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","language":"English","publisher":"U.S. Geological Survey","doi":"10.3133/ofr78198","usgsCitation":"Peterson, D.L., and Hassemer, J.H., 1978, Principal facts and profiles of gravity data from parts of Meade, Pennington, Haakon, and Jackson Counties, South Dakota: U.S. Geological Survey Open-File Report 78-198, Report: 14 p.; 5 Plates: 23.40 × 20.15 inches or smaller, https://doi.org/10.3133/ofr78198.","productDescription":"Report: 14 p.; 5 Plates: 23.40 × 20.15 inches or smaller","costCenters":[],"links":[{"id":410224,"rank":7,"type":{"id":36,"text":"NGMDB Index 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Donald L.","contributorId":28597,"corporation":false,"usgs":true,"family":"Peterson","given":"Donald","email":"","middleInitial":"L.","affiliations":[],"preferred":false,"id":161756,"contributorType":{"id":1,"text":"Authors"},"rank":1},{"text":"Hassemer, Jerry H.","contributorId":8103,"corporation":false,"usgs":true,"family":"Hassemer","given":"Jerry","email":"","middleInitial":"H.","affiliations":[],"preferred":false,"id":161755,"contributorType":{"id":1,"text":"Authors"},"rank":2}]}} ,{"id":7858,"text":"ofr78913 - 1978 - Quality of water in Pascagoula and Escatawpa Rivers, Jackson County, Mississippi","interactions":[],"lastModifiedDate":"2023-03-03T21:24:47.196279","indexId":"ofr78913","displayToPublicDate":"1978-01-01T00:00:00","publicationYear":"1978","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":"78-913","title":"Quality of water in Pascagoula and Escatawpa Rivers, Jackson County, Mississippi","docAbstract":"The chemical and physical properties and the range of concentrations of most constituents in water in the Pascagoula and Escatawpa Rivers during the period May 17-19, 1977, varied rapidly between high and low tides, primarily as the result of interactions of freshwater inflow with highly mineralized Gulf waters. The water at a downstream site of the 11-mile study reach on the Pascagoula River was saline. On May 19, 1977, the dissolved-solids concentration at that site was 14,500 milligrams per liter. At the same time, the water at the mouth of Escatawpa River had a dissolved-solids concentration of 4,600 milligrams per liter. The specific conductance of the water at the downstream sites of both rivers increased with depth and progressively decreased upstream to sites where freshwater inflow was predominant. The specific conductance decreased upstream from a maximum of 40,000 micromhos per centimeter at 25°Celsius at site P1 to 60 micromhos at site P12 on Pascagoula River and from 30,000 micromhos at site E1 to 45 micromhos at site E9 on Escatawpa River.
There was evidence of oxygen deficiency (less than 3.0 milligrams per liter) at many sites in deep pools where there is little circulation and mixing of the more dense saltwater. Dissolved-oxygen concentrations ranged from 2.1 to 8.2 milligrams per liter.
Biochemical oxygen demand ranged from 0.1 to 3.5 milligrams per liter and was generally less than 2.0 milligrams per liter at most sites.
A large part of the total organic carbon in the lower Pascagoula River was carried into the study area by freshwater inflow. Very little organic carbon was being discharged by the Escatawpa River into the Pascagoula River.
Total nitrogen moved out of Pascagoula and Escatawpa Rivers at an extremely slow rate and in concentrations of less than 0.1 milligram per liter.
The water temperature near the surface at downstream sites on Escatawpa River at low tide was elevated as much as 2.5°C (4.5°F), suggesting thermal loading.
The fecal coliform and fecal streptococcal bacteria in Pascagoula and Escatawpa Rivers were in concentrations indicative of manmade pollution. The ratio of the concentrations in which these bacteria were present suggests that both rivers receive human enteric wastes.
