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Probably consolidated sediments (sedimentary rock), then the rock basalt.
Is the morphological landscape of dissoloution and percipation of near surface bed rock.
Karst topography is usually formed when acidic water dissolves layers of bedrock. Common attributes include sinkholes and other depressions in the rock.
False. The oceans are underlain by marine sediments and then a type of igneous rock known as basalt.
Karst topography is a landscape shaped by the dissolution of a layer or layers of soluble bedrock, usually carbonate rock such as limestone or dolomite.[1]Due to subterranean drainage, there may be very limited surface water, even to the absence of all rivers and lakes. Many karst regions display distinctive surface features, with sinkholes or dolines being the most common. However, distinctive karst surface features may be completely absent where the soluble rock is mantled, such as by glacial debris, or confined by a superimposed non-soluble rock strata. Some karst regions include thousands of caves, even though evidence of caves that are big enough for human exploration is not a required characteristic of karst.
limestone
limestone
limestone
Limestone is usually associated with karst topography.
Limestone is usually associated with karst topography.
Limestone is usually associated with karst topography.
No it is definitely not.
Karst topography results from the dissolution of limestone or other water soluble rock.
limestone
This is known as the asthenosphere.
Karst Limestone
A wave cut platform is formed. == ==