In addition to lakes and streams, the Faroese wetlands also include a number of fens. Together, they cover 18 km2, which corresponds to 1.3 % of the Faroe Islands’ total area. The origin of the fens varies. Where old lakes have gradually been overgrown by bog moss, basin fens arise, while sloping fens, ‘tilrenningarmýrur’, are formed on mountain sides where the water cannot escape. In the valleys and lowlands, you can also find bogs.
Peat is often formed since plant residues and other organic material break down only slowly in the fens, although the layers are relatively thin. Throughout time, the peat has been cut and dried so that it could be used as fuel, and for centuries peat served as a valuable source of energy in Faroese households.
Today, there is renewed interest in the fens. Not because of peat extraction, but for their ability to bind carbon. This makes them a potential key element in the future climate policy.
Further reading
- Akraberg
- Birds on the Faroe Islands
- Climate on the Faroe Islands
- Fresh Waters on the Faroe Islands
- Geology on the Faroe Islands
- Hvannhagi
- Insects and arachnids on the Faroe Islands
- Lakes on the Faroe Islands
- Landscapes and coasts on the Faroe Islands
- Nature and environmental management
- Plant life on land on the Faroe Islands
- Streams on the Faroe Islands
- Weather conditions on the Faroe Islands
- Wildlife in the sea around the Faroe Islands
- Wildlife on the Faroe Islands
Read more about Nature and landscape on the Faroe Islands