{"pageNumber":"358","pageRowStart":"8925","pageSize":"25","recordCount":10959,"records":[{"id":7127,"text":"ofr811115 - 1982 - An evaluation of water-quality monitoring in the Brandywine Creek basin, Pennsylvania, 1973-78","interactions":[],"lastModifiedDate":"2017-06-20T10:02:13","indexId":"ofr811115","displayToPublicDate":"1994-01-01T00:00:00","publicationYear":"1982","noYear":false,"publicationType":{"id":18,"text":"Report"},"publicationSubtype":{"id":5,"text":"USGS Numbered Series"},"seriesTitle":{"id":330,"text":"Open-File Report","code":"OFR","onlineIssn":"2331-1258","printIssn":"0196-1497","active":true,"publicationSubtype":{"id":5}},"seriesNumber":"81-1115","title":"An evaluation of water-quality monitoring in the Brandywine Creek basin, Pennsylvania, 1973-78","docAbstract":"Data recorded from 1973 through 1978 by monitors on West Branch Brandywine Creek at Modena, East Branch Brandywine Creek below Downingtown, and Brandywine Creek at Chadds Ford were analyzed to evaluate the effectiveness of the monitors in describing water-quality conditions. The data show that the stream at Modena and below Downingtown had periods of low dissolved oxygen, and that the stream below Downingtown had a particularly severe dissolved-oxygen deficiency from May through September 1974. The pH at all three sites exceeded 9.0 at times and the pH below Downingtown occasionally dropped below 6.0. The most critical period in the basin was from March to November when pH was most likely to exceed water-quality standards and dissolved oxygen was most likely to fall below the standards. Without the monitors, the extent and magnitude of these problems would not have been detected.","language":"English","publisher":"U.S. Geological Survey","publisherLocation":"Harrisburg, PA","doi":"10.3133/ofr811115","usgsCitation":"Murphy, J., Ritter, J., Brown, A., and Chiarella, J., 1982, An evaluation of water-quality monitoring in the Brandywine Creek basin, Pennsylvania, 1973-78: U.S. Geological Survey Open-File Report 81-1115, iv, 28 p., https://doi.org/10.3133/ofr811115.","productDescription":"iv, 28 p.","additionalOnlineFiles":"N","costCenters":[{"id":532,"text":"Pennsylvania Water Science Center","active":true,"usgs":true}],"links":[{"id":141561,"rank":0,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/of/1981/1115/report-thumb.jpg"},{"id":277911,"type":{"id":11,"text":"Document"},"url":"https://pubs.usgs.gov/of/1981/1115/report.pdf"}],"country":"United States","state":"Pennsylvania","geographicExtents":"{ \"type\": \"FeatureCollection\", \"features\": [ { \"type\": \"Feature\", \"properties\": {}, \"geometry\": { \"type\": \"Polygon\", \"coordinates\": [ [ [ -76.0000,39.7283 ], [ -76.0000,40.1250 ], [ -75.2563,40.1250 ], [ -75.2563,39.7283 ], [ -76.0000,39.7283 ] ] ] } } ] }","noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"4f4e4ad8e4b07f02db68484c","contributors":{"authors":[{"text":"Murphy, J.J.","contributorId":69144,"corporation":false,"usgs":true,"family":"Murphy","given":"J.J.","email":"","affiliations":[],"preferred":false,"id":154391,"contributorType":{"id":1,"text":"Authors"},"rank":1},{"text":"Ritter, J.R.","contributorId":22350,"corporation":false,"usgs":true,"family":"Ritter","given":"J.R.","email":"","affiliations":[],"preferred":false,"id":154389,"contributorType":{"id":1,"text":"Authors"},"rank":2},{"text":"Brown, A.E.","contributorId":48557,"corporation":false,"usgs":true,"family":"Brown","given":"A.E.","email":"","affiliations":[],"preferred":false,"id":154390,"contributorType":{"id":1,"text":"Authors"},"rank":3},{"text":"Chiarella, J.P.","contributorId":17603,"corporation":false,"usgs":true,"family":"Chiarella","given":"J.P.","email":"","affiliations":[],"preferred":false,"id":154388,"contributorType":{"id":1,"text":"Authors"},"rank":4}]}}
,{"id":7214,"text":"ofr82242 - 1982 - Gulf of Mexico summary report 3 August 1982: A revision of Outer Continental Shelf oil and gas activities in the Gulf of Mexico and their onshore impacts: Gulf of Mexico summary report 2, August 1981","interactions":[],"lastModifiedDate":"2022-11-16T19:34:34.998977","indexId":"ofr82242","displayToPublicDate":"1994-01-01T00:00:00","publicationYear":"1982","noYear":false,"publicationType":{"id":18,"text":"Report"},"publicationSubtype":{"id":5,"text":"USGS Numbered Series"},"seriesTitle":{"id":330,"text":"Open-File Report","code":"OFR","onlineIssn":"2331-1258","printIssn":"0196-1497","active":true,"publicationSubtype":{"id":5}},"seriesNumber":"82-242","title":"Gulf of Mexico summary report 3 August 1982: A revision of Outer Continental Shelf oil and gas activities in the Gulf of Mexico and their onshore impacts: Gulf of Mexico summary report 2, August 1981","docAbstract":"<p>Now, and for the near future, the Gulf of Mexico will remain the most developed Outer Continental Shelf (OCS) region in the United States and the world. Virtually all production from the U.S. OCS emanates from the Gulf of Mexico. In calendar year 1981, for the two primary categories of hydrocarbons produced from the OCS, oil/condensate and gas, Gulf production accounted for over 94 and 99 percent, respectively. Oil production for 1981 was 0.27 billion barrels, and gas production was 4.84 trillion cubic feet. Although most of the shallow-water areas of the Gulf of Mexico Continental Shelf have been explored, considerable amounts of hydrocarbons may yet be discovered in deepwater locations. Industry has been developing the technology to explore deepwater areas, and interest in these portions of the Gulf is increasing.</p><p>As of December 1981, the total of all identified oil and gas fields in the Gulf of Mexico OCS increased to 505 from 482 at the end of the previous year; this net increase of 23 fields discovered in 1981 compares to net increases of 50 in 1980, 51 in 1979, and 25 in 1978. The number of active fields increased from 466 in 1981, and fields for which reserve estimates have been made increased from 419 to 445. As of January 1982, 19,736 offshore oil and gas wells had been drilled in the Gulf of Mexico OCS; most of the wells (17,257) are off the coast of Louisiana. Currently, there are 2,027 active oil and gas leases in the Gulf of Mexico; 1,200 of them are producing leases.</p><p>The Department of the Interior's 5-year OCS oil and gas leasing schedule projects 2 to 3 Gulf of Mexico lease sales per year through 1987, for a total of 12 offerings, and starting in 1983, the Gulf will be divided into three planning areas. Resource estimates issued for the following Gulf of Mexico lease sales are as follows: Lease Sale 67--75.16 million barrels of oil and 1.03 trillion cubic feet of gas; Lease Sale 69--48.24 million barrels of oil and .785 trillion cubic feet of gas; Lease Sale 72--97 million barrels of oil and 1.04 trillion cubic feet of gas; Lease Sale 74--29 million barrels of oil and .525 trillion cubic feet of gas; and Lease Sale 79--123 million barrels of oil and .157 trillion cubic feet of gas.</p><p>Since 1972, oil production in the Gulf of Mexico has declined each year, and gas production, thought to have reached its peak in 1981, is also expected to begin a noticeable decline. To date, most of the oil and gas discovered in the Gulf has occurred on the Texas-Louisiana Shelf, but in the future, oil and gas exploration is likely to include a number of areas where previous leasing has not been extensive. The West Florida Shelf, especially the area off the coast of southwest Florida and the deepwater areas southeast of the Mississippi River Delta, are potential areas for future exploration. As production begins to decline from mature fields, smaller fields will become economically producible, and implementation of secondary and tertiary recovery techniques will make it possible to extract more oil and gas from reservoirs than was possible previously.</p><p>Each year, hundreds of miles of pipelines are added to the existing network in the Gulf of Mexico. Recently, there have been a number of proposals for deepwater ports and transshipment terminals as well as projects including the deepening or widening of existing conventional ports. The process of transportation planning in the Gulf of Mexico is done by industry and government through the Intergovernmental Planning Program and its Regional Technical Working Group.</p><p>The Gulf Coast region is an area of significant onshore oil and gas activity, with many cities and towns offering a wide range of services and supplies to onshore and offshore oil operators and their ancillary industries. While the western and central Gulf oil and gas support infrastructure is quite extensive and complex, the support facilities in the eastern Gulf are still in the early stages of development. In the likely event of a decline in Gulf OCS production, imported oil may be substituted for dwindling domestic stocks at Gulf Coast refineries. Planners must consider impacts generated by changes in oil and gas productivity and focus on finding alternative uses for facilities and alternative employment for workers.&nbsp;</p>","language":"English","publisher":"U.S. Geological Survey","doi":"10.3133/ofr82242","usgsCitation":"Havran, K.J., Wiese, J., Collins, K.M., and Kurz, F.N., 1982, Gulf of Mexico summary report 3 August 1982: A revision of Outer Continental Shelf oil and gas activities in the Gulf of Mexico and their onshore impacts: Gulf of Mexico summary report 2, August 1981: U.S. Geological Survey Open-File Report 82-242, Report: ix, 99 p.; 3 Plates: 35.33 x 16.43 inches or smaller, https://doi.org/10.3133/ofr82242.","productDescription":"Report: ix, 99 p.; 3 Plates: 35.33 x 16.43 inches or smaller","costCenters":[],"links":[{"id":409398,"rank":5,"type":{"id":17,"text":"Plate"},"url":"https://pubs.usgs.gov/of/1982/0242/plate-1.pdf","linkFileType":{"id":1,"text":"pdf"}},{"id":409397,"rank":4,"type":{"id":17,"text":"Plate"},"url":"https://pubs.usgs.gov/of/1982/0242/plate-2.pdf","linkFileType":{"id":1,"text":"pdf"}},{"id":409396,"rank":3,"type":{"id":17,"text":"Plate"},"url":"https://pubs.usgs.gov/of/1982/0242/plate-3.pdf","linkFileType":{"id":1,"text":"pdf"}},{"id":140826,"rank":0,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/of/1982/0242/report-thumb.jpg"},{"id":409395,"rank":2,"type":{"id":11,"text":"Document"},"url":"https://pubs.usgs.gov/of/1982/0242/report.pdf","linkFileType":{"id":1,"text":"pdf"}}],"country":"United States","state":"Alabama, Florida, Louisiana, Mississippi, Texas","otherGeospatial":"Gulf of Mexico Outer Continental Shelf","geographicExtents":"{\n  \"type\": \"FeatureCollection\",\n  \"features\": [\n    {\n      \"type\": \"Feature\",\n      \"properties\": {},\n      \"geometry\": {\n        \"type\": \"Polygon\",\n        \"coordinates\": [\n          [\n            [\n              -96.240234375,\n              26.82407078047018\n            ],\n            [\n              -83.14453125,\n              26.82407078047018\n            ],\n            [\n              -83.14453125,\n              30.14512718337613\n            ],\n            [\n              -96.240234375,\n              30.14512718337613\n            ],\n            [\n              -96.240234375,\n              26.82407078047018\n            ]\n          ]\n        ]\n      }\n    }\n  ]\n}","noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"4f4e4a81e4b07f02db64a1ab","contributors":{"authors":[{"text":"Havran, Kenneth J.","contributorId":40983,"corporation":false,"usgs":true,"family":"Havran","given":"Kenneth","email":"","middleInitial":"J.","affiliations":[],"preferred":false,"id":154784,"contributorType":{"id":1,"text":"Authors"},"rank":1},{"text":"Wiese, J.D.","contributorId":82303,"corporation":false,"usgs":true,"family":"Wiese","given":"J.D.","email":"","affiliations":[],"preferred":false,"id":154785,"contributorType":{"id":1,"text":"Authors"},"rank":2},{"text":"Collins, Karen M.","contributorId":11216,"corporation":false,"usgs":true,"family":"Collins","given":"Karen","email":"","middleInitial":"M.","affiliations":[],"preferred":false,"id":154783,"contributorType":{"id":1,"text":"Authors"},"rank":3},{"text":"Kurz, Frederick N.","contributorId":47785,"corporation":false,"usgs":true,"family":"Kurz","given":"Frederick","email":"","middleInitial":"N.","affiliations":[],"preferred":false,"id":154782,"contributorType":{"id":1,"text":"Authors"},"rank":4}]}}
