USDA Forest Service
 

Tongass National Forest

 
A photo collage showing broken karst topography and cave features.
About The Tongass
 
Cabins
 
Campgrounds
 
Boating
 
Fishing
 
Caves and Karst
 
Glaciers
 
Hiking
 
Picnicking
 
Visitor Centers
 
Visitor Programs
 
Wilderness
 
Wildlife Viewing
 
Winter Recreation
  Local Links
  Prince of Wales
  Recreation
  Conservation Education
  Island Info
  Projects & Plans
 
Chugach National Forest
Alaska Region
Forest Service Headquarters
   
Evaluate Our Service
We welcome your comments on our service and your suggestions for improvement.

Tongass National Forest
Federal Building
648 Mission Street
Ketchikan, AK 99901

(907) 225-3101
(907) 228-6222 (TTY)

e-mail comments to:
Web Manager

United States Department of Agriculture Forest Service.

E-gov logo links to E-Gov.gov

Link to USA.gov.

USDA USDA Forest Service
Tongass Home » Districts and Offices » Prince of Wales Island » Recreation » El Capitan Cave

Formations

El Capitan Cave has beautiful deposition features. As the water runs through the limestone and eats away passages, it picks up small particles of calcite. These microscopic particles are deposited on the surfaces of the caves. These deposits form secondary formations, or speleothems.

Unfortunately, before the gate was installed, people explored the cave and destroyed many of the flowstone formations. When these formations are removed, they can never be replaced and a valuable source of information is lost forever.

Secondary lighting shows the yellowish color of the calcite stalagmites and stalactites.

Stalactites and Stalagmites are likely familiar to most. It is helpful to remember stalactites "hang tight" to the ceiling, while stalagmites "might" rise from the floors and walls.

Stalactites form when there is a slow drip of water coming from the ceiling.

Stalagmites form when the drops are falling too fast to totally evaporate without dripping. All the particles do not have time to collect on the ceiling, so some accumulate on the cave floor.

A pillar has formed in the limestone where a stalactite from the ceiling has formed together with a stalagmite.

 

 

 

When stalactites and stalagmites come together in the middle, they are called cave columns or pillars.

 

Draperies are another beautiful formation visible inside the cave. They form when there is a high volume of water flowing over an angled cave wall. Sometimes they are called "cave bacon." The water flow can pick up other minerals, leaving multi-colored ribbons in the drapery. When backlit, these draperies sometimes resemble a large slab of bacon.

Near the end of the tour, a drip pool has formed and the rings of the flowstone which it has formed in are clearly visible.

 

 

This small drip pool is a well-loved formation in El Cap. Formed over a very long period of time - with a single drip of water working through layers of limestone and flowstone.

 

Flowstone has a variety of looks.

 

Flowstone is formed by water flowing over the surface of limestone (right and below).

This image shows the drip pool in flowstone from a different angle, further back Wet, slick flowstone forms when water flows over the surface of the limestone depositing calcite.

Near the otter natal den in El Captain, a multi layered wall comprised of draperies is on display. Two soda straws of light colored calcite are shown forming with a drip of water at the base of each.

 

"Soda straws" (left) are thin hollow stalactites of calcite formed as water flows inside the tube and crystalizes at the end, one drop at a time over millenia. Multiple layers of flowstone form draperies along the cave wall (right).

 

Previous Page
A caver icon links to the previous page of the cave tour.
Next Page
A caver icon links to the next page of the cave tour.

USDA Forest Service - Tongass National Forest Accessibility Statement
Last Modified: April 08, 2009