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The study was made by the U.S. Geological Survey in fiscal cooperation with the Connecticut Department of Environmental Protection. Collection sites for data used in the study are shown in plate A. A companion report interprets the ground-water, quality-of-water, and surfacewater data collected for the study (Connecticut Water Resources Bulletin No. 27, in parparation).\nThe Quinnipiac River basin~ as used in this report~ is a 360-square-mile\narea in south-central Connecticut drained principally by the Quinnipiac River\nand its tributaries and several smaller streams~ which drain directly to Long\nIsland Sound. (See front cover and plate A.) The study area includes all or\nparts of the following towns: Ansonia, Berlin, Bethany, Branford, Bristol,\nCheshire, Derby, Durham, East Haven, Farmington, Guilford, Hamden, Meriden,\nMiddlefield, Middletown, Milford, New Britain, New Haven, North Branford, North\nHaven, Orange, Plainville, Prospect, Southington, Wallingford, West Haven, Wolcott,\nand Woodbridge.\nData collected for this investigation from July 1969 to December 1971 were\nsupplemented by data collected during previous investigations. This report includes\nsome records of wells and test holes published in Connecticut Water\nResources Bulletin No. 5 and also includes some records used but not published\nin Connecticut Water Resources Bulletin No. 14.\nTable 5 contains old but previously unpublished analyses of water from wells\nin New Haven collected primarily from 1938 to 1949. Ownership of the sampled\nwells, as shown in table 1 and table 5, was determined at the time of the original\ninventory, and this information may now be outdated. Many of these wells\nhave been destroyed since they were last sampled and others, though still in\nexistence, are no longer in use.","language":"English","publisher":"Connecticut Department of Environmental Protection","collaboration":"Prepared by the U.S. Geological Survey in cooperation with the Connecticut Department of Environmental Protection","usgsCitation":"Mazzaferro, D.L., 1973, Hydrogeologic data for the Quinnipiac River basin, Connecticut: Connecticut Water Resources Bulletin 26, Report: 54 p.; 1 Plate: 33.36 x 54.39 inches.","productDescription":"Report: 54 p.; 1 Plate: 33.36 x 54.39 inches","numberOfPages":"58","additionalOnlineFiles":"Y","costCenters":[],"links":[{"id":258817,"rank":300,"type":{"id":11,"text":"Document"},"url":"https://pubs.usgs.gov/ctwrb/0026/report.pdf","size":"2919","linkFileType":{"id":1,"text":"pdf"}},{"id":258818,"rank":0,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/ctwrb/0026/report-thumb.jpg"},{"id":286038,"type":{"id":17,"text":"Plate"},"url":"https://pubs.usgs.gov/unnumbered/70038339/plate-a.pdf"}],"scale":"48000","country":"United States","state":"Connecticut","otherGeospatial":"Quinnipiac River Basin","geographicExtents":"{ \"type\": \"FeatureCollection\", \"features\": [ { \"type\": \"Feature\", \"properties\": {}, \"geometry\": { \"type\": \"Polygon\", \"coordinates\": [ [ [ -73.083333,41.166667 ], [ -73.083333,41.708333 ], [ -72.666667,41.708333 ], [ -72.666667,41.166667 ], [ -73.083333,41.166667 ] ] ] } } ] }","noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"505a33b1e4b0c8380cd5f1b9","contributors":{"authors":[{"text":"Mazzaferro, David L.","contributorId":89539,"corporation":false,"usgs":true,"family":"Mazzaferro","given":"David","email":"","middleInitial":"L.","affiliations":[],"preferred":false,"id":463905,"contributorType":{"id":1,"text":"Authors"},"rank":1}]}}
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,{"id":70006566,"text":"70006566 - 1973 - Versatile combustion-amalgamation technique for the photometric determination of mercury in fish and environmental samples","interactions":[],"lastModifiedDate":"2025-03-03T16:00:13.34117","indexId":"70006566","displayToPublicDate":"2012-01-01T00:00:00","publicationYear":"1973","noYear":false,"publicationType":{"id":2,"text":"Article"},"publicationSubtype":{"id":10,"text":"Journal Article"},"seriesTitle":{"id":2533,"text":"Journal of the Association of Official Analytical Chemists","active":true,"publicationSubtype":{"id":10}},"title":"Versatile combustion-amalgamation technique for the photometric determination of mercury in fish and environmental samples","docAbstract":"<p><span>Total mercury in a variety of substances is determined rapidly and precisely by direct sample combustion, collection of released mercury by amalgamation, and photometric measurement of mercury volatilized from the heated amalgam. Up to 0.2 g fish tissue is heated in a stream of O</span><sub>2</sub><span>&nbsp;(1.2 L/min) for 3.5 min in 1 tube of a 2-tube induction furnace. The released mercury vapor and combustion products are carried by the stream of O</span><sub>2</sub><span>&nbsp;through a series of traps (6% NaOH scrubber, water condenser, and Mg(ClO</span><sub>4</sub><span>)</span><sub>2</sub><span>&nbsp;drying tube) and the mercury is collected in a 10 mm diameter column of 24 gauge gold wire (8 g) cut into 3 mm lengths. The resulting amalgam is heated in the second tube of the induction furnace and the volatilized mercury is measured with a mercury vapor meter equipped with a recorder-integrator. Total analysis time is approximately 8 min/sample. The detection limit is less than 0.002&nbsp;</span><i>μ</i><span>g and the system is easily converted for use with other biological materials, water, and sediments.