{"pageNumber":"4863","pageRowStart":"121550","pageSize":"25","recordCount":184569,"records":[{"id":44428,"text":"wri864147 - 1986 - Hydrogeology of the eastern part of the Salt River Valley area, Maricopa and Pinal Counties, Arizona","interactions":[],"lastModifiedDate":"2012-02-02T00:10:32","indexId":"wri864147","displayToPublicDate":"1994-01-01T00:00:00","publicationYear":"1986","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":"86-4147","title":"Hydrogeology of the eastern part of the Salt River Valley area, Maricopa and Pinal Counties, Arizona","docAbstract":"The Salt River Valley is a major agricultural and metropolitan area in semiarid south-central Arizona. Groundwater in the permeable sedimentary deposits underlying the area is a major water supply for agricultural, municipal, and industrial users. Groundwater levels have declined as much as 400 ft in recent years. Management of the remaining groundwater resources and their protection from contamination will require knowledge of the hydrogeologic framework and the water-bearing characteristics of the sedimentary units in the groundwater system. The rocks in the eastern part of the Salt River Valley are divided into six units--crystalline rocks, extrusive rocks, red units, lower unit, middle unit, and upper unit. The crystalline and extrusive rocks underlie the basin and form virtually impermeable hydrologic boundaries. The red, lower, middle and upper sedimentary units contain most of the groundwater. The red unit contains usable quantities of ground water, principally near Scottsdale, where it yields as much as 1 ,000 gallons/min (gpm) of water to wells. The lower unit, which makes up the largest volume of sedimentary deposits, consists mostly of mudstone, clay, silt, and evaporite deposits that may be as much as 10,000 ft thick in the central part of the basin. Wells tapping the mudstone, clay, silt yield 50 (gpm) or less but the conglomerate and the sand and gravel may yield as much as 3,500 gpm. The middle unit is the principal water-bearing unit in the basin and consists mostly of silt, siltstone, and silty sand and gravel. The unit is as much as 1,000 ft thick in the central part of the basin and as much as 700 ft is saturated. The unit will yield as much as 1,000 gpm where the saturated thickness is at least 500 ft. Locally, north of Mesa, the unit yields as much as 4,000 gpm. The upper unit is gravel, sand, and silt and is saturated only in a small area in the southwestern part of the basin. Where saturated, the unit may yield as much as 4,500 gpm. The upper unit transmits recharge derived from sheet flow, from flood flow in ephemeral streams, and from irrigation to the water table. (Author 's abstract)","language":"ENGLISH","doi":"10.3133/wri864147","usgsCitation":"Laney, R., and Hahn, M.E., 1986, Hydrogeology of the eastern part of the Salt River Valley area, Maricopa and Pinal Counties, Arizona: U.S. Geological Survey Water-Resources Investigations Report 86-4147, 8 maps on 4 sheets ; sheets 97 x 86 cm. and smaller, folded in envelope 32 x 25 cm., https://doi.org/10.3133/wri864147.","productDescription":"8 maps on 4 sheets ; sheets 97 x 86 cm. and smaller, folded in envelope 32 x 25 cm.","costCenters":[],"links":[{"id":172360,"rank":0,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/thumbnails/usgs_thumb.jpg"},{"id":81729,"rank":402,"type":{"id":17,"text":"Plate"},"url":"https://pubs.usgs.gov/wri/1986/4147/plate-3.pdf","linkFileType":{"id":1,"text":"pdf"}},{"id":81730,"rank":403,"type":{"id":17,"text":"Plate"},"url":"https://pubs.usgs.gov/wri/1986/4147/plate-4.pdf","linkFileType":{"id":1,"text":"pdf"}},{"id":81727,"rank":400,"type":{"id":17,"text":"Plate"},"url":"https://pubs.usgs.gov/wri/1986/4147/plate-1.pdf","linkFileType":{"id":1,"text":"pdf"}},{"id":81728,"rank":401,"type":{"id":17,"text":"Plate"},"url":"https://pubs.usgs.gov/wri/1986/4147/plate-2.pdf","linkFileType":{"id":1,"text":"pdf"}}],"noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"4f4e4a2ee4b07f02db614e97","contributors":{"authors":[{"text":"Laney, R. L.","contributorId":83889,"corporation":false,"usgs":true,"family":"Laney","given":"R. L.","affiliations":[],"preferred":false,"id":229752,"contributorType":{"id":1,"text":"Authors"},"rank":1},{"text":"Hahn, Mary Ellen","contributorId":83188,"corporation":false,"usgs":true,"family":"Hahn","given":"Mary","email":"","middleInitial":"Ellen","affiliations":[],"preferred":false,"id":229751,"contributorType":{"id":1,"text":"Authors"},"rank":2}]}} ,{"id":44425,"text":"wri864119 - 1986 - Potentiometric surface, ground-water withdrawals, and recharge area for the Nanafalia-Clayton aquifer in Alabama, fall 1982","interactions":[],"lastModifiedDate":"2012-02-02T00:10:31","indexId":"wri864119","displayToPublicDate":"1994-01-01T00:00:00","publicationYear":"1986","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":"86-4119","title":"Potentiometric surface, ground-water withdrawals, and recharge area for the Nanafalia-Clayton aquifer in Alabama, fall 1982","docAbstract":"The U.S. Geological Survey began a nationwide program in 1978, termed Regional Aquifer-System Analysis (RASA), to study a number of the major aquifer systems that provide a significant part of the country 's water supply. One of the aquifer systems chosen for study was the thick and extensive sequence of sands for Cretaceous and early Tertiary age that underlies the Coastal Plain of the southeastern United States. This system, which extends from Mississippi eastward to South Carolina, is called the Southeastern Coastal Plain aquifer system. It can be divided geohydrologically into several separate aquifers. This map, one of a series that portray the potentiometric surface, groundwater withdrawal, and recharge areas for the aquifers in Alabama that are included in the regional system, deals with the Nanafalia-Clayton aquifer. (Lantz-PTT)","language":"ENGLISH","doi":"10.3133/wri864119","usgsCitation":"Williams, J.S., DeJarnette, S.S., and Planert, M., 1986, Potentiometric surface, ground-water withdrawals, and recharge area for the Nanafalia-Clayton aquifer in Alabama, fall 1982: U.S. Geological Survey Water-Resources Investigations Report 86-4119, 1 map : col. ; 55 x 36 cm., on sheet 59 x 97 cm., folded in envelope 31 x 23 cm., https://doi.org/10.3133/wri864119.","productDescription":"1 map : col. ; 55 x 36 cm., on sheet 59 x 97 cm., folded in envelope 31 x 23 cm.","costCenters":[],"links":[{"id":173785,"rank":0,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/thumbnails/usgs_thumb.jpg"},{"id":81724,"rank":400,"type":{"id":17,"text":"Plate"},"url":"https://pubs.usgs.gov/wri/1986/4119/plate-1.pdf","linkFileType":{"id":1,"text":"pdf"}}],"noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"4f4e4ad3e4b07f02db682635","contributors":{"authors":[{"text":"Williams, John