The process of weathering (the creation of smaller rock particles from a larger rock body), begins as soon as the rock body is exposed to any cause of weathering. The weathering could start immediately in the case of extrusive igneous rock, which is formed from molten material on the surface, when acid in water chemically attacks the surface. Igneous rock underground can begin to weather simply by the erosion of the rock above it, which releases pressure on it, causing the rock body to expand and fracture.
When a rock is exposed to weather, it can undergo weathering processes like physical breakdown due to temperature changes, chemical alteration from rainwater or acids, and biological weathering from plant roots or burrowing animals. Over time, these weathering processes can cause the rock to erode and break down into smaller pieces.
The type of weathering that does not alter the chemical composition of the rock is called physical weathering. The acid weathering usually alter the chemical composition of a rock.
All soil begins as rock that is broken down by weathering and biological activity over time.
The effect of weathering is to reduce the volume of the igneous rock.
Weathering may change the rock into many shapes.
By weathering either by physical or chemical weathering.
It is water weathering
by weathering
It is the process of weathering.
Any and all rock can be changed into sediment by weathering and erosion.
Ice freezing in a crack of a rock is considered weathering.
The process of breaking down of rocks and minerals on the surface is known as rock weathering.