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,{"id":70210561,"text":"70210561 - 1934 - Geologic and structure contour map of the southern half of the Cedar Creek anticline, Fallon County, Montana and Bowman County, North Dakota","interactions":[],"lastModifiedDate":"2022-05-27T20:46:40.709939","indexId":"70210561","displayToPublicDate":"1934-12-31T13:04:53","publicationYear":"1934","noYear":false,"publicationType":{"id":18,"text":"Report"},"publicationSubtype":{"id":6,"text":"USGS Unnumbered Series"},"title":"Geologic and structure contour map of the southern half of the Cedar Creek anticline, Fallon County, Montana and Bowman County, North Dakota","docAbstract":"<p>No abstract available.</p>","language":"English","publisher":"U.S. Geological Survey","doi":"10.3133/70210561","usgsCitation":"Dobbin, C.E., and Larsen, R., 1934, Geologic and structure contour map of the southern half of the Cedar Creek anticline, Fallon County, Montana and Bowman County, North Dakota, 1 Plate: 30.81 x 52.75 inches, https://doi.org/10.3133/70210561.","productDescription":"1 Plate: 30.81 x 52.75 inches","costCenters":[],"links":[{"id":401335,"rank":3,"type":{"id":17,"text":"Plate"},"url":"https://pubs.usgs.gov/unnumbered/70210561/plate-1.pdf","linkFileType":{"id":1,"text":"pdf"}},{"id":396947,"rank":1,"type":{"id":36,"text":"NGMDB Index Page"},"url":"https://ngmdb.usgs.gov/Prodesc/proddesc_93439.htm"},{"id":396950,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/unnumbered/70210561/report-thumb.jpg"}],"country":"United States","state":"Montana, North Dakota","county":"Bowman County, Fallon County","otherGeospatial":"Cedar Creek anticline","geographicExtents":"{\n  \"type\": \"FeatureCollection\",\n  \"features\": [\n    {\n      \"type\": \"Feature\",\n      \"properties\": {},\n      \"geometry\": {\n        \"type\": \"Polygon\",\n        \"coordinates\": [\n          [\n            [\n              -104.9061,\n              45.8819\n            ],\n            [\n              -102.995,\n              45.8819\n            ],\n            [\n              -102.995,\n              46.685\n            ],\n            [\n              -104.9061,\n              46.685\n            ],\n            [\n              -104.9061,\n              45.8819\n            ]\n          ]\n        ]\n      }\n    }\n  ]\n}","noUsgsAuthors":false,"publicationStatus":"PW","contributors":{"authors":[{"text":"Dobbin, C. E.","contributorId":115816,"corporation":false,"usgs":true,"family":"Dobbin","given":"C.","email":"","middleInitial":"E.","affiliations":[],"preferred":false,"id":837676,"contributorType":{"id":1,"text":"Authors"},"rank":1},{"text":"Larsen, R. M.","contributorId":94394,"corporation":false,"usgs":true,"family":"Larsen","given":"R. M.","affiliations":[],"preferred":false,"id":837677,"contributorType":{"id":1,"text":"Authors"},"rank":2}]}}
,{"id":70221659,"text":"70221659 - 1934 - Progressive regional metamorphism of the lower kittanning coal bed of western Pennsylvania","interactions":[],"lastModifiedDate":"2021-06-27T15:27:12.34985","indexId":"70221659","displayToPublicDate":"1934-09-01T10:21:04","publicationYear":"1934","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":"Progressive regional metamorphism of the lower kittanning coal bed of western Pennsylvania","docAbstract":"<p>No abstract available.&nbsp;</p>","language":"English","publisher":"Society of Economic Geologists","doi":"10.2113/gsecongeo.29.6.511","usgsCitation":"Stadnichenko, T., 1934, Progressive regional metamorphism of the lower kittanning coal bed of western Pennsylvania: Economic Geology, v. 29, no. 6, p. 511-543, https://doi.org/10.2113/gsecongeo.29.6.511.","productDescription":"33 p.","startPage":"511","endPage":"543","costCenters":[],"links":[{"id":386781,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/thumbnails/outside_thumb.jpg"}],"country":"United  States","state":"Pennsylvania","otherGeospatial":"western Pennsylvania","geographicExtents":"{\n  \"type\": \"FeatureCollection\",\n  \"features\": [\n    {\n      \"type\": \"Feature\",\n      \"properties\": {},\n      \"geometry\": {\n        \"type\": \"Polygon\",\n        \"coordinates\": [\n          [\n            [\n              -80.44189453125,\n              39.740986355883564\n            ],\n            [\n              -77.2119140625,\n              39.740986355883564\n            ],\n            [\n              -77.2119140625,\n              42.342305278572816\n            ],\n            [\n              -80.44189453125,\n              42.342305278572816\n            ],\n            [\n              -80.44189453125,\n              39.740986355883564\n            ]\n          ]\n        ]\n      }\n    }\n  ]\n}","volume":"29","issue":"6","noUsgsAuthors":false,"publicationDate":"1934-09-01","publicationStatus":"PW","contributors":{"authors":[{"text":"Stadnichenko, T.","contributorId":37066,"corporation":false,"usgs":true,"family":"Stadnichenko","given":"T.","affiliations":[],"preferred":false,"id":818361,"contributorType":{"id":1,"text":"Authors"},"rank":1}]}}
,{"id":70206682,"text":"70206682 - 1934 - Field evidence about the viscosity of lavas","interactions":[],"lastModifiedDate":"2024-09-24T17:52:36.60478","indexId":"70206682","displayToPublicDate":"1934-06-30T17:42:20","publicationYear":"1934","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":"Field evidence about the viscosity of lavas","docAbstract":"<p><span>There appears to be surprisingly little definite information on the viscosity of lavas. With few exceptions writers content themselves with such general and indefinite terms as “mobile”, “viscous”, or “highly viscous”. 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 \"}}]}","volume":"15","issue":"1","noUsgsAuthors":false,"publicationDate":"2014-08-18","publicationStatus":"PW","contributors":{"authors":[{"text":"Ross, Clarence S.","contributorId":7251,"corporation":false,"usgs":true,"family":"Ross","given":"Clarence S.","affiliations":[],"preferred":false,"id":775358,"contributorType":{"id":1,"text":"Authors"},"rank":1}]}}
,{"id":70206681,"text":"70206681 - 1934 - The Rôle of volatiles in the formation of Virginia titanium deposits","interactions":[],"lastModifiedDate":"2019-11-16T17:40:10","indexId":"70206681","displayToPublicDate":"1934-06-30T17:35:19","publicationYear":"1934","noYear":false,"publicationType":{"id":2,"text":"Article"},"publicationSubtype":{"id":10,"text":"Journal Article"},"seriesTitle":{"id":1578,"text":"Eos, Transactions, American Geophysical Union","onlineIssn":"2324-9250","printIssn":"0096-394","active":true,"publicationSubtype":{"id":10}},"title":"The Rôle of volatiles in the formation of Virginia titanium deposits","docAbstract":"<p><span>The feldspathic rock with which the titanium deposits of Virginia are associated appears to be an anorthosite, although the plagioclase is somewhat more sodic than in normal anorthosites. That is, this rock shows evidence of having been introduced as a mush‐like mass of crystals and intersititial magma, and of undergoing very thorough crushing during introduction. This rook was later very thoroughly altered by hydrothermal solutions which migrated through the fractures in the feldspar rook and new minerals including the titanium minerals—rutile and ilmenite—were introduced. The elements introduced into the feldspathic rock ware TiO</span><sub>2</sub><span>&nbsp;FeO, MgO, P</span><sub>2</sub><span>O</span><sub>5</sub><span>, and F. The other elements that went into the formation of new minerals were derived from the feldspar originally present. There was a distinct order in the abstraction of the introduced elements from the carrying solutions, as shown by the zonal relatione of the secondary minerals. Ferrous iron was abstracted first in the formation of the ferromagnesian silicates and ilmenite. Magnesium and titanium, in the absence of iron, traveled farther from the source of the solutions and deposited rutile and magnesian silicates. At greater distances most of the introduced elements had been abstracted from the solutions but notwithstanding this the feldspar was extensively altered, but without any marked changes between the chemical composition of the original feldspar rook and the resulting altered rook. ©1934. American Geophysical Union. All Rights Reserved.