out beneath crowded urban and industrial areas where accurate predictions have facilitated use of the surface and reduced undesirable impacts. Concerted efforts to understand subsidence processes in the United States are recent. Empirical methods of subsidence analysis and prediction based on local conditions seem better suited to the current state of knowledge of the varied geologic and topographic conditions in domestic coal mining regions than do theoretical/mathematical approaches. In order to develop broadly applicable subsidence prediction methods and models for the United States, more information is needed on magnitude and timing of ground movements and geologic properties.","language":"ENGLISH","publisher":"U.S. Geological Survey,","doi":"10.3133/cir876","usgsCitation":"Lee, F.T., and Abel, J., 1983, Subsidence from underground mining; environmental analysis and planning considerations: U.S. Geological Survey Circular 876, iv, 28 p. :ill., maps ;26 cm., https://doi.org/10.3133/cir876.","productDescription":"iv, 28 p. :ill., maps ;26 cm.","costCenters":[],"links":[{"id":124669,"rank":0,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/circ/1983/0876/report-thumb.jpg"},{"id":30794,"rank":300,"type":{"id":11,"text":"Document"},"url":"https://pubs.usgs.gov/circ/1983/0876/report.pdf","linkFileType":{"id":1,"text":"pdf"}}],"noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"4f4e4b05e4b07f02db699ae9","contributors":{"authors":[{"text":"Lee, Fitzhugh T.","contributorId":82272,"corporation":false,"usgs":true,"family":"Lee","given":"Fitzhugh","email":"","middleInitial":"T.","affiliations":[],"preferred":false,"id":147500,"contributorType":{"id":1,"text":"Authors"},"rank":1},{"text":"Abel, John F.","contributorId":84351,"corporation":false,"usgs":true,"family":"Abel","given":"John F.","affiliations":[],"preferred":false,"id":147501,"contributorType":{"id":1,"text":"Authors"},"rank":2}]}}
,{"id":37731,"text":"wl515 - 1983 - Senegal's trade in cage birds, 1979-81","interactions":[],"lastModifiedDate":"2012-02-02T00:10:01","indexId":"wl515","displayToPublicDate":"1994-01-01T00:00:00","publicationYear":"1983","noYear":false,"publicationType":{"id":18,"text":"Report"},"publicationSubtype":{"id":1,"text":"Federal Government Series"},"seriesTitle":{"id":98,"text":"Wildlife Leaflet","active":false,"publicationSubtype":{"id":1}},"seriesNumber":"515","title":"Senegal's trade in cage birds, 1979-81","language":"ENGLISH","publisher":"U.S. Fish and Wildlife Service","usgsCitation":"Ruelle, P., and Bruggers, R.L., 1983, Senegal's trade in cage birds, 1979-81: Wildlife Leaflet 515, 11 p. : ill. ; 27 cm.","productDescription":"11 p. : ill. ; 27 cm.","costCenters":[],"links":[{"id":161853,"rank":0,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/thumbnails/outside_thumb.jpg"}],"noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"4f4e49ffe4b07f02db5f7916","contributors":{"authors":[{"text":"Ruelle, Philippe","contributorId":83797,"corporation":false,"usgs":true,"family":"Ruelle","given":"Philippe","email":"","affiliations":[],"preferred":false,"id":218516,"contributorType":{"id":1,"text":"Authors"},"rank":1},{"text":"Bruggers, Richard L.","contributorId":9125,"corporation":false,"usgs":true,"family":"Bruggers","given":"Richard","email":"","middleInitial":"L.","affiliations":[],"preferred":false,"id":218515,"contributorType":{"id":1,"text":"Authors"},"rank":2}]}}
