The drilling and logging activity described in this report was undertaken in July 1981, as part of the Energy Lands program of the U.S. Geological Survey. The general objectives of the project of which this work is a part are to provide an understanding of the nature, location, and extent of the engineering geology and environmental geology concerns in areas of potential coal development in the Cook Inlet region, Alaska. The lithologic, geotechnical, and geophysical data presented in this report include some of the data needed to evaluate geologic hazards, and to predict the response of geologic materials to large-scale coal mining and related development in the Chuitna West coal field of the Beluga coal resource area. Specifically, the information may be used in evaluation of natural- and cut-slope stability, spoil-pile stability, ground response to seismic activity, blasting effects, excavatability, ground-water conditions, and erosion potential.
The drill site (fig. 1, point C), located on the edge of a small, gently sloping basin draining northwestward into the Chuitna River, is approximately 90 km, (55 mi) west of Anchorage, Alaska, and 29 km (18 mi) northwest of Tyonek, a native village on the northwest side of Cook Inlet.
No abstract available.
","language":"English","publisher":"U.S. Geological Survey","doi":"10.3133/i1313D","usgsCitation":"Posner, A., and Zenone, C., 1983, Chemical quality of ground water in the Culpeper Basin, Virginia and Maryland: U.S. Geological Survey IMAP 1313, 1 Plate: 33.00 x 47.71 inches, https://doi.org/10.3133/i1313D.","productDescription":"1 Plate: 33.00 x 47.71 inches","costCenters":[],"links":[{"id":493434,"rank":4,"type":{"id":36,"text":"NGMDB Index Page"},"url":"https://ngmdb.usgs.gov/Prodesc/proddesc_9142.htm","linkFileType":{"id":5,"text":"html"}},{"id":256116,"rank":3,"type":{"id":17,"text":"Plate"},"url":"https://pubs.usgs.gov/imap/1313d/plate-1.pdf","linkFileType":{"id":1,"text":"pdf"}},{"id":256117,"rank":2,"type":{"id":11,"text":"Document"},"url":"https://pubs.usgs.gov/imap/1313d/report.pdf","linkFileType":{"id":1,"text":"pdf"}},{"id":256118,"rank":1,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/imap/1313d/report-thumb.jpg"}],"scale":"125000","state":"Maryland, Virginia","otherGeospatial":"Culpeper Basin","geographicExtents":"{\n \"type\": \"FeatureCollection\",\n \"features\": [\n {\n \"type\": \"Feature\",\n \"properties\": {},\n \"geometry\": {\n \"coordinates\": [\n [\n [\n -78.28,\n 39.489\n ],\n [\n -78.28,\n 38.205\n ],\n [\n -77.218,\n 38.205\n ],\n [\n -77.218,\n 39.489\n ],\n [\n -78.28,\n 39.489\n ]\n ]\n ],\n \"type\": \"Polygon\"\n }\n }\n ]\n}","noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"4f4e49dfe4b07f02db5e3bd3","contributors":{"authors":[{"text":"Posner, Alex","contributorId":18376,"corporation":false,"usgs":true,"family":"Posner","given":"Alex","email":"","affiliations":[],"preferred":false,"id":275189,"contributorType":{"id":1,"text":"Authors"},"rank":1},{"text":"Zenone, Chester","contributorId":8094,"corporation":false,"usgs":true,"family":"Zenone","given":"Chester","email":"","affiliations":[],"preferred":false,"id":275188,"contributorType":{"id":1,"text":"Authors"},"rank":2}]}} ,{"id":64778,"text":"i1406 - 1983 - Geologic map, tectonic map and structure sections of the Muddy and northern Black Mountains, Clark County, Nevada","interactions":[{"subject":{"id":43587,"text":"ofr81796 - 1981 - Geologic map, tectonic map, and structure sections of the Muddy and northern Black Mountains, Clark County, Nevada","indexId":"ofr81796","publicationYear":"1981","noYear":false,"title":"Geologic map, tectonic map, and structure sections of the Muddy and northern Black Mountains, Clark County, Nevada"},"predicate":"SUPERSEDED_BY","object":{"id":64778,"text":"i1406 - 1983 - Geologic map, tectonic map and structure sections of the Muddy and northern Black Mountains, Clark County, Nevada","indexId":"i1406","publicationYear":"1983","noYear":false,"title":"Geologic map, tectonic map and structure sections of the Muddy and northern Black Mountains, Clark County, Nevada"},"id":1}],"lastModifiedDate":"2012-02-10T00:10:52","indexId":"i1406","displayToPublicDate":"1994-01-01T00:00:00","publicationYear":"1983","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":"1406","subseriesTitle":"NONE","title":"Geologic map, tectonic map and structure sections of the Muddy and northern Black Mountains, Clark County, Nevada","language":"ENGLISH","doi":"10.3133/i1406","usgsCitation":"Bohannon, 1983, Geologic map, tectonic map and structure sections of the Muddy and northern Black Mountains, Clark County, Nevada: U.S. Geological Survey IMAP 1406, 2 maps and 4 structure sections on 2 sheets :col. ;sheets 94 x 140 cm., 81 x 112 cm., folded in envelope 30 x 24 cm., https://doi.org/10.3133/i1406.","productDescription":"2 maps and 4 structure sections on 2 sheets :col. ;sheets 94 x 140 cm., 81 x 112 cm., folded in envelope 30 x 24 cm.","costCenters":[],"links":[{"id":106716,"rank":700,"type":{"id":15,"text":"Index Page"},"url":"https://ngmdb.usgs.gov/Prodesc/proddesc_9189.htm","linkFileType":{"id":5,"text":"html"},"description":"9189"},{"id":186947,"rank":0,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/thumbnails/usgs_thumb.jpg"}],"scale":"62500","geographicExtents":"{ \"type\": \"FeatureCollection\", \"features\": [ { \"type\": \"Feature\", \"properties\": {}, \"geometry\": { \"type\": \"Polygon\", \"coordinates\": [ [ [ -114.41666666666667,36.166666666666664 ], [ -114.41666666666667,36.5 ], [ -114.41666666666667,36.5 ], [ -114.41666666666667,36.166666666666664 ], [ -114.41666666666667,36.166666666666664 ] ] ] } } ] }","noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"4f4e4ae1e4b07f02db68867d","contributors":{"authors":[{"text":"Bohannon","contributorId":127969,"corporation":true,"usgs":false,"organization":"Bohannon","id":533641,"contributorType":{"id":1,"text":"Authors"},"rank":1}]}} ,{"id":29423,"text":"wri824022 - 1983 - Quality of ground water in southern Buchanan County, Virginia","interactions":[],"lastModifiedDate":"2012-02-02T00:08:57","indexId":"wri824022","displayToPublicDate":"1994-01-01T00:00:00","publicationYear":"1983","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":"82-4022","title":"Quality of ground water in southern Buchanan County, Virginia","docAbstract":"In seven small contiguous stream basins in the coal area of southwest Virginia, ground water is predominantly bicarbonate in anion composition, with calcium as the major cation in the ridges and sodium the major cation in the lower altitudes. Sulfate is the major anion in water associated with coal seams and in stream waters draining areas extensively disturbed by mining activities. Water found along a major linear feature in the Big Prater Creek valley and water from deep wells in Levisa Fork basin contain chloride as the predominant anion. Hydrogen ion activities (pH) in the ground water range from 5.2 to 8.4. Iron concentrations as high as 14,000 micrograms per liter are present in domestic wells. The chemical composition of most streams changes with diminishing discharge and at baseflow is similar to the composition of local ground water. At high flows, streams draining mined areas are enriched with sulfate. (USGS)","language":"ENGLISH","publisher":"U.S. Geological