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Big Pines, California

1924 establishments in CaliforniaAngeles National ForestHill and mountain resortsLos Angeles County, California, geography stubsPopulated places established in 1924
San Gabriel MountainsSki areas and resorts in CaliforniaTourist attractions in Los Angeles County, CaliforniaUnincorporated communities in CaliforniaUnincorporated communities in Los Angeles County, CaliforniaUse American English from July 2025Use mdy dates from July 2023Wrightwood, California
Jackson Lake, in Wrightwood, California (1)
Jackson Lake, in Wrightwood, California (1)

Big Pines is an unincorporated community in Los Angeles County, California, United States. It is in the Angeles National Forest, San Gabriel Mountains.

Excerpt from the Wikipedia article Big Pines, California (License: CC BY-SA 3.0, Authors, Images).

Big Pines, California
Angeles Crest Highway,

Geographical coordinates (GPS) Address Website Nearby Places
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Wikipedia: Big Pines, CaliforniaContinue reading on Wikipedia

Geographical coordinates (GPS)

Latitude Longitude
N 34.378888888889 ° E -117.69 °
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Address

Angeles National Forest Visitor Center - Big Pines

Angeles Crest Highway 24537
92397
California, United States
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Website
fs.usda.gov

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Jackson Lake, in Wrightwood, California (1)
Jackson Lake, in Wrightwood, California (1)
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Nearby Places

1812 San Juan Capistrano earthquake

The 1812 San Juan Capistrano earthquake, also known simply as the Capistrano earthquake or the Wrightwood earthquake, occurred on December 8 at 15:00 UTC (07:00 a.m. local time) in Alta California. At the time, this was a colonial territory of the Spanish Empire. Damage occurred at several of the missions in the region of Pueblo de Los Ángeles, including Mission San Gabriel Arcángel and Mission San Juan Capistrano, where 40 parishioners were killed during the collapse of a church at an early morning service. Tree-ring and paleoseismic evidence show that there is a strong likelihood that the earthquake originated along the Mojave segment of the San Andreas Fault near Wrightwood, but other faults have been suggested as the cause. Several studies in the 1980s placed the shock along the southern Newport–Inglewood Fault near the zone of highest reported intensity. This fault is near the coast and the most significant damage at the missions, but later work at trench sites along the San Andreas Fault excluded it for this large-to-very-large shock. Dynamic rupture modelling enabled another proposal in the 2010s involving a dual-rupture scenario with both the San Andreas and San Jacinto Fault Zones. Each of these studies worked with limited data, and the effects of the shock and various fault rupture details led to Mercalli intensities of VII (Very strong) to IX (Violent) being proposed. Magnitudes from 6.9 Mla on the low end to 7.5 Mw on the high end were also presented.