{"pageNumber":"1462","pageRowStart":"36525","pageSize":"25","recordCount":46706,"records":[{"id":30301,"text":"wri894161 - 1989 - Sediment-transport characteristics and effects of sediment transport on benthic invertebrates in the Fountain Creek drainage basin upstream from Widefield, southeastern Colorado, 1985-88","interactions":[],"lastModifiedDate":"2012-02-02T00:08:55","indexId":"wri894161","displayToPublicDate":"1994-01-01T00:00:00","publicationYear":"1989","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":"89-4161","title":"Sediment-transport characteristics and effects of sediment transport on benthic invertebrates in the Fountain Creek drainage basin upstream from Widefield, southeastern Colorado, 1985-88","docAbstract":"Sediment and benthic-invertebrate data were collected during water years 1985 through 1988 in the Fountain Creek drainage basin upstream from Widefield, Colorado. Sediment data collected include suspended-sediment concentrations and particle size analysis of suspended sediment, bedload, and bed material. Sediment-transport equations were derived for total suspended-sediment discharge and suspended-sand discharge at seven periodic sampling sites. Annual suspended-sediment loads for water years 1985 through 1988 and mean suspended-sediment yields were computed for the seven periodic sampling sites. Mean annual suspended-sediment yield for 1985 through 1988 increased about 73% downstream in the Fountain Creek drainage basin primarily as a result of sediment discharging from Monument Creek. Bedload discharge was computed at six of the periodic sampling sites and ranged from 2.6 to 3,570 tons/day. Bedload discharge, as a percentage of total sediment discharge, ranged from 6 to 92%, and the smaller values occurred during rainfall runoff. Number of taxa, species density, and similarity indices were determined for benthic invertebrates at five of the periodic sampling sites. Multiple comparison tests were used to test for similarity of benthic invertebrates between the five sites. Multiple-regression analysis was done to determine the effects of sediment transport on benthic-invertebrate densities. Median grain size of bed material collected in conjunction with benthic- invertebrate samples and flooding during the 30 days prior to sampling consistently accounted for the most variation in mean densities of total organisms and major taxa groups sampled. (USGS)","language":"ENGLISH","publisher":"U.S. Geological Survey,","doi":"10.3133/wri894161","usgsCitation":"Von Guerard, P., 1989, Sediment-transport characteristics and effects of sediment transport on benthic invertebrates in the Fountain Creek drainage basin upstream from Widefield, southeastern Colorado, 1985-88: U.S. Geological Survey Water-Resources Investigations Report 89-4161, xi, 225 p. :ill. ;28 cm., https://doi.org/10.3133/wri894161.","productDescription":"xi, 225 p. :ill. ;28 cm.","costCenters":[],"links":[{"id":159769,"rank":0,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/wri/1989/4161/report-thumb.jpg"},{"id":59093,"rank":300,"type":{"id":11,"text":"Document"},"url":"https://pubs.usgs.gov/wri/1989/4161/report.pdf","linkFileType":{"id":1,"text":"pdf"}}],"noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"4f4e49e0e4b07f02db5e3e64","contributors":{"authors":[{"text":"Von Guerard, Paul","contributorId":40620,"corporation":false,"usgs":true,"family":"Von Guerard","given":"Paul","affiliations":[],"preferred":false,"id":203018,"contributorType":{"id":1,"text":"Authors"},"rank":1}]}}
,{"id":18867,"text":"ofr89410 - 1989 - Chemical, geologic, and hydrologic data from the study of acidic contamination in the Miami Wash-Pinal Creek area, Arizona, water years 1984-87","interactions":[],"lastModifiedDate":"2012-02-02T00:07:30","indexId":"ofr89410","displayToPublicDate":"1994-01-01T00:00:00","publicationYear":"1989","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":"89-410","title":"Chemical, geologic, and hydrologic data from the study of acidic contamination in the Miami Wash-Pinal Creek area, Arizona, water years 1984-87","docAbstract":"Occurrence and movement of acidic contamination in the aquifer and streams of the Pinal Creek basin near Globe, Arizona, is the focus of an ongoing study by the U.S. Geological Survey. Groundwater data from that study for water years 1984 to 1987 include location, construction information, and site plans for six groups of monitoring wells, mineralogic and particle-size analyses of drill cuttings, water level measurements, and chemical analyses of water samples from 39 wells. Surface water data for 13 sites in this study include discharge measurements and chemical analysis of water and streambed sediment samples. Monthly discharge data are presented for one site. Monthly precipitation amounts and statistics of long-term precipitation are presented for two sites. (USGS)","language":"ENGLISH","publisher":"Dept. of the Interior, U.S. Geological Survey ;\r\nBooks and Open-File Reports [distributor],","doi":"10.3133/ofr89410","usgsCitation":"Eychaner, J., Rehmann, M., and Brown, J.G., 1989, Chemical, geologic, and hydrologic data from the study of acidic contamination in the Miami Wash-Pinal Creek area, Arizona, water years 1984-87: U.S. Geological Survey Open-File Report 89-410, iii, 105 p. :ill. ;28 cm., https://doi.org/10.3133/ofr89410.","productDescription":"iii, 105 p. :ill. ;28 cm.","costCenters":[],"links":[{"id":151689,"rank":0,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/of/1989/0410/report-thumb.jpg"},{"id":48262,"rank":300,"type":{"id":11,"text":"Document"},"url":"https://pubs.usgs.gov/of/1989/0410/report.pdf","linkFileType":{"id":1,"text":"pdf"}}],"noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"4f4e49dfe4b07f02db5e32a3","contributors":{"authors":[{"text":"Eychaner, J.H.","contributorId":34511,"corporation":false,"usgs":true,"family":"Eychaner","given":"J.H.","affiliations":[],"preferred":false,"id":179887,"contributorType":{"id":1,"text":"Authors"},"rank":1},{"text":"Rehmann, M.R.","contributorId":24376,"corporation":false,"usgs":true,"family":"Rehmann","given":"M.R.","email":"","affiliations":[],"preferred":false,"id":179885,"contributorType":{"id":1,"text":"Authors"},"rank":2},{"text":"Brown, J. G.","contributorId":28263,"corporation":false,"usgs":true,"family":"Brown","given":"J.","email":"","middleInitial":"G.","affiliations":[],"preferred":false,"id":179886,"contributorType":{"id":1,"text":"Authors"},"rank":3}]}}
,{"id":30594,"text":"wri884223 - 1989 - Geohydrology of the Escondido hydrologic subarea, San Diego County, California","interactions":[],"lastModifiedDate":"2012-02-02T00:09:12","indexId":"wri884223","displayToPublicDate":"1994-01-01T00:00:00","publicationYear":"1989","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":"88-4223","title":"Geohydrology of the Escondido hydrologic subarea, San Diego County, California","docAbstract":"The San Diego region of California is undergoing rapid growth with a corresponding increase in the demand for water. To update the basin plan developed in 1975 by the California Regional Water Quality Control Board, San Diego Region, water-level and water quality data for the 44-sq mi Escondido hydrologic subarea were collected and analyzed. Water-level measurements indicate that groundwater in most of the subarea was within 20 ft of land surface. Groundwater generally moves from the weathered crystalline rocks on hillsides into the alluvium. Groundwater moves from north to south in Reidy Canyon and from east to west in the alluvium along Escondido Creek. Water from all 20 wells sampled in 1987 had dissolved-solids concentrations greater than the U.S. Environmental Protection Agency recommended limit of 500 mg/L; concentrations ranged from 720 to 4,500 mg/L. Nitrate (as nitrogen) concentrations ranged from 1.1 to 86 mg/L. Water from 14 of the 20 wells had nitrate (as nitrogen) concentrations greater than the U.S. Environmental Agency recommended limit of 10 mg/L. (USGS)","language":"ENGLISH","publisher":"U.S. Geological Survey,","doi":"10.3133/wri884223","usgsCitation":"Woolfenden, L.R., 1989, Geohydrology of the Escondido hydrologic subarea, San Diego County, California: U.S. Geological Survey Water-Resources Investigations Report 88-4223, iv, 21 p. :ill. ;28 cm., https://doi.org/10.3133/wri884223.","productDescription":"iv, 21 p. :ill. ;28 cm.","costCenters":[],"links":[{"id":124165,"rank":0,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/wri/1988/4223/report-thumb.jpg"},{"id":59352,"rank":300,"type":{"id":11,"text":"Document"},"url":"https://pubs.usgs.gov/wri/1988/4223/report.pdf","linkFileType":{"id":1,"text":"pdf"}}],"noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"4f4e4b1be4b07f02db6a89b7","contributors":{"authors":[{"text":"Woolfenden, L. R. 0000-0003-3500-4709","orcid":"https://orcid.org/0000-0003-3500-4709","contributorId":36945,"corporation":false,"usgs":true,"family":"Woolfenden","given":"L.","email":"","middleInitial":"R.","affiliations":[],"preferred":false,"id":203510,"contributorType":{"id":1,"text":"Authors"},"rank":1}]}}
,{"id":66369,"text":"i1907 - 1989 - Geologic map of the Latir Volcanic Field and adjacent areas, northern New Mexico","interactions":[],"lastModifiedDate":"2022-08-26T19:40:16.281788","indexId":"i1907","displayToPublicDate":"1994-01-01T00:00:00","publicationYear":"1989","noYear":false,"publicationType":{"id":18,"text":"Report"},"publicationSubtype":{"id":5,"text":"USGS Numbered Series"},"seriesTitle":{"id":320,"text":"IMAP","code":"I","active":false,"publicationSubtype":{"id":5}},"seriesNumber":"1907","title":"Geologic map of the Latir Volcanic Field and adjacent areas, northern New Mexico","docAbstract":"This map was first published as a printed edition in 1989. The geologic data have now been captured digitally and are presented here along with images of the printed map sheet and component parts as PDF files.\nThis map encompasses all or parts of ten 7.5 minute quadrangles in the Taos Range of the Sangre de Cristo Mountains in northern New Mexico. Geologic mapping was initiated in this area by the U.S. Geological Survey in response to its mandate under the Wilderness Act of 1964 to evaluate the mineral resource potential of the Latir and Wheeler Peak Wildernesses and the Columbine-Hondo Wilderness Study Area in the Carson National Forest. The mapping was later extended to adjacent areas in order to better understand the regional geology and geologic history of the range.\nThe present map focuses on the early Tertiary (largely Oligocene) Latir Volcanic Field and plutonic rocks associated with it. The basement rocks in the map area are Paleoproterozic amphibolite-facies metasedimentary and metavolcanic rocks intruded by large bodies of quartz monzonite, granodiorite and gabbro dated at between 1,750 and 1,690 Ma. The basement rocks are locally overlain by Mississippian limestone or by Pennsylvanian and Permian redbeds. The basement rocks were thrust eastward across a thick section of similar late Paleozoic rocks along low-angle faults during the Laramide Orogeny. Post-Laramide erosion largely removed the sedimentary cover from the basement rocks and reduced the topography to a low-relief surface locally overlain by scattered lenses of Eocene to Oligocene shale, sandstone, and conglomerate. It was on this surface that the earliest rocks of the Latir Volcanic Field were deposited, beginning in the Oligocene, about 30 Ma.\nThe early volcanic rocks comprise a thick sequence of andesite, dacite, and minor rhyolite, deposited as flows, breccia, and volcaniclastic sediments from numerous local volcanic centers; thin layers of rhyolite tuff are from distant eruptions, some probably in the San Juan Mountains. These volcanic rocks probably record early growth of an upper-crustal batholith. At 25 Ma enormous eruptions of peralkaline rhyolite ash-flow tuff were accompanied by collapse of the roof of the growing batholith to form the Questa Caldera, a volcanic depression at least 14 km across. The ash flows traveled for tens of kilometers from the caldera rims to form a widespread sheet of densely welded tuff; ash also fell back to fill the subsiding caldera depression. Concurrent extension along northwest-trending faults segmented the volcanic edifice and rotated the originally sub-horizontal layers, so that some are nearly vertical. Formation of the caldera was accompanied by further batholith growth, involving intrusion of large plutons of granite, granodiorite, and related rocks into both caldera fill and the adjacent rocks, including both the earlier volcanic rocks and the basement rocks. The large molybdenum deposit along the Red River east of Questa is related to the emplacement of one of these late granitic plutons. Intrusive activity continued into the Miocene.