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","language":"English","publisher":"Society of Economic Geologists","doi":"10.2113/gsecongeo.62.6.862","usgsCitation":"Lanphere, M.A., 1967, Studies in the Providenclia area, Mexico, II, K-Ar and Rb-Sr ages of intrusive rocks and hydrothermal minerals: Economic Geology, v. 62, no. 6, p. 862-863, https://doi.org/10.2113/gsecongeo.62.6.862.","productDescription":"2 p.","startPage":"862","endPage":"863","costCenters":[],"links":[{"id":386350,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/thumbnails/outside_thumb.jpg"}],"country":"Mexico","otherGeospatial":"Providenclia area","geographicExtents":"{\n \"type\": \"FeatureCollection\",\n \"features\": [\n {\n \"type\": \"Feature\",\n \"properties\": {},\n \"geometry\": {\n \"type\": \"Polygon\",\n \"coordinates\": [\n [\n [\n -101.4697265625,\n 18.771115062337024\n ],\n [\n -96.50390625,\n 18.771115062337024\n ],\n [\n -96.50390625,\n 22.63429269379353\n ],\n [\n -101.4697265625,\n 22.63429269379353\n ],\n [\n -101.4697265625,\n 18.771115062337024\n ]\n ]\n ]\n }\n }\n ]\n}","volume":"62","issue":"6","noUsgsAuthors":false,"publicationDate":"1967-09-01","publicationStatus":"PW","contributors":{"authors":[{"text":"Lanphere, M. A.","contributorId":35298,"corporation":false,"usgs":true,"family":"Lanphere","given":"M.","email":"","middleInitial":"A.","affiliations":[],"preferred":false,"id":817279,"contributorType":{"id":1,"text":"Authors"},"rank":1}]}} ,{"id":70210846,"text":"70210846 - 1967 - Ancient geomagnetic field intensities—I Historic and archaeological data: Sets H1–H9","interactions":[],"lastModifiedDate":"2020-06-29T16:05:46.329454","indexId":"70210846","displayToPublicDate":"1967-09-01T11:01:55","publicationYear":"1967","noYear":false,"publicationType":{"id":2,"text":"Article"},"publicationSubtype":{"id":10,"text":"Journal Article"},"seriesTitle":{"id":1803,"text":"Geophysical Journal International","active":true,"publicationSubtype":{"id":10}},"title":"Ancient geomagnetic field intensities—I Historic and archaeological data: Sets H1–H9","docAbstract":"No abstract available.
","language":"English","publisher":"Oxford Academic","doi":"10.1111/j.1365-246X.1967.tb03140.x","usgsCitation":"Smith, P.J., 1967, Ancient geomagnetic field intensities—I Historic and archaeological data: Sets H1–H9: Geophysical Journal International, v. 13, no. 4, p. 417-419, https://doi.org/10.1111/j.1365-246X.1967.tb03140.x.","productDescription":"3 p.","startPage":"417","endPage":"419","costCenters":[],"links":[{"id":480343,"rank":0,"type":{"id":40,"text":"Open Access Publisher Index Page"},"url":"https://doi.org/10.1111/j.1365-246x.1967.tb03140.x","text":"Publisher Index Page"},{"id":375981,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/thumbnails/outside_thumb.jpg"}],"volume":"13","issue":"4","noUsgsAuthors":false,"publicationStatus":"PW","contributors":{"authors":[{"text":"Smith, Peter J.","contributorId":225580,"corporation":false,"usgs":false,"family":"Smith","given":"Peter","email":"","middleInitial":"J.","affiliations":[],"preferred":false,"id":791701,"contributorType":{"id":1,"text":"Authors"},"rank":1}]}} ,{"id":70010485,"text":"70010485 - 1967 - Enclosed bark as a pollen trap","interactions":[],"lastModifiedDate":"2026-02-09T15:58:48.987708","indexId":"70010485","displayToPublicDate":"1967-09-01T00:00:00","publicationYear":"1967","noYear":false,"publicationType":{"id":2,"text":"Article"},"publicationSubtype":{"id":10,"text":"Journal Article"},"seriesTitle":{"id":3338,"text":"Science","active":true,"publicationSubtype":{"id":10}},"title":"Enclosed bark as a pollen trap","docAbstract":"Counts were made of pollen in traps formed by enclosed bark in two remnants of bristlecone pine, Pinus aristata Engelm., from the White Mountains of east-central California. The traps, dated by tree-rings at A.D. 350 and 1300 B.C., contained a major complex of pine-sagebrush pollen and traces of other species, representing the equivalent of the present vegetation.
","language":"English","publisher":"American Association for the Advancement of Science","doi":"10.1126/science.157.3792.1067","issn":"00368075","usgsCitation":"Adam, D., Ferguson, C., and Lamarch, V., 1967, Enclosed bark as a pollen trap: Science, v. 157, no. 3792, p. 1067-1068, https://doi.org/10.1126/science.157.3792.1067.","productDescription":"2 p.","startPage":"1067","endPage":"1068","costCenters":[],"links":[{"id":219240,"rank":1,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/thumbnails/outside_thumb.jpg"}],"country":"United States","state":"California","otherGeospatial":"White Mountains","geographicExtents":"{\n \"type\": \"FeatureCollection\",\n \"features\": [\n {\n \"type\": \"Feature\",\n \"properties\": {},\n \"geometry\": {\n \"coordinates\": [\n [\n [\n -118.47740391404712,\n 37.84573086539517\n ],\n [\n -118.47740391404712,\n 37.24138647578789\n ],\n [\n -118.04023510512017,\n 37.24138647578789\n ],\n [\n -118.04023510512017,\n 37.84573086539517\n ],\n [\n -118.47740391404712,\n 37.84573086539517\n ]\n ]\n ],\n \"type\": \"Polygon\"\n }\n }\n ]\n}","volume":"157","issue":"3792","noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"505a091be4b0c8380cd51df2","contributors":{"authors":[{"text":"Adam, D.P.","contributorId":14815,"corporation":false,"usgs":true,"family":"Adam","given":"D.P.","email":"","affiliations":[],"preferred":false,"id":359031,"contributorType":{"id":1,"text":"Authors"},"rank":1},{"text":"Ferguson, C.W.","contributorId":37888,"corporation":false,"usgs":true,"family":"Ferguson","given":"C.W.","email":"","affiliations":[],"preferred":false,"id":359032,"contributorType":{"id":1,"text":"Authors"},"rank":2},{"text":"Lamarch, V.C. Jr.","contributorId":42348,"corporation":false,"usgs":true,"family":"Lamarch","given":"V.C.","suffix":"Jr.","email":"","affiliations":[],"preferred":false,"id":359033,"contributorType":{"id":1,"text":"Authors"},"rank":3}]}} ,{"id":70011660,"text":"70011660 - 1967 - Holocene changes in sea level: Evidence in Micronesia","interactions":[],"lastModifiedDate":"2026-02-09T16:06:55.109181","indexId":"70011660","displayToPublicDate":"1967-08-04T00:00:00","publicationYear":"1967","noYear":false,"publicationType":{"id":2,"text":"Article"},"publicationSubtype":{"id":10,"text":"Journal Article"},"seriesTitle":{"id":3338,"text":"Science","active":true,"publicationSubtype":{"id":10}},"title":"Holocene changes in sea level: Evidence in Micronesia","docAbstract":"Investigation of 33 islands, scattered widely across the Caroline and Marshall Island groups in the Central Pacific revealed no emerged reefs in which corals had unquestionably formed in situ, or other direct evidence of postglacial high stands of sea level. Low unconsolidated rock terraces and ridges of reefflat islands, mostly lying between tide levels, were composed of rubble conglomerates; carbon-14 dating of 11 samples from the conglomerates so far may suggest a former slightly higher sea level (nine samples range between 1890 and 3450 and one approaches 4500 years ago). However, recent hurricanes have produced ridges of comparable height and material, and in the same areas relics from World War II have been found cemented in place. Thus these datings do not in themselves necessarily indicate formerly higher sea levels. Rubble tracts are produced by storms under present conditions without any change in datum, and there seems to be no compelling evidence that they were not so developed during various periods in the past.
