﻿. 
  322 
  PL. 
  VI 
  

  

  

  Sea 
  level 
  

  

  NE 
  

  

  Sea 
  le\'el 
  

  

  :tion 
  

  

  TO 
  

  

  e 
  135 
  oc 
  

  

  

  %K 
  

  

  LEGEND 
  

  

  SEDIMENTARY 
  ROCKS 
  

   Qat 
  

  

  Alluvium 
  

  

  ii._. 
  

  

  Qt 
  

  

  Terrace 
  deposits 
  

  

  ' 
  includinq 
  alluvium 
  ejrcept 
  

  

  in 
  larger 
  valleys) 
  

  

  UNCONFORM 
  ITY 
  

  

  r" 
  T 
  7i 
  

  

  Fernando 
  formation 
  

  

  UNCONFORM 
  ITY 
  

  

  Tm 
  

  

  Monterey 
  snale 
  

  

  ! 
  siliceous, 
  bituminbus,diatomaceous 
  

   shales 
  and 
  limestone) 
  

  

  F 
  

  

  1 
  3 
  

  

  Tuff 
  interbeddrd 
  

   "with, 
  the 
  Monberev 
  

  

  r 
  

  

  Ttv 
  

  

  Vaqueros 
  , 
  So 
  spe, 
  and. 
  Tejon 
  formations 
  , 
  

   imdafFererLtiated 
  

   ( 
  including 
  some 
  Monterey 
  ui 
  Santa 
  Thez 
  Ranpe 
  

  

  ston 
  

  

  Sandstone, 
  shale 
  conglomerate 
  , 
  and. 
  limestone) 
  

  

  Pre 
  -Monterey 
  

  

  ' 
  sandstone, 
  shale, 
  and 
  conglomerate 
  I 
  

  

  UNCONFORMITY 
  

  

  i 
  

   U) 
  

  

  3 
  > 
  

   (t 
  

  

  "i 
  

   ft 
  

  

  u 
  

  

  Jf 
  

  

  Francis 
  can 
  formation 
  

   I 
  chiefly 
  serjjeniine 
  intruded 
  in 
  

   sandsbone^jasper, 
  and. 
  associated 
  

   metamorpnzc 
  guxacopharu 
  'schist 
  > 
  

  

  IB 
  

  

  > 
  W 
  

   /< 
  

  

  3 
  

  

  .Asphalt 
  

   IGNEOUS 
  ROCKS 
  

  

  Post-Monterey 
  intra 
  sives 
  

  

  I 
  intrusive 
  diabase 
  ) 
  

  

  Pre 
  -M 
  onterev 
  ixl 
  trusives 
  

   (intrusive 
  basalt, 
  diabase, 
  gabbro, 
  

   peridotite. 
  and. 
  serpentine.) 
  

  

  U 
  

  

  h 
  

  

  < 
  

  

  hi 
  

  

  1 
  0. 
  

  

  L907 
  

  

  