{"pageNumber":"3890","pageRowStart":"97225","pageSize":"25","recordCount":185169,"records":[{"id":60068,"text":"mf2283 - 1995 - Geologic map of the Cuchara Quadrangle, Huerfano County, Colorado","interactions":[],"lastModifiedDate":"2012-02-10T00:10:34","indexId":"mf2283","displayToPublicDate":"1995-06-01T00:00:00","publicationYear":"1995","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":"2283","title":"Geologic map of the Cuchara Quadrangle, Huerfano County, Colorado","language":"ENGLISH","doi":"10.3133/mf2283","usgsCitation":"Lindsey, D.A., 1995, Geologic map of the Cuchara Quadrangle, Huerfano County, Colorado: U.S. Geological Survey Miscellaneous Field Studies Map 2283, 1 map ;58 x 46 cm., on sheet 94 x 127 cm., folded in envelope 30 x 24 cm., https://doi.org/10.3133/mf2283.","productDescription":"1 map ;58 x 46 cm., on sheet 94 x 127 cm., folded in envelope 30 x 24 cm.","costCenters":[],"links":[{"id":105336,"rank":700,"type":{"id":15,"text":"Index Page"},"url":"https://ngmdb.usgs.gov/Prodesc/proddesc_5903.htm","linkFileType":{"id":5,"text":"html"},"description":"5903"},{"id":180640,"rank":0,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/thumbnails/usgs_thumb.jpg"}],"scale":"0","geographicExtents":"{ \"type\": \"FeatureCollection\", \"features\": [ { \"type\": \"Feature\", \"properties\": {}, \"geometry\": { \"type\": \"Polygon\", \"coordinates\": [ [ [ -105.11749999999999,37.3675 ], [ -105.11749999999999,37.5 ], [ -105,37.5 ], [ -105,37.3675 ], [ -105.11749999999999,37.3675 ] ] ] } } ] }","noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"4f4e4b09e4b07f02db69bda1","contributors":{"authors":[{"text":"Lindsey, D. A.","contributorId":49814,"corporation":false,"usgs":true,"family":"Lindsey","given":"D.","email":"","middleInitial":"A.","affiliations":[],"preferred":false,"id":263091,"contributorType":{"id":1,"text":"Authors"},"rank":1}]}}
,{"id":70018786,"text":"70018786 - 1995 - Deep-sea biostratigraphy of prograding platform margins (Neogene, Bahamas): Key evidence linked to depositional rhythm","interactions":[],"lastModifiedDate":"2024-09-30T17:03:55.384101","indexId":"70018786","displayToPublicDate":"1995-06-01T00:00:00","publicationYear":"1995","noYear":false,"publicationType":{"id":2,"text":"Article"},"publicationSubtype":{"id":10,"text":"Journal Article"},"seriesTitle":{"id":2673,"text":"Marine Micropaleontology","active":true,"publicationSubtype":{"id":10}},"title":"Deep-sea biostratigraphy of prograding platform margins (Neogene, Bahamas): Key evidence linked to depositional rhythm","docAbstract":"<p><span>New foraminiferal evidence from two boreholes on the paleoshelf and slope of western Great Bahama Bank has wide-ranging implications for understanding formation and evolution of carbonate-platform margins. The new data, abundant well-preserved planktic foraminifera, were obtained by disaggregating samples from intercalated pelagic layers and selected parts of thick hemipelagic limestone. Earlier efforts to obtain biostratigraphic ages identified six biostratigraphic units in each borehole, provided biozonal age alternatives for both holes, and resulted in different Pliocene biozones between them. The new data define six units in one hole and seven in the other, bracket the biozones present and their ages, indicate different sedimentation rates, and show that within the limits of biostratigraphic resolution the biozones are correlative between the holes. Most importantly, the revised ages show that the paleoshelf borehole probably penetrated the late Miocene rather than middle Miocene.</span></p><p><span>The oldest unit is on the paleoshelf and the youngest (uppermost Pliocene) is on the slope. Between the holes, the stratigraphic interval spans the temporal interval from an inferred maximum of ~ 10.2 Ma to a minimum of ~ 1.6 Ma. Although the biozones range sequentially from the&nbsp;<i>Neogloboquadrina acostaensis</i>&nbsp;(N16) Zone to the basal part of the&nbsp;<i>Globorotalia truncatulinoides truncatulinoides</i>&nbsp;(N22) Zone (&nbsp;<i>Globorotalia crassaformis viola</i>&nbsp;Subzone), absence of key species indicates that deposition was discontinuous. Numerous periods of erosion and/or nondeposition are inferred, the largest of which is a condensed section/ hiatus (~ 1.2 Myr) above the paleoslope Miocene/Pliocene boundary. In addition, the late Pliocene&nbsp;<i>Globorotalia tosaensis tosaensis</i>&nbsp;(N21) Zone is not recognized on the slope. Its absence is consistent with a widespread regional unconformity.</span></p><p><span>Sedimentation rates and depths of series boundaries vary widely in both holes. The paleoslope Miocene/Pliocene boundary lies at ~540 m below top of the hole. The lower/upper Pliocene boundary is placed at or near 444 m. Position of the Pliocene/ Pleistocene boundary is less certain but is within the top 382 m of the hole. Its placement anywhere within this interval is a reasonable assessment considering an exceptionally high rate of sedimentation (~562 m/Myr; 168.6 m interval, based on topmost foraminiferal sample; 1.9–1.6 Ma). As expected, the lowest sedimentation rate occurs in the condensed section overlying the Miocene/Pliocene boundary (~ 5 m/Myr, 9.5 m, 5.3–4.1 Ma).</span></p><p><span>The paleoshelf Miocene/Pliocene boundary lies below a hiatal condensed section (295–278 m below top of the hole) that has a greater sedimentation rate (~ 89 m/Myr, 17.7 m, 5.5–5.3 Ma) than that at the slope. The lower/upper Pliocene boundary is placed at or near a depth of 236 m, and the Pliocene/Pleistocene boundary lies within the top 113 m of the hole. Sedimentation rates on the shelf range from ~ 15 m/Myr above the condensed section (22.9 m, 5.3–3.8 Ma) to a late Pliocene high of ~ 183 m/Myr (54.9 m interval, based on the point at which the age-depth line crosses the 1.9 Myr mark between the topmost two fossiliferous samples; 2.2–1.9 Ma).</span></p>","language":"English","publisher":"Elsevier","doi":"10.1016/0377-8398(95)00021-R","usgsCitation":"Lidz, B., and McNeill, D., 1995, Deep-sea biostratigraphy of prograding platform margins (Neogene, Bahamas): Key evidence linked to depositional rhythm: Marine Micropaleontology, v. 25, no. 2-3, p. 87-125, https://doi.org/10.1016/0377-8398(95)00021-R.","productDescription":"39 p.","startPage":"87","endPage":"125","costCenters":[],"links":[{"id":479212,"rank":2,"type":{"id":40,"text":"Open Access Publisher Index Page"},"url":"https://doi.org/10.1016/0377-8398(95)00021-r","text":"Publisher Index Page"},{"id":227494,"rank":1,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/thumbnails/outside_thumb.jpg"}],"country":"Bahamas","geographicExtents":"{\"type\":\"FeatureCollection\",\"features\":[{\"type\":\"Feature\",\"geometry\":{\"type\":\"MultiPolygon\",\"coordinates\":[[[[-77.53466,23.75975],[-77.78,23.71],[-78.03405,24.28615],[-78.40848,24.57564],[-78.19087,25.2103],[-77.89,25.17],[-77.54,24.34],[-77.53466,23.75975]]],[[[-77.82,26.58],[-78.91,26.42],[-78.98,26.79],[-78.51,26.87],[-77.85,26.84],[-77.82,26.58]]],[[[-77,26.59],[-77.17255,25.87918],[-77.35641,26.00735],[-77.34,26.53],[-77.78802,26.92516],[-77.79,27.04],[-77,26.59]]]]},\"properties\":{\"name\":\"The Bahamas\"}}]}","volume":"25","issue":"2-3","noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"5059fe2ee4b0c8380cd4eb8c","contributors":{"authors":[{"text":"Lidz, Barbara H.","contributorId":64576,"corporation":false,"usgs":true,"family":"Lidz","given":"Barbara H.","affiliations":[],"preferred":false,"id":380758,"contributorType":{"id":1,"text":"Authors"},"rank":1},{"text":"McNeill, D.F.","contributorId":68901,"corporation":false,"usgs":true,"family":"McNeill","given":"D.F.","email":"","affiliations":[],"preferred":false,"id":380759,"contributorType":{"id":1,"text":"Authors"},"rank":2}]}}
