A cruise on the- DESV STARELLA was conducted between October 23. 1979, and November 8, 1979, by the U.S. Geologic.al Survey (USGS) in cooperation with the United Kingdom's Institute of Oceanographic Sciences (IOS). The purpose of the study was to gain an overview of the morphology of large areas of the Continental Slope and upper Continental Rise off the eastern ·united States. Sidescan-sonar and single-channel seismic-reflection data were collected along the tracklines. The ship's position. was monitored using LORAN_C and satellite navigation techniques.
The sidescan data were collected using the !OS-developed Geologic Long-Range Inclined Asdic, Mark II (GLORIA II) system. GLORIA was operated at either a 20-second or 40-second sweep, giving maximum slant-range distances of 15 or 30 kilometers, respectively, to each side of the towed fish. The sidescan data were collected on graphic recorders and analog tapes. The tapes were played onto photographic paper in a facsimile machine; then these prints were photographically stretched to produce approximately isometric images .. The images were not corrected for slant-range distortion. Mosaics at a scale of 1:250,000 (Mercator projection) were made from the photographic images.
The seismic· data consist of 40-in3 airgun and 10-kHz echo-sounder profiles. The airgun data were recorded on EPC recorders at both 8- and 4- second sweep rates. The 10-kHz echo-sounder data were recorded on a wet-paper recorder at a 2-second sweep rate.
Approximately 4,820 km of seismic and sonar-data wera collected from four areas of interest and along the lines connecting those areas. Area 1 includes the Continental Slope and upper Rise seaward of Georges Bank, between Northeast Channel and Alvin Canyon. Numerous lines were run here, resulting in approximately 2,500 km of seismic data and complete and overlapping GLORIA coverage of the area. A similar survey, consisting of approximately 1 2 200 km of trackline, was run in area 2, which includes the Continental Slope and upper Rise seaward of the middle Atlantic states between Hudson Canyon and Baltimore Canyon. A single line, 250 km long, was run through area 3 along the base of the Continental Slope from Cape Hatteras to latitude 33°N. off North and South Carolina. Two parallel lines, totaling 870 km, were run through area 4 along the Blake Escarpment, from the Blake Spur south to latitude 27°40'N. One line was run along the top of the escarpment and the other was run along the base of the escarpment.
All the data can be studied at the U.S. Geological Survey offices in Woods Hole, MA 02543. Microfilm copies of the sidescan-monitor record as well as the airgun and 10-kHz profiles can be purchased only from the National Geophysical Data Center, NOAA, Code E64, 325 Broadway, Boulder, CO 80303 (303/497-6338). Photographic copies of the GLORIA mosaics can also be obtained only from this address.
","language":"English","publisher":"U.S. Geological Survey","publisherLocation":"Reston, VA","doi":"10.3133/ofr821095","usgsCitation":"Scanlon, K.M., 1982, GLORIA sidescan and seismic data collected by the DESV STARELLA along the continental slope and upper continental rise of the Eastern United States in 1979: U.S. Geological Survey Open-File Report 82-1095, 3 p., https://doi.org/10.3133/ofr821095.","productDescription":"3 p.","costCenters":[],"links":[{"id":143369,"rank":0,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/thumbnails/ofr821095.PNG"},{"id":259857,"rank":300,"type":{"id":11,"text":"Document"},"url":"https://pubs.usgs.gov/of/1982/1095/ofr19821095.pdf","text":"Report","size":"1.94 MB","linkFileType":{"id":1,"text":"pdf"},"description":"OFR 1982-1095"}],"contact":"Coastal and Marine Geology Program U.S. Geological Survey
384 Woods Hole Road
Woods Hole, MA 02543
Salinity, temperature, light transmission, oxygen saturation, pH, pCO2, chlorophyll a fluorescence, and the concentrations of nitrate, nitrite, dissolved silica, orthophosphate, and ammonia are continuously measured with a system designed primarily for estuarine studies. Near-surface water (2-m depth) is sampled continuously while the vessel is underway; on station, water to depths of 100 m is sampled with a submersible pump. The system is comprised of commercially available instruments, equipment, and components, and of specialized items designed and fabricated by the authors. Data are read from digital displays, analog strip-chart recorders, and a teletype printout, and can be logged in disc storage for subsequent plotting. Data records made in San Francisco Bay illustrate physical, biological, and chemical estuarine processes, such as mixing and phytoplankton net production. The system resolves large- and small-scale events, which contributes to its reliability and usefulness.
