{"pageNumber":"6498","pageRowStart":"162425","pageSize":"25","recordCount":185159,"records":[{"id":70176049,"text":"70176049 - 1969 - Records of wells and springs, San Antonio area, Texas","interactions":[],"lastModifiedDate":"2016-08-24T11:25:02","indexId":"70176049","displayToPublicDate":"1969-01-01T00:00:00","publicationYear":"1969","noYear":false,"publicationType":{"id":18,"text":"Report"},"publicationSubtype":{"id":2,"text":"State or Local Government Series"},"title":"Records of wells and springs, San Antonio area, Texas","docAbstract":"<p>No abstract available.</p>","language":"English","publisher":"Edwards Underground Water District","usgsCitation":"Rettman, P., 1969, Records of wells and springs, San Antonio area, Texas, 29 p.","productDescription":"29 p.","onlineOnly":"N","additionalOnlineFiles":"N","costCenters":[{"id":583,"text":"Texas Water Science Center","active":true,"usgs":true}],"links":[{"id":327785,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/thumbnails/outside_thumb.jpg"}],"noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"57c6b0ffe4b0f2f0cebe66b0","contributors":{"authors":[{"text":"Rettman, Paul","contributorId":68699,"corporation":false,"usgs":true,"family":"Rettman","given":"Paul","affiliations":[],"preferred":false,"id":646937,"contributorType":{"id":1,"text":"Authors"},"rank":1}]}}
,{"id":1000121,"text":"1000121 - 1969 - Cisco (<i>Coregonus artedii</i>) mortalities in a southern Michigan lake, July 1968","interactions":[],"lastModifiedDate":"2016-02-18T11:06:58","indexId":"1000121","displayToPublicDate":"1969-01-01T00:00:00","publicationYear":"1969","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":"Cisco (<i>Coregonus artedii</i>) mortalities in a southern Michigan lake, July 1968","docAbstract":"<p>Cisco die-offs are common in the summer in certain lakes of northern Indiana and southern Michigan, along the southern boundary of the national distribution of coregonine fishes. Although numerous cisco die-offs have been reported, few, if any, have been accompanied by environmental information at the time of the die-off. On 31 July and 1 August 1968, we investigated a cisco die-off on Halfmoon Lake, on the border of Washtenaw and Livingston Counties, Michigan.</p>","language":"English","publisher":"Wiley","doi":"10.4319/lo.1969.14.6.0958","usgsCitation":"Colby, P.J., and Brooke, L.T., 1969, Cisco (<i>Coregonus artedii</i>) mortalities in a southern Michigan lake, July 1968: Limnology and Oceanography, v. 14, no. 6, p. 958-960, https://doi.org/10.4319/lo.1969.14.6.0958.","productDescription":"3 p.","startPage":"958","endPage":"960","onlineOnly":"N","additionalOnlineFiles":"N","costCenters":[{"id":324,"text":"Great Lakes Science Center","active":true,"usgs":true}],"links":[{"id":480323,"rank":1,"type":{"id":40,"text":"Open Access Publisher Index Page"},"url":"https://doi.org/10.4319/lo.1969.14.6.0958","text":"Publisher Index Page"},{"id":132856,"rank":0,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/thumbnails/outside_thumb.jpg"}],"volume":"14","issue":"6","noUsgsAuthors":false,"publicationDate":"2003-12-22","publicationStatus":"PW","scienceBaseUri":"4f4e49dfe4b07f02db5e32f9","contributors":{"authors":[{"text":"Colby, Peter J.","contributorId":89831,"corporation":false,"usgs":true,"family":"Colby","given":"Peter","email":"","middleInitial":"J.","affiliations":[],"preferred":false,"id":308108,"contributorType":{"id":1,"text":"Authors"},"rank":1},{"text":"Brooke, Larry T.","contributorId":99100,"corporation":false,"usgs":true,"family":"Brooke","given":"Larry","email":"","middleInitial":"T.","affiliations":[],"preferred":false,"id":308109,"contributorType":{"id":1,"text":"Authors"},"rank":2}]}}
,{"id":1000318,"text":"1000318 - 1969 - Insecticides and the Great Lakes","interactions":[],"lastModifiedDate":"2012-02-02T00:04:41","indexId":"1000318","displayToPublicDate":"1969-01-01T00:00:00","publicationYear":"1969","noYear":false,"publicationType":{"id":2,"text":"Article"},"publicationSubtype":{"id":10,"text":"Journal Article"},"seriesTitle":{"id":2623,"text":"Limnos","active":true,"publicationSubtype":{"id":10}},"title":"Insecticides and the Great Lakes","docAbstract":"Cracks in the perfect image of DDT appeared when traces of the insecticide began to show up in a wide variety of organisms throughout the world.  As more and more people investigated this problem, it became increasingly evident that terrestrial and aquatic animals were accumulating comparatively high concentrations of DDT from extremely low levels in their environment.  It also became apparent that DDT and all of the other chlorinated hydrocarbon insecticides were not species-specific, but were toxic to all forms of animal life including man.  In 1965, when the Great Lakes Fishery Laboratory of the U.S. Bureau of Commercial Fisheries began to monitor pesticide residues in fish from the Great Lakes, it was discovered that the fish contained not only DDT, but also dieldrin, another chlorinated hydrocarbon insecticide.  Fish from Lake Michigan in particular contained relatively high levels of both of these insecticides; concentrations of DDT were in the parts per million (ppm) range, a factor at least several million times greater than the few parts per trillion found in the water.  Two questions presented themselves: first, How did these insecticides get into the water? and second, How did the fish build up such high concentrations in their bodies from such low concentrations in the water?","largerWorkType":{"id":2,"text":"Article"},"largerWorkTitle":"Limnos","largerWorkSubtype":{"id":10,"text":"Journal Article"},"language":"English","collaboration":"Out-of-print","usgsCitation":"Reinert, R.E., 1969, Insecticides and the Great Lakes: Limnos, v. 2, no. 3, p. 3-9.","productDescription":"p. 3-9","startPage":"3","endPage":"9","numberOfPages":"6","costCenters":[{"id":324,"text":"Great Lakes Science Center","active":true,"usgs":true}],"links":[{"id":133130,"rank":0,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/thumbnails/outside_thumb.jpg"}],"volume":"2","issue":"3","noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"4f4e4a80e4b07f02db6497ad","contributors":{"authors":[{"text":"Reinert, Robert E.","contributorId":101214,"corporation":false,"usgs":true,"family":"Reinert","given":"Robert","email":"","middleInitial":"E.","affiliations":[],"preferred":false,"id":308381,"contributorType":{"id":1,"text":"Authors"},"rank":1}]}}
,{"id":70011611,"text":"70011611 - 1969 - Heat flow measurements on the southeast coast of Australia","interactions":[],"lastModifiedDate":"2020-11-29T17:55:48.524254","indexId":"70011611","displayToPublicDate":"1969-01-01T00:00:00","publicationYear":"1969","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 measurements on the southeast coast of Australia","docAbstract":"<div id=\"abstracts\" class=\"Abstracts u-font-serif\"><div id=\"ab1\" class=\"abstract author\" lang=\"en\"><div id=\"aep-abstract-sec-id7\"><p>Three boreholes have been drilled for the Australian National University near the southeast coast of New South Wales, Australia. The heat flows found are 1.1, 1.0, and 1.3 μcal/cm<sup>2</sup>sec. The errors resulting from the proximity of the sea and a lake, surface temperature change, conductivity structure and water flow have been examined. The radioactive heat production in some of the intrusive rocks of the area have also been measured. The heat flows are much lower than the values of about 2.0 found elsewhere in south eastern Australia. The lower values appear to be part of a distinct heat flow province in eastern Australia.</p></div></div></div>","language":"English","publisher":"Elsevier","doi":"10.1016/0012-821X(69)90004-1","issn":"0012821X","usgsCitation":"Hyndman, R., Jaeger, J., and Sass, J., 1969, Heat flow measurements on the southeast coast of Australia: Earth and Planetary Science Letters, v. 7, no. 1, p. 12-16, https://doi.org/10.1016/0012-821X(69)90004-1.","productDescription":"5 p.","startPage":"12","endPage":"16","numberOfPages":"5","costCenters":[],"links":[{"id":220850,"rank":0,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/thumbnails/outside_thumb.jpg"}],"country":"Australia","geographicExtents":"{\n  \"type\": \"FeatureCollection\",\n  \"features\": [\n    {\n      \"type\": \"Feature\",\n      \"properties\": {},\n      \"geometry\": {\n        \"type\": \"Polygon\",\n        \"coordinates\": [\n          [\n            [\n              148.86474609375,\n              -38.496593518947556\n            ],\n            [\n              151.01806640625,\n              -38.496593518947556\n            ],\n            [\n              151.01806640625,\n              -34.27083595164999\n            ],\n            [\n              148.86474609375,\n              -34.27083595164999\n            ],\n            [\n              148.86474609375,\n              -38.496593518947556\n            ]\n          ]\n        ]\n      }\n    }\n  ]\n}","volume":"7","issue":"1","noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"505a3003e4b0c8380cd5d2cc","contributors":{"authors":[{"text":"Hyndman, R.D.","contributorId":45831,"corporation":false,"usgs":true,"family":"Hyndman","given":"R.D.","email":"","affiliations":[],"preferred":false,"id":361538,"contributorType":{"id":1,"text":"Authors"},"rank":1},{"text":"Jaeger, J.C.","contributorId":54217,"corporation":false,"usgs":false,"family":"Jaeger","given":"J.C.","email":"","affiliations":[{"id":16691,"text":"Research School of Earth Sciences, Australian National University","active":true,"usgs":false}],"preferred":false,"id":361539,"contributorType":{"id":1,"text":"Authors"},"rank":2},{"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":361540,"contributorType":{"id":1,"text":"Authors"},"rank":3}]}}