Survey,","doi":"10.3133/wri824022","usgsCitation":"Rogers, S.M., and Powell, J.D., 1983, Quality of ground water in southern Buchanan County, Virginia: U.S. Geological Survey Water-Resources Investigations Report 82-4022, vi, 32 p. :ill., maps.; 12 over-size sheets, scale 1:48,000, https://doi.org/10.3133/wri824022.","productDescription":"vi, 32 p. :ill., maps.; 12 over-size sheets, scale 1:48,000","costCenters":[],"links":[{"id":159705,"rank":0,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/wri/1982/4022/report-thumb.jpg"},{"id":58269,"rank":400,"type":{"id":17,"text":"Plate"},"url":"https://pubs.usgs.gov/wri/1982/4022/plate-1.pdf","linkFileType":{"id":1,"text":"pdf"}},{"id":58270,"rank":300,"type":{"id":11,"text":"Document"},"url":"https://pubs.usgs.gov/wri/1982/4022/report.pdf","linkFileType":{"id":1,"text":"pdf"}}],"scale":"48000","noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"4f4e4a8fe4b07f02db654b0a","contributors":{"authors":[{"text":"Rogers, Stanley M.","contributorId":37761,"corporation":false,"usgs":true,"family":"Rogers","given":"Stanley","email":"","middleInitial":"M.","affiliations":[],"preferred":false,"id":201505,"contributorType":{"id":1,"text":"Authors"},"rank":1},{"text":"Powell, John D.","contributorId":6045,"corporation":false,"usgs":true,"family":"Powell","given":"John","email":"","middleInitial":"D.","affiliations":[],"preferred":false,"id":201504,"contributorType":{"id":1,"text":"Authors"},"rank":2}]}} ,{"id":7073,"text":"ofr83261 - 1983 - Cost-effectiveness of the stream-gaging program in Maine","interactions":[{"subject":{"id":7073,"text":"ofr83261 - 1983 - Cost-effectiveness of the stream-gaging program in Maine","indexId":"ofr83261","publicationYear":"1983","noYear":false,"title":"Cost-effectiveness of the stream-gaging program in Maine"},"predicate":"SUPERSEDED_BY","object":{"id":32,"text":"wsp2244 - 1984 - Cost effectiveness of the stream-gaging program in Maine; A prototype for nationwide implementation","indexId":"wsp2244","publicationYear":"1984","noYear":false,"title":"Cost effectiveness of the stream-gaging program in Maine; A prototype for nationwide implementation"},"id":1}],"supersededBy":{"id":32,"text":"wsp2244 - 1984 - Cost effectiveness of the stream-gaging program in Maine; A prototype for nationwide implementation","indexId":"wsp2244","publicationYear":"1984","noYear":false,"title":"Cost effectiveness of the stream-gaging program in Maine; A prototype for nationwide implementation"},"lastModifiedDate":"2019-11-07T12:18:47","indexId":"ofr83261","displayToPublicDate":"1994-01-01T00:00:00","publicationYear":"1983","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":"83-261","title":"Cost-effectiveness of the stream-gaging program in Maine","docAbstract":"Data uses and funding sources were identified for the 51 continuous stream gages currently being operated in Maine. Three stream-gages were identified as having insufficient reason to continue their operation. Operation of these stations were identified as having uses specific only to short-term studies; it is recommended that these stations be discontinued at the end of the data-collection phases of the studies. The remaining 45 stations should be maintained in the program for the foreseeable future. The current policy for operation of the 45-station program would require $180,300 per year. The average standard error of estimation of streamflow record is 18.5 percent. It was shown that this overall level of accuracy at the 45 sites could be maintained with a budget of \\$170,000 if the gaging resources were redistributed among the gages. A minimum budget of \\$155,000 is required to operate the 45-gage program; a budget less than this does not permit proper service and maintenance of the gages and recorders. At the minimum budget, the average standard error is 26.0 percent. The maximum budget analyzed was \\$350,000, which resulted in an average standard error of 9.2 percent. Large parts of Maine 's interior were identified as having sparse stream-flow data. It was recommended that this sparsity should be remedied as funds can be made available. (USGS)
","language":"English","publisher":"U.S. Geological Survey","publisherLocation":"Reston, VA","doi":"10.3133/ofr83261","usgsCitation":"Fontaine, R.A., Moss, M.E., Smath, J., and Thomas, W.O., 1983, Cost-effectiveness of the stream-gaging program in Maine: U.S. Geological Survey Open-File Report 83-261, v, 81 p. , https://doi.org/10.3133/ofr83261.","productDescription":"v, 81 p. ","costCenters":[],"links":[{"id":369041,"rank":2,"type":{"id":11,"text":"Document"},"url":"https://pubs.usgs.gov/of/1983/0261/report.pdf","linkFileType":{"id":1,"text":"pdf"}},{"id":140167,"rank":0,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/of/1983/0261/report-thumb.jpg"}],"country":"United States","state":"Maine","geographicExtents":"{\n \"type\": \"FeatureCollection\",\n \"features\": [\n {\n \"type\": \"Feature\",\n \"properties\": {},\n \"geometry\": {\n \"type\": \"Polygon\",\n \"coordinates\": [\n [\n [\n -71.2353515625,\n 42.956422511073335\n ],\n [\n -66.95068359374999,\n 42.956422511073335\n ],\n [\n -66.95068359374999,\n 47.65058757118734\n ],\n [\n -71.2353515625,\n 47.65058757118734\n ],\n [\n -71.2353515625,\n 42.956422511073335\n ]\n ]\n ]\n }\n }\n ]\n}","noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"4f4e4a80e4b07f02db649314","contributors":{"authors":[{"text":"Fontaine, Richard A. rfontain@usgs.gov","contributorId":2379,"corporation":false,"usgs":true,"family":"Fontaine","given":"Richard","email":"rfontain@usgs.gov","middleInitial":"A.","affiliations":[],"preferred":true,"id":154179,"contributorType":{"id":1,"text":"Authors"},"rank":1},{"text":"Moss, M. E.","contributorId":50500,"corporation":false,"usgs":true,"family":"Moss","given":"M.","email":"","middleInitial":"E.","affiliations":[],"preferred":false,"id":154181,"contributorType":{"id":1,"text":"Authors"},"rank":2},{"text":"Smath, J.A.","contributorId":15174,"corporation":false,"usgs":true,"family":"Smath","given":"J.A.","email":"","affiliations":[],"preferred":false,"id":154180,"contributorType":{"id":1,"text":"Authors"},"rank":3},{"text":"Thomas, W. O.","contributorId":101246,"corporation":false,"usgs":true,"family":"Thomas","given":"W.","email":"","middleInitial":"O.","affiliations":[],"preferred":false,"id":154182,"contributorType":{"id":1,"text":"Authors"},"rank":4}]}} ,{"id":29520,"text":"wri834074 - 1983 - Effects of ground-water development in the North Fort Hood area, Coryell County, Texas","interactions":[],"lastModifiedDate":"2016-08-09T13:48:15","indexId":"wri834074","displayToPublicDate":"1994-01-01T00:00:00","publicationYear":"1983","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":"83-4074","title":"Effects of ground-water development in the North Fort Hood area, Coryell County, Texas","docAbstract":"The U.S. Army Corps of Engineers is studying the adequacy of the existing ground-water supplies of North Fort Hood, located in Coryell County in central Texas and an important part of the U.S. Army's Fort Hood Military Reservation. The U.S. Geological Survey was requested to compile the available ground-water data, collect additional data, and assess the effects of the long-term development of ground water in the North Fort Hood area.
