Mudflows are facilitated by specific conditions and increased water content, making them common in dry regions after heavy rains.
Mudflows are a common form of mass movement after heavy rains in dry regions.
Their occurrence is facilitated by conditions like unconsolidated surface materials, steep slopes, and sparse vegetation, which create a perfect environment for mudflows to develop.
Increased water content from heavy rains significantly contributes to the triggering of mudflows, making them more prevalent in areas with sparse vegetation and heavy rainfall.
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