During July 1977, fifty-one gravity stations were obtained in the Gerlach Extension Known Geothermal Resource Area and vicinity, northwestern Nevada. Elevations for twenty-seven stations were estimated from lake bed topographic contours. Horizontal positions for these stations were determined from topographic maps and vehicle odometer.
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Donald L.","contributorId":28597,"corporation":false,"usgs":true,"family":"Peterson","given":"Donald","email":"","middleInitial":"L.","affiliations":[],"preferred":false,"id":161768,"contributorType":{"id":1,"text":"Authors"},"rank":1},{"text":"Kaufmann, Harold E.","contributorId":102891,"corporation":false,"usgs":true,"family":"Kaufmann","given":"Harold","email":"","middleInitial":"E.","affiliations":[],"preferred":false,"id":161769,"contributorType":{"id":1,"text":"Authors"},"rank":2}]}} ,{"id":11174,"text":"ofr78116 - 1978 - Mercury analysis of sediments from cores in Clear Lake, Lake County, California","interactions":[],"lastModifiedDate":"2026-02-04T17:30:20.820826","indexId":"ofr78116","displayToPublicDate":"1994-01-01T00:00:00","publicationYear":"1978","noYear":false,"publicationType":{"id":18,"text":"Report"},"publicationSubtype":{"id":5,"text":"USGS Numbered Series"},"seriesTitle":{"id":330,"text":"Open-File Report","code":"OFR","onlineIssn":"2331-1258","printIssn":"0196-1497","active":true,"publicationSubtype":{"id":5}},"seriesNumber":"78-116","title":"Mercury analysis of sediments from cores in Clear Lake, Lake County, California","docAbstract":"Cores of late Quaternary sediments were collected from several sites in Clear Lake (fig. 1). Samples from two of these cores (fig. 2, 3) have been analyzed for their mercury content as part of a study on the time of emplacement of the mercury ore body at the nearby Sulphur Bank mine (fig. 1). The samples were analyzed in laboratories of the U.S. Geological Survey by the mercury vapor detector method (Vaughn and McCarthy, 1964; Vaughn, 1967). The analyses of core 6, except samples 332, 341, 343, 386, 406, and 462, were done by Mr. Kam Leong (Table 1); the remaining analyses were done by Mr. Allen Meier. Analyses of core 10 (table 2) were done by Mr. Meier. Meier reported interference by organic material in the samples he analyzed. Because the two sets of data are not in agreement, most of the samples submitted to Leong and Meier are being reanalyzed.
","language":"English","publisher":"U.S. Geological Survey","doi":"10.3133/ofr78116","usgsCitation":"Sims, J.D., 1978, Mercury analysis of sediments from cores in Clear Lake, Lake County, California: U.S. Geological Survey Open-File Report 78-116, 8 p., https://doi.org/10.3133/ofr78116.","productDescription":"8 p.","costCenters":[],"links":[{"id":143945,"rank":1,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/of/1978/0116/report-thumb.jpg"},{"id":499519,"rank":2,"type":{"id":11,"text":"Document"},"url":"https://pubs.usgs.gov/of/1978/0116/report.pdf","linkFileType":{"id":1,"text":"pdf"}}],"country":"United States","state":"California","county":"Lake County","otherGeospatial":"Clear 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\"}}]}","noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"4f4e4a4ae4b07f02db6248a5","contributors":{"authors":[{"text":"Sims, John D.","contributorId":60202,"corporation":false,"usgs":true,"family":"Sims","given":"John","email":"","middleInitial":"D.","affiliations":[],"preferred":false,"id":162672,"contributorType":{"id":1,"text":"Authors"},"rank":1}]}} ,{"id":11610,"text":"ofr78796 - 1978 - Geologic names of Ordovician rock-stratigraphic units exposed in Kentucky","interactions":[],"lastModifiedDate":"2026-02-17T19:39:23.311283","indexId":"ofr78796","displayToPublicDate":"1994-01-01T00:00:00","publicationYear":"1978","noYear":false,"publicationType":{"id":18,"text":"Report"},"publicationSubtype":{"id":5,"text":"USGS