","language":"English","publisher":"American Association for the Advancement of Science","doi":"10.1126/science.157.3788.542","issn":"00368075","usgsCitation":"Shepard, F., Curray, J.R., Newman, W., Bloom, A., Newell, N., Tracey, J.I., and Veeh, H., 1967, Holocene changes in sea level: Evidence in Micronesia: Science, v. 157, no. 3788, p. 542-544, https://doi.org/10.1126/science.157.3788.542.","productDescription":"3 p.","startPage":"542","endPage":"544","costCenters":[],"links":[{"id":221603,"rank":1,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/thumbnails/outside_thumb.jpg"}],"otherGeospatial":"Caroline Islands, Marshall Islands","geographicExtents":"{\n \"type\": \"FeatureCollection\",\n \"features\": [\n {\n \"type\": \"Feature\",\n \"properties\": {},\n \"geometry\": {\n \"coordinates\": [\n [\n [\n 133.1239933290849,\n 9.7892225885888\n ],\n [\n 133.1239933290849,\n -0.2640485063964064\n ],\n [\n 148.38286324801322,\n -0.2640485063964064\n ],\n [\n 148.38286324801322,\n 9.7892225885888\n ],\n [\n 133.1239933290849,\n 9.7892225885888\n ]\n ]\n ],\n \"type\": \"Polygon\"\n }\n }\n ]\n}","volume":"157","issue":"3788","noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"505a31d8e4b0c8380cd5e296","contributors":{"authors":[{"text":"Shepard, F.P.","contributorId":75684,"corporation":false,"usgs":true,"family":"Shepard","given":"F.P.","email":"","affiliations":[],"preferred":false,"id":361643,"contributorType":{"id":1,"text":"Authors"},"rank":1},{"text":"Curray, Joseph R.","contributorId":92424,"corporation":false,"usgs":false,"family":"Curray","given":"Joseph","email":"","middleInitial":"R.","affiliations":[{"id":6728,"text":"Scripps Inst Oceanography","active":true,"usgs":false}],"preferred":false,"id":361644,"contributorType":{"id":1,"text":"Authors"},"rank":2},{"text":"Newman, W.A.","contributorId":94434,"corporation":false,"usgs":true,"family":"Newman","given":"W.A.","email":"","affiliations":[],"preferred":false,"id":361645,"contributorType":{"id":1,"text":"Authors"},"rank":3},{"text":"Bloom, A.L.","contributorId":67219,"corporation":false,"usgs":true,"family":"Bloom","given":"A.L.","email":"","affiliations":[],"preferred":false,"id":361642,"contributorType":{"id":1,"text":"Authors"},"rank":4},{"text":"Newell, N.D.","contributorId":52324,"corporation":false,"usgs":true,"family":"Newell","given":"N.D.","email":"","affiliations":[],"preferred":false,"id":361641,"contributorType":{"id":1,"text":"Authors"},"rank":5},{"text":"Tracey, J. I. Jr.","contributorId":17205,"corporation":false,"usgs":true,"family":"Tracey","given":"J.","suffix":"Jr.","email":"","middleInitial":"I.","affiliations":[],"preferred":false,"id":361639,"contributorType":{"id":1,"text":"Authors"},"rank":6},{"text":"Veeh, H.H.","contributorId":31906,"corporation":false,"usgs":true,"family":"Veeh","given":"H.H.","email":"","affiliations":[],"preferred":false,"id":361640,"contributorType":{"id":1,"text":"Authors"},"rank":7}]}} ,{"id":70221304,"text":"70221304 - 1967 - Closed system differentiation of sulfides in olivine Diabase, Missouri","interactions":[],"lastModifiedDate":"2021-06-09T16:25:21.608533","indexId":"70221304","displayToPublicDate":"1967-08-01T11:17:30","publicationYear":"1967","noYear":false,"publicationType":{"id":2,"text":"Article"},"publicationSubtype":{"id":10,"text":"Journal Article"},"seriesTitle":{"id":1472,"text":"Economic Geology","active":true,"publicationSubtype":{"id":10}},"title":"Closed system differentiation of sulfides in olivine Diabase, Missouri","docAbstract":"Two small bodies of Precambrian basic intrusive rock in southeastern Missouri show uninterrupted differentiation of olivine diabase that produced ferrogabbro. Olivine diabase, foliated gabbro and coarse gabbro constitute the major textural rock types. Gravitational settling of plagio-clase, olivine and Fe-Ti oxides occurred in both intrusives and iron enrichment is a conspicuous feature. Plagioclase ranges from An58 to An35 and olivine varies from Fa36 to Fa57. Because these rocks were intruded into volcanic rocks at a substantial depth and were slowly cooled in an apparently closed system, they afford an opportunity to trace the differentiation trends exhibited by the disseminated sulfides. Pyrrhotite, chal-copyrite, pentlandite, sphalerite and cubanite are the most abundant sulfides deposited initially as unmixed sulfide solid solutions which were essentially coprecipitates with the major silicates. Paragenesis and abundance of primary sulfides are directly related to the differentiation parameters shown by the silicates. The extreme fractionation of these intrusives did not lead to a large concentration of any of the sulfides at any stage during consolidation.
","language":"English","publisher":"Society of Economic Geologists","doi":"10.2113/gsecongeo.62.5.595","usgsCitation":"Desborough, G.A., 1967, Closed system differentiation of sulfides in olivine Diabase, Missouri: Economic Geology, v. 62, no. 5, p. 595-613, https://doi.org/10.2113/gsecongeo.62.5.595.","productDescription":"19 p.","startPage":"595","endPage":"613","costCenters":[],"links":[{"id":386351,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/thumbnails/outside_thumb.jpg"}],"country":"United States","state":"Missouri","geographicExtents":"{\n \"type\": \"FeatureCollection\",\n \"features\": [\n {\n \"type\": \"Feature\",\n \"properties\": {},\n \"geometry\": {\n \"type\": \"Polygon\",\n \"coordinates\": [\n [\n [\n -91.73583984374999,\n 40.613952441166596\n ],\n [\n -95.767822265625,\n 40.588928169693745\n ],\n [\n -95.657958984375,\n 40.27952566881291\n ],\n [\n -94.63623046875,\n 38.95940879245423\n ],\n [\n -94.63623046875,\n 36.500805317604794\n ],\n [\n -90.120849609375,\n 36.491973470593685\n ],\n [\n -90.362548828125,\n 35.97800618085566\n ],\n [\n -89.62646484375,\n 35.99578538642032\n ],\n [\n -89.09912109375,\n 36.73888412439431\n ],\n [\n -89.088134765625,\n 36.98500309285596\n ],\n [\n -89.62646484375,\n 37.80544394934271\n ],\n [\n -90.3515625,\n 38.229550455326134\n ],\n [\n -90.098876953125,\n 38.85682013474361\n ],\n [\n -90.5712890625,\n 38.87392853923629\n ],\n [\n -90.780029296875,\n 39.30029918615029\n ],\n [\n -91.483154296875,\n 39.90973623453719\n ],\n [\n -91.73583984374999,\n 40.613952441166596\n ]\n ]\n ]\n }\n }\n ]\n}","volume":"62","issue":"5","noUsgsAuthors":false,"publicationDate":"1967-08-01","publicationStatus":"PW","contributors":{"authors":[{"text":"Desborough, G. A.","contributorId":34527,"corporation":false,"usgs":true,"family":"Desborough","given":"G.","email":"","middleInitial":"A.","affiliations":[],"preferred":false,"id":817280,"contributorType":{"id":1,"text":"Authors"},"rank":1}]}} ,{"id":5221275,"text":"5221275 - 1967 - Lead poisoning in a sample of Maryland mourning doves","interactions":[],"lastModifiedDate":"2025-02-12T15:54:01.875257","indexId":"5221275","displayToPublicDate":"1967-07-03T00:00:00","publicationYear":"1967","noYear":false,"publicationType":{"id":2,"text":"Article"},"publicationSubtype":{"id":10,"text":"Journal Article"},"seriesTitle":{"id":2508,"text":"Journal of Wildlife Management","active":true,"publicationSubtype":{"id":10}},"title":"Lead poisoning in a sample of Maryland mourning doves","docAbstract":"A sick mourning dove (Zenuidura macroura) collected in Maryland with 2 lead shot in the gizzard showed acid-fast intranuclear inclusion bodies in the kidney tubular cells. The liver and the tibia contained 72 ppm and 187 ppm lead (wet weight) respectively. Four gizzards from 62 doves killed by hunters contained lead shot. The lead content of 43 dove livers ranged from 0.4-14.0 ppm (wet weight); 40 of these doves were collected by hunters, and the other 3 were dying of trichomoniasis.
