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M.","contributorId":76714,"corporation":false,"usgs":true,"family":"Batson","given":"R.","email":"","middleInitial":"M.","affiliations":[],"preferred":false,"id":272779,"contributorType":{"id":1,"text":"Authors"},"rank":1}]}} ,{"id":61354,"text":"mf2111 - 1990 - High-resolution seismic stratigraphy of the upper continental rise seaward of Georges Bank","interactions":[],"lastModifiedDate":"2025-05-29T20:37:36.063036","indexId":"mf2111","displayToPublicDate":"1994-01-01T00:00:00","publicationYear":"1990","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":"2111","title":"High-resolution seismic stratigraphy of the upper continental rise seaward of Georges Bank","docAbstract":"No abstract available.
","language":"English","publisher":"U.S. Geological Survey","doi":"10.3133/mf2111","usgsCitation":"Danforth, W.W., and Schwab, W.C., 1990, High-resolution seismic stratigraphy of the upper continental rise seaward of Georges Bank: U.S. Geological Survey Miscellaneous Field Studies Map 2111, Reports: 10 p.; 11 Plates: 54.50 × 36.50 inches or smaller, https://doi.org/10.3133/mf2111.","productDescription":"Reports: 10 p.; 11 Plates: 54.50 × 36.50 inches or smaller","costCenters":[],"links":[{"id":88948,"rank":6,"type":{"id":17,"text":"Plate"},"url":"https://pubs.usgs.gov/mf/1990/2111/plate-03.pdf","linkFileType":{"id":1,"text":"pdf"}},{"id":88956,"rank":14,"type":{"id":17,"text":"Plate"},"url":"https://pubs.usgs.gov/mf/1990/2111/plate-11.pdf","linkFileType":{"id":1,"text":"pdf"}},{"id":88955,"rank":13,"type":{"id":17,"text":"Plate"},"url":"https://pubs.usgs.gov/mf/1990/2111/plate-10.pdf","linkFileType":{"id":1,"text":"pdf"}},{"id":88954,"rank":12,"type":{"id":17,"text":"Plate"},"url":"https://pubs.usgs.gov/mf/1990/2111/plate-09.pdf","linkFileType":{"id":1,"text":"pdf"}},{"id":88953,"rank":11,"type":{"id":17,"text":"Plate"},"url":"https://pubs.usgs.gov/mf/1990/2111/plate-08.pdf","linkFileType":{"id":1,"text":"pdf"}},{"id":88952,"rank":10,"type":{"id":17,"text":"Plate"},"url":"https://pubs.usgs.gov/mf/1990/2111/plate-07.pdf","linkFileType":{"id":1,"text":"pdf"}},{"id":88949,"rank":7,"type":{"id":17,"text":"Plate"},"url":"https://pubs.usgs.gov/mf/1990/2111/plate-04.pdf","linkFileType":{"id":1,"text":"pdf"}},{"id":409130,"rank":2,"type":{"id":36,"text":"NGMDB Index Page"},"url":"https://ngmdb.usgs.gov/Prodesc/proddesc_5711.htm","linkFileType":{"id":5,"text":"html"}},{"id":180620,"rank":1,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/mf/1990/2111/report-thumb.jpg"},{"id":88957,"rank":3,"type":{"id":11,"text":"Document"},"url":"https://pubs.usgs.gov/mf/1990/2111/report.pdf","linkFileType":{"id":1,"text":"pdf"}},{"id":88950,"rank":8,"type":{"id":17,"text":"Plate"},"url":"https://pubs.usgs.gov/mf/1990/2111/plate-05.pdf","linkFileType":{"id":1,"text":"pdf"}},{"id":88951,"rank":9,"type":{"id":17,"text":"Plate"},"url":"https://pubs.usgs.gov/mf/1990/2111/plate-06.pdf","linkFileType":{"id":1,"text":"pdf"}},{"id":88947,"rank":5,"type":{"id":17,"text":"Plate"},"url":"https://pubs.usgs.gov/mf/1990/2111/plate-02.pdf","linkFileType":{"id":1,"text":"pdf"}},{"id":88946,"rank":4,"type":{"id":17,"text":"Plate"},"url":"https://pubs.usgs.gov/mf/1990/2111/plate-01.pdf","linkFileType":{"id":1,"text":"pdf"}}],"scale":"147000","country":"United States","otherGeospatial":"Georges Bank","geographicExtents":"{\n \"type\": \"FeatureCollection\",\n \"features\": [\n {\n \"type\": \"Feature\",\n \"properties\": {},\n \"geometry\": {\n \"type\": \"Polygon\",\n \"coordinates\": [\n [\n [\n -71,\n 39.4167\n ],\n [\n -71,\n 41\n ],\n [\n -66,\n 41\n ],\n [\n -66,\n 39.4167\n ],\n [\n -71,\n 39.4167\n ]\n ]\n ]\n }\n }\n ]\n}","noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"4f4e4ae1e4b07f02db68880a","contributors":{"authors":[{"text":"Danforth, W. W.","contributorId":16386,"corporation":false,"usgs":true,"family":"Danforth","given":"W.","email":"","middleInitial":"W.","affiliations":[],"preferred":false,"id":265495,"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":265496,"contributorType":{"id":1,"text":"Authors"},"rank":2}]}} ,{"id":29818,"text":"wri894187 - 1990 - Automatic tracer-dilution method used for stage-discharge ratings and streamflow hydrographs on small Iowa streams","interactions":[],"lastModifiedDate":"2016-03-09T13:58:11","indexId":"wri894187","displayToPublicDate":"1994-01-01T00:00:00","publicationYear":"1990","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":"89-4187","title":"Automatic tracer-dilution method used for stage-discharge ratings and streamflow hydrographs on small Iowa streams","docAbstract":"An automatic system was designed to concurrently measure stage and discharge for the purpose of developing stage-discharge ratings and high flow hydrographs on small streams. Stage, or gage height, is recorded by an analog-to-digital recorder and discharge is determined by the constant-rate tracer-dilution method The system measures flow above a base stage set by the user. To test the effectiveness of the system and its components, eight systems, with a variety of equipment, were installed at crest-stage gaging stations across Iowa A fluorescent dye, rhodamine-WT, was used as the tracer.
\nTracer-dilution discharge measurements were made during 14 flow periods at six stations from 1986 through 1988 water years. Ratings were developed at three stations with the aid of these measurements. A loop rating was identified at one station during rapidly-changing flow conditions. Incomplete mixing and dye loss to sediment apparently were problems at some stations. Stage hydrographs were recorded for 38 flows at seven stations. Limited data on background fluorescence during high flows were also obtained.
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These data, accumulated during many water years, constitute a valuable data base for developing an improved understanding of the water resources of the State. To make these data readily available to interested parties outside the Geological Survey, the data are published annually in this report series entitled \"Water Resources Data for Arizona.\"
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B.","contributorId":23963,"corporation":false,"usgs":true,"family":"Garrett","given":"W.","email":"","middleInitial":"B.","affiliations":[],"preferred":false,"id":257729,"contributorType":{"id":1,"text":"Authors"},"rank":3},{"text":"Konieczki, A.D.","contributorId":28218,"corporation":false,"usgs":true,"family":"Konieczki","given":"A.D.","affiliations":[],"preferred":false,"id":257730,"contributorType":{"id":1,"text":"Authors"},"rank":4}]}} ,{"id":41416,"text":"ofr90312 - 1990 - Preliminary geologic map of the Dooley Mountain quadrangle, Baker County, Oregon","interactions":[],"lastModifiedDate":"2012-02-02T00:10:34","indexId":"ofr90312","displayToPublicDate":"1994-01-01T00:00:00","publicationYear":"1990","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":"90-312","title":"Preliminary geologic map of the Dooley Mountain quadrangle, Baker County, Oregon","language":"ENGLISH","doi":"10.3133/ofr90312","usgsCitation":"Evans, J.G., 1990, Preliminary geologic map of the Dooley Mountain quadrangle, Baker County, Oregon: U.S. Geological Survey Open-File Report 90-312, 1 map :photocopy ;58 x 41 cm., on sheet 153 x 107 cm., https://doi.org/10.3133/ofr90312.","productDescription":"1 map :photocopy ;58 x 41 cm., on sheet 153 x 107 cm.","costCenters":[],"links":[{"id":108835,"rank":700,"type":{"id":15,"text":"Index