{"pageNumber":"2956","pageRowStart":"73875","pageSize":"25","recordCount":184612,"records":[{"id":70223169,"text":"70223169 - 2002 - Flood pulsing in the regeneration and maintenance of species in riverine forested wetlands of the southeastern United States","interactions":[],"lastModifiedDate":"2021-08-13T19:12:34.736506","indexId":"70223169","displayToPublicDate":"2002-05-01T13:27:21","publicationYear":"2002","noYear":false,"publicationType":{"id":5,"text":"Book chapter"},"title":"Flood pulsing in the regeneration and maintenance of species in riverine forested wetlands of the southeastern United States","docAbstract":"<p>No abstract available.</p>","largerWorkType":{"id":4,"text":"Book"},"largerWorkTitle":"Flood pulsing in wetlands: Restoring the natural hydrological balance","largerWorkSubtype":{"id":15,"text":"Monograph"},"language":"English","publisher":"John Wiley & Sons, Inc.","publisherLocation":"Hoboken, NJ","usgsCitation":"Middleton, B.A., 2002, Flood pulsing in the regeneration and maintenance of species in riverine forested wetlands of the southeastern United States, chap. <i>of</i> Flood pulsing in wetlands: Restoring the natural hydrological balance, p. 223-294.","startPage":"223","endPage":"294","numberOfPages":"72","costCenters":[{"id":17705,"text":"Wetland and Aquatic Research Center","active":true,"usgs":true}],"links":[{"id":387928,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/thumbnails/outside_thumb.jpg"},{"id":387927,"rank":1,"type":{"id":15,"text":"Index Page"},"url":"https://www.wiley.com/en-us/Flood+Pulsing+in+Wetlands%3A+Restoring+the+Natural+Hydrological+Balance-p-9780471418078","description":"Index Page"}],"country":"United States","geographicExtents":"{\n  \"type\": \"FeatureCollection\",\n  \"features\": [\n    {\n      \"type\": \"Feature\",\n      \"properties\": {},\n      \"geometry\": {\n        \"type\": \"Polygon\",\n        \"coordinates\": [\n          [\n            [\n              -94.9658203125,\n              24.287026865376436\n            ],\n            [\n              -71.6748046875,\n              24.287026865376436\n            ],\n            [\n              -71.6748046875,\n              41.04621681452063\n            ],\n            [\n              -94.9658203125,\n              41.04621681452063\n            ],\n            [\n              -94.9658203125,\n              24.287026865376436\n            ]\n          ]\n        ]\n      }\n    }\n  ]\n}","noUsgsAuthors":false,"publicationStatus":"PW","contributors":{"editors":[{"text":"Middleton, Beth A. 0000-0002-1220-2326 middletonb@usgs.gov","orcid":"https://orcid.org/0000-0002-1220-2326","contributorId":2029,"corporation":false,"usgs":true,"family":"Middleton","given":"Beth","email":"middletonb@usgs.gov","middleInitial":"A.","affiliations":[{"id":17705,"text":"Wetland and Aquatic Research Center","active":true,"usgs":true}],"preferred":true,"id":821205,"contributorType":{"id":2,"text":"Editors"},"rank":1}],"authors":[{"text":"Middleton, Beth A. 0000-0002-1220-2326 middletonb@usgs.gov","orcid":"https://orcid.org/0000-0002-1220-2326","contributorId":2029,"corporation":false,"usgs":true,"family":"Middleton","given":"Beth","email":"middletonb@usgs.gov","middleInitial":"A.","affiliations":[{"id":17705,"text":"Wetland and Aquatic Research Center","active":true,"usgs":true}],"preferred":true,"id":821204,"contributorType":{"id":1,"text":"Authors"},"rank":1}]}}
,{"id":70243114,"text":"70243114 - 2002 - Crustal structure across the Bering Strait, Alaska: Onshore recordings of a marine seismic survey","interactions":[],"lastModifiedDate":"2023-04-28T17:03:14.506487","indexId":"70243114","displayToPublicDate":"2002-05-01T11:55:57","publicationYear":"2002","noYear":false,"publicationType":{"id":5,"text":"Book chapter"},"publicationSubtype":{"id":24,"text":"Book Chapter"},"title":"Crustal structure across the Bering Strait, Alaska: Onshore recordings of a marine seismic survey","docAbstract":"<p>No abstract available.</p>","largerWorkType":{"id":4,"text":"Book"},"largerWorkTitle":"Tectonic evolution of the Bering Shelf-Chukchi Sea-Arctic margin and adjacent landmasses","largerWorkSubtype":{"id":15,"text":"Monograph"},"language":"English","publisher":"Geological Society of America","doi":"10.1130/0-8137-2360-4.25","usgsCitation":"Wolf, L.W., McCaleb, R.C., Stone, D., Brocher, T.M., Fujita, K., and Klemperer, S.L., 2002, Crustal structure across the Bering Strait, Alaska: Onshore recordings of a marine seismic survey, chap. <i>of</i> Tectonic evolution of the Bering Shelf-Chukchi Sea-Arctic margin and adjacent landmasses, v. 360, p. 25-37, https://doi.org/10.1130/0-8137-2360-4.25.","productDescription":"13 p.","startPage":"25","endPage":"37","costCenters":[{"id":237,"text":"Earthquake Science Center","active":true,"usgs":true}],"links":[{"id":416513,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/thumbnails/outside_thumb.jpg"}],"country":"Russia, United States","otherGeospatial":"Bering Sea, Bering Strait region, Chukchi Sea","geographicExtents":"{\n  \"type\": \"FeatureCollection\",\n  \"features\": [\n    {\n      \"type\": \"Feature\",\n      \"properties\": {},\n      \"geometry\": {\n        \"coordinates\": [\n          [\n            [\n              -145,\n              72\n            ],\n            [\n              -179.9,\n              72\n            ],\n            [\n              -179.9,\n              60\n            ],\n            [\n              -145,\n              60\n            ],\n            [\n              -145,\n              72\n            ]\n          ]\n        ],\n        \"type\": \"Polygon\"\n      }\n    }\n  ]\n}","volume":"360","noUsgsAuthors":false,"publicationStatus":"PW","contributors":{"authors":[{"text":"Wolf, Lorraine W.","contributorId":72817,"corporation":false,"usgs":false,"family":"Wolf","given":"Lorraine","email":"","middleInitial":"W.","affiliations":[],"preferred":false,"id":871092,"contributorType":{"id":1,"text":"Authors"},"rank":1},{"text":"McCaleb, Robert C.","contributorId":304593,"corporation":false,"usgs":false,"family":"McCaleb","given":"Robert","email":"","middleInitial":"C.","affiliations":[],"preferred":false,"id":871093,"contributorType":{"id":1,"text":"Authors"},"rank":2},{"text":"Stone, David B.","contributorId":65324,"corporation":false,"usgs":true,"family":"Stone","given":"David B.","affiliations":[],"preferred":false,"id":871094,"contributorType":{"id":1,"text":"Authors"},"rank":3},{"text":"Brocher, Thomas M. 0000-0002-9740-839X brocher@usgs.gov","orcid":"https://orcid.org/0000-0002-9740-839X","contributorId":262,"corporation":false,"usgs":true,"family":"Brocher","given":"Thomas","email":"brocher@usgs.gov","middleInitial":"M.","affiliations":[{"id":237,"text":"Earthquake Science Center","active":true,"usgs":true}],"preferred":true,"id":871095,"contributorType":{"id":1,"text":"Authors"},"rank":4},{"text":"Fujita, Kazuya","contributorId":15654,"corporation":false,"usgs":true,"family":"Fujita","given":"Kazuya","email":"","affiliations":[],"preferred":false,"id":871096,"contributorType":{"id":1,"text":"Authors"},"rank":5},{"text":"Klemperer, Simon L.","contributorId":106929,"corporation":false,"usgs":true,"family":"Klemperer","given":"Simon","email":"","middleInitial":"L.","affiliations":[{"id":6986,"text":"Stanford University","active":true,"usgs":false}],"preferred":false,"id":871097,"contributorType":{"id":1,"text":"Authors"},"rank":6}]}}
,{"id":70243175,"text":"70243175 - 2002 - Tension cracks, eruptive fissures, dikes, and faults related to late Pleistocene-Holocene basaltic volcanism and implications for the distribution of hydraulic conductivity in the eastern Snake River Plain, Idaho","interactions":[],"lastModifiedDate":"2023-05-02T16:57:22.161119","indexId":"70243175","displayToPublicDate":"2002-05-01T11:43:08","publicationYear":"2002","noYear":false,"publicationType":{"id":5,"text":"Book chapter"},"publicationSubtype":{"id":24,"text":"Book Chapter"},"title":"Tension cracks, eruptive fissures, dikes, and faults related to late Pleistocene-Holocene basaltic volcanism and implications for the distribution of hydraulic conductivity in the eastern Snake River Plain, Idaho","docAbstract":"<p>No abstract available.</p>","largerWorkType":{"id":4,"text":"Book"},"largerWorkTitle":"Geology, hydrogeology, and environmental remediation: Idaho National Engineering and Environmental Laboratory, eastern Snake River plain, 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,{"id":70243234,"text":"70243234 - 2002 - Cretaceous mid-crustal metamorphism and exhumation of the Koolen gneiss dome, Chukotka Peninsula, northeastern Russia","interactions":[],"lastModifiedDate":"2023-05-04T15:36:16.41698","indexId":"70243234","displayToPublicDate":"2002-05-01T10:31:01","publicationYear":"2002","noYear":false,"publicationType":{"id":5,"text":"Book chapter"},"publicationSubtype":{"id":24,"text":"Book Chapter"},"title":"Cretaceous mid-crustal metamorphism and exhumation of the Koolen gneiss dome, Chukotka Peninsula, northeastern Russia","docAbstract":"<p>No abstract available.</p>","largerWorkType":{"id":4,"text":"Book"},"largerWorkTitle":"Tectonic evolution of the Bering Shelf-Chukchi Sea-Artic Margin and adjacent landmasses","largerWorkSubtype":{"id":15,"text":"Monograph"},"language":"English","publisher":"Geological Society of America","doi":"10.1130/0-8137-2360-4.147","usgsCitation":"Akinin, V.V., and Calvert, A.T., 2002, Cretaceous mid-crustal metamorphism and exhumation of the Koolen gneiss dome, Chukotka Peninsula, northeastern Russia, chap. <i>of</i> Tectonic evolution of the Bering Shelf-Chukchi Sea-Artic Margin and adjacent landmasses, v. 360, p. 147-165, https://doi.org/10.1130/0-8137-2360-4.147.","productDescription":"19 p.","startPage":"147","endPage":"165","costCenters":[{"id":312,"text":"Geology, Minerals, Energy, and Geophysics Science Center","active":true,"usgs":true},{"id":617,"text":"Volcano Science Center","active":true,"usgs":true}],"links":[{"id":416720,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/thumbnails/outside_thumb.jpg"}],"country":"Russia","otherGeospatial":"Chukotka Peninsula","geographicExtents":"{\n  \"type\": \"FeatureCollection\",\n  \"features\": [\n    {\n      \"type\": \"Feature\",\n      \"properties\": {},\n      \"geometry\": {\n        \"coordinates\": [\n          [\n            [\n              -174.41044224555822,\n              67.14237226826035\n            ],\n            [\n              -174.41044224555822,\n              63.9992328894586\n            ],\n            [\n              -169.54283338936494,\n              63.9992328894586\n            ],\n            [\n              -169.54283338936494,\n              67.14237226826035\n            ],\n            [\n              -174.41044224555822,\n              67.14237226826035\n            ]\n          ]\n        ],\n        \"type\": \"Polygon\"\n      }\n    }\n  ]\n}","volume":"360","noUsgsAuthors":false,"publicationStatus":"PW","contributors":{"editors":[{"text":"Miller, Elizabeth L.","contributorId":29896,"corporation":false,"usgs":true,"family":"Miller","given":"Elizabeth","email":"","middleInitial":"L.","affiliations":[],"preferred":false,"id":871643,"contributorType":{"id":2,"text":"Editors"},"rank":1},{"text":"Grantz, Arthur agrantz@usgs.gov","contributorId":2585,"corporation":false,"usgs":true,"family":"Grantz","given":"Arthur","email":"agrantz@usgs.gov","affiliations":[{"id":312,"text":"Geology, Minerals, Energy, and Geophysics Science Center","active":true,"usgs":true}],"preferred":true,"id":871644,"contributorType":{"id":2,"text":"Editors"},"rank":2},{"text":"Klemperer, Simon L.","contributorId":106929,"corporation":false,"usgs":true,"family":"Klemperer","given":"Simon","email":"","middleInitial":"L.","affiliations":[{"id":6986,"text":"Stanford University","active":true,"usgs":false}],"preferred":false,"id":871645,"contributorType":{"id":2,"text":"Editors"},"rank":3}],"authors":[{"text":"Akinin, Vyacheslav V","contributorId":247821,"corporation":false,"usgs":false,"family":"Akinin","given":"Vyacheslav","email":"","middleInitial":"V","affiliations":[{"id":49665,"text":"North East Scientific Research Institute, Far East Branc, Russian Academy of Sciences, Magadan, Russia","active":true,"usgs":false}],"preferred":false,"id":871641,"contributorType":{"id":1,"text":"Authors"},"rank":1},{"text":"Calvert, Andrew T. 0000-0001-5237-2218 acalvert@usgs.gov","orcid":"https://orcid.org/0000-0001-5237-2218","contributorId":2694,"corporation":false,"usgs":true,"family":"Calvert","given":"Andrew","email":"acalvert@usgs.gov","middleInitial":"T.","affiliations":[{"id":617,"text":"Volcano Science Center","active":true,"usgs":true},{"id":312,"text":"Geology, Minerals, Energy, and Geophysics Science Center","active":true,"usgs":true}],"preferred":true,"id":871642,"contributorType":{"id":1,"text":"Authors"},"rank":2}]}}
