The hot spring north of Delta, Utah, is of particular interest because it has yielded commercial manganese ore; 715 tons of manganese oxide ore that averaged 20% manganese and 0.26% sulphur is recorded. The deposits occur as a thin bed and as lenses and nodules in a dome about 1,600 feet across and 15 feet high that has been formed subsequent to the dessication of Pleistocene Lake Bonneville. The alkaline hot waters, which reach temperatures of 182 degrees F. and have a total discharge of over 1,200 gallons a minute, average 3,900 parts per million in dissolved solids, with NaCl, CaSO 4 , MgCl 2 , and CaCO 3 . Five complete analyses show a manganese content of from 0 to 1.2 parts per million. Nevertheless, no appreciable manganese seems to be precipitating at present. The bed of manganese and iron oxides is scarcely more than a foot thick and is mostly covered by porous calcite. The ore is a porous aggregate of psilomelane and pyrolusite in which the vugs are lined with limonite. These minerals have been formed through the action of hot alkaline solutions over a long period; the original mineral was probably wad. The barium oxide is believed to be chemically combined with the manganese oxides. Probably all these materials have been leached from underlying rocks or deposits by hot circulating groundwaters and may not have a magmatic source.
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waterfowl","interactions":[],"lastModifiedDate":"2021-10-04T11:43:39.395569","indexId":"70224911","displayToPublicDate":"1939-03-01T06:30:06","publicationYear":"1939","noYear":false,"publicationType":{"id":24,"text":"Conference Paper"},"publicationSubtype":{"id":19,"text":"Conference Paper"},"seriesTitle":{"id":5322,"text":"Transactions of the North American Wildlife and Natural Resources Conference","printIssn":"0078-1355","active":true,"publicationSubtype":{"id":19}},"title":"Recent findings in relation to the control of botulism in waterfowl","docAbstract":"No abstract available.
","largerWorkType":{"id":4,"text":"Book"},"largerWorkTitle":"Transactions of the fourth North American Wildlife Conference","largerWorkSubtype":{"id":12,"text":"Conference publication"},"conferenceTitle":"Fourth North American Wildlife Conference","conferenceDate":"1939","conferenceLocation":"Detroit, MI","language":"English","publisher":"Wildlife Management Institute","usgsCitation":"Coburn, D.R., and Quortrup, E.R., 1939, Recent findings in relation to the control of botulism in waterfowl, in Transactions of the fourth North American Wildlife Conference, v. 4, Detroit, MI, 1939, p. 359-363.","productDescription":"5 p.","startPage":"359","endPage":"363","costCenters":[],"links":[{"id":390164,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/thumbnails/outside_thumb.jpg"}],"country":"United States","state":"Utah","otherGeospatial":"Bear River Migratory Bird Refuge","geographicExtents":"{\n \"type\": \"FeatureCollection\",\n \"features\": [\n {\n \"type\": \"Feature\",\n \"properties\": {},\n \"geometry\": {\n \"type\": \"Polygon\",\n \"coordinates\": [\n [\n [\n -112.19169616699219,\n 41.49006348843993\n ],\n [\n -112.25349426269531,\n 41.49109217223111\n ],\n [\n -112.26516723632812,\n 41.55740776889781\n ],\n [\n -112.44026184082031,\n 41.55483866309426\n ],\n [\n -112.43820190429688,\n 41.53993583569144\n ],\n [\n -112.45880126953125,\n 41.53788000371026\n ],\n [\n -112.45811462402342,\n 41.49314949080981\n ],\n [\n -112.28164672851562,\n 41.42264912910954\n ],\n [\n -112.28782653808594,\n 41.40617085161017\n ],\n [\n -112.21366882324219,\n 41.39483961102923\n ],\n [\n -112.12783813476562,\n 41.41801503608024\n ],\n [\n -112.03994750976562,\n 41.43551987469718\n ],\n [\n -112.04887390136719,\n 41.513204922708034\n ],\n [\n -112.08526611328125,\n 41.54250553376699\n ],\n [\n -112.10655212402342,\n 41.55381099217959\n ],\n [\n -112.12303161621092,\n 41.553297150595185\n ],\n [\n -112.18070983886719,\n 41.51217659012512\n ],\n [\n -112.19169616699219,\n 41.49006348843993\n ]\n ]\n ]\n }\n }\n ]\n}","volume":"4","noUsgsAuthors":false,"publicationStatus":"PW","contributors":{"authors":[{"text":"Coburn, Don R.","contributorId":267169,"corporation":false,"usgs":false,"family":"Coburn","given":"Don","email":"","middleInitial":"R.","affiliations":[],"preferred":false,"id":824586,"contributorType":{"id":1,"text":"Authors"},"rank":1},{"text":"Quortrup, E. 