{"pageNumber":"3891","pageRowStart":"97250","pageSize":"25","recordCount":185169,"records":[{"id":63508,"text":"gp1012 - 1995 - Gravity and basin-depth maps of the Basin and Range Province, Western United States","interactions":[],"lastModifiedDate":"2019-05-13T19:46:26","indexId":"gp1012","displayToPublicDate":"1995-06-01T00:00:00","publicationYear":"1995","noYear":false,"publicationType":{"id":18,"text":"Report"},"publicationSubtype":{"id":5,"text":"USGS Numbered Series"},"seriesTitle":{"id":317,"text":"Geophysical Investigations Map","code":"GP","active":false,"publicationSubtype":{"id":5}},"seriesNumber":"1012","title":"Gravity and basin-depth maps of the Basin and Range Province, Western United States","language":"ENGLISH","doi":"10.3133/gp1012","usgsCitation":"Saltus, R.W., and Jachens, R., 1995, Gravity and basin-depth maps of the Basin and Range Province, Western United States: U.S. Geological Survey Geophysical Investigations Map 1012, 4 maps on 1 sheet :col. ;48 x 40 cm., sheet 148 x 94 cm., folded in envelope 30 x 24 cm., https://doi.org/10.3133/gp1012.","productDescription":"4 maps on 1 sheet :col. ;48 x 40 cm., sheet 148 x 94 cm., folded in envelope 30 x 24 cm.","costCenters":[{"id":615,"text":"Volcano Hazards Program","active":true,"usgs":true}],"links":[{"id":249629,"rank":300,"type":{"id":11,"text":"Document"},"url":"https://pubs.usgs.gov/gp/1012/report.pdf","size":"23","linkFileType":{"id":1,"text":"pdf"}},{"id":249630,"rank":400,"type":{"id":17,"text":"Plate"},"url":"https://pubs.usgs.gov/gp/1012/plate-1.pdf","size":"15462","linkFileType":{"id":1,"text":"pdf"}},{"id":253148,"rank":0,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/gp/1012/report-thumb.jpg"}],"scale":"2500000","geographicExtents":"{ \"type\": \"FeatureCollection\", \"features\": [ { \"type\": \"Feature\", \"properties\": {}, \"geometry\": { \"type\": \"Polygon\", \"coordinates\": [ [ [ -120,32 ], [ -120,42 ], [ -110,42 ], [ -110,32 ], [ -120,32 ] ] ] } } ] }","noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"4f4e4abae4b07f02db67226f","contributors":{"authors":[{"text":"Saltus, R. W.","contributorId":85588,"corporation":false,"usgs":true,"family":"Saltus","given":"R.","middleInitial":"W.","affiliations":[],"preferred":false,"id":269009,"contributorType":{"id":1,"text":"Authors"},"rank":1},{"text":"Jachens, R.C.","contributorId":55433,"corporation":false,"usgs":true,"family":"Jachens","given":"R.C.","email":"","affiliations":[],"preferred":false,"id":269008,"contributorType":{"id":1,"text":"Authors"},"rank":2}]}}
,{"id":6842,"text":"fs13995 - 1995 - Continuous-record network for collection of streamflow data in Massachusetts, 1994","interactions":[],"lastModifiedDate":"2012-02-02T00:05:53","indexId":"fs13995","displayToPublicDate":"1995-06-01T00:00:00","publicationYear":"1995","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":"139-95","title":"Continuous-record network for collection of streamflow data in Massachusetts, 1994","language":"ENGLISH","publisher":"U.S. Geological Survey, Water Resources Division,","doi":"10.3133/fs13995","usgsCitation":"Shepard, T., 1995, Continuous-record network for collection of streamflow data in Massachusetts, 1994: U.S. Geological Survey Fact Sheet 139-95, 1 sheet : map ; 28 cm. map ;, https://doi.org/10.3133/fs13995.","productDescription":"1 sheet : map ; 28 cm. map ;","costCenters":[],"links":[{"id":139780,"rank":0,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/thumbnails/usgs_thumb.jpg"}],"noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"4f4e4b01e4b07f02db698647","contributors":{"authors":[{"text":"Shepard, T.B.","contributorId":23534,"corporation":false,"usgs":true,"family":"Shepard","given":"T.B.","email":"","affiliations":[],"preferred":false,"id":153440,"contributorType":{"id":1,"text":"Authors"},"rank":1}]}}
