The rocks of southwestern Umnak Island (Nikolski area) consist mainly of a slightly deformed marine sedimentary sequence intruded by hypabyssal quartz diorite sills and small plutons. Laminated and thin-bedded argillaceous and tuffaceous mudstone and siltstone reflect volcanic arc sedimentation from late Eocene to early Oligocene time. Zeolite facies minerals formed during diagenesis include heulandite, analcime, quartz, chlorite, and smectite. Radiometric dates from sill rock and plutons yield apparent ages of about 30 Ma, i.e, middle Oligocene. Chemical data from igneous rocks exhibit calc-alkaline and tholeiitic volcanic arc differentiation trends. Dikes of pyroxene basalt yield K/Ar apparent ages as old at 17 Ma, and a columnar-jointed plug of pyroxene basalt is as young as 1 Ma. The fossil ages and radiometric dates from southwestern Umnak Island are similar to those reported from other central and eastern Aleutian islands, and indicate uniformity in the chronology and tectonic development of the archipelago during the Paleogene. Paleomagnetic data suggest possible northward movement but remain equivocal and more work is indicated.
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]\n}","volume":"21","issue":"2","noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"505a73eae4b0c8380cd77307","contributors":{"authors":[{"text":"McLean, H.","contributorId":11212,"corporation":false,"usgs":true,"family":"McLean","given":"H.","email":"","affiliations":[],"preferred":false,"id":367049,"contributorType":{"id":1,"text":"Authors"},"rank":1},{"text":"Hein, J.R. 0000-0002-5321-899X","orcid":"https://orcid.org/0000-0002-5321-899X","contributorId":61429,"corporation":false,"usgs":true,"family":"Hein","given":"J.R.","affiliations":[],"preferred":false,"id":367050,"contributorType":{"id":1,"text":"Authors"},"rank":2}]}} ,{"id":70013939,"text":"70013939 - 1984 - Geochemistry of tholeiitic and alkalic lavas from the Koolau Range, Oahu, Hawaii: Implications for Hawaiian volcanism","interactions":[],"lastModifiedDate":"2020-10-01T18:41:29.620455","indexId":"70013939","displayToPublicDate":"1984-01-01T00:00:00","publicationYear":"1984","noYear":false,"publicationType":{"id":2,"text":"Article"},"publicationSubtype":{"id":10,"text":"Journal Article"},"seriesTitle":{"id":1427,"text":"Earth and Planetary Science Letters","active":true,"publicationSubtype":{"id":10}},"title":"Geochemistry of tholeiitic and alkalic lavas from the Koolau Range, Oahu, Hawaii: Implications for Hawaiian volcanism","docAbstract":"Lavas of the post-erosional, alkalic Honolulu Volcanics have significantly lower 87Sr/86Sr and higher 143Nd/144Nd than the older and underlying Koolau tholeiites which form the Koolau shield of eastern Oahu, Hawaii. Despite significant compositional variation within lavas forming the Honolulu Volcanics, these lavas are isotopically (Sr, Nd, Pb) very similar which contrasts with the isotopic heterogeneity of the Koolau tholeiites. Among Hawaiian tholeiitic suites, the Koolau lavas are geochemically distinct because of their lower iron contents and Sr and Nd isotopic ratios which range to bulk earth values. These geochemical data preclude simple models such as derivation of the Honolulu Volcanics and Koolau tholeiites from a common source by different degrees of melting or by mixing of two geochemically distinct sources. There may be no genetic relationship between the origin and evolution of these two lava suites; however, the trend shown by Koolau Range lavas of increasing 143Nd/144Nd and decreasing 87Sr/86Sr with decreasing eruption age and increasing alkalinity also occurs at Haleakala, East Molokai and Kauai volcanoes. A complex mixing model proposed for Haleakala lavas can account for the variations in Sr and Nd isotopic ratios and incompatible element abundances found in lavas from the Koolau Range. This model may reflect mixing and melting processes occurring during ascent of relatively enriched mantle through relatively depleted MORB-related lithosphere. Although two isotopically distinct components may be sufficient to explain Sr and Nd isotopic variations at individual Hawaiian volcanoes, more than two isotopically distinct materials are required to explain variations of Sr, Nd and Pb isotopic ratios in all Hawaiian lavas.
Black shales of Devonian age in the Appalachian Basin are a unique rock sequence. The high content of organic matter, which imparts the characteristic lithology, has for years attracted considerable interest in the shales as a possible source of energy. The recent energy shortage prompted the U.S. Department of Energy through the Eastern Gas Shales Project of the Morgantown Energy Technology Center to underwrite a research program to determine the geologic, geochemical, and structural characteristics of the Devonian black shales in order to enhance the recovery of gas from the shales. Geologic studies by Federal and State agencies and academic institutions produced a regional stratigraphic network that correlates the 15 ft black shale sequence in Tennessee with 3000 ft of interbedded black and gray shales in central New York. These studies correlate the classic Devonian black shale sequence in New York with the Ohio Shale of Ohio and Kentucky and the Chattanooga Shale of Tennessee and southwestern Virginia. Biostratigraphic and lithostratigraphic markers in conjunction with gamma-ray logs facilitated long-range correlations within the Appalachian Basin. Basinwide correlations, including the subsurface rocks, provided a basis for determining the areal distribution and thickness of the important black shale units. The organic carbon content of the dark shales generally increases from east to west across the basin and is sufficient to qualify as a hydrocarbon source rock. Significant structural features that involve the black shale and their hydrocarbon potential are the Rome trough, Kentucky River and Irvine-Paint Creek fault zone, and regional decollements and ramp zones.
","language":"English","publisher":"Elsevier","doi":"10.1016/0146-6380(84)90011-1","usgsCitation":"Roen, J.B., 1984, Geology of the Devonian black shales of the Appalachian Basin: Organic Geochemistry, v. 5, no. 4, p. 241-254, https://doi.org/10.1016/0146-6380(84)90011-1.","productDescription":"14 p.","startPage":"241","endPage":"254","costCenters":[],"links":[{"id":225802,"rank":1,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/thumbnails/outside_thumb.jpg"}],"country":"United States","state":"Kentucky, Maryland, New York, Ohio, Pennsylvania, Tennessee, Virginia, West Virginia","otherGeospatial":"Appalachian Basin","geographicExtents":"{\"type\":\"FeatureCollection\",\"features\":[{\"type\":\"Feature\",\"geometry\":{\"type\":\"MultiPolygon\",\"coordinates\":[[[[-89.5391,36.498201],[-89.55264,36.577178],[-89.493495,36.4787],[-89.236542,36.566824],[-89.041263,37.202881],[-88.476127,37.068223],[-88.482612,37.354915],[-88.109417,37.472369],[-88.125033,37.707094],[-87.940069,37.88767],[-87.672397,37.829127],[-87.380247,37.935596],[-87.14195,37.816176],[-86.794985,37.988982],[-86.604624,37.858272],[-86.431749,38.126121],[-86.271802,38.137874],[-86.048458,37.959369],[-85.823764,38.280569],[-85.425787,38.52873],[-85.456978,38.689135],[-84.835672,38.784289],[-84.806082,41.696089],[-83.504334,41.731547],[-82.513827,41.384257],[-81.768898,41.491663],[-79.148723,42.553672],[-78.868556,42.770258],[-79.061388,43.251349],[-78.370221,43.376505],[-76.952174,43.270692],[-76.235834,43.529256],[-76.133697,43.940356],[-76.360306,44.070907],[-76.312647,44.199044],[-75.26825,44.855119],[-74.868663,45.001274],[-73.343124,45.01084],[-73.430325,43.590532],[-73.247631,43.51924],[-73.276421,42.746019],[-73.508142,42.086257],[-73.482709,41.21276],[-73.727775,41.100696],[-73.782577,40.837601],[-72.635374,40.990536],[-72.245348,41.161217],[-72.273657,41.051533],[-72.116368,40.999796],[-71.869558,41.075046],[-73.145266,40.645491],[-73.934512,40.545175],[-74.013784,40.756601],[-73.896479,40.981697],[-74.694914,41.357423],[-74.838366,41.277286],[-75.135526,40.973807],[-75.19872,40.705298],[-75.061489,40.422848],[-74.733804,40.174509],[-75.140006,39.888465],[-75.662822,39.82115],[-75.788395,39.700287],[-75.693521,38.460128],[-75.053483,38.451274],[-75.87767,37.135604],[-76.023664,37.268971],[-75.712065,37.936082],[-75.846621,37.925785],[-75.938577,38.272329],[-76.188644,38.267434],[-76.320843,38.459862],[-76.190902,38.621092],[-76.308922,38.813346],[-76.205063,38.892726],[-76.333703,38.984607],[-76.168332,38.996546],[-76.27566,39.160304],[-75.986298,39.510398],[-76.497977,39.204697],[-76.438845,39.0529],[-76.559697,38.767443],[-76.329433,38.073986],[-77.040638,38.444618],[-77.256412,38.396755],[-77.175969,38.604113],[-77.26443,38.582845],[-77.286202,38.347025],[-77.024866,38.386791],[-76.910832,38.197073],[-76.265998,37.91138],[-76.339892,37.655966],[-76.722156,37.83668],[-76.252415,37.447274],[-76.475927,37.250543],[-76.300352,37.00885],[-76.780532,37.209336],[-76.482407,36.917364],[-76.058154,36.916947],[-75.867044,36.550754],[-81.680137,36.585518],[-81.718282,36.350388],[-82.02664,36.130222],[-82.325169,36.119363],[-82.531292,35.972188],[-82.701065,36.034404],[-82.955751,35.809802],[-83.880074,35.518745],[-84.052612,35.269982],[-84.28252,35.227877],[-84.321869,34.988408],[-90.309297,34.995694],[-90.09061,35.118287],[-90.166594,35.274588],[-89.992975,35.560774],[-89.923161,35.514428],[-89.915491,35.754917],[-89.68182,35.88999],[-89.699677,36.230821],[-89.534507,36.261802],[-89.5391,36.498201]],[[-77.038598,38.791513],[-77.002498,38.96541],[-77.0915,38.95651],[-77.038598,38.791513]]],[[[-74.144428,40.53516],[-74.219787,40.502603],[-74.120186,40.642201],[-74.144428,40.53516]]]]},\"properties\":{\"name\":\"Kentucky\",\"nation\":\"USA \"}}]}","volume":"5","issue":"4","noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"505a256fe4b0c8380cd588db","contributors":{"authors":[{"text":"Roen, John B.","contributorId":14425,"corporation":false,"usgs":true,"family":"Roen","given":"John","email":"","middleInitial":"B.","affiliations":[],"preferred":false,"id":367086,"contributorType":{"id":1,"text":"Authors"},"rank":1}]}} ,{"id":70013346,"text":"70013346 - 1984 - Sm-Nd, K-Ar and petrologic study of some kimberlites from eastern United States and their implication for mantle evolution","interactions":[],"lastModifiedDate":"2012-03-12T17:18:40","indexId":"70013346","displayToPublicDate":"1984-01-01T00:00:00","publicationYear":"1984","noYear":false,"publicationType":{"id":2,"text":"Article"},"publicationSubtype":{"id":10,"text":"Journal Article"},"seriesTitle":{"id":1336,"text":"Contributions to Mineralogy and Petrology","active":true,"publicationSubtype":{"id":10}},"title":"Sm-Nd, K-Ar and petrologic study of some kimberlites from eastern United States and their implication for mantle evolution","docAbstract":"We provide new data on Sm-Nd systematics, K-Ar dating and the major element chemistry of kimberlites from the eastern United States (mostly from central New York State) and their constituent mineral phases of olivine, clinopyroxene, garnet, phlogopite and perovskite. In addition, we report Nd-isotopes in a few kimberlites from South Africa, Lesotho and from the eastern part of China. The major element compositions of the New York dike rocks and of their constituent minerals including a xenolith of eclogite are comparable with those from the Kimberley area in South Africa. The K-Ar age of emplacement of the New York dikes is further established to be 143 Ma. We have analyzed the Nd-isotopic composition of the following kimberlites and related rocks: Nine kimberlite pipes from South Africa and Lesotho, two from southern India; one from the U.S.S.R., fifteen kimberlite pipes and related dike rocks from eastern and central U.S. and two pipes from the Shandong Province of eastern China. The age of emplacement of these kimberlites ranges from 1300 million years to 90 million years. The initial Nd-isotopic compositions of these kimberlitic rocks expressed as e{open}NdIwith respect to a chondritic bulk-earth growth-curve show a range between 0 and +4, with the majority of the kimberlites being in the range 0 to +2. This range is not matched by any other suite of mantle-derived igneous rocks. This result strengthens our earlier conclusion that kimberlitic liquids are derived from a relatively primeval and unique mantle reservoir with a nearly chondritic Sm/Nd ratio. ?? 1984 Springer-Verlag.","largerWorkType":{"id":2,"text":"Article"},"largerWorkTitle":"Contributions to Mineralogy and Petrology","largerWorkSubtype":{"id":10,"text":"Journal Article"},"language":"English","publisherLocation":"Springer-Verlag","doi":"10.1007/BF00373709","issn":"00107999","usgsCitation":"Basu, A.R., Rubury, E., Mehnert, H., and Tatsumoto, M., 1984, Sm-Nd, K-Ar and petrologic study of some kimberlites from eastern United States and their implication for mantle evolution: Contributions to Mineralogy and Petrology, v. 86, no. 1, p. 35-44, https://doi.org/10.1007/BF00373709.","startPage":"35","endPage":"44","numberOfPages":"10","costCenters":[],"links":[{"id":220031,"rank":0,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/thumbnails/outside_thumb.jpg"},{"id":205000,"rank":9999,"type":{"id":10,"text":"Digital Object Identifier"},"url":"https://dx.doi.org/10.1007/BF00373709"}],"volume":"86","issue":"1","noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"505b917de4b08c986b31992b","contributors":{"authors":[{"text":"Basu, A. R.","contributorId":99697,"corporation":false,"usgs":true,"family":"Basu","given":"A.","email":"","middleInitial":"R.","affiliations":[],"preferred":false,"id":365861,"contributorType":{"id":1,"text":"Authors"},"rank":1},{"text":"Rubury, E.","contributorId":71692,"corporation":false,"usgs":true,"family":"Rubury","given":"E.","email":"","affiliations":[],"preferred":false,"id":365859,"contributorType":{"id":1,"text":"Authors"},"rank":2},{"text":"Mehnert, H.","contributorId":52326,"corporation":false,"usgs":true,"family":"Mehnert","given":"H.","affiliations":[],"preferred":false,"id":365858,"contributorType":{"id":1,"text":"Authors"},"rank":3},{"text":"Tatsumoto, M.","contributorId":76798,"corporation":false,"usgs":true,"family":"Tatsumoto","given":"M.","email":"","affiliations":[],"preferred":false,"id":365860,"contributorType":{"id":1,"text":"Authors"},"rank":4}]}} ,{"id":70006919,"text":"70006919 - 1984 - Monocrotophos and dicrotophos residues in birds as a result of misuse of organophosphates in Matagorda county Texas USA","interactions":[],"lastModifiedDate":"2020-04-28T17:06:14.439619","indexId":"70006919","displayToPublicDate":"1984-01-01T00:00:00","publicationYear":"1984","noYear":false,"publicationType":{"id":2,"text":"Article"},"publicationSubtype":{"id":10,"text":"Journal Article"},"seriesTitle":{"id":2533,"text":"Journal of the Association of Official Analytical Chemists","active":true,"publicationSubtype":{"id":10}},"title":"Monocrotophos and dicrotophos residues in birds as a result of misuse of organophosphates in Matagorda county Texas USA","docAbstract":"About 1100 birds of 12 spp. [Red-winged blackbird (Agelaius phoeniceus), great-tailed grackle (Quiscalus mexicanus), brown-headed cowbird (Molothrus ater), mourning dove (Zenaida macrours), Eastern meadowlark (Sturnella magna), vesper sparrow (Pooecetes gramineus), common snipe (Gallinago gallinago), blue-winged teal (Anas discors), mottled duck (Anas fulvigula), common moorhen (Gallinula chloropus), redhead (Aythya americana) and ruddy turnstone (Arenaria interpres)] died from organophosphate poisoning in Matagorda County on the Texas Gulf Coast in March and May 1982. Birds died from feeding on rice seed that was illegally treated with dicrotophos or monocrotophos and placed near rice fields as bait to attract and kill birds. Brain acetylcholinesterase inhibition of affected birds averaged 87% (range 82-89%), and contents of gastrointestinal tracts contained residues of dicrotophos (5.6-14 ppm) or monocrotophos (2.1-13 ppm). Rice seed collected at mortality sites contained 210 ppm dicrotophos or 950 ppm monocrotophos. Mortality from dicrotophos poisoning continued for almost 3 wk. The practice of illegally treating rice seed with either of the 2 organophosphates appears to be infrequent but widespread at present.","largerWorkTitle":"","language":"English","publisher":"AOAC International","publisherLocation":"Gaithersburg, MD","doi":"10.1093/jaoac/67.4.827","collaboration":"","usgsCitation":"Flickinger, E.L., White, D.H., Mitchell, C.A., and Lamont, T.G., 1984, Monocrotophos and dicrotophos residues in birds as a result of misuse of organophosphates in Matagorda county Texas USA: Journal of the Association of Official Analytical Chemists, v. 67, no. 4, p. 827-828, https://doi.org/10.1093/jaoac/67.4.827.","productDescription":"2 p.","startPage":"827","endPage":"828","numberOfPages":"2","costCenters":[{"id":606,"text":"Upper Midwest Environmental Sciences Center","active":true,"usgs":true}],"links":[{"id":490002,"rank":0,"type":{"id":40,"text":"Open Access Publisher Index Page"},"url":"https://doi.org/10.1093/jaoac/67.4.827","text":"Publisher Index Page"},{"id":263440,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/thumbnails/outside_thumb.jpg"}],"country":"United States","state":"Texas","county":"Matagorda County","geographicExtents":"{ \"type\": \"FeatureCollection\", \"features\": [ { \"type\": \"Feature\", \"properties\": {}, \"geometry\": { \"type\": \"Polygon\", \"coordinates\": [ [ [ -96.3774,28.4001 ], [ -96.3774,29.2292 ], [ -95.5044,29.2292 ], [ -95.5044,28.4001 ], [ -96.3774,28.4001 ] ] ] } } ] }","volume":"67","issue":"4","noUsgsAuthors":false,"publicationDate":"2020-02-15","publicationStatus":"PW","scienceBaseUri":"50e07632e4b0fec3206ed566","contributors":{"authors":[{"text":"Flickinger, Edward L.","contributorId":48907,"corporation":false,"usgs":true,"family":"Flickinger","given":"Edward","email":"","middleInitial":"L.","affiliations":[],"preferred":false,"id":355463,"contributorType":{"id":1,"text":"Authors"},"rank":1},{"text":"White, Donald H.","contributorId":97868,"corporation":false,"usgs":true,"family":"White","given":"Donald","email":"","middleInitial":"H.","affiliations":[],"preferred":false,"id":355466,"contributorType":{"id":1,"text":"Authors"},"rank":2},{"text":"Mitchell, C. A.","contributorId":54543,"corporation":false,"usgs":true,"family":"Mitchell","given":"C.","email":"","middleInitial":"A.","affiliations":[],"preferred":false,"id":355465,"contributorType":{"id":1,"text":"Authors"},"rank":3},{"text":"Lamont, T. G.","contributorId":51252,"corporation":false,"usgs":true,"family":"Lamont","given":"T.","email":"","middleInitial":"G.","affiliations":[],"preferred":false,"id":355464,"contributorType":{"id":1,"text":"Authors"},"rank":4}]}} ,{"id":70013142,"text":"70013142 - 1984 - Chromite from the Blue Ridge province of North Carolina","interactions":[],"lastModifiedDate":"2023-02-06T17:24:41.688724","indexId":"70013142","displayToPublicDate":"1984-01-01T00:00:00","publicationYear":"1984","noYear":false,"publicationType":{"id":2,"text":"Article"},"publicationSubtype":{"id":10,"text":"Journal Article"},"seriesTitle":{"id":732,"text":"American Journal of Science","active":true,"publicationSubtype":{"id":10}},"title":"Chromite from the Blue Ridge province of North Carolina","docAbstract":"Accessory chromite in dunite shows a variety of textures that indicate alteration. One group, type A, consists of four types of chromite: clean chromite; lattice chromite, in which the invading chlorite occurs along three directions in the (100) plane; optically zoned chromite; and poikiloblastic chromite. Most of type A chromites are surrounded by chromian clinochlore. The other group, type B, consists of euhedral to subhedral chromite grains which are included in olivine or pyroxene. The accessory chromites define a trend exhibited by chromite from other areas that have undergone metamorphism. Olivine-spinel geothermometry indicates equilibration temperatures near 700 degrees C, roughly consistent with mineral assemblages in the host gneisses. Thus, the Blue Ridge dunites are metamorphic rocks and not primary mantle peridotites.
