{"pageNumber":"350","pageRowStart":"8725","pageSize":"25","recordCount":11004,"records":[{"id":20205,"text":"ofr84445 - 1984 - Effects of brine on the chemical quality of water in parts of Creek, Lincoln, Okfuskee, Payne, Pottawatomie, and Seminole counties, Oklahoma","interactions":[{"subject":{"id":20205,"text":"ofr84445 - 1984 - Effects of brine on the chemical quality of water in parts of Creek, Lincoln, Okfuskee, Payne, Pottawatomie, and Seminole counties, Oklahoma","indexId":"ofr84445","publicationYear":"1984","noYear":false,"title":"Effects of brine on the chemical quality of water in parts of Creek, Lincoln, Okfuskee, Payne, Pottawatomie, and Seminole counties, Oklahoma"},"predicate":"SUPERSEDED_BY","object":{"id":70044324,"text":"70044324 - 1986 - Effects of brine on the chemical quality of water in parts of Creek, Lincoln, Okfuskee, Payne, Pottawatomie, and Seminole Counties, Oklahoma","indexId":"70044324","publicationYear":"1986","noYear":false,"title":"Effects of brine on the chemical quality of water in parts of Creek, Lincoln, Okfuskee, Payne, Pottawatomie, and Seminole Counties, Oklahoma"},"id":1}],"supersededBy":{"id":70044324,"text":"70044324 - 1986 - Effects of brine on the chemical quality of water in parts of Creek, Lincoln, Okfuskee, Payne, Pottawatomie, and Seminole Counties, Oklahoma","indexId":"70044324","publicationYear":"1986","noYear":false,"title":"Effects of brine on the chemical quality of water in parts of Creek, Lincoln, Okfuskee, Payne, Pottawatomie, and Seminole Counties, Oklahoma"},"lastModifiedDate":"2017-12-06T13:00:27","indexId":"ofr84445","displayToPublicDate":"1994-01-01T00:00:00","publicationYear":"1984","noYear":false,"publicationType":{"id":18,"text":"Report"},"publicationSubtype":{"id":5,"text":"USGS Numbered Series"},"seriesTitle":{"id":330,"text":"Open-File Report","code":"OFR","onlineIssn":"2331-1258","printIssn":"0196-1497","active":true,"publicationSubtype":{"id":5}},"seriesNumber":"84-445","title":"Effects of brine on the chemical quality of water in parts of Creek, Lincoln, Okfuskee, Payne, Pottawatomie, and Seminole counties, Oklahoma","docAbstract":"

A study of water-quality degradation due to brine contamination was made in an area of about 1,700 square miles in east-central Oklahoma. The study area coincides, in part, with the outcrop of the Vamoosa-Ada aquifer of Pennsylvanian age.

Water samples collected from 180 wells completed in the Vamoosa-Ada aquifer, and at 168 sites from streams draining the Vamoosa-Ada aquifer show scattered occurrences of water-quality degradation by brine. Degradation of water quality by brine is indicated where: (1) Chloride concentration is equal to or greater than 400 milligrams per liter (2) bromide concentration is equal to or greater than 2 milligrams per liter (3) the ratio of lithium to sodium is equal to or less than 0.01, and the chloride concentration is equal to or greater than 400 milligrams per liter, or (4) the ratio of sodium plus chloride to dissolved solids is equal to or greater than 0.64. Other ratios of secondary importance that also indicate water-quality degradation by brine in the area are (1) a sodium/chloride ratio of about 0.46; (2) a sodium/bromide ratio of about 92; and (3) a bromide/chloride ratio of about 0.0048.

","language":"English","publisher":"U.S. Geological Survey","doi":"10.3133/ofr84445","usgsCitation":"Morton, R.B., 1984, Effects of brine on the chemical quality of water in parts of Creek, Lincoln, Okfuskee, Payne, Pottawatomie, and Seminole counties, Oklahoma: U.S. Geological Survey Open-File Report 84-445, Report: 105 p.; Plate: 38.14 x 25.40 inches; Figures 2-9, https://doi.org/10.3133/ofr84445.","productDescription":"Report: 105 p.; Plate: 38.14 x 25.40 inches; Figures 2-9","costCenters":[],"links":[{"id":152355,"rank":0,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/of/1984/0445/report-thumb.jpg"},{"id":349777,"rank":2,"type":{"id":11,"text":"Document"},"url":"https://pubs.usgs.gov/of/1984/0445/report.pdf","linkFileType":{"id":1,"text":"pdf"}},{"id":349778,"rank":3,"type":{"id":17,"text":"Plate"},"url":"https://pubs.usgs.gov/of/1984/0445/plate-1.pdf","text":"Plate 1","linkFileType":{"id":1,"text":"pdf"}},{"id":349779,"rank":4,"type":{"id":29,"text":"Figure"},"url":"https://pubs.usgs.gov/of/1984/0445/figure-2.pdf","text":"Figure 2","linkFileType":{"id":1,"text":"pdf"}},{"id":349780,"rank":5,"type":{"id":29,"text":"Figure"},"url":"https://pubs.usgs.gov/of/1984/0445/figure-3.pdf","text":"Figure 3","linkFileType":{"id":1,"text":"pdf"}},{"id":349781,"rank":6,"type":{"id":29,"text":"Figure"},"url":"https://pubs.usgs.gov/of/1984/0445/figure-4.pdf","text":"Figure 4","linkFileType":{"id":1,"text":"pdf"}},{"id":349782,"rank":7,"type":{"id":29,"text":"Figure"},"url":"https://pubs.usgs.gov/of/1984/0445/figure-5.pdf","text":"Figure 5","linkFileType":{"id":1,"text":"pdf"}},{"id":349784,"rank":9,"type":{"id":29,"text":"Figure"},"url":"https://pubs.usgs.gov/of/1984/0445/figure-7.pdf","text":"Figure 7","linkFileType":{"id":1,"text":"pdf"}},{"id":349783,"rank":8,"type":{"id":29,"text":"Figure"},"url":"https://pubs.usgs.gov/of/1984/0445/figure-6.pdf","text":"Figure 6","linkFileType":{"id":1,"text":"pdf"}},{"id":349785,"rank":10,"type":{"id":29,"text":"Figure"},"url":"https://pubs.usgs.gov/of/1984/0445/figure-8.pdf","text":"Figure 8","linkFileType":{"id":1,"text":"pdf"}},{"id":349786,"rank":11,"type":{"id":29,"text":"Figure"},"url":"https://pubs.usgs.gov/of/1984/0445/figure-9.pdf","text":"Figure 9","linkFileType":{"id":1,"text":"pdf"}}],"country":"United States","state":"Oklahoma","county":"Creek County, Lincoln County, Okfuskee County, Payne County, Pottawatomie County, Seminole County","geographicExtents":"{\"type\":\"FeatureCollection\",\"features\":[{\"type\":\"Feature\",\"geometry\":{\"type\":\"Polygon\",\"coordinates\":[[[-96.3006,36.1632],[-96.3002,36.1577],[-96.2991,36.0778],[-96.085,36.0773],[-96.0281,36.0764],[-96.0288,36.0006],[-96.0286,35.9906],[-96.0304,35.9026],[-96.0326,35.9027],[-96.0319,35.8565],[-96.1928,35.8589],[-96.1936,35.6365],[-96.1944,35.553],[-96.0898,35.5532],[-96.0892,35.3756],[-95.9803,35.3751],[-95.9809,35.2896],[-96.4413,35.2902],[-96.4393,35.1158],[-96.4932,35.116],[-96.4944,35.0275],[-96.4961,34.9076],[-96.5043,34.8978],[-96.5046,34.8878],[-96.5128,34.8775],[-96.5237,34.8678],[-96.5344,34.8671],[-96.5437,34.875],[-96.5585,34.9026],[-96.5572,34.9085],[-96.5608,34.919],[-96.5675,34.9205],[-96.5749,34.9156],[-96.585,34.9163],[-96.5872,34.9159],[-96.5924,34.911],[-96.5975,34.9088],[-96.6045,34.9031],[-96.6186,34.9006],[-96.6337,34.8996],[-96.646,34.9016],[-96.6559,34.9068],[-96.658,34.9123],[-96.6615,34.9274],[-96.6726,34.9312],[-96.6831,34.9364],[-96.6932,34.9357],[-96.7017,34.9314],[-96.7081,34.9242],[-96.715,34.9189],[-96.7146,34.9139],[-96.7074,34.9092],[-96.6986,34.9036],[-96.6927,34.8953],[-96.6891,34.8866],[-96.6921,34.8776],[-96.6951,34.8726],[-96.7032,34.8646],[-96.706,34.8633],[-96.7151,34.858],[-96.732,34.8566],[-96.7391,34.8612],[-96.7411,34.8694],[-96.7465,34.8782],[-96.7529,34.8906],[-96.7549,34.897],[-96.7626,34.9026],[-96.7681,34.9054],[-96.7783,34.9015],[-96.7823,34.8988],[-96.7896,34.899],[-96.7912,34.9004],[-96.7989,34.9087],[-96.8005,34.9119],[-96.7998,34.9142],[-96.7998,34.9332],[-96.8013,34.9396],[-96.8035,34.9419],[-96.8197,34.9431],[-96.8237,34.9428],[-96.8311,34.9393],[-96.8329,34.9357],[-96.8346,34.9348],[-96.8397,34.9326],[-96.8419,34.9336],[-96.843,34.9354],[-96.8446,34.9363],[-96.8599,34.9294],[-96.8668,34.9268],[-96.8785,34.9265],[-96.8902,34.9295],[-96.8991,34.9337],[-96.9041,34.937],[-96.9051,34.9406],[-96.9033,34.9456],[-96.906,34.9497],[-96.9087,34.952],[-96.9086,34.9548],[-96.9096,34.9598],[-96.914,34.963],[-96.9218,34.9654],[-96.933,34.9665],[-96.9431,34.9658],[-96.9494,34.9618],[-96.9563,34.9533],[-96.9627,34.9448],[-96.9662,34.9403],[-96.9685,34.9376],[-96.9709,34.935],[-96.9817,34.9265],[-96.9921,34.9176],[-97.0068,34.9106],[-97.0147,34.9094],[-97.0169,34.9099],[-97.0253,34.9104],[-97.0453,34.918],[-97.0537,34.9205],[-97.0621,34.9202],[-97.0715,34.9244],[-97.0797,34.9318],[-97.0859,34.9328],[-97.1027,34.9313],[-97.1161,34.9356],[-97.1285,34.9344],[-97.1432,34.9305],[-97.1433,35.2021],[-97.1405,35.202],[-97.1442,35.3742],[-97.1437,35.4645],[-97.1452,35.6361],[-97.1436,35.7246],[-97.1438,35.8112],[-97.1433,35.8988],[-97.1405,35.8988],[-97.1409,35.9283],[-97.1428,35.9442],[-97.1423,35.9641],[-97.1557,35.9485],[-97.1729,35.9428],[-97.1872,35.9426],[-97.2013,35.9469],[-97.2163,35.9576],[-97.2252,35.9677],[-97.236,35.9683],[-97.2461,35.9721],[-97.2523,35.9744],[-97.2734,35.9734],[-97.2841,35.9767],[-97.2863,35.9795],[-97.2862,35.9835],[-97.2883,35.9931],[-97.2927,36.0004],[-97.2982,36.0091],[-97.3055,36.011],[-97.3203,36.0108],[-97.3329,36.0078],[-97.3359,36.0024],[-97.34,35.9947],[-97.3475,35.9885],[-97.3556,35.9841],[-97.3569,36.1583],[-97.1426,36.1588],[-97.1417,36.245],[-96.9277,36.246],[-96.8216,36.245],[-96.8212,36.1593],[-96.6245,36.1605],[-96.6244,36.1628],[-96.4294,36.1642],[-96.4232,36.1641],[-96.4175,36.1644],[-96.4118,36.1643],[-96.4072,36.1642],[-96.3947,36.1639],[-96.3758,36.1639],[-96.3673,36.1637],[-96.3365,36.1635],[-96.3297,36.1634],[-96.3058,36.1633],[-96.3006,36.1632]]]},\"properties\":{\"name\":\"Creek\",\"state\":\"OK\"}}]}","noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"4f4e4a4ae4b07f02db624974","contributors":{"authors":[{"text":"Morton, Robert B.","contributorId":50899,"corporation":false,"usgs":true,"family":"Morton","given":"Robert","email":"","middleInitial":"B.","affiliations":[],"preferred":false,"id":182249,"contributorType":{"id":1,"text":"Authors"},"rank":1}]}} ,{"id":40338,"text":"ofr84587 - 1984 - Compilation of selected geophysical references for the Snake River plain, Idaho and eastern Oregon","interactions":[{"subject":{"id":40338,"text":"ofr84587 - 1984 - Compilation of selected geophysical references for the Snake River plain, Idaho and eastern Oregon","indexId":"ofr84587","publicationYear":"1984","noYear":false,"title":"Compilation of selected geophysical references for the Snake River plain, Idaho and eastern Oregon"},"predicate":"SUPERSEDED_BY","object":{"id":63495,"text":"gp969 - 1986 - Compilation of selected geophysical references for the Snake River plain, Idaho and eastern Oregon","indexId":"gp969","publicationYear":"1986","noYear":false,"title":"Compilation of selected geophysical references for the Snake River plain, Idaho and eastern Oregon"},"id":1}],"supersededBy":{"id":63495,"text":"gp969 - 1986 - Compilation of selected geophysical references for the Snake River plain, Idaho and eastern Oregon","indexId":"gp969","publicationYear":"1986","noYear":false,"title":"Compilation of selected geophysical references for the Snake River plain, Idaho and eastern Oregon"},"lastModifiedDate":"2024-01-22T21:06:48.839996","indexId":"ofr84587","displayToPublicDate":"1994-01-01T00:00:00","publicationYear":"1984","noYear":false,"publicationType":{"id":18,"text":"Report"},"publicationSubtype":{"id":5,"text":"USGS Numbered Series"},"seriesTitle":{"id":330,"text":"Open-File Report","code":"OFR","onlineIssn":"2331-1258","printIssn":"0196-1497","active":true,"publicationSubtype":{"id":5}},"seriesNumber":"84-587","title":"Compilation of selected geophysical references for the Snake River plain, Idaho and eastern Oregon","docAbstract":"

This report is one in a series resulting from the U.S. Geological Survey's Snake River Plain RASA (Regional Aquifer System Analysis) study that began in October 1979. 

