{"pageNumber":"218","pageRowStart":"5425","pageSize":"25","recordCount":36989,"records":[{"id":58246,"text":"ofr20041378 - 2004 - Major-element, sulfur, and chlorine compositions of glasses from the submarine flank of Kilauea Volcano, Hawaii, Collected During 1998-2002 Japan Marine Science and Technology Center (JAMSTEC) Cruises","interactions":[],"lastModifiedDate":"2019-05-16T08:50:09","indexId":"ofr20041378","displayToPublicDate":"2004-11-01T00:00:00","publicationYear":"2004","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":"2004-1378","title":"Major-element, sulfur, and chlorine compositions of glasses from the submarine flank of Kilauea Volcano, Hawaii, Collected During 1998-2002 Japan Marine Science and Technology Center (JAMSTEC) Cruises","docAbstract":"<p>No abstract available.</p>","language":"English","publisher":"U.S. Geological Survey","doi":"10.3133/ofr20041378","usgsCitation":"Coombs, M.L., Sisson, T.W., and Lipman, P.W., 2004, Major-element, sulfur, and chlorine compositions of glasses from the submarine flank of Kilauea Volcano, Hawaii, Collected During 1998-2002 Japan Marine Science and Technology Center (JAMSTEC) Cruises (Version 1.0): U.S. Geological Survey Open-File Report 2004-1378, 7 p., https://doi.org/10.3133/ofr20041378.","productDescription":"7 p.","costCenters":[{"id":615,"text":"Volcano Hazards Program","active":true,"usgs":true}],"links":[{"id":5829,"rank":100,"type":{"id":15,"text":"Index Page"},"url":"https://pubs.usgs.gov/of/2004/1378/","linkFileType":{"id":5,"text":"html"}},{"id":185147,"rank":0,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/thumbnails/usgs_thumb.jpg"}],"country":"United States","state":"Hawaii","otherGeospatial":"Kilauea volcano","geographicExtents":"{\n  \"type\": \"FeatureCollection\",\n  \"features\": [\n    {\n      \"type\": \"Feature\",\n      \"properties\": {},\n      \"geometry\": {\n        \"type\": \"Polygon\",\n        \"coordinates\": [\n          [\n            [\n              -155.29131889343262,\n              19.378603724290507\n            ],\n            [\n              -155.2375030517578,\n              19.378603724290507\n            ],\n            [\n              -155.2375030517578,\n              19.416816177675052\n            ],\n            [\n              -155.29131889343262,\n              19.416816177675052\n            ],\n            [\n              -155.29131889343262,\n              19.378603724290507\n            ]\n          ]\n        ]\n      }\n    }\n  ]\n}","edition":"Version 1.0","noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"4f4e4a80e4b07f02db649cb9","contributors":{"authors":[{"text":"Coombs, Michelle L. 0000-0002-6002-6806 mcoombs@usgs.gov","orcid":"https://orcid.org/0000-0002-6002-6806","contributorId":2809,"corporation":false,"usgs":true,"family":"Coombs","given":"Michelle","email":"mcoombs@usgs.gov","middleInitial":"L.","affiliations":[{"id":617,"text":"Volcano Science Center","active":true,"usgs":true}],"preferred":true,"id":258545,"contributorType":{"id":1,"text":"Authors"},"rank":1},{"text":"Sisson, Thomas W. 0000-0003-3380-6425 tsisson@usgs.gov","orcid":"https://orcid.org/0000-0003-3380-6425","contributorId":2341,"corporation":false,"usgs":true,"family":"Sisson","given":"Thomas","email":"tsisson@usgs.gov","middleInitial":"W.","affiliations":[{"id":617,"text":"Volcano Science Center","active":true,"usgs":true}],"preferred":true,"id":258544,"contributorType":{"id":1,"text":"Authors"},"rank":2},{"text":"Lipman, Peter W. 0000-0001-9175-6118 plipman@usgs.gov","orcid":"https://orcid.org/0000-0001-9175-6118","contributorId":3486,"corporation":false,"usgs":true,"family":"Lipman","given":"Peter","email":"plipman@usgs.gov","middleInitial":"W.","affiliations":[{"id":617,"text":"Volcano Science Center","active":true,"usgs":true},{"id":5079,"text":"Pacific Regional Director's Office","active":true,"usgs":true}],"preferred":true,"id":258546,"contributorType":{"id":1,"text":"Authors"},"rank":3}]}}
,{"id":58245,"text":"ofr20041345 - 2004 - Modeling of the Climax Stock and Related Plutons Based on the Inversion of Magnetic Data, Southwest Nevada","interactions":[],"lastModifiedDate":"2012-02-02T00:12:21","indexId":"ofr20041345","displayToPublicDate":"2004-11-01T00:00:00","publicationYear":"2004","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":"2004-1345","title":"Modeling of the Climax Stock and Related Plutons Based on the Inversion of Magnetic Data, Southwest Nevada","docAbstract":"Two models of the Climax and Gold Meadows stocks were generated using a new method of magnetic inversion modeling based on the pseudogravity anomaly. The first model examined the shape of the two stocks and their connection at depth, concluding that the stocks are connected -4000 m below the ground surface. The second model re-examined the shape and depth of the Climax stock using a two-layer model and new magnetic data collected from drill hole ER-8-1. Existing and new magnetic data support a model of a zoned pluton with increasing magnetization with depth. A model of a zoned pluton was generated and adjusted to fit the magnetic anomaly measured over the stock. The model has an upper layer that extends to a depth of 1,700 m and is magnetized at 0.06 A/m, and a lower layer that extends to a maximum depth of 7,600 m and is magnetized at 0.17 A/m. The model matches the outcrop data, but was unable to match the intercept of the Climax stock from drill hole ER-8-1.","language":"ENGLISH","doi":"10.3133/ofr20041345","collaboration":"Prepared in cooperation with the U. S. Department of Energy\r\nNational Nuclear Security Administration, Office of Environmental Management, Nevada Site Office, under Interagency Agreement DE-AI52-01NV13944","usgsCitation":"Phelps, G., Jachens, R.C., Moring, B.C., and Roberts, C.W., 2004, Modeling of the Climax Stock and Related Plutons Based on the Inversion of Magnetic Data, Southwest Nevada (Version 1.0): U.S. Geological Survey Open-File Report 2004-1345, 21 p.; 8 data files, https://doi.org/10.3133/ofr20041345.","productDescription":"21 p.; 8 data files","additionalOnlineFiles":"Y","costCenters":[],"links":[{"id":185036,"rank":0,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/thumbnails/usgs_thumb.jpg"},{"id":5828,"rank":100,"type":{"id":15,"text":"Index Page"},"url":"https://pubs.usgs.gov/of/2004/1345/","linkFileType":{"id":5,"text":"html"}}],"edition":"Version 1.0","noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"4f4e4b05e4b07f02db699879","contributors":{"authors":[{"text":"Phelps, Geoffrey A.","contributorId":17262,"corporation":false,"usgs":true,"family":"Phelps","given":"Geoffrey A.","affiliations":[],"preferred":false,"id":258542,"contributorType":{"id":1,"text":"Authors"},"rank":1},{"text":"Jachens, Robert C. jachens@usgs.gov","contributorId":1180,"corporation":false,"usgs":true,"family":"Jachens","given":"Robert","email":"jachens@usgs.gov","middleInitial":"C.","affiliations":[{"id":312,"text":"Geology, Minerals, Energy, and Geophysics Science Center","active":true,"usgs":true}],"preferred":true,"id":258540,"contributorType":{"id":1,"text":"Authors"},"rank":2},{"text":"Moring, Barry C. 0000-0001-6797-9258 moring@usgs.gov","orcid":"https://orcid.org/0000-0001-6797-9258","contributorId":2794,"corporation":false,"usgs":true,"family":"Moring","given":"Barry","email":"moring@usgs.gov","middleInitial":"C.","affiliations":[{"id":312,"text":"Geology, Minerals, Energy, and Geophysics Science Center","active":true,"usgs":true}],"preferred":true,"id":258541,"contributorType":{"id":1,"text":"Authors"},"rank":3},{"text":"Roberts, Carter W.","contributorId":45282,"corporation":false,"usgs":true,"family":"Roberts","given":"Carter","email":"","middleInitial":"W.","affiliations":[],"preferred":false,"id":258543,"contributorType":{"id":1,"text":"Authors"},"rank":4}]}}
,{"id":58107,"text":"ofr20041361 - 2004 - Preliminary geologic map of the El Cajon 30' x 60' quadrangle, Southern California","interactions":[],"lastModifiedDate":"2012-02-02T00:12:03","indexId":"ofr20041361","displayToPublicDate":"2004-11-01T00:00:00","publicationYear":"2004","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":"2004-1361","title":"Preliminary geologic map of the El Cajon 30' x 60' quadrangle, Southern California","docAbstract":"This data set maps and describes the geology of the El Cajon 30' x 60' quadrangle, southern California.  Compilation of the El Cajon quadrangle is based upon published mapping at various scales, unpublished mapping at 1:24,000 scale, and reconnaissance mapping.  Mapping was done by fieldwork and the use of aerial photographs at 1:24,000 scale.\r\n\r\n      The El Cajon quadrangle includes parts of two physiographic provinces: the Peninsular Ranges Province on the west underlies the major part of the quadrangle; the western Colorado Desert (locally called the Anza-Borrego Desert) underlies the northeastern corner.  The approximate boundary between these two provinces is the Neogene Elsinore Fault Zone, the westernmost on-land strand of the San Andreas Fault System.  Movements within the Elsinore Fault Zone are believed to have resulted in the uplift and westward rotation of the Peninsular Ranges block relative to the western Colorado Desert (Gastil and others, 1975).  As a result, elevations in the El Cajon quadrangle increase from less than 100 m in the westernmost part of the quadrangle to ~2000 m along the irregular mountainous spine of the Peninsular Ranges (the Cuyamaca, Laguna, Tierra Blanca, and Jacumba Mountains); elevations then decrease rapidly eastward to <100 m in the Anza-Borrego Desert.\r\n      Southwest of the Elsinore Fault Zone, the El Cajon quadrangle is underlain by Jurassic and Cretaceous plutonic rocks of the composite Peninsular Ranges Batholith, which contains screens of variably metamorphosed Mesozoic supracrustal rocks.  Late Jurassic and Early Cretaceous volcanic and volcaniclastic rocks that are exposed in the western part of the quadrangle represent an older, superjacent part of the Peninsular Ranges magmatic arc.  Upper Cretaceous and Eocene marine and nonmarine strata were deposited widely upon the eroded batholith but are preserved only in the westernmost part of the quadrangle (the San Diego embayment).  Pliocene and Pleistocene coastal terrace deposits rest unconformably upon the early Tertiary rocks in the southwestern corner of the quadrangle.\r\n      Northeast of the Elsinore Fault Zone, the El Cajon quadrangle exposes extensive Neogene nonmarine and marine sedimentary and volcanic rocks of the Fish Creek-Vallecito basin.  Basement uplifts in this region are composed of crystalline rocks of the eastern Peninsular Ranges Batholith (the Vallecito, Fish Creek, and Coyote Mountains).","language":"ENGLISH","doi":"10.3133/ofr20041361","usgsCitation":"Todd, V.R., 2004, Preliminary geologic map of the El Cajon 30' x 60' quadrangle, Southern California: U.S. Geological Survey Open-File Report 2004-1361, 1 sheet, https://doi.org/10.3133/ofr20041361.","productDescription":"1 sheet","costCenters":[],"links":[{"id":110527,"rank":700,"type":{"id":15,"text":"Index Page"},"url":"https://ngmdb.usgs.gov/Prodesc/proddesc_69595.htm","linkFileType":{"id":5,"text":"html"},"description":"69595"},{"id":181248,"rank":0,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/thumbnails/usgs_thumb.jpg"},{"id":5718,"rank":100,"type":{"id":15,"text":"Index Page"},"url":"https://pubs.usgs.gov/of/2004/1361/","linkFileType":{"id":5,"text":"html"}}],"noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"4f4e4aa9e4b07f02db667fba","contributors":{"authors":[{"text":"Todd, Victoria R. (compiler)","contributorId":51846,"corporation":false,"usgs":true,"family":"Todd","given":"Victoria","suffix":"(compiler)","email":"","middleInitial":"R.","affiliations":[],"preferred":false,"id":258335,"contributorType":{"id":1,"text":"Authors"},"rank":1}]}}