","language":"English","publisher":"American Journal of Science","doi":"10.2475/ajs.284.4-5.507","usgsCitation":"Lipin, B.R., 1984, Chromite from the Blue Ridge province of North Carolina: American Journal of Science, v. 284, no. 4-5, p. 507-529, https://doi.org/10.2475/ajs.284.4-5.507.","productDescription":"23 p.","startPage":"507","endPage":"529","numberOfPages":"23","costCenters":[{"id":245,"text":"Eastern Mineral and Environmental Resources Science Center","active":true,"usgs":true}],"links":[{"id":220465,"rank":1,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/thumbnails/outside_thumb.jpg"}],"country":"United States","state":"North Carolina","otherGeospatial":"Blue Ridge province","geographicExtents":"{\n \"type\": \"FeatureCollection\",\n \"features\": [\n {\n \"type\": \"Feature\",\n \"properties\": {},\n \"geometry\": {\n \"coordinates\": [\n [\n [\n -82.33171420337254,\n 35.16172419965186\n ],\n [\n -80.3549144361715,\n 36.498699563512446\n ],\n [\n -81.74146209797348,\n 36.584654476715144\n ],\n [\n -82.80252728344371,\n 35.94894466653062\n ],\n [\n -84.26280999082724,\n 35.237774229031075\n ],\n [\n -84.35734406944783,\n 35.017268463518306\n ],\n [\n -83.03490976176494,\n 34.9746276516219\n ],\n [\n -82.33171420337254,\n 35.16172419965186\n ]\n ]\n ],\n \"type\": \"Polygon\"\n }\n }\n ]\n}","volume":"284","issue":"4-5","noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"5059f5e2e4b0c8380cd4c489","contributors":{"authors":[{"text":"Lipin, Bruce R. blipin@usgs.gov","contributorId":5723,"corporation":false,"usgs":true,"family":"Lipin","given":"Bruce","email":"blipin@usgs.gov","middleInitial":"R.","affiliations":[],"preferred":true,"id":365391,"contributorType":{"id":1,"text":"Authors"},"rank":1}]}} ,{"id":28191,"text":"wri834126 - 1983 - Chemical and hydrologic assessment of the Caloosahatchee River basin, Lake Okeechobee to Franklin Lock, Florida","interactions":[],"lastModifiedDate":"2023-01-13T20:49:16.597178","indexId":"wri834126","displayToPublicDate":"2021-12-12T20:40:00","publicationYear":"1983","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":"83-4126","title":"Chemical and hydrologic assessment of the Caloosahatchee River basin, Lake Okeechobee to Franklin Lock, Florida","docAbstract":"Annual discharge (1970-79 water years) from Lake Okeechobee to the Caloosahatchee River averaged 51 percent of the total river discharge at Franklin Lock and ranged from 10 to 71 percent of total discharge. Excluding rainfall on the river surface and upstream seepage, surface and subsurface runoff from the basin accounted for the remaining total river discharge at Franklin Lock. Nitrogen and phosphorus were in sufficient supply most of the time to support algal growth in the river. During algal blooms, however, nitrite plus nitrate nitrogen was depleted and probably became limiting. Nitrite plus nitrate was the predominant form of inorganic nitrogen in the river and in most tributaries. Average concentrations in the river were 0.18 to 0.21 milligram per liter. Average concentrations in most tributaries were less than those in the river. Average concentrations of total phosphorus in many tributaries fell within the same range as that in the river (0.08 to 0.15 milligram per liter), but some tributaries in the eastern part of the basin had greater average concentrations.
","language":"English","publisher":"U.S. Geological Survey","publisherLocation":"Reston, VA","doi":"10.3133/wri834126","collaboration":"Prepared in cooperation with Lee County","usgsCitation":"La Rose, H., and McPherson, B.F., 1983, Chemical and hydrologic assessment of the Caloosahatchee River basin, Lake Okeechobee to Franklin Lock, Florida: U.S. Geological Survey Water-Resources Investigations Report 83-4126, vi, 66 p., https://doi.org/10.3133/wri834126.","productDescription":"vi, 66 p.","costCenters":[{"id":27821,"text":"Caribbean-Florida Water Science Center","active":true,"usgs":true}],"links":[{"id":57028,"rank":2,"type":{"id":11,"text":"Document"},"url":"https://pubs.usgs.gov/wri/1983/4126/wri834126.pdf","text":"Report","linkFileType":{"id":1,"text":"pdf"},"description":"WRI 83-4126"},{"id":123966,"rank":1,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/wri/1983/4126/coverthb.jpg"},{"id":411916,"rank":3,"type":{"id":36,"text":"NGMDB Index Page"},"url":"https://ngmdb.usgs.gov/Prodesc/proddesc_35791.htm","linkFileType":{"id":5,"text":"html"}}],"country":"United States","state":"Florida","otherGeospatial":"Caloosahatchee River basin","geographicExtents":"{\n \"type\": \"FeatureCollection\",\n \"features\": [\n {\n \"type\": \"Feature\",\n \"properties\": {},\n \"geometry\": {\n \"type\": \"Polygon\",\n \"coordinates\": [\n [\n [\n -81.711,\n 26.5\n ],\n [\n -81,\n 26.5\n ],\n [\n -81,\n 27\n ],\n [\n -81.711,\n 27\n ],\n [\n -81.711,\n 26.5\n ]\n ]\n ]\n }\n }\n ]\n}","contact":"Caribbean-Florida Water Science Center
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3321 College Avenue
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Samples of brown and white fat from hibernating bats (big brown bat, Eptesicus fuscus; little brown bat, Myotis lucifugus; and eastern pipistrelle, Pipistrellus subflavus) collected in western Maryland, USA, were analysed to determine lipid and DDE content. Amounts of brown fat, expressed as percentages of total bat weight, were the same for all three species. Lipid content of brown fat was significantly less than that of white fat. Lipids of brown fat contained significantly higher (28%) concentrations of DDE than did lipids of white fat. In our mixed-species sample of 14 bats, concentrations of DDE increased exponentially in both brown and white fat as white fat reserves declined. Brown fat facilitates arousal from hibernation by producing heat through rapid metabolism of triglycerides. The question is raised whether organochlorine residues, such as DDE, may be concentrated and then liberated in lethal amounts by the processes of hibernation and arousal.
Analysis of heavy-mineral distribution in modern sediments of Willapa Bay, Washington, indicates a dominance of two mineralogic assemblages, one with approximately equivalent amounts of hornblende, orthopyroxene and clinopyroxene, the other dominated by clinopyroxene. The hornblende-orthopyroxene-clinopyroxene suite is derived from the Columbia River, which discharges into the ocean a short distance south of the bay. The clinopyroxene suite is restricted in modern sediments to sands in rivers flowing into the bay from the east. The heavy-mineral distributions suggest that sand discharged from the Columbia River, borne north by longshore transport, and carried into the bay by tidal currents accounts for most of the sand within the interior of Willapa Bay.
Three heavy-mineral assemblages are present in the surrounding Pleistocene deposits; two of these are identical to the modern assemblages described above. These heavy-mineral assemblages reflect the relative influence of tidal and fluvial processes on the Late Pleistocene deposits; their relative influences are consistent with those inferred on the basis of sedimentary structures and stratigraphic relations in about two-thirds of the samples examined. The anomalies can be explained by recycling of sand from older deposits. The persistence of the two heavy-mineral assemblages suggests that the pattern of estuarine sedimentation in Late Pleistocene deposits closely resembled that of the modern bay.
The third heavy-mineral suite, dominated by epidote, occurs in a few older Pleistocene units. On the north side of the bay, the association of this suite with southwest-directed foresets in crossbedded gravel indicates derivation from the northeast, perhaps from an area of glacial outwash. The presence of this suite in ancient estuarine sands exposed on the east side of the bay suggests that input from this northerly source may have intermittently dominated bay deposition in the past.
","language":"English","publisher":"Elsevier","doi":"10.1016/0037-0738(83)90060-X","issn":"00370738","usgsCitation":"Luepke, G., and Clifton, H.E., 1983, Heavy-mineral distribution in modern and ancient bay deposits, Willapa Bay, Washington, U.S.A.: Sedimentary Geology, v. 35, no. 4, p. 233-247, https://doi.org/10.1016/0037-0738(83)90060-X.","productDescription":"15 p.","startPage":"233","endPage":"247","costCenters":[],"links":[{"id":220693,"rank":1,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/thumbnails/outside_thumb.jpg"}],"country":"United States","state":"Washington","otherGeospatial":"Willapa Bay","geographicExtents":"{\n \"type\": \"FeatureCollection\",\n \"features\": [\n {\n \"type\": \"Feature\",\n \"properties\": {},\n \"geometry\": {\n \"coordinates\": [\n [\n [\n -124.0937343147915,\n 46.746899656305146\n ],\n [\n -124.0937343147915,\n 46.648829449792714\n ],\n [\n -123.82927626347455,\n 46.648829449792714\n ],\n [\n -123.82927626347455,\n 46.746899656305146\n ],\n [\n -124.0937343147915,\n 46.746899656305146\n ]\n ]\n ],\n \"type\": \"Polygon\"\n }\n }\n ]\n}","volume":"35","issue":"4","noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"505a3026e4b0c8380cd5d3ea","contributors":{"authors":[{"text":"Luepke, Gretchen","contributorId":91827,"corporation":false,"usgs":true,"family":"Luepke","given":"Gretchen","email":"","affiliations":[],"preferred":false,"id":360568,"contributorType":{"id":1,"text":"Authors"},"rank":1},{"text":"Clifton, H. Edward","contributorId":46503,"corporation":false,"usgs":true,"family":"Clifton","given":"H.","email":"","middleInitial":"Edward","affiliations":[],"preferred":false,"id":360569,"contributorType":{"id":1,"text":"Authors"},"rank":2}]}} ,{"id":70011225,"text":"70011225 - 1983 - Strain accumulation along the San Andreas fault system east of San Francisco Bay, California","interactions":[],"lastModifiedDate":"2025-08-27T16:49:29.58543","indexId":"70011225","displayToPublicDate":"2003-04-08T00:00:00","publicationYear":"1983","noYear":false,"publicationType":{"id":2,"text":"Article"},"publicationSubtype":{"id":10,"text":"Journal Article"},"seriesTitle":{"id":3525,"text":"Tectonophysics","active":true,"publicationSubtype":{"id":10}},"title":"Strain accumulation along the San Andreas fault system east of San Francisco Bay, California","docAbstract":"The occurrence of several large earthquakes to the east of San Francisco Bay during historical times, and present high levels of microseismicity, indicate that a significant part of the relative plate motion may be occurring east of San Francisco Bay. Furthermore, the Hayward fault is known to be slipping aseismically at the surface, and the Calaveras fault may be slipping aseismically also. These facts raise an important question: Is the observed creep rate accommodating all of the east bay deformation or is there a significant amount of strain accumulating along these faults?
Ground-water data were collected in 1982 at White Sands Missile Range in south-central New Mexico. Depth-to-water measurements in the Post Headquarters supply wells continued to show seasonal declines. Test wells east of the Headquarters well field continue to show long-term declines as well as seasonal fluctuations. The total amount of water pumped from White Sands Missile Range supply wells was 66,226,600 gallons more in 1982 than in 1981. The difference in the specific-conductance values of the water samples collected from the Post Headquarters supply wells in the winter and summer increased in 1982.
