{"pageNumber":"6200","pageRowStart":"154975","pageSize":"25","recordCount":184938,"records":[{"id":5220962,"text":"5220962 - 1974 - An attempt to age mallards using eye lens proteins","interactions":[],"lastModifiedDate":"2025-02-26T21:59:28.666524","indexId":"5220962","displayToPublicDate":"1974-01-01T00:00:00","publicationYear":"1974","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":"An attempt to age mallards using eye lens proteins","docAbstract":"<p>An analysis of insoluble protein content of eye lenses from 59 known-age mallards (<i>Anas platyrhynchos</i>) indicated a slight increase between 8-9 months and 7 years of age. Nearly a complete overlapping of the insoluble protein content of individuals of different ages was apparent showing that the technique cannot be used to separate adult year classes of mallards. These results are contrary to findings reported for selected mammalian species; a possible explanation for the dissimilarity is discussed.</p>","language":"English","publisher":"Wiley","doi":"10.2307/3800209","usgsCitation":"Henny, C.J., and Ludke, J., 1974, An attempt to age mallards using eye lens proteins: Journal of Wildlife Management, v. 38, no. 1, p. 138-141, https://doi.org/10.2307/3800209.","productDescription":"4 p.","startPage":"138","endPage":"141","costCenters":[{"id":531,"text":"Patuxent Wildlife Research Center","active":true,"usgs":true}],"links":[{"id":198752,"rank":1,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/thumbnails/outside_thumb.jpg"}],"volume":"38","issue":"1","noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"4f4e4ad9e4b07f02db6852e8","contributors":{"authors":[{"text":"Henny, Charles J.","contributorId":12578,"corporation":false,"usgs":true,"family":"Henny","given":"Charles","email":"","middleInitial":"J.","affiliations":[],"preferred":false,"id":332763,"contributorType":{"id":1,"text":"Authors"},"rank":1},{"text":"Ludke, J. Larry","contributorId":29033,"corporation":false,"usgs":true,"family":"Ludke","given":"J. Larry","affiliations":[],"preferred":false,"id":332764,"contributorType":{"id":1,"text":"Authors"},"rank":2}]}}
,{"id":70010972,"text":"70010972 - 1974 - Heat flow from eastern Panama and northwestern Colombia","interactions":[],"lastModifiedDate":"2023-12-14T01:02:11.521091","indexId":"70010972","displayToPublicDate":"1974-01-01T00:00:00","publicationYear":"1974","noYear":false,"publicationType":{"id":2,"text":"Article"},"publicationSubtype":{"id":10,"text":"Journal Article"},"seriesTitle":{"id":1427,"text":"Earth and Planetary Science Letters","active":true,"publicationSubtype":{"id":10}},"title":"Heat flow from eastern Panama and northwestern Colombia","docAbstract":"<div id=\"abstracts\" class=\"Abstracts u-font-serif text-s\"><div id=\"ab1\" class=\"abstract author\" lang=\"en\"><div id=\"aep-abstract-sec-id6\"><p>Heat flows were determined at 12 sites in four distinct areas between longitude 77° and 80°W in eastern Panama and northwestern Colombia. Evidently, most of the region is underlain by mafic oceanic crust so that the crustal radiogenic component of heat flow is very small (∼ 0.1 μcal cm<sup>−2</sup><span>&nbsp;</span>sec<sup>−1</sup>). Low heat-flow values (∼ 0.7 μcal cm<sup>−2</sup><span>&nbsp;</span>sec<sup>−1</sup>) in northwestern Colombia may reflect thermal transients associated with shallow subduction. The normal values (∼ 1) at about 78°W are consistent with the mean heat flow from the western Caribbean and the Gulf of Mexico. At 80°W, a fairly high value of 1.8 may define the easterly limit of thermal transients due to Cenozoic volcanic activity in Central America.</p></div></div></div><ul id=\"issue-navigation\" class=\"issue-navigation u-margin-s-bottom u-bg-grey1\"></ul>","language":"English","publisher":"Elsevier","doi":"10.1016/0012-821X(74)90046-6","issn":"0012821X","usgsCitation":"Sass, J., Munroe, R.J., and Moses, T.H., 1974, Heat flow from eastern Panama and northwestern Colombia: Earth and Planetary Science Letters, v. 21, no. 2, p. 134-142, https://doi.org/10.1016/0012-821X(74)90046-6.","productDescription":"9 p.","startPage":"134","endPage":"142","numberOfPages":"9","costCenters":[],"links":[{"id":221208,"rank":1,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/thumbnails/outside_thumb.jpg"}],"country":"Columbia, Panama","geographicExtents":"{\n  \"type\": \"FeatureCollection\",\n  \"features\": [\n    {\n      \"type\": \"Feature\",\n      \"properties\": {},\n      \"geometry\": {\n        \"type\": \"Polygon\",\n        \"coordinates\": [\n          [\n            [\n              -82.79296874999999,\n              -3.513421045640032\n            ],\n            [\n              -66.09375,\n              -3.513421045640032\n            ],\n            [\n              -66.09375,\n              9.535748998133627\n            ],\n            [\n              -82.79296874999999,\n              9.535748998133627\n            ],\n            [\n              -82.79296874999999,\n              -3.513421045640032\n            ]\n          ]\n        ]\n      }\n    }\n  ]\n}","volume":"21","issue":"2","noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"505a2ffde4b0c8380cd5d2a1","contributors":{"authors":[{"text":"Sass, J.H.","contributorId":70749,"corporation":false,"usgs":true,"family":"Sass","given":"J.H.","email":"","affiliations":[{"id":595,"text":"U.S. Geological Survey","active":false,"usgs":true}],"preferred":false,"id":360002,"contributorType":{"id":1,"text":"Authors"},"rank":1},{"text":"Munroe, R. J.","contributorId":56215,"corporation":false,"usgs":true,"family":"Munroe","given":"R.","email":"","middleInitial":"J.","affiliations":[],"preferred":false,"id":360000,"contributorType":{"id":1,"text":"Authors"},"rank":2},{"text":"Moses, T. H. Jr.","contributorId":70385,"corporation":false,"usgs":true,"family":"Moses","given":"T.","suffix":"Jr.","email":"","middleInitial":"H.","affiliations":[],"preferred":false,"id":360001,"contributorType":{"id":1,"text":"Authors"},"rank":3}]}}
,{"id":70011016,"text":"70011016 - 1974 - Comparison of elemental accumulation rates between ferromanganese deposits and sediments in the South Pacific Ocean","interactions":[],"lastModifiedDate":"2021-01-15T14:14:57.113683","indexId":"70011016","displayToPublicDate":"1974-01-01T00:00:00","publicationYear":"1974","noYear":false,"publicationType":{"id":2,"text":"Article"},"publicationSubtype":{"id":10,"text":"Journal Article"},"seriesTitle":{"id":1213,"text":"Chemical Geology","active":true,"publicationSubtype":{"id":10}},"title":"Comparison of elemental accumulation rates between ferromanganese deposits and sediments in the South Pacific Ocean","docAbstract":"<p id=\"simple-para.0010\">Rates of accumulation of Fe and Mn, as well as Cu, Ni, Co, Pb, Zn, Hg, U and Th have been determined for five ferromanganese deposits from four localities in the South Pacific Ocean.</p><p id=\"simple-para.0015\">Manganese is accumulating in nodules and crusts at a rate roughly equivalent to that found to be accumulating in sediments in the same area. Iron shows a deficiency in accumulation in nodules and crusts with respect to sediments, especially near the continents, but also in the central and south-central Pacific. Copper is accumulating in nodules and crusts at a rate one order of magnitude less than the surrounding sediments.</p><p id=\"simple-para.0020\">This is interpreted as meaning that most of the Mn is supplied as an authigenic phase to both sediments and nodules while Fe is supplied mostly by ferromanganese micro-nodules and by detrital and adsorbed components of sediments; and Cu is enriched in sediments relative to nodules and crusts most probably through biological activity.</p>","language":"English","publisher":"Elsevier","doi":"10.1016/0009-2541(74)90019-9","issn":"00092541","usgsCitation":"Kraemer, T., and Schornick, J., 1974, Comparison of elemental accumulation rates between ferromanganese deposits and sediments in the South Pacific Ocean: Chemical Geology, v. 13, no. 3, p. 187-196, https://doi.org/10.1016/0009-2541(74)90019-9.","productDescription":"10 p.","startPage":"187","endPage":"196","numberOfPages":"10","costCenters":[],"links":[{"id":221716,"rank":0,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/thumbnails/outside_thumb.jpg"}],"volume":"13","issue":"3","noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"5059f85ee4b0c8380cd4d066","contributors":{"authors":[{"text":"Kraemer, T.","contributorId":90040,"corporation":false,"usgs":true,"family":"Kraemer","given":"T.","affiliations":[],"preferred":false,"id":360093,"contributorType":{"id":1,"text":"Authors"},"rank":1},{"text":"Schornick, J.C.","contributorId":49790,"corporation":false,"usgs":true,"family":"Schornick","given":"J.C.","affiliations":[],"preferred":false,"id":360092,"contributorType":{"id":1,"text":"Authors"},"rank":2}]}}
