The Rattlesnake Road less Area covers 32,870 acres between long 11°37'30\" and long 111°47'30\" W. and between lat 34°40' and lat 34°45' N., Coconino and Yavapai Counties, in central Arizona. Sedona and 0ak Creek, the nearest population centers, are located, respectively, at the northwest corner and along the west boundary of the roadless area.
\nThe Rattlesnake Roadless Area includes the deeply embayed Mogollon Rim margin of the Colorado Plateau Province and part of the Werde Walley. The Werde Walley is a deeply dissected lacustrine basin, one of several tectonic basins in the Arizona transition zone that separate the Basin and Range Province from the Colorado Plateau Province. Here the plateau surface falls off abruptly to the Werde Valley, drained by the Werde River, the master stream of the region.
\nThe highest point in the roadless area is 6,834 ft at the basalt cap at the north end of Munds Mountain. The lowest point, about 3,480 ft, is along Dry Beaver Creek, near the southwest corner of the roadless area. The maximum relief, more than 2,000 ft, occurs between the Munds-Lee Mountain divide and the valley floors of bordering Oak Creek and Jacks Canyon. The relief between floor and upper canyon rims along the steep-walled and narrow Woods Canyon ranges from 900 ft to more than 1,400 ft; the east side of the canyon has the highest walls.
\nCanyon rims in the roadless area are accessible by several four-wheel-drive trails across the plateau surface from points along Schnebly Hill Road and Highway I-17. Access to Jacks Canyon is by road and four-wheel-drive trail to Jacks Canyon Tank, about 4 mi up the canyon from Highway 179. Access to the head of Jacks Canyon is by foot or horse along a well-maintained trail. Access to the bottom of Woods Canyon is by four-wheel-drive vehicle for about 2 mi from Highway 179 and then by pack trail for about 5 mi more.
","language":"English","publisher":"U.S. Geological Survey","publisherLocation":"Reston, VA","doi":"10.3133/mf1567C","usgsCitation":"Martin, R., 1986, Aeromagnetic map of the Rattlesnake Roadless Area, Coconino and Yavapai counties, Arizona: U.S. Geological Survey Miscellaneous Field Studies Map 1567, Plate: 42.80 x 40.64 inches, https://doi.org/10.3133/mf1567C.","productDescription":"Plate: 42.80 x 40.64 inches","onlineOnly":"N","additionalOnlineFiles":"N","costCenters":[],"links":[{"id":182613,"rank":0,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/thumbnails/mf1567C.JPG"},{"id":327333,"rank":1,"type":{"id":17,"text":"Plate"},"url":"https://pubs.usgs.gov/mf/1567-C/plate-1.pdf","linkFileType":{"id":1,"text":"pdf"}}],"scale":"0","country":"United States","state":"Arizona","county":"Coconino County, Yavapai County","otherGeospatial":"Rattlesnake Roadless Area","geographicExtents":"{ \"type\": \"FeatureCollection\", \"features\": [ { \"type\": \"Feature\", \"properties\": {}, \"geometry\": { \"type\": \"Polygon\", \"coordinates\": [ [ [ -111.78416666666666,34.666666666666664 ], [ -111.78416666666666,34.8675 ], [ -111.61749999999999,34.8675 ], [ -111.61749999999999,34.666666666666664 ], [ -111.78416666666666,34.666666666666664 ] ] ] } } ] }","noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"4f4e4af3e4b07f02db691a49","contributors":{"authors":[{"text":"Martin, R.A.","contributorId":53379,"corporation":false,"usgs":true,"family":"Martin","given":"R.A.","email":"","affiliations":[],"preferred":false,"id":263341,"contributorType":{"id":1,"text":"Authors"},"rank":1}]}} ,{"id":63495,"text":"gp969 - 1986 - Compilation of selected geophysical references for the Snake River plain, Idaho and eastern Oregon","interactions":[{"subject":{"id":40338,"text":"ofr84587 - 1984 - Compilation of selected geophysical references for the Snake River plain, Idaho and eastern Oregon","indexId":"ofr84587","publicationYear":"1984","noYear":false,"title":"Compilation of selected geophysical references for the Snake River plain, Idaho and eastern Oregon"},"predicate":"SUPERSEDED_BY","object":{"id":63495,"text":"gp969 - 1986 - Compilation of selected geophysical references for the Snake River plain, Idaho and eastern Oregon","indexId":"gp969","publicationYear":"1986","noYear":false,"title":"Compilation of selected geophysical references for the Snake River plain, Idaho and eastern Oregon"},"id":1}],"lastModifiedDate":"2025-07-18T17:59:17.777186","indexId":"gp969","displayToPublicDate":"1994-01-01T00:00:00","publicationYear":"1986","noYear":false,"publicationType":{"id":18,"text":"Report"},"publicationSubtype":{"id":5,"text":"USGS Numbered Series"},"seriesTitle":{"id":317,"text":"Geophysical Investigations Map","code":"GP","active":false,"publicationSubtype":{"id":5}},"seriesNumber":"969","title":"Compilation of selected geophysical references for the Snake River plain, Idaho and eastern Oregon","docAbstract":"No abstract available.
","language":"English","publisher":"U.S. Geological Survey","doi":"10.3133/gp969","usgsCitation":"Whitehead, R., 1986, Compilation of selected geophysical references for the Snake River plain, Idaho and eastern Oregon: U.S. Geological Survey Geophysical Investigations Map 969, 1 Plate: 51.75 x 38.21 inches, https://doi.org/10.3133/gp969.","productDescription":"1 Plate: 51.75 x 38.21 inches","costCenters":[],"links":[{"id":253138,"rank":1,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/gp/0969/report-thumb.jpg"},{"id":249608,"rank":2,"type":{"id":11,"text":"Document"},"url":"https://pubs.usgs.gov/gp/0969/report.pdf","linkFileType":{"id":1,"text":"pdf"}},{"id":249609,"rank":3,"type":{"id":17,"text":"Plate"},"url":"https://pubs.usgs.gov/gp/0969/plate-1.pdf","linkFileType":{"id":1,"text":"pdf"}},{"id":492572,"rank":4,"type":{"id":36,"text":"NGMDB Index Page"},"url":"https://ngmdb.usgs.gov/Prodesc/proddesc_6311.htm","linkFileType":{"id":5,"text":"html"}}],"scale":"2000000","country":"United States","state":"Idaho, Oregon","otherGeospatial":"Snake River plain","geographicExtents":"{\n \"type\": \"FeatureCollection\",\n \"features\": [\n {\n \"type\": \"Feature\",\n \"properties\": {},\n \"geometry\": {\n \"type\": \"Polygon\",\n \"coordinates\": [\n [\n [\n -110,\n 42\n ],\n [\n -110,\n 45\n ],\n [\n -118,\n 45\n ],\n [\n -118,\n 42\n ],\n [\n -110,\n 42\n ]\n ]\n ]\n }\n }\n ]\n}","noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"4f4e4b1de4b07f02db6a971b","contributors":{"authors":[{"text":"Whitehead, R.L.","contributorId":34891,"corporation":false,"usgs":true,"family":"Whitehead","given":"R.L.","email":"","affiliations":[],"preferred":false,"id":268988,"contributorType":{"id":1,"text":"Authors"},"rank":1}]}} ,{"id":59843,"text":"mf1826 - 1986 - Structure contour map of the top of the Castlegate Sandstone, eastern part of the Uinta Basin and the western part of the Piceance Creek basin, Utah and Colorado","interactions":[],"lastModifiedDate":"2019-06-13T17:28:41","indexId":"mf1826","displayToPublicDate":"1994-01-01T00:00:00","publicationYear":"1986","noYear":false,"publicationType":{"id":18,"text":"Report"},"publicationSubtype":{"id":5,"text":"USGS Numbered Series"},"seriesTitle":{"id":325,"text":"Miscellaneous Field Studies Map","code":"MF","active":false,"publicationSubtype":{"id":5}},"seriesNumber":"1826","title":"Structure contour map of the top of the Castlegate Sandstone, eastern part of the Uinta Basin and the western part of the Piceance Creek basin, Utah and Colorado","docAbstract":"No abstract available.
","language":"English","publisher":"U.S. Geological Survey","publisherLocation":"Reston, VA","doi":"10.3133/mf1826","usgsCitation":"Johnson, R.C., 1986, Structure contour map of the top of the Castlegate Sandstone, eastern part of the Uinta Basin and the western part of the Piceance Creek basin, Utah and Colorado: U.S. Geological Survey Miscellaneous Field Studies Map 1826, 2 Plates: 56.05 x 40.95 inches and 41.72 x 32.36 inches, https://doi.org/10.3133/mf1826.","productDescription":"2 Plates: 56.05 x 40.95 inches and 41.72 x 32.36 inches","costCenters":[],"links":[{"id":364280,"rank":3,"type":{"id":17,"text":"Plate"},"url":"https://pubs.usgs.gov/mf/1826/plate-2.pdf","linkFileType":{"id":1,"text":"pdf"}},{"id":364279,"rank":2,"type":{"id":17,"text":"Plate"},"url":"https://pubs.usgs.gov/mf/1826/plate-1.pdf","linkFileType":{"id":1,"text":"pdf"}},{"id":185079,"rank":0,"type":{"id":24,"text":"Thumbnail"},"url":" https://pubs.usgs.gov/mf/1826/report-thumb.jpg"}],"scale":"0","country":"United States","state":"Colorado, Utah","otherGeospatial":"Piceance Creek basin","geographicExtents":"{ \"type\": \"FeatureCollection\", \"features\": [ { \"type\": \"Feature\", \"properties\": {}, \"geometry\": { \"type\": \"Polygon\", \"coordinates\": [ [ [ -111,39 ], [ -111,40.75 ], [ -107.75,40.75 ], [ -107.75,39 ], [ -111,39 ] ] ] } } ] }","noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"4f4e4b0ae4b07f02db69d155","contributors":{"authors":[{"text":"Johnson, R. C. 0000-0002-6197-5165","orcid":"https://orcid.org/0000-0002-6197-5165","contributorId":101621,"corporation":false,"usgs":true,"family":"Johnson","given":"R.","middleInitial":"C.","affiliations":[{"id":595,"text":"U.S. Geological Survey","active":false,"usgs":true}],"preferred":false,"id":262699,"contributorType":{"id":1,"text":"Authors"},"rank":1}]}} ,{"id":12093,"text":"ofr86237 - 1986 - Ground-water conditions in Salt Lake Valley, Utah, 1969-83, and predicted effects of increased withdrawals from wells","interactions":[{"subject":{"id":12093,"text":"ofr86237 - 1986 - Ground-water conditions in Salt Lake Valley, Utah, 1969-83, and predicted effects of increased withdrawals from wells","indexId":"ofr86237","publicationYear":"1986","noYear":false,"title":"Ground-water conditions in Salt Lake Valley, Utah, 1969-83, and predicted effects of increased withdrawals from wells"},"predicate":"SUPERSEDED_BY","object":{"id":70043733,"text":"70043733 - 1987 - Ground-water conditions in Salt Lake Valley, Utah, 1969-83, and predicted effects of increased withdrawals from wells","indexId":"70043733","publicationYear":"1987","noYear":false,"title":"Ground-water conditions in Salt Lake Valley, Utah, 1969-83, and predicted effects of increased withdrawals from wells"},"id":1}],"supersededBy":{"id":70043733,"text":"70043733 - 1987 - Ground-water conditions in Salt Lake Valley, Utah, 1969-83, and predicted effects of increased withdrawals from wells","indexId":"70043733","publicationYear":"1987","noYear":false,"title":"Ground-water conditions in Salt Lake Valley, Utah, 1969-83, and predicted effects of increased withdrawals from wells"},"lastModifiedDate":"2025-09-30T15:58:11.205019","indexId":"ofr86237","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":"86-237","title":"Ground-water conditions in Salt Lake Valley, Utah, 1969-83, and predicted effects of increased withdrawals from wells","docAbstract":"This report was prepared in cooperation with several organizations in the Salt Lake Valley and with the Central Utah Water Conservancy District to present results of a study to determine changes in the ground-water conditions in Salt Lake Valley, Utah, from 1969 to 1983, and to predict the aquifer response to projected withdrawals. The average annual recharge and discharge from the ground-water reservoir in Salt Lake Valley, Utah, during 1969-82 were estimated to be about 352,000 and 353,000 acre-feet per year. Withdrawals from wells increased from 107,000 acre-feet per year during 1964-68 to 117,000 acre-feet per year during 1969-82. The greatest increase in use was for public supply and institutions which increased from 35,000 acre-feet per year during 1964-68 to 46,700 acre-feet per year during 1969-82.
From 1969 to 1983 water levels declined from 5 to 15 feet in the southeast part of the valley where pumpage from large public supply wells was greater during 1969-82 than during previous years. From February-March 1969 to February-March 1983 the quantity of ground water in storage in Salt Lake Valley increased by about 33,000 acre-feet.
A digital-computer model was calibrated to simulate, in three-dimensions, the ground-water flow in the principal and shallow-unconfined aquifers in Salt Lake Valley. Simulations were made to project the response to continuing withdrawals through 2020. Alternative pumping rates used were (1) the 1982 rate of pumpage and (2) increasing the 1982 rate of pumpage by 65,000 acre-feet. The simulation at the increased rate of pumpage indicated that drawdowns would reach 40-60 feet in the area east of Sandy. About 75 percent of the increased withdrawal was salvaged from water that otherwise would have been discharged to the Jordan River and its tributaries.
