No abstract available.
","language":"English","publisher":"U.S. Geological Survey","doi":"10.3133/ofr87339","usgsCitation":"Adrian, B.M., Smith, D.B., Hill, R.T., Roemer, T.A., Vaughn, R.B., and Delaney, T.A., 1987, Analytical results and sample locality map of stream-sediment, heavy-mineral-concentrate, and rock samples from the New Water Mountains Wilderness Study Area, La Paz County, Arizona: U.S. Geological Survey Open-File Report 87-339, Report: 34 p.; 1 Plate: 22.15 × 17.10 inches, https://doi.org/10.3133/ofr87339.","productDescription":"Report: 34 p.; 1 Plate: 22.15 × 17.10 inches","costCenters":[],"links":[{"id":40638,"rank":300,"type":{"id":11,"text":"Document"},"url":"https://pubs.usgs.gov/of/1987/0339/report.pdf","linkFileType":{"id":1,"text":"pdf"}},{"id":144833,"rank":0,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/of/1987/0339/report-thumb.jpg"},{"id":40637,"rank":400,"type":{"id":17,"text":"Plate"},"url":"https://pubs.usgs.gov/of/1987/0339/plate-1.pdf","linkFileType":{"id":1,"text":"pdf"}},{"id":394688,"rank":4,"type":{"id":36,"text":"NGMDB Index Page"},"url":"https://ngmdb.usgs.gov/Prodesc/proddesc_17199.htm"}],"country":"United States","state":"Arizona","county":"La Paz County","otherGeospatial":"New Water Mountains Wilderness Study Area","geographicExtents":"{\n \"type\": \"FeatureCollection\",\n \"features\": [\n {\n \"type\": \"Feature\",\n \"properties\": {},\n \"geometry\": {\n \"type\": \"Polygon\",\n \"coordinates\": [\n [\n [\n -114.009,\n 33.5\n ],\n [\n -113.75,\n 33.5\n ],\n [\n -113.75,\n 33.683\n ],\n [\n -114.009,\n 33.683\n ],\n [\n -114.009,\n 33.5\n ]\n ]\n ]\n }\n }\n ]\n}","noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"4f4e4acce4b07f02db67eb4b","contributors":{"authors":[{"text":"Adrian, B. M.","contributorId":71535,"corporation":false,"usgs":true,"family":"Adrian","given":"B.","email":"","middleInitial":"M.","affiliations":[],"preferred":false,"id":166083,"contributorType":{"id":1,"text":"Authors"},"rank":1},{"text":"Smith, D. B. davidsmith@usgs.gov","contributorId":12840,"corporation":false,"usgs":true,"family":"Smith","given":"D.","email":"davidsmith@usgs.gov","middleInitial":"B.","affiliations":[],"preferred":false,"id":166080,"contributorType":{"id":1,"text":"Authors"},"rank":2},{"text":"Hill, R. T.","contributorId":69990,"corporation":false,"usgs":true,"family":"Hill","given":"R.","email":"","middleInitial":"T.","affiliations":[],"preferred":false,"id":166082,"contributorType":{"id":1,"text":"Authors"},"rank":3},{"text":"Roemer, T. A.","contributorId":72784,"corporation":false,"usgs":true,"family":"Roemer","given":"T.","email":"","middleInitial":"A.","affiliations":[],"preferred":false,"id":166084,"contributorType":{"id":1,"text":"Authors"},"rank":4},{"text":"Vaughn, R. B.","contributorId":27043,"corporation":false,"usgs":true,"family":"Vaughn","given":"R.","email":"","middleInitial":"B.","affiliations":[],"preferred":false,"id":166081,"contributorType":{"id":1,"text":"Authors"},"rank":5},{"text":"Delaney, T. A.","contributorId":12049,"corporation":false,"usgs":true,"family":"Delaney","given":"T.","email":"","middleInitial":"A.","affiliations":[],"preferred":false,"id":166079,"contributorType":{"id":1,"text":"Authors"},"rank":6}]}} ,{"id":64579,"text":"i1420(NJ18) - 1987 - Quaternary geologic map of the Chesapeake Bay 4 degrees x 6 degrees quadrangle, United States","interactions":[],"lastModifiedDate":"2023-07-14T13:15:09.850928","indexId":"i1420(NJ18)","displayToPublicDate":"1994-01-01T00:00:00","publicationYear":"1987","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":"1420(NJ-18)","subseriesTitle":"GAUS","title":"Quaternary geologic map of the Chesapeake Bay 4 degrees x 6 degrees quadrangle, United States","docAbstract":"The Quaternary Geologic Map of the Chesapeake Bay 4? x 6? Quadrangle\r\n was mapped as part of the Quaternary Geologic Atlas of the United States.\r\n The atlas was begun as an effort to depict the areal distribution of\r\n surficial geologic deposits and other materials that accumulated or\r\n formed during the past 2+ million years, the period that includes all\r\n activities of the human species. These materials are at the surface of\r\n the Earth. They make up the 'ground' on which we walk, the 'dirt' in\r\n which we dig foundations, and the 'soil' in which we grow crops. Most\r\n of our human activity is related in one way or another to these surface\r\n materials that are referred to collectively by many geologists as\r\n regolith, the mantle of fragmental and generally unconsolidated material\r\n that overlies the bedrock foundation of the continent. The maps were\r\n compiled at 1:1,000,000 scale.","language":"English","publisher":"U.S. Geological Survey","doi":"10.3133/i1420(NJ18)","usgsCitation":"1987, Quaternary geologic map of the Chesapeake Bay 4 degrees x 6 degrees quadrangle, United States: U.S. Geological Survey IMAP 1420(NJ-18), 1 map: 79 x 138 cm., https://doi.org/10.3133/i1420(NJ18).","productDescription":"1 map: 79 x 138 cm.","costCenters":[],"links":[{"id":187408,"rank":1,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/thumbnails/usgs_thumb.jpg"},{"id":106737,"rank":3,"type":{"id":15,"text":"Index Page"},"url":"https://ngmdb.usgs.gov/Prodesc/proddesc_9215.htm","linkFileType":{"id":5,"text":"html"},"description":"9215"},{"id":8784,"rank":2,"type":{"id":15,"text":"Index Page"},"url":"https://pubs.usgs.gov/imap/i-1420/nj-18/","linkFileType":{"id":5,"text":"html"}}],"scale":"1000000","country":"United States","state":"Maryland, Virginia","otherGeospatial":"Chesapeake Bay","geographicExtents":"{ \"type\": \"FeatureCollection\", \"features\": [ { \"type\": \"Feature\", \"properties\": {}, \"geometry\": { \"type\": \"Polygon\", \"coordinates\": [ [ [ -78,36 ], [ -78,40 ], [ -72,40 ], [ -72,36 ], [ -78,36 ] ] ] } } ] }","noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"4f4e4adbe4b07f02db685c06","contributors":{"compilers":[{"text":"Cleaves, Emery T.","contributorId":80249,"corporation":false,"usgs":true,"family":"Cleaves","given":"Emery","email":"","middleInitial":"T.","affiliations":[],"preferred":false,"id":749565,"contributorType":{"id":3,"text":"Compilers"},"rank":1},{"text":"Glaser, John