{"pageNumber":"5088","pageRowStart":"127175","pageSize":"25","recordCount":165549,"records":[{"id":19630,"text":"ofr79335 - 1979 - Hydrologic data for North Creek, Trinity River basin, Texas, 1977","interactions":[],"lastModifiedDate":"2021-09-17T19:52:43.185867","indexId":"ofr79335","displayToPublicDate":"1994-01-01T00:00:00","publicationYear":"1979","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":"79-335","title":"Hydrologic data for North Creek, Trinity River basin, Texas, 1977","docAbstract":"<p>The U.S. Soil Conservation Service is actively engaged in the installation of flood- and soil-erosion reducing structures in Texas under the authority of \"The Flood Control Act of 1936 and 1944\" and \"Watershed Protection and Flood Prevention Act\" (Public Law 566), as amended. The Soil Conservation Service has found that approximately 3,500 floodwaterretarding structures would be physically and economically feasible in Texas. As of September 30, 1977, 1,695 (corrected figure) of these structures had been built.</p><p>This watershed-development program will have varying but important effects on surface- and ground-water resources of river basins, especially where a large number of the floodwater-retarding structures are built. Basic hydrologic data under natural and developed conditions are needed to appraise the effects of the structures on the yield and mode of occurrence of runoff.</p><p>During the period 1951-62, the U.S. Geological Survey began hydrologic investigations in 12 small watersheds (fig. 1). As of Sept. 30, 1977, data collection in eleven of these study areas has been completed and is now in progress in one area. This study is being made in cooperation with the Texas Department of Water Resources, the Soil Conservation Service, the San Antonio River Authority, the city of Dallas, and the Tarrant County Control and Improvement District No. 1. The 12 study areas were chosen to sample watersheds having different rainfall, topography, geology, and soils. In five of the study areas (North, Little Elm, Mukewater, Little Pond-North Elm, and Pin Oak Creeks), streamflow and rainfall records were collected prior to construction of the floodwater-retarding structures, thus affording the opportunity for analyses of the conditions \"before and after\" development. A summary of the development of the floodwater-retarding structures in each study area as of Sept. 30, 1977, is shown in table 1. </p>","language":"English","publisher":"U.S. Geological Survey","doi":"10.3133/ofr79335","collaboration":"Prepared in cooperation with Tarrant County Water Control and Improvement District No. 1, the Soil Conservation Service, and the Texas Department of Water Resources","usgsCitation":"Kidwell, C., 1979, Hydrologic data for North Creek, Trinity River basin, Texas, 1977: U.S. Geological Survey Open-File Report 79-335, 39 p., https://doi.org/10.3133/ofr79335.","productDescription":"39 p.","onlineOnly":"N","additionalOnlineFiles":"N","costCenters":[{"id":583,"text":"Texas Water Science Center","active":true,"usgs":true}],"links":[{"id":389445,"rank":2,"type":{"id":11,"text":"Document"},"url":"https://pubs.usgs.gov/of/1979/0335/report.pdf","linkFileType":{"id":1,"text":"pdf"}},{"id":153183,"rank":0,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/of/1979/0335/report-thumb.jpg"}],"country":"United States","state":"Texas","otherGeospatial":"North Creek, Trinity River basin","geographicExtents":"{\n  \"type\": \"FeatureCollection\",\n  \"features\": [\n    {\n      \"type\": \"Feature\",\n      \"properties\": {},\n      \"geometry\": {\n        \"type\": \"Polygon\",\n        \"coordinates\": [\n          [\n            [\n              -98.42033386230469,\n              33.16801930648876\n            ],\n            [\n              -98.250732421875,\n              33.16801930648876\n            ],\n            [\n              -98.250732421875,\n              33.28519397154413\n            ],\n            [\n              -98.42033386230469,\n              33.28519397154413\n            ],\n            [\n              -98.42033386230469,\n              33.16801930648876\n            ]\n          ]\n        ]\n      }\n    }\n  ]\n}","noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"4f4e4a25e4b07f02db60ed61","contributors":{"authors":[{"text":"Kidwell, C.C.","contributorId":54998,"corporation":false,"usgs":true,"family":"Kidwell","given":"C.C.","email":"","affiliations":[],"preferred":false,"id":181239,"contributorType":{"id":1,"text":"Authors"},"rank":1}]}}
,{"id":19352,"text":"ofr79392 - 1979 - Trace element analysis of marine organisms by anodic stripping voltammetry (ASV)","interactions":[],"lastModifiedDate":"2024-03-27T18:13:25.236074","indexId":"ofr79392","displayToPublicDate":"1994-01-01T00:00:00","publicationYear":"1979","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":"79-392","title":"Trace element analysis of marine organisms by anodic stripping voltammetry (ASV)","docAbstract":"<p>Trace element analysis of marine organisms has generally been conducted by (1) sophisticated instrumentation (e. g., atomic absorption), (2) complicated cookbook laboratory procedures utilizing a host of chemicals and glassware, or (3) a combination of the above. All these procudures present problems to the investigator. For example, analysis by methods other than instrumentation are unable to detect minute amounts of various trace elements and in general are not extremely accurate. Problems common to all procedures are (1) relatively large amounts of sample (2 grams or more) are required for analyses of even the more common trace elements and (2) contamination of samples is almost a certainty due to complicated sample preparation procedures which include large amounts of glassware, chemicals and excessive handling of the sample.</p><p>The development of new anodic stripping voltammetry (ASV methods (Matson, 1968) has provided investigators with an instrument which (1) is capable of accurately detecting trace elements in minute quantities, (2) utilizes very small amounts of sample (0.01 mg) , (3) works on a simple operating principle which simplifies sample preparation thereby reducing the possibility of contamination, (4) can be used aboard small boats, and (5) is relatively inexpensive (compared to other instruments used for trace element analysis). Recent ASV literature (Matson, 1968, Fitzgerald, 1970; Bradford, 1972) has dealt exclusively with the analysis of salt water and sediments and does not provide an adequate method for analysis of marine organic matter. This paper reports on an investigation designed to develop the methodology necessary for ASV analysis of organic material from the marine environment.</p>","language":"English","publisher":"U.S. Geological Survey","doi":"10.3133/ofr79392","usgsCitation":"Hill, G.W., 1979, Trace element analysis of marine organisms by anodic stripping voltammetry (ASV): U.S. Geological Survey Open-File Report 79-392, 12 p., https://doi.org/10.3133/ofr79392.","productDescription":"12 p.","costCenters":[],"links":[{"id":427169,"rank":2,"type":{"id":11,"text":"Document"},"url":"https://pubs.usgs.gov/of/1979/0392/report.pdf","linkFileType":{"id":1,"text":"pdf"}},{"id":151832,"rank":1,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/of/1979/0392/report-thumb.jpg"}],"noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"4f4e4b06e4b07f02db69a2b9","contributors":{"authors":[{"text":"Hill, Gary W.","contributorId":56627,"corporation":false,"usgs":true,"family":"Hill","given":"Gary","email":"","middleInitial":"W.","affiliations":[],"preferred":false,"id":180732,"contributorType":{"id":1,"text":"Authors"},"rank":1}]}}
