{"pageNumber":"5204","pageRowStart":"130075","pageSize":"25","recordCount":184606,"records":[{"id":4082,"text":"cir894 - 1983 - Recommended procedures and methodology of coal description","interactions":[],"lastModifiedDate":"2013-07-22T15:13:05","indexId":"cir894","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":"894","title":"Recommended procedures and methodology of coal description","docAbstract":"This document is the result of a workshop on coal description held for the Branch of Coal Resources of the U.S. Geological Survey in March 1982. It has been prepared to aid and encourage the field-oriented coal scientist to participate directly in petrographic coal-description activities. The objectives and past and current practices of coal description vary widely. These are briefly reviewed and illustrated with examples. Sampling approaches and techniques for collecting columnar samples of fresh coal are also discussed. The recommended procedures and methodology emphasize the fact that obtaining a good megascopic description of a coal bed is much better done in the laboratory with a binocular microscope and under good lighting conditions after the samples have been cut and quickly prepared. For better observation and cross-checking using a petrographic microscope for identification purposes, an in-place polishing procedure (requiring less than 2 min) is routinely used. Methods for using both the petrographic microscope and an automated image analysis system are also included for geologists who have access to such instruments. To describe the material characteristics of a coal bed in terms of microlithotypes or lithotypes, a new nomenclature of (V), (E), (1), (M). (S). (X<sub>1</sub>). (X<sub>2</sub>) and so on is used. The microscopic description of the modal composition of a megascopically observed lithologic type is expressed in terms of (VEIM); subscripts are used to denote the volume percentage of each constituent present. To describe a coal-bed profile, semiquantitative data (without microscopic study) and quantitative data (with microscopic study) are presented in ready-to-understand form. The average total composition of any thickness interval or of the entire coal bed can be plotted on a triangular diagram having V, E, and I+ M +S as the apices. The modal composition of any mixed lithologies such as (X<sub>1</sub>), (X<sub>2</sub>), and so on can also be plotted on such a triangular ternary diagram. Such diagrams can be used either for tracing compositional variations throughout a single coal-bed profile or for comparing variations between different coal beds.","language":"ENGLISH","publisher":"U.S. Geological Survey,","doi":"10.3133/cir894","usgsCitation":"Chao, E., Minkin, J., and Thompson, C., 1983, Recommended procedures and methodology of coal description: U.S. Geological Survey Circular 894, iv, 31 p., https://doi.org/10.3133/cir894.","productDescription":"iv, 31 p.","numberOfPages":"36","costCenters":[],"links":[{"id":139148,"rank":0,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/circ/0894/report-thumb.jpg"},{"id":271070,"type":{"id":11,"text":"Document"},"url":"https://pubs.usgs.gov/circ/0894/report.pdf"}],"noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"4f4e4a74e4b07f02db644603","contributors":{"authors":[{"text":"Chao, E.C.","contributorId":47358,"corporation":false,"usgs":true,"family":"Chao","given":"E.C.","email":"","affiliations":[],"preferred":false,"id":148153,"contributorType":{"id":1,"text":"Authors"},"rank":1},{"text":"Minkin, J.A.","contributorId":38588,"corporation":false,"usgs":true,"family":"Minkin","given":"J.A.","affiliations":[],"preferred":false,"id":148152,"contributorType":{"id":1,"text":"Authors"},"rank":2},{"text":"Thompson, C.L.","contributorId":12189,"corporation":false,"usgs":true,"family":"Thompson","given":"C.L.","email":"","affiliations":[],"preferred":false,"id":148151,"contributorType":{"id":1,"text":"Authors"},"rank":3}]}}
,{"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":10724,"text":"ofr83515 - 1983 - Description of single-channel, high-resolution, seismic-reflection data collected from the continental shelf, slope, and upper rise between Cape Hatteras, North Carolina and Norfolk, Virginia; and Vero Beach and Miami, Florida (Cruise 80-G-9)","interactions":[],"lastModifiedDate":"2024-11-26T20:37:13.703938","indexId":"ofr83515","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":"83-515","title":"Description of single-channel, high-resolution, seismic-reflection data collected from the continental shelf, slope, and upper rise between Cape Hatteras, North Carolina and Norfolk, Virginia; and Vero Beach and Miami, Florida (Cruise 80-G-9)","docAbstract":"<p>No abstract available.</p>","language":"English","publisher":"U.S. Geological Survey,","doi":"10.3133/ofr83515","usgsCitation":"Popenoe, P., and Meyer, F.W., 1983, Description of single-channel, high-resolution, seismic-reflection data collected from the continental shelf, slope, and upper rise between Cape Hatteras, North Carolina and Norfolk, Virginia; and Vero Beach and Miami, Florida (Cruise 80-G-9): U.S. Geological Survey Open-File Report 83-515, 3 p., https://doi.org/10.3133/ofr83515.","productDescription":"3 p.","costCenters":[],"links":[{"id":464539,"rank":4,"type":{"id":36,"text":"NGMDB Index Page"},"url":"https://ngmdb.usgs.gov/Prodesc/proddesc_14082.htm","text":"Vero Beach and Miami, Florida","linkFileType":{"id":5,"text":"html"}},{"id":388783,"rank":3,"type":{"id":36,"text":"NGMDB Index Page"},"url":"https://ngmdb.usgs.gov/Prodesc/proddesc_14081.htm","text":"Cape Hatteras, North Carolina and Norfolk, Virginia","linkFileType":{"id":5,"text":"html"}},{"id":38536,"rank":2,"type":{"id":11,"text":"Document"},"url":"https://pubs.usgs.gov/of/1983/0515/report.pdf","linkFileType":{"id":1,"text":"pdf"}},{"id":143235,"rank":1,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/of/1983/0515/report-thumb.jpg"}],"country":"United States","state":"Florida, North Carolina, Virginia","city":"Miami, Norfolk, Vero Beach","otherGeospatial":"Cape Hatteras","geographicExtents":"{\n  \"type\": \"FeatureCollection\",\n  \"features\": [\n    {\n      \"type\": \"Feature\",\n      \"properties\": {},\n      \"geometry\": {\n        \"type\": \"Polygon\",\n        \"coordinates\": [\n          [\n            [\n              -76.2451171875,\n              36.91696023183306\n            ],\n            [\n              -75.7122802734375,\n              36.115690180653395\n            ],\n            [\n              -75.55847167968749,\n              35.806676609227054\n            ],\n            [\n              -75.52276611328125,\n              35.27701633139884\n            ],\n            [\n              -73.68942260742188,\n              35.33641350071228\n            ],\n            [\n              -73.7457275390625,\n              36.26531407324164\n            ],\n            [\n              -73.90502929687499,\n              37.23470197166817\n            ],\n            [\n              -76.2451171875,\n              36.91696023183306\n            ]\n          ]\n        ]\n      }\n    },\n    {\n      \"type\": \"Feature\",\n      \"properties\": {},\n      \"geometry\": {\n        \"type\": \"Polygon\",\n        \"coordinates\": [\n          [\n            [\n              -80.32928466796874,\n              27.637307020155223\n            ],\n            [\n              -80.04364013671875,\n              26.979604764019346\n            ],\n            [\n              -80.02304077148438,\n              26.779330479911337\n            ],\n            [\n              -80.02166748046875,\n              26.52956523826758\n            ],\n            [\n              -80.10406494140625,\n              25.814727063097408\n            ],\n            [\n              -80.10406494140625,\n              25.70093788144426\n            ],\n            [\n              -79.45037841796875,\n              25.68361258391759\n            ],\n            [\n              -79.43115234375,\n              26.33280692289788\n            ],\n            [\n              -79.70581054687499,\n              26.944108009688595\n            ],\n            [\n              -80.00518798828125,\n              27.36201054924028\n            ],\n            [\n              -80.32928466796874,\n              27.637307020155223\n            ]\n          ]\n        ]\n      }\n    }\n  ]\n}","noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"4f4e4aabe4b07f02db669b7e","contributors":{"authors":[{"text":"Popenoe, Peter","contributorId":62206,"corporation":false,"usgs":true,"family":"Popenoe","given":"Peter","email":"","affiliations":[{"id":678,"text":"Woods Hole Coastal and Marine Science Center","active":true,"usgs":true}],"preferred":false,"id":161860,"contributorType":{"id":1,"text":"Authors"},"rank":1},{"text":"Meyer, Frederick W.","contributorId":39373,"corporation":false,"usgs":true,"family":"Meyer","given":"Frederick","email":"","middleInitial":"W.","affiliations":[],"preferred":false,"id":161859,"contributorType":{"id":1,"text":"Authors"},"rank":2}]}}
,{"id":27732,"text":"wri834179 - 1983 - Three-dimensional digital-computer model of the principal ground-water reservoir of the Sevier Desert, Utah","interactions":[],"lastModifiedDate":"2022-12-09T21:40:24.164154","indexId":"wri834179","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":"83-4179","title":"Three-dimensional digital-computer model of the principal ground-water reservoir of the Sevier Desert, Utah","docAbstract":"<p>The principal ground-water reservoir in part of the Sevier Desert, Utah was modeled using a three-dimensional finite-difference model. The model was calibrated by comparing computed and observed water-level measurements in 1952, simulating results of aquifer tests, and simulating ground-water withdrawals during 1952-81 and comparing computed water-level changes during 1952-82 to observed changes. The results indicate the model is capable of predicting future water-level changes. The report includes a complete listing of the model data for the 1952-82 simulation.</p>","language":"English","publisher":"U.S. Geological Survey","doi":"10.3133/wri834179","usgsCitation":"Holmes, W., 1983, Three-dimensional digital-computer model of the principal ground-water reservoir of the Sevier Desert, Utah: U.S. Geological Survey Water-Resources Investigations Report 83-4179, Report: iv, 127 p.; 1 Plate: 21.06 × 22.53 inches, https://doi.org/10.3133/wri834179.","productDescription":"Report: iv, 127 p.; 1 Plate: 21.06 × 22.53 inches","costCenters":[],"links":[{"id":56573,"rank":1,"type":{"id":11,"text":"Document"},"url":"https://pubs.usgs.gov/wri/1983/4179/report.pdf","linkFileType":{"id":1,"text":"pdf"}},{"id":56572,"rank":2,"type":{"id":17,"text":"Plate"},"url":"https://pubs.usgs.gov/wri/1983/4179/plate-1.pdf","linkFileType":{"id":1,"text":"pdf"}},{"id":158795,"rank":0,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/wri/1983/4179/report-thumb.jpg"},{"id":410238,"rank":4,"type":{"id":36,"text":"NGMDB Index Page"},"url":"https://ngmdb.usgs.gov/Prodesc/proddesc_35828.htm","linkFileType":{"id":5,"text":"html"}}],"country":"United States","state":"Utah","otherGeospatial":"Sevier Desert","geographicExtents":"{\n  \"type\": \"FeatureCollection\",\n  \"features\": [\n    {\n      \"type\": \"Feature\",\n      \"properties\": {},\n      \"geometry\": {\n        \"coordinates\": [\n          [\n            [\n              -112.047,\n              40\n            ],\n            [\n              -113.409,\n              40\n            ],\n            [\n              -113.409,\n              39\n            ],\n            [\n              -112.047,\n              39\n            ],\n            [\n              -112.047,\n              40\n            ]\n          ]\n        ],\n        \"type\": \"Polygon\"\n      }\n    }\n  ]\n}","noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"4f4e4a6ce4b07f02db63e081","contributors":{"authors":[{"text":"Holmes, W. F.","contributorId":7277,"corporation":false,"usgs":true,"family":"Holmes","given":"W. F.","affiliations":[],"preferred":false,"id":198609,"contributorType":{"id":1,"text":"Authors"},"rank":1}]}}
,{"id":28597,"text":"wri834004 - 1983 - Conveyance characteristics of the Nueces River, Cotulla to Simmons, Texas","interactions":[],"lastModifiedDate":"2016-08-09T13:28:30","indexId":"wri834004","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":"83-4004","title":"Conveyance characteristics of the Nueces River, Cotulla to Simmons, Texas","docAbstract":"<p>Analysis of discharge hydrographs for streamflow-gaging stations on the Nueces River at Cotulla, Tilden, and Simmons indicate that significant water losses occur along the 108-mile reach from Cotulla to Simmon during storm-runoff periods. Computed losses along the 83-mile reach from Cotulla to Tilden for 15 storm periods range from 32 to 59 percent of the total runoff volume passing the Cotulla gage. For six storm periods that occurred while the gage at Simmons was in operation, computed losses from Cotulla to Simmons averaged 48 percent of the storm runoff passing the Cotulla gage. Estimates of total-annual losses were made with the aid of a regression model developed to relate monthly rainfall totals to monthly runoff. Total annual water losses, estimated with the aid of the regression model, ranged from 46,000 acre-feet during 1969 to 368,500 acre-feet during 1967, and averaged about 174,000 acre-feet for 1966-77. (USGS)</p>","language":"English","publisher":"U.S. Geological Survey","publisherLocation":"Austin, TX","doi":"10.3133/wri834004","usgsCitation":"Massey, B.C., and Reeves, W.E., 1983, Conveyance characteristics of the Nueces River, Cotulla to Simmons, Texas: U.S. Geological Survey Water-Resources Investigations Report 83-4004, Report: vi, 39 p.; Plate: 17.82 x 12.07 inches, https://doi.org/10.3133/wri834004.","productDescription":"Report: vi, 39 p.; Plate: 17.82 x 12.07 inches","numberOfPages":"45","onlineOnly":"N","additionalOnlineFiles":"N","costCenters":[{"id":583,"text":"Texas Water Science Center","active":true,"usgs":true}],"links":[{"id":57428,"rank":300,"type":{"id":11,"text":"Document"},"url":"https://pubs.usgs.gov/wri/1983/4004/report.pdf","linkFileType":{"id":1,"text":"pdf"}},{"id":124184,"rank":0,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/wri/1983/4004/report-thumb.jpg"},{"id":57427,"rank":400,"type":{"id":17,"text":"Plate"},"url":"https://pubs.usgs.gov/wri/1983/4004/plate-1.pdf","linkFileType":{"id":1,"text":"pdf"}}],"noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"4f4e4a9ae4b07f02db65d46c","contributors":{"authors":[{"text":"Massey, Bernard C.","contributorId":173558,"corporation":false,"usgs":false,"family":"Massey","given":"Bernard","email":"","middleInitial":"C.","affiliations":[],"preferred":false,"id":200090,"contributorType":{"id":1,"text":"Authors"},"rank":1},{"text":"Reeves, William E.","contributorId":99426,"corporation":false,"usgs":true,"family":"Reeves","given":"William","email":"","middleInitial":"E.","affiliations":[],"preferred":false,"id":200089,"contributorType":{"id":1,"text":"Authors"},"rank":2}]}}
