{"pageNumber":"7133","pageRowStart":"178300","pageSize":"25","recordCount":184742,"records":[{"id":70222222,"text":"70222222 - 1948 - Preliminary report on the stratigraphy and structure of the area of the Ipnavik River, Alaska","interactions":[],"lastModifiedDate":"2022-05-31T19:24:02.040102","indexId":"70222222","displayToPublicDate":"1948-12-31T13:49:26","publicationYear":"1948","noYear":false,"publicationType":{"id":18,"text":"Report"},"publicationSubtype":{"id":6,"text":"USGS Unnumbered Series"},"seriesTitle":{"id":5963,"text":"Geological Investigations, Naval Petroleum Reserve No. 4, Alaska","active":false,"publicationSubtype":{"id":6}},"seriesNumber":"16","subseriesTitle":"Preliminary Report","title":"Preliminary report on the stratigraphy and structure of the area of the Ipnavik River, Alaska","docAbstract":"<p>Geological Survey Party 1 returned to Umiat from Wolf Creek on August 5. Plans for the field season of 1947 called for geologic reconnaissance along part of the Ipnavik River and along the Colville River between the Ipnavik and Kurupa Rivers, to be completed before the end of the season. Since not much time remained and the traverse was long--about 70 airline miles--it was decided that the work would progress more rapidly if two parts of the traverse were worked at the same time. Accordingly, Robert F. Thurrell, Jr., and James H. Zumberge, geologists, were transported by plane from Umiat to the confluence of the Ipnavik and the Colville Rivers on August 8. From there they traversed down the Colville to the Kurupa River 1/.</p><p>The other two members of Party 1, Karl Stefansson, geologist, and Elder W. Lebert, cook, remained in Umiat until August 14 when a small plane was finally available to transport them to a camp on the Ipnavik River, about 30 airline miles southwest of the junction of the Ipnavik and the Colville Rivers. The party reached the Colville River on September 2, and arrived at Umiat on September 6.</p>","language":"English","publisher":"U.S. Geological Survey","doi":"10.3133/70222222","usgsCitation":"Stefansson, K., 1948, Preliminary report on the stratigraphy and structure of the area of the Ipnavik River, Alaska: Geological Investigations, Naval Petroleum Reserve No. 4, Alaska 16, 3 p., https://doi.org/10.3133/70222222.","productDescription":"3 p.","costCenters":[],"links":[{"id":401403,"rank":3,"type":{"id":11,"text":"Document"},"url":"https://pubs.usgs.gov/unnumbered/70222222/report.pdf","linkFileType":{"id":1,"text":"pdf"}},{"id":387333,"rank":1,"type":{"id":36,"text":"NGMDB Index Page"},"url":"https://ngmdb.usgs.gov/Prodesc/proddesc_74703.htm","linkFileType":{"id":5,"text":"html"}},{"id":396869,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/unnumbered/70222222/report-thumb.jpg"}],"country":"United States","state":"Alaska","otherGeospatial":"Ipnavik River area","geographicExtents":"{\n  \"type\": \"FeatureCollection\",\n  \"features\": [\n    {\n      \"type\": \"Feature\",\n      \"properties\": {},\n      \"geometry\": {\n        \"type\": \"Polygon\",\n        \"coordinates\": [\n          [\n            [\n              -156.5,\n              68.8833\n            ],\n            [\n              -157.5,\n              68.8833\n            ],\n            [\n              -157.5,\n              68.5\n            ],\n            [\n              -156.5,\n              68.5\n            ],\n            [\n              -156.5,\n              68.8833\n            ]\n          ]\n        ]\n      }\n    }\n  ]\n}","noUsgsAuthors":false,"publicationStatus":"PW","contributors":{"authors":[{"text":"Stefansson, Karl","contributorId":61296,"corporation":false,"usgs":true,"family":"Stefansson","given":"Karl","email":"","affiliations":[],"preferred":false,"id":837466,"contributorType":{"id":1,"text":"Authors"},"rank":1}]}}
,{"id":37851,"text":"37851 - 1948 - Organizations and officials concerned with wildlife protection: 1948","interactions":[],"lastModifiedDate":"2014-07-24T14:03:24","indexId":"37851","displayToPublicDate":"1948-12-01T14:02:48","publicationYear":"1948","noYear":false,"publicationType":{"id":18,"text":"Report"},"publicationSubtype":{"id":1,"text":"Federal Government Series"},"seriesTitle":{"id":98,"text":"Wildlife Leaflet","active":false,"publicationSubtype":{"id":1}},"seriesNumber":"313","title":"Organizations and officials concerned with wildlife protection: 1948","docAbstract":"No abstract available.","language":"English","publisher":"U.S. Department of the Interior","publisherLocation":"Washington, D.C.","usgsCitation":"Hommel, M.L., 1948, Organizations and officials concerned with wildlife protection: 1948: Wildlife Leaflet 313, 33 p.","productDescription":"33 p.","numberOfPages":"33","costCenters":[],"links":[{"id":290944,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/thumbnails/outside_thumb.jpg"}],"noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"57ffd95fe4b0824b2d178604","contributors":{"authors":[{"text":"Hommel, Mary Louise","contributorId":30149,"corporation":false,"usgs":true,"family":"Hommel","given":"Mary","email":"","middleInitial":"Louise","affiliations":[],"preferred":false,"id":218604,"contributorType":{"id":1,"text":"Authors"},"rank":1}]}}
,{"id":70210416,"text":"70210416 - 1948 - Areal evaluation of petroleum possibilities of major stratigraphic units in northern Alaska","interactions":[],"lastModifiedDate":"2022-05-31T20:07:17.612303","indexId":"70210416","displayToPublicDate":"1948-11-01T16:17:55","publicationYear":"1948","noYear":false,"publicationType":{"id":18,"text":"Report"},"publicationSubtype":{"id":6,"text":"USGS Unnumbered Series"},"seriesTitle":{"id":5963,"text":"Geological Investigations, Naval Petroleum Reserve No. 4, Alaska","active":false,"publicationSubtype":{"id":6}},"seriesNumber":"24","title":"Areal evaluation of petroleum possibilities of major stratigraphic units in northern Alaska","docAbstract":"<p>No abstract available.</p>","language":"English","publisher":"U.S. Geological Survey","doi":"10.3133/70210416","usgsCitation":"Payne, T.G., 1948, Areal evaluation of petroleum possibilities of major stratigraphic units in northern Alaska: Geological Investigations, Naval Petroleum Reserve No. 4, Alaska 24, Report: 23 p.; 4 Plates: 26.09 x 11.04 inches or smaller, https://doi.org/10.3133/70210416.","productDescription":"Report: 23 p.; 4 Plates: 26.09 x 11.04 inches or smaller","costCenters":[],"links":[{"id":396528,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/unnumbered/70210416/report-thumb.jpg"},{"id":375261,"rank":1,"type":{"id":36,"text":"NGMDB Index Page"},"url":"https://ngmdb.usgs.gov/Prodesc/proddesc_74607.htm","linkFileType":{"id":5,"text":"html"}},{"id":401084,"rank":3,"type":{"id":11,"text":"Document"},"url":"https://pubs.usgs.gov/unnumbered/70210416/report.pdf","linkFileType":{"id":1,"text":"pdf"}},{"id":401085,"rank":4,"type":{"id":29,"text":"Figure"},"url":"https://pubs.usgs.gov/unnumbered/70210416/figure-1.pdf","text":"Figure 1","linkFileType":{"id":1,"text":"pdf"}},{"id":401086,"rank":5,"type":{"id":29,"text":"Figure"},"url":"https://pubs.usgs.gov/unnumbered/70210416/figure-2.pdf","text":"Figure 2","linkFileType":{"id":1,"text":"pdf"}},{"id":401087,"rank":6,"type":{"id":29,"text":"Figure"},"url":"https://pubs.usgs.gov/unnumbered/70210416/figure-3.pdf","text":"Figure 3","linkFileType":{"id":1,"text":"pdf"}},{"id":401088,"rank":7,"type":{"id":29,"text":"Figure"},"url":"https://pubs.usgs.gov/unnumbered/70210416/figure-4.pdf","text":"Figure 4","linkFileType":{"id":1,"text":"pdf"}}],"country":"United States","state":"Alaska","geographicExtents":"{\n  \"type\": \"FeatureCollection\",\n  \"features\": [\n    {\n      \"type\": \"Feature\",\n      \"properties\": {},\n      \"geometry\": {\n        \"type\": \"Polygon\",\n        \"coordinates\": [\n          [\n            [\n              -167.4755859375,\n              65.38514722188854\n            ],\n            [\n              -141.0205078125,\n              65.38514722188854\n            ],\n            [\n              -141.0205078125,\n              71.5944122077672\n            ],\n            [\n              -167.4755859375,\n              71.5944122077672\n            ],\n            [\n              -167.4755859375,\n              65.38514722188854\n            ]\n          ]\n        ]\n      }\n    }\n  ]\n}","noUsgsAuthors":false,"publicationStatus":"PW","contributors":{"authors":[{"text":"Payne, T. G.","contributorId":66777,"corporation":false,"usgs":true,"family":"Payne","given":"T.","email":"","middleInitial":"G.","affiliations":[],"preferred":false,"id":837037,"contributorType":{"id":1,"text":"Authors"},"rank":1}]}}
,{"id":37854,"text":"37854 - 1948 - Abstract of fur laws, 1948-49","interactions":[],"lastModifiedDate":"2014-07-24T11:22:52","indexId":"37854","displayToPublicDate":"1948-11-01T11:22:20","publicationYear":"1948","noYear":false,"publicationType":{"id":18,"text":"Report"},"publicationSubtype":{"id":1,"text":"Federal Government Series"},"seriesTitle":{"id":98,"text":"Wildlife Leaflet","active":false,"publicationSubtype":{"id":1}},"seriesNumber":"316","title":"Abstract of fur laws, 1948-49","docAbstract":"No abstract available.","language":"English","publisher":"U.S. Department of the Interior","publisherLocation":"Washington, D.C.","usgsCitation":"Ashbrook, F.G., 1948, Abstract of fur laws, 1948-49 (Reissued from Wildlife Leaflet BS-118 (1938)): Wildlife Leaflet 316, 42 p.","productDescription":"42 p.","numberOfPages":"42","costCenters":[],"links":[{"id":290893,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/thumbnails/outside_thumb.jpg"}],"edition":"Reissued from Wildlife Leaflet BS-118 (1938)","noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"57ffd95fe4b0824b2d178606","contributors":{"authors":[{"text":"Ashbrook, Frank G.","contributorId":77980,"corporation":false,"usgs":true,"family":"Ashbrook","given":"Frank","email":"","middleInitial":"G.","affiliations":[],"preferred":false,"id":218607,"contributorType":{"id":1,"text":"Authors"},"rank":1}]}}
