Cave Lighting Project
We are undergoing a year-long lighting project in the cavern. Please be aware of caution tape along pathways inside the cave and use due care.
Scenic Loop Road Closed
The 9-mile scenic Loop Road (Desert Drive) is closed due to weather damage. The road will reopen as soon as repairs are done. This scenic road does not affect road access to the visitor center or the cave.
Cave / Karst Systems
A karst area is one generally characterized by numerous caves, little surface drainage, sinkholes and springs. The Guadalupe Mountains contain many caves, but few of the features are traditionally used to define karst. The caves of the Guadalupe Mountains pre-date the large canyons and well-defined surface features we see today. Since the development of the caves is much older than the surrounding landscape, we see very few of the typical karst features found when caves and the landscape develop at the same time.
Speleogenesis: How Carlsbad Cavern was Formed
Between 4 and 6 million years ago hydrogen-sulfide-rich (H2S) waters began to migrate through fractures and faults in the Capitan limestone. This water mixed with rainwater moving downward from the surface. When the two waters mixed, the H2S combined with the oxygen carried by the rainwater and formed sulfuric acid (H2SO4). This acid dissolved the limestone along fractures and folds in the rock to form Carlsbad Cavern. This process left behind massive gypsum deposits, clay, and silt as evidence of how the cave was formed.
With time, the active level dropped to form deeper cave passages. In abandoned cave passages above, blocks fell from the ceiling and speleothems (cave formations) began to grow. Around 4 million years ago, speleogenesis ceased in the area around Carlsbad Cavern and the cave began to take on the look it has today.
Generalized Stages of Cave Development [214k PDF]
Did You Know?
Bones from ice age animals like jaguars, camels, lions and giant sloths have been found in the entrance areas of some caves in Carlsbad Caverns National Park.