S. johnw@usgs.gov","contributorId":329,"corporation":false,"usgs":true,"family":"Williams","given":"John","email":"johnw@usgs.gov","middleInitial":"S.","affiliations":[],"preferred":true,"id":229742,"contributorType":{"id":1,"text":"Authors"},"rank":1},{"text":"DeJarnette, Sydney S.","contributorId":13947,"corporation":false,"usgs":true,"family":"DeJarnette","given":"Sydney","email":"","middleInitial":"S.","affiliations":[],"preferred":false,"id":229743,"contributorType":{"id":1,"text":"Authors"},"rank":2},{"text":"Planert, Michael","contributorId":56659,"corporation":false,"usgs":true,"family":"Planert","given":"Michael","email":"","affiliations":[],"preferred":false,"id":229744,"contributorType":{"id":1,"text":"Authors"},"rank":3}]}} ,{"id":44421,"text":"wri864084 - 1986 - Maps showing altitude of the potentiometric surface and changes in water levels in the aquifer in the Sparta and Memphis Sands in eastern Arkansas, spring 1985","interactions":[],"lastModifiedDate":"2012-02-02T00:10:31","indexId":"wri864084","displayToPublicDate":"1994-01-01T00:00:00","publicationYear":"1986","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":"86-4084","title":"Maps showing altitude of the potentiometric surface and changes in water levels in the aquifer in the Sparta and Memphis Sands in eastern Arkansas, spring 1985","docAbstract":"Aquifers in the Tertiary Sparta and Memphis Sands are a major source of water supply for much of eastern and south-central Arkansas. Major withdrawals occur from the aquifer for industrial and public supply, with generally lesser but locally significant amounts withdrawn for agricultural uses. Water level data from wells tapping the artesian aquifer in the Sparta and Memphis Sands indicate steadily declining water levels in some areas where relatively large withdrawals occur. In addition, a simulation of water levels using projected withdrawals to the year 1990 indicated increasing water level declines in the aquifer. Because of the potential quantity and quality problems, the continual monitoring of water levels in the aquifer in the Sparta and Memphis Sands is essential for proper aquifer management and the continuation of the use of the aquifer as a major source of water for much of eastern and south-central Arkansas. The U.S. Geological Survey with the cooperation of the Arkansas Geological Commission has been monitoring water levels in the aquifer in the Sparta and Memphis Sands annually throughout the aquifer 's extent within the State of Arkansas. This report, prepared in cooperation with the Arkansas Geological Commission and the Arkansas Soil and Water Conservation Commission interprets water level data through hydrologic maps of the potentiometric surface and water level changes. The potentiometric surface map is based on water levels collected in the spring of 1985. The water level change map is based on a comparison of water levels collected in the spring of 1980 and 1985. This report includes the Sparta Sand and most of the Memphis Sand aquifer within the State of Arkansas. Little or no data are available in the northeastern part of the State where limited withdrawals from the aquifer occur. (Lantz-PTT)","language":"ENGLISH","doi":"10.3133/wri864084","usgsCitation":"Edds, J., and Fitzpatrick, D., 1986, Maps showing altitude of the potentiometric surface and changes in water levels in the aquifer in the Sparta and Memphis Sands in eastern Arkansas, spring 1985: U.S. Geological Survey Water-Resources Investigations Report 86-4084, 1 over-sized sheet, https://doi.org/10.3133/wri864084.","productDescription":"1 over-sized sheet","costCenters":[],"links":[{"id":173196,"rank":0,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/thumbnails/usgs_thumb.jpg"},{"id":81720,"rank":400,"type":{"id":17,"text":"Plate"},"url":"https://pubs.usgs.gov/wri/1986/4084/plate-1.pdf","linkFileType":{"id":1,"text":"pdf"}}],"noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"4f4e4a17e4b07f02db60461f","contributors":{"authors":[{"text":"Edds, Joe","contributorId":48532,"corporation":false,"usgs":true,"family":"Edds","given":"Joe","email":"","affiliations":[],"preferred":false,"id":229736,"contributorType":{"id":1,"text":"Authors"},"rank":1},{"text":"Fitzpatrick, D. J.","contributorId":33313,"corporation":false,"usgs":true,"family":"Fitzpatrick","given":"D. J.","affiliations":[],"preferred":false,"id":229735,"contributorType":{"id":1,"text":"Authors"},"rank":2}]}} ,{"id":18584,"text":"ofr8697 - 1986 - A comparison of analytic and simulation methods for petroleum play analysis and aggregation","interactions":[],"lastModifiedDate":"2012-02-02T00:07:29","indexId":"ofr8697","displayToPublicDate":"1994-01-01T00:00:00","publicationYear":"1986","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":"86-97","title":"A comparison of analytic and simulation methods for petroleum play analysis and aggregation","language":"ENGLISH","publisher":"U.S. Geological Survey,","doi":"10.3133/ofr8697","usgsCitation":"Crovelli, R., 1986, A comparison of analytic and simulation methods for petroleum play analysis and aggregation: U.S. Geological Survey Open-File Report 86-97, i, 21 p. ;28 cm., https://doi.org/10.3133/ofr8697.","productDescription":"i, 21 p. ;28 cm.","costCenters":[],"links":[{"id":151887,"rank":0,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/of/1986/0097/report-thumb.jpg"},{"id":47932,"rank":300,"type":{"id":11,"text":"Document"},"url":"https://pubs.usgs.gov/of/1986/0097/report.pdf","linkFileType":{"id":1,"text":"pdf"}}],"noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"4f4e4b27e4b07f02db6b0ffd","contributors":{"authors":[{"text":"Crovelli, R. A.","contributorId":40969,"corporation":false,"usgs":true,"family":"Crovelli","given":"R. A.","affiliations":[],"preferred":false,"id":179388,"contributorType":{"id":1,"text":"Authors"},"rank":1}]}} ,{"id":44410,"text":"wri864201 - 1986 - Ground-water availability in the eastern part of the Lake Ontario Basin, New York","interactions":[],"lastModifiedDate":"2012-02-02T00:10:31","indexId":"wri864201","displayToPublicDate":"1994-01-01T00:00:00","publicationYear":"1986","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":"86-4201","title":"Ground-water availability in the eastern part of the Lake Ontario Basin, New York","docAbstract":"A set of three maps show surficial geology, significant unconsolidated aquifers and well yield, and selected well locations for the Lake Ontario basin, New York. In the low areas , glaciers and wave action of former high-level lakes deposited permeable sand and