","language":"English","publisher":"U.S. Geological Survey","doi":"10.3133/ofr86237","usgsCitation":"Waddell, K., Seiler, R.L., Santini, M., and Solomon, D.K., 1986, Ground-water conditions in Salt Lake Valley, Utah, 1969-83, and predicted effects of increased withdrawals from wells: U.S. Geological Survey Open-File Report 86-237, vi, 60 p., https://doi.org/10.3133/ofr86237.","productDescription":"vi, 60 p.","costCenters":[],"links":[{"id":144739,"rank":1,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/of/1986/0237/report-thumb.jpg"},{"id":496110,"rank":2,"type":{"id":11,"text":"Document"},"url":"https://pubs.usgs.gov/of/1986/0237/report.pdf","linkFileType":{"id":1,"text":"pdf"}}],"country":"United States","state":"Utah","otherGeospatial":"Salt Lake Valley","geographicExtents":"{\"type\":\"FeatureCollection\",\"features\":[{\"type\":\"Feature\",\"id\":\"47\",\"properties\":{\"name\":\"Utah\",\"nation\":\"USA 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K.M.","contributorId":59009,"corporation":false,"usgs":true,"family":"Waddell","given":"K.M.","email":"","affiliations":[],"preferred":false,"id":165037,"contributorType":{"id":1,"text":"Authors"},"rank":1},{"text":"Seiler, R. L.","contributorId":87546,"corporation":false,"usgs":true,"family":"Seiler","given":"R.","email":"","middleInitial":"L.","affiliations":[],"preferred":false,"id":165039,"contributorType":{"id":1,"text":"Authors"},"rank":2},{"text":"Santini, M.","contributorId":64659,"corporation":false,"usgs":true,"family":"Santini","given":"M.","email":"","affiliations":[],"preferred":false,"id":165038,"contributorType":{"id":1,"text":"Authors"},"rank":3},{"text":"Solomon, D. K.","contributorId":98324,"corporation":false,"usgs":false,"family":"Solomon","given":"D.","email":"","middleInitial":"K.","affiliations":[],"preferred":false,"id":165040,"contributorType":{"id":1,"text":"Authors"},"rank":4}]}} ,{"id":33356,"text":"b1713A - 1986 - Mineral resources of the Castle Peaks Wilderness Study Area, San Bernardino County, California","interactions":[],"lastModifiedDate":"2025-09-09T13:30:04.246716","indexId":"b1713A","displayToPublicDate":"1994-01-01T00:00:00","publicationYear":"1986","noYear":false,"publicationType":{"id":18,"text":"Report"},"publicationSubtype":{"id":5,"text":"USGS Numbered Series"},"seriesTitle":{"id":306,"text":"Bulletin","code":"B","active":false,"publicationSubtype":{"id":5}},"seriesNumber":"1713","chapter":"A","title":"Mineral resources of the Castle Peaks Wilderness Study Area, San Bernardino County, California","docAbstract":"The Castle Peaks Wilderness Study Area (CDCA266) comprises approximately 45,000 acres in the northern New York Mountains, San Bernardino County, California. At the request of the Bureau of Land Management, 39,303 acres of the wilderness study area were studied. The area was investigated during 1982-1985 using combined geologic, geochemical, and geophysical methods. are considered preliminarily suitable for wilderness deignation. There are no mineral reserves or identified resources in the study area. Fluorspar, occurring in sparse veins, has moderate resource potential, as do silver and lead in fault zones, and gold and silver in sparse, high-grade veins and fault breccia. Each area of moderate resource potential encompasses less than one square mile. These same commodities have low resource potential in similar occurrences throughout much of the study area. In addition, there is low resource potential for gold in placer deposits, uranium in altered breccia and gouge, and rare-earth elements in pegmatite dikes. There is no resource potential for oil and gas resources over most of the study area, but the potential is unknown along its western margin. In this report, the area studied is referred to\"the wilderness study area\", or simply \"the study area.\"
","largerWorkTitle":"Mineral resources of Wilderness Study Areas: Eastern California Desert Conservation Area","language":"English","publisher":"U.S. Geological Survey","doi":"10.3133/b1713A","usgsCitation":"Miller, D., Frisken, J.G., Jachens, R.C., and Gese, D.D., 1986, Mineral resources of the Castle Peaks Wilderness Study Area, San Bernardino County, California: U.S. Geological Survey Bulletin 1713, 17 p., https://doi.org/10.3133/b1713A.","productDescription":"17 p.","costCenters":[],"links":[{"id":340330,"rank":2,"type":{"id":11,"text":"Document"},"url":"https://pubs.usgs.gov/bul/1713a/report.pdf","linkFileType":{"id":1,"text":"pdf"}},{"id":164252,"rank":1,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/bul/1713a/report-thumb.jpg"}],"country":"United States","state":"California","county":"San Bernardino","otherGeospatial":"Castle Peaks Wilderness Study Area","geographicExtents":"{\n \"type\": \"FeatureCollection\",\n \"features\": [\n {\n \"type\": \"Feature\",\n \"properties\": {},\n \"geometry\": {\n \"type\": \"Polygon\",\n \"coordinates\": [\n [\n [\n -115.224609375,\n 35.475769157259265\n ],\n [\n -115.32829284667967,\n 35.4550769336729\n ],\n [\n -115.34751892089845,\n 35.45172093634465\n ],\n [\n -115.37498474121092,\n 35.44053326772722\n ],\n [\n -115.38459777832031,\n 35.43102252677332\n ],\n [\n -115.38528442382812,\n 35.423189308372564\n ],\n [\n -115.31867980957031,\n 35.340894535882846\n ],\n [\n -115.3131866455078,\n 35.335853353844065\n ],\n [\n -115.30288696289062,\n 35.33697364369794\n ],\n [\n -115.28572082519533,\n 35.33473304845998\n ],\n [\n -115.26100158691406,\n 35.316245767635834\n ],\n [\n -115.25207519531249,\n 35.314004597852474\n ],\n [\n -115.23902893066408,\n 35.317926604216396\n ],\n [\n -115.22529602050781,\n 35.3072807158836\n ],\n [\n -115.22804260253906,\n 35.29775425972381\n ],\n [\n -115.23834228515626,\n 35.29383127531525\n ],\n [\n -115.24658203125,\n 35.288226682029574\n ],\n [\n -115.24864196777342,\n 35.278137436300966\n ],\n [\n -115.21156311035156,\n 35.24842291350237\n ],\n [\n -115.04127502441406,\n 35.331372039128475\n ],\n [\n -115.224609375,\n 35.475769157259265\n ]\n ]\n ]\n }\n }\n ]\n}","noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"4f4e49fae4b07f02db5f3d0e","contributors":{"authors":[{"text":"Miller, David M. 0000-0003-3711-0441 dmiller@usgs.gov","orcid":"https://orcid.org/0000-0003-3711-0441","contributorId":140769,"corporation":false,"usgs":true,"family":"Miller","given":"David M.","email":"dmiller@usgs.gov","affiliations":[{"id":309,"text":"Geology and Geophysics Science Center","active":true,"usgs":true},{"id":312,"text":"Geology, Minerals, Energy, and Geophysics Science Center","active":true,"usgs":true}],"preferred":true,"id":210635,"contributorType":{"id":1,"text":"Authors"},"rank":1},{"text":"Frisken, James G.","contributorId":76740,"corporation":false,"usgs":true,"family":"Frisken","given":"James","email":"","middleInitial":"G.","affiliations":[],"preferred":false,"id":210638,"contributorType":{"id":1,"text":"Authors"},"rank":2},{"text":"Jachens, Robert C. jachens@usgs.gov","contributorId":1180,"corporation":false,"usgs":true,"family":"Jachens","given":"Robert","email":"jachens@usgs.gov","middleInitial":"C.","affiliations":[{"id":312,"text":"Geology, Minerals, Energy, and Geophysics Science Center","active":true,"usgs":true}],"preferred":true,"id":210637,"contributorType":{"id":1,"text":"Authors"},"rank":3},{"text":"Gese, Diann D.","contributorId":68808,"corporation":false,"usgs":true,"family":"Gese","given":"Diann","email":"","middleInitial":"D.","affiliations":[],"preferred":false,"id":210636,"contributorType":{"id":1,"text":"Authors"},"rank":4}]}} ,{"id":19123,"text":"ofr86405 - 1986 - Multichannel seismic-reflection data collected in 1980 in the eastern Chukchi Sea","interactions":[],"lastModifiedDate":"2016-02-22T08:25:35","indexId":"ofr86405","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":"86-405","title":"Multichannel seismic-reflection data collected in 1980 in the eastern Chukchi Sea","docAbstract":"The U.S. Geological Survey (USGS) collected approximately 2,652 km of 24-channel seismic-reflection data in early September, 1980, over the continental shelf in the eastern Chukchi Sea (Fig. 1). The profiles were collected on the USGS Research Vessel S.P. Lee. The seismic energy source consisted of a tuned array of five airguns with a total volume of 1213 cubic inches of air compressed to approximately 1900 psi. The recording system consisted of a 24-channel, 2400 meter long streamer with a group interval of 100 m, and a GUS (Global Universal Science) model 4200 digital recording instrument. Shots were fired every 50 meters. Navigational control for the survey was provided by a Magnavox integrated navigation system using transit satellites and doppler-sonar augmented by Loran C (Rho-Rho). A 2-millisecond sampling rate was used in the field; the data were later desampled to 4-milliseconds during the demultiplexing process. 8 seconds data length was recorded. Processing was done at the USGS Pacific Marine Geology Multichannel Processing Center in Menlo Park, California, in the sequence: editing-demultiplexing, velocity analysis, CDP stacking, deconvolution-filtering, and plotting on an electrostatic plotter. Plate 1 is a trackline chart showing shotpoint navigation.
","language":"English","publisher":"U.S. Geological Survey","doi":"10.3133/ofr86405","usgsCitation":"Grantz, A., Mann, D.M., and May, S., 1986, Multichannel seismic-reflection data collected in 1980 in the eastern Chukchi Sea: U.S. Geological Survey Open-File Report 86-405, Report: 4 p.; Plate: 34.12 x 33.84 inches, https://doi.org/10.3133/ofr86405.","productDescription":"Report: 4 p.; Plate: 34.12 x 33.84 inches","costCenters":[],"links":[{"id":152492,"rank":0,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/of/1986/0405/report-thumb.jpg"},{"id":48582,"rank":400,"type":{"id":17,"text":"Plate"},"url":"https://pubs.usgs.gov/of/1986/0405/plate-1.pdf","linkFileType":{"id":1,"text":"pdf"}},{"id":48583,"rank":300,"type":{"id":11,"text":"Document"},"url":"https://pubs.usgs.gov/of/1986/0405/report.pdf","linkFileType":{"id":1,"text":"pdf"}}],"country":"United States","state":"Alaska","otherGeospatial":"Chukchi Sea","geographicExtents":"{\n \"type\": \"FeatureCollection\",\n \"features\": [\n {\n \"type\": \"Feature\",\n \"properties\": {},\n \"geometry\": {\n \"type\": \"Polygon\",\n \"coordinates\": [\n [\n [\n -170.48583984375,\n 66.08936427047088\n ],\n [\n -170.48583984375,\n 71.10254274232307\n ],\n [\n -162.1142578125,\n 71.10254274232307\n ],\n [\n -162.1142578125,\n 66.08936427047088\n ],\n [\n -170.48583984375,\n 66.08936427047088\n ]\n ]\n ]\n }\n }\n ]\n}","noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"4f4e4b32e4b07f02db6b4840","contributors":{"authors":[{"text":"Grantz, Arthur agrantz@usgs.gov","contributorId":2585,"corporation":false,"usgs":true,"family":"Grantz","given":"Arthur","email":"agrantz@usgs.gov","affiliations":[{"id":312,"text":"Geology, Minerals, Energy, and Geophysics Science Center","active":true,"usgs":true}],"preferred":true,"id":180344,"contributorType":{"id":1,"text":"Authors"},"rank":1},{"text":"Mann, Dennis M.","contributorId":50528,"corporation":false,"usgs":true,"family":"Mann","given":"Dennis","email":"","middleInitial":"M.","affiliations":[],"preferred":false,"id":180346,"contributorType":{"id":1,"text":"Authors"},"rank":2},{"text":"May, Steven D.","contributorId":56194,"corporation":false,"usgs":true,"family":"May","given":"Steven D.","affiliations":[],"preferred":false,"id":180345,"contributorType":{"id":1,"text":"Authors"},"rank":3}]}} ,{"id":28834,"text":"wri854334 - 1986 - Hydrogeology of sand-plain aquifers in Carlton, Kanabec, and Pine Counties, east-central Minnesota","interactions":[],"lastModifiedDate":"2022-02-03T19:27:52.356527","indexId":"wri854334","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":"85-4334","title":"Hydrogeology of sand-plain aquifers in Carlton, Kanabec, and Pine Counties, east-central Minnesota","docAbstract":"Sand-plain aquifers in parts of Carlton, Kanabec, and Pine Counties in east-central Minnesota constitute a major aquifer system. They consist predominantly of fine to medium outwash sand with a combined areal extent of nearly 500 square miles. Saturated thickness in localized areas is as much as 90 feet. Depth to water generally is less than 20 feet. Transmissivities range from about 100 to 25,000 feet squared per day. Yields to properly constructed wells locally may exceed 2,000 gallons per minute. A reconnaissance of sandstone units underlying the outwash indicates that transmissivities of the sandstone aquifers range from 1,850 to 2,200 feet squared per day, and specific capacities range from 9 to 12 gallons per minute per foot of drawdown. Locally, wells may be capable of supplying several hundred gallons per minute. Regionally, the sand-plain and sandstone aquifers are poorly connected hydraulically at all locations tested except in a small localized area near Quamba in Kanabec County.