,{"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":67536,"text":"i2272 - 1995 - Geologic map of Port Moller, Stepovak Bay, and Simeonof Island quadrangles, Alaska Peninsula, Alaska","interactions":[],"lastModifiedDate":"2017-01-30T08:27:33","indexId":"i2272","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":"2272","title":"Geologic map of Port Moller, Stepovak Bay, and Simeonof Island quadrangles, Alaska Peninsula, Alaska","docAbstract":"<p><span>Geologic mapping of Port Moller, Stevopak Bay, and Simeonof Island 1° by 2° quadrangles on the Alaska Peninsula was conducted as part of the Alaska Mineral Resource Assessment Program (AMRAP). Geologic observations was obtained by using helicopter overflights, vertical aerial photography, and enhanced and extensively processed Landsat imagery (York and others, 1984; Wilson and York, 1985). Helicopter-supported field investigations were conducted from Sand Point in 1982 and 1986 and from both Sand Point and Port Moller in 1985 and 1985. In addition, field work was conducted from the U.S. Geological Survey Research Vessel </span><i>Don J. Miller II</i><span> in 1983 and 1984. The mapping of Burk (1965), Kennedy and Waldron (1955), and Moore (1974) provided an excellent basis for the AMRAP mapping. The present map duplicates both Moore’s map of the outer Shumagin Islands and Kennedy and Waldron’s map of the Pavlof Volcano area with minor additions. However, important changes have been made to Burk’s pioneering work.</span></p>","language":"English","publisher":"U.S. Geological Survey","publisherLocation":"Fairbanks, AK","doi":"10.3133/i2272","usgsCitation":"Wilson, F.H., Detterman, R.L., Miller, J.W., and Case, J.E., 1995, Geologic map of Port Moller, Stepovak Bay, and Simeonof Island quadrangles, Alaska Peninsula, Alaska: U.S. Geological Survey IMAP 2272, 2 Sheets: 43.29 x 33.78 and 36.36 x 28.17 inches, https://doi.org/10.3133/i2272.","productDescription":"2 Sheets: 43.29 x 33.78 and 36.36 x 28.17 inches","costCenters":[{"id":114,"text":"Alaska Science Center","active":true,"usgs":true}],"links":[{"id":188630,"rank":0,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/thumbnails/usgs_thumb.jpg"},{"id":107356,"rank":698,"type":{"id":15,"text":"Index Page"},"url":"https://ngmdb.usgs.gov/Prodesc/proddesc_10206.htm","linkFileType":{"id":5,"text":"html"},"description":"10206"}],"scale":"250000","country":"United States","state":"Alaska","otherGeospatial":"Port Moller quadrangle, Simeonof Island quadrangle, Stepovak Bay quadrangle","geographicExtents":"{ \"type\": \"FeatureCollection\", \"features\": [ { \"type\": \"Feature\", \"properties\": {}, \"geometry\": { \"type\": \"Polygon\", \"coordinates\": [ [ [ -162,54.75 ], [ -162,56 ], [ -158.5,56 ], [ -158.5,54.75 ], [ -162,54.75 ] ] ] } } ] }","noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"4f4e4b12e4b07f02db6a2c80","contributors":{"authors":[{"text":"Wilson, Frederic H. 0000-0003-1761-6437 fwilson@usgs.gov","orcid":"https://orcid.org/0000-0003-1761-6437","contributorId":67174,"corporation":false,"usgs":true,"family":"Wilson","given":"Frederic","email":"fwilson@usgs.gov","middleInitial":"H.","affiliations":[{"id":119,"text":"Alaska Science Center Geology Minerals","active":true,"usgs":true},{"id":114,"text":"Alaska Science Center","active":true,"usgs":true}],"preferred":true,"id":276597,"contributorType":{"id":1,"text":"Authors"},"rank":1},{"text":"Detterman, Robert L.","contributorId":71526,"corporation":false,"usgs":true,"family":"Detterman","given":"Robert","email":"","middleInitial":"L.","affiliations":[],"preferred":false,"id":276600,"contributorType":{"id":1,"text":"Authors"},"rank":2},{"text":"Miller, John W.","contributorId":70357,"corporation":false,"usgs":true,"family":"Miller","given":"John","email":"","middleInitial":"W.","affiliations":[],"preferred":false,"id":276599,"contributorType":{"id":1,"text":"Authors"},"rank":3},{"text":"Case, James E.","contributorId":68702,"corporation":false,"usgs":true,"family":"Case","given":"James","email":"","middleInitial":"E.","affiliations":[],"preferred":false,"id":276598,"contributorType":{"id":1,"text":"Authors"},"rank":4}]}}
