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      • A crack in a rock can fill with water which then freezes as the temperature drops. As the ice expands, it pushes the crack apart, making it larger. When the temperature rises again, the ice melts, and the water fills the newer parts of the crack.
      www.ssc.education.ed.ac.uk/BSL/geography/freezethawd.html
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  2. Freeze-thaw weathering is a fascinating natural process that shapes our landscapes by the power of freezing and thawing water. In this blog post, we will delve into the mechanics of freeze-thaw weathering, its effects on rocks and structures, and its significance in geological processes.

  3. Jul 5, 2020 · Freeze-thaw weathering occurs when rocks are porous (contain holes) or permeable (allow water to pass through). Water enters the rock and freezes. The ice expands by around 9%. This causes pressure on the rock until it cracks. Repeated freeze-thaw can cause the rock to break up. Find out more about weathering. Share this entry.

  4. Freeze-thaw weathering occurs when rocks are porous (contain holes) or permeable (allow water to pass through). Water enters cracks in the rock. When temperatures drop, the water freezes and...

  5. Revision notes on 2.2.2 Weathering Processes for the AQA A Level Geography syllabus, written by the Geography experts at Save My Exams.

  6. Freeze-thaw weathering (Also called frost-shattering) - It occurs in cold climates when temperatures are often around freezing point and where exposed rocks contain many cracks. Water enters the cracks during the warmer day and freezes during the colder night.

  7. Jun 6, 2024 · Freeze-thaw (frost shattering) weathering - this happens when water enters cracks in the rock. At night when the temperature plummets the water can freeze, which makes the water expand, putting pressure on the rock, making the crack bigger. When the ice thaws the pressure on the rock is relieved.

  8. Definition: Freeze-thaw weathering is a process of erosion that happens in cold areas where ice forms. A crack in a rock can fill with water which then freezes as the temperature drops. As the ice expands, it pushes the crack apart, making it larger.

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