If you mean from the cave roofs, and the caves are in limestone, then 'stalactites'. The term refers to such formation in any karst cave irrespective of location.
Caves can be found in various parts of the US, with some notable locations including Carlsbad Caverns National Park in New Mexico, Mammoth Cave National Park in Kentucky, and Luray Caverns in Virginia. These caves offer unique geological formations and underground ecosystems for visitors to explore.
Caves are typically formed in rock formations such as limestone, marble, or volcanic rock. The creation of caves is primarily influenced by water erosion, chemical weathering, and geological processes over millions of years. Inside caves, various mineral deposits and formations such as stalactites and stalagmites can be found.
A speleologist is a person who studies caves. The word speleology, which refers to the scientific study of caves, comes from the Latin word spelaeum (cave) + the Greek word logos (discourse).
People can damage caves by touching or removing formations, littering, defacing walls with graffiti, introducing pollutants, and introducing non-native species. These actions can harm the delicate ecosystem inside caves and degrade natural formations that have taken thousands of years to form.
Columns in caves are tall, cylindrical formations that are created when stalactites from the ceiling and stalagmites from the floor meet and fuse together. They can grow over thousands of years as mineral deposits accumulate in caves. Columns are common features in caves with significant limestone formations.
Stalactites refers to the formations that grow downward from the top of the cave.
Formations that occur in caves include stalactites (hanging formations), stalagmites (rising formations), flowstones (sheet-like deposits), columns (stalactites and stalagmites joining), and helictites (twisted, branching formations). These formations are created by the slow deposition of minerals from dripping water over thousands of years.
Stalactites are stony formations that hang from the ceilings of caves.
Caves formed in limestone, as the vast majority are - but there are many caves that contain few or no "speleothems" as the formations are know collectively. The distribution and scale of the formations is subject to many, complex factors.
StalagmitesFlow stoneandTiered stalagmites.
Caves can be found in various parts of the US, with some notable locations including Carlsbad Caverns National Park in New Mexico, Mammoth Cave National Park in Kentucky, and Luray Caverns in Virginia. These caves offer unique geological formations and underground ecosystems for visitors to explore.
caves
Caves are typically formed in rock formations such as limestone, marble, or volcanic rock. The creation of caves is primarily influenced by water erosion, chemical weathering, and geological processes over millions of years. Inside caves, various mineral deposits and formations such as stalactites and stalagmites can be found.
Stalactites - comprised of the mineral calcite, and although not all limestone caves contain stalactites, these formations always hang from the roofs otherwise they would not be stalactites!
The scientific study of caves is referred to as speleology. It involves the exploration, mapping, and study of caves, including their geological formations, ecosystems, and history.
A speleologist is a person who studies caves. The word speleology, which refers to the scientific study of caves, comes from the Latin word spelaeum (cave) + the Greek word logos (discourse).
In Mauritius, caves are primarily found in the Black River Gorges National Park and the surrounding regions, such as the south and southwest of the island. Notable caves include the Tamarind Falls Caves and the caves near the village of La Vallée des Couleurs. Additionally, the coastal areas, particularly around the island's southwest, feature limestone caves formed by erosion. These natural formations often attract adventure seekers and nature enthusiasts.