,{"id":58244,"text":"ofr20041311 - 2004 - Alaska resource data file: Iditarod quadrangle","interactions":[],"lastModifiedDate":"2025-07-29T11:52:09.044718","indexId":"ofr20041311","displayToPublicDate":"2004-11-01T00:00:00","publicationYear":"2004","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":"2004-1311","title":"Alaska resource data file: Iditarod quadrangle","docAbstract":"<p>No abstract available.</p>","language":"English","publisher":"U.S. Geological Survey","doi":"10.3133/ofr20041311","usgsCitation":"Bundtzen, T., Miller, M.L., and Hawley, C.C., 2004, Alaska resource data file: Iditarod quadrangle (Version 1.0): U.S. Geological Survey Open-File Report 2004-1311, 374 p., https://doi.org/10.3133/ofr20041311.","productDescription":"374 p.","costCenters":[{"id":119,"text":"Alaska Science Center Geology Minerals","active":true,"usgs":true}],"links":[{"id":483995,"rank":4,"type":{"id":18,"text":"Project Site"},"url":"https://doi.org/10.5066/P96MMRFD","linkFileType":{"id":5,"text":"html"}},{"id":483994,"rank":3,"type":{"id":36,"text":"NGMDB Index Page"},"url":"https://ngmdb.usgs.gov/Prodesc/proddesc_69998.htm"},{"id":5827,"rank":2,"type":{"id":15,"text":"Index Page"},"url":"https://pubs.usgs.gov/of/2004/1311/","linkFileType":{"id":5,"text":"html"}},{"id":185035,"rank":1,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/thumbnails/usgs_thumb.jpg"},{"id":486491,"rank":5,"type":{"id":11,"text":"Document"},"url":"https://pubs.usgs.gov/of/2004/1311/of2004-1311.pdf","text":"Report","size":"996 KB","linkFileType":{"id":1,"text":"pdf"}}],"country":"United States","state":"Alaska","otherGeospatial":"Iditarod quadrangle","geographicExtents":"{\n  \"type\": \"FeatureCollection\",\n  \"features\": [\n    {\n      \"type\": \"Feature\",\n      \"properties\": {},\n      \"geometry\": {\n        \"coordinates\": [\n          [\n            [\n              -156,\n              63\n            ],\n            [\n              -159,\n              63\n            ],\n            [\n              -159,\n              62\n            ],\n            [\n              -156,\n              62\n            ],\n            [\n              -156,\n              63\n            ]\n          ]\n        ],\n        \"type\": \"Polygon\"\n      }\n    }\n  ]\n}","edition":"Version 1.0","noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"4f4e4ae2e4b07f02db688e22","contributors":{"authors":[{"text":"Bundtzen, Thomas K.","contributorId":83560,"corporation":false,"usgs":true,"family":"Bundtzen","given":"Thomas K.","affiliations":[],"preferred":false,"id":258538,"contributorType":{"id":1,"text":"Authors"},"rank":1},{"text":"Miller, Marti L. 0000-0003-0285-4942 mlmiller@usgs.gov","orcid":"https://orcid.org/0000-0003-0285-4942","contributorId":561,"corporation":false,"usgs":true,"family":"Miller","given":"Marti","email":"mlmiller@usgs.gov","middleInitial":"L.","affiliations":[{"id":119,"text":"Alaska Science Center Geology Minerals","active":true,"usgs":true}],"preferred":true,"id":258537,"contributorType":{"id":1,"text":"Authors"},"rank":2},{"text":"Hawley, Charles C.","contributorId":97570,"corporation":false,"usgs":true,"family":"Hawley","given":"Charles","email":"","middleInitial":"C.","affiliations":[],"preferred":false,"id":258539,"contributorType":{"id":1,"text":"Authors"},"rank":3}]}}
,{"id":58243,"text":"ofr20041310 - 2004 - Alaska resource data file: Sleetmute quadrangle, Alaska","interactions":[],"lastModifiedDate":"2025-05-23T19:19:11.861954","indexId":"ofr20041310","displayToPublicDate":"2004-11-01T00:00:00","publicationYear":"2004","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":"2004-1310","title":"Alaska resource data file: Sleetmute quadrangle, Alaska","docAbstract":"<p>No abstract available.</p>","language":"English","publisher":"U.S. Geological Survey","doi":"10.3133/ofr20041310","usgsCitation":"Bundtzen, T., and Miller, M.L., 2004, Alaska resource data file: Sleetmute quadrangle, Alaska (Version 1.0): U.S. Geological Survey Open-File Report 2004-1310, 160 p., https://doi.org/10.3133/ofr20041310.","productDescription":"160 p.","costCenters":[],"links":[{"id":5826,"rank":2,"type":{"id":15,"text":"Index Page"},"url":"https://pubs.usgs.gov/of/2004/1310/","linkFileType":{"id":5,"text":"html"}},{"id":486540,"rank":5,"type":{"id":11,"text":"Document"},"url":"https://pubs.usgs.gov/of/2004/1310/of2004-1310.pdf","text":"Report","size":"713 KB","linkFileType":{"id":1,"text":"pdf"},"description":"OFR 2004-1310 PDF"},{"id":484144,"rank":3,"type":{"id":18,"text":"Project Site"},"url":"https://doi.org/10.5066/P96MMRFD","linkFileType":{"id":5,"text":"html"}},{"id":185034,"rank":1,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/thumbnails/usgs_thumb.jpg"},{"id":484145,"rank":4,"type":{"id":36,"text":"NGMDB Index Page"},"url":"https://ngmdb.usgs.gov/Prodesc/proddesc_69997.htm","linkFileType":{"id":5,"text":"html"}}],"country":"United States","state":"Alaska","otherGeospatial":"Sleetmute quadrangle","geographicExtents":"{\n  \"type\": \"FeatureCollection\",\n  \"features\": [\n    {\n      \"type\": \"Feature\",\n      \"properties\": {},\n      \"geometry\": {\n        \"coordinates\": [\n          [\n            [\n              -159,\n              62\n            ],\n            [\n              -159,\n              61\n            ],\n            [\n              -156,\n              61\n            ],\n            [\n              -156,\n              62\n            ],\n            [\n              -159,\n              62\n            ]\n          ]\n        ],\n        \"type\": \"Polygon\"\n      }\n    }\n  ]\n}","edition":"Version 1.0","noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"4f4e4ae0e4b07f02db6882f6","contributors":{"authors":[{"text":"Bundtzen, Thomas K.","contributorId":83560,"corporation":false,"usgs":true,"family":"Bundtzen","given":"Thomas K.","affiliations":[],"preferred":false,"id":258536,"contributorType":{"id":1,"text":"Authors"},"rank":1},{"text":"Miller, Marti L. 0000-0003-0285-4942 mlmiller@usgs.gov","orcid":"https://orcid.org/0000-0003-0285-4942","contributorId":561,"corporation":false,"usgs":true,"family":"Miller","given":"Marti","email":"mlmiller@usgs.gov","middleInitial":"L.","affiliations":[{"id":119,"text":"Alaska Science Center Geology Minerals","active":true,"usgs":true}],"preferred":true,"id":258535,"contributorType":{"id":1,"text":"Authors"},"rank":2}]}}
,{"id":58102,"text":"ofr20041298 - 2004 - Springs on and in the vicinity of Mount Hood volcano, Oregon","interactions":[],"lastModifiedDate":"2012-02-02T00:11:59","indexId":"ofr20041298","displayToPublicDate":"2004-11-01T00:00:00","publicationYear":"2004","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":"2004-1298","title":"Springs on and in the vicinity of Mount Hood volcano, Oregon","docAbstract":"Chemical and isotopic data are presented for nonthermal, thermal, and slightly thermal springs and drill holes and fumaroles on Mount Hood, Oregon. Temperatures of nonthermal springs on Mount Hood decrease with elevation and are similar to air temperatures from nearby weather stations. Dissolved constituents in nonthermal springs generally increase with spring temperatures and reflect weathering of volcanic rock from the action of dissolved carbon dioxide. Isotopic contents of nonthermal springs follow a local meteoric water line and generally become lighter with elevation. Some nonthermal springs at low-elevation have light values of isotopes indicating a high-elevation source for the water. Three hydrothermal systems have been identified on Mount Hood. Swim Warm Springs is interpreted to have a source water that boiled from 187?C, re-equilibrated at 96?C, and then mixed with nonthermal water to produce the range of compositions found in various springs. The Meadows Spring is interpreted to have a source water that boiled from 223?C, re-equilibrated at 94?C, and then mixed with nonthermal water to produce the range of compositions found in the spring over several years. Both systems contain water that originated as precipitation at higher elevation. The summit fumaroles have gas geothermometer temperatures generally over 300?C, indicating that they are not the steam discharge from the Swim and Meadows hydrothermal systems. Representative values of thermal discharge for the three hydrothermal systems are 10 MWt for the fumaroles, 2.2 MWt for Swim, and 1.9 MWt for the Meadows and Cascade springs.","language":"ENGLISH","doi":"10.3133/ofr20041298","usgsCitation":"Nathenson, M., 2004, Springs on and in the vicinity of Mount Hood volcano, Oregon (Version 1.0): U.S. Geological Survey Open-File Report 2004-1298, 43 p., https://doi.org/10.3133/ofr20041298.","productDescription":"43 p.","costCenters":[],"links":[{"id":5715,"rank":100,"type":{"id":15,"text":"Index Page"},"url":"https://pubs.usgs.gov/of/2004/1298/","linkFileType":{"id":5,"text":"html"}},{"id":181220,"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":"4f4e4a5ee4b07f02db633dc5","contributors":{"authors":[{"text":"Nathenson, Manuel 0000-0002-5216-984X mnathnsn@usgs.gov","orcid":"https://orcid.org/0000-0002-5216-984X","contributorId":1358,"corporation":false,"usgs":true,"family":"Nathenson","given":"Manuel","email":"mnathnsn@usgs.gov","affiliations":[{"id":617,"text":"Volcano Science Center","active":true,"usgs":true}],"preferred":true,"id":258324,"contributorType":{"id":1,"text":"Authors"},"rank":1}]}}
