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,{"id":792,"text":"wsp1161 - 1952 - Water levels and artesian pressure in observation wells in the United States, 1949, Part 6, Southwestern States and Hawaii","interactions":[{"subject":{"id":42774,"text":"ofr5110 - 1951 - Preliminary geologic maps of 11 quadrangles in north-central North Dakota (Westhope, Dokken, Mohall, Eckman, Deep River, Denbigh, Saline, Karlsruhe, Balfour, Kongsberg, and Benedict)","indexId":"ofr5110","publicationYear":"1951","noYear":false,"title":"Preliminary geologic maps of 11 quadrangles in north-central North Dakota (Westhope, Dokken, Mohall, Eckman, Deep River, Denbigh, Saline, Karlsruhe, Balfour, Kongsberg, and Benedict)"},"predicate":"SUPERSEDED_BY","object":{"id":792,"text":"wsp1161 - 1952 - Water levels and artesian pressure in observation wells in the United States, 1949, Part 6, Southwestern States and Hawaii","indexId":"wsp1161","publicationYear":"1952","noYear":false,"title":"Water levels and artesian pressure in observation wells in the United States, 1949, Part 6, Southwestern States and Hawaii"},"id":1},{"subject":{"id":52993,"text":"ofr50110 - 1950 - Water levels in observation wells in Santa Barbara County, California, in 1949","indexId":"ofr50110","publicationYear":"1950","noYear":false,"title":"Water levels in observation wells in Santa Barbara County, California, in 1949"},"predicate":"SUPERSEDED_BY","object":{"id":792,"text":"wsp1161 - 1952 - Water levels and artesian pressure in observation wells in the United States, 1949, Part 6, Southwestern States and Hawaii","indexId":"wsp1161","publicationYear":"1952","noYear":false,"title":"Water levels and artesian pressure in observation wells in the United States, 1949, Part 6, Southwestern States and Hawaii"},"id":2}],"lastModifiedDate":"2012-02-02T00:05:09","indexId":"wsp1161","displayToPublicDate":"1994-01-01T00:00:00","publicationYear":"1952","noYear":false,"publicationType":{"id":18,"text":"Report"},"publicationSubtype":{"id":5,"text":"USGS Numbered Series"},"seriesTitle":{"id":341,"text":"Water Supply Paper","code":"WSP","active":false,"publicationSubtype":{"id":5}},"seriesNumber":"1161","title":"Water levels and artesian pressure in observation wells in the United States, 1949, Part 6, Southwestern States and Hawaii","language":"ENGLISH","publisher":"U.S. Govt. Print. Off.,","doi":"10.3133/wsp1161","usgsCitation":"Water Resources Division, U.S. Geological Survey, 1952, Water levels and artesian pressure in observation wells in the United States, 1949, Part 6, Southwestern States and Hawaii: U.S. Geological Survey Water Supply Paper 1161, vi, 298 p. :ill. ;23 cm., https://doi.org/10.3133/wsp1161.","productDescription":"vi, 298 p. :ill. ;23 cm.","costCenters":[],"links":[{"id":136082,"rank":0,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/wsp/1161/report-thumb.jpg"},{"id":25359,"rank":300,"type":{"id":11,"text":"Document"},"url":"https://pubs.usgs.gov/wsp/1161/report.pdf","linkFileType":{"id":1,"text":"pdf"}}],"noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"4f4e4a08e4b07f02db5fa073","contributors":{"authors":[{"text":"Water Resources Division, U.S. Geological Survey","contributorId":128075,"corporation":true,"usgs":false,"organization":"Water Resources Division, U.S. Geological Survey","id":527724,"contributorType":{"id":1,"text":"Authors"},"rank":1}]}}
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,{"id":790,"text":"wsp1158 - 1952 - Water levels and artesian pressure in observation wells in the United States, 1949, Part 3, North-Central States","interactions":[],"lastModifiedDate":"2012-02-02T00:05:10","indexId":"wsp1158","displayToPublicDate":"1994-01-01T00:00:00","publicationYear":"1952","noYear":false,"publicationType":{"id":18,"text":"Report"},"publicationSubtype":{"id":5,"text":"USGS Numbered Series"},"seriesTitle":{"id":341,"text":"Water Supply Paper","code":"WSP","active":false,"publicationSubtype":{"id":5}},"seriesNumber":"1158","title":"Water levels and artesian pressure in observation wells in the United States, 1949, Part 3, North-Central States","language":"ENGLISH","publisher":"U.S. Govt. Print. Off.,","doi":"10.3133/wsp1158","usgsCitation":"Water Resources Division, U.S. Geological Survey, 1952, Water levels and artesian pressure in observation wells in the United States, 1949, Part 3, North-Central States: U.S. Geological Survey Water Supply Paper 1158, vi, 436 p. :ill., https://doi.org/10.3133/wsp1158.","productDescription":"vi, 436 p. :ill.","costCenters":[],"links":[{"id":25357,"rank":300,"type":{"id":11,"text":"Document"},"url":"https://pubs.usgs.gov/wsp/1158/report.pdf","linkFileType":{"id":1,"text":"pdf"}},{"id":136241,"rank":0,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/wsp/1158/report-thumb.jpg"}],"noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"4f4e4a08e4b07f02db5f9f5f","contributors":{"authors":[{"text":"Water Resources Division, U.S. Geological Survey","contributorId":128075,"corporation":true,"usgs":false,"organization":"Water Resources Division, U.S. Geological Survey","id":527722,"contributorType":{"id":1,"text":"Authors"},"rank":1}]}}
