{"pageNumber":"874","pageRowStart":"21825","pageSize":"25","recordCount":46885,"records":[{"id":70157053,"text":"70157053 - 2007 - InSAR imaging of volcanic deformation over cloud-prone areas - Aleutian islands","interactions":[],"lastModifiedDate":"2019-03-04T09:48:02","indexId":"70157053","displayToPublicDate":"2007-03-01T00:00:00","publicationYear":"2007","noYear":false,"publicationType":{"id":2,"text":"Article"},"publicationSubtype":{"id":10,"text":"Journal Article"},"seriesTitle":{"id":3052,"text":"Photogrammetric Engineering and Remote Sensing","active":true,"publicationSubtype":{"id":10}},"title":"InSAR imaging of volcanic deformation over cloud-prone areas - Aleutian islands","docAbstract":"<p>Interferometric synthetic aperture radar (INSAR) is capable of measuring ground-surface deformation with centimeter-tosubcentimeter precision and spatial resolution of tens-of meters over a relatively large region. With its global coverage and all-weather imaging capability, INSAR is an important technique for measuring ground-surface deformation of volcanoes over cloud-prone and rainy regions such as the Aleutian Islands, where only less than 5 percent of optical imagery is usable due to inclement weather conditions. The spatial distribution of surface deformation data, derived from INSAR images, enables the construction of detailed mechanical models to enhance the study of magmatic processes. This paper reviews the basics of INSAR for volcanic deformation mapping and the INSAR studies of ten Aleutian volcanoes associated with both eruptive and noneruptive activity. These studies demonstrate that all-weather INSAR imaging can improve our understanding of how the Aleutian volcanoes work and enhance our capability to predict future eruptions and associated hazards.</p>","language":"English","publisher":"American Society for Photogrammetry and Remote Sensing","doi":"10.14358/PERS.73.3.245","usgsCitation":"Lu, Z., 2007, InSAR imaging of volcanic deformation over cloud-prone areas - Aleutian islands: Photogrammetric Engineering and Remote Sensing, v. 73, no. 3, p. 245-257, https://doi.org/10.14358/PERS.73.3.245.","productDescription":"13 p.","startPage":"245","endPage":"257","onlineOnly":"N","additionalOnlineFiles":"N","costCenters":[{"id":222,"text":"Earth Resources Observation and Science (EROS) Center","active":true,"usgs":true},{"id":615,"text":"Volcano Hazards Program","active":true,"usgs":true}],"links":[{"id":476916,"rank":0,"type":{"id":40,"text":"Open Access Publisher Index Page"},"url":"https://doi.org/10.14358/pers.73.3.245","text":"Publisher Index Page"},{"id":307906,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/thumbnails/outside_thumb.jpg"}],"volume":"73","issue":"3","noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"55e96f38e4b0dacf699e7884","contributors":{"authors":[{"text":"Lu, Zhong 0000-0001-9181-1818 lu@usgs.gov","orcid":"https://orcid.org/0000-0001-9181-1818","contributorId":901,"corporation":false,"usgs":true,"family":"Lu","given":"Zhong","email":"lu@usgs.gov","affiliations":[],"preferred":true,"id":571355,"contributorType":{"id":1,"text":"Authors"},"rank":1}]}}
,{"id":79668,"text":"sir20075027 - 2007 - Hydrology and glacier-lake-outburst floods (1987-2004) and water quality (1998-2003) of the Taku River near Juneau, Alaska","interactions":[],"lastModifiedDate":"2024-02-12T22:52:40.584659","indexId":"sir20075027","displayToPublicDate":"2007-03-01T00:00:00","publicationYear":"2007","noYear":false,"publicationType":{"id":18,"text":"Report"},"publicationSubtype":{"id":5,"text":"USGS Numbered Series"},"seriesTitle":{"id":334,"text":"Scientific Investigations Report","code":"SIR","onlineIssn":"2328-0328","printIssn":"2328-031X","active":true,"publicationSubtype":{"id":5}},"seriesNumber":"2007-5027","title":"Hydrology and glacier-lake-outburst floods (1987-2004) and water quality (1998-2003) of the Taku River near Juneau, Alaska","docAbstract":"The Taku River Basin originates in British Columbia, Canada, and drains an area of 6,600 square miles at the U.S. Geological Survey's Taku River gaging station. Several mines operated within the basin prior to 1957, and mineral exploration has resumed signaling potential for future mining developments. The U.S. Geological Survey in cooperation with the Douglas Indian Association, Alaska Department of Environmental Conservation, and the U.S. Environmental Protection Agency conducted a water-quality and flood-hydrology study of the Taku River. Water-quality sampling of the Taku River from 1998 through 2003 established a baseline for assessing potential effects of future mining operations on water quality.\r\n\r\nThe annual mean discharge of the Taku River is 13,700 cubic feet per second. The monthly mean discharge ranges from a minimum of 1,940 cubic feet per second in February to a maximum of 34,400 cubic feet per second in June. Nearly 90 percent of the annual discharge is from May through November. The highest spring discharges are sourced primarily from snowmelt and moderate discharges are sustained throughout the summer by glacial meltwaters. An ice cover usually forms over the Taku River in December persisting through the winter into March and occasionally into April.\r\n\r\nGlacier-lake-outburst floods originating from two glacier-dammed lakes along the margin of the Tulsequah Glacier in British Columbia, Canada, are the source of the greatest peak discharges on the Taku River. The largest flood during the period of record was 128,000 cubic feet per second on June 25, 2004, resulting from an outburst of Lake No Lake. Lake No Lake is the larger of the two lakes. The outburst-flood contribution to peak discharge was 80,000 cubic feet per second. The volume discharged from Lake No Lake is relatively consistent indicating drainage may be triggered when the lake reaches a critical stage. This suggests prediction of the timing of these outburst floods might be possible if lake-stage data were available. Further increases in the volume of Lake No Lake are unlikely as all tributary glaciers have retreated out of the lake basin. Decreasing outburst-flood volumes from Tulsequah Lake suggests a continued decline in the volume of this lake.\r\n\r\nPhysical and chemical parameters and concentrations of basic water-quality constituents indicate good water quality. Samples collected at the Taku River gaging station contained low concentrations of trace elements in the dissolved phase. Trace elements sampled were within acceptable limits when compared with the Alaska Department of Environmental Conservation aquatic-life criteria for fresh waters. The highest concentrations of total trace elements sampled were collected during glacial-outburst floods and likely are associated with suspended sediments. Total trace-element concentrations generally increase with increasing water discharge, although a high correlation for all constituents sampled does not always exist.","language":"English","publisher":"U.S. Geological Survey","doi":"10.3133/sir20075027","collaboration":"Prepared in cooperation with the Douglas Indian Association,\r\nAlaska Department of Environmental Conservation, and the\r\nU.S. Environmental Protection Agency","usgsCitation":"Neal, E., 2007, Hydrology and glacier-lake-outburst floods (1987-2004) and water quality (1998-2003) of the Taku River near Juneau, Alaska: U.S. Geological Survey Scientific Investigations Report 2007-5027, vi, 28 p., https://doi.org/10.3133/sir20075027.","productDescription":"vi, 28 p.","numberOfPages":"34","temporalStart":"1987-01-01","temporalEnd":"2004-12-31","costCenters":[{"id":114,"text":"Alaska Science Center","active":true,"usgs":true}],"links":[{"id":425579,"rank":3,"type":{"id":36,"text":"NGMDB Index Page"},"url":"https://ngmdb.usgs.gov/Prodesc/proddesc_80746.htm","linkFileType":{"id":5,"text":"html"}},{"id":9305,"rank":2,"type":{"id":15,"text":"Index Page"},"url":"https://pubs.usgs.gov/sir/2007/5027/","linkFileType":{"id":5,"text":"html"}},{"id":190521,"rank":1,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/thumbnails/usgs_thumb.jpg"}],"country":"United States","state":"Alaska","otherGeospatial":"Taku River","geographicExtents":"{\n  \"type\": \"FeatureCollection\",\n  \"features\": [\n    {\n      \"type\": \"Feature\",\n      \"properties\": {},\n      \"geometry\": {\n        \"coordinates\": [\n          [\n            [\n              -131,\n              59.5\n            ],\n            [\n              -134.5,\n              59.5\n            ],\n            [\n              -134.5,\n              57.9\n            ],\n            [\n              -131,\n              57.9\n            ],\n            [\n              -131,\n              59.5\n            ]\n          ]\n        ],\n        \"type\": \"Polygon\"\n      }\n    }\n  ]\n}","noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"4f4e4acce4b07f02db67e92c","contributors":{"authors":[{"text":"Neal, Edward G.","contributorId":68775,"corporation":false,"usgs":true,"family":"Neal","given":"Edward G.","affiliations":[],"preferred":false,"id":290531,"contributorType":{"id":1,"text":"Authors"},"rank":1}]}}
,{"id":79665,"text":"ofr20071055 - 2007 - Geochemical data from produced water contamination investigations: Osage-Skiatook Petroleum Environmental Research (OSPER) sites, Osage County, Oklahoma","interactions":[],"lastModifiedDate":"2022-07-05T19:57:56.110626","indexId":"ofr20071055","displayToPublicDate":"2007-02-28T00:00:00","publicationYear":"2007","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":"2007-1055","displayTitle":"Geochemical Data from Produced Water Contamination Investigations: Osage-Skiatook Petroleum Environmental Research (OSPER) Sites, Osage County, Oklahoma","title":"Geochemical data from produced water contamination investigations: Osage-Skiatook Petroleum Environmental Research (OSPER) sites, Osage County, Oklahoma","docAbstract":"We report chemical and isotopic analyses of 345 water samples collected from the Osage-Skiatook Petroleum Environmental Research (OSPER) project. Water samples were collected as part of an ongoing multi-year USGS investigation to study the transport, fate, natural attenuation, and ecosystem impacts of inorganic salts and organic compounds present in produced water releases at two oil and gas production sites from an aging petroleum field located in Osage County, in northeast Oklahoma. The water samples were collected primarily from monitoring wells and surface waters at the two research sites, OSPER A (legacy site) and OSPER B (active site), during the period March, 2001 to February, 2005. The data include produced water samples taken from seven active oil wells, one coal-bed methane well and two domestic groundwater wells in the vicinity of the OSPER sites.","language":"English","publisher":"U.S. Geological Survey","publisherLocation":"Reston, VA","doi":"10.3133/ofr20071055","usgsCitation":"Thordsen, J., Kharaka, Y.K., Ambats, G., Kakouros, E., and Abbott, M.M., 2007, Geochemical data from produced water contamination investigations: Osage-Skiatook Petroleum Environmental Research (OSPER) sites, Osage County, Oklahoma: U.S. Geological Survey Open-File Report 2007-1055, Report: v, 15 p.; Appendix, https://doi.org/10.3133/ofr20071055.","productDescription":"Report: v, 15 p.; Appendix","numberOfPages":"20","additionalOnlineFiles":"Y","costCenters":[{"id":589,"text":"Toxic Substances Hydrology Program","active":true,"usgs":true}],"links":[{"id":191890,"rank":1,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/thumbnails/usgs_thumb.jpg"},{"id":9301,"rank":100,"type":{"id":11,"text":"Document"},"url":"https://pubs.usgs.gov/of/2007/1055/pdf/ofr20071055.pdf","linkFileType":{"id":5,"text":"html"}},{"id":403011,"rank":4,"type":{"id":36,"text":"NGMDB Index Page"},"url":"https://ngmdb.usgs.gov/Prodesc/proddesc_80747.htm","linkFileType":{"id":5,"text":"html"}},{"id":367808,"rank":3,"type":{"id":3,"text":"Appendix"},"url":"https://pubs.usgs.gov/of/2007/1055/OFR_2007-1055_appendixAB.xls"}],"country":"United States","state":"Oklahoma","county":"Osage County","geographicExtents":"{\"type\":\"FeatureCollection\",\"features\":[{\"type\":\"Feature\",\"geometry\":{\"type\":\"Polygon\",\"coordinates\":[[[-96.0004,37.0002],[-95.9999,36.7735],[-95.9996,36.7654],[-95.9999,36.6864],[-96.0002,36.6792],[-96,36.5122],[-96.0003,36.5059],[-96,36.4255],[-96.0003,36.4201],[-96.0001,36.2509],[-95.9996,36.1632],[-95.9997,36.1601],[-96.0755,36.161],[-96.0852,36.1608],[-96.1832,36.1618],[-96.2003,36.1627],[-96.2659,36.1628],[-96.2756,36.1631],[-96.2745,36.1757],[-96.2692,36.182],[-96.2621,36.1873],[-96.2563,36.1912],[-96.2504,36.197],[-96.2474,36.2014],[-96.2466,36.2055],[-96.2485,36.216],[-96.2545,36.2238],[-96.2601,36.2267],[-96.2652,36.2282],[-96.2715,36.2288],[-96.2777,36.2289],[-96.2828,36.2299],[-96.2913,36.2315],[-96.2976,36.2321],[-96.3073,36.2318],[-96.309,36.2319],[-96.3131,36.2306],[-96.3205,36.229],[-96.3257,36.2286],[-96.3365,36.2289],[-96.3444,36.2318],[-96.3589,36.2421],[-96.3671,36.2509],[-96.3753,36.261],[-96.3831,36.268],[-96.3926,36.2723],[-96.4051,36.2762],[-96.4232,36.2802],[-96.4317,36.2836],[-96.4383,36.2887],[-96.442,36.2974],[-96.4447,36.3043],[-96.4456,36.3106],[-96.4488,36.3171],[-96.4515,36.3217],[-96.4525,36.3253],[-96.4564,36.3281],[-96.4575,36.3299],[-96.4597,36.3314],[-96.4677,36.3329],[-96.4723,36.333],[-96.4809,36.33],[-96.4861,36.3287],[-96.4885,36.3265],[-96.4926,36.3234],[-96.4967,36.3181],[-96.5052,36.3055],[-96.5116,36.3016],[-96.5133,36.3007],[-96.5213,36.3],[-96.5242,36.2991],[-96.5271,36.2987],[-96.5488,36.2996],[-96.5573,36.3016],[-96.564,36.304],[-96.5697,36.3064],[-96.5735,36.311],[-96.5751,36.3161],[-96.5761,36.3197],[-96.5765,36.3247],[-96.5763,36.3315],[-96.5744,36.3364],[-96.5702,36.3436],[-96.5643,36.3485],[-96.5568,36.3511],[-96.5453,36.3535],[-96.5366,36.3566],[-96.5291,36.3596],[-96.5278,36.3623],[-96.5264,36.3713],[-96.5221,36.3803],[-96.5247,36.3881],[-96.528,36.3927],[-96.5392,36.4011],[-96.5478,36.3999],[-96.5594,36.3929],[-96.5659,36.388],[-96.5678,36.3812],[-96.5714,36.3759],[-96.5755,36.3741],[-96.5829,36.3738],[-96.5914,36.3772],[-96.5959,36.3791],[-96.6015,36.3833],[-96.6093,36.3898],[-96.6133,36.408],[-96.616,36.4112],[-96.6234,36.4137],[-96.6279,36.4156],[-96.635,36.4257],[-96.6441,36.4268],[-96.6493,36.4264],[-96.6534,36.4251],[-96.6585,36.4234],[-96.6637,36.4221],[-96.674,36.4237],[-96.6872,36.4235],[-96.718,36.4441],[-96.7236,36.4482],[-96.7205,36.4573],[-96.7196,36.4668],[-96.7143,36.4712],[-96.7142,36.493],[-96.7164,36.4971],[-96.7203,36.4995],[-96.7248,36.5014],[-96.7275,36.5064],[-96.728,36.5105],[-96.7284,36.515],[-96.7295,36.5187],[-96.7282,36.5241],[-96.7292,36.5291],[-96.7307,36.5337],[-96.7373,36.5456],[-96.7443,36.5571],[-96.7545,36.5631],[-96.7618,36.5669],[-96.7774,36.5645],[-96.7844,36.5605],[-96.7954,36.5566],[-96.8006,36.5545],[-96.81,36.5465],[-96.8146,36.5438],[-96.8223,36.5381],[-96.8281,36.5323],[-96.8317,36.5283],[-96.8371,36.5211],[-96.8425,36.5103],[-96.8469,36.4991],[-96.8599,36.4843],[-96.8669,36.4776],[-96.871,36.4741],[-96.8751,36.4719],[-96.8797,36.4711],[-96.8837,36.4711],[-96.89,36.4717],[-96.8928,36.4727],[-96.8986,36.4719],[-96.9044,36.4692],[-96.9084,36.4675],[-96.9142,36.4662],[-96.9199,36.4659],[-96.9234,36.465],[-96.9275,36.4606],[-96.9316,36.457],[-96.9385,36.4562],[-96.9561,36.4588],[-96.9663,36.4653],[-96.9748,36.4664],[-96.9822,36.4692],[-96.9906,36.4766],[-97.0012,36.4872],[-97.0057,36.4905],[-97.0112,36.4987],[-97.0116,36.506],[-97.0109,36.5105],[-97.0096,36.5155],[-97.0083,36.5204],[-97.0025,36.5249],[-96.9978,36.5275],[-96.9915,36.5292],[-96.988,36.531],[-96.9828,36.5327],[-96.977,36.5344],[-96.9667,36.5352],[-96.9564,36.535],[-96.9506,36.5367],[-96.946,36.538],[-96.939,36.5424],[-96.9355,36.5455],[-96.929,36.5513],[-96.9261,36.554],[-96.9243,36.554],[-96.9175,36.5529],[-96.906,36.5536],[-96.9003,36.554],[-96.8968,36.5553],[-96.8921,36.5597],[-96.8909,36.5634],[-96.8873,36.5683],[-96.8866,36.5732],[-96.8876,36.5792],[-96.8932,36.5824],[-96.9034,36.5867],[-96.9162,36.6001],[-96.9387,36.5959],[-96.9468,36.5911],[-96.9526,36.5889],[-96.9549,36.589],[-96.9612,36.5882],[-96.974,36.5843],[-96.982,36.583],[-96.986,36.5827],[-96.9952,36.5837],[-97.0032,36.5839],[-97.0153,36.5827],[-97.029,36.5847],[-97.0415,36.5858],[-97.0512,36.5883],[-97.0568,36.5929],[-97.055,36.5979],[-97.0532,36.601],[-97.0469,36.6018],[-97.0473,36.6054],[-97.049,36.6068],[-97.0547,36.6106],[-97.0551,36.6165],[-97.0528,36.6364],[-97.0617,36.651],[-97.0656,36.6547],[-97.067,36.6656],[-97.0666,36.6829],[-97.0606,36.6918],[-97.0548,36.6926],[-97.0491,36.6939],[-97.0253,36.7012],[-97.0238,36.6953],[-97.017,36.6907],[-97.0038,36.6909],[-96.994,36.6903],[-96.9878,36.6875],[-96.9682,36.6889],[-96.958,36.6865],[-96.9477,36.6836],[-96.9345,36.6852],[-96.9263,36.691],[-96.9262,36.6937],[-96.9267,36.6982],[-96.9254,36.7014],[-96.9206,36.7085],[-96.9204,36.7176],[-96.9151,36.7216],[-96.9061,36.7351],[-96.8907,36.7525],[-96.8786,36.7536],[-96.8689,36.7521],[-96.8604,36.7483],[-96.849,36.7445],[-96.8404,36.7434],[-9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James