{"pageNumber":"3714","pageRowStart":"92825","pageSize":"25","recordCount":185258,"records":[{"id":70129431,"text":"70129431 - 1996 - Seismic reflection profile of the Blake Ridge near sites 994, 995, and 997","interactions":[],"lastModifiedDate":"2022-12-30T15:52:28.414079","indexId":"70129431","displayToPublicDate":"1997-10-22T12:08:00","publicationYear":"1996","noYear":false,"publicationType":{"id":5,"text":"Book chapter"},"publicationSubtype":{"id":24,"text":"Book Chapter"},"chapter":"4","title":"Seismic reflection profile of the Blake Ridge near sites 994, 995, and 997","docAbstract":"Seismic reflection profiles near Sites 994, 995, and 997 were collected with seismic sources that provide maximum resolution with adequate power to image the zone of gas hydrate stability and the region direction beneath it. The overall structure of the sediment drift deposit that constitutes the Blake Ridge consists of southwestward-dipping strata. These strata are approximately conformal to the seafloor on the southwest side of the ridge and are truncated by erosion on the northeast side. A bottom-simulating reflection (BSR) marks the velocity contrast between gas hydrate-bearing sediment and regions containing free gas beneath the zone of gas hydrate stability. The BSR is strong and continuous near the ridge crest but becomes discontinuous on the flanks, where concentration of gas is reduced and dipping strata pass through the level of the base o fgas hydrate stability or the strata are disrupted by faults. Seismic reflection amplitudes appear to be reduced in the region of gas hydrate formation compared to normal amplitudes. A faulted zone ~0.5-0.6 s thick parallels reflections from strata. We infer that this may represent a formerly gas hydrate-bearing zone that was faulted because of a breakdown of hydrate near its phase limit (at the base of the zone). Strong reflections at the top of the faulted zone are caused by free-gas acccumulation at Site 994. Similar strong reflections probably are caused by free-gas accumulations where the top of the faulted zone rises above the BSR, although this would require local free gas within the hydrate-stable zone.","largerWorkType":{"id":4,"text":"Book"},"largerWorkTitle":"Gas hydrate sampling on the Blake Ridge and Carolina Rise Sites 991-997: Proceedings of the Ocean Drilling Program, Initial Reports","largerWorkSubtype":{"id":12,"text":"Conference publication"},"language":"English","publisher":"Texas A&M","doi":"10.2973/odp.proc.ir.164.104.1996","usgsCitation":"Dillon, W.P., Hutchinson, D.R., and Drury, R.M., 1996, Seismic reflection profile of the Blake Ridge near sites 994, 995, and 997, chap. 4 of Gas hydrate sampling on the Blake Ridge and Carolina Rise Sites 991-997: Proceedings of the Ocean Drilling Program, Initial Reports, v. 164, p. 47-56, https://doi.org/10.2973/odp.proc.ir.164.104.1996.","productDescription":"10 p.","startPage":"47","endPage":"56","costCenters":[{"id":186,"text":"Coastal and Marine Geology Program","active":true,"usgs":true},{"id":678,"text":"Woods Hole Coastal and Marine Science Center","active":true,"usgs":true}],"links":[{"id":489220,"rank":2,"type":{"id":40,"text":"Open Access Publisher Index Page"},"url":"https://doi.org/10.2973/odp.proc.ir.164.104.1996","text":"Publisher Index Page"},{"id":295605,"rank":1,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/thumbnails/outside_thumb.jpg"}],"country":"United States","otherGeospatial":"Blake Plateau","geographicExtents":"{\n \"type\": \"FeatureCollection\",\n \"features\": [\n {\n \"type\": \"Feature\",\n \"properties\": {},\n \"geometry\": {\n \"type\": \"Polygon\",\n \"coordinates\": [\n [\n [\n -76,\n 31\n ],\n [\n -75,\n 31\n ],\n [\n -75,\n 32.5\n ],\n [\n -76,\n 32.5\n ],\n [\n -76,\n 31\n ]\n ]\n ]\n }\n }\n ]\n}","volume":"164","noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"5448c721e4b0f888a81b87b3","contributors":{"authors":[{"text":"Dillon, William P. bdillon@usgs.gov","contributorId":79820,"corporation":false,"usgs":true,"family":"Dillon","given":"William","email":"bdillon@usgs.gov","middleInitial":"P.","affiliations":[{"id":678,"text":"Woods Hole Coastal and Marine Science Center","active":true,"usgs":true}],"preferred":false,"id":503708,"contributorType":{"id":1,"text":"Authors"},"rank":1},{"text":"Hutchinson, Deborah R. 0000-0002-2544-5466 dhutchinson@usgs.gov","orcid":"https://orcid.org/0000-0002-2544-5466","contributorId":521,"corporation":false,"usgs":true,"family":"Hutchinson","given":"Deborah","email":"dhutchinson@usgs.gov","middleInitial":"R.","affiliations":[{"id":678,"text":"Woods Hole Coastal and Marine Science Center","active":true,"usgs":true}],"preferred":false,"id":503706,"contributorType":{"id":1,"text":"Authors"},"rank":2},{"text":"Drury, Rebecca M.","contributorId":35668,"corporation":false,"usgs":true,"family":"Drury","given":"Rebecca","email":"","middleInitial":"M.","affiliations":[],"preferred":false,"id":503707,"contributorType":{"id":1,"text":"Authors"},"rank":3}]}} ,{"id":70129430,"text":"70129430 - 1996 - A review of the tectonic problems of the strike-slip northern boundary of the Caribbean Plate and examination by GLORIA","interactions":[],"lastModifiedDate":"2023-01-02T16:10:47.085933","indexId":"70129430","displayToPublicDate":"1997-10-22T11:48:00","publicationYear":"1996","noYear":false,"publicationType":{"id":5,"text":"Book chapter"},"publicationSubtype":{"id":24,"text":"Book Chapter"},"chapter":"9","title":"A review of the tectonic problems of the strike-slip northern boundary of the Caribbean Plate and examination by GLORIA","docAbstract":"No abstract available.","largerWorkType":{"id":4,"text":"Book"},"largerWorkTitle":"Geology of the United States' seafloor: The view from GLORIA","largerWorkSubtype":{"id":15,"text":"Monograph"},"language":"English","publisher":"Cambridge University Press","usgsCitation":"Dillon, W.P., Edgar, N., Scanlon, K.M., and Coleman, D., 1996, A review of the tectonic problems of the strike-slip northern boundary of the Caribbean Plate and examination by GLORIA, chap. 9 of Geology of the United States' seafloor: The view from GLORIA, p. 135-168.","productDescription":"34 p.","startPage":"135","endPage":"168","costCenters":[{"id":186,"text":"Coastal and Marine Geology Program","active":true,"usgs":true},{"id":678,"text":"Woods Hole Coastal and Marine Science Center","active":true,"usgs":true}],"links":[{"id":295602,"rank":1,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/thumbnails/outside_thumb.jpg"}],"country":"Cuba, Dominican Republic, Haiti","otherGeospatial":"Caribbean Sea","geographicExtents":"{\n \"type\": \"FeatureCollection\",\n \"features\": [\n {\n \"type\": \"Feature\",\n \"properties\": {},\n \"geometry\": {\n \"coordinates\": [\n [\n [\n -89.14043852664736,\n 15.770146738057335\n ],\n [\n -87.09475682616744,\n 15.662497960505988\n ],\n [\n -78.91193741181382,\n 18.68251440379322\n ],\n [\n -72.83170201171521,\n 19.651272835101196\n ],\n [\n -69.57667649322153,\n 19.164734568945818\n ],\n [\n -64.59001652472224,\n 19.05308026186796\n ],\n [\n -64.24093614283848,\n 20.49412171309409\n ],\n [\n -73.02339573623509,\n 20.691423123312035\n ],\n [\n -77.57922557893649,\n 20.410668557060305\n ],\n [\n -82.80357322852099,\n 18.908796653400856\n ],\n [\n -89.14043852664736,\n 15.770146738057335\n ]\n ]\n ],\n \"type\": \"Polygon\"\n }\n }\n ]\n}","noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"5448c717e4b0f888a81b87a3","contributors":{"editors":[{"text":"Gardner, J. V.","contributorId":114111,"corporation":false,"usgs":true,"family":"Gardner","given":"J.","email":"","middleInitial":"V.","affiliations":[],"preferred":false,"id":510017,"contributorType":{"id":2,"text":"Editors"},"rank":1},{"text":"Field, M. E.","contributorId":113991,"corporation":false,"usgs":true,"family":"Field","given":"M.","email":"","middleInitial":"E.","affiliations":[],"preferred":false,"id":510016,"contributorType":{"id":2,"text":"Editors"},"rank":2},{"text":"Twichell, D. C.","contributorId":111957,"corporation":false,"usgs":true,"family":"Twichell","given":"D.","email":"","middleInitial":"C.","affiliations":[],"preferred":false,"id":510015,"contributorType":{"id":2,"text":"Editors"},"rank":3}],"authors":[{"text":"Dillon, William P. bdillon@usgs.gov","contributorId":79820,"corporation":false,"usgs":true,"family":"Dillon","given":"William","email":"bdillon@usgs.gov","middleInitial":"P.","affiliations":[{"id":678,"text":"Woods Hole Coastal and Marine Science Center","active":true,"usgs":true}],"preferred":false,"id":503703,"contributorType":{"id":1,"text":"Authors"},"rank":1},{"text":"Edgar, N. Terence","contributorId":74697,"corporation":false,"usgs":true,"family":"Edgar","given":"N. Terence","affiliations":[],"preferred":false,"id":503702,"contributorType":{"id":1,"text":"Authors"},"rank":2},{"text":"Scanlon, Kathryn