","language":"English","publisher":"U.S. Geological Survey","doi":"10.3133/ofr84587","usgsCitation":"Whitehead, R., 1984, Compilation of selected geophysical references for the Snake River plain, Idaho and eastern Oregon: U.S. Geological Survey Open-File Report 84-587, Report: 1 p.; 1 Plate: 54.96 x 35.97 inches, https://doi.org/10.3133/ofr84587.","productDescription":"Report: 1 p.; 1 Plate: 54.96 x 35.97 inches","costCenters":[],"links":[{"id":424703,"rank":3,"type":{"id":17,"text":"Plate"},"url":"https://pubs.usgs.gov/of/1984/0587/plate-1.pdf","linkFileType":{"id":1,"text":"pdf"}},{"id":424702,"rank":2,"type":{"id":11,"text":"Document"},"url":"https://pubs.usgs.gov/of/1984/0587/report.pdf","linkFileType":{"id":1,"text":"pdf"}},{"id":135467,"rank":1,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/of/1984/0587/report-thumb.jpg"}],"scale":"500000","country":"United States","state":"Idaho, Oregon","otherGeospatial":"Snake River plain","geographicExtents":"{\n \"type\": \"FeatureCollection\",\n \"features\": [\n {\n \"type\": \"Feature\",\n \"properties\": {},\n \"geometry\": {\n \"coordinates\": [\n [\n [\n -119.79353516529073,\n 44.75814253835162\n ],\n [\n -119.79353516529073,\n 42.00600446943071\n ],\n [\n -111.1325958997702,\n 42.00600446943071\n ],\n [\n -111.1325958997702,\n 44.75814253835162\n ],\n [\n -119.79353516529073,\n 44.75814253835162\n ]\n ]\n ],\n \"type\": \"Polygon\"\n }\n }\n ]\n}","noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"4f4e4b1de4b07f02db6a9722","contributors":{"authors":[{"text":"Whitehead, R.L.","contributorId":34891,"corporation":false,"usgs":true,"family":"Whitehead","given":"R.L.","email":"","affiliations":[],"preferred":false,"id":223291,"contributorType":{"id":1,"text":"Authors"},"rank":1}]}} ,{"id":25971,"text":"wri844194 - 1984 - Evaluation of the hydrologic system and potential effects of mining in the Dickinson lignite area, eastern slope and western Stark and Hettinger counties, North Dakota","interactions":[],"lastModifiedDate":"2018-02-14T15:41:55","indexId":"wri844194","displayToPublicDate":"1994-01-01T00:00:00","publicationYear":"1984","noYear":false,"publicationType":{"id":18,"text":"Report"},"publicationSubtype":{"id":5,"text":"USGS Numbered Series"},"seriesTitle":{"id":342,"text":"Water-Resources Investigations Report","code":"WRI","active":false,"publicationSubtype":{"id":5}},"seriesNumber":"84-4194","title":"Evaluation of the hydrologic system and potential effects of mining in the Dickinson lignite area, eastern slope and western Stark and Hettinger counties, North Dakota","docAbstract":"

The investigation of the water resources of the Dickinson lignite area, an area of about 500 square miles, was undertaken to define the hydrologic system of the area and to project probable effects of coal mining on the system.

Aquifers occur in sandstone beds in: the Fox Hills Sandstone and the lower Hell Creek Formation of Cretaceous age, the upper Hell Creek Formation of Cretaceous age and the lower Ludlow Member of the Fort Union Formation of Tertiary age, and the upper Ludlow and lower Tongue River Members of the Fort Union Formation of Tertiary age. Aquifers also occur in the sandstone and lignite lenses in the upper Tongue River Member and the Sentinel Butte Member of the Fort Union Formation.

Depths to the Fox Hills-lower Hell Creek aquifer system range from about 1,300 to 1,710 feet. Well yields range from 18 to 100 gallons per minute. The water is soft and is a sodium bicarbonate type. Dissolvedsolids concentrations in samples collected from the aquifer system ranged from 1,230 to 1,690 milligrams per liter.

Depths to the upper Hell Creek-lower Ludlow aquifer system range from about 720 to 1,040 feet. Well yields generally are less than 30 gallons per minute but may be as much as 150 gallons per minute. The water is soft and a sodium bicarbonate type. Dissolved-solids concentrations in samples collected from the aquifer system ranged from 1,010 to 1,450 milligrams per liter.

Depths to the upper Ludlow-lower Tongue River aquifer system range from about 440 to 713 feet. Well yields may range from about 1 to 100 gallons per minute. The water generally is soft and a sodium bicarbonate type but may be moderately hard and a sulfate type in the southwestern part of the area. Dissolved-solids concentrations in samples collected from the aquifer system ranged from 995 to 1,990 milligrams per liter.

Depths to the upper Tongue River-Sentinel Butte aquifer system range from near land surface to about 530 feet below land surface. Well yields generally range from about 1 to 185 gallons per minute. Yields from the lignite parts of the system range from about 2 to 60 gallons per minute. The water generally is a sodium bicarbonate type, but locally sulfate is the dominant anion. Dissolved-solids concentrations in samples collected from the aquifer system generally ranged from 574 to 2,720 milligrams per liter.

","language":"English","publisher":"U.S. Geological Survey","doi":"10.3133/wri844194","usgsCitation":"Armstrong, C.A., 1984, Evaluation of the hydrologic system and potential effects of mining in the Dickinson lignite area, eastern slope and western Stark and Hettinger counties, North Dakota: U.S. Geological Survey Water-Resources Investigations Report 84-4194, Report: v, 35 p.; Plate: 22.55 x 19.31 inches, https://doi.org/10.3133/wri844194.","productDescription":"Report: v, 35 p.; Plate: 22.55 x 19.31 inches","costCenters":[{"id":478,"text":"North Dakota Water Science Center","active":true,"usgs":true},{"id":34685,"text":"Dakota Water Science Center","active":true,"usgs":true}],"links":[{"id":123870,"rank":0,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/wri/1984/4194/report-thumb.jpg"},{"id":54717,"rank":400,"type":{"id":17,"text":"Plate"},"url":"https://pubs.usgs.gov/wri/1984/4194/plate-1.pdf","linkFileType":{"id":1,"text":"pdf"}},{"id":54718,"rank":300,"type":{"id":11,"text":"Document"},"url":"https://pubs.usgs.gov/wri/1984/4194/report.pdf","linkFileType":{"id":1,"text":"pdf"}}],"country":"United States","state":"North Dakota","county":"Hettinger County, Stark County","noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"4f4e4a08e4b07f02db5fa3b1","contributors":{"authors":[{"text":"Armstrong, C. A.","contributorId":66231,"corporation":false,"usgs":true,"family":"Armstrong","given":"C.","email":"","middleInitial":"A.","affiliations":[],"preferred":false,"id":195565,"contributorType":{"id":1,"text":"Authors"},"rank":1}]}} ,{"id":1089,"text":"wsp2215 - 1984 - Availability and quality of water from the Dakota aquifer, northwest Iowa","interactions":[{"subject":{"id":8110,"text":"ofr82264 - 1982 - Availability and quality of water from the Dakota aquifer, northwest Iowa","indexId":"ofr82264","publicationYear":"1982","noYear":false,"title":"Availability and quality of water from the Dakota aquifer, northwest Iowa"},"predicate":"SUPERSEDED_BY","object":{"id":1089,"text":"wsp2215 - 1984 - Availability and quality of water from the Dakota aquifer, northwest Iowa","indexId":"wsp2215","publicationYear":"1984","noYear":false,"title":"Availability and quality of water from the Dakota aquifer, northwest Iowa"},"id":1}],"lastModifiedDate":"2016-03-02T15:59:06","indexId":"wsp2215","displayToPublicDate":"1994-01-01T00:00:00","publicationYear":"1984","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":"2215","title":"Availability and quality of water from the Dakota aquifer, northwest Iowa","docAbstract":"

The Dakota aquifer in northwest Iowa consists of sandstones in the Dakota Formation. It underlies most of the study area and is the most extensive source of ground water in the area. Individual sandstone beds are from less than 10 to more than 150 feet thick. The cumulative thickness of sandstone is more than 200 feet throughout much of the area. The aquifer is confined by overlying Cretaceous limestone and shale, Quaternary glacial deposits and loess. The underlying confining material is shale of the Dakota Formation, undifferentiated Paleozoic age rocks, or Precambrian crystalline rock.

\n

Water flows through the aquifer from the northcentral part of the study area to the east, south and southwest. Recharge is dominantly by infiltration from the land surface through the confining materials. Discharge is to underlying Paleozoic aquifers and to the alluvium and glacial outwash deposits along the Missouri and Big Sioux Rivers in the southwest part of the area. Flow components toward bedrock valleys may reflect discharge to Quaternary sand and gravel deposits in these valleys.

\n

Pumping tests conducted in the study area indicate a narrow\" range of hydraulic conductivities of the Dakota aquifer, from 37 to 50 feet per day. Consequently, an average hydraulic conductivity of 40 feet per day was used to estimate the potential yield to wells completed in the aquifer. Yields of more than 250 gallons per minute can be expected throughout much of the study area and more than 1,000 gallons per minute could be produced in some areas.

\n

The quality of water from the Dakota is a calcium, magnesium, sulfate type. It is generally suitable for irrigation purposes, based on comparisons of sodium adsorption ratios and electrical conductivities. In some areas the aquifer has water with high salinity hazard that may restrict its use to irrigation of only well-drained types of soil. The concentration of radium-226 and other radionuclides exceeds recommended limits at several sites.

\n

The quality of water pumped from the aquifer may be altered by induced leakage from the underlying aquifers in Paleozoic age rocks if withdrawals reverse the pattern of natural flow from the Dakota into the Paleozoic aquifers. Evidence for such a reversal exists in the area around the city of LeMars.

","language":"English","publisher":"U. S. 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No abstract available.

