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Gold and silver ores have been mined from fissure veins in Jurassic quartz monzonite and in the bordering Wenban Limestone of Devonian age. Geochemical data show anomalies of gold, silver, lead, zinc, copper, arsenic, antimony, mercury, and tellurium. 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","language":"English","publisher":"U. S. Geological Survey","doi":"10.3133/ofr68166","usgsCitation":"Lee, W., and Borcherdt, R.D., 1968, Pn spectral variations of the Gasbuggy explosion at intermediate distance ranges: U.S. Geological Survey Open-File Report 68-166, 18 p., https://doi.org/10.3133/ofr68166.","productDescription":"18 p.","costCenters":[],"links":[{"id":491234,"rank":2,"type":{"id":11,"text":"Document"},"url":"https://pubs.usgs.gov/of/1968/0166/report.pdf","linkFileType":{"id":1,"text":"pdf"}},{"id":147660,"rank":1,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/of/1968/0166/report-thumb.jpg"}],"noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"4f4e4ae4e4b07f02db689d92","contributors":{"authors":[{"text":"Lee, William Hung Kan","contributorId":83502,"corporation":false,"usgs":true,"family":"Lee","given":"William Hung Kan","affiliations":[],"preferred":false,"id":169800,"contributorType":{"id":1,"text":"Authors"},"rank":1},{"text":"Borcherdt, Roger D. 0000-0002-8668-0849 borcherdt@usgs.gov","orcid":"https://orcid.org/0000-0002-8668-0849","contributorId":2373,"corporation":false,"usgs":true,"family":"Borcherdt","given":"Roger","email":"borcherdt@usgs.gov","middleInitial":"D.","affiliations":[{"id":237,"text":"Earthquake Science Center","active":true,"usgs":true}],"preferred":true,"id":169801,"contributorType":{"id":1,"text":"Authors"},"rank":2}]}} ,{"id":32794,"text":"pp352I - 1968 - Rates of slope degradation as determined from botanical evidence, White Mountains, California","interactions":[],"lastModifiedDate":"2012-02-02T00:09:20","indexId":"pp352I","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":"352","chapter":"I","title":"Rates of slope degradation as determined from botanical evidence, White Mountains, California","largerWorkType":{"id":18,"text":"Report"},"largerWorkTitle":"Erosion and sedimentation in a semiarid environment","largerWorkSubtype":{"id":5,"text":"USGS Numbered Series"},"language":"ENGLISH","doi":"10.3133/pp352I","usgsCitation":"LaMarche, V.C., 1968, Rates of slope degradation as determined from botanical evidence, White Mountains, California: U.S. Geological Survey Professional Paper 352, p. 341-377, https://doi.org/10.3133/pp352I.","productDescription":"p. 341-377","costCenters":[],"links":[{"id":119887,"rank":0,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/pp/0352i/report-thumb.jpg"},{"id":60774,"rank":400,"type":{"id":17,"text":"Plate"},"url":"https://pubs.usgs.gov/pp/0352i/plate-1.pdf","linkFileType":{"id":1,"text":"pdf"}},{"id":60775,"rank":401,"type":{"id":17,"text":"Plate"},"url":"https://pubs.usgs.gov/pp/0352i/plate-2.pdf","linkFileType":{"id":1,"text":"pdf"}},{"id":60776,"rank":300,"type":{"id":11,"text":"Document"},"url":"https://pubs.usgs.gov/pp/0352i/report.pdf","linkFileType":{"id":1,"text":"pdf"}}],"noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"4f4e4a7fe4b07f02db64893b","contributors":{"authors":[{"text":"LaMarche, Valmore C. 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","language":"English","publisher":"U.S. Geological Survey","publisherLocation":"Washington, D.C.","doi":"10.3133/cir580","usgsCitation":"Eisenhuth, H., 1968, Index of surface-water records to September 30, 1967: Part 10. - The Great Basin: U.S. Geological Survey Circular 580, 37 p., https://doi.org/10.3133/cir580.","productDescription":"37 p.","numberOfPages":"42","costCenters":[],"links":[{"id":117215,"rank":0,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/circ/1968/0580/report-thumb.jpg"},{"id":31079,"rank":300,"type":{"id":11,"text":"Document"},"url":"https://pubs.usgs.gov/circ/1968/0580/report.pdf","linkFileType":{"id":1,"text":"pdf"}}],"country":"United