J. jthordsn@usgs.gov","contributorId":3329,"corporation":false,"usgs":true,"family":"Thordsen","given":"James J.","email":"jthordsn@usgs.gov","affiliations":[{"id":438,"text":"National Research Program - Western Branch","active":true,"usgs":true}],"preferred":true,"id":290526,"contributorType":{"id":1,"text":"Authors"},"rank":1},{"text":"Kharaka, Yousif K. 0000-0001-9861-8260 ykharaka@usgs.gov","orcid":"https://orcid.org/0000-0001-9861-8260","contributorId":1928,"corporation":false,"usgs":true,"family":"Kharaka","given":"Yousif","email":"ykharaka@usgs.gov","middleInitial":"K.","affiliations":[{"id":438,"text":"National Research Program - Western Branch","active":true,"usgs":true}],"preferred":true,"id":290524,"contributorType":{"id":1,"text":"Authors"},"rank":2},{"text":"Ambats, Gil","contributorId":21235,"corporation":false,"usgs":true,"family":"Ambats","given":"Gil","affiliations":[],"preferred":false,"id":290527,"contributorType":{"id":1,"text":"Authors"},"rank":3},{"text":"Kakouros, Evangelos 0000-0002-4778-4039 kakouros@usgs.gov","orcid":"https://orcid.org/0000-0002-4778-4039","contributorId":2587,"corporation":false,"usgs":true,"family":"Kakouros","given":"Evangelos","email":"kakouros@usgs.gov","affiliations":[{"id":37464,"text":"WMA - Laboratory & Analytical Services Division","active":true,"usgs":true},{"id":438,"text":"National Research Program - Western Branch","active":true,"usgs":true}],"preferred":true,"id":290525,"contributorType":{"id":1,"text":"Authors"},"rank":4},{"text":"Abbott, Marvin M.","contributorId":89106,"corporation":false,"usgs":true,"family":"Abbott","given":"Marvin","email":"","middleInitial":"M.","affiliations":[],"preferred":false,"id":290528,"contributorType":{"id":1,"text":"Authors"},"rank":5}]}}
,{"id":79663,"text":"sir20065243 - 2007 - Interpretation of borehole geophysical logs, aquifer-isolation tests, and water-quality data for Sites 1, 3, and 5 at Willow Grove Naval Air Station/Joint Reserve Base, Horsham Township, Montgomery County, Pennsylvania: 2005","interactions":[],"lastModifiedDate":"2022-02-22T19:48:39.279413","indexId":"sir20065243","displayToPublicDate":"2007-02-28T00:00:00","publicationYear":"2007","noYear":false,"publicationType":{"id":18,"text":"Report"},"publicationSubtype":{"id":5,"text":"USGS Numbered Series"},"seriesTitle":{"id":334,"text":"Scientific Investigations Report","code":"SIR","onlineIssn":"2328-0328","printIssn":"2328-031X","active":true,"publicationSubtype":{"id":5}},"seriesNumber":"2006-5243","title":"Interpretation of borehole geophysical logs, aquifer-isolation tests, and water-quality data for Sites 1, 3, and 5 at Willow Grove Naval Air Station/Joint Reserve Base, Horsham Township, Montgomery County, Pennsylvania: 2005","docAbstract":"<p><span>Borehole geophysical logging, heatpulse-flowmeter measurements, borehole television surveys, and aquifer-isolation tests were conducted in 2005 at the Willow Grove Naval Air Station/Joint Reserve Base (NAS/JRB) in Horsham Township, Montgomery County, Pa. This study was done by the U.S. Geological Survey (USGS) in cooperation with the U.S. Navy in support of hydrogeological investigations to address ground-water contamination. Data collected for this study are valuable for understanding ground-water flow in the Stockton Formation at the local and regional scale. The Willow Grove NAS/JRB is underlain by the Stockton Formation, which consists of sedimentary rocks of Triassic age. The rocks of the Stockton Formation form a complex, heterogeneous aquifer with partially connected zones of high permeability. Borehole geophysical logs, heatpulse-flowmeter measurements, and borehole television surveys made in seven boreholes ranging from 70 to 350 ft deep were used to identify potential water-producing fractures and fracture zones and to select intervals for aquifer-isolation tests. An upward vertical hydraulic gradient was measured in one borehole, a downward vertical hydraulic gradient was measured in four boreholes, both an upward and a downward vertical hydraulic gradient were measured in one borehole, and no flow was measurable in one borehole. The aquifer-isolation tests isolated 30 discrete fractures in the seven boreholes for collection of depth-discrete hydraulic and water-quality data. Of the 30 fractures identified as potentially water producing, 26 fractures (87 percent) produced more than 1 gallon per minute of water. The specific capacity of the isolated intervals producing more than 1 gallon per minute ranged from 0.02 to 5.2 gallons per minute per foot. There was no relation between specific capacity and depth of the fracture. Samples for analysis for volatile organic compounds were collected from each isolated zone. Tetrachloroethylene (PCE) was the most prevalent compound at Site 1; concentrations were as great as 62 µg/L (micrograms per liter). 1,1-dichloroethane was the most prevalent compound at Site 3; concentrations were as great as 9.3 µg/L. Toluene was the most prevalent compound at Site 5; concentrations were as great as 77 µg/L. For five out of the six wells (83 percent) sampled for field determinations of water-quality constituents, the interval with the lowest dissolved oxygen concentration had the highest total VOC concentration.</span></p>","language":"English","publisher":"U.S. Geological Survey","doi":"10.3133/sir20065243","collaboration":"In cooperation with the U.S. Navy","usgsCitation":"Sloto, R.A., 2007, Interpretation of borehole geophysical logs, aquifer-isolation tests, and water-quality data for Sites 1, 3, and 5 at Willow Grove Naval Air Station/Joint Reserve Base, Horsham Township, Montgomery County, Pennsylvania: 2005: U.S. Geological Survey Scientific Investigations Report 2006-5243, x, 74 p., https://doi.org/10.3133/sir20065243.","productDescription":"x, 74 p.","numberOfPages":"75","temporalStart":"2005-01-01","temporalEnd":"2005-12-31","costCenters":[{"id":532,"text":"Pennsylvania Water Science Center","active":true,"usgs":true}],"links":[{"id":191992,"rank":0,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/thumbnails/usgs_thumb.jpg"},{"id":396269,"rank":3,"type":{"id":36,"text":"NGMDB Index Page"},"url":"https://ngmdb.usgs.gov/Prodesc/proddesc_80753.htm"},{"id":9299,"rank":100,"type":{"id":15,"text":"Index Page"},"url":"https://pubs.usgs.gov/sir/2006/5243/","linkFileType":{"id":5,"text":"html"}}],"country":"United States","state":"Pennsylvania","county":"Montgomery County","otherGeospatial":"Horsham Township, Willow Grove Naval Air Station/Joint Reserve Base","geographicExtents":"{ \"type\": \"FeatureCollection\", \"features\": [ { \"type\": \"Feature\", \"properties\": {}, \"geometry\": { \"type\": \"Polygon\", \"coordinates\": [ [ [ -75.25,40.0 ], [ -75.25,40.25 ], [ -75.0,40.25 ], [ -75.0,40.0 ], [ -75.25,40.0 ] ] ] } } ] }","noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"4f4e4b1be4b07f02db6a8fc4","contributors":{"authors":[{"text":"Sloto, Ronald A. rasloto@usgs.gov","contributorId":424,"corporation":false,"usgs":true,"family":"Sloto","given":"Ronald","email":"rasloto@usgs.gov","middleInitial":"A.","affiliations":[{"id":532,"text":"Pennsylvania Water Science Center","active":true,"usgs":true}],"preferred":true,"id":290521,"contributorType":{"id":1,"text":"Authors"},"rank":1}]}}
,{"id":79656,"text":"ofr20071013 - 2007 - A 3-Dimensional Model of Water-Bearing Sequences in the Dominguez Gap Region, Long Beach, California","interactions":[],"lastModifiedDate":"2012-02-10T00:11:39","indexId":"ofr20071013","displayToPublicDate":"2007-02-27T00:00:00","publicationYear":"2007","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":"2007-1013","title":"A 3-Dimensional Model of Water-Bearing Sequences in the Dominguez Gap Region, Long Beach, California","docAbstract":"A 3-dimensional computer model of the Quaternary sequence stratigraphy in the Dominguez gap region of Long Beach, California has been developed to provide a robust chronostratigraphic framework for hydrologic and tectonic studies. The model consists of 13 layers within a 16.5 by 16.1 km (10.25 by 10 mile) square area and extends downward to an altitude of -900 meters (-2952.76 feet). Ten sequences of late Pliocene to Holocene age are identified and correlated within the model. Primary data to build the model comes from five reference core holes, extensive high-resolution seismic data obtained in San Pedro Bay, and logs from several hundred water and oil wells drilled in the region. The model is best constrained in the vicinity of the Dominguez gap seawater intrusion barrier where a dense network of subsurface data exist. The resultant stratigraphic framework and geologic structure differs significantly from what has been proposed in earlier studies. \r\n\r\nAn important new discovery from this approach is the recognition of ongoing tectonic deformation throughout nearly all of Quaternary time that has impacted the geometry and character of the sequences. Anticlinal folding along a NW-SE trend, probably associated with Quaternary reactivation of the Wilmington anticline, has uplifted and thinned deposits along the fold crest, which intersects the Dominguez gap seawater barrier near Pacific Coast Highway. A W-NW trending fault system that approximately parallels the fold crest has also been identified. This fault progressively displaces all but the youngest sequences down to the north and serves as the southern termination of the classic Silverado aquifer. \r\n\r\nUplift and erosion of fining-upward paralic sequences along the crest of the young fold has removed or thinned many of the fine-grained beds that serve to protect the underlying Silverado aquifer from seawater contaminated shallow groundwater. As a result of this process, the potential exists for vertical migration of seawater into the producing aquifers and subsequent landward migration of intruded waters beneath the existing Dominguez barrier. Incipient invasion of the Silverado aquifer by chloride-enriched waters is observed in a recently drilled well located along the crest of the fold seaward of the barrier and at a depth of 440 feet (134 meters). \r\n\r\nThese new observations and interpretations indicate that the new sequence-based approach to defining the stratigraphy of the Dominguez Gap area may have important implications for seawater intrusion management. To test this, it will be useful to overlay existing water-quality and water level data onto the framework model and to incorporate the new stratigraphy into a transport model.\r\n","language":"ENGLISH","doi":"10.3133/ofr20071013","collaboration":"In cooperation with the Los Angeles County Department of Public Works and Water Replenishment District of Southern California","usgsCitation":"Ponti, D.J., Ehman, K.D., Edwards, B.D., Tinsley, J., Hildenbrand, T., Hillhouse, J.W., Hanson, R.T., McDougall, K., Powell, C.L., Wan, E., Land, M., Mahan, S., and Sarna-Wojcicki, A.M., 2007, A 3-Dimensional Model of Water-Bearing Sequences in the Dominguez Gap Region, Long Beach, California (Version 1.0): U.S. Geological Survey Open-File Report 2007-1013, iv, 34 p., https://doi.org/10.3133/ofr20071013.","productDescription":"iv, 34 p.","numberOfPages":"38","additionalOnlineFiles":"Y","costCenters":[{"id":648,"text":"Western Earthquake Hazards","active":false,"usgs":true}],"links":[{"id":191968,"rank":0,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/thumbnails/usgs_thumb.jpg"},{"id":9292,"rank":100,"type":{"id":15,"text":"Index Page"},"url":"https://pubs.usgs.gov/of/2007/1013/","linkFileType":{"id":5,"text":"html"}}],"geographicExtents":"{ \"type\": \"FeatureCollection\", \"features\": [ { \"type\": \"Feature\", \"properties\": {}, \"geometry\": { \"type\": \"Polygon\", \"coordinates\": [ [ [ -118.5,33.5 ], [ -118.5,34 ], [ -118,34 ], [ -118,33.5 ], [ -118.5,33.5 ] ] ] } } ] }","edition":"Version 1.0","noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"53cd493ee4b0b290850ef04e","contributors":{"authors":[{"text":"Ponti, Daniel J. 0000-0002-2437-5144 dponti@usgs.gov","orcid":"https://orcid.org/0000-0002-2437-5144","contributorId":1020,"corporation":false,"usgs":true,"family":"Ponti","given":"Daniel","email":"dponti@usgs.gov","middleInitial":"J.","affiliations":[{"id":237,"text":"Earthquake Science Center","active":true,"usgs":true}],"preferred":true,"id":290499,"contributorType":{"id":1,"text":"Authors"},"rank":1},{"text":"Ehman, Kenneth D.","contributorId":64745,"corporation":false,"usgs":true,"family":"Ehman","given":"Kenneth","email":"","middleInitial":"D.","affiliations":[],"preferred":false,"id":290509,"contributorType":{"id":1,"text":"Authors"},"rank":2},{"text":"Edwards, Brian D. bedwards@usgs.gov","contributorId":3161,"corporation":false,"usgs":true,"family":"Edwards","given":"Brian","email":"bedwards@usgs.gov","middleInitial":"D.","affiliations":[{"id":520,"text":"Pacific Coastal and Marine Science Center","active":true,"usgs":true}],"preferred":true,"id":290502,"contributorType":{"id":1,"text":"Authors"},"rank":3},{"text":"Tinsley, John C. III jtinsley@usgs.gov","contributorId":3266,"corporation":false,"usgs":true,"family":"Tinsley","given":"John C.","suffix":"III","email":"jtinsley@usgs.gov","affiliations":[{"id":237,"text":"Earthquake Science Center","active":true,"usgs":true}],"preferred":false,"id":290504,"contributorType":{"id":1,"text":"Authors"},"rank":4},{"text":"Hildenbrand, Thomas","contributorId":100956,"corporation":false,"usgs":true,"family":"Hildenbrand","given":"Thomas","affiliations":[],"preferred":false,"id":290510,"contributorType":{"id":1,"text":"Authors"},"rank":5},{"text":"Hillhouse, John W. 0000-0002-1371-4622 