D.","contributorId":49049,"corporation":false,"usgs":true,"family":"Glaser","given":"John","email":"","middleInitial":"D.","affiliations":[],"preferred":false,"id":877975,"contributorType":{"id":3,"text":"Compilers"},"rank":2},{"text":"Howard, Alan D.","contributorId":106579,"corporation":false,"usgs":true,"family":"Howard","given":"Alan","email":"","middleInitial":"D.","affiliations":[],"preferred":false,"id":877976,"contributorType":{"id":3,"text":"Compilers"},"rank":3},{"text":"Johnson, Gerald H.","contributorId":96771,"corporation":false,"usgs":true,"family":"Johnson","given":"Gerald","email":"","middleInitial":"H.","affiliations":[],"preferred":false,"id":877977,"contributorType":{"id":3,"text":"Compilers"},"rank":4},{"text":"Wheeler, Walter H.","contributorId":26372,"corporation":false,"usgs":true,"family":"Wheeler","given":"Walter","email":"","middleInitial":"H.","affiliations":[],"preferred":false,"id":877978,"contributorType":{"id":3,"text":"Compilers"},"rank":5},{"text":"Sevon, William D.","contributorId":69243,"corporation":false,"usgs":true,"family":"Sevon","given":"William","email":"","middleInitial":"D.","affiliations":[],"preferred":false,"id":877979,"contributorType":{"id":3,"text":"Compilers"},"rank":6},{"text":"Judson, Sheldon","contributorId":20018,"corporation":false,"usgs":true,"family":"Judson","given":"Sheldon","email":"","affiliations":[],"preferred":false,"id":877980,"contributorType":{"id":3,"text":"Compilers"},"rank":7},{"text":"Owens, James P.","contributorId":9691,"corporation":false,"usgs":true,"family":"Owens","given":"James P.","affiliations":[],"preferred":false,"id":877981,"contributorType":{"id":3,"text":"Compilers"},"rank":8},{"text":"Peebles, Pamela C.","contributorId":62685,"corporation":false,"usgs":true,"family":"Peebles","given":"Pamela","email":"","middleInitial":"C.","affiliations":[],"preferred":false,"id":877982,"contributorType":{"id":3,"text":"Compilers"},"rank":9}],"editors":[{"text":"Richmond, Gerald M.","contributorId":87165,"corporation":false,"usgs":true,"family":"Richmond","given":"Gerald M.","affiliations":[],"preferred":false,"id":749564,"contributorType":{"id":2,"text":"Editors"},"rank":1},{"text":"Fullerton, David S. fullerton@usgs.gov","contributorId":448,"corporation":false,"usgs":true,"family":"Fullerton","given":"David","email":"fullerton@usgs.gov","middleInitial":"S.","affiliations":[{"id":318,"text":"Geosciences and Environmental Change Science Center","active":true,"usgs":true}],"preferred":true,"id":877973,"contributorType":{"id":2,"text":"Editors"},"rank":2},{"text":"Weide, David L.","contributorId":48537,"corporation":false,"usgs":true,"family":"Weide","given":"David","email":"","middleInitial":"L.","affiliations":[],"preferred":false,"id":877974,"contributorType":{"id":2,"text":"Editors"},"rank":3}]}} ,{"id":30343,"text":"wri874075 - 1987 - Effluent migration from septic tank systems in two different lithologies, Broward County, Florida","interactions":[],"lastModifiedDate":"2022-01-10T12:39:44.576884","indexId":"wri874075","displayToPublicDate":"1994-01-01T00:00:00","publicationYear":"1987","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":"87-4075","title":"Effluent migration from septic tank systems in two different lithologies, Broward County, Florida","docAbstract":"Two septic tank test sites, one in sand and one in limestone, in Broward County, Florida, were analyzed for effluent migration. Groundwater from shallow wells, both in background areas and hydraulically down-gradient of the septic tank system, was sampled during a 16-month period from April 1983 through August 1984. Water quality indicators were used to determine the effluent affected zone near the septic tank systems. Specific conductance levels and concentrations of chloride, sulfate, ammonium, and nitrate indicated effluent movement primarily in a vertical direction with abrupt dilution as it moved down-gradient. Effluent was detected in the sand to a depth more than 20 ft below the septic tank outlet, but was diluted to near background conditions 50 ft down-gradient from the tank. Effluent in the limestone was detected in all three observation wells to depths exceeding 25 ft below the septic tank outlet and was diluted, but still detectable, 40 ft down-gradient. The primary controls on effluent movement from septic tank systems in Broward County are the lithology and layering of the geologic materials, hydraulic gradients, and the volume and type of use the system receives. (Author 's abstract)","language":"English","publisher":"U.S. Geological Survey","doi":"10.3133/wri874075","collaboration":"Prepared in cooperation with Broward County","usgsCitation":"Waller, B., Howie, B., and Causaras, C., 1987, Effluent migration from septic tank systems in two different lithologies, Broward County, Florida: U.S. Geological Survey Water-Resources Investigations Report 87-4075, iv, 22 p., https://doi.org/10.3133/wri874075.","productDescription":"iv, 22 p.","costCenters":[{"id":27821,"text":"Caribbean-Florida Water Science Center","active":true,"usgs":true}],"links":[{"id":123824,"rank":0,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/wri/1987/4075/coverthb.jpg"},{"id":59137,"rank":299,"type":{"id":11,"text":"Document"},"url":"https://pubs.usgs.gov/wri/1987/4075/report.pdf","text":"Report","size":"1.23 MB","linkFileType":{"id":1,"text":"pdf"}}],"country":"United States","state":"Florida","county":"Broward 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Water Science Center
U.S. Geological Survey
3321 College Avenue
Davie, FL 33314
This report presents the results of a three-step evaluation of the stream-gaging program in Wisconsin. First, data uses and funding sources were identified for the 89 continuous-record gaging stations operated during the 1984 water year. Next, alternative methods of streamflow estimation were examined for three stations. A flow-routing model was used for two of the stations and a statistical model was used for the third. The modeled discharges did not compare well enough with observed discharges to warrant elimination of any of the stations. Finally, an optimization model was used to assess the cost effectiveness of the stream-gaging process.
