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 ¼ of the world’s population live in Karst areas (most of
this ¼ is found in China)
 Formed by Chemical weathering (from rainwater) and
erosion
 Lack of rivers/lakes
 Presence of Swallow Holes – where water disappears
underground
 Presence of hollows – dolines
 Presence of underground water (in caves)
 Limestone is permeable (water can pass through)
 Well jointed (vertical “gaps”)
 Has bedding planes (horizontal “gaps” between layers)
 Easily chemically weathered
 Many cave features are formed by Deposition
 Rainwater (slightly acidic from the CO2 in the air) dissolves
Calcium Carbonate in Limestone.
 The dissolved Calcium Carbonate (called Calcite) is deposited
in caves
 Important source of water – many springs in Limestone
areas.
 Ballygowan water – from limestone area in Limerick
 Very important for tourism
◦ Caves are tourist attractions (e.g. Ailwee Cave)
◦ Unique landscape
◦ Planning restrictions mean landscape is kept unspoilt – no
housing estates/McDonalds/Shopping centres allowed
◦ Historic features
 Unique Ecosystem…. Unusual plants and animals
 Engineering difficulties
◦ Caves may collapse
◦ Industrial Development Restricted
◦ Problems with fresh water contamination due to permeable
nature of landscape – fertiliser, sewerage etc can easily
contaminate drinking water supplies
◦ Agricultural development restricted – farming is difficult
Rock types and landscapes
Rock types and landscapes

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Crayon Activity Handout For the Crayon A
 

Rock types and landscapes

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  • 2.  ¼ of the world’s population live in Karst areas (most of this ¼ is found in China)  Formed by Chemical weathering (from rainwater) and erosion
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  • 11.  Lack of rivers/lakes  Presence of Swallow Holes – where water disappears underground  Presence of hollows – dolines  Presence of underground water (in caves)
  • 12.  Limestone is permeable (water can pass through)  Well jointed (vertical “gaps”)  Has bedding planes (horizontal “gaps” between layers)  Easily chemically weathered
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  • 21.  Many cave features are formed by Deposition  Rainwater (slightly acidic from the CO2 in the air) dissolves Calcium Carbonate in Limestone.  The dissolved Calcium Carbonate (called Calcite) is deposited in caves
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  • 26.  Important source of water – many springs in Limestone areas.  Ballygowan water – from limestone area in Limerick
  • 27.  Very important for tourism ◦ Caves are tourist attractions (e.g. Ailwee Cave) ◦ Unique landscape ◦ Planning restrictions mean landscape is kept unspoilt – no housing estates/McDonalds/Shopping centres allowed ◦ Historic features
  • 28.  Unique Ecosystem…. Unusual plants and animals
  • 29.  Engineering difficulties ◦ Caves may collapse ◦ Industrial Development Restricted ◦ Problems with fresh water contamination due to permeable nature of landscape – fertiliser, sewerage etc can easily contaminate drinking water supplies ◦ Agricultural development restricted – farming is difficult