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The aquifer system consists of a single vertically continuous permeable unit updip and of two major permeable zones (the Upper and Lower Floridan aquifers) separated by one of seven middle confining units downdip. Neither the boundaries of the aquifer system or of its component high- and low-permeability zones necessarily conform to either formation boundaries or time-stratigraphic breaks. The rocks that make up the Floridan aquifer system, its upper and lower confining units, and a surficial aquifer have been separated into several chronostratigraphic units. The external and internal geometry of these stratigraphic units is presented on a series of structure contour and isopach maps and by a series of geohydrologic cross sections and a fence diagram. Paleocene through middle Eocene units consist of an updip clastic facies and a downdip carbonate bank facies, that extends progressively farther north and east in progressively younger units. Upper Eocene and Oligocene strata are predominantly carbonate rocks throughout the study area. Miocene and younger strata are mostly clastic rocks. Subsurface data show that some modifications in current stratigraphic nomenclature are necessary. First, the middle Eocene Lake City Limestone cannot be distinguished lithologically or faunally from the overlying middle Eocene Avon Park 'Limestone.' Accordingly, it is proposed that the term Lake City be abandoned and the term Avon Park Formation be applied to the entire middle Eocene carbonate section of peninsular Florida and southeastern Georgia. A reference well section in Levy County, Fla., is proposed for the expanded Avon Park Formation. The Avon Park is called a 'formation' more properly than a 'limestone' because the unit contains rock types other than limestone. Second, like the Avon Park, the lower Eocene Oldsmar and Paleocene Cedar Keys 'Limestones' of peninsular Florida practically everywhere contain rock types other than limestone. It is therefore proposed that these units be referred to more accurately as Oldsmar Formation and Cedar Keys Formation. The uppermost hydrologic unit in the study area is a surficial aquifer that can be divided into (1) a fluvial sand-and-gravel aquifer in southwestern Alabama and westernmost panhandle Florida, (2) limestone and sandy limestone of the Biscayne aquifer in southeastern peninsular Florida, and (3) a thin blanket of terrace and fluvial sands elsewhere. The surficial aquifer is underlain by a thick sequence of fine clastic rocks and low-permeability carbonate rocks, most of which are part of the middle Miocene Hawthorn Formation and all of which form the upper confining unit of the Floridan aquifer system. In places, the upper confining unit has been removed by erosion or is breached by sinkholes. Water in the Floridan aquifer system thus occurs under unconfined, semiconfined, or fully confined conditions, depending upon the presence, thickness, and integrity of the upper confining unit. Within the Floridan aquifer system, seven low permeability zones of subregional extent split the aquifer system in most places into an Upper and Lower Floridan aquifer. The Upper Floridan aquifer, which consists of all or parts of rocks of Oligocene age, late Eocene age, and the upper half of rocks of middle Eocene age, is highly permeable. The middle confining units that underlie the Upper Floridan are mostly of middle Eocene age but may be as young as Oligocene or as old as early Eocene. Where no middle confining unit exists, the entire aquifer system is comprised of permeable rocks and for hydrologic discussions is treated as the Upper Floridan aquifer.&nbsp;</p>","language":"English","publisher":"U.S. Geological Survey","publisherLocation":"Reston, VA","doi":"10.3133/pp1403B","usgsCitation":"Hydrogeologic framework of the Floridan aquifer system in Florida and in parts of Georgia, Alabama, and South Carolina; 1986; PP; 1403-B; Miller, James A.","productDescription":"Report: viii, 91 p.; 34 Plates: 53.53 x 30.58 inches or smaller","numberOfPages":"91","costCenters":[{"id":27821,"text":"Caribbean-Florida Water Science Center","active":true,"usgs":true}],"links":[{"id":420161,"rank":36,"type":{"id":36,"text":"NGMDB Index 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,{"id":26926,"text":"wri854035 - 1986 - Ground-water movement in the upper glacial aquifer in the Manorville area, Town of Brookhaven, Long Island, New York, in November 1983","interactions":[],"lastModifiedDate":"2025-01-10T18:11:44.126218","indexId":"wri854035","displayToPublicDate":"1986-01-01T00:00:00","publicationYear":"1986","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":"85-4035","title":"Ground-water movement in the upper glacial aquifer in the Manorville area, Town of Brookhaven, Long Island, New York, in November 1983","docAbstract":"<p>Water levels in 52 wells near the Manorville scavenger-waste disposal facility in the Town of Brookhaven were measured in November 1983 to determine the direction and gradients of groundwater flow in the upper glacial aquifer. Groundwater moves south-southeastward (S22 degrees E) from the groundwater divide, about 6 miles north of the facility, to discharge points near East Moriches and beneath Moriches Bay. The hydraulic gradient beneath the disposal facility is 6.5 ft/mi (0.0012 foot/foot), and the rate of horizontal flow is 0.9 to 1.7 ft/day. Vertical movement of groundwater since closure of the disposal facility in 1982 is probably negligible because the vertical gradients are small and the upper glacial aquifer is anisotropic. During operation of the facility, however, groundwater mounding may have developed beneath the unlined settling basins, which could have induced downward movement of water in the upper glacial aquifer.&nbsp;</p>","language":"English","publisher":"U.S. Geological Survey","doi":"10.3133/wri854035","usgsCitation":"Eckhardt, D., and Wexler, E.J., 1986, Ground-water movement in the upper glacial aquifer in the Manorville area, Town of Brookhaven, Long Island, New York, in November 1983: U.S. Geological Survey Water-Resources Investigations Report 85-4035, Report: iv, 12 p.; 2 Plates: 18.18 x 25.03 inches and 19.94 x 26.44 inches, https://doi.org/10.3133/wri854035.","productDescription":"Report: iv, 12 p.; 2 Plates: 18.18 x 25.03 inches and 19.94 x 26.44 inches","costCenters":[],"links":[{"id":124162,"rank":1,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/wri/1985/4035/report-thumb.jpg"},{"id":55816,"rank":2,"type":{"id":11,"text":"Document"},"url":"https://pubs.usgs.gov/wri/1985/4035/report.pdf","linkFileType":{"id":1,"text":"pdf"}},{"id":55814,"rank":3,"type":{"id":17,"text":"Plate"},"url":"https://pubs.usgs.gov/wri/1985/4035/plate-1.pdf","linkFileType":{"id":1,"text":"pdf"}},{"id":55815,"rank":4,"type":{"id":17,"text":"Plate"},"url":"https://pubs.usgs.gov/wri/1985/4035/plate-2.pdf","linkFileType":{"id":1,"text":"pdf"}},{"id":415602,"rank":5,"type":{"id":36,"text":"NGMDB Index Page"},"url":"https://ngmdb.usgs.gov/Prodesc/proddesc_49200.htm","linkFileType":{"id":5,"text":"html"}}],"country":"United States","state":"New York","otherGeospatial":"Brookhaven, Long Island, Manorville area","geographicExtents":"{\n  \"type\": \"FeatureCollection\",\n  \"features\": [\n    {\n      \"type\": \"Feature\",\n      \"properties\": {},\n      \"geometry\": {\n        \"coordinates\": [\n          [\n            [\n              -72.8431,\n              40.875\n            ],\n            [\n              -72.8431,\n              40.75\n            ],\n            [\n              -72.7206,\n              40.75\n            ],\n            [\n              -72.7206,\n              40.875\n            ],\n            [\n              -72.8431,\n              40.875\n            ]\n          ]\n        ],\n        \"type\": \"Polygon\"\n      }\n    }\n  ]\n}","noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"4f4e4aa8e4b07f02db66744a","contributors":{"authors":[{"text":"Eckhardt, D. A.","contributorId":99591,"corporation":false,"usgs":true,"family":"Eckhardt","given":"D. A.","affiliations":[],"preferred":false,"id":197257,"contributorType":{"id":1,"text":"Authors"},"rank":1},{"text":"Wexler, E. J.","contributorId":104931,"corporation":false,"usgs":true,"family":"Wexler","given":"E.","email":"","middleInitial":"J.","affiliations":[],"preferred":false,"id":197258,"contributorType":{"id":1,"text":"Authors"},"rank":2}]}}
,{"id":70180236,"text":"70180236 - 1985 - Sea cliff exposures of metamorphosed carbonate and schist, northern Seward Peninsula: A section in <i>The United States Geological Survey in Alaska: Accomplishments during 1983</i>","interactions":[{"subject":{"id":70180236,"text":"70180236 - 1985 - Sea cliff exposures of metamorphosed carbonate and schist, northern Seward Peninsula: A section in <i>The United States Geological Survey in Alaska: Accomplishments during 1983</i>","indexId":"70180236","publicationYear":"1985","noYear":false,"title":"Sea cliff exposures of metamorphosed carbonate and schist, northern Seward Peninsula: A section in <i>The United States Geological Survey in Alaska: Accomplishments during 1983</i>"},"predicate":"IS_PART_OF","object":{"id":4437,"text":"cir945 - 1985 - The United States Geological Survey in Alaska: Accomplishments during 1983","indexId":"cir945","publicationYear":"1985","noYear":false,"title":"The United States Geological Survey in Alaska: Accomplishments during 1983"},"id":1}],"isPartOf":{"id":4437,"text":"cir945 - 1985 - The United States Geological Survey in Alaska: Accomplishments during 1983","indexId":"cir945","publicationYear":"1985","noYear":false,"title":"The United States Geological Survey in Alaska: Accomplishments during 1983"},"lastModifiedDate":"2018-05-07T21:26:33","indexId":"70180236","displayToPublicDate":"2017-01-01T00:00:00","publicationYear":"1985","noYear":false,"publicationType":{"id":18,"text":"Report"},"publicationSubtype":{"id":5,"text":"USGS Numbered Series"},"seriesTitle":{"id":307,"text":"Circular","code":"CIR","onlineIssn":"2330-5703","printIssn":"1067-084X","active":true,"publicationSubtype":{"id":5}},"seriesNumber":"945","title":"Sea cliff exposures of metamorphosed carbonate and schist, northern Seward Peninsula: A section in <i>The United States Geological Survey in Alaska: Accomplishments during 1983</i>","docAbstract":"<p>Extensive seacliff exposures of marble, metadolostone, and schist occur on the north shore of Seward Peninsula in the Kotzebue A-1 and A-2 Quadrangles (fig. 12). Some of the exposed units have no analogs when compared to rocks mapped to the south in the Bendeleben and Solomon Quadrangles. Others are similar to units exposed to the south, but they differ in metamorphic grade and minor, though significant, compositional characteristics. Carbonate rocks predominate from Ninemile Point westward; schists of varying composition occur with carbonate rocks to the east. The carbonate-dominated section is separated in the vicinity of Ninemile Point from the schist-dominated section by a major fault zone, thought to be the northern extension of the Kugruk fault zone of Sainsbury (1974). </p>","largerWorkType":{"id":18,"text":"Report"},"largerWorkTitle":"The United States Geological Survey in Alaska: Accomplishments during 1983 (Circular 945)","largerWorkSubtype":{"id":5,"text":"USGS Numbered Series"},"language":"English","publisher":"U.S. Geological Survey","publisherLocation":"Alexandria, VA","doi":"10.3133/70180236","usgsCitation":"Dumoulin, J.A., and Till, A.B., 1985, Sea cliff exposures of metamorphosed carbonate and schist, northern Seward Peninsula: A section in <i>The United States Geological Survey in Alaska: Accomplishments during 1983</i>: U.S. Geological Survey Circular 945, 5 p., https://doi.org/10.3133/70180236.","productDescription":"5 p.","startPage":"19","endPage":"22","numberOfPages":"5","costCenters":[{"id":114,"text":"Alaska Science Center","active":true,"usgs":true}],"links":[{"id":334021,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/thumbnails/outside_thumb.jpg"},{"id":334020,"rank":1,"type":{"id":11,"text":"Document"},"url":"https://pubs.usgs.gov/circ/1985/0945/report.pdf#page=30","text":"Start page in larger work"}],"country":"United States","state":"Alaska","otherGeospatial":"Seward Peninsula","noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"5889c7bfe4b0ba3b075e0639","contributors":{"authors":[{"text":"Dumoulin, Julie A. 0000-0003-1754-1287 dumoulin@usgs.gov","orcid":"https://orcid.org/0000-0003-1754-1287","contributorId":203209,"corporation":false,"usgs":true,"family":"Dumoulin","given":"Julie","email":"dumoulin@usgs.gov","middleInitial":"A.","affiliations":[{"id":119,"text":"Alaska Science Center Geology Minerals","active":true,"usgs":true},{"id":114,"text":"Alaska Science Center","active":true,"usgs":true}],"preferred":true,"id":660849,"contributorType":{"id":1,"text":"Authors"},"rank":1},{"text":"Till, Alison B. atill@usgs.gov","contributorId":2482,"corporation":false,"usgs":true,"family":"Till","given":"Alison","email":"atill@usgs.gov","middleInitial":"B.","affiliations":[{"id":119,"text":"Alaska Science Center Geology Minerals","active":true,"usgs":true}],"preferred":true,"id":660850,"contributorType":{"id":1,"text":"Authors"},"rank":2}]}}
