{"pageNumber":"2124","pageRowStart":"53075","pageSize":"25","recordCount":68919,"records":[{"id":7139,"text":"ofr82537 - 1982 - A field study of littoral processes in Estero Bay, California","interactions":[],"lastModifiedDate":"2012-02-02T00:06:08","indexId":"ofr82537","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":"82-537","title":"A field study of littoral processes in Estero Bay, California","docAbstract":"Estero Bay, which lies on the central California coast, has rocky headlands at both ends and sandy beaches within it. The shoreline of the bay has adjusted to be in equilibrium with the predominant wave climate, which is from the northwest. Because of its present shoreline configuration, the net southward littoral transport found along much of the California coast does not occur within Estero Bay. Instead, the sand primarily moves on- and offshore with a reversing longshore component. This sand transport pattern produces a littoral cell within Estero Bay even though there is no submarine canyon in the area. The primary sand sinks for this cell appear to be the sand spit south of Morro Rock and the entrance to Morro Bay itself, although this opinion was not experimentally verified. \r\n\r\nField work during one summer (1978) and the following winter (1979) produced baseline data on the profile of and grain-size distribution across the littoral zone. In the offshore part of the littoral zone we also studied ripple size and type, internal structure, depth of erosion, and mineralogy. Although these data, which were collected along nine transects spaced 2 km apart, are inadequate to yield transport and energy rates, they indicate a northward decrease in wave energy within Estero Bay and a mixing of the sediments in the offshore. Box core and rod height data from grid points in seven meters of water showed that on the order of a meter of erosion occurred in the central part of the bay between the two sampling periods. Offshore, the data were incomplete, but at one station, in 17 m of water, at least 20 cm of erosion occurred.","language":"ENGLISH","publisher":"U.S. Geological Survey,","doi":"10.3133/ofr82537","usgsCitation":"Dingler, J., Anima, R.J., Molzan, D., Luepke, G., and Peterson, C., 1982, A field study of littoral processes in Estero Bay, California: U.S. Geological Survey Open-File Report 82-537, 41 p., ill., maps ;28 cm., https://doi.org/10.3133/ofr82537.","productDescription":"41 p., ill., maps ;28 cm.","costCenters":[],"links":[{"id":141541,"rank":0,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/of/1982/0537/report-thumb.jpg"},{"id":34445,"rank":300,"type":{"id":11,"text":"Document"},"url":"https://pubs.usgs.gov/of/1982/0537/report.pdf","linkFileType":{"id":1,"text":"pdf"}}],"noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"4f4e4b24e4b07f02db6aeb7a","contributors":{"authors":[{"text":"Dingler, J.R.","contributorId":64247,"corporation":false,"usgs":true,"family":"Dingler","given":"J.R.","email":"","affiliations":[],"preferred":false,"id":154444,"contributorType":{"id":1,"text":"Authors"},"rank":1},{"text":"Anima, R. J.","contributorId":106115,"corporation":false,"usgs":true,"family":"Anima","given":"R.","email":"","middleInitial":"J.","affiliations":[],"preferred":false,"id":154446,"contributorType":{"id":1,"text":"Authors"},"rank":2},{"text":"Molzan, D.E.","contributorId":54995,"corporation":false,"usgs":true,"family":"Molzan","given":"D.E.","affiliations":[],"preferred":false,"id":154443,"contributorType":{"id":1,"text":"Authors"},"rank":3},{"text":"Luepke, Gretchen","contributorId":91827,"corporation":false,"usgs":true,"family":"Luepke","given":"Gretchen","email":"","affiliations":[],"preferred":false,"id":154445,"contributorType":{"id":1,"text":"Authors"},"rank":4},{"text":"Peterson, C.L.","contributorId":30986,"corporation":false,"usgs":true,"family":"Peterson","given":"C.L.","email":"","affiliations":[],"preferred":false,"id":154442,"contributorType":{"id":1,"text":"Authors"},"rank":5}]}}
,{"id":8906,"text":"ofr82510 - 1982 - Data for ground-water test hole near Zamora, Central Valley Aquifer Project, California","interactions":[],"lastModifiedDate":"2012-02-02T00:06:16","indexId":"ofr82510","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":"82-510","title":"Data for ground-water test hole near Zamora, Central Valley Aquifer Project, California","docAbstract":"Preliminary data are presented for the first of seven test holes drilled as a part of the Central Valley Aquifer Project which is part of the National Regional Aquifer Systems Analysis Program. The test hole was drilled in the SW 1/4 SE 1/4 sec. 34, T. 12 N. , R. 1 E., Yolo County, California, about 3 miles northeast of the town of Zamora. Drilled to a depth of 2,500 feet below land surface, the hole is cased to a depth of 190 feet and equipped with three piezometer tubes to depths of 947, 1,401, and 2,125 feet. A 5-foot well screen is at the bottom of each piezometer. Eighteen cores and 68 sidewall cores were recovered. Laboratory tests were made for mineralogy, hydraulic conductivity, porosity , consolidation, grain-size distribution, Atterberg limits, X-ray diffraction, diatom identification, thermal conductivity, and chemical analysis of water. Geophysical and thermal gradient logs were made. The hole is sampled periodically for chemical analysis and measured for water level in the three tapped zones. This report presents methods used to obtain field samples, laboratory procedures, and the data obtained. (USGS)","language":"ENGLISH","publisher":"U.S. Geological Survey,","doi":"10.3133/ofr82510","usgsCitation":"French, J., Page, R.W., and Bertoldi, G., 1982, Data for ground-water test hole near Zamora, Central Valley Aquifer Project, California: U.S. Geological Survey Open-File Report 82-510, v, 77 p. :ill., maps ;28 cm., https://doi.org/10.3133/ofr82510.","productDescription":"v, 77 p. :ill., maps ;28 cm.","costCenters":[],"links":[{"id":141746,"rank":0,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/of/1982/0510/report-thumb.jpg"},{"id":36508,"rank":400,"type":{"id":17,"text":"Plate"},"url":"https://pubs.usgs.gov/of/1982/0510/plate-1.pdf","linkFileType":{"id":1,"text":"pdf"}},{"id":36509,"rank":300,"type":{"id":11,"text":"Document"},"url":"https://pubs.usgs.gov/of/1982/0510/report.pdf","linkFileType":{"id":1,"text":"pdf"}}],"noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"4f4e4aa8e4b07f02db667b33","contributors":{"authors":[{"text":"French, J.J.","contributorId":75534,"corporation":false,"usgs":true,"family":"French","given":"J.J.","email":"","affiliations":[],"preferred":false,"id":158525,"contributorType":{"id":1,"text":"Authors"},"rank":1},{"text":"Page, R. W.","contributorId":17215,"corporation":false,"usgs":true,"family":"Page","given":"R.","email":"","middleInitial":"W.","affiliations":[],"preferred":false,"id":158524,"contributorType":{"id":1,"text":"Authors"},"rank":2},{"text":"Bertoldi, G.L.","contributorId":11605,"corporation":false,"usgs":true,"family":"Bertoldi","given":"G.L.","affiliations":[],"preferred":false,"id":158523,"contributorType":{"id":1,"text":"Authors"},"rank":3}]}}