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All four of the bulletins thus far published relate to the geology and ground-water resources of the island of Oahu.1 Together they present the results obtained on this island in the program of ground-water investigation of the Territory that has been conducted in cooperation with the Geological Survey, of the United States Department of the Interior. Bulletin 5 which is in preparation will describe the progress made in developing the ground-water resources of Oahu since Bulletin 1 was issued. In Bulletin 2 is presented the detailed geologic map of Oahu that has resulted from this investigation. The base for this map is the new topographic map of Oahu prepared by the Topographic Branch of the Geological Survey. This bulletin also contains a guide to the geology along the main highways, which can be used advantageously in connection with the geologic map. For 18 years the writer has had the great privilege of working under the technical direction of Mr. 0. E. Meinzer, geologist in charge of the Division of Ground Water, U. S. Geological Survey. Nearly two decades ago Mr. Meinzer envisioned the great benefits that the people of Hawaii would derive from a thorough study of the groundwater resources of these islands. He also recognized that a full knowledge of these resources could be obtained only by a complete understanding of the geology of the islands and the processes which formed them. This bulletin is one of a series that has been made possible largely as a result of his broad vision. Credit is due Mr. W. 0 . Clark for the location of all the dikes shown on plate 2 in the headwaters of Kamananui Stream near the north end of the Koolau Range, and to Dr. C. K. Wentworth for about a dozen dikes north of Kaimuki. Messrs. 0. E. Meinzer, G. R. Mansfield, M. H. Carson, G. A. Macdonald, and S. H. Elbert kindly criticized the manuscript. Mr. Harry L. Taeuber designed the cover and with James Y. Nitta prepared the illustrations. Their work has greatly enriched this bulletin. The topographic maps of 15-minute quadrangles, on a scale of 1 to 20,000 (approximately 3 inches to the mile), were used in the field as a base for the geologic mapping. The data were then transferred to the new topographic map of Oahu, which is on a scale of 1 to 62,500. The resulting geologic map is reproduced as plate 2 (in pocket) of this report. Some of the outcrops are too small to be shown on this smaller map. Plate 2 of this report was listed as plate 2 in Bulletin 1, which was, however, published without the map because of the time required to prepare and engrave the topographic base and the geologic map. The geologic structure sections at the bottom of plate 2 were not described in Bulletin 1, but are discussed below.
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Series"},"seriesTitle":{"id":341,"text":"Water Supply Paper","code":"WSP","active":false,"publicationSubtype":{"id":5}},"seriesNumber":"836","chapter":"C","title":"Artesian-water levels and interference between artesian wells in the vicinity of Lehi, Utah","docAbstract":"In the vicinity of Lehi, Utah, about 25 miles south of Salt Lake City, supplies of artesian water are obtained at depths of 75 to 750 feet from beds of sand and gravel of Pleistocene age. Individual beds are probably lenticular and irregular in shape, as is characteristic of the stream and lake deposits in many parts of the Lake Bonneville Basin. The artesian supplies are obtained from aquifers or groups of aquifers that are more thoroughly separated by impermeable materials than the artesian aquifers of some other ground-water areas in Utah. Most of the wells are between 130 and 200 feet deep. The artesian area in the vicinity of Lehi is only a small part of a ground-water unit that probably includes most of Utah Lake Valley.
