The botany composition provided by the type of source vegetation, determines the peat type. Three types were identified in total: high moor, transitional and low moor.
High moor peat is formed mainly in eutrophic moors characterized by high saturation with nutrients.
This type of peat has:
Transitional peat is formed in moors with a low level of primary production. More than 10% of oligotrophic and eutrophic types of residues are present in the botanical composition of the vegetation of these moors.
Transitional type of peat has:
Low moor peat contains not more than 10% of oligotrophic vegetation. It is formed mainly in river valleys and absorbs a lot of water.
Low moor peat has: