{"pageNumber":"5349","pageRowStart":"133700","pageSize":"25","recordCount":184769,"records":[{"id":40900,"text":"ofr82563 - 1982 - Potentiometric-surface map of water in the Lakota Formation and equivalent units in the northern Great Plains area of Montana","interactions":[],"lastModifiedDate":"2023-01-17T22:48:21.683468","indexId":"ofr82563","displayToPublicDate":"1994-01-01T00:00:00","publicationYear":"1982","noYear":false,"publicationType":{"id":18,"text":"Report"},"publicationSubtype":{"id":5,"text":"USGS Numbered Series"},"seriesTitle":{"id":330,"text":"Open-File Report","code":"OFR","onlineIssn":"2331-1258","printIssn":"0196-1497","active":true,"publicationSubtype":{"id":5}},"seriesNumber":"82-563","title":"Potentiometric-surface map of water in the Lakota Formation and equivalent units in the northern Great Plains area of Montana","docAbstract":"The potentiometric surface of water in the lower Cretaceous Lakota Formation and equivalent units (Cut Bank Sandstone Member , Sunburst Sandstone Member, and Moulton Member of Kootenai formation; Third Cat Creek sandstone of Kootenai Formation; Pryor Conglomerate Member of Kootenai Formation) is shown on a base at a scale of 1:1,000,000. The map is one of a series produced as part of a regional study of aquifers of Cenozoic and Mesozoic age in the northern Great Plains of Montana. The contour interval is 200 feet. Water in the Lakota Formation and equivalent units occurs under water-table and artesian conditions. The direction of regional groundwater movement is east and north from the recharge areas in the Little Belt and Big Snowy Mountains. The average discharge from 20 wells is about 29 gallons per minute and the specific capacity of 18 wells averages 0.75 gallon per minute per foot of drawdown.","language":"English","publisher":"U.S. Geological Survey","doi":"10.3133/ofr82563","usgsCitation":"Levings, G.W., 1982, Potentiometric-surface map of water in the Lakota Formation and equivalent units in the northern Great Plains area of Montana: U.S. Geological Survey Open-File Report 82-563, 1 Plate: 39.76 x 23.47 inches, https://doi.org/10.3133/ofr82563.","productDescription":"1 Plate: 39.76 x 23.47 inches","costCenters":[],"links":[{"id":172092,"rank":1,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/thumbnails/usgs_thumb.jpg"},{"id":412007,"rank":3,"type":{"id":36,"text":"NGMDB Index Page"},"url":"https://ngmdb.usgs.gov/Prodesc/proddesc_75641.htm","linkFileType":{"id":5,"text":"html"}},{"id":78782,"rank":2,"type":{"id":17,"text":"Plate"},"url":"https://pubs.usgs.gov/of/1982/0563/plate-1.pdf","linkFileType":{"id":1,"text":"pdf"}}],"country":"United States","state":"Montana","otherGeospatial":"northern Great Plains area","geographicExtents":"{\n  \"type\": \"FeatureCollection\",\n  \"features\": [\n    {\n      \"type\": \"Feature\",\n      \"properties\": {},\n      \"geometry\": {\n        \"coordinates\": [\n          [\n            [\n              -106.5,\n              49\n            ],\n            [\n              -112.4167,\n              49\n            ],\n            [\n              -112.4167,\n              45\n            ],\n            [\n              -106.5,\n              45\n            ],\n            [\n              -106.5,\n              49\n            ]\n          ]\n        ],\n        \"type\": \"Polygon\"\n      }\n    }\n  ]\n}","noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"4f4e4ad3e4b07f02db6828a9","contributors":{"authors":[{"text":"Levings, Gary Wayne","contributorId":89591,"corporation":false,"usgs":true,"family":"Levings","given":"Gary","email":"","middleInitial":"Wayne","affiliations":[],"preferred":false,"id":224138,"contributorType":{"id":1,"text":"Authors"},"rank":1}]}}
,{"id":69597,"text":"i1538 - 1982 - Petroleum potential of wilderness lands, California","interactions":[],"lastModifiedDate":"2025-08-04T20:14:48.69674","indexId":"i1538","displayToPublicDate":"1994-01-01T00:00:00","publicationYear":"1982","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":"1538","title":"Petroleum potential of wilderness lands, California","docAbstract":"<p>No abstract available.</p>","language":"English","publisher":"U.S. Geological Survey","doi":"10.3133/i1538","isbn":"0607786728","usgsCitation":"Scott, E.W., 1982, Petroleum potential of wilderness lands, California: U.S. Geological Survey IMAP 1538, 1 Plate: 38.81 x 44.96 inches, https://doi.org/10.3133/i1538.","productDescription":"1 Plate: 38.81 x 44.96 inches","costCenters":[],"links":[{"id":493496,"rank":4,"type":{"id":36,"text":"NGMDB 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 \"}}]}","noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"4f4e4ae0e4b07f02db687dbe","contributors":{"authors":[{"text":"Scott, E. W.","contributorId":7257,"corporation":false,"usgs":true,"family":"Scott","given":"E.","middleInitial":"W.","affiliations":[],"preferred":false,"id":280697,"contributorType":{"id":1,"text":"Authors"},"rank":1}]}}
,{"id":42855,"text":"ofr821127 - 1982 - Reconnaissance geologic map of the Tum Tum Lake Quadrangle, Harney County, Oregon","interactions":[],"lastModifiedDate":"2012-02-02T00:05:03","indexId":"ofr821127","displayToPublicDate":"1994-01-01T00:00:00","publicationYear":"1982","noYear":false,"publicationType":{"id":18,"text":"Report"},"publicationSubtype":{"id":5,"text":"USGS Numbered Series"},"seriesTitle":{"id":330,"text":"Open-File Report","code":"OFR","onlineIssn":"2331-1258","printIssn":"0196-1497","active":true,"publicationSubtype":{"id":5}},"seriesNumber":"82-1127","title":"Reconnaissance geologic map of the Tum Tum Lake Quadrangle, Harney County, Oregon","language":"ENGLISH","doi":"10.3133/ofr821127","usgsCitation":"Rytuba, J.J., Vander Meulen, D., Vercoutere, T., Minor, S., Caress, M., and Kriens, B., 1982, Reconnaissance geologic map of the Tum Tum Lake Quadrangle, Harney County, Oregon: U.S. Geological Survey Open-File Report 82-1127, 1 map ;58 x 43 cm., https://doi.org/10.3133/ofr821127.","productDescription":"1 map ;58 x 43 cm.","costCenters":[],"links":[{"id":108425,"rank":700,"type":{"id":15,"text":"Index Page"},"url":"https://ngmdb.usgs.gov/Prodesc/proddesc_13657.htm","linkFileType":{"id":5,"text":"html"},"description":"13657"},{"id":136484,"rank":0,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/thumbnails/usgs_thumb.jpg"},{"id":80685,"rank":400,"type":{"id":17,"text":"Plate"},"url":"https://pubs.usgs.gov/of/1982/1127/plate-1.pdf","linkFileType":{"id":1,"text":"pdf"}}],"noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"4f4e4a70e4b07f02db641237","contributors":{"authors":[{"text":"Rytuba, James J. jrytuba@usgs.gov","contributorId":3043,"corporation":false,"usgs":true,"family":"Rytuba","given":"James","email":"jrytuba@usgs.gov","middleInitial":"J.","affiliations":[{"id":312,"text":"Geology, Minerals, Energy, and Geophysics Science Center","active":true,"usgs":true}],"preferred":true,"id":227265,"contributorType":{"id":1,"text":"Authors"},"rank":1},{"text":"Vander Meulen, D. B.","contributorId":30958,"corporation":false,"usgs":true,"family":"Vander Meulen","given":"D. B.","affiliations":[],"preferred":false,"id":227266,"contributorType":{"id":1,"text":"Authors"},"rank":2},{"text":"Vercoutere, T. L.","contributorId":102445,"corporation":false,"usgs":true,"family":"Vercoutere","given":"T. L.","affiliations":[],"preferred":false,"id":227269,"contributorType":{"id":1,"text":"Authors"},"rank":3},{"text":"Minor, S.A.","contributorId":65047,"corporation":false,"usgs":true,"family":"Minor","given":"S.A.","email":"","affiliations":[],"preferred":false,"id":227267,"contributorType":{"id":1,"text":"Authors"},"rank":4},{"text":"Caress, M.E.","contributorId":99104,"corporation":false,"usgs":true,"family":"Caress","given":"M.E.","email":"","affiliations":[],"preferred":false,"id":227268,"contributorType":{"id":1,"text":"Authors"},"rank":5},{"text":"Kriens, B.J.","contributorId":104869,"corporation":false,"usgs":true,"family":"Kriens","given":"B.J.","affiliations":[],"preferred":false,"id":227270,"contributorType":{"id":1,"text":"Authors"},"rank":6}]}}
,{"id":23339,"text":"ofr82686 - 1982 - Summary of hydrologic data collected at Wytheville National Fish Hatchery No. 2, Max Meadows, Virginia, 1976 to 1979","interactions":[],"lastModifiedDate":"2012-02-02T00:08:11","indexId":"ofr82686","displayToPublicDate":"1994-01-01T00:00:00","publicationYear":"1982","noYear":false,"publicationType":{"id":18,"text":"Report"},"publicationSubtype":{"id":5,"text":"USGS Numbered Series"},"seriesTitle":{"id":330,"text":"Open-File Report","code":"OFR","onlineIssn":"2331-1258","printIssn":"0196-1497","active":true,"publicationSubtype":{"id":5}},"seriesNumber":"82-686","title":"Summary of hydrologic data collected at Wytheville National Fish Hatchery No. 2, Max Meadows, Virginia, 1976 to 1979","docAbstract":"Construction of a section of Interstate Highway 77 through Glade Creek basin in Wythe County, southwestern Virginia, raised concern about its effect on two springs and a well that supply water to a fish hatchery in the basin. Discharge of Glade Creek and the two springs, turbidity of the springs, water levels in the well, water temperature, and chemical quality of the springs and well were monitored during construction and for 6 months after completion of the highway. Analyses of the data showed no trends, anomalies, or changes in quality of water that could be related either to construction activities or to the presence and use of the completed highway.","language":"ENGLISH","publisher":"The Division,","doi":"10.3133/ofr82686","issn":"0094-9140","usgsCitation":"Hendrick, W.E., 1982, Summary of hydrologic data collected at Wytheville National Fish Hatchery No. 2, Max Meadows, Virginia, 1976 to 1979: U.S. Geological Survey Open-File Report 82-686, 28 p. :ill., maps ;28 cm., https://doi.org/10.3133/ofr82686.","productDescription":"28 p. :ill., maps ;28 cm.","costCenters":[],"links":[{"id":156141,"rank":0,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/of/1982/0686/report-thumb.jpg"},{"id":52638,"rank":300,"type":{"id":11,"text":"Document"},"url":"https://pubs.usgs.gov/of/1982/0686/report.pdf","linkFileType":{"id":1,"text":"pdf"}}],"noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"4f4e4b04e4b07f02db69917a","contributors":{"authors":[{"text":"Hendrick, Walter E.","contributorId":83155,"corporation":false,"usgs":true,"family":"Hendrick","given":"Walter","email":"","middleInitial":"E.","affiliations":[],"preferred":false,"id":189934,"contributorType":{"id":1,"text":"Authors"},"rank":1}]}}