\nNearly all ground water in the North Fort Hood area is withdrawn from the Hensell and Hosston Members of the Travis Peak Formation. The total average annual rates of ground-water withdrawals, mostly for public supply, has steadily increased from nearly 0.5 million gallons per day during 1955 to mare than 1.5 million gallons per day during 1980.
\nThe principal effect of the long-term development of ground water in the area has been a large decline of water levels in wells. The water level in a well near Narth Fort Hood declined from a depth of 100 feet during 1943 to nearly 480 feet during 1982. The water level in a well at Gatesville was above ground level during 1898. A nearby well had a water level of 476 feet below land surface during 1982. The long-term average of water-level declines for wells in the area ranges from 8 to more than 9 feet per year.
\nThe historical confined (artesian) conditions of the principal aquifer have changed to water-table conditions in some areas as the artesian head 9 drops below the base of the confining layer due to pumping. The greater storage property of the unconfined system will decrease the rate of water-level declines. However, well yields will continue to decrease in relation to the general decline of hydraulic head in the aquifer.
\nThe ground water in the area is slightly saline and concentrations of some constituents generally exceed chemical-quality limits set by the U.S. Environmental Protection Agency for public water supplies. Hie historical chemical changes in the ground water generally are insignificant and appear unrelated to the large declines of water levels in wells of the area.
","language":"English","publisher":"U.S. Geological Survey","publisherLocation":"Austin, TX","doi":"10.3133/wri834074","usgsCitation":"Sandeen, W., 1983, Effects of ground-water development in the North Fort Hood area, Coryell County, Texas: U.S. Geological Survey Water-Resources Investigations Report 83-4074, Report: v, 48 p.; 2 Plates: 12.16 x 16.33 inches and 11.85 x 16.58 inches, https://doi.org/10.3133/wri834074.","productDescription":"Report: v, 48 p.; 2 Plates: 12.16 x 16.33 inches and 11.85 x 16.58 inches","numberOfPages":"53","onlineOnly":"N","additionalOnlineFiles":"N","costCenters":[{"id":583,"text":"Texas Water Science Center","active":true,"usgs":true}],"links":[{"id":110159,"rank":700,"type":{"id":15,"text":"Index Page"},"url":"https://ngmdb.usgs.gov/Prodesc/proddesc_35705.htm","linkFileType":{"id":5,"text":"html"},"description":"35705"},{"id":58358,"rank":400,"type":{"id":17,"text":"Plate"},"url":"https://pubs.usgs.gov/wri/1983/4074/plate-1.pdf","linkFileType":{"id":1,"text":"pdf"}},{"id":58359,"rank":401,"type":{"id":17,"text":"Plate"},"url":"https://pubs.usgs.gov/wri/1983/4074/plate-2.pdf","linkFileType":{"id":1,"text":"pdf"}},{"id":58360,"rank":300,"type":{"id":11,"text":"Document"},"url":"https://pubs.usgs.gov/wri/1983/4074/report.pdf","linkFileType":{"id":1,"text":"pdf"}},{"id":119416,"rank":0,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/wri/1983/4074/report-thumb.jpg"}],"country":"United States","state":"Texas","county":"Coryell County","noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"4f4e4a2ee4b07f02db615317","contributors":{"authors":[{"text":"Sandeen, W.M.","contributorId":102488,"corporation":false,"usgs":true,"family":"Sandeen","given":"W.M.","affiliations":[],"preferred":false,"id":201656,"contributorType":{"id":1,"text":"Authors"},"rank":1}]}} ,{"id":7836,"text":"ofr83144 - 1983 - Instrumentation used for hydraulic testing of potential water-bearing formations at the Waste Isolation Pilot Plant site in southeastern New Mexico","interactions":[],"lastModifiedDate":"2012-02-02T00:06:03","indexId":"ofr83144","displayToPublicDate":"1994-01-01T00:00:00","publicationYear":"1983","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":"83-144","title":"Instrumentation used for hydraulic testing of potential water-bearing formations at the Waste Isolation Pilot Plant site in southeastern New Mexico","docAbstract":"Requirements for testing hydrologic test wells at the proposed Waste Isolation Pilot Plant near Carlsbad, New Mexico, necessitated the use of inflatable formation packers and pressure transducers. Observations during drilling and initial development indicated small formation yields which would require considerable test times by conventional open-casing methods. A pressure-monitoring system was assembled for performance evaluation utilizing commercially available components. Formation pressures were monitored with a down-hole strain-gage transducer. An inflatable packer equipped with a 1/4-inch-diameter steel tube extending through the inflation element permitted sensing formation pressures in isolated test zones. Surface components of the monitoring system provided AC transducer excitation, signal conditioning for recording directly in engineering units, and both analog and digital recording. Continuous surface monitoring of formation pressures provided a means of determining test status and projecting completion times during any phase of testing. Maximum portability was afforded by battery operation with all surface components mounted in a small self-contained trailer. (USGS)","language":"ENGLISH","publisher":"U.S. Geological Survey,","doi":"10.3133/ofr83144","usgsCitation":"Basler, J., 1983, Instrumentation used for hydraulic testing of potential water-bearing formations at the Waste Isolation Pilot Plant site in southeastern New Mexico: U.S. Geological Survey Open-File Report 83-144, v, 34 p. ill. ;28 cm., https://doi.org/10.3133/ofr83144.","productDescription":"v, 34 p. ill. ;28 cm.","costCenters":[],"links":[{"id":140535,"rank":0,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/of/1983/0144/report-thumb.jpg"},{"id":35350,"rank":300,"type":{"id":11,"text":"Document"},"url":"https://pubs.usgs.gov/of/1983/0144/report.pdf","linkFileType":{"id":1,"text":"pdf"}}],"noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"4f4e49dce4b07f02db5e1c9d","contributors":{"authors":[{"text":"Basler, J.A.","contributorId":85171,"corporation":false,"usgs":true,"family":"Basler","given":"J.A.","email":"","affiliations":[],"preferred":false,"id":156700,"contributorType":{"id":1,"text":"Authors"},"rank":1}]}} ,{"id":7071,"text":"ofr83343 - 1983 - Contour maps, statistical summaries, and analytical data from stream-sediment samples collected from the Glacier Peak study area and analyzed using an aqua-regia leach/inductively coupled plasma method","interactions":[],"lastModifiedDate":"2021-09-21T20:44:32.945046","indexId":"ofr83343","displayToPublicDate":"1994-01-01T00:00:00","publicationYear":"1983","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":"83-343","title":"Contour maps, statistical summaries, and analytical data from stream-sediment samples collected from the Glacier Peak study area and analyzed using an aqua-regia leach/inductively coupled plasma method","docAbstract":"No abstract available.
