No abstract available.
","language":"English","publisher":"U.S. Geological Survey","doi":"10.3133/ofr99462","issn":"0094-9140","usgsCitation":"Harte, P., Flynn, R.H., and Mack, T.J., 1999, Construction and calibration of numerical ground-water-flow models of the western half of the Milford-Souhegan glacial-drift aquifer, Milford, New Hampshire: U.S. Geological Survey Open-File Report 99-462, Report: v, 76 p.; 2 Plates: 17.65 × 17.49 inches and 17.78 × 17.86 inches, https://doi.org/10.3133/ofr99462.","productDescription":"Report: v, 76 p.; 2 Plates: 17.65 × 17.49 inches and 17.78 × 17.86 inches","costCenters":[],"links":[{"id":52607,"rank":300,"type":{"id":11,"text":"Document"},"url":"https://pubs.usgs.gov/of/1999/0462/report.pdf","linkFileType":{"id":1,"text":"pdf"}},{"id":52606,"rank":401,"type":{"id":17,"text":"Plate"},"url":"https://pubs.usgs.gov/of/1999/0462/plate-2.pdf","linkFileType":{"id":1,"text":"pdf"}},{"id":52605,"rank":400,"type":{"id":17,"text":"Plate"},"url":"https://pubs.usgs.gov/of/1999/0462/plate-1.pdf","linkFileType":{"id":1,"text":"pdf"}},{"id":155100,"rank":0,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/of/1999/0462/report-thumb.jpg"},{"id":394729,"rank":5,"type":{"id":36,"text":"NGMDB Index Page"},"url":"https://ngmdb.usgs.gov/Prodesc/proddesc_23024.htm"}],"country":"United States","state":"New Hampshire","city":"Milford","geographicExtents":"{\n \"type\": \"FeatureCollection\",\n \"features\": [\n {\n \"type\": \"Feature\",\n \"properties\": {},\n \"geometry\": {\n \"type\": \"Polygon\",\n \"coordinates\": [\n [\n [\n -71.70501708984375,\n 42.83783543600974\n ],\n [\n -71.67205810546875,\n 42.83783543600974\n ],\n [\n -71.67205810546875,\n 42.849792501926466\n ],\n [\n -71.70501708984375,\n 42.849792501926466\n ],\n [\n -71.70501708984375,\n 42.83783543600974\n ]\n ]\n ]\n }\n }\n ]\n}","noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"4f4e4b12e4b07f02db6a2f14","contributors":{"authors":[{"text":"Harte, P. T. 0000-0002-7718-1204","orcid":"https://orcid.org/0000-0002-7718-1204","contributorId":36143,"corporation":false,"usgs":true,"family":"Harte","given":"P. T.","affiliations":[],"preferred":false,"id":189863,"contributorType":{"id":1,"text":"Authors"},"rank":1},{"text":"Flynn, R. H.","contributorId":44946,"corporation":false,"usgs":true,"family":"Flynn","given":"R.","email":"","middleInitial":"H.","affiliations":[],"preferred":false,"id":189865,"contributorType":{"id":1,"text":"Authors"},"rank":2},{"text":"Mack, Thomas J. 0000-0002-0496-3918","orcid":"https://orcid.org/0000-0002-0496-3918","contributorId":39814,"corporation":false,"usgs":true,"family":"Mack","given":"Thomas","email":"","middleInitial":"J.","affiliations":[],"preferred":false,"id":189864,"contributorType":{"id":1,"text":"Authors"},"rank":3}]}} ,{"id":24306,"text":"ofr99531 - 1999 - Elemental analyses of modern dust in southern Nevada and California","interactions":[],"lastModifiedDate":"2017-03-09T15:36:30","indexId":"ofr99531","displayToPublicDate":"2000-04-01T00:00:00","publicationYear":"1999","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":"99-531","title":"Elemental analyses of modern dust in southern Nevada and California","docAbstract":"Selected samples of modern dust collected in marble traps at sites in southern Nevada and California (Reheis and Kihl, 1995; Reheis, 1997) have been analyzed for elemental composition using instrumental neutron activation analysis (INAA) and inductively coupled plasma atomic emission spectroscopy (ICP-AES) and inductively coupled plasma mass spectroscopy (ICP-MS). For information on these analytical techniques and their levels of precision and accuracy, refer to Baedecker and McKown (1987) for INAA, to Briggs (1996) for ICP-AES, and to Briggs and Meier (1999) for ICP-MS. This report presents the elemental compositions obtained using these techniques on dust samples collected from 1991 through 1997.
The dust-trap sites were established at varying times; some have been maintained since 1984, others since 1991. For details on site location, dust-trap construction, and collection techniques, see Reheis and Kihl (1995) and Reheis (1997). Briefly, the trap consists of a coated angel-food cake pan painted black on the outside and mounted on a post about 2 m above the ground. Glass marbles rest on a circular piece of galvanized hardware cloth (now replaced by stainless-steel mesh), which is fitted into the pan so that it rests 3-4 cm below the rim. The 2-m height eliminates most saltating sand-sized particles. The marbles simulate the effect of a gravelly fan surface and prevent dust that has filtered or washed into the bottom of the pan from being blown back out. The dust traps are fitted with two metal straps looped in an inverted basket shape; the top surfaces of the straps are coated with a sticky material that effectively discourages birds from roosting.
","language":"English","publisher":"U.S. Geological Survey","publisherLocation":"Denver, CO","doi":"10.3133/ofr99531","issn":"0094-9140","usgsCitation":"Reheis, M., Budahn, J., and Lamothe, P.J., 1999, Elemental analyses of modern dust in southern Nevada and California: U.S. Geological Survey Open-File Report 99-531, https://doi.org/10.3133/ofr99531.","costCenters":[],"links":[{"id":156239,"rank":0,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/thumbnails/usgs_thumb.jpg"},{"id":1688,"rank":100,"type":{"id":15,"text":"Index Page"},"url":"https://pubs.usgs.gov/of/1999/ofr-99-0531/","linkFileType":{"id":5,"text":"html"}}],"country":"United States","state":"California, Nevada","noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"4f4e4a1ae4b07f02db6068b9","contributors":{"authors":[{"text":"Reheis, M.C. 0000-0002-8359-323X","orcid":"https://orcid.org/0000-0002-8359-323X","contributorId":36128,"corporation":false,"usgs":true,"family":"Reheis","given":"M.C.","affiliations":[],"preferred":false,"id":191664,"contributorType":{"id":1,"text":"Authors"},"rank":1},{"text":"Budahn, J. R. 0000-0001-9794-8882","orcid":"https://orcid.org/0000-0001-9794-8882","contributorId":83914,"corporation":false,"usgs":true,"family":"Budahn","given":"J. R.","affiliations":[],"preferred":false,"id":191666,"contributorType":{"id":1,"text":"Authors"},"rank":2},{"text":"Lamothe, P. J.","contributorId":45672,"corporation":false,"usgs":true,"family":"Lamothe","given":"P.","email":"","middleInitial":"J.","affiliations":[],"preferred":false,"id":191665,"contributorType":{"id":1,"text":"Authors"},"rank":3}]}} ,{"id":38114,"text":"ofr99408 - 1999 - Digital mining claim density map for federal lands in Washington: 1996","interactions":[],"lastModifiedDate":"2023-06-19T18:52:20.137086","indexId":"ofr99408","displayToPublicDate":"2000-04-01T00:00:00","publicationYear":"1999","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":"99-408","title":"Digital mining claim density map for federal lands in Washington: 1996","docAbstract":"This report describes a digital map generated by the U.S. Geological Survey (USGS) to provide digital spatial mining claim density information for federal lands in Washington as of March 1997. Mining claim data is earth science information deemed to be relevant to the assessment of historic, current, and future ecological, economic, and social systems.\n\nThere is no paper map included in this Open-File report. In accordance with the Federal Land Policy and Management Act of 1976 (FLPMA), all unpatented mining claims, mill, and tunnel sites must be recorded at the appropriate BLM State office. BLM maintains a cumulative computer listing of mining claims in the Mining Claim Recordation System (MCRS) database with locations given by meridian, township, range, and section. A mining claim is considered closed when the claim is relinquished or a formal BLM decision declaring the mining claim null and void has been issued and the appeal period has expired. All other mining claims filed with BLM are considered to be open and actively held. The digital map (figure 1.) with the mining claim density database available in this report are suitable for geographic information system (GIS)-based regional assessments at a scale of 1:100,000 or smaller.","language":"English","publisher":"U.S. Geological Survey","publisherLocation":"Reston, VA","doi":"10.3133/ofr99408","usgsCitation":"Hyndman, P.C., and Campbell, H.W., 1999, Digital mining claim density map for federal lands in Washington: 1996: U.S. Geological Survey Open-File Report 99-408, Report: 18 p., Readme, Metadata, Digital package, https://doi.org/10.3133/ofr99408.","productDescription":"Report: 18 p., Readme, Metadata, Digital package","numberOfPages":"18","costCenters":[{"id":312,"text":"Geology, Minerals, Energy, and Geophysics Science Center","active":true,"usgs":true}],"links":[{"id":165454,"rank":1,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/thumbnails/ofr99408.jpg"},{"id":3453,"rank":6,"type":{"id":15,"text":"Index Page"},"url":"https://pubs.usgs.gov/of/1999/0408/","linkFileType":{"id":5,"text":"html"}},{"id":284971,"rank":5,"type":{"id":20,"text":"Read Me"},"url":"https://pubs.usgs.gov/of/1999/0408/00readme.txt"},{"id":284973,"rank":2,"type":{"id":7,"text":"Companion Files"},"url":"https://pubs.usgs.gov/of/1999/0408/of99-408.tar.Z"},{"id":284972,"rank":4,"type":{"id":16,"text":"Metadata"},"url":"https://pubs.usgs.gov/of/1999/0408/WA_CLMS.MET"},{"id":284970,"rank":3,"type":{"id":11,"text":"Document"},"url":"https://pubs.usgs.gov/of/1999/0408/pdf/of99-408.pdf"}],"country":"United States","state":"Washington","geographicExtents":"{ \"type\": \"FeatureCollection\", \"features\": [ { \"type\": \"Feature\", \"properties\": {}, \"geometry\": { \"type\": \"Polygon\", \"coordinates\": [ [ [ -124.8361,45.5437 ], [ -124.8361,49.0024 ], [ -116.9174,49.0024 ], [ -116.9174,45.5437 ], [ -124.8361,45.5437 ] ] ] } } ] }","noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"53cd550ce4b0b290850f6196","contributors":{"authors":[{"text":"Hyndman, Paul C.","contributorId":88391,"corporation":false,"usgs":true,"family":"Hyndman","given":"Paul","email":"","middleInitial":"C.","affiliations":[],"preferred":false,"id":219027,"contributorType":{"id":1,"text":"Authors"},"rank":1},{"text":"Campbell, Harry