","language":"ENGLISH","publisher":"U.S. Geological Survey,","doi":"10.3133/ofr82551","usgsCitation":"Schemel, L., and Dedini, L., 1982, Continuous water sampling and water analysis in estuaries: U.S. Geological Survey Open-File Report 82-551, 28 p., ill., maps ;28 cm., https://doi.org/10.3133/ofr82551.","productDescription":"28 p., ill., maps ;28 cm.","onlineOnly":"N","additionalOnlineFiles":"N","costCenters":[{"id":552,"text":"San Francisco Bay-Delta","active":false,"usgs":true},{"id":5079,"text":"Pacific Regional Director's Office","active":true,"usgs":true}],"links":[{"id":143179,"rank":0,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/of/1982/0551/report-thumb.jpg"},{"id":38784,"rank":300,"type":{"id":11,"text":"Document"},"url":"https://pubs.usgs.gov/of/1982/0551/report.pdf","linkFileType":{"id":1,"text":"pdf"}}],"noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"4f4e4afde4b07f02db696e86","contributors":{"authors":[{"text":"Schemel, L. E.","contributorId":89529,"corporation":false,"usgs":true,"family":"Schemel","given":"L. E.","affiliations":[],"preferred":false,"id":162381,"contributorType":{"id":1,"text":"Authors"},"rank":1},{"text":"Dedini, L.A.","contributorId":54996,"corporation":false,"usgs":true,"family":"Dedini","given":"L.A.","affiliations":[],"preferred":false,"id":162380,"contributorType":{"id":1,"text":"Authors"},"rank":2}]}} ,{"id":11720,"text":"ofr811180 - 1982 - Comparison of automated satellite systems with conventional systems for hydrologic data collection in west-central Florida","interactions":[],"lastModifiedDate":"2012-02-02T00:06:30","indexId":"ofr811180","displayToPublicDate":"1994-01-01T00:00:00","publicationYear":"1982","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":"81-1180","title":"Comparison of automated satellite systems with conventional systems for hydrologic data collection in west-central Florida","docAbstract":"This report provides results of reliability and cost-effective studies of the goes satellite data-collection system used to operate a small hydrologic data network in west-central Florida. The GOES system, in its present state of development, was found to be about as reliable as conventional methods of data collection. Benefits of using the GOES system include some cost and manpower reduction, improved data accuracy, near real-time data availability, and direct computer storage and analysis of data. The GOES system could allow annual manpower reductions of 19 to 23 percent with reduction in cost for some and increase in cost for other single-parameter sites, such as streamflow, rainfall, and ground-water monitoring stations. Manpower reductions of 46 percent or more appear possible for multiple-parameter sites. Implementation of expected improvements in instrumentation and data handling procedures should further reduce costs. (USGS)","language":"ENGLISH","publisher":"U.S. Geological Survey,","doi":"10.3133/ofr811180","usgsCitation":"Woodham, W.M., 1982, Comparison of automated satellite systems with conventional systems for hydrologic data collection in west-central Florida: U.S. Geological Survey Open-File Report 81-1180, iv, 27 p., map ;28 cm., https://doi.org/10.3133/ofr811180.","productDescription":"iv, 27 p., map ;28 cm.","costCenters":[],"links":[{"id":143920,"rank":0,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/of/1981/1180/report-thumb.jpg"},{"id":39606,"rank":300,"type":{"id":11,"text":"Document"},"url":"https://pubs.usgs.gov/of/1981/1180/report.pdf","linkFileType":{"id":1,"text":"pdf"}}],"noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"4f4e4b23e4b07f02db6ae3a6","contributors":{"authors":[{"text":"Woodham, W. M.","contributorId":72356,"corporation":false,"usgs":true,"family":"Woodham","given":"W.","email":"","middleInitial":"M.","affiliations":[],"preferred":false,"id":163617,"contributorType":{"id":1,"text":"Authors"},"rank":1}]}} ,{"id":11080,"text":"ofr82217 - 1982 - PACERAB; a computer program to create an absentee file for executing PACER (program to analyze coal energy resources)","interactions":[],"lastModifiedDate":"2012-02-02T00:06:26","indexId":"ofr82217","displayToPublicDate":"1994-01-01T00:00:00","publicationYear":"1982","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":"82-217","title":"PACERAB; a