jhillhouse@usgs.gov","orcid":"https://orcid.org/0000-0002-1371-4622","contributorId":2618,"corporation":false,"usgs":true,"family":"Hillhouse","given":"John","email":"jhillhouse@usgs.gov","middleInitial":"W.","affiliations":[],"preferred":true,"id":290501,"contributorType":{"id":1,"text":"Authors"},"rank":6},{"text":"Hanson, Randall T. 0000-0002-9819-7141 rthanson@usgs.gov","orcid":"https://orcid.org/0000-0002-9819-7141","contributorId":801,"corporation":false,"usgs":true,"family":"Hanson","given":"Randall","email":"rthanson@usgs.gov","middleInitial":"T.","affiliations":[{"id":154,"text":"California Water Science Center","active":true,"usgs":true}],"preferred":true,"id":290498,"contributorType":{"id":1,"text":"Authors"},"rank":7},{"text":"McDougall, Kristen 0000-0002-8788-3664","orcid":"https://orcid.org/0000-0002-8788-3664","contributorId":52673,"corporation":false,"usgs":true,"family":"McDougall","given":"Kristen","email":"","affiliations":[{"id":312,"text":"Geology, Minerals, Energy, and Geophysics Science Center","active":true,"usgs":true}],"preferred":true,"id":290507,"contributorType":{"id":1,"text":"Authors"},"rank":8},{"text":"Powell, Charles L. II 0000-0002-1913-555X cpowell@usgs.gov","orcid":"https://orcid.org/0000-0002-1913-555X","contributorId":3243,"corporation":false,"usgs":true,"family":"Powell","given":"Charles","suffix":"II","email":"cpowell@usgs.gov","middleInitial":"L.","affiliations":[{"id":312,"text":"Geology, Minerals, Energy, and Geophysics Science Center","active":true,"usgs":true}],"preferred":false,"id":290503,"contributorType":{"id":1,"text":"Authors"},"rank":9},{"text":"Wan, Elmira 0000-0002-9255-112X ewan@usgs.gov","orcid":"https://orcid.org/0000-0002-9255-112X","contributorId":3434,"corporation":false,"usgs":true,"family":"Wan","given":"Elmira","email":"ewan@usgs.gov","affiliations":[{"id":312,"text":"Geology, Minerals, Energy, and Geophysics Science Center","active":true,"usgs":true}],"preferred":true,"id":290505,"contributorType":{"id":1,"text":"Authors"},"rank":10},{"text":"Land, Michael 0000-0001-5141-0307","orcid":"https://orcid.org/0000-0001-5141-0307","contributorId":56613,"corporation":false,"usgs":true,"family":"Land","given":"Michael","affiliations":[],"preferred":false,"id":290508,"contributorType":{"id":1,"text":"Authors"},"rank":11},{"text":"Mahan, Shannon 0000-0001-5214-7774","orcid":"https://orcid.org/0000-0001-5214-7774","contributorId":19239,"corporation":false,"usgs":true,"family":"Mahan","given":"Shannon","affiliations":[],"preferred":false,"id":290506,"contributorType":{"id":1,"text":"Authors"},"rank":12},{"text":"Sarna-Wojcicki, Andrei M. 0000-0002-0244-9149 asarna@usgs.gov","orcid":"https://orcid.org/0000-0002-0244-9149","contributorId":1046,"corporation":false,"usgs":true,"family":"Sarna-Wojcicki","given":"Andrei","email":"asarna@usgs.gov","middleInitial":"M.","affiliations":[],"preferred":true,"id":290500,"contributorType":{"id":1,"text":"Authors"},"rank":13}]}}
,{"id":79646,"text":"ofr20061371 - 2007 - Guidelines for Coding and Entering Ground-Water Data into the Ground-Water Site Inventory Database Version 4.6, U.S. Geological Survey, Washington Water Science Center","interactions":[],"lastModifiedDate":"2012-03-08T17:16:20","indexId":"ofr20061371","displayToPublicDate":"2007-02-24T00:00:00","publicationYear":"2007","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":"2006-1371","title":"Guidelines for Coding and Entering Ground-Water Data into the Ground-Water Site Inventory Database Version 4.6, U.S. Geological Survey, Washington Water Science Center","docAbstract":"This report establishes and documents the procedures used by the U.S. Geological Survey, Washington Water Science Center, to code and enter ground-water data into the Ground-Water Site Inventory database of the U.S. Geological Survey's Ground Water Site Inventory System. These guidelines are consistent with Version 4.6 of the system, but will be updated as each new version becomes available.\r\n\r\n","language":"ENGLISH","doi":"10.3133/ofr20061371","usgsCitation":"Lane, R.C., 2007, Guidelines for Coding and Entering Ground-Water Data into the Ground-Water Site Inventory Database Version 4.6, U.S. Geological Survey, Washington Water Science Center: U.S. Geological Survey Open-File Report 2006-1371, iv, 104 p., https://doi.org/10.3133/ofr20061371.","productDescription":"iv, 104 p.","numberOfPages":"108","costCenters":[{"id":622,"text":"Washington Water Science Center","active":true,"usgs":true}],"links":[{"id":192013,"rank":0,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/thumbnails/usgs_thumb.jpg"},{"id":9284,"rank":100,"type":{"id":15,"text":"Index Page"},"url":"https://pubs.usgs.gov/of/2006/1371/","linkFileType":{"id":5,"text":"html"}}],"noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"4f4e4a80e4b07f02db64981f","contributors":{"authors":[{"text":"Lane, R. C.","contributorId":6421,"corporation":false,"usgs":true,"family":"Lane","given":"R.","email":"","middleInitial":"C.","affiliations":[],"preferred":false,"id":290470,"contributorType":{"id":1,"text":"Authors"},"rank":1}]}}
,{"id":79648,"text":"sir20075011 - 2007 - Land-Cover Trends of the Sierra Nevada Ecoregion, 1973-2000","interactions":[],"lastModifiedDate":"2012-02-10T00:11:44","indexId":"sir20075011","displayToPublicDate":"2007-02-24T00:00:00","publicationYear":"2007","noYear":false,"publicationType":{"id":18,"text":"Report"},"publicationSubtype":{"id":5,"text":"USGS Numbered Series"},"seriesTitle":{"id":334,"text":"Scientific Investigations Report","code":"SIR","onlineIssn":"2328-0328","printIssn":"2328-031X","active":true,"publicationSubtype":{"id":5}},"seriesNumber":"2007-5011","title":"Land-Cover Trends of the Sierra Nevada Ecoregion, 1973-2000","docAbstract":"The U.S. Geological Survey has developed and is implementing the Land Cover Trends project to estimate and describe the temporal and spatial distribution and variability of contemporary land-use and land-cover change in the United States. As part of the Land Cover Trends project, the purpose of this study was to assess land-use/land-cover change in the Sierra Nevada ecoregion for the period 1973 to 2000 using a probability sampling technique and satellite imagery. We randomly selected 36 100-km2 sample blocks to derive thematic images of land-use/land-cover for five dates of Landsat imagery (1973, 1980, 1986, 1992, 2000). We visually interpreted as many as 11 land-use/land-cover classes using a 60-meter minimum mapping unit from the five dates of imagery yielding four periods for analysis. Change-detection results from post-classification comparison of our mapped data showed that landscape disturbance from fire was the dominant change from 1973-2000. The second most-common change was forest disturbance resulting from harvest of timber resources by way of clear-cutting. The rates of forest regeneration from temporary fire and harvest disturbances coincided with the rates of disturbance from the previous period. Relatively minor landscape changes were caused by new development and reservoir drawdown. Multiple linear regression analysis suggests that land ownership and the proportion of forest and developed cover types were significant determinants of the likelihood of direct human-induced change occurring in sampling units. Driving forces of change include land ownership, land management such as fire suppression policy, and demand for natural resources. \r\n\r\n","language":"ENGLISH","publisher":"Geological Survey (U.S.)","doi":"10.3133/sir20075011","usgsCitation":"Raumann, C.G., and Soulard, C.E., 2007, Land-Cover Trends of the Sierra Nevada Ecoregion, 1973-2000: U.S. Geological Survey Scientific Investigations Report 2007-5011, v, 29 p., https://doi.org/10.3133/sir20075011.","productDescription":"v, 29 p.","numberOfPages":"34","temporalStart":"1973-01-01","temporalEnd":"2000-12-31","costCenters":[{"id":293,"text":"Geographic Analysis and Monitoring Program","active":false,"usgs":true},{"id":296,"text":"Geography Program","active":false,"usgs":true}],"links":[{"id":194446,"rank":0,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/thumbnails/usgs_thumb.jpg"},{"id":9286,"rank":100,"type":{"id":15,"text":"Index Page"},"url":"https://pubs.usgs.gov/sir/2007/5011/","linkFileType":{"id":5,"text":"html"}}],"geographicExtents":"{ \"type\": \"FeatureCollection\", \"features\": [ { \"type\": \"Feature\", \"properties\": {}, \"geometry\": { \"type\": \"Polygon\", \"coordinates\": [ [ [ -122,34.5 ], [ -122,40.5 ], [ -117.5,40.5 ], [ -117.5,34.5 ], [ -122,34.5 ] ] ] } } ] }","noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"4f4e4b23e4b07f02db6adf5f","contributors":{"authors":[{"text":"Raumann, Christian G.","contributorId":65893,"corporation":false,"usgs":true,"family":"Raumann","given":"Christian","email":"","middleInitial":"G.","affiliations":[],"preferred":false,"id":290474,"contributorType":{"id":1,"text":"Authors"},"rank":1},{"text":"Soulard, Christopher E. 0000-0002-5777-9516 csoulard@usgs.gov","orcid":"https://orcid.org/0000-0002-5777-9516","contributorId":2642,"corporation":false,"usgs":true,"family":"Soulard","given":"Christopher","email":"csoulard@usgs.gov","middleInitial":"E.","affiliations":[{"id":657,"text":"Western Geographic Science Center","active":true,"usgs":true}],"preferred":true,"id":290473,"contributorType":{"id":1,"text":"Authors"},"rank":2}]}}
,{"id":79642,"text":"ofr20071037 - 2007 - Water and Sediment Quality in the Yukon River Basin, Alaska, During Water Year 2005","interactions":[],"lastModifiedDate":"2012-02-10T00:11:45","indexId":"ofr20071037","displayToPublicDate":"2007-02-22T00:00:00","publicationYear":"2007","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":"2007-1037","title":"Water and Sediment Quality in the Yukon River Basin, Alaska, During Water Year 2005","docAbstract":"OVERVIEW: This report contains water-quality and sediment-quality data from samples collected in the Yukon River Basin from March through September during the 2005 water year (WY). Samples were collected throughout the year at five stations in the basin (three on the main stem Yukon River, one each on the Tanana and Porcupine Rivers). A broad range of physical, chemical, and biological analyses are presented.\r\n\r\nThis is the final report in a series of five USGS Open-File Reports spanning five WYs, from October 2000 through September 2005. The previous four reports are listed in the references (Schuster, 2003, 2005a, 2005b, 2006).  Water-quality and sediment-quality data from samples collected on the Yukon River and selected major tributaries in Alaska for synoptic studies during WYs 2002-03 are published in Dornblaser and Halm (2006).\r\n\r\n","language":"ENGLISH","doi":"10.3133/ofr20071037","usgsCitation":"Schuster, P.F., 2007, Water and Sediment Quality in the Yukon River Basin, Alaska, During Water Year 2005: U.S. Geological Survey Open-File Report 2007-1037, viii, 65 p., https://doi.org/10.3133/ofr20071037.","productDescription":"viii, 65 p.","numberOfPages":"73","temporalStart":"2005-05-01","temporalEnd":"2005-09-30","costCenters":[],"links":[{"id":195388,"rank":0,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/thumbnails/usgs_thumb.jpg"},{"id":9279,"rank":100,"type":{"id":15,"text":"Index Page"},"url":"https://pubs.usgs.gov/of/2007/1037/","linkFileType":{"id":5,"text":"html"}}],"geographicExtents":"{ \"type\": \"FeatureCollection\", \"features\": [ { \"type\": \"Feature\", \"properties\": {}, \"geometry\": { \"type\": \"Polygon\", \"coordinates\": [ [ [ 156,61 ], [ 156,68 ], [ 130,68 ], [ 130,61 ], [ 156,61 ] ] ] } } ] }","noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"4f4e4a08e4b07f02db5fa386","contributors":{"authors":[{"text":"Schuster, Paul F. 0000-0002-8314-1372 pschuste@usgs.gov","orcid":"https://orcid.org/0000-0002-8314-1372","contributorId":1360,"corporation":false,"usgs":true,"family":"Schuster","given":"Paul","email":"pschuste@usgs.gov","middleInitial":"F.","affiliations":[{"id":438,"text":"National Research Program - Western Branch","active":true,"usgs":true},{"id":5044,"text":"National Research Program - Central Branch","active":true,"usgs":true}],"preferred":true,"id":290464,"contributorType":{"id":1,"text":"Authors"},"rank":1}]}}
,{"id":79638,"text":"ofr20071006 - 2007 - Mapping Phyllic and Argillic-Altered Rocks in Southeastern Afghanistan using Advanced Spaceborne Thermal Emission and Reflection Radiometer (ASTER) Data","interactions":[],"lastModifiedDate":"2018-11-05T11:16:10","indexId":"ofr20071006","displayToPublicDate":"2007-02-22T00:00:00","publicationYear":"2007","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":"2007-1006","title":"Mapping Phyllic and Argillic-Altered Rocks in Southeastern Afghanistan using Advanced Spaceborne Thermal Emission and Reflection Radiometer (ASTER) Data","docAbstract":"Introduction: ASTER data and logical operators were successfully used to map phyllic and argillic-altered rocks in the southeastern part of Afghanistan. Hyperion data were used to correct ASTER band 5 and ASTER data were georegistered to orthorectified Landsat TM data. Logical operator algorithms produced argillic and phyllic byte ASTER images that were converted to vector data and overlain on ASTER and Landsat TM images.\r\n\r\nAlteration and fault patterns indicated that two areas, the Argandab igneous complex, and the Katawaz basin may contain potential polymetallic vein and porphyry copper deposits. ASTER alteration mapping in the Chagai Hills indicates less extensive phyllic and argillic-altered rocks than mapped in the Argandab igneous complex and the Katawaz basin and patterns of alteration are inconclusive to predict potential deposit types.\r\n","language":"ENGLISH","doi":"10.3133/ofr20071006","collaboration":"Prepared in Cooperation with the United States Agency for International Development; USGS Afghanistan Project Product No. 110","usgsCitation":"Mars, J.L., and Rowan, L.C., 2007, Mapping Phyllic and Argillic-Altered Rocks in Southeastern Afghanistan using Advanced Spaceborne Thermal Emission and Reflection Radiometer (ASTER) Data: U.S. Geological Survey Open-File Report 2007-1006, map, 36 by 72 inches, https://doi.org/10.3133/ofr20071006.","productDescription":"map, 36 by 72 inches","onlineOnly":"Y","costCenters":[{"id":245,"text":"Eastern Mineral and Environmental Resources Science Center","active":true,"usgs":true}],"links":[{"id":194650,"rank":0,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/thumbnails/usgs_thumb.jpg"},{"id":9270,"rank":100,"type":{"id":15,"text":"Index Page"},"url":"https://pubs.usgs.gov/of/2007/1006/","linkFileType":{"id":5,"text":"html"}}],"noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"4f4e4b0be4b07f02db69df61","contributors":{"authors":[{"text":"Mars, John L. jmars@usgs.gov","contributorId":3428,"corporation":false,"usgs":true,"family":"Mars","given":"John","email":"jmars@usgs.gov","middleInitial":"L.","affiliations":[],"preferred":false,"id":290449,"contributorType":{"id":1,"text":"Authors"},"rank":1},{"text":"Rowan, Lawrence C.","contributorId":58629,"corporation":false,"usgs":true,"family":"Rowan","given":"Lawrence","email":"","middleInitial":"C.","affiliations":[],"preferred":false,"id":290450,"contributorType":{"id":1,"text":"Authors"},"rank":2}]}}
