Frost Wedging: How Ice Splits Rock — Reading Comprehension

Frost wedging (or freeze-thaw weathering) is a mechanical weathering process where water seeps into cracks in rocks, freezes, and expands—prying the rock apart over time. This powerful force shapes mountains, cliffs, and landscapes in cold or temperate regions.

How It Works

1. Water Enters Cracks: Rain or meltwater fills fractures in bedrock.
2. Freezing Expansion: When temperatures drop, water freezes and expands by 9%, exerting pressure (up to 2,100 kg/cm²).
3. Rock Fractures: Repeated cycles widen cracks until chunks break off.

Key Features

●       Climate Dependence: Most effective where temperatures fluctuate around 0°C (32°F).

●       Rock Type: Works best in porous rocks (sandstone, granite) with many cracks.

●       Resulting Landforms: Creates talus slopes, jagged peaks, and shattered boulders.

Examples

●       Alpine Mountains: Frost wedging sculpts the Matterhorn’s steep faces.

●       Potholes in Roads: The same process damages asphalt in winter.

●       Mars: Frost action may contribute to rock breakdown in polar regions.

Frost wedging is a key part of the rock cycle, breaking down bedrock into sediment. Understanding it helps predict erosion risks and landscape evolution.

Fun Fact: Water is the only common substance on Earth that expands when it freezes, increasing by about 9% in volume! This unique property makes frost wedging powerful enough to split boulders weighing several tons and even crack engine blocks when radiator fluid freezes.

What is the first step in frost wedging?

How much does water expand when freezing?

Which climate is ideal for frost wedging?

What landform does frost wedging create?

Why is granite vulnerable to frost wedging?

Where is frost wedging not a major force?

How does frost wedging affect humans?

What planetary body shows frost weathering?