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 \"}}]}","noUsgsAuthors":false,"publicationStatus":"PW","contributors":{"authors":[{"text":"Colbert, J. L.","contributorId":101680,"corporation":false,"usgs":true,"family":"Colbert","given":"J.","email":"","middleInitial":"L.","affiliations":[],"preferred":false,"id":920402,"contributorType":{"id":1,"text":"Authors"},"rank":1}]}}
,{"id":70095403,"text":"70095403 - 1963 - Public water supplies in Gloucester County, New Jersey","interactions":[],"lastModifiedDate":"2018-01-08T18:32:03","indexId":"70095403","displayToPublicDate":"1963-01-01T16:10:00","publicationYear":"1963","noYear":false,"publicationType":{"id":18,"text":"Report"},"publicationSubtype":{"id":2,"text":"State or Local Government Series"},"seriesTitle":{"id":149,"text":"New Jersey Division of Water Policy and Supply Water Resources Circular","active":false,"publicationSubtype":{"id":2}},"seriesNumber":"9","title":"Public water supplies in Gloucester County, New Jersey","docAbstract":"<p>Gloucester County is in the southwestern part of New Jersey, below Camden, and is a part of the Lower Delaware River Valley. This area is attracting new industry and has shown a population increase of about 47 percent from 1950 to 1960, mostly urban. With the economic growth of the county, the availability and quality of water become increasingly important.</p><p>The county is in the Coastal Plain of New Jersey. It is underlain by unconsolidated sands and clays of Quaternary, Tertiary, and Cretaceous age. The Raritan and Magothy Formations constitute the most important aquifers and yield more than 95 percent of the water pumped by the public water systems in the county. These formations are capable of yielding 1,400 gpm (gallons per minute) or more to large diameter wells. High yielding wells generally can be drilled anywhere in the county, although the formations are deeper toward the Atlantic Ocean. The Cohansey Sand, second most important aquifer, yields up to 800 gpm or more from large diameter wells. This aquifer is present only in the sparsely populated southeastern half of the county. The Wenonah Formation and Mount Laurel Sand are capable of yielding 100 to 200 gpm in certain areas.</p><p>The overall chemical quality of the naturally occurring ground water is good. The water generally meets the U.S. Public Health Service's (1962) suggested limit for dissolved solids; however, in some areas, the water carries objectionable amounts of iron and nitrate in solution and has a low pH. Contamination of ground water by salt-water encroachment or by pollution from industrial activity or organic waste in densely populated areas should be prevented. The quality rather than the quantity of water may be the important factor in future ground-water developments.</p><p>The 21 public water systems in Gloucester County pumped about 1.3 billion gallons of water during 1948 and some 2.7 billion gallons during 1959. This is slightly more than a hundred percent increase in pumpage in 12 year s. The average per capita public water supply consumption in 1959 was approximately 75 gallons per day.</p><p>This report includes a summary of the history of the present installations, groundwater conditions, quality and availability of water, and potential future yield for the 2 public water systems in Gloucester County.</p>","language":"English","publisher":"State of New Jersey Department of Conservation and Economic Development, Division of Water Policy and Supply","collaboration":"Prepared by the U.S. Geological Survey in cooperation with the State of New Jersey","usgsCitation":"Hardt, W.F., 1963, Public water supplies in Gloucester County, New Jersey: New Jersey Division of Water Policy and Supply Water Resources Circular 9, vii, 55 p.","productDescription":"vii, 55 p.","numberOfPages":"64","costCenters":[],"links":[{"id":284195,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/thumbnails/outside_thumb.jpg"},{"id":286049,"type":{"id":11,"text":"Document"},"url":"https://pubs.usgs.gov/unnumbered/70095403/report.pdf"}],"country":"United States","state":"New Jersey","county":"Gloucester County","otherGeospatial":"Lower Delaware River Valley","geographicExtents":"{ \"type\": \"FeatureCollection\", \"features\": [ { \"type\": \"Feature\", \"properties\": {}, \"geometry\": { \"type\": \"Polygon\", \"coordinates\": [ [ [ -75.42875,39.514802 ], [ -75.42875,39.888317 ], [ 74.877189,39.888317 ], [ 74.877189,39.514802 ], [ -75.42875,39.514802 ] ] ] } } ] }","noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"5355952ee4b0120853e8c16f","contributors":{"authors":[{"text":"Hardt, William F.","contributorId":70013,"corporation":false,"usgs":true,"family":"Hardt","given":"William","email":"","middleInitial":"F.","affiliations":[],"preferred":false,"id":491187,"contributorType":{"id":1,"text":"Authors"},"rank":1}]}}
,{"id":70221092,"text":"70221092 - 1963 - Some aspects of sampling salty ground water in coastal aquifers","interactions":[],"lastModifiedDate":"2021-06-01T19:38:26.940939","indexId":"70221092","displayToPublicDate":"1963-01-01T14:34:40","publicationYear":"1963","noYear":false,"publicationType":{"id":2,"text":"Article"},"publicationSubtype":{"id":10,"text":"Journal Article"},"seriesTitle":{"id":3825,"text":"Groundwater","active":true,"publicationSubtype":{"id":10}},"title":"Some aspects of sampling salty ground water in coastal aquifers","docAbstract":"<p><span>Investigations of the fluctuations of chloride content&nbsp;</span><span class=\"ScopusTermHighlight\">in</span><span>&nbsp;wells that tap the zone of diffusion between fresh and salt&nbsp;</span><span class=\"ScopusTermHighlight\">water</span><span>&nbsp;show that the&nbsp;</span><span class=\"ScopusTermHighlight\">salty</span><span>&nbsp;well&nbsp;</span><span class=\"ScopusTermHighlight\">water</span><span>&nbsp;behaves erratically when the well is pumped. Frequently, a static distribution of chloride content that ranges from less than 1,000 ppm at the top to more than 10,000 ppm at the bottom is present&nbsp;</span><span class=\"ScopusTermHighlight\">in</span><span>&nbsp;the open‐hole part of a well. When the well is pumped, the discharge&nbsp;</span><span class=\"ScopusTermHighlight\">water</span><span>&nbsp;tends to come from the upper part of the open hole because less energy is expended by removal of low‐density&nbsp;</span><span class=\"ScopusTermHighlight\">water</span><span>&nbsp;from this region than by removal of high‐density&nbsp;</span><span class=\"ScopusTermHighlight\">water</span><span>&nbsp;from the lower part of the open hole. Where the permeability of strata&nbsp;</span><span class=\"ScopusTermHighlight\">in</span><span>&nbsp;the deep part of the open hole is greater than that&nbsp;</span><span class=\"ScopusTermHighlight\">in</span><span>&nbsp;the shallow part, the tendency for natural selection of the less dense, shallow&nbsp;</span><span class=\"ScopusTermHighlight\">water</span><span>&nbsp;is suppressed, and practically all the&nbsp;</span><span class=\"ScopusTermHighlight\">water</span><span>&nbsp;</span><span class=\"ScopusTermHighlight\">in</span><span>&nbsp;the blend comes from the deep part. As a result of this complex interrelation of hydraulics, distribution and density of the salt&nbsp;</span><span class=\"ScopusTermHighlight\">water</span><span>, and permeability, the depth at which the pumped&nbsp;</span><span class=\"ScopusTermHighlight\">water</span><span>&nbsp;enters the well bore is indeterminate. This deficiency leads to the use of multiple‐depth‐bottle, windshield‐wiper, and electrical‐conductivity&nbsp;</span><span class=\"ScopusTermHighlight\">sampling</span><span>&nbsp;techniques for collection of data used&nbsp;</span><span class=\"ScopusTermHighlight\">in</span><span>&nbsp;constructing maps and cross sections that show the areal‐depth relations of salt&nbsp;</span><span class=\"ScopusTermHighlight\">water</span><span>&nbsp;</span><span class=\"ScopusTermHighlight\">in</span><span>&nbsp;the Biscayne&nbsp;</span><span class=\"ScopusTermHighlight\">aquifer</span><span>&nbsp;of the Miami area, Florida.&nbsp;</span></p>","language":"English","publisher":"Wiley  Blackwell","doi":"10.1111/j.1745-6584.1963.tb01903.x","usgsCitation":"Kohout, F., and Hoy, N., 1963, Some aspects of sampling salty ground water in coastal aquifers: Groundwater, v. 1, no. 1, p. 28-43, https://doi.org/10.1111/j.1745-6584.1963.tb01903.x.","productDescription":"16 p.","startPage":"28","endPage":"43","costCenters":[],"links":[{"id":386072,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/thumbnails/outside_thumb.jpg"}],"volume":"1","issue":"1","noUsgsAuthors":false,"publicationDate":"2006-07-06","publicationStatus":"PW","contributors":{"authors":[{"text":"Kohout, F. A.","contributorId":103979,"corporation":false,"usgs":true,"family":"Kohout","given":"F. A.","affiliations":[],"preferred":false,"id":816732,"contributorType":{"id":1,"text":"Authors"},"rank":1},{"text":"Hoy, N.D.","contributorId":15618,"corporation":false,"usgs":true,"family":"Hoy","given":"N.D.","email":"","affiliations":[],"preferred":false,"id":816733,"contributorType":{"id":1,"text":"Authors"},"rank":2}]}}
