East Bay Hills
The East Bay Hills are a mountain range in the California Coast Ranges subdivision of the Pacific Coast Ranges in northern California, United States. They are the first range of mountains east of San Francisco Bay and stretch from the Carquinez Strait and San Pablo Bay in the north to Alameda Creek/Highway 84 in the south, crossing both Contra Costa and Alameda Counties. Although not formally recognized by United States Geological Survey Geographic Names Information System, the East Bay Hills is included as part of the Diablo Range in the USGS list of multiple GPS coordinates for the Diablo Range.
Geography and geology
The East Bay Hills runs northwest to southeast for approximately with its midpoint at 37° 48' 06" N, 122° 09' 12" W. The tallest peak in the range is Sunol Peak whose summit elevation is.The East Bay Hills consists of multiple named components, from north to south: Franklin Ridge, then the Briones Hills, the Berkeley Hills, the San Leandro Hills centrally, and Walpert Ridge and Pleasanton Ridge to the southwest and southeast, respectively, culminating near Alameda Creek/Highway 84 and Niles Canyon. Further south is a sub-range of the Diablo Range including Mission Peak, Mount Allison, Mount Day and Mount Hamilton that is informally known as the Mount Hamilton Range.
Ecologically, the East Bay Hills are part of the East Bay Hills/Western Diablo Range subregion, which along with the Diablo Range, falls within the Central California Foothills and Coastal Mountains Level III Ecoregion #6.
Geologically, the East Bay Hills are bounded by the Calaveras Fault to the east and the Hayward Fault to the west. The Hayward Fault merges into the Calaveras Fault in east San Jose in Santa Clara County, about south of Fremont and the southern boundary of the East Bay Hills.
The East Bay Hills are a major center of earthquakes and landslides due to the nearby major and minor fault zones. Both the East Bay Hills and Mt. Diablo continue to rise a year, which extrapolates to over 1,000 years assuming constant rate and negligible erosion.