computer program to create an absentee file for executing PACER (program to analyze coal energy resources)","language":"ENGLISH","publisher":"U.S. Geological Survey,","doi":"10.3133/ofr82217","usgsCitation":"Scott, W., 1982, PACERAB; a computer program to create an absentee file for executing PACER (program to analyze coal energy resources): U.S. Geological Survey Open-File Report 82-217, 33 p., 28 cm., https://doi.org/10.3133/ofr82217.","productDescription":"33 p., 28 cm.","costCenters":[],"links":[{"id":143237,"rank":0,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/of/1982/0217/report-thumb.jpg"},{"id":38839,"rank":300,"type":{"id":11,"text":"Document"},"url":"https://pubs.usgs.gov/of/1982/0217/report.pdf","linkFileType":{"id":1,"text":"pdf"}}],"noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"4f4e4ae4e4b07f02db689f8d","contributors":{"authors":[{"text":"Scott, W.A.","contributorId":106121,"corporation":false,"usgs":true,"family":"Scott","given":"W.A.","affiliations":[],"preferred":false,"id":162496,"contributorType":{"id":1,"text":"Authors"},"rank":1}]}} ,{"id":11799,"text":"ofr82135 - 1982 - Paleoshorelines in the Upper Cretaceous Point Lookout Sandstone, southern San Juan Basin, New Mexico","interactions":[],"lastModifiedDate":"2012-02-02T00:06:34","indexId":"ofr82135","displayToPublicDate":"1994-01-01T00:00:00","publicationYear":"1982","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":"82-135","title":"Paleoshorelines in the Upper Cretaceous Point Lookout Sandstone, southern San Juan Basin, New Mexico","docAbstract":"LANDSAT images and aerial photography reveal several parallel linear features as much as 17 km long and 0.7 km wide. Detailed cross sections normal to a linear feature show it to be an exhumed paleoshoreline containing several overlapping sandstone units. Each unit tends to pinchout into the shales of the overlying Menefee Formation, showing a range of depositional environments including upper shoreface, foreshore, washover and eolian. Paleogeomorphic elements, predominately beach ridges and interridge swales, shape the upper surface of the sandstone and produce a relief as great as 4.2 m. The various components found in the paleoshoreline create a trellis-like drainage pattern that contrasts with the regional dendritic drainage pattern; the resulting linear feature is easily discernible on aerial photography and LANDSAT images. The rapid lithologic and thickness changes of the sandstone bodies in these linear features provide excellent potential as stratigraphic trap for hydrocarbons. Paleoshoreline facies are likely to be preserved in areas of thickest marginal marine regressive sand accumulation and similar paleoshoreline systems may be preserved at depth in the Point Lookout (Sandstone) or other Cretaceous sandstones.","language":"ENGLISH","publisher":"U.S. Geological Survey,","doi":"10.3133/ofr82135","usgsCitation":"Zech, R.S., 1982, Paleoshorelines in the Upper Cretaceous Point Lookout Sandstone, southern San Juan Basin, New Mexico: U.S. Geological Survey Open-File Report 82-135, 25 p., ill., maps ;28 cm., https://doi.org/10.3133/ofr82135.","productDescription":"25 p., ill., maps ;28 cm.","costCenters":[],"links":[{"id":144864,"rank":0,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/of/1982/0135/report-thumb.jpg"},{"id":39688,"rank":300,"type":{"id":11,"text":"Document"},"url":"https://pubs.usgs.gov/of/1982/0135/report.pdf","linkFileType":{"id":1,"text":"pdf"}}],"noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"4f4e4ae4e4b07f02db689a74","contributors":{"authors":[{"text":"Zech, R. S.","contributorId":51289,"corporation":false,"usgs":true,"family":"Zech","given":"R.","email":"","middleInitial":"S.","affiliations":[],"preferred":false,"id":163751,"contributorType":{"id":1,"text":"Authors"},"rank":1}]}} ,{"id":11723,"text":"ofr82313 - 1982 - Fluid-inclusion data on samples from Creede, Colorado, in relation to mineral paragenesis","interactions":[],"lastModifiedDate":"2012-02-02T00:06:31","indexId":"ofr82313","displayToPublicDate":"1994-01-01T00:00:00","publicationYear":"1982","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":"82-313","title":"Fluid-inclusion data on samples from Creede, Colorado, in relation to mineral paragenesis","docAbstract":"Published and unpublished data on 2575 fluid inclusions in ore and gangue minerals from the Creede, Colorado, Ag-Pb-Zn-Cu vein deposit collected in our laboratories from 1959 to 1981 have shown that the average salinity (wt. % NaCl equivalent, hereinafter termed wt.