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F.","contributorId":13169,"corporation":false,"usgs":true,"family":"Snieszko","given":"S.","middleInitial":"F.","affiliations":[],"preferred":false,"id":319854,"contributorType":{"id":1,"text":"Authors"},"rank":1}]}}
,{"id":70010602,"text":"70010602 - 1965 - Tectonic deformation associated with the 1964 Alaska earthquake","interactions":[],"lastModifiedDate":"2026-02-11T15:00:12.272329","indexId":"70010602","displayToPublicDate":"1965-06-25T00:00:00","publicationYear":"1965","noYear":false,"publicationType":{"id":2,"text":"Article"},"publicationSubtype":{"id":10,"text":"Journal Article"},"seriesTitle":{"id":3338,"text":"Science","active":true,"publicationSubtype":{"id":10}},"title":"Tectonic deformation associated with the 1964 Alaska earthquake","docAbstract":"<p><span>Alaska's Good Friday earthquake of 27 March 1964 was accompanied by vertical tectonic deformation over an area of 170,000 to 200,000 square kilometers in south-central Alaska. The deformation included two major northeast-trending zones of uplift and subsidence situated between the Aleutian Trench and the Aleutian Volcanic Arc; together they are 700 to 800 kilometers long and from 150 to 250 kilometers wide. The seaward zone is one in which uplift of as much as 10 meters on land and 15 meters on the sea floor has occurred as a result of both crustal warping and local faulting. Submarine uplift within this zone generated a train of seismic sea waves with half-wave amplitudes of more than 7 meters along the coast near the source. The adjacent zone to the northwest is one of subsidence that averages about 1 meter and attains a measured maximum of 2.3 meters. A second zone of slight uplift may exist along all or part of the Aleutian and Alaska ranges northwest of the zone of subsidence.</span></p>","language":"English","publisher":"American Association for the Advancement of Science","doi":"10.1126/science.148.3678.1675","issn":"00368075","usgsCitation":"Plafker, G., 1965, Tectonic deformation associated with the 1964 Alaska earthquake: Science, v. 148, no. 3678, p. 1675-1687, https://doi.org/10.1126/science.148.3678.1675.","productDescription":"13 p.","startPage":"1675","endPage":"1687","costCenters":[],"links":[{"id":219101,"rank":1,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/thumbnails/outside_thumb.jpg"}],"country":"United States","state":"Alaska","otherGeospatial":"Aleutian Trench","geographicExtents":"{\n  \"type\": \"FeatureCollection\",\n  \"features\": [\n    {\n      \"type\": \"Feature\",\n      \"properties\": {},\n      \"geometry\": {\n        \"coordinates\": [\n          [\n            [\n              -179.9,\n              52.89848022223302\n            ],\n            [\n              -179.9,\n              50.34742724365566\n            ],\n            [\n              -165.90072947118094,\n              52.38515601893195\n            ],\n            [\n              -157.1802921694297,\n              54.89759776829018\n            ],\n            [\n              -155.36618380411227,\n              56.73058764922936\n            ],\n            [\n              -158.829392131228,\n              58.11065126044281\n            ],\n            [\n              -172.99044772182424,\n              53.805294237333726\n            ],\n            [\n              -179.9,\n              52.89848022223302\n            ]\n          ]\n        ],\n        \"type\": \"Polygon\"\n      }\n    },\n    {\n      \"type\": \"Feature\",\n      \"properties\": {},\n      \"geometry\": {\n        \"coordinates\": [\n          [\n            [\n              179.9,\n              52.84464206876427\n            ],\n            [\n              172,\n              54.15161662224946\n            ],\n            [\n             172,\n              51.89469832853055\n            ],\n            [\n              179.9,\n              50.32814578749236\n            ],\n            [\n              179.9,\n              52.84464206876427\n            ]\n          ]\n        ],\n        \"type\": \"Polygon\"\n      }\n    }\n  ]\n}","volume":"148","issue":"3678","noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"505ba44ce4b08c986b320232","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":359251,"contributorType":{"id":1,"text":"Authors"},"rank":1}]}}
,{"id":70010832,"text":"70010832 - 1965 - Holocene submergence of the Eastern Shore of Virginia","interactions":[],"lastModifiedDate":"2026-02-10T18:44:41.648721","indexId":"70010832","displayToPublicDate":"1965-06-11T00:00:00","publicationYear":"1965","noYear":false,"publicationType":{"id":2,"text":"Article"},"publicationSubtype":{"id":10,"text":"Journal Article"},"seriesTitle":{"id":3338,"text":"Science","active":true,"publicationSubtype":{"id":10}},"title":"Holocene submergence of the Eastern Shore of Virginia","docAbstract":"Radiocarbon ages of basal peats 4500 years old or younger and the thickness of salt-marsh peat in the lagoon east of Wachapreague, Virginia, are nearly the same as those of equivalent samples from New Jersey and Cape Cod. This suggests that these coasts have had similar submergence histories. Data obtained from the coasts of Connecticut and northeastern Massachusetts indicate that the Atlantic coast of the United States has been differentially warped during the later Holocene.","language":"English","publisher":"American Association for the Advancement of Science","doi":"10.1126/science.148.3676.1464","issn":"00368075","usgsCitation":"Newman, W., and Rusnak, G., 1965, Holocene submergence of the Eastern Shore of Virginia: Science, v. 148, no. 3676, p. 1464-1466, https://doi.org/10.1126/science.148.3676.1464.","productDescription":"3 p.","startPage":"1464","endPage":"1466","costCenters":[],"links":[{"id":218899,"rank":1,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/thumbnails/outside_thumb.jpg"}],"country":"United States","state":"Connecticut, Massachusetts, New Jersey, Virginia","otherGeospatial":"Atlantic coast","geographicExtents":"{\n  \"type\": \"FeatureCollection\",\n  \"features\": [\n    {\n      \"type\": \"Feature\",\n      \"properties\": {},\n      \"geometry\": {\n        \"coordinates\": [\n          [\n            [\n              -71.72870898922105,\n              42.81177931670098\n            ],\n            [\n              -76.07587223384438,\n              42.81177931670098\n            ],\n            [\n              -76.07587223384438,\n              36.4511679954293\n            ],\n            [\n              -71.72870898922105,\n              36.4511679954293\n            ],\n            [\n              -71.72870898922105,\n              42.81177931670098\n            ]\n          ]\n        ],\n        \"type\": \"Polygon\"\n      }\n    }\n  ]\n}","volume":"148","issue":"3676","noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"505a31f6e4b0c8380cd5e3cc","contributors":{"authors":[{"text":"Newman, W.S.","contributorId":12187,"corporation":false,"usgs":true,"family":"Newman","given":"W.S.","email":"","affiliations":[],"preferred":false,"id":359748,"contributorType":{"id":1,"text":"Authors"},"rank":1},{"text":"Rusnak, G.A.","contributorId":80407,"corporation":false,"usgs":true,"family":"Rusnak","given":"G.A.","email":"","affiliations":[],"preferred":false,"id":359749,"contributorType":{"id":1,"text":"Authors"},"rank":2}]}}
,{"id":5210065,"text":"5210065 - 1965 - The occurrence of protozoan blood parasites in Anatidae","interactions":[],"lastModifiedDate":"2020-03-13T12:46:33","indexId":"5210065","displayToPublicDate":"1965-06-09T09:23:16","publicationYear":"1965","noYear":false,"publicationType":{"id":5,"text":"Book chapter"},"publicationSubtype":{"id":24,"text":"Book Chapter"},"title":"The occurrence of protozoan blood parasites in Anatidae","docAbstract":"<p>No abstract available.</p>","largerWorkType":{"id":4,"text":"Book"},"largerWorkTitle":"International Union of Game Biologists, Transactions of the VIth Congress","largerWorkSubtype":{"id":4,"text":"Other Government Series"},"language":"English","publisher":"Nature Conservancy","publisherLocation":"London","collaboration":"OCLC: 2347707","usgsCitation":"Herman, C.M., 1965, The occurrence of protozoan blood parasites in Anatidae, chap. <i>of</i> International Union of Game Biologists, Transactions of the VIth Congress, p. 341-349.","productDescription":"9 p.","startPage":"341","endPage":"349","costCenters":[{"id":531,"text":"Patuxent Wildlife Research Center","active":true,"usgs":true}],"links":[{"id":201284,"rank":0,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/thumbnails/outside_thumb.jpg"}],"noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"4f4e4a80e4b07f02db649407","contributors":{"editors":[{"text":"Blank, T.H.","contributorId":114091,"corporation":false,"usgs":true,"family":"Blank","given":"T.H.","email":"","affiliations":[],"preferred":false,"id":505959,"contributorType":{"id":2,"text":"Editors"},"rank":1}],"authors":[{"text":"Herman, C. M.","contributorId":101335,"corporation":false,"usgs":true,"family":"Herman","given":"C.","email":"","middleInitial":"M.","affiliations":[],"preferred":false,"id":327702,"contributorType":{"id":1,"text":"Authors"},"rank":1}]}}
