A karst topography.
Another name for rough limestone landscape is karst landscape. This type of landscape is characterized by sinkholes, caves, and underground drainage systems resulting from the dissolution of limestone by water.
Limestone is the most common type of rock that underlies a karst landscape. This is because limestone is soluble in water, allowing for the formation of karst topography features such as sinkholes, caves, and underground drainage systems.
Yes! The Burren is a karst-landscape located in western Ireland made up of exposed limestone bedrock.
It is called a karst landscape.
limestone is rough, it crumbles and absorbs water, this is because it is porous which means that it has tiny holes in it. limestone is made up of tiny grains they are circular and are really small
ans2. A karst landscape develops where there is an underlying limestone basement, which is being eroded by rainfall infiltration.Sometimes there are sinkholes, sometimes limestone outcroppings. Generally underground drainage, and generally no surface water.a karst landscape is formed by compressed limestone..
One common name for limestone is calcium carbonate.
The Burren in Ireland is primarily composed of karst landscape made up of limestone rock. This unique geological formation includes limestone pavements, caves, and grykes, which are deep fissures between the rocks.
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.
Limestone is the most common type of rock that underlies a karst landscape. It is a soluble rock that is easily dissolved by water, leading to the formation of features such as sinkholes, caves, and underground rivers.
Rough, and bumpy when freshly fractured, smooth and silky when polished.
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.