,{"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":47680,"text":"wri834283 - 1982 - Map showing the difference between the potentiometric surfaces of the Magothy Aquifer of September 1975 and September 1982 in southern Maryland","interactions":[],"lastModifiedDate":"2012-02-02T00:10:08","indexId":"wri834283","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":"83-4283","title":"Map showing the difference between the potentiometric surfaces of the Magothy Aquifer of September 1975 and September 1982 in southern Maryland","docAbstract":"A map was prepared that shows the net change in the potentiometric surface of the Magothy aquifer in southern Maryland from September 1975 to September 1982. The map is based on measurements from a network of 55 observation wells. During the 8-year period, the potentiometric surface was (1) lowered by at least a few feet throughout the entire southern Maryland area , (2) lowered by at least 10 feet in the southern half of the area, and (3) lowered by 30 to 40 feet in most of northern Charles County. The network of observation wells was developed as part of the cooperative program between the U.S. Geological Survey, the Maryland Geological Survey, and the Maryland Energy Administration. (USGS)","language":"ENGLISH","doi":"10.3133/wri834283","usgsCitation":"Mack, F., Wheeler, J.C., and Curtin, S.E., 1982, Map showing the difference between the potentiometric surfaces of the Magothy Aquifer of September 1975 and September 1982 in southern Maryland: U.S. Geological Survey Water-Resources Investigations Report 83-4283, 1 map ; 21 x 16 cm., on sheet 28 x 22 cm., https://doi.org/10.3133/wri834283.","productDescription":"1 map ; 21 x 16 cm., on sheet 28 x 22 cm.","costCenters":[],"links":[{"id":123355,"rank":0,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/wri/1983/4283/report-thumb.jpg"},{"id":84590,"rank":300,"type":{"id":11,"text":"Document"},"url":"https://pubs.usgs.gov/wri/1983/4283/report.pdf","linkFileType":{"id":1,"text":"pdf"}}],"noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"4f4e4b12e4b07f02db6a2692","contributors":{"authors":[{"text":"Mack, Frederick K.","contributorId":95858,"corporation":false,"usgs":true,"family":"Mack","given":"Frederick K.","affiliations":[],"preferred":false,"id":235996,"contributorType":{"id":1,"text":"Authors"},"rank":1},{"text":"Wheeler, Judith C.","contributorId":13620,"corporation":false,"usgs":true,"family":"Wheeler","given":"Judith","email":"","middleInitial":"C.","affiliations":[],"preferred":false,"id":235995,"contributorType":{"id":1,"text":"Authors"},"rank":2},{"text":"Curtin, Stephen E. securtin@usgs.gov","contributorId":3703,"corporation":false,"usgs":true,"family":"Curtin","given":"Stephen","email":"securtin@usgs.gov","middleInitial":"E.","affiliations":[{"id":374,"text":"Maryland Water Science Center","active":true,"usgs":true}],"preferred":true,"id":235994,"contributorType":{"id":1,"text":"Authors"},"rank":3}]}}
,{"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":47651,"text":"wri824026 - 1982 - Map showing total thickness of the Lakota Formation and equivalent rocks, Montana","interactions":[],"lastModifiedDate":"2012-02-02T00:10:22","indexId":"wri824026","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":"82-4026","title":"Map showing total thickness of the Lakota Formation and equivalent rocks, Montana","language":"ENGLISH","doi":"10.3133/wri824026","usgsCitation":"Feltis, R.D., 1982, Map showing total thickness of the Lakota Formation and equivalent rocks, Montana: U.S. Geological Survey Water-Resources Investigations Report 82-4026, 1 map ; 45 x 68 cm., folded in envelope 25 x 32 cm., https://doi.org/10.3133/wri824026.","productDescription":"1 map ; 45 x 68 cm., folded in envelope 25 x 32 cm.","costCenters":[],"links":[{"id":169551,"rank":0,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/thumbnails/usgs_thumb.jpg"},{"id":84563,"rank":400,"type":{"id":17,"text":"Plate"},"url":"https://pubs.usgs.gov/wri/1982/4026/plate-1.pdf","linkFileType":{"id":1,"text":"pdf"}}],"noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"4f4e4a9fe4b07f02db660f5f","contributors":{"authors":[{"text":"Feltis, Richard D.","contributorId":98773,"corporation":false,"usgs":true,"family":"Feltis","given":"Richard","email":"","middleInitial":"D.","affiliations":[],"preferred":false,"id":235962,"contributorType":{"id":1,"text":"Authors"},"rank":1}]}}
,{"id":48937,"text":"ofr85635 - 1982 - Water Resources Division publications guide; Volume 1, Publications policy and text preparation","interactions":[],"lastModifiedDate":"2012-02-02T00:10:22","indexId":"ofr85635","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":"85-635","title":"Water Resources Division publications guide; Volume 1, Publications policy and text preparation","language":"ENGLISH","doi":"10.3133/ofr85635","usgsCitation":"Finch, A.J., and Aronson, D.A., 1982, Water Resources Division publications guide; Volume 1, Publications policy and text preparation: U.S. Geological Survey Open-File Report 85-635, 497 p., https://doi.org/10.3133/ofr85635.","productDescription":"497 p.","costCenters":[],"links":[{"id":170304,"rank":0,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/of/1985/0635/report-thumb.jpg"},{"id":85831,"rank":300,"type":{"id":11,"text":"Document"},"url":"https://pubs.usgs.gov/of/1985/0635/report.pdf","linkFileType":{"id":1,"text":"pdf"}}],"noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"4f4e4a08e4b07f02db5fa3f0","contributors":{"authors":[{"text":"Finch, Anne J.","contributorId":102494,"corporation":false,"usgs":true,"family":"Finch","given":"Anne","email":"","middleInitial":"J.","affiliations":[],"preferred":false,"id":238651,"contributorType":{"id":1,"text":"Authors"},"rank":1},{"text":"Aronson, David A.","contributorId":89112,"corporation":false,"usgs":true,"family":"Aronson","given":"David","email":"","middleInitial":"A.","affiliations":[],"preferred":false,"id":238650,"contributorType":{"id":1,"text":"Authors"},"rank":2}]}}
,{"id":48756,"text":"ofr82113 - 1982 - Geohydrology of the valley-fill aquifer in the Jamestown area, Chautauqua County, New York","interactions":[],"lastModifiedDate":"2022-07-08T21:04:10.800234","indexId":"ofr82113","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":"82-113","title":"Geohydrology of the valley-fill aquifer in the Jamestown area, Chautauqua County, New York","docAbstract":"This report is the sixth in a series of 11 map sets depicting geohydrologic conditions in selected aquifers in upstate New York. Geohydrologic data are compiled on six maps at 1:24,000 scale. Together, the maps provide a comprehensive overview of a major valley-fill aquifer in southeastern Chautauqua County. The maps include surficial geology, geologic sections, water-infiltration potential of soil zone, aquifer thickness, potentiometric-surface elevations and land use. The valley-fill deposits consist of alluvial silt and sand, glacial-outwash (sand and gravel), ice-contact sand and gravel, till, and lacustrine silt and clay. The sand and gravel beds have relatively high permeabilities whereas the till, silt and clay deposits have relatively low permeabilities. Water-table conditions prevail in u nconfined sand and gravel beds along the valley margin. Artesian conditions prevail in confined sand and gravel buried under silt and clay in the middle of the valley. Recharge occurs mainly along the margin of the valley, where the land surface is highly permeable and runoff from the hillsides is concentrated. The use of land overlying the aquifer is predominantly agricultural and residential with lesser amounts of commercial and industrial uses. (USGS)","language":"English","publisher":"U.S. Geological Survey","doi":"10.3133/ofr82113","usgsCitation":"Anderson, H., Stelz, W., Belli, J.L., and Allen, R.V., 1982, Geohydrology of the valley-fill aquifer in the Jamestown area, Chautauqua County, New York: U.S. Geological Survey Open-File Report 82-113, 7 Plates: 34.32 × 29.14 inches or smaller, https://doi.org/10.3133/ofr82113.","productDescription":"7 Plates: 34.32 × 29.14 inches or smaller","costCenters":[],"links":[{"id":85560,"rank":404,"type":{"id":17,"text":"Plate"},"url":"https://pubs.usgs.gov/of/1982/0113/plate-5.pdf","linkFileType":{"id":1,"text":"pdf"}},{"id":85558,"rank":402,"type":{"id":17,"text":"Plate"},"url":"https://pubs.usgs.gov/of/1982/0113/plate-3.pdf","linkFileType":{"id":1,"text":"pdf"}},{"id":85557,"rank":401,"type":{"id":17,"text":"Plate"},"url":"https://pubs.usgs.gov/of/1982/0113/plate-2.pdf","linkFileType":{"id":1,"text":"pdf"}},{"id":85562,"rank":406,"type":{"id":17,"text":"Plate"},"url":"https://pubs.usgs.gov/of/1982/0113/plate-7.pdf","linkFileType":{"id":1,"text":"pdf"}},{"id":85561,"rank":405,"type":{"id":17,"text":"Plate"},"url":"https://pubs.usgs.gov/of/1982/0113/plate-6.pdf","linkFileType":{"id":1,"text":"pdf"}},{"id":85559,"rank":403,"type":{"id":17,"text":"Plate"},"url":"https://pubs.usgs.gov/of/1982/0113/plate-4.pdf","linkFileType":{"id":1,"text":"pdf"}},{"id":85556,"rank":400,"type":{"id":17,"text":"Plate"},"url":"https://pubs.usgs.gov/of/1982/0113/plate-1.pdf","linkFileType":{"id":1,"text":"pdf"}},{"id":162482,"rank":0,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/thumbnails/usgs_thumb.jpg"},{"id":403322,"rank":9,"type":{"id":36,"text":"NGMDB