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\"}}]}","volume":"31","issue":"3","noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"4f4e4b1ae4b07f02db6a84b7","contributors":{"authors":[{"text":"Locke, L. N.","contributorId":73539,"corporation":false,"usgs":true,"family":"Locke","given":"L.","email":"","middleInitial":"N.","affiliations":[],"preferred":false,"id":333465,"contributorType":{"id":1,"text":"Authors"},"rank":1},{"text":"Bagley, George E.","contributorId":46589,"corporation":false,"usgs":true,"family":"Bagley","given":"George","email":"","middleInitial":"E.","affiliations":[],"preferred":false,"id":333464,"contributorType":{"id":1,"text":"Authors"},"rank":2}]}} ,{"id":1003269,"text":"1003269 - 1967 - Selected strains of fish as bioassay animals","interactions":[],"lastModifiedDate":"2025-08-04T15:27:56.937334","indexId":"1003269","displayToPublicDate":"1967-07-01T00:00:00","publicationYear":"1967","noYear":false,"publicationType":{"id":2,"text":"Article"},"publicationSubtype":{"id":10,"text":"Journal Article"},"seriesTitle":{"id":3196,"text":"Progressive Fish-Culturist","active":true,"publicationSubtype":{"id":10}},"title":"Selected strains of fish as bioassay animals","docAbstract":"No abstract available.
","language":"English","publisher":"American Fisheries Society","doi":"10.1577/1548-8640(1967)29[129:SSOFAB]2.0.CO;2","usgsCitation":"Lennon, R.E., 1967, Selected strains of fish as bioassay animals: Progressive Fish-Culturist, v. 29, no. 3, p. 129-132, https://doi.org/10.1577/1548-8640(1967)29[129:SSOFAB]2.0.CO;2.","productDescription":"4 p.","startPage":"129","endPage":"132","costCenters":[{"id":606,"text":"Upper Midwest Environmental Sciences Center","active":true,"usgs":true}],"links":[{"id":131431,"rank":1,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/thumbnails/outside_thumb.jpg"}],"volume":"29","issue":"3","noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"4f4e4a02e4b07f02db5f8114","contributors":{"authors":[{"text":"Lennon, Robert E.","contributorId":14341,"corporation":false,"usgs":true,"family":"Lennon","given":"Robert","email":"","middleInitial":"E.","affiliations":[],"preferred":false,"id":313046,"contributorType":{"id":1,"text":"Authors"},"rank":1}]}} ,{"id":1000348,"text":"1000348 - 1967 - Growth of lake trout in Lake Superior before the maximum abundance of sea lampreys","interactions":[],"lastModifiedDate":"2026-04-14T19:38:20.466763","indexId":"1000348","displayToPublicDate":"1967-07-01T00:00:00","publicationYear":"1967","noYear":false,"publicationType":{"id":2,"text":"Article"},"publicationSubtype":{"id":10,"text":"Journal Article"},"seriesTitle":{"id":3624,"text":"Transactions of the American Fisheries Society","active":true,"publicationSubtype":{"id":10}},"title":"Growth of lake trout in Lake Superior before the maximum abundance of sea lampreys","docAbstract":"The growth in length of lake trout (Salvelinus namaycush) from the inshore water of Lake Superior in 1953 increased with age from the 3rd to 9th year, and was nearly constant from the 9th to the 12th year. Growth was greatest in the 1st year (4.0 inches) and least in the 2nd and 3rd years (2.3 inches). Between the 4th and 9th years the increments increased from 2.6 to 3.5 inches. Growth was calculated from a curvilinear body‐scale relation. Intraseasonal growth in length extended from late April until well after October; most growth was in late summer and fall. The younger fish started growth earlier, and some mature fish did not increase in length until after the October spawning. Lake trout reached the minimum legal weight (1.5 pounds) in the 7th year of life and the average size taken in the commercial fishery (about 3 pounds) in the 8th year. The annual increase in weight in the 8th year of life was over 64%. Fish used in this study grew more slowly than those from Lakes Michigan and Huron taken during the period when sea lamprey abundance was increasing, but at about the same rate as lake trout of Lake Michigan before the sea lamprey appeared.
","language":"English","publisher":"American Fisheries Society","doi":"10.1577/1548-8659(1967)96[268:GOLTIL]2.0.CO;2","usgsCitation":"Rahrer, J.F., 1967, Growth of lake trout in Lake Superior before the maximum abundance of sea lampreys: Transactions of the American Fisheries Society, v. 96, no. 3, p. 268-277, https://doi.org/10.1577/1548-8659(1967)96[268:GOLTIL]2.0.CO;2.","productDescription":"10 p.","startPage":"268","endPage":"277","costCenters":[{"id":324,"text":"Great Lakes Science Center","active":true,"usgs":true}],"links":[{"id":133477,"rank":1,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/thumbnails/outside_thumb.jpg"}],"country":"Canada, United States","otherGeospatial":"Lake Superior","geographicExtents":"{\n \"type\": \"FeatureCollection\",\n \"features\": [\n {\n \"type\": \"Feature\",\n \"properties\": {},\n \"geometry\": {\n \"coordinates\": [\n [\n [\n -92.24663639591222,\n 49.25115040376892\n ],\n [\n -92.24663639591222,\n 46.37141449520797\n ],\n [\n -83.89188842903135,\n 46.37141449520797\n ],\n [\n -83.89188842903135,\n 49.25115040376892\n ],\n [\n -92.24663639591222,\n 49.25115040376892\n ]\n ]\n ],\n \"type\": \"Polygon\"\n }\n }\n ]\n}","volume":"96","issue":"3","noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"4f4e4a57e4b07f02db62e3c7","contributors":{"authors":[{"text":"Rahrer, Jerold F.","contributorId":76679,"corporation":false,"usgs":true,"family":"Rahrer","given":"Jerold","email":"","middleInitial":"F.","affiliations":[],"preferred":false,"id":308435,"contributorType":{"id":1,"text":"Authors"},"rank":1}]}} ,{"id":70207355,"text":"70207355 - 1967 - Applications of factor analysis in study of chemistry of groundwater quality, Mojave River Valley, California","interactions":[],"lastModifiedDate":"2019-12-19T07:41:52","indexId":"70207355","displayToPublicDate":"1967-06-30T09:51:59","publicationYear":"1967","noYear":false,"publicationType":{"id":2,"text":"Article"},"publicationSubtype":{"id":10,"text":"Journal Article"},"seriesTitle":{"id":3722,"text":"Water Resources Research","onlineIssn":"1944-7973","printIssn":"0043-1397","active":true,"publicationSubtype":{"id":10}},"title":"Applications of factor analysis in study of chemistry of groundwater quality, Mojave River Valley, California","docAbstract":"Factor analysis is applied to results of chemical analyses of 103 water samples from wells in the Upper and Middle Mojave River valley, San Bernardino County, California. Chemical analyses showed that there are three principal chemical types of water, calcium bicarbonate, sodium sulfate, and sodium chloride, as well as many mixtures of the three. Data were studied by factor analysis to learn the relative importance of each principal ion in determining the variations among the samples, and to examine the possibility of chemical equilibrium between aqueous and solid phases in the aquifers. Most of the covariance in the system may be accounted for by variances of Ca+2, Mg+2, Na+1, SO4−2, and Cl−1. There is almost identical loading on the constituents Na+1 and Cl−1. The variance in chemical composition of the hydrochemical system is governed largely by sources of sodium chloride. None of the components is controlled by equilibrium between ions in the water and minerals in the aquifers. Concentrations of NO3−1 and F−1 vary independently of other constituents. Geographic distribution of statistical loadings of the principal constituents at individual wells does not reveal sources of the constituents, which must be deduced from geologic and hydrologic evidence. Factor analysis, however, furnished the critical information on chemical relationships basic to the deduction.
