I'd probably call it a "sinkhole" instead. It may lead to a cave, but the depression itself is not a cave.
No, a funnel-shaped depression of limestone dissolved by rain is called a sinkhole. A cave is a natural underground void or cavity that is typically larger and more complex in structure than a sinkhole.
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.
A vertical gap in limestone is called a grike. The remaining blocks of rock are called klints. The cracks in limestone are called joints.
The rock formed when dissolved minerals cement sediments together is called sedimentary rock. This process occurs over time through the compaction and cementation of particles such as sand, silt, and clay. Examples of sedimentary rocks include sandstone, limestone, and shale.
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.
no
No, a funnel-shaped depression of limestone dissolved by rain is called a sinkhole. A cave is a natural underground void or cavity that is typically larger and more complex in structure than a sinkhole.
Limestone caves are sometimes called solution caves because they are formed through a process called solution weathering. This occurs when water containing carbon dioxide dissolves the limestone rock, creating cave systems over time. The dissolved limestone is carried away in the form of a solution, hence the term "solution cave."
A sinkhole is the term used to describe a depression in the ground caused by a cave collapse. It can also be the result of acidic water dissolving limestone.
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.
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'.
Limestone is called limestone because it has lime in it from the sea water it if formed in.
Recrystallized limestone is generally called marble. Recrystallized quartz sandstone is generally called quartzite. There is no such thing as quartz limestone.
The landscape is called karst topography. This unique landscape forms when limestone bedrock is dissolved by acidic water over time, which leads to the creation of features such as sinkholes, caverns, and underground rivers. Karst topography is commonly found in regions with high levels of limestone, such as in parts of Kentucky, Florida, and China.
A sedimentary rock is a type of rock made from pieces of other rocks, dissolved minerals, or plant and animal matter that collect to form rock layers.
It was called The Great Depression.
The substance dissolved is called the solute. The substance that the solute is dissolved INTO is called the solvent.