{"pageNumber":"5427","pageRowStart":"135650","pageSize":"25","recordCount":165623,"records":[{"id":22064,"text":"ofr76302 - 1976 - Principal facts for gravity stations in the Newark-Gettysburg Triassic Basin, Pennsylvania and adjacent states","interactions":[],"lastModifiedDate":"2012-02-02T00:07:45","indexId":"ofr76302","displayToPublicDate":"1994-01-01T00:00:00","publicationYear":"1976","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":"76-302","title":"Principal facts for gravity stations in the Newark-Gettysburg Triassic Basin, Pennsylvania and adjacent states","language":"ENGLISH","publisher":"U.S. Dept. of the Interior, Geological Survey,","doi":"10.3133/ofr76302","issn":"0094-9140","usgsCitation":"Sumner, J.R., Meyer, R.F., Dunleavy, J., and Fleming, R., 1976, Principal facts for gravity stations in the Newark-Gettysburg Triassic Basin, Pennsylvania and adjacent states: U.S. Geological Survey Open-File Report 76-302, 30 leaves ;28 cm., https://doi.org/10.3133/ofr76302.","productDescription":"30 leaves ;28 cm.","costCenters":[],"links":[{"id":153045,"rank":0,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/thumbnails/usgs_thumb.jpg"}],"noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"4f4e4aa8e4b07f02db667d11","contributors":{"authors":[{"text":"Sumner, John R.","contributorId":97935,"corporation":false,"usgs":true,"family":"Sumner","given":"John","email":"","middleInitial":"R.","affiliations":[],"preferred":false,"id":186929,"contributorType":{"id":1,"text":"Authors"},"rank":1},{"text":"Meyer, R. F.","contributorId":52167,"corporation":false,"usgs":true,"family":"Meyer","given":"R.","email":"","middleInitial":"F.","affiliations":[],"preferred":false,"id":186926,"contributorType":{"id":1,"text":"Authors"},"rank":2},{"text":"Dunleavy, J.M.","contributorId":69585,"corporation":false,"usgs":true,"family":"Dunleavy","given":"J.M.","email":"","affiliations":[],"preferred":false,"id":186927,"contributorType":{"id":1,"text":"Authors"},"rank":3},{"text":"Fleming, R.S.","contributorId":82339,"corporation":false,"usgs":true,"family":"Fleming","given":"R.S.","email":"","affiliations":[],"preferred":false,"id":186928,"contributorType":{"id":1,"text":"Authors"},"rank":4}]}}
,{"id":19824,"text":"ofr76169 - 1976 - Catalog of earthquakes along the San Andreas fault system in central California, July-September 1973","interactions":[],"lastModifiedDate":"2012-02-02T00:07:39","indexId":"ofr76169","displayToPublicDate":"1994-01-01T00:00:00","publicationYear":"1976","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":"76-169","title":"Catalog of earthquakes along the San Andreas fault system in central California, July-September 1973","language":"ENGLISH","publisher":"U.S. Geological Survey,","doi":"10.3133/ofr76169","usgsCitation":"Lester, F., Meagher, K., and Wesson, R.L., 1976, Catalog of earthquakes along the San Andreas fault system in central California, July-September 1973: U.S. Geological Survey Open-File Report 76-169, 38 p. :ill. ;28 cm.; (45 p. - PGS), https://doi.org/10.3133/ofr76169.","productDescription":"38 p. :ill. ;28 cm.; (45 p. - PGS)","costCenters":[],"links":[{"id":152301,"rank":0,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/thumbnails/usgs_thumb.jpg"}],"noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"4f4e49f3e4b07f02db5efa50","contributors":{"authors":[{"text":"Lester, F.W.","contributorId":10767,"corporation":false,"usgs":true,"family":"Lester","given":"F.W.","email":"","affiliations":[],"preferred":false,"id":181579,"contributorType":{"id":1,"text":"Authors"},"rank":1},{"text":"Meagher, K.L.","contributorId":65067,"corporation":false,"usgs":true,"family":"Meagher","given":"K.L.","email":"","affiliations":[],"preferred":false,"id":181581,"contributorType":{"id":1,"text":"Authors"},"rank":2},{"text":"Wesson, R. L.","contributorId":51752,"corporation":false,"usgs":true,"family":"Wesson","given":"R.","email":"","middleInitial":"L.","affiliations":[],"preferred":false,"id":181580,"contributorType":{"id":1,"text":"Authors"},"rank":3}]}}
,{"id":43664,"text":"ofr769 - 1976 - Land use and land cover and associated maps for Pensacola, Fla.","interactions":[],"lastModifiedDate":"2012-02-02T00:10:26","indexId":"ofr769","displayToPublicDate":"1994-01-01T00:00:00","publicationYear":"1976","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":"76-9","title":"Land use and land cover and associated maps for Pensacola, Fla.","language":"ENGLISH","doi":"10.3133/ofr769","usgsCitation":"Water Resources Division, U.S. Geological Survey, 1976, Land use and land cover and associated maps for Pensacola, Fla.: U.S. Geological Survey Open-File Report 76-9, 7 maps., https://doi.org/10.3133/ofr769.","productDescription":"7 maps.","costCenters":[],"links":[{"id":172622,"rank":0,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/thumbnails/usgs_thumb.jpg"}],"noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"4f4e4b27e4b07f02db6b0672","contributors":{"authors":[{"text":"Water Resources Division, U.S. Geological Survey","contributorId":128075,"corporation":true,"usgs":false,"organization":"Water Resources Division, U.S. Geological Survey","id":531288,"contributorType":{"id":1,"text":"Authors"},"rank":1}]}}
,{"id":43665,"text":"ofr7628 - 1976 - Land use and land cover and associated maps for Pensacola, Florida, and Alabama","interactions":[],"lastModifiedDate":"2012-02-02T00:10:26","indexId":"ofr7628","displayToPublicDate":"1994-01-01T00:00:00","publicationYear":"1976","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":"76-28","title":"Land use and land cover and associated maps for Pensacola, Florida, and Alabama","language":"ENGLISH","doi":"10.3133/ofr7628","usgsCitation":"Water Resources Division, U.S. Geological Survey, 1976, Land use and land cover and associated maps for Pensacola, Florida, and Alabama: U.S. Geological Survey Open-File Report 76-28, 5 maps., https://doi.org/10.3133/ofr7628.","productDescription":"5 maps.","costCenters":[],"links":[{"id":172623,"rank":0,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/thumbnails/usgs_thumb.jpg"}],"noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"4f4e4b27e4b07f02db6b065a","contributors":{"authors":[{"text":"Water Resources Division, U.S. Geological Survey","contributorId":128075,"corporation":true,"usgs":false,"organization":"Water Resources Division, U.S. Geological Survey","id":531289,"contributorType":{"id":1,"text":"Authors"},"rank":1}]}}
,{"id":8764,"text":"ofr77281 - 1976 - Geological and geochemical reconnaissance in the central Santander Massif, Departments of Santander and Norte de Santander, Colombia","interactions":[],"lastModifiedDate":"2012-02-02T00:06:14","indexId":"ofr77281","displayToPublicDate":"1994-01-01T00:00:00","publicationYear":"1976","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":"77-281","title":"Geological and geochemical reconnaissance in the central Santander Massif, Departments of Santander and Norte de Santander, Colombia","docAbstract":"The central Santander Massif is composed of Precambrian Bucaramanga Gneiss and pre-Devonian Silgara Formation intruded by Mesozoic quartz diorite, quartz monzonite, and alaskite and Cretaceous or younger porphyry. Triassic (Bocas Formation), Jurassic (Jordan and Giron Formations).and Cretaceous (Tambor, Rosa Blanca, Paja, Tablazo, Simiti, La Luna, and Umir Formations) sedimentary rocks overlie the metamorphic rocks and are younger than most of the intrusions. A geological and geochemical reconnaissance of part of the central Santander Massif included the Vetas and California gold districts. At Vetas the gold is generally in brecciated aphanitic quartz and phyllonite. Dark-gray material in the ore may be graphite. The ore veins follow steep west-northwest- and north-northeast-striking fracture zones. No new gold deposits were found. Additional geochemical studies should concentrate on western Loma Pozo del Rey and on improvement of the gold extraction process. \r\n\r\nAt California the gold is in pyritiferous quartz veins and quartz breccia. Ore containing black sooty material (graphite?) is highly radioactive. Some of the mineralization is post-Lower Cretaceous. Soil samples indicate that gold deposits lie under the