% eq.) and homogenization temperature (Th), and the ranges of these two parameters for fluid inclusions in sphalerite, quartz, fluorite, and rhodochrosite, respectively, are 8.1 (4.6 - 13.4), 239?C (195-274?C); 6.1 (1.1-10.0), 260?C (190->400?C); 10.7 (6.1-11.1), 217?C (213-229?C) and 260?C (247-268?C) (bimodal distribution of Th); and 9.9 (9.3 - 10.6), 214?C (185-249?C). Inclusions have been measured in minerals from four of the five stages of mineralization previously recognized at Creede. The few inclusions of fluids depositing rhodochrosite (A-stage, earliest in the paragenesis) yield Th and salinity values more similar to those of the low-temperature (average Th 217?C) fluids forming some of the much later fluorite (C-stage) than to any of the other fluids. Th measurements on A-stage quartz range from 192?C to 263?C and average 237?C. The early, fine-grained, B-stage sphalerites yielded Th of 214 to 241?C and salinities of 6.1 to 10.2 wt. % eq. \r\n\r\nD-stage sphalerite (late in the paragenesis) has been studied in detail (growth-zone by growth-zone) for several localities along the OH vein and reveals a generally positive correlation among Th, salinity and iron content of the host sphalerite. The deposition of D-stage sphalerite was characterized by repeated cycling through different regions of salinity/Th space, as Th and salinity generally decreased with time. Seventeen salinity-Th measurements were made on D-stage sphalerite from one locality on the Bulldog Mountain vein system, which, like the OH vein, is one of four major ore-producing vein systems at Creede. These data suggest a lower Th for a given salinity fluid from sphalerite on the Bulldog Mountain vein than on the OH vein. The very high values of Th for some quartz samples (mostly D-stage) are believed to be a result of the trapping of both gas and liquid from a boiling fluid in the upper levels of the vein system. Boiling of fluids depositing D-stage quartz is indicated by the presence of steam inclusions in quartz and the extreme variability of Th values measured on quartz. The pressure was low (< 125 kg/cm 2) throughout ore deposition. \r\n\r\nThree major growth zones in D-stage sphalerite are recognized throughout the OH vein. Deposition of the first major zone began from fluids having intermediate salinities and temperatures (7.8-9.2 wt. % eq., 240?C) but the characteristics of the fluids oscillated after that, ranging from 7.2 to 10.1 wt. % eq. and from 225?C to 270?C. Deposition of the second major, most Fe-rich zone began with the hottest, most saline fluids present during D-stage mineralization (. 270?C, 10.5-12.5 wt. % eq., 3 mole % FeS in sphalerite). The fluid then oscillated with respect to Th and salinity (213-274?C, 5.2-12.5 wt. % eq.) but showed a general decrease in both with time. Deposition of the youngest major zone began with a very Fe-poor sphalerite (0.25-0.75 mole % FeS), from the least saline, coolest fluids (5-6.5 wt. % eq., 200-212?C) and ended with a trend of increasing temperature at approximately constant salinity.\r\n\r\nThe fluid-inclusion data can best be explained by a mixing model involving at least two fluids--one hot and saline, the other cool and fresher. Sudden changes in the mixing ratio, presumably from changes in the plumbing, punctuated long periods of remarkably uniform conditions of ore fluid flow and deposition. The effects of other processes such as convection and heat exchange with wall rocks must have been superimposed on this simple mixing model, however. In contrast to an earlier interpretation, several aspects of the inclusion data may be interpreted to suggest exceedingly slow ore deposition. Work in progress may resolve some of these ambiguities and refine","language":"ENGLISH","publisher":"U.S. Geological Survey,","doi":"10.3133/ofr82313","usgsCitation":"Woods, T., Roedder, E., and Bethke, P.M., 1982, Fluid-inclusion data on samples