\nDevelopment of the Rio Grande Rift beginning at about 15 Ma was accompanied by development of the north-south trending normal faults along the western foot of the Taos Range. The rift is filled with thousands of meters of clastic sediments interleaved with basalt flows, some as young as 3.6 Ma. The bounding faults of the rift cut the Questa Caldera so that the western part of the original structure is now deeply buried beneath the rift fill.","language":"English","publisher":"U.S Geological Survey","publisherLocation":"Reston, VA","doi":"10.3133/i1907","usgsCitation":"Lipman, P.W., and Reed, J.C., 1989, Geologic map of the Latir Volcanic Field and adjacent areas, northern New Mexico (Digital Edition-September 2011): U.S. Geological Survey IMAP 1907, Report: 11 p.; 1 Plate: 39.03 × 53.33 inches; Downloads Directory, https://doi.org/10.3133/i1907.","productDescription":"Report: 11 p.; 1 Plate: 39.03 × 53.33 inches; Downloads Directory","onlineOnly":"Y","additionalOnlineFiles":"Y","costCenters":[{"id":308,"text":"Geology and Environmental Change Science Center","active":false,"usgs":true}],"links":[{"id":204078,"rank":0,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/thumbnails/usgs_thumb.jpg"},{"id":107178,"rank":700,"type":{"id":36,"text":"NGMDB Index Page"},"url":"https://ngmdb.usgs.gov/Prodesc/proddesc_9996.htm","linkFileType":{"id":5,"text":"html"},"description":"9996"},{"id":92149,"rank":100,"type":{"id":15,"text":"Index Page"},"url":"https://pubs.usgs.gov/imap/i-1907/","linkFileType":{"id":5,"text":"html"}}],"scale":"48000","country":"United States","state":"New Mexico","otherGeospatial":"Latir Volcanic Field and adjacent areas","geographicExtents":"{\n  \"type\": \"FeatureCollection\",\n  \"features\": [\n    {\n      \"type\": \"Feature\",\n      \"properties\": {},\n      \"geometry\": {\n        \"type\": \"Polygon\",\n        \"coordinates\": [\n          [\n            [\n              -105.625,\n              36.5\n            ],\n            [\n              -105.25,\n              36.5\n            ],\n            [\n              -105.25,\n              37\n            ],\n            [\n              -105.625,\n              37\n            ],\n            [\n              -105.625,\n              36.5\n            ]\n          ]\n        ]\n      }\n    }\n  ]\n}","edition":"Digital Edition-September 2011","noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"4f4e4afde4b07f02db696b37","contributors":{"authors":[{"text":"Lipman, P. W.","contributorId":93470,"corporation":false,"usgs":true,"family":"Lipman","given":"P.","middleInitial":"W.","affiliations":[],"preferred":false,"id":274419,"contributorType":{"id":1,"text":"Authors"},"rank":1},{"text":"Reed, J. C. Jr.","contributorId":97063,"corporation":false,"usgs":true,"family":"Reed","given":"J.","suffix":"Jr.","email":"","middleInitial":"C.","affiliations":[],"preferred":false,"id":274420,"contributorType":{"id":1,"text":"Authors"},"rank":2}]}}
,{"id":30523,"text":"wri894040 - 1989 - Selected water-quality characteristics and flow of ground water in the San Luis basin, including the Conejos River subbasin, Colorado and New Mexico","interactions":[],"lastModifiedDate":"2012-02-02T00:08:54","indexId":"wri894040","displayToPublicDate":"1994-01-01T00:00:00","publicationYear":"1989","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":"89-4040","title":"Selected water-quality characteristics and flow of ground water in the San Luis basin, including the Conejos River subbasin, Colorado and New Mexico","docAbstract":"Chemical analyses of water from 99 wells and 19 springs in the San Luis basin in Colorado and New Mexico were evaluated to determine selected water quality characteristics as an aid in understanding the flow of groundwater in the basin. The evaluation shows that the distribution of chemical water types in the basin is consistent with chemical changes to be expected along flow paths in rocks typical of those in the basin. The San Luis basin area is underlain by a surficial (< 100-ft-thick) unconfined aquifer and, in turn, by a confining bed and a deeper confined aquifer. Previous studies have indicated that the groundwater system is recharged around the edges of the basin and that groundwater then moves toward discharge areas in the topographically closed part of the basin and along principal streams. The evaluation of water quality data showed that groundwater at the perimeter of the San Luis basin is primarily a calcium bicarbonate type, which is typical in recharge areas. Groundwater near the center of the basin is primarily a sodium bicarbonate type, which is typical of groundwater in downgradient areas. The change in principal cation from calcium to sodium indicates chemical evolution of the water along the groundwater flow path and supports previously developed concepts of groundwater movement in the basin. The exchange of calcium for sodium along the flow path also is assumed to occur in the Conejos River subbasin. Upgradient wells yield calcium bicarbonate type water, whereas downgradient wells yield sodium bicarbonate type water. However, an exception to this relation is found at McIntire Spring, which yields calcium bicarbonate type water from a downgradient location. The source of water discharging from the spring may be the confined aquifer, with hydraulic connection along the Manassa fault. The concentration of dissolved solids in water from both the unconfined and confined aquifers increases downgradient. The increase is dramatic in the closed basin, ranging from < 500 mg/L to > 30 ,000 mg/L. In this area, the normal increase in concentration by dissolution of minerals along the flow path is exceeded by the increase due to evapotranspiration from the shallow water table. (Lantz-PTT)","language":"ENGLISH","publisher":"U.S. Geological Survey ;\r\nU.S. Geological Survey, Books and Open-File Reports Section, Federal Center,","doi":"10.3133/wri894040","usgsCitation":"Williams, R., and Hammond, S., 1989, Selected water-quality characteristics and flow of ground water in the San Luis basin, including the Conejos River subbasin, Colorado and New Mexico: U.S. Geological Survey Water-Resources Investigations Report 89-4040, iv, 43 p. :ill., map ;28 cm., https://doi.org/10.3133/wri894040.","productDescription":"iv, 43 p. :ill., map ;28 cm.","costCenters":[],"links":[{"id":159547,"rank":0,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/wri/1989/4040/report-thumb.jpg"},{"id":59302,"rank":400,"type":{"id":17,"text":"Plate"},"url":"https://pubs.usgs.gov/wri/1989/4040/plate-1.pdf","linkFileType":{"id":1,"text":"pdf"}},{"id":59303,"rank":300,"type":{"id":11,"text":"Document"},"url":"https://pubs.usgs.gov/wri/1989/4040/report.pdf","linkFileType":{"id":1,"text":"pdf"}}],"noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"4f4e49dfe4b07f02db5e3d23","contributors":{"authors":[{"text":"Williams, R.S. Jr.","contributorId":46102,"corporation":false,"usgs":true,"family":"Williams","given":"R.S.","suffix":"Jr.","email":"","affiliations":[],"preferred":false,"id":203397,"contributorType":{"id":1,"text":"Authors"},"rank":1},{"text":"Hammond, S.E.","contributorId":17607,"corporation":false,"usgs":true,"family":"Hammond","given":"S.E.","email":"","affiliations":[],"preferred":false,"id":203396,"contributorType":{"id":1,"text":"Authors"},"rank":2}]}}
,{"id":18958,"text":"ofr89413 - 1989 - Lithology, mineralogy, and paleontology of Quaternary lake deposits in Long Valley Caldera, California","interactions":[],"lastModifiedDate":"2012-02-02T00:07:32","indexId":"ofr89413","displayToPublicDate":"1994-01-01T00:00:00","publicationYear":"1989","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":"89-413","title":"Lithology, mineralogy, and paleontology of Quaternary lake deposits in Long Valley Caldera, California","docAbstract":"Drill cores and cuttings from two drill holes, about 3 km apart, in Long Valley caldera, Mono County, California, were studied using x-ray diffraction and optical methods. A thick sequence of tuffs and lake sediments was encountered in LVCH-1 (1,000 ft deep) and Republic well 66-29 (6,920 ft deep), drilled in the southeast part of the Long Valley caldera. Ostracods, diatoms, and isotopic data indicate that the sediments and tuffs were deposited in a shallow caldera lake which changed in salinity over time. Conditions ranged from very saline in the older lake to fresh in the youngest. The sequence of secondary minerals from top to bottom is: clinoptilolite, mordenite, analcime, K-feldspar (and albite). In some geothermal systems, this sequence of secondary minerals is a function of temperature; however, the paleontological and isotopic data indicate that the change in secondary minerals with increasing depth is due to the older strata being deposited in a more saline environment. No mineralogical evidence of hydrothermal alteration is present, although the high lithium content of some clays and feldspars and the isotopic composition of some sulfate (gypsum) seems to require a hydrothermal source. (Lantz-PTT)","language":"ENGLISH","publisher":"U.S. Geological Survey,","doi":"10.3133/ofr89413","usgsCitation":"Fournier, R., 1989, Lithology, mineralogy, and paleontology of Quaternary lake deposits in Long Valley Caldera, California: U.S. Geological Survey Open-File Report 89-413, v, 97 p. :ill., maps ;28 cm., https://doi.org/10.3133/ofr89413.","productDescription":"v, 97 p. :ill., maps ;28 cm.","costCenters":[],"links":[{"id":151414,"rank":0,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/of/1989/0413/report-thumb.jpg"},{"id":48363,"rank":400,"type":{"id":17,"text":"Plate"},"url":"https://pubs.usgs.gov/of/1989/0413/plate-1.pdf","linkFileType":{"id":1,"text":"pdf"}},{"id":48364,"rank":401,"type":{"id":17,"text":"Plate"},"url":"https://pubs.usgs.gov/of/1989/0413/plate-2.pdf","linkFileType":{"id":1,"text":"pdf"}},{"id":48365,"rank":300,"type":{"id":11,"text":"Document"},"url":"https://pubs.usgs.gov/of/1989/0413/report.pdf","linkFileType":{"id":1,"text":"pdf"}}],"noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"4f4e4a61e4b07f02db635e82","contributors":{"authors":[{"text":"Fournier, R.B.","contributorId":63406,"corporation":false,"usgs":true,"family":"Fournier","given":"R.B.","email":"","affiliations":[],"preferred":false,"id":180053,"contributorType":{"id":1,"text":"Authors"},"rank":1}]}}
,{"id":30420,"text":"wri894168 - 1989 - Selected quality assurance data for water samples collected by the US Geological Survey, Idaho National Engineering Laboratory, Idaho, 1980 to 1988","interactions":[],"lastModifiedDate":"2012-02-02T00:08:55","indexId":"wri894168","displayToPublicDate":"1994-01-01T00:00:00","publicationYear":"1989","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":"89-4168","title":"Selected quality assurance data for water samples collected by the US Geological Survey, Idaho National Engineering Laboratory, Idaho, 1980 to 1988","docAbstract":"Multiple water samples from 115 wells and 3 surface water sites were collected between 1980 and 1988 for the ongoing quality assurance program at the Idaho National Engineering Laboratory. The reported results from the six laboratories involved were analyzed for agreement using descriptive statistics. The constituents and properties included: tritium, plutonium-238, plutonium-239, -240 (undivided), strontium-90, americium-241, cesium-137, total dissolved chromium, selected dissolved trace metals, sodium, chloride, nitrate, selected purgeable organic compounds, and specific conductance. Agreement could not be calculated for purgeable organic compounds, trace metals, some nitrates and blank sample analyses because analytical uncertainties were not consistently reported. However, differences between results for most of these data were calculated. The blank samples were not analyzed for differences. The laboratory results analyzed using descriptive statistics showed a median agreement between all useable data pairs of 95%. (USGS)","language":"ENGLISH","publisher":"Dept. of the Interior, U.S. Geological Survey ;\r\nBooks and Open-File Reports [distributor],","doi":"10.3133/wri894168","usgsCitation":"Wegner, S., 1989, Selected quality assurance data for water samples collected by the US Geological Survey, Idaho National Engineering Laboratory, Idaho, 1980 to 1988: U.S. Geological Survey Water-Resources Investigations Report 89-4168, v, 91 p. :ill. ;28 cm., https://doi.org/10.3133/wri894168.","productDescription":"v, 91 p. :ill. ;28 cm.","costCenters":[],"links":[{"id":159806,"rank":0,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/wri/1989/4168/report-thumb.jpg"},{"id":59188,"rank":300,"type":{"id":11,"text":"Document"},"url":"https://pubs.usgs.gov/wri/1989/4168/report.pdf","linkFileType":{"id":1,"text":"pdf"}}],"noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"4f4e49e5e4b07f02db5e6df9","contributors":{"authors":[{"text":"Wegner, S.J.","contributorId":36950,"corporation":false,"usgs":true,"family":"Wegner","given":"S.J.","email":"","affiliations":[],"preferred":false,"id":203219,"contributorType":{"id":1,"text":"Authors"},"rank":1}]}}
