The magnetic anomaly data open-filed in this report represent part of a much larger data set covering most of the conterminous United States. The anomaly map consists of 10 sheets covering an area in the northwestern United States. These were prepared primarily from existing aeromagnetic data, and secondarily from ground data, the latter located primarily in North Dakota and South Dakota.
","language":"English","publisher":"U.S. Geological Survey","doi":"10.3133/ofr81835","usgsCitation":"Zietz, I., 1981, Preliminary composite magnetic anomaly map of part of the Northwestern United States: U.S. Geological Survey Open-File Report 81-835, 13 p., https://doi.org/10.3133/ofr81835.","productDescription":"13 p.","costCenters":[],"links":[{"id":145049,"rank":1,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/of/1981/0835/report-thumb.jpg"},{"id":495477,"rank":2,"type":{"id":11,"text":"Document"},"url":"https://pubs.usgs.gov/of/1981/0835/report.pdf","linkFileType":{"id":1,"text":"pdf"}}],"country":"United States","noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"4f4e4ac9e4b07f02db67c6ed","contributors":{"authors":[{"text":"Zietz, Isidore","contributorId":76708,"corporation":false,"usgs":true,"family":"Zietz","given":"Isidore","affiliations":[],"preferred":false,"id":163766,"contributorType":{"id":1,"text":"Authors"},"rank":1}]}} ,{"id":38645,"text":"pp1134D - 1981 - Biogeochemical variability of plants at native and altered sites, San Juan Basin, New Mexico","interactions":[],"lastModifiedDate":"2012-02-02T00:09:58","indexId":"pp1134D","displayToPublicDate":"1994-01-01T00:00:00","publicationYear":"1981","noYear":false,"publicationType":{"id":18,"text":"Report"},"publicationSubtype":{"id":5,"text":"USGS Numbered Series"},"seriesTitle":{"id":331,"text":"Professional Paper","code":"PP","onlineIssn":"2330-7102","printIssn":"1044-9612","active":true,"publicationSubtype":{"id":5}},"seriesNumber":"1134","chapter":"D","title":"Biogeochemical variability of plants at native and altered sites, San Juan Basin, New Mexico","docAbstract":"The San Juan Basin is becoming a major energy resource region. The anticipated increase in strip mining for coal can be expected to alter the geochemical and biogeochemical environment. because such activities destroy the native vegetation communities, rearrange the rock strata, and disrupt natural soil development. This study investigated the variability in the biogeochemistry of native plant species at both undisturbed and altered sites and assessed the importance of the observed differences. Three studies are involved in this investigation: Study 1, the biogeochemical variability of native species found at sites throughout that part of the basin underlain by economically recoverable coal; Study 2, the biogeochemical variability of native species growing on soils considered favorable for use in the topsoiling of spoil areas; and Study 3, the biogeochemical variability of native species on rehabilitated sites at the San Juan coal mine. \r\n\r\nSummary statistics for concentrations of 35 elements (and ash yield) are reported in Study 1 for galleta grass, broom snakeweed, and fourwing saltbush. The concentrations of manganese, molybdenum, nickel, and uranium (and possibly iron and selenium) in galleta show regional patterns, with the highest values generally found in the south-central region and western edge of the study area. Differences in the concentration of elements between species was generally subtle (less than a factor of two) except for the following: ash yield of saltbush was two times that of the other plants; boron in snakeweed and saltbush was four times greater than in galleta; iron in galleta was two times greater than in saltbush; and, calcium, magnesium, potassium, phosphorus, and sulfur were generally highest in saltbush. \r\n\r\nSummary statistics (including the 95-percent expected range) for concentrations of 35 elements (and ash yield) are reported from Study 2 for galleta and broom snakeweed growing on the Sheppard, Shiprock, and Doak soil association. Significant regional (greater than 10 km) variation for aluminum, iron, sulfur, vanadium, and zirconium in galleta are reported; however, for most elements, a significant proportion of the variation in the data was measured locally (less than 0.1 km). This variation indicates that samples of galleta and snakeweed taken more than 10 km apart vary, in their element composition, little more than plants sampled as close together as 0.1 km. \r\n\r\nThe concentrations of 35 elements (and ash yield) in alkali sacaton and fourwing saltbush, which were collected on a rehabilitation plot at the San Juan mine (Study 3), are compared with those of control samples of similar material from native sites from throughout the ,an Juan Basin. Concentrations of aluminum, arsenic, boron, cobalt, copper, fluorine, iron, lead, manganese, sodium, and uranium in samples of saltbush growing over spoil generally exceed the levels of these elements in control samples. For many elements, concentrations in mine samples are from two to five times higher 1 han concentrations in the control samples. Sodium concentrations i saltbush, however, were 100 times higher in mine samples than in control samples. This high concentration reflects a corresponding : OO-fold increase in the extractable sodium levels in spoil material s compared to C-horizon control samples. Sampled plants from the l1ine area, spaced relatively close together (5 m (meters) or less), vary greatly in their element compositions, apparently in response 1 J the heterogenous composition and element availability of the l1ine soils. Topsoiling to a depth of 20 cm (centimeters) does little to meliorate the uptake of elements from spoil by saltbush.","language":"ENGLISH","doi":"10.3133/pp1134D","usgsCitation":"Gough, L.P., and Severson, R.C., 1981, Biogeochemical variability of plants at native and altered sites, San Juan Basin, New Mexico: U.S. Geological Survey Professional Paper 1134, 26 p., https://doi.org/10.3133/pp1134D.","productDescription":"26 p.","costCenters":[],"links":[{"id":124451,"rank":0,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/pp/1134d/report-thumb.jpg"},{"id":65476,"rank":300,"type":{"id":11,"text":"Document"},"url":"https://pubs.usgs.gov/pp/1134d/report.pdf","linkFileType":{"id":1,"text":"pdf"}}],"noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"4f4e4a49e4b07f02db6247b6","contributors":{"authors":[{"text":"Gough, L. P.","contributorId":64198,"corporation":false,"usgs":true,"family":"Gough","given":"L.","email":"","middleInitial":"P.","affiliations":[],"preferred":false,"id":220211,"contributorType":{"id":1,"text":"Authors"},"rank":1},{"text":"Severson, R. C.","contributorId":46498,"corporation":false,"usgs":true,"family":"Severson","given":"R.","email":"","middleInitial":"C.","affiliations":[],"preferred":false,"id":220210,"contributorType":{"id":1,"text":"Authors"},"rank":2}]}} ,{"id":60612,"text":"mf1201B - 1981 - Aeromagnetic map of the Mokelumne Wilderness and contiguous Rare II further planning areas, central Sierra Nevada, California","interactions":[],"lastModifiedDate":"2014-04-25T06:45:57","indexId":"mf1201B","displayToPublicDate":"1994-01-01T00:00:00","publicationYear":"1981","noYear":false,"publicationType":{"id":18,"text":"Report"},"publicationSubtype":{"id":5,"text":"USGS Numbered Series"},"seriesTitle":{"id":325,"text":"Miscellaneous Field Studies Map","code":"MF","active":false,"publicationSubtype":{"id":5}},"seriesNumber":"1201","chapter":"B","title":"Aeromagnetic map of the Mokelumne Wilderness and contiguous Rare II further planning areas, central Sierra Nevada, California","docAbstract":"The aeromagnetic map consists of parts of two surveys flown at an altitude of 300 m above the average ground surface. One survey (west park of the map_ centered over the Mokelumne Wilderness was flowing in a northeast-southwest direction along slight lines spaced at a horizontal interval of about 800 m (U>S> Geological Survey, 1979b). The survey to the east is part of a regional survey flown in an east-west direction along flight lines spaced at an interval of about 1,600 m (U.S. Geological Survey, 1979a). The join of the aeromagnetic contours along the border between the two surveys is generally conformable. The contour datum of the eastern regional survey, however, is about 650 nT (nanotesla) lower than the Mokelumne Wilderness survey because of difference in data reduction.
\nThe aeromagnetic pattern reflects variations of magnetization within the underlying rocks, but the pattern is complicated by strong topographic effects. That is, magnetic anomaly maxima tend to occur over ridges and hilltops and minima over canyons and depressions. The topographic effect exists mostly because a constant ground clearance could not be maintained at normal aircraft speeds in this area of rugged topographic relief. The recorded flight altitude varied from 30 m to nearly 1,500 m above the ground with local changes that approard 1,000 m in distances of less than 5,000 m.
\nFour magnetic anomalies that can be related to geologic features are discusses., Magnetic highs or lows cause by topography are not discussed.