from Creede, Colorado, in relation to mineral paragenesis: U.S. Geological Survey Open-File Report 82-313, 77 p., ill., maps ;28 cm., https://doi.org/10.3133/ofr82313.","productDescription":"77 p., ill., maps ;28 cm.","costCenters":[],"links":[{"id":143786,"rank":0,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/of/1982/0313/report-thumb.jpg"},{"id":39610,"rank":300,"type":{"id":11,"text":"Document"},"url":"https://pubs.usgs.gov/of/1982/0313/report.pdf","linkFileType":{"id":1,"text":"pdf"}}],"noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"4f4e49d6e4b07f02db5de77a","contributors":{"authors":[{"text":"Woods, T.L.","contributorId":6052,"corporation":false,"usgs":true,"family":"Woods","given":"T.L.","email":"","affiliations":[],"preferred":false,"id":163620,"contributorType":{"id":1,"text":"Authors"},"rank":1},{"text":"Roedder, Edwin","contributorId":25571,"corporation":false,"usgs":true,"family":"Roedder","given":"Edwin","affiliations":[],"preferred":false,"id":163621,"contributorType":{"id":1,"text":"Authors"},"rank":2},{"text":"Bethke, P. M.","contributorId":32921,"corporation":false,"usgs":true,"family":"Bethke","given":"P.","email":"","middleInitial":"M.","affiliations":[],"preferred":false,"id":163622,"contributorType":{"id":1,"text":"Authors"},"rank":3}]}} ,{"id":11399,"text":"ofr82628 - 1982 - Water resources of southeastern Oahu, Hawaii","interactions":[],"lastModifiedDate":"2012-02-02T00:06:21","indexId":"ofr82628","displayToPublicDate":"1994-01-01T00:00:00","publicationYear":"1982","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":"82-628","title":"Water resources of southeastern Oahu, Hawaii","docAbstract":"Southeastern Oahu comprises the eastern end of the Koolau Range and is divided into two roughly equal parts by the crest of the range. The northside of the crest is commonly called the windward side and the southside, the leeward. Precipitous cliffs aproned by a gently sloping landscape are the main topographic features on the windward side. The leeward side is a gentle lava-flow slope incised by steep narrow valleys. \r\n\r\nThe main Koolau fissure zone, including the caldera, lies on the windward side. The leeward side includes minor rift zones that are perpendicular to and intersect the main fissure zone. Dikes in the main fissure zone strike from nearly east-west in the eastern end to about N. 55? W. in the western part. Dikes in the minor rift zones strike from north-south to slightly northeasterly. \r\n\r\nWater use is about 18 Mgal/d (million gallons per day) of which only 4 Mgal/d is obtained locally from ground-water sources. About a third of the 14 Mgal/d deficit is imported from sources northwest of the study area on the windward side and the remainder from sources in the Honolulu and Pearl Harbor areas on the leeward side. The 4 Mgal/d being developed represents only about 3 percent of the area's rainfall compared to a development-rainfall ratio of 20 percent for the rest of the island. \r\n\r\nStreams are short and flashy. Perennial streamflow to the sea occurs only in Maunawili Valley and in the Waimanalo area. Mean annual discharge is estimated at 20 Mgal/d in the windward side and at 15 Mgal/d on the leeward side. Low flow, expressed as the flow that is equaled or exceeded 90 percent of the time, is 5 Mgal/d windward of the crest and zero leeward of it. Most fresh ground water occurs in lava flows of the Koolau Volcanics. It is impounded by dikes in the rift zones and floats on saline ground water as lenses outside the rift zones. Small but important bodies of freshwater are perched in volcanic rocks of the Honolulu Group in Maunawili Valley. Fresh ground water occurs in near-shore calcareous sands that overlie a clay horizon in the Waimanalo area. Deeply buried talus and alluvium also carry fresh ground water in the Waimanalo area. \r\n\r\nWells tapping saline ground water in fresh lava flows of the Honolulu Group provide water for a sea-life park in the Makapuu area. The same aquifer is tapped by wells for disposal of the saline waste water. \r\n\r\nThe current development scheme in the windward side that utilizes only the free-flow equilibrium discharge of dike-impounded water is inefficient and does not cope with the annual