,{"id":19271,"text":"ofr89274 - 1989 - Functional requirements of computer systems for the U.S. Geological Survey, Water Resources Division, 1988-97","interactions":[],"lastModifiedDate":"2012-02-02T00:07:33","indexId":"ofr89274","displayToPublicDate":"1994-01-01T00:00:00","publicationYear":"1989","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":"89-274","title":"Functional requirements of computer systems for the U.S. Geological Survey, Water Resources Division, 1988-97","docAbstract":"Investigating the occurrence, quantity, quality, distribution, and movement of the Nation 's water resources is the principal mission of the U.S. Geological Survey 's Water Resources Division. Reports of these investigations are published and available to the public. To accomplish this mission, the Division requires substantial computer technology to process, store, and analyze data from more than 57,000 hydrologic sites. The Division 's computer resources are organized through the Distributed Information System Program Office that manages the nationwide network of computers. The contract that provides the major computer components for the Water Resources Division 's Distributed information System expires in 1991. Five work groups were organized to collect the information needed to procure a new generation of computer systems for the U. S. Geological Survey, Water Resources Division. Each group was assigned a major Division activity and asked to describe its functional requirements of computer systems for the next decade. The work groups and major activities are: (1) hydrologic information; (2) hydrologic applications; (3) geographic information systems; (4) reports and electronic publishing; and (5) administrative. The work groups identified 42 functions and described their functional requirements for 1988, 1992, and 1997. A few new functions such as Decision Support Systems and Executive Information Systems, were identified, but most are the same as performed today. Although the number of functions will remain about the same, steady growth in the size, complexity, and frequency of many functions is predicted for the next decade. No compensating increase in the Division 's staff is anticipated during this period. To handle the increased workload and perform these functions, new approaches will be developed that use advanced computer technology. The advanced technology is required in a unified, tightly coupled system that will support all functions simultaneously. The new approaches and expanded use of computers will require substantial increases in the quantity and sophistication of the Division 's computer resources. The requirements presented in this report will be used to develop technical specifications that describe the computer resources needed during the 1990's. (USGS)","language":"ENGLISH","publisher":"Dept. of the Interior, U.S. Geological Survey ;\r\nBooks and Open-File Reports [distributor],","doi":"10.3133/ofr89274","usgsCitation":"Hathaway, R., and McNellis, J., 1989, Functional requirements of computer systems for the U.S. Geological Survey, Water Resources Division, 1988-97: U.S. Geological Survey Open-File Report 89-274, iv, 166 p. :ill. ;28 cm., https://doi.org/10.3133/ofr89274.","productDescription":"iv, 166 p. :ill. ;28 cm.","costCenters":[],"links":[{"id":151299,"rank":0,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/of/1989/0274/report-thumb.jpg"},{"id":48734,"rank":300,"type":{"id":11,"text":"Document"},"url":"https://pubs.usgs.gov/of/1989/0274/report.pdf","linkFileType":{"id":1,"text":"pdf"}}],"noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"4f4e4b32e4b07f02db6b4338","contributors":{"authors":[{"text":"Hathaway, R.M.","contributorId":48202,"corporation":false,"usgs":true,"family":"Hathaway","given":"R.M.","email":"","affiliations":[],"preferred":false,"id":180594,"contributorType":{"id":1,"text":"Authors"},"rank":1},{"text":"McNellis, J.M.","contributorId":58662,"corporation":false,"usgs":true,"family":"McNellis","given":"J.M.","email":"","affiliations":[],"preferred":false,"id":180595,"contributorType":{"id":1,"text":"Authors"},"rank":2}]}}
,{"id":15239,"text":"ofr89262 - 1989 - Water-resources activities of the U.S. Geological Survey in Wyoming, fiscal years 1988 and 1989","interactions":[],"lastModifiedDate":"2012-02-02T00:06:52","indexId":"ofr89262","displayToPublicDate":"1994-01-01T00:00:00","publicationYear":"1989","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":"89-262","title":"Water-resources activities of the U.S. Geological Survey in Wyoming, fiscal years 1988 and 1989","docAbstract":"There are two types of water-resources activities of the U.S. Geological Survey in Wyoming: collection of hydrologic data, and water-resources-appraisal projects. During Fiscal Years 1988 and 1989, the work was done in cooperation with 10 State agencies, 5 counties, 3 cities, 2 towns, 1 irrigation district, 2 Indian Tribes, and 8 Federal agencies. Lists and location maps are included for 180 streamflow stations, 16 reservoir stations, 120 surface-water-quality stations, 15 sediment stations, 88 groundwater-level observation wells, and 73 groundwater quality sites, which were in operation during Fiscal Year 1988 and (or) Fiscal Year 1989. During Fiscal Years 1987 and 1988, 17 streamflow stations, 13 surface-water-quality stations, 14 sediment stations, and 7 groundwater level observation wells were discontinued. During Fiscal year 1988 and through the first quarter of Fiscal Year 1989, 21 streamflow stations, 15 surface-water-quality stations, and 3 sediment stations were established or reactivated. Descriptions, location maps, and progress statements are given for 4 data collection projects and 27 water resources-appraisal projects that were active during Fiscal Year 1988 and (or) Fiscal Year 1989. Eleven projects were completed during Fiscal Year 1988 or 1989 and 10 projects that were completed except for the project reports. Also included is a bibliography of reports by U.S. Geological Survey authors about the water resources of Wyoming. (USGS)","language":"ENGLISH","publisher":"U.S. Geological Survey ;\r\nBooks and Open-File Reports Section [distributor],","doi":"10.3133/ofr89262","usgsCitation":"Oden, D.M., 1989, Water-resources activities of the U.S. Geological Survey in Wyoming, fiscal years 1988 and 1989: U.S. Geological Survey Open-File Report 89-262, v, 124 p. :ill. ;28 cm., https://doi.org/10.3133/ofr89262.","productDescription":"v, 124 p. :ill. ;28 cm.","costCenters":[],"links":[{"id":147122,"rank":0,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/of/1989/0262/report-thumb.jpg"},{"id":44186,"rank":300,"type":{"id":11,"text":"Document"},"url":"https://pubs.usgs.gov/of/1989/0262/report.pdf","linkFileType":{"id":1,"text":"pdf"}}],"noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"4f4e49e2e4b07f02db5e4f68","contributors":{"authors":[{"text":"Oden, D. M. (compiler)","contributorId":57083,"corporation":false,"usgs":true,"family":"Oden","given":"D.","suffix":"(compiler)","email":"","middleInitial":"M.","affiliations":[],"preferred":false,"id":170799,"contributorType":{"id":1,"text":"Authors"},"rank":1}]}}
,{"id":31063,"text":"wsp2295B - 1989 - Water-quality data-collection activities in Colorado and Ohio: Phase II- evaluation of 1984 field and laboratory quality-assurance practices","interactions":[{"subject":{"id":12356,"text":"ofr8733 - 1987 - Water-quality data-collection activities in Colorado and Ohio;  Phase II, Evaluation of 1984 field and laboratory quality-assurance practices","indexId":"ofr8733","publicationYear":"1987","noYear":false,"title":"Water-quality data-collection activities in Colorado and Ohio;  Phase II, Evaluation of 1984 field and laboratory quality-assurance practices"},"predicate":"SUPERSEDED_BY","object":{"id":31063,"text":"wsp2295B - 1989 - Water-quality data-collection activities in Colorado and Ohio: Phase II- evaluation of 1984 field and laboratory quality-assurance practices","indexId":"wsp2295B","publicationYear":"1989","noYear":false,"chapter":"B","title":"Water-quality data-collection activities in Colorado and Ohio: Phase II- evaluation of 1984 field and laboratory quality-assurance practices"},"id":1}],"lastModifiedDate":"2012-02-02T00:09:15","indexId":"wsp2295B","displayToPublicDate":"1994-01-01T00:00:00","publicationYear":"1989","noYear":false,"publicationType":{"id":18,"text":"Report"},"publicationSubtype":{"id":5,"text":"USGS Numbered Series"},"seriesTitle":{"id":341,"text":"Water Supply Paper","code":"WSP","active":false,"publicationSubtype":{"id":5}},"seriesNumber":"2295","chapter":"B","title":"Water-quality data-collection activities in Colorado and Ohio: Phase II- evaluation of 1984 field and laboratory quality-assurance practices","language":"ENGLISH","publisher":"U.S.G.P.O. ;For sale by the Books and Open-File Reports Section, U.S. Geological Survey,","doi":"10.3133/wsp2295B","usgsCitation":"Childress, C., Chaney, T.H., Myers, D.A., Norris, J.M., and Hren, J., 1989, Water-quality data-collection activities in Colorado and Ohio: Phase II- evaluation of 1984 field and laboratory quality-assurance practices: U.S. Geological Survey Water Supply Paper 2295, 49 p., https://doi.org/10.3133/wsp2295B.","productDescription":"49 p.","numberOfPages":"49","costCenters":[],"links":[{"id":163627,"rank":0,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/wsp/2295b/report-thumb.jpg"},{"id":59623,"rank":300,"type":{"id":11,"text":"Document"},"url":"https://pubs.usgs.gov/wsp/2295b/report.pdf","linkFileType":{"id":1,"text":"pdf"}}],"noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"4f4e49e3e4b07f02db5e58ac","contributors":{"authors":[{"text":"Childress, Carolyn J. Oblinger","contributorId":57514,"corporation":false,"usgs":true,"family":"Childress","given":"Carolyn J. Oblinger","affiliations":[],"preferred":false,"id":204805,"contributorType":{"id":1,"text":"Authors"},"rank":1},{"text":"Chaney, Thomas H.","contributorId":94712,"corporation":false,"usgs":true,"family":"Chaney","given":"Thomas","email":"","middleInitial":"H.","affiliations":[],"preferred":false,"id":204807,"contributorType":{"id":1,"text":"Authors"},"rank":2},{"text":"Myers, Donna A.","contributorId":18818,"corporation":false,"usgs":true,"family":"Myers","given":"Donna","email":"","middleInitial":"A.","affiliations":[],"preferred":false,"id":204804,"contributorType":{"id":1,"text":"Authors"},"rank":3},{"text":"Norris, J. Michael 0000-0002-7480-0161 mnorris@usgs.gov","orcid":"https://orcid.org/0000-0002-7480-0161","contributorId":1625,"corporation":false,"usgs":true,"family":"Norris","given":"J.","email":"mnorris@usgs.gov","middleInitial":"Michael","affiliations":[{"id":466,"text":"New England Water Science Center","active":true,"usgs":true}],"preferred":true,"id":204803,"contributorType":{"id":1,"text":"Authors"},"rank":4},{"text":"Hren, Janet","contributorId":69554,"corporation":false,"usgs":true,"family":"Hren","given":"Janet","email":"","affiliations":[],"preferred":false,"id":204806,"contributorType":{"id":1,"text":"Authors"},"rank":5}]}}
,{"id":30172,"text":"wri864331 - 1989 - Effect of urban runoff on the quality of lakes in Eagan, Minnesota","interactions":[],"lastModifiedDate":"2018-04-02T11:39:22","indexId":"wri864331","displayToPublicDate":"1994-01-01T00:00:00","publicationYear":"1989","noYear":false,"publicationType":{"id":18,"text":"Report"},"publicationSubtype":{"id":5,"text":"USGS Numbered Series"},"seriesTitle":{"id":342,"text":"Water-Resources Investigations Report","code":"WRI","active":false,"publicationSubtype":{"id":5}},"seriesNumber":"86-4331","title":"Effect of urban runoff on the quality of lakes in Eagan, Minnesota","docAbstract":"<p>Sixteen lakes in the city of Eagan, Minnesota, were sampled during 1982-83 to detect water-quality changes that might have occurred because of urbanization since a previous study conducted during 1972-78. Each of the lakes was sampled five times to determine pH, specific conductance, dissolved oxygen, water temperature, transparency, and concentration of dissolved chloride. Three determinations of chlorophyll were made for each of the lakes near the end of the study, and additional determinations were made for a few lakes of particular interest.</p>\n<p>Most of the lakes have been incorporated into the city's storm-runoff system for use as retention basins during large storms. The chemistry of the lakes appears to be degraded by urban runoff. Chloride concentrations were significantly higher in six lakes than during the previous study, and remained elevated (about 30 milligrams per liter) in four other lakes. The association between increased chloride and specific conductance with runoff from urban areas suggests that the lakes are subject to contamination by chloride commonly present in urban runoff, and chloride concentrations harmful to aquatic life may have been associated with high specific conductance measured in one of the lakes.</p>\n<p>Analysis of the data collected for this study indicate that the chemistry of the lakes changes, adjusting to a variety of influences including (1) alternate loading and flushing by runoff, (2) excessive average-annual precipitation, (3) changing ground-water and lake interactions, and (4) changing land use in the lake watersheds. Some lakes affected by urban runoff had reduced concentrations of total phosphorus; however, other lakes unaffected by urban runoff also had significantly lower phosphorus, suggesting that increased precipitation may have diluted the lake water. Ten phosphorus-loading models tested or developed during the previous study generally were found to be inadequate for describing the results of this study. The trophic status of 12 lakes improved but declined in the other 4 lakes, and productivity increased 38 percent in what had been the least-eutrophic lake.