,{"id":20253,"text":"ofr79233 - 1979 - Uranium and thorium in granitic rocks of northeastern Washington and northern Idaho, with comments on uranium resource potential","interactions":[],"lastModifiedDate":"2012-02-02T00:07:44","indexId":"ofr79233","displayToPublicDate":"1994-01-01T00:00:00","publicationYear":"1979","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":"79-233","title":"Uranium and thorium in granitic rocks of northeastern Washington and northern Idaho, with comments on uranium resource potential","docAbstract":"Northeastern Washington and northern Idaho is a uranium province in which many Cretaceous and Tertiary granitic plutons contain abnormal amounts of uranium. Mean uranium content of 108 samples of granitic rock is 8.8 parts per million (ppm), more than twice normal for rocks of this composition. The mean thorium content, 20.3 ppm, and mean Th/U, 3.19, are normal. The most uraniferous and fertile rocks are the peraluminous two-mica granitic suite, although not all two-mica plutons are enriched in uranium. The muscovite-bearing suite has mean uranium content of 22.3 ppm, mean thorium content of 22.8 ppm, and mean Th/U of 2.82. Porphyritic quartz monzonite of the Midnite mine, which I interpret to be a two-mica granitic rock, is especially radioactive with mean U of 14.7 ppm, mean Th of 32.1 ppm, and mean Th/U of 2.72. Mean uranium and thorium contents of the two-mica granitic plutons are significantly different from those of the calcalkaline hornblende granitic suite, which are mean U, 5.0 ppm; mean Th, 17.6; and mean Th/U, 3.78. Biotite granitic rocks containing no hornblende or muscovite appear to be an intermediate suite in terms of U and Th, or possibly are variants of both hornblende and muscovite type; mean U is 3.88 ppm, mean Th is 14.4 ppm, and mean Th/U is 3.03 as calculated from the more abundant data of Castor and others (1978). occurrence of uranium and thorium in the muscovite and hornblende suites is systematically different. Many muscovite-bearing rocks are much more enriched in uranium (>15 ppm) than they are in thorium, and have a relatively low Th:U correlation coefficient of +0.409. Many of the uraniferous muscovite-bearing rocks contain less than 20 ppm Th, probably a consequence of forming by anatexis of thorium deficient sedimentary rocks. Uranium and thorium variation is much more regular in the hornblende suite, which has a Th:U correlation coefficient of +0.780. Uranium in the muscovite suite is held primarily in magnetite and biotite, and possibly as minute uraninite grains, whereas in the hornblende suite uranium resides primarily in sphene, zircon, and allanite. Many muscovite-bearing plutons are considered fertile by the following two criteria: high uranium content, and uranium residence in labile phases. The hornblende-bearing granitic plutons are not considered fertile, regardless of uranium content, because uranium resides in refractory phases. \r\n\r\nTwenty-one sample localities in four plutons are considered highly anomalous according to one or more of the following attributes: (1) Uranium content =115.8 ppm (total population mean plus 1 d). (2) Thorium content =30.3 ppm (mean plus 1 d) and uranium =8.8 ppm (mean). (3) Th/U lower than 1.68 (mean minus 1 d) and uranium content -18.8 ppm. The four identified highly anomalous plutons are, from southwest to northeast, (1) Cretaceous porphyritic quartz monzonite of the Midnite mine; (2) Cretaceous muscovite quartz monzonite east of Deer Lake; (3) Cretaceous quartz monzonite of Hungry Mountain, and (4) Cretaceous quartz monzonite of Granite Pass. The study area is favorable for at least five types of uranium deposits including: intragranitic hydrothermal veins as in the Massif Central, France; intragranitic supergene veins, as at the Daybreak mine; contact zone deposits, as at the Midnite mine; and basal-type sandstone deposits, as at the Sherwood mine. The fifth type is Rossing-type deposits for which the high-grade metamorphic terrane of the Kettle River Range, Ferry County, seems favorable, if sufficient volume of low-tenor rock can be located. The first four deposit types seem most likely in or adjacent to uraniferous plutons, as no other uranium source rocks have been identified in the area. Contact zone deposits and intragranitic hydrothermal veins, both possibly supergene-enriched, and basal-type deposits in Tertiary sandstone and conglomerate, seem most likely to be of economic importance. Exploration and discovery of potential uranium depositions","language":"ENGLISH","publisher":"U.S. Geological Survey,","doi":"10.3133/ofr79233","usgsCitation":"Nash, J.T., 1979, Uranium and thorium in granitic rocks of northeastern Washington and northern Idaho, with comments on uranium resource potential: U.S. Geological Survey Open-File Report 79-233, 46 p., 1 leaf of plates :ill., maps (1 fold.) ;28 cm., https://doi.org/10.3133/ofr79233.","productDescription":"46 p., 1 leaf of plates :ill., maps (1 fold.) ;28 cm.","costCenters":[],"links":[{"id":153005,"rank":0,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/of/1979/0233/report-thumb.jpg"},{"id":49792,"rank":400,"type":{"id":17,"text":"Plate"},"url":"https://pubs.usgs.gov/of/1979/0233/plate-1.pdf","linkFileType":{"id":1,"text":"pdf"}},{"id":49793,"rank":300,"type":{"id":11,"text":"Document"},"url":"https://pubs.usgs.gov/of/1979/0233/report.pdf","linkFileType":{"id":1,"text":"pdf"}}],"noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"4f4e4a19e4b07f02db605d07","contributors":{"authors":[{"text":"Nash, J. Thomas","contributorId":26306,"corporation":false,"usgs":true,"family":"Nash","given":"J.","email":"","middleInitial":"Thomas","affiliations":[],"preferred":false,"id":182334,"contributorType":{"id":1,"text":"Authors"},"rank":1}]}}
,{"id":19362,"text":"ofr79523 - 1979 - Progress report to the Arkansas State Highway and Transportation Commission for year ending September 30, 1978","interactions":[],"lastModifiedDate":"2022-10-17T20:37:57.470686","indexId":"ofr79523","displayToPublicDate":"1994-01-01T00:00:00","publicationYear":"1979","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":"79-523","title":"Progress report to the Arkansas State Highway and Transportation Commission for year ending September 30, 1978","docAbstract":"<p>The economic design of bridges and culverts requires a knowledge of the magnitude and frequency of floods for all size drainage basins. In addition, an analysis of the hydrologic and hydraulic characteristics at specific sites where unusual circumstances exist is a prerequisite to design.</p><p>The Arkansas State Highway and Transportation Commission and the U.S. Geological Survey have a mutual interest in flood-frequency and open-channel hydraulics and are therefore cooperating in a program to provide information necessary to meet their objectives.</p><p>This report is a summary of the accomplishments of the cooperative program. Included are plans for future work and a brief description of related water-resources programs of the Geological Survey in Arkansas.</p>","language":"English","publisher":"U.S. Geological Survey","doi":"10.3133/ofr79523","collaboration":"Prepared in cooperation with the Arkansas State Highway and Transportation Commission","usgsCitation":"Hines, M.S., 1979, Progress report to the Arkansas State Highway and Transportation Commission for year ending September 30, 1978: U.S. Geological Survey Open-File Report 79-523, Report: ii, 22 p.; 1 Plate: 22.37 x 18.67 inches, https://doi.org/10.3133/ofr79523.","productDescription":"Report: ii, 22 p.; 1 Plate: 22.37 x 18.67 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,{"id":21490,"text":"ofr80334 - 1979 - Drainage areas of streams in Arkansas, Ouachita River basin","interactions":[],"lastModifiedDate":"2022-07-22T16:51:36.120576","indexId":"ofr80334","displayToPublicDate":"1994-01-01T00:00:00","publicationYear":"1979","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":"80-334","title":"Drainage areas of streams in Arkansas, Ouachita River basin","docAbstract":"<p>Drainage areas, determined in accordance with procedure recommended by the Subcommittee on Hydrology of the Federal Inter-Agency River Basin Committee, are listed for points on streams in the Ouachita River basin in Arkansas. Points on the streams are identified by some topographic feature and by latitude and longitude.