","language":"English","publisher":"U.S. Geological Survey","publisherLocation":"Reston, VA","doi":"10.3133/mf1201B","usgsCitation":"Plouff, D., and McKee, E.H., 1981, Aeromagnetic map of the Mokelumne Wilderness and contiguous Rare II further planning areas, central Sierra Nevada, California: U.S. Geological Survey Miscellaneous Field Studies Map 1201, Map: 37.01 x 33.97 inches, https://doi.org/10.3133/mf1201B.","productDescription":"Map: 37.01 x 33.97 inches","costCenters":[],"links":[{"id":286554,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/thumbnails/usgs_thumb.jpg"},{"id":286553,"type":{"id":17,"text":"Plate"},"url":"https://pubs.usgs.gov/mf/1201-B/plate-1.pdf"}],"scale":"62500","datum":"National Geodetic Vertical Datum of 1929","country":"United States","state":"California","otherGeospatial":"Sierra Nevada","geographicExtents":"{ \"type\": \"FeatureCollection\", \"features\": [ { \"type\": \"Feature\", \"properties\": {}, \"geometry\": { \"type\": \"Polygon\", \"coordinates\": [ [ [ -120.25,38.416667 ], [ -120.25,38.75 ], [ -119.75,38.75 ], [ -119.75,38.416667 ], [ -120.25,38.416667 ] ] ] } } ] }","noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"4f4e4af4e4b07f02db691d73","contributors":{"authors":[{"text":"Plouff, Donald","contributorId":94657,"corporation":false,"usgs":true,"family":"Plouff","given":"Donald","email":"","affiliations":[],"preferred":false,"id":264079,"contributorType":{"id":1,"text":"Authors"},"rank":1},{"text":"McKee, Edwin H. mckee@usgs.gov","contributorId":3728,"corporation":false,"usgs":true,"family":"McKee","given":"Edwin","email":"mckee@usgs.gov","middleInitial":"H.","affiliations":[],"preferred":true,"id":264078,"contributorType":{"id":1,"text":"Authors"},"rank":2}]}} ,{"id":56286,"text":"wdrWA812 - 1981 - Water resources data, Washington, water year 1981: Vol. 2 - Eastern Washington","interactions":[],"lastModifiedDate":"2022-12-14T00:49:08.926242","indexId":"wdrWA812","displayToPublicDate":"1994-01-01T00:00:00","publicationYear":"1981","noYear":false,"publicationType":{"id":18,"text":"Report"},"publicationSubtype":{"id":5,"text":"USGS Numbered Series"},"seriesTitle":{"id":340,"text":"Water Data Report","code":"WDR","active":false,"publicationSubtype":{"id":5}},"seriesNumber":"WA-81-2","title":"Water resources data, Washington, water year 1981: Vol. 2 - Eastern Washington","docAbstract":"Water-resources data for the 1981 water year for Washington consist of records of stage, discharge, and water quality of streams; stage, contents, and water quality of lakes and reservoirs; and water levels and water quality of ground-water. This report, in two volumes, contains records for water discharge at 229 gaging stations; stage only at 5 gaging stations; stage and contents at 39 lakes and reservoirs; water quality at 39 gaging stations (including 6 lakes and reservoirs) and 100 wells; and water levels at 164 observation wells. Also included are data for 14 crest-stage and 28 water-quality partial-record stations. Locations of sites in this volume are on figures 4, 5, 6, and 22. Additional water data were collected at various sites not involved in the systematic data-collection program and are published as miscellaneous measurements and analyses. These data represent that part of the national Water Data system operated by the U.S. Geological Survey and cooperating State, local, and Federal agencies in Washington.
","language":"English","publisher":"U.S. Geological Survey","doi":"10.3133/wdrWA812","collaboration":"Prepared in cooperation with the State of Washington and with other agencies","usgsCitation":"Water Resources Division, U.S. Geological Survey, 1981, Water resources data, Washington, water year 1981: Vol. 2 - Eastern Washington: U.S. Geological Survey Water Data Report WA-81-2, x, 276 p., https://doi.org/10.3133/wdrWA812.","productDescription":"x, 276 p.","costCenters":[],"links":[{"id":174739,"rank":0,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/wdr/1981/wa-81-2/report-thumb.jpg"},{"id":410428,"rank":1,"type":{"id":11,"text":"Document"},"url":"https://pubs.usgs.gov/wdr/1981/wa-81-2/report.pdf","linkFileType":{"id":1,"text":"pdf"}}],"country":"United 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\"}}]}","noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"4f4e49f5e4b07f02db5f0ad2","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":532477,"contributorType":{"id":1,"text":"Authors"},"rank":1}]}} ,{"id":57311,"text":"wdrFL814 - 1981 - Water resources data, Florida water year 1981, volume 4, northwest Florida","interactions":[],"lastModifiedDate":"2025-07-22T14:00:58.961085","indexId":"wdrFL814","displayToPublicDate":"1994-01-01T00:00:00","publicationYear":"1981","noYear":false,"publicationType":{"id":18,"text":"Report"},"publicationSubtype":{"id":5,"text":"USGS Numbered Series"},"seriesTitle":{"id":340,"text":"Water Data Report","code":"WDR","active":false,"publicationSubtype":{"id":5}},"seriesNumber":"FL-81-4","title":"Water resources data, Florida water year 1981, volume 4, northwest Florida","docAbstract":"Water resources data for the 1981 water year in Florida consists of continuous or daily discharge for 279 streams, periodic discharge for 52 streams, continuous or daily stage for 64 streams, periodic stage for 82 streams, peak discharge for 78 streams and peak stage for 55 streams; continuous or daily elevations for 77 lakes, periodic elevations for 144 lakes; continuous ground-water levels for 488 wells, periodic ground-water levels for 575 wells, and miscellaneous water-level measurements for 2,317 wells; quality of water data for 444 surface-water sites and 613 wells.
The data for northwest Florida includes continuous or daily discharge for 64 streams, periodic discharge for 19 streams, peak discharge for 41 streams, and continuous or daily stage for 8 streams; continuous elevations for 4 lakes and periodic elevations for 26 lakes; continuous ground-water levels for 38 wells, periodic ground-water levels for 154 wells, and miscellaneous water-level measurements for 264 wells; quality of water for 36 surface-water sites and for 113 wells.
These data represent the National Water Data System records collected by the U.S. Geological Survey and cooperating local, state and federal agencies in Florida.
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\"}}]}","noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"4f4e4a0be4b07f02db5fbcdf","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":533056,"contributorType":{"id":1,"text":"Authors"},"rank":1}]}} ,{"id":48625,"text":"ofr802000 - 1981 - Surficial geophysical data for two cross-valley lines in the middle Eagle River valley, Alaska","interactions":[],"lastModifiedDate":"2012-02-02T00:10:48","indexId":"ofr802000","displayToPublicDate":"1994-01-01T00:00:00","publicationYear":"1981","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":"80-2000","title":"Surficial geophysical data for two cross-valley lines in the middle Eagle River valley, Alaska","docAbstract":"In 1979, six electrical resistivity and four seismic refraction soundings were made in the middle reach of the Eagle River valley northeast of Anchorage, Alaska. Interpretation of the geophysical data collected indicated that depth to bedrock below the valley floor varies between about 350 and 450 feet. Two, and perhaps three, major unconsolidated sedimentary layers are inferred to overlie bedrock, although other significant layers may not have been recognizable. No prior subsurface data were available in this area. A resistivity sounding was made also at a site about 7 miles downstream to explore for a buried bedrock channel. The data here indicated that the bedrock surface is about 50 feet above sea level. Hence, the hypothesis of a buried ancient outlet valley of Eagle River at this location gained more credence. (USGS)","language":"ENGLISH","doi":"10.3133/ofr802000","usgsCitation":"Dearborn, L.L., and Schaefer, D.H., 1981, Surficial geophysical data for two cross-valley lines in the middle Eagle River valley, Alaska: U.S. Geological Survey Open-File Report 80-2000, iii, 14 p. : ill., maps ; 28 cm., https://doi.org/10.3133/ofr802000.","productDescription":"iii, 14 p. : ill., maps ; 28 cm.","costCenters":[],"links":[{"id":171193,"rank":0,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/of/1980/2000/report-thumb.jpg"},{"id":85429,"rank":300,"type":{"id":11,"text":"Document"},"url":"https://pubs.usgs.gov/of/1980/2000/report.pdf","linkFileType":{"id":1,"text":"pdf"}}],"noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"4f4e4ae1e4b07f02db68891d","contributors":{"authors":[{"text":"Dearborn, Larry L.","contributorId":66687,"corporation":false,"usgs":true,"family":"Dearborn","given":"Larry","email":"","middleInitial":"L.","affiliations":[],"preferred":false,"id":237880,"contributorType":{"id":1,"text":"Authors"},"rank":1},{"text":"Schaefer, Donald H.","contributorId":77507,"corporation":false,"usgs":true,"family":"Schaefer","given":"Donald","email":"","middleInitial":"H.","affiliations":[],"preferred":false,"id":237881,"contributorType":{"id":1,"text":"Authors"},"rank":2}]}} ,{"id":27217,"text":"wri8127 - 1981 - Impact of suburban residential development on water resources in the area of Winslow Township, Camden County, New Jersey","interactions":[],"lastModifiedDate":"2024-06-17T21:05:45.95601","indexId":"wri8127","displayToPublicDate":"1994-01-01T00:00:00","publicationYear":"1981","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":"81-27","title":"Impact of suburban residential development on water resources in the area of Winslow Township, Camden County, New Jersey","docAbstract":"Surface-water and ground-water quality, streamflow, and data on ground-water levels in the upper Great Egg Harbor River basin in the vicinity of the Winslow Crossing residential development in Winslow Township are evaluated. The data include continuous streamflow at four sites, monthly stream water quality at seven sites, ground-water levels and periodic ground-water quality in four wells from 1972 through 1978.
Pumpage from the Cohansey Sand in the study area was lower than anticipated because of a slowdown in construction. The average pumpage of 0.48 million gallons per day during 1978 had little effect on ground-water levels.
Dissolved-solids concentrations were lower in a well upgradient from the urbanized area. Elevated levels of dissolved solids, specific conductance, chloride, nitrate, and phosphorus were found in the shallow ground water in the vicinity of the Winslow wastewater treatment plant because of effluent infiltration ponds. Nitrate was greatly reduced in October 1974 by a change in the treatment process, which increased denitrification. Phosphorus concentrations in the ground water remained elevated, however.
Water from the most urbanized drainage basin was a magnesium bicarbonate type, while the less developed basins had sodium chloride sulfate type waters. Water from the two developed basins had higher median pH (7.1) compared with that of the other basins (5.6-6.3).
