How it works
Cave formations are called speleothems: mineral deposits left where water drips, flows or pools in a cave. This drawing has six of the best known with labels, then five more parts of the cave.
Read the full guide
Start with six
Find the stalactites hanging from the roof and the stalagmite under them. Where the two have met there is a column. Soda straws are the thin tubes, flowstone spills down the right wall, and the striped sheet on the left is a drapery, also called cave bacon.
More in the cave
Helictites twist across the roof, cave pearls lie in the pool, and cave popcorn is the knobby patch on the left wall. Water drops fall from roof to floor, and limestone is the rock all around.
Questions and answers
What is the difference between a stalactite and a stalagmite?
A stalactite hangs from the cave roof and usually ends in a point. A stalagmite builds up from the floor under the drips and usually has a rounded top. When the two grow together they make a column.
What are the six most common speleothems?
Lists differ. One encyclopedia image showing six speleothems with labels has flowstone, columns, drapery, stalagmites, stalactites and soda straws. The National Park Service calls stalactites the most common and says cave popcorn probably comes next after stalagmites and flowstone.
What is a speleothem?
A cave formation: a deposit of minerals left over time by water that drips, flows or pools in a cave. Stalactites, stalagmites and flowstone are all speleothems.
How do stalactites form?
Water seeping through limestone carries dissolved mineral. When a drop hangs from the cave roof, a trace of that mineral is left behind. Drop after drop, the deposit grows downward into a stalactite.
What is cave bacon?
A drapery with bands in it. A drapery is a thin, wavy sheet of stone that forms where water runs down a sloping cave roof. The bands make it look like a strip of bacon.