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.
turn up dats it
carbonic acid
its called KARST TOPOGRAPHY
Perhaps you search for sink holes.
Common features in karst topography include sinkholes, caves, underground rivers, and disappearing streams. Karst landscapes are characterized by the dissolution of soluble rocks such as limestone, resulting in unique surface and subsurface landforms.
The physical weathering and chemical weathering process creates Karst topography and landscapes. Caves and Caverns are common of Karst topography.
Common karst landforms include sinkholes, caves, disappearing streams, and karst towers. These landforms are a result of the dissolution of soluble rocks such as limestone, dolomite, and gypsum by groundwater. Karst landscapes are known for their unique and often fragile features created by the erosion of these types of rocks.
A landform not common in karst topography is typically a flat plain or plateau. Karst topography is known for its distinctive features such as sinkholes, caves, and disappearing streams, which are caused by the dissolution of soluble rocks like limestone. Flat plains or plateaus are less likely to form in karst areas due to the erosional processes that create the unique karst features.
Above limestone deposits
Limestone is a common type of rock found in karst areas. Karst landscapes are characterized by the presence of limestone rock that is susceptible to dissolution by natural processes, creating unique surface and subsurface features such as sinkholes, caves, and disappearing streams.
Surface drainage systems.
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Common features in karst topography include sinkholes, caves, disappearing streams, underground drainage systems, and limestone pavements. Karst landscapes are characterized by the dissolution of soluble rocks such as limestone, dolomite, and gypsum, resulting in unique landforms and drainage patterns.
A plateau is not common in an area of karst topography. Karst topography is characterized by sinkholes, caves, and underground drainage systems resulting from the dissolution of soluble rocks like limestone, which typically form distinct landforms such as hills, towers, and valleys, but not plateaus.
James C. Currens has written: 'Flooding of the Sinking Creek karst area in Jessamine and Woodford counties, Kentucky' -- subject(s): Floods 'Mass flux of agricultural nonpoint-source pollutants in a conduit-flow-dominated karst aquifer, Logan County, Kentucky' -- subject(s): Agricultural pollution, Groundwater, Karst Hydrology, Nonpoint source pollution, Pollution 'Characterization and quantification of nonpoint source pollution in a conduit-flow dominated karst aquifer underlying an extensive use agricultural region--phase III' -- subject(s): Agricultural pollution, Groundwater, Karst Hydrology, Nonpoint source pollution, Pollution
Three states where you can find karst topography are Kentucky, Florida, and Missouri. Karst topography is characterized by sinkholes, caves, and underground drainage systems formed by the dissolution of soluble rocks like limestone.