In an arid, high-altitude alpine environment experiencing diurnal freeze-thaw cycles and torrential seasonal rainfall, angular rock fragments disintegrate from steep granite cliffs and accumulate at the base. Subsequent heavy rainfall saturates these loose debris accumulations, causing them to flow rapidly down a narrow drainage channel. Which combination of physical weathering and mass wasting processes accurately accounts for this sequence of landscape evolution?
- Frost shattering followed by mudflowAnswer
- BHydrolysis followed by soil creep
- CMetamorphic recrystallization followed by rock fall
- DCarbonation followed by solifluction
Answer
The initial mechanical disintegration of granite cliffs is caused by frost shattering (frost wedging), and the subsequent rapid downslope movement of saturated debris along a channel is a mudflow.
The correct response correctly identifies frost shattering as the mechanical weathering process driven by freeze-thaw cycles in high-altitude environments, and mudflow as the rapid movement of water-saturated debris down a defined channel.
Step-by-Step Solution
Key Concept
Interaction of Frost Wedging and Rapid Channelized Mass Wasting
Estimated Time:2m 0s