States","state":"California, Nevada, Oregon, Utah, Wyoming","otherGeospatial":"Great Basin","geographicExtents":"{\n \"type\": \"FeatureCollection\",\n \"features\": [\n {\n \"type\": \"Feature\",\n \"properties\": {},\n \"geometry\": {\n \"type\": \"Polygon\",\n \"coordinates\": [\n [\n [\n -115.24658203125,\n 32.676372772089834\n ],\n [\n -115.521240234375,\n 38.26406296833961\n ],\n [\n -115.26855468749999,\n 38.44068226417387\n ],\n [\n -114.76318359375,\n 38.46219172306828\n ],\n [\n -114.7467041015625,\n 38.41055825094609\n ],\n [\n -114.2083740234375,\n 37.54457732085582\n ],\n [\n -114.136962890625,\n 37.58376576718623\n ],\n [\n -114.10400390625,\n 37.6968609874419\n ],\n [\n -114.312744140625,\n 38.53527591154413\n ],\n [\n -114.18090820312499,\n 38.69408504756833\n ],\n [\n -113.8568115234375,\n 38.655488159953\n ],\n [\n -113.6700439453125,\n 37.90953361677018\n ],\n [\n -113.44482421875,\n 37.47485808497102\n ],\n [\n -113.2305908203125,\n 37.431250501793585\n ],\n [\n -113.104248046875,\n 37.448696585910376\n ],\n [\n -111.67053222656249,\n 37.93553306183642\n ],\n [\n -111.2640380859375,\n 38.53527591154413\n ],\n [\n -110.8465576171875,\n 40.22082997283287\n ],\n [\n -110.32470703125,\n 41.75492216766298\n ],\n [\n -110.1708984375,\n 42.439674178149424\n ],\n [\n -111.55517578125,\n 42.52069952914966\n ],\n [\n -112.236328125,\n 41.83682786072714\n ],\n [\n -113.115234375,\n 41.934976500546604\n ],\n [\n -114.49951171875,\n 41.36031866306708\n ],\n [\n -115.75195312499999,\n 41.78769700539063\n ],\n [\n -117.3779296875,\n 42.09822241118974\n ],\n [\n -119.77294921874999,\n 44.32384807250689\n ],\n [\n -120.38818359375,\n 44.040218713142146\n ],\n [\n -120.76171875,\n 44.166444664458595\n ],\n [\n -121.57470703125,\n 44.38669150215206\n ],\n [\n -121.39892578125,\n 43.54854811091286\n ],\n [\n -121.11328124999999,\n 42.89206418807337\n ],\n [\n -120.08056640625,\n 42.74701217318067\n ],\n [\n -119.99267578124999,\n 41.983994270935625\n ],\n [\n -119.99267578124999,\n 41.27780646738183\n ],\n [\n -120.78369140624999,\n 41.244772343082076\n ],\n [\n -121.35498046875,\n 40.84706035607122\n ],\n [\n -120.498046875,\n 40.17887331434696\n ],\n [\n -120.08056640625,\n 39.99395569397331\n ],\n [\n -119.970703125,\n 39.01064750994083\n ],\n [\n -118.85009765625,\n 37.666429212090605\n ],\n [\n -118.10302734374999,\n 36.421282443649496\n ],\n [\n -118.27880859375001,\n 34.994003757575776\n ],\n [\n -118.80615234374999,\n 34.92197103616377\n ],\n [\n -117.46582031249999,\n 34.23451236236987\n ],\n [\n -116.45507812500001,\n 33.815666308702774\n ],\n [\n -116.27929687499999,\n 33.02708758002874\n ],\n [\n -116.03759765625,\n 32.62087018318113\n ],\n [\n -115.24658203125,\n 32.676372772089834\n ]\n ]\n ]\n }\n }\n ]\n}","noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"4f4e49f8e4b07f02db5f2ed0","contributors":{"authors":[{"text":"Eisenhuth, H.P.","contributorId":38140,"corporation":false,"usgs":true,"family":"Eisenhuth","given":"H.P.","email":"","affiliations":[],"preferred":false,"id":147959,"contributorType":{"id":1,"text":"Authors"},"rank":1}]}} ,{"id":3629,"text":"cir605 - 1968 - Gold distribution on the sea floor off the Klamath Mountains, California","interactions":[],"lastModifiedDate":"2017-06-25T15:32:15","indexId":"cir605","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":"605","title":"Gold distribution on the sea floor off the Klamath Mountains, California","docAbstract":"Analyses of 82 samples collected from the surface of the continental shelf between the Oregon-California border and Eureka, Calif., indicate that the background gold content on this shelf is about 0.1 ppb (part per billion). Four anomalous tracts, which range in extent from 10 to 30 square kilometers, have gold values above 10 ppb, and the richest sample contains 300 ppb. The anomalous areas seem to lack a close correlation with water depth, but they