{"pageNumber":"5570","pageRowStart":"139225","pageSize":"25","recordCount":165626,"records":[{"id":70162486,"text":"70162486 - 1974 - Earthquake history of Mississippi","interactions":[],"lastModifiedDate":"2016-03-21T14:37:13","indexId":"70162486","displayToPublicDate":"1974-01-01T00:00:00","publicationYear":"1974","noYear":false,"publicationType":{"id":2,"text":"Article"},"publicationSubtype":{"id":10,"text":"Journal Article"},"seriesTitle":{"id":1435,"text":"Earthquake Information Bulletin (USGS)","active":true,"publicationSubtype":{"id":10}},"title":"Earthquake history of Mississippi","docAbstract":"<p>Since its admission into the Union in 1817, Mississippi has had only four earthquakes of intensity V or greater within its borders. Although the number of earthquakes known to have been centered within Mississippi's boundaries is small, the State has been affected by numerous shocks located in neighboring States. In 1811 and 1812, a series of great earthquakes near the New Madrid Missouri area was felt in Mississippi as far south as the gulf coast. The New Madrid series caused the banks of the Mississippi River to cave in as far as Vicksburg, mroe than 300 miles from the epicentral region. As a result of this great earthquake series, the northwest corner of Mississippi is in seismic risk zone 3, the highest risk zone. Expect for the new Madrid series, effects in Mississippi from earthquakes located outside of the State have been less than intensity V.&nbsp;</p>","language":"English","publisher":"U.S Geological Survey","usgsCitation":"von Hake, C., 1974, Earthquake history of Mississippi: Earthquake Information Bulletin (USGS), v. 6, no. 2, p. 20-21.","productDescription":"2 p.","startPage":"20","endPage":"21","onlineOnly":"N","additionalOnlineFiles":"N","costCenters":[],"links":[{"id":314808,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/thumbnails/outside_thumb.jpg"}],"country":"United States","state":"Mississippi","geographicExtents":"{\n  \"type\": \"FeatureCollection\",\n  \"features\": [\n    {\n      \"type\": \"Feature\",\n      \"properties\": {},\n      \"geometry\": {\n        \"type\": \"Polygon\",\n        \"coordinates\": [\n          [\n            [\n              -90.263671875,\n              35.003003395276714\n            ],\n            [\n              -88.209228515625,\n              35.02099970111467\n            ],\n            [\n              -88.121337890625,\n              34.867904962568716\n            ],\n            [\n              -88.363037109375,\n              32.89803818160524\n            ],\n            [\n              -88.43994140625,\n              32.08257455954592\n            ],\n            [\n              -88.472900390625,\n              31.84956532831343\n            ],\n            [\n              -88.406982421875,\n              30.439202087235607\n            ],\n            [\n              -88.39599609375,\n              30.344435586368462\n            ],\n            [\n              -89.044189453125,\n              30.173624550358536\n            ],\n            [\n              -89.483642578125,\n              30.06909396443887\n            ],\n            [\n              -89.637451171875,\n              30.268556249047727\n            ],\n            [\n              -89.813232421875,\n              30.64736425824319\n            ],\n            [\n              -89.813232421875,\n              30.732392734006083\n            ],\n            [\n              -89.736328125,\n              30.996445897426373\n            ],\n            [\n              -91.614990234375,\n              31.005862904624205\n            ],\n            [\n              -91.614990234375,\n              31.18460913574325\n            ],\n            [\n              -91.527099609375,\n              31.466153715024294\n            ],\n            [\n              -91.351318359375,\n              31.74685416292141\n            ],\n            [\n              -91.01074218749999,\n              32.175612478499325\n            ],\n            [\n              -90.977783203125,\n              32.47269502206151\n            ],\n            [\n              -91.219482421875,\n              32.99023555965106\n            ],\n            [\n              -91.219482421875,\n              33.486435450999885\n            ],\n            [\n              -91.07666015625,\n              33.970697997361626\n            ],\n            [\n              -90.736083984375,\n              34.361576287484176\n            ],\n            [\n              -90.52734374999999,\n              34.63320791137959\n            ],\n            [\n              -90.516357421875,\n              34.768691457552706\n            ],\n            [\n              -90.3515625,\n              34.88593094075317\n            ],\n            [\n              -90.263671875,\n              35.003003395276714\n            ]\n          ]\n        ]\n      }\n    }\n  ]\n}","volume":"6","issue":"2","noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"56a7554de4b0b28f1184d7f1","contributors":{"authors":[{"text":"von Hake, C. A.","contributorId":7699,"corporation":false,"usgs":true,"family":"von Hake","given":"C. A.","affiliations":[],"preferred":false,"id":589675,"contributorType":{"id":1,"text":"Authors"},"rank":1}]}}
,{"id":70168840,"text":"70168840 - 1974 - Laboratory experiments duplicate conditions in the Earth’s crust","interactions":[],"lastModifiedDate":"2016-03-24T15:27:18","indexId":"70168840","displayToPublicDate":"1974-01-01T00:00:00","publicationYear":"1974","noYear":false,"publicationType":{"id":2,"text":"Article"},"publicationSubtype":{"id":10,"text":"Journal Article"},"seriesTitle":{"id":1435,"text":"Earthquake Information Bulletin (USGS)","active":true,"publicationSubtype":{"id":10}},"title":"Laboratory experiments duplicate conditions in the Earth’s crust","docAbstract":"<p>An experimental device that simulates conditions in the Earth's crust at depths of up to 30 kilometers has been constructed by geophysicists working at the U.S Geological Survey laboratories in Menlo Park, California. A high pressure \"bomb\" is being used to experimentally measure the velocity of seismic waves in different types of rock at various confining pressures and temperatures. The principal purpose of these measurements is to determine the elastic and non-elastic properties of rocks and minerals under conditions of high-pressure such as exist deep in the Earth's crust.&nbsp;</p>","language":"English","publisher":"U.S Geological Survey","usgsCitation":"Peselnick, L., Dieterich, J.H., and Stewart, R., 1974, Laboratory experiments duplicate conditions in the Earth’s crust: Earthquake Information Bulletin (USGS), v. 6, no. 1, p. 10-15.","productDescription":"6 p.","startPage":"10","endPage":"15","onlineOnly":"N","additionalOnlineFiles":"N","costCenters":[],"links":[{"id":318588,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/thumbnails/outside_thumb.jpg"}],"volume":"6","issue":"1","noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"56dabfe8e4b015c306f84cc3","contributors":{"authors":[{"text":"Peselnick, L.","contributorId":66825,"corporation":false,"usgs":true,"family":"Peselnick","given":"L.","affiliations":[],"preferred":false,"id":621969,"contributorType":{"id":1,"text":"Authors"},"rank":1},{"text":"Dieterich, James H.","contributorId":81614,"corporation":false,"usgs":true,"family":"Dieterich","given":"James","middleInitial":"H.","affiliations":[],"preferred":false,"id":621970,"contributorType":{"id":1,"text":"Authors"},"rank":2},{"text":"Stewart, R.M.","contributorId":16861,"corporation":false,"usgs":true,"family":"Stewart","given":"R.M.","email":"","affiliations":[],"preferred":false,"id":621971,"contributorType":{"id":1,"text":"Authors"},"rank":3}]}}
,{"id":70162485,"text":"70162485 - 1974 - Earthquake history of Missouri","interactions":[],"lastModifiedDate":"2016-03-21T14:31:55","indexId":"70162485","displayToPublicDate":"1974-01-01T00:00:00","publicationYear":"1974","noYear":false,"publicationType":{"id":2,"text":"Article"},"publicationSubtype":{"id":10,"text":"Journal Article"},"seriesTitle":{"id":1435,"text":"Earthquake Information Bulletin (USGS)","active":true,"publicationSubtype":{"id":10}},"title":"Earthquake history of Missouri","docAbstract":"<p>Most of Missouri's earthquake activity has been concentrated in the southeast corner of the State, which lies within the New Madrid seismic zone. As recently as Merch 29, 1972, the region was jolted by a magnitude 3.7 shock that was felt over a 168,000 square kilometre area including parts of Arkansas, Illinois, Mississippi, and Tennessee.