{"pageNumber":"302","pageRowStart":"7525","pageSize":"25","recordCount":11004,"records":[{"id":70133664,"text":"70133664 - 1995 - Stratigraphic and palaeoenvironmental summary of the south-east Georgia embayment: a correlation of exploratory wells","interactions":[],"lastModifiedDate":"2014-11-18T12:03:59","indexId":"70133664","displayToPublicDate":"1995-01-01T00:00:00","publicationYear":"1995","noYear":false,"publicationType":{"id":2,"text":"Article"},"publicationSubtype":{"id":10,"text":"Journal Article"},"seriesTitle":{"id":2682,"text":"Marine and Petroleum Geology","active":true,"publicationSubtype":{"id":10}},"title":"Stratigraphic and palaeoenvironmental summary of the south-east Georgia embayment: a correlation of exploratory wells","docAbstract":"<p>A Continental Offshore Stratigraphic Test (COST) well and six exploratory wells have been drilled in the south-east Georgia embayment. The oldest rocks penetrated are weakly metamorphosed Lower Ordovician quartz arenites and Silurian shales and argillites in the Transco 1005-1 well and Upper Devonian argillites in the COST GE-1 well. These marine strata, which are equivalent to the Tippecanoe sequence in Florida, underlie the post-rift unconformity and represent part of a disjunct fragment of Gondwana that was sutured to the North American craton during the late Palaeozoic Alleghanian orogeny. The Palaeozoic strata are unconformably overlain by interbedded non-marine Jurassic (Bajocian and younger) sandstones and shales and marginal marine Lower Cretaceous sandstones, calcareous shales and carbonates, which contain scattered beds of coal and evaporite. Together, these rocks are stratigraphically equivalent to the onshore Fort Pierce and Cotton Valley(?) Formations and rocks of the Lower Cretaceous Comanchean Provincial Series. The abundance of carbonates and evaporites in this interval, which reflects marine influences within the embayment, increases upwards, eastwards and southwards. The Upper Cretaceous part of the section is composed mainly of neritic calcareous shales and shaley limestones stratigraphically equivalent to the primarily marginal marine facies of the onshore Atkinson, Cape Fear and Middendorf Formations and Black Creek Group, and to limestones and shales of the Lawson Limestone and Peedee Formations. Cenozoic strata are primarily semiconsolidated marine carbonates. Palaeocene to middle Eocene strata are commonly cherty; middle Miocene to Pliocene strata are massive and locally phosphatic and glauconitic; Quaternary sediments are dominated by unconsolidated carbonate sands. The effects of eustatic changes and shifts in the palaeocirculation are recorded in the Upper Cretaceous and Tertiary strata.</p>","language":"English","publisher":"Elsevier","doi":"10.1016/0264-8172(95)98092-J","usgsCitation":"Poppe, L., Popenoe, P., Poag, C.W., and Swift, B.A., 1995, Stratigraphic and palaeoenvironmental summary of the south-east Georgia embayment: a correlation of exploratory wells: Marine and Petroleum Geology, v. 12, no. 6, p. 677-680, https://doi.org/10.1016/0264-8172(95)98092-J.","productDescription":"4 p.","startPage":"677","endPage":"680","onlineOnly":"N","additionalOnlineFiles":"N","costCenters":[{"id":186,"text":"Coastal and Marine Geology Program","active":true,"usgs":true}],"links":[{"id":296160,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/thumbnails/outside_thumb.jpg"}],"country":"United States","state":"Georgia","volume":"12","issue":"6","noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"546c762ce4b0f4a3478a619e","contributors":{"authors":[{"text":"Poppe, Lawrence J. lpoppe@usgs.gov","contributorId":2149,"corporation":false,"usgs":true,"family":"Poppe","given":"Lawrence J.","email":"lpoppe@usgs.gov","affiliations":[{"id":678,"text":"Woods Hole Coastal and Marine Science Center","active":true,"usgs":true}],"preferred":false,"id":525354,"contributorType":{"id":1,"text":"Authors"},"rank":1},{"text":"Popenoe, Peter","contributorId":62206,"corporation":false,"usgs":true,"family":"Popenoe","given":"Peter","email":"","affiliations":[{"id":678,"text":"Woods Hole Coastal and Marine Science Center","active":true,"usgs":true}],"preferred":false,"id":525355,"contributorType":{"id":1,"text":"Authors"},"rank":2},{"text":"Poag, C. Wylie 0000-0002-6240-4065 wpoag@usgs.gov","orcid":"https://orcid.org/0000-0002-6240-4065","contributorId":2565,"corporation":false,"usgs":true,"family":"Poag","given":"C.","email":"wpoag@usgs.gov","middleInitial":"Wylie","affiliations":[{"id":678,"text":"Woods Hole Coastal and Marine Science Center","active":true,"usgs":true}],"preferred":true,"id":525356,"contributorType":{"id":1,"text":"Authors"},"rank":3},{"text":"Swift, B. Ann","contributorId":92685,"corporation":false,"usgs":true,"family":"Swift","given":"B.","email":"","middleInitial":"Ann","affiliations":[{"id":678,"text":"Woods Hole Coastal and Marine Science Center","active":true,"usgs":true}],"preferred":false,"id":525357,"contributorType":{"id":1,"text":"Authors"},"rank":4}]}}
,{"id":22088,"text":"ofr95832 - 1995 - Quaternary geologic map of the Palisades Creek-Comanche Creek area, eastern Grand Canyon, Arizona","interactions":[],"lastModifiedDate":"2023-04-03T19:57:38.755241","indexId":"ofr95832","displayToPublicDate":"1995-01-01T00:00:00","publicationYear":"1995","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":"95-832","title":"Quaternary geologic map of the Palisades Creek-Comanche Creek area, eastern Grand Canyon, Arizona","docAbstract":"<p>No abstract available.</p>","language":"English","publisher":"U.S. Geological Survey","doi":"10.3133/ofr95832","usgsCitation":"Lucchitta, I., Dehler, C.M., Davis, M.E., Basdekas, P., and Burke, K.J., 1995, Quaternary geologic map of the Palisades Creek-Comanche Creek area, eastern Grand Canyon, Arizona: U.S. Geological Survey Open-File Report 95-832, Report: 39 p.; 2 Plates: 30.00 x 42.00 inches and 32.00 x 42.00 inches, https://doi.org/10.3133/ofr95832.","productDescription":"Report: 39 p.; 2 Plates: 30.00 x 42.00 inches and 32.00 x 42.00 inches","costCenters":[],"links":[{"id":415104,"rank":5,"type":{"id":36,"text":"NGMDB Index Page"},"url":"https://ngmdb.usgs.gov/Prodesc/proddesc_70953.htm","linkFileType":{"id":5,"text":"html"}},{"id":19418,"rank":2,"type":{"id":11,"text":"Document"},"url":"https://pubs.usgs.gov/of/1995/0832/report.pdf","linkFileType":{"id":1,"text":"pdf"}},{"id":19417,"rank":3,"type":{"id":17,"text":"Plate"},"url":"https://pubs.usgs.gov/of/1995/0832/plate-2.pdf","linkFileType":{"id":1,"text":"pdf"}},{"id":19416,"rank":4,"type":{"id":17,"text":"Plate"},"url":"https://pubs.usgs.gov/of/1995/0832/plate-1.pdf","linkFileType":{"id":1,"text":"pdf"}},{"id":153781,"rank":1,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/of/1995/0832/report-thumb.jpg"}],"country":"United States","state":"Arizona","otherGeospatial":"Palisades Creek -Comanche Creek area","geographicExtents":"{\n  \"type\": \"FeatureCollection\",\n  \"features\": [\n    {\n      \"type\": \"Feature\",\n      \"properties\": {},\n      \"geometry\": {\n        \"coordinates\": [\n          [\n            [\n              -111.833,\n              36.1442\n            ],\n            [\n              -111.833,\n              36.1069\n            ],\n            [\n              -111.8083,\n              36.1069\n            ],\n            [\n              -111.8083,\n              36.1442\n            ],\n            [\n              -111.833,\n              36.1442\n            ]\n          ]\n        ],\n        \"type\": \"Polygon\"\n      }\n    }\n  ]\n}","noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"4f4e4a81e4b07f02db64a256","contributors":{"authors":[{"text":"Lucchitta, Ivo","contributorId":94291,"corporation":false,"usgs":true,"family":"Lucchitta","given":"Ivo","email":"","affiliations":[],"preferred":false,"id":187019,"contributorType":{"id":1,"text":"Authors"},"rank":1},{"text":"Dehler, Carol M.","contributorId":25187,"corporation":false,"usgs":true,"family":"Dehler","given":"Carol","email":"","middleInitial":"M.","affiliations":[],"preferred":false,"id":187017,"contributorType":{"id":1,"text":"Authors"},"rank":2},{"text":"Davis, M. E.","contributorId":14844,"corporation":false,"usgs":true,"family":"Davis","given":"M.","email":"","middleInitial":"E.","affiliations":[],"preferred":false,"id":187016,"contributorType":{"id":1,"text":"Authors"},"rank":3},{"text":"Basdekas, P. G.","contributorId":96286,"corporation":false,"usgs":true,"family":"Basdekas","given":"P. G.","affiliations":[],"preferred":false,"id":187020,"contributorType":{"id":1,"text":"Authors"},"rank":4},{"text":"Burke, K. J.","contributorId":52599,"corporation":false,"usgs":true,"family":"Burke","given":"K.","email":"","middleInitial":"J.","affiliations":[],"preferred":false,"id":187018,"contributorType":{"id":1,"text":"Authors"},"rank":5}]}}
,{"id":1015915,"text":"1015915 - 1995 - Are red-tailed hawks and great horned owls diurnal-nocturnal dietary counterparts?","interactions":[],"lastModifiedDate":"2012-02-02T00:04:47","indexId":"1015915","displayToPublicDate":"1995-01-01T00:00:00","publicationYear":"1995","noYear":false,"publicationType":{"id":2,"text":"Article"},"publicationSubtype":{"id":10,"text":"Journal Article"},"seriesTitle":{"id":3783,"text":"The Wilson Bulletin","printIssn":"0043-5643","active":true,"publicationSubtype":{"id":10}},"title":"Are red-tailed hawks and great horned owls diurnal-nocturnal dietary counterparts?","docAbstract":"Red-tailed Hawks (Buteo jamaicensis) and Great Homed Owls (Bubo virginianus)are common in North America where they occupy a wide range of habitats, often sympatrically. The two species are similar in size and have been portrayed as ecological counterparts, eating the same prey by day and night. We tested the trophic similarity of the two species by comparing published dietary data from across the United States. Both species ate primarily mammals and birds, and mean proportions of those two prey types did not differ significantly between diets of the two raptors. Red-tailed Hawks ate significantly more reptiles, and Great Homed Owls significantly more invertebrates. Dietary diversity was not significantly different at the level of prey taxonomic class, and diet overlap between the two species averaged 91%. At the prey species level, dietary overlap averaged only 50%, and at that level Red-tailed Hawk dietary diversity was significantly greater than that of Great Horned Owls. Mean prey mass of Red-tailed Hawks was significantly greater than that of Great Homed Owls. Populations of the two species in the western United States differed trophically more than did eastern populations. We conclude that, although the two species are generalist predators, they take largely different prey species in the same localities resulting in distinctive trophic characteristics.","largerWorkType":{"id":2,"text":"Article"},"largerWorkTitle":"Wilson Bulletin","largerWorkSubtype":{"id":10,"text":"Journal Article"},"language":"English","usgsCitation":"Marti, C., and Kochert, M.N., 1995, Are red-tailed hawks and great horned owls diurnal-nocturnal dietary counterparts?: The Wilson Bulletin, v. 107, no. 4, p. 615-628.","productDescription":"p. 615-628","startPage":"615","endPage":"628","numberOfPages":"14","costCenters":[{"id":290,"text":"Forest and Rangeland Ecosystem Science Center","active":false,"usgs":true}],"links":[{"id":133880,"rank":0,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/thumbnails/outside_thumb.jpg"}],"volume":"107","issue":"4","noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"4f4e4abde4b07f02db674232","contributors":{"authors":[{"text":"Marti, C.D.","contributorId":31359,"corporation":false,"usgs":true,"family":"Marti","given":"C.D.","email":"","affiliations":[],"preferred":false,"id":323299,"contributorType":{"id":1,"text":"Authors"},"rank":1},{"text":"Kochert, Michael N. 0000-0002-4380-3298 mkochert@usgs.gov","orcid":"https://orcid.org/0000-0002-4380-3298","contributorId":3037,"corporation":false,"usgs":true,"family":"Kochert","given":"Michael","email":"mkochert@usgs.gov","middleInitial":"N.","affiliations":[{"id":290,"text":"Forest and Rangeland Ecosystem Science Center","active":false,"usgs":true},{"id":289,"text":"Forest and Rangeland Ecosys Science Center","active":true,"usgs":true}],"preferred":true,"id":323298,"contributorType":{"id":1,"text":"Authors"},"rank":2}]}}
,{"id":1003205,"text":"1003205 - 1995 - The occurrence of mycoplasmas in selected wild North American waterfowl","interactions":[],"lastModifiedDate":"2017-12-21T11:13:55","indexId":"1003205","displayToPublicDate":"1995-01-01T00:00:00","publicationYear":"1995","noYear":false,"publicationType":{"id":2,"text":"Article"},"publicationSubtype":{"id":10,"text":"Journal Article"},"seriesTitle":{"id":2507,"text":"Journal of Wildlife Diseases","active":true,"publicationSubtype":{"id":10}},"title":"The occurrence of mycoplasmas in selected wild North American waterfowl","docAbstract":"<p><span>We determined the prevalence of mycoplasma infection in breeding mallard (</span><i>Anas platyrhynchos</i><span>) and canvasback (</span><i>Aythya valisineria</i><span>) hens and their broods from the central United States (1988 to 1990); and wintering American black duck (</span><i>Anas rubripes</i><span>) and mallard hens from the eastern United States (1990 to 1993). Mycoplasmas were isolated by culturing tracheal swabs from 656 live birds and tissue samples from 112 dead waterfowl. Nine (18%) of 51 mycoplasma isolates were identified as </span><i>Mycoplasma anatis</i><span>; </span><i>M. anatis</i><span> was recovered from four mallards, a black duck, and a gadwall (</span><i>Anas strepera</i><span>) duckling. Nineteen (37%) of 51 mycoplasma isolates were identified as </span><i>Mycoplasma cloacale</i><span>; these isolates were obtained from mallard, canvasback, and black duck adults, and from a mallard duckling. Additional unspeciated mycoplasmas were isolated from mallards, black ducks, and one canvasback.</span></p>","language":"English","publisher":"Wildlife Disease Association","doi":"10.7589/0090-3558-31.3.364","issn":"00903558","usgsCitation":"Goldberg, D., Samuel, M., Thomas, C.B., Sharp, P., Krapu, G., Robb, J., Kenow, K., Korschgen, C.E., Chipley, W., Conroy, M., and Kleven, S., 1995, The occurrence of mycoplasmas in selected wild North American waterfowl: Journal of Wildlife Diseases, v. 31, no. 3, p. 364-371, https://doi.org/10.7589/0090-3558-31.3.364.","productDescription":"8 p.","startPage":"364","endPage":"371","costCenters":[{"id":456,"text":"National Wildlife Health Center","active":true,"usgs":true},{"id":480,"text":"Northern Prairie Wildlife Research Center","active":true,"usgs":true},{"id":606,"text":"Upper Midwest Environmental Sciences Center","active":true,"usgs":true}],"links":[{"id":133688,"rank":0,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/thumbnails/outside_thumb.jpg"}],"country":"United States","volume":"31","issue":"3","noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"4f4e4a80e4b07f02db6494a8","contributors":{"authors":[{"text":"Goldberg, Diana R. 0000-0001-8540-8512","orcid":"https://orcid.org/0000-0001-8540-8512","contributorId":82252,"corporation":false,"usgs":true,"family":"Goldberg","given":"Diana R.","affiliations":[{"id":456,"text":"National Wildlife Health Center","active":true,"usgs":true}],"preferred":false,"id":312950,"contributorType":{"id":1,"text":"Authors"},"rank":1},{"text":"Samuel, M.D.","contributorId":13910,"corporation":false,"usgs":true,"family":"Samuel","given":"M.D.","affiliations":[],"preferred":false,"id":312946,"contributorType":{"id":1,"text":"Authors"},"rank":2},{"text":"Thomas, C. B.","contributorId":87888,"corporation":false,"usgs":false,"family":"Thomas","given":"C.","email":"","middleInitial":"B.","affiliations":[],"preferred":false,"id":312952,"contributorType":{"id":1,"text":"Authors"},"rank":3},{"text":"Sharp, P.","contributorId":88685,"corporation":false,"usgs":false,"family":"Sharp","given":"P.","email":"","affiliations":[],"preferred":false,"id":312953,"contributorType":{"id":1,"text":"Authors"},"rank":4},{"text":"Krapu, Gary L.","contributorId":56994,"corporation":false,"usgs":true,"family":"Krapu","given":"Gary L.","affiliations":[],"preferred":false,"id":312949,"contributorType":{"id":1,"text":"Authors"},"rank":5},{"text":"Robb, J.R.","contributorId":11551,"corporation":false,"usgs":true,"family":"Robb","given":"J.R.","email":"","affiliations":[],"preferred":false,"id":312945,"contributorType":{"id":1,"text":"Authors"},"rank":6},{"text":"Kenow, K.P.","contributorId":18302,"corporation":false,"usgs":true,"family":"Kenow","given":"K.P.","affiliations":[],"preferred":false,"id":312948,"contributorType":{"id":1,"text":"Authors"},"rank":7},{"text":"Korschgen, C. E.","contributorId":9197,"corporation":false,"usgs":true,"family":"Korschgen","given":"C.","email":"","middleInitial":"E.","affiliations":[],"preferred":false,"id":312944,"contributorType":{"id":1,"text":"Authors"},"rank":8},{"text":"Chipley, W.H.","contributorId":14783,"corporation":false,"usgs":true,"family":"Chipley","given":"W.H.","email":"","affiliations":[],"preferred":false,"id":312947,"contributorType":{"id":1,"text":"Authors"},"rank":9},{"text":"Conroy, M.J.","contributorId":84690,"corporation":false,"usgs":true,"family":"Conroy","given":"M.J.","email":"","affiliations":[],"preferred":false,"id":312951,"contributorType":{"id":1,"text":"Authors"},"rank":10},{"text":"Kleven, S.H.","contributorId":92633,"corporation":false,"usgs":true,"family":"Kleven","given":"S.H.","email":"","affiliations":[],"preferred":false,"id":312954,"contributorType":{"id":1,"text":"Authors"},"rank":11}]}}
