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General discussion of the manganese situation in Panama.

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The Willow Creek mining district is a small but important lode gold mining district along the southern border of the Talkeetna Mountains in southern Alaska.
To date the district has produced about 5 percent of Alaska's lode gold output. 

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1962 - Petrology and geochemistry of selected talc-bearing ultramafic rocks and adjacent country rocks in north-central Vermont","indexId":"pp345","publicationYear":"1962","noYear":false,"title":"Petrology and geochemistry of selected talc-bearing ultramafic rocks and adjacent country rocks in north-central Vermont"},"id":1}],"supersededBy":{"id":5763,"text":"pp345 - 1962 - Petrology and geochemistry of selected talc-bearing ultramafic rocks and adjacent country rocks in north-central Vermont","indexId":"pp345","publicationYear":"1962","noYear":false,"title":"Petrology and geochemistry of selected talc-bearing ultramafic rocks and adjacent country rocks in north-central Vermont"},"lastModifiedDate":"2024-11-19T16:52:12.621595","indexId":"ofr5147","displayToPublicDate":"1994-01-01T00:00:00","publicationYear":"1951","noYear":false,"publicationType":{"id":18,"text":"Report"},"publicationSubtype":{"id":5,"text":"USGS Numbered Series"},"seriesTitle":{"id":330,"text":"Open-File 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The Geological Survey carried out a program of diamond-drilling at two localities in Vermont during the period July-September 1950. The deposits chosen for drilling were two of the more promising talc deposits associated with ultramafic rocks of several that had been mapped earlier by the Geological Survey, but could not be evaluated accurately because critical data were lacking that could be obtained only by sub-surface exploration.

The Rousseau talc prospect is in Cambridge township, Lamoille County, Vermont. Surface rights are owned by L. and N. N. Porter; mineral rights are owned by Eastern Magnesia Talc Co. Three drill holes encountered no talc; the other five penetrated from 2 to 110 feet of talc ore. The deposit lies on the west limb of the Green Mountain anticlinorium. The country rock consists of quartz-chlorite-sericite schist and chlorite-albite schist. The schistosity strikes slightly west of north and dips 20° - 40° to the west. The talc deposit is roughly lenticular, and although generally concordant in detail with the schistosity of the country rock, is slightly cross-cutting in overall relationship. The entire deposit is composed of Tit (talc-carbonate rock) and steatite, out is presumably derived from ultramafic igneous rooks which were first serpentinized. The dimensions of the lens are about 700 feet by 500 feet by 130 feet. The talc is of good quality and is suitable, either as a mine run product or as a flotation concentrate, for most industrial uses other than industrial steatite. No pencil stock was encountered.

The Barnes hill talc prospect is in Waterbury township, Washington County, Vermont. Surface rights are divided among Donald P. and Glenola Brown, John Barnes, and Eastern Magnesia Talc Co. One drill hole at Barnes hill was barren. The other six penetrated about 20 to 140 feet of talc ore. The deposit lies on the east limb of the Green Mountain anticlinorium. The country rock outside of the ultramafic rock body consists of quartz-chlorite-sericite schist, chlorite-albite schist; and chlorite amphibolite, which strike generally about N, 20° E. and dip steeply to the east. The ultramafic body is elliptical in plan, about 1,600 feet long and 360 feet wide. The vertical dimension is unknown. The original ultramafic rock has been almost completely serpentinized and is extensively altered to grit and steatite. The talc ore is somewhat irregularly distributed throughout the ultramafic body, but it is possible to delineate with considerable confidence portions of the body that consist predominantly of ore. The largest ore bodies are in the eastern and northern parts of the ultramafic body. The ore contains more or less admixed serpentine, and so is only of intermediate to fairly good color (whiteness). It is suitable for many industrial uses in which purity and high whiteness are not necessary. No pencil stock was seen.