&nbsp;</p>","language":"English","publisher":"U.S Geological Survey","usgsCitation":"von Hake, C., 1974, Earthquake history of Missouri: Earthquake Information Bulletin (USGS), v. 6, no. 3, p. 24-26.","productDescription":"3 p.","startPage":"24","endPage":"26","onlineOnly":"N","additionalOnlineFiles":"N","costCenters":[],"links":[{"id":314807,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/thumbnails/outside_thumb.jpg"}],"country":"United States","state":"Missouri","geographicExtents":"{\n  \"type\": \"FeatureCollection\",\n  \"features\": [\n    {\n      \"type\": \"Feature\",\n      \"properties\": {},\n      \"geometry\": {\n        \"type\": \"Polygon\",\n        \"coordinates\": [\n          [\n            [\n              -95.745849609375,\n              40.588928169693745\n            ],\n            [\n              -91.7578125,\n              40.622291783092706\n            ],\n            [\n              -91.43920898437499,\n              40.371658891506094\n            ],\n            [\n              -91.49414062499999,\n              40.10328591293442\n            ],\n            [\n              -91.351318359375,\n              39.715638134796336\n            ],\n            [\n              -90.966796875,\n              39.41922073655956\n            ],\n            [\n              -90.736083984375,\n              39.18117526158749\n            ],\n            [\n              -90.626220703125,\n              38.856820134743636\n            ],\n            [\n              -90.47241210937499,\n              38.95940879245423\n            ],\n            [\n              -90.10986328125,\n              38.87392853923629\n            ],\n            [\n              -90.186767578125,\n              38.66835610151509\n            ],\n            [\n              -90.3515625,\n              38.35888785866677\n            ],\n            [\n              -90.28564453124999,\n              38.14319750166766\n            ],\n            [\n              -89.901123046875,\n              37.94419750075404\n            ],\n            [\n              -89.549560546875,\n              37.70989935485515\n            ],\n            [\n              -89.439697265625,\n              37.45741810262938\n            ],\n            [\n              -89.461669921875,\n              37.16031654673677\n            ],\n            [\n              -89.26391601562499,\n              36.958671131530316\n            ],\n            [\n              -89.110107421875,\n              36.958671131530316\n            ],\n            [\n              -89.18701171875,\n              36.5978891330702\n            ],\n            [\n              -89.527587890625,\n              36.465471886798134\n            ],\n            [\n              -89.6484375,\n              36.08462129606931\n            ],\n            [\n              -89.736328125,\n              35.98689628443789\n            ],\n            [\n              -90.384521484375,\n              36.00467348670187\n            ],\n            [\n              -90.076904296875,\n              36.33282808737917\n            ],\n            [\n              -90.1318359375,\n              36.474306755095206\n            ],\n            [\n              -94.625244140625,\n              36.50963615733049\n            ],\n            [\n              -94.63623046875,\n              38.98503278695909\n            ],\n            [\n              -94.888916015625,\n              39.27478966170308\n            ],\n            [\n              -95.09765625,\n              39.54641191968671\n            ],\n            [\n              -94.89990234375,\n              39.816975090490004\n            ],\n            [\n              -94.89990234375,\n              39.884450178234395\n            ],\n            [\n              -95.130615234375,\n              39.884450178234395\n            ],\n            [\n              -95.64697265625,\n              40.33817045213394\n            ],\n            [\n              -95.7568359375,\n              40.49709237269567\n            ],\n            [\n              -95.745849609375,\n              40.588928169693745\n            ]\n          ]\n        ]\n      }\n    }\n  ]\n}","volume":"6","issue":"3","noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"56a7554de4b0b28f1184d7f3","contributors":{"authors":[{"text":"von Hake, C. A.","contributorId":7699,"corporation":false,"usgs":true,"family":"von Hake","given":"C. A.","affiliations":[],"preferred":false,"id":589674,"contributorType":{"id":1,"text":"Authors"},"rank":1}]}}
,{"id":70170286,"text":"70170286 - 1974 - The design earthquake and earthquake response spectra","interactions":[],"lastModifiedDate":"2016-04-15T15:39:18","indexId":"70170286","displayToPublicDate":"1974-01-01T00:00:00","publicationYear":"1974","noYear":false,"publicationType":{"id":2,"text":"Article"},"publicationSubtype":{"id":10,"text":"Journal Article"},"seriesTitle":{"id":1435,"text":"Earthquake Information Bulletin (USGS)","active":true,"publicationSubtype":{"id":10}},"title":"The design earthquake and earthquake response spectra","language":"English","publisher":"U.S Geological Survey","usgsCitation":"Hays, W.W., 1974, The design earthquake and earthquake response spectra: Earthquake Information Bulletin (USGS), v. 6, no. 4, p. 18-22.","productDescription":"5 p.","startPage":"18","endPage":"22","onlineOnly":"N","additionalOnlineFiles":"N","costCenters":[],"links":[{"id":320076,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/thumbnails/outside_thumb.jpg"}],"volume":"6","issue":"4","noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"571210b9e4b0ef3b7ca64449","contributors":{"authors":[{"text":"Hays, W. W.","contributorId":66693,"corporation":false,"usgs":true,"family":"Hays","given":"W.","email":"","middleInitial":"W.","affiliations":[],"preferred":false,"id":626762,"contributorType":{"id":1,"text":"Authors"},"rank":1}]}}
,{"id":70169214,"text":"70169214 - 1974 - The Mississippi Valley earthquakes of 1811 and 1812","interactions":[],"lastModifiedDate":"2016-03-31T16:00:58","indexId":"70169214","displayToPublicDate":"1974-01-01T00:00:00","publicationYear":"1974","noYear":false,"publicationType":{"id":2,"text":"Article"},"publicationSubtype":{"id":10,"text":"Journal Article"},"seriesTitle":{"id":1435,"text":"Earthquake Information Bulletin (USGS)","active":true,"publicationSubtype":{"id":10}},"title":"The Mississippi Valley earthquakes of 1811 and 1812","docAbstract":"<p>Shortly after 2 o'clock on the morning of December 16, 1811, the Mississippi River valley was convulsed by an earthquake so severe that it awakened people in cities as distant as Pittsburgh, Pennsylvania, and Norfolk, Virginia. This shock inaugurated what must have been the most frightening sequence of earthquakes ever to occur in the United States. Intermittent strong shaking continued through March 1812 and aftershocks strong enough to be felt occurred through the year 1817. The initial earthquake of December 16 was followed by other principal shocks, one on January 23, 1812, and the other on February 7, 182. Judging from newspaper accounts of damage to buildings, the February 7 earthquake was the biggest of the three.&nbsp;</p>","language":"English","publisher":"U.S Geological Survey","usgsCitation":"Nuttli, O., 1974, The Mississippi Valley earthquakes of 1811 and 1812: Earthquake Information Bulletin (USGS), v. 6, no. 2, p. 8-13.","productDescription":"6 p.","startPage":"8","endPage":"13","onlineOnly":"N","additionalOnlineFiles":"N","costCenters":[],"links":[{"id":319280,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/thumbnails/outside_thumb.jpg"}],"country":"United States","otherGeospatial":"Mississippi Valley","geographicExtents":"{\n  \"type\": \"FeatureCollection\",\n  \"features\": [\n    {\n      \"type\": \"Feature\",\n      \"properties\": {},\n      \"geometry\": {\n        \"type\": \"Polygon\",\n        \"coordinates\": [\n          [\n            [\n              -89.7637939453125,\n              36.804886560237236\n            ],\n            [\n              -89.110107421875,\n              36.81808022778526\n            ],\n            [\n              -88.7640380859375,\n              36.61552763134925\n            ],\n            [\n              -88.8958740234375,\n              36.11125252076159\n            ],\n            [\n              -89.98901367187499,\n              35.567980458012094\n            ],\n            [\n              -90.439453125,\n              35.46961797120201\n            ],\n            [\n              -90.3900146484375,\n              35.89350026142572\n            ],\n            [\n              -89.8516845703125,\n              36.804886560237236\n            ],\n            [\n              -89.7637939453125,\n              36.804886560237236\n            ]\n          ]\n        ]\n      }\n    }\n  ]\n}","volume":"6","issue":"2","noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"56f3be52e4b0f59b85e02f2c","contributors":{"authors":[{"text":"Nuttli, O.W.","contributorId":59818,"corporation":false,"usgs":true,"family":"Nuttli","given":"O.W.","affiliations":[],"preferred":false,"id":623346,"contributorType":{"id":1,"text":"Authors"},"rank":1}]}}
