No abstract available.
","largerWorkType":{"id":24,"text":"Conference Paper"},"largerWorkTitle":"Transport, fate, and effects of silver in the environment: the 2nd international conference proceedings, the University of Wisconsin-Madison, September 11-14, 1994","conferenceTitle":"Transport, fate, and effects of silver in the environment","conferenceDate":"September 11-14, 1994","conferenceLocation":"Madison, WI","language":"English","publisher":"University of Wisconsin","usgsCitation":"Bothner, M., Buchholtz ten Brink, M.R., and Ravizza, G., 1995, Silver and other tracers of sewage particles in coastal and deep sea sediments off the east coast, USA, in Transport, fate, and effects of silver in the environment: the 2nd international conference proceedings, the University of Wisconsin-Madison, September 11-14, 1994, Madison, WI, September 11-14, 1994, p. 61-68.","productDescription":"8 p.","startPage":"61","endPage":"68","onlineOnly":"N","additionalOnlineFiles":"N","costCenters":[{"id":186,"text":"Coastal and Marine Geology Program","active":true,"usgs":true},{"id":678,"text":"Woods Hole Coastal and Marine Science Center","active":true,"usgs":true}],"links":[{"id":296377,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/thumbnails/outside_thumb.jpg"}],"country":"United States","noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"547ee2d0e4b09357f05f8a6f","contributors":{"authors":[{"text":"Bothner, Michael H. mbothner@usgs.gov","contributorId":139855,"corporation":false,"usgs":true,"family":"Bothner","given":"Michael H.","email":"mbothner@usgs.gov","affiliations":[{"id":678,"text":"Woods Hole Coastal and Marine Science Center","active":true,"usgs":true}],"preferred":false,"id":526089,"contributorType":{"id":1,"text":"Authors"},"rank":1},{"text":"Buchholtz ten Brink, Marilyn R.","contributorId":88021,"corporation":false,"usgs":true,"family":"Buchholtz ten Brink","given":"Marilyn","email":"","middleInitial":"R.","affiliations":[{"id":678,"text":"Woods Hole Coastal and Marine Science Center","active":true,"usgs":true}],"preferred":false,"id":526090,"contributorType":{"id":1,"text":"Authors"},"rank":2},{"text":"Ravizza, G.E.","contributorId":105450,"corporation":false,"usgs":true,"family":"Ravizza","given":"G.E.","email":"","affiliations":[{"id":678,"text":"Woods Hole Coastal and Marine Science Center","active":true,"usgs":true}],"preferred":false,"id":526091,"contributorType":{"id":1,"text":"Authors"},"rank":3}]}} ,{"id":70134375,"text":"70134375 - 1995 - East Louisiana continental shelf sediments: a product of delta reworking","interactions":[],"lastModifiedDate":"2014-11-25T15:58:29","indexId":"70134375","displayToPublicDate":"1995-01-01T00:00:00","publicationYear":"1995","noYear":false,"publicationType":{"id":2,"text":"Article"},"publicationSubtype":{"id":10,"text":"Journal Article"},"seriesTitle":{"id":2220,"text":"Journal of Coastal Research","active":true,"publicationSubtype":{"id":10}},"title":"East Louisiana continental shelf sediments: a product of delta reworking","docAbstract":"Data from 77 vibracores were integrated with 6,700 line-km of high- resolution seismic reflection profiles collected off the eastern Louisiana coast in the region of the St. Bernard Delta, the first of the Holocene highstand deltas of the Mississippi River. Seismic fades and sediment facies were integrated in order to establish the stratigraphic details within this relict delta. Results provide a regional geologic framework from which comparisons can be made with other areas. Holocene deposits in the study area overlie a heavily dissected surface interpreted to represent a lowstand erosional surface. Resting on this surface is a thin unit of relatively clean, quartz sand interpreted to have been deposited during early transgression. This unit is overlain by sediments of the St. Bernard Delta, a seaward-prograding, coarsening-upward wedge of sands and muds that contain vertically-stacked units of deltaic succession. Two or more prograding units separated by an unconformity, delineated from regional seismic profiles, may represent laterally shifting subdelta lobes. Surficial sediments consist of a thin unit of sands and muds derived from and reflecting the individual subenvirons of the underlying delta. Holocene inner-shelf development off eastern Louisiana has been controlled by relative sea-level rise and sediment supply. Sediment supply and deposition are a product of delta progradation and delta-lobe switching. The modern shelf configuration and surficial sediment distribution patterns reflect reworking of underlying deltaic deposits. The lack of modern sediment input helps to maintain the imprint of this ancient delta on the modern shelf surface.
","language":"English","publisher":"Coastal Education and Research Foundation","usgsCitation":"Brooks, G.R., Kingdinger, J.L., Penland, S., and Williams, S.J., 1995, East Louisiana continental shelf sediments: a product of delta reworking: Journal of Coastal Research, v. 11, no. 4, p. 1026-1036.","productDescription":"11 p.","startPage":"1026","endPage":"1036","onlineOnly":"N","additionalOnlineFiles":"N","costCenters":[],"links":[{"id":296314,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/thumbnails/outside_thumb.jpg"},{"id":296313,"rank":1,"type":{"id":15,"text":"Index Page"},"url":"https://www.jstor.org/stable/4298408"}],"country":"United States","state":"Louisiana","otherGeospatial":"St . Bernard Delta","volume":"11","issue":"4","noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"5475a830e4b08250614204c6","contributors":{"authors":[{"text":"Brooks, Gregg R.","contributorId":10557,"corporation":false,"usgs":false,"family":"Brooks","given":"Gregg","email":"","middleInitial":"R.","affiliations":[],"preferred":false,"id":525954,"contributorType":{"id":1,"text":"Authors"},"rank":1},{"text":"Kingdinger, Jack L.","contributorId":90655,"corporation":false,"usgs":true,"family":"Kingdinger","given":"Jack","email":"","middleInitial":"L.","affiliations":[],"preferred":false,"id":525955,"contributorType":{"id":1,"text":"Authors"},"rank":2},{"text":"Penland, Shea","contributorId":88401,"corporation":false,"usgs":false,"family":"Penland","given":"Shea","email":"","affiliations":[{"id":5115,"text":"Louisiana State University","active":true,"usgs":false}],"preferred":false,"id":525956,"contributorType":{"id":1,"text":"Authors"},"rank":3},{"text":"Williams, S. Jeffress 0000-0002-1326-7420 jwilliams@usgs.gov","orcid":"https://orcid.org/0000-0002-1326-7420","contributorId":2063,"corporation":false,"usgs":true,"family":"Williams","given":"S.","email":"jwilliams@usgs.gov","middleInitial":"Jeffress","affiliations":[{"id":678,"text":"Woods Hole Coastal and Marine Science Center","active":true,"usgs":true}],"preferred":true,"id":525957,"contributorType":{"id":1,"text":"Authors"},"rank":4}]}} ,{"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":"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.
","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":87317,"text":"87317 - 1995 - Disappearance of the Tarahumara frog","interactions":[{"subject":{"id":87317,"text":"87317 - 1995 - Disappearance of the Tarahumara frog","indexId":"87317","publicationYear":"1995","noYear":false,"title":"Disappearance of the Tarahumara frog"},"predicate":"IS_PART_OF","object":{"id":70148108,"text":"70148108 - 1995 - Our living resources: A report to the nation on the distribution, abundance, and health of U.S. plants, animals, and ecosystems","indexId":"70148108","publicationYear":"1995","noYear":false,"title":"Our living resources: A report to the nation on the distribution, abundance, and health of U.S. plants, animals, and ecosystems"},"id":1}],"isPartOf":{"id":70148108,"text":"70148108 - 1995 - Our living resources: A report to the nation on the distribution, abundance, and health of U.S. plants, animals, and ecosystems","indexId":"70148108","publicationYear":"1995","noYear":false,"title":"Our living resources: A report to the nation on the distribution, abundance, and health of U.S. plants, animals, and ecosystems"},"lastModifiedDate":"2017-04-18T14:53:46","indexId":"87317","displayToPublicDate":"1995-01-01T00:00:00","publicationYear":"1995","noYear":false,"publicationType":{"id":5,"text":"Book chapter"},"publicationSubtype":{"id":24,"text":"Book Chapter"},"title":"Disappearance of the Tarahumara frog","docAbstract":"In the spring of 1983 the last known Tarahumara frog in the United States was found dead. Overall, the species seems to be doing well in Mexico, although the decline of more northern populations are of concern. The Tarahumara frog (Rana tarahumarae) inhabits seasonal and permanent bedrock and bouldery streams in the foothills and main mountain mass of the Sierra Madre Occidental of northwestern Mexico. It ranges from northern Sinaloa, through western Chihuahua and eastern and northern Sonora, and until recently into extreme south-central Arizona (Fig. 1). Arizona localities, all in Santa Cruz County, include three drainages in the Atascosa-Pajarito Mountains (Campbell 1931; Little 1940; Williams 1960) and three in the Santa Rita Mountains (Hale et al. 1977).
