{"pageNumber":"1615","pageRowStart":"40350","pageSize":"25","recordCount":68937,"records":[{"id":29168,"text":"wri944222 - 1995 - Water resources and potential effects of ground-water development in Maggie, Marys, and Susie Creek basins, Elko and Eureka counties, Nevada","interactions":[],"lastModifiedDate":"2012-02-02T00:08:54","indexId":"wri944222","displayToPublicDate":"1995-09-01T00:00:00","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":"94-4222","title":"Water resources and potential effects of ground-water development in Maggie, Marys, and Susie Creek basins, Elko and Eureka counties, Nevada","docAbstract":"The basins of Maggie, Marys, and Susie Creeks in northeastern Nevada are along the Carline trend, an area of large, low-grade gold deposits. Pumping of ground water, mostly for pit dewatering at one of the mines, will reach maximum rates of about 70,000 acre-ft/yr (acre-feet per year) around the year 2000. This pumping is expected to affect ground-water levels, streamflow, and possibly the flow of Carlin spring, which is the water supply for the town of Carlin, Nev. Ground water in the upper Maggie Creek Basin moves from recharge areas in mountain ranges toward the basin axis and discharges as evapotranspiration and as inflow to the stream channel. Ground water in the lower Maggie, Marys, and Susie Creek Basins moves southward from recharge areas in mountain ranges and along the channel of lower Maggie Creek to the discharge area along the Humboldt River. Ground-water underflow between basins is through permeable bedrock of Schroeder Mountain from the upper Maggie Creek Basin to the lower Maggie Creek Basin and through permeable volcanic rocks from lower Maggie Creek to Carlin spring in the Marys Creek Basin. The only source of water to the combined area of the three basins is an estimated 420,000 acre-ft/yr of precipitation. Water leaves as runoff (38,000 acre-ft/yr) and evapotranspiration of soil moisture and ground water (380,000 acre-ft/yr). A small part of annual precipitation (about 25,000 acre-ft/yr) infiltrates the soil zone and becomes ground-water recharge. This ground water eventually is discharged as evapotranspiration (11,000 acre-ft/yr) and as inflow to the Humboldt River channel and nearby springflow (7,000 acre-ft/yr). Total discharge is estimated to be 18,000 acre-ft/yr.","language":"ENGLISH","publisher":"U.S. Geological Survey ;","doi":"10.3133/wri944222","usgsCitation":"Plume, R., 1995, Water resources and potential effects of ground-water development in Maggie, Marys, and Susie Creek basins, Elko and Eureka counties, Nevada: U.S. Geological Survey Water-Resources Investigations Report 94-4222, v, 87 p. :ill., maps (some col.) ;28 cm., https://doi.org/10.3133/wri944222.","productDescription":"v, 87 p. :ill., maps (some col.) ;28 cm.","costCenters":[],"links":[{"id":159497,"rank":0,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/wri/1994/4222/report-thumb.jpg"},{"id":58042,"rank":300,"type":{"id":11,"text":"Document"},"url":"https://pubs.usgs.gov/wri/1994/4222/report.pdf","linkFileType":{"id":1,"text":"pdf"}}],"noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"4f4e48d2e4b07f02db5481b2","contributors":{"authors":[{"text":"Plume, R. W.","contributorId":21975,"corporation":false,"usgs":true,"family":"Plume","given":"R. W.","affiliations":[],"preferred":false,"id":201068,"contributorType":{"id":1,"text":"Authors"},"rank":1}]}}
,{"id":28310,"text":"wri944151 - 1995 - Database of well and areal data, South San Francisco Bay and Peninsula area, California","interactions":[],"lastModifiedDate":"2012-02-02T00:08:44","indexId":"wri944151","displayToPublicDate":"1995-09-01T00:00:00","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":"94-4151","title":"Database of well and areal data, South San Francisco Bay and Peninsula area, California","docAbstract":"A database was developed to organize and manage data compiled for a regional assessment of geohydrologic and water-quality conditions in the south San Francisco Bay and Peninsula area in California. Available data provided by local, State, and Federal agencies and private consultants was utilized in the assessment. The database consists of geographicinformation system data layers and related tables and American Standard Code for Information Interchange files. Documentation of the database is necessary to avoid misinterpretation of the data and to make users aware of potential errors and limitations.  Most of the data compiled were collected from wells and boreholes (collectively referred to as wells in this report). This point-specific data, including construction, water-level, waterquality, pumping test, and lithologic data, are contained in tables and files that are related to a geographic information system data layer that contains the locations of the wells. There are 1,014 wells in the data layer and the related tables contain 35,845 water-level measurements (from 293 of the wells) and 9,292 water-quality samples (from 394 of the wells). Calculation of hydraulic heads and gradients from the water levels can be affected adversely by errors in the determination of the altitude of land surface at the well. Cation and anion balance computations performed on 396 of the water-quality samples indicate high cation and anion balance errors for 51 (13 percent) of the samples. Well drillers' reports were interpreted for 762 of the wells, and digital representations of the lithology of the formations are contained in files following the American Standard Code for Information Interchange. The usefulness of drillers' descriptions of the formation lithology is affected by the detail and thoroughness of the drillers' descriptions, as well as the knowledge, experience, and vocabulary of the individual who described the drill cuttings.  Additional data layers were created that contain political, geohydrologic, and other geographic data. These layers contain features represented by areas and lines rather than discrete points. The layers consist of data representing the thickness of alluvium, surficial geology, physiographic subareas, watershed boundaries, land use, water-supply districts, wastewater treatment districts, and recharge basins. The layers manually digitizing paper maps, acquisition of data already in digital form, or creation of new layers from available layers. The scale of the source data affects the accurate representation of real-world features with the data layer, and, therefore, the scale of the source data must be considered when the data are analyzed and plotted.","language":"ENGLISH","publisher":"U.S. Geological Survey ;\r\nEarth Science Information Center, Open-File Reports Section [distributor],","doi":"10.3133/wri944151","usgsCitation":"Leighton, D., Fio, J., and Metzger, L., 1995, Database of well and areal data, South San Francisco Bay and Peninsula area, California: U.S. Geological Survey Water-Resources Investigations Report 94-4151, vi, 47 p. :ill., maps ;28 cm., https://doi.org/10.3133/wri944151.","productDescription":"vi, 47 p. :ill., maps ;28 cm.","costCenters":[],"links":[{"id":123758,"rank":0,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/wri/1994/4151/report-thumb.jpg"},{"id":57122,"rank":300,"type":{"id":11,"text":"Document"},"url":"https://pubs.usgs.gov/wri/1994/4151/report.pdf","linkFileType":{"id":1,"text":"pdf"}}],"noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"4f4e4abbe4b07f02db6729c3","contributors":{"authors":[{"text":"Leighton, D.A.","contributorId":51792,"corporation":false,"usgs":true,"family":"Leighton","given":"D.A.","email":"","affiliations":[],"preferred":false,"id":199570,"contributorType":{"id":1,"text":"Authors"},"rank":1},{"text":"Fio, J.L.","contributorId":56662,"corporation":false,"usgs":true,"family":"Fio","given":"J.L.","affiliations":[],"preferred":false,"id":199571,"contributorType":{"id":1,"text":"Authors"},"rank":2},{"text":"Metzger, L.F.","contributorId":47829,"corporation":false,"usgs":true,"family":"Metzger","given":"L.F.","email":"","affiliations":[],"preferred":false,"id":199569,"contributorType":{"id":1,"text":"Authors"},"rank":3}]}}
,{"id":29831,"text":"wri944167 - 1995 - A hydrogeologic approach to identify land uses that overlie ground-water flow paths, Broward County, Florida","interactions":[],"lastModifiedDate":"2012-02-02T00:08:54","indexId":"wri944167","displayToPublicDate":"1995-09-01T00:00:00","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":"94-4167","title":"A hydrogeologic approach to identify land uses that overlie ground-water flow paths, Broward County, Florida","docAbstract":"A hydrogeologic approach that integrates the use of hydrogeologic and spatial tools aids in the identification of land uses that overlie ground- water flow paths and permits a better understanding of ground-water flow systems. A mathematical model was used to simulate the ground-water flow system in Broward County, particle-tracking software was used to determine flow paths leading to the monitor wells in Broward County, and a Geographic Information System was used to identify which land uses overlie the flow paths. A procedure using a geographic information system to evaluate the output from a ground-water flow model has been documented. The ground-water flow model was used to represent steady-state conditions during selected wet- and dry-season months, and an advective flow particle- tracking program was used to simulate the direction of ground-water flow in the aquifer system. Digital spatial data layers were created from the particle pathlines that lead to the vicinity of the open interval of selected wells in the Broward County ground-water quality monitoring network. Buffer zone data layers were