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Glendale (PDF) - Hazard Mitigation Web Portal - State of California

Glendale (PDF) - Hazard Mitigation Web Portal - State of California

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Natural <strong>Hazard</strong>s <strong>Mitigation</strong> PlanCity <strong>of</strong> <strong>Glendale</strong>, <strong>California</strong>Section 6 – EarthquakesHollywood Fault: The Hollywood fault is the eastern 9-mile (14 km) long segment <strong>of</strong> the SantaMonica – Hollywood fault system that forms the southern margin <strong>of</strong> the Santa Monica Mountains(locally known as the Hollywood Hills). It has also been considered the westward extension <strong>of</strong> theRaymond fault. From east to west, the fault traverses the Hollywood section <strong>of</strong> Los Angeles, and thecities <strong>of</strong> West Hollywood and Beverly Hills. Its eastern end is mapped immediately south <strong>of</strong><strong>Glendale</strong>’s southern boundary (see Map 6-1 and Plate H-4). Movement on the Hollywood fault overgeologic time is thought responsible for the growth <strong>of</strong> the Hollywood Hills, which is why earlierresearchers characterized this fault as a northward-dipping reverse fault. However, recent studies byDolan et al. (1997, 2000a) and Tsutsumi et al. (2001) show that the Hollywood fault is primarily aleft-lateral strike-slip fault. A lateral component <strong>of</strong> movement on this fault is consistent with itslinear trace and steep, 80- to 90-degree dips (reverse faults typically have irregular, arcuate tracesand shallow dips).2006 PAGE 6 - 22

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