Age and Environmental Interpretation of Middle Cretaceous Dinoflagellate Assemblages from Central Belt Franciscan and Great Valley Sequence Outliers, Northern California Coast Ranges: ABSTRACT

AAPG Bulletin ◽  
1986 ◽  
Vol 70 ◽  
Author(s):  
J. Lucas-Clark
Keyword(s):  
Northern California ◽  
California Coast ◽  
Environmental Interpretation ◽  
Central Belt ◽  
Coast Ranges ◽  
California Coast Ranges ◽  
Great Valley

Northern California Coast Ranges, Domain 4

2007 ◽  
Author(s):  
Earl B. Alexander ◽  
Roger G. Coleman ◽  
Todd Keeler-Wolfe ◽  
Susan P. Harrison
Keyword(s):  
San Francisco ◽  
Northern California ◽  
Coast Range ◽  
Klamath Mountains ◽  
California Coast ◽  
Mountain Ranges ◽  
The North ◽  
Coast Ranges ◽  
California Coast Ranges ◽  
Great Valley

The Northern California Coast Ranges domain is in a mountainous region in which most of the mountain ranges are aligned north–south, or more precisely north, northwest– south southeast, curving around the Klamath Mountains into Oregon where the domain branches to north–south and northeast–southwest trends on the northwest side of the Klamath Mountains. It extends about 600km from the Golden Gate at the entrance to San Francisco Bay north to about the Coquille River in Coos County and nearly to the North Umqua River in Douglas County, Oregon. The domain corresponds to a physiographic region that is bounded by the Pacific Ocean on the west, the Coast Range of Oregon and Washington (Orr and Orr 1996) on the north, the Klamath Mountains on the northeast, the Great Valley of California on the southeast, and on the south by the drainage outlet of the Sacramento and San Joaquin rivers through the Carquinas Straight and San Pablo Bay. Serpentine is scattered in relatively small ultramafic bodies throughout the Northern California Coast Ranges and is concentrated along some of the major faults. For 200 or 300 km south from the Klamath Mountains, the Northern California Coast Ranges region is a rectangular strip 90–110 km wide between the Ocean and the Great Valley of California. The Klamath Mountains crowd the region to a narrow strip only 10 or 12 km wide in Del Norte County. Most of the mountain ranges have approximately concordant summits that are tilted up toward the east–northeast. Therefore, the highest altitudes are on the east, just south of the Klamath Mountains. North Yolla Bolly at 2397 m (7865 feet) and South Yolla Bolly at 2466 m (8092 feet) have the highest summits. Both of these and some neighboring mountains have cirques and moraines indicative of glaciation on their north slopes. There is no evidence of glaciation in any areas with serpentine rocks. Only the Rogue and Klamath rivers cut from east to west all of the way across the Northern California Coast Ranges, except for a few smaller streams such as the Chetco and Smith rivers that have headwaters in the Klamath Mountains.

EARLY PALEOGENE SEDIMENT DISPERSAL AND PALEOGEOGRAPHY OF THE NORTHERN CALIFORNIA COAST RANGES: NEW INSIGHTS FROM DEPTH-PROFILED DETRITAL ZIRCON U-PB AGES

2019 ◽  
Author(s):  
Glenn R. Sharman ◽  
◽  
Robert J. McLaughlin ◽  
Trevor A. Dumitru ◽  
Matthew A. Malkowski
Keyword(s):  
Detrital Zircon ◽  
Northern California ◽  
California Coast ◽  
Sediment Dispersal ◽  
Coast Ranges ◽  
California Coast Ranges ◽  
Early Paleogene

Concordant paleolatitudes from ophiolite sequences in the northern California Coast Ranges, U.S.A.

1991 ◽  
Vol 198 (1) ◽  
pp. 1-21 ◽  
Author(s):  
Edward A. Mankinen ◽  
C.Sherman Gromme ◽  
Kathleen M. Williams
Keyword(s):  
Northern California ◽  
California Coast ◽  
Coast Ranges ◽  
California Coast Ranges
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