gravel to form aquifers that yield more than 10 gal/min of water to wells. Small quantities of water (less than 2 gal/min) can be pumped from dug wells that top till and fine lake-sediment deposits. (USGS)","language":"ENGLISH","doi":"10.3133/wri864201","usgsCitation":"Miller, T.S., 1986, Ground-water availability in the eastern part of the Lake Ontario Basin, New York: U.S. Geological Survey Water-Resources Investigations Report 86-4201, 3 maps ; 66 x 66 cm., on sheets 76 x 76 cm. and 76 x 96 cm., folded in envelope 33 x 25 cm., https://doi.org/10.3133/wri864201.","productDescription":"3 maps ; 66 x 66 cm., on sheets 76 x 76 cm. and 76 x 96 cm., folded in envelope 33 x 25 cm.","costCenters":[],"links":[{"id":173688,"rank":0,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/thumbnails/usgs_thumb.jpg"},{"id":81704,"rank":400,"type":{"id":17,"text":"Plate"},"url":"https://pubs.usgs.gov/wri/1986/4201/plate-1.pdf","linkFileType":{"id":1,"text":"pdf"}},{"id":81705,"rank":401,"type":{"id":17,"text":"Plate"},"url":"https://pubs.usgs.gov/wri/1986/4201/plate-2.pdf","linkFileType":{"id":1,"text":"pdf"}},{"id":81706,"rank":402,"type":{"id":17,"text":"Plate"},"url":"https://pubs.usgs.gov/wri/1986/4201/plate-3.pdf","linkFileType":{"id":1,"text":"pdf"}}],"noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"4f4e4aafe4b07f02db66d355","contributors":{"authors":[{"text":"Miller, Todd S. tsmiller@usgs.gov","contributorId":1190,"corporation":false,"usgs":true,"family":"Miller","given":"Todd","email":"tsmiller@usgs.gov","middleInitial":"S.","affiliations":[{"id":474,"text":"New York Water Science Center","active":true,"usgs":true}],"preferred":true,"id":229719,"contributorType":{"id":1,"text":"Authors"},"rank":1}]}} ,{"id":44407,"text":"wri864183 - 1986 - Potentiometric surface of the Floridan aquifer system in the Northwest Florida Water Management District, May 1985","interactions":[],"lastModifiedDate":"2022-02-22T21:54:39.615731","indexId":"wri864183","displayToPublicDate":"1994-01-01T00:00:00","publicationYear":"1986","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":"86-4183","title":"Potentiometric surface of the Floridan aquifer system in the Northwest Florida Water Management District, May 1985","docAbstract":"

The potentiometric surface map of the Floridan aquifer system in the northwest Florida Water Management District depicts the level to which water rose in tightly cased wells that tap the Floridan aquifer system in May 1985. The surface was mapped by determining the altitude of water levels in a network of wells and is represented on maps by contours that connect points of equal altitude. The northwest Florida Water Management District consists of about 12,000 sq mi, including all or part of 16 counties in northwest Florida. The Florida aquifer system is the principal source of freshwater for north Florida.

","language":"English","publisher":"U.S. Geological Survey","doi":"10.3133/wri864183","usgsCitation":"Rosenau, J.C., and Meadows, P.E., 1986, Potentiometric surface of the Floridan aquifer system in the Northwest Florida Water Management District, May 1985: U.S. Geological Survey Water-Resources Investigations Report 86-4183, 1 Plate: 36.00 × 23.81 inches, https://doi.org/10.3133/wri864183.","productDescription":"1 Plate: 36.00 × 23.81 inches","costCenters":[],"links":[{"id":172931,"rank":0,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/thumbnails/usgs_thumb.jpg"},{"id":396288,"rank":3,"type":{"id":36,"text":"NGMDB Index Page"},"url":"https://ngmdb.usgs.gov/Prodesc/proddesc_36606.htm"},{"id":81695,"rank":400,"type":{"id":17,"text":"Plate"},"url":"https://pubs.usgs.gov/wri/1986/4183/plate-1.pdf","linkFileType":{"id":1,"text":"pdf"}}],"country":"United States","state":"Florida","otherGeospatial":"Northwest Florida Water Management District","geographicExtents":"{\n \"type\": \"FeatureCollection\",\n \"features\": [\n {\n \"type\": \"Feature\",\n \"properties\": {},\n \"geometry\": {\n \"type\": \"Polygon\",\n \"coordinates\": [\n [\n [\n -88.1982421875,\n 29.611670115197377\n ],\n [\n -83.8916015625,\n 29.611670115197377\n ],\n [\n -83.8916015625,\n 31.840232667909365\n ],\n [\n -88.1982421875,\n 31.840232667909365\n ],\n [\n -88.1982421875,\n 29.611670115197377\n ]\n ]\n ]\n }\n }\n ]\n}","noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"4f4e4ad4e4b07f02db682f49","contributors":{"authors":[{"text":"Rosenau, Jack C.","contributorId":88719,"corporation":false,"usgs":true,"family":"Rosenau","given":"Jack","email":"","middleInitial":"C.","affiliations":[],"preferred":false,"id":229715,"contributorType":{"id":1,"text":"Authors"},"rank":1},{"text":"Meadows, Paul E.","contributorId":101631,"corporation":false,"usgs":true,"family":"Meadows","given":"Paul","email":"","middleInitial":"E.","affiliations":[],"preferred":false,"id":229716,"contributorType":{"id":1,"text":"Authors"},"rank":2}]}} ,{"id":28536,"text":"wri864072 - 1986 - Evaluation of the U.S. Geological Survey's gaging-station network in Illinois","interactions":[],"lastModifiedDate":"2012-02-02T00:08:48","indexId":"wri864072","displayToPublicDate":"1994-01-01T00:00:00","publicationYear":"1986","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":"86-4072","title":"Evaluation of the U.S. Geological Survey's gaging-station network in Illinois","docAbstract":"Data collected at 97 of the 176 gaging stations operated in Illinois during 1983 were used to describe rainfall-runoff processes, to monitor and forecast floods, and to monitor and regulate lake levels, discharge from reservoirs, or discharge of navigable streams. Stream-gaging stations on the Illinois River at Havana, East Branch Du Page River, and interior streams of the Mississippi River floodplain; peak-flow stations on small watersheds; and stage-only stations upstream from unsafe high-hazard dams should be considered for inclusion in future stream-gaging programs. The accuracy of regression models for peak-flow and 1-day mean flood-volume characteristics would not be considerably improved if the density of gaging stations and length of record at those gaging stations are increased. Model error masks tradeoffs between accuracy, density, and record length. The large number of streamflow records presently available is sufficient for fairly accurately determining most streamflow characteristics. The accuracy of streamflow records reported for stream gaging stations and peak-flow stations varies widely. The accuracy of streamflow records for 12 stream-gaging stations and 11 peak-flow stations is substantially less than the accuracy of records for the other 143 gaging stations considered. Based on an evaluation of relative worth, 26 gaging stations are