Numbered Series"},"seriesTitle":{"id":330,"text":"Open-File Report","code":"OFR","onlineIssn":"2331-1258","printIssn":"0196-1497","active":true,"publicationSubtype":{"id":5}},"seriesNumber":"78-796","title":"Geologic names of Ordovician rock-stratigraphic units exposed in Kentucky","docAbstract":"This report summarizes and indexes the current usage of geologic names of exposed rock-stratigraphic units of Ordovician age in Kentucky. The Ordovician rocks crop out mainly in two separate areas in Kentucky (fig. 1). The larger area of outcrop, covering much of the middle part of the state, forms the major part of the Blue Grass region of Kentucky. Outcrops of this region are contiguous with outcrops of Ordovician rocks in southwestern Ohio and southeastern Indiana. The smaller area of fairly continuous outcrops of Ordovician rocks lies south of the Blue Grass region along the Cumberland River and its tributaries. These outcrops are contiguous with outcrops of Ordovician rocks in Tennessee. A few isolated exposures of Ordovician rocks lie outside the areas of continuous outcrop.
","language":"English","publisher":"U.S. Geological Survey","doi":"10.3133/ofr78796","usgsCitation":"Weir, G.W., and Cressman, E.R., 1978, Geologic names of Ordovician rock-stratigraphic units exposed in Kentucky: U.S. Geological Survey Open-File Report 78-796, iii, 250 p., https://doi.org/10.3133/ofr78796.","productDescription":"iii, 250 p.","costCenters":[],"links":[{"id":500116,"rank":2,"type":{"id":11,"text":"Document"},"url":"https://pubs.usgs.gov/of/1978/0796/report.pdf","linkFileType":{"id":1,"text":"pdf"}},{"id":145256,"rank":1,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/of/1978/0796/report-thumb.jpg"}],"country":"United 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\"}}]}","noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"4f4e4ae0e4b07f02db688526","contributors":{"authors":[{"text":"Weir, Gordon Whitney","contributorId":59790,"corporation":false,"usgs":true,"family":"Weir","given":"Gordon","email":"","middleInitial":"Whitney","affiliations":[],"preferred":false,"id":163438,"contributorType":{"id":1,"text":"Authors"},"rank":1},{"text":"Cressman, Earle Rupert","contributorId":43324,"corporation":false,"usgs":true,"family":"Cressman","given":"Earle","email":"","middleInitial":"Rupert","affiliations":[],"preferred":false,"id":163437,"contributorType":{"id":1,"text":"Authors"},"rank":2}]}} ,{"id":55168,"text":"wdrHI772 - 1978 - Water resources data for Hawaii and other Pacific areas, water year 1977: Volume 2. Trust Territory of the Pacific Islands, Guam, American Samoa, and Northern Mariana Islands","interactions":[],"lastModifiedDate":"2025-12-04T14:39:16.415495","indexId":"wdrHI772","displayToPublicDate":"1994-01-01T00:00:00","publicationYear":"1978","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":"HI-77-2","title":"Water resources data for Hawaii and other Pacific areas, water year 1977: Volume 2. Trust Territory of the Pacific Islands, Guam, American Samoa, and Northern Mariana Islands","docAbstract":"Volume 2 of water resources data for the 1977 water year for other Pacific areas consist of records of stage, discharge, and water temperature; stage of a reservoir; and water levels in wells and springs. This report contains discharge records for 42 gaging stations; stage only record for 1 gaging station; water temperature for 26 gaging stations; and water levels for 13 observation wells. Also included are 56 low-flow partial-record stations. Additional water data were collected at various sites, not part of the systematic data collection program, and are published as miscellaneous measurements. These data represent that part of the National Water Data System operated by the U.S. Geological Survey and cooperating Governments and Federal agencies in other Pacific areas.
