File:Water resources of the Rio Grande Valley in New Mexico and their development (1907) (14585938048).jpg

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Identifier: waterresourcesof00leew (find matches)
Title: Water resources of the Rio Grande Valley in New Mexico and their development
Year: 1907 (1900s)
Authors: Lee, Willis T. (Willis Thomas), 1864-1926
Subjects: Water-supply
Publisher: Govt. Print. Off.
Contributing Library: The Library of Congress
Digitizing Sponsor: The Library of Congress

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technical requirements of cementmanufacture, and probably more suitable material may be found.The analyses of these samples, given below, must be regarded as pre-liminary, but indicate that good cement materials may be found nearthe dam site. Analysis of limestone from the northern end qfOahaUos Mountains.(C. H. stone, analyst.) Silica (SiOg) and insoluble matter.. 7.94Alumina (AI.2O3) and forric oxide (FeA) 0-80. Lime (CaO) 44. 99 Magnesia (MgO) 1. 23 Copper oxide (CuO) 0. 38 Potassa (K2O) 0. 09 Soda (Na20) 0. 28 Sulfur trioxide (SO3) 0. 30 Carbon dioxide (CO2) calculated to combine with CaO 39. 29 95. 30Moisture 0. 11 Analysis of shale from the northern end ofCahallos Mountains. Silica (SiOa) - 63. 74 Ferric oxide (Fe203) 6. 44 Alumina (AI2O,) 17. 33 Lime (CaO) 5. 51 Magnesia (MgO) 1. 86 Soda (NagO) Undet. Potassa (K2O) Undet. Sulfuric trioxide (SO3) Trace. Ignition loss (H2O, COg) , 94.88 RATIONAL ANALYSIS. Clay substance - - - 27. 20 Quaitz - - - 3. 25 P^eldspathic detritus 69. 55
Text Appearing After Image:
SAN ACACIA AND SAN FELIPE RESERVOIES. 29 SiO * The ratio t^ ^ izrVwy =--6 is well within the limits of the ratio >2.3 or <3.6. The MgO content is low, and the absence of SO3 makesthis material one of the purer clays, considered from a technicalpoint of view. Coal.—Coal has been fomid in Mescal Can3^on about 4 miles southof Elephant Butte. Where exposed at the surface the beds are onlya few inches thick, but are associated with a considerable amount ofcarbonaceous shale. The coal is in the same formation that containsvaluable deposits of coal at Carthage and other places farther north,but the prospects have not been developed. SAN ACACIA RESERVOIR. The narrow gorge at San Acacia is one of the proposed dam sites ofthe Rio Grande region. The broad Belen Valley, to the north, nar-rows abruptly at this point on account of the sheet of basalt whichhere covers the detritus. Measurements made at this point by Mr.R. H. Chapman, of the United States Geological Survey, indicate thata dam

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Author Lee, Willis T. (Willis Thomas), 1864-1926
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Flickr tags
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  • bookid:waterresourcesof00leew
  • bookyear:1907
  • bookdecade:1900
  • bookcentury:1900
  • bookauthor:Lee__Willis_T___Willis_Thomas___1864_1926
  • booksubject:Water_supply
  • bookpublisher:Govt__Print__Off_
  • bookcontributor:The_Library_of_Congress
  • booksponsor:The_Library_of_Congress
  • bookleafnumber:54
  • bookcollection:library_of_congress
  • bookcollection:americana
Flickr posted date
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29 July 2014


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07:12, 28 September 2015Thumbnail for version as of 07:12, 28 September 20151,928 × 3,472 (1.72 MB) (talk | contribs)== {{int:filedesc}} == {{information |description={{en|1=<br> '''Identifier''': waterresourcesof00leew ([https://commons.wikimedia.org/w/index.php?title=Special%3ASearch&profile=default&fulltext=Search&search=insource%3A%2Fwaterresourcesof00leew%2F fin...

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