Karst Landscapes - Underground Features (Leaving Cert Geography): Flashcards

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Karst Landscapes - Underground Features
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Zone of saturation

Area below water table where all spaces filled with groundwater

Primary zone for cave formation

Zone of saturation

Carbonation in cave formation

Rainwater + CO2 forms carbonic acid, dissolves limestone

Hydraulic action

Flowing water pressure breaks limestone, carves passages

Abrasion in caves

Broken limestone pieces scrape walls, widen passages

Dripstone features

Rock formations from calcium carbonate via dripping water

Dissolution process

Calcium carbonate deposited when water evaporates in caves

Calcite

Hard mineral of calcium carbonate from evaporating water

Stalactites

Icicle-shaped formations hanging down from cave roofs

Stalagmites

Shapeless mounds growing upward from cave floors

Why stalagmites have thicker bases

Water splashes & spreads over wider area on floor

Pillars in caves

Stalactites & stalagmites joined from floor to ceiling

Curtains (dripstone)

Ridge-like formations along roof cracks where water flows

Flowstones

Sheet-like formations on walls/floors from flowing water

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