Index Page"},"url":"https://ngmdb.usgs.gov/Prodesc/proddesc_45789.htm","linkFileType":{"id":5,"text":"html"}}],"country":"United States","state":"New York","county":"Chautauqua County","otherGeospatial":"Jamestown area","geographicExtents":"{\n  \"type\": \"FeatureCollection\",\n  \"features\": [\n    {\n      \"type\": \"Feature\",\n      \"properties\": {},\n      \"geometry\": {\n        \"type\": \"Polygon\",\n        \"coordinates\": [\n          [\n            [\n              -79.292,\n              42.083\n            ],\n            [\n              -79.083,\n              42.083\n            ],\n            [\n              -79.083,\n              42.208\n            ],\n            [\n              -79.292,\n              42.208\n            ],\n            [\n              -79.292,\n              42.083\n            ]\n          ]\n        ]\n      }\n    }\n  ]\n}","noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"4f4e4b1ae4b07f02db6a87bf","contributors":{"authors":[{"text":"Anderson, H. R.","contributorId":67487,"corporation":false,"usgs":true,"family":"Anderson","given":"H. R.","affiliations":[],"preferred":false,"id":238160,"contributorType":{"id":1,"text":"Authors"},"rank":1},{"text":"Stelz, W. G.","contributorId":72837,"corporation":false,"usgs":true,"family":"Stelz","given":"W. G.","affiliations":[],"preferred":false,"id":238161,"contributorType":{"id":1,"text":"Authors"},"rank":2},{"text":"Belli, J. L.","contributorId":83561,"corporation":false,"usgs":true,"family":"Belli","given":"J.","email":"","middleInitial":"L.","affiliations":[],"preferred":false,"id":238162,"contributorType":{"id":1,"text":"Authors"},"rank":3},{"text":"Allen, R. V.","contributorId":100862,"corporation":false,"usgs":true,"family":"Allen","given":"R.","email":"","middleInitial":"V.","affiliations":[],"preferred":false,"id":238163,"contributorType":{"id":1,"text":"Authors"},"rank":4}]}}
,{"id":8777,"text":"ofr82775 - 1982 - Hydrology of the Arbuckle Mountain area, south-central Oklahoma","interactions":[{"subject":{"id":8777,"text":"ofr82775 - 1982 - Hydrology of the Arbuckle Mountain area, south-central Oklahoma","indexId":"ofr82775","publicationYear":"1982","noYear":false,"title":"Hydrology of the Arbuckle Mountain area, south-central Oklahoma"},"predicate":"SUPERSEDED_BY","object":{"id":70046124,"text":"70046124 - 1990 - Hydrology of the Arbuckle Mountains area, south-central Oklahoma","indexId":"70046124","publicationYear":"1990","noYear":false,"title":"Hydrology of the Arbuckle Mountains area, south-central Oklahoma"},"id":1}],"supersededBy":{"id":70046124,"text":"70046124 - 1990 - Hydrology of the Arbuckle Mountains area, south-central Oklahoma","indexId":"70046124","publicationYear":"1990","noYear":false,"title":"Hydrology of the Arbuckle Mountains area, south-central Oklahoma"},"lastModifiedDate":"2017-09-29T07:50:47","indexId":"ofr82775","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":"82-775","title":"Hydrology of the Arbuckle Mountain area, south-central Oklahoma","docAbstract":"<p>Rocks that make up the Arbuckle-Simpson aquifer crop out over about 500 square miles in the Arbuckle Mountains province in south-central Oklahoma. The aquifer consists of limestone, dolomite, and sandstone of the Arbuckle and Simpson Groups of Late Cambrian to Middle Ordovician age and is about 5,000 to 9,000 feet thick. The rocks were subjected to intensive folding and faulting associated with major uplift of the area during Early to Late Pennsylvanian time. </p><p>Water in the aquifer is confined in some parts of the area, while in other parts it is unconfined. The average saturated thickness of the aquifer is about 3,500 feet in the outcrop area. Water levels measured in wells fluctuated from 8 to 53 feet each year, primarily in response to recharge from rainfall. </p><p>Recharge to the aquifer is estimated at about 4.7 inches per year. </p><p>The average storage coefficient of the aquifer is estimated at 0.008, and the average transmissivity is estimated at 15,000 feet squared per day. Based on an average saturated thickness of about 3,500 feet and a storage coefficient of 0.008, the volume of ground water contained in the 500-square-mile outcrop area is about 9 million acre-feet. An undetermined amount of fresh water probably exists in the aquifer around the periphery of the aquifer outcrop. </p><p>Base flow of streams that drain the aquifer accounts for about 60 percent of the total annual runoff from the outcrop area and is maintained by numerous springs. The close hydraulic connection between streams in the outcrop area and the aquifer is shown by a close correlation between base flow in Blue River and the fluctuation of ground-water levels in five wells in the Blue River basin. This correlation also exists between the discharge by Byrds Mill Spring and the fluctuation in water level in a nearby observation well; increase and decrease in spring discharge correspond to rise and fall of the water level in the well. </p><p>The chemical quality of water from the Arbuckle-Simpson aquifer is suitable for most industrial and municipal uses. The water is hard and of the bicarbonate type; the average hardness is about 340 milligrams per liter, and the average dissolved-solids concentration is about 360 milligrams per liter. Because springs issue from the aquifer and discharge to streams in the area, the quality of water from springs and base flow in streams is similar to that of ground water. The average dissolved-solids concentration of stream water is slightly less than that of water from wells and springs.&nbsp;</p>","language":"English","publisher":"U.S. Geological Survey","doi":"10.3133/ofr82775","usgsCitation":"Fairchild, R.W., Hanson, R.L., and Davis, R.E., 1982, Hydrology of the Arbuckle Mountain area, south-central Oklahoma: U.S. Geological Survey Open-File Report 82-775, 156 p., https://doi.org/10.3133/ofr82775.","productDescription":"156 p.","numberOfPages":"170","costCenters":[],"links":[{"id":346189,"rank":2,"type":{"id":11,"text":"Document"},"url":"https://pubs.usgs.gov/of/1982/0775/report.pdf","linkFileType":{"id":1,"text":"pdf"}},{"id":143402,"rank":0,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/of/1982/0775/report-thumb.jpg"}],"country":"United States","state":"Oklahoma","geographicExtents":"{\n  \"type\": \"FeatureCollection\",\n  \"features\": [\n    {\n      \"type\": \"Feature\",\n      \"properties\": {},\n      \"geometry\": {\n        \"type\": \"Polygon\",\n        \"coordinates\": [\n          [\n            [\n              -97.37182617187499,\n              34.16295449004889\n            ],\n            [\n              -96.41189575195312,\n              34.16295449004889\n            ],\n            [\n              -96.41189575195312,\n              34.73484137177769\n            ],\n            [\n              -97.37182617187499,\n              34.73484137177769\n            ],\n            [\n              -97.37182617187499,\n              34.16295449004889\n            ]\n          ]\n        ]\n      }\n    }\n  ]\n}","noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"4f4e4a13e4b07f02db601ee9","contributors":{"authors":[{"text":"Fairchild, Roy W.","contributorId":79155,"corporation":false,"usgs":true,"family":"Fairchild","given":"Roy","email":"","middleInitial":"W.","affiliations":[],"preferred":false,"id":158313,"contributorType":{"id":1,"text":"Authors"},"rank":1},{"text":"Hanson, Ronald L.","contributorId":65054,"corporation":false,"usgs":true,"family":"Hanson","given":"Ronald","email":"","middleInitial":"L.","affiliations":[],"preferred":false,"id":158311,"contributorType":{"id":1,"text":"Authors"},"rank":2},{"text":"Davis, Robert E.","contributorId":10403,"corporation":false,"usgs":true,"family":"Davis","given":"Robert","email":"","middleInitial":"E.","affiliations":[],"preferred":false,"id":158312,"contributorType":{"id":1,"text":"Authors"},"rank":3}]}}