,{"id":70180233,"text":"70180233 - 1985 - Preliminary description of a Miocene zone of structural complexity, Port Moller and Stepovak Bay quadrangles, Alaska: A section in <i>The United States Geological Survey in Alaska: Accomplishments during 1983</i>","interactions":[{"subject":{"id":70180233,"text":"70180233 - 1985 - Preliminary description of a Miocene zone of structural complexity, Port Moller and Stepovak Bay quadrangles, Alaska: A section in <i>The United States Geological Survey in Alaska: Accomplishments during 1983</i>","indexId":"70180233","publicationYear":"1985","noYear":false,"title":"Preliminary description of a Miocene zone of structural complexity, Port Moller and Stepovak Bay quadrangles, Alaska: A section in <i>The United States Geological Survey in Alaska: Accomplishments during 1983</i>"},"predicate":"IS_PART_OF","object":{"id":4437,"text":"cir945 - 1985 - The United States Geological Survey in Alaska: Accomplishments during 1983","indexId":"cir945","publicationYear":"1985","noYear":false,"title":"The United States Geological Survey in Alaska: Accomplishments during 1983"},"id":1}],"isPartOf":{"id":4437,"text":"cir945 - 1985 - The United States Geological Survey in Alaska: Accomplishments during 1983","indexId":"cir945","publicationYear":"1985","noYear":false,"title":"The United States Geological Survey in Alaska: Accomplishments during 1983"},"lastModifiedDate":"2017-05-19T18:13:51","indexId":"70180233","displayToPublicDate":"2017-01-01T00:00:00","publicationYear":"1985","noYear":false,"publicationType":{"id":18,"text":"Report"},"publicationSubtype":{"id":5,"text":"USGS Numbered Series"},"seriesTitle":{"id":307,"text":"Circular","code":"CIR","onlineIssn":"2330-5703","printIssn":"1067-084X","active":true,"publicationSubtype":{"id":5}},"seriesNumber":"945","title":"Preliminary description of a Miocene zone of structural complexity, Port Moller and Stepovak Bay quadrangles, Alaska: A section in <i>The United States Geological Survey in Alaska: Accomplishments during 1983</i>","docAbstract":"<p>A zone of structural disruption and complexity along the Pacific coast margin of the Alaska Peninsula (fig. 41) may be related to the Alaska Peninsula and the Chugach terrane boundary. The best exposure of this zone is located on the east shore of Humpback Bay (figs. 42, 43; also Burk, 1965, pl. 8, fig. 4); other exposures are located on the east side of Ivanof Bay, the north and south sides of Lefthand Bay, and in other coastal localities in the area. In some places, such as on the Kupreanof Peninsula, it is not recognized. This zone may extend discontinuously for 110-160 km along the coast; the width of the zone varies from 0.5 to 1 km. Our current data and tentative interpretations are described here, pending completion of additional field research, laboratory, and office studies. </p>","largerWorkType":{"id":18,"text":"Report"},"largerWorkTitle":"The United States Geological Survey in Alaska: Accomplishments during 1983 (Circular 945)","largerWorkSubtype":{"id":5,"text":"USGS Numbered Series"},"language":"English","publisher":"U.S. Geological Survey","publisherLocation":"Alexandria, VA","doi":"10.3133/70180233","usgsCitation":"Wilson, F.H., Case, J.E., and Detterman, R.L., 1985, Preliminary description of a Miocene zone of structural complexity, Port Moller and Stepovak Bay quadrangles, Alaska: A section in <i>The United States Geological Survey in Alaska: Accomplishments during 1983</i>: U.S. Geological Survey Circular 945, 2 p., https://doi.org/10.3133/70180233.","productDescription":"2 p.","startPage":"55","endPage":"56","numberOfPages":"2","costCenters":[{"id":114,"text":"Alaska Science Center","active":true,"usgs":true}],"links":[{"id":334006,"rank":1,"type":{"id":11,"text":"Document"},"url":"https://pubs.usgs.gov/circ/1985/0945/report.pdf#page=67","text":"Start page in larger work"},{"id":334007,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/thumbnails/outside_thumb.jpg"}],"country":"United States","state":"Alaska","otherGeospatial":"Port Moller quadrangle, Stepovak Bay quadrangle","noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"5889c7bfe4b0ba3b075e063b","contributors":{"authors":[{"text":"Wilson, Frederic H. 0000-0003-1761-6437 fwilson@usgs.gov","orcid":"https://orcid.org/0000-0003-1761-6437","contributorId":67174,"corporation":false,"usgs":true,"family":"Wilson","given":"Frederic","email":"fwilson@usgs.gov","middleInitial":"H.","affiliations":[{"id":119,"text":"Alaska Science Center Geology Minerals","active":true,"usgs":true},{"id":114,"text":"Alaska Science Center","active":true,"usgs":true}],"preferred":true,"id":660835,"contributorType":{"id":1,"text":"Authors"},"rank":1},{"text":"Case, James E.","contributorId":68702,"corporation":false,"usgs":true,"family":"Case","given":"James","email":"","middleInitial":"E.","affiliations":[],"preferred":false,"id":660836,"contributorType":{"id":1,"text":"Authors"},"rank":2},{"text":"Detterman, Robert L.","contributorId":71526,"corporation":false,"usgs":true,"family":"Detterman","given":"Robert","email":"","middleInitial":"L.","affiliations":[],"preferred":false,"id":660837,"contributorType":{"id":1,"text":"Authors"},"rank":3}]}}
,{"id":70178908,"text":"70178908 - 1985 - Seepage study of six canals in Salt Lake County, Utah, 1982-1983","interactions":[],"lastModifiedDate":"2016-12-12T11:15:30","indexId":"70178908","displayToPublicDate":"2016-11-01T00:00:00","publicationYear":"1985","noYear":false,"publicationType":{"id":18,"text":"Report"},"publicationSubtype":{"id":4,"text":"Other Government Series"},"seriesTitle":{"id":294,"text":"Technical Publication","active":false,"publicationSubtype":{"id":4}},"seriesNumber":"82","title":"Seepage study of six canals in Salt Lake County, Utah, 1982-1983","docAbstract":"<p>A study of selected reaches of the Utah and Salt Lake, Utah Lake Distributing, Provo Reservoir, Draper Irrigation, East Jordan, and Jordan and Salt Lake City Canals in Salt Lake County, Utah, was made to determine gains or losses of flow in those reaches. Three to five sets of seepage measurements were made on each canal during 1982 or 1983. Adjustments for fluctuations in flow were made from information obtained from water-stage recorders operated at selected locations during the time of each seepage run.</p><p>The study showed an overall net loss of about 9.5 cubic feet per second in the Utah and Salt Lake Canal, 11.0 cubic feet per second in the Utah Lake Distributing canal, 20.5 cubic feet per second in the Provo Reservoir canal, 1.5 cubic feet per second in the Draper Irrigation Canal, and 4.0 cubic feet per second in the East Jordan canal. It also showed a net gain of about 6.0 cubic feet per second in the Jordan and Salt Lake City Canal. The gains and losses are attributed primarily to the relation of the canals to the depth of the water table near the canals.</p>","language":"English","publisher":"Utah Department of Natural Resources, Division of Water Rights","publisherLocation":"Salt Lake City, UT","collaboration":"Prepared by the United States Geological Survey in cooperation with the Utah Department of Natural Resources Division of Water Rights","usgsCitation":"Herbert, L.R., Cruff, R., and Waddell, K., 1985, Seepage study of six canals in Salt Lake County, Utah, 1982-1983: Technical Publication 82, iv, 95 p.","productDescription":"iv, 95 p","numberOfPages":"102","costCenters":[{"id":610,"text":"Utah Water Science Center","active":true,"usgs":true}],"links":[{"id":331893,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/thumbnails/outside_thumb.jpg"},{"id":331891,"rank":1,"type":{"id":15,"text":"Index 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R.","contributorId":39865,"corporation":false,"usgs":true,"family":"Herbert","given":"L.","email":"","middleInitial":"R.","affiliations":[],"preferred":false,"id":655477,"contributorType":{"id":1,"text":"Authors"},"rank":1},{"text":"Cruff, R.W.","contributorId":77510,"corporation":false,"usgs":true,"family":"Cruff","given":"R.W.","email":"","affiliations":[],"preferred":false,"id":655478,"contributorType":{"id":1,"text":"Authors"},"rank":2},{"text":"Waddell, K.M.","contributorId":59009,"corporation":false,"usgs":true,"family":"Waddell","given":"K.M.","email":"","affiliations":[],"preferred":false,"id":655479,"contributorType":{"id":1,"text":"Authors"},"rank":3}]}}
,{"id":5222072,"text":"5222072 - 1985 - Metal contamination in wildlife living near two zinc smelters","interactions":[],"lastModifiedDate":"2023-11-02T10:59:43.443881","indexId":"5222072","displayToPublicDate":"2010-06-16T12:19:32","publicationYear":"1985","noYear":false,"publicationType":{"id":2,"text":"Article"},"publicationSubtype":{"id":10,"text":"Journal Article"},"seriesTitle":{"id":1556,"text":"Environmental Pollution (Series A)","active":true,"publicationSubtype":{"id":10}},"title":"Metal contamination in wildlife living near two zinc smelters","docAbstract":"<p>Wildlife in an oak forest on Blue Mountain was studied 10 km upwind (Bake Oven Knob site) and 2 km downwind (Palmerton site) of two zinc smelters in eastern Pennsylvania, USA. Previous studies at sites near these smelters had shown changes in populations of soil microflora, lichens, green plants and litter-inhabiting arthropods. The 02 soil litter horizon at Palmerton was heavily contaminated with Pb (2700 mg kg<sup>−1</sup>), Zn (24 000 mg kg<sup>−1</sup>), and Cd (710 mg kg<sup>−1</sup>), and to a lesser extent with Cu (440 mg kg<sup>−1</sup>). Various kinds of invertebrates (earthworms, slugs and millipedes) that feed on soil litter or soil organic matter were rare at, or absent from, the Palmerton site. Those collected at Bake Oven Knob tended to have much higher concentrations of metals than did other invertebrates. Frogs, toads and salamanders were very rare at, or absent from, the Palmerton site, but were present at Bake Oven Knob and at other sites on Blue Mountain farther from the smelters. Metal concentrations (dry wt) in different organisms from Palmerton were compared. Concentrations of Pb were highest in shrews (110 mg kg<sup>−1</sup>), followed by songbirds (56 mg kg<sup>−1</sup>), leaves (21 mg kg<sup>−1</sup>), mice (17 mg kg<sup>−1</sup>), carrion insects (14 mg kg<sup>−1</sup>), berries (4·0 mg kg<sup>−1</sup>), moths (4·3 mg kg<sup>−1</sup>) and fungi (3·7 mg kg<sup>−1</sup>). Concentrations of Cd, in contrast, were highest in carrion insects (25 mg kg<sup>−1</sup>), followed by fungi (9·8 mg kg<sup>−1</sup>), leaves (8·1 mg kg<sup>−1</sup>), shrews (7·3 mg kg<sup>−1</sup>), moths (4·9 mg kg<sup>−1</sup>), mice (2·6 mg kg<sup>−1</sup>), songbirds (2·5 mg kg<sup>−1</sup>) and berries (1·2 mg kg<sup>−1</sup>).</p><p>Concentrations of Zn and Cu tended to be highest in the same organisms that had the highest concentrations of Cd. Only a small proportion of the metals in the soil became incorporated into plant foliage, and much of the metal contamination detected in the biota probably came from aerial deposition. The mice from both sites seemed to be healthy. Shrews had higher concentrations of metals than did mice, and one shrew showed evidence of Pb poisoning; its red blood cell ALAD activity was greatly reduced, one kidney contained acid-fast intranuclear inclusion bodies, and the other kidney had 280 mg kg<sup>−1</sup><span>&nbsp;</span>Pb (wet wt). The livers from two cuckoos from Palmerton had elevated Pb concentrations (18 and 25 mg kg<sup>−1</sup>, wet wt). Most of the songbirds seemed to be healthy.