,{"id":1689,"text":"wsp2033 - 1974 - Availability of ground water in the lower Pawcatuck River basin, Rhode Island","interactions":[],"lastModifiedDate":"2023-10-31T20:19:36.788644","indexId":"wsp2033","displayToPublicDate":"1974-01-01T00:00:00","publicationYear":"1974","noYear":false,"publicationType":{"id":18,"text":"Report"},"publicationSubtype":{"id":5,"text":"USGS Numbered Series"},"seriesTitle":{"id":341,"text":"Water Supply Paper","code":"WSP","active":false,"publicationSubtype":{"id":5}},"seriesNumber":"2033","title":"Availability of ground water in the lower Pawcatuck River basin, Rhode Island","docAbstract":"The lower Pawcatuck River basin in southwestern Rhode Island is an area of about 169 square miles underlain by crystalline bedrock over which lies a relatively thin mantle of glacial till and stratified drift. Stratified drift, consisting dominantly of sand and gravel, occurs in irregularly shaped linear deposits that are generally less than a mile wide and less than 125 feet thick; these deposits are found along the Pawcatuck River, its tributaries, and abandoned preglacial channels. Deposits of stratified sand and gravel constitute the principal aquifer in the lower Pawcatuck basin and the only one capable of sustaining yields of 100 gallons per minute or more to individual wells. \r\n\r\nWater available for development in this aquifer consists of water in storage--potential ground-water runoff to streams--plus infiltration that can be induced from streams. Minimum annual ground-water runoff from the sand and gravel aquifer is calculated to be at least 1.17 cubic feet per second per square mile, or 0.76 million gallons per day per square mile. Potential recharge by induced infiltration is estimated to range from about 250 to 600 gallons per day per linear foot of streambed for the principal streams. In most areas, induced infiltration from streams constitutes the major source of water potentially available for development by wells. \r\n\r\nBecause subsurface hydraulic connection in the sand and gravel aquifer is poor in several places, the deposits are conveniently divisible into several ground-water reservoirs. The potential yield from five of the most promising ground-water reservoirs is evaluated by means of mathematical models. Results indicate that continuous withdrawals ranging from 1.3 to 10.3 million gallons per day, and totaling 31 million gallons per day, are obtainable from these reservoirs. Larger yields may be recovered by different well placement, spacing, construction and development, pumping practice, and so forth. \r\n\r\nWithdrawals at the rates indicated will reduce streamflow downstream from pumping centers but generally will not result in streams going dry, provided the water is returned to the basin. Export of water from the basin will require careful consideration of the effects of such withdrawals on low streamflow. Export from the Pawcatuck basin of 27 million gallons per day, estimated to be available from ground-water reservoirs in the upper Pawcatuck basin, in addition to 37.5 million gallons per day available in the lower Pawcatuck basin, will markedly reduce low streamflow. The 90-percent duration flow of the Pawcatuck River at Westerly would be reduced from 75 million gallons per day to perhaps as little as 21 million gallons per day. \r\n\r\nThe chemical quality of water from both the sand and gravel aquifer and associated streams is suitable for most purposes. The water is soft, slightly acidic, and typically has a dissolved-solids content of less than 75 milligrams per liter. Some treatment may be required locally for removal of iron and manganese to meet recommended standards of the U.S. Public Health Service for drinking water.","language":"English","publisher":"U.S. Geological Survey","doi":"10.3133/wsp2033","usgsCitation":"Gonthier, J.B., Johnston, H.E., and Malmberg, G.T., 1974, Availability of ground water in the lower Pawcatuck River basin, Rhode Island: U.S. Geological Survey Water Supply Paper 2033, Report: iv, 40 p.; 5 Plates: 20.00 x 38.88 inches or smaller, https://doi.org/10.3133/wsp2033.","productDescription":"Report: iv, 40 p.; 5 Plates: 20.00 x 38.88 inches or smaller","costCenters":[],"links":[{"id":422303,"rank":8,"type":{"id":36,"text":"NGMDB Index Page"},"url":"https://ngmdb.usgs.gov/Prodesc/proddesc_25524.htm","linkFileType":{"id":5,"text":"html"}},{"id":26771,"rank":5,"type":{"id":17,"text":"Plate"},"url":"https://pubs.usgs.gov/wsp/2033/plate-3.pdf","linkFileType":{"id":1,"text":"pdf"}},{"id":26769,"rank":3,"type":{"id":17,"text":"Plate"},"url":"https://pubs.usgs.gov/wsp/2033/plate-1.pdf","linkFileType":{"id":1,"text":"pdf"}},{"id":137039,"rank":1,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/wsp/2033/report-thumb.jpg"},{"id":26773,"rank":7,"type":{"id":17,"text":"Plate"},"url":"https://pubs.usgs.gov/wsp/2033/plate-5.pdf","linkFileType":{"id":1,"text":"pdf"}},{"id":26772,"rank":6,"type":{"id":17,"text":"Plate"},"url":"https://pubs.usgs.gov/wsp/2033/plate-4.pdf","linkFileType":{"id":1,"text":"pdf"}},{"id":26774,"rank":2,"type":{"id":11,"text":"Document"},"url":"https://pubs.usgs.gov/wsp/2033/report.pdf","linkFileType":{"id":1,"text":"pdf"}},{"id":26770,"rank":4,"type":{"id":17,"text":"Plate"},"url":"https://pubs.usgs.gov/wsp/2033/plate-2.pdf","linkFileType":{"id":1,"text":"pdf"}}],"country":"United States","state":"Rhode Island","otherGeospatial":"lower Pawcatuck River basin","geographicExtents":"{\n  \"type\": \"FeatureCollection\",\n  \"features\": [\n    {\n      \"type\": \"Feature\",\n      \"properties\": {},\n      \"geometry\": {\n        \"coordinates\": [\n          [\n            [\n              -71.843,\n              41.667\n            ],\n            [\n              -71.843,\n              41.345\n            ],\n            [\n              -71.614,\n              41.345\n            ],\n            [\n              -71.614,\n              41.667\n            ],\n            [\n              -71.843,\n              41.667\n            ]\n          ]\n        ],\n        \"type\": \"Polygon\"\n      }\n    }\n  ]\n}","noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"4f4e4a9ae4b07f02db65d91d","contributors":{"authors":[{"text":"Gonthier, Joseph B.","contributorId":74350,"corporation":false,"usgs":true,"family":"Gonthier","given":"Joseph","email":"","middleInitial":"B.","affiliations":[{"id":595,"text":"U.S. Geological Survey","active":false,"usgs":true}],"preferred":false,"id":143976,"contributorType":{"id":1,"text":"Authors"},"rank":1},{"text":"Johnston, Herbert E.","contributorId":16392,"corporation":false,"usgs":true,"family":"Johnston","given":"Herbert","email":"","middleInitial":"E.","affiliations":[],"preferred":false,"id":143975,"contributorType":{"id":1,"text":"Authors"},"rank":2},{"text":"Malmberg, Glenn T.","contributorId":11196,"corporation":false,"usgs":true,"family":"Malmberg","given":"Glenn","email":"","middleInitial":"T.","affiliations":[],"preferred":false,"id":143974,"contributorType":{"id":1,"text":"Authors"},"rank":3}]}}