,{"id":1000748,"text":"1000748 - 1995 - Lake trout rehabilitation in Lake Ontario","interactions":[],"lastModifiedDate":"2016-04-14T11:46:35","indexId":"1000748","displayToPublicDate":"1995-01-01T00:00:00","publicationYear":"1995","noYear":false,"publicationType":{"id":2,"text":"Article"},"publicationSubtype":{"id":10,"text":"Journal Article"},"seriesTitle":{"id":2330,"text":"Journal of Great Lakes Research","active":true,"publicationSubtype":{"id":10}},"title":"Lake trout rehabilitation in Lake Ontario","docAbstract":"<p><span>Attempts to maintain the native lake trout (</span><i>Salvelinus namaycush</i><span>) population in Lake Ontario by stocking fry failed and the species was extirpated by the 1950s. Hatchery fish stocked in the 1960s did not live to maturity because of sea lamprey (</span><i>Petromyzon marinus</i><span>) predation and incidental commercial harvest. Suppression of sea lampreys began with larvicide treatments of Lake Ontario tributaries in 1971 and was enhanced when the tributaries of Oneida Lake and Lake Erie were treated in the 1980s. Annual stocking of hatchery fish was resumed with the 1972 year class and peaked at about 1.8 million yearlings and 0.3 million fingerlings from the 1985&ndash;1990 year classes. Survival of stocked yearlings declined over 50% in the 1980 s and was negatively correlated with the abundance of lake trout &gt; 550 mm long (r = &minus;0.91, P &lt; 0.01, n = 12). A slot length limit imposed by the State of New York for the 1988 fishing season reduced angler harvest. Angler harvest in Canadian waters was 3 times higher in eastern Lake Ontario than in western Lake Ontario. For the 1977&ndash;1984 year classes, mean annual survival rate of lake trout age 6 and older was 0.45 (range: 0.35&ndash;0.56). In U.S. waters during 1985&ndash;1992, the total number of lake trout harvested by anglers was about 2.4 times greater than that killed by sea lampreys. The number of unmarked lake trout &lt; 250 mm long in trawl catches in 1978&ndash;1992 was not different from that expected due to loss of marks and failure to apply marks at the hatchery, and suggested that recruitment of naturally-produced fish was nil. However, many of the obstacles which may have impeded lake trout rehabilitation in Lake Ontario during the 1980s are slowly being removed, and there are signs of a general ecosystem recovery. Significant recruitment of naturally produced lake trout by the year 2000, one interim objective of the rehabilitation plan for the Lake, may be achieved.</span></p>","language":"English","publisher":"Elsevier","doi":"10.1016/S0380-1330(95)71085-1","usgsCitation":"Elrod, J.H., O’Gorman, R., Schneider, C.P., Eckert, T.H., Schaner, T., Bowlby, J.N., and Schleen, L.P., 1995, Lake trout rehabilitation in Lake Ontario: Journal of Great Lakes Research, v. 21, no. Supplement 1, p. 83-107, https://doi.org/10.1016/S0380-1330(95)71085-1.","productDescription":"25 p.","startPage":"83","endPage":"107","onlineOnly":"N","additionalOnlineFiles":"N","costCenters":[{"id":324,"text":"Great Lakes Science Center","active":true,"usgs":true}],"links":[{"id":133138,"rank":0,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/thumbnails/outside_thumb.jpg"}],"volume":"21","issue":"Supplement 1","noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"4f4e4b27e4b07f02db6b104a","contributors":{"authors":[{"text":"Elrod, Joseph H.","contributorId":72737,"corporation":false,"usgs":true,"family":"Elrod","given":"Joseph","email":"","middleInitial":"H.","affiliations":[],"preferred":false,"id":309318,"contributorType":{"id":1,"text":"Authors"},"rank":1},{"text":"O’Gorman, Robert rogorman@usgs.gov","contributorId":3451,"corporation":false,"usgs":true,"family":"O’Gorman","given":"Robert","email":"rogorman@usgs.gov","affiliations":[],"preferred":true,"id":309313,"contributorType":{"id":1,"text":"Authors"},"rank":2},{"text":"Schneider, Clifford P.","contributorId":45251,"corporation":false,"usgs":true,"family":"Schneider","given":"Clifford","email":"","middleInitial":"P.","affiliations":[],"preferred":false,"id":309315,"contributorType":{"id":1,"text":"Authors"},"rank":3},{"text":"Eckert, Thomas H.","contributorId":58585,"corporation":false,"usgs":true,"family":"Eckert","given":"Thomas","email":"","middleInitial":"H.","affiliations":[],"preferred":false,"id":309316,"contributorType":{"id":1,"text":"Authors"},"rank":4},{"text":"Schaner, Ted","contributorId":69939,"corporation":false,"usgs":true,"family":"Schaner","given":"Ted","email":"","affiliations":[],"preferred":false,"id":309317,"contributorType":{"id":1,"text":"Authors"},"rank":5},{"text":"Bowlby, James N.","contributorId":97863,"corporation":false,"usgs":true,"family":"Bowlby","given":"James","email":"","middleInitial":"N.","affiliations":[],"preferred":false,"id":309319,"contributorType":{"id":1,"text":"Authors"},"rank":6},{"text":"Schleen, Larry P.","contributorId":27016,"corporation":false,"usgs":true,"family":"Schleen","given":"Larry","email":"","middleInitial":"P.","affiliations":[],"preferred":false,"id":309314,"contributorType":{"id":1,"text":"Authors"},"rank":7}]}}
,{"id":1003775,"text":"1003775 - 1995 - First record of an hypopus (Acari: Hypoderatidae) from a jaeger (Aves: Charadriiformes: Stercorariidae)","interactions":[],"lastModifiedDate":"2024-11-04T19:52:31.853768","indexId":"1003775","displayToPublicDate":"1995-01-01T00:00:00","publicationYear":"1995","noYear":false,"publicationType":{"id":2,"text":"Article"},"publicationSubtype":{"id":10,"text":"Journal Article"},"seriesTitle":{"id":2385,"text":"Journal of Medical Entomology","active":true,"publicationSubtype":{"id":10}},"title":"First record of an hypopus (Acari: Hypoderatidae) from a jaeger (Aves: Charadriiformes: Stercorariidae)","docAbstract":"<p>Thalassornectes (Alcidectes) aukletae, originally described from two species of auklets (Charadriiformes: Alcidae) from maritime eastern Russia, is reported from a third species of pelagic charadriiform (Stercorariidae), the pomarine jaeger, Stercorarius poinarinus (Temminck), from Florida. The specimens from the jaeger are slightly smaller, the genital apodeme is more heavily sclerotized, paired setae gm are twice as long and there are other minor variations in the idiosomal and leg chaetotaxy. These differences are not considered sufficient to warrant taxonomic separation at the species or subspecies level from the nominate species T. (A.) aukletae. The same hypopus occurring across different families of birds is unusual in the Hypoderatidae. The diversity in hosts from several orders of birds, low intensities of infection in the two species from Africa, low prevalences in alcids from Russia, and rarity of these hypoderatids in all surveyed hosts leads us to speculate that the true host affinities of species in the genus Thalassornectes are unknown. The alternative consideration is that these are simply uncommon species that are very host specific.</p>","language":"English","publisher":"Oxford Academic","doi":"10.1093/jmedent/32.3.394","usgsCitation":"Pence, D.B., and Cole, R.A., 1995, First record of an hypopus (Acari: Hypoderatidae) from a jaeger (Aves: Charadriiformes: Stercorariidae): Journal of Medical Entomology, v. 32, no. 3, p. 394-396, https://doi.org/10.1093/jmedent/32.3.394.","productDescription":"3 p.","startPage":"394","endPage":"396","numberOfPages":"3","onlineOnly":"N","additionalOnlineFiles":"N","costCenters":[{"id":456,"text":"National Wildlife Health Center","active":true,"usgs":true}],"links":[{"id":134274,"rank":1,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/thumbnails/outside_thumb.jpg"}],"country":"United States","state":"Florida","county":"Pinellas County","geographicExtents":"{\"type\":\"FeatureCollection\",\"features\":[{\"type\":\"Feature\",\"geometry\":{\"type\":\"MultiPolygon\",\"coordinates\":[[[[-82.7151,27.6479],[-82.7162,27.631],[-82.7064,27.6286],[-82.6989,27.6383],[-82.7028,27.6272],[-82.7335,27.6118],[-82.7428,27.6411],[-82.734,27.6438],[-82.7254,27.6209],[-82.7151,27.6479]]],[[[-82.7403,27.6764],[-82.7347,27.6744],[-82.7451,27.6531],[-82.7403,27.6764]]],[[[-82.725,27.695],[-82.7167,27.6886],[-82.7228,27.6722],[-82.7167,27.6558],[-82.7297,27.6672],[-82.725,27.695]]],[[[-82.7083,27.7167],[-82.7128,27.7007],[-82.7222,27.7075],[-82.7083,27.7167]]],[[[-82.7482,27.7452],[-82.7347,27.735],[-82.7393,27.7245],[-82.7305,27.725],[-82.7267,27.712],[-82.7366,27.7158],[-82.725,27.7044],[-82.7362,27.6833],[-82.7399,27.717],[-82.7588,27.7573],[-82.7482,27.7452]]],[[[-82.765,27.7869],[-82.7572,27.7778],[-82.7675,27.7722],[-82.7653,27.7611],[-82.7549,27.7406],[-82.7826,27.7817],[-82.765,27.7869]]],[[[-82.8333,27.9661],[-82.8236,27.96],[-82.8497,27.8725],[-82.8287,27.8279],[-82.8195,27.8293],[-82.793,27.7967],[-82.785,27.8039],[-82.7814,27.7844],[-82.8284,27.8219],[-82.8475,27.8567],[-82.8508,27.8925],[-82.8333,27.9661]]],[[[-82.8197,27.9975],[-82.8111,27.9703],[-82.8214,27.9761],[-82.8197,27.9975]]],[[[-82.815,28.0333],[-82.8131,28.0067],[-82.8206,28.0153],[-82.8264,28.0097],[-82.8275,27.9665],[-82.8282,28.0179],[-82.8197,28.0458],[-82.815,28.0333]]],[[[-82.8397,28.1139],[-82.8313,28.1071],[-82.8415,28.1119],[-82.8378,28.1281],[-82.8397,28.1139]]],[[[-82.6513,28.173],[-82.6486,28.0207],[-82.6574,27.9988],[-82.6638,27.9993],[-82.6653,28.0272],[-82.6933,28.0366],[-82.6761,28.0065],[-82.7044,27.9661],[-82.6908,27.9756],[-82.6953,27.9639],[-82.6575,27.9667],[-82.7156,27.9578],[-82.7261,27.9411],[-82.7025,27.9244],[-82.653,27.9087],[-82.6501,27.8959],[-82.6317,27.9083],[-82.6378,27.8911],[-82.6072,27.8737],[-82.5853,27.8797],[-82.6147,27.8631],[-82.5988,27.8652],[-82.5884,27.8311],[-82.5969,27.8264],[-82.6103,27.8417],[-82.6065,27.8267],[-82.59,27.8139],[-82.6122,27.7898],[-82.63,27.7989],[-82.6229,27.7677],[-82.6355,27.7623],[-82.6264,27.7487],[-82.6399,27.7385],[-82.625,27.735],[-82.6264,27.7233],[-82.6358,27.72],[-82.6403,27.7033],[-82.6731,27.7049],[-82.6772,27.6955],[-82.68,27.7136],[-82.6905,27.71],[-82.6979,27.7188],[-82.6925,27.7344],[-82.7139,27.7361],[-82.7336,27.7533],[-82.7503,27.7494],[-82.7422,27.7692],[-82.7475,27.7569],[-82.7564,27.7583],[-82.7475,27.7719],[-82.7619,27.8083],[-82.7564,27.8189],[-82.7783,27.8369],[-82.7794,27.8592],[-82.7843,27.8625],[-82.7836,27.8433],[-82.7657,27.8168],[-82.7697,27.8003],[-82.795,27.8092],[-82.8073,27.8278],[-82.8354,27.839],[-82.8405,27.8495],[-82.8488,27.8767],[-82.8301,27.8984],[-82.8272,27.9231],[-82.7933,27.9881],[-82.7861,28.0481],[-82.825,28.0568],[-82.8378,28.0814],[-82.8374,28.087],[-82.8342,28.0758],[-82.8279,28.0837],[-82.8281,28.0666],[-82.7994,28.0519],[-82.7786,28.0592],[-82.7844,28.0672],[-82.7719,28.0844],[-82.7837,28.0835],[-82.7839,28.1061],[-82.7758,28.1083],[-82.7989,28.1609],[-82.7936,28.1731],[-82.7706,28.16],[-82.7719,28.1519],[-82.7859,28.1737],[-82.6513,28.173]]]]},\"properties\":{\"name\":\"Pinellas\",\"state\":\"FL\"}}]}","volume":"32","issue":"3","noUsgsAuthors":false,"publicationDate":"1995-05-01","publicationStatus":"PW","scienceBaseUri":"4f4e49fae4b07f02db5f3ce1","contributors":{"authors":[{"text":"Pence, Danny B.","contributorId":64624,"corporation":false,"usgs":true,"family":"Pence","given":"Danny","email":"","middleInitial":"B.","affiliations":[],"preferred":false,"id":314235,"contributorType":{"id":1,"text":"Authors"},"rank":1},{"text":"Cole, Rebecca A. 0000-0003-2923-1622","orcid":"https://orcid.org/0000-0003-2923-1622","contributorId":39719,"corporation":false,"usgs":true,"family":"Cole","given":"Rebecca","email":"","middleInitial":"A.","affiliations":[],"preferred":false,"id":314234,"contributorType":{"id":1,"text":"Authors"},"rank":2}]}}
,{"id":1002513,"text":"1002513 - 1995 - Dicofol and DDT residues in lizard carcasses and bird eggs from Texas, Florida, and California","interactions":[],"lastModifiedDate":"2018-01-26T15:45:09","indexId":"1002513","displayToPublicDate":"1995-01-01T00:00:00","publicationYear":"1995","noYear":false,"publicationType":{"id":2,"text":"Article"},"publicationSubtype":{"id":10,"text":"Journal Article"},"seriesTitle":{"id":1103,"text":"Bulletin of Environmental Contamination and Toxicology","active":true,"publicationSubtype":{"id":10}},"title":"Dicofol and DDT residues in lizard carcasses and bird eggs from Texas, Florida, and California","docAbstract":"<p>Dicofol is an organochlorine agricultural pesticide used to control mites. The principal commercial dicofol product is known as Kelthane TM. More than 70% of dicofol product (about 3 million Ib or 1.4 million kg) sold annually in the U.S. is applied in California, Arizona, Texas, and Florida. Florida citrus and California cotton receive more than half the total (Clark 1990). In laboratory studies, dicofol, which is structurally similar to DDT, had adverse impacts on reproduction in fish (deformed larvae, delayed hatching), birds (reduced eggshell thickness, reduced hatchability), and mammals (reduced insemination rate, reduced pregnancy rate, failure to produce young) (see Clark 1990 for review). Overall, the reproduction of birds seems less sensitive to dicofol than to DDE. However, in birds, dietary concentrations of dicofol between 1 and 10 µg/g (wet weight) fed to captive adult females caused such problems as eggshell thinning, reduced hatching success, or reduced fertility in American kestrels (<i>Falco sparverius</i>) (Fry et al. 1988, Clark et al. 1990) and eastern screech-owls (<i>Otus asio</i>) (Wiemeyer et al. 1989). In spite of these laboratory findings, there have been no intensive field investigations of possible reproductive effects of dicofol on wild birds. Such studies must wait until field residue data are sufficient to identify populations with high exposure. If dicofol accumulates in birds in the field and heavily exposed populations can be identified, then their reproduction can be studied. Residues have not been reported from reptiles. Analytical screening of wildlife tissue samples for organochlorine chemicals only rarely includes dicofol, and this may explain why the relative hazard of dicofol to wildlife populations is poorly known. </p>","language":"English","publisher":"Springer","doi":"10.1007/BF00197964","usgsCitation":"Clark, D., Flickinger, E.L., White, D.H., Hothem, R.L., and Belisle, A.A., 1995, Dicofol and DDT residues in lizard carcasses and bird eggs from Texas, Florida, and California: Bulletin of Environmental Contamination and Toxicology, v. 54, no. 6, p. 817-824, https://doi.org/10.1007/BF00197964.","productDescription":"8 p.","startPage":"817","endPage":"824","costCenters":[{"id":455,"text":"National Wetlands Research Center","active":true,"usgs":true},{"id":531,"text":"Patuxent Wildlife Research Center","active":true,"usgs":true}],"links":[{"id":134000,"rank":0,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/thumbnails/outside_thumb.jpg"}],"country":"United States","state":"California, Florida, Texas","volume":"54","issue":"6","noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"4f4e4a9ae4b07f02db65d9e1","contributors":{"authors":[{"text":"Clark, D.R.","contributorId":66654,"corporation":false,"usgs":true,"family":"Clark","given":"D.R.","affiliations":[],"preferred":false,"id":312114,"contributorType":{"id":1,"text":"Authors"},"rank":1},{"text":"Flickinger, Edward L.","contributorId":48907,"corporation":false,"usgs":true,"family":"Flickinger","given":"Edward","email":"","middleInitial":"L.","affiliations":[],"preferred":false,"id":312113,"contributorType":{"id":1,"text":"Authors"},"rank":2},{"text":"White, Donald H.","contributorId":97868,"corporation":false,"usgs":true,"family":"White","given":"Donald","email":"","middleInitial":"H.","affiliations":[],"preferred":false,"id":312117,"contributorType":{"id":1,"text":"Authors"},"rank":3},{"text":"Hothem, R. L.","contributorId":82633,"corporation":false,"usgs":true,"family":"Hothem","given":"R.","email":"","middleInitial":"L.","affiliations":[],"preferred":false,"id":312116,"contributorType":{"id":1,"text":"Authors"},"rank":4},{"text":"Belisle, A. A.","contributorId":77897,"corporation":false,"usgs":true,"family":"Belisle","given":"A.","email":"","middleInitial":"A.","affiliations":[],"preferred":false,"id":312115,"contributorType":{"id":1,"text":"Authors"},"rank":5}]}}
,{"id":52694,"text":"b1988H - 1995 - Upper Devonian-Mississippian stratigraphic sequences in the distal Antler foreland of western Utah and adjoining Nevada","interactions":[{"subject":{"id":52694,"text":"b1988H - 1995 - Upper Devonian-Mississippian stratigraphic sequences in the distal Antler foreland of western Utah and adjoining Nevada","indexId":"b1988H","publicationYear":"1995","noYear":false,"chapter":"H","title":"Upper Devonian-Mississippian stratigraphic sequences in the distal Antler foreland of western Utah and adjoining Nevada"},"predicate":"IS_PART_OF","object":{"id":33239,"text":"b1988 - 1992 - Evolution of sedimentary basins: Eastern Great Basin","indexId":"b1988","publicationYear":"1992","noYear":false,"title":"Evolution of sedimentary basins: Eastern Great Basin"},"id":1}],"isPartOf":{"id":33239,"text":"b1988 - 1992 - Evolution of sedimentary basins: Eastern Great Basin","indexId":"b1988","publicationYear":"1992","noYear":false,"title":"Evolution of sedimentary basins: Eastern Great Basin"},"lastModifiedDate":"2022-08-25T20:27:21.359883","indexId":"b1988H","displayToPublicDate":"1994-01-01T00:00:00","publicationYear":"1995","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":"1988","chapter":"H","title":"Upper Devonian-Mississippian stratigraphic sequences in the distal Antler foreland of western Utah and adjoining Nevada","docAbstract":"<p>No abstract available.</p>","largerWorkType":{"id":18,"text":"Report"},"largerWorkTitle":"Evolution of sedimentary basins: Eastern Great Basin (Bulletin 1988)","largerWorkSubtype":{"id":5,"text":"USGS Numbered Series"},"language":"English","publisher":"U.S. Geological Survey","doi":"10.3133/b1988H","usgsCitation":"Silberling, N.J., Nichols, K.M., Macke, D., and Trappe, J., 1995, Upper Devonian-Mississippian stratigraphic sequences in the distal Antler foreland of western Utah and adjoining Nevada: U.S. Geological Survey Bulletin 1988, iii, 33 p., https://doi.org/10.3133/b1988H.","productDescription":"iii, 33 p.","costCenters":[],"links":[{"id":100218,"rank":300,"type":{"id":11,"text":"Document"},"url":"https://pubs.usgs.gov/bul/1988h/report.pdf","linkFileType":{"id":1,"text":"pdf"}},{"id":405631,"rank":3,"type":{"id":36,"text":"NGMDB Index Page"},"url":"https://ngmdb.usgs.gov/Prodesc/proddesc_22212.htm","linkFileType":{"id":5,"text":"html"}},{"id":174146,"rank":0,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/bul/1988h/report-thumb.jpg"}],"country":"United States","state":"Nevada, Utah","otherGeospatial":"Antler foreland","geographicExtents":"{\n  \"type\": \"FeatureCollection\",\n  \"features\": [\n    {\n      \"type\": \"Feature\",\n      \"properties\": {},\n      \"geometry\": {\n        \"type\": \"Polygon\",\n        \"coordinates\": [\n          [\n            [\n              -115,\n              38\n            ],\n            [\n              -111,\n              38\n            ],\n            [\n              -111,\n              42\n            ],\n            [\n              -115,\n              42\n            ],\n            [\n              -115,\n              38\n            ]\n          ]\n        ]\n      }\n    }\n  ]\n}","noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"4f4e4a23e4b07f02db60d20a","contributors":{"authors":[{"text":"Silberling, Norman J.","contributorId":102438,"corporation":false,"usgs":true,"family":"Silberling","given":"Norman","email":"","middleInitial":"J.","affiliations":[],"preferred":false,"id":245844,"contributorType":{"id":1,"text":"Authors"},"rank":1},{"text":"Nichols, K. M.","contributorId":14832,"corporation":false,"usgs":true,"family":"Nichols","given":"K.","email":"","middleInitial":"M.","affiliations":[],"preferred":false,"id":245841,"contributorType":{"id":1,"text":"Authors"},"rank":2},{"text":"Macke, D. L.","contributorId":101643,"corporation":false,"usgs":true,"family":"Macke","given":"D. L.","affiliations":[],"preferred":false,"id":245843,"contributorType":{"id":1,"text":"Authors"},"rank":3},{"text":"Trappe, Jorg","contributorId":36617,"corporation":false,"usgs":true,"family":"Trappe","given":"Jorg","email":"","affiliations":[],"preferred":false,"id":245842,"contributorType":{"id":1,"text":"Authors"},"rank":4}]}}