</p>","language":"English","publisher":"Elsevier","doi":"10.1016/0143-1471(85)90094-7","usgsCitation":"Beyer, W., Pattee, O.H., Sileo, L., Hoffman, D.J., and Mulhern, B., 1985, Metal contamination in wildlife living near two zinc smelters: Environmental Pollution (Series A), v. 38, no. 1, p. 63-86, https://doi.org/10.1016/0143-1471(85)90094-7.","productDescription":"24 p.","startPage":"63","endPage":"86","costCenters":[{"id":531,"text":"Patuxent Wildlife Research Center","active":true,"usgs":true}],"links":[{"id":198096,"rank":1,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/thumbnails/outside_thumb.jpg"}],"country":"United States","state":"Pennsylvania","otherGeospatial":"Bake Oven Knob, Blue Mountain","geographicExtents":"{\n  \"type\": \"FeatureCollection\",\n  \"features\": [\n    {\n      \"type\": \"Feature\",\n      \"properties\": {},\n      \"geometry\": {\n        \"coordinates\": [\n          [\n            [\n              -75.78720868224616,\n              40.700636729321474\n            ],\n            [\n              -75.77438869190075,\n              40.70682137615654\n            ],\n            [\n              -75.75574143321599,\n              40.716318108447666\n            ],\n            [\n              -75.73534599402986,\n              40.724267819364314\n            ],\n            [\n              -75.72485691101944,\n              40.73486595700689\n            ],\n            [\n              -75.69892556691127,\n              40.737956762527716\n            ],\n            [\n              -75.67969558139289,\n              40.7470075812013\n            ],\n            [\n              -75.66833240813207,\n              40.75649858000574\n            ],\n            [\n              -75.64560606161044,\n              40.76687091272373\n            ],\n            [\n              -75.61384744916288,\n              40.775697154940076\n            ],\n            [\n              -75.60481518323756,\n              40.783639770481955\n            ],\n            [\n              -75.60831154424089,\n              40.796875352513666\n            ],\n            [\n              -75.62754152975982,\n              40.79797819859462\n            ],\n            [\n              -75.65492969095253,\n              40.790919667081596\n            ],\n            [\n              -75.66745831788111,\n              40.792243198903265\n            ],\n            [\n              -75.70766646941978,\n              40.78275730454371\n            ],\n            [\n              -75.73534599402986,\n              40.76709158306798\n            ],\n            [\n              -75.76448233572451,\n              40.75053927390272\n            ],\n            [\n              -75.78487777491063,\n              40.746566106425604\n            ],\n            [\n              -75.81255729952069,\n              40.73265815086202\n            ],\n            [\n              -75.82333774594738,\n              40.71653894657126\n            ],\n            [\n              -75.82683410695122,\n              40.70947176328093\n            ],\n            [\n              -75.81826068013379,\n              40.69375877677078\n            ],\n            [\n              -75.78720868224616,\n              40.700636729321474\n            ]\n          ]\n        ],\n        \"type\": \"Polygon\"\n      }\n    }\n  ]\n}","volume":"38","issue":"1","noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"4f4e4a4be4b07f02db625903","contributors":{"authors":[{"text":"Beyer, W. N. 0000-0002-8911-9141","orcid":"https://orcid.org/0000-0002-8911-9141","contributorId":55379,"corporation":false,"usgs":true,"family":"Beyer","given":"W. N.","affiliations":[],"preferred":false,"id":335438,"contributorType":{"id":1,"text":"Authors"},"rank":1},{"text":"Pattee, O. H.","contributorId":46459,"corporation":false,"usgs":true,"family":"Pattee","given":"O.","email":"","middleInitial":"H.","affiliations":[],"preferred":false,"id":335436,"contributorType":{"id":1,"text":"Authors"},"rank":2},{"text":"Sileo, L.","contributorId":46895,"corporation":false,"usgs":true,"family":"Sileo","given":"L.","email":"","affiliations":[],"preferred":false,"id":335437,"contributorType":{"id":1,"text":"Authors"},"rank":3},{"text":"Hoffman, D. J.","contributorId":12801,"corporation":false,"usgs":true,"family":"Hoffman","given":"D.","email":"","middleInitial":"J.","affiliations":[],"preferred":false,"id":335435,"contributorType":{"id":1,"text":"Authors"},"rank":4},{"text":"Mulhern, B.M.","contributorId":98683,"corporation":false,"usgs":true,"family":"Mulhern","given":"B.M.","email":"","affiliations":[],"preferred":false,"id":335439,"contributorType":{"id":1,"text":"Authors"},"rank":5}]}}
,{"id":70013110,"text":"70013110 - 1985 - Accretion tectonics and crustal structure in Alaska","interactions":[],"lastModifiedDate":"2025-08-25T16:55:09.329596","indexId":"70013110","displayToPublicDate":"2003-04-11T00:00:00","publicationYear":"1985","noYear":false,"publicationType":{"id":2,"text":"Article"},"publicationSubtype":{"id":10,"text":"Journal Article"},"seriesTitle":{"id":3525,"text":"Tectonophysics","active":true,"publicationSubtype":{"id":10}},"title":"Accretion tectonics and crustal structure in Alaska","docAbstract":"<p>The entire width of the North American Cordillera in Alaska is made up of \"suspect terranes\". Pre-Late Cretaceous paleogeography is poorly constrained and the ultimate origins of the many fragments which make up the state are unclear. The Prince William and Chugach terranes accreted since Late Cretaceous time and represent the collapse of much of the northeast Pacific Ocean swept into what today is southern Alaska. Greater Wrangellia, a composite terrane now dispersed into fragments scattered from Idaho to southern Alaska, apparently accreted into Alaska in Late Cretaceous time crushing an enormous deep-marine flysch basin on its inboard side. Most of interior eastern Alaska is the Yukon Tanana terrane, a very large entirely fault-bounded metamorphic-plutonic assemblage covering thousands of square kilometers in Canada as well as Alaska. The original stratigraphy and relationship to North America of the Yukon-Tanana terrane are both obscure. A collapsed Mesozoic flysch basin, similar to the one inboard of Wrangellia, lies along the northern margin. Much of Arctic Alaska was apparently a vast expanse of upper Paleozoic to Early Mesozoic deep marine sediments and mafic volcanic and plutonic rocks now scattered widely as large telescoped sheets and Klippen thrust over the Ruby geanticline and the Brooks Range, and probably underlying the Yukon-Koyukuk basin and the Yukon flats. The Brooks Range itself is a stack of north vergent nappes, the telescoping of which began in Early Cretaceous time. Despite compelling evidence for thousands of kilometers of relative displacement between the accreted terranes, and large amounts of telescoping, translation, and rotation since accretion, the resulting new continental crust added to North America in Alaska carries few obvious signatures that allow application of currently popular simple plate tectonic models. Intraplate telescoping and strike-slip translations, delamination at mid-crustal levels, and large-scale lithospheric wedging were important processes in northern Cordilleran tectonic evolution.&nbsp;</p>","language":"English","publisher":"Elsevier","doi":"10.1016/0040-1951(85)90042-3","issn":"00401951","usgsCitation":"Coney, P., and Jones, D.L., 1985, Accretion tectonics and crustal structure in Alaska: Tectonophysics, v. 119, no. 1-4, p. 265-283, https://doi.org/10.1016/0040-1951(85)90042-3.","productDescription":"19 p.","startPage":"265","endPage":"283","costCenters":[],"links":[{"id":220013,"rank":1,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/thumbnails/outside_thumb.jpg"}],"country":"United 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,{"id":70012687,"text":"70012687 - 1985 - Quaternary sedimentation of the Alaskan Beaufort shelf: Influence of regional tectonics, fluctuating sea levels, and glacial sediment sources","interactions":[],"lastModifiedDate":"2025-08-26T16:42:35.227148","indexId":"70012687","displayToPublicDate":"2003-03-26T00:00:00","publicationYear":"1985","noYear":false,"publicationType":{"id":2,"text":"Article"},"publicationSubtype":{"id":10,"text":"Journal Article"},"seriesTitle":{"id":3525,"text":"Tectonophysics","active":true,"publicationSubtype":{"id":10}},"title":"Quaternary sedimentation of the Alaskan Beaufort shelf: Influence of regional tectonics, fluctuating sea levels, and glacial sediment sources","docAbstract":"<p>The offshore stratigraphy of the Quaternary Gubik Formation of Arctic Alaska has been studied on high-resolution seismic profiles with a maximum sub-seafloor penetration of about 100 m. In general, marine transgressive subunits of the Gubik Formation are wedge-shaped on the shelf, thickening slightly seaward to the shelf break, beyond which they are offset by landslides and slumps. Beneath the eastern third of the Alaskan Beaufort shelf, active folding has created two persistent structural depressions, the Eastern and Western Wedge Terranes, in which the wedge morphology is especially well developed. The youngest transgressive marine wedge, which was deposited in such a way as to fill these depressions, leaving a generally flat present-day shelf surface, is inferred to be late Wisconsin or younger in age because it overlies a prominent disconformity interpreted to have been formed during the late Wisconsin glacial sea-level minimum. The thickness of this youngest wedge, Unit A, locally exceeds 40 m on the outer shelf, yet apparently relict gravel deposits collected from its seabed surface indicate that the depositional rate is presently quite low on the middle and outer shelf. Lithologies of the gravels are exotic to Alaska, but similar to suites exposed in the Canadian Arctic Islands. These observations suggest a depositional scenario in which the retreating Laurentide Ice Sheet shed sediment-laden icebergs from the Canadian Arctic Islands into the Arctic Ocean following the late Wisconsin glacial maximum. These bergs were then rafted westward by the Beaufort Gyre and grounded on the Alaskan shelf by northeasterly prevailing winds. Especially large numbers of bergs accumulated in the wedge terrane embayments-created as sea level rose-and melted there, filling the embayments with their sedimentary cargo. As glacial retreat slowed, depositional rates on the shelf dwindled. </p><p>This mode of deposition in the Alaskan Beaufort wedge terranes may be typical of early post-glacial transgressive phases throughout Quaternary time. It has resulted in the preservation of disconformities that apparently formed during glacioeustatic lowstands, and whose seaward termination depths, appropriately corrected, may yield estimates of lowstand magnitudes. Knowledge of global sea-level fluctuations back through the Sangamon Interglacial (oxygen isotope stage 5e) and possible correlations with dated onshore deposits have facilitated a tentative correlation of major disconformities in the Beaufort Sea record with major 18O enrichment maxima in the oxygen isotope curve back through stage 8. In this tentative scheme, close similarities between the two data sets occur both in magnitudes and in numbers of fluctuations intervening between major correlation points. Further testing of the Quaternary depositional model suggested here and of the resulting sea level curve awaits the collection and dating of core samples from the Beaufort wedge terranes.</p>","language":"English","publisher":"Elsevier","doi":"10.1016/0040-1951(85)90010-1","issn":"00401951","usgsCitation":"Dinter, D.A., 1985, Quaternary sedimentation of the Alaskan Beaufort shelf: Influence of regional tectonics, fluctuating sea levels, and glacial sediment sources: Tectonophysics, v. 114, no. 1-4, p. 133-161, https://doi.org/10.1016/0040-1951(85)90010-1.","productDescription":"29 p.","startPage":"133","endPage":"161","costCenters":[],"links":[{"id":222492,"rank":1,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/thumbnails/outside_thumb.jpg"}],"country":"United States","state":"Alaska","geographicExtents":"{\n  \"type\": \"FeatureCollection\",\n  \"features\": [\n    {\n      \"type\": \"Feature\",\n      \"properties\": {},\n      \"geometry\": {\n        \"coordinates\": [\n          [\n            [\n              -161.46539412646445,\n              71.61325942564287\n            ],\n            [\n              -161.46539412646445,\n              69.23521971003117\n            ],\n            [\n              -140.92461926584397,\n              69.23521971003117\n            ],\n            [\n              -140.92461926584397,\n              71.61325942564287\n            ],\n            [\n              -161.46539412646445,\n              71.61325942564287\n            ]\n          ]\n        ],\n        \"type\": \"Polygon\"\n      }\n    }\n  ]\n}","volume":"114","issue":"1-4","noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"505a92d8e4b0c8380cd80aa9","contributors":{"authors":[{"text":"Dinter, David A.","contributorId":104010,"corporation":false,"usgs":true,"family":"Dinter","given":"David","middleInitial":"A.","affiliations":[],"preferred":false,"id":364225,"contributorType":{"id":1,"text":"Authors"},"rank":1}]}}
