{"pageNumber":"1884","pageRowStart":"47075","pageSize":"25","recordCount":68927,"records":[{"id":27099,"text":"wri884087 - 1988 - Preimpoundment hydrologic conditions in the Swatara Creek (1981-84) and estimated postimpoundment water quality in and downstream from the planned Swatara State Park Reservoir, Lebanon and Schuylkill counties, Pennsylvania","interactions":[],"lastModifiedDate":"2021-09-10T18:34:56.459331","indexId":"wri884087","displayToPublicDate":"1994-01-01T00:00:00","publicationYear":"1988","noYear":false,"publicationType":{"id":18,"text":"Report"},"publicationSubtype":{"id":5,"text":"USGS Numbered Series"},"seriesTitle":{"id":342,"text":"Water-Resources Investigations Report","code":"WRI","active":false,"publicationSubtype":{"id":5}},"seriesNumber":"88-4087","title":"Preimpoundment hydrologic conditions in the Swatara Creek (1981-84) and estimated postimpoundment water quality in and downstream from the planned Swatara State Park Reservoir, Lebanon and Schuylkill counties, Pennsylvania","docAbstract":"The hydrology and water quality of Swatara Creek were studied by the U.S. Geological Survey in cooperation with the Pennsylvania Department of Environmental Resources, Bureau of State Parks, from July 1981 through September 1984. The purpose of the study was to determine the effects of anthracite-coal mining and other point and nonpoint sources on the water quality of a planned 10,500 acre-foot reservoir. The Swatara State Park Reservoir is planned to be used for recreation and drinking-water supply for the city of Lebanon and surrounding communities.\r\n\r\n Annual precipitation during 1982, 1983, and 1984 was about 8 percent below, near normal, and 29 percent above the long-term average, respectively. The average annual precipitation during a year with near-normal precipitation, the 1983 water year, was 47 inches at Pine Grove. Mean streamflows during 1982, 1983, and 1984 were about 15 percent below, 4 percent above, and 50 percent above the long-term average, respectively. The average streamflow to the planned reservoir area during the 1983 water year was about 220 cubic feet per second.\r\n\r\n Inflows to, and downstream discharge from, the planned reservoir wer poorly buffered. Median alkalinity ranged from 4 to 7 mg/L (milligrams per liter) and median acidity ranged from 2 to 5 mg/L at the three sampling locations. Maximum total-recoverable iron, aluminum, and manganese concentrations were 100,000, 66,000, and 2,300 micrograms per liter, respectively. During 1983 the annual discharges of total-recoverable iron, aluminum, and manganese to the planned reservoir area were estimated to be 692, 300, and 95 tons, respectively. About 87 percent of the total-recoverable iron and 91 percent of total-recoverable sluminum measured was in the suspended phase. The data indicated that mine drainage affects the quality of Swatara Creek and will affect the quality of the planned reservoir.\r\n\r\n In addition to mine drainage, point-source nutrient and metal discharges will probably affect the planned reservoir. For example, in September 1983, Swatara Creek was sampled downstream from a point source. A dissolved- phosphorus concentration of 14 mg/L and total ammonia plus organic nitrogen concentration of 8.2 mg/L were measured. At the same location, concentrations of total-recoverable aluminum, chromium, copper, iron, and lead were 35, 300, 110, 1,300, and 32 micrograms per liter, respectively.\r\n\r\n Inflows to the planned Swatara State Park Reservoir are estimated to be acidic and rich in nutrients and select metals. Unless an effort is made to improve the quality of water from point and nonpoint sources, these conditions may impair the planned uses for the reservoir. Conservation releases from the reservoir need to be carefully controlled or these conditions also may degrade the water quality downstream.","language":"English","publisher":"U.S. Geological Survey","doi":"10.3133/wri884087","usgsCitation":"Fishel, D.K., 1988, Preimpoundment hydrologic conditions in the Swatara Creek (1981-84) and estimated postimpoundment water quality in and downstream from the planned Swatara State Park Reservoir, Lebanon and Schuylkill counties, Pennsylvania: U.S. Geological Survey Water-Resources Investigations Report 88-4087, Report: vi, 108 p.; 2 Plates: 16.57 × 10.53 inches and 16.40 × 7.99 inches, https://doi.org/10.3133/wri884087.","productDescription":"Report: vi, 108 p.; 2 Plates: 16.57 × 10.53 inches and 16.40 × 7.99 inches","costCenters":[{"id":532,"text":"Pennsylvania Water Science Center","active":true,"usgs":true}],"links":[{"id":158966,"rank":0,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/wri/1988/4087/report-thumb.jpg"},{"id":55964,"rank":300,"type":{"id":11,"text":"Document"},"url":"https://pubs.usgs.gov/wri/1988/4087/report.pdf","linkFileType":{"id":1,"text":"pdf"}},{"id":55963,"rank":401,"type":{"id":17,"text":"Plate"},"url":"https://pubs.usgs.gov/wri/1988/4087/plate-2.pdf","linkFileType":{"id":1,"text":"pdf"}},{"id":55962,"rank":400,"type":{"id":17,"text":"Plate"},"url":"https://pubs.usgs.gov/wri/1988/4087/plate-1.pdf","linkFileType":{"id":1,"text":"pdf"}},{"id":389084,"rank":5,"type":{"id":36,"text":"NGMDB Index Page"},"url":"https://ngmdb.usgs.gov/Prodesc/proddesc_47007.htm"}],"country":"United States","state":"Pennsylvania","otherGeospatial":"Swatara Creek","geographicExtents":"{\n \"type\": \"FeatureCollection\",\n \"features\": [\n {\n \"type\": \"Feature\",\n \"properties\": {},\n \"geometry\": {\n \"type\": \"Polygon\",\n \"coordinates\": [\n [\n [\n -76.6375,\n 40.4569\n ],\n [\n -76.21,\n 40.4569\n ],\n [\n -76.21,\n 40.66\n ],\n [\n -76.6375,\n 40.66\n ],\n [\n -76.6375,\n 40.4569\n ]\n ]\n ]\n }\n }\n ]\n}","noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"4f4e4acce4b07f02db67e77d","contributors":{"authors":[{"text":"Fishel, D. K.","contributorId":72028,"corporation":false,"usgs":true,"family":"Fishel","given":"D.","email":"","middleInitial":"K.","affiliations":[],"preferred":false,"id":197550,"contributorType":{"id":1,"text":"Authors"},"rank":1}]}} ,{"id":25386,"text":"wri854127 - 1988 - Alternative sources of large seasonal ground-water supplies in the headwaters of the Susquehanna River basin, New York","interactions":[],"lastModifiedDate":"2012-02-02T00:08:29","indexId":"wri854127","displayToPublicDate":"1994-01-01T00:00:00","publicationYear":"1988","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":"85-4127","title":"Alternative sources of large seasonal ground-water supplies in the headwaters of the Susquehanna River basin, New York","docAbstract":"The northern divide of the Susquehanna River basin crosses 29 broad valleys that contain thick glacial deposits but are drained only by small headwater streams. Much groundwater could be withdrawn from sand and gravel deposits in these valleys with little immediate effect on streamflow. A digital model of the headwater reach of one typical valley suggests that pumping 10.8 million gal/day for 2 months every summer would lower the water table as much as 33 ft, cause the upper 1,900 ft of the stream draining the valley to go dry, and reduce streamflow downvalley by 1.2 million gal/day by the time pumping ceased. Saturated thickness of surficial sand and gravel exceeds 40 ft in about half the headwater valley reaches; the valley floor areas range from 0.2 to 9 sq mi. Seepage losses from small streams that carry runoff from adjacent till-covered uplands are a major source of recharge to aquifers in these valleys under natural conditions and would increase if the water table were