candidates for some type of action if budgetary limitations so demand. A candidate stream-gaging stations could be operated during only part of a year, converted to a peak-flow station, or discontinued. Candidate peak-flow stations should be discontinued. (USGS)","language":"ENGLISH","publisher":"U.S. Geological Survey, Water Resources Division,","doi":"10.3133/wri864072","usgsCitation":"Mades, D., and Oberg, K.A., 1986, Evaluation of the U.S. Geological Survey's gaging-station network in Illinois: U.S. Geological Survey Water-Resources Investigations Report 86-4072, vii, 88 p. :ill., maps ;28 cm., https://doi.org/10.3133/wri864072.","productDescription":"vii, 88 p. :ill., maps ;28 cm.","costCenters":[],"links":[{"id":124298,"rank":0,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/wri/1986/4072/report-thumb.jpg"},{"id":57349,"rank":300,"type":{"id":11,"text":"Document"},"url":"https://pubs.usgs.gov/wri/1986/4072/report.pdf","linkFileType":{"id":1,"text":"pdf"}}],"noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"4f4e4a08e4b07f02db5fa4c2","contributors":{"authors":[{"text":"Mades, D. M.","contributorId":40230,"corporation":false,"usgs":true,"family":"Mades","given":"D. M.","affiliations":[],"preferred":false,"id":199981,"contributorType":{"id":1,"text":"Authors"},"rank":1},{"text":"Oberg, K. A.","contributorId":67553,"corporation":false,"usgs":true,"family":"Oberg","given":"K.","email":"","middleInitial":"A.","affiliations":[],"preferred":false,"id":199982,"contributorType":{"id":1,"text":"Authors"},"rank":2}]}} ,{"id":27327,"text":"wri864044 - 1986 - Hydrologic conditions in Connors Bog Area, Anchorage, Alaska","interactions":[],"lastModifiedDate":"2012-02-02T00:08:42","indexId":"wri864044","displayToPublicDate":"1994-01-01T00:00:00","publicationYear":"1986","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":"86-4044","title":"Hydrologic conditions in Connors Bog Area, Anchorage, Alaska","docAbstract":"Connors Bog is a wetland in Anchorage, Alaska, which provides a habitat for many wildlife species and is a popular area for driving off-road vehicles. A landfill, and residential and commercial developments are present in areas which were once wetland. The main source of water is precipitation, which averages about 15 in/yr. Estimates of evapotranspiration, which is the main component of water outflow, range from 10 to 20 in/yr. Minor amounts of groundwater and surface runoff flow into the area from the northeast and southwest and flow out of the area to the northwest and south. Within the wetland, water in peat and sand is unconfined and becomes more mineralized with depth. A leachate beneath and near an abandoned landfill is characterized by concentrations of dissolved solids, dissolved chloride, and total organics that are higher than those of the area 's natural water. The maximum lateral extent of detectable contamination in 1984 was < 500 ft from the landfill 's edge. Water in glacial deposits that underlie a poorly permeable layer of silt and clay is confined. A well completed in this confined aquifer yielded water that had a low concentration of dissolved solids, 150 mg/L. The potentiometric surface of this aquifer was about 20 ft lower than the water table during 1984. Connors Lake occupies a depression that extends below adjacent groundwater levels. The 40-acre lake has a maximum depth of about 9 ft and a low rate of biological production. The quality of water in the lake has not been adversely impacted by nearby residential development or landfill operations. Lake levels appear to be influenced by precipitation and adjacent groundwater levels. (Author 's abstract)","language":"ENGLISH","publisher":"U.S. Geological Survey,","doi":"10.3133/wri864044","usgsCitation":"Glass, R.L., 1986, Hydrologic conditions in Connors Bog Area, Anchorage, Alaska: U.S. Geological Survey Water-Resources Investigations Report 86-4044, iii, 23 p. :ill., maps ;28 cm., https://doi.org/10.3133/wri864044.","productDescription":"iii, 23 p. :ill., maps ;28 cm.","costCenters":[],"links":[{"id":123776,"rank":0,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/wri/1986/4044/report-thumb.jpg"},{"id":56194,"rank":300,"type":{"id":11,"text":"Document"},"url":"https://pubs.usgs.gov/wri/1986/4044/report.pdf","linkFileType":{"id":1,"text":"pdf"}}],"noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"4f4e4a28e4b07f02db6113e8","contributors":{"authors":[{"text":"Glass, R. L.","contributorId":80279,"corporation":false,"usgs":true,"family":"Glass","given":"R.","email":"","middleInitial":"L.","affiliations":[],"preferred":false,"id":197925,"contributorType":{"id":1,"text":"Authors"},"rank":1}]}} ,{"id":1185,"text":"wsp2289 - 1986 - Artesian pressures and water quality in Paleozoic aquifers in the Ten Sleep area of the Bighorn Basin, north-central Wyoming","interactions":[{"subject":{"id":13161,"text":"ofr84621 - 1985 - Artesian pressures and water quality in Paleozoic aquifers in the Ten Sleep area of the Bighorn Basin, north-central Wyoming","indexId":"ofr84621","publicationYear":"1985","noYear":false,"title":"Artesian pressures and water quality in Paleozoic aquifers in the Ten Sleep area of the Bighorn Basin, north-central Wyoming"},"predicate":"SUPERSEDED_BY","object":{"id":1185,"text":"wsp2289 - 1986 - Artesian pressures and water quality in Paleozoic aquifers in the Ten Sleep area of the Bighorn Basin, north-central Wyoming","indexId":"wsp2289","publicationYear":"1986","noYear":false,"title":"Artesian pressures and water quality in Paleozoic aquifers in the Ten Sleep area of the Bighorn Basin, north-central Wyoming"},"id":1}],"lastModifiedDate":"2012-02-02T00:05:16","indexId":"wsp2289","displayToPublicDate":"1994-01-01T00:00:00","publicationYear":"1986","noYear":false,"publicationType":{"id":18,"text":"Report"},"publicationSubtype":{"id":5,"text":"USGS Numbered Series"},"seriesTitle":{"id":341,"text":"Water Supply Paper","code":"WSP","active":false,"publicationSubtype":{"id":5}},"seriesNumber":"2289","title":"Artesian pressures and water quality in Paleozoic aquifers in the Ten Sleep area of the Bighorn Basin, north-central Wyoming","docAbstract":"The major Paleozoic artesian aquifers, the aquifers most favorable for continued development, in the Ten Sleep area of the Bighorn Basin of Wyoming are the Tensleep Sandstone, the Madison Limestone and Bighorn Dolomite (Madison-Bighorn aquifer), and the Flathead Sandstone. The minor aquifers include the Goose Egg and Park City Formations (considered in the Ten Sleep area to be the lateral equivalent of the Phosphoria Formation) and the Amsden Formation. Most wells completed in the major and minor aquifers flow at the land surface. Wellhead pressures