,{"id":60341,"text":"mf1246J - 1985 - Maps showing distribution of tungsten in heavy-mineral concentrates, Richfield 1° x 2° quadrangle, Utah","interactions":[],"lastModifiedDate":"2021-12-22T19:26:09.570433","indexId":"mf1246J","displayToPublicDate":"1994-01-01T07:00:00","publicationYear":"1985","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":"1246","chapter":"J","title":"Maps showing distribution of tungsten in heavy-mineral concentrates, Richfield 1° x 2° quadrangle, Utah","docAbstract":"<p>These maps are part of a folio of maps of the Richfield 1° x 2 ° quadrangle, Utah, prepared under the Conterminuous United States Mineral Assessment Program. Other publications in this folio are listed in the selected references.</p><p>Located in west-central Utah, the Richfield quadrangle covers the eastern part of the Plioche-Marysvale igneous and mineral belt, which extends from the vicinity of Plioche in southeastern Nevada east-northeastward for 250 km (155 mi) into central Utah. The western two-thirds of the Richfield quadrangle is in the Basin and Range province and the eastern third is in the High Plateaus of Utah, a subprovince of the Colorado Plateau.</p><p>Bedrock in the northern part of the Richfield quadrangle consists predominantly of latest Precambrian and Paleozoic sedimentary strata that were thrust eastward during the Sevier orogeny in Cretaceous time onto an autochthon of Mesozoic sedimentary rocks in the eastern part of the quadrangle. The southern part of the quadrangle is largely underlain by Oligocene and younger volcanic rocks and related intrusions. Extensional tectonism in late Cenozoic time broke the bedrock terrane into a series of north-trending fault blocks; the uplifted mountain areas were deeply eroded and the resulting debris deposited in the adjacent basins. Most of the mineral deposits in the Pioche-Marysvale mineral belt were formed during igneous activity in middle and late Cenozoic time.</p><p>The regional sampling program was designed to define broad geochemical patterns and trends which can be utilized along with geologic and geophysical data to assess the mineral resource potential for this quadrangle. These maps of the Richfield 1° x 2° quadrangle show the regional distributions of copper in two fractions of heavy-mineral concentrates of drainage sediments.</p>","language":"English","publisher":"U.S. Geological Survey","publisherLocation":"Denver, CO","doi":"10.3133/mf1246J","usgsCitation":"Miller, W.R., Motooka, J.M., and McHugh, J., 1985, Maps showing distribution of tungsten in heavy-mineral concentrates, Richfield 1° x 2° quadrangle, Utah: U.S. Geological Survey Miscellaneous Field Studies Map 1246, 1 Plate: 35.98 x 27.39 inches, https://doi.org/10.3133/mf1246J.","productDescription":"1 Plate: 35.98 x 27.39 inches","costCenters":[],"links":[{"id":182847,"rank":0,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/thumbnails/mf1246j.jpg"},{"id":393329,"rank":3,"type":{"id":17,"text":"Plate"},"url":"https://pubs.usgs.gov/mf/1246-J/plate-1.pdf","linkFileType":{"id":1,"text":"pdf"}},{"id":390902,"rank":2,"type":{"id":36,"text":"NGMDB Index Page"},"url":"https://ngmdb.usgs.gov/Prodesc/proddesc_6854.htm"}],"scale":"500000","country":"United States","state":"Utah","otherGeospatial":"Richfield quadrangle","geographicExtents":"{ \"type\": \"FeatureCollection\", \"features\": [ { \"type\": \"Feature\", \"properties\": {}, \"geometry\": { \"type\": \"Polygon\", \"coordinates\": [ [ [ -114.0,38.0 ], [ -114.0,39.0 ], [ -112.0,39.0 ], [ -112.0,38.0 ], [ -114.0,38.0 ] ] ] } } ] }","noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"4f4e4a19e4b07f02db6057bd","contributors":{"authors":[{"text":"Miller, William R.","contributorId":53838,"corporation":false,"usgs":true,"family":"Miller","given":"William","email":"","middleInitial":"R.","affiliations":[],"preferred":false,"id":263579,"contributorType":{"id":1,"text":"Authors"},"rank":1},{"text":"Motooka, Jerry M.","contributorId":36611,"corporation":false,"usgs":true,"family":"Motooka","given":"Jerry","email":"","middleInitial":"M.","affiliations":[],"preferred":false,"id":263578,"contributorType":{"id":1,"text":"Authors"},"rank":2},{"text":"McHugh, John B.","contributorId":64651,"corporation":false,"usgs":true,"family":"McHugh","given":"John B.","affiliations":[],"preferred":false,"id":263580,"contributorType":{"id":1,"text":"Authors"},"rank":3}]}}
,{"id":60338,"text":"mf1246G - 1985 - Maps showing distribution of lead in heavy-mineral concentrates, Richfield 1° x 2° quadrangle, Utah","interactions":[],"lastModifiedDate":"2021-10-25T19:01:20.256061","indexId":"mf1246G","displayToPublicDate":"1994-01-01T07:00:00","publicationYear":"1985","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":"1246","chapter":"G","title":"Maps showing distribution of lead in heavy-mineral concentrates, Richfield 1° x 2° quadrangle, Utah","docAbstract":"<p>These maps are part of a folio of maps of the Richfield 1° x 2 ° quadrangle, Utah, prepared under the Conterminuous United States Mineral Assessment Program. Other publications in this folio are listed in the selected references.</p><p>Located in west-central Utah, the Richfield quadrangle covers the eastern part of the Plioche-Marysvale igneous and mineral belt, which extends from the vicinity of Plioche in southeastern Nevada east-northeastward for 250 km (155 mi) into central Utah. The western two-thirds of the Richfield quadrangle is in the Basin and Range province and the eastern third is in the High Plateaus of Utah, a subprovince of the Colorado Plateau.</p><p><br></p><p>Bedrock in the northern part of the Richfield quadrangle consists predominantly of latest Precambrian and Paleozoic sedimentary strata that were thrust eastward during the Sevier orogeny in Cretaceous time onto an autochthon of Mesozoic sedimentary rocks in the eastern part of the quadrangle. The southern part of the quadrangle is largely underlain by Oligocene and younger volcanic rocks and related intrusions. Extensional tectonism in late Cenozoic time broke the bedrock terrane into a series of north-trending fault blocks; the uplifted mountain areas were deeply eroded and the resulting debris deposited in the adjacent basins. Most of the mineral deposits in the Pioche-Marysvale mineral belt were formed during igneous activity in middle and late Cenozoic time.</p><p>The regional sampling program was designed to define broad geochemical patterns and trends which can be utilized along with geologic and geophysical data to assess the mineral resource potential for this quadrangle. These maps of the Richfield 1° x 2° quadrangle show the regional distributions of copper in two fractions of heavy-mineral concentrates of drainage sediments.</p>","language":"English","publisher":"U.S. Geological Survey","publisherLocation":"Denver, CO","doi":"10.3133/mf1246G","usgsCitation":"Miller, W.R., Motooka, J.M., and McHugh, J., 1985, Maps showing distribution of lead in heavy-mineral concentrates, Richfield 1° x 2° quadrangle, Utah: U.S. Geological Survey Miscellaneous Field Studies Map 1246, 1 Plate: 36.38 x 27.85 inches, https://doi.org/10.3133/mf1246G.","productDescription":"1 Plate: 36.38 x 27.85 inches","costCenters":[],"links":[{"id":179800,"rank":0,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/thumbnails/mf1246g.jpg"},{"id":283655,"type":{"id":17,"text":"Plate"},"url":"https://pubs.usgs.gov/mf/1246-G/plate-1.pdf"},{"id":390898,"rank":3,"type":{"id":36,"text":"NGMDB Index Page"},"url":"https://ngmdb.usgs.gov/Prodesc/proddesc_6851.htm"}],"scale":"500000","country":"United States","state":"Utah","otherGeospatial":"Richfield 1° x 2° quadrangle","geographicExtents":"{ \"type\": \"FeatureCollection\", \"features\": [ { \"type\": \"Feature\", \"properties\": {}, \"geometry\": { \"type\": \"Polygon\", \"coordinates\": [ [ [ -114.0,38.0 ], [ -114.0,39.0 ], [ -112.0,39.0 ], [ -112.0,38.0 ], [ -114.0,38.0 ] ] ] } } ] }","noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"4f4e4a19e4b07f02db605779","contributors":{"authors":[{"text":"Miller, William R.","contributorId":53838,"corporation":false,"usgs":true,"family":"Miller","given":"William","email":"","middleInitial":"R.","affiliations":[],"preferred":false,"id":263570,"contributorType":{"id":1,"text":"Authors"},"rank":1},{"text":"Motooka, Jerry M.","contributorId":36611,"corporation":false,"usgs":true,"family":"Motooka","given":"Jerry","email":"","middleInitial":"M.","affiliations":[],"preferred":false,"id":263569,"contributorType":{"id":1,"text":"Authors"},"rank":2},{"text":"McHugh, John B.","contributorId":64651,"corporation":false,"usgs":true,"family":"McHugh","given":"John B.","affiliations":[],"preferred":false,"id":263571,"contributorType":{"id":1,"text":"Authors"},"rank":3}]}}
,{"id":60339,"text":"mf1246H - 1985 - Maps showing distribution of thorium in heavy-mineral concentrates, Richfield 1° x 2° quadrangle, Utah","interactions":[],"lastModifiedDate":"2021-10-25T19:04:27.687858","indexId":"mf1246H","displayToPublicDate":"1994-01-01T07:00:00","publicationYear":"1985","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":"1246","chapter":"H","title":"Maps showing distribution of thorium in heavy-mineral concentrates, Richfield 1° x 2° quadrangle, Utah","docAbstract":"<p>These maps are part of a folio of maps of the Richfield 1° x 2 ° quadrangle, Utah, prepared under the Conterminuous United States Mineral Assessment Program. Other publications in this folio are listed in the selected references.</p><p><br></p><p>Located in west-central Utah, the Richfield quadrangle covers the eastern part of the Plioche-Marysvale igneous and mineral belt, which extends from the vicinity of Plioche in southeastern Nevada east-northeastward for 250 km (155 mi) into central Utah. The western two-thirds of the Richfield quadrangle is in the Basin and Range province and the eastern third is in the High Plateaus of Utah, a subprovince of the Colorado Plateau.</p><p>Bedrock in the northern part of the Richfield quadrangle consists predominantly of latest Precambrian and Paleozoic sedimentary strata that were thrust eastward during the Sevier orogeny in Cretaceous time onto an autochthon of Mesozoic sedimentary rocks in the eastern part of the quadrangle. The southern part of the quadrangle is largely underlain by Oligocene and younger volcanic rocks and related intrusions. Extensional tectonism in late Cenozoic time broke the bedrock terrane into a series of north-trending fault blocks; the uplifted mountain areas were deeply eroded and the resulting debris deposited in the adjacent basins. Most of the mineral deposits in the Pioche-Marysvale mineral belt were formed during igneous activity in middle and late Cenozoic time.</p><p>The regional sampling program was designed to define broad geochemical patterns and trends which can be utilized along with geologic and geophysical data to assess the mineral resource potential for this quadrangle. These maps of the Richfield 1° x 2° quadrangle show the regional distributions of copper in two fractions of heavy-mineral concentrates of drainage sediments.</p>","language":"English","publisher":"U.S. Geological Survey","publisherLocation":"Denver, CO","doi":"10.3133/mf1246H","usgsCitation":"Miller, W.R., Motooka, J.M., and McHugh, J., 1985, Maps showing distribution of thorium in heavy-mineral concentrates, Richfield 1° x 2° quadrangle, Utah: U.S. Geological Survey Miscellaneous Field Studies Map 1246, 1 Plate: 36.21 x 27.70 inches, https://doi.org/10.3133/mf1246H.","productDescription":"1 Plate: 36.21 x 27.70 inches","costCenters":[],"links":[{"id":390900,"rank":3,"type":{"id":36,"text":"NGMDB Index Page"},"url":"https://ngmdb.usgs.gov/Prodesc/proddesc_6852.htm"},{"id":283656,"type":{"id":17,"text":"Plate"},"url":"https://pubs.usgs.gov/mf/1246-H/plate-1.pdf"},{"id":179801,"rank":0,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/thumbnails/mf1246h.jpg"}],"scale":"500000","country":"United States","state":"Utah","otherGeospatial":"Richfield 1° x 2° quadrangle","geographicExtents":"{ \"type\": \"FeatureCollection\", \"features\": [ { \"type\": \"Feature\", \"properties\": {}, \"geometry\": { \"type\": \"Polygon\", \"coordinates\": [ [ [ -114.0,38.0 ], [ -114.0,39.0 ], [ -112.0,39.0 ], [ -112.0,38.0 ], [ -114.0,38.0 ] ] ] } } ] }","noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"4f4e4a19e4b07f02db6057b4","contributors":{"authors":[{"text":"Miller, William R.","contributorId":53838,"corporation":false,"usgs":true,"family":"Miller","given":"William","email":"","middleInitial":"R.","affiliations":[],"preferred":false,"id":263573,"contributorType":{"id":1,"text":"Authors"},"rank":1},{"text":"Motooka, Jerry M.","contributorId":36611,"corporation":false,"usgs":true,"family":"Motooka","given":"Jerry","email":"","middleInitial":"M.","affiliations":[],"preferred":false,"id":263572,"contributorType":{"id":1,"text":"Authors"},"rank":2},{"text":"McHugh, John B.","contributorId":64651,"corporation":false,"usgs":true,"family":"McHugh","given":"John B.","affiliations":[],"preferred":false,"id":263574,"contributorType":{"id":1,"text":"Authors"},"rank":3}]}}
