Stalactites and Stalagmites: Drip by Drip
Deep inside some caves, stone icicles hang from the ceiling, and stone spikes rise from the floor below. They look like they belong in a fantasy movie, but they are made by plain water and time.
Many caves form in limestone, a soft rock. Rainwater picks up a gas from the air and soil, which makes it slightly acidic. As this water trickles down through cracks in the limestone, it dissolves a little of the rock and carries it along.
When a drop reaches the roof of a cave, it hangs there for a moment. Some of the gas escapes into the cave air, and a tiny ring of dissolved rock is left behind. Another drop follows, and then another. Over thousands of years, the rings add up into a hollow stone tube that grows downward. This is a stalactite.
Drops that fall to the floor also leave rock behind. Slowly, a mound builds up and grows toward the ceiling. This is a stalagmite.
If you want to remember which is which, think of the letter c in ceiling, which starts the word stalactite. Sometimes the two meet in the middle and join into a single column. Because they grow so slowly, cave visitors are asked never to touch them.