Flood magnitude-frequency relation applicable to streams in the North Atlantic slope basins, New York to York River, Va., are presented in this report. The relations are based on flood data collected at 487 gaging stations having 5 or more years of record not materially affected by regulation. For sites on most streams, the magnitude of a flood of any given frequency between 1.1 and 50 years can be determined from two curves - one expressing the relation between the mean annual flood and size of draining basin and the other expressing the ratio to the mean annual flood of floods of other recurrence intervals. For New Jersey streams, an adjustment to the mean annual flood is based on the percentage of surface area covered by lakes and swamps in the basin.
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North Atlantic slope basins, New York to York River: U.S. Geological Survey Water Supply Paper 1672, Report: xvii, 585 p.; Plate: 29.23 x 37.19 inches, https://doi.org/10.3133/wsp1672.","productDescription":"Report: xvii, 585 p.; Plate: 29.23 x 37.19 inches","onlineOnly":"N","additionalOnlineFiles":"N","costCenters":[],"links":[{"id":138743,"rank":0,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/wsp/1672/report-thumb.jpg"},{"id":29382,"rank":300,"type":{"id":11,"text":"Document"},"url":"https://pubs.usgs.gov/wsp/1672/report.pdf","linkFileType":{"id":1,"text":"pdf"}},{"id":29381,"rank":400,"type":{"id":17,"text":"Plate"},"url":"https://pubs.usgs.gov/wsp/1672/plate-1.pdf","linkFileType":{"id":1,"text":"pdf"}},{"id":110006,"rank":700,"type":{"id":36,"text":"NGMDB Index Page"},"url":"https://ngmdb.usgs.gov/Prodesc/proddesc_24881.htm","linkFileType":{"id":5,"text":"html"},"description":"24881"}],"country":"United States","state":"Delaware, Maryland, New Jersey, New York, Pennsylvania, Virginia, West Virginia","geographicExtents":"{\n \"type\": \"FeatureCollection\",\n \"features\": [\n {\n \"type\": \"Feature\",\n \"properties\": {},\n \"geometry\": {\n \"type\": \"Polygon\",\n \"coordinates\": [\n [\n [\n -79.4970703125,\n 36.84446074079564\n ],\n [\n -79.4970703125,\n 43.75522505306928\n ],\n [\n -73.388671875,\n 43.75522505306928\n ],\n [\n -73.388671875,\n 36.84446074079564\n ],\n [\n -79.4970703125,\n 36.84446074079564\n ]\n ]\n ]\n }\n }\n ]\n}","noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"4f4e4a80e4b07f02db6495ad","contributors":{"authors":[{"text":"Tice, Richard H.","contributorId":13601,"corporation":false,"usgs":true,"family":"Tice","given":"Richard","email":"","middleInitial":"H.","affiliations":[],"preferred":false,"id":145857,"contributorType":{"id":1,"text":"Authors"},"rank":1}]}} ,{"id":4418,"text":"cir566 - 1968 - Tertiary gold-bearing channel gravel in northern Nevada County, California","interactions":[],"lastModifiedDate":"2012-02-02T00:05:28","indexId":"cir566","displayToPublicDate":"1994-01-01T00:00:00","publicationYear":"1968","noYear":false,"publicationType":{"id":18,"text":"Report"},"publicationSubtype":{"id":5,"text":"USGS Numbered Series"},"seriesTitle":{"id":307,"text":"Circular","code":"CIR","onlineIssn":"2330-5703","printIssn":"1067-084X","active":true,"publicationSubtype":{"id":5}},"seriesNumber":"566","title":"Tertiary gold-bearing channel gravel in northern Nevada County, California","docAbstract":"The remains of a huge Tertiary gravel-filled channel lie in the area between the South and Middle Yuba Rivers in northern Nevada County, Calif. The deposits in this channel were the site of some of the most productive hydraulic gold mines in California between the 1850's and 1884. \r\n\r\nThe gravel occupies a major channel and parts of several tributaries that in Tertiary time cut into a surface of Paleozoic and Mesozoic igneous and metamorphic rocks. The gravel is partly covered by the remains of an extensive sheet of volcanic rocks, but it crops out along the broad crest of the ridge between the canyons of the South and Middle Yuba Rivers. The lower parts of the gravel deposits generally