","language":"English","publisher":"American Geophysical Union","doi":"10.1029/WR003i002p00505","issn":"00431397","usgsCitation":"Dawdy, D., and Feth, J.H., 1967, Applications of factor analysis in study of chemistry of groundwater quality, Mojave River Valley, California: Water Resources Research, v. 3, no. 2, p. 505-510, https://doi.org/10.1029/WR003i002p00505.","productDescription":"6 p. ","startPage":"505","endPage":"510","costCenters":[],"links":[{"id":370397,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/thumbnails/outside_thumb.jpg"}],"country":"United States","state":"California","otherGeospatial":" Mojave River Valley","geographicExtents":"{\n \"type\": \"FeatureCollection\",\n \"features\": [\n {\n \"type\": \"Feature\",\n \"properties\": {},\n \"geometry\": {\n \"type\": \"Polygon\",\n \"coordinates\": [\n [\n [\n -121.6845703125,\n 32.565333160841035\n ],\n [\n -114.5654296875,\n 32.565333160841035\n ],\n [\n -114.5654296875,\n 36.2265501474709\n ],\n [\n -121.6845703125,\n 36.2265501474709\n ],\n [\n -121.6845703125,\n 32.565333160841035\n ]\n ]\n ]\n }\n }\n ]\n}","volume":"3","issue":"2","noUsgsAuthors":false,"publicationDate":"2010-07-09","publicationStatus":"PW","contributors":{"authors":[{"text":"Dawdy, D.R.","contributorId":99956,"corporation":false,"usgs":true,"family":"Dawdy","given":"D.R.","affiliations":[],"preferred":false,"id":777798,"contributorType":{"id":1,"text":"Authors"},"rank":1},{"text":"Feth, J. H.","contributorId":50495,"corporation":false,"usgs":true,"family":"Feth","given":"J.","email":"","middleInitial":"H.","affiliations":[],"preferred":false,"id":777799,"contributorType":{"id":1,"text":"Authors"},"rank":2}]}} ,{"id":70209073,"text":"70209073 - 1967 - Breeding behavior of an uniquely marked Starling ","interactions":[],"lastModifiedDate":"2020-03-13T08:15:03","indexId":"70209073","displayToPublicDate":"1967-06-30T08:04:22","publicationYear":"1967","noYear":false,"publicationType":{"id":2,"text":"Article"},"publicationSubtype":{"id":10,"text":"Journal Article"},"seriesTitle":{"id":3783,"text":"The Wilson Bulletin","printIssn":"0043-5643","active":true,"publicationSubtype":{"id":10}},"title":"Breeding behavior of an uniquely marked Starling ","docAbstract":"No abstract available.
","language":"English","usgsCitation":"Grant , C., 1967, Breeding behavior of an uniquely marked Starling : The Wilson Bulletin, v. 79, no. 5, p. 243-244.","productDescription":"2 p. ","startPage":"243","endPage":"244","costCenters":[],"links":[{"id":373237,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/thumbnails/outside_thumb.jpg"}],"country":"United States ","state":"Colorado ","city":"Denver","otherGeospatial":"Wildlife Research Center","geographicExtents":"{\"type\":\"FeatureCollection\",\"features\":[{\"type\":\"Feature\",\"geometry\":{\"type\":\"Polygon\",\"coordinates\":[[[-105.0518,39.7885],[-104.9271,39.7891],[-104.927,39.7836],[-104.9038,39.7841],[-104.904,39.7985],[-104.8847,39.7986],[-104.8843,39.8132],[-104.8657,39.8134],[-104.866,39.7986],[-104.7913,39.7991],[-104.7916,39.8426],[-104.7329,39.8436],[-104.7313,39.8991],[-104.6928,39.8988],[-104.6929,39.9067],[-104.6352,39.9067],[-104.634,39.899],[-104.6004,39.8988],[-104.5986,39.8736],[-104.6175,39.8739],[-104.619,39.8249],[-104.7622,39.823],[-104.7617,39.7976],[-104.7339,39.7985],[-104.7343,39.769],[-104.8564,39.7688],[-104.8567,39.7543],[-104.8854,39.7545],[-104.8856,39.7396],[-104.8857,39.7323],[-104.8761,39.7322],[-104.8764,39.7177],[-104.8668,39.7176],[-104.8663,39.7104],[-104.8849,39.706],[-104.8851,39.6929],[-104.9025,39.693],[-104.9011,39.6635],[-104.8904,39.6639],[-104.8384,39.6598],[-104.8849,39.633],[-104.8844,39.6239],[-104.9119,39.6242],[-104.9129,39.636],[-104.9205,39.6433],[-104.9402,39.6444],[-104.98,39.666],[-105.0164,39.6659],[-105.0303,39.6542],[-105.0312,39.6351],[-105.0515,39.6353],[-105.0518,39.6104],[-105.1061,39.6099],[-105.1059,39.6334],[-105.0844,39.6333],[-105.0651,39.6449],[-105.0654,39.6667],[-105.0517,39.6666],[-105.0518,39.7885]]]},\"properties\":{\"name\":\"Denver\",\"state\":\"CO\"}}]}","volume":"79","issue":"5","noUsgsAuthors":false,"publicationStatus":"PW","contributors":{"authors":[{"text":"Grant , C. Val","contributorId":223282,"corporation":false,"usgs":false,"family":"Grant ","given":"C. Val","affiliations":[],"preferred":false,"id":784728,"contributorType":{"id":1,"text":"Authors"},"rank":1}]}} ,{"id":70227113,"text":"70227113 - 1967 - Chapter VIII: Lunar theory and processes","interactions":[],"lastModifiedDate":"2021-12-29T19:55:41.004213","indexId":"70227113","displayToPublicDate":"1967-06-01T13:45:47","publicationYear":"1967","noYear":false,"publicationType":{"id":5,"text":"Book chapter"},"publicationSubtype":{"id":24,"text":"Book Chapter"},"title":"Chapter VIII: Lunar theory and processes","docAbstract":"Much valuable new information has been provided by Surveyor III; some of the most significant and interesting events are presented here. Only a limited interpretive discussion is included at this time, pending completion of data reduction and more detailed analysis of information available from the Surveyor mission.
","largerWorkType":{"id":18,"text":"Report"},"largerWorkTitle":"Surveyor III mission report: Part II: Scientific results","largerWorkSubtype":{"id":3,"text":"Organization Series"},"language":"English","publisher":"Jet Propulsion Laboratory","usgsCitation":"Gault, D.E., Collins, R., Gold, T., Green, J., Kuiper, G.P., Masursky, H., O'Keefe, J., Phinney, R., and Shoemaker, E.M., 1967, Chapter VIII: Lunar theory and processes, chap. of Surveyor III mission report: Part II: Scientific results, p. 193-212.","productDescription":"JPL TR-32-1177, 20 p.","startPage":"193","endPage":"212","costCenters":[],"links":[{"id":393616,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/thumbnails/outside_thumb.jpg"},{"id":393613,"rank":1,"type":{"id":11,"text":"Document"},"url":"https://ntrs.nasa.gov/api/citations/19670028832/downloads/19670028832.pdf","size":"443 MB","linkFileType":{"id":1,"text":"pdf"}}],"otherGeospatial":"Moon","noUsgsAuthors":false,"publicationStatus":"PW","contributors":{"authors":[{"text":"Gault, D. E.","contributorId":38580,"corporation":false,"usgs":true,"family":"Gault","given":"D.","email":"","middleInitial":"E.","affiliations":[],"preferred":false,"id":829682,"contributorType":{"id":1,"text":"Authors"},"rank":1},{"text":"Collins, R.","contributorId":12717,"corporation":false,"usgs":true,"family":"Collins","given":"R.","affiliations":[],"preferred":false,"id":829683,"contributorType":{"id":1,"text":"Authors"},"rank":2},{"text":"Gold, T.","contributorId":270013,"corporation":false,"usgs":false,"family":"Gold","given":"T.","email":"","affiliations":[{"id":12722,"text":"Cornell University","active":true,"usgs":false}],"preferred":false,"id":829684,"contributorType":{"id":1,"text":"Authors"},"rank":3},{"text":"Green, J.","contributorId":26439,"corporation":false,"usgs":true,"family":"Green","given":"J.","affiliations":[],"preferred":false,"id":829685,"contributorType":{"id":1,"text":"Authors"},"rank":4},{"text":"Kuiper, G. P.","contributorId":9394,"corporation":false,"usgs":true,"family":"Kuiper","given":"G.","email":"","middleInitial":"P.","affiliations":[],"preferred":false,"id":829686,"contributorType":{"id":1,"text":"Authors"},"rank":5},{"text":"Masursky, H.","contributorId":33823,"corporation":false,"usgs":true,"family":"Masursky","given":"H.","affiliations":[],"preferred":false,"id":829687,"contributorType":{"id":1,"text":"Authors"},"rank":6},{"text":"O'Keefe, J.","contributorId":65698,"corporation":false,"usgs":true,"family":"O'Keefe","given":"J.","affiliations":[],"preferred":false,"id":829688,"contributorType":{"id":1,"text":"Authors"},"rank":7},{"text":"Phinney, R.","contributorId":52735,"corporation":false,"usgs":true,"family":"Phinney","given":"R.","affiliations":[],"preferred":false,"id":829689,"contributorType":{"id":1,"text":"Authors"},"rank":8},{"text":"Shoemaker, Eugene Merle","contributorId":20342,"corporation":false,"usgs":true,"family":"Shoemaker","given":"Eugene","email":"","middleInitial":"Merle","affiliations":[],"preferred":false,"id":829690,"contributorType":{"id":1,"text":"Authors"},"rank":9}]}} ,{"id":70227112,"text":"70227112 - 1967 - Chapter 8: Lunar theory and processes","interactions":[],"lastModifiedDate":"2021-12-29T19:44:54.336467","indexId":"70227112","displayToPublicDate":"1967-06-01T13:32:07","publicationYear":"1967","noYear":false,"publicationType":{"id":5,"text":"Book chapter"},"publicationSubtype":{"id":24,"text":"Book Chapter"},"title":"Chapter 8: Lunar theory and processes","docAbstract":"Significant new information has been provided by Surveyor III's successful landing and operation on the lunar surface; some of the most significant and interesting events are presented here. Pending completion of data reduction and more detailed analysis of the information available from the Surveyor mission, only limited interpretive discussion is included.
