Santa Lucia Range

The Santa Lucia Mountains are part of the Outer South California Coast Ranges, in the Pacific Coast Ranges System. The coastal side of the range rises directly from the shoreline, with oceanfront ridges rising directly 4,000 to 5,000 feet (1,200 to 1,500 m) to the crest of the coastal range. The crest of the range is never more than 11 miles (18 km) from the coast.[2]^: 11 Cone Peak is the steepest coastal elevation in the contiguous United States,[3] rising nearly a mile (1,609 m) above sea level, only three miles (5 km) from the Pacific Ocean.

The range's northern section runs parallel to the southern section of the Diablo Range, part of the Inner South Coast Ranges, which lies to the east across the Salinas Valley. The range's highest summit is Junipero Serra Peak, 1,784 metres (5,853 ft) in Monterey County and the Los Padres National Forest.[4]

The first European to document the Santa Lucias was Juan Rodríguez Cabrillo in 1542 while sailing northward along the coast on a Spanish naval expedition. Cabrillo originally named the southern portion of the range the Sierras de San Martín, as he was passing the area on November 11, the feast day for Saint Martin. He named the northern part Sierras Nevadas because there was snow on it.[9]

The present name for the range was documented in 1602 by Sebastián Vizcaíno, who had been tasked by the Spanish to complete a detailed chart of the coast. Passing by the range around December 14, he named the range Sierra de Santa Lucia in honor of Saint Lucy of Syracuse, for whom many Christians celebrate a feast day on December 13.[9]

The first European land exploration of Alta California, the Spanish Portolá expedition, camped on the coast near Ragged Point in present-day San Luis Obispo County on September 13, 1769. The expedition was forced to bypass the inaccessible coast and travel inland through the San Antonio Valley. The rough trail required much improvement by the scouts, and it was September 24 before the party emerged from the mountains at the San Antonio River near today's settlement of Jolon.[10] They traveled north through the Salinas Valley before arriving at Monterey Bay, where they founded Monterey and named it their capital.[11]

Junipero Serra Peak

The rock of the Santa Lucias is dominated by granitic basement of the Salinian Block, between the San Andreas Fault and Sur-Nacimiento Fault. The core of the Salinian block formed as part of the same batholith which forms the core of the Sierra Nevada Mountains and the Peninsular Ranges of Baja California. It was separated from the North American Plate and transported north by the action of the San Andreas Fault from an original position. It is predominantly Mesozoic granitic and pre-Cretaceous metamorphic rocks. There is some Cretaceous sedimentary rock of the Great Valley Sequence, considerable Miocene marine sediments, and some other Cenozoic sediments. Units west of the Sur-Nacimiento Fault are dominated by rocks of the Franciscan Assemblage.

The basement rocks of the Santa Lucia Range contain Mesozoic Franciscan and Salinian Block rocks.[15] The Franciscan complex is composed of greywacke sandstone and greenstone, with serpentinite bodies and other Ultramafic rocks present. Small areas of marble and limestone lenses form resistant outcrops that are prominent landscape features, often white to light gray in color. The Salinian block is made up of highly fractured, and deeply weathered meta-sediments, especially biotite schist and gneiss, intruded by plutonic (granitic) rocks such as quartz diorite and granodiorite. Both formations have been disrupted and tectonically slivered by motion on the San Andreas and associated fault systems. The Palo Colorado and Church Creek faults are prominent features influencing the linear northwest–southeast alignment of primary drainages.[15]

The Palo Colorado-San Gregorio fault system transitions onshore at Doud Creek, about 7 miles (11 km) south of Point Lobos,[16] exposing the western edge of the Salinian block. Stream canyons frequently follow the north-westerly trending fault lines, rather than descending directly to the coast. The Salinian block is immediately south of the Monterey Submarine Canyon, one of the largest submarine canyon systems in the world, which is believed to have been an ancient outlet for the Colorado River.[16]^: 14

The region is also traversed by the Sur-Hill fault, which is noticeable at Pfeiffer Falls in Pfeiffer Big Sur State Park. The 40 feet (12 m) waterfall were formed when the stream flowed over the hard gneiss of the Salinian block and encountered the softer Santa Margarita Sandstone. The falls were formed when the softer sandstone was worn away.[17]^: 325 The interior canyons are typically deep and narrow, and even in the summer sunshine only reaches many of the canyon bottoms for a few hours. The land is mostly steep, rocky, semi-arid except for the narrow canyons, and inaccessible. The Little Sur River canyon is characteristic of the Ventana Wilderness region: steep-sided, sharp-crested ridges separating valleys.[18] At the mouth of the Little Sur river are some of the largest sand dunes on the Big Sur coast.[17]^: 355

About 50 streams flow out of the mountains into the sea. A few of them, including the Big Sur and Little Sur Rivers, Big Creek, Garrapata Creek, and Salmon Creek, are large enough to support anadromous and resident fish.[19]^: 5

California State Route 1 runs along the Big Sur coast on the coastal slopes of the range, while U.S. Route 101 lies in the Salinas Valley to the East, and crosses the southern Santa Lucia Range over Cuesta Pass to reach San Luis Obispo. The only other road across the Santa Lucia Range is Nacimiento-Fergusson Road, connecting Lucia to Jolon.[20]

Since at least the 1930s, accounts of encounters with Dark Watchers or Los Vigilantes Oscuros have been associated with the Santa Lucia Range, described as shadowy figures which watch hikers from atop mountain ridges.

The Lost Padre Mines of the Carmel Mission have become part of local folklore, with their legacy recounted through various accounts, including those within Randall Reinstadt's works such as Ghosts, Bandits, and Legends of Old Monterey, Carmel and Surrounding Areas and Tales and Treasures of California Missions. These narratives suggest that indigenous communities held knowledge of abundant gold deposits concealed within the untamed terrain of the Santa Lucia Mountains. As legends of these riches were passed down over time, the Lost Padre Mines attracted attention. Versions of these legends appear to have originated from long-time residents of Carmel Valley. The stories if ghosts may be attributed to descendants of and the last residents of the native people who remained hidden deep in the mountains after the missions failed.[21][22][23]

Pacific Southwest Airlines Flight 1771 crashed in the mountains near Cayucos on December 7, 1987 after a gunman killed both pilots, causing the aircraft to crash. A total of 43 people were killed with no survivors.

• Tierra Redonda Mountain

Wikimedia Commons has media related to Santa Lucia Mountains (California).

• Los Padres National Forest — Monterey Ranger District
• Ventana Wilderness Alliance