,{"id":70246275,"text":"70246275 - 2002 - Swimming performance of upstream migrant fishes: New methods, new perspectives","interactions":[],"lastModifiedDate":"2023-06-29T15:46:35.936572","indexId":"70246275","displayToPublicDate":"2002-05-01T10:17:59","publicationYear":"2002","noYear":false,"publicationType":{"id":21,"text":"Thesis"},"publicationSubtype":{"id":28,"text":"Thesis"},"title":"Swimming performance of upstream migrant fishes: New methods, new perspectives","docAbstract":"<p><span>The ability to traverse barriers of high water velocity limits the distributions of many diadromous and other migratory fish species, and is central to effective fishway design. This dissertation provides a detailed analysis of volitional sprinting behavior of six migratory fish species (American shad Alosa sapidissima, alewife A. pseudoharengus, blueback herring A. aestivalis, striped bass Morone saxatilis , walleye Stizostedion vitreum, and white sucker Catostomus commersoni), against controlled water velocities of 1.5–4.5 m · s−1 in a large, open-channel flume. In Chapter 1, I develop models of maximum distance traversed ( Dmax) by fish ascending these flows, accounting for water velocity and other covariate effects. I then demonstrate the application of these models, using them to predict proportions of active migrants capable of traversing a range of distances and flow velocities. Chapter 2 focuses on behavior and swimming performance of American shad, analyzing covariate effects on attempt rate as well as Dmax, and formalizing how rate and distance jointly affect overall rates of passage. Models describe a complex pattern of varying responses of attempt rate and Dmax to hydraulics, temperature, effort expended on and recovery time since the previous attempt. In Chapter 3, I use the effect of swimming speed on fatigue time to calculate an optimal swimming speed that maximizes the over-ground distance fish can traverse, and hence defines their maximum ability to traverse velocity barriers. This speed reduces to a constant groundspeed within a given gait, regardless of the speed of flow. Data from all six species support this view, although only American shad exhibit a clear shift from the optimum prolonged speed to the optimum sprint speed at the predicted critical flow velocity. Throughout this dissertation I make extensive and novel use of statistical techniques developed for survival analysis to analyze and model behavioral data, both with respect to attempt rate and to D max. Chapter 4 provides an overview of these methods and demonstrates their application to a fish passage study of downstream-migrating Atlantic salmon (Salmo salar) smolts. An understanding of the principles described here will help the reader to better understand the findings of the previous three chapters.</span></p>","language":"English","publisher":"University of Massachusetts-Amherst","usgsCitation":"Castro-Santos, T.R., 2002, Swimming performance of upstream migrant fishes: New methods, new perspectives, AAI3056208.","productDescription":"AAI3056208","costCenters":[],"links":[{"id":418629,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/thumbnails/outside_thumb.jpg"},{"id":418627,"rank":1,"type":{"id":15,"text":"Index Page"},"url":"https://scholarworks.umass.edu/dissertations/AAI3056208/"}],"noUsgsAuthors":false,"publicationStatus":"PW","contributors":{"authors":[{"text":"Castro-Santos, Theodore R. 0000-0003-2575-9120 tcastrosantos@usgs.gov","orcid":"https://orcid.org/0000-0003-2575-9120","contributorId":3321,"corporation":false,"usgs":true,"family":"Castro-Santos","given":"Theodore","email":"tcastrosantos@usgs.gov","middleInitial":"R.","affiliations":[{"id":365,"text":"Leetown Science Center","active":true,"usgs":true}],"preferred":true,"id":876605,"contributorType":{"id":1,"text":"Authors"},"rank":1}]}}
,{"id":70243230,"text":"70243230 - 2002 - Constraints on the age of formation of seismically reflective middle and lower crust beneath the Bering Shelf: SHRIMP zircon dating of xenoliths from Saint Lawrence Island","interactions":[],"lastModifiedDate":"2023-05-04T15:14:46.497341","indexId":"70243230","displayToPublicDate":"2002-05-01T10:04:46","publicationYear":"2002","noYear":false,"publicationType":{"id":5,"text":"Book chapter"},"publicationSubtype":{"id":24,"text":"Book Chapter"},"title":"Constraints on the age of formation of seismically reflective middle and lower crust beneath the Bering Shelf: SHRIMP zircon dating of xenoliths from Saint Lawrence Island","docAbstract":"<p>No abstract available.</p>","largerWorkType":{"id":4,"text":"Book"},"largerWorkTitle":"Tectonic evolution of the Bering Shelf-Chukchi Sea-Artic Margin and adjacent landmasses","largerWorkSubtype":{"id":15,"text":"Monograph"},"language":"English","publisher":"Geological Society of America","doi":"10.1130/0-8137-2360-4.195","usgsCitation":"Miller, E.L., Ireland, T.R., Klemperer, S.L., Wirth, K., Akinin, V.V., and Brocher, T.M., 2002, Constraints on the age of formation of seismically reflective middle and lower crust beneath the Bering Shelf: SHRIMP zircon dating of xenoliths from Saint Lawrence Island, chap. <i>of</i> Tectonic evolution of the Bering Shelf-Chukchi Sea-Artic Margin and adjacent landmasses, v. 360, p. 195-208, https://doi.org/10.1130/0-8137-2360-4.195.","productDescription":"14 p.","startPage":"195","endPage":"208","costCenters":[{"id":237,"text":"Earthquake Science Center","active":true,"usgs":true},{"id":312,"text":"Geology, Minerals, Energy, and Geophysics Science Center","active":true,"usgs":true}],"links":[{"id":416717,"rank":1,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/thumbnails/outside_thumb.jpg"}],"country":"United States","state":"Alaska","otherGeospatial":"St Lawrence Island","geographicExtents":"{\n  \"type\": \"FeatureCollection\",\n  \"features\": [\n    {\n      \"type\": \"Feature\",\n      \"properties\": {},\n      \"geometry\": {\n        \"coordinates\": [\n          [\n            [\n              -171.91795090825306,\n              63.86981778154916\n            ],\n            [\n              -171.91795090825306,\n              62.851403902965075\n            ],\n            [\n              -168.62538056669197,\n              62.851403902965075\n            ],\n            [\n              -168.62538056669197,\n              63.86981778154916\n            ],\n            [\n              -171.91795090825306,\n              63.86981778154916\n            ]\n          ]\n        ],\n        \"type\": \"Polygon\"\n      }\n    }\n  ]\n}","volume":"360","noUsgsAuthors":false,"publicationStatus":"PW","contributors":{"editors":[{"text":"Miller, Elizabeth L. 0000-0002-6190-4826","orcid":"https://orcid.org/0000-0002-6190-4826","contributorId":269348,"corporation":false,"usgs":false,"family":"Miller","given":"Elizabeth","email":"","middleInitial":"L.","affiliations":[{"id":55934,"text":"Stanford University Department of Geological Sciences","active":true,"usgs":false}],"preferred":false,"id":871632,"contributorType":{"id":2,"text":"Editors"},"rank":1},{"text":"Grantz, Arthur agrantz@usgs.gov","contributorId":2585,"corporation":false,"usgs":true,"family":"Grantz","given":"Arthur","email":"agrantz@usgs.gov","affiliations":[{"id":312,"text":"Geology, Minerals, Energy, and Geophysics Science Center","active":true,"usgs":true}],"preferred":true,"id":871633,"contributorType":{"id":2,"text":"Editors"},"rank":2},{"text":"Klemperer, Simon L.","contributorId":106929,"corporation":false,"usgs":true,"family":"Klemperer","given":"Simon","email":"","middleInitial":"L.","affiliations":[{"id":6986,"text":"Stanford University","active":true,"usgs":false}],"preferred":false,"id":871634,"contributorType":{"id":2,"text":"Editors"},"rank":3}],"authors":[{"text":"Miller, Elizabeth L.","contributorId":29896,"corporation":false,"usgs":true,"family":"Miller","given":"Elizabeth","email":"","middleInitial":"L.","affiliations":[],"preferred":false,"id":871623,"contributorType":{"id":1,"text":"Authors"},"rank":1},{"text":"Ireland, T. 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,{"id":32368,"text":"ofr02123 - 2002 - Implosion, earthquake, and explosion recordings from the 2000 Seattle Kingdome Seismic Hazards Investigation of Puget Sound (SHIPS), Washington","interactions":[],"lastModifiedDate":"2021-09-07T19:26:54.074006","indexId":"ofr02123","displayToPublicDate":"2002-05-01T00:00:00","publicationYear":"2002","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":"2002-123","title":"Implosion, earthquake, and explosion recordings from the 2000 Seattle Kingdome Seismic Hazards Investigation of Puget Sound (SHIPS), Washington","docAbstract":"<p>This report describes seismic data obtained in Seattle, Washington, March 24-28, 2000, during a Seismic Hazards Investigation of Puget Sound (SHIPS). The seismic recordings obtained by this SHIPS experiment, nicknamed Kingdome SHIPS, were designed to (1) measure site responses throughout Seattle and to (2) help define the location of the Seattle fault. During Kingdome SHIPS, we recorded the Kingdome implosion, four 150-lb (68-kg) shots, and a M<sub>w</sub> = 7.6 teleseism using a dense network of seismographs deployed throughout Seattle. The seismographs were deployed at a nominal spacing of 1 km in a hexagonal grid extending from Green Lake in the north to Boeing Field in the south.</p>\n<br/>\n<p>The Seattle Kingdome was a domed sports stadium located in downtown Seattle near the Seattle fault. The Seattle Kingdome was imploded (demolished) at 8:32 AM local time (16:32 UTC) on March 26 (JD 086), 2000. The seismic energy produced by implosion of the Kingdome was equivalent to a local earthquake magnitude of 2.3. Strong impacts produced by the implosion of the Kingdome generated seismic arrivals to frequencies as low as 0.1 Hz. Two shots located north of the Seattle fault, where the charges were detonated within the ground water column (Discovery and Magnuson Parks), were much more strongly coupled than were the two shots to the south of the Seattle fault, where the shots were detonated above the water table (Lincoln and Seward Parks).</p>\n<br/>\n<p>Thirty-eight RefTek stations, scattered throughout Seattle, recorded the M<sub>w</sub> = 7.6 Japan Volcano Islands earthquake (22.4°N, 143.6°E, 104 km depth) of 28 March 2000 (JD 088). This teleseism produced useful signals for periods between 4 and 7 seconds. Only a few recordings of small magnitude local earthquakes were made, and these recordings are not presented.</p>\n<br/>\n<p>In this report, we describe the acquisition of these data, discuss the processing and merging of the data into common shot gathers, and illustrate the acquired data. We also describe the format and content of the archival tapes containing the SEGY-formatted, common-shot gathers.