Seal Rocks (San Francisco, California)

Seal Rock (or Seal Rocks) is a group of small rock formation islands in the Lands End area of the Outer Richmond District in western San Francisco, California. They are located just offshore in the Pacific Ocean, at the north end of the Ocean Beach, near the Cliff House and Sutro Baths ruins.

For other places with the same name, see Seal Rock (disambiguation).
Seal Rocks
The Seal Rock and Cliff House.
Seal Rocks
Seal Rocks
Seal Rocks
Seal Rocks
Geography
LocationNorthern California
Coordinates37.77826°N 122.51636°W / 37.77826; -122.51636[1]
Adjacent bodies of waterPacific Ocean
Administration
State California
CountySan Francisco
CitySan Francisco
"Sea Lion Rock, Cliff House" photograph circa 1868 by Carleton Watkins.
Perhaps by Alexander Gardner, 'Seal Rocks' in Pacific Ocean, near San Francisco, from Across the Continent on the Kansas Pacific Railway, 1869.
Seal Rocks, Cliff House, San Francisco, California.

The name is derived from the population of Steller's sea lions (Eumetopias jubatus) and California sea lions (Zalophus californianus), who haul out on the rock. Both species are often colloquially called "seals". The formations and wildlife are protected within the Golden Gate National Recreation Area.

Geology

Near the end of the last ice age, this part of the coastline was thought to be between eight and twenty five miles westward of its current position - around five thousand years ago, with the melting of the ice, the sea level rose to its current level.

The coastal features found here today were formed by the actions of waves, wind, and the movement of sand. The geology of this part of the coastline of San Francisco consists of steep rocky cliffs which are punctuated by narrow sandy pocket beaches found at the north end of the city and long sandy stretches at Ocean Beach and Fort Funston to the south. The local features, and indeed the entire San Francisco Peninsula, come from the northern aspect of the Santa Cruz Mountains. Before the urban development seen today, the area landward of Ocean Beach consisted of barren sand fields inland to Twin Peaks. The first known map of the area, dating from 1852, was made by the U.S. Coast and Geodetic Survey and describes the coastline here as being entirely unaltered by humans.

The geologic layers beneath Ocean Beach, starting from the top (i.e. the youngest), are:

  • Placed fill, from various construction activities over the last 100 years or so. The depth of this placed fill varies, but in 1985 it was then estimated to be between 7 to 16 feet (2.1 to 4.9 m) deep.
  • Dune sands, estimated to be 13 to 26 feet (4.0 to 7.9 m) deep.
  • Colma Formation
  • Merced Formation
  • Bedrock. The depth to bedrock is estimated to be between 350 to 400 feet (110 to 120 m).

The Colma and Merced Formations consist generally of poorly-sorted sandy deposits, probably deposited during some earlier period of greater sea levels. The Colma Formation is found under the dune sands and also extends inland.

See also

References
  1. U.S. Geological Survey Geographic Names Information System: Seal Rocks
  • U.S. Geological Survey Geographic Names Information System: Seal Rocks (San Francisco, California)
  • Martin, James A.; Lee, Michael T. (2006). The Islands of San Francisco Bay. San Rafael, CA: Down Window Press. ISBN 0-9787241-0-0.

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