Samples of surface water were collected and analyzed by the Illinois Environmental Protection Agency. The results from water years 1975 to 1977 are presented in three volumes. The history of sampling and analytical methods used during that period are summarized. Stream discharge data from records of the U.S. Geological Survey are included for all sites where samples were collected at gaging stations or near enough that reliable discharge estimates could be made. Volume III includes Ohio River tributaries and Mississippi River tributaries south of Illinois River basin.
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No abstract available.
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Nitrogenous and carbonaceous oxygen consumption were separated by using an inhibitor of nitrification 1-allyl-2-thiourea. The comparison was conducted in the laboratory using samples collected from the water column. Nitrification accounted for 38 to 52 percent of the total oxygen consumption. Nitrifying bacteria were enumerated from the same reach of the river. The population of Nitrosomonas ranged from 10 to 1,000 per milliliter in the water column and 100 to 100,000 per gram of benthic sediment. The nitrobacter population ranged from 10 to 100 per milliliter in the water column and 100 to 1,000 per gram in the benthic sediment. The concentration of ammonium, nitrite, and nitrate as N was determined from water samples collected throughout the study reach. The average rate of ammonium disappearance and of nitrate appearance was 0.02 milligram per liter per hour of flow time. 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\"}}]}","noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"4f4e4aa8e4b07f02db667651","contributors":{"authors":[{"text":"Ehlke, Theodore A.","contributorId":83523,"corporation":false,"usgs":true,"family":"Ehlke","given":"Theodore","email":"","middleInitial":"A.","affiliations":[],"preferred":false,"id":235939,"contributorType":{"id":1,"text":"Authors"},"rank":1}]}} ,{"id":67725,"text":"l52 - 1979 - Land use and land cover, 1973, Seguin, Texas","interactions":[],"lastModifiedDate":"2012-02-10T00:11:24","indexId":"l52","displayToPublicDate":"1994-01-01T00:00:00","publicationYear":"1979","noYear":false,"publicationType":{"id":18,"text":"Report"},"publicationSubtype":{"id":5,"text":"USGS Numbered Series"},"seriesTitle":{"id":321,"text":"Land Use and Land Cover","code":"L","active":false,"publicationSubtype":{"id":5}},"seriesNumber":"52","title":"Land use and land cover, 1973, Seguin, Texas","language":"ENGLISH","doi":"10.3133/l52","usgsCitation":"Water Resources Division, U.S. Geological Survey, 1979, Land use and land cover, 1973, Seguin, Texas: U.S. Geological Survey Land Use and Land Cover 52, -, https://doi.org/10.3133/l52.","productDescription":"-","costCenters":[],"links":[{"id":188620,"rank":0,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/thumbnails/usgs_thumb.jpg"},{"id":261032,"rank":900,"type":{"id":17,"text":"Plate"},"url":"https://pubs.usgs.gov/l/052/plate-1.pdf"}],"scale":"250000","geographicExtents":"{ \"type\": \"FeatureCollection\", \"features\": [ { \"type\": \"Feature\", \"properties\": {}, \"geometry\": { \"type\": \"Polygon\", \"coordinates\": [ [ [ -98,29 ], [ -98,30 ], [ -96,30 ], [ -96,29 ], [ -98,29 ] ] ] } } ] }","noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"4f4e4b24e4b07f02db6ae4d3","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":534471,"contributorType":{"id":1,"text":"Authors"},"rank":1}]}} ,{"id":10714,"text":"ofr791321 - 1979 - Decollement in the southern Allegheny Plateau of Pennsylvania","interactions":[],"lastModifiedDate":"2012-02-02T00:06:25","indexId":"ofr791321","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":"79-1321","title":"Decollement in the southern Allegheny Plateau of Pennsylvania","docAbstract":"Recent field investigations in the Allegheny Plateau north of Williamsport, Pennsylvania have shown the presence of both southward dipping, low-angle thrust faults translated to the north and northward dipping back or antithectic thrusts translated to the south at the leading (north) edge of Barclay syncline. The presence of these thrusts, along with reported anomalous dips along the leading edge of the next syncline to the south (the Bernice or Barbours syncline) may indicate that the Allegheny Plateau of Pennsylvania is underlain by master decollement and that this decollement gives rise to a series of splay thrusts. In some cases such as the Barclay syncline, the combination of these forward and back thrust faults may serve as fracture porosity traps.","language":"ENGLISH","publisher":"U.S. Geological Survey,","doi":"10.3133/ofr791321","usgsCitation":"Pohn, H.A., and Purdy, T.L., 1979, Decollement in the southern Allegheny Plateau of Pennsylvania: U.S. Geological Survey Open-File Report 79-1321, 10 p. :ill., maps ;27 cm., https://doi.org/10.3133/ofr791321.","productDescription":"10 p. :ill., maps ;27 cm.","costCenters":[],"links":[{"id":143309,"rank":0,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/of/1979/1321/report-thumb.jpg"},{"id":38524,"rank":300,"type":{"id":11,"text":"Document"},"url":"https://pubs.usgs.gov/of/1979/1321/report.pdf","linkFileType":{"id":1,"text":"pdf"}}],"noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"4f4e4abbe4b07f02db6725ec","contributors":{"authors":[{"text":"Pohn, Howard A.","contributorId":66681,"corporation":false,"usgs":true,"family":"Pohn","given":"Howard","email":"","middleInitial":"A.","affiliations":[],"preferred":false,"id":161843,"contributorType":{"id":1,"text":"Authors"},"rank":1},{"text":"Purdy, Terri L.","contributorId":87950,"corporation":false,"usgs":true,"family":"Purdy","given":"Terri","email":"","middleInitial":"L.","affiliations":[],"preferred":false,"id":161844,"contributorType":{"id":1,"text":"Authors"},"rank":2}]}} ,{"id":69350,"text":"l28 - 1979 - Land use and land cover, 1974, Pratt, Kansas","interactions":[],"lastModifiedDate":"2012-02-10T00:11:32","indexId":"l28","displayToPublicDate":"1994-01-01T00:00:00","publicationYear":"1979","noYear":false,"publicationType":{"id":18,"text":"Report"},"publicationSubtype":{"id":5,"text":"USGS Numbered Series"},"seriesTitle":{"id":321,"text":"Land Use and Land Cover","code":"L","active":false,"publicationSubtype":{"id":5}},"seriesNumber":"28","title":"Land use and land cover, 1974, Pratt, Kansas","language":"ENGLISH","doi":"10.3133/l28","usgsCitation":"Water Resources Division, U.S. Geological Survey, 1979, Land use and land cover, 1974, Pratt, Kansas: U.S. Geological Survey Land Use and Land Cover 28, -, https://doi.org/10.3133/l28.","productDescription":"-","costCenters":[],"links":[{"id":191021,"rank":0,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/thumbnails/usgs_thumb.jpg"},{"id":261175,"rank":900,"type":{"id":17,"text":"Plate"},"url":"https://pubs.usgs.gov/l/028/plate-1.pdf"}],"scale":"250000","geographicExtents":"{ \"type\": \"FeatureCollection\", \"features\": [ { \"type\": \"Feature\", \"properties\": {}, \"geometry\": { \"type\": \"Polygon\", \"coordinates\": [ [ [ -100,37 ], [ -100,38 ], [ -98,38 ], [ -98,37 ], [ -100,37 ] ] ] } } ] }","noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"4f4e4b23e4b07f02db6ae301","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":534559,"contributorType":{"id":1,"text":"Authors"},"rank":1}]}} ,{"id":10546,"text":"ofr791137 - 1979 - Preliminary study of the geotechnical properties of the Fort Union Formation from the White Tail Butte drill holes 76-103 and 76-108 near Recluse, Wyoming","interactions":[],"lastModifiedDate":"2012-02-02T00:06:20","indexId":"ofr791137","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":"79-1137","title":"Preliminary study of the geotechnical properties of the Fort Union Formation from the White Tail Butte