,{"id":41,"text":"wsp1137B - 1952 - Floods of 1950 in the Red River of the North and Winnipeg River basins","interactions":[],"lastModifiedDate":"2018-03-16T13:11:12","indexId":"wsp1137B","displayToPublicDate":"1994-01-01T00:00:00","publicationYear":"1952","noYear":false,"publicationType":{"id":18,"text":"Report"},"publicationSubtype":{"id":5,"text":"USGS Numbered Series"},"seriesTitle":{"id":341,"text":"Water Supply Paper","code":"WSP","active":false,"publicationSubtype":{"id":5}},"seriesNumber":"1137","chapter":"B","title":"Floods of 1950 in the Red River of the North and Winnipeg River basins","docAbstract":"<p>The floods of April-July 1950 in the Red River of the North and Winnipeg River Basins were the largest that have occurred in several decades and caused the greatest damage that the flooded area has ever sustained. Five lives were lost in the United States, owing to causes directly connected with the floods. The dual peaks--on upper river and tributaries, one in April and the other in May--of nearly the same size and\" the large lake-like body of flood-water ponded between Grand Forks and Winnipeg were notable features of the flood in the Red River of the North Basin. The flood in the Winnipeg River Basin was characterized by the unusually large volume of runoff and the lateness of cresting on the Lake of the Woods.</p><p>The floods were caused by a combination of causes: high antecedent soil moisture, high antecedent runoff, heavy snowfall, delayed breakup, and heavy precipitation during breakup. Mid-March snow-surveys, made in the area by hydrographers of the United States and Canadian services, showed that the snow pack north of Fargo, N. Dak., had an unusually high water content and a runoff potential increasing from west to east. A narrow band, extending from near Grand Forks, N. Dak., east-northeastward across the basin, had a water content of 5 inches or higher. April 15 marked the beginning of rapid melting throughout the basins; most of the snow was turned into water by the end of the first melt period on April 24. A return of winter-like conditions until May 10 brought more snow and set the stage for second flood crests.</p><p>The records of stage and discharge collected on the Red River of the North at Grand Forks, N. Dak., since 1882 show that the important 1897 flood slightly exceeded the 1950 flood in both stage and discharge. Records collected by the Geological Survey and Corps of Engineers on the Red River of the North show that the 1950 flood stages exceeded any previously known from just below the mouth of Turtle River to the international boundary. Records for streams tributary to the Red River of the North between Fargo and the Roseau River show, in general, that the 1950 flood events exceeded those of any known past floods. In the storage basins of the Winnipeg River, Lake of the Woods and Rainy Lake reached a stage comparable to that of 1916; and the Winnipeg River discharge at Slave Falls exceeded the highest previously recorded, maximum, which occurred in 1927. Records of floods on the Red River at Winnipeg show that the 1950 flood did not reach as high a stage as those of 1826, 1852, and 1861. </p><p>The total tabulated damage to Winnipeg, the largest urban center in the area reported on, was about $20,000,000 in the city, and $12,000,000 in surrounding suburbs. The fight against flooding in Greater Winnipeg began on April 21 in the area adjacent to the municipal hospitals and was considered ended with the reopening of Norwood Bridge on June 1. About 80, 000 people were evacuated from their homes in Greater Winnipeg during the flood, and plans were ready to evacuate a greater number had the water risen higher.</p><p>This report contains records of stage and discharge for the flood period at 70 stream-gaging stations, 21 records of mean daily discharge at stream-gaging stations, 11 records of stage at river-height gages, and 7 records of storage or elevation of reservoirs or lakes. A summary table shows crest stages and discharges at 129 points for the 1950 event compared with the highest known past stages and discharges. Also included is a discussion of concurrent meteorology and of past floods on main streams and tributaries.</p>","language":"English","publisher":"U.S. Government Printing Office","publisherLocation":"Washington, D.C.","doi":"10.3133/wsp1137B","usgsCitation":"Water Resources Division, U.S. Geological Survey, 1952, Floods of 1950 in the Red River of the North and Winnipeg River basins: U.S. Geological Survey Water Supply Paper 1137, Report: viii, 325 p.; 5 Plates, https://doi.org/10.3133/wsp1137B.","productDescription":"Report: viii, 325 p.; 5 Plates","costCenters":[{"id":478,"text":"North Dakota Water Science Center","active":true,"usgs":true},{"id":34685,"text":"Dakota Water Science Center","active":true,"usgs":true}],"links":[{"id":24662,"rank":300,"type":{"id":11,"text":"Document"},"url":"https://pubs.usgs.gov/wsp/1137b/report.pdf","linkFileType":{"id":1,"text":"pdf"}},{"id":24660,"rank":403,"type":{"id":17,"text":"Plate"},"url":"https://pubs.usgs.gov/wsp/1137b/plate-4.pdf","linkFileType":{"id":1,"text":"pdf"}},{"id":137368,"rank":0,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/wsp/1137b/report-thumb.jpg"},{"id":24657,"rank":400,"type":{"id":17,"text":"Plate"},"url":"https://pubs.usgs.gov/wsp/1137b/plate-1.pdf","linkFileType":{"id":1,"text":"pdf"}},{"id":24661,"rank":404,"type":{"id":17,"text":"Plate"},"url":"https://pubs.usgs.gov/wsp/1137b/plate-5.pdf","linkFileType":{"id":1,"text":"pdf"}},{"id":24658,"rank":401,"type":{"id":17,"text":"Plate"},"url":"https://pubs.usgs.gov/wsp/1137b/plate-2.pdf","linkFileType":{"id":1,"text":"pdf"}},{"id":24659,"rank":402,"type":{"id":17,"text":"Plate"},"url":"https://pubs.usgs.gov/wsp/1137b/plate-3.pdf","linkFileType":{"id":1,"text":"pdf"}}],"noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"4f4e49dae4b07f02db5e0509","contributors":{"authors":[{"text":"Water Resources Division, U.S. Geological Survey","contributorId":128075,"corporation":true,"usgs":false,"organization":"Water Resources Division, U.S. Geological Survey","id":527158,"contributorType":{"id":1,"text":"Authors"},"rank":1}]}}