,{"id":9228,"text":"ofr83448 - 1983 - Reconnaissance geology of the Thaniyah Quadrangle, sheet 20/42 C, Kingdom of Saudi Arabia","interactions":[],"lastModifiedDate":"2012-02-02T00:06:18","indexId":"ofr83448","displayToPublicDate":"1994-01-01T00:00:00","publicationYear":"1983","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":"83-448","title":"Reconnaissance geology of the Thaniyah Quadrangle, sheet 20/42 C, Kingdom of Saudi Arabia","docAbstract":"The Thaniyah quadrangle, sheet 20/42 C, is located in the transition zone between the Hijaz Mountains and the Najd Plateau of southwestern Saudi Arabia between lat 20?00' and 20?30' N., long 42?00' to 42?30' E. The quadrangle is underlain by Precambrian metavolcanic, metasedimentary, plutonic, and dike rocks. Metavolcanic rocks consist of metamorphosed basalt and andesite with minor dacite and rhyolite and underlie three discontinuous northwest-trending belts. Metasedimentary rocks are confined to small areas underlain by quartzite, metasandstone, marble, and calc-silicate rock. \r\n\r\nPlutonic rocks include an extensive unit of tonalite and quartz diorite and a smaller unit of diorite and quartz diorite, which occupy much of the central part of the quadrangle. A small body of diorite and gabbro and a two-part zone of tonalite gneiss are also present. All of these plutonic rocks are assigned to the An Nimas batholith. \r\n\r\nYounger plutonic rocks include extensive graphic granite and rhyolite in the northeastern part of the quadrangle and several smaller bodies of granitic rocks and of gabbro. \r\n\r\nThe metavolcanic rocks commonly have strong foliation with northwest strike and steep to vertical dip. Diorite and quartz diorite are sheared and brecciated and apparently syntectonic. Tonalite and quartz diorite are both foliate and nonfoliate and were intruded in episodes both preceding and following shearing. The granitic rocks and gabbro are post-tectonic. \r\n\r\nTrends of faults and dikes are mostly related to the Najd faulting episode. \r\n\r\nRadiometric ages, mostly from adjacent quadrangles, suggest that the An Nimas batholith is 835 to 800 Ma, gabbro and granite, except the graphic granite and rhyolite unit, are about 640 to 615 Ma, and the graphic granite and rhyolite 575 to 565 Ma old.\r\n\r\nMetavolcanic rocks similar to those hosting copper and gold mineralization in the Wadi Shuwas mining district adjacent to the southwestern part of the quadrangle are abundant. An ancient copper mine was discovered at the edge of the tonalite gneiss belt east of Wadi Ranyah. Granite and gabbro have economic potential as building stone.","language":"ENGLISH","publisher":"U.S. Geological Survey,","doi":"10.3133/ofr83448","usgsCitation":"Greene, R.C., 1983, Reconnaissance geology of the Thaniyah Quadrangle, sheet 20/42 C, Kingdom of Saudi Arabia: U.S. Geological Survey Open-File Report 83-448, ii, 25 p., 1 over-size sheet, maps ;28 cm., https://doi.org/10.3133/ofr83448.","productDescription":"ii, 25 p., 1 over-size sheet, maps ;28 cm.","costCenters":[],"links":[{"id":142875,"rank":0,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/of/1983/0448/report-thumb.jpg"},{"id":36865,"rank":400,"type":{"id":17,"text":"Plate"},"url":"https://pubs.usgs.gov/of/1983/0448/plate-1.pdf","linkFileType":{"id":1,"text":"pdf"}},{"id":36866,"rank":300,"type":{"id":11,"text":"Document"},"url":"https://pubs.usgs.gov/of/1983/0448/report.pdf","linkFileType":{"id":1,"text":"pdf"}}],"noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"4f4e4a6ce4b07f02db63ec01","contributors":{"authors":[{"text":"Greene, Robert C.","contributorId":36108,"corporation":false,"usgs":true,"family":"Greene","given":"Robert","email":"","middleInitial":"C.","affiliations":[],"preferred":false,"id":159319,"contributorType":{"id":1,"text":"Authors"},"rank":1}]}}