</p>","language":"English","publisher":"U.S. Geological Survey","doi":"10.3133/ofr80334","collaboration":"Prepared in cooperation with the Arkansas State Highway and Transportation Commission","usgsCitation":"Yanchosek, J.J., and Hines, M.S., 1979, Drainage areas of streams in Arkansas, Ouachita River basin: U.S. Geological Survey Open-File Report 80-334, ii, 87 p., https://doi.org/10.3133/ofr80334.","productDescription":"ii, 87 p.","costCenters":[],"links":[{"id":154520,"rank":0,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/of/1980/0334/report-thumb.jpg"},{"id":404365,"rank":2,"type":{"id":11,"text":"Document"},"url":"https://pubs.usgs.gov/of/1980/0334/report.pdf","linkFileType":{"id":1,"text":"pdf"}}],"country":"United States","state":"Arkansas","otherGeospatial":"Ouachita River basin","geographicExtents":"{\n  \"type\": \"FeatureCollection\",\n  \"features\": [\n    {\n      \"type\": \"Feature\",\n      \"properties\": {},\n      \"geometry\": {\n        \"type\": \"Polygon\",\n        \"coordinates\": [\n          [\n            [\n              -94.361572265625,\n              33.02708758002874\n            ],\n            [\n              -92.48291015625,\n              33.02708758002874\n            ],\n            [\n              -92.48291015625,\n              35.02999636902566\n            ],\n            [\n              -94.361572265625,\n              35.02999636902566\n            ],\n            [\n              -94.361572265625,\n              33.02708758002874\n            ]\n          ]\n        ]\n      }\n    }\n  ]\n}","noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"4f4e48b5e4b07f02db53379f","contributors":{"authors":[{"text":"Yanchosek, John J.","contributorId":71977,"corporation":false,"usgs":true,"family":"Yanchosek","given":"John","email":"","middleInitial":"J.","affiliations":[],"preferred":false,"id":184528,"contributorType":{"id":1,"text":"Authors"},"rank":1},{"text":"Hines, Marion S.","contributorId":29388,"corporation":false,"usgs":true,"family":"Hines","given":"Marion","email":"","middleInitial":"S.","affiliations":[],"preferred":false,"id":184527,"contributorType":{"id":1,"text":"Authors"},"rank":2}]}}
,{"id":19627,"text":"ofr79239 - 1979 - Phosphatic Permian rocks of the Adobe Range, Nevada, and their environment of deposition","interactions":[],"lastModifiedDate":"2012-02-02T00:07:42","indexId":"ofr79239","displayToPublicDate":"1994-01-01T00:00:00","publicationYear":"1979","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":"79-239","title":"Phosphatic Permian rocks of the Adobe Range, Nevada, and their environment of deposition","docAbstract":"Permian sedimentary rocks in the Adobe range, northern Nevada, are phosphatic, and although the particles of phosphate are relatively more disseminated, they closely resemble the rocks of the Phosphoria Formation. In the northern Adobe Range, where the entire Permian sequence is approximately correlative with the Phosphoria Formation, it is 200 m thick and averages 1.7 percent P2O5 . In the southern Adobe Range, the Permian sequence is more than 1,700 m thick, and the upper half which is roughly correlative with the Phosphoria Formation averages more than 2 percent P2O5. Some thin beds in rocks of Permian age contain more than 20 percent P2O5. \r\n\r\nPhosphatic rocks of the Adobe Range were deposited in shallow water among islands in the western part of the epicontinental Phosphoria sea. The continental margin and the open ocean lay far to the west. At the same time, the Phosphoria Formation was being deposited in the eastern and central parts of the Phosphoria sea. Theories based on the work of Kasakov done in 1937 relating phosphate deposition directly to sites of upwelling oceanic waters are questioned. Nondeposition of diluent materials such as detritus and carbonate is probably of more importance in producing phosphate in economic concentrations than is geographic position with respect to upwelling waters.","language":"ENGLISH","publisher":"U.S. Geological Survey,","doi":"10.3133/ofr79239","usgsCitation":"Ketner, K., 1979, Phosphatic Permian rocks of the Adobe Range, Nevada, and their environment of deposition: U.S. Geological Survey Open-File Report 79-239, ii, 11 leaves :map ;28 cm.; (14 p. - PGS), https://doi.org/10.3133/ofr79239.","productDescription":"ii, 11 leaves :map ;28 cm.; (14 p. - PGS)","costCenters":[],"links":[{"id":153166,"rank":0,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/of/1979/0239/report-thumb.jpg"},{"id":49101,"rank":300,"type":{"id":11,"text":"Document"},"url":"https://pubs.usgs.gov/of/1979/0239/report.pdf","linkFileType":{"id":1,"text":"pdf"}}],"noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"4f4e4adee4b07f02db6876b6","contributors":{"authors":[{"text":"Ketner, Keith Brindley","contributorId":18332,"corporation":false,"usgs":true,"family":"Ketner","given":"Keith Brindley","affiliations":[],"preferred":false,"id":181236,"contributorType":{"id":1,"text":"Authors"},"rank":1}]}}
,{"id":19745,"text":"ofr79930 - 1979 - Preliminary catalog of earthquakes in northern Imperial Valley, California, October 1978-December 1978","interactions":[],"lastModifiedDate":"2023-10-06T19:44:09.297917","indexId":"ofr79930","displayToPublicDate":"1994-01-01T00:00:00","publicationYear":"1979","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":"79-930","title":"Preliminary catalog of earthquakes in northern Imperial Valley, California, October 1978-December 1978","docAbstract":"<p>The northern section of the Imperial Valley region in southern California is an area of known geothermal resources and high seismicity. To investigate the relationship between geothermal areas and earthquakes in the Imperial Valley, a 16-station seismic network was established in early 1973 by the U. S. Geological Survey. Six more stations were added to the network in November 1976. This catalog contains a description of the network and a list of preliminary data on earthquakes detected and recorded by the network from October 1978 through December 1973.</p>","language":"English","publisher":"U.S. Geological Survey","doi":"10.3133/ofr79930","usgsCitation":"Lamanuzzi, V., Johnson, C., and German, P., 1979, Preliminary catalog of earthquakes in northern Imperial Valley, California, October 1978-December 1978: U.S. Geological Survey Open-File Report 79-930, 12 p., https://doi.org/10.3133/ofr79930.","productDescription":"12 p.","costCenters":[],"links":[{"id":421753,"rank":2,"type":{"id":11,"text":"Document"},"url":"https://pubs.usgs.gov/of/1979/0930/report.pdf","linkFileType":{"id":1,"text":"pdf"}},{"id":154835,"rank":1,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/of/1979/0930/report-thumb.jpg"}],"country":"United States","state":"California","otherGeospatial":"northern Imperial Valley","geographicExtents":"{\n  \"type\": \"FeatureCollection\",\n  \"features\": [\n    {\n      \"type\": \"Feature\",\n      \"properties\": {},\n      \"geometry\": {\n        \"coordinates\": [\n          [\n            [\n              -116.25,\n              32.625\n            ],\n            [\n              -114.75,\n              32.625\n            ],\n            [\n              -114.75,\n              33.25\n            ],\n            [\n              -116.25,\n              33.24\n            ],\n            [\n              -116.25,\n              32.625\n            ]\n          ]\n        ],\n        \"type\": \"Polygon\"\n      }\n    }\n  ]\n}","noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"4f4e4ac9e4b07f02db67c830","contributors":{"authors":[{"text":"Lamanuzzi, V.","contributorId":60260,"corporation":false,"usgs":true,"family":"Lamanuzzi","given":"V.","email":"","affiliations":[],"preferred":false,"id":181433,"contributorType":{"id":1,"text":"Authors"},"rank":1},{"text":"Johnson, C.E.","contributorId":31741,"corporation":false,"usgs":true,"family":"Johnson","given":"C.E.","email":"","affiliations":[],"preferred":false,"id":181432,"contributorType":{"id":1,"text":"Authors"},"rank":2},{"text":"German, P.T.","contributorId":77554,"corporation":false,"usgs":true,"family":"German","given":"P.T.","email":"","affiliations":[],"preferred":false,"id":181434,"contributorType":{"id":1,"text":"Authors"},"rank":3}]}}