","largerWorkType":{"id":4,"text":"Book"},"largerWorkTitle":"Our living resources: A report to the nation on the distribution, abundance, and health of U.S. plants, animals, and ecosystems","largerWorkSubtype":{"id":15,"text":"Monograph"},"language":"English","publisher":"National Biological Service","publisherLocation":"Washington, D.C.","usgsCitation":"Hale, S., Schwalbe, C., Jarchow, J., May, C., Lowe, C., and Johnson, T., 1995, Disappearance of the Tarahumara frog, chap. of Our living resources: A report to the nation on the distribution, abundance, and health of U.S. plants, animals, and ecosystems, p. 138-140.","productDescription":"3 p.","startPage":"138","endPage":"140","costCenters":[{"id":651,"text":"Western Ecological Research Center","active":true,"usgs":true}],"links":[{"id":128205,"rank":0,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/thumbnails/outside_thumb.jpg"},{"id":265981,"type":{"id":11,"text":"Document"},"url":"https://www.webharvest.gov/peth04/20041019015728/https://biology.usgs.gov/s+t/index.htm","linkHelpText":"Archived website"}],"country":"United States","state":"Arizona","noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"4f4e4a82e4b07f02db64ab2b","contributors":{"editors":[{"text":"LaRoe, Edward T.","contributorId":112276,"corporation":false,"usgs":true,"family":"LaRoe","given":"Edward","email":"","middleInitial":"T.","affiliations":[],"preferred":false,"id":504966,"contributorType":{"id":2,"text":"Editors"},"rank":1},{"text":"Farris, Gaye S.","contributorId":84410,"corporation":false,"usgs":true,"family":"Farris","given":"Gaye","email":"","middleInitial":"S.","affiliations":[{"id":455,"text":"National Wetlands Research Center","active":true,"usgs":true}],"preferred":true,"id":504969,"contributorType":{"id":2,"text":"Editors"},"rank":2},{"text":"Puckett, Catherine E. cpuckett@usgs.gov","contributorId":4629,"corporation":false,"usgs":true,"family":"Puckett","given":"Catherine","email":"cpuckett@usgs.gov","middleInitial":"E.","affiliations":[],"preferred":true,"id":504967,"contributorType":{"id":2,"text":"Editors"},"rank":3},{"text":"Doran, Peter D.","contributorId":17533,"corporation":false,"usgs":true,"family":"Doran","given":"Peter","email":"","middleInitial":"D.","affiliations":[],"preferred":false,"id":504968,"contributorType":{"id":2,"text":"Editors"},"rank":4},{"text":"Mac, Michael J.","contributorId":16772,"corporation":false,"usgs":true,"family":"Mac","given":"Michael","email":"","middleInitial":"J.","affiliations":[],"preferred":false,"id":504965,"contributorType":{"id":2,"text":"Editors"},"rank":5}],"authors":[{"text":"Hale, S.F.","contributorId":21104,"corporation":false,"usgs":true,"family":"Hale","given":"S.F.","email":"","affiliations":[],"preferred":false,"id":297647,"contributorType":{"id":1,"text":"Authors"},"rank":1},{"text":"Schwalbe, C.R.","contributorId":35259,"corporation":false,"usgs":false,"family":"Schwalbe","given":"C.R.","email":"","affiliations":[],"preferred":false,"id":297650,"contributorType":{"id":1,"text":"Authors"},"rank":2},{"text":"Jarchow, J.L.","contributorId":95417,"corporation":false,"usgs":true,"family":"Jarchow","given":"J.L.","email":"","affiliations":[],"preferred":false,"id":297652,"contributorType":{"id":1,"text":"Authors"},"rank":3},{"text":"May, C.","contributorId":34854,"corporation":false,"usgs":true,"family":"May","given":"C.","email":"","affiliations":[],"preferred":false,"id":297649,"contributorType":{"id":1,"text":"Authors"},"rank":4},{"text":"Lowe, C.H.","contributorId":60567,"corporation":false,"usgs":true,"family":"Lowe","given":"C.H.","email":"","affiliations":[],"preferred":false,"id":297651,"contributorType":{"id":1,"text":"Authors"},"rank":5},{"text":"Johnson, T.B.","contributorId":21490,"corporation":false,"usgs":true,"family":"Johnson","given":"T.B.","email":"","affiliations":[],"preferred":false,"id":297648,"contributorType":{"id":1,"text":"Authors"},"rank":6}]}} ,{"id":70174186,"text":"70174186 - 1995 - Concentrations of dissolved and particulate Polychlorinated Biphenyls in water from the Saginaw River, Michigan","interactions":[],"lastModifiedDate":"2016-06-28T17:14:13","indexId":"70174186","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":"Concentrations of dissolved and particulate Polychlorinated Biphenyls in water from the Saginaw River, Michigan","docAbstract":"The Saginaw River receives water from a major drainage basin in the east-central portion of the lower peninsula of Michigan. Historically the river has been contaminated with polychlorinated biphenyls (PCBs) from several sources. The present study was conducted to determine the concentrations of PCBs in both the dissolved and particulate phases of water in the lower Saginaw River, as well as the relative contribution of PCBs from the lower portion of the river relative to more upstream locations. Water samples were collected in 1990–1991, during a range of discharge conditions. Suspended particulates were collected from water onto glass-fiber filters by use of a “Penta-plate” filtration apparatus. Filtered water was subsequently passed through XAD-2 macroreticular resin to collect the “dissolved” PCBs. Concentrations of PCBs in both phases were determined by congener specific gas chromatography with electron capture detection. Total concentrations of PCBs ranged from 11 to 31 ng/L. The concentrations of PCBs in the dissolved phase ranged from 1.9 to 16 ng/L. The ratio of total PCBs bound to suspended particulates, relative to dissolved PCBs, was 2:1 and remained fairly constant for discharges less than approximately 400 M3/sec. The loading of total PCBs to Saginaw Bay was estimated to be 225 kg/yr, of which approximately 60% was found to be contributed by the lower 8 km of the Saginaw River.
","language":"English","publisher":"Elsevier","doi":"10.1016/S0380-1330(95)71033-4","usgsCitation":"Verbrugge, D.A., Giesy, J.P., Mora, M.A., Williams, L.L., Rossmann, R., Moll, R.A., and Tuchman, M., 1995, Concentrations of dissolved and particulate Polychlorinated Biphenyls in water from the Saginaw River, Michigan: Journal of Great Lakes Research, v. 21, no. 2, p. 219-233, https://doi.org/10.1016/S0380-1330(95)71033-4.","productDescription":"15 p.","startPage":"219","endPage":"233","onlineOnly":"N","additionalOnlineFiles":"N","costCenters":[{"id":192,"text":"Columbia Environmental Research Center","active":true,"usgs":true}],"links":[{"id":324581,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/thumbnails/outside_thumb.jpg"}],"country":"United States","state":"Michigan","otherGeospatial":"Saginaw River","geographicExtents":"{\n \"type\": \"FeatureCollection\",\n \"features\": [\n {\n \"type\": \"Feature\",\n \"properties\": {},\n \"geometry\": {\n \"type\": \"Polygon\",\n \"coordinates\": [\n [\n [\n -83.86276245117188,\n 43.64899449575356\n ],\n [\n -83.8641357421875,\n 43.62712937016884\n ],\n [\n -83.90945434570312,\n 43.60724507891402\n ],\n [\n -83.91220092773438,\n 43.57044180598564\n ],\n [\n -83.91357421875,\n 43.534611617432816\n ],\n [\n -83.92868041992188,\n 43.49079023700749\n ],\n [\n -83.94378662109375,\n 43.43995745973526\n ],\n [\n -83.97674560546875,\n 43.401056495052906\n ],\n [\n -84.03854370117188,\n 43.375108633273086\n ],\n [\n -84.07699584960938,\n 43.3481510201783\n ],\n [\n -84.10171508789062,\n 43.315186560290485\n ],\n [\n -84.06875610351562,\n 43.3101903843356\n ],\n [\n -84.00421142578125,\n 43.35414263600892\n ],\n [\n -83.93966674804688,\n 43.392075799933046\n ],\n [\n -83.90808105468749,\n 43.45391581188941\n ],\n [\n -83.86825561523438,\n 43.51668853502909\n ],\n [\n -83.8861083984375,\n 43.55451990763498\n ],\n [\n -83.85452270507812,\n 43.605256288140474\n ],\n [\n -83.83392333984375,\n 43.624147145668076\n ],\n [\n -83.83804321289061,\n 43.652969118285434\n ],\n [\n -83.86276245117188,\n 43.64899449575356\n ]\n ]\n ]\n }\n }\n ]\n}","volume":"21","issue":"2","noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"57739faee4b07657d1a90cb4","contributors":{"authors":[{"text":"Verbrugge, David A.","contributorId":172542,"corporation":false,"usgs":false,"family":"Verbrugge","given":"David","email":"","middleInitial":"A.","affiliations":[],"preferred":false,"id":641185,"contributorType":{"id":1,"text":"Authors"},"rank":1},{"text":"Giesy, John P.","contributorId":57426,"corporation":false,"usgs":true,"family":"Giesy","given":"John","email":"","middleInitial":"P.","affiliations":[],"preferred":false,"id":641186,"contributorType":{"id":1,"text":"Authors"},"rank":2},{"text":"Mora, Miguel A. 0000-0002-8393-0216","orcid":"https://orcid.org/0000-0002-8393-0216","contributorId":46643,"corporation":false,"usgs":true,"family":"Mora","given":"Miguel","email":"","middleInitial":"A.","affiliations":[],"preferred":false,"id":641187,"contributorType":{"id":1,"text":"Authors"},"rank":3},{"text":"Williams, Lisa L.","contributorId":172543,"corporation":false,"usgs":false,"family":"Williams","given":"Lisa","email":"","middleInitial":"L.","affiliations":[],"preferred":false,"id":641188,"contributorType":{"id":1,"text":"Authors"},"rank":4},{"text":"Rossmann, Ronald","contributorId":149112,"corporation":false,"usgs":false,"family":"Rossmann","given":"Ronald","email":"","affiliations":[{"id":17646,"text":"U. S. Environmental