Image by Flickr.com, courtesy of Hamed Saber
Freeze-thaw weathering occurs in both mountain and hot desert areas. The freeze-thaw process causes the breakdown of rock material.
Function
Image by Flickr.com, courtesy of Sergio Tudela Romero
Freeze-thaw begins when water enters the cracks in bare rock. During night freezes, the frozen water expands against the rock. When temperatures rise, the ice melts and this causes more room for new water to enter. Over time, the expansion and contraction of water breaks the rock
Water Force
Image by Flickr.com, courtesy of Kevin Dooley
Water in its liquid state has 10 perecent less volume than its frozen state.The power of freezing and thawing water literally can move mountains.
Sand from Rock
Image by Flickr.com, courtesy of John Morgan
Rain in warm temperatures fills rock spaces. Cold night freezes expand the water. Breakdown begins.
Power of Time
Image by Flickr.com, courtesy of Sherrie Thai
Repeated cycles of freeze-thaw over long periods of time cause the change from mountain to sand material.
Breakdown of Matter
Image by Flickr.com, courtesy of Steve Jurvetson
Freeze-thaw results are identified by clean and straight breaks in rock.
Effects
Rocks, caves, sand, potholes and scree (piles of broken rock) are results of the freeze-thaw process
Most recent
- Image by Flickr.com, courtesy of Hamed Saber