","language":"English","publisher":"U.S. Geological Survey","doi":"10.3133/ofr84452","usgsCitation":"Lindholm, G.F., and Goodell, S.A., 1984, Irrigated acreage and other land uses on the Snake River Plain, Idaho and eastern Oregon: U.S. Geological Survey Open-File Report 84-452, 1 Plate: 58.83 x 41.05 inches, https://doi.org/10.3133/ofr84452.","productDescription":"1 Plate: 58.83 x 41.05 inches","costCenters":[],"links":[{"id":398926,"rank":3,"type":{"id":17,"text":"Plate"},"url":"https://pubs.usgs.gov/of/1984/0452/plate-1.pdf","linkFileType":{"id":1,"text":"pdf"}},{"id":161991,"rank":0,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/of/1984/0452/report-thumb.jpg"},{"id":397207,"rank":2,"type":{"id":36,"text":"NGMDB Index Page"},"url":"https://ngmdb.usgs.gov/Prodesc/proddesc_13413.htm"}],"scale":"500000","country":"United States","state":"Idaho, Oregon","otherGeospatial":"Snake River Plain","geographicExtents":"{\n \"type\": \"FeatureCollection\",\n \"features\": [\n {\n \"type\": \"Feature\",\n \"properties\": {},\n \"geometry\": {\n \"type\": \"Polygon\",\n \"coordinates\": [\n [\n [\n -117.183,\n 42.350\n ],\n [\n -111.542,\n 42.350\n ],\n [\n -111.542,\n 44.315\n ],\n [\n -117.183,\n 44.315\n ],\n [\n -117.183,\n 42.350\n ]\n ]\n ]\n }\n }\n ]\n}","noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"4f4e4aa7e4b07f02db6672ad","contributors":{"authors":[{"text":"Lindholm, Gerald F.","contributorId":18374,"corporation":false,"usgs":true,"family":"Lindholm","given":"Gerald","email":"","middleInitial":"F.","affiliations":[],"preferred":false,"id":228116,"contributorType":{"id":1,"text":"Authors"},"rank":1},{"text":"Goodell, S. A.","contributorId":38168,"corporation":false,"usgs":true,"family":"Goodell","given":"S.","email":"","middleInitial":"A.","affiliations":[],"preferred":false,"id":228117,"contributorType":{"id":1,"text":"Authors"},"rank":2}]}} ,{"id":15729,"text":"ofr84233 - 1984 - Hydrology of area 11, Eastern Coal Province, Ohio, Kentucky, and West Virginia","interactions":[],"lastModifiedDate":"2024-12-04T21:00:35.905241","indexId":"ofr84233","displayToPublicDate":"1994-01-01T00:00:00","publicationYear":"1984","noYear":false,"publicationType":{"id":18,"text":"Report"},"publicationSubtype":{"id":5,"text":"USGS Numbered Series"},"seriesTitle":{"id":330,"text":"Open-File Report","code":"OFR","onlineIssn":"2331-1258","printIssn":"0196-1497","active":true,"publicationSubtype":{"id":5}},"seriesNumber":"84-233","title":"Hydrology of area 11, Eastern Coal Province, Ohio, Kentucky, and West Virginia","docAbstract":"

No abstract available.

","language":"English","publisher":"U.S. Geological Survey","doi":"10.3133/ofr84233","usgsCitation":"Roth, D., and Cooper, S., 1984, Hydrology of area 11, Eastern Coal Province, Ohio, Kentucky, and West Virginia: U.S. Geological Survey Open-File Report 84-233, v, 66 p., https://doi.org/10.3133/ofr84233.","productDescription":"v, 66 p.","costCenters":[],"links":[{"id":464766,"rank":3,"type":{"id":36,"text":"NGMDB Index Page"},"url":"https://ngmdb.usgs.gov/Prodesc/proddesc_13321.htm","linkFileType":{"id":5,"text":"html"}},{"id":146462,"rank":1,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/of/1984/0233/report-thumb.jpg"},{"id":95324,"rank":2,"type":{"id":11,"text":"Document"},"url":"https://pubs.usgs.gov/of/1984/0233/report.pdf","linkFileType":{"id":1,"text":"pdf"}}],"country":"United States","state":"Kentucky, Ohio, West Virginia","geographicExtents":"{\n \"type\": \"FeatureCollection\",\n \"features\": [\n {\n \"type\": \"Feature\",\n \"properties\": {},\n \"geometry\": {\n \"coordinates\": [\n [\n [\n -83.86623180747648,\n 36.731743994525004\n ],\n [\n -81.43264711571662,\n 37.927674336656665\n ],\n [\n -81.0549105792823,\n 40.470417310879355\n ],\n [\n -81.04739335783368,\n 41.3198369033787\n ],\n [\n -82.26961292288702,\n 41.177583641541645\n ],\n [\n -84.09257837635606,\n 39.6683312010673\n ],\n [\n -84.68344347599752,\n 37.24430123159996\n ],\n [\n -83.86623180747648,\n 36.731743994525004\n ]\n ]\n ],\n \"type\": \"Polygon\"\n }\n }\n ]\n}","noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"4f4e4a17e4b07f02db604706","contributors":{"authors":[{"text":"Roth, D.K.","contributorId":60275,"corporation":false,"usgs":true,"family":"Roth","given":"D.K.","email":"","affiliations":[],"preferred":false,"id":171607,"contributorType":{"id":1,"text":"Authors"},"rank":1},{"text":"Cooper, S.C.","contributorId":75284,"corporation":false,"usgs":true,"family":"Cooper","given":"S.C.","email":"","affiliations":[],"preferred":false,"id":171608,"contributorType":{"id":1,"text":"Authors"},"rank":2}]}} ,{"id":11190,"text":"ofr84446 - 1984 - Physical and chemical characteristics of water in coal-mine ponds, eastern Oklahoma, June to November 1977-81","interactions":[],"lastModifiedDate":"2021-01-21T17:24:06.763454","indexId":"ofr84446","displayToPublicDate":"1994-01-01T00:00:00","publicationYear":"1984","noYear":false,"publicationType":{"id":18,"text":"Report"},"publicationSubtype":{"id":5,"text":"USGS Numbered Series"},"seriesTitle":{"id":330,"text":"Open-File Report","code":"OFR","onlineIssn":"2331-1258","printIssn":"0196-1497","active":true,"publicationSubtype":{"id":5}},"seriesNumber":"84-446","title":"Physical and chemical characteristics of water in coal-mine ponds, eastern Oklahoma, June to November 1977-81","docAbstract":"Water at 102 sites in 59 coal-mine ponds in eastern Oklahoma was sampled at lease twice during June to November 1977-81 to determine temperature, specific conductance, dissolved oxygen, pH, and dissolved sulfate, chloride, iron, and manganese--as part of a study of the hydrology of the Oklahoma coalfield. These determinations show that during June to October water in ponds deeper than ~10 ft was stratified; ponds which had little or not change of temperature with depth generally were shallow or were sampled in early November. Temperature, dissolved oxygen, and pH usually decreased with depth, whereas specific conductance usually increased with depth. Concentrations of dissolved sulfate, chloride, iron, and manganese varied from site to site. Specific conductance, which is a measure of dissolved solids in the water, ranged from 93 to 4,800 mmho/cm at 25oC. Some physical and chemical characteristics of the mine-pond water are related to the coal bed adjacent to the pond. Mean specific-conductance values and dissolved-sulfate concentrations were greatest in ponds associated with mining of Dawson, Weir-Pittsburg, and Secor coals. Mean dissolved-iron concentrations were greatest in ponds associated with mining of the Dawson, Secor, and Hartshorne coals. Mean dissolved-manganese concentrations were greatest in ponds associated with mining of the Dawson, Weir-Pittsburg, and Secor coals, but greatly exceeded secondary drinking-water limits regardless of coal bed mined.","language":"English","publisher":"U.S. Geological Survey","publisherLocation":"Reston, VA","doi":"10.3133/ofr84446","collaboration":"This report was also published by the Oklahoma Geological Survey as Special Publication 87-2","usgsCitation":"Slack, L.J., and Blumer, S.P., 1984, Physical and chemical characteristics of water in coal-mine ponds, eastern Oklahoma, June to November 1977-81: U.S. Geological Survey Open-File Report 84-446, Report: vi, 183 p.; 1 Plate: 16.79 x 22.84 inches, https://doi.org/10.3133/ofr84446.","productDescription":"Report: vi, 183 p.; 1 Plate: 16.79 x 22.84 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\"}}]}","noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"4f4e4adbe4b07f02db685c5f","contributors":{"authors":[{"text":"Slack, L. J.","contributorId":44157,"corporation":false,"usgs":true,"family":"Slack","given":"L.","email":"","middleInitial":"J.","affiliations":[],"preferred":false,"id":162701,"contributorType":{"id":1,"text":"Authors"},"rank":1},{"text":"Blumer, S. P.","contributorId":23938,"corporation":false,"usgs":true,"family":"Blumer","given":"S.","email":"","middleInitial":"P.","affiliations":[],"preferred":false,"id":162700,"contributorType":{"id":1,"text":"Authors"},"rank":2}]}} ,{"id":8868,"text":"ofr84633 - 1984 - Characteristics of some silver-, and base metal-bearing, epithermal deposits of Mexico and Peru","interactions":[],"lastModifiedDate":"2018-10-22T08:50:04","indexId":"ofr84633","displayToPublicDate":"1994-01-01T00:00:00","publicationYear":"1984","noYear":false,"publicationType":{"id":18,"text":"Report"},"publicationSubtype":{"id":5,"text":"USGS Numbered Series"},"seriesTitle":{"id":330,"text":"Open-File Report","code":"OFR","onlineIssn":"2331-1258","printIssn":"0196-1497","active":true,"publicationSubtype":{"id":5}},"seriesNumber":"84-633","title":"Characteristics of some silver-, and base metal-bearing, epithermal deposits of Mexico and Peru","docAbstract":"

Introduction

\n

Lithotectonic, mineralogical, and geochemical data on two silver- and base metal-bearing deposits from Peru and two from Mexico are compiled to facilitate comparisons with other epithermal deposits. Silver and base metal-bearing deposits of Mexico and Peru constitute an important portion of the world silver production derived from shallow, vein-type deposits hosted in volcanic rocks. Although these deposits are generally similar to epithermal deposits of Nevada and Colorado in the western United States, they have some important differences. Because of this, data on the geological attributes of these deposits are very useful for developing models of ore formation that can be used in mineral exploration. The data collected for this compilation are presented in the following pages in summaries of the important characteristics of each deposit. This compilation, which shows the complexities in the geology of epithermal ore deposits in Mexico and Peru, serves as a basis for further comparisons among epithermal deposits throughout the world. The case studies provide data useful to geologists and exploration!'sts interested in developing models of ore formation to be used in exploration for mineral deposits of this type. The deposits described in this report are the Guanajuato district of Guanajuato, Mexico, the Pachuca-Real del Monte district of Hidalgo, Mexico, the Colqui district of Lima, Peru, and the Julcani district of Huancavelica, Peru.

\n

Although many characteristics of the geology and geochemistry of this type of deposit were considered, the most important criterion for choosing these deposits was that they have substantial quantities of precious- and base-metal mineralization. Additional criteria for selecting the deposits were that they be hosted primarily by calc-alkaline volcanic rocks of intermediate to silicic composition and that they be younger than Tertiary in age. Many deposits in Mexico and Peru and other parts of Central and South America were excluded because the literature describing the districts is not readily available. Furthermore, many districts have not been examined in detail or the information available is of limited geological scope. The four districts that are compiled in this report were chosen because they are described in abundant literature dating from early mining reports on the general geology and mineralogy to very recent data on detailed geochemical and mineralogical studies. They were chosen as being fairly typical, classic examples of near-surface, low-temperature vein deposits as described by Lindgren (1928) in his treatise on ore deposits (Mineral deposits, McGraw-Hill, 1049 p.). These deposits are similar in aspects of their geology and geochemistry to many of the famous, epithermal silver mining districts in Colorado and Nevada including Creede, Colorado, Tonapah, Nevada, and the Sunnyside Mine of the Eureka district, Colorado, and, in the special case of Julcani, to Summitville, Colorado, and Goldfield, Nevada. The characteristics that distinguish them include overall size, production and alteration assemblage. The information documented in each summary will be used in a forthcoming series of papers on the comparative anatomy of precious and base metal deposits in North and South America.