,{"id":16806,"text":"ofr956 - 1995 - Analytical results and sample locality map of rock and soil samples, and samples of the ash of big sagebrush, rabbit brush, and western juniper from the Badlands Wilderness Study Area and the Badlands Wilderness Study Area additions (OR-005-021), Crook and Deschutes counties, Oregon","interactions":[],"lastModifiedDate":"2012-02-02T00:07:18","indexId":"ofr956","displayToPublicDate":"1995-06-01T00:00:00","publicationYear":"1995","noYear":false,"publicationType":{"id":18,"text":"Report"},"publicationSubtype":{"id":5,"text":"USGS Numbered Series"},"seriesTitle":{"id":330,"text":"Open-File Report","code":"OFR","onlineIssn":"2331-1258","printIssn":"0196-1497","active":true,"publicationSubtype":{"id":5}},"seriesNumber":"95-6","title":"Analytical results and sample locality map of rock and soil samples, and samples of the ash of big sagebrush, rabbit brush, and western juniper from the Badlands Wilderness Study Area and the Badlands Wilderness Study Area additions (OR-005-021), Crook and Deschutes counties, Oregon","language":"ENGLISH","publisher":"U.S. Geological Survey,","doi":"10.3133/ofr956","usgsCitation":"King, H.D., Briggs, P., Erickson, M.S., and Bergquist, J., 1995, Analytical results and sample locality map of rock and soil samples, and samples of the ash of big sagebrush, rabbit brush, and western juniper from the Badlands Wilderness Study Area and the Badlands Wilderness Study Area additions (OR-005-021), Crook and Deschutes counties, Oregon: U.S. Geological Survey Open-File Report 95-6, 33 p.; 1 computer disk ;5 1/4 in., https://doi.org/10.3133/ofr956.","productDescription":"33 p.; 1 computer disk ;5 1/4 in.","costCenters":[],"links":[{"id":150551,"rank":0,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/of/1995/0006/report-thumb.jpg"},{"id":45873,"rank":300,"type":{"id":11,"text":"Document"},"url":"https://pubs.usgs.gov/of/1995/0006/report.pdf","linkFileType":{"id":1,"text":"pdf"}}],"noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"4f4e4acee4b07f02db67f48b","contributors":{"authors":[{"text":"King, Harley D. hking@usgs.gov","contributorId":4046,"corporation":false,"usgs":true,"family":"King","given":"Harley","email":"hking@usgs.gov","middleInitial":"D.","affiliations":[],"preferred":true,"id":173686,"contributorType":{"id":1,"text":"Authors"},"rank":1},{"text":"Briggs, Paul H.","contributorId":107691,"corporation":false,"usgs":true,"family":"Briggs","given":"Paul H.","affiliations":[],"preferred":false,"id":173689,"contributorType":{"id":1,"text":"Authors"},"rank":2},{"text":"Erickson, M. S.","contributorId":35302,"corporation":false,"usgs":true,"family":"Erickson","given":"M.","email":"","middleInitial":"S.","affiliations":[],"preferred":false,"id":173687,"contributorType":{"id":1,"text":"Authors"},"rank":3},{"text":"Bergquist, J.R.","contributorId":65090,"corporation":false,"usgs":true,"family":"Bergquist","given":"J.R.","email":"","affiliations":[],"preferred":false,"id":173688,"contributorType":{"id":1,"text":"Authors"},"rank":4}]}}
,{"id":17440,"text":"ofr94512 - 1995 - Observations of the surge-type Black Rapids Glacier, Alaska, during a quiescent period, 1970-92","interactions":[],"lastModifiedDate":"2013-09-18T07:36:51","indexId":"ofr94512","displayToPublicDate":"1995-06-01T00:00:00","publicationYear":"1995","noYear":false,"publicationType":{"id":18,"text":"Report"},"publicationSubtype":{"id":5,"text":"USGS Numbered Series"},"seriesTitle":{"id":330,"text":"Open-File Report","code":"OFR","onlineIssn":"2331-1258","printIssn":"0196-1497","active":true,"publicationSubtype":{"id":5}},"seriesNumber":"94-512","title":"Observations of the surge-type Black Rapids Glacier, Alaska, during a quiescent period, 1970-92","docAbstract":"This report presents 23 years (1970 to 1992) of observations of Black Rapids Glacier, Alaska. Black Rapids Glacier is a surge-type glacier which most recently surged in 1936-37, and is currently in its quiescent phase. This glacier is of special interest because it is a potential hazard to the trans-Alaska oil pipeline. Ten sites on the glacier were monitored from 1972 to 1987, and three sites were monitored from 1988 to 1992. The measurement program presented here includes observations of surface mass balance, ice velocity, and surface altitude made twice each year. Additional one-time data include observations of ice thickness, previously unreported observations of the 1936-37 surge, establishment of the geodetic control monuments, and a new map of Black Rapids Glacier.","language":"ENGLISH","publisher":"U.S. Geological Survey ;U.S.G.S. Earth Science Information Center, Open-File Reports Section [distributor],","doi":"10.3133/ofr94512","collaboration":"The USGS does not support this software or technical questions for the software associated with the publication.","usgsCitation":"Heinrichs, T.A., Mayo, L., Trabant, D., and March, R., 1995, Observations of the surge-type Black Rapids Glacier, Alaska, during a quiescent period, 1970-92: U.S. Geological Survey Open-File Report 94-512, 1 v. (various pagings) :ill., maps ;28 cm. +1 computer disk (3 1/2 in.), https://doi.org/10.3133/ofr94512.","productDescription":"1 v. (various pagings) :ill., maps ;28 cm. +1 computer disk (3 1/2 in.)","costCenters":[],"links":[{"id":150044,"rank":0,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/of/1994/0512/report-thumb.jpg"},{"id":46581,"rank":300,"type":{"id":11,"text":"Document"},"url":"https://pubs.usgs.gov/of/1994/0512/report.pdf","linkFileType":{"id":1,"text":"pdf"}},{"id":277764,"type":{"id":4,"text":"Application Site"},"url":"https://pubs.usgs.gov/of/1994/0512/application.zip"}],"noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"4f4e4afbe4b07f02db6963fb","contributors":{"authors":[{"text":"Heinrichs, Thomas A.","contributorId":93509,"corporation":false,"usgs":true,"family":"Heinrichs","given":"Thomas","email":"","middleInitial":"A.","affiliations":[],"preferred":false,"id":176397,"contributorType":{"id":1,"text":"Authors"},"rank":1},{"text":"Mayo, L.R.","contributorId":21541,"corporation":false,"usgs":true,"family":"Mayo","given":"L.R.","email":"","affiliations":[],"preferred":false,"id":176395,"contributorType":{"id":1,"text":"Authors"},"rank":2},{"text":"Trabant, D.C.","contributorId":42209,"corporation":false,"usgs":true,"family":"Trabant","given":"D.C.","email":"","affiliations":[],"preferred":false,"id":176396,"contributorType":{"id":1,"text":"Authors"},"rank":3},{"text":"March, R.S.","contributorId":16431,"corporation":false,"usgs":true,"family":"March","given":"R.S.","email":"","affiliations":[],"preferred":false,"id":176394,"contributorType":{"id":1,"text":"Authors"},"rank":4}]}}
,{"id":18655,"text":"ofr9556 - 1995 - Extraction of metals from raw clinoptilolite-rich rocks exposed to water in heavy-metal-polluted drainages","interactions":[],"lastModifiedDate":"2012-02-02T00:07:28","indexId":"ofr9556","displayToPublicDate":"1995-06-01T00:00:00","publicationYear":"1995","noYear":false,"publicationType":{"id":18,"text":"Report"},"publicationSubtype":{"id":5,"text":"USGS Numbered Series"},"seriesTitle":{"id":330,"text":"Open-File Report","code":"OFR","onlineIssn":"2331-1258","printIssn":"0196-1497","active":true,"publicationSubtype":{"id":5}},"seriesNumber":"95-56","title":"Extraction of metals from raw clinoptilolite-rich rocks exposed to water in heavy-metal-polluted drainages","language":"ENGLISH","publisher":"U.S. Geological Survey,","doi":"10.3133/ofr9556","usgsCitation":"Desborough, G.A., and Frishman, D., 1995, Extraction of metals from raw clinoptilolite-rich rocks exposed to water in heavy-metal-polluted drainages: U.S. Geological Survey Open-File Report 95-56, iii, 30 p. ill., map ;28 cm., https://doi.org/10.3133/ofr9556.","productDescription":"iii, 30 p. ill., map ;28 cm.","costCenters":[],"links":[{"id":151725,"rank":0,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/of/1995/0056/report-thumb.jpg"},{"id":47992,"rank":300,"type":{"id":11,"text":"Document"},"url":"https://pubs.usgs.gov/of/1995/0056/report.pdf","linkFileType":{"id":1,"text":"pdf"}}],"noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"4f4e4a06e4b07f02db5f8a14","contributors":{"authors":[{"text":"Desborough, George A.","contributorId":101661,"corporation":false,"usgs":true,"family":"Desborough","given":"George","email":"","middleInitial":"A.","affiliations":[],"preferred":false,"id":179501,"contributorType":{"id":1,"text":"Authors"},"rank":1},{"text":"Frishman, David","contributorId":40214,"corporation":false,"usgs":true,"family":"Frishman","given":"David","email":"","affiliations":[],"preferred":false,"id":179500,"contributorType":{"id":1,"text":"Authors"},"rank":2}]}}