Protection Agency, Grosse Ile, MI","active":true,"usgs":false}],"preferred":false,"id":641189,"contributorType":{"id":1,"text":"Authors"},"rank":5},{"text":"Moll, Russell A.","contributorId":172544,"corporation":false,"usgs":false,"family":"Moll","given":"Russell","email":"","middleInitial":"A.","affiliations":[],"preferred":false,"id":641190,"contributorType":{"id":1,"text":"Authors"},"rank":6},{"text":"Tuchman, Marc","contributorId":50118,"corporation":false,"usgs":true,"family":"Tuchman","given":"Marc","affiliations":[],"preferred":false,"id":641191,"contributorType":{"id":1,"text":"Authors"},"rank":7}]}} ,{"id":70019170,"text":"70019170 - 1995 - Superposed local and regional paleostresses: fault-slip analysis of Neogene extensional faulting near coeval caldera complexes, Yucca Flat, Nevada","interactions":[],"lastModifiedDate":"2024-04-25T12:08:32.54356","indexId":"70019170","displayToPublicDate":"1995-01-01T00:00:00","publicationYear":"1995","noYear":false,"publicationType":{"id":2,"text":"Article"},"publicationSubtype":{"id":10,"text":"Journal Article"},"seriesTitle":{"id":2312,"text":"Journal of Geophysical Research","active":true,"publicationSubtype":{"id":10}},"title":"Superposed local and regional paleostresses: fault-slip analysis of Neogene extensional faulting near coeval caldera complexes, Yucca Flat, Nevada","docAbstract":"Numerous reduced stress tensors are computed by multiple inversions of 906 temporally and spatially partitioned fault-slip data from the Yucca Flat region in the southwest Nevada volcanic field to constrain the Neogene paleostress and faulting history and to investigate how the regional tectonic stress field was affected by local caldera magmatism. Perturbed, shallow (<400 m), pre-11 Ma paleostress configurations, determined west and northwest of present (post-11 Ma) Yucca Flat basin, existed during mild extensional faulting and are attributed to superposition of transient caldera-magmatic stresses on the regional stress field. Northwest of Yucca Flat a progressive shift in least principal stress (σ3) directions near known calderas located 5–15 km to the west occurred under a normal-slip stress state during caldera development between about 15 and 13 Ma. A brief (∼0.5 m.y.) change to a strike-slip stress state occurred at about 13 Ma and was accompanied by small-offset, quasi-conjugate strike-slip faulting. This stress state was most distinct, relative to a normal-slip state, near calderas where stress solutions and fault relations indicate closer affinities to a reverse-slip state. Inferred 11.6–11.45 Ma paleostress tensors indicate radial tension associated with either initial caldera collapse or local post-collapse topographic modification of the stress field. Post-11 Ma normal-slip stress tensors are associated with normal- and oblique-slip faults that accommodated subsidence and eastward extension of Yucca Flat basin away from the caldera complexes. These tensors do not indicate stress modifications due to residual caldera-related effects and thus were used to infer post-11 Ma regional stress changes. The stress field has rotated as much as 65° clockwise since 11 Ma during extensional development of Yucca Flat basin, with most of the rotation and extension occurring before about 8.5 Ma. Results suggest that shallow magmatism and caldera development can strongly alter extensional tectonic stress fields, fault patterns, and slip directions in the uppermost crust out to distances of roughly two magma chamber radii away from a magma body.
Winter mean 700 millibar (700 mb) height anomalies, representing the average atmospheric circulation during the snow season, were compared with annual streamflow measured at 140 stream gauges in the western United States. Correlation analysis was used to identify relations between winter mean atmospheric circulation and annual streamflow, and to quantify the degree to which the temporal variability in annual streamflow can be attributed to variations in winter mean atmospheric circulation. Results indicate that winter mean 700 mb height anomalies account for a statistically significant portion of the temporal variability in annual streamflow in the western United States. In general, above-average annual streamflow is associated with negative winter mean 700 mb height anomalies over the eastern North Pacific Ocean and/or the western United States. These anomalies are indicative of anomalous cyclonic circulation which is associated with an anomalous flow of moist air from the eastern North Pacific Ocean into the western United States that increases winter precipitation and snowpack accumulations, and subsequently streamflow. Below-average annual streamflow is associated with positive 700 mb height anomalies over the eastern North Pacific Ocean and/or the western United States. These positive anomalies indicate anomalous anticyclonic circulation which prevents the intrusion of moist air from the eastern North Pacific Ocean into the western United States, increases subsidence, decreases winter precipitation, and results in decreased streamflow. Results also indicate that long-term trends in annual streamflow are related to long-term trends in winter mean 700 mb height anomalies.
","language":"English","publisher":"Inter-Research Science Publisher","doi":"10.3354/cr005139","usgsCitation":"McCabe, G.J., 1995, Relations between winter atmospheric circulation and annual streamflow in the western United States: Climate Research, v. 5, no. 2, p. 139-148, https://doi.org/10.3354/cr005139.","productDescription":"10 p.","startPage":"139","endPage":"148","numberOfPages":"10","costCenters":[],"links":[{"id":479243,"rank":2,"type":{"id":40,"text":"Open Access Publisher Index Page"},"url":"https://doi.org/10.3354/cr005139","text":"Publisher Index Page"},{"id":226438,"rank":1,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/thumbnails/outside_thumb.jpg"}],"country":"United States","otherGeospatial":"western United States","geographicExtents":"{\n \"type\": \"FeatureCollection\",\n \"features\": [\n {\n \"type\": \"Feature\",\n \"properties\": {},\n \"geometry\": {\n \"coordinates\": [\n [\n [\n -101.86697952785629,\n 49.734462939159926\n ],\n [\n -123.78548509076228,\n 49.734462939159926\n ],\n [\n -123.78548509076228,\n 32.67374352182759\n ],\n [\n -101.86697952785629,\n 32.67374352182759\n ],\n [\n -101.86697952785629,\n 49.734462939159926\n ]\n ]\n ],\n \"type\": \"Polygon\"\n }\n }\n ]\n}","volume":"5","issue":"2","noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"50e4a707e4b0e8fec6cdc34b","contributors":{"authors":[{"text":"McCabe, G. J. Jr.","contributorId":77551,"corporation":false,"usgs":true,"family":"McCabe","given":"G.","suffix":"Jr.","email":"","middleInitial":"J.","affiliations":[],"preferred":false,"id":380982,"contributorType":{"id":1,"text":"Authors"},"rank":1}]}} ,{"id":70018925,"text":"70018925 - 1995 - Sediment resuspension mechanisms in Old Tampa Bay, Florida","interactions":[],"lastModifiedDate":"2023-10-03T15:12:47.938555","indexId":"70018925","displayToPublicDate":"1995-01-01T00:00:00","publicationYear":"1995","noYear":false,"publicationType":{"id":2,"text":"Article"},"publicationSubtype":{"id":10,"text":"Journal Article"},"seriesTitle":{"id":1587,"text":"Estuarine, Coastal and Shelf Science","active":true,"publicationSubtype":{"id":10}},"title":"Sediment resuspension mechanisms in Old Tampa Bay, Florida","docAbstract":"The mechanisms that resuspend bottom sediments in Old Tampa Bay, a shallow, microtidal, subtropical estuary in west-central Florida, were determined by analysing data collected during several periods from 1988 to 1990. Hydrodynamic and suspended-solids concentration data were collected at a relatively deep (4 m) site where a permanent platform was built and at a relatively shallow (1·5 m) site where a submersible instrument package was deployed. Bottom sediments were non-cohesive silts and fine sands. The primary sediment resuspension mechanism at both sites was wind waves, which were generated by strong and sustained winds associated with winter storms and tropical storms. At the platform, waves were depth-transitional, and estimated bottom shear stresses were most sensitive to wave period and water depth. Concentrations of suspended solids at this site corresponded well with wave motion, and non-linear wave-current interaction was small. At the shallow-water site, concentrations of suspended solids were elevated during periods of strong north-easterly winds and large bottom orbital velocities. At both sites, wind direction was an important factor in determining the occurrence and magnitude of sediment resuspension. Resuspended sediments settled within several hours as storm intensity diminished. Winds and waves generated by thunderstorms were more transient than those generated by winter storms and tropical storms. Based on the data collected during this study, thunderstorms are less likely to resuspend bottom sediment than winter storms and tropical storms. Maximum tidal currents at the study sites are usually less than 15 cm s−1and did not increase observed concentrations of suspended solids.