\nThe annual budget, in 1984 dollars, for operating the 89 continuous-record gaging stations and 65 additional stations is $557,3000. Based on a Kalman-filter analysis, the theoretical average standard error of instantaneous discharge associated with the current practice of visiting the stations is 13.8%. This overall level of accuracy could be maintained with a budget of $518,6000 if stream-gaging activities were redistributed in an optimal fashion among the gaging stations. For the current budget, the theoretical average standard error would be reduced to 10.1% if the network is operated in an optimal fashion. Furthermore, the average standard error would be reduced to 7.3% if all missing record is eliminated and the network is operated optimally.
\nA minimum budget of $510,000 is required to operate the program; a budget less than this does not permit proper service and maintenance of the gaging stations. At this minimum budget, the theoretical average standard error of instantaneous discharge is 14.4%. The maximum budget analyzed was $650,000 and resulted in an average standard of error of instantaneous discharge of 7.2%.
","language":"English","publisher":"U.S. Geological Survey","doi":"10.3133/wri864125","usgsCitation":"Walker, J., Osen, L., and Hughes, P., 1987, Cost effectiveness of the U.S. Geological Survey's stream-gaging program in Wisconsin: U.S. Geological Survey Water-Resources Investigations Report 86-4125, v, 44 p., https://doi.org/10.3133/wri864125.","productDescription":"v, 44 p.","numberOfPages":"49","onlineOnly":"N","additionalOnlineFiles":"N","costCenters":[{"id":677,"text":"Wisconsin Water Science Center","active":true,"usgs":true}],"links":[{"id":124026,"rank":0,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/wri/1986/4125/report-thumb.jpg"},{"id":59122,"rank":300,"type":{"id":11,"text":"Document"},"url":"https://pubs.usgs.gov/wri/1986/4125/report.pdf","linkFileType":{"id":1,"text":"pdf"}}],"country":"United 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\"}}]}","noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"4f4e4adce4b07f02db6866cd","contributors":{"authors":[{"text":"Walker, J.F.","contributorId":86743,"corporation":false,"usgs":true,"family":"Walker","given":"J.F.","email":"","affiliations":[],"preferred":false,"id":203068,"contributorType":{"id":1,"text":"Authors"},"rank":1},{"text":"Osen, L.L.","contributorId":46993,"corporation":false,"usgs":true,"family":"Osen","given":"L.L.","email":"","affiliations":[],"preferred":false,"id":203067,"contributorType":{"id":1,"text":"Authors"},"rank":2},{"text":"Hughes, P.E.","contributorId":104083,"corporation":false,"usgs":true,"family":"Hughes","given":"P.E.","email":"","affiliations":[],"preferred":false,"id":203069,"contributorType":{"id":1,"text":"Authors"},"rank":3}]}} ,{"id":29635,"text":"wri874031 - 1987 - Geohydrology and susceptibility of Coldwater Spring and Jacksonville fault areas to surface contamination in Calhoun County, Alabama","interactions":[],"lastModifiedDate":"2012-02-02T00:08:56","indexId":"wri874031","displayToPublicDate":"1994-01-01T00:00:00","publicationYear":"1987","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":"87-4031","title":"Geohydrology and susceptibility of Coldwater Spring and Jacksonville fault areas to surface contamination in Calhoun County, Alabama","docAbstract":"Coldwater Spring in eastern Calhoun County, Alabama, is one of the largest springs in Alabama. The spring, which has an average discharge of about 31 million gallons per day, supplies water for about 70,000 people in the Anniston, Alabama area. A potentiometric map of the study area indicates that the recharge area for the aquifer system that supplies the spring is only about 23 square miles. However, base-flow data for streams in the area indicate that this recharge area is not sufficient to account for an average discharge of 31 million gallons per day from Coldwater Spring. Complex folding and faulting of the carbonate and quart zitic rocks that comprise the aquifer system may have produced fractures and joints that increase recharge to the spring. Some recharge to the spring may be derived from outside the recharge area delineated from the potentiometric map or from the surface. This part of the recharge area contamination from the surface. This part of the recharge area consists of flat to gently rolling terrain underlain by cavernous limestone and fractured quartzite. (USGS)","language":"ENGLISH","publisher":"U.S. Geological Survey,","doi":"10.3133/wri874031","usgsCitation":"Scott, J.C., Harris, W.F., and Cobb, R., 1987, Geohydrology and susceptibility of Coldwater Spring and Jacksonville fault areas to surface contamination in Calhoun County, Alabama: U.S. Geological Survey Water-Resources Investigations Report 87-4031, iv, 29 p. :ill., maps ;28 cm., https://doi.org/10.3133/wri874031.","productDescription":"iv, 29 p. :ill., maps ;28 