,{"id":16928,"text":"ofr957 - 1995 - Biogeochemical study of the pinelands in Everglades National Park, Florida","interactions":[],"lastModifiedDate":"2012-02-02T00:07:10","indexId":"ofr957","displayToPublicDate":"1995-06-01T00:00:00","publicationYear":"1995","noYear":false,"publicationType":{"id":18,"text":"Report"},"publicationSubtype":{"id":5,"text":"USGS Numbered Series"},"seriesTitle":{"id":330,"text":"Open-File Report","code":"OFR","onlineIssn":"2331-1258","printIssn":"0196-1497","active":true,"publicationSubtype":{"id":5}},"seriesNumber":"95-7","title":"Biogeochemical study of the pinelands in Everglades National Park, Florida","language":"ENGLISH","publisher":"U.S. Geological Survey :\r\nBooks and Open-File Reports [distributor],","doi":"10.3133/ofr957","usgsCitation":"Jackson, L.L., Briggs, P., Gough, L.P., and Stolte, K., 1995, Biogeochemical study of the pinelands in Everglades National Park, Florida: U.S. Geological Survey Open-File Report 95-7, 85 p. ill., maps ;28 cm., https://doi.org/10.3133/ofr957.","productDescription":"85 p. ill., maps ;28 cm.","costCenters":[],"links":[{"id":149570,"rank":0,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/of/1995/0007/report-thumb.jpg"},{"id":46040,"rank":300,"type":{"id":11,"text":"Document"},"url":"https://pubs.usgs.gov/of/1995/0007/report.pdf","linkFileType":{"id":1,"text":"pdf"}}],"noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"4f4e4a4be4b07f02db625cd2","contributors":{"authors":[{"text":"Jackson, Larry L.","contributorId":18790,"corporation":false,"usgs":true,"family":"Jackson","given":"Larry","email":"","middleInitial":"L.","affiliations":[],"preferred":false,"id":174211,"contributorType":{"id":1,"text":"Authors"},"rank":1},{"text":"Briggs, Paul H.","contributorId":107691,"corporation":false,"usgs":true,"family":"Briggs","given":"Paul H.","affiliations":[],"preferred":false,"id":174214,"contributorType":{"id":1,"text":"Authors"},"rank":2},{"text":"Gough, L. P.","contributorId":64198,"corporation":false,"usgs":true,"family":"Gough","given":"L.","email":"","middleInitial":"P.","affiliations":[],"preferred":false,"id":174213,"contributorType":{"id":1,"text":"Authors"},"rank":3},{"text":"Stolte, K.W.","contributorId":59056,"corporation":false,"usgs":true,"family":"Stolte","given":"K.W.","affiliations":[],"preferred":false,"id":174212,"contributorType":{"id":1,"text":"Authors"},"rank":4}]}}
,{"id":18836,"text":"ofr9543 - 1995 - Impact of the lower Alamosa River water on alfalfa, southwestern San Luis Valley, Colorado: 1994 follow-up study","interactions":[],"lastModifiedDate":"2019-12-07T11:30:31","indexId":"ofr9543","displayToPublicDate":"1995-06-01T00:00:00","publicationYear":"1995","noYear":false,"publicationType":{"id":18,"text":"Report"},"publicationSubtype":{"id":5,"text":"USGS Numbered Series"},"seriesTitle":{"id":330,"text":"Open-File Report","code":"OFR","onlineIssn":"2331-1258","printIssn":"0196-1497","active":true,"publicationSubtype":{"id":5}},"seriesNumber":"95-43","title":"Impact of the lower Alamosa River water on alfalfa, southwestern San Luis Valley, Colorado: 1994 follow-up study","docAbstract":"<p>No abstract available.</p>","language":"English ","publisher":"U.S. Geological Survey","publisherLocation":"Reston, VA","doi":"10.3133/ofr9543","usgsCitation":"Erdman, J.A., and Smith, K.S., 1995, Impact of the lower Alamosa River water on alfalfa, southwestern San Luis Valley, Colorado: 1994 follow-up study: U.S. Geological Survey Open-File Report 95-43, 13 p., https://doi.org/10.3133/ofr9543.","productDescription":"13 p.","costCenters":[{"id":211,"text":"Crustal Geophysics and Geochemistry Science Center","active":true,"usgs":true},{"id":589,"text":"Toxic Substances Hydrology Program","active":true,"usgs":true}],"links":[{"id":151310,"rank":0,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/of/1995/0043/report-thumb.jpg"},{"id":48229,"rank":300,"type":{"id":11,"text":"Document"},"url":"https://pubs.usgs.gov/of/1995/0043/report.pdf","linkFileType":{"id":1,"text":"pdf"}}],"country":"United 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,{"id":27261,"text":"wri944224 - 1995 - Relation of precipitation quality to storm type, and deposition of dissolved chemical constituents from precipitation in Massachusetts, 1983-85","interactions":[],"lastModifiedDate":"2012-02-02T00:08:37","indexId":"wri944224","displayToPublicDate":"1995-06-01T00:00:00","publicationYear":"1995","noYear":false,"publicationType":{"id":18,"text":"Report"},"publicationSubtype":{"id":5,"text":"USGS Numbered Series"},"seriesTitle":{"id":342,"text":"Water-Resources Investigations Report","code":"WRI","active":false,"publicationSubtype":{"id":5}},"seriesNumber":"94-4224","title":"Relation of precipitation quality to storm type, and deposition of dissolved chemical constituents from precipitation in Massachusetts, 1983-85","docAbstract":"Precipitation samples were collected for 83 storms at a rural inland site in Princeton, Mass., and 73 storms at a rural coastal site in Truro, Mass., to examine the quality of precipitation from storms and relate quality to three storm types (oceanic cyclone, continental cyclone, and cold front). At the inland site, Princeton, ranked-means of precipitation depth, storm duration, specific conductance, and concentrations and loads of hydrogen, sulfate, aluminum, bromide, and copper ions were affected by storm type. At the coastal site, Truro, ranked means of precipitation depth, storm duration, and concentrations and loads of calcium, chloride, magnesium, potassium, and sodium ions were affected by storm type. Precipitation chemistry at the coastal site was 85 percent oceanic in orgin, whereas precipitation 72 kilometers inland was 60 percent hydrogen, nitrate, and sulfate ions, reflecting fossil-fuel combustion. Concentrations and loads for specific conductance and 9 chemical constituents on an annual and seasonal basis were determined from National Atmospheric Deposition Program data for spring 1983 through winter 1985 at Quabbin (rural, inland), Waltham (suburban, inland) and Truro (rural, coastal), Massachusetts. Concentrations of magnesium, potassium, sodium, and chloride concentrations were highest at the coast and much lower inland, with very little difference between Waltham and Quabbin. Loads of ammonium, nitrate, sulfate, and hydrogen are highest at Quabbin and are about equal at Waltham and Truro. About twice as much nitrate and hydrogen and about 35 percent more sulfate is deposited at Quabbin than at Waltham or Truro; this pattern indicates that the interior of Massachusetts receives more acidic precipitation than do the eastern or the coastal areas of Massachusetts.","language":"ENGLISH","publisher":"U.S. Geological Survey ;\r\nUSGS Earth Science Information Center, Open-File Reports Section [distributor],","doi":"10.3133/wri944224","usgsCitation":"Gay, F.B., and Melching, C., 1995, Relation of precipitation quality to storm type, and deposition of dissolved chemical constituents from precipitation in Massachusetts, 1983-85: U.S. Geological Survey Water-Resources Investigations Report 94-4224, vi, 82 p. :ill., maps ;28 cm., https://doi.org/10.3133/wri944224.","productDescription":"vi, 82 p. :ill., maps ;28 cm.","costCenters":[],"links":[{"id":158613,"rank":0,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/wri/1994/4224/report-thumb.jpg"},{"id":56136,"rank":300,"type":{"id":11,"text":"Document"},"url":"https://pubs.usgs.gov/wri/1994/4224/report.pdf","linkFileType":{"id":1,"text":"pdf"}}],"noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"4f4e48cfe4b07f02db545a87","contributors":{"authors":[{"text":"Gay, F. B.","contributorId":55002,"corporation":false,"usgs":true,"family":"Gay","given":"F.","email":"","middleInitial":"B.","affiliations":[],"preferred":false,"id":197817,"contributorType":{"id":1,"text":"Authors"},"rank":1},{"text":"Melching, Charles S.","contributorId":23973,"corporation":false,"usgs":true,"family":"Melching","given":"Charles S.","affiliations":[],"preferred":false,"id":197816,"contributorType":{"id":1,"text":"Authors"},"rank":2}]}}