\nGround water in the sand-plain aquifers can be classified chemically, based on predominant ions, as a calcium bicarbonate type that is moderately hard. Concentrations of dissolved solids range from 30 to 610 milligrams per liter. Except for locally high concentrations of iron and manganese, the quality of water is within State drinking-water standards and is suitable for most uses. There are no major differences between the quality of water in the sand-plain and sandstone aquifers.
\nGround-water flow, aquifer response, aquifer development, and drought conditions were simulated for sand-plain aquifers areally extensive enough to be hydrologically significant. Simulation of expanded ground-water development and drought in northern Pine County indicates that regional ground-water levels may be lowered as much as 12 feet and ground-water discharge to streams may be reduced as much as 42 percent. Simulation of expanded development and drought in southern Pine County indicates that regional ground-water levels may be lowered as much as 25 feet and ground-water discharge to streams may be reduced as much as 65 percent. The simulations also indicate that each area, especially the northern Pine County area, will support substantial additional development without dewatering the aquifer or reducing streamflow significantly.
","language":"English","publisher":"U.S. Geological Survey","publisherLocation":"St. Paul, MN","doi":"10.3133/wri854334","collaboration":"Prepared in cooperation with the Onanegozie Resource Conservation and Development Project and the Minnesota Department of Natural Resources","usgsCitation":"Myette, C., 1986, Hydrogeology of sand-plain aquifers in Carlton, Kanabec, and Pine Counties, east-central Minnesota: U.S. Geological Survey Water-Resources Investigations Report 85-4334, Report: vi, 66 p.; 4 Plates: 20.31 x 36.55 inches or smaller, https://doi.org/10.3133/wri854334.","productDescription":"Report: vi, 66 p.; 4 Plates: 20.31 x 36.55 inches or smaller","onlineOnly":"N","additionalOnlineFiles":"N","costCenters":[{"id":392,"text":"Minnesota Water Science Center","active":true,"usgs":true}],"links":[{"id":57709,"rank":403,"type":{"id":17,"text":"Plate"},"url":"https://pubs.usgs.gov/wri/1985/4334/plate-4.pdf","linkFileType":{"id":1,"text":"pdf"}},{"id":57708,"rank":402,"type":{"id":17,"text":"Plate"},"url":"https://pubs.usgs.gov/wri/1985/4334/plate-3.pdf","linkFileType":{"id":1,"text":"pdf"}},{"id":57710,"rank":300,"type":{"id":11,"text":"Document"},"url":"https://pubs.usgs.gov/wri/1985/4334/report.pdf","linkFileType":{"id":1,"text":"pdf"}},{"id":57707,"rank":401,"type":{"id":17,"text":"Plate"},"url":"https://pubs.usgs.gov/wri/1985/4334/plate-2.pdf","linkFileType":{"id":1,"text":"pdf"}},{"id":57706,"rank":400,"type":{"id":17,"text":"Plate"},"url":"https://pubs.usgs.gov/wri/1985/4334/plate-1.pdf","linkFileType":{"id":1,"text":"pdf"}},{"id":123429,"rank":0,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/wri/1985/4334/report-thumb.jpg"},{"id":395395,"rank":7,"type":{"id":36,"text":"NGMDB Index Page"},"url":"https://ngmdb.usgs.gov/Prodesc/proddesc_36460.htm"}],"country":"United States","state":"Minnesota","county":"Carlton County, Kanabec County, Pine County","geographicExtents":"{\"type\":\"FeatureCollection\",\"features\":[{\"type\":\"Feature\",\"geometry\":{\"type\":\"Polygon\",\"coordinates\":[[[-93.0603,46.767],[-92.7423,46.7675],[-92.7317,46.7674],[-92.6654,46.7693],[-92.5972,46.7666],[-92.4819,46.7667],[-92.4733,46.7666],[-92.2991,46.7652],[-92.2963,46.6661],[-92.2883,46.6679],[-92.2884,46.6633],[-92.289,46.5936],[-92.2892,46.5183],[-92.2893,46.4694],[-92.2892,46.4176],[-92.289,46.3442],[-92.2889,46.2632],[-92.2893,46.2192],[-92.2894,46.159],[-92.2896,46.0928],[-92.2897,46.0846],[-92.2899,46.0706],[-92.3025,46.0682],[-92.3144,46.0665],[-92.3225,46.0635],[-92.3289,46.0597],[-92.3335,46.0566],[-92.3356,46.0529],[-92.3383,46.0488],[-92.3383,46.0461],[-92.3392,46.0421],[-92.3419,46.0389],[-92.3419,46.0384],[-92.3421,46.0361],[-92.3405,46.0337],[-92.3386,46.0305],[-92.3393,46.0278],[-92.3418,46.0234],[-92.3447,46.021],[-92.3473,46.0178],[-92.3493,46.0151],[-92.3505,46.014],[-92.3513,46.0134],[-92.352,46.0128],[-92.3547,46.011],[-92.3581,46.0097],[-92.3612,46.0101],[-92.3653,46.0102],[-92.3664,46.0102],[-92.3704,46.0111],[-92.3769,46.0126],[-92.3841,46.0149],[-92.388,46.0149],[-92.3922,46.0166],[-92.3945,46.0186],[-92.3986,46.0203],[-92.4043,46.0219],[-92.4091,46.0223],[-92.4134,46.0229],[-92.418,46.022],[-92.422,46.0211],[-92.4262,46.0195],[-92.4314,46.017],[-92.4363,46.0144],[-92.4391,46.0126],[-92.4405,46.0098],[-92.4412,46.0071],[-92.4418,46.0047],[-92.4419,46.003],[-92.4445,46.0012],[-92.4472,46.0003],[-92.4498,45.9989],[-92.4512,45.9967],[-92.4511,45.9944],[-92.4523,45.9921],[-92.4545,45.9907],[-92.4565,45.9894],[-92.4595,45.9877],[-92.4612,45.9858],[-92.4622,45.9841],[-92.4622,45.9836],[-92.4617,45.9814],[-92.4613,45.9798],[-92.4613,45.9789],[-92.4626,45.9771],[-92.4646,45.9762],[-92.4672,45.9748],[-92.4699,45.9739],[-92.4738,45.9732],[-92.4744,45.9732],[-92.4784,45.9735],[-92.4849,45.9749],[-92.4882,45.9745],[-92.4914,45.9745],[-92.4948,45.9762],[-92.4953,45.9764],[-92.4979,45.9787],[-92.5005,45.9801],[-92.5042,45.98],[-92.5051,45.98],[-92.5084,45.9802],[-92.5116,45.9816],[-92.5143,45.9823],[-92.5148,45.9825],[-92.5182,45.9825],[-92.5234,45.9821],[-92.5272,45.9814],[-92.528,45.9811],[-92.5317,45.9798],[-92.5353,45.9785],[-92.5399,45.9753],[-92.5432,45.9731],[-92.5454,45.9711],[-92.5472,45.9685],[-92.5492,45.9658],[-92.5505,45.9635],[-92.5499,45.9608],[-92.5499,45.958],[-92.5487,45.9553],[-92.5487,45.9525],[-92.5508,45.9508],[-92.552,45.9503],[-92.5526,45.9502],[-92.5547,45.95],[-92.5552,45.95],[-92.5592,45.9499],[-92.5644,45.9498],[-92.5697,45.9484],[-92.5702,45.9483],[-92.5756,45.9468],[-92.5831,45.9439],[-92.5869,45.9419],[-92.5914,45.9414],[-92.596,45.9414],[-92.6007,45.9406],[-92.6011,45.9404],[-92.6039,45.939],[-92.6045,45.9387],[-92.6083,45.9369],[-92.6118,45.9351],[-92.6151,45.9338],[-92.6183,45.9329],[-92.6223,45.9324],[-92.6257,45.9319],[-92.6297,45.9323],[-92.6323,45.9317],[-92.6328,45.9315],[-92.6356,45.9312],[-92.638,45.9289],[-92.6387,45.9271],[-92.6386,45.9257],[-92.6401,45.9243],[-92.6427,45.9239],[-92.6446,45.9239],[-92.6483,45.9236],[-92.6516,45.924],[-92.6548,45.923],[-92.6584,45.9217],[-92.665,45.9182],[-92.6714,45.9152],[-92.6742,45.9131],[-92.6742,45.9117],[-92.6749,45.9099],[-92.6749,45.9081],[-92.6756,45.9058],[-92.6784,45.9043],[-92.6813,45.9031],[-92.6851,45.9012],[-92.6887,45.9004],[-92.6917,45.8991],[-92.6953,45.8972],[-92.698,45.8958],[-92.7012,45.8949],[-92.7045,45.894],[-92.7071,45.8926],[-92.7078,45.8922],[-92.7108,45.8901],[-92.7139,45.8877],[-92.7179,45.8848],[-92.7183,45.8844],[-92.7236,45.8795],[-92.729,45.8736],[-92.732,45.8681],[-92.7331,45.8639],[-92.735,45.8576],[-92.7364,45.851],[-92.7378,45.848],[-92.7387,45.8459],[-92.7424,45.8421],[-92.7463,45.8398],[-92.7516,45.8371],[-92.7568,45.8349],[-92.7609,45.8321],[-92.7625,45.8302],[-92.7619,45.8248],[-92.759,45.8194],[-92.7569,45.8158],[-92.7541,45.8121],[-92.7545,45.8088],[-92.7559,45.8056],[-92.7595,45.8019],[-92.7626,45.7991],[-92.7658,45.7975],[-92.7664,45.7972],[-92.7703,45.7947],[-92.7723,45.7924],[-92.7743,45.7892],[-92.7763,45.786],[-92.777,45.7828],[-92.7777,45.7787],[-92.7791,45.7732],[-92.7811,45.7691],[-92.7829,45.7654],[-92.7849,45.762],[-92.7886,45.7582],[-92.7915,45.7561],[-92.7943,45.7541],[-92.7976,45.7518],[-92.8002,45.75],[-92.8006,45.7497],[-92.8035,45.7477],[-92.8063,45.7454],[-92.8084,45.7435],[-92.8088,45.7431],[-92.8114,45.7409],[-92.8176,45.7369],[-92.8245,45.7332],[-92.8286,45.7318],[-92.8773,45.7316],[-92.9158,45.7313],[-93.1408,45.7312],[-93.5133,45.7335],[-93.5212,45.9801],[-93.4321,45.9815],[-93.428,46.1541],[-93.2337,46.1611],[-93.0512,46.1584],[-93.0495,46.3168],[-93.0532,46.3562],[-93.0527,46.419],[-93.0536,46.5932],[-93.0608,46.5937],[-93.0623,46.6739],[-93.0603,46.767]]]},\"properties\":{\"name\":\"Carlton\",\"state\":\"MN\"}}]}","noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"4f4e4a49e4b07f02db6244e9","contributors":{"authors":[{"text":"Myette, C. F.","contributorId":97115,"corporation":false,"usgs":true,"family":"Myette","given":"C. F.","affiliations":[],"preferred":false,"id":200481,"contributorType":{"id":1,"text":"Authors"},"rank":1}]}} ,{"id":28905,"text":"wri864057 - 1986 - Sediment accumulation in San Leandro Bay, Alameda County, California, during the 20th century -- A preliminary report","interactions":[],"lastModifiedDate":"2021-12-21T20:49:39.877506","indexId":"wri864057","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":"86-4057","title":"Sediment accumulation in San Leandro Bay, Alameda County, California, during the 20th century -- A preliminary report","docAbstract":"Major changes made in the configuration of San Leandro Bay, Alameda County, California, during the 20th century have caused rapid sedimentation within parts of the Bay. Opening of the Oakland tidal channel and removal of 97% of the marshlands formerly surrounding the Bay have decreased tidal velocities and volumes. Marshland removal has decreased the tidal prism by about 25%. Comparison of bathymetric surveys indicates that sedimentation in the vicinity of the San Leandro Bay channel averaged 0.7 cm/annum between 1856 and 1984. Lead-210 data collected at four shallow water sites east of the San Leandro Bay channel indicated that sedimentation rates have averaged between 0.06 and 0.28 cm/annum. Because bioturbation of bottom sediments cannot be discounted, better definition of this range in sedimentation rates would required measuring the activity of lead-210 on incoming sediments. In addition to sediment deposited in the vicinity of the San Leandro Bay channel and open, shallow areas to the east, 850,740 cu m of sediment was deposited between 1948 and 1983 in an area dredged at the mouth of San Leandro Creek. All available data indicate that between 1 ,213,000 and 1,364,000 cu m of sediment was deposited in San Leandro Bay between 1948 and 1983. Sediment yield data from an adjacent drainage basin, when combined with inventories of lead-210 and cesium-137, indicate that most of the sediment deposited in San Leandro Bay is coming from resuspension of bottom sediments or from erosion of marshes or shorelines of San Leandro or San Francisco Bay.