thick blanket of soil on the ridges above the zone of mining. Three principal gold targets are outlined by gold and associated minerals in pan concentrates. The close relation of gold and copper anomalies suggests that copper may be useful as a pathfinder for gold elsewhere in the region. Based on occurrences of gold or high concentrations of pyrite or chalcopyrite in pan concentrates and on analytical data, eight potential gold targets are outlined in the central massif. Reconnaissance of the surrounding region is warranted.","language":"ENGLISH","publisher":"U.S. Geological Survey,","doi":"10.3133/ofr77281","usgsCitation":"Evans, J.G., 1976, Geological and geochemical reconnaissance in the central Santander Massif, Departments of Santander and Norte de Santander, Colombia: U.S. Geological Survey Open-File Report 77-281, iii, 43 p. :ill., 13 maps (12 fold. in envelope) ;29 cm., https://doi.org/10.3133/ofr77281.","productDescription":"iii, 43 p. :ill., 13 maps (12 fold. in envelope) ;29 cm.","costCenters":[],"links":[{"id":94875,"rank":400,"type":{"id":17,"text":"Plate"},"url":"https://pubs.usgs.gov/of/1977/0281/plate-01.pdf","size":"3419","linkFileType":{"id":1,"text":"pdf"}},{"id":94876,"rank":401,"type":{"id":17,"text":"Plate"},"url":"https://pubs.usgs.gov/of/1977/0281/plate-02.pdf","size":"3720","linkFileType":{"id":1,"text":"pdf"}},{"id":94877,"rank":402,"type":{"id":17,"text":"Plate"},"url":"https://pubs.usgs.gov/of/1977/0281/plate-03.pdf","size":"3941","linkFileType":{"id":1,"text":"pdf"}},{"id":94878,"rank":403,"type":{"id":17,"text":"Plate"},"url":"https://pubs.usgs.gov/of/1977/0281/plate-04.pdf","size":"2632","linkFileType":{"id":1,"text":"pdf"}},{"id":94879,"rank":404,"type":{"id":17,"text":"Plate"},"url":"https://pubs.usgs.gov/of/1977/0281/plate-05.pdf","size":"2477","linkFileType":{"id":1,"text":"pdf"}},{"id":94880,"rank":405,"type":{"id":17,"text":"Plate"},"url":"https://pubs.usgs.gov/of/1977/0281/plate-06.pdf","size":"2456","linkFileType":{"id":1,"text":"pdf"}},{"id":94881,"rank":406,"type":{"id":17,"text":"Plate"},"url":"https://pubs.usgs.gov/of/1977/0281/plate-07.pdf","size":"2452","linkFileType":{"id":1,"text":"pdf"}},{"id":94882,"rank":407,"type":{"id":17,"text":"Plate"},"url":"https://pubs.usgs.gov/of/1977/0281/plate-08.pdf","size":"2379","linkFileType":{"id":1,"text":"pdf"}},{"id":94883,"rank":408,"type":{"id":17,"text":"Plate"},"url":"https://pubs.usgs.gov/of/1977/0281/plate-09.pdf","size":"2504","linkFileType":{"id":1,"text":"pdf"}},{"id":94884,"rank":409,"type":{"id":17,"text":"Plate"},"url":"https://pubs.usgs.gov/of/1977/0281/plate-10.pdf","size":"2643","linkFileType":{"id":1,"text":"pdf"}},{"id":94885,"rank":410,"type":{"id":17,"text":"Plate"},"url":"https://pubs.usgs.gov/of/1977/0281/plate-11.pdf","size":"2465","linkFileType":{"id":1,"text":"pdf"}},{"id":94886,"rank":411,"type":{"id":17,"text":"Plate"},"url":"https://pubs.usgs.gov/of/1977/0281/plate-12.pdf","size":"2379","linkFileType":{"id":1,"text":"pdf"}},{"id":141659,"rank":0,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/of/1977/0281/report-thumb.jpg"},{"id":36332,"rank":300,"type":{"id":11,"text":"Document"},"url":"https://pubs.usgs.gov/of/1977/0281/report.pdf","linkFileType":{"id":1,"text":"pdf"}}],"noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"4f4e4b11e4b07f02db6a23d9","contributors":{"authors":[{"text":"Evans, James George","contributorId":73578,"corporation":false,"usgs":true,"family":"Evans","given":"James","email":"","middleInitial":"George","affiliations":[],"preferred":false,"id":158289,"contributorType":{"id":1,"text":"Authors"},"rank":1}]}}
,{"id":25395,"text":"wri7659 - 1976 - Annual summary of ground-water conditions in Arizona","interactions":[],"lastModifiedDate":"2012-02-02T00:08:25","indexId":"wri7659","displayToPublicDate":"1994-01-01T00:00:00","publicationYear":"1976","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":"76-59","title":"Annual summary of ground-water conditions in Arizona","language":"ENGLISH","publisher":"U.S. Geological Survey","doi":"10.3133/wri7659","usgsCitation":"Babcock, H.M., 1976, Annual summary of ground-water conditions in Arizona: U.S. Geological Survey Water-Resources Investigations Report 76-59, v. :diagrs., maps. ;28 cm., https://doi.org/10.3133/wri7659.","productDescription":"v. :diagrs., maps. ;28 cm.","costCenters":[],"links":[{"id":157534,"rank":0,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/thumbnails/usgs_thumb.jpg"}],"noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"4f4e4ac8e4b07f02db67b81d","contributors":{"authors":[{"text":"Babcock, H. M.","contributorId":90698,"corporation":false,"usgs":true,"family":"Babcock","given":"H.","email":"","middleInitial":"M.","affiliations":[],"preferred":false,"id":193514,"contributorType":{"id":1,"text":"Authors"},"rank":1}]}}
,{"id":53607,"text":"wri7670 - 1976 - Availability and chemical quality of ground water in the Crystal River and Cattle Creek Drainage Basins near Glenwood Springs, west-central Colorado","interactions":[],"lastModifiedDate":"2014-01-30T11:50:54","indexId":"wri7670","displayToPublicDate":"1994-01-01T00:00:00","publicationYear":"1976","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":"76-70","title":"Availability and chemical quality of ground water in the Crystal River and Cattle Creek Drainage Basins near Glenwood Springs, west-central Colorado","docAbstract":"Parts of the Crystal River and cattle Creek drainage basins near Glenwood Springs, Colo., have undergone rapid population growth in recent years. This growth has resulted in an increased demand for information for additional domestic, industrial, and municipal water supplies. A knowledge of the occurrence of ground water will permit a more efficient allocation of the resource. Aquifers in the two drainage basins include: alluvium, basalts, the Mesa Verde Formation, Mancos Shale, Dakota Sandstone, Morrison Formation, Entrada Sandstone, Maroon Formation, Eagle Valley Evaporite, and undifferentiated formations. Except for aquifers in the alluvium, and basalt, well yields are generally low and are less than 25 gallons per minute. Well yields form aquifers in the alluvium and basalt can be as much as several hundred gallons per minute. Water quality is dependent of rock type. Calcium bicarbonate is the predominant type of water in the study area. However, calcium sulfate type water may be found in aquifers in the Eagle Valley Evaporite and in the alluvium where the alluvial material has been derived from the Eagle Valley Evaporite. Concentrations of selenium in excess of U.S. Public Health Service standards for drinking water can be found locally in aquifers in the Eagle Valley Evaporite. (Woodard-USGS)","language":"ENGLISH","doi":"10.3133/wri7670","usgsCitation":"Brogden, R.E., and Giles, T., 1976, Availability and chemical quality of ground water in the Crystal River and Cattle Creek Drainage Basins near Glenwood Springs, west-central Colorado: U.S. Geological Survey Water-Resources Investigations Report 76-70, 2 maps : col. ; 70 x 101 cm., https://doi.org/10.3133/wri7670.","productDescription":"2 maps : col. ; 70 x 101 cm.","costCenters":[],"links":[{"id":175166,"rank":0,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/wri/1976/0070/report-thumb.jpg"},{"id":281737,"type":{"id":17,"text":"Plate"},"url":"https://pubs.usgs.gov/wri/1976/0070/plate-1.pdf"},{"id":281738,"type":{"id":17,"text":"Plate"},"url":"https://pubs.usgs.gov/wri/1976/0070/plate-2.pdf"}],"noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"4f4e4aa9e4b07f02db66802d","contributors":{"authors":[{"text":"Brogden, Robert E.","contributorId":56202,"corporation":false,"usgs":true,"family":"Brogden","given":"Robert","email":"","middleInitial":"E.","affiliations":[],"preferred":false,"id":247901,"contributorType":{"id":1,"text":"Authors"},"rank":1},{"text":"Giles, T.F.","contributorId":83096,"corporation":false,"usgs":true,"family":"Giles","given":"T.F.","email":"","affiliations":[],"preferred":false,"id":247902,"contributorType":{"id":1,"text":"Authors"},"rank":2}]}}