,{"id":62827,"text":"gq1759 - 1995 - Geologic map of the Scarecrow Peak quadrangle, Washington County, Utah, and Lincoln County, Nevada","interactions":[],"lastModifiedDate":"2012-02-10T00:10:39","indexId":"gq1759","displayToPublicDate":"1995-06-01T00:00:00","publicationYear":"1995","noYear":false,"publicationType":{"id":18,"text":"Report"},"publicationSubtype":{"id":5,"text":"USGS Numbered Series"},"seriesTitle":{"id":316,"text":"Geologic Quadrangle","code":"GQ","active":false,"publicationSubtype":{"id":5}},"seriesNumber":"1759","title":"Geologic map of the Scarecrow Peak quadrangle, Washington County, Utah, and Lincoln County, Nevada","language":"ENGLISH","doi":"10.3133/gq1759","usgsCitation":"Hintze, L.F., and Axen, G.J., 1995, Geologic map of the Scarecrow Peak quadrangle, Washington County, Utah, and Lincoln County, Nevada: U.S. Geological Survey Geologic Quadrangle 1759, 1 map :col. ;58 x 46 cm., on sheet 81 x 112 cm., folded in envelope 30 x 24 cm., https://doi.org/10.3133/gq1759.","productDescription":"1 map :col. ;58 x 46 cm., on sheet 81 x 112 cm., folded in envelope 30 x 24 cm.","costCenters":[],"links":[{"id":101965,"rank":700,"type":{"id":15,"text":"Index Page"},"url":"https://ngmdb.usgs.gov/Prodesc/proddesc_307.htm","linkFileType":{"id":5,"text":"html"},"description":"307"},{"id":248975,"rank":300,"type":{"id":11,"text":"Document"},"url":"https://pubs.usgs.gov/gq/1759/report.pdf","size":"27","linkFileType":{"id":1,"text":"pdf"}},{"id":251648,"rank":0,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/gq/1759/report-thumb.jpg"}],"scale":"24000","geographicExtents":"{ \"type\": \"FeatureCollection\", \"features\": [ { \"type\": \"Feature\", \"properties\": {}, \"geometry\": { \"type\": \"Polygon\", \"coordinates\": [ [ [ -114.11749999999999,37.1175 ], [ -114.11749999999999,37.25 ], [ -114,37.25 ], [ -114,37.1175 ], [ -114.11749999999999,37.1175 ] ] ] } } ] }","noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"4f4e4ae6e4b07f02db68b4fc","contributors":{"authors":[{"text":"Hintze, Lehi F.","contributorId":104057,"corporation":false,"usgs":true,"family":"Hintze","given":"Lehi","email":"","middleInitial":"F.","affiliations":[],"preferred":false,"id":267918,"contributorType":{"id":1,"text":"Authors"},"rank":1},{"text":"Axen, Gary J.","contributorId":49040,"corporation":false,"usgs":true,"family":"Axen","given":"Gary","email":"","middleInitial":"J.","affiliations":[],"preferred":false,"id":267917,"contributorType":{"id":1,"text":"Authors"},"rank":2}]}}
,{"id":4101,"text":"cir1109 - 1995 - Geomagnetism applications","interactions":[],"lastModifiedDate":"2012-02-02T00:05:39","indexId":"cir1109","displayToPublicDate":"1995-06-01T00:00:00","publicationYear":"1995","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":"1109","title":"Geomagnetism applications","docAbstract":"The social uses of geomagnetism include the physics of the space environment, satellite damage, pipeline corrosion, electric power-grid failure, communication interference, global positioning disruption, mineral-resource detection, interpretation of the Earth's formation and structure, navigation, weather, and magnetoreception in organisms. The need for continuing observations of the geomagnetic field, together with careful archiving of these records and mechanisms for dissemination of these data, is emphasized.","language":"ENGLISH","publisher":"U.S. G.P.O. ;\r\nU.S. Geological Survey, Information Services,","doi":"10.3133/cir1109","usgsCitation":"Campbell, W.H., 1995, Geomagnetism applications: U.S. Geological Survey Circular 1109, iv, 31 p. :ill., maps ;28 cm., https://doi.org/10.3133/cir1109.","productDescription":"iv, 31 p. :ill., maps ;28 cm.","costCenters":[],"links":[{"id":121269,"rank":0,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/circ/1995/1109/report-thumb.jpg"},{"id":31205,"rank":300,"type":{"id":11,"text":"Document"},"url":"https://pubs.usgs.gov/circ/1995/1109/report.pdf","linkFileType":{"id":1,"text":"pdf"}}],"noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"4f4e4ac9e4b07f02db67c5ea","contributors":{"authors":[{"text":"Campbell, Wallace H.","contributorId":52557,"corporation":false,"usgs":true,"family":"Campbell","given":"Wallace","email":"","middleInitial":"H.","affiliations":[],"preferred":false,"id":148189,"contributorType":{"id":1,"text":"Authors"},"rank":1}]}}
,{"id":70185361,"text":"70185361 - 1995 - Chemical evolution of groundwater near a sinkhole lake, northern Florida: 2. Chemical patterns, mass-transfer modeling, and rates of chemical reactions","interactions":[],"lastModifiedDate":"2018-03-21T15:06:46","indexId":"70185361","displayToPublicDate":"1995-06-01T00:00:00","publicationYear":"1995","noYear":false,"publicationType":{"id":2,"text":"Article"},"publicationSubtype":{"id":10,"text":"Journal Article"},"seriesTitle":{"id":3722,"text":"Water Resources Research","onlineIssn":"1944-7973","printIssn":"0043-1397","active":true,"publicationSubtype":{"id":10}},"title":"Chemical evolution of groundwater near a sinkhole lake, northern Florida: 2. Chemical patterns, mass-transfer modeling, and rates of chemical reactions","docAbstract":"<p><span>Chemical patterns along evolutionary groundwater flow paths in silicate and carbonate aquifers were interpreted using solute tracers, carbon and sulfur isotopes, and mass balance reaction modeling for a complex hydrologic system involving groundwater inflow to and outflow from a sinkhole lake in northern Florida. Rates of dominant reactions along defined flow paths were estimated from modeled mass transfer and ages obtained from CFC-modeled recharge dates. Groundwater upgradient from Lake Barco remains oxic as it moves downward, reacting with silicate minerals in a system open to carbon dioxide (CO</span><sub>2</sub><span>), producing only small increases in dissolved species. Beneath and downgradient of Lake Barco the oxic groundwater mixes with lake water leakage in a highly reducing, silicate-carbonate mineral environment. A mixing model, developed for anoxic groundwater downgradient from the lake, accounted for the observed chemical and isotopic composition by combining different proportions of lake water leakage and infiltrating meteoric water. The evolution of major ion chemistry and the<span>&nbsp;</span></span><sup>13</sup><span>C isotopic composition of dissolved carbon species in groundwater downgradient from the lake can be explained by the aerobic oxidation of organic matter in the lake, anaerobic microbial oxidation of organic carbon, and incongruent dissolution of smectite minerals to kaolinite. The dominant process for the generation of methane was by the CO</span><sub>2</sub><span><span>&nbsp;</span>reduction pathway based on the isotopic composition of hydrogen (δ</span><sup>2</sup><span>H(CH</span><sub>4</sub><span>) = −186 to −234‰) and carbon (δ</span><sup>13</sup><span>C(CH</span><sub>4</sub><span>) = −65.7 to −72.3‰). Rates of microbial metabolism of organic matter, estimated from the mass transfer reaction models, ranged from 0.0047 to 0.039 mmol L</span><sup>−1</sup><span><span>&nbsp;</span>yr</span><sup>−1</sup><span><span>&nbsp;</span>for groundwater downgradient from the lake.