,{"id":19249,"text":"ofr79938 - 1979 - Preliminary geology of the Blacktail Mountain drilling site, Flathead County, Montana","interactions":[],"lastModifiedDate":"2012-02-02T00:07:31","indexId":"ofr79938","displayToPublicDate":"1994-01-01T00:00:00","publicationYear":"1979","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":"79-938","title":"Preliminary geology of the Blacktail Mountain drilling site, Flathead County, Montana","docAbstract":"Five argillitic green beds that alternate with six argillitic purple beds in the upper part of the Spokane Formation of the Belt Supergroup of Proterozoic Y age were sampled by 22 shallow core holes. The holes were drilled on a hexagonal pattern over an area about 50 m wide and 150 m long to obtain detailed information on environment of deposition and distribution of anomalous amounts of copper sulfides visible in outcrop, as well as to obtain samples for study of the geochemistry, isotope geology, mineralogy, and physical properties of the rocks and sulfide occurrences. Preliminary megascopic examination of the cores suggests that the purple and green colors represent original oxidizing and reducing environments of deposition on a relatively stable tidal flat and shallow shelf. Two of the five green beds contain zones of copper sulfides, largely bornite and chalcocite with trace amounts of chalcopyrite and covellite. The zones vary somewhat in thickness and stratigraphic position within the mineralized green beds. This report covers only the preliminary results of the ongoing multiple intensive studies of the drilling site and cores. These studies are part of an attempt to develop a model for green-bed copper- silver occurrences in Belt rocks of Proterozoic age. The model is needed to aid appraisal of the mineral potential of these mineral occurrences that are common in much of the 120,000 km2 of Belt terrane.","language":"ENGLISH","publisher":"U.S. Geological Survey,","doi":"10.3133/ofr79938","usgsCitation":"Harrison, J.E., and Reynolds, M.W., 1979, Preliminary geology of the Blacktail Mountain drilling site, Flathead County, Montana: U.S. Geological Survey Open-File Report 79-938, ii, 36 p., 1 over-size sheet :ill. ;28 cm., https://doi.org/10.3133/ofr79938.","productDescription":"ii, 36 p., 1 over-size sheet :ill. ;28 cm.","costCenters":[],"links":[{"id":151425,"rank":0,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/of/1979/0938/report-thumb.jpg"},{"id":48708,"rank":400,"type":{"id":17,"text":"Plate"},"url":"https://pubs.usgs.gov/of/1979/0938/plate-1.pdf","linkFileType":{"id":1,"text":"pdf"}},{"id":48709,"rank":300,"type":{"id":11,"text":"Document"},"url":"https://pubs.usgs.gov/of/1979/0938/report.pdf","linkFileType":{"id":1,"text":"pdf"}}],"noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"4f4e4abce4b07f02db673698","contributors":{"authors":[{"text":"Harrison, Jack Edward","contributorId":49778,"corporation":false,"usgs":true,"family":"Harrison","given":"Jack","email":"","middleInitial":"Edward","affiliations":[],"preferred":false,"id":180558,"contributorType":{"id":1,"text":"Authors"},"rank":1},{"text":"Reynolds, Mitchell W. 0000-0002-9966-3896 mwreynol@usgs.gov","orcid":"https://orcid.org/0000-0002-9966-3896","contributorId":4641,"corporation":false,"usgs":true,"family":"Reynolds","given":"Mitchell","email":"mwreynol@usgs.gov","middleInitial":"W.","affiliations":[{"id":318,"text":"Geosciences and Environmental Change Science Center","active":true,"usgs":true}],"preferred":true,"id":180557,"contributorType":{"id":1,"text":"Authors"},"rank":2}]}}
,{"id":19744,"text":"ofr79931 - 1979 - Preliminary catalog of earthquakes in northern Imperial Valley, California, July 1978 - September 1978","interactions":[],"lastModifiedDate":"2023-10-06T19:53:03.734469","indexId":"ofr79931","displayToPublicDate":"1994-01-01T00:00:00","publicationYear":"1979","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":"79-931","title":"Preliminary catalog of earthquakes in northern Imperial Valley, California, July 1978 - September 1978","docAbstract":"<p>The northern section of the Imperial Valley region in southern California is an area of known geothermal resources and high seismicity. To investigate the relationship between geothermal areas and earthquakes in the Imperial Valley, a 16-station seismic network was established in early 1973 by the U. S. Geological Survey. Six more stations were added to the network in November 1976. This catalog contains a description of the network and a list of preliminary data on earthquakes detected and recorded by the network from July 1978 through September 1978.</p>","language":"English","publisher":"U.S. Geological Survey","doi":"10.3133/ofr79931","usgsCitation":"Lamanuzzi, V., and Johnson, C., 1979, Preliminary catalog of earthquakes in northern Imperial Valley, California, July 1978 - September 1978: U.S. Geological Survey Open-File Report 79-931, 12 p., https://doi.org/10.3133/ofr79931.","productDescription":"12 p.","costCenters":[],"links":[{"id":154834,"rank":1,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/of/1979/0931/report-thumb.jpg"},{"id":421754,"rank":2,"type":{"id":11,"text":"Document"},"url":"https://pubs.usgs.gov/of/1979/0931/report.pdf","linkFileType":{"id":1,"text":"pdf"}}],"country":"United States","state":"California","otherGeospatial":"northern Imperial Valley","geographicExtents":"{\n  \"type\": \"FeatureCollection\",\n  \"features\": [\n    {\n      \"type\": \"Feature\",\n      \"properties\": {},\n      \"geometry\": {\n        \"coordinates\": [\n          [\n            [\n              -116.25,\n              32.625\n            ],\n            [\n              -114.75,\n              32.625\n            ],\n            [\n              -114.75,\n              33.25\n            ],\n            [\n              -116.25,\n              33.24\n            ],\n            [\n              -116.25,\n              32.625\n            ]\n          ]\n        ],\n        \"type\": \"Polygon\"\n      }\n    }\n  ]\n}","noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"4f4e4ac9e4b07f02db67c7d2","contributors":{"authors":[{"text":"Lamanuzzi, V.","contributorId":60260,"corporation":false,"usgs":true,"family":"Lamanuzzi","given":"V.","email":"","affiliations":[],"preferred":false,"id":181431,"contributorType":{"id":1,"text":"Authors"},"rank":1},{"text":"Johnson, C.E.","contributorId":31741,"corporation":false,"usgs":true,"family":"Johnson","given":"C.E.","email":"","affiliations":[],"preferred":false,"id":181430,"contributorType":{"id":1,"text":"Authors"},"rank":2}]}}
,{"id":19287,"text":"ofr79262 - 1979 - Better utilization of ground water in the Piedmont and mountain region of the Southeast","interactions":[{"subject":{"id":19287,"text":"ofr79262 - 1979 - Better utilization of ground water in the Piedmont and mountain region of the Southeast","indexId":"ofr79262","publicationYear":"1979","noYear":false,"title":"Better utilization of ground water in the Piedmont and mountain region of the Southeast"},"predicate":"SUPERSEDED_BY","object":{"id":70042633,"text":"70042633 - 1979 - Better utilization of ground water in the Piedmont and mountain region of the southeast","indexId":"70042633","publicationYear":"1979","noYear":false,"title":"Better utilization of ground water in the Piedmont and mountain region of the southeast"},"id":1}],"supersededBy":{"id":70042633,"text":"70042633 - 1979 - Better utilization of ground water in the Piedmont and mountain region of the southeast","indexId":"70042633","publicationYear":"1979","noYear":false,"title":"Better utilization of ground water in the Piedmont and mountain region of the southeast"},"lastModifiedDate":"2013-01-15T13:42:12","indexId":"ofr79262","displayToPublicDate":"1994-01-01T00:00:00","publicationYear":"1979","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":"79-262","title":"Better utilization of ground water in the Piedmont and mountain region of the Southeast","language":"ENGLISH","publisher":"U.S. Geological Survey","publisherLocation":"Reston, VA","doi":"10.3133/ofr79262","usgsCitation":"Heath, R., 1979, Better utilization of ground water in the Piedmont and mountain region of the Southeast: U.S. Geological Survey Open-File Report 79-262, iv, 22 p. :ill., map ;27 cm., https://doi.org/10.3133/ofr79262.","productDescription":"iv, 22 p. :ill., map ;27 cm.","costCenters":[],"links":[{"id":151706,"rank":0,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/thumbnails/usgs_thumb.jpg"}],"noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"4f4e4a14e4b07f02db602d5c","contributors":{"authors":[{"text":"Heath, Ralph C.","contributorId":53359,"corporation":false,"usgs":true,"family":"Heath","given":"Ralph C.","affiliations":[],"preferred":false,"id":180620,"contributorType":{"id":1,"text":"Authors"},"rank":1}]}}