M.","contributorId":6816,"corporation":false,"usgs":true,"family":"Scanlon","given":"Kathryn","email":"","middleInitial":"M.","affiliations":[],"preferred":false,"id":503705,"contributorType":{"id":1,"text":"Authors"},"rank":3},{"text":"Coleman, Dwight F.","contributorId":81827,"corporation":false,"usgs":true,"family":"Coleman","given":"Dwight F.","affiliations":[],"preferred":false,"id":503704,"contributorType":{"id":1,"text":"Authors"},"rank":4}]}} ,{"id":5042,"text":"fs02196 - 1996 - U.S. Geological Survey programs in Massachusetts","interactions":[],"lastModifiedDate":"2012-02-02T00:05:42","indexId":"fs02196","displayToPublicDate":"1997-10-01T00:00:00","publicationYear":"1996","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":"021-96","title":"U.S. Geological Survey programs in Massachusetts","language":"ENGLISH","publisher":"The Survey,","doi":"10.3133/fs02196","usgsCitation":"Water Resources Division, U.S. Geological Survey, 1996, U.S. Geological Survey programs in Massachusetts: U.S. Geological Survey Fact Sheet 021-96, [4] p. : col. ill., maps ; 28 cm. col. ill., maps ;, https://doi.org/10.3133/fs02196.","productDescription":"[4] p. : col. ill., maps ; 28 cm. col. ill., maps ;","costCenters":[],"links":[{"id":118440,"rank":0,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/thumbnails/fs_021_96.bmp"},{"id":358,"rank":100,"type":{"id":15,"text":"Index Page"},"url":"https://pubs.usgs.gov/FS/FS-021-96","linkFileType":{"id":5,"text":"html"}}],"noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"4f4e4a2ae4b07f02db61236d","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":528416,"contributorType":{"id":1,"text":"Authors"},"rank":1}]}} ,{"id":21851,"text":"ofr96112 - 1996 - Ground-penetrating radar and electromagnetic surveys at the Monroe Crossroads battlefield site, Fort Bragg, North Carolina","interactions":[],"lastModifiedDate":"2012-02-02T00:07:42","indexId":"ofr96112","displayToPublicDate":"1997-10-01T00:00:00","publicationYear":"1996","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":"96-112","title":"Ground-penetrating radar and electromagnetic surveys at the Monroe Crossroads battlefield site, Fort Bragg, North Carolina","docAbstract":"A ground-penetrating radar survey was conducted at the Monroe Crossroads Battlefield site at Fort Bragg, North Carolina, to determine possible locations of subsurface archaeological features. An electromagnetic survey also was conducted at the site to verify and augment the ground-penetrating radar data. The surveys were conducted over a 67,200-square-foot grid with a grid point spacing of 20 feet.\r\n\r\nDuring the ground-penetrating radar survey, 87 subsurface anomalies were detected based on visual inspection of the field records. These anomalies were flagged in the field as they appeared on the ground-penetrating radar records and were located by a land survey. The electromagnetic survey produced two significant readings at ground-penetrating radar anomaly locations.\r\n\r\nThe National Park Service excavated 44 of the 87 anomaly locations at the Civil War battlefield site. Four of these excavations produced significant archaeological features, including one at an abandoned well.","language":"ENGLISH","publisher":"U.S. Geological Survey,","doi":"10.3133/ofr96112","issn":"0566-8174","usgsCitation":"Kessler, R., Strain, R., Marlowe, J.I., and Currin, K., 1996, Ground-penetrating radar and electromagnetic surveys at the Monroe Crossroads battlefield site, Fort Bragg, North Carolina: U.S. Geological Survey Open-File Report 96-112, 1 p. :ill. ;99 x 85 cm. folded to 25 x 22 cm., https://doi.org/10.3133/ofr96112.","productDescription":"1 p. :ill. ;99 x 85 cm. folded to 25 x 22 cm.","costCenters":[],"links":[{"id":153204,"rank":0,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/thumbnails/usgs_thumb.jpg"},{"id":19401,"rank":400,"type":{"id":17,"text":"Plate"},"url":"https://pubs.usgs.gov/of/1996/0112/plate-1.pdf","linkFileType":{"id":1,"text":"pdf"}}],"noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"4f4e4ab0e4b07f02db66d44b","contributors":{"authors":[{"text":"Kessler, Richard","contributorId":104926,"corporation":false,"usgs":true,"family":"Kessler","given":"Richard","email":"","affiliations":[],"preferred":false,"id":185971,"contributorType":{"id":1,"text":"Authors"},"rank":1},{"text":"Strain, R.E.","contributorId":9517,"corporation":false,"usgs":true,"family":"Strain","given":"R.E.","email":"","affiliations":[],"preferred":false,"id":185969,"contributorType":{"id":1,"text":"Authors"},"rank":2},{"text":"Marlowe, J. I. II","contributorId":6939,"corporation":false,"usgs":true,"family":"Marlowe","given":"J.","suffix":"II","email":"","middleInitial":"I.","affiliations":[],"preferred":false,"id":185968,"contributorType":{"id":1,"text":"Authors"},"rank":3},{"text":"Currin, K.B.","contributorId":70642,"corporation":false,"usgs":true,"family":"Currin","given":"K.B.","email":"","affiliations":[],"preferred":false,"id":185970,"contributorType":{"id":1,"text":"Authors"},"rank":4}]}} ,{"id":22932,"text":"ofr96166 - 1996 - Selected ground-water data for the Lummi Indian Reservation, Whatcom County, Washington, 1995","interactions":[],"lastModifiedDate":"2012-02-02T00:07:51","indexId":"ofr96166","displayToPublicDate":"1997-10-01T00:00:00","publicationYear":"1996","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":"96-166","title":"Selected ground-water data for the Lummi Indian Reservation, Whatcom County, Washington, 1995","language":"ENGLISH","publisher":"U.S. Geological Survey ;\r\nEarth Science Information Center, Open-File Reports Section [distributor],","doi":"10.3133/ofr96166","issn":"0094-9140","usgsCitation":"Drost, B., 1996, Selected ground-water data for the Lummi Indian Reservation, Whatcom County, Washington, 1995: U.S. Geological Survey Open-File Report 96-166, iii, 21 p. :ill., col. map ;28 cm., https://doi.org/10.3133/ofr96166.","productDescription":"iii, 21 p. :ill., col. map ;28 cm.","costCenters":[],"links":[{"id":153586,"rank":0,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/of/1996/0166/report-thumb.jpg"},{"id":52333,"rank":400,"type":{"id":17,"text":"Plate"},"url":"https://pubs.usgs.gov/of/1996/0166/plate-1.pdf","linkFileType":{"id":1,"text":"pdf"}},{"id":52334,"rank":300,"type":{"id":11,"text":"Document"},"url":"https://pubs.usgs.gov/of/1996/0166/report.pdf","linkFileType":{"id":1,"text":"pdf"}}],"noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"4f4e4a07e4b07f02db5f965a","contributors":{"authors":[{"text":"Drost, B. W.","contributorId":38526,"corporation":false,"usgs":true,"family":"Drost","given":"B. W.","affiliations":[],"preferred":false,"id":189153,"contributorType":{"id":1,"text":"Authors"},"rank":1}]}} ,{"id":22630,"text":"ofr96212 - 1996 - Documentation of model input and output values for the simulation of the ground-water flow system in the Cretaceous-age Coastal Plain aquifers of South Carolina","interactions":[],"lastModifiedDate":"2017-01-04T13:07:03","indexId":"ofr96212","displayToPublicDate":"1997-10-01T00:00:00","publicationYear":"1996","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":"96-212","title":"Documentation of model input and output values for the simulation of the ground-water flow system in the Cretaceous-age Coastal Plain aquifers of South Carolina","docAbstract":"This report and the attached 3 1/2-inch diskette contain, in compressed format, the data sets for the model of ground-water flow in the Cretaceous-age Coastal Plain aquifers of South Carolina. The data sets can be uncompressed using a program provided with this report. The uncompressed files require approximately 3.7 megabytes of disk space on an IBM-compatible microcomputer1 using the MS-DOS operating system. 