","language":"English","publisher":"U.S. Geological Survey","doi":"10.3133/wri864057","usgsCitation":"Nolan, K., and Fuller, C.C., 1986, Sediment accumulation in San Leandro Bay, Alameda County, California, during the 20th century -- A preliminary report: U.S. Geological Survey Water-Resources Investigations Report 86-4057, iv, 25 p., https://doi.org/10.3133/wri864057.","productDescription":"iv, 25 p.","costCenters":[],"links":[{"id":393251,"rank":2,"type":{"id":36,"text":"NGMDB Index Page"},"url":"https://ngmdb.usgs.gov/Prodesc/proddesc_36516.htm"},{"id":57777,"rank":300,"type":{"id":11,"text":"Document"},"url":"https://pubs.usgs.gov/wri/1986/4057/report.pdf","linkFileType":{"id":1,"text":"pdf"}},{"id":159144,"rank":0,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/wri/1986/4057/report-thumb.jpg"}],"country":"United States","state":"California","county":"Alameda County","otherGeospatial":"San Leandro Bay","geographicExtents":"{\n \"type\": \"FeatureCollection\",\n \"features\": [\n {\n \"type\": \"Feature\",\n \"properties\": {},\n \"geometry\": {\n \"type\": \"Polygon\",\n \"coordinates\": [\n [\n [\n -122.24899291992188,\n 37.73081027834234\n ],\n [\n -122.20298767089842,\n 37.73081027834234\n ],\n [\n -122.20298767089842,\n 37.77207165460913\n ],\n [\n -122.24899291992188,\n 37.77207165460913\n ],\n [\n -122.24899291992188,\n 37.73081027834234\n ]\n ]\n ]\n }\n }\n ]\n}","noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"4f4e4a7fe4b07f02db648d75","contributors":{"authors":[{"text":"Nolan, K.M.","contributorId":36151,"corporation":false,"usgs":true,"family":"Nolan","given":"K.M.","affiliations":[],"preferred":false,"id":200596,"contributorType":{"id":1,"text":"Authors"},"rank":1},{"text":"Fuller, C. C.","contributorId":29858,"corporation":false,"usgs":true,"family":"Fuller","given":"C.","email":"","middleInitial":"C.","affiliations":[],"preferred":false,"id":200595,"contributorType":{"id":1,"text":"Authors"},"rank":2}]}} ,{"id":16393,"text":"ofr86138 - 1986 - Chemical quality of ground water in Salt Lake Valley, Utah, 1969-85","interactions":[{"subject":{"id":16393,"text":"ofr86138 - 1986 - Chemical quality of ground water in Salt Lake Valley, Utah, 1969-85","indexId":"ofr86138","publicationYear":"1986","noYear":false,"title":"Chemical quality of ground water in Salt Lake Valley, Utah, 1969-85"},"predicate":"SUPERSEDED_BY","object":{"id":70044053,"text":"70044053 - 1987 - Chemical quality of ground water in Salt Lake Valley, Utah, 1969-85","indexId":"70044053","publicationYear":"1987","noYear":false,"title":"Chemical quality of ground water in Salt Lake Valley, Utah, 1969-85"},"id":1}],"supersededBy":{"id":70044053,"text":"70044053 - 1987 - Chemical quality of ground water in Salt Lake Valley, Utah, 1969-85","indexId":"70044053","publicationYear":"1987","noYear":false,"title":"Chemical quality of ground water in Salt Lake Valley, Utah, 1969-85"},"lastModifiedDate":"2021-02-23T00:52:45.562195","indexId":"ofr86138","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":"86-138","title":"Chemical quality of ground water in Salt Lake Valley, Utah, 1969-85","docAbstract":"During 1979-84, 35 wells completed in the principal aquifer in the Salt Lake Valley, Utah, that had been sampled during 1962-67 were resampled to determine if water quality changes had occurred. The dissolved solids concentration of the water from 13 of the wells has increased by more than 10% since 1962-67.
Much of the ground water between the mouth of Bingham Canyon and the Jordan River about 10 mi to the east has been contaminated by seepage from reservoirs and evaporation ponds associated with mining activities. Many domestic and irrigation wells yield water with concentrations of dissolved solids that exceed 2,000 mg/L. A reservoir in the mouth of Bingham Canyon contains acidic waters with a pH of 3 to 4 and concentrations of dissolved solids ranging from 43,000 to 68,000 mg/L. Seepage from evaporation ponds, which are about 4.5 mi east of the reservoir, also is acidic and contains similar concentrations of dissolved solids. East of the reservoir, where a steep hydraulic gradient exists along the mountain front, the velocities of contaminant movement were estimated to range from about 680-1,000 ft/yr.
Groundwater underlying part of the community of South Salt Lake near the Jordan River has been contaminated by leachate from uranium-mill tailings. The major effect of the leachate from the tailings of the Vitro Chemical Co. on the shallow unconfined aquifer downgradient from the tailings was the contribution of measurable quantities of dissolved solids, chloride, sulfate, iron, and uranium. The concentration of dissolved solids in uncontaminated water was 1,650 mg/L, whereas downgradient from the tailings area, the concentrations ranged from 2,320-21,000 mg/L. The maximum volume of contaminated water was estimated to be 7,800 acre-ft.
The major effect of the leachate from the Vitro tailings on the confined aquifer was the contribution of measurable quantities of dissolved solids, chloride, sulfate, and iron. The concentration of dissolved solids upgradient from the tailings was 330 mg/L, and beneath and downgradient from the tailings the concentrations were 864 and 1,240 mg/L. The minimum volume of contaminated water in the confined aquifer was estimated to be about 12,000 acre-ft.
A calibrated, 3-dimensional, ground-water flow model was used to simulate potential changes in the potentiometric surface due to hypothetical ground-water withdrawals from a postulated well field in the vicinity of the Salt Lake International Center. Using a pumping rate of 30 cubic feet per second, it would require about 3,900 years for the saline ground water from beneath the lake to travel the 7 miles to the postulated well field. (Lantz-PTT)
","language":"English","publisher":"U.S. Geological Survey","publisherLocation":"Reston, VA","doi":"10.3133/ofr86138","usgsCitation":"Waddell, K., Seiler, R.L., and Solomon, D.K., 1986, Chemical quality of ground water in Salt Lake Valley, Utah, 1969-85: U.S. Geological Survey Open-File Report 86-138, Report: v, 45 p.; 3 Plates: 29.93 x 42.04 inches or smaller, https://doi.org/10.3133/ofr86138.","productDescription":"Report: v, 45 p.; 3 Plates: 29.93 x 42.04 inches or smaller","costCenters":[],"links":[{"id":383563,"rank":5,"type":{"id":17,"text":"Plate"},"url":"https://pubs.usgs.gov/of/1986/0138/Plate-1.pdf","linkFileType":{"id":1,"text":"pdf"}},{"id":383562,"rank":4,"type":{"id":17,"text":"Plate"},"url":"https://pubs.usgs.gov/of/1986/0138/Plate-2.pdf","linkFileType":{"id":1,"text":"pdf"}},{"id":383561,"rank":3,"type":{"id":17,"text":"Plate"},"url":"https://pubs.usgs.gov/of/1986/0138/Plate-3.pdf","linkFileType":{"id":1,"text":"pdf"}},{"id":383560,"rank":2,"type":{"id":11,"text":"Document"},"url":"https://pubs.usgs.gov/of/1986/0138/report.pdf","linkFileType":{"id":1,"text":"pdf"}},{"id":147669,"rank":0,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/of/1986/0138/report-thumb.jpg"}],"country":"United States","state":"Utah","otherGeospatial":"Salt Lake Valley","geographicExtents":"{\n \"type\": \"FeatureCollection\",\n \"features\": [\n {\n \"type\": \"Feature\",\n \"properties\": {},\n \"geometry\": {\n \"type\": \"Polygon\",\n \"coordinates\": [\n [\n [\n -112.12646484375,\n 40.413496049701955\n ],\n [\n -111.4453125,\n 40.413496049701955\n ],\n [\n -111.4453125,\n 40.97989806962013\n ],\n [\n -112.12646484375,\n 40.97989806962013\n ],\n [\n -112.12646484375,\n 40.413496049701955\n ]\n ]\n ]\n }\n }\n ]\n}","noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"4f4e4883e4b07f02db517e7d","contributors":{"authors":[{"text":"Waddell, K.M.","contributorId":59009,"corporation":false,"usgs":true,"family":"Waddell","given":"K.M.","email":"","affiliations":[],"preferred":false,"id":172771,"contributorType":{"id":1,"text":"Authors"},"rank":1},{"text":"Seiler, R. L.","contributorId":87546,"corporation":false,"usgs":true,"family":"Seiler","given":"R.","email":"","middleInitial":"L.","affiliations":[],"preferred":false,"id":172772,"contributorType":{"id":1,"text":"Authors"},"rank":2},{"text":"Solomon, D. K.","contributorId":98324,"corporation":false,"usgs":false,"family":"Solomon","given":"D.","email":"","middleInitial":"K.","affiliations":[],"preferred":false,"id":172773,"contributorType":{"id":1,"text":"Authors"},"rank":3}]}} ,{"id":15904,"text":"ofr86249 - 1986 - Selected hydrologic data for Salt Lake Valley, Utah, October 1968 to October 1985","interactions":[],"lastModifiedDate":"2017-08-31T16:29:35","indexId":"ofr86249","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":"86-249","title":"Selected hydrologic data for Salt Lake Valley, Utah, October 1968 to October 1985","docAbstract":"This report contains hydrologic data collected in Salt Lake Valley from October 1968 to October 1985. The report area is bounded by the Wasatch Range on the east, the Oquirrh Mountains on the west, the Traverse Mountains on the south, and the boundary between Davis and Salt Lake Counties on the north.
Hely and others (1971) defined two aquifers of major importance in the valley the principal aquifer and the shallow aquifer. The principal aquifer is a source of water for public supply and industry, whereas the shallow aquifer in many places contains water that is contaminated and is unsuitable for public supply (Seiler and Waddell, 1984).
Most of the data in this report were collected by the U.S. Geological Survey in cooperation with the Utah Department of Natural Resources, Division of Water Rights, Salt Lake County Water Conservancy District, Central Utah Water Conservancy District, Granger-Hunter Improvement District, Magna Water Co. and Improvement District, City of Midvale, Salt Lake City Department of Public Utilities, City of Sandyr City of South Salt Lake, Taylorsville Bennion Improvement District, City of West Jordan, Holladay Water Company, and White City Water Co. Some of the data were published previously by Hely, Mower, and Horr (1967, 1968, and 1969), lorns, Mower, and Horr (1966a and b), Marine and Price (1963), and Seiler and Waddell (1984).
The purpose of this report is to provide hydrologic data for use by the general public and by officials who manage water resources and to supplement interpretive reports for the area. Information about wells, water levels in wells, and the chemical and physical properties of ground water is given in tables 1-4, and the well locations are shown on plate 1.