","language":"English","publisher":"U.S. Geological Survey","doi":"10.3133/ofr83695","usgsCitation":"Cruz, R.R., 1983, Annual water-resources review, White Sands Missile Range, New Mexico, 1982: U.S. Geological Survey Open-File Report 83-695, iv, 20 p., https://doi.org/10.3133/ofr83695.","productDescription":"iv, 20 p.","costCenters":[],"links":[{"id":47944,"rank":300,"type":{"id":11,"text":"Document"},"url":"https://pubs.usgs.gov/of/1983/0695/report.pdf","linkFileType":{"id":1,"text":"pdf"}},{"id":394070,"rank":3,"type":{"id":36,"text":"NGMDB Index Page"},"url":"https://ngmdb.usgs.gov/Prodesc/proddesc_14176.htm"},{"id":150690,"rank":0,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/of/1983/0695/report-thumb.jpg"}],"country":"United States","state":"New Mexico","otherGeospatial":"White Sands Missile Range","geographicExtents":"{\n \"type\": \"FeatureCollection\",\n \"features\": [\n {\n \"type\": \"Feature\",\n \"properties\": {},\n \"geometry\": {\n \"type\": \"Polygon\",\n \"coordinates\": [\n [\n [\n -106.816,\n 32.316\n ],\n [\n -106.041,\n 32.316\n ],\n [\n -106.041,\n 34.325\n ],\n [\n -106.816,\n 34.325\n ],\n [\n -106.816,\n 32.316\n ]\n ]\n ]\n }\n }\n ]\n}","noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"4f4e4ac8e4b07f02db67b77e","contributors":{"authors":[{"text":"Cruz, R. R.","contributorId":97496,"corporation":false,"usgs":true,"family":"Cruz","given":"R.","email":"","middleInitial":"R.","affiliations":[],"preferred":false,"id":179407,"contributorType":{"id":1,"text":"Authors"},"rank":1}]}} ,{"id":10272,"text":"ofr83286 - 1983 - A hydrogeochemical survey in east-central Nevada","interactions":[],"lastModifiedDate":"2022-07-22T21:20:44.950179","indexId":"ofr83286","displayToPublicDate":"1994-01-01T00:00:00","publicationYear":"1983","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":"83-286","title":"A hydrogeochemical survey in east-central Nevada","docAbstract":"A hydrogeochemical survey utilizing waters from springs and wells was conducted in east-central Nevada. None of the trace elements commonly associated with mineralization were found to be highly anomalous in the study area. Slightly anomalous values for some elements were found in the southern valleys of the study area and in a few scattered areas that contained old mines. Data from this study revealed no new areas of significant mineralization.","language":"English","publisher":"U.S. Geological Survey","doi":"10.3133/ofr83286","usgsCitation":"McHugh, J., Miller, W.R., and Ficklin, W.H., 1983, A hydrogeochemical survey in east-central Nevada: U.S. Geological Survey Open-File Report 83-286, i, 28 p., https://doi.org/10.3133/ofr83286.","productDescription":"i, 28 p.","costCenters":[],"links":[{"id":404396,"rank":3,"type":{"id":36,"text":"NGMDB Index Page"},"url":"https://ngmdb.usgs.gov/Prodesc/proddesc_13966.htm","linkFileType":{"id":5,"text":"html"}},{"id":38129,"rank":300,"type":{"id":11,"text":"Document"},"url":"https://pubs.usgs.gov/of/1983/0286/report.pdf","linkFileType":{"id":1,"text":"pdf"}},{"id":142595,"rank":0,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/of/1983/0286/report-thumb.jpg"}],"country":"United States","state":"Nevada","geographicExtents":"{\n \"type\": \"FeatureCollection\",\n \"features\": [\n {\n \"type\": \"Feature\",\n \"properties\": {},\n \"geometry\": {\n \"type\": \"Polygon\",\n \"coordinates\": [\n [\n [\n -114.49,\n 37.874\n ],\n [\n -114,\n 37.874\n ],\n [\n -114,\n 38.5\n ],\n [\n -114.49,\n 38.5\n ],\n [\n -114.49,\n 37.874\n ]\n ]\n ]\n }\n }\n ]\n}","noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"4f4e4b24e4b07f02db6ae468","contributors":{"authors":[{"text":"McHugh, John B.","contributorId":64651,"corporation":false,"usgs":true,"family":"McHugh","given":"John B.","affiliations":[],"preferred":false,"id":161115,"contributorType":{"id":1,"text":"Authors"},"rank":1},{"text":"Miller, W. Roger","contributorId":60191,"corporation":false,"usgs":true,"family":"Miller","given":"W.","email":"","middleInitial":"Roger","affiliations":[],"preferred":false,"id":161114,"contributorType":{"id":1,"text":"Authors"},"rank":2},{"text":"Ficklin, Walter H.","contributorId":52565,"corporation":false,"usgs":true,"family":"Ficklin","given":"Walter","email":"","middleInitial":"H.","affiliations":[],"preferred":false,"id":161113,"contributorType":{"id":1,"text":"Authors"},"rank":3}]}} ,{"id":44178,"text":"ofr83593 - 1983 - Multichannel seismic-reflection profiles collected in 1979 in the eastern Pacific Ocean off the California coast, south of Pt. Conception","interactions":[],"lastModifiedDate":"2021-11-30T19:16:03.016894","indexId":"ofr83593","displayToPublicDate":"1994-01-01T00:00:00","publicationYear":"1983","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":"83-593","title":"Multichannel seismic-reflection profiles collected in 1979 in the eastern Pacific Ocean off the California coast, south of Pt. Conception","docAbstract":"No abstract available.
","language":"English","publisher":"U.S. Geological Survey","doi":"10.3133/ofr83593","usgsCitation":"Mann, D.M., and Crouch, J.K., 1983, Multichannel seismic-reflection profiles collected in 1979 in the eastern Pacific Ocean off the California coast, south of Pt. Conception: U.S. Geological Survey Open-File Report 83-593, Report: 3 p.; 1 Plate: 40.54 × 28.58 inches, https://doi.org/10.3133/ofr83593.","productDescription":"Report: 3 p.; 1 Plate: 40.54 × 28.58 inches","costCenters":[],"links":[{"id":392251,"rank":4,"type":{"id":36,"text":"NGMDB Index Page"},"url":"https://ngmdb.usgs.gov/Prodesc/proddesc_14120.htm"},{"id":81573,"rank":400,"type":{"id":17,"text":"Plate"},"url":"https://pubs.usgs.gov/of/1983/0593/plate-1.pdf","linkFileType":{"id":1,"text":"pdf"}},{"id":81574,"rank":300,"type":{"id":11,"text":"Document"},"url":"https://pubs.usgs.gov/of/1983/0593/report.pdf","linkFileType":{"id":1,"text":"pdf"}},{"id":162892,"rank":0,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/of/1983/0593/report-thumb.jpg"}],"country":"United States","state":"California","otherGeospatial":"Pacific Ocean, Point Conception","geographicExtents":"{\n \"type\": \"FeatureCollection\",\n \"features\": [\n {\n \"type\": \"Feature\",\n \"properties\": {},\n \"geometry\": {\n \"type\": \"Polygon\",\n \"coordinates\": [\n [\n [\n -120.167,\n 31.167\n ],\n [\n -117.833,\n 31.167\n ],\n [\n -117.833,\n 33.667\n ],\n [\n -120.167,\n 33.667\n ],\n [\n -120.167,\n 31.167\n ]\n ]\n ]\n }\n }\n ]\n}","noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"4f4e4b02e4b07f02db698b02","contributors":{"authors":[{"text":"Mann, Dennis M.","contributorId":50528,"corporation":false,"usgs":true,"family":"Mann","given":"Dennis","email":"","middleInitial":"M.","affiliations":[],"preferred":false,"id":229286,"contributorType":{"id":1,"text":"Authors"},"rank":1},{"text":"Crouch, James K.","contributorId":56645,"corporation":false,"usgs":true,"family":"Crouch","given":"James","email":"","middleInitial":"K.","affiliations":[],"preferred":false,"id":229287,"contributorType":{"id":1,"text":"Authors"},"rank":2}]}} ,{"id":20265,"text":"ofr83334 - 1983 - High-resolution seismic-reflection profiles and sidescan-sonar records collected on eastern Long Island Sound and Block Island Sound","interactions":[],"lastModifiedDate":"2019-10-01T14:20:51","indexId":"ofr83334","displayToPublicDate":"1994-01-01T00:00:00","publicationYear":"1983","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":"83-334","title":"High-resolution seismic-reflection profiles and sidescan-sonar records collected on eastern Long Island Sound and Block Island Sound","docAbstract":"No abstract available.
","language":"English","publisher":"U.S. Geological Survey","publisherLocation":"Reston, VA","doi":"10.3133/ofr83334","usgsCitation":"Needell, S.W., and Lewis, R., 1983, High-resolution seismic-reflection profiles and sidescan-sonar records collected on eastern Long Island Sound and Block Island Sound: U.S. Geological Survey Open-File Report 83-334, 4 p. , https://doi.org/10.3133/ofr83334.","productDescription":"4 p. ","costCenters":[],"links":[{"id":152066,"rank":0,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/of/1983/0334/report-thumb.jpg"},{"id":367645,"rank":2,"type":{"id":11,"text":"Document"},"url":"https://pubs.usgs.gov/of/1983/0334/report.pdf","linkFileType":{"id":1,"text":"pdf"}}],"country":"United States","state":"New York","otherGeospatial":"Long Island Sound, Block Island Sound","geographicExtents":"{\n \"type\": \"FeatureCollection\",\n \"features\": [\n {\n \"type\": \"Feature\",\n \"properties\": {},\n \"geometry\": {\n \"type\": \"Polygon\",\n \"coordinates\": [\n [\n [\n -73.970947265625,\n 40.245991504199026\n ],\n [\n -70.8123779296875,\n 40.245991504199026\n ],\n [\n -70.8123779296875,\n 41.430371882652814\n ],\n [\n -73.970947265625,\n 41.430371882652814\n ],\n [\n -73.970947265625,\n 40.245991504199026\n ]\n ]\n ]\n }\n }\n ]\n}","noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"4f4e4a58e4b07f02db62f435","contributors":{"authors":[{"text":"Needell, Sally W.","contributorId":106874,"corporation":false,"usgs":true,"family":"Needell","given":"Sally","email":"","middleInitial":"W.","affiliations":[],"preferred":false,"id":182351,"contributorType":{"id":1,"text":"Authors"},"rank":1},{"text":"Lewis, Ralph S.","contributorId":9288,"corporation":false,"usgs":true,"family":"Lewis","given":"Ralph S.","affiliations":[],"preferred":false,"id":182350,"contributorType":{"id":1,"text":"Authors"},"rank":2}]}} ,{"id":27998,"text":"wri834007 - 1983 - Application of remote-sensing techniques to hydrologic studies in selected coal-mined areas of southeastern Kansas","interactions":[],"lastModifiedDate":"2022-01-10T20:04:36.318938","indexId":"wri834007","displayToPublicDate":"1994-01-01T00:00:00","publicationYear":"1983","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":"83-4007","title":"Application of remote-sensing techniques to hydrologic studies in selected coal-mined areas of southeastern Kansas","docAbstract":"Disturbances resulting from intensive coal mining in the Cherry Creek basin of southeastern Kansas were investigated using color and color-infrared aerial photography in conjunction with water-quality data from simultaneously acquired samples. Imagery was used to identify the type and extent of vegetative cover on strip-mined lands and the extent and success of reclamation practices. Drainage patterns, point sources of acid mine drainage, and recharge areas for underground mines were located for onsite inspection. Comparison of these interpretations with water-quality data illustrated differences between the eastern and western parts of the Cherry Creek basin. Contamination in the eastern part is due largely to circulation of water from unreclaimed strip mines and collapse features through the network of underground mines and subsequent discharge of acidic drainage through seeps. Contamination in the western part is primarily caused by runoff and seepage from strip-mined lands in which surfaces have frequently been graded and limed but are generally devoid of mature stands of soil-anchoring vegetation. The successful use of aerial photography in the study of Cherry Creek basin indicates the potential of using remote-sensing techniques in studies of other coal-mined regions.
