{"pageNumber":"178","pageRowStart":"4425","pageSize":"25","recordCount":6233,"records":[{"id":18412,"text":"ofr94485 - 1995 - Water-level fluctuations, water temperatures, and tilts in sandbars -6.5R, 43.1L, and 172.3L, Grand Canyon, Arizona, 1990-93","interactions":[],"lastModifiedDate":"2012-02-02T00:07:24","indexId":"ofr94485","displayToPublicDate":"1995-08-01T00:00:00","publicationYear":"1995","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":"94-485","title":"Water-level fluctuations, water temperatures, and tilts in sandbars -6.5R, 43.1L, and 172.3L, Grand Canyon, Arizona, 1990-93","docAbstract":"Rill erosion, slumping, and fissuring develop on seepage faces of many sandbars along the Colorado River in the Grand Canyon at low river stage. Three sandbars were instrumented with sensors for continual monitoring of stage, pore pressure, ground-water temperature, and tilt to determine the relation between ground-water flow and sandbar deformation. Data were collected from October 1990 to July 1993 at sandbar -6.5R, which had 17 pore- pressure sensors, 1 stage sensor, 19 temperature sensors, and 8 tilt sensors. Data were collected from April 1991 to March 1993 at sandbar 172.3L, which had 15 pore-pressure sensors, 1 stage sensor, 29 temperature sensors, and 10 tilt sensors. Atten- uation of water-level fluctuation from the zone of fluctuating river stage to the back of the sandbars ranged from 70 percent at sandbar -6.5R to 40 percent for sandbars 43.1L and 172.3L. Shallow tilt occurred at sandbar 43.1L from July 7 to August 10, 1991. Tilt occurred at sandbar 172.3L on May 7-8, June 18-19, and September 1-2, 1991; July 3 and 31, 1992; January 12, 14, 20-21, and 31, 1993; and February 21 and 24, 1993.","language":"ENGLISH","publisher":"U.S. Geological Survey ;\r\nU.S. Geological Survey, Open-File Section,","doi":"10.3133/ofr94485","usgsCitation":"Carpenter, M.C., Crosswhite, J.A., and Carruth, R., 1995, Water-level fluctuations, water temperatures, and tilts in sandbars -6.5R, 43.1L, and 172.3L, Grand Canyon, Arizona, 1990-93: U.S. Geological Survey Open-File Report 94-485, iv, 17 p. :ill., map ;28 cm., https://doi.org/10.3133/ofr94485.","productDescription":"iv, 17 p. :ill., map ;28 cm.","costCenters":[],"links":[{"id":151234,"rank":0,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/of/1994/0485/report-thumb.jpg"},{"id":47749,"rank":300,"type":{"id":11,"text":"Document"},"url":"https://pubs.usgs.gov/of/1994/0485/report.pdf","linkFileType":{"id":1,"text":"pdf"}}],"noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"4f4e49e6e4b07f02db5e7645","contributors":{"authors":[{"text":"Carpenter, Michael C. mcarpent@usgs.gov","contributorId":3977,"corporation":false,"usgs":true,"family":"Carpenter","given":"Michael","email":"mcarpent@usgs.gov","middleInitial":"C.","affiliations":[],"preferred":true,"id":179074,"contributorType":{"id":1,"text":"Authors"},"rank":1},{"text":"Crosswhite, Jason A.","contributorId":46110,"corporation":false,"usgs":true,"family":"Crosswhite","given":"Jason","email":"","middleInitial":"A.","affiliations":[],"preferred":false,"id":179076,"contributorType":{"id":1,"text":"Authors"},"rank":2},{"text":"Carruth, R. L.","contributorId":31413,"corporation":false,"usgs":true,"family":"Carruth","given":"R. L.","affiliations":[],"preferred":false,"id":179075,"contributorType":{"id":1,"text":"Authors"},"rank":3}]}}
,{"id":17722,"text":"ofr94545 - 1995 - Streamflow, water-temperature, and specific-conductance data for selected streams draining into Lake Fryxell, lower Taylor Valley, Victoria Land, Antarctica, 1990-92","interactions":[],"lastModifiedDate":"2012-02-02T00:07:21","indexId":"ofr94545","displayToPublicDate":"1995-08-01T00:00:00","publicationYear":"1995","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":"94-545","title":"Streamflow, water-temperature, and specific-conductance data for selected streams draining into Lake Fryxell, lower Taylor Valley, Victoria Land, Antarctica, 1990-92","docAbstract":"During the 1990-91 and 1991-92 field seasons in Antarctica, streamflow, water-temperature, and specific-conductance data were collected on the major streams draining into Lake Fryxell. Lake Fryxell is a permanently ice-covered, closed-basin lake with 13 tributary streams. Continuous streamflow data were collected at eight sites, and periodic streamflow measurements were made at three sites. Continuous water-temperature and specific- conductance data were collected at seven sites, and periodic water-temperature and specific-conductance data were collected at all sites. Streamflow for all streams measured ranged from 0 to 0.651 cubic meter per second. Water temperatures for all streams measured ranged from 0 to 14.3 degrees Celsius. Specific conductance for all streams measured ranged from 11 to 491 microsiemens per centimeter at 25 degrees Celsius. It is probable that stream- flow in the Lake Fryxell Basin during 1990-92 was greater than average. Examination of the 22-year streamflow record in the Onyx River in the Wright Valley revealed that in 1990 streamflow began earlier than for any previous year recorded and that the peak streamflow of record was exceeded. Similar high-flow conditions occurred during the 1991-92 field season. Thus, the data collected on streams draining into Lake Fryxell during 1990-92 are representative of greater than average stream- flow conditions.","language":"ENGLISH","publisher":"U.S. Geological Survey :\r\nUSGS Earth Science Information Center, Open-File Reports Section [distributor],","doi":"10.3133/ofr94545","usgsCitation":"Von Guerard, P., McKnight, D.M., Harnish, R., Gartner, J.W., and Andrews, E., 1995, Streamflow, water-temperature, and specific-conductance data for selected streams draining into Lake Fryxell, lower Taylor Valley, Victoria Land, Antarctica, 1990-92: U.S. Geological Survey Open-File Report 94-545, 65 p. ill., maps ;28 cm., https://doi.org/10.3133/ofr94545.","productDescription":"65 p. ill., maps ;28 cm.","costCenters":[],"links":[{"id":150069,"rank":0,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/of/1994/0545/report-thumb.jpg"},{"id":21644,"rank":400,"type":{"id":17,"text":"Plate"},"url":"https://pubs.usgs.gov/of/1994/0545/plate-1.pdf","linkFileType":{"id":1,"text":"pdf"}},{"id":46944,"rank":300,"type":{"id":11,"text":"Document"},"url":"https://pubs.usgs.gov/of/1994/0545/report.pdf","linkFileType":{"id":1,"text":"pdf"}}],"noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"4f4e4b15e4b07f02db6a4c86","contributors":{"authors":[{"text":"Von Guerard, Paul","contributorId":40620,"corporation":false,"usgs":true,"family":"Von Guerard","given":"Paul","affiliations":[],"preferred":false,"id":177591,"contributorType":{"id":1,"text":"Authors"},"rank":1},{"text":"McKnight, Diane M.","contributorId":59773,"corporation":false,"usgs":false,"family":"McKnight","given":"Diane","email":"","middleInitial":"M.","affiliations":[{"id":16833,"text":"INSTAAR, University of Colorado","active":true,"usgs":false}],"preferred":false,"id":177593,"contributorType":{"id":1,"text":"Authors"},"rank":2},{"text":"Harnish, R.A.","contributorId":44565,"corporation":false,"usgs":true,"family":"Harnish","given":"R.A.","email":"","affiliations":[],"preferred":false,"id":177592,"contributorType":{"id":1,"text":"Authors"},"rank":3},{"text":"Gartner, J. W.","contributorId":81903,"corporation":false,"usgs":false,"family":"Gartner","given":"J.","email":"","middleInitial":"W.","affiliations":[],"preferred":false,"id":177594,"contributorType":{"id":1,"text":"Authors"},"rank":4},{"text":"Andrews, E.D.","contributorId":13922,"corporation":false,"usgs":true,"family":"Andrews","given":"E.D.","email":"","affiliations":[],"preferred":false,"id":177590,"contributorType":{"id":1,"text":"Authors"},"rank":5}]}}
,{"id":4868,"text":"ds31rel1 - 1995 - Profiles of gamma-ray and magnetic data for aerial surveys over parts of the Western United States from longitude 108 to 126 degrees W. and from latitude 34 to 49 degrees N.","interactions":[],"lastModifiedDate":"2012-02-10T00:10:06","indexId":"ds31rel1","displayToPublicDate":"1995-07-01T00:00:00","publicationYear":"1995","noYear":false,"publicationType":{"id":18,"text":"Report"},"publicationSubtype":{"id":5,"text":"USGS Numbered Series"},"seriesTitle":{"id":310,"text":"Data Series","code":"DS","onlineIssn":"2327-638X","printIssn":"2327-0271","active":false,"publicationSubtype":{"id":5}},"seriesNumber":"31","title":"Profiles of gamma-ray and magnetic data for aerial surveys over parts of the Western United States from longitude 108 to 126 degrees W. and from latitude 34 to 49 degrees N.","docAbstract":"This CD-ROM contains images generated from geophysical data, software for displaying and analyzing the images and software for displaying and examining profile data from aerial surveys flown as part of the National Uranium Resource Evaluation (NURE) Program of the U.S. Department of Energy. The images included are of gamma-ray data (uranium, thorium, and potassium channels), Bouguer gravity data, isostatic residual gravity data, aeromagnetic anomalies, topography, and topography with bathymetry. This publication contains image data for the conterminous United States and profile data for the conterminous United States within the area longitude 108 to 126 degrees W. and latitude 34 to 49 degrees N. The profile data include apparent surface concentrations of potassium, uranium, and thorium, the residual magnetic field, and the height above the ground. The images on this CD-ROM include graytone and color images of each data set, color shaded-relief images of the potential-field and topographic data, and color composite images of the gamma-ray data. The image display and analysis software can register images with geographic and geologic overlays. The profile display software permits the user to view the profiles as well as obtain data listings and export ASCII versions of data for selected flight lines.","language":"ENGLISH","publisher":"U.S. Geological Survey :USGS Information Services,","doi":"10.3133/ds31rel1","isbn":"0607624418","usgsCitation":"Duval, J.S., 1995, Profiles of gamma-ray and magnetic data for aerial surveys over parts of the Western United States from longitude 108 to 126 degrees W. and from latitude 34 to 49 degrees N. (Release 1): U.S. Geological Survey Data Series 31, 1 computer laser optical disc :col. ;4 3/4 in., https://doi.org/10.3133/ds31rel1.","productDescription":"1 computer laser optical disc :col. ;4 3/4 in.","costCenters":[],"links":[{"id":139687,"rank":0,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/thumbnails/usgs_thumb.jpg"}],"scale":"0","geographicExtents":"{ \"type\": \"FeatureCollection\", \"features\": [ { \"type\": \"Feature\", \"properties\": {}, \"geometry\": { \"type\": \"Polygon\", \"coordinates\": [ [ [ -126,34 ], [ -126,49 ], [ -108,49 ], [ -108,34 ], [ -126,34 ] ] ] } } ] }","edition":"Release 1","noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"4f4e4a81e4b07f02db649f6a","contributors":{"authors":[{"text":"Duval, Joseph S.","contributorId":22314,"corporation":false,"usgs":true,"family":"Duval","given":"Joseph","email":"","middleInitial":"S.","affiliations":[],"preferred":false,"id":149981,"contributorType":{"id":1,"text":"Authors"},"rank":1}]}}
,{"id":28664,"text":"wri944128 - 1995 - Water quality of the Boca Raton canal system and effects of the Hillsboro Canal inflow, southeastern Florida, 1990-91","interactions":[],"lastModifiedDate":"2012-02-02T00:08:35","indexId":"wri944128","displayToPublicDate":"1995-07-01T00:00:00","publicationYear":"1995","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":"94-4128","title":"Water quality of the Boca Raton canal system and effects of the Hillsboro Canal inflow, southeastern Florida, 1990-91","docAbstract":"The City of Boca Raton in southeastern Palm Beach County, Florida, is an urban residential area that has sustained a constant population growth with subsequent increase in water use. The Boca Raton network of canals is controlled to provide for drainage of excess water, to maintain proper coastal ground-water levels to prevent saltwater intrusion, and to recharge the surficial aquifer system from which the city withdraws potable water. Most of the water supplied to the Boca Raton canal system and the surficial aquifer system, other than rainfall and runoff, is pumped from the Hillsboro Canal. The Biscayne aquifer, principal hydrogeologic unit of the surficial aquifer system, is highly permeable and there is a close relation between water levels in the canals and the aquifer. The amount of water supplied by seepage from the conservation areas is unknown. Because the Hillsboro Canal flows from Lake Okeechobee and Water Conservation Areas 1 and 2, which are places of more highly mineralized ground water and surface water, the canal is a possible source of contamination. Water samples were collected at 10 canal sites during wet and dry seasons and analyzed for major inorganic ions and related characteristics, nutrients, and trace elements. All concentrations were generally within or less than the drinking-water standards established by the Florida Department of Environmental Protection. The high concentrations of sodium and chloride that were detected in samples from the Boca Raton canal system are probably from the more mineralized water of the Hillsboro Canal. Other water-quality data, gathered from various sources from 1982 through 1991, did not indicate any significant changes nor trends. The effects of the Hillsboro Canal on the water quality of the Boca Raton canal system are indicated by increased concentrations of sodium, chloride, dissolved solids, and total organic carbon. Concentrations of the constituents in the canal water generally decrease with distance from the Hillsboro Canal pumping station and are the result of dilution by receiving canal waters.","language":"ENGLISH","publisher":"U.S. Geological Survey ;\r\nEarth Science Information Center, Open-File Reports Section [distributor],","doi":"10.3133/wri944128","usgsCitation":"McKenzie, D., 1995, Water quality of the Boca Raton canal system and effects of the Hillsboro Canal inflow, southeastern Florida, 1990-91: U.S. Geological Survey Water-Resources Investigations Report 94-4128, iv, 14 p. :ill., map ;28 cm. [PGS - 18 p.], https://doi.org/10.3133/wri944128.","productDescription":"iv, 14 p. :ill., map ;28 cm. [PGS - 18 p.]","costCenters":[],"links":[{"id":2258,"rank":100,"type":{"id":15,"text":"Index Page"},"url":"https://pubs.water.usgs.gov/wri944128","linkFileType":{"id":5,"text":"html"}},{"id":158337,"rank":0,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/thumbnails/usgs_thumb.jpg"}],"noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"4f4e4ac7e4b07f02db67ae85","contributors":{"authors":[{"text":"McKenzie, D.J.","contributorId":75134,"corporation":false,"usgs":true,"family":"McKenzie","given":"D.J.","email":"","affiliations":[],"preferred":false,"id":200196,"contributorType":{"id":1,"text":"Authors"},"rank":1}]}}