Page"},"url":"https://ngmdb.usgs.gov/Prodesc/proddesc_17906.htm","linkFileType":{"id":5,"text":"html"},"description":"17906"},{"id":173809,"rank":0,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/thumbnails/usgs_thumb.jpg"},{"id":21379,"rank":400,"type":{"id":17,"text":"Plate"},"url":"https://pubs.usgs.gov/of/1990/0312/plate-1.pdf","linkFileType":{"id":1,"text":"pdf"}},{"id":21380,"rank":401,"type":{"id":17,"text":"Plate"},"url":"https://pubs.usgs.gov/of/1990/0312/plate-1-preview.pdf","linkFileType":{"id":1,"text":"pdf"}}],"noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"4f4e4ac8e4b07f02db67b9d9","contributors":{"authors":[{"text":"Evans, James George","contributorId":73578,"corporation":false,"usgs":true,"family":"Evans","given":"James","email":"","middleInitial":"George","affiliations":[],"preferred":false,"id":224982,"contributorType":{"id":1,"text":"Authors"},"rank":1}]}} ,{"id":65052,"text":"i2021 - 1990 - Geologic map and distribution of heavy minerals in Tertiary and uppermost Cretaceous rocks of the Recluse 30' x 60' Quadrangle, Campbell and Crook counties, Wyoming","interactions":[],"lastModifiedDate":"2012-02-10T00:11:08","indexId":"i2021","displayToPublicDate":"1994-01-01T00:00:00","publicationYear":"1990","noYear":false,"publicationType":{"id":18,"text":"Report"},"publicationSubtype":{"id":5,"text":"USGS Numbered Series"},"seriesTitle":{"id":320,"text":"IMAP","code":"I","active":false,"publicationSubtype":{"id":5}},"seriesNumber":"2021","subseriesTitle":"NONE","title":"Geologic map and distribution of heavy minerals in Tertiary and uppermost Cretaceous rocks of the Recluse 30' x 60' Quadrangle, Campbell and Crook counties, Wyoming","language":"ENGLISH","doi":"10.3133/i2021","usgsCitation":"Macke, D., and Schumann, R., 1990, Geologic map and distribution of heavy minerals in Tertiary and uppermost Cretaceous rocks of the Recluse 30' x 60' Quadrangle, Campbell and Crook counties, Wyoming: U.S. Geological Survey IMAP 2021, 1 map :col. ;56 x 80 cm., on sheet 86 x 137 cm., folded in envelope 30 x 24 cm., https://doi.org/10.3133/i2021.","productDescription":"1 map :col. ;56 x 80 cm., on sheet 86 x 137 cm., folded in envelope 30 x 24 cm.","costCenters":[],"links":[{"id":107255,"rank":700,"type":{"id":15,"text":"Index Page"},"url":"https://ngmdb.usgs.gov/Prodesc/proddesc_10087.htm","linkFileType":{"id":5,"text":"html"},"description":"10087"},{"id":188967,"rank":0,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/thumbnails/usgs_thumb.jpg"}],"scale":"100000","geographicExtents":"{ \"type\": \"FeatureCollection\", \"features\": [ { \"type\": \"Feature\", \"properties\": {}, \"geometry\": { \"type\": \"Polygon\", \"coordinates\": [ [ [ -106,44.5 ], [ -106,45 ], [ -105,45 ], [ -105,44.5 ], [ -106,44.5 ] ] ] } } ] }","noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"4f4e4b15e4b07f02db6a4990","contributors":{"authors":[{"text":"Macke, D. L.","contributorId":101643,"corporation":false,"usgs":true,"family":"Macke","given":"D. L.","affiliations":[],"preferred":false,"id":272595,"contributorType":{"id":1,"text":"Authors"},"rank":1},{"text":"Schumann, R.R.","contributorId":14429,"corporation":false,"usgs":true,"family":"Schumann","given":"R.R.","email":"","affiliations":[],"preferred":false,"id":272594,"contributorType":{"id":1,"text":"Authors"},"rank":2}]}} ,{"id":68682,"text":"ha720E - 1990 - Hydrogeology of the Cliff House Sandstone in the San Juan structural basin, New Mexico, Colorado, Arizona, and Utah","interactions":[],"lastModifiedDate":"2022-02-03T19:38:10.681088","indexId":"ha720E","displayToPublicDate":"1994-01-01T00:00:00","publicationYear":"1990","noYear":false,"publicationType":{"id":18,"text":"Report"},"publicationSubtype":{"id":5,"text":"USGS