","language":"English","publisher":"U.S. Geological Survey","doi":"10.3133/wri834007","usgsCitation":"Kenny, J.F., and McCauley, J.R., 1983, Application of remote-sensing techniques to hydrologic studies in selected coal-mined areas of southeastern Kansas: U.S. Geological Survey Water-Resources Investigations Report 83-4007, Report: iv, 33 p.; 1 Plate: 16.01 × 18.60 inches, https://doi.org/10.3133/wri834007.","productDescription":"Report: iv, 33 p.; 1 Plate: 16.01 × 18.60 inches","costCenters":[],"links":[{"id":56824,"rank":400,"type":{"id":17,"text":"Plate"},"url":"https://pubs.usgs.gov/wri/1983/4007/plate-1.pdf","linkFileType":{"id":1,"text":"pdf"}},{"id":394124,"rank":4,"type":{"id":36,"text":"NGMDB Index Page"},"url":"https://ngmdb.usgs.gov/Prodesc/proddesc_35653.htm"},{"id":56825,"rank":300,"type":{"id":11,"text":"Document"},"url":"https://pubs.usgs.gov/wri/1983/4007/report.pdf","linkFileType":{"id":1,"text":"pdf"}},{"id":123358,"rank":0,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/wri/1983/4007/report-thumb.jpg"}],"country":"United States","state":"Kansas","geographicExtents":"{\n \"type\": \"FeatureCollection\",\n \"features\": [\n {\n \"type\": \"Feature\",\n \"properties\": {},\n \"geometry\": {\n \"type\": \"Polygon\",\n \"coordinates\": [\n [\n [\n -94.9720,\n 37.158\n ],\n [\n -94.5730,\n 37.158\n ],\n [\n -94.5730,\n 37.333\n ],\n [\n -94.9720,\n 37.333\n ],\n [\n -94.9720,\n 37.158\n ]\n ]\n ]\n }\n }\n ]\n}","noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"4f4e4ac6e4b07f02db67a8ad","contributors":{"authors":[{"text":"Kenny, J. F.","contributorId":100378,"corporation":false,"usgs":true,"family":"Kenny","given":"J.","email":"","middleInitial":"F.","affiliations":[],"preferred":false,"id":199040,"contributorType":{"id":1,"text":"Authors"},"rank":1},{"text":"McCauley, J. R.","contributorId":97533,"corporation":false,"usgs":true,"family":"McCauley","given":"J.","email":"","middleInitial":"R.","affiliations":[],"preferred":false,"id":199039,"contributorType":{"id":1,"text":"Authors"},"rank":2}]}} ,{"id":29224,"text":"wri824065 - 1983 - Numerical simulation of ground-water flow in lower Satus Creek Basin, Yakima Indian Reservation, Washington","interactions":[],"lastModifiedDate":"2012-02-02T00:08:48","indexId":"wri824065","displayToPublicDate":"1994-01-01T00:00:00","publicationYear":"1983","noYear":false,"publicationType":{"id":18,"text":"Report"},"publicationSubtype":{"id":5,"text":"USGS Numbered Series"},"seriesTitle":{"id":342,"text":"Water-Resources Investigations Report","code":"WRI","active":false,"publicationSubtype":{"id":5}},"seriesNumber":"82-4065","title":"Numerical simulation of ground-water flow in lower Satus Creek Basin, Yakima Indian Reservation, Washington","docAbstract":"A multilayer numerical model of steady-state ground-water flow in lower Satus Creek basin was constructed, calibrated using time-averaged data, and used to estimate the long-term effects of proposed irrigation-water management plans on ground-water levels in the area. Model computations showed that irrigation of new lands in the Satus uplands would raise ground-water levels in lower Satus Creek basin and thereby increase the size of the waterlogged areas. The model also demonstrated that pumping water from wells, reducing the amount of irrigation water used in the lowlands, and stopping leakage from Satus No. 2 and 3 Pump Canals were all effective methods to alleviate present waterlogging in some parts of the basin and to counteract some of the anticipated ground-water-level rises that would be caused by irrigating the uplands. The proposed changes in water use affected model-computed ground-water levels most in the eastern part of the basin between Satus No. 2 and No. 3 Pump Canals. The effects on ground-water levels in the western part of the basin between Satus Creek and Satus No. 2 Pump Canal were smaller. (USGS)","language":"ENGLISH","publisher":"U.S. Geological Survey,","doi":"10.3133/wri824065","usgsCitation":"Prych, E., 1983, Numerical simulation of ground-water flow in lower Satus Creek Basin, Yakima Indian Reservation, Washington: U.S. Geological Survey Water-Resources Investigations Report 82-4065, xi, 89 p. :ill., maps ;28 cm., https://doi.org/10.3133/wri824065.","productDescription":"xi, 89 p. :ill., maps ;28 cm.","costCenters":[],"links":[{"id":126894,"rank":0,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/wri/1982/4065/report-thumb.jpg"},{"id":58077,"rank":400,"type":{"id":17,"text":"Plate"},"url":"https://pubs.usgs.gov/wri/1982/4065/plate-1.pdf","linkFileType":{"id":1,"text":"pdf"}},{"id":58078,"rank":300,"type":{"id":11,"text":"Document"},"url":"https://pubs.usgs.gov/wri/1982/4065/report.pdf","linkFileType":{"id":1,"text":"pdf"}}],"noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"4f4e4afce4b07f02db69680c","contributors":{"authors":[{"text":"Prych, E. A.","contributorId":36163,"corporation":false,"usgs":true,"family":"Prych","given":"E. A.","affiliations":[],"preferred":false,"id":201175,"contributorType":{"id":1,"text":"Authors"},"rank":1}]}} ,{"id":25978,"text":"wri824084 - 1983 - Geohydrology of the Meadowbrook artificial-recharge site at East Meadow, Nassau County, New York","interactions":[],"lastModifiedDate":"2023-01-04T20:51:39.419276","indexId":"wri824084","displayToPublicDate":"1994-01-01T00:00:00","publicationYear":"1983","noYear":false,"publicationType":{"id":18,"text":"Report"},"publicationSubtype":{"id":5,"text":"USGS Numbered Series"},"seriesTitle":{"id":342,"text":"Water-Resources Investigations Report","code":"WRI","active":false,"publicationSubtype":{"id":5}},"seriesNumber":"82-4084","title":"Geohydrology of the Meadowbrook artificial-recharge site at East Meadow, Nassau County, New York","docAbstract":"No abstract available.
","language":"English","publisher":"U.S. Geological Survey","doi":"10.3133/wri824084","usgsCitation":"Aronson, D.A., Lindner-Lunsford, J.B., and Katz, B., 1983, Geohydrology of the Meadowbrook artificial-recharge site at East Meadow, Nassau County, New York: U.S. Geological Survey Water-Resources Investigations Report 82-4084, vi, 44 p., https://doi.org/10.3133/wri824084.","productDescription":"vi, 44 p.","costCenters":[],"links":[{"id":54732,"rank":2,"type":{"id":11,"text":"Document"},"url":"https://pubs.usgs.gov/wri/1982/4084/report.pdf","linkFileType":{"id":1,"text":"pdf"}},{"id":121856,"rank":1,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/wri/1982/4084/report-thumb.jpg"},{"id":411381,"rank":3,"type":{"id":36,"text":"NGMDB Index Page"},"url":"https://ngmdb.usgs.gov/Prodesc/proddesc_35595.htm","linkFileType":{"id":5,"text":"html"}}],"country":"United States","state":"New York","county":"Nassau County","otherGeospatial":"East Meadow","geographicExtents":"{\n \"type\": \"FeatureCollection\",\n \"features\": [\n {\n \"type\": \"Feature\",\n \"properties\": {},\n \"geometry\": {\n \"coordinates\": [\n [\n [\n -73.56278176511351,\n 40.79270194265632\n ],\n [\n -73.56278176511351,\n 40.68814281175551\n ],\n [\n -73.45373266539764,\n 40.68814281175551\n ],\n [\n -73.45373266539764,\n 40.79270194265632\n ],\n [\n -73.56278176511351,\n 40.79270194265632\n ]\n ]\n ],\n \"type\": \"Polygon\"\n }\n }\n ]\n}","noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"4f4e4b1be4b07f02db6a8926","contributors":{"authors":[{"text":"Aronson, D. A.","contributorId":20308,"corporation":false,"usgs":true,"family":"Aronson","given":"D.","email":"","middleInitial":"A.","affiliations":[],"preferred":false,"id":195576,"contributorType":{"id":1,"text":"Authors"},"rank":1},{"text":"Lindner-Lunsford, J. B.","contributorId":81938,"corporation":false,"usgs":true,"family":"Lindner-Lunsford","given":"J.","email":"","middleInitial":"B.","affiliations":[],"preferred":false,"id":195577,"contributorType":{"id":1,"text":"Authors"},"rank":2},{"text":"Katz, B. G.","contributorId":82702,"corporation":false,"usgs":true,"family":"Katz","given":"B. G.","affiliations":[],"preferred":false,"id":195578,"contributorType":{"id":1,"text":"Authors"},"rank":3}]}} ,{"id":7237,"text":"ofr82679 - 1983 - Hydrology of area 21, Eastern Coal province, Tennessee, Alabama and Georgia","interactions":[],"lastModifiedDate":"2024-09-24T18:08:13.417331","indexId":"ofr82679","displayToPublicDate":"1994-01-01T00:00:00","publicationYear":"1983","noYear":false,"publicationType":{"id":18,"text":"Report"},"publicationSubtype":{"id":5,"text":"USGS Numbered Series"},"seriesTitle":{"id":330,"text":"Open-File Report","code":"OFR","onlineIssn":"2331-1258","printIssn":"0196-1497","active":true,"publicationSubtype":{"id":5}},"seriesNumber":"82-679","title":"Hydrology of area 21, Eastern Coal province, Tennessee, Alabama and Georgia","docAbstract":"No abstract available.