,{"id":29188,"text":"wri944077 - 1995 - Surface-water-quality assessment of the lower Kansas River basin, Kansas and Nebraska: Dissolved oxygen and Escherichia coli bacteria in streams during low flow, July 1988 through July 1989","interactions":[],"lastModifiedDate":"2022-09-07T21:36:00.154359","indexId":"wri944077","displayToPublicDate":"1995-07-01T00:00:00","publicationYear":"1995","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":"94-4077","title":"Surface-water-quality assessment of the lower Kansas River basin, Kansas and Nebraska: Dissolved oxygen and Escherichia coli bacteria in streams during low flow, July 1988 through July 1989","docAbstract":"The 15,300-square-mile lower Kansas River Basin in Kansas and Nebraska was investigated, as one of the pilot study units of the U.S. Geological Survey's National Water-Quality Assessment (NAWQA) Program, to address a variety of water-quality issues. This report describes sanitary quality of streams as defined by concentrations of dissolved oxygen (DO) and densities of a fecal-indicator bacterium, Escherichia coli (E. coli).  Sixty-one surface-water sampling sites were chosen for this investigation. Synoptic surveys were conducted in July 1988, November 1988, March 1989, and May 1989 to define the concentrations and diel and seasonal variability in concentrations of DO. Synoptic surveys were conducted in July 1988 and July 1989 to define densities of E. coli. Ancillary data included measurements of specific conductance, pH, water temperature. barometric pressure, and concentrations of nutrients, total organic carbon, chlorophyll, and suspended sediment. Surveys were conducted during stable-flow, dry-weather conditions.  During the July 1988 synoptic survey for DO, emphasis was placed on the measurement of DO under maximum stress (high water temperature, low streamflow, and predawn conditions). Of 31 sites sampled just before dawn, 5 had DO concentrations less than the 5.0-milligrams-perliter, l-day minimum warmwater criterion for early life stages as established by the U.S. Environmental Protection Agency (USEPA), and 4 of these 5 sites had concentrations less than the 3.0-milligrams-per-liter criterion for all other life stages. For all four synoptic surveys, a total of 392 DO determinations were made, and 9 (2.3 percent) were less than water-quality criteria. Concentrations of DO less than water-quality criteria in the study unit are localized occurrences and do not reflect regional differences in DO. The most severe DO deficiencies are the result of discharges from wastewater-treatment plants into small tributary streams with inadequate assimilation capacity. Algal respiratory demand in combination with reduced physical reaeration associated with extreme low flow probably also contributes to temporary, localized deficiencies.  Densities of E. coli were determined at 57 surface-water sampling sites during the syn- optic survey in July 1988. Results indicate large regional differences in E. coli densities within the study unit. Densities orE. coli in water at 19 sites in the Big Blue River subbasin, exclusive of the Little Blue River subbasin, ranged from 120 to 260,000 col/100 mL (colonies per 100 milliliters), with a median density of 2,400 col/100 mL. Densities at the 11 sites in the Little Blue River ranged from 100 to 30,000 col/100 mL, with a median density of 940 col/100 mL. Densities at the 27 sites in the Kansas River subbasin ranged from less than 1 to 1,000 col/100 mL, with a median density of 88 col/100 mL. Densities at 84 percent of the sites in the Big Blue River subbasin exceeded the USEPA E. coli criterion of 576 col/100 mL for infrequently used full-body contact recreation, and 53 percent exceeded the 2,000 cot/I00 mL fecal coliform criterion for uses other than full-body contact established by the Kansas Department of Health and Environment. Densities at 73 percent of the sites in the Little Blue River subbasin exceeded the 576 col/100 mL E. coli criterion, and 36 percent exceeded the 2,000 col/100 mL fecal coliform criterion. Densities at one of the sites in the Kansas River subbasin exceeded the 576 col/100 mL E. coli criterion, and none exceeded the 2,000 col/100 mL fecal-coliform criterion.  The largest densities of E. coli in the study unit were the result of discharges from municipal wastewater-treatment plants; however, densities in the Big Blue and Little Blue River subbasins were generally larger than those in the Kansas River subbasin. These larger densities in the Big Blue and Little Blue River subbasins may have been the result of irrigation return flow from fields where manure was used as a soil","language":"English","publisher":"U.S. Geological Survey","doi":"10.3133/wri944077","usgsCitation":"Pope, L.M., 1995, Surface-water-quality assessment of the lower Kansas River basin, Kansas and Nebraska: Dissolved oxygen and Escherichia coli bacteria in streams during low flow, July 1988 through July 1989: U.S. Geological Survey Water-Resources Investigations Report 94-4077, vi, 102 p., https://doi.org/10.3133/wri944077.","productDescription":"vi, 102 p.","costCenters":[],"links":[{"id":58054,"rank":300,"type":{"id":11,"text":"Document"},"url":"https://pubs.usgs.gov/wri/1994/4077/report.pdf","linkFileType":{"id":1,"text":"pdf"}},{"id":159408,"rank":0,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/wri/1994/4077/report-thumb.jpg"},{"id":406352,"rank":3,"type":{"id":36,"text":"NGMDB Index Page"},"url":"https://ngmdb.usgs.gov/Prodesc/proddesc_47973.htm","linkFileType":{"id":5,"text":"html"}}],"country":"United States","state":"Kansas, Nebraska","otherGeospatial":"Kansas River basin","geographicExtents":"{\n  \"type\": \"FeatureCollection\",\n  \"features\": [\n    {\n      \"type\": \"Feature\",\n      \"properties\": {},\n      \"geometry\": {\n        \"type\": \"Polygon\",\n        \"coordinates\": [\n          [\n            [\n              -99,\n              38.650\n            ],\n            [\n              -94.5597,\n              38.650\n            ],\n            [\n              -94.5597,\n              41.2583\n            ],\n            [\n              -99,\n              41.2583\n            ],\n            [\n              -99,\n              38.650\n            ]\n          ]\n        ]\n      }\n    }\n  ]\n}","noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"4f4e4ae5e4b07f02db68a43a","contributors":{"authors":[{"text":"Pope, L. M.","contributorId":71939,"corporation":false,"usgs":true,"family":"Pope","given":"L.","email":"","middleInitial":"M.","affiliations":[],"preferred":false,"id":201111,"contributorType":{"id":1,"text":"Authors"},"rank":1}]}}
,{"id":21504,"text":"ofr9588 - 1995 - Preliminary Geologic Map of the Thousand Oaks 7.5' Quadrangle, Southern California: A Digital Database","interactions":[],"lastModifiedDate":"2012-02-02T00:07:53","indexId":"ofr9588","displayToPublicDate":"1995-07-01T00:00:00","publicationYear":"1995","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":"95-88","title":"Preliminary Geologic Map of the Thousand Oaks 7.5' Quadrangle, Southern California: A Digital Database","docAbstract":"Thousand Oaks is located in Arroyo Conejo, a region spanning both southeastern Ventura County and extreme northwest Los Angeles County in southern California. It was discovered in 1542 by Spanish explorer Juan Rodriquez Cabrillo and eventually became part of the Spanish Rancho El Conejo land grant (conejo means 'rabbit' in Spanish, of which there are many in the area). It is located in the Santa Monica Mountains in the northwestern part of the greater Los Angeles area. The area is bordered by the San Fernando Valley and the city of Los Angeles to the east, Simi Hills to the north, Las Posas Hills and the Santa Rosa Valley to the northwest, Conejo Mountain (also known as Conejo Hills) and Oxnard Plain to the west, and the Santa Monica Mountains and Malibu to the southwest. \r\n\r\nThe geology of the surrounding Santa Monica Mountains is dominated by a sequence of Tertiary sedimentary and volcanic rocks. These include the Tertiary Modelo Formation and the upper part of the Topanga Formation, other minor Tertiary rocks, and Miocene volcanic and intrusive rocks of the Conejo Formation. The basement units within the Santa Monica Mountains are a series of Jurassic and Cretaceous sedimentary rocks. \r\n\r\nThe volcanic rocks of the Conejo Formation underlies much of the surrounding watersheds. The younger Tertiary sedimentary Modelo and Upper Topanga Formations flank the Conejo to the north and south. On the north slope of the Santa Monica Mountains where the Arroyo Conejo and Thousand Oaks are located, the Tertiary formations are gently folded. The south flank of the Santa Monica Mountains is structurally dominated by the Malibu Coast Fault that runs along the foot of the mountains. This fault, and associated structures, creates a complex geologic setting on the south flank of the Santa Monica Mountains. The active nature of the Malibu Coast fault and associated structures accounts for the steep and rugged coastal topography. \r\n\r\nThe most widely exposed rock units in the area are the Plio-Pleistocene marine and nonmarine Pico and Saugus formations, which crop out on the southern flank of South Mountain-Oak Ridge and on the Las Posas uplands and Las Posas Hills. Locally, the Pico Formation consists of marine siltstone and silty shale with minor sandstone and pebbly sandstone. The Saugus Formation overlies and interfingers with the Pico Formation and is composed of interbedded shallow-marine to brackish water sandstone, siltstone, pebble-cobble conglomerate, and coquina beds that grade laterally and vertically into non-marine sandstone, siltstone, and conglomerate. A local member of the Saugus Formation is exposed in the southeast corner of the map area. It is predominantly a volcanic breccia conglomerate that resembles the Conejo Volcanics breccia, but is believed to represent remnants of landslide debris shed from the Conejo Formation into a local trough during Saugus time. \r\n\r\nEroded from, and overlying, these bedrock formations are a series of recent alluvial units. These alluvial units include Quaternary alluvium comprised of alluvium, stream deposits, alluvial fan and floodplain deposits, beach deposits, dissected older alluvial deposits. Also present are Quaternary landslides and colluvium composed of landslide deposits and colluvium deposits. The colluvium represents relatively thick continuous deposits of soil and rock fragments that are common on the steep slopes of the coastal canyons, and generally feed the many landslides, soil slips, and debris flows.","language":"ENGLISH","publisher":"Geological Survey (U.S.)","doi":"10.3133/ofr9588","usgsCitation":"Yerkes, R., and Campbell, R., 1995, Preliminary Geologic Map of the Thousand Oaks 7.5' Quadrangle, Southern California: A Digital Database: U.S. Geological Survey Open-File Report 95-88, Report: 11 p.; ReadMe; GIS Files, https://doi.org/10.3133/ofr9588.","productDescription":"Report: 11 p.; ReadMe; GIS Files","costCenters":[{"id":595,"text":"U.S. Geological Survey","active":false,"usgs":true}],"links":[{"id":154620,"rank":0,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/of/1995/0088/report-thumb.jpg"},{"id":7858,"rank":100,"type":{"id":15,"text":"Index Page"},"url":"https://pubs.usgs.gov/of/1995/of95-088/","linkFileType":{"id":5,"text":"html"}},{"id":51078,"rank":300,"type":{"id":11,"text":"Document"},"url":"https://pubs.usgs.gov/of/1995/0088/report.pdf","linkFileType":{"id":1,"text":"pdf"}}],"noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"4f4e4acce4b07f02db67e6ca","contributors":{"authors":[{"text":"Yerkes, R.F.","contributorId":105752,"corporation":false,"usgs":true,"family":"Yerkes","given":"R.F.","affiliations":[],"preferred":false,"id":184556,"contributorType":{"id":1,"text":"Authors"},"rank":1},{"text":"Campbell, Russell H.","contributorId":91074,"corporation":false,"usgs":true,"family":"Campbell","given":"Russell H.","affiliations":[],"preferred":false,"id":184555,"contributorType":{"id":1,"text":"Authors"},"rank":2}]}}
,{"id":20877,"text":"ofr94475 - 1995 - Water, energy, and biogeochemical budget research at Sleepers River Research Watershed, Vermont","interactions":[],"lastModifiedDate":"2012-02-02T00:07:53","indexId":"ofr94475","displayToPublicDate":"1995-06-01T00:00:00","publicationYear":"1995","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":"94-475","title":"Water, energy, and biogeochemical budget research at Sleepers River Research Watershed, Vermont","docAbstract":"The U.S. Geological Survey has selected the Sleepers River Research Watershed (Sleepers River) near Danville, Vt., as one of five sites for the investigation of Water, Energy, and Biogeochemical Budgets (WEBB). Sleepers River was chosen because it is a well-designed outdoor laboratory with a long history of hydrologic data collection and research, and also because it provides an ideal opportunity for collaboration among the U.S. Geological Survey, other Federal agencies, and universities at the site. The multiple subwatersheds at Sleepers River present a unique opportunity to investigate hydrologic, energy, and biogeochemical processes over a variety of spatial scales. This WEBB study builds on fundamental research on process mechanisms and rates at the plot scale (in this case, a hillslope). Results then are scaled up to interpret the hydrochemical response of first- and higher- order basins. Five research elements make up the Sleepers River WEBB project. Individually, each of the five elements is designed to investigate specific WEBB processes (such as CO2 efflux through a snowpack), address specific WEBB issues (such as scaling and flowpaths), or apply specific WEBB approaches (such as integrated chemical and physical study of a hillslope). The research elements overlap so that many of the processes investigated will be assessed in more than one way, thus allowing independent verification of research results. For example, flowpath information will be derived separately by use of isotopic tracers, conservative chemical solutes, and soil-moisture fluxes. Collectively, the five elements constitute an integrated approach to a comprehensive understanding of WEBB processes needed for the prediction of the effects of global change.","language":"ENGLISH","publisher":"U.S. Geological Survey ;\r\nOpen-File Reports Section [distributor],","doi":"10.3133/ofr94475","usgsCitation":"Shanley, J.B., Sundquist, E., and Kendall, C., 1995, Water, energy, and biogeochemical budget research at Sleepers River Research Watershed, Vermont: U.S. Geological Survey Open-File Report 94-475, iv, 22 p. :ill., map ;28 cm., https://doi.org/10.3133/ofr94475.","productDescription":"iv, 22 p. :ill., map ;28 cm.","costCenters":[],"links":[{"id":154841,"rank":0,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/of/1994/0475/report-thumb.jpg"},{"id":50472,"rank":300,"type":{"id":11,"text":"Document"},"url":"https://pubs.usgs.gov/of/1994/0475/report.pdf","linkFileType":{"id":1,"text":"pdf"}}],"noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"4f4e4a0de4b07f02db5fd156","contributors":{"authors":[{"text":"Shanley, James B. 0000-0002-4234-3437 jshanley@usgs.gov","orcid":"https://orcid.org/0000-0002-4234-3437","contributorId":1953,"corporation":false,"usgs":true,"family":"Shanley","given":"James","email":"jshanley@usgs.gov","middleInitial":"B.","affiliations":[{"id":466,"text":"New England Water Science Center","active":true,"usgs":true},{"id":405,"text":"NH/VT office of New England Water Science Center","active":true,"usgs":true}],"preferred":true,"id":183424,"contributorType":{"id":1,"text":"Authors"},"rank":1},{"text":"Sundquist, E.T.","contributorId":13990,"corporation":false,"usgs":true,"family":"Sundquist","given":"E.T.","email":"","affiliations":[],"preferred":false,"id":183425,"contributorType":{"id":1,"text":"Authors"},"rank":2},{"text":"Kendall, Carol 0000-0002-0247-3405 ckendall@usgs.gov","orcid":"https://orcid.org/0000-0002-0247-3405","contributorId":1462,"corporation":false,"usgs":true,"family":"Kendall","given":"Carol","email":"ckendall@usgs.gov","affiliations":[{"id":438,"text":"National Research Program - Western Branch","active":true,"usgs":true}],"preferred":true,"id":183423,"contributorType":{"id":1,"text":"Authors"},"rank":3}]}}
