(a) List three processes of river erosion (b) Outline four characteristics of each of the following sections of a river valley: (i) upper course (ii) middle...
Assessment:WAEC SSCE - Geography - 2014 (Practical and Physical Geography)Subject:Geography
(b) Outline four characteristics of each of the following sections of a river valley: (i) upper course (ii) middle course (iii) lower course.
(a) Processes of river erosion:
Corrasion (abrasion): the wearing away of the bed and banks by the load (sand, pebbles) the river carries and hurls against them.
Attrition: the load particles knock against one another and are broken into smaller, rounder pieces.
Hydraulic action: the sheer force of the moving water loosens and drags away materials from the bed and banks. (Also corrosion/solution - the chemical dissolving of soluble rocks such as limestone.)
(b) Characteristics of each section of a river valley:
(i) Upper course:
Steep gradient and fast, turbulent flow.
Narrow, deep V-shaped valley with vertical (downward) erosion dominant.
Features such as waterfalls, rapids, gorges and interlocking spurs.
Coarse, angular load and a small, swift channel.
(ii) Middle course:
Gentler gradient and increased volume from tributaries.
Valley widens; lateral (sideways) erosion becomes important.
Development of meanders and a wider floodplain begins.
Both erosion and deposition occur; load becomes finer.
(iii) Lower course:
Very gentle gradient and slow, wide flow with large volume.
Broad, flat floodplain with deposition dominant.
Features such as large meanders, ox-bow lakes, levees, deltas and estuaries.
Fine load (silt and mud) is carried and deposited.
Corrasion (abrasion): the wearing away of the bed and banks by the load (sand, pebbles) the river carries and hurls against them.
Attrition: the load particles knock against one another and are broken into smaller, rounder pieces.
Hydraulic action: the sheer force of the moving water loosens and drags away materials from the bed and banks. (Also corrosion/solution - the chemical dissolving of soluble rocks such as limestone.)
(b) Characteristics of each section of a river valley:
(i) Upper course:
Steep gradient and fast, turbulent flow.
Narrow, deep V-shaped valley with vertical (downward) erosion dominant.
Features such as waterfalls, rapids, gorges and interlocking spurs.
Coarse, angular load and a small, swift channel.
(ii) Middle course:
Gentler gradient and increased volume from tributaries.
Valley widens; lateral (sideways) erosion becomes important.
Development of meanders and a wider floodplain begins.
Both erosion and deposition occur; load becomes finer.
(iii) Lower course:
Very gentle gradient and slow, wide flow with large volume.
Broad, flat floodplain with deposition dominant.
Features such as large meanders, ox-bow lakes, levees, deltas and estuaries.
Fine load (silt and mud) is carried and deposited.