Q1. Which of the following statements best explains the process of soilfluction, its geographic occurrence, and its geomorphic implications, particularly in periglacial and high-latitude environments?
- (a) Soilfluction is a type of chemical weathering in tropical regions where downward movement of clay minerals occurs due to intense leaching under high rainfall.
- (b) Soilfluction refers to the slow, gravity-driven movement of water-saturated regolith over impermeable permafrost layers in periglacial regions, forming lobate structures and contributing to solifluction terraces on gentle slopes.
- (c) Soilfluction is the rapid downslope movement of rock and debris caused by seismic shaking in arid mountainous regions, typically resulting in talus cones and debris aprons.
- (d) Soilfluction occurs exclusively in volcanic terrains where lava alters soil cohesion, triggering landslides with high speed and deep incision.
Answer & solution
Answer: (b) Soilfluction refers to the slow, gravity-driven movement of water-saturated regolith over impermeable permafrost layers in periglacial regions, forming lobate structures and contributing to solifluction terraces on gentle slopes.
Solifluction (Latin solum = soil, fluere = to flow; the paper prints it as "soilfluction") is the slow flow of water-logged soil down a slope under gravity.
In periglacial regions the summer thaw wets only the top active layer while the permafrost beneath stays frozen and impermeable, so the saturated layer creeps downhill even on gentle slopes of 2 to 5 degrees, leaving lobes, terraces and sheets.
Revision note — Mass movements
• Mass movement (mass wasting) is the downslope transfer of rock and soil under gravity alone, without a transporting agent such as a river or glacier; water reduces friction and is the usual trigger.
• Slow movements: soil creep (imperceptible, tilted fences and bent tree trunks), solifluction (saturated soil over permafrost, periglacial zones), rock creep and talus creep.
• Rapid movements: earthflow, mudflow (volcanic mudflows are called lahars), debris avalanche.
• Landslides: slump (backward rotation of the sliding block), debris slide, rockslide (affects material to considerable depth), rockfall (free fall from a cliff, builds talus or scree cones).
• Periglacial means the zone bordering glaciers, with ground that freezes and thaws — Siberia, Alaska, northern Canada, Tibet; its Koppen climate type is ET (tundra), with permafrost and mosses and lichens.
• Related periglacial features: patterned ground (stone polygons), pingos, thermokarst from thawing permafrost.
Do not mix these up
• Solifluction vs soil creep — both are slow, but solifluction needs saturation and a frozen impermeable layer; creep needs neither.
• Solifluction vs mudflow — solifluction moves a few centimetres a year; a mudflow is a rapid, channelled flow after heavy rain or an eruption.
Also asked from this topic: the landslide type with backward rotation of the slipping material (slump); the landslide type that affects material to considerable depth (rockslide); the Koppen climate with permafrost soil and mosses and lichens (ET, tundra).