lowered by seasonal withdrawals. Some aquifers beneath extensive clay layers in these and other valleys of the Susquehanna River basin may be partially independent of streams but not easily evaluated. (USGS)","language":"ENGLISH","publisher":"U.S. Geological Survey,","doi":"10.3133/wri854127","usgsCitation":"Randall, A., Snavely, D.S., Holecek, T., and Waller, R., 1988, Alternative sources of large seasonal ground-water supplies in the headwaters of the Susquehanna River basin, New York: U.S. Geological Survey Water-Resources Investigations Report 85-4127, v, 121 p. :ill., maps ;28 cm., https://doi.org/10.3133/wri854127.","productDescription":"v, 121 p. :ill., maps ;28 cm.","costCenters":[],"links":[{"id":122814,"rank":0,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/wri/1985/4127/report-thumb.jpg"},{"id":54120,"rank":300,"type":{"id":11,"text":"Document"},"url":"https://pubs.usgs.gov/wri/1985/4127/report.pdf","linkFileType":{"id":1,"text":"pdf"}}],"noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"4f4e4adde4b07f02db686aed","contributors":{"authors":[{"text":"Randall, A. D.","contributorId":81077,"corporation":false,"usgs":true,"family":"Randall","given":"A. D.","affiliations":[],"preferred":false,"id":193479,"contributorType":{"id":1,"text":"Authors"},"rank":1},{"text":"Snavely, D. S.","contributorId":103692,"corporation":false,"usgs":true,"family":"Snavely","given":"D.","email":"","middleInitial":"S.","affiliations":[],"preferred":false,"id":193480,"contributorType":{"id":1,"text":"Authors"},"rank":2},{"text":"Holecek, T.P.","contributorId":76358,"corporation":false,"usgs":true,"family":"Holecek","given":"T.P.","email":"","affiliations":[],"preferred":false,"id":193478,"contributorType":{"id":1,"text":"Authors"},"rank":3},{"text":"Waller, R.M.","contributorId":13659,"corporation":false,"usgs":true,"family":"Waller","given":"R.M.","email":"","affiliations":[],"preferred":false,"id":193477,"contributorType":{"id":1,"text":"Authors"},"rank":4}]}} ,{"id":26372,"text":"wri884000 - 1988 - Simulation of five ground-water withdrawal projections for the Black Mesa area, Navajo and Hopi Indian Reservations, Arizona","interactions":[],"lastModifiedDate":"2012-02-02T00:08:32","indexId":"wri884000","displayToPublicDate":"1994-01-01T00:00:00","publicationYear":"1988","noYear":false,"publicationType":{"id":18,"text":"Report"},"publicationSubtype":{"id":5,"text":"USGS Numbered Series"},"seriesTitle":{"id":342,"text":"Water-Resources Investigations Report","code":"WRI","active":false,"publicationSubtype":{"id":5}},"seriesNumber":"88-4000","title":"Simulation of five ground-water withdrawal projections for the Black Mesa area, Navajo and Hopi Indian Reservations, Arizona","docAbstract":"The N Aquifer is the main source of water in the 5,400 sq mi Black Mesa area in the Navajo and Hopi Indian Reservations in northeastern Arizona. Water in the aquifer is under confined conditions in the central 3,300 sq mi of the area. Maximum saturated thickness is about 1,050 ft. Annual groundwater withdrawals from 1972 through 1986 averaged 5,480 acre-ft and included 3,820 acre-ft used to operate a coal mine on Black Mesa. As a result, water levels have declined in a large part of the aquifer. The coal company has applied for a permanent permit under the Surface Mining Control and Reclamation Act of 1977. An existing mathematical model of the aquifer in the Black Mesa area was converted to a newer model program and recalibrated by using revised estimates of selected aquifer parameters and a finer spatial grid. The model was used to simulate four groundwater withdrawal alternatives that combined the existing and proposed mining plans with projected constant or increasing pumpage for nearby communities. A fifth alternative combined increasing community pumpage with no mine withdrawals and was used as a basis for comparison. Simulated water levels for the year 2031 in the coal-lease area are projected to be 60 ft lower than in 1985 for the proposed mining plan combined with growing community pumpage and > 100 ft lower than predevelopment water levels over an area of 1,660 sq mi. Groundwater would rise to within 100 ft of predevelopment levels < 10 yr after mine withdrawals cease. Withdrawals at the mine were a minor factor in determining simulated water levels at most communities in the study area. Water levels at Tuba City were not affected by mine pumpage in any projection. (Author 's abstract)","language":"ENGLISH","publisher":"U.S. Geological Survey,","doi":"10.3133/wri884000","usgsCitation":"Brown, J.G., and Eychaner, J., 1988, Simulation of five ground-water withdrawal projections for the Black Mesa area, Navajo and Hopi Indian Reservations, Arizona: U.S. Geological Survey Water-Resources Investigations Report 88-4000, v, 51 p. :ill., maps ;28 cm., https://doi.org/10.3133/wri884000.","productDescription":"v, 51 p. :ill., maps ;28 cm.","costCenters":[],"links":[{"id":158085,"rank":0,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/wri/1988/4000/report-thumb.jpg"},{"id":55166,"rank":300,"type":{"id":11,"text":"Document"},"url":"https://pubs.usgs.gov/wri/1988/4000/report.pdf","linkFileType":{"id":1,"text":"pdf"}}],"noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"4f4e4a7ee4b07f02db64857d","contributors":{"authors":[{"text":"Brown, J. G.","contributorId":28263,"corporation":false,"usgs":true,"family":"Brown","given":"J.","email":"","middleInitial":"G.","affiliations":[],"preferred":false,"id":196274,"contributorType":{"id":1,"text":"Authors"},"rank":1},{"text":"Eychaner, J.H.","contributorId":34511,"corporation":false,"usgs":true,"family":"Eychaner","given":"J.H.","affiliations":[],"preferred":false,"id":196275,"contributorType":{"id":1,"text":"Authors"},"rank":2}]}} ,{"id":27106,"text":"wri874034 - 1988 - Hydrogeology, aquifer characteristics, and ground-water flow of the surficial aquifer system, Broward County, Florida","interactions":[],"lastModifiedDate":"2022-01-10T12:39:00.489015","indexId":"wri874034","displayToPublicDate":"1994-01-01T00:00:00","publicationYear":"1988","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":"87-4034","title":"Hydrogeology, aquifer characteristics, and ground-water flow of the surficial aquifer system, Broward County, Florida","docAbstract":"The surficial aquifer system, in which an unconfined groundwater flow system exists, comprises the sediments from land surface to the intermediate confining unit (formerly called the Floridan aquiclude) in Broward County, Florida. These sediments have hydraulic conductivities that range more than seven orders of magnitude from about 0.001 ft/d to more than 10,000 ft/d. The sediments are grouped into (1) the Biscayne aquifer, (2) a semiconfining unit, (3) a gray limestone aquifer in west Broward County, and (4) basal sand or clayey sand. The system is about 160 ft thick in west Broward County and more than 350 ft thick in east Broward. Transmissivities, locally variable, show a clear areal trend from greater than 300,000 sq ft/day in southeast Broward County to less than 75,000 sq ft/day in the northwest part of the county. Very high transmissivity is associated with the Biscayne aquifer. Transmissivity of the gray limestone aquifer ranged from about 20,000 to 88,000 sq ft/day. Topography, water levels, geologic framework, and water quality in west Broward County suggest past and present groundwater movement is south or southeast. Drainage and urban development have greatly altered circulation patterns in east Broward County , eliminating the original coastal groundwater ridge, causing rapid surface