{"pageNumber":"6369","pageRowStart":"159200","pageSize":"25","recordCount":184689,"records":[{"id":70227354,"text":"70227354 - 1971 - Tectonics of the Mendocino triple junction","interactions":[],"lastModifiedDate":"2022-01-10T23:11:46.320538","indexId":"70227354","displayToPublicDate":"1971-11-01T17:03:40","publicationYear":"1971","noYear":false,"publicationType":{"id":2,"text":"Article"},"publicationSubtype":{"id":10,"text":"Journal Article"},"seriesTitle":{"id":5935,"text":"Bulletin of the Geological Society of America","active":true,"publicationSubtype":{"id":10}},"title":"Tectonics of the Mendocino triple junction","docAbstract":"

Interpretation of reflection profiles and of the magnetic anomaly pattern over the Gorda Basin and Escarpment gives broad agreement with the triple junction model of McKenzie and Morgan (1969). However, the basin has undergone internal deformation, a local departure from rigid plate tectonics, and the escarpment has had a component of underthrusting by the Gorda block. Faults in the Gorda Basin which disturb young turbidites parallel the trends of magnetic anomalies, suggesting deformation of the oceanic crust along lines of primary weakness. The northeast trends of the faults give a constraint on first-motion solutions for earthquakes within the basin and suggest left-lateral slip on the faults. Analysis of the geometry and timing of the Gorda Basin deformation based on the magnetic pattern gives an average gross tectonic strain rate of 10−14/sec. These observations give a measure of the mechanics of deformation of oceanic lithosphere very close to a spreading rise crest.

","language":"English","publisher":"Geological Society of America","doi":"10.1130/0016-7606(1971)82[2965:TOTMTJ]2.0.CO;2","usgsCitation":"Silver, E.A., 1971, Tectonics of the Mendocino triple junction: Bulletin of the Geological Society of America, v. 82, no. 11, p. 2965-2977, https://doi.org/10.1130/0016-7606(1971)82[2965:TOTMTJ]2.0.CO;2.","productDescription":"13 p.","startPage":"2965","endPage":"2977","costCenters":[],"links":[{"id":394164,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/thumbnails/outside_thumb.jpg"}],"country":"United States","state":"California, Oregon","otherGeospatial":"Mendocino fault, Mendocino junction, San Andreas fault","geographicExtents":"{\n \"type\": \"FeatureCollection\",\n \"features\": [\n {\n \"type\": \"Feature\",\n \"properties\": {},\n \"geometry\": {\n \"type\": \"Polygon\",\n \"coordinates\": [\n [\n [\n -132.451171875,\n 38.91668153637508\n ],\n [\n -123.387451171875,\n 38.91668153637508\n ],\n [\n -123.387451171875,\n 44.53567453241317\n ],\n [\n -132.451171875,\n 44.53567453241317\n ],\n [\n -132.451171875,\n 38.91668153637508\n ]\n ]\n ]\n }\n }\n ]\n}","volume":"82","issue":"11","noUsgsAuthors":false,"publicationStatus":"PW","contributors":{"authors":[{"text":"Silver, Eli A.","contributorId":83505,"corporation":false,"usgs":true,"family":"Silver","given":"Eli","email":"","middleInitial":"A.","affiliations":[],"preferred":false,"id":830551,"contributorType":{"id":1,"text":"Authors"},"rank":1}]}} ,{"id":70227351,"text":"70227351 - 1971 - Age of the Mesozoic oceanic crust in the California Coast Ranges","interactions":[],"lastModifiedDate":"2022-01-10T22:39:22.830265","indexId":"70227351","displayToPublicDate":"1971-11-01T16:26:20","publicationYear":"1971","noYear":false,"publicationType":{"id":2,"text":"Article"},"publicationSubtype":{"id":10,"text":"Journal Article"},"seriesTitle":{"id":5935,"text":"Bulletin of the Geological Society of America","active":true,"publicationSubtype":{"id":10}},"title":"Age of the Mesozoic oceanic crust in the California Coast Ranges","docAbstract":"

K-Ar ages of approximately 155 m.y. were measured on minerals from ophiolites at two localities in the California Coast Ranges. Upper Jurassic rocks of the Great Valley sequence are in depositional contact with underlying ophiolites, which are interpreted as Mesozoic oceanic crust that formed during differentiation of mantle material at a spreading ridge some 15 m.y. before deposition of the Great Valley sequence began.

","language":"English","publisher":"Geological Society of America","doi":"10.1130/0016-7606(1971)82[3209:AOTMOC]2.0.CO;2","usgsCitation":"Lanphere, M.A., 1971, Age of the Mesozoic oceanic crust in the California Coast Ranges: Bulletin of the Geological Society of America, v. 82, no. 11, p. 3209-3211, https://doi.org/10.1130/0016-7606(1971)82[3209:AOTMOC]2.0.CO;2.","productDescription":"3 p.","startPage":"3209","endPage":"3211","costCenters":[],"links":[{"id":394160,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/thumbnails/outside_thumb.jpg"}],"country":"United States","state":"California","otherGeospatial":"Coast Ranges","geographicExtents":"{\n \"type\": \"FeatureCollection\",\n \"features\": [\n {\n \"type\": \"Feature\",\n \"properties\": {},\n \"geometry\": {\n \"type\": \"Polygon\",\n \"coordinates\": [\n [\n [\n -120.355224609375,\n 34.786739162702524\n ],\n [\n -119.70703125,\n 34.542762387234845\n ],\n [\n -119.06982421874999,\n 34.34343606848294\n ],\n [\n -118.66333007812499,\n 34.379712580462204\n ],\n [\n -118.564453125,\n 34.56085936708384\n ],\n [\n -118.95996093749999,\n 35.146862906756304\n ],\n [\n -119.33349609375,\n 35.137879119634185\n ],\n [\n -119.90478515625,\n 35.594785665487244\n ],\n [\n -120.377197265625,\n 36.56260003738545\n ],\n [\n -120.87158203125,\n 37.17782559332976\n ],\n [\n -121.66259765625001,\n 37.94419750075404\n ],\n [\n -122.135009765625,\n 38.89958342598271\n ],\n [\n -122.29980468749999,\n 39.223742741391305\n ],\n [\n -122.56347656249999,\n 40.22921818870117\n ],\n [\n -122.6953125,\n 40.38002840251183\n ],\n [\n -123.33251953125,\n 40.697299008636755\n ],\n [\n -124.178466796875,\n 40.83874913796459\n ],\n [\n -124.43115234375,\n 40.57224011776902\n ],\n [\n -124.43115234375,\n 40.27952566881291\n ],\n [\n -124.01367187499999,\n 39.95185892663005\n ],\n [\n -123.72802734375,\n 39.51251701659638\n ],\n [\n -123.89282226562501,\n 39.30029918615029\n ],\n [\n -123.77197265625,\n 38.94232097947902\n ],\n [\n -123.167724609375,\n 38.47939467327645\n ],\n [\n -123.06884765625,\n 37.92686760148135\n ],\n [\n -122.6513671875,\n 37.79676317682161\n ],\n [\n -122.54150390625,\n 37.23032838760387\n ],\n [\n -122.33276367187499,\n 36.99377838872517\n ],\n [\n -121.904296875,\n 36.88840804313823\n ],\n [\n -121.9482421875,\n 36.712467243386264\n ],\n [\n -122.08007812499999,\n 36.63316209558658\n ],\n [\n -122.025146484375,\n 36.28856319836237\n ],\n [\n -121.28906250000001,\n 35.523285179107816\n ],\n [\n -120.355224609375,\n 34.786739162702524\n ]\n ]\n ]\n }\n }\n ]\n}","volume":"82","issue":"11","noUsgsAuthors":false,"publicationStatus":"PW","contributors":{"authors":[{"text":"Lanphere, Marvin A. alder@usgs.gov","contributorId":2696,"corporation":false,"usgs":true,"family":"Lanphere","given":"Marvin","email":"alder@usgs.gov","middleInitial":"A.","affiliations":[],"preferred":true,"id":830548,"contributorType":{"id":1,"text":"Authors"},"rank":1}]}} ,{"id":70120915,"text":"70120915 - 1971 - Interstitial water studies on small core samples, Deep Sea Drilling Project, Leg 8","interactions":[],"lastModifiedDate":"2019-12-16T14:44:01","indexId":"70120915","displayToPublicDate":"1971-11-01T13:15:15","publicationYear":"1971","noYear":false,"publicationType":{"id":2,"text":"Article"},"publicationSubtype":{"id":10,"text":"Journal Article"},"seriesTitle":{"id":1997,"text":"Initial reports of the Deep Sea Drilling Project","active":true,"publicationSubtype":{"id":10}},"title":"Interstitial water studies on small core samples, Deep Sea Drilling Project, Leg 8","docAbstract":"

Leg 8 sites are dominated by siliceous-calcareous biogenic oozes having depositional rates of 0.1 to 1.5 cm/1000 years. Conservative constituents of pore fluids showed, as have cores from other pelagic areas of the Pacific, insignificant or marginally significant changes with depth and location. However, in Sites 70 and 71, calcium, magnesium and strontium showed major shifts in concentration with depth. These changes appear to be related to recrystallization phenomena in skeletal debris of nannoplankton and to the relative accumulation rate of the sediments.

\n
\n

The chemical anomalies increase relatively smoothly with depth, demonstrating the effectiveness of vertical diffusional communication, and apparent lack of bulk fluid movement, as noted in Leg 7 and other sites.

","language":"English","publisher":"Integrated Ocean Drilling Program Management International","publisherLocation":"College Station, TX","doi":"10.2973/dsdp.proc.8.121.1971","usgsCitation":"Manheim, F., and Sayles, F., 1971, Interstitial water studies on small core samples, Deep Sea Drilling Project, Leg 8: Initial reports of the Deep Sea Drilling Project, v. 8, p. 857-869, https://doi.org/10.2973/dsdp.proc.8.121.1971.","productDescription":"13 p.","startPage":"857","endPage":"869","costCenters":[{"id":186,"text":"Coastal and Marine Geology Program","active":true,"usgs":true},{"id":678,"text":"Woods Hole Coastal and Marine Science Center","active":true,"usgs":true}],"links":[{"id":488231,"rank":0,"type":{"id":40,"text":"Open Access Publisher Index Page"},"url":"http://doi.org/10.2973/dsdp.proc.8.121.1971","text":"Publisher Index Page"},{"id":292461,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/thumbnails/outside_thumb.jpg"}],"otherGeospatial":"Pacific Ocean","geographicExtents":"{ \"type\": \"FeatureCollection\", \"features\": [ { \"type\": \"Feature\", \"properties\": {}, \"geometry\": { \"type\": \"Polygon\", \"coordinates\": [ [ [ -170.0,-20.0 ], [ -170.0,25.0 ], [ -130.0,25.0 ], [ -130.0,-20.0 ], [ -170.0,-20.0 ] ] ] } } ] }","volume":"8","noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"53f25fe7e4b033341871892e","contributors":{"authors":[{"text":"Manheim, F.T. 0000-0003-4005-4524","orcid":"https://orcid.org/0000-0003-4005-4524","contributorId":55421,"corporation":false,"usgs":true,"family":"Manheim","given":"F.T.","affiliations":[],"preferred":false,"id":498609,"contributorType":{"id":1,"text":"Authors"},"rank":1},{"text":"Sayles, F.L.","contributorId":77657,"corporation":false,"usgs":true,"family":"Sayles","given":"F.L.","email":"","affiliations":[],"preferred":false,"id":498610,"contributorType":{"id":1,"text":"Authors"},"rank":2}]}} ,{"id":70227134,"text":"70227134 - 1971 - Mobility of uranium and thorium in glassy and crystallized silicic volcanic rocks","interactions":[],"lastModifiedDate":"2021-12-30T18:09:39.304688","indexId":"70227134","displayToPublicDate":"1971-11-01T11:31:43","publicationYear":"1971","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":"Mobility of uranium and thorium in glassy and crystallized silicic volcanic rocks","docAbstract":"

No abstract available.