,{"id":1013723,"text":"1013723 - 1974 - Various fish species as biological control agents for the dark rice field mosquito in Arkansas rice fields","interactions":[],"lastModifiedDate":"2023-10-25T14:37:41.0231","indexId":"1013723","displayToPublicDate":"1974-01-01T00:00:00","publicationYear":"1974","noYear":false,"publicationType":{"id":2,"text":"Article"},"publicationSubtype":{"id":10,"text":"Journal Article"},"seriesTitle":{"id":1536,"text":"Environmental Entomology","active":true,"publicationSubtype":{"id":10}},"title":"Various fish species as biological control agents for the dark rice field mosquito in Arkansas rice fields","docAbstract":"<p><span>During the summers of 1972–73, 10 fish species were evaluated as predators against larvae of the dark rice field mosquito,&nbsp;</span><i>Psorophora confinnis</i><span>&nbsp;(Lynch-Arribalzaga), near Stuttgart, Ark. Stocking rates were 0.02, 0.03, and 0.06 fish/ft&nbsp;</span><sup>2</sup><span>&nbsp;. At the lowest stocking rate green sunfish,&nbsp;</span><i>Lepomis cyanellus</i><span>&nbsp;Rafinesque, reduced larval numbers by 89.7% and were significantly more effective than adult mosquitofish,&nbsp;</span><i>Gambusia affinis</i><span>&nbsp;(Baird and Girard). The white amur,&nbsp;</span><i>Ctenopharynogodon idella</i><span>&nbsp;Valenciennes, was intermediate in effectiveness when compared with the above. At 0.03 fish/ft&nbsp;</span><sup>2</sup><span>&nbsp;, green sunfish reduced larvae by 99.2% and were significantly more efficient than juvenile mosquitofish, which had little effect on the larval population. At the 0.06 fish/ft&nbsp;</span><sup>2</sup><span>&nbsp;rate mosquitofish; white amur; Israeli carp,&nbsp;</span><i>Cyprinus carpio</i><span>&nbsp;L.; and hybrids (Israeli carp × goldfish) were significantly more effective than bigmouth buffalo,&nbsp;</span><i>Ictiobus cyprinellus</i><span>&nbsp;(Valenciennes); black buffalo,&nbsp;</span><i>Ictiobus niger</i><span>&nbsp;(Rafinesque); goldfish,&nbsp;</span><i>Carassius auratus</i><span>&nbsp;(L.); or juvenile mosquitofish. Recovery counts of fish indicated that fish survived under natural conditions in Arkansas rice fields.</span></p>","language":"English","publisher":"Oxford Academic","doi":"10.1093/ee/3.5.823","usgsCitation":"Davey, R.B., Meisch, M.V., Gray, D.L., Martin, J.M., Sneed, K.E., and Williams, F.J., 1974, Various fish species as biological control agents for the dark rice field mosquito in Arkansas rice fields: Environmental Entomology, v. 3, no. 5, p. 823-826, https://doi.org/10.1093/ee/3.5.823.","productDescription":"4 p.","startPage":"823","endPage":"826","numberOfPages":"4","costCenters":[{"id":365,"text":"Leetown Science Center","active":true,"usgs":true}],"links":[{"id":129407,"rank":1,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/thumbnails/outside_thumb.jpg"}],"country":"United 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,{"id":70168589,"text":"70168589 - 1974 - Searching for prehistoric earthquakes in lake sediments","interactions":[],"lastModifiedDate":"2016-03-22T14:57:26","indexId":"70168589","displayToPublicDate":"1974-01-01T00:00:00","publicationYear":"1974","noYear":false,"publicationType":{"id":2,"text":"Article"},"publicationSubtype":{"id":10,"text":"Journal Article"},"seriesTitle":{"id":1435,"text":"Earthquake Information Bulletin (USGS)","active":true,"publicationSubtype":{"id":10}},"title":"Searching for prehistoric earthquakes in lake sediments","docAbstract":"<p>How often do major earthquakes occur? Do they follow regular patterns of recurrence, and if so, what is the length of the recurrence interval? These questions are of obvious importance to populations located in regions where earthquakes are a commonplace occurrence. They are also relevant questions in regions that are for the most part seismically inactive but that have &nbsp;experienced anomalous earthquakes of destructive force one or more times in recorded history. Also, what about areas that have never experienced an earthquake in historic times? Human history is short when compared to the geologic time scale. Is it possible that places which we regard as seismically inactive might actually have experienced a major earthquake in the recent geologic past? Historic records of earthquakes are too short to allow a true assessment of recurrence intervals; therefore, a method is needed that will enable the seismic history of a region to be exteneded beyond the limit of historic time. &nbsp;&nbsp;</p>","language":"English","publisher":"U.S Geological Survey","usgsCitation":"Sims, J., 1974, Searching for prehistoric earthquakes in lake sediments: Earthquake Information Bulletin (USGS), v. 6, no. 1, p. 3-9.","productDescription":"7 p.","startPage":"3","endPage":"9","onlineOnly":"N","additionalOnlineFiles":"N","costCenters":[],"links":[{"id":318207,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/thumbnails/outside_thumb.jpg"}],"volume":"6","issue":"1","noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"56c99c53e4b059daa47c9ae5","contributors":{"authors":[{"text":"Sims, J.","contributorId":167094,"corporation":false,"usgs":false,"family":"Sims","given":"J.","affiliations":[],"preferred":false,"id":620988,"contributorType":{"id":1,"text":"Authors"},"rank":1}]}}
,{"id":70168599,"text":"70168599 - 1974 - The California geodimeter network; measuring movement along the San Andreas Fault","interactions":[],"lastModifiedDate":"2019-11-14T08:32:18","indexId":"70168599","displayToPublicDate":"1974-01-01T00:00:00","publicationYear":"1974","noYear":false,"publicationType":{"id":2,"text":"Article"},"publicationSubtype":{"id":10,"text":"Journal Article"},"seriesTitle":{"id":1435,"text":"Earthquake Information Bulletin (USGS)","active":true,"publicationSubtype":{"id":10}},"title":"The California geodimeter network; measuring movement along the San Andreas Fault","docAbstract":"<p>Following the great California earthquake of 1906 H. F. Reid, a contemporary seismologist, proposed the elastic rebound theory which in effect says that earthquake potential arises from the accumulation of elastic strain within the Earth's crust, just as the stretching of a rubberband creates the potential for violent rebound upon rupture. A direct manifestation of this crustal strain accumulation is the change in distance between adjacent points along opposite sides of a fault. In order to measure the rate at which strain is accumulating along California's San Andreas fault, a netwrok of precise survey lines which criss-cross the fault along its entire lenght in the State is periodically resurveyed with very accurate electro-opitcal distance measuring devices called geodimeters.&nbsp;</p>","language":"English","publisher":"U.S Geological Survey","publisherLocation":"Reston, VA","usgsCitation":"Savage, J., 1974, The California geodimeter network; measuring movement along the San Andreas Fault: Earthquake Information Bulletin (USGS), v. 6, no. 3, p. 3-7.","productDescription":"4 p.","startPage":"3","endPage":"7","onlineOnly":"N","additionalOnlineFiles":"N","costCenters":[],"links":[{"id":318217,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/thumbnails/outside_thumb.jpg"}],"country":"United States","state":"California","geographicExtents":"{\n  \"type\": \"FeatureCollection\",\n  \"features\": [\n    {\n      \"type\": \"Feature\",\n      \"properties\": {},\n      \"geometry\": {\n        \"type\": \"Polygon\",\n        \"coordinates\": [\n          [\n            [\n              -122.78320312499999,\n              41.178653972331674\n            ],\n            [\n              -124.23339843749999,\n              40.58058466412761\n            ],\n            [\n              -123.57421875,\n              38.788345355085625\n            ],\n            [\n              -121.1572265625,\n              34.63320791137959\n            ],\n            [\n              -117.02636718749999,\n              33.43144133557529\n            ],\n            [\n              -116.71874999999999,\n              34.488447837809304\n            ],\n            [\n              -120.2783203125,\n              38.06539235133249\n            ],\n            [\n              -122.78320312499999,\n              41.178653972331674\n            ]\n          ]\n        ]\n      }\n    }\n  ]\n}","volume":"6","issue":"3","noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"56c99c54e4b059daa47c9b02","contributors":{"authors":[{"text":"Savage, J.C. 0000-0002-5114-7673","orcid":"https://orcid.org/0000-0002-5114-7673","contributorId":102876,"corporation":false,"usgs":true,"family":"Savage","given":"J.C.","affiliations":[],"preferred":false,"id":621002,"contributorType":{"id":1,"text":"Authors"},"rank":1}]}}