,{"id":35240,"text":"b2094B - 1995 - Lead isotopes from the Upper Mississippi Valley district: A regional perspective","interactions":[],"lastModifiedDate":"2022-05-02T20:06:00.095314","indexId":"b2094B","displayToPublicDate":"1995-06-01T00:00:00","publicationYear":"1995","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":"2094","chapter":"B","title":"Lead isotopes from the Upper Mississippi Valley district: A regional perspective","docAbstract":"New lead isotopic data on galena from within and peripheral to the Upper Mississippi Valley lead-zinc district make it possible, by extending coverage to outlying locations, to trace the pathway traversed by the mineralizing fluids beyond the boundary of the main district. All but one of the samples exhibit elevated ratios of the radiogenic isotopes typical of the Upper Mississippi Valley ore deposits; 206PbP04Pb ranges from 19.38 to 24.46, 207PbP04Pb ranges from 15.73 to 16.24, and 208PbP04Pb ranges from 39.24 to 43.69. Galena from the Pints quarry near Waterloo, Iowa, has distinctly lower values of these ratios and may not be related paragenetically to the other samples. Otherwise, the lowest ratios are for samples in the southern part of the region in north-central Illinois, and the highest ratios are for samples to the northeast of the main district in the vicinity of Madison, Wisconsin. Thus, an isotopic pattern rather similar to that observed originally by Heyl and others (1966) prevails regionally, although the predominant fluid flow is now believed to have emanated from the Illinois Basin rather than from the Forest City Basin. Metal-bearing brines being driven northward out of the Illinois Basin probably played the key role in mineralization of the Upper Mississippi Valley district.\r\n\r\nBoth the new and the previously reported lead ratios for the Upper Mississippi Valley district are plotted on 207PbP04Pb and Pb208/pb204Pb versus 206PbP04Pb diagrams, which permit their comparison and the calculation of refined slopes for the expanded data set. A two-stage model age for the time of mineralization can be determined from the 207PbP04Pb_Pb206/Pb204 slope, provided that the source age of the lead is known. With our limited know ledge of this source age, the time of mineralization cannot be tightly constrained but is permissive of a Permian or younger lateral secretion event, as suggested by other geochronological results.","largerWorkType":{"id":18,"text":"Report"},"largerWorkTitle":"Evolution of sedimentary basins - Illinois Basin","largerWorkSubtype":{"id":5,"text":"USGS Numbered Series"},"language":"English","publisher":"U.S. Geological Survey","doi":"10.3133/b2094B","usgsCitation":"Millen, T.M., Zartman, R.E., and Heyl, A.V., 1995, Lead isotopes from the Upper Mississippi Valley district: A regional perspective: U.S. Geological Survey Bulletin 2094, iii, 13 p., https://doi.org/10.3133/b2094B.","productDescription":"iii, 13 p.","costCenters":[{"id":595,"text":"U.S. Geological Survey","active":false,"usgs":true}],"links":[{"id":167399,"rank":0,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/bul/2094b/report-thumb.jpg"},{"id":63119,"rank":300,"type":{"id":11,"text":"Document"},"url":"https://pubs.usgs.gov/bul/2094b/report.pdf","linkFileType":{"id":1,"text":"pdf"}},{"id":399986,"rank":3,"type":{"id":36,"text":"NGMDB Index Page"},"url":"https://ngmdb.usgs.gov/Prodesc/proddesc_22394.htm"}],"country":"United States","state":"Illinois, Iowa, Wisconsin","geographicExtents":"{\n  \"type\": \"FeatureCollection\",\n  \"features\": [\n    {\n      \"type\": \"Feature\",\n      \"properties\": {},\n      \"geometry\": {\n        \"type\": \"Polygon\",\n        \"coordinates\": [\n          [\n            [\n              -92.25,\n              41.5\n            ],\n            [\n              -88,\n              41.5\n            ],\n            [\n              -88,\n              43.5\n            ],\n            [\n              -92.25,\n              43.5\n            ],\n            [\n              -92.25,\n              41.5\n            ]\n          ]\n        ]\n      }\n    }\n  ]\n}","noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"4f4e4b1be4b07f02db6a8945","contributors":{"authors":[{"text":"Millen, Timothy M.","contributorId":79538,"corporation":false,"usgs":true,"family":"Millen","given":"Timothy","email":"","middleInitial":"M.","affiliations":[],"preferred":false,"id":214306,"contributorType":{"id":1,"text":"Authors"},"rank":1},{"text":"Zartman, Robert E.","contributorId":47356,"corporation":false,"usgs":true,"family":"Zartman","given":"Robert","email":"","middleInitial":"E.","affiliations":[],"preferred":false,"id":214305,"contributorType":{"id":1,"text":"Authors"},"rank":2},{"text":"Heyl, Allen Van","contributorId":91078,"corporation":false,"usgs":true,"family":"Heyl","given":"Allen","email":"","middleInitial":"Van","affiliations":[],"preferred":false,"id":214307,"contributorType":{"id":1,"text":"Authors"},"rank":3}]}}
,{"id":27595,"text":"wri944164 - 1995 - Use of fathometers and electrical-conductivity probes to monitor riverbed scour at bridge piers","interactions":[],"lastModifiedDate":"2012-02-02T00:08:39","indexId":"wri944164","displayToPublicDate":"1995-06-01T00:00:00","publicationYear":"1995","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":"94-4164","title":"Use of fathometers and electrical-conductivity probes to monitor riverbed scour at bridge piers","docAbstract":"Two methods, a fathometer system and an electrical- conductivity probe system, were developed to monitor scour at bridge piers. The scour-monitoring systems consisted of a sensor (fathometer or electrical- conductivity probe), power supply, data logger, relay, and system program. The fathometer system was installed and tested at a bridge over the Leipsic River at Leipsic, Delaware, and at a bridge over Sinepuxent Bay near Ocean City. Maryland. Field data collected indicate that fathometers can be used to identify and monitor the riverbed elevation if post processing of the data and trends in the data are used to determine the riverbed location in relation to the transducer. The accuracy of the system is approximately the same as the resolution of the fathometer. Signal scatter can be a major source of error in the data. The electrical- conductivity probe system was installed and tested at a bridge over the Pamunkey River near Hanover, Virginia. The approximate elevation of the riverbed is determined by comparing conductivities of the surface-water flow with conductivities of submerged bed material from sensors located in each. Field data collected indicate that an electrical- conductivity probe, as tested, has limited usefulness in identifying and monitoring the riverbed elevation during high flows. As the discharge increases, the concentration of sediment in the surface-water flow increases, especially near the riverbed. Conductivities, measured at the sensors in the surface-water flow could not be distinguished from conductivities measured at the shallowest sensor in the submerged bed material.","language":"ENGLISH","publisher":"U.S. Geological Survey ;\r\nUSGS Earth Science Information Center, Open-File Reports Section [distributor],","doi":"10.3133/wri944164","usgsCitation":"Hayes, D.C., and Drummond, F., 1995, Use of fathometers and electrical-conductivity probes to monitor riverbed scour at bridge piers: U.S. Geological Survey Water-Resources Investigations Report 94-4164, iv, 17 p. :ill., map ;28 cm., https://doi.org/10.3133/wri944164.","productDescription":"iv, 17 p. :ill., map ;28 cm.","costCenters":[],"links":[{"id":158814,"rank":0,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/wri/1994/4164/report-thumb.jpg"},{"id":56466,"rank":300,"type":{"id":11,"text":"Document"},"url":"https://pubs.usgs.gov/wri/1994/4164/report.pdf","linkFileType":{"id":1,"text":"pdf"}}],"noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"4f4e4882e4b07f02db516b6d","contributors":{"authors":[{"text":"Hayes, Donald C.","contributorId":14000,"corporation":false,"usgs":true,"family":"Hayes","given":"Donald","email":"","middleInitial":"C.","affiliations":[],"preferred":false,"id":198384,"contributorType":{"id":1,"text":"Authors"},"rank":1},{"text":"Drummond, F.E.","contributorId":63057,"corporation":false,"usgs":true,"family":"Drummond","given":"F.E.","email":"","affiliations":[],"preferred":false,"id":198385,"contributorType":{"id":1,"text":"Authors"},"rank":2}]}}
,{"id":38208,"text":"pp1559 - 1995 - Geochemistry and petrology of Oligocene and Miocene ash-flow tuffs of the southeastern Great Basin, Nevada","interactions":[],"lastModifiedDate":"2012-02-02T00:10:01","indexId":"pp1559","displayToPublicDate":"1995-05-01T00:00:00","publicationYear":"1995","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":"1559","title":"Geochemistry and petrology of Oligocene and Miocene ash-flow tuffs of the southeastern Great Basin, Nevada","docAbstract":"The White River Narrows area of Southeast Nevada contains 18 regionally distributed middle Tertiary dacite to rhyolite ash-flow tuffs. Geochemical data provide an excellent opportunity to study stratigraphic and petrologic relations of these tuffs. Chemical data for each of the tuffs are distinctive and provide a significant addition to other data used to identify and correlate these units. Relatively minor compositional variation within the tuffs is noteworthy.","language":"ENGLISH","doi":"10.3133/pp1559","usgsCitation":"du Bray, E.A., 1995, Geochemistry and petrology of Oligocene and Miocene ash-flow tuffs of the southeastern Great Basin, Nevada: U.S. Geological Survey Professional Paper 1559, 62 p., https://doi.org/10.3133/pp1559.","productDescription":"62 p.","costCenters":[],"links":[{"id":122085,"rank":0,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/pp/1559/report-thumb.jpg"},{"id":64511,"rank":300,"type":{"id":11,"text":"Document"},"url":"https://pubs.usgs.gov/pp/1559/report.pdf","linkFileType":{"id":1,"text":"pdf"}}],"noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"4f4e4b1fe4b07f02db6ab705","contributors":{"authors":[{"text":"du Bray, Edward A. 0000-0002-4383-8394 edubray@usgs.gov","orcid":"https://orcid.org/0000-0002-4383-8394","contributorId":755,"corporation":false,"usgs":true,"family":"du Bray","given":"Edward","email":"edubray@usgs.gov","middleInitial":"A.","affiliations":[{"id":164,"text":"Central Energy Resources Science Center","active":true,"usgs":true},{"id":171,"text":"Central Mineral and Environmental Resources Science Center","active":true,"usgs":true}],"preferred":true,"id":219335,"contributorType":{"id":1,"text":"Authors"},"rank":1}]}}
,{"id":28350,"text":"wri944118 - 1995 - Quality of water in the alluvial aquifer and tributary alluvium of the Fountain Creek valley, southwestern El Paso County, Colorado, 1991-92","interactions":[],"lastModifiedDate":"2012-02-02T00:08:35","indexId":"wri944118","displayToPublicDate":"1995-03-01T00:00:00","publicationYear":"1995","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":"94-4118","title":"Quality of water in the alluvial aquifer and tributary alluvium of the Fountain Creek valley, southwestern El Paso County, Colorado, 1991-92","docAbstract":"The alluvial aquifer in Fountain Creek Valley between Colorado Springs and Widefield is the source for several public water-supply systems. Since 1981, concentrations of dissolved nitrite plus nitrate as nitrogen (nitrate) have exceeded the drinking-water standard of 10 milligrams per liter in several areas of the aquifer. Water-quality data collected quarterly from August 1991 through October 1992 from a network of 63 wells were used to define the spatial and temporal variability of dissolved- oxygen, dissolved-solids, major ions, and nitrogen concentrations in the aquifer. Ground water generally was well oxygenated in the main body of the aquifer, but anoxic conditions occurred near the interface of the aquifer and Fountain Creek. Dissolved-solids concentrations generally were larger, and nitrate concentrations generally were smaller near Fountain Creek than in the main body of the aquifer. Dissolved-solids concentrations generally decreased and nitrate concentrations generally increased with distance from the creek. Ground-water flow toward Fountain Creek and relatively small dissolved-solids concentrations in the main body of the aquifer indicated that the primary source of recharge to the aquifer was surface recharge from precipitation and lawn irrigation. Natural soil nitrogen, lawn fertilizers, and leakage from industrial-waste lagoons seem to be major sources of nitrate in ground water.","language":"ENGLISH","publisher":"U.S. Geological Survey :\r\nEarth Science Information Center, Open-File Reports Section [distributor],","doi":"10.3133/wri944118","usgsCitation":"Lewis, M., 1995, Quality of water in the alluvial aquifer and tributary alluvium of the Fountain Creek valley, southwestern El Paso County, Colorado, 1991-92: U.S. Geological Survey Water-Resources Investigations Report 94-4118, iv, 39 p. :ill., maps ;28 cm. [PGS - 61 p.], https://doi.org/10.3133/wri944118.","productDescription":"iv, 39 p. :ill., maps ;28 cm. [PGS - 61 p.]","costCenters":[],"links":[{"id":158324,"rank":0,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/wri/1994/4118/report-thumb.jpg"},{"id":57156,"rank":300,"type":{"id":11,"text":"Document"},"url":"https://pubs.usgs.gov/wri/1994/4118/report.pdf","linkFileType":{"id":1,"text":"pdf"}}],"noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"4f4e4a6de4b07f02db63ef3f","contributors":{"authors":[{"text":"Lewis, M.E.","contributorId":65504,"corporation":false,"usgs":true,"family":"Lewis","given":"M.E.","email":"","affiliations":[],"preferred":false,"id":199645,"contributorType":{"id":1,"text":"Authors"},"rank":1}]}}
,{"id":20559,"text":"ofr95361 - 1995 - Data on quantity and quality of water flowing in drainage systems of dry docks at Puget Sound Naval Shipyard, Bremerton, Washington, 1994","interactions":[],"lastModifiedDate":"2022-07-14T15:45:00.055633","indexId":"ofr95361","displayToPublicDate":"1995-01-01T00:00:00","publicationYear":"1995","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":"95-361","title":"Data on quantity and quality of water flowing in drainage systems of dry docks at Puget Sound Naval Shipyard, Bremerton, Washington, 1994","docAbstract":"<p>Data on the quantity and quality of ground water that drains into dry docks at the Puget Sound Naval Shipyard can be useful for planning environmental remediation work at the shipyard. Ground-water discharges into and total drain-water discharges from individual dry docks were computed from a single set of discharges of individual inflowing drains' and outflowing drain-water collection culverts that were measured in June, July and August 1994. Ground-water inflows to dry docks no. 1, 2, 3, 4, 5, and 6 equalled 0.07, 0.30, 0.29, 0.61, 1.18, and 6.2 cubic feet per second, respectively, and total drain-water discharges from the dry docks equalled 0.07, 0.30, 0.33, 0.61, 1.36, and 11.7 cubic feet per second, respectively. The differences between total outflows and ground-water inflows were mostly cofferdam and floodgate leakage and cooling water from a ship in dry dock no. 6. Observed salinities indicate that 18, 92, 28, 44, 55, and 69 percent of the ground-water inflows to dry docks no. 1 through 6 and 18, 92, 37, 44, 63, and 82 percent of the total outflows from the dry docks was saline water from Sinclair Inlet.</p><p>Concentrations of total copper in samples from 36 sites varied from less than 1 to 71 micrograms per liter, and concentrations of total lead varied from less than 1 to 44 micrograms per liter. None of 43 semi-volatile organic compounds that were analyzed for in samples from 19 sites were detected at concentrations greater than the laboratory minimum reporting level (5 or 10 micrograms per liter). A total of 13 volatile organic compounds were found at concentrations greater than laboratory minimum reporting levels (mostly 0.2 microgram per liter) in 8 samples that were analyzed for 63 volatile organic compounds. Trichloroethene and at least three other chlorinated hydrocarbons were found in each sample.</p>","language":"English","publisher":"U.S. Geological Survey","doi":"10.3133/ofr95361","collaboration":"Prepared in cooperation with the Department of the Navy Engineering Field Activity, Northwest Naval Facilities Engineering Command","usgsCitation":"Prych, E.A., 1995, Data on quantity and quality of water flowing in drainage systems of dry docks at Puget Sound Naval Shipyard, Bremerton, Washington, 1994: U.S. Geological Survey Open-File Report 95-361, v, 58 p., https://doi.org/10.3133/ofr95361.","productDescription":"v, 58 p.","costCenters":[],"links":[{"id":19368,"rank":300,"type":{"id":11,"text":"Document"},"url":"https://pubs.usgs.gov/of/1995/0361/report.pdf","linkFileType":{"id":1,"text":"pdf"}},{"id":152767,"rank":0,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/of/1995/0361/report-thumb.jpg"}],"country":"United States","state":"Washington","city":"Bremerton","otherGeospatial":"Puget Sound Naval Shipyard","geographicExtents":"{\n  \"type\": \"FeatureCollection\",\n  \"features\": [\n    {\n      \"type\": \"Feature\",\n      \"properties\": {},\n      \"geometry\": {\n        \"type\": \"Polygon\",\n        \"coordinates\": [\n          [\n            [\n              -122.66321182250977,\n              47.54913099905259\n            ],\n            [\n              -122.62475967407225,\n              47.54913099905259\n            ],\n            [\n              -122.62475967407225,\n              47.56424909302446\n            ],\n            [\n              -122.66321182250977,\n              47.56424909302446\n            ],\n            [\n              -122.66321182250977,\n              47.54913099905259\n            ]\n          ]\n        ]\n      }\n    }\n  ]\n}","noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"4f4e4ac8e4b07f02db67bd61","contributors":{"authors":[{"text":"Prych, Edmund A.","contributorId":38139,"corporation":false,"usgs":true,"family":"Prych","given":"Edmund","email":"","middleInitial":"A.","affiliations":[],"preferred":false,"id":182842,"contributorType":{"id":1,"text":"Authors"},"rank":1}]}}