,{"id":58158,"text":"ofr20041333 - 2004 - Nutrient concentrations in Upper and Lower Echo, Fallen Leaf, Spooner, and Marlette Lakes and associated outlet streams, California and Nevada, 2002-03","interactions":[],"lastModifiedDate":"2012-02-02T00:12:17","indexId":"ofr20041333","displayToPublicDate":"2004-11-01T00:00:00","publicationYear":"2004","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":"2004-1333","title":"Nutrient concentrations in Upper and Lower Echo, Fallen Leaf, Spooner, and Marlette Lakes and associated outlet streams, California and Nevada, 2002-03","docAbstract":"Five lakes and their outlet streams in the Lake Tahoe Basin were sampled for nutrients during 2002-03. The lakes and streams sampled included Upper Echo, Lower Echo, Fallen Leaf, Spooner, and Marlette Lakes and Echo, Taylor, and Marlette Creeks. Water samples were collected to determine seasonal and spatial concentrations of dissolved nitrite plus nitrate, dissolved ammonia, total Kjeldahl nitrogen, dissolved orthophosphate, total phosphorus, and total bioreactive iron. These data will be used by Tahoe Regional Planning Agency in revising threshold values for waters within the Lake Tahoe Basin. Standard U.S. Geological Survey methods of sample collection and analysis were used and are detailed herein. Data collected during this study and summary statistics are presented in graphical and tabular form.","language":"ENGLISH","doi":"10.3133/ofr20041333","usgsCitation":"Lico, M.S., 2004, Nutrient concentrations in Upper and Lower Echo, Fallen Leaf, Spooner, and Marlette Lakes and associated outlet streams, California and Nevada, 2002-03 (Online only): U.S. Geological Survey Open-File Report 2004-1333, 57 p., https://doi.org/10.3133/ofr20041333.","productDescription":"57 p.","onlineOnly":"Y","costCenters":[],"links":[{"id":5772,"rank":100,"type":{"id":15,"text":"Index Page"},"url":"https://pubs.water.usgs.gov/ofr2004-1333/","linkFileType":{"id":5,"text":"html"}},{"id":183927,"rank":0,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/thumbnails/usgs_thumb.jpg"}],"edition":"Online only","noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"4f4e4afce4b07f02db696791","contributors":{"authors":[{"text":"Lico, Michael S.","contributorId":75897,"corporation":false,"usgs":true,"family":"Lico","given":"Michael","email":"","middleInitial":"S.","affiliations":[],"preferred":false,"id":258420,"contributorType":{"id":1,"text":"Authors"},"rank":1}]}}
,{"id":58109,"text":"ofr20041375 - 2004 - Ambient vibration and earthquake strong-motion data sets for selected USGS extensively instrumented buildings","interactions":[],"lastModifiedDate":"2012-02-02T00:12:03","indexId":"ofr20041375","displayToPublicDate":"2004-11-01T00:00:00","publicationYear":"2004","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":"2004-1375","title":"Ambient vibration and earthquake strong-motion data sets for selected USGS extensively instrumented buildings","language":"ENGLISH","doi":"10.3133/ofr20041375","usgsCitation":"Dunand, F., Rodgers, J.E., Acosta, A.V., Salsman, M., Bard, P., and Çelebi, M., 2004, Ambient vibration and earthquake strong-motion data sets for selected USGS extensively instrumented buildings (Version 1.0): U.S. Geological Survey Open-File Report 2004-1375, 31 p., https://doi.org/10.3133/ofr20041375.","productDescription":"31 p.","costCenters":[],"links":[{"id":181250,"rank":0,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/thumbnails/usgs_thumb.jpg"},{"id":5719,"rank":100,"type":{"id":15,"text":"Index Page"},"url":"https://pubs.usgs.gov/of/2004/1375/","linkFileType":{"id":5,"text":"html"}}],"edition":"Version 1.0","noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"4f4e4adce4b07f02db686928","contributors":{"authors":[{"text":"Dunand, Francois","contributorId":57150,"corporation":false,"usgs":true,"family":"Dunand","given":"Francois","email":"","affiliations":[],"preferred":false,"id":258340,"contributorType":{"id":1,"text":"Authors"},"rank":1},{"text":"Rodgers, Janise E.","contributorId":14892,"corporation":false,"usgs":true,"family":"Rodgers","given":"Janise","email":"","middleInitial":"E.","affiliations":[],"preferred":false,"id":258338,"contributorType":{"id":1,"text":"Authors"},"rank":2},{"text":"Acosta, Arnold V.","contributorId":15273,"corporation":false,"usgs":true,"family":"Acosta","given":"Arnold","email":"","middleInitial":"V.","affiliations":[],"preferred":false,"id":258339,"contributorType":{"id":1,"text":"Authors"},"rank":3},{"text":"Salsman, Marion","contributorId":102571,"corporation":false,"usgs":true,"family":"Salsman","given":"Marion","email":"","affiliations":[],"preferred":false,"id":258342,"contributorType":{"id":1,"text":"Authors"},"rank":4},{"text":"Bard, Pierre-Yves","contributorId":86846,"corporation":false,"usgs":true,"family":"Bard","given":"Pierre-Yves","email":"","affiliations":[],"preferred":false,"id":258341,"contributorType":{"id":1,"text":"Authors"},"rank":5},{"text":"Çelebi, Mehmet 0000-0002-4769-7357 celebi@usgs.gov","orcid":"https://orcid.org/0000-0002-4769-7357","contributorId":3205,"corporation":false,"usgs":true,"family":"Çelebi","given":"Mehmet","email":"celebi@usgs.gov","affiliations":[{"id":237,"text":"Earthquake Science Center","active":true,"usgs":true}],"preferred":false,"id":258337,"contributorType":{"id":1,"text":"Authors"},"rank":6}]}}
,{"id":58035,"text":"ofr20041360 - 2004 - Vitrinite reflectance measurements of cretaceous outcrop samples from the Wyoming Thrustbelt, Southwestern Wyoming","interactions":[],"lastModifiedDate":"2012-02-02T00:12:29","indexId":"ofr20041360","displayToPublicDate":"2004-11-01T00:00:00","publicationYear":"2004","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":"2004-1360","title":"Vitrinite reflectance measurements of cretaceous outcrop samples from the Wyoming Thrustbelt, Southwestern Wyoming","language":"ENGLISH","doi":"10.3133/ofr20041360","usgsCitation":"Pawlewicz, M., and Kirschbaum, M., 2004, Vitrinite reflectance measurements of cretaceous outcrop samples from the Wyoming Thrustbelt, Southwestern Wyoming (Version 1.0): U.S. Geological Survey Open-File Report 2004-1360, 5 p., https://doi.org/10.3133/ofr20041360.","productDescription":"5 p.","costCenters":[],"links":[{"id":183330,"rank":0,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/thumbnails/usgs_thumb.jpg"},{"id":5965,"rank":100,"type":{"id":15,"text":"Index Page"},"url":"https://pubs.usgs.gov/of/2004/1360/","linkFileType":{"id":5,"text":"html"}}],"edition":"Version 1.0","noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"4f4e4a0ee4b07f02db5fda8c","contributors":{"authors":[{"text":"Pawlewicz, Mark","contributorId":69212,"corporation":false,"usgs":true,"family":"Pawlewicz","given":"Mark","email":"","affiliations":[],"preferred":false,"id":258190,"contributorType":{"id":1,"text":"Authors"},"rank":1},{"text":"Kirschbaum, Mark","contributorId":18039,"corporation":false,"usgs":true,"family":"Kirschbaum","given":"Mark","affiliations":[],"preferred":false,"id":258189,"contributorType":{"id":1,"text":"Authors"},"rank":2}]}}
,{"id":58105,"text":"ofr20041309 - 2004 - Application of GPS drifters to track Hawaiian coral spawning","interactions":[],"lastModifiedDate":"2012-02-02T00:12:03","indexId":"ofr20041309","displayToPublicDate":"2004-11-01T00:00:00","publicationYear":"2004","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":"2004-1309","title":"Application of GPS drifters to track Hawaiian coral spawning","language":"ENGLISH","doi":"10.3133/ofr20041309","usgsCitation":"Hatcher, G., Reiss, T.E., and Storlazzi, C., 2004, Application of GPS drifters to track Hawaiian coral spawning (Version 1.0): U.S. Geological Survey Open-File Report 2004-1309, 14 p., https://doi.org/10.3133/ofr20041309.","productDescription":"14 p.","costCenters":[],"links":[{"id":5717,"rank":100,"type":{"id":15,"text":"Index Page"},"url":"https://pubs.usgs.gov/of/2004/1309/","linkFileType":{"id":5,"text":"html"}},{"id":181246,"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":"4f4e4ac7e4b07f02db67ac31","contributors":{"authors":[{"text":"Hatcher, Gerald A. 0000-0001-7705-1509","orcid":"https://orcid.org/0000-0001-7705-1509","contributorId":67586,"corporation":false,"usgs":true,"family":"Hatcher","given":"Gerald A.","affiliations":[{"id":520,"text":"Pacific Coastal and Marine Science Center","active":true,"usgs":true}],"preferred":false,"id":258332,"contributorType":{"id":1,"text":"Authors"},"rank":1},{"text":"Reiss, Thomas E. 0000-0003-0388-7076 treiss@usgs.gov","orcid":"https://orcid.org/0000-0003-0388-7076","contributorId":4149,"corporation":false,"usgs":true,"family":"Reiss","given":"Thomas","email":"treiss@usgs.gov","middleInitial":"E.","affiliations":[{"id":520,"text":"Pacific Coastal and Marine Science Center","active":true,"usgs":true}],"preferred":true,"id":258331,"contributorType":{"id":1,"text":"Authors"},"rank":2},{"text":"Storlazzi, Curt D. 0000-0001-8057-4490","orcid":"https://orcid.org/0000-0001-8057-4490","contributorId":77889,"corporation":false,"usgs":true,"family":"Storlazzi","given":"Curt D.","affiliations":[],"preferred":false,"id":258333,"contributorType":{"id":1,"text":"Authors"},"rank":3}]}}
,{"id":56323,"text":"ofr20041225 - 2004 - Development and Calibration of Two-Dimensional Hydrodynamic Model of the Tanana River near Tok, Alaska","interactions":[],"lastModifiedDate":"2018-04-21T13:44:15","indexId":"ofr20041225","displayToPublicDate":"2004-11-01T00:00:00","publicationYear":"2004","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":"2004-1225","title":"Development and Calibration of Two-Dimensional Hydrodynamic Model of the Tanana River near Tok, Alaska","docAbstract":"Bathymetric and hydraulic data were collected by the U.S. Geological Survey on the Tanana River in proximity to Alaska Department of Transportation and Public Facilities' bridge number 505 at mile 80.5 of the Alaska Highway. Data were collected from August 7-9, 2002, over an approximate 5,000- foot reach of the river. These data were combined with topographic data provided by Alaska Department of Transportation and Public Facilities to generate a two-dimensional hydrodynamic model.\r\n\r\nThe hydrodynamic model was calibrated with water-surface elevations, flow velocities, and flow directions collected at a discharge of 25,600 cubic feet per second. The calibrated model was then used for a simulation of the 100-year recurrence interval discharge of 51,900 cubic feet per second. The existing bridge piers were removed from the model geometry in a second simulation to model the hydraulic conditions in the channel without the piers' influence. The water-surface elevations, flow velocities, and flow directions from these simulations can be used to evaluate the influence of the piers on flow hydraulics and will assist the Alaska Department of Transportation and Public Facilities in the design of a replacement bridge.","language":"ENGLISH","doi":"10.3133/ofr20041225","usgsCitation":"Conaway, J.S., and Moran, E.H., 2004, Development and Calibration of Two-Dimensional Hydrodynamic Model of the Tanana River near Tok, Alaska: U.S. Geological Survey Open-File Report 2004-1225, 22 p., https://doi.org/10.3133/ofr20041225.","productDescription":"22 p.","costCenters":[],"links":[{"id":5699,"rank":100,"type":{"id":15,"text":"Index Page"},"url":"https://pubs.water.usgs.gov/ofr2004-1225/","linkFileType":{"id":5,"text":"html"}},{"id":184839,"rank":0,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/thumbnails/usgs_thumb.jpg"}],"noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"4f4e4aa8e4b07f02db66733f","contributors":{"authors":[{"text":"Conaway, Jeffrey S. 0000-0002-3036-592X jconaway@usgs.gov","orcid":"https://orcid.org/0000-0002-3036-592X","contributorId":2026,"corporation":false,"usgs":true,"family":"Conaway","given":"Jeffrey","email":"jconaway@usgs.gov","middleInitial":"S.","affiliations":[{"id":114,"text":"Alaska Science Center","active":true,"usgs":true},{"id":120,"text":"Alaska Science Center Water","active":true,"usgs":true}],"preferred":true,"id":255231,"contributorType":{"id":1,"text":"Authors"},"rank":1},{"text":"Moran, Edward H. emoran@usgs.gov","contributorId":5445,"corporation":false,"usgs":true,"family":"Moran","given":"Edward","email":"emoran@usgs.gov","middleInitial":"H.","affiliations":[{"id":192,"text":"Columbia Environmental Research Center","active":true,"usgs":true}],"preferred":true,"id":255230,"contributorType":{"id":1,"text":"Authors"},"rank":2}]}}