,{"id":56647,"text":"fwsobs82_10_29 - 1982 - Habitat Suitability Index Models: Eastern meadowlark","interactions":[],"lastModifiedDate":"2022-01-21T18:47:59.909281","indexId":"fwsobs82_10_29","displayToPublicDate":"1994-01-01T00:00:00","publicationYear":"1982","noYear":false,"publicationType":{"id":18,"text":"Report"},"publicationSubtype":{"id":1,"text":"Federal Government Series"},"seriesTitle":{"id":20,"text":"FWS/OBS","active":false,"publicationSubtype":{"id":1}},"seriesNumber":"82/10.29","subseriesTitle":"Habitat Suitability Index","title":"Habitat Suitability Index Models: Eastern meadowlark","docAbstract":"Habitat preferences of the eastern meadowlark (Sturnella magna) are described in this publication, which is one of a series of Habitat Suitability Index (HSI) models. Habitat use information is presented in a synthesis of the literature on the species-habitat requirements of the eastern meadowlark, followed by the development of the HSI model. The model is presented in three formats: graphic, word, and mathematical, and is designed to provide information for use in impact assessment and habitat management activities.","language":"English","publisher":"U.S. Fish and Wildlife Service","usgsCitation":"Schroeder, R.L., and Sousa, P.J., 1982, Habitat Suitability Index Models: Eastern meadowlark: FWS/OBS 82/10.29, vi, 9 p.","productDescription":"vi, 9 p.","costCenters":[{"id":595,"text":"U.S. Geological Survey","active":false,"usgs":true}],"links":[{"id":180941,"rank":0,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/thumbnails/outside_thumb.jpg"}],"noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"4f4e4a80e4b07f02db64999f","contributors":{"authors":[{"text":"Schroeder, Richard L.","contributorId":10368,"corporation":false,"usgs":true,"family":"Schroeder","given":"Richard","email":"","middleInitial":"L.","affiliations":[],"preferred":false,"id":255592,"contributorType":{"id":1,"text":"Authors"},"rank":1},{"text":"Sousa, Patrick J.","contributorId":19206,"corporation":false,"usgs":true,"family":"Sousa","given":"Patrick","email":"","middleInitial":"J.","affiliations":[],"preferred":false,"id":255593,"contributorType":{"id":1,"text":"Authors"},"rank":2}]}}
,{"id":7862,"text":"ofr82999 - 1982 - FLOWCHART; a computer program for plotting flowcharts","interactions":[],"lastModifiedDate":"2012-02-02T00:06:05","indexId":"ofr82999","displayToPublicDate":"1994-01-01T00:00:00","publicationYear":"1982","noYear":false,"publicationType":{"id":18,"text":"Report"},"publicationSubtype":{"id":5,"text":"USGS Numbered Series"},"seriesTitle":{"id":330,"text":"Open-File Report","code":"OFR","onlineIssn":"2331-1258","printIssn":"0196-1497","active":true,"publicationSubtype":{"id":5}},"seriesNumber":"82-999","title":"FLOWCHART; a computer program for plotting flowcharts","docAbstract":"The computer program FLOWCHART can be used to very quickly and easily produce flowcharts of high quality for publication. FLOWCHART centers each element or block of text that it processes on one of a set of (imaginary) vertical lines. It can enclose a text block in a rectangle, circle or other selected figure. It can draw a 'line connecting the midpoint of any side of any figure with the midpoint of any side of any other figure and insert an arrow pointing in the direction of flow. It can write 'yes' or 'no' next to the line joining two figures. \r\n\r\nFLOWCHART creates flowcharts using some basic plotting subroutine* which permit plots to be generated interactively and inspected on a Tektronix compatible graphics screen or plotted in a deferred mode on a Houston Instruments 42' pen plotter. The size of the plot, character set and character height in inches are inputs to the program. Plots generated using the pen plotter can be up to 42' high--the larger size plots being directly usable as visual aids in a talk. \r\n\r\nFLOWCHART centers each block of text on an imaginary column line. (The number of columns and column width are specified as input.) The midpoint of the longest line of text within the block is defined to be the center of the block and is placed on the column line. The spacing of individual words within the block is not altered when the block is positioned. \r\n\r\nThe program writes the first block of text in a designated column and continues placing each subsequent block below the previous block in the same column. A block of text may be placed in a different column by specifying the number of the column and an earlier block of text with which the new block is to be aligned. If block zero is given as the earlier block, the new text is placed in the new column continuing down the page below the previous block. Optionally a column and number of inches from the top of the page may be given for positioning the next block of text. \r\n\r\nThe program will normally draw one of five types of figure to enclose a block of text: a rectangle, circle, diamond, eight sided figure or figure with parallel sides and rounded ends. It can connect the figure with a line to the preceding figure, and place an arrow pointing toward the second figure. Text blocks not in sequence can also be connected and 'yes' or 'no' written next to any line to indicate branching. \r\n\r\nFigure 1 illustrates the various types of figures that can be drawn, spacings, connecting lines and the like.\r\n\r\n* The plotting package employed is Buplot available on the VAX and PDP-1170 computers at the USGS Office of Earthquake Studies, Golden, Colo. Calls to the plotting subroutines must be adjusted if some other plotting package is used.","language":"ENGLISH","publisher":"U.S. Geological Survey,","doi":"10.3133/ofr82999","usgsCitation":"Bender, B., 1982, FLOWCHART; a computer program for plotting flowcharts: U.S. Geological Survey Open-File Report 82-999, 21 p., ill. ;29 cm., https://doi.org/10.3133/ofr82999.","productDescription":"21 p., ill. ;29 cm.","costCenters":[],"links":[{"id":140444,"rank":0,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/of/1982/0999/report-thumb.jpg"},{"id":35376,"rank":300,"type":{"id":11,"text":"Document"},"url":"https://pubs.usgs.gov/of/1982/0999/report.pdf","linkFileType":{"id":1,"text":"pdf"}}],"noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"4f4e4a06e4b07f02db5f8aef","contributors":{"authors":[{"text":"Bender, Bernice","contributorId":38986,"corporation":false,"usgs":true,"family":"Bender","given":"Bernice","email":"","affiliations":[],"preferred":false,"id":156746,"contributorType":{"id":1,"text":"Authors"},"rank":1}]}}
,{"id":44144,"text":"ofr82735 - 1982 - Tracklines of multichannel seismic-reflection data collected by the U.S. Geological Survey in the Beaufort and Chukchi seas in 1977 for which profiles and stack tapes are available","interactions":[],"lastModifiedDate":"2012-02-02T00:04:57","indexId":"ofr82735","displayToPublicDate":"1994-01-01T00:00:00","publicationYear":"1982","noYear":false,"publicationType":{"id":18,"text":"Report"},"publicationSubtype":{"id":5,"text":"USGS Numbered Series"},"seriesTitle":{"id":330,"text":"Open-File Report","code":"OFR","onlineIssn":"2331-1258","printIssn":"0196-1497","active":true,"publicationSubtype":{"id":5}},"seriesNumber":"82-735","title":"Tracklines of multichannel seismic-reflection data collected by the U.S. Geological Survey in the Beaufort and Chukchi seas in 1977 for which profiles and stack tapes are available","language":"ENGLISH","doi":"10.3133/ofr82735","issn":"ma","usgsCitation":"Grantz, A., Mann, D.M., and May, S., 1982, Tracklines of multichannel seismic-reflection data collected by the U.S. Geological Survey in the Beaufort and Chukchi seas in 1977 for which profiles and stack tapes are available: U.S. Geological Survey Open-File Report 82-735, 1 map :photocopy ;68 x 102 cm., https://doi.org/10.3133/ofr82735.","productDescription":"1 map :photocopy ;68 x 102 cm.","costCenters":[],"links":[{"id":134831,"rank":0,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/thumbnails/usgs_thumb.jpg"},{"id":81521,"rank":400,"type":{"id":17,"text":"Plate"},"url":"https://pubs.usgs.gov/of/1982/0735/plate-1.pdf","linkFileType":{"id":1,"text":"pdf"}}],"noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"4f4e4a4de4b07f02db627118","contributors":{"authors":[{"text":"Grantz, Arthur agrantz@usgs.gov","contributorId":2585,"corporation":false,"usgs":true,"family":"Grantz","given":"Arthur","email":"agrantz@usgs.gov","affiliations":[{"id":312,"text":"Geology, Minerals, Energy, and Geophysics Science Center","active":true,"usgs":true}],"preferred":true,"id":229229,"contributorType":{"id":1,"text":"Authors"},"rank":1},{"text":"Mann, D. M.","contributorId":77902,"corporation":false,"usgs":true,"family":"Mann","given":"D.","email":"","middleInitial":"M.","affiliations":[],"preferred":false,"id":229231,"contributorType":{"id":1,"text":"Authors"},"rank":2},{"text":"May, Steven D.","contributorId":56194,"corporation":false,"usgs":true,"family":"May","given":"Steven D.","affiliations":[],"preferred":false,"id":229230,"contributorType":{"id":1,"text":"Authors"},"rank":3}]}}