Numbered Series"},"seriesTitle":{"id":318,"text":"Hydrologic Atlas","code":"HA","active":false,"publicationSubtype":{"id":5}},"seriesNumber":"720","chapter":"E","title":"Hydrogeology of the Cliff House Sandstone in the San Juan structural basin, New Mexico, Colorado, Arizona, and Utah","docAbstract":"This report is one in a series resulting from the U.S. Geological Survey's Regional Aquifer-System Analysis (RASA) study of the San Juan structural basin that began in October 1984. Previous reports in the series describe the hydrogeology of the Dakota Sandstone (Craigg and others, 1989), Point Lookout Sandstone (Craigg and others, 1990), Morrison Formation (Dam and others, 1990), Gallup Sandstone (Kernodle and others, 1989), and Menefee Formation (Levings and others, 1990) in the San Juan structural basin. The purposes of the RASA (Welder, 1986) are to: (1) Define and evaluate the aquifer system; (2) assess the effects of past, present, and potential ground-water use on aquifers and streams; and (3) determine the availability and quality of ground water.
This report summarizes information on the geology and the occurrence and quality of water in the Cliff House Sandstone, one of the primary water-bearing units in the regional aquifer system. Data used in this report were collected during the study or were derived from existing records in the U.S. Geological Survey's computerized National Water Information System (NWIS) data base, the Petroleum Information Corporation's data base, and the Dwight's ENERGYDATA Inc. BRIN data base. Although all data available for the Cliff House Sandstone were considered in formulating the discussions in the text, not all those data could be plotted on the illustrations.
The San Juan structural basin is in New Mexico, Colorado, Arizona, and Utah and has an area of about 21,600 square miles (fig. 1). The structural basin is about 140 miles wide and about 200 miles long. The study area is that part of the structural basin that contains rocks of Triassic or younger age and, therefore, is less extensive than the structural basin. Triassic through Tertiary sedimentary rocks are emphasized in this study because the major aquifers in the basin are present in these rocks. The study area is about 140 miles wide (about the same as the structural basin), 180 miles long, and has an area of about 19,400 square miles.
Altitudes in the study area range from about 4,500 feet in San Juan County, Utah, to about 11,000 feet in Cibola County, New Mexico. Annual precipitation in the high mountainous areas along the north and east margins of the basin is as much as 45 inches, whereas annual precipitation in the lower altitude, central basin is generally less than 8 inches. Mean annual precipitation in the study area is about 12 inches.
Data obtained from documents published by the U.S. Bureau of the Census, 1980 and 1985, were used to estimate the population of the study area. The population of the study area in 1970 was estimated to be about 134,000. The population rose to about 194,000 in 1980, 212,000 in 1982, 221,000 in 1984, and then fell to about 210,000 in 1985. The economy of the basin is supported by exploration and development of petroleum, natural gas, coal, and uranium resources; urban enterprise, farming and ranching; tourism; and recreation. The rise and fall in population were related to changes in the economic strength of the mining, petroleum, and natural-gas industries, and support services. Uranium mining and milling activities grew rapidly until the late 1970's when most uranium-mining activity ended in the study area. Likewise, the oil and gas industry prospered until about 1983 and then declined rapidly, also affecting many jobs in support industries.
