Stalactites grow down the ceiling.
Stalagmites grow up from the floor.
A good way to remember: C for Ceiling, G for Ground.
If they meet they form a Column!
Stalagmites are the type of speleothems found in limestone caves that grow upward from the floor. They form as mineral-rich water drips from the ceiling and deposits calcium carbonate on the cave floor, gradually building up over time.
In theory yes, if the caves' formative stream cuts down to the insouble basement under the limestone. The visible floor ofa cave is often not the host rock, but sediments, boulders, etc covering the true floor.
Stalactites hang from the ceiling of caves and are formed by mineral-rich water dripping down, while stalagmites grow up from the floor of caves from the mineral deposits left behind by dripping water. Stalactites have a tapering icicle-like shape, while stalagmites are more mound-like and grow upward.
Stalactites form from mineral-laden water dripping from the cave ceiling, leaving behind mineral deposits that build up over time. Stalagmites form as the mineral-rich water drips onto the cave floor and deposits minerals, gradually creating a mound over time that grows upwards.
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.
Limestone, like the walls and roof.
Down from ceiling
Stalagmites are the type of speleothems found in limestone caves that grow upward from the floor. They form as mineral-rich water drips from the ceiling and deposits calcium carbonate on the cave floor, gradually building up over time.
In areas where the rocks are made of limestone, water will dissolve the limestone and form underground caves. In these caves water containing dissolved limestone will drip from the roof. As the drips form some of the water evaporates and limestone is deposited out of solution. Thus, from where the drips are occurring and on the floor below, pilers start to form, the pilers on the floor are called 'stalagmites' and the pilers hanging from the roof are called 'stalactites'.
The Nullarbor Plain was once under the ocean and accumulated layers of limestone over millions of years. The limestone caves formed through a combination of chemical weathering and erosion processes, such as the dissolving of limestone by acidic groundwater and the carving out of caverns by flowing water. This resulted in the unique landscape of the Nullarbor Plain being riddled with limestone caves.
Stalactites hang from the ceiling of limestone caves. They form as mineral-rich water drips from the ceiling and deposits mineral formations, which over time build up into icicle-shaped structures pointing downwards. Stalagmites, on the other hand, rise from the cave floor.
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.
CAVES! These are the dripstones (like stone icicles) that hang from the ceiling (stalactites) or the ones growing upward from the floor (stalagmites). The easiest way to remember which is which--imagine that the stalactites are hanging on tightly to the ceiling.
A stalactite is a structure that hangs from the ceiling of a cave and is formed by the precipitation of minerals from dripping water.
It's more accurate to ask what types of rock hold caves, given that a cave is a lack of rock, as i think that's what you mean! Most caves form in limestone, so the floor, walls and roof are of limestone, as are most of the boulders on the floor. Rivers can also wash in cobbles of other rock, such as Millstone grit from above the Limestone in Carboniferous formations. Lava tubes form in low-viscosity lava flows, so are in basalt or similar low-Si rock. You can also find minor caves and rock-shelters formed in other competent rocks by fluvial or sub-aeriel weathering. E,g, sea-caves, and cavities sand-blasted into sandstone rock-faces by desert sand-storms.
Karst landscapes are known for having numerous caves due to the presence of soluble rocks such as limestone, dolomite, or gypsum. These rocks are easily dissolved by water, leading to the formation of caves, sinkholes, and underground rivers.
Stalactites come down from the ceiling. A good way to remember is to think that to come down from the ceiling, they have to hang on 'tite'.