,{"id":70215757,"text":"70215757 - 1948 - Some solutional features of the limestone near Lexington, Kentucky","interactions":[],"lastModifiedDate":"2020-10-28T19:58:10.057194","indexId":"70215757","displayToPublicDate":"1948-10-28T14:34:17","publicationYear":"1948","noYear":false,"publicationType":{"id":2,"text":"Article"},"publicationSubtype":{"id":10,"text":"Journal Article"},"seriesTitle":{"id":1472,"text":"Economic Geology","active":true,"publicationSubtype":{"id":10}},"title":"Some solutional features of the limestone near Lexington, Kentucky","docAbstract":"<p><span>Field work on the Ordovician limestones and shales of the Lexington area, Kentucky, has shown that no appreciable quantity of ground water is transmitted through interstitial openings in these rocks. Ground-water movement is restricted to joint planes and, to a lesser extent, bedding planes that have been enlarged by solution. Studies of these planes indicate that solution has been effective only to a limited depth below the land surface. The bottom of the solutional zone is an exaggerated replica of the land surface, showing a greater depth of the solutional zone below stream valleys. The greater depth is attributed to the greater accumulation of ground water, the dissolving agent, in those areas. Modifications of the ideal condition are effected by the less soluble beds and the configuration of the land surface.</span></p><p><span>The underground drainage systems of the area develop in a manner similar to rectilinear stream patterns, showing a definite alignment along the two joint sets of the area. Directional solution has taken place where one of these joint sets has been developed to the exclusion of the other.</span></p>","language":"English","publisher":"Society of Economic Geologist","doi":"10.2113/gsecongeo.43.1.39","usgsCitation":"Hamilton, D., 1948, Some solutional features of the limestone near Lexington, Kentucky: Economic Geology, v. 43, no. 1, p. 39-52, https://doi.org/10.2113/gsecongeo.43.1.39.","productDescription":"14 p.","startPage":"39","endPage":"52","costCenters":[],"links":[{"id":379896,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/thumbnails/outside_thumb.jpg"}],"country":"United States","state":"Kentucky","otherGeospatial":"Lexington","geographicExtents":"{\n  \"type\": \"FeatureCollection\",\n  \"features\": [\n    {\n      \"type\": \"Feature\",\n      \"properties\": {},\n      \"geometry\": {\n        \"type\": \"Polygon\",\n        \"coordinates\": [\n          [\n            [\n              -85.18798828125,\n              37.54893261064111\n            ],\n            [\n              -83.75976562499999,\n              37.54893261064111\n            ],\n            [\n              -83.75976562499999,\n              38.47939467327645\n            ],\n            [\n              -85.18798828125,\n              38.47939467327645\n            ],\n            [\n              -85.18798828125,\n              37.54893261064111\n            ]\n          ]\n        ]\n      }\n    }\n  ]\n}","volume":"43","issue":"1","noUsgsAuthors":false,"publicationDate":"1948-01-01","publicationStatus":"PW","contributors":{"authors":[{"text":"Hamilton, D.K.","contributorId":244110,"corporation":false,"usgs":false,"family":"Hamilton","given":"D.K.","email":"","affiliations":[],"preferred":false,"id":803313,"contributorType":{"id":1,"text":"Authors"},"rank":1}]}}
,{"id":70215756,"text":"70215756 - 1948 - Annual rainfall and runoff in New England ","interactions":[],"lastModifiedDate":"2020-10-28T19:26:49.356451","indexId":"70215756","displayToPublicDate":"1948-10-28T14:14:43","publicationYear":"1948","noYear":false,"publicationType":{"id":2,"text":"Article"},"publicationSubtype":{"id":10,"text":"Journal Article"},"seriesTitle":{"id":1578,"text":"Eos, Transactions, American Geophysical Union","onlineIssn":"2324-9250","printIssn":"0096-394","active":true,"publicationSubtype":{"id":10}},"title":"Annual rainfall and runoff in New England ","docAbstract":"<ul><li>This paper presents the results of studies of average rainfall and runoff, developed in the Office of the Division Engineer, New England Division, United States Corps of Engineers, in cooperation with the District Engineer, United States Geological Survey, and prepared in connection with flood‐control studies of the Connecticut and Merrimack River basins.</li></ul>","language":"English","publisher":"American Geophysical Union","doi":"10.1029/TR029i006p00903","usgsCitation":"McAleer, J., and Knox, C., 1948, Annual rainfall and runoff in New England : Eos, Transactions, American Geophysical Union, v. 29, no. 6, p. 903-908, https://doi.org/10.1029/TR029i006p00903.","productDescription":"6 p.","startPage":"903","endPage":"908","costCenters":[],"links":[{"id":379887,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/thumbnails/outside_thumb.jpg"}],"country":"United States","state":"Connecticut, Maine, Massachusetts, New Hampshire, New York,  Rhode Island and Vermont.","otherGeospatial":"New England","geographicExtents":"{\n  \"type\": \"FeatureCollection\",\n  \"features\": [\n    {\n      \"type\": \"Feature\",\n      \"properties\": {},\n      \"geometry\": {\n        \"type\": \"Polygon\",\n        \"coordinates\": [\n          [\n            [\n              -79.189453125,\n              42.16340342422401\n            ],\n            [\n              -75.322265625,\n              42.032974332441405\n            ],\n            [\n              -73.828125,\n              40.64730356252251\n            ],\n            [\n              -71.806640625,\n              40.84706035607122\n            ],\n            [\n              -69.697265625,\n              41.57436130598913\n            ],\n            [\n              -70.048828125,\n              42.94033923363181\n            ],\n            [\n              -66.97265625,\n              44.653024159812\n            ],\n            [\n              -67.1484375,\n              45.89000815866184\n            ],\n            [\n              -67.412109375,\n              47.517200697839414\n            ],\n            [\n              -68.64257812499999,\n              47.69497434186282\n            ],\n            [\n              -70.224609375,\n              47.39834920035926\n            ],\n            [\n              -71.103515625,\n              45.583289756006316\n            ],\n            [\n              -74.970703125,\n              45.213003555993964\n            ],\n            [\n              -75.91552734375,\n              44.87144275016589\n            ],\n            [\n              -76.37695312499999,\n              44.4808302785626\n            ],\n            [\n              -76.57470703125,\n              43.628123412124616\n            ],\n            [\n              -79.21142578125,\n              43.51668853502906\n            ],\n            [\n              -79.2333984375,\n              42.956422511073335\n            ],\n            [\n              -79.98046875,\n              42.407234661551875\n            ],\n            [\n              -79.189453125,\n              42.16340342422401\n            ]\n          ]\n        ]\n      }\n    }\n  ]\n}","volume":"29","issue":"6","noUsgsAuthors":false,"publicationDate":"2014-08-18","publicationStatus":"PW","contributors":{"authors":[{"text":"McAleer, J.J.","contributorId":208430,"corporation":false,"usgs":false,"family":"McAleer","given":"J.J.","email":"","affiliations":[],"preferred":false,"id":803311,"contributorType":{"id":1,"text":"Authors"},"rank":1},{"text":"Knox, C. E.","contributorId":91835,"corporation":false,"usgs":true,"family":"Knox","given":"C. E.","affiliations":[],"preferred":false,"id":803312,"contributorType":{"id":1,"text":"Authors"},"rank":2}]}}
,{"id":70215755,"text":"70215755 - 1948 - Lava movement at Parícutin Volcano, Mexico ","interactions":[],"lastModifiedDate":"2020-10-29T12:33:18.490362","indexId":"70215755","displayToPublicDate":"1948-10-28T13:50:23","publicationYear":"1948","noYear":false,"publicationType":{"id":2,"text":"Article"},"publicationSubtype":{"id":10,"text":"Journal Article"},"seriesTitle":{"id":1723,"text":"GSA Bulletin","active":true,"publicationSubtype":{"id":10}},"title":"Lava movement at Parícutin Volcano, Mexico ","docAbstract":"<p>The lava flows of Parícutin Volcano, Mexico, offer an exceptional opportunity to study details of lava movement, because many flows are accessible throughout their length and can be watched from their birth to the cessation of their movement. Petrographically the lavas show no significant difference from one flow to another or in different parts of the same flow. The maximum lava temperature observed was 1070°C.; the maximum estimated rate of flow was 60 meters per minute; the viscosity is probably on the order of 10<sup>5</sup><span>&nbsp;</span>to 10<sup>6</sup><span>&nbsp;</span>poises. The flows start in fissure zones cutting older Parícutin lavas near the southwest base of the volcano. Within a short distance of its orifice a flow is covered with cooled blocks which are broken and slightly abraded as they are carried downstream. Differential movement in a flow takes place principally at its edges, where a reddish breccia and grooved and slickensided surfaces form. Like a glacier, a lava flow develops transverse crescentic ridges and lateral moraines. At its front movement is normally effected by the rolling forward of molten lava within, which carries down cooled blocks from the surface and piles them up ahead of the flow. As a flow dies the lava level lowers in the channel, and small side tongues break through the moraines. Some Parícutin lavas move considerable distances beneath older lava. The longest flow, which covered the town of San Juan in 1944, has a surface of rough curved slabs very different from the blocky surface of other flows but similar to the surface structures developed near lava orifices and by movement of viscous lava through fissures.</p>","language":"English","publisher":"Geological Society of America","doi":"10.1130/0016-7606(1948)59[1267:LMAPVM]2.0.CO;2","usgsCitation":"Krauskopf, K., 1948, Lava movement at Parícutin Volcano, Mexico : GSA Bulletin, v. 59, no. 12, p. 1267-1284, https://doi.org/10.1130/0016-7606(1948)59[1267:LMAPVM]2.0.CO;2.","productDescription":"18 p.","startPage":"1267","endPage":"1284","costCenters":[],"links":[{"id":379885,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/thumbnails/outside_thumb.jpg"}],"country":"Mexico","state":"Michoacan","otherGeospatial":"Paricutin Volcano","geographicExtents":"{\n  \"type\": \"FeatureCollection\",\n  \"features\": [\n    {\n      \"type\": \"Feature\",\n      \"properties\": {},\n      \"geometry\": {\n        \"type\": \"Polygon\",\n        \"coordinates\": [\n          [\n            [\n              -102.5848388671875,\n              19.150357455407473\n            ],\n            [\n              -102.073974609375,\n              19.150357455407473\n            ],\n            [\n              -102.073974609375,\n              19.756364230752375\n            ],\n            [\n              -102.5848388671875,\n              19.756364230752375\n            ],\n            [\n              -102.5848388671875,\n              19.150357455407473\n            ]\n          ]\n        ]\n      }\n    }\n  ]\n}","volume":"59","issue":"12","noUsgsAuthors":false,"publicationStatus":"PW","contributors":{"authors":[{"text":"Krauskopf, K.B.","contributorId":28943,"corporation":false,"usgs":true,"family":"Krauskopf","given":"K.B.","email":"","affiliations":[],"preferred":false,"id":803309,"contributorType":{"id":1,"text":"Authors"},"rank":1}]}}
