Bluegills were exposed to sodium arsenite at various concentrations and treatment frequencies in outdoor pools. The effects of the treatments on the fish and invertebrates in the pools were assessed. Applications totaling 4.0 ppm or more of NaAsO2 during the experiment were reflected in reduced survival and growth of the fish, with immature fish being affected to a greater degree than adults. Some pathological changes were observed in adults. Substantial residues of arsenic were found in the water, bottom soil, and throughout the organs and flesh of the bluegills at the termination of the experiment. Bottom fauna and plankton populations were reduced or inhibited in several pools with the highest concentrations of the herbicide.
","language":"English","publisher":"American Fisheries Society","doi":"10.1577/1548-8659(1966)95[289:SEOSCO]2.0.CO;2","usgsCitation":"Gilderhus, P., 1966, Some effects of sublethal concentrations of sodium arsenite on bluegills and the aquatic environment: Transactions of the American Fisheries Society, v. 95, no. 3, p. 289-296, https://doi.org/10.1577/1548-8659(1966)95[289:SEOSCO]2.0.CO;2.","productDescription":"8 p.","startPage":"289","endPage":"296","costCenters":[{"id":606,"text":"Upper Midwest Environmental Sciences Center","active":true,"usgs":true}],"links":[{"id":131099,"rank":1,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/thumbnails/outside_thumb.jpg"}],"volume":"95","issue":"3","noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"4f4e49e9e4b07f02db5e93b3","contributors":{"authors":[{"text":"Gilderhus, P.A.","contributorId":60156,"corporation":false,"usgs":true,"family":"Gilderhus","given":"P.A.","affiliations":[],"preferred":false,"id":313032,"contributorType":{"id":1,"text":"Authors"},"rank":1}]}} ,{"id":70208668,"text":"70208668 - 1966 - The occurrence of Oestrus ovis L. (Diptera: Oestridae) in the bighorn sheep from Wyoming and Montana","interactions":[],"lastModifiedDate":"2020-02-24T12:16:21","indexId":"70208668","displayToPublicDate":"1966-06-30T12:06:27","publicationYear":"1966","noYear":false,"publicationType":{"id":2,"text":"Article"},"publicationSubtype":{"id":10,"text":"Journal Article"},"seriesTitle":{"id":2414,"text":"Journal of Parasitology","active":true,"publicationSubtype":{"id":10}},"displayTitle":"The occurrence of Oestrus ovis L. (Diptera: Oestridae) in the bighorn sheep from Wyoming and Montana","title":"The occurrence of Oestrus ovis L. (Diptera: Oestridae) in the bighorn sheep from Wyoming and Montana","docAbstract":"Three previous and five new records of the domestic sheep bot, Oestrus ovis, from the bighorn sheep are given. The life history and descriptions of adult and larval forms are presented. The significance of the occurrence of the parasite in the abnormal host is discussed.
","language":"English","publisher":"American Society of Parasitologists","doi":"10.2307/3276337","usgsCitation":"Capelle, K., 1966, The occurrence of Oestrus ovis L. (Diptera: Oestridae) in the bighorn sheep from Wyoming and Montana: Journal of Parasitology, v. 52, no. 3, p. 618-621, https://doi.org/10.2307/3276337.","productDescription":"4 p.","startPage":"618","endPage":"621","costCenters":[{"id":456,"text":"National Wildlife Health Center","active":true,"usgs":true}],"links":[{"id":488869,"rank":0,"type":{"id":40,"text":"Open Access Publisher Index Page"},"url":"https://doi.org/10.2307/3276337","text":"Publisher Index Page"},{"id":372561,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/thumbnails/outside_thumb.jpg"}],"country":"United States","state":"Montana, Wyoming","geographicExtents":"{\n \"type\": \"FeatureCollection\",\n \"features\": [\n {\n \"type\": \"Feature\",\n \"properties\": {},\n \"geometry\": {\n \"type\": \"Polygon\",\n \"coordinates\": [\n [\n [\n -104.0185546875,\n 41.11246878918088\n ],\n [\n -104.0185546875,\n 49.06666839558117\n ],\n [\n -116.19140625,\n 49.06666839558117\n ],\n [\n -115.97167968750001,\n 47.87214396888731\n ],\n [\n -114.47753906249999,\n 46.58906908309182\n ],\n [\n -114.43359375,\n 45.583289756006316\n ],\n [\n -114.0380859375,\n 45.767522962149876\n ],\n [\n -113.4228515625,\n 44.933696389694674\n ],\n [\n -112.8515625,\n 44.465151013519616\n ],\n [\n -111.796875,\n 44.49650533109348\n ],\n [\n -111.181640625,\n 44.5278427984555\n ],\n [\n -111.1376953125,\n 41.07935114946899\n ],\n [\n -104.0185546875,\n 41.11246878918088\n ]\n ]\n ]\n }\n }\n ]\n}","volume":"52","issue":"3","noUsgsAuthors":false,"publicationStatus":"PW","contributors":{"authors":[{"text":"Capelle, K.J.","contributorId":19896,"corporation":false,"usgs":true,"family":"Capelle","given":"K.J.","email":"","affiliations":[],"preferred":false,"id":782947,"contributorType":{"id":1,"text":"Authors"},"rank":1}]}} ,{"id":70210801,"text":"70210801 - 1966 - Magnetotelluric soundings in the southwestern United States","interactions":[],"lastModifiedDate":"2020-06-25T18:15:39.225224","indexId":"70210801","displayToPublicDate":"1966-06-25T13:02:30","publicationYear":"1966","noYear":false,"publicationType":{"id":2,"text":"Article"},"publicationSubtype":{"id":10,"text":"Journal Article"},"seriesTitle":{"id":1808,"text":"Geophysics","active":true,"publicationSubtype":{"id":10}},"title":"Magnetotelluric soundings in the southwestern United States","docAbstract":"Twelve magnetotelluric soundings were made along a 460-mile traverse in the southwestern United States. Spectral analysis of digitized graphic records was used to determine apparent resistivities and phase differences for periods in the range 10-1,000 sec. The geoelectric section to depths of the order of 300 km was found to be divided into three principal layers. The layer nearest the surface has a resistivity of 200 ohm-m or less. The next layer, which begins in Paleozoic carbonate rock or near the top of the Precambrian rocks, has a resistivity of 500 ohm-m or more. The resistivity of the lowest layer is in the range 5-100 ohm-m and the depth to the top is in the range 20-150 km.
","language":"English","publisher":"GeoScienceWorld","doi":"10.1190/1.1439845","usgsCitation":"Plouff, D., 1966, Magnetotelluric soundings in the southwestern United States: Geophysics, v. 31, no. 6, p. 1145-1152, https://doi.org/10.1190/1.1439845.","productDescription":"8 p.","startPage":"1145","endPage":"1152","costCenters":[{"id":312,"text":"Geology, Minerals, Energy, and Geophysics Science Center","active":true,"usgs":true}],"links":[{"id":375923,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/thumbnails/outside_thumb.jpg"}],"country":"United States","state":"Arizona, Utah","otherGeospatial":"Southwestern United States","geographicExtents":"{\n \"type\": \"FeatureCollection\",\n \"features\": [\n {\n \"type\": \"Feature\",\n \"properties\": {},\n \"geometry\": {\n \"type\": \"Polygon\",\n \"coordinates\": [\n [\n [\n -110.8026123046875,\n 36.53170884914869\n ],\n [\n -109.248046875,\n 36.53170884914869\n ],\n [\n -109.248046875,\n 37.913867495923746\n ],\n [\n -110.8026123046875,\n 37.913867495923746\n ],\n [\n -110.8026123046875,\n 36.53170884914869\n ]\n ]\n ]\n }\n }\n ]\n}","volume":"31","issue":"6","noUsgsAuthors":false,"publicationStatus":"PW","contributors":{"authors":[{"text":"Plouff, Donald","contributorId":94657,"corporation":false,"usgs":true,"family":"Plouff","given":"Donald","email":"","affiliations":[],"preferred":false,"id":791511,"contributorType":{"id":1,"text":"Authors"},"rank":1}]}} ,{"id":70171214,"text":"70171214 - 1966 - Contamination of the freshwater ecosystem by pesticides","interactions":[],"lastModifiedDate":"2016-05-25T15:57:22","indexId":"70171214","displayToPublicDate":"1966-06-01T00:00:00","publicationYear":"1966","noYear":false,"publicationType":{"id":2,"text":"Article"},"publicationSubtype":{"id":10,"text":"Journal Article"},"seriesTitle":{"id":2163,"text":"Journal of Applied Ecology","active":true,"publicationSubtype":{"id":10}},"title":"Contamination of the freshwater ecosystem by pesticides","docAbstract":"
A large part of our disquieting present-day pesticide problem is intimately tied to the freshwater ecosystem. Economic poisons are used in so many types of terrain to control so many kinds of organisms that almost all lakes and streams are likely to be contaminated. In addition to accidental contamination many pesticides are deliberately applied directly to fresh waters for suppression of aquatic animals or plants. The problem is intensified because of the extreme susceptibility of freshwater organisms. The complexity of freshwater environments and their variety makes it difficult to comprehend the total effect of pesticides.