,{"id":8872,"text":"ofr78556H - 1982 - Drainage areas of surface water bodies of eastern Maine coastal river basins","interactions":[{"subject":{"id":8872,"text":"ofr78556H - 1982 - Drainage areas of surface water bodies of eastern Maine coastal river basins","indexId":"ofr78556H","publicationYear":"1982","noYear":false,"chapter":"H","title":"Drainage areas of surface water bodies of eastern Maine coastal river basins"},"predicate":"IS_PART_OF","object":{"id":7104,"text":"ofr78556 - 1978 - Drainage areas in Maine","indexId":"ofr78556","publicationYear":"1978","noYear":false,"title":"Drainage areas in Maine"},"id":1}],"isPartOf":{"id":7104,"text":"ofr78556 - 1978 - Drainage areas in Maine","indexId":"ofr78556","publicationYear":"1978","noYear":false,"title":"Drainage areas in Maine"},"lastModifiedDate":"2026-03-06T17:40:06.808527","indexId":"ofr78556H","displayToPublicDate":"1994-01-01T00:00:00","publicationYear":"1982","noYear":false,"publicationType":{"id":18,"text":"Report"},"publicationSubtype":{"id":5,"text":"USGS Numbered Series"},"seriesTitle":{"id":330,"text":"Open-File Report","code":"OFR","onlineIssn":"2331-1258","printIssn":"0196-1497","active":true,"publicationSubtype":{"id":5}},"seriesNumber":"78-556","chapter":"H","title":"Drainage areas of surface water bodies of eastern Maine coastal river basins","docAbstract":"<p>The report contains drainage-area values for: lakes and ponds included in the MIDAS (Maine Informational Display Analysis System) File 906-Z, streams that drain an area greater than 25 square miles, dam sites, and locations where hydrologic data are available. Supplemental information includes State and Federal location systems used to identify these lake and stream sites.</p>","language":"English","publisher":"U.S. Geological Survey","doi":"10.3133/ofr78556H","collaboration":"Prepared in cooperation with the Maine Department of Environmental Protection","usgsCitation":"Fontaine, R.A., 1982, Drainage areas of surface water bodies of eastern Maine coastal river basins: U.S. Geological Survey Open-File Report 78-556, v, 54 p., https://doi.org/10.3133/ofr78556H.","productDescription":"v, 54 p.","costCenters":[],"links":[{"id":142629,"rank":1,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/of/1978/0556-h/report-thumb.jpg"},{"id":430922,"rank":2,"type":{"id":11,"text":"Document"},"url":"https://pubs.usgs.gov/of/1978/0556-h/report.pdf","linkFileType":{"id":1,"text":"pdf"}}],"country":"United States","state":"Maine","otherGeospatial":"eastern Maine coastal river basins","geographicExtents":"{\n  \"type\": \"FeatureCollection\",\n  \"features\": [\n    {\n      \"type\": \"Feature\",\n      \"properties\": {},\n      \"geometry\": {\n        \"coordinates\": [\n          [\n            [\n              -68.9618726405488,\n              46.003610330553045\n            ],\n            [\n              -68.9618726405488,\n              44.18635392825826\n            ],\n            [\n              -66.92340130518438,\n              44.18635392825826\n            ],\n            [\n              -66.92340130518438,\n              46.003610330553045\n            ],\n            [\n              -68.9618726405488,\n              46.003610330553045\n            ]\n          ]\n        ],\n        \"type\": \"Polygon\"\n      }\n    }\n  ]\n}","noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"4f4e4a61e4b07f02db635ee9","contributors":{"authors":[{"text":"Fontaine, Richard A. rfontain@usgs.gov","contributorId":2379,"corporation":false,"usgs":true,"family":"Fontaine","given":"Richard","email":"rfontain@usgs.gov","middleInitial":"A.","affiliations":[],"preferred":true,"id":158467,"contributorType":{"id":1,"text":"Authors"},"rank":1}]}}
,{"id":8829,"text":"ofr82888 - 1982 - Origin of the Mariano Lake uranium deposit, McKinley County, New Mexico","interactions":[],"lastModifiedDate":"2020-04-30T16:28:14.587118","indexId":"ofr82888","displayToPublicDate":"1994-01-01T00:00:00","publicationYear":"1982","noYear":false,"publicationType":{"id":18,"text":"Report"},"publicationSubtype":{"id":5,"text":"USGS Numbered Series"},"seriesTitle":{"id":330,"text":"Open-File Report","code":"OFR","onlineIssn":"2331-1258","printIssn":"0196-1497","active":true,"publicationSubtype":{"id":5}},"seriesNumber":"82-888","title":"Origin of the Mariano Lake uranium deposit, McKinley County, New Mexico","docAbstract":"<p>The Mariano Lake uranium deposit, hosted by the Brushy Basin Member of the Jurassic Morrison Formation, occurs in the trough of an east-west trending syncline at the western end of the Smith Lake-Mariano Lake group of uranium deposits near Crownpoint, New Mexico. The orebody, which contains abundant amorphous organic material, is situated on the reduced side of a regional reduction-oxidation (redox) interface. The presence of amorphous organic material suggests the orebody may represent a tabular (primary) deposit, whereas the close proximity of the orebody to the redox interface is suggestive that uranium was secondarily redistributed by oxidative processes from pre-existing tabular orebodies. Uranium contents correlate positively with both organic carbon and vanadium contents. Petrographic evidence and scanning electron microscope-energy dispersive analyses point to uranium residence in the epigentically introduced amorphous organic material, which coats detrital grains and fills voids. Uranium mineralization was preceded by the following diagenetic alterations: precipitation of pyrite (ẟ<sup>34</sup>S values ranging from-11.0 to-38.2 per mil); precipitation of mixed-layer smectite-illite clays; partial dissolution of some of the detrital feldspar population; and precipitation of quartz and adularia overgrowths. Alterations associated with uranium mineralization include emplacement of amorphous organic material (possibly uranium bearing); destruction of detrital iron-titanium oxide grains; coprecipitation of chlorite and microcrystalline quartz, and precipitation of pyrite and marcasite (ẟ<sup>34</sup>S values for these sulfides ranging from -29.4 to -41.6 per mil). After mineralization, calcite, dolomite, barite, and kaolinite precipitated, and authigenic iron disulfides were replaced by ferric oxides and hydroxides. Geochemical data (primarily the positive correlation of uranium content to both organic carbon and vanadium contents) and petrographic observations (epigentically introduced amorphous organic matter and uranium residence in this organic matter) indicate that the Mariano Lake orebody is a tabular-type uranium deposit. Oxidative processes have not noticeably redistributed and reconcentrated primary uranium in the immediate vicinity of the deposit nor have they greatly modified geochemical characteristics in the ore. Preservation of the Mariano Lake deposit may not only be related to its position along the synclinal trough, where oxidative destruction of the orebody has been inhibited by stagnation of oxidizing ground waters by the structure, but also due to the deflection of ground waters (resulting from low orebody porosity) around the orebody.</p>","language":"English","publisher":"U.S. Geological Survey","doi":"10.3133/ofr82888","usgsCitation":"Fishman, N.S., and Reynolds, R.L., 1982, Origin of the Mariano Lake uranium deposit, McKinley County, New Mexico: U.S. Geological Survey Open-File Report 82-888, iii, 52 p., https://doi.org/10.3133/ofr82888.","productDescription":"iii, 52 p.","costCenters":[{"id":318,"text":"Geosciences and Environmental Change Science Center","active":true,"usgs":true}],"links":[{"id":141608,"rank":0,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/of/1982/0888/report-thumb.jpg"},{"id":36405,"rank":300,"type":{"id":11,"text":"Document"},"url":"https://pubs.usgs.gov/of/1982/0888/report.pdf","linkFileType":{"id":1,"text":"pdf"}}],"country":"United States","state":"New Mexico","county":"McKinley County","geographicExtents":"{\"type\":\"FeatureCollection\",\"features\":[{\"type\":\"Feature\",\"geometry\":{\"type\":\"Polygon\",\"coordinates\":[[[-109.0452,36.006],[-108.7687,36.0063],[-108.3738,36.0044],[-108.2646,36.0038],[-108.1559,36.0027],[-108.1468,36.0028],[-108.1411,36.0029],[-108.1224,36.0028],[-107.8738,36.0034],[-107.8351,36.0035],[-107.6776,36.0031],[-107.66,36.0034],[-107.6423,36.0032],[-107.6247,36.0034],[-107.6213,36.003],[-107.6042,36.0032],[-107.5866,36.003],[-107.5718,36.0027],[-107.5541,36.0025],[-107.5513,36.0026],[-107.5161,36.0026],[-107.4421,36.0008],[-107.4068,36.0007],[-107.3875,36.0009],[-107.3397,36.0006],[-107.317,36.0008],[-107.3056,36.0005],[-107.3054,35.991],[-107.3058,35.9765],[-107.3055,35.9311],[-107.3051,35.8744],[-107.3049,35.8295],[-107.3047,35.8168],[-107.3053,35.7864],[-107.3054,35.7573],[-107.3057,35.7419],[-107.3049,35.7301],[-107.3052,35.7151],[-107.305,35.6997],[-107.3053,35.6852],[-107.305,35.6707],[-107.3048,35.6552],[-107.3046,35.6439],[-107.3041,35.6139],[-107.3032,35.5277],[-107.3035,35.4787],[-107.3025,35.4247],[-107.3016,35.3021],[-107.518,35.3036],[-107.5231,35.3036],[-107.6183,35.3059],[-107.6229,35.3059],[-107.6231,35.3159],[-107.6243,35.3485],[-107.7287,35.3489],[-107.7295,35.3366],[-107.7288,35.3062],[-107.7812,35.3063],[-107.8111,35.3063],[-107.8297,35.3065],[-107.8336,35.3064],[-107.9159,35.3065],[-107.9351,35.3066],[-107.9396,35.3065],[-107.974,35.3064],[-107.992,35.3066],[-108.0473,35.307],[-108.143,35.3057],[-108.151,35.307],[-108.2558,35.3077],[-108.364,35.3065],[-108.4661,35.3081],[-108.4644,35.2214],[-108.4659,35.1623],[-108.4661,35.1355],[-108.4673,35.0501],[-108.4678,34.9597],[-108.497,34.96],[-108.52,34.96],[-108.7809,34.9595],[-109.0458,34.9611],[-109.0458,35.166],[-109.0457,35.1796],[-109.0457,35.1941],[-109.0457,35.2078],[-109.0457,35.2228],[-109.0457,35.2359],[-109.0456,35.3531],[-109.0457,35.6637],[-109.0452,36.006]]]},\"properties\":{\"name\":\"McKinley\",\"state\":\"NM\"}}]}","noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"4f4e4a61e4b07f02db635e15","contributors":{"authors":[{"text":"Fishman, Neil S.","contributorId":106464,"corporation":false,"usgs":true,"family":"Fishman","given":"Neil","email":"","middleInitial":"S.","affiliations":[],"preferred":false,"id":158404,"contributorType":{"id":1,"text":"Authors"},"rank":1},{"text":"Reynolds, Richard L. 0000-0002-4572-2942 rreynolds@usgs.gov","orcid":"https://orcid.org/0000-0002-4572-2942","contributorId":139068,"corporation":false,"usgs":true,"family":"Reynolds","given":"Richard","email":"rreynolds@usgs.gov","middleInitial":"L.","affiliations":[{"id":318,"text":"Geosciences and Environmental Change Science Center","active":true,"usgs":true}],"preferred":true,"id":158403,"contributorType":{"id":1,"text":"Authors"},"rank":2}]}}
,{"id":27999,"text":"wri824074 - 1982 - Physical and hydrologic environments of the Mulberry coal reserves in eastern Kansas","interactions":[],"lastModifiedDate":"2012-02-02T00:08:40","indexId":"wri824074","displayToPublicDate":"1994-01-01T00:00:00","publicationYear":"1982","noYear":false,"publicationType":{"id":18,"text":"Report"},"publicationSubtype":{"id":5,"text":"USGS Numbered Series"},"seriesTitle":{"id":342,"text":"Water-Resources Investigations Report","code":"WRI","active":false,"publicationSubtype":{"id":5}},"seriesNumber":"82-4074","title":"Physical and hydrologic environments of the Mulberry coal reserves in eastern Kansas","docAbstract":"Strippable reserves of Mulberry coal underlie an area of approximately 300 square miles of Miami, Linn, and Bourbon Counties of eastern Kansas. Although subject to State reclamation law, current and projected strip mining of this relatively thin coal seam could alter and hydrologic environment of the study area. Drained by the Marais des Cygnes and Little Osage Rivers and their tributaries, this area is characterized by low relief and moderately impermeable soils. Streamflows are poorly sustained by ground-water discharge and fluctuate widely due to climatic extremes and usage of surface-water supplies. Because ground-water supplies are generally unreliable in quantity and quality, surface water is used to meet most water requirements in the study area. Primary used of surface waters are for domestic supplies, maintenance of wildlife and recreational areas, and cooling needs at LaCygne Power Plant. The prevailing chemical type of the natural streamflow is calcium bicarbonate, with concentrations of dissolved solids generally less than 500 milligrams per liter and pH near neutral. Additional streamflow and water-quality data are needed to evaluate the premining characteristics of and the anticipated changes in the hydrologic environment as strip mining proceeds within the study area. A network of data-collection stations and a sampling scheme have been established to acquire this additional information. (USGS)","language":"ENGLISH","publisher":"U.S. Geological Survey, WRD,","doi":"10.3133/wri824074","usgsCitation":"Kenny, J.F., Bevans, H., and Diaz, A., 1982, Physical and hydrologic environments of the Mulberry coal reserves in eastern Kansas: U.S. Geological Survey Water-Resources Investigations Report 82-4074, 50 p. :ill., maps ;28 cm., https://doi.org/10.3133/wri824074.","productDescription":"50 p. :ill., maps ;28 cm.","costCenters":[],"links":[{"id":122828,"rank":0,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/wri/1982/4074/report-thumb.jpg"},{"id":56826,"rank":300,"type":{"id":11,"text":"Document"},"url":"https://pubs.usgs.gov/wri/1982/4074/report.pdf","linkFileType":{"id":1,"text":"pdf"}}],"noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"4f4e4adbe4b07f02db685c0f","contributors":{"authors":[{"text":"Kenny, J. F.","contributorId":100378,"corporation":false,"usgs":true,"family":"Kenny","given":"J.","email":"","middleInitial":"F.","affiliations":[],"preferred":false,"id":199042,"contributorType":{"id":1,"text":"Authors"},"rank":1},{"text":"Bevans, H.E.","contributorId":102892,"corporation":false,"usgs":true,"family":"Bevans","given":"H.E.","email":"","affiliations":[],"preferred":false,"id":199043,"contributorType":{"id":1,"text":"Authors"},"rank":2},{"text":"Diaz, A.M.","contributorId":27084,"corporation":false,"usgs":true,"family":"Diaz","given":"A.M.","email":"","affiliations":[],"preferred":false,"id":199041,"contributorType":{"id":1,"text":"Authors"},"rank":3}]}}