","language":"English","publisher":"Elsevier","doi":"10.1006/ecss.1995.0041","usgsCitation":"Schoellhamer, D., 1995, Sediment resuspension mechanisms in Old Tampa Bay, Florida: Estuarine, Coastal and Shelf Science, v. 40, no. 6, p. 603-620, https://doi.org/10.1006/ecss.1995.0041.","productDescription":"18 p.","startPage":"603","endPage":"620","costCenters":[],"links":[{"id":226483,"rank":1,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/thumbnails/outside_thumb.jpg"}],"country":"United States","state":"Florida","otherGeospatial":"Old Tampa Bay","geographicExtents":"{\n \"type\": \"FeatureCollection\",\n \"features\": [\n {\n \"type\": \"Feature\",\n \"properties\": {},\n \"geometry\": {\n \"coordinates\": [\n [\n [\n -82.52908503011928,\n 27.842463075881383\n ],\n [\n -82.53898569165497,\n 27.84871611869343\n ],\n [\n -82.5382785015456,\n 27.861221122682508\n ],\n [\n -82.52625626968052,\n 27.876225223280002\n ],\n [\n -82.5276706498999,\n 27.882476318607175\n ],\n [\n -82.52696345979052,\n 27.91060178169785\n ],\n [\n -82.52201312902235,\n 27.933721685430825\n ],\n [\n -82.5361569312162,\n 27.946841593082354\n ],\n [\n -82.54747197297196,\n 27.966830768749787\n ],\n [\n -82.55030073341075,\n 27.97370119293504\n ],\n [\n -82.57222362681155,\n 27.983693756137043\n ],\n [\n -82.59202494988297,\n 27.983693756137043\n ],\n [\n -82.61182627295506,\n 27.99430984001468\n ],\n [\n -82.60758313229692,\n 28.00430049329593\n ],\n [\n -82.61324065317443,\n 28.011792875347226\n ],\n [\n -82.62314131471015,\n 28.02178190736211\n ],\n [\n -82.64223544767222,\n 28.029273073214696\n ],\n [\n -82.64860015865976,\n 28.02178190736211\n ],\n [\n -82.65991520041484,\n 28.01928473623147\n ],\n [\n -82.65991520041484,\n 28.006798011881486\n ],\n [\n -82.66415834107302,\n 28.016787507183167\n ],\n [\n -82.66132958063424,\n 28.031770012640706\n ],\n [\n -82.67971652348695,\n 28.03863629732622\n ],\n [\n -82.68537404436448,\n 28.033642679190493\n ],\n [\n -82.69881065644897,\n 28.044877994058297\n ],\n [\n -82.70446817732655,\n 28.042381358826475\n ],\n [\n -82.69456751579084,\n 28.026151817466484\n ],\n [\n -82.68820280480325,\n 28.018036128946818\n ],\n [\n -82.68537404436448,\n 28.008671112823237\n ],\n [\n -82.67971652348695,\n 28.00430049329593\n ],\n [\n -82.69173875535208,\n 27.989314166059003\n ],\n [\n -82.70800412787536,\n 27.9818202210579\n ],\n [\n -82.70871131798471,\n 27.976199420527166\n ],\n [\n -82.69951784655835,\n 27.976199420527166\n ],\n [\n -82.70729693776532,\n 27.964956940772822\n ],\n [\n -82.71366164875289,\n 27.961833821840997\n ],\n [\n -82.72639107072739,\n 27.956211980026808\n ],\n [\n -82.73063421138552,\n 27.944342685903422\n ],\n [\n -82.73275578171491,\n 27.929348028825274\n ],\n [\n -82.71649040919168,\n 27.929348028825274\n ],\n [\n -82.69951784655835,\n 27.918725554506295\n ],\n [\n -82.69244594546143,\n 27.919350434829852\n ],\n [\n -82.67405900260938,\n 27.90747709121173\n ],\n [\n -82.65496486964736,\n 27.904352310468497\n ],\n [\n -82.65001453887915,\n 27.887476935083313\n ],\n [\n -82.63516354657527,\n 27.88310140829614\n ],\n [\n -82.62738445536831,\n 27.88310140829614\n ],\n [\n -82.6174837938326,\n 27.875600093904765\n ],\n [\n -82.619605364162,\n 27.865597533300388\n ],\n [\n -82.60333999163875,\n 27.860595906739533\n ],\n [\n -82.60192561141936,\n 27.845589642350276\n ],\n [\n -82.592732139993,\n 27.829330512698263\n ],\n [\n -82.52908503011928,\n 27.842463075881383\n ]\n ]\n ],\n \"type\": \"Polygon\"\n }\n }\n ]\n}","volume":"40","issue":"6","noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"505b89bae4b08c986b316e7b","contributors":{"authors":[{"text":"Schoellhamer, D. H. 0000-0001-9488-7340","orcid":"https://orcid.org/0000-0001-9488-7340","contributorId":85624,"corporation":false,"usgs":true,"family":"Schoellhamer","given":"D. H.","affiliations":[],"preferred":false,"id":381112,"contributorType":{"id":1,"text":"Authors"},"rank":1}]}} ,{"id":70019571,"text":"70019571 - 1995 - Structural controls of Holocene reactivation of the Meers fault, southwestern Oklahoma, from magnetic studies","interactions":[],"lastModifiedDate":"2023-12-23T15:30:42.123685","indexId":"70019571","displayToPublicDate":"1995-01-01T00:00:00","publicationYear":"1995","noYear":false,"publicationType":{"id":2,"text":"Article"},"publicationSubtype":{"id":10,"text":"Journal Article"},"seriesTitle":{"id":1786,"text":"Geological Society of America Bulletin","active":true,"publicationSubtype":{"id":10}},"title":"Structural controls of Holocene reactivation of the Meers fault, southwestern Oklahoma, from magnetic studies","docAbstract":"Holocene reactivation of the aseismic Meers fault in southwestern Oklahoma illustrates the limitation of using the historical seismic record for identifying hazardous faults in the central United States. The 26- to 37-km-long fault scarp is one of the few known scamps recording Holocene movement in the central and eastern United States. Two documented late Holocene slip events, each with about 2.5 m of net slip and estimated Ms ranging from 6¾ to 7¼, identify the Meers fault as a potentially hazardous fault.
During Carboniferous and Early Permian tectonism, the Meers fault displaced rocks of sharply contrasting magnetic properties. Analysis of aeromagnetic data and twelve ground-magnetic profiles provides a detailed look at the fault within the magnetic basement. Because subsequent reactivation has been minor and of an opposite sense, the pronounced magnetic anomaly associated with the Meers fault reflects Paleozoic structures in the magnetic basement. The location of the Holocene fault scarp corresponds to the strong horizontal magnetic gradient caused by Paleozoic offset of magnetic basement, indicating that the Paleozoic fault controlled Holocene displacement. Two features apparent in both sets of magnetic data are splays of the Meers fault northwest of the Holocene scarp and dikelike bodies immediately south of the fault.
Magnetic susceptibility measurements and rock magnetic data from unoriented core penetrating a dikelike body were incorporated into models of the ground-magnetic profiles. In most cases, secondary faults mapped or visible on low-sun-angle photographs correspond to faults modeled from magnetic data. This correlation shows that preexisting structures probably controlled secondary faulting. However, secondary faults at the southeastern end of the 26-km long continuous fault scarp, previously interpreted from low-sun-angle photography, are not apparent in the magnetic data.
Of importance to seismic hazard evaluation, the magnetic models show that the northwestern splays probably begin at the northwestern end of the reactivated segment and may indicate a persistent rupture propagation barrier to the west. In addition, the models show the dip of the Meers fault to be nearly vertical to about 0.5 km depth. This dip is consistent with the nearly straight fault trace, results of trenching studies, interpretation of shallow seismicreflection data, and regional gravity and aeromagnetic models. In the present-day strike-slip regional stress field, the observed up-to-the-north Holocene displacement suggests that either the fault continues to dip steeply at depth or the regional stress field is approaching a normal-faulting stress regime. If the former is true, the scarcity of near-vertical faults with similar orientation within the area of the southern Oklahoma aulacogen implies that few are likely candidates for reactivation.
