Title |
No. 14 Original, Abstract of the Testimony, vol. 1, pp. 1-748 |
Subject |
Mines and mineral resources -- Environmental aspects -- Utah; United States -- Trials, litigation, etc.; Utah -- Trials, litigation, etc.; Colorado River (Colo.-Mexico); Colorado River (Colo.-Mexico) -- Environmental aspects |
Description |
Testimony given before special master Charles Warren in a suit brought by the United States against the state of Utah over ownership of the bed of the Colorado River. Much of the testimony was given by river runners, scientists and engineers, petroleum geologists, and placer miners. The testimony constitutes an extensive oral history of the men and women who utilized the Colorado River Basin in Utah prior to 1929. |
Publisher |
Microfilm gift of John Weisheit, 1997 |
Date |
1930-10 |
Type |
Text |
Format |
application/pdf |
Source |
Original format: 12 microfilm reels |
Language |
eng |
Relation |
No. 14 Original. Abstract in Narrative Form of the Testimony Taken before the Special Master, and filed in His Court by Him, vol. 1, pp. 1-748 |
Rights Management |
Digital image copyright 2003, University of Utah. All rights reserved. |
Holding Institution |
J. Willard Marriott Library, University of Utah; Originals in: Utah State Archives; Salt Lake City, Utah. |
Scanning Device |
Sunrise 2000 Microfilm Scanner |
Scanning Contractor |
iArchives Inc., Orem, UT |
Call Number |
ACCN 1702 |
ARK |
ark:/87278/s6pv6n1x |
Setname |
usa_crc |
ID |
110904 |
Reference URL |
https://collections.lib.utah.edu/ark:/87278/s6pv6n1x |
Title |
Abstract Testimony, V 1, p. 0122 |
Format |
application/pdf |
Identifier |
1929-1931-roll11_0303a.jpg |
Holding Institution |
J. Willard Marriott Library, University of Utah Originals in: Utah State Archives; Salt Lake City, Utah. |
Resolution |
Archival TIFF: 3000 x 4600 |
Dimensions |
JPEG: 650 x 1000 |
Bit Depth |
8-bit |
OCR Text |
Show 12 9 ( has Ibas ) crossed ( tlie the ) river at the same points with freight wagons . ( R . 445-446 . ) The average water ( at -it it ) the fords was two to three feet deep ; ( sometimes sometinies ) lower , sometimes higher . The lowest he has ever seen the water is about a foot deep . The river is variable as to depth . Conditions ( changed chaiiged ) since 1880 ( , ) ) in this respect . There were big flats and ( bot- bot ) toms all along the river , and it has changed ; those bottoms are all washed away . The river is over to one side one day and over somewhere else the next day ; it is ( quicksandy quieksandy ) formation ; when the ( Avater water ) hits the ( quicksand quichsand ) it melts it ; when the water is real high , it tears right in and washes out a whole bottom ; practically all the land that was there when they first went there has ( been beeii ) changed and washed out , and new sediment ( formed forined ) in the place of it . He helped in the attempt to control the river by building riprap dikes ( along aloug ) the bank and filling the same with rock . We would riprap the ( banks bank-s banks ) ; that is the only bottom ( 011 on ) the San Juan River as he knows of , where Bluff is located now , that has ( not liot ) been moved ( with Avith ) the high water and the ( quicksand quichsand ) ; they used to riprap there and change the river and put it over on the other side to hold their ( farming faTming ) land from washing away . After you get down ( below belo- belo ) ( BlufE Bluff ) three or four miles , ( the tJie ) country . ( has bas ) ( been beeii ) washed away ; the place they call Sand Island flats , a mile or two wide , that ( lias h1as ) ( all C-111 C111 ) been washed out . |
Setname |
usa_crc |
ID |
110734 |
Reference URL |
https://collections.lib.utah.edu/ark:/87278/s6pv6n1x/110734 |