No abstract available.
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","language":"English","publisher":"U.S. Geological Survey","doi":"10.3133/gp8","usgsCitation":"Henderson, J.R., and Meuschke, J.L., 1950, Total intensity aeromagnetic map of Dubois County, Indiana: U.S. Geological Survey Geophysical Investigations Map 8, 1 Plate: 27.75 × 26.75 inches, https://doi.org/10.3133/gp8.","productDescription":"1 Plate: 27.75 × 26.75 inches","costCenters":[],"links":[{"id":260568,"rank":900,"type":{"id":17,"text":"Plate"},"url":"https://pubs.usgs.gov/gp/0008/plate-1.pdf"},{"id":186790,"rank":0,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/thumbnails/usgs_thumb.jpg"},{"id":392741,"rank":3,"type":{"id":36,"text":"NGMDB Index Page"},"url":"https://ngmdb.usgs.gov/Prodesc/proddesc_3574.htm"}],"scale":"63360","country":"United States","state":"Indiana","county":"Dubois County","geographicExtents":"{\n \"type\": \"FeatureCollection\",\n \"features\": [\n {\n \"type\": \"Feature\",\n \"properties\": {},\n \"geometry\": {\n \"type\": \"Polygon\",\n \"coordinates\": [\n [\n [\n -87.0833,\n 38.5167\n ],\n [\n -86.7083,\n 38.5167\n ],\n [\n -86.7083,\n 38.3667\n ],\n [\n -87.0833,\n 38.3667\n ],\n [\n -87.0833,\n 38.5167\n ]\n ]\n ]\n }\n }\n ]\n}","noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"4f4e4a50e4b07f02db628cfe","contributors":{"authors":[{"text":"Henderson, John R. 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The study area coincides in part with the outcrop of the Vamoosa-Ada aquifer of Pennsylvanian age. Water samples collected from 180 wells completed in the Vamoosa-Ada aquifer and at 167 sites from streams draining the Vamoosa-Ada aquifer show scattered occurrences of water quality degradation by brine. Degradation of water quality by brine is indicated where: (1) chloride concentration is > or = to 400 mg/L; (2) bromide concentration is > or = 2 mg/L; (3) the ratio of sodium plus chloride to dissolved solids is > or = 0.64. Ratios of secondary importance that also indicate water quality degradation by brine in the area are: (1) a ratio of lithium to bromide < or = 0.01, when the chloride concentration is > or = 400 mg/L; (2) a sodium/chloride ratio of about 0.46; (3) a sodium/bromide ratio of about 92; and (4) a bromide/chloride ratio of about 0.0048. Values for bromide, lithium, strontium, dissolved solids, calcium, magnesium, sodium, chloride, and sulfate concentrations were subjected to analysis of variance based on use of the index values in partition data sets. The analysis of variance showed the significance of the indexes for all constituents except sulfate. The two most reliable brine indicators are chloride and bromide. Statistically, chloride is a slightly more reliable index than bromide. The developed indexes can be used to indicate water quality degradation by brine. Accuracy is improved if both indexes are used. When geophysical logs from 133 pairs of oil and gas wells were analyzed, data from 5 pairs of wells indicated a possible rise in the interface between fresh water and salt water in the Vamoosa-Ada aquifer. Therefore , any rise of the interface is local rather than regional. The criteria developed in this study indicate that brine has degraded water quality at 63 sites on streams draining the Vamoosa-Ada aquifer, at 15 water wells completed in the Vamoosa-Ada aquifer, and at 5 oil and gas wells penetrating the Vamoosa-Ada aquifer. (Author 's abstract)","language":"ENGLISH","publisher":"[Interior Duplicating Section],","doi":"10.3133/cir89","usgsCitation":"Read, C.B., Duffner, R.T., Wood, G., and Zapp, A., 1950, Coal resources of New Mexico: U.S. Geological Survey Circular 89, ii, 24 p. :fold. map, tables. ;27 cm., https://doi.org/10.3133/cir89.","productDescription":"ii, 24 p. :fold. map, tables. ;27 