,{"id":70011507,"text":"70011507 - 1969 - A paleomagnetic study of secular variation in New Zealand","interactions":[],"lastModifiedDate":"2020-11-29T18:07:51.155521","indexId":"70011507","displayToPublicDate":"1969-01-01T00:00:00","publicationYear":"1969","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":"A paleomagnetic study of secular variation in New Zealand","docAbstract":"<div id=\"abstracts\" class=\"Abstracts u-font-serif\"><div id=\"aep-abstract-id4\" class=\"abstract author\"><div id=\"aep-abstract-sec-id5\"><p>Ancient secular variation in New Zealand was determined from paleomagnetic measurements on 22 volcanic formations with ages of less than 0.68 m.y. The angular standard deviation from the field of an axial dipole is 13.2° with 95% confidence limits between 10.9° and 16.7°. The angular standard deviation of the corresponding virtual geomagnetic poles is 19.6° with confidence limits between 16.2° and 24.7°. These values are larger than those predicted by most models for secular variation. No difference was detected between the angular secular variation in New Zealand and that at the same latitude in North America.</p></div></div></div>","language":"English","publisher":"Elsevier","doi":"10.1016/0012-821X(69)90165-4","issn":"0012821X","usgsCitation":"Cox, A., 1969, A paleomagnetic study of secular variation in New Zealand: Earth and Planetary Science Letters, v. 6, no. 4, p. 257-267, https://doi.org/10.1016/0012-821X(69)90165-4.","productDescription":"11 p.","startPage":"257","endPage":"267","numberOfPages":"11","costCenters":[],"links":[{"id":221294,"rank":0,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/thumbnails/outside_thumb.jpg"}],"country":"New Zealand","geographicExtents":"{\"type\":\"FeatureCollection\",\"features\":[{\"type\":\"Feature\",\"geometry\":{\"type\":\"MultiPolygon\",\"coordinates\":[[[[173.02037,-40.91905],[173.24723,-41.332],[173.95841,-40.9267],[174.24759,-41.34916],[174.24852,-41.77001],[173.87645,-42.23318],[173.22274,-42.97004],[172.71125,-43.37229],[173.08011,-43.85334],[172.30858,-43.86569],[171.45293,-44.24252],[171.18514,-44.8971],[170.6167,-45.90893],[169.83142,-46.35577],[169.33233,-46.64124],[168.41135,-46.61994],[167.76374,-46.2902],[166.67689,-46.21992],[166.50914,-45.8527],[167.04642,-45.11094],[168.30376,-44.12397],[168.94941,-43.93582],[169.66781,-43.55533],[170.52492,-43.03169],[171.12509,-42.51275],[171.56971,-41.76742],[171.94871,-41.51442],[172.09723,-40.9561],[172.79858,-40.49396],[173.02037,-40.91905]]],[[[174.61201,-36.1564],[175.33662,-37.2091],[175.3576,-36.52619],[175.80889,-36.79894],[175.95849,-37.55538],[176.7632,-37.88125],[177.43881,-37.96125],[178.01035,-37.57982],[178.51709,-37.69537],[178.27473,-38.58281],[177.97046,-39.16634],[177.20699,-39.14578],[176.93998,-39.44974],[177.03295,-39.87994],[176.88582,-40.06598],[176.50802,-40.60481],[176.01244,-41.28962],[175.23957,-41.68831],[175.0679,-41.42589],[174.65097,-41.28182],[175.22763,-40.45924],[174.90016,-39.90893],[173.82405,-39.50885],[173.85226,-39.1466],[174.5748,-38.79768],[174.74347,-38.02781],[174.69702,-37.38113],[174.29203,-36.71109],[174.319,-36.53482],[173.841,-36.12198],[173.05417,-35.23713],[172.63601,-34.52911],[173.00704,-34.45066],[173.5513,-35.00618],[174.32939,-35.2655],[174.61201,-36.1564]]]]},\"properties\":{\"name\":\"New Zealand\"}}]}","volume":"6","issue":"4","noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"5059e4d0e4b0c8380cd46947","contributors":{"authors":[{"text":"Cox, A.","contributorId":89266,"corporation":false,"usgs":true,"family":"Cox","given":"A.","email":"","affiliations":[],"preferred":false,"id":361287,"contributorType":{"id":1,"text":"Authors"},"rank":1}]}}
,{"id":70011612,"text":"70011612 - 1969 - Surface area of vermiculite with nitrogen and carbon dioxide as adsorbates","interactions":[],"lastModifiedDate":"2018-01-25T14:36:50","indexId":"70011612","displayToPublicDate":"1969-01-01T00:00:00","publicationYear":"1969","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":"Surface area of vermiculite with nitrogen and carbon dioxide as adsorbates","docAbstract":"<p>Surface-area studies were made on several homoionic vermiculites with both nitrogen and carbon dioxide as adsorbates. These studies show that only very slight penetration occurs between individual vermiculite platelets. This is in contrast to an earlier investigation of montmorillonite where it was found that the degree of penetration between layers is quite high, particularly for carbon dioxide, and is governed by the size and charge of the interlayer cation. The inability of these adsorbates to penetrate substantially between vermiculite platelets is due primarily to this mineral's high surface-charge density.</p><p>The extent of penetration of nitrogen and carbon dioxide at the edges of vermiculite platelets, though slight, is influenced by the coordinated water retained within the sample at a given degassing temperature. Forces between layers are weakened with increasing water content, which permits slightly greater penetration by adsorbate gases. Thus, the surface area of vermiculite, as determined by gas adsorption, is larger than the calculated external surface area based upon particle size and shape considerations. In addition, \"extra\" surface is provided by the lifting and scrolling of terminal platelets. These morphological features are shown in scanning electron micrographs of a naturally occuring vermiculite.</p>","language":"English","publisher":"The Clay Minerals Society","doi":"10.1346/CCMN.1969.0170403","usgsCitation":"Thomas, J., and Bohor, B., 1969, Surface area of vermiculite with nitrogen and carbon dioxide as adsorbates: Clays and Clay Minerals, v. 17, no. 4, p. 205-209, https://doi.org/10.1346/CCMN.1969.0170403.","productDescription":"5 p.","startPage":"205","endPage":"209","costCenters":[],"links":[{"id":220851,"rank":0,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/thumbnails/outside_thumb.jpg"}],"volume":"17","issue":"4","noUsgsAuthors":false,"publicationDate":"2024-07-01","publicationStatus":"PW","scienceBaseUri":"505b9f95e4b08c986b31e6b0","contributors":{"authors":[{"text":"Thomas, Josephus Jr.","contributorId":11755,"corporation":false,"usgs":false,"family":"Thomas","given":"Josephus","suffix":"Jr.","email":"","affiliations":[],"preferred":false,"id":361541,"contributorType":{"id":1,"text":"Authors"},"rank":1},{"text":"Bohor, Bruce F.","contributorId":104823,"corporation":false,"usgs":true,"family":"Bohor","given":"Bruce F.","affiliations":[],"preferred":false,"id":361542,"contributorType":{"id":1,"text":"Authors"},"rank":2}]}}
,{"id":70011424,"text":"70011424 - 1969 - Chemical composition of selected Kansas brines as an aid to interpreting change in water chemistry with depth","interactions":[],"lastModifiedDate":"2020-11-29T18:29:02.44387","indexId":"70011424","displayToPublicDate":"1969-01-01T00:00:00","publicationYear":"1969","noYear":false,"publicationType":{"id":2,"text":"Article"},"publicationSubtype":{"id":10,"text":"Journal Article"},"seriesTitle":{"id":1213,"text":"Chemical Geology","active":true,"publicationSubtype":{"id":10}},"title":"Chemical composition of selected Kansas brines as an aid to interpreting change in water chemistry with depth","docAbstract":"<p id=\"simple-para.0010\">Chemical analyses of approximately 1,881 samples of water from selected Kansas brines define the variations of water chemistry with depth and aquifer age. The most concentrated brines are found in the Permian rocks which occupy the intermediate section of the geologic column of this area. Salinity decreases below the Permian until the Ordovician (Arbuckle) horizon is reached and then increases until the Precambrian basement rocks are reached. Chemically, the petroleum brines studied in this small area fit the generally accepted pattern of an increase in calcium, sodium and chloride content with increasing salinity. They do not fit the often-predicted trend of increases in the calcium to chloride ratio, calcium content and salinity with depth and geologic age. The calcium to chloride ratio tends to be asymptotic to about 0.2 with increasing chloride content. Sulfate tends to decrease with increasing calcium content. Bicarbonate content is relatively constant with depth.</p><p id=\"simple-para.0015\">If many of the hypotheses concerning the chemistry of petroleum brines are valid, then the brines studied are anomolous. An alternative lies in accepting the thesis that exceptions to these hypotheses are rapidly becoming the rule and that indeed we still do not have a valid and general hypothesis to explain the origin and chemistry of petroleum brines.</p>","language":"English","publisher":"Elsevier","doi":"10.1016/0009-2541(69)90053-9","issn":"00092541","usgsCitation":"Dingman, R., and Angino, E., 1969, Chemical composition of selected Kansas brines as an aid to interpreting change in water chemistry with depth: Chemical Geology, v. 4, no. 1-2, p. 325-339, https://doi.org/10.1016/0009-2541(69)90053-9.","productDescription":"15 p.","startPage":"325","endPage":"339","numberOfPages":"15","costCenters":[],"links":[{"id":221044,"rank":0,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/thumbnails/outside_thumb.jpg"}],"country":"United 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 \"}}]}","volume":"4","issue":"1-2","noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"5059f569e4b0c8380cd4c1f7","contributors":{"authors":[{"text":"Dingman, R.J.","contributorId":40645,"corporation":false,"usgs":true,"family":"Dingman","given":"R.J.","email":"","affiliations":[],"preferred":false,"id":361070,"contributorType":{"id":1,"text":"Authors"},"rank":1},{"text":"Angino, E.E.","contributorId":8972,"corporation":false,"usgs":true,"family":"Angino","given":"E.E.","email":"","affiliations":[],"preferred":false,"id":361069,"contributorType":{"id":1,"text":"Authors"},"rank":2}]}}
