Geologic map of the Dewey quadrangle, Grand County, Utah (M-169)

M169
In stock
1:24,000 Geologic Maps
$7.95
$7.95

By: H. H. Doelling

The Dewey quadrangle is located on the northeast edge of the salt anticline region of the Paradox basin in east-central Utah. Exposed consolidated formations range in age from Permian to Cretaceous. In ascending order, these units include the Permian Cutler Formation; the Triassic Moenkopi Formation, and Chinle Formation; the Jurassic Wingate Sandstone, Kayenta Formation, Navajo Sandstone, Entrada Sandstone, Summerville Formation, and Morrison Formation; and the Cretaceous Cedar Mountain Formation, Dakota Sandstone, and the Tununk and Ferron Members of the Mancos Shale. Mapped surficial deposits are of alluvial, eolian, mass-movement, mixed eolian and alluvial, and mixed eolian and residual origin.

Other Information:
Published: 1996
Pages: 20 p.
Plates: 2 pl.
Scale: 1:24,000
Location: Grand County
Media Type: Paper Map

The cookie settings on this website are set to 'allow all cookies' to give you the very best experience. Please click Accept Cookies to continue to use the site.
لقد تم اشتراكك بنجاح! | You have successfully subscribed!