,{"id":23792,"text":"ofr82862 - 1982 - A national water-use information program","interactions":[],"lastModifiedDate":"2012-02-02T00:08:16","indexId":"ofr82862","displayToPublicDate":"1994-01-01T00:00:00","publicationYear":"1982","noYear":false,"publicationType":{"id":18,"text":"Report"},"publicationSubtype":{"id":5,"text":"USGS Numbered Series"},"seriesTitle":{"id":330,"text":"Open-File Report","code":"OFR","onlineIssn":"2331-1258","printIssn":"0196-1497","active":true,"publicationSubtype":{"id":5}},"seriesNumber":"82-862","title":"A national water-use information program","docAbstract":"The U.S. Geological Survey has compiled estimates of water use every five years since 1950. These estimates have been derived from many sources, and have a wide range of accuracy. Therefore, they fall short of providing a national data base that is both current and reliable. In 1977, the Congress of the United States recognized the need for uniform information on water use and directed the U.S. Geological Survey to establish a National Water-Use Information Program to complement the Survey's data on the availability and quality of the Nation's water resources. \r\n\r\nThe National Water-Use Information Program was designed as a cooperative program between the States and the Federal Government. The goals of the program are: to collect and compile water-use data; to develop and refine computerized water-use data systems at both the State and national levels; to devise new methods and techniques to improve the collection and analysis of water-use information; and to disseminate this information to those involved in establishing water-resources policy and to those managing the resources. \r\n\r\nThe program that started in 1978 in 20 States now includes participation by 47 States. Water-Use information is being compiled for 12 categories of use. Each State will have a automated data system that contains site-specific information about the water use in each category. The National Water-Use Data System will contain information for the 12 categories of use summarized by counties and river basins within each State. \r\n\r\nThe national system will aid in defining how much fresh and saline surface water and ground water is withdrawn and for what purpose, how much water is consumed during use, and how much water is returned to a water body (stream, lake, or aquifer) after use.","language":"ENGLISH","publisher":"U.S. Geological Survey,","doi":"10.3133/ofr82862","issn":"0094-9140","usgsCitation":"Mann, W., Moore, J.E., and Chase, E.B., 1982, A national water-use information program: U.S. Geological Survey Open-File Report 82-862, 15 p. ill., 1 map ;28 cm., https://doi.org/10.3133/ofr82862.","productDescription":"15 p. ill., 1 map ;28 cm.","costCenters":[],"links":[{"id":156846,"rank":0,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/of/1982/0862/report-thumb.jpg"},{"id":53014,"rank":300,"type":{"id":11,"text":"Document"},"url":"https://pubs.usgs.gov/of/1982/0862/report.pdf","linkFileType":{"id":1,"text":"pdf"}}],"noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"4f4e4b13e4b07f02db6a33d6","contributors":{"authors":[{"text":"Mann, William B.","contributorId":21985,"corporation":false,"usgs":true,"family":"Mann","given":"William B.","affiliations":[],"preferred":false,"id":190732,"contributorType":{"id":1,"text":"Authors"},"rank":1},{"text":"Moore, John E.","contributorId":33688,"corporation":false,"usgs":true,"family":"Moore","given":"John","email":"","middleInitial":"E.","affiliations":[],"preferred":false,"id":190733,"contributorType":{"id":1,"text":"Authors"},"rank":2},{"text":"Chase, Edith B.","contributorId":11192,"corporation":false,"usgs":true,"family":"Chase","given":"Edith","email":"","middleInitial":"B.","affiliations":[],"preferred":false,"id":190731,"contributorType":{"id":1,"text":"Authors"},"rank":3}]}}
,{"id":55342,"text":"wdrKS811 - 1982 - Water resources data for Kansas, water year 1981","interactions":[],"lastModifiedDate":"2012-02-02T00:11:37","indexId":"wdrKS811","displayToPublicDate":"1994-01-01T00:00:00","publicationYear":"1982","noYear":false,"publicationType":{"id":18,"text":"Report"},"publicationSubtype":{"id":5,"text":"USGS Numbered Series"},"seriesTitle":{"id":340,"text":"Water Data Report","code":"WDR","active":false,"publicationSubtype":{"id":5}},"seriesNumber":"KS-81-1","title":"Water resources data for Kansas, water year 1981","language":"ENGLISH","doi":"10.3133/wdrKS811","usgsCitation":"Water Resources Division, U.S. Geological Survey, 1982, Water resources data for Kansas, water year 1981: U.S. Geological Survey Water Data Report KS-81-1, 566 p., https://doi.org/10.3133/wdrKS811.","productDescription":"566 p.","costCenters":[],"links":[{"id":177798,"rank":0,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/thumbnails/usgs_thumb.jpg"},{"id":94542,"rank":9999,"type":{"id":10,"text":"Digital Object Identifier"},"url":"https://hdl.handle.net/2027/mdp.39015005839454?urlappend=%3Bseq=5"}],"noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"4f4e4a9ae4b07f02db65db13","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":532335,"contributorType":{"id":1,"text":"Authors"},"rank":1}]}}
,{"id":9203,"text":"ofr82207 - 1982 - Geology and ore deposits of the Section 23 Mine, Ambrosia Lake District, New Mexico","interactions":[],"lastModifiedDate":"2012-02-02T00:06:11","indexId":"ofr82207","displayToPublicDate":"1994-01-01T00:00:00","publicationYear":"1982","noYear":false,"publicationType":{"id":18,"text":"Report"},"publicationSubtype":{"id":5,"text":"USGS Numbered Series"},"seriesTitle":{"id":330,"text":"Open-File Report","code":"OFR","onlineIssn":"2331-1258","printIssn":"0196-1497","active":true,"publicationSubtype":{"id":5}},"seriesNumber":"82-207","title":"Geology and ore deposits of the Section 23 Mine, Ambrosia Lake District, New Mexico","docAbstract":"The section 23 mine is one of about 18 large uranium mines opened in sandstones of the fluvial Westwater Canyon Member of the Jurassic Morrison Formation in the Ambrosia Lake mining district during the early 1960s. The Ambrosia Lake district is one of several mining districts within the Grants mineral belt, an elongate zone containing many uranium deposits along the southern flank of the San Juan basin. \r\n\r\nTwo distinct types of ore occur in the mine. Primary ore occurs as peneconcordant layers of uranium-rich authigenic organic matter that impregnates parts of the reduced sandstone host rocks and which are typically elongate in an east-southeast direction subparallel both to the sedimentary trends and to the present-day regional strike of the strata. These are called prefault or trend ores because of their early genesis and their elongation and alinement. \r\n\r\nA second type of ore in the mine is referred to as postfault, stacked, or redistributed ore. Its genesis was similar to that of the roll-type deposits in Tertiary rocks of Wyoming and Texas. Oxidation, related to the development of a large tongue of oxidized rock extending from Gallup to Ambrosia Lake, destroyed much of the primary ore and redistributed it as massive accumulations of lower grade ores bordering the redox interface at the edge of the tongue. Host rocks in the southern half of sec. 23 (T. 14 N., R. 10 W.) are oxidized and contain only remnants of the original, tabular, organic-rich ore. Thick bodies of roll-type ore are distributed along the leading edge of the oxidized zone, and pristine primary ore is found only near the north edge of the section.\r\n\r\nOrganic matter in the primary ore was derived from humic acids that precipitated in the pores of the sandstones and fixed uranium as both coffinite and urano-organic compounds. Vanadium, molybdenum, and selenium are also associated with the ore. The secondary or roll-type ores are essentially free of organic carbon and contain uranium both as coffinite and uraninite. They also contain vanadium and selenium but are virtually devoid of molybdenum. \r\n\r\nAlthough much has been learned about these deposits since the time this study was conducted, in 1966, a great deal more study will by required to completely elucidate their geologic history.","language":"ENGLISH","publisher":"U.S. Geological Survey],","doi":"10.3133/ofr82207","usgsCitation":"Granger, H., and Santos, E., 1982, Geology and ore deposits of the Section 23 Mine, Ambrosia Lake District, New Mexico: U.S. Geological Survey Open-File Report 82-207, 74 p. ill., maps ;29 cm., https://doi.org/10.3133/ofr82207.","productDescription":"74 p. ill., maps ;29 cm.","costCenters":[],"links":[{"id":141973,"rank":0,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/of/1982/0207/report-thumb.jpg"},{"id":36812,"rank":300,"type":{"id":11,"text":"Document"},"url":"https://pubs.usgs.gov/of/1982/0207/report.pdf","linkFileType":{"id":1,"text":"pdf"}}],"noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"4f4e4b30e4b07f02db6b409a","contributors":{"authors":[{"text":"Granger, H.C.","contributorId":15203,"corporation":false,"usgs":true,"family":"Granger","given":"H.C.","email":"","affiliations":[],"preferred":false,"id":159279,"contributorType":{"id":1,"text":"Authors"},"rank":1},{"text":"Santos, E.S.","contributorId":95883,"corporation":false,"usgs":true,"family":"Santos","given":"E.S.","email":"","affiliations":[],"preferred":false,"id":159280,"contributorType":{"id":1,"text":"Authors"},"rank":2}]}}
