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Zenger
Zenger
Environment
Martin M Barillas

Mounting Pressure: Slow-Moving Section Of San Andreas Fault Remains A Danger

The San Andreas Fault, visible as the line between grey metamorphic quartz monzonite and brown sedimentary sandstone and siltstone, is seen at Tejon Pass on June 30, 2006, near Gorman, California. The rift of tan and brown layers indicates the site of the surface rupture of a magnitude-8.0 earthquake in 1857 that was the largest quake in California?s recorded history. (David McNew/Getty Images)

The San Andreas Fault in California is creeping slowly but may soon give the country a jolt, similar to the 1906 earthquake that killed 3,000 and leveled San Francisco.

The 800-mile-long fault runs from north to south through California and Mexico, forming the boundary between the North American and Pacific tectonic plates. The two plates grind against each other along the fault, producing seismic events, moving 0.79 to 1.38 inches per year in a process called continental drift.

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