Spine arrangements on silicified specimens of Waagenoconcha abichi (Waagen) from the Khisor Range of West Pakistan suggest that the juvenile shell attached itself to a foreign object, and that the adult shell lay on its ventral valve in the substrate, anchored and stabilized by a dense corona of long slender spines around the ventral visceral disc.
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","language":"English","publisher":"American Association for the Advancement of Science","doi":"10.1126/science.152.3721.544","issn":"00368075","usgsCitation":"Hess, H., and Ladd, H.S., 1966, Mohole: Preliminary drilling: Science, v. 152, no. 3721, p. 544-545, https://doi.org/10.1126/science.152.3721.544.","productDescription":"2 p.","startPage":"544","endPage":"545","costCenters":[],"links":[{"id":219261,"rank":1,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/thumbnails/outside_thumb.jpg"}],"volume":"152","issue":"3721","noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"505a5ce6e4b0c8380cd70008","contributors":{"authors":[{"text":"Hess, H.H.","contributorId":11754,"corporation":false,"usgs":true,"family":"Hess","given":"H.H.","email":"","affiliations":[],"preferred":false,"id":359347,"contributorType":{"id":1,"text":"Authors"},"rank":1},{"text":"Ladd, H. S.","contributorId":95537,"corporation":false,"usgs":true,"family":"Ladd","given":"H.","email":"","middleInitial":"S.","affiliations":[],"preferred":false,"id":359348,"contributorType":{"id":1,"text":"Authors"},"rank":2}]}} ,{"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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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":70171413,"text":"70171413 - 1966 - Behavior and transport of radionuclides in the Columbia River between Hanford and Vancouver, Washington","interactions":[],"lastModifiedDate":"2016-05-31T11:04:54","indexId":"70171413","displayToPublicDate":"1966-04-01T00:00:00","publicationYear":"1966","noYear":false,"publicationType":{"id":2,"text":"Article"},"publicationSubtype":{"id":10,"text":"Journal Article"},"seriesTitle":{"id":2620,"text":"Limnology and Oceanography","active":true,"publicationSubtype":{"id":10}},"title":"Behavior and transport of radionuclides in the Columbia River between Hanford and Vancouver, Washington","docAbstract":"No abstract available.
","language":"English","publisher":"ASLO","doi":"10.4319/lo.1966.11.2.0235","usgsCitation":"Perkins, R., Nelson, J., and Haushild, W., 1966, Behavior and transport of radionuclides in the Columbia River between Hanford and Vancouver, Washington: Limnology and Oceanography, v. 11, no. 2, p. 235-248, https://doi.org/10.4319/lo.1966.11.2.0235.","productDescription":"14 p.","startPage":"235","endPage":"248","onlineOnly":"N","additionalOnlineFiles":"N","costCenters":[{"id":622,"text":"Washington Water Science Center","active":true,"usgs":true}],"links":[{"id":321900,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/thumbnails/outside_thumb.jpg"}],"volume":"11","issue":"2","noUsgsAuthors":false,"publicationDate":"2003-12-22","publicationStatus":"PW","scienceBaseUri":"574eb5b4e4b0ee97d51a8395","contributors":{"authors":[{"text":"Perkins, R.W.","contributorId":77221,"corporation":false,"usgs":true,"family":"Perkins","given":"R.W.","email":"","affiliations":[],"preferred":false,"id":630917,"contributorType":{"id":1,"text":"Authors"},"rank":1},{"text":"Nelson, J.L.","contributorId":26320,"corporation":false,"usgs":true,"family":"Nelson","given":"J.L.","email":"","affiliations":[],"preferred":false,"id":630918,"contributorType":{"id":1,"text":"Authors"},"rank":2},{"text":"Haushild, W.L.","contributorId":48953,"corporation":false,"usgs":true,"family":"Haushild","given":"W.L.","affiliations":[],"preferred":false,"id":630919,"contributorType":{"id":1,"text":"Authors"},"rank":3}]}} ,{"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":70221263,"text":"70221263 - 1966 - Nomenclature in the machine age","interactions":[],"lastModifiedDate":"2021-06-08T18:30:18.222289","indexId":"70221263","displayToPublicDate":"1966-03-01T13:26:56","publicationYear":"1966","noYear":false,"publicationType":{"id":2,"text":"Article"},"publicationSubtype":{"id":10,"text":"Journal Article"},"seriesTitle":{"id":3511,"text":"Systematic Zoology","active":true,"publicationSubtype":{"id":10}},"title":"Nomenclature in the machine age","docAbstract":"No abstract available.