</p>","language":"English","publisher":"U.S. Geological Survey","doi":"10.3133/ofr02123","usgsCitation":"Brocher, T.M., Pratt, T.L., Weaver, C.S., Snelson, C.M., and Frankel, A.D., 2002, Implosion, earthquake, and explosion recordings from the 2000 Seattle Kingdome Seismic Hazards Investigation of Puget Sound (SHIPS), Washington: U.S. Geological Survey Open-File Report 2002-123, 29 p., https://doi.org/10.3133/ofr02123.","productDescription":"29 p.","numberOfPages":"29","costCenters":[{"id":237,"text":"Earthquake Science Center","active":true,"usgs":true}],"links":[{"id":283452,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/thumbnails/ofr02123.jpg"},{"id":60357,"rank":300,"type":{"id":11,"text":"Document"},"url":"https://pubs.usgs.gov/of/2002/0123/pdf/of02-123.pdf","linkFileType":{"id":1,"text":"pdf"}},{"id":3356,"rank":100,"type":{"id":15,"text":"Index Page"},"url":"https://pubs.usgs.gov/of/2002/0123/","linkFileType":{"id":5,"text":"html"}},{"id":388913,"rank":4,"type":{"id":36,"text":"NGMDB Index Page"},"url":"https://ngmdb.usgs.gov/Prodesc/proddesc_51520.htm"}],"country":"United States","state":"Washington","city":"Seattle","otherGeospatial":"Puget Sound","geographicExtents":"{ \"type\": \"FeatureCollection\", \"features\": [ { \"type\": \"Feature\", \"properties\": {}, \"geometry\": { \"type\": \"Polygon\", \"coordinates\": [ [ [ -122.459696,47.481968 ], [ -122.459696,47.734139 ], [ -122.224433,47.734139 ], [ -122.224433,47.481968 ], [ -122.459696,47.481968 ] ] ] } } ] }","noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"4f4e4b23e4b07f02db6ae04e","contributors":{"authors":[{"text":"Brocher, Thomas M. 0000-0002-9740-839X brocher@usgs.gov","orcid":"https://orcid.org/0000-0002-9740-839X","contributorId":262,"corporation":false,"usgs":true,"family":"Brocher","given":"Thomas","email":"brocher@usgs.gov","middleInitial":"M.","affiliations":[{"id":237,"text":"Earthquake Science Center","active":true,"usgs":true}],"preferred":true,"id":208431,"contributorType":{"id":1,"text":"Authors"},"rank":1},{"text":"Pratt, Thomas L. 0000-0003-3131-3141 tpratt@usgs.gov","orcid":"https://orcid.org/0000-0003-3131-3141","contributorId":3279,"corporation":false,"usgs":true,"family":"Pratt","given":"Thomas","email":"tpratt@usgs.gov","middleInitial":"L.","affiliations":[{"id":300,"text":"Geologic Hazards Science Center","active":true,"usgs":true},{"id":237,"text":"Earthquake Science Center","active":true,"usgs":true}],"preferred":true,"id":208434,"contributorType":{"id":1,"text":"Authors"},"rank":2},{"text":"Weaver, Craig S. craig@usgs.gov","contributorId":2690,"corporation":false,"usgs":true,"family":"Weaver","given":"Craig","email":"craig@usgs.gov","middleInitial":"S.","affiliations":[{"id":237,"text":"Earthquake Science Center","active":true,"usgs":true}],"preferred":true,"id":208433,"contributorType":{"id":1,"text":"Authors"},"rank":3},{"text":"Snelson, Catherine M.","contributorId":106369,"corporation":false,"usgs":true,"family":"Snelson","given":"Catherine","email":"","middleInitial":"M.","affiliations":[],"preferred":false,"id":208435,"contributorType":{"id":1,"text":"Authors"},"rank":4},{"text":"Frankel, Arthur D. 0000-0001-9119-6106 afrankel@usgs.gov","orcid":"https://orcid.org/0000-0001-9119-6106","contributorId":1363,"corporation":false,"usgs":true,"family":"Frankel","given":"Arthur","email":"afrankel@usgs.gov","middleInitial":"D.","affiliations":[{"id":237,"text":"Earthquake Science Center","active":true,"usgs":true}],"preferred":false,"id":208432,"contributorType":{"id":1,"text":"Authors"},"rank":5}]}}
,{"id":32360,"text":"ofr0225 - 2002 - Digital archive; Report upon the Colorado River of the West explored in 1857 and 1858 by Lieutenant Joseph C. Ives, geological report with maps by John S. Newberry","interactions":[],"lastModifiedDate":"2012-02-02T00:09:11","indexId":"ofr0225","displayToPublicDate":"2002-05-01T00:00:00","publicationYear":"2002","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":"2002-25","title":"Digital archive; Report upon the Colorado River of the West explored in 1857 and 1858 by Lieutenant Joseph C. Ives, geological report with maps by John S. Newberry","language":"ENGLISH","doi":"10.3133/ofr0225","isbn":"0607984511","usgsCitation":"McKinney, K.C., 2002, Digital archive; Report upon the Colorado River of the West explored in 1857 and 1858 by Lieutenant Joseph C. Ives, geological report with maps by John S. Newberry (Version 1.0): U.S. Geological Survey Open-File Report 2002-25, 1 CD-ROM : ill., maps ; 4 3/4 in., https://doi.org/10.3133/ofr0225.","productDescription":"1 CD-ROM : ill., maps ; 4 3/4 in.","costCenters":[],"links":[{"id":161365,"rank":0,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/thumbnails/usgs_thumb.jpg"}],"edition":"Version 1.0","noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"4f4e4b32e4b07f02db6b4617","contributors":{"authors":[{"text":"McKinney, Kevin C. kcmckinney@usgs.gov","contributorId":3406,"corporation":false,"usgs":true,"family":"McKinney","given":"Kevin","email":"kcmckinney@usgs.gov","middleInitial":"C.","affiliations":[],"preferred":true,"id":208411,"contributorType":{"id":1,"text":"Authors"},"rank":1}]}}
,{"id":33045,"text":"wri024068 - 2002 - Techniques for estimating selected streamflow characteristics of rural, unregulated streams in Ohio","interactions":[],"lastModifiedDate":"2022-02-09T20:10:38.612992","indexId":"wri024068","displayToPublicDate":"2002-05-01T00:00:00","publicationYear":"2002","noYear":false,"publicationType":{"id":18,"text":"Report"},"publicationSubtype":{"id":5,"text":"USGS Numbered Series"},"seriesTitle":{"id":342,"text":"Water-Resources Investigations Report","code":"WRI","active":false,"publicationSubtype":{"id":5}},"seriesNumber":"2002-4068","displayTitle":"Techniques for Estimating Selected  Streamflow Characteristics of Rural, Unregulated Streams in Ohio","title":"Techniques for estimating selected streamflow characteristics of rural, unregulated streams in Ohio","docAbstract":"<p>This report provides equations for estimating mean annual streamflow, mean monthly streamflows, harmonic mean streamflow, and streamflow quartiles (the 25th-, 50th-, and 75th-percentile streamflows) as a function of selected basin characteristics for rural, unregulated streams in Ohio. The equations were developed from streamflow statistics and basin-characteristics data for as many as 219 active or discontinued streamflow-gaging stations on rural, unregulated streams in Ohio with 10 or more years of homogenous daily streamflow record. Streamflow statistics and basin-characteristics data for the 219 stations are presented in this report.</p><p>Simple equations (based on drainage area only) and best-fit equations (based on drainage area and at least two other basin characteristics) were developed by means of ordinary least-squares regression techniques. Application of the best-fit equations generally involves quantification of basin characteristics that require or are facilitated by use of a geographic information system. In contrast, the simple equations can be used with information that can be obtained without use of a geographic information system; however, the simple equations have larger prediction errors than the best-fit equations and exhibit geographic biases for most streamflow statistics. The best-fit equations should be used instead of the simple equations whenever possible.</p>","language":"English","publisher":"U.S. Geological Survey","publisherLocation":"Reston, VA","doi":"10.3133/wri024068","collaboration":"Prepared in cooperation with the Ohio Department of Natural Resources, Division of Water, Department of Transportation, and the U.S. Department of Transportation, Federal Highway Administration","usgsCitation":"Koltun, G., and Whitehead, M.T., 2002, Techniques for estimating selected streamflow characteristics of rural, unregulated streams in Ohio: U.S. Geological Survey Water-Resources Investigations Report 2002-4068, iv, 50 p., https://doi.org/10.3133/wri024068.","productDescription":"iv, 50 p.","costCenters":[{"id":513,"text":"Ohio Water Science Center","active":true,"usgs":true}],"links":[{"id":395722,"rank":3,"type":{"id":36,"text":"NGMDB Index 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 \"}}]}","contact":"<p><a href=\"dc_oh@usgs.gov\" data-mce-href=\"dc_oh@usgs.gov\">Director</a>, <a href=\"https://www.usgs.gov/centers/oki-water/\" data-mce-href=\"https://www.usgs.gov/centers/oki-water/\">Ohio Water Science Center</a><br>U.S. Geological Survey<br>6460 Busch Blvd. <br>Columbus, OH 43229</p>","tableOfContents":"<ul><li>Abstract</li><li>Introduction</li><li>Compilation of Streamflow Data</li><li>Determination of Streamflow Statistics</li><li>Basin Characteristics</li><li>Development of Equations for Estimating Streamflow Statistics</li><li>Techniques for Estimating Selected Streamflow Characteristics</li><li>Summary</li><li>References</li><li>Appendixes</li></ul>","noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"4f4e4adbe4b07f02db685c57","contributors":{"authors":[{"text":"Koltun, G. F. 0000-0003-0255-2960","orcid":"https://orcid.org/0000-0003-0255-2960","contributorId":49817,"corporation":false,"usgs":true,"family":"Koltun","given":"G. F.","affiliations":[],"preferred":false,"id":209762,"contributorType":{"id":1,"text":"Authors"},"rank":1},{"text":"Whitehead, Matthew T. mtwhiteh@usgs.gov","contributorId":2158,"corporation":false,"usgs":true,"family":"Whitehead","given":"Matthew","email":"mtwhiteh@usgs.gov","middleInitial":"T.","affiliations":[{"id":513,"text":"Ohio Water Science Center","active":true,"usgs":true}],"preferred":false,"id":209761,"contributorType":{"id":1,"text":"Authors"},"rank":2}]}}
,{"id":33053,"text":"wri004083 - 2002 - Application of advanced geophysical logging methods in the characterization of a fractured-sedimentary bedrock aquifer, Ventura County, California","interactions":[],"lastModifiedDate":"2019-10-15T15:20:04","indexId":"wri004083","displayToPublicDate":"2002-05-01T00:00:00","publicationYear":"2002","noYear":false,"publicationType":{"id":18,"text":"Report"},"publicationSubtype":{"id":5,"text":"USGS Numbered Series"},"seriesTitle":{"id":342,"text":"Water-Resources Investigations Report","code":"WRI","active":false,"publicationSubtype":{"id":5}},"seriesNumber":"2000-4083","title":"Application of advanced geophysical logging methods in the characterization of a fractured-sedimentary bedrock aquifer, Ventura County, California","docAbstract":"<p>An integrated suite of advanced geophysical logging methods was used to characterize the geology and hydrology of three boreholes completed in fractured-sedimentary bedrock in Ventura County, California. The geophysical methods included caliper, gamma, electromagnetic induction, borehole deviation, optical and acoustic televiewer, borehole radar, fluid resistivity, temperature, and electromagnetic flowmeter. The geophysical logging 1) provided insights useful for the overall geohydrologic characterization of the bedrock and 2) enhanced the value of information collected by other methods from the boreholes including core-sample analysis, multiple-level monitoring, and packer testing.</p><p>The logged boreholes, which have open intervals of 100 to 200 feet, penetrate a sequence of interbedded sandstone and mudstone with bedding striking 220 to 250 degrees and dipping 15 to 40 degrees to the northwest. Fractures intersected by the boreholes include fractures parallel to bedding and fractures with variable strike that dip moderately to steeply. Two to three flow zones were detected in each borehole. The flow zones consist of bedding-parallel or steeply dipping fractures or a combination of bedding-parallel fractures and moderately to steeply dipping fractures. About 75 to more than 90 percent of the measured flow under pumped conditions was produced by only one of the flow zones in each borehole.</p>","language":"English","publisher":"U.S. Geological Survey","publisherLocation":"Reston, VA","doi":"10.3133/wri004083","collaboration":" Prepared in cooperation with the  University of Waterloo, Canada","usgsCitation":"Williams, J., Lane, J.W., Singha, K., and Haeni, F.P., 2002, Application of advanced geophysical logging methods in the characterization of a fractured-sedimentary bedrock aquifer, Ventura County, California: U.S. Geological Survey Water-Resources Investigations Report 2000-4083, 28 p. , https://doi.org/10.3133/wri004083.","productDescription":"28 p. ","costCenters":[{"id":493,"text":"Office of Ground Water","active":true,"usgs":true}],"links":[{"id":161169,"rank":0,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/wri/2000/4083/coverthb.jpg"},{"id":323968,"rank":2,"type":{"id":11,"text":"Document"},"url":"https://pubs.usgs.gov/wri/2000/4083/wri20004083.pdf","text":"Report","size":"1.13 MB","linkFileType":{"id":1,"text":"pdf"},"description":"WRI 2000-4083"}],"country":"United States","state":"California","county":"Ventura County","geographicExtents":"{\n  \"type\": \"FeatureCollection\",\n  \"features\": [\n    {\n      \"type\": \"Feature\",\n      \"properties\": {},\n      \"geometry\": {\n        \"type\": \"Polygon\",\n        \"coordinates\": [\n          [\n            [\n              -119.03823852539061,\n              34.093041824023096\n            ],\n            [\n              -118.67774963378906,\n              34.093041824023096\n            ],\n            [\n              -118.67774963378906,\n              34.326426048404265\n            ],\n            [\n              -119.03823852539061,\n              34.326426048404265\n            ],\n            [\n              -119.03823852539061,\n              34.093041824023096\n            ]\n          ]\n        ]\n      }\n    }\n  ]\n}","contact":"<p>Director, New York Water Science Center<br> U.S. Geological Survey<br> 425 Jordan Rd<br> Troy, NY 12180<br> (518) 285-5695 <br> <a href=\"http://ny.water.usgs.gov/\" data-mce-href=\"http://ny.water.usgs.gov/\">http://ny.water.usgs.gov/</a></p>","tableOfContents":"<ul><li>Introduction</li><li>Geophysical Logging Methods</li><li>Geophysical Log&nbsp;Anaysis</li><li>Summary</li><li>References</li></ul>","noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"4f4e4ac6e4b07f02db67aab0","contributors":{"authors":[{"text":"Williams, John 0000-0002-6054-6908 jhwillia@usgs.gov","orcid":"https://orcid.org/0000-0002-6054-6908","contributorId":1553,"corporation":false,"usgs":true,"family":"Williams","given":"John","email":"jhwillia@usgs.gov","affiliations":[{"id":474,"text":"New York Water Science Center","active":true,"usgs":true}],"preferred":true,"id":209780,"contributorType":{"id":1,"text":"Authors"},"rank":1},{"text":"Lane, John W. Jr. jwlane@usgs.gov","contributorId":1738,"corporation":false,"usgs":true,"family":"Lane","given":"John","suffix":"Jr.","email":"jwlane@usgs.gov","middleInitial":"W.","affiliations":[{"id":486,"text":"OGW Branch of Geophysics","active":true,"usgs":true}],"preferred":false,"id":209781,"contributorType":{"id":1,"text":"Authors"},"rank":2},{"text":"Singha, Kamini","contributorId":76733,"corporation":false,"usgs":true,"family":"Singha","given":"Kamini","affiliations":[],"preferred":false,"id":209783,"contributorType":{"id":1,"text":"Authors"},"rank":3},{"text":"Haeni, F. Peter","contributorId":41479,"corporation":false,"usgs":true,"family":"Haeni","given":"F.","email":"","middleInitial":"Peter","affiliations":[],"preferred":false,"id":209782,"contributorType":{"id":1,"text":"Authors"},"rank":4}]}}
