Cueva del Nitro
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Cueva del Nitro is a limestone cave system located 6 kilometers (4 miles) from Zapatoca, Colombia, in the area of vereda Agua Fría.
The cave is an example of karst geology, meaning the landscape was formed by water dissolving the bedrock over millions of years. This process created the cave's jagged tunnels and large chambers. Geologically, the cave belongs to the Rosablanca Formation and dates back to the Early Cretaceous period (approximately 125 million years ago).
Visitors can access the cave via a guided route. Inside, the system features active underground water currents and extensive mineral formations, including stalactites (hanging from the ceiling), stalagmites (growing from the ground), columns, and flowstone.