Naturally occurring strontium was found in both surface and ground waters during an investigation of the water resources of Champaign County, Ohio. The strontium is related to the presence of celestite (strontium sulfate) in rocks associated with evaporite deposition. The principal source of celestite in Ohio is in rocks of Late Silurian age. Celestite is present also in the glacial deposits of western Ohio, which contain rock material of Late Silurian age. Total time in contact with the rock material seems to have a large effect upon concentrations of strontium in ground water. Streamflow, during low-flow periods, is made up largely of ground-water seepage and contains detectable strontium. Strontium has been found in ground water in other counties in western Ohio and in the brines of eastern Ohio.
","language":"English","publisherLocation":"Society of Economic Geologist","doi":"10.2113/gsecongeo.55.1.176","usgsCitation":"Feulner, A., and Hubble, J., 1960, Occurrence of strontium in the surface and ground waters of Champaign county, Ohio: Economic Geology, v. 55, no. 1, p. 176-186, https://doi.org/10.2113/gsecongeo.55.1.176.","productDescription":"11 p.","startPage":"176","endPage":"186","costCenters":[],"links":[{"id":385794,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/thumbnails/outside_thumb.jpg"}],"country":"United States","state":"Ohio","county":"Champaign County","geographicExtents":"{\n \"type\": \"FeatureCollection\",\n \"features\": [\n {\n \"type\": \"Feature\",\n \"properties\": {},\n \"geometry\": {\n \"type\": \"Polygon\",\n \"coordinates\": [\n [\n [\n -83.83186340332031,\n 40.063884174719156\n ],\n [\n -83.64303588867186,\n 40.063884174719156\n ],\n [\n -83.64303588867186,\n 40.16680597002458\n ],\n [\n -83.83186340332031,\n 40.16680597002458\n ],\n [\n -83.83186340332031,\n 40.063884174719156\n ]\n ]\n ]\n }\n }\n ]\n}","volume":"55","issue":"1","noUsgsAuthors":false,"publicationDate":"1960-01-01","publicationStatus":"PW","contributors":{"authors":[{"text":"Feulner, A.J.","contributorId":70796,"corporation":false,"usgs":true,"family":"Feulner","given":"A.J.","affiliations":[],"preferred":false,"id":816098,"contributorType":{"id":1,"text":"Authors"},"rank":1},{"text":"Hubble, J.H.","contributorId":99624,"corporation":false,"usgs":true,"family":"Hubble","given":"J.H.","email":"","affiliations":[],"preferred":false,"id":816099,"contributorType":{"id":1,"text":"Authors"},"rank":2}]}} ,{"id":1094,"text":"1094 - 1960 - Geology and ground-water hydrology of the Redlands-Beaumont area, California, with special reference to ground-water outflow","interactions":[],"lastModifiedDate":"2024-09-03T21:05:26.158835","indexId":"1094","displayToPublicDate":"1960-01-01T12:39:48","publicationYear":"1960","noYear":false,"publicationType":{"id":18,"text":"Report"},"publicationSubtype":{"id":6,"text":"USGS Unnumbered Series"},"title":"Geology and ground-water hydrology of the Redlands-Beaumont area, California, with special reference to ground-water outflow","docAbstract":"The Redlands-Beaumont area is bordered by the Santa Ana River on the north, the San Bernadina River on the northeast, the Yucaipa Hills and the San Gorgonio Pass on the east, and the Badlands and the San Jacinto fault on the south and south-west. Large alluvial fans underlie much of the area, but other landforms include alluvial benches, dissected alluvial hills, plains, terraces, and bedrock hills which locally protrude above the floors of the alluvial valleys.
","language":"English","publisher":"U.S. Geological Survey","doi":"10.3133/1094","collaboration":"Prepared in cooperation with the San Bernardino County Flood Control District.","usgsCitation":"Burnham, W., and Dutcher, L.C., 1960, Geology and ground-water hydrology of the Redlands-Beaumont area, California, with special reference to ground-water outflow, 352 p., https://doi.org/10.3133/1094.","productDescription":"352 p.","costCenters":[],"links":[{"id":433421,"rank":2,"type":{"id":11,"text":"Document"},"url":"https://pubs.usgs.gov/unnumbered/1094/report.pdf","linkFileType":{"id":1,"text":"pdf"}},{"id":289641,"rank":1,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/unnumbered/1094/report-thumb.jpg"}],"country":"United States","state":"California","city":"Beaumont, Redlands","geographicExtents":"{\n \"type\": \"FeatureCollection\",\n \"features\": [\n {\n \"type\": \"Feature\",\n \"properties\": {},\n \"geometry\": {\n \"coordinates\": [\n [\n [\n -117.2637864386227,\n 34.105233250065254\n ],\n [\n -117.2637864386227,\n 33.87256760375355\n ],\n [\n -116.9107764193285,\n 33.87256760375355\n ],\n [\n -116.9107764193285,\n 34.105233250065254\n ],\n [\n -117.2637864386227,\n 34.105233250065254\n ]\n ]\n ],\n \"type\": \"Polygon\"\n }\n }\n ]\n}","noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"53be6474e4b0527d5d4097b6","contributors":{"authors":[{"text":"Burnham, W.L.","contributorId":58668,"corporation":false,"usgs":true,"family":"Burnham","given":"W.L.","email":"","affiliations":[],"preferred":false,"id":143166,"contributorType":{"id":1,"text":"Authors"},"rank":1},{"text":"Dutcher, Lee Carlton","contributorId":32229,"corporation":false,"usgs":true,"family":"Dutcher","given":"Lee","email":"","middleInitial":"Carlton","affiliations":[],"preferred":false,"id":143165,"contributorType":{"id":1,"text":"Authors"},"rank":2}]}} ,{"id":70160871,"text":"70160871 - 1960 - Geology and ground-water resources of the island of Kauai, Hawaii","interactions":[],"lastModifiedDate":"2016-01-06T08:58:28","indexId":"70160871","displayToPublicDate":"1960-01-01T12:15:00","publicationYear":"1960","noYear":false,"publicationType":{"id":18,"text":"Report"},"publicationSubtype":{"id":4,"text":"Other Government Series"},"seriesTitle":{"id":242,"text":"Bulletin","active":false,"publicationSubtype":{"id":4}},"seriesNumber":"13","title":"Geology and ground-water resources of the island of Kauai, Hawaii","docAbstract":"Kauai is one of the oldest, and is structurally the most complicated, of the Hawaiian Islands. Like the others, it consists principally of a huge shield volcano, built up from the sea floor by many thousands of thin flows of basaltic lava. The volume of the Kauai shield was on the order of 1,000 cubic miles. Through much of its growth it must have resembled rather closely the presently active shield volcano Mauna Loa, on the island of Hawaii. When the Kauai volcano started its growth is not known with certainty, but it is believed that activity started late in the Tertiary period, possibly in the early or middle part of the Pliocene epoch. Growth of the shield was rapid and probably was completed before the end of the Pliocene.