,{"id":29045,"text":"wri8233 - 1982 - Floods of May 1981 in west-central Montana","interactions":[],"lastModifiedDate":"2019-08-05T11:48:39","indexId":"wri8233","displayToPublicDate":"1994-01-01T00:00:00","publicationYear":"1982","noYear":false,"publicationType":{"id":18,"text":"Report"},"publicationSubtype":{"id":5,"text":"USGS Numbered Series"},"seriesTitle":{"id":342,"text":"Water-Resources Investigations Report","code":"WRI","active":false,"publicationSubtype":{"id":5}},"seriesNumber":"82-33","title":"Floods of May 1981 in west-central Montana","docAbstract":"Extensive flooding occurred in west-central Montana during May 22-23, 1981, as a result of a series of rainstorms. Flooding was particularly severe in the communities of East Helena, Belt, and Deer Lodge. Although no lives were lost, total flood damages were estimated by the Montana Disaster Emergency Services Division to be in excess of $30 million. Peak discharges were determined at 75 sites in the flooded area. At 25 sites the May 1981 peak discharge exceeded the computed 100-year frequency flood, and at 29 sites, where previous flow records are available, the May 1981 peak discharge exceeded the previous peak of record. (USGS)","language":"English","publisher":"U.S. Geological Survey","publisherLocation":"Reston, VA","doi":"10.3133/wri8233","usgsCitation":"Parrett, C., Omang, R.J., Hull, J.A., and Fassler, J.W., 1982, Floods of May 1981 in west-central Montana: U.S. Geological Survey Water-Resources Investigations Report 82-33, iv, 20 p. , https://doi.org/10.3133/wri8233.","productDescription":"iv, 20 p. ","costCenters":[],"links":[{"id":366261,"rank":2,"type":{"id":11,"text":"Document"},"url":"https://pubs.usgs.gov/wri/1982/0033/report.pdf","linkFileType":{"id":1,"text":"pdf"}},{"id":158920,"rank":0,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/wri/1982/0033/report-thumb.jpg"}],"country":"United States","state":"Montana","geographicExtents":"{\n  \"type\": \"FeatureCollection\",\n  \"features\": [\n    {\n      \"type\": \"Feature\",\n      \"properties\": {},\n      \"geometry\": {\n        \"type\": \"Polygon\",\n        \"coordinates\": [\n          [\n            [\n              -112.576904296875,\n              45.836454050187726\n            ],\n            [\n              -109.5556640625,\n              45.836454050187726\n            ],\n            [\n              -109.5556640625,\n              47.45037978769006\n            ],\n            [\n              -112.576904296875,\n              47.45037978769006\n            ],\n            [\n              -112.576904296875,\n              45.836454050187726\n            ]\n          ]\n        ]\n      }\n    }\n  ]\n}","noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"4f4e49d9e4b07f02db5df9df","contributors":{"authors":[{"text":"Parrett, Charles","contributorId":9635,"corporation":false,"usgs":true,"family":"Parrett","given":"Charles","email":"","affiliations":[],"preferred":false,"id":200849,"contributorType":{"id":1,"text":"Authors"},"rank":1},{"text":"Omang, R. J.","contributorId":31365,"corporation":false,"usgs":true,"family":"Omang","given":"R.","email":"","middleInitial":"J.","affiliations":[],"preferred":false,"id":200850,"contributorType":{"id":1,"text":"Authors"},"rank":2},{"text":"Hull, J. A.","contributorId":39345,"corporation":false,"usgs":true,"family":"Hull","given":"J.","email":"","middleInitial":"A.","affiliations":[],"preferred":false,"id":200852,"contributorType":{"id":1,"text":"Authors"},"rank":3},{"text":"Fassler, John W.","contributorId":33741,"corporation":false,"usgs":true,"family":"Fassler","given":"John","email":"","middleInitial":"W.","affiliations":[],"preferred":false,"id":200851,"contributorType":{"id":1,"text":"Authors"},"rank":4}]}}
,{"id":7457,"text":"ofr821033 - 1982 - Probabilistic estimates of maximum acceleration and velocity in rock in the contiguous United States","interactions":[],"lastModifiedDate":"2012-02-02T00:06:13","indexId":"ofr821033","displayToPublicDate":"1994-01-01T00:00:00","publicationYear":"1982","noYear":false,"publicationType":{"id":18,"text":"Report"},"publicationSubtype":{"id":5,"text":"USGS Numbered Series"},"seriesTitle":{"id":330,"text":"Open-File Report","code":"OFR","onlineIssn":"2331-1258","printIssn":"0196-1497","active":true,"publicationSubtype":{"id":5}},"seriesNumber":"82-1033","title":"Probabilistic estimates of maximum acceleration and velocity in rock in the contiguous United States","docAbstract":"Maximum horizontal accelerations and velocities caused by earthquakes are mapped for exposure times of 10, 50 and 250 years at the 90-percent probability level of nonexceedance for the contiguous United States. In many areas these new maps differ significantly from the 1976 probabilistic acceleration map by Algermlssen and Perkins because of the increase in detail, resulting from greater emphasis on the geologic basis for seismic source zones. This new emphasis is possible because of extensive data recently acquired on Holocene and Quaternary faulting in the western United States and new interpretations of geologic structures controlling the seismicity pattern in the central and eastern United States. ","language":"ENGLISH","publisher":"U.S. Geological Survey,","doi":"10.3133/ofr821033","usgsCitation":"Algermissen, S.T., Perkins, D.M., Thenhaus, P., Hanson, S., and Bender, B., 1982, Probabilistic estimates of maximum acceleration and velocity in rock in the contiguous United States: U.S. Geological Survey Open-File Report 82-1033, 107 p., ill., maps ;28 cm., https://doi.org/10.3133/ofr821033.","productDescription":"107 p., ill., maps ;28 cm.","costCenters":[],"links":[{"id":142072,"rank":0,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/of/1982/1033/report-thumb.jpg"},{"id":34868,"rank":400,"type":{"id":17,"text":"Plate"},"url":"https://pubs.usgs.gov/of/1982/1033/plate-1.pdf","linkFileType":{"id":1,"text":"pdf"}},{"id":34869,"rank":401,"type":{"id":17,"text":"Plate"},"url":"https://pubs.usgs.gov/of/1982/1033/plate-2.pdf","linkFileType":{"id":1,"text":"pdf"}},{"id":34870,"rank":402,"type":{"id":17,"text":"Plate"},"url":"https://pubs.usgs.gov/of/1982/1033/plate-3.pdf","linkFileType":{"id":1,"text":"pdf"}},{"id":34871,"rank":403,"type":{"id":17,"text":"Plate"},"url":"https://pubs.usgs.gov/of/1982/1033/plate-4.pdf","linkFileType":{"id":1,"text":"pdf"}},{"id":34872,"rank":404,"type":{"id":17,"text":"Plate"},"url":"https://pubs.usgs.gov/of/1982/1033/plate-5.pdf","linkFileType":{"id":1,"text":"pdf"}},{"id":34873,"rank":405,"type":{"id":17,"text":"Plate"},"url":"https://pubs.usgs.gov/of/1982/1033/plate-6.pdf","linkFileType":{"id":1,"text":"pdf"}},{"id":34874,"rank":300,"type":{"id":11,"text":"Document"},"url":"https://pubs.usgs.gov/of/1982/1033/report.pdf","linkFileType":{"id":1,"text":"pdf"}}],"noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"4f4e4a9fe4b07f02db660d58","contributors":{"authors":[{"text":"Algermissen, Sylvester Theodore","contributorId":94300,"corporation":false,"usgs":true,"family":"Algermissen","given":"Sylvester","email":"","middleInitial":"Theodore","affiliations":[],"preferred":false,"id":155704,"contributorType":{"id":1,"text":"Authors"},"rank":1},{"text":"Perkins, D. M.","contributorId":83922,"corporation":false,"usgs":true,"family":"Perkins","given":"D.","email":"","middleInitial":"M.","affiliations":[],"preferred":false,"id":155703,"contributorType":{"id":1,"text":"Authors"},"rank":2},{"text":"Thenhaus, P.C.","contributorId":46089,"corporation":false,"usgs":true,"family":"Thenhaus","given":"P.C.","affiliations":[],"preferred":false,"id":155701,"contributorType":{"id":1,"text":"Authors"},"rank":3},{"text":"Hanson, S.L.","contributorId":47361,"corporation":false,"usgs":true,"family":"Hanson","given":"S.L.","email":"","affiliations":[],"preferred":false,"id":155702,"contributorType":{"id":1,"text":"Authors"},"rank":4},{"text":"Bender, B.L.","contributorId":99976,"corporation":false,"usgs":true,"family":"Bender","given":"B.L.","email":"","affiliations":[],"preferred":false,"id":155705,"contributorType":{"id":1,"text":"Authors"},"rank":5}]}}
,{"id":8787,"text":"ofr82156 - 1982 - Effects of Late Cretaceous and Cenozoic faulting on the geology and hydrology of the coastal plain near the Savannah River, Georgia and South Carolina","interactions":[],"lastModifiedDate":"2016-12-14T12:22:31","indexId":"ofr82156","displayToPublicDate":"1994-01-01T00:00:00","publicationYear":"1982","noYear":false,"publicationType":{"id":18,"text":"Report"},"publicationSubtype":{"id":5,"text":"USGS Numbered Series"},"seriesTitle":{"id":330,"text":"Open-File Report","code":"OFR","onlineIssn":"2331-1258","printIssn":"0196-1497","active":true,"publicationSubtype":{"id":5}},"seriesNumber":"82-156","title":"Effects of Late Cretaceous and Cenozoic faulting on the geology and hydrology of the coastal plain near the Savannah River, Georgia and South Carolina","docAbstract":"Geologic and hydrologic investigations by the U.S. Geological Survey have defined stratigraphic and hydraulic anomalies suggestive of faulting within Coastal Plain sediments between the Ogeechee River in east-central Georgia and the Edisto River in west-central South Carolina. Examination of borehole cuttings, cores, and geophysical logs from test wells indicate that Triassic rocks and Upper Cretaceous and lower Tertiary Coastal Plain sediments near the Barnwell-Allendale County line near Millett, South Carolina, are offset by a northeast-trending fault downthrown to the northwest. The location of this suspected Coastal Plain fault generally coincides with the location of an inferred fault in basement rocks as interpreted from aeromagnetic surveys. Apparent vertical offsets range from about 700 feet at the base of Upper Cretaceous sediments to about 20 feet in strata of Late Eocene age. As a result, the Upper Cretaceous Middendorf Formation which directly overlies crystalline and Triassic rocks updip (northwest) of this fault, is absent immediately downdip of the fault. The thickness of Tipper Cretaceous sediments is also sharply reduced from about 700 feet to about 180 feet across the fault.\r\n\r\nSediments of the basal Coastal Plain aquifer are largely truncated by uplifted Triassic rocks at the fault near Millett, South Carolina. Lateral ground-water flow near the Savannah River Is consequently disrupted updip of the fault and ground water is transferred vertically into overlying sediments and possibly into the Savannah River. At several locations, abrupt changes in potentiometric head occur across this fault. Computed transmissivity of the basal Coastal Plain aquifer is also radically reduced downdip of the fault, sharply reversing a downdip trend of rapidly increasing aquifer transmissivity. \r\n\r\nOther anomalous potentiometric data along a northeast-trending line between Statesboro, Georgia, and Fairfax, South Carolina, suggest the possibility of similar faulting in correlative geologic units. The location of the suspected fault near Statesboro, Georgia, generally coincides with the eastward extension of the Gulf Trough, a regional potentiometric anomaly in central Georgia.","language":"ENGLISH","publisher":"U.S. Geological Survey,","doi":"10.3133/ofr82156","usgsCitation":"Faye, R., and Prowell, D., 1982, Effects of Late Cretaceous and Cenozoic faulting on the geology and hydrology of the coastal plain near the Savannah River, Georgia and South Carolina: U.S. Geological Survey Open-File Report 82-156, 85 p., 8 over-size sheets, ill., maps ;28 cm., https://doi.org/10.3133/ofr82156.","productDescription":"85 p., 8 over-size sheets, ill., maps ;28 cm.","costCenters":[{"id":13634,"text":"South Atlantic Water Science 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,{"id":7503,"text":"ofr82916 - 1982 - Selected hydrologic data, Price River basin, Utah, water years 1979 and 1980","interactions":[],"lastModifiedDate":"2017-09-01T14:57:41","indexId":"ofr82916","displayToPublicDate":"1994-01-01T00:00:00","publicationYear":"1982","noYear":false,"publicationType":{"id":18,"text":"Report"},"publicationSubtype":{"id":5,"text":"USGS Numbered Series"},"seriesTitle":{"id":330,"text":"Open-File Report","code":"OFR","onlineIssn":"2331-1258","printIssn":"0196-1497","active":true,"publicationSubtype":{"id":5}},"seriesNumber":"82-916","title":"Selected hydrologic data, Price River basin, Utah, water years 1979 and 1980","docAbstract":"<p>The Price River basin in east-central Utah includes a significant part of the Wasatch Plateau and Book Cliffs coal-fields area (pi. 1) and currently (1980) is part of the most active coal-mining areas in the State.</p><p>This report presents data gathered by the U.S. Geological Survey as part of a hydrologic study carried out during the water years 1979 and 1980 in cooperation with the U.S. Bureau of Land Management. The data were obtained in the field or from private, State, and other Federal agencies. The purpose of this report is to make the data available to those engaged in coal mining, to those assessing water resources that may possibly be affected by coal mining, and to supplement two interpretive reports that will be published at a later date. Other sources of hydrologic data in the Price River basin include Waddell and others, 1978 and Sumsion, 1979.</p>","language":"English","publisher":"U.S. Geological Survey","publisherLocation":"Salt Lake City, UT","doi":"10.3133/ofr82916","collaboration":"Prepared in cooperation with the U.S. Bureau of Land Management","usgsCitation":"Waddell, K., Dodge, J., Darby, D., and Theobald, S., 1982, Selected hydrologic data, Price River basin, Utah, water years 1979 and 1980: U.S. Geological Survey Open-File Report 82-916, Report: iv, 73 p.; Plate: 23.85 in. x 22.64 in., https://doi.org/10.3133/ofr82916.","productDescription":"Report: iv, 73 p.; Plate: 23.85 in. x 22.64 in.","numberOfPages":"77","costCenters":[{"id":610,"text":"Utah Water Science Center","active":true,"usgs":true}],"links":[{"id":34957,"rank":400,"type":{"id":17,"text":"Plate"},"url":"https://pubs.usgs.gov/of/1982/0916/plate-1.pdf","linkFileType":{"id":1,"text":"pdf"}},{"id":34958,"rank":300,"type":{"id":11,"text":"Document"},"url":"https://pubs.usgs.gov/of/1982/0916/report.pdf","linkFileType":{"id":1,"text":"pdf"}},{"id":142129,"rank":0,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/of/1982/0916/report-thumb.jpg"}],"noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"4f4e4a05e4b07f02db5f8830","contributors":{"authors":[{"text":"Waddell, K.M.","contributorId":59009,"corporation":false,"usgs":true,"family":"Waddell","given":"K.M.","email":"","affiliations":[],"preferred":false,"id":155918,"contributorType":{"id":1,"text":"Authors"},"rank":1},{"text":"Dodge, J.E.","contributorId":21133,"corporation":false,"usgs":true,"family":"Dodge","given":"J.E.","email":"","affiliations":[],"preferred":false,"id":155915,"contributorType":{"id":1,"text":"Authors"},"rank":2},{"text":"Darby, D.W.","contributorId":49333,"corporation":false,"usgs":true,"family":"Darby","given":"D.W.","email":"","affiliations":[],"preferred":false,"id":155916,"contributorType":{"id":1,"text":"Authors"},"rank":3},{"text":"Theobald, S.M.","contributorId":51270,"corporation":false,"usgs":true,"family":"Theobald","given":"S.M.","email":"","affiliations":[],"preferred":false,"id":155917,"contributorType":{"id":1,"text":"Authors"},"rank":4}]}}