Branch County has abundant water resources throughout most of its area. Almost all the water used is supplied by wells that obtain water from glacial drift deposits and locally from fractures and sandy beds in the Coldwater Shale. Glacial drift in buried bedrock valleys may yield large quantities of water to wells. Well yields are generally adequate for domestic and farm supplies. Properly developed large-diameter wells tapping thick beds of sand and gravel of the glacial drift can yield up to several thousands of gallons per minute locally. The hundreds of lakes and the many perennial streams have great recreational value. They are also a large potential source of water for some supplies. For example, it is estimated that 88 billion gallons of water runs off in streams of the county in an average year, and the lakes o the county hold about 42billion gallons of water in storage.
Problems of water supply to wells exist locally in some moraine and till areas of where the glacial drift is thin and the underlying bedrock yields only small quantities of water or none at all.
Ground water is generally hard to very hard and often contains excessive iron. Salty water is mainly a problem in areas where bedrock is the chief source.
Floods are not a serious problem largely because of the storage capacity of the lakes and the permeable materials in some stream basins. Based on measurements at eight stream sites the estimated amount of flow for 90 percent of the time ranges from 80,000 to 150,000 gallons per day per square mile of drainage area.
A special study of low levels in land-locked Gilead Lake indicated that this lake is semiperched and mostly dependent upon the water table for tits levels.
","language":"English","publisher":"Michigan Geological Survey","publisherLocation":"Lansing, MI","collaboration":"Prepared by U.S. Geological Survey in cooperation with County of Branch, and Michigan Geological Survey","usgsCitation":"Giroux, P., Stoimenoff, L., Nowlin, J., and Skinner, E., 1966, Water resources of Branch County, Michigan: Water Investigation, viii, 74 p.","productDescription":"viii, 74 p.","costCenters":[{"id":382,"text":"Michigan Water Science Center","active":true,"usgs":true}],"links":[{"id":338222,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/thumbnails/outside_thumb.jpg"},{"id":338218,"rank":1,"type":{"id":11,"text":"Document"},"url":"https://www.michigan.gov/documents/deq/WI_06_Aopt_309864_7.pdf","linkFileType":{"id":1,"text":"pdf"}}],"country":"United States","state":"Michigan","county":"Branch County","geographicExtents":"{\"type\":\"FeatureCollection\",\"features\":[{\"type\":\"Feature\",\"geometry\":{\"type\":\"Polygon\",\"coordinates\":[[[-84.8285,42.0724],[-84.8274,41.9861],[-84.8277,41.898],[-84.8273,41.8108],[-84.8273,41.7606],[-84.8673,41.7608],[-85.1978,41.7605],[-85.2212,41.7607],[-85.2913,41.7606],[-85.2923,41.811],[-85.2933,41.8969],[-85.2936,41.9854],[-85.2928,42.0717],[-85.1771,42.0733],[-85.0609,42.0734],[-85.0022,42.0732],[-84.8285,42.0724]]]},\"properties\":{\"name\":\"Branch\",\"state\":\"MI\"}}]}","noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"58d4df19e4b05ec79911d209","contributors":{"authors":[{"text":"Giroux, P.R.","contributorId":59055,"corporation":false,"usgs":true,"family":"Giroux","given":"P.R.","email":"","affiliations":[],"preferred":false,"id":685945,"contributorType":{"id":1,"text":"Authors"},"rank":1},{"text":"Stoimenoff, L.E.","contributorId":34157,"corporation":false,"usgs":true,"family":"Stoimenoff","given":"L.E.","email":"","affiliations":[],"preferred":false,"id":685946,"contributorType":{"id":1,"text":"Authors"},"rank":2},{"text":"Nowlin, J. O.","contributorId":40604,"corporation":false,"usgs":true,"family":"Nowlin","given":"J. O.","affiliations":[],"preferred":false,"id":685947,"contributorType":{"id":1,"text":"Authors"},"rank":3},{"text":"Skinner, E.L.","contributorId":53412,"corporation":false,"usgs":true,"family":"Skinner","given":"E.L.","email":"","affiliations":[{"id":595,"text":"U.S. Geological Survey","active":false,"usgs":true}],"preferred":false,"id":685948,"contributorType":{"id":1,"text":"Authors"},"rank":4}]}} ,{"id":70010736,"text":"70010736 - 1966 - Geomagnetic polarity epochs: A new polarity event and the age of the Brunhes-Matuyama boundary","interactions":[],"lastModifiedDate":"2026-02-10T16:39:10.879439","indexId":"70010736","displayToPublicDate":"1966-05-20T00:00:00","publicationYear":"1966","noYear":false,"publicationType":{"id":2,"text":"Article"},"publicationSubtype":{"id":10,"text":"Journal Article"},"seriesTitle":{"id":3338,"text":"Science","active":true,"publicationSubtype":{"id":10}},"title":"Geomagnetic polarity epochs: A new polarity event and the age of the Brunhes-Matuyama boundary","docAbstract":"Recent paleomagnetic-radiometric data from six rhyolite domes in the Valles Caldera, New Mexico, indicate that the last change in polarity of the earth's magnetic field from reversed to normal (the Brunhes-Matuyama boundary) occurred at about 0.7 million years ago. A previously undiscovered geomagnetic polarity event, herein named the \"Jaramillo normal event,\" occurred about 0.9 million years ago.","language":"English","publisher":"American Association for the Advancement of Science","doi":"10.1126/science.152.3725.1060","issn":"00368075","usgsCitation":"Doell, R., and Dalrymple, G.B., 1966, Geomagnetic polarity epochs: A new polarity event and the age of the Brunhes-Matuyama boundary: Science, v. 152, no. 3725, p. 1060-1061, https://doi.org/10.1126/science.152.3725.1060.","productDescription":"2 p.","startPage":"1060","endPage":"1061","costCenters":[],"links":[{"id":219561,"rank":1,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/thumbnails/outside_thumb.jpg"}],"country":"United States","state":"New Mexico","otherGeospatial":"Valles Caldera","geographicExtents":"{\n \"type\": \"FeatureCollection\",\n \"features\": [\n {\n \"type\": \"Feature\",\n \"properties\": {},\n \"geometry\": {\n \"coordinates\": [\n [\n [\n -106.64619231455076,\n 35.94364196549704\n ],\n [\n -106.64619231455076,\n 35.82353517773839\n ],\n [\n -106.42705212925159,\n 35.82353517773839\n ],\n [\n -106.42705212925159,\n 35.94364196549704\n ],\n [\n -106.64619231455076,\n 35.94364196549704\n ]\n ]\n ],\n \"type\": \"Polygon\"\n }\n }\n ]\n}","volume":"152","issue":"3725","noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"505a275de4b0c8380cd597f4","contributors":{"authors":[{"text":"Doell, Richard R.","contributorId":66683,"corporation":false,"usgs":true,"family":"Doell","given":"Richard R.","affiliations":[],"preferred":false,"id":359530,"contributorType":{"id":1,"text":"Authors"},"rank":1},{"text":"Dalrymple, G. B.","contributorId":10407,"corporation":false,"usgs":true,"family":"Dalrymple","given":"G.","email":"","middleInitial":"B.","affiliations":[],"preferred":false,"id":359529,"contributorType":{"id":1,"text":"Authors"},"rank":2}]}} ,{"id":70221232,"text":"70221232 - 1966 - Preliminary investigation of the source of lead and strontium in deep geothermal brines underlying the Salton Sea geothermal area","interactions":[],"lastModifiedDate":"2021-06-09T15:03:31.857207","indexId":"70221232","displayToPublicDate":"1966-05-01T08:59:08","publicationYear":"1966","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":"Preliminary investigation of the source of lead and strontium in deep geothermal brines underlying the Salton Sea geothermal area","docAbstract":"A radiogenic tracer study has been made of lead and strontium in deep geothermal brines, salt from brine, and the upper Quaternary rhyolite domes near the Salton Sea in the Imperial Valley, California. The data on the brines and rhyolite glasses are compared to those from Quaternary Colorado River and Tertiary sediments of the area. The brines sampled contain '-'100 ppm Pb, sufficient for consideration as a possible ore-forming fluid. The isotopic data indicate that 80-100 percent of the strontium and 50-100 percent of the lead in these brines were acquired from the associated sediments. The isotopic compositions of lead and strontium in the Quaternary rhyolite glasses are distinctly different from those of the sediments and brines. The strontium data suggest that the rhyolite glasses were derived from basaltic or gabbroic material but may have attained as much as 40 percent of their strontium from upper crustal rocks such as the sediments analyzed.