generally are less than 50 pounds per square inch for the Tensleep Sandstone, 150-250 pounds per square inch for the Madison-Bighorn aquifer, and more than 400 pounds per square inch for the Flathead Sandstone. Flowing wells completed in the Madison-Bighorn aquifer and the Flathead Sandstone yield more than 1,000 gallons per minute. The initial test of one well completed in the Madison-Bighorn aquifer indicated a flow rate of 14,000 gallons per minute. Transmissivities range from 500 to 1,900 feet squared per day for the Madison-Bighorn aquifer and from about 90 to 325 feet squared per day for the Tensleep and Flathead Sandstones. \r\n\r\nSignificant secondary permeability from fracturing in the Paleozoic aquifers allows local upward interformational movement of water, and this affects the altitude of the potentiometric surfaces of the Tensleep Sandstone and the Madison-Bighorn aquifer. Water moves upward from the Tensleep and other formations, through the Goose Egg Formation, to discharge at the land surface as springs. Much of the spring flow is diverted for irrigation or is used for rearing fish. \r\n\r\nDecreases from original well pressures were not apparent in wells completed in the Tensleep Sandstone or in the Madison-Bighorn aquifer in the study area except for a few wells in or near the town of Ten Sleep. Most wells completed in the Flathead Sandstone, which also are open to the Madison-Bighorn aquifer, show a decrease of pressure from the time of completion to 1978. The decrease of pressure is partly the result of water moving from the Flathead Sandstone into the Madison-Bighorn aquifer, which has a lower potentiometric surface than does the Flathead Sandstone, even during the time the wells are not in operation. Pressure in some small-capacity wells completed in the Goose Egg Formation also has decreased near Ten Sleep. Most of the wells, particularly the irrigation wells, show a progressive decrease in pressure during the irrigation season but recover during periods of nonuse. Measurements of the pressure were made principally in 1953, 1962, 1970, and 1975-78. \r\n\r\nWell water from the Paleozoic aquifers generally contains minimal concentrations of dissolved solids and individual constituents but excessive hardness. Dissolved-solids concentrations of water are less than 300 milligrams per liter in the Tensleep Sandstone and the Madison-Bighorn aquifer, less than 200 milligrams per liter in the Flathead Sandstone, and as much as 450 milligrams per liter in the Goose Egg Formation. Bicarbonate is the major constituent, followed by calcium and magnesium. Relatively large concentrations of sulfate, as much as 490 milligrams per liter, were found, mainly in water from the Goose Egg Formation. The water has low sodium (alkali) and medium salinity; therefore, the water is satisfactory for irrigation and most other uses, if excessive hardness is not a detrimental factor. \r\n\r\nWellhead temperatures range from 11 ? to 27.5 ? Celsius (51 ? to 81.5 ? Fahrenheit) within a range in depth of approximately 250 to 4,000 feet. This gives a geothermal gradient of about 0.44 ? Celsius per 100 feet (0.79 ? Fahrenheit per 100 feet).","language":"ENGLISH","publisher":"U.S. G.P.O.,","doi":"10.3133/wsp2289","usgsCitation":"Cooley, M.E., 1986, Artesian pressures and water quality in Paleozoic aquifers in the Ten Sleep area of the Bighorn Basin, north-central Wyoming: U.S. Geological Survey Water Supply Paper 2289, iv, 54 p. :ill., maps ;28 cm.; 5 plates in pocket, https://doi.org/10.3133/wsp2289.","productDescription":"iv, 54 p. :ill., maps ;28 cm.; 5 plates in pocket","costCenters":[],"links":[{"id":138030,"rank":0,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/wsp/2289/report-thumb.jpg"},{"id":26042,"rank":400,"type":{"id":17,"text":"Plate"},"url":"https://pubs.usgs.gov/wsp/2289/plate-1.pdf","linkFileType":{"id":1,"text":"pdf"}},{"id":26043,"rank":401,"type":{"id":17,"text":"Plate"},"url":"https://pubs.usgs.gov/wsp/2289/plate-2.pdf","linkFileType":{"id":1,"text":"pdf"}},{"id":26044,"rank":402,"type":{"id":17,"text":"Plate"},"url":"https://pubs.usgs.gov/wsp/2289/plate-3.pdf","linkFileType":{"id":1,"text":"pdf"}},{"id":26045,"rank":403,"type":{"id":17,"text":"Plate"},"url":"https://pubs.usgs.gov/wsp/2289/plate-4.pdf","linkFileType":{"id":1,"text":"pdf"}},{"id":26046,"rank":404,"type":{"id":17,"text":"Plate"},"url":"https://pubs.usgs.gov/wsp/2289/plate-5.pdf","linkFileType":{"id":1,"text":"pdf"}},{"id":26047,"rank":300,"type":{"id":11,"text":"Document"},"url":"https://pubs.usgs.gov/wsp/2289/report.pdf","linkFileType":{"id":1,"text":"pdf"}}],"noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"4f4e48c9e4b07f02db542320","contributors":{"authors":[{"text":"Cooley, Maurice E.","contributorId":8077,"corporation":false,"usgs":true,"family":"Cooley","given":"Maurice","email":"","middleInitial":"E.","affiliations":[],"preferred":false,"id":143318,"contributorType":{"id":1,"text":"Authors"},"rank":1}]}} ,{"id":43544,"text":"ofr8612 - 1986 - Land use and land cover and associated maps for Greenwood, Mississippi; Arkansas; Louisiana","interactions":[],"lastModifiedDate":"2012-02-02T00:10:28","indexId":"ofr8612","displayToPublicDate":"1994-01-01T00:00:00","publicationYear":"1986","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":"86-12","title":"Land use and land cover and associated maps for Greenwood, Mississippi; Arkansas; Louisiana","language":"ENGLISH","doi":"10.3133/ofr8612","usgsCitation":"Water Resources Division, U.S. Geological Survey, 1986, Land use and land cover and associated maps for Greenwood, Mississippi; Arkansas; Louisiana: U.S. Geological Survey Open-File Report 86-12, maps :photocopy ;56 x 92 cm., on sheet 76 x 107 cm., https://doi.org/10.3133/ofr8612.","productDescription":"maps :photocopy ;56 x 92 cm., on sheet 76 x 107 cm.","costCenters":[],"links":[{"id":173751,"rank":0,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/thumbnails/usgs_thumb.jpg"}],"noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"4f4e4b28e4b07f02db6b112c","contributors":{"authors":[{"text":"Water Resources Division, U.S. Geological Survey","contributorId":128075,"corporation":true,"usgs":false,"organization":"Water Resources Division, U.S. Geological Survey","id":531230,"contributorType":{"id":1,"text":"Authors"},"rank":1}]}} ,{"id":48941,"text":"ofr86240 - 1986 - Confined-drift aquifers in Minnesota","interactions":[],"lastModifiedDate":"2018-03-12T10:25:53","indexId":"ofr86240","displayToPublicDate":"1994-01-01T00:00:00","publicationYear":"1986","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":"86-240","title":"Confined-drift aquifers in Minnesota","docAbstract":"

No abstract available.