Toward the end of the growth of the shield, its summit collapsed to form a broad caldera, the largest that has been found in the Hawaiian Islands. Like the calderas of Kilauea and Mauna Loa, that of Kauai volcano had boundaries that were, in part, rather indefinite. The principal depression was bordered by less depressed fault blocks, some of which merged imperceptibly with the outer slopes of the volcano. Elsewhere the caldera rim was low, and flows spilled over it onto the outer slopes. The well-defined central depression of the Kauai caldera was approximately 10 to 12 miles across.
At about the same time as the formation of the major caldera, another, smaller caldera was formed by collapse around a minor eruptive center on the southeastern side of the Kauai shield. Lavas accumulated in the calderas, gradually filling them and burying banks of talus that formed along the foot of the boundary cliffs. The caldera-filling lavas differed from those that built the major portion of the shield in being much thicker and more massive as a result of ponding in the depressions. The petrographic types for the most part are the same throughout. Both the flank flows that built most of the shield and the flows that filled the calderas are predominantly olivine basalt. Picrite-basalt (oceanite), containing very abundant large phenocrysts of olivine, and basalt containing little or no olivine are present but together comprise less than 10 percent of the whole. Late in the period of filling of the major caldera a small amount of basaltic andesine andesite was extruded.
Near the end of the period of filling of the major caldera further collapse occurred, forming a large graben on the southwestern side of the shield. Lava flows erupting within the caldera poured southwestward over the cliff bounding the graben and spread over the gently sloping graben floor. Near the present Waimea Canyon their advance was obstructed by the fault scarp at the west edge of the graben. The cliff along the northeast edge of the graben eventually was buried by lava flows from within the caldera, but that along the west edge continued to stand above the level of the flows in the graben. The flows that accumulated in the graben are of the same types as those that filled the caldera, and like them are mostly thick and massive because of ponding by the graben walls and of the gentle slopes of the graben floor over which they spread.
The rocks of the major Kauai shield volcano are known as the Waimea Canyon volcanic series. The thin flows that accumulated on the flanks of the shield, which compose the major portion of the volcanic edifice, are named the Napali formation of the Waimea Canyon volcanic series. The rocks that accumulated in the big summit caldera are named the Olokele formation, and those that filled the small caldera on the southeast flank of the shield are named the Haupu formation. The volcanic rocks accumulated in the graben on the southwestern side of the shield are named the Makaweli formation of the Waimea Canyon volcanic series, and sedimentary rocks interbedded with them are known as the Mokuone member of the Makaweli formation.
Few vents of the Waimea Canyon volcanic series have been recognized, probably because most of them have been destroyed by erosion or are buried by later lavas. Large numbers of dikes cut the lavas of the Napali formation along Waimea Canyon and the Napali Coast and along the east edge of the Waialeale massif. Fewer dikes are found in the other members of the series. Some tendency toward radial arrangement of the dikes is present, but the dominant trend all over the island is east-northeastward.
Another great collapse took place on the eastern flank of the volcano at about the time the major shield became extinct, or shortly afterward. A subcircular graben 6 or 7 miles across sank several thousand feet, forming a broad depression between the Waialeale massif on the west and Kalepa and Nonou ridges on the east. This collapsed structure cannot be as clearly demonstrated as the Makaweli graben on the southwest side of the shield, because its walls have been greatly eroded and its floor is deeply buried by lavas of the later Koloa volcanic series. It appears, however, to be the only reasonable explanation of the physiography of the eastern side of the island.
After the completion of the great Kauai shield came a long period of erosion during which no volcanic activity occurred. Waves cut high sea cliffs around the island, and streams cut canyons as much as 3,000 feet deep. Thick soil formed over much of the mountain.
Then volcanism was renewed. Eruption occurred from a series of minor vents arranged in nearly north-south and northeast-southwest lines across the eastern two-thirds of the island. The lavas, cinder cones, and ash beds of this period of volcanism are known as the Koloa volcanic series. Lavas of the Koloa volcanic series include olivine basalt, picrite-basalt (mimosite) with few phenocrysts of olivine, basanite, nepheline basalt, melilite-nepheline basalt, and ankaratrite (nepheline basalt very rich in pyroxene and olivine). Inclusions of dunite, composed almost entirely of olivine, are common in flows of the Koloa. Just before and during the eruption of the Koloa volcanic series, voluminous landslides and mudflows brought down a large amount of rock debris and soil from the steep slopes of the mountainous central upland and deposited it as breccias at the foot of the steep slopes in valley heads and along the border of the marginal lowland. Streams distributed part of the material across the lowland. The breccias and conglomerates thus formed, and later buried by lavas of the Koloa volcanic series, are named the Palikea formation of the Koloa volcanic series.
The structures formed at Koloa vents include cinder cones, one tuff cone, and lava cones. The latter are miniature shields resembling the major shield volcano, formed by repeated outpourings of fluid lava. The tuff cone, at the west side of Kilauea Bay, was formed by phreatomagmatic explosions caused by rising magma coming in contact with water-saturated rocks.
Volcanism during Koloa time continued for a long period but was not continuous over the entire area. Locally, long periods of quiet occurred, allowing streams to re-excavate some of the canyons filled by earlier flows of the Koloa volcanic series, and weathering to form soils later buried by new flows. Some of the canyons thus formed during the time when the Koloa was being deposited were several hundred feet deep. Volcanism probably continued throughout most of the Pleistocene epoch. The latest flow of the Koloa volcanic series appears very recent, and rests on lithified calcareous dunes formed during one of the Pleistocene low stands of the sea.
During the Pleistocene epoch stream valleys and sea cliffs were eroded to base levels governed by one or more stands of the sea more than 100 feet below present sea level. Beaches of calcareous sand were formed, and the sand blown inland to form calcareous dunes, now lithified. A test boring near Moloaa penetrated calcareous sand 160 feet below sea level, at the foot of a high sea cliff. Coral reef also was built around part or all of the island, and in part buried by lavas of the Koloa volcanic series. The explosions that built the tuff cone at Kilauea Bay threw up fragments of limestone from a buried reef. Much of the apron of lavas of the Kalna series around the northeastern side of the island probably rests on a platform formed below present sea level by wave erosion and the growth of coral reef.