,{"id":23559,"text":"ofr82913 - 1982 - A summary of selected publications, project activities, and data sources related to hydrology in the Warrior and Plateau coal fields of Alabama","interactions":[],"lastModifiedDate":"2012-02-02T00:08:09","indexId":"ofr82913","displayToPublicDate":"1994-01-01T00:00:00","publicationYear":"1982","noYear":false,"publicationType":{"id":18,"text":"Report"},"publicationSubtype":{"id":5,"text":"USGS Numbered Series"},"seriesTitle":{"id":330,"text":"Open-File Report","code":"OFR","onlineIssn":"2331-1258","printIssn":"0196-1497","active":true,"publicationSubtype":{"id":5}},"seriesNumber":"82-913","title":"A summary of selected publications, project activities, and data sources related to hydrology in the Warrior and Plateau coal fields of Alabama","docAbstract":"The report is a reference source on hydrologic information related to coal-mining activities in the Warrior and Plateau coal fields of Alabama. It contains a bibliography of more than 200 references and selected annotations. Also included is information on maps, automated-data bases, water-monitoring programs, and data-source agencies and organizations.","language":"ENGLISH","publisher":"U.S. Dept. of the Interior, Geological Survey,","doi":"10.3133/ofr82913","issn":"0094-9140","usgsCitation":"Kidd, R.E., and Hill, T.J., 1982, A summary of selected publications, project activities, and data sources related to hydrology in the Warrior and Plateau coal fields of Alabama: U.S. Geological Survey Open-File Report 82-913, iv, 63 p. 1 map ;28 cm., https://doi.org/10.3133/ofr82913.","productDescription":"iv, 63 p. 1 map ;28 cm.","costCenters":[],"links":[{"id":156551,"rank":0,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/of/1982/0913/report-thumb.jpg"},{"id":52852,"rank":300,"type":{"id":11,"text":"Document"},"url":"https://pubs.usgs.gov/of/1982/0913/report.pdf","linkFileType":{"id":1,"text":"pdf"}}],"noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"4f4e4b17e4b07f02db6a5fad","contributors":{"authors":[{"text":"Kidd, Robert E.","contributorId":21523,"corporation":false,"usgs":true,"family":"Kidd","given":"Robert","email":"","middleInitial":"E.","affiliations":[],"preferred":false,"id":190317,"contributorType":{"id":1,"text":"Authors"},"rank":1},{"text":"Hill, Thomas J.","contributorId":13270,"corporation":false,"usgs":true,"family":"Hill","given":"Thomas","email":"","middleInitial":"J.","affiliations":[],"preferred":false,"id":190316,"contributorType":{"id":1,"text":"Authors"},"rank":2}]}}
,{"id":7893,"text":"ofr82963 - 1982 - Interfacing an ARL plasma spectrometer to an HP1000 minicomputer","interactions":[],"lastModifiedDate":"2012-02-02T00:05:59","indexId":"ofr82963","displayToPublicDate":"1994-01-01T00:00:00","publicationYear":"1982","noYear":false,"publicationType":{"id":18,"text":"Report"},"publicationSubtype":{"id":5,"text":"USGS Numbered Series"},"seriesTitle":{"id":330,"text":"Open-File Report","code":"OFR","onlineIssn":"2331-1258","printIssn":"0196-1497","active":true,"publicationSubtype":{"id":5}},"seriesNumber":"82-963","title":"Interfacing an ARL plasma spectrometer to an HP1000 minicomputer","language":"ENGLISH","publisher":"U.S. Geological Survey,","doi":"10.3133/ofr82963","usgsCitation":"Bigelow, R.C., 1982, Interfacing an ARL plasma spectrometer to an HP1000 minicomputer: U.S. Geological Survey Open-File Report 82-963, 1 v. (various foliations) ;28 cm., https://doi.org/10.3133/ofr82963.","productDescription":"1 v. (various foliations) ;28 cm.","costCenters":[],"links":[{"id":140042,"rank":0,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/of/1982/0963/report-thumb.jpg"},{"id":35415,"rank":300,"type":{"id":11,"text":"Document"},"url":"https://pubs.usgs.gov/of/1982/0963/report.pdf","linkFileType":{"id":1,"text":"pdf"}}],"noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"4f4e49dbe4b07f02db5e0a68","contributors":{"authors":[{"text":"Bigelow, R. C.","contributorId":90718,"corporation":false,"usgs":true,"family":"Bigelow","given":"R.","email":"","middleInitial":"C.","affiliations":[],"preferred":false,"id":156797,"contributorType":{"id":1,"text":"Authors"},"rank":1}]}}
,{"id":45885,"text":"ofr82463 - 1982 - Oblique map of Loihi Seamount and Papa'u Landslide, Hawaii","interactions":[],"lastModifiedDate":"2012-02-02T00:04:59","indexId":"ofr82463","displayToPublicDate":"1994-01-01T00:00:00","publicationYear":"1982","noYear":false,"publicationType":{"id":18,"text":"Report"},"publicationSubtype":{"id":5,"text":"USGS Numbered Series"},"seriesTitle":{"id":330,"text":"Open-File Report","code":"OFR","onlineIssn":"2331-1258","printIssn":"0196-1497","active":true,"publicationSubtype":{"id":5}},"seriesNumber":"82-463","title":"Oblique map of Loihi Seamount and Papa'u Landslide, Hawaii","language":"ENGLISH","doi":"10.3133/ofr82463","usgsCitation":"Alpha, T.R., Morley, J.M., Gutmacher, C., and Austin, W., 1982, Oblique map of Loihi Seamount and Papa'u Landslide, Hawaii: U.S. Geological Survey Open-File Report 82-463, 1 map ;56 x 66 cm., https://doi.org/10.3133/ofr82463.","productDescription":"1 map ;56 x 66 cm.","costCenters":[],"links":[{"id":135920,"rank":0,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/thumbnails/usgs_thumb.jpg"},{"id":20577,"rank":400,"type":{"id":17,"text":"Plate"},"url":"https://pubs.usgs.gov/of/1982/0463/plate-1.pdf","linkFileType":{"id":1,"text":"pdf"}}],"noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"4f4e4afce4b07f02db6965b2","contributors":{"authors":[{"text":"Alpha, Tau Rho","contributorId":63371,"corporation":false,"usgs":true,"family":"Alpha","given":"Tau","email":"","middleInitial":"Rho","affiliations":[],"preferred":false,"id":232227,"contributorType":{"id":1,"text":"Authors"},"rank":1},{"text":"Morley, J. M.","contributorId":77505,"corporation":false,"usgs":true,"family":"Morley","given":"J.","email":"","middleInitial":"M.","affiliations":[],"preferred":false,"id":232228,"contributorType":{"id":1,"text":"Authors"},"rank":2},{"text":"Gutmacher, C. E.","contributorId":45284,"corporation":false,"usgs":true,"family":"Gutmacher","given":"C. E.","affiliations":[],"preferred":false,"id":232226,"contributorType":{"id":1,"text":"Authors"},"rank":3},{"text":"Austin, W.A.","contributorId":17590,"corporation":false,"usgs":true,"family":"Austin","given":"W.A.","email":"","affiliations":[],"preferred":false,"id":232225,"contributorType":{"id":1,"text":"Authors"},"rank":4}]}}
,{"id":40930,"text":"ofr82564 - 1982 - Potentiometric-surface map of water in the Fox Hills-Lower Hell Creek aquifer in the Northern Great Plains area of Montana","interactions":[],"lastModifiedDate":"2022-08-29T19:42:04.292545","indexId":"ofr82564","displayToPublicDate":"1994-01-01T00:00:00","publicationYear":"1982","noYear":false,"publicationType":{"id":18,"text":"Report"},"publicationSubtype":{"id":5,"text":"USGS Numbered Series"},"seriesTitle":{"id":330,"text":"Open-File Report","code":"OFR","onlineIssn":"2331-1258","printIssn":"0196-1497","active":true,"publicationSubtype":{"id":5}},"seriesNumber":"82-564","title":"Potentiometric-surface map of water in the Fox Hills-Lower Hell Creek aquifer in the Northern Great Plains area of Montana","docAbstract":"The potentiometric surface of water in the Upper Cretaceous Fox Hills-lower Hell Creek aquifer is shown on a base map at a scale of 1:1,000,000. The map is one of a series produced as part of regional study of aquifers of Cenozoic and Mesozoic age in the northern Great Plains of Montana. The contour interval is 100 feet. The map shows that the direction of regional ground-water movement is toward the northeast. Recharge occurs on the flanks of the Black Hills uplift, the Cedar Creek anticline, the southwest part of the Bull Mountains basin, and on the out-crop areas. Discharge from the aquifer occurs along a short reach of the Yellowstone River. The average discharge from 335 wells is about 16 gallons per minute and the specific capacity of 185 wells averages 0.49 gallon per minute per foot of drawdown. (USGS)","language":"English","publisher":"U.S. Geological Survey","doi":"10.3133/ofr82564","usgsCitation":"Levings, G., 1982, Potentiometric-surface map of water in the Fox Hills-Lower Hell Creek aquifer in the Northern Great Plains area of Montana: U.S. Geological Survey Open-File Report 82-564, 1 Plate: 42.07 × 26.32 inches, https://doi.org/10.3133/ofr82564.","productDescription":"1 Plate: 42.07 × 26.32 inches","costCenters":[],"links":[{"id":171437,"rank":0,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/thumbnails/usgs_thumb.jpg"},{"id":78821,"rank":400,"type":{"id":17,"text":"Plate"},"url":"https://pubs.usgs.gov/of/1982/0564/plate-1.pdf","linkFileType":{"id":1,"text":"pdf"}},{"id":405832,"rank":3,"type":{"id":36,"text":"NGMDB Index Page"},"url":"https://ngmdb.usgs.gov/Prodesc/proddesc_75642.htm","linkFileType":{"id":5,"text":"html"}}],"scale":"1000000","country":"United States","state":"Montana","otherGeospatial":"Fox Hills-Lower Hell Creek aquifer","geographicExtents":"{\n  \"type\": \"FeatureCollection\",\n  \"features\": [\n    {\n      \"type\": \"Feature\",\n      \"properties\": {},\n      \"geometry\": {\n        \"type\": \"Polygon\",\n        \"coordinates\": [\n          [\n            [\n              -110.1708984375,\n              45.69083283645816\n            ],\n            [\n              -105.6005859375,\n              45.69083283645816\n            ],\n            [\n              -105.6005859375,\n              48.99463598353405\n            ],\n            [\n              -110.1708984375,\n              48.99463598353405\n            ],\n            [\n              -110.1708984375,\n              45.69083283645816\n            ]\n          ]\n        ]\n      }\n    }\n  ]\n}","noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"4f4e4ae4e4b07f02db68a3af","contributors":{"authors":[{"text":"Levings, Gary W.","contributorId":106889,"corporation":false,"usgs":true,"family":"Levings","given":"Gary W.","affiliations":[],"preferred":false,"id":224196,"contributorType":{"id":1,"text":"Authors"},"rank":1}]}}