</span></p>","language":"English","publisher":"Oxford Academic","publisherLocation":"Gaithersburg, MD","doi":"10.1093/jaoac/56.4.1008","usgsCitation":"Willford, W.A., Hesselberg, R.J., and Bergman, H.L., 1973, Versatile combustion-amalgamation technique for the photometric determination of mercury in fish and environmental samples: Journal of the Association of Official Analytical Chemists, v. 56, no. 4, p. 1008-1014, https://doi.org/10.1093/jaoac/56.4.1008.","productDescription":"7 p.","startPage":"1008","endPage":"1014","numberOfPages":"6","costCenters":[{"id":324,"text":"Great Lakes Science Center","active":true,"usgs":true}],"links":[{"id":263343,"rank":1,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/thumbnails/outside_thumb.jpg"}],"volume":"56","issue":"4","noUsgsAuthors":false,"publicationDate":"2020-02-10","publicationStatus":"PW","scienceBaseUri":"50ae0609e4b03b26ec4d3840","contributors":{"authors":[{"text":"Willford, Wayne A.","contributorId":67446,"corporation":false,"usgs":true,"family":"Willford","given":"Wayne","email":"","middleInitial":"A.","affiliations":[],"preferred":false,"id":354776,"contributorType":{"id":1,"text":"Authors"},"rank":1},{"text":"Hesselberg, Robert J.","contributorId":36074,"corporation":false,"usgs":true,"family":"Hesselberg","given":"Robert","email":"","middleInitial":"J.","affiliations":[],"preferred":false,"id":354775,"contributorType":{"id":1,"text":"Authors"},"rank":2},{"text":"Bergman, Harold L.","contributorId":99099,"corporation":false,"usgs":true,"family":"Bergman","given":"Harold","email":"","middleInitial":"L.","affiliations":[],"preferred":false,"id":354777,"contributorType":{"id":1,"text":"Authors"},"rank":3}]}}
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,{"id":70040755,"text":"70040755 - 1973 - Time-of-travel study, Batten Kill from 0.6 mile east of Vermont-New York border to Clarks Mills, New York","interactions":[],"lastModifiedDate":"2017-09-13T18:25:16","indexId":"70040755","displayToPublicDate":"2012-01-01T00:00:00","publicationYear":"1973","noYear":false,"publicationType":{"id":18,"text":"Report"},"publicationSubtype":{"id":2,"text":"State or Local Government Series"},"seriesTitle":{"id":5495,"text":"New York State Department of Environmental Conservation Report of Investigations","active":true,"publicationSubtype":{"id":2}},"seriesNumber":"RI-12","title":"Time-of-travel study, Batten Kill from 0.6 mile east of Vermont-New York border to Clarks Mills, New York","language":"English","publisher":"New York State Department of Environmental Conservation","publisherLocation":"Albany, NY","usgsCitation":"Shindel, H., 1973, Time-of-travel study, Batten Kill from 0.6 mile east of Vermont-New York border to Clarks Mills, New York: New York State Department of Environmental Conservation Report of Investigations RI-12, 18 p.","productDescription":"18 p.","costCenters":[{"id":474,"text":"New York Water Science Center","active":true,"usgs":true}],"links":[{"id":263189,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/thumbnails/outside_thumb.jpg"}],"country":"United States","state":"New York","geographicExtents":"{ \"type\": \"FeatureCollection\", \"features\": [ { \"type\": \"Feature\", \"properties\": {}, \"geometry\": { \"type\": \"Polygon\", \"coordinates\": [ [ [ -79.76,40.48 ], [ -79.76,45.02 ], [ -71.86,45.02 ], [ -71.86,40.48 ], [ -79.76,40.48 ] ] ] } } ] }","noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"50a61d6fe4b0d446a665ca12","contributors":{"authors":[{"text":"Shindel, H.L.","contributorId":17652,"corporation":false,"usgs":true,"family":"Shindel","given":"H.L.","affiliations":[],"preferred":false,"id":468962,"contributorType":{"id":1,"text":"Authors"},"rank":1}]}}
,{"id":70040756,"text":"70040756 - 1973 - Floods in New York-1969","interactions":[],"lastModifiedDate":"2017-09-13T18:23:07","indexId":"70040756","displayToPublicDate":"2012-01-01T00:00:00","publicationYear":"1973","noYear":false,"publicationType":{"id":18,"text":"Report"},"publicationSubtype":{"id":2,"text":"State or Local Government Series"},"seriesTitle":{"id":5495,"text":"New York State Department of Environmental Conservation Report of Investigations","active":true,"publicationSubtype":{"id":2}},"seriesNumber":"RI-13","title":"Floods in New York-1969","language":"English","publisher":"New York State Department of Environmental Conservation","publisherLocation":"Albany, NY","usgsCitation":"Robison, F., 1973, Floods in New York-1969: New York State Department of Environmental Conservation Report of Investigations RI-13, 33 p.","productDescription":"33 p.","costCenters":[{"id":474,"text":"New York Water Science Center","active":true,"usgs":true}],"links":[{"id":263190,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/thumbnails/outside_thumb.jpg"}],"country":"United States","state":"New York","geographicExtents":"{ \"type\": \"FeatureCollection\", \"features\": [ { \"type\": \"Feature\", \"properties\": {}, \"geometry\": { \"type\": \"Polygon\", \"coordinates\": [ [ [ -79.76,40.48 ], [ -79.76,45.02 ], [ -71.86,45.02 ], [ -71.86,40.48 ], [ -79.76,40.48 ] ] ] } } ] }","noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"50a61d15e4b0d446a665c9d6","contributors":{"authors":[{"text":"Robison, F.L.","contributorId":41889,"corporation":false,"usgs":true,"family":"Robison","given":"F.L.","email":"","affiliations":[],"preferred":false,"id":468963,"contributorType":{"id":1,"text":"Authors"},"rank":1}]}}
,{"id":70001349,"text":"70001349 - 1973 - 18-Tungstotetracobalto(II)diphosphate and related anions: A novel structural class of heteropolyanions","interactions":[],"lastModifiedDate":"2012-03-08T17:16:35","indexId":"70001349","displayToPublicDate":"2010-09-28T23:09:33","publicationYear":"1973","noYear":false,"publicationType":{"id":2,"text":"Article"},"publicationSubtype":{"id":10,"text":"Journal Article"},"seriesTitle":{"id":2536,"text":"Journal of the Chemical Society, Chemical Communications","active":true,"publicationSubtype":{"id":10}},"title":"18-Tungstotetracobalto(II)diphosphate and related anions: A novel structural class of heteropolyanions","docAbstract":"The P2Co4(H2O)2W 18O6810- anion contains four edge-linked coIIO6 octahedra with coplanar cobalt atoms, in addition to two fragments of the Keggin structure.","largerWorkType":{"id":2,"text":"Article"},"largerWorkTitle":"Journal of the Chemical Society, Chemical Communications","largerWorkSubtype":{"id":10,"text":"Journal Article"},"language":"English","doi":"10.1039/C39730000139","issn":"00224936","usgsCitation":"Weakley, T., Evans, H.T., Showell, J., Tourne, G., and Tourne, C., 1973, 18-Tungstotetracobalto(II)diphosphate and related anions: A novel structural class of heteropolyanions: Journal of the Chemical Society, Chemical Communications, no. 4, p. 