","language":"English","publisher":"U.S. Geological Survey","doi":"10.3133/ofr84633","usgsCitation":"Foley, N.K., 1984, Characteristics of some silver-, and base metal-bearing, epithermal deposits of Mexico and Peru: U.S. Geological Survey Open-File Report 84-633, 35 p., https://doi.org/10.3133/ofr84633.","productDescription":"35 p.","onlineOnly":"N","additionalOnlineFiles":"N","costCenters":[{"id":245,"text":"Eastern Mineral and Environmental Resources Science Center","active":true,"usgs":true}],"links":[{"id":142811,"rank":0,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/of/1984/0633/report-thumb.jpg"},{"id":36439,"rank":300,"type":{"id":11,"text":"Document"},"url":"https://pubs.usgs.gov/of/1984/0633/report.pdf","text":"Report","size":"471.64 KB","linkFileType":{"id":1,"text":"pdf"},"description":"Report"}],"country":"Mexico, Peru","state":"Guanajuato, Hidalgo. Huancavelica, Lima","geographicExtents":"{\n \"type\": \"FeatureCollection\",\n \"features\": [\n {\n \"type\": \"Feature\",\n \"properties\": {},\n \"geometry\": {\n \"type\": \"Polygon\",\n \"coordinates\": [\n [\n [\n -101.3,\n 21\n ],\n [\n -101.3,\n 21.1\n ],\n [\n -101.2,\n 21.1\n ],\n [\n -101.2,\n 21\n ],\n [\n -101.3,\n 21\n ]\n ]\n ]\n }\n },\n {\n \"type\": \"Feature\",\n \"properties\": {},\n \"geometry\": {\n \"type\": \"Polygon\",\n \"coordinates\": [\n [\n [\n -98.7,\n 20\n ],\n [\n -98.7,\n 20.1\n ],\n [\n -98.8,\n 20.1\n ],\n [\n -98.8,\n 20\n ],\n [\n -98.7,\n 20\n ]\n ]\n ]\n }\n },\n {\n \"type\": \"Feature\",\n \"properties\": {},\n \"geometry\": {\n \"type\": \"Polygon\",\n \"coordinates\": [\n [\n [\n -76.4,\n -11.5\n ],\n [\n -76.4,\n -11.6\n ],\n [\n -76.5,\n -11.6\n ],\n [\n -76.5,\n -11.5\n ],\n [\n -76.4,\n -11.5\n ]\n ]\n ]\n }\n },\n {\n \"type\": \"Feature\",\n \"properties\": {},\n \"geometry\": {\n \"type\": \"Polygon\",\n \"coordinates\": [\n [\n [\n -74.8,\n -12.9\n ],\n [\n -74.8,\n -13\n ],\n [\n -74.7,\n -13\n ],\n [\n -74.7,\n -12.9\n ],\n [\n -74.8,\n -12.9\n ]\n ]\n ]\n }\n }\n ]\n}","noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"4f4e49e2e4b07f02db5e4f45","contributors":{"authors":[{"text":"Foley, Nora K. 0000-0003-0124-3509 nfoley@usgs.gov","orcid":"https://orcid.org/0000-0003-0124-3509","contributorId":4010,"corporation":false,"usgs":true,"family":"Foley","given":"Nora","email":"nfoley@usgs.gov","middleInitial":"K.","affiliations":[{"id":245,"text":"Eastern Mineral and Environmental Resources Science Center","active":true,"usgs":true}],"preferred":true,"id":158463,"contributorType":{"id":1,"text":"Authors"},"rank":1}]}} ,{"id":27544,"text":"wri834208 - 1984 - Chemical and biological quality of streams at the Indiana Dunes National Lakeshore, Indiana, 1978-80","interactions":[],"lastModifiedDate":"2016-05-25T11:32:26","indexId":"wri834208","displayToPublicDate":"1994-01-01T00:00:00","publicationYear":"1984","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":"83-4208","title":"Chemical and biological quality of streams at the Indiana Dunes National Lakeshore, Indiana, 1978-80","docAbstract":"

A variety of land uses affects water quality of streams at the Indiana Dunes National Lakeshore. Discharge from storm sewers and runoff from roads contributed lead, zinc, and chlorinated hydrocarbons (chlordane, DOT, ODD, DDE, and PCB's) to all streams except Derby ditch. In addition, the Little Calumet River received ammonia from industrial discharges, and organic materials, nitrogen, phosphorus, and fecal coliform from wastewater-treatment-plant and combinedsanitary- and storm-sewer discharges. As a result, water at some sites in the lower reaches of the Little Calumet River contained dissolved-ammonium-nitrogen concentrations exceeding 0.10 milligram per liter, dissolved-oxygen concentrations less than 3.0 milligrams per liter, and fecal coliform populations exceeding 2,000 colonies per 100 milliliters.

\n

Seepage from two landfills may have caused the concentration of dissolved solids in the west Grand Calumet River lagoon to exceed that in the east lagoon. Ammonium concentrations in the west lagoon ranged from 13 to 16 milligrams per liter as nitrogen.

\n

Pesticides used in agricultural areas were the major source of DOT, ODD, DDE, and dieldrin on streambed materials. Runoff from residential areas was a major source of nitrate, organic materials, and chlordane in Derby ditch and Dunes Creek.

\n

Wetland drainage contributed significant amounts of organic materials to streams and at times increased concentrations of dissolved sulfate and iron. Dissolved-iron concentrations correlated with dissolved-organic-carbon concentrations in yellow-brown water of Kintzele and Derby ditches.

","language":"English","publisher":"U.S. Geological Survey","publisherLocation":"Indianapolis, IN","doi":"10.3133/wri834208","collaboration":"National Park Service","usgsCitation":"Hardy, M.A., 1984, Chemical and biological quality of streams at the Indiana Dunes National Lakeshore, Indiana, 1978-80: U.S. Geological Survey Water-Resources Investigations Report 83-4208, viii, 95 p. :ill., maps ;28 cm., https://doi.org/10.3133/wri834208.","productDescription":"viii, 95 p. :ill., maps ;28 cm.","startPage":"1","endPage":"95","numberOfPages":"105","onlineOnly":"N","additionalOnlineFiles":"N","costCenters":[{"id":346,"text":"Indiana Water Science Center","active":true,"usgs":true}],"links":[{"id":123388,"rank":0,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/wri/1983/4208/report-thumb.jpg"},{"id":56400,"rank":300,"type":{"id":11,"text":"Document"},"url":"https://pubs.usgs.gov/wri/1983/4208/report.pdf","linkFileType":{"id":1,"text":"pdf"}}],"country":"United States","state":"Indiana","otherGeospatial":"Indiana Dunes National Lakeshore","geographicExtents":"{\n \"type\": \"FeatureCollection\",\n \"features\": [\n {\n \"type\": \"Feature\",\n \"properties\": {},\n \"geometry\": {\n \"type\": \"Polygon\",\n \"coordinates\": [\n [\n [\n -87.28869438171387,\n 41.621923034123846\n ],\n [\n -87.26963996887207,\n 41.621730547188456\n ],\n [\n -87.26912498474121,\n 41.60806250618307\n ],\n [\n -87.24603652954102,\n 41.608511736657555\n ],\n [\n -87.24303245544434,\n 41.609859409312534\n ],\n [\n -87.24311828613281,\n 41.61306804041503\n ],\n [\n -87.23959922790527,\n 41.61313221140915\n ],\n [\n -87.23779678344727,\n 41.61396642852365\n ],\n [\n -87.23367691040039,\n 41.61441561788573\n ],\n [\n -87.23221778869629,\n 41.61249049859493\n ],\n [\n -87.2306728363037,\n 41.61531398722544\n ],\n [\n -87.2303295135498,\n 41.61614817612265\n ],\n [\n -87.22672462463377,\n 41.61499314246908\n ],\n [\n -87.22346305847167,\n 41.618329849922084\n ],\n [\n -87.22466468811035,\n 41.62558017672615\n ],\n [\n -87.17668533325195,\n 41.63578058345409\n ],\n [\n -87.17471122741699,\n 41.62301378257129\n ],\n [\n -87.17968940734863,\n 41.62275713753768\n ],\n [\n -87.18063354492188,\n 41.621923034123846\n ],\n [\n -87.1805477142334,\n 41.61807318624671\n ],\n [\n -87.18818664550781,\n 41.616725685192804\n ],\n [\n -87.1889591217041,\n 41.61634067972058\n ],\n [\n -87.18844413757324,\n 41.61364557706411\n ],\n [\n -87.18973159790039,\n 41.61358140658068\n ],\n [\n -87.19127655029297,\n 41.60799833014563\n ],\n [\n -87.19874382019043,\n 41.605174521299304\n ],\n [\n -87.19951629638672,\n 41.60645808609603\n ],\n [\n -87.20681190490723,\n 41.607677449000946\n ],\n [\n -87.2068977355957,\n 41.60273567783677\n ],\n [\n -87.21256256103516,\n 41.59978327031246\n ],\n [\n -87.21359252929686,\n 41.603698390215456\n ],\n [\n -87.22123146057129,\n 41.60286404031713\n ],\n [\n -87.22294807434082,\n 41.600040006763784\n ],\n [\n -87.23161697387695,\n 41.600681843423565\n ],\n [\n -87.23153114318848,\n 41.59644560350027\n ],\n [\n -87.25247383117676,\n 41.59792190049485\n ],\n [\n -87.25273132324217,\n 41.60061766004485\n ],\n [\n -87.25496292114258,\n 41.60074602673845\n ],\n [\n -87.2548770904541,\n 41.60382675078074\n ],\n [\n -87.27805137634276,\n 41.60389093096761\n ],\n [\n -87.27865219116211,\n 41.59914142471562\n ],\n [\n -87.34139442443848,\n 41.605880485097465\n ],\n [\n -87.32903480529784,\n 41.60645808609603\n ],\n [\n -87.31126785278319,\n 41.60594466324155\n ],\n [\n -87.30174064636229,\n 41.609153489052005\n ],\n [\n -87.28517532348633,\n 41.609602711929725\n ],\n [\n -87.28526115417479,\n 41.61640484745891\n ],\n [\n -87.28963851928711,\n 41.616854019839494\n ],\n [\n -87.29006767272949,\n 41.62205135842823\n ],\n [\n -87.28869438171387,\n 41.621923034123846\n ]\n ]\n ]\n }\n }\n ]\n}","noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"4f4e499ee4b07f02db5bcbb8","contributors":{"authors":[{"text":"Hardy, M. A.","contributorId":54223,"corporation":false,"usgs":true,"family":"Hardy","given":"M.","email":"","middleInitial":"A.","affiliations":[],"preferred":false,"id":198295,"contributorType":{"id":1,"text":"Authors"},"rank":1}]}} ,{"id":36578,"text":"fwsobs82_10_56 - 1984 - Habitat Suitability Index Models: Walleye","interactions":[],"lastModifiedDate":"2022-02-09T15:19:36.985384","indexId":"fwsobs82_10_56","displayToPublicDate":"1994-01-01T00:00:00","publicationYear":"1984","noYear":false,"publicationType":{"id":18,"text":"Report"},"publicationSubtype":{"id":1,"text":"Federal Government Series"},"seriesTitle":{"id":20,"text":"FWS/OBS","active":false,"publicationSubtype":{"id":1}},"seriesNumber":"82/10.56","subseriesTitle":"Habitat Suitability Index","title":"Habitat Suitability Index Models: Walleye","docAbstract":"

The wall eye is native to freshwater ri vers and 1akes of Canada and the United States, with rare occurrences in brackish water (Scott and Crossman 1973). In the United States, its native range occurs primarily in drainages east of the Rocky Mountains and west of the Appalachians; however, it has been widely introduced into reservoirs outside its native range (Colby et al. 1979). Walleye hybridize with sauger (S. canadense) and blue pike (S. v. glaucum) (Scott and Crossman 1973).

","language":"English","publisher":"U.S. Fish and Wildlife Service","usgsCitation":"McMahon, T., Terrell, J.W., and Nelson, P.C., 1984, Habitat Suitability Index Models: Walleye: FWS/OBS 82/10.56, viii, 43 p.","productDescription":"viii, 43 p.","costCenters":[{"id":595,"text":"U.S. Geological Survey","active":false,"usgs":true}],"links":[{"id":165604,"rank":0,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/thumbnails/outside_thumb.jpg"}],"noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"4f4e4a80e4b07f02db6497a2","contributors":{"authors":[{"text":"McMahon, Thomas E.","contributorId":93548,"corporation":false,"usgs":true,"family":"McMahon","given":"Thomas E.","affiliations":[],"preferred":false,"id":216576,"contributorType":{"id":1,"text":"Authors"},"rank":1},{"text":"Terrell, James W. 0000-0001-5394-5663","orcid":"https://orcid.org/0000-0001-5394-5663","contributorId":92726,"corporation":false,"usgs":true,"family":"Terrell","given":"James","email":"","middleInitial":"W.","affiliations":[{"id":291,"text":"Fort Collins Science Center","active":true,"usgs":true}],"preferred":true,"id":216575,"contributorType":{"id":1,"text":"Authors"},"rank":2},{"text":"Nelson, Patrick C.","contributorId":68799,"corporation":false,"usgs":true,"family":"Nelson","given":"Patrick","email":"","middleInitial":"C.","affiliations":[],"preferred":false,"id":216574,"contributorType":{"id":1,"text":"Authors"},"rank":3}]}} ,{"id":42903,"text":"ofr84274 - 1984 - Preliminary geologic map of the western and southern parts of the Byers Peak, the northwestern part of the Loveland Pass, and the eastern part of the Ute Peak 7 1/2-minute quadrangles, Clear Creek and Grand Counties, Colorado","interactions":[],"lastModifiedDate":"2021-11-29T22:58:01.781728","indexId":"ofr84274","displayToPublicDate":"1994-01-01T00:00:00","publicationYear":"1984","noYear":false,"publicationType":{"id":18,"text":"Report"},"publicationSubtype":{"id":5,"text":"USGS Numbered Series"},"seriesTitle":{"id":330,"text":"Open-File Report","code":"OFR","onlineIssn":"2331-1258","printIssn":"0196-1497","active":true,"publicationSubtype":{"id":5}},"seriesNumber":"84-274","title":"Preliminary geologic map of the western and southern parts of the Byers Peak, the northwestern part of the Loveland Pass, and the eastern part of the Ute Peak 7 1/2-minute quadrangles, Clear Creek and Grand Counties, Colorado","docAbstract":"

No abstract available.

