The Bog of Allen (Irish: Móin Alúine) is a large raised bog in the centre of Ireland between the rivers Liffey and Shannon.
The bog's 958 square kilometres (370 square miles) stretch into counties Offaly, Meath, Kildare, Laois, and Westmeath.[1] Peat is mechanically harvested on a large scale by Bórd na Móna,[citation needed] the government-owned peat production industry. The area has kilometres of narrow gauge industrial railways for transporting turf to processing plants and turf powered power plants. In addition, the cutover portions are used as area for grazing. The bog is crossed by the Grand Canal and the Royal Canal.
Preservationists
editThe Irish Peatland Conservation Council describes the bog as "an important area of peatland, as much a part of Irish natural heritage as the Book of Kells."[2] The bog is much reduced after centuries of industrial exploitation and recent encroachments by development.[citation needed] Efforts are underway to preserve sections of it.[citation needed]
Archaeological significance
editThe peatlands of the Bog of Allen contain a valuable part of the archaeological record.[3] Due to the special preservation conditions within peat, many kinds of artefact which do not normally survive are preserved; these include wooden structures and objects. In many parts of the Bog of Allen industrial milling has uncovered archaeological remains[4] such as trackways. These trackways are wooden walkways constructed through prehistory and into the medieval period which allowed people and animals to cross the extensive areas of peatland, which can give us an insight into the economy and way of life of the societies that existed around the bog. The preservation conditions in bogs also preserve a range of palaeoenvironmental evidence such as pollen and plant macrofossils which are often studied alongside the archaeological evidence to inform about the environment on and around the bog.[citation needed]
Palaeoenvironmental studies
editNumerous studies have focused on reconstructing past environments through the study of palaeoenvironmental proxies preserved in the Bog of Allen. Bogs such as these are of particular interest as ombrotrophic bogs are very sensitive to changes in precipitation. A current study carried out on Daingean Bog is investigating the use of testate amoebae to reconstruct changes in precipitation and to link this to climate variability during the Holocene.[5] Such studies are of value as they may be informative about the response of past societies to climate change.
See also
editReferences
edit- ^ "Bog of Allen Map and Guide". Irish Peatland Conservation Council. Archived from the original on 19 May 2011. Retrieved 19 July 2009.
- ^ "Bog of Allen Survey". Irish Peatland Conservation Council. Archived from the original on 9 December 2010. Retrieved 19 July 2009.
- ^ "Archaeological Finds" (PDF). Bórd na Móna. 2001. Archived from the original (PDF) on 19 November 2007. Retrieved 24 June 2010.
- ^ "Peatland". Archaeological Development Services. Archived from the original on 26 March 2010. Retrieved 24 June 2010.
- ^ Mayewski, Paul A.; Rohling, Eelco E.; Stager, J. Curt; Karlén, Wibjörn; Maasch, Kirk A.; Meeker, L. David; et al. (November 2004). "Holocene Climate Variability" (PDF). Quaternary Research. 62 (3): 243–255. Bibcode:2004QuRes..62..243M. doi:10.1016/j.yqres.2004.07.001. S2CID 17499244. Archived from the original (PDF) on 22 December 2009. Retrieved 24 June 2010.
External links
editChisholm, Hugh, ed. (1911). . Encyclopædia Britannica. Vol. 1 (11th ed.). Cambridge University Press. p. 693.