drill holes 76-103 and 76-108 near Recluse, Wyoming","language":"ENGLISH","publisher":"U.S. Geological Survey,","doi":"10.3133/ofr791137","usgsCitation":"Odum, J.K., and Sebesta, J.J., 1979, Preliminary study of the geotechnical properties of the Fort Union Formation from the White Tail Butte drill holes 76-103 and 76-108 near Recluse, Wyoming: U.S. Geological Survey Open-File Report 79-1137, 12 p., 16 over-size sheets :fold. ill., map ;28 cm., https://doi.org/10.3133/ofr791137.","productDescription":"12 p., 16 over-size sheets :fold. ill., map ;28 cm.","costCenters":[],"links":[{"id":142473,"rank":0,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/of/1979/1137/report-thumb.jpg"},{"id":38389,"rank":300,"type":{"id":11,"text":"Document"},"url":"https://pubs.usgs.gov/of/1979/1137/report.pdf","linkFileType":{"id":1,"text":"pdf"}}],"noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"4f4e4aace4b07f02db66a44c","contributors":{"authors":[{"text":"Odum, Jack K. 0000-0002-3162-0355","orcid":"https://orcid.org/0000-0002-3162-0355","contributorId":97900,"corporation":false,"usgs":true,"family":"Odum","given":"Jack","email":"","middleInitial":"K.","affiliations":[],"preferred":false,"id":161576,"contributorType":{"id":1,"text":"Authors"},"rank":1},{"text":"Sebesta, James J.","contributorId":52181,"corporation":false,"usgs":true,"family":"Sebesta","given":"James","email":"","middleInitial":"J.","affiliations":[],"preferred":false,"id":161575,"contributorType":{"id":1,"text":"Authors"},"rank":2}]}} ,{"id":10548,"text":"ofr791184 - 1979 - Bibliography of selected reports related to studies on earthquake tectonics and risk, 1975-1978","interactions":[],"lastModifiedDate":"2023-11-24T18:07:43.052433","indexId":"ofr791184","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":"79-1184","title":"Bibliography of selected reports related to studies on earthquake tectonics and risk, 1975-1978","docAbstract":"The reports and abstracts included in this bibliography have been selected arbitrarily on the basis of their relation to U.S. Geological Survey studies on earthquake tectonics and risk. U.S. Geological Survey scientists involved in other aspects of earthquake studies have also written many dozens of reports during the same time frame, but such reports are precluded from this collection.
The bibliography contains a subject index, constructed generally from key words found in the titles, and a junior-author index.
Code numbers printed at the left of each reference entry have no significance other than that of making it easy to follow the notations in the subject and junior-author indexes. The reader may notice that some of these code numbers are missing from the ordinary running list; others have been supplemented by A's or B's. This has happened because either references assigned to numbers have been dropped or references originally omitted by mistake have been added.
The references have been typed in accepted U.S. Geological Survey format, which of late means that abbreviations are not used, except for minor notations such as \"v.\" for volume or \"p.\" for page.
","language":"English","publisher":"U.S. Geological Survey","doi":"10.3133/ofr791184","usgsCitation":"Ohl, J.P., 1979, Bibliography of selected reports related to studies on earthquake tectonics and risk, 1975-1978: U.S. Geological Survey Open-File Report 79-1184, 34 p., https://doi.org/10.3133/ofr791184.","productDescription":"34 p.","costCenters":[],"links":[{"id":142475,"rank":1,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/of/1979/1184/report-thumb.jpg"},{"id":422893,"rank":2,"type":{"id":11,"text":"Document"},"url":"https://pubs.usgs.gov/of/1979/1184/report.pdf","linkFileType":{"id":1,"text":"pdf"}}],"noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"4f4e4a4ee4b07f02db627da9","contributors":{"authors":[{"text":"Ohl, Jane P.","contributorId":104062,"corporation":false,"usgs":true,"family":"Ohl","given":"Jane","email":"","middleInitial":"P.","affiliations":[{"id":595,"text":"U.S. Geological Survey","active":false,"usgs":true}],"preferred":false,"id":161578,"contributorType":{"id":1,"text":"Authors"},"rank":1}]}} ,{"id":28294,"text":"wri794 - 1979 - Analytical method for dissolved-organic carbon fractionation","interactions":[],"lastModifiedDate":"2017-12-06T13:58:46","indexId":"wri794","displayToPublicDate":"1994-01-01T00:00:00","publicationYear":"1979","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":"79-4","title":"Analytical method for dissolved-organic carbon fractionation","docAbstract":"A standard procedure for analytical-scale dissolved organic carbon fractionation is presented, whereby dissolved organic carbon in water is first fractionated by a nonionic macroreticular resin into acid, base, and neutral hydrophobic organic solute fractions, and next fractionated by ion-exchange resins into acid, base, and neutral hydrophilic solute fractions. The hydrophobic solutes are defined as those sorbed on a nonionic, acrylic-ester macroreticular resin and are differentiated into acid, base, and nautral fractions by sorption/desorption controlled by pH adjustment. The hydrophilic bases are next sorbed on strong-acid ion-exchange resin, followed by sorption of hydrophilic acids on a strong-base ion-exchange resin. Hydrophilic neutrals are not sorbed and remain dissolved in the deionized water at the end of the fractionation procedure. The complete fractionation can be performed on a 200-milliliter filtered water sample, whose dissolved organic carbon content is 5-25 mg/L and whose specific conductance is less than 2,000 μmhos/cm at 25°C. The applications of dissolved organic carbon fractionation analysis range from field studies of changes of organic solute composition with synthetic fossil fuel production, to fundamental studies of the nature of sorption processes.
","language":"English","publisher":"U.S. Geological Survey","doi":"10.3133/wri794","usgsCitation":"Leenheer, J.A., and Huffman, E.W., 1979, Analytical method for dissolved-organic carbon fractionation: U.S. Geological Survey Water-Resources Investigations Report 79-4, iii, 16 p., https://doi.org/10.3133/wri794.","productDescription":"iii, 16 p.","numberOfPages":"23","costCenters":[],"links":[{"id":159366,"rank":0,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/wri/1979/0004/report-thumb.jpg"},{"id":349809,"rank":2,"type":{"id":11,"text":"Document"},"url":"https://pubs.usgs.gov/wri/1979/0004/report.pdf","linkFileType":{"id":1,"text":"pdf"}}],"noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"4f4e4acee4b07f02db67fa01","contributors":{"authors":[{"text":"Leenheer, Jerry A.","contributorId":72420,"corporation":false,"usgs":true,"family":"Leenheer","given":"Jerry","email":"","middleInitial":"A.","affiliations":[],"preferred":false,"id":199541,"contributorType":{"id":1,"text":"Authors"},"rank":1},{"text":"Huffman, Edward W. D. Jr.","contributorId":79519,"corporation":false,"usgs":true,"family":"Huffman","given":"Edward","suffix":"Jr.","email":"","middleInitial":"W. D.","affiliations":[],"preferred":false,"id":199542,"contributorType":{"id":1,"text":"Authors"},"rank":2}]}} ,{"id":10276,"text":"ofr79675 - 1979 - Uranium results for 147 water samples from the Elkhorn Wilderness Study Area, Montana","interactions":[],"lastModifiedDate":"2022-07-08T19:05:06.292418","indexId":"ofr79675","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":"79-675","title":"Uranium results for 147 water samples from the Elkhorn Wilderness Study Area, Montana","docAbstract":"One hundred forty seven water samples were corrected from the Elkhorn Wilderness during the summer of 1977 as a part of a mineral resource assessment study. Each sample was analyzed for uranium. Specific conductance and pH were also measured. Sample analyses and site locations are presented in this report.