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G.","contributorId":68764,"corporation":false,"usgs":true,"family":"Campbell","given":"B.","email":"","middleInitial":"G.","affiliations":[],"preferred":false,"id":188602,"contributorType":{"id":1,"text":"Authors"},"rank":1},{"text":"van Heeswijk, Marijke heeswijk@usgs.gov","contributorId":1537,"corporation":false,"usgs":true,"family":"van Heeswijk","given":"Marijke","email":"heeswijk@usgs.gov","affiliations":[],"preferred":true,"id":188601,"contributorType":{"id":1,"text":"Authors"},"rank":2}]}} ,{"id":28927,"text":"wri954282 - 1996 - Water and bed-material quality of selected streams and reservoirs in the Research Triangle area of North Carolina, 1988-94","interactions":[],"lastModifiedDate":"2017-01-27T12:15:15","indexId":"wri954282","displayToPublicDate":"1997-10-01T00:00:00","publicationYear":"1996","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":"95-4282","title":"Water and bed-material quality of selected streams and reservoirs in the Research Triangle area of North Carolina, 1988-94","docAbstract":"The Triangle Area Water Supply Monitoring Project was formed by a consortium of local governments and governmental agencies in cooperation with the U.S. Geological Survey to supplement existing data on conventional pollutants, nutrients, and metals to enable eventual determination of long-term trends; to examine spatial differences among water supplies within the region, especially differences between smaller upland sources, large multipurpose reservoirs, and run-of-river supplies; to provide tributary loading inlake data for predictive modeling of Falls of the Neuse and B. Everett Jordan reservoirs; and to establish a database for synthetic organic compounds.\r\n\r\nWater-quality sampling began in October 1988 at 35 sites located on area run-of-river and reservoir water supplies and their tributaries. Sampling has continued through 1994. Samples were analyzed for major ions, nutrients, trace metals, pesticides, and semivolatile and volatile organic compounds. Monthly concentration data, high-flow concentration data, and data on daily mean streamflow at most stream sites were used to calculate loadings of nitrogen, phosphorus, suspended sediment, and trace metals to reservoirs.\r\n\r\nStream and lake sites were assigned to one of five site categories-- (1) rivers, (2) large multipurpose reservoirs, (3) small water-supply reservoirs, (4) streams below urban areas and wastewater-treatment plants, and (5) headwater streams--according to general site characteristics. Concentrations of nitrogen species, phosphorus species, and selected trace metals were compared by site category using nonparametric analysis of variance techniques and qualitatively (trace metals). Wastewater-treatment plant effluents and urban runoff had a significant impact on water quality compared to reservoirs and headwater streams. Streams draining these areas had more mineralized water than streams draining undeveloped areas. Moreover, median nitrogen and nitrite plus nitrate concentrations were significantly greater than all other site categories. Phosphorus was significantly greater than for reservoir sites or headwater streams. Few concentrations of trace metals were greater than the minimum reporting limit, and U.S. Environmental Protection Agency drinking-water standards were rarely exceeded. Detections, when they occurred, were most frequent for sites below urban areas and wastewater-treatment plant effluents.\r\n\r\nA small number of samples for analysis of acetanilide, triazine, carbamate, and chlorophenoxy acid pesticides indicate that some of these compounds are generally present in area waters in small concentrations. Organochlorine and organophosphorus pesticides are ubiquitous in the study area in very small concentrations. Trihalomethanes were detected at sites below urban areas and wastewater-treatment plants. Otherwise, volatile organic compounds and semivolatile compounds were generally not detected.\r\n\r\nSuspended-sediment, nitrogen, phosphorus, lead, and zinc loads into Falls Lake, Jordan Lake, University Lake, Cane Creek Reservoir, Little River Reservoir, and Lake Michie were calculated. In general, reservoirs act as traps for suspended sediment and constituents associated with suspended sediments.\r\n\r\nDuring 1989-94, annual suspended-sediment load to Falls Lake ranged from 29,500 to 88,200 tons. Because Lake Michie trapped from 83 to 93 percent of the suspended sediment delivered by Flat River, Flat River is a minor contributor of suspended sediment to Falls Lake. Yields of suspended sediment from Little River, Little Lick Creek, and Flat River Basins were between 184 and 223 tons per square mile and appear to have increased increased slightly from yields reported in a study for the period 1970-79. Annual suspended-sediment load to Jordan Lake ranged from 271,000 to 622,000 tons from 1989 through 1994 water years. The Haw River contributed more than 75 percent of the tota load to Jordan Lake. The suspended-sediment yields for Haw River and Northeast Cree","language":"ENGLISH","publisher":"U.S. Geological Survey ;\r\nInformation Services [distributor],","doi":"10.3133/wri954282","usgsCitation":"Oblinger, C.J., and Treece, M., 1996, Water and bed-material quality of selected streams and reservoirs in the Research Triangle area of North Carolina, 1988-94: U.S. Geological Survey Water-Resources Investigations Report 95-4282, v, 79 p. :ill., maps ;28 cm., https://doi.org/10.3133/wri954282.","productDescription":"v, 79 p. :ill., maps ;28 cm.","costCenters":[{"id":13634,"text":"South Atlantic Water Science Center","active":true,"usgs":true}],"links":[{"id":57800,"rank":300,"type":{"id":11,"text":"Document"},"url":"https://pubs.usgs.gov/wri/1995/4282/report.pdf","linkFileType":{"id":1,"text":"pdf"}},{"id":159158,"rank":0,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/wri/1995/4282/report-thumb.jpg"}],"country":"United States","state":"North 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Jr.","contributorId":60255,"corporation":false,"usgs":true,"family":"Treece","given":"M.W.","suffix":"Jr.","email":"","affiliations":[],"preferred":false,"id":200633,"contributorType":{"id":1,"text":"Authors"},"rank":2}]}} ,{"id":24052,"text":"ofr9675 - 1996 - Geophysical logs and groundwater chemistry in the A/M Area, final report, Savannah River site, South Carolina","interactions":[],"lastModifiedDate":"2017-01-05T11:08:26","indexId":"ofr9675","displayToPublicDate":"1997-10-01T00:00:00","publicationYear":"1996","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":"96-75","title":"Geophysical logs and groundwater chemistry in the A/M Area, final report, Savannah River site, South Carolina","language":"ENGLISH","publisher":"U.S. Geological 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H.","contributorId":42238,"corporation":false,"usgs":true,"family":"Nelson","given":"P.","email":"","middleInitial":"H.","affiliations":[],"preferred":false,"id":191223,"contributorType":{"id":1,"text":"Authors"},"rank":1},{"text":"Kibler, J. 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The data collected at each site included net radiation, air temperature at two heights, dew-point temperature at two heights, windspeed at two heights, soil heat flux, and soil temperature in the interval between the land surface and the buried heat-flux plates.","language":"ENGLISH","publisher":"U.S. Geological Survey ;Information Services [distributor],","doi":"10.3133/ofr96170","issn":"0094-9140","collaboration":"The USGS does not support this software or technical questions for the software associated with the publication.","usgsCitation":"Nichols, W.D., and Rapp, T., 1996, Micrometeorological data for energy-budget studies near Rogers Spring, Ash Meadows National Wildlife Refuge, Nye County, Nevada, 1994: U.S. Geological Survey Open-File Report 96-170, iv, 49 p. :ill. ;28 cm. +1 computer disk (3 1/2 in.), https://doi.org/10.3133/ofr96170.","productDescription":"iv, 49 p. :ill. ;28 cm. +1 computer disk (3 1/2 in.)","costCenters":[],"links":[{"id":156222,"rank":0,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/of/1996/0170/report-thumb.jpg"},{"id":53231,"rank":300,"type":{"id":11,"text":"Document"},"url":"https://pubs.usgs.gov/of/1996/0170/report.pdf","linkFileType":{"id":1,"text":"pdf"}},{"id":277647,"type":{"id":4,"text":"Application Site"},"url":"https://pubs.usgs.gov/of/1996/0170/application.zip"}],"noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"4f4e4a57e4b07f02db62e466","contributors":{"authors":[{"text":"Nichols, W. D.","contributorId":73220,"corporation":false,"usgs":true,"family":"Nichols","given":"W.","middleInitial":"D.","affiliations":[],"preferred":false,"id":191232,"contributorType":{"id":1,"text":"Authors"},"rank":1},{"text":"Rapp, T.R.","contributorId":51784,"corporation":false,"usgs":true,"family":"Rapp","given":"T.R.","email":"","affiliations":[],"preferred":false,"id":191231,"contributorType":{"id":1,"text":"Authors"},"rank":2}]}} ,{"id":21644,"text":"ofr9670 - 1996 - Catalog of earthquake hypocenters for Augustine, Redoubt, Iliamna, and Mount Spurr volcanoes, Alaska: January 1, 1991 - December 31, 1993","interactions":[],"lastModifiedDate":"2019-06-06T13:02:02","indexId":"ofr9670","displayToPublicDate":"1997-10-01T00:00:00","publicationYear":"1996","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":"96-70","title":"Catalog of earthquake hypocenters for Augustine, Redoubt, Iliamna, and Mount Spurr volcanoes, Alaska: January 1, 1991 - December 31, 1993","docAbstract":"