,{"id":70215754,"text":"70215754 - 1948 - Submarine geology of Bikini atoll ","interactions":[],"lastModifiedDate":"2020-10-29T12:34:05.344607","indexId":"70215754","displayToPublicDate":"1948-10-28T13:23:35","publicationYear":"1948","noYear":false,"publicationType":{"id":2,"text":"Article"},"publicationSubtype":{"id":10,"text":"Journal Article"},"seriesTitle":{"id":1723,"text":"GSA Bulletin","active":true,"publicationSubtype":{"id":10}},"title":"Submarine geology of Bikini atoll ","docAbstract":"<div class=\"article-section-wrapper js-article-section js-content-section  \"><p>The program of investigations made in connection with the atomic bomb tests in the summer of 1946 at Bikini Atoll provided a rare opportunity for obtaining information on the physiography and sediments of atolls. The outer slopes around Bikini Atoll rise from a depth of about 2500 fathoms in a long gradually steepening curve. Between 0 and 200 fathoms the average slope is 25°. On the windward side, the reef at the top of the slope is bordered by a narrow 15-fathom terrace, but on the leeward side by a steep, locally vertical, cliff extending to 35 fathoms. Contours of the outer slopes reveal that a flat-topped mass having nearly the area of Bikini lagoon but below 700 fathoms extends to the northwest. The lagoon itself is saucer-shaped and has a maximum depth of 34 fathoms. Around the lagoon and bordering the inner side of the reef and islands is a 12-fathom terrace. Coral knolls rise abruptly from the lagoon floor, and some of them reach to within a few fathoms of the surface. The middle of the lagoon is floored chiefly by algal debris, whereas the shallow edges are covered by algal and foraminiferal sand. Coral comprises a relatively small percentage of the bottom materials. The outer slopes consist of algal debris grading outward to fine sand and finally to<span>&nbsp;</span><i>Globigerina</i><span>&nbsp;</span>sand.</p></div>","language":"English","publisher":"Geological Society of America","doi":"10.1130/0016-7606(1948)59[855:SGOBA]2.0.CO;2","usgsCitation":"Emery, K., 1948, Submarine geology of Bikini atoll : GSA Bulletin, v. 59, no. 9, p. 855-860, https://doi.org/10.1130/0016-7606(1948)59[855:SGOBA]2.0.CO;2.","productDescription":"6 p.","startPage":"855","endPage":"860","costCenters":[],"links":[{"id":379884,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/thumbnails/outside_thumb.jpg"}],"otherGeospatial":"Bikini Atoll","geographicExtents":"{\n  \"type\": \"FeatureCollection\",\n  \"features\": [\n    {\n      \"type\": \"Feature\",\n      \"properties\": {},\n      \"geometry\": {\n        \"type\": \"Polygon\",\n        \"coordinates\": [\n          [\n            [\n              167.255859375,\n              6.642782900356179\n            ],\n            [\n              169.69482421875,\n              6.642782900356179\n            ],\n            [\n              169.69482421875,\n              9.481572085088517\n            ],\n            [\n              167.255859375,\n              9.481572085088517\n            ],\n            [\n              167.255859375,\n              6.642782900356179\n            ]\n          ]\n        ]\n      }\n    }\n  ]\n}","volume":"59","issue":"9","noUsgsAuthors":false,"publicationStatus":"PW","contributors":{"authors":[{"text":"Emery, K.O.","contributorId":67865,"corporation":false,"usgs":true,"family":"Emery","given":"K.O.","email":"","affiliations":[],"preferred":false,"id":803308,"contributorType":{"id":1,"text":"Authors"},"rank":1}]}}
,{"id":70215753,"text":"70215753 - 1948 - Age of the Kingsbury conglomerate is Eocene ","interactions":[],"lastModifiedDate":"2020-10-29T12:35:26.313699","indexId":"70215753","displayToPublicDate":"1948-10-28T12:56:46","publicationYear":"1948","noYear":false,"publicationType":{"id":2,"text":"Article"},"publicationSubtype":{"id":10,"text":"Journal Article"},"seriesTitle":{"id":1723,"text":"GSA Bulletin","active":true,"publicationSubtype":{"id":10}},"title":"Age of the Kingsbury conglomerate is Eocene ","docAbstract":"<div class=\"article-section-wrapper js-article-section js-content-section  \"><p>The Kingsbury conglomerate and immediately overlying gravels on the east side of the Bighorn Mountains in Wyoming interfinger eastward with “Wasatch” strata. The latter contain Eocene vertebrates, species of which have been found in the Kingsbury conglomerate. In addition, the “Wasatch” strata contain an Eocene flora that includes the floating fern, Salvinia preauriculata Berry, which, because it is not found in earlier beds, permits recognition of the Paleocene-Eocene boundary in the Rocky Mountains and Plains region.</p></div>","language":"English","publisher":"Geological Society of America","doi":"10.1130/0016-7606(1948)59[1165:AOTKCI]2.0.CO;2","usgsCitation":"Brown, R., 1948, Age of the Kingsbury conglomerate is Eocene : GSA Bulletin, v. 59, no. 11, p. 1165-1172, https://doi.org/10.1130/0016-7606(1948)59[1165:AOTKCI]2.0.CO;2.","productDescription":"8 p.","startPage":"1165","endPage":"1172","costCenters":[],"links":[{"id":379879,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/thumbnails/outside_thumb.jpg"}],"country":"United States","state":"Wyoming","otherGeospatial":"Kingsbury Conglomerate","geographicExtents":"{\"type\":\"FeatureCollection\",\"features\":[{\"type\":\"Feature\",\"geometry\":{\"type\":\"Polygon\",\"coordinates\":[[[-110.048476,40.997555],[-110.121639,40.997101],[-110.125709,40.99655],[-110.237848,40.995427],[-110.250709,40.996089],[-110.375714,40.994947],[-110.500718,40.994746],[-110.539819,40.996346],[-110.715026,40.996347],[-110.750727,40.996847],[-111.046723,40.997959],[-111.046551,41.251716],[-111.0466,41.360692],[-111.046264,41.377731],[-111.045789,41.565571],[-111.045818,41.579845],[-111.046689,42.001567],[-111.047109,42.142497],[-111.047107,42.148971],[-111.047058,42.182672],[-111.047097,42.194773],[-111.047074,42.280787],[-111.04708,42.34942],[-111.046801,42.504946],[-111.046719,42.513118],[-111.046017,42.582723],[-111.043564,42.722624],[-111.044135,42.874924],[-111.043959,42.96445],[-111.043957,42.969482],[-111.043924,42.975063],[-111.044129,43.018702],[-111.044156,43.020052],[-111.044206,43.022614],[-111.044034,43.024581],[-111.044034,43.024844],[-111.044033,43.026411],[-111.044094,43.02927],[-111.043997,43.041415],[-111.044058,43.04464],[-111.044063,43.046302],[-111.044086,43.054819],[-111.044117,43.060309],[-111.04415,43.066172],[-111.044162,43.068222],[-111.044143,43.072364],[-111.044235,43.177121],[-111.044266,43.177236],[-111.044232,43.18444],[-111.044168,43.189244],[-111.044229,43.195579],[-111.044617,43.31572],[-111.045205,43.501136],[-111.045706,43.659112],[-111.04588,43.681033],[-111.046118,43.684902],[-111.046051,43.685812],[-111.04611,43.687848],[-111.046421,43.722059],[-111.046435,43.726545],[-111.04634,43.726957],[-111.046715,43.815832],[-111.046515,43.908376],[-111.046917,43.974978],[-111.047064,43.983467],[-111.047349,43.999921],[-111.049077,44.020072],[-111.048751,44.060403],[-111.048751,44.060838],[-111.048633,44.062903],[-111.048452,44.114831],[-111.049119,44.124923],[-111.049695,44.353626],[-111.049148,44.374925],[-111.049216,44.435811],[-111.049194,44.438058],[-111.048974,44.474072],[-111.055208,44.624927],[-111.055333,44.666263],[-111.055511,44.725343],[-111.056416,44.749928],[-111.056888,44.866658],[-111.055629,44.933578],[-111.056207,44.935901],[-111.055199,45.001321],[-111.044275,45.001345],[-110.785008,45.002952],[-110.761554,44.999934],[-110.750767,44.997948],[-110.705272,44.992324],[-110.552433,44.992237],[-110.547165,44.992459],[-110.48807,44.992361],[-110.402927,44.99381],[-110.362698,45.000593],[-110.342131,44.999053],[-110.324441,44.999156],[-110.28677,44.99685],[-110.199503,44.996188],[-110.110103,45.003905],[-110.026347,45.003665],[-110.025544,45.003602],[-109.99505,45.003174],[-109.875735,45.003275],[-109.798687,45.002188],[-109.75073,45.001605],[-109.663673,45.002536],[-109.574321,45.002631],[-109.386432,45.004887],[-109.375713,45.00461],[-109.269294,45.005283],[-109.263431,45.005345],[-109.103445,45.005904],[-109.08301,44.99961],[-109.062262,44.999623],[-108.621313,45.000408],[-108.578484,45.000484],[-108.565921,45.000578],[-108.500679,44.999691],[-108.271201,45.000251],[-108.249345,44.999458],[-108.238139,45.000206],[-108.218479,45.000541],[-108.14939,45.001062],[-108.000663,45.001223],[-107.997353,45.001565],[-107.911743,45.001292],[-107.750654,45.000778],[-107.608854,45.00086],[-107.607824,45.000929],[-107.49205,45.00148],[-107.351441,45.001407],[-107.13418,45.000109],[-107.125633,44.999388],[-107.105685,44.998734],[-107.084939,44.996599],[-107.074996,44.997004],[-107.050801,44.996424],[-106.892875,44.995947],[-106.888773,44.995885],[-106.263586,44.993788],[-106.024814,44.993688],[-105.928184,44.993647],[-105.914258,44.999986],[-105.913382,45.000941],[-105.848065,45.000396],[-105.076607,45.000347],[-105.038405,45.000345],[-105.025266,45.00029],[-105.019284,45.000329],[-105.01824,45.000437],[-104.765063,44.999183],[-104.759855,44.999066],[-104.72637,44.999518],[-104.665171,44.998618],[-104.663882,44.998869],[-104.470422,44.998453],[-104.470117,44.998453],[-104.250145,44.99822],[-104.057698,44.997431],[-104.055914,44.874986],[-104.056496,44.867034],[-104.055963,44.768236],[-104.055963,44.767962],[-104.055934,44.72372],[-104.05587,44.723422],[-104.055777,44.700466],[-104.055938,44.693881],[-104.05581,44.691343],[-104.055877,44.571016],[-104.055892,44.543341],[-104.055927,44.51773],[-104.055389,44.249983],[-104.054487,44.180381],[-104.054562,44.141081],[-104.05495,43.93809],[-104.055077,43.936535],[-104.055488,43.853477],[-104.055488,43.853476],[-104.055138,43.750421],[-104.055133,43.747105],[-104.054902,43.583852],[-104.054885,43.583512],[-104.05484,43.579368],[-104.055032,43.558603],[-104.054787,43.503328],[-104.054786,43.503072],[-104.054779,43.477815],[-104.054766,43.428914],[-104.054614,43.390949],[-104.054403,43.325914],[-104.054218,43.30437],[-104.053884,43.297047],[-104.053876,43.289801],[-104.053127,43.000585],[-104.052863,42.754569],[-104.052809,42.749966],[-104.052583,42.650062],[-104.052741,42.633982],[-104.052586,42.630917],[-104.052773,42.611766],[-104.052775,42.61159],[-104.052775,42.610813],[-104.053107,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 \"}}]}","volume":"59","issue":"11","noUsgsAuthors":false,"publicationStatus":"PW","contributors":{"authors":[{"text":"Brown, Roland W.","contributorId":91556,"corporation":false,"usgs":true,"family":"Brown","given":"Roland W.","affiliations":[],"preferred":false,"id":803307,"contributorType":{"id":1,"text":"Authors"},"rank":1}]}}