,{"id":58611,"text":"mf1240E - 1982 - Mineral resource potential map of the Kalmiopsis Wilderness, southwestern Oregon","interactions":[],"lastModifiedDate":"2018-11-05T10:16:37","indexId":"mf1240E","displayToPublicDate":"1994-01-01T00:00:00","publicationYear":"1982","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":"1240","chapter":"E","title":"Mineral resource potential map of the Kalmiopsis Wilderness, southwestern Oregon","docAbstract":"<p>Under the provisions of the Wilderness Act (Public Law 88-577, September 3, 1964) and the Joint conference Report on Senate Bill 4, 88th Congress, the U.S. Geological Survey and the U.S. Bureau of Mines have been conducting mineral surveys of wilderness and primitive areas. Areas officially designated as \"wilderness,\" wild,\" or \"canoe\" when the act was passed were incorporated into the National Wilderness Preservation System, and some of them are presently being studied. The act provided that areas under consideration for wilderness designation should be studied for suitability for incorporation into the Wilderness System. The mineral surveys constitute one aspect of the suitability studies. The act directs that the results of such surveys are to be made available to the public and be submitted to the President and the Congress. This report discusses the results of a mineral survey of the Kalmiopsis Wilderness, Siskiyou National Forest, Josephine and Curry Counties, Oregon. The area was established as a wilderness by Public Law 88-577, September 1964.</p>","language":"English","publisher":"U.S. Geological Survey","doi":"10.3133/mf1240E","usgsCitation":"Page, N.J., Miller, M.S., Grimes, D.J., Leinz, R.W., Blakely, R.J., Lipin, B.R., Foose, M.P., and Gray, F., 1982, Mineral resource potential map of the Kalmiopsis Wilderness, southwestern Oregon: U.S. Geological Survey Miscellaneous Field Studies Map 1240, Report: 7 p.; Plate: 37.46 x 45.21 inches, https://doi.org/10.3133/mf1240E.","productDescription":"Report: 7 p.; Plate: 37.46 x 45.21 inches","onlineOnly":"N","additionalOnlineFiles":"N","costCenters":[{"id":245,"text":"Eastern Mineral and Environmental Resources Science Center","active":true,"usgs":true}],"links":[{"id":183623,"rank":0,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/thumbnails/mf1240E.jpg"},{"id":310115,"rank":1,"type":{"id":11,"text":"Document"},"url":"https://pubs.usgs.gov/mf/1240-E/report.pdf","text":"Report","linkFileType":{"id":1,"text":"pdf"}},{"id":310116,"rank":2,"type":{"id":17,"text":"Plate"},"url":"https://pubs.usgs.gov/mf/1240-E/plate-1.pdf","text":"Plate 1"}],"scale":"62","country":"United States","state":"Oregon","otherGeospatial":"Kalmiopsis Wilderness","geographicExtents":"{ \"type\": \"FeatureCollection\", \"features\": [ { \"type\": \"Feature\", \"properties\": {}, \"geometry\": { \"type\": \"Polygon\", \"coordinates\": [ [ [ -124.25,42 ], [ -124.25,42.5 ], [ -123.75,42.5 ], [ -123.75,42 ], [ -124.25,42 ] ] ] } } ] }","noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"4f4e4b23e4b07f02db6ade15","contributors":{"authors":[{"text":"Page, Norman J.","contributorId":46492,"corporation":false,"usgs":true,"family":"Page","given":"Norman","email":"","middleInitial":"J.","affiliations":[],"preferred":false,"id":260053,"contributorType":{"id":1,"text":"Authors"},"rank":1},{"text":"Miller, Michael S.","contributorId":52588,"corporation":false,"usgs":true,"family":"Miller","given":"Michael","email":"","middleInitial":"S.","affiliations":[],"preferred":false,"id":260056,"contributorType":{"id":1,"text":"Authors"},"rank":2},{"text":"Grimes, David J.","contributorId":36925,"corporation":false,"usgs":true,"family":"Grimes","given":"David","email":"","middleInitial":"J.","affiliations":[],"preferred":false,"id":576285,"contributorType":{"id":1,"text":"Authors"},"rank":3},{"text":"Leinz, Reinhard W.","contributorId":60628,"corporation":false,"usgs":true,"family":"Leinz","given":"Reinhard","email":"","middleInitial":"W.","affiliations":[],"preferred":false,"id":576286,"contributorType":{"id":1,"text":"Authors"},"rank":4},{"text":"Blakely, Richard J. 0000-0003-1701-5236 blakely@usgs.gov","orcid":"https://orcid.org/0000-0003-1701-5236","contributorId":1540,"corporation":false,"usgs":true,"family":"Blakely","given":"Richard","email":"blakely@usgs.gov","middleInitial":"J.","affiliations":[{"id":312,"text":"Geology, Minerals, Energy, and Geophysics Science Center","active":true,"usgs":true},{"id":662,"text":"Western Mineral and Environmental Resources Science Center","active":true,"usgs":true}],"preferred":true,"id":576287,"contributorType":{"id":1,"text":"Authors"},"rank":5},{"text":"Lipin, Bruce R. blipin@usgs.gov","contributorId":5723,"corporation":false,"usgs":true,"family":"Lipin","given":"Bruce","email":"blipin@usgs.gov","middleInitial":"R.","affiliations":[],"preferred":true,"id":576288,"contributorType":{"id":1,"text":"Authors"},"rank":6},{"text":"Foose, Michael P. mfoose@usgs.gov","contributorId":4756,"corporation":false,"usgs":true,"family":"Foose","given":"Michael","email":"mfoose@usgs.gov","middleInitial":"P.","affiliations":[],"preferred":true,"id":576289,"contributorType":{"id":1,"text":"Authors"},"rank":7},{"text":"Gray, Floyd 0000-0002-0223-8966 fgray@usgs.gov","orcid":"https://orcid.org/0000-0002-0223-8966","contributorId":603,"corporation":false,"usgs":true,"family":"Gray","given":"Floyd","email":"fgray@usgs.gov","affiliations":[{"id":662,"text":"Western Mineral and Environmental Resources Science Center","active":true,"usgs":true},{"id":312,"text":"Geology, Minerals, Energy, and Geophysics Science Center","active":true,"usgs":true}],"preferred":true,"id":576290,"contributorType":{"id":1,"text":"Authors"},"rank":8}]}}
,{"id":56201,"text":"wdrNY811 - 1982 - Water resources data, New York, water year 1981; Volume 1. Eastern New York excluding Long Island","interactions":[],"lastModifiedDate":"2024-07-22T21:02:49.725547","indexId":"wdrNY811","displayToPublicDate":"1994-01-01T00:00:00","publicationYear":"1982","noYear":false,"publicationType":{"id":18,"text":"Report"},"publicationSubtype":{"id":5,"text":"USGS Numbered Series"},"seriesTitle":{"id":340,"text":"Water Data Report","code":"WDR","active":false,"publicationSubtype":{"id":5}},"seriesNumber":"NY-81-1","title":"Water resources data, New York, water year 1981; Volume 1. Eastern New York excluding Long Island","docAbstract":"<p>Water resources data for the 1981 water year for New York consist of records of stage, discharge, and water quality of streams; stage, contents, and water quality of lakes and reservoirs; and water levels of ground-water wells. This volume contains records for water discharge at 105 gaging stations; stage only at 6 gaging stations; and stage and contents at 4 gaging stations and 19 other lakes and reservoirs; water quality at 29 gaging stations, 5 precipitation stations and 4 partial-record stations; and water levels at 23 observation wells. Also included are data for 50 crest-stage and 14 low-flow partial-record stations. Additional water data were collected at various sites not involved in the systematic data-collection program and are published as miscellaneous measurements and analyses. These data together with the data in Volumes 2 and 3 represent that part of the National Water Data System operated by the U.S. Geological Survey and cooperating State, local, and Federal agencies in New York.</p>","language":"English","publisher":"U.S. Geological Survey","doi":"10.3133/wdrNY811","collaboration":"Prepared in cooperation with the State of New York and with other agencies","usgsCitation":"Water Resources Division, U.S. Geological Survey, 1982, Water resources data, New York, water year 1981; Volume 1. Eastern New York excluding Long Island: U.S. Geological Survey Water Data Report NY-81-1, viii, 318 p., https://doi.org/10.3133/wdrNY811.","productDescription":"viii, 318 p.","costCenters":[],"links":[{"id":431318,"rank":2,"type":{"id":11,"text":"Document"},"url":"https://pubs.usgs.gov/wdr/1981/ny-81-1/report.pdf","linkFileType":{"id":1,"text":"pdf"}},{"id":180910,"rank":1,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/wdr/1981/ny-81-1/report-thumb.jpg"}],"country":"United States","state":"New York","otherGeospatial":"eastern New York excluding Long Island","geographicExtents":"{\n  \"type\": \"FeatureCollection\",\n  \"features\": [\n    {\n      \"type\": \"Feature\",\n      \"properties\": {},\n      \"geometry\": {\n        \"coordinates\": [\n          [\n            [\n              -73.50726953585145,\n              44.98041799746011\n            ],\n            [\n              -76.02932029130172,\n              44.98041799746011\n            ],\n            [\n              -76.02932029130172,\n              41.044913356229046\n            ],\n            [\n              -73.50726953585145,\n              41.044913356229046\n            ],\n            [\n              -73.50726953585145,\n              44.98041799746011\n            ]\n          ]\n        ],\n        \"type\": \"Polygon\"\n      }\n    }\n  ]\n}","noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"4f4e49f5e4b07f02db5f0f16","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":532449,"contributorType":{"id":1,"text":"Authors"},"rank":1}]}}
,{"id":58575,"text":"mf1493A - 1982 - Mineral resource potential map of the Bighorn Mountains Wilderness Study Area (CDCA-217), San Bernardino County, California","interactions":[{"subject":{"id":46460,"text":"ofr82962 - 1982 - Mineral resource potential map of the Bighorn Mountains Wilderness Study Area (CDCA-217), San Bernardino County, California","indexId":"ofr82962","publicationYear":"1982","noYear":false,"title":"Mineral resource potential map of the Bighorn Mountains Wilderness Study Area (CDCA-217), San Bernardino County, California"},"predicate":"SUPERSEDED_BY","object":{"id":58575,"text":"mf1493A - 1982 - Mineral resource potential map of the Bighorn Mountains Wilderness Study Area (CDCA-217), San Bernardino County, California","indexId":"mf1493A","publicationYear":"1982","noYear":false,"chapter":"A","title":"Mineral resource potential map of the Bighorn Mountains Wilderness Study Area (CDCA-217), San Bernardino County, California"},"id":1}],"lastModifiedDate":"2015-10-20T13:14:35","indexId":"mf1493A","displayToPublicDate":"1994-01-01T00:00:00","publicationYear":"1982","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":"1493","chapter":"A","title":"Mineral resource potential map of the Bighorn Mountains Wilderness Study Area (CDCA-217), San Bernardino County, California","docAbstract":"<p>Geological, geochemical, and geophysical evidence, together with a review of historical mining and prospecting activities, suggests that most of the Bighorn Mountains Wilderness Study Area has low potential for the discovery of all types of mineral and energy resources-including precious and base metals, building stone and aggregate, fossil fuels, radioactive-mineral resources, and geothermal resources. Low-grade mineralization has been documented in one small area near Rattlesnake Canyon, and this area has low to moderate potential for future small-scale exploration and development of precious and base metals. Thorium and uranium enrichment have been documented in two small areas in the eastern part of the wilderness study area; these two areas have low to moderate potential for future small-scale exploration and development of radioactive-mineral resources.