139-140, https://doi.org/10.1039/C39730000139.","startPage":"139","endPage":"140","costCenters":[],"links":[{"id":203315,"rank":0,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/thumbnails/outside_thumb.jpg"},{"id":19096,"rank":9999,"type":{"id":10,"text":"Digital Object Identifier"},"url":"https://dx.doi.org/10.1039/C39730000139"}],"issue":"4","noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"4f4e4acce4b07f02db67e505","contributors":{"authors":[{"text":"Weakley, T.J.R.","contributorId":107403,"corporation":false,"usgs":true,"family":"Weakley","given":"T.J.R.","email":"","affiliations":[],"preferred":false,"id":346735,"contributorType":{"id":1,"text":"Authors"},"rank":1},{"text":"Evans, H. T. Jr.","contributorId":41859,"corporation":false,"usgs":true,"family":"Evans","given":"H.","suffix":"Jr.","email":"","middleInitial":"T.","affiliations":[],"preferred":false,"id":346731,"contributorType":{"id":1,"text":"Authors"},"rank":2},{"text":"Showell, J.S.","contributorId":61136,"corporation":false,"usgs":true,"family":"Showell","given":"J.S.","affiliations":[],"preferred":false,"id":346732,"contributorType":{"id":1,"text":"Authors"},"rank":3},{"text":"Tourne, G.F.","contributorId":105833,"corporation":false,"usgs":true,"family":"Tourne","given":"G.F.","email":"","affiliations":[],"preferred":false,"id":346734,"contributorType":{"id":1,"text":"Authors"},"rank":4},{"text":"Tourne, C.M.","contributorId":77276,"corporation":false,"usgs":true,"family":"Tourne","given":"C.M.","email":"","affiliations":[],"preferred":false,"id":346733,"contributorType":{"id":1,"text":"Authors"},"rank":5}]}}
,{"id":70001345,"text":"70001345 - 1973 - Recurrence of seismic migrations along the central California segment of the San Andreas fault system","interactions":[],"lastModifiedDate":"2020-12-23T21:57:35.031797","indexId":"70001345","displayToPublicDate":"2010-09-28T23:09:33","publicationYear":"1973","noYear":false,"publicationType":{"id":2,"text":"Article"},"publicationSubtype":{"id":10,"text":"Journal Article"},"seriesTitle":{"id":2840,"text":"Nature","active":true,"publicationSubtype":{"id":10}},"title":"Recurrence of seismic migrations along the central California segment of the San Andreas fault system","docAbstract":"<div id=\"Abs1-section\" class=\"c-article-section\"><div id=\"Abs1-content\" class=\"c-article-section__content\"><p>VERIFICATIONS of tectonic concepts<sup>1</sup><span>&nbsp;</span>concerning seafloor spreading are emerging in a manner that has direct bearing on earthquake prediction. Although the gross pattern of worldwide seismicity contributed to the formulation of the plate tectonic hypothesis, it is the space-time characteristics of this seismicity that may contribute more toward understanding the kinematics and dynamics of the driving mechanism long speculated to originate in the mantle. If the lithosphere is composed of plates that move essentially as rigid bodies, then there should be seismic edge effects associated with this movement. It is these interplate effects, especially seismic migration patterns, that we discuss here. The unidirectional propagation at constant velocity (80 km yr<sup>−1</sup><span>&nbsp;</span>east to west) for earthquakes (<i>M</i>≥7.2) on the Antblian fault for the period 1939 to 1956 (ref. 2) is one of the earliest observations of such a phenomenon. Similar studies<sup>3,4</sup><span>&nbsp;</span>of the Alaska Aleutian seismic zone and certain regions of the west coast of South America suggest unidirectional and recurring migrations of earthquakes (<i>M</i>≥7.7) occur in these areas. Between these two regions along the great transform faults of the west coast of North America, there is some evidence<sup>5</sup><span>&nbsp;</span>for unidirectional, constant velocity and recurrent migration of great earthquakes. The small population of earthquakes (M&gt;7.2) in Savage's investigation<sup>5</sup><span>&nbsp;</span>indicates a large spatial gap along the San Andreas system in central California from 1830 to 1970. Previous work on the seismicity of this gap in central California indicates that the recurrence curves remain relatively constant, independent of large earthquakes, for periods up to a century<sup>6</sup>. Recurrence intervals for earthquakes along the San Andreas Fault have been calculated empirically by Wallace<sup>7</sup><span>&nbsp;</span>on the basis of geological evidence, surface measurements and assumptions restricted to the surficial seismic layer. Here we examine the evidence for recurrence of seismic migrations along the San Andreas fault system of central California for earthquakes of magnitude<span>&nbsp;</span><i>M</i>≥5.</p></div></div>","language":"English","publisher":"Nature","doi":"10.1038/244213a0","issn":"00280836","usgsCitation":"Wood, M., and Allen, S., 1973, Recurrence of seismic migrations along the central California segment of the San Andreas fault system: Nature, v. 244, no. 5413, p. 213-215, https://doi.org/10.1038/244213a0.","productDescription":"3 p.","startPage":"213","endPage":"215","costCenters":[],"links":[{"id":203665,"rank":0,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/thumbnails/outside_thumb.jpg"}],"country":"United States","state":"California","otherGeospatial":"San Andreas fault","geographicExtents":"{\n  \"type\": \"FeatureCollection\",\n  \"features\": [\n    {\n      \"type\": \"Feature\",\n      \"properties\": {},\n      \"geometry\": {\n        \"type\": \"Polygon\",\n        \"coordinates\": [\n          [\n            [\n              -120.84960937499999,\n              34.288991865037524\n            ],\n            [\n              -118.01513671875,\n              33.8339199536547\n            ],\n            [\n              -114.82910156249999,\n              34.939985151560435\n            ],\n            [\n              -116.45507812500001,\n              37.64903402157866\n            ],\n            [\n              -122.32177734375,\n              37.24782120155428\n            ],\n            [\n              -120.84960937499999,\n              34.288991865037524\n            ]\n          ]\n        ]\n      }\n    }\n  ]\n}","volume":"244","issue":"5413","noUsgsAuthors":false,"publicationDate":"1973-07-01","publicationStatus":"PW","scienceBaseUri":"4f4e4a60e4b07f02db6353a1","contributors":{"authors":[{"text":"Wood, M.D.","contributorId":63930,"corporation":false,"usgs":true,"family":"Wood","given":"M.D.","email":"","affiliations":[],"preferred":false,"id":346730,"contributorType":{"id":1,"text":"Authors"},"rank":1},{"text":"Allen, S.S.","contributorId":15747,"corporation":false,"usgs":true,"family":"Allen","given":"S.S.","email":"","affiliations":[],"preferred":false,"id":346729,"contributorType":{"id":1,"text":"Authors"},"rank":2}]}}
