• Join over 1.2 million students every month
  • Accelerate your learning by 29%
  • Unlimited access for just £4.99 per month

Types of Weathering

Page
  1. 1
    1
  2. 2
    2
  • Essay length: 589 words
  • Submitted: 24/05/2012
Share this essay:
GCSE Physical Geography

The first 200 words of this essay...

Weathering

Weathering is when rocks start to break or decay which is caused by nature like acidic rain or the change of temperature.

Freeze Thaw Weathering

Freeze Thaw weathering is a physical (also know as mechanical weathering) weathering which cracks parts of the rocks. Physical weathering is when it breaks a rock without chemicals. Freeze Thaw weathering is also known as frost shattering because of it's actions as when water leaks into a crack in a rock, the water can freeze in night and thaw in the morning as you can see on the diagram on the right which explains this. The temperature has to constantly rise and decrease or this process will fail as the repetition of this process is what that breaks the rock. As the water freezes in the night the rock will expand which creates stress on the rock (also because of the minerals expanding in different rates) which will make the cracks wider and wider. Soon the temperature will rise and therefore the ice will thaw making the water go more into the rock as the cracks gets wider and the rock contracts. After the this repetitive process keeps going on

Read more
The above preview is unformatted text

Found what you're looking for?

  • Start learning 29% faster today
  • Over 150,000 essays available
  • Just £4.99 a month

Marked by a teacher

This essay has been marked by one of our great teachers. You can read the full teachers notes when you download the essay.

Peer reviewed

This essay has been reviewed by one of our specialist student essay reviewing squad. Read the full review on the essay page.

Peer reviewed

This essay has been reviewed by one of our specialist student essay reviewing squad. Read the full review under the essay preview on this page.