W.","contributorId":67509,"corporation":false,"usgs":true,"family":"Campbell","given":"Harry","email":"","middleInitial":"W.","affiliations":[],"preferred":false,"id":219026,"contributorType":{"id":1,"text":"Authors"},"rank":2}]}} ,{"id":6813,"text":"fs17699 - 1999 - Seismograms live from around the world","interactions":[],"lastModifiedDate":"2014-04-03T11:22:01","indexId":"fs17699","displayToPublicDate":"2000-03-01T00:00:00","publicationYear":"1999","noYear":false,"publicationType":{"id":18,"text":"Report"},"publicationSubtype":{"id":5,"text":"USGS Numbered Series"},"seriesTitle":{"id":313,"text":"Fact Sheet","code":"FS","onlineIssn":"2327-6932","printIssn":"2327-6916","active":true,"publicationSubtype":{"id":5}},"seriesNumber":"176-99","title":"Seismograms live from around the world","docAbstract":"You can view earthquakes as they happen! Seismograms from seismic stations around the world are broadcast live, via the Internet, and are updated every 30 minutes, With an Internet connection and a web browser, you can view current seismograms and earthquake locations on your own computer. With special software also available via the Internet, you can obtain seismic data as it arrives from a global network of seismograph stations.","language":"English","publisher":"U.S. Geological Survey","doi":"10.3133/fs17699","usgsCitation":"Woodward, R.L., Shedlock, K.M., and Bolton, H.F., 1999, Seismograms live from around the world: U.S. Geological Survey Fact Sheet 176-99, 2 p., https://doi.org/10.3133/fs17699.","productDescription":"2 p.","numberOfPages":"2","costCenters":[],"links":[{"id":140865,"rank":0,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/thumbnails/fs17699.jpg"},{"id":285421,"type":{"id":11,"text":"Document"},"url":"https://pubs.usgs.gov/fs/0176-99/report.pdf"}],"noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"4f4e4a09e4b07f02db5fa86b","contributors":{"authors":[{"text":"Woodward, Robert L.","contributorId":92656,"corporation":false,"usgs":true,"family":"Woodward","given":"Robert","email":"","middleInitial":"L.","affiliations":[],"preferred":false,"id":153384,"contributorType":{"id":1,"text":"Authors"},"rank":1},{"text":"Shedlock, Kaye M.","contributorId":61788,"corporation":false,"usgs":true,"family":"Shedlock","given":"Kaye","email":"","middleInitial":"M.","affiliations":[],"preferred":false,"id":153383,"contributorType":{"id":1,"text":"Authors"},"rank":2},{"text":"Bolton, Harold F. bolton@usgs.gov","contributorId":4074,"corporation":false,"usgs":true,"family":"Bolton","given":"Harold","email":"bolton@usgs.gov","middleInitial":"F.","affiliations":[],"preferred":true,"id":153382,"contributorType":{"id":1,"text":"Authors"},"rank":3}]}} ,{"id":23472,"text":"ofr99217 - 1999 - Modifications to the diffusion analogy surface-water flow model (DAFLOW) for coupling to the modular finite-difference ground-water flow model (MODFLOW)","interactions":[],"lastModifiedDate":"2012-02-02T00:08:15","indexId":"ofr99217","displayToPublicDate":"2000-03-01T00:00:00","publicationYear":"1999","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":"99-217","title":"Modifications to the diffusion analogy surface-water flow model (DAFLOW) for coupling to the modular finite-difference ground-water flow model (MODFLOW)","language":"ENGLISH","publisher":"U.S. Dept. of the Interior, U.S. Geological Survey ;\r\nFederal Center,","doi":"10.3133/ofr99217","issn":"0094-9140","usgsCitation":"Jobson, H., and Harbaugh, A., 1999, Modifications to the diffusion analogy surface-water flow model (DAFLOW) for coupling to the modular finite-difference ground-water flow model (MODFLOW): U.S. Geological Survey Open-File Report 99-217, vi, 107 p. :ill. ;28 cm., https://doi.org/10.3133/ofr99217.","productDescription":"vi, 107 p. :ill. ;28 cm.","costCenters":[],"links":[{"id":156853,"rank":0,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/of/1999/0217/report-thumb.jpg"},{"id":52784,"rank":300,"type":{"id":11,"text":"Document"},"url":"https://pubs.usgs.gov/of/1999/0217/report.pdf","linkFileType":{"id":1,"text":"pdf"}}],"noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"4f4e4a0be4b07f02db5fbfbc","contributors":{"authors":[{"text":"Jobson, H.E.","contributorId":44952,"corporation":false,"usgs":true,"family":"Jobson","given":"H.E.","affiliations":[],"preferred":false,"id":190168,"contributorType":{"id":1,"text":"Authors"},"rank":1},{"text":"Harbaugh, A.W.","contributorId":15208,"corporation":false,"usgs":true,"family":"Harbaugh","given":"A.W.","email":"","affiliations":[],"preferred":false,"id":190167,"contributorType":{"id":1,"text":"Authors"},"rank":2}]}} ,{"id":32259,"text":"ofr998 - 1999 - Bedrock geologic map of the Windham quadrangle, Rockingham and Hillsborough counties, New Hampshire","interactions":[],"lastModifiedDate":"2022-03-29T21:19:47.650022","indexId":"ofr998","displayToPublicDate":"2000-03-01T00:00:00","publicationYear":"1999","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":"99-8","title":"Bedrock geologic map of the Windham quadrangle, Rockingham and Hillsborough counties, New Hampshire","docAbstract":"No abstract available.
","language":"English","publisher":"U.S. Geological Survey","doi":"10.3133/ofr998","usgsCitation":"Walsh, G., and Clark, S.F., 1999, Bedrock geologic map of the Windham quadrangle, Rockingham and Hillsborough counties, New Hampshire: U.S. Geological Survey Open-File Report 99-8, HTML Document, https://doi.org/10.3133/ofr998.","productDescription":"HTML Document","costCenters":[],"links":[{"id":161172,"rank":0,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/thumbnails/usgs_thumb.jpg"},{"id":397817,"rank":3,"type":{"id":36,"text":"NGMDB Index Page"},"url":"https://ngmdb.usgs.gov/Prodesc/proddesc_19246.htm"},{"id":3245,"rank":100,"type":{"id":15,"text":"Index Page"},"url":"https://pubs.usgs.gov/openfile/of99-8/","linkFileType":{"id":5,"text":"html"}}],"country":"United States","state":"New Hampshire","county":"Hillsborough County, Rockingham County","otherGeospatial":"Windham quadrangle","geographicExtents":"{\n \"type\": \"FeatureCollection\",\n \"features\": [\n {\n \"type\": \"Feature\",\n \"properties\": {},\n \"geometry\": {\n \"type\": \"Polygon\",\n \"coordinates\": [\n [\n [\n -71.375,\n 42.75\n ],\n [\n -71.25,\n 42.75\n ],\n [\n -71.25,\n 42.875\n ],\n [\n -71.375,\n 42.875\n ],\n [\n -71.375,\n 42.75\n ]\n ]\n ]\n }\n }\n ]\n}","noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"4f4e4a61e4b07f02db635d36","contributors":{"authors":[{"text":"Walsh, G. J. 0000-0003-4264-8836","orcid":"https://orcid.org/0000-0003-4264-8836","contributorId":47409,"corporation":false,"usgs":true,"family":"Walsh","given":"G. J.","affiliations":[],"preferred":false,"id":208094,"contributorType":{"id":1,"text":"Authors"},"rank":1},{"text":"Clark, S. F. Jr.","contributorId":32577,"corporation":false,"usgs":true,"family":"Clark","given":"S.","suffix":"Jr.","email":"","middleInitial":"F.","affiliations":[],"preferred":false,"id":208093,"contributorType":{"id":1,"text":"Authors"},"rank":2}]}} ,{"id":5490,"text":"fs03099 - 1999 - New Hampshire","interactions":[],"lastModifiedDate":"2012-02-02T00:05:41","indexId":"fs03099","displayToPublicDate":"2000-03-01T00:00:00","publicationYear":"1999","noYear":false,"publicationType":{"id":18,"text":"Report"},"publicationSubtype":{"id":5,"text":"USGS Numbered Series"},"seriesTitle":{"id":313,"text":"Fact Sheet","code":"FS","onlineIssn":"2327-6932","printIssn":"2327-6916","active":true,"publicationSubtype":{"id":5}},"seriesNumber":"030-99","title":"New Hampshire","language":"ENGLISH","publisher":"U.S. Geological Survey,","doi":"10.3133/fs03099","usgsCitation":"Water Resources Division, U.S. Geological Survey, 1999, New Hampshire: U.S. Geological Survey Fact Sheet 030-99, 1 folded sheet (4 p.) : col. ill., col. maps ; 28 cm. col. ill., col. maps ;, https://doi.org/10.3133/fs03099.","productDescription":"1 folded sheet (4 p.) : col. ill., col. maps ; 28 cm. col. ill., col. maps ;","costCenters":[],"links":[{"id":117621,"rank":0,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/thumbnails/fs_030_99.bmp"},{"id":669,"rank":100,"type":{"id":15,"text":"Index Page"},"url":"https://pubs.usgs.gov/FS/FS-030-99/","linkFileType":{"id":5,"text":"html"}}],"noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"4f4e4b24e4b07f02db6ae3fc","contributors":{"authors":[{"text":"Water Resources Division, U.S. Geological Survey","contributorId":128075,"corporation":true,"usgs":false,"organization":"Water Resources Division, U.S. Geological Survey","id":528612,"contributorType":{"id":1,"text":"Authors"},"rank":1}]}} ,{"id":5602,"text":"fs15499 - 1999 - Historical Mapping","interactions":[{"subject":{"id":5550,"text":"fs02494 - 1996 - Looking for an old map","indexId":"fs02494","publicationYear":"1996","noYear":false,"title":"Looking for an old map"},"predicate":"SUPERSEDED_BY","object":{"id":5602,"text":"fs15499 - 1999 - Historical Mapping","indexId":"fs15499","publicationYear":"1999","noYear":false,"title":"Historical Mapping"},"id":1},{"subject":{"id":47867,"text":"fs03494 - 1994 - Out-of-print maps","indexId":"fs03494","publicationYear":"1994","noYear":false,"title":"Out-of-print maps"},"predicate":"SUPERSEDED_BY","object":{"id":5602,"text":"fs15499 - 1999 - Historical Mapping","indexId":"fs15499","publicationYear":"1999","noYear":false,"title":"Historical Mapping"},"id":2}],"lastModifiedDate":"2012-02-29T17:02:31","indexId":"fs15499","displayToPublicDate":"2000-03-01T00:00:00","publicationYear":"1999","noYear":false,"publicationType":{"id":18,"text":"Report"},"publicationSubtype":{"id":5,"text":"USGS Numbered Series"},"seriesTitle":{"id":313,"text":"Fact Sheet","code":"FS","onlineIssn":"2327-6932","printIssn":"2327-6916","active":true,"publicationSubtype":{"id":5}},"seriesNumber":"154-99","title":"Historical Mapping","docAbstract":"Maps become out of date over time. Maps that are out of date, however, can be useful to historians, attorneys, environmentalists, genealogists, and others interested in researching the background of a particular area. Local historians can compare a series of maps of the same area compiled over a long period of