,{"id":70215752,"text":"70215752 - 1948 - Quality of water in the upper Colorado River basin","interactions":[],"lastModifiedDate":"2021-04-06T15:23:39.269743","indexId":"70215752","displayToPublicDate":"1948-10-28T12:21:45","publicationYear":"1948","noYear":false,"publicationType":{"id":2,"text":"Article"},"publicationSubtype":{"id":10,"text":"Journal Article"},"seriesTitle":{"id":1578,"text":"Eos, Transactions, American Geophysical Union","onlineIssn":"2324-9250","printIssn":"0096-394","active":true,"publicationSubtype":{"id":10}},"title":"Quality of water in the upper Colorado River basin","docAbstract":"<p>In a drainage area as large as the Colorado River Basin there are naturally large differences in the quality of the surface waters. The chemical character of the water at six gaging stations on the Colorado River from near the headwaters to near the mouth is shown by the analyses in Table 1.</p><p>It will be seen that the concentration of dissolved solids increased from 64 ppm (0.09 tons per ac ft) in the headwaters to 699 ppm (0.95 tons per ac ft) near the mouth.</p>","language":"English","publisher":"American Geophysical Union","doi":"10.1029/TR029i003p00375","usgsCitation":"Howard, C.S., 1948, Quality of water in the upper Colorado River basin: Eos, Transactions, American Geophysical Union, v. 29, no. 3, p. 375-378, https://doi.org/10.1029/TR029i003p00375.","productDescription":"4 p.","startPage":"375","endPage":"378","costCenters":[],"links":[{"id":379878,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/thumbnails/outside_thumb.jpg"}],"country":"United States","state":"Colorado","otherGeospatial":"Upper Colorado River 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 \"}}]}","volume":"29","issue":"3","noUsgsAuthors":false,"publicationDate":"2014-08-18","publicationStatus":"PW","contributors":{"authors":[{"text":"Howard, C. S.","contributorId":73180,"corporation":false,"usgs":true,"family":"Howard","given":"C.","email":"","middleInitial":"S.","affiliations":[],"preferred":false,"id":803306,"contributorType":{"id":1,"text":"Authors"},"rank":1}]}}
,{"id":70215751,"text":"70215751 - 1948 - Fluctuations in concentration of dissolved solids of some southwestern streams","interactions":[],"lastModifiedDate":"2020-10-28T17:15:15.508813","indexId":"70215751","displayToPublicDate":"1948-10-28T12:11:05","publicationYear":"1948","noYear":false,"publicationType":{"id":2,"text":"Article"},"publicationSubtype":{"id":10,"text":"Journal Article"},"seriesTitle":{"id":1578,"text":"Eos, Transactions, American Geophysical Union","onlineIssn":"2324-9250","printIssn":"0096-394","active":true,"publicationSubtype":{"id":10}},"title":"Fluctuations in concentration of dissolved solids of some southwestern streams","docAbstract":"<p><span>The concentration of dissolved solids in waters of streams of the Southwestern United Stated fluctuates widely as the stream discharge changes. These fluctuations may be extensive in a period of a few days or even a few hours. Data in this paper show the extent of the day‐to‐day changes in specific conductance and discharge of the Rio Grande at San Acacia, New Mexico, during the spring run‐off period of 1945. Data also are presented to show rapid fluctuations in concentration for the Pecos River near Artesia, New Mexico, the Gila River near Bylas, Arizona, and the Rio Grande at San Acacia during typical summer months. Hourly changes in chloride and discharge are shown for a day of approximately normal flow for the Pecos River near Malaga, New Mexico, and for a 36‐hour period of extremely low flow for the Gila River near Fort Thomas, Arizona.</span></p>","language":"English","publisher":"American Geophysical Union","doi":"10.1029/TR029i001p00080","usgsCitation":"Hem, J., 1948, Fluctuations in concentration of dissolved solids of some southwestern streams: Eos, Transactions, American Geophysical Union, v. 29, no. 1, p. 80-84, https://doi.org/10.1029/TR029i001p00080.","productDescription":"5 p.","startPage":"80","endPage":"84","costCenters":[],"links":[{"id":379877,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/thumbnails/outside_thumb.jpg"}],"country":"United States","state":"Arizona, New Mexico","otherGeospatial":"Southwestern Streams","geographicExtents":"{\n  \"type\": \"FeatureCollection\",\n  \"features\": [\n    {\n      \"type\": \"Feature\",\n      \"properties\": {},\n      \"geometry\": {\n        \"type\": \"Polygon\",\n        \"coordinates\": [\n          [\n            [\n              -110.41259765625,\n              32.7503226078097\n            ],\n            [\n              -108.30322265624999,\n              32.7503226078097\n            ],\n            [\n              -108.30322265624999,\n              34.488447837809304\n            ],\n            [\n              -110.41259765625,\n              34.488447837809304\n            ],\n            [\n              -110.41259765625,\n              32.7503226078097\n            ]\n          ]\n        ]\n      }\n    }\n  ]\n}","volume":"29","issue":"1","noUsgsAuthors":false,"publicationDate":"2014-08-18","publicationStatus":"PW","contributors":{"authors":[{"text":"Hem, J.D.","contributorId":54576,"corporation":false,"usgs":true,"family":"Hem","given":"J.D.","affiliations":[],"preferred":false,"id":803305,"contributorType":{"id":1,"text":"Authors"},"rank":1}]}}
,{"id":70215693,"text":"70215693 - 1948 - Geology and ground-water resources of Iwo Jima ","interactions":[],"lastModifiedDate":"2020-10-27T20:28:58.557427","indexId":"70215693","displayToPublicDate":"1948-10-27T15:01:22","publicationYear":"1948","noYear":false,"publicationType":{"id":2,"text":"Article"},"publicationSubtype":{"id":10,"text":"Journal Article"},"seriesTitle":{"id":1723,"text":"GSA Bulletin","active":true,"publicationSubtype":{"id":10}},"title":"Geology and ground-water resources of Iwo Jima ","docAbstract":"<p>Iwo Jima, in the western Pacific Ocean, consists of Motoyama, a broad volcanic cone, at the north, and Mt. Suribachi at the south, with an undulating isthmus between. Motoyama is largely light-gray-buff tuff. A thick andesitic lava flow under Suribachi, exposed in several places, is overlain by a thick deposit of cinder and scoria. The isthmus (called Tidorigahara by the Japanese) is underlain by more than 200 feet of loose black volcanic ash and fine cinder derived from Suribachi. Several small coral reefs are located about 340 and 110 feet above present sea level.</p><p>Iwo Jima first came into existence, probably early in Pleistocene time, with the building above sea level of the tuff cone of Motoyama. Quite late in the active life of Motoyama, volcanic activity on the southwestern flank resulted in the formation of Suribachi. This activity may have started with the welling up of the andesitic lava which underlies Suribachi. Following the major eruption of Suribachi, relative sea level changed, and the sea stood about 360 feet higher than at present. The broad cone of Motoyama was beveled; the relative sea level then dropped 240 feet, with minor halts to about 120 feet above present level. As the island rose, Suribachi burst forth in its last stage of explosive activity. Wave erosion cut deeply into the andesite flow of Suribachi, and a prominent bench level was formed 120 feet above present sea level.</p><p>The Japanese on the island were often faced with serious water shortages. Americans drilled wells and obtained moderately large supplies of usable water. The temperature of the water ranges from 105° to 179° F., and the water is somewhat mineralized. The most favorable area for ground-water development is the isthmus.</p>","language":"English","publisher":"Geological Society of America","doi":"10.1130/0016-7606(1948)59[995:GAGROI]2.0.CO;2","usgsCitation":"Swenson, F.A., 1948, Geology and ground-water resources of Iwo Jima : GSA Bulletin, v. 59, no. 10, p. 995-1008, https://doi.org/10.1130/0016-7606(1948)59[995:GAGROI]2.0.CO;2.","productDescription":"14 p.","startPage":"995","endPage":"1008","costCenters":[],"links":[{"id":379832,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/thumbnails/outside_thumb.jpg"}],"country":"Japan","otherGeospatial":"Iwo Jima","geographicExtents":"{\n  \"type\": \"FeatureCollection\",\n  \"features\": [\n    {\n      \"type\": \"Feature\",\n      \"properties\": {},\n      \"geometry\": {\n        \"type\": \"Polygon\",\n        \"coordinates\": [\n          [\n            [\n              141.251220703125,\n              24.693814995267424\n            ],\n            [\n              141.4057159423828,\n              24.693814995267424\n            ],\n            [\n              141.4057159423828,\n              24.85092688067188\n            ],\n            [\n              141.251220703125,\n              24.85092688067188\n            ],\n            [\n              141.251220703125,\n              24.693814995267424\n            ]\n          ]\n        ]\n      }\n    }\n  ]\n}","volume":"59","issue":"10","noUsgsAuthors":false,"publicationStatus":"PW","contributors":{"authors":[{"text":"Swenson, F. A.","contributorId":71622,"corporation":false,"usgs":true,"family":"Swenson","given":"F.","email":"","middleInitial":"A.","affiliations":[{"id":595,"text":"U.S. Geological Survey","active":false,"usgs":true}],"preferred":false,"id":803152,"contributorType":{"id":1,"text":"Authors"},"rank":1}]}}
