D. 132.6

_Volcanic Ash Flow._ The rimrock north of the John Day River between

here and Dayville is a volcanic ash flow that erupted about five million

years ago as red hot pumice highly charged with gas. A rapidly moving

incandescent cloud probably filled the ancient John Day River valley and

deposited ash to a depth of more than 100 feet over a distance of 60 to

70 miles. As shown in Figure 4, the ash flow blankets about 200 feet of

gravels that had been deposited in the valley. The rimrock and the

gravels above and below it constitute the Rattlesnake Formation.

[Illustration: Fig. 4.—View northwest across the John Day River valley

toward Picture Gorge.]

The Geologic Setting of the John Day Country: Grant County, Oregon · 第 6 / 22 题