northwestern Colorado. The major portion of the range and all areas

rising above 3,050 m (10,000 ft) lie within five Utah counties (Daggett,

Duchesne, Summit, Uintah and Wasatch). The high elevation segment of

the range in Utah is commonly referred to as the High Uintas. This

report will consider only the so-called High Uintas.

portions of Wayne, Garfield, Sevier, and Emery Counties. Situated on

the western edge of the Colorado Plateau, this scenic land is adjacent to

Dixie and Fishlake National Forests and Goblin Valley State Park.

Other Park Service areas nearby include Zion and Bryce Canyon

National Parks, and Cedar Breaks National Monument to the west;

Canyonlands National Park and Arches National Park to the east; and

Glen Canyon National Recreation Area to the south and east.

1967. Most common and destructive are dry mantle floods, which flow as

a muddy mortar-like substance containing 40 to 55 percent water. Hundreds

of tons of protective topsoil are removed from watershed lands,

debris and boulders are picked up as the flow travels down steep stream

channel gradients, and then the flood is debouched into communities and

on to productive cropland.

evaluation for dams in the Wasatch Mountains in north-central Utah. The

major objectives of this study were to identify potential earthquake sources

in the region and to estimate MCEs (maximum credible earthquakes) for these

sources. The conclusions presented in this report are based on geologic

mapping, trenching, study of aerial photography, mapping and correlation of

Quaternary deposits, soil profile descriptions and sampling, and analysis of

historic seismicity. The Regional Study area includes an area on the eastern

margin of the Basin and Range province that extends east from the Wasatch

Front to the Uinta Mountains and from the Idaho-Wyoming border south to the

Wasatch Plateau.

The ultimate phase will expand on the initial phase development. Its purpose will be to increase the transbasin diversion to the Bonneville Basin and to provide water for replacement and additional use in the Uinta Basin. Water for the Uinta Basin will be provided by developments on streams originating in the basin and from the Green River either by pumping or by gravity flow through a tunnel heading at the existing Flaming Gorge Reservoir. This report has been prepared as a means of bringing together all of the available data that may be useful in outlining and conducting an orderly investigation of the ultimate phase as a whole.