Skip to main content

Search the Special Collections and Archives Portal

upr000048 100

Image

File
Download upr000048-100.tif (image/tiff; 26.17 MB)

Information

Digital ID

upr000048-100
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

«> IbUsHI : KM ? aWfSmwffi Las Vegas, Kev., Aug. 29, 1913. • 'r• F. R. McHaruee. Lob Angeles, Cal. Lear Sir: 1 beg to acknowledge receipt of your letter under date of Au­gust 27 and contents noted. Prior to receiving tints letter on yeater- day, I drove out to see Buol’s well which, is 2 b/4 miles above our Spring and very close to the Islington well which has oeen flowing a- bout 70" for over one year. The Buol well is 950 feet from the Eg- lington well and Mr. Eglington advises me that he can see sorae change in hie well since the Buol well was struck. A very conservative es­timate of Buol’e well, as given by men who are accustomed to guessing at the wells of this section is 80" instead of 100" as reported to you. I note you say Pr. Buol took occasion to suggest that it might be well for us to purchase land contiguous to our lands surrounding the spring as a protection, but, before this is done, I should like to suggest that the condition^ be well looked into by an engineer of geological knowledge and get a thorough report on the probability of wells being sunk ofx of our land causing any damage to our present springs, as I do not wish to express a personal opinion in this matter for my knowl­edge of geological formation is very limited. The land adjoining our holdings at tne springs and back south and west for three quarters of a mile is very rocky and on the .hard pan which comes to the surface al- •v_