","language":"English","publisher":"U.S. Geological Survey","doi":"10.3133/ofr86249","collaboration":"Prepared in cooperation with the Utah Department of Natural Resources","usgsCitation":"Seiler, R.L., 1986, Selected hydrologic data for Salt Lake Valley, Utah, October 1968 to October 1985: U.S. Geological Survey Open-File Report 86-249, Report: iv, 57 p.; Plate: 19.82 in. x 21.44 in., https://doi.org/10.3133/ofr86249.","productDescription":"Report: iv, 57 p.; Plate: 19.82 in. x 21.44 in.","numberOfPages":"60","onlineOnly":"Y","costCenters":[{"id":610,"text":"Utah Water Science Center","active":true,"usgs":true}],"links":[{"id":44887,"rank":400,"type":{"id":17,"text":"Plate"},"url":"https://pubs.usgs.gov/of/1986/0249/plate-1.pdf","linkFileType":{"id":1,"text":"pdf"}},{"id":44888,"rank":300,"type":{"id":11,"text":"Document"},"url":"https://pubs.usgs.gov/of/1986/0249/report.pdf","linkFileType":{"id":1,"text":"pdf"}},{"id":150233,"rank":0,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/of/1986/0249/report-thumb.jpg"}],"country":"United States","state":"Utah","otherGeospatial":"Salt Lake Valley","publicComments":"This is also Utah Hydrologic-Data Report no. 44","noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"4f4e4a4de4b07f02db627239","contributors":{"authors":[{"text":"Seiler, R. L.","contributorId":87546,"corporation":false,"usgs":true,"family":"Seiler","given":"R.","email":"","middleInitial":"L.","affiliations":[],"preferred":false,"id":171910,"contributorType":{"id":1,"text":"Authors"},"rank":1}]}} ,{"id":27038,"text":"wri864210 - 1986 - Hydraulic characteristics of Upper Cretaceous and Lower Tertiary clastic aquifers: Eastern Alabama, Georgia, and western South Carolina","interactions":[],"lastModifiedDate":"2019-08-20T13:19:18","indexId":"wri864210","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":"86-4210","title":"Hydraulic characteristics of Upper Cretaceous and Lower Tertiary clastic aquifers: Eastern Alabama, Georgia, and western South Carolina","docAbstract":"Transmissivity and storativity data for the clastic sediments of the northern Coastal Plain of eastern Alabama, Georgia, and western South Carolina were compiled and evaluated. Transmissivity values ranged from less than 100 to about 35,000 ft sq/day; storativity ranged from about 0.00002 to 0.0002. Data for lower Tertiary sediments represented by the Clayton and Tallahatta Formations and equivalent Midwayan and Claibornian sediments are listed for 17 sites. Transmissivity values of these sediments range from about 500 to 10,000 ft sq/day. Transmissivity values for the Cretaceous Providence Sand and Cusseta Sand and equivalent Navarroan-Tayloran sediments are listed for 10 sites and range from about 500 to 34,000 ft sq/day. Transmissivity values for the Blufftown and Eutaw Formations and equivalent Cretaceous Tayloran-Austinian sediments are listed for 16 sites and range from about 3000 to 35,000 ft sq/day. Transmissivity of the Cretaceous Tuscaloosa Formation and equivalent Eaglefordian sediments is listed for 5 sites and ranges from about 30 to 500 ft sq/day. Estimates of transmissivity based on well specific capacity were computed by using the modified nonequilibrium formula and linear regression analysis. The regression analysis was based on log-transformed paired transmissivity and specific-capacity data at 48 pumping wells. The regression model provided better estimates of transmissivity than the modified nonequilibrium formula. (Author 's abstract)","language":"English","publisher":"U.S. Geological Survey","publisherLocation":"Reston, VA","doi":"10.3133/wri864210","usgsCitation":"Faye, R.E., and McFadden, K.W., 1986, Hydraulic characteristics of Upper Cretaceous and Lower Tertiary clastic aquifers: Eastern Alabama, Georgia, and western South Carolina: U.S. Geological Survey Water-Resources Investigations Report 86-4210, Report: viii, 22 p.; 1 Plate: 28.96 x 23.59 inches; 4 Sheets: 14.79 x 18.46 inches or smaller, https://doi.org/10.3133/wri864210.","productDescription":"Report: viii, 22 p.; 1 Plate: 28.96 x 23.59 inches; 4 Sheets: 14.79 x 18.46 inches or smaller","costCenters":[{"id":13634,"text":"South Atlantic Water Science Center","active":true,"usgs":true}],"links":[{"id":158581,"rank":0,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/wri/1986/4210/report-thumb.jpg"},{"id":366719,"rank":3,"type":{"id":17,"text":"Plate"},"url":"https://pubs.usgs.gov/wri/1986/4210/plate-1.pdf","linkFileType":{"id":1,"text":"pdf"}},{"id":366720,"rank":5,"type":{"id":17,"text":"Plate"},"url":"https://pubs.usgs.gov/wri/1986/4210/sheet-2.pdf","text":"Sheet 2","linkFileType":{"id":1,"text":"pdf"}},{"id":366718,"rank":2,"type":{"id":11,"text":"Document"},"url":"https://pubs.usgs.gov/wri/1986/4210/report.pdf","linkFileType":{"id":1,"text":"pdf"}},{"id":366721,"rank":6,"type":{"id":17,"text":"Plate"},"url":"https://pubs.usgs.gov/wri/1986/4210/sheet-3.pdf","text":"Sheet 3","linkFileType":{"id":1,"text":"pdf"}},{"id":366722,"rank":7,"type":{"id":17,"text":"Plate"},"url":"https://pubs.usgs.gov/wri/1986/4210/sheet-4.pdf","text":"Sheet 4","linkFileType":{"id":1,"text":"pdf"}},{"id":366744,"rank":4,"type":{"id":17,"text":"Plate"},"url":"https://pubs.usgs.gov/wri/1986/4210/sheet-1.pdf","text":"Sheet 1","linkFileType":{"id":1,"text":"pdf"}}],"country":"United States","state":"Alabama, Georgia, South Carolina","geographicExtents":"{\"type\":\"FeatureCollection\",\"features\":[{\"type\":\"Feature\",\"geometry\":{\"type\":\"MultiPolygon\",\"coordinates\":[[[[-87.984916,35.005881],[-85.466713,34.982972],[-83.619985,34.986592],[-83.620185,34.992091],[-83.108714,35.000768],[-82.787867,35.085024],[-82.776357,35.081349],[-82.781973,35.066817],[-82.757704,35.068019],[-82.728961,35.091978],[-82.694898,35.098456],[-82.68604,35.124545],[-82.662381,35.118123],[-82.642237,35.129215],[-82.629031,35.126155],[-82.547436,35.160306],[-82.52593,35.156749],[-82.476136,35.175486],[-82.460092,35.178143],[-82.448969,35.165037],[-82.439595,35.165863],[-82.419744,35.198613],[-82.390439,35.215395],[-82.371298,35.181449],[-82.361469,35.190831],[-82.326917,35.185056],[-82.27492,35.200071],[-81.043625,35.149877],[-81.051204,35.133237],[-81.038968,35.126299],[-81.032806,35.108049],[-81.052078,35.096276],[-81.058029,35.07319],[-81.041489,35.044703],[-80.93495,35.107409],[-80.782042,34.935782],[-80.796997,34.823874],[-79.675299,34.804744],[-78.541087,33.851112],[-78.584841,33.844282],[-78.714116,33.800138],[-78.812931,33.743472],[-78.938076,33.639826],[-79.028516,33.533365],[-79.084588,33.483669],[-79.135441,33.403867],[-79.180318,33.254141],[-79.172394,33.206577],[-79.18787,33.173712],[-79.24609,33.124865],[-79.329909,33.089986],[-79.359961,33.006672],[-79.403712,33.003903],[-79.423447,33.015085],[-79.483499,33.001265],[-79.506923,33.032813],[-79.522449,33.03535],[-79.55756,33.021269],[-79.580725,33.006447],[-79.617611,32.952726],[-79.606194,32.925953],[-79.574951,32.934526],[-79.576006,32.906235],[-79.631149,32.888606],[-79.695141,32.850398],[-79.719879,32.825796],[-79.716761,32.813627],[-79.726389,32.805996],[-79.811021,32.77696],[-79.84035,32.756816],[-79.866742,32.757422],[-79.870336,32.727777],[-79.888028,32.695177],[-79.884961,32.684402],[-79.975248,32.639537],[-79.999374,32.611851],[-80.121368,32.590523],[-80.148406,32.578479],[-80.171764,32.546118],[-80.20523,32.555547],[-80.332438,32.478104],[-80.363956,32.496098],[-80.413487,32.470672],[-80.423454,32.497989],[-80.439407,32.503472],[-80.472068,32.496964],[-80.484617,32.460976],[-80.480156,32.447048],[-80.467588,32.425259],[-80.446075,32.423721],[-80.429941,32.401782],[-80.455192,32.326458],[-80.545688,32.282076],[-80.596394,32.273549],[-80.658634,32.248638],[-80.669166,32.216783],[-80.721463,32.160427],[-80.812503,32.109746],[-80.844431,32.109709],[-80.858735,32.099581],[-80.905378,32.051943],[-80.885517,32.0346],[-80.84313,32.024226],[-80.841913,32.002643],[-80.862814,31.969346],[-80.911207,31.943769],[-80.929101,31.944964],[-80.930279,31.956705],[-80.948491,31.95723],[-80.972392,31.94127],[-80.975714,31.923602],[-80.968494,31.915822],[-80.934508,31.90918],[-80.99269,31.857641],[-81.065255,31.877095],[-81.05907,31.850106],[-81.075812,31.829031],[-81.039808,31.823],[-81.036873,31.812721],[-81.068116,31.768735],[-81.130634,31.722692],[-81.192784,31.733245],[-81.203572,31.719448],[-81.161084,31.691401],[-81.149369,31.699304],[-81.131137,31.695774],[-81.133493,31.623348],[-81.173079,31.555908],[-81.186114,31.568032],[-81.204315,31.568183],[-81.214536,31.557601],[-81.254218,31.55594],[-81.260076,31.54828],[-81.258809,31.52906],[-81.217948,31.527284],[-81.199518,31.537596],[-81.17831,31.52241],[-81.278798,31.367214],[-81.282923,31.326491],[-81.25482,31.315452],[-81.274688,31.289454],[-81.288403,31.211065],[-81.314183,31.207938],[-81.339028,31.186918],[-81.368241,31.136534],[-81.399677,31.134113],[-81.401267,31.072781],[-81.420474,31.016703],[-81.451444,31.015515],[-81.493651,30.977528],[-81.475789,30.965976],[-81.453568,30.965573],[-81.447388,30.956732],[-81.426929,30.956615],[-81.420108,30.974076],[-81.408484,30.977718],[-81.403409,30.957914],[-81.405153,30.908203],[-81.460061,30.769912],[-81.45947,30.741979],[-81.444124,30.709714],[-81.472597,30.713312],[-81.489537,30.7261],[-81.528278,30.723359],[-81.544679,30.713969],[-81.601206,30.728141],[-81.617663,30.722046],[-81.625098,30.733017],[-81.646137,30.727591],[-81.662173,30.746521],[-81.672824,30.738935],[-81.692815,30.7471],[-81.719927,30.744634],[-81.745035,30.765039],[-81.768192,30.773954],[-81.779171,30.768062],[-81.806652,30.789683],[-81.868608,30.792754],[-81.89572,30.821098],[-81.910926,30.815889],[-81.949787,30.827493],[-81.959759,30.821168],[-81.961989,30.800443],[-81.979061,30.776415],[-82.017051,30.791657],[-82.022866,30.787991],[-82.011597,30.763122],[-82.035964,30.750998],[-82.043795,30.729641],[-82.036426,30.706585],[-82.050432,30.676266],[-82.049507,30.655548],[-82.027338,30.606726],[-82.012109,30.593773],[-82.005477,30.563495],[-82.018361,30.531184],[-82.016982,30.478779],[-82.036203,30.43846],[-82.036825,30.377884],[-82.047917,30.363265],[-82.081106,30.358806],[-82.116385,30.367335],[-82.165192,30.358035],[-82.189847,30.375938],[-82.210291,30.42459],[-82.201416,30.485164],[-82.225026,30.50783],[-82.234952,30.533066],[-82.231916,30.55627],[-82.214818,30.568517],[-83.499876,30.645671],[-84.86346,30.711506],[-84.8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\"}}]}","noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"4f4e4a51e4b07f02db62a303","contributors":{"authors":[{"text":"Faye, Robert E.","contributorId":92221,"corporation":false,"usgs":true,"family":"Faye","given":"Robert","email":"","middleInitial":"E.","affiliations":[],"preferred":false,"id":197451,"contributorType":{"id":1,"text":"Authors"},"rank":1},{"text":"McFadden, Keith W. keithmc@usgs.gov","contributorId":1446,"corporation":false,"usgs":true,"family":"McFadden","given":"Keith","email":"keithmc@usgs.gov","middleInitial":"W.","affiliations":[],"preferred":true,"id":197450,"contributorType":{"id":1,"text":"Authors"},"rank":2}]}} ,{"id":15444,"text":"ofr86242 - 1986 - Ground-water levels in the alluvial aquifer in eastern Arkansas, 1985","interactions":[],"lastModifiedDate":"2012-02-02T00:07:07","indexId":"ofr86242","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":"86-242","title":"Ground-water levels in the alluvial aquifer in eastern Arkansas, 1985","docAbstract":"This report, prepared by the U.S. Geological Survey in cooperation with the Arkansas Soil and Water Conservation Commission, the U.S. Soil Conservation Service and local Conservation Districts, contains groundwater level measurements in 485 wells tapping the Mississippi River Valley alluvial aquifer of eastern Arkansas. The measurements were made by district Soil Conservation Service personnel during 1985. The purpose of this report is to provide these data to other State and Federal agencies as well as to private landowners. The shallowest pre-pumping water levels occurred in Clay, Independence, and Mississippi County where most water levels were within 20 feet of land surface. Counties where water levels of 100 feet below land surface or greater were measured included: Arkansas, Lonoke, Poinsett, and Prairie. Water-level measurements made during the post-pumping (recovery) season averaged 3.65 feet less than those made during the pre-pumping season. A comparison of pre-pumping water-level measurements made in 1984 to those made in 1985 shows an average rise of 1.0 foot within the area (Edds and Spencer, 1985). (USGS)","language":"ENGLISH","publisher":"U.S. Geological Survey,","doi":"10.3133/ofr86242","usgsCitation":"Plafcan, M., 1986, Ground-water levels in the alluvial aquifer in eastern Arkansas, 1985: U.S. Geological Survey Open-File Report 86-242, iv, 29 p. :ill., map ;28 cm., https://doi.org/10.3133/ofr86242.","productDescription":"iv, 29 p. :ill., map ;28 cm.","costCenters":[],"links":[{"id":148492,"rank":0,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/of/1986/0242/report-thumb.jpg"},{"id":44414,"rank":300,"type":{"id":11,"text":"Document"},"url":"https://pubs.usgs.gov/of/1986/0242/report.pdf","linkFileType":{"id":1,"text":"pdf"}}],"noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"4f4e4aa8e4b07f02db6674f0","contributors":{"authors":[{"text":"Plafcan, Maria","contributorId":20338,"corporation":false,"usgs":true,"family":"Plafcan","given":"Maria","email":"","affiliations":[],"preferred":false,"id":171147,"contributorType":{"id":1,"text":"Authors"},"rank":1}]}} ,{"id":27013,"text":"wri854270 - 1986 - Hydrology of the leeward aquifers, southeast Oahu, Hawaii","interactions":[],"lastModifiedDate":"2022-02-03T21:51:40.946903","indexId":"wri854270","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":"85-4270","title":"Hydrology of the leeward aquifers, southeast Oahu, Hawaii","docAbstract":"The leeward southeast Oahu ground-water area includes the Waialae and Wailupe-Hawaii Kai aquifers. The Waialae aquifer is separated from the ground water of Kaimuki to the west by Palolo valley fill and the Kaau rift zone, and from the Wailupe-Hawaii Kai aquifer to the east by a line of northeast-trending volcanic dikes. The distinct ground-water head changes across these boundaries indicate that the aquifers are separate, with little or no leakage between them.\r\n\r\nA water budget of leeward southeast Oahu determined the quantity and spatial distribution of ground-water recharge. These estimates of recharge, 6 million gallons per day over the Waialae area and 9.1 million gallons per day over the Wailupe-Hawaii Kai area, were used as input to a finite-element two-dimensional ground-water flow model. Ground-water heads were simulated in the modeled aquifer for several pumping scenarios. Projected pumpage from the recently drilled wells int he area is predicted to draw the water table down about one foot from its present mean position.\r\n\r\nThe existing ground-water development of 1.4 million gallons per day is small compared to the quantity of ground water that flows through the area and discharges to the sea. Because the Waialae and Wailupe-Hawaii Kai aquifers are isolated from adjacent ground-water bodies, they can be fully developed without affecting ground-water resources outside the area.","language":"English","publisher":"Geological Survey (U.S.)","doi":"10.3133/wri854270","usgsCitation":"Eyre, P.R., Ewart, C., and Shade, P.J., 1986, Hydrology of the leeward aquifers, southeast Oahu, Hawaii: U.S. Geological Survey Water-Resources Investigations Report 85-4270, vii, 75 p., https://doi.org/10.3133/wri854270.","productDescription":"vii, 75 p.","costCenters":[{"id":525,"text":"Pacific Islands Water Science Center","active":true,"usgs":true}],"links":[{"id":395413,"rank":3,"type":{"id":36,"text":"NGMDB Index Page"},"url":"https://ngmdb.usgs.gov/Prodesc/proddesc_36412.htm"},{"id":55898,"rank":300,"type":{"id":11,"text":"Document"},"url":"https://pubs.usgs.gov/wri/1985/4270/report.pdf","linkFileType":{"id":1,"text":"pdf"}},{"id":123879,"rank":0,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/wri/1985/4270/report-thumb.jpg"}],"country":"United States","state":"Hawaii","otherGeospatial":"Oahu","geographicExtents":"{\n \"type\": \"FeatureCollection\",\n \"features\": [\n {\n \"type\": \"Feature\",\n \"properties\": {},\n \"geometry\": {\n \"type\": \"Polygon\",\n \"coordinates\": [\n [\n [\n -157.825,\n 21.031\n ],\n [\n -157.65,\n 21.031\n ],\n [\n -157.65,\n 21.321\n ],\n [\n -157.825,\n 21.321\n ],\n [\n -157.825,\n 21.031\n ]\n ]\n ]\n }\n }\n ]\n}","noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"4f4e4ad4e4b07f02db683083","contributors":{"authors":[{"text":"Eyre, Paul R.","contributorId":15242,"corporation":false,"usgs":true,"family":"Eyre","given":"Paul","email":"","middleInitial":"R.","affiliations":[],"preferred":false,"id":197406,"contributorType":{"id":1,"text":"Authors"},"rank":1},{"text":"Ewart, Charles J.","contributorId":88759,"corporation":false,"usgs":true,"family":"Ewart","given":"Charles J.","affiliations":[],"preferred":false,"id":197408,"contributorType":{"id":1,"text":"Authors"},"rank":2},{"text":"Shade, Patricia J.","contributorId":30618,"corporation":false,"usgs":true,"family":"Shade","given":"Patricia","email":"","middleInitial":"J.","affiliations":[],"preferred":false,"id":197407,"contributorType":{"id":1,"text":"Authors"},"rank":3}]}} ,{"id":17989,"text":"ofr86309 - 1986 - Description of sediment data collected by the U.S. Geological Survey in small watersheds in coal-mining areas of the eastern United States, 1980-84","interactions":[],"lastModifiedDate":"2016-05-09T10:35:33","indexId":"ofr86309","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":"86-309","title":"Description of sediment data collected by the U.S. Geological Survey in small watersheds in coal-mining areas of the eastern United States, 1980-84","docAbstract":"Hydrologic data were collected by the U.S. Geological Survey from 20 small watersheds in the surface-mining areas of the eastern United States from 1980 through 1984 as part of the Survey1 s coal-hydrology program. Each data set includes sediment-concentration, streamflow, and precipitation data collected at 5- or 15-minute intervals. One reason for collecting the data was to test the sediment component of a watershed model. However, adequate testing requires reliable calibration data collected at several points during the rise and fall of hydrographs of several storms. Therefore, the quantity and quality of the data sets needed to be described to determine which sets could be used to test a model adequately. The data sets are described in a table that presents information about watershed characteristics, period of record, and amount of useful sediment data. Also, similar data sets collected by 10 Survey project offices during other Survey programs are described in a similar table.
