1. Existing rock is broken down by weathering and eroding into smaller particles and dissolved minerals
2. These are carried away, separated and redeposited elsewhere as rocks with different compositions and properties
3. Alluvial/Placer deposits - carried by flowing water and deposited when flow slows down
4. Evaporites - formed when water evaporates from mineral-rich solutions and minerals crystallise
5. Biological deposits - produced from dead animals and plants, e.g. fossil fuels
6. Chemical precipitates - e.g. manganese nodules on deep sea beds