La Laguna de Chico Lopez

Francisco “Chico” Lopez was an early Californio rancher whose name became attached to what is now Elizabeth Lake, once widely known as La Laguna de Chico Lopez.

He was part of the Lopez family that held long-standing land and grazing rights in the western Antelope Valley during the Mexican and early American periods of California. The Lopez holdings were associated with the Rancho San Francisco grant, centered near present-day Newhall. Still, their herds often ranged north and west into the Sierra Pelona and Antelope Valley foothills.

By the 1840s, Chico Lopez was running sheep and cattle in the region surrounding the lake. Travelers and surveyors used his name to identify the landmark—“Chico Lopez’s Lake” or “La Laguna de Chico Lopez.” The lake served as a watering stop along the early trails crossing the San Andreas rift zone between Soledad Canyon and the Antelope Valley.

Later, as American settlers arrived in the 1860s and 1870s, the Lopez name persisted in maps and local speech until the site was renamed Elizabeth Lake. The renaming is attributed to surveyor Benjamin Davis Wilson (Don Benito Wilson), who supposedly named it for a relative or acquaintance during his expeditions through the area.

Though details of Chico Lopez’s later life are scarce, his legacy survives in the early place-name and in the transition from the Californio ranching era to the American homesteading period in the western Mojave frontier.

Elizabeth Lake

Silver Road

Borax Road

Tejon Pass

Fort Tejon Road

Don Benito Wilson

Tiburcio Vasquez

Tejon Ranch (Winter)

Rainbow Basin Geology

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Rainbow Basin

Rainbow Basin is a geological formation in the Mojave Desert of California. It is known for its unique and colorful rock formations, which provide valuable insights into the region’s geological history. Here are some key aspects of the geology of Rainbow Basin:

  1. Sedimentary Rocks: Rainbow Basin primarily comprises sedimentary rocks accumulated over millions of years. These rocks include sandstones, shales, and mudstones. The different layers of sedimentary rocks represent different periods of geological history.
  2. Fossilized Marine Life: Within the sedimentary rocks of Rainbow Basin, fossils of marine life from the Miocene epoch (approximately 15-20 million years ago) have been found. These fossils include shells, bones, and other remnants of ancient sea creatures. This suggests that a shallow sea once covered the area.
  3. Faulting and Uplift: The geology of Rainbow Basin has been influenced by tectonic forces. The region is situated near the intersection of several fault lines, including the Garlock Fault. These fault movements have caused the uplift of the rocks, exposing them to erosion and creating the unique landscape seen today.
  4. Erosion and Weathering: Over time, erosion and weathering have shaped the colorful rock formations in Rainbow Basin. These processes have created intricate patterns and exposed layers of colored sediments, giving the area its name.
  5. Geological Time Scale: The rocks at Rainbow Basin span a significant portion of the geological time scale, providing geologists with valuable information about the changing environments and life forms that existed in the area millions of years ago.
  6. Geological Tours: Rainbow Basin is a popular destination for geological enthusiasts and tourists interested in its unique geology. There are guided tours and interpretive exhibits that provide insights into the geological history of the area.
Rainbow Basin photo
Rainbow Basin, Barstow, Ca.

In summary, Rainbow Basin is a geological wonder in the Mojave Desert, characterized by its sedimentary rocks, fossils, faulting, erosion, and vibrant colors. It offers a glimpse into the geological history of California and the forces that have shaped its landscape over millions of years.

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