","language":"English","publisher":"U.S. Geological Survey","publisherLocation":"Indianapolis, IN","doi":"10.3133/ofr86309","usgsCitation":"Arihood, L.D., 1986, Description of sediment data collected by the U.S. Geological Survey in small watersheds in coal-mining areas of the eastern United States, 1980-84: U.S. Geological Survey Open-File Report 86-309, iii, 15 p. :map ;28 cm., https://doi.org/10.3133/ofr86309.","productDescription":"iii, 15 p. :map ;28 cm.","startPage":"1","endPage":"15","numberOfPages":"18","onlineOnly":"N","additionalOnlineFiles":"N","costCenters":[{"id":346,"text":"Indiana Water Science Center","active":true,"usgs":true}],"links":[{"id":149896,"rank":0,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/of/1986/0309/report-thumb.jpg"},{"id":47233,"rank":300,"type":{"id":11,"text":"Document"},"url":"https://pubs.usgs.gov/of/1986/0309/report.pdf","linkFileType":{"id":1,"text":"pdf"}}],"country":"United States","noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"4f4e4ab0e4b07f02db66d3c9","contributors":{"authors":[{"text":"Arihood, L. D. 0000-0001-5792-3699","orcid":"https://orcid.org/0000-0001-5792-3699","contributorId":74388,"corporation":false,"usgs":true,"family":"Arihood","given":"L.","email":"","middleInitial":"D.","affiliations":[],"preferred":false,"id":178337,"contributorType":{"id":1,"text":"Authors"},"rank":1}]}} ,{"id":1409,"text":"wsp2278 - 1986 - Application of a parameter-estimation technique to modeling the regional aquifer underlying the eastern Snake River plain, Idaho","interactions":[{"subject":{"id":19013,"text":"ofr84461 - 1984 - Application of a parameter-estimation technique to modeling the regional aquifer underlying the eastern Snake River Plain, Idaho","indexId":"ofr84461","publicationYear":"1984","noYear":false,"title":"Application of a parameter-estimation technique to modeling the regional aquifer underlying the eastern Snake River Plain, Idaho"},"predicate":"SUPERSEDED_BY","object":{"id":1409,"text":"wsp2278 - 1986 - Application of a parameter-estimation technique to modeling the regional aquifer underlying the eastern Snake River plain, Idaho","indexId":"wsp2278","publicationYear":"1986","noYear":false,"title":"Application of a parameter-estimation technique to modeling the regional aquifer underlying the eastern Snake River plain, Idaho"},"id":1}],"lastModifiedDate":"2012-02-02T00:05:18","indexId":"wsp2278","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":"2278","title":"Application of a parameter-estimation technique to modeling the regional aquifer underlying the eastern Snake River plain, Idaho","docAbstract":"A nonlinear, least-squares regression technique for the estimation of ground-water flow model parameters was applied to the regional aquifer underlying the eastern Snake River Plain, Idaho. The technique uses a computer program to simulate two-dimensional, steady-state ground-water flow. Hydrologic data for the 1980 water year were used to calculate recharge rates, boundary fluxes, and spring discharges. Ground-water use was estimated from irrigated land maps and crop consumptive-use figures. These estimates of ground-water withdrawal, recharge rates, and boundary flux, along with leakance, were used as known values in the model calibration of transmissivity. Leakance values were adjusted between regression solutions by comparing model-calculated to measured spring discharges. In other simulations, recharge and leakance also were calibrated as prior-information regression parameters, which limits the variation of these parameters using a normalized standard error of estimate. \r\n\r\nResults from a best-fit model indicate a wide areal range in transmissivity from about 0.05 to 44 feet squared per second and in leakance from about 2.2x10 -9 to 6.0 x 10 -8 feet per second per foot. Along with parameter values, model statistics also were calculated, including the coefficient of correlation between calculated and observed head (0.996), the standard error of the estimates for head (40 feet), and the parameter coefficients of variation (about 10-40 percent). Additional boundary flux was added in some areas during calibration to achieve proper fit to ground-water flow directions. Model fit improved significantly when areas that violated model assumptions were removed. It also improved slightly when y-direction (northwest-southeast) transmissivity values were larger than x-direction (northeast-southwest) transmissivity values. The model was most sensitive to changes in recharge, and in some areas, to changes in transmissivity, particularly near the spring discharge area from Milner Dam to King Hill.","language":"ENGLISH","publisher":"U.S. G.P.O. ;\r\nFor sale by the Distribution Branch, Text Products Section, U.S. Geological Survey,","doi":"10.3133/wsp2278","usgsCitation":"Garabedian, S.P., 1986, Application of a parameter-estimation technique to modeling the regional aquifer underlying the eastern Snake River plain, Idaho: U.S. Geological Survey Water Supply Paper 2278, iv, 60 p. :ill., maps ;28 cm.; 4 plates in pocket, https://doi.org/10.3133/wsp2278.","productDescription":"iv, 60 p. :ill., maps ;28 cm.; 4 plates in pocket","costCenters":[],"links":[{"id":138002,"rank":0,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/wsp/2278/report-thumb.jpg"},{"id":26500,"rank":400,"type":{"id":17,"text":"Plate"},"url":"https://pubs.usgs.gov/wsp/2278/plate-1.pdf","linkFileType":{"id":1,"text":"pdf"}},{"id":26501,"rank":401,"type":{"id":17,"text":"Plate"},"url":"https://pubs.usgs.gov/wsp/2278/plate-2.pdf","linkFileType":{"id":1,"text":"pdf"}},{"id":26502,"rank":402,"type":{"id":17,"text":"Plate"},"url":"https://pubs.usgs.gov/wsp/2278/plate-3.pdf","linkFileType":{"id":1,"text":"pdf"}},{"id":26503,"rank":403,"type":{"id":17,"text":"Plate"},"url":"https://pubs.usgs.gov/wsp/2278/plate-4.pdf","linkFileType":{"id":1,"text":"pdf"}},{"id":26504,"rank":300,"type":{"id":11,"text":"Document"},"url":"https://pubs.usgs.gov/wsp/2278/report.pdf","linkFileType":{"id":1,"text":"pdf"}}],"noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"4f4e4ac6e4b07f02db67ab19","contributors":{"authors":[{"text":"Garabedian, Stephen P.","contributorId":91090,"corporation":false,"usgs":true,"family":"Garabedian","given":"Stephen","email":"","middleInitial":"P.","affiliations":[],"preferred":false,"id":143703,"contributorType":{"id":1,"text":"Authors"},"rank":1}]}} ,{"id":14402,"text":"ofr86588 - 1986 - Genesis and evolution of the Baid al Jimalah tungsten deposit, Kingdom of Saudi Arabia","interactions":[],"lastModifiedDate":"2015-09-22T14:37:05","indexId":"ofr86588","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":"86-588","title":"Genesis and evolution of the Baid al Jimalah tungsten deposit, Kingdom of Saudi Arabia","docAbstract":"The Baid al Jimalah tungsten deposit flat 25°09 N., long 42°41' E.) is a swarm of steeply dipping, sheeted, tungsten-bearing quartz veins. It is spatially, temporally, and genetically associated with a 569 Ma, highly differentiated, porphyritic granite that intrudes late Proterozoic, immature sandstones of the Murdama group.
\nThe bulk of the vein constituents came from hydrothermal fluids exsolved from a granite cupola at a depth of about 3.1 km during a single cycle of magma intrusion and hydrothermal mineralization. Hypogene mineralization can be divided into 3 main periods: early quartz-molybdenite stockwork veins, wolframite- and scheelite-bearing greisen veins, and late, barren veins. Each of the three periods can be divided into several stages that are transitional to each other. The greisen veins, in particular, show replacement of earlier mineral assemblages by later ones. The veins at Baid al Jimalah East, approximately 1.5 km to the east of the Baid al Jimalah tungsten deposit, are genetically related to it and probably formed while the greisen mineralization was being deposited.
\nEarly stockwork mineralization was formed near magmatic temperatures (580°-700°C) from low salinity fluids (1-2 weight percent NaCl equivalent). Two fluids were present, one low density and CO2 rich, the other high density and H2O rich. Greisen mineralization was formed from fluids in the liquid state at temperatures mostly between 390° and 430°C with salinities between 4.5 and 10.9 weight percent NaCl equivalent. Late, barren mineralization formed from liquids with salinities between 0.5 and 3.0 weight percent NaCl equivalent and at temperatures at least as low as 238°C. The veins at Baid al Jimalah East formed from liquids between 0 and 4.2 weight percent NaCl equivalent at temperatures largely between 300° and 375°C. Depth of mineralization was greater than 3.1 km. The temperatures given above have been corrected for pressure assuming this depth, and are 75-80°C higher than the fluid inclusion filling temperatures. Important volatile constituents of the hydrothermal fluids were CO2 and CH4, in addition to H2O and HF.
\nBaid al Jimalah is similar in character and origin to other tungsten-tin greisen deposits in the world, especially the Hemerdon deposit in Devon, England. It is also analogous to Climax-type molybdenum deposits, which contain virtually identical mineral assemblages, but with the relative intensities of the molybdenum and tungsten mineralization reversed.