,{"id":70215691,"text":"70215691 - 1948 - Reefs of Bikini, Marshall Islands ","interactions":[],"lastModifiedDate":"2020-10-28T16:39:06.745647","indexId":"70215691","displayToPublicDate":"1948-10-27T14:49:11","publicationYear":"1948","noYear":false,"publicationType":{"id":2,"text":"Article"},"publicationSubtype":{"id":10,"text":"Journal Article"},"seriesTitle":{"id":1723,"text":"GSA Bulletin","active":true,"publicationSubtype":{"id":10}},"title":"Reefs of Bikini, Marshall Islands ","docAbstract":"<p>Systematic surveys made at Bikini before and after the atomi bomb tests (Operation Crossroads) in the summer of 1946 afforded an unusual opportunity to examine the reefs and islands of one of the larger atolls of Micronesia. The existing reef appears to be developed on an older surface that extends as a terrace into the lagoon and beyond the seaward margin of the reef. A sketch map shows the distribution of the terraces in relation to the existing reefs.</p><p>Reef zonation is briefly described, and a classification of reef types based upon the characteristics of the marginal zone is presented. Illustrations are given from Bikini's reefs and those of near-by atolls. A sketch map shows the distribution of the reef types at Bikini relative to prevailing winds and currents. The processes of reef growth and unusual areas wherein the existing reef appears to be undergoing destruction are also described and figured.</p>","language":"English","publisher":"Geological Society of America","doi":"10.1130/0016-7606(1948)59[861:ROBMI]2.0.CO;2","usgsCitation":"Tracey, J.I., Lapham, H., and Hoffmeister, J.E., 1948, Reefs of Bikini, Marshall Islands : GSA Bulletin, v. 59, no. 9, p. 861-878, https://doi.org/10.1130/0016-7606(1948)59[861:ROBMI]2.0.CO;2.","productDescription":"18 p.","startPage":"861","endPage":"878","costCenters":[],"links":[{"id":379875,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/thumbnails/outside_thumb.jpg"}],"country":"Marshall Islands","otherGeospatial":"Bikini Reefs","geographicExtents":"{\n  \"type\": \"FeatureCollection\",\n  \"features\": [\n    {\n      \"type\": \"Feature\",\n      \"properties\": {},\n      \"geometry\": {\n        \"type\": \"Polygon\",\n        \"coordinates\": [\n          [\n            [\n              163.916015625,\n              4.214943141390651\n            ],\n            [\n              173.14453125,\n              4.214943141390651\n            ],\n            [\n              173.14453125,\n              13.068776734357694\n            ],\n            [\n              163.916015625,\n              13.068776734357694\n            ],\n            [\n              163.916015625,\n              4.214943141390651\n            ]\n          ]\n        ]\n      }\n    }\n  ]\n}","volume":"59","issue":"9","noUsgsAuthors":false,"publicationStatus":"PW","contributors":{"authors":[{"text":"Tracey, J. I. Jr.","contributorId":17205,"corporation":false,"usgs":true,"family":"Tracey","given":"J.","suffix":"Jr.","email":"","middleInitial":"I.","affiliations":[],"preferred":false,"id":803302,"contributorType":{"id":1,"text":"Authors"},"rank":1},{"text":"Lapham, H.S.","contributorId":66383,"corporation":false,"usgs":true,"family":"Lapham","given":"H.S.","email":"","affiliations":[],"preferred":false,"id":803303,"contributorType":{"id":1,"text":"Authors"},"rank":2},{"text":"Hoffmeister, J. E.","contributorId":220861,"corporation":false,"usgs":false,"family":"Hoffmeister","given":"J.","email":"","middleInitial":"E.","affiliations":[],"preferred":false,"id":803304,"contributorType":{"id":1,"text":"Authors"},"rank":3}]}}
,{"id":70215690,"text":"70215690 - 1948 - Precedence of modern plant names over names based on fossils","interactions":[],"lastModifiedDate":"2021-03-25T21:18:38.284594","indexId":"70215690","displayToPublicDate":"1948-10-27T14:24:46","publicationYear":"1948","noYear":false,"publicationType":{"id":2,"text":"Article"},"publicationSubtype":{"id":10,"text":"Journal Article"},"seriesTitle":{"id":3338,"text":"Science","active":true,"publicationSubtype":{"id":10}},"title":"Precedence of modern plant names over names based on fossils","docAbstract":"<p>No abstract available.</p>","language":"English","publisher":"American Association for the Advancement of Science","doi":"10.1126/science.108.2809.483","usgsCitation":"Schopf, J., 1948, Precedence of modern plant names over names based on fossils: Science, v. 108, no. 2809, https://doi.org/10.1126/science.108.2809.483.","productDescription":"1 p.","startPage":"483","costCenters":[],"links":[{"id":379830,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/thumbnails/outside_thumb.jpg"}],"volume":"108","issue":"2809","noUsgsAuthors":false,"publicationStatus":"PW","contributors":{"authors":[{"text":"Schopf, James M.","contributorId":94297,"corporation":false,"usgs":true,"family":"Schopf","given":"James M.","affiliations":[],"preferred":false,"id":803148,"contributorType":{"id":1,"text":"Authors"},"rank":1}]}}
,{"id":70215689,"text":"70215689 - 1948 - Mineralogy and petrology of the currant creek magnesite deposits and associated rocks of Nevada","interactions":[],"lastModifiedDate":"2020-10-28T11:58:38.091226","indexId":"70215689","displayToPublicDate":"1948-10-27T14:15:47","publicationYear":"1948","noYear":false,"publicationType":{"id":2,"text":"Article"},"publicationSubtype":{"id":10,"text":"Journal Article"},"seriesTitle":{"id":1723,"text":"GSA Bulletin","active":true,"publicationSubtype":{"id":10}},"title":"Mineralogy and petrology of the currant creek magnesite deposits and associated rocks of Nevada","docAbstract":"<p>Cryptocrystalline magnesite occurs as relatively small dense, white masses in a Tertiary volcanic tuff, here named the Currant tuff, in White Pine and Nye counties, 29 miles southwest of Ely, Nevada. The deposits are small, but some of the magnesite is of very high quality with almost no iron or aluminum. However, much of the magnesite is mixed with dolomite and calcite, and a serpentinelike mineral occurs in one of the deposits in sufficient abundance to be of possible use in ceramics.</p><p>In scattered areas the tuff has been altered by solutions rich in magnesium and bicarbonic acid to dolomite, magnesite, magnesium silicate, and calcite. Mineral and chemical characteristics are the same throughout the entire rock assemblage of flows and tuffs, suggesting that all the rocks have been derived from the same parent magma. The tuff formation, which ranges in thickness from a few feet to over 400 feet, occurs between two groups of volcanic flows here referred to as the lower volcanics and the upper volcanics. The lower volcanics is composed mainly of flows of hypersthene dacite, but in the southwestern part of the area flows of a hypersthene andesite of balsaltic habit occur between the dacite and the overlying Currant tuff. The upper volcanics which overlie the Currant tuff consist of porphyritic quartz latite and an overlying massive latite crystal tuff. The Currant tuff containing the magnesite has both unmodified and reworked tuff members.</p><p>The formation of hydrothermal dolomite, magnesite, and deweylite is discussed in detail, and the physical chemistry of solutions containing calcium, magnesium, and carbon dioxide is applied in an explanation of the origin of magnesium-rich solutions.</p>","language":"English","publisher":"Geological Society of America","doi":"10.1130/0016-7606(1948)59[11:MAPOTC]2.0.CO;2","usgsCitation":"Faust, G., and Callaghan, E., 1948, Mineralogy and petrology of the currant creek magnesite deposits and associated rocks of Nevada: GSA Bulletin, v. 59, no. 1, p. 11-74, https://doi.org/10.1130/0016-7606(1948)59[11:MAPOTC]2.0.CO;2.","productDescription":"64  p.","startPage":"11","endPage":"74","costCenters":[],"links":[{"id":379829,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/thumbnails/outside_thumb.jpg"}],"country":"United States","state":"Nevada","county":"White Pine County, Nye County","geographicExtents":"{\"type\":\"FeatureCollection\",\"features\":[{\"type\":\"Feature\",\"geometry\":{\"type\":\"Polygon\",\"coordinates\":[[[-114.999,38.6777],[-114.9996,38.592],[-114.9997,38.4315],[-114.9994,38.3894],[-115.0004,38.0507],[-115.1185,38.0508],[-115.1436,38.0508],[-115.326,38.0515],[-115.3453,38.0514],[-115.4003,38.051],[-115.4587,38.0506],[-115.6394,38.0512],[-115.6581,38.051],[-115.8404,38.0504],[-115.8931,38.0507],[-115.8938,37.723],[-115.8969,37.5498],[-115.8975,37.2796],[-115.8982,37.1926],[-115.8942,36.8425],[-115.8941,36.686],[-115.8945,36.6702],[-115.8949,36.598],[-115.8949,36.5962],[-115.8946,36.5858],[-115.8947,36.5005],[-115.8945,36.4806],[-115.8949,36.462],[-115.8944,36.457],[-115.8948,36.3087],[-115.8945,36.2923],[-115.8943,36.1957],[-115.8945,36.1608],[-115.8948,36.1163],[-115.8948,36.0927],[-115.895,36.0015],[-115.9178,36.0192],[-115.9518,36.0457],[-115.9925,36.0773],[-116.049,36.1211],[-116.0624,36.1314],[-116.1039,36.1636],[-116.1287,36.1829],[-116.1702,36.2152],[-116.173,36.2174],[-116.2311,36.2626],[-116.2834,36.3028],[-116.2954,36.3122],[-116.3752,36.373],[-116.5107,36.4764],[-116.5247,36.4871],[-116.5589,36.5131],[-116.574,36.5245],[-116.5946,36.54],[-116.6556,36.5867],[-116.6583,36.5888],[-116.6764,36.6024],[-116.706,36.6248],[-116.7895,36.6877],[-116.8424,36.7276],[-116.8453,36.7298],[-116.8806,36.7568],[-116.8912,36.7648],[-116.9237,36.7891],[-116.9641,36.8193],[-116.9783,36.8299],[-116.981,36.8319],[-117.0046,36.8495],[-117.164,36.9688],[-117.1639,36.9698],[-117.1637,37.0182],[-117.164,37.0894],[-117.1642,37.171],[-117.1641,37.1909],[-117.1641,37.1936],[-117.1665,37.6995],[-117.1664,37.714],[-117.1663,37.7285],[-117.1663,37.7435],[-117.1662,37.7585],[-117.1657,38.0019],[-117.2198,38.0482],[-117.2397,38.0483],[-117.239,38.0641],[-117.2408,38.0705],[-117.2653,38.0932],[-117.6896,38.4731],[-118.0197,38.7599],[-118.197,38.9154],[-118.1972,38.9993],[-117.8559,39.0746],[-117.7748,39.092],[-117.7008,39.1058],[-117.6409,39.1149],[-117.5946,39.1231],[-117.4742,39.1431],[-117.3823,39.1562],[-117.3609,39.1585],[-117.3318,39.1629],[-117.3063,39.1634],[-117.2849,39.1633],[-117.1995,39.1632],[-117.0856,39.1628],[-117.0322,39.1626],[-117.0144,39.1626],[-116.9871,