","language":"English","publisher":"Society of Economic Geologists","doi":"10.2113/gsecongeo.61.3.462","usgsCitation":"Doe, B.R., Hedge, C., and White, D., 1966, Preliminary investigation of the source of lead and strontium in deep geothermal brines underlying the Salton Sea geothermal area: Economic Geology, v. 61, no. 3, p. 462-483, https://doi.org/10.2113/gsecongeo.61.3.462.","productDescription":"22 p.","startPage":"462","endPage":"483","costCenters":[],"links":[{"id":386285,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/thumbnails/outside_thumb.jpg"}],"country":"United States","state":"California","otherGeospatial":"Salton Sea","geographicExtents":"{\n \"type\": \"FeatureCollection\",\n \"features\": [\n {\n \"type\": \"Feature\",\n \"properties\": {},\n \"geometry\": {\n \"type\": \"Polygon\",\n \"coordinates\": [\n [\n [\n -116.27929687499999,\n 32.99945000822837\n ],\n [\n -115.46630859375,\n 32.99945000822837\n ],\n [\n -115.46630859375,\n 33.75174787568194\n ],\n [\n -116.27929687499999,\n 33.75174787568194\n ],\n [\n -116.27929687499999,\n 32.99945000822837\n ]\n ]\n ]\n }\n }\n ]\n}","volume":"61","issue":"3","noUsgsAuthors":false,"publicationDate":"1966-05-01","publicationStatus":"PW","contributors":{"authors":[{"text":"Doe, B. R.","contributorId":52173,"corporation":false,"usgs":true,"family":"Doe","given":"B.","email":"","middleInitial":"R.","affiliations":[],"preferred":false,"id":817152,"contributorType":{"id":1,"text":"Authors"},"rank":1},{"text":"Hedge, C. E.","contributorId":73611,"corporation":false,"usgs":true,"family":"Hedge","given":"C. E.","affiliations":[],"preferred":false,"id":817153,"contributorType":{"id":1,"text":"Authors"},"rank":2},{"text":"White, D. E.","contributorId":139650,"corporation":false,"usgs":false,"family":"White","given":"D. E.","affiliations":[{"id":6672,"text":"former: USGS Southwest Biological Science Center, Colorado Plateau Research Station, Flagstaff, AZ. Current address: TN-SCORE, Univ of Tennessee, Knoxville, TN, e-mail: jennen@gmail.com","active":true,"usgs":false}],"preferred":false,"id":817155,"contributorType":{"id":1,"text":"Authors"},"rank":3}]}} ,{"id":70221231,"text":"70221231 - 1966 - Stratified deposits of the oxides and carbonates of manganese","interactions":[],"lastModifiedDate":"2021-06-08T13:55:30.965707","indexId":"70221231","displayToPublicDate":"1966-05-01T08:51:42","publicationYear":"1966","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":"Stratified deposits of the oxides and carbonates of manganese","docAbstract":"Compared with the stratified deposits of iron minerals, those of manganese minerals have received little attention until recent years. Before 1930, students of the stratified deposits of manganese minerals have generally concluded that the contained manganese was derived from the decomposition of the rocks that formed the borders of the basins. Only in a few places have geologists recognized that if these rocks were the principal source of the contained manganese the basins should contain also enormous quantities of iron minerals, whereas most of the large deposits of manganese contain little iron. Even though more than 100 years ago some geologists proposed that the iron contained in some deposits of stratified iron minerals was probably derived from hydrothermal waters related to centers of volcanism, not until about 1930 was this source of manganese in similar deposits seriously proposed. This mode of origin was given the name \"volcanogene sedimentaire\" by French geologists working in Morocco. Since then, other names, such as \"exhalative sedimentaire,\" have been used by geologists working in several European districts. Because of the development of new techniques for the study of the chemical and physical features of the minerals, and because close attention to the lithologic environments of the beds is being given more and more during recent years, it has seemed advisable to review the features of stratified deposits of the manganese minerals in many parts of the world and over a wide range in age. This study indicates that at least three sources may have contributed the manganese in the large deposits of iron-free oxides and carbonates: (1) the rocks that form the borders of the basins, either marine or continental; (2) the nearby underlying sediments, largely of igneous origin, decomposed by warm waters largely derived from depth; and (3) waters of hydrothermal origin derived from great depths during epochs of volcanism from which iron minerals with little manganese are deposited in deep zones, then minerals with much iron and more manganese at intermediate depths, and, finally, manganese minerals with little iron near the surface. As the hot waters of many thermal springs contain more manganese than iron, such waters could yield the pure manganese oxides and carbonates found in stratified deposits. Several kinds of evidence indicate that most of the manganese in the large stratified deposits of the oxides and carbonates of manganese in many parts of the world has been derived from hydrothermal waters from depth related to centers of volcanism. Obviously, manganese derived from decay of the rocks on the lands adjacent to large basins-marine and continental -may have been added to that derived from centers of volcanism to form the sedimentary deposits found in the basins.
","language":"English","publisher":"Society of Economic Geologists","doi":"10.2113/gsecongeo.61.3.431","usgsCitation":"Hewett, D.F., 1966, Stratified deposits of the oxides and carbonates of manganese: Economic Geology, v. 61, no. 3, p. 431-461, https://doi.org/10.2113/gsecongeo.61.3.431.","productDescription":"31 p.","startPage":"431","endPage":"461","costCenters":[],"links":[{"id":386284,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/thumbnails/outside_thumb.jpg"}],"volume":"61","issue":"3","noUsgsAuthors":false,"publicationDate":"1966-05-01","publicationStatus":"PW","contributors":{"authors":[{"text":"Hewett, D. F.","contributorId":19927,"corporation":false,"usgs":true,"family":"Hewett","given":"D.","email":"","middleInitial":"F.","affiliations":[],"preferred":false,"id":817151,"contributorType":{"id":1,"text":"Authors"},"rank":1}]}} ,{"id":70171218,"text":"70171218 - 1966 - Dechlorination of DDT by Aerobacter aerogenes","interactions":[],"lastModifiedDate":"2016-05-25T16:08:49","indexId":"70171218","displayToPublicDate":"1966-04-29T00:00:00","publicationYear":"1966","noYear":false,"publicationType":{"id":2,"text":"Article"},"publicationSubtype":{"id":10,"text":"Journal Article"},"seriesTitle":{"id":3338,"text":"Science","active":true,"publicationSubtype":{"id":10}},"title":"Dechlorination of DDT by Aerobacter aerogenes","docAbstract":"Dechlorination of DDT to DDD in higher animals requires the presence of molecular oxygen, but in microorganisms the presence of oxygen hinders dechlorination. In cell-free preparations of Aerobacter aerogenes, the use of selected metabolic inhibitors indicated that reduced Fe(II) cytochrome oxidase was responsible for DDT dechlorination. This finding may possibly explain. the persistence of DDT residues in soils and sediments.
","language":"English","publisher":"American Association for the Advancement of Science","doi":"10.1126/science.152.3722.647","usgsCitation":"Wedemeyer, G., 1966, Dechlorination of DDT by Aerobacter aerogenes: Science, v. 152, no. 3722, p. 647-647, https://doi.org/10.1126/science.152.3722.647.","productDescription":"1 p.","startPage":"647","endPage":"647","onlineOnly":"N","additionalOnlineFiles":"N","costCenters":[{"id":192,"text":"Columbia Environmental Research Center","active":true,"usgs":true}],"links":[{"id":321679,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/thumbnails/outside_thumb.jpg"}],"volume":"152","issue":"3722","noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"5746ccb4e4b07e28b662dc66","contributors":{"authors":[{"text":"Wedemeyer, Gary gwedemeyer@usgs.gov","contributorId":5504,"corporation":false,"usgs":true,"family":"Wedemeyer","given":"Gary","email":"gwedemeyer@usgs.gov","affiliations":[],"preferred":true,"id":630293,"contributorType":{"id":1,"text":"Authors"},"rank":1}]}} ,{"id":5220442,"text":"5220442 - 1966 - Proportion of recovered duck bands that are reported","interactions":[],"lastModifiedDate":"2025-02-12T15:25:10.156198","indexId":"5220442","displayToPublicDate":"1966-04-04T00:00:00","publicationYear":"1966","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":"Proportion of recovered duck bands that are reported","docAbstract":"Band-reporting rates (the proportion of duck bands recovered by hunters that are actually reported to the Bird Banding Laboratory) appear to have decreased between the late 1950's and early 1960's. About one-half the banded ducks bagged during the 1958-59 and 1959-60 hunting seasons were reported-a rate similar to those recorded in other studies conducted during the early and mid-1950's. Band-reporting rates were lower for the 1962-63 and 1962-64 hunting seasons; less than one-third of the banded ducks bagged were reported. This decrease in band-reporting rates was concurrent with significant changes in duck hunting regulations, the volume of duck banding, and the method used to relay information to the person who reports a band. Band-reporting rates differed for various species of ducks. In general, band-reporting rates were high on canvasbacks (Aythya valisineria), redheads (A. americana), and pintails (Anas acuta) and low for teals (Anas discors and A. carolinensis).