The Alaska Volcano Observatory (AVO), a cooperative program of the U.S. Geological Survey, the Geophysical Institute of the University of Alaska, Fairbanks, and the Alaska Division of Geological and Geophysical Surveys, has maintained a program of seismic monitoring at potentially active volcanoes in the Cook Inlet region since 1988. The principal objectives of this program include the seismic surveillance of the Cook Inlet volcanoes and the investigation of seismic processes associated with active volcanism. This catalog reflects the status and evolution of the seismic monitoring program, and presents the basic seismic data for the time interval January 1, 1991, to December 31, 1993. For an interpretation of these data the reader should refer to several recent articles on volcano related seismicity in the Cook Inlet region (e.g. Jolly and others, 1994; Power and others, 1995; and McNutt and others, 1995). A similar catalog covers the period from October 12, 1989 to December 31, 1991 (Power and others 1993).

\n

The AVO seismic monitoring program has undergone significant changes during the catalog period. The changes included 1) new seismic stations placed at Mount Spurr and Redoubt Volcano, resulting in increased earthquake detection capability and improved earthquake locations, 2) the addition of several regional stations to the seismic data acquisition system which improved location quality near the volcano and enhanced our ability to scale eruptions and measure magnitudes of the largest volcanic earthquakes, 3) installation of a new event detection algorithm XDETECT (Rogers, 1993), which offered increased data collection capabilities , 4) modifications to the earthquake location program HYPOELLIPSE (Lahr, 1989) which now allows distinct velocity models and station corrections at each volcanic center, and 5) the addition of seismic stations at Augustine and niamna volcanoes to the data acquisition/location system.

\n

The 1992 eruptions at Mount Spurr's Crater Peak vent provided the highlight of the catalog period. The crisis included three sub-plinian eruptions, which occurred on June 27, August 18, and September 16-17, 1992. The three eruptions punctuated a complex seismic sequence which included volcano-tectonic (VT) earthquakes, tremor, and both deep and shallow long period (LP) earthquakes. The seismic sequence began on August 18, 1991, with a small swarm of volcano-tectonic events beneath Crater Peak, and spread throughout the volcanic complex by November of the same year. Elevated levels of seismicity persisted at Mount Spurr beyond the catalog time period.

","language":"English","publisher":"U.S. Geological Survey,","doi":"10.3133/ofr9670","issn":"0566-8174","usgsCitation":"Jolly, A.D., Power, J.A., Stihler, S.D., Rao, L.N., Davidson, G., Paskievitch, J.F., Estes, S., and Lahr, J.C., 1996, Catalog of earthquake hypocenters for Augustine, Redoubt, Iliamna, and Mount Spurr volcanoes, Alaska: January 1, 1991 - December 31, 1993: U.S. Geological Survey Open-File Report 96-70, 89 p., https://doi.org/10.3133/ofr9670.","productDescription":"89 p.","onlineOnly":"N","additionalOnlineFiles":"N","costCenters":[{"id":615,"text":"Volcano Hazards Program","active":true,"usgs":true}],"links":[{"id":51197,"rank":300,"type":{"id":11,"text":"Document"},"url":"https://pubs.usgs.gov/of/1996/0070/report.pdf","text":"Report","size":"1.20 MB","linkFileType":{"id":1,"text":"pdf"},"description":"Report"},{"id":154487,"rank":0,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/of/1996/0070/report-thumb.jpg"}],"country":"United States","state":"Alaska","geographicExtents":"{\n \"type\": \"FeatureCollection\",\n \"features\": [\n {\n \"type\": \"Feature\",\n \"properties\": {},\n \"geometry\": {\n \"type\": \"Polygon\",\n \"coordinates\": [\n [\n [\n -154.13818359375,\n 59.20968817840924\n ],\n [\n -154.13818359375,\n 61.695081959115974\n ],\n [\n -152.7099609375,\n 61.695081959115974\n ],\n [\n -152.7099609375,\n 59.20968817840924\n ],\n [\n -154.13818359375,\n 59.20968817840924\n ]\n ]\n ]\n }\n }\n ]\n}","noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"4f4e49f3e4b07f02db5efb11","contributors":{"authors":[{"text":"Jolly, Arthur D.","contributorId":57913,"corporation":false,"usgs":true,"family":"Jolly","given":"Arthur","email":"","middleInitial":"D.","affiliations":[],"preferred":false,"id":185040,"contributorType":{"id":1,"text":"Authors"},"rank":1},{"text":"Power, John A. 0000-0002-7233-4398 jpower@usgs.gov","orcid":"https://orcid.org/0000-0002-7233-4398","contributorId":2768,"corporation":false,"usgs":true,"family":"Power","given":"John","email":"jpower@usgs.gov","middleInitial":"A.","affiliations":[],"preferred":true,"id":185035,"contributorType":{"id":1,"text":"Authors"},"rank":2},{"text":"Stihler, Scott D.","contributorId":31373,"corporation":false,"usgs":true,"family":"Stihler","given":"Scott","email":"","middleInitial":"D.","affiliations":[],"preferred":false,"id":185038,"contributorType":{"id":1,"text":"Authors"},"rank":3},{"text":"Rao, Lalitha N.","contributorId":174441,"corporation":false,"usgs":false,"family":"Rao","given":"Lalitha","email":"","middleInitial":"N.","affiliations":[{"id":13662,"text":"Geophysical Institute, University of Alaska, Fairbanks","active":true,"usgs":false}],"preferred":false,"id":185042,"contributorType":{"id":1,"text":"Authors"},"rank":4},{"text":"Davidson, Gail","contributorId":76344,"corporation":false,"usgs":true,"family":"Davidson","given":"Gail","email":"","affiliations":[],"preferred":false,"id":185041,"contributorType":{"id":1,"text":"Authors"},"rank":5},{"text":"Paskievitch, John F. jpaskie@usgs.gov","contributorId":3709,"corporation":false,"usgs":true,"family":"Paskievitch","given":"John","email":"jpaskie@usgs.gov","middleInitial":"F.","affiliations":[{"id":615,"text":"Volcano Hazards Program","active":true,"usgs":true}],"preferred":true,"id":185039,"contributorType":{"id":1,"text":"Authors"},"rank":6},{"text":"Estes, Steve","contributorId":55881,"corporation":false,"usgs":true,"family":"Estes","given":"Steve","email":"","affiliations":[],"preferred":false,"id":185037,"contributorType":{"id":1,"text":"Authors"},"rank":7},{"text":"Lahr, John C.","contributorId":20328,"corporation":false,"usgs":true,"family":"Lahr","given":"John","email":"","middleInitial":"C.","affiliations":[],"preferred":false,"id":185036,"contributorType":{"id":1,"text":"Authors"},"rank":8}]}} ,{"id":6872,"text":"fs24996 - 1996 - Causes of variations in water quality and aquatic ecology in rivers of the Upper Mississippi River Basin, Minnesota and Wisconsin","interactions":[],"lastModifiedDate":"2018-04-02T11:11:19","indexId":"fs24996","displayToPublicDate":"1997-10-01T00:00:00","publicationYear":"1996","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":"249-96","title":"Causes of variations in water quality and aquatic ecology in rivers of the Upper Mississippi River Basin, Minnesota and Wisconsin","docAbstract":"

Physical and aquatic biological conditions differ among the Mississippi River and its major tributaries (the St. Croix and Minnesota Rivers) in Minnesota and Wisconsin. The quality of surface water and the ecological condition of rivers affect the ways in which we use them. The St. Croix River is used for recreation; the Mississippi River is used for recreation and is a corridor for commerce; and the Minnesota River primarily drains agricultural lands. Analysis of the environmental framework of the basins and water-quality and ecological information by the National Water-Quality Assessment (NAWQA) Program shows that the conditions of the rivers are a product of a combination of factors including climate, hydrology, geology, soils, land use, land cover, water management, and water use.