,{"id":26699,"text":"wri834194 - 1983 - Estimating generalized flood skew coefficients for Michigan","interactions":[],"lastModifiedDate":"2016-09-16T10:19:33","indexId":"wri834194","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":"83-4194","title":"Estimating generalized flood skew coefficients for Michigan","docAbstract":"<p>Current estimates of station skew indicate that estimates of generalized skew obtained from the skew map of the United States prepared by the U.S. Water Resources Council have a -0.27 bias for Michigan. Station skew was recomputed using currently recommended statistical procedures of the Water Resources Council, and available data through 1982. Generalized skew is combined with station skew in order to improve estimates of flood-flow frequencies. As a result of this study, the mean station skew for each of three designated regions can be used to estimate generalized skew in Michigan. The Upper Peninsula has a skew of 0.12; the southwest part of the Lower Peninsula has a skew of 0.081; the remainder of the Lower Peninsula has a skew of -0.17. The mean-square error associated with generalized skew determined on the basis of designated regions is 0.2. </p>","language":"English","publisher":"U.S. Geological Survey","publisherLocation":"Lansing, MI","doi":"10.3133/wri834194","collaboration":"Prepared jointly with Michigan Department of Natural Resources, Water Management Division","usgsCitation":"Croskey, H., and Holtschlag, D., 1983, Estimating generalized flood skew coefficients for Michigan: U.S. Geological Survey Water-Resources Investigations Report 83-4194, iv, 27 p., https://doi.org/10.3133/wri834194.","productDescription":"iv, 27 p.","costCenters":[{"id":382,"text":"Michigan Water Science Center","active":true,"usgs":true}],"links":[{"id":121931,"rank":0,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/wri/1983/4194/report-thumb.jpg"},{"id":55570,"rank":300,"type":{"id":11,"text":"Document"},"url":"https://pubs.usgs.gov/wri/1983/4194/report.pdf","linkFileType":{"id":1,"text":"pdf"}}],"country":"United 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J. 0000-0001-5185-4928","orcid":"https://orcid.org/0000-0001-5185-4928","contributorId":102493,"corporation":false,"usgs":true,"family":"Holtschlag","given":"D. J.","affiliations":[],"preferred":false,"id":196849,"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":28771,"text":"wri834018 - 1983 - Hydrology of the Little Androscoggin River Valley aquifer, Oxford County, Maine","interactions":[],"lastModifiedDate":"2012-02-02T00:08:52","indexId":"wri834018","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":"83-4018","title":"Hydrology of the Little Androscoggin River Valley aquifer, Oxford County, Maine","docAbstract":"The Little Androscoggin River valley aquifer, a 15-square-mile sand and gravel valley-fill aquifer in southwestern Maine, is the source of water for the towns of Norway, Oxford, and South Paris. Estimated inflows to the aquifer during the 1981 water year were 16.4 cubic feet per second from precipitation directly on the aquifer, 11.2 cubic feet per second from till covered uplands adjacent to the aquifer, and 1.4 cubic feet per second from surface-water leakage. Outflows from the aquifer were 26.7 cubic feet per second to surface water and 2.3 cubic feet per second to wells. A finite-difference ground-water flow model was used to simulate conditions observed in the aquifer during 1981. Model conditions observed in the aquifer during 1981. Model simulations indicate that a 50 percent reduction of average 1981 recharge to the aquifer would cause water level declines of up to 20 feet in some areas. Model simulations of increased pumping at a high yield well in the northern part of the aquifer indicate that resulting changes in the water table will not be sufficient to intercept groundwater contaminated by a sludge disposal site. Water in the aquifer is low in dissolved solids (average for 38 samples was 67 mg/L), slightly acidic and soft. Ground-water contamination has occurred near a sludge-disposal site and in the vicinity of a sanitary landfill. Dissolved solids in ground water near the sludge disposal site were as much as ten times greater than average background values for the aquifer. (USGS)","language":"ENGLISH","publisher":"U.S. Geological Survey,","doi":"10.3133/wri834018","usgsCitation":"Morrissey, D.J., 1983, Hydrology of the Little Androscoggin River Valley aquifer, Oxford County, Maine: U.S. Geological Survey Water-Resources Investigations Report 83-4018, viii, 87 p. :ill., maps ;28 cm., https://doi.org/10.3133/wri834018.","productDescription":"viii, 87 p. :ill., maps ;28 cm.","costCenters":[],"links":[{"id":123306,"rank":0,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/wri/1983/4018/report-thumb.jpg"},{"id":57638,"rank":400,"type":{"id":17,"text":"Plate"},"url":"https://pubs.usgs.gov/wri/1983/4018/plate-1.pdf","linkFileType":{"id":1,"text":"pdf"}},{"id":57639,"rank":401,"type":{"id":17,"text":"Plate"},"url":"https://pubs.usgs.gov/wri/1983/4018/plate-2.pdf","linkFileType":{"id":1,"text":"pdf"}},{"id":57640,"rank":402,"type":{"id":17,"text":"Plate"},"url":"https://pubs.usgs.gov/wri/1983/4018/plate-3.pdf","linkFileType":{"id":1,"text":"pdf"}},{"id":57641,"rank":403,"type":{"id":17,"text":"Plate"},"url":"https://pubs.usgs.gov/wri/1983/4018/plate-4.pdf","linkFileType":{"id":1,"text":"pdf"}},{"id":57642,"rank":404,"type":{"id":17,"text":"Plate"},"url":"https://pubs.usgs.gov/wri/1983/4018/plate-5.pdf","linkFileType":{"id":1,"text":"pdf"}},{"id":57643,"rank":405,"type":{"id":17,"text":"Plate"},"url":"https://pubs.usgs.gov/wri/1983/4018/plate-6.pdf","linkFileType":{"id":1,"text":"pdf"}},{"id":57644,"rank":406,"type":{"id":17,"text":"Plate"},"url":"https://pubs.usgs.gov/wri/1983/4018/plate-7.pdf","linkFileType":{"id":1,"text":"pdf"}},{"id":57645,"rank":407,"type":{"id":17,"text":"Plate"},"url":"https://pubs.usgs.gov/wri/1983/4018/plate-8.pdf","linkFileType":{"id":1,"text":"pdf"}},{"id":57646,"rank":300,"type":{"id":11,"text":"Document"},"url":"https://pubs.usgs.gov/wri/1983/4018/report.pdf","linkFileType":{"id":1,"text":"pdf"}}],"noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"4f4e478fe4b07f02db48a40b","contributors":{"authors":[{"text":"Morrissey, D. J.","contributorId":51305,"corporation":false,"usgs":true,"family":"Morrissey","given":"D.","email":"","middleInitial":"J.","affiliations":[],"preferred":false,"id":200369,"contributorType":{"id":1,"text":"Authors"},"rank":1}]}}