cm.","costCenters":[],"links":[{"id":123345,"rank":0,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/circ/1950/0089/report-thumb.jpg"},{"id":30546,"rank":400,"type":{"id":17,"text":"Plate"},"url":"https://pubs.usgs.gov/circ/1950/0089/plate-1.pdf","linkFileType":{"id":1,"text":"pdf"}},{"id":30547,"rank":300,"type":{"id":11,"text":"Document"},"url":"https://pubs.usgs.gov/circ/1950/0089/report.pdf","linkFileType":{"id":1,"text":"pdf"}}],"noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"4f4e4804e4b07f02db4ceff3","contributors":{"authors":[{"text":"Read, Charles Brian","contributorId":68716,"corporation":false,"usgs":true,"family":"Read","given":"Charles","email":"","middleInitial":"Brian","affiliations":[],"preferred":false,"id":147108,"contributorType":{"id":1,"text":"Authors"},"rank":1},{"text":"Duffner, R. 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Maximum withdrawals were at the kaolin mining and processing centers in Twiggs, Wilkinson, and Washington Counties, where water levels have declined as much as 50 ft since 1944-50. In the southern two-thirds of the study area, water levels have shown little, if any, change. Declining water levels and increasing competition for groundwater have caused concern over the adequacy of groundwater supplies. This report defines the areal extent and describes the geohydrology of the Paleocene-Upper Cretaceous aquifers of east-central Georgia, and evaluates the effects of man on the groundwater flow system. Geohydrologic data from four test wells indicate that the aquifers consist of alternating layers of sand and clay that are largely of deltaic origin. In the northern third of the study area, the confining unit between the Dublin and Midville aquifer systems is absent and the aquifer systems combine to form the Dublin-Midville aquifer system. The aquifer systems range in thickness from 80 to 645 ft and their transmissivities range from 800 to 39,000 sq ft/day. The hydraulic conductivity ranges from 15 to 530 ft/day. Wells yield as much as 3,400 gpm (gallons per minute). Chemical analyses of water from 49 wells indicate that water from both aquifer systems is of good quality except in the central part of the study area, where iron concentrations are as high as 6,700 micrograms/L and exceed the 300 micrograms/L recommended limit for drinking water. The principal recharge to the aquifer systems is from precipitation that occurs within and adjacent to the outcrop areas. The principal discharge is to streams in the outcrop area. 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","language":"English","publisher":"U.S. Geological Survey","doi":"10.3133/gp34","usgsCitation":"Dempsey, W.J., Henderson, J.R., and Duffner, R.T., 1950, Total intensity aeromagnetic map of Whitley County, Indiana: U.S. Geological Survey Geophysical Investigations Map 34, 1 Plate: 27.00 × 25.42 inches, https://doi.org/10.3133/gp34.","productDescription":"1 Plate: 27.00 × 25.42 inches","costCenters":[],"links":[{"id":392828,"rank":3,"type":{"id":36,"text":"NGMDB Index Page"},"url":"https://ngmdb.usgs.gov/Prodesc/proddesc_3274.htm"},{"id":260611,"rank":900,"type":{"id":17,"text":"Plate"},"url":"https://pubs.usgs.gov/gp/0034/plate-1.pdf"},{"id":187223,"rank":0,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/thumbnails/usgs_thumb.jpg"}],"scale":"63360","country":"United States","state":"Indiana","county":"Whitley County","geographicExtents":"{\"type\":\"FeatureCollection\",\"features\":[{\"type\":\"Feature\",\"geometry\":{\"type\":\"Polygon\",\"coordinates\":[[[-85.309,41.265],[-85.3111,41.1788],[-85.3397,41.1781],[-85.3381,41.0901],[-85.3346,41.0061],[-85.4516,41.0053],[-85.5654,41.0035],[-85.5655,41.0012],[-85.644,41.0013],[-85.6836,41.0015],[-85.6849,41.0465],[-85.6856,41.0896],[-85.6876,41.179],[-85.6522,41.1787],[-85.6518,41.2668],[-85.6527,41.2949],[-85.5384,41.295],[-85.5387,41.2664],[-85.4245,41.2655],[-85.3096,41.265],[-85.309,41.265]]]},\"properties\":{\"name\":\"Whitley\",\"state\":\"IN\"}}]}","noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"4f4e4b04e4b07f02db699171","contributors":{"authors":[{"text":"Dempsey, William J.","contributorId":21517,"corporation":false,"usgs":true,"family":"Dempsey","given":"William","email":"","middleInitial":"J.","affiliations":[],"preferred":false,"id":269876,"contributorType":{"id":1,"text":"Authors"},"rank":1},{"text":"Henderson, John R. 