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Geography - Cajon Pass

Lone Pine Canyon




















Lone Pine Canyon is one of the key natural gateways into Cajon Pass, on the eastern side near Wrightwood. The canyon runs down the San Gabriel Mountains and historically provided a natural route from the high desert around Victor Valley into the Los Angeles Basin.

A few points of note:

Geography: Lone Pine Canyon cuts down through the San Andreas Fault zone, making it a dramatic, steep-sided wash. It joins the greater Cajon Pass corridor, which has long been the main passage between Southern California and the Mojave Desert.

History: In the 19th century, this canyon was used as part of the wagon route through Cajon Pass before the modern highways and rail lines were built. Travelers coming down from the Mojave could descend Lone Pine Canyon into Cajon. Later, stage and freight routes sometimes used it, though it was rough and prone to washouts.

Modern day: Today, Lone Pine Canyon Road runs through it, connecting Wrightwood to Cajon Pass and Interstate 15. It’s a steep and winding drive, offering views of the pass and the fault-scarred mountains.

Geological significance: Because it lies right on the San Andreas Fault, the canyon has visible fault scarps and disrupted terrain. Cajon Pass itself is famous as one of the few low crossings of the San Gabriel and San Bernardino ranges, made possible by this major fault line.

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1800s – Native trails Indigenous peoples of the region, such as the Serrano and Cahuilla, used natural passes like Cajon and its side canyons, including Lone Pine Canyon, as travel and trade routes between the desert and the Los Angeles Basin.

1820s–1840s – Early Mexican period Cajon Pass became part of the route of El Camino Real and later the Mormon Road. Lone Pine Canyon served as a steep but direct descent for pack animals and small wagon trains moving between the high desert and the valley.

1851 – Mormon settlers The Mormon Battalion settlers who established San Bernardino passed through Cajon Pass. Lone Pine Canyon was recognized as one of the viable, if rugged, descents on the eastern side.

1850s–1860s – Freight and stage use Freight wagons, mail carriers, and stagecoaches used routes branching into Lone Pine Canyon when conditions allowed. Washouts, steep grades, and fault scarps made it challenging, but it remained part of the regional travel network.

1870s – Railroad surveys The Southern Pacific and later the California Southern Railroad surveyed Cajon Pass. They avoided Lone Pine Canyon itself because its grades were too steep, but its alignment highlighted how the San Andreas Fault had created passages through the mountains.

1880s–1890s – Road improvements Wagon roads were graded through Cajon Pass. Lone Pine Canyon became more of a local connector for ranching and mountain settlement around present-day Wrightwood, though still tied to the larger corridor.

Early 1900s – Automobiles With the rise of autos, Lone Pine Canyon Road developed into a local route. The canyon was narrow and steep, so it was less suitable for heavy traffic compared to the main Cajon routes, but it offered a connection from the mountain communities into the desert.

1930s–1950s – Wrightwood growth As Wrightwood grew as a resort town, Lone Pine Canyon Road became its eastern lifeline, linking it down into Cajon Pass and toward the freeway system.

1970s–present – Modern highway system Interstate 15 took over the main role of Cajon Pass travel, but Lone Pine Canyon Road remains a scenic, twisting connection from Wrightwood into Cajon. The canyon is also closely watched geologically because it follows the trace of the San Andreas Fault.

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