What are Speleothems?
Speleothems
Mineral formations in caves (e.g., stalactites, stalagmites) formed by deposition from mineral-rich water.
Key Features:
Formation Process:
Created when water dissolves minerals (calcite/gypsum) from rocks and redeposits them in caves through evaporation/chemical reactions.
Types:
Stalactites: Hang from ceilings (drip-formed).
Stalagmites: Rise from floors (drip-formed).
Flowstones: Sheet-like deposits from flowing water.
Soda straws: Thin, hollow tube stalactites.
Scientific Importance:
Climate Archives: Record past environmental changes.
Dating: Uranium-series methods provide precise age estimates (up to millions of years).
Proxy Data:
Isotopes (δ¹⁸O, δ¹³C) reveal past rainfall/temperature.
Layer thickness indicates water availability.
Global Examples:
Carlsbad Caverns (USA), caves in Italy/China.
UPSC Relevance:
GS-1 (Geography): Paleoclimatology, karst landscapes.
GS-3 (Env.): Climate change studies using natural archives.
Example: "Green Arabia" study used speleothems to prove humid phases in Arabian deserts.