,{"id":95298,"text":"95298 - 1995 - Acidic deposition (\"acid rain\")","interactions":[{"subject":{"id":95298,"text":"95298 - 1995 - Acidic deposition (\"acid rain\")","indexId":"95298","publicationYear":"1995","noYear":false,"title":"Acidic deposition (\"acid rain\")"},"predicate":"IS_PART_OF","object":{"id":70148108,"text":"70148108 - 1995 - Our living resources: A report to the nation on the distribution, abundance, and health of U.S. plants, animals, and ecosystems","indexId":"70148108","publicationYear":"1995","noYear":false,"title":"Our living resources: A report to the nation on the distribution, abundance, and health of U.S. plants, animals, and ecosystems"},"id":1}],"isPartOf":{"id":70148108,"text":"70148108 - 1995 - Our living resources: A report to the nation on the distribution, abundance, and health of U.S. plants, animals, and ecosystems","indexId":"70148108","publicationYear":"1995","noYear":false,"title":"Our living resources: A report to the nation on the distribution, abundance, and health of U.S. plants, animals, and ecosystems"},"lastModifiedDate":"2017-04-19T11:19:36","indexId":"95298","displayToPublicDate":"1995-01-01T00:00:00","publicationYear":"1995","noYear":false,"publicationType":{"id":5,"text":"Book chapter"},"publicationSubtype":{"id":24,"text":"Book Chapter"},"title":"Acidic deposition (\"acid rain\")","docAbstract":"<p>Acidic deposition, or \"acid rain,\" describes any form of precipitation, including rain, snow, and fog, with a pH of 5.5 or below (Note: pH values below 7 are acidic; vinegar has a pH of 3). It often results when the acidity of normal precipitation is increased by sulfates and nitrates that are emitted into the atmosphere from burning fossil fuels. This form of airborne contamination is considered harmful, both directly and indirectly, to a host of plant and animal species.</p><p>Although acid rain can fall virtually anywhere, ecological damages in environmentally sensitive areas downwind of industrial and urban emissions are a major concern. This includes areas that have a reduced capacity to neutralize acid inputs because of low alkalinity soils and areas that contain species with a low tolerance to acid conditions. To determine the distribution of acidic deposition and evaluate its biological effects, research and monitoring are being conducted by the federal government with support from states, universities, and private industry.&nbsp;&nbsp;&nbsp;&nbsp;&nbsp;&nbsp;&nbsp;&nbsp;&nbsp;&nbsp;&nbsp;&nbsp;</p><p>The national extent of the acid rain problem has been estimated by sampling water from 3,000 lakes and 500 streams (Irving 1991), representing more than 28,000 lakes and 56,000 stream reaches with a total of 200,000 km (125,000 mi). Some particularly sensitive areas, such as the Adirondack Mountain region, have been more intensively sampled and the biota examined in detail for effects from acidity.&nbsp;&nbsp;&nbsp;&nbsp;&nbsp;&nbsp;&nbsp;&nbsp;&nbsp;</p><p>To identify trends in aquatic ecosystems, present and historical survey data on water chemistry and associated biota are compared. In lakes, the chemical and biological history and pH trends may be inferred or reconstructed in some cases by examining assemblages of fossil diatoms and aquatic invertebrates in the sediment layers. In terrestrial ecosystems, vegetation damage is surveyed and effects of acidic deposition to plants and animals are determined from laboratory and field exposure experiments. Natural variation in populations and the complex interactions between acidity and other ecosystem components make it difficult to extend many of the research findings to populations or communities. Acidity can also modify ecosystem processes such as decomposition and the flow of nutrients. Therefore, models are often used to predict such effects by combining information on individual species' effects, population distributions, and the patterns and amounts of acidic deposition.</p>","largerWorkType":{"id":4,"text":"Book"},"largerWorkTitle":"Our living resources: A report to the nation on the distribution, abundance, and health of U.S. plants, animals, and ecosystems","largerWorkSubtype":{"id":15,"text":"Monograph"},"language":"English","publisher":"National Biological Service","publisherLocation":"Washington, D.C.","usgsCitation":"Schreiber, R.K., 1995, Acidic deposition (\"acid rain\"), chap. <i>of</i> Our living resources: A report to the nation on the distribution, abundance, and health of U.S. plants, animals, and ecosystems, p. 418-420.","productDescription":"3 p.","startPage":"418","endPage":"420","costCenters":[{"id":365,"text":"Leetown Science Center","active":true,"usgs":true}],"links":[{"id":127448,"rank":0,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/thumbnails/outside_thumb.jpg"},{"id":339948,"rank":2,"type":{"id":11,"text":"Document"},"url":"https://www.webharvest.gov/peth04/20041019015728/https://biology.usgs.gov/s+t/index.htm","linkHelpText":"Archived website"}],"noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"4f4e4b13e4b07f02db6a350b","contributors":{"editors":[{"text":"LaRoe, Edward T.","contributorId":112276,"corporation":false,"usgs":true,"family":"LaRoe","given":"Edward","email":"","middleInitial":"T.","affiliations":[],"preferred":false,"id":505506,"contributorType":{"id":2,"text":"Editors"},"rank":1},{"text":"Farris, Gaye S.","contributorId":84410,"corporation":false,"usgs":true,"family":"Farris","given":"Gaye","email":"","middleInitial":"S.","affiliations":[{"id":455,"text":"National Wetlands Research Center","active":true,"usgs":true}],"preferred":true,"id":505509,"contributorType":{"id":2,"text":"Editors"},"rank":2},{"text":"Puckett, Catherine E. cpuckett@usgs.gov","contributorId":4629,"corporation":false,"usgs":true,"family":"Puckett","given":"Catherine","email":"cpuckett@usgs.gov","middleInitial":"E.","affiliations":[],"preferred":true,"id":505507,"contributorType":{"id":2,"text":"Editors"},"rank":3},{"text":"Doran, Peter D.","contributorId":17533,"corporation":false,"usgs":true,"family":"Doran","given":"Peter","email":"","middleInitial":"D.","affiliations":[],"preferred":false,"id":505508,"contributorType":{"id":2,"text":"Editors"},"rank":4},{"text":"Mac, Michael J.","contributorId":16772,"corporation":false,"usgs":true,"family":"Mac","given":"Michael","email":"","middleInitial":"J.","affiliations":[],"preferred":false,"id":505505,"contributorType":{"id":2,"text":"Editors"},"rank":5}],"authors":[{"text":"Schreiber, R. Kent","contributorId":58145,"corporation":false,"usgs":true,"family":"Schreiber","given":"R.","email":"","middleInitial":"Kent","affiliations":[],"preferred":false,"id":298836,"contributorType":{"id":1,"text":"Authors"},"rank":1}]}}
,{"id":54860,"text":"wdrNY942 - 1995 - Water resources data, New York, water year 1994. Volume 2. Long Island","interactions":[],"lastModifiedDate":"2025-03-14T19:23:59.537356","indexId":"wdrNY942","displayToPublicDate":"1995-01-01T00:00:00","publicationYear":"1995","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":"NY-94-2","title":"Water resources data, New York, water year 1994. Volume 2. Long Island","docAbstract":"<p>Water resources data for the 1994 water year for New York 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 wells. This volume contains records for water discharge at 20 gaging stations; water quality at 19 gaging stations, and 32 wells; and water levels at 754 observation wells. Also included are data for 78 low-flow 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 and analyses. These data, together with the data in Volume 1 and 3 represent that part of the National Water Data system operated by the U.S. Geological Survey in cooperation with State, Federal, and other agencies in New York </p>","language":"English","publisher":"U.S. Geological Survey","doi":"10.3133/wdrNY942","collaboration":"Prepared in cooperation with the State of New York and with other agencies","usgsCitation":"Spinello, A.G., Pena-Cruz, G., McGrath, K., and Eagen, V.K., 1995, Water resources data, New York, water year 1994. Volume 2. Long Island: U.S. Geological Survey Water Data Report NY-94-2, vii, 240 p., https://doi.org/10.3133/wdrNY942.","productDescription":"vii, 240 p.","costCenters":[],"links":[{"id":416551,"rank":1,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/wdr/1994/ny-94-2/report-thumb.jpg"},{"id":483392,"rank":2,"type":{"id":11,"text":"Document"},"url":"https://pubs.usgs.gov/wdr/1994/ny-94-2/report.pdf","linkFileType":{"id":1,"text":"pdf"}}],"country":"United States","state":"New York","otherGeospatial":"Long Island","geographicExtents":"{\n  \"type\": \"FeatureCollection\",\n  \"features\": [\n    {\n      \"type\": \"Feature\",\n      \"properties\": {},\n      \"geometry\": {\n        \"type\": \"Polygon\",\n        \"coordinates\": [\n          [\n            [\n              -74.14672851562499,\n              40.47620304302563\n            ],\n            [\n              -71.751708984375,\n              40.47620304302563\n            ],\n            [\n              -71.751708984375,\n              41.25716209782705\n            ],\n            [\n              -74.14672851562499,\n              41.25716209782705\n            ],\n            [\n              -74.14672851562499,\n              40.47620304302563\n            ]\n          ]\n        ]\n      }\n    }\n  ]\n}","noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"4f4e4a0ae4b07f02db5fb17a","contributors":{"authors":[{"text":"Spinello, A. G.","contributorId":19983,"corporation":false,"usgs":true,"family":"Spinello","given":"A.","email":"","middleInitial":"G.","affiliations":[],"preferred":false,"id":251797,"contributorType":{"id":1,"text":"Authors"},"rank":1},{"text":"Pena-Cruz, G.","contributorId":26747,"corporation":false,"usgs":true,"family":"Pena-Cruz","given":"G.","email":"","affiliations":[],"preferred":false,"id":251799,"contributorType":{"id":1,"text":"Authors"},"rank":2},{"text":"McGrath, K.","contributorId":33175,"corporation":false,"usgs":true,"family":"McGrath","given":"K.","email":"","affiliations":[],"preferred":false,"id":251800,"contributorType":{"id":1,"text":"Authors"},"rank":3},{"text":"Eagen, V. K.","contributorId":20353,"corporation":false,"usgs":true,"family":"Eagen","given":"V.","email":"","middleInitial":"K.","affiliations":[],"preferred":false,"id":251798,"contributorType":{"id":1,"text":"Authors"},"rank":4}]}}
,{"id":70018806,"text":"70018806 - 1995 - Determination of nanogram per liter concentrations of volatile organic compounds in water by capillary gas chromatography and selected ion monitoring mass spectrometry and its use to define groundwater flow directions in Edwards Aquifer, Texas","interactions":[],"lastModifiedDate":"2021-05-27T15:41:13.404596","indexId":"70018806","displayToPublicDate":"1995-01-01T00:00:00","publicationYear":"1995","noYear":false,"publicationType":{"id":2,"text":"Article"},"publicationSubtype":{"id":10,"text":"Journal Article"},"seriesTitle":{"id":761,"text":"Analytical Chemistry","active":true,"publicationSubtype":{"id":10}},"title":"Determination of nanogram per liter concentrations of volatile organic compounds in water by capillary gas chromatography and selected ion monitoring mass spectrometry and its use to define groundwater flow directions in Edwards Aquifer, Texas","docAbstract":"A method has been developed to measure nanogram per liter amounts of selected volatile organic compounds (VOCs) including dichlorodifluoromethane, trichlorofluoromethane, cis-1,2-dichloroethene, trichloroethene, tetrachloroethene, and the isomers of dichlorobenzene in water. The method uses purge-and-trap techniques on a 100 mL sample, gas chromatography with a megabore capillary column, and electron impact, selected ion monitoring mass spectrometry. Minimum detection levels for these compounds ranged from 1 to 4 ng/L in water. Recoveries from organic-free distilled water and natural groundwater ranged from 70.5% for dichlorodifluoromethane to 107.8% for 1,4-dichlorobenzene. Precision was generally best for cis-1,2-dichloroethene, tetrachloroethene, and the dichlorobenzene isomers and worst for dichlorodifluoromethane and trichlorofluoromethane. Blank data indicated persistent, trace-level introduction of dichlorodifluoromethane, 1,4-dichlorobenzene, and tetrachloroemene to samples during storage and shipment at concentrations less than the method reporting limits. The largest concentrations of the selected VOCs in 27 water samples from the Edwards aquifer near San Antonio, TX, were from confined-zone wells near an abandoned landfill. The results defined a zone of water with no detectable VOCs in nearly all of the aquifer west of San Antonio and from part of the confined zone beneath San Antonio.","largerWorkType":{"id":2,"text":"Article"},"largerWorkTitle":"Analytical Chemistry","largerWorkSubtype":{"id":10,"text":"Journal Article"},"language":"English","doi":"10.1021/ac00116a008","issn":"00032700","usgsCitation":"Buszka, P., Rose, D., Ozuna, G., and Groschen, G., 1995, Determination of nanogram per liter concentrations of volatile organic compounds in water by capillary gas chromatography and selected ion monitoring mass spectrometry and its use to define groundwater flow directions in Edwards Aquifer, Texas: Analytical Chemistry, v. 67, no. 20, p. 3659-3667, https://doi.org/10.1021/ac00116a008.","startPage":"3659","endPage":"3667","numberOfPages":"9","costCenters":[{"id":452,"text":"National Water Quality Laboratory","active":true,"usgs":true}],"links":[{"id":227050,"rank":0,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/thumbnails/outside_thumb.jpg"}],"volume":"67","issue":"20","noUsgsAuthors":false,"publicationDate":"2002-05-01","publicationStatus":"PW","scienceBaseUri":"5059ffb8e4b0c8380cd4f35e","contributors":{"authors":[{"text":"Buszka, P.M.","contributorId":49001,"corporation":false,"usgs":true,"family":"Buszka","given":"P.M.","affiliations":[],"preferred":false,"id":380809,"contributorType":{"id":1,"text":"Authors"},"rank":1},{"text":"Rose, D.L.","contributorId":36960,"corporation":false,"usgs":true,"family":"Rose","given":"D.L.","email":"","affiliations":[],"preferred":false,"id":380808,"contributorType":{"id":1,"text":"Authors"},"rank":2},{"text":"Ozuna, G. B.","contributorId":25205,"corporation":false,"usgs":true,"family":"Ozuna","given":"G. B.","affiliations":[],"preferred":false,"id":380807,"contributorType":{"id":1,"text":"Authors"},"rank":3},{"text":"Groschen, G.E.","contributorId":17260,"corporation":false,"usgs":true,"family":"Groschen","given":"G.E.","email":"","affiliations":[],"preferred":false,"id":380806,"contributorType":{"id":1,"text":"Authors"},"rank":4}]}}
