The question has answered itself! The generic name for such landscape is 'karst', from the Slovac name for the type-area.
no
in stream valleys
A karst topography is that which composes of limestone and its associated features and structures.•Karst topography and caves develop in limestone rocks due to their solubility in dilute acidic groundwater.•The solubility of limestone in water and weak acid solutions leads to karst landscapes.•Regions overlying limestone bedrock tend to have fewer visible above-ground sources (ponds and streams), as surface water easily drains downward through joints in the limestone.•While draining, water and organic acid from the soil slowly (over thousands or millions of years) enlarges these cracks, dissolving the calcium carbonate and carrying it away in solution.•Most cave systems are through limestone bedrock.•Cooling groundwater or mixing of different groundwater will also create conditions suitable for cave formation.Karst topography occurs when the underlying bedrock is dissolved. The bedrock is made of gypsum, limestone or dolomite. This causes sinkholes and caverns to form.
Erosion is displacement of solids (sediment, soil, rock and other particles) usually by the agents of currents such as, wind, water, or ice by downward or down-slope movement in response to gravity or by living organisms (in the case of bioerosion).
How have valleys change over time?How have valleys change over time?How have valleys change over time?
no
The type of landscape you're describing is a karst landscape. It is characterized by soluble bedrock such as limestone that dissolves over time to create features like caverns, sinkholes, and valleys due to the process of chemical weathering.
This type of landscape is likely a karst landscape, characterized by the presence of limestone bedrock that is easily eroded by water. Rainwater dissolves the limestone, leading to the formation of caverns, sinkholes, and deep valleys over time. Karst landscapes are common in regions with high levels of precipitation and are known for their unique topography and underground features.
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.
Karst landscape is a type of landscape where caves, deep valleys, and sinkholes are common. This type of landscape is formed by the dissolution of soluble rocks such as limestone, dolomite, or gypsum by groundwater. The result is distinctive topographical features like caves, sinkholes, and underground drainage systems.
This type of landscape is called a karst landscape. Karst landscapes are characterized by unique landforms such as sinkholes, caves, and underground drainage systems that result from the dissolution of soluble rocks like limestone. These areas often have distinctive surface features and underground networks formed by the erosion of the limestone bedrock.
The landscape you are referring to is likely characterized by karst topography. Karst landscapes are formed by the dissolution of soluble rocks such as limestone, creating features like caves, deep valleys, and sinkholes. These areas often have unique water drainage systems, as water flows underground through the porous rock layers.
A type of landscape that features caves, deep valleys, and sinkholes is called a karst landscape. Karst landscapes are formed when soluble rocks such as limestone or dolomite are eroded by water, creating unique underground drainage systems and surface features.
its called KARST TOPOGRAPHY
in stream valleys
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.
This type of landscape is called a karst landscape. It is characterized by its unique geological features such as limestone caves, sinkholes, and underground streams. Karst landscapes are typically found in regions with abundant rainfall that can dissolve soluble rocks like limestone.