Page 258 - (DK Eyewitness) Travel Guide - Ireland
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256      IRELAND  REGION  B Y  REGION


               The Raised Bogs of the Midlands

        Peatland or bog, which covers about 15 per cent of the Irish landscape, exists in two
        principal forms. Most extensive is the thin blanket bog found chiefly in the west, while
        the dome-shaped raised bogs are more characteristic of the Midlands – notably in an
        area known as the Bog of Allen. Although Irish boglands are some of the largest in
        Europe, the use of peat for fuel and fertilizer has greatly reduced their extent, threatening
        not only the shape of the Irish landscape but also the survival of a unique habitat and
        the unusual plants and insects it supports.


                                                     Peat cutters still
                                                     gather turf (as peat
                                                     is known locally) by
                                                     hand in parts of
                                                     Ireland. It is then set
                                                     in stacks to dry. Peat
                                                     makes a good fuel,
                                                     because it is rich in
                                                     partially decayed
                                                     vegetation, laid
                                                     down over
        Unspoiled expanse of the Bog of Allen        thousands of years.

          Fen plants           Birch and   Fen plants (reeds   Fen peat
                             willow scrub  and sedges)






                            Moraine (glacial
                               deposits)  Mud
         8000 BC: Shallow meltwater lakes that formed   6000 BC: As the fen vegetation died, it sank to
         after the Ice Age gradually filled with mud. Reeds,   the lake bed but did not decompose fully in the
         sedges and other fen plants began to dominate   waterlogged conditions, forming a layer of peat.
         in the marshy conditions which resulted.  This slowly built up and also spread outwards.
         Fen peat           Fresh sphagnum   Pine and      Raised bog
                                 peat  alder trees








                         Buried tree stumps              Tree stumps
         3000 BC: As the peat built up and the lake slowly   Present day: Few raised
         disappeared, plant life in the developing bog had   bogs are actively growing
         to rely almost exclusively on rainwater, which is   today. Those that remain
         acid. Fen plants could not survive in these acidic   contain a fascinating
         conditions and gave way to bog mosses, mainly   historical record of the
         species of sphagnum. As these mosses died, they   landscape. The survival of
         formed a layer of sphagnum peat on the surface   ancient tree stumps
         of the bog which, over the centuries, attained a   shows how well plants
         distinctive domed shape.    are preserved in peat.  Sphagnum moss





   256-257_EW_Ireland.indd   256                            08/03/17   11:07 am
     Eyewitness Travel   LAYERS PRINTED:
     Catalogue template    “UK” LAYER
     (Source v2)
     Date 14th November 2012
     Size 125mm x 217mm
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