,{"id":60340,"text":"mf1246I - 1985 - Maps showing distribution of tin in heavy-mineral concentrates, Richfield 1° x 2° quadrangle, Utah","interactions":[],"lastModifiedDate":"2021-10-25T19:06:12.463908","indexId":"mf1246I","displayToPublicDate":"1994-01-01T07:00:00","publicationYear":"1985","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":"1246","chapter":"I","title":"Maps showing distribution of tin in heavy-mineral concentrates, Richfield 1° x 2° quadrangle, Utah","docAbstract":"<p>These maps are part of a folio of maps of the Richfield 1° x 2 ° quadrangle, Utah, prepared under the Conterminuous United States Mineral Assessment Program. Other publications in this folio are listed in the selected references.</p><p>Located in west-central Utah, the Richfield quadrangle covers the eastern part of the Plioche-Marysvale igneous and mineral belt, which extends from the vicinity of Plioche in southeastern Nevada east-northeastward for 250 km (155 mi) into central Utah. The western two-thirds of the Richfield quadrangle is in the Basin and Range province and the eastern third is in the High Plateaus of Utah, a subprovince of the Colorado Plateau.</p><p><br></p><p>Bedrock in the northern part of the Richfield quadrangle consists predominantly of latest Precambrian and Paleozoic sedimentary strata that were thrust eastward during the Sevier orogeny in Cretaceous time onto an autochthon of Mesozoic sedimentary rocks in the eastern part of the quadrangle. The southern part of the quadrangle is largely underlain by Oligocene and younger volcanic rocks and related intrusions. Extensional tectonism in late Cenozoic time broke the bedrock terrane into a series of north-trending fault blocks; the uplifted mountain areas were deeply eroded and the resulting debris deposited in the adjacent basins. Most of the mineral deposits in the Pioche-Marysvale mineral belt were formed during igneous activity in middle and late Cenozoic time.</p><p>The regional sampling program was designed to define broad geochemical patterns and trends which can be utilized along with geologic and geophysical data to assess the mineral resource potential for this quadrangle. These maps of the Richfield 1° x 2° quadrangle show the regional distributions of copper in two fractions of heavy-mineral concentrates of drainage sediments.</p>","language":"English","publisher":"U.S. Geological Survey","publisherLocation":"Denver, CO","doi":"10.3133/mf1246I","usgsCitation":"Miller, W.R., Motooka, J.M., and McHugh, J., 1985, Maps showing distribution of tin in heavy-mineral concentrates, Richfield 1° x 2° quadrangle, Utah: U.S. Geological Survey Miscellaneous Field Studies Map 1246, 1 Plate: 36.15 x 27.85 inches, https://doi.org/10.3133/mf1246I.","productDescription":"1 Plate: 36.15 x 27.85 inches","costCenters":[],"links":[{"id":182846,"rank":0,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/thumbnails/mf1246i.jpg"},{"id":390901,"rank":3,"type":{"id":36,"text":"NGMDB Index Page"},"url":"https://ngmdb.usgs.gov/Prodesc/proddesc_6853.htm"},{"id":283657,"type":{"id":17,"text":"Plate"},"url":"https://pubs.usgs.gov/mf/1246-I/plate-1.pdf"}],"scale":"500000","country":"United States","state":"Utah","otherGeospatial":"Richfield 1° x 2° quadrangle","geographicExtents":"{ \"type\": \"FeatureCollection\", \"features\": [ { \"type\": \"Feature\", \"properties\": {}, \"geometry\": { \"type\": \"Polygon\", \"coordinates\": [ [ [ -114.0,38.0 ], [ -114.0,39.0 ], [ -112.0,39.0 ], [ -112.0,38.0 ], [ -114.0,38.0 ] ] ] } } ] }","noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"4f4e4a19e4b07f02db6057ba","contributors":{"authors":[{"text":"Miller, William R.","contributorId":53838,"corporation":false,"usgs":true,"family":"Miller","given":"William","email":"","middleInitial":"R.","affiliations":[],"preferred":false,"id":263576,"contributorType":{"id":1,"text":"Authors"},"rank":1},{"text":"Motooka, Jerry M.","contributorId":36611,"corporation":false,"usgs":true,"family":"Motooka","given":"Jerry","email":"","middleInitial":"M.","affiliations":[],"preferred":false,"id":263575,"contributorType":{"id":1,"text":"Authors"},"rank":2},{"text":"McHugh, John B.","contributorId":64651,"corporation":false,"usgs":true,"family":"McHugh","given":"John B.","affiliations":[],"preferred":false,"id":263577,"contributorType":{"id":1,"text":"Authors"},"rank":3}]}}
,{"id":60337,"text":"mf1246F - 1985 - Maps showing distribution of copper in heavy-mineral concentrates, Richfield 1° x 2° quadrangle, Utah","interactions":[],"lastModifiedDate":"2021-10-25T18:59:37.497209","indexId":"mf1246F","displayToPublicDate":"1994-01-01T07:00:00","publicationYear":"1985","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":"1246","chapter":"F","title":"Maps showing distribution of copper in heavy-mineral concentrates, Richfield 1° x 2° quadrangle, Utah","docAbstract":"<p>These maps are part of a folio of maps of the Richfield 1° x 2 ° quadrangle, Utah, prepared under the Conterminuous United States Mineral Assessment Program. Other publications in this folio are listed in the selected references.</p><p>Located in west-central Utah, the Richfield quadrangle covers the eastern part of the Plioche-Marysvale igneous and mineral belt, which extends from the vicinity of Plioche in southeastern Nevada east-northeastward for 250 km (155 mi) into central Utah. The western two-thirds of the Richfield quadrangle is in the Basin and Range province and the eastern third is in the High Plateaus of Utah, a subprovince of the Colorado Plateau.</p><p><br></p><p>Bedrock in the northern part of the Richfield quadrangle consists predominantly of latest Precambrian and Paleozoic sedimentary strata that were thrust eastward during the Sevier orogeny in Cretaceous time onto an autochthon of Mesozoic sedimentary rocks in the eastern part of the quadrangle. The southern part of the quadrangle is largely underlain by Oligocene and younger volcanic rocks and related intrusions. Extensional tectonism in late Cenozoic time broke the bedrock terrane into a series of north-trending fault blocks; the uplifted mountain areas were deeply eroded and the resulting debris deposited in the adjacent basins. Most of the mineral deposits in the Pioche-Marysvale mineral belt were formed during igneous activity in middle and late Cenozoic time.</p><p><br></p><p>The regional sampling program was designed to define broad geochemical patterns and trends which can be utilized along with geologic and geophysical data to assess the mineral resource potential for this quadrangle. These maps of the Richfield 1° x 2° quadrangle show the regional distributions of copper in two fractions of heavy-mineral concentrates of drainage sediments.</p>","language":"English","publisher":"U.S. Geological Survey","publisherLocation":"Denver, CO","doi":"10.3133/mf1246F","usgsCitation":"Miller, W.R., Motooka, J.M., and McHugh, J., 1985, Maps showing distribution of copper in heavy-mineral concentrates, Richfield 1° x 2° quadrangle, Utah: U.S. Geological Survey Miscellaneous Field Studies Map 1246, 1 Plate: 36.31 x 27.27 inches, https://doi.org/10.3133/mf1246F.","productDescription":"1 Plate: 36.31 x 27.27 inches","costCenters":[],"links":[{"id":179799,"rank":0,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/thumbnails/mf1246f.PNG"},{"id":390897,"rank":3,"type":{"id":36,"text":"NGMDB Index Page"},"url":"https://ngmdb.usgs.gov/Prodesc/proddesc_6850.htm"},{"id":283654,"type":{"id":17,"text":"Plate"},"url":"https://pubs.usgs.gov/mf/1246-F/plate-1.pdf"}],"scale":"500000","country":"United States","state":"Utah","otherGeospatial":"Richfield 1° x 2° quadrangle","geographicExtents":"{ \"type\": \"FeatureCollection\", \"features\": [ { \"type\": \"Feature\", \"properties\": {}, \"geometry\": { \"type\": \"Polygon\", \"coordinates\": [ [ [ -114.0,38.0 ], [ -114.0,39.0 ], [ -112.0,39.0 ], [ -112.0,38.0 ], [ -114.0,38.0 ] ] ] } } ] }","noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"4f4e4a19e4b07f02db605711","contributors":{"authors":[{"text":"Miller, William R.","contributorId":53838,"corporation":false,"usgs":true,"family":"Miller","given":"William","email":"","middleInitial":"R.","affiliations":[],"preferred":false,"id":263567,"contributorType":{"id":1,"text":"Authors"},"rank":1},{"text":"Motooka, Jerry M.","contributorId":36611,"corporation":false,"usgs":true,"family":"Motooka","given":"Jerry","email":"","middleInitial":"M.","affiliations":[],"preferred":false,"id":263566,"contributorType":{"id":1,"text":"Authors"},"rank":2},{"text":"McHugh, John B.","contributorId":64651,"corporation":false,"usgs":true,"family":"McHugh","given":"John B.","affiliations":[],"preferred":false,"id":263568,"contributorType":{"id":1,"text":"Authors"},"rank":3}]}}
,{"id":47631,"text":"wri854009 - 1985 - Altitude and configuration of the water table in the High Plains aquifer in Kansas, 1980","interactions":[],"lastModifiedDate":"2012-02-02T00:10:24","indexId":"wri854009","displayToPublicDate":"1994-01-01T00:00:00","publicationYear":"1985","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":"85-4009","title":"Altitude and configuration of the water table in the High Plains aquifer in Kansas, 1980","docAbstract":"The High Plains aquifer in Kansas is a part of a regional system that extends from South Dakota to Texas. The aquifer in Kansas underlies an area of 31,000 square miles in the western and south-central part of the State. This aquifer is a hydraulically connected assemblage of unconsolidated water-bearing deposits of Tertiary and Quaternary age. Maps published at a scale of 1:500 ,000 show the altitude and configuration of the water table in Kansas during 1980. Ground water moves from higher altitudes in the western part of the high Plains to lower altitudes in the eastern part at an average rate of 10 feet per mile. The up-gradient flexure of water-table contours along some of the valleys indicates that ground water discharges to the streams in those areas. (USGS)","language":"ENGLISH","doi":"10.3133/wri854009","usgsCitation":"Pabst, M.E., and Stullken, L.E., 1985, Altitude and configuration of the water table in the High Plains aquifer in Kansas, 1980: U.S. Geological Survey Water-Resources Investigations Report 85-4009, 1 map : photocopy ; 70 x 90 cm., on sheet 93 x 130 cm., folded to 22 x 22 cm., https://doi.org/10.3133/wri854009.","productDescription":"1 map : photocopy ; 70 x 90 cm., on sheet 93 x 130 cm., folded to 22 x 22 cm.","costCenters":[],"links":[{"id":169948,"rank":0,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/thumbnails/usgs_thumb.jpg"},{"id":84559,"rank":400,"type":{"id":17,"text":"Plate"},"url":"https://pubs.usgs.gov/wri/1985/4009/plate-1.pdf","linkFileType":{"id":1,"text":"pdf"}}],"noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"4f4e4adce4b07f02db6869b2","contributors":{"authors":[{"text":"Pabst, Marilyn E.","contributorId":25566,"corporation":false,"usgs":true,"family":"Pabst","given":"Marilyn","email":"","middleInitial":"E.","affiliations":[],"preferred":false,"id":235926,"contributorType":{"id":1,"text":"Authors"},"rank":1},{"text":"Stullken, Lloyd E.","contributorId":60609,"corporation":false,"usgs":true,"family":"Stullken","given":"Lloyd","email":"","middleInitial":"E.","affiliations":[],"preferred":false,"id":235927,"contributorType":{"id":1,"text":"Authors"},"rank":2}]}}