","language":"English","publisher":"Society of Economic Geologists","doi":"10.2113/gsecongeo.66.7.1061","usgsCitation":"Rosholt, J.N., , P., and Noble, D.C., 1971, Mobility of uranium and thorium in glassy and crystallized silicic volcanic rocks: Economic Geology, v. 66, no. 7, p. 1061-1069, https://doi.org/10.2113/gsecongeo.66.7.1061.","productDescription":"9 p.","startPage":"1061","endPage":"1069","costCenters":[],"links":[{"id":393660,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/thumbnails/outside_thumb.jpg"}],"country":"United States","state":"California, Colorado, Nebraska, Nevada, New Mexico, Wyoming","otherGeospatial":"Belted Range, Cougar Creek, Glass Mountain, Grassy Lake Reservoir, Kane Springs Wash caldera, Little Glass Mountain, Mono Crater, Muller Island, Ruby Mountain, Sappa formation, Saucer Mesa, Shirley Basin, Shoshone Mountain, Soldier Meadow, Thirsty Canyon, Valles Caldera","geographicExtents":"{\n \"type\": \"FeatureCollection\",\n \"features\": 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]\n}","volume":"66","issue":"7","noUsgsAuthors":false,"publicationDate":"1971-11-01","publicationStatus":"PW","contributors":{"authors":[{"text":"Rosholt, J. N.","contributorId":11325,"corporation":false,"usgs":true,"family":"Rosholt","given":"J.","email":"","middleInitial":"N.","affiliations":[],"preferred":false,"id":829754,"contributorType":{"id":1,"text":"Authors"},"rank":1},{"text":" Prijana","contributorId":270684,"corporation":false,"usgs":false,"given":"Prijana","email":"","affiliations":[],"preferred":false,"id":829755,"contributorType":{"id":1,"text":"Authors"},"rank":2},{"text":"Noble, Donald C.","contributorId":64676,"corporation":false,"usgs":true,"family":"Noble","given":"Donald","email":"","middleInitial":"C.","affiliations":[],"preferred":false,"id":829756,"contributorType":{"id":1,"text":"Authors"},"rank":3}]}} ,{"id":70227133,"text":"70227133 - 1971 - Precision and detection limits of certain minor and trace elements in silicates by electron microprobe analysis","interactions":[],"lastModifiedDate":"2021-12-30T17:27:47.232956","indexId":"70227133","displayToPublicDate":"1971-11-01T11:23:23","publicationYear":"1971","noYear":false,"publicationType":{"id":2,"text":"Article"},"publicationSubtype":{"id":10,"text":"Journal Article"},"seriesTitle":{"id":761,"text":"Analytical Chemistry","active":true,"publicationSubtype":{"id":10}},"title":"Precision and detection limits of certain minor and trace elements in silicates by electron microprobe analysis","docAbstract":"

No abstract available.

","language":"English","publisher":"American Chemical Society","doi":"10.1021/ac60307a033","usgsCitation":"Heidel, R.H., 1971, Precision and detection limits of certain minor and trace elements in silicates by electron microprobe analysis: Analytical Chemistry, v. 43, no. 13, p. 1907-1908, https://doi.org/10.1021/ac60307a033.","productDescription":"2 p.","startPage":"1907","endPage":"1908","costCenters":[],"links":[{"id":393659,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/thumbnails/outside_thumb.jpg"}],"volume":"43","issue":"13","noUsgsAuthors":false,"publicationDate":"2002-05-01","publicationStatus":"PW","contributors":{"authors":[{"text":"Heidel, Robert H.","contributorId":77647,"corporation":false,"usgs":true,"family":"Heidel","given":"Robert","email":"","middleInitial":"H.","affiliations":[],"preferred":false,"id":829753,"contributorType":{"id":1,"text":"Authors"},"rank":1}]}} ,{"id":70227431,"text":"70227431 - 1971 - Effects of karst features on circulation of water in carbonate rocks in coastal areas","interactions":[],"lastModifiedDate":"2022-01-14T17:11:28.34317","indexId":"70227431","displayToPublicDate":"1971-11-01T10:59:39","publicationYear":"1971","noYear":false,"publicationType":{"id":2,"text":"Article"},"publicationSubtype":{"id":10,"text":"Journal Article"},"seriesTitle":{"id":2342,"text":"Journal of Hydrology","active":true,"publicationSubtype":{"id":10}},"title":"Effects of karst features on circulation of water in carbonate rocks in coastal areas","docAbstract":"

The normal balance between fresh water in coastal aquifers and sea water applies also to carbonate-rock aquifers that have been karstified, but there are local modifications in the balance that need to be considered. Uneven distribution of permeability, expressed by a network of solution channels bounded by relatively impermeabler rock, causes an uneven distribution of head of the environmental water along the seacoast. Where sinkholes and (or) vertical solution shafts below sea level penetrate the aquifer, the fresh ground water may discharge through these karst features if the fresh-water head is greater than that of the salt water. However, under some conditions the salt-water head may exceed that of the fresh water, and the direction of movement is reversed as sea water flows into the aquifer. This sea-water flow into the aquifer occurs (1) where sinkholes, acting as “cased wells,” penetrate less permeable rock before reaching a lateral solution channel and (2) where (or when) the fresh-water head is less than that required to balance the salt water. On Andros Island, Bahamas, the range in tide (as much as 5 feet) from low tide to high tide is sufficient to cause such a reversal locally. During low tide the salt-water head becomes sufficiently low that the ground-water head exceeds that of the sea water, and the ground water flows through the sinkholes to the ocean floor; during high tide sea water flows in the sinkholes. In the Adriatic Sea along the coast of Yugoslavia, apparently the fresh-water head is sufficient to produce perennial springs in some localities, but in other areas, as in the Bay of Kastela near Split, the fresh-water head becomes low enough during some seasons that the flow is reversed and salt water enters the aquifer through the karst features.

The development of sinkholes and other karst features near the present coast and extending below sea level occurred generally during a low stand of the Pleistocene sea when the top of the saturated zone stood lower than the bottom of the deepest sinkholes or natural wells.

Integrated evaluations of (1) the distribution of permeability in coastal karst regions and (2) the principles relating to the dynamic balance between fresh aquifer water and sea water are leading to better knowledge of methods that may salvage much karst water which is lost to the sea.

","language":"English","publisher":"Elsevier","doi":"10.1016/0022-1694(71)90003-5","usgsCitation":"Stringfield, V.T., and LeGrand, H.E., 1971, Effects of karst features on circulation of water in carbonate rocks in coastal areas: Journal of Hydrology, v. 14, no. 2, p. 139-157, https://doi.org/10.1016/0022-1694(71)90003-5.","productDescription":"19 p.","startPage":"139","endPage":"157","costCenters":[],"links":[{"id":394394,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/thumbnails/outside_thumb.jpg"}],"country":"The Bahamas, Croatia","city":"Split","otherGeospatial":"Adriatic Sea, Andros Island, Yugoslavia","geographicExtents":"{\n \"type\": \"FeatureCollection\",\n \"features\": [\n {\n \"type\": \"Feature\",\n \"properties\": {},\n \"geometry\": {\n \"type\": \"Polygon\",\n \"coordinates\": [\n [\n [\n -77.5634765625,\n 23.717468136962662\n ],\n [\n -77.4920654296875,\n 23.85067404608915\n ],\n [\n -77.50030517578125,\n 23.92099179936676\n ],\n [\n -77.54150390625,\n 24.13171516246295\n ],\n [\n -77.57720947265624,\n 24.20939467509706\n ],\n [\n -77.6129150390625,\n 24.246964554300924\n ],\n [\n -77.6568603515625,\n 24.259485382998978\n ],\n [\n -77.69805908203125,\n 24.42214378185897\n ],\n [\n -77.7117919921875,\n 24.529633541314364\n ],\n [\n -77.73101806640625,\n 24.542126388899305\n ],\n [\n -77.74200439453125,\n 24.60956626326091\n ],\n [\n -77.7227783203125,\n 24.65450599548674\n ],\n [\n -77.75299072265625,\n 24.701924833689933\n ],\n [\n -77.783203125,\n 24.749325626697196\n ],\n [\n -77.8765869140625,\n 24.844072974931866\n ],\n [\n -77.92877197265625,\n 24.928785481052262\n ],\n [\n -77.947998046875,\n 24.996015742094006\n ],\n [\n -77.98370361328125,\n 24.98107885823501\n ],\n [\n -77.94525146484375,\n 25.08311136003093\n ],\n [\n -77.969970703125,\n 25.098035823821835\n ],\n [\n -78.00018310546875,\n 25.095548539604252\n ],\n [\n -77.9644775390625,\n 25.145284610685064\n ],\n [\n -78.01391601562499,\n 25.19002975536265\n ],\n [\n -78.046875,\n 25.207426209065783\n ],\n [\n -78.10455322265625,\n 25.162687451233257\n ],\n [\n -78.13751220703125,\n 25.19002975536265\n ],\n [\n -78.23638916015625,\n 25.19002975536265\n ],\n [\n -78.189697265625,\n 25.05076877966861\n ],\n [\n -78.189697265625,\n 24.98107885823501\n ],\n [\n -78.21441650390625,\n 24.948709386318527\n ],\n [\n -78.19244384765625,\n 24.90885835502671\n ],\n [\n -78.27484130859375,\n 24.82911768116273\n ],\n [\n -78.4149169921875,\n 24.67946552658519\n ],\n [\n -78.46710205078125,\n 24.69443884773434\n ],\n [\n -78.55499267578125,\n 24.674474019870782\n ],\n [\n -78.4698486328125,\n 24.58958786341259\n ],\n [\n -78.23638916015625,\n 24.42214378185897\n ],\n [\n -78.1512451171875,\n 24.36210962726063\n ],\n [\n -78.11553955078124,\n 24.352101162808903\n ],\n [\n -78.057861328125,\n 24.23694700391751\n ],\n [\n -77.9754638671875,\n 24.12920858513251\n ],\n [\n -77.92877197265625,\n 24.06151244228103\n ],\n [\n -77.85186767578125,\n 23.998798966043488\n ],\n [\n -77.82989501953125,\n 23.87579191610102\n ],\n [\n -77.87384033203124,\n 23.747639913652666\n ],\n [\n -77.72003173828125,\n 23.659619388708066\n ],\n [\n -77.5634765625,\n 23.717468136962662\n ]\n ]\n ]\n }\n },\n {\n \"type\": \"Feature\",\n \"properties\": {},\n \"geometry\": {\n \"type\": \"Polygon\",\n \"coordinates\": [\n [\n [\n 15.776367187499998,\n 42.53689200787315\n ],\n [\n 17.3199462890625,\n 42.53689200787315\n ],\n [\n 17.3199462890625,\n 43.723474896114794\n ],\n [\n 15.776367187499998,\n 43.723474896114794\n ],\n [\n 15.776367187499998,\n 42.53689200787315\n ]\n ]\n ]\n }\n }\n ]\n}","volume":"14","issue":"2","noUsgsAuthors":false,"publicationStatus":"PW","contributors":{"authors":[{"text":"Stringfield, V. T.","contributorId":72369,"corporation":false,"usgs":true,"family":"Stringfield","given":"V.","email":"","middleInitial":"T.","affiliations":[],"preferred":false,"id":830883,"contributorType":{"id":1,"text":"Authors"},"rank":1},{"text":"LeGrand, H. E.","contributorId":54571,"corporation":false,"usgs":true,"family":"LeGrand","given":"H.","email":"","middleInitial":"E.","affiliations":[],"preferred":false,"id":830884,"contributorType":{"id":1,"text":"Authors"},"rank":2}]}} ,{"id":1007632,"text":"1007632 - 1971 - Review: The kinds of mankind: An introduction to race and racism, by Morton Klass and Hal Hellman","interactions":[],"lastModifiedDate":"2023-02-22T16:57:27.634561","indexId":"1007632","displayToPublicDate":"1971-11-01T00:00:00","publicationYear":"1971","noYear":false,"publicationType":{"id":2,"text":"Article"},"publicationSubtype":{"id":10,"text":"Journal Article"},"seriesTitle":{"id":707,"text":"American Biology Teacher","active":true,"publicationSubtype":{"id":10}},"title":"Review: The kinds of mankind: An introduction to race and racism, by Morton Klass and Hal Hellman","docAbstract":"