are related to areas underlain by soft Cenozoic strata that contain small quantities of dispersed gold originally derived from lodes in the Klarnath Mountains. This relationship suggests that the offshore gold accumulations are lag concentrates produced from the Cenozoic deposits by wave erosion during the postglacial rise in sea level. Gold contents at the surface are too low for economic recovery, and drilling will be required to determine whether the anomalous areas are underlain by higher grade material.","language":"English","publisher":"U.S. Geological Survey","doi":"10.3133/cir605","usgsCitation":"Moore, G.W., and Silver, E.A., 1968, Gold distribution on the sea floor off the Klamath Mountains, California: U.S. Geological Survey Circular 605, iii, 9 p. :maps. ;27 cm., https://doi.org/10.3133/cir605.","productDescription":"iii, 9 p. :maps. ;27 cm.","costCenters":[],"links":[{"id":30672,"rank":300,"type":{"id":11,"text":"Document"},"url":"https://pubs.usgs.gov/circ/1968/0605/report.pdf","linkFileType":{"id":1,"text":"pdf"}},{"id":122611,"rank":0,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/circ/1968/0605/report-thumb.jpg"}],"noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"4f4e4abde4b07f02db6740e3","contributors":{"authors":[{"text":"Moore, George William","contributorId":89123,"corporation":false,"usgs":true,"family":"Moore","given":"George","email":"","middleInitial":"William","affiliations":[],"preferred":false,"id":147288,"contributorType":{"id":1,"text":"Authors"},"rank":1},{"text":"Silver, Eli A.","contributorId":83505,"corporation":false,"usgs":true,"family":"Silver","given":"Eli","email":"","middleInitial":"A.","affiliations":[],"preferred":false,"id":147287,"contributorType":{"id":1,"text":"Authors"},"rank":2}]}} ,{"id":4002,"text":"cir578 - 1968 - Index of surface-water records to September 30, 1967 - Part 8, Western Gulf of Mexico basins","interactions":[],"lastModifiedDate":"2012-02-02T00:05:34","indexId":"cir578","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":"578","title":"Index of surface-water records to September 30, 1967 - Part 8, Western Gulf of Mexico basins","language":"ENGLISH","publisher":"U.S. Dept. of the Interior, Geological Survey,","doi":"10.3133/cir578","usgsCitation":"Eisenhuth, H., 1968, Index of surface-water records to September 30, 1967 - Part 8, Western Gulf of Mexico basins: U.S. Geological Survey Circular 578, 51 p. :ill., map ;26 cm., https://doi.org/10.3133/cir578.","productDescription":"51 p. :ill., map ;26 cm.","costCenters":[],"links":[{"id":117477,"rank":0,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/circ/1968/0578/report-thumb.jpg"},{"id":31087,"rank":300,"type":{"id":11,"text":"Document"},"url":"https://pubs.usgs.gov/circ/1968/0578/report.pdf","linkFileType":{"id":1,"text":"pdf"}}],"noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"4f4e49f8e4b07f02db5f2c81","contributors":{"authors":[{"text":"Eisenhuth, H.P.","contributorId":38140,"corporation":false,"usgs":true,"family":"Eisenhuth","given":"H.P.","email":"","affiliations":[],"preferred":false,"id":147967,"contributorType":{"id":1,"text":"Authors"},"rank":1}]}} ,{"id":2326,"text":"wsp1859B - 1968 - Chemical quality of surface waters in Devils Lake basin North Dakota, 1952-60","interactions":[],"lastModifiedDate":"2024-07-30T19:22:21.418399","indexId":"wsp1859B","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":"1859","chapter":"B","title":"Chemical quality of surface waters in Devils Lake basin North Dakota, 1952-60","docAbstract":"Above-normal precipitation in 1954, 1956, and 1957 caused the water surface of Devils Lake to rise to an altitude of 1,419.3 feet, its highest in 40 years. Nearly all the water entering the lake flowed through Big Coulee, and about three-fourths of that inflow was at rates greater than 100 cubic feet per second. At these rates, the inflow contained less than 600 ppm (parts per million) dissolved solids and was of the calcium bicarbonate type.