Winslow Crossing’s development had only a slight effect on the quality of water in Great Egg Harbor River. The river receives point and non-point discharges upstream from Winslow Crossing, and the quality of the water generally improves as the river flows downstream.
Streamflow and rainfall were slightly above normal. Unit hydrograph analysis of one basin showed an 80 percent increase in the peak discharge of a 60-minute unit hydrograph (from approximately 150 to 270 cubic feet per second) after the development of 14 percent of the basin. Installation of a stormwater detention basin reduced the peak discharge to 220 ft3/s. Sediment discharge from this basin averaged 0.24 tons/d/mi2 during construction but decreased to the preconstruction level of 0.06 tons/d/mi2 after the completion of construction and the installation of the detention basin.
","language":"English","publisher":"U.S. Geological Survey","doi":"10.3133/wri8127","collaboration":"Prepared in cooperation with the New Jersey Department of Environmental Protection, Division of Water Resources","usgsCitation":"Fusillo, T.V., 1981, Impact of suburban residential development on water resources in the area of Winslow Township, Camden County, New Jersey: U.S. Geological Survey Water-Resources Investigations Report 81-27, v, 38 p., https://doi.org/10.3133/wri8127.","productDescription":"v, 38 p.","costCenters":[],"links":[{"id":430338,"rank":3,"type":{"id":36,"text":"NGMDB Index Page"},"url":"https://ngmdb.usgs.gov/Prodesc/proddesc_35468.htm","linkFileType":{"id":5,"text":"html"}},{"id":13712,"rank":2,"type":{"id":15,"text":"Index Page"},"url":"https://pubs.usgs.gov/wri/wri81-27/","linkFileType":{"id":5,"text":"html"}},{"id":159054,"rank":1,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/thumbnails/usgs_thumb.jpg"}],"scale":"24000","country":"United States","state":"New Jersey","county":"Camden County","otherGeospatial":"Winslow Township","geographicExtents":"{\n \"type\": \"FeatureCollection\",\n \"features\": [\n {\n \"type\": \"Feature\",\n \"properties\": {},\n \"geometry\": {\n \"coordinates\": [\n [\n [\n -74.92751168208186,\n 39.722640427523686\n ],\n [\n -74.92751168208186,\n 39.60993944176701\n ],\n [\n -74.7738739637236,\n 39.60993944176701\n ],\n [\n -74.7738739637236,\n 39.722640427523686\n ],\n [\n -74.92751168208186,\n 39.722640427523686\n ]\n ]\n ],\n \"type\": \"Polygon\"\n }\n }\n ]\n}","noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"4f4e49fae4b07f02db5f4351","contributors":{"authors":[{"text":"Fusillo, Thomas V.","contributorId":106097,"corporation":false,"usgs":true,"family":"Fusillo","given":"Thomas","email":"","middleInitial":"V.","affiliations":[],"preferred":false,"id":197749,"contributorType":{"id":1,"text":"Authors"},"rank":1}]}} ,{"id":49474,"text":"ofr81438 - 1981 - Single-channel seismic-reflection profiles and sidescan-sonar records collected on Georges Bank","interactions":[],"lastModifiedDate":"2024-05-22T20:45:24.410563","indexId":"ofr81438","displayToPublicDate":"1994-01-01T00:00:00","publicationYear":"1981","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":"81-438","title":"Single-channel seismic-reflection profiles and sidescan-sonar records collected on Georges Bank","docAbstract":"Subbottom seismic-reflection, echo-sounding, and sidescan-sonar records were collected by the U.S. Geological Survey during two cruises over Georges Bank aboard the R/V OCEANUS (cruise 056, March 6-15, 1979 and cruise 067, August 6-13, 1979) (fig. 1). The data collected during these two cruises contributed to a study of bed-form types and distribution and of sediment transport paths on Georges Bank.
The equipment used on these cruises consisted of an EG&G Uniboom 12-kHz echo-sounder, and Klein sidescan-sonar system. The Uniboom data were collected on the OCEANUS 067 cruise along 185 km of trackline (fig. 1), and the 12-kHz echo-sounder and sidescan-sonar data were collected during both cruises along 465 km of trackline.
Navigation during both cruises consisted of Loran-C fixes logged at least every 15 minutes. After the cruise, the navigation data were digitized and stored on magnetic tape.
The original records can be studied at the U.S. Geological Survey Data Library at Woods Hole, MA 02543. Microfilm copies of the subbottom, echo-sounding, and sidescan-sonar records can be purchased only from the National Geophysical and Solar-Terrestrial Data Center, NOAA/EDIS/NGSDC, Code D621, 325 Broadway, Boulder, CO 80303 (303-497-6338).
","language":"English","publisher":"U.S. Geological Survey","doi":"10.3133/ofr81438","usgsCitation":"Twichell, D.C., 1981, Single-channel seismic-reflection profiles and sidescan-sonar records collected on Georges Bank: U.S. Geological Survey Open-File Report 81-438, 6 p., https://doi.org/10.3133/ofr81438.","productDescription":"6 p.","costCenters":[],"links":[{"id":429171,"rank":2,"type":{"id":11,"text":"Document"},"url":"https://pubs.usgs.gov/of/1981/0438/report.pdf","linkFileType":{"id":1,"text":"pdf"}},{"id":170097,"rank":1,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/of/1981/0438/report-thumb.jpg"}],"country":"Canada, United States","otherGeospatial":"Georges Bank","geographicExtents":"{\n \"type\": \"FeatureCollection\",\n \"features\": [\n {\n \"type\": \"Feature\",\n \"properties\": {},\n \"geometry\": {\n \"coordinates\": [\n [\n [\n -71.42948334835658,\n 44.49353837387295\n ],\n [\n -71.42948334835658,\n 41.84744897972644\n ],\n [\n -64.59270246359314,\n 41.84744897972644\n ],\n [\n -64.59270246359314,\n 44.49353837387295\n ],\n [\n -71.42948334835658,\n 44.49353837387295\n ]\n ]\n ],\n \"type\": \"Polygon\"\n }\n }\n ]\n}","noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"4f4e49f6e4b07f02db5f17b7","contributors":{"authors":[{"text":"Twichell, David C.","contributorId":87481,"corporation":false,"usgs":true,"family":"Twichell","given":"David","email":"","middleInitial":"C.","affiliations":[],"preferred":false,"id":239708,"contributorType":{"id":1,"text":"Authors"},"rank":1}]}} ,{"id":10640,"text":"ofr81922 - 1981 - Hydrologic data for urban studies in the San Antonio, Texas, metropolitan area, 1978","interactions":[],"lastModifiedDate":"2022-11-16T19:38:09.654274","indexId":"ofr81922","displayToPublicDate":"1994-01-01T00:00:00","publicationYear":"1981","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":"81-922","title":"Hydrologic data for urban studies in the San Antonio, Texas, metropolitan area, 1978","docAbstract":"Hydrologic investigations of urban drainage basins in Texas were begun by the U.S. Geological Survey in 1954. These studies are now in progress in Austin, Houston, and San Antonio. Studies were completed in the Fort Worth metropolitan area at the end of the 1977 water year, and in the Dallas metropolitan area at the end of the 1979 water year.
The Geological Survey, in cooperation with the Texas Department of Water Resources, expanded the existing streamflow network in the San Antonio metropolitan area in May 1968 to begin urban hydrology studies in this area. In September 1968, the program was further expanded to include the collection of water-quality data.
