Karst Landscapes Flashcards

1
Q

With reference to an Irish landscape, examine the processes, which have influenced the development of any underground feature in a Karst landscape (30m)

A

See notes

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2
Q

Define karst landscape

A

A distinctive landscape with areas of exposed limestone

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3
Q

Define limestone pavement

A

Large flat area of exposed limestone rock that has its soil cover removed

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4
Q

Define clint

A

Flat topped residual blocks that separate grikes

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5
Q

Define grikes

A

Joints that have been widened and deepened due to carbonation

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6
Q

Define swallow hole

A

Large, cone shaped cavities that are open to the sky

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7
Q

Define doline

A

Smallest closed depression. Develops when joints in limestone widen or roof collapses in underground cave

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8
Q

Define uvula

A

Much larger depression, several swallow holes or dolines combine

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9
Q

Define Polje

A

Largest enclosed depression. Steep sides, flat floor, may be several km in area

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10
Q

Define dry valley

A

Valley carved out by a river now without water for all/most of year

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11
Q

Define Turlough

A

Temporary, seasonal lake that occupies hollow in limestone landscape

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12
Q

Define cave

A

Any naturally formed underground passage that is large enough to enter

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13
Q

Define cavern

A

Large underground room

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14
Q

Define stalactites

A

Dripstone deposit; hanging from ceiling of cave

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15
Q

Define stalagmites

A

Dripstone deposits that build from ground up

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16
Q

Define columns

A

When stalactites and stalagmites grow until they join to form a pillar

17
Q

Define curtains

A

Dripstone deposits which form on slanted ceilings, forming a curtain of calcite

18
Q

Define ground water table

A

Area underground that is permanently saturated with water

19
Q

Draw diagram of underground karst features

A

N/A

20
Q

How is limestone pavement formed?

A

Limestone pavements are flat, exposed surfaces of limestone. These features form when a layer of soil is removed, exposing the limestone to chemical weathering. Rainwater, which is slightly acidic due to dissolved carbon dioxide, seeps into cracks in the limestone. Over time, the rainwater dissolves the rock along these cracks, widening them to form deep fissures called grikes. The blocks of limestone left between the grikes are known as clints.

21
Q

How are caves formed?

A

Water flowing through the cracks in limestone dissolves the rock over time, creating large, hollow spaces underground

22
Q

How are stalactites formed?

A

Formed when water containing dissolved calcium bicarbonate drips from the ceiling of a cave. As the water evaporates it leaves behind deposits of calcium carbonate, which grow downwards over time

23
Q

How are stalagmites formed?

A

Water drips onto cave floor, leaving calcium carbonate deposits that grow upward

24
Q

How are pillars formed?

A

Stalagmites and stalactites meet and merge

25
Q

How are swallow holes formed?

A

Natural depressions where rivers or streams disappear underground, dissolving the limestone as they flow into the bedrock

26
Q

Formation of two igneous rocks, examples in Ireland (30m)

A

See notes

27
Q

Examine how different rock types produce distinctive landscapes, with reference to examples that you have studied (30m)

A

See notes

28
Q

Define zone of saturation

A

Rock and soil below the water table

29
Q

When was the limestone in the Burren exposed?

A

12,000 years ago