","language":"English","publisher":"U.S. Geological Survey","doi":"10.3133/ofr79675","usgsCitation":"McHugh, J., and Miller, W.R., 1979, Uranium results for 147 water samples from the Elkhorn Wilderness Study Area, Montana: U.S. Geological Survey Open-File Report 79-675, 11 p., https://doi.org/10.3133/ofr79675.","productDescription":"11 p.","costCenters":[],"links":[{"id":403292,"rank":2,"type":{"id":11,"text":"Document"},"url":"https://pubs.usgs.gov/of/1979/0675/report.pdf","linkFileType":{"id":1,"text":"pdf"}},{"id":142611,"rank":0,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/of/1979/0675/report-thumb.jpg"}],"country":"United States","state":"Montana","otherGeospatial":"Elkhorn Wilderness Study Area","geographicExtents":"{\n \"type\": \"FeatureCollection\",\n \"features\": [\n {\n \"type\": \"Feature\",\n \"properties\": {},\n \"geometry\": {\n \"type\": \"Polygon\",\n \"coordinates\": [\n [\n [\n -112.1,\n 46.2\n ],\n [\n -111.6,\n 46.2\n ],\n [\n -111.6,\n 46.56\n ],\n [\n -112.1,\n 46.56\n ],\n [\n -112.1,\n 46.2\n ]\n ]\n ]\n }\n }\n ]\n}","noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"4f4e4a18e4b07f02db6053a0","contributors":{"authors":[{"text":"McHugh, John B.","contributorId":64651,"corporation":false,"usgs":true,"family":"McHugh","given":"John B.","affiliations":[],"preferred":false,"id":161123,"contributorType":{"id":1,"text":"Authors"},"rank":1},{"text":"Miller, William R.","contributorId":53838,"corporation":false,"usgs":true,"family":"Miller","given":"William","email":"","middleInitial":"R.","affiliations":[],"preferred":false,"id":161122,"contributorType":{"id":1,"text":"Authors"},"rank":2}]}} ,{"id":10289,"text":"ofr791605 - 1979 - Observations on the geology and petroleum potential of the Cold Bay-False Pass area, Alaska Peninsula","interactions":[],"lastModifiedDate":"2012-02-02T00:06:22","indexId":"ofr791605","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":"79-1605","title":"Observations on the geology and petroleum potential of the Cold Bay-False Pass area, Alaska Peninsula","docAbstract":"Upper Jurassic strata in the Black Hills area consist mainly of fossiliferous, tightly cemented, gently folded sandstone deposited in a shallow marine environment. Upper Cretaceous strata on Sanak Island are strongly deformed and show structural features of broken formations similar to those observed in the Franciscan assemblage of California. Rocks exposed on Sanak Island do not crop out on the peninsular mainland or on Unimak Island, and probably make up the acoustic and economic basement of nearby Sanak basin. Tertiary sedimentary rocks on the outermost part of the Alaska Peninsula consist of Oligocene, Miocene, and lower Pliocene volcaniclastic sandstone, siltstone, and conglomerate deposited in nonmarine and very shallow marine environments. Interbedded airfall and ash-flow tuff deposits indicate active volcanism during Oligocene time. Locally, Oligocene strata are intruded by quartz diorite plutons of probable Miocene age. \r\n\r\nReservoir properties of Mesozoic and Tertiary rocks are generally poor due to alteration of chemically unstable volcanic rock fragments. Igneous intrusions have further reduced porosity and permeability by silicification of sandstone. Organic-rich source rocks for petroleum generation are not abundant in Neogene strata. Upper Jurassic rocks in the Black Hills area have total organic carbon contents of less than 0.5 percent. \r\n\r\nDeep sediment-filled basins on the Shumagin Shelf probably contain more source rocks than onshore correlatives, but reservoir quality is not likely to be better than in onshore outcrops. The absence of well-developed folds in most Tertiary rocks, both onshore and in nearby offshore basins, reduces the possibility of hydrocarbon entrapment in anticlines.","language":"ENGLISH","publisher":"U.S. Geological Survey,","doi":"10.3133/ofr791605","usgsCitation":"McLean, H.J., 1979, Observations on the geology and petroleum potential of the Cold Bay-False Pass area, Alaska Peninsula: U.S. Geological Survey Open-File Report 79-1605, 35 p. :ill., maps ;28 cm., https://doi.org/10.3133/ofr791605.","productDescription":"35 p. :ill., maps ;28 cm.","costCenters":[],"links":[{"id":143427,"rank":0,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/of/1979/1605/report-thumb.jpg"},{"id":38142,"rank":300,"type":{"id":11,"text":"Document"},"url":"https://pubs.usgs.gov/of/1979/1605/report.pdf","linkFileType":{"id":1,"text":"pdf"}}],"noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"4f4e4afbe4b07f02db696427","contributors":{"authors":[{"text":"McLean, Hugh James","contributorId":99559,"corporation":false,"usgs":true,"family":"McLean","given":"Hugh","email":"","middleInitial":"James","affiliations":[],"preferred":false,"id":161144,"contributorType":{"id":1,"text":"Authors"},"rank":1}]}} ,{"id":57643,"text":"wdrID771 - 1979 - Water Resources Data for Idaho, Water Year 1977","interactions":[],"lastModifiedDate":"2012-02-02T00:12:00","indexId":"wdrID771","displayToPublicDate":"1994-01-01T00:00:00","publicationYear":"1979","noYear":false,"publicationType":{"id":18,"text":"Report"},"publicationSubtype":{"id":5,"text":"USGS Numbered Series"},"seriesTitle":{"id":340,"text":"Water Data Report","code":"WDR","active":false,"publicationSubtype":{"id":5}},"seriesNumber":"ID-77-1","title":"Water Resources Data for Idaho, Water Year 1977","language":"ENGLISH","doi":"10.3133/wdrID771","usgsCitation":"Water Resources Division, U.S. Geological Survey, 1979, Water Resources Data for Idaho, Water Year 1977: U.S. Geological Survey Water Data Report ID-77-1, 640 p., 21 fig., https://doi.org/10.3133/wdrID771.","productDescription":"640 p., 21 fig.","costCenters":[],"links":[{"id":181637,"rank":0,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/thumbnails/usgs_thumb.jpg"}],"scale":"48","noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"4f4e4a0de4b07f02db5fcf3e","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":533173,"contributorType":{"id":1,"text":"Authors"},"rank":1}]}} ,{"id":17281,"text":"ofr791567 - 1979 - Inventory of drilling activities of the U.S. Geological Survey in the United States, fiscal years 1979-1980","interactions":[],"lastModifiedDate":"2024-02-26T18:06:45.553961","indexId":"ofr791567","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":"79-1567","title":"Inventory of drilling activities of the U.S. Geological Survey in the United States, fiscal years 1979-1980","docAbstract":"No abstract available.
