By Doris Sloan
In a full of life and interesting variety, Sloan describes forces comparable to the flow of tectonic plates, erosion, the waves at the coast, and human task. She offers heritage info at the techniques, time-frame, and rocks which are the foremost to figuring out the Bay region panorama and geologic background, then turns to unique areas of the Bay sector and to San Francisco Bay itself.
* beautifully illustrated with 139 colour images, forty-one drawings, and 29 maps
* Covers Alameda, Contra Costa, Marin, Napa, San Francisco, San Mateo, Santa Clara, Solano, and Sonoma counties
* supplies transparent, nontechnical causes of complicated themes together with plate tectonics and the Bay Area's fault systems
* indicates locales in parks and open area preserves to view Bay region geology in action
Read or Download Geology of the San Francisco Bay Region (California Natural History Guides) PDF
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Extra info for Geology of the San Francisco Bay Region (California Natural History Guides)
Snow Mountain and its pals on ridge in historical past include Franciscan rocks. T H E R E M A R ok A B L E R O C ok S O F T H E B AY A R E A sixty seven The nice Valley series within the Bay quarter has been divided into 4 terranes (table 2). 3 of them, the Del Puerto, Healdsburg, and Elder Creek Terranes, encompass oceanic crust (the ophiolite) and diverse varieties of turbidite rocks. The Del Puerto Terrane additionally contains silica-rich volcanics, and the Healdsburg Terrane encompasses a conglomerate with certain cobbles. The resource of the conglomerate remains to be unknown, yet a few proof indicates it was once shaped in southern California. The fourth, the purpose area Terrane, that's stumbled on simply west of the San Andreas Fault, involves rocks which are fairly diﬀerent from all of the different nice Valley rocks and maybe could be installed a class in their personal. They contain not just ocean crust and turbidite rocks, but additionally a conglomerate at Anchor Bay in Mendocino County whose cobbles fit rocks stumbled on 350 miles to the south at the east facet of the San Andreas Fault. As defined in bankruptcy 2, this conglomerate has been used to estimate the volume of oﬀset at the fault. Salinian advanced: customer from Down South The 3rd form of basement rock within the Bay quarter contains plutonic rocks of the Salinian complicated, also known as the Salinia Terrane (table 2). They ensue simply west of the San Andreas Fault in Marin, Sonoma, and San Mateo Counties and on the Farallon Islands. just like the Franciscan rocks, they have been shaped somewhere else in the course of the Mesozoic plate collisions. They have been dropped at the Bay region through circulate at the San Andreas Fault approach, and the Bay sector is the northernmost position the place Salinian rocks ensue. Salinian complicated rocks additionally shaped in a subduction atmosphere. They contain plutonic rocks shaped in magma chambers a long way lower than the outside because the subducting plate partly melted (ﬁg. 17). they've been uncovered by way of erosion of the overlying rocks. In composition, these on Bodega Head, element Reyes (pl. 26), the Farallon Islands, and Montara Mountain are quite wealthy in silica, rocks known as “granitic. ” they're comparable in composition to the granitic rocks present in the Sierra Nevada and are of comparable age: eighty to a hundred and ten million years previous. The Salinian complicated granitics have been shaped numerous hundred miles to the south. Geologic facts means that they shaped as a southern extension of the Sierra Nevada and later have been separated from the Sierra by way of San Andreas Fault movement and rafted sixty eight T H E R E M A R ok A B L E R O C ok S O F T H E B AY A R E A Plate 26. Granitic rocks at McClures seashore, element Reyes. northward with the Paciﬁc Plate. Paleomagnetic reports have advised an foundation even farther to the south, yet newer paintings doesn't aid this concept. The San Andreas Fault process is chargeable for their displacement, and their presence within the Bay quarter is simply transitority. they're geologic viewers touring with the Paciﬁc Plate because it strikes previous us towards Alaska. Older Metamorphic Rocks At a couple of locales within the Bay quarter, small patches of older metamorphosed rocks happen with the granitic rocks.