,{"id":68110,"text":"ha730M - 1995 - Ground Water Atlas of the United States: Segment 12, Connecticut, Maine, Massachusetts, New Hampshire, New York, Rhode Island, Vermont","interactions":[{"subject":{"id":68110,"text":"ha730M - 1995 - Ground Water Atlas of the United States: Segment 12, Connecticut, Maine, Massachusetts, New Hampshire, New York, Rhode Island, Vermont","indexId":"ha730M","publicationYear":"1995","noYear":false,"chapter":"M","title":"Ground Water Atlas of the United States: Segment 12, Connecticut, Maine, Massachusetts, New Hampshire, New York, Rhode Island, Vermont"},"predicate":"IS_PART_OF","object":{"id":68687,"text":"ha730 - 2000 - Ground Water Atlas of the United States","indexId":"ha730","publicationYear":"2000","noYear":false,"title":"Ground Water Atlas of the United States"},"id":1}],"isPartOf":{"id":68687,"text":"ha730 - 2000 - Ground Water Atlas of the United States","indexId":"ha730","publicationYear":"2000","noYear":false,"title":"Ground Water Atlas of the United States"},"lastModifiedDate":"2017-05-30T15:37:02","indexId":"ha730M","displayToPublicDate":"1994-01-01T00:00:00","publicationYear":"1995","noYear":false,"publicationType":{"id":18,"text":"Report"},"publicationSubtype":{"id":5,"text":"USGS Numbered Series"},"seriesTitle":{"id":318,"text":"Hydrologic Atlas","code":"HA","active":false,"publicationSubtype":{"id":5}},"seriesNumber":"730","chapter":"M","title":"Ground Water Atlas of the United States: Segment 12, Connecticut, Maine, Massachusetts, New Hampshire, New York, Rhode Island, Vermont","docAbstract":"<p>The State of New York and the six New England States of Maine, Vermont, New Hampshire, Massachusetts, Connecticut, and Rhode Island compose Segment 12 of this Atlas (fig. 1). The seven States have a total land area of about 116,000 square miles (table 1); all but a small area in southwestern New York has been glaciated. </p><p>Population in the States of Segment 12 totals about 30,408,000 (table 1) and is concentrated in southern and eastern Massachusetts, Connecticut, Rhode Island, and especially New York (fig. 1). The northern part of the segment and the mountainous areas of New York and much of New Hampshire, Vermont, and Maine are sparsely populated. </p><p>The percentage of population supplied from ground-water sources during 1980 was 54 to 60 percent in Maine, New Hampshire, and Vermont (table 1). Nearly all rural, domestic, and small-community water systems obtain water from wells that are, in comparison with other sources, the safest and the least expensive to install and maintain. Where water demand is great-in the urban areas of New York, Connecticut, Massachusetts, and Rhode Island-sophisticated reservoir, pipeline, and purification systems are economically feasible and are needed to meet demands. Surface water is the principal source of supply in these four States, and ground water was used to supply only 24 to 35 percent of their population during 1980 (table 1).</p>","largerWorkTitle":"Ground Water Atlas of the United States","language":"English","publisher":"U.S. Geological Survey","doi":"10.3133/ha730M","isbn":"0607868732","usgsCitation":"Olcott, P.G., 1995, Ground Water Atlas of the United States: Segment 12, Connecticut, Maine, Massachusetts, New Hampshire, New York, Rhode Island, Vermont: U.S. Geological Survey Hydrologic Atlas 730, 28 p., https://doi.org/10.3133/ha730M.","productDescription":"28 p.","startPage":"M1","endPage":"M28","costCenters":[{"id":595,"text":"U.S. Geological Survey","active":false,"usgs":true}],"links":[{"id":11490,"rank":100,"type":{"id":15,"text":"Index Page"},"url":"https://pubs.usgs.gov/ha/ha730/ch_m/index.html","linkFileType":{"id":5,"text":"html"}},{"id":186515,"rank":0,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/ha/730m/report-thumb.jpg"},{"id":115251,"rank":300,"type":{"id":11,"text":"Document"},"url":"https://pubs.usgs.gov/ha/730m/report.pdf","text":"Report","size":"56.57 MB","linkFileType":{"id":1,"text":"pdf"},"description":"Report"}],"country":"United States","state":"Connecticut, Maine, Massachusetts, New Hampshire, New York, Rhode Island, Vermont","geographicExtents":"{\"type\":\"FeatureCollection\",\"features\":[{\"type\":\"Feature\",\"geometry\":{\"type\":\"MultiPolygon\",\"coordinates\":[[[[-71.860513,41.320248],[-71.886302,41.33641],[-71.945652,41.337799],[-71.988153,41.320577],[-72.084487,41.319634],[-72.11182,41.299098],[-72.184122,41.323997],[-72.212924,41.291365],[-72.248161,41.299488],[-72.261487,41.282926],[-72.333894,41.282916],[-72.386629,41.261798],[-72.398688,41.278172],[-72.451925,41.278885],[-72.546833,41.250718],[-72.583336,41.271698],[-72.617237,41.271998],[-72.671673,41.267151],[-72.69547,41.244948],[-72.754444,41.266913],[-72.895445,41.243697],[-72.916827,41.282033],[-73.013465,41.205479],[-73.054947,41.208468],[-73.07761,41.195176],[-73.108352,41.153718],[-73.130253,41.146797],[-73.177774,41.166697],[-73.235058,41.143996],[-73.262358,41.117496],[-73.286759,41.127896],[-73.372296,41.10402],[-73.435063,41.056696],[-73.468239,41.051347],[-73.477364,41.035997],[-73.493327,41.048173],[-73.516903,41.038738],[-73.528866,41.016397],[-73.535338,41.03192],[-73.570068,41.001597],[-73.595699,41.015995],[-73.643478,41.002171],[-73.683273,40.948998],[-73.756776,40.912599],[-73.784803,40.878528],[-73.781206,40.838891],[-73.793785,40.855583],[-73.81281,40.846737],[-73.811889,40.825363],[-73.781369,40.794907],[-73.728275,40.8529],[-73.730675,40.8654],[-73.675573,40.856999],[-73.633771,40.898198],[-73.499941,40.918166],[-73.485365,40.946397],[-73.406074,40.920235],[-73.392862,40.955297],[-73.352761,40.926697],[-73.229285,40.905121],[-73.148994,40.928898],[-73.140785,40.966178],[-73.110368,40.971938],[-72.774104,40.965314],[-72.714425,40.985596],[-72.585327,40.997587],[-72.477306,41.052212],[-72.445242,41.086116],[-72.397,41.096307],[-72.356087,41.133635],[-72.278789,41.158722],[-72.238211,41.15949],[-72.300374,41.112274],[-72.306381,41.13784],[-72.32663,41.132162],[-72.335177,41.106917],[-72.317238,41.088659],[-72.280373,41.080402],[-72.260515,41.042065],[-72.190563,41.032579],[-72.153857,41.051859],[-72.10216,40.991509],[-71.96704,41.047772],[-71.959595,41.071237],[-71.857494,41.073558],[-71.903736,41.040166],[-72.39585,40.86666],[-73.054963,40.666371],[-73.262106,40.621476],[-73.306396,40.620756],[-73.319257,40.635795],[-73.562372,40.583703],[-73.774928,40.590759],[-73.934512,40.545175],[-73.95005,40.573363],[-74.00903,40.572846],[-74.001591,40.590684],[-74.032856,40.604421],[-74.042412,40.624847],[-74.018272,40.659019],[-74.013784,40.756601],[-73.929006,40.889578],[-73.893979,40.997197],[-74.694914,41.357423],[-74.691129,41.367324],[-74.740963,41.40512],[-74.736688,41.429228],[-74.790417,41.42166],[-74.805655,41.442101],[-74.834635,41.430796],[-74.8542,41.443166],[-74.888691,41.438259],[-74.917282,41.477041],[-74.981652,41.479945],[-74.984372,41.506611],[-75.003706,41.511118],[-75.023018,41.533147],[-75.018524,41.551802],[-75.074613,41.605711],[-75.043562,41.62364],[-75.052736,41.688393],[-75.067278,41.705434],[-75.052226,41.711396],[-75.053431,41.752538],[-75.10464,41.774203],[-75.074409,41.815088],[-75.113334,41.822782],[-75.114399,41.843583],[-75.161541,41.849836],[-75.174574,41.87266],[-75.183937,41.860515],[-75.257825,41.862154],[-75.279094,41.938917],[-75.318168,41.954236],[-75.342204,41.972872],[-75.341125,41.992772],[-75.359579,41.999445],[-79.761374,41.999067],[-79.761951,42.26986],[-79.453533,42.411157],[-79.351989,42.48892],[-79.148723,42.553672],[-79.111361,42.613358],[-79.06376,42.644758],[-79.04886,42.689158],[-78.918157,42.737258],[-78.853455,42.783958],[-78.865592,42.852358],[-78.891655,42.884845],[-78.912458,42.886557],[-78.905659,42.923357],[-78.918859,42.946857],[-79.019964,42.994756],[-79.01053,43.064389],[-79.074467,43.077855],[-79.042366,43.143655],[-79.070469,43.262454],[-78.634346,43.357624],[-78.370221,43.376505],[-77.976438,43.369159],[-77.760231,43.341161],[-77.551022,43.235763],[-77.341092,43.280661],[-77.111866,43.287945],[-76.958402,43.270005],[-76.69836,43.344436],[-76.630774,43.413356],[-76.486962,43.47535],[-76.417581,43.521285],[-76.297103,43.51287],[-76.228701,43.532987],[-76.199138,43.600454],[-76.205436,43.718751],[-76.229268,43.804135],[-76.283307,43.843923],[-76.28272,43.858601],[-76.243384,43.877975],[-76.202257,43.864898],[-76.133267,43.892975],[-76.125023,43.912773],[-76.139086,43.962111],[-76.22805,43.982737],[-76.264294,43.978009],[-76.269672,44.001148],[-76.296755,44.013307],[-76.300532,44.057188],[-76.360306,44.070907],[-76.363835,44.111696],[-76.312647,44.199044],[-76.206777,44.214543],[-76.164265,44.239603],[-76.161833,44.280777],[-76.000998,44.347534],[-75.970185,44.342835],[-75.912985,44.368084],[-75.82083,44.432244],[-75.807778,44.471644],[-75.76623,44.515851],[-75.413885,44.76889],[-75.333744,44.806378],[-75.283136,44.849156],[-75.027125,44.946568],[-74.992756,44.977449],[-74.907956,44.983359],[-74.826578,45.01585],[-74.731301,44.990422],[-74.702018,45.003322],[-74.146814,44.9915],[-73.059685,45.015869],[-72.310073,45.003822],[-71.502487,45.013367],[-71.497917,45.070589],[-71.427208,45.127364],[-71.437216,45.142333],[-71.39781,45.203553],[-71.443882,45.235462],[-71.38317,45.234904],[-71.357253,45.253336],[-71.362831,45.267617],[-71.284396,45.302434],[-71.231572,45.253472],[-71.13943,45.242958],[-71.097772,45.301906],[-71.00905,45.319022],[-71.004848,45.345419],[-70.921435,45.313867],[-70.912111,45.296197],[-70.9217,45.279445],[-70.892822,45.239172],[-70.84443,45.234513],[-70.848554,45.263325],[-70.807058,45.322464],[-70.819828,45.340109],[-70.802648,45.364933],[-70.826033,45.398408],[-70.798677,45.424146],[-70.755567,45.428361],[-70.712286,45.390611],[-70.634661,45.383608],[-70.635498,45.427817],[-70.717047,45.487732],[-70.723167,45.507606],[-70.688214,45.563981],[-70.5584,45.666671],[-70.525831,45.666551],[-70.469869,45.701639],[-70.400404,45.719834],[-70.383552,45.734869],[-70.417641,45.79377],[-70.253704,45.902981],[-70.263315,45.920152],[-70.24092,45.939095],[-70.252963,45.955234],[-70.31297,45.961856],[-70.309725,45.98021],[-70.287754,45.99182],[-70.317629,46.01908],[-70.278169,46.059671],[-70.306734,46.061344],[-70.284554,46.098713],[-70.254021,46.0996],[-70.239566,46.142762],[-70.292736,46.191599],[-70.248421,46.267072],[-70.205719,46.299865],[-70.208733,46.328961],[-70.191412,46.348072],[-70.141164,46.362669],[-70.096286,46.40943],[-70.057061,46.415036],[-69.997086,46.69523],[-69.22442,47.459686],[-69.082508,47.423976],[-69.043947,47.427634],[-69.050367,47.259821],[-68.90524,47.180919],[-68.717867,47.240919],[-68.607906,47.247497],[-68.582984,47.285493],[-68.507432,47.296636],[-68.448844,47.282547],[-68.376829,47.28852],[-68.380334,47.340242],[-68.329879,47.36023],[-68.234604,47.355035],[-68.15515,47.32542],[-68.137059,47.296068],[-67.955669,47.199542],[-67.883844,47.105834],[-67.789761,47.065744],[-67.781095,45.943032],[-67.750422,45.917898],[-67.803318,45.883718],[-67.796514,45.859961],[-67.755068,45.82367],[-67.806598,45.794723],[-67.806308,45.755405],[-67.781892,45.731189],[-67.809833,45.729274],[-67.803148,45.696127],[-67.817892,45.693705],[-67.720401,45.662522],[-67.729908,45.689012],[-67.64581,45.613597],[-67.631762,45.621409],[-67.499444,45.587014],[-67.455406,45.604665],[-67.429716,45.583773],[-67.420976,45.550029],[-67.435044,45.528783],[-67.416416,45.503515],[-67.462882,45.508691],[-67.503157,45.485367],[-67.473366,45.425328],[-67.418747,45.37726],[-67.460554,45.300379],[-67.489464,45.282653],[-67.404629,45.159926],[-67.345585,45.126392],[-67.298209,45.146672],[-67.283619,45.192022],[-67.227324,45.163652],[-67.161247,45.162879],[-67.090786,45.068721],[-67.117688,45.05673],[-67.082074,45.029608],[-67.033474,44.939923],[-66.984466,44.912557],[-66.990351,44.882551],[-66.978142,44.856963],[-66.996523,44.844654],[-66.986318,44.820657],[-66.950569,44.814539],[-67.02615,44.768199],[-67.062239,44.769543],[-67.073439,44.741957],[-67.098931,44.741311],[-67.103957,44.717444],[-67.155119,44.66944],[-67.213025,44.63922],[-67.24726,44.641664],[-67.293403,44.599265],[-67.32297,44.609394],[-67.293665,44.634316],[-67.309627,44.659316],[-67.299176,44.705705],[-67.308538,44.707454],[-67.376742,44.681852],[-67.363158,44.631825],[-67.386605,44.626974],[-67.405492,44.594236],[-67.428367,44.609136],[-67.457747,44.598014],[-67.505804,44.636837],[-67.551133,44.621938],[-67.575056,44.560659],[-67.568159,44.531117],[-67.648506,44.525403],[-67.685861,44.537155],[-67.71419,44.495238],[-67.733986,44.496252],[-67.753854,44.543661],[-67.774001,44.547438],[-67.781556,44.520577],[-67.79726,44.520685],[-67.808837,44.544081],[-67.839896,44.558771],[-67.856684,44.523934],[-67.851648,44.484901],[-67.868774,44.465272],[-67.855108,44.419434],[-67.887323,44.433066],[-67.899571,44.394078],[-67.92132,44.433066],[-67.931453,44.411848],[-67.955737,44.416278],[-67.978876,44.387034],[-68.006102,44.409562],[-68.049334,44.33073],[-68.067047,44.335692],[-68.077873,44.373047],[-68.11229,44.401588],[-68.117746,44.475038],[-68.194554,44.47189],[-68.189937,44.484901],[-68.213861,44.492456],[-68.224354,44.464335],[-68.261708,44.484062],[-68.299063,44.437893],[-68.247438,44.433276],[-68.249956,44.417747],[-68.184532,44.369145],[-68.173608,44.328397],[-68.233435,44.288578],[-68.289409,44.283858],[-68.290818,44.247673],[-68.317588,44.225101],[-68.401268,44.252244],[-68.430946,44.298624],[-68.398035,44.376191],[-68.360318,44.389674],[-68.3791,44.430049],[-68.427874,44.3968],[-68.429648,44.439136],[-68.455095,44.447498],[-68.461072,44.378504],[-68.483317,44.388157],[-68.472824,44.404106],[-68.480379,44.432647],[-68.529905,44.39907],[-68.565161,44.39907],[-68.545434,44.355],[-68.566936,44.317603],[-68.538595,44.299902],[-68.519516,44.265046],[-68.525302,44.227554],[-68.733004,44.328388],[-68.762021,44.329597],[-68.795063,44.30786],[-68.827197,44.31216],[-68.814811,44.362194],[-68.821767,44.40894],[-68.783679,44.473879],[-68.880271,44.428112],[-68.897104,44.450643],[-68.927452,44.448039],[-68.990767,44.415033],[-68.948164,44.355882],[-68.954465,44.32405],[-68.979005,44.296327],[-69.003682,44.294582],[-69.005071,44.274071],[-69.040193,44.233673],[-69.054546,44.171542],[-69.077776,44.165043],[-69.080331,44.117824],[-69.100863,44.104529],[-69.092,44.085734],[-69.056303,44.095162],[-69.031878,44.079036],[-69.048917,44.062506],[-69.064299,44.069911],[-69.073767,44.046135],[-69.125738,44.019623],[-69.124475,44.007419],[-69.170345,43.995637],[-69.214205,43.935583],[-69.259838,43.921427],[-69.280498,43.95744],[-69.31427,43.942951],[-69.305176,43.956676],[-69.331411,43.974311],[-69.398455,43.971804],[-69.423324,43.915507],[-69.483498,43.88028],[-69.50329,43.837673],[-69.514889,43.831298],[-69.520301,43.868498],[-69.543912,43.881615],[-69.552606,43.841347],[-69.575466,43.841972],[-69.588551,43.81836],[-69.604179,43.813551],[-69.594705,43.858878],[-69.621086,43.826814],[-69.634932,43.845907],[-69.649798,43.836287],[-69.653337,43.79103],[-69.705838,43.823024],[-69.719723,43.786685],[-69.752801,43.75594],[-69.780097,43.755397],[-69.835323,43.721125],[-69.838689,43.70514],[-69.851297,43.703581],[-69.868673,43.742701],[-69.862155,43.758962],[-69.884066,43.778035],[-69.953246,43.768806],[-70.001645,43.717666],[-69.998793,43.740385],[-70.041351,43.738053],[-69.99821,43.798684],[-70.026193,43.822587],[-70.002874,43.848239],[-70.009869,43.859315],[-70.064671,43.813259],[-70.107229,43.809178],[-70.176023,43.76079],[-70.172525,43.773615],[-70.190014,43.771866],[-70.215666,43.707737],[-70.254144,43.676839],[-70.211204,43.625765],[-70.217087,43.596717],[-70.196911,43.565146],[-70.244331,43.551849],[-70.272497,43.562616],[-70.361214,43.52919],[-70.385615,43.487031],[-70.380233,43.46423],[-70.349684,43.442032],[-70.39089,43.402607],[-70.421282,43.395777],[-70.460717,43.34325],[-70.517695,43.344037],[-70.553854,43.321886],[-70.593907,43.249295],[-70.575787,43.221859],[-70.638355,43.114182],[-70.673114,43.070314],[-70.703818,43.059825],[-70.704696,43.070989],[-70.718936,43.03235],[-70.810069,42.909549],[-70.817731,42.850613],[-70.80522,42.781798],[-70.770453,42.704824],[-70.778552,42.69852],[-70.689