","language":"English","publisher":"U.S. Geological Survey","doi":"10.3133/ofr81922","collaboration":"Prepared in cooperation with the Texas Department of Water Resources","usgsCitation":"Perez, R., 1981, Hydrologic data for urban studies in the San Antonio, Texas, metropolitan area, 1978: U.S. Geological Survey Open-File Report 81-922, 91 p., https://doi.org/10.3133/ofr81922.","productDescription":"91 p.","onlineOnly":"N","additionalOnlineFiles":"N","costCenters":[{"id":583,"text":"Texas Water Science Center","active":true,"usgs":true}],"links":[{"id":409400,"rank":2,"type":{"id":11,"text":"Document"},"url":"https://pubs.usgs.gov/of/1981/0922/report.pdf","linkFileType":{"id":1,"text":"pdf"}},{"id":144071,"rank":0,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/of/1981/0922/report-thumb.jpg"}],"country":"United States","state":"Texas","city":"San Antonio","geographicExtents":"{\n \"type\": \"FeatureCollection\",\n \"features\": [\n {\n \"type\": \"Feature\",\n \"properties\": {},\n \"geometry\": {\n \"type\": \"Polygon\",\n \"coordinates\": [\n [\n [\n -98.8165283203125,\n 29.123373210819224\n ],\n [\n -98.19580078125,\n 29.123373210819224\n ],\n [\n -98.19580078125,\n 29.699982298744377\n ],\n [\n -98.8165283203125,\n 29.699982298744377\n ],\n [\n -98.8165283203125,\n 29.123373210819224\n ]\n ]\n ]\n }\n }\n ]\n}","noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"4f4e4a1be4b07f02db6079f2","contributors":{"authors":[{"text":"Perez, Roberto","contributorId":97114,"corporation":false,"usgs":true,"family":"Perez","given":"Roberto","email":"","affiliations":[],"preferred":false,"id":161726,"contributorType":{"id":1,"text":"Authors"},"rank":1}]}} ,{"id":11195,"text":"ofr81801 - 1981 - Hydrogeologic data for Dawson, McCone, Prairie, and Richland counties, east-central Montana","interactions":[],"lastModifiedDate":"2012-02-02T00:06:38","indexId":"ofr81801","displayToPublicDate":"1994-01-01T00:00:00","publicationYear":"1981","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":"81-801","title":"Hydrogeologic data for Dawson, McCone, Prairie, and Richland counties, east-central Montana","language":"ENGLISH","publisher":"U.S. Geological Survey,","doi":"10.3133/ofr81801","usgsCitation":"Slagle, S.E., 1981, Hydrogeologic data for Dawson, McCone, Prairie, and Richland counties, east-central Montana: U.S. Geological Survey Open-File Report 81-801, iii, 104 p. ill., maps ;28 cm., https://doi.org/10.3133/ofr81801.","productDescription":"iii, 104 p. ill., maps ;28 cm.","costCenters":[],"links":[{"id":144715,"rank":0,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/of/1981/0801/report-thumb.jpg"},{"id":38957,"rank":400,"type":{"id":17,"text":"Plate"},"url":"https://pubs.usgs.gov/of/1981/0801/plate-1.pdf","linkFileType":{"id":1,"text":"pdf"}},{"id":38958,"rank":300,"type":{"id":11,"text":"Document"},"url":"https://pubs.usgs.gov/of/1981/0801/report.pdf","linkFileType":{"id":1,"text":"pdf"}}],"noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"4f4e4a50e4b07f02db628a96","contributors":{"authors":[{"text":"Slagle, Steven E.","contributorId":35284,"corporation":false,"usgs":true,"family":"Slagle","given":"Steven","email":"","middleInitial":"E.","affiliations":[],"preferred":false,"id":162708,"contributorType":{"id":1,"text":"Authors"},"rank":1}]}} ,{"id":10125,"text":"ofr81220 - 1981 - Potentially favorable areas for large-yield wells in the Red River Formation and Madison Limestone in parts of Montana, North Dakota, South Dakota, Wyoming, and Nebraska","interactions":[{"subject":{"id":10125,"text":"ofr81220 - 1981 - Potentially favorable areas for large-yield wells in the Red River Formation and Madison Limestone in parts of Montana, North Dakota, South Dakota, Wyoming, and Nebraska","indexId":"ofr81220","publicationYear":"1981","noYear":false,"title":"Potentially favorable areas for large-yield wells in the Red River Formation and Madison Limestone in parts of Montana, North Dakota, South Dakota, Wyoming, and Nebraska"},"predicate":"SUPERSEDED_BY","object":{"id":45714,"text":"pp1273E - 1983 - Potentially favorable areas for large-yield wells in the Red River Formation and Madison Limestone in parts of Montana, North Dakota, South Dakota, and Wyoming","indexId":"pp1273E","publicationYear":"1983","noYear":false,"chapter":"E","title":"Potentially favorable areas for large-yield wells in the Red River Formation and Madison Limestone in parts of Montana, North Dakota, South Dakota, and Wyoming"},"id":1}],"supersededBy":{"id":45714,"text":"pp1273E - 1983 - Potentially favorable areas for large-yield wells in the Red River Formation and Madison Limestone in parts of Montana, North Dakota, South Dakota, and Wyoming","indexId":"pp1273E","publicationYear":"1983","noYear":false,"title":"Potentially favorable areas for large-yield wells in the Red River Formation and Madison Limestone in parts of Montana, North Dakota, South Dakota, and Wyoming"},"lastModifiedDate":"2022-08-09T15:28:15.441093","indexId":"ofr81220","displayToPublicDate":"1994-01-01T00:00:00","publicationYear":"1981","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":"81-220","title":"Potentially favorable areas for large-yield wells in the Red River Formation and Madison Limestone in parts of Montana, North Dakota, South Dakota, Wyoming, and Nebraska","docAbstract":"The need for large quantities of energy has created interest in the Fort Union coal region of the Northern Great Plains. Extensive development of this coal, which may include onsite steam-power generation, gasification, liquefaction, and slurry-pipeline transport of the coal from this region, would place a heavy demand on the region's limited streamflow. Paleozoic rocks that underlie the Fort Union coal region and aquifers in these rocks, including the Red River Formation and the Madison Limestone, might supply, at least on a temporary basis, a significant part of the water required for coal development. The area of study covers approximately 200,000 square miles, and includes eastern Montana, western North Dakota and South Dakota, northeastern Wyoming, and northwestern Nebraska. This report, one of a series in the Madison Limestone study, uses hydrologic and geologic data to outline potentially favorable areas for well construction - that is, areas in which there is a good probability that large-yield wells (more than 500 gallons per minute) can be completed in the Red River Formation and in the Madison Limestone. Potentially favorable areas in terms of aquifer characteristics, for both the Red River Formation and the Madison Limestone, are given a numerical evaluation from 1 to 3 based on the number of the following criteria that are met: (1) the presence of more than 100 feet of relatively porous rock, (2) the presence of more than 100 feet of dolomite, and (3) the presence of known geologic structures which could affect yield. Areas rated 3 are those in which all three criteria are satisfied; areas rated 2 are those in which two criteria are satisfied; and areas rated 1 are those in which only one criterion is satisfied. The criteria selected for this analysis were chosen because they can be recognized and mapped over the entire study area. Local features such as minor structures, solution zones, and rock facies of small extent were not included in this regional evaluation. In addition, water quality was considered in a general way in defining the favorable areas, by excluding areas in which the electrical resistivity of formation water, as calculated from geophysical well logs, was less than 1 ohm-meter. The numerical scales of the Red River Formation and Madison Limestone are summed to show potentially favorable areas for the combined aquifers. Certain additional factors which may be important to a prospective water user were not included in the numerical ranking - these include depths to the two aquifers, calcite saturation, water temperature, total dissolved solids, and piezometric head in relation to land surface. For a complete evaluation, potential users should consider these factors plus local structures, facies, and solution zones in conjunction with the numerical rankings reflecting aquifer characteristics. To facilitate consideration of piezometric head, maps are included in this report showing areas in which the piezometric head falls in certain ranges with respect to land surface.
","language":"English","publisher":"U.S. Geological Survey","doi":"10.3133/ofr81220","usgsCitation":"MacCary, L., Cushing, E.M., and Brown, D.L., 1981, Potentially favorable areas for large-yield wells in the Red River Formation and Madison Limestone in parts of Montana, North Dakota, South Dakota, Wyoming, and Nebraska: U.S. Geological Survey Open-File Report 81-220, Report: vi, 29 p.; 1 Plate: 17.86 x 21.76 inches, https://doi.org/10.3133/ofr81220.","productDescription":"Report: vi, 29 p.; 1 Plate: 17.86 x 21.76 inches","costCenters":[],"links":[{"id":405012,"rank":3,"type":{"id":17,"text":"Plate"},"url":"https://pubs.usgs.gov/of/1981/0220/plate-1.pdf","linkFileType":{"id":1,"text":"pdf"}},{"id":405011,"rank":2,"type":{"id":11,"text":"Document"},"url":"https://pubs.usgs.gov/of/1981/0220/report.pdf","linkFileType":{"id":1,"text":"pdf"}},{"id":145531,"rank":0,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/of/1981/0220/report-thumb.jpg"}],"country":"United States","state":"Montana, Nebraska, North Dakota, South Dakota, Wyoming","geographicExtents":"{\n \"type\": \"FeatureCollection\",\n \"features\": [\n {\n \"type\": \"Feature\",\n \"properties\": {},\n \"geometry\": {\n \"type\": \"Polygon\",\n \"coordinates\": [\n [\n [\n -115.13671875,\n 40.111688665595956\n ],\n [\n -96.328125,\n 40.111688665595956\n ],\n [\n -96.328125,\n 49.03786794532644\n ],\n [\n -115.13671875,\n 49.03786794532644\n ],\n [\n -115.13671875,\n 40.111688665595956\n ]\n ]\n ]\n }\n }\n ]\n}","noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"4f4e4b1ae4b07f02db6a86be","contributors":{"authors":[{"text":"MacCary, L.M.","contributorId":13200,"corporation":false,"usgs":true,"family":"MacCary","given":"L.M.","email":"","affiliations":[],"preferred":false,"id":160852,"contributorType":{"id":1,"text":"Authors"},"rank":1},{"text":"Cushing, E. M.","contributorId":94273,"corporation":false,"usgs":true,"family":"Cushing","given":"E.","email":"","middleInitial":"M.","affiliations":[],"preferred":false,"id":160854,"contributorType":{"id":1,"text":"Authors"},"rank":2},{"text":"Brown, David L.","contributorId":55425,"corporation":false,"usgs":true,"family":"Brown","given":"David","email":"","middleInitial":"L.","affiliations":[],"preferred":false,"id":160853,"contributorType":{"id":1,"text":"Authors"},"rank":3}]}} ,{"id":25857,"text":"wri8111 - 1981 - Water-resources information for the Withlacoochee River region, west-central Florida","interactions":[],"lastModifiedDate":"2020-11-04T18:10:43.464809","indexId":"wri8111","displayToPublicDate":"1994-01-01T00:00:00","publicationYear":"1981","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":"81-11","title":"Water-resources information for the Withlacoochee River region, west-central Florida","docAbstract":"Daily water use in the Withlacoochee River region in 1977 averaged about 2,005 million gallons per day, 94 percent of which was saline surface water used in thermoelectric power-generation cooling. Industrial and irrigation uses required 73 percent of the freshwater. The largest user of freshwater was Hernando County, using 43.0 million gallons per day.
The ground-water system is comprised of up to three different aquifers--the surficial, the secondary artesian, and the Floridan. Little is known about the surficial and secondary artesian aquifers.
The Floridan aquifer consists mostly of limestones and dolomites, and is as much as 1,500 feet thick. Transmissivities are known to be as high as 25 million feet squared per day. Yields of 2,000 gallons per minute from 12-inch wells are possible. Although the range in fluctuations of the potentiometric surface is as great as 20 feet, no significant change has occurred since the 1930's when data were first collected.