,{"id":70170539,"text":"70170539 - 1974 - Locating the world’s earthquakes","interactions":[],"lastModifiedDate":"2016-04-24T12:36:53","indexId":"70170539","displayToPublicDate":"1974-01-01T00:00:00","publicationYear":"1974","noYear":false,"publicationType":{"id":2,"text":"Article"},"publicationSubtype":{"id":10,"text":"Journal Article"},"seriesTitle":{"id":1435,"text":"Earthquake Information Bulletin (USGS)","active":true,"publicationSubtype":{"id":10}},"title":"Locating the world’s earthquakes","language":"English","publisher":"U.S Geological Survey","usgsCitation":"Derr, J., 1974, Locating the world’s earthquakes: Earthquake Information Bulletin (USGS), v. 6, no. 5, p. 11-15.","productDescription":"5 p.","startPage":"11","endPage":"15","onlineOnly":"N","additionalOnlineFiles":"N","costCenters":[],"links":[{"id":320485,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/thumbnails/outside_thumb.jpg"}],"volume":"6","issue":"5","noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"571dee2be4b071321fe56405","contributors":{"authors":[{"text":"Derr, J.S.","contributorId":37477,"corporation":false,"usgs":true,"family":"Derr","given":"J.S.","email":"","affiliations":[],"preferred":false,"id":627545,"contributorType":{"id":1,"text":"Authors"},"rank":1}]}}
,{"id":5220962,"text":"5220962 - 1974 - An attempt to age mallards using eye lens proteins","interactions":[],"lastModifiedDate":"2025-02-26T21:59:28.666524","indexId":"5220962","displayToPublicDate":"1974-01-01T00:00:00","publicationYear":"1974","noYear":false,"publicationType":{"id":2,"text":"Article"},"publicationSubtype":{"id":10,"text":"Journal Article"},"seriesTitle":{"id":2508,"text":"Journal of Wildlife Management","active":true,"publicationSubtype":{"id":10}},"title":"An attempt to age mallards using eye lens proteins","docAbstract":"<p>An analysis of insoluble protein content of eye lenses from 59 known-age mallards (<i>Anas platyrhynchos</i>) indicated a slight increase between 8-9 months and 7 years of age. Nearly a complete overlapping of the insoluble protein content of individuals of different ages was apparent showing that the technique cannot be used to separate adult year classes of mallards. These results are contrary to findings reported for selected mammalian species; a possible explanation for the dissimilarity is discussed.</p>","language":"English","publisher":"Wiley","doi":"10.2307/3800209","usgsCitation":"Henny, C.J., and Ludke, J., 1974, An attempt to age mallards using eye lens proteins: Journal of Wildlife Management, v. 38, no. 1, p. 138-141, https://doi.org/10.2307/3800209.","productDescription":"4 p.","startPage":"138","endPage":"141","costCenters":[{"id":531,"text":"Patuxent Wildlife Research Center","active":true,"usgs":true}],"links":[{"id":198752,"rank":1,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/thumbnails/outside_thumb.jpg"}],"volume":"38","issue":"1","noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"4f4e4ad9e4b07f02db6852e8","contributors":{"authors":[{"text":"Henny, Charles J.","contributorId":12578,"corporation":false,"usgs":true,"family":"Henny","given":"Charles","email":"","middleInitial":"J.","affiliations":[],"preferred":false,"id":332763,"contributorType":{"id":1,"text":"Authors"},"rank":1},{"text":"Ludke, J. Larry","contributorId":29033,"corporation":false,"usgs":true,"family":"Ludke","given":"J. Larry","affiliations":[],"preferred":false,"id":332764,"contributorType":{"id":1,"text":"Authors"},"rank":2}]}}
,{"id":70181903,"text":"70181903 - 1974 -  Fish Immunology, Chapter 4: Techniques used in immunology of fishes","interactions":[],"lastModifiedDate":"2017-02-14T18:11:08","indexId":"70181903","displayToPublicDate":"1974-01-01T00:00:00","publicationYear":"1974","noYear":false,"publicationType":{"id":5,"text":"Book chapter"},"publicationSubtype":{"id":24,"text":"Book Chapter"},"title":" Fish Immunology, Chapter 4: Techniques used in immunology of fishes","docAbstract":"<p>No abstract available&nbsp;</p>","largerWorkType":{"id":4,"text":"Book"},"largerWorkTitle":"Disease of Fishes","language":"English","publisher":"T.F.H. Inc. Pub.","usgsCitation":"Anderson, D.P., 1974,  Fish Immunology, Chapter 4: Techniques used in immunology of fishes, chap. <i>of</i> Disease of Fishes.","costCenters":[{"id":654,"text":"Western Fisheries Research Center","active":true,"usgs":true}],"links":[{"id":335443,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/thumbnails/outside_thumb.jpg"}],"noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"58a4254ce4b0c825128ad4f9","contributors":{"authors":[{"text":"Anderson, D. P.","contributorId":32469,"corporation":false,"usgs":true,"family":"Anderson","given":"D.","email":"","middleInitial":"P.","affiliations":[],"preferred":false,"id":668958,"contributorType":{"id":1,"text":"Authors"},"rank":1}]}}
,{"id":70010972,"text":"70010972 - 1974 - Heat flow from eastern Panama and northwestern Colombia","interactions":[],"lastModifiedDate":"2023-12-14T01:02:11.521091","indexId":"70010972","displayToPublicDate":"1974-01-01T00:00:00","publicationYear":"1974","noYear":false,"publicationType":{"id":2,"text":"Article"},"publicationSubtype":{"id":10,"text":"Journal Article"},"seriesTitle":{"id":1427,"text":"Earth and Planetary Science Letters","active":true,"publicationSubtype":{"id":10}},"title":"Heat flow from eastern Panama and northwestern Colombia","docAbstract":"<div id=\"abstracts\" class=\"Abstracts u-font-serif text-s\"><div id=\"ab1\" class=\"abstract author\" lang=\"en\"><div id=\"aep-abstract-sec-id6\"><p>Heat flows were determined at 12 sites in four distinct areas between longitude 77° and 80°W in eastern Panama and northwestern Colombia. Evidently, most of the region is underlain by mafic oceanic crust so that the crustal radiogenic component of heat flow is very small (∼ 0.1 μcal cm<sup>−2</sup><span>&nbsp;</span>sec<sup>−1</sup>). Low heat-flow values (∼ 0.7 μcal cm<sup>−2</sup><span>&nbsp;</span>sec<sup>−1</sup>) in northwestern Colombia may reflect thermal transients associated with shallow subduction. The normal values (∼ 1) at about 78°W are consistent with the mean heat flow from the western Caribbean and the Gulf of Mexico. At 80°W, a fairly high value of 1.8 may define the easterly limit of thermal transients due to Cenozoic volcanic activity in Central America.</p></div></div></div><ul id=\"issue-navigation\" class=\"issue-navigation u-margin-s-bottom u-bg-grey1\"></ul>","language":"English","publisher":"Elsevier","doi":"10.1016/0012-821X(74)90046-6","issn":"0012821X","usgsCitation":"Sass, J., Munroe, R.J., and Moses, T.H., 1974, Heat flow from eastern Panama and northwestern Colombia: Earth and Planetary Science Letters, v. 21, no. 2, p. 134-142, https://doi.org/10.1016/0012-821X(74)90046-6.","productDescription":"9 p.","startPage":"134","endPage":"142","numberOfPages":"9","costCenters":[],"links":[{"id":221208,"rank":1,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/thumbnails/outside_thumb.jpg"}],"country":"Columbia, Panama","geographicExtents":"{\n  \"type\": \"FeatureCollection\",\n  \"features\": [\n    {\n      \"type\": \"Feature\",\n      \"properties\": {},\n      \"geometry\": {\n        \"type\": \"Polygon\",\n        \"coordinates\": [\n          [\n            [\n              -82.79296874999999,\n              -3.513421045640032\n            ],\n            [\n              -66.09375,\n              -3.513421045640032\n            ],\n            [\n              -66.09375,\n              9.535748998133627\n            ],\n            [\n              -82.79296874999999,\n              9.535748998133627\n            ],\n            [\n              -82.79296874999999,\n              -3.513421045640032\n            ]\n          ]\n        ]\n      }\n    }\n  ]\n}","volume":"21","issue":"2","noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"505a2ffde4b0c8380cd5d2a1","contributors":{"authors":[{"text":"Sass, J.H.","contributorId":70749,"corporation":false,"usgs":true,"family":"Sass","given":"J.H.","email":"","affiliations":[{"id":595,"text":"U.S. Geological Survey","active":false,"usgs":true}],"preferred":false,"id":360002,"contributorType":{"id":1,"text":"Authors"},"rank":1},{"text":"Munroe, R. J.","contributorId":56215,"corporation":false,"usgs":true,"family":"Munroe","given":"R.","email":"","middleInitial":"J.","affiliations":[],"preferred":false,"id":360000,"contributorType":{"id":1,"text":"Authors"},"rank":2},{"text":"Moses, T. H. Jr.","contributorId":70385,"corporation":false,"usgs":true,"family":"Moses","given":"T.","suffix":"Jr.","email":"","middleInitial":"H.","affiliations":[],"preferred":false,"id":360001,"contributorType":{"id":1,"text":"Authors"},"rank":3}]}}
