Skip to main content

Search the Special Collections and Archives Portal

upr000013 35

Image

File
Download upr000013-035.tif (image/tiff; 25.7 MB)

Information

Digital ID

upr000013-035
    Details

    Rights

    This material is made available to facilitate private study, scholarship, or research. It may be protected by copyright, trademark, privacy, publicity rights, or other interests not owned by UNLV. Users are responsible for determining whether permissions are necessary from rights owners for any intended use and for obtaining all required permissions. Acknowledgement of the UNLV University Libraries is requested. For more information, please see the UNLV Special Collections policies on reproduction and use (https://www.library.unlv.edu/speccol/research_and_services/reproductions) or contact us at special.collections@unlv.edu.

    Digital Provenance

    Digitized materials: physical originals can be viewed in Special Collections and Archives reading room

    Publisher

    University of Nevada, Las Vegas. Libraries

    ^ Phosphorous Pentoxide (P.2 0 5)----—0.23 per cent Sulphur Trioxide (S.0.3) —---——0.52 * Carbon Dioxide (C.0.2) ----— ---3.24 * Volatile Matter--------------------- 3.15 " Humus-------------------0.78 per cent Nitrogen in humus---—-10.91 " * Ash-----------------------0.65 " ® Sol. Phos. Acid---------0.01 w ® This soil is a sandy loam containing a large quantity of all the mineral constituents necessary for plant life. This soil is especially rich in the most important plant constituents such as phosphoric acid, potash and lime* The soil does not contain an excess of alkali forming salts. From the analysis submitted and from my knowledge of soils of this character, X have no doubt but that it is well adapted to vines, vegetables, deciduous fruits and alfalfa. There is no tendency on this tract to an excess of alkali, and I have no hesitation at all in saying that the soil is first class in every respect. The Water. I do not believe that Mr. Bull or his associates have done any work in actual development of water. It is true that there are a number of wells in the walley and that these wells are evidently successful. Although I asked Mr. Bull repeatedly as to the wells and as to the ffjjfew, I was unable to get any information on this matter. I did, how­ever, visit wells in the valley that have been dug by other people. I visited particularly a well belonging to Mr. Keith, who is in the N.F.Quarter of Sec.6, Township 10 N., Range 4 E. Hr. Keith was present and said that his well was 210 feet deep and that the water level is 190 feet. In digging - 2-