","language":"English","publisher":"U.S. Geological Survey,","doi":"10.3133/ofr83343","usgsCitation":"Church, S.E., Motooka, J.M., Werschky, R.S., Bigelow, R.C., and Van Trump, G., 1983, Contour maps, statistical summaries, and analytical data from stream-sediment samples collected from the Glacier Peak study area and analyzed using an aqua-regia leach/inductively coupled plasma method: U.S. Geological Survey Open-File Report 83-343, ii, 116 p., https://doi.org/10.3133/ofr83343.","productDescription":"ii, 116 p.","costCenters":[],"links":[{"id":389572,"rank":3,"type":{"id":36,"text":"NGMDB Index Page"},"url":"https://ngmdb.usgs.gov/Prodesc/proddesc_13990.htm"},{"id":34397,"rank":300,"type":{"id":11,"text":"Document"},"url":"https://pubs.usgs.gov/of/1983/0343/report.pdf","linkFileType":{"id":1,"text":"pdf"}},{"id":140165,"rank":0,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/of/1983/0343/report-thumb.jpg"}],"country":"United States","state":"Washington","otherGeospatial":"Glacier Peak study area","geographicExtents":"{\n \"type\": \"FeatureCollection\",\n \"features\": [\n {\n \"type\": \"Feature\",\n \"properties\": {},\n \"geometry\": {\n \"type\": \"Polygon\",\n \"coordinates\": [\n [\n [\n -121.5,\n 47.9180\n ],\n [\n -120.5,\n 47.9180\n ],\n [\n -120.5,\n 48.5\n ],\n [\n -121.5,\n 48.5\n ],\n [\n -121.5,\n 47.9180\n ]\n ]\n ]\n }\n }\n ]\n}","noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"4f4e4a9ae4b07f02db65d4a9","contributors":{"authors":[{"text":"Church, S. E.","contributorId":58260,"corporation":false,"usgs":true,"family":"Church","given":"S.","email":"","middleInitial":"E.","affiliations":[],"preferred":false,"id":154174,"contributorType":{"id":1,"text":"Authors"},"rank":1},{"text":"Motooka, J. M.","contributorId":8834,"corporation":false,"usgs":true,"family":"Motooka","given":"J.","middleInitial":"M.","affiliations":[],"preferred":false,"id":154171,"contributorType":{"id":1,"text":"Authors"},"rank":2},{"text":"Werschky, R. S.","contributorId":19149,"corporation":false,"usgs":true,"family":"Werschky","given":"R.","email":"","middleInitial":"S.","affiliations":[],"preferred":false,"id":154172,"contributorType":{"id":1,"text":"Authors"},"rank":3},{"text":"Bigelow, R. C.","contributorId":90718,"corporation":false,"usgs":true,"family":"Bigelow","given":"R.","email":"","middleInitial":"C.","affiliations":[],"preferred":false,"id":154175,"contributorType":{"id":1,"text":"Authors"},"rank":4},{"text":"Van Trump, George","contributorId":19156,"corporation":false,"usgs":true,"family":"Van Trump","given":"George","email":"","affiliations":[],"preferred":false,"id":154173,"contributorType":{"id":1,"text":"Authors"},"rank":5}]}} ,{"id":18478,"text":"ofr83542 - 1983 - Sources and mechanisms of recharge for ground water in the west-central Amargosa Desert, Nevada– A geochemical interpretation","interactions":[{"subject":{"id":18478,"text":"ofr83542 - 1983 - Sources and mechanisms of recharge for ground water in the west-central Amargosa Desert, Nevada– A geochemical interpretation","indexId":"ofr83542","publicationYear":"1983","noYear":false,"title":"Sources and mechanisms of recharge for ground water in the west-central Amargosa Desert, Nevada– A geochemical interpretation"},"predicate":"SUPERSEDED_BY","object":{"id":5784,"text":"pp712F - 1985 - Sources and mechanisms of recharge for ground water in the west-central Amargosa Desert, Nevada; a geochemical interpretation","indexId":"pp712F","publicationYear":"1985","noYear":false,"chapter":"F","title":"Sources and mechanisms of recharge for ground water in the west-central Amargosa Desert, Nevada; a geochemical interpretation"},"id":1}],"supersededBy":{"id":5784,"text":"pp712F - 1985 - Sources and mechanisms of recharge for ground water in the west-central Amargosa Desert, Nevada; a geochemical interpretation","indexId":"pp712F","publicationYear":"1985","noYear":false,"title":"Sources and mechanisms of recharge for ground water in the west-central Amargosa Desert, Nevada; a geochemical interpretation"},"lastModifiedDate":"2021-12-09T21:45:56.659916","indexId":"ofr83542","displayToPublicDate":"1994-01-01T00:00:00","publicationYear":"1983","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":"83-542","title":"Sources and mechanisms of recharge for ground water in the west-central Amargosa Desert, Nevada– A geochemical interpretation","docAbstract":"Ground water in the west-central Amargosa Desert, Nevada, was recharged primarily by overland flow of snowmelt in or near the present-day stream channels, rather than by subsurface flow from highland recharge areas to the north. Geochemical arguments, including reaction mechanisms, are used to support these findings. Carbon-, hydrogen-, and oxygen-isotope data show that much of the recharge in the area occurred during late Wisconsin time. Absence of ground-water recharge prior to late Pleistocene is considered to indicate that either climatic conditions were unfavorable for recharge or that ground-water velocities were such that they transported this earlier recharge away from the study aea. 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Surface-water discharge was determined at 11,076 stations; stage data on streams, reservoirs, and lakes were recorded at 2,136 stations; and surface-water quality was determined at 4,610 stations. Ground-water levels were measured at 35,621 stations, and the quality of ground water was determined at 7,648 stations nationwide. Information on precipitation quantity was collected at 800 stations, and quality of precipitation was analyzed at 121 stations. 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","language":"English","publisher":"U.S. Geological Survey","doi":"10.3133/ofr83150","usgsCitation":"Strause, J.L., and Ranzau, C., 1983, Approximate water-level changes in wells in the Chicot and Evangeline aquifers, 1977-83 and 1982-83 and measured compaction, 1973-83 in Harris and Galvestan counties, Texas: U.S. Geological Survey Open-File Report 83-150, 7 p., https://doi.org/10.3133/ofr83150.","productDescription":"7 p.","onlineOnly":"N","additionalOnlineFiles":"N","costCenters":[{"id":583,"text":"Texas Water Science Center","active":true,"usgs":true}],"links":[{"id":176676,"rank":0,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/of/1983/0150/report-thumb.jpg"},{"id":79465,"rank":300,"type":{"id":11,"text":"Document"},"url":"https://pubs.usgs.gov/of/1983/0150/report.pdf","linkFileType":{"id":1,"text":"pdf"}}],"noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"4f4e4ac5e4b07f02db67a152","contributors":{"authors":[{"text":"Strause, Jeffrey L.","contributorId":61420,"corporation":false,"usgs":true,"family":"Strause","given":"Jeffrey","email":"","middleInitial":"L.","affiliations":[],"preferred":false,"id":225470,"contributorType":{"id":1,"text":"Authors"},"rank":1},{"text":"Ranzau, C.E. Jr.","contributorId":41831,"corporation":false,"usgs":true,"family":"Ranzau","given":"C.E.","suffix":"Jr.","email":"","affiliations":[],"preferred":false,"id":225469,"contributorType":{"id":1,"text":"Authors"},"rank":2}]}} ,{"id":7039,"text":"ofr83646 - 1983 - Chemical analyses and statistical summaries for samples of rock, minus-60-mesh (0.25-mm) stream sediment, and nonmagnetic heavy-mineral concentrate, Mount Raymond Roadless Area, Madera County, California","interactions":[],"lastModifiedDate":"2022-10-31T18:36:13.853905","indexId":"ofr83646","displayToPublicDate":"1994-01-01T00:00:00","publicationYear":"1983","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":"83-646","title":"Chemical analyses and statistical summaries for samples of rock, minus-60-mesh (0.25-mm) stream sediment, and nonmagnetic heavy-mineral concentrate, Mount Raymond Roadless Area, Madera County, California","docAbstract":"No abstract available.