runoff and short groundwater flow paths, and saltwater intrusion. (USGS)","language":"English","publisher":"U.S. Geological Survey","doi":"10.3133/wri874034","collaboration":"Prepared in cooperation with the South Florida Water Management District","usgsCitation":"Fish, J., 1988, Hydrogeology, aquifer characteristics, and ground-water flow of the surficial aquifer system, Broward County, Florida: U.S. Geological Survey Water-Resources Investigations Report 87-4034, vi, 92 p., https://doi.org/10.3133/wri874034.","productDescription":"vi, 92 p.","costCenters":[{"id":27821,"text":"Caribbean-Florida Water Science 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","noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"4f4e4a2de4b07f02db6148c9","contributors":{"authors":[{"text":"Fish, J.E.","contributorId":101658,"corporation":false,"usgs":true,"family":"Fish","given":"J.E.","email":"","affiliations":[],"preferred":false,"id":197561,"contributorType":{"id":1,"text":"Authors"},"rank":1}]}} ,{"id":26324,"text":"wri884070 - 1988 - Tolerances of plants to drought and salinity in the western United States","interactions":[],"lastModifiedDate":"2012-02-02T00:08:25","indexId":"wri884070","displayToPublicDate":"1994-01-01T00:00:00","publicationYear":"1988","noYear":false,"publicationType":{"id":18,"text":"Report"},"publicationSubtype":{"id":5,"text":"USGS Numbered Series"},"seriesTitle":{"id":342,"text":"Water-Resources Investigations Report","code":"WRI","active":false,"publicationSubtype":{"id":5}},"seriesNumber":"88-4070","title":"Tolerances of plants to drought and salinity in the western United States","docAbstract":"Differing capacities of plant species to tolerate drought and salinity are causative factors for presence of species and communities in various habitats. It is proposed that minimum xylem pressure potentials measured are indicative of drought tolerance and that minimum cell osmotic potentials are indicative of salt tolerance of plant species. Of 85 species measured, Nuttall saltbush (Atriplex nuttallii nuttallii) was found to be the most drought tolerant. Saltbrush (Atriplex confertifolia, A. nuttallii, A. canescens, and A. torreyi) had the lowest cell osmotic potentials measured. Although pickleweed (Allenrolfea occidentalis) grows in the saltiest soil measured, it did not have the lowest cell osmotic potential. This apparent inconsistency may be explained by the succulent characteristics of pickleweed. (USGS)","language":"ENGLISH","publisher":"U.S. Geological Survey,","doi":"10.3133/wri884070","usgsCitation":"Branson, F.A., Miller, R.F., and Sorenson, S.K., 1988, Tolerances of plants to drought and salinity in the western United States: U.S. Geological Survey Water-Resources Investigations Report 88-4070, iv, 16 p. :ill., maps ;28 cm., https://doi.org/10.3133/wri884070.","productDescription":"iv, 16 p. :ill., maps ;28 cm.","costCenters":[],"links":[{"id":157660,"rank":0,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/wri/1988/4070/report-thumb.jpg"},{"id":55114,"rank":300,"type":{"id":11,"text":"Document"},"url":"https://pubs.usgs.gov/wri/1988/4070/report.pdf","linkFileType":{"id":1,"text":"pdf"}}],"noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"4f4e4a53e4b07f02db62b398","contributors":{"authors":[{"text":"Branson, Farrel Allen","contributorId":53823,"corporation":false,"usgs":true,"family":"Branson","given":"Farrel","email":"","middleInitial":"Allen","affiliations":[],"preferred":false,"id":196181,"contributorType":{"id":1,"text":"Authors"},"rank":1},{"text":"Miller, Reuben Fred","contributorId":75967,"corporation":false,"usgs":true,"family":"Miller","given":"Reuben","email":"","middleInitial":"Fred","affiliations":[],"preferred":false,"id":196182,"contributorType":{"id":1,"text":"Authors"},"rank":2},{"text":"Sorenson, Stephen K.","contributorId":90314,"corporation":false,"usgs":true,"family":"Sorenson","given":"Stephen","email":"","middleInitial":"K.","affiliations":[],"preferred":false,"id":196183,"contributorType":{"id":1,"text":"Authors"},"rank":3}]}} ,{"id":11979,"text":"ofr87682 - 1988 - Climatic data for Mirror Lake, West Thornton, New Hampshire: 1985","interactions":[],"lastModifiedDate":"2020-05-12T15:55:45.000535","indexId":"ofr87682","displayToPublicDate":"1994-01-01T00:00:00","publicationYear":"1988","noYear":false,"publicationType":{"id":18,"text":"Report"},"publicationSubtype":{"id":5,"text":"USGS Numbered Series"},"seriesTitle":{"id":330,"text":"Open-File Report","code":"OFR","onlineIssn":"2331-1258","printIssn":"0196-1497","active":true,"publicationSubtype":{"id":5}},"seriesNumber":"87-682","title":"Climatic data for Mirror Lake, West Thornton, New Hampshire: 1985","docAbstract":"Research on the hydrology of Mirror Lake, West Thornton, New Hampshire, includes a study of evaporation. Those climatic data needed for energy-budget and mass-transfer evaporation studies are presented, including: water surface temperature, dry-bulb and wet-bulb air temperatures, vapor pressure at and above the water surface, wind speed, and short- and long-wave radiation. Data are collected at raft and land stations. (USGS)","language":"English","publisher":"U.S. Geological Survey","publisherLocation":"Reston, VA","doi":"10.3133/ofr87682","usgsCitation":"Sturrock, A.M., Buso, D., Scarborough, J., and Winter, T.C., 1988, Climatic data for Mirror Lake, West Thornton, New Hampshire: 1985: U.S. Geological Survey Open-File Report 87-682, iii, 64 leaves , https://doi.org/10.3133/ofr87682.","productDescription":"iii, 64 leaves ","costCenters":[],"links":[{"id":374663,"rank":2,"type":{"id":11,"text":"Document"},"url":"https://pubs.usgs.gov/of/1987/0682/report.pdf","linkFileType":{"id":1,"text":"pdf"}},{"id":143761,"rank":0,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/of/1987/0682/report-thumb.jpg"}],"country":"United States","state":"New Hampshire","city":"West Thorton","otherGeospatial":"Mirror Lake","geographicExtents":"{\n \"type\": \"FeatureCollection\",\n \"features\": [\n {\n \"type\": \"Feature\",\n \"properties\": {},\n \"geometry\": {\n \"type\": \"Polygon\",\n \"coordinates\": [\n [\n [\n -71.69540405273438,\n 43.94141717295212\n ],\n [\n -71.68913841247559,\n 43.94141717295212\n ],\n [\n -71.68913841247559,\n 43.94648475051101\n ],\n [\n -71.69540405273438,\n 43.94648475051101\n ],\n [\n -71.69540405273438,\n 43.94141717295212\n ]\n ]\n ]\n }\n }\n ]\n}","noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"4f4e48cfe4b07f02db545eef","contributors":{"authors":[{"text":"Sturrock, Alex M.","contributorId":48948,"corporation":false,"usgs":true,"family":"Sturrock","given":"Alex","email":"","middleInitial":"M.","affiliations":[],"preferred":false,"id":164502,"contributorType":{"id":1,"text":"Authors"},"rank":1},{"text":"Buso, D.C.","contributorId":31392,"corporation":false,"usgs":true,"family":"Buso","given":"D.C.","email":"","affiliations":[],"preferred":false,"id":164501,"contributorType":{"id":1,"text":"Authors"},"rank":2},{"text":"Scarborough, J.L.","contributorId":94673,"corporation":false,"usgs":true,"family":"Scarborough","given":"J.L.","email":"","affiliations":[],"preferred":false,"id":164503,"contributorType":{"id":1,"text":"Authors"},"rank":3},{"text":"Winter, T. C.","contributorId":23485,"corporation":false,"usgs":true,"family":"Winter","given":"T.","email":"","middleInitial":"C.","affiliations":[],"preferred":false,"id":164500,"contributorType":{"id":1,"text":"Authors"},"rank":4}]}} ,{"id":20982,"text":"ofr88112 - 1988 - The national water-use information program-ground-water