,{"id":70221190,"text":"70221190 - 1965 - Gamma-ray spectrometer studies of hydro-thermally altered rocks","interactions":[],"lastModifiedDate":"2021-06-04T18:58:38.973435","indexId":"70221190","displayToPublicDate":"1965-06-01T13:55:22","publicationYear":"1965","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":"Gamma-ray spectrometer studies of hydro-thermally altered rocks","docAbstract":"<p><span>The uranium, thorium, and potassium content of hydrothermally&nbsp;</span>altered<span>&nbsp;</span>rocks<span>&nbsp;in the vicinity of several copper and copper-lead-zinc deposits in Arizona was determined by chemical analysis. Potassium in the more intensely&nbsp;</span>altered<span>&nbsp;zones is about twice that in unaltered areas. There is no corresponding increase in thorium, so a higher potassium/thorium ratio also results from alteration; abnormally high uranium, locally in secular disequilibrium, was observed at the Bagdad porphyry copper deposit. A truck-mounted gammarray&nbsp;</span>spectrometer<span>&nbsp;was used to obtain a spectrum of&nbsp;</span>gamma<span>&nbsp;emission at each sample location. Equating the spectrometric with the chemical data gave standard errors of 0.6 percent potassium, 3 ppm thorium, and 10 ppm uranium for the outcrop analyses with the&nbsp;</span>spectrometer<span>. The amount of potassium introduced by hydrothermal alteration is thought sufficient in quantity to be detected by either surface or aerial spectrometry; spectrometric detection of anomalous uranium is probably marginal, owing to the disequilibrium. The potassium/thorium ratio may provide a means of distinguishing, in such surveys, between hydrothermally&nbsp;</span>altered<span>&nbsp;high-potassium zones and unaltered extrinsically high-potassium intrusives.&nbsp;</span></p>","language":"English","publisher":"Society of Economic Geologists","doi":"10.2113/gsecongeo.60.4.653","usgsCitation":"Moxham, R., Foote, R., and Bunker, C.M., 1965, Gamma-ray spectrometer studies of hydro-thermally altered rocks: Economic Geology, v. 60, no. 4, p. 653-671, https://doi.org/10.2113/gsecongeo.60.4.653.","productDescription":"19 p.","startPage":"653","endPage":"671","costCenters":[],"links":[{"id":386235,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/thumbnails/outside_thumb.jpg"}],"volume":"60","issue":"4","noUsgsAuthors":false,"publicationDate":"1965-06-01","publicationStatus":"PW","contributors":{"authors":[{"text":"Moxham, R.M.","contributorId":42234,"corporation":false,"usgs":true,"family":"Moxham","given":"R.M.","email":"","affiliations":[],"preferred":false,"id":817022,"contributorType":{"id":1,"text":"Authors"},"rank":1},{"text":"Foote, R.S.","contributorId":259302,"corporation":false,"usgs":false,"family":"Foote","given":"R.S.","email":"","affiliations":[],"preferred":false,"id":817023,"contributorType":{"id":1,"text":"Authors"},"rank":2},{"text":"Bunker, C. M.","contributorId":75138,"corporation":false,"usgs":true,"family":"Bunker","given":"C.","email":"","middleInitial":"M.","affiliations":[],"preferred":false,"id":817024,"contributorType":{"id":1,"text":"Authors"},"rank":3}]}}
,{"id":70221189,"text":"70221189 - 1965 - Electrochemical geothermometer: A possible new method of geothermometry with electro-conductive minerals","interactions":[],"lastModifiedDate":"2021-06-04T18:30:14.836495","indexId":"70221189","displayToPublicDate":"1965-06-01T13:28:08","publicationYear":"1965","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":"Electrochemical geothermometer: A possible new method of geothermometry with electro-conductive minerals","docAbstract":"<p><span>It was demonstrated with artificially processed sulfides that the minimum temperature of equilibration of&nbsp;</span>a<span>&nbsp;pair of&nbsp;</span>electro<span>-</span>conductive<span>&nbsp;</span>minerals<span>&nbsp;can be determined electrochemically. The procedure consists of setting up an&nbsp;</span>electrochemical<span>&nbsp;cell with the&nbsp;</span>mineral<span>&nbsp;electrodes and&nbsp;</span>a<span>&nbsp;suitable electrolyte, changing the temperature of the cell slowly in&nbsp;</span>a<span>&nbsp;furnace, and finding the temperature at which the emf of the cell becomes zero. The experimental results strongly suggest that this&nbsp;</span>electrochemical<span>&nbsp;</span>method<span>&nbsp;could be used as&nbsp;</span>a<span>&nbsp;</span>new<span>&nbsp;</span>method<span>&nbsp;of&nbsp;</span>geothermometry<span>.&nbsp;</span></p>","language":"English","publisher":"Society of Economic Geologists","doi":"10.2113/gsecongeo.60.4.812","usgsCitation":"Sato, M., 1965, Electrochemical geothermometer: A possible new method of geothermometry with electro-conductive minerals: Economic Geology, v. 60, no. 4, p. 812-818, https://doi.org/10.2113/gsecongeo.60.4.812.","productDescription":"7 p.","startPage":"812","endPage":"818","costCenters":[],"links":[{"id":386234,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/thumbnails/outside_thumb.jpg"}],"volume":"60","issue":"4","noUsgsAuthors":false,"publicationDate":"1965-06-01","publicationStatus":"PW","contributors":{"authors":[{"text":"Sato, M.","contributorId":50201,"corporation":false,"usgs":true,"family":"Sato","given":"M.","email":"","affiliations":[],"preferred":false,"id":817021,"contributorType":{"id":1,"text":"Authors"},"rank":1}]}}
,{"id":70010807,"text":"70010807 - 1965 - Low deuterium content of Lake Vanda, Antarctica","interactions":[],"lastModifiedDate":"2026-02-10T18:50:44.868847","indexId":"70010807","displayToPublicDate":"1965-05-28T00:00:00","publicationYear":"1965","noYear":false,"publicationType":{"id":2,"text":"Article"},"publicationSubtype":{"id":10,"text":"Journal Article"},"seriesTitle":{"id":3338,"text":"Science","active":true,"publicationSubtype":{"id":10}},"title":"Low deuterium content of Lake Vanda, Antarctica","docAbstract":"Lake Vanda in Victoria Land, Antarctica, is permanently ice-covered and permanently stratified, with warm, salty water near the bottom. Deuterium analyses of lake water from several levels indicate that the lake has a low deuterium content, and that it is stratified with respect to this isotope. This low deuterium content supports the evidence from the lake's ionic content that the saline layer is not of marine origin, and it indicates that evaporation from the ice surface has taken place. The stratification of the lake with respect to deuterium suggests that the upper and lower layers of water were formed at different times from different sources of glacial melt water.","language":"English","publisher":"American Association for the Advancement of Science","doi":"10.1126/science.148.3674.1226","issn":"00368075","usgsCitation":"Ragotzkie, R., and Friedman, I., 1965, Low deuterium content of Lake Vanda, Antarctica: Science, v. 148, no. 3674, p. 1226-1227, https://doi.org/10.1126/science.148.3674.1226.","productDescription":"2 p.","startPage":"1226","endPage":"1227","costCenters":[],"links":[{"id":218673,"rank":1,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/thumbnails/outside_thumb.jpg"}],"otherGeospatial":"Lake Vanda, Victoria Land, Antarctica","geographicExtents":"{\n  \"type\": \"FeatureCollection\",\n  \"features\": [\n    {\n      \"type\": \"Feature\",\n      \"properties\": {},\n      \"geometry\": {\n        \"coordinates\": [\n          [\n            [\n              155.94852787212506,\n              -78.21218030941368\n            ],\n            [\n              171.0951946664561,\n              -78.21218030941368\n            ],\n            [\n              171.0951946664561,\n              -75.70367410122311\n            ],\n            [\n              155.94852787212506,\n              -75.70367410122311\n            ],\n            [\n              155.94852787212506,\n              -78.21218030941368\n            ]\n          ]\n        ],\n        \"type\": \"Polygon\"\n      }\n    }\n  ]\n}","volume":"148","issue":"3674","noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"505a4a01e4b0c8380cd68a59","contributors":{"authors":[{"text":"Ragotzkie, R.A.","contributorId":67213,"corporation":false,"usgs":true,"family":"Ragotzkie","given":"R.A.","email":"","affiliations":[],"preferred":false,"id":359691,"contributorType":{"id":1,"text":"Authors"},"rank":1},{"text":"Friedman, I.","contributorId":95596,"corporation":false,"usgs":true,"family":"Friedman","given":"I.","email":"","affiliations":[],"preferred":false,"id":359692,"contributorType":{"id":1,"text":"Authors"},"rank":2}]}}