,{"id":6716,"text":"fs09595 - 1995 - Using geochemical data to identify sources of salinity to the freshwater Navajo aquifer in southeastern Utah","interactions":[],"lastModifiedDate":"2017-02-03T11:38:41","indexId":"fs09595","displayToPublicDate":"1994-01-01T00:00:00","publicationYear":"1995","noYear":false,"publicationType":{"id":18,"text":"Report"},"publicationSubtype":{"id":5,"text":"USGS Numbered Series"},"seriesTitle":{"id":313,"text":"Fact Sheet","code":"FS","onlineIssn":"2327-6932","printIssn":"2327-6916","active":true,"publicationSubtype":{"id":5}},"seriesNumber":"095-95","title":"Using geochemical data to identify sources of salinity to the freshwater Navajo aquifer in southeastern Utah","docAbstract":"<p><span>Ground water is an important freshwater source for domestic and livestock uses in southeastern Utah because of the arid climate and unavailability of surface water from the San Juan River. The study area includes about 1,200 square miles in the southeastern corner of Utah (fig. 1). Precipitation on mountainous areas north, south, and east of the study area (fig. 2) seeps into the Navajo and overlying aquifers where the sandstones that contain the aquifers are exposed at the surface along mountain flanks. The ground water then moves slowly away from the mountainous areas toward the area of lowest elevation 109°30' in the region, the San Juan River. The ground water reappears at land surface where it discharges as seepage to the San Juan River or is consumed by vegetation on the flood plain. Generally, wells finished in the Navajo aquifer near the San Juan River do not require pumping because water flows freely from the well casing when it is not sealed.</span></p>","language":"English","publisher":"U.S. Geological Survey","publisherLocation":"Salt Lake City, UT","doi":"10.3133/fs09595","usgsCitation":"Naftz, D.L., Spangler, L.E., and Peterman, Z., 1995, Using geochemical data to identify sources of salinity to the freshwater Navajo aquifer in southeastern Utah: U.S. Geological Survey Fact Sheet 095-95, 4 p., https://doi.org/10.3133/fs09595.","productDescription":"4 p.","numberOfPages":"4","costCenters":[{"id":218,"text":"Denver Federal Center","active":false,"usgs":true},{"id":610,"text":"Utah Water Science Center","active":true,"usgs":true},{"id":5050,"text":"WY-MT Water Science Center","active":true,"usgs":true}],"links":[{"id":125233,"rank":0,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/fs/1995/0095/report-thumb.jpg"},{"id":34107,"rank":300,"type":{"id":11,"text":"Document"},"url":"https://pubs.usgs.gov/fs/1995/0095/report.pdf","linkFileType":{"id":1,"text":"pdf"}}],"country":"United States","state":"Utah","noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"4f4e4a16e4b07f02db603c4f","contributors":{"authors":[{"text":"Naftz, David L. 0000-0003-1130-6892 dlnaftz@usgs.gov","orcid":"https://orcid.org/0000-0003-1130-6892","contributorId":1041,"corporation":false,"usgs":true,"family":"Naftz","given":"David","email":"dlnaftz@usgs.gov","middleInitial":"L.","affiliations":[{"id":610,"text":"Utah Water Science Center","active":true,"usgs":true},{"id":5050,"text":"WY-MT Water Science Center","active":true,"usgs":true}],"preferred":true,"id":153209,"contributorType":{"id":1,"text":"Authors"},"rank":1},{"text":"Spangler, Lawrence E. 0000-0003-3928-8809 spangler@usgs.gov","orcid":"https://orcid.org/0000-0003-3928-8809","contributorId":973,"corporation":false,"usgs":true,"family":"Spangler","given":"Lawrence","email":"spangler@usgs.gov","middleInitial":"E.","affiliations":[{"id":610,"text":"Utah Water Science Center","active":true,"usgs":true}],"preferred":true,"id":153208,"contributorType":{"id":1,"text":"Authors"},"rank":2},{"text":"Peterman, Zell E. 0000-0002-5694-8082 peterman@usgs.gov","orcid":"https://orcid.org/0000-0002-5694-8082","contributorId":620,"corporation":false,"usgs":true,"family":"Peterman","given":"Zell E.","email":"peterman@usgs.gov","affiliations":[{"id":218,"text":"Denver Federal Center","active":false,"usgs":true}],"preferred":false,"id":153207,"contributorType":{"id":1,"text":"Authors"},"rank":3}]}}
,{"id":54165,"text":"wdrCO951 - 1995 - Water Resources Data, Colorado, Water Year 1995--Volume 1. Missouri River Basin, Arkansas River Basin, and Rio Grande Basin","interactions":[],"lastModifiedDate":"2012-02-02T00:12:07","indexId":"wdrCO951","displayToPublicDate":"1994-01-01T00:00:00","publicationYear":"1995","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":"CO-95-1","title":"Water Resources Data, Colorado, Water Year 1995--Volume 1. Missouri River Basin, Arkansas River Basin, and Rio Grande Basin","docAbstract":"Water-resources data for Colorado for the 1995 water year 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 wells and springs. This report (Volumes 1 and 2) contains discharge records for 335 gaging stations, stage and contents of 26 lakes and reservoirs, 1 partial-record low-flow station, peak-flow information for 37 crest-stage partial-record stations; water quality for 134 gaging stations and for 9 lakes and reservoirs, supplemental water quality for 186 gaged sites; water quality for 29 miscellaneous sites, and 15 observation wells, and meteorological data for 30 sites. Nine pertinent stations operated by bordering States also are included in this report. The records were collected and computed by the Water Resources Division of the U.S. Geological Survey under the direction of D.J. Lystrom, District Chief. These data represent that part of the National Water Data System collected by the U.S. Geological Survey and cooperating State and Federal agencies.","language":"ENGLISH","doi":"10.3133/wdrCO951","usgsCitation":"Crowfoot, R., Ugland, R., Maura, W., Steger, R., and O’Neill, G.B., 1995, Water Resources Data, Colorado, Water Year 1995--Volume 1. Missouri River Basin, Arkansas River Basin, and Rio Grande Basin: U.S. Geological Survey Water Data Report CO-95-1, 506 p.; 5 figs., https://doi.org/10.3133/wdrCO951.","productDescription":"506 p.; 5 figs.","costCenters":[],"links":[{"id":5611,"rank":100,"type":{"id":15,"text":"Index Page"},"url":"https://pubs.water.usgs.gov/wdrCO951","linkFileType":{"id":5,"text":"html"}},{"id":181172,"rank":0,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/thumbnails/usgs_thumb.jpg"}],"noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"4f4e4a0be4b07f02db5fbde1","contributors":{"authors":[{"text":"Crowfoot, R.M.","contributorId":6116,"corporation":false,"usgs":true,"family":"Crowfoot","given":"R.M.","affiliations":[],"preferred":false,"id":249394,"contributorType":{"id":1,"text":"Authors"},"rank":1},{"text":"Ugland, R.C.","contributorId":14044,"corporation":false,"usgs":true,"family":"Ugland","given":"R.C.","email":"","affiliations":[],"preferred":false,"id":249395,"contributorType":{"id":1,"text":"Authors"},"rank":2},{"text":"Maura, W.S.","contributorId":65094,"corporation":false,"usgs":true,"family":"Maura","given":"W.S.","affiliations":[],"preferred":false,"id":249396,"contributorType":{"id":1,"text":"Authors"},"rank":3},{"text":"Steger, R.D.","contributorId":78008,"corporation":false,"usgs":true,"family":"Steger","given":"R.D.","email":"","affiliations":[],"preferred":false,"id":249398,"contributorType":{"id":1,"text":"Authors"},"rank":4},{"text":"O’Neill, G. B.","contributorId":72450,"corporation":false,"usgs":true,"family":"O’Neill","given":"G.","email":"","middleInitial":"B.","affiliations":[],"preferred":false,"id":249397,"contributorType":{"id":1,"text":"Authors"},"rank":5}]}}
,{"id":24122,"text":"ofr95383 - 1995 - Geophysical log data from Basalt Aquifers near Waipahu on the Island of Oahu and Pahoa on the Island of Hawaii, Hawaii","interactions":[],"lastModifiedDate":"2019-12-07T11:25:12","indexId":"ofr95383","displayToPublicDate":"1994-01-01T00:00:00","publicationYear":"1995","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":"95-383","title":"Geophysical log data from Basalt Aquifers near Waipahu on the Island of Oahu and Pahoa on the Island of Hawaii, Hawaii","docAbstract":"Two relatively new geophysical logging techniques, the digitally enhanced borehole acoustic televiewer and the heat-pulse flowmeter, were tested from 1987 to 1991 at two sites in Hawaii: Waipahu on the island of Oahu, and Pahoa on the island of Hawaii. Although these data were obtained in an effort to test and improve these two logging techniques, the measurements are of interest to hydrologists studying the aquifers in Hawaii. This report presents a review of the measurements conducted during this effort and summarizes the data obtained in a form designed to make that data available to hydrologists studying the movement of ground water in Hawaiian aquifers. Caliper logs obtained at the Waipahu site indicate the distribution of openings in interbed clinker zones between relatively dense and impermeable basalt flows. The flowmeter data indicate the pattern of flow induced along seven observation boreholes that provide conduits between interbed zones in the vicinity of the Mahoe Pumping Station at the Waipahu site. The televiewer image logs obtained in some of the Waipahu Mahoe boreholes do not show any significant vertical or steeply dipping fractures that might allow communication across the dense interior of basalt flows. Acoustic televiewer logs obtained at the Pahoa site show that a number of steeply dipping fractures and dikes cut across basalt flows. Although flow under ambient hydraulic-head conditions in the Waipahu Mahoe Observation boreholes is attributed to hydraulic gradients associated with pumping from a nearby pumping station, flow in the Waipio Deep Observation borehole on Oahu and flow in the Scientific Observation borehole on Hawaii are attributed to the effects of natural recharge and downward decreasing hydraulic heads associated with that recharge.","language":"English","publisher":"U.S. Geological Survey ","publisherLocation":"Reston, VA","doi":"10.3133/ofr95383","issn":"0094-9140","usgsCitation":"Paillet, F.L., and Hess, A.E., 1995, Geophysical log data from Basalt Aquifers near Waipahu on the Island of Oahu and Pahoa on the Island of Hawaii, Hawaii: U.S. Geological Survey Open-File Report 95-383, vii, 62 p., https://doi.org/10.3133/ofr95383.","productDescription":"vii, 62 p.","costCenters":[{"id":589,"text":"Toxic Substances Hydrology Program","active":true,"usgs":true},{"id":595,"text":"U.S. Geological Survey","active":false,"usgs":true}],"links":[{"id":156838,"rank":0,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/of/1995/0383/report-thumb.jpg"},{"id":53276,"rank":300,"type":{"id":11,"text":"Document"},"url":"https://pubs.usgs.gov/of/1995/0383/report.pdf","linkFileType":{"id":1,"text":"pdf"}}],"country":"United States","state":"Hawaii","geographicExtents":"{ \"type\": \"FeatureCollection\", \"features\": [ { \"type\": \"Feature\", \"properties\": {}, \"geometry\": { \"type\": \"Polygon\", \"coordinates\": [ [ [ -158.5,21 ], [ -158.5,22 ], [ -157.5,22 ], [ -157.5,21 ], [ -158.5,21 ] ] ] } } ] }","noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"4f4e4b05e4b07f02db69977e","contributors":{"authors":[{"text":"Paillet, Frederick L.","contributorId":38191,"corporation":false,"usgs":true,"family":"Paillet","given":"Frederick","email":"","middleInitial":"L.","affiliations":[],"preferred":false,"id":191355,"contributorType":{"id":1,"text":"Authors"},"rank":1},{"text":"Hess, Alfred E.","contributorId":91900,"corporation":false,"usgs":true,"family":"Hess","given":"Alfred","email":"","middleInitial":"E.","affiliations":[],"preferred":false,"id":191356,"contributorType":{"id":1,"text":"Authors"},"rank":2}]}}
,{"id":54166,"text":"wdrCO952 - 1995 - Water Resources Data, Colorado, Water Year 1995--Volume 2. Colorado River Basin","interactions":[],"lastModifiedDate":"2012-02-02T00:12:07","indexId":"wdrCO952","displayToPublicDate":"1994-01-01T00:00:00","publicationYear":"1995","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":"CO-95-2","title":"Water Resources Data, Colorado, Water Year 1995--Volume 2. Colorado River Basin","docAbstract":"Water-resources data for Colorado for the 1995 water year 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 wells and springs. This report (Volumes 1 and 2) contains discharge records for 335 gaging stations, stage and contents of 26 lakes and reservoirs, 1 partial-record low-flow station, peak-flow information for 37 crest-stage partial-record stations; water quality for 134 gaging stations and for 9 lakes and reservoirs, supplemental water quality for 186 gaged sites; water quality for 29 miscellaneous sites, and 15 observation wells, and meteorological data for 30 sites. Nine pertinent stations operated by bordering States also are included in this report. The records were collected and computed by the Water Resources Division of the U.S. Geological Survey under the direction of D.J. Lystrom, District Chief. These data represent that part of the National Water Data System collected by the U.S. Geological Survey and cooperating State and Federal agencies.","language":"ENGLISH","doi":"10.3133/wdrCO952","usgsCitation":"Crowfoot, R., Ugland, R., Maura, W., Jenkins, R., and O’Neill, G.B., 1995, Water Resources Data, Colorado, Water Year 1995--Volume 2. Colorado River Basin: U.S. Geological Survey Water Data Report CO-95-2, 471 p.; 5 figs., https://doi.org/10.3133/wdrCO952.","productDescription":"471 p.; 5 figs.","costCenters":[],"links":[{"id":5612,"rank":100,"type":{"id":15,"text":"Index Page"},"url":"https://pubs.water.usgs.gov/wdrCO952","linkFileType":{"id":5,"text":"html"}},{"id":181173,"rank":0,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/thumbnails/usgs_thumb.jpg"}],"noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"4f4e4a0be4b07f02db5fbdf9","contributors":{"authors":[{"text":"Crowfoot, R.M.","contributorId":6116,"corporation":false,"usgs":true,"family":"Crowfoot","given":"R.M.","affiliations":[],"preferred":false,"id":249399,"contributorType":{"id":1,"text":"Authors"},"rank":1},{"text":"Ugland, R.C.","contributorId":14044,"corporation":false,"usgs":true,"family":"Ugland","given":"R.C.","email":"","affiliations":[],"preferred":false,"id":249400,"contributorType":{"id":1,"text":"Authors"},"rank":2},{"text":"Maura, W.S.","contributorId":65094,"corporation":false,"usgs":true,"family":"Maura","given":"W.S.","affiliations":[],"preferred":false,"id":249402,"contributorType":{"id":1,"text":"Authors"},"rank":3},{"text":"Jenkins, R.A.","contributorId":48192,"corporation":false,"usgs":true,"family":"Jenkins","given":"R.A.","email":"","affiliations":[],"preferred":false,"id":249401,"contributorType":{"id":1,"text":"Authors"},"rank":4},{"text":"O’Neill, G. B.","contributorId":72450,"corporation":false,"usgs":true,"family":"O’Neill","given":"G.","email":"","middleInitial":"B.","affiliations":[],"preferred":false,"id":249403,"contributorType":{"id":1,"text":"Authors"},"rank":5}]}}