,{"id":70011058,"text":"70011058 - 1974 - Oil shale development and its environmental considerations","interactions":[],"lastModifiedDate":"2012-03-12T17:18:35","indexId":"70011058","displayToPublicDate":"1974-01-01T00:00:00","publicationYear":"1974","noYear":false,"publicationType":{"id":24,"text":"Conference Paper"},"publicationSubtype":{"id":19,"text":"Conference Paper"},"title":"Oil shale development and its environmental considerations","docAbstract":"The petroleum shortage recently experienced by many nations throughout the world has created an intense interest in obtaining new and supplemental energy sources. In the United States, this interest has been centered on oil shale. Any major action by the federal government having significant environmental effects requires compliance with the National Environmental Policy Act of 1969 (NEPA). Since most oil shale is found on federal lands, and since its development involves significant environmental impacts, leasing oil shale lands to private interests must be in compliance with NEPA. For oil shale, program planning began at approximately the same time that NEPA was signed into law. By structuring the program to permit a resource and technological inventory by industry and the federal agencies, the Department of the Interior was able simultaneously to conduct the environmental assessments required by the act. This required: 1. Clearly defined program objections; 2. An organization which could integrate public policy with diverse scientific disciplines and environmental concerns; and 3. Flexible decisionmaking to adjust to policy changes as well as to evolving interpretations on EPA as clarified by court decisions. This paper outlines the program, the organization structure that was created for this specific task, and the environmental concerns which were investigated. The success of the program has been demonstrated by meeting the requirements of NEPA, without court challenge, and by industry's acceptance of a leasing program that included the most stringent environmental protection provisions ever required. The need for energy development has spurred the acceptance of the program. However, by its awareness and willingness to meet the environmental challenges of the future, industry has shown a reasonable understanding of its commitments. The pros and cons of development were publicly considered in hearings and analyzed in the final environmental statement. This action aided greatly in preventing legal challenges. The prototype oil shale program is now under way and this new energy source, developed with strict environmental safeguards, may soon be available to our nation.","largerWorkTitle":"Preprints","language":"English","issn":"05693799","usgsCitation":"Stone, R., Johnson, H., and Decora, A., 1974, Oil shale development and its environmental considerations, <i>in</i> Preprints, v. 19, no. 3.","startPage":"510","costCenters":[],"links":[{"id":220955,"rank":0,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/thumbnails/outside_thumb.jpg"}],"volume":"19","issue":"3","noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"505a6cf8e4b0c8380cd74ecc","contributors":{"authors":[{"text":"Stone, R.T.","contributorId":75680,"corporation":false,"usgs":true,"family":"Stone","given":"R.T.","email":"","affiliations":[],"preferred":false,"id":360185,"contributorType":{"id":1,"text":"Authors"},"rank":1},{"text":"Johnson, H.","contributorId":61163,"corporation":false,"usgs":true,"family":"Johnson","given":"H.","affiliations":[],"preferred":false,"id":360184,"contributorType":{"id":1,"text":"Authors"},"rank":2},{"text":"Decora, A.","contributorId":45455,"corporation":false,"usgs":true,"family":"Decora","given":"A.","email":"","affiliations":[],"preferred":false,"id":360183,"contributorType":{"id":1,"text":"Authors"},"rank":3}]}}
,{"id":70010217,"text":"70010217 - 1974 - Spectrophotometric determination of molybdenum in rocks with thiocyanate","interactions":[],"lastModifiedDate":"2021-01-22T14:18:04.09582","indexId":"70010217","displayToPublicDate":"1974-01-01T00:00:00","publicationYear":"1974","noYear":false,"publicationType":{"id":2,"text":"Article"},"publicationSubtype":{"id":10,"text":"Journal Article"},"seriesTitle":{"id":760,"text":"Analytica Chimica Acta","active":true,"publicationSubtype":{"id":10}},"title":"Spectrophotometric determination of molybdenum in rocks with thiocyanate","docAbstract":"<div id=\"aep-abstract-id4\" class=\"abstract author\"><div id=\"aep-abstract-sec-id5\"><p id=\"simple-para.0010\">A rapid procedure for the determination of microgram amounts of molybdenum in rocks is described. After acid decomposition, molybdenum is extracted from a hydrochloric acid solution into xylene with tributyl phosphate. After back-extraction with water, molybdenum is extracted as the α-benzoinoximate into chloroform, stripped into hydrochloric acid extracted as the thiocyanate into amyl alcohol, and determined spectrophotometrically. The molybdenum thiocyanate color produced is stable, sensitive, and reproducible. Results of analyses of several of the U.S. Geological Survey standard rocks are given.</p></div></div><div id=\"aep-abstract-id6\" class=\"abstract author\" lang=\"fr\"><br></div>","language":"English","publisher":"Elsevier","doi":"10.1016/S0003-2670(01)80897-7","issn":"00032670","usgsCitation":"Lillie, E., and Greenland, L., 1974, Spectrophotometric determination of molybdenum in rocks with thiocyanate: Analytica Chimica Acta, v. 69, no. 2, p. 313-320, https://doi.org/10.1016/S0003-2670(01)80897-7.","productDescription":"8 p.","startPage":"313","endPage":"320","numberOfPages":"8","costCenters":[],"links":[{"id":219133,"rank":0,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/thumbnails/outside_thumb.jpg"}],"volume":"69","issue":"2","noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"505b95a9e4b08c986b31b043","contributors":{"authors":[{"text":"Lillie, E.G.","contributorId":13370,"corporation":false,"usgs":true,"family":"Lillie","given":"E.G.","email":"","affiliations":[],"preferred":false,"id":358330,"contributorType":{"id":1,"text":"Authors"},"rank":1},{"text":"Greenland, L. P.","contributorId":56368,"corporation":false,"usgs":true,"family":"Greenland","given":"L. P.","affiliations":[],"preferred":false,"id":358331,"contributorType":{"id":1,"text":"Authors"},"rank":2}]}}
,{"id":70010257,"text":"70010257 - 1974 - Argillization by descending acid at Steamboat Springs, Nevada","interactions":[],"lastModifiedDate":"2018-01-25T15:07:20","indexId":"70010257","displayToPublicDate":"1974-01-01T00:00:00","publicationYear":"1974","noYear":false,"publicationType":{"id":2,"text":"Article"},"publicationSubtype":{"id":10,"text":"Journal Article"},"seriesTitle":{"id":1245,"text":"Clays and Clay Minerals","onlineIssn":"1552-8367","printIssn":"0009-8604","active":true,"publicationSubtype":{"id":10}},"title":"Argillization by descending acid at Steamboat Springs, Nevada","docAbstract":"<p>Steamboat Springs, Nevada, an area of present-day hot springs, clearly illustrates the genetic dependence of some kaolin deposits on hot-spring activity. Andesite, granodiorite and arkosic sediments are locally altered at the land surface to siliceous residues consisting of primary quartz and anatase, plus opal from primary silicates. These siliceous residues commonly exhibit the textural and structural features of their unaltered equivalents. Beneath the siliceous residues, kaolin and alunite replace primary silicates and fill open spaces, forming a blanketlike deposit. Beneath the kaolin-alunite zone, montmorillonite, commonly accompanied by pyrite, replaces the primary silicates. On the ground surface, the same alteration mineral zones can be traced outward from the siliceous residue; however, hematite rather than pyrite accompanies montmorillonite.</p><p>Chemical analysis indicates that sulfuric acid is the active altering agent. The acid forms from hydrogen sulfide that exsolves from deep thermal water, rises above the water table and is oxidized by sulfur-oxidizing bacteria living near the ground surface. This acid dissolves in precipitation or condensed water vapor and percolates downward destroying most of the primary minerals producing a siliceous residue. Coincidence of the water table with the downward transition from siliceous residue to kaolin-alunite signifies decreasing hydrogen metasomatism because of dilution of descending acid by ground water.</p><p>In hot-spring areas, beds of siliceous sinter deposited at the surface by hypogene thermal water look, superficially, like areas of surficial acid alteration. Features diagnostic of a surficial alteration are the relict rock structures of a siliceous residue and a kaolin-alunite zone immediately beneath.</p>","language":"English","publisher":"The Clay Minerals Society","doi":"10.1346/CCMN.1974.0220104","usgsCitation":"Schoen, R., White, D.E., and Hemley, J., 1974, Argillization by descending acid at Steamboat Springs, Nevada: Clays and Clay Minerals, v. 22, no. 1, p. 1-22, https://doi.org/10.1346/CCMN.1974.0220104.","productDescription":"22 p.","startPage":"1","endPage":"22","costCenters":[],"links":[{"id":219749,"rank":0,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/thumbnails/outside_thumb.jpg"}],"country":"United States","state":"Nevada","otherGeospatial":"Steamboat Springs","volume":"22","issue":"1","noUsgsAuthors":false,"publicationDate":"2024-07-01","publicationStatus":"PW","scienceBaseUri":"5059ed75e4b0c8380cd49803","contributors":{"authors":[{"text":"Schoen, Robert","contributorId":22418,"corporation":false,"usgs":true,"family":"Schoen","given":"Robert","email":"","affiliations":[],"preferred":false,"id":358467,"contributorType":{"id":1,"text":"Authors"},"rank":1},{"text":"White, Donald E.","contributorId":76787,"corporation":false,"usgs":true,"family":"White","given":"Donald","email":"","middleInitial":"E.","affiliations":[],"preferred":false,"id":358466,"contributorType":{"id":1,"text":"Authors"},"rank":2},{"text":"Hemley, J.J.","contributorId":59556,"corporation":false,"usgs":true,"family":"Hemley","given":"J.J.","email":"","affiliations":[],"preferred":false,"id":358468,"contributorType":{"id":1,"text":"Authors"},"rank":3}]}}