,{"id":70168582,"text":"70168582 - 1974 - Seismicity and earthquake hazards of the Wasatch Front, Utah","interactions":[],"lastModifiedDate":"2016-03-22T14:42:27","indexId":"70168582","displayToPublicDate":"1974-01-01T00:00:00","publicationYear":"1974","noYear":false,"publicationType":{"id":2,"text":"Article"},"publicationSubtype":{"id":10,"text":"Journal Article"},"seriesTitle":{"id":1435,"text":"Earthquake Information Bulletin (USGS)","active":true,"publicationSubtype":{"id":10}},"title":"Seismicity and earthquake hazards of the Wasatch Front, Utah","docAbstract":"<p>The impressive topographic break at the base of the Wasatch Range immediately east of Salt Lake City, Utah, marks the location where Mormon colonizer Brigham Young said in 1847. \"This is the place\" Actually, \"the place\" is termed the Wasatch Front because the Wasatch Range to the east, which rises to heights of 3,600 m, fronts the valleys to the west. The densely settled Wasatch Front area has about 900,000 people, 80 percent of Utah's total population. This population is centered around Salt Lake City, a rapidly growing industrial and tourist center.&nbsp;</p>","language":"English","publisher":"U.S Geological Survey","usgsCitation":"Spall, H., 1974, Seismicity and earthquake hazards of the Wasatch Front, Utah: Earthquake Information Bulletin (USGS), v. 6, no. 4, p. 12-17.","productDescription":"6 p.","startPage":"12","endPage":"17","onlineOnly":"N","additionalOnlineFiles":"N","costCenters":[],"links":[{"id":318202,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/thumbnails/outside_thumb.jpg"}],"country":"United States","state":"Utah","otherGeospatial":"Wasatch Front","geographicExtents":"{\n  \"type\": \"FeatureCollection\",\n  \"features\": [\n    {\n      \"type\": \"Feature\",\n      \"properties\": {},\n      \"geometry\": {\n        \"type\": \"Polygon\",\n        \"coordinates\": [\n          [\n            [\n              -111.9451904296875,\n              39.63530729658601\n            ],\n            [\n              -111.796875,\n              39.64799732373418\n            ],\n            [\n              -111.7913818359375,\n              39.825413103424786\n            ],\n            [\n              -111.7529296875,\n              40.01078714046552\n            ],\n            [\n              -111.566162109375,\n              40.10328591293442\n            ],\n            [\n              -111.676025390625,\n              40.333983227838104\n            ],\n            [\n              -111.785888671875,\n              40.49291502689579\n            ],\n            [\n              -111.829833984375,\n              40.826280356677124\n            ],\n            [\n              -111.8792724609375,\n              41.17451935556443\n            ],\n            [\n              -112.0001220703125,\n              41.35207214451295\n            ],\n            [\n              -112.0660400390625,\n              41.6770148220322\n            ],\n            [\n              -112.09899902343749,\n              41.75082413553287\n            ],\n            [\n              -112.1759033203125,\n              42.00032514831621\n            ],\n            [\n              -112.2747802734375,\n              42.00032514831621\n            ],\n            [\n              -112.2308349609375,\n              41.49623534616764\n            ],\n            [\n              -112.236328125,\n              41.19105625669688\n            ],\n            [\n              -111.983642578125,\n              40.979898069620155\n            ],\n            [\n              -112.1319580078125,\n              40.81380923056961\n            ],\n            [\n              -112.03857421875,\n              40.48455955508278\n            ],\n            [\n              -111.96716308593749,\n              39.787433886224406\n            ],\n            [\n              -111.9451904296875,\n              39.63530729658601\n            ]\n          ]\n        ]\n      }\n    }\n  ]\n}","volume":"6","issue":"4","noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"56c84acce4b0b3c9ae3810a1","contributors":{"authors":[{"text":"Spall, H.","contributorId":99290,"corporation":false,"usgs":true,"family":"Spall","given":"H.","affiliations":[],"preferred":false,"id":620950,"contributorType":{"id":1,"text":"Authors"},"rank":1}]}}
,{"id":70168606,"text":"70168606 - 1974 - Earthquake prediction; new studies yield promising results","interactions":[],"lastModifiedDate":"2016-03-22T16:30:24","indexId":"70168606","displayToPublicDate":"1974-01-01T00:00:00","publicationYear":"1974","noYear":false,"publicationType":{"id":2,"text":"Article"},"publicationSubtype":{"id":10,"text":"Journal Article"},"seriesTitle":{"id":1435,"text":"Earthquake Information Bulletin (USGS)","active":true,"publicationSubtype":{"id":10}},"title":"Earthquake prediction; new studies yield promising results","docAbstract":"<p>On Agust 3, 1973, a small earthquake (magnitude 2.5) occurred near Blue Mountain Lake in the Adirondack region of northern New York State. This seemingly unimportant event was of great significance, however, because it was predicted. Seismologsits at the Lamont-Doherty geologcal Observatory of Columbia University accurately foretold the time, place, and magnitude of the event. Their prediction was based on certain pre-earthquake processes that are best explained by a hypothesis known as \"dilatancy,\" a concept that has injected new life and direction into the science of earthquake prediction. Although much mroe reserach must be accomplished before we can expect to predict potentially damaging earthquakes with any degree of consistency, results such as this indicate that we are on a promising road.&nbsp;</p>","language":"English","publisher":"U.S Geological Survey","usgsCitation":"Robinson, R., 1974, Earthquake prediction; new studies yield promising results: Earthquake Information Bulletin (USGS), v. 6, no. 2, p. 14-17.","productDescription":"4 p.","startPage":"14","endPage":"17","onlineOnly":"N","additionalOnlineFiles":"N","costCenters":[],"links":[{"id":318224,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/thumbnails/outside_thumb.jpg"}],"volume":"6","issue":"2","noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"56c99c45e4b059daa47c9aa5","contributors":{"authors":[{"text":"Robinson, R.","contributorId":99694,"corporation":false,"usgs":true,"family":"Robinson","given":"R.","affiliations":[],"preferred":false,"id":621013,"contributorType":{"id":1,"text":"Authors"},"rank":1}]}}
,{"id":70010202,"text":"70010202 - 1974 - The role of lava erosion in the formation of lunar rilles and Martian channels","interactions":[],"lastModifiedDate":"2021-01-22T14:19:57.287669","indexId":"70010202","displayToPublicDate":"1974-01-01T00:00:00","publicationYear":"1974","noYear":false,"publicationType":{"id":2,"text":"Article"},"publicationSubtype":{"id":10,"text":"Journal Article"},"seriesTitle":{"id":1963,"text":"Icarus","active":true,"publicationSubtype":{"id":10}},"title":"The role of lava erosion in the formation of lunar rilles and Martian channels","docAbstract":"<div id=\"abstracts\" class=\"Abstracts u-font-serif\"><div id=\"aep-abstract-id4\" class=\"abstract author\"><div id=\"aep-abstract-sec-id5\"><p>Lava tubes and channels develop around active sources of low viscosity lava. The channels normally form without erosion; however, sustained flow can result in the incision of a lava channel and simulation of fluvial erosion features. Lava erosion by means of thermal incision was modelled by computer, erosion rates calculated, and these compared with rates observed terrestrially. Lunar sinuous rilles are examined in light of the proposed lava erosion. The mechanism explains many features of lunar rilles that were heretofore puzzling and implies erosion rates comparable to terrestrial rates. Many Mars channels also appear to form by the action of lava; however, the larger, more spectacular Mars channels do not appear to have been formed by the same process.</p></div></div></div><ul id=\"issue-navigation\" class=\"issue-navigation u-margin-s-bottom u-bg-grey1\"></ul>","language":"English","publisher":"Elsevier","doi":"10.1016/0019-1035(74)90162-6","issn":"00191035","usgsCitation":"Carr, M.H., 1974, The role of lava erosion in the formation of lunar rilles and Martian channels: Icarus, v. 22, no. 1, p. 1-23, https://doi.org/10.1016/0019-1035(74)90162-6.","productDescription":"23 p.","startPage":"1","endPage":"23","numberOfPages":"23","costCenters":[],"links":[{"id":218935,"rank":0,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/thumbnails/outside_thumb.jpg"}],"volume":"22","issue":"1","noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"505baf7de4b08c986b324827","contributors":{"authors":[{"text":"Carr, M. H.","contributorId":84727,"corporation":false,"usgs":true,"family":"Carr","given":"M.","email":"","middleInitial":"H.","affiliations":[{"id":131,"text":"Astrogeology Science Center","active":true,"usgs":true}],"preferred":false,"id":358302,"contributorType":{"id":1,"text":"Authors"},"rank":1}]}}