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In order to assess potential flood hazards, monitor channel adjustments, and construct a sediment budget for disturbed drainages on the east and southeast flanks of the volcano, channel cross sections were monumented and surveyed on Pine Creek, Muddy River, and Smith Creek during September and October of 1980. Additional cross sections were monumented and surveyed on Swift Creek, Bean Creek , and Clearwater Creek during 1981. This network of channel cross sections has been resurveyed annually. Selected cross sections have been surveyed more frequently, following periods of higher flow. Longitudinal stream profiles of the low-water thalweg and (or) water surfaces were surveyed periodically for selected short reaches of channel. Corresponding map views for these reaches were constructed using the survey data and aerial photographs. This report presents plots of channel cross-section profiles, longitudinal stream profiles, and channel maps constructed from survey data collected during water years 1983-84. (USGS)","language":"ENGLISH","publisher":"U.S. Geological Survey,","doi":"10.3133/ofr85631","usgsCitation":"Martinson, H.A., Hammond, H., Mast, W., and Mango, P., 1986, Channel geometry and hydrologic data for six eruption-affected tributaries of the Lewis River, Mount St. Helens, Washington, water years 1983-84: U.S. Geological Survey Open-File Report 85-631, v, 161 p. :ill., maps ;28 cm., https://doi.org/10.3133/ofr85631.","productDescription":"v, 161 p. :ill., maps ;28 cm.","costCenters":[],"links":[{"id":143714,"rank":0,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/of/1985/0631/report-thumb.jpg"},{"id":39963,"rank":300,"type":{"id":11,"text":"Document"},"url":"https://pubs.usgs.gov/of/1985/0631/report.pdf","linkFileType":{"id":1,"text":"pdf"}}],"noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"4f4e49e4e4b07f02db5e62ad","contributors":{"authors":[{"text":"Martinson, H. 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Research on the hydrology of the Cottonwood Lake area, Stutsman County, North Dakota, includes study of evaporation. Presented here are those climatic data needed for energy-budget and mass-transfer evaporation studies, including: water-surface temperature, sediment 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 were collected at raft and land stations.

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Plant species were identified and dry weight determined for selected sites. Information on competition between Hydrilla verticillata and other species was measured. Water-quality characteristics measured include temperature, specific conductance, dissolved oxygen, pH, and transparency as indicated by Secchi depth. A map was made of the distribution of submersed aquatic vegetation based on transect samples and a complete shoreline survey. (USGS)","language":"ENGLISH","publisher":"U.S. Geological Survey,","doi":"10.3133/ofr86126","usgsCitation":"Rybicki, N.B., Anderson, R.T., Shapiro, J., Jones, C., and Carter, V., 1986, Data on the distribution and abundance of submersed aquatic vegetation in the tidal Potomac River, Maryland, Virginia, and the District of Columbia, 1985: U.S. Geological Survey Open-File Report 86-126, iii, 49 p. :maps ;28 cm., https://doi.org/10.3133/ofr86126.","productDescription":"iii, 49 p. :maps ;28 cm.","costCenters":[],"links":[{"id":145642,"rank":0,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/of/1986/0126/report-thumb.jpg"},{"id":39994,"rank":300,"type":{"id":11,"text":"Document"},"url":"https://pubs.usgs.gov/of/1986/0126/report.pdf","linkFileType":{"id":1,"text":"pdf"}}],"noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"4f4e4ac9e4b07f02db67c6c6","contributors":{"authors":[{"text":"Rybicki, N. B.","contributorId":97504,"corporation":false,"usgs":true,"family":"Rybicki","given":"N.","email":"","middleInitial":"B.","affiliations":[],"preferred":false,"id":164609,"contributorType":{"id":1,"text":"Authors"},"rank":1},{"text":"Anderson, R. T.","contributorId":17614,"corporation":false,"usgs":true,"family":"Anderson","given":"R.","email":"","middleInitial":"T.","affiliations":[],"preferred":false,"id":164606,"contributorType":{"id":1,"text":"Authors"},"rank":2},{"text":"Shapiro, J.M.","contributorId":47376,"corporation":false,"usgs":true,"family":"Shapiro","given":"J.M.","email":"","affiliations":[],"preferred":false,"id":164607,"contributorType":{"id":1,"text":"Authors"},"rank":3},{"text":"Jones, C.L.","contributorId":60218,"corporation":false,"usgs":true,"family":"Jones","given":"C.L.","email":"","affiliations":[],"preferred":false,"id":164608,"contributorType":{"id":1,"text":"Authors"},"rank":4},{"text":"Carter, Virginia","contributorId":12018,"corporation":false,"usgs":true,"family":"Carter","given":"Virginia","email":"","affiliations":[],"preferred":false,"id":164605,"contributorType":{"id":1,"text":"Authors"},"rank":5}]}} ,{"id":12005,"text":"ofr86403W - 1986 - Data on the solute concentration within the subsurface flows of Little Lost Man Creek in response to a transport experiment, Redwood National Park, northwest California","interactions":[],"lastModifiedDate":"2012-02-02T00:06:35","indexId":"ofr86403W","displayToPublicDate":"1994-01-01T00:00:00","publicationYear":"1986","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":"86-403","chapter":"W","title":"Data on the solute concentration within the subsurface flows of Little Lost Man Creek in response to a transport experiment, Redwood National Park, northwest California","docAbstract":"A solute transport experiment was conducted on a 327-m reach of Little Lost Man Creek, a small stream in Humboldt County, California. Solutes were injected for 20 days. Chloride was used as a conservative tracer; lithium, potassium, and strontium were used as reactive tracers. In addition, nitrate and phosphate were added as biological reactants. Eighteen shallow wells were dug along the length of the study reach, 1-10 m laterally from the edge of the stream. The wells and sites in the stream were monitored for the injected solutes during and after the injection. Solute concentrations in the wells and stream are indicative of transport properties of stream and subsurface channel flow. This report presents the results of the analyses of the well samples and chemical data relevant to the interpretation of hydrological and chemical interaction between the stream and adjacent channel subsurface flows in the streambed. Calculations of the percentage of streamwater in the wellwater were made from conservative tracer measurements. The composition of wellwater ranged from 47% to 100% streamwater with most values above 90%. The time for water to travel from the beginning of the study reach to the wells was approximately three times as great as the travel time in the stream at the same distance down the reach. The three conclusions that can be drawn are (1) water in the stream exchanges extensively