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to download report - Geological Survey of Ireland

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Landslide VulnerabilityThe degree <strong>of</strong> loss resulting from the occurrence <strong>of</strong> a landslide <strong>of</strong> a given magnitude (Varnes, 1984)LandslipA synonym for “landslide” – the term “Landslip” no longer in much usageMass MovementMovement <strong>of</strong> a portion <strong>of</strong> the land surface, usually downslope – a general descriptive termMoraineA mound, ridge, or other distinct accumulation <strong>of</strong> unsorted, unstratified glacial drift deposited by (former) icesheets and glaciersMudFine-grained soils dominated by material <strong>of</strong> clay <strong>to</strong> sand-size, in a wet condition. < 2mm in diameterOrogenyThe process <strong>of</strong> the formation <strong>of</strong> mountains and more specifically the process by which structures in fold-belt mountains wereformed – folding, thrusting, faultingPeriglacialAn environment in which frost action is an important fac<strong>to</strong>r, or phenomena induced by a periglacial climate beyond the periphery <strong>of</strong>the icesheetPermafrostAny soil or subsoil occurring in arctic, sub-arctic, or alpine regions which has been frozen continuously for a long timeQuaternaryThe upper system <strong>of</strong> the Cenozoic Era beginning 2.3 million years ago and which forms the current period <strong>of</strong> geological time. It is madeup <strong>of</strong> the Pleis<strong>to</strong>cene (Ice Age) and the Holocene (Postglacial ) EpochsRaised BogAn accumulation <strong>of</strong> peat with its greatest thickness being at the centre giving it a convex-upward surface. They are found in themidlands <strong>of</strong> <strong>Ireland</strong> and are principally composed <strong>of</strong> moss peatRaster imageAn image composed <strong>of</strong> a rectangular grid <strong>of</strong> pixels. Each pixel contains a defined value about its colour, size, and location in theimage.RegolithThe layer <strong>of</strong> fragmented and unconsolidated rock material overlying the bedrockScreeRock fragments, usually coarse and angular, derived from and lying at the base <strong>of</strong> cliffs or very steep slopesShear StrengthThe internal resistance <strong>of</strong> a body <strong>to</strong> shear stress, typically including a frictional part and a part independent <strong>of</strong> friction called cohesionSlickensidesA lineated fault or slip surface, having groove lineations which may indicate the direction <strong>of</strong> slippage on the surfaceSlideA mass movement <strong>of</strong> earth material under shear stress along one or several surfaces. The movement may be rotational or planar(translational)SolifluctionThe slow viscous downslope flow <strong>of</strong> waterlogged soil, usually in areas underlain by frozen ground ie. in periglacial areasSpreadThe dominant movement in a spreading landslide is lateral extension due <strong>to</strong> shearing or tensional fracturesTalusSee “Scree”TillLargely unsorted and unstratified material deposited directly underneath a glacier and consisting <strong>of</strong> a heterogeneous mixture <strong>of</strong> clay,silt, sand, gravel, and bouldersToppleA mass movement that consists <strong>of</strong> the forward rotation <strong>of</strong> units <strong>of</strong> rock about a pivot point under the force <strong>of</strong> gravityTsunamiA gravitational seawave produced by any large-scale, short duration disturbance <strong>of</strong> the sea-floor due <strong>to</strong> an earthquake, sea floorsubsidence or a volcanic eruption98

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