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Eolaíocht
Groundwater is the water that soaks into the ground from rain and can be stored beneath the ground. Groundwater floods occur when the water stored beneath the ground rises above the land surface. The Groundwater Flooding Medium Probability map shows the expected flood extent of g
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Eolaíocht
Groundwater is the water that soaks into the ground from rain and can be stored beneath the ground. Groundwater floods occur when the water stored beneath the ground rises above the land surface. The Groundwater Flooding High Probability map shows the expected flood extent of gro
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Groundwater is the water that soaks into the ground from rain and can be stored beneath the ground. Groundwater floods occur when the water stored beneath the ground rises above the land surface. The Groundwater Flooding Low Probability map shows the expected flood extent of grou
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Groundwater is the water that soaks into the ground from rain and can be stored beneath the ground. Groundwater floods occur when the water stored beneath the ground rises above the land surface. The Winter 2015/2016 Surface Water Flooding map shows fluvial (rivers) and pluvial (
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Groundwater is the water that soaks into the ground from rain and can be stored beneath the ground. Groundwater floods occur when the water stored beneath the ground rises above the land surface.
The Historic Groundwater Flood Map shows the observed peak flood extents caused by
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Eolaíocht
Groundwater sources, particularly public, group scheme and industrial supplies, are of critical importance in many regions.
The Group Scheme Preliminary Source Protection Areas dataset comprises Zones of Contribution to groundwater abstraction points that supply Group Water Schem
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Groundwater sources, particularly public, group scheme and industrial supplies, are of critical importance in many regions.
The Public Supply Source Protection Areas dataset comprises Source Protection Areas (SPAs) around groundwater abstraction points that are managed by Irish W
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Landslide locations and extents help us locate where landslides have occurred. Ireland's location, terrain and climate result in landslides occurring mainly in areas with steep slopes where rock meets the surface and peat covers the terrain. Landslides have the potential to cause
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Eolaíocht
A landslide is the movement of material down a slope. This includes rock, earth, mud and peat. Landslides in Ireland mainly occur on steep mountain slopes.
A landslide susceptibility map shows areas where a landslide could occur, how likely it will occur and what causes them. The -
Geological heritage or ‘geoheritage’ is the term used to describe sites or places with features of geology that have important scientific, educational, cultural, or visual value. There are many types of sites. They are made from past and present geological processes (wearing away
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Timpeallacht
The latest topsoils data from the Tellus project, managed by the Geological Survey Ireland.
The Topsoil (c.5–20 cm deep) samples were analysed for: Analytical Method: ICP(-OES/-MS) following aqua regia digestion; soil pH, soil loss-on-ignition at 450°C The survey was conducted on -
Landslide susceptibility mapping using GIS mapping to map areas prone to landslides. Adopting a test methodology for systematic landslide susceptibility mapping for the whole of Ireland.
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Following two major landslide incidences in Ireland in 2003 in Galway and Mayo the Geological Survey Ireland established the Irish Landslides Working Group (ILWG) in 2004. It was felt important that it should be a multi-disciplinary team, bringing together various types of expert
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Eolas Teagmhála
Aonad Sonraí OscailteAn Roinn Caiteachais Phoiblí Bonneagair Athchóiriúcháin Seirbhíse Poiblí agus Digitiúcháin,
Teach Faiche Stiabhna,
Ardán Phort an Iarla, D02 PH42 BAC 2 Éire.
Tabhair aiseolas dúinn
Is mór ag an Aonad Sonraí Oscailte do chuid aiseolais, ceisteanna nó tuairimí. Bímid sásta i gcónaí cloisteáil uait.
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