","language":"English","publisher":"U.S. Geological Survey","doi":"10.3133/ofr82679","usgsCitation":"May, V., 1983, Hydrology of area 21, Eastern Coal province, Tennessee, Alabama and Georgia: U.S. Geological Survey Open-File Report 82-679, vi, 92 p., https://doi.org/10.3133/ofr82679.","productDescription":"vi, 92 p.","costCenters":[{"id":13634,"text":"South Atlantic Water Science Center","active":true,"usgs":true}],"links":[{"id":94755,"rank":2,"type":{"id":11,"text":"Document"},"url":"https://pubs.usgs.gov/of/1982/0679/report.pdf","linkFileType":{"id":1,"text":"pdf"}},{"id":462210,"rank":3,"type":{"id":36,"text":"NGMDB Index Page"},"url":"https://ngmdb.usgs.gov/Prodesc/proddesc_13802.htm","linkFileType":{"id":5,"text":"html"}},{"id":139837,"rank":1,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/of/1982/0679/report-thumb.jpg"}],"country":"United States","state":"Alabama, Georgia, Tennessee","otherGeospatial":"Eastern Coal Province","geographicExtents":"{\n \"type\": \"FeatureCollection\",\n \"features\": [\n {\n \"type\": \"Feature\",\n \"properties\": {},\n \"geometry\": {\n \"type\": \"Polygon\",\n \"coordinates\": [\n [\n [\n -86.15478515625,\n 34.38877925439021\n ],\n [\n -86.15478515625,\n 35.8356283888737\n ],\n [\n -84.869384765625,\n 35.8356283888737\n ],\n [\n -84.869384765625,\n 34.38877925439021\n ],\n [\n -86.15478515625,\n 34.38877925439021\n ]\n ]\n ]\n }\n }\n ]\n}","noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"4f4e4a17e4b07f02db604430","contributors":{"authors":[{"text":"May, V.J.","contributorId":71539,"corporation":false,"usgs":true,"family":"May","given":"V.J.","email":"","affiliations":[],"preferred":false,"id":154863,"contributorType":{"id":1,"text":"Authors"},"rank":1}]}} ,{"id":10642,"text":"ofr8335 - 1983 - Hydrologic data for urban studies in the San Antonio, Texas, metropolitan area, 1981","interactions":[],"lastModifiedDate":"2017-03-29T14:22:44","indexId":"ofr8335","displayToPublicDate":"1994-01-01T00:00:00","publicationYear":"1983","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":"83-35","title":"Hydrologic data for urban studies in the San Antonio, Texas, metropolitan area, 1981","docAbstract":"Hydrologic investigations of urban drainage basins in Texas were begun by the U.S. Geological Survey in 1954. These studies are now in progress in Austin and Houston. Studies were completed in the Fort Worth metropolitan area at the end of the 1977 water year, and in the Dallas metropolitan area at the end of the 1979 water year. The study in the San Antonio area was completed at the end of the 1981 water year.
The Geological Survey, in cooperation with the Texas Department of Water Resources, expanded the existing streamflow network in the San Antonio metropolitan area in May 1968 to begin urban hydrology studies in this area. In September 1968, the program was further expanded to include the collection of water-quality data. The Texas Department of Water Resources ended its participation in the project in 1979, and the city of San Antonio funded the program through the 1981 water year.
The operation and maintenance of stations 08178000, San Antonio River at San Antonio; 08178700, Salado Creek (upper station) at San Antonio; and 08178800, Salado Creek (lower station) at San Antonio are funded by the city of San Antonio and the U.S Geological Survey.
The operation and maintenance and collection of water-quality data at station 08178720, Lorence Creek at Thousand Oaks Blvd., San Antonio, station 08178640, West Elm Creek at San Antonio, and station 08178645, East Elm Creek at San Antonio, are funded by the Edwards Underground Water District in cooperation with the Texas Department of Hater Resources and the U.S. Geological Survey. Station 08178640, West Elm Creek at San Antonio, and station 08178645, East Elm Creek at San Antonio will provide hydrologic data on similar and adjacent watersheds. The West Elm watershed is still predominately rural but is undergoing extensive urbanization in some areas. The East Elm watershed is relatively stable and undeveloped.
The objectives of the San Antonio urban hydrology study are:
Annual publication of the San Antonio urban studies was initiated in 1969.
A definition of terms related to streamflow, water quality, and other hydrologic data, as used in this report, are defined in the U.S. Geological Survey's 1979 and 1980 \"Water resources data for Texas\" reports.
","language":"English","publisher":"U.S. Geological Survey","doi":"10.3133/ofr8335","collaboration":"Prepared in cooperation with the Texas Department of Water Resources","usgsCitation":"Perez, R., 1983, Hydrologic data for urban studies in the San Antonio, Texas, metropolitan area, 1981: U.S. Geological Survey Open-File Report 83-35, v, 58 p., https://doi.org/10.3133/ofr8335.","productDescription":"v, 58 p.","onlineOnly":"N","additionalOnlineFiles":"N","costCenters":[{"id":583,"text":"Texas Water Science Center","active":true,"usgs":true}],"links":[{"id":38476,"rank":300,"type":{"id":11,"text":"Document"},"url":"https://pubs.usgs.gov/of/1983/0035/report.pdf","text":"Report","size":"1.18 MB","linkFileType":{"id":1,"text":"pdf"},"description":"Report"},{"id":144085,"rank":0,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/of/1983/0035/report-thumb.jpg"}],"country":"United States","state":"Texas","city":"San Antonio","geographicExtents":"{\n \"type\": \"FeatureCollection\",\n \"features\": [\n {\n \"type\": \"Feature\",\n \"properties\": {},\n \"geometry\": {\n \"type\": \"Polygon\",\n \"coordinates\": [\n [\n [\n -98.8165283203125,\n 29.123373210819224\n ],\n [\n -98.19580078125,\n 29.123373210819224\n ],\n [\n -98.19580078125,\n 29.699982298744377\n ],\n [\n -98.8165283203125,\n 29.699982298744377\n ],\n [\n -98.8165283203125,\n 29.123373210819224\n ]\n ]\n ]\n }\n }\n ]\n}","noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"4f4e4a1be4b07f02db6078df","contributors":{"authors":[{"text":"Perez, Roberto","contributorId":97114,"corporation":false,"usgs":true,"family":"Perez","given":"Roberto","email":"","affiliations":[],"preferred":false,"id":161728,"contributorType":{"id":1,"text":"Authors"},"rank":1}]}} ,{"id":5797,"text":"pp1253 - 1983 - Stratigraphy and paleontology of Mid-Cretaceous rocks in Minnesota and contiguous areas","interactions":[],"lastModifiedDate":"2024-11-18T19:11:49.604403","indexId":"pp1253","displayToPublicDate":"1994-01-01T00:00:00","publicationYear":"1983","noYear":false,"publicationType":{"id":18,"text":"Report"},"publicationSubtype":{"id":5,"text":"USGS Numbered Series"},"seriesTitle":{"id":331,"text":"Professional Paper","code":"PP","onlineIssn":"2330-7102","printIssn":"1044-9612","active":true,"publicationSubtype":{"id":5}},"seriesNumber":"1253","title":"Stratigraphy and paleontology of Mid-Cretaceous rocks in Minnesota and contiguous areas","docAbstract":"PART A: Molluscan fossils are locally abundant at outcrops of Upper Cretaceous rocks in eastern North and South Dakota, northeastern Nebraska, northwestern Iowa, and western and northern Minnesota. Other Cretaceous mollusks have been found in the glacial deposits in Minnesota, Iowa, and Illinois. \r\n\r\nThe oldest well dated marine mollusks are of earliest late Cenomanian age and occur in northwestern Iowa. Mollusks of marginal marine \r\nand nonmarine environments in northwestern Iowa and south-central Minnesota are probably of slightly younger late Cenomanian age. The youngest mollusks treated in this report are bivalves of Santonian age found in the Niobrara Formation in eastern North and South Dakota. \r\n\r\nThe collections indicate the presence or former presence of the following ammonite zones in the northeastern part of the Western Interior seaway: \r\n\r\nSantonian: Scaphites depressus-Clioscaphites choteauensis \r\n\r\nConiacian: Scaphites uentrocosus; Scaphites preuentricosus \r\n\r\nTuronian: Scaphites coruensis; Scaphites whitfieldi; Prionocyclus hyatti; Subprionocyclus percarinatus; Collignoniceras woollgari; Watinoceras coloradoense \r\n\r\nCenomanian: Dunueganoceras albertense; Dunueganoceras pondi\r\n\r\nPART B: Sedimentary rocks of early Late Cretaceous age occur in the eastern parts of North Dakota, South Dakota, and Nebraska, and in Minnesota and western Iowa. They are generally included in, from oldest to youngest, the Dakota Formation, Graneros Shale, Greenhorn Formation, Carlile Shale, and Niobrara Formation. However, in eastern North Dakota, they are also assigned to, in ascending order, the Belle Fourche Shale, Greenhorn Formation, Carlile Shale, and Niobrara Formation. The Graneros Shale and laterally equivalent strata in the Belle Fourche Shale grade eastward into the Coleraine Formation of northeastern Minnesota and probably into the Windrow Formation of southeastern Minnesota. Cretaceous beds locally overlie rocks of Precambrian, Paleozoic, and Jurassic ages, and they are generally overlain by glacial drift and alluvium of Quaternary age. In Minnesota and adjoining areas, formations of mid-Cretaceous age commonly overlap the dissected surface of Precambrian rocks. The thickness of the lower Upper Cretaceous sequence ranges from about 223 m in eastern North Dakota and about 200 m in northeastern Nebraska to a featheredge in Minnesota and Iowa. \r\n\r\nThese lower Upper Cretaceous formations are composed mainly of shale, siltstone, sandstone, and limestone units of marine and nonmarine origin and were deposited near the eastern shore of a transgressing and regressing epicontinental sea in Cenomanian Turonian Coniacian. and Santonian time. During the late Cenoanian, the strandline was in Minnesota and was oriented generally northnortheast. Interpretations of the depositional environments of the strata and of fossils from outcrops and from clasts in glacial drift indicate that the Cretaceous seaway extended from this region northeastward across Canada to Greenland in the Turonian Coniacian, and Santonian. \r\n\r\nThe Cretaceous