No abstract available.

","language":"English","publisher":"University of California Press","doi":"10.2307/4443671","usgsCitation":"Douglas, C.L., 1971, Review: The kinds of mankind: An introduction to race and racism, by Morton Klass and Hal Hellman: American Biology Teacher, v. 33, no. 8, https://doi.org/10.2307/4443671.","productDescription":"1 p.","startPage":"505","costCenters":[{"id":651,"text":"Western Ecological Research Center","active":true,"usgs":true}],"links":[{"id":486805,"rank":2,"type":{"id":40,"text":"Open Access Publisher Index Page"},"url":"https://doi.org/10.2307/4443671","text":"Publisher Index Page"},{"id":130655,"rank":1,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/thumbnails/outside_thumb.jpg"}],"volume":"33","issue":"8","noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"4f4e4a16e4b07f02db603df5","contributors":{"authors":[{"text":"Douglas, Charles L.","contributorId":10742,"corporation":false,"usgs":true,"family":"Douglas","given":"Charles","email":"","middleInitial":"L.","affiliations":[],"preferred":false,"id":315759,"contributorType":{"id":1,"text":"Authors"},"rank":1}]}} ,{"id":70210299,"text":"70210299 - 1971 - Mean annual precipitation and precipitation depth-duration-frequency data for the San Francisco Bay region, California","interactions":[],"lastModifiedDate":"2025-01-21T17:17:00.918436","indexId":"70210299","displayToPublicDate":"1971-10-26T12:16:27","publicationYear":"1971","noYear":false,"publicationType":{"id":18,"text":"Report"},"publicationSubtype":{"id":6,"text":"USGS Unnumbered Series"},"seriesTitle":{"id":5961,"text":"Basic Data Contribution","active":false,"publicationSubtype":{"id":6}},"seriesNumber":"32","title":"Mean annual precipitation and precipitation depth-duration-frequency data for the San Francisco Bay region, California","docAbstract":"

This report presents precipitation data for the San Francisco Bay region in a form suitable for use as criteria for both drainage design and the study of the stability of land slopes. The data presented include (1) an isohyetal map showing long-term mean annual precipitation and (2) a table of storm precipitation depths, corresponding to various durations and frequencies, that are applicable to any site in the region. The regimen of precipitation in the region is such that depth-duration frequency characteristics for a site are closely related to the mean annual precipitation for that site.

","language":"English","publisher":"U.S. Geological Survey","doi":"10.3133/70210299","collaboration":"Prepared in cooperation with the U.S. Department of Housing and Urban Development as part of the San Francisco Bay Region Environment and Resources Planning Study","usgsCitation":"Rantz, S., 1971, Mean annual precipitation and precipitation depth-duration-frequency data for the San Francisco Bay region, California: Basic Data Contribution 32, Report: iii, 23 p.; 1 Plate: 20.39 x 24.58 inches, https://doi.org/10.3133/70210299.","productDescription":"Report: iii, 23 p.; 1 Plate: 20.39 x 24.58 inches","costCenters":[],"links":[{"id":466254,"rank":1,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/unnumbered/70210299/report-thumb.jpg"},{"id":466255,"rank":2,"type":{"id":11,"text":"Document"},"url":"https://pubs.usgs.gov/unnumbered/70210299/report.pdf","linkFileType":{"id":1,"text":"pdf"}},{"id":466256,"rank":3,"type":{"id":17,"text":"Plate"},"url":"https://pubs.usgs.gov/unnumbered/70210299/plate-1.pdf","linkFileType":{"id":1,"text":"pdf"}}],"country":"United States","state":"California","city":"San Francisco","geographicExtents":"{\n \"type\": \"FeatureCollection\",\n \"features\": [\n {\n \"type\": \"Feature\",\n \"properties\": {},\n \"geometry\": {\n \"coordinates\": [\n [\n [\n -123.75,\n 39\n ],\n [\n -123.75,\n 36.5\n ],\n [\n -121.083333,\n 36.5\n ],\n [\n -121.083333,\n 39\n ],\n [\n -123.75,\n 39\n ]\n ]\n ],\n \"type\": \"Polygon\"\n }\n }\n ]\n}","noUsgsAuthors":false,"publicationStatus":"PW","contributors":{"authors":[{"text":"Rantz, S. E.","contributorId":34106,"corporation":false,"usgs":true,"family":"Rantz","given":"S. E.","affiliations":[],"preferred":false,"id":924668,"contributorType":{"id":1,"text":"Authors"},"rank":1}]}} ,{"id":70227399,"text":"70227399 - 1971 - EROS — New observation vantage points and processes","interactions":[],"lastModifiedDate":"2022-01-12T23:23:03.525266","indexId":"70227399","displayToPublicDate":"1971-10-03T17:16:18","publicationYear":"1971","noYear":false,"publicationType":{"id":24,"text":"Conference Paper"},"publicationSubtype":{"id":19,"text":"Conference Paper"},"title":"EROS — New observation vantage points and processes","docAbstract":"

The EROS Program objective is to utilize aircraft and spacecraft remote-sensing technology as complementary parts of integrated data collection, processing, and dissemination systems to support resources research and management functions of the Department of the Interior. The Program develops and coordinates research in the applications of new sensors for resources applications in cooperation with NASA. At present there are two major areas of activity: present there are two major areas of activity: The first is related to the Earth Resources Technology Satellite (ERTS). The second is a suite of projects designed to determine the applicability of new aerial and satellite sensing systems and techniques to geologic, geographic, hydrologic, and topographic mapping and for supporting natural resources management functions of the Department of the Interior. Programs with similar goals for agriculture and forestry, and for oceanography are being conducted in the Departments of Agriculture, Commerce, the Naval Oceanographic Office, and in a number of colleges and universities.

The first satellite designed specifically for resources research and applications, ERTS-A, is to be launched in early 1972. It will be an unmanned satellite carrying three experimental systems: A three camera Return Beam Vidicon (RBV) system, a 4-band Multispectral Scanning (MSS) radiometer system, and a Data Collection System (DCS). The RBV cameras will photograph simultaneously and instantaneously areas of the earth 100 × 100 nautical miles - or 10,000 square nautical miles - in the blue-green (.475-.575mu m), the red (.580-.680mu m), and the near infrared (.690-.830mu m). The MSS will record three wavelength bands in the same general spectral range and the fourth band (8.0 mu m) will extend farther into the infrared...

","conferenceTitle":"Fall Meeting of the Society of Petroleum Engineers of AIME","conferenceDate":"October 3-6, 1971","conferenceLocation":"New Orleans, Louisiana, United States","language":"English","publisher":"Society of Petroleum Engineers","doi":"10.2118/3451-MS","usgsCitation":"Fary, R.W., 1971, EROS — New observation vantage points and processes, Fall Meeting of the Society of Petroleum Engineers of AIME, New Orleans, Louisiana, United States, October 3-6, 1971, SPE-3451-MS, https://doi.org/10.2118/3451-MS.","productDescription":"SPE-3451-MS","costCenters":[],"links":[{"id":394296,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/thumbnails/outside_thumb.jpg"}],"otherGeospatial":"Earth","noUsgsAuthors":false,"publicationDate":"1971-10-03","publicationStatus":"PW","contributors":{"authors":[{"text":"Fary, Raymond W. Jr.","contributorId":22830,"corporation":false,"usgs":true,"family":"Fary","given":"Raymond","suffix":"Jr.","email":"","middleInitial":"W.","affiliations":[],"preferred":false,"id":830742,"contributorType":{"id":1,"text":"Authors"},"rank":1}]}} ,{"id":70227400,"text":"70227400 - 1971 - Third International Seminar for Hydrology Professors","interactions":[],"lastModifiedDate":"2022-01-12T23:30:38.905719","indexId":"70227400","displayToPublicDate":"1971-10-01T17:25:01","publicationYear":"1971","noYear":false,"publicationType":{"id":2,"text":"Article"},"publicationSubtype":{"id":10,"text":"Journal Article"},"seriesTitle":{"id":7458,"text":"Eos Science News","active":true,"publicationSubtype":{"id":10}},"title":"Third International Seminar for Hydrology Professors","docAbstract":"

The Third International Seminar for Hydrology Professors was held at Purdue University in Lafayette, Indiana. There were 72 U.S. participants from 25 States and 19 participants from 15 other countries as follows: three from Canada; two each from Costa Rica and Peru; and one each from The Republic of China, Colombia, El Salvador, France, India, Republic of Korea, Mexico, New Zealand, Portugal, Romania, Turkey, and the United Arab Republic. Seventy-eight of the participants were college or university professors and 13 represented various state and national research and technical agencies.