","language":"English","publisher":"U.S. Geological Survey","doi":"10.3133/ofr84274","usgsCitation":"Eppinger, R., Theobald, P., and Carlson, R.R., 1984, Preliminary geologic map of the western and southern parts of the Byers Peak, the northwestern part of the Loveland Pass, and the eastern part of the Ute Peak 7 1/2-minute quadrangles, Clear Creek and Grand Counties, Colorado: U.S. Geological Survey Open-File Report 84-274, 1 Plate: 34.99 × 40.47 inches, https://doi.org/10.3133/ofr84274.","productDescription":"1 Plate: 34.99 × 40.47 inches","costCenters":[],"links":[{"id":168159,"rank":0,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/thumbnails/usgs_thumb.jpg"},{"id":108400,"rank":700,"type":{"id":36,"text":"NGMDB Index Page"},"url":"https://ngmdb.usgs.gov/Prodesc/proddesc_13332.htm","linkFileType":{"id":5,"text":"html"},"description":"13332"},{"id":80717,"rank":400,"type":{"id":17,"text":"Plate"},"url":"https://pubs.usgs.gov/of/1984/0274/plate-1.pdf","linkFileType":{"id":1,"text":"pdf"}}],"country":"United States","state":"Colorado","county":"Clear Creek, Grand County","otherGeospatial":"Byers Peak, the northwestern part of the Loveland Pass, and the eastern part of the Ute Peak 7-1/2 minute quadrangles","geographicExtents":"{\n \"type\": \"FeatureCollection\",\n \"features\": [\n {\n \"type\": \"Feature\",\n \"properties\": {},\n \"geometry\": {\n \"type\": \"Polygon\",\n \"coordinates\": [\n [\n [\n -106.0514,\n 39.7\n ],\n [\n -105.875,\n 39.7\n ],\n [\n -105.875,\n 39.875\n ],\n [\n -106.0514,\n 39.875\n ],\n [\n -106.0514,\n 39.7\n ]\n ]\n ]\n }\n }\n ]\n}","noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"4f4e4abde4b07f02db674131","contributors":{"authors":[{"text":"Eppinger, R. G.","contributorId":100837,"corporation":false,"usgs":true,"family":"Eppinger","given":"R. G.","affiliations":[],"preferred":false,"id":227372,"contributorType":{"id":1,"text":"Authors"},"rank":1},{"text":"Theobald, P. K.","contributorId":45293,"corporation":false,"usgs":true,"family":"Theobald","given":"P. K.","affiliations":[],"preferred":false,"id":227370,"contributorType":{"id":1,"text":"Authors"},"rank":2},{"text":"Carlson, Robert R.","contributorId":71944,"corporation":false,"usgs":true,"family":"Carlson","given":"Robert","email":"","middleInitial":"R.","affiliations":[],"preferred":false,"id":227371,"contributorType":{"id":1,"text":"Authors"},"rank":3}]}} ,{"id":36484,"text":"fwsobs83_17 - 1984 - The ecology of tidal freshwater marshes of the United States East Coast: a community profile","interactions":[],"lastModifiedDate":"2012-02-02T00:09:28","indexId":"fwsobs83_17","displayToPublicDate":"1994-01-01T00:00:00","publicationYear":"1984","noYear":false,"publicationType":{"id":18,"text":"Report"},"publicationSubtype":{"id":1,"text":"Federal Government Series"},"seriesTitle":{"id":20,"text":"FWS/OBS","active":false,"publicationSubtype":{"id":1}},"seriesNumber":"83/17","title":"The ecology of tidal freshwater marshes of the United States East Coast: a community profile","language":"ENGLISH","publisher":"U.S. Fish and Wildlife Service","usgsCitation":"Odum, W.E., Smith, T.J., Hoover, J., and McIvor, C.C., 1984, The ecology of tidal freshwater marshes of the United States East Coast: a community profile: FWS/OBS 83/17, ix, 177 p. : ill.; 28 cm.","productDescription":"ix, 177 p. : ill.; 28 cm.","costCenters":[],"links":[{"id":163899,"rank":0,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/thumbnails/outside_thumb.jpg"}],"noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"4f4e4aa9e4b07f02db668231","contributors":{"authors":[{"text":"Odum, William E.","contributorId":77984,"corporation":false,"usgs":true,"family":"Odum","given":"William","email":"","middleInitial":"E.","affiliations":[],"preferred":false,"id":216401,"contributorType":{"id":1,"text":"Authors"},"rank":1},{"text":"Smith, T. J. III","contributorId":24303,"corporation":false,"usgs":true,"family":"Smith","given":"T.","suffix":"III","email":"","middleInitial":"J.","affiliations":[],"preferred":false,"id":216399,"contributorType":{"id":1,"text":"Authors"},"rank":2},{"text":"Hoover, J.K.","contributorId":11666,"corporation":false,"usgs":true,"family":"Hoover","given":"J.K.","email":"","affiliations":[],"preferred":false,"id":216398,"contributorType":{"id":1,"text":"Authors"},"rank":3},{"text":"McIvor, Carole C.","contributorId":73254,"corporation":false,"usgs":true,"family":"McIvor","given":"Carole","email":"","middleInitial":"C.","affiliations":[],"preferred":false,"id":216400,"contributorType":{"id":1,"text":"Authors"},"rank":4}]}} ,{"id":15627,"text":"ofr84713 - 1984 - Ground-water resources of Limestone County, Texas","interactions":[],"lastModifiedDate":"2016-08-11T16:35:01","indexId":"ofr84713","displayToPublicDate":"1994-01-01T00:00:00","publicationYear":"1984","noYear":false,"publicationType":{"id":18,"text":"Report"},"publicationSubtype":{"id":5,"text":"USGS Numbered Series"},"seriesTitle":{"id":330,"text":"Open-File Report","code":"OFR","onlineIssn":"2331-1258","printIssn":"0196-1497","active":true,"publicationSubtype":{"id":5}},"seriesNumber":"84-713","title":"Ground-water resources of Limestone County, Texas","docAbstract":"

Limestone County, located in east-central Texas, has small to plentiful ground-water supplies available, depending upon the location within the county. The Wilcox Group in the eastern part of the county has adequate supplies to meet the expected water demands in the foreseeable future. The thicker zones of the Wilcox Group can supply yields in excess of 500 gallons per minute. The Midway Group can supply yields in excess of 100 gallons per minute from the Tehuacana Member of the Kincaid Formation. This represents the largest well yields from the Midway Group in Texas. The Midway Group elsewhere in the State is mostly a poor water producer and is not considered an aquifer. The Taylor Marl and Navarro Group furnish only small quantities of ground water to wells in the western part of the county where these units crop out. The Hosston and Travis Peak Formations are present at depths in excess of 2,000 feet. These formations, which contain slightly saline water in the western part of the county, could be expected to produce water with a temperature of about 150°F that might be used for heating purposes.

\n

About 0.9 million gallons per day of ground water was used for all purposes in 1980. This use has declined since 1955 but is expected to increase as additional public-supply and industrial wells are being developed. The Wilcox Group is capable of annually yielding at least 14,000 acre-feet or 11.6 million gallons per day of water to wells on a long-term basis.

\n

Generally, the ground water is of acceptable quality for most uses. Relatively high dissolved-solids and iron concentrations are the major water-quality problems. Water-quality problems that may be the result of man's activities are limited to a small oilfield area near Mexia.

\n

Lignite mining from the Wilcox Group is expected to take place in the foreseeable future. The collection of additional hydrologic data on the Wilcox would be desirable before, during, and after mining.

","language":"English","publisher":"U.S. Geological Survey","publisherLocation":"Ausitn, TX","doi":"10.3133/ofr84713","usgsCitation":"Rettman, P., 1984, Ground-water resources of Limestone County, Texas: U.S. Geological Survey Open-File Report 84-713, vi, 92 p., https://doi.org/10.3133/ofr84713.","productDescription":"vi, 92 p.","onlineOnly":"N","additionalOnlineFiles":"N","costCenters":[{"id":583,"text":"Texas Water Science Center","active":true,"usgs":true}],"links":[{"id":147309,"rank":0,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/of/1984/0713/report-thumb.jpg"},{"id":44590,"rank":300,"type":{"id":11,"text":"Document"},"url":"https://pubs.usgs.gov/of/1984/0713/report.pdf","linkFileType":{"id":1,"text":"pdf"}}],"country":"United States","state":"Texas","county":"Limestone County","geographicExtents":"{\"type\":\"FeatureCollection\",\"features\":[{\"type\":\"Feature\",\"geometry\":{\"type\":\"Polygon\",\"coordinates\":[[[-96.4998,31.8005],[-96.4298,31.7011],[-96.2333,31.4115],[-96.3228,31.3661],[-96.3236,31.3593],[-96.5948,31.2235],[-96.8,31.5192],[-96.9329,31.7114],[-96.7184,31.8195],[-96.4998,31.8005]]]},\"properties\":{\"name\":\"Limestone\",\"state\":\"TX\"}}]}","noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"4f4e4afde4b07f02db696d38","contributors":{"authors":[{"text":"Rettman, P.L.","contributorId":60663,"corporation":false,"usgs":true,"family":"Rettman","given":"P.L.","affiliations":[],"preferred":false,"id":171457,"contributorType":{"id":1,"text":"Authors"},"rank":1}]}} ,{"id":9617,"text":"ofr84867 - 1984 - Assessment of ground-water contamination by coal-tar derivatives, St. Louis Park area, Minnesota","interactions":[],"lastModifiedDate":"2018-03-12T12:06:21","indexId":"ofr84867","displayToPublicDate":"1994-01-01T00:00:00","publicationYear":"1984","noYear":false,"publicationType":{"id":18,"text":"Report"},"publicationSubtype":{"id":5,"text":"USGS Numbered Series"},"seriesTitle":{"id":330,"text":"Open-File Report","code":"OFR","onlineIssn":"2331-1258","printIssn":"0196-1497","active":true,"publicationSubtype":{"id":5}},"seriesNumber":"84-867","title":"Assessment of ground-water contamination by coal-tar derivatives, St. Louis Park area, Minnesota","docAbstract":"

Operation of a coal-tar distillation and wood-preserving facility in St. Louis Park, Minnesota, during 1918-72 contaminated ground water with coal-tar derivatives and inorganic chemicals. Coal-tar derivatives entered the groundwater system through three major paths: (1) Spills and drippings that percolated to the water table, (2) surface runoff and plant process water that was discharged to wetlands south of the former plant site, and (3) movement of coal tar directly into bedrock aquifers through a multiaquifer well on the site.

\n

In the drift, Platteville, and St. Peter aquifers, ground water flows laterally from west to east and vertically downward. Near the former plant site, creosote-like organic fluids have migrated vertically downward through the drift and are being partially dissolved by ground water. Ground water has preferentially mobilized low-molecular-weight compounds such as phenolic compounds, alkyl-benzenes, and naphthalene, although polynuclear aromatic hydrocarbons as heavy as benzo(a)pyrene have been mobilized at low concentrations. Sorption of high-molecular-weight compounds has retarded their migration down the hydraulic gradient compared to low-molecular-weight compounds in the plume. Some simple phenolic compounds are being degraded to methane and carbon dioxide by bacteria under anaerobic conditions in the drift-PlattevilleSt. Peter aquifer system. Other low-molecular-weight aromatic compounds are apparently being degraded by aerobic bacteria at the periphery of the plume where oxygen is available. Intermediate degradation products such as volatile fatty acids are likely present, but complete conversion of the organic contaminants to innocuous inorganic substances has not been demonstrated. Near and south of 36th and Wooddale Avenues, contaminants enter the St. Peter aquifer where the Glenwood confining unit has been eroded in a buried bedrock valley. Contaminants previously entered the Prairie du Chien-Jordan aquifer through at least one multiaquif er well (W38). Other sources of contaminants and the low concentrations of contaminants hamper delineation of the maximum areal extent of contaminants that are resistant to biologic degradation. These biorefractory compounds will probably continue to migrate down the hydraulic gradients in the drift and Platteville and St. Peter aquifers.

\n

Of particular concern with respect to the health risk to humans are the polynuclear aromatic hydrocarbons, which are a major constituent of coal tar and are found in municipal wells near the site that are completed in the Prairie du Chien-Jordan aquifer. The Prairie du Chien-Jordan aquifer lies 250 to 500 feet below land surface and is relatively well protected from nearsurface sources of contamination by overlying rocks. However, the aquifer has been contaminated since at least 1932 because coal-tar derivatives have entered the aquifer through multiaquifer wells. The most significant single source of contamination in the aquifer is a well drilled on the site in 1917 (well W23) that has contained liquid coal-tar since at least 1958. The introduction, dissolution, and movement of this coal-tar in ground water has contaminated nearby municipal wells. The composition of the tar in well W23, and the ratio of concentrations of individual compounds in water from well W23 to those in municipal well SLP15, are consistent with known hydrologic, chemical, and biologic processes, and the conclusion that contaminants in well SLP15 are due primarily to contaminants introduced at well W23. Most of the major polynuclear aromatic hydrocarbons in the tar, although slightly soluble in water and strongly sorbed by aquifer materials, have moved greater distances at higher concentrations than have the lower-molecular-weight, more soluble compounds such as phenolic compounds and naphthalene. The latter are apparently being degraded by bacteria.