</span></p>","language":"English","publisher":"American Geophysical Union","doi":"10.1029/TR015i001p00245","issn":"00028606","usgsCitation":"Ross, C.S., 1934, The Rôle of volatiles in the formation of Virginia titanium deposits: Eos, Transactions, American Geophysical Union, v. 15, no. 1, p. 245-245, https://doi.org/10.1029/TR015i001p00245.","productDescription":"1 p. ","startPage":"245","endPage":"245","costCenters":[],"links":[{"id":369266,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/thumbnails/outside_thumb.jpg"}],"country":"United States","state":"Virginia 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,{"id":70221684,"text":"70221684 - 1934 - Relation of stream‐flow to ground‐water levels","interactions":[],"lastModifiedDate":"2021-06-28T17:37:08.351486","indexId":"70221684","displayToPublicDate":"1934-06-01T12:31:54","publicationYear":"1934","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":"Relation of stream‐flow to ground‐water levels","docAbstract":"<p><span>In recent years the&nbsp;</span>Water<span>&nbsp;Resources Branch of the United States Geological Surrey has given considerable attention to the&nbsp;</span>relation<span>&nbsp;of&nbsp;</span>ground<span>‐</span>water<span>&nbsp;to&nbsp;</span>stream<span>‐</span>flow<span>. One locality in which this&nbsp;</span>relation<span>&nbsp;is being studied is about 13 miles from Washington, near Colesvllle, Maryland, where a Kinnison float‐gage is being maintained in a well In connection with the operation of a gaging‐station on the Northwest Branch of the Anacostia River. The well is opposite the gaging‐station, on a gentle slope about one. fifth of a mile from the&nbsp;</span>stream<span>, where the land‐surface ia about 20 feet above the bed of the&nbsp;</span>stream<span>. The well is an abandoned dug well 20 feet deep and is lined with loose stone and presumably admits&nbsp;</span>water<span>&nbsp;freely. The fluctuations of the&nbsp;</span>water<span>‐</span>level<span>&nbsp;in the well are believed to afford a fairly close index of fluctuations in the&nbsp;</span>water<span>‐table at the well‐site and may be typical of the fluctuations that occur in a large part of the area drained by the Northwest Branch above the gaging‐station, consisting of about 21 square miles of gently rolling farm‐land. During the period of the observations herein considered the&nbsp;</span>water<span>‐</span>level<span>&nbsp;in the well ranged from 10 to 16 feet below the&nbsp;</span>ground<span>‐surface at the well and from 10 to 4 feet above the bed of the&nbsp;</span>stream<span>.&nbsp;</span></p>","language":"English","publisher":"American Geophysical Union","doi":"10.1029/TR015i002p00414","usgsCitation":"Harrold, L., 1934, Relation of stream‐flow to ground‐water levels: Eos, Transactions, American Geophysical Union, v. 15, no. 2, p. 414-416, https://doi.org/10.1029/TR015i002p00414.","productDescription":"3 p.","startPage":"414","endPage":"416","costCenters":[],"links":[{"id":386811,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/thumbnails/outside_thumb.jpg"}],"country":"United  States","state":"Maryland","city":"Colesville","geographicExtents":"{\n  \"type\": \"FeatureCollection\",\n  \"features\": [\n    {\n      \"type\": \"Feature\",\n      \"properties\": {},\n      \"geometry\": {\n        \"type\": \"Polygon\",\n        \"coordinates\": [\n          [\n            [\n              -77.02136993408203,\n              39.06264886527909\n            ],\n            [\n              -76.98051452636719,\n              39.06264886527909\n            ],\n            [\n              -76.98051452636719,\n              39.08397168286113\n            ],\n            [\n              -77.02136993408203,\n              39.08397168286113\n            ],\n            [\n              -77.02136993408203,\n              39.06264886527909\n            ]\n          ]\n        ]\n      }\n    }\n  ]\n}","volume":"15","issue":"2","noUsgsAuthors":false,"publicationDate":"2014-08-18","publicationStatus":"PW","contributors":{"authors":[{"text":"Harrold, L.L.","contributorId":260661,"corporation":false,"usgs":false,"family":"Harrold","given":"L.L.","email":"","affiliations":[],"preferred":false,"id":818424,"contributorType":{"id":1,"text":"Authors"},"rank":1}]}}
