chemical
Oxidation is a type of chemical weathering where minerals in rocks react with oxygen to form new minerals. It typically leads to the rusting of iron-bearing minerals in rocks.
Physical weathering is a type of weathering in which minerals react with dissolved oxygen in water. This causes chemical changes to take place in the minerals.
Hydrolysis is a source of chemical weathering, where minerals in rocks are broken down by the chemical reaction with water.
The breaking down and wearing away of the earth's rocks by the atmosphere is called weathering. Oxidation is a type of chemical weathering that occurs when minerals in rocks react with oxygen.
Precipitation (source of chemical weathering) Plant roots (source of chemical weathering) Freezing and thawing (source of mechanical weathering) Human activities (source of mechanical weathering)
chemical
Oxidation is a type of chemical weathering where minerals in rocks react with oxygen to form new minerals. It typically leads to the rusting of iron-bearing minerals in rocks.
That would be oxidation.
That would be oxidation.
Yes, oxidation is a type of chemical weathering that does require the presence of water to occur. Oxygen in the air combines with minerals in rocks when water is present, leading to the breakdown of those minerals through oxidation.
This is an oxidation reaction.
oxidation causes iron to change color. oxidation causes rust.
Mechanical
what chemical weathering called oxidation causes
Oxygen is not a type of weathering. However, oxygen can play a role in certain types of chemical weathering processes, such as oxidation, where oxygen reacts with minerals in rocks to break them down.
Chemical weathering is a type of weathering that breaks down rocks by changing the substances within them. This process involves the dissolution, carbonation, oxidation, and hydrolysis of minerals in the rocks, leading to their decomposition.
Physical weathering is a type of weathering in which minerals react with dissolved oxygen in water. This causes chemical changes to take place in the minerals.