,{"id":54433,"text":"wdrCA942 - 1995 - Water Resources Data, California, Water Year 1994. Volume 2. Pacific Slope Basins from Arroyo Grande to Oregon State Line except Central Valley","interactions":[],"lastModifiedDate":"2012-09-01T01:01:51","indexId":"wdrCA942","displayToPublicDate":"1994-01-01T00:00:00","publicationYear":"1995","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":"CA-94-2","title":"Water Resources Data, California, Water Year 1994. Volume 2. Pacific Slope Basins from Arroyo Grande to Oregon State Line except Central Valley","docAbstract":"Water-resources data for the 1994 water year for California consist of records of stage, discharge, and water quality of streams; stage and contents in lakes and reservoirs; and water levels and water quality in wells. Volume 2 contains discharge records for 113 streamflow-gaging stations, 1 low-flow partial-record streamflow station, and 2 miscellaneous measurement stations; stage and contents for 9 lakes and reservoirs; precipitation records for 3 stations; and water-quality records for 22 streamflow-gaging stations. These data represent that part of the National Water Data System operated by the U.S. Geological Survey and with other agencies.","language":"English","publisher":"U.S. Geological Survey","publisherLocation":"Sacramento, CA","doi":"10.3133/wdrCA942","collaboration":"Prepared in cooperation with the California Department of Water Resources and with other agencies.","usgsCitation":"Ayers, W.Y., 1995, Water Resources Data, California, Water Year 1994. Volume 2. Pacific Slope Basins from Arroyo Grande to Oregon State Line except Central Valley (Legacy Report): U.S. Geological Survey Water Data Report CA-94-2, xviii, 357 p., https://doi.org/10.3133/wdrCA942.","productDescription":"xviii, 357 p.","numberOfPages":"380","costCenters":[{"id":631,"text":"Water Resources Division-California District","active":false,"usgs":true}],"links":[{"id":177260,"rank":0,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/thumbnails/wdr_CA_94_2.jpg"},{"id":260085,"rank":300,"type":{"id":11,"text":"Document"},"url":"https://pubs.usgs.gov/wdr/1994/ca-94/WDR-1994-vol2.pdf","linkFileType":{"id":1,"text":"pdf"}}],"country":"United States","state":"California","otherGeospatial":"Arroyo Grande;Pacific Slope Basins","geographicExtents":"{ \"type\": \"FeatureCollection\", \"features\": [ { \"type\": \"Feature\", \"properties\": {}, \"geometry\": { \"type\": \"Polygon\", \"coordinates\": [ [ [ -124.4,35 ], [ -124.4,42 ], [ -119.83333333333333,42 ], [ -119.83333333333333,35 ], [ -124.4,35 ] ] ] } } ] }","edition":"Legacy Report","noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"4f4e4a0ce4b07f02db5fc28f","contributors":{"authors":[{"text":"Ayers, Wendell Y.","contributorId":87614,"corporation":false,"usgs":true,"family":"Ayers","given":"Wendell","email":"","middleInitial":"Y.","affiliations":[],"preferred":false,"id":250347,"contributorType":{"id":1,"text":"Authors"},"rank":1}]}}
,{"id":54687,"text":"wdrMI941 - 1995 - Water resources data, Michigan, water year 1994","interactions":[],"lastModifiedDate":"2017-09-29T08:57:32","indexId":"wdrMI941","displayToPublicDate":"1994-01-01T00:00:00","publicationYear":"1995","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":"MI-94-1","title":"Water resources data, Michigan, water year 1994","docAbstract":"<p>Water resources data for the 1994 water year for Michigan consists of records of stage, discharge, and water quality of streams; stage and contents of lakes and reservoirs; and ground water levels. This report contains discharge records for 145 streamflow-gaging stations; stage only records for 2 river-gaging stations and 11 lake-gaging stations; stage and contents for 4 lakes and reservoirs; water-quality records for 15 streamflow-gaging stations; water-level records for 44 ground-water wells. Also included are 32 crest-stage partial-record stations and 2 low-flow partial-record stations. Additional water data were collected at various sites not involved in the systematic data-collection program. Miscellaneous data were collected at 50 measuring sites. These data represent that part of the National Water Data System collected by the U.S. Geological Survey and cooperating State, local, and Federal agencies in Michigan.</p>","language":"English","publisher":"U.S. Geological Survey","doi":"10.3133/wdrMI941","collaboration":"Prepared in cooperation with the State of Michigan and with other agencies","usgsCitation":"Blumer, S.P., Behrendt, T., Ellis, J., Minnerick, R., LeuVoy, R., and Whited, C., 1995, Water resources data, Michigan, water year 1994: U.S. Geological Survey Water Data Report MI-94-1, xviii, 282 p., https://doi.org/10.3133/wdrMI941.","productDescription":"xviii, 282 p.","costCenters":[{"id":382,"text":"Michigan Water Science Center","active":true,"usgs":true}],"links":[{"id":346238,"rank":2,"type":{"id":11,"text":"Document"},"url":"https://pubs.usgs.gov/wdr/1994/mi-94-1/report.pdf","linkFileType":{"id":1,"text":"pdf"}},{"id":174039,"rank":0,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/wdr/1994/mi-94-1/report-thumb.jpg"}],"country":"United States","state":"Michigan","geographicExtents":"{\"type\":\"FeatureCollection\",\"features\":[{\"type\":\"Feature\",\"geometry\":{\"type\":\"MultiPolygon\",\"coordinates\":[[[[-85.825955,45.404296],[-85.833516,45.378175],[-85.88301,45.443479],[-85.834891,45.428356],[-85.825955,45.404296]]],[[[-86.093536,45.007838],[-86.133655,44.996874],[-86.154824,45.002394],[-86.156689,45.010535],[-86.141644,45.040251],[-86.117908,45.048478],[-86.079103,45.030795],[-86.100315,45.02624],[-86.093536,45.007838]]],[[[-86.033174,45.15842],[-85.993194,45.152805],[-85.976803,45.138363],[-85.984095,45.087073],[-85.976883,45.06266],[-85.99736,45.055929],[-86.058653,45.100776],[-86.065016,45.140266],[-86.050473,45.158418],[-86.033174,45.15842]]],[[[-88.684434,48.115785],[-88.656915,48.139225],[-88.547033,48.174891],[-88.524753,48.165291],[-88.501088,48.168181],[-88.482039,48.179915],[-88.422601,48.190975],[-88.418244,48.18037],[-88.419875,48.170731],[-88.459697,48.158551],[-88.566938,48.093719],[-88.578053,48.084373],[-88.579784,48.058669],[-88.670073,48.011446],[-88.899184,47.9533],[-88.962664,47.923512],[-88.968903,47.901675],[-88.942387,47.895436],[-88.899698,47.902445],[-88.911665,47.891344],[-89.157738,47.824015],[-89.19017,47.831603],[-89.201812,47.850243],[-89.234533,47.851718],[-89.228507,47.858039],[-89.255202,47.876102],[-89.179154,47.93503],[-88.940886,48.01959],[-88.915032,48.020681],[-88.835714,48.056752],[-88.787556,48.063035],[-88.764256,48.085189],[-88.684434,48.115785]]],[[[-84.612845,45.834528],[-84.650783,45.85921],[-84.646876,45.884642],[-84.622515,45.87753],[-84.578328,45.820092],[-84.432472,45.786732],[-84.421267,45.792694],[-84.42159,45.805651],[-84.403208,45.784394],[-84.35602,45.771895],[-84.372248,45.745784],[-84.405852,45.722417],[-84.484128,45.73071],[-84.612845,45.834528]]],[[[-85.524448,45.829794],[-85.450206,45.796677],[-85.450206,45.776452],[-85.462581,45.765864],[-85.507263,45.778237],[-85.532009,45.798172],[-85.524448,45.829794]]],[[[-85.696872,45.69725],[-85.701809,45.736129],[-85.688849,45.747238],[-85.651866,45.743139],[-85.649353,45.722552],[-85.672187,45.696633],[-85.696872,45.69725]]],[[[-85.360952,45.817554],[-85.351434,45.795663],[-85.359048,45.776627],[-85.377132,45.769013],[-85.394264,45.778531],[-85.377132,45.812795],[-85.360952,45.817554]]],[[[-85.566441,45.760222],[-85.53562,45.750394],[-85.506133,45.754715],[-85.497656,45.746246],[-85.515145,45.749451],[-85.520803,45.737247],[-85.498777,45.726291],[-85.494016,45.698476],[-85.506104,45.681148],[-85.490252,45.652122],[-85.487026,45.621211],[-85.534064,45.578198],[-85.561634,45.572213],[-85.618049,45.582647],[-85.630016,45.598166],[-85.604521,45.639256],[-85.604881,45.681932],[-85.572309,45.711449],[-85.566441,45.760222]]],[[[-86.626187,45.573581],[-86.622023,45.55633],[-86.636895,45.542053],[-86.648792,45.543243],[-86.661284,45.574176],[-86.712328,45.610939],[-86.67727,45.613689],[-86.626187,45.573581]]],[[[-83.880387,41.720089],[-84.806082,41.696089],[-84.805883,41.760216],[-86.823628,41.76024],[-86.717037,41.819349],[-86.619442,41.893827],[-86.582197,41.942241],[-86.485223,42.118239],[-86.356218,42.254166],[-86.297168,42.358207],[-86.261573,42.443894],[-86.226037,42.592811],[-86.22905,42.637693],[-86.206834,42.719424],[-86.210737,42.859128],[-86.232707,43.015762],[-86.280756,43.136015],[-86.407832,43.338436],[-86.479276,43.515335],[-86.529507,43.593462],[-86.540916,43.633158],[-86.529686,43.676849],[-86.463436,43.744687],[-86.43114,43.815569],[-86.462756,43.969655],[-86.508827,44.032755],[-86.514704,44.057672],[-86.421576,44.128962],[-86.362847,44.208113],[-86.343793,44.249608],[-86.26871,44.345324],[-86.248083,44.420946],[-86.248914,44.483004],[-86.220697,44.566742],[-86.22545,44.59459],[-86.259029,44.663654],[-86.256796,44.686769],[-86.232482,44.70605],[-86.09074,44.740544],[-86.074658,44.766792],[-86.065966,44.821522],[-86.072468,44.884788],[-86.066745,44.905685],[-86.038332,44.915696],[-86.021513,44.902774],[-85.992535,44.900026],[-85.9316,44.968788],[-85.897626,44.962014],[-85.869852,44.939031],[-85.807403,44.949814],[-85.780439,44.977932],[-85.771395,45.015181],[-85.746444,45.051229],[-85.695715,45.076461],[-85.656024,45.145788],[-85.618639,45.186771],[-85.606963,45.178477],[-85.585986,45.180381],[-85.551072,45.210742],[-85.540497,45.210169],[-85.526734,45.189316],[-85.531461,45.177247],[-85.564897,45.153962],[-85.599801,45.149286],[-85.614319,45.127562],[-85.583198,45.071304],[-85.566066,45.059201],[-85.56613,45.043633],[-85.597181,45.040547],[-85.599652,45.021749],[-85.621878,45.004529],[-85.602356,44.974272],[-85.602034,44.926743],[-85.621403,44.923123],[-85.645456,44.883645],[-85.652355,44.849092],[-85.637,44.790078],[-85.640781,44.775561],[-85.627982,44.767508],[-85.593833,44.768651],[-85.581717,44.807784],[-85.532931,44.87319],[-85.530729,44.889182],[-85.559524,44.888113],[-85.564509,44.895246],[-85.533553,44.925762],[-85.520034,44.973996],[-85.475204,44.991053],[-85.464944,44.961062],[-85.48574,44.953626],[-85.500872,44.85883],[-85.555894,44.818256],[-85.57517,44.762766],[-85.554774,44.748917],[-85.527216,44.748235],[-85.504775,44.768082],[-85.509251,44.787334],[-85.499591,44.803838],[-85.462943,44.825044],[-85.3958,44.931018],[-85.378286,44.998587],[-85.380659,45.046319],[-85.366412,45.069023],[-85.366908,45.116938],[-85.386726,45.189497],[-85.388593,45.23524],[-85.371593,45.270834],[-85.307646,45.31314],[-85.262996,45.319507],[-85.196704,45.360641],[-85.143651,45.370369],[-85.032813,45.361251],[-84.91585,45.393115],[-84.912956,45.409776],[-84.922006,45.421914],[-84.990041,45.427618],[-84.978373,45.420171],[-85.040272,45.436509],[-85.087756,45.476335],[-85.115479,45.539406],[-85.119026,45.573002],[-85.07491,45.629242],[-85.007026,45.65636],[-84.942636,45.714292],[-84.951745,45.737326],[-85.011433,45.757962],[-85.00741,45.763168],[-84.805114,45.746378],[-84.781995,45.760345],[-84.7798,45.76965],[-84.79229,45.778464],[-84.780313,45.787224],[-84.734065,45.788205],[-84.715996,45.766174],[-84.573631,45.710381],[-84.46168,45.652404],[-84.442348,45.654771],[-84.427495,45.669201],[-84.376403,45.655565],[-84.329537,45.66438],[-84.215268,45.634767],[-84.128867,45.562284],[-84.122309,45.523788],[-84.095905,45.497298],[-84.056138,45.489349],[-84.028813,45.497225],[-83.939261,45.493189],[-83.909472,45.485784],[-83.806622,45.419159],[-83.721815,45.413304],[-83.599273,45.352561],[-83.570361,45.347198],[-83.538306,45.358167],[-83.514717,45.34646],[-83.488826,45.355872],[-83.422486,45.290989],[-83.381743,45.268983],[-83.41241,45.238905],[-83.363678,45.166469],[-83.316118,45.141958],[-83.30788,45.099093],[-83.265896,45.026844],[-83.340257,45.041545],[-83.36747,45.062268],[-83.399255,45.070364],[-83.433798,45.057616],[-83.453363,45.035331],[-83.446342,45.016655],[-83.431254,45.007998],[-83.450013,44.990219],[-83.433032,44.93289],[-83.404596,44.918761],[-83.39396,44.903056],[-83.320503,44.880571],[-83.321241,44.852962],[-83.300648,44.829831],[-83.296265,44.743502],[-83.274674,44.70477],[-83.287802,44.657703],[-83.31445,44.608926],[-83.308471,44.539902],[-83.326824,44.444411],[-83.321553,44.409119],[-83.333757,44.372486],[-83.332533,44.340464],[-83.343738,44.329763],[-83.373607,44.327784],[-83.414301,44.294543],[-83.425762,44.272487],[-83.442731,44.265361],[-83.460958,44.278176],[-83.500392,44.27661],[-83.53771,44.248171],[-83.567744,44.155899],[-83.573071,44.101298],[-83.591361,44.079237],[-83.58409,44.056748],[-83.650116,44.052404],[-83.679654,44.036365],[-83.687892,44.020709],[-83.680108,43.994196],[-83.76283,43.985361],[-83.82808,43.989003],[-83.877047,43.959351],[-83.890912,43.923314],[-83.907388,43.918062],[-83.916815,43.89905],[-83.929375,43.777091],[-83.945426,43.759946],[-83.954792,43.760932],[-83.939297,43.715369],[-83.909479,43.672622],[-83.852076,43.644922],[-83.770693,43.628691],[-83.769886,43.634924],[-83.725793,43.618691],[-83.703446,43.597646],[-83.669795,43.59079],[-83.553707,43.685432],[-83.540187,43.708746],[-83.515853,43.718157],[-83.506657,43.710907],[-83.48007,43.714636],[-83.470053,43.723418],[-83.440171,43.761694],[-83.446752,43.77186],[-83.438311,43.786846],[-83.411453,43.805033],[-83.407647,43.831998],[-83.33227,43.880522],[-83.331788,43.893901],[-83.347365,43.91216],[-83.30569,43.922489],[-83.28231,43.938031],[-83.26185,43.969021],[-83.227093,43.981003],[-83.058741,44.006224],[-83.024604,44.045174],[-82.990728,44.048846],[-82.967439,44.066138],[-82.915976,44.070503],[-82.889831,44.050952],[-82.793205,44.023247],[-82.783198,44.009366],[-82.746255,43.996037],[-82.678642,43.88373],[-82.65545,43.867883],[-82.643166,43.852468],[-82.647784,43.842684],[-82.633641,43.831224],[-82.612224,43.739771],[-82.597911,43.590016],[-82.539517,43.437539],[-82.523086,43.225361],[-82.486684,43.104688],[-82.415937,43.005555],[-82.42455,42.993393],[-82.412965,42.977041],[-82.455027,42.926866],[-82.469912,42.887459],[-82.468961,42.852314],[-82.482045,42.808629],[-82.467483,42.76191],[-82.510533,42.665172],[-82.518782,42.613888],[-82.589779,42.550678],[-82.640916,42.554973],[-82.686417,42.518597],[-82.664335,42.546244],[-82.680758,42.557909],[-82.688061,42.588417],[-82.701152,42.585991],[-82.713042,42.597904],[-82.683482,42.609433],[-82.690124,42.625033],[-82.669103,42.637225],[-82.645715,42.631145],[-82.630922,42.64211],[-82.623043,42.655951],[-82.630851,42.673341],[-82.700964,42.689548],[-82.813518,42.640833],[-82.819017,42.616333],[-82.789017,42.603434],[-82.782414,42.564834],[-82.834216,42.567849],[-82.874416,42.523535],[-82.883915,42.471836],[-82.870572,42.451235],[-82.894013,42.389437],[-82.915114,42.378137],[-82.928815,42.359437],[-82.92397,42.352068],[-83.064121,42.317738],[-83.096521,42.290138],[-83.128022,42.238839],[-83.133923,42.17474],[-83.121323,42.125742],[-83.133511,42.088143],[-83.157624,42.085542],[-83.188598,42.066431],[-83.181475,42.019301],[-83.187246,42.007573],[-83.208647,42.00504],[-83.216835,41.98862],[-83.248741,41.972735],[-83.269521,41.939042],[-83.292761,41.944616],[-83.315859,41.935893],[-83.341557,41.879956],[-83.366187,41.865505],[-83.379705,41.871729],[-83.40822,41.832654],[-83.436298,41.816471],[-83.443364,41.789118],[-83.42418,41.741042],[-83.503433,41.731547],[-83.880387,41.720089]]],[[[-88.116846,45.921703],[-88.189789,45.952208],[-88.209585,45.94428],[-88.239672,45.948982],[-88.249117,45.963663],[-88.292381,45.951115],[-88.316894,45.960969],[-88.326003,45.9553],[-88.334628,45.968808],[-88.380183,45.991654],[-88.414849,45.975483],[-88.458658,45.999391],[-88.492495,45.992157],[-88.509516,46.019169],[-88.565485,46.015708],[-88.589,46.005077],[-88.598093,46.017623],[-88.613063,45.990627],[-88.663697,45.989084],[-88.674606,46.010567],[-88.698716,46.017903],[-88.718397,46.013284],[-88.730675,46.026535],[-88.776187,46.015931],[-88.784