Because the inflow was more dilute than the lake water, the dissolved solids in the lake decreased from 8,680 ppm in 1952 to about 6,000 ppm in 1956 and 1957. Subsequently, however, they increased to slightly more than 8,000 ppm and averaged 6,800 ppm for the 1954-60 period. Sodium and sulfate were the principal dissolved constituents in the lake water. Although the concentration of dissolved solids varied significantly from time to time, the relative proportions of the chief constituents remained nearly the same.
Water flowed from Devils Lake to Mission Bay in 1956,1957, and 1958, and some flowed from Mission Bay into East Bay. However, no water moved between East Devils Lake, western Stump Lake, and eastern Stump Lake during 1952-60; these lakes received only local runoff, and the variations in their water volume caused only minor variations in dissolved solids. For the periods sampled, concentrations averaged 60,700 ppm for East Devils Lake, 23,100 ppm for western Stump Lake, and 127,000 ppm for eastern Stump Lake.
Sodium and sulfate were the chief dissolved constituents in all the lakes of the Devils Lake chain. Water in eastern Stump Lake was saturated with sodium sulfate and precipitated large quantities of granular, hydrated sodium sulfate crystals on the lakebed and shore in fall and winter. A discontinuous layer of consolidated sodium sulfate crystals formed a significant part of the bed throughout the year.
Measured concentrations! of zinc, iron, manganese, fluoride, arsenic, boron, copper, and lead were not high enough to harm fish. Data on alpha and beta particle activities in Devils Lake were insufficient to determine if present activities are less than, equal to, or more than activities before nuclear tests began.
Miscellaneous surface waters not in the Devils Lake chain contained dissolved solids that ranged from 239 to 61,200 ppm. The lakes that spill infrequently and have little or no ground-water inflow and outflow generally contain high concentrations of dissolved solids.
Salt balance computations for Devils Lake for 1952-60 indicate that a net of as much as 89,000 tons of salts was removed from the bed by the water in some years and as much as 35,000 tons was added to the bed in other years. For the 9-year period, the tons removed exceeded the tons added; the net removed averaged 2.7 tons per acre per year. Pickup of these salts from the bed increased the dissolved solids in the lake water an average of 193 ppni per year. Between 1952 and 1960, 201,000 tons of salt was added to the bed of East Devils Lake, 15,100 tons to the bed of western Stump Lake, and 421,000 tons to the bed of eastern Stump Lake.
Laboratory examination of shore and bed material indicated that the shore contained less weight of salt per unit weight of dry, inorganic material than the bed. Calcium and bicarbonate were the chief constituents dissolved from bed material of Devils Lake, whereas sodium and sulfate were the chief constituents dissolved from bed material of East Bay, East Devils Lake, and eastern and western Stump Lakes. Generally, calcium and bicarbonate were the chief constitutents dissolved from shore material of all these lakes.
Evidence indicates that not more than 20 percent of the salt that \"disappeared\" from the water of Devils Lake west of State Route 20 as the lake altitudes decreased years ago will redissolve if the lake altitude is restored.
