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Geology of the Golden Gate Headlands - National Park Service

Geology of the Golden Gate Headlands - National Park Service 2025

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The document outlines a free teacher workshop titled 'Dissonant Voices: Dialectics of Place' hosted by the Golden Gate National Recreation Area for middle and high school teachers. Scheduled from July 31 to August 3, 2012, the workshop focuses on various historical topics related to the Golden Gate area, including cultural identity, community resistance, and significant historical events. It aims to enhance educators' skills in using historic resources for inquiry-based learning and critical thinking in the classroom. Participants can receive a stipend and CEUs, with an application process that includes a refundable fee.

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Begin by entering your name in the designated field. Ensure that you print clearly for easy reading.
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Indicate the school you are affiliated with and the subjects you teach to help us understand your background.
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What is the geology of the Marin Headlands?

The Marin Headlands contains abundant exposures of a rock of biological origin, radiolarian chert. Over eons, innumerable skeletons of this tiny phytoplankton slowly rained down to the ocean floor to form the chert layers that underlie about half of the Marin Headlands.

What is the geology of Fort Funston?

Fort Funston sits on a bluff made up of soft, sedimentary rocks that are part of the Merced Formation, a sedimentary deposit formed in a basin along the San Andreas fault during the Ice Ages of the last three million years.

What is the geology of Golden Gate park?

Most of the basement rocks in the park belong to the Franciscan Complex. These rocks were originally deposited in a marine environment in a sequence beginning with basalt and greenstone, followed by chert and limestone, and finally graywacke sandstone and shale.

What is the geology of the Arches National Park?

The vast majority of arches in Arches National Park are within the Entrada Sandstone, including at Devils Garden and Klondike bluffs. Grains in the Entrada Sandstone are nearly spherical, creating a very porous (full of tiny spaces) rock.

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