,{"id":43513,"text":"ofr76122 - 1976 - Land use and land cover and associated maps for Tucson, Ariz.","interactions":[],"lastModifiedDate":"2012-02-02T00:11:01","indexId":"ofr76122","displayToPublicDate":"1994-01-01T00:00:00","publicationYear":"1976","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":"76-122","title":"Land use and land cover and associated maps for Tucson, Ariz.","language":"ENGLISH","doi":"10.3133/ofr76122","usgsCitation":"Water Resources Division, U.S. Geological Survey, 1976, Land use and land cover and associated maps for Tucson, Ariz.: U.S. Geological Survey Open-File Report 76-122, 5 maps., https://doi.org/10.3133/ofr76122.","productDescription":"5 maps.","costCenters":[],"links":[{"id":169019,"rank":0,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/thumbnails/usgs_thumb.jpg"}],"noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"4f4e4b24e4b07f02db6aeb3e","contributors":{"authors":[{"text":"Water Resources Division, U.S. Geological Survey","contributorId":128075,"corporation":true,"usgs":false,"organization":"Water Resources Division, U.S. Geological Survey","id":531215,"contributorType":{"id":1,"text":"Authors"},"rank":1}]}}
,{"id":26303,"text":"wri7537 - 1976 - Distribution and movement of zinc and other heavy metals in South San Francisco Bay, California","interactions":[],"lastModifiedDate":"2012-02-02T00:08:17","indexId":"wri7537","displayToPublicDate":"1994-01-01T00:00:00","publicationYear":"1976","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":"75-37","title":"Distribution and movement of zinc and other heavy metals in South San Francisco Bay, California","language":"ENGLISH","publisher":"Water Resources Division, U.S. Geological Survey,","doi":"10.3133/wri7537","usgsCitation":"Bradford, W.L., 1976, Distribution and movement of zinc and other heavy metals in South San Francisco Bay, California: U.S. Geological Survey Water-Resources Investigations Report 75-37, iv, 58 p. :ill. ;27 cm., https://doi.org/10.3133/wri7537.","productDescription":"iv, 58 p. :ill. ;27 cm.","costCenters":[],"links":[{"id":118990,"rank":0,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/wri/1975/0037/report-thumb.jpg"},{"id":55106,"rank":300,"type":{"id":11,"text":"Document"},"url":"https://pubs.usgs.gov/wri/1975/0037/report.pdf","linkFileType":{"id":1,"text":"pdf"}}],"noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"4f4e4a80e4b07f02db64966b","contributors":{"authors":[{"text":"Bradford, Wesley L.","contributorId":95451,"corporation":false,"usgs":true,"family":"Bradford","given":"Wesley","email":"","middleInitial":"L.","affiliations":[],"preferred":false,"id":196143,"contributorType":{"id":1,"text":"Authors"},"rank":1}]}}
,{"id":8738,"text":"ofr76543 - 1976 - Soil moisture in the Black River Basin, New York, during 1972-73: International Field Year for the Great Lakes (IFYGL)","interactions":[],"lastModifiedDate":"2012-02-02T00:06:18","indexId":"ofr76543","displayToPublicDate":"1994-01-01T00:00:00","publicationYear":"1976","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":"76-543","title":"Soil moisture in the Black River Basin, New York, during 1972-73: International Field Year for the Great Lakes (IFYGL)","docAbstract":"Soil-moisture data were collected and analyzed to provide an estimate of the quantity of water in temporary storage in the Black River Basin, New York, during the International Field Year for the Great Lakes (IFYGL) (April 1, 1972 to March 31, 1973). A portable neutron logger was used to record monthly soil-moisture profiles in the unsaturated zone at 11 sites in the basin. Moisture content, computed in inches of depth over the basin, ranged from 51.41 inches in April to 37.62 inches in August. Thickness of the unsaturated zone was greatest in April and was least in June. The observed absence of a pulse, or wave, of moisture moving down through the soil at most sites may be due to the infrequency of measurements, the location of sites in sandy, well-drained areas, and a relatively constant source of moisture (precipitation) at the surface. The study does not indicate a strong correlation between volume of snowmelt and soil-moisture; this may be due to the high porosity and permeability of soil material at the observation sites. Although nine pairs of monthly basin runoff and soil-moisture content data during IFYGL has a linear correlation coefficient of 0.82, too few data are available to develop a statistical relationship. (Woodard-USGS)","language":"ENGLISH","publisher":"U.S. Geological Survey,","doi":"10.3133/ofr76543","usgsCitation":"Embree, W.N., 1976, Soil moisture in the Black River Basin, New York, during 1972-73: International Field Year for the Great Lakes (IFYGL): U.S. Geological Survey Open-File Report 76-543, iv, 33 leaves :ill., maps ;27 cm.; (53 p. - PGS), https://doi.org/10.3133/ofr76543.","productDescription":"iv, 33 leaves :ill., maps ;27 cm.; (53 p. - PGS)","costCenters":[],"links":[{"id":142874,"rank":0,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/thumbnails/usgs_thumb.jpg"}],"noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"4f4e4b05e4b07f02db699ef7","contributors":{"authors":[{"text":"Embree, William N.","contributorId":41428,"corporation":false,"usgs":true,"family":"Embree","given":"William","email":"","middleInitial":"N.","affiliations":[],"preferred":false,"id":158240,"contributorType":{"id":1,"text":"Authors"},"rank":1}]}}
,{"id":20003,"text":"ofr76455 - 1976 - Black monazite from Taiwan","interactions":[],"lastModifiedDate":"2012-02-02T00:07:34","indexId":"ofr76455","displayToPublicDate":"1994-01-01T00:00:00","publicationYear":"1976","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":"76-455","title":"Black monazite from Taiwan","language":"ENGLISH","publisher":"U.S. Geological Survey,","doi":"10.3133/ofr76455","usgsCitation":"Overstreet, W.C., and Matzko, J., 1976, Black monazite from Taiwan: U.S. Geological Survey Open-File Report 76-455, iii, 41 p. :ill. ;28 cm., https://doi.org/10.3133/ofr76455.","productDescription":"iii, 41 p. :ill. ;28 cm.","costCenters":[],"links":[{"id":152497,"rank":0,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/thumbnails/usgs_thumb.jpg"}],"noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"4f4e4a1ce4b07f02db607d60","contributors":{"authors":[{"text":"Overstreet, William C.","contributorId":73586,"corporation":false,"usgs":true,"family":"Overstreet","given":"William","email":"","middleInitial":"C.","affiliations":[],"preferred":false,"id":181886,"contributorType":{"id":1,"text":"Authors"},"rank":1},{"text":"Matzko, John J.","contributorId":79459,"corporation":false,"usgs":true,"family":"Matzko","given":"John J.","affiliations":[],"preferred":false,"id":181887,"contributorType":{"id":1,"text":"Authors"},"rank":2}]}}
,{"id":43512,"text":"ofr7612 - 1976 - Land use and land cover and associated maps for Tampa, Fla.","interactions":[],"lastModifiedDate":"2012-02-02T00:11:01","indexId":"ofr7612","displayToPublicDate":"1994-01-01T00:00:00","publicationYear":"1976","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":"76-12","title":"Land use and land cover and associated maps for Tampa, Fla.","language":"ENGLISH","doi":"10.3133/ofr7612","usgsCitation":"Water Resources Division, U.S. Geological Survey, 1976, Land use and land cover and associated maps for Tampa, Fla.: U.S. Geological Survey Open-File Report 76-12, 7 maps., https://doi.org/10.3133/ofr7612.","productDescription":"7 maps.","costCenters":[],"links":[{"id":169018,"rank":0,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/thumbnails/usgs_thumb.jpg"}],"noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"4f4e4b24e4b07f02db6aec47","contributors":{"authors":[{"text":"Water Resources Division, U.S. Geological Survey","contributorId":128075,"corporation":true,"usgs":false,"organization":"Water Resources Division, U.S. Geological Survey","id":531214,"contributorType":{"id":1,"text":"Authors"},"rank":1}]}}