,{"id":48243,"text":"ofr741066 - 1974 - The chemical composition and estimated minimum thermal reservoir temperatures of the principal hot springs of northern and central Nevada","interactions":[],"lastModifiedDate":"2022-07-07T19:09:19.724679","indexId":"ofr741066","displayToPublicDate":"1974-01-01T00:00:00","publicationYear":"1974","noYear":false,"publicationType":{"id":18,"text":"Report"},"publicationSubtype":{"id":5,"text":"USGS Numbered Series"},"seriesTitle":{"id":330,"text":"Open-File Report","code":"OFR","onlineIssn":"2331-1258","printIssn":"0196-1497","active":true,"publicationSubtype":{"id":5}},"seriesNumber":"74-1066","title":"The chemical composition and estimated minimum thermal reservoir temperatures of the principal hot springs of northern and central Nevada","docAbstract":"<p>Fifty-five of the principal hot springs in northern and central Nevada have been sampled for chemical analyses. Major element constituents, sodium, potassium, calcium, and silica suggest minimum thermal-aquifer temperatures of 140°C or more at 16 of the hot spring complexes. At least five of the hot springs issue mixed waters which may indicate thermal-aquifer temperatures significantly lower than the true thermal-aquifer temperature.</p><p>Sodium is the principal cation in almost all the spring waters. Four springs in northern Nye County and adjacent Eureka County have approximately equal amounts of sodium and calcium. Bicarbonate is the principal anion in most of the spring waters. However, the sampled hot springs on the western edge of the State have chloride as the principal anion. A diffuse zone of bicarbonate chloride waters with or without sulfate separates the chloride and bicarbonate regions.</p>","language":"English","publisher":"U.S. Geological Survey","doi":"10.3133/ofr741066","usgsCitation":"Mariner, R.H., Rapp, J.B., Willey, L., and Presser, T.S., 1974, The chemical composition and estimated minimum thermal reservoir temperatures of the principal hot springs of northern and central Nevada: U.S. Geological Survey Open-File Report 74-1066, 32 p., https://doi.org/10.3133/ofr741066.","productDescription":"32 p.","costCenters":[],"links":[{"id":403210,"rank":2,"type":{"id":11,"text":"Document"},"url":"https://pubs.usgs.gov/of/1974/1066/report.pdf","linkFileType":{"id":1,"text":"pdf"}},{"id":172000,"rank":0,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/of/1974/1066/report-thumb.jpg"}],"country":"United States","state":"Nevada","geographicExtents":"{\n  \"type\": \"FeatureCollection\",\n  \"features\": [\n    {\n      \"type\": \"Feature\",\n      \"properties\": {},\n      \"geometry\": {\n        \"type\": \"Polygon\",\n        \"coordinates\": [\n          [\n            [\n              -120.003662109375,\n              42.00032514831621\n            ],\n            [\n              -120.0146484375,\n              39.01918369029134\n            ],\n            [\n              -118.421630859375,\n              37.88352498087131\n            ],\n            [\n              -114.04907226562499,\n              38.004819966413194\n            ],\n            [\n              -114.0380859375,\n              42.00848901572399\n            ],\n            [\n              -120.003662109375,\n              42.00032514831621\n            ]\n          ]\n        ]\n      }\n    }\n  ]\n}","noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"4f4e4aaae4b07f02db66939c","contributors":{"authors":[{"text":"Mariner, Robert H.","contributorId":81075,"corporation":false,"usgs":true,"family":"Mariner","given":"Robert","email":"","middleInitial":"H.","affiliations":[],"preferred":false,"id":237027,"contributorType":{"id":1,"text":"Authors"},"rank":1},{"text":"Rapp, J. B.","contributorId":28987,"corporation":false,"usgs":true,"family":"Rapp","given":"J.","email":"","middleInitial":"B.","affiliations":[],"preferred":false,"id":237025,"contributorType":{"id":1,"text":"Authors"},"rank":2},{"text":"Willey, L.M.","contributorId":44607,"corporation":false,"usgs":true,"family":"Willey","given":"L.M.","email":"","affiliations":[],"preferred":false,"id":237026,"contributorType":{"id":1,"text":"Authors"},"rank":3},{"text":"Presser, T. S.","contributorId":93875,"corporation":false,"usgs":true,"family":"Presser","given":"T.","email":"","middleInitial":"S.","affiliations":[],"preferred":false,"id":237028,"contributorType":{"id":1,"text":"Authors"},"rank":4}]}}
,{"id":2000017,"text":"2000017 - 1974 - A review of the literature on the use of Bayluscide in fisheries","interactions":[],"lastModifiedDate":"2012-02-02T00:15:01","indexId":"2000017","displayToPublicDate":"1974-01-01T00:00:00","publicationYear":"1974","noYear":false,"publicationType":{"id":18,"text":"Report"},"publicationSubtype":{"id":1,"text":"Federal Government Series"},"seriesTitle":{"id":43,"text":"Literature Review","active":false,"publicationSubtype":{"id":1}},"seriesNumber":"74-02","title":"A review of the literature on the use of Bayluscide in fisheries","docAbstract":"In the United States Bayluscide has had multiple uses. The 70% wettable powder has been used in Puerto Rico for snail control and the 5% granular formulation has been tested in Michigan and Wisconsin against freshwater snails serving as inter mediate hosts of the trematode causing swimmers' itch. Bayluscide has also been used in field trials as a fish toxicant. Its most important use in North America, however, has been to control sea lampreys, Petromyzon marinus, in the Great Lakes, a necessary prerequisite for the restoration of Great Lakes sport and commercial fisheries. Since 1966 the 5% granular formulation has been used by the U.S. Fish and Wildlife Service and the Canadian Department of Environment as a toxicant to survey populations of larval sea lampreys in Great Lakes estuaries and deepwater tributaries. The Canadian Government also uses Bayluscide to control sea lampreys, but in the United States the present registration restricts use to population surveys only. Literature on the mixtures of Bayluscide and the selective lamprey toxicant, TFM, used since 1964 by both the U.S. and Canadian agencies to control larval sea lampreys in the Great Lakes, has been reviewed elsewhere and is not included in this review.","language":"English","publisher":"U.S. Fish and Wildlife Service","collaboration":"Out-of-print","usgsCitation":"Hamilton, S.E., 1974, A review of the literature on the use of Bayluscide in fisheries: Literature Review 74-02, 60 p.","productDescription":"60 p.","startPage":"0","endPage":"60","numberOfPages":"60","costCenters":[{"id":324,"text":"Great Lakes Science Center","active":true,"usgs":true}],"links":[{"id":198330,"rank":0,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/thumbnails/outside_thumb.jpg"}],"noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"4f4e4b19e4b07f02db6a7ee3","contributors":{"authors":[{"text":"Hamilton, Sandra E.","contributorId":62318,"corporation":false,"usgs":true,"family":"Hamilton","given":"Sandra","email":"","middleInitial":"E.","affiliations":[],"preferred":false,"id":324934,"contributorType":{"id":1,"text":"Authors"},"rank":1}]}}
,{"id":2000018,"text":"2000018 - 1974 - A review of the literature on the use of TFM-Bayluscide in fisheries","interactions":[],"lastModifiedDate":"2016-03-14T10:56:40","indexId":"2000018","displayToPublicDate":"1974-01-01T00:00:00","publicationYear":"1974","noYear":false,"publicationType":{"id":18,"text":"Report"},"publicationSubtype":{"id":1,"text":"Federal Government Series"},"seriesTitle":{"id":43,"text":"Literature Review","active":false,"publicationSubtype":{"id":1}},"seriesNumber":"74-03","title":"A review of the literature on the use of TFM-Bayluscide in fisheries","docAbstract":"<p>Since 1956 the Great Lakes Fishery Commission has been responsible for formulating and implementing a program to eradicate or control the sea lamprey in the Great Lakes. The U.S. Fish and Wildlife Service and the Sea Lamprey Control Centre of the Canadian Department of the Environment act as agents for the Commission in sea lamprey control. In the search for a selective lampricide that would control lampreys without destroying fish and other aquatic organisms, about 6,000 chemicals were tested at the Hammond Bay Biological Station of the U.S. Fish and Wildlife Service, largely during the mid 1950's. One compound, TFM, which is selectively toxic to sea lampreys was developed for field use. In 1963 Bayluscide was discovered to be extremely toxic to sea lampreys. Because Bayluscide is also very toxic to fish, being virtually nonselective between lampreys and rainbow trout, only 3% by weight can be added to TFM without losing the selective toxicity of TFM. Addition of small amounts of Bayluscide to TFM, however, effects substantial savings by greatly reducing the amount of TFM needed for effective treatment of lamprey populations. Since 1963 mixtures of TFM and Bayluscide have been used as a lampricide in tributaries of the Great Lakes by both the U.S. and Canadian governments.</p>","language":"English","publisher":"U.S. Fish and Wildlife Service","usgsCitation":"Hamilton, S.E., 1974, A review of the literature on the use of TFM-Bayluscide in fisheries: Literature Review 74-03, 53 p.","productDescription":"53 p.","onlineOnly":"N","additionalOnlineFiles":"N","costCenters":[{"id":324,"text":"Great Lakes Science Center","active":true,"usgs":true}],"links":[{"id":198331,"rank":0,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/thumbnails/outside_thumb.jpg"}],"noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"4f4e4b19e4b07f02db6a7ec2","contributors":{"authors":[{"text":"Hamilton, Sandra E.","contributorId":62318,"corporation":false,"usgs":true,"family":"Hamilton","given":"Sandra","email":"","middleInitial":"E.","affiliations":[],"preferred":false,"id":324935,"contributorType":{"id":1,"text":"Authors"},"rank":1}]}}
