(a) List three landforms that are associated with extrusive volcanic action. (b) With the aid of a diagram, describe the characteristics and mode of formati...
Assessment:WAEC SSCE - Geography - 2021 (Practical and Physical Geography)Subject:Geography
(a) List three landforms that are associated with extrusive volcanic action.
(b) With the aid of a diagram, describe the characteristics and mode of formation of laccoliths.
(a) Landforms associated with extrusive volcanic action
Lava plains or lava plateaux.
Shield volcanoes (basic lava cones).
Composite cones (strato-volcanoes).
(b) Laccolith
A laccolith is a concordant intrusive igneous body formed when viscous magma is injected between sedimentary rock beds. It has a nearly flat base and a rounded or dome-shaped upper surface, giving it a mushroom-like form.
Diagram of a laccolith
A laccolith is a concordant intrusion with a flat base and a domed roof that uplifts the overlying rock strata.
Characteristics
It is an intrusive igneous landform, formed below the Earth's surface.
It lies concordantly, that is, generally parallel to the bedding planes of the surrounding sedimentary rocks.
It has a broad, almost flat floor and a convex, dome-shaped roof.
It arches and uplifts the overlying sedimentary strata.
It is commonly fed from below by a narrow pipe-like conduit or dyke.
It is composed of hard igneous rock and may stand out as a rounded hill or upland after denudation removes the cover rocks.
Mode of formation
Viscous magma rises from the interior through a line of weakness or a pipe-like conduit.
On reaching a resistant rock layer, the magma cannot easily continue vertically upward.
It therefore spreads sideways along a bedding plane between sedimentary strata.
Because the magma is thick and does not spread far, it accumulates locally and pushes the overlying beds upward into a dome.
The magma cools and solidifies beneath the arched strata to form a laccolith.
Subsequent erosion may remove the overlying sedimentary rocks and expose the resistant laccolith as an upland feature.
(a) Landforms associated with extrusive volcanic action
Lava plains or lava plateaux.
Shield volcanoes (basic lava cones).
Composite cones (strato-volcanoes).
(b) Laccolith
A laccolith is a concordant intrusive igneous body formed when viscous magma is injected between sedimentary rock beds. It has a nearly flat base and a rounded or dome-shaped upper surface, giving it a mushroom-like form.
Diagram of a laccolith
A laccolith is a concordant intrusion with a flat base and a domed roof that uplifts the overlying rock strata.
Characteristics
It is an intrusive igneous landform, formed below the Earth's surface.
It lies concordantly, that is, generally parallel to the bedding planes of the surrounding sedimentary rocks.
It has a broad, almost flat floor and a convex, dome-shaped roof.
It arches and uplifts the overlying sedimentary strata.
It is commonly fed from below by a narrow pipe-like conduit or dyke.
It is composed of hard igneous rock and may stand out as a rounded hill or upland after denudation removes the cover rocks.
Mode of formation
Viscous magma rises from the interior through a line of weakness or a pipe-like conduit.
On reaching a resistant rock layer, the magma cannot easily continue vertically upward.
It therefore spreads sideways along a bedding plane between sedimentary strata.
Because the magma is thick and does not spread far, it accumulates locally and pushes the overlying beds upward into a dome.
The magma cools and solidifies beneath the arched strata to form a laccolith.
Subsequent erosion may remove the overlying sedimentary rocks and expose the resistant laccolith as an upland feature.