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Salt Point State Park

Salt Point State Park
Gerstle Cove
Location Sonoma County, California, USA
Coordinates
Area 6,000 acres (2,400 ha)
Governing body California Department of Parks and Recreation

Salt Point State Park is a camping, fishing, scuba diving and many others. The weather is cool with fog and cold winds even during the summer.

The rocks of Salt Point are sedimentary sandstone. Due to the large amounts of sandstone, small cave-like features called tafoni can be found along the shore of Salt Point.

Contents

  • Cultural and natural history 1
    • Gerstle Cove 1.1
  • Wildlife 2
    • Land 2.1
    • Marine 2.2
  • Geology 3
    • Rocks 3.1
    • Deep-sea fans 3.2

Cultural and natural history

This park is named for the formation of salt crystals in the cracks and crevices of the rocky coastline. The native Kashaya Pomo collected salt from this area for many years. They used abalone chisels to scrape the salt off the rocks.

In 1853, Samuel Duncan and Joshua Hendy built a sawmill on a ridge located above Salt Point. A couple of years later they leased the land to a San Francisco company which quarried the sandstone. They used the sandstone to create the streets and buildings in San Francisco along with the naval facility at Mare Island. It is also possible to see drill holes in the sandstone at Gerstle Cove and at the marine terrace just north of it. In 1870, Duncan sold his property to Frederick Funcke and Lewis Gerstle. They shipped 5,000 cords of wood yearly and used most of the land to graze their cattle.

Gerstle Cove

The eyebolts used to anchor ships down are still visible at Gerstle cove. This is where sandstone and wood were loaded onto cargo ships. At first, they used wire cables anchored to the cliff side to load wood and stone onto the ships. Two chutes were eventually made; the Miller chute and the Funcke & Co. chute. There was a horse-drawn railroad that lead from the Miller sawmills to where the boats were loaded. The sawmill had a daily capacity of 18,000 board feet (42 m3).

Wildlife

Land

Bishop pine at Salt Point

Brush and grasslands cover the ground on the marine terraces; at higher elevations (approximately 100 to 300 feet (30 to 91 m) in elevation) Douglas fir forest dominates. At slightly higher staircase levels (about 300 to 500 feet (91 to 152 m)), a mixed fir forest of bishop pine and Douglas-fir is present intermixed with second growth coast redwood, madrones and tanoak. At 1,000 feet (300 m) there is a large open prairie where animals such as elk previously grazed. In addition, at an elevation of about 550 feet (170 m) within Salt Point State Park is a pygmy forest including the Mendocino cypress, bishop pine and Arctostaphylos. The reason these trees do not attain their normal height is due to the highly acidic soils with minimal nutrients and a hardpan layer close to the surface.

The native animals that roam the land include the black-tailed deer, raccoon, coyote, bobcat, gray fox, badger, striped skunk, and dozens of varieties of rodents such as squirrels, chipmunks, and the field mouse. Bears and cougars occasionally range the area, although visitors rarely see them.

The forest, grassland, and ocean shore area host a huge variety of birds, including pelicans, ospreys, woodpeckers (including the pileated woodpecker), and oystercatchers. Steller's jay and ravens are common in unattended campsites in search of food.

Marine

tide pools
During April, abalone. It takes this abalone 10 years to reach a diameter of seven inches (178 mm). Between the months of December and April, it is possible to see gray whales migrating south to Baja California for breeding.

Stewarts Point State Marine Reserve & Stewarts Point State Marine Conservation Area, Salt Point State Marine Conservation Area and Gerstle Cove State Marine Reserve adjoin Salt Point State Park. Like underwater parks, these marine protected areas help conserve ocean wildlife and marine ecosystems.

Geology

The coast in this park is lined with jagged rocks and steep ocean cliffs. The rocks are shaped and formed by the continuous crashing of the waves. These rocks provide an array of tide pools while the tide is out.

Rocks

Sandstone with tafoni
The rocks of Salt Point are sedimentary, mainly sandstone. All of these rocks are tilted, exposing older rocks. The rocks at the north end of the park's coast are younger than the rocks at of the southern end. Salt Point is named for the tafoni where the ocean water crystallizes in the honeycomb like crevices. This tafoni is caused when the salt crystals interact with the sandstone making parts of the sandstone harden while other parts soften.

Deep-sea fans

The layers of sedimentary rock show evidence of a deep-sea fan. A deep-sea fan is caused when there is dense, turbulent sediment filled water flowing down a submarine canyon. This highly dense water is called a turbidity current. Something that may cause a turbidity current are earthquakes or storms that create a submarine slide. When this sediment filled water leaves the end of the canyon it spreads out in a fan like shape. The sediment is thinner and thinner the farther away the sediment is from the submarine canyon. All of these layers of sedimentary rock are created thousands of feet below the ocean’s surface but now the layers are visible above the surface of the water. This is because the Pacific plate and the North American plate are moving against each other; since the oceanic plate is lower, it is being forced below the continental plate in a process called subduction. While the oceanic plate is being subducted, the continental plate is scraping off the top layers of the oceanic plate slowly bringing them to the

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