","language":"English","publisher":"U.S. Geological Survey","doi":"10.3133/ofr83646","usgsCitation":"Sutley, S.J., Chaffee, M., Fey, D., and Hill, R.H., 1983, Chemical analyses and statistical summaries for samples of rock, minus-60-mesh (0.25-mm) stream sediment, and nonmagnetic heavy-mineral concentrate, Mount Raymond Roadless Area, Madera County, California: U.S. Geological Survey Open-File Report 83-646, Report: i, 22 p.; 1 Plate: 12.97 × 12.54 inches, https://doi.org/10.3133/ofr83646.","productDescription":"Report: i, 22 p.; 1 Plate: 12.97 × 12.54 inches","costCenters":[],"links":[{"id":408896,"rank":4,"type":{"id":36,"text":"NGMDB Index Page"},"url":"https://ngmdb.usgs.gov/Prodesc/proddesc_14147.htm","linkFileType":{"id":5,"text":"html"}},{"id":34331,"rank":300,"type":{"id":11,"text":"Document"},"url":"https://pubs.usgs.gov/of/1983/0646/report.pdf","linkFileType":{"id":1,"text":"pdf"}},{"id":34330,"rank":400,"type":{"id":17,"text":"Plate"},"url":"https://pubs.usgs.gov/of/1983/0646/plate-1.pdf","linkFileType":{"id":1,"text":"pdf"}},{"id":140796,"rank":0,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/of/1983/0646/report-thumb.jpg"}],"country":"United States","state":"California","county":"Madera County","otherGeospatial":"Mount Raymond Roadless Area","geographicExtents":"{\n \"type\": \"FeatureCollection\",\n \"features\": [\n {\n \"type\": \"Feature\",\n \"properties\": {},\n \"geometry\": {\n \"coordinates\": [\n [\n [\n -119.598,\n 37.548\n ],\n [\n -119.598,\n 37.442\n ],\n [\n -119.458,\n 37.442\n ],\n [\n -119.458,\n 37.548\n ],\n [\n -119.598,\n 37.548\n ]\n ]\n ],\n \"type\": \"Polygon\"\n }\n }\n ]\n}","noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"4f4e49e2e4b07f02db5e4baf","contributors":{"authors":[{"text":"Sutley, S. 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","language":"English","publisher":"U.S. Geological Survey","doi":"10.3133/ofr8391","usgsCitation":"Eberlein, G., Churkin, M., Carter, C., Berg, H.C., and Ovenshine, A., 1983, Geology of the Craig quadrangle, Alaska: U.S. Geological Survey Open-File Report 83-91, Report: 52 p.; 4 Plates: 38.93 × 35.04 inches or smaller, https://doi.org/10.3133/ofr8391.","productDescription":"Report: 52 p.; 4 Plates: 38.93 × 35.04 inches or smaller","costCenters":[],"links":[{"id":397481,"rank":7,"type":{"id":36,"text":"NGMDB Index Page"},"url":"https://ngmdb.usgs.gov/Prodesc/proddesc_14268.htm"},{"id":34576,"rank":400,"type":{"id":17,"text":"Plate"},"url":"https://pubs.usgs.gov/of/1983/0091/plate-1.pdf","linkFileType":{"id":1,"text":"pdf"}},{"id":34580,"rank":300,"type":{"id":11,"text":"Document"},"url":"https://pubs.usgs.gov/of/1983/0091/report.pdf","linkFileType":{"id":1,"text":"pdf"}},{"id":34577,"rank":400,"type":{"id":17,"text":"Plate"},"url":"https://pubs.usgs.gov/of/1983/0091/plate-2.pdf","linkFileType":{"id":1,"text":"pdf"}},{"id":140157,"rank":0,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/of/1983/0091/report-thumb.jpg"},{"id":34579,"rank":402,"type":{"id":17,"text":"Plate"},"url":"https://pubs.usgs.gov/of/1983/0091/plate-4.pdf","linkFileType":{"id":1,"text":"pdf"}},{"id":34578,"rank":401,"type":{"id":17,"text":"Plate"},"url":"https://pubs.usgs.gov/of/1983/0091/plate-3.pdf","linkFileType":{"id":1,"text":"pdf"}}],"scale":"250000","country":"United States","state":"Alaska","otherGeospatial":"Craig quadrangle","geographicExtents":"{\n \"type\": \"FeatureCollection\",\n \"features\": [\n {\n \"type\": \"Feature\",\n \"properties\": {},\n \"geometry\": {\n \"type\": \"Polygon\",\n \"coordinates\": [\n [\n [\n -134.667,\n 55\n ],\n [\n -132,\n 55\n ],\n [\n -132,\n 56\n ],\n [\n -134.667,\n 56\n ],\n [\n -134.667,\n 55\n ]\n ]\n ]\n }\n }\n ]\n}","noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"4f4e4ad4e4b07f02db68328d","contributors":{"authors":[{"text":"Eberlein, G. 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The atlas was begun as an effort to depict the areal distribution of surficial geologic deposits and other materials that accumulated or formed during the past 2+ million years, the period that includes all activities of the human species. These materials are at the surface of the earth. They make up the 'ground' on which we walk, the 'dirt' in which we dig foundations, and the 'soil' in which we grow crops. Most of our human activity is related in one way or another to these surface materials that are referred to collectively by many geologists as regolith, the mantle of fragmental and generally unconsolidated material that overlies the bedrock foundation of the continent. The maps were compiled at 1:1,000,000 scale.","language":"ENGLISH","doi":"10.3133/i1420(NK16)","usgsCitation":"Bleuer, N.K., Mickelson, D.M., Farrand, W.R., Goldthwait, R.P., and Fullerton, D.S., 1983, Quaternary geologic map of the Chicago 4 degrees x 6 degrees quadrangle, United States: U.S. Geological Survey IMAP 1420(NK-16), 1 map :col. ;44 x 51 cm., on sheet 74 x 139 cm. folded in envelope 30 x 24 cm., https://doi.org/10.3133/i1420(NK16).","productDescription":"1 map :col. ;44 x 51 cm., on sheet 74 x 139 cm. folded in envelope 30 x 24 cm.","costCenters":[],"links":[{"id":187409,"rank":0,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/thumbnails/usgs_thumb.jpg"},{"id":6074,"rank":100,"type":{"id":15,"text":"Index Page"},"url":"https://pubs.usgs.gov/imap/i-1420/nk-16/","linkFileType":{"id":5,"text":"html"}},{"id":100786,"rank":400,"type":{"id":17,"text":"Plate"},"url":"https://pubs.usgs.gov/imap/1420nk16/plate-1.pdf","size":"12692","linkFileType":{"id":1,"text":"pdf"}},{"id":106740,"rank":700,"type":{"id":15,"text":"Index Page"},"url":"https://ngmdb.usgs.gov/Prodesc/proddesc_9218.htm","linkFileType":{"id":5,"text":"html"},"description":"9218"}],"scale":"1000000","geographicExtents":"{ \"type\": \"FeatureCollection\", \"features\": [ { \"type\": \"Feature\", \"properties\": {}, \"geometry\": { \"type\": \"Polygon\", \"coordinates\": [ [ [ -90,40 ], [ -90,44 ], [ -84,44 ], [ -84,40 ], [ -90,40 ] ] ] } } ] }","noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"4f4e4a54e4b07f02db62bff4","contributors":{"compilers":[{"text":"Lineback, Jerry