","language":"English","publisher":"U.S. Geological Survey","doi":"10.3133/ofr791567","usgsCitation":"1979, Inventory of drilling activities of the U.S. Geological Survey in the United States, fiscal years 1979-1980: U.S. Geological Survey Open-File Report 79-1567, 47 p., https://doi.org/10.3133/ofr791567.","productDescription":"47 p.","costCenters":[],"links":[{"id":425992,"rank":2,"type":{"id":11,"text":"Document"},"url":"https://pubs.usgs.gov/of/1979/1567/report.pdf","linkFileType":{"id":1,"text":"pdf"}},{"id":150178,"rank":1,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/of/1979/1567/report-thumb.jpg"}],"country":"United States","geographicExtents":"{\n \"type\": \"FeatureCollection\",\n \"features\": [\n {\n \"type\": \"Feature\",\n \"properties\": {},\n \"geometry\": {\n \"type\": \"Polygon\",\n \"coordinates\": [\n [\n [\n -130.67138671875,\n 54.686534234529695\n ],\n [\n -129.9462890625,\n 55.36662484928637\n ],\n [\n -130.1220703125,\n 56.145549500679074\n 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}\n }\n ]\n}","noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"4f4e4939e4b07f02db5876e3","contributors":{"compilers":[{"text":"Muffler, L.J. Patrick 0000-0001-6638-7218 pmuffler@usgs.gov","orcid":"https://orcid.org/0000-0001-6638-7218","contributorId":3322,"corporation":false,"usgs":true,"family":"Muffler","given":"L.J.","email":"pmuffler@usgs.gov","middleInitial":"Patrick","affiliations":[{"id":617,"text":"Volcano Science Center","active":true,"usgs":true}],"preferred":true,"id":895410,"contributorType":{"id":3,"text":"Compilers"},"rank":1},{"text":"Hofeling, Carol Lynn","contributorId":52200,"corporation":false,"usgs":true,"family":"Hofeling","given":"Carol","email":"","middleInitial":"Lynn","affiliations":[],"preferred":false,"id":895411,"contributorType":{"id":3,"text":"Compilers"},"rank":2}]}} ,{"id":20915,"text":"ofr79428 - 1979 - Geologic description of selected strong-motion accelerograph sites, Part II","interactions":[],"lastModifiedDate":"2022-10-17T20:36:34.2281","indexId":"ofr79428","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":"79-428","title":"Geologic description of selected strong-motion accelerograph sites, Part II","docAbstract":"One of the major tasks of the U.S. Geological Survey as regards seismic engineering is the collection and dissemination of strong-motion accelerograph records. When analyzing these records certain information describing the instrument site is important: local geology; instrument housing (buildings, dams, bridges, instrument shelters, etc.); local topography; and proximity of an accelerograph to man-made structures that might influence the record. This report describes local geologic conditions of selected sites and is the second in a series of continuing reports covering strong-motion accelerograph sites in the western hemisphere. See Open File Report 78-1005 for part one.
","language":"English","publisher":"U.S. Geological Survey","doi":"10.3133/ofr79428","usgsCitation":"Silverstein, B., 1979, Geologic description of selected strong-motion accelerograph sites, Part II: U.S. Geological Survey Open-File Report 79-428, 34 p., https://doi.org/10.3133/ofr79428.","productDescription":"34 p.","costCenters":[],"links":[{"id":408429,"rank":2,"type":{"id":11,"text":"Document"},"url":"https://pubs.usgs.gov/of/1979/0428/report.pdf","linkFileType":{"id":1,"text":"pdf"}},{"id":153912,"rank":0,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/of/1979/0428/report-thumb.jpg"}],"noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"4f4e4b17e4b07f02db6a631e","contributors":{"authors":[{"text":"Silverstein, B.L.","contributorId":92256,"corporation":false,"usgs":true,"family":"Silverstein","given":"B.L.","email":"","affiliations":[],"preferred":false,"id":183493,"contributorType":{"id":1,"text":"Authors"},"rank":1}]}} ,{"id":10320,"text":"ofr79677 - 1979 - A digital model for simulation of ground-water hydrology in the Houston area, Texas","interactions":[{"subject":{"id":10320,"text":"ofr79677 - 1979 - A digital model for simulation of ground-water hydrology in the Houston area, Texas","indexId":"ofr79677","publicationYear":"1979","noYear":false,"title":"A digital model for simulation of ground-water hydrology in the Houston area, Texas"},"predicate":"SUPERSEDED_BY","object":{"id":70043066,"text":"70043066 - 1979 - A digital model for simulation of ground-water hydrology in the Houston area, Texas","indexId":"70043066","publicationYear":"1979","noYear":false,"title":"A digital model for simulation of ground-water hydrology in the Houston area, Texas"},"id":1}],"supersededBy":{"id":70043066,"text":"70043066 - 1979 - A digital model for simulation of ground-water hydrology in the Houston area, Texas","indexId":"70043066","publicationYear":"1979","noYear":false,"title":"A digital model for simulation of ground-water hydrology in the Houston area, Texas"},"lastModifiedDate":"2017-06-14T12:08:30","indexId":"ofr79677","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":"79-677","title":"A digital model for simulation of ground-water hydrology in the Houston area, Texas","docAbstract":"No abstract available.
","language":"English","publisher":"U.S. Geological Survey","doi":"10.3133/ofr79677","usgsCitation":"Meyer, W.R., and Carr, J.E., 1979, A digital model for simulation of ground-water hydrology in the Houston area, Texas: U.S. Geological Survey Open-File Report 79-677, 143 p., https://doi.org/10.3133/ofr79677.","productDescription":"143 p.","onlineOnly":"N","additionalOnlineFiles":"N","costCenters":[{"id":583,"text":"Texas Water Science Center","active":true,"usgs":true}],"links":[{"id":143632,"rank":0,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/thumbnails/usgs_thumb.jpg"}],"country":"United States","state":"Texas","city":"Houston","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 30.95876857077987\n ],\n [\n -97.7783203125,\n 30.798474179567823\n ],\n [\n -97.349853515625,\n 28.603814407841327\n ],\n [\n -96.94335937499999,\n 27.89734922968426\n ],\n [\n -96.844482421875,\n 27.994401411046148\n ],\n [\n -96.52587890625,\n 28.17855984939698\n ],\n [\n -95.657958984375,\n 28.65203063036226\n ],\n [\n -94.28466796874999,\n 29.53522956294847\n ],\n [\n -94.361572265625,\n 30.95876857077987\n ]\n ]\n ]\n }\n }\n ]\n}","noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"4f4e4b25e4b07f02db6aedc5","contributors":{"authors":[{"text":"Meyer, Walter Richard","contributorId":30209,"corporation":false,"usgs":true,"family":"Meyer","given":"Walter","email":"","middleInitial":"Richard","affiliations":[],"preferred":false,"id":161192,"contributorType":{"id":1,"text":"Authors"},"rank":1},{"text":"Carr, Jerry E.","contributorId":47758,"corporation":false,"usgs":true,"family":"Carr","given":"Jerry","email":"","middleInitial":"E.","affiliations":[],"preferred":false,"id":161193,"contributorType":{"id":1,"text":"Authors"},"rank":2}]}} ,{"id":10327,"text":"ofr791524 - 1979 - Stress-relief borehole measurements before and after quarrying a block of Barre Granite at Barre, Vermont","interactions":[],"lastModifiedDate":"2024-02-26T18:17:03.221331","indexId":"ofr791524","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":"79-1524","title":"Stress-relief borehole measurements before and after quarrying a block of Barre Granite at Barre, Vermont","docAbstract":"In situ stresses were measured in a 10X10X5.7-m block of Barre Granite of Devonian age at the Wetmore and Morse granite quarry at Barre, Vt., before and after it was quarried. The stresses were measured with the U.S. Bureau of Mines borehole deformation gage in both the horizontal and vertical planes. Anomalously high stresses in both planes were observed in the block before quarrying. Relatively small stresses remained in the block after quarrying. Stresses measured in the floor beneath the block and from a horizontal boring in the 67-m vertical backwall behind the block, however, showed that the quarrying caused little change other than to the block.