created, surrounding the particle pathlines to represent the area of contribution to the water sampled from the monitor wells. Spatial data layers, combined with a land-use data layer, were used to identify the land uses that overlie the ground-water flow paths leading to the monitor wells. The simulation analysis was performed on five Broward County wells with different hydraulic parameters to determine the source of ground-water stress, determine selected particle pathlines, and identify land use in buffer zones in the vicinity of the wells. The flow paths that lead to the grid cells containing wells G-2355, G-2373, and G-2373A did not vary between the wet- and dry-season conditions. Changes in the area of contribution for wells G-2345X and G-2369 were attributed to variations in rainfall patterns, well-field pumpage, and surface-water management practices. Additionally, using a different open interval at a site, such as for wells G-2373 and G-2373A, can result in a very different area that overlies the flow path leading to the monitor well.","language":"ENGLISH","publisher":"U.S. Dept. of the Interior, U.S. Geological Survey ;\r\nEarth Science Information Center, Open-File Reports Section [distributor],","doi":"10.3133/wri944167","usgsCitation":"Sonenshein, R., 1995, A hydrogeologic approach to identify land uses that overlie ground-water flow paths, Broward County, Florida: U.S. Geological Survey Water-Resources Investigations Report 94-4167, iv, 59 p. :ill., maps ;28 cm., https://doi.org/10.3133/wri944167.","productDescription":"iv, 59 p. :ill., maps ;28 cm.","costCenters":[],"links":[{"id":124240,"rank":0,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/wri/1994/4167/report-thumb.jpg"},{"id":58628,"rank":300,"type":{"id":11,"text":"Document"},"url":"https://pubs.usgs.gov/wri/1994/4167/report.pdf","linkFileType":{"id":1,"text":"pdf"}}],"noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"4f4e4b23e4b07f02db6ae0ca","contributors":{"authors":[{"text":"Sonenshein, R.S.","contributorId":10415,"corporation":false,"usgs":true,"family":"Sonenshein","given":"R.S.","email":"","affiliations":[],"preferred":false,"id":202207,"contributorType":{"id":1,"text":"Authors"},"rank":1}]}}
,{"id":29619,"text":"wri944211 - 1995 - Effect of the Cedar River on the quality of the ground-water supply for Cedar Rapids, Iowa","interactions":[],"lastModifiedDate":"2024-01-09T22:54:20.267928","indexId":"wri944211","displayToPublicDate":"1995-09-01T00:00:00","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":"94-4211","title":"Effect of the Cedar River on the quality of the ground-water supply for Cedar Rapids, Iowa","docAbstract":"<p>The Surface Water Treatment Rule under the 1986 Amendment to the Safe Drinking Water Act requires that public-water supplies be evaluated for susceptibility to surface-water effects. The alluvial aquifer adjacent to the Cedar River is evaluated for biogenic material and monitored for selected water-quality properties and constituents to determine the effect of surface water on the water supply for the City of Cedar Rapids, Iowa. Results from monitoring of selected water-quality properties and constituents showed an inverse relation to river stage or discharge. Water-quality properties and constituents of the alluvial aquifer changed as water flowed from the river to the municipal well as a result of drawdown. The values of specific conductance, pH, temperature, and dissolved oxygen at observation well CRM-4 and municipal well Seminole 10 generally follow the trends of values for the Cedar River. Values at observation well CRM-3 and the municipal water-treatment plant showed very little correlation with values from the river. The traveltime of water through the aquifer could be an indication of the susceptibility of the alluvial aquifer to surface-water effects. Estimated traveltimes from the Cedar River to municipal well Seminole 10 ranged from 7 to 17 days.</p>\n<p>Above-normal streamflow and precipitation during the study could have increased the effect the river had on the alluvial aquifer and on the possibility of contamination by a pathogen. Microscopic particulate analysis of 29 samples found no <i>Giardia</i> cysts or <i>Crytosporidium</i> oocysts in water collected from municipal wells. Data also indicate that the aquifer is filtering out large numbers of algae, diatoms, rotifers, and nematodes as well as filtering out <i>Cryptosporidium</i>, <i>Giardia</i>, and other protozoa. The number of algae, diatoms, rotifers, protozoa, and vegetative debris for selected municipal wells tested showed at least a reduction to 1 per 1,000 of the number found in the river. A relative risk factor and a log-reduction rate were determined for the aquifer in the vicinity of selected wells. One municipal well had a high-risk factor, three other wells had a moderate-risk factor, and four wells had a low-risk factor. The filtering efficiency of the aquifer is equivalent to a 3 log-reduction rate or 99.99-percent reduction in particulates.</p>","language":"English","publisher":"U.S. Geological Survey","publisherLocation":"Iowa City, IA","doi":"10.3133/wri944211","collaboration":"Prepared in cooperation with the City of Cedar Rapids, Iowa","usgsCitation":"Schulmeyer, P., 1995, Effect of the Cedar River on the quality of the ground-water supply for Cedar Rapids, Iowa: U.S. Geological Survey Water-Resources Investigations Report 94-4211, v, 68 p., https://doi.org/10.3133/wri944211.","productDescription":"v, 68 p.","onlineOnly":"N","additionalOnlineFiles":"N","costCenters":[{"id":351,"text":"Iowa Water Science Center","active":true,"usgs":true}],"links":[{"id":424246,"rank":3,"type":{"id":36,"text":"NGMDB Index Page"},"url":"https://ngmdb.usgs.gov/Prodesc/proddesc_48080.htm","linkFileType":{"id":5,"text":"html"}},{"id":122754,"rank":1,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/wri/1994/4211/report-thumb.jpg"},{"id":58442,"rank":2,"type":{"id":11,"text":"Document"},"url":"https://pubs.usgs.gov/wri/1994/4211/report.pdf","linkFileType":{"id":1,"text":"pdf"}}],"country":"United States","state":"Iowa","city":"Cedar Rapids","geographicExtents":"{\n  \"type\": \"FeatureCollection\",\n  \"features\": [\n    {\n      \"type\": \"Feature\",\n      \"properties\": {},\n      \"geometry\": {\n        \"type\": \"Polygon\",\n        \"coordinates\": [\n          [\n            [\n              -91.7959213256836,\n              41.95336258301847\n            ],\n            [\n              -91.7959213256836,\n              42.07478160216737\n            ],\n            [\n              -91.6366195678711,\n              42.07478160216737\n            ],\n            [\n              -91.6366195678711,\n              41.95336258301847\n            ],\n            [\n              -91.7959213256836,\n              41.95336258301847\n            ]\n          ]\n        ]\n      }\n    }\n  ]\n}","noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"4f4e4a4be4b07f02db6254a3","contributors":{"authors":[{"text":"Schulmeyer, P.M.","contributorId":17208,"corporation":false,"usgs":true,"family":"Schulmeyer","given":"P.M.","affiliations":[],"preferred":false,"id":201825,"contributorType":{"id":1,"text":"Authors"},"rank":1}]}}
,{"id":18703,"text":"ofr95165 - 1995 - Nonpoint sources of pesticides in the San Joaquin River, California; input from winter storms, 1992-93","interactions":[],"lastModifiedDate":"2012-02-02T00:07:30","indexId":"ofr95165","displayToPublicDate":"1995-09-01T00:00:00","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":"95-165","title":"Nonpoint sources of pesticides in the San Joaquin River, California; input from winter storms, 1992-93","docAbstract":"Organophosphate insecticides, including chlor- pyrifos, diazinon, and methidathion, are applied to dormant orchards in the San Joaquin Valley, California, during late December through January. This time frame coincides with the period of heaviest rainfall in the valley, and rainfall mobilizes a portion of these pesticides from the orchards. The pesticides enter the San Joaquin River and have been detected along the perennial reach of the river. A storm on the evening of February 7 and the morning of February 8, 1993, deposited more than an inch and a half of rain in the San Joaquin Valley. Two distinct peaks of organophosphate pesticide concentrations were measured at the mouth of the San Joaquin River during a single rise in discharge. Both peaks were attributed to contrasts between the soil texture and hydrology of the eastern and western valley. The fine soil texture and small size of the western tributary basins contributed to rapid runoff. Diazinon concentrations peaked within hours after rainfall ended and then decreased because of a combination of dilution with pesticide-free runoff from the nearby Coast Ranges and decreased pesticide concentrations in the agricultural runoff. Data for the Merced River, a large tributary of the eastern San Joaquin Valley, are sparse, but indicate that peak concentrations occurred at least a day after those of the western tributary streams. That delay may be due to the presence of well-drained soils, the larger size of the drainage basins, and the management of surface-water drainage networks. Runoff from a subsequent storm, on February 18 and 19, contained significantly lower concentrations of most organophosphate pesticides, indicating that runoff from the first storm had already removed most of the pesticides available for rainfall-induced transport.","language":"ENGLISH","publisher":"U.S. Geological Survey ;\r\nU.S.G.S. Earth Science Information Center, Open-File Reports Section [distributor],","doi":"10.3133/ofr95165","usgsCitation":"Domagalski, J.L., 1995, Nonpoint sources of pesticides in the San Joaquin River, California; input from winter storms, 1992-93: U.S. Geological Survey Open-File Report 95-165, iv, 15 p. :ill., maps ;28 cm., https://doi.org/10.3133/ofr95165.","productDescription":"iv, 15 p. :ill., maps ;28 cm.","costCenters":[],"links":[{"id":151849,"rank":0,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/of/1995/0165/report-thumb.jpg"},{"id":48061,"rank":300,"type":{"id":11,"text":"Document"},"url":"https://pubs.usgs.gov/of/1995/0165/report.pdf","linkFileType":{"id":1,"text":"pdf"}}],"noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"4f4e4b32e4b07f02db6b479f","contributors":{"authors":[{"text":"Domagalski, Joseph L. 0000-0002-6032-757X joed@usgs.gov","orcid":"https://orcid.org/0000-0002-6032-757X","contributorId":1330,"corporation":false,"usgs":true,"family":"Domagalski","given":"Joseph","email":"joed@usgs.gov","middleInitial":"L.","affiliations":[{"id":154,"text":"California Water Science Center","active":true,"usgs":true}],"preferred":true,"id":179589,"contributorType":{"id":1,"text":"Authors"},"rank":1}]}}