,{"id":44452,"text":"wri854223 - 1985 - Maps showing altitude of the potentiometric surface and changes in water level of the Sparta sand and Memphis sand aquifers in Eastern Arkansas, spring 1984","interactions":[],"lastModifiedDate":"2023-01-11T22:12:34.260931","indexId":"wri854223","displayToPublicDate":"1994-01-01T00:00:00","publicationYear":"1985","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":"85-4223","title":"Maps showing altitude of the potentiometric surface and changes in water level of the Sparta sand and Memphis sand aquifers in Eastern Arkansas, spring 1984","docAbstract":"<p>No abstract available.</p>","language":"English","publisher":"U.S. Geological Survey","doi":"10.3133/wri854223","usgsCitation":"Edds, J., and Fitzpatrick, D.J., 1985, Maps showing altitude of the potentiometric surface and changes in water level of the Sparta sand and Memphis sand aquifers in Eastern Arkansas, spring 1984: U.S. Geological Survey Water-Resources Investigations Report 85-4223, 1 Plate: 42.34 x 36.73 inches, https://doi.org/10.3133/wri854223.","productDescription":"1 Plate: 42.34 x 36.73 inches","costCenters":[],"links":[{"id":169743,"rank":1,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/thumbnails/usgs_thumb.jpg"},{"id":411751,"rank":3,"type":{"id":36,"text":"NGMDB Index Page"},"url":"https://ngmdb.usgs.gov/Prodesc/proddesc_36370.htm"},{"id":81777,"rank":2,"type":{"id":17,"text":"Plate"},"url":"https://pubs.usgs.gov/wri/1985/4223/plate-1.pdf","linkFileType":{"id":1,"text":"pdf"}}],"country":"United States","state":"Arkansas","otherGeospatial":"Sparta Sand and Memphis Sand aquifers","geographicExtents":"{\n  \"type\": \"FeatureCollection\",\n  \"features\": [\n    {\n      \"type\": \"Feature\",\n      \"properties\": {},\n      \"geometry\": {\n        \"coordinates\": [\n          [\n            [\n              -91.19531829632703,\n              32.980389869575575\n            ],\n            [\n              -91.14779829500537,\n              33.27064745917005\n            ],\n            [\n              -91.233210345451,\n              33.61919543404866\n            ],\n            [\n              -90.7751855375397,\n              34.36276687353285\n            ],\n            [\n              -90.1315710108,\n              35.2080953870105\n            ],\n            [\n              -89.85930607945734,\n              35.58890534894552\n            ],\n            [\n              -89.62948021702829,\n              35.8924267847421\n            ],\n            [\n              -89.64923488521559,\n              36.03010744154139\n            ],\n            [\n              -90.24379748836697,\n              36.02900594885763\n            ],\n            [\n              -89.92840007471217,\n              36.3446893320513\n            ],\n            [\n              -90.06040729879555,\n              36.51927069670744\n            ],\n            [\n              -92.26347695592654,\n              36.5187478937554\n            ],\n            [\n              -92.42507489328582,\n              33.0076778799659\n            ],\n            [\n              -91.19531829632703,\n              32.980389869575575\n            ]\n          ]\n        ],\n        \"type\": \"Polygon\"\n      }\n    }\n  ]\n}","noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"4f4e4a17e4b07f02db60461a","contributors":{"authors":[{"text":"Edds, Joe","contributorId":48532,"corporation":false,"usgs":true,"family":"Edds","given":"Joe","email":"","affiliations":[],"preferred":false,"id":229792,"contributorType":{"id":1,"text":"Authors"},"rank":1},{"text":"Fitzpatrick, Daniel J.","contributorId":31367,"corporation":false,"usgs":true,"family":"Fitzpatrick","given":"Daniel","email":"","middleInitial":"J.","affiliations":[],"preferred":false,"id":229791,"contributorType":{"id":1,"text":"Authors"},"rank":2}]}}
,{"id":48859,"text":"ofr84145B - 1985 - Streamflow statistics and drainage-basin characteristics for the Southwestern and Eastern Regions, Washington: Volume II. Eastern Washington","interactions":[],"lastModifiedDate":"2021-10-28T19:11:25.560714","indexId":"ofr84145B","displayToPublicDate":"1994-01-01T00:00:00","publicationYear":"1985","noYear":false,"publicationType":{"id":18,"text":"Report"},"publicationSubtype":{"id":5,"text":"USGS Numbered Series"},"seriesTitle":{"id":330,"text":"Open-File Report","code":"OFR","onlineIssn":"2331-1258","printIssn":"0196-1497","active":true,"publicationSubtype":{"id":5}},"seriesNumber":"84-145","chapter":"B","title":"Streamflow statistics and drainage-basin characteristics for the Southwestern and Eastern Regions, Washington: Volume II. Eastern Washington","docAbstract":"<p>No abstract available.</p>","language":"English","publisher":"U.S. Geological Survey","doi":"10.3133/ofr84145B","usgsCitation":"Williams, J.R., and Pearson, H.E., 1985, Streamflow statistics and drainage-basin characteristics for the Southwestern and Eastern Regions, Washington: Volume II. Eastern Washington: U.S. Geological Survey Open-File Report 84-145, Report: 662 p.; 1 Plate: 32.03 × 36.42 inches, https://doi.org/10.3133/ofr84145B.","productDescription":"Report: 662 p.; 1 Plate: 32.03 × 36.42 inches","costCenters":[],"links":[{"id":391100,"rank":4,"type":{"id":36,"text":"NGMDB Index Page"},"url":"https://ngmdb.usgs.gov/Prodesc/proddesc_13292.htm"},{"id":85683,"rank":300,"type":{"id":11,"text":"Document"},"url":"https://pubs.usgs.gov/of/1984/0145b/report.pdf","linkFileType":{"id":1,"text":"pdf"}},{"id":85682,"rank":400,"type":{"id":17,"text":"Plate"},"url":"https://pubs.usgs.gov/of/1984/0145b/plate-1.pdf","linkFileType":{"id":1,"text":"pdf"}},{"id":170006,"rank":0,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/of/1984/0145b/report-thumb.jpg"}],"country":"United States","state":"Washington","geographicExtents":"{\n  \"type\": \"FeatureCollection\",\n  \"features\": [\n    {\n      \"type\": \"Feature\",\n      \"properties\": {},\n      \"geometry\": {\n        \"type\": \"Polygon\",\n        \"coordinates\": [\n          [\n            [\n              -121.493,\n              45.643\n            ],\n            [\n              -116.903,\n              45.643\n            ],\n            [\n              -116.903,\n              49\n            ],\n            [\n              -121.493,\n              49\n            ],\n            [\n              -121.493,\n              45.643\n            ]\n          ]\n        ]\n      }\n    }\n  ]\n}","noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"4f4e4b15e4b07f02db6a4d3b","contributors":{"authors":[{"text":"Williams, John R.","contributorId":107260,"corporation":false,"usgs":true,"family":"Williams","given":"John","email":"","middleInitial":"R.","affiliations":[{"id":595,"text":"U.S. Geological Survey","active":false,"usgs":true}],"preferred":false,"id":238447,"contributorType":{"id":1,"text":"Authors"},"rank":1},{"text":"Pearson, Harold E.","contributorId":18046,"corporation":false,"usgs":true,"family":"Pearson","given":"Harold","email":"","middleInitial":"E.","affiliations":[],"preferred":false,"id":238446,"contributorType":{"id":1,"text":"Authors"},"rank":2}]}}
,{"id":44480,"text":"wri844360 - 1985 - Ground-water levels in the Columbia River basalt and overlying materials, spring 1983, southeastern Washington","interactions":[],"lastModifiedDate":"2022-05-19T18:40:18.783766","indexId":"wri844360","displayToPublicDate":"1994-01-01T00:00:00","publicationYear":"1985","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":"84-4360","title":"Ground-water levels in the Columbia River basalt and overlying materials, spring 1983, southeastern Washington","docAbstract":"A 2 1/2-year study of the Columbia Plateau in Washington was begun in March 1982 to define spatial and temporal variations in dissolved sodium in aquifers of the Columbia River Basalt Group and to relate these variations to the groundwater system and its geologic framework. This report is part of that study and describes groundwater level contours for four major geohydrologic units in southeastern Washington, constructed from water-level data collected from approximately 1,100 wells during the spring of 1983, data from U.S. Geological Survey studies in the area, and other indirect methods. Configuration of the groundwater level contours is controlled by: (1) extent of a geohydrologic unit and geologic structure, (2) recharge from precipitation and surface water bodies, (3) rivers, lakes, and coulees that drain the groundwater system, and (4) hydraulic conductivities of each unit. Upgradient flexures of water level contours north of Connel, Washington, show effects of prolonged irrigation while downgradient flexures in an area south of Potholes Reservoir, in the vicinity of the East Low Irrigation Canal, show the effects of increased man-induced recharge. (USGS)","language":"English","publisher":"U.S. Geological Survey","doi":"10.3133/wri844360","usgsCitation":"Bauer, H.H., Vaccaro, J.J., and Lane, R.C., 1985, Ground-water levels in the Columbia River basalt and overlying materials, spring 1983, southeastern Washington: U.S. Geological Survey Water-Resources Investigations Report 84-4360, 4 Plates: 44.10 × 29.00 inches or smaller, https://doi.org/10.3133/wri844360.","productDescription":"4 Plates: 44.10 × 29.00 inches or smaller","costCenters":[],"links":[{"id":134642,"rank":0,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/thumbnails/usgs_thumb.jpg"},{"id":400826,"rank":6,"type":{"id":36,"text":"NGMDB Index Page"},"url":"https://ngmdb.usgs.gov/Prodesc/proddesc_36191.htm"},{"id":81838,"rank":403,"type":{"id":17,"text":"Plate"},"url":"https://pubs.usgs.gov/wri/1984/4360/plate-4.pdf","linkFileType":{"id":1,"text":"pdf"}},{"id":81837,"rank":402,"type":{"id":17,"text":"Plate"},"url":"https://pubs.usgs.gov/wri/1984/4360/plate-3.pdf","linkFileType":{"id":1,"text":"pdf"}},{"id":81836,"rank":401,"type":{"id":17,"text":"Plate"},"url":"https://pubs.usgs.gov/wri/1984/4360/plate-2.pdf","linkFileType":{"id":1,"text":"pdf"}},{"id":81835,"rank":400,"type":{"id":17,"text":"Plate"},"url":"https://pubs.usgs.gov/wri/1984/4360/plate-1.pdf","linkFileType":{"id":1,"text":"pdf"}}],"scale":"500000","country":"United States","state":"Washington","otherGeospatial":"Columbia River basalt","geographicExtents":"{\n  \"type\": \"FeatureCollection\",\n  \"features\": [\n    {\n      \"type\": \"Feature\",\n      \"properties\": {},\n      \"geometry\": {\n        \"type\": \"Polygon\",\n        \"coordinates\": [\n          [\n            [\n              -121,\n              45.603\n            ],\n            [\n              -116.903,\n              45.603\n            ],\n            [\n              -116.903,\n              48.2440\n            ],\n            [\n              -121,\n              48.2440\n            ],\n            [\n              -121,\n              45.603\n            ]\n          ]\n        ]\n      }\n    }\n  ]\n}","noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"4f4e4b13e4b07f02db6a384e","contributors":{"authors":[{"text":"Bauer, H. H.","contributorId":85142,"corporation":false,"usgs":true,"family":"Bauer","given":"H.","email":"","middleInitial":"H.","affiliations":[],"preferred":false,"id":229850,"contributorType":{"id":1,"text":"Authors"},"rank":1},{"text":"Vaccaro, John J. jvaccaro@usgs.gov","contributorId":5848,"corporation":false,"usgs":true,"family":"Vaccaro","given":"John","email":"jvaccaro@usgs.gov","middleInitial":"J.","affiliations":[{"id":622,"text":"Washington Water Science Center","active":true,"usgs":true}],"preferred":true,"id":229848,"contributorType":{"id":1,"text":"Authors"},"rank":2},{"text":"Lane, R. C.","contributorId":6421,"corporation":false,"usgs":true,"family":"Lane","given":"R.","email":"","middleInitial":"C.","affiliations":[],"preferred":false,"id":229849,"contributorType":{"id":1,"text":"Authors"},"rank":3}]}}
