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Las Trampas Peak

Coordinates:37°50′00″N122°03′53″W / 37.8332594°N 122.064685°W /37.8332594; -122.064685
From Wikipedia, the free encyclopedia
Mountain in SF Bay Area Coast Ranges
Las Trampas Peak
La Sierra de Las Trampas
Las Trampas Peak in the early spring near Alamo, CA
Highest point
Elevation556 m (1,824 ft)
Coordinates37°50′00″N122°03′53″W / 37.8332594°N 122.064685°W /37.8332594; -122.064685
Geography
Map
LocationContra Costa County, CA
CountryUnited States
StateCalifornia
countyContra Costa County
Geology
Rock typesedimentary

Las Trampas Peak is a 1,827 ft (557 m) peak in theInner Coast Ranges in westernContra Costa County, California, in theSan Francisco Bay Area.[1]

Las Trampas Peak as seen from the west under a rainbow (August 13th, 2023)

Etymology

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

Geography

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Las Trampas Peak and its surrounding environs are located in theInner Coast Ranges in theSan Francisco Bay Area'sContra Costa County, more specifically in theBerkeley Hills subrange.

The peak is the apex and terminus of an approximately 8 mile-long north-south running ridge composed ofMiocene marinesedimentary rock, known asLas Trampas Ridge.[1]

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

Geology

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Fossil Sand Dollar in grey sandstone
Fossilizedsand dollars insandstone from theMiocene on outcrops just below Las Trampas Peak (October 8th, 2022)

Like much of Contra Costa County, Las Trampas peak and its surroundings are largely composed offossiliferous sedimentary rocks from theGreat 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 theMiocene epoch (~23 mya to ~5 mya)[4][5]

Ecology

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Fog flows over theBerkeley Hills during a summer sunset, as seen from Las Trampas Peak (June 13th, 2023)

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 includingColumbian black-tail deer,Coyotes,Bobcats and numerous species of birds.[2]

The north slope of the mountain is thickly forested withCalifornia Coast Ranges mixed evergreen forest, dominant trees includeCoast Live Oak,Valley oak andcalifornia bay among others.

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

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

References

[edit]
  1. ^ab"California Topographic Maps - Perry-Castañeda Map Collection - UT Library Online".maps.lib.utexas.edu. Retrieved2023-07-26.
  2. ^abcKnight, Walter (1973).The Story of Las Trampas(PDF). East Bay Regional Parks District.
  3. ^Contra Costa County Watershed Atlas(PDF). Contra Costa County Community Development Department, Contra Costa County Public Works Committee. 2004. p. 79.
  4. ^abc"Las Trampas Wilderness Regional Preserve".East Bay Parks. Retrieved2023-10-11.
  5. ^Ham, Cornelius K. (1952).Geology of Las Trampas Ridge : Berkeley Hills, California. Davis Libraries University of California. Sacramento : California State Print. Office.
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