,{"id":70221683,"text":"70221683 - 1934 - A study of salt‐water encroachment in the Galveston Area, Texas","interactions":[],"lastModifiedDate":"2021-06-28T17:23:06.351397","indexId":"70221683","displayToPublicDate":"1934-06-01T12:18:04","publicationYear":"1934","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":"A study of salt‐water encroachment in the Galveston Area, Texas","docAbstract":"<p>A<span>&nbsp;survey of the ground‐</span>water<span>&nbsp;resources of the region&nbsp;</span>in<span>&nbsp;which Houston and&nbsp;</span>Galveston<span>&nbsp;are situated was started&nbsp;</span>in<span>&nbsp;December 1930 by the United States Geological Survey&nbsp;</span>in<span>&nbsp;cooperation with the&nbsp;</span>Texas<span>&nbsp;Board of&nbsp;</span>Water<span>&nbsp;Engineers.&nbsp;</span>In<span>&nbsp;connection with this survey&nbsp;</span>a<span>&nbsp;special&nbsp;</span>study<span>&nbsp;is being made of the geochemical relations of the ground‐waters of an&nbsp;</span>area<span>&nbsp;about 25 miles wide and 90 miles long, extending from&nbsp;</span>Galveston<span>&nbsp;northwestward through Houston. This&nbsp;</span>study<span>&nbsp;considers the influence on the ground‐waters of the age and degree of weathering of the outcrop formations, base‐exchange materials,&nbsp;</span>salt<span>‐domes, and&nbsp;</span>salt<span>‐</span>water<span>&nbsp;</span>encroachment<span>.&nbsp;</span>In<span>&nbsp;this paper, however, attention is confined to&nbsp;</span>salt<span>‐</span>water<span>&nbsp;</span>encroachment<span>&nbsp;along the line from&nbsp;</span>Galveston<span>&nbsp;to Houston (Fig. 1).</span></p>","language":"English","publisher":"American Geophysical Union","doi":"10.1029/TR015i002p00432","usgsCitation":"Turner, S., and Foster, M.D., 1934, A study of salt‐water encroachment in the Galveston Area, Texas: Eos, Transactions, American Geophysical Union, v. 15, no. 2, p. 432-435, https://doi.org/10.1029/TR015i002p00432.","productDescription":"4 p.","startPage":"432","endPage":"435","costCenters":[],"links":[{"id":386810,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/thumbnails/outside_thumb.jpg"}],"country":"United  States","state":"Texas","city":"Galveston","geographicExtents":"{\n  \"type\": \"FeatureCollection\",\n  \"features\": [\n    {\n      \"type\": \"Feature\",\n      \"properties\": {},\n      \"geometry\": {\n        \"type\": \"Polygon\",\n        \"coordinates\": [\n          [\n            [\n              -94.8175048828125,\n              29.439597566602902\n            ],\n            [\n              -95.0372314453125,\n              29.216904948184734\n            ],\n            [\n              -95.29541015625,\n              28.9913248161703\n            ],\n            [\n              -95.25146484374999,\n              28.926439238621036\n            ],\n            [\n              -94.69390869140625,\n              29.26962881522664\n            ],\n            [\n              -94.47143554687499,\n              29.470687864832556\n            ],\n            [\n              -94.50164794921875,\n              29.537619205973428\n            ],\n            [\n              -94.8175048828125,\n              29.439597566602902\n            ]\n          ]\n        ]\n      }\n    }\n  ]\n}","volume":"15","issue":"2","noUsgsAuthors":false,"publicationDate":"2014-08-18","publicationStatus":"PW","contributors":{"authors":[{"text":"Turner, Samuel F.","contributorId":23982,"corporation":false,"usgs":true,"family":"Turner","given":"Samuel F.","affiliations":[],"preferred":false,"id":818422,"contributorType":{"id":1,"text":"Authors"},"rank":1},{"text":"Foster, Margaret D.","contributorId":21141,"corporation":false,"usgs":true,"family":"Foster","given":"Margaret","email":"","middleInitial":"D.","affiliations":[],"preferred":false,"id":818423,"contributorType":{"id":1,"text":"Authors"},"rank":2}]}}
]}