Additional measurements were also taken in granite in the Barre, Vt., area near the Wetmore and Morse and Adam quarries and in schist near the Pirie quarry.
","language":"English","publisher":"U.S. Geological Survey","doi":"10.3133/ofr791524","usgsCitation":"Miller, D.R., and Brethauer, G., 1979, Stress-relief borehole measurements before and after quarrying a block of Barre Granite at Barre, Vermont: U.S. Geological Survey Open-File Report 79-1524, iii, 39 p., https://doi.org/10.3133/ofr791524.","productDescription":"iii, 39 p.","costCenters":[],"links":[{"id":426010,"rank":2,"type":{"id":11,"text":"Document"},"url":"https://pubs.usgs.gov/of/1979/1524/report.pdf","linkFileType":{"id":1,"text":"pdf"}},{"id":143476,"rank":1,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/of/1979/1524/report-thumb.jpg"}],"country":"United States","state":"Vermont","city":"Barre","geographicExtents":"{\n \"type\": \"FeatureCollection\",\n \"features\": [\n {\n \"type\": \"Feature\",\n \"properties\": {},\n \"geometry\": {\n \"coordinates\": [\n [\n [\n -72.51031800958445,\n 44.20106872307667\n ],\n [\n -72.51031800958445,\n 44.18825020749779\n ],\n [\n -72.48435054746014,\n 44.18825020749779\n ],\n [\n -72.48435054746014,\n 44.20106872307667\n ],\n [\n -72.51031800958445,\n 44.20106872307667\n ]\n ]\n ],\n \"type\": \"Polygon\"\n }\n }\n ]\n}","noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"4f4e4b15e4b07f02db6a4c53","contributors":{"authors":[{"text":"Miller, Danny R.","contributorId":75536,"corporation":false,"usgs":true,"family":"Miller","given":"Danny","email":"","middleInitial":"R.","affiliations":[],"preferred":false,"id":161202,"contributorType":{"id":1,"text":"Authors"},"rank":1},{"text":"Brethauer, G.E.","contributorId":69548,"corporation":false,"usgs":true,"family":"Brethauer","given":"G.E.","email":"","affiliations":[],"preferred":false,"id":161201,"contributorType":{"id":1,"text":"Authors"},"rank":2}]}} ,{"id":10702,"text":"ofr79295 - 1979 - Petroleum source potential of rocks dredged from the continental slope in the eastern Gulf of Alaska","interactions":[],"lastModifiedDate":"2012-02-02T00:06:25","indexId":"ofr79295","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":"79-295","title":"Petroleum source potential of rocks dredged from the continental slope in the eastern Gulf of Alaska","docAbstract":"A bedrock dredging program by the R/V Sea Sounder in 1977 and 1978 along the continental slope in the eastern Gulf of Alaska revealed a previously unknown Eocene sedimentary sequence that includes argillaceous rocks with favorable petroleum source rock characteristics. Seven of 36 dredge hauls that sampled outcrop contain argillaceous rocks with more than l percent and as much as 1.64 percent organic carbon. Some of the rocks in samples of probable early Eocene age have undergone a thermal history that has resulted in generation of hydrocarbons. The organic matter appears to be hydrogen deficient, however, which could indicate that the rocks are more likely to be a source of gas rather than liquid hydrocarbon, unless the hydrogen loss is due to weathering. \r\n\r\nThe Eocene rocks are associated with sandstone and conglomerate on the continental slope. They dip northward beneath younger Tertiary strata in the outer continental shelf where they could be an important petroleum source and exploratory target.","language":"ENGLISH","publisher":"U.S. Geological Survey,","doi":"10.3133/ofr79295","usgsCitation":"Plafker, G., and Claypool, G.E., 1979, Petroleum source potential of rocks dredged from the continental slope in the eastern Gulf of Alaska: U.S. Geological Survey Open-File Report 79-295, 20 p. :ill., map ;28 cm., https://doi.org/10.3133/ofr79295.","productDescription":"20 p. :ill., map ;28 cm.","costCenters":[],"links":[{"id":143258,"rank":0,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/of/1979/0295/report-thumb.jpg"},{"id":38521,"rank":300,"type":{"id":11,"text":"Document"},"url":"https://pubs.usgs.gov/of/1979/0295/report.pdf","linkFileType":{"id":1,"text":"pdf"}}],"noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"4f4e4adee4b07f02db68736a","contributors":{"authors":[{"text":"Plafker, George","contributorId":3920,"corporation":false,"usgs":false,"family":"Plafker","given":"George","email":"","affiliations":[],"preferred":false,"id":161823,"contributorType":{"id":1,"text":"Authors"},"rank":1},{"text":"Claypool, George Edwin","contributorId":99972,"corporation":false,"usgs":true,"family":"Claypool","given":"George","email":"","middleInitial":"Edwin","affiliations":[],"preferred":false,"id":161824,"contributorType":{"id":1,"text":"Authors"},"rank":2}]}} ,{"id":10510,"text":"ofr791565 - 1979 - Annotated geologic bibliography for the Richfield 1° x 2° Quadrangle, Utah","interactions":[],"lastModifiedDate":"2024-02-26T18:15:49.299728","indexId":"ofr791565","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":"79-1565","title":"Annotated geologic bibliography for the Richfield 1° x 2° Quadrangle, Utah","docAbstract":"No abstract available.