The ground-water reservoir in Utah Lake Valley was seriously depleted after the years of subnormal precipitation that culminated in the drought of 1934. However, in the vicinity of Lehi the static levels in 1934 were about the same as during 1904, a year which marked the culmination of a previous drought period. The water levels in the summer of 1935 were about the same as in 1934, indicating that the recharge to the ground-water reservoir was again sufficient to balance the discharge; and during the following year there was a marked rise of the water level in all wells, commonly 5 to 10 feet in amount. The static levels in the vicinity of Lehi fluctuate each year through a range of as much as 15 feet and are ordinarily highest during March or April and lowest during August or September. This fluctuation is due in part to the closing of flowing irrigation wells during the winter.
A series of tests was made to determine the extent of interference between artesian wells. Among the wells that are between 130 and 200 feet deep, the operation of certain wells was found to cause a change in the static level in wells as much as 1 1/5 miles distant. The operation of these shallower wells, however, had no apparent effect upon the static level in the wells more than about 200 feet deep nor did the operation of these deeper wells appear to affect the static level in the shallow wells. The deep and shallow aquifers thus appear to be separated by fairly continuous beds of impermeable material.
","language":"English","publisher":"U.S. Government Printing Office","publisherLocation":"Washington, D.C.","doi":"10.3133/wsp836C","usgsCitation":"Taylor, G., and Thomas, H.E., 1939, Artesian-water levels and interference between artesian wells in the vicinity of Lehi, Utah: U.S. Geological Survey Water Supply Paper 836, iii, p. 107-156, https://doi.org/10.3133/wsp836C.","productDescription":"iii, p. 107-156","costCenters":[{"id":610,"text":"Utah Water Science Center","active":true,"usgs":true}],"links":[{"id":426329,"rank":2,"type":{"id":11,"text":"Document"},"url":"https://pubs.usgs.gov/wsp/0836c/report.pdf","linkFileType":{"id":1,"text":"pdf"}},{"id":424659,"rank":1,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/wsp/0836c/report-thumb.jpg"}],"country":"United States","state":"Utah","city":"Lehi","geographicExtents":"{\n \"type\": \"FeatureCollection\",\n \"features\": [\n {\n \"type\": \"Feature\",\n \"properties\": {},\n \"geometry\": {\n \"coordinates\": [\n [\n [\n -111.91556814972844,\n 40.47199314973861\n ],\n [\n -111.91556814972844,\n 40.3565858491277\n ],\n [\n -111.79650310365341,\n 40.3565858491277\n ],\n [\n -111.79650310365341,\n 40.47199314973861\n ],\n [\n -111.91556814972844,\n 40.47199314973861\n ]\n ]\n ],\n \"type\": \"Polygon\"\n }\n }\n ]\n}","noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"4f4e4abbe4b07f02db672c63","contributors":{"authors":[{"text":"Taylor, G.H.","contributorId":85158,"corporation":false,"usgs":true,"family":"Taylor","given":"G.H.","email":"","affiliations":[],"preferred":false,"id":145803,"contributorType":{"id":1,"text":"Authors"},"rank":1},{"text":"Thomas, H. E.","contributorId":12829,"corporation":false,"usgs":true,"family":"Thomas","given":"H.","email":"","middleInitial":"E.","affiliations":[],"preferred":false,"id":145802,"contributorType":{"id":1,"text":"Authors"},"rank":2}]}} ,{"id":70164438,"text":"70164438 - 1939 - The age, growth, and feeding habits of the whitefish Coregonus clupeaformis (Mitchell), of Lake Champlain","interactions":[],"lastModifiedDate":"2016-02-04T09:59:11","indexId":"70164438","displayToPublicDate":"1939-01-01T00:00:00","publicationYear":"1939","noYear":false,"publicationType":{"id":2,"text":"Article"},"publicationSubtype":{"id":10,"text":"Journal Article"},"seriesTitle":{"id":3624,"text":"Transactions of the American Fisheries Society","active":true,"publicationSubtype":{"id":10}},"title":"The age, growth, and feeding habits of the whitefish Coregonus clupeaformis (Mitchell), of Lake Champlain","docAbstract":"This study is based on 120 whitefish collected in northern Lake Champlain (Missisquoi Bay) in 1930 and on 175 whitefish taken in southern Lake Champlain in 1931. Since the whitefish population had not been exploited commercially after 1912 in United States waters and after 1915 in Canadian waters, its study should be of interest in showing the characteristics of a population practically untouched by man. Data have been presented on length