","language":"English","publisher":"Elsevier","doi":"10.2307/sysbio/15.1.88b","usgsCitation":"Yochelson, E.L., 1966, Nomenclature in the machine age: Systematic Zoology, v. 15, no. 1, p. 88-91, https://doi.org/10.2307/sysbio/15.1.88b.","productDescription":"4 p.","startPage":"88","endPage":"91","costCenters":[],"links":[{"id":386309,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/thumbnails/outside_thumb.jpg"}],"volume":"15","issue":"1","noUsgsAuthors":false,"publicationStatus":"PW","contributors":{"authors":[{"text":"Yochelson, E. L.","contributorId":50948,"corporation":false,"usgs":true,"family":"Yochelson","given":"E.","email":"","middleInitial":"L.","affiliations":[],"preferred":false,"id":817188,"contributorType":{"id":1,"text":"Authors"},"rank":1}]}} ,{"id":70010678,"text":"70010678 - 1966 - The 1965 eruption of Taal Volcano","interactions":[],"lastModifiedDate":"2026-02-10T17:35:37.349757","indexId":"70010678","displayToPublicDate":"1966-02-25T00:00:00","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":"The 1965 eruption of Taal Volcano","docAbstract":"Catastrophic explosions are caused by lake water entering a volcanic conduit.","language":"English","publisher":"American Association for the Advancement of Science","doi":"10.1126/science.151.3713.955","issn":"00368075","usgsCitation":"Moore, J., Nakamura, K., and Alcaraz, A., 1966, The 1965 eruption of Taal Volcano: Science, v. 151, no. 3713, p. 955-960, https://doi.org/10.1126/science.151.3713.955.","productDescription":"6 p.","startPage":"955","endPage":"960","costCenters":[],"links":[{"id":219467,"rank":1,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/thumbnails/outside_thumb.jpg"}],"country":"Philippines","city":"Luzon","otherGeospatial":"Taal Volcano","geographicExtents":"{\n \"type\": \"FeatureCollection\",\n \"features\": [\n {\n \"type\": \"Feature\",\n \"properties\": {},\n \"geometry\": {\n \"coordinates\": [\n [\n [\n 120.84548034568735,\n 14.125033242660678\n ],\n [\n 120.84548034568735,\n 13.840055850805584\n ],\n [\n 121.14872418766669,\n 13.840055850805584\n ],\n [\n 121.14872418766669,\n 14.125033242660678\n ],\n [\n 120.84548034568735,\n 14.125033242660678\n ]\n ]\n ],\n \"type\": \"Polygon\"\n }\n }\n ]\n}","volume":"151","issue":"3713","noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"505ba620e4b08c986b320ee8","contributors":{"authors":[{"text":"Moore, J.G.","contributorId":67496,"corporation":false,"usgs":true,"family":"Moore","given":"J.G.","email":"","affiliations":[],"preferred":false,"id":359410,"contributorType":{"id":1,"text":"Authors"},"rank":1},{"text":"Nakamura, K.","contributorId":78866,"corporation":false,"usgs":true,"family":"Nakamura","given":"K.","email":"","affiliations":[],"preferred":false,"id":359411,"contributorType":{"id":1,"text":"Authors"},"rank":2},{"text":"Alcaraz, A.","contributorId":58772,"corporation":false,"usgs":true,"family":"Alcaraz","given":"A.","email":"","affiliations":[],"preferred":false,"id":359409,"contributorType":{"id":1,"text":"Authors"},"rank":3}]}} ,{"id":1014078,"text":"1014078 - 1966 - Lymphocystis virus: Isolation and propagation in centrarchid fish cell lines","interactions":[],"lastModifiedDate":"2026-02-10T17:14:35.1122","indexId":"1014078","displayToPublicDate":"1966-02-25T00:00:00","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":"Lymphocystis virus: Isolation and propagation in centrarchid fish cell lines","docAbstract":"A virus from fish with lymphocystis disease was isolated in fish cell cultures. Eleven serial transfers were made and the pathognomonic lymphocystis cells were produced in vitro in each transfer. Fish inoculated with 6th- and 9th-passage material developed the disease, and virus was reisolated from them.
","language":"English","publisher":"American Association for the Advancement of Science","doi":"10.1126/science.151.3713.1004","usgsCitation":"Wolf, K., Gravell, M., and Malsberger, R., 1966, Lymphocystis virus: Isolation and propagation in centrarchid fish cell lines: Science, v. 151, no. 3713, p. 1004-1005, https://doi.org/10.1126/science.151.3713.1004.","productDescription":"2 p.","startPage":"1004","endPage":"1005","costCenters":[{"id":365,"text":"Leetown Science Center","active":true,"usgs":true}],"links":[{"id":129645,"rank":1,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/thumbnails/outside_thumb.jpg"}],"volume":"151","issue":"3713","noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"4f4e4a7fe4b07f02db648ab5","contributors":{"authors":[{"text":"Wolf, K.","contributorId":16344,"corporation":false,"usgs":true,"family":"Wolf","given":"K.","email":"","affiliations":[],"preferred":false,"id":319742,"contributorType":{"id":1,"text":"Authors"},"rank":1},{"text":"Gravell, M.","contributorId":47729,"corporation":false,"usgs":true,"family":"Gravell","given":"M.","email":"","affiliations":[],"preferred":false,"id":319743,"contributorType":{"id":1,"text":"Authors"},"rank":2},{"text":"Malsberger, R.G.","contributorId":60147,"corporation":false,"usgs":true,"family":"Malsberger","given":"R.G.","email":"","affiliations":[],"preferred":false,"id":319744,"contributorType":{"id":1,"text":"Authors"},"rank":3}]}} ,{"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":547,"text":"Rocky Mountain Geographic Science Center","active":true,"usgs":true},{"id":318,"text":"Geosciences and Environmental Change 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":70207933,"text":"70207933 - 1966 - The September 28–30, 1965 eruption of Taal Volcano, Philippines","interactions":[],"lastModifiedDate":"2020-01-20T13:54:25","indexId":"70207933","displayToPublicDate":"1966-01-20T13:49:54","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":"The September 28–30, 1965 eruption of Taal Volcano, Philippines","docAbstract":"A moderately violent phreatomagmatic explosive eruption of Taal Volcano, Philippines, occurred from 28 to 30 September, 1965. The main phreatic explosions, which were preceded by ejection of basaltic spatter, opened a new crater 1.5 km long and 0.3 km wide on the southwest side of Volcano Island in Lake Taal. The eruption covered an area of about 60 square kilometers with a blanket of ash more than 25 cm thick and killed approximately 200 persons.