\n

The direction and rate of contaminant movement within the Prairie du Chien-Jordan aquifer changes with time because the ground-water-flow system continually adjusts to hydraulic stresses caused by ground-water withdrawals and flow through multiaquifer wells. Contaminants can move rapidly through the Prairie du Chien-Jordan because the upper part of the aquifer is a carbonate rock having fracture and solution-channel permeability, low effective porosity, and relatively small surface area for sorption. Consequently, the concentration and composition of contaminants in water pumped from individual industrial and municipal wells completed in the aquifer fluctuate with time. Although contaminants have been in the aquifer for at least 50 years and their spatial distribution is complex, concentrations remain highest near their points of introduction through multiaquifer wells near and on the site of the former plant.

\n

Contaminants reached the Ironton-Galesville aquifer through at least two deep multiaquifer wells (W23 and W38), but the extent of contamination in this aquifer, and in the underlying Mount Simon-Hinckley aquifer, is not known.

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The most prominant are the Ohio, Chattanooga, and New Albany Shales. A leaching study was done on six fresh oil shale samples and one retorted oil shale sample. Leaching reagents were distilled water, 0.0005 N sulfuric acid, and 0.05 N sulfuric acid. The concentration of constituents in the leachates were highly variable. The concentration of sodium, manganese, and zinc in the retorted shale leachate was several orders of magnitude higher than those of the leachates of fresh shale samples. The major oil shale outcrop covers approximately 1,000 square miles in a horseshoe pattern from Vanceburg, Lewis County , in the east, to Louisville, Jefferson County, in the west. The Kentucky, Red, and Licking Rivers cross the outcrop belt, the Rolling Fork River flows along the strike of the shale in the southwest part of the outcrop, and the Ohio River flows past the outcrop at the ends of the horseshoe. Oil shale does not appear to significantly alter the water quality of these streams. Oil shale is not an aquifer, but seeps and springs found in the shale indicate that water moves through it. Ground water quality is highly variable. (USGS)","language":"English","publisher":"U.S. Geological Survey","publisherLocation":"Reston, VA","doi":"10.3133/wri844073","usgsCitation":"Leung, S.S., Leist, D., Davis, R.W., and Cordiviola, S., 1984, Leaching study of oil shale in Kentucky: With a section on hydrologic reconnaissance of the oil shale outcrop in Kentucky: U.S. Geological Survey Water-Resources Investigations Report 84-4073, Report: viii, 68 p.; 1 Plate: 26.54 x 26.30 inches, https://doi.org/10.3133/wri844073.","productDescription":"Report: viii, 68 p.; 1 Plate: 26.54 x 26.30 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\"}}]}","noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"4f4e4b32e4b07f02db6b490e","contributors":{"authors":[{"text":"Leung, Samuel S.","contributorId":19594,"corporation":false,"usgs":true,"family":"Leung","given":"Samuel","email":"","middleInitial":"S.","affiliations":[],"preferred":false,"id":194447,"contributorType":{"id":1,"text":"Authors"},"rank":1},{"text":"Leist, D.W.","contributorId":27892,"corporation":false,"usgs":true,"family":"Leist","given":"D.W.","email":"","affiliations":[],"preferred":false,"id":194449,"contributorType":{"id":1,"text":"Authors"},"rank":2},{"text":"Davis, R. W.","contributorId":93459,"corporation":false,"usgs":true,"family":"Davis","given":"R.","email":"","middleInitial":"W.","affiliations":[],"preferred":false,"id":194450,"contributorType":{"id":1,"text":"Authors"},"rank":3},{"text":"Cordiviola, Steven","contributorId":24814,"corporation":false,"usgs":true,"family":"Cordiviola","given":"Steven","email":"","affiliations":[],"preferred":false,"id":194448,"contributorType":{"id":1,"text":"Authors"},"rank":4}]}} ,{"id":28212,"text":"wri844200 - 1984 - Sediment yields in eastern Montana; summary of data and proposed techniques for estimating sediment yields from small, ungaged watersheds","interactions":[],"lastModifiedDate":"2021-11-22T21:47:23.420128","indexId":"wri844200","displayToPublicDate":"1994-01-01T00:00:00","publicationYear":"1984","noYear":false,"publicationType":{"id":18,"text":"Report"},"publicationSubtype":{"id":5,"text":"USGS Numbered Series"},"seriesTitle":{"id":342,"text":"Water-Resources Investigations Report","code":"WRI","active":false,"publicationSubtype":{"id":5}},"seriesNumber":"84-4200","title":"Sediment yields in eastern Montana; summary of data and proposed techniques for estimating sediment yields from small, ungaged watersheds","docAbstract":"Sediment-yield data for 121 sites in eastern Montana have been compiled from results of studies conducted by various Federal, State, and private agencies. Methods used to determine mean annual sediment yields included reservoir sedimentation surveys, suspended-sediment sampling in streams, and estimates of gross erosion and indirect estimation based on physical characteristics of the basin. Multiple-regression equations were developed and evaluated for their adequacy in estimating mean annual sediment yields from small, ungaged watersheds in eastern Montana. Sediment yields determined from reservoir surveys were used as the dependent variable because they were considered the most representative of long-term yields. Independent variables consisted of basin characteristics which could be measured from maps or obtained from published sources. Consequently, equations developed in this study do not require onsite data. Evaluation of equations indicated that the best prediction capability was obtained when reservoir basins were segregated into classes of similar vegetation/soil complex. The predictive capability of regression equations developed for each of three classes of vegetation/soil complex, as indicated by the coefficient of determination (R2), ranged from 0.59 to 0.96. Corresponding standard errors ranged from 95 to 20 percent. The equations are applicable for small drainage basins of 2 square miles or less within the study area. (USGS)","language":"English","publisher":"U.S. Geological Survey","doi":"10.3133/wri844200","usgsCitation":"Lambing, J., 1984, Sediment yields in eastern Montana; summary of data and proposed techniques for estimating sediment yields from small, ungaged watersheds: U.S. Geological Survey Water-Resources Investigations Report 84-4200, iv, 45 p., https://doi.org/10.3133/wri844200.","productDescription":"iv, 45 p.","costCenters":[],"links":[{"id":392019,"rank":2,"type":{"id":36,"text":"NGMDB Index Page"},"url":"https://ngmdb.usgs.gov/Prodesc/proddesc_36060.htm"},{"id":57046,"rank":300,"type":{"id":11,"text":"Document"},"url":"https://pubs.usgs.gov/wri/1984/4200/report.pdf","linkFileType":{"id":1,"text":"pdf"}},{"id":159645,"rank":0,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/wri/1984/4200/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 -108,\n 45\n ],\n [\n -104.054,\n 45\n ],\n [\n -104.054,\n 48.197\n ],\n [\n -108,\n 48.197\n ],\n [\n -108,\n 45\n ]\n ]\n ]\n }\n }\n ]\n}","noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"4f4e4a0be4b07f02db5fbeea","contributors":{"authors":[{"text":"Lambing, J. H.","contributorId":100860,"corporation":false,"usgs":true,"family":"Lambing","given":"J. H.","affiliations":[],"preferred":false,"id":199405,"contributorType":{"id":1,"text":"Authors"},"rank":1}]}} ,{"id":34758,"text":"b1558D - 1984 - White clays of Pennsylvania","interactions":[],"lastModifiedDate":"2017-07-05T12:23:48","indexId":"b1558D","displayToPublicDate":"1994-01-01T00:00:00","publicationYear":"1984","noYear":false,"publicationType":{"id":18,"text":"Report"},"publicationSubtype":{"id":5,"text":"USGS Numbered Series"},"seriesTitle":{"id":306,"text":"Bulletin","code":"B","active":false,"publicationSubtype":{"id":5}},"seriesNumber":"1558","chapter":"D","title":"White clays of Pennsylvania","docAbstract":"

The white clays of Pennsylvania are composed chiefly of kaolinite and various amounts of illite. Most of the white clays are silty and a few are sandy. Quartz or chert is the only nonclay mineral in the whitest material; goethite is also present in the colored samples high in iron. The average alumina content is slightly more than 20 percent in samples from three clay pits and less than 15 percent in samples from five clay pits. The white clay deposits are found in eastern, south-central, and central Pennsylvania. They occur in rocks of the Appalachian basin that range in age from Cambrian to Devonian; however, their age of formation is Cretaceous or later. Some of the deposits are the result of katamorphic alteration, and some are the result of weathered material being transported and deposited in sinkaoles or caverns. The presence of alunite in one deposit suggests the possibility that the clay may be the result of both katamorphic and hydrothermal alteration.