frequencies, age composition, growth, coefficient of condition, sex ratio, standard length-total length relationship, and feeding habits. The data indicated that the Missisquoi Bay population was disturbed (probably by the early fall seining of 1930) before our samples were taken so that the original length distributions no longer existed. The southern Lake Champlain material, however, showed a consistency which indicated that the population had not been exploited to any extensive degree, if at all. When the northern population was compared with the southern the former was found to differ from the latter in the following respects, which differences pointed to some disturbance of the northern stock in the lake
\n| 1. | \n\n By possession of lower modes and smaller grand averages of length. \n | \n
| 2. | \n\n By absence of very old individuals. \n | \n
| 3. | \n\n By absence of a series of equally abundant age groups or, in other words, by the presence of a decided dominance of one or two age groups. \n | \n
| 4. | \n\n By a radical disagreement between the sexes in their age-frequency distribution. \n | \n
| 5. | \n\n By a disagreement between the sexes with respect to maximum lengths attained. \n | \n
All of the differences between the two collections could, however, not be attributed to exploitation. The following characteristics indicated the presence of two distinct populations in the lake
\n| 1. | \n\n Presence of a spawning ground at each end of the lake. \n | \n
| 2. | \n\n Differences in calculated lengths and increments of length (growth rates). \n | \n
| 3. | \n\n Differences in the actual lengths and weights of corresponding age groups at capture. \n | \n
| 4. | \n\n Differences in the coefficient of condition and the length-weight relationship. \n | \n
The discovery of the presence of apparently two separate populations of whitefish in Lake Champlain was wholly unexpected by us.
","language":"English","publisher":"Taylor & Francis","doi":"10.1577/1548-8659(1938)68[152:TAGAFH]2.0.CO;2","usgsCitation":"Van Oosten, J., and Deason, H.J., 1939, The age, growth, and feeding habits of the whitefish Coregonus clupeaformis (Mitchell), of Lake Champlain: Transactions of the American Fisheries Society, v. 68, no. 1, p. 152-162, https://doi.org/10.1577/1548-8659(1938)68[152:TAGAFH]2.0.CO;2.","productDescription":"11 p.","startPage":"152","endPage":"162","onlineOnly":"N","additionalOnlineFiles":"N","costCenters":[{"id":324,"text":"Great Lakes Science Center","active":true,"usgs":true}],"links":[{"id":316578,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/thumbnails/outside_thumb.jpg"}],"volume":"68","issue":"1","noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"56b48468e4b0cc79998053ab","contributors":{"authors":[{"text":"Van Oosten, John","contributorId":23479,"corporation":false,"usgs":true,"family":"Van Oosten","given":"John","email":"","affiliations":[],"preferred":false,"id":597352,"contributorType":{"id":1,"text":"Authors"},"rank":1},{"text":"Deason, Hilary J.","contributorId":66628,"corporation":false,"usgs":true,"family":"Deason","given":"Hilary","email":"","middleInitial":"J.","affiliations":[],"preferred":false,"id":597353,"contributorType":{"id":1,"text":"Authors"},"rank":2}]}} ,{"id":70180151,"text":"70180151 - 1938 - Report of cooperative stream measurements, U.S. Geological Survey: A part of chapter 9 in Twenty-first biennial report of the State Engineer to the governor of Utah: 1936-1938","interactions":[],"lastModifiedDate":"2017-01-24T16:00:54","indexId":"70180151","displayToPublicDate":"2017-01-01T00:00:00","publicationYear":"1938","noYear":false,"publicationType":{"id":18,"text":"Report"},"publicationSubtype":{"id":2,"text":"State or Local Government Series"},"seriesTitle":{"id":5276,"text":"Utah State Engineer Biennial Report","active":false,"publicationSubtype":{"id":2}},"seriesNumber":"21","chapter":"9","title":"Report of cooperative stream measurements, U.S. Geological Survey: A part of chapter 9 in Twenty-first biennial report of the State Engineer to the governor of Utah: 1936-1938","docAbstract":"Investigations for the surface-water resources of the State have been continued during the biennium under the standard form of co-operative agreement between the U.S. Geological Survey and the State of Utah through their respective agents. The nature, extent, and value of these co-operative investigations are discussed in the State Engineer’s Twentieth Biennial Report (pp. 51-58, incl.).