411,46.032709],[-88.811948,46.021609],[-88.837991,46.030176],[-89.09163,46.138505],[-90.120489,46.336852],[-90.116844,46.355153],[-90.157851,46.409291],[-90.163422,46.434605],[-90.220532,46.503403],[-90.263018,46.502777],[-90.277131,46.524487],[-90.312581,46.517113],[-90.310329,46.536852],[-90.331887,46.553278],[-90.344338,46.552087],[-90.349462,46.53808],[-90.39332,46.532615],[-90.41562,46.563169],[-90.327626,46.607744],[-90.306609,46.602741],[-90.164026,46.645515],[-90.028392,46.67439],[-89.918466,46.740324],[-89.846962,46.796556],[-89.790663,46.818469],[-89.678469,46.832923],[-89.619329,46.81889],[-89.516895,46.841025],[-89.415154,46.843983],[-89.228362,46.912751],[-89.128698,46.992599],[-89.086742,46.985298],[-89.02893,47.00114],[-88.998907,46.99531],[-88.972802,47.002096],[-88.925586,47.040923],[-88.890708,47.099024],[-88.848176,47.115065],[-88.816684,47.139938],[-88.764351,47.155762],[-88.676624,47.216918],[-88.573997,47.245989],[-88.498756,47.295256],[-88.418841,47.371058],[-88.285635,47.422146],[-88.23944,47.429923],[-88.217822,47.448738],[-88.040291,47.475999],[-87.801184,47.473301],[-87.715942,47.439816],[-87.710471,47.4062],[-87.75138,47.405066],[-87.815371,47.38479],[-87.8567,47.395387],[-87.957058,47.38726],[-87.965598,47.368645],[-87.938787,47.346777],[-87.94336,47.335899],[-88.06009,47.295796],[-88.163059,47.216278],[-88.227552,47.199938],[-88.242109,47.172184],[-88.239487,47.151176],[-88.231797,47.149609],[-88.239895,47.139436],[-88.262537,47.145087],[-88.281652,47.138239],[-88.297547,47.098639],[-88.346501,47.079407],[-88.367624,47.019213],[-88.410157,46.978782],[-88.443901,46.972251],[-88.474217,46.889034],[-88.483748,46.831727],[-88.462349,46.786711],[-88.438427,46.786714],[-88.38141,46.838466],[-88.375577,46.857313],[-88.352145,46.857009],[-88.244437,46.929612],[-88.145561,46.966409],[-88.132957,46.962237],[-88.185964,46.920025],[-88.175197,46.90458],[-88.083937,46.920112],[-88.004298,46.906982],[-87.900695,46.909682],[-87.847037,46.884163],[-87.816794,46.891154],[-87.783216,46.879927],[-87.766243,46.861446],[-87.741857,46.865274],[-87.72588,46.827426],[-87.69459,46.827182],[-87.681561,46.842392],[-87.662261,46.815157],[-87.6333,46.812107],[-87.595307,46.78295],[-87.581674,46.729399],[-87.523308,46.688488],[-87.503238,46.647796],[-87.469023,46.635918],[-87.464108,46.614811],[-87.442612,46.602776],[-87.383961,46.59307],[-87.381649,46.580059],[-87.392974,46.572523],[-87.375613,46.54714],[-87.393985,46.533183],[-87.352448,46.501324],[-87.259116,46.488283],[-87.12744,46.494014],[-87.008724,46.532723],[-86.964534,46.516549],[-86.947077,46.472064],[-86.903742,46.466138],[-86.889094,46.458499],[-86.883919,46.441514],[-86.850111,46.434114],[-86.816026,46.437892],[-86.803557,46.466669],[-86.768516,46.479072],[-86.735929,46.475231],[-86.70323,46.439378],[-86.686412,46.454965],[-86.683819,46.498079],[-86.701929,46.511571],[-86.709325,46.543914],[-86.678182,46.561039],[-86.656479,46.558453],[-86.62738,46.53371],[-86.646393,46.485776],[-86.627441,46.47754],[-86.612173,46.493295],[-86.609039,46.470239],[-86.586168,46.463324],[-86.469306,46.551422],[-86.437167,46.54896],[-86.34989,46.578035],[-86.161681,46.669475],[-86.138295,46.672935],[-86.119862,46.657256],[-86.099843,46.654615],[-85.877908,46.690914],[-85.751345,46.67743],[-85.50951,46.675786],[-85.257999,46.753078],[-85.173042,46.763634],[-85.063556,46.757856],[-84.954009,46.771362],[-85.007616,46.728339],[-85.027513,46.697451],[-85.037056,46.600995],[-85.025491,46.546397],[-85.056133,46.52652],[-85.049847,46.503963],[-85.025598,46.483028],[-84.969464,46.47629],[-84.937145,46.489252],[-84.921931,46.469962],[-84.861448,46.46993],[-84.829491,46.444071],[-84.769151,46.453523],[-84.678423,46.487694],[-84.63102,46.484868],[-84.573522,46.427895],[-84.551496,46.418522],[-84.503719,46.43919],[-84.471848,46.434289],[-84.455527,46.453897],[-84.463322,46.467435],[-84.445149,46.489016],[-84.420274,46.501077],[-84.343599,46.507713],[-84.275814,46.492821],[-84.254434,46.500821],[-84.226131,46.53392],[-84.193729,46.53992],[-84.177428,46.52692],[-84.128925,46.530119],[-84.111225,46.504119],[-84.146172,46.41852],[-84.138906,46.372221],[-84.106247,46.321963],[-84.119629,46.315013],[-84.115563,46.268225],[-84.097766,46.256512],[-84.118175,46.233968],[-84.14595,46.224995],[-84.182732,46.23545],[-84.219494,46.231992],[-84.249164,46.206461],[-84.247687,46.17989],[-84.221001,46.163062],[-84.196669,46.16615],[-84.177298,46.183993],[-84.125022,46.180209],[-84.100126,46.15077],[-84.026536,46.131648],[-84.061329,46.113482],[-84.072398,46.09669],[-84.066257,46.087438],[-83.989526,46.032823],[-83.943933,46.031465],[-83.900535,45.998918],[-83.873147,45.993426],[-83.845399,46.025679],[-83.830146,46.022324],[-83.818202,46.002425],[-83.794055,45.995801],[-83.765277,46.018363],[-83.773785,46.051471],[-83.796555,46.056688],[-83.81252,46.073469],[-83.824036,46.103638],[-83.815826,46.108529],[-83.771821,46.090999],[-83.728165,46.090957],[-83.703861,46.103366],[-83.63498,46.103953],[-83.581315,46.089613],[-83.547202,46.047868],[-83.532913,46.011328],[-83.473946,45.988558],[-83.510623,45.929324],[-83.561838,45.912562],[-83.65766,45.945463],[-83.687695,45.935389],[-83.78611,45.933375],[-83.803332,45.943362],[-83.835505,45.941843],[-83.840869,45.952726],[-83.879616,45.966196],[-83.921257,45.958075],[-83.985141,45.967133],[-84.017565,45.959046],[-84.090391,45.967256],[-84.111174,45.978675],[-84.169368,45.966919],[-84.238174,45.967595],[-84.253993,45.956727],[-84.330346,45.956043],[-84.376429,45.931962],[-84.428239,45.958144],[-84.443086,45.977825],[-84.459956,45.970343],[-84.488536,45.98882],[-84.507201,45.991169],[-84.514071,45.971292],[-84.532392,45.969448],[-84.540995,46.019501],[-84.563891,46.032459],[-84.609063,46.026418],[-84.656567,46.052654],[-84.692735,46.027019],[-84.685254,45.973454],[-84.723039,45.967279],[-84.738849,45.945792],[-84.713614,45.920366],[-84.734002,45.907026],[-84.721277,45.873911],[-84.702122,45.853935],[-84.720609,45.848116],[-84.725734,45.837045],[-84.746985,45.835597],[-84.828996,45.871209],[-84.842147,45.898005],[-84.917288,45.930576],[-84.971232,45.984208],[-85.020951,46.012845],[-85.14516,46.050035],[-85.197523,46.044878],[-85.222416,46.060629],[-85.266385,46.065779],[-85.335466,46.092459],[-85.381263,46.082086],[-85.409463,46.100585],[-85.426916,46.101964],[-85.445835,46.086426],[-85.499422,46.09692],[-85.539479,46.080416],[-85.603785,46.030363],[-85.663966,45.967013],[-85.697203,45.960158],[-85.8092,45.979931],[-85.842404,45.965247],[-85.893196,45.967253],[-85.922737,45.948287],[-85.926017,45.932104],[-85.910264,45.922112],[-85.920581,45.920994],[-85.998868,45.950968],[-86.094753,45.966704],[-86.159415,45.953765],[-86.208255,45.962978],[-86.22906,45.94857],[-86.278007,45.942057],[-86.324232,45.90608],[-86.332625,45.851813],[-86.349134,45.83416],[-86.351658,45.798132],[-86.369918,45.789254],[-86.415971,45.793793],[-86.439661,45.760669],[-86.47905,45.757416],[-86.486028,45.746608],[-86.51457,45.752337],[-86.53328,45.710849],[-86.580936,45.71192],[-86.587528,45.666456],[-86.625132,45.663819],[-86.616893,45.606796],[-86.687208,45.634253],[-86.695275,45.648175],[-86.708038,45.649202],[-86.718191,45.67732],[-86.705184,45.690901],[-86.689102,45.687862],[-86.665677,45.702217],[-86.67148,45.72053],[-86.633138,45.747654],[-86.631018,45.782019],[-86.583391,45.778242],[-86.576858,45.801473],[-86.557215,45.808172],[-86.555186,45.831696],[-86.529208,45.853043],[-86.529573,45.874974],[-86.541464,45.890234],[-86.583304,45.898784],[-86.603293,45.876626],[-86.625736,45.868295],[-86.632478,45.843309],[-86.645998,45.833888],[-86.721113,45.845431],[-86.749638,45.867796],[-86.78208,45.860195],[-86.773279,45.811385],[-86.821523,45.770356],[-86.838658,45.741831],[-86.838746,45.722307],[-86.944158,45.695833],[-86.964275,45.672761],[-86.984588,45.705812],[-86.975224,45.75313],[-86.988438,45.810621],[-87.00508,45.831718],[-87.031435,45.837238],[-87.057439,45.812483],[-87.064302,45.758828],[-87.05555,45.751535],[-87.057444,45.736822],[-87.070442,45.718779],[-87.059953,45.708893],[-87.093365,45.701473],[-87.172241,45.661788],[-87.196852,45.636275],[-87.333407,45.446056],[-87.327749,45.425307],[-87.3925,45.369028],[-87.431684,45.316383],[-87.438908,45.293405],[-87.600796,45.146842],[-87.612019,45.123377],[-87.601086,45.104092],[-87.581969,45.097206],[-87.590208,45.095264],[-87.657135,45.107568],[-87.683902,45.144135],[-87.735135,45.171538],[-87.741805,45.197051],[-87.72796,45.207956],[-87.698248,45.281512],[-87.648126,45.339396],[-87.656624,45.367295],[-87.690281,45.389822],[-87.754104,45.349442],[-87.823028,45.35265],[-87.848368,45.340676],[-87.871204,45.360056],[-87.886949,45.35311],[-87.850969,45.401925],[-87.860432,45.423504],[-87.855298,45.441379],[-87.812976,45.464159],[-87.793447,45.498372],[-87.803364,45.537016],[-87.832296,45.558767],[-87.831689,45.568035],[-87.790874,45.564096],[-87.777671,45.609204],[-87.824676,45.653211],[-87.780808,45.680349],[-87.809075,45.699717],[-87.810144,45.71023],[-87.85548,45.726943],[-87.875813,45.753888],[-87.963452,45.75822],[-87.986429,45.769596],[-87.982617,45.782944],[-87.995876,45.795435],[-88.072091,45.780261],[-88.129461,45.809288],[-88.13611,45.819029],[-88.073134,45.871952],[-88.101814,45.883504],[-88.105677,45.904387],[-88.095354,45.913895],[-88.116846,45.921703]]]]},\"properties\":{\"name\":\"Michigan\",\"nation\":\"USA  \"}}]}\n","noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"4f4e4a0ae4b07f02db5fb6a8","contributors":{"authors":[{"text":"Blumer, S. P.","contributorId":23938,"corporation":false,"usgs":true,"family":"Blumer","given":"S.","email":"","middleInitial":"P.","affiliations":[],"preferred":false,"id":251172,"contributorType":{"id":1,"text":"Authors"},"rank":1},{"text":"Behrendt, T.E.","contributorId":27887,"corporation":false,"usgs":true,"family":"Behrendt","given":"T.E.","email":"","affiliations":[],"preferred":false,"id":251173,"contributorType":{"id":1,"text":"Authors"},"rank":2},{"text":"Ellis, J.M.","contributorId":29502,"corporation":false,"usgs":true,"family":"Ellis","given":"J.M.","email":"","affiliations":[],"preferred":false,"id":251174,"contributorType":{"id":1,"text":"Authors"},"rank":3},{"text":"Minnerick, R. J.","contributorId":52255,"corporation":false,"usgs":true,"family":"Minnerick","given":"R. J.","affiliations":[],"preferred":false,"id":251176,"contributorType":{"id":1,"text":"Authors"},"rank":4},{"text":"LeuVoy, R.L.","contributorId":56706,"corporation":false,"usgs":true,"family":"LeuVoy","given":"R.L.","email":"","affiliations":[],"preferred":false,"id":251177,"contributorType":{"id":1,"text":"Authors"},"rank":5},{"text":"Whited, C.R.","contributorId":49387,"corporation":false,"usgs":true,"family":"Whited","given":"C.R.","email":"","affiliations":[],"preferred":false,"id":251175,"contributorType":{"id":1,"text":"Authors"},"rank":6}]}}
,{"id":54435,"text":"wdrCA944 - 1995 - Water Resources Data, California, Water Year 1994. Volume 4. Northern Central Valley Basins and the Great Basin from Honey Lake Basin to Oregon State Line","interactions":[],"lastModifiedDate":"2012-09-01T01:01:51","indexId":"wdrCA944","displayToPublicDate":"1994-01-01T00:00:00","publicationYear":"1995","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":"CA-94-4","title":"Water Resources Data, California, Water Year 1994. Volume 4. Northern Central Valley Basins and the Great Basin from Honey Lake Basin to Oregon State Line","docAbstract":"Water-resources data for the 1994 water year for California consist of records of stage, discharge, and water quality of streams, stage and contents in lakes and reservoirs, and water levels and water quality in wells. Volume 4 contains discharge records for 187 gaging stations, stage and contents for 47lakes and reservoirs, precipitation data for 3 stations, and water quality for 6 stations. Also included are two low-flow partial-record stations. 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 California.","language":"English","publisher":"U.S. Geological Survey","publisherLocation":"Sacramento, CA","doi":"10.3133/wdrCA944","collaboration":"Prepared in cooperation with the California Department of Water Resources and with other agencies.","usgsCitation":"Friebel, M., Markham, K., Anderson, S., and Rockwell, G., 1995, Water Resources Data, California, Water Year 1994. Volume 4. Northern Central Valley Basins and the Great Basin from Honey Lake Basin to Oregon State Line (Legacy Report): U.S. Geological Survey Water Data Report CA-94-4, xviii, 431 p., https://doi.org/10.3133/wdrCA944.","productDescription":"xviii, 431 p.","numberOfPages":"456","costCenters":[{"id":631,"text":"Water Resources Division-California District","active":false,"usgs":true}],"links":[{"id":177262,"rank":0,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/thumbnails/wdr_CA_94_4.jpg"},{"id":260087,"rank":300,"type":{"id":11,"text":"Document"},"url":"https://pubs.usgs.gov/wdr/1994/ca-94/WDR-1994-vol4.pdf","linkFileType":{"id":1,"text":"pdf"}}],"country":"United States","state":"California","otherGeospatial":"Great Basin;Honey Lake Basin;Northern Central Valley Basins","geographicExtents":"{ \"type\": \"FeatureCollection\", \"features\": [ { \"type\": \"Feature\", \"properties\": {}, \"geometry\": { \"type\": \"Polygon\", \"coordinates\": [ [ [ -123,38 ], [ -123,42 ], [ -120,42 ], [ -120,38 ], [ -123,38 ] ] ] } } ] }","edition":"Legacy Report","noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"4f4e4a0ce4b07f02db5fc2b6","contributors":{"authors":[{"text":"Friebel, M.F.","contributorId":23207,"corporation":false,"usgs":true,"family":"Friebel","given":"M.F.","email":"","affiliations":[],"preferred":false,"id":250352,"contributorType":{"id":1,"text":"Authors"},"rank":1},{"text":"Markham, K.L.","contributorId":14041,"corporation":false,"usgs":true,"family":"Markham","given":"K.L.","email":"","affiliations":[],"preferred":false,"id":250351,"contributorType":{"id":1,"text":"Authors"},"rank":2},{"text":"Anderson, S.W.","contributorId":25628,"corporation":false,"usgs":true,"family":"Anderson","given":"S.W.","email":"","affiliations":[],"preferred":false,"id":250353,"contributorType":{"id":1,"text":"Authors"},"rank":3},{"text":"Rockwell, G.L.","contributorId":47408,"corporation":false,"usgs":true,"family":"Rockwell","given":"G.L.","email":"","affiliations":[],"preferred":false,"id":250354,"contributorType":{"id":1,"text":"Authors"},"rank":4}]}}