,{"id":1674,"text":"wsp2240 - 1983 - Estimation of nonpoint source loadings of phosphorus for lakes in the Puget Sound region, Washington","interactions":[{"subject":{"id":9135,"text":"ofr82161 - 1983 - Estimation of nonpoint sources of phosphorus for lakes in the Puget Sound region, Washington","indexId":"ofr82161","publicationYear":"1983","noYear":false,"title":"Estimation of nonpoint sources of phosphorus for lakes in the Puget Sound region, Washington"},"predicate":"SUPERSEDED_BY","object":{"id":1674,"text":"wsp2240 - 1983 - Estimation of nonpoint source loadings of phosphorus for lakes in the Puget Sound region, Washington","indexId":"wsp2240","publicationYear":"1983","noYear":false,"title":"Estimation of nonpoint source loadings of phosphorus for lakes in the Puget Sound region, Washington"},"id":1}],"lastModifiedDate":"2012-02-02T00:05:23","indexId":"wsp2240","displayToPublicDate":"1994-01-01T00:00:00","publicationYear":"1983","noYear":false,"publicationType":{"id":18,"text":"Report"},"publicationSubtype":{"id":5,"text":"USGS Numbered Series"},"seriesTitle":{"id":341,"text":"Water Supply Paper","code":"WSP","active":false,"publicationSubtype":{"id":5}},"seriesNumber":"2240","title":"Estimation of nonpoint source loadings of phosphorus for lakes in the Puget Sound region, Washington","docAbstract":"Control of eutrophication of lakes in watersheds undergoing development is facilitated by estimates of the amounts of phosphorus (P) that reach the lakes from areas under various types of land use. Using a mass-balance model, the author calculated P loadings from present-day P concentrations measured in lake water and from other easily measured physical characteristics in a total of 28 lakes in drainage basins that contain only forest and residential land. The loadings from background sources (forest-land drainage and bulk precipitation) to each of the lakes were estimated by methods developed in a previous study. Differences between estimated present-day P loadings and loadings from background sources were attributed to changes in land use. The mean increase in annual P yield resulting from conversion of forest to residential land use was 7 kilograms per square kilometer, not including septic tank system contributions. Calculated loadings from septic systems were found to correlate best with the number of near-shore dwellings around each lake in 1940. The regression equation expressing this relationship explained 36 percent of the sample variance. There was no significant correlation between estimated septic tank system P loadings and number of dwellings present in 1960 or 1970. The evidence indicates that older systems might contribute more phosphorus to lakes than newer systems, and that there may be substantial time lags between septic system installation and significant impacts on lake-water P concentrations. For lakes in basins that contain agricultural land, the P loading attributable to agriculture can be calculated as the difference between the estimated total loading and the sum of estimated loadings from nonagricultural sources. A comprehensive system for evaluating errors in all loading estimates is presented. The empirical relationships developed allow preliminary approximations of the cumulative impact development has had on P loading and the amounts of P loading from generalized land-use categories for Puget Sound lowland lakes. In addition, the sensitivity of a lake to increased loading can be evaluated using the mass-balance model. The data required are presently available for most lakes. Estimates of P loading are useful in developing water-quality goals, setting priorities for lake studies, and designing studies of individual lakes. The suitability of a method for management of individual lakes will often be limited by relatively high levels of uncertainty, especially if the method is used to evaluate relatively small increases in P loading.","language":"ENGLISH","publisher":"U.S. G.P.O.,","doi":"10.3133/wsp2240","usgsCitation":"Gilliom, R.J., 1983, Estimation of nonpoint source loadings of phosphorus for lakes in the Puget Sound region, Washington: U.S. Geological Survey Water Supply Paper 2240, iv, 24 p. :ill., 1 map ;28 cm., https://doi.org/10.3133/wsp2240.","productDescription":"iv, 24 p. :ill., 1 map ;28 cm.","costCenters":[],"links":[{"id":138235,"rank":0,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/wsp/2240/report-thumb.jpg"},{"id":26749,"rank":300,"type":{"id":11,"text":"Document"},"url":"https://pubs.usgs.gov/wsp/2240/report.pdf","linkFileType":{"id":1,"text":"pdf"}}],"noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"4f4e4a0ae4b07f02db5fb25d","contributors":{"authors":[{"text":"Gilliom, Robert J. rgilliom@usgs.gov","contributorId":488,"corporation":false,"usgs":true,"family":"Gilliom","given":"Robert","email":"rgilliom@usgs.gov","middleInitial":"J.","affiliations":[{"id":451,"text":"National Water Quality Assessment Program","active":true,"usgs":true}],"preferred":true,"id":143954,"contributorType":{"id":1,"text":"Authors"},"rank":1}]}}
,{"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":29032,"text":"wri834062 - 1983 - Ground-water quality in the western Snake River basin, Swan Falls to Glenns Ferry, Idaho","interactions":[],"lastModifiedDate":"2012-02-02T00:08:44","indexId":"wri834062","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":"83-4062","title":"Ground-water quality in the western Snake River basin, Swan Falls to Glenns Ferry, Idaho","docAbstract":"Water-quality data were collected from 92 wells in the western Snake River basin, Swan Falls to Glenns Ferry, Idaho. Current data were compiled with pre-1980 data from 116 wells to define water-quality conditions in major aquifers. Factors affecting water quality are composition of aquifer materials, water temperature, and source of recharge. Mixing of water by interaquifer flow, from confined, hot water aquifers (40 degrees Celsius or greater) with water from cold water aquifers (less than 20 degrees Celsius) occurs along regional complex fault systems, and through partially cased boreholes. Cold water generally contains calcium, magnesium, and bicarbonate plus carbonate ions; hot water generally contains sodium, potassium, and bicarbonate plus carbonate ions. Warm water (between 20 degrees and 40 degrees Celsius) has an intermediate chemical composition resulting from mixing. Ground-water quality is acceptable for most uses, although it locally contains chemical constituents or physical properties that may restrict its use. Effects of thermal water used for irrigation on quality of shallow ground water are inconclusive. Long-term increase in concentrations of several constituents in parts of the study area may be due to effects of land- and water-use activities, such as infiltration of septic-tank effluent. (USGS)","language":"ENGLISH","publisher":"U.S. Geological Survey,","doi":"10.3133/wri834062","usgsCitation":"Parliman, D., 1983, Ground-water quality in the western Snake River basin, Swan Falls to Glenns Ferry, Idaho: U.S. Geological Survey Water-Resources Investigations Report 83-4062, ix, 94 p. :ill., maps ;28 cm., https://doi.org/10.3133/wri834062.","productDescription":"ix, 94 p. :ill., maps ;28 cm.","costCenters":[],"links":[{"id":123476,"rank":0,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/wri/1983/4062/report-thumb.jpg"},{"id":57893,"rank":300,"type":{"id":11,"text":"Document"},"url":"https://pubs.usgs.gov/wri/1983/4062/report.pdf","linkFileType":{"id":1,"text":"pdf"}}],"noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"4f4e4a90e4b07f02db6557df","contributors":{"authors":[{"text":"Parliman, D. J.","contributorId":64220,"corporation":false,"usgs":true,"family":"Parliman","given":"D. J.","affiliations":[],"preferred":false,"id":200828,"contributorType":{"id":1,"text":"Authors"},"rank":1}]}}