As the sea rose around the island, the valley mouths were alluviated. Several levels of the sea higher than the present one probably are represented. Some stream terraces may be graded to a stand of the sea as high as 260 feet above present sea level, but no positive evidence for stands higher than 25 feet have been found. Well-preserved shorelines are recognized approximately 25 and 5 feet above sea level. Much of the present coral reef appears to have been formed when the sea stood about 5 feet higher than now, and reduced to its present level by solutional weathering and wave erosion.
The lavas of the Napali formation of the Waimea Canyon volcanic series are highly permeable. They carry basal water over much of the island, and yield it freely to wells. This water is fresh everywhere except very close to the coast on the leeward side of the island. In some areas they may contain water confined at high levels between dikes. The lavas of the Olokele and Haupu formations are moderately to poorly permeable. They probably contain fresh water at sea level, but would not yield it readily to wells. Locally, ash beds perch small bodies of fresh water at high levels in the lavas of the Olokele formation, but these are of no economic importance. The lavas of the Makaweli formation also arc moderately to poorly permeable. They carry fresh or brackish water at sea level. In general, they yield water to wells less readily than the lavas of the Napali formation, but more readily than the lavas of the Olokele. The conglomerates and breccias of the Mokuone member are poorly permeable, but are not known to perch more than a slight amount of water in the overlying lavas,
The lava flows of the Koloa volcanic series are poorly to moderately permeable. They carry fresh or brackish water at sea level, but generally yield it slowly to wells. Locally, small bodies of fresh water are perched at high levels in the lavas of the Koloa by beds of ash and soil and by breccia and conglomerate of the Palikea formation.
Both the older and the younger alluvium generally are poorly permeable, but contain small amounts of fresh or brackish water. The lithified calcareous dunes are permeable, but they appear to contain only brackish water. Lagoon deposits on the Mana plain are poorly to moderately permeable and yield brackish water to wells.
The investigation of the ground-water resources of Monmouth County is part of a Statewide water-resources program. This study was made by the U.S. Geological Survey in cooperation with the new Jersey Department of Conservation and Economic Development, Division of Water Policy and Supply. It was under the general direction of Philip E. LaMoreaux, Chief of the Ground Water Branch of the U.S. Geological Survey, and under the direct supervision of Allen Sinnott, District Geologist.
This report presents data for most of the public-supply wells and for several irrigation wells in Monmouth County. The data for these wells are believed to be representative of large-capacity wells tapping the major aquifers present in the county. The information is released at this time in advance of an interpretive report because of its value to prospective users of ground water in Monmouth County. An earlier report presented data on small-capacity wells tapping both major and minor aquifers in the county. The data in these two reports form, in part, the basis for a comprehensive interpretive report on the ground-water resources of Monmouth County, now in preparation. Also to be included in the latter report are data for certain large-capacity industrial wells.
","language":"English","publisher":"State of New Jersey Department of Conservation and Economic Development, Division of Water Policy and Supply","usgsCitation":"Jablonski, L.A., 1960, Factual data for public-supply wells and selected irrigation wells in Monmouth County, New Jersey: New Jersey Division of Water Policy and Supply Water Resources Circular 4, iii, 29 p.","productDescription":"iii, 29 p.","numberOfPages":"33","costCenters":[],"links":[{"id":290118,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/thumbnails/outside_thumb.jpg"},{"id":290117,"type":{"id":11,"text":"Document"},"url":"https://pubs.usgs.gov/unnumbered/70114183/report.pdf"}],"country":"United States","state":"New Jersey","county":"Monmouth County","geographicExtents":"{ \"type\": \"FeatureCollection\", \"features\": [ { \"type\": \"Feature\", \"properties\": {}, \"geometry\": { \"type\": \"Polygon\", \"coordinates\": [ [ [ -74.613529,40.07913 ], [ -74.613529,40.478576 ], [ -73.972184,40.478576 ], [ -73.972184,40.07913 ], [ -74.613529,40.07913 ] ] ] } } ] }","noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"53aa9dede4b065055fab1665","contributors":{"authors":[{"text":"Jablonski, Leo A.","contributorId":16324,"corporation":false,"usgs":true,"family":"Jablonski","given":"Leo","email":"","middleInitial":"A.","affiliations":[],"preferred":false,"id":495256,"contributorType":{"id":1,"text":"Authors"},"rank":1}]}} ,{"id":70220574,"text":"70220574 - 1960 - A geologic-profile plotter","interactions":[],"lastModifiedDate":"2021-05-19T14:38:28.190746","indexId":"70220574","displayToPublicDate":"1960-01-01T09:35:07","publicationYear":"1960","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 geologic-profile plotter","docAbstract":"Design and uses are described of an easy-to-construct instrument that facilitates construction of profiles of land surfaces, geologic formations, or other features such as profiles of geophysical or geochemical anomalies. Response to data from users of the instrument indicates that it is both faster and more convenient than previous methods.