carry the highest values of placer gold. Traditionally, the richest deposits of all are found in the so-called blue gravel, which, when present, lies just above the bedrock and consists of a very coarse, poorly sorted mixture of cobbles, pebbles, sand, and clay. It is unoxidized, and, at least locally, contains appreciable quantities of secondary sulfide minerals, chiefly pyrite. \r\n\r\nInformation in drill logs from private sources indicates that a 2-mile stretch of the channel near North Columbia contains over half a million ounces of gold dispersed through about 22 million cubic yards of gravel at a grade .averaging about 81 cents per cubic yard. The deposit is buried at depths ranging from 100 to 400 feet. \r\n\r\nSeveral geophysical methods have been tested for their feasibility in determining the configuration of the buried bedrock surface, in delineating channel gravel buried under volcanic rocks, and in identifying concentrations of heavy minerals within the gravel. Although the data have not yet been completely processed, preliminary conclusions indicate that some methods may be quite useful. A combination of seismic-refraction and gravity methods was used to determine the depth and configuration of the bottom of the channel to an accuracy within 10 percent as checked by the drill holes. Seismic-refraction methods have identified depressions which are in the bedrock surface, below volcanic rocks, and which may be occupied by gravels. Seismic methods, however, cannot actually recognize the presence of low-velocity gravels beneath the higher velocity volcanic rocks. Electromagnetic methods, supplemented in part by induced-polarization methods, show promise of being able to recognize and trace blue gravel buried less than 200 feet deep. A broad vague magnetic anomaly across the channel suggests that more precise magnetic studies might delineate concentrations of magnetic material. The usefulness of resistivity methods appears from this study to be quite restricted because of irregular topography and the variable conductivity of layers within the gravel.","language":"ENGLISH","doi":"10.3133/cir566","usgsCitation":"Peterson, D.W., Yeend, W., Oliver, H.W., and Mattick, R., 1968, Tertiary gold-bearing channel gravel in northern Nevada County, California: U.S. Geological Survey Circular 566, iii, 22 p. :ill., maps. ;27 cm., https://doi.org/10.3133/cir566.","productDescription":"iii, 22 p. :ill., maps. ;27 cm.","costCenters":[],"links":[{"id":124415,"rank":0,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/circ/1968/0566/report-thumb.jpg"},{"id":31523,"rank":300,"type":{"id":11,"text":"Document"},"url":"https://pubs.usgs.gov/circ/1968/0566/report.pdf","linkFileType":{"id":1,"text":"pdf"}}],"noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"4f4e4ad9e4b07f02db684fd5","contributors":{"authors":[{"text":"Peterson, D. 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W.","contributorId":85570,"corporation":false,"usgs":true,"family":"Oliver","given":"H.","email":"","middleInitial":"W.","affiliations":[],"preferred":false,"id":149091,"contributorType":{"id":1,"text":"Authors"},"rank":3},{"text":"Mattick, R.E.","contributorId":85162,"corporation":false,"usgs":true,"family":"Mattick","given":"R.E.","affiliations":[],"preferred":false,"id":149090,"contributorType":{"id":1,"text":"Authors"},"rank":4}]}} ,{"id":2257,"text":"wsp1855 - 1968 - Ground-water levels in the United States, 1961-65, southwestern States","interactions":[],"lastModifiedDate":"2024-01-31T21:32:21.660914","indexId":"wsp1855","displayToPublicDate":"1994-01-01T00:00:00","publicationYear":"1968","noYear":false,"publicationType":{"id":18,"text":"Report"},"publicationSubtype":{"id":5,"text":"USGS Numbered Series"},"seriesTitle":{"id":341,"text":"Water Supply Paper","code":"WSP","active":false,"publicationSubtype":{"id":5}},"seriesNumber":"1855","title":"Ground-water levels in the United States, 1961-65, southwestern States","docAbstract":"No abstract available.