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\"}}]}","noUsgsAuthors":false,"publicationStatus":"PW","contributors":{"authors":[{"text":"Busch, W. F.","contributorId":67968,"corporation":false,"usgs":true,"family":"Busch","given":"W.","email":"","middleInitial":"F.","affiliations":[],"preferred":false,"id":829262,"contributorType":{"id":1,"text":"Authors"},"rank":1},{"text":"Shaw, L. C.","contributorId":21162,"corporation":false,"usgs":true,"family":"Shaw","given":"L.","email":"","middleInitial":"C.","affiliations":[],"preferred":false,"id":829263,"contributorType":{"id":1,"text":"Authors"},"rank":2}]}} ,{"id":70221246,"text":"70221246 - 1966 - Packer testing in water wells near Sarasota, Florida","interactions":[],"lastModifiedDate":"2021-06-08T15:03:04.793505","indexId":"70221246","displayToPublicDate":"1966-04-01T09:58:04","publicationYear":"1966","noYear":false,"publicationType":{"id":2,"text":"Article"},"publicationSubtype":{"id":10,"text":"Journal Article"},"seriesTitle":{"id":3825,"text":"Groundwater","active":true,"publicationSubtype":{"id":10}},"title":"Packer testing in water wells near Sarasota, Florida","docAbstract":"During February and March 1964, the U. S. Geological Survey ran caliper, conductance, and temperature logs on several wells in the Sarasota area. The Florida Geological Survey had previously run gamma ray and electric logs on the same wells. Two flowing wells were selected for packer testing. The two wells are about the same depth, penetrate essentially the same geologic horizons, and are about 16 miles apart. The packers were set in the wells between the producing horizons of the formations penetrated and each of the horizons was tested for head, amount of production, and quality of water. One of the tests produced excellent results, indicating that the various producing zones were effectively isolated by the packers and that different quality of water, quantity of water, and a different head was available from each zone. The other test did not show sharp differences but did indicate the extent of contamination of the producing horizons in a flowing well which had been capped for approximately two years. These tests indicate that packer testing can measurably add to knowledge of the separation of permeable zones.
","language":"English","publisher":"NGWA The Groundwater Association","doi":"10.1111/j.1745-6584.1966.tb01595.x","usgsCitation":"Sutcliffe, H., and Joyner, B., 1966, Packer testing in water wells near Sarasota, Florida: Groundwater, v. 4, no. 2, p. 23-27, https://doi.org/10.1111/j.1745-6584.1966.tb01595.x.","productDescription":"5 p.","startPage":"23","endPage":"27","costCenters":[],"links":[{"id":386293,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/thumbnails/outside_thumb.jpg"}],"country":"United States","state":"Florida","city":"Sarasota","geographicExtents":"{\n \"type\": \"FeatureCollection\",\n \"features\": [\n {\n \"type\": \"Feature\",\n \"properties\": {},\n \"geometry\": {\n \"type\": \"Polygon\",\n \"coordinates\": [\n [\n [\n -82.5732421875,\n 27.186242185608737\n ],\n [\n -82.408447265625,\n 27.186242185608737\n ],\n [\n -82.408447265625,\n 27.410785702577023\n ],\n [\n -82.5732421875,\n 27.410785702577023\n ],\n [\n -82.5732421875,\n 27.186242185608737\n ]\n ]\n ]\n }\n }\n ]\n}","volume":"4","issue":"2","noUsgsAuthors":false,"publicationDate":"2006-07-06","publicationStatus":"PW","contributors":{"authors":[{"text":"Sutcliffe, Horace Jr.","contributorId":96725,"corporation":false,"usgs":true,"family":"Sutcliffe","given":"Horace","suffix":"Jr.","email":"","affiliations":[],"preferred":false,"id":817162,"contributorType":{"id":1,"text":"Authors"},"rank":1},{"text":"Joyner, B.F.","contributorId":55899,"corporation":false,"usgs":true,"family":"Joyner","given":"B.F.","email":"","affiliations":[],"preferred":false,"id":817163,"contributorType":{"id":1,"text":"Authors"},"rank":2}]}} ,{"id":70207356,"text":"70207356 - 1966 - Nitrogen compounds in natural water—A review","interactions":[],"lastModifiedDate":"2019-12-18T10:17:42","indexId":"70207356","displayToPublicDate":"1966-03-31T10:00:09","publicationYear":"1966","noYear":false,"publicationType":{"id":2,"text":"Article"},"publicationSubtype":{"id":10,"text":"Journal Article"},"seriesTitle":{"id":3722,"text":"Water Resources Research","onlineIssn":"1944-7973","printIssn":"0043-1397","active":true,"publicationSubtype":{"id":10}},"title":"Nitrogen compounds in natural water—A review","docAbstract":"Nitrogen compounds in natural water are significant in public health, agriculture, industry, and geochemistry. The many sources of nitrogen compounds and the deep involvement of nitrogen in the life processes of organisms makes the study of such compounds difficult. The sources include natural aerosols, precipitation, fixation by micro‐organisms in soil and water, decaying organic matter, and animal and industrial wastes, as well as probably undiscovered sources in consolidated and unconsolidated rocks. Nitrogen compounds are both oxidized and reduced by organisms. Some nitrogen compounds are adsorbed on clay. The theoretical end product in water and the compound probably most often determined is NO3−1. The concentration of nitregen compounds ranges from 0.0 to >100 ppm (parts per million) in surface water and from 0.0 to >1000 ppm in groundwater. Seasonal fluctuations occur. Much further research is needed, including improvements in methods of analysis, further investigation of sources, and detailed study of the nitrogen cycle in small drainage basins. (Key words: Geochemistry; quality of water.) This paper is not subject to U.S. copyright. Published in 1966 by the American Geophysical Union.
","language":"English","publisher":"American Geophysical Union","doi":"10.1029/WR002i001p00041","issn":"00431397","usgsCitation":"Feth, J.H., 1966, Nitrogen compounds in natural water—A review: Water Resources Research, v. 2, no. 1, p. 41-58, https://doi.org/10.1029/WR002i001p00041.","productDescription":"18 p. ","startPage":"41","endPage":"58","costCenters":[],"links":[{"id":370398,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/thumbnails/outside_thumb.jpg"}],"volume":"2","issue":"1","noUsgsAuthors":false,"publicationDate":"2010-07-09","publicationStatus":"PW","contributors":{"authors":[{"text":"Feth, J. H.","contributorId":50495,"corporation":false,"usgs":true,"family":"Feth","given":"J.","email":"","middleInitial":"H.","affiliations":[],"preferred":false,"id":777800,"contributorType":{"id":1,"text":"Authors"},"rank":1}]}} ,{"id":70206893,"text":"70206893 - 1966 - Hot brines and recent iron deposits in deeps of the Red Sea","interactions":[],"lastModifiedDate":"2019-11-26T10:37:35","indexId":"70206893","displayToPublicDate":"1966-03-30T10:28:56","publicationYear":"1966","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":"Hot brines and recent iron deposits in deeps of the Red Sea","docAbstract":"Sedimentary iron and heavy-metal deposits of undetermined size have been found in the middle of the Red Sea some 2000 meters below the surface of the sea (Fig. 1). This discovery has been made from the Research Vessel Atlantis II, which is still at sea engaged in a series of oceanographic investigations which ultimately will end in November 1965, after the ship has circumnavigated the globe. The discovery is significant because the environment and the processes controlling deposition of heavy metals are observable and appear to be still active.