,{"id":70010597,"text":"70010597 - 1965 - Radiocarbon determinations for estimating groundwater flow velocities in central Florida","interactions":[],"lastModifiedDate":"2026-02-10T21:24:21.878527","indexId":"70010597","displayToPublicDate":"1965-04-23T00:00:00","publicationYear":"1965","noYear":false,"publicationType":{"id":2,"text":"Article"},"publicationSubtype":{"id":10,"text":"Journal Article"},"seriesTitle":{"id":3338,"text":"Science","active":true,"publicationSubtype":{"id":10}},"title":"Radiocarbon determinations for estimating groundwater flow velocities in central Florida","docAbstract":"<p><span id=\"_mce_caret\" data-mce-bogus=\"1\" data-mce-type=\"format-caret\"><span>Carbon-14 activity was determined from HCO</span><sub>3</sub><sup>-</sup><span>&nbsp;in samples of groundwater obtained from the principal artesian aquifer in Florida. From these data the \"age\" of water obtained from a series of wells, each progressively farther down gradient on the piezometric surface, was established. Relative carbon-14 ages indicated a velocity of groundwater movement of 23 feet (7 meters) per year for about 85 miles (137 kilometers) of travel. A velocity of 23 feet per year was calculated independently from Darcy's law.</span></span></p>","language":"English","publisher":"American Association for the Advancement of Science","doi":"10.1126/science.148.3669.494","issn":"00368075","usgsCitation":"Hanshaw, B., Back, W., and Rubin, M., 1965, Radiocarbon determinations for estimating groundwater flow velocities in central Florida: Science, v. 148, no. 3669, p. 494-495, https://doi.org/10.1126/science.148.3669.494.","productDescription":"2 p.","startPage":"494","endPage":"495","costCenters":[],"links":[{"id":219096,"rank":1,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/thumbnails/outside_thumb.jpg"}],"country":"United States","state":"Florida","otherGeospatial":"central Florida","geographicExtents":"{\n  \"type\": \"FeatureCollection\",\n  \"features\": [\n    {\n      \"type\": \"Feature\",\n      \"properties\": {},\n      \"geometry\": {\n        \"coordinates\": [\n          [\n            [\n              -82.9572772353431,\n              29.55750556929405\n            ],\n            [\n              -82.9572772353431,\n              27.102727498933774\n            ],\n            [\n              -80.334695107516,\n              27.102727498933774\n            ],\n            [\n              -80.334695107516,\n              29.55750556929405\n            ],\n            [\n              -82.9572772353431,\n              29.55750556929405\n            ]\n          ]\n        ],\n        \"type\": \"Polygon\"\n      }\n    }\n  ]\n}","volume":"148","issue":"3669","noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"505a93e3e4b0c8380cd810ad","contributors":{"authors":[{"text":"Hanshaw, B.B.","contributorId":25928,"corporation":false,"usgs":true,"family":"Hanshaw","given":"B.B.","email":"","affiliations":[],"preferred":false,"id":359240,"contributorType":{"id":1,"text":"Authors"},"rank":1},{"text":"Back, W.","contributorId":33839,"corporation":false,"usgs":true,"family":"Back","given":"W.","email":"","affiliations":[],"preferred":false,"id":359241,"contributorType":{"id":1,"text":"Authors"},"rank":2},{"text":"Rubin, M.","contributorId":88079,"corporation":false,"usgs":true,"family":"Rubin","given":"M.","email":"","affiliations":[],"preferred":false,"id":359242,"contributorType":{"id":1,"text":"Authors"},"rank":3}]}}
,{"id":70010596,"text":"70010596 - 1965 - Alaskan glaciers: Recent observations in respect to the earthquake-advance theory","interactions":[],"lastModifiedDate":"2026-02-10T21:31:56.04714","indexId":"70010596","displayToPublicDate":"1965-04-16T00:00:00","publicationYear":"1965","noYear":false,"publicationType":{"id":2,"text":"Article"},"publicationSubtype":{"id":10,"text":"Journal Article"},"seriesTitle":{"id":3338,"text":"Science","active":true,"publicationSubtype":{"id":10}},"title":"Alaskan glaciers: Recent observations in respect to the earthquake-advance theory","docAbstract":"Preliminary aerial photographic studies indicate that the Alaskan earthquake produced some rockfalls but no significant snow and ice avalanches on glaciers. No rapid, short-lived glacier advances (surges) are conclusively associated with this earthquake. Recent evidence fails to support the earthquake-advance theory of Tarr and Martin.","language":"English","publisher":"American Association for the Advancement of Science","doi":"10.1126/science.148.3668.366","issn":"00368075","usgsCitation":"Post, A., 1965, Alaskan glaciers: Recent observations in respect to the earthquake-advance theory: Science, v. 148, no. 3668, p. 366-368, https://doi.org/10.1126/science.148.3668.366.","productDescription":"3 p.","startPage":"366","endPage":"368","costCenters":[],"links":[{"id":219095,"rank":1,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/thumbnails/outside_thumb.jpg"}],"country":"United 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,{"id":70218179,"text":"70218179 - 1965 - Role of fluid pressure in mechanics of overthrust faulting: Reply","interactions":[],"lastModifiedDate":"2024-09-25T15:16:34.568141","indexId":"70218179","displayToPublicDate":"1965-04-01T18:17:18","publicationYear":"1965","noYear":false,"publicationType":{"id":2,"text":"Article"},"publicationSubtype":{"id":10,"text":"Journal Article"},"seriesTitle":{"id":1723,"text":"GSA Bulletin","active":true,"publicationSubtype":{"id":10}},"title":"Role of fluid pressure in mechanics of overthrust faulting: Reply","docAbstract":"<p><span>Davis cites four areas of low-angle faulting in which he believes that high fluid pressures can have played no important part in the development and movement of the thrust plates, but it seems to us that the concept or some variant of it may help to explain the observed field relationships in the three out of these four areas with which we have had some first-hand experience. In the areas of the Heart Mountain thrust of Wyoming, the Muddy Mountain thrust of Nevada, and the structurally higher, crystalline thrust sheets of the Swiss Alps, field relationships which include evidence of dehydration reactions during metamorphism of evaporites and of pelitic rocks suggest that interstitial fluid pressures may have been high and thus have played an essential part in the development of the thrust faults. In the fourth area cited by Davis, that of his own studies in the Klamath Mountains of California, we have had no first-hand experience and thus are not competent to answer his criticisms.</span></p>","language":"English","publisher":"Geological Society of America","doi":"10.1130/0016-7606(1965)76[469:ROFPIM]2.0.CO;2","usgsCitation":"Rubey, W.W., and Hubbert, M.K., 1965, Role of fluid pressure in mechanics of overthrust faulting: Reply: GSA Bulletin, v. 76, no. 4, p. 469-474, https://doi.org/10.1130/0016-7606(1965)76[469:ROFPIM]2.0.CO;2.","productDescription":"6 p.","startPage":"469","endPage":"474","costCenters":[],"links":[{"id":383306,"rank":1,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/thumbnails/outside_thumb.jpg"}],"volume":"76","issue":"4","noUsgsAuthors":false,"publicationStatus":"PW","contributors":{"authors":[{"text":"Rubey, William W.","contributorId":16899,"corporation":false,"usgs":true,"family":"Rubey","given":"William","email":"","middleInitial":"W.","affiliations":[],"preferred":false,"id":810371,"contributorType":{"id":1,"text":"Authors"},"rank":1},{"text":"Hubbert, M. King","contributorId":50197,"corporation":false,"usgs":true,"family":"Hubbert","given":"M.","email":"","middleInitial":"King","affiliations":[],"preferred":false,"id":810372,"contributorType":{"id":1,"text":"Authors"},"rank":2}]}}
,{"id":70221195,"text":"70221195 - 1965 - Geology and biology of the sea floor as deduced from simulaneous photographs and samples","interactions":[],"lastModifiedDate":"2021-06-04T20:30:18.324547","indexId":"70221195","displayToPublicDate":"1965-04-01T15:26:14","publicationYear":"1965","noYear":false,"publicationType":{"id":2,"text":"Article"},"publicationSubtype":{"id":10,"text":"Journal Article"},"seriesTitle":{"id":2620,"text":"Limnology and Oceanography","active":true,"publicationSubtype":{"id":10}},"title":"Geology and biology of the sea floor as deduced from simulaneous photographs and samples","docAbstract":"<p>During 1963, 260 paired photographs and large bottom samples were taken on the continental shelf and slope off northeastern United States. The photographs revealed surface characteristics of the sediments and natural attitudes of benthic animals; the samples retrieved specimens for geological and biological examination and identification.</p><p>Samples are the best source materials for making textural studies of sediments consisting mostly of sand, silt, or clay, but photographs are better than samples for bottoms too bouldery for proper sampling. Ripple marks and other surface irregularities revealed by the photographs supplement textural studies of the samples in deducing effects of wave movements and currents upon bottom materials.</p><p>For biological studies, the photographs yield much information on relationships of the benthic fauna to bottom materials, but they fail to provide useful data on biomasses. Biomasses and accurate taxonomic identifications are far better made upon samples. Thus, a combination of photographs and accompanying samples provides maximum information for biological as well as geological purposes.</p>","language":"English","publisher":"Association for the Sciences of Limnology and Oceanography","doi":"10.4319/lo.1965.10.1.0001","usgsCitation":"Emery, K., Merrill, A., and Trumbull, J.V., 1965, Geology and biology of the sea floor as deduced from simulaneous photographs and samples: Limnology and Oceanography, v. 10, no. 1, p. 1-21, https://doi.org/10.4319/lo.1965.10.1.0001.","productDescription":"21 p.","startPage":"1","endPage":"21","costCenters":[],"links":[{"id":480357,"rank":0,"type":{"id":40,"text":"Open Access Publisher Index Page"},"url":"https://doi.org/10.4319/lo.1965.10.1.0001","text":"Publisher Index Page"},{"id":386240,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/thumbnails/outside_thumb.jpg"}],"volume":"10","issue":"1","noUsgsAuthors":false,"publicationDate":"2003-12-22","publicationStatus":"PW","contributors":{"authors":[{"text":"Emery, K.O.","contributorId":67865,"corporation":false,"usgs":true,"family":"Emery","given":"K.O.","email":"","affiliations":[],"preferred":false,"id":817031,"contributorType":{"id":1,"text":"Authors"},"rank":1},{"text":"Merrill, A.S.","contributorId":36676,"corporation":false,"usgs":true,"family":"Merrill","given":"A.S.","email":"","affiliations":[],"preferred":false,"id":817032,"contributorType":{"id":1,"text":"Authors"},"rank":2},{"text":"Trumbull, James V. A.","contributorId":8457,"corporation":false,"usgs":true,"family":"Trumbull","given":"James","email":"","middleInitial":"V. A.","affiliations":[],"preferred":false,"id":817033,"contributorType":{"id":1,"text":"Authors"},"rank":3}]}}