,{"id":79636,"text":"ofr20071047 - 2007 - Antarctica: A Keystone in a Changing World--Online Proceedings for the Tenth International Symposium on Antarctic Earth Sciences.  Santa Barbara, California, U.S.A.--August 26 to September 1, 2007","interactions":[],"lastModifiedDate":"2016-09-27T15:56:50","indexId":"ofr20071047","displayToPublicDate":"2007-02-16T00:00:00","publicationYear":"2007","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":"2007-1047","title":"Antarctica: A Keystone in a Changing World--Online Proceedings for the Tenth International Symposium on Antarctic Earth Sciences.  Santa Barbara, California, U.S.A.--August 26 to September 1, 2007","docAbstract":"Overview: The International Symposium on Antarctic Earth Sciences (ISAES) is held once every four years to provide an international forum for presenting research results and new ideas and for planning future Antarctic geoscience research projects. This Tenth ISAES coincides with the International Polar Year (IPY; 50th Anniversary of the International Geophysical Year) and has been structured to showcase the great breadth of geoscience research being done in Antarctic regions by more than more than 100 institutions located in over 30 countries. The science program of the Symposium encompasses six broad themes that cover key topics on evolution and interactions of the geosphere, cryosphere and biosphere and their cross-linkages with past and historic paleoclimates. Emphasis is also on deciphering the climate records in ice cores, geologic cores, rock outcrops and those inferred from climate models. New technologies for the coming decades of geoscience data collection are also highlighted. Ten keynote presentations at the symposium outline the foundation for the research sessions of the symposium and the structure of the Online Proceedings and Proceedings Book for the Tenth ISAES. \r\n\r\nThe ISAES is traditionally a cornerstone meeting for the Scientific Committee on Antarctic Research (SCAR). In recognition of the Tenth ISAES being held in the U.S. for the first time in 30 years and during IPY, the publication of the symposium proceedings is being handled as a special collaborative effort of the U.S. National Science Foundation, the U.S. Geological Survey, The National Academies Polar Research Board and The National Academies Press. The National Academies Polar Research Board oversees the activities of SCAR in the U.S. \r\n\r\nSpecial attention has been directed at publication formats for the symposium, to expedite the open and wide sharing of mature and preliminary research results presented in talks and posters at the Tenth ISAES. All symposium presentations are documented by a short Summary printed in the Symposium Program Booklet and either a short research paper or an extended abstract. The research papers and extended abstracts are compiled in this Online Proceedings and are replicated on a DVD-ROM that is placed in the back of the Tenth ISAES Proceedings Book. The Proceedings Book has printed versions of the keynote talks and an overview paper of the symposium. \r\n\r\nThe short research papers and extended abstracts have been handled differently. Research papers present mature research results and syntheses. They have been peer-reviewed using standard journal procedures. Following revisions and acceptances by co-editors, the papers have been formatted for publication and proofread by authors. Each paper has been assigned a Digital Object Identification (DOI) number and separate html link, and posted online (as part of this USGS Open-File Report series) to ensure open and wide access to the research results. \r\n\r\nExtended abstracts focus on preliminary research results and have not been peer reviewed. They have had only minimal editorial review and revision. Authors have formatted and proofread their papers. Extended abstracts were not given DOI numbers and are included together in a separate chapter of this online Proceedings. \r\n\r\nUSGS publications staff and Stanford-student editorial assistants indexed and compiled the PDF versions of the short research papers and extended abstracts for inclusion in this online Proceedings. USGS staff created the master DVD-ROM that contains a replica of the Online Proceedings for the Tenth ISAES, and provided the DVD-ROM copies that are included in the Tenth ISAES Proceedings Book published by The National Academies Press in the U.S. A team of more than 25 co-editors coordinated with the numerous authors and peer reviewers in handling the many research papers and extended abstracts that are included herein. Handling the large volume of short papers and extended abstracts, getting most of them onli","language":"ENGLISH","doi":"10.3133/of2007-1047","issn":"01961497 ","isbn":"1411317882 ","usgsCitation":"2007, Antarctica: A Keystone in a Changing World--Online Proceedings for the Tenth International Symposium on Antarctic Earth Sciences.  Santa Barbara, California, U.S.A.--August 26 to September 1, 2007 (Version 1.0): U.S. Geological Survey Open-File Report 2007-1047, DVD-ROM, https://doi.org/10.3133/of2007-1047.","productDescription":"DVD-ROM","temporalStart":"2007-08-26","temporalEnd":"2007-09-01","costCenters":[{"id":645,"text":"Western Coastal and Marine Geology","active":false,"usgs":true}],"links":[{"id":190495,"rank":0,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/thumbnails/ofr20071047.jpg"},{"id":9267,"rank":100,"type":{"id":15,"text":"Index Page"},"url":"https://pubs.usgs.gov/of/2007/1047/","linkFileType":{"id":5,"text":"html"}}],"geographicExtents":"{ \"type\": \"FeatureCollection\", \"features\": [ { \"type\": \"Feature\", \"properties\": {}, \"geometry\": { \"type\": \"Polygon\", \"coordinates\": [ [ [ 180,-90 ], [ 180,-57 ], [ -180,-57 ], [ -180,-90 ], [ 180,-90 ] ] ] } } ] }","edition":"Version 1.0","noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"4f4e4ac7e4b07f02db67b622","contributors":{"editors":[{"text":"Cooper, Alan","contributorId":74242,"corporation":false,"usgs":true,"family":"Cooper","given":"Alan","affiliations":[],"preferred":false,"id":504046,"contributorType":{"id":2,"text":"Editors"},"rank":1},{"text":"Raymond, Carol","contributorId":113907,"corporation":false,"usgs":true,"family":"Raymond","given":"Carol","affiliations":[],"preferred":false,"id":504048,"contributorType":{"id":2,"text":"Editors"},"rank":2},{"text":"ISAES Editorial Team","contributorId":128301,"corporation":true,"usgs":false,"organization":"ISAES Editorial Team","id":536185,"contributorType":{"id":2,"text":"Editors"},"rank":3}]}}
,{"id":70180921,"text":"70180921 - 2007 - Interannual covariability between actual evapotranspiration and PAL and GIMMS NDVIs of northern Asia","interactions":[],"lastModifiedDate":"2017-02-08T10:35:29","indexId":"70180921","displayToPublicDate":"2007-02-15T00:00:00","publicationYear":"2007","noYear":false,"publicationType":{"id":2,"text":"Article"},"publicationSubtype":{"id":10,"text":"Journal Article"},"seriesTitle":{"id":3254,"text":"Remote Sensing of Environment","printIssn":"0034-4257","active":true,"publicationSubtype":{"id":10}},"title":"Interannual covariability between actual evapotranspiration and PAL and GIMMS NDVIs of northern Asia","docAbstract":"<p><span>This study examined the covariability between interannual changes in the normalized difference vegetation index (NDVI) and actual evapotranspiration (ET). To reduce possible uncertainty in the NDVI time series, two NDVI datasets derived from Pathfinder AVHRR Land (PAL) data and the Global Inventory Monitoring and Modeling Studies (GIMMS) group were used. Analyses were conducted using data over northern Asia from 1982 to 2000. Interannual changes over 19&nbsp;years in the PAL-NDVI and GIMMS-NDVI were compared with interannual changes in ET estimated from model-assimilated atmospheric data and gridded precipitation data. For both NDVI datasets, the annual maximum correlation with ET occurred in June, which is the beginning of the vegetation growing season. The PAL and GIMMS datasets showed a significant, positive correlation between interannual changes in the NDVI and ET over most of the vegetated land area in June. These results suggest that interannual changes in vegetation activity predominantly control interannual changes in ET in June. Based on analyses of interannual changes in temperature, precipitation, and the NDVI in June, the study area can be roughly divided into two regions, the warmth-dominated northernmost region and the wetness-dominated southern region, indicating that interannual changes in vegetation and the resultant interannual changes in ET are controlled by warmth and wetness in these two regions, respectively.</span></p>","language":"English","publisher":"Elsevier","publisherLocation":"New York","doi":"10.1016/j.rse.2006.10.016","usgsCitation":"Suzuki, R., Masuda, K., and Dye, D.G., 2007, Interannual covariability between actual evapotranspiration and PAL and GIMMS NDVIs of northern Asia: Remote Sensing of Environment, v. 106, no. 3, p. 387-398, https://doi.org/10.1016/j.rse.2006.10.016.","productDescription":"13 p.","startPage":"387","endPage":"398","costCenters":[{"id":657,"text":"Western Geographic Science Center","active":true,"usgs":true}],"links":[{"id":334941,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/thumbnails/outside_thumb.jpg"}],"volume":"106","issue":"3","noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"589c3c3fe4b0efcedb741072","contributors":{"authors":[{"text":"Suzuki, Rikie","contributorId":179126,"corporation":false,"usgs":false,"family":"Suzuki","given":"Rikie","email":"","affiliations":[],"preferred":false,"id":662825,"contributorType":{"id":1,"text":"Authors"},"rank":1},{"text":"Masuda, Kooiti","contributorId":179127,"corporation":false,"usgs":false,"family":"Masuda","given":"Kooiti","email":"","affiliations":[],"preferred":false,"id":662826,"contributorType":{"id":1,"text":"Authors"},"rank":2},{"text":"Dye, Dennis G. 0000-0002-7100-272X ddye@usgs.gov","orcid":"https://orcid.org/0000-0002-7100-272X","contributorId":4233,"corporation":false,"usgs":true,"family":"Dye","given":"Dennis","email":"ddye@usgs.gov","middleInitial":"G.","affiliations":[{"id":657,"text":"Western Geographic Science Center","active":true,"usgs":true}],"preferred":true,"id":662827,"contributorType":{"id":1,"text":"Authors"},"rank":3}]}}
,{"id":79629,"text":"ofr20061395 - 2007 - Peak stages from backwater conditions at streamflow-gaging stations in and near South Dakota through water year 2001","interactions":[],"lastModifiedDate":"2017-10-14T14:18:45","indexId":"ofr20061395","displayToPublicDate":"2007-02-13T00:00:00","publicationYear":"2007","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":"2006-1395","title":"Peak stages from backwater conditions at streamflow-gaging stations in and near South Dakota through water year 2001","docAbstract":"Stream stages associated with the annual peak discharge are presented for 182 streamflow-gaging stations in and near South Dakota. The peak stage at a station can occur as the result of the annual maximum discharge, but also as the result of backwater conditions. Backwater, often caused by ice, can produce a peak stage higher than the stage coincident with annual maximum discharge. The U.S. Geological Survey has cooperated with the South Dakota Department of Transportation to prepare this report, which provides a summary of peak-stage data through water year 2001 for gaging stations in and near South Dakota where annual peak stages resulting from backwater conditions have exceeded stages associated with annual peak discharge by as much as several feet. Where applicable, data summaries include the flood stage that is assigned by the National Weather Service.\r\n\r\n","language":"English","publisher":"U.S. Geological Survey","doi":"10.3133/ofr20061395","collaboration":"Prepared in cooperation with the South Dakota Department of Transportation","usgsCitation":"Thompson, R.F., 2007, Peak stages from backwater conditions at streamflow-gaging stations in and near South Dakota through water year 2001: U.S. Geological Survey Open-File Report 2006-1395, iv, 55 p., https://doi.org/10.3133/ofr20061395.","productDescription":"iv, 55 p.","numberOfPages":"59","onlineOnly":"Y","costCenters":[{"id":562,"text":"South Dakota Water Science Center","active":true,"usgs":true},{"id":34685,"text":"Dakota Water Science Center","active":true,"usgs":true}],"links":[{"id":192105,"rank":0,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/thumbnails/usgs_thumb.jpg"},{"id":9258,"rank":100,"type":{"id":15,"text":"Index Page"},"url":"https://pubs.usgs.gov/of/2006/1395/","linkFileType":{"id":5,"text":"html"}}],"country":"United States","state":"South Dakota","noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"4f4e4ae1e4b07f02db688a31","contributors":{"authors":[{"text":"Thompson, Ryan F. 0000-0002-4544-6108 rcthomps@usgs.gov","orcid":"https://orcid.org/0000-0002-4544-6108","contributorId":2702,"corporation":false,"usgs":true,"family":"Thompson","given":"Ryan","email":"rcthomps@usgs.gov","middleInitial":"F.","affiliations":[{"id":562,"text":"South Dakota Water Science Center","active":true,"usgs":true},{"id":34685,"text":"Dakota Water Science Center","active":true,"usgs":true}],"preferred":true,"id":290419,"contributorType":{"id":1,"text":"Authors"},"rank":1}]}}
