Linked from

The 45 pages that link to Speleothem, each with the reason it gives.

• KarstRelated: Speleothems preserve records that can help reconstruct past climate and groundwater conditions.

• CalciteRelated: Many cave speleothems grow as calcite precipitates from dripping water.

• Oxygen isotope ratioRelated: Its oxygen isotope composition can preserve changes in rainfall and cave conditions.

• Carbonate mineralRelated: Cave formations grow as dissolved carbonate is deposited from groundwater.

• Uranium-series datingRelated: Uranium-bearing cave carbonates can preserve datable uranium-thorium disequilibrium.

• Cave formationRelated: Cave growth creates settings where mineral-rich water deposits speleothems.

• CenoteRelated: Cave deposits near cenotes preserve records of past rainfall and climate.

• Lechuguilla CaveRelated: The cave contains unusually varied speleothems, including delicate gypsum formations.

• Cave passageRelated: Speleothems grow on passage floors, walls, and ceilings.

• Nullarbor PlainRelated: Speleothems in Nullarbor caves preserve records of past water and climate.

• PaleothermometerRelated: Its carbonate can preserve isotope signals used to investigate cave and regional temperatures.

• Friouato CavesRelated: Deposits can form where mineral-rich water drips through limestone chambers.

• Sof Omar CavesRelated: Such deposits can record water movement and mineral processes inside limestone caves.

• δ18ORelated: Its δ18O can preserve changes in rainfall and moisture sources.