,{"id":61492,"text":"mf2388 - 2002 - Generalized surficial geologic map of the Pueblo 1° x 2° quadrangle, Colorado","interactions":[],"lastModifiedDate":"2021-10-08T21:53:41.514908","indexId":"mf2388","displayToPublicDate":"2002-05-01T00:00:00","publicationYear":"2002","noYear":false,"publicationType":{"id":18,"text":"Report"},"publicationSubtype":{"id":5,"text":"USGS Numbered Series"},"seriesTitle":{"id":325,"text":"Miscellaneous Field Studies Map","code":"MF","active":false,"publicationSubtype":{"id":5}},"seriesNumber":"2388","title":"Generalized surficial geologic map of the Pueblo 1° x 2° quadrangle, Colorado","docAbstract":"Fifty-three types of surficial geologic deposits and residual materials of Quaternary age are described in a pamphlet and located on a map of the greater Pueblo area, in part of the Front Range, in the Wet and Sangre de Cristo Mountains, and on the plains east of Colorado Springs and Pueblo. Deposits formed by landslides, wind, and glaciers, as well as colluvium, residuum, alluvium, and others are described in terms of predominant grain size, mineral or rock composition (e.g., gypsiferous, calcareous, granitic, andesitic), thickness, and other physical characteristics. Origins and ages of the deposits and geologic hazards related to them are noted. Many lines drawn between units on our map were placed by generalizing contacts on published maps. However, in 1997-1999 we mapped new boundaries as well. The map was projected to the UTM projection. This large map area extends from near Salida (on the west edge), eastward about 107 mi (172 km), and from Antero Reservoir and Woodland Park on the north edge to near Colorado City at the south edge (68 mi; 109 km).","language":"English","publisher":"U.S. Geological Survey","publisherLocation":"Reston, VA","doi":"10.3133/mf2388","usgsCitation":"Moore, D.W., Straub, A.W., Berry, M.E., Baker, M.L., and Brandt, T.R., 2002, Generalized surficial geologic map of the Pueblo 1° x 2° quadrangle, Colorado: U.S. Geological Survey Miscellaneous Field Studies Map 2388, HTML Document, https://doi.org/10.3133/mf2388.","productDescription":"HTML Document","costCenters":[],"links":[{"id":187068,"rank":0,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/thumbnails/usgs_thumb.jpg"},{"id":6055,"rank":100,"type":{"id":15,"text":"Index Page"},"url":"https://pubs.usgs.gov/mf/2002/mf-2388/","linkFileType":{"id":5,"text":"html"}},{"id":110293,"rank":700,"type":{"id":36,"text":"NGMDB Index Page"},"url":"https://ngmdb.usgs.gov/Prodesc/proddesc_51522.htm","linkFileType":{"id":5,"text":"html"},"description":"51522"}],"scale":"250000","country":"United States","state":"Colorado","otherGeospatial":"Pueblo 1° x 2° quadrangle","geographicExtents":"{ \"type\": \"FeatureCollection\", \"features\": [ { \"type\": \"Feature\", \"properties\": {}, \"geometry\": { \"type\": \"Polygon\", \"coordinates\": [ [ [ -106,38 ], [ -106,39 ], [ -104,39 ], [ -104,38 ], [ -106,38 ] ] ] } } ] }","noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"4f4e4b24e4b07f02db6aec5c","contributors":{"authors":[{"text":"Moore, D. W.","contributorId":93431,"corporation":false,"usgs":true,"family":"Moore","given":"D.","email":"","middleInitial":"W.","affiliations":[],"preferred":false,"id":265808,"contributorType":{"id":1,"text":"Authors"},"rank":1},{"text":"Straub, A. W.","contributorId":65164,"corporation":false,"usgs":true,"family":"Straub","given":"A.","email":"","middleInitial":"W.","affiliations":[],"preferred":false,"id":265804,"contributorType":{"id":1,"text":"Authors"},"rank":2},{"text":"Berry, M. E.","contributorId":78817,"corporation":false,"usgs":true,"family":"Berry","given":"M.","email":"","middleInitial":"E.","affiliations":[],"preferred":false,"id":265807,"contributorType":{"id":1,"text":"Authors"},"rank":3},{"text":"Baker, M. L.","contributorId":77234,"corporation":false,"usgs":true,"family":"Baker","given":"M.","email":"","middleInitial":"L.","affiliations":[],"preferred":false,"id":265805,"contributorType":{"id":1,"text":"Authors"},"rank":4},{"text":"Brandt, T. R.","contributorId":77553,"corporation":false,"usgs":true,"family":"Brandt","given":"T.","email":"","middleInitial":"R.","affiliations":[],"preferred":false,"id":265806,"contributorType":{"id":1,"text":"Authors"},"rank":5}]}}
,{"id":32336,"text":"fs03602 - 2002 - Occurrence of bacteria in Blue Marsh Lake and selected tributaries, Berks County, Pennsylvania: September-October 2001","interactions":[],"lastModifiedDate":"2022-12-06T20:38:19.568005","indexId":"fs03602","displayToPublicDate":"2002-05-01T00:00:00","publicationYear":"2002","noYear":false,"publicationType":{"id":18,"text":"Report"},"publicationSubtype":{"id":5,"text":"USGS Numbered Series"},"seriesTitle":{"id":313,"text":"Fact Sheet","code":"FS","onlineIssn":"2327-6932","printIssn":"2327-6916","active":true,"publicationSubtype":{"id":5}},"seriesNumber":"036-02","title":"Occurrence of bacteria in Blue Marsh Lake and selected tributaries, Berks County, Pennsylvania: September-October 2001","docAbstract":"<p>The Commonwealth of Pennsylvania has water-quality standards that limit the number of specific bacteria in water that is considered safe for recreational use. Bacteria such as fecal streptococci, fecal coliforms, and <i>Escherichia coli</i> <i>(E. coli</i>) are used to assess recreational water quality because they usually live in the intestines of warm-blooded animals. Fecal indicator bacteria commonly are associated with waterborne disease-causing organisms (pathogens). These indicator bacteria are used routinely as a measure of the quality of water for recreational activities such as swimming, boating, and water skiing. If the indicator bacteria are present, effective measures could be taken to prevent the transmission or epidemic outbreak of waterborne diseases as a result of contamination of these waters from human or animal waste.</p><p>Blue Marsh Lake is on Tulpehocken Creek in Berks County, Pa., and drains a largely agricultural basin. Land use in the basin is approximately 60 percent cropland, and 85 percent of the farms are livestock and poultry farms.</p><p>The potential sources of fecal bacteria are:</p><ul><ul><li>geese that inhabit the recreational areas of the lake,</li><li>humans that visit the Dry Brooks Day Use Area (swimming area), and</li><li>farm animals, wastewater facilities, and household septic systems in the basin (bacteria from these sources could enter the lake through tributaries).</li></ul></ul><p>To meet the recreational water-quality standard, lake water may not have more than 200 colony-forming units (CFU) of fecal coliforms per 100 milliliters (mL). During the week of July 23, 2001, data collected by the U.S. Army Corps of Engineers (USACE) at the swimming area at Blue Marsh Lake showed concentrations of fecal coliforms in the water exceeding the standard. To determine the extent of elevated concentrations of fecal indicator bacteria, further study of the lake and selected tributaries was needed.</p>","language":"English","publisher":"U.S. Geological Survey","publisherLocation":"Reston, VA","doi":"10.3133/fs03602","collaboration":"Prepared in cooperation with the Berks County Conservancy","usgsCitation":"Zimmerman, M.L., 2002, Occurrence of bacteria in Blue Marsh Lake and selected tributaries, Berks County, Pennsylvania: September-October 2001: U.S. Geological Survey Fact Sheet 036-02, 2 p., https://doi.org/10.3133/fs03602.","productDescription":"2 p.","costCenters":[{"id":532,"text":"Pennsylvania Water Science Center","active":true,"usgs":true}],"links":[{"id":410114,"rank":3,"type":{"id":36,"text":"NGMDB Index Page"},"url":"https://ngmdb.usgs.gov/Prodesc/proddesc_51829.htm","linkFileType":{"id":5,"text":"html"}},{"id":121759,"rank":0,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/fs/2002/0036/coverthb.jpg"},{"id":60349,"rank":300,"type":{"id":11,"text":"Document"},"url":"https://pubs.usgs.gov/fs/2002/0036/fs20020036.pdf","text":"Report","linkFileType":{"id":1,"text":"pdf"},"description":"FS 2002-0036"}],"country":"United States","state":"Pennsylvania","county":"Berks County","otherGeospatial":"Blue Marsh Lake","geographicExtents":"{\n  \"type\": \"FeatureCollection\",\n  \"features\": [\n    {\n      \"type\": \"Feature\",\n      \"properties\": {},\n      \"geometry\": {\n        \"type\": \"Polygon\",\n        \"coordinates\": [\n          [\n            [\n              -76.1239242553711,\n              40.35360859593346\n            ],\n            [\n              -75.99517822265625,\n              40.35360859593346\n            ],\n            [\n              -75.99517822265625,\n              40.43153030189336\n            ],\n            [\n              -76.1239242553711,\n              40.43153030189336\n            ],\n            [\n              -76.1239242553711,\n              40.35360859593346\n            ]\n          ]\n        ]\n      }\n    }\n  ]\n}","contact":"<p><a href=\"mailto:dc_pa@usgs.gov\" data-mce-href=\"mailto:dc_pa@usgs.gov\">Director</a>, <a href=\"https://pa.water.usgs.gov/\" data-mce-href=\"https://pa.water.usgs.gov/\">Pennsylvania Water Science Center</a><br> U.S. Geological Survey<br> 215 Limekiln Road <br> New Cumberland, PA 17070</p>","tableOfContents":"<ul><li>How Was This Study Done?</li><li>What Were the Study Results?</li><li>References Cited</li></ul>","noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"4f4e4af6e4b07f02db6929c7","contributors":{"authors":[{"text":"Zimmerman, Michele L.","contributorId":44199,"corporation":false,"usgs":true,"family":"Zimmerman","given":"Michele","email":"","middleInitial":"L.","affiliations":[],"preferred":false,"id":208297,"contributorType":{"id":1,"text":"Authors"},"rank":1}]}}