39.1625],[-116.9158,39.1631],[-116.7562,39.1622],[-116.7301,39.1625],[-116.5996,39.1616],[-116.5859,39.162],[-116.4815,39.1616],[-116.3497,39.1618],[-116.2358,39.1616],[-116.0548,39.1624],[-115.9082,39.1615],[-115.9059,39.2947],[-115.9059,39.3219],[-115.9061,39.3369],[-115.9063,39.4638],[-115.8939,39.4605],[-115.8741,39.4652],[-115.8693,39.4679],[-115.8649,39.4755],[-115.8684,39.4806],[-115.8695,39.4851],[-115.8658,39.4901],[-115.8598,39.4922],[-115.8525,39.499],[-115.8518,39.5017],[-115.8524,39.5035],[-115.8523,39.5053],[-115.8444,39.5143],[-115.8414,39.5151],[-115.836,39.5182],[-115.8334,39.525],[-115.8279,39.5322],[-115.8271,39.5381],[-115.8306,39.5417],[-115.8341,39.5481],[-115.8363,39.5536],[-115.8374,39.5577],[-115.8361,39.564],[-115.8318,39.5685],[-115.83,39.5707],[-115.8263,39.5748],[-115.814,39.5891],[-115.8127,39.5945],[-115.8138,39.6],[-115.8195,39.6082],[-115.8164,39.6127],[-115.8181,39.6195],[-115.8227,39.6264],[-115.826,39.6378],[-115.8259,39.6446],[-115.8282,39.6478],[-115.8245,39.6523],[-115.8226,39.6563],[-115.823,39.6663],[-115.8234,39.6727],[-115.8233,39.6786],[-115.8237,39.6858],[-115.8248,39.6913],[-115.8312,39.6963],[-115.8314,39.7168],[-115.8305,39.7276],[-115.8315,39.7367],[-115.8266,39.7398],[-115.8236,39.7425],[-115.8223,39.7461],[-115.8193,39.747],[-115.815,39.7492],[-115.8119,39.7541],[-115.8106,39.7595],[-115.8129,39.7641],[-115.8128,39.7677],[-115.8127,39.7727],[-115.8126,39.7782],[-115.8118,39.7845],[-115.8093,39.7904],[-115.8085,39.7976],[-115.8102,39.8008],[-115.8137,39.8072],[-115.8152,39.8176],[-115.8121,39.8226],[-115.8085,39.8257],[-115.8054,39.8288],[-115.8023,39.8329],[-115.7986,39.8369],[-115.7967,39.8432],[-115.7984,39.846],[-115.7971,39.8496],[-115.7958,39.8527],[-115.7951,39.8595],[-115.8039,39.8678],[-115.8013,39.8746],[-115.8012,39.8787],[-115.8052,39.8896],[-115.8068,39.896],[-115.8061,39.9014],[-115.8036,39.905],[-115.8023,39.91],[-115.8081,39.9196],[-115.8139,39.9255],[-115.8162,39.9306],[-115.8173,39.9356],[-115.816,39.9387],[-115.8146,39.9464],[-115.8145,39.9528],[-115.8156,39.9573],[-115.8173,39.96],[-115.8241,39.9769],[-115.8276,39.981],[-115.8323,39.987],[-115.8334,39.9897],[-115.8344,39.9979],[-115.8344,40.0006],[-115.8337,40.0043],[-115.8341,40.0115],[-115.8302,40.0251],[-115.8283,40.0282],[-115.8288,40.0323],[-115.8317,40.0355],[-115.8346,40.0437],[-115.8315,40.0478],[-115.8278,40.0522],[-115.8276,40.0581],[-115.8317,40.0636],[-115.837,40.0682],[-115.8375,40.071],[-115.8344,40.0755],[-115.8349,40.0805],[-115.8384,40.085],[-115.8376,40.0946],[-115.8346,40.0959],[-115.8321,40.0995],[-115.8289,40.1076],[-115.8294,40.1121],[-115.8305,40.1167],[-115.8374,40.1286],[-115.6972,40.1289],[-115.6046,40.1284],[-115.5295,40.1264],[-115.4561,40.1266],[-115.4441,40.1264],[-11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George T.","contributorId":15186,"corporation":false,"usgs":true,"family":"Faust","given":"George T.","affiliations":[],"preferred":false,"id":803146,"contributorType":{"id":1,"text":"Authors"},"rank":1},{"text":"Callaghan, Eugene","contributorId":79855,"corporation":false,"usgs":true,"family":"Callaghan","given":"Eugene","email":"","affiliations":[],"preferred":false,"id":803147,"contributorType":{"id":1,"text":"Authors"},"rank":2}]}}
,{"id":70215688,"text":"70215688 - 1948 - Petrography of Iwo Jima","interactions":[],"lastModifiedDate":"2020-10-27T19:07:39.383567","indexId":"70215688","displayToPublicDate":"1948-10-27T13:58:11","publicationYear":"1948","noYear":false,"publicationType":{"id":2,"text":"Article"},"publicationSubtype":{"id":10,"text":"Journal Article"},"seriesTitle":{"id":1723,"text":"GSA Bulletin","active":true,"publicationSubtype":{"id":10}},"title":"Petrography of Iwo Jima","docAbstract":"<p><span>The rocks of Iwo Jima are augite and augite-hornblende trachyandesites, distinctly more alkalic than the ordinary andesites of Japanese volcanoes or the average world andesite. They are described, and chemical analyses are listed. Fumarolic gases have altered some rocks to a mixture of opal and clay minerals and have cemented tuff with opal, calcite, zeolite, and iron oxides.</span></p>","language":"English","publisher":"Geological Society of America","doi":"10.1130/0016-7606(1948)59[1009:POIJ]2.0.CO;2","usgsCitation":"Macdonald, G.A., 1948, Petrography of Iwo Jima: GSA Bulletin, v. 59, no. 10, p. 1009-1018, https://doi.org/10.1130/0016-7606(1948)59[1009:POIJ]2.0.CO;2.","productDescription":"10 p.","startPage":"1009","endPage":"1018","costCenters":[],"links":[{"id":379828,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/thumbnails/outside_thumb.jpg"}],"country":"Japan","otherGeospatial":"Iwo Jima","geographicExtents":"{\n  \"type\": \"FeatureCollection\",\n  \"features\": [\n    {\n      \"type\": \"Feature\",\n      \"properties\": {},\n      \"geometry\": {\n        \"type\": \"Polygon\",\n        \"coordinates\": [\n          [\n            [\n              141.2134552001953,\n              24.688824063094287\n            ],\n            [\n              141.39198303222656,\n              24.688824063094287\n            ],\n            [\n              141.39198303222656,\n              24.879584553440623\n            ],\n            [\n              141.2134552001953,\n              24.879584553440623\n            ],\n            [\n              141.2134552001953,\n              24.688824063094287\n            ]\n          ]\n        ]\n      }\n    }\n  ]\n}","volume":"59","issue":"10","noUsgsAuthors":false,"publicationStatus":"PW","contributors":{"authors":[{"text":"Macdonald, G. A.","contributorId":86824,"corporation":false,"usgs":true,"family":"Macdonald","given":"G.","email":"","middleInitial":"A.","affiliations":[],"preferred":false,"id":803145,"contributorType":{"id":1,"text":"Authors"},"rank":1}]}}
,{"id":70215687,"text":"70215687 - 1948 - Report of the Research Committee on Runoff, 1947–1948","interactions":[],"lastModifiedDate":"2021-04-06T15:16:50.678326","indexId":"70215687","displayToPublicDate":"1948-10-27T13:25:04","publicationYear":"1948","noYear":false,"publicationType":{"id":2,"text":"Article"},"publicationSubtype":{"id":10,"text":"Journal Article"},"seriesTitle":{"id":1578,"text":"Eos, Transactions, American Geophysical Union","onlineIssn":"2324-9250","printIssn":"0096-394","active":true,"publicationSubtype":{"id":10}},"title":"Report of the Research Committee on Runoff, 1947–1948","docAbstract":"<p><span>Since 1946, the Committee has given consideration to terminology as related to the field of runoff. As the science of hydrology develops, there is increasing need for a more definite and uniform terminology in order to promote use of more precise language in technical literature. While it may not be possible or desirable at this time to standardize completely, it appears entirely possible to standardize many of the terms in common usage. This Committee has begun a compilation of letter symbols and terms related to runoff.</span></p>","language":"English","publisher":"American Geophysical Union","doi":"10.1029/TR029i006p00923","usgsCitation":"McDonald, C.C., 1948, Report of the Research Committee on Runoff, 1947–1948: Eos, Transactions, American Geophysical Union, v. 29, no. 6, p. 923-926, https://doi.org/10.1029/TR029i006p00923.","productDescription":"4 p.","startPage":"923","endPage":"926","costCenters":[],"links":[{"id":379825,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/thumbnails/outside_thumb.jpg"}],"volume":"29","issue":"6","noUsgsAuthors":false,"publicationDate":"2014-08-18","publicationStatus":"PW","contributors":{"authors":[{"text":"McDonald, C. C.","contributorId":69204,"corporation":false,"usgs":true,"family":"McDonald","given":"C.","email":"","middleInitial":"C.","affiliations":[],"preferred":false,"id":813566,"contributorType":{"id":1,"text":"Authors"},"rank":1}]}}
,{"id":70215685,"text":"70215685 - 1948 - Report of Committee on Ground Water, 1945–1946","interactions":[],"lastModifiedDate":"2021-03-17T14:36:25.886627","indexId":"70215685","displayToPublicDate":"1948-10-27T13:19:47","publicationYear":"1948","noYear":false,"publicationType":{"id":2,"text":"Article"},"publicationSubtype":{"id":10,"text":"Journal Article"},"seriesTitle":{"id":1578,"text":"Eos, Transactions, American Geophysical Union","onlineIssn":"2324-9250","printIssn":"0096-394","active":true,"publicationSubtype":{"id":10}},"title":"Report of Committee on Ground Water, 1945–1946","docAbstract":"<p><span>The principal activity of the Committee during the year was the arranging and presentation of a symposium on methods of estimating ground‐water supplies. The response was gratifying and resulted in the presentation of 11 interesting papers at the 1946 meeting. The report of the Subcommittee on Permeability by C. E. Jacob, Chairman, is given as Appendix A. At a meeting of the Executive Committee of the Section of Hydrology in June 1946, this Subcommittee of the Committee on Ground Water was changed to the Committee on Permeability of the Section of Hydrology, with Jacob continuing as Chairman. This will give the new Committee much greater latitude in dealing with a subject which is of concern to several of the Research Committees.</span></p>","language":"English","publisher":"American Geophysical Union","doi":"10.1029/TR029i001p00117","usgsCitation":"Lohman, S.W., 1948, Report of Committee on Ground Water, 1945–1946: Eos, Transactions, American Geophysical Union, v. 29, no. 1, p. 117-123, https://doi.org/10.1029/TR029i001p00117.","productDescription":"7 p.","startPage":"117","endPage":"123","costCenters":[],"links":[{"id":379876,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/thumbnails/outside_thumb.jpg"}],"volume":"29","issue":"1","noUsgsAuthors":false,"publicationDate":"2014-08-18","publicationStatus":"PW","contributors":{"authors":[{"text":"Lohman, S. W.","contributorId":45318,"corporation":false,"usgs":true,"family":"Lohman","given":"S.","email":"","middleInitial":"W.","affiliations":[],"preferred":false,"id":803144,"contributorType":{"id":1,"text":"Authors"},"rank":1}]}}