</p>","language":"English","publisher":"U.S. Geological Survey","doi":"10.3133/mf1493A","usgsCitation":"Matti, J.C., Cox, B.F., Rodriguez, E.A., Obi, C.M., Powell, R.E., Hinkle, M., Griscom, A., Sabine, C., and Cwick, G.J., 1982, Mineral resource potential map of the Bighorn Mountains Wilderness Study Area (CDCA-217), San Bernardino County, California: U.S. Geological Survey Miscellaneous Field Studies Map 1493, Report: 8 p.; Plate: 45.83 x 38.60 inches, https://doi.org/10.3133/mf1493A.","productDescription":"Report: 8 p.; Plate: 45.83 x 38.60 inches","numberOfPages":"10","onlineOnly":"N","additionalOnlineFiles":"N","costCenters":[],"links":[{"id":181313,"rank":0,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/thumbnails/mf1493A.PNG"},{"id":310170,"rank":2,"type":{"id":17,"text":"Plate"},"url":"https://pubs.usgs.gov/mf/1493-A/plate-1.pdf","text":"Plate"},{"id":310169,"rank":1,"type":{"id":11,"text":"Document"},"url":"https://pubs.usgs.gov/mf/1493-A/report.pdf","text":"Report","linkFileType":{"id":1,"text":"pdf"}}],"country":"United States","state":"California","county":"San Bernardino County","geographicExtents":"{ \"type\": \"FeatureCollection\", \"features\": [ { \"type\": \"Feature\", \"properties\": {}, \"geometry\": { \"type\": \"Polygon\", \"coordinates\": [ [ [ -116.75,34.200833333333335 ], [ -116.75,34.3675 ], [ -116.45083333333334,34.3675 ], [ -116.45083333333334,34.200833333333335 ], [ -116.75,34.200833333333335 ] ] ] } } ] }","noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"4f4e4afde4b07f02db696cef","contributors":{"authors":[{"text":"Matti, Jonathan C. jmatti@usgs.gov","contributorId":3666,"corporation":false,"usgs":true,"family":"Matti","given":"Jonathan","email":"jmatti@usgs.gov","middleInitial":"C.","affiliations":[{"id":312,"text":"Geology, Minerals, Energy, and Geophysics Science Center","active":true,"usgs":true}],"preferred":false,"id":259862,"contributorType":{"id":1,"text":"Authors"},"rank":1},{"text":"Cox, Brett F. bcox@usgs.gov","contributorId":5793,"corporation":false,"usgs":true,"family":"Cox","given":"Brett","email":"bcox@usgs.gov","middleInitial":"F.","affiliations":[],"preferred":true,"id":259863,"contributorType":{"id":1,"text":"Authors"},"rank":2},{"text":"Rodriguez, Eduardo A.","contributorId":83540,"corporation":false,"usgs":true,"family":"Rodriguez","given":"Eduardo","email":"","middleInitial":"A.","affiliations":[],"preferred":false,"id":259864,"contributorType":{"id":1,"text":"Authors"},"rank":3},{"text":"Obi, Curtis M.","contributorId":86829,"corporation":false,"usgs":true,"family":"Obi","given":"Curtis","email":"","middleInitial":"M.","affiliations":[],"preferred":false,"id":259865,"contributorType":{"id":1,"text":"Authors"},"rank":4},{"text":"Powell, Robert E. 0000-0001-7682-1655 rpowell@usgs.gov","orcid":"https://orcid.org/0000-0001-7682-1655","contributorId":4210,"corporation":false,"usgs":true,"family":"Powell","given":"Robert","email":"rpowell@usgs.gov","middleInitial":"E.","affiliations":[{"id":312,"text":"Geology, Minerals, Energy, and Geophysics Science Center","active":true,"usgs":true}],"preferred":true,"id":259866,"contributorType":{"id":1,"text":"Authors"},"rank":5},{"text":"Hinkle, Margaret","contributorId":36918,"corporation":false,"usgs":true,"family":"Hinkle","given":"Margaret","affiliations":[],"preferred":false,"id":259860,"contributorType":{"id":1,"text":"Authors"},"rank":6},{"text":"Griscom, Andrew","contributorId":23520,"corporation":false,"usgs":true,"family":"Griscom","given":"Andrew","email":"","affiliations":[],"preferred":false,"id":259861,"contributorType":{"id":1,"text":"Authors"},"rank":7},{"text":"Sabine, Charles","contributorId":88407,"corporation":false,"usgs":true,"family":"Sabine","given":"Charles","email":"","affiliations":[],"preferred":false,"id":576232,"contributorType":{"id":1,"text":"Authors"},"rank":8},{"text":"Cwick, Gary J.","contributorId":86022,"corporation":false,"usgs":true,"family":"Cwick","given":"Gary","email":"","middleInitial":"J.","affiliations":[],"preferred":false,"id":576233,"contributorType":{"id":1,"text":"Authors"},"rank":9}]}}
,{"id":59050,"text":"mf1475D - 1982 - Mineral resource potential map of the Vermilion Cliffs-Paria Canyon instant study area, Coconino County, Arizona, and Kane County, Utah","interactions":[],"lastModifiedDate":"2015-10-20T13:09:32","indexId":"mf1475D","displayToPublicDate":"1994-01-01T00:00:00","publicationYear":"1982","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":"1475","chapter":"D","title":"Mineral resource potential map of the Vermilion Cliffs-Paria Canyon instant study area, Coconino County, Arizona, and Kane County, Utah","docAbstract":"<p>In general, the mineral potential of the study area is low; in the past the area has yielded only several hundred tons of uranium ore, and there have been a number of unsuccessful efforts to produce gold.</p>\n<p>The generally small uraniferous deposits are in the Chinle Formation, mostly in the basal Shinarump Member, and mostly on the east side of the Paria Plateau. To the south and west, around the plateau, the Shinarump host rock pinches out or is present in only a few places, and the same relationships are likely below the plateau, where the host rocks are deeply buried, from 1,500 to 3,000 ft below the surface. These factors suggest the total uranium-copper-vanadium-silver potential to be very low.</p>\n<p>Gold and mercury occur in very low concentrations in the clayey units of the Petrified Forest Member of the Chinle. Gold concentrations are 40 ppb and less, and the gold is present in very fine particles; recovery is very difficult. Overall, the mercury concentrations are so low that no realistic mineral resource potential can be estimated.</p>\n<p>Nonmetallic mineral materials of possible value include limestone, flagstone, clay, and gravel, but they are of only local interest. No oil or gas resources are known in the study area. Coal resources within the area are nonexistent, but the Dakota Sandstone does contain coaly beds a few miles to the north.</p>\n<p>Water is perhaps the most significant resource needed in the study area. A number of perennial springs support the few local ranchers and tourist facilities. Some ground water would be available below the plateau, but drilling depths would be more than 2,000 ft (600-700 m).</p>","language":"English","publisher":"U.S. Geological Survey","doi":"10.3133/mf1475D","usgsCitation":"Bush, A., and Lane, M., 1982, Mineral resource potential map of the Vermilion Cliffs-Paria Canyon instant study area, Coconino County, Arizona, and Kane County, Utah: U.S. Geological Survey Miscellaneous Field Studies Map 1475, Report: 11 p.; Plate: 46.25 x 38.48 inches, https://doi.org/10.3133/mf1475D.","productDescription":"Report: 11 p.; Plate: 46.25 x 38.48 inches","onlineOnly":"N","additionalOnlineFiles":"N","costCenters":[],"links":[{"id":183527,"rank":0,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/thumbnails/mf1475D.jpg"},{"id":310159,"rank":1,"type":{"id":11,"text":"Document"},"url":"https://pubs.usgs.gov/mf/1475-D/report.pdf","text":"Report","linkFileType":{"id":1,"text":"pdf"}},{"id":310160,"rank":2,"type":{"id":17,"text":"Plate"},"url":"https://pubs.usgs.gov/mf/1475-D/plate-1.pdf","text":"Plate","linkFileType":{"id":1,"text":"pdf"}}],"country":"United States","state":"Arizona","county":"Coconino County, Kane County","geographicExtents":"{ \"type\": \"FeatureCollection\", \"features\": [ { \"type\": \"Feature\", \"properties\": {}, \"geometry\": { \"type\": \"Polygon\", \"coordinates\": [ [ [ -112.25,36.75 ], [ -112.25,37 ], [ -111.75,37 ], [ -111.75,36.75 ], [ -112.25,36.75 ] ] ] } } ] }","noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"4f4e4a61e4b07f02db6357d1","contributors":{"authors":[{"text":"Bush, Alfred L.","contributorId":48977,"corporation":false,"usgs":true,"family":"Bush","given":"Alfred L.","affiliations":[],"preferred":false,"id":261327,"contributorType":{"id":1,"text":"Authors"},"rank":1},{"text":"Lane, Michael","contributorId":39756,"corporation":false,"usgs":true,"family":"Lane","given":"Michael","affiliations":[],"preferred":false,"id":261326,"contributorType":{"id":1,"text":"Authors"},"rank":2}]}}
,{"id":60223,"text":"mf1342C - 1982 - Geophysical survey of the Centennial Mountains Wilderness Study Area and contiguous areas, Beaverhead County, Montana and Clark and Fremont counties, Idaho","interactions":[],"lastModifiedDate":"2018-10-22T14:19:58","indexId":"mf1342C","displayToPublicDate":"1994-01-01T00:00:00","publicationYear":"1982","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":"1342","chapter":"C","title":"Geophysical survey of the Centennial Mountains Wilderness Study Area and contiguous areas, Beaverhead County, Montana and Clark and Fremont counties, Idaho","docAbstract":"<p>Parts of both the Targhee and Beaverhead National Forests are within the study area. Four contiguous parcels of land, totaling about 96,176 acres (38,922 ha) make up the area. The first of these encompasses about 46,126 acres (18,667 ha), is wholly in Montana, and includes an addition by the Bureau of Land Management. The second area, in the Targhee National Forest, consists of some 38,750 acres (15,682 ha) within Idaho. The third and fourth parcels include about 11,300 acres (4,573 ha) in the Beaverhead..and Targhee National Forests that overlies the Mt. Jefferson and Sawtell Peak areas in the eastern part of the Centennial Mountains.</p>","language":"English","publisher":"U.S. Geological Survey","doi":"10.3133/mf1342C","usgsCitation":"Martin, R., 1982, Geophysical survey of the Centennial Mountains Wilderness Study Area and contiguous areas, Beaverhead County, Montana and Clark and Fremont counties, Idaho: U.S. Geological Survey Miscellaneous Field Studies Map 1342, 33.80 x 40.03 inches, https://doi.org/10.3133/mf1342C.","productDescription":"33.80 x 40.03 inches","costCenters":[],"links":[{"id":358634,"rank":2,"type":{"id":17,"text":"Plate"},"url":"https://pubs.usgs.gov/mf/1342-C/plate-1.pdf","linkFileType":{"id":1,"text":"pdf"}},{"id":182616,"rank":0,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/mf/1342-C/report-thumb.jpg"}],"scale":"0","country":"United States","state":"Idaho, Montana","county":"Beaverhead County, Clark County, Fremont County","geographicExtents":"{\n  \"type\": \"FeatureCollection\",\n  \"features\": [\n    {\n      \"type\": \"Feature\",\n      \"properties\": {},\n      \"geometry\": {\n        \"type\": \"Polygon\",\n        \"coordinates\": [\n          [\n            [\n              -112.25,\n              44.5\n            ],\n            [\n              -112.25,\n              44.6667\n            ],\n            [\n              -111.25,\n              44.6667\n            ],\n            [\n              -111.25,\n              44.5\n            ],\n            [\n              -112.25,\n              44.5\n            ]\n          ]\n        ]\n      }\n    }\n  ]\n}","noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"4f4e4ac7e4b07f02db67b49f","contributors":{"authors":[{"text":"Martin, R.A.","contributorId":53379,"corporation":false,"usgs":true,"family":"Martin","given":"R.A.","email":"","affiliations":[],"preferred":false,"id":263344,"contributorType":{"id":1,"text":"Authors"},"rank":1}]}}
,{"id":46897,"text":"ofr82552 - 1982 - Geohydrology of the preglacial Genesee Valley, Monroe County, New York","interactions":[],"lastModifiedDate":"2021-09-07T18:32:27.017525","indexId":"ofr82552","displayToPublicDate":"1994-01-01T00:00:00","publicationYear":"1982","noYear":false,"publicationType":{"id":18,"text":"Report"},"publicationSubtype":{"id":5,"text":"USGS Numbered Series"},"seriesTitle":{"id":330,"text":"Open-File Report","code":"OFR","onlineIssn":"2331-1258","printIssn":"0196-1497","active":true,"publicationSubtype":{"id":5}},"seriesNumber":"82-552","title":"Geohydrology of the preglacial Genesee Valley, Monroe County, New York","docAbstract":"This report is last in a series of 11 map sets depicting geohydrologic conditions in selected aquifers in upstate New York. Geohydrologic data are compiled on five maps at 1:24,000 scale. Together the maps provide a comprehensive overview of a buried glacio-fluvial aquifer in Monroe County. The maps include surficial geology, geologic sections, bedrock topography, water-infiltration potential of soil zone, potentiometric surface altitude, and land use. The buried-valley deposits consist of ice-contact sand and gravel, till, and glaciolacustrine sand, silt, and clay. The sand and gravel have relatively high permeabilities whereas the till, silt, and clay deposits have relatively low permeabilities. Water-table conditions prevail in unconfined sand and gravel, whereas artesian conditions prevail in the northern part of the system within sand and gravel confined by silty deposits. Recharge occurs principally over the southern part of the aquifer, due to permeable land-surface conditions. Ground-water movement is towards the Irondequoit Bay and Lake Ontario, where discharge occurs. Several communities have wells capable of producing several hundred gallons per minute from the aquifer. The use of land overlying the aquifer is predominantly residential with lesser amounts of industrial uses. (USGS)","language":"English","publisher":"U.S. Geological Survey","doi":"10.3133/ofr82552","usgsCitation":"Waller, R.M., Holecek, T.J., Stelz, W., and Belli, J.L., 1982, Geohydrology of the preglacial Genesee Valley, Monroe County, New York: U.S. Geological Survey Open-File Report 82-552, 5 Plates: 28.49 × 36.65 or smaller, https://doi.org/10.3133/ofr82552.","productDescription":"5 Plates: 28.49 × 36.65 or