Photographer’s Note
This was taken inside Carlsbad Cavern in New Mexico USA. The story of the creation of Carlsbad Cavern begins 250 million years ago with the creation of a 400 mile long reef in an inland sea that covered this region. This horseshoe shaped reef formed from the remains of sponges, algae and seashells and from calcite that precipitated directly from the water. Cracks developed in the reef as it grew seaward. Eventually the sea evaporated and the reef was buried under deposits of salts and gypsum.
Then, a few million years ago, uplift and erosion of the area began to uncover the buried rock reef. Rainwater, made slightly acidic from the air and soil, seeped down into the cracks in the reef, slowly dissolving the limestone and beginning the process that would form large underground chambers. At the same time, hydrogen sulfide gas was migrating upward from vast oil and gas deposits beneath the ancient reef. This gas dissolved in the percolating ground water to form sulfuric acid. The added power of this corrosive substance explains the size of the passageways. The exposed reef became part of the Guadalupe Mountains and the underground chambers became the wonder of Carlsbad Cavern.
The decoration of Carlsbad Cavern with stalactites, stalagmites and an incredible variety of other formations began more than 500,000 years ago after much of the cavern had been carved out. It happened slowly, drop by drop, at a time when a wetter, cooler climate prevailed. The creation of each formation depended on water that dripped or seeped down into the limestone bedrock and into the cave. As a raindrop fell to the ground and percolated downward, it absorbed carbon dioxide gas from the air and soil, and a weak acid was formed. As it continued to move downward the drop dissolved a little limestone, absorbing a bit of the basic ingredient needed to build most cave formations--the mineral calcite.
Once the drop finally emerged in the cave, the carbon dioxide escaped into the cave air. No longer able to hold the dissolved calcite, the drop deposited its tiny mineral load as a crystal of calcite. Billions and billions of drops later, thousands of cave formations had taken shape. And, oh, the shapes they took! Where water dripped slowly from the ceiling, soda straws and larger stalactites appeared. Water falling on the floor created stalagmites. Sometimes a stalactite and stalagmite joined, forming a column.
A truely amazing site to see in person and you could spend days and never see even 1/2 of the caverns.
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Photo Information
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Copyright: Julie Wyatt (j_wyatt)
(685) - Genre: Places
- Medium: Color
- Date Taken: 2003-12-27
- Categories: Nature
- Camera: Canon PowerShot G2
- Exposure: f/2.2, 1/60 seconds
- Photo Version: Original Version, Workshop
- Theme(s): Caves and Cave Sights, vision souterraine-2 [view contributor(s)]
- Date Submitted: 2005-01-14 23:57
Discussions
- To LCannon: It is hard to get a shot inside a cave. Now (2)
by j_wyatt, last updated 01-16 08:11 - To Lovamour: glad you liked them! There were (1)
by j_wyatt, last updated 01-16 00:24