,{"id":79631,"text":"ofr20071022 - 2007 - Compositional Data for Bengal Delta Sediment Collected from a Borehole at Rajoir, Bangladesh","interactions":[],"lastModifiedDate":"2012-02-02T00:14:12","indexId":"ofr20071022","displayToPublicDate":"2007-02-13T00:00:00","publicationYear":"2007","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":"2007-1022","title":"Compositional Data for Bengal Delta Sediment Collected from a Borehole at Rajoir, Bangladesh","docAbstract":"Processes active within sediment of the Bengal basin have attracted world concern because of the locally high content of arsenic dissolved in ground water drawn from that sediment. Sediment samples were collected from a borehole in the town of Rajoir, Rajoir upazila, Madaripur district, Bangladesh, to investigate the processes contributing to arsenic contamination. The samples were mineralogically and chemically analyzed to determine compositional variations related to the arsenic content of the sediment. Mineralogy of the sediment was determined using powder X-ray diffraction. Bulk chemical composition was measured by Combustion; Inductively Coupled Plasma Atomic Emission Spectroscopy; Energy Dispersive X-ray Fluorescence; and Hydride Generation Atomic Absorption Spectrophotometry. Sediment was treated with 0.5 N HCl and resulting solutions were analyzed, primarily to evaluate the abundance and oxidation state of acid-soluble iron. Acid-volatile sulfide, acid-soluble sulfate, and reducible sulfide were also measured on a few samples. Sediment sampled at Rajoir is typically unlithified, gray, micaceous, feldspathic arenaceous sand with a few silt and clay layers. Arsenic content of the sediment ranges from 0.6 to 21 ppm with a median of 1.2 ppm.\r\n","language":"ENGLISH","doi":"10.3133/ofr20071022","collaboration":"In cooperation with the Geological Survey of Bangladesh and Bangladesh Water Development Board","usgsCitation":"Breit, G.N., Yount, J., Uddin, N., Muneem, A.A., Lowers, H., Berry, C.J., and Whitney, J.W., 2007, Compositional Data for Bengal Delta Sediment Collected from a Borehole at Rajoir, Bangladesh: U.S. Geological Survey Open-File Report 2007-1022, vi, 40 p., https://doi.org/10.3133/ofr20071022.","productDescription":"vi, 40 p.","numberOfPages":"46","onlineOnly":"Y","costCenters":[],"links":[{"id":190643,"rank":0,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/thumbnails/usgs_thumb.jpg"},{"id":9260,"rank":100,"type":{"id":15,"text":"Index Page"},"url":"https://pubs.usgs.gov/of/2007/1022/","linkFileType":{"id":5,"text":"html"}}],"noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"4f4e4b1ae4b07f02db6a7fdc","contributors":{"authors":[{"text":"Breit, George N. 0000-0003-2188-6798 gbreit@usgs.gov","orcid":"https://orcid.org/0000-0003-2188-6798","contributorId":1480,"corporation":false,"usgs":true,"family":"Breit","given":"George","email":"gbreit@usgs.gov","middleInitial":"N.","affiliations":[{"id":171,"text":"Central Mineral and Environmental Resources Science Center","active":true,"usgs":true},{"id":211,"text":"Crustal Geophysics and Geochemistry Science Center","active":true,"usgs":true}],"preferred":true,"id":290428,"contributorType":{"id":1,"text":"Authors"},"rank":1},{"text":"Yount, James C.","contributorId":39341,"corporation":false,"usgs":true,"family":"Yount","given":"James C.","affiliations":[],"preferred":false,"id":290429,"contributorType":{"id":1,"text":"Authors"},"rank":2},{"text":"Uddin, Nehal","contributorId":60721,"corporation":false,"usgs":true,"family":"Uddin","given":"Nehal","email":"","affiliations":[],"preferred":false,"id":290431,"contributorType":{"id":1,"text":"Authors"},"rank":3},{"text":"Muneem, Ad. Atual","contributorId":49873,"corporation":false,"usgs":true,"family":"Muneem","given":"Ad.","email":"","middleInitial":"Atual","affiliations":[],"preferred":false,"id":290430,"contributorType":{"id":1,"text":"Authors"},"rank":4},{"text":"Lowers, Heather 0000-0001-5360-9264 hlowers@usgs.gov","orcid":"https://orcid.org/0000-0001-5360-9264","contributorId":710,"corporation":false,"usgs":true,"family":"Lowers","given":"Heather","email":"hlowers@usgs.gov","affiliations":[{"id":211,"text":"Crustal Geophysics and Geochemistry Science Center","active":true,"usgs":true}],"preferred":false,"id":290425,"contributorType":{"id":1,"text":"Authors"},"rank":5},{"text":"Berry, Cyrus J. cjberry@usgs.gov","contributorId":946,"corporation":false,"usgs":true,"family":"Berry","given":"Cyrus","email":"cjberry@usgs.gov","middleInitial":"J.","affiliations":[{"id":171,"text":"Central Mineral and Environmental Resources Science Center","active":true,"usgs":true}],"preferred":true,"id":290427,"contributorType":{"id":1,"text":"Authors"},"rank":6},{"text":"Whitney, John W. 0000-0003-3824-3692 jwhitney@usgs.gov","orcid":"https://orcid.org/0000-0003-3824-3692","contributorId":804,"corporation":false,"usgs":true,"family":"Whitney","given":"John","email":"jwhitney@usgs.gov","middleInitial":"W.","affiliations":[{"id":318,"text":"Geosciences and Environmental Change Science Center","active":true,"usgs":true}],"preferred":true,"id":290426,"contributorType":{"id":1,"text":"Authors"},"rank":7}]}}
,{"id":79621,"text":"ds242 - 2007 - Archive of digital chirp seismic reflection data collected during USGS cruise 05SCC01 offshore of Port Fourchon and Timbalier Bay, Louisiana, August 2005","interactions":[],"lastModifiedDate":"2014-08-27T10:46:52","indexId":"ds242","displayToPublicDate":"2007-02-10T00:00:00","publicationYear":"2007","noYear":false,"publicationType":{"id":18,"text":"Report"},"publicationSubtype":{"id":5,"text":"USGS Numbered Series"},"seriesTitle":{"id":310,"text":"Data Series","code":"DS","onlineIssn":"2327-638X","printIssn":"2327-0271","active":false,"publicationSubtype":{"id":5}},"seriesNumber":"242","title":"Archive of digital chirp seismic reflection data collected during USGS cruise 05SCC01 offshore of Port Fourchon and Timbalier Bay, Louisiana, August 2005","docAbstract":"<p>In August of 2005, the U.S. Geological Survey conducted geophysical surveys offshore of Port Fourchon and Timbalier Bay, Louisiana, and in nearby waterbodies. This report serves as an archive of unprocessed digital chirp seismic reflection data, trackline maps, navigation files, GIS information, Field Activity Collection System (FACS) logs, observer's logbook, and formal FGDC metadata. Filtered and gained digital images of the seismic profiles are also provided. \nThe archived trace data are in standard Society of Exploration Geophysicists (SEG) SEG-Y format (Barry and others, 1975) and may be downloaded and processed with commercial or public domain software such as Seismic Unix (SU). Example SU processing scripts and USGS software for viewing the SEG-Y files (Zihlman, 1992) are also provided.</p>","language":"English","publisher":"U.S. Geological Survey","publisherLocation":"Reston, VA","doi":"10.3133/ds242","usgsCitation":"Harrison, A.S., Dadisman, S.V., Flocks, J.G., Wiese, D.S., and Calderon, K., 2007, Archive of digital chirp seismic reflection data collected during USGS cruise 05SCC01 offshore of Port Fourchon and Timbalier Bay, Louisiana, August 2005: U.S. Geological Survey Data Series 242, HTML Document, https://doi.org/10.3133/ds242.","productDescription":"HTML Document","costCenters":[{"id":186,"text":"Coastal and Marine Geology Program","active":true,"usgs":true}],"links":[{"id":192668,"rank":0,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/thumbnails/ds242.PNG"},{"id":9248,"rank":100,"type":{"id":15,"text":"Index Page"},"url":"https://pubs.usgs.gov/ds/2007/242/","linkFileType":{"id":5,"text":"html"}}],"country":"United States","state":"Louisiana","otherGeospatial":"Port Fourchon;Timbalier Bay","geographicExtents":"{ \"type\": \"FeatureCollection\", \"features\": [ { \"type\": \"Feature\", \"properties\": {}, \"geometry\": { \"type\": \"Polygon\", \"coordinates\": [ [ [ -90.418,29.0222 ], [ -90.418,29.1144 ], [ -89.956,29.1144 ], [ -89.956,29.0222 ], [ -90.418,29.0222 ] ] ] } } ] }","noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"4f4e4b05e4b07f02db699cc9","contributors":{"authors":[{"text":"Harrison, Arnell S. 0000-0002-5581-2255","orcid":"https://orcid.org/0000-0002-5581-2255","contributorId":35021,"corporation":false,"usgs":true,"family":"Harrison","given":"Arnell","email":"","middleInitial":"S.","affiliations":[],"preferred":false,"id":290402,"contributorType":{"id":1,"text":"Authors"},"rank":1},{"text":"Dadisman, Shawn V. sdadisman@usgs.gov","contributorId":2207,"corporation":false,"usgs":true,"family":"Dadisman","given":"Shawn","email":"sdadisman@usgs.gov","middleInitial":"V.","affiliations":[],"preferred":true,"id":290400,"contributorType":{"id":1,"text":"Authors"},"rank":2},{"text":"Flocks, James G. 0000-0002-6177-7433 jflocks@usgs.gov","orcid":"https://orcid.org/0000-0002-6177-7433","contributorId":816,"corporation":false,"usgs":true,"family":"Flocks","given":"James","email":"jflocks@usgs.gov","middleInitial":"G.","affiliations":[{"id":574,"text":"St. Petersburg Coastal and Marine Science Center","active":true,"usgs":true}],"preferred":true,"id":290399,"contributorType":{"id":1,"text":"Authors"},"rank":3},{"text":"Wiese, Dana S. dwiese@usgs.gov","contributorId":2476,"corporation":false,"usgs":true,"family":"Wiese","given":"Dana","email":"dwiese@usgs.gov","middleInitial":"S.","affiliations":[{"id":574,"text":"St. Petersburg Coastal and Marine Science Center","active":true,"usgs":true}],"preferred":true,"id":290401,"contributorType":{"id":1,"text":"Authors"},"rank":4},{"text":"Calderon, Karynna","contributorId":92739,"corporation":false,"usgs":true,"family":"Calderon","given":"Karynna","email":"","affiliations":[],"preferred":false,"id":290403,"contributorType":{"id":1,"text":"Authors"},"rank":5}]}}
,{"id":79620,"text":"ofr20061046 - 2007 - Surficial sediment character of the New York-New Jersey offshore continental shelf region: A GIS compilation","interactions":[],"lastModifiedDate":"2023-01-18T22:49:36.347276","indexId":"ofr20061046","displayToPublicDate":"2007-02-10T00:00:00","publicationYear":"2007","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":"2006-1046","title":"Surficial sediment character of the New York-New Jersey offshore continental shelf region: A GIS compilation","docAbstract":"<p>Broad continental shelf regions such as the New York Bight are the product of a complex geologic history and dynamic oceanographic processes, dominated by the Holocene marine transgression (>100 m sea-level rise) following the end of the last Pleistocene ice advance ~ 20,000 years ago. The area of the U.S. Exclusive Economic Zone (U.S. EEZ) territory, extending 200 nautical miles seaward from the coast, is larger than the continental U.S. and contains submerged landforms that provide a variety of natural functions and societal benefits, such as: critical habitats for fisheries, ship navigation and homeland security, and engineering activities (i.e. oil and gas platforms, pipeline and cable routes, potential wind-energy-generation sites).</p>\n<br> \n<p>Some parts of the continental margins, particularly inner-continental shelf regions, also contain unconsolidated hard-mineral deposits such as sand and gravel that are regarded as potential aggregate resources to meet or augment needs not met by onshore deposits (Williams, 1992). The present distribution of surficial sediment off the northeastern United States is shaped from the deposits left by the last glaciation and reflects the cumulative effects of sediment erosion, transport, sorting, and deposition by storm and tidal processes during the Holocene rise in sea level. As a result, the sediments on the sea floor represent both an historical record of former conditions and a guide to possible future sedimentary environments.</p>\n<br>\n<p>The U.S. Geological Survey (USGS) through the Coastal and Marine Geology Program, in cooperation with the University of Colorado and other partners, has compiled extant sediment character and textural data as well as other geologic information on the sea floor from all regions around the U.S. into the usSEABED data system (Reid and others, 2005; Buczkowski and others, 2006; Reid and others, 2006). The usSEABED system, which contains information on sediment grain size and lithology for more than 340,500 stations within the U.S. EEZ. has been developed and populated with data as part of the USGS Marine Aggregate Resources and Processes and the National Benthic Habitats projects in order to provide the base-line data needed to update the current maps of offshore surficial geologic character and sediment distribution. The maps are also used to characterize benthic sea floor environments important for marine ecosystems.</p>\n<br>\n<p>U.S. Geological Survey, Data Series 118 (Reid and others, 2005), of the usSEABED data release series, represents the combined efforts of the USGS and several other government agencies to provide a unified resource for accessing and preserving records of U.S. east coast sea floor geologic information and sediment texture data.</p> \n<br>\n<p>For this present report, we have chosen to focus on the New York-New Jersey region, an area that has been intensely studied by the USGS for many years to address many complex issues.</p>\n<br>\n<p>This report illustrates the uses of the usSEABED database for GIS applications, while offering additional insight into the resources and data available from the USGS and its collaborative institutions.</p>\n<br>\n<p>This report is based on data contained in U.S. Geological Survey Data Series 118 (Reid and others, 2005) and shows an assortment of example GIS products that are possible using usSEABED. All data are intended to be GIS-ready and should not require any additional cleanup, formatting, or renaming of fields in order to use the data in a Geographic Information System. This project employs the Environmental Systems Research Institute's (ESRI) ArcView™ software. Many of these maps were made as part of the ongoing USGS study to assess marine aggregate resources offshore New York and New Jersey, but these maps can serve many other purposes. The marine science community, educators, students and others are encouraged to use these data to generate GIS products for their own purposes.</p>\n<br>\n<p>The objectives of the Marine Aggregate Resources and Processes project are to produce a series of new geologic maps and reports of the sea floor that will provide scientific insights into the character and geologic development of U.S. continental margins and to use these maps and information to assess the potential availability of offshore sand and gravel resources. The mapping and aggregate resource assessments are being conducted on a national scale using the usSEABED data base as described in Williams and others (2003). Potential uses for these data include: (1) defining the geological variability of the sea floor in relation to benthic habitat diversity; (2) improving our understanding of the processes that control the distribution and transport of bottom sediments and benthic habitats; (3) locating aggregate resources for beach nourishment and industrial applications; and (4) providing a detailed geospatial framework for future marine science research, monitoring, and management activities. The initial assessments are in progress for the New York Bight and Louisiana offshore areas.</p>","language":"English","publisher":"U.S. Geological Survey","publisherLocation":"Reston, VA","doi":"10.3133/ofr20061046","usgsCitation":"Williams, S.J., Arsenault, M.A., Poppe, L., Reid, J.A., Reid, J.M., and Jenkins, C.J., 2007, Surficial sediment character of the New York-New Jersey offshore continental shelf region: A GIS compilation: U.S. Geological Survey Open-File Report 2006-1046, 74 p., https://doi.org/10.3133/ofr20061046.","productDescription":"74 p.","numberOfPages":"74","additionalOnlineFiles":"Y","costCenters":[{"id":186,"text":"Coastal and Marine Geology Program","active":true,"usgs":true},{"id":520,"text":"Pacific Coastal and Marine Science Center","active":true,"usgs":true},{"id":678,"text":"Woods Hole Coastal and Marine Science Center","active":true,"usgs":true}],"links":[{"id":195536,"rank":1,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/thumbnails/ofr20061046.PNG"},{"id":412051,"rank":4,"type":{"id":36,"text":"NGMDB Index Page"},"url":"https://ngmdb.usgs.gov/Prodesc/proddesc_80666.htm","linkFileType":{"id":5,"text":"html"}},{"id":295126,"rank":2,"type":{"id":11,"text":"Document"},"url":"https://pubs.usgs.gov/of/2006/1046/htmldocs/images/pdf/report.pdf","linkFileType":{"id":1,"text":"pdf"}},{"id":9246,"rank":3,"type":{"id":15,"text":"Index Page"},"url":"https://pubs.usgs.gov/of/2006/1046/","linkFileType":{"id":5,"text":"html"}}],"country":"United States","state":"New Jersey, New York","geographicExtents":"{\n  \"type\": \"FeatureCollection\",\n  \"features\": [\n    {\n      \"type\": \"Feature\",\n      \"properties\": {},\n      \"geometry\": {\n        \"coordinates\": [\n          [\n            [\n              -75.48869077222176,\n              41.37104207310469\n            ],\n            [\n              -75.48869077222176,\n              38.85910355852292\n            ],\n            [\n              -71.10831522330642,\n              38.85910355852292\n            ],\n            [\n              -71.10831522330642,\n              41.37104207310469\n            ],\n            [\n              -75.48869077222176,\n              41.37104207310469\n            ]\n          ]\n        ],\n        \"type\": \"Polygon\"\n      }\n    }\n  ]\n}","noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"4f4e4ae3e4b07f02db6893b6","contributors":{"authors":[{"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":290393,"contributorType":{"id":1,"text":"Authors"},"rank":1},{"text":"Arsenault, Matthew A.","contributorId":22872,"corporation":false,"usgs":true,"family":"Arsenault","given":"Matthew","email":"","middleInitial":"A.","affiliations":[],"preferred":false,"id":290397,"contributorType":{"id":1,"text":"Authors"},"rank":2},{"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":290394,"contributorType":{"id":1,"text":"Authors"},"rank":3},{"text":"Reid, Jane A. 0000-0003-1771-3894 jareid@usgs.gov","orcid":"https://orcid.org/0000-0003-1771-3894","contributorId":2826,"corporation":false,"usgs":true,"family":"Reid","given":"Jane","email":"jareid@usgs.gov","middleInitial":"A.","affiliations":[{"id":520,"text":"Pacific Coastal and Marine Science Center","active":true,"usgs":true}],"preferred":true,"id":290395,"contributorType":{"id":1,"text":"Authors"},"rank":4},{"text":"Reid, Jamey M.","contributorId":68386,"corporation":false,"usgs":true,"family":"Reid","given":"Jamey","email":"","middleInitial":"M.","affiliations":[],"preferred":false,"id":290398,"contributorType":{"id":1,"text":"Authors"},"rank":5},{"text":"Jenkins, Chris J.","contributorId":14066,"corporation":false,"usgs":false,"family":"Jenkins","given":"Chris","email":"","middleInitial":"J.","affiliations":[],"preferred":false,"id":290396,"contributorType":{"id":1,"text":"Authors"},"rank":6}]}}