cm.","costCenters":[],"links":[{"id":123630,"rank":0,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/wri/1987/4031/report-thumb.jpg"},{"id":58455,"rank":400,"type":{"id":17,"text":"Plate"},"url":"https://pubs.usgs.gov/wri/1987/4031/plate-1.pdf","linkFileType":{"id":1,"text":"pdf"}},{"id":58456,"rank":300,"type":{"id":11,"text":"Document"},"url":"https://pubs.usgs.gov/wri/1987/4031/report.pdf","linkFileType":{"id":1,"text":"pdf"}}],"noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"4f4e4b1be4b07f02db6a8c0a","contributors":{"authors":[{"text":"Scott, J. C.","contributorId":75901,"corporation":false,"usgs":true,"family":"Scott","given":"J.","email":"","middleInitial":"C.","affiliations":[],"preferred":false,"id":201854,"contributorType":{"id":1,"text":"Authors"},"rank":1},{"text":"Harris, W. F.","contributorId":66303,"corporation":false,"usgs":true,"family":"Harris","given":"W.","email":"","middleInitial":"F.","affiliations":[],"preferred":false,"id":201853,"contributorType":{"id":1,"text":"Authors"},"rank":2},{"text":"Cobb, R.H.","contributorId":31027,"corporation":false,"usgs":true,"family":"Cobb","given":"R.H.","email":"","affiliations":[],"preferred":false,"id":201852,"contributorType":{"id":1,"text":"Authors"},"rank":3}]}} ,{"id":41187,"text":"ofr87594 - 1987 - Preliminary bedrock geologic map of the International Falls 1 degree x 2 degree Quadrangle, Minnesota, U.S.A., and Ontario, Canada","interactions":[],"lastModifiedDate":"2012-02-02T00:10:32","indexId":"ofr87594","displayToPublicDate":"1994-01-01T00:00:00","publicationYear":"1987","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":"87-594","title":"Preliminary bedrock geologic map of the International Falls 1 degree x 2 degree Quadrangle, Minnesota, U.S.A., and Ontario, Canada","language":"ENGLISH","doi":"10.3133/ofr87594","usgsCitation":"Day, W.C., Southwick, D.L., Schulz, K.J., and Klein, T.L., 1987, Preliminary bedrock geologic map of the International Falls 1 degree x 2 degree Quadrangle, Minnesota, U.S.A., and Ontario, Canada: U.S. Geological Survey Open-File Report 87-594, 1 map :photocopy ;45 x 60 cm., on sheet 78 x 116 cm., https://doi.org/10.3133/ofr87594.","productDescription":"1 map :photocopy ;45 x 60 cm., on sheet 78 x 116 cm.","costCenters":[],"links":[{"id":173370,"rank":0,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/thumbnails/usgs_thumb.jpg"},{"id":79017,"rank":400,"type":{"id":17,"text":"Plate"},"url":"https://pubs.usgs.gov/of/1987/0594/plate-1.pdf","linkFileType":{"id":1,"text":"pdf"}}],"noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"4f4e4ac9e4b07f02db67c969","contributors":{"authors":[{"text":"Day, Warren C. 0000-0002-9278-2120 wday@usgs.gov","orcid":"https://orcid.org/0000-0002-9278-2120","contributorId":1308,"corporation":false,"usgs":true,"family":"Day","given":"Warren","email":"wday@usgs.gov","middleInitial":"C.","affiliations":[{"id":387,"text":"Mineral Resources Program","active":true,"usgs":true}],"preferred":true,"id":224625,"contributorType":{"id":1,"text":"Authors"},"rank":1},{"text":"Southwick, D. L.","contributorId":57130,"corporation":false,"usgs":true,"family":"Southwick","given":"D.","email":"","middleInitial":"L.","affiliations":[],"preferred":false,"id":224626,"contributorType":{"id":1,"text":"Authors"},"rank":2},{"text":"Schulz, K. J.","contributorId":79131,"corporation":false,"usgs":true,"family":"Schulz","given":"K.","email":"","middleInitial":"J.","affiliations":[],"preferred":false,"id":224628,"contributorType":{"id":1,"text":"Authors"},"rank":3},{"text":"Klein, T. L.","contributorId":76322,"corporation":false,"usgs":true,"family":"Klein","given":"T.","email":"","middleInitial":"L.","affiliations":[],"preferred":false,"id":224627,"contributorType":{"id":1,"text":"Authors"},"rank":4}]}} ,{"id":16066,"text":"ofr87692 - 1987 - Preliminary water-use estimates in the United States in 1985","interactions":[],"lastModifiedDate":"2012-02-02T00:07:16","indexId":"ofr87692","displayToPublicDate":"1994-01-01T00:00:00","publicationYear":"1987","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":"87-692","title":"Preliminary water-use estimates in the United States in 1985","docAbstract":"Preliminary 1985 water use estimates are tabulated by State for the Und States, Puerto Rico, the Virgin Islands, and the District of Columbia. Preliminary estimates of water withdrawn from surface water and groundwater sources for offstream water use categories are presented prior to publication of the final estimates in a U.S. Geological Survey Circular to allow for the timely release of the estimates to the general public. (Author 's abstract)","language":"ENGLISH","publisher":"U.S. Geological Survey,","doi":"10.3133/ofr87692","usgsCitation":"Solley, W., Pierce, R., and Merk, C., 1987, Preliminary water-use estimates in the United States in 1985: U.S. Geological Survey Open-File Report 87-692, 5 p. ;28 cm., https://doi.org/10.3133/ofr87692.","productDescription":"5 p. ;28 cm.","costCenters":[],"links":[{"id":150347,"rank":0,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/of/1987/0692/report-thumb.jpg"},{"id":44999,"rank":300,"type":{"id":11,"text":"Document"},"url":"https://pubs.usgs.gov/of/1987/0692/report.pdf","linkFileType":{"id":1,"text":"pdf"}}],"noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"4f4e4a9be4b07f02db65e66e","contributors":{"authors":[{"text":"Solley, W.B.","contributorId":25960,"corporation":false,"usgs":true,"family":"Solley","given":"W.B.","affiliations":[],"preferred":false,"id":172179,"contributorType":{"id":1,"text":"Authors"},"rank":1},{"text":"Pierce, R.R.","contributorId":52201,"corporation":false,"usgs":true,"family":"Pierce","given":"R.R.","email":"","affiliations":[],"preferred":false,"id":172180,"contributorType":{"id":1,"text":"Authors"},"rank":2},{"text":"Merk, C.F.","contributorId":67517,"corporation":false,"usgs":true,"family":"Merk","given":"C.F.","email":"","affiliations":[],"preferred":false,"id":172181,"contributorType":{"id":1,"text":"Authors"},"rank":3}]}} ,{"id":30144,"text":"wri864359 - 1987 - Hydraulic tests and chemical quality of water at well USW VH-1, Crater Flat, Nye County, Nevada","interactions":[],"lastModifiedDate":"2012-02-02T00:09:03","indexId":"wri864359","displayToPublicDate":"1994-01-01T00:00:00","publicationYear":"1987","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":"86-4359","title":"Hydraulic tests and chemical quality of water at well USW VH-1, Crater Flat, Nye County, Nevada","language":"ENGLISH","publisher":"U.S. Geological Survey,","doi":"10.3133/wri864359","usgsCitation":"Thordarson, W., and Howells, L., 1987, Hydraulic tests and chemical quality of water at well USW VH-1, Crater Flat, Nye County, Nevada: U.S. Geological Survey Water-Resources Investigations Report 86-4359, iv, 20 p. :ill., map ;28 cm., https://doi.org/10.3133/wri864359.","productDescription":"iv, 20 p. :ill., map ;28 cm.","costCenters":[],"links":[{"id":160475,"rank":0,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/wri/1986/4359/report-thumb.jpg"},{"id":58956,"rank":300,"type":{"id":11,"text":"Document"},"url":"https://pubs.usgs.gov/wri/1986/4359/report.pdf","linkFileType":{"id":1,"text":"pdf"}}],"noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"4f4e4a51e4b07f02db629b70","contributors":{"authors":[{"text":"Thordarson, William","contributorId":23539,"corporation":false,"usgs":true,"family":"Thordarson","given":"William","email":"","affiliations":[],"preferred":false,"id":202758,"contributorType":{"id":1,"text":"Authors"},"rank":1},{"text":"Howells, L.W.","contributorId":89887,"corporation":false,"usgs":true,"family":"Howells","given":"L.W.","email":"","affiliations":[],"preferred":false,"id":202759,"contributorType":{"id":1,"text":"Authors"},"rank":2}]}} ,{"id":30145,"text":"wri864342 - 1987 - Hydrogeology of the Faultless site, Nye County, Nevada","interactions":[],"lastModifiedDate":"2012-02-02T00:09:03","indexId":"wri864342","displayToPublicDate":"1994-01-01T00:00:00","publicationYear":"1987","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":"86-4342","title":"Hydrogeology of the Faultless site, Nye County, Nevada","language":"ENGLISH","publisher":"U.S. Geological Survey,","doi":"10.3133/wri864342","usgsCitation":"Thordarson, W., 1987, Hydrogeology of the Faultless site, Nye County, Nevada: U.S. Geological Survey Water-Resources Investigations Report 86-4342, v, 40 p. :ill., maps ;28 cm., https://doi.org/10.3133/wri864342.","productDescription":"v, 40 p. :ill., maps ;28 cm.","costCenters":[],"links":[{"id":119483,"rank":0,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/wri/1986/4342/report-thumb.jpg"},{"id":58957,"rank":300,"type":{"id":11,"text":"Document"},"url":"https://pubs.usgs.gov/wri/1986/4342/report.pdf","linkFileType":{"id":1,"text":"pdf"}}],"noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"4f4e4a2ee4b07f02db61518c","contributors":{"authors":[{"text":"Thordarson, William","contributorId":23539,"corporation":false,"usgs":true,"family":"Thordarson","given":"William","email":"","affiliations":[],"preferred":false,"id":202760,"contributorType":{"id":1,"text":"Authors"},"rank":1}]}} ,{"id":16396,"text":"ofr87757 - 1987 - Utah ground-water quality","interactions":[],"lastModifiedDate":"2012-02-02T00:07:02","indexId":"ofr87757","displayToPublicDate":"1994-01-01T00:00:00","publicationYear":"1987","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":"87-757","title":"Utah ground-water quality","language":"ENGLISH","publisher":"U.S. Geological Survey,","doi":"10.3133/ofr87757","usgsCitation":"Waddell, K., and Maxell, M., 1987, Utah ground-water quality: U.S. Geological Survey Open-File Report 87-757, iv, 10 p. :ill., maps ;28 cm., https://doi.org/10.3133/ofr87757.","productDescription":"iv, 10 p. :ill., maps ;28 cm.","costCenters":[],"links":[{"id":147694,"rank":0,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/of/1987/0757/report-thumb.jpg"},{"id":45362,"rank":300,"type":{"id":11,"text":"Document"},"url":"https://pubs.usgs.gov/of/1987/0757/report.pdf","linkFileType":{"id":1,"text":"pdf"}}],"noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"4f4e4a14e4b07f02db602e2f","contributors":{"authors":[{"text":"Waddell, K.M.","contributorId":59009,"corporation":false,"usgs":true,"family":"Waddell","given":"K.M.","email":"","affiliations":[],"preferred":false,"id":172779,"contributorType":{"id":1,"text":"Authors"},"rank":1},{"text":"Maxell, M.H.","contributorId":51756,"corporation":false,"usgs":true,"family":"Maxell","given":"M.H.","email":"","affiliations":[],"preferred":false,"id":172778,"contributorType":{"id":1,"text":"Authors"},"rank":2}]}} ,{"id":29637,"text":"wri864360 - 1987 - Geohydrology and susceptibility of major aquifers to surface contamination in Alabama; Area 