,{"id":70221083,"text":"70221083 - 1963 - Observations on archaeological remains in northeastern Bolivia","interactions":[],"lastModifiedDate":"2021-06-01T18:46:01.956628","indexId":"70221083","displayToPublicDate":"1963-01-01T13:41:45","publicationYear":"1963","noYear":false,"publicationType":{"id":2,"text":"Article"},"publicationSubtype":{"id":10,"text":"Journal Article"},"seriesTitle":{"id":700,"text":"American Antiquity","active":true,"publicationSubtype":{"id":10}},"title":"Observations on archaeological remains in northeastern Bolivia","docAbstract":"<p><span class=\"ScopusTermHighlight\">In</span><span>&nbsp;the Department of Beni,&nbsp;</span><span class=\"ScopusTermHighlight\">northeastern</span><span>&nbsp;</span><span class=\"ScopusTermHighlight\">Bolivia</span><span>, there are remnants of cultivated fields, roadways, and canals that are distributed over an area of 15,000 square miles. These features are interpreted as indicating the former existence of a highly organized, populous, agrarian society that antedates the culture of the Indian tribes now&nbsp;</span><span class=\"ScopusTermHighlight\">in</span><span>&nbsp;the area.&nbsp;</span></p>","language":"English","publisher":"Society for American Archaeology","doi":"10.2307/278279","usgsCitation":"Plafker, G., 1963, Observations on archaeological remains in northeastern Bolivia: American Antiquity, v. 28, no. 3, p. 372-378, https://doi.org/10.2307/278279.","productDescription":"7 p.","startPage":"372","endPage":"378","costCenters":[],"links":[{"id":386057,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/thumbnails/outside_thumb.jpg"}],"country":"Bolivia","otherGeospatial":"northeastern Bolivia","geographicExtents":"{\n  \"type\": \"FeatureCollection\",\n  \"features\": [\n    {\n      \"type\": \"Feature\",\n      \"properties\": {},\n      \"geometry\": {\n        \"type\": \"Polygon\",\n        \"coordinates\": [\n          [\n            [\n              -64.6875,\n              -17.978733095556155\n            ],\n            [\n              -59.67773437500001,\n              -17.978733095556155\n            ],\n            [\n              -59.67773437500001,\n              -12.125264218331578\n            ],\n            [\n              -64.6875,\n              -12.125264218331578\n            ],\n            [\n              -64.6875,\n              -17.978733095556155\n            ]\n          ]\n        ]\n      }\n    }\n  ]\n}","volume":"28","issue":"3","noUsgsAuthors":false,"publicationDate":"2017-01-20","publicationStatus":"PW","contributors":{"authors":[{"text":"Plafker, George 0000-0003-3972-0390","orcid":"https://orcid.org/0000-0003-3972-0390","contributorId":36603,"corporation":false,"usgs":true,"family":"Plafker","given":"George","affiliations":[],"preferred":false,"id":816712,"contributorType":{"id":1,"text":"Authors"},"rank":1}]}}
,{"id":37742,"text":"37742 - 1963 - Publications on national wildlife refuges","interactions":[],"lastModifiedDate":"2014-07-22T13:39:49","indexId":"37742","displayToPublicDate":"1963-01-01T13:39:30","publicationYear":"1963","noYear":false,"publicationType":{"id":18,"text":"Report"},"publicationSubtype":{"id":1,"text":"Federal Government Series"},"seriesTitle":{"id":98,"text":"Wildlife Leaflet","active":false,"publicationSubtype":{"id":1}},"seriesNumber":"450","title":"Publications on national wildlife refuges","docAbstract":"No abstract available.","language":"English","usgsCitation":"U.S. Fish and Wildlife Service, 1963, Publications on national wildlife refuges: Wildlife Leaflet 450, 4 p.","productDescription":"4 p.","numberOfPages":"4","costCenters":[],"links":[{"id":290721,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/thumbnails/outside_thumb.jpg"}],"noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"57ffcfdae4b0824b2d176136","contributors":{"authors":[{"text":"U.S. Fish and Wildlife Service","contributorId":128143,"corporation":true,"usgs":false,"organization":"U.S. Fish and Wildlife Service","id":529693,"contributorType":{"id":1,"text":"Authors"},"rank":1}]}}
,{"id":70221066,"text":"70221066 - 1963 - The atomic ratios of natural ferruginous biotites with reference to 'the stability relations of the ferruginous biotite, annite'","interactions":[],"lastModifiedDate":"2021-06-01T16:49:03.824921","indexId":"70221066","displayToPublicDate":"1963-01-01T11:45:56","publicationYear":"1963","noYear":false,"publicationType":{"id":2,"text":"Article"},"publicationSubtype":{"id":10,"text":"Journal Article"},"seriesTitle":{"id":2420,"text":"Journal of Petrology","active":true,"publicationSubtype":{"id":10}},"title":"The atomic ratios of natural ferruginous biotites with reference to 'the stability relations of the ferruginous biotite, annite'","docAbstract":"<p class=\"chapter-para\">The atomic ratios given by Eugster and Wones (1962) for analyses of high FeO-low MgO micas cited by Foster (1960) are in error. The recalculated atomic ratios herein presented show that only three of the thirteen have low (OH+F), and only one has characteristics that may possibly be due to loss of water during determination. None of the analyses exhibit characteristics suggestive of oxidation of iron and loss of H, as in progression towards oxyannite.</p><p class=\"chapter-para\">The average recalculated octahedral occupancy is 2.69, not 2.91 as in the previous calculation.</p><p class=\"chapter-para\">The differences between atomic ratios calculated on the basis ot determined H<sub>2</sub>O<sup>+</sup><span>&nbsp;</span>and F and those calculated on the basis of the theoretical O<sub>10</sub><span>&nbsp;</span>(OH)<sub>2</sub><span>&nbsp;</span>content are not great enough to change the essential compositional character of these micas as interpreted by Foster (1960). However, they do affect significantly the calculated octahedral occupancy.</p>","language":"English","publisher":"Oxford University Press","doi":"10.1093/petrology/4.2.302","usgsCitation":"Foster, M.D., Wones, D.R., and Eugster, H., 1963, The atomic ratios of natural ferruginous biotites with reference to 'the stability relations of the ferruginous biotite, annite': Journal of Petrology, v. 4, no. 2, p. 302-306, https://doi.org/10.1093/petrology/4.2.302.","productDescription":"5 p.","startPage":"302","endPage":"306","costCenters":[],"links":[{"id":386038,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/thumbnails/outside_thumb.jpg"}],"volume":"4","issue":"2","noUsgsAuthors":false,"publicationStatus":"PW","contributors":{"authors":[{"text":"Foster, Margaret D.","contributorId":21141,"corporation":false,"usgs":true,"family":"Foster","given":"Margaret","email":"","middleInitial":"D.","affiliations":[],"preferred":false,"id":816682,"contributorType":{"id":1,"text":"Authors"},"rank":1},{"text":"Wones, David R.","contributorId":47455,"corporation":false,"usgs":true,"family":"Wones","given":"David","email":"","middleInitial":"R.","affiliations":[],"preferred":false,"id":816683,"contributorType":{"id":1,"text":"Authors"},"rank":2},{"text":"Eugster, H.P.","contributorId":99992,"corporation":false,"usgs":true,"family":"Eugster","given":"H.P.","email":"","affiliations":[],"preferred":false,"id":816684,"contributorType":{"id":1,"text":"Authors"},"rank":3}]}}