,{"id":30169,"text":"wri824116 - 1983 - Appraisal of water-quality conditions, lower Black River, Windsor County, Vermont","interactions":[],"lastModifiedDate":"2012-02-02T00:08:50","indexId":"wri824116","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":"82-4116","title":"Appraisal of water-quality conditions, lower Black River, Windsor County, Vermont","docAbstract":"Six hydroelectric power dams are planned along a 22-mile reach of the lower Black River in southeastern Windsor County, Vermont. Data were collected at 10 stations, during water years 1977-81, to appraise quality conditions before construction. Average specific conductance of Black River is 101 micromhos indicating low concentrations of dissolved solids. Concentrations of common constituents and minor elements were generally low and within safe levels for aquatic life. Near-saturated dissolved oxygen concentrations and relatively low mean total organic carbon concentrations indicate little oxygen-consuming substances in Black River. Mean total nitrogen concentrations ranged from 0.31 mg/L (milligrams per liter) to 0.61 mg/L. The highest concentrations were most likely due to secondary waste discharges entering the river. Nitrate was the primary form of inorganic nitrogen, mean concentrations ranged from 0.13 to 0.27 mg/L. Concentrations seem high enough to promote excessive algal growth in the proposed Hawks Mountain Reservoir. Mean concentrations of total phosphorus ranged from 0.014 to 0.112 mg/L as P. Maximum concentrations at all stations generally exceeded U.S. Environmental Protection Agency suggested levels for water entering lakes and reservoirs. Mean orthophosphorus concentrations ranged from 0.005 to 0.029 mg/L, suggesting a potential for nuisance algal conditions to develop in the proposed reservoir. Mean algal growth potential concentrations ranged from 1.3 to 8.8 mg/L, falling within the moderately high to high productivity range. No pesticides and polychlorinated biphenyls were detected. (USGS)","language":"ENGLISH","publisher":"U.S. Geological Survey,","doi":"10.3133/wri824116","usgsCitation":"Toppin, K., 1983, Appraisal of water-quality conditions, lower Black River, Windsor County, Vermont: U.S. Geological Survey Water-Resources Investigations Report 82-4116, 61 p. :ill., map ;28 cm., https://doi.org/10.3133/wri824116.","productDescription":"61 p. :ill., map ;28 cm.","costCenters":[],"links":[{"id":123968,"rank":0,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/wri/1982/4116/report-thumb.jpg"},{"id":58970,"rank":300,"type":{"id":11,"text":"Document"},"url":"https://pubs.usgs.gov/wri/1982/4116/report.pdf","linkFileType":{"id":1,"text":"pdf"}}],"noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"4f4e4ac6e4b07f02db67a305","contributors":{"authors":[{"text":"Toppin, K. W.","contributorId":35776,"corporation":false,"usgs":true,"family":"Toppin","given":"K. W.","affiliations":[],"preferred":false,"id":202800,"contributorType":{"id":1,"text":"Authors"},"rank":1}]}}
,{"id":28606,"text":"wri834204 - 1983 - Hydrogeologic data from the US Geological Survey test wells near Waycross, Ware County, Georgia","interactions":[],"lastModifiedDate":"2021-01-27T19:08:55.570722","indexId":"wri834204","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":"83-4204","title":"Hydrogeologic data from the US Geological Survey test wells near Waycross, Ware County, Georgia","docAbstract":"Two wells were constructed near Waycross, Ware County, Georgia, from July 1980 to May 1981 to collect stratigraphic, structural, geophysical, hydrologic, hydraulic, and geochemical information for the U.S. Geological Survey Tertiary Limestone Regional Aquifer-System Analysis. Data collection included geologic sampling and coring, borehole geophysical logging, packer testing, water-level measuring, water-quality sampling, and aquifer testing. In the study area, the Tertiary limestone aquifer system is about 1,300 feet thick and is confined and overlain by about 610 feet of clastic sediments. The aquifer system consists of limestone, dolomite, and minor evaporites and has high porosity and permeability. A 4-day continuous discharge aquifer test was conducted, from which a transmissivity of about 1 million feet squared per day and a storage coefficient of 0.0001 were calculated. Water from the upper part of the aquifer is of a calcium bicarbonate type. The deeper highly mineralized zone produces a sodium bicarbonate type water in which concentrations of magnesium, sulfate, chloride, sodium, and some trace metals increase with depth. 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,{"id":27729,"text":"wri824059 - 1983 - Use of digital land-cover data from the Landsat satellite in estimating streamflow characteristics in the Cumberland Plateau of Tennessee","interactions":[],"lastModifiedDate":"2017-03-29T14:35:11","indexId":"wri824059","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":"82-4059","title":"Use of digital land-cover data from the Landsat satellite in estimating streamflow characteristics in the Cumberland Plateau of Tennessee","docAbstract":"Streamflow may be estimated with regression equations that relate streamflow characteristics to characteristics of the drainage basin. A statistical experiment was performed to compare the accuracy of equations using basin characteristics derived from maps and climatological records (control group equations) with the accuracy of equations using basin characteristics derived from Landsat data as well as maps and climatological records (experimental group equations). Results show that when the equations in both groups are arranged into six flow categories, there is no substantial difference in accuracy between control group equations and experimental group equations for this particular site where drainage area accounts for more than 90 percent of the variance in all streamflow characteristics (except low flows and most annual peak logarithms). (USGS)","language":"English","publisher":"U.S. Geological Survey","doi":"10.3133/wri824059","usgsCitation":"Hollyday, E., and Hansen, G., 1983, Use of digital land-cover data from the Landsat satellite in estimating streamflow characteristics in the Cumberland Plateau of Tennessee: U.S. Geological Survey Water-Resources Investigations Report 82-4059, v, 48 p., https://doi.org/10.3133/wri824059.","productDescription":"v, 48 p.","costCenters":[{"id":222,"text":"Earth Resources Observation and Science (EROS) Center","active":true,"usgs":true}],"links":[{"id":158788,"rank":0,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/thumbnails/usgs_thumb.jpg"},{"id":2116,"rank":100,"type":{"id":15,"text":"Index Page"},"url":"https://pubs.water.usgs.gov/wri824059","linkFileType":{"id":5,"text":"html"}},{"id":338667,"rank":3,"type":{"id":11,"text":"Document"},"url":"https://pubs.usgs.gov/wri/wri824059/pdf/wrir_82-4059_a.pdf"}],"noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"4f4e4a17e4b07f02db604670","contributors":{"authors":[{"text":"Hollyday, E. F.","contributorId":95062,"corporation":false,"usgs":true,"family":"Hollyday","given":"E. F.","affiliations":[],"preferred":false,"id":198604,"contributorType":{"id":1,"text":"Authors"},"rank":1},{"text":"Hansen, G.R.","contributorId":68785,"corporation":false,"usgs":true,"family":"Hansen","given":"G.R.","email":"","affiliations":[],"preferred":false,"id":198603,"contributorType":{"id":1,"text":"Authors"},"rank":2}]}}