weather cycle. The flow available for development under this scheme is greatest in the rainy winter months when demand is the lowest and least in the summer months when demand is the highest. A more optimal scheme would be to change this natural flow pattern by depleting storage by pumping to increase flow in the high-demand summer months and allowing the depleted storage to recover naturally in the low-demand winter months. Depleting storage would lower water levels which would provide more room for infiltration and provide less opportunity for evapotranspiration. \r\n\r\nThe basal-water reservoir in the leeward side is isolated hydrologically from abutting reservoirs outside the area and can and should be fully exploited. The existing development of the basal-water reservoir is small compared to the natural ground-water flow and that part not being developed is wasting to the sea. Because the area is hydrologically isolated, development will not be detrimental to or reduce the ground-water supply outside the area.","language":"ENGLISH","publisher":"U.S. Geological Survey,","doi":"10.3133/ofr82628","usgsCitation":"Takasaki, K., and Mink, J., 1982, Water resources of southeastern Oahu, Hawaii: U.S. Geological Survey Open-File Report 82-628, viii, 97 p. :ill., maps ;28 cm., https://doi.org/10.3133/ofr82628.","productDescription":"viii, 97 p. :ill., maps ;28 cm.","costCenters":[],"links":[{"id":142573,"rank":0,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/of/1982/0628/report-thumb.jpg"},{"id":39220,"rank":300,"type":{"id":11,"text":"Document"},"url":"https://pubs.usgs.gov/of/1982/0628/report.pdf","linkFileType":{"id":1,"text":"pdf"}}],"noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"4f4e49dee4b07f02db5e3158","contributors":{"authors":[{"text":"Takasaki, K. J.","contributorId":44523,"corporation":false,"usgs":true,"family":"Takasaki","given":"K. J.","affiliations":[],"preferred":false,"id":163073,"contributorType":{"id":1,"text":"Authors"},"rank":1},{"text":"Mink, John F.","contributorId":89510,"corporation":false,"usgs":true,"family":"Mink","given":"John F.","affiliations":[],"preferred":false,"id":163074,"contributorType":{"id":1,"text":"Authors"},"rank":2}]}} ,{"id":10563,"text":"ofr82826 - 1982 - MDS-CRIB user's manual; using GIPSY","interactions":[],"lastModifiedDate":"2012-02-02T00:06:28","indexId":"ofr82826","displayToPublicDate":"1994-01-01T00:00:00","publicationYear":"1982","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":"82-826","title":"MDS-CRIB user's manual; using GIPSY","language":"ENGLISH","publisher":"U.S. Geological Survey,","doi":"10.3133/ofr82826","usgsCitation":"Orris, G., and Stolz, M., 1982, MDS-CRIB user's manual; using GIPSY: U.S. Geological Survey Open-File Report 82-826, 61 p., ill. ;28 cm., https://doi.org/10.3133/ofr82826.","productDescription":"61 p., ill. ;28 cm.","costCenters":[],"links":[{"id":144133,"rank":0,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/of/1982/0826/report-thumb.jpg"},{"id":38398,"rank":300,"type":{"id":11,"text":"Document"},"url":"https://pubs.usgs.gov/of/1982/0826/report.pdf","linkFileType":{"id":1,"text":"pdf"}}],"noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"4f4e4a7fe4b07f02db648bb2","contributors":{"authors":[{"text":"Orris, G. J.","contributorId":80252,"corporation":false,"usgs":true,"family":"Orris","given":"G. J.","affiliations":[],"preferred":false,"id":161597,"contributorType":{"id":1,"text":"Authors"},"rank":1},{"text":"Stolz, Melissa","contributorId":100853,"corporation":false,"usgs":true,"family":"Stolz","given":"Melissa","email":"","affiliations":[],"preferred":false,"id":161598,"contributorType":{"id":1,"text":"Authors"},"rank":2}]}} ,{"id":10587,"text":"ofr82649 - 1982 - January 1982 water levels, and data related to water-level changes, western and south-central Kansas","interactions":[],"lastModifiedDate":"2012-02-02T00:06:25","indexId":"ofr82649","displayToPublicDate":"1994-01-01T00:00:00","publicationYear":"1982","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":"82-649","title":"January 1982 water levels, and data related to water-level changes, western and south-central Kansas","docAbstract":"Water-level measurements were made, mostly in January 1982, in about 1,530 