with water in the rest of the channel; (2) the interstitial water in the channel gravels achieves almost the same composition as the stream; and (3) under low flow conditions the stream gravels contain a significant portion of the stream volume. Plots of normalized chloride, lithium, and strontium concentrations at three stream sites are included. (Author 's abstract)","language":"ENGLISH","publisher":"U.S. Geological Survey,","doi":"10.3133/ofr86403W","usgsCitation":"Zellweger, G.W., Kennedy, V.C., Bencala, K., Avanzino, R., Jackman, A.P., and Triska, F., 1986, Data on the solute concentration within the subsurface flows of Little Lost Man Creek in response to a transport experiment, Redwood National Park, northwest California: U.S. Geological Survey Open-File Report 86-403, 69 p.; 1 v. (various foliations) :ill., map ;28 cm., https://doi.org/10.3133/ofr86403W.","productDescription":"69 p.; 1 v. (various foliations) :ill., map ;28 cm.","costCenters":[],"links":[{"id":145087,"rank":0,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/of/1986/0403w/report-thumb.jpg"},{"id":39998,"rank":300,"type":{"id":11,"text":"Document"},"url":"https://pubs.usgs.gov/of/1986/0403w/report.pdf","linkFileType":{"id":1,"text":"pdf"}}],"noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"4f4e4ac7e4b07f02db67b1fb","contributors":{"authors":[{"text":"Zellweger, Gary W.","contributorId":71171,"corporation":false,"usgs":true,"family":"Zellweger","given":"Gary","email":"","middleInitial":"W.","affiliations":[],"preferred":false,"id":164636,"contributorType":{"id":1,"text":"Authors"},"rank":1},{"text":"Kennedy, V. C.","contributorId":46080,"corporation":false,"usgs":true,"family":"Kennedy","given":"V.","email":"","middleInitial":"C.","affiliations":[],"preferred":false,"id":164633,"contributorType":{"id":1,"text":"Authors"},"rank":2},{"text":"Bencala, K.E.","contributorId":105312,"corporation":false,"usgs":true,"family":"Bencala","given":"K.E.","email":"","affiliations":[],"preferred":false,"id":164637,"contributorType":{"id":1,"text":"Authors"},"rank":3},{"text":"Avanzino, R.J.","contributorId":37336,"corporation":false,"usgs":true,"family":"Avanzino","given":"R.J.","affiliations":[],"preferred":false,"id":164632,"contributorType":{"id":1,"text":"Authors"},"rank":4},{"text":"Jackman, A. P.","contributorId":46957,"corporation":false,"usgs":true,"family":"Jackman","given":"A.","email":"","middleInitial":"P.","affiliations":[],"preferred":false,"id":164634,"contributorType":{"id":1,"text":"Authors"},"rank":5},{"text":"Triska, F.J.","contributorId":69560,"corporation":false,"usgs":true,"family":"Triska","given":"F.J.","email":"","affiliations":[],"preferred":false,"id":164635,"contributorType":{"id":1,"text":"Authors"},"rank":6}]}} ,{"id":11905,"text":"ofr86586 - 1986 - Analytical results and sample locality map of stream-sediment and heavy-mineral-concentrate samples from the Mt. Katmai quadrangle, and portions of the Naknek, Afognak, and Iliamna quadrangles, Alaska","interactions":[],"lastModifiedDate":"2022-07-22T21:47:25.881646","indexId":"ofr86586","displayToPublicDate":"1994-01-01T00:00:00","publicationYear":"1986","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":"86-586","title":"Analytical results and sample locality map of stream-sediment and heavy-mineral-concentrate samples from the Mt. Katmai quadrangle, and portions of the Naknek, Afognak, and Iliamna quadrangles, Alaska","docAbstract":"

No abstract available.

","language":"English","publisher":"U.S. Geological Survey","doi":"10.3133/ofr86586","usgsCitation":"Bailey, E., Sutley, S.J., Arbogast, B., Willson, W.R., and Church, S.E., 1986, Analytical results and sample locality map of stream-sediment and heavy-mineral-concentrate samples from the Mt. Katmai quadrangle, and portions of the Naknek, Afognak, and Iliamna quadrangles, Alaska: U.S. Geological Survey Open-File Report 86-586, Report: 126 p.; 1 Plate: 47.93 × 26.88 inches, https://doi.org/10.3133/ofr86586.","productDescription":"Report: 126 p.; 1 Plate: 47.93 × 26.88 inches","costCenters":[],"links":[{"id":404399,"rank":4,"type":{"id":36,"text":"NGMDB Index Page"},"url":"https://ngmdb.usgs.gov/Prodesc/proddesc_19018.htm","linkFileType":{"id":5,"text":"html"}},{"id":39846,"rank":300,"type":{"id":11,"text":"Document"},"url":"https://pubs.usgs.gov/of/1986/0586/report.pdf","linkFileType":{"id":1,"text":"pdf"}},{"id":39845,"rank":400,"type":{"id":17,"text":"Plate"},"url":"https://pubs.usgs.gov/of/1986/0586/plate-1.pdf","linkFileType":{"id":1,"text":"pdf"}},{"id":145415,"rank":0,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/of/1986/0586/report-thumb.jpg"}],"country":"United States","state":"Alaska","otherGeospatial":"Mt. Katmai quadrangle and portions of the Naknek, Afognak, and Iliamna quadrangles","geographicExtents":"{\n \"type\": \"FeatureCollection\",\n \"features\": [\n {\n \"type\": \"Feature\",\n \"properties\": {},\n \"geometry\": {\n \"type\": \"Polygon\",\n \"coordinates\": [\n [\n [\n -158,\n 58\n ],\n [\n -153,\n 58\n ],\n [\n -153,\n 59.25\n ],\n [\n -158,\n 59.25\n ],\n [\n -158,\n 58\n ]\n ]\n ]\n }\n }\n ]\n}","noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"4f4e4acce4b07f02db67ec7b","contributors":{"authors":[{"text":"Bailey, E. A.","contributorId":100399,"corporation":false,"usgs":true,"family":"Bailey","given":"E. A.","affiliations":[],"preferred":false,"id":164153,"contributorType":{"id":1,"text":"Authors"},"rank":1},{"text":"Sutley, S. J.","contributorId":91484,"corporation":false,"usgs":true,"family":"Sutley","given":"S.","email":"","middleInitial":"J.","affiliations":[],"preferred":false,"id":164152,"contributorType":{"id":1,"text":"Authors"},"rank":2},{"text":"Arbogast, B. F.","contributorId":60623,"corporation":false,"usgs":true,"family":"Arbogast","given":"B. F.","affiliations":[],"preferred":false,"id":164151,"contributorType":{"id":1,"text":"Authors"},"rank":3},{"text":"Willson, W. R.","contributorId":18358,"corporation":false,"usgs":true,"family":"Willson","given":"W.","email":"","middleInitial":"R.","affiliations":[],"preferred":false,"id":164149,"contributorType":{"id":1,"text":"Authors"},"rank":4},{"text":"Church, S. E.","contributorId":58260,"corporation":false,"usgs":true,"family":"Church","given":"S.","email":"","middleInitial":"E.","affiliations":[],"preferred":false,"id":164150,"contributorType":{"id":1,"text":"Authors"},"rank":5}]}} ,{"id":11901,"text":"ofr86204 - 1986 - Analytical results and sample locality map of stream-sediment and heavy-mineral-concentrate samples from the Circle quadrangle, Alaska","interactions":[],"lastModifiedDate":"2022-09-15T20:32:59.429479","indexId":"ofr86204","displayToPublicDate":"1994-01-01T00:00:00","publicationYear":"1986","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":"86-204","title":"Analytical results and sample locality map of stream-sediment and heavy-mineral-concentrate samples from the Circle quadrangle, Alaska","docAbstract":"

No abstract available.