,{"id":1001293,"text":"1001293 - 1974 - Use of small fences to protect ground bird nests from mammalian predators","interactions":[],"lastModifiedDate":"2018-01-05T10:45:09","indexId":"1001293","displayToPublicDate":"1974-01-01T00:00:00","publicationYear":"1974","noYear":false,"publicationType":{"id":2,"text":"Article"},"publicationSubtype":{"id":10,"text":"Journal Article"},"seriesTitle":{"id":3111,"text":"Prairie Naturalist","active":true,"publicationSubtype":{"id":10}},"title":"Use of small fences to protect ground bird nests from mammalian predators","docAbstract":"Abstract has not been submitted","largerWorkType":{"id":2,"text":"Article"},"largerWorkTitle":"Prairie Naturalist","largerWorkSubtype":{"id":10,"text":"Journal Article"},"language":"English","usgsCitation":"Sargeant, A., Kruse, A., and Afton, A., 1974, Use of small fences to protect ground bird nests from mammalian predators: Prairie Naturalist, v. 6, no. 3/4, p. 60-63.","productDescription":"4 p.","startPage":"60","endPage":"63","costCenters":[{"id":480,"text":"Northern Prairie Wildlife Research Center","active":true,"usgs":true}],"links":[{"id":130587,"rank":0,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/thumbnails/outside_thumb.jpg"}],"volume":"6","issue":"3/4","noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"4f4e4a17e4b07f02db604365","contributors":{"authors":[{"text":"Sargeant, A.B.","contributorId":13171,"corporation":false,"usgs":true,"family":"Sargeant","given":"A.B.","email":"","affiliations":[],"preferred":false,"id":310821,"contributorType":{"id":1,"text":"Authors"},"rank":1},{"text":"Kruse, A.D.","contributorId":19900,"corporation":false,"usgs":true,"family":"Kruse","given":"A.D.","email":"","affiliations":[],"preferred":false,"id":310822,"contributorType":{"id":1,"text":"Authors"},"rank":2},{"text":"Afton, A. D.","contributorId":83467,"corporation":false,"usgs":true,"family":"Afton","given":"A. D.","affiliations":[],"preferred":false,"id":310823,"contributorType":{"id":1,"text":"Authors"},"rank":3}]}}
,{"id":70010019,"text":"70010019 - 1974 - Martian volcanism: Additional observations and evidence for pyroclastic activity","interactions":[],"lastModifiedDate":"2021-02-04T14:45:41.022604","indexId":"70010019","displayToPublicDate":"1974-01-01T00:00:00","publicationYear":"1974","noYear":false,"publicationType":{"id":2,"text":"Article"},"publicationSubtype":{"id":10,"text":"Journal Article"},"seriesTitle":{"id":1963,"text":"Icarus","active":true,"publicationSubtype":{"id":10}},"title":"Martian volcanism: Additional observations and evidence for pyroclastic activity","docAbstract":"<div id=\"abstracts\" class=\"Abstracts u-font-serif\"><div id=\"aep-abstract-id4\" class=\"abstract author\"><div id=\"aep-abstract-sec-id5\"><p>Inspection of the Mariner 9 B-camera (resolution 100–200m) and A-camera (resolution 1–2km) photographs of Mars reveals numerous analogs of terrestrial and lunar volcanic features. In addition to the exceptionally large constructional features in the Tharsis region, many other large and small landforms present probably are related to endogenic processes.</p></div></div></div><ul id=\"issue-navigation\" class=\"issue-navigation u-margin-s-bottom u-bg-grey1\"></ul>","language":"English","publisher":"Elsevier","doi":"10.1016/0019-1035(74)90085-2","issn":"00191035","usgsCitation":"West, M., 1974, Martian volcanism: Additional observations and evidence for pyroclastic activity: Icarus, v. 21, no. 1, p. 1-11, https://doi.org/10.1016/0019-1035(74)90085-2.","productDescription":"11 p.","startPage":"1","endPage":"11","numberOfPages":"11","costCenters":[],"links":[{"id":219342,"rank":0,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/thumbnails/outside_thumb.jpg"}],"volume":"21","issue":"1","noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"505a5235e4b0c8380cd6c243","contributors":{"authors":[{"text":"West, M.","contributorId":54729,"corporation":false,"usgs":true,"family":"West","given":"M.","email":"","affiliations":[],"preferred":false,"id":357704,"contributorType":{"id":1,"text":"Authors"},"rank":1}]}}
,{"id":70010201,"text":"70010201 - 1974 - A probe for sampling interstitial waters of stream sediments and bog soils","interactions":[],"lastModifiedDate":"2025-03-06T16:22:00.645396","indexId":"70010201","displayToPublicDate":"1974-01-01T00:00:00","publicationYear":"1974","noYear":false,"publicationType":{"id":2,"text":"Article"},"publicationSubtype":{"id":10,"text":"Journal Article"},"seriesTitle":{"id":2302,"text":"Journal of Geochemical Exploration","active":true,"publicationSubtype":{"id":10}},"title":"A probe for sampling interstitial waters of stream sediments and bog soils","docAbstract":"<div id=\"abstracts\" class=\"Abstracts u-font-serif\"><div id=\"aep-abstract-id4\" class=\"abstract author\"><div id=\"aep-abstract-sec-id5\"><p><span>A probe for sampling interstitial waters of stream sediments and bog soils is described. Samples can be obtained within a stratigraphic interval of 2–3 cm, to a depth of 60–80 cm, and with little or no contamination of the samples by sediment or air.</span></p></div></div></div><ul id=\"issue-navigation\" class=\"issue-navigation u-margin-s-bottom u-bg-grey1\"></ul>","language":"English","publisher":"Elsevier","doi":"10.1016/0375-6742(74)90034-X","issn":"03756742","usgsCitation":"Nowlan, G., and Carollo, C., 1974, A probe for sampling interstitial waters of stream sediments and bog soils: Journal of Geochemical Exploration, v. 3, no. 2, p. 199-205, https://doi.org/10.1016/0375-6742(74)90034-X.","productDescription":"7 p.","startPage":"199","endPage":"205","numberOfPages":"7","costCenters":[],"links":[{"id":218934,"rank":1,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/thumbnails/outside_thumb.jpg"}],"volume":"3","issue":"2","noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"5059e50ae4b0c8380cd46aab","contributors":{"authors":[{"text":"Nowlan, G.A.","contributorId":99131,"corporation":false,"usgs":true,"family":"Nowlan","given":"G.A.","affiliations":[],"preferred":false,"id":358301,"contributorType":{"id":1,"text":"Authors"},"rank":1},{"text":"Carollo, C.","contributorId":73068,"corporation":false,"usgs":true,"family":"Carollo","given":"C.","email":"","affiliations":[],"preferred":false,"id":358300,"contributorType":{"id":1,"text":"Authors"},"rank":2}]}}
,{"id":70010200,"text":"70010200 - 1974 - 40Ar/39Ar age spectra of some undisturbed terrestrial samples","interactions":[],"lastModifiedDate":"2021-01-28T14:24:09.832532","indexId":"70010200","displayToPublicDate":"1974-01-01T00:00:00","publicationYear":"1974","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":"40Ar/39Ar age spectra of some undisturbed terrestrial samples","docAbstract":"<div id=\"abstracts\" class=\"Abstracts u-font-serif\"><div id=\"aep-abstract-id5\" class=\"abstract author\"><div id=\"aep-abstract-sec-id6\"><p><sup>40</sup>Ar/<sup>39</sup>Ar age spectra and<span>&nbsp;</span><sup>40</sup>Ar/<sup>36</sup>Ar vs<span>&nbsp;</span><sup>39</sup>Ar/<sup>36</sup>Ar isochrons were determined by incremental heating for 11 terrestrial rocks and minerals whose geology indicates that they represent essentially undisturbed systems. The samples include muscovite, biotite, hornblende, sanidine, plagioclase, dacite, diabase and basalt and range in age from 40 to 1700 m.y. For each sample, the<span>&nbsp;</span><sup>40</sup>Ar/<sup>39</sup>Ar ratios, corrected for atmospheric and neutron-generated argon isotopes, are the same for most of the gas fractions released and the age spectra, which show pronounced plateaus, thus are consistent with models previously proposed for undisturbed samples. Plateau ages and isochron ages calculated using plateau age fractions are concordant and appear to be meaningful estimates of the crystallization and cooling ages of these samples. Seemingly anomalous age spectrum points can be attributed entirely to small amounts of previously unrecognized argon loss and to gas fractions that contain too small (less than 2 per cent) a proportion of the<span>&nbsp;</span><sup>39</sup>Ar released to be geologically significant. The use of a quantitative abscissa for age spectrum diagrams is recommended so that the size of each gas fraction is readily apparent. Increments containing less than about 4–5 per cent of the total<span>&nbsp;</span><sup>39</sup>Ar released should be interpreted cautiously. Both the age spectrum and isochron methods of data reduction for incremental heating experiments are worthwhile, as each gives slightly different but complementary information about the sample from the same basic data. Use of a least-squares fit that allows for correlated errors is recommended for<span>&nbsp;</span><sup>40</sup>Ar/<sup>36</sup>Ar vs<span>&nbsp;</span><sup>39</sup>Ar/<sup>36</sup>Ar isochrons. The results indicate that the<span>&nbsp;</span><sup>40</sup>Ar/<sup>39</sup>Ar incremental heating technique can be used to distinguish disturbed from undisturbed rock and mineral systems and will be a valuable geochronological tool in geologically complex terranes.