,{"id":70221193,"text":"70221193 - 1965 - Environmental framework of ground‐water contamination","interactions":[],"lastModifiedDate":"2021-06-04T19:19:40.178242","indexId":"70221193","displayToPublicDate":"1965-04-01T14:15:00","publicationYear":"1965","noYear":false,"publicationType":{"id":2,"text":"Article"},"publicationSubtype":{"id":10,"text":"Journal Article"},"seriesTitle":{"id":3825,"text":"Groundwater","active":true,"publicationSubtype":{"id":10}},"title":"Environmental framework of ground‐water contamination","docAbstract":"<p><span>Ramifications of&nbsp;</span>contamination<span>&nbsp;are increasingly involved in the majority of&nbsp;</span>ground‐water<span>&nbsp;problems. The volume of usable&nbsp;</span>ground<span>&nbsp;</span>water<span>&nbsp;is shrinking in many places because of dispersion of contaminated&nbsp;</span>water<span>. Consideration of&nbsp;</span>ground‐water<span>&nbsp;</span>contamination<span>&nbsp;as a multitude of independent problems, separately solvable as each problem arises, is outmoded; wise policies, relating&nbsp;</span>water<span>&nbsp;supply to&nbsp;</span>contamination<span>&nbsp;potential, are needed to alleviate and to forestall problems. Methodology of managing&nbsp;</span>contamination<span>&nbsp;problems calls for appropriate classification of the hydrogeologic environment; these classifications include aspects of interdependent factors such as permeability, sorption, hydraulic gradient, position of&nbsp;</span>water<span>&nbsp;table relative to some base, and distance from source of&nbsp;</span>contamination<span>. Effective evaluations relate the dynamics of the hydrogeologic environment to contingencies involving&nbsp;</span>contamination<span>, as man changes his&nbsp;</span>water<span>‐development and waste‐disposal practices. Ways of&nbsp;</span>contamination<span>&nbsp;and pertinent parts of the physical environment include: waste‐disposal practices (at or near land surface and in deep formations), artificial recharge (at land surface and in aquifers), accidents, and salt‐</span>water<span>&nbsp;</span>contamination<span>&nbsp;of aquifers (shallow depth from salty surface&nbsp;</span>water<span>&nbsp;and at variable depths from subjacent salty aquifers). Evaluation of waste‐disposal problems calls for appreciation of two opposing tendencies–the tendency of wastes to move with&nbsp;</span>ground<span>&nbsp;</span>water<span>&nbsp;and the tendency to be attenuated near disposal sites by decay or inherent decrease in potency, by chemical and physical sorption, and by dilution through dispersion of&nbsp;</span>ground<span>&nbsp;</span>water<span>. Mixed wastes of differing attenuation habits represent special complex problems.</span></p>","language":"English","publisher":"Wiley Blackwell","doi":"10.1111/j.1745-6584.1965.tb01204.x","usgsCitation":"LeGrand, H.E., 1965, Environmental framework of ground‐water contamination: Groundwater, v. 3, no. 2, p. 11-15, https://doi.org/10.1111/j.1745-6584.1965.tb01204.x.","productDescription":"5 p.","startPage":"11","endPage":"15","costCenters":[],"links":[{"id":386238,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/thumbnails/outside_thumb.jpg"}],"volume":"3","issue":"2","noUsgsAuthors":false,"publicationDate":"2006-07-06","publicationStatus":"PW","contributors":{"authors":[{"text":"LeGrand, H. E.","contributorId":54571,"corporation":false,"usgs":true,"family":"LeGrand","given":"H.","email":"","middleInitial":"E.","affiliations":[],"preferred":false,"id":817027,"contributorType":{"id":1,"text":"Authors"},"rank":1}]}}
,{"id":70221192,"text":"70221192 - 1965 - Water levels: Water levels and trends November 1964-January 1965 (Abstracted from U. 5. Geological Survey “Water Resources Review”)","interactions":[],"lastModifiedDate":"2021-06-04T19:13:15.344472","indexId":"70221192","displayToPublicDate":"1965-04-01T14:09:56","publicationYear":"1965","noYear":false,"publicationType":{"id":2,"text":"Article"},"publicationSubtype":{"id":10,"text":"Journal Article"},"seriesTitle":{"id":3825,"text":"Groundwater","active":true,"publicationSubtype":{"id":10}},"title":"Water levels: Water levels and trends November 1964-January 1965 (Abstracted from U. 5. Geological Survey “Water Resources Review”)","docAbstract":"<p>No abstract available.&nbsp;</p>","language":"English","publisher":"NGWA The Groundwater Association","doi":"10.1111/j.1745-6584.1965.tb01212.x","usgsCitation":"Mesnier, G., 1965, Water levels: Water levels and trends November 1964-January 1965 (Abstracted from U. 5. Geological Survey “Water Resources Review”): Groundwater, v. 3, no. 2, p. 45-45, https://doi.org/10.1111/j.1745-6584.1965.tb01212.x.","productDescription":"1 p.","startPage":"45","endPage":"45","costCenters":[],"links":[{"id":386237,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/thumbnails/outside_thumb.jpg"}],"volume":"3","issue":"2","noUsgsAuthors":false,"publicationDate":"2006-07-06","publicationStatus":"PW","contributors":{"authors":[{"text":"Mesnier, G.N.","contributorId":32981,"corporation":false,"usgs":true,"family":"Mesnier","given":"G.N.","affiliations":[],"preferred":false,"id":817026,"contributorType":{"id":1,"text":"Authors"},"rank":1}]}}
,{"id":1014310,"text":"1014310 - 1965 - Use of microhematocrit values to sex largemouth bass","interactions":[],"lastModifiedDate":"2025-08-01T16:21:54.674476","indexId":"1014310","displayToPublicDate":"1965-04-01T00:00:00","publicationYear":"1965","noYear":false,"publicationType":{"id":2,"text":"Article"},"publicationSubtype":{"id":10,"text":"Journal Article"},"seriesTitle":{"id":3196,"text":"Progressive Fish-Culturist","active":true,"publicationSubtype":{"id":10}},"title":"Use of microhematocrit values to sex largemouth bass","docAbstract":"<p>No abstract available.&nbsp;</p>","language":"English","publisher":"American Fisheries Society","doi":"10.1577/1548-8640(1965)27[87:UOMVTS]2.0.CO;2","usgsCitation":"Steucke, E.W., and Atherton, C.R., 1965, Use of microhematocrit values to sex largemouth bass: Progressive Fish-Culturist, v. 27, no. 2, p. 87-90, https://doi.org/10.1577/1548-8640(1965)27[87:UOMVTS]2.0.CO;2.","productDescription":"4 p.","startPage":"87","endPage":"90","costCenters":[{"id":365,"text":"Leetown Science Center","active":true,"usgs":true}],"links":[{"id":131971,"rank":1,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/thumbnails/outside_thumb.jpg"}],"volume":"27","issue":"2","noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"4f4e4a17e4b07f02db604559","contributors":{"authors":[{"text":"Steucke, Erwin W. Jr.","contributorId":23798,"corporation":false,"usgs":true,"family":"Steucke","given":"Erwin","suffix":"Jr.","email":"","middleInitial":"W.","affiliations":[],"preferred":false,"id":320172,"contributorType":{"id":1,"text":"Authors"},"rank":1},{"text":"Atherton, Charles R.","contributorId":29367,"corporation":false,"usgs":false,"family":"Atherton","given":"Charles","middleInitial":"R.","affiliations":[],"preferred":false,"id":944641,"contributorType":{"id":1,"text":"Authors"},"rank":2}]}}