","language":"English","publisher":"U.S. Geological Survey","doi":"10.3133/wsp1855","usgsCitation":"McGuinness, C.L., 1968, Ground-water levels in the United States, 1961-65, southwestern States: U.S. Geological Survey Water Supply Paper 1855, v, 125 p., https://doi.org/10.3133/wsp1855.","productDescription":"v, 125 p.","costCenters":[],"links":[{"id":425180,"rank":3,"type":{"id":36,"text":"NGMDB Index Page"},"url":"https://ngmdb.usgs.gov/Prodesc/proddesc_25071.htm","text":"Arizona","linkFileType":{"id":5,"text":"html"}},{"id":28040,"rank":2,"type":{"id":11,"text":"Document"},"url":"https://pubs.usgs.gov/wsp/1855/report.pdf","linkFileType":{"id":1,"text":"pdf"}},{"id":425181,"rank":4,"type":{"id":36,"text":"NGMDB Index Page"},"url":"https://ngmdb.usgs.gov/Prodesc/proddesc_25072.htm","text":"Calfornia","linkFileType":{"id":5,"text":"html"}},{"id":425184,"rank":7,"type":{"id":36,"text":"NGMDB Index Page"},"url":"https://ngmdb.usgs.gov/Prodesc/proddesc_25075.htm","text":"New 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Series"},"seriesTitle":{"id":341,"text":"Water Supply Paper","code":"WSP","active":false,"publicationSubtype":{"id":5}},"seriesNumber":"1859","chapter":"E","title":"Hydrology of Crater, East and Davis Lakes, Oregon; with section on Chemistry of the Lakes","docAbstract":"Crater, East, and Davis Lakes are small bodies of fresh water that occupy topographically closed basins in Holocene volcanic terrane. Because the annual water supply exceeds annual evaporation, water must be lost by seepage from each lake. The seepage rates vary widely both in volume and in percentage of the total water supply. Crater Lake loses about 89 cfs (cubic feet per second), equivalent to about 72 percent of its average annual supply. East Lake loses about 2.3 cfs, or about 44 percent of its estimated supply. Davis Lake seepage varies greatly with lake level, but the average loss is about 150 cfs, more than 90 percent of its total supply. The destination of the seepage loss is not definitely known for any of the lakes. \r\n\r\nAn approximate water budget was computed for stationary level for each lake, by using estimates 'by the writer to supplement the hydrologic data available. The three lake waters are dilute. Crater Lake contains about 80 ppm, (parts per million) of dissolved solids---mostly silica, sodium, and bicarbonate, and lesser amounts of calcium, sulfate, and chloride. Much of the dissolved-solids content of Crater Lake---especially the sulfate and chloride---may be related to fumarole and thermal-spring activity that presumably followed the collapse of Mount Mazama. Although Grater Lake loses an estimated 7,000 tons of its 1.5million-ton salt content each year by leakage, the chemical character of the lake did not change appreciably between 1912 and 1964. East Lake contains 200 ppm of dissolved solids, which includes major proportions of calcium, sodium, bicarbonate, and sulfate, but almost no chloride. The lake apparently receives much of its dissolved solids from subsurface thermal springs. Annual solute loss from East Lake by leakage is about 450 tons, or 3 percent of the lake's 15,000-ton estimated solute content. Davis Lake contains only 48 ppm of dissolved solids, much of which is silica and bicarbonate; chloride is almost completely absent. Approximate physical and hydrologic data for the lakes are summarized in the following table.\r\n\r\n[Table]","language":"ENGLISH","publisher":"U.S. G.P.O.,","doi":"10.3133/wsp1859E","usgsCitation":"Phillips, K.N., and Van Denburgh, A.S., 1968, Hydrology of Crater, East and Davis Lakes, Oregon; with section on Chemistry of the Lakes: U.S. Geological Survey Water Supply Paper 1859, iv, 60 p. :ill. ;24 cm., https://doi.org/10.3133/wsp1859E.","productDescription":"iv, 60 p. :ill. ;24 cm.","costCenters":[{"id":518,"text":"Oregon Water Science Center","active":true,"usgs":true}],"links":[{"id":138755,"rank":0,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/wsp/1859e/report-thumb.jpg"},{"id":28614,"rank":300,"type":{"id":11,"text":"Document"},"url":"https://pubs.usgs.gov/wsp/1859e/report.pdf","linkFileType":{"id":1,"text":"pdf"}}],"noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"4f4e4a17e4b07f02db604971","contributors":{"authors":[{"text":"Phillips, Kenneth N.","contributorId":34105,"corporation":false,"usgs":true,"family":"Phillips","given":"Kenneth","email":"","middleInitial":"N.","affiliations":[],"preferred":false,"id":145287,"contributorType":{"id":1,"text":"Authors"},"rank":1},{"text":"Van Denburgh, A. S.","contributorId":23928,"corporation":false,"usgs":true,"family":"Van Denburgh","given":"A.","email":"","middleInitial":"S.","affiliations":[],"preferred":false,"id":145286,"contributorType":{"id":1,"text":"Authors"},"rank":2}]}} ,{"id":2059,"text":"wsp1839O - 1968 - A hydrogeologic study of the ground-water reservoirs contributing base runoff to Four Mile Creek, east-central Iowa","interactions":[],"lastModifiedDate":"2012-02-02T00:05:22","indexId":"wsp1839O","displayToPublicDate":"1994-01-01T00:00:00","publicationYear":"1968","noYear":false,"publicationType":{"id":18,"text":"Report"},"publicationSubtype":{"id":5,"text":"USGS