





^\ 







j:^Ji,,- : '~-^i 



r^Sfe 



«tjv ■• ' 





Two active Asphaltum Springs in :i corner of 



the Pit." 



According to Geological Reports, this deposit is well designated as 

 Pleistocene, or early Quaternary, and a portion of the great Elysian 

 Park anticline. From this anticline there extends a special formation 



15 