","language":"English","publisher":"U.S. Geological Survey","publisherLocation":"Washington, D.C.","doi":"10.3133/wsp1859B","usgsCitation":"Mitten, H.T., Scott, C., and Rosene, P.G., 1968, Chemical quality of surface waters in Devils Lake basin North Dakota, 1952-60: U.S. Geological Survey Water Supply Paper 1859, Report: iv, 42 p.; 1 Plate: 27.00 x 38.00 inches, https://doi.org/10.3133/wsp1859B.","productDescription":"Report: iv, 42 p.; 1 Plate: 27.00 x 38.00 inches","costCenters":[{"id":478,"text":"North Dakota Water Science Center","active":true,"usgs":true},{"id":34685,"text":"Dakota Water Science Center","active":true,"usgs":true}],"links":[{"id":28169,"rank":2,"type":{"id":11,"text":"Document"},"url":"https://pubs.usgs.gov/wsp/1859b/report.pdf","linkFileType":{"id":1,"text":"pdf"}},{"id":28168,"rank":3,"type":{"id":17,"text":"Plate"},"url":"https://pubs.usgs.gov/wsp/1859b/plate-1.pdf","linkFileType":{"id":1,"text":"pdf"}},{"id":137586,"rank":1,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/wsp/1859b/report-thumb.jpg"},{"id":431666,"rank":4,"type":{"id":36,"text":"NGMDB Index Page"},"url":"https://ngmdb.usgs.gov/Prodesc/proddesc_25080.htm","linkFileType":{"id":5,"text":"html"}}],"country":"United States","state":"North Dakota","otherGeospatial":"Devils Lake basin","geographicExtents":"{\n \"type\": \"FeatureCollection\",\n \"features\": [\n {\n \"type\": \"Feature\",\n \"properties\": {},\n \"geometry\": {\n \"coordinates\": [\n [\n [\n -99.4066978557347,\n 48.373675264950265\n ],\n [\n -99.4066978557347,\n 47.70314111203487\n ],\n [\n -98.18978187218303,\n 47.70314111203487\n ],\n [\n -98.18978187218303,\n 48.373675264950265\n ],\n [\n -99.4066978557347,\n 48.373675264950265\n ]\n ]\n ],\n \"type\": \"Polygon\"\n }\n }\n ]\n}","noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"4f4e49dfe4b07f02db5e3305","contributors":{"authors":[{"text":"Mitten, Hugh T.","contributorId":103652,"corporation":false,"usgs":true,"family":"Mitten","given":"Hugh","email":"","middleInitial":"T.","affiliations":[],"preferred":false,"id":145018,"contributorType":{"id":1,"text":"Authors"},"rank":1},{"text":"Scott, C.H.","contributorId":101634,"corporation":false,"usgs":true,"family":"Scott","given":"C.H.","email":"","affiliations":[],"preferred":false,"id":145017,"contributorType":{"id":1,"text":"Authors"},"rank":2},{"text":"Rosene, Philip G.","contributorId":48942,"corporation":false,"usgs":true,"family":"Rosene","given":"Philip","email":"","middleInitial":"G.","affiliations":[],"preferred":false,"id":145016,"contributorType":{"id":1,"text":"Authors"},"rank":3}]}} ,{"id":37252,"text":"rp63_part1 - 1968 - National survey of needs for hatchery fish [Part I of II]","interactions":[],"lastModifiedDate":"2016-11-03T16:52:42","indexId":"rp63_part1","displayToPublicDate":"1994-01-01T00:00:00","publicationYear":"1968","noYear":false,"publicationType":{"id":18,"text":"Report"},"publicationSubtype":{"id":1,"text":"Federal Government Series"},"seriesTitle":{"id":79,"text":"Resource Publication","active":false,"publicationSubtype":{"id":1}},"seriesNumber":"63","title":"National survey of needs for hatchery fish [Part I of II]","docAbstract":"No abstract available.