","language":"English","publisher":"Elsevier","doi":"10.1016/0016-7037(66)90007-X","usgsCitation":"Miller, A., Densmore, C., Degens, E., Hathaway, J., Manheim, F., McFarlin, P., Pocklington, R., and Jokela, A., 1966, Hot brines and recent iron deposits in deeps of the Red Sea: Geochimica et Cosmochimica Acta, v. 30, no. 3, p. 341-359 & IN1, https://doi.org/10.1016/0016-7037(66)90007-X.","productDescription":"20 p.","startPage":"341","endPage":"359 & IN1","costCenters":[{"id":678,"text":"Woods Hole Coastal and Marine Science Center","active":true,"usgs":true}],"links":[{"id":369625,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/thumbnails/outside_thumb.jpg"}],"otherGeospatial":"Red Sea","geographicExtents":"{\n \"type\": \"FeatureCollection\",\n \"features\": [\n {\n \"type\": \"Feature\",\n \"properties\": {},\n \"geometry\": {\n \"type\": \"Polygon\",\n \"coordinates\": [\n [\n [\n 43.33007812499999,\n 12.168225677390119\n ],\n [\n 43.5498046875,\n 12.64033830684679\n ],\n [\n 42.7587890625,\n 15.453680224345835\n ],\n [\n 42.5390625,\n 17.056784609942554\n ],\n [\n 40.42968749999999,\n 19.89072302399691\n ],\n [\n 39.2431640625,\n 21.3303150734318\n ],\n [\n 39.111328125,\n 22.59372606392931\n ],\n [\n 37.8369140625,\n 24.327076540018634\n ],\n [\n 37.001953125,\n 24.806681353851964\n ],\n [\n 37.08984375,\n 25.24469595130604\n ],\n [\n 35.1123046875,\n 28.188243641850313\n ],\n [\n 34.80468749999999,\n 29.34387539941801\n ],\n [\n 34.1015625,\n 27.955591004642553\n ],\n [\n 32.431640625,\n 29.99300228455108\n ],\n [\n 32.3876953125,\n 29.34387539941801\n ],\n [\n 33.4423828125,\n 27.761329874505233\n ],\n [\n 35.5078125,\n 23.845649887659352\n ],\n [\n 35.6396484375,\n 22.87744046489713\n ],\n [\n 36.9140625,\n 21.94304553343818\n ],\n [\n 37.3974609375,\n 18.521283325496277\n ],\n [\n 38.5400390625,\n 18.020527657852337\n ],\n [\n 39.3310546875,\n 16.003575733881327\n ],\n [\n 39.7705078125,\n 15.284185114076433\n ],\n [\n 40.6494140625,\n 14.902321826141808\n ],\n [\n 43.1103515625,\n 12.597454504832005\n ],\n [\n 43.33007812499999,\n 12.168225677390119\n ]\n ]\n ]\n }\n }\n ]\n}","volume":"30","issue":"3","noUsgsAuthors":false,"publicationStatus":"PW","contributors":{"authors":[{"text":"Miller, A.R.","contributorId":87560,"corporation":false,"usgs":true,"family":"Miller","given":"A.R.","email":"","affiliations":[],"preferred":false,"id":776171,"contributorType":{"id":1,"text":"Authors"},"rank":1},{"text":"Densmore, C.D.","contributorId":94320,"corporation":false,"usgs":true,"family":"Densmore","given":"C.D.","email":"","affiliations":[],"preferred":false,"id":776172,"contributorType":{"id":1,"text":"Authors"},"rank":2},{"text":"Degens, E.T.","contributorId":76321,"corporation":false,"usgs":true,"family":"Degens","given":"E.T.","email":"","affiliations":[],"preferred":false,"id":776173,"contributorType":{"id":1,"text":"Authors"},"rank":3},{"text":"Hathaway, J.C.","contributorId":94280,"corporation":false,"usgs":true,"family":"Hathaway","given":"J.C.","email":"","affiliations":[],"preferred":false,"id":776174,"contributorType":{"id":1,"text":"Authors"},"rank":4},{"text":"Manheim, F.T. 0000-0003-4005-4524","orcid":"https://orcid.org/0000-0003-4005-4524","contributorId":55421,"corporation":false,"usgs":true,"family":"Manheim","given":"F.T.","affiliations":[],"preferred":false,"id":776175,"contributorType":{"id":1,"text":"Authors"},"rank":5},{"text":"McFarlin, P.F.","contributorId":33334,"corporation":false,"usgs":true,"family":"McFarlin","given":"P.F.","email":"","affiliations":[],"preferred":false,"id":776176,"contributorType":{"id":1,"text":"Authors"},"rank":6},{"text":"Pocklington, R.","contributorId":10050,"corporation":false,"usgs":true,"family":"Pocklington","given":"R.","email":"","affiliations":[],"preferred":false,"id":776177,"contributorType":{"id":1,"text":"Authors"},"rank":7},{"text":"Jokela, A.","contributorId":34153,"corporation":false,"usgs":true,"family":"Jokela","given":"A.","email":"","affiliations":[],"preferred":false,"id":776178,"contributorType":{"id":1,"text":"Authors"},"rank":8}]}} ,{"id":70010675,"text":"70010675 - 1966 - Oxygen and carbon isotopic composition of limestones and dolomites, Bikini and Eniwetok atolls","interactions":[],"lastModifiedDate":"2026-02-10T17:10:28.077354","indexId":"70010675","displayToPublicDate":"1966-03-04T00:00:00","publicationYear":"1966","noYear":false,"publicationType":{"id":2,"text":"Article"},"publicationSubtype":{"id":10,"text":"Journal Article"},"seriesTitle":{"id":3338,"text":"Science","active":true,"publicationSubtype":{"id":10}},"title":"Oxygen and carbon isotopic composition of limestones and dolomites, Bikini and Eniwetok atolls","docAbstract":"Aragonitic, unconsolidated sediments from the borings on the Eniwetok and Bikini atolls are isotopically identical with unaltered skeletal fragments, whereas the recrystallized limestones exhibit isotopic variations resulting from alteration in meteoric waters during periods of emergence. Dolomites and associated calcites are enriched in O18, perhaps because of interaction with hypersaline brines.
","language":"English","publisher":"AAAS","doi":"10.1126/science.151.3714.1082","usgsCitation":"Gross, M.G., and Tracey, J.I., 1966, Oxygen and carbon isotopic composition of limestones and dolomites, Bikini and Eniwetok atolls: Science, v. 151, no. 3714, p. 1082-1084, https://doi.org/10.1126/science.151.3714.1082.","productDescription":"3 p.","startPage":"1082","endPage":"1084","costCenters":[],"links":[{"id":219401,"rank":1,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.er.usgs.gov/thumbnails/outside_thumb.jpg"}],"country":"Republic of the Marshall Islands","otherGeospatial":"Bikini Atoll, Eniwetok Atoll","geographicExtents":"{\n \"type\": \"FeatureCollection\",\n \"features\": [\n {\n \"type\": \"Feature\",\n \"properties\": {},\n \"geometry\": {\n \"type\": \"Polygon\",\n \"coordinates\": [\n [\n [\n 161.47705078125,\n 11.070602913977819\n ],\n [\n 162.828369140625,\n 11.070602913977819\n ],\n [\n 162.828369140625,\n 11.942601073545658\n ],\n [\n 161.47705078125,\n 11.942601073545658\n ],\n [\n 161.47705078125,\n 11.070602913977819\n ]\n ]\n ]\n }\n },\n {\n \"type\": \"Feature\",\n \"properties\": {},\n \"geometry\": {\n \"type\": \"Polygon\",\n \"coordinates\": [\n [\n [\n 164.99267578125,\n 11.092165893502\n ],\n [\n 165.8935546875,\n 11.092165893502\n ],\n [\n 165.8935546875,\n 12.093038580274138\n ],\n [\n 164.99267578125,\n 12.093038580274138\n ],\n [\n 164.99267578125,\n 11.092165893502\n ]\n ]\n ]\n }\n }\n ]\n}","volume":"151","issue":"3714","noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"505a727ae4b0c8380cd76b05","contributors":{"authors":[{"text":"Gross, M. Grant","contributorId":50145,"corporation":false,"usgs":true,"family":"Gross","given":"M.","email":"","middleInitial":"Grant","affiliations":[],"preferred":false,"id":359406,"contributorType":{"id":1,"text":"Authors"},"rank":1},{"text":"Tracey, Joshua I. Jr.","contributorId":55420,"corporation":false,"usgs":true,"family":"Tracey","given":"Joshua","suffix":"Jr.","email":"","middleInitial":"I.","affiliations":[],"preferred":false,"id":359405,"contributorType":{"id":1,"text":"Authors"},"rank":2}]}} ,{"id":70221264,"text":"70221264 - 1966 - Rhizoconcretions in vitric ash-fall tuff, Nye County, Nevada","interactions":[],"lastModifiedDate":"2021-06-09T15:00:46.553398","indexId":"70221264","displayToPublicDate":"1966-03-01T13:31:52","publicationYear":"1966","noYear":false,"publicationType":{"id":2,"text":"Article"},"publicationSubtype":{"id":10,"text":"Journal Article"},"seriesTitle":{"id":1786,"text":"Geological Society of America Bulletin","active":true,"publicationSubtype":{"id":10}},"title":"Rhizoconcretions in vitric ash-fall tuff, Nye County, Nevada","docAbstract":"Small, vertically elongate concretionlike structures, here called rhizoconcretions, are found in scattered localities in and near the southern part of the Belted Range of Nye County, Nevada. The rhizoconcretions occur within a stratigraphically restricted zone in bedded vitric ash-fall tuff of late Tertiary age. The rhizoconcretions differ in mineralogy from their host rock in that they are cemented by a binder of undetermined composition, possibly a zeolite, whereas the host tuffs are un-cemented. These structures appear to have formed during diagenesis of the tuff by means of capillary movement of subsurface waters that reacted with volcanic glass within the conduits to form the cementing material.