,{"id":79624,"text":"tm4E1 - 2007 - Guidelines for preparation of State water-use estimates for 2005","interactions":[],"lastModifiedDate":"2012-02-02T00:14:22","indexId":"tm4E1","displayToPublicDate":"2007-02-10T00:00:00","publicationYear":"2007","noYear":false,"publicationType":{"id":18,"text":"Report"},"publicationSubtype":{"id":5,"text":"USGS Numbered Series"},"seriesTitle":{"id":335,"text":"Techniques and Methods","code":"TM","onlineIssn":"2328-7055","printIssn":"2328-7047","active":true,"publicationSubtype":{"id":5}},"seriesNumber":"4-E1","title":"Guidelines for preparation of State water-use estimates for 2005","docAbstract":"The U.S. Geological Survey (USGS) has estimated the use of water in the United States at 5-year intervals since 1950. This report describes the water-use categories and data elements required for the 2005 national water-use compilation conducted as part of the USGS National Water Use Information Program. The report identifies sources of water-use information, provides standard methods and techniques for estimating water use at the county level, and outlines steps for preparing documentation for the United States, the District of Columbia, Puerto Rico, and the U.S. Virgin Islands.\r\n\r\nAs part of this USGS program to document water use on a national scale for the year 2005, estimates of water withdrawals for the categories of public supply, self-supplied domestic, industrial, irrigation, and thermoelectric power at the county level are prepared for each State using the guidelines in this report. Estimates of water withdrawals for aquaculture, livestock, and mining are prepared for each State using a county-based national model, although study chiefs in each State have the option of producing independent county estimates of water withdrawals for these categories. Estimates of deliveries of water from public supplies for domestic use by county also will be prepared for each State for 2005. As a result, domestic water use can be determined for each State by combining self-supplied domestic withdrawals and publicly supplied domestic deliveries. Fresh ground-water and surfacewater estimates will be prepared for all categories of use; and saline ground-water and surface-water estimates by county will be prepared for the categories of public supply, industrial, and thermoelectric power. Power production for thermoelectric power will be compiled for 2005. If data are available, reclaimed wastewater use will be compiled for the industrial and irrigation categories.\r\n\r\nOptional water-use categories are commercial, hydroelectric power, and wastewater treatment. Optional data elements are public-supply deliveries to commercial, industrial, and thermoelectric-power users; consumptive use; irrigation conveyance loss; and number of facilities. Aggregation of water-use data by eight-digit hydrologic cataloging unit and by principal aquifer also is optional.\r\n\r\nWater-use data compiled by the States will be stored in the USGS Aggregate Water-Use Data System (AWUDS). This database is a comprehensive aggregated database designed to store both mandatory and optional data elements. AWUDS contains several routines that can be used for quality assurance and quality control of the data, and produces tables of wateruse data compiled for 1985, 1990, 1995, and 2000.\r\n","language":"ENGLISH","doi":"10.3133/tm4E1","collaboration":"Book 4, Chapter E1","usgsCitation":"Hutson, S.S., 2007, Guidelines for preparation of State water-use estimates for 2005: U.S. Geological Survey Techniques and Methods 4-E1, viii, 28 p., https://doi.org/10.3133/tm4E1.","productDescription":"viii, 28 p.","numberOfPages":"36","onlineOnly":"Y","costCenters":[{"id":494,"text":"Office of Groundwater","active":false,"usgs":true}],"links":[{"id":194445,"rank":0,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/thumbnails/usgs_thumb.jpg"},{"id":9252,"rank":100,"type":{"id":15,"text":"Index Page"},"url":"https://pubs.usgs.gov/tm/2007/tm4e1/","linkFileType":{"id":5,"text":"html"}}],"noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"4f4e4a51e4b07f02db62a088","contributors":{"authors":[{"text":"Hutson, Susan S. sshutson@usgs.gov","contributorId":2040,"corporation":false,"usgs":true,"family":"Hutson","given":"Susan","email":"sshutson@usgs.gov","middleInitial":"S.","affiliations":[{"id":374,"text":"Maryland Water Science Center","active":true,"usgs":true}],"preferred":true,"id":290408,"contributorType":{"id":1,"text":"Authors"},"rank":1}]}}
,{"id":79618,"text":"ofr20071029 - 2007 - Landsat ETM+ False-Color Image Mosaics of Afghanistan","interactions":[],"lastModifiedDate":"2012-02-02T00:14:19","indexId":"ofr20071029","displayToPublicDate":"2007-02-08T00:00:00","publicationYear":"2007","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":"2007-1029","title":"Landsat ETM+ False-Color Image Mosaics of Afghanistan","docAbstract":"In 2005, the U.S. Agency for International Development and the U.S. Trade and Development Agency contracted with the U.S. Geological Survey to perform assessments of the natural resources within Afghanistan. The assessments concentrate on the resources that are related to the economic development of that country. Therefore, assessments were initiated in oil and gas, coal, mineral resources, water resources, and earthquake hazards. All of these assessments require geologic, structural, and topographic information throughout the country at a finer scale and better accuracy than that provided by the existing maps, which were published in the 1970's by the Russians and Germans. The very rugged terrain in Afghanistan, the large scale of these assessments, and the terrorist threat in Afghanistan indicated that the best approach to provide the preliminary assessments was to use remotely sensed, satellite image data, although this may also apply to subsequent phases of the assessments. Therefore, the first step in the assessment process was to produce satellite image mosaics of Afghanistan that would be useful for these assessments. This report discusses the production of the Landsat false-color image database produced for these assessments, which was produced from the calibrated Landsat ETM+ image mosaics described by Davis (2006).","language":"ENGLISH","doi":"10.3133/ofr20071029","usgsCitation":"Davis, P.A., 2007, Landsat ETM+ False-Color Image Mosaics of Afghanistan (Version 1.0): U.S. Geological Survey Open-File Report 2007-1029, 22 p., https://doi.org/10.3133/ofr20071029.","productDescription":"22 p.","numberOfPages":"22","costCenters":[{"id":131,"text":"Astrogeology Science Center","active":true,"usgs":true}],"links":[{"id":194640,"rank":0,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/thumbnails/usgs_thumb.jpg"},{"id":9243,"rank":100,"type":{"id":15,"text":"Index Page"},"url":"https://pubs.usgs.gov/of/2007/1029/","linkFileType":{"id":5,"text":"html"}}],"edition":"Version 1.0","noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"4f4e4b23e4b07f02db6adee4","contributors":{"authors":[{"text":"Davis, Philip A. pdavis@usgs.gov","contributorId":692,"corporation":false,"usgs":true,"family":"Davis","given":"Philip","email":"pdavis@usgs.gov","middleInitial":"A.","affiliations":[],"preferred":true,"id":290390,"contributorType":{"id":1,"text":"Authors"},"rank":1}]}}
,{"id":70202249,"text":"70202249 - 2007 - Global spatial deconvolution of Lunar Prospector Th abundances","interactions":[],"lastModifiedDate":"2019-02-18T11:16:10","indexId":"70202249","displayToPublicDate":"2007-02-07T11:14:06","publicationYear":"2007","noYear":false,"publicationType":{"id":2,"text":"Article"},"publicationSubtype":{"id":10,"text":"Journal Article"},"seriesTitle":{"id":1807,"text":"Geophysical Research Letters","active":true,"publicationSubtype":{"id":10}},"title":"Global spatial deconvolution of Lunar Prospector Th abundances","docAbstract":"<p><span>We have completed the first global spatial deconvolution analysis of planetary gamma‐ray data for lunar Th abundances as measured by the Lunar Prospector Gamma‐ray Spectrometer. We tested two different spatial deconvolution techniques – Jansson's method and the Pixon method – and determined that the Pixon method provides superior performance. The final deconvolved map results in a spatial resolution improvement of a factor of 1.5–2. The newly deconvolved data allow us to clearly delineate nearside Th enhancements and depressions, validate enhanced Th abundances associated with specific lunar red spots, and reveal new details of the Th distribution at the Aristarchus plateau.</span></p>","language":"English","publisher":"American Geophysical Union","publisherLocation":"Washington, D.C.","doi":"10.1029/2006GL028530","usgsCitation":"Lawrence, D.J., Puetter, R., Elphic, R., Feldman, W.C., Hagerty, J., Prettyman, T.H., and Spudis, P.D., 2007, Global spatial deconvolution of Lunar Prospector Th abundances: Geophysical Research Letters, v. 34, no. 3, 5 p., https://doi.org/10.1029/2006GL028530.","productDescription":"5 p.","costCenters":[{"id":131,"text":"Astrogeology Science Center","active":true,"usgs":true}],"links":[{"id":361316,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/thumbnails/outside_thumb.jpg"}],"volume":"34","issue":"3","noUsgsAuthors":false,"publicationDate":"2007-02-07","publicationStatus":"PW","contributors":{"authors":[{"text":"Lawrence, D. J.","contributorId":84952,"corporation":false,"usgs":false,"family":"Lawrence","given":"D.","email":"","middleInitial":"J.","affiliations":[],"preferred":false,"id":757487,"contributorType":{"id":1,"text":"Authors"},"rank":1},{"text":"Puetter, R.C.","contributorId":213336,"corporation":false,"usgs":false,"family":"Puetter","given":"R.C.","email":"","affiliations":[],"preferred":false,"id":757488,"contributorType":{"id":1,"text":"Authors"},"rank":2},{"text":"Elphic, R.C.","contributorId":101061,"corporation":false,"usgs":true,"family":"Elphic","given":"R.C.","email":"","affiliations":[],"preferred":false,"id":757489,"contributorType":{"id":1,"text":"Authors"},"rank":3},{"text":"Feldman, W. C.","contributorId":40767,"corporation":false,"usgs":false,"family":"Feldman","given":"W.","email":"","middleInitial":"C.","affiliations":[],"preferred":false,"id":757490,"contributorType":{"id":1,"text":"Authors"},"rank":4},{"text":"Hagerty, Justin 0000-0003-3800-7948 jhagerty@usgs.gov","orcid":"https://orcid.org/0000-0003-3800-7948","contributorId":911,"corporation":false,"usgs":true,"family":"Hagerty","given":"Justin","email":"jhagerty@usgs.gov","affiliations":[{"id":131,"text":"Astrogeology Science Center","active":true,"usgs":true}],"preferred":true,"id":757491,"contributorType":{"id":1,"text":"Authors"},"rank":5},{"text":"Prettyman, Thomas H.","contributorId":197551,"corporation":false,"usgs":false,"family":"Prettyman","given":"Thomas","email":"","middleInitial":"H.","affiliations":[],"preferred":false,"id":757492,"contributorType":{"id":1,"text":"Authors"},"rank":6},{"text":"Spudis, P. D.","contributorId":58719,"corporation":false,"usgs":true,"family":"Spudis","given":"P.","email":"","middleInitial":"D.","affiliations":[{"id":12445,"text":"Lunar and Planetary Institute","active":true,"usgs":false}],"preferred":false,"id":757493,"contributorType":{"id":1,"text":"Authors"},"rank":7}]}}
,{"id":79617,"text":"sir20065318 - 2007 - A Deep Percolation Model for Estimating Ground-Water Recharge: Documentation of Modules for the Modular Modeling System of the U.S. Geological Survey","interactions":[],"lastModifiedDate":"2012-03-08T17:16:20","indexId":"sir20065318","displayToPublicDate":"2007-02-07T00:00:00","publicationYear":"2007","noYear":false,"publicationType":{"id":18,"text":"Report"},"publicationSubtype":{"id":5,"text":"USGS Numbered Series"},"seriesTitle":{"id":334,"text":"Scientific Investigations Report","code":"SIR","onlineIssn":"2328-0328","printIssn":"2328-031X","active":true,"publicationSubtype":{"id":5}},"seriesNumber":"2006-5318","title":"A Deep Percolation Model for Estimating Ground-Water Recharge: Documentation of Modules for the Modular Modeling System of the U.S. Geological Survey","docAbstract":"A daily water-budget model for estimating ground-water recharge, the Deep Percolation Model, was modularized for inclusion into the U.S. Geological Survey's Modular Modeling System. The model was modularized in order to facilitate estimation of ground-water recharge under a large range in climatic, landscape, and land-use and land-cover conditions. The model can be applied to areas as large as regions or as small as a field plot.\r\n\r\nAn overview of the Modular Modeling System and the Deep Percolation Model is presented. Data requirements, parameters, and variables for the model are described. The modules that compose the Deep Percolation Model are documented.\r\n\r\n","language":"ENGLISH","doi":"10.3133/sir20065318","collaboration":"Prepared in cooperation with the Bureau of Reclamation, Yakama Nation, and Washington State Department of Ecology","usgsCitation":"Vaccaro, J.J., 2007, A Deep Percolation Model for Estimating Ground-Water Recharge: Documentation of Modules for the Modular Modeling System of the U.S. Geological Survey: U.S. Geological Survey Scientific Investigations Report 2006-5318, iv, 30 p., https://doi.org/10.3133/sir20065318.","productDescription":"iv, 30 p.","numberOfPages":"34","costCenters":[{"id":622,"text":"Washington Water Science Center","active":true,"usgs":true}],"links":[{"id":191982,"rank":0,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/thumbnails/usgs_thumb.jpg"},{"id":9240,"rank":100,"type":{"id":15,"text":"Index Page"},"url":"https://pubs.usgs.gov/sir/2006/5318/","linkFileType":{"id":5,"text":"html"}}],"noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"53cd4952e4b0b290850ef0d1","contributors":{"authors":[{"text":"Vaccaro, J. J.","contributorId":48173,"corporation":false,"usgs":true,"family":"Vaccaro","given":"J.","email":"","middleInitial":"J.","affiliations":[],"preferred":false,"id":290389,"contributorType":{"id":1,"text":"Authors"},"rank":1}]}}