","language":"English","publisher":"Geological Society of America","doi":"10.1130/0016-7606(1995)107<0098:SCOHRO>2.3.CO;2","usgsCitation":"Jones-Cecil, M., 1995, Structural controls of Holocene reactivation of the Meers fault, southwestern Oklahoma, from magnetic studies: Geological Society of America Bulletin, v. 107, no. 1, p. 98-112, https://doi.org/10.1130/0016-7606(1995)107<0098:SCOHRO>2.3.CO;2.","productDescription":"15 p.","startPage":"98","endPage":"112","numberOfPages":"15","costCenters":[],"links":[{"id":227920,"rank":1,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/thumbnails/outside_thumb.jpg"}],"volume":"107","issue":"1","noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"505b9bdae4b08c986b31d11a","contributors":{"authors":[{"text":"Jones-Cecil, M.","contributorId":33471,"corporation":false,"usgs":true,"family":"Jones-Cecil","given":"M.","affiliations":[],"preferred":false,"id":383205,"contributorType":{"id":1,"text":"Authors"},"rank":1}]}} ,{"id":85339,"text":"85339 - 1995 - Migratory bird population changes in North Dakota","interactions":[{"subject":{"id":85339,"text":"85339 - 1995 - Migratory bird population changes in North Dakota","indexId":"85339","publicationYear":"1995","noYear":false,"title":"Migratory bird population changes in North Dakota"},"predicate":"IS_PART_OF","object":{"id":70148108,"text":"70148108 - 1995 - Our living resources: A report to the nation on the distribution, abundance, and health of U.S. plants, animals, and ecosystems","indexId":"70148108","publicationYear":"1995","noYear":false,"title":"Our living resources: A report to the nation on the distribution, abundance, and health of U.S. plants, animals, and ecosystems"},"id":1}],"isPartOf":{"id":70148108,"text":"70148108 - 1995 - Our living resources: A report to the nation on the distribution, abundance, and health of U.S. plants, animals, and ecosystems","indexId":"70148108","publicationYear":"1995","noYear":false,"title":"Our living resources: A report to the nation on the distribution, abundance, and health of U.S. plants, animals, and ecosystems"},"lastModifiedDate":"2017-12-27T11:30:03","indexId":"85339","displayToPublicDate":"1995-01-01T00:00:00","publicationYear":"1995","noYear":false,"publicationType":{"id":5,"text":"Book chapter"},"publicationSubtype":{"id":24,"text":"Book Chapter"},"title":"Migratory bird population changes in North Dakota","docAbstract":"The status of migratory bird populations in North America has received increased attention in recent years. Much of this consideration has been on Neotropical migrants, especially those associated with eastern forests. The status of migratory bird populations in the Great Plains has received far less attention. During the past quarter-century, populations of many species of birds that breed in the northern Great Plains have increased or declined, as indicated by trends from the North American Breeding Bird Survey.
In 1967 Stewart and Kantrud (1972) conducted a survey of breeding bird populations throughout North Dakota. This study offered a rare glimpse of bird populations breeding in the northern Great Plains as well as important baseline data on breeding bird populations. These data help us evaluate relationships between birds and habitat conditions. We repeated the survey to compare bird populations in North Dakota during 1967 with those in 1992 and 1993.
","largerWorkType":{"id":4,"text":"Book"},"largerWorkTitle":"Our living resources: A report to the nation on the distribution, abundance, and health of U.S. plants, animals, and ecosystems","largerWorkSubtype":{"id":15,"text":"Monograph"},"language":"English","publisher":"National Biological Service","publisherLocation":"Washington, D.C.","usgsCitation":"Igl, L.D., and Johnson, D.H., 1995, Migratory bird population changes in North Dakota, chap. of Our living resources: A report to the nation on the distribution, abundance, and health of U.S. plants, animals, and ecosystems, p. 298-300.","productDescription":"3 p.","startPage":"298","endPage":"300","costCenters":[{"id":480,"text":"Northern Prairie Wildlife Research Center","active":true,"usgs":true}],"links":[{"id":127761,"rank":0,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/thumbnails/outside_thumb.jpg"},{"id":339916,"rank":2,"type":{"id":11,"text":"Document"},"url":"https://www.webharvest.gov/peth04/20041019015728/https://biology.usgs.gov/s+t/index.htm","linkHelpText":"Archived website"}],"country":"United States","state":"North Dakota","noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"4f4e4a60e4b07f02db6355a0","contributors":{"editors":[{"text":"LaRoe, Edward T.","contributorId":112276,"corporation":false,"usgs":true,"family":"LaRoe","given":"Edward","email":"","middleInitial":"T.","affiliations":[],"preferred":false,"id":504422,"contributorType":{"id":2,"text":"Editors"},"rank":1},{"text":"Farris, Gaye S.","contributorId":84410,"corporation":false,"usgs":true,"family":"Farris","given":"Gaye","email":"","middleInitial":"S.","affiliations":[{"id":455,"text":"National Wetlands Research Center","active":true,"usgs":true}],"preferred":true,"id":504425,"contributorType":{"id":2,"text":"Editors"},"rank":2},{"text":"Puckett, Catherine E. cpuckett@usgs.gov","contributorId":4629,"corporation":false,"usgs":true,"family":"Puckett","given":"Catherine","email":"cpuckett@usgs.gov","middleInitial":"E.","affiliations":[],"preferred":true,"id":504423,"contributorType":{"id":2,"text":"Editors"},"rank":3},{"text":"Doran, Peter D.","contributorId":17533,"corporation":false,"usgs":true,"family":"Doran","given":"Peter","email":"","middleInitial":"D.","affiliations":[],"preferred":false,"id":504424,"contributorType":{"id":2,"text":"Editors"},"rank":4},{"text":"Mac, Michael J.","contributorId":16772,"corporation":false,"usgs":true,"family":"Mac","given":"Michael","email":"","middleInitial":"J.","affiliations":[],"preferred":false,"id":504421,"contributorType":{"id":2,"text":"Editors"},"rank":5}],"authors":[{"text":"Igl, Lawrence D. 0000-0003-0530-7266 ligl@usgs.gov","orcid":"https://orcid.org/0000-0003-0530-7266","contributorId":2381,"corporation":false,"usgs":true,"family":"Igl","given":"Lawrence","email":"ligl@usgs.gov","middleInitial":"D.","affiliations":[{"id":480,"text":"Northern Prairie Wildlife Research Center","active":true,"usgs":true}],"preferred":true,"id":295931,"contributorType":{"id":1,"text":"Authors"},"rank":1},{"text":"Johnson, Douglas H. 0000-0002-7778-6641 douglas_h_johnson@usgs.gov","orcid":"https://orcid.org/0000-0002-7778-6641","contributorId":1387,"corporation":false,"usgs":true,"family":"Johnson","given":"Douglas","email":"douglas_h_johnson@usgs.gov","middleInitial":"H.","affiliations":[{"id":480,"text":"Northern Prairie Wildlife Research Center","active":true,"usgs":true}],"preferred":true,"id":295932,"contributorType":{"id":1,"text":"Authors"},"rank":2}]}} ,{"id":70185154,"text":"70185154 - 1995 - Evidence of Emperor Geese breeding in Russia and staging in Alaska","interactions":[],"lastModifiedDate":"2017-03-15T13:27:03","indexId":"70185154","displayToPublicDate":"1995-01-01T00:00:00","publicationYear":"1995","noYear":false,"publicationType":{"id":2,"text":"Article"},"publicationSubtype":{"id":10,"text":"Journal Article"},"seriesTitle":{"id":3544,"text":"The Auk","onlineIssn":"1938-4254","printIssn":"0004-8038","active":true,"publicationSubtype":{"id":10}},"title":"Evidence of Emperor Geese breeding in Russia and staging in Alaska","docAbstract":"Emperor Geese (Chen canagica) breed primarily on the Yukon-Kuskokwim Delta, Alaska (Eisenhauer and Kirkpatrick 1977), but a small, poorly quantified proportion of the world's population is known to breed in the Russia Far East (Kistchinski 1976, 1988, Portenko 1981). Eisenhauer and Kirkpatrick (1977) stated that 80 to 90% of all Emperor Geese breed on the Yukon-Kuskokwim Delta, Alaska, and current estimates for numbers of breeding pairs in this area are 20,000 to 25,000 (R. A. Stehn, National Biological Service, Anchorage, Alaska, unpubl. data). In Russia, Emperor Geese are distributed primarily along the north coast of the Chukotka Peninsula between Kolyuchin Bay and Cape Shmidt, and in the Anadyr Lowlands along the coast of Anadyr Bay (Fig. 1; Kistchinski 1988, Kondratyev 1992, 1993), Kistchinski (1976) noted that up to 80% of these geese are nonbreeding birds. Recent aerial surveys of Emperor Goose habitats along the eastern coast of Russia indicated a minimum of 3,000 to 5,000 geese, although very few were on nests or with young, and only 127 total broods were seen during these surveys (J. I. Hodges, Fish and Wildlife Service (FWS), Juneau, Alaska, unpubl. data) It is not known if these two continental distributions of breeding Emperor Geese commingle and use similar areas during migration and for winter. Aerial surveys of the Alaska Peninsula during spring and fall indicate that lagoons on the northern coast are the primary staging areas for this species, and it is presumed that virtually all Emperor Geese use the Alaska Peninsula during migration (Petersen and Gill 1982). Emperor Geese winter throughout the Aleutian and Kommandorsky islands (Byrd et al., 1974). In the late fall, geese arrive in the western and eastern Aleutian Islands before arriving in the central Aleutians, thus suggesting that geese may be coming to this wintering area from both continents (G. V. Byrd pers, comm.). Speculations of previous investigators that Emperor Geese breeding in Russia use the Alaska Peninsula for staging (Eisenhauer and Kirkpatrick 1977, A. Krechmar pers. comm.) have not been confirmed. Here we report observations of two geese banded as juveniles in Russia and observed on the Alaska Peninsula during their first fall migration.