,{"id":19207,"text":"ofr79228 - 1979 - Analyses of surficial deposits, central Brooks Range, Alaska","interactions":[],"lastModifiedDate":"2024-02-14T22:27:25.096787","indexId":"ofr79228","displayToPublicDate":"1994-01-01T00:00:00","publicationYear":"1979","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":"79-228","title":"Analyses of surficial deposits, central Brooks Range, Alaska","docAbstract":"<p>Seventy-nine sediment samples from the central Brooks Range were analyzed for grain-size distribution, shape and composition of grains, and other physical properties. Four statistical measures (sorting, mean diameter, skewness, and kurtosis) were then computed for the sand-to-clay size fraction of all samples.</p><p>Fan sediments resemble the other alluvial-gravel deposits in consisting of sand and gravel from which very fine sand and the smaller size fractions have been removed by running water. Sorting and rounding of particles is best at the distal ends of large fans. Modern alluvium is better sorted than most fan deposits, with more rounded clasts and generally higher ratios of sand to gravel. Other alluvial deposits from terraces and heavily dissected erosion remnants generally are comparable to modern alluvium. All classes of alluvial gravel are characterized by removal of fines and by decreasing values of mean 0, kurtosis, and skewness as sorting increases. Most samples also have high clay/silt ratios that probably were caused by deflation on windswept bars and floodplains.</p><p>Lacustrine deposits have clay percentages ranging from about 85 to 35, with silt predominant in more than one-half of the samples. Several samples contain sand and gravel that presumably were ice rafted. Clay-sized particles are unweathered mineral grains, implying that glacial abrasion was their primary source.</p><p>Flow-slide deposits are very poorly sorted mixtures of gravel, sand, and silt, with clay content averaging only about one percent. Clasts consist of angular fragments of local bedrock, usually schist and phyllite, and matrix materials usually are highly micaceous. Although related flow types, a mud-flow and a debris-flow in till, are generally similar to flow-slide deposits, the mudflow has been modified by running water and the debris flow reflects the composition of its parent till. Other colluvial deposits commonly have high silt and low clay contents, but one solifluction deposit has abundant clay derived from till. Several of the flow-slides and other colluvial deposits are polygenetic, having undergone several episodes of flow that incorporated different types of sediment.<br></p><p>Sand deposits include silty floodplain and basin-fill deposits as well as five relatively pure and well sorted dunal and river-bar sands. The silt-rich deposits probably contain large amounts of loess that fell into late-Pleistocene basin fillings and muskegs and later was redeposited on Holocene floodplains. The five dunal and bar sands are dominantly medium to fine sand; relatively well sorted, symmetric to coarse skewed, and leptokurtic. The dunal sands can be distinguished by the presence of very fine sand: wind apparently is less effective than flowing water in removing the finest sand fraction.</p><p>The glacial deposits consist of till, ice-content stratified drift, and outwash. Till is a poorly sorted mixed sediment that resembles many flow de-posits but typically contains more clay. Two clay-deficient tills resemble fan deposits, implying effective washing by meltwater during glacial transport or deposition of these deposits. The ice-contact stratified drift varies in character from fan-like gravel deposits to sand accumulations nearly as well sorted as those of river bars. Almost all samples reflect some restriction in washing of fines by meltwater, probably owing to irregular topography and resulting poor drainage on and around stagnating glaciers. Most outwash deposits have less fine sand than modern alluvium, probably reflecting the generally high energy of glacial meltwater streams and the absence of vegetation from their floodplains. Samples from the southern Brooks Range are better sorted than those from northern Brooks Range valleys, and their statistical values lie close to those of modern alluvium.</p><p>Comparisons between the different classes of sediments are facilitated by combining them into (1) gravel, (2) sand, silt, and clay, and (3) mixed deposits. Deposits of unknown or uncertain origin may then be compared directly against sediments from modern streams, dunes, flow-slides and other known sources, and alternative origins of aberrant samples in each of the sediment classes can also be examined. Several samples that initially were classed as fan, lacustrine, or glacial proved to be mixed deposits created by frost-churning, frost-lifting of stones, flowage down faces of river bluffs, and other postdepositional processes.</p><p>Sorting and mean <span>ϕ</span> of matrix materials were useful in distinguishing the different sediment classes, separating them into contrasting subgroups, and identifying atypical samples. Skewness and kurtosis were generally less useful in this study.</p>","language":"English","publisher":"U.S. Geological Survey","doi":"10.3133/ofr79228","usgsCitation":"Hamilton, T.D., Trexler, J., and McCalpin, J., 1979, Analyses of surficial deposits, central Brooks Range, Alaska: U.S. Geological Survey Open-File Report 79-228, iv, 95 p., https://doi.org/10.3133/ofr79228.","productDescription":"iv, 95 p.","costCenters":[],"links":[{"id":425672,"rank":2,"type":{"id":11,"text":"Document"},"url":"https://pubs.usgs.gov/of/1979/0228/report.pdf","linkFileType":{"id":1,"text":"pdf"}},{"id":150755,"rank":1,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/of/1979/0228/report-thumb.jpg"}],"country":"United States","state":"Alaska","otherGeospatial":"Brooks Range","geographicExtents":"{\n  \"type\": \"FeatureCollection\",\n  \"features\": [\n    {\n      \"type\": \"Feature\",\n      \"properties\": {},\n      \"geometry\": {\n        \"coordinates\": [\n          [\n            [\n              -161.26152963188818,\n              68.52322762665835\n            ],\n            [\n              -161.26152963188818,\n              67.19731766361306\n            ],\n            [\n              -143.62139800284058,\n              67.19731766361306\n            ],\n            [\n              -143.62139800284058,\n              68.52322762665835\n            ],\n            [\n              -161.26152963188818,\n              68.52322762665835\n            ]\n          ]\n        ],\n        \"type\": \"Polygon\"\n      }\n    }\n  ]\n}","noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"4f4e4ad0e4b07f02db680d46","contributors":{"authors":[{"text":"Hamilton, Thomas D.","contributorId":91474,"corporation":false,"usgs":true,"family":"Hamilton","given":"Thomas","email":"","middleInitial":"D.","affiliations":[],"preferred":false,"id":180495,"contributorType":{"id":1,"text":"Authors"},"rank":1},{"text":"Trexler, James H.","contributorId":85612,"corporation":false,"usgs":true,"family":"Trexler","given":"James H.","affiliations":[],"preferred":false,"id":180494,"contributorType":{"id":1,"text":"Authors"},"rank":2},{"text":"McCalpin, James","contributorId":72005,"corporation":false,"usgs":true,"family":"McCalpin","given":"James","affiliations":[],"preferred":false,"id":180493,"contributorType":{"id":1,"text":"Authors"},"rank":3}]}}