,{"id":57948,"text":"ofr20041342 - 2004 - Lead isotopic compositions of common arsenical pesticides used in New England","interactions":[],"lastModifiedDate":"2012-02-02T00:12:00","indexId":"ofr20041342","displayToPublicDate":"2004-10-01T00:00:00","publicationYear":"2004","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":"2004-1342","title":"Lead isotopic compositions of common arsenical pesticides used in New England","docAbstract":"The three most important arsenical pesticides and herbicides that were extensively used on apple, blueberry, and potato crops in New England from mid-1800s to recent times are lead arsenate, calcium arsenate, and sodium arsenate. Lead arsenate was probably the most heavily used of the arsenical pesticides until it was banned in 1988. Other metal-arsenic pesticides were also used but in lesser amounts. A recent report identified areas in New England where arsenical pesticides were used extensively (Robinson and Ayuso, 2004). On the basis of factor analysis of metal concentrations in stream sediment samples, a positive correlation with pesticide use was shown in regions having stream sediment sample populations that contained concentrations of high arsenic and lead. Lead isotope compositions of stream sediments from areas with heavy use of the pesticides could not be entirely explained by lead originating from rock sulfides and their weathering products. An industrial lead contribution (mostly from atmospheric deposition of lead) was suggested in general to explain the lead isotopic distributions of the stream sediments that could not be accounted for by the natural lead in the environment. We concluded that when agricultural land previously contaminated with arsenical pesticides is urbanized, pesticide residues in the soils and stream sediments could be released into the groundwater. No lead isotopic data characterizing the compositions of pesticides were available for comparison. \r\n\r\nWe have determined the lead isotopic compositions of commonly used pesticides in New England, such as lead arsenate, sodium metaarsenite, and calcium arsenate, in order to assist in future isotopic comparisons and to better establish anthropogenic sources of Pb and As. New data are also presented for copper acetoarsenite (or Paris green), methyl arsonic acid and methane arsonic acid, as well as for arsanilic acid, all of which are used as feed additives to promote swine and poultry growth. The new data characterize these anthropogenic sources. The data show that the arsenical pesticides have similar compositions: 208Pb/207Pb = 2.3839-2.4721, 206Pb/207Pb = 1.1035-1.2010, and 206Pb/204Pb = 17.070-18.759 and, more importantly, that the pesticides overlap the composition of the stream sediments that represent the areas with the most extensive agricultural use. Copper acetoarsenite (Paris green), arsenic oxide, methyl arsonic acid, methane arsonic acid, and arsanilic acid were also analyzed and have lead isotope compositions that range widely. An important source of arsenic and metals to most of the stream sediment samples in New England appears to be weathering products from rocks and industrial lead, but the extensive use of arsenical pesticides and herbicides up to about the 1960s can also be a significant anthropogenic source in agricultural regions.","language":"ENGLISH","doi":"10.3133/ofr20041342","usgsCitation":"Ayuso, R., Foley, N., Robinson, G., Wandless, G., and Dillingham, J., 2004, Lead isotopic compositions of common arsenical pesticides used in New England (Version 1.0; Online only): U.S. Geological Survey Open-File Report 2004-1342, 14 p., https://doi.org/10.3133/ofr20041342.","productDescription":"14 p.","onlineOnly":"Y","costCenters":[],"links":[{"id":5907,"rank":100,"type":{"id":15,"text":"Index Page"},"url":"https://pubs.usgs.gov/of/2004/1342/","linkFileType":{"id":5,"text":"html"}},{"id":181952,"rank":0,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/thumbnails/usgs_thumb.jpg"}],"edition":"Version 1.0; Online only","noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"4f4e4ae1e4b07f02db688a95","contributors":{"authors":[{"text":"Ayuso, Robert","contributorId":96350,"corporation":false,"usgs":true,"family":"Ayuso","given":"Robert","email":"","affiliations":[],"preferred":false,"id":257974,"contributorType":{"id":1,"text":"Authors"},"rank":1},{"text":"Foley, Nora","contributorId":9342,"corporation":false,"usgs":true,"family":"Foley","given":"Nora","affiliations":[],"preferred":false,"id":257970,"contributorType":{"id":1,"text":"Authors"},"rank":2},{"text":"Robinson, Gilpin Jr. grobinso@usgs.gov","contributorId":23625,"corporation":false,"usgs":true,"family":"Robinson","given":"Gilpin","suffix":"Jr.","email":"grobinso@usgs.gov","affiliations":[],"preferred":false,"id":257971,"contributorType":{"id":1,"text":"Authors"},"rank":3},{"text":"Wandless, Gregory","contributorId":77233,"corporation":false,"usgs":true,"family":"Wandless","given":"Gregory","affiliations":[],"preferred":false,"id":257973,"contributorType":{"id":1,"text":"Authors"},"rank":4},{"text":"Dillingham, Jeremy","contributorId":49451,"corporation":false,"usgs":true,"family":"Dillingham","given":"Jeremy","email":"","affiliations":[],"preferred":false,"id":257972,"contributorType":{"id":1,"text":"Authors"},"rank":5}]}}
,{"id":57811,"text":"ofr20041283 - 2004 - Proceedings of the twentieth annual meeting of the Society for Organic Petrology","interactions":[],"lastModifiedDate":"2022-06-15T19:52:33.975934","indexId":"ofr20041283","displayToPublicDate":"2004-10-01T00:00:00","publicationYear":"2004","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":"2004-1283","title":"Proceedings of the twentieth annual meeting of the Society for Organic Petrology","docAbstract":"<p>The Society for Organic Petrology (TSOP; pronounced \"Tee'-sop\") was established in 1984 to consolidate and foster the organizational activities of scientists and engineers involved with coal petrology, kerogen petrology, organic geochemistry, and related disciplines. The following report, \"Proceedings of the Twentieth Annual Meeting of The Society for Organic Petrology\" (ISSN 1060-7250), features technical talks, poster presentations, business meetings, short courses, and field trips from the Fall 2003 annual meeting held in Washington, D.C.</p>","language":"English","publisher":"U.S. Geological Survey","doi":"10.3133/ofr20041283","usgsCitation":"2004, Proceedings of the twentieth annual meeting of the Society for Organic Petrology (Version 1.0): U.S. Geological Survey Open-File Report 2004-1283, 126 p., https://doi.org/10.3133/ofr20041283.","productDescription":"126 p.","costCenters":[{"id":241,"text":"Eastern Energy Resources Science Center","active":true,"usgs":true},{"id":678,"text":"Woods Hole Coastal and Marine Science Center","active":true,"usgs":true}],"links":[{"id":184709,"rank":0,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/thumbnails/usgs_thumb.jpg"},{"id":402235,"rank":3,"type":{"id":36,"text":"NGMDB Index Page"},"url":"https://ngmdb.usgs.gov/Prodesc/proddesc_68866.htm","linkFileType":{"id":5,"text":"html"}},{"id":5789,"rank":100,"type":{"id":15,"text":"Index Page"},"url":"https://pubs.usgs.gov/of/2004/1283/","linkFileType":{"id":5,"text":"html"}}],"edition":"Version 1.0","noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"4f4e4a9ee4b07f02db660372","contributors":{"compilers":[{"text":"Karlsen, Alex W.","contributorId":78789,"corporation":false,"usgs":true,"family":"Karlsen","given":"Alex W.","affiliations":[],"preferred":false,"id":727899,"contributorType":{"id":3,"text":"Compilers"},"rank":1}],"editors":[{"text":"Bragg, Linda J.","contributorId":103717,"corporation":false,"usgs":true,"family":"Bragg","given":"Linda","email":"","middleInitial":"J.","affiliations":[],"preferred":false,"id":727894,"contributorType":{"id":2,"text":"Editors"},"rank":1},{"text":"Lentz, Erika E. elentz@usgs.gov","contributorId":167611,"corporation":false,"usgs":true,"family":"Lentz","given":"Erika","email":"elentz@usgs.gov","middleInitial":"E.","affiliations":[{"id":678,"text":"Woods Hole Coastal and Marine Science Center","active":true,"usgs":true}],"preferred":false,"id":727895,"contributorType":{"id":2,"text":"Editors"},"rank":2},{"text":"Warwick, Peter D. 0000-0002-3152-7783 pwarwick@usgs.gov","orcid":"https://orcid.org/0000-0002-3152-7783","contributorId":762,"corporation":false,"usgs":true,"family":"Warwick","given":"Peter","email":"pwarwick@usgs.gov","middleInitial":"D.","affiliations":[{"id":241,"text":"Eastern Energy Resources Science Center","active":true,"usgs":true}],"preferred":false,"id":727896,"contributorType":{"id":2,"text":"Editors"},"rank":3},{"text":"Finkelman, Robert B.","contributorId":38138,"corporation":false,"usgs":false,"family":"Finkelman","given":"Robert B.","affiliations":[{"id":6643,"text":"University of California - Berkeley","active":true,"usgs":false}],"preferred":false,"id":727897,"contributorType":{"id":2,"text":"Editors"},"rank":4},{"text":"Trippi, Michael H. 0000-0002-1398-3427 mtrippi@usgs.gov","orcid":"https://orcid.org/0000-0002-1398-3427","contributorId":941,"corporation":false,"usgs":true,"family":"Trippi","given":"Michael","email":"mtrippi@usgs.gov","middleInitial":"H.","affiliations":[{"id":241,"text":"Eastern Energy Resources Science Center","active":true,"usgs":true}],"preferred":true,"id":727898,"contributorType":{"id":2,"text":"Editors"},"rank":5}]}}