,{"id":3346,"text":"cir911 - 1983 - U.S. Geological Survey Polar research symposium; abstracts with program","interactions":[],"lastModifiedDate":"2012-02-02T00:05:37","indexId":"cir911","displayToPublicDate":"1994-01-01T00:00:00","publicationYear":"1983","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":"911","title":"U.S. Geological Survey Polar research symposium; abstracts with program","language":"ENGLISH","publisher":"U.S. Geological Survey,","doi":"10.3133/cir911","usgsCitation":"Water Resources Division, U.S. Geological Survey, 1983, U.S. Geological Survey Polar research symposium; abstracts with program: U.S. Geological Survey Circular 911, v, 55 p. :ill., maps ;27 cm., https://doi.org/10.3133/cir911.","productDescription":"v, 55 p. :ill., maps ;27 cm.","costCenters":[],"links":[{"id":118127,"rank":0,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/circ/1983/0911/report-thumb.jpg"},{"id":30355,"rank":300,"type":{"id":11,"text":"Document"},"url":"https://pubs.usgs.gov/circ/1983/0911/report.pdf","linkFileType":{"id":1,"text":"pdf"}}],"noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"4f4e4a2be4b07f02db61302e","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":528121,"contributorType":{"id":1,"text":"Authors"},"rank":1}]}}
,{"id":28554,"text":"wri834043 - 1983 - Streamflow losses and changes in ground-water levels along the Salt and Gila Rivers near Phoenix, Arizona — February 1978 to June 1980","interactions":[],"lastModifiedDate":"2021-12-14T20:52:13.450069","indexId":"wri834043","displayToPublicDate":"1994-01-01T00:00:00","publicationYear":"1983","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":"83-4043","title":"Streamflow losses and changes in ground-water levels along the Salt and Gila Rivers near Phoenix, Arizona — February 1978 to June 1980","docAbstract":"From March 1978 to June 1980, high runoff from the Salt and Verde drainage basins combined with large carryover storage in a reservoir system led to the release of about 8.26 million acre-feet of water. About 2.89 million acre-feet of the water was diverted above Granite Reef Dam, and about 5.45 million acre-feet was released into the normally dry channel of the Salt River. The total streamflow losses in the 74-mile reach between Granite Reef and Gillespie Dams were at least 474,000 acre-feet. Most of the water infiltrated into the permeable alluvial deposits along the Sal and Gila Rivers and increased the amount of ground water in storage. From February 1978 to May 1980, ground-water levels in 169 wells that tap the alluvial deposits in the Salt River Valley rose an average of 35.5 feet. The rise in ground-water levels was a direct result of the infiltrating floodwaters and a marked decrease in ground-water pumpage. (USGS)","language":"English","publisher":"U.S. Geological Survey","doi":"10.3133/wri834043","usgsCitation":"Mann, L., and Rohne, P., 1983, Streamflow losses and changes in ground-water levels along the Salt and Gila Rivers near Phoenix, Arizona — February 1978 to June 1980: U.S. Geological Survey Water-Resources Investigations Report 83-4043, Report: iv, 10 p.; 3 Plates: 22.33 × 15.61 inches or smaller, https://doi.org/10.3133/wri834043.","productDescription":"Report: iv, 10 p.; 3 Plates: 22.33 × 15.61 inches or smaller","costCenters":[],"links":[{"id":57385,"rank":402,"type":{"id":17,"text":"Plate"},"url":"https://pubs.usgs.gov/wri/1983/4043/plate-3.pdf","linkFileType":{"id":1,"text":"pdf"}},{"id":57384,"rank":401,"type":{"id":17,"text":"Plate"},"url":"https://pubs.usgs.gov/wri/1983/4043/plate-2.pdf","linkFileType":{"id":1,"text":"pdf"}},{"id":159198,"rank":0,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/wri/1983/4043/report-thumb.jpg"},{"id":392884,"rank":6,"type":{"id":36,"text":"NGMDB Index Page"},"url":"https://ngmdb.usgs.gov/Prodesc/proddesc_35683.htm"},{"id":57386,"rank":300,"type":{"id":11,"text":"Document"},"url":"https://pubs.usgs.gov/wri/1983/4043/report.pdf","linkFileType":{"id":1,"text":"pdf"}},{"id":57383,"rank":400,"type":{"id":17,"text":"Plate"},"url":"https://pubs.usgs.gov/wri/1983/4043/plate-1.pdf","linkFileType":{"id":1,"text":"pdf"}}],"country":"United States","state":"Arizona","city":"Phoenix","otherGeospatial":"Salt and Gila