time to learn how the area developed. A succession of such maps can provide a vivid picture of how a place changed over time.","language":"ENGLISH","publisher":"Geological Survey (U.S.)","doi":"10.3133/fs15499","usgsCitation":"Water Resources Division, U.S. Geological Survey, 1999, Historical Mapping (Supersedes FS-024-94 and FS-034-94): U.S. Geological Survey Fact Sheet 154-99, 2 p., https://doi.org/10.3133/fs15499.","productDescription":"2 p.","costCenters":[{"id":595,"text":"U.S. Geological Survey","active":false,"usgs":true}],"links":[{"id":388,"rank":100,"type":{"id":15,"text":"Index Page"},"url":"https://pubs.usgs.gov/fs/1999/0154/","linkFileType":{"id":5,"text":"html"}},{"id":121137,"rank":0,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/fs/1999/0154/report-thumb.jpg"},{"id":32113,"rank":300,"type":{"id":11,"text":"Document"},"url":"https://pubs.usgs.gov/fs/1999/0154/report.pdf","linkFileType":{"id":1,"text":"pdf"}}],"edition":"Supersedes FS-024-94 and FS-034-94","noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"4f4e4b23e4b07f02db6adeac","contributors":{"authors":[{"text":"Water Resources Division, U.S. Geological Survey","contributorId":128075,"corporation":true,"usgs":false,"organization":"Water Resources Division, U.S. Geological Survey","id":528684,"contributorType":{"id":1,"text":"Authors"},"rank":1}]}} ,{"id":23090,"text":"ofr9994 - 1999 - Methods of analysis by the U.S. Geological Survey National Water Quality Laboratory-Comparison of a nitric acid in-bottle digestion procedure to other whole-water digestion procedures","interactions":[],"lastModifiedDate":"2021-05-28T16:47:12.720319","indexId":"ofr9994","displayToPublicDate":"2000-03-01T00:00:00","publicationYear":"1999","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":"99-94","title":"Methods of analysis by the U.S. Geological Survey National Water Quality Laboratory-Comparison of a nitric acid in-bottle digestion procedure to other whole-water digestion procedures","docAbstract":"A hydrochloric acid in-bottle digestion\r\nprocedure is used to partially digest wholewater\r\nsamples prior to determining\r\nrecoverable elements by various analytical\r\nmethods. The use of hydrochloric acid is\r\nproblematic for some methods of analysis\r\nbecause of spectral interference. The inbottle\r\ndigestion procedure has been\r\nmodified to eliminate such interference by\r\nusing nitric acid instead of hydrochloric acid\r\nin the digestion. Implications of this\r\nmodification are evaluated by comparing\r\nresults for a series of synthetic whole-water\r\nsamples. Results are also compared with\r\nthose obtained by using U.S. Environmental\r\nProtection Agency (1994) (USEPA) Method\r\n200.2 total-recoverable digestion procedure.\r\nPercentage yields that use the nitric acid inbottle\r\ndigestion procedure are within 10\r\npercent of the hydrochloric acid in-bottle\r\nyields for 25 of the 26 elements determined\r\nin two of the three synthetic whole-water\r\nsamples tested. Differences in percentage\r\nyields for the third synthetic whole-water\r\nsample were greater than 10 percent for 16\r\nof the 26 elements determined. The USEPA\r\nmethod was the most rigorous for\r\nsolubilizing elements from particulate matter\r\nin all three synthetic whole-water samples.\r\nNevertheless, the variability in the\r\npercentage yield by using the USEPA\r\ndigestion procedure was generally greater than\r\nthe in-bottle digestion procedure, presumably\r\nbecause of the difficulty in controlling the\r\ndigestion conditions accurately.","language":"English","publisher":"U.S. Dept. of the Interior, U.S. Geological Survey :\r\nBranch of Information Services [distributor],","doi":"10.3133/ofr9994","usgsCitation":"Garbarino, J.R., and Hoffman, G.L., 1999, Methods of analysis by the U.S. Geological Survey National Water Quality Laboratory-Comparison of a nitric acid in-bottle digestion procedure to other whole-water digestion procedures: U.S. Geological Survey Open-File Report 99-94, vi, 21 p., https://doi.org/10.3133/ofr9994.","productDescription":"vi, 21 p.","costCenters":[{"id":452,"text":"National Water Quality Laboratory","active":true,"usgs":true}],"links":[{"id":1507,"rank":100,"type":{"id":15,"text":"Index Page"},"url":"https://nwql.usgs.gov/Public/pubs/OFR99-094.html","linkFileType":{"id":5,"text":"html"}},{"id":52460,"rank":300,"type":{"id":11,"text":"Document"},"url":"https://pubs.usgs.gov/of/1999/0094/report.pdf","linkFileType":{"id":1,"text":"pdf"}},{"id":157063,"rank":0,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/of/1999/0094/report-thumb.jpg"}],"noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"4f4e4a54e4b07f02db62bb90","contributors":{"authors":[{"text":"Garbarino, John R. jrgarb@usgs.gov","contributorId":2189,"corporation":false,"usgs":true,"family":"Garbarino","given":"John","email":"jrgarb@usgs.gov","middleInitial":"R.","affiliations":[{"id":5046,"text":"Branch of Analytical Serv (NWQL)","active":true,"usgs":true}],"preferred":true,"id":189415,"contributorType":{"id":1,"text":"Authors"},"rank":1},{"text":"Hoffman, Gerald L.","contributorId":89172,"corporation":false,"usgs":true,"family":"Hoffman","given":"Gerald","email":"","middleInitial":"L.","affiliations":[],"preferred":false,"id":189416,"contributorType":{"id":1,"text":"Authors"},"rank":2}]}} ,{"id":5019,"text":"fs14999 - 1999 - Bottom sediments of Lorence Creek Lake, San Antonio, Texas, reflect contaminant trends in an urbanizing watershed","interactions":[],"lastModifiedDate":"2016-08-19T14:14:52","indexId":"fs14999","displayToPublicDate":"2000-03-01T00:00:00","publicationYear":"1999","noYear":false,"publicationType":{"id":18,"text":"Report"},"publicationSubtype":{"id":5,"text":"USGS Numbered Series"},"seriesTitle":{"id":313,"text":"Fact Sheet","code":"FS","onlineIssn":"2327-6932","printIssn":"2327-6916","active":true,"publicationSubtype":{"id":5}},"seriesNumber":"149-99","title":"Bottom sediments of Lorence Creek Lake, San Antonio, Texas, reflect contaminant trends in an urbanizing watershed","docAbstract":"Historical use of pesticides and rapid urbanization have left their mark on the chemistry of bottom sediments in Lorence Creek Lake (fig. 1) in the northern part of San Antonio, Tex. Several metals, organochlorine compounds (pesticides and polychlorinated biphenyls [PCBs]), and polycyclic aromatic hydrocarbons (PAHs) detected in bottom sediments of the lake have temporal trends indicating anthropogenic (human) sources. Lorence Creek Lake is not unique; the same metals and organic compounds are routinely found in lake sediments in urbanizing watersheds (Van Metre and Callender, in press).
","language":"English","publisher":"U.S. Geological Survey","doi":"10.3133/fs14999","usgsCitation":"Ging, P.B., Van Metre, P., and Callender, E., 1999, Bottom sediments of Lorence Creek Lake, San Antonio, Texas, reflect contaminant trends in an urbanizing watershed: U.S. Geological Survey Fact Sheet 149-99, 4 p., https://doi.org/10.3133/fs14999.","productDescription":"4 p.","onlineOnly":"N","additionalOnlineFiles":"N","costCenters":[{"id":583,"text":"Texas Water Science Center","active":true,"usgs":true}],"links":[{"id":117793,"rank":0,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/thumbnails/fs_149_99.bmp"},{"id":264,"rank":100,"type":{"id":15,"text":"Index Page"},"url":"https://pubs.usgs.gov/FS/Fs14999","linkFileType":{"id":5,"text":"html"}},{"id":327094,"rank":101,"type":{"id":11,"text":"Document"},"url":"https://pubs.usgs.gov/fs/Fs14999/14999.pdf"}],"noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"4f4e4a14e4b07f02db602752","contributors":{"authors":[{"text":"Ging, Patricia B. 0000-0001-5491-8448 pbging@usgs.gov","orcid":"https://orcid.org/0000-0001-5491-8448","contributorId":1788,"corporation":false,"usgs":true,"family":"Ging","given":"Patricia","email":"pbging@usgs.gov","middleInitial":"B.","affiliations":[{"id":583,"text":"Texas Water Science Center","active":true,"usgs":true}],"preferred":true,"id":150298,"contributorType":{"id":1,"text":"Authors"},"rank":1},{"text":"Van Metre, P. C.","contributorId":92999,"corporation":false,"usgs":true,"family":"Van Metre","given":"P. C.","affiliations":[],"preferred":false,"id":150300,"contributorType":{"id":1,"text":"Authors"},"rank":2},{"text":"Callender, Edward","contributorId":69535,"corporation":false,"usgs":true,"family":"Callender","given":"Edward","affiliations":[],"preferred":false,"id":150299,"contributorType":{"id":1,"text":"Authors"},"rank":3}]}} ,{"id":60292,"text":"mf2330 - 1999 - Bituminous coal production in the Appalachian Basin: Past, present, and future","interactions":[],"lastModifiedDate":"2022-10-12T20:42:01.657828","indexId":"mf2330","displayToPublicDate":"2000-03-01T00:00:00","publicationYear":"1999","noYear":false,"publicationType":{"id":18,"text":"Report"},"publicationSubtype":{"id":5,"text":"USGS Numbered Series"},"seriesTitle":{"id":325,"text":"Miscellaneous Field Studies Map","code":"MF","active":false,"publicationSubtype":{"id":5}},"seriesNumber":"2330","title":"Bituminous coal production in the Appalachian Basin: Past, present, and future","docAbstract":"This report on Appalachian basin coal production consists of four maps and associated graphs and tables, with links to the basic data that were used to construct the maps. Plate 1 shows the time (year) of maximum coal production, by county. For illustration purposes, the years of maximum production are grouped into decadal units. Plate 2 shows the amount of coal produced (tons) during the year of maximum coal production for each county. Plate 3 illustrates the cumulative coal production (tons) for each county since about the beginning of the 20th century. Plate 4 shows 1996 annual production by county. During the current (third) cycle of coal production in the Appalachian basin, only seven major coal-producing counties (those with more than 500 million tons cumulative production), including Greene County, Pa.; Boone, Kanawha, Logan, Mingo, and Monongalia Counties, W.Va.; and Pike County, Ky., exhibit a general increase in coal production. Other major coal-producing counties have either declined to a small percentage of their maximum production