,{"id":70174346,"text":"70174346 - 1974 - Aerial observations of suspended sediment plumes in San Francisco Bay and the adjacent Pacific Ocean","interactions":[],"lastModifiedDate":"2016-07-26T16:31:21","indexId":"70174346","displayToPublicDate":"1974-01-01T00:00:00","publicationYear":"1974","noYear":false,"publicationType":{"id":2,"text":"Article"},"publicationSubtype":{"id":10,"text":"Journal Article"},"seriesTitle":{"id":2446,"text":"Journal of Research of the U.S. Geological Survey","active":true,"publicationSubtype":{"id":10}},"title":"Aerial observations of suspended sediment plumes in San Francisco Bay and the adjacent Pacific Ocean","docAbstract":"<p>No abstract avaiable&nbsp;</p>","language":"English","publisher":"U.S Geological Survey","usgsCitation":"Carlson, P., and McCulloch, D.S., 1974, Aerial observations of suspended sediment plumes in San Francisco Bay and the adjacent Pacific Ocean: Journal of Research of the U.S. Geological Survey, v. 2, p. 519-526.","productDescription":"8 p.","startPage":"519","endPage":"526","onlineOnly":"N","additionalOnlineFiles":"N","costCenters":[{"id":552,"text":"San Francisco Bay-Delta","active":false,"usgs":true},{"id":5079,"text":"Pacific Regional Director's Office","active":true,"usgs":true}],"links":[{"id":324954,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/thumbnails/outside_thumb.jpg"},{"id":324953,"rank":1,"type":{"id":15,"text":"Index Page"},"url":"https://nmbl.org/cgi-bin/koha/opac-detail.pl?biblionumber=50435&shelfbrowse_itemnumber=50858"}],"volume":"2","noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"5780ceafe4b08116168222a4","contributors":{"authors":[{"text":"Carlson, P.R.","contributorId":97055,"corporation":false,"usgs":true,"family":"Carlson","given":"P.R.","email":"","affiliations":[],"preferred":false,"id":641983,"contributorType":{"id":1,"text":"Authors"},"rank":1},{"text":"McCulloch, D. S.","contributorId":78315,"corporation":false,"usgs":true,"family":"McCulloch","given":"D.","email":"","middleInitial":"S.","affiliations":[],"preferred":false,"id":641984,"contributorType":{"id":1,"text":"Authors"},"rank":2}]}}
,{"id":1001230,"text":"1001230 - 1974 - The prairie: to know it is to appreciate it","interactions":[],"lastModifiedDate":"2018-01-02T13:15:53","indexId":"1001230","displayToPublicDate":"1974-01-01T00:00:00","publicationYear":"1974","noYear":false,"publicationType":{"id":2,"text":"Article"},"publicationSubtype":{"id":10,"text":"Journal Article"},"seriesTitle":{"id":1365,"text":"Dakota Farmer","active":true,"publicationSubtype":{"id":10}},"title":"The prairie: to know it is to appreciate it","docAbstract":"Abstract has not been submitted","largerWorkType":{"id":2,"text":"Article"},"largerWorkTitle":"Dakota Farmer","largerWorkSubtype":{"id":10,"text":"Journal Article"},"language":"English","usgsCitation":"Lokemoen, J.T., and Krapu, G., 1974, The prairie: to know it is to appreciate it: Dakota Farmer, v. 94, no. 7, p. 38-39.","productDescription":"2 p.","startPage":"38","endPage":"39","costCenters":[{"id":480,"text":"Northern Prairie Wildlife Research Center","active":true,"usgs":true}],"links":[{"id":130644,"rank":0,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/thumbnails/outside_thumb.jpg"}],"volume":"94","issue":"7","noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"4f4e4a70e4b07f02db641c68","contributors":{"authors":[{"text":"Lokemoen, J. T.","contributorId":79049,"corporation":false,"usgs":true,"family":"Lokemoen","given":"J.","email":"","middleInitial":"T.","affiliations":[],"preferred":false,"id":310726,"contributorType":{"id":1,"text":"Authors"},"rank":1},{"text":"Krapu, Gary L.","contributorId":56994,"corporation":false,"usgs":true,"family":"Krapu","given":"Gary L.","affiliations":[],"preferred":false,"id":310725,"contributorType":{"id":1,"text":"Authors"},"rank":2}]}}
,{"id":1001205,"text":"1001205 - 1974 - Nematode parasites of waterfowl (Anseriformes) from western United States","interactions":[],"lastModifiedDate":"2018-01-04T10:54:41","indexId":"1001205","displayToPublicDate":"1974-01-01T00:00:00","publicationYear":"1974","noYear":false,"publicationType":{"id":2,"text":"Article"},"publicationSubtype":{"id":10,"text":"Journal Article"},"seriesTitle":{"id":3768,"text":"Wildlife Disease","active":true,"publicationSubtype":{"id":10}},"title":"Nematode parasites of waterfowl (Anseriformes) from western United States","docAbstract":"Thirty-four species of nematodes were found in 415 Anseriformes (Anatidae) of 27 species; 93.7% of birds over 4 weeks old were infected. Data on prevalence, host specificity, age of host, and geographic distribution are given. Infections were more intense in sick birds and birds in poor physical condition. Accidental or abnormal infection was more likely in sick than in normal birds. From 1 to 13 species of nematodes are reported from each host species, including 118 new host records, 3 nematodes new for North America, and 1 new species. Multiple infections were present in 76.5% of birds parasitized; eight species of nematodes were found in one whistling swan (Olor columbianus).","largerWorkType":{"id":2,"text":"Article"},"largerWorkTitle":"Wildlife Disease","largerWorkSubtype":{"id":10,"text":"Journal Article"},"language":"English","publisher":"U.S. Fish and Wildlife Service","usgsCitation":"McDonald, M., 1974, Nematode parasites of waterfowl (Anseriformes) from western United States: Wildlife Disease, no. 64, p. 19-19.","productDescription":"1 p.","startPage":"19","endPage":"19","costCenters":[{"id":480,"text":"Northern Prairie Wildlife Research Center","active":true,"usgs":true}],"links":[{"id":129103,"rank":0,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/thumbnails/outside_thumb.jpg"}],"issue":"64","noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"4f4e4affe4b07f02db697e1b","contributors":{"authors":[{"text":"McDonald, M.E.","contributorId":33661,"corporation":false,"usgs":true,"family":"McDonald","given":"M.E.","email":"","affiliations":[],"preferred":false,"id":310700,"contributorType":{"id":1,"text":"Authors"},"rank":1}]}}
,{"id":7000075,"text":"7000075 - 1974 - Landslides","interactions":[],"lastModifiedDate":"2012-02-02T00:15:08","indexId":"7000075","displayToPublicDate":"1974-01-01T00:00:00","publicationYear":"1974","noYear":false,"publicationType":{"id":18,"text":"Report"},"publicationSubtype":{"id":6,"text":"USGS Unnumbered Series"},"seriesTitle":{"id":363,"text":"General Interest Publication","active":false,"publicationSubtype":{"id":6}},"title":"Landslides","language":"ENGLISH","doi":"10.3133/7000075","usgsCitation":"Water Resources Division, U.S. Geological Survey, 1974, Landslides: General Interest Publication, 8 p., https://doi.org/10.3133/7000075.","productDescription":"8 p.","costCenters":[],"links":[{"id":196278,"rank":0,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/thumbnails/usgs_thumb.jpg"}],"noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"4f4e4b1fe4b07f02db6ab803","contributors":{"authors":[{"text":"Water Resources Division, U.S. Geological Survey","contributorId":128075,"corporation":true,"usgs":false,"organization":"Water Resources Division, U.S. Geological Survey","id":535098,"contributorType":{"id":1,"text":"Authors"},"rank":1}]}}
,{"id":7000076,"text":"7000076 - 1974 - The United States Geological Survey","interactions":[],"lastModifiedDate":"2012-02-02T00:15:08","indexId":"7000076","displayToPublicDate":"1974-01-01T00:00:00","publicationYear":"1974","noYear":false,"publicationType":{"id":18,"text":"Report"},"publicationSubtype":{"id":6,"text":"USGS Unnumbered Series"},"seriesTitle":{"id":363,"text":"General Interest Publication","active":false,"publicationSubtype":{"id":6}},"title":"The United States Geological Survey","language":"ENGLISH","doi":"10.3133/7000076","usgsCitation":"Water Resources Division, U.S. Geological Survey, 1974, The United States Geological Survey: General Interest Publication, 27 p. : ill. ; 24 cm., https://doi.org/10.3133/7000076.","productDescription":"27 p. : ill. ; 24 cm.","costCenters":[],"links":[{"id":196279,"rank":0,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/thumbnails/usgs_thumb.jpg"}],"noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"4f4e4ab0e4b07f02db66d5f7","contributors":{"authors":[{"text":"Water Resources Division, U.S. Geological Survey","contributorId":128075,"corporation":true,"usgs":false,"organization":"Water Resources Division, U.S. Geological Survey","id":535099,"contributorType":{"id":1,"text":"Authors"},"rank":1}]}}