Rivers","geographicExtents":"{\n  \"type\": \"FeatureCollection\",\n  \"features\": [\n    {\n      \"type\": \"Feature\",\n      \"properties\": {},\n      \"geometry\": {\n        \"type\": \"Polygon\",\n        \"coordinates\": [\n          [\n            [\n              -112.5494384765625,\n              33.211116472416855\n            ],\n            [\n              -111.6815185546875,\n              33.211116472416855\n            ],\n            [\n              -111.6815185546875,\n              33.660353121928814\n            ],\n            [\n              -112.5494384765625,\n              33.660353121928814\n            ],\n            [\n              -112.5494384765625,\n              33.211116472416855\n            ]\n          ]\n        ]\n      }\n    }\n  ]\n}","noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"4f4e4b15e4b07f02db6a4daa","contributors":{"authors":[{"text":"Mann, L. J.","contributorId":39392,"corporation":false,"usgs":true,"family":"Mann","given":"L. J.","affiliations":[],"preferred":false,"id":200017,"contributorType":{"id":1,"text":"Authors"},"rank":1},{"text":"Rohne, P. B.","contributorId":20368,"corporation":false,"usgs":true,"family":"Rohne","given":"P. B.","affiliations":[],"preferred":false,"id":200016,"contributorType":{"id":1,"text":"Authors"},"rank":2}]}}
,{"id":68039,"text":"ha659 - 1983 - Hydraulic characteristics of the principal bedrock aquifers in the Denver Basin, Colorado","interactions":[],"lastModifiedDate":"2012-02-10T00:11:29","indexId":"ha659","displayToPublicDate":"1994-01-01T00:00:00","publicationYear":"1983","noYear":false,"publicationType":{"id":18,"text":"Report"},"publicationSubtype":{"id":5,"text":"USGS Numbered Series"},"seriesTitle":{"id":318,"text":"Hydrologic Atlas","code":"HA","active":false,"publicationSubtype":{"id":5}},"seriesNumber":"659","title":"Hydraulic characteristics of the principal bedrock aquifers in the Denver Basin, Colorado","language":"ENGLISH","doi":"10.3133/ha659","usgsCitation":"Robson, S.G., 1983, Hydraulic characteristics of the principal bedrock aquifers in the Denver Basin, Colorado: U.S. Geological Survey Hydrologic Atlas 659, 12 maps on 3 sheets :col. ;sheets 92 x 87 cm., https://doi.org/10.3133/ha659.","productDescription":"12 maps on 3 sheets :col. ;sheets 92 x 87 cm.","costCenters":[],"links":[{"id":186134,"rank":0,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/thumbnails/usgs_thumb.jpg"},{"id":91827,"rank":401,"type":{"id":17,"text":"Plate"},"url":"https://pubs.usgs.gov/ha/659/plate-1.pdf","linkFileType":{"id":1,"text":"pdf"}},{"id":91828,"rank":402,"type":{"id":17,"text":"Plate"},"url":"https://pubs.usgs.gov/ha/659/plate-2.pdf","linkFileType":{"id":1,"text":"pdf"}},{"id":89294,"rank":402,"type":{"id":17,"text":"Plate"},"url":"https://pubs.usgs.gov/ha/659/plate-3.pdf","linkFileType":{"id":1,"text":"pdf"}}],"scale":"500000","geographicExtents":"{ \"type\": \"FeatureCollection\", \"features\": [ { \"type\": \"Feature\", \"properties\": {}, \"geometry\": { \"type\": \"Polygon\", \"coordinates\": [ [ [ -105,39 ], [ -105,40 ], [ -104,40 ], [ -104,39 ], [ -105,39 ] ] ] } } ] }","noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"4f4e4a51e4b07f02db62a273","contributors":{"authors":[{"text":"Robson, Stanley G.","contributorId":73187,"corporation":false,"usgs":true,"family":"Robson","given":"Stanley","email":"","middleInitial":"G.","affiliations":[],"preferred":false,"id":277549,"contributorType":{"id":1,"text":"Authors"},"rank":1}]}}