,{"id":54649,"text":"wdrMARI941 - 1995 - Water resources data, Massachusetts and Rhode Island, water year 1994","interactions":[],"lastModifiedDate":"2025-09-24T20:59:59.176727","indexId":"wdrMARI941","displayToPublicDate":"1994-01-01T00:00:00","publicationYear":"1995","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":"MA-RI-94-1","title":"Water resources data, Massachusetts and Rhode Island, water year 1994","docAbstract":"<p>Water resources data for the 1994 water year for Massachusetts and Rhode Island consists of records of stage, discharge, and water quality of streams; contents of lakes and reservoirs; and ground-water levels. This report contains discharge records for 83 gaging stations, month end contents of 4 lakes and reservoirs, water quality at 31 gaging stations, and water levels for 136 observation wells. Data also are included for 60 low-flow partial-record stations. Miscellaneous hydrologic data were collected at various sites that were not a part of the systematic data-collection program and are published as miscellaneous discharge measurements and quality of ground water. A few pertinent stations in bordering States are also included in this report. 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 Massachusetts and Rhode Island.</p>","language":"English","publisher":"U.S. Geological Survey","doi":"10.3133/wdrMARI941","collaboration":"Prepared in cooperation with the States of Massachusetts and Rhode Island and with other agencies.","usgsCitation":"Gadoury, R.A., Socolow, R., Girouard, G., and Ramsbey, L., 1995, Water resources data, Massachusetts and Rhode Island, water year 1994: U.S. Geological Survey Water Data Report MA-RI-94-1, xvi, 314 p., https://doi.org/10.3133/wdrMARI941.","productDescription":"xvi, 314 p.","costCenters":[],"links":[{"id":181398,"rank":1,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/wdr/1994/mari-94-1/report-thumb.jpg"},{"id":496060,"rank":2,"type":{"id":11,"text":"Document"},"url":"https://pubs.usgs.gov/wdr/1994/mari-94-1/report.pdf","linkFileType":{"id":1,"text":"pdf"}}],"country":"United States","state":"Massachusetts, Rhode Island","geographicExtents":"{\n  \"type\": \"FeatureCollection\",\n  \"features\": [\n    {\n      \"type\": \"Feature\",\n      \"properties\": {},\n      \"geometry\": {\n        \"coordinates\": [\n          [\n            [\n              -73.50297488831188,\n              42.97016577848564\n            ],\n            [\n              -73.50297488831188,\n              41.11994266161375\n            ],\n            [\n              -69.8918541821574,\n              41.11994266161375\n            ],\n            [\n              -69.8918541821574,\n              42.97016577848564\n            ],\n            [\n              -73.50297488831188,\n              42.97016577848564\n            ]\n          ]\n        ],\n        \"type\": \"Polygon\"\n      }\n    }\n  ]\n}","noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"4f4e4a0ae4b07f02db5fb697","contributors":{"authors":[{"text":"Gadoury, R. A.","contributorId":26334,"corporation":false,"usgs":true,"family":"Gadoury","given":"R.","middleInitial":"A.","affiliations":[],"preferred":false,"id":251031,"contributorType":{"id":1,"text":"Authors"},"rank":1},{"text":"Socolow, R.S.","contributorId":17639,"corporation":false,"usgs":true,"family":"Socolow","given":"R.S.","affiliations":[],"preferred":false,"id":251030,"contributorType":{"id":1,"text":"Authors"},"rank":2},{"text":"Girouard, G.G.","contributorId":88017,"corporation":false,"usgs":true,"family":"Girouard","given":"G.G.","affiliations":[],"preferred":false,"id":251033,"contributorType":{"id":1,"text":"Authors"},"rank":3},{"text":"Ramsbey, L.R.","contributorId":78393,"corporation":false,"usgs":true,"family":"Ramsbey","given":"L.R.","email":"","affiliations":[],"preferred":false,"id":251032,"contributorType":{"id":1,"text":"Authors"},"rank":4}]}}
,{"id":70179105,"text":"70179105 - 1994 - Hydrology of Cache Valley, Cache County, Utah, and adjacent part of Idaho, with emphasis on simulation of ground-water flow","interactions":[],"lastModifiedDate":"2016-12-30T10:03:13","indexId":"70179105","displayToPublicDate":"2016-11-01T00:00:00","publicationYear":"1994","noYear":false,"publicationType":{"id":18,"text":"Report"},"publicationSubtype":{"id":4,"text":"Other Government Series"},"seriesTitle":{"id":294,"text":"Technical Publication","active":false,"publicationSubtype":{"id":4}},"seriesNumber":"108","title":"Hydrology of Cache Valley, Cache County, Utah, and adjacent part of Idaho, with emphasis on simulation of ground-water flow","docAbstract":"<p>A hydrologic investigation of Cache Valley was done to better understand the ground-water system in unconsolidated basin-fill deposits and the interaction between ground water and surface water. Ground-water recharge occurs by infiltration of precipitation and unconsumed irrigation water, seepage from canals and streams, and subsurface inflow from adjacent consolidated rock and adjacent unconsolidated basin-fill deposit ground-water systems. Ground-water discharge occurs as seepage to streams and reservoirs, spring discharge, evapotranspiration, and withdrawal from wells.</p><p>Water levels declined during 1984-90. Less-than-average precipitation during 1987-90 and increased pumping from irrigation and public-supply wells contributed to the declines.</p><p>A ground-water-flow model was used to simulate flow in the unconsolidated basin-fill deposits. Data primarily from 1969 were used to calibrate the model to steady-state conditions. Transient-state calibration was done by simulating ground-water conditions on a yearly basis for 1982-90.</p><p>A hypothetical simulation in which the dry conditions of 1990 were continued for 5 years projected an average lO-foot water-level decline between Richmond and Hyrum. When increased pumpage was simulated by adding three well fields, each pumping 10 cubic feet per second, in the Logan, Smithfield, and College Ward areas, water-level declines greater than 10 feet were projected in most of the southeastern part of the valley and discharge from springs and seepage to streams and reservoirs decreased.<br></p>","language":"English","publisher":"Utah Department of Natural Resources, Division of Water Rights","publisherLocation":"Salt Lake City, UT","collaboration":"Prepared by the United States Geological Survey in cooperation with the Utah Department of Natural Resources Division of Water Resources Division of Water Rights","usgsCitation":"Kariya, K.A., Roark, D.M., and Hanson, K.M., 1994, Hydrology of Cache Valley, Cache County, Utah, and adjacent part of Idaho, with emphasis on simulation of ground-water flow: Technical Publication 108, vi, 120 p.","productDescription":"vi, 120 p.","numberOfPages":"130","costCenters":[{"id":610,"text":"Utah Water Science Center","active":true,"usgs":true}],"links":[{"id":332218,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/thumbnails/outside_thumb.jpg"},{"id":332216,"rank":1,"type":{"id":15,"text":"Index Page"},"url":"https://www.waterrights.utah.gov/cgi-bin/libview.exe?Modinfo=Viewpub&LIBNUM=20-6-570"},{"id":332217,"rank":2,"type":{"id":11,"text":"Document"},"url":"https://waterrights.utah.gov/docSys/v920/y920/y920000e.pdf"}],"country":"United States","state":"Idaho, Utah","county":"Cache County","otherGeospatial":"Cache Valley","geographicExtents":"{\n  \"type\": \"FeatureCollection\",\n  \"features\": [\n    {\n      \"type\": \"Feature\",\n      \"properties\": {},\n      \"geometry\": {\n        \"type\": \"Polygon\",\n        \"coordinates\": [\n          [\n            [\n              -112.1868896484375,\n              41.071069130806414\n            ],\n            [\n              -112.1868896484375,\n              42.54093947168063\n            ],\n            [\n              -111.6650390625,\n              42.54093947168063\n            ],\n            [\n              -111.6650390625,\n              41.071069130806414\n            ],\n            [\n              -112.1868896484375,\n              41.071069130806414\n            ]\n          ]\n        ]\n      }\n    }\n  ]\n}","noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"58550b8ce4b02bdf681568d1","contributors":{"authors":[{"text":"Kariya, Kim A.","contributorId":177522,"corporation":false,"usgs":false,"family":"Kariya","given":"Kim","email":"","middleInitial":"A.","affiliations":[],"preferred":false,"id":656059,"contributorType":{"id":1,"text":"Authors"},"rank":1},{"text":"Roark, D. Michael mroark@usgs.gov","contributorId":127806,"corporation":false,"usgs":true,"family":"Roark","given":"D.","email":"mroark@usgs.gov","middleInitial":"Michael","affiliations":[{"id":472,"text":"New Mexico Water Science Center","active":true,"usgs":true}],"preferred":true,"id":656060,"contributorType":{"id":1,"text":"Authors"},"rank":2},{"text":"Hanson, Karen M. khanson@usgs.gov","contributorId":936,"corporation":false,"usgs":true,"family":"Hanson","given":"Karen","email":"khanson@usgs.gov","middleInitial":"M.","affiliations":[{"id":423,"text":"National Geospatial Program","active":true,"usgs":true}],"preferred":true,"id":656061,"contributorType":{"id":1,"text":"Authors"},"rank":3}]}}
,{"id":70174583,"text":"70174583 - 1994 - San Francisco Bay/delta regional monitoring program plankton and water quality pilot study, 1993, in 1993 Annual Report, San Francisco Estuary Regional Monitoring Program for Trace Substances: San Francisco Estuary Institute","interactions":[],"lastModifiedDate":"2018-09-13T10:43:32","indexId":"70174583","displayToPublicDate":"2016-01-06T09:30:00","publicationYear":"1994","noYear":false,"publicationType":{"id":18,"text":"Report"},"publicationSubtype":{"id":2,"text":"State or Local Government Series"},"title":"San Francisco Bay/delta regional monitoring program plankton and water quality pilot study, 1993, in 1993 Annual Report, San Francisco Estuary Regional Monitoring Program for Trace Substances: San Francisco Estuary Institute","docAbstract":"<p>The pilot program described here is motivated by a fundamental principle of the Regional Monitoring Strategy, namely &ldquo;...the development of data that will provide information on status and trends in the Estuary.&rdquo; As pointed out in the Strategy, knowledge of status and trends serves two primary purposes: (1) to become aware of or anticipate deleterious conditions in the Estuary, and (2) to assess the effectiveness of management actions. This program addresses these two purposes by focusing on aquatic resources, one of the five key management issues identified by the Comprehensive Conservation and Management Plan and central to the Regional Monitoring Strategy. It also bears on at least two of the other management issues - pollutants and water use.</p>\n<p>A regional monitoring program must cover many types of resources, including pelagic and benthic channel habitat, shoal habitat, wetlands, river channels, sloughs, and small bays and harbors. This particular program centers on the pelagic channel habitat. However, because of the intimate connection between channel habitat and many or most of these other habitats, channel measurements reflect to some extent the status of and trends in other resource types as well. A primary aim of this program is to provide a high-resolution description of critical aspects of habitat quality, which can be used along with other information (1) to determine the suitability of habitat for aquatic resources; (2) to monitor responsiveness of the habitat to freshwater flow variability; and (3) to provide a context for understanding pollutant distributions. In a single transect, measurements are made throughout the water column at up to 37 stations to define physical (salinity, temperature, suspended particulate matter, and light penetration), chemical (dissolved oxygen) and biological (chlorophyll <i>a</i>) characteristics that influence both chemical and biological reactions.</p>\n<p>A second aim of the program is to investigate planktonic indicators of ecosystem structure and function. Phytoplankton <i>production </i>is the major single source of energy for the San Francisco Bay food web. Our measurements of chlorophyll and light penetration can be used to provide an estimate of this production, and therefore the availability of food for organisms at higher trophic levels. Phytoplankton <i>community composition</i> at the species level, which can be a sensitive indicator of habitat change, is also a standard component of this program. Community composition data enable detection of species known to be responsible for harmful or nuisance algal blooms. In 1993, two other indicators were also evaluated, <i>photosynthetic parameters </i>and <i>water column respiration</i>. Photosynthetic parameters partially characterize the physiological state of the phytoplankton and may provide indirect evidence of nutrient deficiency or the effects of pollutants. Water column respiration serves as a simple integrated measure of organic matter metabolism by the plankton, including bacteria, phytoplankton, and microzooplankton. It therefore reflects the total supply of organic matter, whether from photosynthesis, tidal marsh efflux, point sources, or upstream in the Delta. These biological indicators therefore contain much information about the flow of energy into the food web.</p>","largerWorkType":{"id":18,"text":"Report"},"largerWorkTitle":"San Francisco Estuary Regional Monitoring Program for trace substances: 1993 annual report","largerWorkSubtype":{"id":2,"text":"State or Local Government Series"},"language":"English","publisher":"San Francisco Estuary Regional Monitoring Institute","publisherLocation":"San Francisco, CA","usgsCitation":"Jassby, A.D., Cloern, J.E., Caffrey, J., Cole, B., and Rudek, J., 1994, San Francisco Bay/delta regional monitoring program plankton and water quality pilot study, 1993, in 1993 Annual Report, San Francisco Estuary Regional Monitoring Program for Trace Substances: San Francisco Estuary Institute, 12 p.","productDescription":"12 p.","startPage":"117","endPage":"128","onlineOnly":"N","additionalOnlineFiles":"N","temporalStart":"1993-03-01","costCenters":[{"id":552,"text":"San Francisco Bay-Delta","active":false,"usgs":true},{"id":589,"text":"Toxic Substances Hydrology Program","active":true,"usgs":true}],"links":[{"id":325189,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/thumbnails/outside_thumb.jpg"},{"id":325188,"rank":1,"type":{"id":11,"text":"Document"},"url":"https://www.sfei.org/sites/default/files/biblio_files/1993_RMP_Annual_Report.pdf","text":"1993 Annual Report : San Francisco Estuary Regional Monitoring Program for Trace Substances","size":"2.7 MB","linkFileType":{"id":1,"text":"pdf"},"description":"1993 Annual Report : San Francisco Estuary Regional Monitoring Program for Trace Substances"}],"country":"United States","state":"California","county":"San Francisco","city":"San Francisco","otherGeospatial":"San Francisco Bay","geographicExtents":"{\n  \"type\": \"FeatureCollection\",\n  \"features\": [\n    {\n      \"type\": \"Feature\",\n      \"properties\": {},\n      \"geometry\": {\n        \"type\": \"Polygon\",\n        \"coordinates\": [\n          [\n            [\n              -123.03314208984374,\n              37.14499280340638\n            ],\n            [\n              -123.03314208984374,\n              38.30933576918588\n            ],\n            [\n              -121.2506103515625,\n              38.30933576918588\n            ],\n            [\n              -121.2506103515625,\n              37.14499280340638\n            ],\n            [\n              -123.03314208984374,\n              37.14499280340638\n            ]\n          ]\n        ]\n      }\n    }\n  ]\n}","noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"57876631e4b0d27deb36e1aa","contributors":{"authors":[{"text":"Jassby, Alan D.","contributorId":66403,"corporation":false,"usgs":true,"family":"Jassby","given":"Alan","email":"","middleInitial":"D.","affiliations":[],"preferred":false,"id":642371,"contributorType":{"id":1,"text":"Authors"},"rank":1},{"text":"Cloern, James E. 0000-0002-5880-6862 jecloern@usgs.gov","orcid":"https://orcid.org/0000-0002-5880-6862","contributorId":1488,"corporation":false,"usgs":true,"family":"Cloern","given":"James","email":"jecloern@usgs.gov","middleInitial":"E.","affiliations":[{"id":438,"text":"National Research Program - Western Branch","active":true,"usgs":true},{"id":37277,"text":"WMA - Earth System Processes Division","active":true,"usgs":true}],"preferred":true,"id":642372,"contributorType":{"id":1,"text":"Authors"},"rank":2},{"text":"Caffrey, J.","contributorId":147320,"corporation":false,"usgs":false,"family":"Caffrey","given":"J.","email":"","affiliations":[],"preferred":false,"id":642373,"contributorType":{"id":1,"text":"Authors"},"rank":3},{"text":"Cole, B.","contributorId":36744,"corporation":false,"usgs":true,"family":"Cole","given":"B.","email":"","affiliations":[],"preferred":false,"id":642374,"contributorType":{"id":1,"text":"Authors"},"rank":4},{"text":"Rudek, J.","contributorId":67904,"corporation":false,"usgs":true,"family":"Rudek","given":"J.","email":"","affiliations":[],"preferred":false,"id":642375,"contributorType":{"id":1,"text":"Authors"},"rank":5}]}}
]}