,{"id":325,"text":"wsp1153 - 1952 - Surface water supply of the United States, 1949, Part XIII, Snake River basin","interactions":[],"lastModifiedDate":"2012-02-02T00:05:12","indexId":"wsp1153","displayToPublicDate":"1994-01-01T00:00:00","publicationYear":"1952","noYear":false,"publicationType":{"id":18,"text":"Report"},"publicationSubtype":{"id":5,"text":"USGS Numbered Series"},"seriesTitle":{"id":341,"text":"Water Supply Paper","code":"WSP","active":false,"publicationSubtype":{"id":5}},"seriesNumber":"1153","title":"Surface water supply of the United States, 1949, Part XIII, Snake River basin","language":"ENGLISH","publisher":"Govt. Print. Off.,","doi":"10.3133/wsp1153","usgsCitation":"Water Resources Division, U.S. Geological Survey, 1952, Surface water supply of the United States, 1949, Part XIII, Snake River basin: U.S. Geological Survey Water Supply Paper 1153, viii, 264 p. :ill. ;24 cm., https://doi.org/10.3133/wsp1153.","productDescription":"viii, 264 p. :ill. ;24 cm.","costCenters":[],"links":[{"id":137275,"rank":0,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/wsp/1153/report-thumb.jpg"},{"id":24887,"rank":300,"type":{"id":11,"text":"Document"},"url":"https://pubs.usgs.gov/wsp/1153/report.pdf","linkFileType":{"id":1,"text":"pdf"}}],"noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"4f4e4afce4b07f02db69664a","contributors":{"authors":[{"text":"Water Resources Division, U.S. Geological Survey","contributorId":128075,"corporation":true,"usgs":false,"organization":"Water Resources Division, U.S. Geological Survey","id":527307,"contributorType":{"id":1,"text":"Authors"},"rank":1}]}}
,{"id":800,"text":"wsp1167 - 1952 - Water levels and artesian pressures in observation wells in the United States, 1950, Part 3, North-Central States","interactions":[],"lastModifiedDate":"2012-02-02T00:05:09","indexId":"wsp1167","displayToPublicDate":"1994-01-01T00:00:00","publicationYear":"1952","noYear":false,"publicationType":{"id":18,"text":"Report"},"publicationSubtype":{"id":5,"text":"USGS Numbered Series"},"seriesTitle":{"id":341,"text":"Water Supply Paper","code":"WSP","active":false,"publicationSubtype":{"id":5}},"seriesNumber":"1167","title":"Water levels and artesian pressures in observation wells in the United States, 1950, Part 3, North-Central States","language":"ENGLISH","publisher":"U.S. Govt. Print. Off.,","doi":"10.3133/wsp1167","usgsCitation":"Water Resources Division, U.S. Geological Survey, 1952, Water levels and artesian pressures in observation wells in the United States, 1950, Part 3, North-Central States: U.S. Geological Survey Water Supply Paper 1167, vi, 198 p. :ill. ;23 cm., https://doi.org/10.3133/wsp1167.","productDescription":"vi, 198 p. :ill. ;23 cm.","costCenters":[],"links":[{"id":136198,"rank":0,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/wsp/1167/report-thumb.jpg"},{"id":25367,"rank":300,"type":{"id":11,"text":"Document"},"url":"https://pubs.usgs.gov/wsp/1167/report.pdf","linkFileType":{"id":1,"text":"pdf"}}],"noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"4f4e4a08e4b07f02db5f9fe6","contributors":{"authors":[{"text":"Water Resources Division, U.S. Geological Survey","contributorId":128075,"corporation":true,"usgs":false,"organization":"Water Resources Division, U.S. Geological Survey","id":527729,"contributorType":{"id":1,"text":"Authors"},"rank":1}]}}
,{"id":39243,"text":"pp243B - 1952 - Tertiary stratigraphy of South Carolina","interactions":[],"lastModifiedDate":"2017-01-11T11:25:29","indexId":"pp243B","displayToPublicDate":"1994-01-01T00:00:00","publicationYear":"1952","noYear":false,"publicationType":{"id":18,"text":"Report"},"publicationSubtype":{"id":5,"text":"USGS Numbered Series"},"seriesTitle":{"id":331,"text":"Professional Paper","code":"PP","onlineIssn":"2330-7102","printIssn":"1044-9612","active":true,"publicationSubtype":{"id":5}},"seriesNumber":"243","chapter":"B","title":"Tertiary stratigraphy of South Carolina","largerWorkType":{"id":18,"text":"Report"},"largerWorkTitle":"Shorter contributions to general geology, 1952","largerWorkSubtype":{"id":5,"text":"USGS Numbered Series"},"language":"ENGLISH","doi":"10.3133/pp243B","usgsCitation":"Cooke, C.W., and MacNeil, F.S., 1952, Tertiary stratigraphy of South Carolina: U.S. Geological Survey Professional Paper 243, p. 19-29, 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,{"id":633,"text":"wsp1181 - 1952 - Surface water supply of the United States, 1950, Part XI, Pacific slope basins in California","interactions":[],"lastModifiedDate":"2012-02-02T00:05:08","indexId":"wsp1181","displayToPublicDate":"1994-01-01T00:00:00","publicationYear":"1952","noYear":false,"publicationType":{"id":18,"text":"Report"},"publicationSubtype":{"id":5,"text":"USGS Numbered Series"},"seriesTitle":{"id":341,"text":"Water Supply Paper","code":"WSP","active":false,"publicationSubtype":{"id":5}},"seriesNumber":"1181","title":"Surface water supply of the United States, 1950, Part XI, Pacific