Numbered Series"},"seriesTitle":{"id":341,"text":"Water Supply Paper","code":"WSP","active":false,"publicationSubtype":{"id":5}},"seriesNumber":"1839","chapter":"O","title":"A hydrogeologic study of the ground-water reservoirs contributing base runoff to Four Mile Creek, east-central Iowa","language":"ENGLISH","publisher":"U.S. G.P.O.,","doi":"10.3133/wsp1839O","usgsCitation":"Kunkle, G.R., 1968, A hydrogeologic study of the ground-water reservoirs contributing base runoff to Four Mile Creek, east-central Iowa: U.S. Geological Survey Water Supply Paper 1839, iv, 41 p. :ill., maps ;24 cm., https://doi.org/10.3133/wsp1839O.","productDescription":"iv, 41 p. :ill., maps ;24 cm.","costCenters":[],"links":[{"id":138562,"rank":0,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/wsp/1839o/report-thumb.jpg"},{"id":27602,"rank":300,"type":{"id":11,"text":"Document"},"url":"https://pubs.usgs.gov/wsp/1839o/report.pdf","linkFileType":{"id":1,"text":"pdf"}},{"id":27601,"rank":400,"type":{"id":17,"text":"Plate"},"url":"https://pubs.usgs.gov/wsp/1839o/plate-1.pdf","linkFileType":{"id":1,"text":"pdf"}}],"noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"4f4e4b23e4b07f02db6ae3d1","contributors":{"authors":[{"text":"Kunkle, George R.","contributorId":54972,"corporation":false,"usgs":true,"family":"Kunkle","given":"George","email":"","middleInitial":"R.","affiliations":[],"preferred":false,"id":144612,"contributorType":{"id":1,"text":"Authors"},"rank":1}]}} ,{"id":2341,"text":"wsp1854 - 1968 - Ground-water hydrology of the Sevier Desert, Utah","interactions":[],"lastModifiedDate":"2017-09-04T17:15:01","indexId":"wsp1854","displayToPublicDate":"1994-01-01T00:00:00","publicationYear":"1968","noYear":false,"publicationType":{"id":18,"text":"Report"},"publicationSubtype":{"id":5,"text":"USGS Numbered Series"},"seriesTitle":{"id":341,"text":"Water Supply Paper","code":"WSP","active":false,"publicationSubtype":{"id":5}},"seriesNumber":"1854","title":"Ground-water hydrology of the Sevier Desert, Utah","docAbstract":"The Sevier Desert, as used in this report, comprises the main part of the Sevier Desert, the Tintic Valley, and the southeastern part of the Old River Bed. It covers an area of about 3,000 square miles and occupies a large basin in the eastern part of the Basin and Range physiographic province.
Large alluvial fans extend from the mountain fronts into the basin where they interfinger with eolian and lacustrine deposits and with fluvial deposits of the Sevier River. These unconsolidated deposits form a multiaquifer artesian system that is more than 1,000 feet thick and that extends from near the area of main recharge along the east side of the basin to Sevier Lake.
Most of the recharge to the ground-water reservoir results from water entering alluvial fans as percolation from streams, irrigation ditches, and irrigated fields. Another important source may be water in the limestone, quartzite, and other consolidated rocks in the mountains that border the basin. Leakage from the Central Utah Canal is a major source of recharge to the water-table aquifer.
Flowing wells are common in the central lowland part of the Sevier Desert, but as a result of below-normal precipitation and an increase in withdrawals from wells during 1950-64, the area of flowing wells has decreased. The quantity of ground water being wasted from flowing wells is not more than a few hundred acre-feet a year.
The amount of water discharged by withdrawal from wells has increased nearly 15 times since 1950 (from 2,000 acre-feet in 1950 to 30,000 acre-feet in 1964). As a result of this increasing withdrawal, the water levels in observation wells have declined 4 feet in areas of small withdrawals to more than 7 feet near centers of pumping for public supplies and irrigation.
An estimated 135,000-175,000 acre-feet of ground water is consumed by evapotranspiration each year in the 440,000 acres of desert that mainly support phreatophytes. This rate of discharge has changed little since 1950. The consumptive waste of ground water by undesirable phreatophytes, principally saltcedar and pickleweed, was not a serious problem in 1964 but could become a serious problem in the near future if saltcedar is permitted to spread.
Water levels in wells changed little during 1935-40. During 1941-50, however, water levels rose in response to the general above-normal precipitation during 1939-47. During 1950-64 water levels declined, partly in response to below-normal precipitation and partly in response to an increase in pumping from irrigation wells. Although the period 1961-63 was one of above-normal precipitation, water levels continued the overall decline that was started in 1950. The decline, therefore, probably is due to increased pumping.
The amount of water that could be obtained from storage if the piezometric surface in the artesian aquifer were lowered 20 feet is estimated to be 120,006 acre-feet. The specific capacities of wells used for irrigation and public supply range from 5 to 215 gallons per minute per foot of drawdown. Specific capacities generally decrease with increasing distances away from the edge of the basin.