","language":"English","publisher":"U.S. Geological Survey","doi":"10.3133/wdrHI772","collaboration":"Prepared in cooperation with the Trust Territory of the Pacific Islands, the Governments of Guam, American Samoa, and Northern Mariana Islands, and with other agencies","usgsCitation":"Water Resources Division, U.S. Geological Survey, 1978, Water resources data for Hawaii and other Pacific areas, water year 1977: Volume 2. 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It extends from Duluth to the Canadian border.
\nBoth maximum and minimum altitudes for Minnesota occur in the watershed; 2.301 ft (701 ) at Eagle Mountain, about 12 mi (19 km) northwest of Grand Marais, and 602 ft (184 m), the normal level of Lake Superior. Total relief is nearly 1,700 ft (518 m). The North Shore area (Duluth to the Canadian border) has a southeastward slope that is especially precipitous adjacent to Lake Superior.
\nConforming to this topography, the drainage includes a series of 17 southeastward-flowing streams averaging 23 mi (36 km) in length, with an average gradient from headwaters to mouth of about 57 ft/mi (10.8 m/km). The streams are deeply entrenched and characterized by swift flows, many rapids and waterfalls, and especially steep gradients in the 3 to 5 mi (4.8 to 8.0 km) before entering Lake Superior.
\nThe Pigeon River drains the extreme northern part of the watershed and forms the international border between the United States and Canada. More than half of the 610 mi2 (1580 km2) drainage basin of the Pigeon River lies in Canada.
\nThe Nemadji River and tributaries drain the Nemadji Basin, the southern detached part of the watershed. Topographically, the Nemadji Basin is roughly spoon shaped with maximum total relief in Minnesota of about 800 ft (244 m). More than half of the approximately 55-mi (88-km) long river flows northeastward through Wisconsin before reaching Lake Superior.
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Alaska","indexId":"ha612","publicationYear":"1978","noYear":false,"title":"Water resources of the Kodiak-Shelikof subregion, south-central Alaska"},"id":1}],"lastModifiedDate":"2023-03-17T20:49:19.59126","indexId":"ha612","displayToPublicDate":"1994-01-01T00:00:00","publicationYear":"1978","noYear":false,"publicationType":{"id":18,"text":"Report"},"publicationSubtype":{"id":5,"text":"USGS Numbered Series"},"seriesTitle":{"id":318,"text":"Hydrologic Atlas","code":"HA","active":false,"publicationSubtype":{"id":5}},"seriesNumber":"612","title":"Water resources of the Kodiak-Shelikof subregion, south-central Alaska","docAbstract":"Hydrologic data for the Kodiak-Shelikof subregion of south-central Alaska are summarized to provide a basis for planning water resources development, identifying water problems and evaluating existing water quality and availability. Average annual precipitation, measured at a few coastal locations in this maritime climatic zone, ranges from 23 to 127 inches. Mean annual runoff for the Kodiak Island group ranges from 4 to 8 cfs/sq mi. A maximum instantaneous runoff of 457 cfs/sq mi has been determined from a small basin on Kodiak Island. Lowest measured stream discharges range from no flow to 0.91 cfs/sq mi. Surface water is the primary source of water supplies for the city of Kodiak and other communities. The geology of the subregion is characterized by metamorphosed sedimentary and volcanic rocks with only a thin mantle of unconsolidated material. A few small, alluvium-filled coastal valleys offer the most favorable conditions for ground-water development, but moderate yields (50-100 gal/min) have been obtained from wells in fractured bedrock. Water in streams and lakes generally has a dissolved-solids concentration less than 60 mg/L, and the water varies from a calcium-bicarbonate type to a sodium-chloride type. The chemical composition of ground waters has a dilute calcium-bicarbonate type in unconsolidated materials and a sodium-bicarbonate type in bedrock. The dissolved solids in the groundwater ranges from 170 to 250 mg/L.
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