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Science
Dataset owned by Failte Ireland Dataset sourced from Failte Ireland Tourism content July 2010
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Science
Dataset owned and provided by OSi as part of the OSI core database 2009.
Polyline dataset representative of disused railways around Ireland
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Science
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Development plans are created by Local Authorities to provided planned future land use. Usually updated every 5 years, these plans for an important guide for sustainable development in Local Government.
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Development plans are created by Local Authorities to provided planned future land use. Usually updated every 5 years, these plans for an important guide for sustainable development in Local Government.
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Science
A trail is usually a path, track or unpaved lane or road. Trails in Co. Wexford include Coillte Recrecational Trail, National Loop Walk, Cycling and other trails.
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Development plans are created by Local Authorities to provided planned future land use. Usually updated every 5 years, these plans for an important guide for sustainable development in Local Government.
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Development plans are created by Local Authorities to provided planned future land use. Usually updated every 5 years, these plans for an important guide for sustainable development in Local Government.
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The data here include SFI research programmes from 2011 that were managed end-to-end in SFI’s Grants and Awards Management System. Programmes were gradually managed through the Grants and Awards Management System from 2011, and therefore awards made under programmes prior to 2011
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A borehole is any hole drilled or dug into the ground. The hole is usually deep, narrow and round. The material (soil and or rock) from the hole is collected and tested in a laboratory to find out the structure and type of the soil and or rock beneath the ground. A borehole recor
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Science
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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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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Bedrock is the solid rock at or below the land surface. Over much of Ireland, the bedrock is covered by materials such as soil and gravel. The Bedrock map shows what the land surface of the North East, Midlands, Cork and Dublin would be made up of if these materials were remove
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Groundwater is the water stored below ground in tiny cracks in the rock or in very small spaces between sand grains. It comes from rainwater that soaks into the ground into an aquifer. An aquifer is a body of rock and/or sediment that holds groundwater. The process of rain fillin
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Science
Water tracing involves tagging water to see where it goes. The time the tracers take to get from one point to the other is also usually recorded. It is most commonly used in karst environments to ascertain groundwater flow rates, directions and catchment definitions (Zone of Con
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Science
Different aquifers have differing abilities to store and transmit water. Based on the hydrogeological characteristics and on the value of the groundwater resource, GSI has classified Ireland’s land surface into aquifer categories. GSI Aquifer classes are divided into three main
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This Hydrostratigraphic Rock Unit Groups map is a reclassification of the 1:100,000 bedrock geology map, created by grouping bedrock formations and members into 27 Rock Unit Group categories based on their hydrogeological properties and other factors.
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