,{"id":31751,"text":"ofr95115 - 1995 - Potentiometric surface of the Upper Floridan aquifer in the St. Johns River Water Management District and vicinity, Florida, September 1994","interactions":[],"lastModifiedDate":"2021-10-21T18:50:20.299836","indexId":"ofr95115","displayToPublicDate":"1995-09-01T00:00:00","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":"95-115","title":"Potentiometric surface of the Upper Floridan aquifer in the St. Johns River Water Management District and vicinity, Florida, September 1994","docAbstract":"This map depicts the potentiometric surface of the Upper Floridan aquifer in the St. Johns River Water Management District and vicinity for September 1994. The map is based on water-level measurements made at more than 900 wells and springs. Ninety-two new wells were added to the September 1994 map--42 in southern Georgia and 50 in Florida. Data on the map were contoured using 5-foot contour intervals in most areas. The potentiometric surface of this karstic aquifer generally reflects land surface topography. Potentiometric-surface highs often correspond to topographic highs, which are areas of surficial recharge to the Upper Floridan aquifer. Springs within topographic lows along with areas of more diffuse upward leakage are natural zones of discharge. Municipal, agricultural, and industrial withdrawals have lowered the potentiometric surface in some areas. The potentiometric surface ranged from 131 feet above sea lvel in Polk County to 86 feet below sea level in southern Georgia near the St. Marys River. With the additon of new wells in southern Georgia, water level data now indicate two distinct depressions at industrial well fields near the St. Marys River in southern Georgia and eastern Nassau County where previously there was only one depression indicated. Water levels measured in September 1994 generally were about 0 to 4 feet higher than those measured in September 1993, except in Seminole County, where increases of 1 to 7 feet above September 1993 levels were recorded at most wells. Generally, September 1994 water levels were 1 to to 5 feet higher than levels in May 1994 except in Union, Gradford, Alachua, Levy, and western Marion Counties where levels remained nearly unchanged, and in Seminole and northwestern Orange Counties where water levels generally were 3 to 12 feet higher than levels in May 1994.","language":"English","publisher":"U.S. Geological Survey","doi":"10.3133/ofr95115","usgsCitation":"Knowles, L., 1995, Potentiometric surface of the Upper Floridan aquifer in the St. Johns River Water Management District and vicinity, Florida, September 1994: U.S. Geological Survey Open-File Report 95-115, 1 Plate: 30.00 × 50.00 inches, https://doi.org/10.3133/ofr95115.","productDescription":"1 Plate: 30.00 × 50.00 inches","costCenters":[],"links":[{"id":160176,"rank":0,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/thumbnails/usgs_thumb.jpg"},{"id":390756,"rank":3,"type":{"id":36,"text":"NGMDB Index Page"},"url":"https://ngmdb.usgs.gov/Prodesc/proddesc_18401.htm"},{"id":19545,"rank":400,"type":{"id":17,"text":"Plate"},"url":"https://pubs.usgs.gov/of/1995/0115/plate-1.pdf","linkFileType":{"id":1,"text":"pdf"}}],"country":"United States","state":"Florida","otherGeospatial":"Upper Floridan aquifer in the St. Johns River Water Management District and vicinity","geographicExtents":"{\n  \"type\": \"FeatureCollection\",\n  \"features\": [\n    {\n      \"type\": \"Feature\",\n      \"properties\": {},\n      \"geometry\": {\n        \"type\": \"Polygon\",\n        \"coordinates\": [\n          [\n            [\n              -83,\n              26.5\n            ],\n            [\n              -80,\n              26.5\n            ],\n            [\n              -80,\n              31\n            ],\n            [\n              -83,\n              31\n            ],\n            [\n              -83,\n              26.5\n            ]\n          ]\n        ]\n      }\n    }\n  ]\n}","noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"4f4e4ad4e4b07f02db682dfa","contributors":{"authors":[{"text":"Knowles, Leel","contributorId":62252,"corporation":false,"usgs":true,"family":"Knowles","given":"Leel","affiliations":[],"preferred":false,"id":206872,"contributorType":{"id":1,"text":"Authors"},"rank":1}]}}
,{"id":30002,"text":"wri944223 - 1995 - Hydrogeology and simulation of ground-water flow in the Eutaw-McShan aquifer and in the Tuscaloosa aquifer system in northeastern Mississippi","interactions":[],"lastModifiedDate":"2023-03-14T18:33:38.551861","indexId":"wri944223","displayToPublicDate":"1995-09-01T00:00:00","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":"94-4223","title":"Hydrogeology and simulation of ground-water flow in the Eutaw-McShan aquifer and in the Tuscaloosa aquifer system in northeastern Mississippi","docAbstract":"The Eutaw-McShan aquifer and Tuscaloosa aquifer system in northeastern Mississippi were investi- gated to better understand the hydrogeology and the ground-water flow in and between the aquifers. A numerical model was developed to simulate ground- water flow for prepumping and pumping conditions, and model simulatons projected the possible effects of increased ground-water withdrawals. The five aquifers studied, from youngest to oldest, are the Eutaw-McShan, Gordo, Coker, massive sand, and the Lower Cretaceous aquifers. The finite-difference computer code MODFLOW was used to represent the flow system. The model grid covers 33,440 square miles, primarily in northeastern Mississippi, but includes parts of northwestern Alabama, southwestern Tennessee, and eastern Arkansas. A comparison of the simulated predevelopment and 1992 potentiometric surfaces for the aquifers shows an overall water- level decline. Simulated water levels declined an average of 53 and 44 feet in the confined parts of the Eutaw-McShan and Gordo aquifers, respectively. However, the area near Tupelo had a significant rise in water levels due to decreased pumpage from the Eutaw-McShan and Gordo aquifers compared to the simulated potentiometric surface for 1978.","language":"English","publisher":"U.S. Geological Survey","doi":"10.3133/wri944223","usgsCitation":"Strom, E.W., and Mallory, M.J., 1995, Hydrogeology and simulation of ground-water flow in the Eutaw-McShan aquifer and in the Tuscaloosa aquifer system in northeastern Mississippi: U.S. Geological Survey Water-Resources Investigations Report 94-4223, vi, 83 p., https://doi.org/10.3133/wri944223.","productDescription":"vi, 83 p.","costCenters":[],"links":[{"id":58808,"rank":2,"type":{"id":11,"text":"Document"},"url":"https://pubs.usgs.gov/wri/1994/4223/report.pdf","linkFileType":{"id":1,"text":"pdf"}},{"id":121828,"rank":1,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/wri/1994/4223/report-thumb.jpg"},{"id":414116,"rank":3,"type":{"id":36,"text":"NGMDB Index Page"},"url":"https://ngmdb.usgs.gov/Prodesc/proddesc_48090.htm","linkFileType":{"id":5,"text":"html"}}],"country":"United States","state":"Mississippi","otherGeospatial":"Eutaw-McShan aquifer, Tuscaloosa aquifer","geographicExtents":"{\n  \"type\": \"FeatureCollection\",\n  \"features\": [\n    {\n      \"type\": \"Feature\",\n      \"properties\": {},\n      \"geometry\": {\n        \"coordinates\": [\n          [\n            [\n              -89.6436,\n              34.9133\n            ],\n            [\n              -89.6436,\n              32.4958\n            ],\n            [\n              -87.7056,\n              32.4958\n            ],\n            [\n              -87.7056,\n              34.9133\n            ],\n            [\n              -89.6436,\n              34.9133\n            ]\n          ]\n        ],\n        \"type\": \"Polygon\"\n      }\n    }\n  ]\n}","noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"4f4e4a4ae4b07f02db6252dc","contributors":{"authors":[{"text":"Strom, E. W.","contributorId":90776,"corporation":false,"usgs":true,"family":"Strom","given":"E.","email":"","middleInitial":"W.","affiliations":[],"preferred":false,"id":202510,"contributorType":{"id":1,"text":"Authors"},"rank":1},{"text":"Mallory, M. J.","contributorId":10398,"corporation":false,"usgs":true,"family":"Mallory","given":"M.","email":"","middleInitial":"J.","affiliations":[],"preferred":false,"id":202509,"contributorType":{"id":1,"text":"Authors"},"rank":2}]}}