perspective","interactions":[],"lastModifiedDate":"2012-02-02T00:07:55","indexId":"ofr88112","displayToPublicDate":"1994-01-01T00:00:00","publicationYear":"1988","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":"88-112","title":"The national water-use information program-ground-water perspective","language":"ENGLISH","publisher":"U.S. Geological Survey,","doi":"10.3133/ofr88112","usgsCitation":"Solley, W., 1988, The national water-use information program-ground-water perspective: U.S. Geological Survey Open-File Report 88-112, 2 p. :ill. ;28 cm., https://doi.org/10.3133/ofr88112.","productDescription":"2 p. :ill. ;28 cm.","costCenters":[],"links":[{"id":154351,"rank":0,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/of/1988/0112/report-thumb.jpg"},{"id":50562,"rank":300,"type":{"id":11,"text":"Document"},"url":"https://pubs.usgs.gov/of/1988/0112/report.pdf","linkFileType":{"id":1,"text":"pdf"}}],"noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"4f4e4a80e4b07f02db64998a","contributors":{"authors":[{"text":"Solley, W.B.","contributorId":25960,"corporation":false,"usgs":true,"family":"Solley","given":"W.B.","affiliations":[],"preferred":false,"id":183617,"contributorType":{"id":1,"text":"Authors"},"rank":1}]}} ,{"id":55571,"text":"wdrLA871 - 1988 - Water resources data, Louisiana, water year 1987","interactions":[],"lastModifiedDate":"2025-05-22T19:58:35.535689","indexId":"wdrLA871","displayToPublicDate":"1994-01-01T00:00:00","publicationYear":"1988","noYear":false,"publicationType":{"id":18,"text":"Report"},"publicationSubtype":{"id":5,"text":"USGS Numbered Series"},"seriesTitle":{"id":340,"text":"Water Data Report","code":"WDR","active":false,"publicationSubtype":{"id":5}},"seriesNumber":"LA-87-1","title":"Water resources data, Louisiana, water year 1987","docAbstract":"

Water resources data for the 1987 water year for Louisiana consist of records of stage, discharge, and water quality of streams; stage, contents, and water quality of lakes and reservoirs; and water levels and water quality of ground water. This report contains records for water discharge at 63 gaging stations; stage only for 19 gaging stations and 7 lakes; water quality for 48 surface-water stations (including 19 gaging stations), 6 lakes, and 77 wells; and water levels for 346 observation wells. Also included are data for 103 crest-stage and flood-profile partial-record stations. Additional water data were collected at various sites not involved in the systematic data-collection program, and are published as miscellaneous measurements. These data represent that part of the National Water Data System operated by the U.S. Geological Survey and cooperating State and Federal agencies in Louisiana.

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No abstract available. 

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B.","contributorId":11161,"corporation":false,"usgs":true,"family":"Campbell","given":"J.","email":"","middleInitial":"B.","affiliations":[],"preferred":false,"id":254978,"contributorType":{"id":1,"text":"Authors"},"rank":1},{"text":"Coon, W.F.","contributorId":102524,"corporation":false,"usgs":true,"family":"Coon","given":"W.F.","email":"","affiliations":[],"preferred":false,"id":254981,"contributorType":{"id":1,"text":"Authors"},"rank":2},{"text":"Sherwood, D. A.","contributorId":65824,"corporation":false,"usgs":true,"family":"Sherwood","given":"D.","email":"","middleInitial":"A.","affiliations":[],"preferred":false,"id":254979,"contributorType":{"id":1,"text":"Authors"},"rank":3},{"text":"Deloff, D.D.","contributorId":72855,"corporation":false,"usgs":true,"family":"Deloff","given":"D.D.","email":"","affiliations":[],"preferred":false,"id":254980,"contributorType":{"id":1,"text":"Authors"},"rank":4}]}} ,{"id":21283,"text":"ofr88143 - 1988 - U.S. Geological Survey ground-water studies in Illinois","interactions":[],"lastModifiedDate":"2012-02-02T00:07:58","indexId":"ofr88143","displayToPublicDate":"1994-01-01T00:00:00","publicationYear":"1988","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":"88-143","title":"U.S. Geological Survey ground-water studies in Illinois","language":"ENGLISH","publisher":"U.S. Geological Survey,","doi":"10.3133/ofr88143","usgsCitation":"Voelker, D.C., Nicholas, J., and Norton, K., 1988, U.S. Geological Survey ground-water studies in Illinois: U.S. Geological Survey Open-File Report 88-143, 2 p.:ill. ;28 cm., https://doi.org/10.3133/ofr88143.","productDescription":"2 p.:ill. ;28 cm.","costCenters":[],"links":[{"id":155181,"rank":0,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/of/1988/0143/report-thumb.jpg"},{"id":50834,"rank":300,"type":{"id":11,"text":"Document"},"url":"https://pubs.usgs.gov/of/1988/0143/report.pdf","linkFileType":{"id":1,"text":"pdf"}}],"noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"4f4e4a2ae4b07f02db6129c8","contributors":{"authors":[{"text":"Voelker, D. C.","contributorId":36572,"corporation":false,"usgs":true,"family":"Voelker","given":"D.","email":"","middleInitial":"C.","affiliations":[],"preferred":false,"id":184139,"contributorType":{"id":1,"text":"Authors"},"rank":1},{"text":"Nicholas, J.R.","contributorId":26673,"corporation":false,"usgs":true,"family":"Nicholas","given":"J.R.","email":"","affiliations":[],"preferred":false,"id":184138,"contributorType":{"id":1,"text":"Authors"},"rank":2},{"text":"Norton, K.L.","contributorId":41027,"corporation":false,"usgs":true,"family":"Norton","given":"K.L.","email":"","affiliations":[],"preferred":false,"id":184140,"contributorType":{"id":1,"text":"Authors"},"rank":3}]}} ,{"id":44630,"text":"wri884061 - 1988 - Map of bedrock-surface topography in parts of the Paterson and Pompton Plains quadrangles, New Jersey","interactions":[],"lastModifiedDate":"2012-02-02T00:11:01","indexId":"wri884061","displayToPublicDate":"1994-01-01T00:00:00","publicationYear":"1988","noYear":false,"publicationType":{"id":18,"text":"Report"},"publicationSubtype":{"id":5,"text":"USGS Numbered Series"},"seriesTitle":{"id":342,"text":"Water-Resources Investigations Report","code":"WRI","active":false,"publicationSubtype":{"id":5}},"seriesNumber":"88-4061","title":"Map of bedrock-surface topography in parts of the Paterson and Pompton Plains quadrangles, New Jersey","docAbstract":"A seismic-refraction survey was done by the U.S. Geological Survey, in cooperation with the U.S. Army Corps of Engineers (ACOE), to define the altitudes of the bedrock surface beneath part of a proposed water diversion tunnel to control periodic heavy flooding along parts of the Passaic and Pompton Rivers in northeastern New Jersey. The altitude of the top of the tunnel is planned to be approximately at sea level. The ACOE would like to have a minimum of 40 ft of bedrock above the top of the tunnel for construction and engineering purposes. The results of the study show that the bedrock ranges in altitude from 40 to 140 ft above sea level, and that there is a northeast trending bedrock valley that overlies the proposed tunnel alignment. (USGS)","language":"ENGLISH","doi":"10.3133/wri884061","usgsCitation":"Lacombe, P., and Duran, P., 1988, Map of bedrock-surface topography in parts of the Paterson and Pompton Plains quadrangles, New Jersey: U.S. Geological Survey Water-Resources Investigations Report 88-4061, 1 map ; 20 x 29 cm., on sheet 94 x 63 cm., folded in envelope 30 x 24 cm., https://doi.org/10.3133/wri884061.","productDescription":"1 map ; 20 x 29 cm., on sheet 94 x 63 cm., folded in envelope 30 x 24 