Author Question: What are some important clues that indicate that a slope has experienced landslide activity in the ... (Read 34 times)

yoroshambo

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What are some important clues that indicate that a slope has experienced landslide activity in the
  distant past? What will be an ideal response?



Question 2

Why do the rainfall thresholds for debris flows and landslides for California semiarid regions and
  Contra Costa and Marin Counties in Central California vary? What will be an ideal response?




fraziera112

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Answer to Question 1

Landslide areas commonly have irregular (hummocky) terrain, depressions with or without standing
water, amphitheater-like overall shape, an absence of through-going stream channels, concentrations of
water-loving plants, and spring lines along their margins. These features stand out in contrast to
adjacent hill slope areas. In a broad sense, landslide affected slopes are flatter than surrounding areas.
Ironically, this has attracted development in some areas because of reduced grading costs



Answer to Question 2

Semiarid areas have little vegetation and abundant loose surface debris. There are few root systems to
retain the weak soils. Less rainfall Intensity/duration is needed to start a debris flow or landslide. The
differences between Contra Costa and Marin Counties are due to topography (Marin is steeper) and
geology (Marin has less cohesive rock).




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