,{"id":70112336,"text":"70112336 - 1976 - Thermographic mosaic of Yellowstone National Park","interactions":[],"lastModifiedDate":"2017-01-18T15:14:20","indexId":"70112336","displayToPublicDate":"1990-06-12T15:21:00","publicationYear":"1976","noYear":false,"publicationType":{"id":2,"text":"Article"},"publicationSubtype":{"id":10,"text":"Journal Article"},"seriesTitle":{"id":3052,"text":"Photogrammetric Engineering and Remote Sensing","active":true,"publicationSubtype":{"id":10}},"title":"Thermographic mosaic of Yellowstone National Park","docAbstract":"<p>An uncontrolled thermographic mosaic, which covers most of the area of Yellowstone National Park, has been compiled. The recording of aerial thermographic data on videotape is established as one of the prerequisites for the preparation of more accurate mosaics. Post-mission processing of the videotape record can rectify the nadir line to a topographic map base, correct for v/h variations in adjacent flight lines, correct for yaw distortions, rectify distortions caused by pitch, and rectify distortions produced by non-linearity of the side-wise scan. Installation of a thermal infrared scanning radiometer in a gyrostabilized mount and post-mission processing of the videotape record (principally rectification of side-wise scan distortion) would yield a controlled, photogrammetrically accurate thermographic mosaic. However, the techniques used in the preparation of the uncontrolled thermographic mosaic of Yellowstone National Park can be immediately applied to the preparation of regional thermographic mosaics, important to geologists and other scientists and engineers in studies of geothermal and volcanic areas, and to other types of environmental investigations such as pollution studies of large water bodies (e.g., harbors, estuaries, lakes, etc.), where a precise planimetric image is not critical.</p>","language":"English","publisher":"American Society of Photogrammetry","publisherLocation":"Falls Church, VA","usgsCitation":"Williams, R., Hasell, P.G., Sellman, A.N., and Smedes, H.W., 1976, Thermographic mosaic of Yellowstone National Park: Photogrammetric Engineering and Remote Sensing, v. 42, no. 10, p. 1315-1324.","productDescription":"10 p.","startPage":"1315","endPage":"1324","numberOfPages":"10","costCenters":[{"id":222,"text":"Earth Resources Observation and Science (EROS) Center","active":true,"usgs":true}],"links":[{"id":288546,"type":{"id":15,"text":"Index Page"},"url":"https://www.asprs.org/Photogrammetric-Engineering-and-Remote-Sensing/PE-RS-Archive-Search-2009-and-earlier.html"},{"id":288547,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/thumbnails/outside_thumb.jpg"}],"country":"United States","state":"Idaho;Montana;Wyoming","otherGeospatial":"Yellowstone National Park","geographicExtents":"{ \"type\": \"FeatureCollection\", \"features\": [ { \"type\": \"Feature\", \"properties\": {}, \"geometry\": { \"type\": \"Polygon\", \"coordinates\": [ [ [ -111.156,44.1324 ], [ -111.156,45.109 ], [ -109.8242,45.109 ], [ -109.8242,44.1324 ], [ -111.156,44.1324 ] ] ] } } ] }","volume":"42","issue":"10","noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"539acc59e4b0e83db6d09037","contributors":{"authors":[{"text":"Williams, Richard S. Jr.","contributorId":90679,"corporation":false,"usgs":true,"family":"Williams","given":"Richard S.","suffix":"Jr.","affiliations":[],"preferred":false,"id":494686,"contributorType":{"id":1,"text":"Authors"},"rank":1},{"text":"Hasell, Philip G. Jr.","contributorId":77054,"corporation":false,"usgs":true,"family":"Hasell","given":"Philip","suffix":"Jr.","email":"","middleInitial":"G.","affiliations":[],"preferred":false,"id":494685,"contributorType":{"id":1,"text":"Authors"},"rank":2},{"text":"Sellman, Albert N.","contributorId":14741,"corporation":false,"usgs":true,"family":"Sellman","given":"Albert","email":"","middleInitial":"N.","affiliations":[],"preferred":false,"id":494683,"contributorType":{"id":1,"text":"Authors"},"rank":3},{"text":"Smedes, Harry W.","contributorId":35383,"corporation":false,"usgs":true,"family":"Smedes","given":"Harry","email":"","middleInitial":"W.","affiliations":[],"preferred":false,"id":494684,"contributorType":{"id":1,"text":"Authors"},"rank":4}]}}
,{"id":70112330,"text":"70112330 - 1976 - A qualitative evaluation of Landsat imagery of Australian rangelands","interactions":[],"lastModifiedDate":"2017-03-31T13:16:31","indexId":"70112330","displayToPublicDate":"1990-06-12T15:14:00","publicationYear":"1976","noYear":false,"publicationType":{"id":2,"text":"Article"},"publicationSubtype":{"id":10,"text":"Journal Article"},"seriesTitle":{"id":3545,"text":"The Australian Rangeland Journal","active":true,"publicationSubtype":{"id":10}},"title":"A qualitative evaluation of Landsat imagery of Australian rangelands","docAbstract":"The capability of multidate, multispectral ERTS-1 imagery of three different rangeland areas within Australia was evaluated for its usefulness in preparing inventories of rangeland types, assessing on a broad scale range condition within these rangeland types, and assessing the response of rangelands to rainfall events over large areas. For the three divergent rangeland test areas, centered on Broken W, Alice Springs and Kalgoorlie, detailed interpretation of the imagery only partially satisfied the information requirements set. It was most useful in the Broken Hill area where fenceline contrasts in range condition were readily visible. At this and the other sites an overstorey of trees made interpretation difficult. Whilst the low resolution characteristics and the lack of stereoscopic coverage hindered interpretation it was felt that this type of imagery with its vast coverage, present low cost and potential for repeated sampling is a useful addition to conventional aerial photography for all rangeland types.","language":"English","publisher":"Australian Rangeland Society","publisherLocation":"Cottesloe, Australia","doi":"10.1071/RJ9760053","usgsCitation":"Graetz, R., Carneggie, D.M., Hacker, R., Lendon, C., and Wilcox, D., 1976, A qualitative evaluation of Landsat imagery of Australian rangelands: The Australian Rangeland Journal, v. 1, no. 1, p. 53-59, https://doi.org/10.1071/RJ9760053.","productDescription":"7 p.","startPage":"53","endPage":"59","numberOfPages":"7","costCenters":[{"id":222,"text":"Earth Resources Observation and Science (EROS) Center","active":true,"usgs":true}],"links":[{"id":288543,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/thumbnails/outside_thumb.jpg"},{"id":288542,"type":{"id":10,"text":"Digital Object Identifier"},"url":"https://dx.doi.org/10.1071/RJ9760053"}],"country":"Australia","geographicExtents":"{ \"type\": \"FeatureCollection\", \"features\": [ { \"type\": \"Feature\", \"properties\": {}, \"geometry\": { \"type\": \"Polygon\", \"coordinates\": [ [ [ 112.9,-54.8 ], [ 112.9,-9.2 ], [ 159.3,-9.2 ], [ 159.3,-54.8 ], [ 112.9,-54.8 ] ] ] } } ] }","volume":"1","issue":"1","noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"539acbe4e4b0e83db6d08ead","contributors":{"authors":[{"text":"Graetz, R.D.","contributorId":64568,"corporation":false,"usgs":true,"family":"Graetz","given":"R.D.","email":"","affiliations":[],"preferred":false,"id":494679,"contributorType":{"id":1,"text":"Authors"},"rank":1},{"text":"Carneggie, David M.","contributorId":62758,"corporation":false,"usgs":true,"family":"Carneggie","given":"David","email":"","middleInitial":"M.","affiliations":[],"preferred":false,"id":494678,"contributorType":{"id":1,"text":"Authors"},"rank":2},{"text":"Hacker, R.","contributorId":70691,"corporation":false,"usgs":true,"family":"Hacker","given":"R.","email":"","affiliations":[],"preferred":false,"id":494680,"contributorType":{"id":1,"text":"Authors"},"rank":3},{"text":"Lendon, C.","contributorId":72304,"corporation":false,"usgs":true,"family":"Lendon","given":"C.","email":"","affiliations":[],"preferred":false,"id":494681,"contributorType":{"id":1,"text":"Authors"},"rank":4},{"text":"Wilcox, D.G.","contributorId":62141,"corporation":false,"usgs":true,"family":"Wilcox","given":"D.G.","email":"","affiliations":[],"preferred":false,"id":494677,"contributorType":{"id":1,"text":"Authors"},"rank":5}]}}
