well to be nice i am not smart
Almost all caves were formed by the actions of water. It dissolves the rock and and forms the caverns and spectacular views.
Stalactites in caves are typically formed from minerals such as calcite or aragonite, which are deposited by dripping water containing dissolved minerals. These minerals precipitate out of the water over time, creating the elongated formations we see in caves.
Caves formed from minerals dissolving and re-forming typically occur in limestone, where acidic groundwater dissolves the limestone rock to create voids. As the water carries the dissolved minerals, it can re-deposit them as stalactites, stalagmites, and other cave formations when conditions change. Over time, these processes shape the cave environment.
Yes, caves are formed when carbonic acid, which is created by the reaction of water with carbon dioxide, dissolves underground limestone. Over time, the dissolved limestone is carried away by water, creating large openings and chambers that we call caves.
Limestone caves are formed through a process called chemical weathering. Rainwater, which is slightly acidic, dissolves the limestone rock over time, creating small cracks. These cracks then widen as more water flows through, eventually forming caves. Additionally, some limestone caves are formed through the erosion of underground rivers.
Most caves are in limestone, and formed by carbonic acid - rain-water acidified by dissolved carbon-dioxide from the atmosphere - dissolving the rock as it sinks through the joints and other fractures in the rock mass.
Caves can also be created by underground water erosion, where water dissolves and carries away rock to form caves in limestone and other soluble bedrock. Additionally, caves can be formed through volcanic activity, such as lava caves formed from flowing lava, or glacier caves created by melting ice in glaciers.
caves
The reaction of carbonic acid in rain and groundwater with the carbonate rock.
Caves and sinkholes are formed by the erosion of soft rock formations by flowing groundwater. Over time, the water dissolves and carries away the rock, creating these underground or surface features.
There are models that show the development of caves under specific conditions in limestone rocks. Of course there are figures that show the formation and the development of a variety of passageways in caves. You can find all these staff in literature related with karst geomorphology.
Erosional caves are formed when water dissolves and carves through soluble rock formations like limestone, creating passageways and chambers underground. Over time, the continuous flow of water erodes the rock and forms distinctive cave structures. As the water table changes and the rock continues to weather, erosional caves can further evolve and change shape.