,{"id":9115,"text":"ofr82793 - 1982 - Heat-flow measurements at shot points along the 1978 Saudi Arabia seismic deep-refraction line; Part I, Results of the measurements","interactions":[],"lastModifiedDate":"2012-02-02T00:06:14","indexId":"ofr82793","displayToPublicDate":"1994-01-01T00:00:00","publicationYear":"1982","noYear":false,"publicationType":{"id":18,"text":"Report"},"publicationSubtype":{"id":5,"text":"USGS Numbered Series"},"seriesTitle":{"id":330,"text":"Open-File Report","code":"OFR","onlineIssn":"2331-1258","printIssn":"0196-1497","active":true,"publicationSubtype":{"id":5}},"seriesNumber":"82-793","title":"Heat-flow measurements at shot points along the 1978 Saudi Arabia seismic deep-refraction line; Part I, Results of the measurements","docAbstract":"Heat-flow measurements were made at five onland shot points of the 1978 Saudi Arabian seismic deep-refraction line, which sample major tectonic elements of the Arabian Shield along a profile from Ar Riyad to the Farasan Islands. Because of the pattern drilling at each shot point, several holes (60 m deep) could be logged for temperature at each site and thus allow a better estimate of the geothermal gradient. Each site was mapped and sampled in detail, and modal and. chemical analyses of representative specimens were made in the laboratory. Thermal conductivities were computed from the modal analyses and single-mineral conductivity data. \r\n\r\nThe resulting heat-flow values, combined with published values for the Red Sea and coastal plain, indicate a three-level pattern, with a heat flow of about 4.5 heat-flow unit (HFU) over the Red Sea axial trough, about 3.0 HFU over the shelf and coastal plain, and an essentially constant 1.0 HFU over the Arabian Shield at points well away from the suture zone with the oceanic crust. At three sites where the rocks are granitic, gamma-ray spectrometry techniques were employed to estimate thorium, potassium, and uranium concentrations. The resulting plot of heat generation versus heat flow suggests that in the Arabian Shield the relationship between heat flow and heat production is not linear. More heat-flow data are essential to establish or reject this conclusion.","language":"ENGLISH","publisher":"U.S. Geological Survey,","doi":"10.3133/ofr82793","usgsCitation":"Gettings, M.E., and Showail, A., 1982, Heat-flow measurements at shot points along the 1978 Saudi Arabia seismic deep-refraction line; Part I, Results of the measurements: U.S. Geological Survey Open-File Report 82-793, iii, 102 p., ill., maps ;28 cm., https://doi.org/10.3133/ofr82793.","productDescription":"iii, 102 p., ill., maps ;28 cm.","costCenters":[],"links":[{"id":141929,"rank":0,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/of/1982/0793/report-thumb.jpg"},{"id":36727,"rank":300,"type":{"id":11,"text":"Document"},"url":"https://pubs.usgs.gov/of/1982/0793/report.pdf","linkFileType":{"id":1,"text":"pdf"}}],"noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"4f4e4a69e4b07f02db63c289","contributors":{"authors":[{"text":"Gettings, M. E.","contributorId":25148,"corporation":false,"usgs":true,"family":"Gettings","given":"M.","email":"","middleInitial":"E.","affiliations":[],"preferred":false,"id":159125,"contributorType":{"id":1,"text":"Authors"},"rank":1},{"text":"Showail, Abdullah","contributorId":63014,"corporation":false,"usgs":true,"family":"Showail","given":"Abdullah","email":"","affiliations":[],"preferred":false,"id":159126,"contributorType":{"id":1,"text":"Authors"},"rank":2}]}}
,{"id":5761,"text":"pp1220 - 1982 - Intrusive rocks of the Holden and Lucerne quadrangles, Washington— The relation of depth zones, composition, textures, and emplacement of plutons","interactions":[],"lastModifiedDate":"2021-12-08T23:02:46.402317","indexId":"pp1220","displayToPublicDate":"1994-01-01T00:00:00","publicationYear":"1982","noYear":false,"publicationType":{"id":18,"text":"Report"},"publicationSubtype":{"id":5,"text":"USGS Numbered Series"},"seriesTitle":{"id":331,"text":"Professional Paper","code":"PP","onlineIssn":"2330-7102","printIssn":"1044-9612","active":true,"publicationSubtype":{"id":5}},"seriesNumber":"1220","title":"Intrusive rocks of the Holden and Lucerne quadrangles, Washington— The relation of depth zones, composition, textures, and emplacement of plutons","docAbstract":"<p>The core of the northern Cascade Range in Washington consists of Precambrian and upper Paleozoic metamorphic rocks cut by numerous plutons, ranging in age from early Triassic to Miocene. The older plutons have been eroded to catazonal depths, whereas subvolcanic rocks are exposed in the youngest plutons. The Holden and Lucerne quadrangles span a -sizeable and representative part of this core. The oldest of the formations mapped in these quadrangles is the Swakane Biotite Gneiss, which was shown on the quadrangle maps as Cretaceous and older in age. The Swakane has yielded a middle Paleozoic metamorphic age, and also contains evidence of zircon inherited from some parent material more than 1,650 m.y. old. In this report, the Swakane is assigned an early Paleozoic or older age. It consists mostly of biotite gneiss, but interlayered with it are scattered layers and lenses of hornblende schist and gneiss, clinozoisite-epidote gneiss, and quartzite. Thickness of the Swakane is many thousands of meters, and the base is not exposed. The biotite gneiss is probably derived from a pile of siliceous volcanic rocks containing scattered sedimentary beds and basalt flows. Overlying the Swakane is a thick sequence of eugeosynclinal upper Paleozoic rocks metamorphosed to amphibolite grade. The sequence includes quartzite and thin layers of marble, hornblende schist and gneiss, graphitic schist, and smaller amounts of schist and gneiss of widely varying compositions. The layers have been tightly and complexly folded, and, in places, probably had been thrust over the overlying Swakane prior to metamorphism. Youngest of the supracrustal rocks in the area are shale, arkosic sandstone, and conglomerate of the Paleocene Swauk Formation. These rocks are preserved in the Chiwaukum graben, a major structural element of the region. </p><p>Of uncertain age, but possibly as old as any of the intrusive rocks in the area, are small masses of ultramafic rocks, now almost completely altered to serpentine. These occur either as included irregular masses in later intrusives or as tectonically emplaced lenses in metamorphic rocks. Also of uncertain age but probably much younger, perhaps as young as Eocene, are larger masses of hornblendite and hornblende periodotite that grade into hornblende gabbro. These are exposed on the surface and in the underground workings of the Holden mine. Oldest of the granitoid intrusives are the narrow, nearly concordant Dumbell Mountain plutons, having a radiometric age of about 220 m.y. They consist of gneissic hornblende-quartz diorite and quartz diorite gneiss. Most contacts consist of lit-par-lit zones, but some are gradational or more rarely sharp. The plutons are typically catazonal. Closely resembling the Dumbell Mountain plutons in outcrop appearance, but differing considerably in composition, are the Bearcat Ridge plutons. These consist of gneissic quartz diorite and granodiorite. The Bearcat Ridge plutons are not in contact with older dated plutons, but because their textural and structural characteristics so closely resemble those of the Dumbell Mountain plutons, they are considered to be the same age. Their composition, however, is suggestive of a much younger age. Cutting the Dumbell Mountain plutons is the Leroy Creek pluton, consisting of gneissic biotite-quartz diorite and trondjhemite. The gneissic foliation in the Leroy Creek is characterized by a strong and pervasive swirling. Cutting both the Dumbell Mountain and Leroy Creek plutons are the almost dikelike Seven-fingered Jack plutons. These range in composition from gabbro to quartz diorite; associated with them are contact complexes of highly varied rocks characterized by gabbro and coarse-grained hornblendite. Most of the rocks are gneissic, but some are massive and structureless.&nbsp;</p><p>Dikes, sills, small stocks, and irregular clots of leucocratic quartz diorite and granodiorite are abundant in the Swakane Biotite Gneiss and are locally abundant in the Seven-fingered Jack and other plutons. Although the leucocratic rocks vary little in appearance or composition, some, particularly those in the Swakane, were formed by metamorphic segregation, whereas the others are probably felsic differentiates of intrusive rocks.</p><p>The Tenpeak and White Mountain plutons are closely similar and are probably connected at depth. Rocks of the Tenpeak are more varied and range in composition from gabbro to granodiorite; quartz diorite is not only most common in the Tenpeak, but also constitutes, by far, the greatest bulk of the White Mountain pluton. Much of the rock in both plutons is somewhat gneissic, but some is nongneissic. The north end of the White Mountain pluton is bordered by a contact complex similar to those associated with the Seven-fingered Jack and other plutons in the area. Maximum potassium/argon ages determined on hornblende from the Tenpeak are about 90 m.y. Probably somewhat younger than the Tenpeak and White Mountain plutons is the Sulphur Mountain pluton. Only a small part of the pluton extends into the Holden quadrangle, and here the rocks are gneissic granodiorite.