</p>","language":"English","publisher":"U.S. Geological Survey","publisherLocation":"St. Paul, MN","doi":"10.3133/wri864331","collaboration":"Prepared in cooperation with the city of Eagan, Minnesota","usgsCitation":"Tornes, L., 1989, Effect of urban runoff on the quality of lakes in Eagan, Minnesota: U.S. Geological Survey Water-Resources Investigations Report 86-4331, iv, 64 p., https://doi.org/10.3133/wri864331.","productDescription":"iv, 64 p.","onlineOnly":"N","additionalOnlineFiles":"N","costCenters":[{"id":392,"text":"Minnesota Water Science Center","active":true,"usgs":true}],"links":[{"id":119669,"rank":0,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/wri/1986/4331/report-thumb.jpg"},{"id":58973,"rank":300,"type":{"id":11,"text":"Document"},"url":"https://pubs.usgs.gov/wri/1986/4331/report.pdf","linkFileType":{"id":1,"text":"pdf"}}],"country":"United States","state":"Minnesota","city":"Eagan","geographicExtents":"{\n  \"type\": \"FeatureCollection\",\n  \"features\": [\n    {\n      \"type\": \"Feature\",\n      \"properties\": {},\n      \"geometry\": {\n        \"type\": \"Polygon\",\n        \"coordinates\": [\n          [\n            [\n              -93.10895919799805,\n              44.86195288021061\n            ],\n            [\n              -93.10741424560545,\n              44.77464578614771\n            ],\n            [\n              -93.23152542114258,\n              44.77428020677966\n            ],\n            [\n              -93.22998046875,\n              44.8278737920029\n            ],\n            [\n              -93.22551727294922,\n              44.82957822522573\n            ],\n            [\n              -93.21521759033203,\n              44.83615199553088\n            ],\n            [\n              -93.20938110351561,\n              44.84114269070498\n            ],\n            [\n              -93.20680618286133,\n              44.84625466193982\n            ],\n            [\n              -93.20388793945312,\n              44.8523397505366\n            ],\n            [\n              -93.2028579711914,\n              44.858059147643786\n            ],\n            [\n              -93.2025146484375,\n              44.86207455511034\n            ],\n            [\n              -93.18775177001953,\n              44.860736117070026\n            ],\n            [\n              -93.15668106079102,\n              44.861466178040175\n            ],\n            [\n              -93.14809799194336,\n              44.861709529639704\n            ],\n            [\n              -93.1450080871582,\n              44.86243957826663\n            ],\n            [\n              -93.13093185424805,\n              44.862561252137745\n            ],\n            [\n              -93.11256408691406,\n              44.86243957826663\n            ],\n            [\n              -93.10895919799805,\n              44.86195288021061\n            ]\n          ]\n        ]\n      }\n    }\n  ]\n}","noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"4f4e4b24e4b07f02db6ae799","contributors":{"authors":[{"text":"Tornes, L. H.","contributorId":103675,"corporation":false,"usgs":true,"family":"Tornes","given":"L. H.","affiliations":[],"preferred":false,"id":202803,"contributorType":{"id":1,"text":"Authors"},"rank":1}]}}
,{"id":30332,"text":"wri884215 - 1989 - Procedure for evaluating observation-well networks in Wyoming, and application to northeastern Wyoming, 1986","interactions":[],"lastModifiedDate":"2012-02-02T00:08:51","indexId":"wri884215","displayToPublicDate":"1994-01-01T00:00:00","publicationYear":"1989","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":"88-4215","title":"Procedure for evaluating observation-well networks in Wyoming, and application to northeastern Wyoming, 1986","docAbstract":"A sequence of steps was developed for evaluating and modifying the existing, long-term, observation-well network in any part of Wyoming. The State was subdivided geographically into nine groundwater areas, including the northeastern Wyoming groundwater area, based on major structural features. Northeastern Wyoming was the first of the nine areas to be evaluated using these procedures. The stratigraphic units of Wyoming were grouped into five rock units on the basis of age, similar depositional environments, and water-yielding properties. Activities likely to affect groundwater in northeastern Wyoming were evaluated. The most important monitoring needs in the area are related to: (1) Oil-field waterflooding; (2) surface mining of coal; (3) increasing municipal use of groundwater, and (4) need for general resource information. The 18 observation wells in the existing (1986) network meet most of the needs identified. Seven additional wells need to be added to the network, whereas four wells in the network can be discontinued. Water level data from the 18 observation wells are presented by county. Maps and hydrographs are accompanied by brief discussions of information related to the records obtained. (USGS)","language":"ENGLISH","publisher":"Dept. of the Interior, U.S. Geological Survey ;\r\nBooks and Open-File Reports [distributor],","doi":"10.3133/wri884215","usgsCitation":"Wallace, J., and Crist, M.A., 1989, Procedure for evaluating observation-well networks in Wyoming, and application to northeastern Wyoming, 1986: U.S. Geological Survey Water-Resources Investigations Report 88-4215, iv, 29 p. :ill. ;28 cm., https://doi.org/10.3133/wri884215.","productDescription":"iv, 29 p. :ill. ;28 cm.","costCenters":[],"links":[{"id":159290,"rank":0,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/wri/1988/4215/report-thumb.jpg"},{"id":59130,"rank":300,"type":{"id":11,"text":"Document"},"url":"https://pubs.usgs.gov/wri/1988/4215/report.pdf","linkFileType":{"id":1,"text":"pdf"}}],"noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"4f4e4b06e4b07f02db69a1b8","contributors":{"authors":[{"text":"Wallace, J.C.","contributorId":25944,"corporation":false,"usgs":true,"family":"Wallace","given":"J.C.","email":"","affiliations":[],"preferred":false,"id":203074,"contributorType":{"id":1,"text":"Authors"},"rank":1},{"text":"Crist, M. A.","contributorId":84799,"corporation":false,"usgs":true,"family":"Crist","given":"M.","email":"","middleInitial":"A.","affiliations":[],"preferred":false,"id":203075,"contributorType":{"id":1,"text":"Authors"},"rank":2}]}}
,{"id":55821,"text":"wdrNM881 - 1989 - Water resources data, New Mexico, water year 1988","interactions":[],"lastModifiedDate":"2013-07-15T13:33:24","indexId":"wdrNM881","displayToPublicDate":"1994-01-01T00:00:00","publicationYear":"1989","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":"NM-88-1","title":"Water resources data, New Mexico, water year 1988","docAbstract":"Water resources data for the 1988 water year for New Mexico consist of records of discharge and water quality of streams; stage, contents and water quality of lakes and reservoirs; and water levels and water quality in wells and springs. This report contains discharge records for 165 gaging stations; stage and contents for 26 lakes and reservoirs; water quality for 64 gaging stations and 76 wells; and water levels at 105 observation wells. Also included are 108 crest-stage partial-record stations. Additional water data were collected at various sites, not involved in the systematic data collection program, and are published as miscellaneous measurements. Also, one seepage investigation is published this year. These data represent that part of the National Water Data System collected by the U.S. Geological Survey and cooperating State and Federal agencies in New Mexico.","language":"ENGLISH","publisher":"U.S. Geological Survey","doi":"10.3133/wdrNM881","collaboration":"Prepared in cooperation with the State of New Mexico and with other agencies","usgsCitation":"Borland, J.P., and Beal, L.V., 1989, Water resources data, New Mexico, water year 1988: U.S. Geological Survey Water Data Report NM-88-1, 504 p., https://doi.org/10.3133/wdrNM881.","productDescription":"504 p.","costCenters":[{"id":629,"text":"Water Resources Division","active":false,"usgs":true}],"links":[{"id":185373,"rank":0,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/thumbnails/usgs_thumb.jpg"},{"id":270299,"type":{"id":11,"text":"Document"},"url":"https://pubs.usgs.gov/wdr/1988/nm-88-1/report.pdf"}],"country":"United States","state":"New Mexico","geographicExtents":"{ \"type\": \"FeatureCollection\", \"features\": [ { \"type\": \"Feature\", \"properties\": {}, \"geometry\": { \"type\": \"Polygon\", \"coordinates\": [ [ [ -109.0502,31.3322 ], [ -109.0502,37.0003 ], [ -103.002,37.0003 ], [ -103.002,31.3322 ], [ -109.0502,31.3322 ] ] ] } } ] }","noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"4f4e49f5e4b07f02db5f0f6d","contributors":{"authors":[{"text":"Borland, John P.","contributorId":88249,"corporation":false,"usgs":true,"family":"Borland","given":"John","email":"","middleInitial":"P.","affiliations":[],"preferred":false,"id":254323,"contributorType":{"id":1,"text":"Authors"},"rank":1},{"text":"Beal, Linda V.","contributorId":26367,"corporation":false,"usgs":true,"family":"Beal","given":"Linda","email":"","middleInitial":"V.","affiliations":[],"preferred":false,"id":254322,"contributorType":{"id":1,"text":"Authors"},"rank":2}]}}
,{"id":30224,"text":"wri884197 - 1989 - Lithologic, geophysical, and well-construction data for observation wells in the Melton Valley area, Oak Ridge Reservation, Tennessee","interactions":[],"lastModifiedDate":"2012-02-02T00:08:54","indexId":"wri884197","displayToPublicDate":"1994-01-01T00:00:00","publicationYear":"1989","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":"88-4197","title":"Lithologic, geophysical, and well-construction data for observation wells in the Melton Valley area, Oak Ridge Reservation, Tennessee","docAbstract":"Nineteen wells were installed at nine sites in the Melton Valley area. The wells are intended to provide information on water levels in both regolith and bedrock, aquifer characteristics, and subsurface lithology. Well depths range from 24 to 86 ft for shallow wells, and from 126 to 301 ft for deep wells. Four inch diameter cores were obtained from four of the deep wells. Caliper, gamma, neutron, and gamma-gamma density borehole geophysical logs were obtained for each deep well. Lithologic description of cores and analysis of geophysical logs indicate that one deep well (UA2) is completed entirely within the Nolichucky Shale; one deep well (UD2) is completely entirely within the Pumpkin Valley Shale; two deep wells (UB2, UE2) are completed entirely within the Maryville Limestone; four deep wells (UF2, UG2, UH2, UI2) penetrate both the Nolichucky Shale and the Maryville Limestone. Well UC2, located near the crest of Haw Ridge, penetrates an imbricate splay of the Copper Creek thrust fault, which places the older Rome Formation above the younger Chickamauga Limestone, at a depth of about 100 to 117 ft. (USGS)","language":"ENGLISH","publisher":"U.S. Geological Survey,","doi":"10.3133/wri884197","usgsCitation":"Tucci, P., and Hanchar, D., 1989, Lithologic, geophysical, and well-construction data for observation wells in the Melton Valley area, Oak Ridge Reservation, Tennessee: U.S. Geological Survey Water-Resources Investigations Report 88-4197, iv, 22 p. :ill., one map ;28 cm., https://doi.org/10.3133/wri884197.","productDescription":"iv, 22 p. :ill., one map ;28 cm.","costCenters":[],"links":[{"id":124027,"rank":0,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/wri/1988/4197/report-thumb.jpg"},{"id":59007,"rank":300,"type":{"id":11,"text":"Document"},"url":"https://pubs.usgs.gov/wri/1988/4197/report.pdf","linkFileType":{"id":1,"text":"pdf"}}],"noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"4f4e4a61e4b07f02db635af9","contributors":{"authors":[{"text":"Tucci, Patrick ptucci@usgs.gov","contributorId":926,"corporation":false,"usgs":true,"family":"Tucci","given":"Patrick","email":"ptucci@usgs.gov","affiliations":[],"preferred":true,"id":202888,"contributorType":{"id":1,"text":"Authors"},"rank":1},{"text":"Hanchar, D. W.","contributorId":87986,"corporation":false,"usgs":true,"family":"Hanchar","given":"D. W.","affiliations":[],"preferred":false,"id":202889,"contributorType":{"id":1,"text":"Authors"},"rank":2}]}}