formations are deformed into broad, shallow synclines in eastern North and South Dakota and in northeastern Nebraska. A west-trending anticline, the Sioux uplift, separates the synclines in southeastern South Dakota. Sparse evidence of minor faulting in the formations exists in northeastern South Dakota, along the strike of a major southwest-trending zone of tectonism in the Precambrian basement rocks. The structural relief in the region, on the top of the Greenhorn Formation, is at least 250 m between eastern North Dakota and northeastern Minnesota, and at least 200 m between northeastern Nebraska and northwestern Iowa. \r\n\r\nA comparison of the Cretaceous stratigraphy of the Minnesota region and of areas in Wyoming indicates that some marine transgressions and regressions were synchronous in the two regions. The transgression during Greenhorn time, the regression during early Carlile time, and the transgression dur","language":"English","publisher":"U.S. Geological Survey","doi":"10.3133/pp1253","usgsCitation":"Cobban, W.A., and Merewether, E., 1983, Stratigraphy and paleontology of Mid-Cretaceous rocks in Minnesota and contiguous areas: U.S. Geological Survey Professional Paper 1253, iv, 52 p., https://doi.org/10.3133/pp1253.","productDescription":"iv, 52 p.","costCenters":[],"links":[{"id":402556,"rank":3,"type":{"id":36,"text":"NGMDB Index Page"},"url":"https://ngmdb.usgs.gov/Prodesc/proddesc_74506.htm","text":"Molluscan fossil record from the northeastern part of the Upper Cretaceous seaway, Western Interior","linkFileType":{"id":5,"text":"html"}},{"id":117719,"rank":1,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/pp/1253/report-thumb.jpg"},{"id":32482,"rank":2,"type":{"id":11,"text":"Document"},"url":"https://pubs.usgs.gov/pp/1253/report.pdf","linkFileType":{"id":1,"text":"pdf"}},{"id":464249,"rank":4,"type":{"id":36,"text":"NGMDB Index Page"},"url":"https://ngmdb.usgs.gov/Prodesc/proddesc_74507.htm","text":"Lower Upper Cretaceous strata in Minnesota and adjacent areas -- time-stratigraphic correlations and structural attitudes","linkFileType":{"id":5,"text":"html"}}],"country":"United States","state":"Iowa, Minnesota, Nebraska, North Dakota, South Dakota","geographicExtents":"{\n \"type\": \"FeatureCollection\",\n \"features\": [\n {\n \"type\": \"Feature\",\n \"properties\": {},\n \"geometry\": {\n \"type\": \"Polygon\",\n \"coordinates\": [\n [\n [\n -98.0859375,\n 41.902277040963696\n ],\n [\n -94.921875,\n 42.09822241118974\n ],\n [\n -90.703125,\n 43.51668853502906\n ],\n [\n -92.63671875,\n 45.213003555993964\n ],\n [\n -91.845703125,\n 46.86019101567027\n ],\n [\n -89.56054687499999,\n 48.10743118848039\n ],\n [\n -93.779296875,\n 48.69096039092549\n ],\n [\n -94.921875,\n 48.922499263758255\n ],\n [\n -94.74609375,\n 49.32512199104001\n ],\n [\n -95.44921875,\n 49.15296965617042\n ],\n [\n -99.140625,\n 48.980216985374994\n ],\n [\n -98.0859375,\n 41.902277040963696\n ]\n ]\n ]\n }\n }\n ]\n}","noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"4f4e4b1be4b07f02db6a8a6e","contributors":{"authors":[{"text":"Cobban, William Aubrey","contributorId":78317,"corporation":false,"usgs":true,"family":"Cobban","given":"William","email":"","middleInitial":"Aubrey","affiliations":[],"preferred":false,"id":151598,"contributorType":{"id":1,"text":"Authors"},"rank":1},{"text":"Merewether, E.A.","contributorId":32517,"corporation":false,"usgs":true,"family":"Merewether","given":"E.A.","affiliations":[],"preferred":false,"id":151597,"contributorType":{"id":1,"text":"Authors"},"rank":2}]}} ,{"id":10766,"text":"ofr82638 - 1983 - Hydrology of area 34, eastern region, interior coal province, Kentucky, Indiana and Illinois","interactions":[],"lastModifiedDate":"2022-07-13T00:18:36.408378","indexId":"ofr82638","displayToPublicDate":"1994-01-01T00:00:00","publicationYear":"1983","noYear":false,"publicationType":{"id":18,"text":"Report"},"publicationSubtype":{"id":5,"text":"USGS Numbered Series"},"seriesTitle":{"id":330,"text":"Open-File Report","code":"OFR","onlineIssn":"2331-1258","printIssn":"0196-1497","active":true,"publicationSubtype":{"id":5}},"seriesNumber":"82-638","title":"Hydrology of area 34, eastern region, interior coal province, Kentucky, Indiana and Illinois","docAbstract":"No abstract available.
","language":"English","publisher":"U.S. Geological Survey","doi":"10.3133/ofr82638","usgsCitation":"Quinones, F., York, K.L., and Plebuch, R., 1983, Hydrology of area 34, eastern region, interior coal province, Kentucky, Indiana and Illinois: U.S. Geological Survey Open-File Report 82-638, v, 83 p., https://doi.org/10.3133/ofr82638.","productDescription":"v, 83 p.","costCenters":[],"links":[{"id":94993,"rank":300,"type":{"id":11,"text":"Document"},"url":"https://pubs.usgs.gov/of/1982/0638/report.pdf","linkFileType":{"id":1,"text":"pdf"}},{"id":143407,"rank":0,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/of/1982/0638/report-thumb.jpg"},{"id":403556,"rank":3,"type":{"id":36,"text":"NGMDB Index Page"},"url":"https://ngmdb.usgs.gov/Prodesc/proddesc_13783.htm","linkFileType":{"id":5,"text":"html"}}],"country":"United States","state":"Illinois, Indiana, Kentucky","otherGeospatial":"area 34, Eastern Region, Interior Coal Province","geographicExtents":"{\n \"type\": \"FeatureCollection\",\n \"features\": [\n {\n \"type\": \"Feature\",\n \"properties\": {},\n \"geometry\": {\n \"type\": \"Polygon\",\n \"coordinates\": [\n [\n [\n -88.217,\n 36.818\n ],\n [\n -85.6,\n 36.818\n ],\n [\n -85.6,\n 38.018\n ],\n [\n -88.217,\n 38.018\n ],\n [\n -88.217,\n 36.818\n ]\n ]\n ]\n }\n }\n ]\n}","noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"4f4e4a13e4b07f02db60206e","contributors":{"authors":[{"text":"Quinones, F.","contributorId":93037,"corporation":false,"usgs":true,"family":"Quinones","given":"F.","email":"","affiliations":[],"preferred":false,"id":161928,"contributorType":{"id":1,"text":"Authors"},"rank":1},{"text":"York, K. L.","contributorId":72384,"corporation":false,"usgs":true,"family":"York","given":"K.","email":"","middleInitial":"L.","affiliations":[],"preferred":false,"id":161927,"contributorType":{"id":1,"text":"Authors"},"rank":2},{"text":"Plebuch, R. O.","contributorId":29429,"corporation":false,"usgs":true,"family":"Plebuch","given":"R. O.","affiliations":[],"preferred":false,"id":161926,"contributorType":{"id":1,"text":"Authors"},"rank":3}]}} ,{"id":24977,"text":"pp1245 - 1983 - Historical surface deformation near Oildale, California","interactions":[],"lastModifiedDate":"2017-04-25T14:33:04","indexId":"pp1245","displayToPublicDate":"1994-01-01T00:00:00","publicationYear":"1983","noYear":false,"publicationType":{"id":18,"text":"Report"},"publicationSubtype":{"id":5,"text":"USGS Numbered Series"},"seriesTitle":{"id":331,"text":"Professional Paper","code":"PP","onlineIssn":"2330-7102","printIssn":"1044-9612","active":true,"publicationSubtype":{"id":5}},"seriesNumber":"1245","title":"Historical surface deformation near Oildale, California","docAbstract":"Historical surface deformation recognized in the southern San Joaquin Valley and adjacent Sierra Nevada foothills near Oildale, Calif., includes: normal and apparently aseismic dip slip along four faults; subsidence within or adjacent to the Kern Front, Poso Creek, Mount Poso, and Fruitvale oil fields; and uplift of much of the area within and north of the Kern River oil field. As much as 0.34 m of vertical separation has been observed along a 5.2-km segment of the Kern Front fault, the structural barrier separating the Kern Front oil field on the west from the Kern River field to the east. Similar separations of as much as 0.15 m and 0.32 m, respectively, have also been identified along the surface traces of two en echelon faults between the Premier and Enas areas of the Poso Creek oil field and the fault that defines the southeast flank of the Premier area. The measured height changes are based on both unadjusted observed elevations and minimally constrained adjusted elevations developed from repeated control levelings referred to a relatively stable local bench mark; measurement error in the reported vertical movements probably is less than 0.05 m. Differential subsidence of at least 0.31 m (1903-68) and 0.05 m (1926/27/30/31-59) has occurred within the Kern Front and Fruitvale oil fields, respectively; subsidence of as much as 0.33 m (1903-53) and 0.19 m (1931-63) has also been measured along the north edge of the Premier area of the Poso Creek oil field and the south edge of the Main area of the Mount Poso field, respectively. Differential uplift of as much as 0.11 m and 0.13 m occurred within and immediately north of the Kern River oil field between 1903 and 1968, and similar uplift of as much as 0.19 m was measured along the north edge of the Dominion area of the Mount Poso field between 1931 and 1963.
Differential subsidence within the Kern Front and Fruitvale oil fields and along the edges of the Poso Creek and Mount Poso fields is attributable to subsurface compaction owing to fluid withdrawal; absence of subsidence within the much larger Kern River field probably is the result of either production from compaction-resistant materials or natural water flooding that has acted to preserve reservoir fluid pressures in the generally shallow producing beds. Contemporary displacements on the Kern Front fault and those along the faults within and adjacent to the Poso Creek oil field are attributable largely or entirely to changes in the subsurface stress regime associated with reservoir compaction; accumulated elastic strain of tectonic derivation conceivably contributed to the development of these displacements. The apparent uplift within and north of the Kern River oil field and along the north edge of the Mount Poso field probably is due in part to compaction of as much as 0.055 m beneath the reference bench mark; most of this apparent uplift, however, is interpreted as an effect of tectonic tilting.