,{"id":58050,"text":"ofr20041347 - 2004 - Rainfall, runoff, and water-quality data for the urban storm-water program in the Albuquerque, New Mexico, metropolitan area, water year 2002","interactions":[],"lastModifiedDate":"2025-06-05T18:34:13.933998","indexId":"ofr20041347","displayToPublicDate":"2004-10-01T00:00:00","publicationYear":"2004","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":"2004-1347","title":"Rainfall, runoff, and water-quality data for the urban storm-water program in the Albuquerque, New Mexico, metropolitan area, water year 2002","docAbstract":"<p>Urbanization has dramatically increased precipitation runoff to the system of drainage channels and natural stream channels in the Albuquerque, New Mexico, metropolitan area. Rainfall and runoff data are important for planning and designing future storm-water conveyance channels in newly developing areas. Storm-water quality also is monitored in accordance with the National Pollutant Discharge Elimination System mandated by the U.S. Environmental Protection Agency. The Albuquerque Metropolitan Arroyo Flood Control Authority, the City of Albuquerque, and the U.S. Geological Survey began a cooperative program to collect hydrologic data to help assess the quality and quantity of surface-water resources in the Albuquerque area. This report presents water-quality, streamflow, and rainfall data collected from October 1, 2001, to September 30, 2002 (water year 2002). Also provided is a station analysis for each of the 20 streamflow-gaging sites and 41 rainfall-gaging sites, which includes a description of monitoring equipment, problems associated with data collection during the year, and other information used to compute streamflow discharges or rainfall records. A hydrographic comparison shows the effects that the largest drainage channel in the metropolitan area, the North Floodway Channel, has on total flow in the Rio Grande.</p>","language":"English","publisher":"U.S. Geological Survey","doi":"10.3133/ofr20041347","collaboration":"Prepared in cooperation with the Albuquerque Metropolitan Arroyo Flood Control Authority and the City of Albuquerque","usgsCitation":"Kelly, T., Romero, O., and Turner, E., 2004, Rainfall, runoff, and water-quality data for the urban storm-water program in the Albuquerque, New Mexico, metropolitan area, water year 2002: U.S. Geological Survey Open-File Report 2004-1347, iv, 119 p., https://doi.org/10.3133/ofr20041347.","productDescription":"iv, 119 p.","costCenters":[],"links":[{"id":183996,"rank":1,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/of/2004/1347/report-thumb.jpg"},{"id":489805,"rank":2,"type":{"id":11,"text":"Document"},"url":"https://pubs.usgs.gov/of/2004/1347/report.pdf","linkFileType":{"id":1,"text":"pdf"}}],"country":"United States","state":"New Mexico","city":"Albuquerque","geographicExtents":"{\n  \"type\": \"FeatureCollection\",\n  \"features\": [\n    {\n      \"type\": \"Feature\",\n      \"properties\": {},\n      \"geometry\": {\n        \"coordinates\": [\n          [\n            [\n              -107.0159062021065,\n              35.40557093842378\n            ],\n            [\n              -107.0159062021065,\n              34.77880064470824\n            ],\n            [\n              -106.13498380427245,\n              34.77880064470824\n            ],\n            [\n              -106.13498380427245,\n              35.40557093842378\n            ],\n            [\n              -107.0159062021065,\n              35.40557093842378\n            ]\n          ]\n        ],\n        \"type\": \"Polygon\"\n      }\n    }\n  ]\n}","noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"4f4e4a80e4b07f02db6496f4","contributors":{"authors":[{"text":"Kelly, Todd","contributorId":89168,"corporation":false,"usgs":true,"family":"Kelly","given":"Todd","email":"","affiliations":[],"preferred":false,"id":258219,"contributorType":{"id":1,"text":"Authors"},"rank":1},{"text":"Romero, Orlando","contributorId":92335,"corporation":false,"usgs":true,"family":"Romero","given":"Orlando","affiliations":[],"preferred":false,"id":258220,"contributorType":{"id":1,"text":"Authors"},"rank":2},{"text":"Turner, Eric","contributorId":101145,"corporation":false,"usgs":true,"family":"Turner","given":"Eric","email":"","affiliations":[],"preferred":false,"id":258221,"contributorType":{"id":1,"text":"Authors"},"rank":3}]}}
,{"id":58048,"text":"ofr20041334 - 2004 - NADM Conceptual Model 1.0 -- A Conceptual Model for Geologic Map Information","interactions":[],"lastModifiedDate":"2012-02-02T00:12:15","indexId":"ofr20041334","displayToPublicDate":"2004-10-01T00:00:00","publicationYear":"2004","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":"2004-1334","title":"NADM Conceptual Model 1.0 -- A Conceptual Model for Geologic Map Information","docAbstract":"Executive Summary -- The NADM Data Model Design Team was established in 1999 by the North American Geologic Map Data Model Steering Committee (NADMSC) with the purpose of drafting a geologic map data model for consideration as a standard for developing interoperable geologic map-centered databases by state, provincial, and federal geological surveys. The model is designed to be a technology-neutral conceptual model that can form the basis for a web-based interchange format using evolving information technology (e.g., XML, RDF, OWL), and guide implementation of geoscience databases in a common conceptual framework. The intended purpose is to allow geologic information sharing between geologic map data providers and users, independent of local information system implementation. \r\nThe model emphasizes geoscience concepts and relationships related to information presented on geologic maps. Design has been guided by an informal requirements analysis, documentation of existing databases, technology developments, and other standardization efforts in the geoscience and computer-science communities. \r\nA key aspect of the model is the notion that representation of the conceptual framework (ontology) that underlies geologic map data must be part of the model, because this framework changes with time and understanding, and varies between information providers. The top level of the model distinguishes geologic concepts, geologic representation concepts, and metadata. The geologic representation part of the model provides a framework for representing the ontology that underlies geologic map data through a controlled vocabulary, and for establishing the relationships between this vocabulary and a geologic map visualization or portrayal. Top-level geologic classes in the model are Earth material (substance), geologic unit (parts of the Earth), geologic age, geologic structure, fossil, geologic process, geologic relation, and geologic event.","language":"ENGLISH","doi":"10.3133/ofr20041334","usgsCitation":"North American Geologic Map Data Model (NADM) Steering Committee Data Model Design Team, 2004, NADM Conceptual Model 1.0 -- A Conceptual Model for Geologic Map Information: U.S. Geological Survey Open-File Report 2004-1334, 60 p., https://doi.org/10.3133/ofr20041334.","productDescription":"60 p.","costCenters":[],"links":[{"id":5978,"rank":100,"type":{"id":15,"text":"Index Page"},"url":"https://pubs.usgs.gov/of/2004/1334/","linkFileType":{"id":5,"text":"html"}},{"id":183917,"rank":0,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/thumbnails/usgs_thumb.jpg"}],"noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"4f4e4b32e4b07f02db6b492d","contributors":{"authors":[{"text":"North American Geologic Map Data Model (NADM) Steering Committee Data Model Design Team","contributorId":127896,"corporation":true,"usgs":false,"organization":"North American Geologic Map Data Model (NADM) Steering Committee Data Model Design Team","id":533190,"contributorType":{"id":1,"text":"Authors"},"rank":1}]}}
,{"id":58025,"text":"ofr20041277 - 2004 - Stream habitat and water-quality information for sites in the Buffalo River Basin and nearby basins of Arkansas, 2001-2002","interactions":[],"lastModifiedDate":"2012-02-02T00:12:31","indexId":"ofr20041277","displayToPublicDate":"2004-10-01T00:00:00","publicationYear":"2004","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":"2004-1277","title":"Stream habitat and water-quality information for sites in the Buffalo River Basin and nearby basins of Arkansas, 2001-2002","docAbstract":"The Buffalo River lies in north-central Arkansas and is a tributary of the White River. Stream-habitat and water-quality information are presented for 52 sites in the Buffalo River Basin and adjacent areas of the White River Basin. The information was collected during the summers of 2001 and 2002 to supplement fish community sampling during the same time period.","language":"ENGLISH","doi":"10.3133/ofr20041277","usgsCitation":"Petersen, J., 2004, Stream habitat and water-quality information for sites in the Buffalo River Basin and nearby basins of Arkansas, 2001-2002: U.S. Geological Survey Open-File Report 2004-1277, 16 p., https://doi.org/10.3133/ofr20041277.","productDescription":"16 p.","costCenters":[],"links":[{"id":183450,"rank":0,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/thumbnails/usgs_thumb.jpg"},{"id":5955,"rank":100,"type":{"id":15,"text":"Index Page"},"url":"https://pubs.water.usgs.gov/ofr2004-1277/","linkFileType":{"id":5,"text":"html"}}],"noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"4f4e4b16e4b07f02db6a54ab","contributors":{"authors":[{"text":"Petersen, James C. petersen@usgs.gov","contributorId":2437,"corporation":false,"usgs":true,"family":"Petersen","given":"James C.","email":"petersen@usgs.gov","affiliations":[{"id":129,"text":"Arkansas Water Science Center","active":true,"usgs":true}],"preferred":false,"id":258167,"contributorType":{"id":1,"text":"Authors"},"rank":1}]}}
,{"id":58024,"text":"ofr20041294 - 2004 - The Memphis, Shelby County, Tennessee, seismic hazard maps","interactions":[],"lastModifiedDate":"2012-02-02T00:12:31","indexId":"ofr20041294","displayToPublicDate":"2004-10-01T00:00:00","publicationYear":"2004","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":"2004-1294","title":"The Memphis, Shelby County, Tennessee, seismic hazard maps","language":"ENGLISH","doi":"10.3133/ofr20041294","usgsCitation":"Cramer, C.H., Gomberg, J.S., Schweig, E.S., Waldron, B.A., and Tucker, K., 2004, The Memphis, Shelby County, Tennessee, seismic hazard maps (Version 1.0): U.S. Geological Survey Open-File Report 2004-1294, 41 p., https://doi.org/10.3133/ofr20041294.","productDescription":"41 p.","costCenters":[],"links":[{"id":183449,"rank":0,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/thumbnails/usgs_thumb.jpg"},{"id":5954,"rank":100,"type":{"id":15,"text":"Index Page"},"url":"https://pubs.usgs.gov/of/2004/1294/","linkFileType":{"id":5,"text":"html"}}],"edition":"Version 1.0","noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"4f4e49f6e4b07f02db5f1418","contributors":{"authors":[{"text":"Cramer, Chris H.","contributorId":32196,"corporation":false,"usgs":true,"family":"Cramer","given":"Chris","email":"","middleInitial":"H.","affiliations":[],"preferred":false,"id":258164,"contributorType":{"id":1,"text":"Authors"},"rank":1},{"text":"Gomberg, Joan S. 0000-0002-0134-2606 gomberg@usgs.gov","orcid":"https://orcid.org/0000-0002-0134-2606","contributorId":1269,"corporation":false,"usgs":true,"family":"Gomberg","given":"Joan","email":"gomberg@usgs.gov","middleInitial":"S.","affiliations":[{"id":237,"text":"Earthquake Science Center","active":true,"usgs":true}],"preferred":true,"id":258162,"contributorType":{"id":1,"text":"Authors"},"rank":2},{"text":"Schweig, Eugene S. 0000-0003-3669-9741 schweig@usgs.gov","orcid":"https://orcid.org/0000-0003-3669-9741","contributorId":1271,"corporation":false,"usgs":true,"family":"Schweig","given":"Eugene","email":"schweig@usgs.gov","middleInitial":"S.","affiliations":[{"id":318,"text":"Geosciences and Environmental Change Science Center","active":true,"usgs":true}],"preferred":true,"id":258163,"contributorType":{"id":1,"text":"Authors"},"rank":3},{"text":"Waldron, Brian A.","contributorId":96767,"corporation":false,"usgs":true,"family":"Waldron","given":"Brian","email":"","middleInitial":"A.","affiliations":[],"preferred":false,"id":258166,"contributorType":{"id":1,"text":"Authors"},"rank":4},{"text":"Tucker, Kathleen","contributorId":65921,"corporation":false,"usgs":true,"family":"Tucker","given":"Kathleen","affiliations":[],"preferred":false,"id":258165,"contributorType":{"id":1,"text":"Authors"},"rank":5}]}}