","language":"English","publisher":"Society of Economic Geologists","doi":"10.2113/gsecongeo.55.1.201","usgsCitation":"Marsh, O., 1960, A geologic-profile plotter: Economic Geology, v. 55, no. 1, p. 201-204, https://doi.org/10.2113/gsecongeo.55.1.201.","productDescription":"4 p.","startPage":"201","endPage":"204","costCenters":[],"links":[{"id":385766,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/thumbnails/outside_thumb.jpg"}],"volume":"55","issue":"1","noUsgsAuthors":false,"publicationDate":"1960-01-01","publicationStatus":"PW","contributors":{"authors":[{"text":"Marsh, O.T.","contributorId":64672,"corporation":false,"usgs":true,"family":"Marsh","given":"O.T.","email":"","affiliations":[],"preferred":false,"id":816063,"contributorType":{"id":1,"text":"Authors"},"rank":1}]}} ,{"id":2001402,"text":"2001402 - 1960 - Microhematocrit as a tool in fishery research and management","interactions":[],"lastModifiedDate":"2012-02-02T00:15:02","indexId":"2001402","displayToPublicDate":"1960-01-01T02:00:00","publicationYear":"1960","noYear":false,"publicationType":{"id":18,"text":"Report"},"publicationSubtype":{"id":1,"text":"Federal Government Series"},"seriesTitle":{"id":84,"text":"Special Scientific Report - Fisheries","active":false,"publicationSubtype":{"id":1}},"seriesNumber":"341","title":"Microhematocrit as a tool in fishery research and management","docAbstract":"No abstract available at this time","language":"English","publisher":"U.S. Fish and Wildlife Service","collaboration":"80/FH","usgsCitation":"Snieszko, S.F., Camper, J., Howard, F., and Pettijohn, L., 1960, Microhematocrit as a tool in fishery research and management: Special Scientific Report - Fisheries 341, 15 p.","productDescription":"15 p.","startPage":"0","endPage":"15","numberOfPages":"15","costCenters":[{"id":365,"text":"Leetown Science Center","active":true,"usgs":true}],"links":[{"id":198179,"rank":0,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/thumbnails/outside_thumb.jpg"}],"noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"4f4e4a51e4b07f02db629d53","contributors":{"authors":[{"text":"Snieszko, S. F.","contributorId":13169,"corporation":false,"usgs":true,"family":"Snieszko","given":"S.","middleInitial":"F.","affiliations":[],"preferred":false,"id":325655,"contributorType":{"id":1,"text":"Authors"},"rank":1},{"text":"Camper, J.","contributorId":70884,"corporation":false,"usgs":true,"family":"Camper","given":"J.","affiliations":[],"preferred":false,"id":325658,"contributorType":{"id":1,"text":"Authors"},"rank":2},{"text":"Howard, F.","contributorId":20862,"corporation":false,"usgs":true,"family":"Howard","given":"F.","email":"","affiliations":[],"preferred":false,"id":325656,"contributorType":{"id":1,"text":"Authors"},"rank":3},{"text":"Pettijohn, L.L.","contributorId":32878,"corporation":false,"usgs":true,"family":"Pettijohn","given":"L.L.","email":"","affiliations":[],"preferred":false,"id":325657,"contributorType":{"id":1,"text":"Authors"},"rank":4}]}} ,{"id":81395,"text":"81395 - 1960 - A \"virus\" disease of chinook salmon","interactions":[],"lastModifiedDate":"2016-01-04T13:43:40","indexId":"81395","displayToPublicDate":"1960-01-01T00:00:00","publicationYear":"1960","noYear":false,"publicationType":{"id":18,"text":"Report"},"publicationSubtype":{"id":1,"text":"Federal Government Series"},"seriesTitle":{"id":29,"text":"Fishery Leaflet","active":false,"publicationSubtype":{"id":1}},"seriesNumber":"497","title":"A \"virus\" disease of chinook salmon","docAbstract":"Epizootics among chinook salmon fingerlings at the Coleman National Fish Hatchery have occurred periodically since 1941. A virus or virus-like filterable agent has been demonstrated to be the causative agent of this disease.
","language":"English","publisher":"U.S. Fish and Wildlife Service","usgsCitation":"Ross, A.J., and Rucker, R., 1960, A \"virus\" disease of chinook salmon: Fishery Leaflet 497, 3 p.","productDescription":"3 p.","numberOfPages":"3","onlineOnly":"N","additionalOnlineFiles":"N","costCenters":[{"id":365,"text":"Leetown Science Center","active":true,"usgs":true},{"id":654,"text":"Western Fisheries Research Center","active":true,"usgs":true}],"links":[{"id":199054,"rank":0,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/thumbnails/outside_thumb.jpg"},{"id":313215,"rank":1,"type":{"id":11,"text":"Document"},"url":"https://spo.nmfs.noaa.gov/Fishery%20Leaflets/leaflet497.pdf","text":"pdf"},{"id":313216,"rank":2,"type":{"id":15,"text":"Index Page"},"url":"https://spo.nwr.noaa.gov/fisheryleaflets.htm"}],"noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"568ba5bde4b0e7594ee7763c","contributors":{"authors":[{"text":"Ross, A. J.","contributorId":105267,"corporation":false,"usgs":true,"family":"Ross","given":"A.","email":"","middleInitial":"J.","affiliations":[],"preferred":false,"id":295328,"contributorType":{"id":1,"text":"Authors"},"rank":1},{"text":"Rucker, R.R.","contributorId":104000,"corporation":false,"usgs":true,"family":"Rucker","given":"R.R.","email":"","affiliations":[],"preferred":false,"id":295327,"contributorType":{"id":1,"text":"Authors"},"rank":2}]}} ,{"id":5220720,"text":"5220720 - 1960 - Contact dermatitis incurred from cottontail stomach contents","interactions":[],"lastModifiedDate":"2025-02-05T15:28:42.947494","indexId":"5220720","displayToPublicDate":"1960-01-01T00:00:00","publicationYear":"1960","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":"Contact dermatitis incurred from cottontail stomach contents","docAbstract":"No abstract available.
","language":"English","publisher":"Wiley","doi":"10.2307/3797363","usgsCitation":"Clark, G.M., Locke, L.N., and Schmid, F.C., 1960, Contact dermatitis incurred from cottontail stomach contents: Journal of Wildlife Management, v. 24, no. 1, p. 94-94, https://doi.org/10.2307/3797363.","productDescription":"1 p.","startPage":"94","endPage":"94","costCenters":[{"id":531,"text":"Patuxent Wildlife Research Center","active":true,"usgs":true}],"links":[{"id":487095,"rank":2,"type":{"id":40,"text":"Open Access Publisher Index Page"},"url":"https://doi.org/10.2307/3797363","text":"Publisher Index Page"},{"id":197129,"rank":1,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/thumbnails/outside_thumb.jpg"}],"country":"United States","state":"Maryland, New 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Bibliography and index of rock analyses in the periodical and serial literature of the Republic of Ireland and of Northern Ireland","interactions":[],"lastModifiedDate":"2024-03-07T15:45:26.430497","indexId":"70009816","displayToPublicDate":"1960-01-01T00:00:00","publicationYear":"1960","noYear":false,"publicationType":{"id":2,"text":"Article"},"publicationSubtype":{"id":10,"text":"Journal Article"},"seriesTitle":{"id":1759,"text":"Geochimica et Cosmochimica Acta","active":true,"publicationSubtype":{"id":10}},"title":"Data of rock analyses-VII. Bibliography and index of rock analyses in the periodical and serial literature of the Republic of Ireland and of Northern Ireland","docAbstract":"No abstract available.
