#speleothem

[segmentedleg]

File:Son Doong Cave DB (1).jpg

[spiritheyregone]

"Lily pad room" at Onondaga Cave State Park, Missouri. (Flickr)

[mjhartwork]

missing primavera

[lraquel]

Tubular stalactites, also known as soda straws. Their existence next to a traversed cave path is rare - usually getting knocked off by passers by. I was fortunate to see them on my tour of Round Spring Cave in Missouri.  Undisturbed specimens have been recorded at 30 feet long. 

Water seeping through the rock drips from the ceiling leaving minerals behind. The hallow center is formed by a blockage - preventing the stalactite from filling in.  

Growing only a few millimeters per year, this formation is about as older as I am.

Learn more here.  Near Shannon County Missouri 2012.

[earthstory]

pankotaiferi

#postojna

[lutnistas]

Vrelo Cave in the Matka Canyon ( North Macedonia ) 

[room-without-a-window]

Stalagmite in Algar da Figueira, Maciço Calcário Estremenho

23/04/17 - Afonso Theias

Speleology #2

[itssedimentary]

Speleothems

Imagine that there’s a faucet that’s slowly dripping. If the faucet is left to drip long enough, you’ll notice that it will leave behind deposits from the dissolved minerals in the water. Now, imagine if you left your faucet dripping long enough to create a mineral deposit that was a meter-plus tall. This process is the basic mechanism behind how speleothems form.

Speleothems are cave formations built by secondary mineral deposition. The majority of speleothems are composed of calcium carbonate (CaCO3) derived from the limestone or dolostone bedrock that comprise a karst. 

As rainwater interacts with CO2 in the atmosphere and in soils, it becomes weakly acidic. When this water travels down through calcium carbonate bedrock, it reacts with and dissolves the bedrock via carbonate dissolution reactions. When the solution reaches the cave, the lower partial pressure in the cave will cause degassing and drive precipitation of CaCO3, developing speleothems over time.

The best-known types of speleothems are dripstones formed by drips of mineral saturated water, just like from a leaky faucet. Drip by drip, dripstones grow either from the roof down or the ground up. Typically, a dripstone will grow less than 10 cm every thousand years. Stalactites hang down from the ceiling, while stalagmites grow up from the ground. (An easy way to remember the difference is that stalactites hold tight on the ceiling while stalagmites might grow to reach the roof.)

Stalactites and stalagmites both come in various forms, depending on the supply and location of their water source. The most delicate type of stalactites are soda straws, which are very long, thin and cylindrical in shape. If a stalactite and a stalagmite grow to reach one another, they will fuse to create a column. Columns reach from the floor to the roof of a cave, making them the most formidable of all speleothems.

In addition to dripstones, flowstones are another type of speleothem. Flowstones are deposited from thin sheets of flowing water, rather than discrete drops. Flowstones tend to coat cave walls and floors. Deposits can even form ‘draperies’ under hanging portions of a wall. These draperies may be layered and slightly transparent, giving them the moniker of cave “bacon.”

Photo sources in order: [x], [x], [x], [x], [x], [x], [x]