,{"id":70011506,"text":"70011506 - 1969 - Dilemma posed by uranium-series dates on archaeologically significant bones from Valsequillo, Puebla, Mexico","interactions":[],"lastModifiedDate":"2020-11-29T18:10:04.921448","indexId":"70011506","displayToPublicDate":"1969-01-01T00:00:00","publicationYear":"1969","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":"Dilemma posed by uranium-series dates on archaeologically significant bones from Valsequillo, Puebla, Mexico","docAbstract":"<div id=\"abstracts\" class=\"Abstracts u-font-serif\"><div id=\"aep-abstract-id7\" class=\"abstract author\"><div id=\"aep-abstract-sec-id8\"><p>In an attempt to date stone artifacts of Early Man excavated from several sites at the Valsequillo Reservoir, a few kilometers south of Puebla, Mexico, Szabo applied the uranium-series method on bone samples known to be either from the same geologic formation as the sites or in direct association with the artifacts. The geologic context of the bones was studied by Malde, and the archaeological sites were excavated by Irwin-Williams. A date determined for bone associated with an artifact (Caulapan sample M-B-6, see below) agrees with a radiocarbon date for fossil mollusks in the same bed and indicates man's presence more than 20 000 years ago. However, some of these bone dates exceed 200 000 years. Because such dates for man in North America conflict with all prior archaeological evidence here and abroad, we are confronted by a dilemna — either to defend the dates against an onslaught of archaeological thought, or to abandon the uranium method in this application as being so much wasted effort. Faced with these equally undesirable alternatives, and unable to decide where the onus fairly lies (if a choice must be made), we give the uranium-series dates as a possible stimulus for further mutual work in isotopic dating of archaeological material. A sample from the Lindenmeier archaeological site north of Fort Collins and another from a Pleistocene terrace along the Arkansas River, both in Colorado, were also dated.</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(69)90163-0","issn":"0012821X","usgsCitation":"Szabo, B.J., Malde, H., and Irwin-Williams, C., 1969, Dilemma posed by uranium-series dates on archaeologically significant bones from Valsequillo, Puebla, Mexico: Earth and Planetary Science Letters, v. 6, no. 4, p. 237-244, https://doi.org/10.1016/0012-821X(69)90163-0.","productDescription":"8 p.","startPage":"237","endPage":"244","numberOfPages":"8","costCenters":[],"links":[{"id":221293,"rank":0,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/thumbnails/outside_thumb.jpg"}],"country":"Mexico","otherGeospatial":"Puebla","geographicExtents":"{\n  \"type\": \"FeatureCollection\",\n  \"features\": [\n    {\n      \"type\": \"Feature\",\n      \"properties\": {},\n      \"geometry\": {\n        \"type\": \"Polygon\",\n        \"coordinates\": [\n          [\n            [\n              -98.7396240234375,\n              18.411866765202845\n            ],\n            [\n              -97.22900390625,\n              18.411866765202845\n            ],\n            [\n              -97.22900390625,\n              19.68397023588844\n            ],\n            [\n              -98.7396240234375,\n              19.68397023588844\n            ],\n            [\n              -98.7396240234375,\n              18.411866765202845\n            ]\n          ]\n        ]\n      }\n    }\n  ]\n}","volume":"6","issue":"4","noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"505a019fe4b0c8380cd4fc9b","contributors":{"authors":[{"text":"Szabo, Barney J.","contributorId":6848,"corporation":false,"usgs":true,"family":"Szabo","given":"Barney","email":"","middleInitial":"J.","affiliations":[],"preferred":false,"id":361284,"contributorType":{"id":1,"text":"Authors"},"rank":1},{"text":"Malde, H.E.","contributorId":65863,"corporation":false,"usgs":true,"family":"Malde","given":"H.E.","affiliations":[],"preferred":false,"id":361286,"contributorType":{"id":1,"text":"Authors"},"rank":2},{"text":"Irwin-Williams, C.","contributorId":64388,"corporation":false,"usgs":true,"family":"Irwin-Williams","given":"C.","email":"","affiliations":[],"preferred":false,"id":361285,"contributorType":{"id":1,"text":"Authors"},"rank":3}]}}
,{"id":70011528,"text":"70011528 - 1969 - Equipment and techniques for low-altitude aerial sensing of water-vapor concentration and movement","interactions":[],"lastModifiedDate":"2020-11-29T18:06:39.211886","indexId":"70011528","displayToPublicDate":"1969-01-01T00:00:00","publicationYear":"1969","noYear":false,"publicationType":{"id":2,"text":"Article"},"publicationSubtype":{"id":10,"text":"Journal Article"},"seriesTitle":{"id":3254,"text":"Remote Sensing of Environment","printIssn":"0034-4257","active":true,"publicationSubtype":{"id":10}},"title":"Equipment and techniques for low-altitude aerial sensing of water-vapor concentration and movement","docAbstract":"<div id=\"abstracts\" class=\"Abstracts u-font-serif\"><div id=\"ab1\" class=\"abstract author\" lang=\"en\"><div id=\"aep-abstract-sec-id2\"><p>Progress in the development of equipment and techniques for making rapid measurements of moisture movement through the atmosphere over a large area is described. Airborne sensing elements measure relative humidity, temperature, and air currents. These data are telemetered to a ground-based station and recorded. A radar unit tracks the aircraft and electronically plots its position on a base map of the area being studied. Thus the distribution of atmospheric conditions can be directly related to the underlying terrain and vegetation features.</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/S0034-4257(69)90044-3","issn":"00344257","usgsCitation":"Howell, R., 1969, Equipment and techniques for low-altitude aerial sensing of water-vapor concentration and movement: Remote Sensing of Environment, v. 1, no. 1, p. 13-18, https://doi.org/10.1016/S0034-4257(69)90044-3.","productDescription":"6 p.","startPage":"13","endPage":"18","numberOfPages":"6","costCenters":[],"links":[{"id":221757,"rank":0,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/thumbnails/outside_thumb.jpg"}],"volume":"1","issue":"1","noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"505a0a2ae4b0c8380cd5221c","contributors":{"authors":[{"text":"Howell, R.L.","contributorId":90041,"corporation":false,"usgs":true,"family":"Howell","given":"R.L.","email":"","affiliations":[],"preferred":false,"id":361327,"contributorType":{"id":1,"text":"Authors"},"rank":1}]}}
,{"id":70011502,"text":"70011502 - 1969 - Pecoraite, Ni6Si4O10(OH)8, nickel analog of clinochrysotile, formed in the wolf creek meteorite","interactions":[],"lastModifiedDate":"2019-11-27T07:39:21","indexId":"70011502","displayToPublicDate":"1969-01-01T00:00:00","publicationYear":"1969","noYear":false,"publicationType":{"id":2,"text":"Article"},"publicationSubtype":{"id":10,"text":"Journal Article"},"seriesTitle":{"id":3338,"text":"Science","active":true,"publicationSubtype":{"id":10}},"title":"Pecoraite, Ni6Si4O10(OH)8, nickel analog of clinochrysotile, formed in the wolf creek meteorite","docAbstract":"Pecoraite is a new phase in the natural system H2O-NiO-MgO- SiO2, the nickel analog of clinochrysotile. It occurs in cracks in the Wolf Creek meteorite in Australia where it was formed under hydrothermal conditions. Particles of pecoraite are very small curved plates which have begun to coil; some have achieved spiral form.","language":"English","publisher":"Science","doi":"10.1126/science.165.3888.59","issn":"00368075","usgsCitation":"Faust, G.T., Fahey, J.J., Mason, B., and Dwornik, E., 1969, Pecoraite, Ni6Si4O10(OH)8, nickel analog of clinochrysotile, formed in the wolf creek meteorite: Science, v. 165, no. 3888, p. 59-60, https://doi.org/10.1126/science.165.3888.59.","productDescription":"2 p. ","startPage":"59","endPage":"60","numberOfPages":"2","costCenters":[],"links":[{"id":221179,"rank":0,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/thumbnails/outside_thumb.jpg"}],"country":"Australia ","geographicExtents":"{\"type\":\"FeatureCollection\",\"features\":[{\"type\":\"Feature\",\"geometry\":{\"type\":\"MultiPolygon\",\"coordinates\":[[[[145.39798,-40.79255],[146.36412,-41.1377],[146.90858,-41.00055],[147.68926,-40.80826],[148.28907,-40.87544],[148.35986,-42.06245],[148.0173,-42.40702],[147.91405,-43.21152],[147.56456,-42.93769],[146.87034,-43.6346],[146.66333,-43.58085],[146.04838,-43.54974],[145.43193,-42.69378],[145.29509,-42.03361],[144.71807,-41.16255],[144.74375,-40.70398],[145.39798,-40.79255]]],[[[143.56181,-13.76366],[143.9221,-14.54831],[144.56371,-14.17118],[144.89491,-14.59446],[145.37472,-14.98498],[145.27199,-15.42821],[145.48526,-16.28567],[145.63703,-16.78492],[145.8889,-16.90693],[146.16031,-17.76165],[146.06367,-18.28007],[146.38748,-18.95827],[147.47108,-19.48072],[148.1776,-19.95594],[148.84841,-20.39121],[148.71747,-20.63347],[149.28942,-21.26051],[149.67834,-22.34251],[150.07738,-22.12278],[150.48294,-22.55614],[150.72727,-22.4024],[150.89955,-23.46224],[151.60918,-24.07626],[152.07354,-24.45789],[152.8552,-25.2675],[153.13616,-26.07117],[153.16195,-26.64132],[153.09291,-27.2603],[153.56947,-28.11007],[153.51211,-28.99508],[153.3391,-29.4582],[153.06924,-30.35024],[153.0896,-30.92364],[152.89158,-31.64045],[152.45,-32.55],[151.70912,-33.04134],[151.34397,-33.81602],[151.01056,-34.31036],[150.71414,-35.17346],[150.32822,-35.67188],[150.07521,-36.42021],[149.94612,-37.10905],[149.99728,-37.42526],[149.42388,-37.77268],[148.30462,-37.80906],[147.38173,-38.21922],[146.92212,-38.60653],[146.31792,-39.03576],[145.48965,-38.59377],[144.87698,-38.41745],[145.03221,-37.89619],[144.48568,-38.08532],[143.60997,-38.80947],[142.74543,-38.53827],[142.17833,-38.38003],[141.60658,-38.30851],[140.63858,-38.01933],[139.99216,-37.40294],[139.80659,-36.6436],[139.57415,-36.13836],[139.08281,-35.73275],[138.12075,-35.6123],[138.44946,-35.12726],[138.20756,-34.38472],[137.71917,-35.07683],[136.82941,-35.26053],[137.35237,-34.70734],[137.50389,-34.13027],[137.89012,-33.64048],[137.81033,-32.90001],[136.99684,-33.75277],[136.37207,-34.09477],[135.98904,-34.89012],[135.20821,-34.47867],[135.23922,-33.94795],[134.61342,-33.22278],[134.0859,-32.84807],[134.2739,-32.61723],[132.99078,-32.01122],[132.28808,-31.98265],[131.32633,-31.4958],[129.53579,-31.59042],[128.24094,-31.94849],[127.10287,-32.28227],[126.14871,-32.21597],[125.08862,-32.72875],[124.22165,-32.95949],[124.02895,-33.48385],[123.65967,-33.89018],[122.81104,-33.91447],[122.18306,-34.0034],[121.29919,-33.82104],[120.58027,-33.93018],[119.8937,-33.97607],[119.2989,-34.50937],[119.00734,-34.46415],[118.50572,-34.74682],[118.02497,-35.06473],[117.29551,-35.02546],[116.62511,-35.0251],[115.56435,-34.38643],[115.02681,-34.19652],[115.04862,-33.62343],[115.54512,-33.48726],[115.71467,-33.25957],[115.67938,-32.90037],[115.80165,-32.20506],[115.68961,-31.61244],[115.16091,-30.60159],[114.99704,-30.03072],[115.04004,-29.4611],[114.64197,-28.81023],[114.6165,-28.5164],[114.17358,-28.11808],[114.04888,-27.33477],[113.4775,-26.54313],[113.33895,-26.11655],[113.77836,-26.54903],[113.44096,-25.62128],[113.9369,-25.91123],[114.23285,-26.29845],[114.21616,-25.78628],[113.72126,-24.99894],[113.62534,-24.68397],[113.39352,-24.38476],[113.50204,-23.80635],[113.70699,-23.56022],[113.84342,-23.05999],[113.73655,-22.47548],[114.14976,-21.75588],[114.22531,-22.51749],[114.64776,-21.82952],[115.46017,-21.49517],[115.94737,-21.06869],[116.71162,-20.70168],[117.16632,-20.6236],[117.44155,-20.7469],[118.22956,-20.37421],[118.83609,-20.26331],[118.98781,-20.0442],[119.25249,-19.95294],[119.80523,-19.97651],[120.85622,-19.68371],[121.39986,-19.23976],[121.65514,-18.70532],[122.24167,-18.19765],[122.28662,-17.7986],[122.31277,-17.25497],[123.01257,-16.4052],[123.43379,-17.26856],[123.85934,-17.06904],[123.50324,-16.59651],[123.81707,-16.11132],[124.25829,-16.32794],[124.37973,-15.56706],[124.92615,-15.0751],[125.16728,-14.6804],[125.67009,-14.51007],[125.6858,-14.23066],[126.12515,-14.34734],[126.14282,-14.09599],[126.58259,-13.95279],[127.06587,-13.81797],[127.80463,-14.27691],[128.35969,-14.86917],[128.98554,-14.87599],[129.62147,-14.96978],[129.4096,-14.42067],[129.88864,-13.6187],[130.33947,-13.35738],[130.18351,-13.10752],[130.6178,-12.53639],[131.22349,-12.18365],[131.73509,-12.30245],[132.5753,-12.11404],[132.55721,-11.60301],[131.8247,-11.27378],[132.35722,-11.12852],[133.01956,-11.37641],[133.55085,-11.78652],[134.39307,-12.04237],[134.67863,-11.94118],[135.29849,-12.24861],[135.88269,-11.96227],[136.25838,-12.04934],[136.49248,-11.85721],[136.95162,-12.35196],[136.68512,-12.88722],[136.30541,-13.29123],[135.96176,-13.32451],[136.07762,-13.72428],[135.78384,-14.22399],[135.42866,-14.71543],[135.50018,-14.99774],[136.29517,-15.55026],[137.06536,-15.87076],[137.58047,-16.21508],[138.30322,-16.8076],[138.58516,-16.80662],[139.10854,-17.06268],[139.26057,-17.3716],[140.21525,-17.7108],[140.87546,-17.36907],[141.07111,-16.83205],[141.2741,-16.38887],[141.39822,-15.84053],[141.70218,-15.04492],[141.56338,-14.56133],[141.63552,-14.27039],[141.51987,-13.69808],[141.65092,-12.94469],[141.84269,-12.74155],[141.68699,-12.40761],[141.92863,-11.87747],[142.11849,-11.32804],[142.14371,-11.04274],[142.51526,-10.66819],[142.79731,-11.15735],[142.86676,-11.78471],[143.11595,-11.90563],[143.15863,-12.32566],[143.52212,-12.83436],[143.59716,-13.40042],[143.56181,-13.76366]]]]},\"properties\":{\"name\":\"Australia\"}}]}","volume":"165","issue":"3888","noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"505a7624e4b0c8380cd77f4b","contributors":{"authors":[{"text":"Faust, G. T.","contributorId":25982,"corporation":false,"usgs":true,"family":"Faust","given":"G.","email":"","middleInitial":"T.","affiliations":[],"preferred":false,"id":361273,"contributorType":{"id":1,"text":"Authors"},"rank":1},{"text":"Fahey, J. J.","contributorId":80665,"corporation":false,"usgs":true,"family":"Fahey","given":"J.","email":"","middleInitial":"J.","affiliations":[],"preferred":false,"id":361275,"contributorType":{"id":1,"text":"Authors"},"rank":2},{"text":"Mason, B.","contributorId":43021,"corporation":false,"usgs":true,"family":"Mason","given":"B.","email":"","affiliations":[],"preferred":false,"id":361274,"contributorType":{"id":1,"text":"Authors"},"rank":3},{"text":"Dwornik, E.J.","contributorId":99128,"corporation":false,"usgs":true,"family":"Dwornik","given":"E.J.","email":"","affiliations":[],"preferred":false,"id":361276,"contributorType":{"id":1,"text":"Authors"},"rank":4}]}}
,{"id":70011501,"text":"70011501 - 1969 - Oxygen isotope fractionation in divalent metal carbonates","interactions":[],"lastModifiedDate":"2020-11-30T13:41:37.401641","indexId":"70011501","displayToPublicDate":"1969-01-01T00:00:00","publicationYear":"1969","noYear":false,"publicationType":{"id":2,"text":"Article"},"publicationSubtype":{"id":10,"text":"Journal Article"},"seriesTitle":{"id":2207,"text":"Journal of Chemical Physics","active":true,"publicationSubtype":{"id":10}},"title":"Oxygen isotope fractionation in divalent metal carbonates","docAbstract":"<div class=\"hlFld-Abstract\"><div class=\"sectionInfo abstractSectionHeading\"><div id=\"fragmentNav_0\" class=\"sectionHeading\">Equilibrium fractionation factors for the distribution of <sup>18</sup>O between alkaline‐earth carbonates and water have been&nbsp;measured&nbsp;over the&nbsp;temperature&nbsp;range 0–500°C. The fractionation factors&nbsp;<span class=\"equationTd inline-formula\"><span id=\"MathJax-Element-1-Frame\" class=\"MathJax\" data-mathml=\"<math xmlns=\">α\"&gt;<span id=\"MathJax-Span-1\" class=\"math\"><span id=\"MathJax-Span-2\" class=\"mrow\"><span id=\"MathJax-Span-3\" class=\"mi\">α</span></span></span><span class=\"MJX_Assistive_MathML\">α</span></span></span>&nbsp;can be represented by the equations<br></div></div><div class=\"NLM_paragraph\"><table class=\"formula-display mce-item-table\" border=\"0\"><tbody><tr><td class=\"equationTd\"><div class=\"MathJax_Display\"><span id=\"MathJax-Element-2-Frame\" class=\"MathJax\" data-mathml=\"<math xmlns=\">CaCO3–H2O, 1000lnα = 2.78(106T−2)− 3.39,\"&gt;<span id=\"MathJax-Span-4\" class=\"math\"><span><span id=\"MathJax-Span-5\" class=\"mrow\"><span id=\"MathJax-Span-6\" class=\"msub\"><span id=\"MathJax-Span-7\" class=\"mi\">CaCO</span><span id=\"MathJax-Span-8\" class=\"mrow\"><span id=\"MathJax-Span-9\" class=\"mn\">3</span></span></span><span id=\"MathJax-Span-10\" class=\"mi\">–</span><span id=\"MathJax-Span-11\" class=\"msub\"><span id=\"MathJax-Span-12\" class=\"mi\">H</span><span id=\"MathJax-Span-13\" class=\"mrow\"><span id=\"MathJax-Span-14\" class=\"mn\">2</span></span></span><span id=\"MathJax-Span-15\" class=\"mi\">O</span><span id=\"MathJax-Span-16\" class=\"mtext\">, 1000</span><span id=\"MathJax-Span-17\" class=\"mi\">ln</span><span id=\"MathJax-Span-18\" class=\"msup\"><span id=\"MathJax-Span-19\" class=\"mtext\">α = 2.78(10</span><span id=\"MathJax-Span-20\" class=\"mrow\"><span id=\"MathJax-Span-21\" class=\"mn\">6</span></span></span><span id=\"MathJax-Span-22\" class=\"msup\"><span id=\"MathJax-Span-23\" class=\"mi\">T</span><span id=\"MathJax-Span-24\" class=\"mrow\"><span id=\"MathJax-Span-25\" class=\"mtext\">−2</span></span></span><span id=\"MathJax-Span-26\" class=\"mtext\">)− 3.39,</span></span></span></span><span class=\"MJX_Assistive_MathML MJX_Assistive_MathML_Block\">CaCO3–H2O, 1000lnα = 2.78(106T−2)− 3.39,</span></span></div></td><td class=\"formulaLabel\"><br></td></tr></tbody></table><table class=\"formula-display mce-item-table\" border=\"0\"><tbody><tr><td class=\"equationTd\"><div class=\"MathJax_Display\"><span id=\"MathJax-Element-3-Frame\" class=\"MathJax\" data-mathml=\"<math xmlns=\">SrCO3–H2O, 1000lnα = 2.69(106T−2)− 3.74,\"&gt;<span id=\"MathJax-Span-27\" class=\"math\"><span><span id=\"MathJax-Span-28\" class=\"mrow\"><span id=\"MathJax-Span-29\" class=\"msub\"><span id=\"MathJax-Span-30\" class=\"mi\">SrCO</span><span id=\"MathJax-Span-31\" class=\"mrow\"><span id=\"MathJax-Span-32\" class=\"mn\">3</span></span></span><span id=\"MathJax-Span-33\" class=\"mi\">–</span><span id=\"MathJax-Span-34\" class=\"msub\"><span id=\"MathJax-Span-35\" class=\"mi\">H</span><span id=\"MathJax-Span-36\" class=\"mrow\"><span id=\"MathJax-Span-37\" class=\"mn\">2</span></span></span><span id=\"MathJax-Span-38\" class=\"mi\">O</span><span id=\"MathJax-Span-39\" class=\"mtext\">, 1000</span><span id=\"MathJax-Span-40\" class=\"mi\">ln</span><span id=\"MathJax-Span-41\" class=\"msup\"><span id=\"MathJax-Span-42\" class=\"mtext\">α = 2.69(10</span><span id=\"MathJax-Span-43\" class=\"mrow\"><span id=\"MathJax-Span-44\" class=\"mn\">6</span></span></span><span id=\"MathJax-Span-45\" class=\"msup\"><span id=\"MathJax-Span-46\" class=\"mi\">T</span><span id=\"MathJax-Span-47\" class=\"mrow\"><span id=\"MathJax-Span-48\" class=\"mtext\">−2</span></span></span><span id=\"MathJax-Span-49\" class=\"mtext\">)− 3.74,</span></span></span></span><span class=\"MJX_Assistive_MathML MJX_Assistive_MathML_Block\">SrCO3–H2O, 1000lnα = 2.69(106T−2)− 3.74,</span></span></div></td><td class=\"formulaLabel\"><br></td></tr></tbody></table><table class=\"formula-display mce-item-table\" border=\"0\"><tbody><tr><td class=\"equationTd\"><div class=\"MathJax_Display\"><span id=\"MathJax-Element-4-Frame\" class=\"MathJax\" data-mathml=\"<math xmlns=\">BaCO3–H2O, 1000lnα = 2.57(106T−2)− 4.73.