","language":"English","publisher":"Elsevier","doi":"10.1016/0016-7037(60)90057-0","issn":"00167037","usgsCitation":"Woodland, M., 1960, Data of rock analyses-VII. Bibliography and index of rock analyses in the periodical and serial literature of the Republic of Ireland and of Northern Ireland: Geochimica et Cosmochimica Acta, v. 20, no. 2, p. 149-153, https://doi.org/10.1016/0016-7037(60)90057-0.","productDescription":"5 p.","startPage":"149","endPage":"153","numberOfPages":"5","costCenters":[],"links":[{"id":219033,"rank":1,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/thumbnails/outside_thumb.jpg"}],"volume":"20","issue":"2","noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"5059fd8de4b0c8380cd4e89d","contributors":{"authors":[{"text":"Woodland, M.V.","contributorId":35065,"corporation":false,"usgs":true,"family":"Woodland","given":"M.V.","email":"","affiliations":[],"preferred":false,"id":357216,"contributorType":{"id":1,"text":"Authors"},"rank":1}]}} ,{"id":70010538,"text":"70010538 - 1960 - Comparison of the chemical composition and magnetic properties of tektites and glasses formed by fusion of terrestrial rocks","interactions":[],"lastModifiedDate":"2012-03-12T17:18:24","indexId":"70010538","displayToPublicDate":"1960-01-01T00:00:00","publicationYear":"1960","noYear":false,"publicationType":{"id":2,"text":"Article"},"publicationSubtype":{"id":10,"text":"Journal Article"},"seriesTitle":{"id":2840,"text":"Nature","active":true,"publicationSubtype":{"id":10}},"title":"Comparison of the chemical composition and magnetic properties of tektites and glasses formed by fusion of terrestrial rocks","docAbstract":"[No abstract available]","largerWorkType":{"id":2,"text":"Article"},"largerWorkTitle":"Nature","largerWorkSubtype":{"id":10,"text":"Journal Article"},"language":"English","doi":"10.1038/1871089a0","issn":"00280836","usgsCitation":"Friedman, I., Thorpe, A., and Senftle, F.E., 1960, Comparison of the chemical composition and magnetic properties of tektites and glasses formed by fusion of terrestrial rocks: Nature, v. 187, no. 4743, p. 1089-1092, https://doi.org/10.1038/1871089a0.","startPage":"1089","endPage":"1092","numberOfPages":"4","costCenters":[],"links":[{"id":204966,"rank":9999,"type":{"id":10,"text":"Digital Object Identifier"},"url":"https://dx.doi.org/10.1038/1871089a0"},{"id":219762,"rank":0,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/thumbnails/outside_thumb.jpg"}],"volume":"187","issue":"4743","noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"5059f899e4b0c8380cd4d1f2","contributors":{"authors":[{"text":"Friedman, I.","contributorId":95596,"corporation":false,"usgs":true,"family":"Friedman","given":"I.","email":"","affiliations":[],"preferred":false,"id":359131,"contributorType":{"id":1,"text":"Authors"},"rank":1},{"text":"Thorpe, A.","contributorId":70534,"corporation":false,"usgs":true,"family":"Thorpe","given":"A.","affiliations":[],"preferred":false,"id":359130,"contributorType":{"id":1,"text":"Authors"},"rank":2},{"text":"Senftle, F. E.","contributorId":47788,"corporation":false,"usgs":true,"family":"Senftle","given":"F.","email":"","middleInitial":"E.","affiliations":[],"preferred":false,"id":359129,"contributorType":{"id":1,"text":"Authors"},"rank":3}]}} ,{"id":70009817,"text":"70009817 - 1960 - Equivalent weight of humic acid from peat","interactions":[],"lastModifiedDate":"2020-11-16T16:50:27.572933","indexId":"70009817","displayToPublicDate":"1960-01-01T00:00:00","publicationYear":"1960","noYear":false,"publicationType":{"id":2,"text":"Article"},"publicationSubtype":{"id":10,"text":"Journal Article"},"seriesTitle":{"id":1759,"text":"Geochimica et Cosmochimica Acta","active":true,"publicationSubtype":{"id":10}},"title":"Equivalent weight of humic acid from peat","docAbstract":"By means of discontinuous titration, the equivalent weight of humic acid isolated from a peat was found to increase from 144 to 183 between the third and fifty-second day after the humic acid was dissolved. Infra-red studies showed that the material had probably condensed with loss of carbonyl groups.
","language":"English","publisher":"Elsevier","doi":"10.1016/0016-7037(60)90137-X","usgsCitation":"Pommer, A., and Breger, I.A., 1960, Equivalent weight of humic acid from peat: Geochimica et Cosmochimica Acta, v. 20, no. 1, p. 45-50, https://doi.org/10.1016/0016-7037(60)90137-X.","productDescription":"6 p.","startPage":"45","endPage":"50","numberOfPages":"6","costCenters":[],"links":[{"id":219034,"rank":0,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/thumbnails/outside_thumb.jpg"}],"volume":"20","issue":"1","noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"505a0a2ee4b0c8380cd5222c","contributors":{"authors":[{"text":"Pommer, A. M.","contributorId":20795,"corporation":false,"usgs":false,"family":"Pommer","given":"A. M.","affiliations":[],"preferred":false,"id":357217,"contributorType":{"id":1,"text":"Authors"},"rank":1},{"text":"Breger, Irving A.","contributorId":65205,"corporation":false,"usgs":true,"family":"Breger","given":"Irving","email":"","middleInitial":"A.","affiliations":[],"preferred":false,"id":357218,"contributorType":{"id":1,"text":"Authors"},"rank":2}]}} ,{"id":70010537,"text":"70010537 - 1960 - Anisotropy of the magnetic susceptibility of gallium","interactions":[],"lastModifiedDate":"2020-11-16T17:04:42.468012","indexId":"70010537","displayToPublicDate":"1960-01-01T00:00:00","publicationYear":"1960","noYear":false,"publicationType":{"id":2,"text":"Article"},"publicationSubtype":{"id":10,"text":"Journal Article"},"seriesTitle":{"id":2171,"text":"Journal of Applied Physics","active":true,"publicationSubtype":{"id":10}},"title":"Anisotropy of the magnetic susceptibility of gallium","docAbstract":"The bulk magnetic susceptibilities of single gallium crystals and polycrystalline gallium spheres were measured at 25°C. The following anisotropic diamagnetic susceptibilities were found: a axis (−0.119±0.001)×10−6 emu/g, b axis (−0.416±0.002)×10−6 emu/g, and c axis (−0.229±0.001) emu/g. The susceptibility of the polycrystalline spheres, assumed to be the average value for the bulk susceptibility of gallium, was (−0.257±0.003)×10−6 emu/g at 25°C, and (−0.299±0.003)×10−6 emu/g at −196°C. The susceptibility of liquid gallium was (0.0031±0.001)×10−6 emu/g at 30°C and 100°C. Rotational diagrams of the susceptibilities in the three orthogonal planes of the unit cell were not sinusoidal. The anisotropy in the single crystals was presumably caused by the partial overlap of Brillouin zone boundaries by the Fermi‐energy surface. The large change in susceptibility associated with the change in state was attributed to the absence of effective mass influence in the liquid state.