","largerWorkType":{"id":18,"text":"Report"},"largerWorkTitle":"Surveyor III: A preliminary report","largerWorkSubtype":{"id":1,"text":"Federal Government Series"},"language":"English","publisher":"National Aeronautics and Space Administration","usgsCitation":"Gault, D.E., Collins, R.J., Gold, T., Green, J., Kuiper, G.P., Masursky, H., O'Keefe, J., Phinney, R., and Shoemaker, E.M., 1967, Chapter 8: Lunar theory and processes, chap. of Surveyor III: A preliminary report, p. 141-156.","productDescription":"NASA SP-146, 26 p.","startPage":"141","endPage":"156","costCenters":[],"links":[{"id":393611,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/thumbnails/outside_thumb.jpg"},{"id":393610,"rank":1,"type":{"id":11,"text":"Document"},"url":"https://ntrs.nasa.gov/api/citations/19670023253/downloads/19670023253.pdf","size":"61.4 MB","linkFileType":{"id":1,"text":"pdf"}}],"otherGeospatial":"Moon","noUsgsAuthors":false,"publicationStatus":"PW","contributors":{"compilers":[{"text":"Newell, Homer E.","contributorId":270651,"corporation":false,"usgs":false,"family":"Newell","given":"Homer","email":"","middleInitial":"E.","affiliations":[{"id":37453,"text":"National Aeronautics and Space Administration","active":true,"usgs":false}],"preferred":false,"id":829681,"contributorType":{"id":3,"text":"Compilers"},"rank":1}],"authors":[{"text":"Gault, D. E.","contributorId":38580,"corporation":false,"usgs":true,"family":"Gault","given":"D.","email":"","middleInitial":"E.","affiliations":[],"preferred":false,"id":829672,"contributorType":{"id":1,"text":"Authors"},"rank":1},{"text":"Collins, R. J.","contributorId":77655,"corporation":false,"usgs":true,"family":"Collins","given":"R.","email":"","middleInitial":"J.","affiliations":[],"preferred":false,"id":829673,"contributorType":{"id":1,"text":"Authors"},"rank":2},{"text":"Gold, T.","contributorId":270013,"corporation":false,"usgs":false,"family":"Gold","given":"T.","email":"","affiliations":[{"id":12722,"text":"Cornell University","active":true,"usgs":false}],"preferred":false,"id":829674,"contributorType":{"id":1,"text":"Authors"},"rank":3},{"text":"Green, J.","contributorId":26439,"corporation":false,"usgs":true,"family":"Green","given":"J.","affiliations":[],"preferred":false,"id":829675,"contributorType":{"id":1,"text":"Authors"},"rank":4},{"text":"Kuiper, G. P.","contributorId":9394,"corporation":false,"usgs":true,"family":"Kuiper","given":"G.","email":"","middleInitial":"P.","affiliations":[],"preferred":false,"id":829676,"contributorType":{"id":1,"text":"Authors"},"rank":5},{"text":"Masursky, H.","contributorId":33823,"corporation":false,"usgs":true,"family":"Masursky","given":"H.","affiliations":[],"preferred":false,"id":829677,"contributorType":{"id":1,"text":"Authors"},"rank":6},{"text":"O'Keefe, J.","contributorId":65698,"corporation":false,"usgs":true,"family":"O'Keefe","given":"J.","affiliations":[],"preferred":false,"id":829678,"contributorType":{"id":1,"text":"Authors"},"rank":7},{"text":"Phinney, R.","contributorId":52735,"corporation":false,"usgs":true,"family":"Phinney","given":"R.","affiliations":[],"preferred":false,"id":829679,"contributorType":{"id":1,"text":"Authors"},"rank":8},{"text":"Shoemaker, Eugene Merle","contributorId":20342,"corporation":false,"usgs":true,"family":"Shoemaker","given":"Eugene","email":"","middleInitial":"Merle","affiliations":[],"preferred":false,"id":829680,"contributorType":{"id":1,"text":"Authors"},"rank":9}]}} ,{"id":70221315,"text":"70221315 - 1967 - Second session occurrence of ground water in different geologic environments","interactions":[],"lastModifiedDate":"2022-11-22T18:03:25.629766","indexId":"70221315","displayToPublicDate":"1967-06-01T13:17:29","publicationYear":"1967","noYear":false,"publicationType":{"id":2,"text":"Article"},"publicationSubtype":{"id":10,"text":"Journal Article"},"seriesTitle":{"id":2126,"text":"JAWRA","active":true,"publicationSubtype":{"id":10}},"title":"Second session occurrence of ground water in different geologic environments","docAbstract":"No abstract available.
","language":"English","publisher":"Wiley","doi":"10.1111/j.1752-1688.1967.tb05879.x","usgsCitation":"McGuinness, C.L., 1967, Second session occurrence of ground water in different geologic environments: JAWRA, v. 3, no. 2, https://doi.org/10.1111/j.1752-1688.1967.tb05879.x.","productDescription":"1 p.","startPage":"3","costCenters":[],"links":[{"id":386361,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/thumbnails/outside_thumb.jpg"}],"volume":"3","issue":"2","noUsgsAuthors":false,"publicationDate":"2007-06-08","publicationStatus":"PW","contributors":{"authors":[{"text":"McGuinness, C. L.","contributorId":20313,"corporation":false,"usgs":true,"family":"McGuinness","given":"C.","email":"","middleInitial":"L.","affiliations":[],"preferred":false,"id":817291,"contributorType":{"id":1,"text":"Authors"},"rank":1}]}} ,{"id":70221312,"text":"70221312 - 1967 - Effects on ground‐water quality and induced infiltration of wastes disposed into the Hocking River at Lancaster, Ohio","interactions":[],"lastModifiedDate":"2021-06-09T17:54:59.74169","indexId":"70221312","displayToPublicDate":"1967-06-01T12:50:42","publicationYear":"1967","noYear":false,"publicationType":{"id":2,"text":"Article"},"publicationSubtype":{"id":10,"text":"Journal Article"},"seriesTitle":{"id":3825,"text":"Groundwater","active":true,"publicationSubtype":{"id":10}},"title":"Effects on ground‐water quality and induced infiltration of wastes disposed into the Hocking River at Lancaster, Ohio","docAbstract":"Watercourse aquifer systems in many areas are adversely affected by wastes disposed into surface‐water sources, resulting in either reduced streambed permeability, infiltration of wastes into the aquifer, or both. These conditions are illustrated at Lancaster, Ohio, where low streambed permeability in the vicinity of the municipal well field, resulting from the discharge of wastes to the Hocking River, seriously retards the infiltration of surface water and lessens the available yield of the wells. The wastes consist of brine and iron‐laden effluent from the municipal treatment plant, discharged within the area of influence of the pumped wells to a stream already carrying much organic waste and other debris. Upstream from the discharge sewer, muck and organic debris have accumulated thickly on the streambed, while downstream from the sewer the streambed sediments have become tightly cemented by iron and other constituents in the waste water. There is evidence that, despite reduced streambed permeability, wastes have entered the aquifer and have materially contributed to declines in well efficiency and to recurring problems of well maintenance. Conditions such as those illustrated at Lancaster occur also at Dayton and are not uncommon elsewhere in Ohio. Indirect contamination of aquifers and adverse physical and chemical alteration of streambed sediments, resulting from surface‐water waste disposal, may in many places pose a threat to the ground‐water supply. This fact should not be overlooked in determining water‐quality standards to be established under the Water Quality Act of 1965.
