194 



CALIFORNIA ACADEMY OF SCIENCES [Proc. 4th Sek. 



The principal evidences of climate during Tejon time are 

 yielded by a study of plants and invertebrate marine forms. 

 Of these, the plants give very strong evidence of a mild climate 

 far to the north. Palms have been reported from the carbona- 

 ceous deposits of Washington and from the Peacock mine in 



Fig. 1. Map of California showing probable extent of the Tejon and Martinez Seas. The line 

 ■which in general is the more easterly marks the maximuoQ inland extension of the Tejon .Sea and the 

 other line indicates the probable easterly limit of the Martinez Sea. 



1. Te.'on of Roond V»lley, Mendocino County; 2, Tejon neBr OroTille: 3, Tejon of MaryBville Butten: 4. Tejon at 

 mouth of Merced River 0«&on ; 6, Tejon of the Tehachapi Mountains; 6. Martinez of Rock Creek; 7. Tejon of San Diego 

 County; 8. Tejon and Martinet at Clear Lake. 9. Martinei north of Suisnn; 10. Martinez and Tejon at Benicia; 11. Type 

 locality of Martinez. 12. Martinez and Tejon north of Mount Diablo; 13. Martinez and Tejon south of Mount Diablo. 

 14. Martinez of San, Pedro Point. San Mateo County; 15. Tejon at New Idria; 16. Tejon at Coalinga District; 17. TejoD 

 .. .k. c ^1... Valley; 18, Maninez of Calabasaa Quadrangle; 19. Tejon and Ma ' . . - . . 



of the Santa Ajia MoiiDt«in 