Confined-drift aquifers in six aquifer zones identified in a 1,300-square-mile area of west-central Minnesota near Brooten and Belgrade range in thickness from 5 to 110 feet. Transmissivities generally range from 500 to 10,000 feet squared per day, and theoretical well yields generally range from 100 to 900 gallons per minute.
\nRegional ground-water flow in the confined-drift aquifers is to the southeast with local discharge to the East and Middle Branches of the Chippewa River, the North Fork Crow and Sauk Rivers, and to smaller streams, lakes, wetlands, and wells. Water levels near high-capacity pumped wells generally fluctuate 5 to 40 feet annually, compared to annual fluctuations of less than 5 feet in the unconfined aquifer.
\nWater from confined-drift aquifers generally is suitable for most uses. The water is hard to very hard and contains locally elevated concentrations of iron, manganese, and dissolved solids.
\nResults from a ground-water-flow model indicate that increased pumping from confined aquifers in the area would not adversely affect water levels. The addition of 10 to 20 hypothetical wells, pumping 123 to 246 million gallons per year, generally resulted in regional water-level declines of 0.1 to 1.0 feet. Simulations showed that the reduced recharge and increased pumping resulting from a 3-year drought probably would lower water levels between 5 and 10 feet regionally in the confined-drift aquifers and as much as 20 feet locally in the unconfined aquifer. Ground-water discharge to the East Branch Chippewa and North Fork Crow Rivers during the simulated drought would be reduced by 38 percent of 1984 conditions.
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","language":"English","publisher":"U.S. Geological Survey","doi":"10.3133/ofr90415","usgsCitation":"Pierce, K.L., and Morgan, L.A., 1990, The track of the Yellowstone hotspot: Volcanism, faulting, and uplift: U.S. Geological Survey Open-File Report 90-415, i, 70 p., https://doi.org/10.3133/ofr90415.","productDescription":"i, 70 p.","costCenters":[],"links":[{"id":393456,"rank":3,"type":{"id":36,"text":"NGMDB Index Page"},"url":"https://ngmdb.usgs.gov/Prodesc/proddesc_17928.htm"},{"id":50001,"rank":300,"type":{"id":11,"text":"Document"},"url":"https://pubs.usgs.gov/of/1990/0415/report.pdf","linkFileType":{"id":1,"text":"pdf"}},{"id":153321,"rank":0,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/of/1990/0415/report-thumb.jpg"}],"country":"United States","state":"Idaho, Montana, Wyoming","otherGeospatial":"Yellowstone hotspot","geographicExtents":"{\n \"type\": \"FeatureCollection\",\n \"features\": [\n {\n \"type\": \"Feature\",\n \"properties\": {},\n \"geometry\": {\n \"type\": \"Polygon\",\n \"coordinates\": [\n [\n [\n -113.75244140624999,\n 42.16340342422401\n ],\n [\n -108.30322265624999,\n 42.16340342422401\n ],\n [\n -108.30322265624999,\n 46.649436163350245\n ],\n [\n -113.75244140624999,\n 46.649436163350245\n ],\n [\n -113.75244140624999,\n 42.16340342422401\n ]\n ]\n ]\n }\n }\n ]\n}","noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"4f4e4a60e4b07f02db634ba3","contributors":{"authors":[{"text":"Pierce, K. L.","contributorId":12404,"corporation":false,"usgs":true,"family":"Pierce","given":"K.","email":"","middleInitial":"L.","affiliations":[],"preferred":false,"id":182692,"contributorType":{"id":1,"text":"Authors"},"rank":1},{"text":"Morgan, L. A.","contributorId":16350,"corporation":false,"usgs":true,"family":"Morgan","given":"L.","email":"","middleInitial":"A.","affiliations":[],"preferred":false,"id":182693,"contributorType":{"id":1,"text":"Authors"},"rank":2}]}} ,{"id":68463,"text":"ha714 - 1990 - Hydrologic characteristics of soils in the High Plains, northern Great Plains, and Central Texas Carbonates Regional Aquifer Systems","interactions":[],"lastModifiedDate":"2017-09-20T16:41:29","indexId":"ha714","displayToPublicDate":"1994-01-01T00:00:00","publicationYear":"1990","noYear":false,"publicationType":{"id":18,"text":"Report"},"publicationSubtype":{"id":5,"text":"USGS Numbered Series"},"seriesTitle":{"id":318,"text":"Hydrologic Atlas","code":"HA","active":false,"publicationSubtype":{"id":5}},"seriesNumber":"714","title":"Hydrologic characteristics of soils in the High Plains, northern Great Plains, and Central Texas Carbonates Regional Aquifer Systems","docAbstract":"Certain physical characteristics of soils, including permeability, available water capacity, thickness, and topographic position, have a measurable effect on the hydrology of an area. These characteristics control the rate at which precipitation infiltrates or is transmitted through the soil, and thus they have an important role in determining the rates of actual evapotranspiration (consumptive water use), groundwater recharge, and surface runoff. In studies of groundwater hydrology, it is useful to differentiate soils spatially according to their physical characteristics and to assign values that indicate their hydrologic responses.
The principal purpose of this report is to describe the relation between the hydrologic characteristics of the soils in the study area and those environmental factors that affect the development and distribution of the soils. This objective will be achieved by (1) defining both qualitatively and quantitatively those soil characteristics that affect hydrology, and (2) classifying and delineating the boundaries of the soils in the study area according to these hydrologic characteristics.
The study area includes the High Plains, Northern Great Plains, the Central Texas Carbonates, and parts of the Central Midwest Regional Aquifer Systems as described by the U.S. Geological Survey Regional Aquifer-System Analysis (RASA) Program (Sun, 1986, p.5and Sun, personal commun., June 1985) and shown in figures 1 through 5. The spatial patterns of the soils classified according to their quantifiable hydrologic characteristics will subsequently serve as an integral component in the analysis of actual evapotranspiration (consumptive water use), consumptive irrigation requirements, and potential ground-water recharge of the study area.
The classification system used to describe the soils in this report is compatible with that of Dugan (1986). Dugan described the same characteristics of soils that are immediately underlain by principal aquifers of Cretaceous or older age in adjacent parts of the Central Midwest Regional Aquifer System. However, map scales and mapping detail are different between this report and the report by Dugan (1986) because of the size of the study area.
No abstract available.
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","language":"English","publisher":"U.S. Geological Survey","doi":"10.3133/ofr88450R","usgsCitation":"Perry, W.J., 1990, A review of the geology and petroleum potential of southwest Montana: U.S. Geological Survey Open-File Report 88-450, 13 p., https://doi.org/10.3133/ofr88450R.","productDescription":"13 p.","costCenters":[],"links":[{"id":406253,"rank":3,"type":{"id":36,"text":"NGMDB Index Page"},"url":"https://ngmdb.usgs.gov/Prodesc/proddesc_17447.htm","linkFileType":{"id":5,"text":"html"}},{"id":49976,"rank":300,"type":{"id":11,"text":"Document"},"url":"https://pubs.usgs.gov/of/1988/0450r/report.pdf","linkFileType":{"id":1,"text":"pdf"}},{"id":152732,"rank":0,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/of/1988/0450r/report-thumb.jpg"}],"country":"United