402,42.653319],[-70.630077,42.692699],[-70.623815,42.665481],[-70.595474,42.660336],[-70.591469,42.639821],[-70.61842,42.62864],[-70.654727,42.582234],[-70.675747,42.594669],[-70.698574,42.577393],[-70.871382,42.546404],[-70.866279,42.522617],[-70.831091,42.503596],[-70.835991,42.490496],[-70.857791,42.490296],[-70.894292,42.460896],[-70.934993,42.457896],[-70.933155,42.437833],[-70.901992,42.420297],[-70.936393,42.418097],[-70.943612,42.452092],[-70.96047,42.446166],[-70.990595,42.407098],[-70.953022,42.343973],[-70.998253,42.352788],[-71.01568,42.326019],[-70.98909,42.267449],[-70.910941,42.265412],[-70.895778,42.292436],[-70.915588,42.302463],[-70.882764,42.30886],[-70.851093,42.26827],[-70.770964,42.249197],[-70.722269,42.207959],[-70.714301,42.168783],[-70.63848,42.081579],[-70.643208,42.050821],[-70.66936,42.037116],[-70.670934,42.007786],[-70.695809,42.013346],[-70.710034,41.999544],[-70.662476,41.960592],[-70.616491,41.940204],[-70.583572,41.950007],[-70.552941,41.929641],[-70.525567,41.85873],[-70.54103,41.815754],[-70.471552,41.761563],[-70.290957,41.734312],[-70.263654,41.714115],[-70.189254,41.751982],[-70.024734,41.787364],[-70.003842,41.80852],[-70.000188,41.886938],[-70.024335,41.89882],[-70.030537,41.929154],[-70.044995,41.930049],[-70.065671,41.911658],[-70.064084,41.878924],[-70.095595,42.032832],[-70.155415,42.062409],[-70.186816,42.05045],[-70.186295,42.021308],[-70.196693,42.022429],[-70.245385,42.063733],[-70.189305,42.082337],[-70.058531,42.040363],[-69.986085,41.949597],[-69.935952,41.809422],[-69.928261,41.6917],[-69.967869,41.627503],[-69.988215,41.554704],[-70.004136,41.54212],[-70.016584,41.550772],[-69.994357,41.576846],[-69.973153,41.646963],[-70.007011,41.671579],[-70.191061,41.645259],[-70.265424,41.609333],[-70.28132,41.635125],[-70.351634,41.634687],[-70.379151,41.611361],[-70.437246,41.605329],[-70.485571,41.554244],[-70.633607,41.538254],[-70.79027,41.446339],[-70.948431,41.409193],[-70.928165,41.431265],[-70.906011,41.425708],[-70.802186,41.460864],[-70.658659,41.543385],[-70.64204,41.583066],[-70.652449,41.60521],[-70.640003,41.624616],[-70.652614,41.637829],[-70.638695,41.649427],[-70.646308,41.678433],[-70.661475,41.681756],[-70.623652,41.707398],[-70.718739,41.73574],[-70.728933,41.723433],[-70.719575,41.685002],[-70.755347,41.694326],[-70.765463,41.641575],[-70.809118,41.656437],[-70.816351,41.645995],[-70.800215,41.631753],[-70.810279,41.624873],[-70.852518,41.626919],[-70.852551,41.588526],[-70.887643,41.632422],[-70.913202,41.619266],[-70.899981,41.593504],[-70.927172,41.611253],[-70.931338,41.5842],[-70.946911,41.581089],[-70.931545,41.540169],[-71.035514,41.499047],[-71.085663,41.509292],[-71.136867,41.493942],[-71.19302,41.457931],[-71.213563,41.545818],[-71.212417,41.61829],[-71.240709,41.619225],[-71.227989,41.528297],[-71.24071,41.474872],[-71.285639,41.487805],[-71.304394,41.454502],[-71.337695,41.448902],[-71.362743,41.460379],[-71.316519,41.47756],[-71.330831,41.518364],[-71.288376,41.573274],[-71.271862,41.623986],[-71.212136,41.641945],[-71.19564,41.67509],[-71.224798,41.710498],[-71.25956,41.642595],[-71.280366,41.672575],[-71.299159,41.649531],[-71.306095,41.672575],[-71.291217,41.702666],[-71.31482,41.723808],[-71.350057,41.727835],[-71.37791,41.666646],[-71.445923,41.691144],[-71.444468,41.664409],[-71.409302,41.662643],[-71.40377,41.589321],[-71.447712,41.5804],[-71.414825,41.523126],[-71.417621,41.477934],[-71.483295,41.371722],[-71.555381,41.373316],[-71.857432,41.306318],[-71.860513,41.320248]]],[[[-70.59628,41.471905],[-70.567356,41.471208],[-70.547567,41.415831],[-70.506984,41.400242],[-70.501306,41.385391],[-70.450431,41.420703],[-70.451084,41.348161],[-70.709826,41.341723],[-70.747541,41.329952],[-70.775665,41.300982],[-70.838777,41.347209],[-70.774974,41.349176],[-70.686881,41.441334],[-70.603555,41.482384],[-70.59628,41.471905]]],[[[-70.092142,41.297741],[-70.031332,41.339332],[-70.030924,41.367453],[-70.049564,41.3879],[-70.033514,41.385816],[-69.960181,41.264546],[-70.001586,41.239353],[-70.118669,41.242351],[-70.256164,41.288123],[-70.275526,41.310464],[-70.229541,41.290171],[-70.092142,41.297741]]],[[[-70.152589,43.746794],[-70.145911,43.772119],[-70.128271,43.774009],[-70.152589,43.746794]]],[[[-70.171245,43.663498],[-70.205934,43.633633],[-70.188047,43.673762],[-70.171245,43.663498]]],[[[-70.186213,43.682655],[-70.21313,43.662973],[-70.201893,43.685483],[-70.186213,43.682655]]],[[[-70.163884,43.692404],[-70.135563,43.700658],[-70.168227,43.675136],[-70.163884,43.692404]]],[[[-70.087621,43.699913],[-70.115908,43.682978],[-70.095727,43.709278],[-70.087621,43.699913]]],[[[-70.119671,43.748621],[-70.097318,43.757292],[-70.124136,43.70832],[-70.138711,43.727559],[-70.119671,43.748621]]],[[[-68.499465,44.12419],[-68.491521,44.109833],[-68.51706,44.10341],[-68.511266,44.125082],[-68.499465,44.12419]]],[[[-68.358388,44.125082],[-68.330716,44.110598],[-68.365176,44.101464],[-68.376593,44.112207],[-68.358388,44.125082]]],[[[-68.453236,44.189998],[-68.416434,44.187047],[-68.384903,44.154955],[-68.438518,44.11618],[-68.456813,44.145268],[-68.502096,44.152388],[-68.453236,44.189998]]],[[[-68.680773,44.279242],[-68.623554,44.255622],[-68.605906,44.230772],[-68.624994,44.197637],[-68.618872,44.18107],[-68.681899,44.138212],[-68.720435,44.169185],[-68.722956,44.219607],[-68.680458,44.262105],[-68.680773,44.279242]]],[[[-68.355279,44.199096],[-68.31606,44.200244],[-68.347416,44.169459],[-68.378872,44.184222],[-68.355279,44.199096]]],[[[-68.472831,44.219767],[-68.453843,44.201683],[-68.48452,44.202886],[-68.482726,44.227058],[-68.472831,44.219767]]],[[[-68.792139,44.237819],[-68.769833,44.222787],[-68.780055,44.203129],[-68.829593,44.21689],[-68.839422,44.236547],[-68.792139,44.237819]]],[[[-68.23638,44.266254],[-68.211329,44.257074],[-68.23713,44.25343],[-68.248913,44.235443],[-68.274427,44.237099],[-68.274719,44.258675],[-68.23638,44.266254]]],[[[-68.498637,44.369686],[-68.478785,44.319563],[-68.489641,44.313705],[-68.530394,44.333583],[-68.518573,44.381022],[-68.501364,44.382281],[-68.498637,44.369686]]],[[[-68.618212,44.012367],[-68.635315,44.018886],[-68.652881,44.003845],[-68.661594,44.075837],[-68.6181,44.096706],[-68.584074,44.070578],[-68.618212,44.012367]]],[[[-68.785601,44.053503],[-68.818441,44.032046],[-68.889717,44.032516],[-68.913406,44.08519],[-68.907812,44.105518],[-68.943105,44.10973],[-68.935327,44.13038],[-68.825067,44.186338],[-68.818423,44.160978],[-68.780693,44.143274],[-68.820515,44.130198],[-68.772639,44.078439],[-68.785601,44.053503]]],[[[-67.619761,44.519754],[-67.582113,44.513459],[-67.590627,44.49415],[-67.562651,44.472104],[-67.574206,44.45173],[-67.588346,44.449754],[-67.619761,44.519754]]],[[[-68.942826,44.281073],[-68.919301,44.309872],[-68.90353,44.378613],[-68.868444,44.38144],[-68.860649,44.364425],[-68.896587,44.321986],[-68.88746,44.303094],[-68.916872,44.242866],[-68.95189,44.218719],[-68.965264,44.259332],[-68.942826,44.281073]]],[[[-74.144428,40.53516],[-74.219787,40.502603],[-74.254588,40.502303],[-74.247808,40.543396],[-74.210887,40.560902],[-74.1894,40.642121],[-74.075884,40.648101],[-74.059184,40.593502],[-74.144428,40.53516]]],[[[-72.132225,41.104387],[-72.126704,41.115139],[-72.084207,41.101524],[-72.086975,41.058292],[-72.095711,41.05402],[-72.103152,41.086484],[-72.139233,41.092451],[-72.132225,41.104387]]],[[[-71.943563,41.286675],[-71.926802,41.290122],[-72.036846,41.249794],[-72.023422,41.270994],[-71.943563,41.286675]]],[[[-71.383586,41.464782],[-71.399568,41.448596],[-71.373618,41.573214],[-71.359868,41.556308],[-71.360403,41.483121],[-71.383586,41.464782]]],[[[-71.3312,41.580318],[-71.325877,41.623988],[-71.366165,41.66098],[-71.338696,41.658782],[-71.342514,41.644791],[-71.30555,41.622523],[-71.307381,41.597984],[-71.3312,41.580318]]],[[[-71.58955,41.196557],[-71.576661,41.224434],[-71.561093,41.224207],[-71.565752,41.184373],[-71.547051,41.153684],[-71.611706,41.153239],[-71.58955,41.196557]]]]},\"properties\":{\"name\":\"Connecticut\",\"nation\":\"USA  \"}}]}","noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"4f4e4b32e4b07f02db6b4289","contributors":{"authors":[{"text":"Olcott, Perry G.","contributorId":17249,"corporation":false,"usgs":true,"family":"Olcott","given":"Perry","email":"","middleInitial":"G.","affiliations":[],"preferred":false,"id":277659,"contributorType":{"id":1,"text":"Authors"},"rank":1}]}}
,{"id":67980,"text":"ha734 - 1995 - Watershed characterization for precipitation-runoff modeling system, north fork, American River and east fork, Carson River watersheds, California","interactions":[],"lastModifiedDate":"2015-10-28T11:29:03","indexId":"ha734","displayToPublicDate":"1994-01-01T00:00:00","publicationYear":"1995","noYear":false,"publicationType":{"id":18,"text":"Report"},"publicationSubtype":{"id":5,"text":"USGS Numbered Series"},"seriesTitle":{"id":318,"text":"Hydrologic Atlas","code":"HA","active":false,"publicationSubtype":{"id":5}},"seriesNumber":"734","title":"Watershed characterization for precipitation-runoff modeling system, north fork, American River and east fork, Carson River watersheds, California","docAbstract":"<p>As part of its Global Change Hydrology Program, the U.S. Geological Survey (USGS) is investigating the potential effects of climate change on the water resources of several river basins in the United States. The American River Basin in California represents the windward slope of the north-central Sierra Nevada, and the California part of the Carson River Basin, most of which is in Nevada, represents the leeward slope. Parts of the American River and Carson River Basins&mdash;the North Fork American River and East Fork Carson River watersheds, both in California&mdash;were studied to determine the sensitivity of water resources to potential climate change. The water resources of both basins are derived primarily from snowmelt. A geographic information system (GIS) data base has been created to facilitate paired-basin analysis. The GIS data base incorporates (1) land-surface data, which include elevation, land use and land cover, soil type, and geology; (2) hydrologic data, such as stream networks and streamflow-gaging stations; and (3) climatic data, such as snow-course, snow-telemetry, radiosonde, and meteorological data. Precipitation-runoff models were developed and calibrated for the North Fork watershed within the American River Basin and for the East Fork watershed within the Carson River Basin. (These watersheds were selected to represent the climatic and physiographic variability of the two larger basins.) Synthesized climate scenarios then were used in the model to predict potential effects of climate change.</p>","language":"ENGLISH","doi":"10.3133/ha734","usgsCitation":"Smith, J.L., and Reece, B.D., 1995, Watershed characterization for precipitation-runoff modeling system, north fork, American River and east fork, Carson River watersheds, California: U.S. Geological Survey Hydrologic Atlas 734, 1 maps on 1 sheet :col ;11 x 14 cm. and 11 x 10 cm., on sheet 109 x 104 cm., folded in envelope 30 x 24 cm., https://doi.org/10.3133/ha734.","productDescription":"1 maps on 1 sheet :col ;11 x 14 cm. and 11 x 10 cm., on sheet 109 x 104 cm., folded in envelope 30 x 24 cm.","onlineOnly":"N","additionalOnlineFiles":"N","costCenters":[],"links":[{"id":252271,"rank":0,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/ha/734/report-thumb.jpg"},{"id":251445,"rank":300,"type":{"id":11,"text":"Document"},"url":"https://pubs.usgs.gov/ha/734/report.pdf","size":"37","linkFileType":{"id":1,"text":"pdf"}},{"id":251446,"rank":400,"type":{"id":17,"text":"Plate"},"url":"https://pubs.usgs.gov/ha/734/plate-1.pdf","size":"11336","linkFileType":{"id":1,"text":"pdf"}}],"scale":"545000","geographicExtents":"{ \"type\": \"FeatureCollection\", \"features\": [ { \"type\": \"Feature\", \"properties\": {}, \"geometry\": { \"type\": \"Polygon\", \"coordinates\": [ [ [ -119.91666666666667,38.35 ], [ -119.91666666666667,38.75 ], [ -119.58333333333333,38.75 ], [ -119.58333333333333,38.35 ], [ -119.91666666666667,38.35 ] ] ] } } ] }","noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"4f4e49e2e4b07f02db5e4b3b","contributors":{"authors":[{"text":"Smith, J. LaRue jlsmith@usgs.gov","contributorId":1863,"corporation":false,"usgs":true,"family":"Smith","given":"J.","email":"jlsmith@usgs.gov","middleInitial":"LaRue","affiliations":[],"preferred":true,"id":277442,"contributorType":{"id":1,"text":"Authors"},"rank":1},{"text":"Reece, Brian D. bdreece@usgs.gov","contributorId":2129,"corporation":false,"usgs":true,"family":"Reece","given":"Brian","email":"bdreece@usgs.gov","middleInitial":"D.","affiliations":[],"preferred":true,"id":277443,"contributorType":{"id":1,"text":"Authors"},"rank":2}]}}
,{"id":56131,"text":"wdrNY941 - 1995 - Water resources data, New York, water year 1994, volume 1, eastern New York, excluding Long Island","interactions":[],"lastModifiedDate":"2019-05-14T11:18:38","indexId":"wdrNY941","displayToPublicDate":"1994-01-01T00:00:00","publicationYear":"1995","noYear":false,"publicationType":{"id":18,"text":"Report"},"publicationSubtype":{"id":5,"text":"USGS Numbered Series"},"seriesTitle":{"id":340,"text":"Water Data Report","code":"WDR","active":false,"publicationSubtype":{"id":5}},"seriesNumber":"NY-94-1","title":"Water resources data, New York, water year 1994, volume 1, eastern New York, excluding Long Island","docAbstract":"<p>Water resources data for the 1994 water year for New York consist of records of stage, discharge, and water quality of streams; stage, content, and water quality of lakes and reservoirs; and ground water levels. This volume contains records for water discharge at 122 gaging stations; stage only at 4 gaging stations; stage and contents at 4 gaging stations, and 19 other lakes and reservoirs; water quality at 38 gaging stations; and water levels at 22 observation wells. Also included are data for 30 crest-stage partial-record stations. Location of all these sites are shown on figure 8. Additional water data were collected at various sites not in the systematic data-collection program and are published as miscellaneous measurements and analyses. These data, together with the data in volumes 2 and 3, represent that part of the National Water Data System operated by the U.S. Geological Survey in cooperation with State, Municipal, and Federal agencies in New York. </p>","language":"English","publisher":"U.S. Geological Survey","doi":"10.3133/wdrNY941","collaboration":"Prepared in cooperation with the State of New York and with other agencies","usgsCitation":"Firda, G.D., Lumia, R., Murray, P.M., and Freeman, W.O., 1995, Water resources data, New York, water year 1994, volume 1, eastern New York, excluding Long Island: U.S. Geological Survey Water Data Report NY-94-1, xiv, 488 p., https://doi.org/10.3133/wdrNY941.","productDescription":"xiv, 488 p.","costCenters":[],"links":[{"id":363759,"rank":2,"type":{"id":11,"text":"Document"},"url":"https://pubs.usgs.gov/wdr/1994/ny-94-1/report.pdf","linkFileType":{"id":1,"text":"pdf"}},{"id":180937,"rank":0,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/wdr/1994/ny-94-1/report-thumb.jpg"}],"country":"United States","state":"New York","geographicExtents":"{\n  \"type\": \"FeatureCollection\",\n  \"features\": [\n    {\n      \"type\": \"Feature\",\n      \"properties\": {},\n      \"geometry\": {\n        \"type\": \"Polygon\",\n        \"coordinates\": [\n          [\n            [\n              -76.25,\n              41\n            ],\n            [\n              -73.1,\n              41\n            ],\n            [\n              -73.1,\n              45\n            ],\n            [\n              -76.25,\n              45\n            ],\n            [\n              -76.25,\n              41\n            ]\n          ]\n        ]\n      }\n    }\n  ]\n}","noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"4f4e4a2ae4b07f02db6121dc","contributors":{"authors":[{"text":"Firda, Gary D. gfirda@usgs.gov","contributorId":1552,"corporation":false,"usgs":true,"family":"Firda","given":"Gary","email":"gfirda@usgs.gov","middleInitial":"D.","affiliations":[],"preferred":true,"id":254805,"contributorType":{"id":1,"text":"Authors"},"rank":1},{"text":"Lumia, Richard rlumia@usgs.gov","contributorId":4579,"corporation":false,"usgs":true,"family":"Lumia","given":"Richard","email":"rlumia@usgs.gov","affiliations":[],"preferred":true,"id":254802,"contributorType":{"id":1,"text":"Authors"},"rank":2},{"text":"Murray, Patricia M. pmurray@usgs.gov","contributorId":4863,"corporation":false,"usgs":true,"family":"Murray","given":"Patricia","email":"pmurray@usgs.gov","middleInitial":"M.","affiliations":[],"preferred":true,"id":254804,"contributorType":{"id":1,"text":"Authors"},"rank":3},{"text":"Freeman, Ward O. wfreeman@usgs.gov","contributorId":1999,"corporation":false,"usgs":true,"family":"Freeman","given":"Ward","email":"wfreeman@usgs.gov","middleInitial":"O.","affiliations":[],"preferred":true,"id":254803,"contributorType":{"id":1,"text":"Authors"},"rank":4}]}}