,{"id":15167,"text":"ofr79206 - 1979 - Proceedings of the First membership conference of the National Water Data Exchange, May 9-11, 1978, Denver, Colorado","interactions":[],"lastModifiedDate":"2012-02-02T00:07:00","indexId":"ofr79206","displayToPublicDate":"1994-01-01T00:00:00","publicationYear":"1979","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":"79-206","title":"Proceedings of the First membership conference of the National Water Data Exchange, May 9-11, 1978, Denver, Colorado","docAbstract":"This report contains the proceedings of the first membership conference of the National Water Data Exchange (NAWDEX). The purpose of the conference was to acquaint participants in the NAWDEX program with the systems, data resources, and services available throughout the membership, to establish improved personal relationships within the membership, and to serve as a forum for the exchange of ideas and expertise on matters relating to improving the operation of NAWDEX and identifying the needs of the water-data community. Sixteen papers were presented at the conference which describe data systems of member organizations, needs of the data community, and programs of national interest. These papers are published in their entirety in this proceedings volume. Four working panels were also conducted dealing with (1) Program Administration, Management, and Coordination; (2) Recommended Standards for the Handling and Exchange of Water Data; (3) Water Data Indexing and Technical Systems Development; and (4) Request, Response and Service Activities. The reports and conclusions of these panels are included also. (Woodard-USGS)","language":"ENGLISH","publisher":"U.S. Geological Survey,","doi":"10.3133/ofr79206","usgsCitation":"Myers, B.M., and Nokes, J.M., 1979, Proceedings of the First membership conference of the National Water Data Exchange, May 9-11, 1978, Denver, Colorado: U.S. Geological Survey Open-File Report 79-206, viii, 260 p. :ill., maps ;26 cm., https://doi.org/10.3133/ofr79206.","productDescription":"viii, 260 p. :ill., maps ;26 cm.","costCenters":[],"links":[{"id":94446,"rank":9999,"type":{"id":10,"text":"Digital Object Identifier"},"url":"https://hdl.handle.net/2027/mdp.39015010198052?urlappend=%3Bseq=7"},{"id":112984,"rank":300,"type":{"id":11,"text":"Document"},"url":"https://pubs.usgs.gov/of/1979/0206/report.pdf","size":"14704","linkFileType":{"id":1,"text":"pdf"}},{"id":147968,"rank":0,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/of/1979/0206/report-thumb.jpg"}],"noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"4f4e4a8fe4b07f02db654dd9","contributors":{"authors":[{"text":"Myers, Beverly M.","contributorId":31733,"corporation":false,"usgs":true,"family":"Myers","given":"Beverly","email":"","middleInitial":"M.","affiliations":[],"preferred":false,"id":170679,"contributorType":{"id":1,"text":"Authors"},"rank":1},{"text":"Nokes, Janet M.","contributorId":103274,"corporation":false,"usgs":true,"family":"Nokes","given":"Janet","email":"","middleInitial":"M.","affiliations":[],"preferred":false,"id":170680,"contributorType":{"id":1,"text":"Authors"},"rank":2}]}}
,{"id":15015,"text":"ofr80348 - 1979 - Hydrologic data collected at closure of Gainesville Lock and Dam, Tombigbee River near Gainesville, Alabama","interactions":[],"lastModifiedDate":"2022-07-25T17:49:21.159366","indexId":"ofr80348","displayToPublicDate":"1994-01-01T00:00:00","publicationYear":"1979","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":"80-348","title":"Hydrologic data collected at closure of Gainesville Lock and Dam, Tombigbee River near Gainesville, Alabama","docAbstract":"<p>The Gainesville Lock and Dam is the first of ten lock and dam projects on the Tennessee-Tombigbee Waterway to be completed. The structure was completed in 1978 and filling of the reservoir commenced March 20, 1978 resulting in changes in stream stage and discharge, ground-water levels, and chemical quality of the water.</p>","language":"English","publisher":"U.S. Geological Survey","doi":"10.3133/ofr80348","collaboration":"Prepared in cooperation with the U.S. Army Corps of Engineers","usgsCitation":"Ming, E.G., and Sedberry, F.C., 1979, Hydrologic data collected at closure of Gainesville Lock and Dam, Tombigbee River near Gainesville, Alabama: U.S. Geological Survey Open-File Report 80-348, v, 33 p., https://doi.org/10.3133/ofr80348.","productDescription":"v, 33 p.","costCenters":[],"links":[{"id":404428,"rank":2,"type":{"id":11,"text":"Document"},"url":"https://pubs.usgs.gov/of/1980/0348/report.pdf","linkFileType":{"id":1,"text":"pdf"}},{"id":148023,"rank":0,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/of/1980/0348/report-thumb.jpg"}],"country":"United States","state":"Alabama","city":"Gainesville","otherGeospatial":"Tombigbee River","geographicExtents":"{\n  \"type\": \"FeatureCollection\",\n  \"features\": [\n    {\n      \"type\": \"Feature\",\n      \"properties\": {},\n      \"geometry\": {\n        \"type\": \"Polygon\",\n        \"coordinates\": [\n          [\n            [\n              -88.17695617675781,\n              32.8092074693633\n            ],\n            [\n              -88.13438415527344,\n              32.8092074693633\n            ],\n            [\n              -88.13438415527344,\n              32.834019798849624\n            ],\n            [\n              -88.17695617675781,\n              32.834019798849624\n            ],\n            [\n              -88.17695617675781,\n              32.8092074693633\n            ]\n          ]\n        ]\n      }\n    }\n  ]\n}","noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"4f4e4ad5e4b07f02db683504","contributors":{"authors":[{"text":"Ming, E. Grady","contributorId":62227,"corporation":false,"usgs":true,"family":"Ming","given":"E.","email":"","middleInitial":"Grady","affiliations":[],"preferred":false,"id":170416,"contributorType":{"id":1,"text":"Authors"},"rank":1},{"text":"Sedberry, Fletcher C.","contributorId":56238,"corporation":false,"usgs":true,"family":"Sedberry","given":"Fletcher","email":"","middleInitial":"C.","affiliations":[],"preferred":false,"id":170415,"contributorType":{"id":1,"text":"Authors"},"rank":2}]}}
,{"id":13204,"text":"ofr80167 - 1979 - The brightness of lights on Earth at night, digitally recorded by DMSP satellite","interactions":[],"lastModifiedDate":"2017-05-09T15:14:50","indexId":"ofr80167","displayToPublicDate":"1994-01-01T00:00:00","publicationYear":"1979","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":"80-167","title":"The brightness of lights on Earth at night, digitally recorded by DMSP satellite","docAbstract":"<p>The U.S. Air Force has operated its Defense Meteorological Satellite Program (DMSP) for nearly a decade, and film images from the system have been openly available since 1973. Films are well suited for the study of weather, and users of such films have derived much useful data. For many potential remote sensing applications, however, a quantitative measurement of the brightness of the imaged light patterns is needed, and it cannot be extracted with adequte accuracy from the films. Such information is contained in the telemetry from the spacecraft and is retained on digital tapes, which store the images for a few days while they await filming. For practical reasons, it has not heretofore been feasible for the Air Force to provide a remote-sensing user with these digital data, and the quantitative brightness information has been lost with the erasure of tapes for re-use. </p><p>For the purpose of evaluation of tapes as a means for remote sensing, the Air Force recently did provide to the author six examples containing records of nighttime DMSP imagery similar to that which has previously 1 been evaluated by SRI International in a film format. The