{"pageNumber":"353","pageRowStart":"8800","pageSize":"25","recordCount":10959,"records":[{"id":10000,"text":"ofr801049 - 1983 - Ground water in the northern part of Clackamas County, Oregon","interactions":[],"lastModifiedDate":"2022-08-26T20:47:39.65998","indexId":"ofr801049","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":"80-1049","title":"Ground water in the northern part of Clackamas County, Oregon","docAbstract":"<p>Northern Clackamas County is part of the rapidly growing Portland metropolitan area. Population of this 250-square-mile area increased about 50 percent between 1970 and 1976. The study area includes a small segment of the Willamette River alluvial valley near Canby, and extends northward to the Clackamas River and eastward to the western boundary of Mount Hood National Forest. Also included is the narrow, well-populated corridor along U.S. Highway 26 from Cherryville to Government Camp.</p><p>The main part of the study area is largely a rolling upland underlain by volcanic and stream-deposited rocks ranging in age from Eocene to Holocene. In most places, these rocks yield water in quantities adequate for individual homes. Locally, ground-water supplies are adequate for small irrigation, industrial, or public-supply uses. Depths of wells range from 50 to 1,000 feet; wells generally are shallowest in lowlands near streams and deepest in upland locations near deeply incised stream valleys.</p><p>All aquifers receive recharge at sufficient rates to sustain present rates of natural and man-produced discharge. All aquifers could supply additional water, but careful engineering is needed to avoid overdevelopment problems for the Columbia River Basalt Group near Oregon City.</p><p>Chemical analyses indicate that the ground water in the study area is of good quality for drinking and other uses. Mineralized water reported from some wells northeast of Canby may be from rocks of the Skamania Volcanics, which locally are at shallow depth. Although ground water locally may be subject to bacterial contamination where it occurs at shallow depths in alluvium and other unconsolidated deposits, no contaminated water was identified during the study.</p>","language":"English","publisher":"U.S. Geological Survey","doi":"10.3133/ofr801049","collaboration":"Prepared in cooperation with the Oregon Water Resources Department","usgsCitation":"Leonard, A., and Collins, C.A., 1983, Ground water in the northern part of Clackamas County, Oregon: U.S. Geological Survey Open-File Report 80-1049, Report: v, 85 p., 2 Plates: 34.53 x 24.34 inches and 34.96 x 24.88 inches, https://doi.org/10.3133/ofr801049.","productDescription":"Report: v, 85 p., 2 Plates: 34.53 x 24.34 inches and 34.96 x 24.88 inches","onlineOnly":"N","additionalOnlineFiles":"N","costCenters":[{"id":518,"text":"Oregon Water Science Center","active":true,"usgs":true}],"links":[{"id":405726,"rank":4,"type":{"id":17,"text":"Plate"},"url":"https://pubs.usgs.gov/of/1980/1049/plate-1.pdf","linkFileType":{"id":1,"text":"pdf"}},{"id":405725,"rank":3,"type":{"id":17,"text":"Plate"},"url":"https://pubs.usgs.gov/of/1980/1049/plate-2.pdf","linkFileType":{"id":1,"text":"pdf"}},{"id":142557,"rank":0,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/of/1980/1049/report-thumb.jpg"},{"id":405724,"rank":2,"type":{"id":11,"text":"Document"},"url":"https://pubs.usgs.gov/of/1980/1049/report.pdf","linkFileType":{"id":1,"text":"pdf"}}],"country":"United States","state":"Oregon","county":"Clackamas County","geographicExtents":"{\n  \"type\": \"FeatureCollection\",\n  \"features\": [\n    {\n      \"type\": \"Feature\",\n      \"properties\": {},\n      \"geometry\": {\n        \"type\": \"Polygon\",\n        \"coordinates\": [\n          [\n            [\n              -122.76123046875,\n              45.01141864227728\n            ],\n            [\n              -121.84936523437499,\n              45.01141864227728\n            ],\n            [\n              -121.84936523437499,\n              45.45627757127799\n            ],\n            [\n              -122.76123046875,\n              45.45627757127799\n            ],\n            [\n              -122.76123046875,\n              45.01141864227728\n            ]\n          ]\n        ]\n      }\n    }\n  ]\n}","noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"4f4e4ab0e4b07f02db66d750","contributors":{"authors":[{"text":"Leonard, A.R.","contributorId":101669,"corporation":false,"usgs":true,"family":"Leonard","given":"A.R.","email":"","affiliations":[],"preferred":false,"id":160652,"contributorType":{"id":1,"text":"Authors"},"rank":1},{"text":"Collins, C. 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,{"id":17370,"text":"ofr83507 - 1983 - Mineral resources of the eastern Pioneer Mountains, Beaverhead County, Montana","interactions":[{"subject":{"id":17370,"text":"ofr83507 - 1983 - Mineral resources of the eastern Pioneer Mountains, Beaverhead County, Montana","indexId":"ofr83507","publicationYear":"1983","noYear":false,"title":"Mineral resources of the eastern Pioneer Mountains, Beaverhead County, Montana"},"predicate":"SUPERSEDED_BY","object":{"id":33390,"text":"b1766 - 1988 - Mineral resources of the eastern Pioneer Mountains, Beaverhead County, Montana","indexId":"b1766","publicationYear":"1988","noYear":false,"title":"Mineral resources of the eastern Pioneer Mountains, Beaverhead County, Montana"},"id":1}],"supersededBy":{"id":33390,"text":"b1766 - 1988 - Mineral resources of the eastern Pioneer Mountains, Beaverhead County, Montana","indexId":"b1766","publicationYear":"1988","noYear":false,"title":"Mineral resources of the eastern Pioneer Mountains, Beaverhead County, Montana"},"lastModifiedDate":"2019-09-26T13:27:09","indexId":"ofr83507","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":"83-507","title":"Mineral resources of the eastern Pioneer Mountains, Beaverhead County, Montana","docAbstract":"<p>No abstract available.</p>","language":"English","publisher":"U.S. Geological Survey","publisherLocation":"Reston, VA","doi":"10.3133/ofr83507","usgsCitation":"Pearson, R.C., Berger, B.R., Kaufmann, H.E., Hanna, W.F., and Zen, E., 1983, Mineral resources of the eastern Pioneer Mountains, Beaverhead County, Montana: U.S. Geological Survey Open-File Report 83-507, ii, 56 p., https://doi.org/10.3133/ofr83507.","productDescription":"ii, 56 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C.","contributorId":30978,"corporation":false,"usgs":true,"family":"Pearson","given":"R.","email":"","middleInitial":"C.","affiliations":[],"preferred":false,"id":176133,"contributorType":{"id":1,"text":"Authors"},"rank":1},{"text":"Berger, B. R.","contributorId":77914,"corporation":false,"usgs":true,"family":"Berger","given":"B.","email":"","middleInitial":"R.","affiliations":[],"preferred":false,"id":176136,"contributorType":{"id":1,"text":"Authors"},"rank":2},{"text":"Kaufmann, H. E.","contributorId":40215,"corporation":false,"usgs":true,"family":"Kaufmann","given":"H.","email":"","middleInitial":"E.","affiliations":[],"preferred":false,"id":176135,"contributorType":{"id":1,"text":"Authors"},"rank":3},{"text":"Hanna, W. F.","contributorId":6835,"corporation":false,"usgs":true,"family":"Hanna","given":"W.","email":"","middleInitial":"F.","affiliations":[],"preferred":false,"id":176132,"contributorType":{"id":1,"text":"Authors"},"rank":4},{"text":"Zen, E-an","contributorId":38564,"corporation":false,"usgs":true,"family":"Zen","given":"E-an","affiliations":[],"preferred":false,"id":176134,"contributorType":{"id":1,"text":"Authors"},"rank":5}]}}
,{"id":1348,"text":"wsp2216 - 1983 - Daily water and sediment discharges from selected rivers of the eastern United States; a time-series modeling approach","interactions":[],"lastModifiedDate":"2012-02-02T00:05:13","indexId":"wsp2216","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":"2216","title":"Daily water and sediment discharges from selected rivers of the eastern United States; a time-series modeling approach","docAbstract":"Time-series models were constructed for analysis of daily runoff and sediment discharge data from selected rivers of the Eastern United States. Logarithmic transformation and first-order differencing of the data sets were necessary to produce second-order, stationary time series and remove seasonal trends. \r\n\r\nCyclic models accounted for less than 42 percent of the variance in the water series and 31 percent in the sediment series. Analysis of the apparent oscillations of given frequencies occurring in the data indicates that frequently occurring storms can account for as much as 50 percent of the variation in sediment discharge. \r\n\r\nComponents of the frequency analysis indicate that a linear representation is reasonable for the water-sediment system. Models that incorporate lagged water discharge as input prove superior to univariate techniques in modeling and prediction of sediment discharges. The random component of the models includes errors in measurement and model hypothesis and indicates no serial correlation. An index of sediment production within or between drain-gage basins can be calculated from model parameters.","language":"ENGLISH","publisher":"U.S. Geological Survey,","doi":"10.3133/wsp2216","usgsCitation":"Fitzgerald, M.G., and Karlinger, M.R., 1983, Daily water and sediment discharges from selected rivers of the eastern United States; a time-series modeling approach: U.S. Geological Survey Water Supply Paper 2216, vi, 24 p. :ill., 1 map ;27 cm., https://doi.org/10.3133/wsp2216.","productDescription":"vi, 24 p. :ill., 1 map ;27 cm.","costCenters":[],"links":[{"id":137526,"rank":0,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/wsp/2216/report-thumb.jpg"},{"id":26423,"rank":300,"type":{"id":11,"text":"Document"},"url":"https://pubs.usgs.gov/wsp/2216/report.pdf","linkFileType":{"id":1,"text":"pdf"}}],"noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"4f4e4a96e4b07f02db65acb2","contributors":{"authors":[{"text":"Fitzgerald, Michael G.","contributorId":42942,"corporation":false,"usgs":true,"family":"Fitzgerald","given":"Michael","email":"","middleInitial":"G.","affiliations":[],"preferred":false,"id":143606,"contributorType":{"id":1,"text":"Authors"},"rank":1},{"text":"Karlinger, Michael R.","contributorId":10777,"corporation":false,"usgs":true,"family":"Karlinger","given":"Michael","email":"","middleInitial":"R.","affiliations":[],"preferred":false,"id":143605,"contributorType":{"id":1,"text":"Authors"},"rank":2}]}}