","language":"English","publisher":"U.S. Geological Survey","publisherLocation":"Reston, VA","doi":"10.3133/ofr86588","usgsCitation":"Kamilli, R.J., 1986, Genesis and evolution of the Baid al Jimalah tungsten deposit, Kingdom of Saudi Arabia: U.S. Geological Survey Open-File Report 86-588, iv, 54 p., https://doi.org/10.3133/ofr86588.","productDescription":"iv, 54 p.","onlineOnly":"N","additionalOnlineFiles":"N","costCenters":[],"links":[{"id":43083,"rank":300,"type":{"id":11,"text":"Document"},"url":"https://pubs.usgs.gov/of/1986/0588/report.pdf","linkFileType":{"id":1,"text":"pdf"}},{"id":148345,"rank":0,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/of/1986/0588/report-thumb.jpg"}],"country":"Saudi Arabia","geographicExtents":"{\n \"type\": \"FeatureCollection\",\n \"features\": [\n {\n \"type\": \"Feature\",\n \"properties\": {},\n \"geometry\": {\n \"type\": \"Polygon\",\n \"coordinates\": [\n [\n [\n 42.5,\n 25\n ],\n [\n 42.5,\n 25.5\n ],\n [\n 43,\n 25.5\n ],\n [\n 43,\n 25\n ],\n [\n 42.5,\n 25\n ]\n ]\n ]\n }\n }\n ]\n}","noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"4f4e4b24e4b07f02db6aebc3","contributors":{"authors":[{"text":"Kamilli, Robert J. bkamilli@usgs.gov","contributorId":5795,"corporation":false,"usgs":true,"family":"Kamilli","given":"Robert","email":"bkamilli@usgs.gov","middleInitial":"J.","affiliations":[{"id":5079,"text":"Pacific Regional Director's Office","active":true,"usgs":true}],"preferred":true,"id":169393,"contributorType":{"id":1,"text":"Authors"},"rank":1}]}} ,{"id":29733,"text":"wri854165 - 1986 - Geohydrology and ground-water quality on Shelter Island, Suffolk County, New York, 1983-84","interactions":[],"lastModifiedDate":"2012-02-02T00:09:02","indexId":"wri854165","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":"85-4165","title":"Geohydrology and ground-water quality on Shelter Island, Suffolk County, New York, 1983-84","docAbstract":"Shelter Island, with an area of about 11 sq mi, lies between the north and south forks of eastern Long Island in Suffolk County. The thin upper glacial (water table) aquifer contains the lens-shaped freshwater body that is the sole source of freshwater for the Town 's population of about 2,200 year-round and 10,000 summer residents. Chloride concentrations in groundwater above the freshwater/saltwater interface, defined as 40 mg/L Cl-, are relatively constant with depth. Below the interface, however, chloride concentrations increase rapidly--as much as an order of magnitude within 10 ft--until they reach 19 ,000 mg/L, the chloride concentration of seawater. Chloride concentrations in shallow groundwater from wells screened in or near the zone of diffusion may range over two orders of magnitude in response to variations in recharge and groundwater withdrawal. After the summer season of relatively low recharge and peak water demand, the thickness of the freshwater lens is < 20 ft in many nearshore areas. A map showing the configuration of the water table in December 1983 indicates freshwater mounds in the center of the island, in the Mashomack Preserve, on the Dering Harbor-Hay Beach peninsula, and in the area between Shelter Island Heights and West Neck Bay. Areas in which the supply of fresh groundwater is severely limited include all coastal areas, the southernmost part of the West Neck peninsula, and Little Ram Island. Water levels in most locations are < 6 ft above sea level. During 1974-83, seasonal water table fluctuations were greater than variations that occurred from year to year. Groundwater quality on Shelter Island is generally good and usually meets Federal and State drinking water standards. However, many wells contain water that has excessive concentrations of dissolved iron and manganese (up to 5.0 mg/L and 3.0 mg/L, respectively), and elevated chloride and dissolved solids concentrations (up to 310 mg/L and 585 mg/L, respectively) have been found in some nearshore wells. Increased withdrawal of fresh groundwater in nearshore areas will cause further landward movement of saline groundwater; in other areas, excessive pumping may cause upconing. A system of widely spaced pumping wells that avoid nearshore areas would minimize these effects. (Lantz-PTT)","language":"ENGLISH","publisher":"U.S. Geological Survey,","doi":"10.3133/wri854165","usgsCitation":"Simmons, D.L., 1986, Geohydrology and ground-water quality on Shelter Island, Suffolk County, New York, 1983-84: U.S. Geological Survey Water-Resources Investigations Report 85-4165, v, 39 p. :ill., maps ;28 cm., https://doi.org/10.3133/wri854165.","productDescription":"v, 39 p. :ill., maps ;28 cm.","costCenters":[],"links":[{"id":124346,"rank":0,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/wri/1985/4165/report-thumb.jpg"},{"id":58540,"rank":300,"type":{"id":11,"text":"Document"},"url":"https://pubs.usgs.gov/wri/1985/4165/report.pdf","linkFileType":{"id":1,"text":"pdf"}}],"noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"4f4e4b1be4b07f02db6a8d10","contributors":{"authors":[{"text":"Simmons, D. L.","contributorId":105325,"corporation":false,"usgs":true,"family":"Simmons","given":"D.","email":"","middleInitial":"L.","affiliations":[],"preferred":false,"id":202032,"contributorType":{"id":1,"text":"Authors"},"rank":1}]}} ,{"id":14115,"text":"ofr86525B - 1986 - Bibliographies and location maps of aeromagnetic and aeroradiometric publications of the states west of the Mississippi River and east of approximately 104 degrees longitude","interactions":[],"lastModifiedDate":"2024-06-11T19:34:13.610236","indexId":"ofr86525B","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":"86-525","chapter":"B","title":"Bibliographies and location maps of aeromagnetic and aeroradiometric publications of the states west of the Mississippi River and east of approximately 104 degrees longitude","docAbstract":"Bibliographies and location maps of selected publications containing aeromagnetic and/or aeroradiometric data have been compiled for each state. These state indexes have been grouped together to form seven open-file reports: four for the conterminous United States (see index map below), one for Alaska and Hawaii, one for Puerto Rico and large areas of the United States (U.S. Regional), and one for the Department of Energy (DOE) National Uranium Resource Evaluation (NURE) Program reports.
","language":"English","publisher":"U.S. Geological Survey","doi":"10.3133/ofr86525B","usgsCitation":"Hill, P.L., 1986, Bibliographies and location maps of aeromagnetic and aeroradiometric publications of the states west of the Mississippi River and east of approximately 104 degrees longitude: U.S. Geological Survey Open-File Report 86-525, 48 p., https://doi.org/10.3133/ofr86525B.","productDescription":"48 p.","costCenters":[],"links":[{"id":145930,"rank":1,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/of/1986/0525-b/report-thumb.jpg"},{"id":429911,"rank":2,"type":{"id":11,"text":"Document"},"url":"https://pubs.usgs.gov/of/1986/0525-b/report.pdf","linkFileType":{"id":1,"text":"pdf"}}],"country":"United States","state":"Arkansas, Iowa, Kansas, Louisiana, Minnesota, Missouri, Nebraska, North Dakota, Oklahoma, South Dakota, Texas","otherGeospatial":"states west of the Mississippi River and east of approximately 104 degrees longitude","geographicExtents":"{\n \"type\": \"FeatureCollection\",\n \"features\": [\n {\n \"type\": \"Feature\",\n \"properties\": {},\n \"geometry\": {\n \"coordinates\": [\n [\n [\n -104.14299366032347,\n 49.079090763509726\n ],\n [\n -104.14299366032347,\n 28.17534714104103\n ],\n [\n -90.34370419028087,\n 28.17534714104103\n ],\n [\n -90.34370419028087,\n 49.079090763509726\n ],\n [\n -104.14299366032347,\n 49.079090763509726\n ]\n ]\n ],\n \"type\": \"Polygon\"\n }\n }\n ]\n}","noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"4f4e4a52e4b07f02db62a7ba","contributors":{"authors":[{"text":"Hill, Patricia L. pathill@usgs.gov","contributorId":1327,"corporation":false,"usgs":true,"family":"Hill","given":"Patricia","email":"pathill@usgs.gov","middleInitial":"L.","affiliations":[],"preferred":true,"id":168948,"contributorType":{"id":1,"text":"Authors"},"rank":1}]}} ,{"id":28008,"text":"wri844353 - 1986 - Three-dimensional model simulation of steady-state ground-water flow in the Albuquerque-Belen Basin, New Mexico","interactions":[],"lastModifiedDate":"2012-02-02T00:08:41","indexId":"wri844353","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":"84-4353","title":"Three-dimensional model simulation of steady-state ground-water flow in the Albuquerque-Belen Basin, New Mexico","docAbstract":"As part of the Southwest Alluvial Basins study, model was constructed to simulate the alluvial aquifer system underlying the Albuquerque-Belen Basin. The model was used to simulate the steady-state flow condition assumed to have existed prior to 1960. Until this time there apparently were no long-term groundwater level changes of a significant magnitude outside the immediate vicinity of Albuquerque. Therefore, the construction of a steady-state flow model of the aquifer system based on reported hydrologic data predating 1960 was justified. During construction of the steady-state model, simulated hydraulic conductivity values were adjusted, within acceptable physical limits, until a best fit between measured or reported and computed heads at 34 control wells was achieved. The modeled area was divided into six sub-areas, or zones, within each of which hydraulic conductivity was assumed to be uniform. The model consisted of six layers for each of which simulated transmissivity was proportional to the layer thickness. Adjustments to simulated hydraulic conductivity values in the different zones resulted in final values that ranged from a low of 0.25 ft/day in the west to 50 ft/day in the eastern part of the basin. The error of the simulation, defined as the absolute difference between the computed and the measured or reported water level at the corresponding point in the physical system being modeled, ranged from 0.6 ft to 36 ft, with an average of 14.6 ft for the 34 control wells. (Author 's abstract)","language":"ENGLISH","publisher":"U.S. Geological Survey,","doi":"10.3133/wri844353","usgsCitation":"Kernodle, J.M., and Scott, W.B., 1986, Three-dimensional model simulation of steady-state ground-water flow in the Albuquerque-Belen Basin, New Mexico: U.S. Geological Survey Water-Resources Investigations Report 84-4353, v, 58 p. :ill., maps ;28 cm., https://doi.org/10.3133/wri844353.","productDescription":"v, 58 p. :ill., maps ;28 cm.","costCenters":[],"links":[{"id":158694,"rank":0,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/wri/1984/4353/report-thumb.jpg"},{"id":56833,"rank":300,"type":{"id":11,"text":"Document"},"url":"https://pubs.usgs.gov/wri/1984/4353/report.pdf","linkFileType":{"id":1,"text":"pdf"}}],"noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"4f4e4b06e4b07f02db69a2fe","contributors":{"authors":[{"text":"Kernodle, J. M.","contributorId":81139,"corporation":false,"usgs":true,"family":"Kernodle","given":"J.","email":"","middleInitial":"M.","affiliations":[],"preferred":false,"id":199059,"contributorType":{"id":1,"text":"Authors"},"rank":1},{"text":"Scott, W. B.","contributorId":87887,"corporation":false,"usgs":true,"family":"Scott","given":"W.","email":"","middleInitial":"B.","affiliations":[],"preferred":false,"id":199060,"contributorType":{"id":1,"text":"Authors"},"rank":2}]}} ,{"id":14113,"text":"ofr86525D - 1986 - Bibliographies and location maps of aeromagnetic and aeroradiometric publications for the states east of the Mississippi River and south of the Ohio and Potomac rivers","interactions":[],"lastModifiedDate":"2024-07-10T19:54:34.83269","indexId":"ofr86525D","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":"86-525","chapter":"D","title":"Bibliographies and location maps of aeromagnetic and aeroradiometric publications for the states east of the Mississippi River and south of the Ohio and Potomac rivers","docAbstract":"Bibliographies and location maps of selected publications containing aeromagnetic and/or aeroradiometric data have been compiled for each state. These state indexes have been grouped together to form seven open-file reports: four for the conterminous United States (see index map below), one for Alaska and Hawaii, one for Puerto Rico and large areas of the United States (U.S. Regional), and one for the Department of Energy (DOE) National Uranium Resource Evaluation (NURE) Program reports.
","language":"English","publisher":"U.S. Geological Survey","doi":"10.3133/ofr86525D","usgsCitation":"Hill, P.L., 1986, Bibliographies and location maps of aeromagnetic and aeroradiometric publications for the states east of the Mississippi River and south of the Ohio and Potomac rivers: U.S. Geological Survey Open-File Report 86-525, 57 p., https://doi.org/10.3133/ofr86525D.","productDescription":"57 p.","costCenters":[],"links":[{"id":430918,"rank":2,"type":{"id":11,"text":"Document"},"url":"https://pubs.usgs.gov/of/1986/0525-d/report.pdf","linkFileType":{"id":1,"text":"pdf"}},{"id":145928,"rank":1,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/of/1986/0525-d/report-thumb.jpg"}],"country":"United States","state":"Alabama, Florida, Georgia, Kentucky, Mississippi, North Carolina, South Carolina, Tennessee, Virginia, West Virginia","geographicExtents":"{\n \"type\": \"FeatureCollection\",\n \"features\": [\n {\n \"type\": \"Feature\",\n \"properties\": {},\n \"geometry\": {\n \"coordinates\": [\n [\n [\n -89.86975209915929,\n 37.59658513375486\n ],\n [\n -89.86975209915929,\n 25.180019543822752\n ],\n [\n -76.97459987799849,\n 25.180019543822752\n ],\n [\n -76.97459987799849,\n 37.59658513375486\n ],\n [\n -89.86975209915929,\n 37.59658513375486\n ]\n ]\n ],\n \"type\": \"Polygon\"\n }\n }\n ]\n}","noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"4f4e4a52e4b07f02db62acf1","contributors":{"authors":[{"text":"Hill, Patricia L. pathill@usgs.gov","contributorId":1327,"corporation":false,"usgs":true,"family":"Hill","given":"Patricia","email":"pathill@usgs.gov","middleInitial":"L.","affiliations":[],"preferred":true,"id":168946,"contributorType":{"id":1,"text":"Authors"},"rank":1}]}} ,{"id":14112,"text":"ofr86525C - 1986 - Bibliographies and location maps of aeromagnetic and aeroradiometric publications for the states east of the Mississippi River and north of the Ohio and Potomac rivers","interactions":[],"lastModifiedDate":"2024-07-10T20:07:47.839363","indexId":"ofr86525C","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":"86-525","chapter":"C","title":"Bibliographies and location maps of aeromagnetic and aeroradiometric publications for the states east of the Mississippi River and north of the Ohio and Potomac rivers","docAbstract":"Bibliographies and location maps of selected publications containing aeromagnetic and/or aeroradiometric data have been compiled for each state. These state indexes have been grouped together to form seven open-file reports: four for the conterminous United States (see index map below), one for Alaska and Hawaii, one for Puerto Rico and large areas of the United States (U.S. Regional), and one for the Department of Energy (DOE) National Uranium Resource Evaluation (NURE) Program reports.