,{"id":70209095,"text":"70209095 - 1963 - Preliminary report on the water resources of Kohala Mountain and Mauna Kea, Hawaii","interactions":[],"lastModifiedDate":"2020-03-16T10:35:26","indexId":"70209095","displayToPublicDate":"1963-01-01T11:35:09","publicationYear":"1963","noYear":false,"publicationType":{"id":18,"text":"Report"},"publicationSubtype":{"id":2,"text":"State or Local Government Series"},"seriesTitle":{"id":5942,"text":"Circular","active":false,"publicationSubtype":{"id":2}},"seriesNumber":"C14","title":"Preliminary report on the water resources of Kohala Mountain and Mauna Kea, Hawaii","docAbstract":"<p>No abstract available.</p>","language":"English","publisher":"State of Hawaii","publisherLocation":"Honolulu, Hawaii","collaboration":"Prepared by the U.S. Geological Survey in cooperation with the Division of Water and Land Development, Department of Land and Natural Resources","usgsCitation":"Davis, D.A., and Yamanaga, G., 1963, Preliminary report on the water resources of Kohala Mountain and Mauna Kea, Hawaii: Circular C14, vi, 44 p.","productDescription":"vi, 44 p.","costCenters":[],"links":[{"id":373285,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/thumbnails/outside_thumb.jpg"}],"country":"United States","state":"Hawaii","otherGeospatial":"Kohala Mountain, Mauna Kea","geographicExtents":"{\n  \"type\": \"FeatureCollection\",\n  \"features\": [\n    {\n      \"type\": \"Feature\",\n      \"properties\": {},\n      \"geometry\": {\n        \"type\": \"Polygon\",\n        \"coordinates\": [\n          [\n            [\n              -155.7964324951172,\n              20.033999524160667\n            ],\n            [\n              -155.57395935058594,\n              20.033999524160667\n            ],\n            [\n              -155.57395935058594,\n              20.209689679623374\n            ],\n            [\n              -155.7964324951172,\n              20.209689679623374\n            ],\n            [\n              -155.7964324951172,\n              20.033999524160667\n            ]\n          ]\n        ]\n      }\n    },\n    {\n      \"type\": \"Feature\",\n      \"properties\": {},\n      \"geometry\": {\n        \"type\": \"Polygon\",\n        \"coordinates\": [\n          [\n            [\n              -155.64193725585938,\n              19.711768236041355\n            ],\n            [\n              -155.3404998779297,\n              19.711768236041355\n            ],\n            [\n              -155.3404998779297,\n              19.930104752803004\n            ],\n            [\n              -155.64193725585938,\n              19.930104752803004\n            ],\n            [\n              -155.64193725585938,\n              19.711768236041355\n            ]\n          ]\n        ]\n      }\n    }\n  ]\n}","noUsgsAuthors":false,"publicationStatus":"PW","contributors":{"authors":[{"text":"Davis, Dan A.","contributorId":81188,"corporation":false,"usgs":true,"family":"Davis","given":"Dan","email":"","middleInitial":"A.","affiliations":[],"preferred":false,"id":784917,"contributorType":{"id":1,"text":"Authors"},"rank":1},{"text":"Yamanaga, George","contributorId":57117,"corporation":false,"usgs":true,"family":"Yamanaga","given":"George","email":"","affiliations":[{"id":595,"text":"U.S. Geological Survey","active":false,"usgs":true}],"preferred":false,"id":784918,"contributorType":{"id":1,"text":"Authors"},"rank":2}]}}
,{"id":70221064,"text":"70221064 - 1963 - Glaucophane-bearing metamorphic rock types of the Cazadero area, California","interactions":[],"lastModifiedDate":"2021-06-01T16:35:06.232245","indexId":"70221064","displayToPublicDate":"1963-01-01T11:31:12","publicationYear":"1963","noYear":false,"publicationType":{"id":2,"text":"Article"},"publicationSubtype":{"id":10,"text":"Journal Article"},"seriesTitle":{"id":2420,"text":"Journal of Petrology","active":true,"publicationSubtype":{"id":10}},"title":"Glaucophane-bearing metamorphic rock types of the Cazadero area, California","docAbstract":"<p class=\"chapter-para\">A detailed field and laboratory study has been made of a well-exposed glaucophane schist sequence within the Jurassic and Cretaceous Franciscan Formation of northern California. Three types of glaucophane-bearing metamorphic rocks have been distinguished in and around the area of the detailed study. Each is characterized by distinctive textures and mineral assemblages that are interpreted to represent different grades of metamorphism within the glaucophane schist facies.</p><p class=\"chapter-para\">From the combination of small- and large-scale mapping in the area described it is clear that coarsely schistose blocks, tens of feet in diameter, commonly rest directly upon and within less intensely metamorphosed terrain. In the Cazadero area these isolated blocks of coarsely crystalline rocks are concentrated in a band that is roughly concordant with some of the major faulting, and their metamorphic fabric shows no consistent relation to local or regional structures. It is tentatively suggested that these blocks have been transported upward tectonically and that they are not stratigraphically equivalent to the other types of glaucophane-bearing metamorphic rocks in the area.</p><p class=\"chapter-para\">Chemical and petrographic evidence indicates that basalt and sediments have been converted to glaucophane-bearing rocks under conditions of metamorphism that were essentially isochemical, except for fugitive components and some minor elements.</p>","language":"English","publisher":"Oxford University Press","doi":"10.1093/petrology/4.2.260","usgsCitation":"Coleman, R.G., and Lee, D.E., 1963, Glaucophane-bearing metamorphic rock types of the Cazadero area, California: Journal of Petrology, v. 4, no. 2, p. 260-301, https://doi.org/10.1093/petrology/4.2.260.","productDescription":"42 p.","startPage":"260","endPage":"301","costCenters":[],"links":[{"id":386036,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/thumbnails/outside_thumb.jpg"}],"country":"United  States","state":"California","otherGeospatial":"Cazadero area","geographicExtents":"{\n  \"type\": \"FeatureCollection\",\n  \"features\": [\n    {\n      \"type\": \"Feature\",\n      \"properties\": {},\n      \"geometry\": {\n        \"type\": \"Polygon\",\n        \"coordinates\": [\n          [\n            [\n              -123.1787109375,\n              38.44390909175749\n            ],\n            [\n              -122.77084350585938,\n              38.44390909175749\n            ],\n            [\n              -122.77084350585938,\n              38.72623322072787\n            ],\n            [\n              -123.1787109375,\n              38.72623322072787\n            ],\n            [\n              -123.1787109375,\n              38.44390909175749\n            ]\n          ]\n        ]\n      }\n    }\n  ]\n}","volume":"4","issue":"2","noUsgsAuthors":false,"publicationStatus":"PW","contributors":{"authors":[{"text":"Coleman, R. G.","contributorId":75170,"corporation":false,"usgs":true,"family":"Coleman","given":"R.","email":"","middleInitial":"G.","affiliations":[],"preferred":false,"id":816678,"contributorType":{"id":1,"text":"Authors"},"rank":1},{"text":"Lee, D. E.","contributorId":96705,"corporation":false,"usgs":true,"family":"Lee","given":"D.","email":"","middleInitial":"E.","affiliations":[],"preferred":false,"id":816679,"contributorType":{"id":1,"text":"Authors"},"rank":2}]}}