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summary of selected trace element, nutrient, and pesticide data for bed sediments, 1969-90","interactions":[],"lastModifiedDate":"2021-10-21T21:23:42.956553","indexId":"wri964104","displayToPublicDate":"1997-10-01T00:00:00","publicationYear":"1996","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":"96-4104","title":"Water-quality assessment of the Albermarle-Pamlico drainage basin, North Carolina and Virginia— A summary of selected trace element, nutrient, and pesticide data for bed sediments, 1969-90","docAbstract":"Spatial distributions of metals and trace elements, nutrients, and pesticides and polychiorinated biphenyls (PCB's) in bed sediment were characterized using data collected from 1969 through 1990 and stored in the U.S. Geological Survey's National Water Data Storage and Retrieval (WATSTORE) system and the U.S. Environmental Protection Agency's Storage and Retrieval (STORET) system databases. Bed-sediment data from WATSTORE and STORET were combined to form a single database of 1,049 records representing 301 sites. Data were examined for concentrations of 16 metals and trace elements, 4 nutrients, 10 pesticides, and PCB's. Maximum bed-sediment concentrations were evaluated relative to sediment-quality guidelines developed by the National Oceanic and Atmospheric Administration, the Ontario Ministry of Environment and Energy, and the Virginia Department of Environmental Quality.\r\n\r\nSites were not selected randomly; therefore, results should not be interpreted as representing average conditions. Many sites were located in or around lakes and reservoirs, urban areas, and areas where special investigations were conducted. Lakes and reservoirs function as effective sediment traps, and elevated concentrations of some constituents occurred at these sites. High concentrations of many metals and trace elements also occurred near urban areas where streams receive runoff or inputs from industrial, residential, and municipal activities. Elevated nutrient concentrations occurred near lakes, reservoirs, and the mouths of major rivers.\r\n\r\nThe highest concentrations of arsenic, beryllium, chromium, iron. mercury, nickel, and selenium occurred in the Roanoke River Basin and may be a result of geologic formations or accumulations of bed sediment in lakes and reservoirs. The highest concentrations of cadmium, lead, and thallium were detected in the Chowan River Basin; copper and zinc were reported highest in the Neuse River Basin. Total phosphorus and total ammonia plus organic nitrogen concentrations exceeded the sediment evaluation guidelines in each major river basin, possibly resulting from wastewater inputs and agricultural applications. Exceedances of pesticide guidelines were detected in the upper Neuse River Basin near Falls Lake and in the lower Tar River Basin.","language":"English","publisher":"U.S. Geological Survey","doi":"10.3133/wri964104","usgsCitation":"Skrobialowski, S., 1996, Water-quality assessment of the Albermarle-Pamlico drainage basin, North Carolina and Virginia— A summary of selected trace element, nutrient, and pesticide data for bed sediments, 1969-90: U.S. Geological Survey Water-Resources Investigations Report 96-4104, vi, 33 p., https://doi.org/10.3133/wri964104.","productDescription":"vi, 33 p.","costCenters":[{"id":13634,"text":"South Atlantic Water Science Center","active":true,"usgs":true}],"links":[{"id":390790,"rank":3,"type":{"id":36,"text":"NGMDB Index Page"},"url":"https://ngmdb.usgs.gov/Prodesc/proddesc_48462.htm"},{"id":160078,"rank":0,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/wri/1996/4104/report-thumb.jpg"},{"id":58545,"rank":300,"type":{"id":11,"text":"Document"},"url":"https://pubs.usgs.gov/wri/1996/4104/report.pdf","linkFileType":{"id":1,"text":"pdf"}}],"country":"United States","state":"North Carolina, Virginia","otherGeospatial":"Albermarle-Pamlico drainage basin","geographicExtents":"{\n \"type\": \"FeatureCollection\",\n \"features\": [\n {\n \"type\": \"Feature\",\n \"properties\": {},\n \"geometry\": {\n \"type\": \"Polygon\",\n \"coordinates\": [\n [\n [\n -80.4833,\n 34.8667\n ],\n [\n -76,\n 34.8667\n ],\n [\n -76,\n 37.4667\n ],\n [\n -80.4833,\n 37.4667\n ],\n [\n -80.4833,\n 34.8667\n ]\n ]\n ]\n }\n }\n ]\n}","noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"4f4e49e5e4b07f02db5e6fc4","contributors":{"authors":[{"text":"Skrobialowski, S. 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The U.S. Geological Survey (USGS) is the Federal Government's primary source of data on the quantity and quality of the Nation's water resources, its principal civilian map making agency, and its primary provider of information on natural hazards and mineral, energy, and biological resources. The USGS makes unbiased scientific information available equally to all interested parties.

\n

Most USGS work in Texas involves the appraisal of the State's water resources in cooperation with more than 80 local, State, and Federal agencies. The foundation of a wide range of hydrologic data-collection and interpretive programs is the stream-gaging program. The Texas network of streamflow-gaging stations, which provides water data for water-resources planning and design, hydrologic research, and operation of water-resources projects, is part of a nationwide aggregation of networks that is unique because of nationally consistent, prescribed standards by which the data are collected and processed.

\n

The USGS continues to expand collection of data for paper and digital maps. The best-known products of the USGS in Texas are its 1:24,000-scale topographic maps. These maps depict basic natural and cultural features of the landscape. Maps at this scale (1 inch on the map represents 2,000 feet on the ground) are useful for civil engineering, land-use planning, and natural-resource monitoring, and have long been favorites with the general public for a wide variety of outdoor uses.

\n

The USGS also continues to monitor geologic conditions in Texas associated with rare but potentially dangerous earthquakes. Recently, the Nation Biological Service (now the Biological Resources Division) joined the USGS to continue their appraisal of the nation's biological resources.