","largerWorkType":{"id":18,"text":"Report"},"largerWorkTitle":"Twenty-first biennial report of the State Engineer to the governor of Utah: 1936-1938","largerWorkSubtype":{"id":2,"text":"State or Local Government Series"},"language":"English","usgsCitation":"Purton, A., 1938, Report of cooperative stream measurements, U.S. Geological Survey: A part of chapter 9 in Twenty-first biennial report of the State Engineer to the governor of Utah: 1936-1938: Utah State Engineer Biennial Report 21, 4 p.","productDescription":"4 p.","startPage":"104","endPage":"107","numberOfPages":"4","costCenters":[{"id":610,"text":"Utah Water Science Center","active":true,"usgs":true}],"links":[{"id":333866,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/thumbnails/outside_thumb.jpg"},{"id":333862,"rank":1,"type":{"id":15,"text":"Index Page"},"url":"https://www.waterrights.utah.gov/cgi-bin/libview.exe?Modinfo=Viewpub&LIBNUM=50-1-366","text":"Full Text of Biennial Report"}],"country":"United States","state":"Utah","noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"5888770de4b05ccb964bab67","contributors":{"authors":[{"text":"Purton, A.B.","contributorId":18338,"corporation":false,"usgs":true,"family":"Purton","given":"A.B.","email":"","affiliations":[],"preferred":false,"id":660520,"contributorType":{"id":1,"text":"Authors"},"rank":1}]}} ,{"id":70179613,"text":"70179613 - 1938 - Investigations conducted by the U.S. Geological Survey: A part of Chapter 5 in Twenty-first biennial report of the State Engineer to the governor of Utah: 1936-1938","interactions":[],"lastModifiedDate":"2017-01-24T15:37:15","indexId":"70179613","displayToPublicDate":"2016-12-01T00:00:00","publicationYear":"1938","noYear":false,"publicationType":{"id":18,"text":"Report"},"publicationSubtype":{"id":2,"text":"State or Local Government Series"},"seriesTitle":{"id":5276,"text":"Utah State Engineer Biennial Report","active":false,"publicationSubtype":{"id":2}},"seriesNumber":"21","chapter":"5","title":"Investigations conducted by the U.S. Geological Survey: A part of Chapter 5 in Twenty-first biennial report of the State Engineer to the governor of Utah: 1936-1938","docAbstract":"A summary of past investigations in Utah and a description of the work done during the 1934-36 biennium are included in the State Engineer’s Twentieth Biennial Report (pp. 91-106). Co-operative investigation with the State Engineer, begun on July 1, 1935, has been continued during the past biennium. To provide for this work, the 1935 Utah State Legislature appropriated \\$10,000 to the State Engineer, this sum being matched by the U. S. Geological Survey during the biennium ending June 30, 1937. During its 1937 session the State Legislature appropriated \\$5000 for continuation of co-operative work in underground waters. An equal sum was provided by the U. S. Geological Survey and investigations have continued during the fiscal year ending June 30, 1938.
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