,{"id":14328,"text":"ofr74130 - 1974 - Progress report on flood magnitude and frequency of Vermont streams","interactions":[],"lastModifiedDate":"2024-01-09T15:25:47.914198","indexId":"ofr74130","displayToPublicDate":"1974-01-01T00:00:00","publicationYear":"1974","noYear":false,"publicationType":{"id":18,"text":"Report"},"publicationSubtype":{"id":5,"text":"USGS Numbered Series"},"seriesTitle":{"id":330,"text":"Open-File Report","code":"OFR","onlineIssn":"2331-1258","printIssn":"0196-1497","active":true,"publicationSubtype":{"id":5}},"seriesNumber":"74-130","title":"Progress report on flood magnitude and frequency of Vermont streams","docAbstract":"<p>A technique is presented for estimating the magnitude and frequency of floods on streams in Vermont with drainage areas between 0.27 and 1,040 square miles. Multiple-regression techniques are used to define the relation between flood peaks, collected at a network of gaging stations maintained by the U.S. Geological Survey, and a set of basin characteristics. Results show that flood peaks may be estimated from knowledge of the basin's drainage area, average seasonal snowfall, area of lakes and ponds, and maximum 24-hour rainfall having a recurrence interval of 2 years. The relations are presented graphically for user convenience.</p>","language":"English","publisher":"U.S. Geological Survey","doi":"10.3133/ofr74130","collaboration":"Prepared in cooperation with the the Vermont Highway Department and the Federal Highway Administration","usgsCitation":"Johnson, C.G., and Tasker, G.D., 1974, Progress report on flood magnitude and frequency of Vermont streams: U.S. Geological Survey Open-File Report 74-130, 37 p., https://doi.org/10.3133/ofr74130.","productDescription":"37 p.","costCenters":[],"links":[{"id":148517,"rank":1,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/of/1974/0130/report-thumb.jpg"},{"id":422928,"rank":2,"type":{"id":11,"text":"Document"},"url":"https://pubs.usgs.gov/of/1974/0130/report.pdf","linkFileType":{"id":1,"text":"pdf"}}],"country":"United 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,{"id":70010217,"text":"70010217 - 1974 - Spectrophotometric determination of molybdenum in rocks with thiocyanate","interactions":[],"lastModifiedDate":"2021-01-22T14:18:04.09582","indexId":"70010217","displayToPublicDate":"1974-01-01T00:00:00","publicationYear":"1974","noYear":false,"publicationType":{"id":2,"text":"Article"},"publicationSubtype":{"id":10,"text":"Journal Article"},"seriesTitle":{"id":760,"text":"Analytica Chimica Acta","active":true,"publicationSubtype":{"id":10}},"title":"Spectrophotometric determination of molybdenum in rocks with thiocyanate","docAbstract":"<div id=\"aep-abstract-id4\" class=\"abstract author\"><div id=\"aep-abstract-sec-id5\"><p id=\"simple-para.0010\">A rapid procedure for the determination of microgram amounts of molybdenum in rocks is described. After acid decomposition, molybdenum is extracted from a hydrochloric acid solution into xylene with tributyl phosphate. After back-extraction with water, molybdenum is extracted as the α-benzoinoximate into chloroform, stripped into hydrochloric acid extracted as the thiocyanate into amyl alcohol, and determined spectrophotometrically. The molybdenum thiocyanate color produced is stable, sensitive, and reproducible. Results of analyses of several of the U.S. Geological Survey standard rocks are given.</p></div></div><div id=\"aep-abstract-id6\" class=\"abstract author\" lang=\"fr\"><br></div>","language":"English","publisher":"Elsevier","doi":"10.1016/S0003-2670(01)80897-7","issn":"00032670","usgsCitation":"Lillie, E., and Greenland, L., 1974, Spectrophotometric determination of molybdenum in rocks with thiocyanate: Analytica Chimica Acta, v. 69, no. 2, p. 313-320, https://doi.org/10.1016/S0003-2670(01)80897-7.","productDescription":"8 p.","startPage":"313","endPage":"320","numberOfPages":"8","costCenters":[],"links":[{"id":219133,"rank":0,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/thumbnails/outside_thumb.jpg"}],"volume":"69","issue":"2","noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"505b95a9e4b08c986b31b043","contributors":{"authors":[{"text":"Lillie, E.G.","contributorId":13370,"corporation":false,"usgs":true,"family":"Lillie","given":"E.G.","email":"","affiliations":[],"preferred":false,"id":358330,"contributorType":{"id":1,"text":"Authors"},"rank":1},{"text":"Greenland, L. P.","contributorId":56368,"corporation":false,"usgs":true,"family":"Greenland","given":"L. P.","affiliations":[],"preferred":false,"id":358331,"contributorType":{"id":1,"text":"Authors"},"rank":2}]}}
,{"id":1013769,"text":"1013769 - 1974 - An antigenic comparison between infectious hematopoietic necrosis virus (OSV strain) and the virus of haemorrhagic septicaemia of rainbow trout (Salmo gairdneri) (Denmark strain) by cross neutralization","interactions":[],"lastModifiedDate":"2025-04-07T16:13:05.897382","indexId":"1013769","displayToPublicDate":"1974-01-01T00:00:00","publicationYear":"1974","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":"An antigenic comparison between infectious hematopoietic necrosis virus (OSV strain) and the virus of haemorrhagic septicaemia of rainbow trout (Salmo gairdneri) (Denmark strain) by cross neutralization","docAbstract":"<p><span>The infectious hematopoietic necrosis virus (OSV strain) and the virus of haemorrhagic septicaemia of rainbow trout (</span><i>Salmo gairdneri</i><span>) (Denmark strain) were examined for possible antigenic relationship by plaque neutralization using homologous and heterologous antisera. No neutralization of either virus was observed on exposure to heterologous antiserum. This indicates that there is no antigenic relationship between these two viruses as determined by this method.</span></p>","language":"English","publisher":"Wildlife Disease Association","doi":"10.7589/0090-3558-10.2.101","usgsCitation":"McAllister, P.E., Fryer, J.L., and Pilcher, K., 1974, An antigenic comparison between infectious hematopoietic necrosis virus (OSV strain) and the virus of haemorrhagic septicaemia of rainbow trout (Salmo gairdneri) (Denmark strain) by cross neutralization: Journal of Wildlife Diseases, v. 10, no. 2, p. 101-103, https://doi.org/10.7589/0090-3558-10.2.101.","productDescription":"3 p.","startPage":"101","endPage":"103","costCenters":[{"id":365,"text":"Leetown Science Center","active":true,"usgs":true}],"links":[{"id":488610,"rank":2,"type":{"id":40,"text":"Open Access Publisher Index Page"},"url":"https://doi.org/10.7589/0090-3558-10.2.101","text":"Publisher Index Page"},{"id":129479,"rank":1,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/thumbnails/outside_thumb.jpg"}],"volume":"10","issue":"2","noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"4f4e4adae4b07f02db6857ac","contributors":{"authors":[{"text":"McAllister, P. E.","contributorId":71913,"corporation":false,"usgs":true,"family":"McAllister","given":"P.","email":"","middleInitial":"E.","affiliations":[],"preferred":false,"id":319226,"contributorType":{"id":1,"text":"Authors"},"rank":1},{"text":"Fryer, J. L.","contributorId":21900,"corporation":false,"usgs":true,"family":"Fryer","given":"J.","email":"","middleInitial":"L.","affiliations":[],"preferred":false,"id":319224,"contributorType":{"id":1,"text":"Authors"},"rank":2},{"text":"Pilcher, K.S.","contributorId":42557,"corporation":false,"usgs":true,"family":"Pilcher","given":"K.S.","email":"","affiliations":[],"preferred":false,"id":319225,"contributorType":{"id":1,"text":"Authors"},"rank":3}]}}