8","interactions":[],"lastModifiedDate":"2012-02-02T00:08:56","indexId":"wri864360","displayToPublicDate":"1994-01-01T00:00:00","publicationYear":"1987","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":"86-4360","title":"Geohydrology and susceptibility of major aquifers to surface contamination in Alabama; Area 8","docAbstract":"The U.S. Geological Survey, in cooperation with the Alabama Department of Environmental Management, is conducting a series of geohydrologic studies to delineate the major aquifers and their susceptibility to contamination in Alabama. This report delineates and describes the geohydrology and susceptibility of the major aquifers to contamination in Area 8--Autauga, Chilton, Elmore, Lowndes, and Montgomery Counties. The major aquifers in the study area are the Eutaw, Gordo, and Coker aquifers of Cretaceous age. One or more of these aquifers are sources of public water supply in each of the five counties. The recharge areas for these aquifers are in Autauga, Chilton, Elmore, and Montgomery and Prattville. Maximum groundwater use in the Prattville area is more than 8 mgd (million gallons per day). Estimated maximum groundwater withdrawal for all uses in the study area is about 65 mgd. The potentiometric map of the Gordo aquifer indicates that the Alabama River may serve as a recharging boundary to the Gordo aquifer along the flood plain of the river in the Montgomery-Prattville area. The river also is acting as a recharging boundary to the Eutaw and Coker aquifers, where the potentiometric surfaces in the aquifers have been lowered. All recharge areas for the major aquifers are susceptible to contamination from the surface. However, the areas that are highly susceptible to contamination extend from Jemison to Clanton in Chilton County where the Coker aquifer generally is < 100 ft below land surface, and the flood plains of the Alabama, Coosa, and Tallapoosa Rivers, which are underlain by alluvial deposits that are in hydraulic contact with the major aquifers. Within the highly susceptible areas, the areas especially susceptible to contamination are the flood plain of the Alabama River in the Montgomery area and the flood plain of the Tallapoosa River. Pumpage from the major aquifers in this area has significantly lowered the potentiometric surface in the aquifers resulting in a downward gradient between the major aquifers and the Alabama River and the alluvial deposits underlying the flood plain along the river. (Lantz-PTT)","language":"ENGLISH","publisher":"U.S. Geological Survey,","doi":"10.3133/wri864360","usgsCitation":"Scott, J.C., Cobb, R., and Castleberry, R., 1987, Geohydrology and susceptibility of major aquifers to surface contamination in Alabama; Area 8: U.S. Geological Survey Water-Resources Investigations Report 86-4360, v, 65 p. :ill., maps (some col.) ;28 cm., https://doi.org/10.3133/wri864360.","productDescription":"v, 65 p. :ill., maps (some col.) ;28 cm.","costCenters":[],"links":[{"id":123691,"rank":0,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/wri/1986/4360/report-thumb.jpg"},{"id":58459,"rank":400,"type":{"id":17,"text":"Plate"},"url":"https://pubs.usgs.gov/wri/1986/4360/plate-1.pdf","linkFileType":{"id":1,"text":"pdf"}},{"id":58460,"rank":300,"type":{"id":11,"text":"Document"},"url":"https://pubs.usgs.gov/wri/1986/4360/report.pdf","linkFileType":{"id":1,"text":"pdf"}}],"noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"4f4e4ae0e4b07f02db688120","contributors":{"authors":[{"text":"Scott, J. C.","contributorId":75901,"corporation":false,"usgs":true,"family":"Scott","given":"J.","email":"","middleInitial":"C.","affiliations":[],"preferred":false,"id":201858,"contributorType":{"id":1,"text":"Authors"},"rank":1},{"text":"Cobb, R.H.","contributorId":31027,"corporation":false,"usgs":true,"family":"Cobb","given":"R.H.","email":"","affiliations":[],"preferred":false,"id":201857,"contributorType":{"id":1,"text":"Authors"},"rank":2},{"text":"Castleberry, R.D.","contributorId":101700,"corporation":false,"usgs":true,"family":"Castleberry","given":"R.D.","email":"","affiliations":[],"preferred":false,"id":201859,"contributorType":{"id":1,"text":"Authors"},"rank":3}]}} ,{"id":13380,"text":"ofr87406 - 1987 - Records of massive sulfide occurrences in Arizona","interactions":[],"lastModifiedDate":"2012-02-02T00:06:42","indexId":"ofr87406","displayToPublicDate":"1994-01-01T00:00:00","publicationYear":"1987","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":"87-406","title":"Records of massive sulfide occurrences in Arizona","language":"ENGLISH","publisher":"U.S. Geological Survey,","doi":"10.3133/ofr87406","usgsCitation":"Donnelly, M.E., Conway, C.M., and Earhart, R.L., 1987, Records of massive sulfide occurrences in Arizona: U.S. Geological Survey Open-File Report 87-406, i, 42 p. ;28 cm., https://doi.org/10.3133/ofr87406.","productDescription":"i, 42 p. ;28 cm.","costCenters":[],"links":[{"id":145184,"rank":0,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/of/1987/0406/report-thumb.jpg"},{"id":41807,"rank":300,"type":{"id":11,"text":"Document"},"url":"https://pubs.usgs.gov/of/1987/0406/report.pdf","linkFileType":{"id":1,"text":"pdf"}}],"noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"4f4e4a61e4b07f02db635762","contributors":{"authors":[{"text":"Donnelly, Michael