,{"id":55586,"text":"wdrLA881 - 1989 - Water resources data, Louisiana, water year 1988","interactions":[],"lastModifiedDate":"2025-02-10T17:21:48.928","indexId":"wdrLA881","displayToPublicDate":"1994-01-01T00:00:00","publicationYear":"1989","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":"LA-88-1","title":"Water resources data, Louisiana, water year 1988","docAbstract":"<p>Water resources data for the 1988 water year for Louisiana 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 contains records for water discharge at 61 gaging stations; stage only for 19 gaging stations and 7 lakes; water quality for 39 surface-water stations (including 15 gaging stations), and 118 wells; and water levels for 215 observation wells. Also included are data for 103 crest-stage and flood-profile partial-record stations. Additional water data were collected at various sites not involved in the systematic data-collection program, and are published as miscellaneous measurements. These data represent that part of the National Water Data System operated by the U.S. Geological Survey and cooperating State and Federal agencies in Louisiana.</p>","language":"English","publisher":"U.S. Geological Survey","doi":"10.3133/wdrLA881","collaboration":"Prepared in cooperation with the Louisiana Department of Transportation and Development and with other State and Federal agencies","usgsCitation":"Arcement, G., Dantin, L., Garrison, C., and Stuart, C., 1989, Water resources data, Louisiana, water year 1988: U.S. Geological Survey Water Data Report LA-88-1, x, 413 p., https://doi.org/10.3133/wdrLA881.","productDescription":"x, 413 p.","costCenters":[],"links":[{"id":481881,"rank":2,"type":{"id":11,"text":"Document"},"url":"https://pubs.usgs.gov/wdr/1988/la-88-1/report.pdf","linkFileType":{"id":1,"text":"pdf"}},{"id":182043,"rank":1,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/thumbnails/usgs_thumb.jpg"}],"country":"United States","state":"Louisiana","geographicExtents":"{\"type\":\"FeatureCollection\",\"features\":[{\"type\":\"Feature\",\"geometry\":{\"type\":\"MultiPolygon\",\"coordinates\":[[[[-88.865067,29.752714],[-88.940346,29.657234],[-88.944435,29.658806],[-88.941605,29.674833],[-88.911751,29.699348],[-88.873611,29.758043],[-88.867973,29.79133],[-88.84301,29.82596],[-88.836296,29.855221],[-88.843277,29.86381],[-88.8312,29.878839],[-88.828247,29.920717],[-88.837379,29.944878],[-88.835495,29.974138],[-88.840866,29.995613],[-88.857368,30.027826],[-88.881454,30.053202],[-88.855583,30.034414],[-88.841225,30.012789],[-88.824158,29.970461],[-88.817017,29.93425],[-88.818146,29.889109],[-88.826538,29.847092],[-88.865067,29.752714]]],[[[-89.486709,29.621003],[-89.535202,29.648567],[-89.621109,29.657101],[-89.632698,29.671724],[-89.64975,29.672941],[-89.641228,29.635773],[-89.647324,29.625414],[-89.684486,29.624804],[-89.688141,29.615055],[-89.684486,29.602867],[-89.668648,29.580322],[-89.684486,29.563263],[-89.681092,29.534487],[-89.699698,29.523423],[-89.700501,29.515967],[-89.665813,29.49002],[-89.63533,29.489294],[-89.617558,29.468298],[-89.596533,29.456303],[-89.589536,29.437662],[-89.577096,29.433692],[-89.548686,29.465723],[-89.528429,29.454702],[-89.531943,29.425679],[-89.508551,29.386168],[-89.487308,29.393346],[-89.47714,29.411241],[-89.457303,29.393148],[-89.380001,29.391785],[-89.355528,29.381569],[-89.340304,29.381412],[-89.336589,29.378228],[-89.347615,29.365],[-89.350694,29.349544],[-89.32317,29.343982],[-89.303766,29.357455],[-89.283028,29.356467],[-89.2653,29.345352],[-89.24087,29.310081],[-89.224192,29.313792],[-89.200389,29.344418],[-89.189354,29.345061],[-89.179547,29.339608],[-89.165015,29.303039],[-89.140275,29.291085],[-89.129688,29.265632],[-89.100106,29.25022],[-89.095544,29.238028],[-89.105833,29.231608],[-89.106244,29.215912],[-89.10065,29.206314],[-89.090724,29.199992],[-89.068265,29.204166],[-89.067371,29.208636],[-89.029103,29.220956],[-89.015192,29.211561],[-89.000674,29.180091],[-89.00529,29.164949],[-89.013254,29.16328],[-89.024269,29.170043],[-89.047233,29.157833],[-89.03873,29.14238],[-89.032004,29.144747],[-89.023942,29.1337],[-89.051953,29.106554],[-89.062335,29.070234],[-89.09126,29.066931],[-89.105009,29.073641],[-89.121542,29.069074],[-89.143453,29.047591],[-89.162326,29.011713],[-89.16985,29.008703],[-89.186061,29.017993],[-89.18215,29.025486],[-89.189893,29.032635],[-89.197871,29.029701],[-89.211144,29.040813],[-89.217201,29.067275],[-89.225865,29.07866],[-89.23631,29.084605],[-89.254726,29.083261],[-89.25364,29.064954],[-89.259354,29.058358],[-89.29109,29.053097],[-89.315389,29.039081],[-89.32485,29.013805],[-89.338249,29.012935],[-89.383814,28.947434],[-89.41148,28.925011],[-89.419865,28.929709],[-89.408157,28.965341],[-89.398104,28.977016],[-89.375049,28.985368],[-89.334735,29.040335],[-89.354798,29.072543],[-89.374522,29.084174],[-89.405654,29.086936],[-89.411154,29.105838],[-89.409371,29.127855],[-89.432932,29.149023],[-89.455829,29.190991],[-89.482844,29.215053],[-89.5366,29.236212],[-89.606651,29.252023],[-89.671781,29.289028],[-89.697258,29.296679],[-89.782149,29.311132],[-89.850305,29.311768],[-89.853699,29.34064],[-89.820824,29.377486],[-89.816155,29.393518],[-89.826049,29.415589],[-89.843553,29.421677],[-89.845075,29.434615],[-89.832898,29.463536],[-89.849642,29.477996],[-89.902179,29.460011],[-89.932598,29.429288],[-89.95543,29.428527],[-89.991961,29.463536],[-90.01251,29.462775],[-90.032298,29.427005],[-90.029468,29.388136],[-90.036374,29.363661],[-90.031815,29.344251],[-90.034275,29.322661],[-90.028536,29.307083],[-90.013778,29.30271],[-90.009678,29.294785],[-90.019517,29.282213],[-90.057094,29.281331],[-90.060511,29.267729],[-90.070622,29.262537],[-90.101231,29.259804],[-90.096038,29.240673],[-90.073355,29.227282],[-90.073355,29.210611],[-90.04291,29.211765],[-90.005718,29.240627],[-89.969981,29.255753],[-89.959509,29.267677],[-89.951175,29.266124],[-89.950756,29.260801],[-90.022029,29.216065],[-90.104162,29.150407],[-90.174273,29.105301],[-90.223587,29.085075],[-90.245283,29.085824],[-90.348768,29.057817],[-90.349891,29.063681],[-90.325514,29.075138],[-90.29293,29.078761],[-90.253141,29.093772],[-90.250044,29.108067],[-90.234235,29.110268],[-90.234405,29.128824],[-90.248629,29.13837],[-90.280516,29.142521],[-90.27832,29.150691],[-90.302846,29.175098],[-90.300885,29.196171],[-90.293183,29.199789],[-90.275851,29.193668],[-90.271251,29.204639],[-90.286621,29.225694],[-90.311663,29.237954],[-90.311523,29.256374],[-90.332796,29.276956],[-90.367166,29.274128],[-90.372565,29.258923],[-90.387924,29.252786],[-90.383857,29.235606],[-90.399465,29.201046],[-90.432912,29.188132],[-90.443954,29.19583],[-90.472489,29.192688],[-90.467233,29.202549],[-90.494928,29.216713],[-90.46832,29.227532],[-90.462866,29.249809],[-90.450674,29.263739],[-90.510555,29.290925],[-90.526216,29.276492],[-90.552005,29.278512],[-90.565436,29.285111],[-90.582525,29.276037],[-90.589724,29.248521],[-90.583924,29.242886],[-90.565378,29.242475],[-90.544547,29.230683],[-90.544311,29.224292],[-90.556501,29.219913],[-90.560889,29.204261],[-90.618413,29.20329],[-90.624161,29.210366],[-90.633819,29.209128],[-90.645612,29.175867],[-90.636973,29.164572],[-90.647042,29.12858],[-90.677724,29.118742],[-90.700893,29.12147],[-90.718035,29.116611],[-90.731239,29.122886],[-90.764189,29.113374],[-90.773458,29.100133],[-90.799444,29.087377],[-90.803699,29.063709],[-90.79872,29.054841],[-90.765188,29.049403],[-90.7253,29.066616],[-90.692205,29.059607],[-90.63924,29.072848],[-90.637495,29.066608],[-90.730899,29.042259],[-90.839345,29.039167],[-90.844849,29.048721],[-90.841226,29.054266],[-90.844593,29.06728],[-90.862757,29.094863],[-90.877583,29.104891],[-90.898215,29.131342],[-90.961278,29.180817],[-90.981458,29.171211],[-91.000096,29.169481],[-91.023955,29.174784],[-91.031786,29.182188],[-91.094015,29.187711],[-91.129141,29.215863],[-91.199647,29.221287],[-91.278792,29.247776],[-91.334885,29.298775],[-91.33275,29.305816],[-91.291821,29.311357],[-91.276647,29.329825],[-91.266589,29.361218],[-91.251546,29.368659],[-91.238515,29.371999],[-91.222377,29.360703],[-91.207299,29.360703],[-91.197465,29.369882],[-91.200087,29.38955],[-91.218463,29.407235],[-91.211999,29.420931],[-91.221166,29.436421],[-91.258226,29.446954],[-91.265649,29.472362],[-91.2813,29.481547],[-91.294325,29.476894],[-91.335742,29.485886],[-91.356625,29.515191],[-91.402214,29.511914],[-91.420449,29.515745],[-91.447345,29.544749],[-91.468748,29.544299],[-91.517274,29.52974],[-91.531021,29.531543],[-91.525523,29.551904],[-91.537445,29.565888],[-91.553537,29.632766],[-91.570589,29.638312],[-91.625114,29.626195],[-91.648941,29.633635],[-91.627286,29.662132],[-91.626826,29.684753],[-91.618479,29.710816],[-91.621512,29.735429],[-91.632829,29.742576],[-91.667128,29.745822],[-91.710935,29.738993],[-91.737253,29.74937],[-91.752259,29.748264],[-91.783674,29.740689],[-91.85864,29.703121],[-91.88075,29.710839],[-91.875637,29.722316],[-91.878355,29.751025],[-91.859151,29.783331],[-91.854677,29.807436],[-91.869998,29.828328],[-91.889118,29.836023],[-91.90689,29.83094],[-91.915989,29.815654],[-91.940723,29.817008],[-91.983871,29.794516],[-92.056398,29.772313],[-92.107486,29.744429],[-92.144431,29.716418],[-92.149349,29.697052],[-92.111787,29.62177],[-92.093419,29.618694],[-92.02532,29.625647],[-92.000371,29.613143],[-91.965031,29.608019],[-91.935024,29.612239],[-91.922825,29.633173],[-91.898996,29.63701],[-91.882318,29.62977],[-91.863018,29.633739],[-91.841294,29.62962],[-91.838297,29.616041],[-91.821693,29.606049],[-91.784976,29.595204],[-91.774686,29.576387],[-91.712002,29.56474],[-91.711654,29.55427],[-91.765448,29.520844],[-91.771927,29.504871],[-91.770516,29.488953],[-91.782387,29.482882],[-91.800121,29.486828],[-91.821576,29.473925],[-91.8385,29.478874],[-91.862324,29.502393],[-91.878746,29.502937],[-91.906175,29.518052],[-91.969312,29.536893],[-92.02681,29.566805],[-92.046316,29.584362],[-92.158624,29.581616],[-92.21259,29.562479],[-92.25186,29.539354],[-92.309357,29.533026],[-92.402165,29.551269],[-92.61627,29.578729],[-92.744126,29.617608],[-92.974305,29.71398],[-93.088182,29.749125],[-93.226934,29.777519],[-93.295573,29.775071],[-93.344993,29.759618],[-93.475252,29.769242],[-93.68364,29.747153],[-93.766048,29.7295],[-93.837971,29.690619],[-93.87002,29.735482],[-93.891637,29.744618],[-93.893862,29.767289],[-93.926504,29.78956],[-93.927992,29.80964],[-93.91636,29.824968],[-93.86357,29.857177],[-93.838374,29.882855],[-93.818998,29.914822],[-93.807815,29.954549],[-93.786935,29.99058],[-93.741078,30.021571],[-93.737446,30.037283],[-93.722791,30.051162],[-93.70082,30.056274],[-93.70058,30.063666],[-93.716405,30.069122],[-93.734085,30.08613],[-93.702436,30.112721],[-93.701252,30.137376],[-93.69498,30.135185],[-93.688212,30.141376],[-93.717397,30.193439],[-93.720946,30.209852],[-93.705083,30.242752],[-93.706608,30.281187],[-93.714319,30.294282],[-93.738699,30.303794],[-93.765822,30.333318],[-93.756352,30.356166],[-93.757654,30.390423],[-93.722314,30.420729],[-93.702665,30.429947],[-93.6978,30.440583],[-93.716678,30.494006],[-93.710117,30.5064],[-93.714322,30.518562],[-93.740253,30.539569],[-93.729195,30.544842],[-93.727844,30.57407],[-93.712454,30.588479],[-93.681235,30.596102],[-93.6831,30.640763],[-93.654971,30.670184],[-93.629904,30.67994],[-93.609544,30.723139],[-93.619129,30.742002],[-93.607757,30.757657],[-93.592828,30.763986],[-93.584265,30.796663],[-93.563243,30.806218],[-93.554057,30.824941],[-93.558608,30.868822],[-93.567451,30.878524],[-93.567788,30.888302],[-93.556493,30.901451],[-93.551942,30.918646],[-93.530936,30.924534],[-93.526245,30.939411],[-93.549841,30.967118],[-93.567972,30.977981],[-93.571906,30.987614],[-93.566017,31.004567],[-93.539526,31.008498],[-93.516943,31.023662],[-93.516407,31.02955],[-93.532069,31.055264],[-93.52301,31.065241],[-93.526044,31.070773],[-93.546644,31.082989],[-93.551034,31.091111],[-93.549717,31.10516],[-93.539619,31.121844],[-93.544888,31.148844],[-93.53683,31.15862],[-93.533307,31.184463],[-93.55254,31.185605],[-93.588503,31.165581],[-93.598828,31.174679],[-93.607288,31.205403],[-93.604319,31.220794],[-93.616007,31.23396],[-93.613942,31.259375],[-93.620343,31.271025],[-93.642516,31.269508],[-93.668928,31.297975],[-93.68688,31.305166],[-93.663892,31.361953],[-93.66892,31.3664],[-93.671644,31.393352],[-93.704879,31.410881],[-93.697603,31.428409],[-93.70093,31.437784],[-93.749476,31.46869],[-93.74987,31.478929],[-93.730998,31.492119],[-93.726736,31.5116],[-93.739318,31.51505],[-93.743376,31.525196],[-93.780835,31.525384],[-93.798087,31.534044],[-93.818582,31.554826],[-93.834923,31.58621],[-93.838057,31.606795],[-93.827852,31.616551],[-93.818717,31.614556],[-93.816838,31.622509],[-93.818037,31.647892],[-93.826462,31.666919],[-93.804479,31.685664],[-93.802452,31.693186],[-93.814587,31.707444],[-93.819048,31.728858],[-93.830647,31.745811],[-93.822598,31.773559],[-93.834649,31.783309],[-93.839951,31.798597],[-93.874761,31.821661],[-93.874822,31.840611],[-93.884117,31.847606],[-93.889197,31.867693],[-93.901888,31.880063],[-93.904766,31.890599],[-93.927672,31.891497],[-93.938002,31.906917],[-93.971712,31.920384],[-94.018664,31.990843],[-94.029283,31.995865],[-94.041833,31.992402],[-94.042964,33.019219],[-93.073167,33.017898],[-91.166073,33.004106],[-91.173308,32.986088],[-91.201842,32.961212],[-91.199415,32.952314],[-91.214027,32.93032],[-91.199775,32.908512],[-91.170235,32.899391],[-91.15169,32.901935],[-91.134041,32.917676],[-91.131304,32.926919],[-91.137863,32.952756],[-91.130721,32.962257],[-91.137524,32.96955],[-91.135517,32.979657],[-91.111757,32.988361],[-91.09693,32.986412],[-91.080355,32.962794],[-91.081913,32.944768],[-91.064804,32.926464],[-91.064449,32.901064],[-91.070602,32.888659],[-91.105631,32.858396],[