Peat and Peatlands
Peat is really just made up of around 98% water and 2% dead plants that once grew on the bog surface. This doesn’t sound very exciting or valuable but it can be very useful: peat has been used for thousands of years as a source of fuel in areas where wood was scarce and it is used extensively now as garden compost. However, because peat grows so slowly, it is not a renewable resource and will eventually run out if we carry on destroying it.

The future for peatlands: threats and conservation
Scottish Wildlife Trust Peatlands Campaign:
www.swt.org.uk/

Why should we care?
Bogs are very wet and difficult to walk on and they often look bleak and lifeless but this is far from the truth. They contain many special or endangered plants and animals which cannot live anywhere else.

A watery oasis: biodiversity on peatlands
RSPB:
www.rspb.org.uk
Irish Peatland Conservation Council:
www.ipcc.ie/index.html
Link to GHMCNP

The Peat Library
People who work on conservation, plant or animal ecology are not the only ones interested in bogs. Peat bogs are also very valuable to people who study the past: archaeologists, palaeoecologists (investigating past ecology) and palaeoclimatologists (who study changes in the climate in the past).

There are two characteristics of bogs that make them so important as records of the past:

1. Peat provides almost perfect conditions for preserving organic materials and these can tell us a huge amount about past environments, as you can read below.

2. Peat ‘grows’ upwards through time, with the oldest part of the bog at the bottom and the youngest on top, under the living surface.  These layers are called a stratigraphy or a stratigraphic sequence.

How a bog ‘grows’>

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