,{"id":70001355,"text":"70001355 - 1973 - A pneumatic sample changer for gamma-ray spectroscopy","interactions":[],"lastModifiedDate":"2020-12-23T22:07:14.196079","indexId":"70001355","displayToPublicDate":"2010-09-28T23:09:32","publicationYear":"1973","noYear":false,"publicationType":{"id":2,"text":"Article"},"publicationSubtype":{"id":10,"text":"Journal Article"},"seriesTitle":{"id":3276,"text":"Review of Scientific Instruments","active":true,"publicationSubtype":{"id":10}},"title":"A pneumatic sample changer for gamma-ray spectroscopy","docAbstract":"<div class=\"tab-content article-content publication-tabs\"><div class=\"tab tab-pane active\"><div class=\"article_tabel\"><div class=\"article_row\"><div class=\"article_left\"><div class=\"hlFld-Abstract\"><div class=\"NLM_paragraph\">A gravity‐feed, pneumatic‐ejection sample changer has been developed. The changer is suitable for both flat and well‐type detectors and permits the continuous use of gamma‐ray<span>&nbsp;</span>spectroscopy<span>&nbsp;</span>equipment 24 h a day, 7 days a week. The electronic circuitry has a fail‐safe feature which stops the operation of the changer if a malfunction occurs.</div></div></div></div></div></div></div>","language":"English","publisher":"AIP","doi":"10.1063/1.1686384","issn":"00346748","usgsCitation":"Massoni, C.J., Fones, R., and Simon, F., 1973, A pneumatic sample changer for gamma-ray spectroscopy: Review of Scientific Instruments, v. 44, no. 9, p. 1350-1352, https://doi.org/10.1063/1.1686384.","productDescription":"3 p.","startPage":"1350","endPage":"1352","costCenters":[],"links":[{"id":203801,"rank":0,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/thumbnails/outside_thumb.jpg"}],"volume":"44","issue":"9","noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"4f4e4b1ce4b07f02db6a954b","contributors":{"authors":[{"text":"Massoni, C. J.","contributorId":29082,"corporation":false,"usgs":true,"family":"Massoni","given":"C.","middleInitial":"J.","affiliations":[],"preferred":false,"id":346736,"contributorType":{"id":1,"text":"Authors"},"rank":1},{"text":"Fones, R.V.","contributorId":91224,"corporation":false,"usgs":true,"family":"Fones","given":"R.V.","email":"","affiliations":[],"preferred":false,"id":346738,"contributorType":{"id":1,"text":"Authors"},"rank":2},{"text":"Simon, F.O.","contributorId":41808,"corporation":false,"usgs":true,"family":"Simon","given":"F.O.","email":"","affiliations":[],"preferred":false,"id":346737,"contributorType":{"id":1,"text":"Authors"},"rank":3}]}}
,{"id":70001340,"text":"70001340 - 1973 - Apollo 17 \"Orange soil\" and meteorite impact on liquid lava","interactions":[],"lastModifiedDate":"2020-12-23T22:08:50.422933","indexId":"70001340","displayToPublicDate":"2010-09-28T23:09:32","publicationYear":"1973","noYear":false,"publicationType":{"id":2,"text":"Article"},"publicationSubtype":{"id":10,"text":"Journal Article"},"seriesTitle":{"id":2840,"text":"Nature","active":true,"publicationSubtype":{"id":10}},"title":"Apollo 17 \"Orange soil\" and meteorite impact on liquid lava","docAbstract":"<div id=\"Abs1-section\" class=\"c-article-section\"><div id=\"Abs1-content\" class=\"c-article-section__content\"><p>THE “orange soil” from Shorty Crater differs greatly from ordinary lunar soils in that it consists of<span>&nbsp;</span><span class=\"stix\">∼</span>99% 10–300 µm smooth shiny spherules and broken fragments of spherules of transparent orange glass, about 20% of which contain partly crystallized to opaque material. The remaining 1 % is chiefly crystalline basalt fragments. Although the colour of the individual orange spherule varies with thickness from yellow–orange to red–brown, all orange glass in our sample (74220, 70; 0.25 g) has a uniform index of refraction (<span class=\"stix\">∼</span><span>&nbsp;</span>1.712). By contrast, other lunar soils contain spherules ranging from 1.50 to 1.75. The orange glass is also completely free of bubbles, to the limit of resolution of the light microscope, whereas bubbles are present in many other spherule samples. The spherules generally appear spherical in a normal microscope mount, but when viewed from two directions many are found to be oblate spheroids with axial ratios varying from near 1.00 to as low as 0.42 (Fig. 1<i>a</i>). Some have fissioned during free flight<sup>1</sup><span>&nbsp;</span>and all stages of the fission process are found, as described for the Apollo 11 samples. Only a few spherules seem to have been distorted by landing while still soft. One notable exception is the occurrence of small spherules of orange glass conforming and adhering to the surface of larger black spherules (Fig. 1<i>b</i>).</p></div></div>","language":"English","publisher":"Nature","doi":"10.1038/244210a0","issn":"00280836","usgsCitation":"Roedder, E., and Weiblen, P., 1973, Apollo 17 \"Orange soil\" and meteorite impact on liquid lava: Nature, v. 244, no. 5413, p. 210-212, https://doi.org/10.1038/244210a0.","productDescription":"3 p.","startPage":"210","endPage":"212","costCenters":[],"links":[{"id":203666,"rank":0,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/thumbnails/outside_thumb.jpg"}],"volume":"244","issue":"5413","noUsgsAuthors":false,"publicationDate":"1973-07-01","publicationStatus":"PW","scienceBaseUri":"4f4e4ac7e4b07f02db67ad2c","contributors":{"authors":[{"text":"Roedder, E.","contributorId":100986,"corporation":false,"usgs":true,"family":"Roedder","given":"E.","affiliations":[],"preferred":false,"id":346728,"contributorType":{"id":1,"text":"Authors"},"rank":1},{"text":"Weiblen, P.W.","contributorId":31884,"corporation":false,"usgs":true,"family":"Weiblen","given":"P.W.","email":"","affiliations":[],"preferred":false,"id":346727,"contributorType":{"id":1,"text":"Authors"},"rank":2}]}}