smaller","costCenters":[],"links":[{"id":172002,"rank":0,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/thumbnails/usgs_thumb.jpg"},{"id":83789,"rank":404,"type":{"id":17,"text":"Plate"},"url":"https://pubs.usgs.gov/of/1982/0552/plate-5.pdf","linkFileType":{"id":1,"text":"pdf"}},{"id":83788,"rank":403,"type":{"id":17,"text":"Plate"},"url":"https://pubs.usgs.gov/of/1982/0552/plate-4.pdf","linkFileType":{"id":1,"text":"pdf"}},{"id":388906,"rank":7,"type":{"id":36,"text":"NGMDB Index Page"},"url":"https://ngmdb.usgs.gov/Prodesc/proddesc_45788.htm"},{"id":83787,"rank":402,"type":{"id":17,"text":"Plate"},"url":"https://pubs.usgs.gov/of/1982/0552/plate-3.pdf","linkFileType":{"id":1,"text":"pdf"}},{"id":83786,"rank":401,"type":{"id":17,"text":"Plate"},"url":"https://pubs.usgs.gov/of/1982/0552/plate-2.pdf","linkFileType":{"id":1,"text":"pdf"}},{"id":83785,"rank":400,"type":{"id":17,"text":"Plate"},"url":"https://pubs.usgs.gov/of/1982/0552/plate-1.pdf","linkFileType":{"id":1,"text":"pdf"}}],"country":"United States","state":"New York","county":"Monroe County","otherGeospatial":"East Rochester-Irondequoit Bay Area","geographicExtents":"{\n  \"type\": \"FeatureCollection\",\n  \"features\": [\n    {\n      \"type\": \"Feature\",\n      \"properties\": {},\n      \"geometry\": {\n        \"type\": \"Polygon\",\n        \"coordinates\": [\n          [\n            [\n              -77.4580,\n              43.2500\n            ],\n            [\n              -77.5500,\n              43.2500\n            ],\n            [\n              -77.5500,\n              43.0830\n            ],\n            [\n              -77.4580,\n              43.0830\n            ],\n            [\n              -77.4580,\n              43.2500\n            ]\n          ]\n        ]\n      }\n    }\n  ]\n}","noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"4f4e4b1ae4b07f02db6a884b","contributors":{"authors":[{"text":"Waller, Roger Milton","contributorId":22320,"corporation":false,"usgs":true,"family":"Waller","given":"Roger","email":"","middleInitial":"Milton","affiliations":[],"preferred":false,"id":234276,"contributorType":{"id":1,"text":"Authors"},"rank":1},{"text":"Holecek, T. J.","contributorId":51362,"corporation":false,"usgs":true,"family":"Holecek","given":"T.","email":"","middleInitial":"J.","affiliations":[],"preferred":false,"id":234278,"contributorType":{"id":1,"text":"Authors"},"rank":2},{"text":"Stelz, W.B.","contributorId":43811,"corporation":false,"usgs":true,"family":"Stelz","given":"W.B.","email":"","affiliations":[],"preferred":false,"id":234277,"contributorType":{"id":1,"text":"Authors"},"rank":3},{"text":"Belli, J. L.","contributorId":83561,"corporation":false,"usgs":true,"family":"Belli","given":"J.","email":"","middleInitial":"L.","affiliations":[],"preferred":false,"id":234279,"contributorType":{"id":1,"text":"Authors"},"rank":4}]}}
,{"id":56284,"text":"wdrWA802 - 1982 - Water resources data for Washington, water year 1980: Vol. 2 - Eastern Washington","interactions":[],"lastModifiedDate":"2025-07-21T17:52:28.421042","indexId":"wdrWA802","displayToPublicDate":"1994-01-01T00:00:00","publicationYear":"1982","noYear":false,"publicationType":{"id":18,"text":"Report"},"publicationSubtype":{"id":5,"text":"USGS Numbered Series"},"seriesTitle":{"id":340,"text":"Water Data Report","code":"WDR","active":false,"publicationSubtype":{"id":5}},"seriesNumber":"WA-80-2","title":"Water resources data for Washington, water year 1980: Vol. 2 - Eastern Washington","docAbstract":"<p>Water Resources data for the 1980 water year for Washington consists 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 ground-water wells. This report in two volumes contains records for water discharge at 233 gaging stations stage only at 5 gaging stations; stage and contents at 41 lakes and reservoirs; and water quality at 39 gaging stations (including 6 lakes and reservoirs) and 100 wells; and water levels at 164 observation wells. Also included are data for 14 crest-stage, and 89 water-quality partial-record stations. Additional water data were collected at various sites not involved in the systematic data-collection program and are published as miscellaneous measurements analyses. These data represent that part of the National Water Data System operated by the U.S. Geological Survey and cooperating State, local and Federal agencies in Washington.</p>","language":"English","publisher":"U.S. Geological Survey","doi":"10.3133/wdrWA802","collaboration":"Prepared in cooperation with the State of Washington and with other agencies","usgsCitation":"Water Resources Division, U.S. Geological Survey, 1982, Water resources data for Washington, water year 1980: Vol. 2 - Eastern Washington: U.S. Geological Survey Water Data Report WA-80-2, x, 332 p., https://doi.org/10.3133/wdrWA802.","productDescription":"x, 332 p.","costCenters":[],"links":[{"id":492667,"rank":2,"type":{"id":11,"text":"Document"},"url":"https://pubs.usgs.gov/wdr/1980/wa-80-2/report.pdf","linkFileType":{"id":1,"text":"pdf"}},{"id":174737,"rank":1,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/wdr/1980/wa-80-2/report-thumb.jpg"}],"country":"United 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,{"id":47320,"text":"ofr81496 - 1982 - Geologic map of the Redwood Creek drainage basin, Humboldt County, California","interactions":[],"lastModifiedDate":"2022-01-07T21:12:18.954209","indexId":"ofr81496","displayToPublicDate":"1994-01-01T00:00:00","publicationYear":"1982","noYear":false,"publicationType":{"id":18,"text":"Report"},"publicationSubtype":{"id":5,"text":"USGS Numbered Series"},"seriesTitle":{"id":330,"text":"Open-File Report","code":"OFR","onlineIssn":"2331-1258","printIssn":"0196-1497","active":true,"publicationSubtype":{"id":5}},"seriesNumber":"81-496","title":"Geologic map of the Redwood Creek drainage basin, Humboldt County, California","docAbstract":"A 1:62,500-scale geologic map with 14 rock stratigraphic units and an accompanying explanatory text are used to describe the geology of the Redwood Creek drainage basin of northwestern California. A large part of Redwood National Park is located in the downstream part of this actively eroding drainage basin. The bedrock consists primarily of Mesozoic sedimentary and metamorphic rocks. The structurally complex Franciscan assemblage of rocks underlies most of the basin, but rocks of the Klammath Mountain tectonic province occurs in a small eastern part of the basin. Most major boundaries between Mesozoic rock units are north-northwest trending faults parallel to the regional structural trend. Extensive areas of surficial coastal plain sediments, landslide deposits, stream terrace deposits and modern alluvium are also present; these areas help identify loci of vigorous recent erosion. (USGS)","language":"English","publisher":"U.S. Geological Survey","doi":"10.3133/ofr81496","usgsCitation":"Harden, D.R., Kelsey, H., Morrison, S., and Stephens, T., 1982, Geologic map of the Redwood Creek drainage basin, Humboldt County, California: U.S. Geological Survey Open-File Report 81-496, 1 Plate: 32.46 x 56.62 inches, https://doi.org/10.3133/ofr81496.","productDescription":"1 Plate: 32.46 x 56.62 inches","costCenters":[],"links":[{"id":394062,"rank":2,"type":{"id":17,"text":"Plate"},"url":"https://pubs.usgs.gov/of/1981/0496/plate-1.pdf","linkFileType":{"id":1,"text":"pdf"}},{"id":172519,"rank":0,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/of/1981/0496/report-thumb.jpg"}],"scale":"62500","country":"United States","state":"California","county":"Humboldt County","otherGeospatial":"Redwood Creek drainage basin","geographicExtents":"{\n  \"type\": \"FeatureCollection\",\n  \"features\": [\n    {\n      \"type\": \"Feature\",\n      \"properties\": {},\n      \"geometry\": {\n        \"type\": \"Polygon\",\n        \"coordinates\": [\n          [\n            [\n              -124.1667,\n              40.66667\n            ],\n            [\n              -123.6667,\n              40.66667\n            ],\n            [\n              -123.6667,\n              41.41667\n            ],\n            [\n              -124.1667,\n              41.41667\n            ],\n            [\n              -124.1667,\n              40.66667\n            ]\n          ]\n        ]\n      }\n    }\n  ]\n}","noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"4f4e4ae4e4b07f02db689c3c","contributors":{"authors":[{"text":"Harden, Deborah Reid","contributorId":10042,"corporation":false,"usgs":true,"family":"Harden","given":"Deborah","email":"","middleInitial":"Reid","affiliations":[],"preferred":false,"id":235050,"contributorType":{"id":1,"text":"Authors"},"rank":1},{"text":"Kelsey, H.M.","contributorId":84300,"corporation":false,"usgs":true,"family":"Kelsey","given":"H.M.","email":"","affiliations":[],"preferred":false,"id":235053,"contributorType":{"id":1,"text":"Authors"},"rank":2},{"text":"Morrison, S.D.","contributorId":49849,"corporation":false,"usgs":true,"family":"Morrison","given":"S.D.","email":"","affiliations":[],"preferred":false,"id":235052,"contributorType":{"id":1,"text":"Authors"},"rank":3},{"text":"Stephens, T.A.","contributorId":48239,"corporation":false,"usgs":true,"family":"Stephens","given":"T.A.","email":"","affiliations":[],"preferred":false,"id":235051,"contributorType":{"id":1,"text":"Authors"},"rank":4}]}}
,{"id":59016,"text":"mf1337D - 1982 - Mineral resource potential map of the James River Face Wilderness, Bedford and Rockbridge counties, Virginia","interactions":[],"lastModifiedDate":"2015-10-20T11:06:57","indexId":"mf1337D","displayToPublicDate":"1994-01-01T00:00:00","publicationYear":"1982","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":"1337","chapter":"D","title":"Mineral resource potential map of the James River Face Wilderness, Bedford and Rockbridge counties, Virginia","docAbstract":"<p>The rocks in the James River Face Wilderness are shales and quartzites that overlie a meta-igneous basement. They are folded into a large southwestward-plunging anticline that is cut off on the east and south by an extensive thrust fault that brings old basement rocks over the younger sedimentary rocks. Geochemical studies of stream sediments, soils, and rocks do not reveal any unusually high metal concentrations, but a large resource of metallurgical-grade quartzite and shale suitable for structural clay products and lightweight aggregate is in the wilderness. Antietam (Erwin) Quartzite has been quarried at three sites in the wilderness as raw material for silicon used in the manufacture of ferrosilicon. Other uses included crushed rock for concrete aggregate, road metal, and railroad ballast, and sand for cement and mortar. Potential uses include ganister for silica brick and specialty sands such as filter and furnace sand. Firing tests on samples of shale from the Harpers (Hampton) Formation show that it could be used for the manufacture of brick and as lightweight aggregate. Of marginal economic interest are heavy-mineral layers in the basal Unicoi (Weverton) Formation.</p>","largerWorkType":{"id":18,"text":"Report"},"largerWorkSubtype":{"id":5,"text":"USGS Numbered Series"},"language":"English","publisher":"U.S. Geological Survey","doi":"10.3133/mf1337D","usgsCitation":"Brown, C.E., and Gazdik, G., 1982, Mineral resource potential map of the James River Face Wilderness, Bedford and Rockbridge counties, Virginia: U.S. Geological Survey Miscellaneous Field Studies Map 1337, Report: 6 p.; 1 Plate: 18.1 x 15.4 inches, https://doi.org/10.3133/mf1337D.","productDescription":"Report: 6 p.; 1 Plate: 18.1 x 15.4 inches","startPage":"1","endPage":"6","numberOfPages":"6","onlineOnly":"N","additionalOnlineFiles":"N","costCenters":[],"links":[{"id":185084,"rank":0,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/thumbnails/MF1337D.JPG"},{"id":310119,"rank":1,"type":{"id":11,"text":"Document"},"url":"https://pubs.usgs.gov/mf/1337-D/report.pdf","text":"Report","linkFileType":{"id":1,"text":"pdf"}},{"id":310120,"rank":2,"type":{"id":17,"text":"Plate"},"url":"https://pubs.usgs.gov/mf/1337-D/plate-1.pdf","text":"Plate","linkFileType":{"id":1,"text":"pdf"}}],"scale":"0","country":"United States","state":"Virginia","county":"Bedford County, Rockbridge County","geographicExtents":"{ \"type\": \"FeatureCollection\", \"features\": [ { \"type\": \"Feature\", \"properties\": {}, \"geometry\": { \"type\": \"Polygon\", \"coordinates\": [ [ [ -79.5,37.534166666666664 ], [ -79.5,37.6175 ], [ -79.36749999999999,37.6175 ], [ -79.36749999999999,37.534166666666664 ], [ -79.5,37.534166666666664 ] ] ] } } ] }","noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"4f4e4b1fe4b07f02db6ab75b","contributors":{"authors":[{"text":"Brown, C. Erwin","contributorId":96261,"corporation":false,"usgs":true,"family":"Brown","given":"C.","email":"","middleInitial":"Erwin","affiliations":[],"preferred":false,"id":261274,"contributorType":{"id":1,"text":"Authors"},"rank":1},{"text":"Gazdik, Gertrude C.","contributorId":76736,"corporation":false,"usgs":true,"family":"Gazdik","given":"Gertrude C.","affiliations":[],"preferred":false,"id":261273,"contributorType":{"id":1,"text":"Authors"},"rank":2}]}}