,{"id":70112328,"text":"70112328 - 1976 - Estudio general de la region del Lago Titicaca evaluando en forma preliminar un sistema de analisis interactivo de imagenes multiespectrales","interactions":[],"lastModifiedDate":"2017-01-18T15:15:05","indexId":"70112328","displayToPublicDate":"1990-06-12T15:01:00","publicationYear":"1976","noYear":false,"publicationType":{"id":2,"text":"Article"},"publicationSubtype":{"id":10,"text":"Journal Article"},"seriesTitle":{"id":3294,"text":"Revista tecnica de Yacimientos Petroliferos fiscales Bolivianos","active":true,"publicationSubtype":{"id":10}},"title":"Estudio general de la region del Lago Titicaca evaluando en forma preliminar un sistema de analisis interactivo de imagenes multiespectrales","docAbstract":"<p>ERTS-1 digital data in the form of computer compatible tapes provide the geoscientist with an unusual opportunity to test the maximum flexibility of the satellite system using interactive computers, such as the General Electric Image 100 System.  Approximately 9 hours of computer and operator time were used to analyze the Lake Titicaca image, 1443-14073, acquired 9 October 1973.  The total area of the lake and associate wetlands was calculated and found to be within 3 percent of previous measurements.  The area was subdivided by reflectance characteristics employing cluster analysis of all 4 bands and later compared with density values of band 4.  Reflectance variations may be attributed to surface roughness, water depth and bottom characteristics, turbidity, and floating matter.  Wetland marsh vegetation, vegetation related to ground-water effluents, natural grasses, and farm crops were separated by cluster analysis.  Sandstone, limestone, sand dunes, and several volcanic rock types were similarly separated and displayed by assigned colors and extended through the entire scene.  Waste dumps of the Matilde Zinc Mine and smaller mine workings were tentatively identified by signature analysis.</p>\n<br/>\n<p>Histograms of reflectance values and map printouts were automatically obtained as a record of each of the principal themes.  These themes were also stored on a work tape for later display and photographic record as well as to serve in training.</p>\n<br/>\n<p>The Image 100 System is rapid, extremely flexible and very useful to the investigator in identifying subtle features that may not be noticed by conventional image analysis.  The entire scene, which covers 34,225 km<sup>2</sup>, was analyzed at a scale of 1:600,000, and portions at 1:98,000 and 1:25,000, during a 9-hour period at a rental cost of $250 per hour.  Costs to the user can be reduced by restricting its uses to specific areas, objectives, and procedures, rather than undertaking a complete analysis of a total scene.</p>","language":"Spanish","usgsCitation":"Brockmann, C., and Carter, W.D., 1976, Estudio general de la region del Lago Titicaca evaluando en forma preliminar un sistema de analisis interactivo de imagenes multiespectrales: Revista tecnica de Yacimientos Petroliferos fiscales Bolivianos, v. 5, no. 1, p. 5-31.","productDescription":"27 p.","startPage":"5","endPage":"31","numberOfPages":"27","costCenters":[{"id":222,"text":"Earth Resources Observation and Science (EROS) Center","active":true,"usgs":true}],"links":[{"id":288538,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/thumbnails/outside_thumb.jpg"}],"otherGeospatial":"Lake Titicaca","geographicExtents":"{ \"type\": \"FeatureCollection\", \"features\": [ { \"type\": \"Feature\", \"properties\": {}, \"geometry\": { \"type\": \"Polygon\", \"coordinates\": [ [ [ -70.0311,-16.5924 ], [ -70.0311,-15.2333 ], [ -68.6767,-15.2333 ], [ -68.6767,-16.5924 ], [ -70.0311,-16.5924 ] ] ] } } ] }","volume":"5","issue":"1","noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"539acbf5e4b0e83db6d08f18","contributors":{"authors":[{"text":"Brockmann, C.E.","contributorId":11948,"corporation":false,"usgs":true,"family":"Brockmann","given":"C.E.","email":"","affiliations":[],"preferred":false,"id":494675,"contributorType":{"id":1,"text":"Authors"},"rank":1},{"text":"Carter, William D.","contributorId":64567,"corporation":false,"usgs":true,"family":"Carter","given":"William","email":"","middleInitial":"D.","affiliations":[],"preferred":false,"id":494676,"contributorType":{"id":1,"text":"Authors"},"rank":2}]}}
,{"id":70161976,"text":"70161976 - 1976 - The survival of coho salmon (Oncorhynchus kisutch) eggs in two Wisconsin tributaries of Lake Michigan","interactions":[],"lastModifiedDate":"2016-07-27T10:50:41","indexId":"70161976","displayToPublicDate":"1980-01-01T00:00:00","publicationYear":"1976","noYear":false,"publicationType":{"id":2,"text":"Article"},"publicationSubtype":{"id":10,"text":"Journal Article"},"seriesTitle":{"id":737,"text":"American Midland Naturalist","active":true,"publicationSubtype":{"id":10}},"title":"The survival of coho salmon (Oncorhynchus kisutch) eggs in two Wisconsin tributaries of Lake Michigan","docAbstract":"<p>Natural reproduction of coho salmon (Oncorhynchus kisutch) in two Wisconsin tributaries of Lake Michigan (Little Scarboro Creek, Kewaunee Co., and Fischer Creek, Manitowoc Co.), is limited by an unusually high mortality of eggs and preemergent embryos. Of approximately 1800 coho salmon eggs planted in six study redds (spawning beds) within Fischer Creek (November 1972), none survived to hatching. The 1500 eggs planted in five study redds within Little Scarboro Creek produced 21 sac fry.</p>\n<p>The bottom materials of both streams are comprised of at least 15% (by volume) particles smaller than 0.84 mm in diam. Streambed gravels containing this quantity of sand, silt and clay do not allow for intragravel water of sufficient dissolved oxygen concentration or velocity to meet the oxygen requirements of developing salmon eggs. Water surrounding eggs planted in Fischer Creek and Little Scarboro Creek had mean dissolved oxygen concentrations of 3.96 and 6.22 mg/liter, respectively.</p>\n<p>The extremely low mean (2.83 C and 2.67 C) water temperatures of Fischer Creek and Little Scarboro Creek were an added cause of egg loss. In response to low temperature, planted eggs hatched after a prolonged development period of approximately 145 days. Gravel shifts caused by variable stream flow in Fischer Creek may also be responsible for killing naturally deposited eggs there</p>","language":"English","publisher":"University of Notre Dame","doi":"10.2307/2424083","usgsCitation":"Cloern, J.E., 1976, The survival of coho salmon (Oncorhynchus kisutch) eggs in two Wisconsin tributaries of Lake Michigan: American Midland Naturalist, v. 96, no. 2, p. 451-461, https://doi.org/10.2307/2424083.","productDescription":"11 p.","startPage":"451","endPage":"461","onlineOnly":"N","additionalOnlineFiles":"N","costCenters":[{"id":552,"text":"San Francisco Bay-Delta","active":false,"usgs":true},{"id":5079,"text":"Pacific Regional Director's Office","active":true,"usgs":true}],"links":[{"id":314136,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/thumbnails/outside_thumb.jpg"}],"country":"United States","state":"Wisconsin","volume":"96","issue":"2","noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"5694e067e4b039675d005ea6","contributors":{"authors":[{"text":"Cloern, James E. 0000-0002-5880-6862 jecloern@usgs.gov","orcid":"https://orcid.org/0000-0002-5880-6862","contributorId":1488,"corporation":false,"usgs":true,"family":"Cloern","given":"James","email":"jecloern@usgs.gov","middleInitial":"E.","affiliations":[{"id":37277,"text":"WMA - Earth System Processes Division","active":true,"usgs":true},{"id":438,"text":"National Research Program - Western Branch","active":true,"usgs":true}],"preferred":true,"id":588238,"contributorType":{"id":1,"text":"Authors"},"rank":1}]}}