or are annually maintaining a moderate level of production. In general, the areas with current high coal production have large blocks of coal that are suitable for mining underground with highly efficient longwall methods, or are occupied by very large scale, relatively low cost surface mining operations. The estimated cumulative production for combined bituminous and anthracite coal is about 100 billion tons or less for the Appalachian basin. In general, it is anticipated that the remaining resources will be progressively of lower quality, will cost more to mine, and will become economical only as new technologies for extraction, beneficiation, and consumption are developed, and then only if prices for coal increase.","language":"English","publisher":"U.S. Geological Survey","doi":"10.3133/mf2330","usgsCitation":"Milici, R.C., 1999, Bituminous coal production in the Appalachian Basin: Past, present, and future (Online version 1.0): U.S. Geological Survey Miscellaneous Field Studies Map 2330, HTML Document, https://doi.org/10.3133/mf2330.","productDescription":"HTML Document","costCenters":[],"links":[{"id":109906,"rank":700,"type":{"id":36,"text":"NGMDB Index Page"},"url":"https://ngmdb.usgs.gov/Prodesc/proddesc_23427.htm","linkFileType":{"id":5,"text":"html"},"description":"23427"},{"id":6022,"rank":100,"type":{"id":15,"text":"Index Page"},"url":"https://pubs.usgs.gov/mf-maps/mf-2330/","linkFileType":{"id":5,"text":"html"}},{"id":183603,"rank":0,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/thumbnails/usgs_thumb.jpg"}],"scale":"250000","country":"United States","otherGeospatial":"Appalachian Basin","geographicExtents":"{\n \"type\": \"FeatureCollection\",\n \"features\": [\n {\n \"type\": \"Feature\",\n \"properties\": {},\n \"geometry\": {\n \"type\": \"Polygon\",\n \"coordinates\": [\n [\n [\n -88.333,\n 32.633\n ],\n [\n -76.867,\n 32.633\n ],\n [\n -76.867,\n 41.817\n ],\n [\n -88.333,\n 41.817\n ],\n [\n -88.333,\n 32.633\n ]\n ]\n ]\n }\n }\n ]\n}","edition":"Online version 1.0","noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"4f4e49e5e4b07f02db5e6fed","contributors":{"authors":[{"text":"Milici, R. C.","contributorId":58688,"corporation":false,"usgs":true,"family":"Milici","given":"R.","email":"","middleInitial":"C.","affiliations":[],"preferred":false,"id":263460,"contributorType":{"id":1,"text":"Authors"},"rank":1}]}} ,{"id":29545,"text":"wri984257 - 1999 - Potential for advection of volatile organic compounds in ground water to the Cochato River, Baird & McGuire Superfund Site, Holbrook, Massachusetts, March and April 1998","interactions":[],"lastModifiedDate":"2017-10-17T15:00:37","indexId":"wri984257","displayToPublicDate":"2000-03-01T00:00:00","publicationYear":"1999","noYear":false,"publicationType":{"id":18,"text":"Report"},"publicationSubtype":{"id":5,"text":"USGS Numbered Series"},"seriesTitle":{"id":342,"text":"Water-Resources Investigations Report","code":"WRI","active":false,"publicationSubtype":{"id":5}},"seriesNumber":"98-4257","title":"Potential for advection of volatile organic compounds in ground water to the Cochato River, Baird & McGuire Superfund Site, Holbrook, Massachusetts, March and April 1998","docAbstract":"In March and April 1998, a network of water-to-vapor diffusion samplers was installed along the Cochato River at the Baird & McGuire Superfund Site in Holbrook, Massachusetts, where a plume of volatile organic compounds (VOCs) is present in ground water. The purpose of installing the sampler network was to determine if VOCs were present in river-bottom sediments while a ground-water extraction system was operating and after the system had been shut down for two weeks. Water-to-water diffusion samplers placed at selected locations provided supplemental information about concentrations of VOCs in pore water in the river-bottom sediments. Water levels in piezometers and river stage were measured concurrently to determine if ground water was discharging to the river.
Benzene, toluene, ethylbenzene and xylenes (BTEX compounds) were detected in water-tovapor and water-to-water diffusion samplers located in the area where the plume is known to pass beneath the river for both pumping and nonpumping conditions. Concentrations of total BTEX compounds in water-to-vapor diffusion samplers ranged from non-detect upriver and downriver from the plume area to greater than 200 parts per million by volume in the plume area. Concentrations of total BTEX compounds were not significantly different for pumping than for non-pumping conditions. Concentrations of total BTEX compounds in water-to-water diffusion samplers ranged from non-detect to 680 micrograms per liter. The limited number of water-to-water diffusion samplers did not indicate that concentrations were higher for pumping or non-pumping conditions. Trichloroethylene and tetrachloroethylene also were detected in water-to-vapor diffusion samplers downriver from the area where the BTEX compounds were detected. Water levels in four piezometers were consistently higher than the river stage, indicating an upward hydraulic gradient and ground-water discharge to the river. The concentrations of VOCs in riverbottom sediments and the upward hydraulic gradients observed indicate that contaminants from the Baird & McGuire ground-water plume were discharging to the Cochato River during the study period for both pumping and non-pumping conditions.
","language":"English","publisher":"U.S. Geological Survey","doi":"10.3133/wri984257","collaboration":"Prepared in cooperation with the U.S. Army Corps of Engineers and U.S. Environmental Protection Agency","usgsCitation":"Savoie, J., Lyford, F.P., and Clifford, S., 1999, Potential for advection of volatile organic compounds in ground water to the Cochato River, Baird & McGuire Superfund Site, Holbrook, Massachusetts, March and April 1998: U.S. Geological Survey Water-Resources Investigations Report 98-4257, Report: iv, 19 p.; Plate: 30.85 x 21.21 inches, https://doi.org/10.3133/wri984257.","productDescription":"Report: iv, 19 p.; Plate: 30.85 x 21.21 inches","costCenters":[],"links":[{"id":290199,"type":{"id":17,"text":"Plate"},"url":"https://pubs.usgs.gov/wri/1998/4257/plate-1.pdf","linkFileType":{"id":1,"text":"pdf"}},{"id":290200,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/wri/1998/4257/report-thumb.jpg"},{"id":346720,"rank":3,"type":{"id":11,"text":"Document"},"url":"https://pubs.usgs.gov/wri/1998/4257/report.pdf","linkFileType":{"id":1,"text":"pdf"}}],"country":"United States","state":"Massachusetts","city":"Holbrook","otherGeospatial":"Cochato River","geographicExtents":"{ \"type\": \"FeatureCollection\", \"features\": [ { \"type\": \"Feature\", \"properties\": {}, \"geometry\": { \"type\": \"Polygon\", \"coordinates\": [ [ [ -71.027062,42.149166 ], [ -71.027062,42.153542 ], [ -71.022276,42.153542 ], [ -71.022276,42.149166 ], [ -71.027062,42.149166 ] ] ] } } ] }","noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"4f4e4ad5e4b07f02db68384f","contributors":{"authors":[{"text":"Savoie, Jennifer G.","contributorId":52218,"corporation":false,"usgs":true,"family":"Savoie","given":"Jennifer G.","affiliations":[],"preferred":false,"id":201695,"contributorType":{"id":1,"text":"Authors"},"rank":1},{"text":"Lyford, Forest P.","contributorId":43334,"corporation":false,"usgs":true,"family":"Lyford","given":"Forest","email":"","middleInitial":"P.","affiliations":[],"preferred":false,"id":201694,"contributorType":{"id":1,"text":"Authors"},"rank":2},{"text":"Clifford, Scott","contributorId":63042,"corporation":false,"usgs":true,"family":"Clifford","given":"Scott","email":"","affiliations":[],"preferred":false,"id":201696,"contributorType":{"id":1,"text":"Authors"},"rank":3}]}} ,{"id":26555,"text":"wri984233 - 1999 - Geology and ground-water resources of the Lawrenceville area, Georgia","interactions":[],"lastModifiedDate":"2022-03-28T18:47:58.827142","indexId":"wri984233","displayToPublicDate":"2000-03-01T00:00:00","publicationYear":"1999","noYear":false,"publicationType":{"id":18,"text":"Report"},"publicationSubtype":{"id":5,"text":"USGS Numbered Series"},"seriesTitle":{"id":342,"text":"Water-Resources Investigations Report","code":"WRI","active":false,"publicationSubtype":{"id":5}},"seriesNumber":"98-4233","title":"Geology and ground-water resources of the Lawrenceville area, Georgia","docAbstract":"The population of the Atlanta Metropolitan area continues to grow at a rapid pace and the demand for water supplies steadily increases. Exploration for ground-water resources, as a supplement to surface-water supplies, is being undertaken by many city and county governments. The application of effective investigative methods to characterization of the complex igneous and metamorphic fractured bedrock aquifers of the Piedmont physiographic province is essential to the success of these ground-water exploration programs. The U.S. Geological Survey, in cooperation with the City of Lawrenceville, Ga., began a study in December 1994 to apply various investigative techniques for field characterization of fractured crystalline-bedrock aquifers near Lawrenceville.\r\n\r\nFive major lithologic units were mapped in the Lawrenceville, Ga., area as part of an ongoing study of ground-water resources-amphibolite, biotite gneiss, button schist, granite gneiss, and quartzite/aluminous schist. These units generally are thin in outcrop width, have low angles of dip (nearly 0 to 20 degrees, dip reversals occur over short distances), and exhibit some shearing characteristics. The most productive unit for ground-water resources, on the basis of subsurface data collected through 1997, is the amphibolite. Historically, two wells drilled into this unit are recognized as having possibly the highest yields in the Piedmont region of northern Georgia. The City of Lawrenceville refurbished one well at the Rhodes Jordan Wellfield in 1990, and has pumped this well at an average rate of about 230 gallons per minute since 1995. In general, the composition of water collected from the bedrock wells, regolith wells, and City Lake is similar; calcium and bicarbonate are the dominant cation and anion, respectively. Water from the regolith wells and the lake have lower concentrations of major ions than does water from the bedrock wells. Many of the ground-water samples collected from the Rhodes Jordan Wellfield during October-November 1995, and from the wellfield and three additional observation well sites during August 1996, contain volatile organic compounds. Volatile organic compounds were detected in ground-water samples collected from several bedrock and regolith wells located in urban areas. Trace concentrations of tetrachloroethylene, trichloroethylene, 1,1-dichloroethane, trichlorofluoromethane, 1,1,1-trichloroethane, and cis-1,2-dichloroethene were detected. Methyl-tert-butyl ether (MTBE)-a compound used to increase the octane level in gasoline-was detected at concentrations above expected urban background levels in bedrock wells in the Rhodes Jordan Wellfield. Concentrations of MTBE ranged from 0.6 to 12 micrograms per liter in October-November 1995, and from 0.6 to 26 micrograms per liter in August 1996.