The potholes and caverns formed in limestone by water seeping through limestone bedrock is an example of such weathering.
Biological weathering takes place in moderate temperatures. Abrasion weathering is caused by moving water or wind. That can happen in moderate temperatures.
physical weathering refers to weathering that occurs because of brute force, while chemical weathering refers to weathering that take place because change in the molecular composition of the substance
Striations are "scratches" left in bedrock by glaciers. A small particle of rock, generally pebble sized or smaller, becomes entrained in the base of the glacier and dragged along the surface of the bedrock. These can often be seen on hard bedrock surfaces that are resistant to subsequent weathering after the retreat of the glacier. Erratics are large rocks that are found out of place in the landscape, i.e. not near where they were formed. They are removed from their provenance by a glacier and transported away, before being deposited in a different part or the landscape when the glacier melts.
biological weathering occurs in cool, humid clmates.
In Miami
In Bedrock
Bedrock
Weathering of rocks occur on the outer surface.
About 8~15 blocks above the lowest bedrock you can find. Making a staircase to the bottom of the world, then counting up is recommended.
The breaking down of rocks is weathering. Their movement from one place to another place is erosion.
Biological weathering takes place in moderate temperatures. Abrasion weathering is caused by moving water or wind. That can happen in moderate temperatures.
differential weathering
physical weathering refers to weathering that occurs because of brute force, while chemical weathering refers to weathering that take place because change in the molecular composition of the substance
You're probably thinking of "Bedrock Twitch", sung by (fictional rocker) Rock Roll from 'The Flintstones'. "There's a place I know where the hipsters go, called Bedrock. Twitch, twitch."
Striations are "scratches" left in bedrock by glaciers. A small particle of rock, generally pebble sized or smaller, becomes entrained in the base of the glacier and dragged along the surface of the bedrock. These can often be seen on hard bedrock surfaces that are resistant to subsequent weathering after the retreat of the glacier. Erratics are large rocks that are found out of place in the landscape, i.e. not near where they were formed. They are removed from their provenance by a glacier and transported away, before being deposited in a different part or the landscape when the glacier melts.
The main form of weathering in a desert is decomposition.
biological weathering occurs in cool, humid clmates.