,{"id":70274625,"text":"70274625 - 1963 - Hawaiian Volcano Observatory record book 1963","interactions":[],"lastModifiedDate":"2026-04-17T14:55:37.597774","indexId":"70274625","displayToPublicDate":"1963-01-01T10:51:47","publicationYear":"1963","noYear":false,"publicationType":{"id":18,"text":"Report"},"publicationSubtype":{"id":3,"text":"Organization Series"},"title":"Hawaiian Volcano Observatory record book 1963","docAbstract":"<p>The Hawaiian Volcano Observatory (HVO) record books are annual journals in which field observations of eruptive activity at Kīlauea and Mauna Loa volcanoes, on the Island of Hawaiʻi, were compiled by HVO staff for most years from 1912 through early 1966. In addition to descriptive observations, the record books also contain hundreds of annotated photographs and sketches, as well as temperature and transit measurements. When photographs are included, the camera settings and film types used are noted. The field notes, sketches, and photographs used to compile the record books provide an unparalleled record of eruptive activity and were the basis for published newspaper reports and periodic bulletins, such as the <a href=\"../publication/70268164\" data-mce-href=\"../publication/70268164\">Hawaiian Volcano Observatory bulletins</a> and <a href=\"../publication/70246900\" data-mce-href=\"../publication/70246900\">The volcano letter</a>. &nbsp;</p><p>HVO staff also painstakingly prepared a second copy of each early record book, virtually identical to the original, complete with photographs and sketches. The original version of the record book was kept at HVO, while the duplicate went to the Hawaiian Volcano Research Association, which was created by a group of Honolulu, Hawaiʻi, businessmen to promote HVO’s work. The Hawaiian Volcano Research Association, which dissolved decades ago, held the duplicate books in Honolulu, where they were more readily accessible to the public. After 1923, HVO stopped duplicating the books—at least, no duplicate records for subsequent years have been found. During the decade of the 1940s, preparation of the record books stopped altogether. In 1952, compilation of the record books resumed and continued, with long gaps, until early 1966. Entries in these later volumes are sparse, and these books are little more than photo albums of the episodic eruptions of Kīlauea.&nbsp;</p><p>The original record books were held at HVO and, later, at Hawai‘i Volcanoes National Park. In 1972, the original record books for the years 1912 through 1939 were transferred to the Bishop Museum, in Honolulu, for safekeeping. These record books are now stored in archival boxes at that institution (accession number 172.265). The duplicate set of record books held by the Hawaiian Volcano Research Association were bound into volumes at an unknown date and turned over to the U.S. Geological Survey. This set of record books, spanning 1912 through 1923, is now housed in the rare book room of the U.S. Geological Survey Library in Reston, Virginia (catalog number 220(950) H3d). The record books for 1952 through early 1966 remain in storage at HVO. After 1955, typed annotations were no longer placed in the record books, and only photographs, most with captions, were included. Although the volumes titled “Record Book” end with the 1955 volume, the photograph albums that followed are similar, and the record book designation is retained for simplicity. Note that the photographs in these albums were not all originally arranged in chronological order.&nbsp;</p>","language":"English","publisher":"Hawaiian Volcano Observatory","usgsCitation":"Hawaiian Volcano Observatory, 1963, Hawaiian Volcano Observatory record book 1963, 14 p.","productDescription":"14 p.","costCenters":[{"id":336,"text":"Hawaiian Volcano Observatory","active":false,"usgs":true}],"links":[{"id":503196,"rank":2,"type":{"id":11,"text":"Document"},"url":"https://pubs.usgs.gov/unnumbered/70274625/report.pdf","linkFileType":{"id":1,"text":"pdf"}},{"id":503195,"rank":1,"type":{"id":22,"text":"Related Work"},"url":"https://pubs.usgs.gov/publication/70274518","text":"Hawaiian Volcano Observatory record books"},{"id":503197,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/thumbnails/outside_thumb.jpg"}],"country":"United 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,{"id":70263266,"text":"wdrCA632 - 1963 - Surface water records of California, 1963; Volume 2: Northern Great Basin and Central Valley","interactions":[],"lastModifiedDate":"2025-02-14T15:46:09.61915","indexId":"wdrCA632","displayToPublicDate":"1963-01-01T10:45:35","publicationYear":"1963","noYear":false,"publicationType":{"id":18,"text":"Report"},"publicationSubtype":{"id":5,"text":"USGS Numbered Series"},"seriesTitle":{"id":340,"text":"Water Data Report","code":"WDR","active":false,"publicationSubtype":{"id":5}},"seriesNumber":"CA-63-2","title":"Surface water records of California, 1963; Volume 2: Northern Great Basin and Central Valley","docAbstract":"<p>The surface-water records for the 1963 water year for gaging stations, partial-record stations, and miscellaneous sites within the State of California are given in this report. For convenience there are also included records for a few pertinent gaging stations in bordering States. The records were collected and computed by the Water Resources Division of the U.S. Geological Survey, under the direction of Walter Hofmann, district engineer. Surface Water Branch.</p><p>Through September 30, 1960, the records of discharge and stage of streams and contents and stage of lakes or reservoirs were published in an annual series of U.S. Geological Survey water-supply papers entitled \"Surface Water Supply of the United States.\" Since 1951 there have been 20 volumes in the series; each volume covered an area whose boundaries coincided with those of certain natural drainage areas. The records in California were contained in parts 9, 10, and 11 of that series.</p><p>Beginning with the 1961 water year, streamflow records and related data are being released by the Geological Survey in annual reports on a State-boundary basis. Distribution of these basic data reports is limited and primarily for local needs. The records later will be published in Geological Survey water-supply papers at 5-year intervals. These 5-year water-supply papers will show daily discharge and will be compiled on the same geographical areas Previously used for the annual series; however, some of the 14 Parts of conterminous United States will be further subdivided.</p>","language":"English","publisher":"U.S. Geological Survey","doi":"10.3133/wdrCA632","collaboration":"Prepared in cooperation with the State of California and with other agencies","usgsCitation":"Water Resources Division, U.S. Geological Survey, 1963, Surface water records of California, 1963; Volume 2: Northern Great Basin and Central Valley: U.S. Geological Survey Water Data Report CA-63-2, xiii, 465-938 p., https://doi.org/10.3133/wdrCA632.","productDescription":"xiii, 465-938 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,{"id":1686,"text":"1686 - 1963 - Dispersion in natural streams","interactions":[],"lastModifiedDate":"2022-08-17T19:54:23.991124","indexId":"1686","displayToPublicDate":"1963-01-01T10:28:08","publicationYear":"1963","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":"Dispersion in natural streams","docAbstract":"<p>Eleven tests were conducted to study the dispersion patterns of a radiotracer in five natural stream channels and in one canal. The radiotracer was injected as a line source. The patterns of dispersion that were observed in these channels were compared with patterns predicted by the theoretical models for one-dimensional flow developed by Taylor and other investigators. Analysis of the relation between time and concentration of the tracer at several sections in each of the six reaches shows that the available theoretical models are not adequate to describe the dispersion patterns actually observed. Dispersion coefficients determined from the test data are from 2 to 30 times greater than those predicted by the theoretical models. It is apparent that a better understanding of the dispersal phenomenon is needed in order to predict dispersion patterns in natural streams. </p>","language":"English","publisher":"U.S. Geological Survey,","publisherLocation":"Washington, D.C.","doi":"10.3133/1686","collaboration":"Prepared in cooperation with the United States Atomic Energy Commission","usgsCitation":"Godfrey, R.G., and Frederick, B.J., 1963, Dispersion in natural streams: Open-File Report, viii, 75 p., https://doi.org/10.3133/1686.","productDescription":"viii, 75 p.","numberOfPages":"83","costCenters":[],"links":[{"id":405280,"rank":2,"type":{"id":11,"text":"Document"},"url":"https://pubs.usgs.gov/unnumbered/1686/report.pdf","linkFileType":{"id":1,"text":"pdf"}},{"id":289868,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/unnumbered/1686/report-thumb.jpg"}],"noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"53c4fc0ce4b0b58d96eeb581","contributors":{"authors":[{"text":"Godfrey, Richard G.","contributorId":100046,"corporation":false,"usgs":true,"family":"Godfrey","given":"Richard","email":"","middleInitial":"G.","affiliations":[],"preferred":false,"id":143970,"contributorType":{"id":1,"text":"Authors"},"rank":1},{"text":"Frederick, Bernard J.","contributorId":106808,"corporation":false,"usgs":true,"family":"Frederick","given":"Bernard","email":"","middleInitial":"J.","affiliations":[],"preferred":false,"id":143971,"contributorType":{"id":1,"text":"Authors"},"rank":2}]}}