slope basins in California","language":"ENGLISH","publisher":"U.S. Govt. Print. Off.,","doi":"10.3133/wsp1181","usgsCitation":"Water Resources Division, U.S. Geological Survey, 1952, Surface water supply of the United States, 1950, Part XI, Pacific slope basins in California: U.S. Geological Survey Water Supply Paper 1181, xi, 455 p. :ill. ;23 cm., https://doi.org/10.3133/wsp1181.","productDescription":"xi, 455 p. :ill. ;23 cm.","costCenters":[],"links":[{"id":135974,"rank":0,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/wsp/1181/report-thumb.jpg"},{"id":25196,"rank":300,"type":{"id":11,"text":"Document"},"url":"https://pubs.usgs.gov/wsp/1181/report.pdf","linkFileType":{"id":1,"text":"pdf"}}],"noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"4f4e4afce4b07f02db696680","contributors":{"authors":[{"text":"Water Resources Division, U.S. Geological Survey","contributorId":128075,"corporation":true,"usgs":false,"organization":"Water Resources Division, U.S. Geological Survey","id":527605,"contributorType":{"id":1,"text":"Authors"},"rank":1}]}}
,{"id":632,"text":"wsp1180 - 1952 - Surface water supply of the United States, 1950, Part X, The Great Basin","interactions":[],"lastModifiedDate":"2012-02-02T00:05:08","indexId":"wsp1180","displayToPublicDate":"1994-01-01T00:00:00","publicationYear":"1952","noYear":false,"publicationType":{"id":18,"text":"Report"},"publicationSubtype":{"id":5,"text":"USGS Numbered Series"},"seriesTitle":{"id":341,"text":"Water Supply Paper","code":"WSP","active":false,"publicationSubtype":{"id":5}},"seriesNumber":"1180","title":"Surface water supply of the United States, 1950, Part X, The Great Basin","language":"ENGLISH","publisher":"U.S. Govt. Print. Off.,","doi":"10.3133/wsp1180","usgsCitation":"Water Resources Division, U.S. Geological Survey, 1952, Surface water supply of the United States, 1950, Part X, The Great Basin: U.S. Geological Survey Water Supply Paper 1180, viii, 234 p. :ill. ;23 cm., https://doi.org/10.3133/wsp1180.","productDescription":"viii, 234 p. :ill. ;23 cm.","costCenters":[],"links":[{"id":135973,"rank":0,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/wsp/1180/report-thumb.jpg"},{"id":25195,"rank":300,"type":{"id":11,"text":"Document"},"url":"https://pubs.usgs.gov/wsp/1180/report.pdf","linkFileType":{"id":1,"text":"pdf"}}],"noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"4f4e4afce4b07f02db696674","contributors":{"authors":[{"text":"Water Resources Division, U.S. Geological Survey","contributorId":128075,"corporation":true,"usgs":false,"organization":"Water Resources Division, U.S. Geological Survey","id":527604,"contributorType":{"id":1,"text":"Authors"},"rank":1}]}}
,{"id":636,"text":"wsp1172 - 1952 - Surface water supply of the United States, 1950, Part II, South Atlantic slope and eastern Gulf of Mexico basins","interactions":[],"lastModifiedDate":"2012-02-02T00:05:08","indexId":"wsp1172","displayToPublicDate":"1994-01-01T00:00:00","publicationYear":"1952","noYear":false,"publicationType":{"id":18,"text":"Report"},"publicationSubtype":{"id":5,"text":"USGS Numbered Series"},"seriesTitle":{"id":341,"text":"Water Supply Paper","code":"WSP","active":false,"publicationSubtype":{"id":5}},"seriesNumber":"1172","title":"Surface water supply of the United States, 1950, Part II, South Atlantic slope and eastern Gulf of Mexico basins","language":"ENGLISH","publisher":"U.S. Govt. Print. Off.,","doi":"10.3133/wsp1172","usgsCitation":"Water Resources Division, U.S. Geological Survey, 1952, Surface water supply of the United States, 1950, Part II, South Atlantic slope and eastern Gulf of Mexico basins: U.S. Geological Survey Water Supply Paper 1172, xii, 565 p. :ill. ;23 cm., https://doi.org/10.3133/wsp1172.","productDescription":"xii, 565 p. :ill. ;23 cm.","costCenters":[],"links":[{"id":135977,"rank":0,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/wsp/1172/report-thumb.jpg"},{"id":25199,"rank":300,"type":{"id":11,"text":"Document"},"url":"https://pubs.usgs.gov/wsp/1172/report.pdf","linkFileType":{"id":1,"text":"pdf"}}],"noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"4f4e4afce4b07f02db696596","contributors":{"authors":[{"text":"Water Resources Division, U.S. Geological Survey","contributorId":128075,"corporation":true,"usgs":false,"organization":"Water Resources Division, U.S. Geological Survey","id":527608,"contributorType":{"id":1,"text":"Authors"},"rank":1}]}}
,{"id":16048,"text":"ofr52140 - 1952 - Preliminary report on the Passamaquoddy bedrock survey, July-August, 1951","interactions":[],"lastModifiedDate":"2022-03-01T19:31:59.019027","indexId":"ofr52140","displayToPublicDate":"1994-01-01T00:00:00","publicationYear":"1952","noYear":false,"publicationType":{"id":18,"text":"Report"},"publicationSubtype":{"id":5,"text":"USGS Numbered Series"},"seriesTitle":{"id":330,"text":"Open-File Report","code":"OFR","onlineIssn":"2331-1258","printIssn":"0196-1497","active":true,"publicationSubtype":{"id":5}},"seriesNumber":"52-140","title":"Preliminary report on the Passamaquoddy bedrock survey, July-August, 1951","docAbstract":"<p>In order to understand the results of the Passamaquoddy bedrock survey and the details of the method of obtaining them, it is desirable to have, in outline, a general idea of the methods and their application. In this part of the report a general account of the operation will be developed. The details will be found in subsequent parts of the report. At this point a statement of the general objective and some mention of the plans for reaching it are in order.