Solution cave features

Solutional sculpturings

Superimposed on the walls of cave passages are many small solutional sculpturings that record further details of water flow. Pockets of various sizes and kinds are cut back into the walls and ceiling. Some of these have ax-blade shapes and form where water seeping into the cave passage is mixed with the water already in the passage. If the seepage water and the passage water have the correct chemistry, corrosive water forms in the mixing zone and dissolves away the joint-controlled wall and ceiling pockets. Other wall and ceiling pockets are rounded kettle holes or circular cylinders that extend into the solid bedrock of the ceiling with no obvious influence from joints. The ceilings of tropical caves often contain large numbers of the cylindrical cavities, which are used as roosting places by bats. Small secondary channels are carved into the floors or ceilings by flowing water. Floor channels provide evidence of the presence of small later-stage streams that occupied the cave passage after it had been drained of its original flow. Ceiling channels are thought to be the result of upward solutional erosion by cave streams that occurred when the main channel was completely filled with clays, sand, and gravel.

Among the most significant of the solutional sculpturings are the small scooplike depressions known as scallops. Scallops vary in size from a few centimetres to more than one metre. They are asymmetrical in cross section, having a steep wall on the upstream side and a gentler slope on the downstream side. Scallops thus provide information as to the direction of water flow in passages that have been dry for hundreds of thousands of years. The size of a scallop is inversely proportional to the flow velocity of water in the passage. As a consequence, scallops serve not only as paleo-direction indicators but also as paleo-flow meters. Scallops that are a few centimetres wide indicate flow velocities on the order of a few metres per second. The largest scallops, those that are more than one metre wide, indicate flow velocities of a few centimetres per second.

The flow velocity of conduit water is sufficient to transport clastic sediment through a cave system. The clastic material is derived from borderlands where it is carried into the karst by sinking streams, from overlying sandstone and shale caprock, from surface soils that are washed underground through sinkholes, and from the insoluble residue of the limestone bedrock. Some of these clastic materials are deposited in caves where they remain as clay, silt, and sand on the cave floors. Some drainage systems carry larger cobble- and boulder-sized materials that are often found in cave streambeds. Most caves have undergone several periods of deposition and excavation, and so remnant beds and pockets of sediment have been left high on cave walls and ledges. These sediments contain iron-bearing magnetic particles, which indicate the position of the Earth’s magnetic field at the time when the sediments were deposited. The age of the sedimentary deposits can be determined by measuring the paleomagnetic record in cave sediments and correlating it with the established geomagnetic polarity time scale. Using this method, investigators have ascertained that the age of the sediments in Mammoth Cave is more than 2,000,000 years.

Depositional materials and features