,{"id":70227487,"text":"70227487 - 1963 - Salt anticlines of the Paradox Basin","interactions":[],"lastModifiedDate":"2022-01-19T17:52:47.815094","indexId":"70227487","displayToPublicDate":"1963-01-01T10:21:54","publicationYear":"1963","noYear":false,"publicationType":{"id":24,"text":"Conference Paper"},"publicationSubtype":{"id":19,"text":"Conference Paper"},"title":"Salt anticlines of the Paradox Basin","docAbstract":"<p>No abstract available.</p>","largerWorkType":{"id":4,"text":"Book"},"largerWorkTitle":"Symposium on salt: Geology, mining, evaporated salt, solution mining, underground storage","largerWorkSubtype":{"id":12,"text":"Conference publication"},"conferenceTitle":"First Salt Symposium","conferenceDate":"May, 1962","conferenceLocation":"Cleveland, Ohio","language":"English","publisher":"Northern Ohio Geological Society","usgsCitation":"Elston, D.P., and Shoemaker, E.M., 1963, Salt anticlines of the Paradox Basin, <i>in</i> Symposium on salt: Geology, mining, evaporated salt, solution mining, underground storage, v. 1, Cleveland, Ohio, May, 1962, p. 131-146.","productDescription":"16 p.","startPage":"131","endPage":"146","costCenters":[],"links":[{"id":394519,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/thumbnails/outside_thumb.jpg"}],"country":"United States","state":"Colorado, Utah","otherGeospatial":"Paradox Basin","geographicExtents":"{\n  \"type\": \"FeatureCollection\",\n  \"features\": [\n    {\n      \"type\": \"Feature\",\n      \"properties\": {},\n      \"geometry\": {\n        \"type\": \"Polygon\",\n        \"coordinates\": [\n          [\n            [\n              -107.89672851562499,\n              37.3002752813443\n            ],\n            [\n              -108.028564453125,\n              38.39764411353178\n            ],\n            [\n              -110.81359863281249,\n              39.80431612840032\n            ],\n            [\n              -110.76416015625,\n              38.41055825094609\n            ],\n            [\n              -110.863037109375,\n              37.155938651244625\n            ],\n            [\n              -109.09423828125,\n              36.94989178681327\n            ],\n            [\n              -107.89672851562499,\n              37.3002752813443\n            ]\n          ]\n        ]\n      }\n    }\n  ]\n}","volume":"1","noUsgsAuthors":false,"publicationStatus":"PW","contributors":{"editors":[{"text":"Bersticker, A. C.","contributorId":271202,"corporation":false,"usgs":false,"family":"Bersticker","given":"A.","email":"","middleInitial":"C.","affiliations":[],"preferred":false,"id":831166,"contributorType":{"id":2,"text":"Editors"},"rank":1},{"text":"Hoekstra, K. E.","contributorId":271203,"corporation":false,"usgs":false,"family":"Hoekstra","given":"K.","email":"","middleInitial":"E.","affiliations":[],"preferred":false,"id":831167,"contributorType":{"id":2,"text":"Editors"},"rank":2},{"text":"Hall, J. F.","contributorId":41606,"corporation":false,"usgs":true,"family":"Hall","given":"J.","email":"","middleInitial":"F.","affiliations":[],"preferred":false,"id":831168,"contributorType":{"id":2,"text":"Editors"},"rank":3}],"authors":[{"text":"Elston, Donald Parker","contributorId":38150,"corporation":false,"usgs":true,"family":"Elston","given":"Donald","email":"","middleInitial":"Parker","affiliations":[],"preferred":false,"id":831155,"contributorType":{"id":1,"text":"Authors"},"rank":1},{"text":"Shoemaker, Eugene Merle","contributorId":20342,"corporation":false,"usgs":true,"family":"Shoemaker","given":"Eugene","email":"","middleInitial":"Merle","affiliations":[],"preferred":false,"id":831156,"contributorType":{"id":1,"text":"Authors"},"rank":2}]}}
,{"id":70168617,"text":"70168617 - 1963 - Cedar River basin floods","interactions":[],"lastModifiedDate":"2021-04-07T14:11:13.515477","indexId":"70168617","displayToPublicDate":"1963-01-01T10:15:00","publicationYear":"1963","noYear":false,"publicationType":{"id":18,"text":"Report"},"publicationSubtype":{"id":2,"text":"State or Local Government Series"},"seriesTitle":{"id":105,"text":"Bulletin","active":false,"publicationSubtype":{"id":2}},"seriesNumber":"27","title":"Cedar River basin floods","docAbstract":"<p>No abstract available</p>","language":"English","publisher":"U.S. Geological Survey","publisherLocation":"Iowa City","collaboration":"Ames, Iowa Department of Transportation, Iowa Highway Research Board","usgsCitation":"Schwob, H., 1963, Cedar River basin floods: Bulletin 27, 59 p.","productDescription":"59 p.","numberOfPages":"59","onlineOnly":"N","additionalOnlineFiles":"N","costCenters":[{"id":351,"text":"Iowa Water Science 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,{"id":1486,"text":"1486 - 1963 - Papers presented at the Texas District Conference, Austin, Texas, June 24-27, 1963","interactions":[],"lastModifiedDate":"2014-07-14T08:44:09","indexId":"1486","displayToPublicDate":"1963-01-01T08:43:28","publicationYear":"1963","noYear":false,"publicationType":{"id":18,"text":"Report"},"publicationSubtype":{"id":6,"text":"USGS Unnumbered Series"},"title":"Papers presented at the Texas District Conference, Austin, Texas, June 24-27, 1963","docAbstract":"No abstract available.","language":"English","publisher":"U.S. Geological Survey","publisherLocation":"Austin, TX","doi":"10.3133/1486","usgsCitation":"Water Resources Division, U.S. Geological Survey, 1963, Papers presented at the Texas District Conference, Austin, Texas, June 24-27, 1963, i, 134 p., https://doi.org/10.3133/1486.","productDescription":"i, 134 p.","numberOfPages":"135","costCenters":[],"links":[{"id":289833,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/thumbnails/usgs_thumb.jpg"}],"noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"53c4fc61e4b0b58d96eeb5f2","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":527860,"contributorType":{"id":1,"text":"Authors"},"rank":1}]}}
,{"id":70198450,"text":"wsp15361 - 1963 - Estimating the transmissibility of aquifers from the specific capacity of wells","interactions":[],"lastModifiedDate":"2023-08-18T11:36:57.75017","indexId":"wsp15361","displayToPublicDate":"1963-01-01T08:31:52","publicationYear":"1963","noYear":false,"publicationType":{"id":18,"text":"Report"},"publicationSubtype":{"id":5,"text":"USGS Numbered Series"},"seriesTitle":{"id":341,"text":"Water Supply Paper","code":"WSP","active":false,"publicationSubtype":{"id":5}},"seriesNumber":"1536","chapter":"1","title":"Estimating the transmissibility of aquifers from the specific capacity of wells","docAbstract":"<p>No abstract available</p>","language":"English","publisher":"U.S. Geological Survey","doi":"10.3133/wsp15361","usgsCitation":"Theis, C.V., Brown, R.H., and Meyer, R.R., 1963, Estimating the transmissibility of aquifers from the specific capacity of wells: U.S. Geological Survey Water Supply Paper 1536, 10 p., https://doi.org/10.3133/wsp15361.","productDescription":"10 p.","startPage":"331","endPage":"340","costCenters":[],"links":[{"id":356127,"rank":2,"type":{"id":11,"text":"Document"},"url":"https://pubs.usgs.gov/wsp/1536i/report.pdf"},{"id":356238,"rank":1,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/thumbnails/usgs_thumb.jpg"}],"noUsgsAuthors":false,"publicationStatus":"PW","contributors":{"authors":[{"text":"Theis, Charles V.","contributorId":48080,"corporation":false,"usgs":true,"family":"Theis","given":"Charles","email":"","middleInitial":"V.","affiliations":[],"preferred":false,"id":741488,"contributorType":{"id":1,"text":"Authors"},"rank":1},{"text":"Brown, Russell H.","contributorId":106151,"corporation":false,"usgs":true,"family":"Brown","given":"Russell","email":"","middleInitial":"H.","affiliations":[],"preferred":false,"id":741489,"contributorType":{"id":1,"text":"Authors"},"rank":2},{"text":"Meyer, R. R.","contributorId":20725,"corporation":false,"usgs":true,"family":"Meyer","given":"R.","email":"","middleInitial":"R.","affiliations":[],"preferred":false,"id":741490,"contributorType":{"id":1,"text":"Authors"},"rank":3}]}}