-91.143559,32.844739],[-91.161669,32.812465],[-91.164397,32.785821],[-91.157614,32.776033],[-91.165328,32.751301],[-91.154461,32.742339],[-91.123152,32.742798],[-91.054481,32.722259],[-91.063946,32.702926],[-91.118258,32.674075],[-91.152081,32.641508],[-91.151318,32.615919],[-91.141148,32.597209],[-91.119854,32.584795],[-91.049796,32.607188],[-91.038415,32.636443],[-91.025769,32.646573],[-91.014286,32.640482],[-91.0035,32.624845],[-91.010228,32.601927],[-91.03617,32.579556],[-91.080398,32.556442],[-91.061685,32.536448],[-90.994481,32.506331],[-90.988278,32.49119],[-91.004206,32.48214],[-91.038106,32.49044],[-91.093741,32.549128],[-91.116708,32.500139],[-91.116008,32.48314],[-91.095308,32.458741],[-91.052907,32.438442],[-91.029606,32.433542],[-90.993863,32.45085],[-90.96959,32.43949],[-90.966255,32.421027],[-90.99408,32.403862],[-91.004506,32.368144],[-90.993625,32.354047],[-90.912363,32.339454],[-90.897762,32.35436],[-90.89206,32.370579],[-90.878289,32.374548],[-90.882161,32.357552],[-90.905173,32.315497],[-90.933991,32.290343],[-90.951351,32.283199],[-90.963079,32.296285],[-90.979475,32.293702],[-90.982985,32.270294],[-90.969403,32.25252],[-90.98029,32.243601],[-90.983434,32.221305],[-90.991227,32.214662],[-91.001192,32.215173],[-91.021507,32.236149],[-91.039007,32.242349],[-91.050307,32.237949],[-91.061408,32.21865],[-91.071108,32.22605],[-91.083708,32.22645],[-91.113009,32.20655],[-91.133587,32.213432],[-91.162062,32.199035],[-91.174552,32.154978],[-91.165452,32.13429],[-91.113866,32.125731],[-91.08163,32.133992],[-91.053175,32.124237],[-91.048507,32.150152],[-91.058907,32.171251],[-91.057647,32.177354],[-91.050207,32.178451],[-91.00619,32.156957],[-91.004106,32.146152],[-91.017606,32.125153],[-91.030799,32.120566],[-91.034707,32.101053],[-91.080008,32.079154],[-91.082308,32.047555],[-91.103708,32.050255],[-91.139309,32.081754],[-91.16031,32.070354],[-91.16131,32.059755],[-91.15141,32.049255],[-91.088108,32.034455],[-91.075908,32.016828],[-91.104108,31.990357],[-91.16441,31.982557],[-91.18481,31.965557],[-91.19321,31.935658],[-91.18471,31.935058],[-91.18321,31.916159],[-91.20101,31.909159],[-91.234899,31.876863],[-91.267712,31.86266],[-91.266612,31.851161],[-91.245624,31.833165],[-91.255611,31.812662],[-91.269212,31.809162],[-91.284912,31.818362],[-91.293413,31.86016],[-91.333814,31.853261],[-91.345714,31.842861],[-91.365529,31.761628],[-91.355214,31.758063],[-91.325973,31.76151],[-91.286045,31.772062],[-91.263043,31.766995],[-91.259611,31.76129],[-91.263406,31.754468],[-91.275545,31.745515],[-91.338663,31.750005],[-91.365034,31.748184],[-91.371804,31.742948],[-91.397115,31.711364],[-91.395715,31.644165],[-91.401015,31.620365],[-91.421116,31.611565],[-91.436716,31.612665],[-91.474318,31.625365],[-91.497665,31.645371],[-91.515462,31.630372],[-91.517233,31.61346],[-91.488618,31.587466],[-91.466317,31.586066],[-91.422716,31.597065],[-91.403915,31.589766],[-91.405415,31.576466],[-91.414915,31.562166],[-91.443916,31.542466],[-91.479718,31.530366],[-91.511217,31.532612],[-91.52292,31.519841],[-91.515157,31.50338],[-91.518148,31.483483],[-91.513366,31.444396],[-91.500046,31.42052],[-91.472065,31.395925],[-91.471098,31.376917],[-91.47887,31.364955],[-91.504163,31.36495],[-91.521836,31.37517],[-91.532336,31.390275],[-91.539458,31.414021],[-91.537002,31.423184],[-91.545013,31.433026],[-91.565179,31.423447],[-91.576265,31.410498],[-91.578334,31.399067],[-91.568953,31.377629],[-91.55568,31.386413],[-91.546207,31.38248],[-91.548967,31.347255],[-91.507977,31.312943],[-91.508858,31.291644],[-91.515614,31.27821],[-91.564192,31.261633],[-91.637672,31.26768],[-91.654027,31.255753],[-91.652019,31.242691],[-91.644356,31.234414],[-91.601616,31.208573],[-91.588939,31.188959],[-91.591502,31.173118],[-91.624217,31.133729],[-91.626476,31.119125],[-91.61857,31.107328],[-91.56415,31.06683],[-91.559907,31.054119],[-91.564397,31.038965],[-91.578413,31.02403],[-91.636942,30.999416],[-89.728147,31.002431],[-89.73554,30.999715],[-89.728563,30.994396],[-89.736086,30.974446],[-89.727072,30.967395],[-89.735686,30.966573],[-89.756333,30.943498],[-89.744448,30.920577],[-89.750073,30.91293],[-89.7626,30.913736],[-89.758719,30.897319],[-89.773553,30.896862],[-89.770027,30.882254],[-89.779194,30.875185],[-89.768237,30.866392],[-89.771722,30.854677],[-89.783384,30.856022],[-89.780947,30.848542],[-89.790805,30.832131],[-89.781168,30.820123],[-89.785894,30.815962],[-89.800049,30.819078],[-89.804065,30.803247],[-89.811171,30.798921],[-89.806763,30.789069],[-89.816418,30.796054],[-89.821078,30.792523],[-89.831537,30.76761],[-89.826053,30.742322],[-89.816075,30.739366],[-89.83687,30.734661],[-89.836945,30.728201],[-89.828061,30.725018],[-89.83006,30.71631],[-89.845801,30.707314],[-89.835848,30.699555],[-89.835478,30.691166],[-89.847201,30.670038],[-89.837894,30.672514],[-89.841787,30.665557],[-89.852263,30.662934],[-89.836047,30.657298],[-89.821868,30.644024],[-89.818081,30.634019],[-89.823278,30.60823],[-89.814563,30.606152],[-89.818527,30.592688],[-89.807118,30.587337],[-89.808184,30.568795],[-89.790318,30.567524],[-89.803887,30.560581],[-89.794532,30.556554],[-89.791046,30.545046],[-89.780246,30.544607],[-89.775355,30.538848],[-89.768133,30.51502],[-89.76057,30.515761],[-89.758575,30.505942],[-89.726154,30.49256],[-89.715886,30.477797],[-89.68341,30.451793],[-89.678514,30.414012],[-89.683686,30.405873],[-89.657191,30.356515],[-89.629727,30.339287],[-89.626606,30.315457],[-89.639872,30.307281],[-89.64344,30.287682],[-89.631411,30.279662],[-89.631789,30.256924],[-89.614156,30.244595],[-89.615856,30.223195],[-89.596655,30.211796],[-89.574454,30.181697],[-89.562253,30.182397],[-89.541453,30.195397],[-89.533352,30.194797],[-89.524504,30.180753],[-89.537493,30.171745],[-89.562825,30.168667],[-89.587062,30.150648],[-89.617542,30.156422],[-89.640989,30.138612],[-89.656986,30.118381],[-89.678156,30.10829],[-89.683712,30.076018],[-89.72957,30.059628],[-89.731452,30.05104],[-89.7163,30.02811],[-89.724649,30.022454],[-89.733323,30.022054],[-89.763216,30.042108],[-89.818561,30.043328],[-89.857558,30.004439],[-89.844202,29.955645],[-89.829023,29.939228],[-89.804463,29.932588],[-89.748492,29.945831],[-89.727933,29.95878],[-89.71291,29.946349],[-89.742727,29.935894],[-89.746273,29.928221],[-89.742479,29.90817],[-89.711158,29.879287],[-89.692004,29.868722],[-89.660568,29.862909],[-89.613159,29.87216],[-89.598129,29.881409],[-89.591194,29.897018],[-89.592346,29.917253],[-89.574997,29.959455],[-89.574425,29.983738],[-89.58136,29.994722],[-89.501587,30.034037],[-89.494064,30.040972],[-89.499275,30.058893],[-89.493484,30.072191],[-89.481926,30.079128],[-89.458946,30.06345],[-89.418465,30.049747],[-89.372375,30.054729],[-89.368637,30.047256],[-89.372375,30.036671],[-89.422813,30.015495],[-89.432785,30.008022],[-89.433411,29.991205],[-89.432785,29.978752],[-89.40538,29.965672],[-89.379227,29.963804],[-89.378601,29.919588],[-89.368019,29.911491],[-89.331894,29.91585],[-89.315453,29.923208],[-89.273315,29.99382],[-89.250534,30.002361],[-89.243706,29.997236],[-89.249969,29.975597],[-89.218071,29.97275],[-89.231178,29.925484],[-89.244843,29.93004],[-89.280144,29.924915],[-89.318306,29.898149],[-89.322289,29.887333],[-89.289253,29.880499],[-89.241425,29.88961],[-89.236298,29.886763],[-89.236298,29.877081],[-89.269897,29.859997],[-89.383789,29.838928],[-89.383217,29.830385],[-89.372971,29.82526],[-89.345634,29.820135],[-89.342781,29.798496],[-89.33197,29.790524],[-89.318306,29.788815],[-89.277298,29.807608],[-89.277298,29.799635],[-89.284134,29.795649],[-89.284706,29.770021],[-89.269325,29.760912],[-89.271034,29.756355],[-89.305199,29.756926],[-89.337662,29.779135],[-89.354179,29.781412],[-89.367271,29.775148],[-89.386063,29.788815],[-89.394608,29.784828],[-89.399162,29.770592],[-89.428207,29.74155],[-89.42421,29.697638],[-89.44812,29.703316],[-89.530258,29.74375],[-89.560181,29.735472],[-89.572922,29.746616],[-89.634048,29.752981],[-89.651237,29.749479],[-89.644562,29.710957],[-89.618446,29.700768],[-89.592979,29.702042],[-89.599663,29.690262],[-89.596802,29.684212],[-89.573883,29.674025],[-89.53376,29.670204],[-89.487915,29.630405],[-89.486709,29.621003]]]]},\"properties\":{\"name\":\"Louisiana\",\"nation\":\"USA  \"}}]}","noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"4f4e4b04e4b07f02db6996a7","contributors":{"authors":[{"text":"Arcement, G.J.","contributorId":59058,"corporation":false,"usgs":true,"family":"Arcement","given":"G.J.","affiliations":[],"preferred":false,"id":253764,"contributorType":{"id":1,"text":"Authors"},"rank":1},{"text":"Dantin, L.J.","contributorId":61891,"corporation":false,"usgs":true,"family":"Dantin","given":"L.J.","email":"","affiliations":[],"preferred":false,"id":253765,"contributorType":{"id":1,"text":"Authors"},"rank":2},{"text":"Garrison, C.R.","contributorId":100006,"corporation":false,"usgs":true,"family":"Garrison","given":"C.R.","email":"","affiliations":[],"preferred":false,"id":253766,"contributorType":{"id":1,"text":"Authors"},"rank":3},{"text":"Stuart, C.G.","contributorId":58644,"corporation":false,"usgs":true,"family":"Stuart","given":"C.G.","email":"","affiliations":[],"preferred":false,"id":253763,"contributorType":{"id":1,"text":"Authors"},"rank":4}]}}
,{"id":30618,"text":"wri884116 - 1989 - Effects of river discharge and high-tide stage on salinity intrusion in the Weeki Wachee, Crystal, and Withlacoochee River estuaries, southwest Florida","interactions":[],"lastModifiedDate":"2023-01-11T19:20:43.62085","indexId":"wri884116","displayToPublicDate":"1994-01-01T00:00:00","publicationYear":"1989","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":"88-4116","title":"Effects of river discharge and high-tide stage on salinity intrusion in the Weeki Wachee, Crystal, and Withlacoochee River estuaries, southwest Florida","docAbstract":"<p>The Weeki Wachee, Crystal, and Withlacoochee Rivers are coastal streams flowing into the Gulf of Mexico that may be affected by either future surface water or groundwater withdrawals. Reduction of river discharge will affect the upstream extent of saltwater intrusion in the rivers; however, under certain reduced low-flow discharges, the estimated change in upstream extent of saltwater intrusion is on the order of several tenths of a mile and frequently is within the range of predicted error. Data on flow, tides, and salinity describe the physical characteristics of the Weeki Wachee, Crystal, and Withlacoochee River systems. Vertical and longitudinal salinity profiles indicate that salinity of the rivers increases downstream and varies substantially at any given location. The Weeki Wachee River system is the best mixed of the three. The Crystal River system exhibited the next best mixed system, and the Withlacoochee River system exhibited the most variation in its salinity regime. The daily maximum upstream extent of salinity intrusion is described by multiple linear-regression analysis based on daily mean streamflow of each river and high-tide stage of the gulf. The equations are used to show the effects of discharge on the daily maximum upstream extent of salinity intrusion in the rivers.</p>","language":"English","publisher":"U.S. Geological Survey","doi":"10.3133/wri884116","usgsCitation":"Yobbi, D.K., and Knochenmus, L.A., 1989, Effects of river discharge and high-tide stage on salinity intrusion in the Weeki Wachee, Crystal, and Withlacoochee River estuaries, southwest Florida: U.S. Geological Survey Water-Resources Investigations Report 88-4116, v, 63 p., https://doi.org/10.3133/wri884116.","productDescription":"v, 63 p.","costCenters":[],"links":[{"id":411726,"rank":3,"type":{"id":36,"text":"NGMDB Index Page"},"url":"https://ngmdb.usgs.gov/Prodesc/proddesc_47032.htm","linkFileType":{"id":5,"text":"html"}},{"id":59383,"rank":2,"type":{"id":11,"text":"Document"},"url":"https://pubs.usgs.gov/wri/1988/4116/report.pdf","linkFileType":{"id":1,"text":"pdf"}},{"id":123856,"rank":1,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/wri/1988/4116/report-thumb.jpg"}],"country":"United States","state":"Florida","otherGeospatial":"Weekee, Crystal, and Withlacoochee River estuaries","geographicExtents":"{\n  \"type\": \"FeatureCollection\",\n  \"features\": [\n    {\n      \"type\": \"Feature\",\n      \"properties\": {},\n      \"geometry\": {\n        \"coordinates\": [\n          [\n            [\n              -82.75,\n              29.1167\n            ],\n            [\n              -82.75,\n              28.4364\n            ],\n            [\n              -82.4217,\n              28.4364\n            ],\n            [\n              -82.4217,\n              29.1167\n            ],\n            [\n              -82.75,\n              29.1167\n            ]\n          ]\n        ],\n        \"type\": \"Polygon\"\n      }\n    }\n  ]\n}","noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"4f4e4b24e4b07f02db6ae8ea","contributors":{"authors":[{"text":"Yobbi, D. K.","contributorId":56622,"corporation":false,"usgs":true,"family":"Yobbi","given":"D.","email":"","middleInitial":"K.","affiliations":[],"preferred":false,"id":203549,"contributorType":{"id":1,"text":"Authors"},"rank":1},{"text":"Knochenmus, L. A.","contributorId":60683,"corporation":false,"usgs":true,"family":"Knochenmus","given":"L.","email":"","middleInitial":"A.","affiliations":[],"preferred":false,"id":203550,"contributorType":{"id":1,"text":"Authors"},"rank":2}]}}