E.","contributorId":13640,"corporation":false,"usgs":true,"family":"Donnelly","given":"Michael","email":"","middleInitial":"E.","affiliations":[],"preferred":false,"id":167709,"contributorType":{"id":1,"text":"Authors"},"rank":1},{"text":"Conway, Clay M.","contributorId":106860,"corporation":false,"usgs":true,"family":"Conway","given":"Clay","email":"","middleInitial":"M.","affiliations":[],"preferred":false,"id":167711,"contributorType":{"id":1,"text":"Authors"},"rank":2},{"text":"Earhart, Robert L.","contributorId":74729,"corporation":false,"usgs":true,"family":"Earhart","given":"Robert","email":"","middleInitial":"L.","affiliations":[],"preferred":false,"id":167710,"contributorType":{"id":1,"text":"Authors"},"rank":3}]}} ,{"id":29833,"text":"wri874080 - 1987 - Chemical characteristics of water in the surficial aquifer system, Dade County, Florida","interactions":[],"lastModifiedDate":"2022-01-10T12:41:32.20032","indexId":"wri874080","displayToPublicDate":"1994-01-01T00:00:00","publicationYear":"1987","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":"87-4080","title":"Chemical characteristics of water in the surficial aquifer system, Dade County, Florida","docAbstract":"Geohydrologic test drilling was conducted throughout Dade County to describe the chemical characteristics of water from geohydrologic units in the surficial aquifer system. Water quality analysis of samples collected from the test wells completed in central Dade County indicates that the Biscayne aquifer (unit A), the upper clastic unit of the Tamiami Formation (unit B), and parts of a limestone, sandstone, and sand unit of the Tamiami Formation (unit C) have been effectively flushed of residual seawater, and contain primarily calcium bicarbonate groundwater. The lower parts of unit C and the lower clastic unit of the Tamiami Formation (unit D) primarily contain calcium-sodium bicarbonate or sodium bicarbonate type water. An analysis of variance test indicates that water in units A and B is not significantly (0.05 probability level) different in composition. Mean concentrations of dissolved solids, sodium, and chloride are significantly different between units A and C, whereas mean concentrations of dissolved solids, calcium, sodium, and chloride are significantly different between units A and D. Groundwater in the surficial aquifer system in northwestern Dade County is more mineralized than groundwater that occurs elsewhere in the county (except in coastal areas affected by saltwater). An analysis of variance test indicates that mean concentrations of dissolved solids, sodium, and chloride at sites in northwestern Dade County, developed in units A and C, are significantly different from the mean concentrations of these constituents at sites throughout the rest of the county. Water in this part of the surficial aquifer system is similar to highly mineralized water found in western Broward County. However, in northwestern Dade County, the groundwater has been diluted to a greater extent by less mineralized recharge water. Overall, groundwater in the four major geohydrologic units of the surficial aquifer system of Dade County is suitable for most uses. Maximum concentrations of sodium, chloride, color, fluoride, iron, and dissolved solids in some areas of Dade County, however, exceed maximum contaminant levels established by the Florida Primary and Secondary Drinking Water Regulations standards. (Author 's abstract)","language":"English","publisher":"U.S. Geological Survey","publisherLocation":"Reston, VA","doi":"10.3133/wri874080","collaboration":"Prepared in cooperation with the South Florida Water Management District","usgsCitation":"Sonntag, W.H., 1987, Chemical characteristics of water in the surficial aquifer system, Dade County, Florida: U.S. Geological Survey Water-Resources Investigations Report 87-4080, iv, 42 p., https://doi.org/10.3133/wri874080.","productDescription":"iv, 42 p.","costCenters":[{"id":27821,"text":"Caribbean-Florida Water Science Center","active":true,"usgs":true}],"links":[{"id":124300,"rank":0,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/wri/1987/4080/coverthb.jpg"},{"id":58630,"rank":399,"type":{"id":17,"text":"Plate"},"url":"https://pubs.usgs.gov/wri/1987/4080/plate-1.pdf","linkFileType":{"id":1,"text":"pdf"}},{"id":58632,"rank":299,"type":{"id":11,"text":"Document"},"url":"https://pubs.usgs.gov/wri/1987/4080/report.pdf","text":"Report","size":"9.47 MB","linkFileType":{"id":1,"text":"pdf"},"description":"WRI 87-4080"},{"id":58631,"rank":400,"type":{"id":17,"text":"Plate"},"url":"https://pubs.usgs.gov/wri/1987/4080/plate-2.pdf","linkFileType":{"id":1,"text":"pdf"}}],"country":"United States","state":"Florida","county":"Dade County","geographicExtents":"{\n \"type\": \"FeatureCollection\",\n \"features\": [\n {\n \"type\": \"Feature\",\n \"properties\": {},\n \"geometry\": {\n \"type\": \"Polygon\",\n \"coordinates\": [\n [\n [\n -80.5572509765625,\n 25.591994180254712\n ],\n [\n -79.95574951171875,\n 25.591994180254712\n ],\n [\n -79.95574951171875,\n 26.162833742569937\n ],\n [\n -80.5572509765625,\n 26.162833742569937\n ],\n [\n -80.5572509765625,\n 25.591994180254712\n ]\n ]\n ]\n }\n }\n ]\n}","contact":"Caribbean-Florida Water Science Center
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No abstract available.
