Correct option is D
Solifluction is a slow type of mass movement that occurs in regions with permafrost or seasonal freeze-thaw cycles. It involves the gradual downslope movement of water-saturated soil due to gravity. Since it progresses slowly over time, it does not fall into the category of fast mass movements like rockfalls, mudflows, or slumps.
Information Booster:
- Solifluction is common in cold climates where the ground remains frozen for much of the year.
- The top layer of soil moves downslope when thawed, while the frozen lower layer prevents drainage.
- It leads to the formation of lobate (tongue-shaped) or sheet-like structures on slopes.
- It is different from landslides or mudflows, which are rapid.
- Solifluction occurs in tundra regions and high-altitude areas.
- Human activities like deforestation can accelerate this process by reducing soil stability.
Additional Knowledge:
(a) Rock Fall: This is a fast mass movement where rocks or debris fall freely from a cliff or steep slope due to gravity. It occurs suddenly and is one of the fastest types of mass movement.
(b) Mud Flow: A very rapid flow of water-saturated soil and debris down a slope. It is common in volcanic eruptions (lahars) and heavy rainfall areas.
(c) Bed Rock Slump: A moderately fast type of mass movement where a section of bedrock or soil moves downslope along a curved surface, often due to water saturation and weak rock layers.