,{"id":9421,"text":"ofr83172 - 1983 - Garnet peridotites from Williams kimberlites, north-central Montana, U.S.A","interactions":[],"lastModifiedDate":"2022-10-31T19:54:25.920382","indexId":"ofr83172","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":"83-172","title":"Garnet peridotites from Williams kimberlites, north-central Montana, U.S.A","docAbstract":"<p>Two Williams kimberlites, 250x350m and 37x390m, in the eastern part of a swarm of 30 middle Eocene alnoitic diatremes in north-central Montana, USA, contain xenoliths of garnet-bearing lherzolites, harzburgites and dunites, in addition to spinel peridotites and upper and lower crustal amphibolites and granulites. Colluvial purple, red, and pink garnets are dominantly Mg- and Cr-rich, indicating their derivation From peridotites or megacrysts, and have CaO and Cr<sub>2</sub>O<sub>3</sub> contents that fall in the lherzolite trend. </p><p>Temperatures were calculated by the Lindsley-Dixon 20 kb method for lherzolites and by the O'Neill-Wood method for harzburgites and dunites, and pressures were calculated by the MacGregor method, or were assumed to be 50 kb for dunites. Most peridotites equilibrated at 1220-1350°C and 50-60 kb, well above a 44mW/m<sup>2</sup> shield geotherm and on or at higher P than the graphite-diamond boundary. Four lherzolites are low T-P (830-990°C, 23-42 kb) and are close to the shield geotherm. All four low T-P lherzolites have coarse textures whereas the high T-P cluster has both coarse and porphyroclastic textures, indicating a range of conditions of deformation and recrystallization in a restricted high T-P range. The tiny size (0.01-0.2 mm) of granulated and euhedral olivines in several xenoliths shows that deformation was occurring just prior to incorporation in kimberlite and that ascent was rapid enough (40-70 km/hr) to retard Further coarsening of fine-grained olivine. For other high T-P peridotites, cessation of deformation and beginning of recrystallization before or during inclusion in kimberlite is suggested by larger (up to 3mm) euhedral olivines in a matrix of fine granulated olivine or by optical continuity of large and nearby small olivines. </p><p>Two low T-P lherzolites contain distinctive, phlogopite-rimmed, 5-8mm clots of moderate-Cr garnet + Cr-spinel + Cr-diopside + enstatite that are inferred to have formed by reaction of an initial high-Cr garnet brought into the garnet + spinel stability Field. This suggests a reduction in pressure and temperature prior to inclusion in the kimberlite, followed by metasomatic introduction of phlogopite. These textural and compositional variations of peridotites seem most compatible with kimberlite generation and ascent during dynamic diapiric perturbation of the upper mantle.</p>","language":"English","publisher":"U.S. Geological Survey","doi":"10.3133/ofr83172","usgsCitation":"Hearn, B., and McGee, E.S., 1983, Garnet peridotites from Williams kimberlites, north-central Montana, U.S.A: U.S. Geological Survey Open-File Report 83-172, i, 26 p., https://doi.org/10.3133/ofr83172.","productDescription":"i, 26 p.","costCenters":[],"links":[{"id":408926,"rank":3,"type":{"id":36,"text":"NGMDB Index Page"},"url":"https://ngmdb.usgs.gov/Prodesc/proddesc_13923.htm","linkFileType":{"id":5,"text":"html"}},{"id":37132,"rank":300,"type":{"id":11,"text":"Document"},"url":"https://pubs.usgs.gov/of/1983/0172/report.pdf","linkFileType":{"id":1,"text":"pdf"}},{"id":141823,"rank":0,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/of/1983/0172/report-thumb.jpg"}],"country":"United States","state":"Montana","geographicExtents":"{\n  \"type\": \"FeatureCollection\",\n  \"features\": [\n    {\n      \"type\": \"Feature\",\n      \"properties\": {},\n      \"geometry\": {\n        \"coordinates\": [\n          [\n            [\n              -108.667,\n              47.867\n            ],\n            [\n              -108.667,\n              47.842\n            ],\n            [\n              -108.708,\n              47.842\n            ],\n            [\n              -108.708,\n              47.867\n            ],\n            [\n              -108.667,\n              47.867\n            ]\n          ]\n        ],\n        \"type\": \"Polygon\"\n      }\n    }\n  ]\n}","noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"4f4e4b28e4b07f02db6b135c","contributors":{"authors":[{"text":"Hearn, B.C.","contributorId":7700,"corporation":false,"usgs":true,"family":"Hearn","given":"B.C.","affiliations":[],"preferred":false,"id":159657,"contributorType":{"id":1,"text":"Authors"},"rank":1},{"text":"McGee, E. S.","contributorId":75927,"corporation":false,"usgs":true,"family":"McGee","given":"E.","email":"","middleInitial":"S.","affiliations":[],"preferred":false,"id":159658,"contributorType":{"id":1,"text":"Authors"},"rank":2}]}}
,{"id":38149,"text":"ofr82445 - 1983 - Aquifer systems in the Great Basin region of Nevada, Utah, and adjacent states: A study plan","interactions":[],"lastModifiedDate":"2022-10-17T15:30:33.03952","indexId":"ofr82445","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":"82-445","title":"Aquifer systems in the Great Basin region of Nevada, Utah, and adjacent states: A study plan","docAbstract":"<p>The Great Basin Regional Aquifer Study includes about 140,000 square miles in parts of Nevada, Utah, California, Idaho, Oregon, and Arizona. Within that area, 240 hydrographic areas occupy structural depressions formed primarily by basin-and-range faulting. The principal aquifers are in basin- fill deposits; however, permeable carbonate rocks underlie valleys in much of eastern Nevada and western Utah and are significant regional aquifers. Anticipated future water needs require a better understanding of the resource so that wise management will be possible. In October 1980, the U.S Geological Survey started a 4-year study to (1) describe the ground-water systems as they existed under natural conditions and as they exist today, (2) analyze the changes that have led to the systems' present condition, (3) tie the results of this and previous studies together in a regional analysis, and (4) provide means by which effects of future ground-water development can be estimated.</p><p>A plan of work is presented that describes the general approach to be taken in this study. It defines (1) the major task necessary to meet objectives and (2) constraints on the scope of work. The approach has been strongly influenced by the diverse nature of ground-water flow systems and the large number of basins. A detailed appraisal of 240 individual areas would require more resources than are available. Consequently, the general approach is to study selected \"typical\" areas and key hydrologic processes. Effort during the first 3 years will be directed toward describing the regional hydrology, conducting detailed studies of \"type\" areas, and studying selected hydrologic processes. Effort during the final year will be directed toward developing a regional analyses of results.</p><p>Special studies that will address hydrologic processes, key components of the ground-water system, and improved use of technology include evaluations of regional geochemistry, regional hydrogeology, recharge, ground-water discharge, and the use of remote sensing. Areas selected for study using ground-water flow models include the regional carbonate-rock province in eastern Nevada and western Utah, six valleys Las Vegas, Carson, Paradise, Dixie, Smith Creek, and Stagecoach in Nevada, plus Jordan Valley, the Milford area, and Tule Valley in Utah.</p>","language":"English","publisher":"U.S. Geological Survey","publisherLocation":"Carson City, NV","doi":"10.3133/ofr82445","usgsCitation":"Harrill, J.R., Welch, A., Prudic, D.E., Thomas, J.M., Carman, R.L., Plume, R.W., Gates, J., and Mason, J.L., 1983, Aquifer systems in the Great Basin region of Nevada, Utah, and adjacent states: A study plan: U.S. Geological Survey Open-File Report 82-445, Report: v, 49 p.; Plate: 24.00 in. x 20.00 in., https://doi.org/10.3133/ofr82445.","productDescription":"Report: v, 49 p.; Plate: 24.00 in. x 20.00 in.","numberOfPages":"54","costCenters":[{"id":610,"text":"Utah Water Science Center","active":true,"usgs":true}],"links":[{"id":64410,"rank":300,"type":{"id":11,"text":"Document"},"url":"https://pubs.usgs.gov/of/1982/0445/report.pdf","linkFileType":{"id":1,"text":"pdf"}},{"id":162631,"rank":0,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/of/1982/0445/report-thumb.jpg"},{"id":20564,"rank":400,"type":{"id":17,"text":"Plate"},"url":"https://pubs.usgs.gov/of/1982/0445/plate-1.pdf","linkFileType":{"id":1,"text":"pdf"}}],"country":"United States","state":"Nevada, Utah","noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"4f4e4ac5e4b07f02db679f6b","contributors":{"authors":[{"text":"Harrill, James R.","contributorId":99533,"corporation":false,"usgs":true,"family":"Harrill","given":"James","email":"","middleInitial":"R.","affiliations":[],"preferred":false,"id":219211,"contributorType":{"id":1,"text":"Authors"},"rank":1},{"text":"Welch, Alan H.","contributorId":45286,"corporation":false,"usgs":true,"family":"Welch","given":"Alan H.","affiliations":[],"preferred":false,"id":219205,"contributorType":{"id":1,"text":"Authors"},"rank":2},{"text":"Prudic, David E. deprudic@usgs.gov","contributorId":3430,"corporation":false,"usgs":true,"family":"Prudic","given":"David","email":"deprudic@usgs.gov","middleInitial":"E.","affiliations":[{"id":465,"text":"Nevada Water Science Center","active":true,"usgs":true}],"preferred":true,"id":219206,"contributorType":{"id":1,"text":"Authors"},"rank":3},{"text":"Thomas, James M.","contributorId":195094,"corporation":false,"usgs":false,"family":"Thomas","given":"James","email":"","middleInitial":"M.","affiliations":[],"preferred":false,"id":219210,"contributorType":{"id":1,"text":"Authors"},"rank":4},{"text":"Carman, Rita L.","contributorId":6468,"corporation":false,"usgs":true,"family":"Carman","given":"Rita","email":"","middleInitial":"L.","affiliations":[],"preferred":false,"id":219207,"contributorType":{"id":1,"text":"Authors"},"rank":5},{"text":"Plume, Russell W. rwplume@usgs.gov","contributorId":2303,"corporation":false,"usgs":true,"family":"Plume","given":"Russell","email":"rwplume@usgs.gov","middleInitial":"W.","affiliations":[],"preferred":true,"id":219208,"contributorType":{"id":1,"text":"Authors"},"rank":6},{"text":"Gates, Joseph S.","contributorId":21647,"corporation":false,"usgs":true,"family":"Gates","given":"Joseph S.","affiliations":[],"preferred":false,"id":219212,"contributorType":{"id":1,"text":"Authors"},"rank":7},{"text":"Mason, James L.","contributorId":14397,"corporation":false,"usgs":true,"family":"Mason","given":"James","email":"","middleInitial":"L.","affiliations":[],"preferred":false,"id":219209,"contributorType":{"id":1,"text":"Authors"},"rank":8}]}}
,{"id":9403,"text":"ofr82568 - 1983 - Instructions for using the U.S. Geological Survey data base of wells on Long Island, New York","interactions":[],"lastModifiedDate":"2012-02-02T00:06:14","indexId":"ofr82568","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":"82-568","title":"Instructions for using the U.S. Geological Survey data base of wells on Long Island, New York","docAbstract":"The population of central and eastern Long Island, New York depends on ground water for its supply of fresh water. Data on more than 7,500 wells on the island have been collected by various State and local agencies and compiled by the U.S. Geological Survey since 1906. During 1975-81, the Geological Survey developed a data base for its Data General Nova 1220 minicomputer to store and process the well information. The data base is composed of seven sections, each of which may be revised and updated. Three types of magnetic devices with limited capacity are used for data storage--disk, Linctape, and 9-track tape. This breakdown makes each section small enough to store and update on a small minicomputer while allowing simultaneous data retrieval from all sections. This manual gives complete instructions for revising, storing, and retrieving well data. Most programming is in FORTRAN, but some is in assembly language. (USGS)","language":"ENGLISH","publisher":"U.S. Geological Survey,","doi":"10.3133/ofr82568","usgsCitation":"Hawkins, G.W., and Terlecki, G.M., 1983, Instructions for using the U.S. Geological Survey data base of wells on Long Island, New York: U.S. Geological Survey Open-File Report 82-568, 194 p. (in various pagings) :ill. ;28 cm., https://doi.org/10.3133/ofr82568.","productDescription":"194 p. (in various pagings) :ill. ;28 cm.","costCenters":[],"links":[{"id":142196,"rank":0,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/of/1982/0568/report-thumb.jpg"},{"id":37116,"rank":300,"type":{"id":11,"text":"Document"},"url":"https://pubs.usgs.gov/of/1982/0568/report.pdf","linkFileType":{"id":1,"text":"pdf"}}],"noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"4f4e4ab0e4b07f02db66d6fe","contributors":{"authors":[{"text":"Hawkins, George W.","contributorId":42966,"corporation":false,"usgs":true,"family":"Hawkins","given":"George","email":"","middleInitial":"W.","affiliations":[],"preferred":false,"id":159624,"contributorType":{"id":1,"text":"Authors"},"rank":1},{"text":"Terlecki, Gregory M.","contributorId":93910,"corporation":false,"usgs":true,"family":"Terlecki","given":"Gregory","email":"","middleInitial":"M.","affiliations":[],"preferred":false,"id":159625,"contributorType":{"id":1,"text":"Authors"},"rank":2}]}}