,{"id":70185356,"text":"70185356 - 1995 - State-dependent anisotrophy: Comparison of quasi-analytical solutions with stochastic results for steady gravity drainage","interactions":[],"lastModifiedDate":"2019-02-25T09:49:12","indexId":"70185356","displayToPublicDate":"1995-09-01T00:00:00","publicationYear":"1995","noYear":false,"publicationType":{"id":2,"text":"Article"},"publicationSubtype":{"id":10,"text":"Journal Article"},"seriesTitle":{"id":3722,"text":"Water Resources Research","onlineIssn":"1944-7973","printIssn":"0043-1397","active":true,"publicationSubtype":{"id":10}},"title":"State-dependent anisotrophy: Comparison of quasi-analytical solutions with stochastic results for steady gravity drainage","docAbstract":"<p><span>Anisotropy in large-scale unsaturated hydraulic conductivity of layered soils changes with the moisture state. Here, state-dependent anisotropy is computed under conditions of large-scale gravity drainage. Soils represented by Gardner's exponential function are perfectly stratified, periodic, and inclined. Analytical integration of Darcy’s law across each layer results in a system of nonlinear equations that is solved iteratively for capillary suction at layer interfaces and for the Darcy flux normal to layering. Computed fluxes and suction profiles are used to determine both upscaled hydraulic conductivity in the principal directions and the corresponding “state-dependent” anisotropy ratio as functions of the mean suction. Three groups of layered soils are analyzed and compared with independent predictions from the stochastic results of Yeh et al. (1985b). The small-perturbation approach predicts appropriate behaviors for anisotropy under nonarid conditions. However, the stochastic results are limited to moderate values of mean suction; this limitation is linked to a Taylor series approximation in terms of a group of statistical and geometric parameters. Two alternative forms of the Taylor series provide upper and lower bounds for the state-dependent anisotropy of relatively dry soils.</span></p>","language":"English","publisher":"American Geophysical Union","doi":"10.1029/95WR00790","usgsCitation":"Green, T.R., and Freyberg, D.L., 1995, State-dependent anisotrophy: Comparison of quasi-analytical solutions with stochastic results for steady gravity drainage: Water Resources Research, v. 31, no. 9, p. 2201-2211, https://doi.org/10.1029/95WR00790.","productDescription":"11 p. ","startPage":"2201","endPage":"2211","costCenters":[{"id":589,"text":"Toxic Substances Hydrology Program","active":true,"usgs":true}],"links":[{"id":337917,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/thumbnails/outside_thumb.jpg"}],"volume":"31","issue":"9","noUsgsAuthors":false,"publicationDate":"2010-07-09","publicationStatus":"PW","scienceBaseUri":"58d23b93e4b0236b68f82916","contributors":{"authors":[{"text":"Green, Timothy R.","contributorId":93587,"corporation":false,"usgs":true,"family":"Green","given":"Timothy","email":"","middleInitial":"R.","affiliations":[],"preferred":false,"id":685309,"contributorType":{"id":1,"text":"Authors"},"rank":1},{"text":"Freyberg, David L.","contributorId":189597,"corporation":false,"usgs":false,"family":"Freyberg","given":"David","email":"","middleInitial":"L.","affiliations":[],"preferred":false,"id":685310,"contributorType":{"id":1,"text":"Authors"},"rank":2}]}}
,{"id":70195998,"text":"70195998 - 1995 - The interaction of groundwater with prairie pothole wetlands in the Cottonwood Lake area, east-central North Dakota 1979-1990","interactions":[],"lastModifiedDate":"2026-04-28T14:26:10.398652","indexId":"70195998","displayToPublicDate":"1995-09-01T00:00:00","publicationYear":"1995","noYear":false,"publicationType":{"id":2,"text":"Article"},"publicationSubtype":{"id":10,"text":"Journal Article"},"seriesTitle":{"id":3750,"text":"Wetlands","onlineIssn":"1943-6246","printIssn":"0277-5212","active":true,"publicationSubtype":{"id":10}},"title":"The interaction of groundwater with prairie pothole wetlands in the Cottonwood Lake area, east-central North Dakota 1979-1990","docAbstract":"<p><span>The interaction of ground water with prairie wetlands in the Cottonwood Lake area has been the focus of research by the U.S. Geological Survey and the U.S. Fish and Wildlife Service since 1977. During this time, climatic conditions at the site ranged from near the driest to near the wettest of the century. Water levels in wetlands and in water-table wells throughout the study area responded to these changing climate conditions in a variety of ways. The topographically highest wetlands recharged ground water whenever they received water from precipitation. The wetland of principal interest, Wetland P1, which is at an intermediate altitude, received ground-water discharge much of the time, but it also had transpiration-induced seepage from it along parts of its perimeter during all but the wettest year. The large fluctuations of the water table in response to recharge and transpiration reflect the ease with which water moves vertically through the fractured till. Lateral movement of ground water is much slower; pore-water moves vertically through the fractured till. Lateral movement of ground water is much slower; pore-water velocities are generally less than 3 m yr</span><sup>−1</sup><span>. The water supply to the wetlands is largely from precipitation during fall, winter, and spring. During these periods, precipitation either falls directly on the wetland, or precipitation that falls on the upland runs over frozen soils or saturated soils into the wetland. The average ratio of stage rise to total overwinter precipitation was 2.59 for the 12-year study period. After plants leaf out, precipitation generally results in much lower rises of the wetland water level. The average ratio of stage rise to over-summer precipitation was less than 1.0.</span></p>","language":"English","publisher":"Springer Nature","doi":"10.1007/BF03160700","usgsCitation":"Winter, T.C., and Rosenberry, D.O., 1995, The interaction of groundwater with prairie pothole wetlands in the Cottonwood Lake area, east-central North Dakota 1979-1990: Wetlands, v. 15, no. 3, p. 193-211, https://doi.org/10.1007/BF03160700.","productDescription":"19 p.","startPage":"193","endPage":"211","costCenters":[{"id":478,"text":"North Dakota Water Science Center","active":true,"usgs":true},{"id":34685,"text":"Dakota Water Science Center","active":true,"usgs":true}],"links":[{"id":352430,"rank":1,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/thumbnails/outside_thumb.jpg"}],"country":"United States","state":"North Dakota","otherGeospatial":"Cottonwood Lake","geographicExtents":"{\n  \"type\": \"FeatureCollection\",\n  \"features\": [\n    {\n      \"type\": \"Feature\",\n      \"properties\": {},\n      \"geometry\": {\n        \"coordinates\": [\n          [\n            [\n              -100.79449016470934,\n              46.78519489556359\n            ],\n            [\n              -100.79449016470934,\n              46.76599669842659\n            ],\n            [\n              -100.7706816672288,\n              46.76599669842659\n            ],\n            [\n              -100.7706816672288,\n              46.78519489556359\n            ],\n            [\n              -100.79449016470934,\n              46.78519489556359\n            ]\n          ]\n        ],\n        \"type\": \"Polygon\"\n      }\n    }\n  ]\n}","volume":"15","issue":"3","noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"5aff20d0e4b0da30c1bfd5e3","contributors":{"authors":[{"text":"Winter, Thomas C.","contributorId":84736,"corporation":false,"usgs":true,"family":"Winter","given":"Thomas","email":"","middleInitial":"C.","affiliations":[],"preferred":false,"id":730867,"contributorType":{"id":1,"text":"Authors"},"rank":1},{"text":"Rosenberry, Donald O. 0000-0003-0681-5641 rosenber@usgs.gov","orcid":"https://orcid.org/0000-0003-0681-5641","contributorId":1312,"corporation":false,"usgs":true,"family":"Rosenberry","given":"Donald","email":"rosenber@usgs.gov","middleInitial":"O.","affiliations":[{"id":438,"text":"National Research Program - Western Branch","active":true,"usgs":true},{"id":5044,"text":"National Research Program - Central Branch","active":true,"usgs":true}],"preferred":true,"id":730868,"contributorType":{"id":1,"text":"Authors"},"rank":2}]}}
,{"id":18284,"text":"ofr95285 - 1995 - A selected bibliography of water-related research in the upper Klamath Basin, Oregon","interactions":[],"lastModifiedDate":"2017-02-07T09:54:54","indexId":"ofr95285","displayToPublicDate":"1995-09-01T00:00:00","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":"95-285","title":"A selected bibliography of water-related research in the upper Klamath Basin, Oregon","docAbstract":"A bibliography containing 165 selected references was compiled to assist local, State, and Federal agencies that have ongoing water-related research interests in the Upper Klamath Basin. The report has two parts. Part 1 is a list of bibliographic citations alphabetized by author, and Part 2 is a subject index that references bibliographic entries. Categories of the subject index include chemistry, ecology, geology, hydrology, land use, and water management related reports. Maps, reports, proposals, theses, dissertations, and journal articles are referenced. Some of the environmental issues addressed by references in the bibliography are hypereutrophication, nuisance algal blooms, endangered fish species, water allocation questions, wetland and riparian habitat restoration, and pesticide and fertilizer utilization.","language":"ENGLISH","publisher":"U.S. Geological Survey ;\r\nU.S.G.S. Earth Science Information Center, Open-File Reports Section [distributor],","doi":"10.3133/ofr95285","usgsCitation":"Brownell, D.L., and Rinallo, M.R., 1995, A selected bibliography of water-related research in the upper Klamath Basin, Oregon: U.S. Geological Survey Open-File Report 95-285, iii, 23 p. :map ;28 cm., https://doi.org/10.3133/ofr95285.","productDescription":"iii, 23 p. :map ;28 cm.","costCenters":[{"id":518,"text":"Oregon Water Science Center","active":true,"usgs":true}],"links":[{"id":47639,"rank":300,"type":{"id":11,"text":"Document"},"url":"https://pubs.usgs.gov/of/1995/0285/report.pdf","linkFileType":{"id":1,"text":"pdf"}},{"id":149224,"rank":0,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/of/1995/0285/report-thumb.jpg"},{"id":1042,"rank":100,"type":{"id":15,"text":"Index Page"},"url":"https://or.water.usgs.gov/pubs_dir/Html/OFR95-285/klamath_bib.html","linkFileType":{"id":5,"text":"html"}}],"noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"4f4e4b17e4b07f02db6a64eb","contributors":{"authors":[{"text":"Brownell, Dorie L.","contributorId":50539,"corporation":false,"usgs":true,"family":"Brownell","given":"Dorie","email":"","middleInitial":"L.","affiliations":[],"preferred":false,"id":178848,"contributorType":{"id":1,"text":"Authors"},"rank":1},{"text":"Rinallo, Mia R.","contributorId":98333,"corporation":false,"usgs":true,"family":"Rinallo","given":"Mia","email":"","middleInitial":"R.","affiliations":[],"preferred":false,"id":178849,"contributorType":{"id":1,"text":"Authors"},"rank":2}]}}