,{"id":53934,"text":"itr1 - 1995 - Population biology of the Florida manatee","interactions":[],"lastModifiedDate":"2018-10-22T19:17:08","indexId":"itr1","displayToPublicDate":"1994-01-01T00:00:00","publicationYear":"1995","noYear":false,"publicationType":{"id":18,"text":"Report"},"publicationSubtype":{"id":1,"text":"Federal Government Series"},"seriesTitle":{"id":37,"text":"Information and Technology Report","active":false,"publicationSubtype":{"id":1}},"seriesNumber":"1","title":"Population biology of the Florida manatee","docAbstract":"<p>The Florida manatee (<i>Trichechus manatus latirostris</i>) is a unique element of the U.S. fauna. It is a distinct subspecies of the West Indian manatee (Domning and Hayek 1986) and one of the largest inshore mammals of the continent, reaching weights to 1,650 kg (Rathbun et al. 1990). Annual migratory circuits of some individuals through the intracoastal waterways of the Atlantic Coast are 1,700 km round trips at seasonal travel rates as high as 50km/day (*3 Reid and O'Shea 1989; Reid et al. 1991), resulting in one of the longest remaining intact mammalian migrations in the eastern United States.</p>","language":"English","publisher":"U.S. Fish and Wildlife Service","publisherLocation":"Arlington, VA","usgsCitation":"Ackerman, B.B., and Percival, H.F., 1995, Population biology of the Florida manatee: Information and Technology Report 1, vi, 289 p.","productDescription":"vi, 289 p.","costCenters":[{"id":291,"text":"Fort Collins Science Center","active":true,"usgs":true},{"id":416,"text":"National Ecology Research Center","active":false,"usgs":true}],"links":[{"id":178068,"rank":0,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/thumbnails/outside_thumb.jpg"}],"noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"4f4e4adee4b07f02db687338","contributors":{"editors":[{"text":"O’Shea, Thomas J. 0000-0002-0758-9730","orcid":"https://orcid.org/0000-0002-0758-9730","contributorId":207270,"corporation":false,"usgs":true,"family":"O’Shea","given":"Thomas","email":"","middleInitial":"J.","affiliations":[{"id":291,"text":"Fort Collins Science Center","active":true,"usgs":true}],"preferred":true,"id":749305,"contributorType":{"id":2,"text":"Editors"},"rank":1}],"authors":[{"text":"Ackerman, Bruce B.","contributorId":6526,"corporation":false,"usgs":true,"family":"Ackerman","given":"Bruce","email":"","middleInitial":"B.","affiliations":[],"preferred":false,"id":248717,"contributorType":{"id":1,"text":"Authors"},"rank":1},{"text":"Percival, H. Franklin percivalf@usgs.gov","contributorId":2424,"corporation":false,"usgs":true,"family":"Percival","given":"H.","email":"percivalf@usgs.gov","middleInitial":"Franklin","affiliations":[],"preferred":true,"id":248716,"contributorType":{"id":1,"text":"Authors"},"rank":2}]}}
,{"id":6716,"text":"fs09595 - 1995 - Using geochemical data to identify sources of salinity to the freshwater Navajo aquifer in southeastern Utah","interactions":[],"lastModifiedDate":"2017-02-03T11:38:41","indexId":"fs09595","displayToPublicDate":"1994-01-01T00:00:00","publicationYear":"1995","noYear":false,"publicationType":{"id":18,"text":"Report"},"publicationSubtype":{"id":5,"text":"USGS Numbered Series"},"seriesTitle":{"id":313,"text":"Fact Sheet","code":"FS","onlineIssn":"2327-6932","printIssn":"2327-6916","active":true,"publicationSubtype":{"id":5}},"seriesNumber":"095-95","title":"Using geochemical data to identify sources of salinity to the freshwater Navajo aquifer in southeastern Utah","docAbstract":"<p><span>Ground water is an important freshwater source for domestic and livestock uses in southeastern Utah because of the arid climate and unavailability of surface water from the San Juan River. The study area includes about 1,200 square miles in the southeastern corner of Utah (fig. 1). Precipitation on mountainous areas north, south, and east of the study area (fig. 2) seeps into the Navajo and overlying aquifers where the sandstones that contain the aquifers are exposed at the surface along mountain flanks. The ground water then moves slowly away from the mountainous areas toward the area of lowest elevation 109°30' in the region, the San Juan River. The ground water reappears at land surface where it discharges as seepage to the San Juan River or is consumed by vegetation on the flood plain. Generally, wells finished in the Navajo aquifer near the San Juan River do not require pumping because water flows freely from the well casing when it is not sealed.</span></p>","language":"English","publisher":"U.S. Geological Survey","publisherLocation":"Salt Lake City, UT","doi":"10.3133/fs09595","usgsCitation":"Naftz, D.L., Spangler, L.E., and Peterman, Z., 1995, Using geochemical data to identify sources of salinity to the freshwater Navajo aquifer in southeastern Utah: U.S. Geological Survey Fact Sheet 095-95, 4 p., https://doi.org/10.3133/fs09595.","productDescription":"4 p.","numberOfPages":"4","costCenters":[{"id":218,"text":"Denver Federal Center","active":false,"usgs":true},{"id":610,"text":"Utah Water Science Center","active":true,"usgs":true},{"id":5050,"text":"WY-MT Water Science Center","active":true,"usgs":true}],"links":[{"id":125233,"rank":0,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/fs/1995/0095/report-thumb.jpg"},{"id":34107,"rank":300,"type":{"id":11,"text":"Document"},"url":"https://pubs.usgs.gov/fs/1995/0095/report.pdf","linkFileType":{"id":1,"text":"pdf"}}],"country":"United States","state":"Utah","noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"4f4e4a16e4b07f02db603c4f","contributors":{"authors":[{"text":"Naftz, David L. 0000-0003-1130-6892 dlnaftz@usgs.gov","orcid":"https://orcid.org/0000-0003-1130-6892","contributorId":1041,"corporation":false,"usgs":true,"family":"Naftz","given":"David","email":"dlnaftz@usgs.gov","middleInitial":"L.","affiliations":[{"id":5050,"text":"WY-MT Water Science Center","active":true,"usgs":true},{"id":610,"text":"Utah Water Science Center","active":true,"usgs":true}],"preferred":true,"id":153209,"contributorType":{"id":1,"text":"Authors"},"rank":1},{"text":"Spangler, Lawrence E. 0000-0003-3928-8809 spangler@usgs.gov","orcid":"https://orcid.org/0000-0003-3928-8809","contributorId":973,"corporation":false,"usgs":true,"family":"Spangler","given":"Lawrence","email":"spangler@usgs.gov","middleInitial":"E.","affiliations":[{"id":610,"text":"Utah Water Science Center","active":true,"usgs":true}],"preferred":true,"id":153208,"contributorType":{"id":1,"text":"Authors"},"rank":2},{"text":"Peterman, Zell E. 0000-0002-5694-8082 peterman@usgs.gov","orcid":"https://orcid.org/0000-0002-5694-8082","contributorId":620,"corporation":false,"usgs":true,"family":"Peterman","given":"Zell E.","email":"peterman@usgs.gov","affiliations":[{"id":218,"text":"Denver Federal Center","active":false,"usgs":true}],"preferred":false,"id":153207,"contributorType":{"id":1,"text":"Authors"},"rank":3}]}}
,{"id":27518,"text":"wri954121 - 1995 - Use of surface and borehole geophysical surveys to determine fracture orientation and other site characteristics in crystalline bedrock terrain, Millville and Uxbridge, Massachusetts","interactions":[],"lastModifiedDate":"2019-10-15T07:27:24","indexId":"wri954121","displayToPublicDate":"1994-01-01T00:00:00","publicationYear":"1995","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":"95-4121","title":"Use of surface and borehole geophysical surveys to determine fracture orientation and other site characteristics in crystalline bedrock terrain, Millville and Uxbridge, Massachusetts","docAbstract":"Four geophysical techniques were used to determine bedrock-fracture orientation and other site characteristics that can be used to determine ground-water movement and contaminant transport at a fractured crystalline bedrock site in Millville and Uxbridge, Massachusetts. Azimuthal seismic- refraction and azimuthal square-array direct-current resistivity surveys were conducted at three sites. Borehole-radar surveys were conducted in a cluster of three wells. Ground-penetrating radar surveys were conducted along roads in the study area. Azimuthal seismic-refraction data indicated a primary fracture strike between 56 and 101 degrees at three sites. Graphical and analytical analysis of azimuthal square-array resistivity data indicated a primary fracture strike from 45 to 90 degrees at three sites. Directional borehole-radar data from three wells indicated 46 fractures or fracture zones located as far as 147 feet from the surveyed wells. Patterns of low radar-wave velocity and high radar- wave attenuation from cross-hole radar surveys of two well pairs were interpreted as a planar fracture zone that strikes 297 degrees and dips 55 degrees south. Ground-penetrating radar surveys with 100-MHz antennas penetrated as much as 150 feet of bedrock where the bedrock surface was at or near land surface. Horizontal and subhorizontal fractures were observed on the ground-penetrating radar records at numerous locations. Correlation of data sets indicates good agreement and indicates primary high- angle fracturing striking east-northeast. Secondary bedrock porosity and average fracture aperture determined from square-array resistivity data averaged 0.0044 and 0.0071 foot. Depths to bedrock observed on the ground-penetrating radar records were 0 to 20 feet below land surface along most of the area surveyed. A bedrock depth from 45 to 50 feet below land surface was observed along one section of Conestoga Drive.","language":"English","publisher":"U.S. Geological Survey ","publisherLocation":"Reston, VA","doi":"10.3133/wri954121","usgsCitation":"Hansen, B.P., and Lane, J.W., 1995, Use of surface and borehole geophysical surveys to determine fracture orientation and other site characteristics in crystalline bedrock terrain, Millville and Uxbridge, Massachusetts: U.S. Geological Survey Water-Resources Investigations Report 95-4121, iv, 25 p. , https://doi.org/10.3133/wri954121.","productDescription":"iv, 25 p. ","costCenters":[{"id":493,"text":"Office of Ground Water","active":true,"usgs":true}],"links":[{"id":158838,"rank":0,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/wri/1995/4121/report-thumb.jpg"},{"id":56377,"rank":300,"type":{"id":11,"text":"Document"},"url":"https://pubs.usgs.gov/wri/1995/4121/report.pdf","linkFileType":{"id":1,"text":"pdf"}}],"country":"United States","state":"Massachusetts ","county":"Worcester County","geographicExtents":"{\"type\":\"FeatureCollection\",\"features\":[{\"type\":\"Feature\",\"geometry\":{\"type\":\"Polygon\",\"coordinates\":[[[-71.9287,42.713],[-71.8994,42.7121],[-71.8969,42.7037],[-71.8743,42.6869],[-71.8699,42.6833],[-71.8656,42.6842],[-71.8637,42.6792],[-71.8574,42.6752],[-71.8561,42.6679],[-71.8585,42.6338],[-71.8448,42.6379],[-71.7943,42.6367],[-71.775,42.6363],[-71.775,42.644],[-71.6646,42.6115],[-71.6757,42.5519],[-71.6787,42.5301],[-71.6358,42.5238],[-71.6389,42.5315],[-71.6364,42.5347],[-71.6358,42.5397],[-71.6234,42.5515],[-71.6227,42.552],[-71.6209,42.5524],[-71.6203,42.5524],[-71.6103,42.5465],[-71.6078,42.5452],[-71.5947,42.5434],[-71.5929,42.5443],[-71.5804,42.5502],[-71.5393,42.5429],[-71.5319,42.5202],[-71.5294,42.5193],[-71.5437,42.5002],[-71.5604,42.4748],[-71.5436,42.4666],[-71.5591,42.4121],[-71.5852,42.4071],[-71.6045,42.3975],[-71.5802,42.3871],[-71.6081,42.3707],[-71.6032,42.3675],[-71.6069,42.3616],[-71.61,42.358],[-71.6261,42.3493],[-71.6174,42.3416],[-71.6044,42.3371],[-71.6044,42.3312],[-71.5975,42.3212],[-71.5851,42.3112],[-71.5708,42.3198],[-71.5498,42.3271],[-71.5312,42.3285],[-71.5163,42.3303],[-71.5082,42.3276],[-71.4865,42.3303],[-71.4846,42.3208],[-71.4859,42.3103],[-71.5051,42.2731],[-71.5057,42.2681],[-71.5057,42.2644],[-71.5076,42.2635],[-71.5144,42.2676],[-71.5225,42.2662],[-71.5324,42.2662],[-71.5404,42.2626],[-71.5448,42.2644],[-71.5534,42.2676],[-71.5609,42.2676],[-71.5869,42.2594],[-71.603,42.2171],[-71.5831,42.1949],[-71.572,42.194],[-71.5726,42.1922],[-71.5565,42.1913],[-71.5558,42.1822],[-71.5391,42.1895],[-71.5076,42.1886],[-71.5026,42.1913],[-71.497,42.1663],[-71.4778,42.1654],[-71.4778,42.1568],[-71.4779,42.1318],[-71.5007,42.1177],[-71.5001,42.1141],[-71.5026,42.1118],[-71.4989,42.1036],[-71.4952,42.1014],[-71.4983,42.095],[-71.4983,42.0169],[-71.5366,42.0159],[-71.5588,42.0153],[-71.6681,42.0122],[-71.7979,42.0089],[-71.7991,42.0238],[-71.8856,42.0254],[-71.9436,42.0264],[-71.9696,42.0274],[-71.9763,42.0277],[-72.003,42.0291],[-72.0814,42.0287],[-72.1023,42.0295],[-72.1358,42.0307],[-72.1345,42.162],[-72.1988,42.1535],[-72.2008,42.1612],[-72.2498,42.1787],[-72.2641,42.1836],[-72.263,42.1931],[-72.2649,42.1963],[-72.2607,42.2054],[-72.2417,42.2241],[-72.2208,42.2452],[-72.2171,42.2488],[-72.2103,42.247],[-72.2116,42.2556],[-72.2166,42.2561],[-72.218,42.2697],[-72.213,42.2697],[-72.2119,42.2825],[-72.2039,42.2889],[-72.2033,42.2911],[-72.2108,42.2943],[-72.2164,42.2942],[-72.2164,42.2988],[-72.2121,42.302],[-72.2134,42.3052],[-72.2116,42.3102],[-72.2116,42.3111],[-72.219,42.3101],[-72.2611,42.3035],[-72.2618,42.3053],[-72.2747,42.3021],[-72.28,42.3289],[-72.2769,42.3293],[-72.2782,42.3366],[-72.2813,42.3361],[-72.284,42.352],[-72.2902,42.352],[-72.3013,42.3483],[-72.305,42.3451],[-72.3062,42.3441],[-72.3093,42.3441],[-72.3143,42.3432],[-72.3119,42.3523],[-72.3114,42.3582],[-72.312,42.3627],[-72.3128,42.3736],[-72.3122,42.3791],[-72.3129,42.3832],[-72.313,42.3886],[-72.3149,42.3954],[-72.3131,42.4018],[-72.3095,42.4086],[-72.3077,42.4141],[-72.3058,42.4178],[-72.3022,42.4232],[-72.2979,42.426],[-72.2942,42.4301],[-72.2899,42.4342],[-72.2887,42.4356],[-72.2874,42.437],[-72.2831,42.4411],[-72.2917,42.4796],[-72.2448,42.5135],[-72.2686,42.533],[-72.2706,42.5434],[-72.2765,42.5702],[-72.2772,42.5774],[-72.2747,42.5779],[-72.2666,42.5775],[-72.2616,42.5757],[-72.2669,42.6007],[-72.2631,42.5998],[-72.26,42.6007],[-72.2582,42.6044],[-72.2532,42.6053],[-72.2545,42.6116],[-72.2421,42.6135],[-72.2384,42.614],[-72.2278,42.615],[-72.2272,42.6218],[-72.2297,42.6218],[-72.2291,42.6236],[-72.2316,42.625],[-72.2304,42.6268],[-72.2279,42.6264],[-72.2261,42.6291],[-72.2255,42.6332],[-72.2287,42.6382],[-72.2249,42.6386],[-72.2295,42.6627],[-72.242,42.6617],[-72.2427,42.6694],[-72.257,42.668],[-72.2584,42.6753],[-72.2721,42.6743],[-72.2832,42.7229],[-72.1097,42.7183],[-71.9287,42.713]]]},\"properties\":{\"name\":\"Worcester\",\"state\":\"MA\"}}]}","noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"4f4e49d0e4b07f02db5dae95","contributors":{"authors":[{"text":"Hansen, Bruce P.","contributorId":90727,"corporation":false,"usgs":true,"family":"Hansen","given":"Bruce","email":"","middleInitial":"P.","affiliations":[],"preferred":false,"id":198251,"contributorType":{"id":1,"text":"Authors"},"rank":1},{"text":"Lane, John W. Jr. jwlane@usgs.gov","contributorId":1738,"corporation":false,"usgs":true,"family":"Lane","given":"John","suffix":"Jr.","email":"jwlane@usgs.gov","middleInitial":"W.","affiliations":[{"id":486,"text":"OGW Branch of Geophysics","active":true,"usgs":true}],"preferred":false,"id":198250,"contributorType":{"id":1,"text":"Authors"},"rank":2}]}}
,{"id":24844,"text":"ofr95434 - 1995 - Ground-Water Hydrographs and 5-Year Ground-Water-Level Changes, 1984-93, for Selected Areas In and Adjacent to New Mexico","interactions":[],"lastModifiedDate":"2012-02-10T00:10:07","indexId":"ofr95434","displayToPublicDate":"1994-01-01T00:00:00","publicationYear":"1995","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":"95-434","title":"Ground-Water Hydrographs and 5-Year Ground-Water-Level Changes, 1984-93, for Selected Areas In and Adjacent to New Mexico","docAbstract":"A cooperative observation-well monitoring program was begun in New Mexico in 1925 between the U.S. Geological Survey and the New Mexico State Engineer Office. The majority of the wells are  located in New Mexico; however, a few are in Texas east of Curry and Roosevelt County, New Mexico, and in Colorado along the Rio Grande. The program presently includes 22 wells equipped with continuous water-level recorders and 34 monitoring areas in which selected wells are measured periodically, usually every 5 years, to record changes in ground-water levels. These monitoring areas are those where ground water is used in large quantities for irrigation, municipal, or industrial purposes. Water-level data and water-level changes computed from these data are used to determine areas of ground-water-level rises and declines. This information is necessary for management of ground-water resources in New Mexico.\r\n\r\nIncluded in this report are hydrographs of ground-water levels obtained from 22 wells equipped with continuous water-level recorders and maps of ground-water-level changes computed for a 5-year period in each of 34 monitoring areas. Well locations and ground-water-level data for a 5-year period are listed in tables for each monitoring area. Where available, plots of annual precipitation data for climatological stations within or adjacent to each monitoring area are included.","language":"ENGLISH","publisher":"Geological Survey (U.S.)","doi":"10.3133/ofr95434","issn":"0094-9140","collaboration":"Prepared in cooperation with the New Mexico State Engineer Office","usgsCitation":"Wilkins, D.W., and Garcia, B.M., 1995, Ground-Water Hydrographs and 5-Year Ground-Water-Level Changes, 1984-93, for Selected Areas In and Adjacent to New Mexico: U.S. Geological Survey Open-File Report 95-434, ix, 267 p. **PUBLICATION PAGES ARE IN INCORRECT ORDER**, https://doi.org/10.3133/ofr95434.","productDescription":"ix, 267 p. **PUBLICATION PAGES ARE IN INCORRECT ORDER**","temporalStart":"1984-01-01","temporalEnd":"1993-12-31","costCenters":[{"id":595,"text":"U.S. Geological Survey","active":false,"usgs":true}],"links":[{"id":157125,"rank":0,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/of/1995/0434/report-thumb.jpg"},{"id":53844,"rank":300,"type":{"id":11,"text":"Document"},"url":"https://pubs.usgs.gov/of/1995/0434/report.pdf","linkFileType":{"id":1,"text":"pdf"}}],"geographicExtents":"{ \"type\": \"FeatureCollection\", \"features\": [ { \"type\": \"Feature\", \"properties\": {}, \"geometry\": { \"type\": \"Polygon\", \"coordinates\": [ [ [ -109,31 ], [ -109,37 ], [ -103,37 ], [ -103,31 ], [ -109,31 ] ] ] } } ] }","noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"4f4e4ab0e4b07f02db66d626","contributors":{"authors":[{"text":"Wilkins, D. W.","contributorId":97471,"corporation":false,"usgs":true,"family":"Wilkins","given":"D.","email":"","middleInitial":"W.","affiliations":[],"preferred":false,"id":192672,"contributorType":{"id":1,"text":"Authors"},"rank":1},{"text":"Garcia, Benjamin M.","contributorId":31792,"corporation":false,"usgs":true,"family":"Garcia","given":"Benjamin","email":"","middleInitial":"M.","affiliations":[],"preferred":false,"id":192671,"contributorType":{"id":1,"text":"Authors"},"rank":2}]}}