,{"id":70207282,"text":"70207282 - 1965 - Relation of carbon 14 concentrations to saline water contamination of coastal aquifers","interactions":[],"lastModifiedDate":"2019-12-17T07:00:43","indexId":"70207282","displayToPublicDate":"1965-03-31T16:24:40","publicationYear":"1965","noYear":false,"publicationType":{"id":2,"text":"Article"},"publicationSubtype":{"id":10,"text":"Journal Article"},"seriesTitle":{"id":3721,"text":"Water Resources Management","onlineIssn":"1573-1650","printIssn":"0920-4741","active":true,"publicationSubtype":{"id":10}},"title":"Relation of carbon 14 concentrations to saline water contamination of coastal aquifers","docAbstract":"<p><span>Naturally occurring stable or radioactive isotopes may be used in some places to identify the origin of saline water that contaminates some coastal aquifers. In a recent study to determine the origin of saline water in the Ocala Limestone aquifer near Brunswick, Georgia, the following sources were analyzed for C</span><sup>14</sup><span>&nbsp;and deuterium concentrations: potable water from the Ocala Limestone, contaminated water from the Ocala Limestone, saune water from the underlying Claiborne Group, and nearby ocean water. The chloride concentration of the groundwater ranges from about 25 ppm in the potable water to more than 2000 ppm in the deeper part of the Claiborne Group. From an interpretation of piezometric maps and other hydrologic data, previous investigators had concluded that the source of the contaminating water was the Claiborne Group and not the nearby ocean. The essentially uniform range of low values of −965 to −987‰ of the modern standard (National Bureau Standard C</span><sup>14</sup><span>&nbsp;oxalic acid) for the C</span><sup>14</sup><span>&nbsp;activity of the groundwater samples (regardless of the degree of contamination) is in agreement with this conclusion. If recent ocean water, which had a C</span><sup>14</sup><span>&nbsp;value of +285‰, were the source of contamination, the contaminated water would have had a C</span><sup>14</sup><span>&nbsp;activity higher than the activity of the fresh water. Deuterium analyses are not inconsistent with the interpretation that water from the Claiborne Group, rather than recent ocean water, is the source of the contaminating water. The concurrence of the hydrologic and the isotopic data in this area where the hydrology is well known suggests that isotopic analysis may be used to identify the origin of water in different portions of a hydrologic environment.&nbsp;</span></p>","language":"English","publisher":"American Geophysical Union","doi":"10.1029/WR001i001p00109","issn":"00431397","usgsCitation":"Hanshaw, B., Back, W., Rubin, M., and Wait, R.L., 1965, Relation of carbon 14 concentrations to saline water contamination of coastal aquifers: Water Resources Management, v. 1, no. 1, p. 109-114, https://doi.org/10.1029/WR001i001p00109.","productDescription":"6 p. ","startPage":"109","endPage":"114","costCenters":[],"links":[{"id":370289,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/thumbnails/outside_thumb.jpg"}],"country":"United States","state":"Georgia","county":"Glynn County","city":"Brunswick","geographicExtents":"{\n  \"type\": \"FeatureCollection\",\n  \"features\": [\n    {\n      \"type\": \"Feature\",\n      \"properties\": {},\n      \"geometry\": {\n        \"type\": \"Polygon\",\n        \"coordinates\": [\n          [\n            [\n              -81.73828125,\n              30.92107637538488\n            ],\n            [\n              -81.221923828125,\n              30.92107637538488\n            ],\n            [\n              -81.221923828125,\n              31.39115752282472\n            ],\n            [\n              -81.73828125,\n              31.39115752282472\n            ],\n            [\n              -81.73828125,\n              30.92107637538488\n            ]\n          ]\n        ]\n      }\n    }\n  ]\n}","volume":"1","issue":"1","noUsgsAuthors":false,"publicationDate":"2010-07-09","publicationStatus":"PW","contributors":{"authors":[{"text":"Hanshaw, B.B.","contributorId":25928,"corporation":false,"usgs":true,"family":"Hanshaw","given":"B.B.","email":"","affiliations":[],"preferred":false,"id":777532,"contributorType":{"id":1,"text":"Authors"},"rank":1},{"text":"Back, W.","contributorId":33839,"corporation":false,"usgs":true,"family":"Back","given":"W.","email":"","affiliations":[],"preferred":false,"id":777533,"contributorType":{"id":1,"text":"Authors"},"rank":2},{"text":"Rubin, Meyer","contributorId":107283,"corporation":false,"usgs":true,"family":"Rubin","given":"Meyer","email":"","affiliations":[],"preferred":false,"id":777690,"contributorType":{"id":1,"text":"Authors"},"rank":3},{"text":"Wait, Robert L.","contributorId":12839,"corporation":false,"usgs":true,"family":"Wait","given":"Robert","email":"","middleInitial":"L.","affiliations":[],"preferred":false,"id":777691,"contributorType":{"id":1,"text":"Authors"},"rank":4}]}}
,{"id":70010809,"text":"70010809 - 1965 - Quaternary correlations across Bering Strait","interactions":[],"lastModifiedDate":"2026-02-12T15:34:43.035498","indexId":"70010809","displayToPublicDate":"1965-03-05T00:00:00","publicationYear":"1965","noYear":false,"publicationType":{"id":2,"text":"Article"},"publicationSubtype":{"id":10,"text":"Journal Article"},"seriesTitle":{"id":3338,"text":"Science","active":true,"publicationSubtype":{"id":10}},"title":"Quaternary correlations across Bering Strait","docAbstract":"Recent Soviet and American studies cast new light on the history of the Bering land bridge.","language":"English","publisher":"American Association for the Advancement of Science","doi":"10.1126/science.147.3662.1107","issn":"00368075","usgsCitation":"Hopkins, D., MacNeil, F., Merklin, R., and Petrov, O., 1965, Quaternary correlations across Bering Strait: Science, v. 147, no. 3662, p. 1107-1114, https://doi.org/10.1126/science.147.3662.1107.","productDescription":"8 p.","startPage":"1107","endPage":"1114","costCenters":[],"links":[{"id":218675,"rank":1,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/thumbnails/outside_thumb.jpg"}],"country":"Russia, United States","otherGeospatial":"Bering land bridge","geographicExtents":"{\n  \"type\": \"FeatureCollection\",\n  \"features\": [\n    {\n      \"type\": \"Feature\",\n      \"properties\": {},\n      \"geometry\": {\n        \"coordinates\": [\n          [\n            [\n              -164.09090104089262,\n              67.6924535999915\n            ],\n            [\n              -174.08881441266908,\n              67.6924535999915\n            ],\n            [\n              -174.08881441266908,\n              63.49155843993441\n            ],\n            [\n              -164.09090104089262,\n              63.49155843993441\n            ],\n            [\n              -164.09090104089262,\n              67.6924535999915\n            ]\n          ]\n        ],\n        \"type\": \"Polygon\"\n      }\n    }\n  ]\n}","volume":"147","issue":"3662","noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"505a928be4b0c8380cd80904","contributors":{"authors":[{"text":"Hopkins, D.M.","contributorId":103646,"corporation":false,"usgs":true,"family":"Hopkins","given":"D.M.","email":"","affiliations":[],"preferred":false,"id":359698,"contributorType":{"id":1,"text":"Authors"},"rank":1},{"text":"MacNeil, F. S.","contributorId":34564,"corporation":false,"usgs":true,"family":"MacNeil","given":"F. S.","affiliations":[],"preferred":false,"id":359696,"contributorType":{"id":1,"text":"Authors"},"rank":2},{"text":"Merklin, R.L.","contributorId":106631,"corporation":false,"usgs":true,"family":"Merklin","given":"R.L.","email":"","affiliations":[],"preferred":false,"id":359699,"contributorType":{"id":1,"text":"Authors"},"rank":3},{"text":"Petrov, O.M.","contributorId":82453,"corporation":false,"usgs":true,"family":"Petrov","given":"O.M.","email":"","affiliations":[],"preferred":false,"id":359697,"contributorType":{"id":1,"text":"Authors"},"rank":4}]}}
,{"id":37782,"text":"37782 - 1965 - Trapping starlings","interactions":[],"lastModifiedDate":"2014-07-23T16:31:08","indexId":"37782","displayToPublicDate":"1965-03-01T16:30:44","publicationYear":"1965","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":"467","title":"Trapping starlings","docAbstract":"No abstract available.","language":"English","publisher":"U.S. Department of the Interior","publisherLocation":"Washington, D.C.","usgsCitation":"U.S. Bureau of Sport Fisheries and Wildlife, 1965, Trapping starlings: Wildlife Leaflet 467, 2 p.","productDescription":"2 p.","numberOfPages":"2","costCenters":[],"links":[{"id":290839,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/thumbnails/outside_thumb.jpg"}],"noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"57ffcdb6e4b0824b2d175959","contributors":{"authors":[{"text":"U.S. Bureau of Sport Fisheries and Wildlife","contributorId":128149,"corporation":true,"usgs":false,"organization":"U.S. Bureau of Sport Fisheries and Wildlife","id":529718,"contributorType":{"id":1,"text":"Authors"},"rank":1}]}}
,{"id":70221196,"text":"70221196 - 1965 - The U. S. Geological Survey's gravity program in Washington, Idaho, Montana, and Wyoming","interactions":[],"lastModifiedDate":"2021-06-04T20:57:49.146304","indexId":"70221196","displayToPublicDate":"1965-03-01T15:52:58","publicationYear":"1965","noYear":false,"publicationType":{"id":2,"text":"Article"},"publicationSubtype":{"id":10,"text":"Journal Article"},"seriesTitle":{"id":1578,"text":"Eos, Transactions, American Geophysical Union","onlineIssn":"2324-9250","printIssn":"0096-394","active":true,"publicationSubtype":{"id":10}},"title":"The U. S. Geological Survey's gravity program in Washington, Idaho, Montana, and Wyoming","docAbstract":"<p><span>The following summary of the&nbsp;</span>U<span>.&nbsp;</span>S<span>.&nbsp;</span>Geological<span>&nbsp;</span>Survey<span>&nbsp;</span>gravity<span>&nbsp;</span>program<span>&nbsp;</span>in<span>&nbsp;</span>Washington<span>,&nbsp;</span>Idaho<span>,&nbsp;</span>Montana<span>, and&nbsp;</span>Wyoming<span>&nbsp;is one of a series of short papers that outline&nbsp;</span>Geological<span>&nbsp;</span>Survey<span>&nbsp;</span>gravity<span>&nbsp;projects&nbsp;</span>in<span>&nbsp;the western United States. The substance of this summary is a list of references of published papers on&nbsp;</span>U<span>.&nbsp;</span>S<span>.