","language":"English","publisher":"AIP Publishing","doi":"10.1063/1.1735451","usgsCitation":"Pankey, T., 1960, Anisotropy of the magnetic susceptibility of gallium: Journal of Applied Physics, v. 31, no. 10, p. 1802-1804, https://doi.org/10.1063/1.1735451.","productDescription":"3 p.","startPage":"1802","endPage":"1804","numberOfPages":"3","costCenters":[],"links":[{"id":219761,"rank":0,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/thumbnails/outside_thumb.jpg"}],"volume":"31","issue":"10","noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"5059ec00e4b0c8380cd4901c","contributors":{"authors":[{"text":"Pankey, T. Jr.","contributorId":99833,"corporation":false,"usgs":true,"family":"Pankey","given":"T.","suffix":"Jr.","email":"","affiliations":[],"preferred":false,"id":359128,"contributorType":{"id":1,"text":"Authors"},"rank":1}]}} ,{"id":70010774,"text":"70010774 - 1960 - Theoretical stusy of the reaction between 2,2',4' - trihydroxyazobenzene-5-sulfonic acid and zirconium","interactions":[],"lastModifiedDate":"2015-06-22T09:47:06","indexId":"70010774","displayToPublicDate":"1960-01-01T00:00:00","publicationYear":"1960","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":"Theoretical stusy of the reaction between 2,2',4' - trihydroxyazobenzene-5-sulfonic acid and zirconium","docAbstract":"Zirconium reacts with 2,2',4'-trihydroxyazobenzene-5-sulfonic acid in acid solutions to Form two complexes in which the ratios of dye to zirconium are 1 to 1 and 2 to 1. Both complexes are true chelates, with zirconium acting as a bridge between the two orthohydroxy dye groups. Apparent equilibrium constants for the reactions to form each of the complexes are determined. The reactions are used as a basis for the determination of the active component in the dye and a graphical method for the determination of reagent purity is described. Four absorption spectra covering the wave length region from 350 to 750 mu are given, which completely define the color system associated with the reactions in solutions where the hydrochloric acid concentration ranges from 0.0064N to about 7N.
","language":"English","publisher":"ACS Publications","doi":"10.1021/ac50153a037","issn":"00032700","usgsCitation":"Fletcher, M., 1960, Theoretical stusy of the reaction between 2,2',4' - trihydroxyazobenzene-5-sulfonic acid and zirconium: Analytical Chemistry, v. 32, no. 13, p. 1827-1836, https://doi.org/10.1021/ac50153a037.","productDescription":"10 p.","startPage":"1827","endPage":"1836","onlineOnly":"N","additionalOnlineFiles":"N","costCenters":[],"links":[{"id":218727,"rank":0,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/thumbnails/outside_thumb.jpg"}],"volume":"32","issue":"13","noUsgsAuthors":false,"publicationDate":"2002-05-01","publicationStatus":"PW","scienceBaseUri":"505bb1fbe4b08c986b325524","contributors":{"authors":[{"text":"Fletcher, Mary H.","contributorId":52954,"corporation":false,"usgs":true,"family":"Fletcher","given":"Mary H.","affiliations":[],"preferred":false,"id":359618,"contributorType":{"id":1,"text":"Authors"},"rank":1}]}} ,{"id":1014047,"text":"1014047 - 1960 - Infectious pancreatic necrosis of trout: I. A tissue-culture study","interactions":[],"lastModifiedDate":"2025-07-31T15:25:52.799954","indexId":"1014047","displayToPublicDate":"1960-01-01T00:00:00","publicationYear":"1960","noYear":false,"publicationType":{"id":2,"text":"Article"},"publicationSubtype":{"id":10,"text":"Journal Article"},"seriesTitle":{"id":3196,"text":"Progressive Fish-Culturist","active":true,"publicationSubtype":{"id":10}},"title":"Infectious pancreatic necrosis of trout: I. A tissue-culture study","docAbstract":"No abstract available.
","language":"English","publisher":"Oxford Academic","doi":"10.1577/1548-8659(1960)22[64:IPNOT]2.0.CO;2","usgsCitation":"Wolf, K., Dunbar, C.E., and Snieszko, S.F., 1960, Infectious pancreatic necrosis of trout: I. A tissue-culture study: Progressive Fish-Culturist, v. 22, no. 2, p. 64-68, https://doi.org/10.1577/1548-8659(1960)22[64:IPNOT]2.0.CO;2.","productDescription":"5 p.","startPage":"64","endPage":"68","numberOfPages":"5","costCenters":[{"id":365,"text":"Leetown Science Center","active":true,"usgs":true}],"links":[{"id":131356,"rank":1,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/thumbnails/outside_thumb.jpg"}],"volume":"22","issue":"2","noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"4f4e49f1e4b07f02db5ee8d5","contributors":{"authors":[{"text":"Wolf, K.","contributorId":16344,"corporation":false,"usgs":true,"family":"Wolf","given":"K.","email":"","affiliations":[],"preferred":false,"id":319682,"contributorType":{"id":1,"text":"Authors"},"rank":1},{"text":"Dunbar, C. E.","contributorId":96623,"corporation":false,"usgs":true,"family":"Dunbar","given":"C.","middleInitial":"E.","affiliations":[],"preferred":false,"id":319683,"contributorType":{"id":1,"text":"Authors"},"rank":2},{"text":"Snieszko, S. F.","contributorId":13169,"corporation":false,"usgs":true,"family":"Snieszko","given":"S.","middleInitial":"F.","affiliations":[],"preferred":false,"id":319681,"contributorType":{"id":1,"text":"Authors"},"rank":3}]}} ,{"id":1000394,"text":"1000394 - 1960 - The yellow perch of Lake Erie","interactions":[],"lastModifiedDate":"2012-02-02T00:04:04","indexId":"1000394","displayToPublicDate":"1960-01-01T00:00:00","publicationYear":"1960","noYear":false,"publicationType":{"id":2,"text":"Article"},"publicationSubtype":{"id":10,"text":"Journal