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south-central Alaska, is underlain by slightly metamorphosed Mesozoic sedimentary rocks, and by sandstones, conglomerates and coaly minerals of the Tertiary Kenai Formation. The bedrock is locally covered by extensive surficial deposits of Quaternary and Recent (Holocene) age. The Mesozoic strata are cut by a quartz monzonite batholith in the Tokositna Mountains and by alaskitic dikes and plugs in the Peters and Dutch Hills. A silica-carbonate dike, which formed by alteration of a mafic or ultramafic dike, was noted in the Peters Hills.\r\n\r\nThe major ore deposits are gold placer deposits of several types, including stream and bench deposits of Recent (Holocene) age, glacial-fluviatile deposits of Quaternary age, and conglomerates of Tertiary age. Quartz-rich conglomerates and breccias have also been productive and are interesting and controversial genetically. The present study indicates that they are closely related to shear zones containing quartz veins and highly altered rocks; previously the origin of the associated altered rocks had been ascribed to deep weathering.\r\n\r\nThe report also contains descriptions of a few gold lode prospects and of geochemically anomalous areas such as those at Bunco Creek and near Mount Goldie.","language":"ENGLISH","publisher":"U.S. Geological Survey],","doi":"10.3133/ofr6835","usgsCitation":"Clark, A.L., and Hawley, C.C., 1968, Reconnaissance geology, mineral occurrences, and geochemical anomalies of the Yentna district, Alaska: U.S. Geological Survey Open-File Report 68-35, 86 p. ill., maps ;27 cm., https://doi.org/10.3133/ofr6835.","productDescription":"86 p. ill., maps ;27 cm.","costCenters":[],"links":[{"id":106417,"rank":700,"type":{"id":15,"text":"Index Page"},"url":"https://ngmdb.usgs.gov/Prodesc/proddesc_8311.htm","linkFileType":{"id":5,"text":"html"},"description":"8311"},{"id":144700,"rank":0,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/of/1968/0035/report-thumb.jpg"},{"id":41488,"rank":400,"type":{"id":17,"text":"Plate"},"url":"https://pubs.usgs.gov/of/1968/0035/plate-1.pdf","linkFileType":{"id":1,"text":"pdf"}},{"id":41489,"rank":401,"type":{"id":17,"text":"Plate"},"url":"https://pubs.usgs.gov/of/1968/0035/plate-2.pdf","linkFileType":{"id":1,"text":"pdf"}},{"id":41490,"rank":402,"type":{"id":17,"text":"Plate"},"url":"https://pubs.usgs.gov/of/1968/0035/plate-3.pdf","linkFileType":{"id":1,"text":"pdf"}},{"id":41491,"rank":300,"type":{"id":11,"text":"Document"},"url":"https://pubs.usgs.gov/of/1968/0035/report.pdf","linkFileType":{"id":1,"text":"pdf"}}],"noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"4f4e4a6ce4b07f02db63ea88","contributors":{"authors":[{"text":"Clark, Allen L.","contributorId":96258,"corporation":false,"usgs":true,"family":"Clark","given":"Allen","email":"","middleInitial":"L.","affiliations":[],"preferred":false,"id":167156,"contributorType":{"id":1,"text":"Authors"},"rank":1},{"text":"Hawley, C. C.","contributorId":102070,"corporation":false,"usgs":true,"family":"Hawley","given":"C.","email":"","middleInitial":"C.","affiliations":[],"preferred":false,"id":167157,"contributorType":{"id":1,"text":"Authors"},"rank":2}]}} ,{"id":6340,"text":"pp516F - 1968 - Airborne measurements of terrestrial radioactivity as an aid to geologic mapping","interactions":[],"lastModifiedDate":"2012-02-02T00:05:45","indexId":"pp516F","displayToPublicDate":"1994-01-01T00:00:00","publicationYear":"1968","noYear":false,"publicationType":{"id":18,"text":"Report"},"publicationSubtype":{"id":5,"text":"USGS Numbered Series"},"seriesTitle":{"id":331,"text":"Professional Paper","code":"PP","onlineIssn":"2330-7102","printIssn":"1044-9612","active":true,"publicationSubtype":{"id":5}},"seriesNumber":"516","chapter":"F","title":"Airborne measurements of terrestrial radioactivity as an aid to geologic mapping","language":"ENGLISH","publisher":"U.S. Govt. Print. Off.,","doi":"10.3133/pp516F","usgsCitation":"Pitkin, J.A., 1968, Airborne measurements of terrestrial radioactivity as an aid to geologic mapping: U.S. Geological Survey Professional Paper 516, p. F1-F29, https://doi.org/10.3133/pp516F.","productDescription":"p. 