külmumissulatumine

Külmumissulatumine, also known as freeze-thaw weathering or cryo-weathering, is a geomorphic process that occurs when water penetrates cracks and pores in rocks or soil. When the temperature drops below freezing, the water turns into ice, expanding in volume. This expansion exerts pressure on the surrounding material, widening existing cracks or creating new ones. As temperatures rise above freezing, the ice melts, and the water can penetrate deeper into the newly formed or enlarged openings. This cycle of freezing and thawing, repeated over time, can lead to the disintegration and breakdown of rocks and soil into smaller fragments.

The effectiveness of külmumissulatumine depends on several factors. The presence of water is essential, making the process more prevalent in regions with significant precipitation or frost events. The rate at which temperatures fluctuate around the freezing point is also important; frequent freeze-thaw cycles accelerate the process. The type of rock or soil also plays a role, with porous materials being more susceptible to water infiltration and subsequent ice formation. This weathering process is a significant contributor to the formation of talus slopes, frost-shattered landscapes, and the breakdown of building materials in cold climates. It is a natural mechanism that shapes the Earth's surface.