Article"},"seriesTitle":{"id":2937,"text":"Ohio Conservation Bulletin","active":true,"publicationSubtype":{"id":10}},"title":"The yellow perch of Lake Erie","docAbstract":"Abstract has not been submitted","largerWorkType":{"id":2,"text":"Article"},"largerWorkTitle":"Ohio Conservation Bulletin","largerWorkSubtype":{"id":10,"text":"Journal Article"},"language":"English","collaboration":"Out-of-print","usgsCitation":"Van Meter, H.D., 1960, The yellow perch of Lake Erie: Ohio Conservation Bulletin, v. 24, no. 11, p. 22-23.","productDescription":"p. 22-23","startPage":"22","endPage":"23","numberOfPages":"1","costCenters":[{"id":324,"text":"Great Lakes Science Center","active":true,"usgs":true}],"links":[{"id":128905,"rank":0,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/thumbnails/outside_thumb.jpg"}],"volume":"24","issue":"11","noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"4f4e4a57e4b07f02db62e88c","contributors":{"authors":[{"text":"Van Meter, Harry D.","contributorId":36887,"corporation":false,"usgs":true,"family":"Van Meter","given":"Harry","email":"","middleInitial":"D.","affiliations":[],"preferred":false,"id":308501,"contributorType":{"id":1,"text":"Authors"},"rank":1}]}} ,{"id":1000470,"text":"1000470 - 1960 - Seasonal abundance and vertical movements of planktonic crustacea in Lake Michigan","interactions":[],"lastModifiedDate":"2012-03-02T17:16:04","indexId":"1000470","displayToPublicDate":"1960-01-01T00:00:00","publicationYear":"1960","noYear":false,"publicationType":{"id":2,"text":"Article"},"publicationSubtype":{"id":10,"text":"Journal Article"},"seriesTitle":{"id":1663,"text":"Fishery Bulletin","printIssn":"0090-0656","active":true,"publicationSubtype":{"id":10}},"title":"Seasonal abundance and vertical movements of planktonic crustacea in Lake Michigan","docAbstract":"U. 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Fish and Wildlife Service Fishery Bulletin no. 172","largerWorkType":{"id":2,"text":"Article"},"largerWorkTitle":"Fishery Bulletin","largerWorkSubtype":{"id":10,"text":"Journal Article"},"language":"English","publisher":"U.S. Fish and Wildlife Service","collaboration":"Out-of-print","usgsCitation":"Wells, L., 1960, Seasonal abundance and vertical movements of planktonic crustacea in Lake Michigan: Fishery Bulletin, v. 60, p. 343-369.","productDescription":"p. 343-369","startPage":"343","endPage":"369","numberOfPages":"26","costCenters":[{"id":324,"text":"Great Lakes Science Center","active":true,"usgs":true}],"links":[{"id":130394,"rank":0,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/thumbnails/outside_thumb.jpg"}],"volume":"60","noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"4f4e4a0ce4b07f02db5fc431","contributors":{"authors":[{"text":"Wells, LaRue","contributorId":75476,"corporation":false,"usgs":true,"family":"Wells","given":"LaRue","email":"","affiliations":[],"preferred":false,"id":308592,"contributorType":{"id":1,"text":"Authors"},"rank":1}]}} ,{"id":1000358,"text":"1000358 - 1960 - The bottom fauna of Lake Huron","interactions":[],"lastModifiedDate":"2016-03-10T13:32:13","indexId":"1000358","displayToPublicDate":"1960-01-01T00:00:00","publicationYear":"1960","noYear":false,"publicationType":{"id":2,"text":"Article"},"publicationSubtype":{"id":10,"text":"Journal Article"},"seriesTitle":{"id":3624,"text":"Transactions of the American Fisheries Society","active":true,"publicationSubtype":{"id":10}},"title":"The bottom fauna of Lake Huron","docAbstract":"The examination of 63 bottom samples, collected in Lake Huron in 1952 and 1956, revealed that Pontoporeia affinis was the dominant organism in both deep and shallow water. The next most abundant organisms in deep water were oligochaetes, fingernail clams, and midge larvae. Midge larvae were more numerous than either oligochaetes or fingernail clams in shallow water. The nmnber of organisms per square meter was similar to that determined from a similar study on Lake Michigan.
","language":"English","publisher":"Taylor & Francis","doi":"10.1577/1548-8659(1960)89[193:TBFOLH]2.0.CO;2","usgsCitation":"Teter, H.D., 1960, The bottom fauna of Lake Huron: Transactions of the American Fisheries Society, v. 89, no. 2, p. 193-197, https://doi.org/10.1577/1548-8659(1960)89[193:TBFOLH]2.0.CO;2.","productDescription":"5 p.","startPage":"193","endPage":"197","onlineOnly":"N","additionalOnlineFiles":"N","costCenters":[{"id":324,"text":"Great Lakes Science Center","active":true,"usgs":true}],"links":[{"id":128938,"rank":0,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/thumbnails/outside_thumb.jpg"}],"volume":"89","issue":"2","noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"4f4e4aaae4b07f02db6696c7","contributors":{"authors":[{"text":"Teter, Howard D.","contributorId":22282,"corporation":false,"usgs":true,"family":"Teter","given":"Howard","email":"","middleInitial":"D.","affiliations":[],"preferred":false,"id":308449,"contributorType":{"id":1,"text":"Authors"},"rank":1}]}} ,{"id":1000368,"text":"1000368 - 1960 - Colorimetric determination of halogenated nitrophenols added to streams as sea lamprey larvicides","interactions":[],"lastModifiedDate":"2016-03-10T13:34:18","indexId":"1000368","displayToPublicDate":"1960-01-01T00:00:00","publicationYear":"1960","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":"Colorimetric determination of halogenated nitrophenols added to streams as sea lamprey larvicides","docAbstract":"No abstract available.