,{"id":29911,"text":"wri834002 - 1983 - Ground-water contamination at Wurtsmith Air Force Base, Michigan","interactions":[],"lastModifiedDate":"2017-01-25T14:09:18","indexId":"wri834002","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":"83-4002","title":"Ground-water contamination at Wurtsmith Air Force Base, Michigan","docAbstract":"<p>A sand and gravel aquifer of glacial origin underlies Wurtsmith Air Force Base in northeastern lower Michigan. The aquifer overlies a thick clay layer at an average depth of 65 feet. The water table is about 10 feet below land surface in the western part of the Base and about 25 feet below land surface in the eastern part. A ground-water divide cuts diagonally across the Base from northwest to southeast. South of the divide, ground water flows to the Au Sable River; north of the divide, it flows to Van Etten Creek and Van Etten Lake. Mathematical models were used to aid in calculating rates of groundwater flow. Rates range from about 0.8 feet per day in the eastern part of the Base to about 0.3 feet per day in the western part. Models also were used as an aid in making decisions regarding purging of contaminated water from the aquifer. </p><p>In 1977, trichloroethylene was detected in the Air Force Base water-supply system. It had leaked from a buried storage tank near Building 43 in the southeastern part of the Base and moved northeastward under the influence of the natural ground-water gradient and the pumping of Base water-supply wells. In the most highly contaminated part of the plume, concentrations are greater than 1,000 micrograms per liter. Current purge pumping is removing some of the trichloroethylene, and seems to have arrested its eastward movement. Pumping of additional purge wells could increase the rate of removal. </p><p>Trichloroethylene has also been detected in ground water in the vicinity of the Base alert apron, where a plume from an unknown source extends northeastward off Base. A smaller, less well-defined area of contamination also occurs just north of the larger plume. Trichloroethylene, identified near the waste-treatment plant, seepage lagoons, and the northern landfill area, is related to activities and operations in these areas. Dichloroethylene and trichloroethylene occur in significant quantities westward of Building 43, upgradient from the major spill site. Benzene, indicative of ground-water contamination by a fuel substance, occurs in an area northeast of the bulk-fuel storage area. Analysis of a variety of chemical, physical, and biologic characteristics of water on the Base indicate that there is a measurable affect on ground-water quality from landfills, the seepage lagoon, and the waste-treatment plant.</p>","language":"English","publisher":"U.S. Geological Survey","publisherLocation":"Lansing, MI","doi":"10.3133/wri834002","collaboration":"Prepared in cooperation with the U.S. Air Force","usgsCitation":"Stark, J., Cummings, T., and Twenter, F.R., 1983, Ground-water contamination at Wurtsmith Air Force Base, Michigan: U.S. Geological Survey Water-Resources Investigations Report 83-4002, Document: ix, 93 p.; Plate: 41.58 x 35.42 inches, https://doi.org/10.3133/wri834002.","productDescription":"Document: ix, 93 p.; Plate: 41.58 x 35.42 inches","costCenters":[{"id":382,"text":"Michigan Water Science Center","active":true,"usgs":true}],"links":[{"id":58728,"rank":400,"type":{"id":17,"text":"Plate"},"url":"https://pubs.usgs.gov/wri/1983/4002/plate-1.pdf","linkFileType":{"id":1,"text":"pdf"}},{"id":58729,"rank":300,"type":{"id":11,"text":"Document"},"url":"https://pubs.usgs.gov/wri/1983/4002/report.pdf","linkFileType":{"id":1,"text":"pdf"}},{"id":119514,"rank":0,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/wri/1983/4002/report-thumb.jpg"}],"country":"United States","state":"Michigan","otherGeospatial":"Wurtsmith Air Force Base","geographicExtents":"{\n  \"type\": \"FeatureCollection\",\n  \"features\": [\n    {\n      \"type\": \"Feature\",\n      \"properties\": {},\n      \"geometry\": {\n        \"type\": \"Polygon\",\n        \"coordinates\": [\n          [\n            [\n              -83.416667,\n              44.483333\n            ],\n            [\n              -83.416667,\n              44.425\n            ],\n            [\n              -83.325,\n              44.425\n            ],\n            [\n              -83.325,\n              44.483333\n            ],\n            [\n              -83.416667,\n              44.483333\n            ]\n          ]\n        ]\n      }\n    }\n  ]\n}","noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"4f4e4aafe4b07f02db66d05d","contributors":{"authors":[{"text":"Stark, J. R.","contributorId":100406,"corporation":false,"usgs":true,"family":"Stark","given":"J. R.","affiliations":[],"preferred":false,"id":202340,"contributorType":{"id":1,"text":"Authors"},"rank":1},{"text":"Cummings, T. R.","contributorId":104082,"corporation":false,"usgs":true,"family":"Cummings","given":"T. R.","affiliations":[],"preferred":false,"id":202341,"contributorType":{"id":1,"text":"Authors"},"rank":2},{"text":"Twenter, F. R.","contributorId":81080,"corporation":false,"usgs":true,"family":"Twenter","given":"F.","email":"","middleInitial":"R.","affiliations":[],"preferred":false,"id":202339,"contributorType":{"id":1,"text":"Authors"},"rank":3}]}}
,{"id":19670,"text":"ofr83815 - 1983 - Geoelectric structure of the Gila-San Francisco Wilderness Area, Graham and Greenlee Counties, Arizona, from audio-magnetotelluric data","interactions":[],"lastModifiedDate":"2022-09-01T21:00:22.928432","indexId":"ofr83815","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":"83-815","title":"Geoelectric structure of the Gila-San Francisco Wilderness Area, Graham and Greenlee Counties, Arizona, from audio-magnetotelluric data","docAbstract":"Electromagnetic induction data using distant field sources, mostly of natural origin, in the frequency range of 4.5-27,000 Hz are analyzed to depict the geoelectric structure in an area of volcanic-rock cover located in southeastern Arizona between the Morenci and Safford porphyry copper deposits. The data for each station consist of scalar electromagnetic measurements at descrete frequencies for two-orthogonal magnetic and electric field pairs. Observations spaced about 5-km apart indicate resistivities in the range of 100-700 ohm-m for the unweathered Tertiary volcanic rocks to a depth of 200 to 500 m. Beneath this zone the data indicate resistivities in the range of 10-100 ohm-m that suggest the existence of an older volcanic rock unit. The less resistive unit appears to be displaced upward beneath Turtle Mountain, an area bounded to the northeast and southwest by mapped Basin and Range faults, and bounded to the southeast by an unmapped fault of older origin that trends northeast. Lateral changes in the resistivity of the two main geoelectric layers result in lowered resistivity in an area of known hot-springs near the confluence of the Gila and San Francisco Rivers, as well as along a north-south trending zone located on the east flank of Turtle Mountain, about 5-km (3-mi) west-northwest of the hot springs. This second anomaly is at a probable depth of 400-500 m and is interpreted to indicate a buried fault or fracture zone.","language":"English","publisher":"U.S. Geological Survey","doi":"10.3133/ofr83815","usgsCitation":"Klein, D.P., and Baer, M.J., 1983, Geoelectric structure of the Gila-San Francisco Wilderness Area, Graham and Greenlee Counties, Arizona, from audio-magnetotelluric data: U.S. Geological Survey Open-File Report 83-815, 109 p., https://doi.org/10.3133/ofr83815.","productDescription":"109 p.","costCenters":[],"links":[{"id":406098,"rank":3,"type":{"id":36,"text":"NGMDB Index Page"},"url":"https://ngmdb.usgs.gov/Prodesc/proddesc_14236.htm","linkFileType":{"id":5,"text":"html"}},{"id":49135,"rank":300,"type":{"id":11,"text":"Document"},"url":"https://pubs.usgs.gov/of/1983/0815/report.pdf","linkFileType":{"id":1,"text":"pdf"}},{"id":152182,"rank":0,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/of/1983/0815/report-thumb.jpg"}],"country":"United States","state":"Arizona","county":"Graham County, Greenlee County","otherGeospatial":"Gila-San Francisco Wilderness Area","geographicExtents":"{\n  \"type\": \"FeatureCollection\",\n  \"features\": [\n    {\n      \"type\": \"Feature\",\n      \"properties\": {},\n      \"geometry\": {\n        \"type\": \"Polygon\",\n        \"coordinates\": [\n          [\n            [\n              -109.566,\n              33.076\n            ],\n            [\n              -109.32,\n              33.076\n            ],\n            [\n              -109.32,\n              32.833\n            ],\n            [\n              -109.566,\n              32.833\n            ],\n            [\n              -109.566,\n              33.076\n            ]\n          ]\n        ]\n      }\n    }\n  ]\n}","noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"4f4e4b1de4b07f02db6a9b4e","contributors":{"authors":[{"text":"Klein, D. P.","contributorId":36555,"corporation":false,"usgs":true,"family":"Klein","given":"D.","email":"","middleInitial":"P.","affiliations":[{"id":595,"text":"U.S. Geological Survey","active":false,"usgs":true}],"preferred":false,"id":181308,"contributorType":{"id":1,"text":"Authors"},"rank":1},{"text":"Baer, M. J.","contributorId":102487,"corporation":false,"usgs":true,"family":"Baer","given":"M.","email":"","middleInitial":"J.","affiliations":[],"preferred":false,"id":181309,"contributorType":{"id":1,"text":"Authors"},"rank":2}]}}