","language":"English","publisher":"U.S. Geological Survey","doi":"10.3133/ofr5147","usgsCitation":"Chidester, A., 1951, Diamond-drill exploration of the Rousseau talc prospect, Cambridge, Vermont, and the Barnes Hill prospect, Waterbury, Vermont: U.S. Geological Survey Open-File Report 51-47, 25 p., https://doi.org/10.3133/ofr5147.","productDescription":"25 p.","costCenters":[],"links":[{"id":146806,"rank":1,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/of/1951/0047/report-thumb.jpg"},{"id":464290,"rank":2,"type":{"id":11,"text":"Document"},"url":"https://pubs.usgs.gov/of/1951/0047/report.pdf","linkFileType":{"id":1,"text":"pdf"}}],"country":"United States","state":"Vermont","city":"Cambridge, Waterbury","otherGeospatial":"Barnes Hill Talc Prospect, Rousseau Talc Prospect","geographicExtents":"{\n \"type\": \"FeatureCollection\",\n \"features\": [\n {\n \"type\": \"Feature\",\n \"properties\": {},\n \"geometry\": {\n \"coordinates\": [\n [\n [\n -72.93708688666885,\n 44.679266350635686\n ],\n [\n -72.93708688666885,\n 44.25416576861355\n ],\n [\n -72.69592514555329,\n 44.25416576861355\n ],\n [\n -72.69592514555329,\n 44.679266350635686\n ],\n [\n -72.93708688666885,\n 44.679266350635686\n ]\n ]\n ],\n \"type\": \"Polygon\"\n }\n }\n ]\n}","noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"4f4e4a9be4b07f02db65db41","contributors":{"authors":[{"text":"Chidester, A.H.","contributorId":42940,"corporation":false,"usgs":true,"family":"Chidester","given":"A.H.","email":"","affiliations":[],"preferred":false,"id":167092,"contributorType":{"id":1,"text":"Authors"},"rank":1}]}} ,{"id":43656,"text":"ofr5184 - 1951 - Geologic maps of the Leadville drainage tunnel, Colorado","interactions":[],"lastModifiedDate":"2019-04-30T15:04:43","indexId":"ofr5184","displayToPublicDate":"1994-01-01T00:00:00","publicationYear":"1951","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":"51-84","title":"Geologic maps of the Leadville drainage tunnel, Colorado","language":"English","publisher":"U.S. Geological Survey","doi":"10.3133/ofr5184","usgsCitation":"Tweto, O., 1951, Geologic maps of the Leadville drainage tunnel, Colorado: U.S. Geological Survey Open-File Report 51-84, 11 plates, https://doi.org/10.3133/ofr5184.","productDescription":"11 plates","costCenters":[],"links":[{"id":172655,"rank":0,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/of/1951/0084/report-thumb.jpg"},{"id":363396,"rank":2,"type":{"id":17,"text":"Plate"},"url":"https://pubs.usgs.gov/of/1951/0084/plate-1.pdf","linkFileType":{"id":1,"text":"pdf"}},{"id":363397,"rank":3,"type":{"id":17,"text":"Plate"},"url":"https://pubs.usgs.gov/of/1951/0084/plate-2.pdf","linkFileType":{"id":1,"text":"pdf"}},{"id":363398,"rank":4,"type":{"id":17,"text":"Plate"},"url":"https://pubs.usgs.gov/of/1951/0084/plate-3.pdf","linkFileType":{"id":1,"text":"pdf"}},{"id":363399,"rank":5,"type":{"id":17,"text":"Plate"},"url":"https://pubs.usgs.gov/of/1951/0084/plate-4.pdf","linkFileType":{"id":1,"text":"pdf"}},{"id":363400,"rank":6,"type":{"id":17,"text":"Plate"},"url":"https://pubs.usgs.gov/of/1951/0084/plate-5.pdf","linkFileType":{"id":1,"text":"pdf"}},{"id":363401,"rank":7,"type":{"id":17,"text":"Plate"},"url":"https://pubs.usgs.gov/of/1951/0084/plate-6.pdf","linkFileType":{"id":1,"text":"pdf"}},{"id":363402,"rank":8,"type":{"id":17,"text":"Plate"},"url":"https://pubs.usgs.gov/of/1951/0084/plate-7.pdf","linkFileType":{"id":1,"text":"pdf"}},{"id":363403,"rank":9,"type":{"id":17,"text":"Plate"},"url":"https://pubs.usgs.gov/of/1951/0084/plate-8.pdf","linkFileType":{"id":1,"text":"pdf"}},{"id":363404,"rank":10,"type":{"id":17,"text":"Plate"},"url":"https://pubs.usgs.gov/of/1951/0084/plate-9.pdf","linkFileType":{"id":1,"text":"pdf"}},{"id":363405,"rank":11,"type":{"id":17,"text":"Plate"},"url":"https://pubs.usgs.gov/of/1951/0084/plate-10.pdf","linkFileType":{"id":1,"text":"pdf"}},{"id":363406,"rank":12,"type":{"id":17,"text":"Plate"},"url":"https://pubs.usgs.gov/of/1951/0084/plate-11.pdf","linkFileType":{"id":1,"text":"pdf"}}],"noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"4f4e4ae0e4b07f02db688105","contributors":{"authors":[{"text":"Tweto, Ogden","contributorId":52939,"corporation":false,"usgs":true,"family":"Tweto","given":"Ogden","affiliations":[],"preferred":false,"id":228515,"contributorType":{"id":1,"text":"Authors"},"rank":1}]}} ,{"id":3814,"text":"cir131 - 1951 - Exploratory drilling in the Prairie du Chien Group of the Wisconsin zinc-lead district by the U.S. Geological Survey in 1949-1950","interactions":[],"lastModifiedDate":"2021-10-14T20:03:23.3867","indexId":"cir131","displayToPublicDate":"1994-01-01T00:00:00","publicationYear":"1951","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":"131","title":"Exploratory drilling in the Prairie du Chien Group of the Wisconsin zinc-lead district by the U.S. Geological Survey in 1949-1950","docAbstract":"

