The question has answered itself! The generic name for such landscape is 'karst', from the Slovac name for the type-area.
No, alluvial fans are typically found in arid regions and are formed by the deposition of sediment carried by water flowing out of a canyon or valley. Groundwater erosion of limestone forms features such as valleys, sinkholes, and caverns in karst landscapes, where soluble rock like limestone is dissolved by acidic water. These two processes occur in different geologic settings and are not directly related.
Groundwater is typically closest to the Earth's surface in stream valleys due to the topography and geology of these areas. Water from streams can infiltrate into the ground, recharging the groundwater system and bringing it closer to the surface in these valley locations. This proximity to the surface in stream valleys makes them important areas for groundwater recharge and interactions between surface water and groundwater.
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.
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.
in stream valleys
No, alluvial fans are typically found in arid regions and are formed by the deposition of sediment carried by water flowing out of a canyon or valley. Groundwater erosion of limestone forms features such as valleys, sinkholes, and caverns in karst landscapes, where soluble rock like limestone is dissolved by acidic water. These two processes occur in different geologic settings and are not directly related.
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.
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.
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.
The question could also be asked: In an area dominated by sinkholes, the sinkholes can dominate the landscape to produce a series of pits with occasional spires of undissolved rock. This type of landscape is called? Same answer below: KARST - from the Slovenian word "kras" for the type-area.
its called KARST TOPOGRAPHY
Groundwater is typically closest to the Earth's surface in stream valleys due to the topography and geology of these areas. Water from streams can infiltrate into the ground, recharging the groundwater system and bringing it closer to the surface in these valley locations. This proximity to the surface in stream valleys makes them important areas for groundwater recharge and interactions between surface water and groundwater.
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.