","language":"English","publisher":"U.S. Government Publishing Office","doi":"10.3133/pp1245","usgsCitation":"Castle, R.O., Church, J.P., Yerkes, R.F., and Manning, J.C., 1983, Historical surface deformation near Oildale, California: U.S. Geological Survey Professional Paper 1245, Report: iv, 42 p.; 2 Plates: 25.12 x 36.22 inches and 29.04 x 39.66 inches, https://doi.org/10.3133/pp1245.","productDescription":"Report: iv, 42 p.; 2 Plates: 25.12 x 36.22 inches and 29.04 x 39.66 inches","costCenters":[],"links":[{"id":104580,"rank":700,"type":{"id":15,"text":"Index Page"},"url":"https://ngmdb.usgs.gov/Prodesc/proddesc_4766.htm","linkFileType":{"id":5,"text":"html"},"description":"4766"},{"id":126340,"rank":0,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/pp/1245/report-thumb.jpg"},{"id":53963,"rank":300,"type":{"id":11,"text":"Document"},"url":"https://pubs.usgs.gov/pp/1245/report.pdf","text":"Report","size":"4.09 MB","linkFileType":{"id":1,"text":"pdf"},"description":"Report"},{"id":340319,"rank":4,"type":{"id":17,"text":"Plate"},"url":"https://pubs.usgs.gov/pp/1245/plate-1.pdf","linkFileType":{"id":1,"text":"pdf"}},{"id":340320,"rank":5,"type":{"id":17,"text":"Plate"},"url":"https://pubs.usgs.gov/pp/1245/plate-2.pdf","linkFileType":{"id":1,"text":"pdf"}}],"country":"United States","state":"California","geographicExtents":"{\n \"type\": \"FeatureCollection\",\n \"features\": [\n {\n \"type\": \"Feature\",\n \"properties\": {},\n \"geometry\": {\n \"type\": \"Polygon\",\n \"coordinates\": [\n [\n [\n -119.2,\n 35.3\n ],\n [\n -118.8,\n 35.3\n ],\n [\n -118.8,\n 35.7\n ],\n [\n -119.2,\n 35.7\n ],\n [\n -119.2,\n 35.3\n ]\n ]\n ]\n }\n }\n ]\n}","noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"4f4e4a54e4b07f02db62c2a7","contributors":{"authors":[{"text":"Castle, Robert O.","contributorId":22741,"corporation":false,"usgs":true,"family":"Castle","given":"Robert","email":"","middleInitial":"O.","affiliations":[],"preferred":false,"id":192930,"contributorType":{"id":1,"text":"Authors"},"rank":1},{"text":"Church, Jack P.","contributorId":6480,"corporation":false,"usgs":true,"family":"Church","given":"Jack","email":"","middleInitial":"P.","affiliations":[],"preferred":false,"id":192928,"contributorType":{"id":1,"text":"Authors"},"rank":2},{"text":"Yerkes, Robert F.","contributorId":64239,"corporation":false,"usgs":true,"family":"Yerkes","given":"Robert","email":"","middleInitial":"F.","affiliations":[],"preferred":false,"id":192931,"contributorType":{"id":1,"text":"Authors"},"rank":3},{"text":"Manning, John C.","contributorId":10460,"corporation":false,"usgs":true,"family":"Manning","given":"John","email":"","middleInitial":"C.","affiliations":[],"preferred":false,"id":192929,"contributorType":{"id":1,"text":"Authors"},"rank":4}]}} ,{"id":8802,"text":"ofr83686 - 1983 - Ground-water quality data for Oklahoma, 1981","interactions":[],"lastModifiedDate":"2012-02-02T00:06:18","indexId":"ofr83686","displayToPublicDate":"1994-01-01T00:00:00","publicationYear":"1983","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":"83-686","title":"Ground-water quality data for Oklahoma, 1981","docAbstract":"The U.S. Geological Survey has collected data on Oklahoma's ground-water resources since 1934. Most of these data were collected as part of specific ground-water studies conducted in cooperation with various Federal, State, and local agencies. Ground-water quality data, as well as data on construction, yield, water levels, and other physical well parameters collected prior to 1981 are available from the U.S. Geological Survey, Oklahoma District Office.\r\nAlthough water-quality data for wells, test holes, and springs have been published, they are scattered though a variety of reports and are not readily available on a statewide basis. The purpose of this report is to make available, annually, all of the ground-water quality data collected by the U.S. Geological Survey in the Sate of Oklahoma. This report contains ground-water quality data collected in 1981 from 524 sites in 15 counties, predominately in eastern Oklahoma.","language":"ENGLISH","publisher":"U.S. Geological Survey,","doi":"10.3133/ofr83686","usgsCitation":"Ferree, D.M., 1983, Ground-water quality data for Oklahoma, 1981: U.S. Geological Survey Open-File Report 83-686, iv, 81 p. ill. ;28 cm., https://doi.org/10.3133/ofr83686.","productDescription":"iv, 81 p. ill. ;28 cm.","costCenters":[],"links":[{"id":142928,"rank":0,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/of/1983/0686/report-thumb.jpg"},{"id":36384,"rank":300,"type":{"id":11,"text":"Document"},"url":"https://pubs.usgs.gov/of/1983/0686/report.pdf","linkFileType":{"id":1,"text":"pdf"}}],"noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"4f4e4aa8e4b07f02db66732f","contributors":{"authors":[{"text":"Ferree, Dale M.","contributorId":96690,"corporation":false,"usgs":true,"family":"Ferree","given":"Dale","email":"","middleInitial":"M.","affiliations":[],"preferred":false,"id":158355,"contributorType":{"id":1,"text":"Authors"},"rank":1}]}} ,{"id":17758,"text":"ofr83694 - 1983 - Surface water and climatologic data, Salt Lake County, Utah, water year 1981, with selected data for water years 1980 and 1982","interactions":[],"lastModifiedDate":"2017-09-01T14:33:23","indexId":"ofr83694","displayToPublicDate":"1994-01-01T00:00:00","publicationYear":"1983","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":"83-694","title":"Surface water and climatologic data, Salt Lake County, Utah, water year 1981, with selected data for water years 1980 and 1982","docAbstract":"This report contains precipitation, atmospheric-deposition, water- discharge and water-quality data collected in Salt Lake County as part of two investigations by the U.S. Geological Survey. The purpose of this report is to release data collected mainly during the 1981 water year. Selected data collected during the 1980 water year not previously published or revised and the 1982 water year also are included in this report.
The first investigation, which was carried out from September 1979 to August 1982, was an urban-runoff study done in cooperation with the Salt Lake County Division of Flood Control and Water Quality. The objectives of the urban-runoff study were to identify the impact of urban runoff on the quantity and quality of the water in the canals east of the Jordan River and on the major tributaries to the river.
The second investigation, which was carried out from December 1979 to September 1983, is a study of water-quality problems in the Jordan River. The study was done primarily to provide information about toxic substances, dissolved-oxygen depletion, sanitary quality, and turbidity and suspended sediment in the Jordan River. It also was funded in part by the Salt Lake County Division of Flood Control and Water Quality.
Several Salt Lake County employees assisted in the collection of water- quality samples from storm runoff. Of those employees, Lee R. Armstrong, Gilbert H. Heal, Steven J. Mitckes, and Ben Santistevan worked on a daily basis with the authors and made a significant contribution in the collection of the data contained in this report. Organizations that furnished data are acknowledged in the station descriptions in tables 1 and 4.
Information for previously published water-discharge, water-quality, atmospheric-deposition, and precipitation data for Salt Lake County are reported by Pyper and others (1981); Dustin (1977); Hely and others (1971) and references that they cited; and Feth and others (1964). Additional water- discharge and water-quality data, published annually by the U.S. Geological Survey, and climatologic data, published monthly by the National Oceanic and Atmospheric Administration, are available for Salt Lake County. (See for example, U.S. Geological Survey, 1982 and National Oceanic and Atmospheric Administration, 1982.)
","language":"English","publisher":"U.S. Geological Survey","publisherLocation":"Salt Lake City, UT","doi":"10.3133/ofr83694","collaboration":"Prepared in cooperation with the Salt Lake County Division of Flood Control and Water Quality","usgsCitation":"McCormack, H., Christensen, R., Stephens, D.W., Pyper, G., Weigel, J.F., and Conroy, L., 1983, Surface water and climatologic data, Salt Lake County, Utah, water year 1981, with selected data for water years 1980 and 1982: U.S. Geological Survey Open-File Report 83-694, Report: iv, 586 p.; Plate: 25.89 in. x 19.85 in., https://doi.org/10.3133/ofr83694.","productDescription":"Report: iv, 586 p.; Plate: 25.89 in. x 19.85 in.","numberOfPages":"590","costCenters":[{"id":610,"text":"Utah Water Science Center","active":true,"usgs":true}],"links":[{"id":150927,"rank":0,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/of/1983/0694/report-thumb.jpg"},{"id":46986,"rank":400,"type":{"id":17,"text":"Plate"},"url":"https://pubs.usgs.gov/of/1983/0694/plate-1.pdf","linkFileType":{"id":1,"text":"pdf"}},{"id":46987,"rank":300,"type":{"id":11,"text":"Document"},"url":"https://pubs.usgs.gov/of/1983/0694/report.pdf","linkFileType":{"id":1,"text":"pdf"}}],"country":"United States","state":"Utah","county":"Salt Lake County","noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"4f4e4affe4b07f02db697b87","contributors":{"authors":[{"text":"McCormack, H.F.","contributorId":93453,"corporation":false,"usgs":true,"family":"McCormack","given":"H.F.","email":"","affiliations":[],"preferred":false,"id":177712,"contributorType":{"id":1,"text":"Authors"},"rank":1},{"text":"Christensen, R.C.","contributorId":56670,"corporation":false,"usgs":true,"family":"Christensen","given":"R.C.","email":"","affiliations":[],"preferred":false,"id":177709,"contributorType":{"id":1,"text":"Authors"},"rank":2},{"text":"Stephens, D. W.","contributorId":68335,"corporation":false,"usgs":true,"family":"Stephens","given":"D.","email":"","middleInitial":"W.","affiliations":[],"preferred":false,"id":177710,"contributorType":{"id":1,"text":"Authors"},"rank":3},{"text":"Pyper, G. E.","contributorId":35337,"corporation":false,"usgs":true,"family":"Pyper","given":"G. E.","affiliations":[],"preferred":false,"id":177708,"contributorType":{"id":1,"text":"Authors"},"rank":4},{"text":"Weigel, J. F.","contributorId":74394,"corporation":false,"usgs":true,"family":"Weigel","given":"J.","email":"","middleInitial":"F.","affiliations":[],"preferred":false,"id":177711,"contributorType":{"id":1,"text":"Authors"},"rank":5},{"text":"Conroy, L.S.","contributorId":6051,"corporation":false,"usgs":true,"family":"Conroy","given":"L.S.","email":"","affiliations":[],"preferred":false,"id":177707,"contributorType":{"id":1,"text":"Authors"},"rank":6}]}} ]}