,{"id":8822,"text":"ofr82354 - 1982 - Chemical and physical characteristics of water in estuaries of Texas, October 1976-September 1978","interactions":[],"lastModifiedDate":"2016-08-11T14:46:56","indexId":"ofr82354","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":"82-354","title":"Chemical and physical characteristics of water in estuaries of Texas, October 1976-September 1978","docAbstract":"<p>The Texas Water Plan (1968) proposes development and utilization of water resources in Texas and includes provision for the use and preservation of water in the estuaries of the State. Management of estuarine waters requires knowledge of the hydrodynamics and of the continuing changes in the chemical and physical characteristics of water in the estuaries.</p>\n<p>In September 1967, the U.S. Geological Survey and the Texas Department of Water Resources began a cooperative water-resources investigation of the principal estuaries along the Texas coast (fig. 1) except the Rio Grande estuary,&nbsp;which is under the jurisdiction of the International Boundary and Water Commission, United States and Mexico.</p>\n<p>The objectives of the investigation are to define: (1) The occurrence, source, and distribution of nutrients; (2) the physical, organic, and inorganic water-quality constituents and their areal distribution and time variations; (3) the chemical and physical characteristics of Gulf water that enters the estuaries; (4) the occurrence, quality, quantity, and dispersion of drainage entering the estuarine systems; and (5) the current patterns, directions, and rates of water movement.</p>\n<p>The coastal waters of Texas are not classical estuaries, but are similar to them in ecosystems and mixing phenomena. A description of various types of estuaries is presented in \"Estuaries\" edited by Lauff (1967, p. 3-11). The term estuary as used in this report, refers to concomitant water bodies in which streamflow mixes with seawater.</p>","language":"English","publisher":"U.S. Geological Survey","publisherLocation":"Austin, TX","doi":"10.3133/ofr82354","usgsCitation":"Fisher, J., 1982, Chemical and physical characteristics of water in estuaries of Texas, October 1976-September 1978: U.S. Geological Survey Open-File Report 82-354, Report: 213 p.; 3 Plates: 9.90 x 14.91 inches or smaller, https://doi.org/10.3133/ofr82354.","productDescription":"Report: 213 p.; 3 Plates: 9.90 x 14.91 inches or smaller","onlineOnly":"N","additionalOnlineFiles":"N","costCenters":[{"id":583,"text":"Texas Water Science Center","active":true,"usgs":true}],"links":[{"id":141691,"rank":0,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/of/1982/0354/report-thumb.jpg"},{"id":36397,"rank":400,"type":{"id":17,"text":"Plate"},"url":"https://pubs.usgs.gov/of/1982/0354/plate-1.pdf","linkFileType":{"id":1,"text":"pdf"}},{"id":36398,"rank":401,"type":{"id":17,"text":"Plate"},"url":"https://pubs.usgs.gov/of/1982/0354/plate-2.pdf","linkFileType":{"id":1,"text":"pdf"}},{"id":36399,"rank":402,"type":{"id":17,"text":"Plate"},"url":"https://pubs.usgs.gov/of/1982/0354/plate-3.pdf","linkFileType":{"id":1,"text":"pdf"}},{"id":36400,"rank":300,"type":{"id":11,"text":"Document"},"url":"https://pubs.usgs.gov/of/1982/0354/report.pdf","linkFileType":{"id":1,"text":"pdf"}}],"noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"4f4e49e1e4b07f02db5e47f9","contributors":{"authors":[{"text":"Fisher, J.C.","contributorId":99974,"corporation":false,"usgs":true,"family":"Fisher","given":"J.C.","email":"","affiliations":[],"preferred":false,"id":158389,"contributorType":{"id":1,"text":"Authors"},"rank":1}]}}
,{"id":42129,"text":"ofr821083 - 1982 - Aeromagnetic map of the Sierra Owens area, California","interactions":[],"lastModifiedDate":"2012-02-02T00:11:06","indexId":"ofr821083","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":"82-1083","title":"Aeromagnetic map of the Sierra Owens area, California","language":"ENGLISH","doi":"10.3133/ofr821083","usgsCitation":"Water Resources Division, U.S. Geological Survey, 1982, Aeromagnetic map of the Sierra Owens area, California: U.S. Geological Survey Open-File Report 82-1083, 1 map ;79 x 65 cm., https://doi.org/10.3133/ofr821083.","productDescription":"1 map ;79 x 65 cm.","costCenters":[],"links":[{"id":168686,"rank":0,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/thumbnails/usgs_thumb.jpg"},{"id":79862,"rank":400,"type":{"id":17,"text":"Plate"},"url":"https://pubs.usgs.gov/of/1982/1083/plate-1.pdf","linkFileType":{"id":1,"text":"pdf"}}],"noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"4f4e4aeee4b07f02db6911fa","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":530854,"contributorType":{"id":1,"text":"Authors"},"rank":1}]}}
,{"id":1287,"text":"wsp2199 - 1982 - Verification of step-backwater computations on ephemeral streams in northeastern Wyoming","interactions":[],"lastModifiedDate":"2017-09-20T16:40:25","indexId":"wsp2199","displayToPublicDate":"1994-01-01T00:00:00","publicationYear":"1982","noYear":false,"publicationType":{"id":18,"text":"Report"},"publicationSubtype":{"id":5,"text":"USGS Numbered Series"},"seriesTitle":{"id":341,"text":"Water Supply Paper","code":"WSP","active":false,"publicationSubtype":{"id":5}},"seriesNumber":"2199","title":"Verification of step-backwater computations on ephemeral streams in northeastern Wyoming","docAbstract":"Step-backwater computations were verified by subsequent discharge measurements at three ephemeral streamflow stations in northeastern Wyoming. The standard step-backwater method for gradually varied, subcritical flow was used in computing the water-surface profiles and stage-discharge ratings. Step-backwater computations were made at selected intervals from I through 1,000 cubic feet per second on Lodgepole Creek, through 150 cubic feet per second on Raven Creek, and through 600 cubic feet per second on Sand Creek. Stage-discharge rating curves and discharge measurements are illustrated for the three sites, with lines of 15-percent departure from the rating curves drawn to measure accuracy of the results. All discharge measurements showed departures of less than 15 percent at the high end of the rating curves.","language":"ENGLISH","publisher":"U.S. G.P.O.,","doi":"10.3133/wsp2199","usgsCitation":"Druse, S.A., 1982, Verification of step-backwater computations on ephemeral streams in northeastern Wyoming: U.S. Geological Survey Water Supply Paper 2199, iii, 12 p. :ill., maps ;28 cm., https://doi.org/10.3133/wsp2199.","productDescription":"iii, 12 p. :ill., maps ;28 cm.","costCenters":[{"id":5050,"text":"WY-MT Water Science Center","active":true,"usgs":true}],"links":[{"id":136999,"rank":0,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/wsp/2199/report-thumb.jpg"},{"id":26256,"rank":300,"type":{"id":11,"text":"Document"},"url":"https://pubs.usgs.gov/wsp/2199/report.pdf","linkFileType":{"id":1,"text":"pdf"}}],"noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"4f4e4a13e4b07f02db6021b5","contributors":{"authors":[{"text":"Druse, Stanley A.","contributorId":7252,"corporation":false,"usgs":true,"family":"Druse","given":"Stanley","email":"","middleInitial":"A.","affiliations":[],"preferred":false,"id":143503,"contributorType":{"id":1,"text":"Authors"},"rank":1}]}}
,{"id":28216,"text":"wri824048 - 1982 - Time of travel of selected Arkansas streams","interactions":[],"lastModifiedDate":"2012-02-02T00:08:52","indexId":"wri824048","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":"82-4048","title":"Time of travel of selected Arkansas streams","docAbstract":"Between 1971 and 1981, time-of-travel and dispersion measurements were made in 15 streams in Arkansas. Most of the streams studied were at or near base flow. Graphs are presented for predicting traveltime of solutes in segments of the streams studied. The relationship of time of passage and peak unit concentration to traveltime is presented for two of the streams. Examples of use and application of the data are given. (USGS)","language":"ENGLISH","publisher":"U.S. Geological Survey,","doi":"10.3133/wri824048","usgsCitation":"Lamb, T., 1982, Time of travel of selected Arkansas streams: U.S. Geological Survey Water-Resources Investigations Report 82-4048, v, 64 p. :ill., maps ;28 cm., https://doi.org/10.3133/wri824048.","productDescription":"v, 64 p. :ill., maps ;28 cm.","costCenters":[],"links":[{"id":159652,"rank":0,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/wri/1982/4048/report-thumb.jpg"},{"id":57050,"rank":300,"type":{"id":11,"text":"Document"},"url":"https://pubs.usgs.gov/wri/1982/4048/report.pdf","linkFileType":{"id":1,"text":"pdf"}}],"noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"4f4e4b05e4b07f02db699c84","contributors":{"authors":[{"text":"Lamb, T.E.","contributorId":58272,"corporation":false,"usgs":true,"family":"Lamb","given":"T.E.","email":"","affiliations":[],"preferred":false,"id":199410,"contributorType":{"id":1,"text":"Authors"},"rank":1}]}}