,{"id":70000800,"text":"70000800 - 1973 - Population dynamics of pond zooplankton, I. Diaptomus pallidus Herrick","interactions":[],"lastModifiedDate":"2012-03-08T17:16:37","indexId":"70000800","displayToPublicDate":"2010-09-28T23:09:29","publicationYear":"1973","noYear":false,"publicationType":{"id":2,"text":"Article"},"publicationSubtype":{"id":10,"text":"Journal Article"},"seriesTitle":{"id":1919,"text":"Hydrobiologia","onlineIssn":"1573-5117","printIssn":"0018-8158","active":true,"publicationSubtype":{"id":10}},"title":"Population dynamics of pond zooplankton, I. Diaptomus pallidus Herrick","docAbstract":"The simultaneous and lag relationships between 27 environmental variables and seven population components of a perennial calanoid copepod were examined by simple and partial correlations and stepwise regression. The analyses consistently explained more than 70% of the variation of a population component. The multiple correlation coefficient (R) usually was highest in no lag or in 3-week or 4-week lag except for clutch size in which R was highest in 1-week lag. Population control, egg-bearing, and clutch size were affected primarily by environmental components categorized as weather; food apparently was relatively minor in affecting population control or reproduction. ?? 1973 Dr. W. Junk B.V. Publishers.","largerWorkType":{"id":2,"text":"Article"},"largerWorkTitle":"Hydrobiologia","largerWorkSubtype":{"id":10,"text":"Journal Article"},"language":"English","publisher":"Kluwer Academic Publishers","doi":"10.1007/BF00014119","issn":"00188158","usgsCitation":"Armitage, K., Saxena, B., and Angino, E., 1973, Population dynamics of pond zooplankton, I. Diaptomus pallidus Herrick: Hydrobiologia, v. 42, no. 2-3, p. 295-333, https://doi.org/10.1007/BF00014119.","startPage":"295","endPage":"333","costCenters":[],"links":[{"id":19020,"rank":9999,"type":{"id":10,"text":"Digital Object Identifier"},"url":"https://dx.doi.org/10.1007/BF00014119"},{"id":203367,"rank":0,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/thumbnails/outside_thumb.jpg"}],"volume":"42","issue":"2-3","noUsgsAuthors":false,"publicationDate":"1973-08-01","publicationStatus":"PW","scienceBaseUri":"4f4e4ad6e4b07f02db68410e","contributors":{"authors":[{"text":"Armitage, K.B.","contributorId":6567,"corporation":false,"usgs":true,"family":"Armitage","given":"K.B.","email":"","affiliations":[],"preferred":false,"id":346532,"contributorType":{"id":1,"text":"Authors"},"rank":1},{"text":"Saxena, B.","contributorId":55944,"corporation":false,"usgs":true,"family":"Saxena","given":"B.","email":"","affiliations":[],"preferred":false,"id":346534,"contributorType":{"id":1,"text":"Authors"},"rank":2},{"text":"Angino, E.E.","contributorId":8972,"corporation":false,"usgs":true,"family":"Angino","given":"E.E.","email":"","affiliations":[],"preferred":false,"id":346533,"contributorType":{"id":1,"text":"Authors"},"rank":3}]}}
,{"id":70001384,"text":"70001384 - 1973 - Population dynamics of pond zooplankton II Daphnia ambigua Scourfield","interactions":[],"lastModifiedDate":"2012-03-08T17:16:34","indexId":"70001384","displayToPublicDate":"2010-09-28T23:09:23","publicationYear":"1973","noYear":false,"publicationType":{"id":2,"text":"Article"},"publicationSubtype":{"id":10,"text":"Journal Article"},"seriesTitle":{"id":1919,"text":"Hydrobiologia","onlineIssn":"1573-5117","printIssn":"0018-8158","active":true,"publicationSubtype":{"id":10}},"title":"Population dynamics of pond zooplankton II Daphnia ambigua Scourfield","docAbstract":"Calcium was the most important of 27 environmental components affecting density for a 50 week period. Simultaneous stepwise regression accounted for more variability in total number/1 and in the number of ovigerous females/1 than did any of the lag analyses; 1-week lag accounted for the greatest amount of variability in clutch size. Total number and clutch size were little affected by measures of food. ?? 1973 Dr. W. Junk b.v. Publishers.","largerWorkType":{"id":2,"text":"Article"},"largerWorkTitle":"Hydrobiologia","largerWorkSubtype":{"id":10,"text":"Journal Article"},"language":"English","publisher":"Kluwer Academic Publishers","doi":"10.1007/BF00047022","issn":"00188158","usgsCitation":"Angino, E., Armitage, K., and Saxena, B., 1973, Population dynamics of pond zooplankton II Daphnia ambigua Scourfield: Hydrobiologia, v. 42, no. 4, p. 491-507, https://doi.org/10.1007/BF00047022.","startPage":"491","endPage":"507","costCenters":[],"links":[{"id":203686,"rank":0,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/thumbnails/outside_thumb.jpg"},{"id":19099,"rank":9999,"type":{"id":10,"text":"Digital Object Identifier"},"url":"https://dx.doi.org/10.1007/BF00047022"}],"volume":"42","issue":"4","noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"4f4e4ad6e4b07f02db68404f","contributors":{"authors":[{"text":"Angino, E.E.","contributorId":8972,"corporation":false,"usgs":true,"family":"Angino","given":"E.E.","email":"","affiliations":[],"preferred":false,"id":346741,"contributorType":{"id":1,"text":"Authors"},"rank":1},{"text":"Armitage, K.B.","contributorId":6567,"corporation":false,"usgs":true,"family":"Armitage","given":"K.B.","email":"","affiliations":[],"preferred":false,"id":346740,"contributorType":{"id":1,"text":"Authors"},"rank":2},{"text":"Saxena, B.","contributorId":55944,"corporation":false,"usgs":true,"family":"Saxena","given":"B.","email":"","affiliations":[],"preferred":false,"id":346742,"contributorType":{"id":1,"text":"Authors"},"rank":3}]}}