,{"id":57778,"text":"ofr20041250 - 2004 - Flood of June 4-5, 2002, in the Maquoketa River Basin, east-central Iowa","interactions":[],"lastModifiedDate":"2016-02-01T12:58:46","indexId":"ofr20041250","displayToPublicDate":"2004-10-01T00:00:00","publicationYear":"2004","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":"2004-1250","title":"Flood of June 4-5, 2002, in the Maquoketa River Basin, east-central Iowa","docAbstract":"<p>Severe flooding occurred on June 4-5, 2002, in the Maquoketa River Basin in Delaware, Dubuque, Jackson, and Jones Counties, following thunderstorm activity over east-central Iowa. The rain gage at Cascade, Iowa, recorded a 14-hour rainfall of 6.0 inches at noon on June 4. Radar indications estimated as much as 8 to 10 inches of rain fell in the upper-middle part of the Maquoketa River Basin. Peak discharges on the Maquoketa River at Monticello of 47,500 cubic feet per second (recurrence interval estimated to be greater than 500 years as computed using flood-estimation equations developed by the U.S. Geological Survey), and at the Maquoketa River near Maquoketa streamflow-gaging station of 47,900 cubic feet per second (recurrence interval about 50 years), were determined for the flood. The peak discharge of the 2002 flood is nearly equal that of the 1944 flood (48,000 cubic feet per second), the largest flood on record in the Maquoketa River Basin. The 2002 flood is the largest known flood in the North Fork Maquoketa River Basin. A peak discharge of 22,600 cubic feet per second (recurrence interval about 110 years) was determined for the flood at the North Fork Maquoketa River near Fulton gaging station. Information about the basin and flood history, the 2002 thunderstorms and associated flooding, and a profile of high-water marks are presented for selected reaches along the Maquoketa and North Fork Maquoketa Rivers.</p>","language":"English","publisher":"U.S. Geological Survey","publisherLocation":"Reston, VA","doi":"10.3133/ofr20041250","collaboration":"Prepared in cooperation with the Iowa Department of Transportation and the Iowa Highway Research Board (Project HR-140)","usgsCitation":"Eash, D.A., 2004, Flood of June 4-5, 2002, in the Maquoketa River Basin, east-central Iowa (3rd Edition): U.S. Geological Survey Open-File Report 2004-1250, iv, 30 p., https://doi.org/10.3133/ofr20041250.","productDescription":"iv, 30 p.","onlineOnly":"N","additionalOnlineFiles":"N","costCenters":[{"id":351,"text":"Iowa Water Science 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 \"}}]}","edition":"3rd Edition","tableOfContents":"<p>Abstract<br />Introduction<br />&nbsp; &nbsp; &nbsp;Acknowledgments<br />Basin Description<br />Flood History<br />&nbsp; &nbsp; &nbsp;Flood of June 15, 1925<br />&nbsp; &nbsp; &nbsp;Flood of June 27, 1944<br />&nbsp; &nbsp; &nbsp;Flood of June 13, 1947<br />Flood of June 4-5, 2002<br />&nbsp; &nbsp; &nbsp;Storm Description<br />&nbsp; &nbsp; &nbsp;Flood Description<br />Flood Profile<br />Summary<br />References<br />Appendix: Temporary Bench Marks and Reference Points</p>","noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"4f4e48afe4b07f02db52f3cf","contributors":{"authors":[{"text":"Eash, David A. 0000-0002-2749-8959 daeash@usgs.gov","orcid":"https://orcid.org/0000-0002-2749-8959","contributorId":1887,"corporation":false,"usgs":true,"family":"Eash","given":"David","email":"daeash@usgs.gov","middleInitial":"A.","affiliations":[{"id":351,"text":"Iowa Water Science Center","active":true,"usgs":true}],"preferred":true,"id":257769,"contributorType":{"id":1,"text":"Authors"},"rank":1}]}}
,{"id":57804,"text":"ofr20041201 - 2004 - Hydraulic conductivity of near-surface alluvium in the vicinity of Cattlemans Detention Basin, South Lake Tahoe, California","interactions":[],"lastModifiedDate":"2012-02-02T00:12:21","indexId":"ofr20041201","displayToPublicDate":"2004-10-01T00:00:00","publicationYear":"2004","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":"2004-1201","title":"Hydraulic conductivity of near-surface alluvium in the vicinity of Cattlemans Detention Basin, South Lake Tahoe, California","docAbstract":"Cattlemans detention basin, South Lake Tahoe, California is designed to capture and reduce urban runoff and pollutants originating from developed areas before entering Cold Creek, which is tributary to Trout Creek and to Lake Tahoe. The effectiveness of the basin in reducing sediment and nutrient loads currently is being assessed with a five-year study. Hydraulic conductivity of the alluvium near the detention basin is needed to estimate ground-water flow and subsurface nutrient transport. Hydraulic conductivity was estimated using slug tests in 27 monitoring wells that surround the detention basin. For each test, water was poured rapidly into a well, changes in water-level were monitored, and the observed changes were analyzed using the Bouwer and Rice method. Each well was tested one to four times. A total of 24 wells were tested more than once. Of the 24 wells, the differences among the tests were within 10 percent of the average. Estimated hydraulic conductivities of basin alluvium range from 0.5 to 70 feet per day with an average of 17.8 feet per day. This range is consistent with the sandy alluvial deposits observed in the area of Cattlemans detention basin.","language":"ENGLISH","doi":"10.3133/ofr20041201","usgsCitation":"Green, J.M., Henkelman, K.K., and Caskey, R.M., 2004, Hydraulic conductivity of near-surface alluvium in the vicinity of Cattlemans Detention Basin, South Lake Tahoe, California: U.S. Geological Survey Open-File Report 2004-1201, 18 p., https://doi.org/10.3133/ofr20041201.","productDescription":"18 p.","costCenters":[],"links":[{"id":5764,"rank":100,"type":{"id":15,"text":"Index Page"},"url":"https://pubs.water.usgs.gov/ofr2004-1201/","linkFileType":{"id":5,"text":"html"}},{"id":184119,"rank":0,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/thumbnails/usgs_thumb.jpg"}],"noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"4f4e4a51e4b07f02db62a2f1","contributors":{"authors":[{"text":"Green, Jena M.","contributorId":77597,"corporation":false,"usgs":true,"family":"Green","given":"Jena","email":"","middleInitial":"M.","affiliations":[],"preferred":false,"id":257839,"contributorType":{"id":1,"text":"Authors"},"rank":1},{"text":"Henkelman, Katherine K.","contributorId":26751,"corporation":false,"usgs":true,"family":"Henkelman","given":"Katherine","email":"","middleInitial":"K.","affiliations":[],"preferred":false,"id":257837,"contributorType":{"id":1,"text":"Authors"},"rank":2},{"text":"Caskey, Rachel M.","contributorId":74817,"corporation":false,"usgs":true,"family":"Caskey","given":"Rachel","email":"","middleInitial":"M.","affiliations":[],"preferred":false,"id":257838,"contributorType":{"id":1,"text":"Authors"},"rank":3}]}}
,{"id":57801,"text":"ofr20041255 - 2004 - VPV--The velocity profile viewer user manual","interactions":[],"lastModifiedDate":"2012-02-02T00:12:21","indexId":"ofr20041255","displayToPublicDate":"2004-10-01T00:00:00","publicationYear":"2004","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":"2004-1255","title":"VPV--The velocity profile viewer user manual","docAbstract":"The Velocity Profile Viewer (VPV) is a tool for visualizing time series of velocity profiles developed by the U.S. Geological Survey (USGS). The USGS uses VPV to preview and present measured velocity data from acoustic Doppler current profilers and simulated velocity data from three-dimensional estuarine, river, and lake hydrodynamic models. The data can be viewed as an animated three-dimensional profile or as a stack of time-series graphs that each represents a location in the water column.\r\n\r\n    The graphically displayed data are shown at each time step like frames of animation. The animation can play at several different speeds or can be suspended on one frame. The viewing angle and time can be manipulated using mouse interaction. A number of options control the appearance of the profile and the graphs. VPV cannot edit or save data, but it can create a Post-Script file showing the velocity profile in three dimensions. This user manual describes how to use each of these features. VPV is available and can be downloaded for free from the World Wide Web at http://ca.water.usgs.gov/program/sfbay/vpv.","language":"ENGLISH","doi":"10.3133/ofr20041255","usgsCitation":"Donovan, J.M., 2004, VPV--The velocity profile viewer user manual (Online Only): U.S. Geological Survey Open-File Report 2004-1255, 63 p., https://doi.org/10.3133/ofr20041255.","productDescription":"63 p.","onlineOnly":"Y","costCenters":[],"links":[{"id":184034,"rank":0,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/thumbnails/usgs_thumb.jpg"},{"id":5761,"rank":100,"type":{"id":15,"text":"Index Page"},"url":"https://pubs.water.usgs.gov/ofr2004-1255/","linkFileType":{"id":5,"text":"html"}}],"edition":"Online Only","noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"4f4e4a14e4b07f02db602cf0","contributors":{"authors":[{"text":"Donovan, John M. 0000-0002-7957-5397 jmd@usgs.gov","orcid":"https://orcid.org/0000-0002-7957-5397","contributorId":1255,"corporation":false,"usgs":true,"family":"Donovan","given":"John","email":"jmd@usgs.gov","middleInitial":"M.","affiliations":[{"id":154,"text":"California Water Science Center","active":true,"usgs":true}],"preferred":true,"id":257827,"contributorType":{"id":1,"text":"Authors"},"rank":1}]}}