,{"id":38519,"text":"pp1352 - 1989 - Investigations of the characteristics, origin, and residence time of the upland residual mantle of the Piedmont of Fairfax County, Virginia","interactions":[],"lastModifiedDate":"2012-02-02T00:10:16","indexId":"pp1352","displayToPublicDate":"1994-01-01T00:00:00","publicationYear":"1989","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":"1352","title":"Investigations of the characteristics, origin, and residence time of the upland residual mantle of the Piedmont of Fairfax County, Virginia","docAbstract":"Undisturbed cores of upland regolith developed from a variety of crystalline rocks of the Piedmont province in Fairfax County, Va., have been obtained by using a combination of Shelby tubes, Denison sampler, and modified diamond core drilling. The core study correlated variations in chemistry, mineralogy, and texture with engineering properties throughout individual weathering profiles and contrasted these parameters among weathering profiles developed from various parent rocks. Coring sites were chosen to obtain a maximum depth of weathering on diverse lithologies. The rocks that were investigated included metapelite, metagraywacke, granite, diabase, and serpentinite. Four to twelve samples per core were selected for analysis of petrography, texture, clay mineralogy, and major-element chemistry. The number of samples was determined on the basis of (1) the thickness of the weathering profile (from about 1 m in serpentinite to more than 30 m in pelitic schist) and (2) megascopic changes in the weathering profile. Shear strength and compressibility were determined on corresponding segments of core. Standard penetration tests were performed adjacent to coring sites to evaluate in-place engineering properties. \r\n\r\nThe regolith profiles on all rocks can be subdivided into soil, massive subsoil, saprolite, and weathered rock zones. Major differences in thicknesses of these zones are related to parent rock. Total regolith thickness is related to saprolite thickness. Saprolite is thickest on quartzofeldspathic metapelite, metagraywacke, and granite; thinner on diabase; and thinnest on serpentinite. Thickness of saprolite is related to rock structure and mineralogy. \r\n\r\nGeochemical changes of saprolite developed from each rock type follow predictable trends from fresh rock to soil profile, with increases in Ti, AI, Fe 3 +, and H 2 0+relative to absolute losses of Si, Fe2+, Mg, Ca, and Na. These variations are more pronounced in the weathering profiles above mafic and ultramafic rocks than in those above metagraywacke. Clay minerals in granite, schist, and metagraywacke saprolites are kaolinite, dioctahedral vermiculite, interlayered mica-vermiculite, and minor illite. Gibbsite is developed in near-surface samples of schist. \r\n\r\nStandard penetration test data for the upper 7 m of saprolite above schist, metagraywacke, and granite suggest alternations between stronger and weaker horizons that correlate with megascopic ally identified zones: soil, massive subsoil, and saprolite. The data correlate with density. Shear strength increases fairly regularly downward in the weathering profile. The engineering behavior of diabase saprolite is controlled by a dense, plastic, near-surface clay layer (montmorillonite and kaolinite) overlying rock that is weathered to a granular state (grus); the engineering properties of serpentinite are controlled by a very thin weathering profile. \r\n\r\nSimilarities in regolith thickness, zonation, mineralogy, and chemistry of quartzofeldspathic rocks indicate the existence of fundamental geochemical and geomechanical controls on regolith evolution on the Piedmont upland. Data from the profiles of quartzofeldspathic regolith are used to construct a model suggesting the principal rate-control steps in the development and downwasting of the upland regolith. This model is consistent with available information about Piedmont hydrology and tectonic uplift.","language":"ENGLISH","doi":"10.3133/pp1352","usgsCitation":"Pavich, M., Leo, G.W., Obermeier, S., and Estabrook, J., 1989, Investigations of the characteristics, origin, and residence time of the upland residual mantle of the Piedmont of Fairfax County, Virginia: U.S. Geological Survey Professional Paper 1352, 58 p., 3 plates in pocket, https://doi.org/10.3133/pp1352.","productDescription":"58 p., 3 plates in pocket","costCenters":[],"links":[{"id":124379,"rank":0,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/pp/1352/report-thumb.jpg"},{"id":65256,"rank":400,"type":{"id":17,"text":"Plate"},"url":"https://pubs.usgs.gov/pp/1352/plate-1.pdf","linkFileType":{"id":1,"text":"pdf"}},{"id":65257,"rank":401,"type":{"id":17,"text":"Plate"},"url":"https://pubs.usgs.gov/pp/1352/plate-2.pdf","linkFileType":{"id":1,"text":"pdf"}},{"id":65258,"rank":402,"type":{"id":17,"text":"Plate"},"url":"https://pubs.usgs.gov/pp/1352/plate-3.pdf","linkFileType":{"id":1,"text":"pdf"}},{"id":65259,"rank":300,"type":{"id":11,"text":"Document"},"url":"https://pubs.usgs.gov/pp/1352/report.pdf","linkFileType":{"id":1,"text":"pdf"}}],"noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"4f4e4aa8e4b07f02db667411","contributors":{"authors":[{"text":"Pavich, M.J.","contributorId":70788,"corporation":false,"usgs":true,"family":"Pavich","given":"M.J.","email":"","affiliations":[],"preferred":false,"id":219984,"contributorType":{"id":1,"text":"Authors"},"rank":1},{"text":"Leo, G. W.","contributorId":102899,"corporation":false,"usgs":true,"family":"Leo","given":"G.","email":"","middleInitial":"W.","affiliations":[],"preferred":false,"id":219985,"contributorType":{"id":1,"text":"Authors"},"rank":2},{"text":"Obermeier, S. F.","contributorId":17602,"corporation":false,"usgs":true,"family":"Obermeier","given":"S. F.","affiliations":[],"preferred":false,"id":219982,"contributorType":{"id":1,"text":"Authors"},"rank":3},{"text":"Estabrook, J.R.","contributorId":41423,"corporation":false,"usgs":true,"family":"Estabrook","given":"J.R.","email":"","affiliations":[],"preferred":false,"id":219983,"contributorType":{"id":1,"text":"Authors"},"rank":4}]}}
,{"id":47477,"text":"b1875B - 1989 - North American Datum of 1983, map data conversion tables; United States west of 96 degrees West longitude (including Hawaii)","interactions":[],"lastModifiedDate":"2012-02-02T00:10:47","indexId":"b1875B","displayToPublicDate":"1994-01-01T00:00:00","publicationYear":"1989","noYear":false,"publicationType":{"id":18,"text":"Report"},"publicationSubtype":{"id":5,"text":"USGS Numbered Series"},"seriesTitle":{"id":306,"text":"Bulletin","code":"B","active":false,"publicationSubtype":{"id":5}},"seriesNumber":"1875","chapter":"B","title":"North American Datum of 1983, map data conversion tables; United States west of 96 degrees West longitude (including Hawaii)","language":"ENGLISH","doi":"10.3133/b1875B","usgsCitation":"Water Resources Division, U.S. Geological Survey, 1989, North American Datum of 1983, map data conversion tables; United States west of 96 degrees West longitude (including Hawaii): U.S. Geological Survey Bulletin 1875, p. B1-B431, https://doi.org/10.3133/b1875B.","productDescription":"p. B1-B431","costCenters":[],"links":[{"id":172278,"rank":0,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/bul/1875b/report-thumb.jpg"},{"id":84416,"rank":300,"type":{"id":11,"text":"Document"},"url":"https://pubs.usgs.gov/bul/1875b/report.pdf","linkFileType":{"id":1,"text":"pdf"}}],"noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"4f4e4afde4b07f02db696daf","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":531745,"contributorType":{"id":1,"text":"Authors"},"rank":1}]}}
,{"id":15323,"text":"ofr89335 - 1989 - Isotopic evidence for evolution of sub-continental mantle during Red Sea rifting","interactions":[],"lastModifiedDate":"2015-09-29T11:40:11","indexId":"ofr89335","displayToPublicDate":"1994-01-01T00:00:00","publicationYear":"1989","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":"89-335","title":"Isotopic evidence for evolution of sub-continental mantle during Red Sea rifting","docAbstract":"<p>Tertiary igneous rocks from near Al Lith, Saudi Arabia are alkaline to subalkaline and bimodal in composition, and document early and late rift volcanism (&ge;30 Ma to ~20 Ma, 11 Ma and 3 Ma) in the central part of the Red Sea rift. Isotopic and trace-element data from twenty-five samples are presented and used to characterize basalt sources in the early rift.</p>\n<p>Inferred primary isotopic compositions of alkalic basalts and some tholeiites indicate a common mantle source. Many of the felsic volcanics are isotopically indistinguishable from these mafic rocks; they likely represent products of fractional crystallization, or anatectic melts of mafic Al Lith precursors. <sup>l43</sup>Nd/<sup>144</sup>Nd and <sup>87</sup>Sr/<sup>86</sup>Sr ratios for most Al Lith rocks show limited variation (<sup>87</sup>Sr/<sup>86</sup>Sr<sub>i</sub> = 0.7030 to 0.7033, &epsilon; -Nd=+6 to +8). They plot near enriched MORB and between the isotopic compositions of recent magmas from the Red Sea spreading axis and less depleted to enriched basalts from the East African rift. Pb isotopic compositions are MORB-like and moderately radiogenic in <sup>206</sup>Pb/<sup>204</sup>Pb. Normalized incompatible trace-element abundances and oceanic Pb/Ce indicate sources similar to those for enriched MORB and OIB and distinct from subduction-dominated source regions. As in many continental basalt fields, high <sup>l43</sup>Nd/<sup>144</sup>Nd and relatively low Sr and Pb isotopic ratios, despite incompatible-element enrichment, indicate that source enrichment was not an ancient event; it probably took place as a precursor to rift magmatism.</p>\n<p>These data are consistent with a multi-stage model of sub-rift mantle evolution. Depleted lithospheric mantle in the spinel-lherzolite fades was veined by incompatible-element rich fluids, then partially melted. Melt equilibration and fractionation took place over a large depth range, producing transitional alkaline-subalkaline basalts during early rift magmatism. In the axis of the rift, depleted asthenospheric mantle upwelled and displaced the veined lithosphere, eventually producing MORB at the Red Sea axis. However, basalts from the veined lithospheric mantle continue to be erupted from the Arabian margin of the rift.</p>\n<p>Anomalous, old (&gt; 2 Ga) continental-affinity Pb, radiogenic Sr and low &epsilon;-Nd values found in some of the subalkaline Al Lith rocks are explained by crustal contamination, not by Dupal mantle sources.</p>","language":"English","publisher":"U.S. Geological Survey","publisherLocation":"Reston, VA","doi":"10.3133/ofr89335","usgsCitation":"Pallister, J.S., and Hegner, E., 1989, Isotopic evidence for evolution of sub-continental mantle during Red Sea rifting: U.S. Geological Survey Open-File Report 89-335, ii, 25 p., https://doi.org/10.3133/ofr89335.","productDescription":"ii, 25 p.","onlineOnly":"N","additionalOnlineFiles":"N","costCenters":[],"links":[{"id":44253,"rank":300,"type":{"id":11,"text":"Document"},"url":"https://pubs.usgs.gov/of/1989/0335/report.pdf","linkFileType":{"id":1,"text":"pdf"}},{"id":146457,"rank":0,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/of/1989/0335/report-thumb.jpg"}],"country":"Saudi Arabia","geographicExtents":"{\n  \"type\": \"FeatureCollection\",\n  \"features\": [\n    {\n      \"type\": \"Feature\",\n      \"properties\": {},\n      \"geometry\": {\n        \"type\": \"Polygon\",\n        \"coordinates\": [\n          [\n            [\n              39,\n              20\n            ],\n            [\n              39,\n              21\n            ],\n            [\n              40.5,\n              21\n            ],\n            [\n              40.5,\n              20\n            ],\n            [\n              39,\n              20\n            ]\n          ]\n        ]\n      }\n    }\n  ]\n}","noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"4f4e4aa7e4b07f02db667012","contributors":{"authors":[{"text":"Pallister, John S. 0000-0002-2041-2147 jpallist@usgs.gov","orcid":"https://orcid.org/0000-0002-2041-2147","contributorId":2024,"corporation":false,"usgs":true,"family":"Pallister","given":"John","email":"jpallist@usgs.gov","middleInitial":"S.","affiliations":[{"id":114,"text":"Alaska Science Center","active":true,"usgs":true},{"id":617,"text":"Volcano Science Center","active":true,"usgs":true}],"preferred":true,"id":170955,"contributorType":{"id":1,"text":"Authors"},"rank":1},{"text":"Hegner, Ernst","contributorId":57465,"corporation":false,"usgs":true,"family":"Hegner","given":"Ernst","email":"","affiliations":[],"preferred":false,"id":170956,"contributorType":{"id":1,"text":"Authors"},"rank":2}]}}