\r\n\r\nContinuous ground-water-level data suggest that the fractured crystalline-bedrock aquifer (amphibolite unit) at the Rhodes Jordan Wellfield, generally is dewatered to a depth near a productive fracture during the regular pumping cycle of 18 hours per day, 5 days on and 2 days off per week. However, when the stress on the aquifer is increased by extending the pumping period up to as much as 18 days, or by pumping longer that 18 hours per day, the aquifer exhibits an unusual condition of recovery. Areal effects of pumping have been observed at distances of as much as one mile, extending across surface-water drainage divides.","language":"English","publisher":"U.S. Geological Survey","doi":"10.3133/wri984233","usgsCitation":"Chapman, M.J., Crawford, T.J., and Tharpe, W.T., 1999, Geology and ground-water resources of the Lawrenceville area, Georgia: U.S. Geological Survey Water-Resources Investigations Report 98-4233, Report: v, 46 p.; 2 Plates; 36.00 × 22.00 inches, https://doi.org/10.3133/wri984233.","productDescription":"Report: v, 46 p.; 2 Plates; 36.00 × 22.00 inches","costCenters":[{"id":13634,"text":"South Atlantic Water Science Center","active":true,"usgs":true}],"links":[{"id":397732,"rank":3,"type":{"id":36,"text":"NGMDB Index Page"},"url":"https://ngmdb.usgs.gov/Prodesc/proddesc_18959.htm"},{"id":9247,"rank":100,"type":{"id":15,"text":"Index Page"},"url":"https://pubs.usgs.gov/wri/wri984233/","linkFileType":{"id":5,"text":"html"}},{"id":157313,"rank":0,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/thumbnails/usgs_thumb.jpg"}],"country":"United States","state":"Georgia","city":"Lawrenceville","geographicExtents":"{\n \"type\": \"FeatureCollection\",\n \"features\": [\n {\n \"type\": \"Feature\",\n \"properties\": {},\n \"geometry\": {\n \"type\": \"Polygon\",\n \"coordinates\": [\n [\n [\n -84.26239013671875,\n 33.80596747503222\n ],\n [\n -84.26239013671875,\n 34.09872793958119\n ],\n [\n -83.79959106445312,\n 34.09872793958119\n ],\n [\n -83.79959106445312,\n 33.80596747503222\n ],\n [\n -84.26239013671875,\n 33.80596747503222\n ]\n ]\n ]\n }\n }\n ]\n}","noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"4f4e4adae4b07f02db68550b","contributors":{"authors":[{"text":"Chapman, Melinda J. 0000-0003-4021-0320 mjchap@usgs.gov","orcid":"https://orcid.org/0000-0003-4021-0320","contributorId":1597,"corporation":false,"usgs":true,"family":"Chapman","given":"Melinda","email":"mjchap@usgs.gov","middleInitial":"J.","affiliations":[{"id":493,"text":"Office of Ground Water","active":true,"usgs":true},{"id":476,"text":"North Carolina Water Science Center","active":true,"usgs":true}],"preferred":true,"id":196606,"contributorType":{"id":1,"text":"Authors"},"rank":1},{"text":"Crawford, Thomas J.","contributorId":73640,"corporation":false,"usgs":true,"family":"Crawford","given":"Thomas","email":"","middleInitial":"J.","affiliations":[],"preferred":false,"id":196607,"contributorType":{"id":1,"text":"Authors"},"rank":2},{"text":"Tharpe, W. Todd","contributorId":74413,"corporation":false,"usgs":true,"family":"Tharpe","given":"W.","email":"","middleInitial":"Todd","affiliations":[],"preferred":false,"id":196608,"contributorType":{"id":1,"text":"Authors"},"rank":3}]}} ,{"id":6549,"text":"fs11599 - 1999 - Coal Resource Assessments in the Northern and Central Appalachian Coal Region","interactions":[],"lastModifiedDate":"2012-02-02T00:05:58","indexId":"fs11599","displayToPublicDate":"2000-03-01T00:00:00","publicationYear":"1999","noYear":false,"publicationType":{"id":18,"text":"Report"},"publicationSubtype":{"id":5,"text":"USGS Numbered Series"},"seriesTitle":{"id":313,"text":"Fact Sheet","code":"FS","onlineIssn":"2327-6932","printIssn":"2327-6916","active":true,"publicationSubtype":{"id":5}},"seriesNumber":"115-99","title":"Coal Resource Assessments in the Northern and Central Appalachian Coal Region","language":"ENGLISH","publisher":"U.S. Geological Survey,","doi":"10.3133/fs11599","usgsCitation":"Water Resources Division, U.S. Geological Survey, 1999, Coal Resource Assessments in the Northern and Central Appalachian Coal Region: U.S. Geological Survey Fact Sheet 115-99, 4 p., https://doi.org/10.3133/fs11599.","productDescription":"4 p.","costCenters":[],"links":[{"id":117704,"rank":0,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/thumbnails/fs_115_99.bmp"},{"id":831,"rank":100,"type":{"id":15,"text":"Index Page"},"url":"https://pubs.usgs.gov/factsheet/fs115-99","linkFileType":{"id":5,"text":"html"}}],"noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"4f4e49d6e4b07f02db5de04f","contributors":{"authors":[{"text":"Water Resources Division, U.S. Geological Survey","contributorId":128075,"corporation":true,"usgs":false,"organization":"Water Resources Division, U.S. Geological Survey","id":528713,"contributorType":{"id":1,"text":"Authors"},"rank":1}]}} ,{"id":5404,"text":"fs04499 - 1999 - Tennessee","interactions":[],"lastModifiedDate":"2012-02-02T00:05:51","indexId":"fs04499","displayToPublicDate":"2000-03-01T00:00:00","publicationYear":"1999","noYear":false,"publicationType":{"id":18,"text":"Report"},"publicationSubtype":{"id":5,"text":"USGS Numbered Series"},"seriesTitle":{"id":313,"text":"Fact Sheet","code":"FS","onlineIssn":"2327-6932","printIssn":"2327-6916","active":true,"publicationSubtype":{"id":5}},"seriesNumber":"044-99","title":"Tennessee","language":"ENGLISH","publisher":"U.S. Geological Survey,","doi":"10.3133/fs04499","usgsCitation":"Water Resources Division, U.S. Geological Survey, 1999, Tennessee: U.S. Geological Survey Fact Sheet 044-99, 1 folded page ([4] p.) : col. ill., col. map ; 28 x 44 cm. folded to 28 x 22 cm. col. ill., col. map ;, https://doi.org/10.3133/fs04499.","productDescription":"1 folded page ([4] p.) : col. ill., col. map ; 28 x 44 cm. folded to 28 x 22 cm. col. ill., col. map ;","costCenters":[],"links":[{"id":117136,"rank":0,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/thumbnails/fs_044_99.bmp"},{"id":519,"rank":100,"type":{"id":15,"text":"Index Page"},"url":"https://pubs.usgs.gov/FS/FS-044-99/","linkFileType":{"id":5,"text":"html"}}],"noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"4f4e4ad9e4b07f02db6851c4","contributors":{"authors":[{"text":"Water Resources Division, U.S. Geological Survey","contributorId":128075,"corporation":true,"usgs":false,"organization":"Water Resources Division, U.S. Geological Survey","id":528560,"contributorType":{"id":1,"text":"Authors"},"rank":1}]}} ,{"id":24111,"text":"ofr99243 - 1999 - Stream and aquifer biology of south-central Texas — A literature review, 1973-97","interactions":[],"lastModifiedDate":"2021-12-14T20:30:11.944529","indexId":"ofr99243","displayToPublicDate":"2000-03-01T00:00:00","publicationYear":"1999","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":"99-243","title":"Stream and aquifer biology of south-central Texas — A literature review, 1973-97","docAbstract":"This report summarizes in table format 32 aquatic vertebrate (primarily fish), 54 aquatic invertebrate, and 13 aquatic plant studies available for the area of the South-Central Texas study unit of the U.S. Geological Survey National Water-Quality Assessment. The studies, published mostly during 1973–97, pertain to the Guadalupe, San Antonio, and Nueces River Basins, the San Antonio-Nueces and Nueces-Rio Grande Coastal Basins, and the Edwards aquifer where it underlies the upper parts of the three river basins. The biology of the study-unit streams is determined mostly by the characteristics of the ecoregions they transect—the Edwards Plateau, Texas Blackland Prairies, East Central Texas Plains, Western Gulf Coastal Plain, and Southern Texas Plains.
About 20 percent of the previous fish and invertebrate studies and about 75 percent of the aquatic plant surveys have centered on Comal Springs in Comal County and San Marcos Springs in Hays County. Although several important studies are available for the San Antonio region, documentation of aquatic biology for the remainder of the study unit is relatively sparse. The streams in the study unit, particularly in the Edwards Plateau, support three dominant biological groups—fish, aquatic invertebrates, and plants. Potential threats to these organisms include impoundments and flood-control projects, siltation from erosion, ground-water pumping, recreational activities, wastewater discharge, and introduction of non-native species. More than 30 non-native fish, invertebrate, and plant species have been introduced into the region. Of the 19 aquatic species Federally listed as endangered or threatened in Texas, 8 are associated with springs and spring runs in the study unit. All of the endangered species in the study unit are associated with springs and spring runs.
A large number of endemic species in the study unit are associated with subterranean aquatic ecosystems, most likely a consequence of the unique proximity of the varied topographic and hydrologic conditions of the area and of the geological development of the Edwards aquifer. Ninety-one endemics, including 44 species found solely underground, are associated with the aquatic ecosystems (including springs) of the Edwards aquifer.