","language":"English","publisher":"U.S. Geological Survey","doi":"10.3133/ofr791565","usgsCitation":"Nelson, M., and Bromfield, C.S., 1979, Annotated geologic bibliography for the Richfield 1° x 2° Quadrangle, Utah: U.S. Geological Survey Open-File Report 79-1565, 66 p., https://doi.org/10.3133/ofr791565.","productDescription":"66 p.","costCenters":[],"links":[{"id":145542,"rank":1,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/of/1979/1565/report-thumb.jpg"},{"id":426008,"rank":2,"type":{"id":11,"text":"Document"},"url":"https://pubs.usgs.gov/of/1979/1565/report.pdf","linkFileType":{"id":1,"text":"pdf"}}],"country":"United States","state":"Utah","otherGeospatial":"Richfield Quadrangle","geographicExtents":"{ \"type\": \"FeatureCollection\", \"features\": [ { \"type\": \"Feature\", \"properties\": {}, \"geometry\": { \"type\": \"Polygon\", \"coordinates\": [ [ [ -114,38 ], [ -114,39 ], [ -112,39 ], [ -112,38 ], [ -114,38 ] ] ] } } ] }","noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"4f4e4ac8e4b07f02db67bd1d","contributors":{"authors":[{"text":"Nelson, M.G.","contributorId":86346,"corporation":false,"usgs":true,"family":"Nelson","given":"M.G.","email":"","affiliations":[],"preferred":false,"id":161520,"contributorType":{"id":1,"text":"Authors"},"rank":1},{"text":"Bromfield, Calvin Stanton","contributorId":12048,"corporation":false,"usgs":true,"family":"Bromfield","given":"Calvin","email":"","middleInitial":"Stanton","affiliations":[],"preferred":false,"id":161519,"contributorType":{"id":1,"text":"Authors"},"rank":2}]}} ,{"id":10395,"text":"ofr791661 - 1979 - Primary and secondary faulting in the Najd fault system, Kingdom of Saudi Arabia","interactions":[],"lastModifiedDate":"2012-02-02T00:06:31","indexId":"ofr791661","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":"79-1661","title":"Primary and secondary faulting in the Najd fault system, Kingdom of Saudi Arabia","docAbstract":"The Najd fault system is a major transcurrent (strike-slip) fault system of Proterozoic age in the Arabian Shield. The system is a braided complex of parallel and curved en echelon faults. Complex arrays of secondary structures including strike-slip, oblique-slip, thrust, and normal faults, together with folds and dike swarms, are associated with some major faults, particularly near their terminations. The secondary structures indicate that compressional and extensional and dilational conditions existed synchronously in different parts of the fault zone. The outcrop traces of faults and syntectonic dikes have been used to interpret the configuration of principal compressive stresses during formation of parts of the secondary fracture systems. Second-order deformation was a series of separate events in a complex episodic faulting history. Comparison with model studies indicates that master faults extended in length in stages and periodically developed arrays of secondary structures. Propagation of the major faults took place along splay trajectories, which inter-connected to form a subparallel sheeted and braided zone. Interpretation of the aeromagnetic maps indicates that the Najd system is broader at depth than the outcropping fault complex, and that more continuous structures underlie arrays of faults at surface. The fault pattern is mechanically explicable in terms of simple shear between rigid blocks beneath the exposed structures.","language":"ENGLISH","publisher":"U.S. Geological Survey,","doi":"10.3133/ofr791661","usgsCitation":"Moore, J.M., 1979, Primary and secondary faulting in the Najd fault system, Kingdom of Saudi Arabia: U.S. Geological Survey Open-File Report 79-1661, i, 26 p. ;28 cm., https://doi.org/10.3133/ofr791661.","productDescription":"i, 26 p. ;28 cm.","costCenters":[],"links":[{"id":143927,"rank":0,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/of/1979/1661/report-thumb.jpg"},{"id":38227,"rank":300,"type":{"id":11,"text":"Document"},"url":"https://pubs.usgs.gov/of/1979/1661/report.pdf","linkFileType":{"id":1,"text":"pdf"}}],"noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"4f4e4aaae4b07f02db668d34","contributors":{"authors":[{"text":"Moore, John McMahon","contributorId":10429,"corporation":false,"usgs":true,"family":"Moore","given":"John","email":"","middleInitial":"McMahon","affiliations":[],"preferred":false,"id":161315,"contributorType":{"id":1,"text":"Authors"},"rank":1}]}} ,{"id":20939,"text":"ofr79271 - 1979 - Hydrologic data for urban studies in the Austin, Texas, metropolitan area, 1977","interactions":[],"lastModifiedDate":"2026-01-08T19:32:40.184218","indexId":"ofr79271","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":"79-271","title":"Hydrologic data for urban studies in the Austin, Texas, metropolitan area, 1977","docAbstract":"No abstract available.
","language":"English","publisher":"U.S. Geological Survey","doi":"10.3133/ofr79271","collaboration":"Prepared in cooperation with the City of Austin and the Texas Department of Water Resources","usgsCitation":"Slade, R., Gordon, J., and Mitchell, R., 1979, Hydrologic data for urban studies in the Austin, Texas, metropolitan area, 1977: U.S. Geological Survey Open-File Report 79-271, 192 p., https://doi.org/10.3133/ofr79271.","productDescription":"192 p.","onlineOnly":"N","additionalOnlineFiles":"N","costCenters":[{"id":583,"text":"Texas Water Science Center","active":true,"usgs":true}],"links":[{"id":153957,"rank":1,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/of/1979/0271/report-thumb.jpg"},{"id":498437,"rank":2,"type":{"id":11,"text":"Document"},"url":"https://pubs.usgs.gov/of/1979/0271/report.pdf","linkFileType":{"id":1,"text":"pdf"}}],"country":"United States","state":"Texas","city":"Austin","geographicExtents":"{\n \"type\": \"FeatureCollection\",\n \"features\": [\n {\n \"type\": \"Feature\",\n \"properties\": {},\n \"geometry\": {\n \"type\": \"Polygon\",\n \"coordinates\": [\n [\n [\n -98.09280395507812,\n 29.991812888666043\n ],\n [\n -97.38006591796874,\n 29.991812888666043\n ],\n [\n -97.38006591796874,\n 30.615459280672667\n ],\n [\n -98.09280395507812,\n 30.615459280672667\n ],\n [\n -98.09280395507812,\n 29.991812888666043\n ]\n ]\n ]\n }\n }\n ]\n}","noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"4f4e4ad4e4b07f02db683267","contributors":{"authors":[{"text":"Slade, R.M.","contributorId":84364,"corporation":false,"usgs":true,"family":"Slade","given":"R.M.","affiliations":[],"preferred":false,"id":183543,"contributorType":{"id":1,"text":"Authors"},"rank":1},{"text":"Gordon, J.D.","contributorId":26684,"corporation":false,"usgs":true,"family":"Gordon","given":"J.D.","email":"","affiliations":[],"preferred":false,"id":183542,"contributorType":{"id":1,"text":"Authors"},"rank":2},{"text":"Mitchell, R.N.","contributorId":94301,"corporation":false,"usgs":true,"family":"Mitchell","given":"R.N.","email":"","affiliations":[],"preferred":false,"id":183544,"contributorType":{"id":1,"text":"Authors"},"rank":3}]}} ,{"id":10628,"text":"ofr79448 - 1979 - The subsurface geology of the Florida-Hatteras shelf, slope, and inner Blake Plateau","interactions":[],"lastModifiedDate":"2022-09-02T20:24:12.862875","indexId":"ofr79448","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":"79-448","title":"The