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","language":"English","publisher":"U.S. Geological Survey","doi":"10.3133/b1251I","usgsCitation":"Smith, J.F., and Ketner, K., 1968, Devonian and Mississippian rocks and the date of the Roberts Mountains thrust in the Carlin-Pinon Range area, Nevada: U.S. Geological Survey Bulletin 1251, iii, 18 p., https://doi.org/10.3133/b1251I.","productDescription":"iii, 18 p.","costCenters":[],"links":[{"id":413774,"rank":3,"type":{"id":36,"text":"NGMDB Index Page"},"url":"https://ngmdb.usgs.gov/Prodesc/proddesc_21334.htm","linkFileType":{"id":5,"text":"html"}},{"id":63808,"rank":2,"type":{"id":11,"text":"Document"},"url":"https://pubs.usgs.gov/bul/1251i/report.pdf","linkFileType":{"id":1,"text":"pdf"}},{"id":165571,"rank":1,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/bul/1251i/report-thumb.jpg"}],"country":"United States","state":"Nevada","otherGeospatial":"Roberts Mountains thrust","geographicExtents":"{\n \"type\": \"FeatureCollection\",\n \"features\": [\n {\n \"type\": \"Feature\",\n \"properties\": {},\n \"geometry\": {\n \"coordinates\": [\n [\n [\n -115.75,\n 40.75\n ],\n [\n -116.25,\n 40.75\n ],\n [\n -116.25,\n 40.25\n ],\n [\n -115.75,\n 40.25\n ],\n [\n -115.75,\n 40.75\n ]\n ]\n ],\n \"type\": \"Polygon\"\n }\n }\n ]\n}","noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"4f4e4a9be4b07f02db65dcbf","contributors":{"authors":[{"text":"Smith, J. 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1968 - Geologic map of the Gracey quadrangle, Trigg and Christian Counties, Kentucky","interactions":[],"lastModifiedDate":"2012-02-10T00:10:45","indexId":"gq753","displayToPublicDate":"1994-01-01T00:00:00","publicationYear":"1968","noYear":false,"publicationType":{"id":18,"text":"Report"},"publicationSubtype":{"id":5,"text":"USGS Numbered Series"},"seriesTitle":{"id":316,"text":"Geologic Quadrangle","code":"GQ","active":false,"publicationSubtype":{"id":5}},"seriesNumber":"753","title":"Geologic map of the Gracey quadrangle, Trigg and Christian Counties, Kentucky","language":"ENGLISH","doi":"10.3133/gq753","usgsCitation":"Nelson, W.H., and Seeland, D.A., 1968, Geologic map of the Gracey quadrangle, Trigg and Christian Counties, Kentucky: U.S. Geological Survey Geologic Quadrangle 753, 1 map :col. ;78 x 83 cm., https://doi.org/10.3133/gq753.","productDescription":"1 map :col. ;78 x 83 cm.","costCenters":[],"links":[{"id":103474,"rank":700,"type":{"id":15,"text":"Index Page"},"url":"https://ngmdb.usgs.gov/Prodesc/proddesc_2060.htm","linkFileType":{"id":5,"text":"html"},"description":"2060"},{"id":248555,"rank":300,"type":{"id":11,"text":"Document"},"url":"https://pubs.usgs.gov/gq/0753/report.pdf","size":"33","linkFileType":{"id":1,"text":"pdf"}},{"id":253699,"rank":0,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/gq/0753/report-thumb.jpg"}],"scale":"24000","geographicExtents":"{ \"type\": \"FeatureCollection\", \"features\": [ { \"type\": \"Feature\", \"properties\": {}, \"geometry\": { \"type\": \"Polygon\", \"coordinates\": [ [ [ -87.75,36.8675 ], [ -87.75,37 ], [ -87.61749999999999,37 ], [ -87.61749999999999,36.8675 ], [ -87.75,36.8675 ] ] ] } } ] }","noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"4f4e4b02e4b07f02db698c86","contributors":{"authors":[{"text":"Nelson, Willis H.","contributorId":84777,"corporation":false,"usgs":true,"family":"Nelson","given":"Willis","email":"","middleInitial":"H.","affiliations":[],"preferred":false,"id":267304,"contributorType":{"id":1,"text":"Authors"},"rank":1},{"text":"Seeland, David Arthur","contributorId":9279,"corporation":false,"usgs":true,"family":"Seeland","given":"David","email":"","middleInitial":"Arthur","affiliations":[],"preferred":false,"id":267303,"contributorType":{"id":1,"text":"Authors"},"rank":2}]}} ,{"id":62691,"text":"gq668 - 1968 - Geologic map of the Brandenburg Mountain quadrangle, Pinal County, Arizona","interactions":[],"lastModifiedDate":"2012-02-10T00:10:47","indexId":"gq668","displayToPublicDate":"1994-01-01T00:00:00","publicationYear":"1968","noYear":false,"publicationType":{"id":18,"text":"Report"},"publicationSubtype":{"id":5,"text":"USGS Numbered