,{"id":70001379,"text":"70001379 - 1973 - A semiobjective method for condensing classifications","interactions":[],"lastModifiedDate":"2012-03-08T17:16:36","indexId":"70001379","displayToPublicDate":"2010-09-28T23:09:22","publicationYear":"1973","noYear":false,"publicationType":{"id":2,"text":"Article"},"publicationSubtype":{"id":10,"text":"Journal Article"},"seriesTitle":{"id":2554,"text":"Journal of the International Association for Mathematical Geology","active":true,"publicationSubtype":{"id":10}},"title":"A semiobjective method for condensing classifications","docAbstract":"A simple, semiobjective method is described to reduce the number of groups in a classification to an arbitrary level without losing contact with the geologic information contained in the evolving groups. The method, operated in a stepwise or cyclic manner, employs some of the commonly used numerical techniques, but avoids strict adherence to them to obtain geologically more meaningful results. The method is illustrated in a facies study of the upper Paleozoic rocks of southeastern Utah. ?? 1973 Plenum Publishing Corporation.","largerWorkType":{"id":2,"text":"Article"},"largerWorkTitle":"Journal of the International Association for Mathematical Geology","largerWorkSubtype":{"id":10,"text":"Journal Article"},"language":"English","publisher":"Kluwer Academic Publishers-Plenum Publishers","doi":"10.1007/BF02111815","issn":"00205958","usgsCitation":"Demirmen, F., 1973, A semiobjective method for condensing classifications: Journal of the International Association for Mathematical Geology, v. 5, no. 3, p. 285-296, https://doi.org/10.1007/BF02111815.","startPage":"285","endPage":"296","costCenters":[],"links":[{"id":203733,"rank":0,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/thumbnails/outside_thumb.jpg"},{"id":19098,"rank":9999,"type":{"id":10,"text":"Digital Object Identifier"},"url":"https://dx.doi.org/10.1007/BF02111815"}],"volume":"5","issue":"3","noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"4f4e4b17e4b07f02db6a6569","contributors":{"authors":[{"text":"Demirmen, F.","contributorId":16144,"corporation":false,"usgs":true,"family":"Demirmen","given":"F.","email":"","affiliations":[],"preferred":false,"id":346739,"contributorType":{"id":1,"text":"Authors"},"rank":1}]}}
,{"id":70001390,"text":"70001390 - 1973 - Vesicles, water, and sulfur in Reykjanes Ridge basalts","interactions":[],"lastModifiedDate":"2020-12-23T22:20:49.285414","indexId":"70001390","displayToPublicDate":"2010-09-28T23:09:21","publicationYear":"1973","noYear":false,"publicationType":{"id":2,"text":"Article"},"publicationSubtype":{"id":10,"text":"Journal Article"},"seriesTitle":{"id":1336,"text":"Contributions to Mineralogy and Petrology","active":true,"publicationSubtype":{"id":10}},"title":"Vesicles, water, and sulfur in Reykjanes Ridge basalts","docAbstract":"<p>Dredge hauls of fresh submarine basalt collected from the axis of the Reykjanes Ridge (Mid-Atlantic Ridge) south of Iceland were taken aboard<span>&nbsp;</span><i>R/ V TRIDENT</i><span>&nbsp;</span>in 1967 and 1971. The samples show systematic changes as the water depth of collection (and eruption) decreases: radially elongate vesicles and concentric zones of vesicles appear at about 700 m depth and are conspicuous to shallow water; the smoothed volume percent of vesicles increases from 5% at 1000 m, 10% at 700 m, to 16% at 500 m, and the scatter in degree of vesicularity increases in shallower water; specific gravity decreases from 2.7±0.1 at 1000 m to 2.3±0.3 at 100 m.</p><p>Bulk sulfur content for the outer 2 cm averages 843 ppm up to a depth of 200 m, then drops off rapidly in shallower water owing to degassing. Sulfur content below 200 m is independent of depth (or geographic position), and the melt is apparently saturated with sulfur, but the excess cannot escape the lava unless another vehicle carries it out. Only shallower than 200 m, where intense vesiculation of other gases occurs can excess sulfur be lost from the lava erupting on the sea floor.</p><p>H<sub>2</sub>O<sup>+110°</sup><span>&nbsp;</span>averages about 0.35 percent and H<sub>2</sub>O<sup>+150°</sup><span>&nbsp;</span>about 0.25 percent, and both apparently decrease in water shallower than 200 m as a result of degassing. H<sub>2</sub>O<sup>+</sup><span>&nbsp;</span>(below 200 m) decreases with distance from Iceland or increasing depth, presumably as a result of either adsorption of water on the surface of shallower, more vesicular rocks; or more likely due to the presence of the Iceland hot mantle plume supplying undifferentiated primordial material, relative to lavas of the Reykjanes Ridge supplied from the low velocity layer already depleted in volatiles and large lithophile elements. The H<sub>2</sub>O<sup>+110°</sup>/S ratio of lava erupting below 200 m water depth ranges from 3 to 5 which is comparable to reliable gas analyses from oceanic basaltic volcanoes.</p>","language":"English","publisher":"Springer","doi":"10.1007/BF00375036","issn":"00107999","usgsCitation":"Moore, J., and Schilling, J., 1973, Vesicles, water, and sulfur in Reykjanes Ridge basalts: Contributions to Mineralogy and Petrology, v. 41, no. 2, p. 105-118, https://doi.org/10.1007/BF00375036.","productDescription":"14 p.","startPage":"105","endPage":"118","costCenters":[],"links":[{"id":203331,"rank":0,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/thumbnails/outside_thumb.jpg"}],"country":"Iceland","geographicExtents":"{\"type\":\"FeatureCollection\",\"features\":[{\"type\":\"Feature\",\"geometry\":{\"type\":\"Polygon\",\"coordinates\":[[[-14.5087,66.45589],[-14.73964,65.80875],[-13.60973,65.12667],[-14.90983,64.36408],[-17.79444,63.67875],[-18.65625,63.49638],[-19.97275,63.64363],[-22.76297,63.96018],[-21.77848,64.40212],[-23.95504,64.89113],[-22.1844,65.08497],[-22.22742,65.37859],[-24.32618,65.61119],[-23.65051,66.26252],[-22.13492,66.41047],[-20.57628,65.73211],[-19.05684,66.2766],[-17.79862,65.99385],[-16.16782,66.52679],[-14.5087,66.45589]]]},\"properties\":{\"name\":\"Iceland\"}}]}","volume":"41","issue":"2","noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"4f4e4a13e4b07f02db601ece","contributors":{"authors":[{"text":"Moore, J.G.","contributorId":67496,"corporation":false,"usgs":true,"family":"Moore","given":"J.G.","email":"","affiliations":[],"preferred":false,"id":346744,"contributorType":{"id":1,"text":"Authors"},"rank":1},{"text":"Schilling, J.-G.","contributorId":55127,"corporation":false,"usgs":true,"family":"Schilling","given":"J.-G.","email":"","affiliations":[],"preferred":false,"id":346743,"contributorType":{"id":1,"text":"Authors"},"rank":2}]}}