,{"id":70174024,"text":"70174024 - 1976 - Limnological data for the major streams in Chester County, Pennsylvania","interactions":[],"lastModifiedDate":"2016-06-23T10:57:06","indexId":"70174024","displayToPublicDate":"1977-01-01T00:00:00","publicationYear":"1976","noYear":false,"publicationType":{"id":18,"text":"Report"},"publicationSubtype":{"id":6,"text":"USGS Unnumbered Series"},"seriesTitle":{"id":375,"text":"Open-File Report","active":false,"publicationSubtype":{"id":6}},"title":"Limnological data for the major streams in Chester County, Pennsylvania","docAbstract":"<p>Limnological data on major streams in Chester County, Pennsylvania are tabulated to provide a base line as to the present stream conditions. As land-use patterns change and further urbanization takes place, it is anticipated that these data will serve as a basis for comparison of conditions in the future. The 13 basins encompass a total drainage area of 1,812 km2 (697 mi2) of the 1,976 km2 (760 mi2) within Chester County. Four of the streams are tributaries to the Schuylkill River and include Pickering, Stony Run, Pigeon, and French Creek. Tributaries to the Delaware River include Darby, Crum, Ridley, Chester, Red Clay, and White Clay Creeks. The Elk Creeks flow into the Chesapeake Bay. The Brandywine is a tributary to the Christiana River, itself a tributary to the Delaware. The Octoraro Creek is a tributary to the Susquehanna River. Chester County, which is located in the Piedmont area of Pennsylvania, is undergoing rapid transition from a rural to suburban condition as the population increases.</p>\n<p>This basic-data report contains the chemical, physical, and biological information collected for the period fall 1969 through fall 1974. The network of 50 stations is shown in figure 1, which is followed by a listing (table 1) of station numbers and a brief description of station locations. Table 2 shows the physical, chemical, and bacteriological data collected by station and date. Table 3 shows the benthic invertebrate data collected by station and date.</p>","language":"English","publisher":"U.S. Geological Survey","publisherLocation":"Harrisburg, PA","doi":"10.3133/70174024","collaboration":"Prepared in cooperation with the Chester County Water Resources Authority, Chester County Department of Health, and Chester County Board of Commissioners","usgsCitation":"Lium, B.W., 1976, Limnological data for the major streams in Chester County, Pennsylvania: Open-File Report, iv, 219 p., https://doi.org/10.3133/70174024.","productDescription":"iv, 219 p.","onlineOnly":"N","additionalOnlineFiles":"N","costCenters":[{"id":532,"text":"Pennsylvania Water Science Center","active":true,"usgs":true}],"links":[{"id":324281,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/thumbnails/70174024.jpg"},{"id":324289,"type":{"id":11,"text":"Document"},"url":"https://pubs.usgs.gov/unnumbered/70174024/report.pdf","linkFileType":{"id":1,"text":"pdf"}}],"country":"United 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,{"id":70207303,"text":"70207303 - 1976 - Deep evaporitic strata off New York and New Jersey-Evidence from interstitial water chemistry of drill cores","interactions":[],"lastModifiedDate":"2019-12-16T13:44:55","indexId":"70207303","displayToPublicDate":"1976-12-31T13:38:17","publicationYear":"1976","noYear":false,"publicationType":{"id":2,"text":"Article"},"publicationSubtype":{"id":10,"text":"Journal Article"},"seriesTitle":{"id":2446,"text":"Journal of Research of the U.S. Geological Survey","active":true,"publicationSubtype":{"id":10}},"title":"Deep evaporitic strata off New York and New Jersey-Evidence from interstitial water chemistry of drill cores","docAbstract":"<p>No abstract available.</p>","language":"English","publisher":"U.S. Geological Survey","usgsCitation":"Manheim, F.T., and Hall, R., 1976, Deep evaporitic strata off New York and New Jersey-Evidence from interstitial water chemistry of drill cores: Journal of Research of the U.S. Geological Survey, v. 4, no. 6, p. 697-702.","productDescription":"6 p.","startPage":"697","endPage":"702","costCenters":[],"links":[{"id":370314,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/thumbnails/outside_thumb.jpg"}],"country":"United States","state":"New Jersey, New York","geographicExtents":"{\n  \"type\": \"FeatureCollection\",\n  \"features\": [\n    {\n      \"type\": \"Feature\",\n      \"properties\": {},\n      \"geometry\": {\n        \"type\": \"Polygon\",\n        \"coordinates\": [\n          [\n            [\n              -74.14672851562499,\n              37.21283151445594\n            ],\n            [\n              -68.02734375,\n              37.21283151445594\n            ],\n            [\n              -68.02734375,\n              41.1290213474951\n            ],\n            [\n              -74.14672851562499,\n              41.1290213474951\n            ],\n            [\n              -74.14672851562499,\n              37.21283151445594\n            ]\n          ]\n        ]\n      }\n    }\n  ]\n}","volume":"4","issue":"6","noUsgsAuthors":false,"publicationStatus":"PW","contributors":{"authors":[{"text":"Manheim, Frank T. 0000-0003-4005-4524","orcid":"https://orcid.org/0000-0003-4005-4524","contributorId":20770,"corporation":false,"usgs":true,"family":"Manheim","given":"Frank","email":"","middleInitial":"T.","affiliations":[],"preferred":false,"id":777633,"contributorType":{"id":1,"text":"Authors"},"rank":1},{"text":"Hall, R.E.","contributorId":7007,"corporation":false,"usgs":true,"family":"Hall","given":"R.E.","email":"","affiliations":[],"preferred":false,"id":777634,"contributorType":{"id":1,"text":"Authors"},"rank":2}]}}
,{"id":70211332,"text":"70211332 - 1976 - Ground-water resources of the White River Junction area, Vermont","interactions":[],"lastModifiedDate":"2022-05-27T21:44:51.448863","indexId":"70211332","displayToPublicDate":"1976-12-31T13:33:03","publicationYear":"1976","noYear":false,"publicationType":{"id":18,"text":"Report"},"publicationSubtype":{"id":6,"text":"USGS Unnumbered Series"},"title":"Ground-water resources of the White River Junction area, Vermont","docAbstract":"<p>A study of the ground-water resources of the White River Junction area, Windsor County, Vermont, was begun in 1969 as part of a cooperative program between the Vermont Department of Water Resources and the U.S. Geological Survey. The purpose of the study was to provide technical appraisal of potential sources of water to meet the expanded needs of many towns in Windsor County, as pointed out by the Rural Comprehensive Water and Sewer Plan (Vermont Department of Water Resources, 1969). Funding was made available by the U.S. Department of Agriculture, Farmers Home Administration, for water-resources exploration, including the testing of the quantity and quality of the water in sand and gravel aquifers. The geology was mapped, and private and municipal water supplies were inventoried in 1969.</p>","language":"English","publisher":"U.S. Geological Survey","doi":"10.3133/70211332","usgsCitation":"Hodges, A.L., and Butterfield, D., 1976, Ground-water resources of the White River Junction area, Vermont, Report: 27 p.; 3 Plates: 47.72 x 26.30 inches, https://doi.org/10.3133/70211332.","productDescription":"Report: 27 p.; 3 Plates: 47.72 x 26.30 inches","costCenters":[],"links":[{"id":401345,"rank":6,"type":{"id":17,"text":"Plate"},"url":"https://pubs.usgs.gov/unnumbered/70211332/plate-3.pdf","linkFileType":{"id":1,"text":"pdf"}},{"id":401344,"rank":5,"type":{"id":17,"text":"Plate"},"url":"https://pubs.usgs.gov/unnumbered/70211332/plate-2.pdf","linkFileType":{"id":1,"text":"pdf"}},{"id":401343,"rank":4,"type":{"id":17,"text":"Plate"},"url":"https://pubs.usgs.gov/unnumbered/70211332/plate-1.pdf","linkFileType":{"id":1,"text":"pdf"}},{"id":401342,"rank":3,"type":{"id":11,"text":"Document"},"url":"https://pubs.usgs.gov/unnumbered/70211332/report.pdf","linkFileType":{"id":1,"text":"pdf"}},{"id":376683,"rank":1,"type":{"id":36,"text":"NGMDB Index Page"},"url":"https://ngmdb.usgs.gov/Prodesc/proddesc_105932.htm","linkFileType":{"id":5,"text":"html"}},{"id":376760,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/unnumbered/70211332/report-thumb.jpg"}],"country":"United States","state":"Vermont","otherGeospatial":"White River Junction area","geographicExtents":"{\n  \"type\": \"FeatureCollection\",\n  \"features\": [\n    {\n      \"type\": \"Feature\",\n      \"properties\": {},\n      \"geometry\": {\n        \"type\": \"Polygon\",\n        \"coordinates\": [\n          [\n            [\n              -72.5,\n              43.5\n            ],\n            [\n              -72,\n              43.5\n            ],\n            [\n              -72,\n              43.75\n            ],\n            [\n              -72.5,\n              43.75\n            ],\n            [\n              -72.5,\n              43.5\n            ]\n          ]\n        ]\n      }\n    }\n  ]\n}","noUsgsAuthors":false,"publicationStatus":"PW","contributors":{"authors":[{"text":"Hodges, Arthur L. Jr.","contributorId":62075,"corporation":false,"usgs":true,"family":"Hodges","given":"Arthur","suffix":"Jr.","email":"","middleInitial":"L.","affiliations":[],"preferred":false,"id":837463,"contributorType":{"id":1,"text":"Authors"},"rank":1},{"text":"Butterfield, David","contributorId":28607,"corporation":false,"usgs":true,"family":"Butterfield","given":"David","affiliations":[],"preferred":false,"id":837464,"contributorType":{"id":1,"text":"Authors"},"rank":2}]}}