wells in western and south-central Kansas. The measurements were made in mid-winter when pumping was minimal and water levels had recovered, for the most part, from the effects of pumping during the previous irrigation season. Annual hydrologic data are provided for relating water-level changes from a ' base-reference year ' (predevelopment year), a year of abnormally high rainfall and minimum pumpage (1966 or 1974), and each of seven consecutive years of measurement (1976-82), the ' base-reference year ' is designated as 1940 for the southwestern area, 1944 for the south-central area, and 1950 for the northwestern and west-central areas. Water levels for the ' base-reference year ' are established by measurements made during that year and by interpretation of maps showing water-level altitudes. Data also are provided for relating the average annual water-level changes, saturated thicknesses of the deposits, and percentage changes in saturated thicknesses. (USGS)","language":"ENGLISH","publisher":"U.S. Geological Survey,","doi":"10.3133/ofr82649","usgsCitation":"Pabst, M., 1982, January 1982 water levels, and data related to water-level changes, western and south-central Kansas: U.S. Geological Survey Open-File Report 82-649, 167 p. :map ;28 cm., https://doi.org/10.3133/ofr82649.","productDescription":"167 p. :map ;28 cm.","costCenters":[],"links":[{"id":143111,"rank":0,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/of/1982/0649/report-thumb.jpg"},{"id":38413,"rank":300,"type":{"id":11,"text":"Document"},"url":"https://pubs.usgs.gov/of/1982/0649/report.pdf","linkFileType":{"id":1,"text":"pdf"}}],"noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"4f4e4aa7e4b07f02db666fde","contributors":{"authors":[{"text":"Pabst, M.E.","contributorId":17608,"corporation":false,"usgs":true,"family":"Pabst","given":"M.E.","email":"","affiliations":[],"preferred":false,"id":161637,"contributorType":{"id":1,"text":"Authors"},"rank":1}]}} ,{"id":11010,"text":"ofr82982 - 1982 - List of published articles on mineralogy and geochemistry for which translations by U.S. Geological Survey members are deposited at the USGS Library in Reston, Virginia","interactions":[],"lastModifiedDate":"2018-07-31T11:13:08","indexId":"ofr82982","displayToPublicDate":"1994-01-01T00:00:00","publicationYear":"1982","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":"82-982","title":"List of published articles on mineralogy and geochemistry for which translations by U.S. Geological Survey members are deposited at the USGS Library in Reston, Virginia","docAbstract":"No abstract available.
","language":"English","publisher":"U.S. Geological Survey","doi":"10.3133/ofr82982","usgsCitation":"Schafer, C.M., Conte, C.J., and Fleischer, M., 1982, List of published articles on mineralogy and geochemistry for which translations by U.S. Geological Survey members are deposited at the USGS Library in Reston, Virginia: U.S. Geological Survey Open-File Report 82-982, 129 p., https://doi.org/10.3133/ofr82982.","productDescription":"129 p.","costCenters":[],"links":[{"id":144074,"rank":0,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/of/1982/0982/report-thumb.jpg"},{"id":38779,"rank":300,"type":{"id":11,"text":"Document"},"url":"https://pubs.usgs.gov/of/1982/0982/report.pdf","text":"Report","size":"1.39 MB","linkFileType":{"id":1,"text":"pdf"},"description":"Report"}],"noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"4f4e4b15e4b07f02db6a4f36","contributors":{"authors":[{"text":"Schafer, Constance M.","contributorId":67092,"corporation":false,"usgs":true,"family":"Schafer","given":"Constance","email":"","middleInitial":"M.","affiliations":[],"preferred":false,"id":162373,"contributorType":{"id":1,"text":"Authors"},"rank":1},{"text":"Conte, Constance J.","contributorId":80284,"corporation":false,"usgs":true,"family":"Conte","given":"Constance","email":"","middleInitial":"J.","affiliations":[],"preferred":false,"id":162372,"contributorType":{"id":1,"text":"Authors"},"rank":2},{"text":"Fleischer, Michael","contributorId":65835,"corporation":false,"usgs":true,"family":"Fleischer","given":"Michael","email":"","affiliations":[],"preferred":false,"id":162371,"contributorType":{"id":1,"text":"Authors"},"rank":3}]}} ]}