,{"id":10335,"text":"ofr821061 - 1983 - Preliminary geologic map of the Coolin area","interactions":[],"lastModifiedDate":"2021-11-19T22:38:11.434816","indexId":"ofr821061","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":"82-1061","title":"Preliminary geologic map of the Coolin area","docAbstract":"<p>No abstract available.</p>","language":"English","publisher":"U.S. Geological Survey","doi":"10.3133/ofr821061","usgsCitation":"Miller, F.K., 1983, Preliminary geologic map of the Coolin area: U.S. Geological Survey Open-File Report 82-1061, Report: 20 p.; 1 Plate: 24.18 × 35.29 inches, https://doi.org/10.3133/ofr821061.","productDescription":"Report: 20 p.; 1 Plate: 24.18 × 35.29 inches","costCenters":[],"links":[{"id":391962,"rank":4,"type":{"id":36,"text":"NGMDB Index Page"},"url":"https://ngmdb.usgs.gov/Prodesc/proddesc_13635.htm"},{"id":38188,"rank":300,"type":{"id":11,"text":"Document"},"url":"https://pubs.usgs.gov/of/1982/1061/report.pdf","linkFileType":{"id":1,"text":"pdf"}},{"id":38187,"rank":400,"type":{"id":17,"text":"Plate"},"url":"https://pubs.usgs.gov/of/1982/1061/plate-1.pdf","linkFileType":{"id":1,"text":"pdf"}},{"id":143502,"rank":0,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/of/1982/1061/report-thumb.jpg"}],"country":"United States","state":"Idaho","otherGeospatial":"Coolin area","geographicExtents":"{\n  \"type\": \"FeatureCollection\",\n  \"features\": [\n    {\n      \"type\": \"Feature\",\n      \"properties\": {},\n      \"geometry\": {\n        \"type\": \"Polygon\",\n        \"coordinates\": [\n          [\n            [\n              -117,\n              48.25\n            ],\n            [\n              -116.75,\n              48.25\n            ],\n            [\n              -116.75,\n              48.5\n            ],\n            [\n              -117,\n              48.5\n            ],\n            [\n              -117,\n              48.25\n            ]\n          ]\n        ]\n      }\n    }\n  ]\n}","noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"4f4e4ac8e4b07f02db67bada","contributors":{"authors":[{"text":"Miller, Fred K.","contributorId":89503,"corporation":false,"usgs":true,"family":"Miller","given":"Fred","email":"","middleInitial":"K.","affiliations":[],"preferred":false,"id":161214,"contributorType":{"id":1,"text":"Authors"},"rank":1}]}}
,{"id":4469,"text":"cir902A - 1983 - Petroleum resource assessments of the wilderness lands in the western United States; Petroleum potential of wilderness lands in the Western United States","interactions":[],"lastModifiedDate":"2012-02-02T00:05:43","indexId":"cir902A","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":"902","chapter":"A","title":"Petroleum resource assessments of the wilderness lands in the western United States; Petroleum potential of wilderness lands in the Western United States","language":"ENGLISH","publisher":"U.S. Dept. of the Interior, Geological Survey,","doi":"10.3133/cir902A","usgsCitation":"Miller, B., 1983, Petroleum resource assessments of the wilderness lands in the western United States; Petroleum potential of wilderness lands in the Western United States: U.S. Geological Survey Circular 902, iii, A1-A10 p. :ill., maps ;26 cm.26 cm., https://doi.org/10.3133/cir902A.","productDescription":"iii, A1-A10 p. :ill., maps ;26 cm.26 cm.","costCenters":[],"links":[{"id":139685,"rank":0,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/circ/1983/0902a/report-thumb.jpg"},{"id":112509,"rank":300,"type":{"id":11,"text":"Document"},"url":"https://pubs.usgs.gov/circ/1983/0902a/report.pdf","size":"865","linkFileType":{"id":1,"text":"pdf"}}],"noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"4f4e4adfe4b07f02db6877c7","contributors":{"authors":[{"text":"Miller, Betty M.","contributorId":92231,"corporation":false,"usgs":true,"family":"Miller","given":"Betty M.","affiliations":[],"preferred":false,"id":149295,"contributorType":{"id":1,"text":"Authors"},"rank":1}]}}
,{"id":4470,"text":"cir902B - 1983 - Digital cartography; petroleum potential of wilderness lands in the Western United States","interactions":[],"lastModifiedDate":"2012-02-02T00:05:43","indexId":"cir902B","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":"902","chapter":"B","title":"Digital cartography; petroleum potential of wilderness lands in the Western United States","language":"ENGLISH","publisher":"U.S. Dept. of the Interior, Geological Survey,","doi":"10.3133/cir902B","usgsCitation":"Domaratz, M.A., and Stapleton, J.A., 1983, Digital cartography; petroleum potential of wilderness lands in the Western United States: U.S. Geological Survey Circular 902, iii, B1-B4 p. ;26 cm.26 cm., https://doi.org/10.3133/cir902B.","productDescription":"iii, B1-B4 p. ;26 cm.26 cm.","costCenters":[],"links":[{"id":139686,"rank":0,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/circ/1983/0902b/report-thumb.jpg"},{"id":112510,"rank":300,"type":{"id":11,"text":"Document"},"url":"https://pubs.usgs.gov/circ/1983/0902b/report.pdf","size":"391","linkFileType":{"id":1,"text":"pdf"}}],"noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"4f4e4a9ae4b07f02db65d577","contributors":{"authors":[{"text":"Domaratz, Michael A. mdomaratz@usgs.gov","contributorId":5233,"corporation":false,"usgs":true,"family":"Domaratz","given":"Michael","email":"mdomaratz@usgs.gov","middleInitial":"A.","affiliations":[],"preferred":true,"id":149296,"contributorType":{"id":1,"text":"Authors"},"rank":1},{"text":"Stapleton, Jo Anne","contributorId":34908,"corporation":false,"usgs":true,"family":"Stapleton","given":"Jo","email":"","middleInitial":"Anne","affiliations":[],"preferred":false,"id":149297,"contributorType":{"id":1,"text":"Authors"},"rank":2}]}}