cm.","costCenters":[],"links":[{"id":168912,"rank":0,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/thumbnails/usgs_thumb.jpg"},{"id":81959,"rank":400,"type":{"id":17,"text":"Plate"},"url":"https://pubs.usgs.gov/wri/1988/4061/plate-1.pdf","linkFileType":{"id":1,"text":"pdf"}}],"noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"4f4e4a91e4b07f02db656cf6","contributors":{"authors":[{"text":"Lacombe, Pierre J. placombe@usgs.gov","contributorId":2486,"corporation":false,"usgs":true,"family":"Lacombe","given":"Pierre J.","email":"placombe@usgs.gov","affiliations":[{"id":532,"text":"Pennsylvania Water Science Center","active":true,"usgs":true}],"preferred":false,"id":230145,"contributorType":{"id":1,"text":"Authors"},"rank":1},{"text":"Duran, Philip B.","contributorId":56699,"corporation":false,"usgs":true,"family":"Duran","given":"Philip B.","affiliations":[],"preferred":false,"id":230146,"contributorType":{"id":1,"text":"Authors"},"rank":2}]}} ,{"id":21454,"text":"ofr88149 - 1988 - U.S. Geological Survey ground-water studies in Pennsylvania","interactions":[],"lastModifiedDate":"2017-06-06T14:24:04","indexId":"ofr88149","displayToPublicDate":"1994-01-01T00:00:00","publicationYear":"1988","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":"88-149","title":"U.S. Geological Survey ground-water studies in Pennsylvania","docAbstract":"

In Pennsylvania, large water demands generally are met from surface-water sources; small water demands generally are met from ground-water sources. Ground-water sources supply 6 percent of the total water used in Pennsylvania. Of the ground water used in 1984,55 percent was for industry, 23 percent for public supply, 15 percent for rural domestic supplies, 5 percent for livestock, and 2 percent for irrigation. Public supplies provide ground water to about 2,180,000 people, and rural self-supplied systems provide ground water to about 3,000,000 people.  The major issues related to ground water in Pennsylvania are: Adequacy of supplies, Contamination by hazardous wastes, and Effects of coal mining, oil and gas production, and agriculture.

","language":"English","publisher":"U.S. Geological Survey","doi":"10.3133/ofr88149","usgsCitation":"Wood, C.R., 1988, U.S. Geological Survey ground-water studies in Pennsylvania: U.S. Geological Survey Open-File Report 88-149, 2 p. :map ;28 cm., https://doi.org/10.3133/ofr88149.","productDescription":"2 p. :map ;28 cm.","costCenters":[{"id":532,"text":"Pennsylvania Water Science Center","active":true,"usgs":true}],"links":[{"id":154000,"rank":0,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/of/1988/0149/report-thumb.jpg"},{"id":51018,"rank":300,"type":{"id":11,"text":"Document"},"url":"https://pubs.usgs.gov/of/1988/0149/report.pdf","linkFileType":{"id":1,"text":"pdf"}}],"country":"United 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\"}}]}","noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"4f4e4a2ae4b07f02db612768","contributors":{"authors":[{"text":"Wood, C. R.","contributorId":100386,"corporation":false,"usgs":true,"family":"Wood","given":"C.","email":"","middleInitial":"R.","affiliations":[],"preferred":false,"id":184456,"contributorType":{"id":1,"text":"Authors"},"rank":1}]}} ,{"id":45719,"text":"pp1311 - 1988 - The Manti, Utah, landslide","interactions":[],"lastModifiedDate":"2022-05-06T21:59:19.692644","indexId":"pp1311","displayToPublicDate":"1994-01-01T00:00:00","publicationYear":"1988","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":"1311","title":"The Manti, Utah, landslide","docAbstract":"PART A: The Manti landslide is in Manti Canyon on the west side of the Wasatch Plateau in central Utah. In early June 1974, coincident with the melting of a snowpack, a rock slump/debris flow occurred on the south rim of Manti Canyon. Part of the slumped material mixed with meltwater and mobilized into a series of debris flows that traveled down the slope a distance of as much as 1.2 km. Most of the flows were deposited either at the base of the steep rocks of the canyon rim or at the site of an old, silted reservoir. A small part of the debris flow deposit stopped on the head of the very large, relatively inactive Manti landslide. The upper part of the landslide began moving as cracks propagated downslope. A little more than a year later, August 1975, movement extended the full length of the old landslide, and about 19 million m 3 of debris about 3 km long and as much as 800 m wide threatened to block the canyon. \r\n\r\nThe upper part of the landslide apparently had moved small amounts between 1939 and 1974. This part of the landslide, identifiable on pre-1974 aerial photographs, consisted of well-defined linears on the landslide flanks and two large internal toe bulges about 2 km downslope from the head. \r\n\r\nThe abrupt reactivation in 1974 proceeded quickly after the debris flows had provided a surcharge in the head and crown area. Movement propagated downslope at 4-5 m/h for the first few days following reactivation. During 1974, the reactivation probably encompassed all the parts of the landslide that had moved small amounts between 1939 and 1974. Movement nearly or completely stopped during the winter of 1974-75, but began again in the spring of 1975. The landslide enlarged from the flanks of the internal toe bulges to Manti Creek at a rate of 2-3 m/h. Movement stopped again during the winter of 1975-76 and began again in the spring of 1976. Thereafter, the displacements have been small compared to earlier. \r\n\r\nThe displacement rates for the landslide were variable depending on where and when they were measured. At the waterline crossing, about 500 m downslope from the head, the maximum rate was about 1 mid, and the peak rate occurred within the first 30 days following reactivation. Almost a year later, during the spring of 1975, the rates there were 0.1-0.3 mid. By the time movement had propagated 2.5 km downslope to Manti Creek, more than 40 m of displacement had occurred at the waterline. \r\n\r\nCracks were first noted at Manti Creek on June 21,1975, but movement was initially very slow there. The maximum rate of sliding of about 3.1 mid occurred during the period September 1-19,1975, and the movement decreased and stopped during the winter of 1975-76. At the time the lower part of the landslide was moving rapidly, the rate farther upslope was small. The result was that the landslide changed from being in compression, which was caused by loading from above, to being in extension, which was caused by the lower part moving faster than the upper part. One of the results of the extension was that the landslide pulled apart on a steeper segment of the slope and exposed the failure surface. Since the fall of 1975, the landslide has been separated into two independent parts. There has been no movement in the lower part, whereas movements in the upper part have continued at a rate of a few meters per year. \r\n\r\nAlthough the landslide is 6.5 km from the nearest permanent dwelling, it cost nearly $2 million in actual damages and in preparation for a major disaster that did not occur. The waterline for the city of Manti was replaced and a well was drilled to provide an emergency water supply.