\"&gt;<span id=\"MathJax-Span-50\" class=\"math\"><span><span id=\"MathJax-Span-51\" class=\"mrow\"><span id=\"MathJax-Span-52\" class=\"msub\"><span id=\"MathJax-Span-53\" class=\"mi\">BaCO</span><span id=\"MathJax-Span-54\" class=\"mrow\"><span id=\"MathJax-Span-55\" class=\"mn\">3</span></span></span><span id=\"MathJax-Span-56\" class=\"mi\">–</span><span id=\"MathJax-Span-57\" class=\"msub\"><span id=\"MathJax-Span-58\" class=\"mi\">H</span><span id=\"MathJax-Span-59\" class=\"mrow\"><span id=\"MathJax-Span-60\" class=\"mn\">2</span></span></span><span id=\"MathJax-Span-61\" class=\"mi\">O</span><span id=\"MathJax-Span-62\" class=\"mtext\">, 1000</span><span id=\"MathJax-Span-63\" class=\"mi\">ln</span><span id=\"MathJax-Span-64\" class=\"msup\"><span id=\"MathJax-Span-65\" class=\"mtext\">α = 2.57(10</span><span id=\"MathJax-Span-66\" class=\"mrow\"><span id=\"MathJax-Span-67\" class=\"mn\">6</span></span></span><span id=\"MathJax-Span-68\" class=\"msup\"><span id=\"MathJax-Span-69\" class=\"mi\">T</span><span id=\"MathJax-Span-70\" class=\"mrow\"><span id=\"MathJax-Span-71\" class=\"mtext\">−2</span></span></span><span id=\"MathJax-Span-72\" class=\"mtext\">)− 4.73.</span></span></span></span><span class=\"MJX_Assistive_MathML MJX_Assistive_MathML_Block\">BaCO3–H2O, 1000lnα = 2.57(106T−2)− 4.73.</span></span></div></td><td class=\"formulaLabel\"><br></td></tr></tbody></table>Measurements<span>&nbsp;</span>on MnCO<sub>3</sub>, CdCO<sub>3</sub>, and PbCO<sub>3</sub><span>&nbsp;</span>were made at isolated<span>&nbsp;</span>temperatures.<span>&nbsp;</span>A statistical‐mechanical calculation of the isotopic partition function ratios gives reasonably good agreement with experiment. Both cationic size and mass are important in isotopic fractionation, the former predominantly in its<span>&nbsp;</span>effect<span>&nbsp;</span>on the internal vibrations of the anion, the latter in its<span>&nbsp;</span>effect<span>&nbsp;</span>on the<span>&nbsp;</span>lattice vibrations.</div></div>","language":"English","publisher":"American Institute of Physics","doi":"10.1063/1.1671982","issn":"00219606","usgsCitation":"O’Neil, J.R., Clayton, R., and Mayeda, T., 1969, Oxygen isotope fractionation in divalent metal carbonates: Journal of Chemical Physics, v. 51, no. 12, p. 5547-5558, https://doi.org/10.1063/1.1671982.","productDescription":"12 p.","startPage":"5547","endPage":"5558","numberOfPages":"12","costCenters":[],"links":[{"id":221178,"rank":0,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/thumbnails/outside_thumb.jpg"}],"volume":"51","issue":"12","noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"505a7296e4b0c8380cd76bb0","contributors":{"authors":[{"text":"O’Neil, J. R.","contributorId":69633,"corporation":false,"usgs":true,"family":"O’Neil","given":"J.","email":"","middleInitial":"R.","affiliations":[],"preferred":false,"id":361272,"contributorType":{"id":1,"text":"Authors"},"rank":1},{"text":"Clayton, R.N.","contributorId":36291,"corporation":false,"usgs":true,"family":"Clayton","given":"R.N.","email":"","affiliations":[],"preferred":false,"id":361271,"contributorType":{"id":1,"text":"Authors"},"rank":2},{"text":"Mayeda, T.K.","contributorId":30755,"corporation":false,"usgs":true,"family":"Mayeda","given":"T.K.","email":"","affiliations":[],"preferred":false,"id":361270,"contributorType":{"id":1,"text":"Authors"},"rank":3}]}}
,{"id":70010091,"text":"70010091 - 1969 - Anorthosite belts, continental drift, and the anorthosite event","interactions":[],"lastModifiedDate":"2020-11-29T19:53:05.269104","indexId":"70010091","displayToPublicDate":"1969-01-01T00:00:00","publicationYear":"1969","noYear":false,"publicationType":{"id":2,"text":"Article"},"publicationSubtype":{"id":10,"text":"Journal Article"},"seriesTitle":{"id":3338,"text":"Science","active":true,"publicationSubtype":{"id":10}},"title":"Anorthosite belts, continental drift, and the anorthosite event","docAbstract":"<div class=\"panel-pane pane-highwire-panel-tabs-container article__body\"><div class=\"pane-content\"><div id=\"panels-ajax-tab-container-highwire_article_tabs\" class=\"panels-ajax-tab-container\" data-panels-ajax-tab-preloaded=\"jnl_sci_tab_art\"><div class=\"panels-ajax-tab-wrap-jnl_sci_tab_art\"><div class=\"panel-display panel-1col clearfix\"><div class=\"panel-panel panel-col\"><div><div class=\"panel-pane pane-highwire-markup\"><div class=\"pane-content\"><div class=\"highwire-markup\"><div id=\"content-block-markup\" data-highwire-cite-ref-tooltip-instance=\"highwire_reflinks_tooltip\" data-highwire-glossary-tooltip-instance=\"highwire_reflinks_tooltip\"><div class=\"article abstract-view \"><div id=\"abstract-1\" class=\"section abstract\"><p id=\"p-1\">Most anorthosites lie in two principal belts when plotted on a predrift continental reconstruction. Anorthosite ages in the belts cluster around 1300 ± 200 million years and range from 1100 to 1700 million years. This suggests that anorthosites are the product of a unique cataclysmic event or a thermal event that was normal only during the earth's early history.</p></div></div><span id=\"related-urls\"></span></div></div></div></div></div></div></div></div></div></div></div>","language":"English","publisher":"AAAS","doi":"10.1126/science.164.3882.944","issn":"00368075","usgsCitation":"Herz, N., 1969, Anorthosite belts, continental drift, and the anorthosite event: Science, v. 164, no. 3882, p. 944-947, https://doi.org/10.1126/science.164.3882.944.","productDescription":"4 p.","startPage":"944","endPage":"947","numberOfPages":"4","costCenters":[],"links":[{"id":219591,"rank":0,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/thumbnails/outside_thumb.jpg"}],"volume":"164","issue":"3882","noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"5059ec4ee4b0c8380cd491b0","contributors":{"authors":[{"text":"Herz, N.","contributorId":97626,"corporation":false,"usgs":true,"family":"Herz","given":"N.","affiliations":[],"preferred":false,"id":357876,"contributorType":{"id":1,"text":"Authors"},"rank":1}]}}
,{"id":70010053,"text":"70010053 - 1969 - Determination of fixed water in rocks by infrared absorption","interactions":[],"lastModifiedDate":"2019-12-13T07:42:15","indexId":"70010053","displayToPublicDate":"1969-01-01T00:00:00","publicationYear":"1969","noYear":false,"publicationType":{"id":2,"text":"Article"},"publicationSubtype":{"id":10,"text":"Journal Article"},"seriesTitle":{"id":761,"text":"Analytical Chemistry","active":true,"publicationSubtype":{"id":10}},"title":"Determination of fixed water in rocks by infrared absorption","docAbstract":"<p>No abstract available.</p>","language":"English","publisher":"ACS","doi":"10.1021/ac60272a028","issn":"00032700","usgsCitation":"Breger, I.A., and Chandler, J., 1969, Determination of fixed water in rocks by infrared absorption: Analytical Chemistry, v. 41, no. 3, p. 506-510, https://doi.org/10.1021/ac60272a028.","productDescription":"5 p.","startPage":"506","endPage":"510","numberOfPages":"5","costCenters":[],"links":[{"id":218776,"rank":0,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/thumbnails/outside_thumb.jpg"}],"volume":"41","issue":"3","noUsgsAuthors":false,"publicationDate":"2002-05-01","publicationStatus":"PW","scienceBaseUri":"5059ffa5e4b0c8380cd4f2e6","contributors":{"authors":[{"text":"Breger, Irving A.","contributorId":65205,"corporation":false,"usgs":true,"family":"Breger","given":"Irving","email":"","middleInitial":"A.","affiliations":[],"preferred":false,"id":357782,"contributorType":{"id":1,"text":"Authors"},"rank":1},{"text":"Chandler, J.C.","contributorId":76864,"corporation":false,"usgs":true,"family":"Chandler","given":"J.C.","email":"","affiliations":[],"preferred":false,"id":357783,"contributorType":{"id":1,"text":"Authors"},"rank":2}]}}
,{"id":70010052,"text":"70010052 - 1969 - Earthquake prediction and control","interactions":[],"lastModifiedDate":"2020-03-24T14:22:12","indexId":"70010052","displayToPublicDate":"1969-01-01T00:00:00","publicationYear":"1969","noYear":false,"publicationType":{"id":2,"text":"Article"},"publicationSubtype":{"id":10,"text":"Journal Article"},"seriesTitle":{"id":3338,"text":"Science","active":true,"publicationSubtype":{"id":10}},"title":"Earthquake prediction and control","docAbstract":"Scientists look beyond prediction to controlled release of stored strain energy in active fault zones.","language":"English","publisher":"Elsevier","doi":"10.1126/science.166.3912.1467","issn":"00368075","usgsCitation":"Pakiser, L.C., Eaton, J.P., Healy, J.H., and Raleigh, C., 1969, Earthquake prediction and control: Science, v. 166, no. 3912, p. 1467-1474, https://doi.org/10.1126/science.166.3912.1467.","productDescription":"8 p.","startPage":"1467","endPage":"1474","numberOfPages":"8","costCenters":[],"links":[{"id":218775,"rank":0,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/thumbnails/outside_thumb.jpg"}],"volume":"166","issue":"3912","noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"505a04fbe4b0c8380cd50bd5","contributors":{"authors":[{"text":"Pakiser, L. C.","contributorId":83512,"corporation":false,"usgs":true,"family":"Pakiser","given":"L.","email":"","middleInitial":"C.","affiliations":[],"preferred":false,"id":357780,"contributorType":{"id":1,"text":"Authors"},"rank":1},{"text":"Eaton, J. P.","contributorId":105313,"corporation":false,"usgs":true,"family":"Eaton","given":"J.","email":"","middleInitial":"P.","affiliations":[],"preferred":false,"id":357781,"contributorType":{"id":1,"text":"Authors"},"rank":2},{"text":"Healy, J. H.","contributorId":48968,"corporation":false,"usgs":true,"family":"Healy","given":"J.","email":"","middleInitial":"H.","affiliations":[],"preferred":false,"id":357779,"contributorType":{"id":1,"text":"Authors"},"rank":3},{"text":"Raleigh, C.B.","contributorId":40219,"corporation":false,"usgs":true,"family":"Raleigh","given":"C.B.","email":"","affiliations":[],"preferred":false,"id":357778,"contributorType":{"id":1,"text":"Authors"},"rank":4}]}}