","conferenceTitle":"Third International Seminar for Hydrology Professors","conferenceDate":"July 18-30, 1971","conferenceLocation":"Lafayette, Indiana, United States","language":"English","publisher":"American Geophysical Union","doi":"10.1029/EO052i010p00723-01","usgsCitation":"Shown, L.M., 1971, Third International Seminar for Hydrology Professors: Eos Science News, v. 52, no. 10, p. 723-723, https://doi.org/10.1029/EO052i010p00723-01.","productDescription":"1 p.","startPage":"723","endPage":"723","costCenters":[],"links":[{"id":394297,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/thumbnails/outside_thumb.jpg"}],"country":"United States","state":"Indiana","city":"Lafayette","geographicExtents":"{\n \"type\": \"FeatureCollection\",\n \"features\": [\n {\n \"type\": \"Feature\",\n \"properties\": {},\n \"geometry\": {\n \"type\": \"Polygon\",\n \"coordinates\": [\n [\n [\n -86.98356628417969,\n 40.34235741658335\n ],\n [\n -86.78031921386719,\n 40.34235741658335\n ],\n [\n -86.78031921386719,\n 40.52528265385008\n ],\n [\n -86.98356628417969,\n 40.52528265385008\n ],\n [\n -86.98356628417969,\n 40.34235741658335\n ]\n ]\n ]\n }\n }\n ]\n}","volume":"52","issue":"10","noUsgsAuthors":false,"publicationDate":"2012-04-12","publicationStatus":"PW","contributors":{"authors":[{"text":"Shown, Lynn M.","contributorId":7326,"corporation":false,"usgs":true,"family":"Shown","given":"Lynn","email":"","middleInitial":"M.","affiliations":[],"preferred":false,"id":830743,"contributorType":{"id":1,"text":"Authors"},"rank":1}]}} ,{"id":70206432,"text":"70206432 - 1971 - The problem of groundwater discharge into the seas","interactions":[],"lastModifiedDate":"2019-11-03T16:48:57","indexId":"70206432","displayToPublicDate":"1971-10-01T16:34:10","publicationYear":"1971","noYear":false,"publicationType":{"id":2,"text":"Article"},"publicationSubtype":{"id":10,"text":"Journal Article"},"seriesTitle":{"id":1578,"text":"Eos, Transactions, American Geophysical Union","onlineIssn":"2324-9250","printIssn":"0096-394","active":true,"publicationSubtype":{"id":10}},"displayTitle":"The problem of groundwater discharge into the seas","title":"The problem of groundwater discharge into the seas","docAbstract":"

Introductory Note: The dynamic equilibrium of the various factors involved in the world water balance or budget is the central scientific problem of the International Hydrological Decade. One of the potentially vital elements of the balance is groundwater discharge to the oceans. To paraphrase the authors of the following Russian publication, the world water budget can't be properly balanced, statically or dynamically, until there are improved values for the amount of groundwater that is discharged directly to oceans, seas, and enclosed lakes. The following report, with its bibliography, presents some Russian approaches to the problem and provides a few bits of numerical information. The report was translated by Frank W. Trainer of the U.S. Geological Survey. The text has been slightly reduced in the interests of saving space but the bibliography is given in full and has been transcribed into more or less standard U.S. Geological Survey bibliographical style. ©1971. American Geophysical Union. All Rights Reserved.

","language":"English ","doi":"10.1029/EO052i010p00717","issn":"00963941","usgsCitation":"Kudelin, B., Zekster, I., Meskheteli, A., Brusilovsky, S., and Trainer, F., 1971, The problem of groundwater discharge into the seas: Eos, Transactions, American Geophysical Union, v. 52, no. 10, p. 717-722, https://doi.org/10.1029/EO052i010p00717.","productDescription":"6 p.","startPage":"717","endPage":"722","costCenters":[],"links":[{"id":368910,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/thumbnails/outside_thumb.jpg"}],"volume":"52","issue":"10","noUsgsAuthors":false,"publicationDate":"2012-04-12","publicationStatus":"PW","contributors":{"authors":[{"text":"Kudelin, B.I.","contributorId":220224,"corporation":false,"usgs":false,"family":"Kudelin","given":"B.I.","email":"","affiliations":[],"preferred":false,"id":774523,"contributorType":{"id":1,"text":"Authors"},"rank":1},{"text":"Zekster, I.S.","contributorId":220225,"corporation":false,"usgs":false,"family":"Zekster","given":"I.S.","email":"","affiliations":[],"preferred":false,"id":774524,"contributorType":{"id":1,"text":"Authors"},"rank":2},{"text":"Meskheteli, A.V.","contributorId":220226,"corporation":false,"usgs":false,"family":"Meskheteli","given":"A.V.","email":"","affiliations":[],"preferred":false,"id":774525,"contributorType":{"id":1,"text":"Authors"},"rank":3},{"text":"Brusilovsky, S.A.","contributorId":220227,"corporation":false,"usgs":false,"family":"Brusilovsky","given":"S.A.","email":"","affiliations":[],"preferred":false,"id":774526,"contributorType":{"id":1,"text":"Authors"},"rank":4},{"text":"Trainer, F.W.","contributorId":26007,"corporation":false,"usgs":true,"family":"Trainer","given":"F.W.","email":"","affiliations":[],"preferred":false,"id":774527,"contributorType":{"id":1,"text":"Authors"},"rank":5}]}} ,{"id":70227314,"text":"70227314 - 1971 - Earth-science studies of a nuclear test area in the western Aleutian Islands: Supplementary hydrologic information: Discussion","interactions":[],"lastModifiedDate":"2022-01-07T21:06:37.284904","indexId":"70227314","displayToPublicDate":"1971-10-01T14:54:24","publicationYear":"1971","noYear":false,"publicationType":{"id":2,"text":"Article"},"publicationSubtype":{"id":10,"text":"Journal Article"},"seriesTitle":{"id":5935,"text":"Bulletin of the Geological Society of America","active":true,"publicationSubtype":{"id":10}},"title":"Earth-science studies of a nuclear test area in the western Aleutian Islands: Supplementary hydrologic information: Discussion","docAbstract":"

No abstract available.

","language":"English","publisher":"Geological Society of America","doi":"10.1130/0016-7606(1971)82[2963:ESOANT]2.0.CO;2","usgsCitation":"Ballance, W.C., and Gard, L.M., 1971, Earth-science studies of a nuclear test area in the western Aleutian Islands: Supplementary hydrologic information: Discussion: Bulletin of the Geological Society of America, v. 82, no. 10, p. 2963-2963, https://doi.org/10.1130/0016-7606(1971)82[2963:ESOANT]2.0.CO;2.","productDescription":"1 p.","startPage":"2963","endPage":"2963","costCenters":[],"links":[{"id":394063,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/thumbnails/outside_thumb.jpg"}],"country":"United States","state":"Alaska","otherGeospatial":"Aleutian Islands, Amchitka","geographicExtents":"{\n \"type\": \"FeatureCollection\",\n \"features\": [\n {\n \"type\": \"Feature\",\n \"properties\": {},\n \"geometry\": {\n \"type\": \"Polygon\",\n \"coordinates\": [\n [\n [\n -181.22222900390625,\n 51.56255861691012\n ],\n [\n 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-181.27716064453125,\n 51.58389660297626\n ],\n [\n -181.24557495117188,\n 51.581336573511145\n ],\n [\n -181.22222900390625,\n 51.56255861691012\n ]\n ]\n ]\n }\n }\n ]\n}","volume":"82","issue":"10","noUsgsAuthors":false,"publicationStatus":"PW","contributors":{"authors":[{"text":"Ballance, W. C.","contributorId":98315,"corporation":false,"usgs":true,"family":"Ballance","given":"W.","email":"","middleInitial":"C.","affiliations":[],"preferred":false,"id":830410,"contributorType":{"id":1,"text":"Authors"},"rank":1},{"text":"Gard, L. M.","contributorId":91507,"corporation":false,"usgs":true,"family":"Gard","given":"L.","email":"","middleInitial":"M.","affiliations":[],"preferred":false,"id":830411,"contributorType":{"id":1,"text":"Authors"},"rank":2}]}} ,{"id":70223311,"text":"70223311 - 1971 - Age and chemistry of tertiary volcanic rocks in north-central Arizona and relation of the rocks to the Colorado Plateaus","interactions":[],"lastModifiedDate":"2021-08-20T20:23:04.905588","indexId":"70223311","displayToPublicDate":"1971-10-01T14:31:55","publicationYear":"1971","noYear":false,"publicationType":{"id":2,"text":"Article"},"publicationSubtype":{"id":10,"text":"Journal Article"},"seriesTitle":{"id":1786,"text":"Geological Society of America Bulletin","active":true,"publicationSubtype":{"id":10}},"title":"Age and chemistry of tertiary volcanic rocks in north-central Arizona and relation of the rocks to the Colorado Plateaus","docAbstract":"

During late Miocene (14.8 m.y.) to early Pliocene (10.1 m.y.) time, local latite and widespread basaltic flows accumulated with associated continental sedimentary deposits in north-central Arizona. Some of these rocks were displaced and tilted by normal faults, and new drainage, now occupied in part by basalt flows of late Pliocene age (average 5 m.y., maximum of 6 m.y.), was established at the southern margin of the Colorado Plateaus. The time of faulting and uplift of the Colorado Plateaus in this region is thus bracketed between about 10.1 and 6 m.y. ago.

Five analyzed basalts fall within the tholeiitic basalt field of the alkali-silica diagram and twenty are in the alkalic basalt field; in general, they are similar to other alkali-olivine basalts from the western United States.

","language":"English","publisher":"Geological Society of America","doi":"10.1130/0016-7606(1971)82[2767:AACOTV]2.0.CO;2","usgsCitation":"McKee, E.H., and Anderson, C.A., 1971, Age and chemistry of tertiary volcanic rocks in north-central Arizona and relation of the rocks to the Colorado Plateaus: Geological Society of America Bulletin, v. 82, no. 10, p. 2767-2782, https://doi.org/10.1130/0016-7606(1971)82[2767:AACOTV]2.0.CO;2.","productDescription":"18 p.","startPage":"2767","endPage":"2782","costCenters":[],"links":[{"id":388258,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/thumbnails/outside_thumb.jpg"}],"country":"United States","state":"Arizona","otherGeospatial":"Colorado Plateaus, Mogollon Rim","geographicExtents":"{\n \"type\": \"FeatureCollection\",\n \"features\": [\n {\n \"type\": \"Feature\",\n \"properties\": {},\n \"geometry\": {\n \"type\": \"Polygon\",\n \"coordinates\": [\n [\n [\n -113.587646484375,\n 35.209721645221386\n ],\n [\n -112.6318359375,\n 33.76088200086917\n ],\n [\n -111.851806640625,\n 33.57343808567733\n ],\n [\n -111.2091064453125,\n 33.358061612778876\n ],\n [\n -109.0557861328125,\n 33.32134852669881\n ],\n [\n -109.0557861328125,\n 34.4793919710481\n ],\n [\n -111.22558593749999,\n 35.0254981588326\n ],\n [\n -112.423095703125,\n 35.205233347514536\n ],\n [\n -113.587646484375,\n 35.209721645221386\n ]\n ]\n ]\n }\n }\n ]\n}","volume":"82","issue":"10","noUsgsAuthors":false,"publicationStatus":"PW","contributors":{"authors":[{"text":"McKee, Edwin H. mckee@usgs.gov","contributorId":3728,"corporation":false,"usgs":true,"family":"McKee","given":"Edwin","email":"mckee@usgs.gov","middleInitial":"H.","affiliations":[],"preferred":true,"id":821689,"contributorType":{"id":1,"text":"Authors"},"rank":1},{"text":"Anderson, Charles A.","contributorId":81108,"corporation":false,"usgs":true,"family":"Anderson","given":"Charles","email":"","middleInitial":"A.","affiliations":[],"preferred":false,"id":821690,"contributorType":{"id":1,"text":"Authors"},"rank":2}]}} ,{"id":70227464,"text":"70227464 - 1971 - Metamorphism of Precambrian granitic xenoliths in a mica peridotite at Rose Dome, Woodson County, Kansas: Part 2, petrologic and mineralogic studies","interactions":[],"lastModifiedDate":"2022-01-18T18:39:29.59557","indexId":"70227464","displayToPublicDate":"1971-10-01T12:27:17","publicationYear":"1971","noYear":false,"publicationType":{"id":2,"text":"Article"},"publicationSubtype":{"id":10,"text":"Journal Article"},"seriesTitle":{"id":5935,"text":"Bulletin of the Geological Society of America","active":true,"publicationSubtype":{"id":10}},"title":"Metamorphism of Precambrian granitic xenoliths in a mica peridotite at Rose Dome, Woodson County, Kansas: Part 2, petrologic and mineralogic studies","docAbstract":"