&nbsp;</span>Geological<span>&nbsp;</span>Survey<span>&nbsp;</span>gravity<span>&nbsp;projects&nbsp;</span>in<span>&nbsp;the northwestern states together with an index map (Figure 1) showing the location of the project, the approximate a real coverage reported&nbsp;</span>in<span>&nbsp;the publication, and the contour map given&nbsp;</span>in<span>&nbsp;the publication. Areas&nbsp;</span>in<span>&nbsp;Figure 1 are related to the References (part 2) by a number code.&nbsp;</span>In<span>&nbsp;addition, the&nbsp;</span>gravity<span>&nbsp;projects&nbsp;</span>in<span>&nbsp;progress are listed&nbsp;</span>in<span>&nbsp;Table 1, indicating the area&nbsp;</span>in<span>&nbsp;which the work is being done and the person&nbsp;</span>in<span>&nbsp;charge of the project. Capital letter relate the locations of the projects&nbsp;</span>in<span>&nbsp;Figure 1 to the list of projects&nbsp;</span>in<span>&nbsp;Table 1. No attempt has been made to indicate the areal coverage or contour interval of the projects&nbsp;</span>in<span>&nbsp;progress.&nbsp;</span></p>","language":"English","publisher":"American Geophysical Union","doi":"10.1029/TR046i001p00214","usgsCitation":"Hill, D., 1965, The U. S. Geological Survey's gravity program in Washington, Idaho, Montana, and Wyoming: Eos, Transactions, American Geophysical Union, v. 46, no. 1, p. 214-217, https://doi.org/10.1029/TR046i001p00214.","productDescription":"4 p.","startPage":"214","endPage":"217","costCenters":[],"links":[{"id":386241,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/thumbnails/outside_thumb.jpg"}],"country":"United  States","state":"Washington, Idaho, Montana, Wyoming","geographicExtents":"{\n  \"type\": \"FeatureCollection\",\n  \"features\": [\n    {\n      \"type\": \"Feature\",\n      \"properties\": {},\n      \"geometry\": {\n        \"type\": \"Polygon\",\n        \"coordinates\": [\n          [\n            [\n              -123.00292968749999,\n              49.095452162534826\n            ],\n            [\n              -122.958984375,\n              48.16608541901253\n            ],\n            [\n              -124.8046875,\n              48.40003249610685\n            ],\n            [\n              -123.96972656249999,\n              46.10370875598026\n            ],\n            [\n              -122.73925781250001,\n              46.13417004624326\n            ],\n            [\n              -122.56347656249999,\n              45.644768217751924\n            ],\n            [\n              -116.89453125,\n              46.07323062540835\n            ],\n            [\n              -117.20214843749999,\n              44.402391829093915\n            ],\n            [\n              -117.1142578125,\n              42.09822241118974\n            ],\n            [\n              -111.005859375,\n              42.13082130188811\n            ],\n            [\n              -111.0498046875,\n              41.04621681452063\n            ],\n            [\n              -103.974609375,\n              41.0130657870063\n            ],\n            [\n              -104.1064453125,\n              48.980216985374994\n            ],\n            [\n              -123.00292968749999,\n              49.095452162534826\n            ]\n          ]\n        ]\n      }\n    }\n  ]\n}","volume":"46","issue":"1","noUsgsAuthors":false,"publicationDate":"2014-08-18","publicationStatus":"PW","contributors":{"authors":[{"text":"Hill, D.P.","contributorId":27432,"corporation":false,"usgs":true,"family":"Hill","given":"D.P.","email":"","affiliations":[],"preferred":false,"id":817034,"contributorType":{"id":1,"text":"Authors"},"rank":1}]}}
,{"id":70221191,"text":"70221191 - 1965 - The system arsenic-antimony","interactions":[],"lastModifiedDate":"2021-06-04T19:04:00.612551","indexId":"70221191","displayToPublicDate":"1965-03-01T14:01:40","publicationYear":"1965","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 system arsenic-antimony","docAbstract":"<p><span>The one atmosphere isobaric phase relations have been determined for the&nbsp;</span>system<span>&nbsp;As-Sb, using a simple experimental arrangement where a low melting temperature alkali halide melt acts as a reaction vessel. The one atmosphere univariant temperature, where a liquid of composition 45.5 mol % As, plus a solid of composition 62 mol % As and a gas of composition 89 mol % As coexist, is 666° ± 3° C. The one atmosphere sublimation point of As was measured as 611° ±2° C.&nbsp;</span>Arsenic<span>&nbsp;and&nbsp;</span>antimony<span>&nbsp;are hexagonal isostructural compounds with a complete solid solution series between them. The a cell edge and volume of the unit cell vary linearly with composition in mol percent. The c edge changes in a markedly nonlinear manner with composition. The measured unit-cell parameters at 25° C are: As, a = 3.760 ± 0.001 A, c = 10.555 ± 0.003A, V = 129.2A3; Sb, a = 4.310 ± 0.001 A, c - 11.279 ± 0.003A, V = 181.4A3.</span></p>","language":"English","publisher":"Society of Economic Geologists","doi":"10.2113/gsecongeo.60.2.228","usgsCitation":"Skinner, B.J., 1965, The system arsenic-antimony: Economic Geology, v. 60, no. 2, p. 228-239, https://doi.org/10.2113/gsecongeo.60.2.228.","productDescription":"12 p.","startPage":"228","endPage":"239","costCenters":[],"links":[{"id":386236,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/thumbnails/outside_thumb.jpg"}],"volume":"60","issue":"2","noUsgsAuthors":false,"publicationDate":"1965-03-01","publicationStatus":"PW","contributors":{"authors":[{"text":"Skinner, B. J.","contributorId":64867,"corporation":false,"usgs":true,"family":"Skinner","given":"B.","email":"","middleInitial":"J.","affiliations":[],"preferred":false,"id":817025,"contributorType":{"id":1,"text":"Authors"},"rank":1}]}}
,{"id":37781,"text":"37781 - 1965 - Directory of National Wildlife Refuges","interactions":[],"lastModifiedDate":"2014-07-23T13:54:57","indexId":"37781","displayToPublicDate":"1965-02-01T13:54:31","publicationYear":"1965","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":"466","title":"Directory of National Wildlife Refuges","docAbstract":"No abstract available.","language":"English","publisher":"U.S. Department of the Interior","publisherLocation":"Washington, D.C.","usgsCitation":"U.S. Bureau of Sport Fisheries and Wildlife, 1965, Directory of National Wildlife Refuges: Wildlife Leaflet 466, 18 p.","productDescription":"18 p.","numberOfPages":"18","costCenters":[],"links":[{"id":290826,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/thumbnails/outside_thumb.jpg"}],"noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"57ffcdb6e4b0824b2d17595b","contributors":{"authors":[{"text":"U.S. Bureau of Sport Fisheries and Wildlife","contributorId":128149,"corporation":true,"usgs":false,"organization":"U.S. Bureau of Sport Fisheries and Wildlife","id":529717,"contributorType":{"id":1,"text":"Authors"},"rank":1}]}}
,{"id":70221205,"text":"70221205 - 1965 - Nature and origin of the high-grade hematite ores of Minas Gerais, Brazil","interactions":[],"lastModifiedDate":"2021-06-04T21:48:30.190007","indexId":"70221205","displayToPublicDate":"1965-01-01T16:45:35","publicationYear":"1965","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":"Nature and origin of the high-grade hematite ores of Minas Gerais, Brazil","docAbstract":"<p><span>The&nbsp;</span>high<span>-</span>grade<span>&nbsp;</span>hematite<span>&nbsp;deposits of&nbsp;</span>Minas<span>&nbsp;</span>Gerais<span>,&nbsp;</span>Brazil<span>, are those averaging more than 66% Fe and less than 1.5% H20+. They occur in the Caue Itabirite, a metamorphosed oxide-facies iron formation of Pre-cambrian age. This formation was intricately folded during an orogeny that metamorphosed pelitic rocks to the greenschist and almandine-amphi-bole fades, accompanied by the formation of granitic rocks. The folding produced much plastic rock flowage toward the axes of many folds, thickness of the itabirite ranging from a few to more than 1,400 m. Of 40&nbsp;</span>ore<span>&nbsp;bodies on which enough information for judgments is available, 11 probably contain more than 100 million tons, 22 between 10 and 100 million tons, and 7 less than 10 million tons. At least two are thought to be larger than 400 million tons. The great majority of these&nbsp;</span>ore<span>&nbsp;bodies are associated with folded structures in the host itabirite, a few are associated with preore thrust faults, and some with abrupt steepening of regional linear structure. Most of the&nbsp;</span>ore<span>&nbsp;occurs in the lower, more siliceous two-thirds of the itabirite; some occurs in the upper third, which is locally dolomitic. Some of the&nbsp;</span>ore<span>&nbsp;is foliated, some unfoliated; the unfoliated cuts the foliated and heals&nbsp;</span>ore<span>&nbsp;breccias. The&nbsp;</span>ore<span>&nbsp;mineral is dominantly&nbsp;</span>hematite<span>.&nbsp;</span>Ore<span>&nbsp;was formed during the metamorphic cycle, after the folding. It is localized in relatively low-pressure, hence higher permeability, parts of folds.