digital data create many new applications for these images, owing to a combination of several factors, the most important of which are the preservation of photometric information and of full spatial resolution. In this evaluation, stress has been placed upon determination of the broad potential value of the data rather than the full exploitation of any one aspect of it. The effort was guided by an objective to develop handling methods for the vast body of numbers--methods which will be practical for use in a research or engineering environment where budgets are limited, and specialized capabilities and image reproduction equipment has not already been developed. We report the degree of success obtained in this effort, pointing out the relative strengths and the relative limitations, as compared to the sophisticated, weather-oriented data processing which is well suited for the Air Force requirements. </p><p>Both geometric and photometric calibration methods are evaluated. An image can be considered as a 3-dimensional array, X, Y, Z, in which X and Y are the coordinates of a picture element (pixel) and Z is the brightness at that location. A method of approach to handling these parameters, particularly Y and Z, is developed in a form quite different from that which serves the operational applications. </p><p>The user of digital data will need the film images which are generated by the Air Force from the same data as is provided on digital tape. In the first stages of analysis, the films provide both a convenient index and a guide to identification of large patterns in the data. Additionally, the infrared (8 to 13 0 film provides a valuable indicator of cloud cover. </p><p>Two general conclusions are drawn from this study. Firstly, the digital DMSP data have great potential value but their cost, in terms of the interruption of the present operational routine, is quite high. Therefore, if a program is undertaken to provide for the open availability of an archive of digital records, great care must be exercised in selecting only those records which have unusually high value in order that the effort will be cost-effective. Secondly, it is concluded that several aspects of the program, well designed for Air Force operational purposes, are not adapted to earth-sensing needs. This is probably inevitable, since the two applications are largely different and in some ways incompatible. For example, the nighttime visual sensor saturates in the center of major cities and in moderately large fires (such as gas flares). This saturation prevents the analyst from integrating photometric parameters. For weather observation, this inability is unimportant, and acceptance of such saturation makes feasible a decrease in the data rate. </p><p>Such limitations in the data will probably be overcome only through modifying the existing system or the implementation of a similar system designed specifically to serve earth-sensing needs. </p>","language":"English","publisher":"U.S. Geological Survey","publisherLocation":"Reston, VA","doi":"10.3133/ofr80167","usgsCitation":"Croft, T.A., 1979, The brightness of lights on Earth at night, digitally recorded by DMSP satellite: U.S. Geological Survey Open-File Report 80-167, vi, 57 p., https://doi.org/10.3133/ofr80167.","productDescription":"vi, 57 p.","numberOfPages":"66","costCenters":[],"links":[{"id":341010,"rank":2,"type":{"id":11,"text":"Document"},"url":"https://pubs.usgs.gov/of/1980/0167/report.pdf","linkFileType":{"id":1,"text":"pdf"}},{"id":146748,"rank":0,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/of/1980/0167/report-thumb.jpg"}],"noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"4f4e4aaae4b07f02db66963d","contributors":{"authors":[{"text":"Croft, Thomas A.","contributorId":33328,"corporation":false,"usgs":true,"family":"Croft","given":"Thomas","email":"","middleInitial":"A.","affiliations":[],"preferred":false,"id":167400,"contributorType":{"id":1,"text":"Authors"},"rank":1}]}}
,{"id":13956,"text":"ofr791066 - 1979 - Derivation of homogeneous streamflow records for the Green River basin, Kentucky","interactions":[],"lastModifiedDate":"2012-02-02T00:06:53","indexId":"ofr791066","displayToPublicDate":"1994-01-01T00:00:00","publicationYear":"1979","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":"79-1066","title":"Derivation of homogeneous streamflow records for the Green River basin, Kentucky","docAbstract":"Four flood-control reservoirs, Green River Lake, Nolin River Lake, Barren River Lake, and Rough River Lake, were completed in the Green River basin of Kentucky between 1959 and 1969. A digital computer model of these reservoirs and the stream reaches from the reservoirs downstream to the Green River at Calhoun, Ky., was developed to simulate mean daily streamflows. Simulations of 1941 through 1971 water year streamflows were made for both the pre-reservoir and post-reservoir basin conditions, thus supplying homogeneous data sets for low-flow analyses of eight stream sites. The 7-day, 10-year recurrence interval, minimum discharges of the simulated regulated flows exceed those of the simulated natural flows by about 30 cubic feet per second for the Barren River at Bowling Green, Ky., and about 260 cubic feet per second for the Green River at Calhous, Ky. Analyses of the pre-reservoir simulations show that, for seven of the stream sites, the model yields streamflow which have annual minimum 7-day average discharges that are not significantly different, at the 95 percent significance level, from those of the observed flows. Results of the post-reservoir simulations show that actual reservoir operation was not closely matched by the model. Therefore, the low-flow characteristics of the simulated regulated streamflows are merely estimates of those that could be expected if the basin were regulated according to the modeled reservoir operating criteria. (USGS)","language":"ENGLISH","publisher":"U.S. Geological Survey,","doi":"10.3133/ofr791066","usgsCitation":"Hale, T., 1979, Derivation of homogeneous streamflow records for the Green River basin, Kentucky: U.S. Geological Survey Open-File Report 79-1066, vii, 96 p. :ill. ;28 cm., https://doi.org/10.3133/ofr791066.","productDescription":"vii, 96 p. :ill. ;28 cm.","costCenters":[],"links":[{"id":147132,"rank":0,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/thumbnails/usgs_thumb.jpg"}],"noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"4f4e4ab0e4b07f02db66d709","contributors":{"authors":[{"text":"Hale, T.W.","contributorId":43763,"corporation":false,"usgs":true,"family":"Hale","given":"T.W.","email":"","affiliations":[],"preferred":false,"id":168695,"contributorType":{"id":1,"text":"Authors"},"rank":1}]}}
,{"id":13163,"text":"ofr791516 - 1979 - Mineral map of the Bopolu Quadrangle, Liberia","interactions":[],"lastModifiedDate":"2012-02-02T00:06:48","indexId":"ofr791516","displayToPublicDate":"1994-01-01T00:00:00","publicationYear":"1979","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":"79-1516","title":"Mineral map of the Bopolu Quadrangle, Liberia","language":"ENGLISH","publisher":"U.S. Geological Survey,","doi":"10.3133/ofr791516","usgsCitation":"Coonrad, W.L., 1979, Mineral map of the Bopolu Quadrangle, Liberia: U.S. Geological Survey Open-File Report 79-1516, i, 27 p., 1 over-size sheet, scale 1:250,000 ;27 cm., https://doi.org/10.3133/ofr791516.","productDescription":"i, 27 p., 1 over-size sheet, scale 1:250,000 ;27 cm.","costCenters":[],"links":[{"id":145952,"rank":0,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/of/1979/1516/report-thumb.jpg"},{"id":41561,"rank":300,"type":{"id":11,"text":"Document"},"url":"https://pubs.usgs.gov/of/1979/1516/report.pdf","linkFileType":{"id":1,"text":"pdf"}},{"id":41560,"rank":400,"type":{"id":17,"text":"Plate"},"url":"https://pubs.usgs.gov/of/1979/1516/plate-1.pdf","linkFileType":{"id":1,"text":"pdf"}}],"scale":"250000","noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"4f4e4a61e4b07f02db635b82","contributors":{"authors":[{"text":"Coonrad, W. L.","contributorId":69946,"corporation":false,"usgs":true,"family":"Coonrad","given":"W.","email":"","middleInitial":"L.","affiliations":[],"preferred":false,"id":167336,"contributorType":{"id":1,"text":"Authors"},"rank":1}]}}