</p><p>The High Pass and Buck Creek plutons are tabular, somewhat silllike masses of granodioritic and quartz dioritic composition. Rocks in the Buck Creek pluton are entirely gneissic, whereas rocks only near the contacts or in the thinner parts of the High Pass are gneissic. In most places, the contacts of both plutons consist of lit-par-lit zones, but numerous dikes of the High Pass are present in the host rocks, especially the Sulphur Mountain pluton.</p><p>The Riddle Peaks pluton consists of layered and unlayered hornblende gabbro. Inasmuch as the pluton is cut on all sides by later intrusive rocks, its age relative to older plutons is not known, but it is almost certainly pre-Tertiary. Much of the gabbro is rhythmically layered, but some is unlayered or only vaguely layered. In places, thick sheets of unlayered gabbro alternate with equally thick sheets of rhythmically layered gabbro. The rock is mostly fresh and unaltered or recrystallized. No pseudosedimentary structures other than the gravity-stratified rhythmic layers were seen.</p><p>The Cardinal Peak pluton has a core consisting largely of granodiorite and quartz diorite and a rim of contact complexes containing large amounts of gabbro and coarse-grained hornblendite. The northern part of the intrusive is highly protoclastic throughout and contains numerous spindle- and canoe-shaped masses a third of a meter to several meters across and a few meters to several tens of meters long that are either partly or completely enveloped by rinds of fine-grained protoclastic material. These masses seem to have behaved as roller bearings during intrusion of the partly crystalline magma.</p>","language":"English","publisher":"U.S. Geological Survey","doi":"10.3133/pp1220","usgsCitation":"Cater, F., 1982, Intrusive rocks of the Holden and Lucerne quadrangles, Washington— The relation of depth zones, composition, textures, and emplacement of plutons: U.S. Geological Survey Professional Paper 1220, vi, 108 p., https://doi.org/10.3133/pp1220.","productDescription":"vi, 108 p.","costCenters":[],"links":[{"id":121620,"rank":0,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/pp/1220/report-thumb.jpg"},{"id":32345,"rank":300,"type":{"id":11,"text":"Document"},"url":"https://pubs.usgs.gov/pp/1220/report.pdf","linkFileType":{"id":1,"text":"pdf"}},{"id":392664,"rank":2,"type":{"id":36,"text":"NGMDB Index Page"},"url":"https://ngmdb.usgs.gov/Prodesc/proddesc_74463.htm"}],"country":"United States","state":"Washington","otherGeospatial":"Holden and Lucerne quadrangles","geographicExtents":"{\n  \"type\": \"FeatureCollection\",\n  \"features\": [\n    {\n      \"type\": \"Feature\",\n      \"properties\": {},\n      \"geometry\": {\n        \"type\": \"Polygon\",\n        \"coordinates\": [\n          [\n            [\n              -121,\n              48\n            ],\n            [\n              -120.5,\n              48\n            ],\n            [\n              -120.5,\n              48.25\n            ],\n            [\n              -121,\n              48.25\n            ],\n            [\n              -121,\n              48\n            ]\n          ]\n        ]\n      }\n    }\n  ]\n}","noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"4f4e49bee4b07f02db5d1227","contributors":{"authors":[{"text":"Cater, Fred W.","contributorId":26295,"corporation":false,"usgs":true,"family":"Cater","given":"Fred W.","affiliations":[],"preferred":false,"id":151539,"contributorType":{"id":1,"text":"Authors"},"rank":1}]}}
,{"id":40934,"text":"ofr82565 - 1982 - Potentiometric-surface map of water in the Eagle Sandstone and equivalent units in the northern Great Plains area of Montana","interactions":[],"lastModifiedDate":"2022-09-27T20:51:53.126062","indexId":"ofr82565","displayToPublicDate":"1994-01-01T00:00:00","publicationYear":"1982","noYear":false,"publicationType":{"id":18,"text":"Report"},"publicationSubtype":{"id":5,"text":"USGS Numbered Series"},"seriesTitle":{"id":330,"text":"Open-File Report","code":"OFR","onlineIssn":"2331-1258","printIssn":"0196-1497","active":true,"publicationSubtype":{"id":5}},"seriesNumber":"82-565","title":"Potentiometric-surface map of water in the Eagle Sandstone and equivalent units in the northern Great Plains area of Montana","docAbstract":"<p>The potentiometric surface of water in the Upper Cretaceous Eagle Sandstone and equivalent units (Virgelle Sandstone and Telegraph Creek Formation) is shown on a base map at a scale of 1:1,000,000. The map is one of a series of maps produced as part of a regional study of aquifers of Cenozoic and Mesozoic age in the northern Great plains of Montana. The contour interval is 200 feet. The map shows that the directions of regional ground-water movement is from west to east except in the extreme northwestern corner where the movement is from east to west. Water is discharged from the Eagle Sandstone to the Missouri River south of the Bearpaw Mountains. In the area north of the Bearpaw Mountains, depressurization from gas production may account for the decline in the potentiometric surface. The average discharge from 115 wells is about 23 gallons per minute and the specific capacity of 85 wells averages 1.4 gallons per minute per foot of drawdown.</p>","language":"English","publisher":"U.S. Geological Survey","doi":"10.3133/ofr82565","usgsCitation":"Levings, G., 1982, Potentiometric-surface map of water in the Eagle Sandstone and equivalent units in the northern Great Plains area of Montana: U.S. Geological Survey Open-File Report 82-565, 1 Plate: 40.81 × 22.83 inches, https://doi.org/10.3133/ofr82565.","productDescription":"1 Plate: 40.81 × 22.83 inches","costCenters":[],"links":[{"id":78824,"rank":400,"type":{"id":17,"text":"Plate"},"url":"https://pubs.usgs.gov/of/1982/0565/plate-1.pdf","linkFileType":{"id":1,"text":"pdf"}},{"id":407484,"rank":3,"type":{"id":36,"text":"NGMDB Index Page"},"url":"https://ngmdb.usgs.gov/Prodesc/proddesc_75643.htm","linkFileType":{"id":5,"text":"html"}},{"id":171535,"rank":0,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/thumbnails/usgs_thumb.jpg"}],"country":"United States","state":"Montana","geographicExtents":"{\n  \"type\": \"FeatureCollection\",\n  \"features\": [\n    {\n      \"type\": \"Feature\",\n      \"properties\": {},\n      \"geometry\": {\n        \"type\": \"Polygon\",\n        \"coordinates\": [\n          [\n            [\n              -112.5,\n              45\n            ],\n            [\n              -104.0417,\n              45\n            ],\n            [\n              -104.0417,\n              49\n            ],\n            [\n              -112.5,\n              49\n            ],\n            [\n              -112.5,\n              45\n            ]\n          ]\n        ]\n      }\n    }\n  ]\n}","noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"4f4e4afde4b07f02db696b88","contributors":{"authors":[{"text":"Levings, Gary W.","contributorId":106889,"corporation":false,"usgs":true,"family":"Levings","given":"Gary W.","affiliations":[],"preferred":false,"id":224205,"contributorType":{"id":1,"text":"Authors"},"rank":1}]}}
,{"id":23607,"text":"ofr81330 - 1982 - Ground-water quality and data on wells and springs in Pennsylvania; Volume III, Delaware River basin","interactions":[],"lastModifiedDate":"2017-06-22T11:08:23","indexId":"ofr81330","displayToPublicDate":"1994-01-01T00:00:00","publicationYear":"1982","noYear":false,"publicationType":{"id":18,"text":"Report"},"publicationSubtype":{"id":5,"text":"USGS Numbered Series"},"seriesTitle":{"id":330,"text":"Open-File Report","code":"OFR","onlineIssn":"2331-1258","printIssn":"0196-1497","active":true,"publicationSubtype":{"id":5}},"seriesNumber":"81-330","title":"Ground-water quality and data on wells and springs in Pennsylvania; Volume III, Delaware River basin","docAbstract":"Volume III presents ground-water quality and physical data on about 1,250 wells and springs in the Delaware River Basin in Pennsylvania. Locations are shown on site-location maps derived from the hydrologic unit map. Codes showing the geologic age and aquifer are provided.","language":"English","publisher":"U.S. Geological Survey","publisherLocation":"Harrisburg,, PA","doi":"10.3133/ofr81330","issn":"0094-9140","collaboration":"Prepared in cooperation with the  Pennsylvania Department of Environmental Resources","usgsCitation":"Koester, H., and Miller, D., 1982, Ground-water quality and data on wells and springs in Pennsylvania; Volume III, Delaware River basin: U.S. Geological Survey Open-File Report 81-330, iii, 111 p., https://doi.org/10.3133/ofr81330.","productDescription":"iii, 111 p.","numberOfPages":"116","additionalOnlineFiles":"N","costCenters":[{"id":532,"text":"Pennsylvania Water Science Center","active":true,"usgs":true}],"links":[{"id":154891,"rank":0,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/of/1981/0330/report-thumb.jpg"},{"id":277909,"type":{"id":11,"text":"Document"},"url":"https://pubs.usgs.gov/of/1981/0330/report.pdf"}],"country":"United States","state":"Pennsylvania","geographicExtents":"{ \"type\": \"FeatureCollection\", \"features\": [ { \"type\": \"Feature\", \"properties\": {}, \"geometry\": { \"type\": \"Polygon\", \"coordinates\": [ [ [ -76.8054,39.7241 ], [ -76.8054,41.9983 ], [ -74.707,41.9983 ], [ -74.707,39.7241 ], [ -76.8054,39.7241 ] ] ] } } ] }","noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"4f4e4aa8e4b07f02db6673f1","contributors":{"authors":[{"text":"Koester, H.E.","contributorId":26323,"corporation":false,"usgs":true,"family":"Koester","given":"H.E.","email":"","affiliations":[],"preferred":false,"id":190398,"contributorType":{"id":1,"text":"Authors"},"rank":1},{"text":"Miller, D.R.","contributorId":106147,"corporation":false,"usgs":true,"family":"Miller","given":"D.R.","email":"","affiliations":[],"preferred":false,"id":190399,"contributorType":{"id":1,"text":"Authors"},"rank":2}]}}