</span></p>","language":"English","publisher":"American Geophysical Union","doi":"10.1029/95WR00220","usgsCitation":"Katz, B.G., Plummer, N., Busenberg, E., Revesz, K.M., Jones, B.F., and Lee, T.M., 1995, Chemical evolution of groundwater near a sinkhole lake, northern Florida: 2. Chemical patterns, mass-transfer modeling, and rates of chemical reactions: Water Resources Research, v. 31, no. 6, p. 1565-1584, https://doi.org/10.1029/95WR00220.","productDescription":"20 p. ","startPage":"1565","endPage":"1584","costCenters":[{"id":589,"text":"Toxic Substances Hydrology Program","active":true,"usgs":true}],"links":[{"id":337922,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/thumbnails/outside_thumb.jpg"}],"volume":"31","issue":"6","noUsgsAuthors":false,"publicationDate":"2010-07-09","publicationStatus":"PW","scienceBaseUri":"58d23b93e4b0236b68f8291a","contributors":{"authors":[{"text":"Katz, Brian G. bkatz@usgs.gov","contributorId":1093,"corporation":false,"usgs":true,"family":"Katz","given":"Brian","email":"bkatz@usgs.gov","middleInitial":"G.","affiliations":[],"preferred":true,"id":685329,"contributorType":{"id":1,"text":"Authors"},"rank":1},{"text":"Plummer, Niel 0000-0002-4020-1013 nplummer@usgs.gov","orcid":"https://orcid.org/0000-0002-4020-1013","contributorId":190100,"corporation":false,"usgs":true,"family":"Plummer","given":"Niel","email":"nplummer@usgs.gov","affiliations":[{"id":436,"text":"National Research Program - Eastern Branch","active":true,"usgs":true}],"preferred":true,"id":685330,"contributorType":{"id":1,"text":"Authors"},"rank":2},{"text":"Busenberg, Eurybiades ebusenbe@usgs.gov","contributorId":2271,"corporation":false,"usgs":true,"family":"Busenberg","given":"Eurybiades","email":"ebusenbe@usgs.gov","affiliations":[{"id":436,"text":"National Research Program - Eastern Branch","active":true,"usgs":true}],"preferred":true,"id":685331,"contributorType":{"id":1,"text":"Authors"},"rank":3},{"text":"Revesz, Kinga M. krevesz@usgs.gov","contributorId":506,"corporation":false,"usgs":true,"family":"Revesz","given":"Kinga","email":"krevesz@usgs.gov","middleInitial":"M.","affiliations":[],"preferred":true,"id":685332,"contributorType":{"id":1,"text":"Authors"},"rank":4},{"text":"Jones, Blair F. bfjones@usgs.gov","contributorId":2784,"corporation":false,"usgs":true,"family":"Jones","given":"Blair","email":"bfjones@usgs.gov","middleInitial":"F.","affiliations":[{"id":436,"text":"National Research Program - Eastern Branch","active":true,"usgs":true}],"preferred":true,"id":685333,"contributorType":{"id":1,"text":"Authors"},"rank":5},{"text":"Lee, Terrie M. tmlee@usgs.gov","contributorId":2461,"corporation":false,"usgs":true,"family":"Lee","given":"Terrie","email":"tmlee@usgs.gov","middleInitial":"M.","affiliations":[],"preferred":true,"id":685334,"contributorType":{"id":1,"text":"Authors"},"rank":6}]}}
,{"id":70185359,"text":"70185359 - 1995 - Chemical evolution of groundwater near a sinkhole lake, northern Florida: 1. Flow patterns, age of groundwater, and influence of lakewater leakage","interactions":[],"lastModifiedDate":"2018-03-21T15:06:56","indexId":"70185359","displayToPublicDate":"1995-06-01T00:00:00","publicationYear":"1995","noYear":false,"publicationType":{"id":2,"text":"Article"},"publicationSubtype":{"id":10,"text":"Journal Article"},"seriesTitle":{"id":3722,"text":"Water Resources Research","onlineIssn":"1944-7973","printIssn":"0043-1397","active":true,"publicationSubtype":{"id":10}},"title":"Chemical evolution of groundwater near a sinkhole lake, northern Florida: 1. Flow patterns, age of groundwater, and influence of lakewater leakage","docAbstract":"<p><span>Leakage from sinkhole lakes significantly influences recharge to the Upper Floridan aquifer in poorly confined sediments in northern Florida. Environmental isotopes (oxygen 18, deuterium, and tritium), chlorofluorocarbons (CFCs: CFC-11, CCl</span><sub>3</sub><span>F; CFC-12, CCl</span><sub>2</sub><span>F</span><sub>2</sub><span>; and CFC-113, C</span><sub>2</sub><span>Cl</span><sub>3</sub><span>F</span><sub>3</sub><span>), and solute tracers were used to investigate groundwater flow patterns near Lake Barco, a seepage lake in a mantled karst setting in northern Florida. Stable isotope data indicated that the groundwater downgradient from the lake contained 11–67% lake water leakage, with a limit of detection of lake water in groundwater of 4.3%. The mixing fractions of lake water leakage, which passed through organic-rich sediments in the lake bottom, were directly proportional to the observed methane concentrations and increased with depth in the groundwater flow system. In aerobic groundwater upgradient from Lake Barco, CFC-modeled recharge dates ranged from 1987 near the water table to the mid 1970s for water collected at a depth of 30 m below the water table. CFC-modeled recharge dates (based on CFC-12) for anaerobic groundwater downgradient from the lake ranged from the late 1950s to the mid 1970s and were consistent with tritium data. CFC-modeled recharge dates based on CFC-11 indicated preferential microbial degradation in anoxic waters. Vertical hydraulic conductivities, calculated using CFC-12 modeled recharge dates and Darcy's law, were 0.17, 0.033, and 0.019 m/d for the surficial aquifer, intermediate confining unit, and lake sediments, respectively. These conductivities agreed closely with those used in the calibration of a three-dimensional groundwater flow model for transient and steady state flow conditions.</span></p>","language":"English","publisher":"American Geophysical Union","doi":"10.1029/95WR00221","usgsCitation":"Katz, B.G., Lee, T.M., Plummer, N., and Busenberg, E., 1995, Chemical evolution of groundwater near a sinkhole lake, northern Florida: 1. Flow patterns, age of groundwater, and influence of lakewater leakage: Water Resources Research, v. 31, no. 6, p. 1549-1564, https://doi.org/10.1029/95WR00221.","productDescription":"16 p. ","startPage":"1549","endPage":"1564","costCenters":[{"id":589,"text":"Toxic Substances Hydrology Program","active":true,"usgs":true}],"links":[{"id":337921,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/thumbnails/outside_thumb.jpg"}],"country":"United States","state":"Florida","otherGeospatial":"Lake Barco","geographicExtents":"{\n  \"type\": \"FeatureCollection\",\n  \"features\": [\n    {\n      \"type\": \"Feature\",\n      \"properties\": {},\n      \"geometry\": {\n        \"type\": \"Polygon\",\n        \"coordinates\": [\n          [\n            [\n              -82.00907707214355,\n              29.67850809103362\n            ],\n            [\n              -82.01105117797852,\n              29.675599772669415\n            ],\n            [\n              -82.00924873352051,\n              29.674182869145277\n            ],\n            [\n              -82.00693130493164,\n              29.674257443512726\n            ],\n            [\n              -82.00590133666992,\n              29.675823492453357\n            ],\n            [\n              -82.00624465942383,\n              29.67761323280481\n            ],\n            [\n              -82.00761795043945,\n              29.67835894854861\n            ],\n            [\n              -82.00907707214355,\n              29.67850809103362\n            ]\n          ]\n        ]\n      }\n    }\n  ]\n}","volume":"31","issue":"6","noUsgsAuthors":false,"publicationDate":"2010-07-09","publicationStatus":"PW","scienceBaseUri":"58d23b94e4b0236b68f8291c","contributors":{"authors":[{"text":"Katz, Brian G. bkatz@usgs.gov","contributorId":1093,"corporation":false,"usgs":true,"family":"Katz","given":"Brian","email":"bkatz@usgs.gov","middleInitial":"G.","affiliations":[],"preferred":true,"id":685316,"contributorType":{"id":1,"text":"Authors"},"rank":1},{"text":"Lee, Terrie M. tmlee@usgs.gov","contributorId":2461,"corporation":false,"usgs":true,"family":"Lee","given":"Terrie","email":"tmlee@usgs.gov","middleInitial":"M.","affiliations":[],"preferred":true,"id":685317,"contributorType":{"id":1,"text":"Authors"},"rank":2},{"text":"Plummer, Niel 0000-0002-4020-1013 nplummer@usgs.gov","orcid":"https://orcid.org/0000-0002-4020-1013","contributorId":190100,"corporation":false,"usgs":true,"family":"Plummer","given":"Niel","email":"nplummer@usgs.gov","affiliations":[{"id":436,"text":"National Research Program - Eastern Branch","active":true,"usgs":true}],"preferred":true,"id":685318,"contributorType":{"id":1,"text":"Authors"},"rank":3},{"text":"Busenberg, Eurybiades ebusenbe@usgs.gov","contributorId":2271,"corporation":false,"usgs":true,"family":"Busenberg","given":"Eurybiades","email":"ebusenbe@usgs.gov","affiliations":[{"id":436,"text":"National Research Program - Eastern Branch","active":true,"usgs":true}],"preferred":true,"id":685319,"contributorType":{"id":1,"text":"Authors"},"rank":4}]}}