,{"id":26845,"text":"wri824107 - 1982 - Machine-readable data files from the Madison Limestone and northern Great Plains regional aquifer system analysis projects, Montana, Nebraska, North Dakota, South Dakota, and Wyoming","interactions":[],"lastModifiedDate":"2012-02-02T00:08:21","indexId":"wri824107","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":"82-4107","title":"Machine-readable data files from the Madison Limestone and northern Great Plains regional aquifer system analysis projects, Montana, Nebraska, North Dakota, South Dakota, and Wyoming","docAbstract":"Lists of machine-readable data files were developed for the Madison Limestone and Northern Great Plains Regional Aquifer System Analysis (RASA) projects. They are stored on magnetic tape and available from the U.S. Geological Survey. Record format, file content, and size are given for: (1) Drill-stem-test data for Paleozoic and Mesozoic formations, (2) geologic data from the Madison Limestone project, (3) data sets used in the regional simulation model, (4) head data for the Lower and Upper Cretaceous aquifers, and (5) geologic data for Mesozoic formations of the Northern Great Plains. (USGS)","language":"ENGLISH","publisher":"U.S. Geological Survey,","doi":"10.3133/wri824107","usgsCitation":"Downey, J.S., 1982, Machine-readable data files from the Madison Limestone and northern Great Plains regional aquifer system analysis projects, Montana, Nebraska, North Dakota, South Dakota, and Wyoming: U.S. Geological Survey Water-Resources Investigations Report 82-4107, iv, 30 p. :ill. ;28 cm., https://doi.org/10.3133/wri824107.","productDescription":"iv, 30 p. :ill. ;28 cm.","costCenters":[],"links":[{"id":122712,"rank":0,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/wri/1982/4107/report-thumb.jpg"},{"id":55736,"rank":300,"type":{"id":11,"text":"Document"},"url":"https://pubs.usgs.gov/wri/1982/4107/report.pdf","linkFileType":{"id":1,"text":"pdf"}}],"noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"4f4e4a7fe4b07f02db6490ac","contributors":{"authors":[{"text":"Downey, J. S.","contributorId":100013,"corporation":false,"usgs":true,"family":"Downey","given":"J.","email":"","middleInitial":"S.","affiliations":[],"preferred":false,"id":197106,"contributorType":{"id":1,"text":"Authors"},"rank":1}]}}
,{"id":43692,"text":"ofr82258 - 1982 - Hydrologic maps of Ogallala Aquifer, west-central Kansas, 1979-81","interactions":[],"lastModifiedDate":"2012-02-02T00:10:10","indexId":"ofr82258","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":"82-258","title":"Hydrologic maps of Ogallala Aquifer, west-central Kansas, 1979-81","docAbstract":"A mathematical technique, called kriging, was programmed for a computer to interpolate hydrologic data based on a network of measured values in west-central Kansas. The computer program generated estimated values at the center of each 1-mile section in the Western Kansas Groundwater Management District No. 1 and facilitated contouring of selected hydrologic data that are needed in the effective management of ground water for irrigation. The kriging technique produced various maps that illustrated hydrologic conditions in the Ogallala aquifer, the principal source of water in west-central Kansas. Maps of the aquifer, which use a 3-year average, included the 1979-81 water-table altitudes, which ranged from about 2,580 to 3,720 feet; the 1979-81 saturated thicknesses, which ranged from about 0 to 250 feet; and the percentage changes in saturated thickness from 1950 to 1979-81, which ranged from about a 40-percent increase to a 100-percent decrease. A map showing errors of estimate also was provided as a measure of reliability for the 1979-81 water-table altitudes. Errors of estimate ranged from 2 to 24 feet. (USGS)","language":"ENGLISH","doi":"10.3133/ofr82258","usgsCitation":"Spinazola, J.M., 1982, Hydrologic maps of Ogallala Aquifer, west-central Kansas, 1979-81: U.S. Geological Survey Open-File Report 82-258, 4 maps on 4 sheets :photocopy ;62 x 126 cm., https://doi.org/10.3133/ofr82258.","productDescription":"4 maps on 4 sheets :photocopy ;62 x 126 cm.","costCenters":[],"links":[{"id":162526,"rank":0,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/thumbnails/usgs_thumb.jpg"},{"id":20547,"rank":400,"type":{"id":17,"text":"Plate"},"url":"https://pubs.usgs.gov/of/1982/0258/plate-1.pdf","linkFileType":{"id":1,"text":"pdf"}},{"id":20548,"rank":401,"type":{"id":17,"text":"Plate"},"url":"https://pubs.usgs.gov/of/1982/0258/plate-2.pdf","linkFileType":{"id":1,"text":"pdf"}},{"id":20549,"rank":402,"type":{"id":17,"text":"Plate"},"url":"https://pubs.usgs.gov/of/1982/0258/plate-3.pdf","linkFileType":{"id":1,"text":"pdf"}},{"id":20550,"rank":403,"type":{"id":17,"text":"Plate"},"url":"https://pubs.usgs.gov/of/1982/0258/plate-4.pdf","linkFileType":{"id":1,"text":"pdf"}}],"noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"4f4e4a1ae4b07f02db6067a2","contributors":{"authors":[{"text":"Spinazola, Joseph M.","contributorId":102044,"corporation":false,"usgs":true,"family":"Spinazola","given":"Joseph","email":"","middleInitial":"M.","affiliations":[],"preferred":false,"id":228566,"contributorType":{"id":1,"text":"Authors"},"rank":1}]}}
,{"id":1719,"text":"wsp2079 - 1982 - An annotated key to the identification of commonly occurring and dominant genera of algae observed in the phytoplankton of the United States","interactions":[],"lastModifiedDate":"2012-02-02T00:05:15","indexId":"wsp2079","displayToPublicDate":"1994-01-01T00:00:00","publicationYear":"1982","noYear":false,"publicationType":{"id":18,"text":"Report"},"publicationSubtype":{"id":5,"text":"USGS Numbered Series"},"seriesTitle":{"id":341,"text":"Water Supply Paper","code":"WSP","active":false,"publicationSubtype":{"id":5}},"seriesNumber":"2079","title":"An annotated key to the identification of commonly occurring and dominant genera of algae observed in the phytoplankton of the United States","docAbstract":"In early 1979, a retrieval was made for all phytoplankton data contained in the computerized data file of the U. S. Geological Survey. The retrieval revealed the analytical results of 17,959 samples collected and processed between October 1973 and October 1978. Of the approximately 500 genera of freshwater algae reported in the United States, the U.S. Geological Survey observed 321 genera in the phytoplankton. Fifty-two genera were considered to be commonly occurring and 42 genera were considered to be community dominants. The report lists, describes, and provides a detailed taxonomic key to the identification of 58 genera of algae considered either commonly occurring or dominant. Also included is a summary of environmental conditions under which each algal genus was observed, as well as a glossary and an extensive list of selected references.","language":"ENGLISH","publisher":"U.S. G.P.O.,","doi":"10.3133/wsp2079","usgsCitation":"Greeson, P.E., 1982, An annotated key to the identification of commonly occurring and dominant genera of algae observed in the phytoplankton of the United States: U.S. Geological Survey Water Supply Paper 2079, vi, 138 p. :ill. ;24 cm., https://doi.org/10.3133/wsp2079.","productDescription":"vi, 138 p. :ill. ;24 cm.","costCenters":[],"links":[{"id":136941,"rank":0,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/wsp/2079/report-thumb.jpg"},{"id":26807,"rank":300,"type":{"id":11,"text":"Document"},"url":"https://pubs.usgs.gov/wsp/2079/report.pdf","linkFileType":{"id":1,"text":"pdf"}}],"noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"4f4e4adae4b07f02db685770","contributors":{"authors":[{"text":"Greeson, Phillip E.","contributorId":25556,"corporation":false,"usgs":true,"family":"Greeson","given":"Phillip","email":"","middleInitial":"E.","affiliations":[],"preferred":false,"id":144012,"contributorType":{"id":1,"text":"Authors"},"rank":1}]}}