","language":"English","publisher":"ACS Publications","doi":"10.1021/ac60168a036","usgsCitation":"Smith, M.A., Applegate, V.C., and Johnson, B.G., 1960, Colorimetric determination of halogenated nitrophenols added to streams as sea lamprey larvicides: Analytical Chemistry, v. 32, no. 12, p. 1670-1675, https://doi.org/10.1021/ac60168a036.","productDescription":"6 p.","startPage":"1670","endPage":"1675","onlineOnly":"N","additionalOnlineFiles":"N","costCenters":[{"id":324,"text":"Great Lakes Science Center","active":true,"usgs":true}],"links":[{"id":129062,"rank":0,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/thumbnails/outside_thumb.jpg"}],"volume":"32","issue":"12","noUsgsAuthors":false,"publicationDate":"2002-05-01","publicationStatus":"PW","scienceBaseUri":"4f4e4b24e4b07f02db6ae7c5","contributors":{"authors":[{"text":"Smith, Manning A.","contributorId":77090,"corporation":false,"usgs":false,"family":"Smith","given":"Manning","email":"","middleInitial":"A.","affiliations":[],"preferred":false,"id":308469,"contributorType":{"id":1,"text":"Authors"},"rank":1},{"text":"Applegate, Vernon C.","contributorId":39317,"corporation":false,"usgs":true,"family":"Applegate","given":"Vernon","email":"","middleInitial":"C.","affiliations":[],"preferred":false,"id":308467,"contributorType":{"id":1,"text":"Authors"},"rank":2},{"text":"Johnson, B. G. H.","contributorId":48511,"corporation":false,"usgs":false,"family":"Johnson","given":"B.","email":"","middleInitial":"G. H.","affiliations":[],"preferred":false,"id":308468,"contributorType":{"id":1,"text":"Authors"},"rank":3}]}} ,{"id":1003288,"text":"1003288 - 1960 - The new Fish Control Laboratory at La Crosse","interactions":[],"lastModifiedDate":"2013-04-17T21:21:11","indexId":"1003288","displayToPublicDate":"1960-01-01T00:00:00","publicationYear":"1960","noYear":false,"publicationType":{"id":2,"text":"Article"},"publicationSubtype":{"id":10,"text":"Journal Article"},"seriesTitle":{"id":964,"text":"Badger Sportsman","active":true,"publicationSubtype":{"id":10}},"title":"The new Fish Control Laboratory at La Crosse","docAbstract":"Abstract has not been submitted","largerWorkType":{"id":2,"text":"Article"},"largerWorkTitle":"Badger Sportsman","largerWorkSubtype":{"id":10,"text":"Journal Article"},"language":"English","usgsCitation":"Lennon, R.E., 1960, The new Fish Control Laboratory at La Crosse: Badger Sportsman, v. 16, no. 6.","productDescription":"p. 5","startPage":"5","numberOfPages":"-4","costCenters":[{"id":606,"text":"Upper Midwest Environmental Sciences Center","active":true,"usgs":true}],"links":[{"id":129673,"rank":0,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/thumbnails/outside_thumb.jpg"}],"volume":"16","issue":"6","noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"4f4e4a80e4b07f02db649925","contributors":{"authors":[{"text":"Lennon, R. E.","contributorId":37275,"corporation":false,"usgs":true,"family":"Lennon","given":"R.","middleInitial":"E.","affiliations":[],"preferred":false,"id":313074,"contributorType":{"id":1,"text":"Authors"},"rank":1}]}} ,{"id":1000343,"text":"1000343 - 1960 - Lake Erie walleyes--again on the upswing?","interactions":[],"lastModifiedDate":"2012-02-02T00:04:05","indexId":"1000343","displayToPublicDate":"1960-01-01T00:00:00","publicationYear":"1960","noYear":false,"publicationType":{"id":2,"text":"Article"},"publicationSubtype":{"id":10,"text":"Journal Article"},"seriesTitle":{"id":2937,"text":"Ohio Conservation Bulletin","active":true,"publicationSubtype":{"id":10}},"title":"Lake Erie walleyes--again on the upswing?","docAbstract":"SUMMARY The effect of DDT dust on wildlife was studied at Camp Bullis, Bexar County, Texas, in the summer of 1947. Studies were made on a 206.6 acre plot that was treated with DDT for experimental control of the Lone Star tick (Amblyomrna americanum). A dust consisting of one part of DDT to nine parts of pyrophyllite was applied at an average rate of 4.4 pounds of DDT per acre. The limits of DDT concentration that affected wildlife cannot be stated exactly because of a heavy rain that fell near the end of the dusting, and because of irregularity in DDT deposition. Since absolute uniformity of dusting could not be expected in any large scale DDT application, the effects observed in these trials were probably fairly representative. However, continued dry weather would have permitted longer exposure to DDT, possibly with more severe effects than those found in this study. The vegetation of the experimental area was roughly 70 percent ungrazed tall-grass prairie and 30 percent trees and shrubs. Ground and bush feeding birds were severely affected. Cardinals, lark sparrows, field sparrows, Bewick's wrens, Carolina wrens, Kentucky warblers, yellow-breasted chats, blue grosbeaks, and painted buntings were nearly or entirely eliminated from the treated area. Birds affected, but less drastically reduced in numbers, were yellow-billed cuckoo, black and white warbler, yellow-throated vireo, and white-eyed vireo. Birds found dead in the DDT area were 9 cardinals, 2 painted buntings, 2 lark sparrows, 1 yellow-breasted chat, and 1 white-eyed vireo. Bird mortality had begun by the day after dusting and was largely over by the end of the fifth day. Census of deer in DDT and check areas before and after treatment showed no reduction in deer numbers and no diminution in use of the DDT area. No deer or fawns were found dead or affected. Box-trapping of raccoons in DDT and check areas before and after treatment showed no effects that could be attributed to DDT. Limited observations on armadillos, striped skunks, and rabbits gave no indication of pronounced damage to these forms. No mammals of any kind were found dead or affected in or near the DDT area. Four rough green snakes and one Texan spiny lizard were found dead in the DDT area. Mortality was probably high among insectivorous reptiles.","largerWorkType":{"id":2,"text":"Article"},"largerWorkTitle":"Ohio Conservation Bulletin","largerWorkSubtype":{"id":10,"text":"Journal Article"},"language":"English","collaboration":"Out-of-print","usgsCitation":"Seldon, C.P., and Van Meter, H.D., 1960, Lake Erie walleyes--again on the upswing?: Ohio Conservation Bulletin, v. 24, no. 1, p. 5-7.","productDescription":"p. 5-7","startPage":"5","endPage":"7","numberOfPages":"2","costCenters":[{"id":324,"text":"Great Lakes Science Center","active":true,"usgs":true}],"links":[{"id":128894,"rank":0,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/thumbnails/outside_thumb.jpg"}],"volume":"24","issue":"1","noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"4f4e4b2fe4b07f02db6b4075","contributors":{"authors":[{"text":"Seldon, Charles P.","contributorId":57398,"corporation":false,"usgs":true,"family":"Seldon","given":"Charles","email":"","middleInitial":"P.","affiliations":[],"preferred":false,"id":308428,"contributorType":{"id":1,"text":"Authors"},"rank":1},{"text":"Van Meter, Harry D.","contributorId":36887,"corporation":false,"usgs":true,"family":"Van Meter","given":"Harry","email":"","middleInitial":"D.","affiliations":[],"preferred":false,"id":308427,"contributorType":{"id":1,"text":"Authors"},"rank":2}]}} ]}