Xxxii GEOLOGY OF THE HIGH PLATEAUS. 



Heliotypb vn.— Pink Cliffs.— Lower Eocene.— PaunsIgunt Plateau. 



The picture represents the sonthem termination of the Pannsfigunt, and is a good example of the 

 sculpture which is seen in this formation around the rim of the P^ria Amphitheater for a distance of 

 40 miles. The rocks are exquisitely colored. 



HELIOTYPE VIII. — CKOSS-BEDDED JultASSIC SANDSTONE. 



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

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



Heuotype IX.— Cross-bedded Jurassic sandstone. 



The same as the preceding. 



Seliotype X.— The Eed Gate.— Lower Trias.— SHDfiEtJMP. 



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 formation. 



Heliotype XL— Phonolite.— East Fork CaSon. 