\r\n\r\nPART B: The Manti landslide abuts, at its toe, another large landslide called the North slide. In 1975, public officials were concerned that continued movement of the Manti landslide would trigger reactivation of the North slide. In response to this threat, four borings were placed in the North slide to obtain samples for testing and information","language":"English","publisher":"U.S. Geological Survey","doi":"10.3133/pp1311","usgsCitation":"Fleming, R.W., Johnson, R.B., Schuster, R.L., and Williams, G.P., 1988, The Manti, Utah, landslide: U.S. Geological Survey Professional Paper 1311, Report: x, 69 p.; 1 Plate: 34.00 × 28.50 inches, https://doi.org/10.3133/pp1311.","productDescription":"Report: x, 69 p.; 1 Plate: 34.00 × 28.50 inches","costCenters":[],"links":[{"id":82301,"rank":400,"type":{"id":17,"text":"Plate"},"url":"https://pubs.usgs.gov/pp/1311/plate-1.pdf","linkFileType":{"id":1,"text":"pdf"}},{"id":82302,"rank":300,"type":{"id":11,"text":"Document"},"url":"https://pubs.usgs.gov/pp/1311/report.pdf","linkFileType":{"id":1,"text":"pdf"}},{"id":400321,"rank":4,"type":{"id":36,"text":"NGMDB Index Page"},"url":"https://ngmdb.usgs.gov/Prodesc/proddesc_74240.htm"},{"id":120560,"rank":0,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/pp/1311/report-thumb.jpg"}],"country":"United States","state":"Utah","city":"Manti","geographicExtents":"{\n \"type\": \"FeatureCollection\",\n \"features\": [\n {\n \"type\": \"Feature\",\n \"properties\": {},\n \"geometry\": {\n \"type\": \"Polygon\",\n \"coordinates\": [\n [\n [\n -111.75,\n 39.1\n ],\n [\n -111.5,\n 39.1\n ],\n [\n -111.5,\n 39.29073420338177\n ],\n [\n -111.75,\n 39.29073420338177\n ],\n [\n -111.75,\n 39.1\n ]\n ]\n ]\n }\n }\n ]\n}","noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"4f4e4ac8e4b07f02db67b9c5","contributors":{"authors":[{"text":"Fleming, R. W.","contributorId":89110,"corporation":false,"usgs":true,"family":"Fleming","given":"R.","email":"","middleInitial":"W.","affiliations":[],"preferred":false,"id":231915,"contributorType":{"id":1,"text":"Authors"},"rank":1},{"text":"Johnson, R. B.","contributorId":64218,"corporation":false,"usgs":true,"family":"Johnson","given":"R.","email":"","middleInitial":"B.","affiliations":[],"preferred":false,"id":231914,"contributorType":{"id":1,"text":"Authors"},"rank":2},{"text":"Schuster, R. L.","contributorId":19135,"corporation":false,"usgs":true,"family":"Schuster","given":"R.","email":"","middleInitial":"L.","affiliations":[],"preferred":false,"id":231913,"contributorType":{"id":1,"text":"Authors"},"rank":3},{"text":"Williams, G. P.","contributorId":97472,"corporation":false,"usgs":true,"family":"Williams","given":"G.","email":"","middleInitial":"P.","affiliations":[],"preferred":false,"id":231916,"contributorType":{"id":1,"text":"Authors"},"rank":4}]}} ,{"id":21513,"text":"ofr88311 - 1988 - Streamflow and water-quality data for three major tributaries to Reelfoot Lake, west Tennessee, October 1987-March 1988","interactions":[],"lastModifiedDate":"2012-02-02T00:07:44","indexId":"ofr88311","displayToPublicDate":"1994-01-01T00:00:00","publicationYear":"1988","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":"88-311","title":"Streamflow and water-quality data for three major tributaries to Reelfoot Lake, west Tennessee, October 1987-March 1988","docAbstract":"Streamflow and water quality data were collected for three major tributaries to Reelfoot Lake, in West Tennessee, for the period October 1987 through March 1988. The data are presented in graphs and tables. Mean daily discharge data were collected at one site each in the drainage basins of North Reelfoot Creek, South Reelfoot Creek, and Running Slough. Daily mean suspended-sediment concentration data were collected at a site in the North Reelfoot Creek basin. Water quality samples were collected during storm events at the same locations that daily mean streamflow data were collected. Water quality samples were analyzed for concentrations of nutrients and triazine herbicides. Water temperature and specific conductance were measured at the time that samples were collected. (USGS)","language":"ENGLISH","publisher":"U.S. Geological Survey,","doi":"10.3133/ofr88311","usgsCitation":"Yurewicz, M., Carey, W.P., and Garrett, J., 1988, Streamflow and water-quality data for three major tributaries to Reelfoot Lake, west Tennessee, October 1987-March 1988: U.S. Geological Survey Open-File Report 88-311, iii, 20 p. :ill., map ;28 cm., https://doi.org/10.3133/ofr88311.","productDescription":"iii, 20 p. :ill., map ;28 cm.","costCenters":[],"links":[{"id":153087,"rank":0,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/thumbnails/usgs_thumb.jpg"},{"id":1216,"rank":100,"type":{"id":15,"text":"Index Page"},"url":"https://pubs.water.usgs.gov/ofr_88-311","linkFileType":{"id":5,"text":"html"}}],"noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"4f4e4b15e4b07f02db6a4e72","contributors":{"authors":[{"text":"Yurewicz, M.C.","contributorId":40237,"corporation":false,"usgs":true,"family":"Yurewicz","given":"M.C.","email":"","affiliations":[],"preferred":false,"id":184572,"contributorType":{"id":1,"text":"Authors"},"rank":1},{"text":"Carey, W. P.","contributorId":105749,"corporation":false,"usgs":true,"family":"Carey","given":"W.","email":"","middleInitial":"P.","affiliations":[],"preferred":false,"id":184574,"contributorType":{"id":1,"text":"Authors"},"rank":2},{"text":"Garrett, J.W.","contributorId":87958,"corporation":false,"usgs":true,"family":"Garrett","given":"J.W.","email":"","affiliations":[],"preferred":false,"id":184573,"contributorType":{"id":1,"text":"Authors"},"rank":3}]}} ,{"id":20573,"text":"ofr88145 - 1988 - U.S. Geological Survey ground-water studies in Tennessee","interactions":[],"lastModifiedDate":"2012-02-02T00:07:43","indexId":"ofr88145","displayToPublicDate":"1994-01-01T00:00:00","publicationYear":"1988","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":"88-145","title":"U.S. Geological Survey ground-water studies in Tennessee","language":"ENGLISH","publisher":"U.S. Geological Survey,","doi":"10.3133/ofr88145","usgsCitation":"Quinones, F., 1988, U.S. Geological Survey ground-water studies in Tennessee: U.S. Geological Survey Open-File Report 88-145, 2 p. :ill. ;28 cm., https://doi.org/10.3133/ofr88145.","productDescription":"2 p. :ill. ;28 cm.","costCenters":[],"links":[{"id":152918,"rank":0,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/of/1988/0145/report-thumb.jpg"},{"id":50094,"rank":300,"type":{"id":11,"text":"Document"},"url":"https://pubs.usgs.gov/of/1988/0145/report.pdf","linkFileType":{"id":1,"text":"pdf"}}],"noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"4f4e4a2ae4b07f02db612729","contributors":{"authors":[{"text":"Quinones, Ferdinand","contributorId":44138,"corporation":false,"usgs":true,"family":"Quinones","given":"Ferdinand","email":"","affiliations":[],"preferred":false,"id":182872,"contributorType":{"id":1,"text":"Authors"},"rank":1}]}} ,{"id":55126,"text":"wdrWY871 - 1988 - Water resources data, Wyoming, water year 1987","interactions":[],"lastModifiedDate":"2025-08-19T13:28:17.520867","indexId":"wdrWY871","displayToPublicDate":"1994-01-01T00:00:00","publicationYear":"1988","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":"WY-87-1","title":"Water resources data, Wyoming, water year 1987","docAbstract":"

Water resources data for the 1987 water year for Wyoming consists of records of stage, discharge and water quality of streams; stage and contents of lakes and reservoirs; and water levels and water quality of ground water. This report contains discharge records for 172 gaging stations; stage and contents for 16 lakes and reservoirs; water quality for 67 gaging stations, and 52 ungaged stations; and water levels for 5 observation wells. Additional water data were collected at various sites, not part of the systematic data collection program, and are published as miscellaneous measurements. These data represent that part of the National Water Data System operated by the U.S. Geological Survey and cooperating State and Federal agencies in Wyoming.