,{"id":31748,"text":"ofr94483 - 1995 - Ground-water use by public-supply systems in Tennessee, 1990","interactions":[],"lastModifiedDate":"2021-11-30T22:42:27.834564","indexId":"ofr94483","displayToPublicDate":"1995-09-01T00:00:00","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":"94-483","title":"Ground-water use by public-supply systems in Tennessee, 1990","docAbstract":"Ground-water use by public water-supply systems during 1990 was inventoried in Tennessee. Ground- water withdrawals were estimated to average 269 million gallons per day (Mgal/d), or 38 percent of the total public-supply water use. This volume represents an increase of 34 percent in the use of ground water for public supply since 1980 when public-supply withdrawals were 200 Mgal/d. About 212 Mgal/d (79 percent) were withdrawn from the Tertiary sand and Cretaceous sand aquifers in western Tennessee. The largest ground-water with- drawals for public-supply occurred in Shelby County (154 Mgal/d or 57 percent of the total withdrawals for public supply). Thirty-four of the 267 principal public water-supply systems withdrew 1 Mgal/d or more and accounted for 83 percent of ground water withdrawn for public supply.","language":"English","publisher":"U.S. Geological Survey","doi":"10.3133/ofr94483","usgsCitation":"Hutson, S.S., 1995, Ground-water use by public-supply systems in Tennessee, 1990: U.S. Geological Survey Open-File Report 94-483, 1 Plate: 36.36 × 24.53 inches, https://doi.org/10.3133/ofr94483.","productDescription":"1 Plate: 36.36 × 24.53 inches","costCenters":[],"links":[{"id":160396,"rank":0,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/thumbnails/usgs_thumb.jpg"},{"id":392276,"rank":3,"type":{"id":36,"text":"NGMDB Index Page"},"url":"https://ngmdb.usgs.gov/Prodesc/proddesc_12541.htm"},{"id":21637,"rank":400,"type":{"id":17,"text":"Plate"},"url":"https://pubs.usgs.gov/of/1994/0483/plate-1.pdf","linkFileType":{"id":1,"text":"pdf"}}],"country":"United 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,{"id":26289,"text":"wri944165 - 1995 - Application of surface geophysical techniques in a study of the geomorphology of the lower Copper River, Alaska","interactions":[],"lastModifiedDate":"2012-02-02T00:08:17","indexId":"wri944165","displayToPublicDate":"1995-09-01T00:00:00","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":"94-4165","title":"Application of surface geophysical techniques in a study of the geomorphology of the lower Copper River, Alaska","docAbstract":"As part of a geomorphology study of the lower Copper River, three surface geophysical techniques were tested for their ability to detect infilled scour holes at bridge piers, old river channels, and subbottom deposits in a glacier-formed lake. The methods were (1) ground-penetrating radar, (2) continuous seismic reflection using a color fathometer, and (3) continuous seismic reflection using a tuned transducer. In water depths less than 20 feet, ground-penetrating radar detected infilled scour holes at bridge piers and old river channels on land. Continuous seismic reflection using a tuned transducer was effective in water and detected infilled scour holes at bridge piers and subbottom deposits in a glacier lake. The color fathometer was useful in determining depths of water but was not able to penetrate the subbottom.","language":"ENGLISH","publisher":"U.S. Geological Survey ;\r\nEarth Science Information Center, Open-File Reports Section [distributor],","doi":"10.3133/wri944165","usgsCitation":"Brabets, T.P., 1995, Application of surface geophysical techniques in a study of the geomorphology of the lower Copper River, Alaska: U.S. Geological Survey Water-Resources Investigations Report 94-4165, iv, 47 p. :ill. (some col.), maps ;28 cm., https://doi.org/10.3133/wri944165.","productDescription":"iv, 47 p. :ill. (some col.), maps ;28 cm.","costCenters":[],"links":[{"id":122774,"rank":0,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/wri/1994/4165/report-thumb.jpg"},{"id":55097,"rank":300,"type":{"id":11,"text":"Document"},"url":"https://pubs.usgs.gov/wri/1994/4165/report.pdf","linkFileType":{"id":1,"text":"pdf"}}],"noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"4f4e4ac6e4b07f02db67a7d4","contributors":{"authors":[{"text":"Brabets, T. P.","contributorId":103289,"corporation":false,"usgs":true,"family":"Brabets","given":"T.","email":"","middleInitial":"P.","affiliations":[],"preferred":false,"id":196123,"contributorType":{"id":1,"text":"Authors"},"rank":1}]}}
,{"id":27408,"text":"wri934162 - 1995 - Hydrogeology of south-central St. Croix, U.S. Virgin Islands","interactions":[],"lastModifiedDate":"2022-01-10T20:42:38.339298","indexId":"wri934162","displayToPublicDate":"1995-09-01T00:00:00","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":"93-4162","title":"Hydrogeology of south-central St. Croix, U.S. Virgin Islands","docAbstract":"The subsurface geology of south-central St. Croix consists of alluvium and underlying carbonate rocks. The alluvial deposits consist of sand and gravel with cobbles and boulders and, locally, thin lenses of silt and clay. The carbonate rocks consist of the Oligocene to Middle Miocene age Jealousy formation, the Miocene and Pliocene are Kingshill Limestone, and the Pliocene and younger age Post-Kingshill Carbonates. Ground water occurs under water-table conditions in the alluvial, Post-Kingshill Carbonates, and Kingshill Limestone deposits. These deposits are hydraulically connected and are considered to be a single hydrologic unit. The top of the water-table aquifer can range from 5 to 68 feet below land surface. The top of the Jealousy Formation is considered to be the bottom of the water- table aquifer and generally is from 85 to greater than 120 feet below land surface. Aquifer yields in south- central St. Croix can range from less than 5 gallons per minute to 80 gallons per minute. The ground- water in the study area is of the sodium-chloride type. Ground-water samples collected from selected wells had chloride concentrations ranging from 64 to 4,400 milligrams per liter, and dissolved solid concen- trations ranging from 619 to 7,540 milligrams per liter. Connate water is suspected as being the source of sodium chloride in the ground water.","language":"English","publisher":"U.S. Geological Survey","doi":"10.3133/wri934162","usgsCitation":"Graves, R.P., 1995, Hydrogeology of south-central St. Croix, U.S. Virgin Islands: U.S. Geological Survey Water-Resources Investigations Report 93-4162, v, 33 p., https://doi.org/10.3133/wri934162.","productDescription":"v, 33 p.","costCenters":[],"links":[{"id":394132,"rank":3,"type":{"id":36,"text":"NGMDB Index Page"},"url":"https://ngmdb.usgs.gov/Prodesc/proddesc_47862.htm"},{"id":56267,"rank":300,"type":{"id":11,"text":"Document"},"url":"https://pubs.usgs.gov/wri/1993/4162/report.pdf","linkFileType":{"id":1,"text":"pdf"}},{"id":119772,"rank":0,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/wri/1993/4162/report-thumb.jpg"}],"country":"U.S. Virgin Islands","otherGeospatial":"St. Croix","geographicExtents":"{\n  \"type\": \"FeatureCollection\",\n  \"features\": [\n    {\n      \"type\": \"Feature\",\n      \"properties\": {},\n      \"geometry\": {\n        \"type\": \"Polygon\",\n        \"coordinates\": [\n          [\n            [\n              -64.8217,\n              17.6889\n            ],\n            [\n              -64.7444,\n              17.6889\n            ],\n            [\n              -64.7444,\n              17.7292\n            ],\n            [\n              -64.8217,\n              17.7292\n            ],\n            [\n              -64.8217,\n              17.6889\n            ]\n          ]\n        ]\n      }\n    }\n  ]\n}","noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"4f4e4a2fe4b07f02db615cbf","contributors":{"authors":[{"text":"Graves, R. P.","contributorId":99179,"corporation":false,"usgs":true,"family":"Graves","given":"R.","email":"","middleInitial":"P.","affiliations":[],"preferred":false,"id":198062,"contributorType":{"id":1,"text":"Authors"},"rank":1}]}}