,{"id":70170237,"text":"70170237 - 1974 - New cooperative seismograph networks established in southern California","interactions":[],"lastModifiedDate":"2016-04-12T15:41:18","indexId":"70170237","displayToPublicDate":"1974-01-01T00:00:00","publicationYear":"1974","noYear":false,"publicationType":{"id":2,"text":"Article"},"publicationSubtype":{"id":10,"text":"Journal Article"},"seriesTitle":{"id":1435,"text":"Earthquake Information Bulletin (USGS)","active":true,"publicationSubtype":{"id":10}},"title":"New cooperative seismograph networks established in southern California","docAbstract":"<p>Southern California has more active faults located close to large, urban population centers than any other region in the United States. Reduction of risk to life and property posed by potential earthquakes along these active faults is a primary motivation for a cooperative earthquake research program between the U.S Geological Survey and major universities in Southern California.&nbsp;</p>","language":"English","publisher":"U.S Geological Survey","usgsCitation":"Hill, D., 1974, New cooperative seismograph networks established in southern California: Earthquake Information Bulletin (USGS), v. 6, no. 3, p. 8-11.","productDescription":"4 p.","startPage":"8","endPage":"11","onlineOnly":"N","additionalOnlineFiles":"N","costCenters":[],"links":[{"id":320001,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/thumbnails/outside_thumb.jpg"}],"country":"United States","state":"California","geographicExtents":"{\n  \"type\": \"FeatureCollection\",\n  \"features\": [\n    {\n      \"type\": \"Feature\",\n      \"properties\": {},\n      \"geometry\": {\n        \"type\": \"Polygon\",\n        \"coordinates\": [\n          [\n            [\n              -120.838623046875,\n              35.209721645221386\n            ],\n            [\n              -115.81787109375,\n              35.074964853989556\n            ],\n            [\n              -114.04907226562499,\n              34.35250666867596\n            ],\n            [\n              -114.45556640625,\n              33.660353121928814\n            ],\n            [\n              -114.521484375,\n              32.76880048488168\n            ],\n            [\n              -114.7412109375,\n              32.61161640317033\n            ],\n            [\n              -115.8837890625,\n              32.648625783736726\n            ],\n            [\n              -117.16918945312499,\n              32.54681317351514\n            ],\n            [\n              -118.707275390625,\n              32.722598604044066\n            ],\n            [\n              -120.62988281249999,\n              33.970697997361626\n            ],\n            [\n              -120.9375,\n              35.02099970111467\n            ],\n            [\n              -120.838623046875,\n              35.209721645221386\n            ]\n          ]\n        ]\n      }\n    }\n  ]\n}","volume":"6","issue":"3","noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"570e1c35e4b0ef3b7ca24c3a","contributors":{"authors":[{"text":"Hill, D.P.","contributorId":27432,"corporation":false,"usgs":true,"family":"Hill","given":"D.P.","email":"","affiliations":[],"preferred":false,"id":626567,"contributorType":{"id":1,"text":"Authors"},"rank":1}]}}
,{"id":70170238,"text":"70170238 - 1974 - A geologic and geophysical study of the Charleston, South Carolina, earthquake zone","interactions":[],"lastModifiedDate":"2016-04-12T15:47:13","indexId":"70170238","displayToPublicDate":"1974-01-01T00:00:00","publicationYear":"1974","noYear":false,"publicationType":{"id":2,"text":"Article"},"publicationSubtype":{"id":10,"text":"Journal Article"},"seriesTitle":{"id":1435,"text":"Earthquake Information Bulletin (USGS)","active":true,"publicationSubtype":{"id":10}},"title":"A geologic and geophysical study of the Charleston, South Carolina, earthquake zone","docAbstract":"<p>A maximum Modified Mercalli intensity of X was reported in Charleston. Damage to buildings was extensive, railroads were made impassable, and communications were disrupted. During the earthquake 27 people were killed, and 56 later died as a result of exposure and injuries sustained during the shaking. The earthquake was reported felt as far as New England, Wisconsin, and Missouri, an area of 5 million square kilometres.&nbsp;</p>","language":"English","publisher":"U.S Geological Survey","usgsCitation":"Higgins, B., and Popenoe, P., 1974, A geologic and geophysical study of the Charleston, South Carolina, earthquake zone: Earthquake Information Bulletin (USGS), v. 6, no. 6, p. 16-23.","productDescription":"8 p.","startPage":"16","endPage":"23","onlineOnly":"N","additionalOnlineFiles":"N","costCenters":[],"links":[{"id":320003,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/thumbnails/outside_thumb.jpg"}],"country":"United States","state":"South Carolina","geographicExtents":"{\n  \"type\": \"FeatureCollection\",\n  \"features\": [\n    {\n      \"type\": \"Feature\",\n      \"properties\": {},\n      \"geometry\": {\n        \"type\": \"Polygon\",\n        \"coordinates\": [\n          [\n            [\n              -79.85275268554688,\n              33.15594830078649\n            ],\n            [\n              -80.068359375,\n              33.18813395605041\n            ],\n            [\n              -80.23727416992188,\n              33.089240433964726\n            ],\n            [\n              -80.26611328125,\n              32.95221579117345\n            ],\n            [\n              -80.34027099609375,\n              32.64400044827676\n            ],\n            [\n              -80.25650024414062,\n              32.531762869982266\n            ],\n            [\n              -80.1397705078125,\n              32.54681317351514\n            ],\n            [\n              -79.9310302734375,\n              32.65209462833938\n            ],\n            [\n              -79.78958129882812,\n              32.75263255213169\n            ],\n            [\n              -79.6563720703125,\n              32.8149783969858\n            ],\n            [\n              -79.55337524414062,\n              32.91187391621322\n            ],\n            [\n              -79.54376220703125,\n              32.96949953291244\n            ],\n            [\n              -79.79644775390625,\n              33.14560040196164\n            ],\n            [\n              -79.85275268554688,\n              33.15594830078649\n            ]\n          ]\n        ]\n      }\n    }\n  ]\n}","volume":"6","issue":"6","noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"570e1c2ce4b0ef3b7ca24c17","contributors":{"authors":[{"text":"Higgins, B.B.","contributorId":8091,"corporation":false,"usgs":true,"family":"Higgins","given":"B.B.","email":"","affiliations":[],"preferred":false,"id":626568,"contributorType":{"id":1,"text":"Authors"},"rank":1},{"text":"Popenoe, P.","contributorId":105434,"corporation":false,"usgs":true,"family":"Popenoe","given":"P.","email":"","affiliations":[],"preferred":false,"id":626569,"contributorType":{"id":1,"text":"Authors"},"rank":2}]}}
,{"id":2002167,"text":"2002167 - 1974 - Refined burning prescriptions for Yosemite National Park","interactions":[],"lastModifiedDate":"2012-02-02T00:14:53","indexId":"2002167","displayToPublicDate":"1974-01-01T00:00:00","publicationYear":"1974","noYear":false,"publicationType":{"id":18,"text":"Report"},"publicationSubtype":{"id":1,"text":"Federal Government Series"},"seriesTitle":{"id":59,"text":"Occasional Paper","active":false,"publicationSubtype":{"id":1}},"seriesNumber":"2","title":"Refined burning prescriptions for Yosemite National Park","docAbstract":"No abstract available at this time","language":"English","publisher":"National Park Service","usgsCitation":"van Wagtendonk, J., 1974, Refined burning prescriptions for Yosemite National Park: Occasional Paper 2, 21 p.","productDescription":"21 p.","startPage":"0","endPage":"21","numberOfPages":"21","costCenters":[{"id":651,"text":"Western Ecological Research Center","active":true,"usgs":true}],"links":[{"id":199251,"rank":0,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/thumbnails/outside_thumb.jpg"}],"noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"4f4e4a60e4b07f02db635190","contributors":{"authors":[{"text":"van Wagtendonk, J. W.","contributorId":85111,"corporation":false,"usgs":true,"family":"van Wagtendonk","given":"J. W.","affiliations":[],"preferred":false,"id":326096,"contributorType":{"id":1,"text":"Authors"},"rank":1}]}}