,{"id":8793,"text":"ofr82324 - 1982 - Radioactivity and geochemistry of selected mineral-spring waters in the Western United States; basic data and multivariate statistical analysis","interactions":[],"lastModifiedDate":"2012-02-02T00:06:19","indexId":"ofr82324","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":"82-324","title":"Radioactivity and geochemistry of selected mineral-spring waters in the Western United States; basic data and multivariate statistical analysis","docAbstract":"Multivariate statistical analyses were performed on data from 156 mineral-spring sites in nine Western States to analyze relationships among the various parameters measured in the spring waters. Correlation analysis and R-mode factor analysis indicate that three major factors affect water composition in the spring systems studied: (1) duration of water circulation, (2) depth of water circulation, and (3) partial pressure of carbon dioxide. An examination of factor scores indicates that several types of hydrogeologic systems were sampled. Most of the samples are (1) older water from deeper circulating systems having relatively high salinity, high temperature, and low Eh or (2) younger water from shallower circulating systems having relatively low salinity, low temperature, and high Eh. The rest of the samples are from more complex systems. Any of the systems can have a relatively high or low content of dissolved carbonate species, resulting in a low or high pH, respectively. Uranium concentrations are commonly higher in waters of relatively low temperature and high Eh, and radium concentrations are commonly higher in waters having a relatively high carbonate content (low pH) and, secondarily, relatively high salinity. \r\n\r\nWater samples were collected and (or) measurements were taken at 156 of the 171 mineral-spring sites visited. Various samples were analyzed for radium, uranium, radon, helium, and radium-228 as well as major ions and numerous trace elements. On-site measurements for physical properties including temperature, specific conductance, pH, Eh, and dissolved oxygen were made. All constituents and properties show a wide range of values. Radium concentrations range from less than 0.01 to 300 picocuries per liter; they average 1.48 picocuries per liter and have an anomaly threshold value of 171 picocuries per liter for the samples studied. Uranium concentrations range from less than 0.01 to 120 micrograms per liter and average 0.26 micrograms per liter; they have an anomaly threshold value of 48.1 micrograms per liter. Radon content ranges from less than 10 to 110,000 picocuries per liter, averages 549 picocuries per liter and has an anomaly threshold of 20,400 picocuries per liter. Helium content ranges from -1,300 to +13,000 parts per billion relative to atmospheric helium; it averages +725 parts per billion and has an anomaly threshold of 10,000 parts per billion. Radium-228 concentrations range from less than 2.0 to 33 picocuries per liter; no anomaly threshold was determined owing to the small number of samples. All of the anomaly thresholds may be somewhat high because the sampling was biased toward springs likely to be radioactive. \r\n\r\nThe statistical variance in radium and uranium concentrations unaccounted for by the identified factors testifies to the complexity of some hydrogeologic systems. Unidentified factors related to geologic setting and the presence of uranium-rich rocks in the systems also affect the observed concentrations of the radioactive elements in the water. The association of anomalous radioactivity in several springs with nearby known uranium occurrences indicates that other springs having anomalous radioactivity may also be associated with uranium occurrences as yet undiscovered.","language":"ENGLISH","publisher":"U.S. Geological Survey,","doi":"10.3133/ofr82324","usgsCitation":"Felmlee, J., and Cadigan, R.A., 1982, Radioactivity and geochemistry of selected mineral-spring waters in the Western United States; basic data and multivariate statistical analysis: U.S. Geological Survey Open-File Report 82-324, ii, 107 p. :ill., maps ;28 cm., https://doi.org/10.3133/ofr82324.","productDescription":"ii, 107 p. :ill., maps ;28 cm.","costCenters":[],"links":[{"id":142733,"rank":0,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/of/1982/0324/report-thumb.jpg"},{"id":36377,"rank":300,"type":{"id":11,"text":"Document"},"url":"https://pubs.usgs.gov/of/1982/0324/report.pdf","linkFileType":{"id":1,"text":"pdf"}}],"noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"4f4e4a60e4b07f02db634cbd","contributors":{"authors":[{"text":"Felmlee, J.K.","contributorId":106114,"corporation":false,"usgs":true,"family":"Felmlee","given":"J.K.","email":"","affiliations":[],"preferred":false,"id":158341,"contributorType":{"id":1,"text":"Authors"},"rank":1},{"text":"Cadigan, R. A.","contributorId":57844,"corporation":false,"usgs":true,"family":"Cadigan","given":"R.","email":"","middleInitial":"A.","affiliations":[],"preferred":false,"id":158340,"contributorType":{"id":1,"text":"Authors"},"rank":2}]}}
,{"id":1310,"text":"wsp2196B - 1982 - Production and decomposition of forest litter fall on the Apalachicola River flood plain, Florida: Chapter B, Apalachicola River quality assessment","interactions":[{"subject":{"id":8725,"text":"ofr82252 - 1982 - Production and decomposition of forest litter fall on the Apalachicola River flood plain, Florida","indexId":"ofr82252","publicationYear":"1982","noYear":false,"title":"Production and decomposition of forest litter fall on the Apalachicola River flood plain, Florida"},"predicate":"SUPERSEDED_BY","object":{"id":1310,"text":"wsp2196B - 1982 - Production and decomposition of forest litter fall on the Apalachicola River flood plain, Florida: Chapter B, Apalachicola River quality assessment","indexId":"wsp2196B","publicationYear":"1982","noYear":false,"chapter":"B","title":"Production and decomposition of forest litter fall on the Apalachicola River flood plain, Florida: Chapter B, Apalachicola River quality assessment"},"id":1}],"lastModifiedDate":"2012-02-02T00:05:17","indexId":"wsp2196B","displayToPublicDate":"1994-01-01T00:00:00","publicationYear":"1982","noYear":false,"publicationType":{"id":18,"text":"Report"},"publicationSubtype":{"id":5,"text":"USGS Numbered Series"},"seriesTitle":{"id":341,"text":"Water Supply Paper","code":"WSP","active":false,"publicationSubtype":{"id":5}},"seriesNumber":"2196","chapter":"B","title":"Production and decomposition of forest litter fall on the Apalachicola River flood plain, Florida: Chapter B, Apalachicola River quality assessment","docAbstract":"Measurements of litter fall (leaves and other particulate organic material) and leaf decomposition were made on the bottom-land hardwood swamp of the Apalachicola River flood plain in 1979-80. Litter fall was collected monthly from nets located in 16 study plots. The plots represented five forest types in the swamp and levee areas of the Apalachicola River flood plain. Forty-three species of trees, vines, and other plants contributed to the total litter fall, but more than 90 percent of the leaf material originated from 12 species. Nonleaf material made up 42 percent of the total litter fall. Average litter fall was determined to be 800 grams per square meter per year, resulting in an annual deposition of 3.6 ? 