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Karst topography is created by chemical weathering, specifically by the dissolution of soluble rocks such as limestone and dolomite. This process forms features like sinkholes, caves, and underground drainage systems.
Caves usually and mostly forms in sedimentary rocks. Example, Limestone.
relief and topography both gives us the knowledge of the elevation and the type of land forms of a place but topography also tells us about the surface shape and the distribution of land forms in a region.
Limestone is the type of rock that usually underlies a karst topography. Limestone is soluble in water, allowing for the formation of sinkholes, caves, and other karst features through the process of erosion.
Sinkholes, caves, disappearing streams, and limestone pavements are major landforms associated with Karst Topography.
The physical weathering and chemical weathering process creates Karst topography and landscapes. Caves and Caverns are common of Karst topography.
its called KARST TOPOGRAPHY
In places that are mostly humid where Karst topography can usually be found. Karst topography can be best described as landscapes that have underground systems like caves.
There is not a particular kind of limestone needed to make a canyon or valley. They and caves form through erosion of most limestones, but their development is subject to a good deal of local geological and hydrological control.
Limestone is the type of rock often associated with the formation of caverns and karst topography. It is composed mainly of calcium carbonate, which is soluble in water, allowing for the creation of caves, sinkholes, and other karst features through the process of dissolution.
The acid in the water forms it
Yes, soluble rocks, such as limestone, gypsum, and salt, are commonly associated with areas of karst topography. This type of landscape forms as a result of the dissolution of these soluble rocks by water, leading to features like sinkholes, caves, and underground rivers. The process of chemical weathering creates unique geological formations and drainage patterns typically seen in karst regions.