","language":"English","publisher":"U.S. Geological Survey","doi":"10.3133/ofr78913","collaboration":"Prepared in cooperation with Mississippi Air and Water Pollution Control Commission","usgsCitation":"Bednar, G.A., 1978, Quality of water in Pascagoula and Escatawpa Rivers, Jackson County, Mississippi: U.S. Geological Survey Open-File Report 78-913, v, 91 p., https://doi.org/10.3133/ofr78913.","productDescription":"v, 91 p.","costCenters":[],"links":[{"id":141453,"rank":1,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/of/1978/0913/report-thumb.jpg"},{"id":413500,"rank":2,"type":{"id":11,"text":"Document"},"url":"https://pubs.usgs.gov/of/1978/0913/report.pdf","linkFileType":{"id":1,"text":"pdf"}}],"country":"United States","state":"Mississippi","county":"Jackson County","otherGeospatial":"Escatawpa River, Pascagoula River","geographicExtents":"{\n \"type\": \"FeatureCollection\",\n \"features\": [\n {\n \"type\": \"Feature\",\n \"properties\": {},\n \"geometry\": {\n \"type\": \"Polygon\",\n \"coordinates\": [\n [\n [\n -88.83333333,\n 30.321915039121063\n ],\n [\n -88.39462280273438,\n 30.321915039121063\n ],\n [\n -88.39462280273438,\n 30.70833333\n ],\n [\n -88.83333333,\n 30.70833333\n ],\n [\n -88.83333333,\n 30.321915039121063\n ]\n ]\n ]\n }\n }\n ]\n}","noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"4f4e4a8be4b07f02db6516b2","contributors":{"authors":[{"text":"Bednar, Gene A.","contributorId":81881,"corporation":false,"usgs":true,"family":"Bednar","given":"Gene","email":"","middleInitial":"A.","affiliations":[],"preferred":false,"id":156742,"contributorType":{"id":1,"text":"Authors"},"rank":1}]}} ,{"id":7997,"text":"ofr78482 - 1978 - Selected uranium and uranium-thorium occurrences in New Hampshire","interactions":[],"lastModifiedDate":"2023-04-18T20:37:29.020095","indexId":"ofr78482","displayToPublicDate":"1978-01-01T00:00:00","publicationYear":"1978","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":"78-482","title":"Selected uranium and uranium-thorium occurrences in New Hampshire","docAbstract":"Secondary uranium mineralization occurs in a northwest-trending fracture zone in the Devonian Concord Granite in recent rock cuts along Interstate Highway 89 near New London, New Hampshire. A detailed plane table map of this occurrence was prepared. Traverses using total gamma ray scintillometers throughout the pluton of Concord Granite identified two additional areas in which very small amounts of secondary mineralization occurs in the marginal zones of the body. All three areas lie along the same northwest trend. A ground radiometry survey of a large part of the Jurassic White Mountain batholith was conducted. Emphasis was placed on those areas from which earlier sampling by Butler (1975) had been done. No unusual geological characteristics were apparent around sample localities from which anomalous U and Th had been reported.. The results of this survey confirm previous conclusions that the red, coarse-grained, biotite granite phase of the Conway Granite is more radioactive than other phases of the Conway Granite or other rock types of the White Mountain Plutonic-Volcanic Series. Aplites associated with the Conway Granite were found generally to be as radioactive as the red Conway Granite.
","language":"English","publisher":"U.S. Geological Survey","doi":"10.3133/ofr78482","usgsCitation":"Bothner, W.A., 1978, Selected uranium and uranium-thorium occurrences in New Hampshire: U.S. Geological Survey Open-File Report 78-482, Report: ii, 42 p.; 2 Plates: 25.56 x 19.36 inches and 19.96 x 16.35 inches, https://doi.org/10.3133/ofr78482.","productDescription":"Report: ii, 42 p.; 2 Plates: 25.56 x 19.36 inches and 19.96 x 16.35 inches","costCenters":[],"links":[{"id":415952,"rank":5,"type":{"id":36,"text":"NGMDB Index 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