,{"id":8287,"text":"ofr83187 - 1983 - Zinc, lead, and barite deposits and occurrences in Paleozoic rocks, east-central United States","interactions":[],"lastModifiedDate":"2012-02-02T00:06:00","indexId":"ofr83187","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":"83-187","title":"Zinc, lead, and barite deposits and occurrences in Paleozoic rocks, east-central United States","language":"ENGLISH","publisher":"U.S. Geological Survey,","doi":"10.3133/ofr83187","usgsCitation":"Clark, S.H., and Neeley, C.L., 1983, Zinc, lead, and barite deposits and occurrences in Paleozoic rocks, east-central United States: U.S. Geological Survey Open-File Report 83-187, 81 p. map ;28 cm., https://doi.org/10.3133/ofr83187.","productDescription":"81 p. map ;28 cm.","costCenters":[],"links":[{"id":140753,"rank":0,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/of/1983/0187/report-thumb.jpg"},{"id":35897,"rank":400,"type":{"id":17,"text":"Plate"},"url":"https://pubs.usgs.gov/of/1983/0187/plate-1.pdf","linkFileType":{"id":1,"text":"pdf"}},{"id":35898,"rank":300,"type":{"id":11,"text":"Document"},"url":"https://pubs.usgs.gov/of/1983/0187/report.pdf","linkFileType":{"id":1,"text":"pdf"}}],"noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"4f4e49d5e4b07f02db5ddeba","contributors":{"authors":[{"text":"Clark, Sandra H.","contributorId":40986,"corporation":false,"usgs":true,"family":"Clark","given":"Sandra","email":"","middleInitial":"H.","affiliations":[],"preferred":false,"id":157499,"contributorType":{"id":1,"text":"Authors"},"rank":1},{"text":"Neeley, Cathy L.","contributorId":47365,"corporation":false,"usgs":true,"family":"Neeley","given":"Cathy","email":"","middleInitial":"L.","affiliations":[],"preferred":false,"id":157500,"contributorType":{"id":1,"text":"Authors"},"rank":2}]}}
,{"id":32570,"text":"pp1170E - 1983 - A sillimanite gneiss dome in the Yukon crystalline terrane, east-central Alaska: Petrography and garnet-biotite geothermometry","interactions":[],"lastModifiedDate":"2022-12-20T19:46:25.517242","indexId":"pp1170E","displayToPublicDate":"1994-01-01T00:00:00","publicationYear":"1983","noYear":false,"publicationType":{"id":18,"text":"Report"},"publicationSubtype":{"id":5,"text":"USGS Numbered Series"},"seriesTitle":{"id":331,"text":"Professional Paper","code":"PP","onlineIssn":"2330-7102","printIssn":"1044-9612","active":true,"publicationSubtype":{"id":5}},"seriesNumber":"1170","chapter":"E","title":"A sillimanite gneiss dome in the Yukon crystalline terrane, east-central Alaska: Petrography and garnet-biotite geothermometry","docAbstract":"<p>No abstract available.</p>","language":"English","publisher":"U.S. Geological Survey","doi":"10.3133/pp1170E","usgsCitation":"Dusel-Bacon, C., and Foster, H., 1983, A sillimanite gneiss dome in the Yukon crystalline terrane, east-central Alaska: Petrography and garnet-biotite geothermometry: U.S. Geological Survey Professional Paper 1170, iii, 25 p., https://doi.org/10.3133/pp1170E.","productDescription":"iii, 25 p.","costCenters":[],"links":[{"id":60395,"rank":1,"type":{"id":11,"text":"Document"},"url":"https://pubs.usgs.gov/pp/1170e/report.pdf","linkFileType":{"id":1,"text":"pdf"}},{"id":119552,"rank":0,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/pp/1170e/report-thumb.jpg"},{"id":410805,"rank":3,"type":{"id":36,"text":"NGMDB Index Page"},"url":"https://ngmdb.usgs.gov/Prodesc/proddesc_74409.htm","linkFileType":{"id":5,"text":"html"}}],"country":"United States","state":"Alaska","geographicExtents":"{\n  \"type\": \"FeatureCollection\",\n  \"features\": [\n    {\n      \"type\": \"Feature\",\n      \"properties\": {},\n      \"geometry\": {\n        \"coordinates\": [\n          [\n            [\n              -146.180,\n              64.8106\n            ],\n            [\n              -146.180,\n              64.2978\n            ],\n            [\n              -145.1628,\n              64.2978\n            ],\n            [\n              -145.1628,\n              64.8106\n            ],\n            [\n              -146.180,\n              64.8106\n            ]\n          ]\n        ],\n        \"type\": \"Polygon\"\n      }\n    }\n  ]\n}","noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"4f4e4b17e4b07f02db6a6546","contributors":{"authors":[{"text":"Dusel-Bacon, Cynthia 0000-0001-8481-739X cdusel@usgs.gov","orcid":"https://orcid.org/0000-0001-8481-739X","contributorId":2797,"corporation":false,"usgs":true,"family":"Dusel-Bacon","given":"Cynthia","email":"cdusel@usgs.gov","affiliations":[{"id":312,"text":"Geology, Minerals, Energy, and Geophysics Science Center","active":true,"usgs":true}],"preferred":true,"id":208701,"contributorType":{"id":1,"text":"Authors"},"rank":1},{"text":"Foster, H.L.","contributorId":34894,"corporation":false,"usgs":true,"family":"Foster","given":"H.L.","email":"","affiliations":[],"preferred":false,"id":208702,"contributorType":{"id":1,"text":"Authors"},"rank":2}]}}
,{"id":19423,"text":"ofr83774 - 1983 - Geohydrology and water resources of the Papago Farms-Great Plain area, Papago Indian Reservation, Arizona, and the upper Rio Sonoyta area, Sonora, Mexico","interactions":[{"subject":{"id":19423,"text":"ofr83774 - 1983 - Geohydrology and water resources of the Papago Farms-Great Plain area, Papago Indian Reservation, Arizona, and the upper Rio Sonoyta area, Sonora, Mexico","indexId":"ofr83774","publicationYear":"1983","noYear":false,"title":"Geohydrology and water resources of the Papago Farms-Great Plain area, Papago Indian Reservation, Arizona, and the upper Rio Sonoyta area, Sonora, Mexico"},"predicate":"SUPERSEDED_BY","object":{"id":1899,"text":"wsp2258 - 1985 - Geohydrology and water resources of the Papago Farms-Great Plain area, Papago Indian Reservation, Arizona, and the upper Rio Sonoyta area, Sonora, Mexico","indexId":"wsp2258","publicationYear":"1985","noYear":false,"title":"Geohydrology and water resources of the Papago Farms-Great Plain area, Papago Indian Reservation, Arizona, and the upper Rio Sonoyta area, Sonora, Mexico"},"id":1}],"supersededBy":{"id":1899,"text":"wsp2258 - 1985 - Geohydrology and water resources of the Papago Farms-Great Plain area, Papago Indian Reservation, Arizona, and the upper Rio Sonoyta area, Sonora, Mexico","indexId":"wsp2258","publicationYear":"1985","noYear":false,"title":"Geohydrology and water resources of the Papago Farms-Great Plain area, Papago Indian Reservation, Arizona, and the upper Rio Sonoyta area, Sonora, Mexico"},"lastModifiedDate":"2021-01-26T19:53:48.989552","indexId":"ofr83774","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":"83-774","title":"Geohydrology and water resources of the Papago Farms-Great Plain area, Papago Indian Reservation, Arizona, and the upper Rio Sonoyta area, Sonora, Mexico","docAbstract":"<p>The Papago Farms-Great Plain and upper Rio Sonoyta study area includes about 490 square miles in south-central Arizona and north-central Sonora, Mexico. In the study area 23,700 acre-feet of ground water from the basin-fill deposits was used to irrigate more than 5,000 acres in 1981. Surface water is not a reliable source for irrigation or public supply. Ground water enters the area as underflow from the north and east and as recharge from the mountains, moves through basin-margin sediments, around the basin-center clays, and exits the area to the west beneath the Rio Sonoyta. Ground-water withdrawals in the upper Rio Sonoyta area do not appear to have an effect on water levels in the Papago Farms-Great Plain area. Depth to water ranges from 500 feet near the southern boundary to 150 feet in the center of study area. About 10 million acre-feet of recoverable ground water is stored in the upper 400 feet of the aquifer. Storage is being depleted at a rate of 19,000 acre-feet per year. The ground water is a sodium and bicarbonate type and has an anomalously high content of arsenic and fluoride. (USGS)</p>","language":"English","publisher":"U.S. Geological Survey","publisherLocation":"Reston, VA","doi":"10.3133/ofr83774","usgsCitation":"Hollett, K., 1983, Geohydrology and water resources of the Papago Farms-Great Plain area, Papago Indian Reservation, Arizona, and the upper Rio Sonoyta area, Sonora, Mexico: U.S. Geological Survey Open-File Report 83-774, vi, 76 p., https://doi.org/10.3133/ofr83774.","productDescription":"vi, 76 p.","costCenters":[],"links":[{"id":382608,"rank":2,"type":{"id":11,"text":"Document"},"url":"https://pubs.usgs.gov/of/1983/0774/report.pdf","linkFileType":{"id":1,"text":"pdf"}},{"id":152621,"rank":0,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/of/1983/0774/report-thumb.jpg"}],"country":"United States","state":"Arizona","otherGeospatial":"Papago Indian Reservation","geographicExtents":"{\n  \"type\": \"FeatureCollection\",\n  \"features\": [\n    {\n      \"type\": \"Feature\",\n      \"properties\": {},\n      \"geometry\": {\n        \"type\": \"Polygon\",\n        \"coordinates\": [\n          [\n            [\n              -113.2470703125,\n              31.765537409484374\n            ],\n            [\n              -111.236572265625,\n              31.765537409484374\n            ],\n            [\n              -111.236572265625,\n              33.0178760185549\n            ],\n            [\n              -113.2470703125,\n              33.0178760185549\n            ],\n            [\n              -113.2470703125,\n              31.765537409484374\n            ]\n          ]\n        ]\n      }\n    }\n  ]\n}","noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"4f4e4b1be4b07f02db6a8b25","contributors":{"authors":[{"text":"Hollett, K.J.","contributorId":23570,"corporation":false,"usgs":true,"family":"Hollett","given":"K.J.","affiliations":[],"preferred":false,"id":180879,"contributorType":{"id":1,"text":"Authors"},"rank":1}]}}
,{"id":7624,"text":"ofr83157 - 1983 - Proceedings of Conference XVIII: a workshop on \"Continuing actions to reduce losses from earthquakes in the Mississippi Valley area,\" 24-26 May, 1982, St. Louis, Missouri","interactions":[],"lastModifiedDate":"2018-09-19T18:47:58","indexId":"ofr83157","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":"83-157","title":"Proceedings of Conference XVIII: a workshop on \"Continuing actions to reduce losses from earthquakes in the Mississippi Valley area,\" 24-26 May, 1982, St. Louis, Missouri","docAbstract":"<p>The U.S. Geological Survey and the Federal Emergency Management Agency \nsponsored a workshop on, \"Continuing Actions to Reduce Losses from Earthquakes \nin the Mississippi Valley area,\" in St. Louis, Missouri, on May 24-26, 1982. \nSeventy individuals (see Appendix A) representing local, State, and Federal \ngovernment; business and industry; and the research community participated in \nthe three day workshop. Collectively, the participants had backgrounds in \ndisaster preparedness, disaster response and recovery, geology, geophysics, \nseismology, engineering, architecture, social science, law, insurance, and \nland-use planning. Two-thirds of them came from the Mississippi Valley area\nabout one half of these had also attended an earlier USGS-FEMA workshop held \nin Knoxville, Tennessee on September 16-18, 1981 (Hays, 1982).</p>\n<br/>\n<p>The St. Louis workshop is the 18th in the continuing series of \nconferences and workshops which the Geological Survey initiated in 1977 to \nimprove the transfer and application of research results throughout the \nNation. It is the second workshop to focus on dealing with the earthquake \nthreat in the Eastern United States. The first one, \"Preparing for and \nResponding to a Damaging Earthquake in the Eastern United States,\" was held in \nKnoxville, Tennessee, and emphasized the development of a draft 5-year plan to \nimprove the state-of-earthquake-preparedness. The Knoxville workshop \ndemonstrated that policymakers and members of the scientific-technical \ncommunity can assimilate and synthesize a great deal of information and work \ntogether to devise practical plans. The St. Louis workshop, a sequel to the \nKnoxville workshop, identified those actions out of the range of possible \nactions which are most achievable; that is, the actions having the highest\npayoff and trre lowest cost and effort requirements. These action plans, which \nidentify steps that can be undertaken immediately to reduce losses from \nearthquakes in each of the seven States in the Mississippi Valley area, are \ncontained in this report. The draft 5-year plan for the Central United \nStates, prepared in the Knoxville workshop, was the starting point of the \nsmall group discussions in the St. Louis workshop which lead to the action \nplans contained in this report. For completeness, the draft 5-year plan for \nthe Central United States is reproduced as Appendix B.