They even smell Green!
Bogs form when the following conditions come together:
- Dampness = poor drainage. Bogs form in the Canadian Shield
because this type of rock does not drain very well. They can also form over large clay
deposits.
- Stagnant = minimal inflow (rain or snow) and outflow (evaporation)
- Lack of nutrients (see points 1 & 2)
Bogs tend to be acidic which limits what kind of plants can live there.
Examples of acid loving plants are Sphagnum Mosses & Labrador Tea. Due to the limited nutrient content of the bog environment, the plants tend to
be slow-growing and perennial. Some bog plants like pitcher plants are
"carnivorous" and get their nutrients by capturing
and "digesting" insects.
Peat (like in Ireland) forms because layers of partially decomposed
vegetation form. Actually, anything that falls into a bog decomposes very slowly. This is why they put boardwalks across bogs.
Water in bogs gets its dark brown colour from tannins in the leaves, which
is the same way that tea gets its colour.
Because sphagnum moss absorbs water like a sponge, water is also scarce for bog plants. Therefore, these plants, like plants in a desert have adapted to conserve water. For example, some
bog plants have a waxy covering on their leaves.
Other bog plants include:
- some orchid species
- cranberry
- bog rosemary
- bog laurel
Some trees such as Black Spruce and Tamarack grow at the edges of a bog or in locations where some soil has accumulated.
The removal of peat moss for use in home gardens contributes to the loss of
bog habitat.
Bogs I have Known
Fens are a closely-related type of wetland.
Bog Links