,{"id":70221109,"text":"70221109 - 1963 - The peg claims spodumene pegmatites, Maine","interactions":[],"lastModifiedDate":"2021-06-02T12:49:55.069107","indexId":"70221109","displayToPublicDate":"1963-01-01T07:45:25","publicationYear":"1963","noYear":false,"publicationType":{"id":2,"text":"Article"},"publicationSubtype":{"id":10,"text":"Journal Article"},"seriesTitle":{"id":1472,"text":"Economic Geology","active":true,"publicationSubtype":{"id":10}},"title":"The peg claims spodumene pegmatites, Maine","docAbstract":"<p><span>The&nbsp;</span><span class=\"ScopusTermHighlight\">Peg</span><span>&nbsp;</span><span class=\"ScopusTermHighlight\">Claims</span><span>&nbsp;</span><span class=\"ScopusTermHighlight\">pegmatites</span><span>&nbsp;are located southwest of Rockland in the towns of Warren and Cushing, Knox County,&nbsp;</span><span class=\"ScopusTermHighlight\">Maine</span><span>. These&nbsp;</span><span class=\"ScopusTermHighlight\">pegmatites</span><span>&nbsp;are representative of a group of zoned, granitic, lithium-bearing&nbsp;</span><span class=\"ScopusTermHighlight\">pegmatites</span><span>&nbsp;in which&nbsp;</span><span class=\"ScopusTermHighlight\">spodumene</span><span>&nbsp;is present nearly from wall to wall. The&nbsp;</span><span class=\"ScopusTermHighlight\">pegmatites</span><span>&nbsp;are discordant, steeply dipping, tabular bodies in the Penobscot quartz-mica schist near the Waldoboro granite. A narrow quartz-tourmaline-muscovite-apatite aureole is commonly developed around each of the&nbsp;</span><span class=\"ScopusTermHighlight\">pegmatites</span><span>&nbsp;and around inclusions of country rock in the&nbsp;</span><span class=\"ScopusTermHighlight\">pegmatites</span><span>. The&nbsp;</span><span class=\"ScopusTermHighlight\">pegmatites</span><span>&nbsp;are zoned, and each may be subdivided into: (1) a narrow quartz-muscovite border zone; (2) a narrow albite-quartz-muscovite wall zone; (3) and an albite-quartz-</span><span class=\"ScopusTermHighlight\">spodumene</span><span>-perthite core that constitutes most of the&nbsp;</span><span class=\"ScopusTermHighlight\">pegmatite</span><span>. Cross-cutting, fine-grained, quartz-albite-</span><span class=\"ScopusTermHighlight\">spodumene</span><span>-muscovite lenses are found within&nbsp;</span><span class=\"ScopusTermHighlight\">pegmatite</span><span>&nbsp;cores. The bulk mineralogy and variations in the mineralogy from zone to zone of the largest body (Dike 1) were determined by megascopic mineral point-counts. There is a decrease of albite, quartz, and muscovite and an increase of&nbsp;</span><span class=\"ScopusTermHighlight\">spodumene</span><span>&nbsp;and perthite from the border and wall zones into the core. The alkali contents of Dike 1 and of each of its zones were determined by flame photometer and X-ray fluorescence analyses. The amount of Na20 decreases and the amounts of K&nbsp;</span><sub>2</sub><span>O, Li&nbsp;</span><sub>2</sub><span>0, Rb&nbsp;</span><sub>2</sub><span>0, and CS&nbsp;</span><sub>2</sub><span>O increase from the border and wall zones into the core. Estimated bulk compositions of Dike 1 and of each of its zones were computed. It is concluded that the distribution, structural features, bulk chemistry, and the mineralogical, chemical, and textural zoning of the&nbsp;</span><span class=\"ScopusTermHighlight\">pegmatites</span><span>&nbsp;are consistent with development by fractional crystallization of a pegma-titic fluid in a restricted system.</span></p>","language":"English","publisher":"Society of Economic Geologists","doi":"10.2113/gsecongeo.58.1.84","usgsCitation":"Sundelius, H., 1963, The peg claims spodumene pegmatites, Maine: Economic Geology, v. 58, no. 1, p. 84-106, https://doi.org/10.2113/gsecongeo.58.1.84.","productDescription":"23 p.","startPage":"84","endPage":"106","costCenters":[],"links":[{"id":386118,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/thumbnails/outside_thumb.jpg"}],"country":"United  States","state":"Maine","geographicExtents":"{\n  \"type\": \"FeatureCollection\",\n  \"features\": [\n    {\n      \"type\": \"Feature\",\n      \"properties\": {},\n      \"geometry\": {\n        \"type\": \"Polygon\",\n        \"coordinates\": [\n          [\n            [\n              -68.15917968749999,\n              47.3834738721015\n            ],\n            [\n              -68.92822265625,\n              47.204642388766935\n            ],\n            [\n              -69.01611328125,\n              47.39834920035926\n            ],\n            [\n              -69.27978515625,\n              47.502358951968574\n            ],\n            [\n              -69.98291015625,\n              46.7248003746672\n            ],\n            [\n              -70.048828125,\n              46.40756396630067\n            ],\n            [\n              -70.33447265624999,\n              46.17983040759436\n            ],\n            [\n              -70.77392578125,\n              45.506346901083425\n            ],\n            [\n              -70.99365234375,\n              45.336701909968134\n            ],\n            [\n              -70.99365234375,\n              43.32517767999296\n            ],\n            [\n              -70.72998046875,\n              43.100982876188546\n            ],\n            [\n              -70.400390625,\n              43.37311218382002\n            ],\n            [\n              -69.12597656249999,\n              44.008620115415354\n            ],\n            [\n              -66.99462890625,\n              44.63739123445585\n            ],\n            [\n              -66.81884765625,\n              44.77793589631623\n            ],\n            [\n              -67.21435546875,\n              45.22848059584359\n            ],\n            [\n              -67.74169921875,\n              47.08508535995386\n            ],\n            [\n              -68.15917968749999,\n              47.3834738721015\n            ]\n          ]\n        ]\n      }\n    }\n  ]\n}","volume":"58","issue":"1","noUsgsAuthors":false,"publicationDate":"1963-01-01","publicationStatus":"PW","contributors":{"authors":[{"text":"Sundelius, H. W.","contributorId":44511,"corporation":false,"usgs":true,"family":"Sundelius","given":"H. W.","affiliations":[],"preferred":false,"id":816787,"contributorType":{"id":1,"text":"Authors"},"rank":1}]}}
,{"id":70009994,"text":"70009994 - 1963 - Releasing-addition method for the flame-photometric determination of calcium in thermal waters","interactions":[],"lastModifiedDate":"2020-11-19T17:52:04.214257","indexId":"70009994","displayToPublicDate":"1963-01-01T00:00:00","publicationYear":"1963","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":"Releasing-addition method for the flame-photometric determination of calcium in thermal waters","docAbstract":"<p><span>Study of the interferences of silica and sulfate in the flame-photometric determination of calcium in thermal waters has led to the development of a method requiring no prior chemical separations. The interference effects of silica, sulfate, potassium, sodium, aluminum, and phosphate are overcome by an addition technique coupled with the use of magnesium as a releasing agent.</span></p>","language":"English","publisher":"Elsevier","doi":"10.1016/0016-7037(63)90115-7","usgsCitation":"Rowe, J., 1963, Releasing-addition method for the flame-photometric determination of calcium in thermal waters: Geochimica et Cosmochimica Acta, v. 27, no. 8, p. 915-923, https://doi.org/10.1016/0016-7037(63)90115-7.","productDescription":"9 p.","startPage":"915","endPage":"923","numberOfPages":"9","costCenters":[],"links":[{"id":218692,"rank":0,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/thumbnails/outside_thumb.jpg"}],"volume":"27","issue":"8","noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"505aa6b3e4b0c8380cd84fd3","contributors":{"authors":[{"text":"Rowe, J.J.","contributorId":29460,"corporation":false,"usgs":true,"family":"Rowe","given":"J.J.","affiliations":[],"preferred":false,"id":357610,"contributorType":{"id":1,"text":"Authors"},"rank":1}]}}
