Stalactites are found hanging from the roof of a cave, as opposed to stalagmites, which grow up from the floor. Remembering the difference is easy - stalactites are "tite" to the ceiling!
the ocean
A shake hole is a type of geological depression or sinkhole typically found in karst landscapes, formed by the collapse of a cave roof or the dissolution of underlying limestone. These features often appear as circular or oval-shaped holes and can vary in size. Shake holes can collect water, leading to the formation of temporary ponds or wetlands, and are often associated with unique ecosystems. They are significant in understanding subsurface water flow and the dynamics of karst environments.
The Cave of Wonders
TERRA COTTA ROOF
mad man on the roof
They are formed by the deposit of minerals. They are left behind by evaporation.
stalagtite
stalagtite
A sinkhole is formed when the roof of a cave collapses.
A deposit on the roof of a cave is typically referred to as a stalactite, which is a mineral formation hanging from the ceiling that is formed by the dripping of mineral-rich water. Stalactites are a common feature in caves and can vary in size and shape depending on the minerals present in the water dripping from the cave ceiling.
stalactite
This is called a "Stalactite"
stalactites are a deposit, usually of calcium carbonate, shaped like an icicle,hanging from the roof of a cave or the like, and formed by thedripping of percolating calcareous water.
The calcium deposit formed from water dripping through the roof of a cavern is called a stalactite. Stalactites hang from the roof of the cave and are formed as mineral-rich water drips down and leaves behind calcium deposits that slowly build up over time.
A sinkhole forms.
A large hole formed when a roof of a cave collapses.
A large hole formed when a roof of a cave collapses.