The clouds that formed during the explosive eruption rose to heights of 15 to 20 km and deposited fine ash as far as 80 km west of the vent. At the base of the main explosion column, flat, turbulent clouds spread radially, with hurricane velocity, transporting ash, mud, lapilli and blocks. The horizontally moving, debris-laden clouds, sandblasted trees, coated the blast side of trees and houses with mud, and deposited coarse ejecta with dune-type bedding in a zone roughly 4 km in all directions from the explosion crater.
","language":"English","publisher":"Springer Nature","doi":"10.1007/BF02597143","usgsCitation":"Moore, J.G., Nakamura, K., and Alcaraz, A., 1966, The September 28–30, 1965 eruption of Taal Volcano, Philippines: Bulletin Volcanologique, v. 29, p. 75-76, https://doi.org/10.1007/BF02597143.","productDescription":"2 p.","startPage":"75","endPage":"76","costCenters":[{"id":617,"text":"Volcano Science Center","active":true,"usgs":true}],"links":[{"id":371385,"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":779805,"contributorType":{"id":1,"text":"Authors"},"rank":1},{"text":"Nakamura, K.","contributorId":78866,"corporation":false,"usgs":true,"family":"Nakamura","given":"K.","email":"","affiliations":[],"preferred":false,"id":779806,"contributorType":{"id":1,"text":"Authors"},"rank":2},{"text":"Alcaraz, A.","contributorId":58772,"corporation":false,"usgs":true,"family":"Alcaraz","given":"A.","email":"","affiliations":[],"preferred":false,"id":779807,"contributorType":{"id":1,"text":"Authors"},"rank":3}]}} ,{"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":70010627,"text":"70010627 - 1966 - Mica polytypes: Systematic description and identification","interactions":[],"lastModifiedDate":"2026-02-10T17:39:30.165809","indexId":"70010627","displayToPublicDate":"1966-01-14T00:00:00","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":"Mica polytypes: Systematic description and identification","docAbstract":"X-ray studies of mica specimens from a variety of geological localities show that biotite and certain lithium-rich mica samples are composed of a mixture of different polytypes. Many of the biotite structures are new complex polytypes not before reported. A new method of designating mica polytypes is proposed. Techniques are described for the systematic generation of all the possible layer-stacking sequences of mica polytypes and for the verification of the stacking sequences in newly discovered forms.","language":"English","publisher":"American Association for the Advancement of Science","doi":"10.1126/science.151.3707.191","issn":"00368075","usgsCitation":"Ross, M., Takeda, H., and Wones, D.R., 1966, Mica polytypes: Systematic description and identification: Science, v. 151, no. 3707, p. 191-193, https://doi.org/10.1126/science.151.3707.191.","productDescription":"3 p.","startPage":"191","endPage":"193","costCenters":[],"links":[{"id":219174,"rank":1,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/thumbnails/outside_thumb.jpg"}],"volume":"151","issue":"3707","noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"505a5631e4b0c8380cd6d3f6","contributors":{"authors":[{"text":"Ross, M.","contributorId":8026,"corporation":false,"usgs":true,"family":"Ross","given":"M.","email":"","affiliations":[],"preferred":false,"id":359290,"contributorType":{"id":1,"text":"Authors"},"rank":1},{"text":"Takeda, H.","contributorId":90462,"corporation":false,"usgs":true,"family":"Takeda","given":"H.","email":"","affiliations":[],"preferred":false,"id":359291,"contributorType":{"id":1,"text":"Authors"},"rank":2},{"text":"Wones, D. R.","contributorId":104079,"corporation":false,"usgs":true,"family":"Wones","given":"D.","email":"","middleInitial":"R.","affiliations":[],"preferred":false,"id":359292,"contributorType":{"id":1,"text":"Authors"},"rank":3}]}} ,{"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":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":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":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}]}} ]}