,{"id":70010787,"text":"70010787 - 1963 - Boron-oxygen polyanion in the crystal structure of tunellite","interactions":[],"lastModifiedDate":"2020-11-19T19:02:14.950786","indexId":"70010787","displayToPublicDate":"1963-01-01T00:00:00","publicationYear":"1963","noYear":false,"publicationType":{"id":2,"text":"Article"},"publicationSubtype":{"id":10,"text":"Journal Article"},"seriesTitle":{"id":3338,"text":"Science","active":true,"publicationSubtype":{"id":10}},"title":"Boron-oxygen polyanion in the crystal structure of tunellite","docAbstract":"<p><span>The crystal structure of tunellite, SrO·3B</span><sub>2</sub><span>O</span><sub>3</sub><span>·4H</span><sub>2</sub><span>O, with infinite sheets of composition n[B</span><sub>6</sub><span>O</span><sub>9</sub><span>(OH)</span><sub>2</sub><span>]</span><sup>2-</sup><span>, has cations and water molecules in the spaces within the sheets. Adjacent sheets are held together by hydrogen bonding through the water molecules. The boron-oxygen polyanions provide the first example in hydrated borate crystals of one oxygen linked to three borons.</span></p>","language":"English","publisher":"AAAS","doi":"10.1126/science.141.3586.1178","usgsCitation":"Clark, J.R., 1963, Boron-oxygen polyanion in the crystal structure of tunellite: Science, v. 141, no. 3586, p. 1178-1179, https://doi.org/10.1126/science.141.3586.1178.","productDescription":"2 p.","startPage":"1178","endPage":"1179","numberOfPages":"2","costCenters":[],"links":[{"id":218663,"rank":0,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/thumbnails/outside_thumb.jpg"}],"volume":"141","issue":"3586","noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"5059f222e4b0c8380cd4b015","contributors":{"authors":[{"text":"Clark, J. R.","contributorId":55764,"corporation":false,"usgs":true,"family":"Clark","given":"J.","email":"","middleInitial":"R.","affiliations":[],"preferred":false,"id":359647,"contributorType":{"id":1,"text":"Authors"},"rank":1}]}}
,{"id":2600,"text":"wsp1539V - 1963 - Availability of ground water in the Bear River valley, Wyoming, with a section on the chemical quality of the water","interactions":[],"lastModifiedDate":"2023-11-01T21:34:49.498797","indexId":"wsp1539V","displayToPublicDate":"1963-01-01T00:00:00","publicationYear":"1963","noYear":false,"publicationType":{"id":18,"text":"Report"},"publicationSubtype":{"id":5,"text":"USGS Numbered Series"},"seriesTitle":{"id":341,"text":"Water Supply Paper","code":"WSP","active":false,"publicationSubtype":{"id":5}},"seriesNumber":"1539","chapter":"V","title":"Availability of ground water in the Bear River valley, Wyoming, with a section on the chemical quality of the water","docAbstract":"<p>No abstract available.</p>","language":"English","publisher":"U.S. Geological Survey","doi":"10.3133/wsp1539V","usgsCitation":"Robinove, C.J., Berry, D.W., and Connor, J.G., 1963, Availability of ground water in the Bear River valley, Wyoming, with a section on the chemical quality of the water: U.S. Geological Survey Water Supply Paper 1539, Report: iv, 44 p.; 2 Plates: 25.00 x 42.75 inches and 27.00 x 11.88 inches, https://doi.org/10.3133/wsp1539V.","productDescription":"Report: iv, 44 p.; 2 Plates: 25.00 x 42.75 inches and 27.00 x 11.88 inches","costCenters":[],"links":[{"id":422319,"rank":5,"type":{"id":36,"text":"NGMDB Index Page"},"url":"https://ngmdb.usgs.gov/Prodesc/proddesc_24743.htm","linkFileType":{"id":5,"text":"html"}},{"id":28882,"rank":2,"type":{"id":11,"text":"Document"},"url":"https://pubs.usgs.gov/wsp/1539v/report.pdf","linkFileType":{"id":1,"text":"pdf"}},{"id":28881,"rank":4,"type":{"id":17,"text":"Plate"},"url":"https://pubs.usgs.gov/wsp/1539v/plate-2.pdf","linkFileType":{"id":1,"text":"pdf"}},{"id":28880,"rank":3,"type":{"id":17,"text":"Plate"},"url":"https://pubs.usgs.gov/wsp/1539v/plate-1.pdf","linkFileType":{"id":1,"text":"pdf"}},{"id":138893,"rank":1,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/wsp/1539v/report-thumb.jpg"}],"country":"United States","state":"Wyoming","otherGeospatial":"Bear River Valley","geographicExtents":"{\n  \"type\": \"FeatureCollection\",\n  \"features\": [\n    {\n      \"type\": \"Feature\",\n      \"properties\": {},\n      \"geometry\": {\n        \"coordinates\": [\n          [\n            [\n              -110.8033,\n              42.221\n            ],\n            [\n              -111.048,\n              42.221\n            ],\n            [\n              -111.048,\n              41\n            ],\n            [\n              -110.8033,\n              41\n            ],\n            [\n              -110.8033,\n              42.221\n            ]\n          ]\n        ],\n        \"type\": \"Polygon\"\n      }\n    }\n  ]\n}","noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"4f4e4a9ee4b07f02db66035d","contributors":{"authors":[{"text":"Robinove, Charles Joseph","contributorId":71153,"corporation":false,"usgs":true,"family":"Robinove","given":"Charles","email":"","middleInitial":"Joseph","affiliations":[],"preferred":false,"id":145473,"contributorType":{"id":1,"text":"Authors"},"rank":1},{"text":"Berry, Delmar W.","contributorId":25107,"corporation":false,"usgs":true,"family":"Berry","given":"Delmar","email":"","middleInitial":"W.","affiliations":[],"preferred":false,"id":145472,"contributorType":{"id":1,"text":"Authors"},"rank":2},{"text":"Connor, John G.","contributorId":34489,"corporation":false,"usgs":true,"family":"Connor","given":"John","email":"","middleInitial":"G.","affiliations":[],"preferred":false,"id":887319,"contributorType":{"id":1,"text":"Authors"},"rank":3}]}}
,{"id":34618,"text":"b1141K - 1963 - Geology of the Clark Fork quadrangle, Idaho-Montana","interactions":[],"lastModifiedDate":"2023-03-09T20:14:25.842564","indexId":"b1141K","displayToPublicDate":"1963-01-01T00:00:00","publicationYear":"1963","noYear":false,"publicationType":{"id":18,"text":"Report"},"publicationSubtype":{"id":5,"text":"USGS Numbered Series"},"seriesTitle":{"id":306,"text":"Bulletin","code":"B","active":false,"publicationSubtype":{"id":5}},"seriesNumber":"1141","chapter":"K","title":"Geology of the Clark Fork quadrangle, Idaho-Montana","docAbstract":"<p>No abstract available.</p>","language":"English","publisher":"U.S. Geological Survey","doi":"10.3133/b1141K","usgsCitation":"Harrison, J.E., and Jobin, D.A., 1963, Geology of the Clark Fork quadrangle, Idaho-Montana: U.S. Geological Survey Bulletin 1141, Report: iv, 38 p.; 2 Plates: 23.19 x 29.50 inches and 10.26 x 23.12 inches, https://doi.org/10.3133/b1141K.","productDescription":"Report: iv, 38 p.; 2 Plates: 23.19 x 29.50 inches and 10.26 x 23.12 inches","costCenters":[],"links":[{"id":109399,"rank":5,"type":{"id":36,"text":"NGMDB Index Page"},"url":"https://ngmdb.usgs.gov/Prodesc/proddesc_20869.htm","linkFileType":{"id":5,"text":"html"},"description":"20869"},{"id":92862,"rank":4,"type":{"id":17,"text":"Plate"},"url":"https://pubs.usgs.gov/bul/1141k/plate-2.pdf","linkFileType":{"id":1,"text":"pdf"}},{"id":92861,"rank":3,"type":{"id":17,"text":"Plate"},"url":"https://pubs.usgs.gov/bul/1141k/plate-1.pdf","linkFileType":{"id":1,"text":"pdf"}},{"id":92863,"rank":2,"type":{"id":11,"text":"Document"},"url":"https://pubs.usgs.gov/bul/1141k/report.pdf","linkFileType":{"id":1,"text":"pdf"}},{"id":166929,"rank":1,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/bul/1141k/report-thumb.jpg"}],"country":"United States","state":"Idaho,Montana","otherGeospatial":"Clark Fork quadrangle","geographicExtents":"{\n  \"type\": \"FeatureCollection\",\n  \"features\": [\n    {\n      \"type\": \"Feature\",\n      \"properties\": {},\n      \"geometry\": {\n        \"coordinates\": [\n          [\n            [\n              -116.25,\n              48.25\n            ],\n            [\n              -116.25,\n              48\n            ],\n            [\n              -116,\n              48\n            ],\n            [\n              -116,\n              48.25\n            ],\n            [\n              -116.25,\n              48.25\n            ]\n          ]\n        ],\n        \"type\": \"Polygon\"\n      }\n    }\n  ]\n}","noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"4f4e4ad4e4b07f02db683132","contributors":{"authors":[{"text":"Harrison, Jack Edward","contributorId":49778,"corporation":false,"usgs":true,"family":"Harrison","given":"Jack","email":"","middleInitial":"Edward","affiliations":[],"preferred":false,"id":213272,"contributorType":{"id":1,"text":"Authors"},"rank":1},{"text":"Jobin, Daniel Alfred","contributorId":32587,"corporation":false,"usgs":true,"family":"Jobin","given":"Daniel","email":"","middleInitial":"Alfred","affiliations":[],"preferred":false,"id":213271,"contributorType":{"id":1,"text":"Authors"},"rank":2}]}}