,{"id":70001402,"text":"70001402 - 1973 - Thermochemical parameters of minerals from oxygen-buffered hydrothermal equilibrium data: Method, application to annite and almandine","interactions":[],"lastModifiedDate":"2020-12-23T22:12:29.55059","indexId":"70001402","displayToPublicDate":"2010-09-28T23:09:21","publicationYear":"1973","noYear":false,"publicationType":{"id":2,"text":"Article"},"publicationSubtype":{"id":10,"text":"Journal Article"},"seriesTitle":{"id":1336,"text":"Contributions to Mineralogy and Petrology","active":true,"publicationSubtype":{"id":10}},"title":"Thermochemical parameters of minerals from oxygen-buffered hydrothermal equilibrium data: Method, application to annite and almandine","docAbstract":"<div id=\"Abs1-section\" class=\"c-article-section\"><div id=\"Abs1-content\" class=\"c-article-section__content\"><p>Reversed univariant hydrothermal phase-equilibrium reactions, in which a redox reaction occurs and is controlled by oxygen buffers, can be used to extract thermochemical data on minerals. The dominant gaseous species present, even for relatively oxidizing buffers such as the QFM buffer, are H<sub>2</sub>O and H<sub>2</sub>; the main problem is to calculate the chemical potentials of these components in a binary mixture. The mixing of these two species in the gas phase was assumed by Eugster and Wones (1962) to be ideal; this assumption allows calculation of the chemical potentials of the two components in a binary gas mixture, using data in the literature. A simple-mixture model of nonideal mixing, such as that proposed by Shaw (1967), can also be combined with the equations of state for oxygen buffers to permit derivation of the chemical potentials of the two components. The two mixing models yield closely comparable results for the more oxidizing buffers such as the QFM buffer. For reducing buffers such as IQF, the nonideal-mixing correction can be significant and the Shaw model is better.</p><p>The procedure of calculation of mineralogical thermochemical data, in reactions where hydrogen and H<sub>2</sub>O simultaneously appear, is applied to the experimental data on annite, given by Wones<span>&nbsp;</span><i>et al.</i><span>&nbsp;</span>(1971), and on almandine, given by Hsu (1968). For annite the results are: Standard entropy of formation from the elements,<span>&nbsp;</span><i>S</i><span>&nbsp;</span><span class=\"c-stack\"><sup>0</sup><sub>f</sub></span><span>&nbsp;</span>(298, 1)=−283.35±2.2 gb/gf,<span>&nbsp;</span><i>S</i><span>&nbsp;</span><sup>0</sup><span>&nbsp;</span>(298, 1) =+92.5 gb/gf.<span>&nbsp;</span><i>G</i><span>&nbsp;</span><span class=\"c-stack\"><sup>0</sup><sub>f</sub></span><span>&nbsp;</span>(298, 1)=−1148.2±6 kcal, and<span>&nbsp;</span><i>H</i><span>&nbsp;</span><span class=\"c-stack\"><sup>0</sup><sub>f</sub></span><span>&nbsp;</span>(298, 1)=−1232.7±7 kcal. For almandine, the calculation takes into account the mutual solution of FeAl<sub>2</sub>O<sub>4</sub><span>&nbsp;</span>(Hc) in magnetite and of Fe<sub>3</sub>O<sub>4</sub><span>&nbsp;</span>(Mt) in hercynite and the temperature dependence of this solid solution, as given by Turnock and Eugster (1962); the calculations assume a regular-solution model for this binary spinel system. The standard entropy of formation of almandine,<span>&nbsp;</span><i>S</i><span>&nbsp;</span><span class=\"c-stack\"><sup>0</sup><sub>f,A</sub></span><span>&nbsp;</span>(298, 1) is −272.33±3 gb/gf. The third law entropy,<span>&nbsp;</span><i>S</i><span>&nbsp;</span><sup>0</sup><span>&nbsp;</span>(298, 1) is +68.3±3 gb/gf, a value much less than the oxide-sum estimate but the deviation is nearly the same as that of grossularite, referring to a comparable set of oxide standard states. The Gibbs free energy<span>&nbsp;</span><i>G</i><span>&nbsp;</span><span class=\"c-stack\"><sup>0</sup><sub>f,A</sub></span><span>&nbsp;</span>(298, 1) is −1192.36±4 kcal, and the enthalpy<span>&nbsp;</span><i>H</i><span>&nbsp;</span><span class=\"c-stack\"><sup>0</sup><sub>f,A</sub></span><span>&nbsp;</span>(298, 1) is −1273.56±5 kcal.</p></div></div>","language":"English","publisher":"Springer","doi":"10.1007/BF00374246","issn":"00107999","usgsCitation":"Zen, E., 1973, Thermochemical parameters of minerals from oxygen-buffered hydrothermal equilibrium data: Method, application to annite and almandine: Contributions to Mineralogy and Petrology, v. 39, no. 1, p. 65-80, https://doi.org/10.1007/BF00374246.","productDescription":"16 p.","startPage":"65","endPage":"80","costCenters":[],"links":[{"id":203486,"rank":0,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/thumbnails/outside_thumb.jpg"}],"volume":"39","issue":"1","noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"4f4e4a08e4b07f02db5fa617","contributors":{"authors":[{"text":"Zen, E-An","contributorId":47064,"corporation":false,"usgs":true,"family":"Zen","given":"E-An","email":"","affiliations":[],"preferred":false,"id":346747,"contributorType":{"id":1,"text":"Authors"},"rank":1}]}}
,{"id":70001404,"text":"70001404 - 1973 - Role of reef fauna in sediment transport and distribution - Studies from Tektite I and II","interactions":[],"lastModifiedDate":"2022-11-18T18:04:13.758327","indexId":"70001404","displayToPublicDate":"2010-09-28T00:00:00","publicationYear":"1973","noYear":false,"publicationType":{"id":2,"text":"Article"},"publicationSubtype":{"id":10,"text":"Journal Article"},"seriesTitle":{"id":1886,"text":"Helgoländer Wissenschaftliche Meeresuntersuchungen","active":true,"publicationSubtype":{"id":10}},"title":"Role of reef fauna in sediment transport and distribution - Studies from Tektite I and II","docAbstract":"1. Reef organisms may play a major role in the transport and distribution of sediment on the sea floor adjacent to coral reefs. 2. Some fish such as Malacanthus plumieri (Bloch) selectively transport and collect certain types of sediment (such as larger coral and shell fragments). 3. The random movement of crawling or burrowing organisms may cause a large amount of sediment to be shifted laterally on the sea floor. On slopes, a net downhill displacement may result. 