,{"id":20877,"text":"ofr94475 - 1995 - Water, energy, and biogeochemical budget research at Sleepers River Research Watershed, Vermont","interactions":[],"lastModifiedDate":"2012-02-02T00:07:53","indexId":"ofr94475","displayToPublicDate":"1995-06-01T00:00:00","publicationYear":"1995","noYear":false,"publicationType":{"id":18,"text":"Report"},"publicationSubtype":{"id":5,"text":"USGS Numbered Series"},"seriesTitle":{"id":330,"text":"Open-File Report","code":"OFR","onlineIssn":"2331-1258","printIssn":"0196-1497","active":true,"publicationSubtype":{"id":5}},"seriesNumber":"94-475","title":"Water, energy, and biogeochemical budget research at Sleepers River Research Watershed, Vermont","docAbstract":"The U.S. Geological Survey has selected the Sleepers River Research Watershed (Sleepers River) near Danville, Vt., as one of five sites for the investigation of Water, Energy, and Biogeochemical Budgets (WEBB). Sleepers River was chosen because it is a well-designed outdoor laboratory with a long history of hydrologic data collection and research, and also because it provides an ideal opportunity for collaboration among the U.S. Geological Survey, other Federal agencies, and universities at the site. The multiple subwatersheds at Sleepers River present a unique opportunity to investigate hydrologic, energy, and biogeochemical processes over a variety of spatial scales. This WEBB study builds on fundamental research on process mechanisms and rates at the plot scale (in this case, a hillslope). Results then are scaled up to interpret the hydrochemical response of first- and higher- order basins. Five research elements make up the Sleepers River WEBB project. Individually, each of the five elements is designed to investigate specific WEBB processes (such as CO2 efflux through a snowpack), address specific WEBB issues (such as scaling and flowpaths), or apply specific WEBB approaches (such as integrated chemical and physical study of a hillslope). The research elements overlap so that many of the processes investigated will be assessed in more than one way, thus allowing independent verification of research results. For example, flowpath information will be derived separately by use of isotopic tracers, conservative chemical solutes, and soil-moisture fluxes. Collectively, the five elements constitute an integrated approach to a comprehensive understanding of WEBB processes needed for the prediction of the effects of global change.","language":"ENGLISH","publisher":"U.S. Geological Survey ;\r\nOpen-File Reports Section [distributor],","doi":"10.3133/ofr94475","usgsCitation":"Shanley, J.B., Sundquist, E., and Kendall, C., 1995, Water, energy, and biogeochemical budget research at Sleepers River Research Watershed, Vermont: U.S. Geological Survey Open-File Report 94-475, iv, 22 p. :ill., map ;28 cm., https://doi.org/10.3133/ofr94475.","productDescription":"iv, 22 p. :ill., map ;28 cm.","costCenters":[],"links":[{"id":154841,"rank":0,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/of/1994/0475/report-thumb.jpg"},{"id":50472,"rank":300,"type":{"id":11,"text":"Document"},"url":"https://pubs.usgs.gov/of/1994/0475/report.pdf","linkFileType":{"id":1,"text":"pdf"}}],"noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"4f4e4a0de4b07f02db5fd156","contributors":{"authors":[{"text":"Shanley, James B. 0000-0002-4234-3437 jshanley@usgs.gov","orcid":"https://orcid.org/0000-0002-4234-3437","contributorId":1953,"corporation":false,"usgs":true,"family":"Shanley","given":"James","email":"jshanley@usgs.gov","middleInitial":"B.","affiliations":[{"id":405,"text":"NH/VT office of New England Water Science Center","active":true,"usgs":true},{"id":466,"text":"New England Water Science Center","active":true,"usgs":true}],"preferred":true,"id":183424,"contributorType":{"id":1,"text":"Authors"},"rank":1},{"text":"Sundquist, E.T.","contributorId":13990,"corporation":false,"usgs":true,"family":"Sundquist","given":"E.T.","email":"","affiliations":[],"preferred":false,"id":183425,"contributorType":{"id":1,"text":"Authors"},"rank":2},{"text":"Kendall, Carol 0000-0002-0247-3405 ckendall@usgs.gov","orcid":"https://orcid.org/0000-0002-0247-3405","contributorId":1462,"corporation":false,"usgs":true,"family":"Kendall","given":"Carol","email":"ckendall@usgs.gov","affiliations":[{"id":438,"text":"National Research Program - Western Branch","active":true,"usgs":true}],"preferred":true,"id":183423,"contributorType":{"id":1,"text":"Authors"},"rank":3}]}}
,{"id":38209,"text":"pp1538I - 1995 - Characterization of the Cottonwood Grove and Ridgely faults near Reelfoot Lake, Tennessee, from high-resolution seismic reflection data","interactions":[],"lastModifiedDate":"2012-02-02T00:10:01","indexId":"pp1538I","displayToPublicDate":"1995-06-01T00:00:00","publicationYear":"1995","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":"1538","chapter":"I","title":"Characterization of the Cottonwood Grove and Ridgely faults near Reelfoot Lake, Tennessee, from high-resolution seismic reflection data","docAbstract":"In the winter of 1811-12, three of the largest historic earthquakes in the United States occurred near New Madrid, Missouri. Seismicity continues to the present day throughout a tightly clustered pattern of epicenters centered on the bootheel of Missouri, including parts of northeastern Arkansas, northwestern Tennessee, western Kentucky, and southern Illinois. In 1990, the New Madrid seismic zone/Central United States became the first seismically active region east of the Rocky Mountains to be designated a priority research area within the National Earthquake Hazards Reduction Program (NEHRP). This Professional Paper is a collection of papers, some published separately, presenting results of the newly intensified research program in this area. Major components of this research program include tectonic framework studies, seismicity and deformation monitoring and modeling, improved seismic hazard and risk assessments, and cooperative hazard mitigation studies.","language":"ENGLISH","doi":"10.3133/pp1538I","usgsCitation":"Stephenson, W.J., Shedlock, K.M., and Odum, J.K., 1995, Characterization of the Cottonwood Grove and Ridgely faults near Reelfoot Lake, Tennessee, from high-resolution seismic reflection data: U.S. Geological Survey Professional Paper 1538, p. I1-I10, https://doi.org/10.3133/pp1538I.","productDescription":"p. I1-I10","costCenters":[],"links":[{"id":123991,"rank":0,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/pp/1538i/report-thumb.jpg"},{"id":64512,"rank":300,"type":{"id":11,"text":"Document"},"url":"https://pubs.usgs.gov/pp/1538i/report.pdf","linkFileType":{"id":1,"text":"pdf"}}],"noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"4f4e49e2e4b07f02db5e4d0d","contributors":{"authors":[{"text":"Stephenson, William J. 0000-0001-8699-0786 wstephens@usgs.gov","orcid":"https://orcid.org/0000-0001-8699-0786","contributorId":695,"corporation":false,"usgs":true,"family":"Stephenson","given":"William","email":"wstephens@usgs.gov","middleInitial":"J.","affiliations":[{"id":300,"text":"Geologic Hazards Science Center","active":true,"usgs":true}],"preferred":true,"id":219336,"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":219337,"contributorType":{"id":1,"text":"Authors"},"rank":2},{"text":"Odum, Jack K. 0000-0002-3162-0355","orcid":"https://orcid.org/0000-0002-3162-0355","contributorId":97900,"corporation":false,"usgs":true,"family":"Odum","given":"Jack","email":"","middleInitial":"K.","affiliations":[],"preferred":false,"id":219338,"contributorType":{"id":1,"text":"Authors"},"rank":3}]}}
,{"id":35946,"text":"b2120 - 1995 - The \"checkerboard method\"; a new way to estimate the numbers of undiscovered hydrocarbon accumulations in sparsely drilled areas","interactions":[],"lastModifiedDate":"2012-02-02T00:09:35","indexId":"b2120","displayToPublicDate":"1995-06-01T00:00:00","publicationYear":"1995","noYear":false,"publicationType":{"id":18,"text":"Report"},"publicationSubtype":{"id":5,"text":"USGS Numbered Series"},"seriesTitle":{"id":306,"text":"Bulletin","code":"B","active":false,"publicationSubtype":{"id":5}},"seriesNumber":"2120","title":"The \"checkerboard method\"; a new way to estimate the numbers of undiscovered hydrocarbon accumulations in sparsely drilled areas","language":"ENGLISH","publisher":"U.S. G.P.O. ; For sale by U.S. Geological Survey, Information Services,","doi":"10.3133/b2120","usgsCitation":"Stanley, R.G., 1995, The \"checkerboard method\"; a new way to estimate the numbers of undiscovered hydrocarbon accumulations in sparsely drilled areas: U.S. Geological Survey Bulletin 2120, iii, 8 p. :maps ;28 cm., https://doi.org/10.3133/b2120.","productDescription":"iii, 8 p. :maps ;28 cm.","costCenters":[],"links":[{"id":166436,"rank":0,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/bul/2120/report-thumb.jpg"},{"id":63901,"rank":300,"type":{"id":11,"text":"Document"},"url":"https://pubs.usgs.gov/bul/2120/report.pdf","linkFileType":{"id":1,"text":"pdf"}}],"noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"4f4e4ad5e4b07f02db6836ef","contributors":{"authors":[{"text":"Stanley, Richard G. 0000-0001-6192-8783 rstanley@usgs.gov","orcid":"https://orcid.org/0000-0001-6192-8783","contributorId":1832,"corporation":false,"usgs":true,"family":"Stanley","given":"Richard","email":"rstanley@usgs.gov","middleInitial":"G.","affiliations":[{"id":312,"text":"Geology, Minerals, Energy, and Geophysics Science Center","active":true,"usgs":true}],"preferred":true,"id":215495,"contributorType":{"id":1,"text":"Authors"},"rank":1}]}}