","largerWorkTitle":"Contributions to the geology of mineral deposits","language":"English","publisher":"U.S. Government Printing Office","doi":"10.3133/b1558D","usgsCitation":"Hosterman, J.W., 1984, White clays of Pennsylvania: U.S. Geological Survey Bulletin 1558, iv, 38 p., https://doi.org/10.3133/b1558D.","productDescription":"iv, 38 p.","startPage":"D1","endPage":"D38","costCenters":[],"links":[{"id":62632,"rank":300,"type":{"id":11,"text":"Document"},"url":"https://pubs.usgs.gov/bul/1558d/report.pdf","text":"Report","size":"4.23 MB","linkFileType":{"id":1,"text":"pdf"},"description":"Report"},{"id":165880,"rank":0,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/bul/1558d/report-thumb.jpg"}],"country":"United States","state":"Pennsylvania","county":"Blair County, Centre County, Cumberland County, Huntingdon County, Lancaster County, Monroe County, York County","geographicExtents":"{\"type\":\"FeatureCollection\",\"features\":[{\"type\":\"Feature\",\"geometry\":{\"type\":\"MultiPolygon\",\"coordinates\":[[[[-78.2587,40.2971],[-78.2906,40.2448],[-78.4353,40.3009],[-78.4429,40.2778],[-78.4449,40.2519],[-78.4497,40.2451],[-78.5057,40.2868],[-78.622,40.3253],[-78.6037,40.3477],[-78.5587,40.3675],[-78.5547,40.422],[-78.5592,40.4437],[-78.5421,40.4734],[-78.5408,40.5042],[-78.511,40.5353],[-78.4743,40.5514],[-78.4411,40.5975],[-78.4468,40.6242],[-78.4405,40.6442],[-78.4266,40.6475],[-78.4102,40.6431],[-78.3511,40.722],[-78.3739,40.7472],[-78.3746,40.7567],[-78.3541,40.77],[-78.3381,40.7973],[-78.3169,40.8075],[-78.3019,40.8225],[-78.3021,40.8343],[-78.2883,40.8498],[-78.2676,40.8477],[-78.2476,40.8569],[-78.2466,40.8714],[-78.2381,40.8733],[-78.2478,40.8764],[-78.2418,40.8814],[-78.2333,40.8792],[-78.2284,40.8824],[-78.2213,40.8915],[-78.2281,40.9028],[-78.2214,40.9096],[-78.1857,40.9212],[-78.1706,40.9362],[-78.1561,40.9431],[-78.1598,40.9531],[-78.1677,40.953],[-78.1684,40.9589],[-78.1483,40.9568],[-78.1452,40.9486],[-78.1368,40.965],[-78.1326,40.9641],[-78.1324,40.9482],[-78.1202,40.9442],[-78.0789,40.9566],[-78.0796,40.963],[-78.0894,40.9707],[-78.0822,40.9839],[-78.0853,40.9934],[-78.0689,40.9984],[-78.0634,40.9953],[-78.0635,41.003],[-78.0556,41.0085],[-78.0593,41.0139],[-78.0672,41.0148],[-78.0673,41.022],[-78.0783,41.0329],[-78.0565,41.0393],[-78.0614,41.0457],[-78.059,41.0529],[-78.07,41.0524],[-78.0731,41.0592],[-78.0877,41.0596],[-78.0853,41.0682],[-78.0957,41.0741],[-78.0927,41.0777],[-78.1107,41.1135],[-78.1077,41.1189],[-78.0986,41.1213],[-78.09,41.1172],[-78.084,41.1268],[-78.0675,41.1246],[-78.0694,41.1309],[-78.0572,41.1328],[-78.0536,41.1446],[-78.0408,41.1478],[-78.0372,41.1533],[-78.0153,41.1534],[-78.0103,41.1448],[-78.0024,41.1462],[-77.9964,41.1648],[-77.9885,41.163],[-77.9843,41.1703],[-77.9739,41.1731],[-77.9729,41.2035],[-77.9595,41.2176],[-77.9369,41.2104],[-77.9376,41.224],[-77.9205,41.2291],[-77.9108,41.2441],[-77.8968,41.2537],[-77.8934,41.177],[-77.8055,41.1804],[-77.7454,41.1093],[-77.729,41.1129],[-77.7168,41.108],[-77.7052,41.1148],[-77.6948,41.1098],[-77.6643,41.1094],[-77.6576,41.1022],[-77.6326,41.0954],[-77.5948,41.0741],[-77.5698,41.0668],[-77.5631,41.0591],[-77.5801,41.0496],[-77.5082,40.963],[-77.3317,40.9887],[-77.1427,41.0441],[-77.2032,40.993],[-77.2796,40.9097],[-77.3594,40.8486],[-77.3788,40.8454],[-77.5938,40.7611],[-77.6526,40.7438],[-77.6817,40.7297],[-77.6743,40.7183],[-77.698,40.707],[-77.6979,40.697],[-77.7058,40.6938],[-77.7015,40.6807],[-77.6852,40.6861],[-77.6827,40.683],[-77.7498,40.6343],[-77.7753,40.6243],[-77.8277,40.572],[-77.8385,40.5479],[-77.8165,40.5004],[-77.8934,40.4262],[-77.8958,40.4185],[-77.8891,40.3954],[-77.8697,40.3937],[-77.8727,40.3846],[-77.8599,40.3687],[-77.8437,40.3697],[-77.8213,40.3625],[-77.8111,40.3698],[-77.7634,40.3694],[-77.7502,40.3785],[-77.7022,40.2662],[-77.7208,40.2534],[-77.77,40.2016],[-77.8632,40.064],[-77.9223,40.1037],[-78.0813,40.1362],[-78.1932,40.1973],[-78.2386,40.2252],[-78.2587,40.2971]]],[[[-77.1386,40.0718],[-77.1814,40.0324],[-77.3022,40.015],[-77.4019,39.9933],[-77.4703,39.9444],[-77.4529,39.9725],[-77.4811,39.9925],[-77.5033,40.0147],[-77.5219,40.0505],[-77.5418,40.0736],[-77.546,40.0913],[-77.5598,40.0976],[-77.5634,40.1217],[-77.5821,40.1348],[-77.5917,40.1362],[-77.5941,40.1439],[-77.6104,40.1588],[-77.6183,40.1778],[-77.5936,40.1915],[-77.5617,40.2169],[-77.534,40.2223],[-77.4099,40.2971],[-77.3677,40.3157],[-77.3586,40.3152],[-77.3586,40.3089],[-77.4057,40.2794],[-77.4208,40.2654],[-77.4202,40.259],[-77.4118,40.2572],[-77.3907,40.2631],[-77.3303,40.2934],[-77.3243,40.2902],[-77.3304,40.278],[-77.3111,40.2698],[-77.2357,40.2869],[-77.0898,40.3028],[-77.0138,40.3048],[-76.954,40.3155],[-76.9159,40.3298],[-76.9136,40.318],[-76.9234,40.294],[-76.9068,40.2658],[-76.8614,40.2266],[-76.8379,40.2202],[-76.8285,40.2042],[-76.8002,40.2],[-76.7535,40.1757],[-76.7488,40.1675],[-76.7455,40.1353],[-76.7234,40.122],[-76.696,40.1549],[-76.6791,40.1503],[-76.6645,40.1652],[-76.6459,40.1669],[-76.6174,40.1812],[-76.6089,40.1902],[-76.5733,40.1954],[-76.4372,40.2387],[-76.3134,40.2567],[-76.1514,40.3158],[-75.8757,40.1371],[-75.9412,40.1093],[-75.935,40.0394],[-75.9869,39.9675],[-75.992,39.9544],[-75.9875,39.9399],[-75.9805,39.9334],[-75.9968,39.9282],[-75.9961,39.9028],[-75.9885,39.895],[-75.9912,39.8801],[-75.9877,39.8732],[-75.9932,39.8697],[-76.0015,39.8738],[-76.0091,39.8544],[-76.0211,39.8537],[-76.0191,39.8337],[-76.032,39.8207],[-76.0303,39.813],[-76.0506,39.7846],[-76.0615,39.7789],[-76.066,39.7644],[-76.0841,39.7592],[-76.0909,39.7452],[-76.1011,39.7449],[-76.0959,39.7362],[-76.0996,39.7285],[-76.1104,39.7268],[-76.1115,39.735],[-76.1198,39.7364],[-76.1188,39.726],[-76.1337,39.728],[-76.1392,39.7223],[-76.9998,39.7197],[-77.0002,39.8314],[-76.9888,39.8359],[-76.9815,39.8477],[-76.9581,39.8567],[-76.9652,39.8721],[-76.9771,39.8749],[-76.9848,39.9007],[-76.972,39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John W.","contributorId":48962,"corporation":false,"usgs":true,"family":"Hosterman","given":"John","email":"","middleInitial":"W.","affiliations":[],"preferred":false,"id":213529,"contributorType":{"id":1,"text":"Authors"},"rank":1}]}} ,{"id":25126,"text":"cir930B - 1984 - International strategic minerals inventory summary report; chromium","interactions":[],"lastModifiedDate":"2018-11-05T10:20:12","indexId":"cir930B","displayToPublicDate":"1994-01-01T00:00:00","publicationYear":"1984","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":"930","chapter":"B","title":"International strategic minerals inventory summary report; chromium","docAbstract":"Major world resources of chromium, a strategic mineral commodity, are described in this summary report of information in the International Strategic Minerals Inventory {ISMI}. ISMI is a cooperative data-collection effort of earth-science and mineral-resource agencies in Australia, Canada, the Federal Republic of Germany, the Republic of South Africa, and the United States of America. This report, designed to be of benefit to policy analysts, contains two parts. Part I presents an overview of the resources and potential supply of chromium on the basis of inventory information. Part II contains tables of some of the geologic information and mineral-resource and production data that were collected by ISMI participants.","language":"ENGLISH","publisher":"U.S. Dept. of the Interior, Geological Survey,","doi":"10.3133/cir930B","usgsCitation":"DeYoung, J., Lee, M.P., and Lipin, B., 1984, International strategic minerals inventory summary report; chromium: U.S. Geological Survey Circular 930, v. :ill. ;26 cm.; 41 p., https://doi.org/10.3133/cir930B.","productDescription":"v. :ill. ;26 cm.; 41 p.","costCenters":[{"id":245,"text":"Eastern Mineral and Environmental Resources Science Center","active":true,"usgs":true}],"links":[{"id":54106,"rank":300,"type":{"id":11,"text":"Document"},"url":"https://pubs.usgs.gov/circ/1984/0930b/report.pdf","linkFileType":{"id":1,"text":"pdf"}},{"id":122560,"rank":0,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/circ/1984/0930b/report-thumb.jpg"}],"noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"4f4e49dbe4b07f02db5e0829","contributors":{"authors":[{"text":"DeYoung, J.H. Jr.","contributorId":86367,"corporation":false,"usgs":true,"family":"DeYoung","given":"J.H.","suffix":"Jr.","email":"","affiliations":[],"preferred":false,"id":193259,"contributorType":{"id":1,"text":"Authors"},"rank":1},{"text":"Lee, M. P.","contributorId":40198,"corporation":false,"usgs":true,"family":"Lee","given":"M.","email":"","middleInitial":"P.","affiliations":[],"preferred":false,"id":193257,"contributorType":{"id":1,"text":"Authors"},"rank":2},{"text":"Lipin, B. R.","contributorId":61031,"corporation":false,"usgs":true,"family":"Lipin","given":"B. R.","affiliations":[],"preferred":false,"id":193258,"contributorType":{"id":1,"text":"Authors"},"rank":3}]}} ,{"id":14814,"text":"ofr84614 - 1984 - Changes in channel geomorphology of six eruption-affected tributaries of the Lewis River, 1980-82, Mount St. Helens, Washington","interactions":[],"lastModifiedDate":"2021-11-09T21:40:08.279249","indexId":"ofr84614","displayToPublicDate":"1994-01-01T00:00:00","publicationYear":"1984","noYear":false,"publicationType":{"id":18,"text":"Report"},"publicationSubtype":{"id":5,"text":"USGS Numbered Series"},"seriesTitle":{"id":330,"text":"Open-File Report","code":"OFR","onlineIssn":"2331-1258","printIssn":"0196-1497","active":true,"publicationSubtype":{"id":5}},"seriesNumber":"84-614","title":"Changes in channel geomorphology of six eruption-affected tributaries of the Lewis River, 1980-82, Mount St. Helens, Washington","docAbstract":"The May 18, 1980, eruption of Mount St. Helens generated a lateral blast, lahars and tephra deposits that altered tributary channels in the Lewis River drainage basin. In order to assess potential flood hazards, study channel adjustments, and construct a sediment budget for the perturbed drainages on the east and southeast flanks of the volcano, channel cross sections were monumented and surveyed on Pine Creek, Muddy River, and Smith Creek during September and October of 1980. Additional cross sections were monumented and surveyed on Swift Creek, Bean Creek, and Clearwater Creek during the summer of 1981. The network of 88 channel cross sections has been resurveyed annually. Selected cross sections have been surveyed more frequently, following periods of higher flow. The repetitive cross-section surveys provide measurements of bank erosion or accretion and of channel erosion or aggradation. The report presents channel cross-section profiles constructed from the survey data collected during water years 1980-82. (USGS)","language":"English","publisher":"U.S. Geological Survey","doi":"10.3133/ofr84614","usgsCitation":"Martinson, H.A., Finneran, S.D., and Topinka, L.J., 1984, Changes in channel geomorphology of six eruption-affected tributaries of the Lewis River, 1980-82, Mount St. Helens, Washington: U.S. Geological Survey Open-File Report 84-614, v, 113 p., https://doi.org/10.3133/ofr84614.","productDescription":"v, 113 p.","costCenters":[],"links":[{"id":391540,"rank":3,"type":{"id":36,"text":"NGMDB Index Page"},"url":"https://ngmdb.usgs.gov/Prodesc/proddesc_13473.htm"},{"id":43601,"rank":300,"type":{"id":11,"text":"Document"},"url":"https://pubs.usgs.gov/of/1984/0614/report.pdf","linkFileType":{"id":1,"text":"pdf"}},{"id":148747,"rank":0,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/of/1984/0614/report-thumb.jpg"}],"country":"United States","state":"Washington","otherGeospatial":"Lewis River, Mount St. Helens","geographicExtents":"{\n \"type\": \"FeatureCollection\",\n \"features\": [\n {\n \"type\": \"Feature\",\n \"properties\": {},\n \"geometry\": {\n \"type\": \"Polygon\",\n \"coordinates\": [\n [\n [\n -122.125,\n 46.028\n ],\n [\n -122,\n 46.028\n ],\n [\n -122,\n 46.304\n ],\n [\n -122.125,\n 46.304\n ],\n [\n -122.125,\n 46.028\n ]\n ]\n ]\n }\n }\n ]\n}","noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"4f4e49e5e4b07f02db5e6d54","contributors":{"authors":[{"text":"Martinson, H. A.","contributorId":16834,"corporation":false,"usgs":true,"family":"Martinson","given":"H.","email":"","middleInitial":"A.","affiliations":[],"preferred":false,"id":170063,"contributorType":{"id":1,"text":"Authors"},"rank":1},{"text":"Finneran, S. D.","contributorId":94322,"corporation":false,"usgs":true,"family":"Finneran","given":"S.","email":"","middleInitial":"D.","affiliations":[],"preferred":false,"id":170065,"contributorType":{"id":1,"text":"Authors"},"rank":2},{"text":"Topinka, L. J.","contributorId":80285,"corporation":false,"usgs":true,"family":"Topinka","given":"L.","email":"","middleInitial":"J.","affiliations":[],"preferred":false,"id":170064,"contributorType":{"id":1,"text":"Authors"},"rank":3}]}} ,{"id":29589,"text":"wri834237 - 1984 - Water levels and water-level changes in the Prairie du Chien-Jordan and Mount Simon-Hinckley aquifers, Twin Cities metropolitan area, Minnesota, 1971-80","interactions":[],"lastModifiedDate":"2018-04-02T10:23:19","indexId":"wri834237","displayToPublicDate":"1994-01-01T00:00:00","publicationYear":"1984","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":"83-4237","title":"Water levels and water-level changes in the Prairie du Chien-Jordan and Mount Simon-Hinckley aquifers, Twin Cities metropolitan area, Minnesota, 1971-80","docAbstract":"

The ground-water system in the Twin Cities Metropolitan Area includes five aquifers; two of these aquifers the Prairie du Chien-Jordan and the Mount Simon-Hinckley supply about 80 percent and 10 percent, respectively, of the ground water pumped for public supply. Water levels and changes in water levels in these two aquifers differ greatly in the Twin Cities Metropolitan Area. The Mississippi, Minnesota, and St. Croix Rivers are in hydraulic connection with and influence the pattern of flow in the upper aquifer, the Prairie du Chien-Jordan. Water generally flows toward these streams from water-level highs northeast, northwest, and south of Minneapolis and St. Paul. Consequently, heavy pumping has caused only localized cones of depression in the potentiometric surface of this aquifer. In contrast, the Mount Simon-Hinckley, which has only a slight hydraulic connection to the streams, is greatly influenced by pumping. Pumping in the urban centers of Minneapolis and St. Paul has caused a large cone of depression in the Mount Simon-Hinckley potentiometric surface. During 1971, the measurable cone was centered in eastcentral Hennepin County, was about 25 miles in diameter, and was as much as 150 feet deep at its center.