,{"id":79616,"text":"ofr20071011 - 2007 - Circulation and physical processes within the San Gabriel River Estuary during summer 2005","interactions":[],"lastModifiedDate":"2014-09-11T13:58:43","indexId":"ofr20071011","displayToPublicDate":"2007-02-07T00:00:00","publicationYear":"2007","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":"2007-1011","title":"Circulation and physical processes within the San Gabriel River Estuary during summer 2005","docAbstract":"<p>The Southern California Coastal Water Research Project (SCCWRP) is developing a hydrodynamic model of the SGR estuary, which is part of the comprehensive water-quality model of the SGR estuary and watershed investigated by SCCWRP and other local agencies. The hydrodynamic model will help understanding of 1) the exchange processes between the estuary and coastal ocean; 2) the circulation patterns in the estuary; 3) upstream natural runoff and the cooling discharge from PGS.</p>\n<br>\n<p>Like all models, the SGR hydrodynamic model is only useful after it is fully calibrated and validated. In May 2005, SCCWRP requested the assistance of the U.S. geological Survey (USGS) Coastal and Marine Geology team (CMG) in collecting data on the hydrodynamic conditions in the estuary during the summer dry season. The summer was chosen for field data collection as this was assumed to be the season with the greatest potential for chronic degraded water quality due to low river flow and high thermal stratification within the estuary (due to both higher average air temperature and PGS output). Water quality can be degraded in winter as well, when higher river discharge events bring large volumes of water from the Los Angeles basin into the estuary. The objectives of this project were to 1) collect hydrodynamic data along the SGR estuary; 2) study exchange processes within the estuary through analysis of the hydrodynamic data; and 3) provide field data for model calibration and validation. As the data only exist for the summer season, the results herein only apply to summer conditions.</p>","language":"English","publisher":"U.S. Geological Survey","publisherLocation":"Reston, VA","doi":"10.3133/ofr20071011","usgsCitation":"Rosenberger, K., Xu, J., Stein, E.D., Noble, M.A., and Gartner, A.L., 2007, Circulation and physical processes within the San Gabriel River Estuary during summer 2005 (Version 1.0): U.S. Geological Survey Open-File Report 2007-1011, Report: 48 p.; Appendix: 66 p., https://doi.org/10.3133/ofr20071011.","productDescription":"Report: 48 p.; Appendix: 66 p.","temporalStart":"2005-05-01","temporalEnd":"2005-10-31","costCenters":[{"id":645,"text":"Western Coastal and Marine Geology","active":false,"usgs":true}],"links":[{"id":190748,"rank":0,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/thumbnails/ofr20071011.PNG"},{"id":9239,"rank":100,"type":{"id":15,"text":"Index Page"},"url":"https://pubs.usgs.gov/of/2007/1011/","linkFileType":{"id":5,"text":"html"}},{"id":293761,"type":{"id":3,"text":"Appendix"},"url":"https://pubs.usgs.gov/of/2007/1011/of2007-1011Appendices.pdf"},{"id":293760,"type":{"id":11,"text":"Document"},"url":"https://pubs.usgs.gov/of/2007/1011/of2007-1011.pdf"}],"country":"United States","state":"California","otherGeospatial":"San Gabriel River Estuary","geographicExtents":"{ \"type\": \"FeatureCollection\", \"features\": [ { \"type\": \"Feature\", \"properties\": {}, \"geometry\": { \"type\": \"Polygon\", \"coordinates\": [ [ [ -118.25,33.666667 ], [ -118.25,33.75 ], [ -118.0,33.75 ], [ -118.0,33.666667 ], [ -118.25,33.666667 ] ] ] } } ] }","edition":"Version 1.0","noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"4f4e4abce4b07f02db672cb4","contributors":{"authors":[{"text":"Rosenberger, Kurt J.","contributorId":12934,"corporation":false,"usgs":true,"family":"Rosenberger","given":"Kurt J.","affiliations":[],"preferred":false,"id":290386,"contributorType":{"id":1,"text":"Authors"},"rank":1},{"text":"Xu, Jingping jpx@usgs.gov","contributorId":2574,"corporation":false,"usgs":true,"family":"Xu","given":"Jingping","email":"jpx@usgs.gov","affiliations":[{"id":520,"text":"Pacific Coastal and Marine Science Center","active":true,"usgs":true}],"preferred":true,"id":290385,"contributorType":{"id":1,"text":"Authors"},"rank":2},{"text":"Stein, Eric D.","contributorId":20023,"corporation":false,"usgs":true,"family":"Stein","given":"Eric","email":"","middleInitial":"D.","affiliations":[],"preferred":false,"id":290387,"contributorType":{"id":1,"text":"Authors"},"rank":3},{"text":"Noble, Marlene A. mnoble@usgs.gov","contributorId":1429,"corporation":false,"usgs":true,"family":"Noble","given":"Marlene","email":"mnoble@usgs.gov","middleInitial":"A.","affiliations":[{"id":520,"text":"Pacific Coastal and Marine Science Center","active":true,"usgs":true}],"preferred":true,"id":290384,"contributorType":{"id":1,"text":"Authors"},"rank":4},{"text":"Gartner, Anne L.","contributorId":32620,"corporation":false,"usgs":true,"family":"Gartner","given":"Anne","email":"","middleInitial":"L.","affiliations":[],"preferred":false,"id":290388,"contributorType":{"id":1,"text":"Authors"},"rank":5}]}}
,{"id":79614,"text":"ofr20061387 - 2007 - Status review of the Marbled Murrelet (Brachyramphus marmoratus) in Alaska and British Columbia","interactions":[],"lastModifiedDate":"2020-11-04T15:14:20.775367","indexId":"ofr20061387","displayToPublicDate":"2007-02-04T00:00:00","publicationYear":"2007","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":"2006-1387","displayTitle":"Status review of the Marbled Murrelet (<i>Brachyramphus marmoratus</i>) in Alaska and British Columbia","title":"Status review of the Marbled Murrelet (Brachyramphus marmoratus) in Alaska and British Columbia","docAbstract":"<p><span>The Marbled Murrelet (</span><i>Brachyramphus marmoratus</i><span>) is a small, diving seabird inhabiting inshore waters of the Northeastern Pacific Ocean. This species feeds on small, schooling fishes and zooplankton, and nests primarily on the moss-covered branches of large, old-growth conifers, and also, in some parts of its range, on the ground. We reviewed existing information on this species to evaluate its current status in the northern part of its range—Alaska (U.S.) and British Columbia (Canada). Within the southern part of its range (Washington, Oregon, and California, U.S.), the Marbled Murrelet was listed as a threatened species under the Endangered Species Act (ESA) in 1993, and the U.S. Fish and Wildlife Service (USFWS) needed information on the species throughout its range for ESA deliberations. We compiled published information on the conservation status, population biology, foraging ecology, population genetics, population status and trends, demography, marine and nesting habitat characteristics, threats, and ongoing conservation efforts for Marbled Murrelets in Alaska and British Columbia. We conducted a new genetic study using samples from a segment of the range that had not been included in previous studies (Washington, Oregon) and additional nuclear intron and microsatellite markers. We also analyzed available at-sea survey data from several locations for trend. To understand the reasonableness of the empirical trend data, we developed demographic models incorporating stochasticity to discern what population trends were possible by chance. The genetic studies substantially confirmed previous findings on population structure in the Marbled Murrelet. Our present work finds three populations: (1) one comprising birds in the central and western Aleutian Islands; (2) one comprising birds in central California; and (3)&nbsp;one comprising birds within the center of the range from the eastern Aleutians to northern California. Our knowledge of genetic structure within this central population is limited and it requires additional study. Compiling available abundance information, we estimated that in the recent past, Marbled Murrelets in Alaska numbered on the order of 1 million birds. We were unable to generate a similar estimate for historical population size in British Columbia. Using trend information from at-sea surveys spanning a wide geographic range in Alaska, murrelet numbers declined significantly at five of eight trend sites at annual rates of -5.4 to -12.7 percent since the early 1990s. Applying these rates of decline to the historical population estimate, the current murrelet population in Alaska is projected to be on the order of 270,000 birds. This represents an overall population decline of about 70 percent during the past 25 years. In British Columbia, available trend data indicate that murrelet populations there have experienced similar declines. We updated a recent (2002) population estimate for British Columbia, concluding that there are now between 54,000 and 92,000 murrelets in British Columbia. The rates of decline we observed are within, but at the high end of, a range of rates expected by chance. Given that declines were estimated for sites over essentially the entire northern range of the species, there is cause for concern about the species’ status. In their marine habitats, Marbled Murrelets overlap with salmon (Oncorhynchus sp.) gillnetting operations in British Columbia and in Alaska (especially in Prince William Sound and Southeast Alaska), and annual bycatch mortality is likely in the low thousands per year, although bycatch rates are difficult to measure. The species’ inshore distribution coincides with high levels of vessel traffic and makes them especially vulnerable to both chronic oil pollution and to catastrophic spills (e.g., the 1989&nbsp;</span><i>Exxon Valdez</i><span>&nbsp;oil spill [EVOS] in south-central Alaska, which is estimated to have killed 12,000 to 15,000 murrelets). In their forested nesting habitats, Marbled Murrelets have lost about 15 percent of their suitable nesting habitat in Southeast Alaska, and 33 to 49 percent in British Columbia, from industrial-scale logging within the past half century. Increased predation also may be a threat to murrelet populations, related to fragmentation and edge effects from logging and development, and recent population increases observed for some important murrelet predators, including Bald Eagles (</span><i>Haliaeetus leucocephalus</i><span>), Common Ravens (</span><i>Corvus corax</i><span>), and Steller’s Jays (</span><i>Cyanocitta stelleri</i><span>). Nesting habitat losses cannot explain the declines observed in areas where industrial logging has not occurred on a large scale (e.g., Prince William Sound) or at all (Glacier Bay). The apparent change in population size and rates of decline reported for the Marbled Murrelet are large, and we therefore considered alternative explanations and precedents for changes of similar magnitude in other marine wildlife populations in the Northeastern Pacific Ocean. The declines are likely real, and related to combined and cumulative effects from climate-related changes in the marine ecosystem (most likely the 1977 regime shift) and human activities (logging, gillnet bycatch, oil pollution). Much uncertainty about the decline could be alleviated by continuing to repeat boat surveys in Prince William Sound and lower Cook Inlet, and by repeating the boat survey of Southeast Alaska that was conducted in 1994. This survey used a statistically sound design and covered the region that has been and likely remains the center of the species’ abundance. Important questions remain to be addressed about methods for measuring population status and change, adult mortality (major sources, density dependence, seasonal concordance), and the movements of wintering populations.</span></p>","language":"English","publisher":"U.S. Geological Survey","publisherLocation":"Reston, VA","doi":"10.3133/ofr20061387","usgsCitation":"Piatt, J.F., Kuletz, K., Burger, A., Hatch, S.A., Friesen, V.L., Birt, T., Arimitsu, M.L., Drew, G., Harding, A., and Bixler, K., 2007, Status review of the Marbled Murrelet (Brachyramphus marmoratus) in Alaska and British Columbia: U.S. Geological Survey Open-File Report 2006-1387, xiv, 258 p., https://doi.org/10.3133/ofr20061387.","productDescription":"xiv, 258 p.","numberOfPages":"274","costCenters":[{"id":116,"text":"Alaska Science Center Biology 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,{"id":79611,"text":"tm4A6 - 2007 - The National Streamflow Statistics Program: A Computer Program for Estimating Streamflow Statistics for Ungaged Sites","interactions":[],"lastModifiedDate":"2023-03-10T13:02:12.06327","indexId":"tm4A6","displayToPublicDate":"2007-02-04T00:00:00","publicationYear":"2007","noYear":false,"publicationType":{"id":18,"text":"Report"},"publicationSubtype":{"id":5,"text":"USGS Numbered Series"},"seriesTitle":{"id":335,"text":"Techniques and Methods","code":"TM","onlineIssn":"2328-7055","printIssn":"2328-7047","active":true,"publicationSubtype":{"id":5}},"seriesNumber":"4-A6","title":"The National Streamflow Statistics Program: A Computer Program for Estimating Streamflow Statistics for Ungaged Sites","docAbstract":"The National Streamflow Statistics (NSS) Program is a computer program that should be useful to engineers, hydrologists, and others for planning, management, and design applications. NSS compiles all current U.S. Geological Survey (USGS) regional regression equations for estimating streamflow statistics at ungaged sites in an easy-to-use interface that operates on computers with Microsoft Windows operating systems. NSS expands on the functionality of the USGS National Flood Frequency Program, and replaces it.\r\n\r\nThe regression equations included in NSS are used to transfer streamflow statistics from gaged to ungaged sites through the use of watershed and climatic characteristics as explanatory or predictor variables. Generally, the equations were developed on a statewide or metropolitan-area basis as part of cooperative study programs. Equations are available for estimating rural and urban flood-frequency statistics, such as the 1 00-year flood, for every state, for Puerto Rico, and for the island of Tutuila, American Samoa. Equations are available for estimating other statistics, such as the mean annual flow, monthly mean flows, flow-duration percentiles, and low-flow frequencies (such as the 7-day, 0-year low flow) for less than half of the states. All equations available for estimating streamflow statistics other than flood-frequency statistics assume rural (non-regulated, non-urbanized) conditions.\r\n\r\nThe NSS output provides indicators of the accuracy of the estimated streamflow statistics. The indicators may include any combination of the standard error of estimate, the standard error of prediction, the equivalent years of record, or 90 percent prediction intervals, depending on what was provided by the authors of the equations.\r\n\r\nThe program includes several other features that can be used only for flood-frequency estimation. These include the ability to generate flood-frequency plots, and plots of typical flood hydrographs for selected recurrence intervals, estimates of the probable maximum flood, extrapolation of the 500-year flood when an equation for estimating it is not available, and weighting techniques to improve flood-frequency estimates for gaging stations and ungaged sites on gaged streams.