105 metric tons of organic material in the 454-square-kilometer flood plain. \r\n\r\nThe levee communities have less tree biomass but greater tree diversity than do swamp communities. The levee vegetation, containing less tree biomass, produces slightly more litter fall per unit of ground surface area than does the swamp vegetation. The swamps are dominated by three genera: tupelo (Nyssa), cypress (Taxodium) and ash (Fraxinus). These genera account for more than 50 percent of the total leaf fall in the flood plain, but they are the least productive, on a weight-perbiomass basis, of any of the 12 major leaf producers. \r\n\r\nDecomposition rates of leaves from five common floodplain tree species were measured using a standard leaf-bag technique. Leaf decomposition was highly species dependent. Tupelo (Nyssa spp.) and sweetgum (Liquidambar styraciflua) leaves decomposed completely in 6 months when flooded by river water. Leaves of baldcypress (Taxodium distichum) and diamond-leaf oak (Quercus laurifolia) were much more resistant. Water hickory (Carya aquatica) leaves showed intermediate decomposition rates. Decomposition of all species was greatly reduced in dry environments. Carbon and biomass loss rates from the leaves were nearly linear over a 6-month period, but nitrogen and phosphorus leaching was nearly complete within 1 month. Much of the organic substance may be recycled in the forest ecosystem, but annual flooding of the river provides an important mechanism for mobilization of the litter-fall products.","language":"ENGLISH","publisher":"U.S. G.P.O.,","doi":"10.3133/wsp2196B","usgsCitation":"Elder, J.F., and Cairns, D.J., 1982, Production and decomposition of forest litter fall on the Apalachicola River flood plain, Florida: Chapter B, Apalachicola River quality assessment: U.S. Geological Survey Water Supply Paper 2196, v, 42 p. :ill. (some col.), maps ;28 cm., https://doi.org/10.3133/wsp2196B.","productDescription":"v, 42 p. :ill. (some col.), maps ;28 cm.","costCenters":[],"links":[{"id":138035,"rank":0,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/wsp/2196b/report-thumb.jpg"},{"id":26343,"rank":300,"type":{"id":11,"text":"Document"},"url":"https://pubs.usgs.gov/wsp/2196b/report.pdf","linkFileType":{"id":1,"text":"pdf"}}],"noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"4f4e4a8be4b07f02db651db7","contributors":{"authors":[{"text":"Elder, John F.","contributorId":23919,"corporation":false,"usgs":true,"family":"Elder","given":"John","email":"","middleInitial":"F.","affiliations":[{"id":595,"text":"U.S. Geological Survey","active":false,"usgs":true}],"preferred":false,"id":143542,"contributorType":{"id":1,"text":"Authors"},"rank":1},{"text":"Cairns, Duncan J.","contributorId":52152,"corporation":false,"usgs":true,"family":"Cairns","given":"Duncan","email":"","middleInitial":"J.","affiliations":[],"preferred":false,"id":143543,"contributorType":{"id":1,"text":"Authors"},"rank":2}]}}
,{"id":43293,"text":"ofr82228 - 1982 - Land use and land cover and associated maps for Belleville, Illinois; Indiana","interactions":[],"lastModifiedDate":"2012-02-02T00:10:10","indexId":"ofr82228","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":"82-228","title":"Land use and land cover and associated maps for Belleville, Illinois; Indiana","language":"ENGLISH","doi":"10.3133/ofr82228","usgsCitation":"Water Resources Division, U.S. Geological Survey, 1982, Land use and land cover and associated maps for Belleville, Illinois; Indiana: U.S. Geological Survey Open-File Report 82-228, maps ;45 x 70 cm., https://doi.org/10.3133/ofr82228.","productDescription":"maps ;45 x 70 cm.","costCenters":[],"links":[{"id":161601,"rank":0,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/thumbnails/usgs_thumb.jpg"}],"noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"4f4e4b28e4b07f02db6b1700","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":531097,"contributorType":{"id":1,"text":"Authors"},"rank":1}]}}
,{"id":57534,"text":"wdrFL812A - 1982 - Water resources data, Florida, water year 1981; Volume 2A. South Florida surface water","interactions":[],"lastModifiedDate":"2023-01-13T19:48:05.779624","indexId":"wdrFL812A","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":"FL-81-2A","title":"Water resources data, Florida, water year 1981; Volume 2A. South Florida surface water","docAbstract":"<p>Water resources data for the 1981 water year for south Florida consist of records of stage, discharge, and water quality of streams; elevation and water quality of lakes and reservoirs; water-levels and water quality of wells; and discharge and water quality of springs. Additional water data were collected at various sites, not part of the systematic data collection program, and are published as miscellaneous measurements. These data represent that part of the National Water Data System operated by the U.S. Geological Survey and cooperating state and federal agencies in Florida.</p>","language":"English","publisher":"U.S. Geological Survey","doi":"10.3133/wdrFL812A","collaboration":"Prepared in cooperation with the State of Florida and with other agencies","usgsCitation":"Water Resources Division, U.S. Geological Survey, 1982, Water resources data, Florida, water year 1981; Volume 2A. 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,{"id":9968,"text":"wri82444 - 1982 - Water use in Wisconsin, 1979","interactions":[],"lastModifiedDate":"2015-10-08T13:37:47","indexId":"wri82444","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":"82-444","title":"Water use in Wisconsin, 1979","docAbstract":"<p>This report summarizes the uses of water in Wisconsin for 1979, except aesthetics, navigation, and recreational use.</p>\n<p>The greatest single use of water, an instream use, was for hydroelectric power production. About 26 trillion gallons, or 93 percent, was used for this purpose. Of the other 7 percent where water is pumped to a different location, 81 percent (6 percent of all water use) was cooling water for thermoelectric powerplants.</p>\n<p>Withdrawals of surface water and ground water by public and private systems are for residential, industrial, commercial, irrigation, and stock uses.</p>","language":"English","publisher":"U.S. Geological Survey","doi":"10.3133/wri82444","collaboration":"Prepared in cooperation with the Wisconsin Department of Natural Resources","usgsCitation":"Lawrence, C., and Ellefson, B., 1982, Water use in Wisconsin, 1979: U.S. Geological Survey Water-Resources Investigations Report 82-444, iv, 102 p., https://doi.org/10.3133/wri82444.","productDescription":"iv, 102 p.","numberOfPages":"106","onlineOnly":"N","additionalOnlineFiles":"N","costCenters":[{"id":677,"text":"Wisconsin Water Science 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,{"id":27190,"text":"wri824106 - 1982 - Effects of volcanic ash on the benthic environment of a mountain stream, northern Idaho","interactions":[],"lastModifiedDate":"2013-11-21T13:32:31","indexId":"wri824106","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":"82-4106","title":"Effects of volcanic ash on the benthic environment of a mountain stream, northern Idaho","docAbstract":"The May 18, 1980, eruption of Mount St. Helens deposited about 15 millimeters of volcanic ash on the Big Creek basin in northern Idaho. Much of the uncompacted ash remained on hillsides a year after the eruption. Physical and chemical analyses of water samples from Big Creek collected from December 1980 to December 1981 showed no anomalies attributable to ash. Qualitative collections showed benthic invertebrates to be abundant and diverse in Big Creek. Experiments conducted in an unimpacted mountain stream revealed a small quantity of volcanic ash may be beneficial not detrimental to invertebrate communities. Benthic invertebrates were most abundant on ash-covered artificial substrates, with detritovores dominating the communities on all substrates. (USGS)","language":"English","publisher":"U.S. Geological Survey","doi":"10.3133/wri824106","usgsCitation":"Frenzel, S., 1982, Effects of volcanic ash on the benthic environment of a mountain stream, northern Idaho: U.S. Geological Survey Water-Resources Investigations Report 82-4106, iii, 32 p., https://doi.org/10.3133/wri824106.","productDescription":"iii, 32 p.","numberOfPages":"37","costCenters":[{"id":343,"text":"Idaho Water Science Center","active":true,"usgs":true}],"links":[{"id":123146,"rank":0,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/wri/1982/4106/report-thumb.jpg"},{"id":56065,"rank":300,"type":{"id":11,"text":"Document"},"url":"https://pubs.usgs.gov/wri/1982/4106/report.pdf","linkFileType":{"id":1,"text":"pdf"}}],"country":"United States","state":"Idaho","otherGeospatial":"Big Creek Basin;Gedney Creek Basin","geographicExtents":"{ \"type\": \"FeatureCollection\", \"features\": [ { \"type\": \"Feature\", \"properties\": {}, \"geometry\": { \"type\": \"Polygon\", \"coordinates\": [ [ [ -117.0,46.0 ], [ -117.0,48.0 ], [ -114.5,48.0 ], [ -114.5,46.0 ], [ -117.0,46.0 ] ] ] } } ] }","noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"4f4e4ad6e4b07f02db68426a","contributors":{"authors":[{"text":"Frenzel, S.A.","contributorId":9246,"corporation":false,"usgs":true,"family":"Frenzel","given":"S.A.","email":"","affiliations":[],"preferred":false,"id":197712,"contributorType":{"id":1,"text":"Authors"},"rank":1}]}}