,{"id":1000285,"text":"1000285 - 1969 - Rearing of sea lamprey, Petromyzon marinus, embryos in distilled water","interactions":[],"lastModifiedDate":"2023-12-06T22:36:47.712241","indexId":"1000285","displayToPublicDate":"1969-01-01T00:00:00","publicationYear":"1969","noYear":false,"publicationType":{"id":2,"text":"Article"},"publicationSubtype":{"id":10,"text":"Journal Article"},"seriesTitle":{"id":1337,"text":"Copeia","active":true,"publicationSubtype":{"id":10}},"title":"Rearing of sea lamprey, Petromyzon marinus, embryos in distilled water","docAbstract":"Most embryological studies of lampreys in the Great Lakes have been conducted with filtered water from Lake Huron.  Although this water was entirely satisfactory for the earlier work, the present need for knowledge of the effects of various compounds on embryological development requires that the initial medium be sterile.  The purpose of the present study was to determine whether sea lamprey embryos could be successfully reared in distilled water.  Mature sea lampreys were collected from the Ocqueoc River, Presque Isle County, Michigan, and transferred to the Hammond Bay Biological Station where eggs were stripped and fertilized according to the method of Piavis.  After activation was ascertained to be 90-100% complete, the embryos were washed 3-5 timesexperimentals with commercially obtained U.S.P. distilled water and controls with filtered Lake Huron water.","language":"English","publisher":"American Society of Ichthyologists and Herpetologists (ASIH)","doi":"10.2307/1441724","usgsCitation":"Piavis, G.W., and Howell, J.H., 1969, Rearing of sea lamprey, Petromyzon marinus, embryos in distilled water: Copeia, v. 1969, no. 1, p. 204-205, https://doi.org/10.2307/1441724.","productDescription":"2 p.","startPage":"204","endPage":"205","numberOfPages":"2","costCenters":[{"id":324,"text":"Great Lakes Science Center","active":true,"usgs":true}],"links":[{"id":128671,"rank":1,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/thumbnails/outside_thumb.jpg"}],"volume":"1969","issue":"1","noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"4f4e4a53e4b07f02db62b2b9","contributors":{"authors":[{"text":"Piavis, George W.","contributorId":63755,"corporation":false,"usgs":true,"family":"Piavis","given":"George","email":"","middleInitial":"W.","affiliations":[],"preferred":false,"id":308338,"contributorType":{"id":1,"text":"Authors"},"rank":1},{"text":"Howell, John H.","contributorId":39720,"corporation":false,"usgs":true,"family":"Howell","given":"John","email":"","middleInitial":"H.","affiliations":[],"preferred":false,"id":308337,"contributorType":{"id":1,"text":"Authors"},"rank":2}]}}
,{"id":70176050,"text":"70176050 - 1969 - Quantity and quality of low flow in the Hondo Creek Basin, Texas, March 27-28, 1968","interactions":[],"lastModifiedDate":"2016-08-24T11:27:10","indexId":"70176050","displayToPublicDate":"1969-01-01T00:00:00","publicationYear":"1969","noYear":false,"publicationType":{"id":18,"text":"Report"},"publicationSubtype":{"id":2,"text":"State or Local Government Series"},"title":"Quantity and quality of low flow in the Hondo Creek Basin, Texas, March 27-28, 1968","docAbstract":"<p>No abstract available.</p>","language":"English","publisher":"Edwards Underground Water District","usgsCitation":"Reeves, W., and Rettman, P., 1969, Quantity and quality of low flow in the Hondo Creek Basin, Texas, March 27-28, 1968, 9 p.","productDescription":"9 p.","onlineOnly":"N","additionalOnlineFiles":"N","costCenters":[{"id":583,"text":"Texas Water Science Center","active":true,"usgs":true}],"links":[{"id":327786,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/thumbnails/outside_thumb.jpg"}],"noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"57c6b0f9e4b0f2f0cebe6646","contributors":{"authors":[{"text":"Reeves, W.E.","contributorId":79518,"corporation":false,"usgs":true,"family":"Reeves","given":"W.E.","email":"","affiliations":[],"preferred":false,"id":646938,"contributorType":{"id":1,"text":"Authors"},"rank":1},{"text":"Rettman, P.L.","contributorId":60663,"corporation":false,"usgs":true,"family":"Rettman","given":"P.L.","affiliations":[],"preferred":false,"id":646939,"contributorType":{"id":1,"text":"Authors"},"rank":2}]}}
,{"id":70011576,"text":"70011576 - 1969 - Saline water in southeastern New Mexico","interactions":[],"lastModifiedDate":"2020-11-29T17:59:16.005627","indexId":"70011576","displayToPublicDate":"1969-01-01T00:00:00","publicationYear":"1969","noYear":false,"publicationType":{"id":2,"text":"Article"},"publicationSubtype":{"id":10,"text":"Journal Article"},"seriesTitle":{"id":1213,"text":"Chemical Geology","active":true,"publicationSubtype":{"id":10}},"title":"Saline water in southeastern New Mexico","docAbstract":"<p id=\"simple-para.0010\">Saline waters from formations of several geologic ages are being studied in a seven-county area in southeastern New Mexico and western Texas, where more than 30,000 oil and gas tests have been drilled in the past 40 years. This area of 7,500 sq. miles, which is stratigraphically complex, includes the northern and eastern margins of the Delaware Basin between the Guadalupe and Glass Mountains.</p><p id=\"simple-para.0015\">Chloride-ion concentrations in water produced from rocks of various ages and depths have been mapped in Lea County, New Mexico, using machine map-plotting techniques and trend analyses. Anomalously low chloride concentrations (1,000–3,000 mg/l) were found along the western margin of the Central Basin platform in the San Andres and Capitan Limestone Formations of Permian age. These low chloride-ion concentrations may be due to preferential circulation of ground water through the more porous and permeable rocks.</p><p id=\"simple-para.0020\">Data being used in the study were obtained principally from oil companies and from related service companies. The P.B.W.D.S. (Permian Basin Well Data System) scout-record magnetic-tape file was used as a framework in all computer operations. Shallow or non-oil-field water analyses acquired from state, municipal, or federal agencies were added to these data utilizing P.B.W.D.S.-compatible reference numbers and decimal latitude-longitude coordinates. Approximately 20,000 water analyses collected from over 65 sources were coded, recorded on punch cards and stored on magnetic tape for computer operations. Extensive manual and computer error checks for duplication and accuracy were made to eliminate data errors resulting from poorly located or identified samples; non-representative or contaminated samples; mistakes in coding, reproducing or key-punching; laboratory errors; and inconsistent reporting. The original 20,000 analyses considered were reduced to 6,000 representative analyses which are being used in the saline water studies.</p>","language":"English","publisher":"Elsevier","doi":"10.1016/0009-2541(69)90054-0","issn":"00092541","usgsCitation":"Hiss, W.L., Peterson, J., and Ramsey, T., 1969, Saline water in southeastern New Mexico: Chemical Geology, v. 4, no. 1-2, p. 341-360, https://doi.org/10.1016/0009-2541(69)90054-0.","productDescription":"20 p.","startPage":"341","endPage":"360","numberOfPages":"20","costCenters":[],"links":[{"id":221375,"rank":0,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/thumbnails/outside_thumb.jpg"}],"country":"United States","state":"New Mexico","geographicExtents":"{\n  \"type\": \"FeatureCollection\",\n  \"features\": [\n    {\n      \"type\": \"Feature\",\n      \"properties\": {},\n      \"geometry\": {\n        \"type\": \"Polygon\",\n        \"coordinates\": [\n          [\n            [\n              -106.45751953125,\n              31.765537409484374\n            ],\n            [\n              -102.7001953125,\n              31.765537409484374\n            ],\n            [\n              -102.7001953125,\n              33.247875947924385\n            ],\n            [\n              -106.45751953125,\n              33.247875947924385\n            ],\n            [\n              -106.45751953125,\n              31.765537409484374\n            ]\n          ]\n        ]\n      }\n    }\n  ]\n}","volume":"4","issue":"1-2","noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"505aafd5e4b0c8380cd877e0","contributors":{"authors":[{"text":"Hiss, W. L.","contributorId":15614,"corporation":false,"usgs":true,"family":"Hiss","given":"W.","middleInitial":"L.","affiliations":[],"preferred":false,"id":361443,"contributorType":{"id":1,"text":"Authors"},"rank":1},{"text":"Peterson, J.B.","contributorId":90389,"corporation":false,"usgs":true,"family":"Peterson","given":"J.B.","email":"","affiliations":[],"preferred":false,"id":361445,"contributorType":{"id":1,"text":"Authors"},"rank":2},{"text":"Ramsey, T.R.","contributorId":39125,"corporation":false,"usgs":true,"family":"Ramsey","given":"T.R.","email":"","affiliations":[],"preferred":false,"id":361444,"contributorType":{"id":1,"text":"Authors"},"rank":3}]}}