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Tyler Bend is on the Buffalo River about 1.5 miles upstream from U.S. Highway 65. The National Park Service is developing several recreational park sites along this scenic river. The magnitude, frequency, duration and velocities of floods are primary factors needed for establishing guidelines for developing facilities and managing park sites. The Park Service plans to develop park facilities at Tyler Bend and needs flood information at this site. This report provides information on the 100-, 75-, 50-, 30-, 20-, 10-, and 5-year floods on the Buffalo River at Tyler Bend. It was prepared by the U.S. Geological Survey in cooperation with the National Park Service and is based on data collected during the December 1982 flood, gaging station data for the Buffalo River near St. Joe, Arkansas and a Statewide flood-frequency report. (Lantz-PTT)","language":"ENGLISH","doi":"10.3133/wri874180","usgsCitation":"Neely, B., 1987, Flood characteristics of the Buffalo River at Tyler Bend, Arkansas: U.S. Geological Survey Water-Resources Investigations Report 87-4180, 1 map ; sheet 91 x 118 cm., https://doi.org/10.3133/wri874180.","productDescription":"1 map ; sheet 91 x 118 cm.","costCenters":[],"links":[{"id":168556,"rank":0,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/thumbnails/usgs_thumb.jpg"},{"id":81690,"rank":400,"type":{"id":17,"text":"Plate"},"url":"https://pubs.usgs.gov/wri/1987/4180/plate-1.pdf","linkFileType":{"id":1,"text":"pdf"}}],"noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"4f4e49f2e4b07f02db5ef1f6","contributors":{"authors":[{"text":"Neely, Braxtel L.","contributorId":37335,"corporation":false,"usgs":true,"family":"Neely","given":"Braxtel L.","affiliations":[],"preferred":false,"id":229707,"contributorType":{"id":1,"text":"Authors"},"rank":1}]}} ,{"id":44393,"text":"wri874049 - 1987 - Ground-water withdrawals from the confined aquifers in the Coastal Plain of Virginia, 1891-1983","interactions":[],"lastModifiedDate":"2012-02-02T00:11:01","indexId":"wri874049","displayToPublicDate":"1994-01-01T00:00:00","publicationYear":"1987","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":"87-4049","title":"Ground-water withdrawals from the confined aquifers in the Coastal Plain of Virginia, 1891-1983","language":"ENGLISH","doi":"10.3133/wri874049","usgsCitation":"Kull, T., and Laczniak, R.J., 1987, Ground-water withdrawals from the confined aquifers in the Coastal Plain of Virginia, 1891-1983: U.S. Geological Survey Water-Resources Investigations Report 87-4049, 37 p., https://doi.org/10.3133/wri874049.","productDescription":"37 p.","costCenters":[],"links":[{"id":169116,"rank":0,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/thumbnails/usgs_thumb.jpg"}],"noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"4f4e4afce4b07f02db69663d","contributors":{"authors":[{"text":"Kull, T.K.","contributorId":95120,"corporation":false,"usgs":true,"family":"Kull","given":"T.K.","email":"","affiliations":[],"preferred":false,"id":229692,"contributorType":{"id":1,"text":"Authors"},"rank":1},{"text":"Laczniak, R. J.","contributorId":46104,"corporation":false,"usgs":true,"family":"Laczniak","given":"R.","email":"","middleInitial":"J.","affiliations":[],"preferred":false,"id":229691,"contributorType":{"id":1,"text":"Authors"},"rank":2}]}} ,{"id":14537,"text":"ofr87207 - 1987 - Columbia Glacier in 1986; 800 meters retreat","interactions":[],"lastModifiedDate":"2012-02-02T00:06:46","indexId":"ofr87207","displayToPublicDate":"1994-01-01T00:00:00","publicationYear":"1987","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":"87-207","title":"Columbia Glacier in 1986; 800 meters retreat","docAbstract":"Columbia Glacier, in Prince William Sound, Alaska, continued its rapid retreat in 1986, with a retreat of 800 m. Average velocity of the lower portion of the glacier, 10 September 1986 to 26 January 1987, was three km/yr, or about one-half of the velocity during similar periods for the previous three years. This reduced velocity is a new development in the progression of the retreat, and if the calving rate follows the pattern of previous years, will result in continued retreat. (Author 's abstract)","language":"ENGLISH","publisher":"U.S. Geological Survey,","doi":"10.3133/ofr87207","usgsCitation":"Krimmel, R.M., 1987, Columbia Glacier in 1986; 800 meters retreat: U.S. Geological Survey Open-File Report 87-207, i, 7 p. :ill., map ;28 cm., https://doi.org/10.3133/ofr87207.","productDescription":"i, 7 p. :ill., map ;28 cm.","costCenters":[],"links":[{"id":146290,"rank":0,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/of/1987/0207/report-thumb.jpg"},{"id":43216,"rank":300,"type":{"id":11,"text":"Document"},"url":"https://pubs.usgs.gov/of/1987/0207/report.pdf","linkFileType":{"id":1,"text":"pdf"}}],"noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"4f4e4b24e4b07f02db6ae820","contributors":{"authors":[{"text":"Krimmel, R. 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R.","contributorId":34911,"corporation":false,"usgs":true,"family":"Kirk","given":"A.","email":"","middleInitial":"R.","affiliations":[],"preferred":false,"id":267767,"contributorType":{"id":1,"text":"Authors"},"rank":1},{"text":"Zech, R. S.","contributorId":51289,"corporation":false,"usgs":true,"family":"Zech","given":"R.","email":"","middleInitial":"S.","affiliations":[],"preferred":false,"id":267768,"contributorType":{"id":1,"text":"Authors"},"rank":2}]}} ,{"id":14536,"text":"ofr87219 - 1987 - Columbia Glacier, Alaska, photogrammetry data set, 1981-82 and 1984-85","interactions":[],"lastModifiedDate":"2012-02-02T00:06:46","indexId":"ofr87219","displayToPublicDate":"1994-01-01T00:00:00","publicationYear":"1987","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":"87-219","title":"Columbia Glacier, Alaska, photogrammetry data set, 1981-82 and 1984-85","docAbstract":"Photogrammetric processing of 12 sets of vertical aerial photography of the Columbia Glacier, Alaska, has measured the altitude and velocity fields of the lowest 14,000 m of the glacier during the periods of September 1981 to October 1982 and October 1984 to September 1985. The data set consists of the location of 3,604 points on the glacier, 1,161 points along the glacier terminus, and 1,116 points along the top of the terminus ice cliff. During the 1981 to 1985 period the terminus of the glacier receded 1,350 m, the ice near the terminus thinned at a rate of 18 m/year, and ice velocity near the terminus tripled, reaching as much as 6,000 m/year. (Author 's abstract)","language":"ENGLISH","publisher":"U.S. Geological Survey,","doi":"10.3133/ofr87219","usgsCitation":"Krimmel, R.M., 1987, Columbia Glacier, Alaska, photogrammetry data set, 1981-82 and 1984-85: U.S. Geological Survey Open-File Report 87-219, iii, 104 p. :ill., map ;28 cm., https://doi.org/10.3133/ofr87219.","productDescription":"iii, 104 p. :ill., map ;28 cm.","costCenters":[],"links":[{"id":146289,"rank":0,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/of/1987/0219/report-thumb.jpg"},{"id":43215,"rank":300,"type":{"id":11,"text":"Document"},"url":"https://pubs.usgs.gov/of/1987/0219/report.pdf","linkFileType":{"id":1,"text":"pdf"}}],"noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"4f4e4b24e4b07f02db6ae813","contributors":{"authors":[{"text":"Krimmel, R. 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