Sedimentary deposits are thought to exist up to 9 kilometers deep. From 9 kilometers to about 18 kilometers metamorphic layers likely exist. However, temperatures would be very high, along with toxic gases like sulfur. So explorable cave passage at that depth is unlikely. Drill cores in Wyoming have found limestone nearly 26,000 feet deep. Can anyone verify if that Mississipian layer is soluble enough to form explorable caves?
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Caves at that depth are not very likely but may form by dissolution by very deep, acidic, geothermal fluids. The normal limit really is not ever so deep below the base level - the altitude of the resurgence for their formative streams. Although they can form deep "sumps" like the U-bend under a sink, the limestone formation's own depth sets the limit, whatever the rock below it. So although sedimentary rock may be 9km deep, the cavernous limestone is likely to be far less.
Also, it's not the solubility of the limestone that's the problem. It's the physical nature of the formation, the relationship to basement and cover rocks, and hydrology of its region that matter.
The Krubera Cave, also known as Voronya Cave, is the deepest cave system on Earth, located in the Arabika Massif of the Western Caucasus in Abkhazia, Georgia. It reaches a depth of 2,197 meters (7,208 feet).
While a funnel-shaped depression of limestone eroded by rainwater is called a limestone pavement or a doline, a cave is a naturally occurring underground void typically formed through chemical weathering and erosion processes such as the dissolution of limestone by acidic groundwater.
If too much limestone dissolves in an underground cave, it can weaken the structural integrity of the cave and lead to collapse or sinkholes. This process is known as karstification and can occur over a long period of time as water continuously dissolves the limestone rock.
I'm not really sure what you had in mind. Given that the cave is in limestone (as the vast majority of them are) there has to be a dimensional limit to the dissolution and erosion processes. The floor is there by default: it is the lowest surface along a passage at that given time in the cave's development.
The ground-water is a solution of calcium carbonate it has dissolved from the limestone above the cave. The mineral is subsequently precipitated as deposits of calcite in the cave: stalatcties & stalagmites, and flowstone on the floor and walls.
No, Hermit Cave is not the deepest cave in Utah. Nutty Putty Cave holds that honor, with a depth of over 380 feet.
The Voronya cave and Vrtoglavica cave
Limestone and limestone formations.
The voronja cave system.
ressseudufoillis
It kind of depends on your definition of deepest cave :) It is usually taken to mean the greatest vertical distance from the cave mouth to its deepest explored point, so the deepest caves actually start pretty high up to begin with. The deepest known cave is Krubera in Georgia at over 2kms deep. It doesn't extend below sea level. However there may be other caves that are deeper, but not explored, and Krubera may well extend to below sea level, we just haven't found a way to get down that far (the limestone massif it is situated in extends below sea level and there have been tests releasing dye into the cave- the dye came out offshore in the black sea I believe). There are plenty of caves that do extend below sea level- all sea caves will have done so at some point.
The Krubera Cave, also known as Voronya Cave, is the deepest cave system on Earth, located in the Arabika Massif of the Western Caucasus in Abkhazia, Georgia. It reaches a depth of 2,197 meters (7,208 feet).
it is a 'karst' cave, i.e. formed by the action of water on limestone.
From dissolution and erosion of limestone by acidic water over time.
Limestone doesn't exactly "help" a cave unless the stalagmite's and such are what you are looking for. Limestone is what creates those.
The joints, bedding-planes and faults provide conduits for water to penetrate the limestone mass; and it is the water, slightly acidified by absorbed carbon dioxide, that dissolves the rock to form the cave.
Limestone caves are sometimes called solution caves because they are formed through a process called solution weathering. This occurs when water containing carbon dioxide dissolves the limestone rock, creating cave systems over time. The dissolved limestone is carried away in the form of a solution, hence the term "solution cave."