","language":"English","publisher":"U.S. Geological Survey","doi":"10.3133/ofr99243","issn":"0094-9140","usgsCitation":"Ourso, R.T., and Hornig, C., 1999, Stream and aquifer biology of south-central Texas — A literature review, 1973-97: U.S. Geological Survey Open-File Report 99-243, vi, 38 p., https://doi.org/10.3133/ofr99243.","productDescription":"vi, 38 p.","costCenters":[{"id":583,"text":"Texas Water Science Center","active":true,"usgs":true}],"links":[{"id":1772,"rank":100,"type":{"id":15,"text":"Index Page"},"url":"https://pubs.water.usgs.gov/ofr99-243","linkFileType":{"id":5,"text":"html"}},{"id":156342,"rank":0,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/thumbnails/usgs_thumb.jpg"},{"id":392880,"rank":3,"type":{"id":36,"text":"NGMDB Index Page"},"url":"https://ngmdb.usgs.gov/Prodesc/proddesc_22916.htm"}],"country":"United States","state":"Texas","geographicExtents":"{\n \"type\": \"FeatureCollection\",\n \"features\": [\n {\n \"type\": \"Feature\",\n \"properties\": {},\n \"geometry\": {\n \"type\": \"Polygon\",\n \"coordinates\": [\n [\n [\n -102.5,\n 27.567\n ],\n [\n -98.617,\n 27.567\n ],\n [\n -98.617,\n 30.183\n ],\n [\n -102.5,\n 30.183\n ],\n [\n -102.5,\n 27.567\n ]\n ]\n ]\n }\n }\n ]\n}","noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"4f4e4b16e4b07f02db6a51db","contributors":{"authors":[{"text":"Ourso, Robert T. 0000-0002-5952-8681 rtourso@usgs.gov","orcid":"https://orcid.org/0000-0002-5952-8681","contributorId":203207,"corporation":false,"usgs":true,"family":"Ourso","given":"Robert","email":"rtourso@usgs.gov","middleInitial":"T.","affiliations":[{"id":120,"text":"Alaska Science Center Water","active":true,"usgs":true},{"id":114,"text":"Alaska Science Center","active":true,"usgs":true}],"preferred":true,"id":191333,"contributorType":{"id":1,"text":"Authors"},"rank":1},{"text":"Hornig, C. E.","contributorId":100423,"corporation":false,"usgs":true,"family":"Hornig","given":"C. E.","affiliations":[],"preferred":false,"id":191334,"contributorType":{"id":1,"text":"Authors"},"rank":2}]}} ,{"id":22899,"text":"ofr99213 - 1999 - Index of hydrologic characteristics and data resources for the Gwynns Falls watershed, Baltimore County and Baltimore City, Maryland","interactions":[],"lastModifiedDate":"2021-12-02T19:58:06.583871","indexId":"ofr99213","displayToPublicDate":"2000-03-01T00:00:00","publicationYear":"1999","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":"99-213","title":"Index of hydrologic characteristics and data resources for the Gwynns Falls watershed, Baltimore County and Baltimore City, Maryland","docAbstract":"The Gwynns Falls watershed has been selected as the primary study area for the Baltimore Ecosystem Study, as part of the National Science Foundation?s Long-Term Ecological Research program. Because the Baltimore Ecosystem Study will be investigating long-term hydrologic changes in the Gwynns Falls watershed, a compilation of existing data resources for the watershed is necessary. \r\n\r\nThis report discusses hydrologic characteristics and presents a compilation of historical data resources for the Gwynns Falls watershed. Tables are presented that list active and discontinued continuous-record streamflow-gaging stations, nontidal crest-stage partial-record stations, low-flow partial-record stations, and water-quality partial-record stations operated by the U.S. Geological Survey, Maryland-Delaware-D. C. District, in the Gwynns Falls watershed. Statistics regarding the number of inventoried ground-water wellsin or bordering the Gwynns Falls watershed also are presented. A summary of additional data resources for the Gwynns Falls watershed is provided. This includes (1) an inventory of selected U.S. Geological Survey studies and reports that contain historical data or basin characteristics for streams in the watershed, (2) a listing of indirect flood-discharge measurements that have been made at several monitoring stations in the watershed, (3) a brief discussion of channel-stability and bridge-scour data collected by the U.S. Geological Survey in the watershed during 1990?95, (4) a listing of climatological data stations in the watershed and in the surrounding regional area, and (5) a listing of other selected reports that include data or information on the Gwynns Falls watershed.","language":"English","publisher":"U.S. Geological Survey","doi":"10.3133/ofr99213","issn":"0094-9140","usgsCitation":"Doheny, E.J., 1999, Index of hydrologic characteristics and data resources for the Gwynns Falls watershed, Baltimore County and Baltimore City, Maryland: U.S. Geological Survey Open-File Report 99-213, iv, 17 p., https://doi.org/10.3133/ofr99213.","productDescription":"iv, 17 p.","costCenters":[],"links":[{"id":154213,"rank":0,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/thumbnails/usgs_thumb.jpg"},{"id":1362,"rank":100,"type":{"id":15,"text":"Index Page"},"url":"https://pubs.water.usgs.gov/ofr99-213/","linkFileType":{"id":5,"text":"html"}},{"id":392398,"rank":2,"type":{"id":36,"text":"NGMDB Index Page"},"url":"https://ngmdb.usgs.gov/Prodesc/proddesc_22763.htm"}],"country":"United States","state":"Maryland","county":"Baltimore County","city":"Baltimore","otherGeospatial":"Gwynns Falls watershed","geographicExtents":"{\n \"type\": \"FeatureCollection\",\n \"features\": [\n {\n \"type\": \"Feature\",\n \"properties\": {},\n \"geometry\": {\n \"type\": \"Polygon\",\n \"coordinates\": [\n [\n [\n -77.04711914062499,\n 39.193948213963665\n ],\n [\n -76.5802001953125,\n 39.193948213963665\n ],\n [\n -76.5802001953125,\n 39.68182601089365\n ],\n [\n -77.04711914062499,\n 39.68182601089365\n ],\n [\n -77.04711914062499,\n 39.193948213963665\n ]\n ]\n ]\n }\n }\n ]\n}","noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"4f4e49dbe4b07f02db5e0ddc","contributors":{"authors":[{"text":"Doheny, Edward J. 0000-0002-6043-3241 ejdoheny@usgs.gov","orcid":"https://orcid.org/0000-0002-6043-3241","contributorId":4495,"corporation":false,"usgs":true,"family":"Doheny","given":"Edward","email":"ejdoheny@usgs.gov","middleInitial":"J.","affiliations":[{"id":374,"text":"Maryland Water Science Center","active":true,"usgs":true}],"preferred":false,"id":189098,"contributorType":{"id":1,"text":"Authors"},"rank":1}]}} ,{"id":22185,"text":"ofr99456 - 1999 - Streamflow information for the next century, a plan for the National Streamflow Information Program of the U.S. Geological Survey","interactions":[],"lastModifiedDate":"2012-02-02T00:08:01","indexId":"ofr99456","displayToPublicDate":"2000-03-01T00:00:00","publicationYear":"1999","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":"99-456","title":"Streamflow information for the next century, a plan for the National Streamflow Information Program of the U.S. Geological Survey","language":"ENGLISH","publisher":"U.S. Dept. of the Interior, U.S. Geological Survey ;\r\nCopies of this report available on request from U.S. Geological Survey Information Services,","doi":"10.3133/ofr99456","issn":"0094-9140","usgsCitation":"Water Resources Division, U.S. Geological Survey, 1999, Streamflow information for the next century, a plan for the National Streamflow Information Program of the U.S. Geological Survey: U.S. Geological Survey Open-File Report 99-456, 13 p. , https://doi.org/10.3133/ofr99456.","productDescription":"13 p. ","costCenters":[],"links":[{"id":154999,"rank":0,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/thumbnails/usgs_thumb.jpg"},{"id":1519,"rank":100,"type":{"id":15,"text":"Index Page"},"url":"https://pubs.water.usgs.gov/ofr99-456","linkFileType":{"id":5,"text":"html"}}],"noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"4f4e4b15e4b07f02db6a4d98","contributors":{"authors":[{"text":"Water Resources Division, U.S. Geological Survey","contributorId":128075,"corporation":true,"usgs":false,"organization":"Water Resources Division, U.S. Geological Survey","id":529093,"contributorType":{"id":1,"text":"Authors"},"rank":1}]}} ,{"id":4803,"text":"pp1613 - 1999 - Magma migration and resupply during the 1974 summit eruptions of Kilauea Volcano, Hawaii","interactions":[],"lastModifiedDate":"2012-02-10T00:10:06","indexId":"pp1613","displayToPublicDate":"2000-03-01T00:00:00","publicationYear":"1999","noYear":false,"publicationType":{"id":18,"text":"Report"},"publicationSubtype":{"id":5,"text":"USGS Numbered Series"},"seriesTitle":{"id":331,"text":"Professional Paper","code":"PP","onlineIssn":"2330-7102","printIssn":"1044-9612","active":true,"publicationSubtype":{"id":5}},"seriesNumber":"1613","title":"Magma migration and resupply during the 1974 summit eruptions of Kilauea Volcano, Hawaii","docAbstract":"The purpose of this paper is to present a complete account of contrasting yet related eruptions, thus filling a gap in the published narratives of recent activity of Kilauea; and to examine their significance within a broader context of regional magmatic and eruptive dynamics. We have gained a historical perspective and can view these three eruptions within a multidecade context of the eruptive behavior of not only Kilauea, but also of the adjacent Mauna Loa.","language":"ENGLISH","publisher":"U.S. Dept. of the Interior, U.S. Geological Survey ;Information Services [distributor],","doi":"10.3133/pp1613","usgsCitation":"Lockwood, J.P., Tilling, R.I., Holcomb, R.T., Klein, F.W., Okamura, A.T., and Peterson, D.W., 1999, Magma migration and resupply during the 1974 summit eruptions of Kilauea Volcano, Hawaii (Online version 1.0): U.S. Geological Survey Professional Paper 1613, iv, 37 p., https://doi.org/10.3133/pp1613.","productDescription":"iv, 37 p.","costCenters":[{"id":615,"text":"Volcano Hazards Program","active":true,"usgs":true}],"links":[{"id":117054,"rank":0,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/pp/1613/report-thumb.jpg"},{"id":8936,"rank":100,"type":{"id":15,"text":"Index Page"},"url":"https://pubs.usgs.gov/pp/pp1613/","linkFileType":{"id":5,"text":"html"}},{"id":31764,"rank":300,"type":{"id":11,"text":"Document"},"url":"https://pubs.usgs.gov/pp/1613/report.pdf","linkFileType":{"id":1,"text":"pdf"}}],"geographicExtents":"{ \"type\": \"FeatureCollection\", \"features\": [ { \"type\": \"Feature\", \"properties\": {}, \"geometry\": { \"type\": \"Polygon\", \"coordinates\": [ [ [ -155.5,19 ], [ -155.5,19.5 ], [ -154.5,19.5 ], [ -154.5,19 ], [ -155.5,19 ] ] ] } } ] }","edition":"Online version 1.0","noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"4f4e4a7fe4b07f02db649217","contributors":{"authors":[{"text":"Lockwood, John P. 0000-0002-6562-0222","orcid":"https://orcid.org/0000-0002-6562-0222","contributorId":30976,"corporation":false,"usgs":true,"family":"Lockwood","given":"John","email":"","middleInitial":"P.","affiliations":[],"preferred":false,"id":149792,"contributorType":{"id":1,"text":"Authors"},"rank":1},{"text":"Tilling, Robert I. 0000-0003-4263-7221 