XXXli GEOLOGY OF THE HIGH PLATEAUS. 



Heliottpe VII. — Pink Cliffs. — Lower Eocene. — Paunsagunt Plateau. 



The picture represents the southern termination of the Paunsagunt, and is a good example of the 

 sculpture which is seen in this formation around the rim of the Paria Amphitheater for a distance of 

 40 miles. The rocks are exquisitely colored. 



Heliottpe VIII. — Cross-bedded Jurassic sandstone. 



Taken in Johnson's Canon, on the road from Sevier Valley to Lower Kanab. Much finer instances 

 may he seen in any of the deep canons cut in this formation. 



Heliottpe LX — Cross-bedded Jurassic sandstone. 



The same as the preceding. 



Heliottpe X. — The Eed Gate.— Lower Trias.— Shes/rump. 



Taken at the southeast flank of Thousand Lake Mountain. The beds in the cliff are variegated 

 in color, being banded horizontally, and the colors are very deep and rich. The sculpture is very charac- 

 teristic of the formatiop. 



Heliottpe XI.— Phonolite.— East Fork CaSon. 



