normally damp weather with a lot of rain or snow depending where you are in the world
The weathering process is chemical weathering, specifically dissolution. The acid in the rain reacts with the calcium carbonate in the limestone, causing it to dissolve and wear away over time.
Limestone is dissolved by carbonic acid through a process called chemical weathering. Carbonic acid forms when rainwater combines with carbon dioxide in the atmosphere or soil, creating a weak acid that gradually breaks down the calcium carbonate in limestone over time.
Limestone is the type of rock that is commonly dissolved by water to form stalactites and stalagmites in caves. This process occurs over thousands of years when calcium carbonate in the limestone is slowly deposited as water drips from the cave ceiling.
The rocks found in most caves are typically sedimentary rocks such as limestone, shale, and sandstone. These types of rocks are more susceptible to erosion by water, which is a common process in cave formation. Additionally, sedimentary rocks often contain minerals that are easily dissolved by water, leading to the creation of cave features like stalactites and stalagmites.
You would likely find sedimentary rock in caves, as it is common for caves to form in limestone, dolomite, or sandstone due to the processes of erosion and underground water flow. Igneous and metamorphic rocks are less common in caves, but can also be present in certain geological settings.
chemical weathering called karsting and it createskarst topography. ... Dissolution of soluble limestone creates limestone cavessource yahoo answers
Carbonic acid
igneous rock
differential weathering water wears away some areas but not all
The weathering process is chemical weathering, specifically dissolution. The acid in the rain reacts with the calcium carbonate in the limestone, causing it to dissolve and wear away over time.
It depends on the cave. Since many caves are limestone (water carves it nicely), you usually find limestone. But granite is common in New Hampshire & Vermont.
Limestone is dissolved by carbonic acid through a process called chemical weathering. Carbonic acid forms when rainwater combines with carbon dioxide in the atmosphere or soil, creating a weak acid that gradually breaks down the calcium carbonate in limestone over time.
Limestone is the type of rock that is commonly dissolved by water to form stalactites and stalagmites in caves. This process occurs over thousands of years when calcium carbonate in the limestone is slowly deposited as water drips from the cave ceiling.
Physical weathering
The rocks found in most caves are typically sedimentary rocks such as limestone, shale, and sandstone. These types of rocks are more susceptible to erosion by water, which is a common process in cave formation. Additionally, sedimentary rocks often contain minerals that are easily dissolved by water, leading to the creation of cave features like stalactites and stalagmites.
The 2 kinds of weathering are the Mechanical or Physical Weathering and the Mechanical Weathering.
Mammoth Cave is typically associated with the Happy Hollow Member of the Girkin Limestone, which is a fossiliferous, marine limestone deposited in a shallow, tropical sea during the Mississippian Period. This limestone contains abundant fossilized shell fragments and marine organisms, reflecting the environment in which it was formed.