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Off.,","doi":"10.3133/b964E","usgsCitation":"McAllister, J.F., Flores Williams, H., and Ruiz, C.F., 1950, Quicksilver deposits of Chile: U.S. Geological Survey Bulletin 964, p. 361-400, maps (11 fold. in pocket) ;24 cm., https://doi.org/10.3133/b964E.","productDescription":"p. 361-400, maps (11 fold. in pocket) ;24 cm.","costCenters":[],"links":[{"id":96813,"rank":400,"type":{"id":17,"text":"Plate"},"url":"https://pubs.usgs.gov/bul/0964e/plate-20.pdf","size":"493","linkFileType":{"id":1,"text":"pdf"}},{"id":96814,"rank":401,"type":{"id":17,"text":"Plate"},"url":"https://pubs.usgs.gov/bul/0964e/plate-21.pdf","size":"665","linkFileType":{"id":1,"text":"pdf"}},{"id":96815,"rank":402,"type":{"id":17,"text":"Plate"},"url":"https://pubs.usgs.gov/bul/0964e/plate-22.pdf","size":"788","linkFileType":{"id":1,"text":"pdf"}},{"id":96816,"rank":403,"type":{"id":17,"text":"Plate"},"url":"https://pubs.usgs.gov/bul/0964e/plate-23.pdf","size":"427","linkFileType":{"id":1,"text":"pdf"}},{"id":96817,"rank":404,"type":{"id":17,"text":"Plate"},"url":"https://pubs.usgs.gov/bul/0964e/plate-24.pdf","size":"58","linkFileType":{"id":1,"text":"pdf"}},{"id":96818,"rank":405,"type":{"id":17,"text":"Plate"},"url":"https://pubs.usgs.gov/bul/0964e/plate-25.pdf","size":"160","linkFileType":{"id":1,"text":"pdf"}},{"id":96819,"rank":406,"type":{"id":17,"text":"Plate"},"url":"https://pubs.usgs.gov/bul/0964e/plate-26.pdf","size":"83","linkFileType":{"id":1,"text":"pdf"}},{"id":96820,"rank":407,"type":{"id":17,"text":"Plate"},"url":"https://pubs.usgs.gov/bul/0964e/plate-27.pdf","size":"475","linkFileType":{"id":1,"text":"pdf"}},{"id":96821,"rank":408,"type":{"id":17,"text":"Plate"},"url":"https://pubs.usgs.gov/bul/0964e/plate-28.pdf","size":"75","linkFileType":{"id":1,"text":"pdf"}},{"id":96822,"rank":409,"type":{"id":17,"text":"Plate"},"url":"https://pubs.usgs.gov/bul/0964e/plate-29.pdf","size":"139","linkFileType":{"id":1,"text":"pdf"}},{"id":96823,"rank":410,"type":{"id":17,"text":"Plate"},"url":"https://pubs.usgs.gov/bul/0964e/plate-30.pdf","size":"47","linkFileType":{"id":1,"text":"pdf"}},{"id":167530,"rank":0,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/bul/0964e/report-thumb.jpg"},{"id":63044,"rank":300,"type":{"id":11,"text":"Document"},"url":"https://pubs.usgs.gov/bul/0964e/report.pdf","linkFileType":{"id":1,"text":"pdf"}}],"noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"4f4e4a55e4b07f02db62cf00","contributors":{"authors":[{"text":"McAllister, James Franklin","contributorId":16841,"corporation":false,"usgs":true,"family":"McAllister","given":"James","email":"","middleInitial":"Franklin","affiliations":[],"preferred":false,"id":214183,"contributorType":{"id":1,"text":"Authors"},"rank":1},{"text":"Flores Williams, Hector","contributorId":26578,"corporation":false,"usgs":true,"family":"Flores Williams","given":"Hector","email":"","affiliations":[],"preferred":false,"id":214184,"contributorType":{"id":1,"text":"Authors"},"rank":2},{"text":"Ruiz, Carlos F.","contributorId":91918,"corporation":false,"usgs":true,"family":"Ruiz","given":"Carlos","email":"","middleInitial":"F.","affiliations":[],"preferred":false,"id":214185,"contributorType":{"id":1,"text":"Authors"},"rank":3}]}} ]}