,{"id":70185382,"text":"70185382 - 1995 - Gross-beta activity in ground water: natural sources and artifacts of sampling and laboratory analysis","interactions":[],"lastModifiedDate":"2022-10-17T15:23:29.393021","indexId":"70185382","displayToPublicDate":"1995-09-01T00:00:00","publicationYear":"1995","noYear":false,"publicationType":{"id":2,"text":"Article"},"publicationSubtype":{"id":10,"text":"Journal Article"},"seriesTitle":{"id":835,"text":"Applied Geochemistry","active":true,"publicationSubtype":{"id":10}},"title":"Gross-beta activity in ground water: natural sources and artifacts of sampling and laboratory analysis","docAbstract":"<p>Gross-beta activity has been used as an indicator of beta-emitting isotopes in water since at least the early 1950s. Originally designed for detection of radioactive releases from nuclear facilities and weapons tests, analysis of gross-beta activity is widely used in studies of naturally occurring radioactivity in ground water. Analyses of about 800 samples from 5 ground-water regions of the United States provide a basis for evaluating the utility of this measurement. The data suggest that measured gross-beta activities are due to (1) long-lived radionuclides in ground water, and (2) ingrowth of beta-emitting radionuclides during holding times between collection of samples and laboratory measurements.</p><p>Although<sup>40</sup>K and<sup>228</sup>Ra appear to be the primary sources of beta activity in ground water, the sum of<sup>40</sup>K plus<sup>228</sup>Ra appears to be less than the measured gross-beta activity in most ground-water samples. The difference between the contribution from these radionuclides and gross-beta activity is most pronounced in ground water with gross-beta activities &gt; 10 pCi/L, where these 2 radionuclides account for less than one-half the measured ross-beta activity. One exception is groundwater from the Coastal Plain of New Jersey, where<sup>40</sup>K plus<sup>228</sup>Ra generally contribute most of the gross-beta activity. In contrast,<sup>40</sup>K and<sup>228</sup>Ra generally contribute most of beta activity in ground water with gross-beta activities &lt; 1 pCi/L.</p><p>The gross-beta technique does not measure all beta activity in ground water. Although<sup>3</sup>H contributes beta activity to some ground water, it is driven from the sample before counting and therefore is not detected by gross-beta measurements. Beta-emitting radionuclides with half-lives shorter than a few days can decay to low values between sampling and counting. Although little is known about concentrations of most short-lived beta-emitting radionuclides in environmental ground water (water unaffected by direct releases from nuclear facilities and weapons tests), their activities are expected to be low.</p><p>Ingrowth of beta-emitting radionuclides during sample holding times can contribute to gross-beta activity, particularly in ground water with gross-beta activities &gt; 10 pCi/L. Ingrowth of beta-emitting progeny of<sup>238</sup>U, specifically<sup>234</sup>Pa and<sup>234</sup>Th, contributes much of the measured gross-beta activity in ground water from 4 of the 5 areas studied. Consequently, gross-beta activity measurements commonly overestimate the abundance of beta-emitting radionuclides actually present in ground water. Differing sample holding times before analysis lead to differing amounts of ingrowth of the two progeny. Therefore, holding times can affect observed gross-beta measurements, particularly in ground water with<sup>238</sup>U activities that are moderate to high compared with the activity of<sup>40</sup>K plus<sup>228</sup>Ra. Uncertainties associated with counting efficiencies for beta particles with different energies further complicate the interpretation of gross-beta measurements.</p>","language":"English","publisher":"Elsevier","doi":"10.1016/0883-2927(95)00020-8","usgsCitation":"Welch, A., Szabo, Z., Parkhurst, D.L., Van Metre, P.C., and Mullin, A.H., 1995, Gross-beta activity in ground water: natural sources and artifacts of sampling and laboratory analysis: Applied Geochemistry, v. 10, no. 5, p. 491-503, https://doi.org/10.1016/0883-2927(95)00020-8.","productDescription":"13 p.","startPage":"491","endPage":"503","costCenters":[{"id":589,"text":"Toxic Substances Hydrology Program","active":true,"usgs":true}],"links":[{"id":337945,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/thumbnails/outside_thumb.jpg"}],"volume":"10","issue":"5","noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"58d23b93e4b0236b68f82910","contributors":{"authors":[{"text":"Welch, Alan H.","contributorId":45286,"corporation":false,"usgs":true,"family":"Welch","given":"Alan H.","affiliations":[],"preferred":false,"id":685396,"contributorType":{"id":1,"text":"Authors"},"rank":1},{"text":"Szabo, Zoltan 0000-0002-0760-9607 zszabo@usgs.gov","orcid":"https://orcid.org/0000-0002-0760-9607","contributorId":138827,"corporation":false,"usgs":true,"family":"Szabo","given":"Zoltan","email":"zszabo@usgs.gov","affiliations":[{"id":470,"text":"New Jersey Water Science Center","active":true,"usgs":true}],"preferred":true,"id":814580,"contributorType":{"id":1,"text":"Authors"},"rank":2},{"text":"Parkhurst, David L. 0000-0003-3348-1544 dlpark@usgs.gov","orcid":"https://orcid.org/0000-0003-3348-1544","contributorId":1088,"corporation":false,"usgs":true,"family":"Parkhurst","given":"David","email":"dlpark@usgs.gov","middleInitial":"L.","affiliations":[{"id":5044,"text":"National Research Program - Central Branch","active":true,"usgs":true}],"preferred":true,"id":814581,"contributorType":{"id":1,"text":"Authors"},"rank":3},{"text":"Van Metre, Peter C. 0000-0001-7564-9814","orcid":"https://orcid.org/0000-0001-7564-9814","contributorId":211144,"corporation":false,"usgs":true,"family":"Van Metre","given":"Peter","email":"","middleInitial":"C.","affiliations":[{"id":583,"text":"Texas Water Science Center","active":true,"usgs":true},{"id":27111,"text":"National Water Quality Program","active":true,"usgs":true},{"id":374,"text":"Maryland Water Science Center","active":true,"usgs":true},{"id":451,"text":"National Water Quality Assessment Program","active":true,"usgs":true},{"id":37277,"text":"WMA - Earth System Processes Division","active":true,"usgs":true}],"preferred":true,"id":814582,"contributorType":{"id":1,"text":"Authors"},"rank":4},{"text":"Mullin, Ann H. ahmullin@usgs.gov","contributorId":2188,"corporation":false,"usgs":true,"family":"Mullin","given":"Ann","email":"ahmullin@usgs.gov","middleInitial":"H.","affiliations":[],"preferred":true,"id":814583,"contributorType":{"id":1,"text":"Authors"},"rank":5}]}}
,{"id":20267,"text":"ofr95153 - 1995 - Records of wells and chemical analyses of ground water in Charles Mix and Douglas counties, South Dakota","interactions":[],"lastModifiedDate":"2012-02-02T00:07:40","indexId":"ofr95153","displayToPublicDate":"1995-09-01T00:00:00","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":"95-153","title":"Records of wells and chemical analyses of ground water in Charles Mix and Douglas counties, South Dakota","docAbstract":"The U.S. Geological Survey, in cooperation with the South Dakota Department of Environmental and Natural Resources, maintains a data base of information on water resources in the State of South Dakota. The ground-water site data for Charles Mix and Douglas Counties are presented in two tables, with the data organized by county and location. The chemical data for ground-water sites also are located in a table organized by geologic unit and location.","language":"ENGLISH","publisher":"U.S. Geological Survey ;\r\nU.S.G.S. Earth Science Information Center, Open-File Reports Section [distributor],","doi":"10.3133/ofr95153","usgsCitation":"Neitzert, K.M., 1995, Records of wells and chemical analyses of ground water in Charles Mix and Douglas counties, South Dakota: U.S. Geological Survey Open-File Report 95-153, iii, 129 p. :ill., map ;28 cm., https://doi.org/10.3133/ofr95153.","productDescription":"iii, 129 p. :ill., map ;28 cm.","costCenters":[],"links":[{"id":152283,"rank":0,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/of/1995/0153/report-thumb.jpg"},{"id":49802,"rank":300,"type":{"id":11,"text":"Document"},"url":"https://pubs.usgs.gov/of/1995/0153/report.pdf","linkFileType":{"id":1,"text":"pdf"}}],"noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"4f4e4a53e4b07f02db62b695","contributors":{"authors":[{"text":"Neitzert, Kathleen M. kmneitze@usgs.gov","contributorId":1833,"corporation":false,"usgs":true,"family":"Neitzert","given":"Kathleen","email":"kmneitze@usgs.gov","middleInitial":"M.","affiliations":[{"id":562,"text":"South Dakota Water Science Center","active":true,"usgs":true}],"preferred":true,"id":182355,"contributorType":{"id":1,"text":"Authors"},"rank":1}]}}
,{"id":18902,"text":"ofr94357 - 1995 - Geohydrologic framework, historical development of the ground-water system, and general hydrologic and water-quality conditions in 1990, South San Francisco Bay and Peninsula area, California","interactions":[],"lastModifiedDate":"2012-02-02T00:07:32","indexId":"ofr94357","displayToPublicDate":"1995-09-01T00:00:00","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":"94-357","title":"Geohydrologic framework, historical development of the ground-water system, and general hydrologic and water-quality conditions in 1990, South San Francisco Bay and Peninsula area, California","language":"ENGLISH","publisher":"U.S. Geological Survey ;\r\nEarth Science Information Center, Open-File Reports Section [distributor],","doi":"10.3133/ofr94357","usgsCitation":"Fio, J.L., and Leighton, D.A., 1995, Geohydrologic framework, historical development of the ground-water system, and general hydrologic and water-quality conditions in 1990, South San Francisco Bay and Peninsula area, California: U.S. Geological Survey Open-File Report 94-357, vi, 46 p. :ill., maps ;28 cm., https://doi.org/10.3133/ofr94357.","productDescription":"vi, 46 p. :ill., maps ;28 cm.","costCenters":[],"links":[{"id":151476,"rank":0,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/of/1994/0357/report-thumb.jpg"},{"id":48302,"rank":300,"type":{"id":11,"text":"Document"},"url":"https://pubs.usgs.gov/of/1994/0357/report.pdf","linkFileType":{"id":1,"text":"pdf"}}],"noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"4f4e4b1be4b07f02db6a8e7d","contributors":{"authors":[{"text":"Fio, John L.","contributorId":77543,"corporation":false,"usgs":true,"family":"Fio","given":"John","email":"","middleInitial":"L.","affiliations":[],"preferred":false,"id":179950,"contributorType":{"id":1,"text":"Authors"},"rank":1},{"text":"Leighton, David A.","contributorId":95493,"corporation":false,"usgs":true,"family":"Leighton","given":"David","email":"","middleInitial":"A.","affiliations":[],"preferred":false,"id":179951,"contributorType":{"id":1,"text":"Authors"},"rank":2}]}}