,{"id":4834,"text":"pp1067F - 1983 - Postdepositional alteration of surface and near-surface minerals in selected coastal plain formations of the Middle Atlantic States","interactions":[],"lastModifiedDate":"2012-02-02T00:05:52","indexId":"pp1067F","displayToPublicDate":"1994-01-01T00:00:00","publicationYear":"1983","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":"1067","chapter":"F","title":"Postdepositional alteration of surface and near-surface minerals in selected coastal plain formations of the Middle Atlantic States","language":"ENGLISH","publisher":"U.S. G.P.O.,","doi":"10.3133/pp1067F","usgsCitation":"Owens, J.P., Hess, M., Denny, C.S., and Dwornik, E., 1983, Postdepositional alteration of surface and near-surface minerals in selected coastal plain formations of the Middle Atlantic States: U.S. Geological Survey Professional Paper 1067, p. F1-F45, https://doi.org/10.3133/pp1067F.","productDescription":"p. F1-F45","costCenters":[],"links":[{"id":117162,"rank":0,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/pp/1067f/report-thumb.jpg"},{"id":31772,"rank":300,"type":{"id":11,"text":"Document"},"url":"https://pubs.usgs.gov/pp/1067f/report.pdf","linkFileType":{"id":1,"text":"pdf"}}],"noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"4f4e4ad5e4b07f02db683a41","contributors":{"authors":[{"text":"Owens, James Patrick","contributorId":105706,"corporation":false,"usgs":true,"family":"Owens","given":"James","email":"","middleInitial":"Patrick","affiliations":[],"preferred":false,"id":149875,"contributorType":{"id":1,"text":"Authors"},"rank":1},{"text":"Hess, M.M.","contributorId":14812,"corporation":false,"usgs":true,"family":"Hess","given":"M.M.","email":"","affiliations":[],"preferred":false,"id":149872,"contributorType":{"id":1,"text":"Authors"},"rank":2},{"text":"Denny, C. S.","contributorId":87530,"corporation":false,"usgs":true,"family":"Denny","given":"C.","email":"","middleInitial":"S.","affiliations":[],"preferred":false,"id":149873,"contributorType":{"id":1,"text":"Authors"},"rank":3},{"text":"Dwornik, E.J.","contributorId":99128,"corporation":false,"usgs":true,"family":"Dwornik","given":"E.J.","email":"","affiliations":[],"preferred":false,"id":149874,"contributorType":{"id":1,"text":"Authors"},"rank":4}]}}
,{"id":65116,"text":"i1319 - 1983 - Geologic map and sections of the central Pioneer Mountains, Blaine and Custer counties, central Idaho","interactions":[],"lastModifiedDate":"2012-02-10T00:11:08","indexId":"i1319","displayToPublicDate":"1994-01-01T00:00:00","publicationYear":"1983","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":"1319","subseriesTitle":"NONE","title":"Geologic map and sections of the central Pioneer Mountains, Blaine and Custer counties, central Idaho","language":"ENGLISH","doi":"10.3133/i1319","usgsCitation":"Dover, J.H., 1983, Geologic map and sections of the central Pioneer Mountains, Blaine and Custer counties, central Idaho: U.S. Geological Survey IMAP 1319, 1 map :col. ;86 x 63 cm., sheet 104 x 126 cm., folded in envelope 30 x 24 cm., https://doi.org/10.3133/i1319.","productDescription":"1 map :col. ;86 x 63 cm., sheet 104 x 126 cm., folded in envelope 30 x 24 cm.","costCenters":[],"links":[{"id":106694,"rank":700,"type":{"id":15,"text":"Index Page"},"url":"https://ngmdb.usgs.gov/Prodesc/proddesc_9151.htm","linkFileType":{"id":5,"text":"html"},"description":"9151"},{"id":189745,"rank":0,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/thumbnails/usgs_thumb.jpg"}],"scale":"48000","geographicExtents":"{ \"type\": \"FeatureCollection\", \"features\": [ { \"type\": \"Feature\", \"properties\": {}, \"geometry\": { \"type\": \"Polygon\", \"coordinates\": [ [ [ -114.36749999999999,43.6175 ], [ -114.36749999999999,44 ], [ -114,44 ], [ -114,43.6175 ], [ -114.36749999999999,43.6175 ] ] ] } } ] }","noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"4f4e4b13e4b07f02db6a353f","contributors":{"authors":[{"text":"Dover, J. H.","contributorId":75545,"corporation":false,"usgs":true,"family":"Dover","given":"J.","email":"","middleInitial":"H.","affiliations":[],"preferred":false,"id":272683,"contributorType":{"id":1,"text":"Authors"},"rank":1}]}}