,{"id":46381,"text":"ofr82917 - 1982 - Map of the Antelope Valley - East Kern Water Agency area, California, showing ground-water subunits, areas, and well hydrographs (1962-82)","interactions":[],"lastModifiedDate":"2021-11-03T19:34:39.794005","indexId":"ofr82917","displayToPublicDate":"1994-01-01T00:00:00","publicationYear":"1982","noYear":false,"publicationType":{"id":18,"text":"Report"},"publicationSubtype":{"id":5,"text":"USGS Numbered Series"},"seriesTitle":{"id":330,"text":"Open-File Report","code":"OFR","onlineIssn":"2331-1258","printIssn":"0196-1497","active":true,"publicationSubtype":{"id":5}},"seriesNumber":"82-917","title":"Map of the Antelope Valley - East Kern Water Agency area, California, showing ground-water subunits, areas, and well hydrographs (1962-82)","docAbstract":"<p>No abstract available.</p>","language":"English","publisher":"U.S. Geological Survey","doi":"10.3133/ofr82917","usgsCitation":"Glenn, F.M., 1982, Map of the Antelope Valley - East Kern Water Agency area, California, showing ground-water subunits, areas, and well hydrographs (1962-82): U.S. Geological Survey Open-File Report 82-917, 1 Plate: 40.00 × 41.00 inches, https://doi.org/10.3133/ofr82917.","productDescription":"1 Plate: 40.00 × 41.00 inches","costCenters":[],"links":[{"id":168900,"rank":0,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/thumbnails/usgs_thumb.jpg"},{"id":391350,"rank":3,"type":{"id":36,"text":"NGMDB Index Page"},"url":"https://ngmdb.usgs.gov/Prodesc/proddesc_13856.htm"},{"id":20754,"rank":400,"type":{"id":17,"text":"Plate"},"url":"https://pubs.usgs.gov/of/1982/0917/plate-1.pdf","linkFileType":{"id":1,"text":"pdf"}}],"country":"United States","state":"California","otherGeospatial":"Antelope Valley - East Kern Water Agency area","geographicExtents":"{\n  \"type\": \"FeatureCollection\",\n  \"features\": [\n    {\n      \"type\": \"Feature\",\n      \"properties\": {},\n      \"geometry\": {\n        \"type\": \"Polygon\",\n        \"coordinates\": [\n          [\n            [\n              -118.75,\n              34.409\n            ],\n            [\n              -117.662,\n              34.409\n            ],\n            [\n              -117.662,\n              35.361\n            ],\n            [\n              -118.75,\n              35.361\n            ],\n            [\n              -118.75,\n              34.409\n            ]\n          ]\n        ]\n      }\n    }\n  ]\n}","noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"4f4e4a93e4b07f02db658301","contributors":{"authors":[{"text":"Glenn, Florence M.","contributorId":35293,"corporation":false,"usgs":true,"family":"Glenn","given":"Florence","email":"","middleInitial":"M.","affiliations":[],"preferred":false,"id":233190,"contributorType":{"id":1,"text":"Authors"},"rank":1}]}}
,{"id":46166,"text":"ofr8287 - 1982 - Maps showing ground-water conditions in the Bill Williams area, Mohave, Yavapai, and Yuma Counties, Arizona - 1980","interactions":[],"lastModifiedDate":"2022-07-12T22:37:02.052835","indexId":"ofr8287","displayToPublicDate":"1994-01-01T00:00:00","publicationYear":"1982","noYear":false,"publicationType":{"id":18,"text":"Report"},"publicationSubtype":{"id":5,"text":"USGS Numbered Series"},"seriesTitle":{"id":330,"text":"Open-File Report","code":"OFR","onlineIssn":"2331-1258","printIssn":"0196-1497","active":true,"publicationSubtype":{"id":5}},"seriesNumber":"82-87","title":"Maps showing ground-water conditions in the Bill Williams area, Mohave, Yavapai, and Yuma Counties, Arizona - 1980","docAbstract":"<p>The Bill Williams area includes about 3,200 mi<sup>2</sup> in Mohave, Yavapai, and Yuma Counties in west-central Arizona. The west half of the area is in the Basin and Range lowlands water province, and the east half is in the Central high-lands water province (see index map). The Basin and Range lowlands province generally is characterized by high mountains separated by broad valleys filled with deposits that commonly store large amounts of ground water. The Central highlands province consists mostly of rugged mountain masses made up of igneous, metamorphic, and well-consolidated sedimentary rocks that contain little space for the storage of ground water except where highly fractured or faulted. A few small valleys between the mountains contain varying thicknesses of water.-bearing deposits. The area is drained by the Bill Williams River and its major tributaries-the Big Sandy River and the Santa Maria River. Many reaches of the Big Sandy and Santa Maria Rivers and their major tributaries are perennial; the flow is sustained by ground-water discharge (Brown and others, 1978, sheet 2). In the Bill Williams area most of the water used is from ground water, although a small amount of surface water also may be diverted. About 18,000 acre-ft of ground water was withdrawn in 1979 (U.S. Geological Survey, 1981). About 17,000 acre-ft was used for the irrigation of 5,200 acres, and the rest was used for domestic, stock, and public supplies. Most of the irrigated land is in Skull Valley and along lower Kirkland Creek and the Bill Williams River. Only selected wells are shown on the maps in areas of high well density. The hydrologic data on which these maps are based are available, for the most part, in computer-printout form and may be consulted at the Arizona Department of Water Resources, 99 East Virginia, Phoenix, and at U.S. Geological Survey offices in: Federal Building, 301 West Congress Street, Tucson, and Valley Center, Suite 1880, Phoenix. Material from which copies can be made at private expense is available at the Tucson and Phoenix offices of the U.S. Geological Survey.</p>","language":"English","publisher":"U.S. Geological Survey","doi":"10.3133/ofr8287","collaboration":"Prepared in cooperation with the Arizona Department of Water Resources","usgsCitation":"Sanger, H.W., and Littin, G.R., 1982, Maps showing ground-water conditions in the Bill Williams area, Mohave, Yavapai, and Yuma Counties, Arizona - 1980: U.S. Geological Survey Open-File Report 82-87, 2 Plates: 50.00 × 38.44 inches and 49.36 × 37.97 inches, https://doi.org/10.3133/ofr8287.","productDescription":"2 Plates: 50.00 × 38.44 inches and 49.36 × 37.97 inches","temporalStart":"1980-01-01","temporalEnd":"1980-12-31","costCenters":[{"id":595,"text":"U.S. Geological Survey","active":false,"usgs":true}],"links":[{"id":172690,"rank":0,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/thumbnails/usgs_thumb.jpg"},{"id":83126,"rank":400,"type":{"id":17,"text":"Plate"},"url":"https://pubs.usgs.gov/of/1982/0087/plate-1.pdf","linkFileType":{"id":1,"text":"pdf"}},{"id":83127,"rank":401,"type":{"id":17,"text":"Plate"},"url":"https://pubs.usgs.gov/of/1982/0087/plate-2.pdf","linkFileType":{"id":1,"text":"pdf"}},{"id":403564,"rank":4,"type":{"id":36,"text":"NGMDB Index Page"},"url":"https://ngmdb.usgs.gov/Prodesc/proddesc_13846.htm","linkFileType":{"id":5,"text":"html"}}],"scale":"250000","country":"United States","state":"Arizona","county":"Mohave County, Yavapai County, Yuma County","otherGeospatial":"Bill Williams area","geographicExtents":"{\n  \"type\": \"FeatureCollection\",\n  \"features\": [\n    {\n      \"type\": \"Feature\",\n      \"properties\": {},\n      \"geometry\": {\n        \"type\": \"Polygon\",\n        \"coordinates\": [\n          [\n            [\n              -114.119,\n              34.035\n            ],\n            [\n              -112.542,\n              34.035\n            ],\n            [\n              -112.542,\n              34.955\n            ],\n            [\n              -114.119,\n              34.955\n            ],\n            [\n              -114.119,\n              34.035\n            ]\n          ]\n        ]\n      }\n    }\n  ]\n}","noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"4f4e4a81e4b07f02db64a0fe","contributors":{"authors":[{"text":"Sanger, H. W.","contributorId":79161,"corporation":false,"usgs":true,"family":"Sanger","given":"H.","email":"","middleInitial":"W.","affiliations":[],"preferred":false,"id":232738,"contributorType":{"id":1,"text":"Authors"},"rank":1},{"text":"Littin, G. R.","contributorId":95924,"corporation":false,"usgs":true,"family":"Littin","given":"G.","email":"","middleInitial":"R.","affiliations":[],"preferred":false,"id":232739,"contributorType":{"id":1,"text":"Authors"},"rank":2}]}}
,{"id":58624,"text":"mf1458C - 1982 - Mineral resource potential map of the Muddy Mountains Wilderness Study Area, Clark County, Nevada","interactions":[],"lastModifiedDate":"2015-10-20T11:21:30","indexId":"mf1458C","displayToPublicDate":"1994-01-01T00:00:00","publicationYear":"1982","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":"1458","chapter":"C","title":"Mineral resource potential map of the Muddy Mountains Wilderness Study Area, Clark County, Nevada","docAbstract":"<p>The Muddy Mountains Wilderness Study Area (WSA 050-0229), Clark County, Nevada, has a high potential for mineral deposits of calcium borates and lithium. The known and potential mineral deposits are concentrated in the east-central and south-central parts of the study area (see map). Zeolites (in particular clinoptilolite) are present in some tuff beds throughout much of the study area, and this resource potential is probably moderate to high. Stream-sediment sampling suggests that the Muddy Mountains area has little potential for mineral deposits of metals (other than lithium). Clay minerals are mined at one locality in the (!rea (see map). Building stone and silica sand have moderate to low potential in some places. Oil and gas potential within the study area is low, but complete evaluation of its potential is not possible without drilling.</p>","language":"English","publisher":"U.S. Geological Survey","doi":"10.3133/mf1458C","usgsCitation":"Bohannon, R.G., Leszcykowski, A.M., Esparza, L.E., and Rumsey, C.M., 1982, Mineral resource potential map of the Muddy Mountains Wilderness Study Area, Clark County, Nevada: U.S. Geological Survey Miscellaneous Field Studies Map 1458, Report: 11 p.; Plate: 43.58 x 21.94 inches, https://doi.org/10.3133/mf1458C.","productDescription":"Report: 11 p.; Plate: 43.58 x 21.94 inches","onlineOnly":"N","additionalOnlineFiles":"N","costCenters":[],"links":[{"id":184761,"rank":0,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/thumbnails/mf1458C.jpg"},{"id":310132,"rank":1,"type":{"id":11,"text":"Document"},"url":"https://pubs.usgs.gov/mf/1458-C/report.pdf","text":"Report","linkFileType":{"id":1,"text":"pdf"}},{"id":310133,"rank":2,"type":{"id":17,"text":"Plate"},"url":"https://pubs.usgs.gov/mf/1458-C/plate-1.pdf","text":"Plate","linkFileType":{"id":1,"text":"pdf"}}],"country":"United States","state":"Nevada","county":"Clark County","otherGeospatial":"Muddy Mountains Wilderness Study Area","geographicExtents":"{ \"type\": \"FeatureCollection\", \"features\": [ { \"type\": \"Feature\", \"properties\": {}, \"geometry\": { \"type\": \"Polygon\", \"coordinates\": [ [ [ -114.83333333333333,36.25 ], [ -114.83333333333333,36.333333333333336 ], [ -114.58333333333333,36.333333333333336 ], [ -114.58333333333333,36.25 ], [ -114.83333333333333,36.25 ] ] ] } } ] }","noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"4f4e4b23e4b07f02db6adec6","contributors":{"authors":[{"text":"Bohannon, Robert G. rbohannon@usgs.gov","contributorId":2255,"corporation":false,"usgs":true,"family":"Bohannon","given":"Robert","email":"rbohannon@usgs.gov","middleInitial":"G.","affiliations":[],"preferred":true,"id":260120,"contributorType":{"id":1,"text":"Authors"},"rank":1},{"text":"Leszcykowski, Andrew M.","contributorId":78387,"corporation":false,"usgs":true,"family":"Leszcykowski","given":"Andrew","email":"","middleInitial":"M.","affiliations":[],"preferred":false,"id":260122,"contributorType":{"id":1,"text":"Authors"},"rank":2},{"text":"Esparza, Leon E.","contributorId":70112,"corporation":false,"usgs":true,"family":"Esparza","given":"Leon","email":"","middleInitial":"E.","affiliations":[],"preferred":false,"id":260121,"contributorType":{"id":1,"text":"Authors"},"rank":3},{"text":"Rumsey, Clayton M.","contributorId":50514,"corporation":false,"usgs":true,"family":"Rumsey","given":"Clayton","email":"","middleInitial":"M.","affiliations":[],"preferred":false,"id":260119,"contributorType":{"id":1,"text":"Authors"},"rank":4}]}}