The quality of water within the Floridan aquifer is generally excellent except near the Gulf Coast and in extreme east Marion County, near the St. Johns River where saltwater is present in the aquifer. Iron and hydrogen sulfide are sometimes a problem, but they can usually be con-trolled by proper well design and aeration of the water. Concentrations of sulfate do not exceed 250 milligrams per liter in the study area, and only in a small part of the area do dissolved-solids concentrations exceed 250 milligrams per liter.
Summaries were compiled of more than 1,000 wells, 43 continuous-record gaging stations, 21 lakes, and 46 springs. The predominant chemical type for both streams and springs is calcium and magnesium bicarbonate due to the dissolution process of the carbonate rocks. Along the coastal areas and near the St. Johns River, water is commonly of the sodium chloride type. The majority of the streams have average dissolved-solids concentrations between 100 and 200 milligrams per liter, maximum-observed specific conductance between 250 and 750 micro-mhos per centimeter, and average total nitrogen concentrations of less than 1.2 milligrams per liter.
Data for six lakes showed that the range of stage between the 90 and 10 percent exceedance stages is as great as 4.5 feet and as small as 2.2 feet. Little water-quality data for lakes are available, especially for the important constituents such as biochemical oxygen demand, total nitrogen, total phosphorus, and total carbon.
Flow-duration data for springs show small ranges in discharge. The differences between the 10 and 90 percent exceedance discharges are 350 cubic feet per second for Silver Springs and 280 cubic feet per second for Rainbow Springs, the two largest springs in the area. Water quality of the springs is relatively constant with time because of the water's long residence time within the carbonate rocks.
","language":"English","publisher":"U.S. Geological Survey","doi":"10.3133/wri8111","collaboration":"Prepared in cooperation with the U.S. Army Corps of Engineers","usgsCitation":"Miller, R.A., Anderson, W., Navoy, A.S., Smoot, J.L., and Belles, R.G., 1981, Water-resources information for the Withlacoochee River region, west-central Florida: U.S. Geological Survey Water-Resources Investigations Report 81-11, xi, 130 p., https://doi.org/10.3133/wri8111.","productDescription":"xi, 130 p.","costCenters":[],"links":[{"id":380157,"rank":2,"type":{"id":11,"text":"Document"},"url":"https://pubs.usgs.gov/wri/1981/0011/report.pdf","linkFileType":{"id":1,"text":"pdf"}},{"id":158287,"rank":0,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/wri/1981/0011/report-thumb.jpg"}],"country":"United States","state":"Florida","otherGeospatial":"Withlacoochee River region","geographicExtents":"{\n \"type\": \"FeatureCollection\",\n \"features\": [\n {\n \"type\": \"Feature\",\n \"properties\": {},\n \"geometry\": {\n \"type\": \"Polygon\",\n \"coordinates\": [\n [\n [\n -83.5894775390625,\n 28.434883464940082\n ],\n [\n -81.54052734375,\n 28.434883464940082\n ],\n [\n -81.54052734375,\n 29.82158272057499\n ],\n [\n -83.5894775390625,\n 29.82158272057499\n ],\n [\n -83.5894775390625,\n 28.434883464940082\n ]\n ]\n ]\n }\n }\n ]\n}","noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"4f4e4a08e4b07f02db5f9d16","contributors":{"authors":[{"text":"Miller, Robert A.","contributorId":52938,"corporation":false,"usgs":true,"family":"Miller","given":"Robert","email":"","middleInitial":"A.","affiliations":[],"preferred":false,"id":195369,"contributorType":{"id":1,"text":"Authors"},"rank":1},{"text":"Anderson, Warren","contributorId":7712,"corporation":false,"usgs":true,"family":"Anderson","given":"Warren","affiliations":[],"preferred":false,"id":195367,"contributorType":{"id":1,"text":"Authors"},"rank":2},{"text":"Navoy, Anthony S. anavoy@usgs.gov","contributorId":2464,"corporation":false,"usgs":true,"family":"Navoy","given":"Anthony","email":"anavoy@usgs.gov","middleInitial":"S.","affiliations":[],"preferred":true,"id":195365,"contributorType":{"id":1,"text":"Authors"},"rank":3},{"text":"Smoot, James L.","contributorId":13605,"corporation":false,"usgs":true,"family":"Smoot","given":"James","email":"","middleInitial":"L.","affiliations":[],"preferred":false,"id":195368,"contributorType":{"id":1,"text":"Authors"},"rank":4},{"text":"Belles, Roger G.","contributorId":6423,"corporation":false,"usgs":true,"family":"Belles","given":"Roger","email":"","middleInitial":"G.","affiliations":[],"preferred":false,"id":195366,"contributorType":{"id":1,"text":"Authors"},"rank":5}]}} ,{"id":47186,"text":"ofr801283 - 1981 - Floods of September 16, 1975 in the Tallaboa Valley, Puerto Rico","interactions":[],"lastModifiedDate":"2018-12-19T08:49:28","indexId":"ofr801283","displayToPublicDate":"1994-01-01T00:00:00","publicationYear":"1981","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":"80-1283","title":"Floods of September 16, 1975 in the Tallaboa Valley, Puerto Rico","docAbstract":"This report provides a record of the flood of September 16, 1975, and associated hydrologic data. These data can be used in making rational decisions in formulating effective flood-plain regulations that would minimize flood problems in the Tallaboa Valley.
The Tallaboa Valley (fig. 1) lies on the southwestern coast of Puerto Rico about 12 km (7.5 mi) west of the city of Ponce. The climate is semiarid with a mean annual precipitation of about 1,020 mm (40 in). It is a relatively small valley which until the late fifties was dedicated mainly to the product ion of sugarcane. Since then, the economy started changing from agriculture to industry. At present the lower part of the valley is completely industrialized. The upper part of the valley is used for agriculture--mostly as pastureland. The reach from Highway 132 downstream to the new Highway 2 is mainly agricultural with a few scattered communities. The lower part of the valley that includes the area from the Highway 2 bridge to the mouth is covered with heavy industry concerned with the refinement of oil, and associated industries.
The continuous growth of industry and consequently of the urban area of Peñuelas has encouraged growth onto the
flood plain. The study area is subject to flooding by the Rio Tallaboa and the Rio Guayanes, its main tributary. The Rio Guayanes is the- cause of flooding in the urban area of Penuelas, encompassing the reach from the northern edge of town downstream to Highway 132 where it joins the Rio Tallaboa.
Data are generally referred to in SI (International System) units followed by corresponding inch-pound units in parentheses. The SI units.may be converted to inch-pound units by multiplying the units given by the factors shown.
","language":"English","publisher":"U.S. Geological Survey","doi":"10.3133/ofr801283","usgsCitation":"Johnson, K.G., 1981, Floods of September 16, 1975 in the Tallaboa Valley, Puerto Rico (WRI/OFR): U.S. Geological Survey Open-File Report 80-1283, 5 Plates: 17.00 x 22.00 inches, https://doi.org/10.3133/ofr801283.","productDescription":"5 Plates: 17.00 x 22.00 inches","costCenters":[],"links":[{"id":360545,"rank":2,"type":{"id":17,"text":"Plate"},"url":"https://pubs.usgs.gov/of/1980/1283/plate-1.pdf","linkFileType":{"id":1,"text":"pdf"}},{"id":360546,"rank":3,"type":{"id":17,"text":"Plate"},"url":"https://pubs.usgs.gov/of/1980/1283/plate-2.pdf","linkFileType":{"id":1,"text":"pdf"}},{"id":360547,"rank":4,"type":{"id":17,"text":"Plate"},"url":"https://pubs.usgs.gov/of/1980/1283/plate-3.pdf","linkFileType":{"id":1,"text":"pdf"}},{"id":135211,"rank":0,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/of/1980/1283/report-thumb.jpg"},{"id":360548,"rank":5,"type":{"id":17,"text":"Plate"},"url":"https://pubs.usgs.gov/of/1980/1283/plate-4.pdf","linkFileType":{"id":1,"text":"pdf"}},{"id":360549,"rank":6,"type":{"id":17,"text":"Plate"},"url":"https://pubs.usgs.gov/of/1980/1283/plate-5.pdf","linkFileType":{"id":1,"text":"pdf"}}],"state":"Puerto Rico","otherGeospatial":"Tallaboa Valley","geographicExtents":"{\n \"type\": \"FeatureCollection\",\n \"features\": [\n {\n \"type\": \"Feature\",\n \"properties\": {},\n \"geometry\": {\n \"type\": \"Polygon\",\n \"coordinates\": [\n [\n [\n -66.7690658569336,\n 17.96567026450932\n ],\n [\n -66.67808532714842,\n 17.96567026450932\n ],\n [\n -66.67808532714842,\n 18.116160664342022\n ],\n [\n -66.7690658569336,\n 18.116160664342022\n ],\n [\n -66.7690658569336,\n 17.96567026450932\n ]\n ]\n ]\n }\n }\n ]\n}","edition":"WRI/OFR","noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"4f4e49d8e4b07f02db5df88c","contributors":{"authors":[{"text":"Johnson, Karl