,{"id":11366,"text":"ofr82203A - 1982 - Multielement chemical and statistical analyses from a uranium hydrogeochemical and stream-sediment survey in and near the Elkhorn Mountains, Jefferson County, Montana. Part I: Surface water","interactions":[],"lastModifiedDate":"2022-09-14T19:18:54.035728","indexId":"ofr82203A","displayToPublicDate":"1994-01-01T00:00:00","publicationYear":"1982","noYear":false,"publicationType":{"id":18,"text":"Report"},"publicationSubtype":{"id":5,"text":"USGS Numbered Series"},"seriesTitle":{"id":330,"text":"Open-File Report","code":"OFR","onlineIssn":"2331-1258","printIssn":"0196-1497","active":true,"publicationSubtype":{"id":5}},"seriesNumber":"82-203","chapter":"A","title":"Multielement chemical and statistical analyses from a uranium hydrogeochemical and stream-sediment survey in and near the Elkhorn Mountains, Jefferson County, Montana. Part I: Surface water","docAbstract":"<p>Fifty-two surface-water samples, collected from an area south of Helena, Jefferson County, were analyzed for 51 chemical species. Of these variables, 35 showed detectable variation over the area, and 29 were utilized in a correlation analysis. </p><p>Two populations are distinguished in the collected samples and are especially evident in the plot of Ca versus U. Samples separated on the basis of U versus Ca proved to represent drainage areas of two differing lithologies. One group was from waters that drain the Boulder batholith, the other from those that drain the Elkhorn Mountains volcanic rocks. These two groups of samples, in general, proved to have parallel but different linear trends between U and other elements. Therefore, the two groups of samples were treated separately in the statistical analyses. </p><p>Over the area that drains the Boulder batholith, U concentrations in water ranged from 0.37 to 13.0 <span>μ</span>g/l , with a mean of 1.9 <span>μ</span>g/l. The samples from streams draining volcanic areas ranged from 0.04 to 1.5 <span>μ</span>g/l, with a mean of 0.42 <span>μ</span>g/l. The highest U values (12 and 13 <span>μ</span>g/l) occur along Badger Creek, Rawhide Creek, Little Buffalo Gulch, and an unnamed tributary to Clancy Creek. </p><p>Conductivity, hardness, Ba, Ca, CI, K, Mg, Na and Sr are significantly correlated with U at or better than the 95 percent confidence limit in both populations. For water draining the Boulder batholith, uranium correlates significantly with akalinity, pH, bicarbonate, Li, Mo, NO2+NO3, P04, SiO2, SO4, F, and inorganic carbon. These correlations are similar to those found in a previous study of water samples in north-central New Mexico (Wenrich-Verbeek, 1977b). Uranium in water from the volcanic terrane does not show correlations with any of the above constituents, but does correlate well with V. This relationship with V is absent within the Boulder batholith samples.</p>","language":"English","publisher":"U.S. Geological Survey","doi":"10.3133/ofr82203A","usgsCitation":"Suits, V., and Wenrich, K., 1982, Multielement chemical and statistical analyses from a uranium hydrogeochemical and stream-sediment survey in and near the Elkhorn Mountains, Jefferson County, Montana. Part I: Surface water: U.S. Geological Survey Open-File Report 82-203, ii, 94 p., https://doi.org/10.3133/ofr82203A.","productDescription":"ii, 94 p.","costCenters":[],"links":[{"id":143129,"rank":0,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/of/1982/0203a/report-thumb.jpg"},{"id":39192,"rank":300,"type":{"id":11,"text":"Document"},"url":"https://pubs.usgs.gov/of/1982/0203a/report.pdf","linkFileType":{"id":1,"text":"pdf"}},{"id":406713,"rank":3,"type":{"id":36,"text":"NGMDB Index Page"},"url":"https://ngmdb.usgs.gov/Prodesc/proddesc_13681.htm","linkFileType":{"id":5,"text":"html"}}],"country":"United States","state":"Montana","county":"Jefferson County","otherGeospatial":"Elkhorn Mountains","geographicExtents":"{\n  \"type\": \"FeatureCollection\",\n  \"features\": [\n    {\n      \"type\": \"Feature\",\n      \"properties\": {},\n      \"geometry\": {\n        \"type\": \"Polygon\",\n        \"coordinates\": [\n          [\n            [\n              -112.25,\n              46.25\n            ],\n            [\n              -111.75,\n              46.25\n            ],\n            [\n              -111.75,\n              46.5\n            ],\n            [\n              -112.25,\n              46.5\n            ],\n            [\n              -112.25,\n              46.25\n            ]\n          ]\n        ]\n      }\n    }\n  ]\n}","noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"4f4e4b32e4b07f02db6b48a0","contributors":{"authors":[{"text":"Suits, V. J.","contributorId":30988,"corporation":false,"usgs":true,"family":"Suits","given":"V. J.","affiliations":[],"preferred":false,"id":163008,"contributorType":{"id":1,"text":"Authors"},"rank":1},{"text":"Wenrich, K. J.","contributorId":40203,"corporation":false,"usgs":true,"family":"Wenrich","given":"K. J.","affiliations":[],"preferred":false,"id":163009,"contributorType":{"id":1,"text":"Authors"},"rank":2}]}}
,{"id":9621,"text":"ofr821055 - 1982 - Description of beds exposed at Fort Funston, Golden Gate National Recreation Area, northwestern San Francisco Peninsula, California","interactions":[],"lastModifiedDate":"2012-02-02T00:06:15","indexId":"ofr821055","displayToPublicDate":"1994-01-01T00:00:00","publicationYear":"1982","noYear":false,"publicationType":{"id":18,"text":"Report"},"publicationSubtype":{"id":5,"text":"USGS Numbered Series"},"seriesTitle":{"id":330,"text":"Open-File Report","code":"OFR","onlineIssn":"2331-1258","printIssn":"0196-1497","active":true,"publicationSubtype":{"id":5}},"seriesNumber":"82-1055","title":"Description of beds exposed at Fort Funston, Golden Gate National Recreation Area, northwestern San Francisco Peninsula, California","language":"ENGLISH","publisher":"U.S. Geological Survey,","doi":"10.3133/ofr821055","usgsCitation":"Hunter, R.E., and Clifton, H., 1982, Description of beds exposed at Fort Funston, Golden Gate National Recreation Area, northwestern San Francisco Peninsula, California: U.S. Geological Survey Open-File Report 82-1055, 31 p., ill. ;28 cm., https://doi.org/10.3133/ofr821055.","productDescription":"31 p., ill. ;28 cm.","costCenters":[],"links":[{"id":141759,"rank":0,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/of/1982/1055/report-thumb.jpg"},{"id":37353,"rank":300,"type":{"id":11,"text":"Document"},"url":"https://pubs.usgs.gov/of/1982/1055/report.pdf","linkFileType":{"id":1,"text":"pdf"}}],"noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"4f4e4aa8e4b07f02db667a6d","contributors":{"authors":[{"text":"Hunter, R. E.","contributorId":48148,"corporation":false,"usgs":true,"family":"Hunter","given":"R.","email":"","middleInitial":"E.","affiliations":[],"preferred":false,"id":160009,"contributorType":{"id":1,"text":"Authors"},"rank":1},{"text":"Clifton, H.E.","contributorId":44151,"corporation":false,"usgs":true,"family":"Clifton","given":"H.E.","affiliations":[],"preferred":false,"id":160008,"contributorType":{"id":1,"text":"Authors"},"rank":2}]}}
,{"id":7909,"text":"ofr82953 - 1982 - Schlumberger sounding investigations in the Date Creek basin, Arizona","interactions":[],"lastModifiedDate":"2012-02-02T00:06:00","indexId":"ofr82953","displayToPublicDate":"1994-01-01T00:00:00","publicationYear":"1982","noYear":false,"publicationType":{"id":18,"text":"Report"},"publicationSubtype":{"id":5,"text":"USGS Numbered Series"},"seriesTitle":{"id":330,"text":"Open-File Report","code":"OFR","onlineIssn":"2331-1258","printIssn":"0196-1497","active":true,"publicationSubtype":{"id":5}},"seriesNumber":"82-953","title":"Schlumberger sounding investigations in the Date Creek basin, Arizona","language":"ENGLISH","publisher":"U.S. Geological Survey,","doi":"10.3133/ofr82953","usgsCitation":"Bisdorf, R., 1982, Schlumberger sounding investigations in the Date Creek basin, Arizona: U.S. Geological Survey Open-File Report 82-953, 56 p., ill. (some col.), maps ;28 cm., https://doi.org/10.3133/ofr82953.","productDescription":"56 p., ill. (some col.), maps ;28 cm.","costCenters":[],"links":[{"id":140687,"rank":0,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/of/1982/0953/report-thumb.jpg"},{"id":35453,"rank":300,"type":{"id":11,"text":"Document"},"url":"https://pubs.usgs.gov/of/1982/0953/report.pdf","linkFileType":{"id":1,"text":"pdf"}}],"noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"4f4e4a0de4b07f02db5fd490","contributors":{"authors":[{"text":"Bisdorf, R.J.","contributorId":42960,"corporation":false,"usgs":true,"family":"Bisdorf","given":"R.J.","email":"","affiliations":[],"preferred":false,"id":156817,"contributorType":{"id":1,"text":"Authors"},"rank":1}]}}