","language":"English","publisher":"U.S. Geological Survey","doi":"10.3133/wdrWY871","usgsCitation":"Druse, S.A., Glass, W.R., McCollum, P.B., and Peterson, D.A., 1988, Water resources data, Wyoming, water year 1987: U.S. Geological Survey Water Data Report WY-87-1, ix, 396 p., https://doi.org/10.3133/wdrWY871.","productDescription":"ix, 396 p.","costCenters":[],"links":[{"id":174026,"rank":1,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/wdr/1987/wy-87-1/report-thumb.jpg"},{"id":494265,"rank":2,"type":{"id":11,"text":"Document"},"url":"https://pubs.usgs.gov/wdr/1987/wy-87-1/report.pdf","linkFileType":{"id":1,"text":"pdf"}}],"country":"United 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U.S. Geological Survey National Water-Quality Assessment program","docAbstract":"Beginning in 1986, the Congress appropriated funds for the U.S. Geological Survey to test and refine concepts for a National Water Quality Assessment Program. At present, the program is in a pilot phase with field studies occurring in seven areas around the Nation. In 1990, a committee of the National Academy of Sciences will complete an evaluation of the design and potential utility of the program. A decision about moving to full-scale implementation will be made upon completion of this evaluation. The program is intended to address a wide range of national water quality issues that include chemical contamination, acidification, eutrophication, salinity, sedimentation, and sanitary quality. The goals of the program are to: (1) provide nationally consistent descriptions of current water quality conditions for a large part of the Nation 's water resources; (2) define long-term trends (or lack of trends) in water quality; and (3) identify and describe the relations of both current conditions and trends in water quality to natural and human factors. This information will be provided to water managers, policy makers, and the public to provide an improved scientific basis for evaluating the effectiveness of water quality management programs and for predicting the likely effects of contemplated changes in land- and water-management practices. (USGS)","language":"ENGLISH","publisher":"U.S. Geological Survey,","doi":"10.3133/ofr8895","usgsCitation":"Hirsch, R., Alley, W., and Wilber, W.G., 1988, A summary of the U.S. Geological Survey National Water-Quality Assessment program: U.S. Geological Survey Open-File Report 88-95, 7 p. ;28 cm., https://doi.org/10.3133/ofr8895.","productDescription":"7 p. ;28 cm.","costCenters":[],"links":[{"id":146050,"rank":0,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/of/1988/0095/report-thumb.jpg"},{"id":42761,"rank":300,"type":{"id":11,"text":"Document"},"url":"https://pubs.usgs.gov/of/1988/0095/report.pdf","linkFileType":{"id":1,"text":"pdf"}}],"noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"4f4e4b17e4b07f02db6a6056","contributors":{"authors":[{"text":"Hirsch, R.M.","contributorId":58639,"corporation":false,"usgs":true,"family":"Hirsch","given":"R.M.","email":"","affiliations":[],"preferred":false,"id":168966,"contributorType":{"id":1,"text":"Authors"},"rank":1},{"text":"Alley, W.M.","contributorId":6853,"corporation":false,"usgs":true,"family":"Alley","given":"W.M.","email":"","affiliations":[],"preferred":false,"id":168965,"contributorType":{"id":1,"text":"Authors"},"rank":2},{"text":"Wilber, W. G.","contributorId":98337,"corporation":false,"usgs":true,"family":"Wilber","given":"W.","email":"","middleInitial":"G.","affiliations":[],"preferred":false,"id":168967,"contributorType":{"id":1,"text":"Authors"},"rank":3}]}} ,{"id":19479,"text":"ofr88704 - 1988 - Ground-water data for Michigan 1987","interactions":[],"lastModifiedDate":"2012-02-02T00:07:29","indexId":"ofr88704","displayToPublicDate":"1994-01-01T00:00:00","publicationYear":"1988","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":"88-704","title":"Ground-water data for Michigan 1987","language":"ENGLISH","publisher":"U.S. Geological Survey,","doi":"10.3133/ofr88704","usgsCitation":"Huffman, G., and Whited, C., 1988, Ground-water data for Michigan 1987: U.S. Geological Survey Open-File Report 88-704, v, 56 p. :ill., maps ;28 cm., https://doi.org/10.3133/ofr88704.","productDescription":"v, 56 p. :ill., maps ;28 cm.","costCenters":[],"links":[{"id":151859,"rank":0,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/of/1988/0704/report-thumb.jpg"},{"id":48949,"rank":300,"type":{"id":11,"text":"Document"},"url":"https://pubs.usgs.gov/of/1988/0704/report.pdf","linkFileType":{"id":1,"text":"pdf"}}],"noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"4f4e4aafe4b07f02db66cf80","contributors":{"authors":[{"text":"Huffman, G.C.","contributorId":44150,"corporation":false,"usgs":true,"family":"Huffman","given":"G.C.","email":"","affiliations":[],"preferred":false,"id":180980,"contributorType":{"id":1,"text":"Authors"},"rank":1},{"text":"Whited, C.R.","contributorId":49387,"corporation":false,"usgs":true,"family":"Whited","given":"C.R.","email":"","affiliations":[],"preferred":false,"id":180981,"contributorType":{"id":1,"text":"Authors"},"rank":2}]}} ,{"id":27357,"text":"wri864083 - 1988 - Procedures for determining drainage areas using a digitizer, digital computer, and topographic maps","interactions":[],"lastModifiedDate":"2012-02-02T00:08:41","indexId":"wri864083","displayToPublicDate":"1994-01-01T00:00:00","publicationYear":"1988","noYear":false,"publicationType":{"id":18,"text":"Report"},"publicationSubtype":{"id":5,"text":"USGS Numbered Series"},"seriesTitle":{"id":342,"text":"Water-Resources Investigations Report","code":"WRI","active":false,"publicationSubtype":{"id":5}},"seriesNumber":"86-4083","title":"Procedures for determining drainage areas using a digitizer, digital computer, and topographic maps","language":"ENGLISH","publisher":"U.S. Geological Survey,","doi":"10.3133/wri864083","usgsCitation":"Gold, R., and Winkless, D., 1988, Procedures for determining drainage areas using a digitizer, digital computer, and topographic maps: U.S. Geological Survey Water-Resources Investigations Report 86-4083, iv, 33 p. :ill., map ;28 cm., https://doi.org/10.3133/wri864083.","productDescription":"iv, 33 p. :ill., map ;28 