,{"id":70215684,"text":"70215684 - 1948 - Development of limestone reservoirs in Comal County, Texas","interactions":[],"lastModifiedDate":"2020-10-28T12:00:02.648533","indexId":"70215684","displayToPublicDate":"1948-10-27T13:13:15","publicationYear":"1948","noYear":false,"publicationType":{"id":2,"text":"Article"},"publicationSubtype":{"id":10,"text":"Journal Article"},"seriesTitle":{"id":1578,"text":"Eos, Transactions, American Geophysical Union","onlineIssn":"2324-9250","printIssn":"0096-394","active":true,"publicationSubtype":{"id":10}},"title":"Development of limestone reservoirs in Comal County, Texas","docAbstract":"<p><span>The Edwards limestone, and to a lesser extent the Comanche Peak limestone and the lower part of the Glen Rose limestone below, all of Lower Cretaceous age, form one of the most extensive ground‐water reservoirs in Texas. As a result of normal faulting, these formations are connected by underground channels to form a hydrologic unit which is partly artesian and partly unconfined. Observations in Comal County show that the development of the reservoir by solution is closely related to the geologic history, in which complex faulting and the disconformity between the Edwards and Georgetown limestones are important factors. Various phases of development are shown in different fault blocks, depending upon length of exposure at the surface. The Edwards limestone, which contains the main channels of underground drainage, is almost uniformly permeable from top to bottom, whereas the older, but more recently exposed lower part of the Glen Rose limestone is generally relatively impermeable except where exposed by mature streams.</span></p>","language":"English","publisher":"American Geophysical Union","doi":"10.1029/TR029i004p00503","usgsCitation":"George, W., 1948, Development of limestone reservoirs in Comal County, Texas: Eos, Transactions, American Geophysical Union, v. 29, no. 4, p. 503-510, https://doi.org/10.1029/TR029i004p00503.","productDescription":"8 p.","startPage":"503","endPage":"510","costCenters":[],"links":[{"id":379823,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/thumbnails/outside_thumb.jpg"}],"country":"United States","state":"Texas","county":"Comal County","geographicExtents":"{\"type\":\"FeatureCollection\",\"features\":[{\"type\":\"Feature\",\"geometry\":{\"type\":\"Polygon\",\"coordinates\":[[[-98.2986,30.0395],[-98.1102,29.9036],[-98.0389,29.8493],[-97.9996,29.7537],[-98.0895,29.6857],[-98.2045,29.6363],[-98.3124,29.5973],[-98.3149,29.6014],[-98.3191,29.6033],[-98.3279,29.6053],[-98.3295,29.6058],[-98.3305,29.6086],[-98.3341,29.6109],[-98.3383,29.6128],[-98.3419,29.6147],[-98.3445,29.6175],[-98.3439,29.623],[-98.3432,29.6303],[-98.3452,29.6345],[-98.3478,29.6381],[-98.3498,29.6423],[-98.3492,29.645],[-98.3475,29.6496],[-98.3464,29.6523],[-98.3479,29.6551],[-98.3516,29.657],[-98.3589,29.6589],[-98.361,29.6603],[-98.3625,29.6631],[-98.364,29.6645],[-98.3677,29.6659],[-98.3724,29.6656],[-98.3772,29.6638],[-98.3793,29.6643],[-98.3803,29.6657],[-98.3833,29.6721],[-98.3842,29.6786],[-98.3826,29.6822],[-98.3794,29.6849],[-98.3783,29.689],[-98.3787,29.6913],[-98.3813,29.6945],[-98.3828,29.6973],[-98.3828,29.7001],[-98.3806,29.7028],[-98.3779,29.7046],[-98.3722,29.705],[-98.3601,29.7048],[-98.3543,29.7047],[-98.3511,29.7051],[-98.3458,29.7101],[-98.3425,29.715],[-98.3419,29.7192],[-98.3424,29.7228],[-98.3449,29.7265],[-98.3527,29.7308],[-98.3559,29.7317],[-98.3606,29.7318],[-98.3638,29.7282],[-98.3676,29.7237],[-98.3734,29.7215],[-98.376,29.7215],[-98.377,29.7261],[-98.3779,29.7316],[-98.3795,29.7348],[-98.3889,29.7345],[-98.3941,29.736],[-98.3978,29.737],[-98.3988,29.7397],[-98.4014,29.7439],[-98.4045,29.7467],[-98.4081,29.7476],[-98.4134,29.7468],[-98.4182,29.7446],[-98.4203,29.7419],[-98.4219,29.7391],[-98.4226,29.7341],[-98.4216,29.73],[-98.4216,29.729],[-98.4253,29.7277],[-98.4279,29.7278],[-98.4296,29.726],[-98.4301,29.7241],[-98.4291,29.7218],[-98.4291,29.7195],[-98.4318,29.7182],[-98.4371,29.7178],[-98.4402,29.7188],[-98.4428,29.7188],[-98.4449,29.7202],[-98.4459,29.723],[-98.4458,29.7276],[-98.4452,29.7326],[-98.4462,29.734],[-98.4499,29.7345],[-98.4546,29.7327],[-98.4588,29.7337],[-98.463,29.7361],[-98.4661,29.7379],[-98.4719,29.7376],[-98.4772,29.7353],[-98.4851,29.735],[-98.5008,29.738],[-98.5086,29.7413],[-98.5122,29.7436],[-98.5143,29.7446],[-98.5196,29.7455],[-98.5238,29.7456],[-98.5254,29.7447],[-98.529,29.7452],[-98.5332,29.7485],[-98.5357,29.7526],[-98.5399,29.7541],[-98.5441,29.7527],[-98.5473,29.7528],[-98.5499,29.7547],[-98.5493,29.756],[-98.5488,29.7565],[-98.5488,29.7592],[-98.5498,29.7602],[-98.5524,29.7606],[-98.5535,29.7602],[-98.5545,29.7588],[-98.5562,29.7566],[-98.5572,29.7557],[-98.5604,29.7534],[-98.5662,29.7526],[-98.5741,29.7504],[-98.5783,29.7495],[-98.5805,29.7473],[-98.5816,29.7445],[-98.5837,29.7432],[-98.5874,29.7446],[-98.59,29.7469],[-98.5936,29.7488],[-98.5983,29.7489],[-98.6015,29.7494],[-98.6051,29.7499],[-98.6052,29.748],[-98.6047,29.7457],[-98.6026,29.7448],[-98.6016,29.7425],[-98.6048,29.7407],[-98.61,29.7399],[-98.6137,29.7395],[-98.6174,29.7409],[-98.6216,29.7423],[-98.6231,29.7428],[-98.6257,29.7437],[-98.6321,29.7429],[-98.6384,29.7416],[-98.6431,29.7403],[-98.6458,29.7403],[-98.6468,29.7426],[-98.6478,29.7477],[-98.4138,29.9442],[-98.2986,30.0395]]]},\"properties\":{\"name\":\"Comal\",\"state\":\"TX\"}}]}","volume":"29","issue":"4","noUsgsAuthors":false,"publicationDate":"2014-08-18","publicationStatus":"PW","contributors":{"authors":[{"text":"George, W.O.","contributorId":41886,"corporation":false,"usgs":true,"family":"George","given":"W.O.","email":"","affiliations":[],"preferred":false,"id":803143,"contributorType":{"id":1,"text":"Authors"},"rank":1}]}}
,{"id":70215683,"text":"70215683 - 1948 - Hydrology of limestone terrane in Schoharie County, New York","interactions":[],"lastModifiedDate":"2021-04-07T13:48:14.233831","indexId":"70215683","displayToPublicDate":"1948-10-27T13:02:34","publicationYear":"1948","noYear":false,"publicationType":{"id":2,"text":"Article"},"publicationSubtype":{"id":10,"text":"Journal Article"},"seriesTitle":{"id":1578,"text":"Eos, Transactions, American Geophysical Union","onlineIssn":"2324-9250","printIssn":"0096-394","active":true,"publicationSubtype":{"id":10}},"title":"Hydrology of limestone terrane in Schoharie County, New York","docAbstract":"<p><span>During the summer of 1946 the writer studied the ground‐water resources of Schoharie County, New York, as a part of the program of ground‐water investigation being carried on in cooperation between the United States Geological Survey and the New York State Water Power and Control Commission. Because the outcrop belt of Devonian and Upper Silurian carbonate rocks is wider in Schoharie County than in other parts of the State, the effects of solution on these formations is better displayed here than elsewhere. The conditions described below probably apply on a smaller scale to the areas to the west, where the upper formations are cut out by an unconformity, and to the east in the Helderberg area, where similar effects have been described by Goldring [see “References” at end of paper, 1935]. However, it is probable that solution in the limestones in the Hudson Valley is not comparable because of the folded condition of the rocks.</span></p>","language":"English","publisher":"American Geophysical Union","doi":"10.1029/TR029i002p00251","usgsCitation":"Berdan, J.M., 1948, Hydrology of limestone terrane in Schoharie County, New York: Eos, Transactions, American Geophysical Union, v. 29, no. 2, p. 251-253, https://doi.org/10.1029/TR029i002p00251.","productDescription":"3 p.","startPage":"251","endPage":"253","costCenters":[],"links":[{"id":379822,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/thumbnails/outside_thumb.jpg"}],"country":"United States","state":"New York","county":"Schoharie County","geographicExtents":"{\"type\":\"FeatureCollection\",\"features\":[{\"type\":\"Feature\",\"geometry\":{\"type\":\"Polygon\",\"coordinates\":[[[-74.264,42.7981],[-74.2622,42.7963],[-74.2579,42.7949],[-74.2548,42.793],[-74.2529,42.7898],[-74.2511,42.7857],[-74.2506,42.7825],[-74.2525,42.7798],[-74.2545,42.7707],[-74.2572,42.7621],[-74.261,42.7585],[-74.266,42.7572],[-74.2729,42.7573],[-74.2848,42.7569],[-74.2941,42.7566],[-74.2998,42.7552],[-74.3035,42.7535],[-74.3042,42.7521],[-74.3067,42.7485],[-74.2779,42.7196],[-74.2711,42.7195],[-74.2687,42.714],[-74.2424,42.7174],[-74.2393,42.7178],[-74.2026,42.7107],[-74.1838,42.7123],[-74.1773,42.73],[-74.1619,42.7166],[-74.168,42.6912],[-74.1684,42.674],[-74.1697,42.6672],[-74.1718,42.6595],[-74.1757,42.6499],[-74.1833,42.64],[-74.1878,42.6342],[-74.1903,42.6324],[-74.1949,42.6201],[-74.1963,42.6165],[-74.2197,42.5927],[-74.2198,42.5899],[-74.2218,42.5845],[-74.2237,42.5813],[-74.23,42.5764],[-74.2338,42.5737],[-74.2357,42.5705],[-74.2392,42.5488],[-74.2321,42.5323],[-74.2298,42.521],[-74.2263,42.5046],[-74.227,42.5014],[-74.2354,42.4837],[-74.2425,42.4688],[-74.2457,42.4648],[-74.2509,42.4516],[-74.2652,42.4177],[-74.2636,42.4063],[-74.253,42.4071],[-74.246,42.3839],[-74.246,42.3816],[-74.2472,42.3807],[-74.2497,42.3807],[-74.2547,42.3812],[-74.2591,42.3795],[-74.2666,42.3732],[-74.2748,42.3673],[-74.2804,42.3647],[-74.2861,42.3629],[-74.2954,42.363],[-74.2997,42.363],[-74.306,42.3599],[-74.3078,42.359],[-74.3141,42.3595],[-74.3227,42.3605],[-74.3314,42.3601],[-74.3389,42.3602],[-74.3426,42.3584],[-74.3469,42.3594],[-74.3513,42.3617],[-74.358,42.3676],[-74.3617,42.3699],[-74.3685,42.3704],[-74.3778,42.3701],[-74.389,42.3697],[-74.3977,42.3675],[-74.4432,42.3547],[-74.6168,42.4219],[-74.7145,42.5175],[-74.671,42.5654],[-74.652,42.5926],[-74.6317,42.6242],[-74.6382,42.6511],[-74.6501,42.6935],[-74.6621,42.7322],[-74.6681,42.7513],[-74.668,42.764],[-74.6645,42.7917],[-74.6504,42.828],[-74.5619,42.8092],[-74.4562,42.7716],[-74.3311,42.7828],[-74.2893,42.7838],[-74.264,42.7981]]]},\"properties\":{\"name\":\"Schoharie\",\"state\":\"NY\"}}]}","volume":"29","issue":"2","noUsgsAuthors":false,"publicationDate":"2014-08-18","publicationStatus":"PW","contributors":{"authors":[{"text":"Berdan, Jean Milton","contributorId":86758,"corporation":false,"usgs":true,"family":"Berdan","given":"Jean","email":"","middleInitial":"Milton","affiliations":[],"preferred":false,"id":803142,"contributorType":{"id":1,"text":"Authors"},"rank":1}]}}
,{"id":70215682,"text":"70215682 - 1948 - Report of Research Committee on Runoff, 1946–1947","interactions":[],"lastModifiedDate":"2020-10-27T17:59:55.899671","indexId":"70215682","displayToPublicDate":"1948-10-27T12:41:50","publicationYear":"1948","noYear":false,"publicationType":{"id":2,"text":"Article"},"publicationSubtype":{"id":10,"text":"Journal Article"},"seriesTitle":{"id":1578,"text":"Eos, Transactions, American Geophysical Union","onlineIssn":"2324-9250","printIssn":"0096-394","active":true,"publicationSubtype":{"id":10}},"title":"Report of Research Committee on Runoff, 1946–1947","docAbstract":"<p>The membership of the Committee has remained unchanged during the year. There has been some discussion of committee activities between individual members and in small groups. The further discussion of runoff terminology has resulted in no new developments of special note.</p><p>The following statements have been received from members of the committee concerning activities of the agencies with which they are associated.</p>","language":"English","publisher":"American Geophysical Union","doi":"10.1029/TR029i002p00263","usgsCitation":"Davenport, R.W., 1948, Report of Research Committee on Runoff, 1946–1947: Eos, Transactions, American Geophysical Union, v. 29, no. 2, p. 263-265, https://doi.org/10.1029/TR029i002p00263.","productDescription":"3 p.","startPage":"263","endPage":"265","costCenters":[],"links":[{"id":379820,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/thumbnails/outside_thumb.jpg"}],"volume":"29","issue":"2","noUsgsAuthors":false,"publicationDate":"2014-08-18","publicationStatus":"PW","contributors":{"authors":[{"text":"Davenport, R. W.","contributorId":41798,"corporation":false,"usgs":true,"family":"Davenport","given":"R.","email":"","middleInitial":"W.","affiliations":[],"preferred":false,"id":803141,"contributorType":{"id":1,"text":"Authors"},"rank":1}]}}
,{"id":70215681,"text":"70215681 - 1948 - Runoff from rain and snow","interactions":[],"lastModifiedDate":"2021-04-02T14:46:48.221141","indexId":"70215681","displayToPublicDate":"1948-10-27T12:31:09","publicationYear":"1948","noYear":false,"publicationType":{"id":2,"text":"Article"},"publicationSubtype":{"id":10,"text":"Journal Article"},"seriesTitle":{"id":1578,"text":"Eos, Transactions, American Geophysical Union","onlineIssn":"2324-9250","printIssn":"0096-394","active":true,"publicationSubtype":{"id":10}},"title":"Runoff from rain and snow","docAbstract":"<p><span>The basic principles of the idealized hydrologic cycle are reviewed with emphasis on storage and movement of water in the soil. A distinction is made between ground‐water runoff and overland runoff in terms of storage and lag, expressed as accumulated deviations from uniform flow over a period of several years. These functions are presented for the period 1920 through 1945 for three rivers in central Oregon: John Day, Deschutes, and Metolius, which exemplify minimum, moderate, and maximum effects, respectively, of storage and lag. The Metolius River is shown to have extremely small fluctuations in discharge from year to year, ascribed to a great portion of its flow being derived from ground‐water runoff; and its response to fluctuations in annual precipitation lags behind that of the John Day River by about five years. Specific techniques and measures for improving seasonal water supply forecasts are suggested.</span></p>","language":"English","publisher":"American Geophysical Union","doi":"10.1029/TR029i004p00511","usgsCitation":"Piper, A.M., 1948, Runoff from rain and snow: Eos, Transactions, American Geophysical Union, v. 29, no. 4, p. 511-524, https://doi.org/10.1029/TR029i004p00511.","productDescription":"14 p.","startPage":"511","endPage":"524","costCenters":[],"links":[{"id":379816,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/thumbnails/outside_thumb.jpg"}],"country":"United 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 \"}}]}","volume":"29","issue":"4","noUsgsAuthors":false,"publicationDate":"2014-08-18","publicationStatus":"PW","contributors":{"authors":[{"text":"Piper, A. M.","contributorId":102865,"corporation":false,"usgs":true,"family":"Piper","given":"A.","email":"","middleInitial":"M.","affiliations":[],"preferred":false,"id":803140,"contributorType":{"id":1,"text":"Authors"},"rank":1}]}}
,{"id":70215680,"text":"70215680 - 1948 - Trends in runoff in the Pacific Northwest","interactions":[],"lastModifiedDate":"2021-03-19T22:32:03.584067","indexId":"70215680","displayToPublicDate":"1948-10-27T12:12:00","publicationYear":"1948","noYear":false,"publicationType":{"id":2,"text":"Article"},"publicationSubtype":{"id":10,"text":"Journal Article"},"seriesTitle":{"id":1578,"text":"Eos, Transactions, American Geophysical Union","onlineIssn":"2324-9250","printIssn":"0096-394","active":true,"publicationSubtype":{"id":10}},"title":"Trends in runoff in the Pacific Northwest","docAbstract":"<p><span>The diminution in runoff in the Pacific Northwest, particularly the Columbia River Basin, during the past 50 years, and its hydrologic significance are discussed in this paper. An analysis of the rainfall‐runoff relations for the Basin is made in order to explain the different influence of short‐ and long‐term precipitation factors on the diminution of runoff. The indicated effects of long‐term precipitation may reflect the influence of ground‐water storage.</span></p>","language":"English","publisher":"American Geophysical Union","doi":"10.1029/TR029i003p00387","usgsCitation":"McDonald, C.C., and Langbein, W.B., 1948, Trends in runoff in the Pacific Northwest: Eos, Transactions, American Geophysical Union, v. 29, no. 3, p. 387-397, https://doi.org/10.1029/TR029i003p00387.","productDescription":"11 p.","startPage":"387","endPage":"397","costCenters":[],"links":[{"id":379814,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/thumbnails/outside_thumb.jpg"}],"country":"United States","state":"Oregon, Washington","otherGeospatial":"Pacific 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 \"}}]}","volume":"29","issue":"3","noUsgsAuthors":false,"publicationDate":"2014-08-18","publicationStatus":"PW","contributors":{"authors":[{"text":"McDonald, C. C.","contributorId":69204,"corporation":false,"usgs":true,"family":"McDonald","given":"C.","email":"","middleInitial":"C.","affiliations":[],"preferred":false,"id":803138,"contributorType":{"id":1,"text":"Authors"},"rank":1},{"text":"Langbein, W. B.","contributorId":102053,"corporation":false,"usgs":true,"family":"Langbein","given":"W.","email":"","middleInitial":"B.","affiliations":[],"preferred":false,"id":803139,"contributorType":{"id":1,"text":"Authors"},"rank":2}]}}
,{"id":70215679,"text":"70215679 - 1948 - Quality of water in the northwest","interactions":[],"lastModifiedDate":"2021-03-16T20:54:25.168523","indexId":"70215679","displayToPublicDate":"1948-10-27T11:52:33","publicationYear":"1948","noYear":false,"publicationType":{"id":2,"text":"Article"},"publicationSubtype":{"id":10,"text":"Journal Article"},"seriesTitle":{"id":1578,"text":"Eos, Transactions, American Geophysical Union","onlineIssn":"2324-9250","printIssn":"0096-394","active":true,"publicationSubtype":{"id":10}},"title":"Quality of water in the northwest","docAbstract":"<h3 class=\"article-section__header main main\">Abstract</h3><div class=\"article-section__content en main\"><p>The quality of natural waters, as judged by the dissolved mineral content, is quite varied throughout the Northwest. The concentrations of dissolved solids range from less than 50 ppm for many of the surface waters in Washington and Oregon, to several thousand ppm in the alkaline lakes of these states. On the whole, the quality of the natural waters is good but in some areas the waters have become unsatisfactory for many purposes, including irrigation, through contamination with wastes from industrial processes, which may include drainage from irrigated lands.</p></div>","language":"English","publisher":"American Geophysical Union","doi":"10.1029/TR029i003p00379","usgsCitation":"Howard, C.S., 1948, Quality of water in the northwest: Eos, Transactions, American Geophysical Union, v. 29, no. 3, p. 379-383, https://doi.org/10.1029/TR029i003p00379.","productDescription":"5 p.","startPage":"379","endPage":"383","costCenters":[],"links":[{"id":379801,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/thumbnails/outside_thumb.jpg"}],"country":"United States","state":"Oregon, Washington","otherGeospatial":"The 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 \"}}]}","volume":"29","issue":"3","noUsgsAuthors":false,"publicationDate":"2014-08-18","publicationStatus":"PW","contributors":{"authors":[{"text":"Howard, C. 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,{"id":70215677,"text":"70215677 - 1948 - Effect of water temperature on flow of a natural stream","interactions":[],"lastModifiedDate":"2020-10-27T16:42:53.600045","indexId":"70215677","displayToPublicDate":"1948-10-27T11:34:00","publicationYear":"1948","noYear":false,"publicationType":{"id":2,"text":"Article"},"publicationSubtype":{"id":10,"text":"Journal Article"},"seriesTitle":{"id":1578,"text":"Eos, Transactions, American Geophysical Union","onlineIssn":"2324-9250","printIssn":"0096-394","active":true,"publicationSubtype":{"id":10}},"title":"Effect of water temperature on flow of a natural stream","docAbstract":"<p><span>Approximately three per cent of the variation in streamflow of the Kootenai River near Copeland, Idaho, has been found to be associated with variation in water temperature. This has been determined by correlation analysis of residuals in streamflow that were not accounted for by either gage height or slope.</span></p>","language":"English","publisher":"American Geophysical Union","doi":"10.1029/TR029i002p00240","usgsCitation":"Eisenlohr, W.S., 1948, Effect of water temperature on flow of a natural stream: Eos, Transactions, American Geophysical Union, v. 29, no. 2, p. 240-242, https://doi.org/10.1029/TR029i002p00240.","productDescription":"3 p.","startPage":"240","endPage":"242","costCenters":[],"links":[{"id":379798,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/thumbnails/outside_thumb.jpg"}],"volume":"29","issue":"2","noUsgsAuthors":false,"publicationDate":"2014-08-18","publicationStatus":"PW","contributors":{"authors":[{"text":"Eisenlohr, William Stewart Jr.","contributorId":115220,"corporation":false,"usgs":false,"family":"Eisenlohr","given":"William","suffix":"Jr.","email":"","middleInitial":"Stewart","affiliations":[],"preferred":false,"id":803113,"contributorType":{"id":1,"text":"Authors"},"rank":1}]}}
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