File:Reports (1908) (14804758303).jpg

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Identifier: reports9190miss (find matches)
Title: (Reports)
Year: 1903 (1900s)
Authors: Missouri. Division of Geological Survey and Water Resources
Subjects: Geology Mines and mineral resources
Publisher: Rollo (etc.)
Contributing Library: University of Illinois Urbana-Champaign
Digitizing Sponsor: University of Illinois Urbana-Champaign

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osed crystals of galena were observed in anumber of instances. There appears to be an unusual amount of pyrite associatedwith the galena. It was observed in the disseminated ore and inthe horizontal sheets, as well as in the cavities. In some places itconstitutes as much as 25 to 30 per cent of the ore. Pyrite, how-ever, appears to predominate at horizons where decomposition hasprogressed farthest and it has been my observation that wherethe pyrite and galena individuals are of the same size the pyrite isthe more persistent of the two. In the upper level the ore is very bunchy and contains a highpercentage of pyrite. In the west drift a good bunch of ore20 x 30 x 20 was mined about 40 feet from the shaft, while somescattering ore was obtained from the south drift. COLUMBIA NO. 1 (Doe Run Lead Co.). This mine is at present flooded, not having been operated sinceit passed into the hands of the Doe Run Lead Company. The shaftwas sunk in 1899 but operations were not started until January,
Text Appearing After Image:
DOE RUN LEAD CO. 189 1900. This mine and the Columbia No. 2, have been operated some-what intermittently, having been leased at one time by The Com-mercial Lead Company. During the period of its existence theColumbia Lead Company produced from its two mines about 18,112short tons of concentrates valued at about $704,000. The collar of the shaft at Columbia Mine No. 1 is about 800.00feet above sea level while the bottom is at an elevation of 513 feetA. T. The shaft is therefore 287.00 feet deep. These measure-ments are not exact, the topographic map indicating that the col-lar of the shaft is about 810 rather than 800 feet above sea level.The underground workings are shown in Plate CXIL The shaft is entirely within the Bonneterre formation, start-ing about 35 to 45 feet below the top and bottoming about 25 to40 feet above the Lamotte sandstone. This mine is located in thevicinity of a number of large sink holes, into which the water fromthe surrounding land drains. It is not known that

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Volume
InfoField
1908
Flickr tags
InfoField
  • bookid:reports9190miss
  • bookyear:1903
  • bookdecade:1900
  • bookcentury:1900
  • bookauthor:Missouri__Division_of_Geological_Survey_and_Water_Resources
  • booksubject:Geology
  • booksubject:Mines_and_mineral_resources
  • bookpublisher:Rollo__etc__
  • bookcontributor:University_of_Illinois_Urbana_Champaign
  • booksponsor:University_of_Illinois_Urbana_Champaign
  • bookleafnumber:270
  • bookcollection:university_of_illinois_urbana-champaign
  • bookcollection:americana
Flickr posted date
InfoField
30 July 2014

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4 August 2015

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current06:00, 9 September 2015Thumbnail for version as of 06:00, 9 September 20152,619 × 1,888 (681 KB)SteinsplitterBot (talk | contribs)Bot: Image rotated by 270°
17:10, 4 August 2015Thumbnail for version as of 17:10, 4 August 20151,889 × 2,619 (684 KB) (talk | contribs)== {{int:filedesc}} == {{subst:chc}} {{information |description={{en|1=<br> '''Identifier''': reports9190miss ([https://commons.wikimedia.org/w/index.php?title=Special%3ASearch&profile=default&fulltext=Search&search=insource%3A%2Freports9190miss%2F fin...

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