,{"id":20081,"text":"ofr94456 - 1995 - Meteorological, stream-discharge, and water-quality data for water year 1992 from two basins in central Nevada","interactions":[],"lastModifiedDate":"2012-02-02T00:07:44","indexId":"ofr94456","displayToPublicDate":"1995-09-01T00:00:00","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":"94-456","title":"Meteorological, stream-discharge, and water-quality data for water year 1992 from two basins in central Nevada","language":"ENGLISH","publisher":"U.S. Geological Survey :\r\nEarth Science Information Center, Open-File Reports Section [distributor],","doi":"10.3133/ofr94456","usgsCitation":"McKinley, P.W., and Oliver, T., 1995, Meteorological, stream-discharge, and water-quality data for water year 1992 from two basins in central Nevada: U.S. Geological Survey Open-File Report 94-456, iv, 66 p. :ill., map ;28 cm., https://doi.org/10.3133/ofr94456.","productDescription":"iv, 66 p. :ill., map ;28 cm.","costCenters":[],"links":[{"id":153146,"rank":0,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/of/1994/0456/report-thumb.jpg"},{"id":49634,"rank":300,"type":{"id":11,"text":"Document"},"url":"https://pubs.usgs.gov/of/1994/0456/report.pdf","linkFileType":{"id":1,"text":"pdf"}}],"noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"4f4e4a51e4b07f02db6297f4","contributors":{"authors":[{"text":"McKinley, P. W.","contributorId":16414,"corporation":false,"usgs":true,"family":"McKinley","given":"P.","email":"","middleInitial":"W.","affiliations":[],"preferred":false,"id":182028,"contributorType":{"id":1,"text":"Authors"},"rank":1},{"text":"Oliver, T.A.","contributorId":95500,"corporation":false,"usgs":true,"family":"Oliver","given":"T.A.","email":"","affiliations":[],"preferred":false,"id":182029,"contributorType":{"id":1,"text":"Authors"},"rank":2}]}}
,{"id":20772,"text":"ofr94317 - 1995 - Selected hydrologic data from Fortymile Wash in the Yucca Mountain area, Nevada, water year 1992","interactions":[],"lastModifiedDate":"2012-02-02T00:07:35","indexId":"ofr94317","displayToPublicDate":"1995-09-01T00:00:00","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":"94-317","title":"Selected hydrologic data from Fortymile Wash in the Yucca Mountain area, Nevada, water year 1992","language":"ENGLISH","publisher":"U.S. Geological Survey :\r\nUSGS Earth Science Information Center, Open-File Reports Section [distributor],","doi":"10.3133/ofr94317","usgsCitation":"Savard, C.S., 1995, Selected hydrologic data from Fortymile Wash in the Yucca Mountain area, Nevada, water year 1992: U.S. Geological Survey Open-File Report 94-317, iv, 38 p. :ill., map ;28 cm., https://doi.org/10.3133/ofr94317.","productDescription":"iv, 38 p. :ill., map ;28 cm.","costCenters":[],"links":[{"id":152513,"rank":0,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/of/1994/0317/report-thumb.jpg"},{"id":50322,"rank":300,"type":{"id":11,"text":"Document"},"url":"https://pubs.usgs.gov/of/1994/0317/report.pdf","linkFileType":{"id":1,"text":"pdf"}}],"noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"4f4e4a06e4b07f02db5f8c41","contributors":{"authors":[{"text":"Savard, Charles S. cssavard@usgs.gov","contributorId":3538,"corporation":false,"usgs":true,"family":"Savard","given":"Charles","email":"cssavard@usgs.gov","middleInitial":"S.","affiliations":[{"id":465,"text":"Nevada Water Science Center","active":true,"usgs":true}],"preferred":true,"id":183225,"contributorType":{"id":1,"text":"Authors"},"rank":1}]}}
,{"id":17235,"text":"ofr95143 - 1995 - Hydrogeologic data for the northern Rocky Mountains intermontane basins, Montana","interactions":[],"lastModifiedDate":"2012-02-02T00:07:15","indexId":"ofr95143","displayToPublicDate":"1995-09-01T00:00:00","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":"95-143","title":"Hydrogeologic data for the northern Rocky Mountains intermontane basins, Montana","docAbstract":"The U.S. Geological Survey began a Regional Aquifer- System Analysis of the Northern Rocky Mountains Intermontane Basins of western Montana and central and central and northern Idaho in 1990 to establish a regional framework of information for aquifers in 54 intermontane basins in an area of about 77,500 square miles. Selected hydrogeologic data have been used as part of this analysis to define the hydro- logic systems. Records of 1,376 wells completed in 31 of the 34 intermontane basins in the Montana part of the study area are tabulated in this report. Data consist of location, alttiude of land surface, date well constructed, geologic unit, depth of well, diameter of casing, type of finish, top of open interval, primary use of water, water level, date water level measured, discharge, specific capacity, source of discharge data, type of log available, date water-quality parameters measured, specific conductance, pH, and temperature. Hydrographs for selected wells also are included. Locations of wells and basins are shown on the accompanying plate.","language":"ENGLISH","publisher":"U.S. Geological Survey,","doi":"10.3133/ofr95143","usgsCitation":"Dutton, D., Lawlor, S.M., Briar, D., and Tresch, R., 1995, Hydrogeologic data for the northern Rocky Mountains intermontane basins, Montana: U.S. Geological Survey Open-File Report 95-143, iv, 94 p. :ill., maps ;28 cm., https://doi.org/10.3133/ofr95143.","productDescription":"iv, 94 p. :ill., maps ;28 cm.","costCenters":[],"links":[{"id":149311,"rank":0,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/of/1995/0143/report-thumb.jpg"},{"id":46384,"rank":300,"type":{"id":11,"text":"Document"},"url":"https://pubs.usgs.gov/of/1995/0143/report.pdf","linkFileType":{"id":1,"text":"pdf"}}],"noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"4f4e4a4fe4b07f02db628a0a","contributors":{"authors":[{"text":"Dutton, DeAnn M. ddutton@usgs.gov","contributorId":20762,"corporation":false,"usgs":true,"family":"Dutton","given":"DeAnn M.","email":"ddutton@usgs.gov","affiliations":[{"id":5050,"text":"WY-MT Water Science Center","active":true,"usgs":true}],"preferred":false,"id":175539,"contributorType":{"id":1,"text":"Authors"},"rank":1},{"text":"Lawlor, Sean M. 0000-0001-5988-7548 slawlor@usgs.gov","orcid":"https://orcid.org/0000-0001-5988-7548","contributorId":1895,"corporation":false,"usgs":true,"family":"Lawlor","given":"Sean","email":"slawlor@usgs.gov","middleInitial":"M.","affiliations":[{"id":685,"text":"Wyoming-Montana Water Science Center","active":false,"usgs":true}],"preferred":true,"id":175538,"contributorType":{"id":1,"text":"Authors"},"rank":2},{"text":"Briar, D.W.","contributorId":58287,"corporation":false,"usgs":true,"family":"Briar","given":"D.W.","affiliations":[],"preferred":false,"id":175541,"contributorType":{"id":1,"text":"Authors"},"rank":3},{"text":"Tresch, R.E.","contributorId":30646,"corporation":false,"usgs":true,"family":"Tresch","given":"R.E.","email":"","affiliations":[],"preferred":false,"id":175540,"contributorType":{"id":1,"text":"Authors"},"rank":4}]}}
,{"id":29612,"text":"wri934140 - 1995 - Potential for chemical transport beneath a storm-runoff recharge (retention) basin for an industrial catchment in Fresno, California","interactions":[],"lastModifiedDate":"2012-02-02T00:08:56","indexId":"wri934140","displayToPublicDate":"1995-09-01T00:00:00","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":"93-4140","title":"Potential for chemical transport beneath a storm-runoff recharge (retention) basin for an industrial catchment in Fresno, California","docAbstract":"A wide variety of chemicals from urban runoff were found at elevated concentrations in sediment that accumulated in a storm-runoff recharge basin in an industrial part of the city of Fresno. The chemicals include as many as 20 inorganic elements and about the same number of organic compounds, primarily organochlorine pesticides and polycyclic aromatic hydrocarbons. Most of these contaminants were found to be sorbed to the upper 4 centimeters of sediment, which also is the maximum depth to which atmospheric lead-210 penetrated. None of the contaminants were detected above background concentrations in the sediment at depths greater than 16 centimeters. In shallow sediment, zinc is the inorganic element that showed the greatest enrichment; its concentration was 38 times higher in surface sediment (0-1 centimeter) than in deeper strata (below 16 centi- meters). Organic carbon enrichment in the surface sediment was nearly 1,000 times. Although batch- elutriation experiments demonstrated the potential for leaching of contaminants attached to sediments, a sharp decrease in concentrations with increasing sediment depth, and the extremely low level of contaminants in two monitor wells adjacent to the basin, confirmed the absence of contaminant transport to the water table. Continued long-term protection for ground water is afforded by an approximately 8-meter-thick unsaturated zone beneath the basin. On the basis of its hundredfold-higher concentration in the recharge pond then in ground water, zinc is indicated as the most sensitive surrogate for monitoring possible ground-water degradation by inorganic cations.","language":"ENGLISH","publisher":"U.S. Dept. of the Interior, U.S. Geological Survey ;\r\nFor sale by the U.S. Geological Survey, Earth Science Information Center, Open-File Reports Section,","doi":"10.3133/wri934140","usgsCitation":"Schroeder, R.A., 1995, Potential for chemical transport beneath a storm-runoff recharge (retention) basin for an industrial catchment in Fresno, California: U.S. Geological Survey Water-Resources Investigations Report 93-4140, vi, 38 p. :ill., map ;28 cm., https://doi.org/10.3133/wri934140.","productDescription":"vi, 38 p. :ill., map ;28 cm.","costCenters":[],"links":[{"id":123543,"rank":0,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/wri/1993/4140/report-thumb.jpg"},{"id":58435,"rank":300,"type":{"id":11,"text":"Document"},"url":"https://pubs.usgs.gov/wri/1993/4140/report.pdf","linkFileType":{"id":1,"text":"pdf"}}],"noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"4f4e4b06e4b07f02db69a2be","contributors":{"authors":[{"text":"Schroeder, R. A.","contributorId":15554,"corporation":false,"usgs":true,"family":"Schroeder","given":"R.","email":"","middleInitial":"A.","affiliations":[],"preferred":false,"id":201813,"contributorType":{"id":1,"text":"Authors"},"rank":1}]}}