,{"id":20504,"text":"ofr9544 - 1995 - Lithology and X-ray mineralogy of the Shell 410-1 well, U.S. North Atlantic outer continental shelf","interactions":[],"lastModifiedDate":"2012-02-02T00:07:35","indexId":"ofr9544","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":"95-44","title":"Lithology and X-ray mineralogy of the Shell 410-1 well, U.S. North Atlantic outer continental shelf","language":"ENGLISH","publisher":"U.S. Geological Survey,","doi":"10.3133/ofr9544","usgsCitation":"Poppe, L., 1995, Lithology and X-ray mineralogy of the Shell 410-1 well, U.S. North Atlantic outer continental shelf: U.S. Geological Survey Open-File Report 95-44, 9 p.  :map ;28 cm., https://doi.org/10.3133/ofr9544.","productDescription":"9 p.  :map ;28 cm.","costCenters":[],"links":[{"id":152669,"rank":0,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/of/1995/0044/report-thumb.jpg"},{"id":50040,"rank":300,"type":{"id":11,"text":"Document"},"url":"https://pubs.usgs.gov/of/1995/0044/report.pdf","linkFileType":{"id":1,"text":"pdf"}}],"noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"4f4e4a61e4b07f02db635bd6","contributors":{"authors":[{"text":"Poppe, Lawrence J. lpoppe@usgs.gov","contributorId":2149,"corporation":false,"usgs":true,"family":"Poppe","given":"Lawrence J.","email":"lpoppe@usgs.gov","affiliations":[{"id":678,"text":"Woods Hole Coastal and Marine Science Center","active":true,"usgs":true}],"preferred":false,"id":182763,"contributorType":{"id":1,"text":"Authors"},"rank":1}]}}
,{"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":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":70018830,"text":"70018830 - 1995 - Age of Fishcreekian transgression","interactions":[],"lastModifiedDate":"2025-03-12T15:00:46.815558","indexId":"70018830","displayToPublicDate":"1995-06-01T00:00:00","publicationYear":"1995","noYear":false,"publicationType":{"id":2,"text":"Article"},"publicationSubtype":{"id":10,"text":"Journal Article"},"seriesTitle":{"id":3000,"text":"Palaios","active":true,"publicationSubtype":{"id":10}},"title":"Age of Fishcreekian transgression","docAbstract":"<p>No abstract available.&nbsp;</p>","language":"English","publisher":"GeoScienceWorld","doi":"10.2307/3515253","usgsCitation":"McDougall, K., 1995, Age of Fishcreekian transgression: Palaios, v. 10, no. 3, p. 199-220, https://doi.org/10.2307/3515253.","productDescription":"22 p.","startPage":"199","endPage":"220","costCenters":[],"links":[{"id":226658,"rank":1,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/thumbnails/outside_thumb.jpg"}],"country":"United States","state":"Alask","otherGeospatial":"Fish Creek","geographicExtents":"{\n  \"type\": \"FeatureCollection\",\n  \"features\": [\n    {\n      \"type\": \"Feature\",\n      \"properties\": {},\n      \"geometry\": {\n        \"coordinates\": [\n          [\n            [\n              -152.63657191021738,\n              70.7113266240219\n            ],\n            [\n              -152.63657191021738,\n              69.92062163052967\n            ],\n            [\n              -150.540274310732,\n              69.92062163052967\n            ],\n            [\n              -150.540274310732,\n              70.7113266240219\n            ],\n            [\n              -152.63657191021738,\n              70.7113266240219\n            ]\n          ]\n        ],\n        \"type\": \"Polygon\"\n      }\n    }\n  ]\n}","volume":"10","issue":"3","noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"5059e8ede4b0c8380cd47f9f","contributors":{"authors":[{"text":"McDougall, Kristin","contributorId":84673,"corporation":false,"usgs":true,"family":"McDougall","given":"Kristin","affiliations":[],"preferred":false,"id":380881,"contributorType":{"id":1,"text":"Authors"},"rank":1}]}}