Field, drill-core, petrographic, and mineralogic studies show that the Precambrian granitic rocks exposed on Rose Dome, Woodson County, Kansas, were emplaced as inclusions of basement rock in a mica peridotite magma that intruded the Pennsylvanian section of Rose Dome during Late Cretaceous time. High temperatures of the alkaline ultramafic magma (probably greater than 800° C) led to metamorphism of the granitic inclusions and the formation of high sanidine and high albite from original microcline and albite. Contact metamorphic effects on country rock include the development of buchite-like sanidine-magnesian biotite hornfels from Weston Shale (Pennsylvanian) that was intruded by the mica peridotite.

The high temperatures of the peridotite magma also led to partial melting of the granitic rocks; a quartzofeldspathic matrix shows volcanic textures and binds mineral and rock fragments together to produce the varied range of textures and structures of the granitic xenoliths. Partial melting of the granitic rocks accounts for those features that led earlier workers to conclude that the “granite” on Rose Dome had intruded the Pennsylvanian section. Those features included xenoliths of hornfels enclosed by granitic material and apparently intrusive relationships between the granitic rocks and metamorphosed shale. The lack of concordance in the Rb-Sr ages of the granitic rocks (Part 1) may stem partly from melting of the “granite” and exchange of ions with the mica peridotite magma, from the “sampling” of different levels of granitic crust by the upwelling peridotite magma, or from weathering.

","language":"English","publisher":"Geological Society of America","doi":"10.1130/0016-7606(1971)82[2869:MOPGXI]2.0.CO;2","usgsCitation":"Franks, P.C., Bickford, M.E., and Wagner, H.C., 1971, Metamorphism of Precambrian granitic xenoliths in a mica peridotite at Rose Dome, Woodson County, Kansas: Part 2, petrologic and mineralogic studies: Bulletin of the Geological Society of America, v. 82, no. 10, p. 2869-2889, https://doi.org/10.1130/0016-7606(1971)82[2869:MOPGXI]2.0.CO;2.","productDescription":"21 p.","startPage":"2869","endPage":"2889","costCenters":[],"links":[{"id":394454,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/thumbnails/outside_thumb.jpg"}],"country":"United States","state":"Kansas","county":"Woodson County","otherGeospatial":"Rose Dome","geographicExtents":"{\n \"type\": \"FeatureCollection\",\n \"features\": [\n {\n \"type\": \"Feature\",\n \"properties\": {},\n \"geometry\": {\n \"type\": \"Polygon\",\n \"coordinates\": [\n [\n [\n -95.71469306945801,\n 37.77695634643178\n ],\n [\n -95.70407152175903,\n 37.77695634643178\n ],\n [\n -95.70407152175903,\n 37.78426582053905\n ],\n [\n -95.71469306945801,\n 37.78426582053905\n ],\n [\n -95.71469306945801,\n 37.77695634643178\n ]\n ]\n ]\n }\n }\n ]\n}","volume":"82","issue":"10","noUsgsAuthors":false,"publicationStatus":"PW","contributors":{"authors":[{"text":"Franks, Paul C.","contributorId":37802,"corporation":false,"usgs":true,"family":"Franks","given":"Paul","email":"","middleInitial":"C.","affiliations":[],"preferred":false,"id":831043,"contributorType":{"id":1,"text":"Authors"},"rank":1},{"text":"Bickford, M. E.","contributorId":6891,"corporation":false,"usgs":false,"family":"Bickford","given":"M.","email":"","middleInitial":"E.","affiliations":[],"preferred":false,"id":831044,"contributorType":{"id":1,"text":"Authors"},"rank":2},{"text":"Wagner, Holly C.","contributorId":55407,"corporation":false,"usgs":true,"family":"Wagner","given":"Holly","email":"","middleInitial":"C.","affiliations":[],"preferred":false,"id":831045,"contributorType":{"id":1,"text":"Authors"},"rank":3}]}} ,{"id":70227136,"text":"70227136 - 1971 - A method for discriminating between biogenic and chemical origins of the ore-stage pyrite in a roll-type uranium deposit","interactions":[],"lastModifiedDate":"2021-12-30T18:33:39.258583","indexId":"70227136","displayToPublicDate":"1971-10-01T12:20:01","publicationYear":"1971","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":"A method for discriminating between biogenic and chemical origins of the ore-stage pyrite in a roll-type uranium deposit","docAbstract":"

Some roll-type uranium deposits are marginal to an altered tongue in sandstone beds that originally contained more-or-less uniformly distributed pyrite. Mineralizing solutions percolated through the sandstone, oxidized nearly all the pre-existing pyrite, and then redeposited part of the pyrite downstream in an embryonic ore zone. The pyrite and the entire ore zone continued to migrate downstream in the sandstone, much as a sand dune migrates. The amount of pyrite in mature deposits varies systematically with the position in the ore body. It is postulated that the rate at which the pyrite was redeposited controlled the systematic variation in distribution of pyrite.Biogenic and chemical models which are described in the literature provide alternate explanations for the genesis of roll-type uranium deposits in sandstone. The different theoretical rates for the precipitation of pyrite in the two genetic models provide a distinctive distribution of pyrite that characterizes each process. The theoretical difference between the biogenic and chemical models provides a mathematical technique for identifying the origin of a deposit. Mathematical analysis of the pyrite content of a uranium deposit in the Shirley Basin, Wyoming, illustrates a practical application of the theory. Although a definite conclusion about the origin of roll-type deposits would require considerably more data than are now available, the pyrite content of this deposit does correspond to the theoretical pyrite content of the chemical model, suggesting that a disproportionation reaction was involved in its formation.

","language":"English","publisher":"Society of Economic Geologists","doi":"10.2113/gsecongeo.66.6.919","usgsCitation":"Warren, C.G., 1971, A method for discriminating between biogenic and chemical origins of the ore-stage pyrite in a roll-type uranium deposit: Economic Geology, v. 66, no. 6, p. 919-928, https://doi.org/10.2113/gsecongeo.66.6.919.","productDescription":"10 p.","startPage":"919","endPage":"928","costCenters":[],"links":[{"id":393662,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/thumbnails/outside_thumb.jpg"}],"country":"United States","state":"Wyoming","otherGeospatial":"Shirley Basin","geographicExtents":"{\n \"type\": \"FeatureCollection\",\n \"features\": [\n {\n \"type\": \"Feature\",\n \"properties\": {},\n \"geometry\": {\n \"type\": \"Polygon\",\n \"coordinates\": [\n [\n [\n -106.27349853515625,\n 42.190372799976615\n ],\n [\n -106.2652587890625,\n 42.183249931734096\n ],\n [\n -106.23023986816406,\n 42.261049162113856\n ],\n [\n -106.23435974121094,\n 42.374778361114195\n ],\n [\n -106.402587890625,\n 42.420415239489934\n ],\n [\n -106.435546875,\n 42.3143853165376\n ],\n [\n -106.43074035644531,\n 42.250376512405275\n ],\n [\n -106.27349853515625,\n 42.190372799976615\n ]\n ]\n ]\n }\n }\n ]\n}","volume":"66","issue":"6","noUsgsAuthors":false,"publicationDate":"1971-10-01","publicationStatus":"PW","contributors":{"authors":[{"text":"Warren, C. G.","contributorId":41427,"corporation":false,"usgs":true,"family":"Warren","given":"C.","email":"","middleInitial":"G.","affiliations":[],"preferred":false,"id":829758,"contributorType":{"id":1,"text":"Authors"},"rank":1}]}} ,{"id":70227306,"text":"70227306 - 1971 - Mesozoic granitic rocks in northwestern Nevada: A link between the Sierra Nevada and Idaho batholiths","interactions":[],"lastModifiedDate":"2022-01-07T18:29:30.567099","indexId":"70227306","displayToPublicDate":"1971-10-01T12:15:45","publicationYear":"1971","noYear":false,"publicationType":{"id":2,"text":"Article"},"publicationSubtype":{"id":10,"text":"Journal Article"},"seriesTitle":{"id":5935,"text":"Bulletin of the Geological Society of America","active":true,"publicationSubtype":{"id":10}},"title":"Mesozoic granitic rocks in northwestern Nevada: A link between the Sierra Nevada and Idaho batholiths","docAbstract":"

Extensive areas in northwestern Nevada are underlain by granodiorite and quartz monzonite plutons, as well as less common smaller bodies of quartz diorite. Twenty-six K/Ar age determinations on rocks from this suite range from about 175 to 85 m.y., but most of the plutons are between 105 and 85 m.y. old. This Late Cretaceous intrusive epoch extending from 105 to 85 m.y. ago is here named the Lovelock intrusive epoch. Twenty-three whole-rock chemical analyses show that the granitic rocks of northwestern Nevada form a homogeneous differentiation series with a narrow range in major element distribution. The granitic plutons of northwestern Nevada are chemically and petrographically indistinguishable from granitic intrusives of equivalent age in the Sierra Nevada and Idaho batholiths, and form a link between these two major batholiths.

