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Karst is a term used to describe landscapes that are formed by chemical weathering process controlled by groundwater activity.
Why does karst topography only exist in some geographic locations? Most regions do not have limestone under the soil. Which is missing in most areas that do not have Karst topography? Limestone.
Limestone stalactites form extremely slowly – usually less than 10cm every thousand years – and radiometric dating has shown that some are over 190,000 years old. Stalactites can also form by a different chemical process when water drips through concrete, and this is much faster.
Sinkholes are formed when the land surface above collapses or sinks into the cavities or when surface material is carried downward into the voids. Drought, along with resulting high groundwater withdrawals, can make conditions favorable for sinkholes to form.
Explanation: Karst is a topography that is formed by solubilization of the rocks like limestone, gypsum, and dolomite in water. The Karst is feature which develops the sinkholes and caves underground because of the underground drainage system develops due to storage of the groundwater.
Rock solubility and water are the primary factors in karst development. Arid climates, whether hot or cold, support little karst. … Consequently, karst landscapes generally lack well-developed surface drainage but have underground drainage conduits, or caves.
The action of surface water and groundwater in the chemical weathering or chemical erosion of soluble carbonate rocks such as magnesium carbonates (dolomites) and calcium carbonates (limestone) produces landforms that are called karst topography.
Karst Topography is the formation of landforms due to solution and deposition on any limestone or dolomitic region by the action of groundwater or surface water. Landforms and its evolution is an important segment of the Geography syllabus of the IAS Exam.
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Evaporites are the most soluble of common rocks; they are dissolved readily to form the same range of karst features that typically are found in limestones and dolomites. … Evaporite outcrops typically contain sinkholes, caves, disappearing streams, and springs.
The U.S. Commonwealth of Puerto Rico has areas of well-developed karst in both Mesozoic and Cenozoic limestones. Most of the larger karst features, including very large and abundant sinkholes, are in the northwestern and north-central parts of the island.
Terms in this set (27)
Karst is a landscape formed by erosion of rocks such as limestone that dissovles in water in a process called chemical weathering.
Limestone areas are predominantly affected by chemical weathering when rainwater, which contains a weak carbonic acid, reacts with limestone. This causes the limestone to dissolve. … Carbon dioxide in the atmosphere forms very dilute carbonic acid when it dissolves in rain.
quiz 11 geol
Question | Answer |
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Which of the following is associated with areas of karst topography? sinkholes – soluble rock – caverns | all of these |
A ________ is the icicle-like speleothem that grows down from the roof of a cavern | stalactite |
The INITIAL stages of Karst Topography are: Sinkholes, potholes, and caverns. Natural void in Rock created by Solution large enough for people to enter.
Globally, 1.18 billion people (16.5% of the global population) live on karst. The highest absolute number occurs in Asia (661.7 million), whereas the highest percentages are in Europe (25.3%) and North America (23.5%).
In this type of karst landscape, the pattern of surface stream channels and stream valleys is still in evidence, though much of the drainage may be underground. Tributary surface streams may sink underground, and there may be streambeds that carry water only during seasons of high flow or during extreme floods.