rtilling@usgs.gov","orcid":"https://orcid.org/0000-0003-4263-7221","contributorId":2567,"corporation":false,"usgs":true,"family":"Tilling","given":"Robert","email":"rtilling@usgs.gov","middleInitial":"I.","affiliations":[],"preferred":true,"id":149789,"contributorType":{"id":1,"text":"Authors"},"rank":2},{"text":"Holcomb, Robin T.","contributorId":46938,"corporation":false,"usgs":true,"family":"Holcomb","given":"Robin","email":"","middleInitial":"T.","affiliations":[],"preferred":false,"id":149793,"contributorType":{"id":1,"text":"Authors"},"rank":3},{"text":"Klein, Fred W. klein@usgs.gov","contributorId":4417,"corporation":false,"usgs":true,"family":"Klein","given":"Fred","email":"klein@usgs.gov","middleInitial":"W.","affiliations":[{"id":237,"text":"Earthquake Science Center","active":true,"usgs":true}],"preferred":true,"id":149790,"contributorType":{"id":1,"text":"Authors"},"rank":4},{"text":"Okamura, Arnold T.","contributorId":53782,"corporation":false,"usgs":true,"family":"Okamura","given":"Arnold","email":"","middleInitial":"T.","affiliations":[],"preferred":false,"id":149794,"contributorType":{"id":1,"text":"Authors"},"rank":5},{"text":"Peterson, Donald W.","contributorId":11209,"corporation":false,"usgs":true,"family":"Peterson","given":"Donald","email":"","middleInitial":"W.","affiliations":[],"preferred":false,"id":149791,"contributorType":{"id":1,"text":"Authors"},"rank":6}]}} ,{"id":3462,"text":"cir1180 - 1999 - Areas Susceptible to Irrigation-Induced Selenium Contamination of Water and Biota in the Western United States","interactions":[],"lastModifiedDate":"2012-02-10T00:10:06","indexId":"cir1180","displayToPublicDate":"2000-03-01T00:00:00","publicationYear":"1999","noYear":false,"publicationType":{"id":18,"text":"Report"},"publicationSubtype":{"id":5,"text":"USGS Numbered Series"},"seriesTitle":{"id":307,"text":"Circular","code":"CIR","onlineIssn":"2330-5703","printIssn":"1067-084X","active":true,"publicationSubtype":{"id":5}},"seriesNumber":"1180","title":"Areas Susceptible to Irrigation-Induced Selenium Contamination of Water and Biota in the Western United States","docAbstract":"The U.S. Department of the Interior (DOI) studied contamination induced by irrigation drainage in 26 areas of the Western United States during 1986-95. Comprehensive compilation, synthesis, and evaluation of the data resulting from these studies were initiated by DOI in 1992. Soils and ground water in irrigated areas of the West can contain high concentrations of selenium because of (1) residual selenium from the soil's parent rock beneath irrigated land; (2) selenium derived from rocks in mountains upland from irrigated land by erosion and transport along local drainages, and (3) selenium brought into the area in surface water imported for irrigation. Application of irrigation water to seleniferous soils can dissolve and mobilize selenium and create hydraulic gradients that cause the discharge of seleniferous ground water into irrigation drains. Given a source of selenium, the magnitude of selenium contamination in drainage-affected aquatic ecosystems is strongly related to the aridity of the area and the presence of terminal lakes and ponds. Marine sedimentary rocks and deposits of Late Cretaceous or Tertiary age are generally seleniferous in the Western United States. Depending on their origin and history, some Tertiary continental sedimentary deposits also are seleniferous. Irrigation of areas associated with these rocks and deposits can result in concentrations of selenium in water that exceed criteria for the protection of freshwater aquatic life. \r\n\r\nGeologic and climatic data for the Western United States were evaluated and incorporated into a geographic information system (GIS) to produce a map identifying areas susceptible to irrigation-induced selenium contamination. Land is considered susceptible where a geologic source of selenium is in or near the area and where the evaporation rate is more than 2.5 times the precipitation rate. In the Western United States, about 160,000 square miles of land, which includes about 4,100 square miles (2.6 million acres) of land irrigated for agriculture, has been identified as being susceptible. Biological data were used to evaluate the reliability of the map. In 12 of DOl's 26 study areas, concentrations of selenium measured in bird eggs were elevated sufficiently to significantly reduce hatchability of the eggs. The GIS map identifies 9 of those 12 areas. Deformed bird embryos having classic symptoms of selenium toxicosis were found in four of the study areas, and the map identifies all four as susceptible to irrigation-induced selenium contamination.","language":"ENGLISH","publisher":"Geological Survey (U.S.)","doi":"10.3133/cir1180","isbn":"0607920823","collaboration":"Prepared in cooperation with the U.S. Fish and Wildlife Service, the Bureau of Reclamation, and the Bureau of Indian Affairs","usgsCitation":"Seiler, R.L., Skorupa, J.P., and Peltz, L.A., 1999, Areas Susceptible to Irrigation-Induced Selenium Contamination of Water and Biota in the Western United States: U.S. Geological Survey Circular 1180, iv, 36 p., https://doi.org/10.3133/cir1180.","productDescription":"iv, 36 p.","costCenters":[{"id":451,"text":"National Water Quality Assessment Program","active":true,"usgs":true}],"links":[{"id":124547,"rank":0,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/thumbnails/cir_1180.bmp"},{"id":11746,"rank":100,"type":{"id":15,"text":"Index Page"},"url":"https://pubs.usgs.gov/circ/circ1180/","linkFileType":{"id":5,"text":"html"}}],"geographicExtents":"{ \"type\": \"FeatureCollection\", \"features\": [ { \"type\": \"Feature\", \"properties\": {}, \"geometry\": { \"type\": \"Polygon\", \"coordinates\": [ [ [ -125,25 ], [ -125,49 ], [ -90,49 ], [ -90,25 ], [ -125,25 ] ] ] } } ] }","noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"4f4e4b16e4b07f02db6a55b0","contributors":{"authors":[{"text":"Seiler, Ralph L.","contributorId":13609,"corporation":false,"usgs":true,"family":"Seiler","given":"Ralph","email":"","middleInitial":"L.","affiliations":[],"preferred":false,"id":146971,"contributorType":{"id":1,"text":"Authors"},"rank":1},{"text":"Skorupa, Joseph P.","contributorId":54980,"corporation":false,"usgs":true,"family":"Skorupa","given":"Joseph","email":"","middleInitial":"P.","affiliations":[],"preferred":false,"id":146973,"contributorType":{"id":1,"text":"Authors"},"rank":2},{"text":"Peltz, Lorri A.","contributorId":29401,"corporation":false,"usgs":true,"family":"Peltz","given":"Lorri","email":"","middleInitial":"A.","affiliations":[{"id":12701,"text":"US Geological Survey","active":true,"usgs":false}],"preferred":false,"id":146972,"contributorType":{"id":1,"text":"Authors"},"rank":3}]}} ,{"id":27717,"text":"wri994008 - 1999 - Estimating the magnitude of peak flows for streams in Maine for selected recurrence intervals","interactions":[{"subject":{"id":27717,"text":"wri994008 - 1999 - Estimating the magnitude of peak flows for streams in Maine for selected recurrence intervals","indexId":"wri994008","publicationYear":"1999","noYear":false,"displayTitle":"Estimating the Magnitude of Peak Flows for Streams in Maine for Selected Recurrence Intervals","title":"Estimating the magnitude of peak flows for streams in Maine for selected recurrence intervals"},"predicate":"SUPERSEDED_BY","object":{"id":70215422,"text":"sir20205092 - 2020 - Estimating flood magnitude and frequency on gaged and ungaged streams in Maine","indexId":"sir20205092","publicationYear":"2020","noYear":false,"title":"Estimating flood magnitude and frequency on gaged and ungaged streams in Maine"},"id":1}],"supersededBy":{"id":70215422,"text":"sir20205092 - 2020 - Estimating flood magnitude and frequency on gaged and ungaged streams in Maine","indexId":"sir20205092","publicationYear":"2020","noYear":false,"title":"Estimating flood magnitude and frequency on gaged and ungaged streams in Maine"},"lastModifiedDate":"2025-02-07T16:38:58.124541","indexId":"wri994008","displayToPublicDate":"2000-03-01T00:00:00","publicationYear":"1999","noYear":false,"publicationType":{"id":18,"text":"Report"},"publicationSubtype":{"id":5,"text":"USGS Numbered Series"},"seriesTitle":{"id":342,"text":"Water-Resources Investigations Report","code":"WRI","active":false,"publicationSubtype":{"id":5}},"seriesNumber":"99-4008","displayTitle":"Estimating the Magnitude of Peak Flows for Streams in Maine for Selected Recurrence Intervals","title":"Estimating the magnitude of peak flows for streams in Maine for selected recurrence intervals","docAbstract":"This report gives estimates of, and presents techniques for estimating, the magnitude of peak flows for streams in Maine for recurrence intervals of 2, 5, 10, 25, 50, 100, and 500 years. A flowchart in this report guides the user to the appropriate estimates and (or) estimating techniques for a site on a specific stream. \r\n\r\nSection 1, 'Estimates of peak flows and maximum recorded flows at USGS streamflow-gaging stations,' contains peak-flow estimates and the maximum recorded flows at 98 U.S. Geological Survey (USGS) streamflow-gaging stations. In the development of the peak-flow estimates at gaging stations, a new generalized skew coefficient was calculated for Maine. This single statewide value of 0.029 (with a standard error of prediction of 0.297) is more accurate for Maine than the national skew isoline map in Bulletin 17B of the Interagency Advisory Committee on Water Data. \r\n\r\nTwo techniques are presented to estimate the peak flows for ungaged, unregulated streams in rural drainage basins. These two techniques were developed using generalized least squares regression procedures at 70 USGS gaging stations in Maine and eastern New Hampshire. Section 2, 'Estimating peak flows for ungaged, unregulated streams in rural drainage basins,' uses the final explanatory variables of drainage area and basin wetlands. The average standard error of prediction for the 100-year peak flow regression equation in section 2 was 48.6 percent to -32.7 percent. Drainage area was the only explanatory variable used in section 3, 'Estimating peak flows for ungaged, unregulated streams in rural drainage basins - Simplified technique.' The average standard error of prediction for the 100-year peak flow regression equation in section 3 was 80.3 percent to -44.5 percent. \r\n\r\nSection 4 of the report describes techniques for estimating peak flows for ungaged sites on gaged, unregulated streams in rural drainage basins. Section 5, 'Estimating peak flows for ungaged, unregulated streams in urbanized drainage basins,' describes regression equations for use when a drainage basin is urbanized. These urban regression equations come from a previous USGS nationwide study. As stated in section 6, because peak flows on regulated streams are dependent on variable human actions, estimating peak flows at ungaged sites on regulated streams is beyond the scope of this report.","language":"English","publisher":"U.S. Geological Survey","doi":"10.3133/wri994008","collaboration":"Prepared in cooperation with the Maine Department of Transportation","usgsCitation":"Hodgkins, G.A., 