</p><p>The purpose of the Passamaquoddy survey was to determine the submarine geology in certain areas of Passamaquoddy and Cobscook Bays--the sea-bottom topography, the bedrock topography, the thickness of sediment overlying the bedrock beneath the sea, and the type of sediment. The information is needed for the planning of major engineering structures that may be built in the area. It developed in planning the study that detailed surveys could be limited to several areas where dams may be located.</p><p>To determine bottom or bedrock topography, elevations of each were determined by sonic methods at a number of closely spaced locations (about 400 feet apart), evenly distributed on range lines 1,000 or 800 feet apart, in each of eight areas. Contour lines were then drawn to produce the desired topographic maps. Sonic soundings are necessarily referred to the existing water surface. To ascertain specific elevations in an area of large tidal variations is a complex problem. The details are discussed in the section on Vertical Control by Charles E. Knox (part 8). The basic datum is mean low water as determined by the U. S. Coast and Geodetic Survey.</p><p>Equally important is the accurate positioning horizontally of each sounding location or fix. All such positioning was by the use of the standard three point fix procedure, using sextants. A net of shore points tied to the first-order control net of the Coast and Geodetic Survey was set up for this purpose, and all positions were thus accurately located. These problems are discussed in a section on Horizontal Control by Norman Duckworth (part 7).</p><p>The general planning was done in conferences held in May 1951 at the Boston office of the Corps of Engineers, and in Eastport, Maine, after a brief reconnaissance of the area. A detailed account of the conferences is given in a memorandum by Herman J. Kropper of the New England Division, Corps of Engineers, reproduced in this report as part 4. Detailed survey procedures were developed on May 18, 1951, at a conference attended by P. J. A. Scott and Norman Duckworth of the Corps of Engineers and W. O. Smith of the Geological Survey.</p><p>In order to make the necessary geophysical interpretation of the sound records, adequate geologic control had to be established. A preliminary field <br>study of the geology was made by G. G. Parker of the Geological Survey during the period May 15-17, 1951. Subsequently Dr. T. E. Upson of the Geological Survey made the detailed geologic study required for the project. <br></p><p>Two sonar units were used for the survey. One was a low-frequency high-power sonar unit developed by the Edo Corp. to meet specifications established by the Geological Survey. It was used to collect the bulk of the bedrock and bottom data. The other, of higher frequency and lower power, was manufactured by Bludworth Marine, Inc., end was required for adequate determination of water depths in shoal areas. The Edo equipment is&nbsp; described by Dr. Charles E. Mongan, Jr., in part 6 of this report.</p>","language":"English","publisher":"U.S. Geological Survey","doi":"10.3133/ofr52140","collaboration":"Prepared in cooperation with the New England Division Corps of Engineers, U.S. Army","usgsCitation":"Smith, W.O., and Upson, J., 1952, Preliminary report on the Passamaquoddy bedrock survey, July-August, 1951: U.S. Geological Survey Open-File Report 52-140, Report: ii, 49 p.; Plates: 14.88 x 10.12 inches and 13.48 x 19.59 inches, https://doi.org/10.3133/ofr52140.","productDescription":"Report: ii, 49 p.; Plates: 14.88 x 10.12 inches and 13.48 x 19.59 inches","costCenters":[],"links":[{"id":396611,"rank":4,"type":{"id":17,"text":"Plate"},"url":"https://pubs.usgs.gov/of/1952/0140/plate-2.pdf","linkFileType":{"id":1,"text":"pdf"}},{"id":396610,"rank":3,"type":{"id":17,"text":"Plate"},"url":"https://pubs.usgs.gov/of/1952/0140/plate-1.pdf","linkFileType":{"id":1,"text":"pdf"}},{"id":396609,"rank":2,"type":{"id":11,"text":"Document"},"url":"https://pubs.usgs.gov/of/1952/0140/report.pdf","linkFileType":{"id":1,"text":"pdf"}},{"id":148479,"rank":0,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/of/1952/0140/report-thumb.jpg"}],"country":"Canada, United States","state":"Maine","city":"Eastport","otherGeospatial":"Passamaquoddy Bay","geographicExtents":"{\n  \"type\": \"FeatureCollection\",\n  \"features\": [\n    {\n      \"type\": \"Feature\",\n      \"properties\": {},\n      \"geometry\": {\n        \"type\": \"Polygon\",\n        \"coordinates\": [\n          [\n            [\n              -67.15393066406249,\n              44.85489529604183\n            ],\n            [\n              -66.82708740234375,\n              44.85489529604183\n            ],\n            [\n              -66.82708740234375,\n              45.17622870105657\n            ],\n            [\n              -67.15393066406249,\n              45.17622870105657\n            ],\n            [\n              -67.15393066406249,\n              44.85489529604183\n            ]\n          ]\n        ]\n      }\n    }\n  ]\n}","noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"4f4e4aafe4b07f02db66c9be","contributors":{"authors":[{"text":"Smith, William Ogden","contributorId":20337,"corporation":false,"usgs":true,"family":"Smith","given":"William","email":"","middleInitial":"Ogden","affiliations":[],"preferred":false,"id":172145,"contributorType":{"id":1,"text":"Authors"},"rank":1},{"text":"Upson, J. E.","contributorId":49342,"corporation":false,"usgs":true,"family":"Upson","given":"J. E.","affiliations":[],"preferred":false,"id":172146,"contributorType":{"id":1,"text":"Authors"},"rank":2}]}}