States","state":"Montana","geographicExtents":"{\n \"type\": \"FeatureCollection\",\n \"features\": [\n {\n \"type\": \"Feature\",\n \"properties\": {},\n \"geometry\": {\n \"type\": \"Polygon\",\n \"coordinates\": [\n [\n [\n -112.82,\n 44.525\n ],\n [\n -108.82,\n 44.525\n ],\n [\n -108.82,\n 46.406\n ],\n [\n -112.82,\n 46.406\n ],\n [\n -112.82,\n 44.525\n ]\n ]\n ]\n }\n }\n ]\n}","noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"4f4e4b19e4b07f02db6a7f43","contributors":{"authors":[{"text":"Perry, W. J. Jr.","contributorId":64266,"corporation":false,"usgs":true,"family":"Perry","given":"W.","suffix":"Jr.","email":"","middleInitial":"J.","affiliations":[],"preferred":false,"id":182649,"contributorType":{"id":1,"text":"Authors"},"rank":1}]}} ,{"id":64528,"text":"i1803D - 1990 - Map showing mineral resource assessment for silver, cobalt, and base metals in Proterozoic sedimentary rocks and for iron, chromium, nickel, talc, chlorite, gold, and graphite in Archean crystalline rocks, Dillon 1° x 2° quadrangle, Idaho and Montana","interactions":[],"lastModifiedDate":"2021-09-20T18:46:26.19441","indexId":"i1803D","displayToPublicDate":"1994-01-01T00:00:00","publicationYear":"1990","noYear":false,"publicationType":{"id":18,"text":"Report"},"publicationSubtype":{"id":5,"text":"USGS Numbered Series"},"seriesTitle":{"id":320,"text":"IMAP","code":"I","active":false,"publicationSubtype":{"id":5}},"seriesNumber":"1803","chapter":"D","title":"Map showing mineral resource assessment for silver, cobalt, and base metals in Proterozoic sedimentary rocks and for iron, chromium, nickel, talc, chlorite, gold, and graphite in Archean crystalline rocks, Dillon 1° x 2° quadrangle, Idaho and Montana","docAbstract":"No abstract available.
","language":"English","publisher":"U.S. Geological Survey","doi":"10.3133/i1803D","usgsCitation":"Pearson, R.C., Hanna, W.F., James, H.L., Loen, J., Moll, S.H., Ruppel, E.T., and Trautwein, C., 1990, Map showing mineral resource assessment for silver, cobalt, and base metals in Proterozoic sedimentary rocks and for iron, chromium, nickel, talc, chlorite, gold, and graphite in Archean crystalline rocks, Dillon 1° x 2° quadrangle, Idaho and Montana: U.S. Geological Survey IMAP 1803, 1 Plate: 46.65 × 37.04 inches, https://doi.org/10.3133/i1803D.","productDescription":"1 Plate: 46.65 × 37.04 inches","costCenters":[{"id":222,"text":"Earth Resources Observation and Science (EROS) Center","active":true,"usgs":true}],"links":[{"id":389490,"rank":4,"type":{"id":36,"text":"NGMDB Index Page"},"url":"https://ngmdb.usgs.gov/Prodesc/proddesc_9927.htm"},{"id":255008,"rank":400,"type":{"id":17,"text":"Plate"},"url":"https://pubs.usgs.gov/imap/1803d/plate-1.pdf","linkFileType":{"id":1,"text":"pdf"}},{"id":255010,"rank":0,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/imap/1803d/report-thumb.jpg"},{"id":255009,"rank":300,"type":{"id":11,"text":"Document"},"url":"https://pubs.usgs.gov/imap/1803d/report.pdf","linkFileType":{"id":1,"text":"pdf"}}],"scale":"250000","country":"United States","state":"Idaho, Montana","otherGeospatial":"Dillon 1° x 2° quadrangle","geographicExtents":"{ \"type\": \"FeatureCollection\", \"features\": [ { \"type\": \"Feature\", \"properties\": {}, \"geometry\": { \"type\": \"Polygon\", \"coordinates\": [ [ [ -114,45 ], [ -114,46 ], [ -112,46 ], [ -112,45 ], [ -114,45 ] ] ] } } ] }","noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"4f4e4a75e4b07f02db644a09","contributors":{"authors":[{"text":"Pearson, R. 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