,{"id":32361,"text":"ofr0233 - 2002 - Landslides triggered by Hurricane Mitch in Tegucigalpa, Honduras","interactions":[],"lastModifiedDate":"2017-03-07T11:42:52","indexId":"ofr0233","displayToPublicDate":"2002-05-01T00:00:00","publicationYear":"2002","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":"2002-33","title":"Landslides triggered by Hurricane Mitch in Tegucigalpa, Honduras","docAbstract":"<p>The arrival of Hurricane Mitch in Honduras in the latter part of the 1998 hurricane season produced effects that were unprecedented in their widespread nature throughout Central America. After winds from the storm had blown down more than 70 percent of the conifer forest on the Bay Island of Guanaja, the hurricane turned inland and stalled over the mainland of Honduras for 3 days. The resulting deluge of rainfall produced devastating flooding and landslides that resulted in more than 9,000 fatalities and 3 million people displaced. Although the eye of Hurricane Mitch passed through the northern part of Honduras, the greatest rainfall totals and intensities occurred in the southern part of the country near Choluteca. For the three days October 29-31, 1998, total rainfall at Choluteca exceeded 900 mm. Not surprisingly, it was in this area that the highest landslide concentrations occurred.</p>","language":"English","publisher":"U.S. Geological Survey","doi":"10.3133/ofr0233","usgsCitation":"Harp, E.L., Castaneda, M., and Held, M.D., 2002, Landslides triggered by Hurricane Mitch in Tegucigalpa, Honduras: U.S. Geological Survey Open-File Report 2002-33, Also available in Spanish. 11 p., 1 over-size sheet., https://doi.org/10.3133/ofr0233.","productDescription":"Also available in Spanish. 11 p., 1 over-size sheet.","costCenters":[],"links":[{"id":3343,"rank":100,"type":{"id":15,"text":"Index Page"},"url":"https://pubs.usgs.gov/of/2002/ofr-02-0033/","linkFileType":{"id":5,"text":"html"}},{"id":161366,"rank":0,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/thumbnails/usgs_thumb.jpg"}],"country":"Honduras","geographicExtents":"{\"type\":\"FeatureCollection\",\"features\":[{\"type\":\"Feature\",\"geometry\":{\"type\":\"Polygon\",\"coordinates\":[[[-87.31665,12.98469],[-87.48941,13.29753],[-87.79311,13.38448],[-87.7235,13.78505],[-87.85952,13.89331],[-88.06534,13.96463],[-88.504,13.84549],[-88.54123,13.98015],[-88.84307,14.14051],[-89.05851,14.34003],[-89.35333,14.42413],[-89.14554,14.67802],[-89.22522,14.87429],[-89.15481,15.06642],[-88.68068,15.34625],[-88.22502,15.72772],[-88.12115,15.68866],[-87.90181,15.86446],[-87.61568,15.8788],[-87.52292,15.79728],[-87.36776,15.84694],[-86.90319,15.75671],[-86.44095,15.78284],[-86.11923,15.89345],[-86.00195,16.00541],[-85.68332,15.95365],[-85.444,15.88575],[-85.18244,15.90916],[-84.98372,15.99592],[-84.52698,15.85722],[-84.36826,15.83516],[-84.06305,15.64824],[-83.77398,15.42407],[-83.41038,15.2709],[-83.14722,14.99583],[-83.48999,15.01627],[-83.62858,14.88007],[-83.97572,14.74944],[-84.22834,14.74876],[-84.44934,14.62161],[-84.64958,14.66681],[-84.82004,14.81959],[-84.9245,14.79049],[-85.05279,14.55154],[-85.14875,14.5602],[-85.16536,14.35437],[-85.51441,14.07901],[-85.69867,13.96008],[-85.80129,13.83605],[-86.09626,14.03819],[-86.31214,13.77136],[-86.52071,13.77849],[-86.75509,13.75485],[-86.73382,13.26309],[-86.88056,13.2542],[-87.00577,13.02579],[-87.31665,12.98469]]]},\"properties\":{\"name\":\"Honduras\"}}]}","noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"4f4e4b1be4b07f02db6a91bc","contributors":{"authors":[{"text":"Harp, Edwin L. harp@usgs.gov","contributorId":1290,"corporation":false,"usgs":true,"family":"Harp","given":"Edwin","email":"harp@usgs.gov","middleInitial":"L.","affiliations":[{"id":218,"text":"Denver Federal Center","active":false,"usgs":true}],"preferred":false,"id":208412,"contributorType":{"id":1,"text":"Authors"},"rank":1},{"text":"Castaneda, Mario","contributorId":25605,"corporation":false,"usgs":true,"family":"Castaneda","given":"Mario","affiliations":[],"preferred":false,"id":208413,"contributorType":{"id":1,"text":"Authors"},"rank":2},{"text":"Held, Matthew D.","contributorId":37384,"corporation":false,"usgs":true,"family":"Held","given":"Matthew","email":"","middleInitial":"D.","affiliations":[],"preferred":false,"id":208414,"contributorType":{"id":1,"text":"Authors"},"rank":3}]}}
,{"id":32365,"text":"ofr0268 - 2002 - Results of streamflow gain-loss studies in Texas, with emphasis on gains from and losses to major and minor aquifers, Texas, 2000","interactions":[],"lastModifiedDate":"2017-01-12T15:27:19","indexId":"ofr0268","displayToPublicDate":"2002-05-01T00:00:00","publicationYear":"2002","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":"2002-68","title":"Results of streamflow gain-loss studies in Texas, with emphasis on gains from and losses to major and minor aquifers, Texas, 2000","docAbstract":"Data for all 366 known streamflow gain-loss studies conducted by the U.S. Geological Survey in Texas were aggregated. A water-budget equation that includes discharges for main channels, tributaries, return flows, and withdrawals was used to document the channel gain or loss for each of 2,872 subreaches for the studies. The channel gain or loss represents discharge from or recharge to aquifers crossed by the streams. Where applicable, the major or minor aquifer outcrop traversed by each subreach was identified, as was the length and location for each subreach. These data will be used to estimate recharge or discharge for major and minor aquifers in Texas, as needed by the Ground-Water Availability Modeling Program being conducted by the Texas Water Development Board. The data also can be used, along with current flow rates for streamflow-gaging stations, to estimate streamflow at sites remote from gaging stations, including sites where streamflow availability is needed for permitted withdrawals.","language":"English","publisher":"U.S. Geological Survey","doi":"10.3133/ofr0268","collaboration":"In cooperation with the Texas Water Development Board","usgsCitation":"Slade, R.M., Bentley, J.T., and Michaud, D., 2002, Results of streamflow gain-loss studies in Texas, with emphasis on gains from and losses to major and minor aquifers, Texas, 2000: U.S. Geological Survey Open-File Report 2002-68, HTML Document; Report: iii, 131 p., https://doi.org/10.3133/ofr0268.","productDescription":"HTML Document; Report: iii, 131 p.","costCenters":[{"id":583,"text":"Texas Water Science 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,{"id":32377,"text":"ofr02162 - 2002 - Multibeam mapping of the Los Angeles, California Margin","interactions":[],"lastModifiedDate":"2014-03-07T10:53:28","indexId":"ofr02162","displayToPublicDate":"2002-05-01T00:00:00","publicationYear":"2002","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":"2002-162","title":"Multibeam mapping of the Los Angeles, California Margin","docAbstract":"<p>The Los Angeles, California Margin was mapped using multibeam echosounders during three separate surveys (Figure 1). In 1996, the USGS surveyed the shelf and slope in Santa Monica Bay from Pt. Dume to south of the Palos Verdes Peninsula. The mapping was accomplished using a Kongsberg Simrad EM1000 multibeam sonar system that provided high-quality bathymetry and quantitative backscatter. In 1998, the USGS continued the mapping to the south and surveyed the outer shelf, slope, and proximal basin off Long Beach and Newport using a Kongsberg Simrad EM300 multibeam sonar system. In 1999, the Los Angeles Margin mapping was completed with the surveying of the inner Long Beach shelf from the Palos Verdes Peninsula, south to Newport. This survey used a dual Kongsberg Simrad EM3000D multibeam sonar system.</p>\n<br/>\n<p>These three surveys were conducted to support USGS projects studying marine pollution and geohazards along the Los Angeles Margin.</p>","language":"English","publisher":"U.S. Geological Survey","doi":"10.3133/ofr02162","usgsCitation":"Gardner, J.V., and Dartnell, P., 2002, Multibeam mapping of the Los Angeles, California Margin: U.S. Geological Survey Open-File Report 2002-162, HTML Document, https://doi.org/10.3133/ofr02162.","productDescription":"HTML Document","onlineOnly":"Y","costCenters":[{"id":520,"text":"Pacific Coastal and Marine Science Center","active":true,"usgs":true}],"links":[{"id":163574,"rank":0,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/thumbnails/ofr02162.gif"},{"id":3362,"rank":100,"type":{"id":15,"text":"Index Page"},"url":"https://pubs.usgs.gov/of/2002/0162/","linkFileType":{"id":5,"text":"html"}},{"id":283469,"type":{"id":11,"text":"Document"},"url":"https://pubs.usgs.gov/of/2002/0162/intro.html"}],"country":"United States","state":"California","otherGeospatial":"Los Angeles Margin","geographicExtents":"{ \"type\": \"FeatureCollection\", \"features\": [ { \"type\": \"Feature\", \"properties\": {}, \"geometry\": { \"type\": \"Polygon\", \"coordinates\": [ [ [ -119.212,33.3017 ], [ -119.212,34.3373 ], [ -117.5016,34.3373 ], [ -117.5016,33.3017 ], [ -119.212,33.3017 ] ] ] } } ] }","noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"4f4e4b02e4b07f02db698bd6","contributors":{"authors":[{"text":"Gardner, James V.","contributorId":93035,"corporation":false,"usgs":true,"family":"Gardner","given":"James","email":"","middleInitial":"V.","affiliations":[],"preferred":false,"id":208469,"contributorType":{"id":1,"text":"Authors"},"rank":1},{"text":"Dartnell, Peter 0000-0002-9554-729X pdartnell@usgs.gov","orcid":"https://orcid.org/0000-0002-9554-729X","contributorId":2688,"corporation":false,"usgs":true,"family":"Dartnell","given":"Peter","email":"pdartnell@usgs.gov","affiliations":[{"id":520,"text":"Pacific Coastal and Marine Science Center","active":true,"usgs":true}],"preferred":true,"id":208468,"contributorType":{"id":1,"text":"Authors"},"rank":2}]}}
,{"id":32358,"text":"ofr01473 - 2002 - Coalbed gas in Hungary; a preliminary report","interactions":[],"lastModifiedDate":"2025-12-09T17:47:29.212991","indexId":"ofr01473","displayToPublicDate":"2002-05-01T00:00:00","publicationYear":"2002","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":"2001-473","title":"Coalbed gas in Hungary; a preliminary report","docAbstract":"<p>No abstract available.</p>","language":"English","publisher":"U.S. Geological Survey","doi":"10.3133/ofr01473","usgsCitation":"Landis, E., Rohrbacher, T., Barker, C., Fodor, B., and Gombar, G., 2002, Coalbed gas in Hungary; a preliminary report (Version 1.0): U.S. Geological Survey Open-File Report 2001-473, 28 p., https://doi.org/10.3133/ofr01473.","productDescription":"28 p.","costCenters":[],"links":[{"id":3341,"rank":2,"type":{"id":15,"text":"Index Page"},"url":"https://pubs.usgs.gov/of/2001/ofr-01-473/index.html","linkFileType":{"id":5,"text":"html"}},{"id":161288,"rank":1,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/thumbnails/usgs_thumb.jpg"}],"edition":"Version 1.0","noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"4f4e4b24e4b07f02db6aec52","contributors":{"authors":[{"text":"Landis, E.R.","contributorId":40605,"corporation":false,"usgs":true,"family":"Landis","given":"E.R.","email":"","affiliations":[],"preferred":false,"id":208406,"contributorType":{"id":1,"text":"Authors"},"rank":1},{"text":"Rohrbacher, T.J.","contributorId":56274,"corporation":false,"usgs":true,"family":"Rohrbacher","given":"T.J.","affiliations":[],"preferred":false,"id":208408,"contributorType":{"id":1,"text":"Authors"},"rank":2},{"text":"Barker, C.E.","contributorId":69991,"corporation":false,"usgs":true,"family":"Barker","given":"C.E.","affiliations":[],"preferred":false,"id":208409,"contributorType":{"id":1,"text":"Authors"},"rank":3},{"text":"Fodor, Bela","contributorId":53850,"corporation":false,"usgs":true,"family":"Fodor","given":"Bela","email":"","affiliations":[],"preferred":false,"id":208407,"contributorType":{"id":1,"text":"Authors"},"rank":4},{"text":"Gombar, Gizella","contributorId":39830,"corporation":false,"usgs":true,"family":"Gombar","given":"Gizella","email":"","affiliations":[],"preferred":false,"id":208405,"contributorType":{"id":1,"text":"Authors"},"rank":5}]}}