","language":"English","publisher":"Geological Society of America","doi":"10.1130/0016-7606(1971)82[2933:MGRINN]2.0.CO;2","usgsCitation":"Smith, J., McKee, E.H., Tatlock, D.B., and Marvin, R.F., 1971, Mesozoic granitic rocks in northwestern Nevada: A link between the Sierra Nevada and Idaho batholiths: Bulletin of the Geological Society of America, v. 82, no. 10, p. 2933-2944, https://doi.org/10.1130/0016-7606(1971)82[2933:MGRINN]2.0.CO;2.","productDescription":"12 p.","startPage":"2933","endPage":"2944","costCenters":[],"links":[{"id":394036,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/thumbnails/outside_thumb.jpg"}],"country":"United States","state":"California, Idaho, Nevada","otherGeospatial":"Idaho batholith, Sierra Nevada batholith","geographicExtents":"{\n \"type\": \"FeatureCollection\",\n \"features\": [\n {\n \"type\": \"Feature\",\n \"properties\": {},\n \"geometry\": {\n \"type\": \"Polygon\",\n \"coordinates\": [\n [\n [\n -119.77294921874999,\n 39.86758762451019\n ],\n [\n -117.48779296875,\n 39.86758762451019\n ],\n [\n -117.48779296875,\n 42.05745022024682\n ],\n [\n -119.77294921874999,\n 42.05745022024682\n ],\n [\n -119.77294921874999,\n 39.86758762451019\n ]\n ]\n ]\n }\n }\n ]\n}","volume":"82","issue":"10","noUsgsAuthors":false,"publicationStatus":"PW","contributors":{"authors":[{"text":"Smith, James G.","contributorId":98712,"corporation":false,"usgs":true,"family":"Smith","given":"James G.","affiliations":[],"preferred":false,"id":830383,"contributorType":{"id":1,"text":"Authors"},"rank":1},{"text":"McKee, Edwin H. mckee@usgs.gov","contributorId":3728,"corporation":false,"usgs":true,"family":"McKee","given":"Edwin","email":"mckee@usgs.gov","middleInitial":"H.","affiliations":[],"preferred":true,"id":830384,"contributorType":{"id":1,"text":"Authors"},"rank":2},{"text":"Tatlock, Donald Bruce","contributorId":17250,"corporation":false,"usgs":true,"family":"Tatlock","given":"Donald","email":"","middleInitial":"Bruce","affiliations":[],"preferred":false,"id":830385,"contributorType":{"id":1,"text":"Authors"},"rank":3},{"text":"Marvin, Richard F.","contributorId":23125,"corporation":false,"usgs":true,"family":"Marvin","given":"Richard","email":"","middleInitial":"F.","affiliations":[],"preferred":false,"id":830386,"contributorType":{"id":1,"text":"Authors"},"rank":4}]}} ,{"id":70227135,"text":"70227135 - 1971 - The effect of salinity on the maximum thermal gradient of a hydrothermal system at hydrostatic pressure","interactions":[],"lastModifiedDate":"2021-12-30T18:18:10.161992","indexId":"70227135","displayToPublicDate":"1971-10-01T12:13:39","publicationYear":"1971","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 effect of salinity on the maximum thermal gradient of a hydrothermal system at hydrostatic pressure","docAbstract":"

The effect of salinity on the temperature-depth relations of a brine of constant composition, enclosed in a vein system, but freely connected to the surface, and everywhere at the boiling point for the hydrostatic head, was calculated by using a mathematical model. The Na-Ca-K-Cl brines which are found in thermal springs and in fluid inclusions in ore minerals were approximated by the available data for vapor-saturated NaCl-H2O solutions. In general, the results are similar to those calculated by D. E. White in 1968 for H 2 O, except that the gradients are steeper because of the increase in density and the decrease in vapor pressure caused by the dissolved salt. As a practical rule, the depth to an isotherm in a 5, 10, 15, 20, and 25 wt percent NaCl brine system is, respectively, 92, 84, 77, 70, and 63 percent (+ or -2 percent) of the depth to the same isotherm in an H2O system. From the data presented, the minimum depth to the growth site of crystals containing fluid inclusions which indicate boiling of the brine can be estimated. Among other applications, these results are useful toward the understanding of the behavior of brines in geothermal areas which may or may not contain compositional stratification.

","language":"English","publisher":"Society of Economic Geologists","doi":"10.2113/gsecongeo.66.6.940","usgsCitation":"Haas, J.L., 1971, The effect of salinity on the maximum thermal gradient of a hydrothermal system at hydrostatic pressure: Economic Geology, v. 66, no. 6, p. 940-946, https://doi.org/10.2113/gsecongeo.66.6.940.","productDescription":"7 p.","startPage":"940","endPage":"946","costCenters":[],"links":[{"id":393661,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/thumbnails/outside_thumb.jpg"}],"volume":"66","issue":"6","noUsgsAuthors":false,"publicationDate":"1971-10-01","publicationStatus":"PW","contributors":{"authors":[{"text":"Haas, John L. Jr.","contributorId":53816,"corporation":false,"usgs":true,"family":"Haas","given":"John","suffix":"Jr.","email":"","middleInitial":"L.","affiliations":[],"preferred":false,"id":829757,"contributorType":{"id":1,"text":"Authors"},"rank":1}]}} ,{"id":70227432,"text":"70227432 - 1971 - Geochemical interpretations of groundwater flow systems","interactions":[],"lastModifiedDate":"2022-01-14T17:25:16.842313","indexId":"70227432","displayToPublicDate":"1971-10-01T11:15:29","publicationYear":"1971","noYear":false,"publicationType":{"id":2,"text":"Article"},"publicationSubtype":{"id":10,"text":"Journal Article"},"seriesTitle":{"id":2529,"text":"Journal of the American Water Resources Association","active":true,"publicationSubtype":{"id":10}},"title":"Geochemical interpretations of groundwater flow systems","docAbstract":"

Interest in the geochemistry of groundwater is increasing owing to the great number of current projects involving underground liquid waste storage, artificial recharge of potable water, accidental contamination of groundwater bodies, sanitary landfills, and pollution monitoring. Geochemical techniques used to facilitate the understanding of a groundwater system range from extremely simple to those requiring sophisticated theories, equipment, and procedures. An interpretation of the simple trilinear diagram for samples collected from the Yucatan Peninsula of Mexico provided evidence that the fresh-water body was only a few tens of meters thick and was underlain everywhere by an extensive body of salt water. A geochemical technique that has been used effectively to identify the source of salt water in coastal aquifers is measurement of the carbon-14 concentrations. Carbon-14 has been used in a regional carbonate aquifer to determine the velocity of groundwater movement, rates of chemical reactions, and distribution of hydraulic conductivity. The application of principles of irreversible thermodynamics to groundwater systems provides a basis for constructing models which permit prediction, over both time and space, of changes in head distribution and chemical character of the water resulting from imposed stresses on the system. In essence, proper application of irreversible thermodynamics combines the potential theory of Hubbert with principles of reversible chemical thermodynamics, such as solution of carbonate minerals, to describe and explain controlling chemical reactions and processes of groundwater systems.

","language":"English","publisher":"Wiley","doi":"10.1111/j.1752-1688.1971.tb05021.x","usgsCitation":"Back, W., and Hanshaw, B.B., 1971, Geochemical interpretations of groundwater flow systems: Journal of the American Water Resources Association, v. 7, no. 5, p. 1008-1016, https://doi.org/10.1111/j.1752-1688.1971.tb05021.x.","productDescription":"9 p.","startPage":"1008","endPage":"1016","costCenters":[],"links":[{"id":394396,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/thumbnails/outside_thumb.jpg"}],"country":"Mexico, United States","state":"Florida, South Carolina","otherGeospatial":"Hilton Head Island, Yucatan Peninsula","geographicExtents":"{\n \"type\": \"FeatureCollection\",\n \"features\": [\n {\n \"type\": \"Feature\",\n \"properties\": {},\n \"geometry\": {\n \"type\": \"Polygon\",\n \"coordinates\": [\n [\n [\n -80.83534240722656,\n 32.111659100104504\n ],\n [\n -80.82435607910156,\n 32.10467965495091\n ],\n [\n -80.81336975097656,\n 32.10526129575663\n ],\n [\n -80.75363159179688,\n 32.1343386118551\n ],\n [\n -80.72479248046875,\n 32.15119920972557\n ],\n [\n -80.69183349609375,\n 32.19188435632485\n ],\n [\n -80.66230773925781,\n 32.21861041216938\n ],\n [\n -80.68222045898438,\n 32.246490096781194\n ],\n [\n -80.73165893554688,\n 32.27668343339886\n ],\n [\n -80.74127197265625,\n 32.26739424574946\n ],\n [\n -80.75637817382812,\n 32.27900558170509\n ],\n [\n -80.76736450195312,\n 32.27203895845447\n ],\n [\n -80.76667785644531,\n 32.262168659780905\n ],\n [\n -80.76873779296875,\n 32.25810410713092\n ],\n [\n -80.7769775390625,\n 32.26042673093089\n ],\n [\n -80.78384399414062,\n 32.253458681254116\n ],\n [\n -80.79277038574219,\n 32.229647143457754\n ],\n [\n -80.7879638671875,\n 32.22093404590531\n ],\n [\n -80.7879638671875,\n 32.184329917587384\n ],\n [\n -80.80032348632812,\n 32.1674754490803\n ],\n [\n -80.82092285156249,\n 32.141897196425795\n ],\n [\n -80.83534240722656,\n 32.111659100104504\n ]\n ]\n ]\n }\n },\n {\n \"type\": \"Feature\",\n \"properties\": {},\n \"geometry\": {\n \"type\": \"Polygon\",\n \"coordinates\": [\n [\n [\n -84.0673828125,\n 29.99300228455108\n ],\n [\n -83.5400390625,\n 29.611670115197377\n ],\n [\n -83.21044921875,\n 29.19053283229458\n ],\n [\n -82.90283203125,\n 29.017748018496047\n ],\n [\n -82.99072265625,\n 27.819644755099446\n ],\n [\n -82.24365234375,\n 26.45090222367262\n ],\n [\n -79.91455078125,\n 26.64745870265938\n ],\n [\n -79.89257812499999,\n 26.96124577052697\n ],\n [\n -81.32080078125,\n 30.259067203213018\n ],\n [\n -84.0673828125,\n 29.99300228455108\n ]\n ]\n ]\n }\n },\n {\n \"type\": \"Feature\",\n \"properties\": {},\n \"geometry\": {\n \"type\": \"Polygon\",\n \"coordinates\": [\n [\n [\n -91.5380859375,\n 18.979025953255267\n ],\n [\n -92.43896484375,\n 18.771115062337024\n ],\n [\n -89.296875,\n 17.790535393588975\n ],\n [\n -89.14306640625,\n 17.99963161491187\n ],\n [\n -88.857421875,\n 17.95783210227242\n ],\n [\n -88.48388671874999,\n 18.521283325496277\n ],\n [\n -88.06640625,\n 18.458768120015126\n ],\n [\n -88.04443359375,\n 18.208480196039883\n ],\n [\n -87.802734375,\n 18.166730410221938\n ],\n [\n -87.34130859375,\n 19.331878440818787\n ],\n [\n -87.34130859375,\n 20.014645445341365\n ],\n [\n -86.72607421875,\n 20.324023603422518\n ],\n [\n -86.6162109375,\n 20.940919670394646\n ],\n [\n -87.0556640625,\n 21.718679805703154\n ],\n [\n -87.2314453125,\n 21.555284406923192\n ],\n [\n -88.04443359375,\n 21.739091217718574\n ],\n [\n -89.82421875,\n 21.37124437061831\n ],\n [\n -90.615234375,\n 20.981956742832327\n ],\n [\n -90.65917968749999,\n 19.993998469485504\n ],\n [\n -90.9228515625,\n 19.414792438099557\n ],\n [\n -91.5380859375,\n 18.979025953255267\n ]\n ]\n ]\n }\n }\n ]\n}","volume":"7","issue":"5","noUsgsAuthors":false,"publicationDate":"2007-06-08","publicationStatus":"PW","contributors":{"authors":[{"text":"Back, William","contributorId":59007,"corporation":false,"usgs":true,"family":"Back","given":"William","email":"","affiliations":[],"preferred":false,"id":830885,"contributorType":{"id":1,"text":"Authors"},"rank":1},{"text":"Hanshaw, Bruce B.","contributorId":47350,"corporation":false,"usgs":true,"family":"Hanshaw","given":"Bruce","email":"","middleInitial":"B.","affiliations":[],"preferred":false,"id":830886,"contributorType":{"id":1,"text":"Authors"},"rank":2}]}} ,{"id":70227462,"text":"70227462 - 1971 - Investigation of magnetization and density of a north Atlantic seamount using Poisson's theorem","interactions":[],"lastModifiedDate":"2022-01-18T17:59:30.431472","indexId":"70227462","displayToPublicDate":"1971-10-01T10:51:21","publicationYear":"1971","noYear":false,"publicationType":{"id":2,"text":"Article"},"publicationSubtype":{"id":10,"text":"Journal Article"},"seriesTitle":{"id":1808,"text":"Geophysics","active":true,"publicationSubtype":{"id":10}},"title":"Investigation of magnetization and density of a north Atlantic seamount using Poisson's theorem","docAbstract":"

