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Cover of the Geologic Resources Inventory report for Golden Gate, with a photograph of the bridge.

The Golden Gate Geologic Resources Inventory report, which covers Muir Woods. Image from the NPS Geodiversity Atlas

Muir Woods National Monument (MUWO) lies a few miles northwest of San Francisco in Marin County, California.

ProclaimedJanuary 9, 1908
Sizeabout 224 hectares (554 acres)
Protectsthe last remnant of old-growth redwood forest near the Bay Area
The treesmore than 76 m (250 ft) tall, averaging 600 to 800 years old; the oldest at least 1,200
Named fornaturalist and writer John Muir, a key advocate of the national park idea
Managedas a distinct unit within Golden Gate National Recreation Area

Its creation is seen as an important moment in early 20th-century American conservation (National Park Service 2016, 2017; Port 2016).

This page is part of the National Park Service's Geodiversity Atlas, a product of the Geologic Resources Inventory. Geodiversity means the whole range of a park's geologic and soil resources and processes — rocks, minerals, sediments, fossils, landforms and the processes that shape them — and the atlas supports education, geoconservation, and management that treats the living and non-living parts of an ecosystem together.

Hikers in a redwood forest.

Hikers among the redwoods. Image from the NPS Geodiversity Atlas

The rocks

The monument's bedrock is entirely the Franciscan Complex, of Jurassic to Eocene age — a varied suite of rocks formed in an ancient subduction zone off the western coast (Elder 2013).

  • How: as the oceanic Farallon Plate converged with the continental North American Plate, some Franciscan rocks were sheared and faulted into mélange — French for "mixture" — broken blocks from a few meters (yards) across to many square kilometers (miles) (Sloan 2006).
  • Mélange — soft and sheared — is the monument's main bedrock; around the Bay Area it forms rounded hills among tougher Franciscan rocks.
  • Chert and metachert form a large, fault-bounded block in the monument's far east, surrounded by mélange.
  • Quaternary alluvium lines lower Redwood Creek.

Muir Woods belongs to the Pacific Border physiographic province and shares its geologic history and some of its formations with a region much larger than the monument.

Maps, reports and data

Geologic map of Muir Woods National Monument.

Geologic Resources Inventory map of Muir Woods. Image from the NPS Geodiversity Atlas

The Geologic Resources Inventory produces digital geologic maps and reports for more than 270 natural resource parks, and many products are still in progress:

ProductWhat it is
Scoping summariesrecords of meetings where park staff and local geologists set the mapping plan and the report's contents
Digital geologic mapsGIS files, a user guide and supporting map information; newer ones add Google Earth data and online map services
Reportsthe park's setting and significance, notable features and processes, management issues, and geologic history, built on the maps
Postersa PDF view of the GIS data; newer ones add aerial imagery or shaded relief. Included with the reports
Projectsthe basics of the program and every product for a park

Aerial photograph of Muir Beach and the Redwood Creek restoration site.

Muir Beach and the Redwood Creek restoration site from the air. Image from the NPS Geodiversity Atlas

More: Redwood Creek restoration at Muir Beach · park home · geologic time · California Geological Survey

Sources

Based on "NPS Geodiversity Atlas—Muir Woods National Monument, California," National Park Service; a work of the United States government in the public domain.

In these publicationsMuir Woods National Monument

LanguagesEnglish

Licence: CC0 1.0 (public domain) · Adapted from www.nps.gov

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