G.","contributorId":7680,"corporation":false,"usgs":true,"family":"Johnson","given":"Karl","email":"","middleInitial":"G.","affiliations":[],"preferred":false,"id":234791,"contributorType":{"id":1,"text":"Authors"},"rank":1}]}} ,{"id":10023,"text":"ofr81326 - 1981 - Selected drill-stem-test data from the Northern Great Plains area of Montana","interactions":[],"lastModifiedDate":"2012-02-02T00:06:31","indexId":"ofr81326","displayToPublicDate":"1994-01-01T00:00:00","publicationYear":"1981","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":"81-326","title":"Selected drill-stem-test data from the Northern Great Plains area of Montana","docAbstract":"Selected drill-stem-test data were collected for use in the hydrologic analysis of aquifers in the northern Great Plains area of Montana. To supplement existing data defining the potentiometric surface of various aquifers, shut-in pressures recorded during drill-stem tests of oil and gas test wells were used to calculate the altitude of the potentiometric surface. The transmissivity of the aquifers also was calculated if sufficient data existed. Records for 627 drill-stem tests from 523 wells are tabulated in this report. Data include well location, well name, formation tested, well epth, tested interval, date tested, test number, flow period, transmissivity, shut-in pressure, and altitude of water surface. Locations of the wells are shown on a map at a scale of 1:1,000,000. (USGS)","language":"ENGLISH","publisher":"U.S. Geological Survey,","doi":"10.3133/ofr81326","usgsCitation":"Levings, G., 1981, Selected drill-stem-test data from the Northern Great Plains area of Montana: U.S. Geological Survey Open-File Report 81-326, iii, 23 p., 1 over-size sheet; 26 cm., https://doi.org/10.3133/ofr81326.","productDescription":"iii, 23 p., 1 over-size sheet; 26 cm.","costCenters":[],"links":[{"id":143857,"rank":0,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/of/1981/0326/report-thumb.jpg"},{"id":37861,"rank":400,"type":{"id":17,"text":"Plate"},"url":"https://pubs.usgs.gov/of/1981/0326/plate-1.pdf","linkFileType":{"id":1,"text":"pdf"}},{"id":37862,"rank":300,"type":{"id":11,"text":"Document"},"url":"https://pubs.usgs.gov/of/1981/0326/report.pdf","linkFileType":{"id":1,"text":"pdf"}}],"noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"4f4e4a08e4b07f02db5fa5c4","contributors":{"authors":[{"text":"Levings, Gary W.","contributorId":106889,"corporation":false,"usgs":true,"family":"Levings","given":"Gary W.","affiliations":[],"preferred":false,"id":160689,"contributorType":{"id":1,"text":"Authors"},"rank":1}]}} ,{"id":10024,"text":"ofr81534 - 1981 - Selected hydrogeologic data from the Northern Great Plains area of Montana","interactions":[],"lastModifiedDate":"2012-02-02T00:06:31","indexId":"ofr81534","displayToPublicDate":"1994-01-01T00:00:00","publicationYear":"1981","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":"81-534","title":"Selected hydrogeologic data from the Northern Great Plains area of Montana","docAbstract":"Selected hydrologic data have been used in a 4-year study of aquifers of Cenozoic and Mesozoic age in the northern Great Plains to define the hydrologic system and to generate hydrologic maps. Records of 6,754 wells and 188 springs are tabulated in the report. The well data include site location, county, date completed, depth of well, casing diameter, type of lift, use of water, principal aquifer, altitude of land surface, water level, discharge, specific capacity, specific conductance, and water temperature. The spring data include site location, county, use of water, principal aquifer, altitude of land surface, type of spring, discharge, date discharge measured, specific conductance, and water temperature. Locations of the wells and springs are shown on a map at a scale of 1:1,000,000. (USGS)","language":"ENGLISH","publisher":"U.S. Geological Survey,","doi":"10.3133/ofr81534","usgsCitation":"Levings, G., 1981, Selected hydrogeologic data from the Northern Great Plains area of Montana: U.S. Geological Survey Open-File Report 81-534, iii, 244 p., 1 over-size sheet ;28 cm., https://doi.org/10.3133/ofr81534.","productDescription":"iii, 244 p., 1 over-size sheet ;28 cm.","costCenters":[],"links":[{"id":143878,"rank":0,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/of/1981/0534/report-thumb.jpg"},{"id":37863,"rank":400,"type":{"id":17,"text":"Plate"},"url":"https://pubs.usgs.gov/of/1981/0534/plate-1.pdf","linkFileType":{"id":1,"text":"pdf"}},{"id":37864,"rank":300,"type":{"id":11,"text":"Document"},"url":"https://pubs.usgs.gov/of/1981/0534/report.pdf","linkFileType":{"id":1,"text":"pdf"}}],"noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"4f4e4a07e4b07f02db5f93cd","contributors":{"authors":[{"text":"Levings, Gary W.","contributorId":106889,"corporation":false,"usgs":true,"family":"Levings","given":"Gary W.","affiliations":[],"preferred":false,"id":160690,"contributorType":{"id":1,"text":"Authors"},"rank":1}]}} ,{"id":11090,"text":"ofr8192 - 1981 - Cooperative tectonic studies from seismic network in central Italy","interactions":[],"lastModifiedDate":"2025-09-15T13:35:14.292268","indexId":"ofr8192","displayToPublicDate":"1994-01-01T00:00:00","publicationYear":"1981","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":"81-92","title":"Cooperative tectonic studies from seismic network in central Italy","docAbstract":"The purpose of the subject contract work was to explore the possibility of tectonic research-work based on seismic data from a local network carried out as a cooperative effort between the Institute Nazionale di Geofisica (ING), Rome, and Columbia University (L-DGO), New York. This effort has been rather successful, and we hope to be able to continue this collaboration in the future.
","language":"English","publisher":"U.S. Geological Survey","doi":"10.3133/ofr8192","usgsCitation":"Seeber, L., and Scholz, C., 1981, Cooperative tectonic studies from seismic network in central Italy: U.S. Geological Survey Open-File Report 81-92, 37 p., https://doi.org/10.3133/ofr8192.","productDescription":"37 p.","costCenters":[],"links":[{"id":495481,"rank":2,"type":{"id":11,"text":"Document"},"url":"https://pubs.usgs.gov/of/1981/0092/report.pdf","linkFileType":{"id":1,"text":"pdf"}},{"id":143287,"rank":1,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/of/1981/0092/report-thumb.jpg"}],"country":"Italy","geographicExtents":"{\n \"type\": \"FeatureCollection\",\n \"features\": [\n {\n \"type\": \"Feature\",\n \"properties\": {},\n \"geometry\": {\n \"coordinates\": [\n [\n [\n 4.554081425373113,\n 47.058493865117384\n ],\n [\n 4.554081425373113,\n 34.76766728148691\n ],\n [\n 18.935068554332958,\n 34.76766728148691\n ],\n [\n 18.935068554332958,\n 47.058493865117384\n ],\n [\n 4.554081425373113,\n 47.058493865117384\n ]\n ]\n ],\n \"type\": \"Polygon\"\n }\n }\n ]\n}","noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"4f4e4adce4b07f02db68640c","contributors":{"authors":[{"text":"Seeber, L.","contributorId":37329,"corporation":false,"usgs":true,"family":"Seeber","given":"L.","email":"","affiliations":[],"preferred":false,"id":162515,"contributorType":{"id":1,"text":"Authors"},"rank":1},{"text":"Scholz, C.H.","contributorId":85595,"corporation":false,"usgs":true,"family":"Scholz","given":"C.H.","email":"","affiliations":[],"preferred":false,"id":162516,"contributorType":{"id":1,"text":"Authors"},"rank":2}]}} ,{"id":10784,"text":"ofr8149 - 1981 - Current meter observations within lower Cook Inlet, Alaska, 1978-1979 from the R/V Sea Sounder, Pacific-Arctic Branch, U.S. Geological Survey","interactions":[],"lastModifiedDate":"2024-01-24T20:28:51.153141","indexId":"ofr8149","displayToPublicDate":"1994-01-01T00:00:00","publicationYear":"1981","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":"81-49","title":"Current meter observations within lower Cook Inlet, Alaska, 1978-1979 from the R/V Sea Sounder, Pacific-Arctic Branch, U.S. Geological Survey","docAbstract":"The U.S. Geological Survey under contract to the U.S. Bureau of Land Management conducted geo-environmental hazard studies within lower Cook Inlet, Alaska from 1975 through 1979 (Bouma and Hampton, 1976; Bouma and others, 1977 a,b, 1978 ; Hampton and Bouma 1979). As part of this effort the U.S. Geological Survey research vessel, R/V SEA SOUNDER, conducted two cruises in 1978 and one cruise in 1979 (Table 1). A number of stations were occupied for various periods of time (Fig. 1) during which tidal current speed and direction data was recorded. Some 1978 data was obtained concurrently with bottom boundary layer experiments conducted with a large instrumented tripod system referred to as GEOPROBE (Cacchione and Drake, 1979).