","language":"English","publisher":"American Ornithological Society","doi":"10.2307/4089035","usgsCitation":"Schmutz, J.A., and Kondratyev, A.V., 1995, Evidence of Emperor Geese breeding in Russia and staging in Alaska: The Auk, v. 112, no. 4, p. 1037-1038, https://doi.org/10.2307/4089035.","productDescription":"2 p.","startPage":"1037","endPage":"1038","costCenters":[{"id":114,"text":"Alaska Science Center","active":true,"usgs":true}],"links":[{"id":337640,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/thumbnails/outside_thumb.jpg"}],"country":"Russia, United States","state":"Alaska","volume":"112","issue":"4","noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"58ca52ffe4b0849ce97c8756","contributors":{"authors":[{"text":"Schmutz, Joel A. 0000-0002-6516-0836 jschmutz@usgs.gov","orcid":"https://orcid.org/0000-0002-6516-0836","contributorId":1805,"corporation":false,"usgs":true,"family":"Schmutz","given":"Joel","email":"jschmutz@usgs.gov","middleInitial":"A.","affiliations":[{"id":117,"text":"Alaska Science Center Biology WTEB","active":true,"usgs":true},{"id":114,"text":"Alaska Science Center","active":true,"usgs":true}],"preferred":true,"id":684550,"contributorType":{"id":1,"text":"Authors"},"rank":1},{"text":"Kondratyev, Alexander V.","contributorId":60160,"corporation":false,"usgs":false,"family":"Kondratyev","given":"Alexander","email":"","middleInitial":"V.","affiliations":[],"preferred":false,"id":684551,"contributorType":{"id":1,"text":"Authors"},"rank":2}]}} ,{"id":70187033,"text":"70187033 - 1995 - Assessment of forest fragmentation in southern New England using remote sensing and geographic information systems technology","interactions":[],"lastModifiedDate":"2017-04-20T11:08:00","indexId":"70187033","displayToPublicDate":"1995-01-01T00:00:00","publicationYear":"1995","noYear":false,"publicationType":{"id":2,"text":"Article"},"publicationSubtype":{"id":10,"text":"Journal Article"},"seriesTitle":{"id":1321,"text":"Conservation Biology","active":true,"publicationSubtype":{"id":10}},"title":"Assessment of forest fragmentation in southern New England using remote sensing and geographic information systems technology","docAbstract":"Spatial patterns and rates of forest fragmentation were assessed using digital remote sensing data for a region in southern New England that included 157 townships in southern New Hampshire and northeastern Massachusetts. The study area has undergone marked population increases over the last several decades. Following classification of 1973 and 1988 Landsat Multispectral Scanner data into forest and nonforest classes, data were incorporated into a geographic information system. The natural logarithms of forest area to perimeter ratios, referred to as the forest continuity index, were used to assess patterns and trends of forest fragmentation across the region Forest continuity index values were extracted from each township for both data sets and compared with population data. Forest continuity index values were found to decrease with increasing population density until about 200 persons per square kilometer, after which the relationship stabilized. With slight population increases at low densities forest continuity index values declined sharply, implying abrupt increases in forest fragmentation. Results from the study indicated good negative correlations (r2 values of 0.81 and 0.77) between the Multispectral Scanner-derived forest continuity index and natural logs of township population density. Socioeconomic indicators such as affluence and commuting patterns did not appear to correlate well with forest fragmentation estimates. Decreases in forest continuity index values occurred throughout much of the study region between 1973 and 1988, suggesting that forest fragmentation is occurring over large regions within the eastern United States. It is technologically feasible to assess patterns and rates of forest fragmentation across much larger areas than analyzed in this study; such analyses would provide useful overviews enabling objective assessment of the magnitude of forest fragmentation.
","language":"English","publisher":"Wiley","doi":"10.1046/j.1523-1739.1995.9020439.x","usgsCitation":"Vogelmann, J., 1995, Assessment of forest fragmentation in southern New England using remote sensing and geographic information systems technology: Conservation Biology, v. 9, no. 2, p. 439-449, https://doi.org/10.1046/j.1523-1739.1995.9020439.x.","productDescription":"11 p.","startPage":"439","endPage":"449","costCenters":[{"id":222,"text":"Earth Resources Observation and Science (EROS) Center","active":true,"usgs":true}],"links":[{"id":339961,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/thumbnails/outside_thumb.jpg"}],"country":"United States","state":"Massachusetts, New Hampshire","geographicExtents":"{\n \"type\": \"FeatureCollection\",\n \"features\": [\n {\n \"type\": \"Feature\",\n \"properties\": {},\n \"geometry\": {\n \"type\": \"Polygon\",\n \"coordinates\": [\n [\n [\n -72.4053955078125,\n 42.26511445833756\n ],\n [\n -70.5487060546875,\n 42.26511445833756\n ],\n [\n -70.5487060546875,\n 43.329173667843904\n ],\n [\n -72.4053955078125,\n 43.329173667843904\n ],\n [\n -72.4053955078125,\n 42.26511445833756\n ]\n ]\n ]\n }\n }\n ]\n}","volume":"9","issue":"2","noUsgsAuthors":false,"publicationDate":"2003-01-31","publicationStatus":"PW","scienceBaseUri":"58f877c4e4b0b7ea54521c4c","contributors":{"authors":[{"text":"Vogelmann, James E. 0000-0002-0804-5823 vogel@usgs.gov","orcid":"https://orcid.org/0000-0002-0804-5823","contributorId":649,"corporation":false,"usgs":true,"family":"Vogelmann","given":"James E.","email":"vogel@usgs.gov","affiliations":[{"id":223,"text":"Earth Resources Observation and Science (EROS) Center (Geography)","active":false,"usgs":true}],"preferred":false,"id":692022,"contributorType":{"id":1,"text":"Authors"},"rank":1}]}} ,{"id":70018745,"text":"70018745 - 1995 - Basement and cover-rock deformation during Laramide contraction in the northern Madison Range (Montana) and its influence on Cenozoic basin formation","interactions":[],"lastModifiedDate":"2023-01-20T17:10:20.209986","indexId":"70018745","displayToPublicDate":"1995-01-01T00:00:00","publicationYear":"1995","noYear":false,"publicationType":{"id":2,"text":"Article"},"publicationSubtype":{"id":10,"text":"Journal Article"},"seriesTitle":{"id":701,"text":"American Association of Petroleum Geologists Bulletin","active":true,"publicationSubtype":{"id":10}},"title":"Basement and cover-rock deformation during Laramide contraction in the northern Madison Range (Montana) and its influence on Cenozoic basin formation","docAbstract":"Two major Laramide fault systems converge in the northwestern Madison Range: the northwest-striking, southwest-vergent Spanish Peaks reverse fault and the north-striking, east-vergent Hilgard thrust system. Analysis of foliation attitudes in basement gneiss north and south of the Spanish Peaks fault indicates that the basement in thrusted blocks of the Hilgard thrust system has been rotated by an amount similar to that of the basement-cover contact. Steeply dipping, north-striking breccia zones enclosing domains of relatively undeformed basement may have permitted domino-style rotation of basement blocks during simple shear between pairs of thrusts.
In most places along the Hilgard thrust system, a large basement overhang, produced by thrusting of Archean blocks above rocks as young as Late Cretaceous, overlies a tight footwall syncline. This tight folding is largely concentric and was accommodated by flexural slip, resulting in severe crowding in synclinal hinges that resulted in observed or inferred features such as bedding-plane slip, imbricate and out-of-syncline thrusting, and hinge collapse.
The north-striking Madison normal fault system, a zone of Tertiary and Quaternary valley-forming normal faults, is approximately parallel to the Hilgard thrust system. In some places, normal faults are reactivated thrusts on which large basement overhangs of the Hilgard thrust system were dropped back into the Madison Valley and covered by Tertiary basin-fill deposits, leaving only the rocks of the footwall synclines exposed. In other places, both the thrusted Archean blocks and the near-isoclinal footwall synclines are well preserved.
This paired fault system (the Madison normal fault system and the Hilgard thrust system) of the northern Madison Range is strikingly similar to other paired systems in southwestern Montana along and adjacent to the western margins of the Ruby Range, Snowcrest Range, Greenhorn Range, Tobacco Root Mountains, and Bridger Range. Such systems may be the result of collapse of the crestal zones of large Laramide basement uplifts (arches) during Tertiary extension.
No hydrocarbon discoveries have been made in this unique structural province. However, petroleum exploration here has focused on basement-cored anticlines, both surface and subthrust, related to the two major Laramide fault systems and on the fault-bounded blocks of Tertiary rocks within the post-Laramide extensional basins. The interplay of the two Laramide fault systems during both Laramide shortening and Tertiary extension has produced a variety of possible structural traps in the Madison Range that have not yet been thoroughly investigated.
