Las Trampas Peak

The name "Las Trampas" or "the traps" in Spanish, is derived from the indigenous Saclan Bay Miwok peoples' technique of using the area's steep canyons to trap herds of Tule elk and other game species for hunting.[2]

Las Trampas Peak and its surrounding environs are located in the Inner Coast Ranges in the San Francisco Bay Area's Contra Costa County, more specifically in the Berkeley Hills subrange.

The peak is the apex and terminus of an approximately 8 mile-long north-south running ridge composed of Miocene marine sedimentary rock, known as Las Trampas ridge.[1]

Las Trampas Creek and its tributary Grizzly Creek begin on the mountain. Las Trampas Creek is one of the largest sub-watersheds within the Walnut Creek Basin, comprising an area over 17,000 sq acres in size.[3]

Like much of Contra Costa County, Las Trampas peak and its surroundings are largely composed of sedimentary rocks from the Great Valley Sequence.[2] These formations have been heavily altered by millions of years of faulting and rifting, a process that is still ongoing.[4]

The region around Las Trampas Peak is tectonically active, with earthquakes being a common occurrence.

Certain bands in the area contain abundant fossils of prehistoric sea life from the Miocene epoch (~23 mya to ~5 mya)[4]

A mosaic of habitats typical of the region in the Canyon of Bollinger Creek, which begins on the south flank of Las Trampas Peak

Due to its location within a protected wilderness area, Las Trampas Regional Wilderness, Las Trampas Peak and its surrounding hills are home to many species of wildlife including Columbian black-tail deer, Coyotes, Bobcats and numerous species of birds.[2]

The north slope of the mountain is thickly forested with California Coast Ranges mixed evergreen forest, dominant trees include Coast Live Oak, Valley oak and california bay among others.

The exposed south-facing slope of the mountain is covered in Chaparral.

The east and west sides of the mountain are both mixtures of forest, scrub and grassland, largely depending on the local geology.[4]