,{"id":4421,"text":"cir875 - 1982 - U.S. Geological Survey activities, fiscal year 1981","interactions":[],"lastModifiedDate":"2012-02-02T00:05:28","indexId":"cir875","displayToPublicDate":"1994-01-01T00:00:00","publicationYear":"1982","noYear":false,"publicationType":{"id":18,"text":"Report"},"publicationSubtype":{"id":5,"text":"USGS Numbered Series"},"seriesTitle":{"id":307,"text":"Circular","code":"CIR","onlineIssn":"2330-5703","printIssn":"1067-084X","active":true,"publicationSubtype":{"id":5}},"seriesNumber":"875","title":"U.S. Geological Survey activities, fiscal year 1981","docAbstract":"This U.S. Geological Survey Activities report for fiscal year 1981 presents a summary of the work performed between October 1, 1980 and September 30, 1981. The main sections of this report are: (1) The Year in Review; a brief overview of the significant events of the Geological Survey during fiscal year 1980; (2) Perspectives; essays focusing on specific events (rather than scientific topics) and programs involving multi-Division participation; (3) Missions, Organization, and Budget; a description of the Geological Survey 's major duties and assignments and of the organizational structure that supports its missions; and (4) Division Chapters; a description of the significant accomplishments (rather than a comprehensive program by program discussion) of each of the eight operating Divisions and Offices. Also included are supplementary information regarding key personnel, cooperators, and selected summary budgetary tables. (USGS)","language":"ENGLISH","publisher":"U.S. Geological Survey,","doi":"10.3133/cir875","usgsCitation":"Water Resources Division, U.S. Geological Survey, 1982, U.S. Geological Survey activities, fiscal year 1981: U.S. Geological Survey Circular 875, v, 161 p. :ill. ;26 cm., https://doi.org/10.3133/cir875.","productDescription":"v, 161 p. :ill. ;26 cm.","costCenters":[],"links":[{"id":117572,"rank":0,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/circ/1982/0875/report-thumb.jpg"},{"id":31526,"rank":300,"type":{"id":11,"text":"Document"},"url":"https://pubs.usgs.gov/circ/1982/0875/report.pdf","linkFileType":{"id":1,"text":"pdf"}}],"noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"4f4e4a53e4b07f02db62b40e","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":528221,"contributorType":{"id":1,"text":"Authors"},"rank":1}]}}
,{"id":8590,"text":"ofr82486 - 1982 - Survey of helium in natural water wells and springs in southwest Montana and vicinity, and Imperial Valley, California; Part IV, Jan. 1-Dec. 31, 1981","interactions":[],"lastModifiedDate":"2012-02-02T00:06:09","indexId":"ofr82486","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":"82-486","title":"Survey of helium in natural water wells and springs in southwest Montana and vicinity, and Imperial Valley, California; Part IV, Jan. 1-Dec. 31, 1981","language":"ENGLISH","publisher":"U.S. Geological Survey,","doi":"10.3133/ofr82486","usgsCitation":"Doering, W.P., and Friedman, I., 1982, Survey of helium in natural water wells and springs in southwest Montana and vicinity, and Imperial Valley, California; Part IV, Jan. 1-Dec. 31, 1981: U.S. Geological Survey Open-File Report 82-486, 33 p. ill., maps ;28 cm., https://doi.org/10.3133/ofr82486.","productDescription":"33 p. ill., maps ;28 cm.","costCenters":[],"links":[{"id":141071,"rank":0,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/of/1982/0486/report-thumb.jpg"},{"id":36184,"rank":300,"type":{"id":11,"text":"Document"},"url":"https://pubs.usgs.gov/of/1982/0486/report.pdf","linkFileType":{"id":1,"text":"pdf"}}],"noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"4f4e4ae1e4b07f02db688807","contributors":{"authors":[{"text":"Doering, W. P.","contributorId":7270,"corporation":false,"usgs":true,"family":"Doering","given":"W.","email":"","middleInitial":"P.","affiliations":[],"preferred":false,"id":157995,"contributorType":{"id":1,"text":"Authors"},"rank":1},{"text":"Friedman, Irving","contributorId":90664,"corporation":false,"usgs":true,"family":"Friedman","given":"Irving","email":"","affiliations":[],"preferred":false,"id":157996,"contributorType":{"id":1,"text":"Authors"},"rank":2}]}}
,{"id":27184,"text":"wri824015 - 1982 - Estimates of vertical hydraulic conductivity and regional ground-water flow rates in rocks of Jurassic and Cretaceous age, San Juan Basin, New Mexico and Colorado","interactions":[],"lastModifiedDate":"2012-02-02T00:08:26","indexId":"wri824015","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":"82-4015","title":"Estimates of vertical hydraulic conductivity and regional ground-water flow rates in rocks of Jurassic and Cretaceous age, San Juan Basin, New Mexico and Colorado","docAbstract":"The San Juan structural basin northwestern New Mexico was modeled in three dimensions using a finite-difference, steady-state model. The modeled space was divided into seven layers of square prisms that were 6 miles on a side in the horizontal directions. In the vertical direction, the layers of prisms ranged in thickness from 300 to 1,500 feet. The model included the geologic section between the base of the Entrada Sandstone and the top of Mesaverde Group. Principal aquifers in this section are mostly confined and include the Entrada Sandstone, the Westwater Canyon Member of the Morrison Formation , and the Gallup Sandstone. Values for vertical hydraulic conductivities from 10 to the minus 12th power to 10 to the minus 11th power feet per second for the confining layers gave a good simulation of head differences between layers, but a sensitivity analysis indicated that these values could be between 10 and 100 times greater. The model-derived steady-state flow was about 30 cubic feet per second. About one-half of the flow was in the San Juan River drainage basin about one-third in the Rio Grande drainage basin, and one-sixth in the Puerco River drainage basin. (USGS)","language":"ENGLISH","publisher":"U.S. Geological Survey,","doi":"10.3133/wri824015","usgsCitation":"Frenzel, P.F., and Lyford, F.P., 1982, Estimates of vertical hydraulic conductivity and regional ground-water flow rates in rocks of Jurassic and Cretaceous age, San Juan Basin, New Mexico and Colorado: U.S. Geological Survey Water-Resources Investigations Report 82-4015, viii, 67 p. :ill., maps ;28 cm., https://doi.org/10.3133/wri824015.","productDescription":"viii, 67 p. :ill., maps ;28 cm.","costCenters":[],"links":[{"id":123082,"rank":0,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/wri/1982/4015/report-thumb.jpg"},{"id":56058,"rank":300,"type":{"id":11,"text":"Document"},"url":"https://pubs.usgs.gov/wri/1982/4015/report.pdf","linkFileType":{"id":1,"text":"pdf"}}],"noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"4f4e4a0ce4b07f02db5fca36","contributors":{"authors":[{"text":"Frenzel, P. F.","contributorId":98726,"corporation":false,"usgs":true,"family":"Frenzel","given":"P.","email":"","middleInitial":"F.","affiliations":[],"preferred":false,"id":197705,"contributorType":{"id":1,"text":"Authors"},"rank":1},{"text":"Lyford, F. P.","contributorId":30223,"corporation":false,"usgs":true,"family":"Lyford","given":"F.","email":"","middleInitial":"P.","affiliations":[],"preferred":false,"id":197704,"contributorType":{"id":1,"text":"Authors"},"rank":2}]}}
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