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Above limestone deposits
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Marjorie Mary Sweeting has written:
'Karst landforms' -- subject(s): Karst
'Karst in China' -- subject(s): Karst
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James F. Baichtal has written:
'Karst landscapes and associated resources' -- subject(s): Caves, Hydrology, Karst, Karst, Karst Hydrology, Paleontology
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A karst environment, or karst topography.
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An area with many sinkholes is called a sinkhole-prone region. These regions often have underlying soluble rock such as limestone or gypsum that can dissolve over time, leading to the formation of sinkholes. It is important to be cautious in such areas to prevent accidents or property damage.
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A karst specialist is a geologist or hydrologist who specifically studies karst landscapes, which are characterized by soluble rock formations such as limestone that create unique landforms like caves, sinkholes, and underground rivers. These specialists investigate the hydrology, geology, and ecology of karst regions to understand how they form, evolve, and impact the environment.
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The physical weathering and chemical weathering process creates Karst topography and landscapes. Caves and Caverns are common of Karst topography.
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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.
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Karst topography results from the dissolution of limestone or other water soluble rock.
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Adam Karst was born on April 1, 1979, in Southampton, Ontario, Canada.
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Spencer Fleury has written:
'Land use policy and practice on karst terrains' -- subject(s): Karst conservation, Land use, Law and legislation, Karst
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Limestone is usually associated with karst topography.
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West Virginia area. Because of the Lurray Caverns
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Limestone is usually associated with karst topography.
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Slovak Karst National Park was created on 2002-03-01.
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Mole Creek Karst National Park was created in 1996.
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Britni Karst was born on March 16, 1985, in Fort Wayne, Indiana, USA.
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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.
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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.
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No, magma is not required to form karst topography. Karst topography is primarily formed by the dissolution of soluble rocks such as limestone, dolomite, and gypsum by water, leading to the creation of sinkholes, caverns, and underground drainage systems.
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M. M. Sweeting has written:
'Karst landforms' -- subject(s): Karst
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John Karst was born October 15, 1893, in Philadelphia, PA, USA.
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Karst van der Meulen was born in 1949, in Sneek, Friesland, Netherlands.
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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.
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Mass wasting is not required for karst topography to form, as karst topography primarily results from the dissolution of soluble rocks like limestone, dolomite, and gypsum by groundwater. However, mass wasting processes can influence the development of karst features by altering the landscape and accelerating erosion.
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karst topography will contain mostly easily erodable bedrock, such as limestone and dolomite.
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