,{"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":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":19303,"text":"ofr94688 - 1995 - Heat capacity and enthalpy of formation of synthetic alunite","interactions":[],"lastModifiedDate":"2012-02-02T00:07:31","indexId":"ofr94688","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":"94-688","title":"Heat capacity and enthalpy of formation of synthetic alunite","language":"ENGLISH","publisher":"U.S. Geological Survey,","doi":"10.3133/ofr94688","usgsCitation":"Hemingway, B.S., and Robie, R.A., 1995, Heat capacity and enthalpy of formation of synthetic alunite: U.S. Geological Survey Open-File Report 94-688, 8 leaves ;28 cm., https://doi.org/10.3133/ofr94688.","productDescription":"8 leaves ;28 cm.","costCenters":[],"links":[{"id":151354,"rank":0,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/of/1994/0688/report-thumb.jpg"},{"id":48773,"rank":300,"type":{"id":11,"text":"Document"},"url":"https://pubs.usgs.gov/of/1994/0688/report.pdf","linkFileType":{"id":1,"text":"pdf"}}],"noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"4f4e4a6ae4b07f02db63d19d","contributors":{"authors":[{"text":"Hemingway, Bruch S.","contributorId":19542,"corporation":false,"usgs":true,"family":"Hemingway","given":"Bruch","email":"","middleInitial":"S.","affiliations":[],"preferred":false,"id":180649,"contributorType":{"id":1,"text":"Authors"},"rank":1},{"text":"Robie, Richard A.","contributorId":92235,"corporation":false,"usgs":true,"family":"Robie","given":"Richard","email":"","middleInitial":"A.","affiliations":[],"preferred":false,"id":180650,"contributorType":{"id":1,"text":"Authors"},"rank":2}]}}
,{"id":19132,"text":"ofr9545 - 1995 - Bibliography of mineral resource and regional geologic studies for the states of Virginia, North Carolina, South Carolina and Georgia","interactions":[],"lastModifiedDate":"2013-09-18T07:16:25","indexId":"ofr9545","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":"95-45","title":"Bibliography of mineral resource and regional geologic studies for the states of Virginia, North Carolina, South Carolina and Georgia","language":"ENGLISH","publisher":"U.S. Geological Survey,","doi":"10.3133/ofr9545","collaboration":"The USGS does not support this software or technical questions for the software associated with the publication.","usgsCitation":"Gray, K.J., and Klein, T.L., 1995, Bibliography of mineral resource and regional geologic studies for the states of Virginia, North Carolina, South Carolina and Georgia: U.S. Geological Survey Open-File Report 95-45, 1 computer disk ;3 1/2 in., https://doi.org/10.3133/ofr9545.","productDescription":"1 computer disk ;3 1/2 in.","costCenters":[],"links":[{"id":152821,"rank":0,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/thumbnails/usgs_thumb.jpg"},{"id":277749,"type":{"id":4,"text":"Application Site"},"url":"https://pubs.usgs.gov/of/1995/0045/application.zip"}],"noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"4f4e4a4ee4b07f02db627f77","contributors":{"authors":[{"text":"Gray, Karen J.","contributorId":93516,"corporation":false,"usgs":true,"family":"Gray","given":"Karen","email":"","middleInitial":"J.","affiliations":[],"preferred":false,"id":180367,"contributorType":{"id":1,"text":"Authors"},"rank":1},{"text":"Klein, T. L.","contributorId":76322,"corporation":false,"usgs":true,"family":"Klein","given":"T.","email":"","middleInitial":"L.","affiliations":[],"preferred":false,"id":180366,"contributorType":{"id":1,"text":"Authors"},"rank":2}]}}