</p>","language":"English","publisher":"U.S. Geological Survey","publisherLocation":"Reston, VA","doi":"10.3133/ofr83157","usgsCitation":"Hays, W., and Kitzmiller, C., 1983, Proceedings of Conference XVIII: a workshop on \"Continuing actions to reduce losses from earthquakes in the Mississippi Valley area,\" 24-26 May, 1982, St. Louis, Missouri: U.S. Geological Survey Open-File Report 83-157, 140 p., https://doi.org/10.3133/ofr83157.","productDescription":"140 p.","numberOfPages":"169","costCenters":[{"id":414,"text":"National Earthquake Hazards Reduction Program","active":false,"usgs":true}],"links":[{"id":139730,"rank":0,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/of/1983/0157/report-thumb.jpg"},{"id":277916,"type":{"id":11,"text":"Document"},"url":"https://pubs.usgs.gov/of/1983/0157/report.pdf"}],"country":"United States","noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"4f4e4a9ee4b07f02db660813","contributors":{"editors":[{"text":"Gori, Paula L.","contributorId":75520,"corporation":false,"usgs":true,"family":"Gori","given":"Paula","email":"","middleInitial":"L.","affiliations":[],"preferred":false,"id":745696,"contributorType":{"id":2,"text":"Editors"},"rank":1}],"authors":[{"text":"Hays, Walter W.","contributorId":66669,"corporation":false,"usgs":true,"family":"Hays","given":"Walter W.","affiliations":[],"preferred":false,"id":156330,"contributorType":{"id":1,"text":"Authors"},"rank":1},{"text":"Kitzmiller, Carla (compiler)","contributorId":27852,"corporation":false,"usgs":true,"family":"Kitzmiller","given":"Carla","suffix":"(compiler)","email":"","affiliations":[],"preferred":false,"id":156329,"contributorType":{"id":1,"text":"Authors"},"rank":2}]}}
,{"id":56202,"text":"wdrNY821 - 1983 - Water resources data, New York, water year 1982, volume 1, eastern New York, excluding Long Island","interactions":[],"lastModifiedDate":"2020-05-12T23:04:07.044521","indexId":"wdrNY821","displayToPublicDate":"1994-01-01T00:00:00","publicationYear":"1983","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":"NY-82-1","title":"Water resources data, New York, water year 1982, volume 1, eastern New York, excluding Long Island","docAbstract":"<p>No abstract available.&nbsp;</p>","language":"English","publisher":"U.S. Geological Survey","publisherLocation":"Reston, VA","doi":"10.3133/wdrNY821","usgsCitation":"Zembrzuski, T., Burke, P.M., Archer, R., and Robideau, J., 1983, Water resources data, New York, water year 1982, volume 1, eastern New York, excluding Long Island: U.S. Geological Survey Water Data Report NY-82-1, viii, 267 p. , https://doi.org/10.3133/wdrNY821.","productDescription":"viii, 267 p. 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Jr.","contributorId":75594,"corporation":false,"usgs":true,"family":"Zembrzuski","given":"T.J.","suffix":"Jr.","email":"","affiliations":[],"preferred":false,"id":254914,"contributorType":{"id":1,"text":"Authors"},"rank":1},{"text":"Burke, P. M.","contributorId":8478,"corporation":false,"usgs":true,"family":"Burke","given":"P.","email":"","middleInitial":"M.","affiliations":[],"preferred":false,"id":254911,"contributorType":{"id":1,"text":"Authors"},"rank":2},{"text":"Archer, R.J.","contributorId":55069,"corporation":false,"usgs":true,"family":"Archer","given":"R.J.","email":"","affiliations":[],"preferred":false,"id":254913,"contributorType":{"id":1,"text":"Authors"},"rank":3},{"text":"Robideau, J.A.","contributorId":17617,"corporation":false,"usgs":true,"family":"Robideau","given":"J.A.","email":"","affiliations":[],"preferred":false,"id":254912,"contributorType":{"id":1,"text":"Authors"},"rank":4}]}}
,{"id":53499,"text":"fwsobs82_10_45 - 1983 - Habitat Suitability Index Models: Fisher","interactions":[],"lastModifiedDate":"2016-09-16T10:10:29","indexId":"fwsobs82_10_45","displayToPublicDate":"1994-01-01T00:00:00","publicationYear":"1983","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":"82/10.45","subseriesTitle":"Habitat Suitability Index","title":"Habitat Suitability Index Models: Fisher","docAbstract":"<p>The fisher (Martes pennanti) is the largest member of its genus and is found only i n North America (Powell 1982). Within the contiguous United States, indigenous and reintroduced populations presently inhabit portions of the Appalachian Mountains from New England south to West Virginia in the east; northern Wisconsin, Minnesota, and Michigan's upper peninsula in the Midwest; northern Idaho and western Montana in the Northwest; and as far south as northern California along the West Coast.</p>","language":"English","publisher":"U.S. Fish and Wildlife Service","usgsCitation":"Allen, A.W., 1983, Habitat Suitability Index Models: Fisher: FWS/OBS 82/10.45, vi, 19 p.","productDescription":"vi, 19 p.","costCenters":[{"id":595,"text":"U.S. Geological Survey","active":false,"usgs":true}],"links":[{"id":8271,"rank":300,"type":{"id":11,"text":"Document"},"url":"https://archive.usgs.gov/archive/sites/www.nwrc.usgs.gov/wdb/pub/hsi/hsi-045.pdf","linkFileType":{"id":1,"text":"pdf"}},{"id":177823,"rank":0,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/thumbnails/outside_thumb.jpg"}],"noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"4f4e4a80e4b07f02db6498a6","contributors":{"authors":[{"text":"Allen, Arthur W.","contributorId":40648,"corporation":false,"usgs":true,"family":"Allen","given":"Arthur","email":"","middleInitial":"W.","affiliations":[],"preferred":false,"id":247706,"contributorType":{"id":1,"text":"Authors"},"rank":1}]}}
,{"id":44502,"text":"wri834031 - 1983 - Hydrogeologic and water-quality characteristics of the Mount Simon-Hinckley aquifer, southeast Minnesota","interactions":[],"lastModifiedDate":"2023-03-13T21:30:44.488946","indexId":"wri834031","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":"83-4031","title":"Hydrogeologic and water-quality characteristics of the Mount Simon-Hinckley aquifer, southeast Minnesota","docAbstract":"<p>The Mount Simon-Hinckley aquifer in southeast Minnesota consists of a thick sequence of sandstone that generally yields large quantities of good-quality water to wells. The aquifer is most important as a source of water supply in the Twin Cities area, where it supplies approximately 10 percent of the ground water used. It is the uppermost bedrock aquifer and, locally, the principal source of domestic supply where it is present north of the Twin Cities. Yield to wells are generally about 500 gallons per minute but may be as high as 2,000 gallons per minute. The aquifer is a good potential source of water because of (1) large quantities of water in storage, (2) adequate yields to wells, and (3) good water quality.</p>\n<p>The quality of water in the aquifer is generally acceptable for municipal, industrial, and domestic uses. The dissolved-solids concentration in water from the aquifer ranges from a minimum of 48 milligrams per liter to a maximum of 2,810 milligrams per liter. The lowest values are in the eastern and northern parts of the aquifer, where bedrock is at or close to land surface. The highest concentrations are in the southwestern part of the aquifer, where leakage from over lying Cretaceous rocks is highly mineralized water. Magnesium and sulfate concentrations are also high in the southwest. The dissolved-solids concentration generally increases with depth in the aquifer. The predominant water type in the aquifer is calcium magnesium bicarbonate, although sodium chloride waters are present at depth and in the discharge areas along large rivers.</p>\n<p>This report is one of a series of the hydrogeology and water quality of the 14 principal aquifers in Minnesota prepared by the U.S. Geological Survey. The U.S. Environmental Protection Agency requested these studies because of the need for information to develop its Underground Injection Control Program.</p>","language":"English","publisher":"U.S. Geological Survey","publisherLocation":"Reston, VA","doi":"10.3133/wri834031","collaboration":"Prepared in cooperation with the U.S. Environmental Protection Agency","usgsCitation":"Wolf, R.J., Ruhl, J.F., and Adolphson, D.G., 1983, Hydrogeologic and water-quality characteristics of the Mount Simon-Hinckley aquifer, southeast Minnesota: U.S. Geological Survey Water-Resources Investigations Report 83-4031, 2 Plates: 39.71 x 33.69 inches and 33.46 x 39.65 inches, https://doi.org/10.3133/wri834031.","productDescription":"2 Plates: 39.71 x 33.69 inches and 33.46 x 39.65 inches","onlineOnly":"N","additionalOnlineFiles":"N","costCenters":[{"id":392,"text":"Minnesota Water Science Center","active":true,"usgs":true}],"links":[{"id":81877,"rank":3,"type":{"id":17,"text":"Plate"},"url":"https://pubs.usgs.gov/wri/1983/4031/plate-2.pdf","linkFileType":{"id":1,"text":"pdf"}},{"id":135250,"rank":1,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/thumbnails/usgs_thumb.jpg"},{"id":81876,"rank":2,"type":{"id":17,"text":"Plate"},"url":"https://pubs.usgs.gov/wri/1983/4031/plate-1.pdf","linkFileType":{"id":1,"text":"pdf"}},{"id":414058,"rank":4,"type":{"id":36,"text":"NGMDB Index Page"},"url":"https://ngmdb.usgs.gov/Prodesc/proddesc_35674.htm","linkFileType":{"id":5,"text":"html"}}],"country":"United States","state":"Minnesota","otherGeospatial":"Mount Simon-Hinckley aquifer","geographicExtents":"{ \"type\": \"FeatureCollection\", \"features\": [ { \"type\": \"Feature\", \"properties\": {}, \"geometry\": { \"type\": \"Polygon\", \"coordinates\": [ [ [ -92.88665771484375, 45.625563438215956 ], [ -92.87841796875, 45.67740123855739 ], [ -92.8619384765625, 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,{"id":46247,"text":"ofr82116 - 1983 - Map showing ground-water conditions in the Tonto basin area, Gila County, Arizona; 1978-79","interactions":[],"lastModifiedDate":"2022-04-20T22:40:32.0983","indexId":"ofr82116","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":"82-116","title":"Map showing ground-water conditions in the Tonto basin area, Gila County, Arizona; 1978-79","docAbstract":"<p>The Tonto basin area includes about 955 mi<sup>2</sup> in central Arizona. The area is bounded on the north by the Mogollon Rim, on the east by the Sierra Ancha Mountains, on the west by the Mazatzal Mountains, and on the south by Theodore Roosevelt Lake. The area is drained by Tonto Creek, which flows north to south and discharges into Theodore Roosevelt Lake.&nbsp;</p><p>Because the Tonta basin area is entirely within the Tonto National Forest, only about 3 percent of the land is privately owned and, for the most part, wells inventoried were on private land. Only selected wells are shown on the map because of the high well density on the private land.</p>","language":"English","publisher":"U.S. Geological Survey","doi":"10.3133/ofr82116","collaboration":"Prepared in cooperation with the Arizona Department of Water Resources","usgsCitation":"Denis, E., 1983, Map showing ground-water conditions in the Tonto basin area, Gila County, Arizona; 1978-79: U.S. Geological Survey Open-File Report 82-116, 1 Plate: 31.41 x 36.54 inches, https://doi.org/10.3133/ofr82116.","productDescription":"1 Plate: 31.41 x 36.54 inches","costCenters":[],"links":[{"id":399364,"rank":2,"type":{"id":17,"text":"Plate"},"url":"https://pubs.usgs.gov/of/1982/0116/plate-1.pdf","linkFileType":{"id":1,"text":"pdf"}},{"id":170961,"rank":0,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/of/1982/0116/report-thumb.jpg"}],"country":"United States","state":"Arizona","county":"Gila County","otherGeospatial":"Tonto basin 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E.E.","contributorId":53756,"corporation":false,"usgs":true,"family":"Denis","given":"E.E.","email":"","affiliations":[],"preferred":false,"id":232939,"contributorType":{"id":1,"text":"Authors"},"rank":1}]}}