,{"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":4471,"text":"cir902H - 1983 - Petroleum potential of wilderness lands in Nevada","interactions":[{"subject":{"id":4471,"text":"cir902H - 1983 - Petroleum potential of wilderness lands in Nevada","indexId":"cir902H","publicationYear":"1983","noYear":false,"chapter":"H","title":"Petroleum potential of wilderness lands in Nevada"},"predicate":"IS_PART_OF","object":{"id":4364,"text":"cir902AP - 1983 - Petroleum potential of wilderness lands in the Western United States","indexId":"cir902AP","publicationYear":"1983","noYear":false,"chapter":"A-P","title":"Petroleum potential of wilderness lands in the Western United States"},"id":1}],"isPartOf":{"id":4364,"text":"cir902AP - 1983 - Petroleum potential of wilderness lands in the Western United States","indexId":"cir902AP","publicationYear":"1983","noYear":false,"title":"Petroleum potential of wilderness lands in the Western United 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,{"id":9307,"text":"ofr83531 - 1983 - Water-resources studies in Utah by the U.S. Geological Survey, July 1, 1982 to June 30, 1983","interactions":[],"lastModifiedDate":"2017-09-01T14:41:43","indexId":"ofr83531","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":"83-531","title":"Water-resources studies in Utah by the U.S. Geological Survey, July 1, 1982 to June 30, 1983","docAbstract":"<p>This report summarizes the progress on water-resources studies in Utah by the U.S. Geological Survey during the period July 1, 1982, to June 30, 1983. Much of the work was done in cooperation with the State of Utah and local agencies. Additional supporting funds were transferred from other Federal agencies or appropriated directly to the Geological Survey.</p>","language":"English","publisher":"U.S. Geological Survey","publisherLocation":"Salt Lake City, UT","doi":"10.3133/ofr83531","usgsCitation":"1983, Water-resources studies in Utah by the U.S. Geological Survey, July 1, 1982 to June 30, 1983: U.S. Geological Survey Open-File Report 83-531, 49, https://doi.org/10.3133/ofr83531.","productDescription":"49","numberOfPages":"51","costCenters":[{"id":610,"text":"Utah Water Science Center","active":true,"usgs":true}],"links":[{"id":37022,"rank":300,"type":{"id":11,"text":"Document"},"url":"https://pubs.usgs.gov/of/1983/0531/report.pdf","linkFileType":{"id":1,"text":"pdf"}},{"id":140917,"rank":0,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/of/1983/0531/report-thumb.jpg"}],"country":"United States","state":"Utah","noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"4f4e48c8e4b07f02db5413f6","contributors":{"compilers":[{"text":"Hamblin, Linda S.","contributorId":52202,"corporation":false,"usgs":true,"family":"Hamblin","given":"Linda","email":"","middleInitial":"S.","affiliations":[],"preferred":false,"id":659124,"contributorType":{"id":3,"text":"Compilers"},"rank":1}]}}
,{"id":18664,"text":"ofr8411 - 1983 - Analytical results and sample locality map of stream-sediment and panned-concentrate samples from the Inyo Mountains (CDCA 122), Hunter Mountains (CDCA 123), Panamint (CDCA 127), and Wildrose (CDCA 134) Wilderness Study Areas, Inyo County, California","interactions":[],"lastModifiedDate":"2023-08-30T20:58:34.836281","indexId":"ofr8411","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":"84-11","title":"Analytical results and sample locality map of stream-sediment and panned-concentrate samples from the Inyo Mountains (CDCA 122), Hunter Mountains (CDCA 123), Panamint (CDCA 127), and Wildrose (CDCA 134) Wilderness Study Areas, Inyo County, California","docAbstract":"<p>No abstract available.</p>","language":"English","publisher":"U.S. Geological Survey","doi":"10.3133/ofr8411","usgsCitation":"Detra, D., Kilburn, J., and Chazin, B., 1983, Analytical results and sample locality map of stream-sediment and panned-concentrate samples from the Inyo Mountains (CDCA 122), Hunter Mountains (CDCA 123), Panamint (CDCA 127), and Wildrose (CDCA 134) Wilderness Study Areas, Inyo County, California: U.S. Geological Survey Open-File Report 84-11, Report: i, 58.; 1 Plate: 22.61 x 29.82 inches, https://doi.org/10.3133/ofr8411.","productDescription":"Report: i, 58.; 1 Plate: 22.61 x 29.82 inches","costCenters":[],"links":[{"id":420336,"rank":4,"type":{"id":36,"text":"NGMDB Index Page"},"url":"https://ngmdb.usgs.gov/Prodesc/proddesc_12907.htm","linkFileType":{"id":5,"text":"html"}},{"id":48002,"rank":2,"type":{"id":11,"text":"Document"},"url":"https://pubs.usgs.gov/of/1984/0011/report.pdf","linkFileType":{"id":1,"text":"pdf"}},{"id":48001,"rank":3,"type":{"id":17,"text":"Plate"},"url":"https://pubs.usgs.gov/of/1984/0011/plate-1.pdf","linkFileType":{"id":1,"text":"pdf"}},{"id":150682,"rank":1,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/of/1984/0011/report-thumb.jpg"}],"country":"United States","state":"California","county":"Inyo County","geographicExtents":"{\n  \"type\": \"FeatureCollection\",\n  \"features\": [\n    {\n      \"type\": \"Feature\",\n      \"properties\": {},\n      \"geometry\": {\n        \"coordinates\": [\n          [\n            [\n              -118,\n              37\n            ],\n            [\n              -118,\n              36.25\n            ],\n            [\n              -117.25,\n              36.25\n            ],\n            [\n              -117.25,\n              37\n            ],\n            [\n              -118,\n              37\n            ]\n          ]\n        ],\n        \"type\": \"Polygon\"\n      }\n    }\n  ]\n}","noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"4f4e4acce4b07f02db67eba2","contributors":{"authors":[{"text":"Detra, D.E.","contributorId":72358,"corporation":false,"usgs":true,"family":"Detra","given":"D.E.","email":"","affiliations":[],"preferred":false,"id":179521,"contributorType":{"id":1,"text":"Authors"},"rank":1},{"text":"Kilburn, J.E.","contributorId":42205,"corporation":false,"usgs":true,"family":"Kilburn","given":"J.E.","email":"","affiliations":[],"preferred":false,"id":179519,"contributorType":{"id":1,"text":"Authors"},"rank":2},{"text":"Chazin, B.","contributorId":43043,"corporation":false,"usgs":true,"family":"Chazin","given":"B.","affiliations":[],"preferred":false,"id":179520,"contributorType":{"id":1,"text":"Authors"},"rank":3}]}}
,{"id":9467,"text":"ofr83873 - 1983 - Water quality data for selected streams tributary to the tidal Potomac River and Estuary, Maryland and Virginia, 1979-81 water years","interactions":[],"lastModifiedDate":"2012-02-02T00:06:17","indexId":"ofr83873","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":"83-873","title":"Water quality data for selected streams tributary to the tidal Potomac River and Estuary, Maryland and Virginia, 1979-81 water years","docAbstract":"Observations of the physical, chemical, and biological water quality of five streams draining to the tidal Potomac River and Estuary during the 1979-81 water years are tabulated. The streams sampled are Rock Creek, the Northwest and Northeast Branches of the Anacostia River, the Occoquan River, and St. Clements Creek. Samples, usually collected during storms, were routinely analyzed for sediment, biochemical oxygen demand, dissolved silica, and the total and dissolved forms of phosphorus and of nitrogen species. Additional analyses for specific conductance, chlorophyll-a, and phytoplankton abundance and generic composition were done on a few samples taken during the 1980 water year. Observations of water temperature were made during the same period. Selected measurements of the turbidity of the raw water intake for the Occoquan Water Treatment Plant also are included. (Author 's abstract)","language":"ENGLISH","publisher":"U.S. Geological Survey,","doi":"10.3133/ofr83873","usgsCitation":"Hickman, R., 1983, Water quality data for selected streams tributary to the tidal Potomac River and Estuary, Maryland and Virginia, 1979-81 water years: U.S. Geological Survey Open-File Report 83-873, ii, 69 p. :map ;28 cm., https://doi.org/10.3133/ofr83873.","productDescription":"ii, 69 p. :map ;28 cm.","costCenters":[],"links":[{"id":142640,"rank":0,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/of/1983/0873/report-thumb.jpg"},{"id":37169,"rank":300,"type":{"id":11,"text":"Document"},"url":"https://pubs.usgs.gov/of/1983/0873/report.pdf","linkFileType":{"id":1,"text":"pdf"}}],"noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"4f4e4a07e4b07f02db5f9b82","contributors":{"authors":[{"text":"Hickman, R.E.","contributorId":30230,"corporation":false,"usgs":true,"family":"Hickman","given":"R.E.","email":"","affiliations":[],"preferred":false,"id":159738,"contributorType":{"id":1,"text":"Authors"},"rank":1}]}}