,{"id":4097,"text":"cir887 - 1983 - Mineral resource assessment of the Iron River 1° x 2° quadrangle, Michigan and Wisconsin","interactions":[{"subject":{"id":8196,"text":"ofr82223 - 1982 - Mineral-resource assessment of the Iron River 1° x 2° quadrangle, Michigan and Wisconsin","indexId":"ofr82223","publicationYear":"1982","noYear":false,"title":"Mineral-resource assessment of the Iron River 1° x 2° quadrangle, Michigan and Wisconsin"},"predicate":"SUPERSEDED_BY","object":{"id":4097,"text":"cir887 - 1983 - Mineral resource assessment of the Iron River 1° x 2° quadrangle, Michigan and Wisconsin","indexId":"cir887","publicationYear":"1983","noYear":false,"title":"Mineral resource assessment of the Iron River 1° x 2° quadrangle, Michigan and Wisconsin"},"id":1}],"lastModifiedDate":"2021-09-30T19:09:26.525097","indexId":"cir887","displayToPublicDate":"1994-01-01T00:00:00","publicationYear":"1983","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":"887","title":"Mineral resource assessment of the Iron River 1° x 2° quadrangle, Michigan and Wisconsin","docAbstract":"The Iron River 1? x 2? quadrangle contains identified resources of copper and iron. Copper-rich shale beds in the north part of the quadrangle contain 12.2 billion pounds (5.5 billion kilograms) of copper in well-studied deposits including 9.2 billion pounds (4.2 billion kilograms) that are economically minable by 1980 standards. At least several billion pounds of copper probably exist in other parts of the same shale beds, but not enough data are available to measure the amount. \r\n\r\nA small amount, about 250 million pounds (113 million kilograms), of native copper is known to remain in one abandoned mine, and additional but unknown amounts remain in other abandoned mines. About 13.25 billion tons (12.02 billion metric tons) of banded iron-formation averaging roughly 30 percent iron are known within 500 feet (152.4 meters) of the surface in the Gogebic, Marquette, and Iron River-Crystal Falls districts. A small percentage of that might someday be minable as taconite, but none is now believed to be economic. Some higher grade iron concentrations exist in the same iron-formations. Such material was the basis of former mining of iron in the region, but a poor market for such ore and depletion of many deposits have led to the decline of iron mining in the quadrangle. Iron mines of the quadrangle were not being worked in 1980. \r\n\r\nMany parts of the quadrangle contain belts of favorable host rocks for mineral deposits. Although deposits are not known in these belts, undiscovered deposits of copper, zinc, lead, silver, uranium, phosphate, nickel, chromium, platinum, gold, and diamonds could exist.","language":"English","publisher":"U.S. Geological Survey,","doi":"10.3133/cir887","usgsCitation":"Cannon, W.F., 1983, Mineral resource assessment of the Iron River 1° x 2° quadrangle, Michigan and Wisconsin: U.S. Geological Survey Circular 887, iii, 21 p., https://doi.org/10.3133/cir887.","productDescription":"iii, 21 p.","numberOfPages":"24","costCenters":[],"links":[{"id":390061,"rank":3,"type":{"id":36,"text":"NGMDB Index Page"},"url":"https://ngmdb.usgs.gov/Prodesc/proddesc_23959.htm"},{"id":31201,"rank":300,"type":{"id":11,"text":"Document"},"url":"https://pubs.usgs.gov/circ/1983/0887/report.pdf","linkFileType":{"id":1,"text":"pdf"}},{"id":124548,"rank":0,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/circ/1983/0887/report-thumb.jpg"}],"country":"United States","state":"Michigan, Wisconsin","otherGeospatial":"Iron River 1° x 2° quadrangle","geographicExtents":"{\n  \"type\": \"FeatureCollection\",\n  \"features\": [\n    {\n      \"type\": \"Feature\",\n      \"properties\": {},\n      \"geometry\": {\n        \"type\": \"Polygon\",\n        \"coordinates\": [\n          [\n            [\n              -90,\n              46\n            ],\n            [\n              -88,\n              46\n            ],\n            [\n              -88,\n              47\n            ],\n            [\n              -90,\n              47\n            ],\n            [\n              -90,\n              46\n            ]\n          ]\n        ]\n      }\n    }\n  ]\n}","noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"4f4e4ac8e4b07f02db67c213","contributors":{"authors":[{"text":"Cannon, William F. 0000-0002-2699-8118 wcannon@usgs.gov","orcid":"https://orcid.org/0000-0002-2699-8118","contributorId":1883,"corporation":false,"usgs":true,"family":"Cannon","given":"William","email":"wcannon@usgs.gov","middleInitial":"F.","affiliations":[{"id":245,"text":"Eastern Mineral and Environmental Resources Science Center","active":true,"usgs":true}],"preferred":true,"id":148183,"contributorType":{"id":1,"text":"Authors"},"rank":1}]}}
,{"id":61512,"text":"mf1500B - 1983 - Geochemical map of the Ten Mile West Roadless Area, Boise and Elmore Counties, Idaho","interactions":[],"lastModifiedDate":"2012-02-10T00:10:31","indexId":"mf1500B","displayToPublicDate":"1994-01-01T00:00:00","publicationYear":"1983","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":"1500","chapter":"B","title":"Geochemical map of the Ten Mile West Roadless Area, Boise and Elmore Counties, Idaho","language":"ENGLISH","doi":"10.3133/mf1500B","usgsCitation":"Kiilsgaard, T.H., 1983, Geochemical map of the Ten Mile West Roadless Area, Boise and Elmore Counties, Idaho: U.S. Geological Survey Miscellaneous Field Studies Map 1500, Sheet 33 inches x 41 inches, https://doi.org/10.3133/mf1500B.","productDescription":"Sheet 33 inches x 41 inches","costCenters":[],"links":[{"id":105926,"rank":700,"type":{"id":15,"text":"Index Page"},"url":"https://ngmdb.usgs.gov/Prodesc/proddesc_7283.htm","linkFileType":{"id":5,"text":"html"},"description":"7283"},{"id":179906,"rank":0,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/thumbnails/usgs_thumb.jpg"}],"scale":"62500","geographicExtents":"{ \"type\": \"FeatureCollection\", \"features\": [ { \"type\": \"Feature\", \"properties\": {}, \"geometry\": { \"type\": \"Polygon\", \"coordinates\": [ [ [ -115.5,43.8675 ], [ -115.5,44.1175 ], [ -115.11749999999999,44.1175 ], [ -115.11749999999999,43.8675 ], [ -115.5,43.8675 ] ] ] } } ] }","noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"4f4e4b23e4b07f02db6ae1cb","contributors":{"authors":[{"text":"Kiilsgaard, T. H.","contributorId":102043,"corporation":false,"usgs":true,"family":"Kiilsgaard","given":"T.","email":"","middleInitial":"H.","affiliations":[],"preferred":false,"id":265849,"contributorType":{"id":1,"text":"Authors"},"rank":1}]}}
,{"id":18907,"text":"ofr83909 - 1983 - Self-potential measurements at Newberry Crater, Oregon","interactions":[],"lastModifiedDate":"2012-02-02T00:07:32","indexId":"ofr83909","displayToPublicDate":"1994-01-01T00:00:00","publicationYear":"1983","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":"83-909","title":"Self-potential measurements at Newberry Crater, Oregon","language":"ENGLISH","publisher":"U.S. Geological Survey,","doi":"10.3133/ofr83909","usgsCitation":"Fitterman, D., and Grette, R., 1983, Self-potential measurements at Newberry Crater, Oregon: U.S. Geological Survey Open-File Report 83-909, 12 p. :ill., maps ;28 cm., https://doi.org/10.3133/ofr83909.","productDescription":"12 p. :ill., maps ;28 cm.","costCenters":[],"links":[{"id":151481,"rank":0,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/of/1983/0909/report-thumb.jpg"},{"id":48306,"rank":300,"type":{"id":11,"text":"Document"},"url":"https://pubs.usgs.gov/of/1983/0909/report.pdf","linkFileType":{"id":1,"text":"pdf"}}],"noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"4f4e49ffe4b07f02db5f7aee","contributors":{"authors":[{"text":"Fitterman, D.V. 0000-0001-5600-3401","orcid":"https://orcid.org/0000-0001-5600-3401","contributorId":70386,"corporation":false,"usgs":true,"family":"Fitterman","given":"D.V.","email":"","affiliations":[],"preferred":false,"id":179962,"contributorType":{"id":1,"text":"Authors"},"rank":1},{"text":"Grette, R.O.","contributorId":14434,"corporation":false,"usgs":true,"family":"Grette","given":"R.O.","email":"","affiliations":[],"preferred":false,"id":179961,"contributorType":{"id":1,"text":"Authors"},"rank":2}]}}