,{"id":59808,"text":"mf1540B - 1983 - Aeromagnetic map and interpretation of geophysical data from the Condrey Mountain Roadless Area, Siskiyou County, California","interactions":[],"lastModifiedDate":"2016-08-22T14:06:01","indexId":"mf1540B","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":"1540","chapter":"B","title":"Aeromagnetic map and interpretation of geophysical data from the Condrey Mountain Roadless Area, Siskiyou County, California","docAbstract":"<p>The Condrey Mountain Roadless Area lies within the Klamath Mountains geologic province, a province composed of four eastward-dipping imbricate thrust slices or belts consisting predominantly of marine arc-related volcanic and sedimentary rocks, but also including significant amounts of ultramafic and other ophiolitic rocks (Irwin, 1981). From west to east the four Klamath Mountains thrust slices are called the western Jurassic belt, the western Paleozoic and Triassic belt, the central metamorphic belt, and the eastern Klamath belt. The Condrey Mountain Road less Area is located within a structural window in the western Paleozoic and Triassic belt, a window in which the structural dome comprised of the Condrey Mountain Schist is exposed (Coleman and others, 1983). North, east and south of the roadless area, the Condrey Mountain Schist is separated from the overlying western Paleozoic and Triassic belt by a low-angle regional thrust, whereas to the west the two units are in high-angle fault contact (Coleman and others, 1983).</p>\n<p>The Condrey Mountain schist consists mainly of sedimentary and volcanic rocks metamorphosed to greenschist facies. Metasedimentary rocks are exposed over most of the eastern and central parts of the structural window. Metavolcanic rocks occupy the western part of the window but also occur in small exposures within the metasedimentary rocks and along the eastern and southern margins of the window. Tabular bodies of metaserpentinite, the largest of which crops out near White Mountain, are contained within the metasedimentary rocks. Densities of hand samples from 11 sites scattered throughout the Condrey Mountain window average 2.66&plusmn;0.05 g/cm<sup>3</sup>. The four samples of metavolcanic rocks yielded a higher average density than the seven samples of metasedimentary rocks (2.71&plusmn;0.04 g/cm<sup>3</sup> versus 2.63&plusmn;0.03 g/cm<sup>3</sup>).</p>\n<p>Along the western edge of the Condrey Mountain Road less Area, numerous narrow north-trending zones of mineralized schist extend from near Copper Butte on the south, northward to Elliot Creek (Coleman and others, 1983). These zones contain abundant pyrite mineralization associated with pyrrhotite, chalcopyrite, qalena, and sphalerite. The Blue Ledge mine area, 2 mi north-northeast of Copper Butte, is located in a zone of mineralized schist.</p>\n<p>The western Paleozoic and Triassic belt that nearly surrounds the Condrey Mountain Schist is a melange of sedimentary, volcanic, and ultramafic rocks metamorphosed to amphibolite facies (Coleman and others, 1983). Only two samples of the metamorphic melange were collected near the Condrcy Mountain Road less Area, but extensive sampling of this unit southwest of the roadless area yielded an average sample density of 2.86&plusmn;0.15 g/cm<sup>3</sup> (112 samples) (Jachens and others, 1983).</p>","language":"English","publisher":"U.S. Geological Survey","publisherLocation":"Reston, VA","doi":"10.3133/mf1540B","usgsCitation":"Jachens, R., and Elder, W., 1983, Aeromagnetic map and interpretation of geophysical data from the Condrey Mountain Roadless Area, Siskiyou County, California: U.S. Geological Survey Miscellaneous Field Studies Map 1540, Plate: 47.54 x 29.96 inches, https://doi.org/10.3133/mf1540B.","productDescription":"Plate: 47.54 x 29.96 inches","onlineOnly":"N","additionalOnlineFiles":"N","costCenters":[],"links":[{"id":183643,"rank":0,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/thumbnails/mf1540B.JPG"},{"id":327288,"rank":1,"type":{"id":17,"text":"Plate"},"url":"https://pubs.usgs.gov/mf/1540-B/plate-1.pdf","linkFileType":{"id":1,"text":"pdf"}}],"scale":"0","country":"United States","state":"California","county":"Siskiyou County","otherGeospatial":"Condrey Mountain Roadless Area","geographicExtents":"{ \"type\": \"FeatureCollection\", \"features\": [ { \"type\": \"Feature\", \"properties\": {}, \"geometry\": { \"type\": \"Polygon\", \"coordinates\": [ [ [ -123.25,41.833333333333336 ], [ -123.25,42 ], [ -122.75,42 ], [ -122.75,41.833333333333336 ], [ -123.25,41.833333333333336 ] ] ] } } ] }","noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"4f4e4b00e4b07f02db69835b","contributors":{"authors":[{"text":"Jachens, R.C.","contributorId":55433,"corporation":false,"usgs":true,"family":"Jachens","given":"R.C.","email":"","affiliations":[],"preferred":false,"id":262631,"contributorType":{"id":1,"text":"Authors"},"rank":1},{"text":"Elder, W.P.","contributorId":65467,"corporation":false,"usgs":true,"family":"Elder","given":"W.P.","email":"","affiliations":[],"preferred":false,"id":262632,"contributorType":{"id":1,"text":"Authors"},"rank":2}]}}
,{"id":61514,"text":"mf1554 - 1983 - Environmental-stratigraphic cross sections of the Cretaceous Fox Hills Sandstone and Hell Creek Formation and Paleocene Fort Union Formation, Richland and Roosevelt Counties, Montana","interactions":[],"lastModifiedDate":"2016-08-23T10:42:11","indexId":"mf1554","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":"1554","title":"Environmental-stratigraphic cross sections of the Cretaceous Fox Hills Sandstone and Hell Creek Formation and Paleocene Fort Union Formation, Richland and Roosevelt Counties, Montana","docAbstract":"<p>This study was conducted to determine the stratigraphic, lithofacies, and deopsitional relationships of the Cretaceous Fox Hills Sandstone and Hell Creek Formation and The Paleocene Fort Union Formation. These relationships, shown in sections A-A', B-B', C-C', and D-D', we established form nearly continuous exposures in the Missouri River valley in Richland and Roosevelt Counties, Mont. The river valley topography is characterized by badlands, which permitted detailed description and construction of the stratigraphic framework of the formations within a 30-mi-long belt of exposures paralleling the Missouri River. This area of study is on the western flank of the Williston Basin and east of the Poplar Dome. The latter structure imparted a northeasterly regional dip to the rocks, which averages 25 ft per mi and is as much as 100 ft per mi according to Spencer (1980). The regional dip resulted in exposure of older rocks (Cretaceous) in the west to younger rocks (Tertiary) in the east.&nbsp;</p>","language":"English","publisher":"U.S. Geological Survey","publisherLocation":"Reston, VA","doi":"10.3133/mf1554","isbn":"0607812842","usgsCitation":"Flores, R.M., and Lepp, C., 1983, Environmental-stratigraphic cross sections of the Cretaceous Fox Hills Sandstone and Hell Creek Formation and Paleocene Fort Union Formation, Richland and Roosevelt Counties, Montana: U.S. Geological Survey Miscellaneous Field Studies Map 1554, 42.07 x 49.32 in, https://doi.org/10.3133/mf1554.","productDescription":"42.07 x 49.32 in","onlineOnly":"N","additionalOnlineFiles":"N","costCenters":[],"links":[{"id":179908,"rank":0,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/thumbnails/mf1554.PNG"},{"id":327610,"rank":1,"type":{"id":17,"text":"Plate"},"url":"https://pubs.usgs.gov/mf/1554/plate-1.pdf","linkFileType":{"id":1,"text":"pdf"}}],"scale":"1","country":"United States","state":"Montana","otherGeospatial":"Missouri River","geographicExtents":"{ \"type\": \"FeatureCollection\", \"features\": [ { \"type\": \"Feature\", \"properties\": {}, \"geometry\": { \"type\": \"Polygon\", \"coordinates\": [ [ [ -105,48.083333333333336 ], [ -105,48.166666666666664 ], [ -104.35111111111111,48.166666666666664 ], [ -104.35111111111111,48.083333333333336 ], [ -105,48.083333333333336 ] ] ] } } ] }","noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"4f4e4a13e4b07f02db602208","contributors":{"authors":[{"text":"Flores, R. M.","contributorId":106899,"corporation":false,"usgs":true,"family":"Flores","given":"R.","email":"","middleInitial":"M.","affiliations":[],"preferred":false,"id":265852,"contributorType":{"id":1,"text":"Authors"},"rank":1},{"text":"Lepp, C.L.","contributorId":76821,"corporation":false,"usgs":true,"family":"Lepp","given":"C.L.","email":"","affiliations":[],"preferred":false,"id":265851,"contributorType":{"id":1,"text":"Authors"},"rank":2}]}}
,{"id":59031,"text":"mf1424 - 1983 - Structure maps and seismic stratigraphy of the Yakataga segment of the continental margin, northern Gulf of Alaska","interactions":[],"lastModifiedDate":"2015-10-20T11:19:54","indexId":"mf1424","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":"1424","title":"Structure maps and seismic stratigraphy of the Yakataga segment of the continental margin, northern Gulf of Alaska","docAbstract":"<p>Multichannel seismic-reflection data show the late Cenozoic structure, seismic stratigraphy, and geologic history of the Yakataga segment of the continental margin, between Icy Bay and Kayak Island, northern Gulf of Alaska. The structure of the Yakataga segment consists of broad folds and associated thrust faults beneath the continental shelf and slope, trending generally northeast in the eastern part of the s~gment to east-west in the western part. Anticlines are generally asymmetric and doubly plunging and are commonly bounded on the seaward side by high-angle thrust faults. The degree of deformation is less intense than is observed in adjacent onshore areas. The age of deformation decreases seaward and the deformation shows an overall southeastward migration with time. Structures of similar age define three structural zones; structural growth was roughly contemporaneous in each structural zone, although the local growth pattern is complex in detail. Deformation within each structural zone was followed by subsidence and burial by rapidly deposited marine sediment. Deformation appears to have been continuous during the late Cenozoic, rather than a series of discrete events, because subsidence of a particular structural zone is accompanied by initiation of growth on a younger, more seaward zone. Varying degrees of reactivation of the older structures within recent time have resulted in renewed uplift of these structures. Average sedimentation, uplift, and subsidence rates are all extremely high, and generally range from about 1 to 2 m/1,000 yr; these rates can locally be much higher. The average strike of structures in the Yakataga segment indicates northwest-southeastward compression and is consistent with the current convergence direction between the Pacific and North America plates. Observed shortening within the segment is much less than required by the late Cenozoic convergence rate (about 6 cm/yr), and the major deformation is taken up elsewhere, primarily onshore. Thus, the deformation of the Yakataga segment is caused by minor shortening of the continental margin between Cross Sound and Kayak Island, which together comprise the Yakutat block, as the margin moves northwestward with the Pacific plate and collides with the North America plate.