","language":"English","publisher":"U.S. Geological Survey","doi":"10.3133/ofr86525C","usgsCitation":"Hill, P.L., 1986, Bibliographies and location maps of aeromagnetic and aeroradiometric publications for the states east of the Mississippi River and north of the Ohio and Potomac rivers: U.S. Geological Survey Open-File Report 86-525, 90 p., https://doi.org/10.3133/ofr86525C.","productDescription":"90 p.","costCenters":[],"links":[{"id":430926,"rank":2,"type":{"id":11,"text":"Document"},"url":"https://pubs.usgs.gov/of/1986/0525-c/report.pdf","linkFileType":{"id":1,"text":"pdf"}},{"id":145927,"rank":1,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/of/1986/0525-c/report-thumb.jpg"}],"country":"United States","state":"Connecticut, Delaware, Illinois, Indiana, Maine, Maryland, Massachusetts, Michigan, New Hampshire, New Jersey, New York, Ohio, Pennsylvania, Rhode Island, Vermont, Wisconsin","geographicExtents":"{\n \"type\": \"FeatureCollection\",\n \"features\": [\n {\n \"type\": \"Feature\",\n \"properties\": {},\n \"geometry\": {\n \"coordinates\": [\n [\n [\n -92.41774076717402,\n 46.883809678880965\n ],\n [\n -92.41774076717402,\n 38.282193972189646\n ],\n [\n -67.51383254688923,\n 38.282193972189646\n ],\n [\n -67.51383254688923,\n 46.883809678880965\n ],\n [\n -92.41774076717402,\n 46.883809678880965\n ]\n ]\n ],\n \"type\": \"Polygon\"\n }\n }\n ]\n}","noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"4f4e4a52e4b07f02db62acea","contributors":{"authors":[{"text":"Hill, Patricia L. pathill@usgs.gov","contributorId":1327,"corporation":false,"usgs":true,"family":"Hill","given":"Patricia","email":"pathill@usgs.gov","middleInitial":"L.","affiliations":[],"preferred":true,"id":168945,"contributorType":{"id":1,"text":"Authors"},"rank":1}]}} ,{"id":14068,"text":"ofr85151 - 1986 - Floods of June-July 1982, in Iowa","interactions":[],"lastModifiedDate":"2016-03-07T13:45:30","indexId":"ofr85151","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":"85-151","title":"Floods of June-July 1982, in Iowa","docAbstract":"Record flood-peak discharges occurred in June and July, 1982, in southwestern, south-central, and east-central Iowa. The record flood peaks resulted from rainfalls of 6 to 8 inches on soil saturated from persistent moderate to heavy rainfalls that began in May and continued through mid July.
\nMay was the wettest across Iowa since 1959, averaging just over 7 inches statewide to rank as Iowa's 6th wettest May in 100 years of State records. Statewide rainfall for July averaged in excess of 6 inches to rank among the 3rd wettest July in Iowa since 1958.
\nOne of the greatest floods ever recorded in the State occurred on Cedar Creek in south-central Iowa on July 3, 1982. The flood peak discharge at the gaging station near Bussey (05489000) was 4.4 times that of a regional 100-year flood. The gage height exceeded the record flood stage of July 4, 1981, by 5.78 feet. Flood peak discharges on other streams ranged up to 2.7 times that of a regional 100-year flood.
","language":"English","publisher":"U.S. Geological Survey","publisherLocation":"Iowa City","doi":"10.3133/ofr85151","collaboration":"Prepared in cooperation with: Highway Research Board, Highway Division, Iowa Department of Transportation","usgsCitation":"Heinitz, A., 1986, Floods of June-July 1982, in Iowa: U.S. Geological Survey Open-File Report 85-151, v, 24 p.: ill., maps; 28 cm., https://doi.org/10.3133/ofr85151.","productDescription":"v, 24 p.: ill., maps; 28 cm.","onlineOnly":"N","additionalOnlineFiles":"N","costCenters":[{"id":351,"text":"Iowa Water Science Center","active":true,"usgs":true}],"links":[{"id":42710,"rank":300,"type":{"id":11,"text":"Document"},"url":"https://pubs.usgs.gov/of/1985/0151/report.pdf","linkFileType":{"id":1,"text":"pdf"}},{"id":147047,"rank":0,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/of/1985/0151/report-thumb.jpg"}],"country":"United 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Antonio area, Texas","docAbstract":"Twenty-seven geohydrology sections illustrate structural and stratigraphic relationships within the 180-mi-long Edwards aquifer. These sections were used to interpret the location of barriers within the Edwards aquifer. The sections are oriented generally south-southeast, which is approximately normal to both the east-northeast trending Edwards aquifer and the strike of the major faults of the Balcones fault zone. Section lengths represent the distance necessary to cross the aquifer, which is 5 to 40 mi wide. The updip (north) end of the sections are drawn to indicate exposures of the Glen Rose Formation; from there the sections indicate downdip geologic conditions within the freshwater zone and the saline water zone. The sections are approximately parallel and illustrate geologic conditions at 5- to 10-mile intervals. The sections indicate the geologic conditions from near the eastern boundary of the aquifer in Hays County to near the western boundary of the aquifer in Uvalde County. Several sections show places where faults have sufficient vertical displacement to offset the entire, or almost entire, thickness of the aquifer. At these places the faults are barriers to groundwater flow directly downdip across the fault. (Author 's abstract)
","language":"English","publisher":"U.S. Geological Survey","publisherLocation":"Austin, TX","doi":"10.3133/wri854259","usgsCitation":"Small, T.A., 1986, Hydrogeologic sections of the Edwards Aquifer and its confining units in the San Antonio area, Texas: U.S. Geological Survey Water-Resources Investigations Report 85-4259, Report: iii, 52 p.; 7 Plates: 14.08 x 8.63 inches or smaller, https://doi.org/10.3133/wri854259.","productDescription":"Report: iii, 52 p.; 7 Plates: 14.08 x 8.63 inches or smaller","numberOfPages":"46","onlineOnly":"N","additionalOnlineFiles":"N","costCenters":[{"id":583,"text":"Texas Water Science Center","active":true,"usgs":true}],"links":[{"id":58590,"rank":400,"type":{"id":17,"text":"Plate"},"url":"https://pubs.usgs.gov/wri/1985/4259/plate-1.pdf","linkFileType":{"id":1,"text":"pdf"}},{"id":58591,"rank":401,"type":{"id":17,"text":"Plate"},"url":"https://pubs.usgs.gov/wri/1985/4259/plate-2.pdf","linkFileType":{"id":1,"text":"pdf"}},{"id":122765,"rank":0,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/wri/1985/4259/report-thumb.jpg"},{"id":58592,"rank":402,"type":{"id":17,"text":"Plate"},"url":"https://pubs.usgs.gov/wri/1985/4259/plate-3.pdf","linkFileType":{"id":1,"text":"pdf"}},{"id":58593,"rank":403,"type":{"id":17,"text":"Plate"},"url":"https://pubs.usgs.gov/wri/1985/4259/plate-4.pdf","linkFileType":{"id":1,"text":"pdf"}},{"id":58594,"rank":404,"type":{"id":17,"text":"Plate"},"url":"https://pubs.usgs.gov/wri/1985/4259/plate-5.pdf","linkFileType":{"id":1,"text":"pdf"}},{"id":58595,"rank":405,"type":{"id":17,"text":"Plate"},"url":"https://pubs.usgs.gov/wri/1985/4259/plate-6.pdf","linkFileType":{"id":1,"text":"pdf"}},{"id":58596,"rank":406,"type":{"id":17,"text":"Plate"},"url":"https://pubs.usgs.gov/wri/1985/4259/plate-7.pdf","linkFileType":{"id":1,"text":"pdf"}},{"id":58597,"rank":300,"type":{"id":11,"text":"Document"},"url":"https://pubs.usgs.gov/wri/1985/4259/report.pdf","linkFileType":{"id":1,"text":"pdf"}}],"country":"United States","state":"Texas","city":"San Antonio","otherGeospatial":"Edwards Aquifer","noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"4f4e4a4ee4b07f02db627a09","contributors":{"authors":[{"text":"Small, Ted A.","contributorId":77533,"corporation":false,"usgs":true,"family":"Small","given":"Ted","email":"","middleInitial":"A.","affiliations":[],"preferred":false,"id":202135,"contributorType":{"id":1,"text":"Authors"},"rank":1}]}} ,{"id":28000,"text":"wri864038 - 1986 - Water demands in Kansas, 1944-84","interactions":[],"lastModifiedDate":"2012-02-02T00:08:40","indexId":"wri864038","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":"86-4038","title":"Water demands in Kansas, 1944-84","docAbstract":"The State of Kansas has administered water rights according to an appropriations doctrine since 1945. Water rights are issued by the Kansas State Board of Agriculture, Division of Water Resources, for eight categories of beneficial use. Water rights data and limited information on reported water use are stored on a computerized State data base; the U.S. Geological Survey cooperates with the State on maintenance of this system. This report analyzes trends in appropriations from 1944-84 for surface and groundwater for three major categories of use: irrigation, public supply, and industry. Demands for water, represented by these appropriations, are compared for three geographic areas within the State. These areas correspond to general patterns of water availability, population, and enterprises. As of 1984, 87% of the water appropriated for the three major types of use was for irrigation; most of this demand was for groundwater in the western one-third of the State. Seventy-five percent of the water demands in the central one-third of Kansas were met by groundwater; appropriations for irrigation represent the largest demand on water supplies in this area but must compete with appropriations for public supply and industry. Demands for surface water have increased substantially only in the eastern part of the State for industrial use and public supplies. The most prominent trends in water rights permit activity were related to climatic fluctuations, particularly the drought of the 1950's, legislative changes in the 1970 's requiring permits, and growth of urban populations in the central and eastern areas of the State. Analysis of trends in water appropriations can be useful in understanding the water issues facing Kansas in the future. 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F.","contributorId":100378,"corporation":false,"usgs":true,"family":"Kenny","given":"J.","email":"","middleInitial":"F.","affiliations":[],"preferred":false,"id":199044,"contributorType":{"id":1,"text":"Authors"},"rank":1}]}} ,{"id":13849,"text":"ofr85559 - 1986 - Water use on the Snake River plain, Idaho and eastern Oregon","interactions":[{"subject":{"id":13849,"text":"ofr85559 - 1986 - Water use on the Snake River plain, Idaho and eastern Oregon","indexId":"ofr85559","publicationYear":"1986","noYear":false,"title":"Water use on the Snake River plain, Idaho and eastern Oregon"},"predicate":"SUPERSEDED_BY","object":{"id":38450,"text":"pp1408E - 1988 - Water use on the Snake River plain, Idaho and eastern Oregon","indexId":"pp1408E","publicationYear":"1988","noYear":false,"chapter":"E","title":"Water use on the Snake River plain, Idaho and eastern Oregon"},"id":1}],"supersededBy":{"id":38450,"text":"pp1408E - 1988 - Water use on the Snake River plain, Idaho and eastern Oregon","indexId":"pp1408E","publicationYear":"1988","noYear":false,"title":"Water use on the Snake River plain, Idaho and eastern Oregon"},"lastModifiedDate":"2019-11-12T15:01:43","indexId":"ofr85559","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":"85-559","title":"Water use on the Snake River plain, Idaho and eastern Oregon","docAbstract":"No abstract available.
","language":"English","publisher":"U.S. Geological Survey","publisherLocation":"Reston, VA","doi":"10.3133/ofr85559","usgsCitation":"Goodell, S.A., 1986, Water use on the Snake River plain, Idaho and eastern Oregon: U.S. Geological Survey Open-File Report 85-559, vii, 94 p., https://doi.org/10.3133/ofr85559.","productDescription":"vii, 94 p.","costCenters":[],"links":[{"id":147171,"rank":0,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/of/1985/0559/report-thumb.jpg"},{"id":369150,"rank":2,"type":{"id":11,"text":"Document"},"url":"https://pubs.usgs.gov/of/1985/0559/report.pdf","linkFileType":{"id":1,"text":"pdf"}}],"country":"United States","state":"Idaho, Oregon","otherGeospatial":"Snake River plain","noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"4f4e4a0de4b07f02db5fd15b","contributors":{"authors":[{"text":"Goodell, S. A.","contributorId":38168,"corporation":false,"usgs":true,"family":"Goodell","given":"S.","email":"","middleInitial":"A.","affiliations":[],"preferred":false,"id":168500,"contributorType":{"id":1,"text":"Authors"},"rank":1}]}} ]}