,{"id":44482,"text":"wri844364 - 1985 - Approximate potentiometric surface for the aquifer unit A4, southeastern coastal plain aquifer system of the United States, prior to development","interactions":[],"lastModifiedDate":"2012-02-02T00:04:55","indexId":"wri844364","displayToPublicDate":"1994-01-01T00:00:00","publicationYear":"1985","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":"84-4364","title":"Approximate potentiometric surface for the aquifer unit A4, southeastern coastal plain aquifer system of the United States, prior to development","docAbstract":"A generalized potentiometric surface map prepared as part of a regional analysis of sand aquifer system defines the altitude of water levels under pre-development conditions for aquifer unit A4, the lowermost group of aquifers in the sand aquifer system. Aquifer unit A4, consisting of Upper and Lower Cretaceous sands, is under artesian conditions except locally in the recharge areas. The regional flow direction is to the rivers in the area where the unit outcrops and southward to the Gulf of Mexico in Mississippi, Alabama, and West Georgia. In coastal Georgia and South Carolina, the direction of flow is east northeast parallel to the coast and into North Carolina. (USGS)","language":"ENGLISH","doi":"10.3133/wri844364","usgsCitation":"Stricker, V., Aucott, W.R., Faye, R.E., Williams, J.S., and Mallory, M.J., 1985, Approximate potentiometric surface for the aquifer unit A4, southeastern coastal plain aquifer system of the United States, prior to development: U.S. Geological Survey Water-Resources Investigations Report 84-4364, 1 map : col. ; 35 x 60 cm., on sheet 58 x 72 cm. , https://doi.org/10.3133/wri844364.","productDescription":"1 map : col. ; 35 x 60 cm., on sheet 58 x 72 cm. ","costCenters":[],"links":[{"id":134644,"rank":0,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/thumbnails/usgs_thumb.jpg"},{"id":81840,"rank":400,"type":{"id":17,"text":"Plate"},"url":"https://pubs.usgs.gov/wri/1984/4364/plate-1.pdf","linkFileType":{"id":1,"text":"pdf"}}],"noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"4f4e4ac6e4b07f02db67a1ba","contributors":{"authors":[{"text":"Stricker, V.A.","contributorId":78703,"corporation":false,"usgs":true,"family":"Stricker","given":"V.A.","email":"","affiliations":[],"preferred":false,"id":229854,"contributorType":{"id":1,"text":"Authors"},"rank":1},{"text":"Aucott, Walter R.","contributorId":90275,"corporation":false,"usgs":true,"family":"Aucott","given":"Walter","email":"","middleInitial":"R.","affiliations":[],"preferred":false,"id":229855,"contributorType":{"id":1,"text":"Authors"},"rank":2},{"text":"Faye, Robert E.","contributorId":92221,"corporation":false,"usgs":true,"family":"Faye","given":"Robert","email":"","middleInitial":"E.","affiliations":[],"preferred":false,"id":229856,"contributorType":{"id":1,"text":"Authors"},"rank":3},{"text":"Williams, John S. johnw@usgs.gov","contributorId":329,"corporation":false,"usgs":true,"family":"Williams","given":"John","email":"johnw@usgs.gov","middleInitial":"S.","affiliations":[],"preferred":true,"id":229852,"contributorType":{"id":1,"text":"Authors"},"rank":4},{"text":"Mallory, Michael J.","contributorId":59408,"corporation":false,"usgs":true,"family":"Mallory","given":"Michael","email":"","middleInitial":"J.","affiliations":[],"preferred":false,"id":229853,"contributorType":{"id":1,"text":"Authors"},"rank":5}]}}
,{"id":44485,"text":"wri854019 - 1985 - Approximate potentiometric surface for the aquifer unit A2, Southeastern Coastal Plain aquifer system of the United States, prior to development","interactions":[],"lastModifiedDate":"2012-02-02T00:04:55","indexId":"wri854019","displayToPublicDate":"1994-01-01T00:00:00","publicationYear":"1985","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":"85-4019","title":"Approximate potentiometric surface for the aquifer unit A2, Southeastern Coastal Plain aquifer system of the United States, prior to development","docAbstract":"A generalized potentiometric surface map prepared as part of the southeastern United States, Regional Sand Aquifer-System Analysis defines the altitude of water levels under conditions prior to development for aquifer unit A2, the upper group of aquifers in the sand aquifer system. Aquifer unit A2, consisting of lower Tertiary sands, is under artesian conditions except locally in the recharge areas. The regional flow direction is to the rivers in the area where the unit outcrops, west toward the Mississippi River in Mississippi, and southward to the Gulf of Mexico in Alabama and West Georgia. In eastern Georgia and South Carolina, the flow is southeast toward the Atlantic Ocean. (USGS)","language":"ENGLISH","doi":"10.3133/wri854019","usgsCitation":"Stricker, V., 1985, Approximate potentiometric surface for the aquifer unit A2, Southeastern Coastal Plain aquifer system of the United States, prior to development: U.S. Geological Survey Water-Resources Investigations Report 85-4019, 1 map : col ; 35 x 60 cm., on sheet 58 x 72 cm., https://doi.org/10.3133/wri854019.","productDescription":"1 map : col ; 35 x 60 cm., on sheet 58 x 72 cm.","costCenters":[],"links":[{"id":134665,"rank":0,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/wri/1985/4019/report-thumb.jpg"},{"id":81845,"rank":300,"type":{"id":11,"text":"Document"},"url":"https://pubs.usgs.gov/wri/1985/4019/report.pdf","linkFileType":{"id":1,"text":"pdf"}}],"noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"4f4e4ac6e4b07f02db67a1ac","contributors":{"authors":[{"text":"Stricker, V.A.","contributorId":78703,"corporation":false,"usgs":true,"family":"Stricker","given":"V.A.","email":"","affiliations":[],"preferred":false,"id":229860,"contributorType":{"id":1,"text":"Authors"},"rank":1}]}}
,{"id":56211,"text":"wdrNY841 - 1985 - Water resources data, New York, water year 1984, volume 1, eastern New York, excluding Long Island","interactions":[],"lastModifiedDate":"2019-05-14T10:42:05","indexId":"wdrNY841","displayToPublicDate":"1994-01-01T00:00:00","publicationYear":"1985","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-84-1","title":"Water resources data, New York, water year 1984, volume 1, eastern New York, excluding Long Island","docAbstract":"<p>Water resources for the 1984 water year for New York consist of records of stage, discharge, and water quality of streams; stage, discharge, and water quality of lakes and reservoirs; quality of precipitation, and water levels and quality of water in wells. This volume contains records of water discharge at 96 gaging stations; stage only at 5 gaging stations; and stage and contents at 4 gaging stations and 19 lakes and reservoirs; water quality at 34 gaging stations and 3 precipitation stations, and water levels at 24 observation wells. Locations of these sites are shown on figures 4A and 4B. Also included are data for 66 creststage partial-record stations. Additional water data were collected at various sites not in the systematic data-collection program and are published as miscellaneous measurements. These data together with the data in volumes 2 and 3 represent that part of the national water system collected by the U.S. Geological Survey and cooperating State and Federal agencies in New York. </p>","language":"English","publisher":"U.S. Geological Survey","doi":"10.3133/wdrNY841","collaboration":"Prepared in cooperation with the State of New York and with other agencies","usgsCitation":"Firda, G.D., Lumia, R., Archer, R.J., and Burke, P.M., 1985, Water resources data, New York, water year 1984, volume 1, eastern New York, excluding Long Island: U.S. Geological Survey Water Data Report NY-84-1, viii, 249 p., https://doi.org/10.3133/wdrNY841.","productDescription":"viii, 249 p.","costCenters":[],"links":[{"id":174929,"rank":0,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/wdr/1984/ny-84-1/report-thumb.jpg"},{"id":363750,"rank":2,"type":{"id":11,"text":"Document"},"url":"https://pubs.usgs.gov/wdr/1984/ny-84-1/report.pdf","linkFileType":{"id":1,"text":"pdf"}}],"country":"United States","state":"New York","geographicExtents":"{\n  \"type\": \"FeatureCollection\",\n  \"features\": [\n    {\n      \"type\": \"Feature\",\n      \"properties\": {},\n      \"geometry\": {\n        \"type\": \"Polygon\",\n        \"coordinates\": [\n          [\n            [\n              -76.25,\n              41\n            ],\n            [\n              -73.1,\n              41\n            ],\n            [\n              -73.1,\n              45\n            ],\n            [\n              -76.25,\n              45\n            ],\n            [\n              -76.25,\n              41\n            ]\n          ]\n        ]\n      }\n    }\n  ]\n}","noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"4f4e49f5e4b07f02db5f0df3","contributors":{"authors":[{"text":"Firda, Gary D. gfirda@usgs.gov","contributorId":1552,"corporation":false,"usgs":true,"family":"Firda","given":"Gary","email":"gfirda@usgs.gov","middleInitial":"D.","affiliations":[],"preferred":true,"id":254949,"contributorType":{"id":1,"text":"Authors"},"rank":1},{"text":"Lumia, Richard rlumia@usgs.gov","contributorId":4579,"corporation":false,"usgs":true,"family":"Lumia","given":"Richard","email":"rlumia@usgs.gov","affiliations":[],"preferred":true,"id":254946,"contributorType":{"id":1,"text":"Authors"},"rank":2},{"text":"Archer, Roger J.","contributorId":108106,"corporation":false,"usgs":true,"family":"Archer","given":"Roger","email":"","middleInitial":"J.","affiliations":[],"preferred":false,"id":254948,"contributorType":{"id":1,"text":"Authors"},"rank":3},{"text":"Burke, P. M.","contributorId":8478,"corporation":false,"usgs":true,"family":"Burke","given":"P.","email":"","middleInitial":"M.","affiliations":[],"preferred":false,"id":254947,"contributorType":{"id":1,"text":"Authors"},"rank":4}]}}
,{"id":44487,"text":"wri854031 - 1985 - Approximate potentiometric surface for the aquifer unit A3, southeastern coastal plain aquifer system of the United States, prior to development","interactions":[],"lastModifiedDate":"2012-02-02T00:04:57","indexId":"wri854031","displayToPublicDate":"1994-01-01T00:00:00","publicationYear":"1985","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":"85-4031","title":"Approximate potentiometric surface for the aquifer unit A3, southeastern coastal plain aquifer system of the United States, prior to development","docAbstract":"A generalized potentiometric surface map prepared as part of the southeastern United States, Regional Sand Aquifer-System Analysis defines the altitude of water levels under conditions prior to development for aquifer unit A3, the middle group of aquifers in the sand aquifer system. Aquifer unit A3, consisting of Upper Cretaceous and Tertiary sands, is under artesian conditions except locally in the recharge areas. The regional flow direction is to the rivers in the area where the unit outcrops, west toward the Mississippi River in Mississippi, and southward to the Gulf of Mexico in Alabama and West Georgia. In eastern Georgia, the flow is southeast toward the Atlantic Ocean , and in South Carolina, the direction of flow is southeast toward the Pee Dee River. (USGS)","language":"ENGLISH","doi":"10.3133/wri854031","usgsCitation":"Stricker, V., 1985, Approximate potentiometric surface for the aquifer unit A3, southeastern coastal plain aquifer system of the United States, prior to development: U.S. Geological Survey Water-Resources Investigations Report 85-4031, 1 map : col. ; 35 x 60 cm., on sheet 58 x 72 cm., https://doi.org/10.3133/wri854031.","productDescription":"1 map : col. ; 35 x 60 cm., on sheet 58 x 72 cm.","costCenters":[],"links":[{"id":134698,"rank":0,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/wri/1985/4031/report-thumb.jpg"},{"id":81846,"rank":300,"type":{"id":11,"text":"Document"},"url":"https://pubs.usgs.gov/wri/1985/4031/report.pdf","linkFileType":{"id":1,"text":"pdf"}}],"noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"4f4e4ac6e4b07f02db67a1b3","contributors":{"authors":[{"text":"Stricker, V.A.","contributorId":78703,"corporation":false,"usgs":true,"family":"Stricker","given":"V.A.","email":"","affiliations":[],"preferred":false,"id":229862,"contributorType":{"id":1,"text":"Authors"},"rank":1}]}}
