Chalk And Clay Landscapes

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Chalk and Clay Landscapes

Formation
and
Land Use

The main feature of a chalk
landscape is an escarpment.

The escarpment has two
distinctive slopes- a scarp
slope which is steep and a
dip slope which is more
gentle.

The main features of a clay landscape is a vale- an
area of flat land which is a chalk and clay area is
found between the escarpments.

Chalk And Clay Landscapes

Chalk And Clay Landscapes

Chalk And Clay Landscapes

Chalk And Clay Landscapes

Chalk And Clay Landscapes

Chalk And Clay Landscapes

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Introduction In simple words, the term karst describes a distinctive topography that indicates dissolution of underlying soluble rocks by surface water or ground water. Although commonly associated with carbonate rocks (limestone and dolomite) other highly soluble rocks such as evaporates (gypsum and rock salt) can be sculpted into karst terrain. Essential conditions Relatively thick massive soluble rock, i.e., limestone, dolomite, or chalk. Carbonate rocks should be very close to the ground surface. Limestone should be highly folded, faulted or fractured. Considerable relief so that water is capable of circulation to cause typical karst topography. Moderate to heavy rainfall to cause solution of rocks. Development of Karst terrain As rain falls through the atmosphere it picks up carbon dioxide (CO2). When this rain reaches the ground and passes through the soil it picks up more CO2 and forms a weak solution of carbonic acid. As the acidified rain water trickles down through cracks in the limestone, it begins to dissolve the rock. Over time it progressively enlarges the cracks and openings in the ground an underground drainage system starts to develop. SURFACE FEATURES Examples of some of the most common surface karst features encountered are as follows: Sinkhole A topographically closed depression that is circular or elliptical in shape and with steep to vertical sidewalls. Karst springs These are the natural outflows of karst groundwater onto the surface. They form where the water table reaches the surface. Karst valley: Larger karst landforms include dry valleys and gorges, carved by past rivers that now flow underground Solution valley: The collapse of a cavern over a large area can create a feature referred to as a solution valley or basin, sometimes referred to as a karst gulf Disappearing Stream: A stream that disappears into an underground channel and does not reappear in the same, or even in an adjacent, drainage basin. In karst regions, streams commonly disappear into sinkholes and follow channels through caves. SUBSURFACE FEATURES Cave Karst Caves are voids in the rock that form naturally when water erodes away limestone or other soluble rocks. Karst caves are shaped by chemical weathering of the bedrock. These formations are commonly found in limestone areas. Underground Stream: A body of subsurface water flowing through a cave or a group of communicating caves, as in a karst region Stalactites: Stalactites are mineral depositions that originate from the ceiling of a cave and continue to “grow” downward towards the ground. They are rock formations that have a duct in the center, through which water continues to circulate with minerals. Stalagmites: Stalagmites are mineral depositions originated in the floor of a cave and, unlike stalactites; they do not have the central duct such as stalactites They are usually solid shapes much more rounded and irregular than stalactites.

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