Series"},"seriesTitle":{"id":316,"text":"Geologic Quadrangle","code":"GQ","active":false,"publicationSubtype":{"id":5}},"seriesNumber":"668","title":"Geologic map of the Brandenburg Mountain quadrangle, Pinal County, Arizona","language":"ENGLISH","doi":"10.3133/gq668","usgsCitation":"Krieger, M.L., 1968, Geologic map of the Brandenburg Mountain quadrangle, Pinal County, Arizona: U.S. Geological Survey Geologic Quadrangle 668, 1 map., https://doi.org/10.3133/gq668.","productDescription":"1 map.","costCenters":[],"links":[{"id":103391,"rank":700,"type":{"id":15,"text":"Index Page"},"url":"https://ngmdb.usgs.gov/Prodesc/proddesc_1977.htm","linkFileType":{"id":5,"text":"html"},"description":"1977"},{"id":248847,"rank":300,"type":{"id":11,"text":"Document"},"url":"https://pubs.usgs.gov/gq/0668/report.pdf","size":"416","linkFileType":{"id":1,"text":"pdf"}},{"id":254240,"rank":0,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/gq/0668/report-thumb.jpg"}],"scale":"24000","geographicExtents":"{ \"type\": \"FeatureCollection\", \"features\": [ { \"type\": \"Feature\", \"properties\": {}, \"geometry\": { \"type\": \"Polygon\", \"coordinates\": [ [ [ -110.61749999999999,32.8675 ], [ -110.61749999999999,33 ], [ -110.5,33 ], [ -110.5,32.8675 ], [ -110.61749999999999,32.8675 ] ] ] } } ] }","noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"4f4e4b0be4b07f02db69d92f","contributors":{"authors":[{"text":"Krieger, Medora Louise Hooper","contributorId":10413,"corporation":false,"usgs":true,"family":"Krieger","given":"Medora","email":"","middleInitial":"Louise Hooper","affiliations":[],"preferred":false,"id":267733,"contributorType":{"id":1,"text":"Authors"},"rank":1}]}} ,{"id":67322,"text":"i547 - 1968 - Geologic map of Fox Mountain quadrangle, Santa Barbara County, California","interactions":[],"lastModifiedDate":"2012-02-10T00:11:21","indexId":"i547","displayToPublicDate":"1994-01-01T00:00:00","publicationYear":"1968","noYear":false,"publicationType":{"id":18,"text":"Report"},"publicationSubtype":{"id":5,"text":"USGS Numbered Series"},"seriesTitle":{"id":320,"text":"IMAP","code":"I","active":false,"publicationSubtype":{"id":5}},"seriesNumber":"547","subseriesTitle":"NONE","title":"Geologic map of Fox Mountain quadrangle, Santa Barbara County, California","language":"ENGLISH","doi":"10.3133/i547","usgsCitation":"Vedder, J.G., 1968, Geologic map of Fox Mountain quadrangle, Santa Barbara County, California: U.S. Geological Survey IMAP 547, 1 map., https://doi.org/10.3133/i547.","productDescription":"1 map.","costCenters":[],"links":[{"id":102077,"rank":700,"type":{"id":15,"text":"Index Page"},"url":"https://ngmdb.usgs.gov/Prodesc/proddesc_510.htm","linkFileType":{"id":5,"text":"html"},"description":"510"},{"id":187512,"rank":0,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/thumbnails/usgs_thumb.jpg"}],"scale":"24000","geographicExtents":"{ \"type\": \"FeatureCollection\", \"features\": [ { \"type\": \"Feature\", \"properties\": {}, \"geometry\": { \"type\": \"Polygon\", \"coordinates\": [ [ [ -119.61749999999999,34.75 ], [ -119.61749999999999,34.8675 ], [ -119.5,34.8675 ], [ -119.5,34.75 ], [ -119.61749999999999,34.75 ] ] ] } } ] }","noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"4f4e4b13e4b07f02db6a3197","contributors":{"authors":[{"text":"Vedder, J. 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","language":"English","publisher":"U.S. Geological Survey","doi":"10.3133/b1242F","usgsCitation":"Sainsbury, C., Hamilton, J.C., and Huffman, C., 1968, Geochemical cycle of selected trace elements in the tin-tungsten-beryllium district, western Seward Peninsula, Alaska — A reconnaissance study: U.S. Geological Survey Bulletin 1242, Report: 42 p.; 2 Plates: 26.42 × 21.57 inches and 27.26 × 18.32 inches, https://doi.org/10.3133/b1242F.","productDescription":"Report: 42 p.; 2 Plates: 26.42 × 21.57 inches and 27.26 × 18.32 inches","costCenters":[],"links":[{"id":109669,"rank":700,"type":{"id":36,"text":"NGMDB Index