,{"id":1001180,"text":"1001180 - 1995 - U.S. Fish and Wildlife Service 1979 wetland classification: A review","interactions":[],"lastModifiedDate":"2026-03-13T15:52:43.746672","indexId":"1001180","displayToPublicDate":"1995-06-01T00:00:00","publicationYear":"1995","noYear":false,"publicationType":{"id":2,"text":"Article"},"publicationSubtype":{"id":10,"text":"Journal Article"},"seriesTitle":{"id":3676,"text":"Vegetatio","active":true,"publicationSubtype":{"id":10}},"title":"U.S. Fish and Wildlife Service 1979 wetland classification: A review","docAbstract":"In 1979 the US Fish and Wildlife Service published and adopted a classification of wetlands and deepwater habitats of the United States. The system was designed for use in a national inventory of wetlands. It was intended to be ecologically based, to furnish the mapping units needed for the inventory, and to provide national consistency in terminology and definition. We review the performance of the classification after 13 years of use. The definition of wetland is based on national lists of hydric soils and plants that occur in wetlands. Our experience suggests that wetland classifications must facilitate mapping and inventory because these data gathering functions are essential to management and preservation of the wetland resource, but the definitions and taxa must have ecological basis. The most serious problem faced in construction of the classification was lack of data for many of the diverse wetland types. Review of the performance of the classification suggests that, for the most part, it was successful in accomplishing its objectives, but that problem areas should be corrected and modification could strengthen its utility. The classification, at least in concept, could be applied outside the United States. Experience gained in use of the classification can furnish guidance as to pitfalls to be avoided in the wetland classification process.","language":"English","publisher":"Springer Nature","doi":"10.1007/BF00045196","usgsCitation":"Cowardin, L., and Golet, F., 1995, U.S. Fish and Wildlife Service 1979 wetland classification: A review: Vegetatio, v. 118, no. 1-2, p. 139-152, https://doi.org/10.1007/BF00045196.","productDescription":"14 p.","startPage":"139","endPage":"152","costCenters":[{"id":480,"text":"Northern Prairie Wildlife Research Center","active":true,"usgs":true}],"links":[{"id":501644,"rank":2,"type":{"id":41,"text":"Open Access External Repository Page"},"url":"https://digitalcommons.uri.edu/nrs_facpubs/101","text":"External Repository"},{"id":133764,"rank":1,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/thumbnails/outside_thumb.jpg"}],"volume":"118","issue":"1-2","noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"4f4e49d5e4b07f02db5ddc12","contributors":{"authors":[{"text":"Cowardin, L.M.","contributorId":106435,"corporation":false,"usgs":true,"family":"Cowardin","given":"L.M.","email":"","affiliations":[],"preferred":false,"id":310664,"contributorType":{"id":1,"text":"Authors"},"rank":1},{"text":"Golet, F.C.","contributorId":32124,"corporation":false,"usgs":true,"family":"Golet","given":"F.C.","email":"","affiliations":[],"preferred":false,"id":310663,"contributorType":{"id":1,"text":"Authors"},"rank":2}]}}
,{"id":17114,"text":"ofr9517 - 1995 - Final report: Acoustic mapping of dredged material disposal sites and deposits in Mamala Bay, Honolulu, Hawaii","interactions":[],"lastModifiedDate":"2021-12-17T20:46:26.7757","indexId":"ofr9517","displayToPublicDate":"1995-06-01T00:00:00","publicationYear":"1995","noYear":false,"publicationType":{"id":18,"text":"Report"},"publicationSubtype":{"id":5,"text":"USGS Numbered Series"},"seriesTitle":{"id":330,"text":"Open-File Report","code":"OFR","onlineIssn":"2331-1258","printIssn":"0196-1497","active":true,"publicationSubtype":{"id":5}},"seriesNumber":"95-17","title":"Final report: Acoustic mapping of dredged material disposal sites and deposits in Mamala Bay, Honolulu, Hawaii","docAbstract":"<p>No abstract available.</p>","language":"English","publisher":"U.S. Geological Survey","doi":"10.3133/ofr9517","usgsCitation":"Torresan, M.E., Hampton, M.A., Gowen, M.H., Barber, J., Zink, L.L., Chase, T.E., Wong, F.L., Gann, J.T., and Dartnell, P., 1995, Final report: Acoustic mapping of dredged material disposal sites and deposits in Mamala Bay, Honolulu, Hawaii: U.S. Geological Survey Open-File Report 95-17, HTML Document, https://doi.org/10.3133/ofr9517.","productDescription":"HTML Document","costCenters":[{"id":520,"text":"Pacific Coastal and Marine Science Center","active":true,"usgs":true}],"links":[{"id":393057,"rank":4,"type":{"id":36,"text":"NGMDB Index Page"},"url":"https://ngmdb.usgs.gov/Prodesc/proddesc_18375.htm"},{"id":46238,"rank":300,"type":{"id":11,"text":"Document"},"url":"https://pubs.usgs.gov/of/1995/0017/report.pdf","linkFileType":{"id":1,"text":"pdf"}},{"id":150187,"rank":0,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/of/1995/0017/report-thumb.jpg"},{"id":1010,"rank":100,"type":{"id":15,"text":"Index Page"},"url":"https://pubs.usgs.gov/of/1995/of95-017/","linkFileType":{"id":5,"text":"html"}}],"country":"United States","state":"Hawaii","city":"Honululu","otherGeospatial":"Mamala Bay","geographicExtents":"{\n  \"type\": \"FeatureCollection\",\n  \"features\": [\n    {\n      \"type\": \"Feature\",\n      \"properties\": {},\n      \"geometry\": {\n        \"type\": \"Polygon\",\n        \"coordinates\": [\n          [\n            [\n              -158.11866760253906,\n              21.22474159644541\n            ],\n            [\n              -157.79457092285156,\n              21.22474159644541\n            ],\n            [\n              -157.79457092285156,\n              21.341827593336323\n            ],\n            [\n              -158.11866760253906,\n              21.341827593336323\n            ],\n            [\n              -158.11866760253906,\n              21.22474159644541\n            ]\n          ]\n        ]\n      }\n    }\n  ]\n}","noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"4f4e4abbe4b07f02db67244c","contributors":{"authors":[{"text":"Torresan, Michael E. mtorresan@usgs.gov","contributorId":4392,"corporation":false,"usgs":true,"family":"Torresan","given":"Michael","email":"mtorresan@usgs.gov","middleInitial":"E.","affiliations":[],"preferred":true,"id":174975,"contributorType":{"id":1,"text":"Authors"},"rank":1},{"text":"Hampton, M. 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,{"id":38210,"text":"pp1538O - 1995 - Reflection seismic profiling of the Wabash Valley fault system in the Illinois Basin","interactions":[],"lastModifiedDate":"2012-02-02T00:10:01","indexId":"pp1538O","displayToPublicDate":"1995-06-01T00:00:00","publicationYear":"1995","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":"1538","chapter":"O","title":"Reflection seismic profiling of the Wabash Valley fault system in the Illinois Basin","language":"ENGLISH","doi":"10.3133/pp1538O","usgsCitation":"Rene, R., and Stanonis, F., 1995, Reflection seismic profiling of the Wabash Valley fault system in the Illinois Basin: U.S. Geological Survey Professional Paper 1538, p. O1-O33, https://doi.org/10.3133/pp1538O.","productDescription":"p. O1-O33","costCenters":[],"links":[{"id":119215,"rank":0,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/pp/1538o/report-thumb.jpg"},{"id":64513,"rank":300,"type":{"id":11,"text":"Document"},"url":"https://pubs.usgs.gov/pp/1538o/report.pdf","linkFileType":{"id":1,"text":"pdf"}}],"noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"4f4e4a60e4b07f02db63510d","contributors":{"authors":[{"text":"Rene, R.M.","contributorId":9312,"corporation":false,"usgs":true,"family":"Rene","given":"R.M.","email":"","affiliations":[],"preferred":false,"id":219339,"contributorType":{"id":1,"text":"Authors"},"rank":1},{"text":"Stanonis, F.L.","contributorId":37791,"corporation":false,"usgs":true,"family":"Stanonis","given":"F.L.","email":"","affiliations":[],"preferred":false,"id":219340,"contributorType":{"id":1,"text":"Authors"},"rank":2}]}}