</p>","language":"English","publisher":"U.S. Geological Survey","doi":"10.3133/mf1424","usgsCitation":"Bruns, T., and Schwab, W.C., 1983, Structure maps and seismic stratigraphy of the Yakataga segment of the continental margin, northern Gulf of Alaska: U.S. Geological Survey Miscellaneous Field Studies Map 1424, Report: 20 p.; 4 Plates: 43.68 x 35.60 inches or smaller, https://doi.org/10.3133/mf1424.","productDescription":"Report: 20 p.; 4 Plates: 43.68 x 35.60 inches or smaller","onlineOnly":"N","additionalOnlineFiles":"N","costCenters":[],"links":[{"id":183714,"rank":0,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/thumbnails/mf1424.jpg"},{"id":105852,"rank":700,"type":{"id":15,"text":"Index Page"},"url":"https://ngmdb.usgs.gov/Prodesc/proddesc_7167.htm","linkFileType":{"id":5,"text":"html"},"description":"7167"},{"id":310127,"rank":701,"type":{"id":11,"text":"Document"},"url":"https://pubs.usgs.gov/mf/1424/report.pdf","text":"Report","linkFileType":{"id":1,"text":"pdf"}},{"id":310128,"rank":702,"type":{"id":17,"text":"Plate"},"url":"https://pubs.usgs.gov/mf/1424/plate-1.pdf","text":"Plate 1","linkFileType":{"id":1,"text":"pdf"}},{"id":310129,"rank":703,"type":{"id":17,"text":"Plate"},"url":"https://pubs.usgs.gov/mf/1424/plate-2.pdf","text":"Plate 2","linkFileType":{"id":1,"text":"pdf"}},{"id":310130,"rank":704,"type":{"id":17,"text":"Plate"},"url":"https://pubs.usgs.gov/mf/1424/plate-3.pdf","text":"Plate 3","linkFileType":{"id":1,"text":"pdf"}},{"id":310131,"rank":705,"type":{"id":17,"text":"Plate"},"url":"https://pubs.usgs.gov/mf/1424/plate-4.pdf","text":"Plate 4","linkFileType":{"id":1,"text":"pdf"}}],"country":"United States","state":"Alaska","geographicExtents":"{ \"type\": \"FeatureCollection\", \"features\": [ { \"type\": \"Feature\", \"properties\": {}, \"geometry\": { \"type\": \"Polygon\", \"coordinates\": [ [ [ -145,59 ], [ -145,60.5 ], [ -141,60.5 ], [ -141,59 ], [ -145,59 ] ] ] } } ] }","noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"4f4e4b0ae4b07f02db69d017","contributors":{"authors":[{"text":"Bruns, T.R.","contributorId":96683,"corporation":false,"usgs":true,"family":"Bruns","given":"T.R.","email":"","affiliations":[],"preferred":false,"id":261298,"contributorType":{"id":1,"text":"Authors"},"rank":1},{"text":"Schwab, W. C.","contributorId":78740,"corporation":false,"usgs":true,"family":"Schwab","given":"W.","email":"","middleInitial":"C.","affiliations":[],"preferred":false,"id":261297,"contributorType":{"id":1,"text":"Authors"},"rank":2}]}}
,{"id":59810,"text":"mf1231D - 1983 - Map showing aeromagnetic interpretation of the Golden Trout Wilderness, Tulare and Inyo counties, California","interactions":[],"lastModifiedDate":"2016-08-22T14:02:14","indexId":"mf1231D","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":"1231","chapter":"D","title":"Map showing aeromagnetic interpretation of the Golden Trout Wilderness, Tulare and Inyo counties, California","docAbstract":"<p>The Golden Trout Wilderness covers 457 mi<sup>2</sup><sup>&nbsp;</sup>in the rugged forested part of the southern Sierra Nevada. &nbsp;It is bounded on the east by Owens Valley, on the north by Sequoia National Park, and on the west and south by U.S. Forest Service multiple-use lands. &nbsp;The east side of the area is accesible from U.S. Highway 395, while the remainder is reached by state, county, and Forest Service roads from the San Joaquin Valley.</p>","language":"English","publisher":"U.S. Geological Survey","publisherLocation":"Reston, VA","doi":"10.3133/mf1231D","usgsCitation":"Jachens, R.C., and Elder, W.P., 1983, Map showing aeromagnetic interpretation of the Golden Trout Wilderness, Tulare and Inyo counties, California: U.S. Geological Survey Miscellaneous Field Studies Map 1231, 57.03 x 40.42 inches, https://doi.org/10.3133/mf1231D.","productDescription":"57.03 x 40.42 inches","onlineOnly":"N","additionalOnlineFiles":"N","costCenters":[],"links":[{"id":183645,"rank":0,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/thumbnails/mf1231D.PNG"},{"id":327286,"rank":1,"type":{"id":17,"text":"Plate"},"url":"https://pubs.usgs.gov/mf/1231-D/plate-1.pdf","linkFileType":{"id":1,"text":"pdf"}}],"scale":"0","country":"United States","state":"California","county":"Inyo County, Tulare County","otherGeospatial":"Golden Trout Wilderness","geographicExtents":"{ \"type\": \"FeatureCollection\", \"features\": [ { \"type\": \"Feature\", \"properties\": {}, \"geometry\": { \"type\": \"Polygon\", \"coordinates\": [ [ [ -118.75,36.083333333333336 ], [ -118.75,36.5 ], [ -118,36.5 ], [ -118,36.083333333333336 ], [ -118.75,36.083333333333336 ] ] ] } } ] }","noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"4f4e4a94e4b07f02db658e59","contributors":{"authors":[{"text":"Jachens, Robert C. jachens@usgs.gov","contributorId":1180,"corporation":false,"usgs":true,"family":"Jachens","given":"Robert","email":"jachens@usgs.gov","middleInitial":"C.","affiliations":[{"id":312,"text":"Geology, Minerals, Energy, and Geophysics Science Center","active":true,"usgs":true}],"preferred":true,"id":262634,"contributorType":{"id":1,"text":"Authors"},"rank":1},{"text":"Elder, William P.","contributorId":61058,"corporation":false,"usgs":true,"family":"Elder","given":"William","email":"","middleInitial":"P.","affiliations":[],"preferred":false,"id":262635,"contributorType":{"id":1,"text":"Authors"},"rank":2}]}}
,{"id":58338,"text":"mf1548 - 1983 - Biostratigraphic correlation chart of some Upper Cretaceous rocks from the Lost Soldier area, Wyoming to west of Craig, Colorado","interactions":[],"lastModifiedDate":"2018-03-26T15:24:45","indexId":"mf1548","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":"1548","title":"Biostratigraphic correlation chart of some Upper Cretaceous rocks from the Lost Soldier area, Wyoming to west of Craig, Colorado","docAbstract":"<p>This chart depicts the time-stratigraphic relations of some Upper Cretaceous rocks along the eastern and southeastern margins of the Greater Green River Basin, south-central Wyoming and northwestern Colorado. The purpose of this report is to release a preferred set of correlations based upon marine mollusk biostratigraphy. The senior author, with the help of B. E. Law, has acquired, synthesized, compiled, and interpreted data from various sources. These include selected published documents (see \"References Cited\") and unpublished reports of fossil identifications by W. A. Cobban who examined collections made by the late J. R. Gill. Numerous measured sections of Gill's were also utilized. It must be emphasized that all interpretations on this chart are based on information obtained from these sources and the senior author has yet to substantiate these correlations in the field. Not all data from the area of this study is included herein because it is either repetitive in nature or its reliability is uncertain. This uncertainty is due to the ambiguity inherent in both fossil identification and stratigraphic interpretation. Questionable unpublished material has been omitted while published data which is inconsistent with the senior author's correlations may be found in the footnotes portion of this report. The rock units are assigned to a range of ammonites that have been related to an absolute time scale. The ammonite zonation and age boundaries are adapted from Obradovich and Cobban (1975). \"D\" numbers are provided for each geographic locality where fossils were collected and described by personnel of the U.S. Geological Survey. These fossils may be accessed at the offices of the Survey in Lakewood, Colorado.</p>","language":"English","publisher":"U.S. Geological Survey","publisherLocation":"Reston, VA","doi":"10.3133/mf1548","isbn":"0607812788","usgsCitation":"Bader, J., Gill, J.R., Cobban, W.A., and Law, B.E., 1983, Biostratigraphic correlation chart of some Upper Cretaceous rocks from the Lost Soldier area, Wyoming to west of Craig, Colorado: U.S. Geological Survey Miscellaneous Field Studies Map 1548, Plate: 50.26 x 37.13 inches, https://doi.org/10.3133/mf1548.","productDescription":"Plate: 50.26 x 37.13 inches","onlineOnly":"N","additionalOnlineFiles":"N","costCenters":[],"links":[{"id":326970,"rank":1,"type":{"id":17,"text":"Plate"},"url":"https://pubs.usgs.gov/mf/1548/plate-1.pdf"},{"id":326972,"rank":2,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/thumbnails/mf1548.JPG"}],"scale":"1","country":"United States","state":"Colorado, Wyoming","otherGeospatial":"Lost Soldier area","geographicExtents":"{ \"type\": \"FeatureCollection\", \"features\": [ { \"type\": \"Feature\", \"properties\": {}, \"geometry\": { \"type\": \"Polygon\", \"coordinates\": [ [ [ -108.25,40 ], [ -108.25,42.5 ], [ -106.8,42.5 ], [ -106.8,40 ], [ -108.25,40 ] ] ] } } ] }","noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"4f4e4a48e4b07f02db622ff1","contributors":{"authors":[{"text":"Bader, J.W.","contributorId":68281,"corporation":false,"usgs":true,"family":"Bader","given":"J.W.","email":"","affiliations":[],"preferred":false,"id":258786,"contributorType":{"id":1,"text":"Authors"},"rank":1},{"text":"Gill, J. R.","contributorId":8125,"corporation":false,"usgs":true,"family":"Gill","given":"J.","email":"","middleInitial":"R.","affiliations":[],"preferred":false,"id":258783,"contributorType":{"id":1,"text":"Authors"},"rank":2},{"text":"Cobban, W. A.","contributorId":21577,"corporation":false,"usgs":true,"family":"Cobban","given":"W.","email":"","middleInitial":"A.","affiliations":[],"preferred":false,"id":258785,"contributorType":{"id":1,"text":"Authors"},"rank":3},{"text":"Law, B. E.","contributorId":17586,"corporation":false,"usgs":true,"family":"Law","given":"B.","email":"","middleInitial":"E.","affiliations":[],"preferred":false,"id":258784,"contributorType":{"id":1,"text":"Authors"},"rank":4}]}}