","language":"English","publisher":"U.S. Fish and Wildlife Service","usgsCitation":"Division Of Fishery Services, 1968, National survey of needs for hatchery fish [Part I of II] (Part 1): Resource Publication 63, iv, 71 p.","productDescription":"iv, 71 p.","costCenters":[],"links":[{"id":162464,"rank":0,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/thumbnails/usgs_thumb.jpg"}],"edition":"Part 1","noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"4f4e4b23e4b07f02db6ae30f","contributors":{"authors":[{"text":"Division Of Fishery Services","contributorId":127987,"corporation":true,"usgs":false,"organization":"Division Of Fishery Services","id":529627,"contributorType":{"id":1,"text":"Authors"},"rank":1}]}} ,{"id":37251,"text":"rp62 - 1968 - Annual report for 1967, Cooperative Fishery Units","interactions":[],"lastModifiedDate":"2016-11-03T16:48:41","indexId":"rp62","displayToPublicDate":"1994-01-01T00:00:00","publicationYear":"1968","noYear":false,"publicationType":{"id":18,"text":"Report"},"publicationSubtype":{"id":1,"text":"Federal Government Series"},"seriesTitle":{"id":79,"text":"Resource Publication","active":false,"publicationSubtype":{"id":1}},"seriesNumber":"62","title":"Annual report for 1967, Cooperative Fishery Units","docAbstract":"No abstract available.
","language":"English","publisher":"U.S. Fish and Wildlife Service","usgsCitation":"Bureau Of Sport Fisheries And Wildlife, 1968, Annual report for 1967, Cooperative Fishery Units (Updates Resource Publication 41 (1967)): Resource Publication 62, iv, 63 p.","productDescription":"iv, 63 p.","costCenters":[],"links":[{"id":162463,"rank":0,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/thumbnails/usgs_thumb.jpg"}],"edition":"Updates Resource Publication 41 (1967)","noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"4f4e4ac8e4b07f02db67b8eb","contributors":{"authors":[{"text":"Bureau Of Sport Fisheries And Wildlife","contributorId":128243,"corporation":true,"usgs":false,"organization":"Bureau Of Sport Fisheries And Wildlife","id":529626,"contributorType":{"id":1,"text":"Authors"},"rank":1}]}} ,{"id":37265,"text":"rp73 - 1968 - Laboratories for fish disease research","interactions":[],"lastModifiedDate":"2016-11-09T11:24:59","indexId":"rp73","displayToPublicDate":"1994-01-01T00:00:00","publicationYear":"1968","noYear":false,"publicationType":{"id":18,"text":"Report"},"publicationSubtype":{"id":1,"text":"Federal Government Series"},"seriesTitle":{"id":79,"text":"Resource Publication","active":false,"publicationSubtype":{"id":1}},"seriesNumber":"73","title":"Laboratories for fish disease research","docAbstract":"No abstract available.
","language":"English","publisher":"U.S. Fish and Wildlife Service","usgsCitation":"Bureau Of Sport Fisheries And Wildlife, 1968, Laboratories for fish disease research: Resource Publication 73, 2 p.","productDescription":"2 p.","costCenters":[],"links":[{"id":162014,"rank":0,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/thumbnails/usgs_thumb.jpg"}],"noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"4f4e4b32e4b07f02db6b4504","contributors":{"authors":[{"text":"Bureau Of Sport Fisheries And Wildlife","contributorId":128243,"corporation":true,"usgs":false,"organization":"Bureau Of Sport Fisheries And Wildlife","id":529631,"contributorType":{"id":1,"text":"Authors"},"rank":1}]}} ,{"id":47296,"text":"ofr6933 - 1968 - Geologic map of Lunar Orbiter site II P-13, Oceanus Procellarum north of equator","interactions":[],"lastModifiedDate":"2022-04-28T20:17:32.759774","indexId":"ofr6933","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":"69-33","title":"Geologic map of Lunar Orbiter site II P-13, Oceanus Procellarum north of equator","docAbstract":"No abstract available.
