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The black star within the red area shows where the later Pilot Ridge debris flow occurred.
Fig. 2 A detailed map for the area affected by the Pilot Ridge debris flow in 1997.
The maximum velocity measured for the Pilot Ridge debris flow was about half the average for other debris flows in the Sierra Nevada (DeGraff, 1994).
The Pilot Ridge debris flow represents a later post-fire debris flow occurrence in a forested terrain and its destructive effects demonstrate the need for mitigation.
The Pilot Ridge debris flow initiated from two locations about 180 m apart at the bifurcated headwaters channel for this small drainage basin (DeGraff, 1997) (Fig. 2).
Fig. 4 Two close up views of roots exposed in the east slide plane where the Pilot Ridge debris flow initiated.
The upper part of the north-facing drainage basin where the Pilot Ridge debris flow initiated was within the area burned by the 1987 Stanislaus Complex Wildfire.
The first case study of the Pilot Ridge debris flow considers the factors resulting in this event and illustrates the hazard posed even in a sparsely inhabited area.
One, known as the Pilot Ridge debris flow, occurred during the 30 minutes prior to 1 00 PM on January 2 , 1997(DeGraff, 1997) (Fig. 2).
The Pilot Ridge debris flow also illustrates how damage can take place within the source area, transport zone, and deposition zone of a debris flow (Hungr et al., 1987).
The Stanislaus Complex wildfire and the subsequent Pilot Ridge debris flow is representative of a later post-wildfire debris flow occurrence in a forested terrain (DeGraff et al., 2015).
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