Limestone was formed from the remains of organisms that lived in ancient seas. Large areas of beautiful countryside in the UK consist of limestone formed when the country was under water. It forms in shallow tropical seas and so it shows that Britain was once much further south than it is today.
Gorge
Stalagmite
Swallow hole
Tufa screen
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Impervious
Permafrost
Permeable
Volcanic
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Igneous
Metamorphic
Punk
Sedimentary
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Kerbs
Pavements
Ridges
Shelves
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Dartmoor
Lake District
Snowdonia
Yorkshire Dales
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Parachuting
Potholing
Skiing
White water rafting
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Cambrian
Carboniferous
Palaeocene
Permian
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Local villages use all the rainwater
Streams disappear underground
Surface water evaporates quickly
They have very low rainfall
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Calcium carbonate
Calcium chloride
Calcium dioxide
Calcium sulfide
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