","language":"English","publisher":"U.S. Geological Survey","doi":"10.3133/ofr86204","usgsCitation":"O'Leary, R., Hoffmann, J.D., Risoli, D., and Tripp, R.B., 1986, Analytical results and sample locality map of stream-sediment and heavy-mineral-concentrate samples from the Circle quadrangle, Alaska: U.S. Geological Survey Open-File Report 86-204, Report: 124 p.; 1 Plate: 24.36 × 23.28 inches, https://doi.org/10.3133/ofr86204.","productDescription":"Report: 124 p.; 1 Plate: 24.36 × 23.28 inches","costCenters":[],"links":[{"id":406791,"rank":4,"type":{"id":36,"text":"NGMDB Index Page"},"url":"https://ngmdb.usgs.gov/Prodesc/proddesc_19005.htm","linkFileType":{"id":5,"text":"html"}},{"id":39838,"rank":300,"type":{"id":11,"text":"Document"},"url":"https://pubs.usgs.gov/of/1986/0204/report.pdf","linkFileType":{"id":1,"text":"pdf"}},{"id":39837,"rank":400,"type":{"id":17,"text":"Plate"},"url":"https://pubs.usgs.gov/of/1986/0204/plate-1.pdf","linkFileType":{"id":1,"text":"pdf"}},{"id":145389,"rank":0,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/of/1986/0204/report-thumb.jpg"}],"country":"United States","state":"Alaska","otherGeospatial":"Circle quadrangle","geographicExtents":"{\n \"type\": \"FeatureCollection\",\n \"features\": [\n {\n \"type\": \"Feature\",\n \"properties\": {},\n \"geometry\": {\n \"type\": \"Polygon\",\n \"coordinates\": [\n [\n [\n -147,\n 65\n ],\n [\n -144,\n 65\n ],\n [\n -144,\n 66\n ],\n [\n -147,\n 66\n ],\n [\n -147,\n 65\n ]\n ]\n ]\n }\n }\n ]\n}","noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"4f4e4acce4b07f02db67e5fd","contributors":{"authors":[{"text":"O'Leary, Richard","contributorId":57463,"corporation":false,"usgs":true,"family":"O'Leary","given":"Richard","affiliations":[],"preferred":false,"id":164134,"contributorType":{"id":1,"text":"Authors"},"rank":1},{"text":"Hoffmann, J. D.","contributorId":53808,"corporation":false,"usgs":true,"family":"Hoffmann","given":"J.","email":"","middleInitial":"D.","affiliations":[],"preferred":false,"id":164133,"contributorType":{"id":1,"text":"Authors"},"rank":2},{"text":"Risoli, D. A.","contributorId":48156,"corporation":false,"usgs":true,"family":"Risoli","given":"D. A.","affiliations":[],"preferred":false,"id":164132,"contributorType":{"id":1,"text":"Authors"},"rank":3},{"text":"Tripp, R. B.","contributorId":88707,"corporation":false,"usgs":true,"family":"Tripp","given":"R.","middleInitial":"B.","affiliations":[],"preferred":false,"id":164135,"contributorType":{"id":1,"text":"Authors"},"rank":4}]}} ,{"id":11895,"text":"ofr86422 - 1986 - Analytical results and sample locality map of nonmagnetic and moderately magnetic heavy-mineral concentrates from stream sediments from the Glens Falls 1° x 2° quadrangle, New York, Vermont, and New Hampshire","interactions":[],"lastModifiedDate":"2021-09-23T19:00:42.750759","indexId":"ofr86422","displayToPublicDate":"1994-01-01T00:00:00","publicationYear":"1986","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":"86-422","title":"Analytical results and sample locality map of nonmagnetic and moderately magnetic heavy-mineral concentrates from stream sediments from the Glens Falls 1° x 2° quadrangle, New York, Vermont, and New Hampshire","docAbstract":"

No abstract available.

","language":"English","publisher":"U.S. Geological Survey,","doi":"10.3133/ofr86422","usgsCitation":"Day, G., Welsch, E.P., Watts, K.C., and Gray, J., 1986, Analytical results and sample locality map of nonmagnetic and moderately magnetic heavy-mineral concentrates from stream sediments from the Glens Falls 1° x 2° quadrangle, New York, Vermont, and New Hampshire: U.S. Geological Survey Open-File Report 86-422, Report: 112 p.; 2 Plates: 26.96 × 22.12 inches and 27.08 × 22.08 inches, https://doi.org/10.3133/ofr86422.","productDescription":"Report: 112 p.; 2 Plates: 26.96 × 22.12 inches and 27.08 × 22.08 inches","costCenters":[],"links":[{"id":39826,"rank":401,"type":{"id":17,"text":"Plate"},"url":"https://pubs.usgs.gov/of/1986/0422/plate-2.pdf","linkFileType":{"id":1,"text":"pdf"}},{"id":389660,"rank":5,"type":{"id":36,"text":"NGMDB Index Page"},"url":"https://ngmdb.usgs.gov/Prodesc/proddesc_17040.htm"},{"id":39827,"rank":300,"type":{"id":11,"text":"Document"},"url":"https://pubs.usgs.gov/of/1986/0422/report.pdf","linkFileType":{"id":1,"text":"pdf"}},{"id":39825,"rank":400,"type":{"id":17,"text":"Plate"},"url":"https://pubs.usgs.gov/of/1986/0422/plate-1.pdf","linkFileType":{"id":1,"text":"pdf"}},{"id":145383,"rank":0,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/of/1986/0422/report-thumb.jpg"}],"country":"United States","state":"New Hampshire, New York, Vermont","otherGeospatial":"Glens Falls 1° x 2° quadrangle","geographicExtents":"{\n \"type\": \"FeatureCollection\",\n \"features\": [\n {\n \"type\": \"Feature\",\n \"properties\": {},\n \"geometry\": {\n \"type\": \"Polygon\",\n \"coordinates\": [\n [\n [\n -74,\n 43\n ],\n [\n -72,\n 43\n ],\n [\n -72,\n 44\n ],\n [\n -74,\n 44\n ],\n [\n -74,\n 43\n ]\n ]\n ]\n }\n }\n ]\n}","noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"4f4e4acee4b07f02db67f483","contributors":{"authors":[{"text":"Day, G.W.","contributorId":63363,"corporation":false,"usgs":true,"family":"Day","given":"G.W.","email":"","affiliations":[],"preferred":false,"id":164106,"contributorType":{"id":1,"text":"Authors"},"rank":1},{"text":"Welsch, E. P.","contributorId":6050,"corporation":false,"usgs":true,"family":"Welsch","given":"E.","email":"","middleInitial":"P.","affiliations":[],"preferred":false,"id":164104,"contributorType":{"id":1,"text":"Authors"},"rank":2},{"text":"Watts, K. C. Jr.","contributorId":36578,"corporation":false,"usgs":true,"family":"Watts","given":"K.","suffix":"Jr.","email":"","middleInitial":"C.","affiliations":[],"preferred":false,"id":164105,"contributorType":{"id":1,"text":"Authors"},"rank":3},{"text":"Gray, J. C.","contributorId":100400,"corporation":false,"usgs":true,"family":"Gray","given":"J. C.","affiliations":[],"preferred":false,"id":164107,"contributorType":{"id":1,"text":"Authors"},"rank":4}]}} ]}