&nbsp;</span>Ore<span>&nbsp;replaced pre-existing itabirite, preserving structures. Regional metamorphism indicates that the metasomatizing fluids were at&nbsp;</span>high<span>&nbsp;temperature and under&nbsp;</span>high<span>&nbsp;confining pressure. Increasing solubility of quartz with gradually rising temperature caused metasomatic replacement of quartz by&nbsp;</span>hematite<span>&nbsp;picked up from iron formation by throughpassing fluids during the rising temperature cycle of metamorphism. Source of fluids is thought to have been first the metasedimentary rocks, then granitic gneiss and intrusive granite; the source of heat to have been the metasomatizing fluids and intrusive granite. The unfoliated iron&nbsp;</span>ore<span>&nbsp;healing brecciated foliated&nbsp;</span>ore<span>&nbsp;was deposited during the waning metamorphic cycle. Gold&nbsp;</span>ore<span>&nbsp;with associated tourmaline and cassiterite is found in porous but not massive iron&nbsp;</span>ore<span>. The abundant soft&nbsp;</span>high<span>-</span>grade<span>&nbsp;</span>hematite<span>&nbsp;</span>ore<span>&nbsp;formed from the more porous parts of the hard&nbsp;</span>ore<span>&nbsp;bodies, where metasomatism had not been complete, by supergene leaching of very minor quantities of&nbsp;</span>hematite<span>&nbsp;from crystal boundaries.</span></p>","language":"English","publisher":"Society of Economic Geologists","doi":"10.2113/gsecongeo.60.1.1","usgsCitation":"Dorr, J.V., 1965, Nature and origin of the high-grade hematite ores of Minas Gerais, Brazil: Economic Geology, v. 60, no. 1, p. 1-46, https://doi.org/10.2113/gsecongeo.60.1.1.","productDescription":"46 p.","startPage":"1","endPage":"46","costCenters":[],"links":[{"id":386250,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/thumbnails/outside_thumb.jpg"}],"country":"Brazil","state":"Minas Gerais","geographicExtents":"{\n  \"type\": \"FeatureCollection\",\n  \"features\": [\n    {\n      \"type\": \"Feature\",\n      \"properties\": {},\n      \"geometry\": {\n        \"type\": \"Polygon\",\n        \"coordinates\": [\n          [\n            [\n              -46.93359375,\n              -21.37124437061831\n            ],\n            [\n              -41.4404296875,\n              -21.37124437061831\n            ],\n            [\n              -41.4404296875,\n              -15.368949896534705\n            ],\n            [\n              -46.93359375,\n              -15.368949896534705\n            ],\n            [\n              -46.93359375,\n              -21.37124437061831\n            ]\n          ]\n        ]\n      }\n    }\n  ]\n}","volume":"60","issue":"1","noUsgsAuthors":false,"publicationDate":"1965-01-01","publicationStatus":"PW","contributors":{"authors":[{"text":"Dorr, J. V.N. II","contributorId":68807,"corporation":false,"usgs":true,"family":"Dorr","given":"J.","suffix":"II","middleInitial":"V.N.","affiliations":[],"preferred":false,"id":817045,"contributorType":{"id":1,"text":"Authors"},"rank":1}]}}
,{"id":877,"text":"877 - 1965 - Water resources data for Utah","interactions":[],"lastModifiedDate":"2014-08-05T16:42:43","indexId":"877","displayToPublicDate":"1965-01-01T16:41:27","publicationYear":"1965","noYear":false,"publicationType":{"id":18,"text":"Report"},"publicationSubtype":{"id":6,"text":"USGS Unnumbered Series"},"title":"Water resources data for Utah","docAbstract":"No abstract available.","language":"English","publisher":"U.S. Department of the Interior","publisherLocation":"Salt Lake City, UT","doi":"10.3133/877","issn":"0360-1633","collaboration":"Prepared in cooperation with the state of Utah and with other agencies.","usgsCitation":"Water Resources Division, U.S. Geological Survey, 1965, Water resources data for Utah, https://doi.org/10.3133/877.","costCenters":[],"links":[{"id":291738,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/thumbnails/usgs_thumb.jpg"}],"country":"United States","state":"Utah","geographicExtents":"{ \"type\": \"FeatureCollection\", \"features\": [ { \"type\": \"Feature\", \"properties\": {}, \"geometry\": { \"type\": \"Polygon\", \"coordinates\": [ [ [ -114.05,37.0 ], [ -114.05,42.0 ], [ -109.04,42.0 ], [ -109.04,37.0 ], [ -114.05,37.0 ] ] ] } } ] }","noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"53e1eff1e4b0fe532be2df63","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":527796,"contributorType":{"id":1,"text":"Authors"},"rank":1}]}}
,{"id":70221203,"text":"70221203 - 1965 - Structural geology of aconcagua province and its relationship to the central Valley Graben, Chile","interactions":[],"lastModifiedDate":"2021-06-04T21:40:36.084822","indexId":"70221203","displayToPublicDate":"1965-01-01T16:34:40","publicationYear":"1965","noYear":false,"publicationType":{"id":2,"text":"Article"},"publicationSubtype":{"id":10,"text":"Journal Article"},"seriesTitle":{"id":1786,"text":"Geological Society of America Bulletin","active":true,"publicationSubtype":{"id":10}},"title":"Structural geology of aconcagua province and its relationship to the central Valley Graben, Chile","docAbstract":"<p>Aconcagua<span>&nbsp;</span>Province<span>&nbsp;is herein divided into three major&nbsp;</span>structural<span>&nbsp;provinces which, for the sake of simplicity, are named the Coastal Cordillera,&nbsp;</span>Central<span>&nbsp;</span>Valley<span>&nbsp;</span>graben<span>, and Andean Cordillera&nbsp;</span>structural<span>&nbsp;provinces to correspond to the three geomorphic provinces recognized farther south. The coastal&nbsp;</span>structural<span>&nbsp;</span>province<span>&nbsp;includes the Coastal Cordillera which is underlain mainly by layered sedimentary and effusive rocks that strike north and dip homoclinally to the east, range from Triassic to Late Cretaceous in age, and are intruded by Cretaceous granodioritic and dioritic rocks. Igneous and metamorphic rocks largely of Paleozoic age comprise the western coastal margin, Along the eastern edge of the&nbsp;</span>province<span>&nbsp;is the Los Angeles fault zone, a wide, poorly defined band of semiparallel, arcuate faults which show downward displacement to the east and which appear to have resulted mainly from intrusion and uplift on the west. The Coastal Cordillera, therefore, may be considered a large horst with an intrusive granodiorite core. The&nbsp;</span>Central<span>&nbsp;</span>Valley<span>&nbsp;</span>graben<span>&nbsp;is bounded on the west by the Los Angeles fault zone and on the east by the Pocuro fault zone. Between these two fault zones is an area 20-30 km wide in which volcanic rocks of Late Cretaceous age are flat lying to gently folded and block faulted. In places, pipelike stocks of andesitic to dioritic igneous rock intrude the area. The Pocuro fault zone is a prominent lineament that marks the eastern limit of the&nbsp;</span>Central<span>&nbsp;</span>Valley<span>&nbsp;at Santiago and has been traced northward for 150 km. It may, however, have a mappable length of more than 1200 km. Vertical displacement downward to the west has been measured near Los Andes to be at least 2000 m. Consequently, this fault zone may rank among the major faults of the world. The Andean&nbsp;</span>structural<span>&nbsp;</span>province<span>&nbsp;is subdivided into the Las Ollas and Juncal subprovinces. The Las Ollas is a mountainous front range that lies east of the Pocuro fault and extends eastward for about 25 km. Upper Cretaceous volcanic strata are gently warped into broad, open, north-trending folds, with local sharp flexures and faulted mainly by normal faults. The eastern part of the subprovince is cut by a narrow belt of Tertiary plutonic rocks, some of which are associated with porphyry copper deposits. The Juncal&nbsp;</span>structural<span>&nbsp;subprovince extends eastward into Argentina. It is typified by close, overturned folding, vertical bedding, and thrust faulting. In general,&nbsp;</span>structural<span>&nbsp;deformation increases in intensity from west to east, with imbricate overthrusting to the east in Argentina. Present evidence indicates that major&nbsp;</span>graben<span>&nbsp;formation began during early Tertiary (pre-Miocene) time as a result of tensional stress developed by strain release of earlier compressional forces that folded the Andes. Post-Miocene uplift of the&nbsp;</span>central<span>&nbsp;Andean region renewed tensional stress and opened deep-seated, north-striking fractures and reinitiated volcanism. Most of the active volcanos of&nbsp;</span>Chile<span>&nbsp;may be aligned along such fractures.