Download Geologic Evolution of the Northernmost Coast Ranges and by K. R. Aalto, G. D. Harper, G. A. Carver, S. M. Cashman, W. PDF

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By K. R. Aalto, G. D. Harper, G. A. Carver, S. M. Cashman, W. C. Miller, H. M. Kelsey(auth.)

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Published by means of the yank Geophysical Union as a part of the Field journey Guidebooks Series.

This guidebook describes the geology of components we'll stopover at within the western Klamath Mountains and Coast levels of northernmost California. Articles are prepared within the order of our go back and forth, from Medford to Crescent urban on road 199, and south to Eureka on coastal road a hundred and one. Authors summarize the nearby geologic environment and result of their examine and previous experiences of the parts we'll stopover at in overview papers. hence the geologic heritage precious for interpretation of box stops is equipped with no the necessity of extra papers.

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Extra resources for Geologic Evolution of the Northernmost Coast Ranges and Western Klamath Mountains, California: Galice, Oregon to Eureka, California July 20-28, 1989

Sample text

Light dotted lines delineate covered areas. An area with solely sandstone olistoliths (labeled BF) exists in the western region. o b v i o u s p o s t - d e p o s i t i o n a l form m o d i f i c a t i o n ( d i s c u s s e d b e l o w ) . However, some a p p e a r t o have s u f f e r e d l i t t l e s t r u c t u r a l m o d i f i c a t i o n . For t h e s e , t h e r e a p p e a r t o b e two s o u r c e s : (1) a p r i m a r y , f i r s t c y c l e source f o r abundant angular, t a b u l a r b l o c k s of sandstone, greenstone and c h e r t ; and ( 2 ) a r e c y c l e d - s e d i m e n t a r y s o u r c e f o r subrounded t o w e l l rounded c l a s t s of t h e s e and o t h e r l i t h o l o g i e s ( F i g u r e 11).

At Enderts Beach a subhorizontal shear zone places northwest to southeast-dipping, thinlybedded, facies E turbidites above thickly-bedded, facies B and C sandstones (Figures 30 and 31). The shear zone is estimated to be 10 m thick at the maximum, but its upper contact is not exposed. The thinly bedded turbidites probably are overlevee interchannel or interlobe submarine fan deposits, once in depositional contact with channel or suprafan lobe sandstones (Aalto, 1986b) . NORTH ISLAN Structures Introduction.

J r . P. G. S. G e o l o g i c a l S u r v e y R e s e a r c h , 1967, U. S . G e o l o g i c a l S u r v e y P r o f e s s i o n a l P a p e r 575-C, C1-C9, 1967. , J r . L. H. D o t t , J r . H. S h a v e r , S o c i e t y o f Economic P a l e o n t o l o g i s t s and M i n e r a l o g i s t s S p e c i a l P u b l i c a t i o n 1 9 , 345-357, 1974. , J r . L. J o n e s , P l a t e t e c t o n i c h i s t o r y of t h e Yolla Bolly junction, northern California, G e o l o g i c a l S o c i e t y o f America C o r d i l l e r a n S e c t i o n Guidebook, 1977.

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