(a) State three characteristics of limestone region (b) Describe the formation of limestone pillar. (c) In what two ways is limestone important to man?
Assessment:WAEC SSCE - Geography - 2016 (Practical and Physical Geography)Subject:Geography
(a) State three characteristics of limestone region (b) Describe the formation of limestone pillar. (c) In what two ways is limestone important to man?
(a) Three characteristics of a limestone (karst) region
The surface is dry, with few surface streams because water sinks quickly through the permeable, well-jointed rock.
The land shows underground drainage, with caves, caverns and disappearing streams (swallow holes/sink holes).
Surface features such as clints and grikes (limestone pavements), dolines and dry valleys are common.
Soils are thin and rocky, so the region is generally poor for agriculture.
(b) Formation of a limestone pillar
A limestone pillar (column) forms inside a cave by the joining of a stalactite and a stalagmite.
Rainwater absorbs carbon dioxide from the air and soil to form a weak carbonic acid.
This acidified water seeps through joints and cracks in the limestone and dissolves the calcium carbonate, carrying it in solution into the cave.
When a drop of this water hangs from the cave roof, some water evaporates and a little calcium carbonate is deposited. Repeated dripping builds a downward-growing icicle-like feature called a stalactite.
Water dripping onto the cave floor also deposits calcium carbonate, building an upward-growing feature called a stalagmite.
Over a very long time the stalactite and stalagmite grow towards each other and eventually join to form a continuous limestone pillar (column).
(c) Two ways limestone is important to man
It is used as a major raw material for the manufacture of cement.
It is used in building (as building stone) and in the iron and steel industry as a flux, and can be used to make lime for agriculture.
(a) Three characteristics of a limestone (karst) region
The surface is dry, with few surface streams because water sinks quickly through the permeable, well-jointed rock.
The land shows underground drainage, with caves, caverns and disappearing streams (swallow holes/sink holes).
Surface features such as clints and grikes (limestone pavements), dolines and dry valleys are common.
Soils are thin and rocky, so the region is generally poor for agriculture.
(b) Formation of a limestone pillar
A limestone pillar (column) forms inside a cave by the joining of a stalactite and a stalagmite.
Rainwater absorbs carbon dioxide from the air and soil to form a weak carbonic acid.
This acidified water seeps through joints and cracks in the limestone and dissolves the calcium carbonate, carrying it in solution into the cave.
When a drop of this water hangs from the cave roof, some water evaporates and a little calcium carbonate is deposited. Repeated dripping builds a downward-growing icicle-like feature called a stalactite.
Water dripping onto the cave floor also deposits calcium carbonate, building an upward-growing feature called a stalagmite.
Over a very long time the stalactite and stalagmite grow towards each other and eventually join to form a continuous limestone pillar (column).
(c) Two ways limestone is important to man
It is used as a major raw material for the manufacture of cement.
It is used in building (as building stone) and in the iron and steel industry as a flux, and can be used to make lime for agriculture.