,{"id":11056,"text":"ofr791609 - 1979 - Catalog of creepmeter measurements in central California for 1976 and 1977","interactions":[],"lastModifiedDate":"2012-02-02T00:06:24","indexId":"ofr791609","displayToPublicDate":"1994-01-01T00:00:00","publicationYear":"1979","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":"79-1609","title":"Catalog of creepmeter measurements in central California for 1976 and 1977","language":"ENGLISH","publisher":"U.S. Geological Survey,","doi":"10.3133/ofr791609","usgsCitation":"Schulz, S.S., and Burford, R.O., 1979, Catalog of creepmeter measurements in central California for 1976 and 1977: U.S. Geological Survey Open-File Report 79-1609, 380 p. :ill., maps ;28 cm., https://doi.org/10.3133/ofr791609.","productDescription":"380 p. :ill., maps ;28 cm.","costCenters":[],"links":[{"id":143333,"rank":0,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/thumbnails/usgs_thumb.jpg"}],"noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"4f4e49f3e4b07f02db5efbb4","contributors":{"authors":[{"text":"Schulz, Sandra S.","contributorId":104864,"corporation":false,"usgs":true,"family":"Schulz","given":"Sandra","email":"","middleInitial":"S.","affiliations":[],"preferred":false,"id":162453,"contributorType":{"id":1,"text":"Authors"},"rank":1},{"text":"Burford, Robert O.","contributorId":52560,"corporation":false,"usgs":true,"family":"Burford","given":"Robert","middleInitial":"O.","affiliations":[],"preferred":false,"id":162452,"contributorType":{"id":1,"text":"Authors"},"rank":2}]}}
,{"id":13949,"text":"ofr80129 - 1979 - Reconnaissance geology of the Jabal 'Afaf Quadrangle, sheet 20/40 D, Kingdom of Saudi Arabia","interactions":[],"lastModifiedDate":"2012-02-02T00:06:53","indexId":"ofr80129","displayToPublicDate":"1994-01-01T00:00:00","publicationYear":"1979","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":"80-129","title":"Reconnaissance geology of the Jabal 'Afaf Quadrangle, sheet 20/40 D, Kingdom of Saudi Arabia","language":"ENGLISH","publisher":"U.S. Geological Survey,","doi":"10.3133/ofr80129","usgsCitation":"Hadley, D.G., and Fleck, R.J., 1979, Reconnaissance geology of the Jabal 'Afaf Quadrangle, sheet 20/40 D, Kingdom of Saudi Arabia: U.S. Geological Survey Open-File Report 80-129, v, 34 p. maps (2 fold. in pocket) ;28 cm., https://doi.org/10.3133/ofr80129.","productDescription":"v, 34 p. maps (2 fold. in pocket) ;28 cm.","costCenters":[],"links":[{"id":147106,"rank":0,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/of/1980/0129/report-thumb.jpg"},{"id":42606,"rank":400,"type":{"id":17,"text":"Plate"},"url":"https://pubs.usgs.gov/of/1980/0129/plate-1.pdf","linkFileType":{"id":1,"text":"pdf"}},{"id":42607,"rank":401,"type":{"id":17,"text":"Plate"},"url":"https://pubs.usgs.gov/of/1980/0129/plate-2.pdf","linkFileType":{"id":1,"text":"pdf"}},{"id":42608,"rank":300,"type":{"id":11,"text":"Document"},"url":"https://pubs.usgs.gov/of/1980/0129/report.pdf","linkFileType":{"id":1,"text":"pdf"}}],"noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"4f4e4a6fe4b07f02db6409dd","contributors":{"authors":[{"text":"Hadley, Donald G.","contributorId":19527,"corporation":false,"usgs":true,"family":"Hadley","given":"Donald","email":"","middleInitial":"G.","affiliations":[],"preferred":false,"id":168686,"contributorType":{"id":1,"text":"Authors"},"rank":1},{"text":"Fleck, Robert Joseph","contributorId":101259,"corporation":false,"usgs":true,"family":"Fleck","given":"Robert","email":"","middleInitial":"Joseph","affiliations":[],"preferred":false,"id":168687,"contributorType":{"id":1,"text":"Authors"},"rank":2}]}}
,{"id":14533,"text":"ofr791058 - 1979 - Programs and activities of the Missouri District, Water Resources Division, U.S. Geological Survey, fiscal year 1979","interactions":[],"lastModifiedDate":"2017-09-29T08:41:13","indexId":"ofr791058","displayToPublicDate":"1994-01-01T00:00:00","publicationYear":"1979","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":"79-1058","title":"Programs and activities of the Missouri District, Water Resources Division, U.S. Geological Survey, fiscal year 1979","docAbstract":"<p>Water-resources investigations of the U.S. Geological Survey in Missouri consist of collecting hydrologic data and conducting interpretive investigations. The data and the results of the investigations are published or released by either the U.S. Geological Survey or by cooperating agencies. This report describes the data-collection activities and investigations in Missouri for the 1979 fiscal year and provides an extensive list of water-resources references for the State.</p>","language":"English","publisher":"U.S. Geological Survey","doi":"10.3133/ofr791058","usgsCitation":"1979, Programs and activities of the Missouri District, Water Resources Division, U.S. Geological Survey, fiscal year 1979: U.S. Geological Survey Open-File Report 79-1058, Report: iii, 57 p.; Plate: 24.20 x 21.80 inches, https://doi.org/10.3133/ofr791058.","productDescription":"Report: iii, 57 p.; Plate: 24.20 x 21.80 inches","numberOfPages":"69","costCenters":[{"id":396,"text":"Missouri Water Science 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,{"id":13833,"text":"ofr791580 - 1979 - Selected water-level records for Oklahoma, 1976-1978","interactions":[],"lastModifiedDate":"2017-09-29T08:42:49","indexId":"ofr791580","displayToPublicDate":"1994-01-01T00:00:00","publicationYear":"1979","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":"79-1580","title":"Selected water-level records for Oklahoma, 1976-1978","docAbstract":"<p>A systematic program to collect water-level records in Oklahoma began in 1937. The objectives of this program are (1) to provide long-term records of water-level fluctuations in representative wells, (2) to facilitate the prediction of water-level trends and indicate future availability of ground-water supplies, and (3) to provide information for use in basic research.</p><p>Water-level data in table 1 are from wells that are measured annually, prior to the irrigation season, to achieve the most natural representation of the static water level. Water-level measurements listed in the column under 1976 may have been made during December 1975 or January, February, March, April, or May, 1976. Measurements listed in the column 1977 may have been made during December 1976 or January, February, March, or April 1977. Figure 1 shows the counties and number of wells therein, where data were obtained for this report.</p><p>Records of water levels in Oklahoma are collected through a cooperative program by the U.S. Geological Survey and the Oklahoma Water Resources Board. The records are tabulated and published by the U.S. Geological Survey on an annual basis.</p><p>The stratigraphic nomenclature and age determinations used in this report are those accepted by the Oklahoma Geological Survey and do not necessarily agree with those of the U.S. Geological Survey except for the Cheyenne Sandstone which is considered to be Purgatoire Sandstone by the Oklahoma Geological Survey (Robert 0. Fay, Personal Communication, August 9, 1979).</p>","language":"English","publisher":"U.S. Geological Survey","doi":"10.3133/ofr791580","usgsCitation":"Goemaat, R.L., and Spiser, D.E., 1979, Selected water-level records for Oklahoma, 1976-1978: U.S. Geological Survey Open-File Report 79-1580, vi, 48 p., https://doi.org/10.3133/ofr791580.","productDescription":"vi, 48 p.","numberOfPages":"57","costCenters":[{"id":516,"text":"Oklahoma Water Science Center","active":true,"usgs":true}],"links":[{"id":346228,"rank":2,"type":{"id":11,"text":"Document"},"url":"https://pubs.usgs.gov/of/1979/1580/report.pdf","linkFileType":{"id":1,"text":"pdf"}},{"id":146092,"rank":0,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/of/1979/1580/report-thumb.jpg"}],"country":"United 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