,{"id":65604,"text":"i2417 - 1995 - Controlled photomosaic of the MTM 45022 Quadrangle, Acidalia Planitia region of Mars","interactions":[],"lastModifiedDate":"2012-02-10T00:11:06","indexId":"i2417","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":"2417","subseriesTitle":"NONE","title":"Controlled photomosaic of the MTM 45022 Quadrangle, Acidalia Planitia region of Mars","language":"ENGLISH","doi":"10.3133/i2417","usgsCitation":"Water Resources Division, U.S. Geological Survey, 1995, Controlled photomosaic of the MTM 45022 Quadrangle, Acidalia Planitia region of Mars: U.S. Geological Survey IMAP 2417, 1 remote-sensing image ;62 x 45 cm., on sheet 97 x 56 cm., folded in envelope 30 x 24 cm., https://doi.org/10.3133/i2417.","productDescription":"1 remote-sensing image ;62 x 45 cm., on sheet 97 x 56 cm., folded in envelope 30 x 24 cm.","costCenters":[],"links":[{"id":189422,"rank":0,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/thumbnails/usgs_thumb.jpg"},{"id":101054,"rank":400,"type":{"id":17,"text":"Plate"},"url":"https://pubs.usgs.gov/imap/2417/plate-1.pdf","size":"9679","linkFileType":{"id":1,"text":"pdf"}}],"scale":"502000","geographicExtents":"{ \"type\": \"FeatureCollection\", \"features\": [ { \"type\": \"Feature\", \"properties\": {}, \"geometry\": { \"type\": \"Polygon\", \"coordinates\": [ [ [ 20,42.5 ], [ 20,47.5 ], [ 25,47.5 ], [ 25,42.5 ], [ 20,42.5 ] ] ] } } ] }","noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"4f4e4ae0e4b07f02db688256","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":533992,"contributorType":{"id":1,"text":"Authors"},"rank":1}]}}
,{"id":66198,"text":"i2359 - 1995 - Maps showing growth of the lava dome at Mount St. Helens, Washington, 1980-1986","interactions":[],"lastModifiedDate":"2019-06-06T13:13:27","indexId":"i2359","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":"2359","subseriesTitle":"NONE","title":"Maps showing growth of the lava dome at Mount St. Helens, Washington, 1980-1986","docAbstract":"<p>No abstract available&nbsp;</p>","language":"ENGLISH","doi":"10.3133/i2359","usgsCitation":"Holcomb, R.T., and Colony, W., 1995, Maps showing growth of the lava dome at Mount St. Helens, Washington, 1980-1986: U.S. Geological Survey IMAP 2359, 18 maps on 1 sheet :col. ;18 x 14 cm. and 26 x 19 cm., sheet 102 x 143 cm., folded in envelope 30 x 24 cm., https://doi.org/10.3133/i2359.","productDescription":"18 maps on 1 sheet :col. ;18 x 14 cm. and 26 x 19 cm., sheet 102 x 143 cm., folded in envelope 30 x 24 cm.","costCenters":[{"id":615,"text":"Volcano Hazards Program","active":true,"usgs":true}],"links":[{"id":255690,"rank":400,"type":{"id":17,"text":"Plate"},"url":"https://pubs.usgs.gov/imap/2359/plate-1.pdf","size":"16337","linkFileType":{"id":1,"text":"pdf"}},{"id":255691,"rank":300,"type":{"id":11,"text":"Document"},"url":"https://pubs.usgs.gov/imap/2359/report.pdf","size":"28","linkFileType":{"id":1,"text":"pdf"}},{"id":255692,"rank":0,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/imap/2359/report-thumb.jpg"}],"scale":"5000","geographicExtents":"{ \"type\": \"FeatureCollection\", \"features\": [ { \"type\": \"Feature\", \"properties\": {}, \"geometry\": { \"type\": \"Polygon\", \"coordinates\": [ [ [ -122.18416666666667,46.18444444444444 ], [ -122.18416666666667,46.20055555555556 ], [ -122.16805555555555,46.20055555555556 ], [ -122.16805555555555,46.18444444444444 ], [ -122.18416666666667,46.18444444444444 ] ] ] } } ] }","noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"4f4e4a19e4b07f02db605abb","contributors":{"authors":[{"text":"Holcomb, R. T.","contributorId":99146,"corporation":false,"usgs":true,"family":"Holcomb","given":"R.","email":"","middleInitial":"T.","affiliations":[],"preferred":false,"id":274148,"contributorType":{"id":1,"text":"Authors"},"rank":1},{"text":"Colony, W.E.","contributorId":62686,"corporation":false,"usgs":true,"family":"Colony","given":"W.E.","email":"","affiliations":[],"preferred":false,"id":274147,"contributorType":{"id":1,"text":"Authors"},"rank":2}]}}
