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.
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.
silica. +++ Wrong. They are of the mineral Calcite: crystalline calcium carbonate derived from the limestone above the cave.
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.
wind
Limestone
Mineral deposits which develop upwards from a cave floor are known as stagmites. Deposits which form from the ceiling are stalactites.
Limestone
a cave
A cave?
stalactite and stalagmite
A cave or sinkhole.
In a cave? Yes, almost - it's actually the calcium carbonate, the main constituent of limetsone, that is dissolved by the ground-water then precipitated as calcite to form stalactites and stalagmites, and similar deposits.
Stalagmites
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.
It causes dissolution which initially creates vesicles within the limestone and may ultimately result in the formation of cave systems.
They are formed by the deposit of minerals. They are left behind by evaporation.
Maybe it is true. Well I think it is true.