,{"id":70010443,"text":"70010443 - 1963 - Deuterium in Iceland waters","interactions":[],"lastModifiedDate":"2020-11-19T18:02:36.570759","indexId":"70010443","displayToPublicDate":"1963-01-01T00:00:00","publicationYear":"1963","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":"Deuterium in Iceland waters","docAbstract":"<p><span>From the deuterium analysis of 159 samples of water collected in Iceland from hot-water boreholes, cold and hot springs, rivers and rain, the geographical distribution of deuterium in surface waters is plotted. On the basis of the deuterium analysis, the water from boreholes near Reykjavik does not originate from local precipitation. The variation of deuterium content of these water wells with time suggests that these data can be used to determine the time of travel of recharge water to the various boreholes, as well as the surface recharge area.</span></p>","language":"English","publisher":"Elsevier","doi":"10.1016/0016-7037(63)90012-7","usgsCitation":"Friedman, I., Sigurgeirsson, T., and Gardarsson, O., 1963, Deuterium in Iceland waters: Geochimica et Cosmochimica Acta, v. 27, no. 6, p. 553-561, https://doi.org/10.1016/0016-7037(63)90012-7.","productDescription":"9 p.","startPage":"553","endPage":"561","numberOfPages":"9","costCenters":[],"links":[{"id":218722,"rank":0,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/thumbnails/outside_thumb.jpg"}],"country":"Iceland","geographicExtents":"{\n  \"type\": \"FeatureCollection\",\n  \"features\": [\n    {\n      \"type\": \"Feature\",\n      \"properties\": {},\n      \"geometry\": {\n        \"type\": \"Polygon\",\n        \"coordinates\": [\n          [\n            [\n              -13.392333984375,\n              65.10914820386473\n            ],\n            [\n              -13.612060546875,\n              65.53572109366296\n            ],\n            [\n              -14.61181640625,\n              66.10716955858042\n            ],\n            [\n              -14.490966796875,\n              66.39915999849539\n            ],\n            [\n              -16.10595703125,\n              66.57011534897919\n            ],\n            [\n              -18.2373046875,\n              66.25801126452266\n            ],\n            [\n              -19.412841796875,\n              66.2004427049685\n            ],\n            [\n              -22.873535156249996,\n              66.52639234726222\n            ],\n            [\n              -23.741455078125,\n              66.18713899424186\n            ],\n            [\n              -24.67529296875,\n              65.49474141843486\n            ],\n            [\n              -23.719482421875,\n              65.33934745143243\n            ],\n            [\n              -22.873535156249996,\n              65.44913291147593\n            ],\n            [\n              -22.269287109374996,\n              65.39887159286903\n            ],\n            [\n              -22.730712890625,\n              65.21528876017474\n            ],\n            [\n              -24.158935546875,\n              64.9095691859575\n            ],\n            [\n              -23.851318359375,\n              64.64270382119375\n            ],\n            [\n              -22.60986328125,\n              64.71787992684128\n            ],\n            [\n              -22.159423828125,\n              64.20637724320852\n            ],\n            [\n              -22.247314453125,\n              64.11060221954631\n            ],\n            [\n              -22.730712890625,\n              64.11060221954631\n            ],\n            [\n              -22.906494140624996,\n              63.95667333648766\n            ],\n            [\n              -22.785644531249996,\n              63.74363097533544\n            ],\n            [\n              -21.357421875,\n              63.77277727885665\n            ],\n            [\n              -19.962158203125,\n              63.44068640036803\n            ],\n            [\n              -18.599853515625,\n              63.31268278043484\n            ],\n            [\n              -17.435302734375,\n              63.64625919492172\n            ],\n            [\n              -16.424560546875,\n              63.74363097533544\n            ],\n            [\n              -14.501953124999998,\n              64.31611045403284\n            ],\n            [\n              -13.392333984375,\n              65.10914820386473\n            ]\n          ]\n        ]\n      }\n    }\n  ]\n}","volume":"27","issue":"6","noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"505a0004e4b0c8380cd4f536","contributors":{"authors":[{"text":"Friedman, I.","contributorId":95596,"corporation":false,"usgs":true,"family":"Friedman","given":"I.","email":"","affiliations":[],"preferred":false,"id":358939,"contributorType":{"id":1,"text":"Authors"},"rank":1},{"text":"Sigurgeirsson, T.","contributorId":78877,"corporation":false,"usgs":true,"family":"Sigurgeirsson","given":"T.","email":"","affiliations":[],"preferred":false,"id":358938,"contributorType":{"id":1,"text":"Authors"},"rank":2},{"text":"Gardarsson, O.","contributorId":45186,"corporation":false,"usgs":true,"family":"Gardarsson","given":"O.","email":"","affiliations":[],"preferred":false,"id":358937,"contributorType":{"id":1,"text":"Authors"},"rank":3}]}}
,{"id":81380,"text":"81380 - 1963 - Parasites of freshwater fish, I Fungi, Fungi (Saprolegnia and relatives) of fish and fish eggs","interactions":[],"lastModifiedDate":"2012-02-02T00:15:02","indexId":"81380","displayToPublicDate":"1963-01-01T00:00:00","publicationYear":"1963","noYear":false,"publicationType":{"id":18,"text":"Report"},"publicationSubtype":{"id":1,"text":"Federal Government Series"},"seriesTitle":{"id":29,"text":"Fishery Leaflet","active":false,"publicationSubtype":{"id":1}},"seriesNumber":"564","title":"Parasites of freshwater fish, I Fungi, Fungi (Saprolegnia and relatives) of fish and fish eggs","language":"English","publisher":"U.S. Fish and Wildlife Service","collaboration":"705/FH","usgsCitation":"Hoffman, G.L., 1963, Parasites of freshwater fish, I Fungi, Fungi (Saprolegnia and relatives) of fish and fish eggs: Fishery Leaflet 564, 6 p.","productDescription":"6 p.","startPage":"0","endPage":"6","numberOfPages":"6","costCenters":[{"id":365,"text":"Leetown Science Center","active":true,"usgs":true}],"links":[{"id":198183,"rank":0,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/thumbnails/outside_thumb.jpg"}],"noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"4f4e4ae3e4b07f02db689261","contributors":{"authors":[{"text":"Hoffman, G. L.","contributorId":70713,"corporation":false,"usgs":true,"family":"Hoffman","given":"G.","email":"","middleInitial":"L.","affiliations":[],"preferred":false,"id":295310,"contributorType":{"id":1,"text":"Authors"},"rank":1}]}}
,{"id":81383,"text":"81383 - 1963 - Sacramento River chinook disease (SRCD)","interactions":[],"lastModifiedDate":"2012-02-02T00:15:02","indexId":"81383","displayToPublicDate":"1963-01-01T00:00:00","publicationYear":"1963","noYear":false,"publicationType":{"id":18,"text":"Report"},"publicationSubtype":{"id":1,"text":"Federal Government Series"},"seriesTitle":{"id":29,"text":"Fishery Leaflet","active":false,"publicationSubtype":{"id":1}},"seriesNumber":"562","title":"Sacramento River chinook disease (SRCD)","language":"English","publisher":"U.S. Fish and Wildlife Service","collaboration":"759/FH","usgsCitation":"Parisot, T., 1963, Sacramento River chinook disease (SRCD): Fishery Leaflet 562, 2 p.","productDescription":"2 p.","startPage":"0","endPage":"2","numberOfPages":"2","costCenters":[{"id":365,"text":"Leetown Science Center","active":true,"usgs":true}],"links":[{"id":198186,"rank":0,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/thumbnails/outside_thumb.jpg"}],"noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"4f4e4a0ee4b07f02db5fe056","contributors":{"authors":[{"text":"Parisot, T. J.","contributorId":43014,"corporation":false,"usgs":true,"family":"Parisot","given":"T. J.","affiliations":[],"preferred":false,"id":295313,"contributorType":{"id":1,"text":"Authors"},"rank":1}]}}
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