,{"id":3366,"text":"cir129 - 1952 - Hydrologic reconnaissance of the Green River in Utah and Colorado","interactions":[{"subject":{"id":52980,"text":"ofr5099 - 1950 - Hydrologic reconnaissance of the Green River in Utah and Colorado","indexId":"ofr5099","publicationYear":"1950","noYear":false,"title":"Hydrologic reconnaissance of the Green River in Utah and Colorado"},"predicate":"SUPERSEDED_BY","object":{"id":3366,"text":"cir129 - 1952 - Hydrologic reconnaissance of the Green River in Utah and Colorado","indexId":"cir129","publicationYear":"1952","noYear":false,"title":"Hydrologic reconnaissance of the Green River in Utah and Colorado"},"id":1}],"lastModifiedDate":"2017-02-21T15:52:17","indexId":"cir129","displayToPublicDate":"1994-01-01T00:00:00","publicationYear":"1952","noYear":false,"publicationType":{"id":18,"text":"Report"},"publicationSubtype":{"id":5,"text":"USGS Numbered Series"},"seriesTitle":{"id":307,"text":"Circular","code":"CIR","onlineIssn":"2330-5703","printIssn":"1067-084X","active":true,"publicationSubtype":{"id":5}},"seriesNumber":"129","title":"Hydrologic reconnaissance of the Green River in Utah and Colorado","docAbstract":"<p>The Green River, rising in Wyoming and draining high mountains in that state, northeast Utah and northwest Colorado, is a major tributary of the Colorado River. In the late summer, after the snow has melted from these mountains, the flow in the Green River reaches its minimum for the year. At that time a large proportion of the water in the river is returned to the atmosphere by evaporation and transpiration.</p><p>During a 21-day period in September 1948, when the flow was least for the year, the average flow of the river as it entered Utah from Wyoming was 515 cfs. In the 437 miles of its course through Utah and Colorado evapotranspiration losses averaged 430 cfs. The average discharge of the Green River into the Colorado was about 975 cfs. Contributions to the river in Utah and Colorado totalled 890 cfsi including 560 from tributaries. The calculated ground-water inflow was about 330 cfs, of which about 75 percent was contributed within the Uinta Basin. Verv little ground water was contributed to the river in the lower 180 miles of its course, where the river flows through canyon lands of the Colorado Plateaus.</p><p>These estimates are based upon information collected during a boat reconnaissance in September 1948, and upon data available from stream-gaging stations along the Green River and many of its tributaries. From these data an accounting was made of the water--as to both quantity and quality--in several segments of the river. For each segment determinations were made of the surface outflow, loss by evapotranspiration, and surface- and ground-water inflow. During the reconnaissance information was also obtained as to the relation of stream flow to regional geology and ground-water hydrology.</p><p>No detailed hydrologic studies have yet been made within the drainage basin of the Green River. On the basis of this recomiaissance, detailed studies in the Uinta Basin, Browns Park, and Echo Park areas are recommended as highly desirable, because of the possible relations of ground-water hydrology to river-basin development projects. Similar reconnaissance can be of value in delineating the areas where detailed hydrologic studies would be most fruitful throughout the upper Colorado River basin.</p>","language":"English","publisher":"U.S. Geological Survey","publisherLocation":"Washington, D.C.","doi":"10.3133/cir129","usgsCitation":"Thomas, H.E., 1952, Hydrologic reconnaissance of the Green River in Utah and Colorado: U.S. Geological Survey Circular 129, Report: iv, 32 p.; 1 Plate: 13.88 x 13.42 inches, https://doi.org/10.3133/cir129.","productDescription":"Report: iv, 32 p.; 1 Plate: 13.88 x 13.42 inches","costCenters":[{"id":610,"text":"Utah Water Science Center","active":true,"usgs":true}],"links":[{"id":30376,"rank":400,"type":{"id":17,"text":"Plate"},"url":"https://pubs.usgs.gov/circ/0129/plate-1.pdf","linkFileType":{"id":1,"text":"pdf"}},{"id":138602,"rank":0,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/circ/0129/report-thumb.jpg"},{"id":271087,"type":{"id":11,"text":"Document"},"url":"https://pubs.usgs.gov/circ/0129/report.pdf"}],"country":"United States","state":"Colorado, Utah","otherGeospatial":"Green River","geographicExtents":"{ \"type\": \"FeatureCollection\", \"features\": [ { \"type\": \"Feature\", \"properties\": {}, \"geometry\": { \"type\": \"Polygon\", \"coordinates\": [ [ [ -0.01638888888888889,8.333333333333334E-4 ], [ -0.01638888888888889,0.0011111111111111111 ], [ -0.016666666666666666,0.0011111111111111111 ], [ -0.016666666666666666,8.333333333333334E-4 ], [ -0.01638888888888889,8.333333333333334E-4 ] ] ] } } ] }","noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"4f4e4a18e4b07f02db605548","contributors":{"authors":[{"text":"Thomas, H. E.","contributorId":12829,"corporation":false,"usgs":true,"family":"Thomas","given":"H.","email":"","middleInitial":"E.","affiliations":[],"preferred":false,"id":146729,"contributorType":{"id":1,"text":"Authors"},"rank":1}]}}