\n

Between 1971 and 1980, average water levels in the Prairie du Chien-Jordan aquifer changed less than 5 feet in most of the study area, but rose or declined as much as 25 feet locally in response to pumpage and recharge. During this period, seasonal declines of water levels from winter to summer lessened, and the area where these declines exceeded 10 feet decreased.

\n

In contrast, between 1971 and 1980, average water levels in the Mount Simon-Hinckley aquifer rose as much as 60 feet in the center of the cone of depression in response to decreased pumping. Also, the measurable cone of depression contracted from about 25 miles to about 15 miles in diameter. However, because of increased summer pumping due to below-average precipitation during 1980, seasonal water levels declined much more and over a wider area during 1980 than in 1971.

\n

Water-level data suggest that (1) little variation in annual pumpage between 1971 and 1980 from the Prairie du Chien-Jordan aquifer produced generally stable water levels in that aquifer, (2) decreased annual pumpage from the Mount Simon-Hinckley aquifer from 1971 to 1980 caused water levels in that aquifer to rise, and (3) a greater seasonal component of pumpage from the Mount Simon-Hinckley aquifer than from the Prairie du Chien-Jordan produced larger and more widespread seasonal water-level declines in the Mount Simon-Hinckley than in the Prairie du Chien-Jordan, particularly during dry years.

","language":"English","publisher":"U.S. Geological Survey","publisherLocation":"St. Paul, MN","doi":"10.3133/wri834237","collaboration":"Prepared in cooperation with the Metropolitan Council of the Twin Cities and Minnesota Department of Natural Resources","usgsCitation":"Schoenberg, M., 1984, Water levels and water-level changes in the Prairie du Chien-Jordan and Mount Simon-Hinckley aquifers, Twin Cities metropolitan area, Minnesota, 1971-80: U.S. Geological Survey Water-Resources Investigations Report 83-4237, Document: iv, 23 p.; 2 Plates: 34.56 x 30.51 inches and 34.60 x 30.78 inches, https://doi.org/10.3133/wri834237.","productDescription":"Document: iv, 23 p.; 2 Plates: 34.56 x 30.51 inches and 34.60 x 30.78 inches","onlineOnly":"N","additionalOnlineFiles":"N","costCenters":[{"id":392,"text":"Minnesota Water Science 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The Hudson River basin includes streams draining the Hoosic River (205 square miles), Kinderhook Creek (20.9 square miles), and Roeliff Jansen Kill (13.3 square miles) basins in western Massachusetts, eastern New York, and southern Vermont. Drainage areas, using the latest available 1:24,000 scale topographic maps, are re-computed for data-collection sites and computed for the first time for streams draining greater than 3 square miles. Basin characteristics representing 14 commonly used indices to estimate various streamflows are presented for the five gaged streams in the Hoosic River basin. Streamflow characteristics, representing statistics computed using a new data base with records through 1979, include annual and monthly flow statistics , duration of daily flow values, and the annual 7-day mean low flow at the 2-year and 10-year recurrence intervals. Seven-day low-flow statistics are presented for 21 partial-record sites. The procedures used to determine the hydrologic characteristics are summarized. This gazetteer of hydrologic characteristics will aid in the planning and siting of water-resources-related activities and will provide a common data base for governmental agencies and the engineering and planning communities.

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The Housatonic River basin includes streams that drain 504 square miles in western Massachusetts and 30.5 square miles in eastern New York. Drainage areas, using the latest available 1:24,000 scale topographic maps, were computed for the first time for streams draining more than 3 square miles and were recomputed for data-collection sites. Streamflow characteristics for four gaged streams were calculated using a new data base with daily flow records through 1981. These characteristics include annual and monthly flow statistics, duration of daily flow values, and the annual 7-day mean low flow at the 2-year and 10-year recurrence intervals. Seven-day low-flow statistics are presented for 52 partial-record sites, and the procedures used to determine the hydrologic characteristics of the basin are summarized. Basin characteristics representing 14 commonly used indices to estimate various streamflows are provided for selected gaging stations. This gazetteer will aid in the planning and siting of water-resources related activities and will provide a common data base for governmental agencies and the engineering and planning communities. 

","language":"English","publisher":"U.S. Geological Survey","doi":"10.3133/wri844285","usgsCitation":"Wandle, S.W., and Lippert, R.G., 1984, Gazetteer of hydrologic characteristics of streams in Massachusetts — Housatonic River basin: U.S. Geological Survey Water-Resources Investigations Report 84-4285, iv, 34 p., https://doi.org/10.3133/wri844285.","productDescription":"iv, 34 p.","costCenters":[],"links":[{"id":394528,"rank":3,"type":{"id":36,"text":"NGMDB Index Page"},"url":"https://ngmdb.usgs.gov/Prodesc/proddesc_36128.htm"},{"id":124256,"rank":0,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/wri/1984/4285/report-thumb.jpg"},{"id":59150,"rank":300,"type":{"id":11,"text":"Document"},"url":"https://pubs.usgs.gov/wri/1984/4285/report.pdf","linkFileType":{"id":1,"text":"pdf"}}],"country":"United States","state":"Massachusetts","otherGeospatial":"Housatonic River basin","geographicExtents":"{\n \"type\": \"FeatureCollection\",\n \"features\": [\n {\n \"type\": \"Feature\",\n \"properties\": {},\n \"geometry\": {\n \"type\": \"Polygon\",\n \"coordinates\": [\n [\n [\n -73.5,\n 42.05\n ],\n [\n -73.028,\n 42.05\n ],\n [\n -73.028,\n 42.567\n ],\n [\n -73.5,\n 42.567\n ],\n [\n -73.5,\n 42.05\n ]\n ]\n ]\n }\n }\n ]\n}","noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"4f4e4b28e4b07f02db6b1172","contributors":{"authors":[{"text":"Wandle, S. 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The study area in eastern and northeastern Massachusetts also includes the minor river basins draining into Massachusetts Bay, Ipswich Bay, or the Atlantic Ocean. Drainage areas using the latest available 1:24,000 scale topographic maps were computed for the first time for streams draining more than 3 square miles and were recomputed for data-collection sites. Streamflow characteristics at 15 gaging stations were calculated using a new data base with daily flow records through 1981. These characteristics include annual and monthly flow statistics, duration of daily flow values, and the annual 7-day mean low flow at the 2-year and 10-year recurrence intervals. Seven-day low-flow statistics are presented for 95 partial-record sites and the procedures used to determine the hydrologic characteristics of a basin are summarized. Basin characteristics representing 14 commonly used indices to estimate various streamflows are presented for 15 gaged streams. 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No abstract available. 

","language":"English","publisher":"U.S. Geological Survey","publisherLocation":"Reston, VA","doi":"10.3133/ofr84437","usgsCitation":"Hoffman, R., and Scoppettone, G., 1984, Effect of water quality on survival of Lahontan Cutthroat trout eggs in the , west-central Nevada and eastern California: U.S. Geological Survey Open-File Report 84-437, vi, 35 p. , https://doi.org/10.3133/ofr84437.","productDescription":"vi, 35 p. ","costCenters":[],"links":[{"id":152084,"rank":0,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/of/1984/0437/report-thumb.jpg"},{"id":369657,"rank":2,"type":{"id":11,"text":"Document"},"url":"https://pubs.usgs.gov/of/1984/0437/report.pdf","linkFileType":{"id":1,"text":"pdf"}}],"country":"United States","state":"California, Nevada","otherGeospatial":"Truckee River","geographicExtents":"{\n \"type\": \"FeatureCollection\",\n \"features\": [\n {\n \"type\": \"Feature\",\n \"properties\": {},\n \"geometry\": {\n \"type\": \"Polygon\",\n \"coordinates\": [\n [\n [\n -120.22064208984375,\n 39.2492708462234\n ],\n [\n -119.344482421875,\n 39.2492708462234\n ],\n [\n -119.344482421875,\n 39.86547951378614\n ],\n [\n -120.22064208984375,\n 39.86547951378614\n ],\n [\n -120.22064208984375,\n 39.2492708462234\n ]\n ]\n ]\n }\n }\n ]\n}","noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"4f4e4a4be4b07f02db62540d","contributors":{"authors":[{"text":"Hoffman, R.J.","contributorId":38582,"corporation":false,"usgs":true,"family":"Hoffman","given":"R.J.","email":"","affiliations":[],"preferred":false,"id":180770,"contributorType":{"id":1,"text":"Authors"},"rank":1},{"text":"Scoppettone, G.G.","contributorId":22793,"corporation":false,"usgs":true,"family":"Scoppettone","given":"G.G.","email":"","affiliations":[],"preferred":false,"id":180769,"contributorType":{"id":1,"text":"Authors"},"rank":2}]}} ,{"id":29841,"text":"wri844251 - 1984 - Aldicarb-pesticide contamination of ground water in eastern Suffolk County, Long Island, New York","interactions":[],"lastModifiedDate":"2012-02-02T00:09:01","indexId":"wri844251","displayToPublicDate":"1994-01-01T00:00:00","publicationYear":"1984","noYear":false,"publicationType":{"id":18,"text":"Report"},"publicationSubtype":{"id":5,"text":"USGS Numbered Series"},"seriesTitle":{"id":342,"text":"Water-Resources Investigations Report","code":"WRI","active":false,"publicationSubtype":{"id":5}},"seriesNumber":"84-4251","title":"Aldicarb-pesticide contamination of ground water in eastern Suffolk County, Long Island, New York","docAbstract":"Aldicarb, a toxic oxime-carbamate pesticide that was believed incapable of reaching ground water, was used in potato-farming areas of eastern Suffolk County, New York during 1975-80. In 1979, aldicarb was found in substantial concentrations in ground water throughout the area. The New York State Department of Health set a limit of 7 micrograms per liter for aldicarb in drinking water. Extensive ground-water sampling into 1980 showed widespread contamination ranging from small amounts to as much as 515 micrograms per liter. In 1980, the U.S. Environmental Protection Agency banned the use of aldicarb on Long Island at the manufacturer 's request. A 1982 sampling study found aldicarb to have penetrated to about 40 feet below the water table in concentrations ranging from below detection limit to 239 micrograms per liter. Despite reputed toxicity, no instance of aldicarb poisoning on Long Island has been documented. The excessive aldicarb concentrations in the ground water of eastern Long Island may persist for decades; the duration has not been precisely determined and remains under investigation. (USGS)","language":"ENGLISH","publisher":"U.S. Geological Survey,","doi":"10.3133/wri844251","usgsCitation":"Soren, J., and Stelz, W., 1984, Aldicarb-pesticide contamination of ground water in eastern Suffolk County, Long Island, New York: U.S. Geological Survey Water-Resources Investigations Report 84-4251, vi, 40 p. :ill., maps ;28 cm., https://doi.org/10.3133/wri844251.","productDescription":"vi, 40 p. :ill., maps ;28 cm.","costCenters":[],"links":[{"id":123646,"rank":0,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/wri/1984/4251/report-thumb.jpg"},{"id":58648,"rank":400,"type":{"id":17,"text":"Plate"},"url":"https://pubs.usgs.gov/wri/1984/4251/plate-1.pdf","linkFileType":{"id":1,"text":"pdf"}},{"id":58649,"rank":300,"type":{"id":11,"text":"Document"},"url":"https://pubs.usgs.gov/wri/1984/4251/report.pdf","linkFileType":{"id":1,"text":"pdf"}}],"noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"4f4e4ae0e4b07f02db688006","contributors":{"authors":[{"text":"Soren, Julian","contributorId":54184,"corporation":false,"usgs":true,"family":"Soren","given":"Julian","email":"","affiliations":[],"preferred":false,"id":202224,"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":202225,"contributorType":{"id":1,"text":"Authors"},"rank":2}]}} ]}