Page"},"url":"https://ngmdb.usgs.gov/Prodesc/proddesc_21325.htm","linkFileType":{"id":5,"text":"html"},"description":"21325"},{"id":167287,"rank":0,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/bul/1242f/report-thumb.jpg"},{"id":97025,"rank":401,"type":{"id":17,"text":"Plate"},"url":"https://pubs.usgs.gov/bul/1242f/plate-2.pdf","linkFileType":{"id":1,"text":"pdf"}},{"id":97024,"rank":400,"type":{"id":17,"text":"Plate"},"url":"https://pubs.usgs.gov/bul/1242f/plate-1.pdf","linkFileType":{"id":1,"text":"pdf"}},{"id":97023,"rank":300,"type":{"id":11,"text":"Document"},"url":"https://pubs.usgs.gov/bul/1242f/report.pdf","linkFileType":{"id":1,"text":"pdf"}}],"country":"United States","state":"Alaska","otherGeospatial":"western Seward Peninsula","geographicExtents":"{\n \"type\": \"FeatureCollection\",\n \"features\": [\n {\n \"type\": \"Feature\",\n \"properties\": {},\n \"geometry\": {\n \"coordinates\": [\n [\n [\n -167.242,\n 65.5\n ],\n [\n -167.242,\n 65.44\n ],\n [\n -167.142,\n 65.44\n ],\n [\n -167.142,\n 65.5\n ],\n [\n -167.242,\n 65.5\n ]\n ]\n ],\n \"type\": \"Polygon\"\n }\n }\n ]\n}","noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"4f4e4b24e4b07f02db6ae54f","contributors":{"authors":[{"text":"Sainsbury, C.L.","contributorId":99968,"corporation":false,"usgs":true,"family":"Sainsbury","given":"C.L.","email":"","affiliations":[],"preferred":false,"id":215074,"contributorType":{"id":1,"text":"Authors"},"rank":1},{"text":"Hamilton, John C. jhamilton@usgs.gov","contributorId":4202,"corporation":false,"usgs":true,"family":"Hamilton","given":"John","email":"jhamilton@usgs.gov","middleInitial":"C.","affiliations":[],"preferred":true,"id":215072,"contributorType":{"id":1,"text":"Authors"},"rank":2},{"text":"Huffman, Claude Jr.","contributorId":14877,"corporation":false,"usgs":true,"family":"Huffman","given":"Claude","suffix":"Jr.","email":"","affiliations":[],"preferred":false,"id":215073,"contributorType":{"id":1,"text":"Authors"},"rank":3}]}} ,{"id":14001,"text":"ofr68119 - 1968 - Redefinition of the terms Kingsport Formation and Mascot Dolomite and subdivisions of the upper part of the Knox Group in eastern Tennessee","interactions":[],"lastModifiedDate":"2025-06-17T16:42:56.511921","indexId":"ofr68119","displayToPublicDate":"1994-01-01T00:00:00","publicationYear":"1968","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":"68-119","title":"Redefinition of the terms Kingsport Formation and Mascot Dolomite and subdivisions of the upper part of the Knox Group in eastern Tennessee","docAbstract":"Upper part of the Knox Group has previously been divided into three formations; however, because of the lack of regionally recognizable boundaries, there has been a marked inconsistency as to the rocks assigned by different workers to the Longview Dolomite, Kingsport Formation and Mascot Dolomite. Regional stratigraphic studies have pointed out that there are only two recognizable major gross lithologic divisions. Because of this limitation, the term Longview, which has been used as a fossil zone, is abandoned; the term Kingsport is redefined to include the limestone and medium to coarsely crystalline dolomite unit, and Mascot is redefined to include the silty to very-finely crystalline dolomite unit from the top of the Kingsport to the unconformity at the top of the Knox Group.
","language":"English","publisher":"U.S. Geological Survey","doi":"10.3133/ofr68119","usgsCitation":"Harris, L.D., 1968, Redefinition of the terms Kingsport Formation and Mascot Dolomite and subdivisions of the upper part of the Knox Group in eastern Tennessee: U.S. Geological Survey Open-File Report 68-119, Report: ii, 52 p.; 6 Figures: 62.53 x 21.41 inches or smaller, https://doi.org/10.3133/ofr68119.","productDescription":"Report: ii, 52 p.; 6 Figures: 62.53 x 21.41 inches or smaller","costCenters":[],"links":[{"id":490870,"rank":8,"type":{"id":29,"text":"Figure"},"url":"https://pubs.usgs.gov/of/1968/0119/figure-6.pdf","text":"Figure 6","linkFileType":{"id":1,"text":"pdf"}},{"id":490867,"rank":5,"type":{"id":29,"text":"Figure"},"url":"https://pubs.usgs.gov/of/1968/0119/figure-3.pdf","text":"Figure 3","linkFileType":{"id":1,"text":"pdf"}},{"id":490866,"rank":4,"type":{"id":29,"text":"Figure"},"url":"https://pubs.usgs.gov/of/1968/0119/figure-2.pdf","text":"Figure 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