The U. S. Geological Survey in cooperation with the Wisconsin Geological and Natural History Survey explored the Prairie du Chien group in the main productive area of the Wisconsin zinc-lead district during 1949-50. Eight properties--Crow Branch diggings, Leix, Harris, Spitzbarth, Kennedy, James, Raisbeck and Vinegar Hill Roaster--were explored using both diamond and churn drills. Twenty holes were drilled that totaled 8,582 feet in depth. The objectives of the exploration were to determine if the Prairie du Chien and other formations below the principal ore-bearing strata (Galena, Decorah, and Platteville formations) of the district are favorable for ore deposits, and to determine the type of ore deposits, if present. Lean deposits of sphalerite, marcasite, and pyrite were found in the Prairie du Chien on five properties--Crow Branch, Leix, Harris, Spitzbarth, and Vinegar Hill Roaster-and also in the Franconia sandstone on the Leix property. In the drilled area the sulfides in the Prairie du Chien group occur in certain more brittle or soluble dolomite beds that contain cavities formed by brecciation or solution.

","language":"English","publisher":"U.S. Geological Survey","doi":"10.3133/cir131","usgsCitation":"Heyl, A.V., Lyons, E.J., and Agnew, A.F., 1951, Exploratory drilling in the Prairie du Chien Group of the Wisconsin zinc-lead district by the U.S. Geological Survey in 1949-1950: U.S. Geological Survey Circular 131, i, 35 p., https://doi.org/10.3133/cir131.","productDescription":"i, 35 p.","costCenters":[],"links":[{"id":390536,"rank":3,"type":{"id":36,"text":"NGMDB Index Page"},"url":"https://ngmdb.usgs.gov/Prodesc/proddesc_23891.htm"},{"id":30884,"rank":300,"type":{"id":11,"text":"Document"},"url":"https://pubs.usgs.gov/circ/1951/0131/report.pdf","linkFileType":{"id":1,"text":"pdf"}},{"id":124602,"rank":0,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/circ/1951/0131/report-thumb.jpg"}],"country":"United States","state":"Wisconsin","otherGeospatial":"Prairie du Chien Group","geographicExtents":"{\n \"type\": \"FeatureCollection\",\n \"features\": [\n {\n \"type\": \"Feature\",\n \"properties\": {},\n \"geometry\": {\n \"type\": \"Polygon\",\n \"coordinates\": [\n [\n [\n -90.5,\n 42.5\n ],\n [\n -90.161,\n 42.5\n ],\n [\n -90.161,\n 42.942\n ],\n [\n -90.5,\n 42.942\n ],\n [\n -90.5,\n 42.5\n ]\n ]\n ]\n }\n }\n ]\n}","noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"4f4e4a0ae4b07f02db5fbc00","contributors":{"authors":[{"text":"Heyl, Allen Van","contributorId":91078,"corporation":false,"usgs":true,"family":"Heyl","given":"Allen","email":"","middleInitial":"Van","affiliations":[],"preferred":false,"id":147655,"contributorType":{"id":1,"text":"Authors"},"rank":1},{"text":"Lyons, Erwin J.","contributorId":87124,"corporation":false,"usgs":true,"family":"Lyons","given":"Erwin","email":"","middleInitial":"J.","affiliations":[],"preferred":false,"id":147654,"contributorType":{"id":1,"text":"Authors"},"rank":2},{"text":"Agnew, Allen F.","contributorId":105702,"corporation":false,"usgs":true,"family":"Agnew","given":"Allen","email":"","middleInitial":"F.","affiliations":[],"preferred":false,"id":147656,"contributorType":{"id":1,"text":"Authors"},"rank":3}]}} ,{"id":4090,"text":"cir148 - 1951 - Water resources of the Atlanta metropolitan area","interactions":[],"lastModifiedDate":"2012-02-02T00:05:33","indexId":"cir148","displayToPublicDate":"1994-01-01T00:00:00","publicationYear":"1951","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":"148","title":"Water resources of the Atlanta metropolitan area","language":"ENGLISH","doi":"10.3133/cir148","usgsCitation":"Carter, R.W., and Herrick, S.M., 1951, Water resources of the Atlanta metropolitan area: U.S. Geological Survey Circular 148, iii, 19 p. :graphs, maps (2 fold. in pocket) ;27 cm., https://doi.org/10.3133/cir148.","productDescription":"iii, 19 p. :graphs, maps (2 fold. in pocket) ;27 