1999, Estimating the magnitude of peak flows for streams in Maine for selected recurrence intervals: U.S. Geological Survey Water-Resources Investigations Report 99-4008, Report: iv, 45 p.; Computer program, https://doi.org/10.3133/wri994008.","productDescription":"Report: iv, 45 p.; Computer program","costCenters":[{"id":371,"text":"Maine Water Science Center","active":true,"usgs":true}],"links":[{"id":481801,"rank":3,"type":{"id":22,"text":"Related Work"},"url":"https://doi.org/10.3133/ofr75292","text":"Superseded Publication:","linkHelpText":"A technique for estimating the magnitude and frequency of floods in Maine(1975)"},{"id":124568,"rank":1,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/wri/1999/4008/report-thumb.jpg"},{"id":56561,"rank":2,"type":{"id":11,"text":"Document"},"url":"https://pubs.usgs.gov/wri/1999/4008/report.pdf","linkFileType":{"id":1,"text":"pdf"}}],"country":"United States","state":"Maine","geographicExtents":"{ \"type\": \"FeatureCollection\", \"features\": [ { \"type\": \"Feature\", \"properties\": {}, \"geometry\": { \"type\": \"Polygon\", \"coordinates\": [ [ [ -72,43 ], [ -72,48 ], [ -66.5,48 ], [ -66.5,43 ], [ -72,43 ] ] ] } } ] }","noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"4f4e4a0ce4b07f02db5fc2df","contributors":{"authors":[{"text":"Hodgkins, Glenn A. 0000-0002-4916-5565 gahodgki@usgs.gov","orcid":"https://orcid.org/0000-0002-4916-5565","contributorId":2020,"corporation":false,"usgs":true,"family":"Hodgkins","given":"Glenn","email":"gahodgki@usgs.gov","middleInitial":"A.","affiliations":[{"id":371,"text":"Maine Water Science Center","active":true,"usgs":true},{"id":466,"text":"New England Water Science Center","active":true,"usgs":true}],"preferred":true,"id":198582,"contributorType":{"id":1,"text":"Authors"},"rank":1}]}} ,{"id":4924,"text":"ds29 - 1999 - The October 17, 1989, Loma Prieta, California, earthquake: selected photographs","interactions":[],"lastModifiedDate":"2012-02-02T00:05:43","indexId":"ds29","displayToPublicDate":"2000-03-01T00:00:00","publicationYear":"1999","noYear":false,"publicationType":{"id":18,"text":"Report"},"publicationSubtype":{"id":5,"text":"USGS Numbered Series"},"seriesTitle":{"id":310,"text":"Data Series","code":"DS","onlineIssn":"2327-638X","printIssn":"2327-0271","active":false,"publicationSubtype":{"id":5}},"seriesNumber":"29","title":"The October 17, 1989, Loma Prieta, California, earthquake: selected photographs","docAbstract":"This CD-ROM contains 103 digitized color 35-mm images from Open-File Report 90-547 (Nakata and others, 1990). Our photographic coverage reflects the time and resources available immediately after the event and is not intended to portray the full extent of earthquake damage. This CD-ROM provides images for use by the interested public, multimedia producers, desktop publishers, and the high-end printing industry.","language":"ENGLISH","publisher":"U.S Department of the Interior, U.S. Geological Survey,","doi":"10.3133/ds29","isbn":"0607866403","usgsCitation":"Nakata, J.K., Meyer, C., Wilshire, H.G., Tinsley, J.C., Updegrove, W., Peterson, D., Ellen, S.D., Haugerud, R., McLaughlin, R.J., Fisher, G., and Diggles, M.F., 1999, The October 17, 1989, Loma Prieta, California, earthquake: selected photographs (Version 1.2): U.S. Geological Survey Data Series 29, 1 CD-ROM, https://doi.org/10.3133/ds29.","productDescription":"1 CD-ROM","costCenters":[],"links":[{"id":139619,"rank":0,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/thumbnails/usgs_thumb.jpg"},{"id":688,"rank":100,"type":{"id":15,"text":"Index Page"},"url":"https://pubs.usgs.gov/dds/dds-29/","linkFileType":{"id":5,"text":"html"}}],"edition":"Version 1.2","noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"4f4e4ac7e4b07f02db67af68","contributors":{"authors":[{"text":"Nakata, John K.","contributorId":32518,"corporation":false,"usgs":true,"family":"Nakata","given":"John","email":"","middleInitial":"K.","affiliations":[],"preferred":false,"id":150127,"contributorType":{"id":1,"text":"Authors"},"rank":1},{"text":"Meyer, C.E.","contributorId":104023,"corporation":false,"usgs":true,"family":"Meyer","given":"C.E.","email":"","affiliations":[],"preferred":false,"id":150135,"contributorType":{"id":1,"text":"Authors"},"rank":2},{"text":"Wilshire, H. G.","contributorId":36125,"corporation":false,"usgs":false,"family":"Wilshire","given":"H.","middleInitial":"G.","affiliations":[],"preferred":false,"id":150128,"contributorType":{"id":1,"text":"Authors"},"rank":3},{"text":"Tinsley, J. C. III","contributorId":39777,"corporation":false,"usgs":true,"family":"Tinsley","given":"J.","suffix":"III","email":"","middleInitial":"C.","affiliations":[],"preferred":false,"id":150130,"contributorType":{"id":1,"text":"Authors"},"rank":4},{"text":"Updegrove, W.S.","contributorId":87922,"corporation":false,"usgs":true,"family":"Updegrove","given":"W.S.","email":"","affiliations":[],"preferred":false,"id":150134,"contributorType":{"id":1,"text":"Authors"},"rank":5},{"text":"Peterson, D.M.","contributorId":57449,"corporation":false,"usgs":true,"family":"Peterson","given":"D.M.","email":"","affiliations":[],"preferred":false,"id":150132,"contributorType":{"id":1,"text":"Authors"},"rank":6},{"text":"Ellen, S. D.","contributorId":12467,"corporation":false,"usgs":true,"family":"Ellen","given":"S.","email":"","middleInitial":"D.","affiliations":[],"preferred":false,"id":150126,"contributorType":{"id":1,"text":"Authors"},"rank":7},{"text":"Haugerud, R. A. 0000-0001-7302-4351","orcid":"https://orcid.org/0000-0001-7302-4351","contributorId":42953,"corporation":false,"usgs":true,"family":"Haugerud","given":"R. A.","affiliations":[],"preferred":false,"id":150131,"contributorType":{"id":1,"text":"Authors"},"rank":8},{"text":"McLaughlin, R. J. 0000-0002-4390-2288","orcid":"https://orcid.org/0000-0002-4390-2288","contributorId":107271,"corporation":false,"usgs":true,"family":"McLaughlin","given":"R.","middleInitial":"J.","affiliations":[],"preferred":false,"id":150136,"contributorType":{"id":1,"text":"Authors"},"rank":9},{"text":"Fisher, G.R.","contributorId":58628,"corporation":false,"usgs":true,"family":"Fisher","given":"G.R.","email":"","affiliations":[],"preferred":false,"id":150133,"contributorType":{"id":1,"text":"Authors"},"rank":10},{"text":"Diggles, M. F.","contributorId":39356,"corporation":false,"usgs":true,"family":"Diggles","given":"M.","email":"","middleInitial":"F.","affiliations":[],"preferred":false,"id":150129,"contributorType":{"id":1,"text":"Authors"},"rank":11}]}} ,{"id":22888,"text":"ofr99254 - 1999 - Method for Examination and Documentation of Basic Information and Metadata from Published Reports Relevant to the Study of Stormwater Runoff Quality","interactions":[],"lastModifiedDate":"2012-03-08T17:16:14","indexId":"ofr99254","displayToPublicDate":"2000-03-01T00:00:00","publicationYear":"1999","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":"99-254","title":"Method for Examination and Documentation of Basic Information and Metadata from Published Reports Relevant to the Study of Stormwater Runoff Quality","docAbstract":"A readily accessible archive of information that is valid, current, and technically defensible is needed to make informed highway-planning, design, and management decisions. The National Highway Runoff Water-Quality Data and Methodology Synthesis (NDAMS) is a cataloging and assessment of the documentation of information relevant to highway-runoff water quality available in published reports. The report review process is based on the NDAMS review sheet, which was designed by the USGS with input from the FHWA, State transportation agencies, and the regulatory community. The report-review process is designed to determine the technical merit of the existing literature in terms of current requirements for data documentation, data quality, quality assurance and quality control (QA/QC), and technical issues that may affect the use of historical data. To facilitate the review process, the NDAMS review sheet is divided into 12 sections: (1) administrative review information, (2) investigation and report information, (3) temporal information, (4) location information (5) water-quality-monitoring information, (6) sample-handling methods, (7) constituent information, (8) sampling focus and matrix, (9) flow monitoring methods, (10) field QA/QC, (11) laboratory, and (12) uncertainty/error analysis.\r\n\r\nThis report describes the NDAMS report reviews and metadata documentation methods and provides an overview of the approach and of the quality-assurance and quality-control program used to implement the review process. Detailed information, including a glossary of relevant terms, a copy of the report-review sheets, and reportreview instructions are completely documented in a series of three appendixes included with this report. Therefore the reviews are repeatable and the methods can be used by transportation research organizations to catalog new reports as they are published.","language":"ENGLISH","publisher":"Geological Survey (U.S.)","doi":"10.3133/ofr99254","issn":"0094-9140","collaboration":"Prepared in cooperation with the Federal Highway Administration (A Contribution to the National Highway Runoff Data and Methodology Synthesis)","usgsCitation":"Dionne, S.G., Granato, G., and Tana, C.K., 1999, Method for Examination and Documentation of Basic Information and Metadata from Published Reports Relevant to the Study of Stormwater Runoff Quality: U.S. Geological Survey Open-File Report 99-254, vi, 156 p., https://doi.org/10.3133/ofr99254.","productDescription":"vi, 156 p.","costCenters":[{"id":377,"text":"Massachusetts-Rhode Island Water Science Center","active":false,"usgs":true}],"links":[{"id":154199,"rank":0,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/thumbnails/usgs_thumb.jpg"},{"id":9505,"rank":100,"type":{"id":15,"text":"Index Page"},"url":"https://pubs.usgs.gov/of/1999/ofr99-254/","linkFileType":{"id":5,"text":"html"}}],"noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"4f4e4a4ae4b07f02db624b3a","contributors":{"authors":[{"text":"Dionne, Shannon G.","contributorId":19964,"corporation":false,"usgs":true,"family":"Dionne","given":"Shannon","email":"","middleInitial":"G.","affiliations":[],"preferred":false,"id":189072,"contributorType":{"id":1,"text":"Authors"},"rank":1},{"text":"Granato, Gregory E. 0000-0002-2561-9913 ggranato@usgs.gov","orcid":"https://orcid.org/0000-0002-2561-9913","contributorId":1692,"corporation":false,"usgs":true,"family":"Granato","given":"Gregory E.","email":"ggranato@usgs.gov","affiliations":[{"id":466,"text":"New England Water Science Center","active":true,"usgs":true}],"preferred":false,"id":189070,"contributorType":{"id":1,"text":"Authors"},"rank":2},{"text":"Tana, Cameron K.","contributorId":6473,"corporation":false,"usgs":true,"family":"Tana","given":"Cameron","email":"","middleInitial":"K.","affiliations":[],"preferred":false,"id":189071,"contributorType":{"id":1,"text":"Authors"},"rank":3}]}} ]}