,{"id":2002169,"text":"2002169 - 1974 - Reproduction and survivorship of the lizard, Uta stansburiana, and the effects of winter rainfall, density and predation on these processes","interactions":[],"lastModifiedDate":"2012-02-02T00:14:54","indexId":"2002169","displayToPublicDate":"1974-01-01T00:00:00","publicationYear":"1974","noYear":false,"publicationType":{"id":18,"text":"Report"},"publicationSubtype":{"id":3,"text":"Organization Series"},"seriesTitle":{"id":180,"text":"IBP Numbered Series","active":false,"publicationSubtype":{"id":3}},"seriesNumber":"RM 74-26","title":"Reproduction and survivorship of the lizard, Uta stansburiana, and the effects of winter rainfall, density and predation on these processes","docAbstract":"No abstract available at this time","language":"English","publisher":"U.S. International Biological Program, Desert Biome","usgsCitation":"Turner, F., Medica, P., and Smith, D., 1974, Reproduction and survivorship of the lizard, Uta stansburiana, and the effects of winter rainfall, density and predation on these processes: IBP Numbered Series RM 74-26, p. 117-128.","productDescription":"p. 117-128","startPage":"117","endPage":"128","numberOfPages":"12","costCenters":[{"id":651,"text":"Western Ecological Research Center","active":true,"usgs":true}],"links":[{"id":199373,"rank":0,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/thumbnails/outside_thumb.jpg"}],"noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"4f4e4a55e4b07f02db62cba4","contributors":{"authors":[{"text":"Turner, F.B.","contributorId":95414,"corporation":false,"usgs":true,"family":"Turner","given":"F.B.","email":"","affiliations":[],"preferred":false,"id":326101,"contributorType":{"id":1,"text":"Authors"},"rank":1},{"text":"Medica, P.A.","contributorId":77079,"corporation":false,"usgs":true,"family":"Medica","given":"P.A.","email":"","affiliations":[],"preferred":false,"id":326099,"contributorType":{"id":1,"text":"Authors"},"rank":2},{"text":"Smith, D.D.","contributorId":85539,"corporation":false,"usgs":true,"family":"Smith","given":"D.D.","email":"","affiliations":[],"preferred":false,"id":326100,"contributorType":{"id":1,"text":"Authors"},"rank":3}]}}
,{"id":2002343,"text":"2002343 - 1974 - Age, growth, sexual maturity, and food of channel catfish in central Lake Oahe, 1968-69","interactions":[],"lastModifiedDate":"2013-02-04T13:42:08","indexId":"2002343","displayToPublicDate":"1974-01-01T00:00:00","publicationYear":"1974","noYear":false,"publicationType":{"id":18,"text":"Report"},"publicationSubtype":{"id":9,"text":"Other Report"},"seriesTitle":{"id":413,"text":"Technical Paper","active":false,"publicationSubtype":{"id":9}},"seriesNumber":"81","title":"Age, growth, sexual maturity, and food of channel catfish in central Lake Oahe, 1968-69","docAbstract":"Channel catfish, <i>Ictalurus punctatus</i>, were collected with gill nets, trawl, and trap nets at three localities in Lake Oahe for the study of year-class strength, growth in length and weight, age composition, sexual maturity, and food. Fish were recruited to all the collection gears at age II. Relatively strong year classes were produced in 1962, 1965, and 1966. Youngest fish were captured in the upper end of the Moreau River embayment, which apparently serves as a nursery area. Growth of age 0 fish was poor probably because the growing season was short; optimum spawning temperature were not reached until mid-summer. Growth of age II and older fish reached a peak in 1963 and declined rather steadily in 1964-68. Males began to mature at age VIII, and all fish of both sexes were mature at age XI. The diet changed from zooplankton to fish as channel catfish increased in length; aquatic insects (primarily chironomid larvae and pupae) were important foods for fish of all sizes. Fish less than 300 mm long selected large zooplankters -- <i>Leptodora kindtii</i> and <i>Daphnia spp</i> -- over smaller copepods. Larger channel catfish ate principally yellow perch, <i>Perca flavescens</i>.","language":"English","publisher":"U.S. Fish and Wildlife Service","collaboration":"Out-of-print","usgsCitation":"Starostka, V.J., and Nelson, W.R., 1974, Age, growth, sexual maturity, and food of channel catfish in central Lake Oahe, 1968-69: Technical Paper 81, 13 p.","productDescription":"13 p.","startPage":"0","endPage":"13","numberOfPages":"13","costCenters":[{"id":324,"text":"Great Lakes Science Center","active":true,"usgs":true}],"links":[{"id":198174,"rank":0,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/thumbnails/outside_thumb.jpg"},{"id":266940,"type":{"id":11,"text":"Document"},"url":"https://hdl.handle.net/2027/uc1.31822006841605?urlappend=%3Bseq=231"}],"noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"4f4e4ae3e4b07f02db68926b","contributors":{"authors":[{"text":"Starostka, Victor J.","contributorId":93550,"corporation":false,"usgs":true,"family":"Starostka","given":"Victor","email":"","middleInitial":"J.","affiliations":[],"preferred":false,"id":326467,"contributorType":{"id":1,"text":"Authors"},"rank":1},{"text":"Nelson, William R.","contributorId":58326,"corporation":false,"usgs":true,"family":"Nelson","given":"William","email":"","middleInitial":"R.","affiliations":[],"preferred":false,"id":326466,"contributorType":{"id":1,"text":"Authors"},"rank":2}]}}
,{"id":96453,"text":"96453 - 1974 - Desert Tortoise Relocation Project: Status Report for 1972","interactions":[],"lastModifiedDate":"2012-02-02T00:03:52","indexId":"96453","displayToPublicDate":"1974-01-01T00:00:00","publicationYear":"1974","noYear":false,"publicationType":{"id":18,"text":"Report"},"publicationSubtype":{"id":9,"text":"Other Report"},"title":"Desert Tortoise Relocation Project: Status Report for 1972","docAbstract":"No abstract available at this time","language":"English","collaboration":"Calif. Division of Highways, State of California.  Contr. No. F-9353, Sec. III. C.3.","usgsCitation":"Berry, K., 1974, Desert Tortoise Relocation Project: Status Report for 1972.","costCenters":[],"links":[{"id":127120,"rank":0,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/thumbnails/outside_thumb.jpg"}],"noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"4f4e4aa9e4b07f02db667f0b","contributors":{"authors":[{"text":"Berry, K.H.","contributorId":17934,"corporation":false,"usgs":true,"family":"Berry","given":"K.H.","email":"","affiliations":[],"preferred":false,"id":299665,"contributorType":{"id":1,"text":"Authors"},"rank":1}]}}
,{"id":70169207,"text":"70169207 - 1974 - Earthquakes, November-December 1973","interactions":[],"lastModifiedDate":"2016-03-31T14:55:54","indexId":"70169207","displayToPublicDate":"1974-01-01T00:00:00","publicationYear":"1974","noYear":false,"publicationType":{"id":2,"text":"Article"},"publicationSubtype":{"id":10,"text":"Journal Article"},"seriesTitle":{"id":1435,"text":"Earthquake Information Bulletin (USGS)","active":true,"publicationSubtype":{"id":10}},"title":"Earthquakes, November-December 1973","docAbstract":"<p>A number of significant earthquakes happened &nbsp;during the last 2 months of 1973. Two major earthquakes (magnitude 7.0-7.9) occurred in the New Hebrides Islands, bringing the final major earthquake total for the year to 11, somewhat below the annual average which is 18. One great earthquake (magntidue 8.0 and above) per year is average, but none &nbsp;occurred in 1973.&nbsp;</p>\n<p>An earthquake in Tennessee, centered about 30 miles south of Knoxville, caused minor damage in the Maryville-Alcoa area and was felt in seven Southeastern States. New Mexico experienced a sharp earthquake on December 24 that caused minor damage in the Grants area.</p>\n<p>Other parts of the world suffered fatalities and significant damage from earthquakes. In Iran, an earthquake killed one person, injured many, and destroyed a number of homes. Earthquake fatalities also occurred in the Azores and in Algeria.&nbsp;</p>","language":"English","publisher":"U.S Geological Survey","usgsCitation":"Person, W., 1974, Earthquakes, November-December 1973: Earthquake Information Bulletin (USGS), v. 6, no. 1, p. 26-27.","productDescription":"2 p.","startPage":"26","endPage":"27","onlineOnly":"N","additionalOnlineFiles":"N","costCenters":[],"links":[{"id":319293,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/thumbnails/outside_thumb.jpg"}],"volume":"6","issue":"1","noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"56f3be34e4b0f59b85e02df3","contributors":{"authors":[{"text":"Person, W. J.","contributorId":91472,"corporation":false,"usgs":true,"family":"Person","given":"W. J.","affiliations":[],"preferred":false,"id":623337,"contributorType":{"id":1,"text":"Authors"},"rank":1}]}}
]}