","language":"English","publisher":"U.S. Geological Survey","doi":"10.3133/ofr8149","usgsCitation":"Rappeport, M., 1981, Current meter observations within lower Cook Inlet, Alaska, 1978-1979 from the R/V Sea Sounder, Pacific-Arctic Branch, U.S. Geological Survey: U.S. Geological Survey Open-File Report 81-49, 78 p., https://doi.org/10.3133/ofr8149.","productDescription":"78 p.","costCenters":[],"links":[{"id":145096,"rank":1,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/of/1981/0049/report-thumb.jpg"},{"id":424898,"rank":3,"type":{"id":11,"text":"Document"},"url":"https://pubs.usgs.gov/of/1981/0049/report.pdf","linkFileType":{"id":1,"text":"pdf"}},{"id":391960,"rank":2,"type":{"id":36,"text":"NGMDB Index Page"},"url":"https://ngmdb.usgs.gov/Prodesc/proddesc_12050.htm"}],"country":"United States","state":"Alaska","otherGeospatial":"lower Cook Inlet","geographicExtents":"{\n \"type\": \"FeatureCollection\",\n \"features\": [\n {\n \"type\": \"Feature\",\n \"properties\": {},\n \"geometry\": {\n \"coordinates\": [\n [\n [\n -154.21122119264936,\n 60.48960645459513\n ],\n [\n -154.21122119264936,\n 58.72825698877193\n ],\n [\n -151.51638403220534,\n 58.72825698877193\n ],\n [\n -151.51638403220534,\n 60.48960645459513\n ],\n [\n -154.21122119264936,\n 60.48960645459513\n ]\n ]\n ],\n \"type\": \"Polygon\"\n }\n }\n ]\n}","noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"4f4e4ab2e4b07f02db66ec85","contributors":{"authors":[{"text":"Rappeport, M.L.","contributorId":48157,"corporation":false,"usgs":true,"family":"Rappeport","given":"M.L.","email":"","affiliations":[],"preferred":false,"id":161956,"contributorType":{"id":1,"text":"Authors"},"rank":1}]}} ,{"id":38605,"text":"pp1225 - 1981 - Petrogenetic modeling of a potential uranium source rock, Granite Mountains, Wyoming","interactions":[],"lastModifiedDate":"2012-02-02T00:10:17","indexId":"pp1225","displayToPublicDate":"1994-01-01T00:00:00","publicationYear":"1981","noYear":false,"publicationType":{"id":18,"text":"Report"},"publicationSubtype":{"id":5,"text":"USGS Numbered Series"},"seriesTitle":{"id":331,"text":"Professional Paper","code":"PP","onlineIssn":"2330-7102","printIssn":"1044-9612","active":true,"publicationSubtype":{"id":5}},"seriesNumber":"1225","title":"Petrogenetic modeling of a potential uranium source rock, Granite Mountains, Wyoming","docAbstract":"Previous studies of the granite of Lankin Dome have led to the conclusion that this granite was a source for the sandstone-type uranium deposits in the basins that surround the Granite Mountains, Wyo. Q-mode factor analysis of 29 samples of this granite shows that five bulk compositions are required to explain the observed variances of 33 constituents in these samples. Models presented in this paper show that the origin of the granite can be accounted for by the mixing of a starting liquid with two ranges of solid compositions such that all five compositions are granitic. \r\n\r\nThere are several features of the granite of Lankin Dome that suggest derivation by partial melting and, because the proposed source region was inhomogeneous, that more than one of the five end members may have been a liquid. Data for the granite are compatible with derivation from rocks similar to those of the metamorphic complex that the granite intrudes. Evidence for crustal derivation by partial melting includes a strongly peraluminous nature, extremely high differentiation indices, high contents of incompatible elements, generally large negative Eu anomalies, and high initial lead and strontium isotopic ratios. If the granite of Lankin Dome originated by partial melting of a heterogeneous metamorphic complex, the initial magma could reasonably have been composed of a range of granitic liquids. \r\n\r\nFive variables were not well accounted for by a five-end-member model. Water, CO 2 , and U0 2 contents and the oxidation state of iron are all subject to variations caused by near-surface processes. The Q-mode factor analysis suggests that these four variables have a distribution determined by postmagmatic processes. The reason for failure of Cs0 2 to vary systematically with the other 33 variables is not known. Other granites that have lost large amounts of uranium possibly can be identified by Q-mode factor analysis.","language":"ENGLISH","doi":"10.3133/pp1225","usgsCitation":"Stuckless, J., and Miesch, A., 1981, Petrogenetic modeling of a potential uranium source rock, Granite Mountains, Wyoming: U.S. Geological Survey Professional Paper 1225, 34 p., https://doi.org/10.3133/pp1225.","productDescription":"34 p.","costCenters":[],"links":[{"id":170415,"rank":0,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/pp/1225/report-thumb.jpg"},{"id":65424,"rank":300,"type":{"id":11,"text":"Document"},"url":"https://pubs.usgs.gov/pp/1225/report.pdf","linkFileType":{"id":1,"text":"pdf"}}],"noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"4f4e4a81e4b07f02db649ee2","contributors":{"authors":[{"text":"Stuckless, J. S.","contributorId":6060,"corporation":false,"usgs":true,"family":"Stuckless","given":"J. S.","affiliations":[],"preferred":false,"id":220153,"contributorType":{"id":1,"text":"Authors"},"rank":1},{"text":"Miesch, A.T.","contributorId":88726,"corporation":false,"usgs":true,"family":"Miesch","given":"A.T.","affiliations":[],"preferred":false,"id":220154,"contributorType":{"id":1,"text":"Authors"},"rank":2}]}} ,{"id":11524,"text":"ofr81912 - 1981 - Flood peaks and discharge summaries in the Delaware River basin","interactions":[],"lastModifiedDate":"2022-11-09T18:25:58.16339","indexId":"ofr81912","displayToPublicDate":"1994-01-01T00:00:00","publicationYear":"1981","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":"81-912","title":"Flood peaks and discharge summaries in the Delaware River basin","docAbstract":"Streamflow data from 299 continuous and crest-stage sites in the Delaware River basin are summarized in this report. The location, drainage area, period of record, type of gage, and average discharge for each gaging site are given. Also included are tables of annual peaks and peaks above base, annual and monthly means, and annual and monthly runoff.
The Troublesome Roadless Area is composed of six tracts of land and contains 2,943 acres (fig. 1). The largest tract of the study area, located 13 mi southwest of Stearns, Ky., is accessible from that town via State Route 92 to Hill Top, and . then southwestwatd along country roads. Unimproved Forest Service roads, abandoned logging roads, and primitive trails provide access by foot or horseback into the interior of each tract of the study area.
Physiographically, the Troublesome Roadless Area is in the Cumberland Plateau section of the Appalachian Plateaus Province and is near the western edge of the Appalachian coal region. The topography is typical of the Cumberland Plateau section, characterized by irregular, narrow-crested ridges, deep narrow canyons, and a dendritic drainage pattern. Troublesome Creek, a small tributary of the South Fork of the Cumberland River, is the source of the area name (fig. 2). Altitudes range from about 1,600 ft on Laurel Ridge in the largest tract to approximately 800 ft along the South Fork of the Cumberland River.
Field investigations by personnel of the U.S. Geological Survey consisted of reconnaissance geologic studies and data collecting, including the measurement of stratigraphic sections and the mapping of poorly exposed coal beds and resistant sandstone units. Additional subsurface information was obtained by studying and interpreting the logs of several coreholes drilled near the study area.
","language":"English","publisher":"U.S. Geological Survey","doi":"10.3133/mf1341A","usgsCitation":"Sigleo, W.R., and Randall, A.H., 1981, Geologic map of the Troublesome Roadless Area, McCreary County, Kentucky: U.S. Geological Survey Miscellaneous Field Studies Map 1341, 1 Plate: 32.14 x 21.74 inches, https://doi.org/10.3133/mf1341A.","productDescription":"1 Plate: 32.14 x 21.74 inches","costCenters":[],"links":[{"id":180269,"rank":1,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/mf/1341-A/report-thumb.jpg"},{"id":358633,"rank":2,"type":{"id":17,"text":"Plate"},"url":"https://pubs.usgs.gov/mf/1341-A/plate-1.pdf","linkFileType":{"id":1,"text":"pdf"}},{"id":496033,"rank":3,"type":{"id":36,"text":"NGMDB Index Page"},"url":"https://ngmdb.usgs.gov/Prodesc/proddesc_6985.htm","linkFileType":{"id":5,"text":"html"}}],"country":"United States","state":"Kentucky","county":"McCreary County","otherGeospatial":"Troublesome Roadless Area","geographicExtents":"{\n \"type\": \"FeatureCollection\",\n \"features\": [\n {\n \"type\": \"Feature\",\n \"properties\": {},\n \"geometry\": {\n \"type\": \"Polygon\",\n \"coordinates\": [\n [\n [\n -84.75,\n 36.5833\n ],\n [\n -84.75,\n 36.667\n ],\n [\n -84.5833,\n 36.667\n ],\n [\n -84.5833,\n 36.5833\n ],\n [\n -84.75,\n 36.5833\n ]\n ]\n ]\n }\n }\n ]\n}","noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"4f4e4ae4e4b07f02db68a398","contributors":{"authors":[{"text":"Sigleo, W. R.","contributorId":74070,"corporation":false,"usgs":true,"family":"Sigleo","given":"W.","email":"","middleInitial":"R.","affiliations":[],"preferred":false,"id":264563,"contributorType":{"id":1,"text":"Authors"},"rank":1},{"text":"Randall, A. H.","contributorId":7564,"corporation":false,"usgs":true,"family":"Randall","given":"A.","middleInitial":"H.","affiliations":[],"preferred":false,"id":264562,"contributorType":{"id":1,"text":"Authors"},"rank":2}]}} ,{"id":8876,"text":"ofr81482 - 1981 - Drainage areas of selected surface-water sites in Florida","interactions":[{"subject":{"id":23049,"text":"ofr80957 - 1980 - Drainage areas of selected surface-water sites in Florida","indexId":"ofr80957","publicationYear":"1980","noYear":false,"title":"Drainage areas of selected surface-water sites in Florida"},"predicate":"SUPERSEDED_BY","object":{"id":8876,"text":"ofr81482 - 1981 - Drainage areas of selected surface-water sites in Florida","indexId":"ofr81482","publicationYear":"1981","noYear":false,"title":"Drainage areas of selected surface-water sites in Florida"},"id":1}],"lastModifiedDate":"2022-08-11T14:01:32.365963","indexId":"ofr81482","displayToPublicDate":"1994-01-01T00:00:00","publicationYear":"1981","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":"81-482","title":"Drainage areas of selected surface-water sites in Florida","docAbstract":"Drainage areas for about 1,600 surface-water sites on streams and lakes in Florida are contained in this report. The sites are generally either U.S. Geological Survey gaging stations or the mouths of gaged streams. Each site is identified by latitude and longitude, by the general stream type, and by the U.S. Geological Survey 7 1/2-minute topographic map on which it can be located. The gaging stations are further identified by a downstream order number, a county code, and a nearby city or town. In addition to drainage areas, the surface areas of lakes are shown for the elevation given on the topographic map. These data were retrieved from the Surface Water Index developed and maintained by the Hydrologic Surveillance Section of the Florida District Office, U.S. Geological Survey.