subsurface geology of the Florida-Hatteras shelf, slope, and inner Blake Plateau","docAbstract":"The structure and stratigraphy of the Florida-Hatteras Slope and inner Blake Plateau was studied by means of 4,780 km of single-channel air gun seismic reflection profiles. Control for the seismic stratigraphy is provided by correlating reflecting units and paleontologically dated stratigraphic units identified in offshore wells and dredge hauls. Many Tertiary unconformities exist, and major regional unconformities at the end of the Oligocene and in the late Paleocene are mapped. Reflecting surfaces believed to represent the tops of the Cretaceous, Paleocene, and Oligocene extend throughout the region. Upper Cretaceous (pre-Maastrichtian) rocks on the southeastern side of the Carolina Platform form a large seaward-facing progradational wedge. The Upper Cretaceous rocks in the Southeast Georgia Embayment, are seismically transparent and on the inner Blake Plateau are cut by numerous small faults, perhaps due to compaction. \r\n\r\nWithin the survey area relatively flat-lying Maastrichtian and Paleocene strata show no evidence that a feature similar to the present Florida-Hatteras Slope existed at the beginning of the Tertiary. Late Paleocene erosion, related to the initiation of the Gulf Stream flow, probably developed this regional unconformity. Eocene and Oligocene sediments landward of the present Gulf Stream form a thick sequence of seaward-dipping progradational beds. A seaward progradational wedge of Miocene to Holocene age covers a regionally traceable unconformity, which separates the Oligocene from the Miocene sediments. Under and seaward of the present Gulf Stream, the Eocene and younger sediment supply was much smaller and the buildup is comparatively insignificant. The difference in accumulation rates in the Eocene and younger sediments, landward and seaward of the Gulf Stream, is responsible for the Florida-Hatteras Slope. Tertiary isopach maps suggest that there is a well developed triangular depocenter under the shelf. The edges of the depocenter correspond with magnetic anomalies and it is suggested that the depocenter is related to differential subsidence during the Tertiary across older crustal structures. The Eocene and Oligocene units contain the aquifer onshore, and the aquifer probably remains in these units offshore. With this assumption the potential aquifer has been identified and traced under the shelf and slope.","language":"English","publisher":"U.S. Geological Survey","doi":"10.3133/ofr79448","usgsCitation":"Paull, C.K., and Dillon, W.P., 1979, The subsurface geology of the Florida-Hatteras shelf, slope, and inner Blake Plateau: U.S. Geological Survey Open-File Report 79-448, 94 p., https://doi.org/10.3133/ofr79448.","productDescription":"94 p.","costCenters":[],"links":[{"id":406184,"rank":3,"type":{"id":36,"text":"NGMDB Index Page"},"url":"https://ngmdb.usgs.gov/Prodesc/proddesc_29112.htm","linkFileType":{"id":5,"text":"html"}},{"id":38458,"rank":300,"type":{"id":11,"text":"Document"},"url":"https://pubs.usgs.gov/of/1979/0448/report.pdf","linkFileType":{"id":1,"text":"pdf"}},{"id":142516,"rank":0,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/of/1979/0448/report-thumb.jpg"}],"country":"United States","otherGeospatial":"Florida-Hatteras shelf, slope, and inner Blake Plateau","geographicExtents":"{\n \"type\": \"FeatureCollection\",\n \"features\": [\n {\n \"type\": \"Feature\",\n \"properties\": {},\n \"geometry\": {\n \"type\": \"Polygon\",\n \"coordinates\": [\n [\n [\n -81.6064453125,\n 28.459033019728043\n ],\n [\n -75.05859375,\n 28.459033019728043\n ],\n [\n -75.05859375,\n 34.08906131584994\n ],\n [\n -81.6064453125,\n 34.08906131584994\n ],\n [\n -81.6064453125,\n 28.459033019728043\n ]\n ]\n ]\n }\n }\n ]\n}","noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"4f4e4a5fe4b07f02db634ad0","contributors":{"authors":[{"text":"Paull, Charles K. 0000-0001-5940-3443","orcid":"https://orcid.org/0000-0001-5940-3443","contributorId":55825,"corporation":false,"usgs":false,"family":"Paull","given":"Charles","email":"","middleInitial":"K.","affiliations":[{"id":7043,"text":"University of North Carolina","active":true,"usgs":false}],"preferred":true,"id":161707,"contributorType":{"id":1,"text":"Authors"},"rank":1},{"text":"Dillon, William P. bdillon@usgs.gov","contributorId":79820,"corporation":false,"usgs":true,"family":"Dillon","given":"William","email":"bdillon@usgs.gov","middleInitial":"P.","affiliations":[{"id":678,"text":"Woods Hole Coastal and Marine Science Center","active":true,"usgs":true}],"preferred":false,"id":161706,"contributorType":{"id":1,"text":"Authors"},"rank":2}]}} ,{"id":26021,"text":"wri7992 - 1979 - Evaluation of methods for estimating ground-water withdrawals in western Kansas","interactions":[],"lastModifiedDate":"2018-11-19T12:17:44","indexId":"wri7992","displayToPublicDate":"1994-01-01T00:00:00","publicationYear":"1979","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":"79-92","title":"Evaluation of methods for estimating ground-water withdrawals in western Kansas","docAbstract":"During 1978, methods of estimating ground-water withdrawals in western Kansas were examined and evaluated, using both existing data from the files of the U.S. Geological Survey and newly collected data.
Values for annual ground-water withdrawals reported to the Division of Water Resources, Kansas State Board of Agriculture, by water users probably contain substantial errors because most individual users do not possess the means to measure or accurately estimate the discharge rates of their wells. Such reported values are estimated to average 10 to 15 percent higher than the actual discharge rate. Values obtained from discharge-totaling meters are reasonably accurate, but few wells are equipped with these meters, and the cost of equipping all wells with meters may be prohibitive. Measured rates of power consumption can give good estimates of total withdrawal from wells where the power consumption is measured. However, power-consumption values cannot be extrapolated reliably from one well to another.
Three techniques are regarded as promising for estimating areal ground-water withdrawals from readily collected data:
Efforts by the Instrument Development Laboratofy of the U.S. Geological Survey to design improved instruments for measuring ground-water withdrawals have produced two promising results:
For the remainder of this study, the three techniques for estimating areal ground-water withdrawals described above will be tested on a larger scale in Groundwater Management District No. 1, an area of about 1,800 square miles in west-central Kansas. About 150 randomly selected wells will be equipped with Running-time Sentry units and monitored for total withdrawal, instantaneous discharge, and power consumption. A few wells will be equipped with prototype discharge-totaling meters. The performance of the Sentry units and discharge-totaling meters will be evaluated. Areal estimates of withdrawal from measured withdrawal values, from average power-consumption coefficients, and from irrigation application by crop will be calculated and compared with each other and with reported values of withdrawal.