cm.","costCenters":[],"links":[{"id":158730,"rank":0,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/wri/1986/4083/report-thumb.jpg"},{"id":56217,"rank":300,"type":{"id":11,"text":"Document"},"url":"https://pubs.usgs.gov/wri/1986/4083/report.pdf","linkFileType":{"id":1,"text":"pdf"}}],"noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"4f4e4a9ee4b07f02db66099b","contributors":{"authors":[{"text":"Gold, R.L.","contributorId":97918,"corporation":false,"usgs":true,"family":"Gold","given":"R.L.","email":"","affiliations":[],"preferred":false,"id":197975,"contributorType":{"id":1,"text":"Authors"},"rank":1},{"text":"Winkless, Dan","contributorId":11254,"corporation":false,"usgs":true,"family":"Winkless","given":"Dan","email":"","affiliations":[],"preferred":false,"id":197974,"contributorType":{"id":1,"text":"Authors"},"rank":2}]}} ,{"id":27854,"text":"wri874253 - 1988 - Water quality of the Lexington Reservoir, Santa Clara County, California, 1978-80","interactions":[],"lastModifiedDate":"2012-02-02T00:08:35","indexId":"wri874253","displayToPublicDate":"1994-01-01T00:00:00","publicationYear":"1988","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":"87-4253","title":"Water quality of the Lexington Reservoir, Santa Clara County, California, 1978-80","docAbstract":"Analysis of water samples from Lexington Reservoir and Los Gatos Creek upstream from the reservoir from June 1978 through September 1980 showed that water generally met water-quality objectives identified by California Regional Water Quality Control Board, San Francisco Bay Region. Water-temperature profiles show that Lexington Reservoir is a warm monomictic lake. During summer, dissolved-oxygen concentrations generally were not reduced below 5.0 mg/L in the hyplimnion; only once during the study did bottom waters become anoxic. Water transparency decreased with depth. The euphotic zone ranged from 1.0 to 5.4 m, depending on suspended solids and algae, and was greater in summer than in spring. Calcium and bicarbonate were dominant ions at all stations except during spring, following the rainy season, when waters were a mixed cation bicarbonate type. Nitrogen concentrations were greater in samples from reservoir stations than in those from Los Gatos Creek, with most of the nitrogen in ammonia and organic forms. The amount of dissolved nitrate appeared to be related to phytoplankton abundance. Phosphorus and trace-element concentrations were low at all stations. Estimates of net primary productivity and Carlson 's trophic-state index, based on chlorophyll-a concentrations, indicated that reservoir classification ranges from oligotrophic to mesotrophic. Blue-green algae generally were predominant in reservoir samples. (USGS)","language":"ENGLISH","publisher":"U.S. Geological Survey,","doi":"10.3133/wri874253","usgsCitation":"Iwatsubo, R., Sylvester, M.A., and Gloege, I., 1988, Water quality of the Lexington Reservoir, Santa Clara County, California, 1978-80: U.S. Geological Survey Water-Resources Investigations Report 87-4253, vi, 64 p. :ill., maps ;28 cm., https://doi.org/10.3133/wri874253.","productDescription":"vi, 64 p. :ill., maps ;28 cm.","costCenters":[],"links":[{"id":158615,"rank":0,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/wri/1987/4253/report-thumb.jpg"},{"id":56674,"rank":300,"type":{"id":11,"text":"Document"},"url":"https://pubs.usgs.gov/wri/1987/4253/report.pdf","linkFileType":{"id":1,"text":"pdf"}}],"noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"4f4e49fee4b07f02db5f7363","contributors":{"authors":[{"text":"Iwatsubo, R.T.","contributorId":79516,"corporation":false,"usgs":true,"family":"Iwatsubo","given":"R.T.","email":"","affiliations":[],"preferred":false,"id":198788,"contributorType":{"id":1,"text":"Authors"},"rank":1},{"text":"Sylvester, M. A.","contributorId":10838,"corporation":false,"usgs":true,"family":"Sylvester","given":"M.","email":"","middleInitial":"A.","affiliations":[],"preferred":false,"id":198786,"contributorType":{"id":1,"text":"Authors"},"rank":2},{"text":"Gloege, I.S.","contributorId":15238,"corporation":false,"usgs":true,"family":"Gloege","given":"I.S.","email":"","affiliations":[],"preferred":false,"id":198787,"contributorType":{"id":1,"text":"Authors"},"rank":3}]}} ,{"id":18865,"text":"ofr88155 - 1988 - U.S. Geological Survey ground-water studies in Hawaii","interactions":[],"lastModifiedDate":"2012-02-02T00:07:30","indexId":"ofr88155","displayToPublicDate":"1994-01-01T00:00:00","publicationYear":"1988","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":"88-155","title":"U.S. Geological Survey ground-water studies in Hawaii","language":"ENGLISH","publisher":"U.S. Geological Survey,","doi":"10.3133/ofr88155","usgsCitation":"Ewart, C., 1988, U.S. Geological Survey ground-water studies in Hawaii: U.S. Geological Survey Open-File Report 88-155, 1 sheet :ill. ;28 cm. (2 p. - PGS), https://doi.org/10.3133/ofr88155.","productDescription":"1 sheet :ill. ;28 cm. (2 p. - PGS)","costCenters":[],"links":[{"id":151671,"rank":0,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/of/1988/0155/report-thumb.jpg"},{"id":48260,"rank":300,"type":{"id":11,"text":"Document"},"url":"https://pubs.usgs.gov/of/1988/0155/report.pdf","linkFileType":{"id":1,"text":"pdf"}}],"noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"4f4e4a2ae4b07f02db612984","contributors":{"authors":[{"text":"Ewart, Charles J.","contributorId":88759,"corporation":false,"usgs":true,"family":"Ewart","given":"Charles J.","affiliations":[],"preferred":false,"id":179882,"contributorType":{"id":1,"text":"Authors"},"rank":1}]}} ,{"id":18629,"text":"ofr88126 - 1988 - U.S. Geological Survey ground-water studies in Montana","interactions":[],"lastModifiedDate":"2012-02-02T00:07:32","indexId":"ofr88126","displayToPublicDate":"1994-01-01T00:00:00","publicationYear":"1988","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":"88-126","title":"U.S. Geological Survey ground-water studies in Montana","language":"ENGLISH","publisher":"U.S. Geological Survey,","doi":"10.3133/ofr88126","usgsCitation":"Davis, R.E., 1988, U.S. Geological Survey ground-water studies in Montana: U.S. Geological Survey Open-File Report 88-126, 2 p. :map ;28 cm., https://doi.org/10.3133/ofr88126.","productDescription":"2 p. :map ;28 cm.","costCenters":[],"links":[{"id":151413,"rank":0,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/of/1988/0126/report-thumb.jpg"},{"id":47969,"rank":300,"type":{"id":11,"text":"Document"},"url":"https://pubs.usgs.gov/of/1988/0126/report.pdf","linkFileType":{"id":1,"text":"pdf"}}],"noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"4f4e4a2ae4b07f02db612851","contributors":{"authors":[{"text":"Davis, R. 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