","language":"English","publisher":"American Association of Petroleum Geologists","doi":"10.1306/8D2B21F5-171E-11D7-8645000102C1865D","usgsCitation":"Kellogg, K., Schmidt, C.J., and Young, S.W., 1995, Basement and cover-rock deformation during Laramide contraction in the northern Madison Range (Montana) and its influence on Cenozoic basin formation: American Association of Petroleum Geologists Bulletin, v. 79, no. 8, p. 1117-1137, https://doi.org/10.1306/8D2B21F5-171E-11D7-8645000102C1865D.","productDescription":"21 p.","startPage":"1117","endPage":"1137","numberOfPages":"21","costCenters":[],"links":[{"id":227582,"rank":1,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/thumbnails/outside_thumb.jpg"}],"country":"United States","state":"Montana","otherGeospatial":"Madison Range","geographicExtents":"{\n \"type\": \"FeatureCollection\",\n \"features\": [\n {\n \"type\": \"Feature\",\n \"properties\": {},\n \"geometry\": {\n \"coordinates\": [\n [\n [\n -110.96298275085888,\n 45.93551953311629\n ],\n [\n -113.14612178278776,\n 45.93551953311629\n ],\n [\n -113.14612178278776,\n 44.48642248439407\n ],\n [\n -110.96298275085888,\n 44.48642248439407\n ],\n [\n -110.96298275085888,\n 45.93551953311629\n ]\n ]\n ],\n \"type\": \"Polygon\"\n }\n }\n ]\n}","volume":"79","issue":"8","noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"5059efdee4b0c8380cd4a4c1","contributors":{"authors":[{"text":"Kellogg, Karl S.","contributorId":89896,"corporation":false,"usgs":true,"family":"Kellogg","given":"Karl S.","affiliations":[],"preferred":false,"id":380633,"contributorType":{"id":1,"text":"Authors"},"rank":1},{"text":"Schmidt, C. J.","contributorId":45066,"corporation":false,"usgs":true,"family":"Schmidt","given":"C.","email":"","middleInitial":"J.","affiliations":[],"preferred":false,"id":380632,"contributorType":{"id":1,"text":"Authors"},"rank":2},{"text":"Young, S. W.","contributorId":19722,"corporation":false,"usgs":true,"family":"Young","given":"S.","email":"","middleInitial":"W.","affiliations":[],"preferred":false,"id":380631,"contributorType":{"id":1,"text":"Authors"},"rank":3}]}} ,{"id":70018829,"text":"70018829 - 1995 - Geologic and societal factors affecting the international oceanic transport of aggregate","interactions":[],"lastModifiedDate":"2012-03-12T17:19:13","indexId":"70018829","displayToPublicDate":"1995-01-01T00:00:00","publicationYear":"1995","noYear":false,"publicationType":{"id":2,"text":"Article"},"publicationSubtype":{"id":10,"text":"Journal Article"},"seriesTitle":{"id":2879,"text":"Nonrenewable Resources","active":true,"publicationSubtype":{"id":10}},"title":"Geologic and societal factors affecting the international oceanic transport of aggregate","docAbstract":"Crushed stone and sand and gravel are the two main sources of natural aggregate, and together comprise approximately half the volume and tonnage of mined material in the United States. Natural aggregate is a bulky, heavy material without special or unique properties, and it is commonly used near its source of production to minimize haulage cost. However, remoteness is no longer an absolute disqualifier for the production of aggregate. Today interstate aggregate routinely is shipped hundreds of kilometers by rail and barge. In addition, during 1992, the United States imported 1,317,000 metric tons of aggregate from Canada and 1,531,000 metric tons from Mexico. A number of ports on the Atlantic Coast and Gulf Coast of the United States receive imports of crushed stone from foreign sources for transport to various parts of the eastern United States. These areas either lack adequate supplies of aggregate or are augmenting their supplies because they have difficulties meeting current demand. These difficulties may include poor stone quality, environmental permitting problems, or transportation. Certain societal and geologic conditions of New York City and Philadelphia along the Atlantic Coast, and Tampa and New Orleans along the Gulf Coast, are discussed to demonstrate the different combinations of issues that contribute to the economic viability of importing crushed stone. ?? 1995 Oxford University Press.","largerWorkType":{"id":2,"text":"Article"},"largerWorkTitle":"Nonrenewable Resources","largerWorkSubtype":{"id":10,"text":"Journal Article"},"language":"English","publisherLocation":"Kluwer Academic Publishers","doi":"10.1007/BF02263378","issn":"09611444","usgsCitation":"Langer, W.H., 1995, Geologic and societal factors affecting the international oceanic transport of aggregate: Nonrenewable Resources, v. 4, no. 4, p. 303-309, https://doi.org/10.1007/BF02263378.","startPage":"303","endPage":"309","numberOfPages":"7","costCenters":[],"links":[{"id":205759,"rank":9999,"type":{"id":10,"text":"Digital Object Identifier"},"url":"https://dx.doi.org/10.1007/BF02263378"},{"id":226612,"rank":0,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/thumbnails/outside_thumb.jpg"}],"volume":"4","issue":"4","noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"505a190de4b0c8380cd55890","contributors":{"authors":[{"text":"Langer, W. H.","contributorId":44932,"corporation":false,"usgs":true,"family":"Langer","given":"W.","email":"","middleInitial":"H.","affiliations":[],"preferred":false,"id":380880,"contributorType":{"id":1,"text":"Authors"},"rank":1}]}} ,{"id":70019652,"text":"70019652 - 1995 - Evolution of tholeiitic diabase sheet systems in the eastern United States: examples from the Culpeper Basin, Virginia-Maryland, and the Gettysburg Basin, Pennsylvania","interactions":[],"lastModifiedDate":"2019-12-20T06:37:35","indexId":"70019652","displayToPublicDate":"1995-01-01T00:00:00","publicationYear":"1995","noYear":false,"publicationType":{"id":2,"text":"Article"},"publicationSubtype":{"id":10,"text":"Journal Article"},"seriesTitle":{"id":2499,"text":"Journal of Volcanology and Geothermal Research","active":true,"publicationSubtype":{"id":10}},"title":"Evolution of tholeiitic diabase sheet systems in the eastern United States: examples from the Culpeper Basin, Virginia-Maryland, and the Gettysburg Basin, Pennsylvania","docAbstract":"High-TiO2, quartz-normative (HTQ) tholeiite sheets of Early Jurassic age have intruded mainly Late Triassic sedimentary rocks in several early Mesozoic basins in the eastern US. Field observations, petrographic study, geochemical analyses and stable isotope data from three HTQ sheet systems were used to develop a general model of magmatic differentiation and magmatic-hydrothermal interaction for HTQ sheets. The three sheet systems have remarkably similar major-oxide and trace-element compositions. Cumulus and evolved diabase in comagmatic sheets separated by tens of kilometers are related by igneous differentiation. Differentiated diabase in all three sheets have petrographic and geochemical signatures and fluid inclusions indicating hydrothermal alteration beginning near magmatic temperatures and continuing to relatively low temperatures. Sulfur and oxygen isotope data are consistent with a magmatic origin for the hydrothermal fluid. -from Authors","language":"English","publisher":"Elsevier","doi":"10.1016/0377-0273(94)00085-U","issn":"03770273","usgsCitation":"Woodruff, L.G., Froelich, A., Belkin, H.E., and Gottfried, D., 1995, Evolution of tholeiitic diabase sheet systems in the eastern United States: examples from the Culpeper Basin, Virginia-Maryland, and the Gettysburg Basin, Pennsylvania: Journal of Volcanology and Geothermal Research, v. 64, no. 3-4, p. 143-169, https://doi.org/10.1016/0377-0273(94)00085-U.","productDescription":"17 p. ","startPage":"143","endPage":"169","numberOfPages":"27","costCenters":[{"id":245,"text":"Eastern Mineral and Environmental Resources Science Center","active":true,"usgs":true}],"links":[{"id":227924,"rank":0,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/thumbnails/outside_thumb.jpg"},{"id":269366,"type":{"id":10,"text":"Digital Object Identifier"},"url":"https://dx.doi.org/10.1016/0377-0273(94)00085-U"}],"country":"United States ","state":"Pennsylvania, Maryland, Virginia","otherGeospatial":"Culpeper Basin, Gettysburg Basin ","geographicExtents":"{\n \"type\": \"FeatureCollection\",\n \"features\": [\n {\n \"type\": \"Feature\",\n \"properties\": {},\n \"geometry\": {\n \"type\": \"Polygon\",\n \"coordinates\": [\n [\n [\n -75.41015624999999,\n 41.1290213474951\n ],\n [\n -77.93701171875,\n 40.07807142745009\n ],\n [\n -78.7060546875,\n 39.06184913429154\n ],\n [\n -79.82666015625,\n 38.013476231041935\n ],\n [\n -79.7607421875,\n 37.405073750176925\n ],\n [\n -78.2666015625,\n 38.496593518947584\n ],\n [\n -76.92626953125,\n 39.65645604812829\n ],\n [\n -75.8056640625,\n 40.195659093364654\n ],\n [\n -74.970703125,\n 40.697299008636755\n ],\n [\n -75.41015624999999,\n 41.1290213474951\n ]\n ]\n ]\n }\n }\n ]\n}","volume":"64","issue":"3-4","noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"505a0d8ee4b0c8380cd530a7","contributors":{"authors":[{"text":"Woodruff, Laurel G. 0000-0002-2514-9923 woodruff@usgs.gov","orcid":"https://orcid.org/0000-0002-2514-9923","contributorId":2224,"corporation":false,"usgs":true,"family":"Woodruff","given":"Laurel","email":"woodruff@usgs.gov","middleInitial":"G.","affiliations":[{"id":245,"text":"Eastern Mineral and Environmental Resources Science Center","active":true,"usgs":true}],"preferred":true,"id":778199,"contributorType":{"id":1,"text":"Authors"},"rank":1},{"text":"Froelich, A.J.","contributorId":13593,"corporation":false,"usgs":true,"family":"Froelich","given":"A.J.","email":"","affiliations":[],"preferred":false,"id":383448,"contributorType":{"id":1,"text":"Authors"},"rank":2},{"text":"Belkin, Harvey E. 0000-0001-7879-6529 hbelkin@usgs.gov","orcid":"https://orcid.org/0000-0001-7879-6529","contributorId":581,"corporation":false,"usgs":true,"family":"Belkin","given":"Harvey","email":"hbelkin@usgs.gov","middleInitial":"E.","affiliations":[{"id":241,"text":"Eastern Energy Resources Science Center","active":true,"usgs":true}],"preferred":true,"id":778200,"contributorType":{"id":1,"text":"Authors"},"rank":3},{"text":"Gottfried, D.","contributorId":92346,"corporation":false,"usgs":true,"family":"Gottfried","given":"D.","email":"","affiliations":[],"preferred":false,"id":383451,"contributorType":{"id":1,"text":"Authors"},"rank":4}]}} ,{"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":"Attempts to maintain the native lake trout (Salvelinus namaycush) 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 (Petromyzon marinus) 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 1985–1990 year classes. Survival of stocked yearlings declined over 50% in the 1980 s and was negatively correlated with the abundance of lake trout > 550 mm long (r = −0.91, P < 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 1977–1984 year classes, mean annual survival rate of lake trout age 6 and older was 0.45 (range: 0.35–0.56). In U.S. waters during 1985–1992, 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 < 250 mm long in trawl catches in 1978–1992 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.
