Fort Tejon, in fact, was not the epicenter, nor was it even near the epicenter of the earthquake. Questions remain, however, as to when it will occur, and whether the next "Big One" will be as big as 1857.
It was universially noticed (Fort Tejon State Historic Park monthly newsletter) Eyewitness Accounts (California Geology) References. The population at the time was Technically, Parkfield was the epicenter of this earthquake, as it was the origin of the rupture, but most scientists would be more concerned with the extent and location of the entire rupture; Fort Tejon was approximately the midway point of the rupture.
on bended knees, and hearts throbbing with terror, made fervent Displacement along the fault was as much as 9 meters (30 feet) in the Carrizo Plain but less along the Palmdale section of the fault, closest to Los Angeles. And the largest earthquake to hit Southern California in historic times occurred on January 9, 1857. Agnew, D. and Sieh, K., 1978, A documentary study of the felt effects of the great California earthquake of 1857: Seismol. The earthquake actually acquired its name because Fort Tejon was the only populated locality near the fault, and naturally, the Fort suffered more damage than the rest of sparsely-populated 1857 Southern California. The 7.9 magnitude Tejon Earthquake (with an intensity of perhaps 8.25), which struck about 8:20 am on the morning of Jan. 9, 1857 is considered by many to be the largest historic earthquake that California has witnessed, vying for that title with the better known San Francisco quake of 1906. At downtown Los Angeles, with a maximum perceived intensity of VI, some homes and buildings were cracked, but no major damage was reported. of the inhabitants fled from their dwellings, the majority of whom,
It came to be known as the great "Fort Tejon" earthquake — although such appellation could be very misleading.
The 1857 and 1906 events were both on the San Andreas Fault, although the 1906 earthquake ruptured the northern segment of the fault, from Hollister (San Benito Co.) northward, for 400 km (250 miles). The peculiar motion
The 1857 quake was the last so-called "Big One" in Southern California, and a similar event will almost certainly happen again in the future. supplications that the imminent and impending danger might be severe which has been experienced on this coast for a long series Though the shock was centered near Parkfield, the event is referred to as the The earthquake is the most recent large event to occur along that portion of the San Andreas Fault, and is estimated to have had a maximum perceived intensity of IX (The 1857 earthquake ruptured about 350 kilometers (220 mi) of the southern part of the San Andreas Fault, the structure that accommodates most of the displacement along the The earthquake ruptured a substantial portion of the southern San Andreas fault, but not the entire length.
(Public domain. Annual ring widths were measured and plotted against the growth year determined by ring counting.
68, pp. On the extreme northern end of the rupture zone, the surface cracking extended 80 kilometers (50 mi) north of Cholame into Evidence of uprooted and displaced trees south of Elizabeth Lake indicates surface faulting along a mole track (an "array of en echelon primary Various accounts of the event indicate the presence of The firsthand reports were most abundant for the shocks felt at 1, 2, and 4 hours before the main shock which were later labeled the predawn, dawn, and sunrise shocks. SCVHistory.com is another service of SCVTV, a 501c3 Nonprofit • Site contents ©SCVTV • Additional copyrights apply experienced during is continuance very much resembled that on board The Great 1857 "Fort Tejon" Earthquake: Shake, Rattle, and Roll! Los Angeles appears to have fared well last time, but it remains unclear how modern structures will respond in the future.
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