,{"id":22621,"text":"ofr9276 - 1995 - Ground-water resources of Kings and Queens Counties, Long Island, New York","interactions":[],"lastModifiedDate":"2017-08-30T14:00:14","indexId":"ofr9276","displayToPublicDate":"1994-01-01T00:00:00","publicationYear":"1995","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":"92-76","title":"Ground-water resources of Kings and Queens Counties, Long Island, New York","docAbstract":"<p>The aquifers beneath Kings and Queens Counties supplied an average of more than 120 Mgal/d (million gallons per day) for industrial and public water supply during 1904-47, but this pumping caused saltwater intrusion and a deterioration of water quality that led to the cessation of pumping for public supply in Kings County in 1947 and in western Queens County in 1974. Since the cessation of pumping in Kings and western Queens Counties, ground-water levels have recovered steadily, and the saltwater has partly dispersed and become diluted. In eastern Queens County, where pumpage for public supply averages 60 Mgal/d, all three major aquifers contain a large cone of depression. The saltwater-freshwater interface in the Jameco-Magothy aquifer already extends inland in southeastern Queens County and is moving toward this cone of depression. The pumping centers' proximity to the north shore also warrants monitoring for saltwater intrusion in the Flushing Bay area. </p><p>Urbanization and development on western Long Island since before the tum of this century have caused significant changes in the ground-water budget (total inflow and outflow) and patterns of movement. Some of the major causes are: ( 1) intensive pumping for industrial and public supply; (2) paving of large land-surface areas; (3) installation of a vast network of combined (stonn and sanitary) sewers; (4) leakage from a water-supply-line network that carries more than 750 Mgal/d; and (5) burial of stream channels and extensive wetland areas near the shore.</p><p>Elevated nitrate and chloride concentrations throughout the upper glacial (water-table) aquifer indicate widespread contamination from land surface. Localized contamination in the underlying Jameco-Magothy aquifer is attributed to downward migration in areas of hydraulic connection between aquifers where the Gardiners Clay is absent A channel eroded through the Raritan confining unit provides a pathway for migration of surface contaminants to the Lloyd aquifer sooner than anticipated Although ground water in the Lloyd aquifer is still pristine, present pumping rates and potentiometric levels in the Lloyd indicate that this aquifer is much more sensitive to withdrawals than the other aquifers are and contains an extremely limited water supply. </p>","language":"English","publisher":"U.S. Geological Survey","doi":"10.3133/ofr9276","issn":"0094-9140","usgsCitation":"Buxton, H.T., and Shernoff, P.K., 1995, Ground-water resources of Kings and Queens Counties, Long Island, New York: U.S. Geological Survey Open-File Report 92-76, Report: vi, 111 p. 8 Plates: 24.0 x 24.0 inches or smaller, https://doi.org/10.3133/ofr9276.","productDescription":"Report: vi, 111 p. 8 Plates: 24.0 x 24.0 inches or smaller","costCenters":[],"links":[{"id":260299,"rank":900,"type":{"id":17,"text":"Plate"},"url":"https://pubs.usgs.gov/of/1992/0076/plate-2.pdf"},{"id":260298,"rank":900,"type":{"id":17,"text":"Plate"},"url":"https://pubs.usgs.gov/of/1992/0076/plate-1.pdf"},{"id":260300,"rank":900,"type":{"id":17,"text":"Plate"},"url":"https://pubs.usgs.gov/of/1992/0076/plate-3.pdf"},{"id":260301,"rank":900,"type":{"id":17,"text":"Plate"},"url":"https://pubs.usgs.gov/of/1992/0076/plate-4.pdf"},{"id":260302,"rank":900,"type":{"id":17,"text":"Plate"},"url":"https://pubs.usgs.gov/of/1992/0076/plate-5.pdf"},{"id":260303,"rank":900,"type":{"id":17,"text":"Plate"},"url":"https://pubs.usgs.gov/of/1992/0076/plate-6.pdf"},{"id":260304,"rank":900,"type":{"id":17,"text":"Plate"},"url":"https://pubs.usgs.gov/of/1992/0076/plate-7.pdf"},{"id":260305,"rank":900,"type":{"id":17,"text":"Plate"},"url":"https://pubs.usgs.gov/of/1992/0076/plate-8.pdf"},{"id":260306,"rank":800,"type":{"id":11,"text":"Document"},"url":"https://pubs.usgs.gov/of/1992/0076/report.pdf"},{"id":260307,"rank":0,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/thumbnails/ofr_92_76.jpg"}],"country":"United States","state":"New York","county":"Kings County, Queens County","geographicExtents":"{\"type\":\"FeatureCollection\",\"features\":[{\"type\":\"Feature\",\"geometry\":{\"type\":\"MultiPolygon\",\"coordinates\":[[[[-73.855,40.6511],[-73.8571,40.644],[-73.8666,40.6398],[-73.8723,40.6448],[-73.8691,40.6389],[-73.8828,40.6286],[-73.9015,40.6247],[-73.914,40.6307],[-73.8913,40.6142],[-73.8945,40.6069],[-73.9075,40.6052],[-73.9056,40.6023],[-73.8822,40.6019],[-73.8764,40.5853],[-73.8814,40.5789],[-73.8942,40.5767],[-73.9014,40.5856],[-73.9117,40.5811],[-73.9459,40.5829],[-73.9314,40.5772],[-73.9519,40.5738],[-74.0111,40.5739],[-74.0073,40.5808],[-73.992,40.5794],[-74.012,40.6012],[-74.0321,40.6058],[-74.0418,40.6243],[-74.0345,40.6439],[-74.005,40.6653],[-74.0161,40.6644],[-74.0183,40.6808],[-73.9958,40.7039],[-73.9808,40.7061],[-73.9746,40.7021],[-73.97,40.7072],[-73.9611,40.7417],[-73.936,40.7698],[-73.9354,40.7779],[-73.9272,40.7778],[-73.9094,40.7911],[-73.8941,40.7845],[-73.8889,40.7741],[-73.875,40.7819],[-73.8728,40.785],[-73.8908,40.79],[-73.8892,40.7989],[-73.8683,40.7881],[-73.8699,40.7798],[-73.8554,40.7714],[-73.8611,40.7654],[-73.8471,40.7611],[-73.8434,40.7643],[-73.8504,40.7701],[-73.8508,40.7819],[-73.8576,40.7836],[-73.8522,40.7949],[-73.8407,40.797],[-73.8319,40.7889],[-73.8193,40.8009],[-73.7947,40.795],[-73.7943,40.7903],[-73.7825,40.7907],[-73.7782,40.7969],[-73.7581,40.7677],[-73.7492,40.7817],[-73.7057,40.7499],[-73.7042,40.7358],[-73.7288,40.7239],[-73.7251,40.6517],[-73.741,40.6469],[-73.7442,40.6375],[-73.7656,40.6289],[-73.7714,40.62],[-73.7788,40.6267],[-73.7906,40.6078],[-73.8003,40.6117],[-73.7858,40.6314],[-73.8196,40.6465],[-73.8228,40.6583],[-73.8263,40.649],[-73.8392,40.645],[-73.848,40.6442],[-73.855,40.6511]]],[[[-73.8653,40.6275],[-73.8656,40.6206],[-73.8781,40.6158],[-73.8772,40.6219],[-73.8653,40.6275]]],[[[-74.0144,40.6931],[-74.0122,40.6889],[-74.0256,40.6847],[-74.0144,40.6931]]],[[[-73.7656,40.6142],[-73.7455,40.6121],[-73.7374,40.594],[-73.8211,40.5822],[-73.941,40.5422],[-73.94,40.5539],[-73.9258,40.5618],[-73.8766,40.5698],[-73.8522,40.5814],[-73.8197,40.5872],[-73.7886,40.6031],[-73.7909,40.5964],[-73.7803,40.6089],[-73.7739,40.6058],[-73.7822,40.5981],[-73.7736,40.5986],[-73.769,40.6089],[-73.7725,40.6106],[-73.7656,40.6142]]],[[[-73.8225,40.6367],[-73.8111,40.599],[-73.815,40.6046],[-73.8206,40.5944],[-73.8342,40.595],[-73.8339,40.5886],[-73.8375,40.5894],[-73.8439,40.5931],[-73.8259,40.5999],[-73.82,40.6092],[-73.8378,40.6156],[-73.8336,40.6372],[-73.8261,40.6361],[-73.825,40.6403],[-73.8225,40.6367]]],[[[-73.7994,40.6261],[-73.8035,40.6157],[-73.8068,40.6216],[-73.7994,40.6261]]],[[[-73.7994,40.61],[-73.795,40.605],[-73.8028,40.6039],[-73.7994,40.61]]],[[[-73.8408,40.6124],[-73.8417,40.6041],[-73.8487,40.6055],[-73.8463,40.6124],[-73.8408,40.6124]]],[[[-73.8586,40.6025],[-73.8522,40.5972],[-73.86,40.596],[-73.8586,40.6025]]]]},\"properties\":{\"name\":\"Kings\",\"state\":\"NY\"}}]}","noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"4f4e4ab0e4b07f02db66d4ab","contributors":{"authors":[{"text":"Buxton, Herbert T. hbuxton@usgs.gov","contributorId":1911,"corporation":false,"usgs":true,"family":"Buxton","given":"Herbert","email":"hbuxton@usgs.gov","middleInitial":"T.","affiliations":[{"id":5056,"text":"Office of the AD Energy and Minerals, and Environmental Health","active":true,"usgs":true}],"preferred":true,"id":188585,"contributorType":{"id":1,"text":"Authors"},"rank":1},{"text":"Shernoff, Peter K.","contributorId":104030,"corporation":false,"usgs":true,"family":"Shernoff","given":"Peter","email":"","middleInitial":"K.","affiliations":[],"preferred":false,"id":188586,"contributorType":{"id":1,"text":"Authors"},"rank":2}]}}
,{"id":70221641,"text":"70221641 - 1994 - Geologic, hydrologic, and water-quality data for a multi-aquifer system in Coastal Plain sediments near Millers Pond, Burke County, Georgia, 1992-93","interactions":[],"lastModifiedDate":"2021-06-25T21:35:21.121506","indexId":"70221641","displayToPublicDate":"2021-06-25T16:28:05","publicationYear":"1994","noYear":false,"publicationType":{"id":18,"text":"Report"},"publicationSubtype":{"id":2,"text":"State or Local Government Series"},"seriesTitle":{"id":5595,"text":"Georgia Geologic Survey Information Circular","active":true,"publicationSubtype":{"id":2}},"seriesNumber":"96","title":"Geologic, hydrologic, and water-quality data for a multi-aquifer system in Coastal Plain sediments near Millers Pond, Burke County, Georgia, 1992-93","docAbstract":"<p>No abstract available.</p>","language":"English","publisher":"Georgia Geologic Survey","usgsCitation":"Clarke, J.S., Falls, W.F., Edwards, L.E., Frederiksen, N.O., Bybell, L.M., Gibson, T.G., and Litwin, R.J., 1994, Geologic, hydrologic, and water-quality data for a multi-aquifer system in Coastal Plain sediments near Millers Pond, Burke County, Georgia, 1992-93: Georgia Geologic Survey Information Circular 96, v, 34 p.","productDescription":"v, 34 p.","costCenters":[{"id":243,"text":"Eastern Geology and Paleoclimate Science Center","active":true,"usgs":true}],"links":[{"id":386762,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/thumbnails/outside_thumb.jpg"}],"country":"United States","state":"Georgia","county":"Burke County","otherGeospatial":"Miller's Pond","geographicExtents":"{\n  \"type\": \"FeatureCollection\",\n  \"features\": [\n    {\n      \"type\": \"Feature\",\n      \"properties\": {},\n      \"geometry\": {\n        \"type\": \"Polygon\",\n        \"coordinates\": [\n          [\n            [\n              -81.9854736328125,\n              33.19301824551205\n            ],\n            [\n              -81.84711456298828,\n              33.19301824551205\n            ],\n            [\n              -81.84711456298828,\n              33.296673231834106\n            ],\n            [\n              -81.9854736328125,\n              33.296673231834106\n            ],\n            [\n              -81.9854736328125,\n              33.19301824551205\n            ]\n          ]\n        ]\n      }\n    }\n  ]\n}","noUsgsAuthors":false,"publicationStatus":"PW","contributors":{"authors":[{"text":"Clarke, John S. jsclarke@usgs.gov","contributorId":400,"corporation":false,"usgs":true,"family":"Clarke","given":"John","email":"jsclarke@usgs.gov","middleInitial":"S.","affiliations":[{"id":316,"text":"Georgia Water Science Center","active":true,"usgs":true}],"preferred":true,"id":818315,"contributorType":{"id":1,"text":"Authors"},"rank":1},{"text":"Falls, William F.","contributorId":260648,"corporation":false,"usgs":false,"family":"Falls","given":"William","email":"","middleInitial":"F.","affiliations":[],"preferred":false,"id":818316,"contributorType":{"id":1,"text":"Authors"},"rank":2},{"text":"Edwards, Lucy E. 0000-0003-4075-3317 leedward@usgs.gov","orcid":"https://orcid.org/0000-0003-4075-3317","contributorId":2647,"corporation":false,"usgs":true,"family":"Edwards","given":"Lucy","email":"leedward@usgs.gov","middleInitial":"E.","affiliations":[{"id":243,"text":"Eastern Geology and Paleoclimate Science Center","active":true,"usgs":true},{"id":40020,"text":"Florence Bascom Geoscience Center","active":true,"usgs":true}],"preferred":true,"id":818317,"contributorType":{"id":1,"text":"Authors"},"rank":3},{"text":"Frederiksen, Norman O.","contributorId":50880,"corporation":false,"usgs":true,"family":"Frederiksen","given":"Norman","email":"","middleInitial":"O.","affiliations":[],"preferred":false,"id":818318,"contributorType":{"id":1,"text":"Authors"},"rank":4},{"text":"Bybell, Laurel M. 0000-0002-4760-7542 lbybell@usgs.gov","orcid":"https://orcid.org/0000-0002-4760-7542","contributorId":1760,"corporation":false,"usgs":true,"family":"Bybell","given":"Laurel","email":"lbybell@usgs.gov","middleInitial":"M.","affiliations":[{"id":243,"text":"Eastern Geology and Paleoclimate Science Center","active":true,"usgs":true}],"preferred":true,"id":818319,"contributorType":{"id":1,"text":"Authors"},"rank":5},{"text":"Gibson, Thomas G.","contributorId":25180,"corporation":false,"usgs":true,"family":"Gibson","given":"Thomas","email":"","middleInitial":"G.","affiliations":[],"preferred":false,"id":818320,"contributorType":{"id":1,"text":"Authors"},"rank":6},{"text":"Litwin, Ronald J. 0000-0002-8661-1296 rlitwin@usgs.gov","orcid":"https://orcid.org/0000-0002-8661-1296","contributorId":2478,"corporation":false,"usgs":true,"family":"Litwin","given":"Ronald","email":"rlitwin@usgs.gov","middleInitial":"J.","affiliations":[{"id":40020,"text":"Florence Bascom Geoscience Center","active":true,"usgs":true},{"id":243,"text":"Eastern Geology and Paleoclimate Science Center","active":true,"usgs":true}],"preferred":true,"id":818321,"contributorType":{"id":1,"text":"Authors"},"rank":7}]}}
,{"id":70179033,"text":"70179033 - 1994 - Ground-water hydrology of Ogden Valley and surrounding area, eastern Weber County, UT, and simulation of ground-water flow in the Valley-fill aquifer system","interactions":[],"lastModifiedDate":"2016-12-13T15:32:36","indexId":"70179033","displayToPublicDate":"2016-11-01T00:00:00","publicationYear":"1994","noYear":false,"publicationType":{"id":18,"text":"Report"},"publicationSubtype":{"id":4,"text":"Other Government Series"},"seriesTitle":{"id":294,"text":"Technical Publication","active":false,"publicationSubtype":{"id":4}},"seriesNumber":"99","title":"Ground-water hydrology of Ogden Valley and surrounding area, eastern Weber County, UT, and simulation of ground-water flow in the Valley-fill aquifer system","docAbstract":"<p>The ground-water resources in Ogden Valley, eastern Weber County, Utah, were the subject of a study to provide a better understanding of the hydrologic system in the valley and to estimate the hydrologic effects of future ground-water development. The study area included the drainage basin of the Ogden River upstream from Pineview Reservoir dam and the drainage basin of Wheeler Creek. Ogden Valley and the surrounding area are underlain by rocks that range in age from Precambrian to Quaternary.</p><p>The consolidated rocks that transmit and yield the most water in the area surrounding Ogden Valley are the Paleozoic carbonate rocks and the Wasatch Formation of Tertiary age. Much of the recharge to the consolidated rocks is from snowmelt that infiltrates the Wasatch Formation, which underlies a large part of the study area. Discharge from the consolidated rocks is by streams, evapotranspiration, springs, subsurface outflow, and pumping from wells. Water in the consolidated rocks is a calcium bicarbonate type and has a dissolved-solids concentration of less than 250 milligrams per liter.</p>","language":"English","publisher":"Utah Department of Natural Resources, Division of Water Rights","publisherLocation":"Salt Lake City, UT","collaboration":"Prepared by the United State Geological Survey in cooperation with the Utah Department of Natural Resources Division of Water Rights","usgsCitation":"Avery, C., 1994, Ground-water hydrology of Ogden Valley and surrounding area, eastern Weber County, UT, and simulation of ground-water flow in the Valley-fill aquifer system: Technical Publication 99, vi, 84 p.","productDescription":"vi, 84 p.","numberOfPages":"93","costCenters":[{"id":610,"text":"Utah Water Science Center","active":true,"usgs":true}],"links":[{"id":332079,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/thumbnails/outside_thumb.jpg"},{"id":332077,"rank":1,"type":{"id":15,"text":"Index Page"},"url":"https://www.waterrights.utah.gov/cgi-bin/libview.exe?Modinfo=Viewpub&LIBNUM=20-6-450"},{"id":332078,"rank":2,"type":{"id":11,"text":"Document"},"url":"https://waterrights.utah.gov/docSys/v920/y920/y9200007.pdf"}],"country":"United States","state":"Utah","county":"Weber County","otherGeospatial":"Ogden Valley","geographicExtents":"{\"type\":\"FeatureCollection\",\"features\":[{\"type\":\"Feature\",\"geometry\":{\"type\":\"Polygon\",\"coordinates\":[[[-111.5102,41.4242],[-111.5017,41.4133],[-111.4974,41.4092],[-111.4901,41.4069],[-111.4834,41.4042],[-111.4797,41.4028],[-111.4773,41.4019],[-111.4748,41.4005],[-111.4718,41.3968],[-111.4749,41.3932],[-111.475,41.3851],[-111.467,41.38],[-111.4591,41.3764],[-111.4524,41.3745],[-111.4457,41.3722],[-111.4402,41.3727],[-111.4334,41.3708],[-111.4267,41.3685],[-111.4243,41.3649],[-111.4188,41.3621],[-111.4262,41.3594],[-111.425,41.3513],[-111.4251,41.3472],[-111.4263,41.344],[-111.4312,41.3431],[-111.4331,41.3418],[-111.4386,41.3382],[-111.4399,41.3264],[-111.4418,41.3227],[-111.4473,41.3155],[-111.4437,41.3078],[-111.4407,41.3028],[-111.4383,41.296],[-111.4408,41.2928],[-111.4451,41.286],[-111.4433,41.2815],[-111.4483,41.2756],[-111.4562,41.2733],[-111.4655,41.2634],[-111.4698,41.2566],[-111.4766,41.2512],[-111.4925,41.2422],[-111.4962,41.2327],[-111.5097,41.2318],[-111.5158,41.2323],[-111.5213,41.2318],[-111.5268,41.2341],[-111.5396,41.2401],[-111.5481,41.2392],[-111.5671,41.2402],[-111.5744,41.2397],[-111.5811,41.2407],[-111.589,41.2416],[-111.6044,41.2326],[-111.6068,41.2253],[-111.6087,41.2158],[-111.6131,41.2081],[-111.6192,41.2059],[-111.6357,41.1996],[-111.6443,41.1928],[-111.665,41.1869],[-111.6791,41.1815],[-111.6913,41.1834],[-111.7035,41.1825],[-111.7139,41.188],[-111.7437,41.2062],[-111.7449,41.2134],[-111.7498,41.2153],[-111.7535,41.2148],[-111.7547,41.2116],[-111.7596,41.2094],[-111.773,41.2194],[-111.798,41.2158],[-111.8048,41.214],[-111.8091,41.2081],[-111.8152,41.2045],[-111.8262,41.2036],[-111.8384,41.1991],[-111.8555,41.1986],[-111.8628,41.1909],[-111.8714,41.1887],[-111.8659,41.1819],[-111.8745,41.1692],[-111.8683,41.1651],[-111.8568,41.1578],[-111.8513,41.1533],[-111.8556,41.1474],[-111.8538,41.141],[-111.8574,41.136],[-111.8885,41.1351],[-111.8983,41.1342],[-111.9111,41.1338],[-111.9288,41.1329],[-111.9471,41.1375],[-111.9581,41.1465],[-111.9703,41.1511],[-111.9837,41.1515],[-111.9941,41.1515],[-111.9943,41.3502],[-111.9916,41.3539],[-111.9773,41.3588],[-111.9693,41.3639],[-111.9622,41.3653],[-111.9648,41.3681],[-111.9741,41.3768],[-111.9736,41.3814],[-111.9754,41.3849],[-111.9668,41.3935],[-111.967,41.3974],[-111.9664,41.4097],[-111.9702,41.414],[-111.9711,41.4202],[-111.9622,41.4257],[-111.9566,41.4341],[-111.9501,41.427],[-111.9356,41.4163],[-111.935,41.4162],[-111.9176,41.4117],[-111.9138,41.4147],[-111.9065,41.4176],[-111.8947,41.4201],[-111.893,41.4206],[-111.8847,41.4255],[-111.8836,41.4265],[-111.8708,41.4214],[-111.881,41.4148],[-111.8754,41.4106],[-111.8757,41.4056],[-111.8683,41.3987],[-111.864,41.398],[-111.8557,41.3947],[-111.8441,41.3919],[-111.8337,41.3874],[-111.8171,41.3896],[-111.8116,41.3869],[-111.7975,41.3901],[-111.792,41.391],[-111.7865,41.3873],[-111.7829,41.3814],[-111.7761,41.3769],[-111.759,41.3682],[-111.7523,41.3691],[-111.7351,41.3759],[-111.7249,41.3764],[-111.7268,41.3857],[-111.7058,41.4051],[-111.7062,41.4133],[-111.7185,41.4155],[-111.7238,41.4234],[-111.7215,41.4276],[-111.7073,41.4252],[-111.6957,41.417],[-111.6885,41.4187],[-111.6785,41.4273],[-111.6661,41.4285],[-111.6512,41.4072],[-111.6448,41.4055],[-111.6402,41.4146],[-111.6239,41.4184],[-111.6187,41.4218],[-111.6117,41.4217],[-111.599,41.4208],[-111.5852,41.4179],[-111.5751,41.4277],[-111.5624,41.4233],[-111.5537,41.4242],[-111.5499,41.4141],[-111.5413,41.406],[-111.5377,41.4111],[-111.531,41.4142],[-111.5182,41.4172],[-111.5172,41.4214],[-111.5102,41.4242]]]},\"properties\":{\"name\":\"Weber\",\"state\":\"UT\"}}]}","noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"585116bde4b08138bf1abd5e","contributors":{"authors":[{"text":"Avery, Charles","contributorId":70739,"corporation":false,"usgs":true,"family":"Avery","given":"Charles","affiliations":[],"preferred":false,"id":655828,"contributorType":{"id":1,"text":"Authors"},"rank":1}]}}