</p></div></div></div>","language":"English","publisher":"Elsevier","doi":"10.1016/0016-7037(74)90146-X","issn":"00167037","usgsCitation":"Dalrymple, G.B., and Lanphere, M.A., 1974, 40Ar/39Ar age spectra of some undisturbed terrestrial samples: Geochimica et Cosmochimica Acta, v. 38, no. 5, p. 715-738, https://doi.org/10.1016/0016-7037(74)90146-X.","productDescription":"24 p.","startPage":"715","endPage":"738","numberOfPages":"24","costCenters":[],"links":[{"id":218933,"rank":0,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/thumbnails/outside_thumb.jpg"}],"volume":"38","issue":"5","noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"5059e261e4b0c8380cd45b25","contributors":{"authors":[{"text":"Dalrymple, G. Brent","contributorId":55146,"corporation":false,"usgs":true,"family":"Dalrymple","given":"G.","email":"","middleInitial":"Brent","affiliations":[],"preferred":false,"id":358299,"contributorType":{"id":1,"text":"Authors"},"rank":1},{"text":"Lanphere, M. A.","contributorId":35298,"corporation":false,"usgs":true,"family":"Lanphere","given":"M.","email":"","middleInitial":"A.","affiliations":[],"preferred":false,"id":358298,"contributorType":{"id":1,"text":"Authors"},"rank":2}]}}
,{"id":70009795,"text":"70009795 - 1974 - The regolith at the Apollo 15 site and its stratigraphic implications","interactions":[],"lastModifiedDate":"2021-02-04T15:12:43.485181","indexId":"70009795","displayToPublicDate":"1974-01-01T00:00:00","publicationYear":"1974","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":"The regolith at the Apollo 15 site and its stratigraphic implications","docAbstract":"<div id=\"abstracts\" class=\"Abstracts u-font-serif\"><div id=\"aep-abstract-id4\" class=\"abstract author\"><div id=\"aep-abstract-sec-id5\"><p>Regolith samples from the Apollo 15 landing site are described in terms of two major fractions, a homogeneous glass fraction and a non-homogeneous glass fraction. The proportions of different components in the homogeneous glass fraction were determined directly by chemical analyses of individual particles. They are mainly green glass, a mare-like glass, and different types of Fra Mauro and Highland type glasses. The proportions of various components in the remainder of each of the soils were determined indirectly by finding the mix of components that best fits their bulk compositions. The mixing model suggests that the Apennine Front consists mainly of rocks of low-K Fra Mauro basalt composition. These may overlie rocks with the composition of anorthositic gabbro. Green glass, which occurs widely throughout the site is believed to be derived from a green glass layer which darkens upland surfaces and lies beneath the local mare surface.</p></div></div></div>","language":"English","publisher":"Elsevier","doi":"10.1016/0016-7037(74)90012-X","issn":"00167037","usgsCitation":"Carr, M.H., and Meyer, C., 1974, The regolith at the Apollo 15 site and its stratigraphic implications: Geochimica et Cosmochimica Acta, v. 38, no. 7, p. 1183-1197, https://doi.org/10.1016/0016-7037(74)90012-X.","productDescription":"15 p.","startPage":"1183","endPage":"1197","numberOfPages":"15","costCenters":[],"links":[{"id":218680,"rank":0,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/thumbnails/outside_thumb.jpg"}],"volume":"38","issue":"7","noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"505baf06e4b08c986b3244d0","contributors":{"authors":[{"text":"Carr, M. H.","contributorId":84727,"corporation":false,"usgs":true,"family":"Carr","given":"M.","email":"","middleInitial":"H.","affiliations":[{"id":131,"text":"Astrogeology Science Center","active":true,"usgs":true}],"preferred":false,"id":357163,"contributorType":{"id":1,"text":"Authors"},"rank":1},{"text":"Meyer, C.E.","contributorId":104023,"corporation":false,"usgs":true,"family":"Meyer","given":"C.E.","email":"","affiliations":[],"preferred":false,"id":357164,"contributorType":{"id":1,"text":"Authors"},"rank":2}]}}
,{"id":70010198,"text":"70010198 - 1974 - Reference samples for the earth sciences","interactions":[],"lastModifiedDate":"2021-02-02T14:26:16.302981","indexId":"70010198","displayToPublicDate":"1974-01-01T00:00:00","publicationYear":"1974","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":"Reference samples for the earth sciences","docAbstract":"<p>A revised list of reference samples of interest to geoscientists has been extended to include samples for the agronomist, the archaeologist and the environmentalist. In addition to the source from which standard samples may be obtained, references or pertinent notes for some samples are included.</p><p>The number of rock reference samples is now almost adequate, and the variety of ore samples will soon be sufficient. There are very few samples for microprobe work. Oil shales will become more important because of the outlook for world petroleum resources. The dryland equivalent of a submarine basalt might be useful in studies of sea-floor spreading and of the geochemistry of basalts.</p><p>The Na- and K-feldspars of BCS (British Chemical Standards—Bureau of Analysed Samples), NBS (National Bureau of Standards), and ANRT (Association Kationale de la Recherche Technique) could serve as trace-element standards if such data were available. Similarly, the present NBS flint and plastic clays, as well as their predecessors, might be useful for archaeological pottery studies. The International Decade for Ocean Exploration may stimulate the preparation of ocean-water standards for trace elements or pollutants and a standard for manganese nodules.</p>","language":"English","publisher":"Elsevier","doi":"10.1016/0016-7037(74)90158-6","issn":"00167037","usgsCitation":"Flanagan, F., 1974, Reference samples for the earth sciences: Geochimica et Cosmochimica Acta, v. 38, no. 12, p. 1731-1744, https://doi.org/10.1016/0016-7037(74)90158-6.","productDescription":"14 p.","startPage":"1731","endPage":"1744","numberOfPages":"14","costCenters":[],"links":[{"id":218931,"rank":0,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/thumbnails/outside_thumb.jpg"}],"volume":"38","issue":"12","noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"50e4a42be4b0e8fec6cdba8c","contributors":{"authors":[{"text":"Flanagan, F.J.","contributorId":50139,"corporation":false,"usgs":true,"family":"Flanagan","given":"F.J.","email":"","affiliations":[],"preferred":false,"id":358295,"contributorType":{"id":1,"text":"Authors"},"rank":1}]}}
,{"id":1003221,"text":"1003221 - 1974 - Monitoring 2,4-D residues at Loxahatchee National Wildlife Refuge","interactions":[],"lastModifiedDate":"2013-03-20T12:44:52","indexId":"1003221","displayToPublicDate":"1974-01-01T00:00:00","publicationYear":"1974","noYear":false,"publicationType":{"id":2,"text":"Article"},"publicationSubtype":{"id":10,"text":"Journal Article"},"seriesTitle":{"id":3038,"text":"Pesticides Monitoring Journal","onlineIssn":" 0031-615","printIssn":" 0031-615","active":true,"publicationSubtype":{"id":10}},"title":"Monitoring 2,4-D residues at Loxahatchee National Wildlife Refuge","docAbstract":"Abstract has not been submitted","largerWorkType":{"id":2,"text":"Article"},"largerWorkTitle":"Pesticides Monitoring Journal","largerWorkSubtype":{"id":10,"text":"Journal Article"},"language":"English","usgsCitation":"Schultz, D., and Whitney, E., 1974, Monitoring 2,4-D residues at Loxahatchee National Wildlife Refuge: Pesticides Monitoring Journal, v. 7, no. 3/4, p. 146-152.","productDescription":"pp. 146-152","startPage":"146","endPage":"152","numberOfPages":"7","costCenters":[{"id":606,"text":"Upper Midwest Environmental Sciences Center","active":true,"usgs":true}],"links":[{"id":133293,"rank":0,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/thumbnails/outside_thumb.jpg"},{"id":269739,"type":{"id":11,"text":"Document"},"url":"https://biodiversitylibrary.org/page/26095456"}],"volume":"7","issue":"3/4","noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"4f4e4a4de4b07f02db6274b6","contributors":{"authors":[{"text":"Schultz, D.P.","contributorId":106054,"corporation":false,"usgs":true,"family":"Schultz","given":"D.P.","email":"","affiliations":[],"preferred":false,"id":312987,"contributorType":{"id":1,"text":"Authors"},"rank":1},{"text":"Whitney, E.W.","contributorId":53347,"corporation":false,"usgs":true,"family":"Whitney","given":"E.W.","email":"","affiliations":[],"preferred":false,"id":312986,"contributorType":{"id":1,"text":"Authors"},"rank":2}]}}