,{"id":59340,"text":"mf1577D - 1983 - Aeromagnetic map of the Arnold Mesa Roadless Area, Yavapai County, Arizona","interactions":[],"lastModifiedDate":"2016-08-22T10:15:54","indexId":"mf1577D","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":"1577","chapter":"D","title":"Aeromagnetic map of the Arnold Mesa Roadless Area, Yavapai County, Arizona","docAbstract":"<p><span>The Wilderness Act (Public Law 88-577, September 3, 1964) and related acts require the U.S. Geological Survey and the U.S. Bureau of Mines to survey certain areas on Federal lands to determine their mineral resource potential. Results must be made available to the public and be submitted to the President&nbsp;and the Congress. This report presents the results of an aeromagnetic survey of the&nbsp;Arnold Mesa Roadless Area (U.S. Forest Service number 03092) in the Prescott and Tonto National Forests,&nbsp;Yavapai County, Arizona. The&nbsp;Arnold Mesa Roadless Area was classified&nbsp;as a further planning area during the Second Roadless Area Review and Evaluation (RARE II) by the U.S. Forest Service, January 1979.</span></p>\n<p><span>The&nbsp;Arnold Mesa Roadless Area is within the transition zone between the Colorado Plateaus to the northeast and the Basin and Range province to the southwest. The transition zone is a belt about 701 miles (120 km) wide that extends diagonally from northwest to south east across central Arizona and parallels the topographic margin of the plateaus. The study area is underlain by Precambrian rocks and gently dipping Paleozoic strata that are largely covered by basaltic lavas and pyroclastic deposits of Miocene age ( McKee and Anderson, 1971). Dacite breccia and tuff are locally interbedded with the basaltic rocks. Sedimentary deposits of late Cenozoic age are dominant in the Verde Valley from about Chasm Creek north; they accumulated in a depositional basin bounded on the west by the Verde fault.</span></p>","language":"English","publisher":"U.S. Geological Survey","doi":"10.3133/mf1577D","usgsCitation":"Davis, W., and Wolfe, E.W., 1983, Aeromagnetic map of the Arnold Mesa Roadless Area, Yavapai County, Arizona: U.S. Geological Survey Miscellaneous Field Studies Map 1577, 49.43 x 35.85 inches, https://doi.org/10.3133/mf1577D.","productDescription":"49.43 x 35.85 inches","onlineOnly":"N","additionalOnlineFiles":"N","costCenters":[],"links":[{"id":183834,"rank":0,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/thumbnails/MF1577D.PNG"},{"id":327199,"rank":1,"type":{"id":17,"text":"Plate"},"url":"https://pubs.usgs.gov/mf/1577-D/plate-1.pdf","linkFileType":{"id":1,"text":"pdf"}}],"scale":"24000","country":"United States","state":"Arizona","county":"Yavapai County","otherGeospatial":"Arnold Mesa Roadless Area, Prescott National Forest, Tonto National Forest","geographicExtents":"{\n  \"type\": \"FeatureCollection\",\n  \"features\": [\n    {\n      \"type\": \"Feature\",\n      \"properties\": {},\n      \"geometry\": {\n        \"type\": \"Polygon\",\n        \"coordinates\": [\n          [\n            [\n              -112,\n              34.5\n            ],\n            [\n              -112,\n              34.2\n            ],\n            [\n              -111.6,\n              34.2\n            ],\n            [\n              -111.6,\n              34.5\n            ],\n            [\n              -112,\n              34.5\n            ]\n          ]\n        ]\n      }\n    }\n  ]\n}","noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"4f4e4afee4b07f02db6972f1","contributors":{"authors":[{"text":"Davis, Willard E.","contributorId":8549,"corporation":false,"usgs":true,"family":"Davis","given":"Willard E.","affiliations":[],"preferred":false,"id":261818,"contributorType":{"id":1,"text":"Authors"},"rank":1},{"text":"Wolfe, Edward W.","contributorId":79878,"corporation":false,"usgs":true,"family":"Wolfe","given":"Edward","email":"","middleInitial":"W.","affiliations":[],"preferred":false,"id":261817,"contributorType":{"id":1,"text":"Authors"},"rank":2}]}}
,{"id":61069,"text":"mf1495B - 1983 - Reconnaissance geologic map of the Selway-Bitterroot Wilderness, Idaho County, Idaho, and Missoula and Ravalli counties, Montana","interactions":[],"lastModifiedDate":"2025-09-24T17:41:14.495224","indexId":"mf1495B","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":"1495","chapter":"B","title":"Reconnaissance geologic map of the Selway-Bitterroot Wilderness, Idaho County, Idaho, and Missoula and Ravalli counties, Montana","docAbstract":"<p>The Selway-Bitterroot Wilderness covers about 1.25 million acres in east-central Idaho and western Montana (fig. 1). The wilderness lies across the Bitterroot Range, which forms the boundary between Idaho and Montana, and includes large portions of the drainages of the Selway, Lochsa, and Bitterroot Rivers. Elevations range from 1,800 ft on the Selway River near the wilderness boundary to 10,157 ft at Trapper Peak in the Bitterroot Mountains. Cities within 50 min of the wilderness include Missoula, Hamilton, and Salmon on the east, and Orofino and Grangeville on the west. Access to trailheads near the edge of the wilderness is limited to dirt roads.&nbsp;</p>","language":"English","publisher":"U.S. Geological Survey","publisherLocation":"Reston, VA","doi":"10.3133/mf1495B","usgsCitation":"Toth, M.I., 1983, Reconnaissance geologic map of the Selway-Bitterroot Wilderness, Idaho County, Idaho, and Missoula and Ravalli counties, Montana: U.S. Geological Survey Miscellaneous Field Studies Map 1495, 1 Plate: 39.49 x 57.80 inches, https://doi.org/10.3133/mf1495B.","productDescription":"1 Plate: 39.49 x 57.80 inches","onlineOnly":"N","additionalOnlineFiles":"N","costCenters":[],"links":[{"id":179812,"rank":1,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/thumbnails/mf1495B.PNG"},{"id":327544,"rank":2,"type":{"id":17,"text":"Plate"},"url":"https://pubs.usgs.gov/mf/1495-B/plate-1.pdf","linkFileType":{"id":1,"text":"pdf"}},{"id":496038,"rank":3,"type":{"id":36,"text":"NGMDB Index 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,{"id":60611,"text":"mf1322B - 1983 - Aeromagnetic and gravity maps of the Freel and Dardanelles Roadless Areas, Alpine and El Dorado counties, California","interactions":[],"lastModifiedDate":"2016-08-23T08:59:44","indexId":"mf1322B","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":"1322","chapter":"B","title":"Aeromagnetic and gravity maps of the Freel and Dardanelles Roadless Areas, Alpine and El Dorado counties, California","docAbstract":"<p>The Freel and Dardanelles Roadless Areas comprise 51 mi<sup>2</sup> (132 km<sup>2</sup>) in the central Sierra Nevada south of Lake Tahoe. &nbsp;The Sierra Nevada crest passes through the eastern part of the area. &nbsp;Prominent mountains include Stevens Peak (elev 10,061 ft), Waterhouse Peak (elev 9,497 ft), and Freel Peak (elev 10,881 ft).</p>","language":"English","publisher":"U.S. Geological Survey","publisherLocation":"Reston, VA","doi":"10.3133/mf1322B","usgsCitation":"Plouff, D., 1983, Aeromagnetic and gravity maps of the Freel and Dardanelles Roadless Areas, Alpine and El Dorado counties, California: U.S. Geological Survey Miscellaneous Field Studies Map 1322, 41.79 x 23.48 inches, https://doi.org/10.3133/mf1322B.","productDescription":"41.79 x 23.48 inches","onlineOnly":"N","additionalOnlineFiles":"N","costCenters":[],"links":[{"id":183043,"rank":0,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/thumbnails/mf1322B.PNG"},{"id":327422,"rank":1,"type":{"id":17,"text":"Plate"},"url":"https://pubs.usgs.gov/mf/1322-B/plate-1.pdf","linkFileType":{"id":1,"text":"pdf"}}],"scale":"0","country":"United States","state":"California","county":"Alpine County, El Dorado County","otherGeospatial":"Freel and Dardaneel Roadless Areas","geographicExtents":"{ \"type\": \"FeatureCollection\", \"features\": [ { \"type\": \"Feature\", \"properties\": {}, \"geometry\": { \"type\": \"Polygon\", \"coordinates\": [ [ [ -120.16666666666667,38.666666666666664 ], [ -120.16666666666667,38.916666666666664 ], [ -119.83333333333333,38.916666666666664 ], [ -119.83333333333333,38.666666666666664 ], [ -120.16666666666667,38.666666666666664 ] ] ] } } ] }","noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"4f4e4b01e4b07f02db6984c8","contributors":{"authors":[{"text":"Plouff, Donald","contributorId":94657,"corporation":false,"usgs":true,"family":"Plouff","given":"Donald","email":"","affiliations":[],"preferred":false,"id":264077,"contributorType":{"id":1,"text":"Authors"},"rank":1}]}}
,{"id":60038,"text":"mf1358D - 1983 - Mineral resource potential map of the Dolly Ann Roadless Area, Alleghany County, Virginia","interactions":[],"lastModifiedDate":"2015-09-24T13:01:31","indexId":"mf1358D","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":"1358","chapter":"D","title":"Mineral resource potential map of the Dolly Ann Roadless Area, Alleghany County, Virginia","docAbstract":"<p>The Dolly Ann Roadless Area comprises 7,900 acres (3,200 ha) in the George Washington National Forest in the Valley and Ridge physiographic province of west-central Virginia. The area is at the southern &middot;end of Warm Springs Mountain in Alleghany County just northeast of Covington, the county seat (index map). U.S. Highway 220 forms part of the western boundary, and U.S. Forest Service Road 125, which parallels Pounding Mill Creek, forms the eastern boundary. The principal streams draining the area are Pounding Mill Creek, Dry Run, and Roaring Run, all tributaries of the Jackson River. The highest point in the area is Big Knob at the north end, 4,072 ft (1241 m) above sea level; the lowest points, about 1,400 ft (427 m) above sea level, are at the south side, along Dry Run and Pounding Mill Creek. In general, the hill slopes are steep and heavily wooded with second- or third-growth hardwoods and scattered pine and hemlock. Dolly Ann Hollow near the east end of the area is a steep, boulder-strewn gorge, quite picturesque, but containing no good trails. A good trail up Dry Run connects a trail crossing the ridge between Bald Knob and Big Knob. No other trails cross the area.</p>","largerWorkType":{"id":18,"text":"Report"},"largerWorkSubtype":{"id":5,"text":"USGS Numbered Series"},"language":"English","publisher":"U.S. Geological Survey","doi":"10.3133/mf1358D","usgsCitation":"Lesure, F.G., and Jones, J.G., 1983, Mineral resource potential map of the Dolly Ann Roadless Area, Alleghany County, Virginia: U.S. Geological Survey Miscellaneous Field Studies Map 1358, Report: 14 p.; 1 Plate: 37.55 x 33.60 inches, https://doi.org/10.3133/mf1358D.","productDescription":"Report: 14 p.; 1 Plate: 37.55 x 33.60 inches","numberOfPages":"14","onlineOnly":"N","additionalOnlineFiles":"N","costCenters":[],"links":[{"id":180429,"rank":0,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/thumbnails/MF1358D.jpg"},{"id":308517,"rank":1,"type":{"id":11,"text":"Document"},"url":"https://pubs.usgs.gov/mf/1358-D/report.pdf","text":"Report","size":"8 MB","linkFileType":{"id":1,"text":"pdf"}},{"id":308518,"rank":2,"type":{"id":17,"text":"Plate"},"url":"https://pubs.usgs.gov/mf/1358-D/plate-1.pdf","text":"Plate 1","size":"23 MB","linkFileType":{"id":1,"text":"pdf"}}],"country":"United States","state":"Virginia","county":"Alleghany County","otherGeospatial":"Dolly Ann Roadless Area","geographicExtents":"{ \"type\": \"FeatureCollection\", \"features\": [ { \"type\": \"Feature\", \"properties\": {}, \"geometry\": { \"type\": \"Polygon\", \"coordinates\": [ [ [ -80,37.75 ], [ -80,37.8675 ], [ -79.86749999999999,37.8675 ], [ -79.86749999999999,37.75 ], [ -80,37.75 ] ] ] } } ] }","noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"4f4e4b1be4b07f02db6a8d62","contributors":{"authors":[{"text":"Lesure, Frank G.","contributorId":20068,"corporation":false,"usgs":true,"family":"Lesure","given":"Frank","email":"","middleInitial":"G.","affiliations":[],"preferred":false,"id":263031,"contributorType":{"id":1,"text":"Authors"},"rank":1},{"text":"Jones, Jay G.","contributorId":45334,"corporation":false,"usgs":true,"family":"Jones","given":"Jay","email":"","middleInitial":"G.","affiliations":[],"preferred":false,"id":263032,"contributorType":{"id":1,"text":"Authors"},"rank":2}]}}
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