\r\n\r\nThis report describes the regionalization techniques used to develop the equations in NSS and provides guidance on the applicability and limitations of the techniques. The report also includes a users manual and a summary of equations available for estimating basin lagtime, which is needed by the program to generate flood hydrographs. The NSS software and accompanying database, and the documentation for the regression equations included in NSS, are available on the Web at http://water.usgs.gov/software/.","language":"English","publisher":"U.S. Geological Survey","doi":"10.3133/tm4A6","collaboration":"Chapter 6 of\r\nBook 4, Hydrologic Analysis and Interpretation\r\nSection A, Statistical Analysis","usgsCitation":"Ries, K.G., With sections by Atkins, J.B., Hummel, P., Gray, M., Dusenbury, R., Jennings, M., Kirby, W., Riggs, H.C., Sauer, V., and Thomas, W., 2007, The National Streamflow Statistics Program: A Computer Program for Estimating Streamflow Statistics for Ungaged Sites: U.S. Geological Survey Techniques and Methods 4-A6, vi, 37 p., https://doi.org/10.3133/tm4A6.","productDescription":"vi, 37 p.","numberOfPages":"43","costCenters":[{"id":41514,"text":"Maryland-Delaware-District of Columbia  Water Science Center","active":true,"usgs":true}],"links":[{"id":124332,"rank":1,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/thumbnails/tm_4_a6.gif"},{"id":9234,"rank":2,"type":{"id":15,"text":"Index Page"},"url":"https://pubs.usgs.gov/tm/2006/tm4a6/","linkFileType":{"id":5,"text":"html"}}],"noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"4f4e4ac7e4b07f02db67b054","contributors":{"authors":[{"text":"Ries, Kernell G. III kries@usgs.gov","contributorId":30312,"corporation":false,"usgs":true,"family":"Ries","given":"Kernell","suffix":"III","email":"kries@usgs.gov","middleInitial":"G.","affiliations":[],"preferred":false,"id":290358,"contributorType":{"id":1,"text":"Authors"},"rank":1},{"text":"With sections by Atkins, J. 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C.","contributorId":17210,"corporation":false,"usgs":true,"family":"Riggs","given":"H.","email":"","middleInitial":"C.","affiliations":[{"id":595,"text":"U.S. Geological Survey","active":false,"usgs":true}],"preferred":false,"id":290357,"contributorType":{"id":1,"text":"Authors"},"rank":8},{"text":"Sauer, V.B.","contributorId":39380,"corporation":false,"usgs":true,"family":"Sauer","given":"V.B.","email":"","affiliations":[],"preferred":false,"id":290361,"contributorType":{"id":1,"text":"Authors"},"rank":9},{"text":"Thomas, W.O. Jr.","contributorId":32133,"corporation":false,"usgs":true,"family":"Thomas","given":"W.O.","suffix":"Jr.","email":"","affiliations":[],"preferred":false,"id":290359,"contributorType":{"id":1,"text":"Authors"},"rank":10}]}}
,{"id":70094223,"text":"ofr20071047SRP060 - 2007 - High-resolution airborne gravity imaging over James Ross Island (West Antarctica)","interactions":[],"lastModifiedDate":"2014-02-18T16:24:14","indexId":"ofr20071047SRP060","displayToPublicDate":"2007-02-01T16:06:00","publicationYear":"2007","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":"2007-1047-SRP-060","title":"High-resolution airborne gravity imaging over James Ross Island (West Antarctica)","docAbstract":"James Ross Island (JRI) exposes a Miocene-Recent alkaline basaltic volcanic complex that developed in a \nback-arc, east of the northern Antarctic Peninsula. JRI has been the focus of several geological studies because it \nprovides a window on Neogene magmatic processes and paleoenvironments. However, little is known about its internal \nstructure. New airborne gravity data were collected as part of the first high-resolution aerogeophysical survey flown over \nthe island and reveal a prominent negative Bouguer gravity anomaly over Mt Haddington. This is intriguing as basaltic \nvolcanoes are typically associated with positive Bouguer anomalies, linked to underlying mafic intrusions. The negative \nBouguer anomaly may be associated with a hitherto unrecognised low-density sub-surface body, such as a breccia-filled \ncaldera, or a partially molten magma chamber.","largerWorkType":{"id":18,"text":"Report"},"largerWorkTitle":"Antarctica: A Keystone in a Changing World--Online Proceedings for the Tenth International Symposium on Antarctic Earth Sciences. Santa Barbara, California, U.S.A.--August 26 to September 1, 2007","largerWorkSubtype":{"id":5,"text":"USGS Numbered Series"},"language":"English","publisher":"U.S. Geological Survey","publisherLocation":"Reston, VA","doi":"10.3133/ofr20071047SRP060","usgsCitation":"Jordan, T., Ferraccioli, F., Jones, P., Smellie, J., Ghidella, M., Corr, H.F., and Zakrajsek, A., 2007, High-resolution airborne gravity imaging over James Ross Island (West Antarctica): U.S. Geological Survey Open-File Report 2007-1047-SRP-060, 4 p., https://doi.org/10.3133/ofr20071047SRP060.","productDescription":"4 p.","additionalOnlineFiles":"N","costCenters":[],"links":[{"id":282511,"type":{"id":11,"text":"Document"},"url":"https://pubs.usgs.gov/of/2007/1047/srp/srp060/of2007-1047srp060.pdf"},{"id":282512,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/thumbnails/ofr20071047SRP060.JPG"}],"otherGeospatial":"Antarctica;James Ross Island","geographicExtents":"{ \"type\": \"FeatureCollection\", \"features\": [ { \"type\": \"Feature\", \"properties\": {}, \"geometry\": { \"type\": \"Polygon\", \"coordinates\": [ [ [ -58.4696,-64.4716 ], [ -58.4696,-63.7787 ], [ -57.0355,-63.7787 ], [ -57.0355,-64.4716 ], [ -58.4696,-64.4716 ] ] ] } } ] }","noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"53cd608de4b0b290850fcfc1","contributors":{"authors":[{"text":"Jordan, T.A.","contributorId":101183,"corporation":false,"usgs":true,"family":"Jordan","given":"T.A.","email":"","affiliations":[],"preferred":false,"id":490581,"contributorType":{"id":1,"text":"Authors"},"rank":1},{"text":"Ferraccioli, Fausto","contributorId":43591,"corporation":false,"usgs":true,"family":"Ferraccioli","given":"Fausto","email":"","affiliations":[],"preferred":false,"id":490575,"contributorType":{"id":1,"text":"Authors"},"rank":2},{"text":"Jones, P.C.","contributorId":70281,"corporation":false,"usgs":true,"family":"Jones","given":"P.C.","email":"","affiliations":[],"preferred":false,"id":490578,"contributorType":{"id":1,"text":"Authors"},"rank":3},{"text":"Smellie, J.L.","contributorId":95385,"corporation":false,"usgs":true,"family":"Smellie","given":"J.L.","affiliations":[],"preferred":false,"id":490579,"contributorType":{"id":1,"text":"Authors"},"rank":4},{"text":"Ghidella, M.","contributorId":95794,"corporation":false,"usgs":true,"family":"Ghidella","given":"M.","affiliations":[],"preferred":false,"id":490580,"contributorType":{"id":1,"text":"Authors"},"rank":5},{"text":"Corr, H. F. J.","contributorId":68214,"corporation":false,"usgs":true,"family":"Corr","given":"H.","email":"","middleInitial":"F. J.","affiliations":[],"preferred":false,"id":490577,"contributorType":{"id":1,"text":"Authors"},"rank":6},{"text":"Zakrajsek, A.F.","contributorId":52483,"corporation":false,"usgs":true,"family":"Zakrajsek","given":"A.F.","email":"","affiliations":[],"preferred":false,"id":490576,"contributorType":{"id":1,"text":"Authors"},"rank":7}]}}
,{"id":70074785,"text":"ofr20071047SRP - 2007 - Main Andean sinistral shear along the Cooper Bay Dislocation Zone, South Georgia?","interactions":[],"lastModifiedDate":"2014-02-03T15:54:22","indexId":"ofr20071047SRP","displayToPublicDate":"2007-02-01T15:43:00","publicationYear":"2007","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":"2007-1047-SRP-034","title":"Main Andean sinistral shear along the Cooper Bay Dislocation Zone, South Georgia?","docAbstract":"The Cooper Bay Dislocation Zone (CBDZ) represents a major NW-SE trending tectonic boundary within\nthe island of South Georgia that juxtaposes components of a Middle Jurassic to mid-Cretaceous island-arc and back-arc-\nbasin system. New detailed structural data from the southern end of the dislocation zone reveal that earliest\ndisplacement along the boundary appears to have been associated with dip-slip reverse shear, characterised by\nwidespread proto- to meso-mylonitic granitic rocks within the basement assemblage exposed to the southwest of the\nshear zone. Along the northeast margin, highly sheared and mylonitised metasedimentary and metabasic rocks reveal\nsinistral strike-slip kinematics and a sub-horizontal mineral lineation. Narrow zones of sinistral shear are locally superimposed within the basement rocks along the SW margin, that together with the presence of brittle sinistral faults\nsuggest that the strike-slip component of deformation postdates the dip-slip. Comparison with the tectonic history of the\nRocas Verdas Marginal Basin, Fuegian Andes, suggests that the sinistral shear event preserved along the CBDZ maybe\nbe related to Late Cretaceous, main Andean orogenic transpression, although a Cenozoic event cannot to ruled out.","largerWorkType":{"id":18,"text":"Report"},"largerWorkTitle":"Antarctica: A Keystone in a Changing World--Online Proceedings for the Tenth International Symposium on Antarctic Earth Sciences. Santa Barbara, California, U.S.A.--August 26 to September 1, 2007","largerWorkSubtype":{"id":5,"text":"USGS Numbered Series"},"language":"English","publisher":"U.S. Geological Survey","publisherLocation":"Reston, VA","doi":"10.3133/ofr20071047SRP","usgsCitation":"Curtis, M., 2007, Main Andean sinistral shear along the Cooper Bay Dislocation Zone, South Georgia?: U.S. Geological Survey Open-File Report 2007-1047-SRP-034, 4 p., https://doi.org/10.3133/ofr20071047SRP.","productDescription":"4 p.","additionalOnlineFiles":"N","costCenters":[],"links":[{"id":281934,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/thumbnails/ofr20071047SRP.JPG"},{"id":281933,"type":{"id":11,"text":"Document"},"url":"https://pubs.usgs.gov/of/2007/1047/srp/srp034/of2007-1047srp034.pdf"}],"otherGeospatial":"Antarctica","geographicExtents":"{ \"type\": \"FeatureCollection\", \"features\": [ { \"type\": \"Feature\", \"properties\": {}, \"geometry\": { \"type\": \"Polygon\", \"coordinates\": [ [ [ 180.0,-90.0 ], [ 180.0,-60.0 ], [ -180.0,-60.0 ], [ -180.0,-90.0 ], [ 180.0,-90.0 ] ] ] } } ] }","noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"53cd655be4b0b290851000aa","contributors":{"authors":[{"text":"Curtis, M.L.","contributorId":55335,"corporation":false,"usgs":true,"family":"Curtis","given":"M.L.","email":"","affiliations":[],"preferred":false,"id":489880,"contributorType":{"id":1,"text":"Authors"},"rank":1}]}}
,{"id":70159343,"text":"70159343 - 2007 - The FORE-SCE model: a practical approach for projecting land cover change using scenario-based modeling","interactions":[],"lastModifiedDate":"2015-10-22T11:52:33","indexId":"70159343","displayToPublicDate":"2007-02-01T00:00:00","publicationYear":"2007","noYear":false,"publicationType":{"id":2,"text":"Article"},"publicationSubtype":{"id":10,"text":"Journal Article"},"seriesTitle":{"id":2367,"text":"Journal of Land Use Science","active":true,"publicationSubtype":{"id":10}},"title":"The FORE-SCE model: a practical approach for projecting land cover change using scenario-based modeling","docAbstract":"<p><span>A wide variety of ecological applications require spatially explicit, historic, current, and projected land use and land cover data. The U.S. Land Cover Trends project is analyzing contemporary (1973&ndash;2000) land-cover change in the conterminous United States. The newly developed FORE-SCE model used Land Cover Trends data and theoretical, statistical, and deterministic modeling techniques to project future land cover change through 2020 for multiple plausible scenarios. Projected proportions of future land use were initially developed, and then sited on the lands with the highest potential for supporting that land use and land cover using a statistically based stochastic allocation procedure. Three scenarios of 2020 land cover were mapped for the western Great Plains in the US. The model provided realistic, high-resolution, scenario-based land-cover products suitable for multiple applications, including studies of climate and weather variability, carbon dynamics, and regional&nbsp;</span><a href=\"http://hydrology.sohl@usgs.gov/\" target=\"_blank\">hydrology.</a></p>","language":"English","publisher":"Taylor & Francis","doi":"10.1080/17474230701218202","usgsCitation":"Sohl, T.L., Sayler, K., Drummond, M.A., and Loveland, T., 2007, The FORE-SCE model: a practical approach for projecting land cover change using scenario-based modeling: Journal of Land Use Science, v. 2, no. 2, p. 103-126, https://doi.org/10.1080/17474230701218202.","productDescription":"24 p.","startPage":"103","endPage":"126","onlineOnly":"N","additionalOnlineFiles":"N","costCenters":[{"id":222,"text":"Earth Resources Observation and Science (EROS) Center","active":true,"usgs":true}],"links":[{"id":476920,"rank":0,"type":{"id":40,"text":"Open Access Publisher Index Page"},"url":"https://doi.org/10.1080/17474230701218202","text":"Publisher Index Page"},{"id":310455,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/thumbnails/outside_thumb.jpg"}],"volume":"2","issue":"2","noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"562a08f4e4b011227bf1fde7","contributors":{"authors":[{"text":"Sohl, Terry L. 0000-0002-9771-4231 sohl@usgs.gov","orcid":"https://orcid.org/0000-0002-9771-4231","contributorId":648,"corporation":false,"usgs":true,"family":"Sohl","given":"Terry","email":"sohl@usgs.gov","middleInitial":"L.","affiliations":[{"id":222,"text":"Earth Resources Observation and Science (EROS) Center","active":true,"usgs":true},{"id":223,"text":"Earth Resources Observation and Science (EROS) Center (Geography)","active":false,"usgs":true}],"preferred":true,"id":578094,"contributorType":{"id":1,"text":"Authors"},"rank":1},{"text":"Sayler, Kristi L. 0000-0003-2514-242X sayler@usgs.gov","orcid":"https://orcid.org/0000-0003-2514-242X","contributorId":2988,"corporation":false,"usgs":true,"family":"Sayler","given":"Kristi","email":"sayler@usgs.gov","middleInitial":"L.","affiliations":[{"id":223,"text":"Earth Resources Observation and Science (EROS) Center (Geography)","active":false,"usgs":true}],"preferred":true,"id":578095,"contributorType":{"id":1,"text":"Authors"},"rank":2},{"text":"Drummond, Mark A. 0000-0001-7420-3503 madrummond@usgs.gov","orcid":"https://orcid.org/0000-0001-7420-3503","contributorId":3053,"corporation":false,"usgs":true,"family":"Drummond","given":"Mark","email":"madrummond@usgs.gov","middleInitial":"A.","affiliations":[{"id":318,"text":"Geosciences and Environmental Change Science Center","active":true,"usgs":true}],"preferred":true,"id":578096,"contributorType":{"id":1,"text":"Authors"},"rank":3},{"text":"Loveland, Thomas R. 0000-0003-3114-6646 loveland@usgs.gov","orcid":"https://orcid.org/0000-0003-3114-6646","contributorId":3005,"corporation":false,"usgs":true,"family":"Loveland","given":"Thomas R.","email":"loveland@usgs.gov","affiliations":[{"id":223,"text":"Earth Resources Observation and Science (EROS) Center (Geography)","active":false,"usgs":true}],"preferred":false,"id":578097,"contributorType":{"id":1,"text":"Authors"},"rank":4}]}}
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