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Santa Monica Mountains National Recreation AreaFinding your way is not always easy. But, wildlife biologists are studying the ways animals find their way in this urban mtn range.
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Santa Monica Mountains National Recreation Area
Geologic Formations
 

 

Each year, thousands of people hike to the highest point in the Santa Monica Mountains—Sandstone Peak (3111’). Sandstone, however, is a sedimentary rock made of marine deposits and other sediments. This peak has very different origins.

Imagine standing on the shores of Malibu 24 million years ago. The dinosaurs are long gone, but the Santa Monica Mountains are yet to be born. Broad plains extend from the middle of California to the coast. Much of the land that makes up the Los Angeles area is underwater.

For millions of years, the ground slowly moves, churns, and presses until the Earth begins to crack and molten lava oozes from underwater vents. Thus, only 15 million years ago, the Santa Monica Mountains and Channel Islands began to glimmer in the ocean depths.

In time, the eruptions became explosive and burst through the water’s surface. For another 3 million years, the mountains continued to grow to over 10,000 feet high. Three times taller than they are now! The elements of wind and rain peal away this surface creating the beaches and valleys we know today.

You can download a map of the Geological History Overview of the Santa Monica Mountains area. (PDF)

– Judy Lively, NPS Park Ranger and Mike Theune, Geology Intern

Sue Nelson, Jill Swift, and Margo Feurer were instrumental in the movement to create a national recreation area near Los Angeles.  

Did You Know?
Four state parks were the triumph of a grassroots movement to protect open spaces minutes from Los Angeles in the 1950s & 60s. Three women, Sue Nelson, Jill Swift, and Margo Feuer further galvenized the movement that helped make Santa Monica Mountains National Recreation Area a reality in 1978.

Last Updated: December 30, 2007 at 15:19 EST