","language":"English","publisher":"U.S. Geological Survey","doi":"10.3133/ofr81482","collaboration":"Prepared in cooperation with the Florida Department of Environmental Regulation","usgsCitation":"Foose, D.W., 1981, Drainage areas of selected surface-water sites in Florida: U.S. Geological Survey Open-File Report 81-482, Report: v, 83 p.; 2 Plates: 21.52 x 31.90 inches and 31.88 x 21.92 inches, https://doi.org/10.3133/ofr81482.","productDescription":"Report: v, 83 p.; 2 Plates: 21.52 x 31.90 inches and 31.88 x 21.92 inches","costCenters":[],"links":[{"id":142632,"rank":0,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/of/1981/0482/report-thumb.jpg"},{"id":405078,"rank":2,"type":{"id":11,"text":"Document"},"url":"https://pubs.usgs.gov/of/1981/0482/report.pdf","linkFileType":{"id":1,"text":"pdf"}},{"id":405079,"rank":4,"type":{"id":17,"text":"Plate"},"url":"https://pubs.usgs.gov/of/1981/0482/plate-1-2.pdf","text":"Plate 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\"}}]}","noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"4f4e4a61e4b07f02db635efe","contributors":{"authors":[{"text":"Foose, Donald W.","contributorId":85144,"corporation":false,"usgs":true,"family":"Foose","given":"Donald","email":"","middleInitial":"W.","affiliations":[],"preferred":false,"id":158472,"contributorType":{"id":1,"text":"Authors"},"rank":1}]}} ,{"id":30025,"text":"wri8144 - 1981 - Erodibility of selected soils and estimates of sediment yields in the San Juan Basin, New Mexico","interactions":[],"lastModifiedDate":"2019-08-05T11:51:47","indexId":"wri8144","displayToPublicDate":"1994-01-01T00:00:00","publicationYear":"1981","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":"81-44","title":"Erodibility of selected soils and estimates of sediment yields in the San Juan Basin, New Mexico","docAbstract":"Onsite rainfall-simulation experiments were conducted to derive field-erodibility indexes for rangeland soils and soils disturbed by mining in coal fields of northwestern New Mexico. Mean indexes on rangeland soils range from 0 grams (of detached soil) on dune soil to 121 grams on wash-transport zones. Mean field-erodibility-index values of soils disturbed by mining range from 16 to 32 grams; they can be extrapolted to nearby coal fields where future mining is expected. Because field-erodibility-index data allow differentiation of erodibilities across a variable landscape, these indexes were used to adjust values of K, the erodibility factor of the Universal Soil Loss Equation. Estimates of soil loss and sediment yield were then calculated for a small basin following mining. (USGS)","language":"English","publisher":"U.S. Geological Survey","publisherLocation":"Reston, VA","doi":"10.3133/wri8144","usgsCitation":"Summer, R.M., 1981, Erodibility of selected soils and estimates of sediment yields in the San Juan Basin, New Mexico: U.S. Geological Survey Water-Resources Investigations Report 81-44, v, 33 p. , https://doi.org/10.3133/wri8144.","productDescription":"v, 33 p. ","costCenters":[],"links":[{"id":366264,"rank":2,"type":{"id":11,"text":"Document"},"url":"https://pubs.usgs.gov/wri/1981/0044/report.pdf","linkFileType":{"id":1,"text":"pdf"}},{"id":160083,"rank":0,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/wri/1981/0044/report-thumb.jpg"}],"country":"United States","state":"New Mexico","otherGeospatial":"San Juan Basin","geographicExtents":"{\n \"type\": \"FeatureCollection\",\n \"features\": [\n {\n \"type\": \"Feature\",\n \"properties\": {},\n \"geometry\": {\n \"type\": \"Polygon\",\n \"coordinates\": [\n [\n [\n -107.26638793945312,\n 36.771892444961026\n ],\n [\n -107.20733642578125,\n 36.771892444961026\n ],\n [\n -107.20733642578125,\n 36.82357691815722\n ],\n [\n -107.26638793945312,\n 36.82357691815722\n ],\n [\n -107.26638793945312,\n 36.771892444961026\n ]\n ]\n ]\n }\n }\n ]\n}","noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"4f4e4a0ee4b07f02db5fe05d","contributors":{"authors":[{"text":"Summer, Rebecca M.","contributorId":21592,"corporation":false,"usgs":true,"family":"Summer","given":"Rebecca","email":"","middleInitial":"M.","affiliations":[],"preferred":false,"id":202550,"contributorType":{"id":1,"text":"Authors"},"rank":1}]}} ,{"id":11701,"text":"ofr81544 - 1981 - Proposed observation-well network and ground-water level program for North Carolina","interactions":[],"lastModifiedDate":"2022-08-15T18:25:32.76623","indexId":"ofr81544","displayToPublicDate":"1994-01-01T00:00:00","publicationYear":"1981","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":"81-544","title":"Proposed observation-well network and ground-water level program for North Carolina","docAbstract":"An initial system of 223 observation wells is proposed for monitoring ground-water levels in North Carolina. These wells are suggested to replace and upgrade nearly 650 observation wells currently measured in separate State and Federal programs, and are arranged in four groups or networks each having specific objectives. These groups are (1) a climatic-effects network, (2) a terrane-effects network, (3) a local-effects network, and (4) an areal-effects network. Recommendations are also made regarding additional observation-well coverage in some areas of the State.
Records-review and network-review procedures constituted the largest amount of effort in this study and required a considerable amount of organization to keep track of well records and water-level data. These procedures are outlined in this report as a guide for those who are contemplating an observation-well program review.
The report also contains suggested organizational contents of a data file, including procedures for records processing, and various forms used to document the review and data-collection efforts.
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D. Jr.","contributorId":51766,"corporation":false,"usgs":true,"family":"Winner","given":"M.","suffix":"Jr.","email":"","middleInitial":"D.","affiliations":[],"preferred":false,"id":163591,"contributorType":{"id":1,"text":"Authors"},"rank":1}]}} ,{"id":11308,"text":"ofr81812 - 1981 - Quality of surface water in the coal-mining areas of western Maryland and adjacent areas of Pennsylvania and West Virginia from April 1979 to June 1980","interactions":[],"lastModifiedDate":"2022-11-07T22:29:13.498675","indexId":"ofr81812","displayToPublicDate":"1994-01-01T00:00:00","publicationYear":"1981","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":"81-812","title":"Quality of surface water in the coal-mining areas of western Maryland and adjacent areas of Pennsylvania and West Virginia from April 1979 to June 1980","docAbstract":"The U.S. Geological Survey is studying the water quality of streams within the Eastern Coal Province. This report contains streamflow, water-quality, and biologic data collected in the North Branch Potomac River basin and in the Maryland portion of the Youghiogheny and Casselman River basins. Data collected from 64 streams from April 1979 to June 1980 are presented in tables. Other sources of hydrologic information within the study area are also described in the report.
","language":"English","publisher":"U.S. Geological Survey","doi":"10.3133/ofr81812","usgsCitation":"Staubitz, W., 1981, Quality of surface water in the coal-mining areas of western Maryland and adjacent areas of Pennsylvania and West Virginia from April 1979 to June 1980: U.S. Geological Survey Open-File Report 81-812, iv, 103 p., https://doi.org/10.3133/ofr81812.","productDescription":"iv, 103 p.","costCenters":[],"links":[{"id":143474,"rank":0,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/of/1981/0812/report-thumb.jpg"},{"id":409212,"rank":2,"type":{"id":11,"text":"Document"},"url":"https://pubs.usgs.gov/of/1981/0812/report.pdf","linkFileType":{"id":1,"text":"pdf"}}],"country":"United States","state":"Maryland, Pennsylvania, West Virginia","geographicExtents":"{\n \"type\": \"FeatureCollection\",\n \"features\": [\n {\n \"type\": \"Feature\",\n \"properties\": {},\n \"geometry\": {\n \"coordinates\": [\n [\n -80.28969170041603,\n 41.89312615647518\n ],\n [\n -82.50936322022069,\n 38.306922117041694\n ],\n [\n -81.87319966505842,\n 37.311317980188036\n ],\n [\n -80.48521218516676,\n 37.32781296260528\n ],\n [\n -78.30298308186588,\n 39.16876312477416\n ],\n [\n -76.40776015918033,\n 38.18999381427713\n ],\n [\n -75.87887149040306,\n 39.99967118674675\n ],\n [\n -75.08277036724041,\n 40.35794926140315\n ],\n [\n -74.96065268678905,\n 41.64102498519725\n ],\n [\n -75.35936924857612,\n 42.27100674103562\n ],\n [\n -79.90219360799962,\n 42.118902705558185\n ]\n ],\n \"type\": \"LineString\"\n }\n }\n ]\n}","noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"4f4e4a8ee4b07f02db654904","contributors":{"authors":[{"text":"Staubitz, W. W.","contributorId":73209,"corporation":false,"usgs":true,"family":"Staubitz","given":"W. W.","affiliations":[],"preferred":false,"id":162907,"contributorType":{"id":1,"text":"Authors"},"rank":1}]}} ]}