","language":"English","publisher":"Wiley","doi":"10.1111/j.1745-6584.1967.tb03662.x","usgsCitation":"Norris, S., 1967, Effects on ground‐water quality and induced infiltration of wastes disposed into the Hocking River at Lancaster, Ohio: Groundwater, v. 5, no. 3, p. 15-19, https://doi.org/10.1111/j.1745-6584.1967.tb03662.x.","productDescription":"5 p.","startPage":"15","endPage":"19","costCenters":[],"links":[{"id":386358,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/thumbnails/outside_thumb.jpg"}],"country":"United States","state":"Ohio","city":"Lancaster","geographicExtents":"{\n \"type\": \"FeatureCollection\",\n \"features\": [\n {\n \"type\": \"Feature\",\n \"properties\": {},\n \"geometry\": {\n \"type\": \"Polygon\",\n \"coordinates\": [\n [\n [\n -82.85888671875,\n 39.605688178320804\n ],\n [\n -82.24365234375,\n 39.605688178320804\n ],\n [\n -82.24365234375,\n 39.85072092501597\n ],\n [\n -82.85888671875,\n 39.85072092501597\n ],\n [\n -82.85888671875,\n 39.605688178320804\n ]\n ]\n ]\n }\n }\n ]\n}","volume":"5","issue":"3","noUsgsAuthors":false,"publicationDate":"2006-07-06","publicationStatus":"PW","contributors":{"authors":[{"text":"Norris, S.E.","contributorId":43771,"corporation":false,"usgs":true,"family":"Norris","given":"S.E.","email":"","affiliations":[],"preferred":false,"id":817288,"contributorType":{"id":1,"text":"Authors"},"rank":1}]}} ,{"id":70221306,"text":"70221306 - 1967 - Epifauna of the Patuxent River Estuary, Maryland, for 1963 and 1964","interactions":[],"lastModifiedDate":"2021-06-09T16:38:55.813498","indexId":"70221306","displayToPublicDate":"1967-06-01T11:32:11","publicationYear":"1967","noYear":false,"publicationType":{"id":2,"text":"Article"},"publicationSubtype":{"id":10,"text":"Journal Article"},"seriesTitle":{"id":1228,"text":"Chesapeake Science","active":true,"publicationSubtype":{"id":10}},"title":"Epifauna of the Patuxent River Estuary, Maryland, for 1963 and 1964","docAbstract":"Methods of collection and analysis of epifaunal communities from six stations in the Patuxent estuary are described. The stations were distributed from Solomons near the mouth of the estuary, upstream to Lower Marlboro, near the limit of salt water intrusion. Species composition and abundance, seasons of attachment, and production of the epifaunal community were determined on material collected from panels submerged for 1, 3, and 12 month periods covering the years 1963 and 1964. Salinity was highest downstream, as was the number of species. Salinity decreased rapidly between the Patuxent River Bridge station and Lower Marlboro, where the number of species was reduced to half. Seasons of attachment corresponded with seasonal temperature changes, with the greatest attachment taking place during the summer months. Over 40 species were identified with 7 of them comprising the bulk of the biomass produced. For the 7 most productive species, seasons of attachment and total numbers collected from areas of one square decimeter from monthly and quarterly panels from each station are shown. The seven species were the barnacle Balanus improvisus; the tunicate, Molgula manhattensis; the hydroids, Cordylophora lacustris and Bimeria franciscana; the amphipod, Corophium lacustre; the anemone Sagartia leucolena; the tubeworm, Polydora ligni. Their respective importance varied with seasons of attachment and location. Comments on the distribution and abundance of the less significant forms are included. Dry and ash-free dry weight (organic carbon) production of the epifaunal community varied from month to month depending on the seasons of attachment of the various species. The highest production for a single month was observed at the upriver station, Lower Marlboro, where barnacles and amphipods produced 2,754 g/m2/30 days dry weight and 351 gc/m2/30 days organic weight during August 1963. At the same station, barnacles, amphipods, and hydroids produced, on quarterly panels, the highest yearly average weight of about 1150 gc/m2/yr organic carbon and on monthly panels, about 6,500 g/m2/yr dry weight or about 3.5 times the least organic weight and 8 times the least dry weight produced at the downriver Station, Queentree Landing.
","language":"English","publisher":"Estuarine Research Federation","doi":"10.2307/1351152","usgsCitation":"Cory, R.L., 1967, Epifauna of the Patuxent River Estuary, Maryland, for 1963 and 1964: Chesapeake Science, v. 8, no. 2, p. 71-89, https://doi.org/10.2307/1351152.","productDescription":"19 p.","startPage":"71","endPage":"89","costCenters":[],"links":[{"id":386353,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/thumbnails/outside_thumb.jpg"}],"country":"United States","state":"Maryland","otherGeospatial":"Patuxent River","geographicExtents":"{\n \"type\": \"FeatureCollection\",\n \"features\": [\n {\n \"type\": \"Feature\",\n \"properties\": {},\n \"geometry\": {\n \"type\": \"Polygon\",\n \"coordinates\": [\n [\n [\n -76.80541992187499,\n 38.238180119798635\n ],\n [\n -76.39617919921875,\n 38.238180119798635\n ],\n [\n -76.39617919921875,\n 38.839707613545144\n ],\n [\n -76.80541992187499,\n 38.839707613545144\n ],\n [\n -76.80541992187499,\n 38.238180119798635\n ]\n ]\n ]\n }\n }\n ]\n}","volume":"8","issue":"2","noUsgsAuthors":false,"publicationStatus":"PW","contributors":{"authors":[{"text":"Cory, R. L.","contributorId":49456,"corporation":false,"usgs":true,"family":"Cory","given":"R.","email":"","middleInitial":"L.","affiliations":[],"preferred":false,"id":817282,"contributorType":{"id":1,"text":"Authors"},"rank":1}]}} ,{"id":70221305,"text":"70221305 - 1967 - The fort gouraud, Mauritania, iron ore deposits","interactions":[],"lastModifiedDate":"2021-06-09T16:31:01.592447","indexId":"70221305","displayToPublicDate":"1967-06-01T11:27:26","publicationYear":"1967","noYear":false,"publicationType":{"id":2,"text":"Article"},"publicationSubtype":{"id":10,"text":"Journal Article"},"seriesTitle":{"id":1472,"text":"Economic Geology","active":true,"publicationSubtype":{"id":10}},"title":"The fort gouraud, Mauritania, iron ore deposits","docAbstract":"In connection with a paper by Baldwin and Gross on the localization of residual hematite ore (for reference, see this Bibliography Vol. 31, No. 7, 02 E67-05748), inaccuracies in the citations from the literature used for purposes of comparison are pointed out, particularly those on Brazilian deposits.
Surveyor III landed on the lunar surface at 00:04 GMT, on Day 110 (April 20), 1967, approximately 23 h after local sunrise on the moon. The television camera was turned on about 1 h after touchdown, and 6315 pictures were taken during the remainder of the lunar day. The camera was operated extensively for the first period of lunar visibility from the Goldstone Tracking Station of the Deep Space Network (DSN) and, except on Day 115 (April 25), on each successive Goldstone pass of the moon. During this period, the sun rose from an elevation angle of 11 deg in the east to within 3 deg of the zenith and then sank almost due west of the spacecraft. Many pictures were obtained of the illuminated eastern horizon in the period immediately preceding sunset. In addition to those received at the Goldstone station, some were obtained at the Canberra, Australia, station of the DSN.
No abstract available.