,{"id":32369,"text":"ofr02125 - 2002 - Mineralogical characterization of strata of the Meade Peak phosphatic shale member of the Permian Phosphoria Formation: Channel and individual rock samples of measured section J and their relationship to measured sections A and B, central part of Rasmussen Ridge, Caribou County, Idaho","interactions":[],"lastModifiedDate":"2023-06-27T15:30:27.38917","indexId":"ofr02125","displayToPublicDate":"2002-05-01T00:00:00","publicationYear":"2002","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":"2002-125","title":"Mineralogical characterization of strata of the Meade Peak phosphatic shale member of the Permian Phosphoria Formation: Channel and individual rock samples of measured section J and their relationship to measured sections A and B, central part of Rasmussen Ridge, Caribou County, Idaho","docAbstract":"The Permian Phosphoria Formation of southeastern Idaho hosts one of the largest phosphate deposits in the world. Despite the economic significance of this Formation, the fine-grained nature of the phosphorite has discouraged detailed mineralogical characterization and quantification studies. Recently, selenium and other potentially toxic trace elements in mine wastes have drawn increased attention to this formation, and motivated additional study. This study uses powder X-ray diffraction (XRD), with Rietveld quantification software, to quantify and characterize the mineralogy of composite channel samples and individual samples collected from the stratigraphic sections measured by the U.S. Geological Survey in the Meade Peak Member of the Permian Phosphoria Formation at the Enoch Valley mine on Rasmussen Ridge, approximately 15 miles northeast of Soda Springs, Idaho.","language":"English","publisher":"U.S. Geological Survey","doi":"10.3133/ofr02125","usgsCitation":"Knudsen, A.C., Gunter, M.E., Herring, J., and Grauch, R., 2002, Mineralogical characterization of strata of the Meade Peak phosphatic shale member of the Permian Phosphoria Formation: Channel and individual rock samples of measured section J and their relationship to measured sections A and B, central part of Rasmussen Ridge, Caribou County, Idaho: U.S. Geological Survey Open-File Report 2002-125, Report: 38 p.; Readme, https://doi.org/10.3133/ofr02125.","productDescription":"Report: 38 p.; Readme","numberOfPages":"38","additionalOnlineFiles":"Y","costCenters":[{"id":312,"text":"Geology, Minerals, Energy, and Geophysics Science Center","active":true,"usgs":true}],"links":[{"id":163401,"rank":1,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/thumbnails/ofr02125.jpg"},{"id":283455,"rank":3,"type":{"id":20,"text":"Read Me"},"url":"https://pubs.usgs.gov/of/2002/0125/README"},{"id":3357,"rank":5,"type":{"id":15,"text":"Index Page"},"url":"https://pubs.usgs.gov/of/2002/0125/","linkFileType":{"id":5,"text":"html"}},{"id":404597,"rank":4,"type":{"id":36,"text":"NGMDB Index Page"},"url":"https://ngmdb.usgs.gov/Prodesc/proddesc_51547.htm","linkFileType":{"id":5,"text":"html"}},{"id":283454,"rank":2,"type":{"id":11,"text":"Document"},"url":"https://pubs.usgs.gov/of/2002/0125/pdf/of02-125.pdf","linkFileType":{"id":1,"text":"pdf"}}],"country":"United States","state":"Idaho","county":"Caribou County","otherGeospatial":"Rasmussen Ridge","geographicExtents":"{\n  \"type\": \"FeatureCollection\",\n  \"features\": [\n    {\n      \"type\": \"Feature\",\n      \"properties\": {},\n      \"geometry\": {\n        \"type\": \"Polygon\",\n        \"coordinates\": [\n          [\n            [\n              -111.4417,\n              42.7333\n            ],\n            [\n              -111.3,\n              42.7333\n            ],\n            [\n              -111.3,\n              42.9167\n            ],\n            [\n              -111.4417,\n              42.9167\n            ],\n            [\n              -111.4417,\n              42.7333\n            ]\n          ]\n        ]\n      }\n    }\n  ]\n}","noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"4f4e4b05e4b07f02db699e56","contributors":{"authors":[{"text":"Knudsen, A. 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,{"id":32371,"text":"ofr02132 - 2002 - Distribution of high-temperature (>150 °C) geothermal resources in California","interactions":[],"lastModifiedDate":"2023-06-27T15:31:50.758053","indexId":"ofr02132","displayToPublicDate":"2002-05-01T00:00:00","publicationYear":"2002","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":"2002-132","title":"Distribution of high-temperature (>150 °C) geothermal resources in California","docAbstract":"California contains, by far, the greatest geothermal generating capacity in the United States, and with the possible exception of Alaska, the greatest potential for the development of additional resources. California has nearly 2/3 of the US geothermal electrical installed capacity of over 3,000 MW. Depending on assumptions regarding reservoir characteristics and future market conditions, additional resources of between 2,000 and 10,000 MWe might be developed (see e.g., Muffler, 1979).","language":"English","publisher":"U.S. Geological Survey","doi":"10.3133/ofr02132","usgsCitation":"Sass, J.H., and Priest, S.S., 2002, Distribution of high-temperature (>150 °C) geothermal resources in California: U.S. Geological Survey Open-File Report 2002-132, 4 p., https://doi.org/10.3133/ofr02132.","productDescription":"4 p.","numberOfPages":"4","additionalOnlineFiles":"Y","costCenters":[{"id":312,"text":"Geology, Minerals, Energy, and Geophysics Science Center","active":true,"usgs":true}],"links":[{"id":3358,"rank":5,"type":{"id":15,"text":"Index 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 \"}}]}","noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"4f4e4a6fe4b07f02db640a17","contributors":{"authors":[{"text":"Sass, John H.","contributorId":69596,"corporation":false,"usgs":true,"family":"Sass","given":"John","email":"","middleInitial":"H.","affiliations":[],"preferred":false,"id":208444,"contributorType":{"id":1,"text":"Authors"},"rank":1},{"text":"Priest, Susan S. spriest@usgs.gov","contributorId":30204,"corporation":false,"usgs":true,"family":"Priest","given":"Susan","email":"spriest@usgs.gov","middleInitial":"S.","affiliations":[],"preferred":false,"id":208443,"contributorType":{"id":1,"text":"Authors"},"rank":2}]}}
,{"id":33056,"text":"wri014033 - 2002 - Borehole-geophysical investigation of the University of Connecticut landfill, Storrs, Connecticut","interactions":[],"lastModifiedDate":"2019-10-15T12:09:46","indexId":"wri014033","displayToPublicDate":"2002-05-01T00:00:00","publicationYear":"2002","noYear":false,"publicationType":{"id":18,"text":"Report"},"publicationSubtype":{"id":5,"text":"USGS Numbered Series"},"seriesTitle":{"id":342,"text":"Water-Resources Investigations Report","code":"WRI","active":false,"publicationSubtype":{"id":5}},"seriesNumber":"2001-4033","title":"Borehole-geophysical investigation of the University of Connecticut landfill, Storrs, Connecticut","docAbstract":"<p>A borehole-geophysical investigation was conducted to help characterize the hydrogeology of the fractured-rock aquifer and the distribution of unconsolidated glacial deposits near the former landfill and chemical waste-disposal pits at the University of Connecticut in Storrs, Connecticut. Eight bedrock boreholes near the landfill and three abandoned domestic wells located nearby were logged using conventional and advanced borehole-geophysical methods from June to October 1999. The conventional geophysical-logging methods included caliper, gamma, fluid temperature, fluid resistivity, and electromagnetic induction. The advanced methods included deviation, optical and acoustic imaging of the borehole wall, heat-pulse flowmeter, and directional radar reflection. Twenty-one shallow piezometers (less than 50-feet deep) were logged with gamma and electromagnetic induction tools to delineate unconsolidated glacial deposits. Five additional shallow bedrock wells were logged with conventional video camera, caliper, electromagnetic induction, and fluid resistivity and temperature tools. </p><p>The rock type, foliation, and fracturing of the site were characterized from high-resolution optical-televiewer (OTV) images of rocks penetrated by the boreholes. The rocks are interpreted as fine- to medium-grained quartz-feldsparbiotite-garnet gneiss and schist with local intrusions of quartz diorite and pegmatite and minor concentrations of sulfide mineralization similar to rocks described as the Bigelow Brook Formation on regional geologic maps. Layers containing high concentrations of sulfide minerals appear as high electrical conductivity zones on electromagneticinduction and borehole-radar logs. Foliation in the rocks generally strikes to the northeast-southwest and dips to the west, consistent with local outcrop observations. The orientation of foliation and small-scale gneissic layering in the rocks, however, varies locally and with depth in some of the boreholes. In two of the boreholes, the foliation strikes predominantly to the northwest and dips to the northeast. Although small-scale faults and lithologic discontinuities were observed in the OTV data, no large-scale faults were observed that appear on regional geologic maps. </p><p>Fractures were located and characterized through the use of conventional geophysical, OTV, acoustic-televiewer (ATV), and borehole-radar logs. The orientation of fractures varies considerably across the site; some fractures are parallel to the foliation, whereas others cross-cut the foliation. Many of the transmissive fractures in the bedrock boreholes strike about N170°E and N320°E with dips of less than 45°. Other transmissive fractures strike about N60°E with dips of more than 60°. Most of the transmissive fractures in the domestic wells strike about N60°E and N22°E with dips of more than 45°. The strike of N60°E is parallel to the trend of a thrust fault that appears on regional geologic maps. Vertical flow in the boreholes was measured with the heat-pulse flowmeter under ambient and (or) pumping conditions. Results of ATV, OTV, and conventional logs were used to locate specific zones for flowmeter testing. Ambient downflow was measured in three boreholes, ambient upflow was measured in two other boreholes, and both ambient downflow and upflow were measured in a sixth borehole. The other five bedrock boreholes and domestic wells did not have measurable vertical flow. The highest rate of ambient flow was measured in the background borehole in which upflow and downflow converged and exited the borehole at a fracture zone near a depth of 62 feet. Ambient flow of about 340 gallons per day was measured. In the other five wells, ambient flow of about 20 to 35 gallons per day was measured. Under low-rate pumping (0.25 to 1 gallon per minute), one to six inflow zones were identified in each well. Usually the fractures that are active under ambient conditions contribute to the well under pumping conditions. To prevent ambient vertical flow and the potential for cross-contamination, temporary borehole liners were installed in five of the boreholes. </p><p>Specific-capacity and open-hole transmissivity values were determined in eight boreholes completed in bedrock. The specific capacity estimated for these boreholes ranges from 0.14 to 1.6 gallons per minute per foot. The values for open-hole transmissivity range over two orders of magnitude and when proportioned to individual fracture transmissivity, range from 23 to 340 feet squared per day. </p><p>Two boreholes had been drilled to intersect electrically conductive zones identified by previous surface-geophysical investigations. The borehole-geophysical results indicate that the boreholes penetrate electrically conductive structures consistent with the anomalies interpreted from the surface-geophysical data. Borehole MW121R was located to intersect a dipping electrically conductive anomaly at about 60 feet, interpreted from the two-dimensional direct currentresistivity survey conducted on the western side of the landfill. The electromagnetic-conductivity log in the borehole contains a high electrical conductivity anomaly at a depth of 69 feet. The magnitude of this anomaly is nearly 10,000 millisiemens per meter and is coincident with a layer containing sulfide mineralization, rather than fractures. </p><p>The other borehole, MW105R, was located to intersect another anomaly south of the landfill. This anomaly was interpreted as a north-south striking, westward dipping feature. In the borehole, two south-striking, westward dipping fractures were identified in the ATV, OTV, and radar logs. The specific conductance of the fluid measured near these fractures was as high as 1,250 microsiemens per centimeter. Water-quality samples collected in October 1999 from an isolated zone from 71.5 to 76.5 feet indicated high specific conductance (810 microsiemens per centimeter), high concentrations of iron and cadmium, negative oxidation-reduction potential, and chlorobenzene. Collectively, these parameters indicate that the high specific conductance in the borehole logs for MW105R was caused by landfill leachate. Therefore, the anomaly identified by boreholeand surface-geophysical surveys is interpreted as a conductive lithologic feature and a permeable fracture zone that contains landfill leachate. </p>","language":"English","publisher":"U.S. Geological Survey","doi":"10.3133/wri014033","usgsCitation":"Johnson, C.D., Haeni, F., Lane, J.W., and White, E.A., 2002, Borehole-geophysical investigation of the University of Connecticut landfill, Storrs, Connecticut: U.S. Geological Survey Water-Resources Investigations Report 2001-4033, vi, 187 p. , https://doi.org/10.3133/wri014033.","productDescription":"vi, 