,{"id":65536,"text":"i2403 - 1995 - Controlled photomosaic of the MTM 20182 Quadrangle, Orcus Patera region of Mars","interactions":[],"lastModifiedDate":"2019-12-23T12:38:24","indexId":"i2403","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":"2403","title":"Controlled photomosaic of the MTM 20182 Quadrangle, Orcus Patera region of Mars","docAbstract":"<p>No abstract available.</p>","language":"English","publisher":"U.S. Geological Survey","doi":"10.3133/i2403","usgsCitation":"Water Resources Division, U.S. Geological Survey, 1995, Controlled photomosaic of the MTM 20182 Quadrangle, Orcus Patera region of Mars: U.S. Geological Survey IMAP 2403, Plate: 26 x 38 inches, https://doi.org/10.3133/i2403.","productDescription":"Plate: 26 x 38 inches","costCenters":[],"links":[{"id":189936,"rank":0,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/thumbnails/usgs_thumb.jpg"},{"id":100989,"rank":400,"type":{"id":17,"text":"Plate"},"url":"https://pubs.usgs.gov/imap/2403/plate-1.pdf","size":"18749","linkFileType":{"id":1,"text":"pdf"}}],"scale":"502000","otherGeospatial":"Mars","noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"4f4e4ae0e4b07f02db688425","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":533923,"contributorType":{"id":1,"text":"Authors"},"rank":1}]}}
,{"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":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":20515,"text":"ofr9558 - 1995 - GPRMODV2; one-dimensional full waveform forward modeling of dispersive ground penetrating radar data, version 2.0","interactions":[],"lastModifiedDate":"2013-09-17T15:17:50","indexId":"ofr9558","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":"95-58","title":"GPRMODV2; one-dimensional full waveform forward modeling of dispersive ground penetrating radar data, version 2.0","language":"ENGLISH","publisher":"U.S. Geological Survey,","doi":"10.3133/ofr9558","collaboration":"The USGS does not support this software or technical questions for the software associated with the publication.","usgsCitation":"Powers, M.H., and Olhoeft, G., 1995, GPRMODV2; one-dimensional full waveform forward modeling of dispersive ground penetrating radar data, version 2.0: U.S. Geological Survey Open-File Report 95-58, 1 computer disk ;3 1/2 in. +1 text (41 p.  ill. ; 28 cm.), https://doi.org/10.3133/ofr9558.","productDescription":"1 computer disk ;3 1/2 in. +1 text (41 p.  ill. ; 28 cm.)","costCenters":[],"links":[{"id":153251,"rank":0,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/of/1995/0058/report-thumb.jpg"},{"id":50048,"rank":300,"type":{"id":11,"text":"Document"},"url":"https://pubs.usgs.gov/of/1995/0058/report.pdf","linkFileType":{"id":1,"text":"pdf"}},{"id":277701,"type":{"id":4,"text":"Application Site"},"url":"https://pubs.usgs.gov/of/1995/0058/application.zip"}],"noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"4f4e4b28e4b07f02db6b15c9","contributors":{"authors":[{"text":"Powers, Michael H. 0000-0002-4480-7856 mhpowers@usgs.gov","orcid":"https://orcid.org/0000-0002-4480-7856","contributorId":851,"corporation":false,"usgs":true,"family":"Powers","given":"Michael","email":"mhpowers@usgs.gov","middleInitial":"H.","affiliations":[{"id":211,"text":"Crustal Geophysics and Geochemistry Science Center","active":true,"usgs":true}],"preferred":true,"id":182786,"contributorType":{"id":1,"text":"Authors"},"rank":1},{"text":"Olhoeft, G.R.","contributorId":10405,"corporation":false,"usgs":true,"family":"Olhoeft","given":"G.R.","email":"","affiliations":[],"preferred":false,"id":182787,"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":38211,"text":"pp1547 - 1995 - Sedimentology, Behavior, and Hazards of Debris Flows at Mount Rainier, Washington","interactions":[{"subject":{"id":20836,"text":"ofr90385 - 1992 - Sedimentology, behavior, and hazards of debris flows at Mount Rainier, Washington","indexId":"ofr90385","publicationYear":"1992","noYear":false,"title":"Sedimentology, behavior, and hazards of debris flows at Mount Rainier, Washington"},"predicate":"SUPERSEDED_BY","object":{"id":38211,"text":"pp1547 - 1995 - Sedimentology, Behavior, and Hazards of Debris Flows at Mount