","language":"English","publisher":"New York Academy of Sciences","doi":"10.1111/j.2164-0947.1967.tb02825.x","usgsCitation":"Manheim, F.T., 1967, Evidence for submarine discharge of water on the Atlantic continental slope of the southern United States, and suggestions for further search: Transactions of the New York Academy of Sciences, v. 29, no. 7 , p. 839-853, https://doi.org/10.1111/j.2164-0947.1967.tb02825.x.","productDescription":"15 p.","startPage":"839","endPage":"853","costCenters":[{"id":678,"text":"Woods Hole Coastal and Marine Science Center","active":true,"usgs":true}],"links":[{"id":369631,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/thumbnails/outside_thumb.jpg"}],"volume":"29","issue":"7 ","noUsgsAuthors":false,"publicationDate":"2012-04-30","publicationStatus":"PW","contributors":{"authors":[{"text":"Manheim, Frank T. 0000-0003-4005-4524","orcid":"https://orcid.org/0000-0003-4005-4524","contributorId":20770,"corporation":false,"usgs":true,"family":"Manheim","given":"Frank","email":"","middleInitial":"T.","affiliations":[],"preferred":false,"id":776181,"contributorType":{"id":1,"text":"Authors"},"rank":1}]}} ,{"id":70010514,"text":"70010514 - 1967 - Drilling on Midway Atoll, Hawaii","interactions":[],"lastModifiedDate":"2026-02-09T16:17:52.266746","indexId":"70010514","displayToPublicDate":"1967-05-26T00:00:00","publicationYear":"1967","noYear":false,"publicationType":{"id":2,"text":"Article"},"publicationSubtype":{"id":10,"text":"Journal Article"},"seriesTitle":{"id":3338,"text":"Science","active":true,"publicationSubtype":{"id":10}},"title":"Drilling on Midway Atoll, Hawaii","docAbstract":"Two holes drilled through reef sediments into basalt have established a geologic section through the Miocene. Midway was built above the sea by flows that were weathered and partially truncated in pre-Miocene time. After submergence, volcanic clays were reworked and covered by limestones. Overall submergence was interrupted at least twice by emergence. The limestones have been leached, recrystallized, and partially dolomitized.","language":"English","publisher":"American Association for the Advancement of Science","doi":"10.1126/science.156.3778.1088","issn":"00368075","usgsCitation":"Ladd, H.S., Tracey, J.I., and Gross, M., 1967, Drilling on Midway Atoll, Hawaii: Science, v. 156, no. 3778, p. 1088-1094, https://doi.org/10.1126/science.156.3778.1088.","productDescription":"7 p.","startPage":"1088","endPage":"1094","costCenters":[],"links":[{"id":219532,"rank":1,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.er.usgs.gov/thumbnails/outside_thumb.jpg"}],"country":"United States","state":"Hawaii","otherGeospatial":"Midway Atoll","geographicExtents":"{\n \"type\": \"FeatureCollection\",\n \"features\": [\n {\n \"type\": \"Feature\",\n \"properties\": {},\n \"geometry\": {\n \"coordinates\": [\n [\n [\n -177.51465541350169,\n 28.331446284943723\n ],\n [\n -177.51465541350169,\n 28.098797965871157\n ],\n [\n -177.17362991676313,\n 28.098797965871157\n ],\n [\n -177.17362991676313,\n 28.331446284943723\n ],\n [\n -177.51465541350169,\n 28.331446284943723\n ]\n ]\n ],\n \"type\": \"Polygon\"\n }\n }\n ]\n}","volume":"156","issue":"3778","noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"505a03e9e4b0c8380cd506d2","contributors":{"authors":[{"text":"Ladd, H. S.","contributorId":95537,"corporation":false,"usgs":true,"family":"Ladd","given":"H.","email":"","middleInitial":"S.","affiliations":[],"preferred":false,"id":359094,"contributorType":{"id":1,"text":"Authors"},"rank":1},{"text":"Tracey, J. I. Jr.","contributorId":17205,"corporation":false,"usgs":true,"family":"Tracey","given":"J.","suffix":"Jr.","email":"","middleInitial":"I.","affiliations":[],"preferred":false,"id":359092,"contributorType":{"id":1,"text":"Authors"},"rank":2},{"text":"Gross, M.G.","contributorId":33047,"corporation":false,"usgs":true,"family":"Gross","given":"M.G.","email":"","affiliations":[],"preferred":false,"id":359093,"contributorType":{"id":1,"text":"Authors"},"rank":3}]}} ,{"id":70011492,"text":"70011492 - 1967 - Slopes on the moon","interactions":[],"lastModifiedDate":"2026-02-09T16:21:55.365904","indexId":"70011492","displayToPublicDate":"1967-05-26T00:00:00","publicationYear":"1967","noYear":false,"publicationType":{"id":2,"text":"Article"},"publicationSubtype":{"id":10,"text":"Journal Article"},"seriesTitle":{"id":3338,"text":"Science","active":true,"publicationSubtype":{"id":10}},"title":"Slopes on the moon","docAbstract":"No abstract available.
","language":"English","publisher":"American Association for the Advancement of Science","doi":"10.1126/science.156.3778.1135.a","issn":"00368075","usgsCitation":"Milton, D., 1967, Slopes on the moon: Science, v. 156, no. 3778, p. 1135-1135, https://doi.org/10.1126/science.156.3778.1135.a.","productDescription":"1 p.","startPage":"1135","endPage":"1135","costCenters":[],"links":[{"id":221049,"rank":1,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/thumbnails/outside_thumb.jpg"}],"otherGeospatial":"Moon","volume":"156","issue":"3778","noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"505b916fe4b08c986b3198d2","contributors":{"authors":[{"text":"Milton, D.J.","contributorId":44121,"corporation":false,"usgs":true,"family":"Milton","given":"D.J.","email":"","affiliations":[],"preferred":false,"id":361248,"contributorType":{"id":1,"text":"Authors"},"rank":1}]}} ,{"id":1007579,"text":"1007579 - 1967 - New records of mammals from Mesa Verde National Park, Colorado","interactions":[],"lastModifiedDate":"2025-03-07T17:09:38.494659","indexId":"1007579","displayToPublicDate":"1967-05-20T00:00:00","publicationYear":"1967","noYear":false,"publicationType":{"id":2,"text":"Article"},"publicationSubtype":{"id":10,"text":"Journal Article"},"seriesTitle":{"id":2373,"text":"Journal of Mammalogy","onlineIssn":"1545-1542","printIssn":"0022-2372","active":true,"publicationSubtype":{"id":10}},"title":"New records of mammals from Mesa Verde National Park, Colorado","docAbstract":"No abstract available.
","language":"English","publisher":"Oxford Academic","doi":"10.2307/1378045","usgsCitation":"Douglas, C.L., 1967, New records of mammals from Mesa Verde National Park, Colorado: Journal of Mammalogy, v. 48, no. 2, p. 322-323, https://doi.org/10.2307/1378045.","productDescription":"2 p.","startPage":"322","endPage":"323","costCenters":[{"id":651,"text":"Western Ecological Research Center","active":true,"usgs":true}],"links":[{"id":130199,"rank":1,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/thumbnails/outside_thumb.jpg"}],"country":"United States","state":"Colorado","otherGeospatial":"Mesa Verde National Park","geographicExtents":"{\n \"type\": \"FeatureCollection\",\n \"features\": [\n {\n \"type\": \"Feature\",\n \"properties\": {},\n \"geometry\": {\n \"coordinates\": [\n [\n [\n -108.57006634732126,\n 37.336930106550284\n ],\n [\n -108.57006634732126,\n 37.1543508614925\n ],\n [\n -108.35069808089543,\n 37.1543508614925\n ],\n [\n -108.35069808089543,\n 37.336930106550284\n ],\n [\n -108.57006634732126,\n 37.336930106550284\n ]\n ]\n ],\n \"type\": \"Polygon\"\n }\n }\n ]\n}","volume":"48","issue":"2","noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"4f4e4afee4b07f02db697594","contributors":{"authors":[{"text":"Douglas, Charles L.","contributorId":10742,"corporation":false,"usgs":true,"family":"Douglas","given":"Charles","email":"","middleInitial":"L.","affiliations":[],"preferred":false,"id":315659,"contributorType":{"id":1,"text":"Authors"},"rank":1}]}} ,{"id":70010484,"text":"70010484 - 1967 - Geochemical evidence of present-day serpentinization","interactions":[],"lastModifiedDate":"2026-02-09T16:33:24.542339","indexId":"70010484","displayToPublicDate":"1967-05-12T00:00:00","publicationYear":"1967","noYear":false,"publicationType":{"id":2,"text":"Article"},"publicationSubtype":{"id":10,"text":"Journal Article"},"seriesTitle":{"id":3338,"text":"Science","active":true,"publicationSubtype":{"id":10}},"title":"Geochemical evidence of present-day serpentinization","docAbstract":"Ultrabasic (pH > 11) water issues from some fresh ultramafic bodies. The properties of the ultrabasic solutions are believed to be due to current reactions yielding serpentine from primary olivines and pyroxenes. The low concentrations of divalent iron. divalent magnesium, and dissolved silica from the serpentinization require an increase in rock volume.