","language":"English","publisher":"Geological Society of America","doi":"10.1130/0016-7606(1966)77[313:RIVATN]2.0.CO;2","usgsCitation":"Luft, S.J., 1966, Rhizoconcretions in vitric ash-fall tuff, Nye County, Nevada: Geological Society of America Bulletin, v. 77, no. 3, p. 313-318, https://doi.org/10.1130/0016-7606(1966)77[313:RIVATN]2.0.CO;2.","productDescription":"6 p.","startPage":"313","endPage":"318","costCenters":[],"links":[{"id":386310,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/thumbnails/outside_thumb.jpg"}],"country":"United States","state":"Nevada","county":"Nye County","geographicExtents":"{\n \"type\": \"FeatureCollection\",\n \"features\": [\n {\n \"type\": \"Feature\",\n \"properties\": {},\n \"geometry\": {\n \"type\": \"Polygon\",\n \"coordinates\": [\n [\n [\n -118.80615234374999,\n 39.46164364205549\n ],\n [\n -119.94873046875,\n 39.00211029922515\n ],\n [\n -116.5869140625,\n 36.500805317604794\n ],\n [\n -116.74072265625,\n 36.958671131530316\n ],\n [\n -117.26806640625,\n 38.07404145941957\n ],\n [\n -116.42211914062499,\n 38.151837403006766\n ],\n [\n -115.26855468749999,\n 38.79690830348427\n ],\n [\n -114.884033203125,\n 39.2492708462234\n ],\n [\n -114.9609375,\n 39.410733055084954\n ],\n [\n -115.93872070312499,\n 39.614152077002664\n ],\n [\n -117.44384765625,\n 39.64799732373418\n ],\n [\n -118.80615234374999,\n 39.46164364205549\n ]\n ]\n ]\n }\n }\n ]\n}","volume":"77","issue":"3","noUsgsAuthors":false,"publicationStatus":"PW","contributors":{"authors":[{"text":"Luft, S. J.","contributorId":95127,"corporation":false,"usgs":true,"family":"Luft","given":"S.","email":"","middleInitial":"J.","affiliations":[],"preferred":false,"id":817189,"contributorType":{"id":1,"text":"Authors"},"rank":1}]}} ,{"id":70222226,"text":"70222226 - 1966 - Tuscarora fault, an Acadian(?) bedding-plane fault in central Appalachian Valley and Ridge Province","interactions":[],"lastModifiedDate":"2021-07-22T13:32:42.822197","indexId":"70222226","displayToPublicDate":"1966-02-01T12:35:47","publicationYear":"1966","noYear":false,"publicationType":{"id":2,"text":"Article"},"publicationSubtype":{"id":10,"text":"Journal Article"},"seriesTitle":{"id":605,"text":"AAPG Bulletin","printIssn":"0149-1423","active":true,"publicationSubtype":{"id":10}},"title":"Tuscarora fault, an Acadian(?) bedding-plane fault in central Appalachian Valley and Ridge Province","docAbstract":"No abstract available.
","language":"English","publisher":"American Association of Petroleum Geologists","doi":"10.1306/5D25B495-16C1-11D7-8645000102C1865D","usgsCitation":"Pierce, K.L., and Armstrong, R.L., 1966, Tuscarora fault, an Acadian(?) bedding-plane fault in central Appalachian Valley and Ridge Province: AAPG Bulletin, v. 50, no. 2, p. 385-390, https://doi.org/10.1306/5D25B495-16C1-11D7-8645000102C1865D.","productDescription":"6 p.","startPage":"385","endPage":"390","costCenters":[],"links":[{"id":387339,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/thumbnails/outside_thumb.jpg"}],"country":"United States","state":"Pennsylvania","otherGeospatial":"Central Appalachian Valley","geographicExtents":"{\n \"type\": \"FeatureCollection\",\n \"features\": [\n {\n \"type\": \"Feature\",\n \"properties\": {},\n \"geometry\": {\n \"type\": \"Polygon\",\n \"coordinates\": [\n [\n [\n -79.013671875,\n 39.7240885773337\n ],\n [\n -77.49755859375,\n 39.7240885773337\n ],\n [\n -77.49755859375,\n 40.39676430557203\n ],\n [\n -79.013671875,\n 40.39676430557203\n ],\n [\n -79.013671875,\n 39.7240885773337\n ]\n ]\n ]\n }\n }\n ]\n}","volume":"50","issue":"2","noUsgsAuthors":false,"publicationStatus":"PW","contributors":{"authors":[{"text":"Pierce, Kenneth L. kpierce@usgs.gov","contributorId":1609,"corporation":false,"usgs":true,"family":"Pierce","given":"Kenneth","email":"kpierce@usgs.gov","middleInitial":"L.","affiliations":[{"id":481,"text":"Northern Rocky Mountain Science Center","active":true,"usgs":true},{"id":318,"text":"Geosciences and Environmental Change Science Center","active":true,"usgs":true},{"id":547,"text":"Rocky Mountain Geographic Science Center","active":true,"usgs":true}],"preferred":true,"id":819649,"contributorType":{"id":1,"text":"Authors"},"rank":1},{"text":"Armstrong, Richard L.","contributorId":58701,"corporation":false,"usgs":true,"family":"Armstrong","given":"Richard","email":"","middleInitial":"L.","affiliations":[],"preferred":false,"id":819650,"contributorType":{"id":1,"text":"Authors"},"rank":2}]}} ,{"id":70207930,"text":"70207930 - 1966 - Gravity slide origin of rift zones of some Hawaiian volcanoes","interactions":[],"lastModifiedDate":"2020-01-20T13:36:19","indexId":"70207930","displayToPublicDate":"1966-01-20T13:32:59","publicationYear":"1966","noYear":false,"publicationType":{"id":2,"text":"Article"},"publicationSubtype":{"id":10,"text":"Journal Article"},"seriesTitle":{"id":1093,"text":"Bulletin Volcanologique","active":true,"publicationSubtype":{"id":10}},"title":"Gravity slide origin of rift zones of some Hawaiian volcanoes","docAbstract":"The east-trending east rift zone of Kilauea volcano on the island of Hawaii is 50 km long and up to 3 km wide. It consists of three elements arranged roughly in three belts from north to south: 1) eruptive fissures, cracks, faults, and narrow grabens, 2) cinder cones (produced by eruptions more localised than the fissure eruptions), and 3) pit craters. Eruptive vents, either fissure or cone, do not occur south of pit craters; vents occur on the floor of some pit craters but are conlined to the north half. Most earthquakes near the rift zone are shallow; they are abundant south of the rift zone but rare north of it.
Precise levelling over a 6-year period shows elevation changes of up to 1 metre. Profiles of elevation change across the rift zone are asymmetrically steep on the north side. Precise triangulation shows that points south of the rift have been moving southward at right angles to the rift zone at rates of as much as 10 cm per year. During the major earthquake of 1868, the south coast of the island subsided as much as 2 metres, and abundant evidence indicates other recent subsidence of the south coast.
The above facts suggest that the rift zone dips south and that it bounds a large segment of the volcano which is sliding down the steep southern flank. Tensional cracks at the head of this slide tap the shallow central reservoir of the volcano at a depth of a few kilometres. The resulting dikes may feed eruptive fissures in the tensional zone at the head (northernmost part) of the slide, or they may pierce the hanging wall of the south-dipping rift zone through more confined conduits and feed the cinder cones. Likewise, shallow collapse into the rift zone on the north produces narrow grabens, whereas deeper collapse farther south (perhaps aided by magma stoping upward) produces circular pit craters.
Submarine topography south of Kilauea caldera indicates a submarine landslide on the south slope of the volcano. The landslide tongue is more than 25 kilometres long and is bounded upslope by a concave escarpment. On land, the northern rim of this escarpment is formed by a series of faults down-dropped on the south, called the Hilina fault system. Dredge hauls from a 300-metre hill on the crest of the landslide tongue at a water depth of 800 metres consists of angular fragments of fresh, glassy, tholeiitic basalt. The high vesicularity of this basalt suggests that it was erupted at a water depth several hundred metres less than that at which it was collected. Presumably, landsliding has carried the lava downward into deeper water.