A.","contributorId":61514,"corporation":false,"usgs":true,"family":"Lineback","given":"Jerry","email":"","middleInitial":"A.","affiliations":[],"preferred":false,"id":749852,"contributorType":{"id":3,"text":"Compilers"},"rank":1}],"editors":[{"text":"Richmond, Gerald M.","contributorId":87165,"corporation":false,"usgs":true,"family":"Richmond","given":"Gerald M.","affiliations":[],"preferred":false,"id":749851,"contributorType":{"id":2,"text":"Editors"},"rank":1}],"authors":[{"text":"Bleuer, Ned K.","contributorId":14512,"corporation":false,"usgs":true,"family":"Bleuer","given":"Ned","email":"","middleInitial":"K.","affiliations":[],"preferred":false,"id":271546,"contributorType":{"id":1,"text":"Authors"},"rank":1},{"text":"Mickelson, David M.","contributorId":57544,"corporation":false,"usgs":true,"family":"Mickelson","given":"David","email":"","middleInitial":"M.","affiliations":[],"preferred":false,"id":271547,"contributorType":{"id":1,"text":"Authors"},"rank":2},{"text":"Farrand, William R.","contributorId":65542,"corporation":false,"usgs":true,"family":"Farrand","given":"William","email":"","middleInitial":"R.","affiliations":[],"preferred":false,"id":271548,"contributorType":{"id":1,"text":"Authors"},"rank":3},{"text":"Goldthwait, Richard P.","contributorId":90392,"corporation":false,"usgs":true,"family":"Goldthwait","given":"Richard","email":"","middleInitial":"P.","affiliations":[],"preferred":false,"id":271549,"contributorType":{"id":1,"text":"Authors"},"rank":4},{"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":271545,"contributorType":{"id":1,"text":"Authors"},"rank":5}]}} ,{"id":7930,"text":"ofr83640 - 1983 - Spectral analysis of the 1976 aeromagnetic survey of Harrat Rahat, Kingdom of Saudi Arabia","interactions":[],"lastModifiedDate":"2012-02-02T00:06:00","indexId":"ofr83640","displayToPublicDate":"1994-01-01T00:00:00","publicationYear":"1983","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":"83-640","title":"Spectral analysis of the 1976 aeromagnetic survey of Harrat Rahat, Kingdom of Saudi Arabia","docAbstract":"Harrat Rahat, an extensive plateau of Cenozoic mafic lava on the Precambrian shield of western Saudi Arabia, has been studied for its water resource and geothermal potential. In support of these investigations, the thickness of the lava sequence at more than 300 points was estimated by spectral analysis of low-level aeromagnetic profiles utilizing the integral Fourier transform of field intensity along overlapping profile segments. The optimum length of segment for analysis was determined to be about 40 km or 600 field samples. Contributions from two discrete magnetic source ensembles could be resolved on almost all spectra computed. The depths to these ensembles correspond closely to the flight height (300 m), and, presumably, to the mean depth to basement near the center of each profile segment. The latter association was confirmed in all three cases where spectral estimates could be directly compared with basement depths measured in drill holes. \r\n\r\nThe maximum thickness estimated for the lava section is 380 m and the mean about 150 m. Data from an isopach map prepared from these results suggest that thickness variations are strongly influenced by pre-harrat, north-northwest-trending topography probably consequent on Cenozoic faulting. The thickest zones show a rough correlation with three axially-disposed volcanic shields.","language":"ENGLISH","publisher":"U.S. Geological Survey,","doi":"10.3133/ofr83640","usgsCitation":"Blank, H.R., and Sadek, H.S., 1983, Spectral analysis of the 1976 aeromagnetic survey of Harrat Rahat, Kingdom of Saudi Arabia: U.S. Geological Survey Open-File Report 83-640, 32 p., 2 over-size sheets, ill., maps ;28 cm., https://doi.org/10.3133/ofr83640.","productDescription":"32 p., 2 over-size sheets, ill., maps ;28 cm.","costCenters":[],"links":[{"id":140734,"rank":0,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/of/1983/0640/report-thumb.jpg"},{"id":35500,"rank":400,"type":{"id":17,"text":"Plate"},"url":"https://pubs.usgs.gov/of/1983/0640/plate-1.pdf","linkFileType":{"id":1,"text":"pdf"}},{"id":35501,"rank":401,"type":{"id":17,"text":"Plate"},"url":"https://pubs.usgs.gov/of/1983/0640/plate-2.pdf","linkFileType":{"id":1,"text":"pdf"}},{"id":35502,"rank":300,"type":{"id":11,"text":"Document"},"url":"https://pubs.usgs.gov/of/1983/0640/report.pdf","linkFileType":{"id":1,"text":"pdf"}}],"noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"4f4e49e2e4b07f02db5e4c62","contributors":{"authors":[{"text":"Blank, H. 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","language":"English","publisher":"U.S. Geological Survey,","doi":"10.3133/wri834131","usgsCitation":"Ryals, G., 1983, Regional geohydrology of the northern Louisiana salt-dome basin, part III, potentiometric levels of the Wilcox-Carrizo and Sparta aquifers: U.S. Geological Survey Water-Resources Investigations Report 83-4131, iv, 16 p., https://doi.org/10.3133/wri834131.","productDescription":"iv, 16 p.","costCenters":[],"links":[{"id":389713,"rank":3,"type":{"id":36,"text":"NGMDB Index Page"},"url":"https://ngmdb.usgs.gov/Prodesc/proddesc_49169.htm"},{"id":58332,"rank":300,"type":{"id":11,"text":"Document"},"url":"https://pubs.usgs.gov/wri/1983/4131/report.pdf","linkFileType":{"id":1,"text":"pdf"}},{"id":159714,"rank":0,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/wri/1983/4131/report-thumb.jpg"}],"country":"United States","state":"Louisiana","otherGeospatial":"Wilcox-Carrizo and Sparta aquifers","geographicExtents":"{\n \"type\": \"FeatureCollection\",\n \"features\": [\n {\n \"type\": \"Feature\",\n \"properties\": {},\n \"geometry\": {\n \"type\": \"Polygon\",\n \"coordinates\": [\n [\n [\n -93.5980224609375,\n 31.69779270531287\n ],\n [\n -92.70263671874999,\n 31.69779270531287\n ],\n [\n -92.70263671874999,\n 32.616243412727385\n ],\n [\n -93.5980224609375,\n 32.616243412727385\n ],\n [\n -93.5980224609375,\n 31.69779270531287\n ]\n ]\n ]\n }\n }\n ]\n}","noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"4f4e4a60e4b07f02db635013","contributors":{"authors":[{"text":"Ryals, G.N.","contributorId":47374,"corporation":false,"usgs":true,"family":"Ryals","given":"G.N.","email":"","affiliations":[],"preferred":false,"id":201603,"contributorType":{"id":1,"text":"Authors"},"rank":1}]}} ,{"id":20547,"text":"ofr8460 - 1983 - Flood-flow characteristics of Lullwater Creek from Ponce de Leon Avenue to proposed Presidential Parkway, Atlanta, Georgia","interactions":[],"lastModifiedDate":"2016-12-14T13:52:13","indexId":"ofr8460","displayToPublicDate":"1994-01-01T00:00:00","publicationYear":"1983","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":"84-60","title":"Flood-flow characteristics of Lullwater Creek from Ponce de Leon Avenue to proposed Presidential Parkway, Atlanta, Georgia","language":"ENGLISH","publisher":"U.S. Geological Survey,","doi":"10.3133/ofr8460","usgsCitation":"Price, M., 1983, Flood-flow characteristics of Lullwater Creek from Ponce de Leon Avenue to proposed Presidential Parkway, Atlanta, Georgia: U.S. Geological Survey Open-File Report 84-60, v, 22 p. :ill., map ;29 cm., https://doi.org/10.3133/ofr8460.","productDescription":"v, 22 p. :ill., map ;29 cm.","costCenters":[{"id":13634,"text":"South Atlantic Water Science Center","active":true,"usgs":true}],"links":[{"id":50066,"rank":300,"type":{"id":11,"text":"Document"},"url":"https://pubs.usgs.gov/of/1984/0060/report.pdf","linkFileType":{"id":1,"text":"pdf"}},{"id":153213,"rank":0,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/of/1984/0060/report-thumb.jpg"},{"id":50065,"rank":400,"type":{"id":17,"text":"Plate"},"url":"https://pubs.usgs.gov/of/1984/0060/plate-1.pdf","linkFileType":{"id":1,"text":"pdf"}}],"country":"United States","state":"Georgia","city":"Atlanta","otherGeospatial":"Lullwater Creek","geographicExtents":"{\n \"type\": \"FeatureCollection\",\n \"features\": [\n {\n \"type\": \"Feature\",\n \"properties\": {},\n \"geometry\": {\n \"type\": \"Polygon\",\n \"coordinates\": [\n [\n [\n -84.34513092041016,\n 33.75445967067027\n ],\n [\n -84.34513092041016,\n 33.807964383611484\n ],\n [\n -84.30951118469238,\n 33.807964383611484\n ],\n [\n -84.30951118469238,\n 33.75445967067027\n ],\n [\n -84.34513092041016,\n 33.75445967067027\n ]\n ]\n ]\n }\n }\n ]\n}","noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"4f4e49d8e4b07f02db5df79e","contributors":{"authors":[{"text":"Price, McGlone","contributorId":42964,"corporation":false,"usgs":true,"family":"Price","given":"McGlone","email":"","affiliations":[],"preferred":false,"id":182825,"contributorType":{"id":1,"text":"Authors"},"rank":1}]}} ,{"id":7438,"text":"ofr83460 - 1983 - Preliminary interpretation of marine sparker reflection profiles offshore from Cape Ann, Massachusetts, to Hampton, New Hampshire","interactions":[],"lastModifiedDate":"2022-09-13T20:22:42.413475","indexId":"ofr83460","displayToPublicDate":"1994-01-01T00:00:00","publicationYear":"1983","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":"83-460","title":"Preliminary interpretation of marine sparker reflection profiles offshore from Cape Ann, Massachusetts, to Hampton, New Hampshire","docAbstract":"No abstract available.
","language":"English","publisher":"U.S. Geological Survey","doi":"10.3133/ofr83460","usgsCitation":"Bothner, W.A., Simpson, R., Eskenasy, D., Shride, A., Oldale, R.F., and Gage, T.B., 1983, Preliminary interpretation of marine sparker reflection profiles offshore from Cape Ann, Massachusetts, to Hampton, New Hampshire: U.S. Geological Survey Open-File Report 83-460, Report: 28 p.; 2 Plates: 18.58 × 18.96 inches and 16.61 × 16.19 inches, https://doi.org/10.3133/ofr83460.","productDescription":"Report: 28 p.; 2 Plates: 18.58 × 18.96 inches and 16.61 × 16.19 inches","costCenters":[],"links":[{"id":406641,"rank":5,"type":{"id":36,"text":"NGMDB Index Page"},"url":"https://ngmdb.usgs.gov/Prodesc/proddesc_14048.htm","linkFileType":{"id":5,"text":"html"}},{"id":34851,"rank":401,"type":{"id":17,"text":"Plate"},"url":"https://pubs.usgs.gov/of/1983/0460/plate-2.pdf","linkFileType":{"id":1,"text":"pdf"}},{"id":34850,"rank":400,"type":{"id":17,"text":"Plate"},"url":"https://pubs.usgs.gov/of/1983/0460/plate-1.pdf","linkFileType":{"id":1,"text":"pdf"}},{"id":34852,"rank":300,"type":{"id":11,"text":"Document"},"url":"https://pubs.usgs.gov/of/1983/0460/report.pdf","linkFileType":{"id":1,"text":"pdf"}},{"id":140391,"rank":0,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/of/1983/0460/report-thumb.jpg"}],"country":"United States","state":"Massachusetts, New Hampshire","city":"Hampton","otherGeospatial":"Cape Ann","geographicExtents":"{\n \"type\": \"FeatureCollection\",\n \"features\": [\n {\n \"type\": \"Feature\",\n \"properties\": {},\n \"geometry\": {\n \"type\": \"Polygon\",\n \"coordinates\": [\n [\n [\n -70.927734375,\n 42.532844281713125\n ],\n [\n -70.4608154296875,\n 42.532844281713125\n ],\n [\n -70.4608154296875,\n 43.00866413845207\n ],\n [\n -70.927734375,\n 43.00866413845207\n ],\n [\n -70.927734375,\n 42.532844281713125\n ]\n ]\n ]\n }\n }\n ]\n}","noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"4f4e4abce4b07f02db67324d","contributors":{"authors":[{"text":"Bothner, Wallace A.","contributorId":80270,"corporation":false,"usgs":true,"family":"Bothner","given":"Wallace","email":"","middleInitial":"A.","affiliations":[{"id":595,"text":"U.S. Geological Survey","active":false,"usgs":true}],"preferred":false,"id":155619,"contributorType":{"id":1,"text":"Authors"},"rank":1},{"text":"Simpson, R.W.","contributorId":76738,"corporation":false,"usgs":true,"family":"Simpson","given":"R.W.","email":"","affiliations":[],"preferred":false,"id":155618,"contributorType":{"id":1,"text":"Authors"},"rank":2},{"text":"Eskenasy, Diane","contributorId":17089,"corporation":false,"usgs":true,"family":"Eskenasy","given":"Diane","affiliations":[],"preferred":false,"id":155614,"contributorType":{"id":1,"text":"Authors"},"rank":3},{"text":"Shride, A. F.","contributorId":23609,"corporation":false,"usgs":true,"family":"Shride","given":"A. F.","affiliations":[],"preferred":false,"id":155615,"contributorType":{"id":1,"text":"Authors"},"rank":4},{"text":"Oldale, R. F.","contributorId":30090,"corporation":false,"usgs":true,"family":"Oldale","given":"R.","email":"","middleInitial":"F.","affiliations":[],"preferred":false,"id":155616,"contributorType":{"id":1,"text":"Authors"},"rank":5},{"text":"Gage, T. B.","contributorId":75610,"corporation":false,"usgs":true,"family":"Gage","given":"T.","email":"","middleInitial":"B.","affiliations":[],"preferred":false,"id":155617,"contributorType":{"id":1,"text":"Authors"},"rank":6}]}} ,{"id":8452,"text":"ofr83526 - 1983 - Water-quality characteristics for selected sites on the Cape Fear River, North Carolina, 1955-80: Variability, loads, and trends of selected constituents","interactions":[],"lastModifiedDate":"2022-12-06T22:28:21.895193","indexId":"ofr83526","displayToPublicDate":"1994-01-01T00:00:00","publicationYear":"1983","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":"83-526","title":"Water-quality characteristics for selected sites on the Cape Fear River, North Carolina, 1955-80: Variability, loads, and trends of selected constituents","docAbstract":"Water-quality data for selected sites in the Cape Fear River basin collected by the U.S. Geological Survey, the North Carolina Department of Natural Resources and Community Development and the University of North Carolina at Chapel Hill are analyzed and interpreted in this report. Emphasis is given to the Cape Fear River at Lock 1 near Kelly, where data are most complete. Other data included in the report were collected from the Cape Fear River at Lillington, the Haw River near the Jordan Dam, and the Deep River at Moncure. \r\n\r\nAvailable data indicate that concentrations of dissolved oxygen at study sites are almost always within U.S. Environmental Protection Agency criteria; however, on two sampling dates, the concentration of dissolved oxygen in the Cape Fear at Lock 1 fell slightly below the 5.0 mg/L recommended for fish populations. Measurements of pH from all stations were frequently below the lower limit of 6.5 pH units recommended for protection of freshwater aquatic life. \r\n\r\nMajor dissolved ions detected are sodium and bicarbonate. Sodium concentration averages 8.6 mg/L and bicarbonate averages 17.5 mg/L at Lock 1. Concentrations of dissolved substances and suspended sediment decrease in the downstream direction, presumably because the more heavily populated part of the basin is near the headwaters of the system. \r\n\r\nHeavy metals, with the exceptions of cadmium and mercury, rarely exceed Environmental Protection Agency criteria for the protection of aquatic life. Concentrations of mercury in the Haw River, which exceed the recommended 0.20 mg/L needed to protect aquatic life, have frequently been reported by other authors. Several of the most toxic metals, arsenic, cadmium, and cobalt, are about five times more concentrated in water from the Haw River site than from other study sites in the basin. Iron and manganese frequently exceed North Carolina water-quality standards. \r\n\r\nAvailable nitrogen averages 1.21 mg/L and available phosphorus averages 0.21 mg/L at Lock 1. Nuisance algal growths have not been identified as a problem in the river. \r\n\r\nComparisons of water-quality data for baseline (natural) and present conditions indicate that more than 50 percent of most dissolved substances and over 80 percent of certain forms of nitrogen and phosph6rus result from development.\r\n\r\nOver the past 25 years, increases in concentrations of specific conductance, dissolved magnesium, dissolved sodium, dissolved potassium, dissolved sulfate, dissolved solids, and total nitrite plus nitrate nitrogen were detected in the Cape Fear River at Lock 1. Values for pH and dissolved silica are decreasing. Concentrations of most dissolved constituents at Lock 1 are increasing. These increases are statistically related to increases in population and manufacturing employment in the basin but are unrelated to agricultural activity.","language":"English","publisher":"U.S. Geological Survey","doi":"10.3133/ofr83526","usgsCitation":"Crawford, J.K., 1983, Water-quality characteristics for selected sites on the Cape Fear River, North Carolina, 1955-80: Variability, loads, and trends of selected constituents: U.S. Geological Survey Open-File Report 83-526, vi, 66 p., https://doi.org/10.3133/ofr83526.","productDescription":"vi, 66 p.","costCenters":[{"id":13634,"text":"South Atlantic Water Science Center","active":true,"usgs":true}],"links":[{"id":140544,"rank":0,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/of/1983/0526/report-thumb.jpg"},{"id":36023,"rank":300,"type":{"id":11,"text":"Document"},"url":"https://pubs.usgs.gov/of/1983/0526/report.pdf","linkFileType":{"id":1,"text":"pdf"}},{"id":410128,"rank":3,"type":{"id":36,"text":"NGMDB Index Page"},"url":"https://ngmdb.usgs.gov/Prodesc/proddesc_14090.htm","linkFileType":{"id":5,"text":"html"}}],"country":"United States","state":"North Carolina","otherGeospatial":"Cape Fear River","geographicExtents":"{\n \"type\": \"FeatureCollection\",\n \"features\": [\n {\n \"type\": \"Feature\",\n \"properties\": {},\n \"geometry\": {\n \"type\": \"Polygon\",\n \"coordinates\": [\n [\n [\n -77.904052734375,\n 33.75174787568194\n ],\n [\n -77.8546142578125,\n 33.988918483762156\n ],\n [\n -77.7996826171875,\n 34.17090836352573\n ],\n [\n -77.53051757812499,\n 34.384246040152185\n ],\n [\n -77.464599609375,\n 34.43409789359469\n ],\n [\n -77.882080078125,\n 35.02099970111467\n ],\n [\n -78.20068359374999,\n 35.133386854253075\n ],\n [\n -78.519287109375,\n 35.209721645221386\n ],\n [\n -78.7335205078125,\n 35.51881428123057\n ],\n [\n -78.83239746093749,\n 35.82226734114509\n ],\n [\n -78.88732910156249,\n 36.01800375871416\n ],\n [\n -79.4366455078125,\n 36.146746777814364\n ],\n [\n -80.03814697265625,\n 36.02189133007692\n ],\n [\n -80.0628662109375,\n 35.957443980673595\n ],\n [\n -80.06904602050781,\n 35.78941187118459\n ],\n [\n -79.815673828125,\n 35.382332329032984\n ],\n [\n -79.5684814453125,\n 35.22991591449646\n ],\n [\n -79.46685791015625,\n 35.074964853989556\n ],\n [\n -79.22515869140625,\n 34.9895035675793\n ],\n [\n -78.88732910156249,\n 34.77545980961412\n ],\n [\n -78.78021240234375,\n 34.70549341022544\n ],\n [\n -78.42041015625,\n 34.31621838080741\n ],\n [\n -78.22265625,\n 33.988918483762156\n ],\n [\n -77.904052734375,\n 33.75174787568194\n ]\n ]\n ]\n }\n }\n ]\n}","noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"4f4e4a9ae4b07f02db65d552","contributors":{"authors":[{"text":"Crawford, J. 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