,{"id":70010186,"text":"70010186 - 1974 - Geophysical evidence for the intersection of the St Paul, Cape Palmas and Grand Cess fracture zones with the continental margin of Liberia, West Africa","interactions":[],"lastModifiedDate":"2021-02-02T14:31:18.888522","indexId":"70010186","displayToPublicDate":"1974-01-01T00:00:00","publicationYear":"1974","noYear":false,"publicationType":{"id":2,"text":"Article"},"publicationSubtype":{"id":10,"text":"Journal Article"},"seriesTitle":{"id":2840,"text":"Nature","active":true,"publicationSubtype":{"id":10}},"title":"Geophysical evidence for the intersection of the St Paul, Cape Palmas and Grand Cess fracture zones with the continental margin of Liberia, West Africa","docAbstract":"<div id=\"Abs1-section\" class=\"c-article-section\"><div id=\"Abs1-content\" class=\"c-article-section__content\"><p>PUBLISHED reconstructions of Gondwana continent<sup>1</sup><span>&nbsp;</span>(Fig. l<i>a</i>) show a gap in fit near the junction of the Americas and Africa. To study this critical area, the Unitedgeo I made geophysical measurements and collected rock samples across the continental margin of Liberia (USGS-IDOE cruise leg 5) in November 1971. Figure I<i>b</i><span>&nbsp;</span>indicates the location of the 5,400 km of ship track on a generalised bathymetric map<sup>2</sup>. We shall discuss the data in detail elsewhere. Here we present the evidence for the existence of three fracture zones, two of which have not been reported previously, intersecting the continental margin at the north end of the South Atlantic, which remained closed probably until Cretaceous time. We suggest that Precambrian structures on the African continent controlled the location of these fracture zones. Figure Ic compares gravity and magnetic profiles and interpretations of the seismic profiles for three selected lines (27, 30 and 34) crossing the Grand Cess, Cape Palmas and St Paul fracture zones, respectively.</p></div></div>","language":"English","publisher":"Nature","doi":"10.1038/248324a0","issn":"00280836","usgsCitation":"Behrendt, J.C., Schlee, J., and Robb, J.M., 1974, Geophysical evidence for the intersection of the St Paul, Cape Palmas and Grand Cess fracture zones with the continental margin of Liberia, West Africa: Nature, v. 248, no. 5446, p. 324-326, https://doi.org/10.1038/248324a0.","productDescription":"3 p.","startPage":"324","endPage":"326","numberOfPages":"3","costCenters":[{"id":678,"text":"Woods Hole Coastal and Marine Science Center","active":true,"usgs":true}],"links":[{"id":218709,"rank":0,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/thumbnails/outside_thumb.jpg"}],"volume":"248","issue":"5446","noUsgsAuthors":false,"publicationDate":"1974-03-01","publicationStatus":"PW","scienceBaseUri":"505a2821e4b0c8380cd59e6f","contributors":{"authors":[{"text":"Behrendt, John C. jbehrendt@usgs.gov","contributorId":25945,"corporation":false,"usgs":true,"family":"Behrendt","given":"John","email":"jbehrendt@usgs.gov","middleInitial":"C.","affiliations":[{"id":213,"text":"Crustal Imaging and Characterization Team","active":false,"usgs":true},{"id":218,"text":"Denver Federal Center","active":false,"usgs":true}],"preferred":false,"id":358239,"contributorType":{"id":1,"text":"Authors"},"rank":1},{"text":"Schlee, J.","contributorId":45821,"corporation":false,"usgs":true,"family":"Schlee","given":"J.","affiliations":[],"preferred":false,"id":358240,"contributorType":{"id":1,"text":"Authors"},"rank":2},{"text":"Robb, James M.","contributorId":73272,"corporation":false,"usgs":true,"family":"Robb","given":"James","email":"","middleInitial":"M.","affiliations":[{"id":678,"text":"Woods Hole Coastal and Marine Science Center","active":true,"usgs":true}],"preferred":false,"id":358241,"contributorType":{"id":1,"text":"Authors"},"rank":3}]}}
,{"id":70010172,"text":"70010172 - 1974 - Problems encountered in the use of neutron methods for elemental analysis on planetary surfaces","interactions":[],"lastModifiedDate":"2021-02-02T14:33:16.669442","indexId":"70010172","displayToPublicDate":"1974-01-01T00:00:00","publicationYear":"1974","noYear":false,"publicationType":{"id":2,"text":"Article"},"publicationSubtype":{"id":10,"text":"Journal Article"},"seriesTitle":{"id":2906,"text":"Nuclear Instruments and Methods","active":true,"publicationSubtype":{"id":10}},"title":"Problems encountered in the use of neutron methods for elemental analysis on planetary surfaces","docAbstract":"<div id=\"abstracts\" class=\"Abstracts u-font-serif\"><div id=\"aep-abstract-id8\" class=\"abstract author\"><div id=\"aep-abstract-sec-id9\"><p>From experimental studies of gamma rays from fast and thermal neutron reactions in hydrogeneous and non-hydrogeneous, semi-infinite samples and from Monte Carlo calculations on soil of a composition which might typically be encountered on planetary surfaces, it is found that gamma rays from fast or inelastic scattering reactions would dominate the observed spectra. With the exception of gamma rays formed by inelastically scattered neutrons on oxygen, useful spectra would be limited to energies below 3 MeV. Other experiments were performed which show that if a gamma-ray detector were placed within 6 m of an isotopic neutron source in a spacecraft, it would be rendered useless for gamma-ray spectrometry below 3 MeV because of internal activation produced by neutron exposure during space travel. Adequate shielding is not practicable because of the size and weight constraints for planetary missions. Thus, it is required that the source be turned off or removed to a safe distance during non-measurement periods. In view of these results an accelerator or an off-on isotopic source would be desirable for practical gamma-ray spectral analysis on planetary surfaces containing but minor amounts of hydrogen.</p></div></div></div><ul id=\"issue-navigation\" class=\"issue-navigation u-margin-s-bottom u-bg-grey1\"></ul>","language":"English","publisher":"Elsevier","doi":"10.1016/0029-554X(74)90289-4","issn":"0029554X","usgsCitation":"Senftle, F., Philbin, P., Moxham, R., Boynton, G., and Trombka, J., 1974, Problems encountered in the use of neutron methods for elemental analysis on planetary surfaces: Nuclear Instruments and Methods, v. 117, no. 2, p. 435-443, https://doi.org/10.1016/0029-554X(74)90289-4.","productDescription":"9 p.","startPage":"435","endPage":"443","numberOfPages":"9","costCenters":[],"links":[{"id":219671,"rank":0,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/thumbnails/outside_thumb.jpg"}],"volume":"117","issue":"2","noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"505a8cd5e4b0c8380cd7e8f2","contributors":{"authors":[{"text":"Senftle, F.","contributorId":24451,"corporation":false,"usgs":true,"family":"Senftle","given":"F.","affiliations":[],"preferred":false,"id":358195,"contributorType":{"id":1,"text":"Authors"},"rank":1},{"text":"Philbin, P.","contributorId":19285,"corporation":false,"usgs":true,"family":"Philbin","given":"P.","affiliations":[],"preferred":false,"id":358194,"contributorType":{"id":1,"text":"Authors"},"rank":2},{"text":"Moxham, R.","contributorId":86100,"corporation":false,"usgs":true,"family":"Moxham","given":"R.","email":"","affiliations":[],"preferred":false,"id":358198,"contributorType":{"id":1,"text":"Authors"},"rank":3},{"text":"Boynton, G.","contributorId":48701,"corporation":false,"usgs":true,"family":"Boynton","given":"G.","affiliations":[],"preferred":false,"id":358196,"contributorType":{"id":1,"text":"Authors"},"rank":4},{"text":"Trombka, J.","contributorId":74135,"corporation":false,"usgs":true,"family":"Trombka","given":"J.","email":"","affiliations":[],"preferred":false,"id":358197,"contributorType":{"id":1,"text":"Authors"},"rank":5}]}}
,{"id":70175504,"text":"70175504 - 1974 - Flood stages and discharges for small streams in Texas : compilation of data through September 1972","interactions":[],"lastModifiedDate":"2016-08-15T15:00:06","indexId":"70175504","displayToPublicDate":"1974-01-01T00:00:00","publicationYear":"1974","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":"Flood stages and discharges for small streams in Texas : compilation of data through September 1972","docAbstract":"<p>No abstract available.</p>","language":"English","publisher":"U.S. Geological Survey","doi":"10.3133/70175504","usgsCitation":"Schroeder, E., 1974, Flood stages and discharges for small streams in Texas : compilation of data through September 1972: Open-File Report, Report: ix, 283 p.; Plate, https://doi.org/10.3133/70175504.","productDescription":"Report: ix, 283 p.; Plate","onlineOnly":"N","additionalOnlineFiles":"N","costCenters":[{"id":583,"text":"Texas Water Science Center","active":true,"usgs":true}],"links":[{"id":326501,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/thumbnails/usgs_thumb.jpg"}],"noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"57b2e7bae4b03bcb0102e8ac","contributors":{"authors":[{"text":"Schroeder, E.E.","contributorId":19970,"corporation":false,"usgs":true,"family":"Schroeder","given":"E.E.","email":"","affiliations":[],"preferred":false,"id":645513,"contributorType":{"id":1,"text":"Authors"},"rank":1}]}}
]}