The relationship between the gravitational and magnetic potentials caused by a uniform distribution of mass and magnetization may be used to obtain independent information about these physical properties. The general relationship in the frequency domain between the Fourier transforms of the gravity and magnetic anomaly fields is established through the Poisson theorem. The discrete Fourier transforms of the sampled continuous functions are used in an analysis which leads to a system of linear equations involving terms in density, magnetization, and calculated finite Fourier-series coefficients. A least squares solution of the system yields the three components of the total magnetization vector divided by the density. From these results, the direction of total magnetization and the minimum of the Koenigsberger ratio Q can be determined uniquely. The remanent magnetization direction and certain other information can be derived for special cases in which the value of one or more of the physical property terms can be assigned. Accurate results were obtained in the analysis of data from a theoretical model. Analysis of gravity and magnetic data from the North Atlantic Gilliss seamount indicates the presence of a significant component of remanent magnetization and leads to derived physical properties which are in fairly close agreement with dredged sample data. The calculated direction of remanent magnetization indicates a paleomagnetic pole position in eastern Siberia, in general agreement with the predicted position for a Cretaceous source in the North Atlantic. The seamount example illustrates certain contingent problems to be considered in practical application of the method.

","language":"English","publisher":"Society of Exploration Geophysicists","doi":"10.1190/1.1440224","usgsCitation":"Cordell, L., and Taylor, P., 1971, Investigation of magnetization and density of a north Atlantic seamount using Poisson's theorem: Geophysics, v. 36, no. 5, p. 919-937, https://doi.org/10.1190/1.1440224.","productDescription":"19 p.","startPage":"919","endPage":"937","costCenters":[],"links":[{"id":394452,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/thumbnails/outside_thumb.jpg"}],"country":"Bermuda","otherGeospatial":"Atlantic Ocean, Gilliss seamount","geographicExtents":"{\n \"type\": \"FeatureCollection\",\n \"features\": [\n {\n \"type\": \"Feature\",\n \"properties\": {},\n \"geometry\": {\n \"type\": \"Polygon\",\n \"coordinates\": [\n [\n [\n -63.182373046875,\n 35.782170703266075\n ],\n [\n -54.349365234375,\n 35.782170703266075\n ],\n [\n -54.349365234375,\n 41.244772343082076\n ],\n [\n -63.182373046875,\n 41.244772343082076\n ],\n [\n -63.182373046875,\n 35.782170703266075\n ]\n ]\n ]\n }\n }\n ]\n}","volume":"36","issue":"5","noUsgsAuthors":false,"publicationStatus":"PW","contributors":{"authors":[{"text":"Cordell, Lindrith","contributorId":40573,"corporation":false,"usgs":true,"family":"Cordell","given":"Lindrith","affiliations":[],"preferred":false,"id":831037,"contributorType":{"id":1,"text":"Authors"},"rank":1},{"text":"Taylor, Patrick","contributorId":172618,"corporation":false,"usgs":false,"family":"Taylor","given":"Patrick","email":"","affiliations":[],"preferred":false,"id":831038,"contributorType":{"id":1,"text":"Authors"},"rank":2}]}} ,{"id":1001352,"text":"1001352 - 1971 - Waterfowl nesting on interstate highway right-of-way in North Dakota","interactions":[],"lastModifiedDate":"2025-02-20T22:41:05.142932","indexId":"1001352","displayToPublicDate":"1971-10-01T00:00:00","publicationYear":"1971","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":"Waterfowl nesting on interstate highway right-of-way in North Dakota","docAbstract":"

We studied 630 acres of roadside along 23 miles of Interstate 94 in Stutsman County, North Dakota, to assess wildlife values of highway rights-of-way. We found 422 duck nests that had an overall success of 57 percent in 1968, 1969, and 1970. Mammalian predators were responsible for 85 percent of the destroyed nests. To test the effect of mowing on duck nest initiation and success, alternate 1-mile blocks of the study area were not mowed in the fall of 1968. In 1969 and 1970, significantly more ducks chose unmowed vegetation in preference to mowed vegetation for nest sites. Mallards (Anas platyrhynchos), pintails (A. acuta), and gadwalls (A. strepera) were especially responsive to unmowed vegetation. Success of duck nests in unmowed vegetation was 62 percent compared with 51 percent in mowed vegetation. Sixteen percent of the nests were unhatched by July 5, the beginning mowing date previously recommended by the North Dakota Highway Department. Wildlife killed by traffic did not increase when half the mile blocks were unmowed, and no significant difference was observed in buildup of snow between mowed and unmowed blocks in the winter of 1968-69. Of 182 motorists interviewed in the study area, 82 percent had not noticed the unmowed rights-of-way. We strongly recommend no mowing of ditch bottoms or back slopes, minimal mowing of inslopes, and no mowing before July 20 to enhance waterfowl nesting and to reduce maintenance costs of highway rights-of-way in duck-producing regions.

","language":"English","publisher":"Wiley","doi":"10.2307/3799786","usgsCitation":"Oetting, R., and Cassel, J., 1971, Waterfowl nesting on interstate highway right-of-way in North Dakota: Journal of Wildlife Management, v. 35, no. 4, p. 774-781, https://doi.org/10.2307/3799786.","productDescription":"8 p.","startPage":"774","endPage":"781","costCenters":[{"id":480,"text":"Northern Prairie Wildlife Research Center","active":true,"usgs":true}],"links":[{"id":133686,"rank":1,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/thumbnails/outside_thumb.jpg"}],"country":"United States","state":"North Dakota","county":"Stutsman County","geographicExtents":"{\"type\":\"FeatureCollection\",\"features\":[{\"type\":\"Feature\",\"geometry\":{\"type\":\"Polygon\",\"coordinates\":[[[-99.2669,47.3268],[-98.8466,47.327],[-98.8392,47.327],[-98.8232,47.3272],[-98.8152,47.3271],[-98.4991,47.327],[-98.467,47.3266],[-98.4677,47.2402],[-98.4685,46.9788],[-98.4412,46.9789],[-98.4396,46.6296],[-98.7894,46.6294],[-99.0379,46.6309],[-99.1616,46.6317],[-99.4122,46.6316],[-99.4498,46.6319],[-99.4477,46.8044],[-99.4476,46.9788],[-99.4821,46.9795],[-99.4824,47.0089],[-99.4822,47.0162],[-99.4821,47.0249],[-99.4826,47.0396],[-99.4827,47.1558],[-99.4801,47.3267],[-99.2669,47.3268]]]},\"properties\":{\"name\":\"Stutsman\",\"state\":\"ND\"}}]}","volume":"35","issue":"4","noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"4f4e49cde4b07f02db5d976c","contributors":{"authors":[{"text":"Oetting, R.B.","contributorId":53733,"corporation":false,"usgs":true,"family":"Oetting","given":"R.B.","email":"","affiliations":[],"preferred":false,"id":310918,"contributorType":{"id":1,"text":"Authors"},"rank":1},{"text":"Cassel, J.F.","contributorId":59750,"corporation":false,"usgs":true,"family":"Cassel","given":"J.F.","email":"","affiliations":[],"preferred":false,"id":310919,"contributorType":{"id":1,"text":"Authors"},"rank":2}]}} ,{"id":70189002,"text":"70189002 - 1971 - Effect of vancomycin, streptomycin and tetracycline pulsating jet lavage on contaminated wounds","interactions":[],"lastModifiedDate":"2025-05-14T16:38:58.920998","indexId":"70189002","displayToPublicDate":"1971-10-01T00:00:00","publicationYear":"1971","noYear":false,"publicationType":{"id":2,"text":"Article"},"publicationSubtype":{"id":10,"text":"Journal Article"},"seriesTitle":{"id":5442,"text":"Military Medicine","active":false,"publicationSubtype":{"id":10}},"title":"Effect of vancomycin, streptomycin and tetracycline pulsating jet lavage on contaminated wounds","docAbstract":"

No abstract available. 