,{"id":57899,"text":"ofr20041296 - 2004 - A summary of the scientific literature on the effects of fire on the concentration of nutrients in surface waters","interactions":[],"lastModifiedDate":"2012-02-02T00:12:14","indexId":"ofr20041296","displayToPublicDate":"2004-10-01T00:00:00","publicationYear":"2004","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":"2004-1296","title":"A summary of the scientific literature on the effects of fire on the concentration of nutrients in surface waters","docAbstract":"This paper provides a detailed review of the chemical changes that occur in soil during a fire, the pathways by which nutrients are transferred from soil to surface-water bodies following a fire, and the temporal and spatial effects of fires on the concentration of nutrients in surface-water bodies during and following a fire that have been reported in the scientific literature. Thirty-nine papers from the scientific literature that represent studies that (1) were done in a variety of environments (savannas, grasslands, temperate forests, alpine forests, and so forth); (2) had a range of sampling frequency and duration, such as during and immediately following a fire (from the start of fire to 1 year later), short-term sampling (from end of fire to 3 years later), and long term-sampling (sampling for greater than 3 years following a fire); and (3) incorporated watersheds with various burn intensities, severities, and histories were reviewed and summarized. The review of the scientific literature has revealed that measurable effects of fires on streamwater quality are most likely to occur if the fire was severe enough to burn large amounts of organic matter, if windy conditions were present during the fire, if heavy rain occurred following the fire, and if the fire occurred in a watershed with steep slopes and soils with little cation-exchange capacity. Measurable effects of fires on lake- and reservoir-water quality are most likely to occur if, in addition to the factors listed for streams, the lake or reservoir is oligotrophic or mesotrophic and the residence time of water in the lake or reservoir is short relative to the length of time elevated concentrations of nutrients occur in runoff. Knowledge of whether a lake or reservoir is nitrogen or phosphorus limited is important because eutrophication of nitrogen-limited lakes may occur following a fire due to increasing nitrogen:phosphorus ratios caused by prolonged increases of nitrogen concentrations, especially nitrate.","language":"ENGLISH","doi":"10.3133/ofr20041296","usgsCitation":"Ranalli, A.J., 2004, A summary of the scientific literature on the effects of fire on the concentration of nutrients in surface waters (Online Only): U.S. Geological Survey Open-File Report 2004-1296, 23 p., https://doi.org/10.3133/ofr20041296.","productDescription":"23 p.","onlineOnly":"Y","costCenters":[],"links":[{"id":5857,"rank":100,"type":{"id":15,"text":"Index Page"},"url":"https://pubs.water.usgs.gov/ofr2004-1296/","linkFileType":{"id":5,"text":"html"}},{"id":185204,"rank":0,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/thumbnails/usgs_thumb.jpg"}],"edition":"Online Only","noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"4f4e4b17e4b07f02db6a5f2f","contributors":{"authors":[{"text":"Ranalli, Anthony J. tranalli@usgs.gov","contributorId":1195,"corporation":false,"usgs":true,"family":"Ranalli","given":"Anthony","email":"tranalli@usgs.gov","middleInitial":"J.","affiliations":[],"preferred":true,"id":257916,"contributorType":{"id":1,"text":"Authors"},"rank":1}]}}
,{"id":57947,"text":"ofr20041336 - 2004 - Lime kiln dust as a potential raw material in portland cement manufacturing","interactions":[],"lastModifiedDate":"2012-02-02T00:12:00","indexId":"ofr20041336","displayToPublicDate":"2004-10-01T00:00:00","publicationYear":"2004","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":"2004-1336","title":"Lime kiln dust as a potential raw material in portland cement manufacturing","docAbstract":"In the United States, the manufacture of portland cement involves burning in a rotary kiln a finely ground proportional mix of raw materials. The raw material mix provides the required chemical combination of calcium, silicon, aluminum, iron, and small amounts of other ingredients. The majority of calcium is supplied in the form of calcium carbonate usually from limestone. Other sources including waste materials or byproducts from other industries can be used to supply calcium (or lime, CaO), provided they have sufficiently high CaO content, have low magnesia content (less than 5 percent), and are competitive with limestone in terms of cost and adequacy of supply. In the United States, the lime industry produces large amounts of lime kiln dust (LKD), which is collected by dust control systems. This LKD may be a supplemental source of calcium for cement plants, if the lime and cement plants are located near enough to each other to make the arrangement economical.","language":"ENGLISH","doi":"10.3133/ofr20041336","usgsCitation":"Miller, M.M., and Callaghan, R.M., 2004, Lime kiln dust as a potential raw material in portland cement manufacturing (Version 1.0; Online only): U.S. Geological Survey Open-File Report 2004-1336, 9 p., https://doi.org/10.3133/ofr20041336.","productDescription":"9 p.","onlineOnly":"Y","costCenters":[],"links":[{"id":181951,"rank":0,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/thumbnails/usgs_thumb.jpg"},{"id":5906,"rank":100,"type":{"id":15,"text":"Index Page"},"url":"https://pubs.usgs.gov/of/2004/1336/","linkFileType":{"id":5,"text":"html"}}],"edition":"Version 1.0; Online only","noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"4f4e4b16e4b07f02db6a52ef","contributors":{"authors":[{"text":"Miller, M. Michael mmiller1@usgs.gov","contributorId":2018,"corporation":false,"usgs":true,"family":"Miller","given":"M.","email":"mmiller1@usgs.gov","middleInitial":"Michael","affiliations":[{"id":432,"text":"National Minerals Information Center","active":true,"usgs":true},{"id":245,"text":"Eastern Mineral and Environmental Resources Science Center","active":true,"usgs":true}],"preferred":true,"id":257969,"contributorType":{"id":1,"text":"Authors"},"rank":1},{"text":"Callaghan, Robert M. rcallaghan@usgs.gov","contributorId":475,"corporation":false,"usgs":true,"family":"Callaghan","given":"Robert","email":"rcallaghan@usgs.gov","middleInitial":"M.","affiliations":[],"preferred":true,"id":257968,"contributorType":{"id":1,"text":"Authors"},"rank":2}]}}
,{"id":58104,"text":"ofr20041353 - 2004 - Dynamics of the physical environment at the USS Arizona memorial: 2002-2004","interactions":[],"lastModifiedDate":"2023-03-22T20:45:22.500744","indexId":"ofr20041353","displayToPublicDate":"2004-10-01T00:00:00","publicationYear":"2004","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":"2004-1353","title":"Dynamics of the physical environment at the USS Arizona memorial: 2002-2004","docAbstract":"<p>No abstract available.</p>","language":"English","publisher":"U.S. Geological Survey","doi":"10.3133/ofr20041353","usgsCitation":"Storlazzi, C., Russell, M.A., Owens, M.D., Field, M.E., and Murphy, L.E., 2004, Dynamics of the physical environment at the USS Arizona memorial: 2002-2004 (Version 1.0): U.S. Geological Survey Open-File Report 2004-1353, 28 p., https://doi.org/10.3133/ofr20041353.","productDescription":"28 p.","costCenters":[{"id":520,"text":"Pacific Coastal and Marine Science Center","active":true,"usgs":true}],"links":[{"id":181222,"rank":1,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/thumbnails/usgs_thumb.jpg"},{"id":414578,"rank":3,"type":{"id":36,"text":"NGMDB Index Page"},"url":"https://ngmdb.usgs.gov/Prodesc/proddesc_69080.htm","linkFileType":{"id":5,"text":"html"}},{"id":5716,"rank":2,"type":{"id":15,"text":"Index Page"},"url":"https://pubs.usgs.gov/of/2004/1353/","linkFileType":{"id":5,"text":"html"}}],"country":"United States","state":"Hawaii","otherGeospatial":"USS Arizona Memorial","geographicExtents":"{\n  \"type\": \"FeatureCollection\",\n  \"features\": [\n    {\n      \"type\": \"Feature\",\n      \"properties\": {},\n      \"geometry\": {\n        \"coordinates\": [\n          [\n            [\n              -157.95033963540192,\n              21.365229540959703\n            ],\n            [\n              -157.95033963540192,\n              21.364365122627703\n            ],\n            [\n              -157.94948215103528,\n              21.364365122627703\n            ],\n            [\n              -157.94948215103528,\n              21.365229540959703\n            ],\n            [\n              -157.95033963540192,\n              21.365229540959703\n            ]\n          ]\n        ],\n        \"type\": \"Polygon\"\n      }\n    }\n  ]\n}","edition":"Version 1.0","noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"4f4e4a59e4b07f02db62fe2d","contributors":{"authors":[{"text":"Storlazzi, Curt D. 0000-0001-8057-4490","orcid":"https://orcid.org/0000-0001-8057-4490","contributorId":77889,"corporation":false,"usgs":true,"family":"Storlazzi","given":"Curt D.","affiliations":[],"preferred":false,"id":258330,"contributorType":{"id":1,"text":"Authors"},"rank":1},{"text":"Russell, Matthew A.","contributorId":74814,"corporation":false,"usgs":true,"family":"Russell","given":"Matthew","email":"","middleInitial":"A.","affiliations":[],"preferred":false,"id":258329,"contributorType":{"id":1,"text":"Authors"},"rank":2},{"text":"Owens, Marshall D.","contributorId":32238,"corporation":false,"usgs":true,"family":"Owens","given":"Marshall","email":"","middleInitial":"D.","affiliations":[],"preferred":false,"id":258327,"contributorType":{"id":1,"text":"Authors"},"rank":3},{"text":"Field, Michael E. mfield@usgs.gov","contributorId":2101,"corporation":false,"usgs":true,"family":"Field","given":"Michael","email":"mfield@usgs.gov","middleInitial":"E.","affiliations":[{"id":520,"text":"Pacific Coastal and Marine Science Center","active":true,"usgs":true}],"preferred":true,"id":258326,"contributorType":{"id":1,"text":"Authors"},"rank":4},{"text":"Murphy, Larry E.","contributorId":57942,"corporation":false,"usgs":true,"family":"Murphy","given":"Larry","email":"","middleInitial":"E.","affiliations":[],"preferred":false,"id":258328,"contributorType":{"id":1,"text":"Authors"},"rank":5}]}}
,{"id":54049,"text":"ofr20041073 - 2004 - Surface- and Ground-Water Monitoring and Mapping of Selected Features at the Blue Ridge Parkway Mt. Pisgah Campground, Haywood County, North Carolina, 2002","interactions":[],"lastModifiedDate":"2016-12-07T16:34:35","indexId":"ofr20041073","displayToPublicDate":"2004-10-01T00:00:00","publicationYear":"2004","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":"2004-1073","title":"Surface- and Ground-Water Monitoring and Mapping of Selected Features at the Blue Ridge Parkway Mt. Pisgah Campground, Haywood County, North Carolina, 2002","docAbstract":"During 2002, a baseline study of hydrologic conditions was conducted, and selected features were mapped within the Mt. Pisgah campground on the Blue Ridge Parkway in Haywood County, North Carolina. Field surveys were performed by using global positioning system equipment one time (January 2002) during the study to locate hydrologic and other types of features in the study area. Water-level and streamflow data and seasonal water-quality samples were collected from a stream that receives all surface-water drainage from the campground area. During 2002, water levels (stage) in the stream ranged from 1.09 to 1.89 feet above gage datum (4,838.06 to 4,838.86 feet above mean sea level). Flow in the stream ranged from 0.05 to 9.7 cubic feet per second. Annual daily mean flow for calendar year 2002 was approximately 0.35 cubic foot per second (about 226,000 gallons per day). Samples collected from the stream had low concentrations of all constituents measured. Four compounds associated with human activity (camphor, N,N-diethyl-meta-toluamide (the insect repellent DEET), tributylphosphate, and methylsalicylate) were detected in the stream samples; however, concentrations were less than detection levels. Stream samples collected in April and September and analyzed for fecal coliform bacteria had densities of 76 and 110 colonies per 100 milliliters of water, respectively. No violations of water-quality standards were noted for any constituent measured in the stream samples.