187 p. ","costCenters":[{"id":493,"text":"Office of Ground Water","active":true,"usgs":true}],"links":[{"id":161201,"rank":0,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/thumbnails/usgs_thumb.jpg"},{"id":3232,"rank":100,"type":{"id":11,"text":"Document"},"url":"https://water.usgs.gov/ogw/bgas/publications/wri014033/wri014033.pdf","linkFileType":{"id":5,"text":"html"}}],"country":"United States","state":"Connecticut","city":"Storrs","geographicExtents":"{\n  \"type\": \"FeatureCollection\",\n  \"features\": [\n    {\n      \"type\": \"Feature\",\n      \"properties\": {},\n      \"geometry\": {\n        \"type\": \"Polygon\",\n        \"coordinates\": [\n          [\n            [\n              -72.27823734283447,\n              41.81108364200336\n            ],\n            [\n              -72.26072788238525,\n              41.81108364200336\n            ],\n            [\n              -72.26072788238525,\n              41.821702387650106\n            ],\n            [\n              -72.27823734283447,\n              41.821702387650106\n            ],\n            [\n              -72.27823734283447,\n              41.81108364200336\n            ]\n          ]\n        ]\n      }\n    }\n  ]\n}","noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"4f4e4a14e4b07f02db6026f8","contributors":{"authors":[{"text":"Johnson, Carole D. 0000-0001-6941-1578 cjohnson@usgs.gov","orcid":"https://orcid.org/0000-0001-6941-1578","contributorId":1891,"corporation":false,"usgs":true,"family":"Johnson","given":"Carole","email":"cjohnson@usgs.gov","middleInitial":"D.","affiliations":[{"id":37277,"text":"WMA - Earth System Processes Division","active":true,"usgs":true}],"preferred":true,"id":209790,"contributorType":{"id":1,"text":"Authors"},"rank":1},{"text":"Haeni, F.P.","contributorId":87105,"corporation":false,"usgs":true,"family":"Haeni","given":"F.P.","affiliations":[],"preferred":false,"id":209791,"contributorType":{"id":1,"text":"Authors"},"rank":2},{"text":"Lane, John W. Jr. jwlane@usgs.gov","contributorId":1738,"corporation":false,"usgs":true,"family":"Lane","given":"John","suffix":"Jr.","email":"jwlane@usgs.gov","middleInitial":"W.","affiliations":[{"id":486,"text":"OGW Branch of Geophysics","active":true,"usgs":true}],"preferred":false,"id":209789,"contributorType":{"id":1,"text":"Authors"},"rank":3},{"text":"White, Eric A. 0000-0002-7782-146X eawhite@usgs.gov","orcid":"https://orcid.org/0000-0002-7782-146X","contributorId":1737,"corporation":false,"usgs":false,"family":"White","given":"Eric","email":"eawhite@usgs.gov","middleInitial":"A.","affiliations":[],"preferred":true,"id":209788,"contributorType":{"id":1,"text":"Authors"},"rank":4}]}}
,{"id":32375,"text":"ofr02158 - 2002 - Moloka'i fieldtrip guidebook: Selected aspects of the geology, geography, and coral reefs of Moloka'i","interactions":[],"lastModifiedDate":"2022-06-29T20:50:43.556901","indexId":"ofr02158","displayToPublicDate":"2002-05-01T00:00:00","publicationYear":"2002","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":"2002-158","title":"Moloka'i fieldtrip guidebook: Selected aspects of the geology, geography, and coral reefs of Moloka'i","docAbstract":"This guidebook was compiled with the express purpose of describing the general geology of Moloka'i and those locations with significance to the U.S. Geological Survey's study of Moloka'i's coral reef, a part of the U.S. Department of Interior's 'Protecting the Nation's Reefs' program.\r\n\r\nThe first portion of the guidebook describes the island and gives the historical background. Fieldtrip stop locations are listed in a logical driving order, essentially from west to east. This order may be changed, or stops deleted, depending on time and scheduling of an individual fieldtrip.","language":"English","publisher":"U.S. Geological Survey","doi":"10.3133/ofr02158","usgsCitation":"Cochran, S., Roberts, L.M., and Evans, K.R., 2002, Moloka'i fieldtrip guidebook: Selected aspects of the geology, geography, and coral reefs of Moloka'i: U.S. Geological Survey Open-File Report 2002-158, vi, 55 p., https://doi.org/10.3133/ofr02158.","productDescription":"vi, 55 p.","onlineOnly":"Y","costCenters":[{"id":645,"text":"Western Coastal and Marine Geology","active":false,"usgs":true}],"links":[{"id":163484,"rank":0,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/thumbnails/usgs_thumb.jpg"},{"id":402718,"rank":3,"type":{"id":36,"text":"NGMDB Index Page"},"url":"https://ngmdb.usgs.gov/Prodesc/proddesc_51459.htm","linkFileType":{"id":5,"text":"html"}},{"id":12045,"rank":100,"type":{"id":15,"text":"Index Page"},"url":"https://pubs.usgs.gov/of/2002/of02-158/","linkFileType":{"id":5,"text":"html"}}],"country":"United States","state":"Hawaii","otherGeospatial":"Moloka'i","geographicExtents":"{\n  \"type\": \"FeatureCollection\",\n  \"features\": [\n    {\n      \"type\": \"Feature\",\n      \"properties\": {},\n      \"geometry\": {\n        \"type\": \"Polygon\",\n        \"coordinates\": [\n          [\n            [\n              -157.30499267578125,\n              21.035800796222002\n            ],\n            [\n              -156.69799804687497,\n              21.035800796222002\n            ],\n            [\n              -156.69799804687497,\n              21.268899719967695\n            ],\n            [\n              -157.30499267578125,\n              21.268899719967695\n            ],\n            [\n              -157.30499267578125,\n              21.035800796222002\n            ]\n          ]\n        ]\n      }\n    }\n  ]\n}","noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"4f4e4b04e4b07f02db699256","contributors":{"authors":[{"text":"Cochran, Susan A.","contributorId":27533,"corporation":false,"usgs":true,"family":"Cochran","given":"Susan A.","affiliations":[],"preferred":false,"id":208463,"contributorType":{"id":1,"text":"Authors"},"rank":1},{"text":"Roberts, Lucile M.","contributorId":7561,"corporation":false,"usgs":true,"family":"Roberts","given":"Lucile","email":"","middleInitial":"M.","affiliations":[],"preferred":false,"id":208462,"contributorType":{"id":1,"text":"Authors"},"rank":2},{"text":"Evans, Kevin R.","contributorId":35724,"corporation":false,"usgs":true,"family":"Evans","given":"Kevin","email":"","middleInitial":"R.","affiliations":[],"preferred":false,"id":208464,"contributorType":{"id":1,"text":"Authors"},"rank":3}]}}
,{"id":32362,"text":"ofr0246 - 2002 - Large-scale cycles of Holocene deposition and erosion at the entrance to Willapa Bay, Washington: Implications for future land loss and coastal change","interactions":[],"lastModifiedDate":"2022-08-09T20:31:21.664571","indexId":"ofr0246","displayToPublicDate":"2002-05-01T00:00:00","publicationYear":"2002","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":"2002-46","title":"Large-scale cycles of Holocene deposition and erosion at the entrance to Willapa Bay, Washington: Implications for future land loss and coastal change","docAbstract":"<p>No abstract available.</p>","language":"English","publisher":"U.S. Geological Survey","doi":"10.3133/ofr0246","usgsCitation":"Morton, R., Purcell, N.A., and Peterson, R.L., 2002, Large-scale cycles of Holocene deposition and erosion at the entrance to Willapa Bay, Washington: Implications for future land loss and coastal change: U.S. Geological Survey Open-File Report 2002-46, iv, 96 p., https://doi.org/10.3133/ofr0246.","productDescription":"iv, 96 p.","costCenters":[],"links":[{"id":405049,"rank":3,"type":{"id":36,"text":"NGMDB Index Page"},"url":"https://ngmdb.usgs.gov/Prodesc/proddesc_51452.htm","linkFileType":{"id":5,"text":"html"}},{"id":60356,"rank":300,"type":{"id":11,"text":"Document"},"url":"https://pubs.usgs.gov/of/2002/0046/report.pdf","linkFileType":{"id":1,"text":"pdf"}},{"id":163928,"rank":0,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/of/2002/0046/report-thumb.jpg"}],"country":"United States","state":"Washington","otherGeospatial":"Willapa Bay","geographicExtents":"{\n  \"type\": \"FeatureCollection\",\n  \"features\": [\n    {\n      \"type\": \"Feature\",\n      \"properties\": {},\n      \"geometry\": {\n        \"type\": \"Polygon\",\n        \"coordinates\": [\n          [\n            [\n              -124.08782958984375,\n              46.66734468444288\n            ],\n            [\n              -123.96286010742188,\n              46.66734468444288\n            ],\n            [\n              -123.96286010742188,\n              46.73986059969267\n            ],\n            [\n              -124.08782958984375,\n              46.73986059969267\n            ],\n            [\n              -124.08782958984375,\n              46.66734468444288\n            ]\n          ]\n        ]\n      }\n    }\n  ]\n}","noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"4f4e4b1be4b07f02db6a8f83","contributors":{"authors":[{"text":"Morton, Robert A.","contributorId":88333,"corporation":false,"usgs":true,"family":"Morton","given":"Robert A.","affiliations":[],"preferred":false,"id":208416,"contributorType":{"id":1,"text":"Authors"},"rank":1},{"text":"Purcell, Noreen A.","contributorId":92714,"corporation":false,"usgs":true,"family":"Purcell","given":"Noreen","email":"","middleInitial":"A.","affiliations":[],"preferred":false,"id":208417,"contributorType":{"id":1,"text":"Authors"},"rank":2},{"text":"Peterson, Russell L.","contributorId":55045,"corporation":false,"usgs":true,"family":"Peterson","given":"Russell","email":"","middleInitial":"L.","affiliations":[],"preferred":false,"id":208415,"contributorType":{"id":1,"text":"Authors"},"rank":3}]}}
,{"id":33062,"text":"wri014244 - 2002 - Spatial patterns and temporal variability in water quality from City of Albuquerque drinking-water supply wells and piezometer nests, with implications for the ground-water flow system","interactions":[],"lastModifiedDate":"2022-09-08T21:57:49.343397","indexId":"wri014244","displayToPublicDate":"2002-05-01T00:00:00","publicationYear":"2002","noYear":false,"publicationType":{"id":18,"text":"Report"},"publicationSubtype":{"id":5,"text":"USGS Numbered Series"},"seriesTitle":{"id":342,"text":"Water-Resources Investigations Report","code":"WRI","active":false,"publicationSubtype":{"id":5}},"seriesNumber":"2001-4244","title":"Spatial patterns and temporal variability in water quality from City of Albuquerque drinking-water supply wells and piezometer nests, with implications for the ground-water flow system","docAbstract":"<p>Water-quality data for 93 City of Albuquerque drinking-water supply wells, 7 deep piezometer nests, and selected additional wells were examined to improve understanding of the regional ground-water system and its response to pumpage. Plots of median values of several major parameters showed discernible water-quality differences both areally and with depth in the aquifer. Areal differences were sufficiently large to enable delineation of five regions of generally distinct water quality, which are consistent with areas of separate recharge defined by previous investigators. Data for deep piezometer nests indicate that water quality generally degrades somewhat with depth, except in areas where local recharge influenced by evapotranspiration or contamination could be affecting shallow water. The orientations of the five water-quality regions indicate that the direction of ground-water flow has historically been primarily north to south. This is generally consistent with maps of predevelopment hydraulic heads, although some areas lack consistency, possibly because of differences in time scales or depths represented by water quality as opposed to hydraulic head. The primary sources of recharge to ground water in the study area appear to be mountain-front recharge along the Sandia Mountains to the east and the Jemez Mountains to the north, seepage from the Rio Grande, and infiltration through Tijeras Arroyo. Elevated concentrations of many chemical constituents in part of the study area appear to be associated with a source of water having large dissolved solids, possibly moving upward from depth. Hydraulic-head data for deep piezometer nests indicate that vertical head gradients differ in direction and magnitude across the study area. Hydraulic-head gradients are downward in the central and western parts of the study area and upward across much of the eastern part, except at the mountain front. Water-quality data for the piezometers indicate that the ground water is not well mixed, even in areas of large vertical gradients. Water levels in most piezometers respond to short-term variations in ground-water withdrawals and to the cumulative effect of long-term withdrawals throughout the area. In most piezometers screened below the water table, water levels respond clearly to seasonal variations in ground-water withdrawals. Water levels decline from about April through July and rise from about September through January. Water levels seem to be declining in most piezometers at a rate less than 1 foot per year. Water-quality data for unfiltered samples collected over a 10-year period from 93 City of Albuquerque drinking-water supply wells were examined for variability and temporal trends in 10 selected parameters. Variability generally was found to be greatest in the Western and Northeast water-quality regions of the study area. For the 10 parameters investigated, temporal trends were found in 5 to 57 wells. Dissolved-solids, sodium, sulfate, chloride, and silica concentrations showed more increasing than decreasing trends; calcium, bicarbonate, and arsenic concentrations, field pH, and water temperature showed more decreasing than increasing trends. The median magnitudes of most of these trends over a 1-year period were not particularly large (generally less than 1.0 milligram per liter), although the magnitudes for a few individual wells were significant. For the 10 parameters investigated, correlations with monthly pumpage volumes were found in 10 to 32 wells. Calcium and sulfate concentrations, field pH, and water temperature showed more positive than negative correlations with monthly pumpage; dissolved-solids, sodium, bicarbonate, chloride, silica, and arsenic concentrations showed more negative than positive correlations.