","language":"English","publisher":"U.S. Geological Survey","doi":"10.3133/wri7992","usgsCitation":"Baker, C.H., 1979, Evaluation of methods for estimating ground-water withdrawals in western Kansas: U.S. Geological Survey Water-Resources Investigations Report 79-92, iv, 70 p., https://doi.org/10.3133/wri7992.","productDescription":"iv, 70 p.","costCenters":[],"links":[{"id":359560,"rank":2,"type":{"id":11,"text":"Document"},"url":"https://pubs.usgs.gov/wri/1979/0092/report.pdf","linkFileType":{"id":1,"text":"pdf"}},{"id":157626,"rank":0,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/wri/1979/0092/report-thumb.jpg"}],"country":"United 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\"}}]}","noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"4f4e49ffe4b07f02db5f781e","contributors":{"authors":[{"text":"Baker, Claud H. Jr.","contributorId":53413,"corporation":false,"usgs":true,"family":"Baker","given":"Claud","suffix":"Jr.","email":"","middleInitial":"H.","affiliations":[],"preferred":false,"id":195656,"contributorType":{"id":1,"text":"Authors"},"rank":1}]}} ,{"id":10629,"text":"ofr791199 - 1979 - Investigation of the Hosgri fault, offshore southern California, Point Sal to Point Conception","interactions":[],"lastModifiedDate":"2022-08-30T21:11:53.140021","indexId":"ofr791199","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":"79-1199","title":"Investigation of the Hosgri fault, offshore southern California, Point Sal to Point Conception","docAbstract":"A high-resolution seismic reflection survey of the inner continental shelf between Point Sal and Point Conception has revealed faults that displace post-Wisconsin strata (less than 17,000-20,000 years). These faults are the Hosgri fault, the Offshore Lompoc fault, and smaller unnamed faults. Faults trending offshore from the adjacent shoreline such as the Pezzoni, Lions Head, Honda, and Pacifico faults, do not show post-Wisconsin activity. \r\n\r\nThe Hosgri fault trends directly toward the coastline between Purisima Point and Point Arguello where it appears to merge with folds and smaller faults in the western Transverse Ranges. This trend of offshore structures toward the Point Arguello-Point Conception area is consistent with a hypothesis that the regional structural fabric of the southern California Coast Ranges and its adjacent offshore area merge with the Transverse Ranges.","language":"English","publisher":"U.S. Geological Survey","doi":"10.3133/ofr791199","usgsCitation":"Payne, C.M., Swanson, O.E., and Schell, B.A., 1979, Investigation of the Hosgri fault, offshore southern California, Point Sal to Point Conception: U.S. Geological Survey Open-File Report 79-1199, Report: iv, 17 p.; 4 Plates: 41.96 × 58.54 inches or smaller, https://doi.org/10.3133/ofr791199.","productDescription":"Report: iv, 17 p.; 4 Plates: 41.96 × 58.54 inches or smaller","costCenters":[{"id":595,"text":"U.S. Geological Survey","active":false,"usgs":true}],"links":[{"id":405956,"rank":7,"type":{"id":36,"text":"NGMDB Index Page"},"url":"https://ngmdb.usgs.gov/Prodesc/proddesc_11077.htm","linkFileType":{"id":5,"text":"html"}},{"id":38463,"rank":300,"type":{"id":11,"text":"Document"},"url":"https://pubs.usgs.gov/of/1979/1199/report.pdf","linkFileType":{"id":1,"text":"pdf"}},{"id":38462,"rank":403,"type":{"id":17,"text":"Plate"},"url":"https://pubs.usgs.gov/of/1979/1199/plate-4.pdf","linkFileType":{"id":1,"text":"pdf"}},{"id":38461,"rank":402,"type":{"id":17,"text":"Plate"},"url":"https://pubs.usgs.gov/of/1979/1199/plate-3.pdf","linkFileType":{"id":1,"text":"pdf"}},{"id":38460,"rank":401,"type":{"id":17,"text":"Plate"},"url":"https://pubs.usgs.gov/of/1979/1199/plate-2.pdf","linkFileType":{"id":1,"text":"pdf"}},{"id":38459,"rank":400,"type":{"id":17,"text":"Plate"},"url":"https://pubs.usgs.gov/of/1979/1199/plate-1.pdf","linkFileType":{"id":1,"text":"pdf"}},{"id":142532,"rank":0,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/of/1979/1199/report-thumb.jpg"}],"country":"United States","state":"California","otherGeospatial":"Point Sal to Point Conception","geographicExtents":"{\n \"type\": \"FeatureCollection\",\n \"features\": [\n {\n \"type\": \"Feature\",\n \"properties\": {},\n \"geometry\": {\n \"type\": \"Polygon\",\n \"coordinates\": [\n [\n [\n -120.992,\n 34.348\n ],\n [\n -120.365,\n 34.348\n ],\n [\n -120.365,\n 35.077\n ],\n [\n -120.992,\n 35.077\n ],\n [\n -120.992,\n 34.348\n ]\n ]\n ]\n }\n }\n ]\n}","noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"4f4e4813e4b07f02db4da23d","contributors":{"authors":[{"text":"Payne, C. M.","contributorId":54595,"corporation":false,"usgs":true,"family":"Payne","given":"C.","email":"","middleInitial":"M.","affiliations":[],"preferred":false,"id":161708,"contributorType":{"id":1,"text":"Authors"},"rank":1},{"text":"Swanson, O. E.","contributorId":83124,"corporation":false,"usgs":true,"family":"Swanson","given":"O.","email":"","middleInitial":"E.","affiliations":[],"preferred":false,"id":161710,"contributorType":{"id":1,"text":"Authors"},"rank":2},{"text":"Schell, B. A.","contributorId":77151,"corporation":false,"usgs":true,"family":"Schell","given":"B.","email":"","middleInitial":"A.","affiliations":[],"preferred":false,"id":161709,"contributorType":{"id":1,"text":"Authors"},"rank":3}]}} ,{"id":47623,"text":"wri7953 - 1979 - Water in the Elizabethtown area: A study of a limestone terrane in north-central Kentucky","interactions":[],"lastModifiedDate":"2022-02-18T20:24:27.44008","indexId":"wri7953","displayToPublicDate":"1994-01-01T00:00:00","publicationYear":"1979","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":"79-53","title":"Water in the Elizabethtown area: A study of a limestone terrane in north-central Kentucky","docAbstract":"The Elizabethtown area of north-central Kentucky contains aquifers and streams that yield adequate quantities of water of suitable quality for most individual domestic needs as well as for industrial, public supply, and irrigation uses.
The area consists of typical karst with numerous sinkholes and subsurface drainage. The bedrock structure controls, in part, the availability of ground water. Potentiometric and structure contours suggest that wells, springs, and streams on anticlines are more likely to have smaller yields or flows and possibly be more affected by droughts, than those on synclines.
Water wells, tapping the St. Louis Limestone of Late Mississippian age, yield from less than 1 to about 540 gallons per minute. The average well is 93 feet deep and has a static water level of 40 feet. Well depths range from 43 to 335 feet. The low average discharges of springs during 7 consecutive days for a 10-year period range from 0.4 to 13.4 cubic feet per second.
Stream discharges average from less than 0.002 cubic feet per second in the headlands, to 458 cubic feet per second for Nolin River at White Mills, just beyond the area of study. Low average discharges of streams during 7 consecutive days for a 10-year interval range from zero to 34 cubic feet per second. Along many intervals of Middle Creek and North Fork Nolin River, during periods of low flow, there may be no surface flow. Such losing streams are common in karstland which lacks surface drainage.
The quality of water from wells and springs is typical of a limestone terrane. It is chiefly a calcium bicarbonate or calcium sulfate type of water. The water is moderately hard to very hard. The water quality of streams at baseflow is similar to that of the ground water. During periods of precipitation, water in streams is diluted by the overland runoff and contains fewer dissolved solids.
Water in the basal gypsum-hearing part of the St. Louis Limestone is likely to have sulfate content in excess of 250 milligrams per liter. The water from this zone may also contain excessive dissolved solids. Water from rocks that have shale beds below the St. Louis Limestone is likely to be saline.
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