","language":"English","publisher":"American Association for the Advancement of Science","doi":"10.1126/science.156.3776.830","issn":"00368075","usgsCitation":"Barnes, I., LaMarche, V.C., and Himmelberg, G., 1967, Geochemical evidence of present-day serpentinization: Science, v. 156, no. 3776, p. 830-832, https://doi.org/10.1126/science.156.3776.830.","productDescription":"3 p.","startPage":"830","endPage":"832","costCenters":[],"links":[{"id":219239,"rank":1,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/thumbnails/outside_thumb.jpg"}],"volume":"156","issue":"3776","noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"505a1634e4b0c8380cd550b3","contributors":{"authors":[{"text":"Barnes, I.","contributorId":23678,"corporation":false,"usgs":true,"family":"Barnes","given":"I.","affiliations":[],"preferred":false,"id":359028,"contributorType":{"id":1,"text":"Authors"},"rank":1},{"text":"LaMarche, Valmore C. Jr.","contributorId":101719,"corporation":false,"usgs":true,"family":"LaMarche","given":"Valmore","suffix":"Jr.","email":"","middleInitial":"C.","affiliations":[],"preferred":false,"id":359030,"contributorType":{"id":1,"text":"Authors"},"rank":2},{"text":"Himmelberg, G.","contributorId":29565,"corporation":false,"usgs":true,"family":"Himmelberg","given":"G.","affiliations":[],"preferred":false,"id":359029,"contributorType":{"id":1,"text":"Authors"},"rank":3}]}} ,{"id":70011561,"text":"70011561 - 1967 - Cliftonite in meteorites: A proposed origin","interactions":[],"lastModifiedDate":"2026-02-09T16:25:43.511339","indexId":"70011561","displayToPublicDate":"1967-05-12T00:00:00","publicationYear":"1967","noYear":false,"publicationType":{"id":2,"text":"Article"},"publicationSubtype":{"id":10,"text":"Journal Article"},"seriesTitle":{"id":3338,"text":"Science","active":true,"publicationSubtype":{"id":10}},"title":"Cliftonite in meteorites: A proposed origin","docAbstract":"Cliftonite, a polycrystalline aggregate of graphite with cubic morphology, is known in ten meteorites. Some workers have considered it to be a pseudomorph after diamond, and have used the proposed diamond ancestry as evidence of a meteoritic parent body of at least lunar dimensions. We have synthesized cliftonite in Fe-Ni-C alloys in vacuum, as a product of decomposition of cohenite [(Fe,Ni)3C]. We therefore suggest that a high pressure origin is unnecessary for meteorites which contain cliftonite, and that these meteorites were formed at low pressures. This conclusion is in agreement with other recent evidence.
","language":"English","publisher":"American Association for the Advancement of Science","doi":"10.1126/science.156.3776.819","issn":"00368075","usgsCitation":"Brett, R., and Higgins, G., 1967, Cliftonite in meteorites: A proposed origin: Science, v. 156, no. 3776, p. 819-820, https://doi.org/10.1126/science.156.3776.819.","productDescription":"2 p.","startPage":"819","endPage":"820","costCenters":[],"links":[{"id":221181,"rank":1,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/thumbnails/outside_thumb.jpg"}],"volume":"156","issue":"3776","noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"5059f645e4b0c8380cd4c65d","contributors":{"authors":[{"text":"Brett, R.","contributorId":106632,"corporation":false,"usgs":true,"family":"Brett","given":"R.","email":"","affiliations":[],"preferred":false,"id":361409,"contributorType":{"id":1,"text":"Authors"},"rank":1},{"text":"Higgins, G.T.","contributorId":52971,"corporation":false,"usgs":true,"family":"Higgins","given":"G.T.","email":"","affiliations":[],"preferred":false,"id":361408,"contributorType":{"id":1,"text":"Authors"},"rank":2}]}} ,{"id":1001559,"text":"1001559 - 1967 - Swimming by a badger","interactions":[],"lastModifiedDate":"2025-03-07T16:58:12.462536","indexId":"1001559","displayToPublicDate":"1967-05-05T00:00:00","publicationYear":"1967","noYear":false,"publicationType":{"id":2,"text":"Article"},"publicationSubtype":{"id":10,"text":"Journal Article"},"seriesTitle":{"id":2373,"text":"Journal of Mammalogy","onlineIssn":"1545-1542","printIssn":"0022-2372","active":true,"publicationSubtype":{"id":10}},"title":"Swimming by a badger","docAbstract":"Abstract not available.
","language":"English","publisher":"Oxford Academic","doi":"10.2307/1378046","usgsCitation":"Duebbert, H., 1967, Swimming by a badger: Journal of Mammalogy, v. 48, no. 2, p. 323-323, https://doi.org/10.2307/1378046.","productDescription":"1 p.","startPage":"323","endPage":"323","costCenters":[{"id":480,"text":"Northern Prairie Wildlife Research Center","active":true,"usgs":true}],"links":[{"id":130613,"rank":1,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/thumbnails/outside_thumb.jpg"}],"volume":"48","issue":"2","noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"4f4e4affe4b07f02db697d5d","contributors":{"authors":[{"text":"Duebbert, Harold F.","contributorId":11544,"corporation":false,"usgs":true,"family":"Duebbert","given":"Harold F.","affiliations":[],"preferred":false,"id":311249,"contributorType":{"id":1,"text":"Authors"},"rank":1}]}} ,{"id":5223205,"text":"5223205 - 1967 - The Peromyscus guardia-interparietalis complex","interactions":[],"lastModifiedDate":"2025-03-07T17:03:57.634306","indexId":"5223205","displayToPublicDate":"1967-05-05T00:00:00","publicationYear":"1967","noYear":false,"publicationType":{"id":2,"text":"Article"},"publicationSubtype":{"id":10,"text":"Journal Article"},"seriesTitle":{"id":2373,"text":"Journal of Mammalogy","onlineIssn":"1545-1542","printIssn":"0022-2372","active":true,"publicationSubtype":{"id":10}},"title":"The Peromyscus guardia-interparietalis complex","docAbstract":"Peromyscus interparietalis is considered to be specifically distinct from P. guardia, of which it was originally considered a subspecies. Each species includes three subspecifically distinct populations, each endemic to an island in the northern Gulf of California, Baja California, Mexico. Two subspecies of P. interparietalis and one of P. guardia are newly described here. The mice are widespread on the islands, apparently favoring no particular microhabitat. Reproduction takes place in early spring.
","language":"English","publisher":"Oxford Academic","doi":"10.2307/1378023","usgsCitation":"Banks, R.C., 1967, The Peromyscus guardia-interparietalis complex: Journal of Mammalogy, v. 48, no. 2, p. 210-218, https://doi.org/10.2307/1378023.","productDescription":"9 p.","startPage":"210","endPage":"218","costCenters":[{"id":531,"text":"Patuxent Wildlife Research Center","active":true,"usgs":true}],"links":[{"id":200118,"rank":1,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/thumbnails/outside_thumb.jpg"}],"country":"Mexico","otherGeospatial":"Gulf of California","geographicExtents":"{\n \"type\": \"FeatureCollection\",\n \"features\": [\n {\n \"type\": \"Feature\",\n \"properties\": {},\n \"geometry\": {\n \"coordinates\": [\n [\n [\n -115.41579354571462,\n 31.889379597866537\n ],\n [\n -115.41579354571462,\n 28.688859536547625\n ],\n [\n -112.12904081522305,\n 28.688859536547625\n ],\n [\n -112.12904081522305,\n 31.889379597866537\n ],\n [\n -115.41579354571462,\n 31.889379597866537\n ]\n ]\n ],\n \"type\": \"Polygon\"\n }\n }\n ]\n}","volume":"48","issue":"2","noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"4f4e4ac7e4b07f02db67ae3e","contributors":{"authors":[{"text":"Banks, Richard C.","contributorId":102933,"corporation":false,"usgs":true,"family":"Banks","given":"Richard","email":"","middleInitial":"C.","affiliations":[],"preferred":false,"id":338120,"contributorType":{"id":1,"text":"Authors"},"rank":1}]}} ]}