,{"id":56288,"text":"wdrWA822 - 1985 - Water resources data, Washington, water year 1982: Vol. 2. Eastern Washington","interactions":[],"lastModifiedDate":"2022-12-14T20:24:54.536411","indexId":"wdrWA822","displayToPublicDate":"1994-01-01T00:00:00","publicationYear":"1985","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":"WA-82-2","title":"Water resources data, Washington, water year 1982: Vol. 2. Eastern Washington","docAbstract":"<p>Water resources data for the 1982 water year for Washington consist of records of stage, discharge, and water quality of streams; stage, contents, and water quality of lakes and reservoirs; and water levels and water quality of wells and springs. This report, in two volumes, contains discharge records for 253 gaging stations; stage only records for 8 gaging stations; stage and contents for 37 lakes and reservoirs; water quality for 81 gaging stations; and water levels for 57 observation wells. Also included are data for 33 crest-stage partial-record stations. Locations of these sites are shown on figures 4, 5, and 19. Additional water data were collected at various sites, not part of the systematic data collection program, and are published as miscellaneous measurements and analyses. These data represent that part of the National Water Data System operated by the U.S. Geological Survey and cooperating State and Federal agencies in Washington.</p>","language":"English","publisher":"U.S. Geological Survey","doi":"10.3133/wdrWA822","collaboration":"Prepared in cooperation with the State of Washington and with other agencies","usgsCitation":"Water Resources Division, U.S. Geological Survey, 1985, Water resources data, Washington, water year 1982: Vol. 2. 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 \"}}]}","noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"4f4e49f5e4b07f02db5f0ae4","contributors":{"authors":[{"text":"Water Resources Division, U.S. Geological Survey","contributorId":128075,"corporation":true,"usgs":false,"organization":"Water Resources Division, U.S. Geological Survey","id":532479,"contributorType":{"id":1,"text":"Authors"},"rank":1}]}}
,{"id":47716,"text":"wri854112 - 1985 - Maps of the Bonsall area of the San Luis Rey River valley, San Diego County, California, showing geology, hydrology, and ground-water quality","interactions":[],"lastModifiedDate":"2015-09-24T15:20:56","indexId":"wri854112","displayToPublicDate":"1994-01-01T00:00:00","publicationYear":"1985","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":"85-4112","title":"Maps of the Bonsall area of the San Luis Rey River valley, San Diego County, California, showing geology, hydrology, and ground-water quality","docAbstract":"<p>In November 1984, 84 wells and 1 spring in the Bonsall area of the San Luis Rey River valley were inventoried by U.S. Geological Survey personnel. Depth to water in 38 wells ranged from 1.3 to 38 ft and 23 wells had depths to water less than 10 feet. Dissolved solids concentration of water from 29 wells and 1 spring sampled in autumn 1983 and spring 1984 ranged from 574 to 2,370 mgs/L. Groundwater with a dissolved solids concentration less than 1,000 mgs/L was generally restricted to the eastern part of the aquifer. The total volume of alluvial fill in the Bonsall area is 113,000 acre-feet; the amount of groundwater storage available in the alluvial aquifer is 18,000 acre-feet. The alluvial aquifer is, in part, surrounded and underlain by colluvium and weathered crystalline rock that add some additional groundwater storage capacity to the system. Data in this report are presented on five maps showing well locations , thickness of alluvial fill, water level contours in November 1983 and hydrographs of selected wells, groundwater quality in spring 1960 and graphs showing changes in dissolved solids concentrations of water from selected wells with time, and groundwater quality in spring 1984. This report is part of a larger cooperative project between the Rainbow Municipal Irrigation District and the U.S. Geological Survey. The purpose of the larger project is to develop an appropriate groundwater management plan for the Bonsall area of the San Luis Rey River valley. (USGS)</p>","language":"English","publisher":"U.S. Geological Survey","doi":"10.3133/wri854112","usgsCitation":"Izbicki, J., 1985, Maps of the Bonsall area of the San Luis Rey River valley, San Diego County, California, showing geology, hydrology, and ground-water quality: U.S. Geological Survey Water-Resources Investigations Report 85-4112, 5 Plates: 27.66 x 29.98 inches or smaller, https://doi.org/10.3133/wri854112.","productDescription":"5 Plates: 27.66 x 29.98 inches or smaller","onlineOnly":"N","additionalOnlineFiles":"N","costCenters":[],"links":[{"id":308562,"rank":301,"type":{"id":17,"text":"Plate"},"url":"https://pubs.usgs.gov/wri/1985/4112/plate-2.pdf","text":"Plate 2","size":"17,543 KB","linkFileType":{"id":1,"text":"pdf"}},{"id":84625,"rank":300,"type":{"id":17,"text":"Plate"},"url":"https://pubs.usgs.gov/wri/1985/4112/plate-1.pdf","text":"Plate 1","size":"16,080 KB","linkFileType":{"id":1,"text":"pdf"}},{"id":169426,"rank":0,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/wri/1985/4112/report-thumb.jpg"},{"id":308563,"rank":302,"type":{"id":17,"text":"Plate"},"url":"https://pubs.usgs.gov/wri/1985/4112/plate-3.pdf","text":"Plate 3","size":"16,194 KB","linkFileType":{"id":1,"text":"pdf"}},{"id":308564,"rank":303,"type":{"id":17,"text":"Plate"},"url":"https://pubs.usgs.gov/wri/1985/4112/plate-4.pdf","text":"Plate 4","size":"17,766 KB","linkFileType":{"id":1,"text":"pdf"}},{"id":308565,"rank":304,"type":{"id":17,"text":"Plate"},"url":"https://pubs.usgs.gov/wri/1985/4112/plate-5.pdf","text":"Plate 5","size":"15,405 KB","linkFileType":{"id":1,"text":"pdf"}}],"country":"United States","state":"California","county":"San Diego County","otherGeospatial":"San Luis Rey River Valley","geographicExtents":"{\n  \"type\": \"FeatureCollection\",\n  \"features\": [\n    {\n      \"type\": \"Feature\",\n      \"properties\": {},\n      \"geometry\": {\n        \"type\": \"Polygon\",\n        \"coordinates\": [\n          [\n            [\n              -117.32437133789061,\n              33.10879798900969\n            ],\n            [\n              -117.32437133789061,\n              33.415967956844625\n            ],\n            [\n              -116.96113586425781,\n              33.415967956844625\n            ],\n            [\n              -116.96113586425781,\n              33.10879798900969\n            ],\n            [\n              -117.32437133789061,\n              33.10879798900969\n            ]\n          ]\n        ]\n      }\n    }\n  ]\n}","noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"4f4e4a0be4b07f02db5fc199","contributors":{"authors":[{"text":"Izbicki, John A. 0000-0003-0816-4408 jaizbick@usgs.gov","orcid":"https://orcid.org/0000-0003-0816-4408","contributorId":1375,"corporation":false,"usgs":true,"family":"Izbicki","given":"John A.","email":"jaizbick@usgs.gov","affiliations":[{"id":595,"text":"U.S. Geological Survey","active":false,"usgs":true}],"preferred":false,"id":236066,"contributorType":{"id":1,"text":"Authors"},"rank":1}]}}
,{"id":43032,"text":"ofr85167 - 1985 - Solute distribution in waters in the Snake River basin, Idaho and eastern Oregon","interactions":[{"subject":{"id":43032,"text":"ofr85167 - 1985 - Solute distribution in waters in the Snake River basin, Idaho and eastern Oregon","indexId":"ofr85167","publicationYear":"1985","noYear":false,"title":"Solute distribution in waters in the Snake River basin, Idaho and eastern Oregon"},"predicate":"SUPERSEDED_BY","object":{"id":68212,"text":"ha696 - 1987 - Solute distribution in ground and surface water in the Snake River Basin, Idaho and eastern Oregon","indexId":"ha696","publicationYear":"1987","noYear":false,"title":"Solute distribution in ground and surface water in the Snake River Basin, Idaho and eastern Oregon"},"id":1}],"supersededBy":{"id":68212,"text":"ha696 - 1987 - Solute distribution in ground and surface water in the Snake River Basin, Idaho and eastern Oregon","indexId":"ha696","publicationYear":"1987","noYear":false,"title":"Solute distribution in ground and surface water in the Snake River Basin, Idaho and eastern Oregon"},"lastModifiedDate":"2025-02-04T15:55:07.925962","indexId":"ofr85167","displayToPublicDate":"1994-01-01T00:00:00","publicationYear":"1985","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":"85-167","title":"Solute distribution in waters in the Snake River basin, Idaho and eastern Oregon","docAbstract":"<p>No abstract available.</p>","language":"English","publisher":"U.S. Geological Survey","doi":"10.3133/ofr85167","usgsCitation":"Low, W.H., 1985, Solute distribution in waters in the Snake River basin, Idaho and eastern Oregon: U.S. Geological Survey Open-File Report 85-167, 2 Sheets: 42.66 x 30.31 inches and 42.92 x 30.19 inches, https://doi.org/10.3133/ofr85167.","productDescription":"2 Sheets: 42.66 x 30.31 inches and 42.92 x 30.19 inches","costCenters":[],"links":[{"id":481664,"rank":2,"type":{"id":26,"text":"Sheet"},"url":"https://pubs.usgs.gov/of/1985/0167/sheet-1.pdf","text":"Sheet 1","linkFileType":{"id":1,"text":"pdf"}},{"id":481665,"rank":3,"type":{"id":26,"text":"Sheet"},"url":"https://pubs.usgs.gov/of/1985/0167/sheet-2.pdf","text":"Sheet 2","linkFileType":{"id":1,"text":"pdf"}},{"id":168474,"rank":1,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/of/1985/0167/report-thumb.jpg"}],"scale":"1000000","country":"United States","state":"Idaho, Oregon","otherGeospatial":"Snake River basin","geographicExtents":"{\n  \"type\": \"FeatureCollection\",\n  \"features\": [\n    {\n      \"type\": \"Feature\",\n      \"properties\": {},\n      \"geometry\": {\n        \"coordinates\": [\n          [\n            [\n              -124.44350530951343,\n              41.74876201297755\n            ],\n            [\n              -110.8748692680008,\n              41.81930230694928\n            ],\n            [\n              -110.9301365737104,\n              45.07345829172931\n            ],\n            [\n              -113.29828921312526,\n              45.01875982801852\n            ],\n            [\n              -114.23963602535332,\n              46.71316881650611\n            ],\n            [\n              -115.95601520351389,\n              49.158009080006195\n            ],\n            [\n              -117.23470852348288,\n              49.145436784766815\n            ],\n            [\n              -117.20750742851405,\n              46.17318965549089\n            ],\n            [\n              -124.31611684872718,\n              46.261807874145376\n            ],\n            [\n              -124.47999791747452,\n              41.82080483009614\n            ],\n            [\n              -124.44350530951343,\n              41.74876201297755\n            ]\n          ]\n        ],\n        \"type\": \"Polygon\"\n      }\n    }\n  ]\n}","noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"4f4e49efe4b07f02db5eda34","contributors":{"authors":[{"text":"Low, Walton H.","contributorId":92672,"corporation":false,"usgs":true,"family":"Low","given":"Walton","email":"","middleInitial":"H.","affiliations":[],"preferred":false,"id":227605,"contributorType":{"id":1,"text":"Authors"},"rank":1}]}}
,{"id":57327,"text":"wdrVA841 - 1985 - Water resources data for Virginia, water year 1984","interactions":[],"lastModifiedDate":"2020-12-07T20:21:22.386101","indexId":"wdrVA841","displayToPublicDate":"1994-01-01T00:00:00","publicationYear":"1985","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":"VA-84-1","title":"Water resources data for Virginia, water year 1984","docAbstract":"<p>No abstract available.</p>","language":"English","publisher":"U.S. Geological Survey","publisherLocation":"Reston, VA","doi":"10.3133/wdrVA841","usgsCitation":"Prugh, B., Easton, F., and Lynch, D.D., 1985, Water resources data for Virginia, water year 1984: U.S. Geological Survey Water Data Report VA-84-1, xi, 405 p., https://doi.org/10.3133/wdrVA841.","productDescription":"xi, 405 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