,{"id":70038750,"text":"70038750 - 1994 - New uranium-series ages of the Waimanalo Limestone, Oahu, Hawaii: implications for sea level during the last interglacial period","interactions":[],"lastModifiedDate":"2012-07-04T01:02:11","indexId":"70038750","displayToPublicDate":"2012-01-01T14:01:00","publicationYear":"1994","noYear":false,"publicationType":{"id":2,"text":"Article"},"publicationSubtype":{"id":10,"text":"Journal Article"},"seriesTitle":{"id":2667,"text":"Marine Geology","active":true,"publicationSubtype":{"id":10}},"title":"New uranium-series ages of the Waimanalo Limestone, Oahu, Hawaii: implications for sea level during the last interglacial period","docAbstract":"The Waimanalo Formation (limestone) of Oahu has been correlated with the last interglacial period based on U-series dating of corals by T.-L. Ku and colleagues. The limestone consists of growth-position corals and overlying coral conglomerate. An apparent bimodal distribution of ages for the growth-position corals (mean age = 133 ka) and the overlying coral conglomerate (mean age = 119 ka) has been interpreted to represent two distinct high stands of sea that occurred within the last interglacial period. Both growth-position corals and overlying, conglomerate coral occur in an outcrop east of Kaena Point and consist mainly of Pocillopora and Porites. U-seriesages of growth-position corals that show closed-system conditions are 120 &plusmn; 3 ka and 127 &plusmn; 4 ka; overlying conglomerate corals have U-seriesages that range from 120 &plusmn; 3 ka to 138 &plusmn; 4 ka. At Kahe Point, conglomerate corals have ages of 120 &plusmn; 3 ka and 134 &plusmn; 4 ka. These data show that the growth position corals are not systematically older than the conglomerate corals; thus, there is no evidence for two distinct high stands of sea. Waimanalo deposits at Kahe Point and Mokapu Point (new U-seriesages of 134 &plusmn; 4 ka and 127 &plusmn; 3 ka) have beach deposits as high as 12.5 m and, at Mokapu Point, growth-position corals as high as 8.5 m. A last-interglacial sea-level stand of +8.5 to +12.5 m conflicts with estimates of +6 m from a number of tectonically stable coastlines and islands in the western Atlantic Ocean. We infer, therefore, that Oahu may be undergoing uplift at a low rate. This uplift may be due to compensatory lithospheric flexure, because the island of Hawaii has been subsiding throughout much of the Quaternary from volcanic loading. Because of this possible uplift, Oahu and islands like it elsewhere in the Pacific cannot be used as reference points for sealevel during the last interglacial period.","largerWorkType":{"id":2,"text":"Article"},"largerWorkTitle":"Marine Geology","largerWorkSubtype":{"id":10,"text":"Journal Article"},"language":"English","publisher":"Elsevier","publisherLocation":"Amsterdam, Netherlands","doi":"10.1016/0025-3227(94)90091-4","usgsCitation":"Muhs, D., and Szabo, B.J., 1994, New uranium-series ages of the Waimanalo Limestone, Oahu, Hawaii: implications for sea level during the last interglacial period: Marine Geology, v. 118, no. 3-4, p. 315-326, https://doi.org/10.1016/0025-3227(94)90091-4.","productDescription":"12 p.","startPage":"315","endPage":"326","costCenters":[{"id":308,"text":"Geology and Environmental Change Science Center","active":false,"usgs":true}],"links":[{"id":257722,"rank":0,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/thumbnails/outside_thumb.jpg"},{"id":257692,"rank":9999,"type":{"id":10,"text":"Digital Object Identifier"},"url":"https://dx.doi.org/10.1016/0025-3227(94)90091-4","linkFileType":{"id":5,"text":"html"}}],"country":"United States","state":"Hawai'i","otherGeospatial":"O'ahu;Waimanalo Limestone","volume":"118","issue":"3-4","noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"505a6620e4b0c8380cd72d20","contributors":{"authors":[{"text":"Muhs, D.R. 0000-0001-7449-251X","orcid":"https://orcid.org/0000-0001-7449-251X","contributorId":61460,"corporation":false,"usgs":true,"family":"Muhs","given":"D.R.","affiliations":[],"preferred":false,"id":464860,"contributorType":{"id":1,"text":"Authors"},"rank":1},{"text":"Szabo, Barney J.","contributorId":6848,"corporation":false,"usgs":true,"family":"Szabo","given":"Barney","email":"","middleInitial":"J.","affiliations":[],"preferred":false,"id":464859,"contributorType":{"id":1,"text":"Authors"},"rank":2}]}}
,{"id":5222772,"text":"5222772 - 1994 - Reproductive success of barn swallows nesting near a selenium-contaminated lake in east Texas, USA","interactions":[],"lastModifiedDate":"2020-01-27T09:55:40","indexId":"5222772","displayToPublicDate":"2010-06-16T12:17:48","publicationYear":"1994","noYear":false,"publicationType":{"id":2,"text":"Article"},"publicationSubtype":{"id":10,"text":"Journal Article"},"seriesTitle":{"id":1555,"text":"Environmental Pollution","active":true,"publicationSubtype":{"id":10}},"title":"Reproductive success of barn swallows nesting near a selenium-contaminated lake in east Texas, USA","docAbstract":"<p><span>Reproductive success and contaminant levels in 1986 and 1987 were compared between Barn Swallows nesting at selenium-contaminated Martin Lake, Texas, USA, and swallows nesting at a reference site. Nests were initiated about the same time or earlier at Martin Lake than at the reference site and clutch size was similar between the two locations. Nest success was significantly higher at Martin Lake than at the reference site and no embryo or chick deformities were documented. Selenium concentrations in 14 of 20 eggs from Martin Lake were above background (&gt; 3 ppm, dry weight); two of 20 eggs contained &gt; 5 ppm, a concentration associated with a 20% embryo mortality/deformity rate in some bird species. Selenium concentrations in the kidneys of adult swallows were higher at Martin Lake (mean = 14 ppm dry weight) than at the reference site (5·8 ppm). DDE, the only detected organochlorine compound, was in two of 10 eggs from Martin Lake; these concentrations were below those associated with chronic poisoning and reproductive problems. The maximum mercury concentration in livers of adult Barn Swallows (0·83 ppm, dry weight) was within the range for background levels (&gt;5 ppm).</span></p>","language":"English","publisher":"Elsevier","doi":"10.1016/0269-7491(94)90070-1","usgsCitation":"King, K.A., Custer, T., and Weaver, D., 1994, Reproductive success of barn swallows nesting near a selenium-contaminated lake in east Texas, USA: Environmental Pollution, v. 84, no. 1, p. 53-58, https://doi.org/10.1016/0269-7491(94)90070-1.","productDescription":"6 p.","startPage":"53","endPage":"58","numberOfPages":"6","costCenters":[{"id":531,"text":"Patuxent Wildlife Research Center","active":true,"usgs":true}],"links":[{"id":198405,"rank":0,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/thumbnails/outside_thumb.jpg"}],"country":"United States","state":"Texas","otherGeospatial":"Martin Lake","geographicExtents":"{\n  \"type\": \"FeatureCollection\",\n  \"features\": [\n    {\n      \"type\": \"Feature\",\n      \"properties\": {},\n      \"geometry\": {\n        \"type\": \"Polygon\",\n        \"coordinates\": [\n          [\n            [\n              -94.6255874633789,\n              32.17619366706981\n            ],\n            [\n              -94.52499389648438,\n              32.17619366706981\n            ],\n            [\n              -94.52499389648438,\n              32.28568142693891\n            ],\n            [\n              -94.6255874633789,\n              32.28568142693891\n            ],\n            [\n              -94.6255874633789,\n              32.17619366706981\n            ]\n          ]\n        ]\n      }\n    }\n  ]\n}","volume":"84","issue":"1","noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"4f4e4a55e4b07f02db62c797","contributors":{"authors":[{"text":"King, Kirk A.","contributorId":9203,"corporation":false,"usgs":true,"family":"King","given":"Kirk","email":"","middleInitial":"A.","affiliations":[],"preferred":false,"id":337101,"contributorType":{"id":1,"text":"Authors"},"rank":1},{"text":"Custer, T. W. 0000-0003-3170-6519","orcid":"https://orcid.org/0000-0003-3170-6519","contributorId":91802,"corporation":false,"usgs":true,"family":"Custer","given":"T. W.","affiliations":[{"id":531,"text":"Patuxent Wildlife Research Center","active":true,"usgs":true}],"preferred":true,"id":337103,"contributorType":{"id":1,"text":"Authors"},"rank":2},{"text":"Weaver, D.A.","contributorId":33284,"corporation":false,"usgs":true,"family":"Weaver","given":"D.A.","email":"","affiliations":[],"preferred":false,"id":337102,"contributorType":{"id":1,"text":"Authors"},"rank":3}]}}
,{"id":70017861,"text":"70017861 - 1994 - Comparison of drier- to wetter-interval estuarine roof facies in the Eastern and Western Interior coal basins, USA","interactions":[],"lastModifiedDate":"2025-06-04T15:59:45.994554","indexId":"70017861","displayToPublicDate":"2003-04-22T00:00:00","publicationYear":"1994","noYear":false,"publicationType":{"id":2,"text":"Article"},"publicationSubtype":{"id":10,"text":"Journal Article"},"seriesTitle":{"id":2996,"text":"Palaeogeography, Palaeoclimatology, Palaeoecology","printIssn":"0031-0182","active":true,"publicationSubtype":{"id":10}},"title":"Comparison of drier- to wetter-interval estuarine roof facies in the Eastern and Western Interior coal basins, USA","docAbstract":"<p>Many of the Carboniferous coals in the eastern interior of the US are associated with siliciclastic roof facies that were deposited within a fluvio-estuarine transition. These facies include a variety of rhythmites, some of which exhibit tidal cycles. Drier-interval coals (Westphalian B-C, Stephanian) tend to be more laterally restricted and more commonly are associated with paleovalleys. Conversely, wetter-interval coals (Westphalian D) are very widespread and are not restricted to paleovalleys. Throughout the Lake Carboniferous, wet paleoclimates associated with these coals lead to valley incision during sea-level lowstand when large tropical rivers downcut older sediments deposited during previous sea-level highstands. During subsequent rise of sea level, these fluvial valleys were flooded and converted to estuaries where tidal ranges and sedimentation rates were significantly amplified. Based on modern analogs and interpretation of many examples of Carboniferous tidal rhythmites, the localized depositional rates in these settings are exceptionally high. The estuaries became sediment sinks, trapping sediment that is pumped in from both fluvial and marine sources. As a result, sedimentation readily keeps pace with rising baselevel. Extensive intertidal flats and shallow subtidal flats are created and prograde over the valley-confined mires. Thick tidal cycles and upright trees (some with attached foliage) record rapid burial of mires. This model is supported with examples of roof facies from the Westphalian B-C of the Eastern Interior Basin, and the Stephanian of the Western Interior Basin. In these areas facies within each cycle range from well-developed, extensive paleosols and coals, to widespread marine shales or limestones. Variations in both sea level and climate resulted in a complex history of valley fill during which coals could be developed at any time (except during widespread flooding). Minable, low-sulfur and low-ash coals occur, but the coals are relatively thin and discontinuous. Conversely, the Westphalian D coals are very widespread and significant peat accumulations were not confined to paleovalleys. Nonetheless, the lowest sulfur coals are related to rapid deposition of roof facies that occurred within the paleovalley whereas high-sulfur coals were formed in areas of lower sedimentation rate of roof facies that occurred beyond the confines of the paleovalley.&nbsp;</p>","language":"English","publisher":"Elsevier","doi":"10.1016/0031-0182(94)90009-4","issn":"00310182","usgsCitation":"Archer, A., Feldman, H.R., Kvale, E., and Lanier, W.P., 1994, Comparison of drier- to wetter-interval estuarine roof facies in the Eastern and Western Interior coal basins, USA: Palaeogeography, Palaeoclimatology, Palaeoecology, v. 106, no. 1-4, p. 171-185, https://doi.org/10.1016/0031-0182(94)90009-4.","productDescription":"15 p.","startPage":"171","endPage":"185","costCenters":[],"links":[{"id":228490,"rank":1,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/thumbnails/outside_thumb.jpg"}],"country":"United States","state":"Arkansas, Illinois, Indiana, Iowa, Kansas, Kentucky, Missouri, Oklahoma","otherGeospatial":"Eastern and Western Interior coal basins","geographicExtents":"{\n  \"type\": \"FeatureCollection\",\n  \"features\": [\n    {\n      \"type\": \"Feature\",\n      \"properties\": {},\n      \"geometry\": {\n        \"coordinates\": [\n          [\n            [\n              -96.65983661812253,\n              36.32189849509018\n            ],\n            [\n              -86.2378733316447,\n              36.32189849509018\n            ],\n            [\n              -86.2378733316447,\n              41.84957669831883\n            ],\n            [\n              -96.65983661812253,\n              41.84957669831883\n            ],\n            [\n              -96.65983661812253,\n              36.32189849509018\n            ]\n          ]\n        ],\n        \"type\": \"Polygon\"\n      }\n    }\n  ]\n}","volume":"106","issue":"1-4","noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"5059f85de4b0c8380cd4d057","contributors":{"authors":[{"text":"Archer, A.W.","contributorId":8620,"corporation":false,"usgs":true,"family":"Archer","given":"A.W.","affiliations":[],"preferred":false,"id":377779,"contributorType":{"id":1,"text":"Authors"},"rank":1},{"text":"Feldman, H. R.","contributorId":29581,"corporation":false,"usgs":true,"family":"Feldman","given":"H.","email":"","middleInitial":"R.","affiliations":[],"preferred":false,"id":377781,"contributorType":{"id":1,"text":"Authors"},"rank":2},{"text":"Kvale, E.P.","contributorId":76076,"corporation":false,"usgs":true,"family":"Kvale","given":"E.P.","affiliations":[],"preferred":false,"id":377782,"contributorType":{"id":1,"text":"Authors"},"rank":3},{"text":"Lanier, William P.","contributorId":73672,"corporation":false,"usgs":true,"family":"Lanier","given":"William","email":"","middleInitial":"P.","affiliations":[],"preferred":false,"id":377780,"contributorType":{"id":1,"text":"Authors"},"rank":4}]}}