</span></p>","language":"English","publisher":"Geological Society of America","doi":"10.1130/0016-7606(1965)76[651:SGOAPA]2.0.CO;2","usgsCitation":"Carter, W.D., and Aguilar, L., 1965, Structural geology of aconcagua province and its relationship to the central Valley Graben, Chile: Geological Society of America Bulletin, v. 76, no. 6, p. 651-664, https://doi.org/10.1130/0016-7606(1965)76[651:SGOAPA]2.0.CO;2.","productDescription":"14 p.","startPage":"651","endPage":"664","costCenters":[],"links":[{"id":386248,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/thumbnails/outside_thumb.jpg"}],"country":"Chile","geographicExtents":"{\n  \"type\": \"FeatureCollection\",\n  \"features\": [\n    {\n      \"type\": \"Feature\",\n      \"properties\": {},\n      \"geometry\": {\n        \"type\": \"Polygon\",\n        \"coordinates\": [\n          [\n            [\n              -69.43359375,\n              -17.434510551522894\n            ],\n            [\n              -70.6201171875,\n              -18.437924653474393\n            ],\n            [\n              -70.6201171875,\n              -23.079731762449878\n            ],\n            [\n              -71.54296874999999,\n              -29.075375179558346\n            ],\n            [\n              -73.65234375,\n              -37.33522435930639\n            ],\n            [\n              -74.619140625,\n              -43.61221676817571\n            ],\n            [\n              -77.51953125,\n              -50.28933925329178\n            ],\n            [\n              -73.7841796875,\n              -55.10351605801966\n            ],\n            [\n              -67.5439453125,\n              -56.02294807962743\n            ],\n            [\n              -68.64257812499999,\n              -52.961875059076014\n            ],\n            [\n              -68.90625,\n              -52.133488040771475\n            ],\n            [\n              -71.982421875,\n              -51.86292391360244\n            ],\n            [\n              -72.421875,\n              -50.68079714532164\n            ],\n            [\n              -71.279296875,\n              -44.496505331093466\n            ],\n            [\n              -70.9716796875,\n              -38.444984668894705\n            ],\n            [\n              -69.873046875,\n              -33.43144133557529\n            ],\n            [\n              -68.291015625,\n              -26.74561038219901\n            ],\n            [\n              -66.9287109375,\n              -22.715390019335942\n            ],\n            [\n              -67.763671875,\n              -22.79643932091949\n            ],\n            [\n              -68.466796875,\n              -19.352610894378625\n            ],\n            [\n              -69.43359375,\n              -17.434510551522894\n            ]\n          ]\n        ]\n      }\n    }\n  ]\n}","volume":"76","issue":"6","noUsgsAuthors":false,"publicationStatus":"PW","contributors":{"authors":[{"text":"Carter, W. D.","contributorId":75633,"corporation":false,"usgs":true,"family":"Carter","given":"W.","email":"","middleInitial":"D.","affiliations":[],"preferred":false,"id":817042,"contributorType":{"id":1,"text":"Authors"},"rank":1},{"text":"Aguilar, Luis","contributorId":192543,"corporation":false,"usgs":false,"family":"Aguilar","given":"Luis","email":"","affiliations":[],"preferred":false,"id":817043,"contributorType":{"id":1,"text":"Authors"},"rank":2}]}}
,{"id":70221202,"text":"70221202 - 1965 - Stratigraphy and heavy minerals of the bays formation, Bays Mountain synclinorium, northeast Tennessee","interactions":[],"lastModifiedDate":"2021-06-04T21:33:21.794355","indexId":"70221202","displayToPublicDate":"1965-01-01T16:29:37","publicationYear":"1965","noYear":false,"publicationType":{"id":2,"text":"Article"},"publicationSubtype":{"id":10,"text":"Journal Article"},"seriesTitle":{"id":1786,"text":"Geological Society of America Bulletin","active":true,"publicationSubtype":{"id":10}},"title":"Stratigraphy and heavy minerals of the bays formation, Bays Mountain synclinorium, northeast Tennessee","docAbstract":"<p><span>The&nbsp;</span>Bays<span>&nbsp;</span>Mountain<span>&nbsp;</span>synclinorium<span>&nbsp;is in the Valley and Ridge province in&nbsp;</span>northeast<span>&nbsp;</span>Tennessee<span>, southwest of Kingsport and west of Greeneville. The more clastic part of the&nbsp;</span>Bays<span>&nbsp;</span>formation<span>&nbsp;lies in the east section of the&nbsp;</span>synclinorium<span>. The thickness of the&nbsp;</span>Bays<span>&nbsp;decreases from about 870 feet on the east to about 600 feet on the west. Presumably, the red beds and primary features of the&nbsp;</span>Bays<span>&nbsp;</span>formation<span>&nbsp;formed under deltaic conditions. A Camarocladia Zone near its base indicates a time-transgression of the&nbsp;</span>Bays<span>. The&nbsp;</span>Bays<span>&nbsp;is older at the base to the east than at its base to the west. The&nbsp;</span>heavy<span>&nbsp;</span>minerals<span>&nbsp;of the&nbsp;</span>Bays<span>&nbsp;were compared with those of the Cambrian and Precambrian(?) sediments, volcanic rocks, and accessory&nbsp;</span>minerals<span>&nbsp;of the crystalline complex which now comprise the Blue Ridge. The&nbsp;</span>minerals<span>&nbsp;identified include nearly all those in the Cambrian and Precambrian(?) sediments as well as additional&nbsp;</span>minerals<span>&nbsp;not found in these older sediments but that are in the crystalline complex. Such&nbsp;</span>minerals<span>&nbsp;indicate that at least a part of the crystalline complex was above sea level during the Middle Ordovician.</span></p>","language":"English","publisher":"Geological Society of America","doi":"10.1130/0016-7606(1965)76[591:SAHMOT]2.0.CO;2","usgsCitation":"Cummings, D., 1965, Stratigraphy and heavy minerals of the bays formation, Bays Mountain synclinorium, northeast Tennessee: Geological Society of America Bulletin, v. 76, no. 5, p. 591-600, https://doi.org/10.1130/0016-7606(1965)76[591:SAHMOT]2.0.CO;2.","productDescription":"10 p.","startPage":"591","endPage":"600","costCenters":[],"links":[{"id":386247,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/thumbnails/outside_thumb.jpg"}],"country":"United States","state":"Tennessee","otherGeospatial":"northeast Tennessee","geographicExtents":"{\n  \"type\": \"FeatureCollection\",\n  \"features\": [\n    {\n      \"type\": \"Feature\",\n      \"properties\": {},\n      \"geometry\": {\n        \"type\": \"Polygon\",\n        \"coordinates\": [\n          [\n            [\n              -84.385986328125,\n              35.02999636902566\n            ],\n            [\n              -82.63916015625,\n              36.05798104702501\n            ],\n            [\n              -81.82617187499999,\n              36.28856319836237\n            ],\n            [\n              -81.6064453125,\n              36.58024660149866\n            ],\n            [\n              -82.85888671875,\n              36.62434536776987\n            ],\n            [\n              -84.17724609375,\n              36.61552763134925\n            ],\n            [\n              -85.166015625,\n              35.0120020431607\n            ],\n            [\n              -84.385986328125,\n              35.02999636902566\n            ]\n          ]\n        ]\n      }\n    }\n  ]\n}","volume":"76","issue":"5","noUsgsAuthors":false,"publicationStatus":"PW","contributors":{"authors":[{"text":"Cummings, D.","contributorId":69705,"corporation":false,"usgs":true,"family":"Cummings","given":"D.","email":"","affiliations":[],"preferred":false,"id":817041,"contributorType":{"id":1,"text":"Authors"},"rank":1}]}}
,{"id":70221200,"text":"70221200 - 1965 - Earthquake magnitudes from hydroseismic data","interactions":[],"lastModifiedDate":"2021-06-04T21:23:32.190063","indexId":"70221200","displayToPublicDate":"1965-01-01T16:20:46","publicationYear":"1965","noYear":false,"publicationType":{"id":2,"text":"Article"},"publicationSubtype":{"id":10,"text":"Journal Article"},"seriesTitle":{"id":3825,"text":"Groundwater","active":true,"publicationSubtype":{"id":10}},"title":"Earthquake magnitudes from hydroseismic data","docAbstract":"<p><span>If earthquakes are recorded on your water‐level charts, you can make your own estimate of&nbsp;</span>earthquake<span>&nbsp;</span>magnitudes<span>! As an aid in doing this, this paper presents two graphs: one to calculate distance from well to&nbsp;</span>earthquake<span>&nbsp;epicenter; the other, a nomogram from which to read&nbsp;</span>hydroseismic<span>&nbsp;</span>magnitude<span>&nbsp;plus log C. Examples given show (1) direct computation of m</span><sub>s</sub><span>+ log C, (2) use of aftershocks to estimate total water‐level fluctuation caused by a major&nbsp;</span>earthquake<span>&nbsp;(when the recorder drum has spun around or when reversals cover up the record), and (3) how to determine if aftershocks theoretically should have been recorded.&nbsp;</span>Hydroseismic<span>&nbsp;</span>magnitude<span>&nbsp;is the surface‐wave&nbsp;</span>magnitude<span>&nbsp;(M</span><sub>s</sub><span>) calculated from seismically induced water‐level fluctuations in wells. As yet it must be computed indirectly from m</span><sub>s</sub><span>+ log C but because log C is a variable the result is only approximate. Log C is believed to represent a resultant controlled by magnification, period of the surface waves, instrumental frictions, well lag, and resonance if the well is underdamped.&nbsp;</span></p>","language":"English","publisher":"NGWA The Groundwater Association","doi":"10.1111/j.1745-6584.1965.tb01196.x","usgsCitation":"Vorhis, R., 1965, Earthquake magnitudes from hydroseismic data: Groundwater, v. 3, no. 1, p. 12-20, https://doi.org/10.1111/j.1745-6584.1965.tb01196.x.","productDescription":"9 p.","startPage":"12","endPage":"20","costCenters":[],"links":[{"id":386245,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/thumbnails/outside_thumb.jpg"}],"volume":"3","issue":"1","noUsgsAuthors":false,"publicationDate":"2006-07-06","publicationStatus":"PW","contributors":{"authors":[{"text":"Vorhis, R.C.","contributorId":32512,"corporation":false,"usgs":true,"family":"Vorhis","given":"R.C.","affiliations":[{"id":595,"text":"U.S. Geological Survey","active":false,"usgs":true}],"preferred":false,"id":817039,"contributorType":{"id":1,"text":"Authors"},"rank":1}]}}
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