,{"id":59546,"text":"mf1415B - 1982 - Geochemical survey of the Cohutta Wilderness and the Hemp Top Roadless Area, northern Georgia and southeastern Tennessee","interactions":[],"lastModifiedDate":"2018-09-14T12:52:09","indexId":"mf1415B","displayToPublicDate":"1994-01-01T00:00:00","publicationYear":"1982","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":"1415","chapter":"B","title":"Geochemical survey of the Cohutta Wilderness and the Hemp Top Roadless Area, northern Georgia and southeastern Tennessee","docAbstract":"<p>The contiguous Cohutta Wilderness and Hemp Top Roadless Area are in the western part of the Blue Ridge physiographic province of northern Georgia and southeastern Tennessee (fig. 1).&nbsp; All of the study area is in Georgia except an irregular strip of land about 1 mi at its widest on the northern end of the Cohutta Wilderness in Tennessee.&nbsp; The area of the Cohutta Wilderness is 34,650 acres; that of the Hemp Top Roadless Area is 2,800 acres.&nbsp; The areas are in rugged mountainous terrain- a strongly dissected upland ranging in altitude from about 980 to 4,200 ft above sea level.&nbsp; Local altitude differences of 1,450-2,000 ft and slopes steeper than 25° are common.&nbsp; The north end of the Cohutta Wilderness is about 6 mi south of the Ocoee River gorge, 10 mi west-southwest of the major copper-and sulfur-mining district at Ducktown, Tenn., and approximately 22 mi southeast of Cleveland, Tenn., in Bradley County, west of the area shown in figure 1.&nbsp; The eastern, central, and northwestern parts of the wilderness are drained by Jacks River and it tributaries; the southwestern part, by the Conasauga River and its tributaries; and the Hemp Top Roadless Area, by Tumbling Creek and some of its western tributaries.&nbsp; All drainage ultimately goes to the Ocoee River and from these into the Hiwassee River.</p>","language":"English","publisher":"U.S. Geological Survey","doi":"10.3133/mf1415B","usgsCitation":"Gair, J.E., 1982, Geochemical survey of the Cohutta Wilderness and the Hemp Top Roadless Area, northern Georgia and southeastern Tennessee: U.S. Geological Survey Miscellaneous Field Studies Map 1415, 2 Plates: 52.33 x 39.84 inches and 48.70 x 31.49 inches, https://doi.org/10.3133/mf1415B.","productDescription":"2 Plates: 52.33 x 39.84 inches and 48.70 x 31.49 inches","costCenters":[],"links":[{"id":183161,"rank":0,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/mf/1415-B/report-thumb.jpg"},{"id":357341,"rank":2,"type":{"id":17,"text":"Plate"},"url":"https://pubs.usgs.gov/mf/1415-B/plate-1.pdf","linkFileType":{"id":1,"text":"pdf"}},{"id":357342,"rank":3,"type":{"id":17,"text":"Plate"},"url":"https://pubs.usgs.gov/mf/1415-B/plate-2.pdf","linkFileType":{"id":1,"text":"pdf"}}],"scale":"0","country":"United States","state":"Georgia, Tennessee","otherGeospatial":"Cohutta Wilderness, Hemp Top Roadless Area","geographicExtents":"{ \"type\": \"FeatureCollection\", \"features\": [ { \"type\": \"Feature\", \"properties\": {}, \"geometry\": { \"type\": \"Polygon\", \"coordinates\": [ [ [ -84.66666666666667,34.833333333333336 ], [ -84.66666666666667,35.016666666666666 ], [ -84.45083333333334,35.016666666666666 ], [ -84.45083333333334,34.833333333333336 ], [ -84.66666666666667,34.833333333333336 ] ] ] } } ] }","noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"4f4e4b20e4b07f02db6aba72","contributors":{"authors":[{"text":"Gair, Jacob E.","contributorId":18381,"corporation":false,"usgs":true,"family":"Gair","given":"Jacob","email":"","middleInitial":"E.","affiliations":[],"preferred":false,"id":262200,"contributorType":{"id":1,"text":"Authors"},"rank":1}]}}
,{"id":47274,"text":"ofr82336 - 1982 - Generalized configuration of the top of the limestone unit of the lower part of the surficial aquifer, Duval County, Florida","interactions":[],"lastModifiedDate":"2022-04-28T20:19:14.74335","indexId":"ofr82336","displayToPublicDate":"1994-01-01T00:00:00","publicationYear":"1982","noYear":false,"publicationType":{"id":18,"text":"Report"},"publicationSubtype":{"id":5,"text":"USGS Numbered Series"},"seriesTitle":{"id":330,"text":"Open-File Report","code":"OFR","onlineIssn":"2331-1258","printIssn":"0196-1497","active":true,"publicationSubtype":{"id":5}},"seriesNumber":"82-336","title":"Generalized configuration of the top of the limestone unit of the lower part of the surficial aquifer, Duval County, Florida","docAbstract":"<p>The top of the limestone unit ranges from about 25 feet above sea level in western Duval County to about 75 feet below sea level locally in the eastern part of the county. The limestone, which is part of the surficial aquifer, is the principal source of water to shallow wells in the county. The unit generally consists of a soft, friable, cavernous, sandy limestone, which ranges from about 5 to 40 feet in thickness. Along the coast and in the southern part of the county, the limestone becomes discontinuous.&nbsp;</p>","language":"English","publisher":"U.S. Geological Survey","doi":"10.3133/ofr82336","collaboration":"Prepared in cooperation with the City of Jacksonville","usgsCitation":"Spechler, R.M., 1982, Generalized configuration of the top of the limestone unit of the lower part of the surficial aquifer, Duval County, Florida: U.S. Geological Survey Open-File Report 82-336, 1 Plate: 34.92 x 28.86 inches, https://doi.org/10.3133/ofr82336.","productDescription":"1 Plate: 34.92 x 28.86 inches","costCenters":[],"links":[{"id":399852,"rank":2,"type":{"id":17,"text":"Plate"},"url":"https://pubs.usgs.gov/of/1982/0336/plate-1.pdf","linkFileType":{"id":1,"text":"pdf"}},{"id":171064,"rank":0,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/of/1982/0336/report-thumb.jpg"}],"country":"United States","state":"Florida","county":"Duval 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,{"id":8665,"text":"ofr811047 - 1982 - Analytical method codes and descriptions for well and outcrop samples: Eastern Gas Shales Project data system","interactions":[],"lastModifiedDate":"2022-08-31T19:08:57.064605","indexId":"ofr811047","displayToPublicDate":"1994-01-01T00:00:00","publicationYear":"1982","noYear":false,"publicationType":{"id":18,"text":"Report"},"publicationSubtype":{"id":5,"text":"USGS Numbered Series"},"seriesTitle":{"id":330,"text":"Open-File Report","code":"OFR","onlineIssn":"2331-1258","printIssn":"0196-1497","active":true,"publicationSubtype":{"id":5}},"seriesNumber":"81-1047","title":"Analytical method codes and descriptions for well and outcrop samples: Eastern Gas Shales Project data system","docAbstract":"<p>The United States Geological Survey and Petroleum Information Corporation (PI) of Denver have created a large computerized file of sample data for the Eastern Gas Shales Project (EGSP) as a responsibility to the U.S. Department of Energy (DOE), Morgantown Energy Technology Center (METC), Morgantown, West Virginia. The EGSP was initiated in 1976 by METC to investigate gas resources in Devonian shales found in the Appalachian basin. An objective of the EGSP is to accumulate a data base characterizing these shale units which can be used to assess future development of the gas resource. More than 30 government and industry participants served as contractors and contributed data from their research.</p>","language":"English","publisher":"U.S. Geological Survey","doi":"10.3133/ofr811047","usgsCitation":"Dyman, T.S., Wilcox, L., and Foster, M., 1982, Analytical method codes and descriptions for well and outcrop samples: Eastern Gas Shales Project data system: U.S. Geological Survey Open-File Report 81-1047, 44 p., https://doi.org/10.3133/ofr811047.","productDescription":"44 p.","costCenters":[],"links":[{"id":406018,"rank":2,"type":{"id":11,"text":"Document"},"url":"https://pubs.usgs.gov/of/1981/1047/report.pdf","linkFileType":{"id":1,"text":"pdf"}},{"id":141172,"rank":0,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/of/1981/1047/report-thumb.jpg"}],"noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"4f4e4acee4b07f02db67fa14","contributors":{"authors":[{"text":"Dyman, T. S.","contributorId":21161,"corporation":false,"usgs":false,"family":"Dyman","given":"T.","middleInitial":"S.","affiliations":[],"preferred":false,"id":158116,"contributorType":{"id":1,"text":"Authors"},"rank":1},{"text":"Wilcox, L.A.","contributorId":8098,"corporation":false,"usgs":true,"family":"Wilcox","given":"L.A.","email":"","affiliations":[],"preferred":false,"id":158115,"contributorType":{"id":1,"text":"Authors"},"rank":2},{"text":"Foster, M.R.","contributorId":82970,"corporation":false,"usgs":true,"family":"Foster","given":"M.R.","email":"","affiliations":[],"preferred":false,"id":158117,"contributorType":{"id":1,"text":"Authors"},"rank":3}]}}
,{"id":70114182,"text":"70114182 - 1982 - Earthquake history of the United States","interactions":[],"lastModifiedDate":"2014-07-15T10:39:29","indexId":"70114182","displayToPublicDate":"1985-01-01T08:28:54","publicationYear":"1982","noYear":false,"publicationType":{"id":18,"text":"Report"},"publicationSubtype":{"id":1,"text":"Federal Government Series"},"seriesTitle":{"id":63,"text":"Publication","active":false,"publicationSubtype":{"id":1}},"seriesNumber":"41-1","title":"Earthquake history of the United States","docAbstract":"<p>This publication is a history of the prominent earthquakes in the United States from historical times through 1970. It supersedes all previous editions with the same or similar titles (see page ii) and, in addition to updating earthquake listings through 1970, contains several additions and corrections to previous issues. It also brings together under a common cover earthquake data previously listed in two separate reports: <i>Earthquake History of the United States, Part I, Stronger Earthquakes of the United States (Exclusive of California and Western Nevada)</i> and <i>Earthquake History of the United States, Part II, Stronger Earthquakes of California and Western Nevada</i>. Another addition to this publication is the inclusion of a section describing earthquakes in the Puerto Rico region.</p>\n<br/>\n<p>For the purpose of listing and describing earthquakes, the United States has been divided into nine regions: (1) Northeastern Region, which includes New England and New York activity and observations of the principal earthquakes of eastern Canada; (2) Eastern Region, including the central Appalachian seismic region activity and the area near Charleston, S.C.; (3) Central Region, which consists of the area between the region just described and the Rocky Mountains; (4) Western Mountain Region, which includes all remaining states except those on the Pacific coast; (5) Washington and Oregon; (6) Alaska; (7) Hawaii; (8) Puerto Rico; and (9) California and Western Nevada. This arrangement has been made chiefly with reference to the natural seismic divisions. It also is a convenient arrangement because there are only three states where there is an important division of earthquake activity: In Tennessee, there are quite distinct areas at opposite ends of the state that fall into different regions. Only central and eastern Nevada are included in the Western Mountain Region, as the activity of the western part is closely associated with that of California. Some earthquake activity has occurred in the part of Texas located in the Western Mountain Region.</p>\n<br/>\n<p>The map facing page 1 shows locations of all earthquakes in the regions that follow. A small map showing the area covered by each region immediately precedes the résumé of each chapter (except for the Alaska, Puerto Rico, and Hawaii regions). The seismic risk map below was developed in January 1969 for the conterminous United States by Dr. S. T. Algermissen of NOAA's Environmental Research Laboratories. Subject to revision as continuing research warrants, it is an updated edition of a map divides the United States into four zones: Zone 0, areas with no reasonable expectancy of earthquake damage; Zone 1, expected minor damage; Zone 2, expected moderate damage; and Zone 3, major destructive earthquakes may occur.</p>","language":"English","publisher":"U.S. Department of Commerce, National Oceanic and Atmospheric Administration; U.S. Department of the Interior, Geological Survey","publisherLocation":"Boulder, CO","usgsCitation":"Coffman, J.L., Von Hake, C.A., and Stover, C.W., 1982, Earthquake history of the United States (Revised edition (through 1970), reprinted 1982 with supplement (1971-80)): Publication 41-1, xii, 208 p., v, 50 p.","productDescription":"xii, 208 p., v, 50 p.","numberOfPages":"277","costCenters":[],"links":[{"id":290115,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/thumbnails/outside_thumb.jpg"},{"id":290114,"type":{"id":11,"text":"Document"},"url":"https://pubs.usgs.gov/unnumbered/70114182/report.pdf"}],"country":"Canada;United States","geographicExtents":"{ \"type\": \"FeatureCollection\", \"features\": [ { \"type\": \"Feature\", \"properties\": {}, \"geometry\": { \"type\": \"Polygon\", \"coordinates\": [ [ [ 173.0,16.916667 ], [ 173.0,71.833333 ], [ -63.9832,71.833333 ], [ -63.9832,16.916667 ], [ 173.0,16.916667 ] ] ] } } ] }","edition":"Revised edition (through 1970), reprinted 1982 with supplement (1971-80)","noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"53aa9de9e4b065055fab1662","contributors":{"editors":[{"text":"Coffman, Jerry L.","contributorId":49706,"corporation":false,"usgs":true,"family":"Coffman","given":"Jerry","email":"","middleInitial":"L.","affiliations":[],"preferred":false,"id":509910,"contributorType":{"id":2,"text":"Editors"},"rank":1},{"text":"von Hake, Carl A.","contributorId":112151,"corporation":false,"usgs":true,"family":"von Hake","given":"Carl","email":"","middleInitial":"A.","affiliations":[],"preferred":false,"id":509911,"contributorType":{"id":2,"text":"Editors"},"rank":2},{"text":"Stover, Carl W.","contributorId":28955,"corporation":false,"usgs":true,"family":"Stover","given":"Carl","email":"","middleInitial":"W.","affiliations":[],"preferred":false,"id":509909,"contributorType":{"id":2,"text":"Editors"},"rank":3}],"authors":[{"text":"Coffman, Jerry L.","contributorId":49706,"corporation":false,"usgs":true,"family":"Coffman","given":"Jerry","email":"","middleInitial":"L.","affiliations":[],"preferred":false,"id":495255,"contributorType":{"id":1,"text":"Authors"},"rank":1},{"text":"Von Hake, Carl A.","contributorId":42634,"corporation":false,"usgs":true,"family":"Von Hake","given":"Carl","email":"","middleInitial":"A.","affiliations":[],"preferred":false,"id":495254,"contributorType":{"id":1,"text":"Authors"},"rank":2},{"text":"Stover, Carl W.","contributorId":28955,"corporation":false,"usgs":true,"family":"Stover","given":"Carl","email":"","middleInitial":"W.","affiliations":[],"preferred":false,"id":495253,"contributorType":{"id":1,"text":"Authors"},"rank":3}]}}
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