&nbsp;</p>","language":"English","publisher":"U.S. Geological Survey","doi":"10.3133/wri014244","usgsCitation":"Bexfield, L.M., and Anderholm, S.K., 2002, Spatial patterns and temporal variability in water quality from City of Albuquerque drinking-water supply wells and piezometer nests, with implications for the ground-water flow system: U.S. Geological Survey Water-Resources Investigations Report 2001-4244, vi, 101 p., https://doi.org/10.3133/wri014244.","productDescription":"vi, 101 p.","costCenters":[],"links":[{"id":161248,"rank":0,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/wri/2001/4244/report-thumb.jpg"},{"id":95938,"rank":300,"type":{"id":11,"text":"Document"},"url":"https://pubs.usgs.gov/wri/2001/4244/report.pdf","linkFileType":{"id":1,"text":"pdf"}},{"id":406411,"rank":2,"type":{"id":36,"text":"NGMDB Index Page"},"url":"https://ngmdb.usgs.gov/Prodesc/proddesc_51519.htm","linkFileType":{"id":5,"text":"html"}}],"country":"United States","state":"New Mexico","city":"Albuquerque","geographicExtents":"{\n  \"type\": \"FeatureCollection\",\n  \"features\": [\n    {\n      \"type\": \"Feature\",\n      \"properties\": {},\n      \"geometry\": {\n        \"type\": \"Polygon\",\n        \"coordinates\": [\n          [\n            [\n              -106.82830810546875,\n              34.98725337980076\n            ],\n            [\n              -106.46232604980467,\n              34.98725337980076\n            ],\n            [\n              -106.46232604980467,\n              35.20691648822763\n            ],\n            [\n              -106.82830810546875,\n              35.20691648822763\n            ],\n            [\n              -106.82830810546875,\n              34.98725337980076\n            ]\n          ]\n        ]\n      }\n    }\n  ]\n}","noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"4f4e49e5e4b07f02db5e6d62","contributors":{"authors":[{"text":"Bexfield, Laura M. 0000-0002-1789-654X bexfield@usgs.gov","orcid":"https://orcid.org/0000-0002-1789-654X","contributorId":1273,"corporation":false,"usgs":true,"family":"Bexfield","given":"Laura","email":"bexfield@usgs.gov","middleInitial":"M.","affiliations":[{"id":472,"text":"New Mexico Water Science Center","active":true,"usgs":true}],"preferred":true,"id":209804,"contributorType":{"id":1,"text":"Authors"},"rank":1},{"text":"Anderholm, Scott K.","contributorId":94270,"corporation":false,"usgs":true,"family":"Anderholm","given":"Scott","email":"","middleInitial":"K.","affiliations":[],"preferred":false,"id":209805,"contributorType":{"id":1,"text":"Authors"},"rank":2}]}}
,{"id":32366,"text":"ofr0292 - 2002 - Technical guidelines for the implementation of the Advanced National Seismic System","interactions":[],"lastModifiedDate":"2017-03-07T13:45:17","indexId":"ofr0292","displayToPublicDate":"2002-05-01T00:00:00","publicationYear":"2002","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":"2002-92","title":"Technical guidelines for the implementation of the Advanced National Seismic System","docAbstract":"<p>The Advanced National Seismic System (ANSS) is a major national initiative led by the US Geological Survey that serves the needs of the earthquake monitoring, engineering, and research communities as well as national, state, and local governments, emergency response organizations, and the general public. Legislation authorizing the ANSS was passed in 2000, and low levels of funding for planning and initial purchases of new seismic instrumentation have been appropriated beginning in FY2000. When fully operational, the ANSS will be an advanced monitoring system (modern digital seismographs and accelerographs, communications networks, data collection and processing centers, and well-trained personnel) distributed across the United States that operates with high performance standards, gathers critical technical data, and effectively provides timely and reliable earthquake products, information, and services to meet the Nation’s needs. The ANSS will automatically broadcast timely and authoritative products describing the occurrence of earthquakes, earthquake source properties, the distribution of ground shaking, and, where feasible, broadcast early warnings and alerts for the onset of strong ground shaking. Most importantly, the ANSS will provide earthquake data, derived products, and information to the public, emergency responders, officials, engineers, educators, researchers, and other ANSS partners rapidly and in forms that are useful for their needs. </p>","language":"English","publisher":"U.S. Geological Survey","publisherLocation":"Reston, VA","doi":"10.3133/ofr0292","usgsCitation":"Committee, A.T., 2002, Technical guidelines for the implementation of the Advanced National Seismic System: U.S. Geological Survey Open-File Report 2002-92, 92 p., https://doi.org/10.3133/ofr0292.","productDescription":"92 p.","costCenters":[],"links":[{"id":163852,"rank":0,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/thumbnails/usgs_thumb.jpg"},{"id":3354,"rank":100,"type":{"id":15,"text":"Index Page"},"url":"https://pubs.usgs.gov/of/2002/ofr-02-0092/","linkFileType":{"id":5,"text":"html"}}],"noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"4f4e4adce4b07f02db6864c4","contributors":{"authors":[{"text":"Committee, ANSS Technical Integration","contributorId":24826,"corporation":false,"usgs":true,"family":"Committee","given":"ANSS","email":"","middleInitial":"Technical Integration","affiliations":[],"preferred":false,"id":208428,"contributorType":{"id":1,"text":"Authors"},"rank":1}]}}
,{"id":32373,"text":"ofr02139 - 2002 - Magnetic susceptibilities measured on rocks of the upper Cook Inlet, Alaska","interactions":[],"lastModifiedDate":"2018-05-20T17:03:08","indexId":"ofr02139","displayToPublicDate":"2002-05-01T00:00:00","publicationYear":"2002","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":"2002-139","title":"Magnetic susceptibilities measured on rocks of the upper Cook Inlet, Alaska","docAbstract":"We have measured magnetic susceptibility in the field on most of the geologic rock formations exposed in the upper Cook Inlet near Anchorage and Kenai, Alaska. Measured susceptibilities range from less than our detection limit of 0.01 x 10-3 (SI) to greater than 100 x 10-3 (SI). As expected, mafic igneous rocks have the highest susceptibilities and some sedimentary rocks the lowest. Rocks of the Tertiary Sterling Formation yielded some moderate to high susceptibility values. Although we do not have detailed information on the magnetic mineralogy of the rocks measured here, the higher susceptibilities are sufficient to explain the magnitudes of some short-wavelength aeromagnetic anomalies observed on recent surveys of the upper Cook Inlet.","language":"English","publisher":"U.S. Geological Survey","doi":"10.3133/ofr02139","usgsCitation":"Alstatt, A., Saltus, R.W., Bruhn, R., and Haeussler, P.J., 2002, Magnetic susceptibilities measured on rocks of the upper Cook Inlet, Alaska: U.S. Geological Survey Open-File Report 2002-139, 18 p., https://doi.org/10.3133/ofr02139.","productDescription":"18 p.","costCenters":[],"links":[{"id":163482,"rank":0,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/thumbnails/usgs_thumb.jpg"},{"id":3359,"rank":100,"type":{"id":15,"text":"Index Page"},"url":"https://pubs.usgs.gov/of/2002/ofr-02-0139/","linkFileType":{"id":5,"text":"html"}}],"country":"United States ","state":"Alaska","noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"4f4e4a80e4b07f02db649365","contributors":{"authors":[{"text":"Alstatt, A.A.","contributorId":36984,"corporation":false,"usgs":true,"family":"Alstatt","given":"A.A.","email":"","affiliations":[],"preferred":false,"id":208453,"contributorType":{"id":1,"text":"Authors"},"rank":1},{"text":"Saltus, R. W.","contributorId":85588,"corporation":false,"usgs":true,"family":"Saltus","given":"R.","middleInitial":"W.","affiliations":[],"preferred":false,"id":208456,"contributorType":{"id":1,"text":"Authors"},"rank":2},{"text":"Bruhn, R.L.","contributorId":46972,"corporation":false,"usgs":true,"family":"Bruhn","given":"R.L.","email":"","affiliations":[],"preferred":false,"id":208454,"contributorType":{"id":1,"text":"Authors"},"rank":3},{"text":"Haeussler, Peter J. 0000-0002-1503-6247 pheuslr@usgs.gov","orcid":"https://orcid.org/0000-0002-1503-6247","contributorId":503,"corporation":false,"usgs":true,"family":"Haeussler","given":"Peter","email":"pheuslr@usgs.gov","middleInitial":"J.","affiliations":[{"id":119,"text":"Alaska Science Center Geology Minerals","active":true,"usgs":true},{"id":114,"text":"Alaska Science Center","active":true,"usgs":true}],"preferred":true,"id":208455,"contributorType":{"id":1,"text":"Authors"},"rank":4}]}}
,{"id":32370,"text":"ofr02129 - 2002 - Leveling, EDM, and crack-monitoring networks in the Koa'e fault system, Kilauea Volcano, Hawai'i","interactions":[],"lastModifiedDate":"2012-02-02T00:09:22","indexId":"ofr02129","displayToPublicDate":"2002-05-01T00:00:00","publicationYear":"2002","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":"2002-129","title":"Leveling, EDM, and crack-monitoring networks in the Koa'e fault system, Kilauea Volcano, Hawai'i","language":"ENGLISH","doi":"10.3133/ofr02129","usgsCitation":"Avery, V., Fiske, R., and Swanson, D., 2002, Leveling, EDM, and crack-monitoring networks in the Koa'e fault system, Kilauea Volcano, Hawai'i: U.S. Geological Survey Open-File Report 2002-129, iv, 44 leaves : ill., maps ; 28 cm. , https://doi.org/10.3133/ofr02129.","productDescription":"iv, 44 leaves : ill., maps ; 28 cm. ","costCenters":[],"links":[{"id":163402,"rank":0,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/of/2002/0129/report-thumb.jpg"},{"id":60358,"rank":300,"type":{"id":11,"text":"Document"},"url":"https://pubs.usgs.gov/of/2002/0129/report.pdf","linkFileType":{"id":1,"text":"pdf"}}],"noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"4f4e4b16e4b07f02db6a5585","contributors":{"authors":[{"text":"Avery, V.F.","contributorId":51811,"corporation":false,"usgs":true,"family":"Avery","given":"V.F.","email":"","affiliations":[],"preferred":false,"id":208442,"contributorType":{"id":1,"text":"Authors"},"rank":1},{"text":"Fiske, R.S.","contributorId":47783,"corporation":false,"usgs":true,"family":"Fiske","given":"R.S.","email":"","affiliations":[],"preferred":false,"id":208441,"contributorType":{"id":1,"text":"Authors"},"rank":2},{"text":"Swanson, Donald","contributorId":47430,"corporation":false,"usgs":true,"family":"Swanson","given":"Donald","email":"","affiliations":[],"preferred":false,"id":208440,"contributorType":{"id":1,"text":"Authors"},"rank":3}]}}
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