,{"id":70009792,"text":"70009792 - 1969 - Magnetic susceptibility studies of Cu(II), Co(II), Ni(II) and Fe(III) on a chelating resin","interactions":[],"lastModifiedDate":"2025-02-07T16:55:14.707905","indexId":"70009792","displayToPublicDate":"1969-01-01T00:00:00","publicationYear":"1969","noYear":false,"publicationType":{"id":2,"text":"Article"},"publicationSubtype":{"id":10,"text":"Journal Article"},"seriesTitle":{"id":2355,"text":"Journal of Inorganic and Nuclear Chemistry","active":true,"publicationSubtype":{"id":10}},"title":"Magnetic susceptibility studies of Cu(II), Co(II), Ni(II) and Fe(III) on a chelating resin","docAbstract":"<p>No abstract available.</p>","language":"English","publisher":"Elsevier","doi":"10.1016/0022-1902(69)80036-9","issn":"00221902","usgsCitation":"Krishnamurthy, M., Hambright, W., Morris, K., Thorpe, A.N., and Alexander, C., 1969, Magnetic susceptibility studies of Cu(II), Co(II), Ni(II) and Fe(III) on a chelating resin: Journal of Inorganic and Nuclear Chemistry, v. 31, no. 3, p. 873-875, https://doi.org/10.1016/0022-1902(69)80036-9.","productDescription":"3 p.","startPage":"873","endPage":"875","numberOfPages":"3","costCenters":[],"links":[{"id":218599,"rank":1,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/thumbnails/outside_thumb.jpg"}],"volume":"31","issue":"3","noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"505a4b92e4b0c8380cd69645","contributors":{"authors":[{"text":"Krishnamurthy, M.","contributorId":52318,"corporation":false,"usgs":true,"family":"Krishnamurthy","given":"M.","email":"","affiliations":[],"preferred":false,"id":357155,"contributorType":{"id":1,"text":"Authors"},"rank":1},{"text":"Hambright, W.P.","contributorId":58016,"corporation":false,"usgs":true,"family":"Hambright","given":"W.P.","email":"","affiliations":[],"preferred":false,"id":357157,"contributorType":{"id":1,"text":"Authors"},"rank":2},{"text":"Morris, K.B.","contributorId":51446,"corporation":false,"usgs":true,"family":"Morris","given":"K.B.","email":"","affiliations":[],"preferred":false,"id":357154,"contributorType":{"id":1,"text":"Authors"},"rank":3},{"text":"Thorpe, A. N.","contributorId":53504,"corporation":false,"usgs":true,"family":"Thorpe","given":"A.","email":"","middleInitial":"N.","affiliations":[],"preferred":false,"id":357156,"contributorType":{"id":1,"text":"Authors"},"rank":4},{"text":"Alexander, C.C.","contributorId":34256,"corporation":false,"usgs":true,"family":"Alexander","given":"C.C.","email":"","affiliations":[],"preferred":false,"id":357153,"contributorType":{"id":1,"text":"Authors"},"rank":5}]}}
,{"id":96404,"text":"96404 - 1969 - Comparative ecology of pinyon mice and deer mice in Mesa Verde National Park, Colorado","interactions":[],"lastModifiedDate":"2022-11-07T17:47:37.814417","indexId":"96404","displayToPublicDate":"1969-01-01T00:00:00","publicationYear":"1969","noYear":false,"publicationType":{"id":4,"text":"Book"},"publicationSubtype":{"id":15,"text":"Monograph"},"title":"Comparative ecology of pinyon mice and deer mice in Mesa Verde National Park, Colorado","docAbstract":"No abstract available at this time","language":"English","publisher":"University of Kansas","publisherLocation":"Lawrence, KS","usgsCitation":"Douglas, C.L., 1969, Comparative ecology of pinyon mice and deer mice in Mesa Verde National Park, Colorado, 84 p.","productDescription":"84 p.","numberOfPages":"84","costCenters":[{"id":651,"text":"Western Ecological Research Center","active":true,"usgs":true}],"links":[{"id":126912,"rank":0,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/thumbnails/outside_thumb.jpg"}],"country":"United States","state":"Colorado","otherGeospatial":"Mesa Verde National Park","geographicExtents":"{\n  \"type\": \"FeatureCollection\",\n  \"features\": [\n    {\n      \"type\": \"Feature\",\n      \"properties\": {},\n      \"geometry\": {\n        \"coordinates\": [\n          [\n            [\n              -108.36425685506853,\n              37.35\n            ],\n            [\n              -108.6,\n              37.35\n            ],\n            [\n              -108.6,\n              37.149986062809944\n            ],\n            [\n              -108.36425685506853,\n              37.149986062809944\n            ],\n            [\n              -108.36425685506853,\n              37.35\n            ]\n          ]\n        ],\n        \"type\": \"Polygon\"\n      }\n    }\n  ]\n}","noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"4f4e4b24e4b07f02db6ae543","contributors":{"editors":[{"text":"Cross, Frank B.","contributorId":112586,"corporation":false,"usgs":true,"family":"Cross","given":"Frank","email":"","middleInitial":"B.","affiliations":[],"preferred":false,"id":505697,"contributorType":{"id":2,"text":"Editors"},"rank":1},{"text":"Humphrey, Philip S.","contributorId":113940,"corporation":false,"usgs":true,"family":"Humphrey","given":"Philip","email":"","middleInitial":"S.","affiliations":[],"preferred":false,"id":505699,"contributorType":{"id":2,"text":"Editors"},"rank":2},{"text":"Jones, J. Knox Jr.","contributorId":112682,"corporation":false,"usgs":true,"family":"Jones","given":"J.","suffix":"Jr.","email":"","middleInitial":"Knox","affiliations":[],"preferred":false,"id":505698,"contributorType":{"id":2,"text":"Editors"},"rank":3}],"authors":[{"text":"Douglas, Charles L.","contributorId":10742,"corporation":false,"usgs":true,"family":"Douglas","given":"Charles","email":"","middleInitial":"L.","affiliations":[],"preferred":false,"id":299582,"contributorType":{"id":1,"text":"Authors"},"rank":1}]}}
,{"id":96405,"text":"96405 - 1969 - Environment of Mesa Verde, Colorado","interactions":[],"lastModifiedDate":"2012-02-02T00:03:50","indexId":"96405","displayToPublicDate":"1969-01-01T00:00:00","publicationYear":"1969","noYear":false,"publicationType":{"id":5,"text":"Book chapter"},"publicationSubtype":{"id":24,"text":"Book Chapter"},"title":"Environment of Mesa Verde, Colorado","docAbstract":"No abstract available at this time","largerWorkType":{"id":18,"text":"Report"},"largerWorkTitle":"Archeological Research Series","largerWorkSubtype":{"id":9,"text":"Other Report"},"language":"English","publisher":"National Park Service","publisherLocation":"Washington, DC","usgsCitation":"Erdman, J., Douglas, C.L., and Marr, J.W., 1969, Environment of Mesa Verde, Colorado, chap. <i>of</i> Archeological Research Series, p. 1-72.","productDescription":"p. 1-72","startPage":"1","endPage":"72","numberOfPages":"72","costCenters":[{"id":651,"text":"Western Ecological Research Center","active":true,"usgs":true}],"links":[{"id":126913,"rank":0,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/thumbnails/outside_thumb.jpg"}],"noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"4f4e4a14e4b07f02db6025c0","contributors":{"authors":[{"text":"Erdman, J.","contributorId":25886,"corporation":false,"usgs":true,"family":"Erdman","given":"J.","affiliations":[],"preferred":false,"id":299583,"contributorType":{"id":1,"text":"Authors"},"rank":1},{"text":"Douglas, C. L.","contributorId":64586,"corporation":false,"usgs":true,"family":"Douglas","given":"C.","email":"","middleInitial":"L.","affiliations":[],"preferred":false,"id":299584,"contributorType":{"id":1,"text":"Authors"},"rank":2},{"text":"Marr, J. W.","contributorId":97839,"corporation":false,"usgs":true,"family":"Marr","given":"J.","email":"","middleInitial":"W.","affiliations":[],"preferred":false,"id":299585,"contributorType":{"id":1,"text":"Authors"},"rank":3}]}}
,{"id":70185797,"text":"pp669C - 1969 - Geologic history of the Colorado River: Chapter C in <i>The Colorado River region and John Wesley Powell (Professional Paper 669)</i>","interactions":[{"subject":{"id":70185797,"text":"pp669C - 1969 - Geologic history of the Colorado River: Chapter C in <i>The Colorado River region and John Wesley Powell (Professional Paper 669)</i>","indexId":"pp669C","publicationYear":"1969","noYear":false,"chapter":"C","title":"Geologic history of the Colorado River: Chapter C in <i>The Colorado River region and John Wesley Powell (Professional Paper 669)</i>"},"predicate":"IS_PART_OF","object":{"id":25022,"text":"pp669 - 1969 - The Colorado River region and John Wesley Powell","indexId":"pp669","publicationYear":"1969","noYear":false,"title":"The Colorado River region and John Wesley Powell"},"id":1}],"isPartOf":{"id":25022,"text":"pp669 - 1969 - The Colorado River region and John Wesley Powell","indexId":"pp669","publicationYear":"1969","noYear":false,"title":"The Colorado River region and John Wesley Powell"},"lastModifiedDate":"2017-03-29T11:00:42","indexId":"pp669C","displayToPublicDate":"1969-01-01T00:00:00","publicationYear":"1969","noYear":false,"publicationType":{"id":18,"text":"Report"},"publicationSubtype":{"id":5,"text":"USGS Numbered Series"},"seriesTitle":{"id":331,"text":"Professional Paper","code":"PP","onlineIssn":"2330-7102","printIssn":"1044-9612","active":true,"publicationSubtype":{"id":5}},"seriesNumber":"669","chapter":"C","title":"Geologic history of the Colorado River: Chapter C in <i>The Colorado River region and John Wesley Powell (Professional Paper 669)</i>","docAbstract":"<p>John Wesley Powell clearly recognized that the spectacular features of the Colorado River - its many grand canyons - were dependent upon the structural history of the mountainous barriers crossed by the river. He conceived of three different historical relationships between rivers and structural features: (1) Newly uplifted land surfaces have rivers that flow down the initial slope of the uplift; these relationships he termed consequent. (2) A river may be older than an uplift that it crosses because it has been able to maintain its course by eroding downward as the uplift progresses; this relationship he named antecedent. (3) An uplifted block may have been buried by younger deposits upon which a river becomes established. The river, in cutting downward, uncovers the uplifted block and becomes incised into it; this relationship he called superimposed.