,{"id":17735,"text":"ofr8745 - 1989 - Summary of data pertaining to land use, rainfall, dryfall, stream discharge, and storm runoff collected as part of a study of the effects of urban runoff on Rapid Creek, Rapid City area, South Dakota","interactions":[],"lastModifiedDate":"2012-02-02T00:07:21","indexId":"ofr8745","displayToPublicDate":"1994-01-01T00:00:00","publicationYear":"1989","noYear":false,"publicationType":{"id":18,"text":"Report"},"publicationSubtype":{"id":5,"text":"USGS Numbered Series"},"seriesTitle":{"id":330,"text":"Open-File Report","code":"OFR","onlineIssn":"2331-1258","printIssn":"0196-1497","active":true,"publicationSubtype":{"id":5}},"seriesNumber":"87-45","title":"Summary of data pertaining to land use, rainfall, dryfall, stream discharge, and storm runoff collected as part of a study of the effects of urban runoff on Rapid Creek, Rapid City area, South Dakota","docAbstract":"The objectives of a 3-year study of urban runoff in the Rapid City area of South Dakota were to characterize the effects of urban runoff from rainfall on the water quality of Rapid Creek, and to evaluate the effects of the runoff on the existing cold-water fishery. In order to meet these objectives, it was necessary to obtain detailed data pertaining to land use, rainfall, dryfall, stream discharge, and storm runoff. This report describes the rationale behind the data collection program, describes the methods used to collect and analyze the data, and presents the data collected and summarized during the study. Six watersheds were investigated, ranging in size from 1 ,610 to 20,990 acres. Water quality data from 6 sites for about 30 rainstorms that occurred between June 1980 and July 1982 are presented. (USGS)","language":"ENGLISH","publisher":"U.S. Geological Survey ;\r\nBooks and Open-File Reports [distributor],","doi":"10.3133/ofr8745","usgsCitation":"Goddard, K., Lockner, T., Harms, L., and Smith, M., 1989, Summary of data pertaining to land use, rainfall, dryfall, stream discharge, and storm runoff collected as part of a study of the effects of urban runoff on Rapid Creek, Rapid City area, South Dakota: U.S. Geological Survey Open-File Report 87-45, vii, 194 p. :ill., map ;28 cm., https://doi.org/10.3133/ofr8745.","productDescription":"vii, 194 p. :ill., map ;28 cm.","costCenters":[],"links":[{"id":150088,"rank":0,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/of/1987/0045/report-thumb.jpg"},{"id":46953,"rank":400,"type":{"id":17,"text":"Plate"},"url":"https://pubs.usgs.gov/of/1987/0045/plate-1.pdf","linkFileType":{"id":1,"text":"pdf"}},{"id":46954,"rank":300,"type":{"id":11,"text":"Document"},"url":"https://pubs.usgs.gov/of/1987/0045/report.pdf","linkFileType":{"id":1,"text":"pdf"}}],"noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"4f4e4b04e4b07f02db699324","contributors":{"authors":[{"text":"Goddard, K.E.","contributorId":82319,"corporation":false,"usgs":true,"family":"Goddard","given":"K.E.","email":"","affiliations":[],"preferred":false,"id":177641,"contributorType":{"id":1,"text":"Authors"},"rank":1},{"text":"Lockner, T.K.","contributorId":29062,"corporation":false,"usgs":true,"family":"Lockner","given":"T.K.","email":"","affiliations":[],"preferred":false,"id":177639,"contributorType":{"id":1,"text":"Authors"},"rank":2},{"text":"Harms, L.L.","contributorId":97374,"corporation":false,"usgs":true,"family":"Harms","given":"L.L.","email":"","affiliations":[],"preferred":false,"id":177642,"contributorType":{"id":1,"text":"Authors"},"rank":3},{"text":"Smith, M.H.","contributorId":36156,"corporation":false,"usgs":true,"family":"Smith","given":"M.H.","email":"","affiliations":[],"preferred":false,"id":177640,"contributorType":{"id":1,"text":"Authors"},"rank":4}]}}
,{"id":47476,"text":"b1875A - 1989 - North American Datum of 1983, map data conversion tables; United States east of 96 degrees West longitude, Puerto Rico and the U. S. Virgin Islands","interactions":[],"lastModifiedDate":"2012-02-02T00:10:24","indexId":"b1875A","displayToPublicDate":"1994-01-01T00:00:00","publicationYear":"1989","noYear":false,"publicationType":{"id":18,"text":"Report"},"publicationSubtype":{"id":5,"text":"USGS Numbered Series"},"seriesTitle":{"id":306,"text":"Bulletin","code":"B","active":false,"publicationSubtype":{"id":5}},"seriesNumber":"1875","chapter":"A","title":"North American Datum of 1983, map data conversion tables; United States east of 96 degrees West longitude, Puerto Rico and the U. S. Virgin Islands","language":"ENGLISH","doi":"10.3133/b1875A","usgsCitation":"Water Resources Division, U.S. Geological Survey, 1989, North American Datum of 1983, map data conversion tables; United States east of 96 degrees West longitude, Puerto Rico and the U. S. Virgin Islands: U.S. Geological Survey Bulletin 1875, p. A1-A351, https://doi.org/10.3133/b1875A.","productDescription":"p. A1-A351","costCenters":[],"links":[{"id":169882,"rank":0,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/bul/1875a/report-thumb.jpg"},{"id":84415,"rank":300,"type":{"id":11,"text":"Document"},"url":"https://pubs.usgs.gov/bul/1875a/report.pdf","linkFileType":{"id":1,"text":"pdf"}}],"noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"4f4e4afde4b07f02db696db4","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":531744,"contributorType":{"id":1,"text":"Authors"},"rank":1}]}}
,{"id":55920,"text":"wdrNV881 - 1989 - Water resources data, Nevada, water year 1988","interactions":[],"lastModifiedDate":"2012-02-02T00:12:20","indexId":"wdrNV881","displayToPublicDate":"1994-01-01T00:00:00","publicationYear":"1989","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":"NV-88-1","title":"Water resources data, Nevada, water year 1988","language":"ENGLISH","doi":"10.3133/wdrNV881","usgsCitation":"Pupacko, A., La Camera, R., Riek, M., and Swartwood, J., 1989, Water resources data, Nevada, water year 1988: U.S. Geological Survey Water Data Report NV-88-1, 271 p., https://doi.org/10.3133/wdrNV881.","productDescription":"271 p.","costCenters":[],"links":[{"id":184614,"rank":0,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/thumbnails/usgs_thumb.jpg"}],"noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"4f4e4b04e4b07f02db6996ac","contributors":{"authors":[{"text":"Pupacko, Alex","contributorId":107713,"corporation":false,"usgs":true,"family":"Pupacko","given":"Alex","email":"","affiliations":[],"preferred":false,"id":254484,"contributorType":{"id":1,"text":"Authors"},"rank":1},{"text":"La Camera, R.J.","contributorId":83932,"corporation":false,"usgs":true,"family":"La Camera","given":"R.J.","affiliations":[],"preferred":false,"id":254482,"contributorType":{"id":1,"text":"Authors"},"rank":2},{"text":"Riek, M.M.","contributorId":93972,"corporation":false,"usgs":true,"family":"Riek","given":"M.M.","email":"","affiliations":[],"preferred":false,"id":254483,"contributorType":{"id":1,"text":"Authors"},"rank":3},{"text":"Swartwood, J.R.","contributorId":81553,"corporation":false,"usgs":true,"family":"Swartwood","given":"J.R.","affiliations":[],"preferred":false,"id":254481,"contributorType":{"id":1,"text":"Authors"},"rank":4}]}}
,{"id":38307,"text":"ofr89300L - 1989 - Preliminary geomagnetic data, College Observatory, Fairbanks, Alaska","interactions":[],"lastModifiedDate":"2012-02-02T00:09:48","indexId":"ofr89300L","displayToPublicDate":"1994-01-01T00:00:00","publicationYear":"1989","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":"89-300","chapter":"L","title":"Preliminary geomagnetic data, College Observatory, Fairbanks, Alaska","language":"ENGLISH","doi":"10.3133/ofr89300L","usgsCitation":"Townshend, J.B., O’Connell, R.V., and Varner, C.A., 1989, Preliminary geomagnetic data, College Observatory, Fairbanks, Alaska: U.S. Geological Survey Open-File Report 89-300, 20 p.:ill. ;28 cm., https://doi.org/10.3133/ofr89300L.","productDescription":"20 p.:ill. ;28 cm.","costCenters":[],"links":[{"id":165246,"rank":0,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/of/1989/0300l/report-thumb.jpg"},{"id":64679,"rank":300,"type":{"id":11,"text":"Document"},"url":"https://pubs.usgs.gov/of/1989/0300l/report.pdf","linkFileType":{"id":1,"text":"pdf"}}],"noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"4f4e4b06e4b07f02db69a2b8","contributors":{"authors":[{"text":"Townshend, John B.","contributorId":70383,"corporation":false,"usgs":true,"family":"Townshend","given":"John","email":"","middleInitial":"B.","affiliations":[],"preferred":false,"id":219583,"contributorType":{"id":1,"text":"Authors"},"rank":1},{"text":"O’Connell, R. V.","contributorId":88755,"corporation":false,"usgs":true,"family":"O’Connell","given":"R.","email":"","middleInitial":"V.","affiliations":[],"preferred":false,"id":219584,"contributorType":{"id":1,"text":"Authors"},"rank":2},{"text":"Varner, Carol Ann","contributorId":66705,"corporation":false,"usgs":true,"family":"Varner","given":"Carol","email":"","middleInitial":"Ann","affiliations":[],"preferred":false,"id":219582,"contributorType":{"id":1,"text":"Authors"},"rank":3}]}}
,{"id":47508,"text":"b1866B - 1989 - Statistical analysis of compositional data from Desmoinesian sandstones in Oklahoma","interactions":[{"subject":{"id":47508,"text":"b1866B - 1989 - Statistical analysis of compositional data from Desmoinesian sandstones in Oklahoma","indexId":"b1866B","publicationYear":"1989","noYear":false,"chapter":"B","title":"Statistical analysis of compositional data from Desmoinesian sandstones in Oklahoma"},"predicate":"IS_PART_OF","object":{"id":33238,"text":"b1866 - 1989 - Evolution of sedimentary basins: Anadarko Basin","indexId":"b1866","publicationYear":"1989","noYear":false,"title":"Evolution of sedimentary basins: Anadarko Basin"},"id":1}],"isPartOf":{"id":33238,"text":"b1866 - 1989 - Evolution of sedimentary basins: Anadarko Basin","indexId":"b1866","publicationYear":"1989","noYear":false,"title":"Evolution of sedimentary basins: Anadarko Basin"},"lastModifiedDate":"2017-06-14T14:45:44","indexId":"b1866B","displayToPublicDate":"1994-01-01T00:00:00","publicationYear":"1989","noYear":false,"publicationType":{"id":18,"text":"Report"},"publicationSubtype":{"id":5,"text":"USGS Numbered Series"},"seriesTitle":{"id":306,"text":"Bulletin","code":"B","active":false,"publicationSubtype":{"id":5}},"seriesNumber":"1866","chapter":"B","title":"Statistical analysis of compositional data from Desmoinesian sandstones in Oklahoma","language":"ENGLISH","doi":"10.3133/b1866B","usgsCitation":"Dyman, T.S., 1989, Statistical analysis of compositional data from Desmoinesian sandstones in Oklahoma: U.S. Geological Survey Bulletin 1866, p. B1-B12; illus. incl. 2 tables, sketch maps, https://doi.org/10.3133/b1866B.","productDescription":"p. B1-B12; illus. incl. 2 tables, sketch maps","costCenters":[],"links":[{"id":168103,"rank":0,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/bul/1866b/report-thumb.jpg"},{"id":84450,"rank":300,"type":{"id":11,"text":"Document"},"url":"https://pubs.usgs.gov/bul/1866b/report.pdf","linkFileType":{"id":1,"text":"pdf"}}],"noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"4f4e49dfe4b07f02db5e3c60","contributors":{"authors":[{"text":"Dyman, Thaddeus S.","contributorId":83971,"corporation":false,"usgs":true,"family":"Dyman","given":"Thaddeus","email":"","middleInitial":"S.","affiliations":[],"preferred":false,"id":235589,"contributorType":{"id":1,"text":"Authors"},"rank":1}]}}
,{"id":17540,"text":"ofr89300A - 1989 - Preliminary geomagnetic data, College Observatory, Fairbanks, Alaska","interactions":[],"lastModifiedDate":"2012-02-02T00:07:12","indexId":"ofr89300A","displayToPublicDate":"1994-01-01T00:00:00","publicationYear":"1989","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":"89-300","chapter":"A","title":"Preliminary geomagnetic data, College Observatory, Fairbanks, Alaska","language":"ENGLISH","publisher":"U.S. Geological Survey,","doi":"10.3133/ofr89300A","usgsCitation":"Townshend, J.B., O’Connell, R.V., and Varner, C.A., 1989, Preliminary geomagnetic data, College Observatory, Fairbanks, Alaska: U.S. Geological Survey Open-File Report 89-300, 21 p. ill. ;28 cm., https://doi.org/10.3133/ofr89300A.","productDescription":"21 p. ill. ;28 cm.","costCenters":[],"links":[{"id":149480,"rank":0,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/of/1989/0300a/report-thumb.jpg"},{"id":46706,"rank":300,"type":{"id":11,"text":"Document"},"url":"https://pubs.usgs.gov/of/1989/0300a/report.pdf","linkFileType":{"id":1,"text":"pdf"}}],"noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"4f4e4b06e4b07f02db69a303","contributors":{"authors":[{"text":"Townshend, John B.","contributorId":70383,"corporation":false,"usgs":true,"family":"Townshend","given":"John","email":"","middleInitial":"B.","affiliations":[],"preferred":false,"id":176804,"contributorType":{"id":1,"text":"Authors"},"rank":1},{"text":"O’Connell, R. V.","contributorId":88755,"corporation":false,"usgs":true,"family":"O’Connell","given":"R.","email":"","middleInitial":"V.","affiliations":[],"preferred":false,"id":176805,"contributorType":{"id":1,"text":"Authors"},"rank":2},{"text":"Varner, Carol Ann","contributorId":66705,"corporation":false,"usgs":true,"family":"Varner","given":"Carol","email":"","middleInitial":"Ann","affiliations":[],"preferred":false,"id":176803,"contributorType":{"id":1,"text":"Authors"},"rank":3}]}}
]}