Lecture 14: Geology of California


1) PreCambrian Craton Formation. 
same processes as talked about during tectonics lecture -- may be different from today
Crops out in southeastern California (fig 16.26 or Rubey 1-3)
WonĠt talk about this much more

2) Early Paleozoic Passive-Margin Sediment Deposition (Cambrian to Devonian)
Essentially continental shelf deposits
Similar to east coast today
Very mature sandstones and limestones
Crop out in Inyo Mts and Great Basin
Now folded and, especially, thrust faulted. in Great Basin

3) Late Paleozoic Transition to Convergent Margin (Devonian to Triassic)
Island arc volcanism and collisions
Thrusting of continental shelf sediments (see above)
Accretion of terranes now cropping out in Sierras and Klamaths
roof pendents (Saddlebag Lake, Convict Lake, near Mammoth Lakes)
Crustal thickening
These structurally complex rocks now form the ranges of the Basin and Range

4) Mesozoic Convergent Margin (Triassic to Tertiary) [draw typical convergent margin]
Formation of Sierra Nevada Batholith
from many different plutons
major crustal thickening
roots of Mesozoic volcanoes
Formation of Great Valley Sequence (a fore-arc basin)
Structurally intact group of volcanic-rich sed rx
Can be correlated to erosion of the Sierra volcanoes
deposited on the Coast Range Ophiolite, (arc-related oceanic crust?)
deoposited in fore-arc basin?
Formation of the Franciscan Complex (which includes many different terranes)
A complex agglomeration of oceanic terranes
all in a mud-matrix melange (i.e., mixture), now very soft and landslide-prone
oceanic in nature
Blocks of blueschist, greeywacky, basalt, chert, and rare limestone
Why does limestone not fit in?
Same age as the GVS, but structurally very different
this is the accretionary wedge (but very disrupted), plus various accreted terranes, 
like the Marin Headlands Terrane
Some of the best evidence for suspect terranes
Paleomagnetic evidence from limestones
Laytonville limestone from south of equator
Permanente limestone from north of equator
Inferred history of alternating convergence and strike-slip faulting.
	Accretion of more terranes all along Western Cordillera

5) Cenozoic San Andreas Fault and Basin and Range Extension
The Atwater Farallon Plate story [draw this, using fig 16.25 as a guide]
Triple junctions
Convergent volcanism restricted to the Cascades
Transpression and pull-apart basins [look for good diagram]
The tranverse ranges
In southern California, these folds form oil and gas traps
Formation of Salinian Block
Piece of Sierras (? or farther south originally??) brought northward
Formation of the Coast Ranges
Basin and Range extension
Volcanism on edges of Basin and Range

6) Glacial Ice Ages and continued faulting
Formation of large glacial lakes
mention ancient shore-lines
These lakes are now playas.
Formation of morains on east side of Sierras
Volcanism on edges of Basin and Range
Long Valley Caldera and associated volcanism
Modac Plateau basaltic volcanism, also along faults

Present-day configuration -- Physiographic Provinces

Sierras - Klamaths Batholith: accreted terranes, thickened crust
Basin and Range -- East side of Sierra, Death Valley, Paniment Valley
Great Valley: fore-arc basin
Coast Ranges: Franciscan complex
Salinian Block: Piece of Sierras(?) brought north by SAF
This is what weĠre standing on.
Cascades
Mention ocean water gets into Mt St Helens, again
Modoc Platea
Mojave Desert -- Garlok Fault