,{"id":17837,"text":"ofr95126 - 1995 - Water-related scientific activities of the U.S. Geological Survey in Nevada, fiscal years 1993-94","interactions":[],"lastModifiedDate":"2012-02-02T00:07:13","indexId":"ofr95126","displayToPublicDate":"1995-09-01T00:00:00","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":"95-126","title":"Water-related scientific activities of the U.S. Geological Survey in Nevada, fiscal years 1993-94","docAbstract":"The U.S. Geological Survey has been collecting water-resources data in Nevada since 1890. Most of the projects that constitute the current Nevada District program can be classified as either basic- data acquisition (about 25 percent) or hydrologic interpretation (about 75 percent). About 39 percent of the activities are supported by cooperative agreements with State and local agencies. Technical projects supported by other Federal agencies make up about 32 percent of the program, and the re- maining 29 percent consists of USGS data collection, interpretive projects, and research. Water con- ditions in most of Nevada during fiscal years 1993 and 1994 continued to be dry, a continuation of drought conditions since late 1986. The major water-resource issues in Nevada include: water allocation in the Truckee River and Carson River Basins; water-supply needs of Las Vegas and the Reno/Sparks area, including water-importation plans; hydrologic effects of weapons testing at the Nevada Test Site; assessment of potential long-term effects of the proposed Yucca Mountain Nuclear Waste Repository; and drought. Future water-resources issues in Nevada are likely to center on water supply for, and environmental effects of, the rapidly growing population centers at Las Vegas, Reno, and Elko; impacts of operations at the Nevada Test Site; management of interstate rivers such as the Truckee, Carson, Walker, and Colorado Rivers; hydrologic and environmental impacts at heavily mined areas; and water-quality management in the Lake Tahoe Basin.","language":"ENGLISH","publisher":"U.S. Geological Survey ;\r\nU.S.G.S. Earth Science Information Center, Open-file Reports Section [distributor],","doi":"10.3133/ofr95126","usgsCitation":"Foglesong, M.T., 1995, Water-related scientific activities of the U.S. Geological Survey in Nevada, fiscal years 1993-94: U.S. Geological Survey Open-File Report 95-126, vii, 69 p. ill., maps ;28 cm., https://doi.org/10.3133/ofr95126.","productDescription":"vii, 69 p. ill., maps ;28 cm.","costCenters":[],"links":[{"id":149512,"rank":0,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/of/1995/0126/report-thumb.jpg"},{"id":47075,"rank":300,"type":{"id":11,"text":"Document"},"url":"https://pubs.usgs.gov/of/1995/0126/report.pdf","linkFileType":{"id":1,"text":"pdf"}}],"noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"4f4e4a08e4b07f02db5fa04a","contributors":{"authors":[{"text":"Foglesong, M. Teresa (compiler)","contributorId":55451,"corporation":false,"usgs":true,"family":"Foglesong","given":"M.","suffix":"(compiler)","email":"","middleInitial":"Teresa","affiliations":[],"preferred":false,"id":178054,"contributorType":{"id":1,"text":"Authors"},"rank":1}]}}
,{"id":31752,"text":"ofr95188 - 1995 - Map showing location of observation wells in Massachusetts and Rhode Island","interactions":[],"lastModifiedDate":"2022-12-02T22:16:07.171275","indexId":"ofr95188","displayToPublicDate":"1995-09-01T00:00:00","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":"95-188","title":"Map showing location of observation wells in Massachusetts and Rhode Island","docAbstract":"This map shows the locations of the 136 observation wells from the observation-well network maintained by the U.S. Geological Survey in Massachusetts and Rhode Island. The wells are identified by town name and well number. The map shows the location of the 10 observation wells that have digital recorders and the 126 observation wells that are measured by local observers. The aquifer material (sand, till, or bedrock) in which a well is located is noted. County and town boundaries are shown on the map. These features are presented at a scale of 1:400,000 (map size is about 38 by 30 inches). The map includes textual information describing the uses of observation-well data. The information is organized by construction, water supply, water quality, and statistical analysis. The map also presents observation well information, which was obtained from the annual data report of the Massachusetts--Rhode Island District. This infor-  mation is presented in tabular form and includes town name, well number, aquifer material in which the well is located, and well depth below the land surface. The map was produced from a digital data base using a Geographic Information System. State boundaries were generated from digital line graphs maintained by the U.S. Geological Survey. Town and county boundaries were digitized from stable-base materials maintained by State agencies. The map was prepared in cooperation with State agencies of Massachusetts and Rhode Island.","language":"English","publisher":"U.S. Geological Survey","doi":"10.3133/ofr95188","usgsCitation":"Rader, J.C., 1995, Map showing location of observation wells in Massachusetts and Rhode Island: U.S. Geological Survey Open-File Report 95-188, 1 Plate: 40.00 × 31.00 inches, https://doi.org/10.3133/ofr95188.","productDescription":"1 Plate: 40.00 × 31.00 inches","costCenters":[],"links":[{"id":160177,"rank":0,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/thumbnails/usgs_thumb.jpg"},{"id":410024,"rank":3,"type":{"id":36,"text":"NGMDB Index Page"},"url":"https://ngmdb.usgs.gov/Prodesc/proddesc_18415.htm","linkFileType":{"id":5,"text":"html"}},{"id":19546,"rank":400,"type":{"id":17,"text":"Plate"},"url":"https://pubs.usgs.gov/of/1995/0188/plate-1.pdf","linkFileType":{"id":1,"text":"pdf"}}],"scale":"400000","country":"United States","state":"Massachusetts, Rhode 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,{"id":19014,"text":"ofr95185 - 1995 - Bibliography of U.S. Geological Survey reports on the water resources of Florida, 1886-1995","interactions":[],"lastModifiedDate":"2012-02-02T00:07:31","indexId":"ofr95185","displayToPublicDate":"1995-09-01T00:00:00","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":"95-185","title":"Bibliography of U.S. Geological Survey reports on the water resources of Florida, 1886-1995","docAbstract":"The U.S. Geological Survey has released a listing of its reports on water resources in Florida for the period 1886-1995. Most of the reports contained in the listing were prepared by the U.S. Geological Survey in cooperation with numerous public agencies in Florida. The compilation has a full bibliographic list of reports arranged alphabetically by senior author. In addition, the reports are indexed by geographic areas and by special topics.","language":"ENGLISH","publisher":"U.S. Dept. of the Interior, U.S. Geological Survey ;\r\nU.S. Geological Survey, Earth Science Information Center, Open-File Reports Section [distributor],","doi":"10.3133/ofr95185","usgsCitation":"Garcia, C.A., and Hoy, N., 1995, Bibliography of U.S. Geological Survey reports on the water resources of Florida, 1886-1995 (6th ed.): U.S. Geological Survey Open-File Report 95-185, iv, 176 p. :map ;28 cm., https://doi.org/10.3133/ofr95185.","productDescription":"iv, 176 p. :map ;28 cm.","costCenters":[],"links":[{"id":151647,"rank":0,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/of/1995/0185/report-thumb.jpg"},{"id":48424,"rank":300,"type":{"id":11,"text":"Document"},"url":"https://pubs.usgs.gov/of/1995/0185/report.pdf","linkFileType":{"id":1,"text":"pdf"}}],"edition":"6th ed.","noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"4f4e4a4ee4b07f02db627d9f","contributors":{"authors":[{"text":"Garcia, Carmen A.","contributorId":10448,"corporation":false,"usgs":true,"family":"Garcia","given":"Carmen","email":"","middleInitial":"A.","affiliations":[],"preferred":false,"id":180147,"contributorType":{"id":1,"text":"Authors"},"rank":1},{"text":"Hoy, N.D.","contributorId":15618,"corporation":false,"usgs":true,"family":"Hoy","given":"N.D.","email":"","affiliations":[],"preferred":false,"id":180148,"contributorType":{"id":1,"text":"Authors"},"rank":2}]}}
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