","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":70018865,"text":"70018865 - 1995 - Geologic framework of a transect of the central Brooks Range: Regional relations and an alternative to the Endicott Mountains allochthon","interactions":[],"lastModifiedDate":"2023-01-20T17:13:53.976037","indexId":"70018865","displayToPublicDate":"1995-01-01T00:00:00","publicationYear":"1995","noYear":false,"publicationType":{"id":2,"text":"Article"},"publicationSubtype":{"id":10,"text":"Journal Article"},"seriesTitle":{"id":701,"text":"American Association of Petroleum Geologists Bulletin","active":true,"publicationSubtype":{"id":10}},"title":"Geologic framework of a transect of the central Brooks Range: Regional relations and an alternative to the Endicott Mountains allochthon","docAbstract":"This paper evaluates the geologic framework and tectonic development of the central Brooks Range based on a transect through the range and Arctic foothills. A geologic cross section constructed through the transect is confirmed by comparing the retrodeformed section with the regional distribution of lithofacies in the central Brooks Range. Stratigraphic relations in the retrodeformed section are further explained by comparing them to similar stratigraphic relations in the Ikpikpuk-Umiat basin under the Arctic coastal plain.
The structural framework of the central Brooks Range and Arctic foothills consists of fold nappes, thrust faults, and detached folds that sole in decollements and late-stage high-angle faults. In the central Brooks Range, shortening is by north-directed thrust faulting and folding of mostly Paleozoic rocks, and transport of any individual thrust sheet relative to underlying rocks is less than 30 km. In the middle of the range, imbricate blocks of lower Paleozoic basement are exposed in the core of the Doonerak anticline, and thrust sheets of stratigraphically higher Paleozoic rocks that overlie basement are exposed in the limbs of the anticline. In the northeast part of the anticline, the Amawk thrust emplaces Silurian and Upper Devonian rocks on a succession of Lower Mississippian an stratigraphically higher rocks that have been detached from the underlying basement along the Blarney Creek thrust. The Slatepile fault system, a system of high-angle faults in the north limb of the Doonerak anticline, drops the core and part of the north limb of the anticline down, giving the impression that the succession of Lower Mississippian and stratigraphically higher rocks that lie on basement south of the system high-angle faults extends under the Upper Devonian rocks that extensively crop out north of the high-angle faults. In the Arctic foothills, the mostly Paleozoic rocks of the north-central Brooks Range extend under Lower Cretaceous rocks of the North Slope foreland basin, and blind thrusts that sole in the Paleozoic rocks ramp up into the Lower Cretaceous and stratigraph cally higher rocks. Also in the Arctic foothills, a thrust sheet that contains the Arctic foothills assemblage overlies rocks of the north-central Brooks Range and Lower Cretaceous rocks of the North Slope foreland basin. Thrust transport of the Arctic foothills assemblage more than 40 km from south of the Doonerak anticline took place during the Early Cretaceous, but thrusting that deformed rocks of the North Slope foreland basin took place during the early Tertiary, with the vertical uplift of the Doonerak anticline being a late-formed feature.
Conclusions based on the retrodeformed cross section contrast significantly with previous work in which the Upper Devonian and stratigraphically higher rocks north of the Doonerak anticline are considered part of the Endicott Mountains allochthon, a regional allochthon that extends the breadth of the Brooks Range. In these models, Upper Devonian and younger rocks in the north-central Brooks Range have been thrust-transported 90 or 200 km from south of the Doonerak anticline, and emplacement of the allochthon could reflect as much as 885 km of tectonic shortening. The Lower Mississippian and stratigraphically higher rocks together with the underlying basement in the
northeast part of the anticline are considered to be in a window in the Endicott Mountains allochthon and to extend northward beneath allochthonous Upper Devonian and stratigraphically higher rocks in the north-central Brooks Range.
Lithofacies patterns in rocks in the central Brooks Range are consistent with the retrodeformed cross section and imply plausible Upper Devonian and Carboniferous depositional systems. Thick Upper Devonian and Lower Mississippian(?) clastic prisms were deposited in basins north of the Doonerak anticline. Mississippian carbonate rocks that overlie these clastic prisms were deposited in differentially subsiding shelf environments that included rocks in the Doonerak anticline. Restored across the Blarney Creek thrust, the Mississippian shelf carbonate rocks that presently lie north of the Doonerak anticline are those that were deposited on basement in the anticline. A carbonate ramp at the south edge of these shelf deposits extends east-southeast across the central Brooks Range and in th retrodeformed section lies south of the Doonerak anticline where Upper and Middle(?) Devonian shaly rocks thicken to the south. Unrestored, the ramp would extend across the Doonerak anticline.
Restored Late Devonian and Carboniferous lithofacies patterns in the central Brooks Range also are plausible from a regional perspective and have implications for exploration of basins under the Arctic coastal plain. The Late Devonian to Early Mississippian(?) basins in the north-central Brooks Range are part of a system of Early(?) Devonian to Early Mississippian(?) clastic basins that extend the length of the Brooks Range and include basins under the Arctic coastal plain. These basins are a template for depositional patterns in overlying rocks. Marine shelves between these basins where Mississippian strata unconformably lie on basement, such as in the northeastern Brooks Range and the Doonerak anticline, have depositional histories that are in contrast to areas that overlie the basi s. The resulting stratigraphic framework, together with the structural framework in the basement rocks that controlled the basins, has had a profound effect on the structural style of the fold belt, the salient effect being folds and thrust faults that are not orthogonal to the direction of structural transport. Stratigraphic relations exposed in the fold belt, especially the distribution of potential source rocks, likely model little-explored basins that underlie the North Slope foreland basin.
","language":"English","publisher":"American Association of Petroleum Geologists","doi":"10.1306/8D2B21EB-171E-11D7-8645000102C1865D","usgsCitation":"Kelley, J., and Brosge, W., 1995, Geologic framework of a transect of the central Brooks Range: Regional relations and an alternative to the Endicott Mountains allochthon: American Association of Petroleum Geologists Bulletin, v. 79, no. 8, p. 1087-1115, https://doi.org/10.1306/8D2B21EB-171E-11D7-8645000102C1865D.","productDescription":"29 p.","startPage":"1087","endPage":"1115","costCenters":[],"links":[{"id":226349,"rank":1,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/thumbnails/outside_thumb.jpg"}],"country":"United States","state":"Alaska","otherGeospatial":"central Brooks Range","geographicExtents":"{\n \"type\": \"FeatureCollection\",\n \"features\": [\n {\n \"type\": \"Feature\",\n \"properties\": {},\n \"geometry\": {\n \"coordinates\": [\n [\n [\n -154.48710859287527,\n 68.47681583657115\n ],\n [\n -154.48710859287527,\n 66.91601910999003\n ],\n [\n -148.70597701501478,\n 66.91601910999003\n ],\n [\n -148.70597701501478,\n 68.47681583657115\n ],\n [\n -154.48710859287527,\n 68.47681583657115\n ]\n ]\n ],\n \"type\": \"Polygon\"\n }\n }\n ]\n}","volume":"79","issue":"8","noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"505a196ae4b0c8380cd559a1","contributors":{"authors":[{"text":"Kelley, John S.","contributorId":23560,"corporation":false,"usgs":true,"family":"Kelley","given":"John S.","affiliations":[],"preferred":false,"id":380961,"contributorType":{"id":1,"text":"Authors"},"rank":1},{"text":"Brosge, W. P.","contributorId":58248,"corporation":false,"usgs":true,"family":"Brosge","given":"W. P.","affiliations":[],"preferred":false,"id":380962,"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":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":"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.
","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":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":"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.
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.
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).
","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":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":"The Florida manatee (Trichechus manatus latirostris) 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.
","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":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":"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.
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.
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.
","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":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":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":"No abstract available.
","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}]}} ]}