,{"id":56643,"text":"fwsobs81_51 - 1982 - Life history requirements of selected finfish and shellfish in Mississippi sound and adjacent areas","interactions":[],"lastModifiedDate":"2018-01-30T11:08:04","indexId":"fwsobs81_51","displayToPublicDate":"1994-01-01T00:00:00","publicationYear":"1982","noYear":false,"publicationType":{"id":18,"text":"Report"},"publicationSubtype":{"id":1,"text":"Federal Government Series"},"seriesTitle":{"id":20,"text":"FWS/OBS","active":false,"publicationSubtype":{"id":1}},"seriesNumber":"81/51","title":"Life history requirements of selected finfish and shellfish in Mississippi sound and adjacent areas","docAbstract":"<p>No abstract available.</p>","language":"English","publisher":"U.S. Fish and Wildlife Service","usgsCitation":"1982, Life history requirements of selected finfish and shellfish in Mississippi sound and adjacent areas: FWS/OBS 81/51, vii, 97 p.","productDescription":"vii, 97 p.","costCenters":[],"links":[{"id":181364,"rank":0,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/thumbnails/outside_thumb.jpg"}],"noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"4f4e4b16e4b07f02db6a53c5","contributors":{"editors":[{"text":"Benson, Norman Gustaf","contributorId":91915,"corporation":false,"usgs":true,"family":"Benson","given":"Norman","email":"","middleInitial":"Gustaf","affiliations":[],"preferred":false,"id":726159,"contributorType":{"id":2,"text":"Editors"},"rank":1}]}}
,{"id":56654,"text":"fwsobs82_10_8 - 1982 - Habitat Suitability Index Models: Bluegill","interactions":[],"lastModifiedDate":"2022-02-15T14:25:36.300362","indexId":"fwsobs82_10_8","displayToPublicDate":"1994-01-01T00:00:00","publicationYear":"1982","noYear":false,"publicationType":{"id":18,"text":"Report"},"publicationSubtype":{"id":1,"text":"Federal Government Series"},"seriesTitle":{"id":20,"text":"FWS/OBS","active":false,"publicationSubtype":{"id":1}},"seriesNumber":"82/10.8","subseriesTitle":"Habitat Suitability Index","title":"Habitat Suitability Index Models: Bluegill","docAbstract":"A literature review encompassing habitat and species characteristics of the bluegill (Lepomis macrochirus) is followed by a discussion of the relationship of habitat variables and life requisites of this species. These data re then incorporated into Habitat Suitability Index models for the bluegill.\r\n\r\nThis is one in a series of publications describing habitat requirements of selected fish and wildlife species. Numerous literature sources have been consulted in an effort to consolidate scientific data on species habitat relationships. These data have subsequently been synthesized into Habitat Suitability Index (HSI) models. the models are based on suitability indices formulated for variables found to affect the life cycle and survival of the species. The models are designed to be modified to evaluate specific habitat alterations using the HSI model building techniques presented in the U.S. Fish and Wildlife Service's Habitat Evaluation Procedures.","language":"English","publisher":"U.S. Fish and Wildlife Service","usgsCitation":"Stuber, R.J., Gebhart, G., and Maughan, O.E., 1982, Habitat Suitability Index Models: Bluegill: FWS/OBS 82/10.8, vi, 26 p.","productDescription":"vi, 26 p.","costCenters":[{"id":595,"text":"U.S. Geological Survey","active":false,"usgs":true}],"links":[{"id":181769,"rank":0,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/thumbnails/outside_thumb.jpg"}],"noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"4f4e4a80e4b07f02db649c68","contributors":{"authors":[{"text":"Stuber, Robert J.","contributorId":10849,"corporation":false,"usgs":true,"family":"Stuber","given":"Robert","email":"","middleInitial":"J.","affiliations":[],"preferred":false,"id":255605,"contributorType":{"id":1,"text":"Authors"},"rank":1},{"text":"Gebhart, Glen","contributorId":52237,"corporation":false,"usgs":true,"family":"Gebhart","given":"Glen","email":"","affiliations":[],"preferred":false,"id":255607,"contributorType":{"id":1,"text":"Authors"},"rank":2},{"text":"Maughan, O. Eugene","contributorId":43006,"corporation":false,"usgs":true,"family":"Maughan","given":"O.","email":"","middleInitial":"Eugene","affiliations":[],"preferred":false,"id":255606,"contributorType":{"id":1,"text":"Authors"},"rank":3}]}}
,{"id":40599,"text":"ofr82119 - 1982 - Chemical quality of water in the upper part of the Floridan aquifer, Duval County, Florida","interactions":[],"lastModifiedDate":"2022-03-02T20:50:43.381919","indexId":"ofr82119","displayToPublicDate":"1994-01-01T00:00:00","publicationYear":"1982","noYear":false,"publicationType":{"id":18,"text":"Report"},"publicationSubtype":{"id":5,"text":"USGS Numbered Series"},"seriesTitle":{"id":330,"text":"Open-File Report","code":"OFR","onlineIssn":"2331-1258","printIssn":"0196-1497","active":true,"publicationSubtype":{"id":5}},"seriesNumber":"82-119","title":"Chemical quality of water in the upper part of the Floridan aquifer, Duval County, Florida","docAbstract":"<p>The Floridan aquifer is the principle source of freshwater in Duval County (fig. 1). Most water-supply wells penetrate only the upper 600 feet of the aquifer because highly mineralized water is found in the deeper zone. Earlier investigations have shown that within the upper 600 feet of the aquifer, the water quality varies considerably. In most areas the water contains very low concentrations of inorganic constituents whereas in other areas the concentrations are much higher.&nbsp;</p><p>In order to determine the areal distribution of the inorganic constituents in the upper part of the aquifer, water samples were collected from selected wells throughout Duval County and analyzed for common chemical constituents.&nbsp;</p>","language":"English","publisher":"U.S. Geological Survey","doi":"10.3133/ofr82119","collaboration":"Prepared in cooperation with the City of Jacksonville","usgsCitation":"Thompson, T., 1982, Chemical quality of water in the upper part of the Floridan aquifer, Duval County, Florida: U.S. Geological Survey Open-File Report 82-119, 1 Plate: 40.12 x 26.04 inches, https://doi.org/10.3133/ofr82119.","productDescription":"1 Plate: 40.12 x 26.04 inches","costCenters":[],"links":[{"id":396672,"rank":2,"type":{"id":17,"text":"Plate"},"url":"https://pubs.usgs.gov/of/1982/0119/plate-1.pdf","linkFileType":{"id":1,"text":"pdf"}},{"id":173378,"rank":0,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/of/1982/0119/report-thumb.jpg"}],"country":"United States","state":"Florida","county":"Duval 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,{"id":40899,"text":"ofr82562 - 1982 - Potentiometric-surface map of water in the Judith River Formation in the northern Great Plains area of Montana","interactions":[],"lastModifiedDate":"2022-09-27T20:57:58.601919","indexId":"ofr82562","displayToPublicDate":"1994-01-01T00:00:00","publicationYear":"1982","noYear":false,"publicationType":{"id":18,"text":"Report"},"publicationSubtype":{"id":5,"text":"USGS Numbered Series"},"seriesTitle":{"id":330,"text":"Open-File Report","code":"OFR","onlineIssn":"2331-1258","printIssn":"0196-1497","active":true,"publicationSubtype":{"id":5}},"seriesNumber":"82-562","title":"Potentiometric-surface map of water in the Judith River Formation in the northern Great Plains area of Montana","docAbstract":"<p>The potentiometric surface of the Judith River Formation is mapped at a scale of 1:1,000,000. The map is one of a series produced as part of a regional study of aquifers of Cenozoic and Mesozoic age in the northern Great Plains of Montana. The contour interval is 200 feet. Water in the Judith River Formation occurs under water-table and artesian conditions. The direction of regional ground-water movement is from west to east. Water is discharged from the Judith River Formation to the Milk River from near Havre, Montana, to Malta and to the Missouri River south of the Bearpaw and Little Rocky Mountains. The average discharge from 236 wells is about 10 gallons per minute, and the specific capacity of 186 wells averages 0.66 gallon per minute per foot of drawdown.</p>","language":"English","publisher":"U.S. Geological Survey","doi":"10.3133/ofr82562","usgsCitation":"Levings, G., 1982, Potentiometric-surface map of water in the Judith River Formation in the northern Great Plains area of Montana: U.S. Geological Survey Open-File Report 82-562, 1 Plate: 40.47 × 23.06 inches, https://doi.org/10.3133/ofr82562.","productDescription":"1 Plate: 40.47 × 23.06 inches","costCenters":[],"links":[{"id":407485,"rank":3,"type":{"id":36,"text":"NGMDB Index Page"},"url":"https://ngmdb.usgs.gov/Prodesc/proddesc_75640.htm","linkFileType":{"id":5,"text":"html"}},{"id":78781,"rank":400,"type":{"id":17,"text":"Plate"},"url":"https://pubs.usgs.gov/of/1982/0562/plate-1.pdf","linkFileType":{"id":1,"text":"pdf"}},{"id":172091,"rank":0,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/thumbnails/usgs_thumb.jpg"}],"country":"United States","state":"Montana","geographicExtents":"{\n  \"type\": \"FeatureCollection\",\n  \"features\": [\n    {\n      \"type\": \"Feature\",\n      \"properties\": {},\n      \"geometry\": {\n        \"type\": \"Polygon\",\n        \"coordinates\": [\n          [\n            [\n              -111,\n              45\n            ],\n            [\n              -104.0418,\n              45\n            ],\n            [\n              -104.0418,\n              49\n            ],\n            [\n              -111,\n              49\n            ],\n            [\n              -111,\n              45\n            ]\n          ]\n        ]\n      }\n    }\n  ]\n}","noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"4f4e4ae4e4b07f02db68a2f5","contributors":{"authors":[{"text":"Levings, Gary W.","contributorId":106889,"corporation":false,"usgs":true,"family":"Levings","given":"Gary W.","affiliations":[],"preferred":false,"id":224137,"contributorType":{"id":1,"text":"Authors"},"rank":1}]}}
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