,{"id":3415,"text":"cir181 - 1952 - Electrical resistivity studies of subsurface conditions near Antigo, Wisconsin","interactions":[],"lastModifiedDate":"2016-11-07T10:01:06","indexId":"cir181","displayToPublicDate":"1994-01-01T00:00:00","publicationYear":"1952","noYear":false,"publicationType":{"id":18,"text":"Report"},"publicationSubtype":{"id":5,"text":"USGS Numbered Series"},"seriesTitle":{"id":307,"text":"Circular","code":"CIR","onlineIssn":"2330-5703","printIssn":"1067-084X","active":true,"publicationSubtype":{"id":5}},"seriesNumber":"181","title":"Electrical resistivity studies of subsurface conditions near Antigo, Wisconsin","docAbstract":"<p>Resistivity measurements are reported for the glaciated area near Antigo, Wis., to locate buried sand and gravel deposits in the glacial drift, which might be developed as aquifers, and to determine depths to the pre-Cambrian bedrock. The results of the resistivity study are presented both as cross sections and as contour maps. The apparent resistivity curves, their interpretation in terms of the thickness and character of the geological materials, as well logs of the area are given. On the basis of the study a number of sites were selected that would be suitable for drilling water-supply wells, no drilling has been done on the sites selected.</p>","language":"English","publisher":"U.S. Geological Survey","publisherLocation":"Washington, D.C.","doi":"10.3133/cir181","usgsCitation":"Spicer, H., 1952, Electrical resistivity studies of subsurface conditions near Antigo, Wisconsin: U.S. Geological Survey Circular 181, 19 p., https://doi.org/10.3133/cir181.","productDescription":"19 p.","numberOfPages":"25","costCenters":[],"links":[{"id":139427,"rank":0,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/thumbnails/usgs_thumb.jpg"},{"id":330789,"rank":2,"type":{"id":11,"text":"Document"},"url":"https://pubs.usgs.gov/circ/0181/report.pdf","linkFileType":{"id":1,"text":"pdf"}}],"country":"United States","state":"Wisconsin","city":"Antigo","geographicExtents":"{\n  \"type\": \"FeatureCollection\",\n  \"features\": [\n    {\n      \"type\": \"Feature\",\n      \"properties\": {},\n      \"geometry\": {\n        \"type\": \"Polygon\",\n        \"coordinates\": [\n          [\n            [\n              -89.27078247070312,\n              45.05412098425883\n            ],\n            [\n              -89.27078247070312,\n              45.30676845797069\n            ],\n            [\n              -89.01397705078125,\n              45.30676845797069\n            ],\n            [\n              -89.01397705078125,\n              45.05412098425883\n            ],\n            [\n              -89.27078247070312,\n              45.05412098425883\n            ]\n          ]\n        ]\n      }\n    }\n  ]\n}","noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"4f4e4a1be4b07f02db606eaa","contributors":{"authors":[{"text":"Spicer, H. Cecil","contributorId":16000,"corporation":false,"usgs":true,"family":"Spicer","given":"H. Cecil","affiliations":[],"preferred":false,"id":146856,"contributorType":{"id":1,"text":"Authors"},"rank":1}]}}
,{"id":14921,"text":"ofr53166 - 1952 - The Permian phosphorite deposits of western United States","interactions":[],"lastModifiedDate":"2025-08-08T17:09:17.21084","indexId":"ofr53166","displayToPublicDate":"1994-01-01T00:00:00","publicationYear":"1952","noYear":false,"publicationType":{"id":18,"text":"Report"},"publicationSubtype":{"id":5,"text":"USGS Numbered Series"},"seriesTitle":{"id":330,"text":"Open-File Report","code":"OFR","onlineIssn":"2331-1258","printIssn":"0196-1497","active":true,"publicationSubtype":{"id":5}},"seriesNumber":"53-166","title":"The Permian phosphorite deposits of western United States","docAbstract":"<p>The Permian marine phosphorite deposits of the western United States were laid down in the Phosphoria formation and its partial stratigraphic equivalents over an area of about 135,000 square miles in Montana, Idaho, Wyoming, Utah, and Nevada. The deposits in the eastern part of the field lie on the western margin of the structurally simple North American craton. The rocks there consist of a few thin, locally glauconitic, nodular phosphorites, generally containing less than 30 percent P<sub>2</sub>0<sub>5</sub>, interbedded with nodular limestones, calcareous mudstones, and sandstones. Eastward these marine beds tongue out into continental redbeds. The deposits in the western part of the field are a part of the complexly folded Cordilleran miogeosyncline. The facies there are of a deeper-water type and include thick phosphorite layers containing as much as 35 percent P<sub>2</sub>0<sub>5&nbsp; </sub><span id=\"_mce_caret\" data-mce-bogus=\"1\" data-mce-type=\"format-caret\">b</span>lack phosphatic mudstones, limestones, and well-bedded black cherts.</p><p>The phosphorite deposits are composed chiefly of colloform carbonate-fluorapatite, quartz, and clay. In addition to phosphorus, they contain several minor elements that are of potential economic interest. The most important of these are fluorine, vanadium, chromium, nickel, rare earths, zinc, and uranium.