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stratified drift and streamflow in the Deerfield River basin, northwestern Massachusetts","docAbstract":"This report presents the results of a study of the geohydrology of stratified drift and streamflow in the Deerfield River Basin, northwestern Massachusetts. Detailed hydrologic information is needed to plan for the optimal use of ground-water and surface-water resources and for development of new drinking-water supplies in the basin. Sources and percentage of water available for recharge on an annual basis from October 1993 to September 1994, to the fine-grained stratified-drift in a narrow valley bordered by upland till and bedrock were: (1) direct infiltration of precipitation on the valley (30 percent); (2) tributary loss from an upland brook as it crosses the valley (7 percent); and (3) ground- and surface-water runoff from the uplands (63 percent). Seventy percent of recharge was available from upland sources. Seasonal variation in recharge caused changes in ground-water levels and flow directions. In early spring, the direction of flow is toward the valley axis, but in late summer, the direction of flow is nearly parallel to the valley axis. Field observations and results of a ground-water flow simulation indicated that water available for recharge was greater than actual recharge during the spring snowmelt and during intense precipitation events. In 1994, estimates of water available for recharge were greater than actual recharge by 10 percent in March and by 60 percent in April; actual recharge to the valley on an annual basis from October 1993 to September 1994 was 20 percent less than original estimates. A map showing thickness of stratified drift in the Connecticut Valley Lowlands indicates a deep north-south trending buried valley. Maximum thickness of the stratified drift is 385 feet. Interpretation of a seismic-reflection survey indicates fine-grained stratified drift may be underlain by coarse-grained deposits ranging in thickness from 0 to 150 feet. Hydraulic properties of the stratified drift were calculated from ground-water-level fluctuations induced by river stage changes using a ground-water-flow model for a site adjacent to the Deerfield River. A comparison of measured and simulated heads resulted in a vertical riverbed hydraulic conductivity of 3 feet per day, anisotropic ratio of horizontal to vertical hydraulic conductivity of 40:1, and storage of 0.040 and 0.0002 for the unconfined and confined layers of the stratified drift. Hydraulic diffusivity (transmissivity divided by the unconfined storage) at the site is about 168,000 feet squared per day. Streamflows at times of low flow were determined for 27 sites that drain areas ranging from 0.57 to 15.8 percent stratified drift. Streamflows exceeded between 80 and 99 percent of the time were determined for sites on the unregulated tributaries to the Deerfield River. Streamflows per square mile of drainage area were greatest from sites at the downstream ends of the North River-Colrain and the Deerfield River-Charlemont stratified-drift valleys. Flow-duration curves for three continuous streamflow-gaging stations on the regulated Deerfield River were compared to flow-duration curves for three continuous streamflow-gaging stations on unregulated tributaries to show the effects of dam regulation on streamflow. Flow- duration curves constructed using instantaneous discharges for the three regulated gaging stations have flat sections that correspond to the predominant streamflows when water is being released from storage from the dams.","language":"ENGLISH","publisher":"U.S. Geological Survey ;\r\nBranch of Information Services [distributor],","doi":"10.3133/wri964115","usgsCitation":"Friesz, P., 1996, Geohydrology of stratified drift and streamflow in the Deerfield River basin, northwestern Massachusetts: U.S. Geological Survey Water-Resources Investigations Report 96-4115, v, 49 p. :ill., maps (some col.) ;28 cm., https://doi.org/10.3133/wri964115.","productDescription":"v, 49 p. :ill., maps (some col.) ;28 cm.","costCenters":[],"links":[{"id":123932,"rank":0,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/wri/1996/4115/report-thumb.jpg"},{"id":56074,"rank":400,"type":{"id":17,"text":"Plate"},"url":"https://pubs.usgs.gov/wri/1996/4115/plate-1.pdf","linkFileType":{"id":1,"text":"pdf"}},{"id":56075,"rank":300,"type":{"id":11,"text":"Document"},"url":"https://pubs.usgs.gov/wri/1996/4115/report.pdf","linkFileType":{"id":1,"text":"pdf"}}],"noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"4f4e4b1be4b07f02db6a8a24","contributors":{"authors":[{"text":"Friesz, P.J.","contributorId":41041,"corporation":false,"usgs":true,"family":"Friesz","given":"P.J.","email":"","affiliations":[],"preferred":false,"id":197726,"contributorType":{"id":1,"text":"Authors"},"rank":1}]}} ,{"id":5044,"text":"fs02796 - 1996 - U.S. Geological Survey programs in Missouri","interactions":[],"lastModifiedDate":"2012-02-02T00:05:42","indexId":"fs02796","displayToPublicDate":"1997-10-01T00:00:00","publicationYear":"1996","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":"027-96","title":"U.S. Geological Survey programs in Missouri","language":"ENGLISH","publisher":"The Survey,","doi":"10.3133/fs02796","usgsCitation":"Water Resources Division, U.S. Geological Survey, 1996, U.S. Geological Survey programs in Missouri: U.S. Geological Survey Fact Sheet 027-96, [4] p. : col. ill., maps ; 28 cm. col. ill., maps ;, https://doi.org/10.3133/fs02796.","productDescription":"[4] p. : col. ill., maps ; 28 cm. col. ill., maps ;","costCenters":[],"links":[{"id":118441,"rank":0,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/thumbnails/fs_027_96.bmp"},{"id":359,"rank":100,"type":{"id":15,"text":"Index Page"},"url":"https://pubs.usgs.gov/FS/FS-027-96","linkFileType":{"id":5,"text":"html"}}],"noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"4f4e4a2ae4b07f02db612307","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":528418,"contributorType":{"id":1,"text":"Authors"},"rank":1}]}} ,{"id":5049,"text":"fs03996 - 1996 - U.S. Geological Survey programs in Rhode Island","interactions":[],"lastModifiedDate":"2012-02-02T00:05:42","indexId":"fs03996","displayToPublicDate":"1997-10-01T00:00:00","publicationYear":"1996","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":"039-96","title":"U.S. Geological Survey programs in Rhode Island","language":"ENGLISH","publisher":"The Survey,","doi":"10.3133/fs03996","usgsCitation":"Water Resources Division, U.S. Geological Survey, 1996, U.S. Geological Survey programs in Rhode Island: U.S. Geological Survey Fact Sheet 039-96, [4] p. : ill. (some col.), maps ; 28 cm. ill. (some col.), maps ;, https://doi.org/10.3133/fs03996.","productDescription":"[4] p. : ill. (some col.), maps ; 28 cm. ill. (some col.), maps ;","costCenters":[],"links":[{"id":118445,"rank":0,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/thumbnails/fs_039_96.bmp"},{"id":364,"rank":100,"type":{"id":15,"text":"Index Page"},"url":"https://pubs.usgs.gov/FS/FS-039-96","linkFileType":{"id":5,"text":"html"}}],"noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"4f4e4a2ae4b07f02db612265","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":528423,"contributorType":{"id":1,"text":"Authors"},"rank":1}]}} ,{"id":23384,"text":"ofr96174 - 1996 - Simulation of ground-water flow in the Saginaw Aquifer, Clinton, Eaton, and