1. The breaking down of rocks into smaller bits is called acidchemicalcontracterosionexpandsforcesfreezeshotphysicalsedimentationtransportationweatheringwind.

2. The wearing away of weathered rock pieces is called acidchemicalcontracterosionexpandsforcesfreezeshotphysicalsedimentationtransportationweatheringwind.

3. The movement of rock pieces by acidchemicalcontracterosionexpandsforcesfreezeshotphysicalsedimentationtransportationweatheringwind, water and glaciers is called acidchemicalcontracterosionexpandsforcesfreezeshotphysicalsedimentationtransportationweatheringwind.

4. When the bits of rock stop moving, a process called acidchemicalcontracterosionexpandsforcesfreezeshotphysicalsedimentationtransportationweatheringwind begins.

5a. Water that is acidchemicalcontracterosionexpandsforcesfreezeshotphysicalsedimentationtransportationweatheringwind speeds up the weathering process of any rock type.
5b. This is an example of acidchemicalcontracterosionexpandsforcesfreezeshotphysicalsedimentationtransportationweatheringwind weathering.

6a. In the winter at low temperatures, water collects in cracks and acidchemicalcontracterosionexpandsforcesfreezeshotphysicalsedimentationtransportationweatheringwind.
6b. When water freezes it acidchemicalcontracterosionexpandsforcesfreezeshotphysicalsedimentationtransportationweatheringwind, splitting the rock into smaller fragments.

7a. Rocks become acidchemicalcontracterosionexpandsforcesfreezeshotphysicalsedimentationtransportationweatheringwind they expand and on cooling they acidchemicalcontracterosionexpandsforcesfreezeshotphysicalsedimentationtransportationweatheringwind.
7b. This causes stress in the rock layer and the acidchemicalcontracterosionexpandsforcesfreezeshotphysicalsedimentationtransportationweatheringwind involved are enough to crack the rock.

8. The processes described in 6. and 7. are examples of acidchemicalcontracterosionexpandsforcesfreezeshotphysicalsedimentationtransportationweatheringwind weathering.