Rainier, Washington","indexId":"pp1547","publicationYear":"1995","noYear":false,"title":"Sedimentology, Behavior, and Hazards of Debris Flows at Mount Rainier, Washington"},"id":1}],"lastModifiedDate":"2012-02-10T00:10:09","indexId":"pp1547","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":"1547","title":"Sedimentology, Behavior, and Hazards of Debris Flows at Mount Rainier, Washington","docAbstract":"Mount Rainier is potentially the most dangerous volcano in the Cascade Range because of its great height, frequent earthquakes, active hydrothermal system, and extensive glacier mantle. Many debris flows and their distal phases have inundated areas far from the volcano during postglacial time. Two types of debris flows, cohesive and noncohesive, have radically different origins and behavior that relate empirically to clay content. The two types are the major subpopulations of debris flows at Mount Rainier. The behavior of cohesive flows is affected by the cohesion and adhesion of particles; noncohesive flows are dominated by particle collisions to the extent that particle cataclasis becomes common during near-boundary shear.\r\n\r\nCohesive debris flows contain more than 3 to 5 percent of clay-size sediment. The composition of these flows changed little as they traveled more than 100 kilometers from Mount Rainier to inundate parts of the now-populated Puget Sound lowland. They originate as deep-seated failures of sectors of the volcanic edifice, and such failures are sufficiently frequent that they are the major destructional process of Mount Rainier's morphologic evolution. In several deposits of large cohesive flows, a lateral, megaclast-bearing facies (with a mounded or hummocky surface) contrasts with a more clay-rich facies in the center of valleys and downstream. Cohesive flows at Mount Rainier do not correlate strongly with volcanic activity and thus can recur without warning, possibly triggered by non-magmatic earthquakes or by changes in the hydrothermal system.\r\n\r\nNoncohesive debris flows contain less than 3 to 5 percent clay-size sediment. They form most commonly by bulking of sediment in water surges, but some originate directly or indirectly from shallow slope failures that do not penetrate the hydrothermally altered core of the volcano. In contrast with cohesive flows, most noncohesive flows transform both from and to other flow types and are, therefore, the middle segments of flow waves that begin and end as flood surges. Proximally, through the bulking of poorly sorted volcaniclastic debris on the flanks of the volcano, flow waves expand rapidly in volume by transforming from water surges through hyperconcentrated stream flow (20 to 60 percent sediment by volume) to debris flow. Distally, the transformations occur more slowly in reverse order - from debris flow, to hyperconcentrated flow, and finally to normal streamflow with less than 20 percent sediment by volume. During runout of the largest noncohesive flows, hyperconcentrated flow has continued for as much as 40 to 70 kilometers.\r\n\r\nLahars (volcanic debris flows and their deposits) have occurred frequently at Mount Rainier over the past several thousand years, and generally they have not clustered within discrete eruptive periods as at Mount St. Helens. An exception is a period of large noncohesive flows during and after construction of the modern summit cone. Deposits from lahar-runout flows, the hyperconcentrated distal phases of lahars, document the frequency and extent of noncohesive lahars. These deposits also record the following transformations of debris flows: (1) the direct, progressive dilution of debris flow to hyperconcentrated flow, (2) deposition of successively finer grained lobes of debris until only the hyperconcentrated tail of the flow remains to continue downstream, and (3) dewatering of coarse debris flow deposits to yield fine-grained debris flow or hyperconcentrated flow.