,{"id":60069,"text":"mf2282 - 1995 - Geologic map of the McCarty Park Quadrangle, Costilla and Huerfano counties, Colorado","interactions":[],"lastModifiedDate":"2012-02-10T00:10:34","indexId":"mf2282","displayToPublicDate":"1995-06-01T00:00:00","publicationYear":"1995","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":"2282","title":"Geologic map of the McCarty Park Quadrangle, Costilla and Huerfano counties, Colorado","language":"ENGLISH","doi":"10.3133/mf2282","usgsCitation":"Lindsey, D.A., 1995, Geologic map of the McCarty Park Quadrangle, Costilla and Huerfano counties, Colorado: U.S. Geological Survey Miscellaneous Field Studies Map 2282, 1 map ;58 x 46 cm., on sheet 94 x 127 cm., folded in envelope 30 x 24 cm., https://doi.org/10.3133/mf2282.","productDescription":"1 map ;58 x 46 cm., on sheet 94 x 127 cm., folded in envelope 30 x 24 cm.","costCenters":[],"links":[{"id":105335,"rank":700,"type":{"id":15,"text":"Index Page"},"url":"https://ngmdb.usgs.gov/Prodesc/proddesc_5902.htm","linkFileType":{"id":5,"text":"html"},"description":"5902"},{"id":180641,"rank":0,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/thumbnails/usgs_thumb.jpg"}],"scale":"0","geographicExtents":"{ \"type\": \"FeatureCollection\", \"features\": [ { \"type\": \"Feature\", \"properties\": {}, \"geometry\": { \"type\": \"Polygon\", \"coordinates\": [ [ [ -105.25,37.3675 ], [ -105.25,37.5 ], [ -105.11749999999999,37.5 ], [ -105.11749999999999,37.3675 ], [ -105.25,37.3675 ] ] ] } } ] }","noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"4f4e4afde4b07f02db696a8a","contributors":{"authors":[{"text":"Lindsey, D. A.","contributorId":49814,"corporation":false,"usgs":true,"family":"Lindsey","given":"D.","email":"","middleInitial":"A.","affiliations":[],"preferred":false,"id":263092,"contributorType":{"id":1,"text":"Authors"},"rank":1}]}}
,{"id":18312,"text":"ofr91596 - 1995 - An empirical equation for modeling rare earth element mineral-mineral partitioning; an application to mantle metasomatism","interactions":[],"lastModifiedDate":"2012-02-02T00:07:29","indexId":"ofr91596","displayToPublicDate":"1995-06-01T00:00:00","publicationYear":"1995","noYear":false,"publicationType":{"id":18,"text":"Report"},"publicationSubtype":{"id":5,"text":"USGS Numbered Series"},"seriesTitle":{"id":330,"text":"Open-File Report","code":"OFR","onlineIssn":"2331-1258","printIssn":"0196-1497","active":true,"publicationSubtype":{"id":5}},"seriesNumber":"91-596","title":"An empirical equation for modeling rare earth element mineral-mineral partitioning; an application to mantle metasomatism","language":"ENGLISH","publisher":"U.S. Geological Survey,","doi":"10.3133/ofr91596","usgsCitation":"Budahn, J.R., 1995, An empirical equation for modeling rare earth element mineral-mineral partitioning; an application to mantle metasomatism: U.S. Geological Survey Open-File Report 91-596, 44 leaves :ill. ;28 cm., https://doi.org/10.3133/ofr91596.","productDescription":"44 leaves :ill. ;28 cm.","costCenters":[],"links":[{"id":151685,"rank":0,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/of/1991/0596/report-thumb.jpg"},{"id":47660,"rank":300,"type":{"id":11,"text":"Document"},"url":"https://pubs.usgs.gov/of/1991/0596/report.pdf","linkFileType":{"id":1,"text":"pdf"}}],"noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"4f4e4ad9e4b07f02db684afa","contributors":{"authors":[{"text":"Budahn, James R. 0000-0001-9794-8882 jbudahn@usgs.gov","orcid":"https://orcid.org/0000-0001-9794-8882","contributorId":1175,"corporation":false,"usgs":true,"family":"Budahn","given":"James","email":"jbudahn@usgs.gov","middleInitial":"R.","affiliations":[{"id":171,"text":"Central Mineral and Environmental Resources Science Center","active":true,"usgs":true}],"preferred":true,"id":178891,"contributorType":{"id":1,"text":"Authors"},"rank":1}]}}
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,{"id":18653,"text":"ofr9549 - 1995 - Acetic acid leachability of lead from clinoptilolite-rich rocks that extracted heavy metals from polluted drainage water in Colorado","interactions":[],"lastModifiedDate":"2012-02-02T00:07:28","indexId":"ofr9549","displayToPublicDate":"1995-06-01T00:00:00","publicationYear":"1995","noYear":false,"publicationType":{"id":18,"text":"Report"},"publicationSubtype":{"id":5,"text":"USGS Numbered Series"},"seriesTitle":{"id":330,"text":"Open-File Report","code":"OFR","onlineIssn":"2331-1258","printIssn":"0196-1497","active":true,"publicationSubtype":{"id":5}},"seriesNumber":"95-49","title":"Acetic acid leachability of lead from clinoptilolite-rich rocks that extracted heavy metals from polluted drainage water in Colorado","language":"ENGLISH","publisher":"U.S. Geological Survey,","doi":"10.3133/ofr9549","usgsCitation":"Desborough, G.A., 1995, Acetic acid leachability of lead from clinoptilolite-rich rocks that extracted heavy metals from polluted drainage water in Colorado: U.S. Geological Survey Open-File Report 95-49, i, 10 p. ill. ;28 cm., https://doi.org/10.3133/ofr9549.","productDescription":"i, 10 p. ill. ;28 cm.","costCenters":[],"links":[{"id":151723,"rank":0,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/of/1995/0049/report-thumb.jpg"},{"id":47990,"rank":300,"type":{"id":11,"text":"Document"},"url":"https://pubs.usgs.gov/of/1995/0049/report.pdf","linkFileType":{"id":1,"text":"pdf"}}],"noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"4f4e4b13e4b07f02db6a3552","contributors":{"authors":[{"text":"Desborough, George A.","contributorId":101661,"corporation":false,"usgs":true,"family":"Desborough","given":"George","email":"","middleInitial":"A.","affiliations":[],"preferred":false,"id":179498,"contributorType":{"id":1,"text":"Authors"},"rank":1}]}}
,{"id":64642,"text":"i2474A - 1995 - West-east stratigraphic transect of Cretaceous rocks in the northern Rocky Mountains and Great Plains regions, southwestern Montana to southwestern Minnesota","interactions":[],"lastModifiedDate":"2012-02-02T00:13:05","indexId":"i2474A","displayToPublicDate":"1995-06-01T00:00:00","publicationYear":"1995","noYear":false,"publicationType":{"id":18,"text":"Report"},"publicationSubtype":{"id":5,"text":"USGS Numbered Series"},"seriesTitle":{"id":320,"text":"IMAP","code":"I","active":false,"publicationSubtype":{"id":5}},"seriesNumber":"2474","subseriesTitle":"NONE","chapter":"A","title":"West-east stratigraphic transect of Cretaceous rocks in the northern Rocky Mountains and Great Plains regions, southwestern Montana to southwestern Minnesota","language":"ENGLISH","doi":"10.3133/i2474A","usgsCitation":"Dyman, T.S., Porter, K.W., Tysdal, R.G., Cobban, W.A., Fox, J.E., Hammond, R.H., Nichols, D.J., Perry, W.J., Rice, D.D., Setterholm, D.R., Shurr, G., Haley, J.C., Lane, D.E., Anderson, S., and Campen, E.B., 1995, West-east stratigraphic transect of Cretaceous rocks in the northern Rocky Mountains and Great Plains regions, southwestern Montana to southwestern Minnesota: U.S. Geological Survey IMAP 2474, 1 section ;on sheet 97 x 138 cm., folded in envelope 30 x 24 cm., https://doi.org/10.3133/i2474A.","productDescription":"1 section ;on sheet 97 x 138 cm., folded in envelope 30 x 24 cm.","costCenters":[],"links":[{"id":107434,"rank":700,"type":{"id":15,"text":"Index Page"},"url":"https://ngmdb.usgs.gov/Prodesc/proddesc_10293.htm","linkFileType":{"id":5,"text":"html"},"description":"10293"},{"id":186887,"rank":0,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/thumbnails/usgs_thumb.jpg"}],"scale":"1000000","noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"4f4e4aa9e4b07f02db668218","contributors":{"authors":[{"text":"Dyman, T. 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