Laserfiche WebLink
<br />..........- <br /> <br />c' <br /> <br /> <br />\ <br /> <br />.,.. "f.~ <br />~~ ".~ <br />",.." '..,~~~~..~. <br />;,!~/, ;,j&':,':. ":.:~~t <br /> <br />~,:.:.~ <br /> <br /> <br />.~;,... <br />. ~"~ <br /> <br />....... - -~ <br />....-..".~ <br /> <br />'~2::: .~_,~ <br /> <br />......... <br /> <br />..:,~,~..... <br /> <br />~'t~ .' p'- ~ <br />~. . <br /> <br />;.............. <br /> <br />_.-D <br /> <br />Figur. B2-Continued. The Dugway Gage and the high.water mark from the 1921 flood (photographs by R.C, Rice, U.S, Geological Survey, <br />September 22, 1921). (e) Downstream view of the high-water section of Ougway Gage painted on cliff next to dugway road. I.G. Cockcroft standing next <br />to gage, High.water mark from the June 1921 flood visible on the cliff at a stage of 2648 feet on the gage (determined by levels on June 7, t922) This <br />stage equals an elevation of 3,132,64 reet above the NGVD1929, <br /> <br />August 10, 1922 <br /> <br />I.G. Cockcroft and Elmer Johnson first tied the elevation of the July 7, 1884. Ilood peak into <br />the Dugway Gage, The 1884 Ilood was the most recent Ilood prior to the June 1921 Ilood <br />that was larger than the 1921 flood, The high-water mark was a crotch in a peach tree at the <br />Lonely Dell Ranch (on river right below the Dugway Gage) from which Jerry Johnson <br />rescued a cottontail rabbit. The cDlrected NGVO 1929 elevation of this mark was 3. 136.90 ft. <br />which equals 30.74 ft above the datum of the Dugway Gage. The elevation of the stump of <br />this tree near Johnson's house was checked by levels by W,E. Dickinson on September 22. <br />1924. On April 13. 1938, J.S. Gatewood estimated that the peak stage of the 18841lood <br />would have been at a stage of about 31.5 ft on the Dugway Gage. However. because the <br />water-surface slope during the 1921 Ilood was between 0,0000 I and 0,00003 hetween the <br />Dugway Gage and the Lonely Dell Ranch, and it is likely that the water-sllIface slope was <br />even lower during the 1884 !lood (because of Ilattening of the water surface in this reach <br />with increasing stage, as shown in this study). the peak stage of the 1884 Ilood was probably <br />no more than 31 ti on the Dugway Gage. <br /> <br />LG. Cockcroft installed a new vet1icallow-water section for the Dugway Gage to replace the <br />old one that had "torn loose." Cockcroft stated that the "new vertical reads 1/2 tenth lower." <br />Roger C. Rice stated that Cockcroft probably installed this new staff gage slightly lower than <br />the original one so that the readings on it and on the lower end of the inclined middle section <br />would agree, Although the original vertical low-water and inclined upper sections were <br />installed relative to the same datum, stage readings tended to be about 0,05 ft lower on the <br />original vertical low-water section than on the inclined middle section, <br /> <br />June 7,1922 <br /> <br />, <br />, <br /> <br />f\"'~!~ <br /> <br />Appendix B 73 <br /> <br />