","language":"English","publisher":"Springer Nature","doi":"10.1007/BF02597189","usgsCitation":"Moore, J.G., 1966, Gravity slide origin of rift zones of some Hawaiian volcanoes: Bulletin Volcanologique, v. 29, p. 719-720, https://doi.org/10.1007/BF02597189.","productDescription":"2 p.","startPage":"719","endPage":"720","costCenters":[{"id":617,"text":"Volcano Science Center","active":true,"usgs":true}],"links":[{"id":371382,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/thumbnails/outside_thumb.jpg"}],"volume":"29","noUsgsAuthors":false,"publicationStatus":"PW","contributors":{"authors":[{"text":"Moore, James G. 0000-0002-7543-2401 jmoore@usgs.gov","orcid":"https://orcid.org/0000-0002-7543-2401","contributorId":2892,"corporation":false,"usgs":true,"family":"Moore","given":"James","email":"jmoore@usgs.gov","middleInitial":"G.","affiliations":[{"id":114,"text":"Alaska Science Center","active":true,"usgs":true},{"id":617,"text":"Volcano Science Center","active":true,"usgs":true}],"preferred":true,"id":779797,"contributorType":{"id":1,"text":"Authors"},"rank":1}]}} ,{"id":34360,"text":"34360 - 1966 - Hydrologic inventory of the Lompoc subarea, Santa Ynez River Basin, Santa Barbara County, California, 1957-62","interactions":[],"lastModifiedDate":"2014-07-11T13:59:00","indexId":"34360","displayToPublicDate":"1966-01-10T13:52:38","publicationYear":"1966","noYear":false,"publicationType":{"id":18,"text":"Report"},"publicationSubtype":{"id":6,"text":"USGS Unnumbered Series"},"seriesTitle":{"id":375,"text":"Open-File Report","active":false,"publicationSubtype":{"id":6}},"title":"Hydrologic inventory of the Lompoc subarea, Santa Ynez River Basin, Santa Barbara County, California, 1957-62","docAbstract":"No abstract available.","language":"English","publisher":"U.S. Geological Survey","publisherLocation":"Sacramento, CA","doi":"10.3133/34360","collaboration":"Prepared in cooperation with the Santa Barbara County Water Agency.","usgsCitation":"Evenson, R.E., and Worts, G., 1966, Hydrologic inventory of the Lompoc subarea, Santa Ynez River Basin, Santa Barbara County, California, 1957-62: Open-File Report, iv, 27 p., https://doi.org/10.3133/34360.","productDescription":"iv, 27 p.","numberOfPages":"31","costCenters":[],"links":[{"id":289799,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/thumbnails/usgs_thumb.jpg"}],"country":"United States","state":"California","city":"Santa Barbara","otherGeospatial":"Santa Ynez","geographicExtents":"{ \"type\": \"FeatureCollection\", \"features\": [ { \"type\": \"Feature\", \"properties\": {}, \"geometry\": { \"type\": \"Polygon\", \"coordinates\": [ [ [ -120.136723,34.581332 ], [ -120.136723,34.635821 ], [ -120.055117,34.635821 ], [ -120.055117,34.581332 ], [ -120.136723,34.581332 ] ] ] } } ] }","noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"53c0ec4ae4b065ccca5fe3e2","contributors":{"authors":[{"text":"Evenson, Robert Edward","contributorId":81809,"corporation":false,"usgs":true,"family":"Evenson","given":"Robert","email":"","middleInitial":"Edward","affiliations":[],"preferred":false,"id":212835,"contributorType":{"id":1,"text":"Authors"},"rank":1},{"text":"Worts, George Frank","contributorId":100830,"corporation":false,"usgs":true,"family":"Worts","given":"George Frank","affiliations":[],"preferred":false,"id":212836,"contributorType":{"id":1,"text":"Authors"},"rank":2}]}} ,{"id":5220434,"text":"5220434 - 1966 - Fall food habits of wood ducks from Lake Marion, South Carolina","interactions":[],"lastModifiedDate":"2025-02-12T15:30:27.681855","indexId":"5220434","displayToPublicDate":"1966-01-03T00:00:00","publicationYear":"1966","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":"Fall food habits of wood ducks from Lake Marion, South Carolina","docAbstract":"A total of 108 stomachs of wood ducks (Aix sponsa) collected from hunters on the upper end of Lake Marion, South Carolina, between November 29 and December 6, 1961, were examined for information on food habits. Six plants made up over 98 percent of the total volume. Five were tree fruits: water and pin oak (Quercus nigra and Q. palustris), baldcypress (Taxodium distichum), sweetgum (Liquidambar styraciflua), and water hickory (Carya aquatica). The sixth important food was corn (Zea mays). In areas being managed for wood ducks and timber, therefore, these tree species should not be removed.
","language":"English","publisher":"Wiley","doi":"10.2307/3797903","usgsCitation":"McGilvrey, F.B., 1966, Fall food habits of wood ducks from Lake Marion, South Carolina: Journal of Wildlife Management, v. 30, no. 1, p. 193-195, https://doi.org/10.2307/3797903.","productDescription":"3 p.","startPage":"193","endPage":"195","costCenters":[{"id":531,"text":"Patuxent Wildlife Research Center","active":true,"usgs":true}],"links":[{"id":193430,"rank":1,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/thumbnails/outside_thumb.jpg"}],"country":"United States","state":"South Carolina","otherGeospatial":"Lake Marion","geographicExtents":"{\n \"type\": \"FeatureCollection\",\n \"features\": [\n {\n \"type\": \"Feature\",\n \"properties\": {},\n \"geometry\": {\n \"coordinates\": [\n [\n [\n -80.60257628664397,\n 33.698146245578016\n ],\n [\n -80.60257628664397,\n 33.35808164366274\n ],\n [\n -80.09009414701697,\n 33.35808164366274\n ],\n [\n -80.09009414701697,\n 33.698146245578016\n ],\n [\n -80.60257628664397,\n 33.698146245578016\n ]\n ]\n ],\n \"type\": \"Polygon\"\n }\n }\n ]\n}","volume":"30","issue":"1","noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"4f4e49ffe4b07f02db5f77e8","contributors":{"authors":[{"text":"McGilvrey, Frank B.","contributorId":104545,"corporation":false,"usgs":true,"family":"McGilvrey","given":"Frank","email":"","middleInitial":"B.","affiliations":[],"preferred":false,"id":331806,"contributorType":{"id":1,"text":"Authors"},"rank":1}]}} ,{"id":5220441,"text":"5220441 - 1966 - Weather and pheasant populations in southwestern North Dakota","interactions":[],"lastModifiedDate":"2025-02-12T15:39:30.196628","indexId":"5220441","displayToPublicDate":"1966-01-03T00:00:00","publicationYear":"1966","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":"Weather and pheasant populations in southwestern North Dakota","docAbstract":"High productivity and survival of ring-necked pheasants (Phasianus colchicus) were correlated with high rainfall and cool temperatures in May and June during an 8-year period in southwestern North Dakota. These findings differed markedly from those of several earlier studies in the less arid midwestern United States where cool, wet weather in the spring generally affected pheasant populations adversely. General trends in the pheasant population could be explained on the basis of precipitation in May and June. The population was relatively high during the mid-1950's when wet and dry May and June periods occurred in alternate years but declined markedly after 2 consecutive years of spring and summer drought. The population remained at a static low during 1960 through 1963 when wet and dry spring and summer periods again occurred alternately.