cm.","costCenters":[],"links":[{"id":117095,"rank":0,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/circ/1951/0148/report-thumb.jpg"},{"id":31189,"rank":400,"type":{"id":17,"text":"Plate"},"url":"https://pubs.usgs.gov/circ/1951/0148/plate-1.pdf","linkFileType":{"id":1,"text":"pdf"}},{"id":31190,"rank":401,"type":{"id":17,"text":"Plate"},"url":"https://pubs.usgs.gov/circ/1951/0148/plate-2.pdf","linkFileType":{"id":1,"text":"pdf"}},{"id":31191,"rank":300,"type":{"id":11,"text":"Document"},"url":"https://pubs.usgs.gov/circ/1951/0148/report.pdf","linkFileType":{"id":1,"text":"pdf"}}],"noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"4f4e49f4e4b07f02db5f063a","contributors":{"authors":[{"text":"Carter, R. W.","contributorId":77125,"corporation":false,"usgs":true,"family":"Carter","given":"R.","email":"","middleInitial":"W.","affiliations":[],"preferred":false,"id":148172,"contributorType":{"id":1,"text":"Authors"},"rank":1},{"text":"Herrick, Stephen M.","contributorId":42199,"corporation":false,"usgs":true,"family":"Herrick","given":"Stephen","email":"","middleInitial":"M.","affiliations":[],"preferred":false,"id":148171,"contributorType":{"id":1,"text":"Authors"},"rank":2}]}} ,{"id":4089,"text":"cir100 - 1951 - Floods in Georgia, frequency and magnitude","interactions":[],"lastModifiedDate":"2016-12-02T09:39:35","indexId":"cir100","displayToPublicDate":"1994-01-01T00:00:00","publicationYear":"1951","noYear":false,"publicationType":{"id":18,"text":"Report"},"publicationSubtype":{"id":5,"text":"USGS Numbered 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\"}}]}","noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"4f4e49e5e4b07f02db5e712e","contributors":{"authors":[{"text":"Carter, Rolland William","contributorId":107257,"corporation":false,"usgs":true,"family":"Carter","given":"Rolland","email":"","middleInitial":"William","affiliations":[],"preferred":false,"id":148170,"contributorType":{"id":1,"text":"Authors"},"rank":1}]}} ,{"id":3690,"text":"cir115 - 1951 - Estimated use of water in the United States - 1950","interactions":[],"lastModifiedDate":"2017-02-21T15:49:32","indexId":"cir115","displayToPublicDate":"1994-01-01T00:00:00","publicationYear":"1951","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":"115","title":"Estimated use of water in the United States - 1950","docAbstract":"

An estimated 170,000 million gallons of water was withdrawn from the ground, lakes, or streams each day on the average during 1950 and used on the farms and in the homes, factories, and business establishments of the United States. An additional 1,100,000 million gallons per day was used to generate hydro-power. Water power is the largest user of water; however, irrigation and industry also are large users of both ground and surface water. More surface water was used for industrial purposes than for irrigation, whereas more ground water was used for irrigation than for industrial purposes (fig. 1). The total withdrawal of surface water was considerably in excess of ground-water withdrawal, as shown by figure 1. Large quantities of water were used also for purposes requiring no diversion, such as navigation, waste disposal, recreation, and support of wildlife.

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Valleys near Gallup, N. Mex., similar to many in the Southwest, were filled in Recent time with alluvium. This material is now being eroded by systems of gullies, and the walls of these gullies provide exposures by which the history of the deposition of the alluvium can be traced.

Alluvial fills near Gallup have been eroded at least twice previously within Recent time. The middle fill of the three that are recognizable contains potsherds of Pueblo II age, indicating that deposition was occurring as late as A. D. 1200.

The chronology of alluviation and degradation for valleys in the Gallup area appears to agree with that for other valleys in the Southwest which have been studied.

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No abstract available.

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