Ingham counties, Michigan","interactions":[{"subject":{"id":23384,"text":"ofr96174 - 1996 - Simulation of ground-water flow in the Saginaw Aquifer, Clinton, Eaton, and Ingham counties, Michigan","indexId":"ofr96174","publicationYear":"1996","noYear":false,"title":"Simulation of ground-water flow in the Saginaw Aquifer, Clinton, Eaton, and Ingham counties, Michigan"},"predicate":"SUPERSEDED_BY","object":{"id":1907,"text":"wsp2480 - 1996 - Simulation of ground-water flow in the Saginaw Aquifer, Clinton, Eaton, and Ingham counties, Michigan","indexId":"wsp2480","publicationYear":"1996","noYear":false,"title":"Simulation of ground-water flow in the Saginaw Aquifer, Clinton, Eaton, and Ingham counties, Michigan"},"id":1}],"supersededBy":{"id":1907,"text":"wsp2480 - 1996 - Simulation of ground-water flow in the Saginaw Aquifer, Clinton, Eaton, and Ingham counties, Michigan","indexId":"wsp2480","publicationYear":"1996","noYear":false,"title":"Simulation of ground-water flow in the Saginaw Aquifer, Clinton, Eaton, and Ingham counties, Michigan"},"lastModifiedDate":"2012-02-02T00:08:12","indexId":"ofr96174","displayToPublicDate":"1997-10-01T00:00:00","publicationYear":"1996","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":"96-174","title":"Simulation of ground-water flow in the Saginaw Aquifer, Clinton, Eaton, and Ingham counties, Michigan","language":"ENGLISH","publisher":"U.S. Geological Survey ;\r\nEarth Science Information Center, Open-File Reports Section [distributor],","doi":"10.3133/ofr96174","issn":"0094-9140","usgsCitation":"Holtschlag, D., Luukkonen, C.L., and Nicholas, J., 1996, Simulation of ground-water flow in the Saginaw Aquifer, Clinton, Eaton, and Ingham counties, Michigan: U.S. Geological Survey Open-File Report 96-174, v, 49 p. :ill., maps ;28 cm., https://doi.org/10.3133/ofr96174.","productDescription":"v, 49 p. :ill., maps ;28 cm.","costCenters":[],"links":[{"id":156187,"rank":0,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/of/1996/0174/report-thumb.jpg"},{"id":52683,"rank":300,"type":{"id":11,"text":"Document"},"url":"https://pubs.usgs.gov/of/1996/0174/report.pdf","linkFileType":{"id":1,"text":"pdf"}}],"noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"4f4e49f8e4b07f02db5f281a","contributors":{"authors":[{"text":"Holtschlag, D. J. 0000-0001-5185-4928","orcid":"https://orcid.org/0000-0001-5185-4928","contributorId":102493,"corporation":false,"usgs":true,"family":"Holtschlag","given":"D. J.","affiliations":[],"preferred":false,"id":190014,"contributorType":{"id":1,"text":"Authors"},"rank":1},{"text":"Luukkonen, C. L.","contributorId":28962,"corporation":false,"usgs":true,"family":"Luukkonen","given":"C.","email":"","middleInitial":"L.","affiliations":[],"preferred":false,"id":190013,"contributorType":{"id":1,"text":"Authors"},"rank":2},{"text":"Nicholas, J.R.","contributorId":26673,"corporation":false,"usgs":true,"family":"Nicholas","given":"J.R.","email":"","affiliations":[],"preferred":false,"id":190012,"contributorType":{"id":1,"text":"Authors"},"rank":3}]}} ,{"id":26728,"text":"wri954223 - 1996 - Water resources of the Wind River Indian Reservation, Wyoming","interactions":[],"lastModifiedDate":"2012-02-02T00:08:30","indexId":"wri954223","displayToPublicDate":"1997-10-01T00:00:00","publicationYear":"1996","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":"95-4223","title":"Water resources of the Wind River Indian Reservation, Wyoming","docAbstract":"Existing data were used in conjunction with onsite measurements to evaluate the water resources on the Wind River Indian Reservation, Wyoming. The reservation is located mainly in the Wind River drainage basin. Ground water is used for public- supply, domestic, agricultural, and industrial purposes, and potentially for irrigation. Deposits of Quaternary age provide water for domestic and public-supply uses. Median well yields from different types of Quaternary deposits ranged from 6 to 20 gallons per minute. The Wind River Formation of Tertiary age is a major source of water for domestic and public-supply uses; well yields ranged from 0.1 to 350 gallons per minute. For the Tensleep Sandstone and Madison Limestone of Paleozoic age, wells might yield as much as 1,000 gallons per minute. The dissolved-solids concentration of water from the Little Wind River and Popo Agie River flood-plain alluvium near mountains was generally less than 400 mg/L (milligrams per liter), but with increasing distance from mountains, the range was about 600 to about 750 mg/L. Dissolved-solids concentrations of water in the Wind River Formation ranged from 211 to 5,110 mg/L. Streams provide most water used for irrigation. Discharge records from streamflow-gaging stations indicate flow characteristics of streams on the reservation are extremely variable. Average annual runoff was 122 to 1,150 acre-feet per square mile on perennial streams with gaging stations. Near the mountains, most perennial streams had dissolved-solids concentrations less than 200 mg/L, and with increasing distance from the mountains, concentrations were about 400 to 600 mg/L.","language":"ENGLISH","publisher":"U.S. Geological Survey ;\r\nEarth Science Information Center, Open-File Reports Section,[distributor],","doi":"10.3133/wri954223","usgsCitation":"Daddow, R.L., 1996, Water resources of the Wind River Indian Reservation, Wyoming: U.S. Geological Survey Water-Resources Investigations Report 95-4223, vii, 121 :ill., maps (some col.) ;28 cm., https://doi.org/10.3133/wri954223.","productDescription":"vii, 121 :ill., maps (some col.) ;28 cm.","costCenters":[],"links":[{"id":123675,"rank":0,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/wri/1995/4223/report-thumb.jpg"},{"id":55603,"rank":400,"type":{"id":17,"text":"Plate"},"url":"https://pubs.usgs.gov/wri/1995/4223/plate-1.pdf","linkFileType":{"id":1,"text":"pdf"}},{"id":55604,"rank":401,"type":{"id":17,"text":"Plate"},"url":"https://pubs.usgs.gov/wri/1995/4223/plate-2.pdf","linkFileType":{"id":1,"text":"pdf"}},{"id":55605,"rank":402,"type":{"id":17,"text":"Plate"},"url":"https://pubs.usgs.gov/wri/1995/4223/plate-3.pdf","linkFileType":{"id":1,"text":"pdf"}},{"id":55606,"rank":403,"type":{"id":17,"text":"Plate"},"url":"https://pubs.usgs.gov/wri/1995/4223/plate-4.pdf","linkFileType":{"id":1,"text":"pdf"}},{"id":55607,"rank":300,"type":{"id":11,"text":"Document"},"url":"https://pubs.usgs.gov/wri/1995/4223/report.pdf","linkFileType":{"id":1,"text":"pdf"}}],"noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"4f4e49e4e4b07f02db5e62c1","contributors":{"authors":[{"text":"Daddow, R. L.","contributorId":35748,"corporation":false,"usgs":true,"family":"Daddow","given":"R.","email":"","middleInitial":"L.","affiliations":[],"preferred":false,"id":196898,"contributorType":{"id":1,"text":"Authors"},"rank":1}]}} ,{"id":22040,"text":"ofr9613 - 1996 - Preliminary inventory of debris-flow and flooding effects of the June 27, 1995, storm in Madison County, Virginia showing time sequence of positions of storm-cell center","interactions":[],"lastModifiedDate":"2023-03-21T18:46:10.135444","indexId":"ofr9613","displayToPublicDate":"1997-10-01T00:00:00","publicationYear":"1996","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":"96-13","title":"Preliminary inventory of debris-flow and flooding effects of the June 27, 1995, storm in Madison County, Virginia showing time sequence of positions of storm-cell center","docAbstract":"