","language":"English","publisher":"Wiley","doi":"10.2307/3797886","usgsCitation":"Martinson, R.K., and Grondahl, C., 1966, Weather and pheasant populations in southwestern North Dakota: Journal of Wildlife Management, v. 30, no. 1, p. 74-81, https://doi.org/10.2307/3797886.","productDescription":"8 p.","startPage":"74","endPage":"81","costCenters":[{"id":531,"text":"Patuxent Wildlife Research Center","active":true,"usgs":true}],"links":[{"id":197854,"rank":1,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/thumbnails/outside_thumb.jpg"}],"country":"United States","state":"North Dakota","otherGeospatial":"southwestern North Dakota","geographicExtents":"{\n \"type\": \"FeatureCollection\",\n \"features\": [\n {\n \"type\": \"Feature\",\n \"properties\": {},\n \"geometry\": {\n \"coordinates\": [\n [\n [\n -103.93222080910647,\n 47.86972251795555\n ],\n [\n -103.93222080910647,\n 46.90542647605757\n ],\n [\n -103.93222080910647,\n 45.94113043415959\n ],\n [\n -101.61946546687363,\n 45.94113043415959\n ],\n [\n -101.9447433938835,\n 47.43516434419189\n ],\n [\n -102.92021424904443,\n 47.90599825882154\n ],\n [\n -103.93222080910647,\n 47.86972251795555\n ]\n ]\n ],\n \"type\": \"Polygon\"\n }\n }\n ]\n}","volume":"30","issue":"1","noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"4f4e49f7e4b07f02db5f23a5","contributors":{"authors":[{"text":"Martinson, R. K.","contributorId":106983,"corporation":false,"usgs":true,"family":"Martinson","given":"R.","middleInitial":"K.","affiliations":[],"preferred":false,"id":331819,"contributorType":{"id":1,"text":"Authors"},"rank":1},{"text":"Grondahl, C.R.","contributorId":62710,"corporation":false,"usgs":true,"family":"Grondahl","given":"C.R.","email":"","affiliations":[],"preferred":false,"id":331818,"contributorType":{"id":1,"text":"Authors"},"rank":2}]}} ,{"id":70047729,"text":"70047729 - 1966 - Soviet books and publications on hydrology (continental) and hydrogeology: titles and some notes on obtaining Soviet monographs","interactions":[],"lastModifiedDate":"2013-12-17T10:36:24","indexId":"70047729","displayToPublicDate":"1966-01-01T16:32:00","publicationYear":"1966","noYear":false,"publicationType":{"id":18,"text":"Report"},"publicationSubtype":{"id":6,"text":"USGS Unnumbered Series"},"title":"Soviet books and publications on hydrology (continental) and hydrogeology: titles and some notes on obtaining Soviet monographs","docAbstract":"A common method of publication for Soviet scientists, which partly supplants periodicals, is the publication of a collection of articles on a general area of research, frequently by members of a given institution. An extensive sampling of world geologic literature for 1961 (Hawkes, 1966) showed that 33 percent of Soviet titles appeared in periodicals whereas 55 percent of North American and 70 percent of Western European literature appeared in this form.
\nThe Soviet predilection for symposia and collections of papers makes searching for information on a given subject more difficult for Westerners because the monographs in question are often not included in exchange agreements (except informal personal ones) with Western libraries and institutions, because they may be primed in small editions, and because such publications frequently escape the notice of Western abstract journals.
\nUnless one is fortunate enough to have many personal contacts in the Soviet Union, there seems to be little alternative to at least a rudimentary knowledge of Russian in order to stay abreast of work published as monographs and in collections.
","largerWorkType":{"id":18,"text":"Report"},"largerWorkTitle":"Water Resources Division Bulletin","largerWorkSubtype":{"id":6,"text":"USGS Unnumbered Series"},"language":"English","publisher":"U.S. Geological Survey","doi":"10.3133/70047729","usgsCitation":"Manheim, F., 1966, Soviet books and publications on hydrology (continental) and hydrogeology: titles and some notes on obtaining Soviet monographs, 4 p., https://doi.org/10.3133/70047729.","productDescription":"4 p.","startPage":"22","endPage":"25","costCenters":[],"links":[{"id":276871,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/unnumbered/70047729/report-thumb.jpg"},{"id":279945,"type":{"id":11,"text":"Document"},"url":"https://pubs.usgs.gov/unnumbered/70047729/report.pdf"}],"country":"Armenia;Azerbaijan;Belarus;Estonia;Georgia;Kazakhstan;Kyrgyzstan;Latvia;Lithuania;Moldova;Russia;Tajikistan;Turkmenistan","otherGeospatial":"Union Of Soviet Socialist Republics","geographicExtents":"{ \"type\": \"FeatureCollection\", \"features\": [ { \"type\": \"Feature\", \"properties\": {}, \"geometry\": { \"type\": \"Polygon\", \"coordinates\": [ [ [ 23.0,35.5 ], [ 23.0,77.7 ], [ 179.9,77.7 ], [ 179.9,35.5 ], [ 23.0,35.5 ] ] ] } } ] }","noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"5215e164e4b02034073ad416","contributors":{"authors":[{"text":"Manheim, Frank T. 0000-0003-4005-4524","orcid":"https://orcid.org/0000-0003-4005-4524","contributorId":45294,"corporation":false,"usgs":true,"family":"Manheim","given":"Frank T.","affiliations":[{"id":678,"text":"Woods Hole Coastal and Marine Science Center","active":true,"usgs":true}],"preferred":false,"id":482836,"contributorType":{"id":1,"text":"Authors"},"rank":1}]}} ,{"id":25182,"text":"25182 - 1966 - Mineral production, royalty income, and related statistics on oil, gas, and other leasable minerals, Federal and Indian lands","interactions":[],"lastModifiedDate":"2014-07-14T16:28:52","indexId":"25182","displayToPublicDate":"1966-01-01T16:28:07","publicationYear":"1966","noYear":false,"publicationType":{"id":18,"text":"Report"},"publicationSubtype":{"id":6,"text":"USGS Unnumbered Series"},"title":"Mineral production, royalty income, and related statistics on oil, gas, and other leasable minerals, Federal and Indian lands","docAbstract":"No abstract available.","language":"English","publisher":"U.S. Dept. of Interior","publisherLocation":"Washington, D.C.","doi":"10.3133/25182","issn":"0271-1656","usgsCitation":"Water Resources Division, U.S. Geological Survey, 1966, Mineral production, royalty income, and related statistics on oil, gas, and other leasable minerals, Federal and Indian lands, v, https://doi.org/10.3133/25182.","productDescription":"v","numberOfPages":"5","costCenters":[],"links":[{"id":290006,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/thumbnails/usgs_thumb.jpg"}],"noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"53c4fc3be4b0b58d96eeb5cf","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":529198,"contributorType":{"id":1,"text":"Authors"},"rank":1}]}} ,{"id":70263595,"text":"70263595 - 1966 - Test well sites and preliminary evaluation of ground-water potential in Tortola, British Virgin Islands","interactions":[],"lastModifiedDate":"2025-02-14T21:16:24.403461","indexId":"70263595","displayToPublicDate":"1966-01-01T16:16:03","publicationYear":"1966","noYear":false,"publicationType":{"id":18,"text":"Report"},"publicationSubtype":{"id":6,"text":"USGS Unnumbered Series"},"title":"Test well sites and preliminary evaluation of ground-water potential in Tortola, British Virgin Islands","docAbstract":"Moderate supplies of potable ground water are believed to be available in the Roadtown and Paraquita Bay areas, and small, possibly brackish supplies in the Long Look and West End areas of Tortola. Two water bearing units of the same hydrologic system have the potential of yielding water to wells: 1) alluvial deposits, possibly as thick as 60 feet and locally containing beds and lenses of gravel 1 to 5 feet thick; and 2) fractured and jointed bedrock, especially where it is overlain by alluvium.
The most productive ground-water areas are expected to be the lower reaches of the larger valleys. Here the alluvial deposits are thickest and the valleys often follow the trace of fault or fracture systems in the bedrock. A potential yield of 195,000 gpd (U.S. gallons per day) is estimated to be available in the Road Bay area, 55,000 gpd in the Long Look area, and 8,000 gpd in the West End area.
Sites are suggested for test and monitoring wells in the lower courses of six of the valleys on the south coast.
","language":"English","publisher":"U.S. Geological Survey","doi":"10.3133/70263595","collaboration":"Work Done in Cooperation with the Government of the Virgin Islands, Ralph M. Paiewonsky, Governor","usgsCitation":"Jordan, D., 1966, Test well sites and preliminary evaluation of ground-water potential in Tortola, British Virgin Islands, 35 p., https://doi.org/10.3133/70263595.","productDescription":"35 p.","costCenters":[],"links":[{"id":482116,"rank":2,"type":{"id":11,"text":"Document"},"url":"https://pubs.usgs.gov/unnumbered/70263595/report.pdf","linkFileType":{"id":1,"text":"pdf"}},{"id":482115,"rank":1,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/unnumbered/70263595/report-thumb.jpg"}],"country":"United States","state":"Virgin Islands","otherGeospatial":"Tortola","geographicExtents":"{\n \"type\": \"FeatureCollection\",\n \"features\": [\n {\n \"type\": \"Feature\",\n \"properties\": {},\n \"geometry\": {\n \"coordinates\": [\n [\n [\n -64.51309561955642,\n 18.51802619929059\n ],\n [\n -64.74978261433117,\n 18.51802619929059\n ],\n [\n -64.74978261433117,\n 18.336353177581245\n ],\n [\n -64.51309561955642,\n 18.336353177581245\n ],\n [\n -64.51309561955642,\n 18.51802619929059\n ]\n ]\n ],\n \"type\": \"Polygon\"\n }\n }\n ]\n}","noUsgsAuthors":false,"publicationStatus":"PW","contributors":{"authors":[{"text":"Jordan, Donald G.","contributorId":9519,"corporation":false,"usgs":true,"family":"Jordan","given":"Donald G.","affiliations":[],"preferred":false,"id":927458,"contributorType":{"id":1,"text":"Authors"},"rank":1}]}} ]}