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
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