</p>","language":"English","publisher":"U.S. Geological Survey","doi":"10.3133/ofr53166","usgsCitation":"McKelvey, V., Swanson, R.W., and Sheldon, R.P., 1952, The Permian phosphorite deposits of western United States: U.S. Geological Survey Open-File Report 53-166, 30 p., https://doi.org/10.3133/ofr53166.","productDescription":"30 p.","costCenters":[],"links":[{"id":493878,"rank":2,"type":{"id":11,"text":"Document"},"url":"https://pubs.usgs.gov/of/1953/0166/report.pdf","linkFileType":{"id":1,"text":"pdf"}},{"id":146276,"rank":1,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/of/1953/0166/report-thumb.jpg"}],"country":"United States","geographicExtents":"{\n  \"type\": \"FeatureCollection\",\n  \"features\": [\n    {\n      \"type\": \"Feature\",\n      \"properties\": {},\n      \"geometry\": {\n        \"type\": \"Polygon\",\n        \"coordinates\": [\n          [\n   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,{"id":72209,"text":"tem476 - 1952 - Progress report on uranium in natural waters","interactions":[],"lastModifiedDate":"2012-02-02T00:14:00","indexId":"tem476","displayToPublicDate":"1994-01-01T00:00:00","publicationYear":"1952","noYear":false,"publicationType":{"id":18,"text":"Report"},"publicationSubtype":{"id":5,"text":"USGS Numbered Series"},"seriesTitle":{"id":338,"text":"Trace Elements Memorandum","code":"TEM","active":false,"publicationSubtype":{"id":5}},"seriesNumber":"476","title":"Progress report on uranium in natural waters","language":"ENGLISH","doi":"10.3133/tem476","usgsCitation":"Fix, P., 1952, Progress report on uranium in natural waters: U.S. Geological Survey Trace Elements Memorandum 476, 12 p., https://doi.org/10.3133/tem476.","productDescription":"12 p.","costCenters":[],"links":[{"id":256823,"rank":300,"type":{"id":11,"text":"Document"},"url":"https://pubs.usgs.gov/tem/0476/report.pdf","size":"797","linkFileType":{"id":1,"text":"pdf"}},{"id":256824,"rank":0,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/tem/0476/report-thumb.jpg"}],"noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"4f4e4a8ae4b07f02db6515be","contributors":{"authors":[{"text":"Fix, Philip F.","contributorId":21649,"corporation":false,"usgs":true,"family":"Fix","given":"Philip F.","affiliations":[],"preferred":false,"id":285189,"contributorType":{"id":1,"text":"Authors"},"rank":1}]}}
,{"id":639,"text":"wsp1178 - 1952 - Surface water supply of the United States, 1950, Part VIII, Western Gulf of Mexico basins","interactions":[],"lastModifiedDate":"2012-02-02T00:05:08","indexId":"wsp1178","displayToPublicDate":"1994-01-01T00:00:00","publicationYear":"1952","noYear":false,"publicationType":{"id":18,"text":"Report"},"publicationSubtype":{"id":5,"text":"USGS Numbered Series"},"seriesTitle":{"id":341,"text":"Water Supply Paper","code":"WSP","active":false,"publicationSubtype":{"id":5}},"seriesNumber":"1178","title":"Surface water supply of the United States, 1950, Part VIII, Western Gulf of Mexico basins","language":"ENGLISH","publisher":"U.S. Govt. Print. Off.,","doi":"10.3133/wsp1178","usgsCitation":"Water Resources Division, U.S. Geological Survey, 1952, Surface water supply of the United States, 1950, Part VIII, Western Gulf of Mexico basins: U.S. Geological Survey Water Supply Paper 1178, ix, 395 p. ;23 cm., https://doi.org/10.3133/wsp1178.","productDescription":"ix, 395 p. ;23 cm.","costCenters":[],"links":[{"id":135980,"rank":0,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/wsp/1178/report-thumb.jpg"},{"id":25202,"rank":300,"type":{"id":11,"text":"Document"},"url":"https://pubs.usgs.gov/wsp/1178/report.pdf","linkFileType":{"id":1,"text":"pdf"}}],"noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"4f4e4afce4b07f02db696569","contributors":{"authors":[{"text":"Water Resources Division, U.S. Geological Survey","contributorId":128075,"corporation":true,"usgs":false,"organization":"Water Resources Division, U.S. Geological Survey","id":527611,"contributorType":{"id":1,"text":"Authors"},"rank":1}]}}
,{"id":625,"text":"wsp1141 - 1952 - Surface water supply of the United States, 1949, Part I, North Atlantic slope basins","interactions":[],"lastModifiedDate":"2012-02-02T00:05:08","indexId":"wsp1141","displayToPublicDate":"1994-01-01T00:00:00","publicationYear":"1952","noYear":false,"publicationType":{"id":18,"text":"Report"},"publicationSubtype":{"id":5,"text":"USGS Numbered Series"},"seriesTitle":{"id":341,"text":"Water Supply Paper","code":"WSP","active":false,"publicationSubtype":{"id":5}},"seriesNumber":"1141","title":"Surface water supply of the United States, 1949, Part I, North Atlantic slope basins","language":"ENGLISH","publisher":"U.S. Govt. Print. Off.,","doi":"10.3133/wsp1141","usgsCitation":"Water Resources Division, U.S. Geological Survey, 1952, Surface water supply of the United States, 1949, Part I, North Atlantic slope basins: U.S. Geological Survey Water Supply Paper 1141, xiv, 745 p. :ill. ;23 cm., https://doi.org/10.3133/wsp1141.","productDescription":"xiv, 745 p. :ill. ;23 cm.","costCenters":[],"links":[{"id":25188,"rank":300,"type":{"id":11,"text":"Document"},"url":"https://pubs.usgs.gov/wsp/1141/report.pdf","linkFileType":{"id":1,"text":"pdf"}},{"id":136422,"rank":0,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/wsp/1141/report-thumb.jpg"}],"noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"4f4e4afce4b07f02db69672d","contributors":{"authors":[{"text":"Water Resources Division, U.S. Geological Survey","contributorId":128075,"corporation":true,"usgs":false,"organization":"Water Resources Division, U.S. Geological Survey","id":527597,"contributorType":{"id":1,"text":"Authors"},"rank":1}]}}
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