","language":"English","publisher":"Oxford Academic","doi":"10.1093/milmed/136.10.810","usgsCitation":"Cutright, D.E., Bhaskar, S.N., Gross, A., Perez, B., Beasley, J.D., and Mulcahy, D.M., 1971, Effect of vancomycin, streptomycin and tetracycline pulsating jet lavage on contaminated wounds: Military Medicine, v. 136, no. 10, p. 810-813, https://doi.org/10.1093/milmed/136.10.810.","productDescription":"4 p.","startPage":"810","endPage":"813","costCenters":[{"id":114,"text":"Alaska Science Center","active":true,"usgs":true}],"links":[{"id":343106,"rank":1,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/thumbnails/outside_thumb.jpg"}],"volume":"136","issue":"10","noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"596622a1e4b0d1f9f05cefd3","contributors":{"authors":[{"text":"Cutright, Duane E.","contributorId":28191,"corporation":false,"usgs":false,"family":"Cutright","given":"Duane","email":"","middleInitial":"E.","affiliations":[],"preferred":false,"id":702386,"contributorType":{"id":1,"text":"Authors"},"rank":1},{"text":"Bhaskar, Surindar N.","contributorId":93815,"corporation":false,"usgs":false,"family":"Bhaskar","given":"Surindar","email":"","middleInitial":"N.","affiliations":[],"preferred":false,"id":702387,"contributorType":{"id":1,"text":"Authors"},"rank":2},{"text":"Gross, Arthur","contributorId":120963,"corporation":false,"usgs":false,"family":"Gross","given":"Arthur","email":"","affiliations":[],"preferred":false,"id":702388,"contributorType":{"id":1,"text":"Authors"},"rank":3},{"text":"Perez, Bienvenido","contributorId":44751,"corporation":false,"usgs":false,"family":"Perez","given":"Bienvenido","email":"","affiliations":[],"preferred":false,"id":702389,"contributorType":{"id":1,"text":"Authors"},"rank":4},{"text":"Beasley, Joe D. III","contributorId":36881,"corporation":false,"usgs":false,"family":"Beasley","given":"Joe","suffix":"III","email":"","middleInitial":"D.","affiliations":[],"preferred":false,"id":702390,"contributorType":{"id":1,"text":"Authors"},"rank":5},{"text":"Mulcahy, Daniel M. dmulcahy@usgs.gov","contributorId":3102,"corporation":false,"usgs":true,"family":"Mulcahy","given":"Daniel","email":"dmulcahy@usgs.gov","middleInitial":"M.","affiliations":[{"id":116,"text":"Alaska Science Center Biology MFEB","active":true,"usgs":true}],"preferred":true,"id":702391,"contributorType":{"id":1,"text":"Authors"},"rank":6}]}} ,{"id":5220426,"text":"5220426 - 1971 - A starling-deterrent wood duck nest box","interactions":[],"lastModifiedDate":"2025-02-20T22:35:22.567121","indexId":"5220426","displayToPublicDate":"1971-10-01T00:00:00","publicationYear":"1971","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":"A starling-deterrent wood duck nest box","docAbstract":"

In many parts of the United States, the starling (Sturnus vulgaris) has I become a serious competitor for nest boxes erected for wood ducks (Aix sponsa). Research at the Patuxent Wildlife Research Center and at Eastern Neck National Wildlife Refuge near Rock Hall, Maryland, demonstrated that horizontal nest structures with semicircular entrance holes 11 inches in diameter were acceptable to nesting wood ducks but discouraged nesting by starlings. Starlings seemed to prefer boxes in open impoundments to those in wooded impoundments, whereas wood ducks seemed to show no preference.

","language":"English","publisher":"Wiley","doi":"10.2307/3799789","usgsCitation":"McGilvrey, F., and Uhler, F.M., 1971, A starling-deterrent wood duck nest box: Journal of Wildlife Management, v. 35, no. 4, p. 793-797, https://doi.org/10.2307/3799789.","productDescription":"5 p.","startPage":"793","endPage":"797","costCenters":[{"id":531,"text":"Patuxent Wildlife Research Center","active":true,"usgs":true}],"links":[{"id":196260,"rank":1,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/thumbnails/outside_thumb.jpg"}],"country":"United States","state":"Maryland","otherGeospatial":"Patuxent Wildlife Research Center","geographicExtents":"{\n \"type\": \"FeatureCollection\",\n \"features\": [\n {\n \"type\": \"Feature\",\n \"properties\": {},\n \"geometry\": {\n \"coordinates\": [\n [\n [\n -76.82185591899788,\n 39.07802646798717\n ],\n [\n -76.82185591899788,\n 38.98396548979565\n ],\n [\n -76.71643624290974,\n 38.98396548979565\n ],\n [\n -76.71643624290974,\n 39.07802646798717\n ],\n [\n -76.82185591899788,\n 39.07802646798717\n ]\n ]\n ],\n \"type\": \"Polygon\"\n }\n }\n ]\n}","volume":"35","issue":"4","noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"4f4e4b17e4b07f02db6a6323","contributors":{"authors":[{"text":"McGilvrey, Frank B.","contributorId":14908,"corporation":false,"usgs":true,"family":"McGilvrey","given":"Frank B.","affiliations":[],"preferred":false,"id":331796,"contributorType":{"id":1,"text":"Authors"},"rank":1},{"text":"Uhler, Francis M.","contributorId":49838,"corporation":false,"usgs":true,"family":"Uhler","given":"Francis","email":"","middleInitial":"M.","affiliations":[],"preferred":false,"id":331797,"contributorType":{"id":1,"text":"Authors"},"rank":2}]}} ,{"id":1014041,"text":"1014041 - 1971 - Channel catfish virus: A new herpesvirus of ictalurid fish","interactions":[],"lastModifiedDate":"2025-02-26T22:43:17.994627","indexId":"1014041","displayToPublicDate":"1971-10-01T00:00:00","publicationYear":"1971","noYear":false,"publicationType":{"id":2,"text":"Article"},"publicationSubtype":{"id":10,"text":"Journal Article"},"seriesTitle":{"id":2497,"text":"Journal of Virology","active":true,"publicationSubtype":{"id":10}},"title":"Channel catfish virus: A new herpesvirus of ictalurid fish","docAbstract":"

Channel catfish virus was studied in ictalurid fish cell culture, the only system of fish, amphibian, avian, and mammalian cells found to be susceptible. Channel catfish virus infection resulted in intranuclear inclusions and extensive syncytium formation. Replication occurred from 10 to 33 C, but not higher. Best growth was from 25 to 33 C, and the amount of virus released nearly equalled the amount which remained cell-associated. The virus was labile to lipid solvents, and indirect determinations with labeled precursors and a metabolic inhibitor showed evidence of deoxyribonucleic acid. Electron microscopy showed progeny virus, about 100 nm in diameter, in various stages of development in cell nuclei by 4 hr. Present also were nuclear masses of exceptionally electron-dense lamellar material, with a unit dimension of 10 to 15 nm. Virus was enveloped at the nuclear membrane and in cytoplasmic vacuoles, resulting in virions having a diameter of 175 to 200 nm. Negative staining demonstrated icosehedral symmetry and 162 capsomeres. Our data indicate that channel catfish virus is a herpesvirus.

","language":"English","publisher":"American Society for Microbiology","doi":"10.1128/jvi.8.4.525-533.1971","usgsCitation":"Wolf, K., and Darlington, R.W., 1971, Channel catfish virus: A new herpesvirus of ictalurid fish: Journal of Virology, v. 8, no. 4, p. 525-533, https://doi.org/10.1128/jvi.8.4.525-533.1971.","productDescription":"9 p.","startPage":"525","endPage":"533","costCenters":[{"id":365,"text":"Leetown Science Center","active":true,"usgs":true}],"links":[{"id":487156,"rank":2,"type":{"id":40,"text":"Open Access Publisher Index Page"},"url":"https://doi.org/10.1128/jvi.8.4.525-533.1971","text":"Publisher Index Page"},{"id":129494,"rank":1,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/thumbnails/outside_thumb.jpg"}],"volume":"8","issue":"4","noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"4f4e49e4e4b07f02db5e63c6","contributors":{"authors":[{"text":"Wolf, K.","contributorId":16344,"corporation":false,"usgs":true,"family":"Wolf","given":"K.","email":"","affiliations":[],"preferred":false,"id":319667,"contributorType":{"id":1,"text":"Authors"},"rank":1},{"text":"Darlington, R. W.","contributorId":64599,"corporation":false,"usgs":true,"family":"Darlington","given":"R.","email":"","middleInitial":"W.","affiliations":[],"preferred":false,"id":319668,"contributorType":{"id":1,"text":"Authors"},"rank":2}]}} ,{"id":1001628,"text":"1001628 - 1971 - A device for monitoring radio-marked animals","interactions":[],"lastModifiedDate":"2025-02-20T22:19:55.564904","indexId":"1001628","displayToPublicDate":"1971-10-01T00:00:00","publicationYear":"1971","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":"A device for monitoring radio-marked animals","docAbstract":"A simple, portable, and economical recording system consisting of a receiver, signal conditioner, recorder, and power source is described. The system was designed to monitor the signal strength from a radio-marked animal at a particular location. Information is stored on recorder chart paper. Radio-marked ducks have been successfully monitored at nest sites, potholes, and other locations.","language":"English","publisher":"Wiley","doi":"10.2307/3799793","usgsCitation":"Gilmer, D., Kuechle, V., and Ball, I., 1971, A device for monitoring radio-marked animals: Journal of Wildlife Management, v. 35, no. 4, p. 829-832, https://doi.org/10.2307/3799793.","productDescription":"4 p.","startPage":"829","endPage":"832","costCenters":[{"id":480,"text":"Northern Prairie Wildlife Research Center","active":true,"usgs":true}],"links":[{"id":130530,"rank":1,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/thumbnails/outside_thumb.jpg"}],"volume":"35","issue":"4","noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"4f4e4b24e4b07f02db6aecc0","contributors":{"authors":[{"text":"Gilmer, D.S.","contributorId":22270,"corporation":false,"usgs":true,"family":"Gilmer","given":"D.S.","email":"","affiliations":[],"preferred":false,"id":311378,"contributorType":{"id":1,"text":"Authors"},"rank":1},{"text":"Kuechle, V.B.","contributorId":83478,"corporation":false,"usgs":true,"family":"Kuechle","given":"V.B.","email":"","affiliations":[],"preferred":false,"id":311380,"contributorType":{"id":1,"text":"Authors"},"rank":2},{"text":"Ball, I.J. Jr.","contributorId":69503,"corporation":false,"usgs":true,"family":"Ball","given":"I.J.","suffix":"Jr.","email":"","affiliations":[],"preferred":false,"id":311379,"contributorType":{"id":1,"text":"Authors"},"rank":3}]}} ,{"id":5220482,"text":"5220482 - 1971 - Book review: Infectious and parasitic diseases of wild birds","interactions":[],"lastModifiedDate":"2025-04-04T16:13:36.767821","indexId":"5220482","displayToPublicDate":"1971-10-01T00:00:00","publicationYear":"1971","noYear":false,"publicationType":{"id":2,"text":"Article"},"publicationSubtype":{"id":10,"text":"Journal Article"},"seriesTitle":{"id":2507,"text":"Journal of Wildlife Diseases","active":true,"publicationSubtype":{"id":10}},"title":"Book review: Infectious and parasitic diseases of wild birds","docAbstract":"

No abstract available.

","language":"English","publisher":"Wildlife Disease Association","doi":"10.7589/0090-3558-7.4.339","usgsCitation":"Locke, L.N., 1971, Book review: Infectious and parasitic diseases of wild birds: Journal of Wildlife Diseases, v. 7, no. 4, p. 339-342, https://doi.org/10.7589/0090-3558-7.4.339.","productDescription":"4 p.","startPage":"339","endPage":"342","costCenters":[{"id":531,"text":"Patuxent Wildlife Research Center","active":true,"usgs":true}],"links":[{"id":487045,"rank":2,"type":{"id":40,"text":"Open Access Publisher Index Page"},"url":"https://doi.org/10.7589/0090-3558-7.4.339","text":"Publisher Index Page"},{"id":194012,"rank":1,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/thumbnails/outside_thumb.jpg"}],"volume":"7","issue":"4","noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"4f4e47e6e4b07f02db4bbc00","contributors":{"authors":[{"text":"Locke, L. N.","contributorId":73539,"corporation":false,"usgs":true,"family":"Locke","given":"L.","email":"","middleInitial":"N.","affiliations":[],"preferred":false,"id":331896,"contributorType":{"id":1,"text":"Authors"},"rank":1}]}} ]}