4. The surface configuration and internal structure of the sediment is rapidly changed by faunal mixing. Ripple marks formed by waves or currents are obliterated by the activity of organisms in only a few weeks in the environment studied. Internal structure (bedding) near the sediment-water interface is similarly destroyed in a short period of time. 5. Larger clasts (including empty shells) on the sea floor tend to be buried by faunal undermining. The rate of burial depends primarily on the grain size of the substrate. 6. The random movement of fauna on the sea floor may produce a predominantly concave-up orientation of pelecypod shells and shell fragments on the sea floor - the opposite of that produced by the activity of waves or currents. ?? 1973 Biologischen Anstalt Helgoland.","language":"English","publisher":"Springer-Verlag","doi":"10.1007/BF01609502","usgsCitation":"Clifton, H., 1973, Role of reef fauna in sediment transport and distribution - Studies from Tektite I and II: Helgoländer Wissenschaftliche Meeresuntersuchungen, v. 24, no. 1-4, p. 91-101, https://doi.org/10.1007/BF01609502.","productDescription":"11 p.","startPage":"91","endPage":"101","costCenters":[],"links":[{"id":480653,"rank":1,"type":{"id":40,"text":"Open Access Publisher Index Page"},"url":"https://doi.org/10.1007/bf01609502","text":"Publisher Index Page"},{"id":203289,"rank":0,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/thumbnails/outside_thumb.jpg"}],"volume":"24","issue":"1-4","noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"4f4e4a0ee4b07f02db5fe281","contributors":{"authors":[{"text":"Clifton, H.E.","contributorId":44151,"corporation":false,"usgs":true,"family":"Clifton","given":"H.E.","affiliations":[],"preferred":false,"id":346748,"contributorType":{"id":1,"text":"Authors"},"rank":1}]}}
,{"id":5220926,"text":"5220926 - 1973 - Molt patterns and weight changes of the American woodcock","interactions":[],"lastModifiedDate":"2012-02-02T00:15:01","indexId":"5220926","displayToPublicDate":"2010-06-16T12:17:56","publicationYear":"1973","noYear":false,"publicationType":{"id":2,"text":"Article"},"publicationSubtype":{"id":10,"text":"Journal Article"},"seriesTitle":{"id":3783,"text":"The Wilson Bulletin","printIssn":"0043-5643","active":true,"publicationSubtype":{"id":10}},"title":"Molt patterns and weight changes of the American woodcock","docAbstract":"A study of molt and changes in body weight of American Woodcock was conducted to better understand the summer and fall behavior of these birds and to indicate periods of physiological stress. The postnuptial molt of adults was a complete molt beginning in late June and ending by the middle of October. In contrast, the postjuvenal molt was a less intensive partial molt beginning in mid-July but also extending to the middle of October. Both male and female adult birds experienced weight loss in August during peak molt. Young birds gradually gained weight throughout the summer. Fat deposition was negatively correlated with molt while fall body weights were positively correlated with fat deposition. The data indicated that the majority of Maine woodcock are not physiologically prepared for migration until mid-October. Weights of adult males during the spring suggested that this is an important period of stress for these birds.","largerWorkType":{"id":2,"text":"Article"},"largerWorkTitle":"Wilson Bulletin","largerWorkSubtype":{"id":10,"text":"Journal Article"},"language":"English","usgsCitation":"Owen, R., and Krohn, W., 1973, Molt patterns and weight changes of the American woodcock: The Wilson Bulletin, v. 85, no. 1, p. 31-41.","productDescription":"31-41","startPage":"31","endPage":"41","numberOfPages":"11","costCenters":[{"id":531,"text":"Patuxent Wildlife Research Center","active":true,"usgs":true}],"links":[{"id":16198,"rank":300,"type":{"id":11,"text":"Document"},"url":"https://elibrary.unm.edu/sora/Wilson/v085n01/p0031-p0041.pdf","linkFileType":{"id":1,"text":"pdf"}},{"id":198218,"rank":0,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/thumbnails/outside_thumb.jpg"}],"volume":"85","issue":"1","noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"4f4e4b04e4b07f02db699251","contributors":{"authors":[{"text":"Owen, Ray B.","contributorId":42670,"corporation":false,"usgs":true,"family":"Owen","given":"Ray B.","affiliations":[],"preferred":false,"id":332695,"contributorType":{"id":1,"text":"Authors"},"rank":1},{"text":"Krohn, W.B.","contributorId":64355,"corporation":false,"usgs":true,"family":"Krohn","given":"W.B.","email":"","affiliations":[],"preferred":false,"id":332696,"contributorType":{"id":1,"text":"Authors"},"rank":2}]}}
,{"id":5223186,"text":"5223186 - 1973 - The seventy-third Christmas bird count.  327.  Little Creek, Va","interactions":[],"lastModifiedDate":"2012-02-02T00:15:38","indexId":"5223186","displayToPublicDate":"2010-06-16T12:17:56","publicationYear":"1973","noYear":false,"publicationType":{"id":2,"text":"Article"},"publicationSubtype":{"id":10,"text":"Journal Article"},"seriesTitle":{"id":708,"text":"American Birds","active":true,"publicationSubtype":{"id":10}},"title":"The seventy-third Christmas bird count.  327.  Little Creek, Va","largerWorkType":{"id":2,"text":"Article"},"largerWorkTitle":"American Birds","largerWorkSubtype":{"id":10,"text":"Journal Article"},"language":"English","usgsCitation":"Sykes, P., 1973, The seventy-third Christmas bird count.  327.  Little Creek, Va: American Birds, v. 27, no. 2.","productDescription":"274","startPage":"274","numberOfPages":"274","costCenters":[{"id":531,"text":"Patuxent Wildlife Research Center","active":true,"usgs":true}],"links":[{"id":199911,"rank":0,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/thumbnails/outside_thumb.jpg"}],"volume":"27","issue":"2","noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"4f4e4a62e4b07f02db6364cb","contributors":{"authors":[{"text":"Sykes, P. Jr.","contributorId":75653,"corporation":false,"usgs":true,"family":"Sykes","given":"P.","suffix":"Jr.","email":"","affiliations":[],"preferred":false,"id":338081,"contributorType":{"id":1,"text":"Authors"},"rank":1}]}}
]}