</p><p>The geologic history of the Colorado River involves all three relationships. In addition, although the position of the river course through a particular structural barrier may have been the result of superposition, the depth of the canyon at that point may be largely due to renewed uplift of the barrier; such deepening of the canyon, therefore, is due to antecedence. The problem of the Colorado River remains today very much as G. K. Gilbert stated it nearly 100 years ago: \"How much is antecedent and how much is superimposed?\" The question must be asked separately for each stretch of the river. </p>","largerWorkType":{"id":18,"text":"Report"},"largerWorkTitle":"The Colorado River region and John Wesley Powell (Professional Paper 669)","largerWorkSubtype":{"id":5,"text":"USGS Numbered Series"},"language":"English","publisher":"U.S. Government Printing Office","publisherLocation":"Washington, D.C.","doi":"10.3133/pp669C","usgsCitation":"Hunt, C.B., 1969, Geologic history of the Colorado River: Chapter C in <i>The Colorado River region and John Wesley Powell (Professional Paper 669)</i>: U.S. Geological Survey Professional Paper 669, iv, 72 p., https://doi.org/10.3133/pp669C.","productDescription":"iv, 72 p.","startPage":"59","endPage":"130","costCenters":[],"links":[{"id":338556,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/thumbnails/usgs_thumb.jpg"},{"id":338554,"rank":1,"type":{"id":11,"text":"Document"},"url":"https://pubs.usgs.gov/pp/0669/report.pdf#page=71"}],"country":"United States","otherGeospatial":"Colorado River","noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"58dcc824e4b02ff32c685772","contributors":{"authors":[{"text":"Hunt, Charles B. cdhunt@usgs.gov","contributorId":16079,"corporation":false,"usgs":true,"family":"Hunt","given":"Charles","email":"cdhunt@usgs.gov","middleInitial":"B.","affiliations":[],"preferred":false,"id":686766,"contributorType":{"id":1,"text":"Authors"},"rank":1}]}}
,{"id":70196156,"text":"70196156 - 1969 - Relation of water loss to moisture content of hydrophytes in a natural pond","interactions":[],"lastModifiedDate":"2018-03-21T16:31:52","indexId":"70196156","displayToPublicDate":"1969-01-01T00:00:00","publicationYear":"1969","noYear":false,"publicationType":{"id":2,"text":"Article"},"publicationSubtype":{"id":10,"text":"Journal Article"},"seriesTitle":{"id":3722,"text":"Water Resources Research","onlineIssn":"1944-7973","printIssn":"0043-1397","active":true,"publicationSubtype":{"id":10}},"title":"Relation of water loss to moisture content of hydrophytes in a natural pond","docAbstract":"<p><span>Hydrophytes growing in natural ponds on the Coteau du Missouri in North Dakota have been studied. Previous studies in the same region showed how transpiration by hydrophytes could be separated from the total water loss from a natural pond, during the period that vegetation was growing in height, on the basis of a correlation between the height of vegetation and a mass‐transfer coefficient. It is shown that a similar separation can be made during the period of declining activity of the vegetation. A significant correlation was found between the ratio of moisture content of vegetation to its oven‐dry weight and the mass‐transfer coefficient. Weekly photographs on Ektachrome Infrared Aero film helped to confirm some of the phenomena observed.</span></p>","language":"English","publisher":"AGU","doi":"10.1029/WR005i002p00527 ","usgsCitation":"Eisenlohr, W.S., 1969, Relation of water loss to moisture content of hydrophytes in a natural pond: Water Resources Research, v. 5, no. 2, p. 527-530, https://doi.org/10.1029/WR005i002p00527 .","productDescription":"4 p.","startPage":"527","endPage":"530","costCenters":[{"id":478,"text":"North Dakota Water Science Center","active":true,"usgs":true},{"id":34685,"text":"Dakota Water Science Center","active":true,"usgs":true}],"links":[{"id":352721,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/thumbnails/outside_thumb.jpg"}],"volume":"5","issue":"2","noUsgsAuthors":false,"publicationDate":"2010-07-09","publicationStatus":"PW","scienceBaseUri":"5aff5cc3e4b0da30c1bfdd7e","contributors":{"authors":[{"text":"Eisenlohr, W. S. Jr.","contributorId":47014,"corporation":false,"usgs":true,"family":"Eisenlohr","given":"W.","suffix":"Jr.","email":"","middleInitial":"S.","affiliations":[],"preferred":false,"id":731531,"contributorType":{"id":1,"text":"Authors"},"rank":1}]}}
,{"id":93777,"text":"93777 - 1969 - The black footed ferret in South Dakota","interactions":[],"lastModifiedDate":"2014-08-14T12:53:15","indexId":"93777","displayToPublicDate":"1969-01-01T00:00:00","publicationYear":"1969","noYear":false,"publicationType":{"id":18,"text":"Report"},"publicationSubtype":{"id":2,"text":"State or Local Government Series"},"seriesNumber":"4","title":"The black footed ferret in South Dakota","docAbstract":"No abstract available.","language":"English","publisher":"South Dakota Department of Game, Fish, and Parks","publisherLocation":"Pierre, SD","usgsCitation":"Henderson, F.R., Springer, P.F., and Adrian, R., 1969, The black footed ferret in South Dakota, iii, 37 p.","productDescription":"iii, 37 p.","costCenters":[{"id":480,"text":"Northern Prairie Wildlife Research Center","active":true,"usgs":true}],"links":[{"id":128444,"rank":0,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/thumbnails/outside_thumb.jpg"}],"noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"4f4e4a4ee4b07f02db6281f2","contributors":{"authors":[{"text":"Henderson, F. Robert","contributorId":32839,"corporation":false,"usgs":true,"family":"Henderson","given":"F.","email":"","middleInitial":"Robert","affiliations":[],"preferred":false,"id":297907,"contributorType":{"id":1,"text":"Authors"},"rank":1},{"text":"Springer, Paul F.","contributorId":70445,"corporation":false,"usgs":true,"family":"Springer","given":"Paul","email":"","middleInitial":"F.","affiliations":[],"preferred":false,"id":297909,"contributorType":{"id":1,"text":"Authors"},"rank":2},{"text":"Adrian, Richard","contributorId":41756,"corporation":false,"usgs":true,"family":"Adrian","given":"Richard","email":"","affiliations":[],"preferred":false,"id":297908,"contributorType":{"id":1,"text":"Authors"},"rank":3}]}}
,{"id":81417,"text":"81417 - 1969 - Pacific salmon","interactions":[],"lastModifiedDate":"2023-03-29T16:11:00.109385","indexId":"81417","displayToPublicDate":"1969-01-01T00:00:00","publicationYear":"1969","noYear":false,"publicationType":{"id":5,"text":"Book chapter"},"publicationSubtype":{"id":24,"text":"Book Chapter"},"title":"Pacific salmon","docAbstract":"<p>No abstract available.</p>","largerWorkType":{"id":4,"text":"Book"},"largerWorkTitle":"The encyclopedia of marine resources","largerWorkSubtype":{"id":15,"text":"Monograph"},"language":"English","publisher":"Van Nostrand Reinhold","publisherLocation":"New York, NY","usgsCitation":"Harry, G.Y., 1969, Pacific salmon, chap. <i>of</i> The encyclopedia of marine resources, p. 588-594.","productDescription":"7 p.","startPage":"588","endPage":"594","costCenters":[{"id":324,"text":"Great Lakes Science Center","active":true,"usgs":true}],"links":[{"id":128020,"rank":1,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/thumbnails/outside_thumb.jpg"}],"noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"4f4e4ae4e4b07f02db689d35","contributors":{"editors":[{"text":"Firth, Frank E.","contributorId":113227,"corporation":false,"usgs":true,"family":"Firth","given":"Frank","email":"","middleInitial":"E.","affiliations":[],"preferred":false,"id":504062,"contributorType":{"id":2,"text":"Editors"},"rank":1}],"authors":[{"text":"Harry, George Y.","contributorId":65029,"corporation":false,"usgs":true,"family":"Harry","given":"George","email":"","middleInitial":"Y.","affiliations":[],"preferred":false,"id":295340,"contributorType":{"id":1,"text":"Authors"},"rank":1}]}}
,{"id":93770,"text":"93770 - 1969 - Safety operation and maintenance of the hurricane aircat boat with particular reference to night capture of birds","interactions":[],"lastModifiedDate":"2017-09-14T10:11:54","indexId":"93770","displayToPublicDate":"1969-01-01T00:00:00","publicationYear":"1969","noYear":false,"publicationType":{"id":18,"text":"Report"},"publicationSubtype":{"id":9,"text":"Other Report"},"title":"Safety operation and maintenance of the hurricane aircat boat with particular reference to night capture of birds","language":"English","publisher":"U.S. Geological Survey, Northern Prairie Wildlife Research Center","publisherLocation":"Jamestown, ND","usgsCitation":"Cowardin, L., 1969, Safety operation and maintenance of the hurricane aircat boat with particular reference to night capture of birds, 9 p.","productDescription":"9 p.","costCenters":[{"id":480,"text":"Northern Prairie Wildlife Research Center","active":true,"usgs":true}],"links":[{"id":128429,"rank":0,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/thumbnails/outside_thumb.jpg"}],"noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"4f4e4a0ee4b07f02db5fe047","contributors":{"authors":[{"text":"Cowardin, L.M.","contributorId":106435,"corporation":false,"usgs":true,"family":"Cowardin","given":"L.M.","email":"","affiliations":[],"preferred":false,"id":297897,"contributorType":{"id":1,"text":"Authors"},"rank":1}]}}
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