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to download report - Geological Survey of Ireland

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PREFACEUntil recently <strong>Ireland</strong> has been regarded as a comparatively benign environment as far as landslides areconcerned. However, two widely publicized landslides in the autumn <strong>of</strong> 2003 that occurred near Polla<strong>to</strong>mish inCo. Mayo and Derrybrien in Co. Galway demonstrated the extent <strong>of</strong> property damage and social upheaval thatcan result from such events. The Mayo event was preceded by periods <strong>of</strong> heavy rainfall which are thought <strong>to</strong>have triggered ground failure; at Derrybrien site construction work for a windfarm is thought <strong>to</strong> have been afurther contribu<strong>to</strong>ry fac<strong>to</strong>r. Fortunately on this occasion there was no loss <strong>of</strong> life or serious injury, althoughhis<strong>to</strong>ric events have done so, such as that at Castlegarde, Co. Limerick in 1708 which claimed 21 lives.The events <strong>of</strong> late 2003 served <strong>to</strong> emphasize our paucity <strong>of</strong> knowledge and understanding <strong>of</strong> such landslidesand bogslides in <strong>Ireland</strong>. To address this situation, GSI in early 2004 established the Irish Landslides WorkingGroup with membership invited from other Government Departments, state agencies and the university sec<strong>to</strong>r.Those who volunteered <strong>to</strong> join the Group brought with them a wide range <strong>of</strong> expertise in geology (both bedrockand glacial deposits), geomorphology, geotechnical engineering, planning and GIS. Since its inception theIrish Landslides Working Group has worked well and in a focused manner <strong>to</strong> deliver this <strong>report</strong> <strong>of</strong> their deliberationsand data gathering.An important conclusion <strong>of</strong> the work <strong>to</strong> date is that the incidence <strong>of</strong> landslide events in upland areas in <strong>Ireland</strong>has been grossly underestimated. The Irish Landslides Database which has been created records just over100 entries his<strong>to</strong>ric landslide events whereas in Britain the British <strong>Geological</strong> <strong>Survey</strong> inven<strong>to</strong>ry records over10,000 events. A pilot survey carried out by GSI in the Breifne uplands, in the north-west <strong>of</strong> <strong>Ireland</strong> in 2005recorded over 700 his<strong>to</strong>ric events over a “county size” area, pointing <strong>to</strong> the fact that nationwide there areprobably many thousands <strong>of</strong> unrecorded events. There is an urgent need <strong>to</strong> document these events as the firststep in delineating landslide-prone areas and in order <strong>to</strong> produce landslide susceptibility maps <strong>to</strong> better informplanning decisions, <strong>to</strong> mitigate future property loss and safeguard our communities. Equally we need <strong>to</strong> betterunderstand these events and how they occur, through focused and applied research programmes.As development expands in <strong>Ireland</strong> with increased population pressure, new housing construction coupled withexpanded infrastructure and communications systems will be required that will inevitably encroach in<strong>to</strong> potentiallyhazardous areas. Predictions <strong>of</strong> accelerated climate change may further exacerbate property loss andenvironmental degradation resulting from more frequent landslide events. We must act now <strong>to</strong> curb the cost <strong>of</strong>future landslide hazards through better understanding and mapping <strong>of</strong> these hazards and by improving ourcapability <strong>to</strong> mitigate and manage such natural disasters.Dr. Peadar McArdleDirec<strong>to</strong>r<strong>Geological</strong> <strong>Survey</strong> <strong>of</strong> <strong>Ireland</strong>i

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