,{"id":70017806,"text":"70017806 - 1994 - Paleoecology of the Fire Clay coal bed in a portion of the Eastern Kentucky Coal Field","interactions":[],"lastModifiedDate":"2025-06-04T16:12:32.694052","indexId":"70017806","displayToPublicDate":"2003-04-22T00:00:00","publicationYear":"1994","noYear":false,"publicationType":{"id":2,"text":"Article"},"publicationSubtype":{"id":10,"text":"Journal Article"},"seriesTitle":{"id":2996,"text":"Palaeogeography, Palaeoclimatology, Palaeoecology","printIssn":"0031-0182","active":true,"publicationSubtype":{"id":10}},"title":"Paleoecology of the Fire Clay coal bed in a portion of the Eastern Kentucky Coal Field","docAbstract":"<p><span>Vertically continuous increment samples of the Fire Clay coal bed (mid-Middle Pennsylvanian, late Westphalian B), collected from a portion of the Central Appalachian Basin, were studied palynologically, petrographically and geochemically in order to partially reconstruct the paleoecology and processes associated with peat formation in the ancient Fire Clay paleomire. Results indicate that four compositional groups can be identified. They are: (1) a&nbsp;</span><i>Lycospora</i><span>—vitrinite dominant group, characterized by high percentages of&nbsp;</span><i>Lycospora</i><span>&nbsp;and vitrinite macerals and generally low, but variable ash yields and sulfur contents; (2) a mixed palynoflora-high vitrinite group that petrographically is similar to group 1 except that it contains a more diverse palynoflora; (3) a mixed palynoflora-moderate/low vitrinite group characterized by various admixtures of lycopsid, fern and calamite miospores, increased percentages of liptinite and inertinite macerals, and low ash yields and sulfur contents; and (4) a mixed palynoflora-high ash yield group characterized by high percentages of small lycopsid, fern, and occasionally calamite and cordaite miospores, high liptinite and inertinite contents, high ash yields, and moderate to high sulfur contents.</span></p><p><span>The Fire Clay coal bed contains a distinctive flint clay parting of probable volcanic origin that naturally divides the bed into two benches. These two benches, (upper and lower), are highly disparte in occurrence, appearance and composition. In the study area the lower bench generally is thin (&lt; 0.5 m), laterally discontinuous and mainly composed of dull (mainly durain) coal lithotypes. Ash yields typically are high; sulfur contents generally are moderate to high. Compositional group 4, the mixed palynoflora—high ash yield group defines all of the increments examined from the lower bench.</span></p><p><span>In contrast, the upper bench is thick (&gt; 0.75 m), laterally continous and mainly comprised of bright (mainly clarain) coal lithotypes. Overall ash yields and sulfur contents for this bench are generally low, although vertical variation is apparent. All of the compositional groups occur in the upper bench; in some columns, notably those that are thick and uninterrupted by clastic partings, groups 1 and 4 often occupy basal coal layers and groups 2 and 3 occur in higher layers. Other columns, especially those taken in areas of thin (&lt; 0.5 m) Fire Clay coal, are dominated by groups 1 and 4.</span></p>","language":"English","publisher":"Elsevier","doi":"10.1016/0031-0182(94)90015-9","issn":"00310182","usgsCitation":"Eble, C., Hower, J., and Andrews, W., 1994, Paleoecology of the Fire Clay coal bed in a portion of the Eastern Kentucky Coal Field: Palaeogeography, Palaeoclimatology, Palaeoecology, v. 106, no. 1-4, p. 287-305, https://doi.org/10.1016/0031-0182(94)90015-9.","productDescription":"19 p.","startPage":"287","endPage":"305","costCenters":[],"links":[{"id":228443,"rank":1,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/thumbnails/outside_thumb.jpg"}],"country":"United States","state":"Kentucky","otherGeospatial":"Eastern Kentucky Coal Field","geographicExtents":"{\n  \"type\": \"FeatureCollection\",\n  \"features\": [\n    {\n      \"type\": \"Feature\",\n      \"properties\": {},\n      \"geometry\": {\n        \"coordinates\": [\n          [\n            [\n              -84.70905950279405,\n              37.89289150405992\n            ],\n            [\n              -84.70905950279405,\n              36.7856367797942\n            ],\n            [\n              -82.8101079120946,\n              36.7856367797942\n            ],\n            [\n              -82.8101079120946,\n              37.89289150405992\n            ],\n            [\n              -84.70905950279405,\n              37.89289150405992\n            ]\n          ]\n        ],\n        \"type\": \"Polygon\"\n      }\n    }\n  ]\n}","volume":"106","issue":"1-4","noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"505a73dbe4b0c8380cd772b2","contributors":{"authors":[{"text":"Eble, C.F.","contributorId":35346,"corporation":false,"usgs":true,"family":"Eble","given":"C.F.","email":"","affiliations":[],"preferred":false,"id":377617,"contributorType":{"id":1,"text":"Authors"},"rank":1},{"text":"Hower, J.C.","contributorId":100541,"corporation":false,"usgs":true,"family":"Hower","given":"J.C.","email":"","affiliations":[],"preferred":false,"id":377619,"contributorType":{"id":1,"text":"Authors"},"rank":2},{"text":"Andrews, W.M. Jr.","contributorId":38303,"corporation":false,"usgs":true,"family":"Andrews","given":"W.M.","suffix":"Jr.","email":"","affiliations":[],"preferred":false,"id":377618,"contributorType":{"id":1,"text":"Authors"},"rank":3}]}}
,{"id":70017617,"text":"70017617 - 1994 - 40Ar/39Ar thermochronologic constraints on the tectonothermal evolution of the northern East Humboldt Range metamorphic core complex, Nevada","interactions":[],"lastModifiedDate":"2025-08-15T15:35:26.949489","indexId":"70017617","displayToPublicDate":"2003-04-02T00:00:00","publicationYear":"1994","noYear":false,"publicationType":{"id":2,"text":"Article"},"publicationSubtype":{"id":10,"text":"Journal Article"},"seriesTitle":{"id":3525,"text":"Tectonophysics","active":true,"publicationSubtype":{"id":10}},"title":"40Ar/39Ar thermochronologic constraints on the tectonothermal evolution of the northern East Humboldt Range metamorphic core complex, Nevada","docAbstract":"<p><span>The northern East Humboldt Range (NEHR) of northeastern Nevada exposes a suite of complexly deformed migmatitic, upper amphibolite-facies rocks in the footwall of the Ruby Mountains-East Humboldt Range (RM-EHR) detachment fault. New&nbsp;</span><sup>40</sup><span>Ar/</span><sup>39</sup><span>Ar data on hornblende, muscovite, biotite, and potassium feldspar help constrain the kinematic and thermal evolution of this terrain during Tertiary extensional exhumation. Hornblende samples from relatively high structural levels yield discordant age spectra that suggest initial cooling during early Tertiary time (63–49 Ma). When coupled with petrological constraints indicating a strongly decompressional&nbsp;</span><i>P-T-t</i><span>&nbsp;path above 550°C, the hornblende data suggest that exhumation of the RM-EHR may have initiated in early Tertiary time, approximately coincident with the initial phases of unroofing in the Wood Hills immediately to the east and with the end of thrusting in the late Mesozoic to early Tertiary Sevier orogenic belt of eastern Nevada and western Utah. This temporal coincidence suggests that gravitational collapse of tectonically thickened crust in the internal zone of the Sevier belt could have driven the initial phases of unroofing.</span></p><p><span>Thermal history during the final stage of exhumation of the NEHR is constrained by discordant hornblende cooling ages of 36-29 Ma from deep structural levels and biotite, muscovite, and potassium feldspar cooling ages of 27-21 Ma from a range of structural levels. Comparison of muscovite, biotite, and potassium feldspar cooling ages with previously published fission-track cooling ages implies very rapid cooling rates at temperatures below the closure temperature for muscovite (270°–350°C), but time gaps of &gt; 7 m.y. between hornblende and mica cooling ages suggest that cooling at higher temperatures was more gradual. In addition, comparison of <sup>40</sup>Ar<sup>39</sup>Ar</span><span>&nbsp;mica cooling ages with previously published fission-track apatite cooling ages suggests pronounced thermal gradients between the NEHR and adjacent areas during latest Oligocene to earliest Miocene time. Such thermal gradients could be readily explained if the RM-EHR detachment fault dipped &gt; 30° between the 300°C and 100°C isotherms. Finally, <sup>40</sup>Ar<sup>39</sup>Ar</span><span id=\"MathJax-Element-2-Frame\" class=\"MathJax_SVG\" data-mathml=\"&lt;math xmlns=&quot;http://www.w3.org/1998/Math/MathML&quot;&gt;&lt;msup&gt;&lt;mi&gt;&lt;/mi&gt;&lt;mn&gt;40&lt;/mn&gt;&lt;/msup&gt;&lt;mtext&gt;Ar&lt;/mtext&gt;&lt;msup&gt;&lt;mi&gt;&lt;/mi&gt;&lt;mn&gt;39&lt;/mn&gt;&lt;/msup&gt;&lt;mtext&gt;Ar&lt;/mtext&gt;&lt;/math&gt;\"></span><span>&nbsp;biotite cooling ages increase southward through the East Humboldt Range, compatible with northward extrapolation of a previously recognized pattern of WNW-younging biotite cooling ages from the Ruby Mountains. A simple model involving the propagation of footwall uplift in the direction of tectonic transport beneath an initially listric normal fault can explain the principle features of the Oligocène to Miocene thermochronologic data set for the RM-EHR.</span></p>","language":"English","publisher":"Elsevier","doi":"10.1016/0040-1951(94)90067-1","issn":"00401951","usgsCitation":"McGrew, A.J., and Snee, L., 1994, 40Ar/39Ar thermochronologic constraints on the tectonothermal evolution of the northern East Humboldt Range metamorphic core complex, Nevada: Tectonophysics, v. 238, no. 1-4, p. 425-450, https://doi.org/10.1016/0040-1951(94)90067-1.","productDescription":"26 p.","startPage":"425","endPage":"450","costCenters":[],"links":[{"id":228938,"rank":1,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/thumbnails/outside_thumb.jpg"}],"country":"United States","state":"Nevada","otherGeospatial":"northern East Humboldt Range","geographicExtents":"{\n  \"type\": \"FeatureCollection\",\n  \"features\": [\n    {\n      \"type\": \"Feature\",\n      \"properties\": {},\n      \"geometry\": {\n        \"coordinates\": [\n          [\n            [\n              -117.76321666030387,\n              42.01049898902764\n            ],\n            [\n              -117.76321666030387,\n              40.617836167615025\n            ],\n            [\n              -114.58273019606733,\n              40.617836167615025\n            ],\n            [\n              -114.58273019606733,\n              42.01049898902764\n            ],\n            [\n              -117.76321666030387,\n              42.01049898902764\n            ]\n          ]\n        ],\n        \"type\": \"Polygon\"\n      }\n    }\n  ]\n}","volume":"238","issue":"1-4","noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"5059e268e4b0c8380cd45b61","contributors":{"authors":[{"text":"McGrew, Allen J.","contributorId":147302,"corporation":false,"usgs":false,"family":"McGrew","given":"Allen","email":"","middleInitial":"J.","affiliations":[],"preferred":false,"id":377034,"contributorType":{"id":1,"text":"Authors"},"rank":1},{"text":"Snee, Lawrence W.","contributorId":81534,"corporation":false,"usgs":true,"family":"Snee","given":"Lawrence W.","affiliations":[],"preferred":false,"id":377035,"contributorType":{"id":1,"text":"Authors"},"rank":2}]}}
,{"id":33086,"text":"wri944026 - 1994 - Multiple flow processes accompanying a dam-break flood in a small upland watershed, Centralia, Washington","interactions":[],"lastModifiedDate":"2014-06-09T13:56:56","indexId":"wri944026","displayToPublicDate":"2002-05-01T00:00:00","publicationYear":"1994","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":"94-4026","title":"Multiple flow processes accompanying a dam-break flood in a small upland watershed, Centralia, Washington","docAbstract":"On October 5, 1991, following 35 consecutive days of dry weather, a 105-meter long, 37-meter wide, 5.2-meter deep concrete-lined watersupply reservoir on a hillside in the eastern edge of Centralia, Washington, suddenly failed, sending 13,250 cubic meters of water rushing down a small, steep tributary channel into the city. Two houses were destroyed, several others damaged, mud and debris were deposited in streets, on lawns, and in basements over four city blocks, and 400 people were evacuated. The cause of failure is believed to have been a sliding failure along a weak seam or joint in the siltstone bedrock beneath the reservoir, possibly triggered by increased seepage into the rock foundation through continued deterioration of concrete panel seams, and a slight rise (0.6 meters) in the pool elevation. A second adjacent reservoir containing 18,900 cubic meters of water also drained, but far more slowly, when a 41-cm diameter connecting pipe was broken by the landslide. The maximum discharge resulting from the dam-failure was about 71 cubic meters per second. A reconstructed hydrograph based on the known reservoir volume and calculated peak discharge indicates the flood duration was about 6.2 minutes. Sedimentologic evidence, high-water mark distribution, and landforms preserved in the valley floor indicate that the dam failure flood consisted of two flow phases: an initial debris flow that deposited coarse bouldery sediment along the slope-area reach as it lost volume, followed soon after by a water-flood that achieved a stage about one-half meter higher than the debris flow. The Centralia dam failure is one of three constructed dams destroyed by rapid foundation failure that defines the upper limits of an envelope curve of peak flood discharge as a function of potential energy for failed constructed dams worldwide.","language":"English","publisher":"U.S. Geological Survey","doi":"10.3133/wri944026","usgsCitation":"Costa, J.E., 1994, Multiple flow processes accompanying a dam-break flood in a small upland watershed, Centralia, Washington: U.S. Geological Survey Water-Resources Investigations Report 94-4026, iv, 24 p., https://doi.org/10.3133/wri944026.","productDescription":"iv, 24 p.","numberOfPages":"24","onlineOnly":"Y","costCenters":[{"id":617,"text":"Volcano Science Center","active":true,"usgs":true}],"links":[{"id":163267,"rank":0,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/thumbnails/wri944026.jpg"},{"id":3287,"rank":100,"type":{"id":15,"text":"Index Page"},"url":"https://pubs.usgs.gov/wri/1994/4026/","linkFileType":{"id":5,"text":"html"}},{"id":288177,"type":{"id":11,"text":"Document"},"url":"https://pubs.usgs.gov/wri/1994/4026/pdf/WRI-94-4026.pdf"}],"country":"United States","state":"Washington","city":"Centralia","geographicExtents":"{ \"type\": \"FeatureCollection\", \"features\": [ { \"type\": \"Feature\", \"properties\": {}, \"geometry\": { \"type\": \"Polygon\", \"coordinates\": [ [ [ -123.0,45.708333 ], [ -123.0,45.75 ], [ -122.916667,45.75 ], [ -122.916667,45.708333 ], [ -123.0,45.708333 ] ] ] } } ] }","noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"4f4e4b32e4b07f02db6b489a","contributors":{"authors":[{"text":"Costa, John E.","contributorId":105743,"corporation":false,"usgs":true,"family":"Costa","given":"John","email":"","middleInitial":"E.","affiliations":[],"preferred":false,"id":209859,"contributorType":{"id":1,"text":"Authors"},"rank":1}]}}
,{"id":6820,"text":"fs07094 - 1994 - Nitrate in ground water in the western Lake Michigan drainage basin, Wisconsin and Michigan","interactions":[],"lastModifiedDate":"2015-09-29T10:07:35","indexId":"fs07094","displayToPublicDate":"1996-10-01T00:00:00","publicationYear":"1994","noYear":false,"publicationType":{"id":18,"text":"Report"},"publicationSubtype":{"id":5,"text":"USGS Numbered Series"},"seriesTitle":{"id":313,"text":"Fact Sheet","code":"FS","onlineIssn":"2327-6932","printIssn":"2327-6916","active":true,"publicationSubtype":{"id":5}},"seriesNumber":"070-94","title":"Nitrate in ground water in the western Lake Michigan drainage basin, Wisconsin and Michigan","docAbstract":"<p>In 1991, the U.S. Geological Survey began the nationwide implementation of the National Water-Quality Assessment (NAWQA) Program. The long-term goals of the NAWQA Program are to describe the status and trends in the quality of a large, representative part of the Nation's surface- and ground-water resources and to provide a sound, scientific understanding of the primary natural and human factors that affect the quality of these resources. The program (as currently planned) consists of 60 study-unit investigations that include parts of most major river basins and aquifer systems in the country. The Western Lake Michigan Drainage Basin encompasses a 20,000-square-mile area in eastern Wisconsin and the Upper Peninsula of Michigan that drains to Lake Michigan and Green Bay (fig. 1).</p>","language":"English","publisher":"U.S. Geological Survey","doi":"10.3133/fs07094","usgsCitation":"Saad, D.A., 1994, Nitrate in ground water in the western Lake Michigan drainage basin, Wisconsin and Michigan: U.S. Geological Survey Fact Sheet 070-94, 2 p., https://doi.org/10.3133/fs07094.","productDescription":"2 p.","numberOfPages":"2","onlineOnly":"N","additionalOnlineFiles":"N","costCenters":[{"id":677,"text":"Wisconsin Water Science Center","active":true,"usgs":true}],"links":[{"id":34158,"rank":300,"type":{"id":11,"text":"Document"},"url":"https://pubs.usgs.gov/fs/1994/0070/report.pdf","linkFileType":{"id":1,"text":"pdf"}},{"id":836,"rank":100,"type":{"id":15,"text":"Index Page"},"url":"https://wi.water.usgs.gov/pubs/FS-070-94/","linkFileType":{"id":5,"text":"html"}},{"id":118350,"rank":0,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/fs/1994/0070/report-thumb.jpg"}],"country":"United States","state":"Michigan, Wisconsin","otherGeospatial":"Lake Michigan","geographicExtents":"{\n  \"type\": \"FeatureCollection\",\n  \"features\": [\n    {\n      \"type\": \"Feature\",\n      \"properties\": {},\n      \"geometry\": {\n        \"type\": \"Polygon\",\n        \"coordinates\": [\n          [\n            [\n              -86.68212890625,\n              45.75219336063106\n            ],\n            [\n              -86.748046875,\n              46.255846818480336\n            ],\n            [\n              -87.69287109375,\n              46.65697731621612\n            ],\n            [\n              -88.099365234375,\n              46.7774927637683\n            ],\n            [\n              -88.29711914062499,\n              46.807579571992385\n            ],\n            [\n              -88.96728515624999,\n              45.29034662473615\n            ],\n            [\n              -89.912109375,\n              43.810747313446996\n            ],\n            [\n              -89.84619140625,\n              43.02071359427862\n            ],\n            [\n              -89.417724609375,\n              42.512601715736665\n            ],\n            [\n              -87.78076171875,\n              42.50450285299051\n            ],\n            [\n              -87.56103515625,\n              42.53689200787317\n            ],\n            [\n              -86.561279296875,\n              45.49094569262732\n            ],\n            [\n              -86.68212890625,\n              45.75219336063106\n            ]\n          ]\n        ]\n      }\n    }\n  ]\n}","noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"4f4e4afee4b07f02db697415","contributors":{"authors":[{"text":"Saad, David A. dasaad@usgs.gov","contributorId":121,"corporation":false,"usgs":true,"family":"Saad","given":"David","email":"dasaad@usgs.gov","middleInitial":"A.","affiliations":[{"id":677,"text":"Wisconsin Water Science Center","active":true,"usgs":true}],"preferred":true,"id":153398,"contributorType":{"id":1,"text":"Authors"},"rank":1}]}}
]}