No abstract available.

","language":"English","publisher":"U.S. Geological Survey","doi":"10.3133/ofr9613","usgsCitation":"Wieczorek, G.F., Morgan, B., Campbell, R.H., Orndorff, R.C., Burton, W., Southworth, C., and Smith, J.A., 1996, Preliminary inventory of debris-flow and flooding effects of the June 27, 1995, storm in Madison County, Virginia showing time sequence of positions of storm-cell center: U.S. Geological Survey Open-File Report 96-13, Report: 8 p.; 1 Plate: 40.00 x 48.00 inches, https://doi.org/10.3133/ofr9613.","productDescription":"Report: 8 p.; 1 Plate: 40.00 x 48.00 inches","costCenters":[],"links":[{"id":414478,"rank":4,"type":{"id":36,"text":"NGMDB Index Page"},"url":"https://ngmdb.usgs.gov/Prodesc/proddesc_18566.htm","linkFileType":{"id":5,"text":"html"}},{"id":51501,"rank":2,"type":{"id":11,"text":"Document"},"url":"https://pubs.usgs.gov/of/1996/0013/report.pdf","linkFileType":{"id":1,"text":"pdf"}},{"id":153831,"rank":1,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/of/1996/0013/report-thumb.jpg"},{"id":19415,"rank":3,"type":{"id":17,"text":"Plate"},"url":"https://pubs.usgs.gov/of/1996/0013/plate-1.pdf","linkFileType":{"id":1,"text":"pdf"}}],"country":"United States","state":"Virginia","county":"Madison County","geographicExtents":"{\"type\":\"FeatureCollection\",\"features\":[{\"type\":\"Feature\",\"geometry\":{\"type\":\"Polygon\",\"coordinates\":[[[-78.2337,38.5357],[-78.1324,38.4472],[-78.1248,38.4435],[-78.1219,38.4402],[-78.1226,38.4357],[-78.128,38.4308],[-78.1268,38.4285],[-78.1193,38.4257],[-78.1171,38.4184],[-78.1071,38.4156],[-78.1025,38.4092],[-78.0968,38.4014],[-78.0964,38.3933],[-78.0994,38.3897],[-78.1083,38.3857],[-78.1142,38.3808],[-78.1185,38.3709],[-78.1187,38.3632],[-78.1158,38.3586],[-78.113,38.3558],[-78.1101,38.3535],[-78.1096,38.3485],[-78.1078,38.3463],[-78.1037,38.3462],[-78.1002,38.3457],[-78.095,38.3425],[-78.0905,38.3347],[-78.0905,38.3316],[-78.0982,38.328],[-78.1031,38.3208],[-78.1078,38.3177],[-78.1067,38.3154],[-78.102,38.314],[-78.0967,38.3139],[-78.0992,38.3058],[-78.1081,38.2991],[-78.1118,38.2942],[-78.123,38.2898],[-78.1261,38.2826],[-78.1302,38.2817],[-78.1342,38.2836],[-78.1407,38.2836],[-78.1443,38.28],[-78.1466,38.2796],[-78.1524,38.2847],[-78.1565,38.2838],[-78.1589,38.282],[-78.1602,38.277],[-78.1585,38.2716],[-78.1591,38.2684],[-78.1662,38.2699],[-78.1697,38.2694],[-78.1732,38.269],[-78.1796,38.2695],[-78.1826,38.2668],[-78.1821,38.2646],[-78.1816,38.2596],[-78.1893,38.2529],[-78.1929,38.247],[-78.1959,38.2457],[-78.2071,38.2426],[-78.2112,38.2427],[-78.2171,38.2418],[-78.2201,38.2342],[-78.2237,38.2319],[-78.2296,38.2315],[-78.2348,38.2339],[-78.2365,38.2339],[-78.2494,38.234],[-78.2511,38.2363],[-78.2564,38.2386],[-78.2598,38.2418],[-78.2662,38.2482],[-78.2696,38.2519],[-78.2684,38.2564],[-78.2671,38.2605],[-78.2729,38.2655],[-78.2782,38.2678],[-78.2834,38.2702],[-78.2875,38.2711],[-78.2892,38.2716],[-78.2933,38.2748],[-78.2985,38.2753],[-78.3015,38.2735],[-78.3045,38.2699],[-78.3127,38.2718],[-78.3168,38.27],[-78.3302,38.2733],[-78.336,38.2797],[-78.3424,38.2821],[-78.346,38.2771],[-78.3489,38.278],[-78.3489,38.2789],[-78.3488,38.2885],[-78.354,38.2899],[-78.3587,38.2922],[-78.3622,38.2949],[-78.3639,38.2977],[-78.3621,38.3008],[-78.3579,38.3022],[-78.3631,38.3117],[-78.363,38.3167],[-78.3636,38.3176],[-78.37,38.3168],[-78.3771,38.3182],[-78.384,38.3246],[-78.3927,38.3292],[-78.3962,38.3342],[-78.4055,38.3388],[-78.4118,38.3516],[-78.4187,38.3589],[-78.428,38.3635],[-78.4286,38.3662],[-78.423,38.3834],[-78.4235,38.388],[-78.427,38.3912],[-78.434,38.3944],[-78.4369,38.3989],[-78.4379,38.4085],[-78.436,38.4171],[-78.433,38.4257],[-78.4356,38.4438],[-78.4343,38.4524],[-78.4355,38.4565],[-78.4448,38.4625],[-78.4465,38.4652],[-78.4504,38.4806],[-78.4461,38.491],[-78.4414,38.4964],[-78.4428,38.5155],[-78.4374,38.5218],[-78.4409,38.5273],[-78.4397,38.53],[-78.4267,38.5326],[-78.4202,38.537],[-78.4111,38.5506],[-78.4046,38.5555],[-78.3857,38.5607],[-78.3803,38.5643],[-78.3809,38.5675],[-78.3849,38.5725],[-78.3872,38.5784],[-78.3871,38.5843],[-78.3817,38.5911],[-78.3692,38.6005],[-78.3619,38.6113],[-78.3518,38.618],[-78.3453,38.622],[-78.3423,38.6261],[-78.3393,38.6279],[-78.3283,38.6182],[-78.2888,38.5839],[-78.2337,38.5357]]]},\"properties\":{\"name\":\"Madison\",\"state\":\"VA\"}}]}","noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"4f4e4abce4b07f02db673227","contributors":{"authors":[{"text":"Wieczorek, G. F.","contributorId":50143,"corporation":false,"usgs":true,"family":"Wieczorek","given":"G.","middleInitial":"F.","affiliations":[],"preferred":false,"id":186807,"contributorType":{"id":1,"text":"Authors"},"rank":1},{"text":"Morgan, B. A.","contributorId":87128,"corporation":false,"usgs":true,"family":"Morgan","given":"B. A.","affiliations":[],"preferred":false,"id":186810,"contributorType":{"id":1,"text":"Authors"},"rank":2},{"text":"Campbell, R. H.","contributorId":52160,"corporation":false,"usgs":true,"family":"Campbell","given":"R.","email":"","middleInitial":"H.","affiliations":[],"preferred":false,"id":186809,"contributorType":{"id":1,"text":"Authors"},"rank":3},{"text":"Orndorff, R. C.","contributorId":17613,"corporation":false,"usgs":true,"family":"Orndorff","given":"R.","email":"","middleInitial":"C.","affiliations":[],"preferred":false,"id":186805,"contributorType":{"id":1,"text":"Authors"},"rank":4},{"text":"Burton, W.C.","contributorId":41439,"corporation":false,"usgs":true,"family":"Burton","given":"W.C.","email":"","affiliations":[],"preferred":false,"id":186806,"contributorType":{"id":1,"text":"Authors"},"rank":5},{"text":"Southworth, C.S.","contributorId":51272,"corporation":false,"usgs":true,"family":"Southworth","given":"C.S.","email":"","affiliations":[],"preferred":false,"id":186808,"contributorType":{"id":1,"text":"Authors"},"rank":6},{"text":"Smith, J. A.","contributorId":101646,"corporation":false,"usgs":true,"family":"Smith","given":"J.","email":"","middleInitial":"A.","affiliations":[],"preferred":false,"id":186811,"contributorType":{"id":1,"text":"Authors"},"rank":7}]}} ,{"id":23264,"text":"ofr9656 - 1996 - Remote video monitoring systems","interactions":[],"lastModifiedDate":"2012-02-02T00:08:03","indexId":"ofr9656","displayToPublicDate":"1997-10-01T00:00:00","publicationYear":"1996","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":"96-56","title":"Remote video monitoring systems","language":"ENGLISH","publisher":"U.S. Geological Survey,","doi":"10.3133/ofr9656","issn":"0094-9140","usgsCitation":"Haines, J.W., and Townsley, B., 1996, Remote video monitoring systems: U.S. Geological Survey Open-File Report 96-56, iii, 32 p. :ill. ;28 cm., https://doi.org/10.3133/ofr9656.","productDescription":"iii, 32 p. :ill. ;28 cm.","costCenters":[],"links":[{"id":156032,"rank":0,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/of/1996/0056/report-thumb.jpg"},{"id":52550,"rank":300,"type":{"id":11,"text":"Document"},"url":"https://pubs.usgs.gov/of/1996/0056/report.pdf","linkFileType":{"id":1,"text":"pdf"}}],"noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"4f4e4ac8e4b07f02db67bf29","contributors":{"authors":[{"text":"Haines, J. W.","contributorId":26319,"corporation":false,"usgs":true,"family":"Haines","given":"J.","email":"","middleInitial":"W.","affiliations":[],"preferred":false,"id":189769,"contributorType":{"id":1,"text":"Authors"},"rank":1},{"text":"Townsley, Bill","contributorId":63422,"corporation":false,"usgs":true,"family":"Townsley","given":"Bill","email":"","affiliations":[],"preferred":false,"id":189770,"contributorType":{"id":1,"text":"Authors"},"rank":2}]}} ,{"id":27580,"text":"wri964196 - 1996 - Pesticides in surface water from three agricultural basins in south-central Georgia, 1993-97","interactions":[],"lastModifiedDate":"2017-01-27T13:41:03","indexId":"wri964196","displayToPublicDate":"1997-10-01T00:00:00","publicationYear":"1996","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":"96-4196","title":"Pesticides in surface water from three agricultural basins in south-central Georgia, 1993-97","docAbstract":"Twenty-two of 43 pesticides analyzed were detected in 128 water samples collected from Tucsawhatchee Creek, the Little River, and the Withlacoochee River. These streams drain agricultural basins in south-central Georgia and were sampled from March 1993 through June 1995. Herbicides were detected more frequently than insecticides. The most frequently detected herbicides were atrazineand metolachlor and the most frequently detected insecticide was carbaryl. Pesticide concentrations in the three streams were low and did not exceed U.S. Environmental Protection Agency drinking water standards. The maximum pesticide concentration was 2.6 ug/L (micrograms per liter) for propargite, a miticide detected in only one sample. The maximum concentrations of the remaining 21 pesticides were less than 0.25 ug/L. The median concentrations were equal to the method detection limit for all pesticides except atrazine (0.008 ug/L) and metolachlor (0.012 ug/L). The ratio of herbicidedetections to nondetections was largest in the planting season, smaller in the harvest season and smallest in the fallow season for the three basins.The same pattern existed for the insecticide ratios in the Little River and the Withlacoochee River. Pairwise correlations between concentrations of atrazine and metolachlor and four parameters (discharge, and concentrations of dissolved organiccarbon, suspended organic carbon, and suspended fine sediment) were evaluated for each stream. The strongest correlations existed between metolachlor and mean daily discharge and metolachlor and fine sediment in the Withlacoochee River. The only significant correlation for the Little River was between atrazine and suspended fine sediment.","language":"ENGLISH","publisher":"U.S. Geological Survey,","doi":"10.3133/wri964196","usgsCitation":"Hatzell, H.H., 1996, Pesticides in surface water from three agricultural basins in south-central Georgia, 1993-97: U.S. Geological Survey Water-Resources Investigations Report 96-4196, 12 p. :ill. (some col.), maps (some col.) ;28 cm., https://doi.org/10.3133/wri964196.","productDescription":"12 p. :ill. 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This report provides low-flow characteristics for 216 continuous-record gaging stations using frequency analysis techniques. Included are low-flow frequency characteristics for 143 unregulated, gaging stations; and sample percentiles for 32 stations that were subject to regulation or diversion, and sample percentiles for 41 stations, regulated and unregulated, that exhibited significant trends in the annual low-flow time series. Estimates of low-flow frequency characteristics are provided for 242 partial-record stations and miscellaneous sites based on correlations with daily mean discharges at continuous-record stations. Low-flow measurement data are available at approximately 1,300 continuous-record gaging stations, partial- record stations and miscellaneous sites. Historic low-flow measurement data are accessible through the U.S. Geological Survey Automatic Data Processing System.","language":"English","publisher":"U.S. Geological Survey","doi":"10.3133/wri934165","collaboration":"Prepared in cooperation with the Florida Department of Environmental Regulation","usgsCitation":"Rumenik, R.P., and Grubbs, J.W., 1996, Low-flow characteristics of Florida streams: U.S. Geological Survey Water-Resources Investigations Report 93-4165, Report: vi, 220 p.; 2 Plates: 32.50 x 35.79 inches and 32.50 x 32.76 inches, https://doi.org/10.3133/wri934165.","productDescription":"Report: vi, 220 p.; 2 Plates: 32.50 x 35.79 inches and 32.50 x 32.76 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