,{"id":29005,"text":"wri834020 - 1983 - Initial assessment of time of travel and mixing through Gulf Island Pond and the lower Androscoggin River, Maine","interactions":[],"lastModifiedDate":"2012-02-02T00:08:52","indexId":"wri834020","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":"83-4020","title":"Initial assessment of time of travel and mixing through Gulf Island Pond and the lower Androscoggin River, Maine","docAbstract":"Flow-stratification patterns were observed in Gulf Island Pond during time-of-travel studies in May and August 1980. The stratification patterns in this 70 million cubic-meter impoundment were due to a temperature differences between inflowing water and reservoir water. Separation was observed at temperature differences of 0.5 degrees C in May 1980 and 1.0 degrees C in August 1980. The pathway taken by inflowing water through the reservoir was governed by the temperature-related density forces acting between the two water masses. Data collected during August 1980 to define differences in dye concentrations with depth at two fixed profile points in Gulf Island Pond showed average water velocity to be seven times faster near the bottom than near the surface. A concept of mass flow was used to analyze data collected at sites downstream from Gulf Island Dam where flow varied rapidly with time. This report presents the mathematical derivation of controid traveltime, skewness, and percentage recovery of dye mass as determined from mass versus time curves. (USGS)","language":"ENGLISH","publisher":"U.S. Geological Survey,","doi":"10.3133/wri834020","usgsCitation":"Parker, G., and Hunt, G., 1983, Initial assessment of time of travel and mixing through Gulf Island Pond and the lower Androscoggin River, Maine: U.S. Geological Survey Water-Resources Investigations Report 83-4020, vii, 60 p. :ill., maps ;28 cm., https://doi.org/10.3133/wri834020.","productDescription":"vii, 60 p. :ill., maps ;28 cm.","costCenters":[],"links":[{"id":123299,"rank":0,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/wri/1983/4020/report-thumb.jpg"},{"id":57872,"rank":300,"type":{"id":11,"text":"Document"},"url":"https://pubs.usgs.gov/wri/1983/4020/report.pdf","linkFileType":{"id":1,"text":"pdf"}}],"noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"4f4e49c1e4b07f02db5d33cb","contributors":{"authors":[{"text":"Parker, G.W.","contributorId":100374,"corporation":false,"usgs":true,"family":"Parker","given":"G.W.","email":"","affiliations":[],"preferred":false,"id":200775,"contributorType":{"id":1,"text":"Authors"},"rank":1},{"text":"Hunt, G.S.","contributorId":20360,"corporation":false,"usgs":true,"family":"Hunt","given":"G.S.","email":"","affiliations":[],"preferred":false,"id":200774,"contributorType":{"id":1,"text":"Authors"},"rank":2}]}}
,{"id":61548,"text":"mf1617A - 1983 - Mineral resource potential map of the Tuolumne River Roadless Area, Tuolumne County, California","interactions":[],"lastModifiedDate":"2012-02-10T00:10:50","indexId":"mf1617A","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":"1617","chapter":"A","title":"Mineral resource potential map of the Tuolumne River Roadless Area, Tuolumne County, California","language":"ENGLISH","doi":"10.3133/mf1617A","usgsCitation":"Harner, J., Seitz, J.F., Plouff, D., and Hyndman, P.C., 1983, Mineral resource potential map of the Tuolumne River Roadless Area, Tuolumne County, California: U.S. Geological Survey Miscellaneous Field Studies Map 1617, 1 map ;32 x 40 cm., on sheet 62 x 85 cm., folded in envelope 25 x 32 cm. +1 pamphlet (13 p. : ill., maps ; 28 cm.), https://doi.org/10.3133/mf1617A.","productDescription":"1 map ;32 x 40 cm., on sheet 62 x 85 cm., folded in envelope 25 x 32 cm. +1 pamphlet (13 p. : ill., maps ; 28 cm.)","costCenters":[],"links":[{"id":106195,"rank":700,"type":{"id":15,"text":"Index Page"},"url":"https://ngmdb.usgs.gov/Prodesc/proddesc_7700.htm","linkFileType":{"id":5,"text":"html"},"description":"7700"},{"id":187305,"rank":0,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/mf/1983/1617a/report-thumb.jpg"},{"id":88982,"rank":400,"type":{"id":17,"text":"Plate"},"url":"https://pubs.usgs.gov/mf/1983/1617a/plate-1.pdf","linkFileType":{"id":1,"text":"pdf"}},{"id":88983,"rank":300,"type":{"id":11,"text":"Document"},"url":"https://pubs.usgs.gov/mf/1983/1617a/report.pdf","linkFileType":{"id":1,"text":"pdf"}}],"scale":"0","geographicExtents":"{ \"type\": \"FeatureCollection\", \"features\": [ { \"type\": \"Feature\", \"properties\": {}, \"geometry\": { \"type\": \"Polygon\", \"coordinates\": [ [ [ -120.25,37.833333333333336 ], [ -120.25,37.916666666666664 ], [ -120,37.916666666666664 ], [ -120,37.833333333333336 ], [ -120.25,37.833333333333336 ] ] ] } } ] }","noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"4f4e4a60e4b07f02db63567a","contributors":{"authors":[{"text":"Harner, J.L.","contributorId":108111,"corporation":false,"usgs":true,"family":"Harner","given":"J.L.","email":"","affiliations":[],"preferred":false,"id":265982,"contributorType":{"id":1,"text":"Authors"},"rank":1},{"text":"Seitz, J. F.","contributorId":92250,"corporation":false,"usgs":true,"family":"Seitz","given":"J.","email":"","middleInitial":"F.","affiliations":[],"preferred":false,"id":265979,"contributorType":{"id":1,"text":"Authors"},"rank":2},{"text":"Plouff, Donald","contributorId":94657,"corporation":false,"usgs":true,"family":"Plouff","given":"Donald","email":"","affiliations":[],"preferred":false,"id":265980,"contributorType":{"id":1,"text":"Authors"},"rank":3},{"text":"Hyndman, P. C.","contributorId":96257,"corporation":false,"usgs":true,"family":"Hyndman","given":"P.","email":"","middleInitial":"C.","affiliations":[],"preferred":false,"id":265981,"contributorType":{"id":1,"text":"Authors"},"rank":4}]}}
,{"id":4472,"text":"cir902I - 1983 - Petroleum potential of wilderness lands in New Mexico","interactions":[{"subject":{"id":4472,"text":"cir902I - 1983 - Petroleum potential of wilderness lands in New Mexico","indexId":"cir902I","publicationYear":"1983","noYear":false,"chapter":"I","title":"Petroleum potential of wilderness lands in New Mexico"},"predicate":"IS_PART_OF","object":{"id":4364,"text":"cir902AP - 1983 - Petroleum potential of wilderness lands in the Western United States","indexId":"cir902AP","publicationYear":"1983","noYear":false,"chapter":"A-P","title":"Petroleum potential of wilderness lands in the Western United States"},"id":1}],"isPartOf":{"id":4364,"text":"cir902AP - 1983 - Petroleum potential of wilderness lands in the Western United States","indexId":"cir902AP","publicationYear":"1983","noYear":false,"title":"Petroleum potential of wilderness lands in the Western United 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