,{"id":65434,"text":"i1521 - 1983 - Controlled photomosaic of the Cebrenia Northwest Quadrangle of Mars","interactions":[],"lastModifiedDate":"2012-02-02T00:13:14","indexId":"i1521","displayToPublicDate":"1994-01-01T00:00:00","publicationYear":"1983","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":"1521","subseriesTitle":"NONE","title":"Controlled photomosaic of the Cebrenia Northwest Quadrangle of Mars","language":"ENGLISH","doi":"10.3133/i1521","usgsCitation":"Water Resources Division, U.S. Geological Survey, 1983, Controlled photomosaic of the Cebrenia Northwest Quadrangle of Mars: U.S. Geological Survey IMAP 1521, 1 photomosaic ;54 x 59 cm., on sheet 86 x 66 cm., folded in envelope 30 x 24 cm., https://doi.org/10.3133/i1521.","productDescription":"1 photomosaic ;54 x 59 cm., on sheet 86 x 66 cm., folded in envelope 30 x 24 cm.","costCenters":[],"links":[{"id":251318,"rank":300,"type":{"id":11,"text":"Document"},"url":"https://pubs.usgs.gov/imap/1521/report.pdf","size":"27","linkFileType":{"id":1,"text":"pdf"}},{"id":251319,"rank":400,"type":{"id":17,"text":"Plate"},"url":"https://pubs.usgs.gov/imap/1521/plate-1.pdf","size":"10541","linkFileType":{"id":1,"text":"pdf"}},{"id":252213,"rank":0,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/imap/1521/report-thumb.jpg"}],"scale":"2000000","noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"4f4e4ae2e4b07f02db688c0f","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":533821,"contributorType":{"id":1,"text":"Authors"},"rank":1}]}}
,{"id":18860,"text":"ofr83625 - 1983 - Forward and inverse cartographic projection procedures","interactions":[],"lastModifiedDate":"2012-02-02T00:07:30","indexId":"ofr83625","displayToPublicDate":"1994-01-01T00:00:00","publicationYear":"1983","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":"83-625","title":"Forward and inverse cartographic projection procedures","docAbstract":"A set of procedures for performing 19 common cartographic transformations between geographic and artesian coordinate systems are presented along with instruction for usage, installation and testing results. These procedures are written in the RATFOR preprocessor language and effort was made to ensure transportability of the code as well as consistency and flexibility of usage.","language":"ENGLISH","publisher":"U.S. Geological Survey,","doi":"10.3133/ofr83625","usgsCitation":"Evenden, G., 1983, Forward and inverse cartographic projection procedures: U.S. Geological Survey Open-File Report 83-625, 1 v. 76 p.  ;28 cm., https://doi.org/10.3133/ofr83625.","productDescription":"1 v. 76 p.  ;28 cm.","costCenters":[],"links":[{"id":151666,"rank":0,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/of/1983/0625/report-thumb.jpg"},{"id":48255,"rank":300,"type":{"id":11,"text":"Document"},"url":"https://pubs.usgs.gov/of/1983/0625/report.pdf","linkFileType":{"id":1,"text":"pdf"}}],"noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"4f4e4b23e4b07f02db6adf5d","contributors":{"authors":[{"text":"Evenden, G. I.","contributorId":52960,"corporation":false,"usgs":true,"family":"Evenden","given":"G. I.","affiliations":[],"preferred":false,"id":179877,"contributorType":{"id":1,"text":"Authors"},"rank":1}]}}
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