\r\n\r\nThree planning or design case histories represent different lengths of postglacial time. Case I is representative of large, infrequent (500 to 1,000 years on average) cohesive debris flows. These flows need to be considered in long-term planning in valleys around the volcano. Case II generalizes the noncohesive debris flows of intermediate size and recurrence (100 to 500 years). This case is appropriate for consideration in some structural design. Case III flows are ","language":"ENGLISH","publisher":"U.S. Geological Survey","doi":"10.3133/pp1547","usgsCitation":"Scott, K.M., Vallance, J., and Pringle, P.T., 1995, Sedimentology, Behavior, and Hazards of Debris Flows at Mount Rainier, Washington: U.S. Geological Survey Professional Paper 1547, 56 p., https://doi.org/10.3133/pp1547.","productDescription":"56 p.","costCenters":[{"id":595,"text":"U.S. Geological Survey","active":false,"usgs":true}],"links":[{"id":104677,"rank":700,"type":{"id":15,"text":"Index Page"},"url":"https://ngmdb.usgs.gov/Prodesc/proddesc_4926.htm","linkFileType":{"id":5,"text":"html"},"description":"4926"},{"id":122086,"rank":0,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/pp/1547/report-thumb.jpg"},{"id":12502,"rank":100,"type":{"id":15,"text":"Index Page"},"url":"https://www.nps.gov/history/history/online_books/geology/publications/pp/1547/index.htm","linkFileType":{"id":5,"text":"html"}},{"id":64514,"rank":400,"type":{"id":17,"text":"Plate"},"url":"https://pubs.usgs.gov/pp/1547/plate-1.pdf","linkFileType":{"id":1,"text":"pdf"}},{"id":64515,"rank":300,"type":{"id":11,"text":"Document"},"url":"https://pubs.usgs.gov/pp/1547/report.pdf","linkFileType":{"id":1,"text":"pdf"}}],"geographicExtents":"{ \"type\": \"FeatureCollection\", \"features\": [ { \"type\": \"Feature\", \"properties\": {}, \"geometry\": { \"type\": \"Polygon\", \"coordinates\": [ [ [ -123,46 ], [ -123,47.75 ], [ -121,47.75 ], [ -121,46 ], [ -123,46 ] ] ] } } ] }","noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"4f4e4a0ae4b07f02db5fb3c0","contributors":{"authors":[{"text":"Scott, K. 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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}]}}
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,{"id":68217,"text":"ha730K - 1995 - Ground Water Atlas of the United States: Segment 10, Illinois, Indiana, Kentucky, Ohio, Tennessee","interactions":[{"subject":{"id":68217,"text":"ha730K - 1995 - Ground Water Atlas of the United States: Segment 10, Illinois, Indiana, Kentucky, Ohio, Tennessee","indexId":"ha730K","publicationYear":"1995","noYear":false,"chapter":"K","title":"Ground Water Atlas of the United States: Segment 10, Illinois, Indiana, Kentucky, Ohio, Tennessee"},"predicate":"IS_PART_OF","object":{"id":68687,"text":"ha730 - 2000 - Ground Water Atlas of the United States","indexId":"ha730","publicationYear":"2000","noYear":false,"title":"Ground Water Atlas of the United States"},"id":1}],"isPartOf":{"id":68687,"text":"ha730 - 2000 - Ground Water Atlas of the United States","indexId":"ha730","publicationYear":"2000","noYear":false,"title":"Ground Water Atlas of the United States"},"lastModifiedDate":"2017-05-30T16:01:32","indexId":"ha730K","displayToPublicDate":"1995-06-01T00:00:00","publicationYear":"1995","noYear":false,"publicationType":{"id":18,"text":"Report"},"publicationSubtype":{"id":5,"text":"USGS Numbered Series"},"seriesTitle":{"id":318,"text":"Hydrologic Atlas","code":"HA","active":false,"publicationSubtype":{"id":5}},"seriesNumber":"730","chapter":"K","title":"Ground Water Atlas of the United States: Segment 10, Illinois, Indiana, Kentucky, Ohio, Tennessee","docAbstract":"<p>This report provides a summary of ground-water conditions and problems in Illinois, Indiana, Kentucky, Ohio, and Tennessee, which compose Segment 10 of the Ground Water Atlas of the United States, an area of about 217,000 square miles. 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