","language":"English","publisher":"U.S. Geological Survey","doi":"10.3133/ofr6933","collaboration":"Prepared in cooperation with the Manned Spacecraft Center, National Aeronautics and Space Administration","usgsCitation":"Carr, M.H., and Titley, S., 1968, Geologic map of Lunar Orbiter site II P-13, Oceanus Procellarum north of equator: U.S. Geological Survey Open-File Report 69-33, 1 Plate: 38.15 x 29.85 inches, https://doi.org/10.3133/ofr6933.","productDescription":"1 Plate: 38.15 x 29.85 inches","costCenters":[],"links":[{"id":399851,"rank":2,"type":{"id":17,"text":"Plate"},"url":"https://pubs.usgs.gov/of/1969/0033/plate-1.pdf","linkFileType":{"id":1,"text":"pdf"}},{"id":172111,"rank":0,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/of/1969/0033/report-thumb.jpg"}],"scale":"100000","projection":"Mercator Projection","noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"4f4e4b12e4b07f02db6a2f01","contributors":{"authors":[{"text":"Carr, M. H.","contributorId":84727,"corporation":false,"usgs":true,"family":"Carr","given":"M.","email":"","middleInitial":"H.","affiliations":[{"id":131,"text":"Astrogeology Science Center","active":true,"usgs":true}],"preferred":false,"id":235000,"contributorType":{"id":1,"text":"Authors"},"rank":1},{"text":"Titley, S.R.","contributorId":60602,"corporation":false,"usgs":true,"family":"Titley","given":"S.R.","affiliations":[],"preferred":false,"id":234999,"contributorType":{"id":1,"text":"Authors"},"rank":2}]}} ,{"id":23395,"text":"ofr68140 - 1968 - A geologic and hydrologic reconnaissance of Lava Beds National Monument and vicinity, California","interactions":[],"lastModifiedDate":"2012-02-02T00:08:12","indexId":"ofr68140","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":"68-140","title":"A geologic and hydrologic reconnaissance of Lava Beds National Monument and vicinity, California","docAbstract":"Lava Beds National Monument is on the Modoc Plateau in Modoc and Siskiyou Counties. The principal geologic units in the vicinity are volcanic rocks, which in places are highly permeable and poorly permeable lake sedimentary deposits, all probably post-Oligocene in age. Yields and specific capacities of wells in the unconfined water body within volcanic rocks and lake deposits range widely, but in general are low in the lake deposits and higher in the volcanic rocks. A confined water body occurring in volcanic rocks underlying the lake deposits yields large quantities of water to three wells in the study area. \r\n\r\nDissolved-solids content of ground water generally increases in proportion to the thickness of lake deposits penetrated and to proximity of the lake deposits. Water from wells drilled in the volcanic rocks several miles from the lake deposits and from wells penetrating the confined water body in volcanic rocks underlying the lake deposits contains small to moderate quantities of dissolved solids. \r\n\r\nGround-water supplies can be developed almost anywhere in the study area by drilling wells to depths below the water table. In addition, there is a reasonable possibility of developing wells in a confined water body underlying the water-table system.","language":"ENGLISH","publisher":"U.S. Dept. of the Interior, Geological Survey, Water Resources Division,","doi":"10.3133/ofr68140","issn":"0094-9140","usgsCitation":"Hotchkiss, W.R., 1968, A geologic and hydrologic reconnaissance of Lava Beds National Monument and vicinity, California: U.S. Geological Survey Open-File Report 68-140, ii, 56 p., [1] folded leaf of plates :ill., maps ;27 cm., https://doi.org/10.3133/ofr68140.","productDescription":"ii, 56 p., [1] folded leaf of plates :ill., maps ;27 cm.","costCenters":[],"links":[{"id":156226,"rank":0,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/of/1968/0140/report-thumb.jpg"},{"id":52695,"rank":400,"type":{"id":17,"text":"Plate"},"url":"https://pubs.usgs.gov/of/1968/0140/plate-1.pdf","linkFileType":{"id":1,"text":"pdf"}},{"id":52696,"rank":300,"type":{"id":11,"text":"Document"},"url":"https://pubs.usgs.gov/of/1968/0140/report.pdf","linkFileType":{"id":1,"text":"pdf"}}],"noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"4f4e4b24e4b07f02db6ae67f","contributors":{"authors":[{"text":"Hotchkiss, W. 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