,{"id":70211331,"text":"70211331 - 1976 - Ground-water resources of the Barre-Montpelier area, Vermont","interactions":[],"lastModifiedDate":"2022-05-27T21:49:45.628094","indexId":"70211331","displayToPublicDate":"1976-12-31T13:21:49","publicationYear":"1976","noYear":false,"publicationType":{"id":18,"text":"Report"},"publicationSubtype":{"id":6,"text":"USGS Unnumbered Series"},"title":"Ground-water resources of the Barre-Montpelier area, Vermont","docAbstract":"<p>A study of the ground-water resources of the Barre - Montpelier area (fig. 1), Washington County, was begun in 1968 as part of a cooperative program between the Vermont Department of Water Resources and the U.S. Geological Survey. The purpose of the study is to provide technical appraisal of potential sources of water to meet the expanded needs of most towns in Washington County, as pointed out by the Rural Comprehensive Water and Sewer Plan (Vermont Department Water Resources, 1969). Funding was made available by the U.S. Department of Agriculture, Farmers Home Administration, for water-resources exploration, including the testing of the quantity and quality of the water in sand and gravel aquifers. The geology of the area was mapped, and private and municipal water supplies were inventoried in 1968.</p>","language":"English","publisher":"U.S. Geological Survey","doi":"10.3133/70211331","usgsCitation":"Hodges, A.L., and Butterfield, D., 1976, Ground-water resources of the Barre-Montpelier area, Vermont, Report: 27 p.; 4 plates: 50.96 x 29.42 inches or smaller, https://doi.org/10.3133/70211331.","productDescription":"Report: 27 p.; 4 plates: 50.96 x 29.42 inches or smaller","costCenters":[],"links":[{"id":401348,"rank":5,"type":{"id":17,"text":"Plate"},"url":"https://pubs.usgs.gov/unnumbered/70211331/plate-2.pdf"},{"id":376684,"rank":2,"type":{"id":36,"text":"NGMDB Index Page"},"url":"https://ngmdb.usgs.gov/Prodesc/proddesc_105931.htm","linkFileType":{"id":5,"text":"html"}},{"id":396867,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/unnumbered/70211331/report-thumb.jpg"},{"id":401350,"rank":7,"type":{"id":17,"text":"Plate"},"url":"https://pubs.usgs.gov/unnumbered/70211331/plate-3-1.pdf","text":"Plate 3 Errata"},{"id":401349,"rank":6,"type":{"id":17,"text":"Plate"},"url":"https://pubs.usgs.gov/unnumbered/70211331/plate-3.pdf"},{"id":401346,"rank":3,"type":{"id":11,"text":"Document"},"url":"https://pubs.usgs.gov/unnumbered/70211331/report.pdf","linkFileType":{"id":1,"text":"pdf"}},{"id":401347,"rank":4,"type":{"id":17,"text":"Plate"},"url":"https://pubs.usgs.gov/unnumbered/70211331/plate-1.pdf"}],"country":"United States","state":"Vermont","otherGeospatial":"Barre-Montpelier area","geographicExtents":"{\n  \"type\": \"FeatureCollection\",\n  \"features\": [\n    {\n      \"type\": \"Feature\",\n      \"properties\": {},\n      \"geometry\": {\n        \"type\": \"Polygon\",\n        \"coordinates\": [\n          [\n            [\n              -72.6847,\n              44.0958\n            ],\n            [\n              -72.3861,\n              44.0958\n            ],\n            [\n              -72.3861,\n              44.2806\n            ],\n            [\n              -72.6847,\n              44.2806\n            ],\n            [\n              -72.6847,\n              44.0958\n            ]\n          ]\n        ]\n      }\n    }\n  ]\n}","noUsgsAuthors":false,"publicationStatus":"PW","contributors":{"authors":[{"text":"Hodges, Arthur L. Jr.","contributorId":62075,"corporation":false,"usgs":true,"family":"Hodges","given":"Arthur","suffix":"Jr.","email":"","middleInitial":"L.","affiliations":[],"preferred":false,"id":837461,"contributorType":{"id":1,"text":"Authors"},"rank":1},{"text":"Butterfield, David","contributorId":28607,"corporation":false,"usgs":true,"family":"Butterfield","given":"David","affiliations":[],"preferred":false,"id":837462,"contributorType":{"id":1,"text":"Authors"},"rank":2}]}}
,{"id":70206966,"text":"70206966 - 1976 - Hydrogeochemistry of Bermuda: A case history of ground-water diagenesis of biocalcarenites","interactions":[],"lastModifiedDate":"2019-12-03T07:47:51","indexId":"70206966","displayToPublicDate":"1976-12-31T11:07:06","publicationYear":"1976","noYear":false,"publicationType":{"id":2,"text":"Article"},"publicationSubtype":{"id":10,"text":"Journal Article"},"seriesTitle":{"id":1786,"text":"Geological Society of America Bulletin","active":true,"publicationSubtype":{"id":10}},"title":"Hydrogeochemistry of Bermuda: A case history of ground-water diagenesis of biocalcarenites","docAbstract":"<p><span>Bermuda is composed of relatively young skeletal limestones currently undergoing diagenesis by the ground water passing through them. The saturated zone consists of separate fresh-water bodies laterally surrounded and underlain by extensive brackish aureoles, in which the meteoric water is mixed with sea water. The meteoric water enters the aquifer after passing through the soil or through marshes (outcrops of the ground-water bodies), in each case causing an influx of CO</span><sub>2</sub><span>&nbsp;to the saturated zone. Examination of the ground-water chemistry enables mapping of (a) the extent of mixing of meteoric ground water and sea water; (b) P</span><sub>CO2</sub><span>; (c) the extent of saturation with calcite and aragonite; (d) concentration of Sr; and (e) the amount of calcium and magnesium derived from the limestones. It is concluded that three processes control the chemistry of Bermudian ground water: (a) generation of elevated CO</span><sub>2</sub><span>&nbsp;partial pressures in soils and marshes; (b) dissolution of metastable carbonate minerals (principally aragonite); and (c) mixing with sea water. Bermuda ground water apparently approaches a steady state of aragonite dissolution (at slight subsaturation) and concurrent precipitation of calcite cement. Large Sr/Ca ratios in the ground water indicate that the dissolution of aragonite is incongruent. Dissolution is most pronounced near the marshes where CO</span><sub>2</sub><span>&nbsp;content is highest. Mixing with sea water is not significant in controlling calcite saturation. Only small amounts of magnesium enter the ground water by incongruent dissolution of magnesium calcite, an apparently slow process on the time scale of passage of the ground water through the saturated zone. All of the waters are well undersaturated with respect to dolomite. It is estimated that the present rate of recrystallization of aragonite to calcite is about 0.32 cm</span><sup>3</sup><span>&nbsp;of aragonite to calcite per m</span><sup>3</sup><span>&nbsp;of the saturated zone per year. At the present rate of chemical weathering, 360 m</span><sup>3</sup><span>&nbsp;of the saturated zone is lost each year through solution and transported to the sea by ground water.&nbsp;</span></p>","language":"English","publisher":"Geological Society of America","doi":"10.1130/0016-7606(1976)87<1301:HOBACH>2.0.CO;2","issn":"00167606","usgsCitation":"Plummer, L., Vacher, H., MacKenzie, F., Bricker, O., and Land, L., 1976, Hydrogeochemistry of Bermuda: A case history of ground-water diagenesis of biocalcarenites: Geological Society of America Bulletin, v. 87, no. 9, p. 1301-1316, https://doi.org/10.1130/0016-7606(1976)87<1301:HOBACH>2.0.CO;2.","productDescription":"16 p. ","startPage":"1301","endPage":"1316","costCenters":[],"links":[{"id":369797,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/thumbnails/outside_thumb.jpg"}],"volume":"87","issue":"9","noUsgsAuthors":false,"publicationStatus":"PW","contributors":{"authors":[{"text":"Plummer, L.N.","contributorId":206803,"corporation":false,"usgs":false,"family":"Plummer","given":"L.N.","email":"","affiliations":[],"preferred":false,"id":776411,"contributorType":{"id":1,"text":"Authors"},"rank":1},{"text":"Vacher, H. L.","contributorId":77075,"corporation":false,"usgs":true,"family":"Vacher","given":"H. L.","affiliations":[],"preferred":false,"id":776412,"contributorType":{"id":1,"text":"Authors"},"rank":2},{"text":"MacKenzie, F.T.","contributorId":25681,"corporation":false,"usgs":true,"family":"MacKenzie","given":"F.T.","email":"","affiliations":[],"preferred":false,"id":776413,"contributorType":{"id":1,"text":"Authors"},"rank":3},{"text":"Bricker, O.P.","contributorId":33717,"corporation":false,"usgs":true,"family":"Bricker","given":"O.P.","affiliations":[],"preferred":false,"id":776414,"contributorType":{"id":1,"text":"Authors"},"rank":4},{"text":"Land, L.S.","contributorId":220974,"corporation":false,"usgs":false,"family":"Land","given":"L.S.","email":"","affiliations":[],"preferred":false,"id":776415,"contributorType":{"id":1,"text":"Authors"},"rank":5}]}}