\r\n\r\nSeven shallow ground-water wells were installed near a natural area in the center of the campground. Ground-water levels measured periodically in these wells and in two existing shallow piezometers generally were highest in the spring and lowest in the fall. Water temperature, pH, and specific conductance were measured in samples collected from the shallow wells in April and September 2002. Measured pH values were consistently lowest in samples from two wells on the west side of the natural area and highest in samples from the well located near the center of the natural area. Specific-conductance values measured in samples from wells on the east side of the natural area were lower than those measured in samples from the other wells. Specific-conductance values measured in samples from two wells on the west side and from one well near the center of the natural area generally were two to three times higher than the specific-conductance values measured in samples from wells on the east side of the natural area.\r\n\r\nSamples for fecal coliform bacteria were collected from six wells on September 11, 2002. The fecal coliform densities in samples from most of the wells were less than or equal to 8 colonies per 100 milliliters. Samples from two of the three wells on the west side of the natural area had coliform densities of 16 and 480 colonies per 100 milliliters.\r\n\r\nOther ground-water samples collected on September 11 and September 24 were analyzed with a spectrophotometer in the U.S. Geological Survey (USGS) North Carolina District Office for nitrate concentrations only. From the samples collected on September 11, estimated nitrate concentrations of 1 milligram per liter or less were detected in three wells, two on the west side and one on the east side of the natural area. Nitrate was not detected with a spectrophotometer in any of the ground-water samples collected on September 24. Indicator test strips also were used in the field to screen for nitrate and nitrite in ground-water samples collected on September 24. Nitrate was detected by test strips in one well on the west side of the natural area, with estimated concentrations of 1 milligram per liter or less indicated. Nitrite was not detected by the test strips in samples collected from any of the wells.","language":"ENGLISH","doi":"10.3133/ofr20041073","usgsCitation":"Smith, D.G., 2004, Surface- and Ground-Water Monitoring and Mapping of Selected Features at the Blue Ridge Parkway Mt. Pisgah Campground, Haywood County, North Carolina, 2002: U.S. Geological Survey Open-File Report 2004-1073, 39 p., https://doi.org/10.3133/ofr20041073.","productDescription":"39 p.","costCenters":[{"id":13634,"text":"South Atlantic Water Science Center","active":true,"usgs":true}],"links":[{"id":174755,"rank":0,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/thumbnails/usgs_thumb.jpg"},{"id":5491,"rank":100,"type":{"id":15,"text":"Index Page"},"url":"https://pubs.water.usgs.gov/of2004-1073/","linkFileType":{"id":5,"text":"html"}}],"country":"United States","state":"North Carolina","county":"Haywood County","otherGeospatial":"Mt. Pisgah Campground,","geographicExtents":"{\n  \"type\": \"FeatureCollection\",\n  \"features\": [\n    {\n      \"type\": \"Feature\",\n      \"properties\": {},\n      \"geometry\": {\n        \"type\": \"Polygon\",\n        \"coordinates\": [\n          [\n            [\n              -83.71307373046874,\n              35.67068501330236\n            ],\n            [\n              -83.71307373046874,\n              35.67068501330236\n            ],\n            [\n              -83.7103271484375,\n              35.67068501330236\n            ],\n            [\n              -83.7103271484375,\n              35.67068501330236\n            ],\n            [\n              -83.71307373046874,\n              35.67068501330236\n            ]\n          ]\n        ]\n      }\n    },\n    {\n      \"type\": \"Feature\",\n      \"properties\": {},\n      \"geometry\": {\n        \"type\": \"Polygon\",\n        \"coordinates\": [\n          [\n            [\n              -83.25027465820312,\n              34.98837848142154\n            ],\n            [\n              -83.25027465820312,\n              35.64390523787731\n            ],\n            [\n              -82.47848510742188,\n              35.64390523787731\n            ],\n            [\n              -82.47848510742188,\n              34.98837848142154\n            ],\n            [\n              -83.25027465820312,\n              34.98837848142154\n            ]\n          ]\n        ]\n      }\n    }\n  ]\n}","noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"4f4e4aeee4b07f02db6911c7","contributors":{"authors":[{"text":"Smith, Douglas G. dgsmith@usgs.gov","contributorId":1532,"corporation":false,"usgs":true,"family":"Smith","given":"Douglas","email":"dgsmith@usgs.gov","middleInitial":"G.","affiliations":[{"id":476,"text":"North Carolina Water Science Center","active":true,"usgs":true}],"preferred":true,"id":249054,"contributorType":{"id":1,"text":"Authors"},"rank":1}]}}
,{"id":53844,"text":"ofr2003503 - 2004 - Ground-water, surface-water, and water-chemistry data, Black Mesa area, northeastern Arizona — 2002-03","interactions":[],"lastModifiedDate":"2021-12-08T22:22:15.539361","indexId":"ofr2003503","displayToPublicDate":"2004-10-01T00:00:00","publicationYear":"2004","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":"2003-503","title":"Ground-water, surface-water, and water-chemistry data, Black Mesa area, northeastern Arizona — 2002-03","docAbstract":"The N aquifer is the major source of water in the 5,400-square-mile area of Black Mesa in northeastern Arizona. Availability of water is an important issue in this area because of continued industrial and municipal use, a growing population, and precipitation of about 6 to 14 inches per year.\r\n\r\nThe monitoring program in the Black Mesa area has been operating since 1971 and is designed to determine the long-term effects of ground-water withdrawals from the N aquifer for industrial and municipal uses. The monitoring program includes measurements of (1) ground-water pumping, (2) ground-water levels, (3) spring discharge, (4) surface-water discharge, (5) ground-water chemistry, and (6) periodic testing of ground-water withdrawal meters.\r\n\r\nIn 2002, total ground-water withdrawals were 8,000 acre-feet, industrial use was 4,640 acre-feet, and municipal use was 3,360 acre-feet. From 2001 to 2002, total withdrawals increased by 4 percent, industrial use increased by 2 percent, and municipal use increased by 7 percent. Flowmeter testing was completed for 32 municipal wells in 2003. The median difference between pumping rates for the permanent meter and a test meter for all the sites tested was -2.0 percent. Values ranged from -13.7 percent at Hopi High School no. 2 to +12.9 percent at Shonto PM3.\r\n\r\nFrom 2002 to 2003, water levels declined in 5 of 13 wells in the unconfined part of the aquifer, and the median change was 0.0 foot. Water levels declined in 8 of 13 wells in the confined part of the aquifer, and the median change was -1.1 feet.\r\n\r\nFrom the prestress period (prior to 1965) to 2003, the median water-level change for 26 wells was -8.3 feet. Median water-level changes were -0.4 foot for 13 wells in the unconfirned part of the aquifer and -60.3 feet for 13 wells in the confined part.\r\n\r\nDischarges were measured once in 2002 and once in 2003 at four springs. Discharge decreased by 16 percent at Pasture Canyon Spring, increased 10 percent at Moenkopi Spring and 90 percent at an unnamed spring near Dennehotso, and did not change at Burro Spring. For the past 11 years, discharges from the four springs have fluctuated; however, an increasing or decreasing trend is not apparent.\r\n\r\nContinuous records of surface-water discharge have been collected from 1976 to 2002 at Moenkopi Wash, 1996 to 2002 at Laguna Creek, 1993 to 2002 at Dinnebito Wash, and 1994 to 2002 at Polacca Wash. Median flows for November, December, January, and February of each water year were used as an index of ground-water discharge to those streams. Since 1995, the median winter flows have decreased for Moenkopi Wash, Dinnebito Wash, and Polacca Wash. Since the first continuous record of surface-water discharge in 1997, there is no consistent trend in the median winter flow for Laguna Creek.\r\n\r\nIn 2003, water samples were collected from 12 wells and 4 springs and analyzed for selected chemical constituents. Dissolved-solids concentrations ranged from 118 to 642 milligrams per liter. Water samples from 10 of the wells and from all of the springs had less than 500 milligrams per liter of dissolved solids. There are no appreciable time trends in the chemistry of water samples from 7 wells and 4 springs; 7 wells had more than 8 years of data, and the 4 springs had more than 10 years of data.","language":"English","publisher":"U.S. Geological Survey","doi":"10.3133/ofr2003503","usgsCitation":"Truini, M., and Thomas, B.E., 2004, Ground-water, surface-water, and water-chemistry data, Black Mesa area, northeastern Arizona — 2002-03: U.S. Geological Survey Open-File Report 2003-503, vi, 43 p., https://doi.org/10.3133/ofr2003503.","productDescription":"vi, 43 p.","costCenters":[],"links":[{"id":175150,"rank":0,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/thumbnails/usgs_thumb.jpg"},{"id":392657,"rank":3,"type":{"id":36,"text":"NGMDB Index Page"},"url":"https://ngmdb.usgs.gov/Prodesc/proddesc_67778.htm"},{"id":5275,"rank":100,"type":{"id":15,"text":"Index Page"},"url":"https://pubs.water.usgs.gov/ofr03503/","linkFileType":{"id":5,"text":"html"}}],"country":"United States","state":"Arizona","otherGeospatial":"Black Mesa area","geographicExtents":"{\n  \"type\": \"FeatureCollection\",\n  \"features\": [\n    {\n      \"type\": \"Feature\",\n      \"properties\": {},\n      \"geometry\": {\n        \"type\": \"Polygon\",\n        \"coordinates\": [\n          [\n            [\n              -111.4167,\n              35.6167\n            ],\n            [\n             -109.75,\n              35.6167\n            ],\n            [\n              -109.75,\n              36.7778\n            ],\n            [\n              -111.4167,\n              36.7778\n            ],\n            [\n              -111.4167,\n              35.6167\n            ]\n          ]\n        ]\n      }\n    }\n  ]\n}","noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"4f4e4b12e4b07f02db6a2700","contributors":{"authors":[{"text":"Truini, Margot mtruini@usgs.gov","contributorId":599,"corporation":false,"usgs":true,"family":"Truini","given":"Margot","email":"mtruini@usgs.gov","affiliations":[{"id":128,"text":"Arizona Water Science Center","active":true,"usgs":true}],"preferred":true,"id":248478,"contributorType":{"id":1,"text":"Authors"},"rank":1},{"text":"Thomas, Blakemore E.","contributorId":93871,"corporation":false,"usgs":true,"family":"Thomas","given":"Blakemore","email":"","middleInitial":"E.","affiliations":[],"preferred":false,"id":248479,"contributorType":{"id":1,"text":"Authors"},"rank":2}]}}
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