,{"id":70207630,"text":"70207630 - 1976 - Trace-element variations at Summer Coon volcano, San Juan Mountains, Colorado, and the origin of continental-interior andesite","interactions":[],"lastModifiedDate":"2020-06-04T14:48:43.64956","indexId":"70207630","displayToPublicDate":"1976-12-31T11:03:30","publicationYear":"1976","noYear":false,"publicationType":{"id":2,"text":"Article"},"publicationSubtype":{"id":10,"text":"Journal Article"},"seriesTitle":{"id":1723,"text":"GSA Bulletin","active":true,"publicationSubtype":{"id":10}},"title":"Trace-element variations at Summer Coon volcano, San Juan Mountains, Colorado, and the origin of continental-interior andesite","docAbstract":"<p>The Oligocene Summer Coon center, an eroded continental-interior volcano of the eastern San Juan Mountains, Colorado, was the source of magmas ranging in composition from basaltic andesite to rhyolite. Previous Pb and Sr isotope studies indicate derivation of the magmas from an isotopically homogeneous source. This study presents new data for rare-earth elements (REE), U, Th, Ba, Sr, Rb, and Ni from 10 samples of the Summer Coon sequence. Alkali elements are high in all rocks; as SiO<sub>2</sub><span>&nbsp;</span>increases, Ba increases from 900 to 2,000 ppm, Rb increases from 35 to 90 ppm, Sr decreases from 900 to 350 ppm, K/Rb decreases slightly, Ba/Sr increases, U increases from 0.5 to 2.5 ppm, and Th increases from 2 to 7 ppm. Chondrite-normalized REE patterns are strongly fractionated in comparison with oceanic-arc andesite-dacite sequences. La is 80 to 120 times chondritic abundance, but Yb and Lu are less than 10 times chondritic abundance. Small negative Eu anomalies characterize the rhyolites. Nickel in the andesites is 40 to 70 ppm.</p><p>The origin of the andesite is interpreted in terms of nonmodal partial melting of a trace-element—enriched garnet-bearing source, possibly subducted crust that has converted to eclogite. Rhyodacite and rhyolite are interpreted as low-pressure crystal-fractionation products of silicic andesite, in which crystallizing phases are hornblende rich in REE and plagioclase.</p>","language":"English","publisher":"GSA","doi":"10.1130/0016-7606(1976)87<1477:TVASCV>2.0.CO;2","usgsCitation":"Zielinski, R.A., and Lipman, P.W., 1976, Trace-element variations at Summer Coon volcano, San Juan Mountains, Colorado, and the origin of continental-interior andesite: GSA Bulletin, v. 87, no. 10, p. 1477-1485, https://doi.org/10.1130/0016-7606(1976)87<1477:TVASCV>2.0.CO;2.","productDescription":"9 p.","startPage":"1477","endPage":"1485","costCenters":[{"id":164,"text":"Central Energy Resources Science Center","active":true,"usgs":true},{"id":5079,"text":"Pacific Regional Director's Office","active":true,"usgs":true}],"links":[{"id":370899,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/thumbnails/outside_thumb.jpg"}],"country":"United States","state":"Colorado","otherGeospatial":"Summer Coon volcanic center","geographicExtents":"{\n  \"type\": \"FeatureCollection\",\n  \"features\": [\n    {\n      \"type\": \"Feature\",\n      \"properties\": {},\n      \"geometry\": {\n        \"type\": \"Polygon\",\n        \"coordinates\": [\n          [\n            [\n              -106.4794921875,\n              37.37015718405753\n            ],\n            [\n              -105.6005859375,\n              37.37015718405753\n            ],\n            [\n              -105.6005859375,\n              38.496593518947584\n            ],\n            [\n              -106.4794921875,\n              38.496593518947584\n            ],\n            [\n              -106.4794921875,\n              37.37015718405753\n            ]\n          ]\n        ]\n      }\n    }\n  ]\n}","volume":"87","issue":"10","noUsgsAuthors":false,"publicationStatus":"PW","contributors":{"authors":[{"text":"Zielinski, Robert A. 0000-0002-4047-5129 rzielinski@usgs.gov","orcid":"https://orcid.org/0000-0002-4047-5129","contributorId":1593,"corporation":false,"usgs":true,"family":"Zielinski","given":"Robert","email":"rzielinski@usgs.gov","middleInitial":"A.","affiliations":[{"id":164,"text":"Central Energy Resources Science Center","active":true,"usgs":true}],"preferred":true,"id":778681,"contributorType":{"id":1,"text":"Authors"},"rank":1},{"text":"Lipman, Peter W. 0000-0001-9175-6118 plipman@usgs.gov","orcid":"https://orcid.org/0000-0001-9175-6118","contributorId":3486,"corporation":false,"usgs":true,"family":"Lipman","given":"Peter","email":"plipman@usgs.gov","middleInitial":"W.","affiliations":[{"id":617,"text":"Volcano Science Center","active":true,"usgs":true},{"id":5079,"text":"Pacific Regional Director's Office","active":true,"usgs":true}],"preferred":true,"id":778682,"contributorType":{"id":1,"text":"Authors"},"rank":2}]}}
,{"id":70197787,"text":"70197787 - 1976 - Preliminary report on the 17th cruise of the Dimitri Mendeleev","interactions":[],"lastModifiedDate":"2023-12-19T00:44:17.76315","indexId":"70197787","displayToPublicDate":"1976-12-31T00:00:00","publicationYear":"1976","noYear":false,"publicationType":{"id":2,"text":"Article"},"publicationSubtype":{"id":10,"text":"Journal Article"},"seriesTitle":{"id":1578,"text":"Eos, Transactions, American Geophysical Union","onlineIssn":"2324-9250","printIssn":"0096-394","active":true,"publicationSubtype":{"id":10}},"title":"Preliminary report on the 17th cruise of the Dimitri Mendeleev","docAbstract":"<p>No abstract available.</p>","language":"English","publisher":"American Geophysical Union","usgsCitation":"Brown, E.H., Coleman, R.G., Echiverria, L., Fisher, R., and Irwin, W., 1976, Preliminary report on the 17th cruise of the Dimitri Mendeleev: Eos, Transactions, American Geophysical Union, v. 57, no. 12, p. 1027-1027.","productDescription":"1 p.","startPage":"1027","endPage":"1027","costCenters":[{"id":312,"text":"Geology, Minerals, Energy, and Geophysics Science Center","active":true,"usgs":true}],"links":[{"id":355199,"rank":1,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/thumbnails/outside_thumb.jpg"}],"volume":"57","issue":"12","noUsgsAuthors":false,"publicationStatus":"PW","contributors":{"authors":[{"text":"Brown, E. H.","contributorId":78757,"corporation":false,"usgs":true,"family":"Brown","given":"E.","email":"","middleInitial":"H.","affiliations":[],"preferred":false,"id":738489,"contributorType":{"id":1,"text":"Authors"},"rank":1},{"text":"Coleman, R. G.","contributorId":75170,"corporation":false,"usgs":true,"family":"Coleman","given":"R.","email":"","middleInitial":"G.","affiliations":[],"preferred":false,"id":738490,"contributorType":{"id":1,"text":"Authors"},"rank":2},{"text":"Echiverria, L.M.","contributorId":205789,"corporation":false,"usgs":false,"family":"Echiverria","given":"L.M.","email":"","affiliations":[],"preferred":false,"id":738491,"contributorType":{"id":1,"text":"Authors"},"rank":3},{"text":"Fisher, R.L.","contributorId":68028,"corporation":false,"usgs":true,"family":"Fisher","given":"R.L.","email":"","affiliations":[],"preferred":false,"id":738492,"contributorType":{"id":1,"text":"Authors"},"rank":4},{"text":"Irwin, W. P.","contributorId":82347,"corporation":false,"usgs":true,"family":"Irwin","given":"W. P.","affiliations":[],"preferred":false,"id":738493,"contributorType":{"id":1,"text":"Authors"},"rank":5}]}}
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