Drainage of West Africa

Drainage of West Africa refers to the system of rivers and streams that collect and transport water across West African countries into the Atlantic Ocean, Lake Chad, or inland basins. The region has three main drainage systems: long rivers crossing multiple countries, short coastal rivers, and inland drainage systems.

Quick Summary

  • West Africa has three distinct drainage systems based on length and destination
  • Long rivers like Niger, Volta, and Senegal flow through multiple countries
  • Short rivers drain directly into the Atlantic Ocean along the coast
  • Inland drainage systems flow into Lake Chad with no ocean outlet
  • River patterns are influenced by relief, climate, and geological structure

Understanding West African Drainage Systems

When we talk about drainage in West Africa, we mean how rivers collect rainwater and move it across the land. Think of it like gutters on a roof – they collect water and direct it somewhere. In West Africa, rivers collect water from rains and move it either to the Atlantic Ocean or to Lake Chad.

West Africa receives heavy rainfall, especially in coastal areas where some places get over 3,000mm of rain each year. All this water needs somewhere to go. The pattern of how water flows across West Africa creates three major drainage types.

The Three Main Drainage Systems

1. Long Rivers (Trans-boundary Rivers)

Long rivers are the giants of West Africa. They flow through many countries before reaching the sea. These rivers can be over 1,000 kilometres long and pass through different climate zones.

River Niger is the longest river in West Africa at 4,180 kilometres. It starts in the Fouta Djallon highlands in Guinea, flows northeast through Mali, then curves southeast through Niger and Nigeria before emptying into the Atlantic Ocean through the Niger Delta. About 180 million people depend on the Niger River for water, farming, and fishing.

River Volta stretches 1,600 kilometres and drains much of Ghana, Burkina Faso, Togo, Benin, and Ivory Coast. The Black Volta and White Volta join to form the main Volta River. The Akosombo Dam on this river created Lake Volta, one of the world’s largest man-made lakes.

River Senegal flows 1,086 kilometres through Guinea, Mali, Mauritania, and Senegal. It forms part of the border between Senegal and Mauritania before entering the Atlantic Ocean at Saint-Louis.

River Gambia runs 1,130 kilometres from the Fouta Djallon in Guinea through Senegal and The Gambia. The country of The Gambia exists as a narrow strip along both banks of this river.

2. Short Rivers (Coastal Rivers)

Short rivers flow directly from highland areas to the Atlantic Ocean. They are typically less than 500 kilometres long and stay within one or two countries. Because they flow short distances, they move slowly and don’t cut deep valleys.

Examples include:

  • River Ogun (480km) in southwest Nigeria flows from Oyo State to Lagos Lagoon
  • River Osun (330km) in Nigeria joins the Lagos Lagoon system
  • River Tano (400km) flows through Ghana and Ivory Coast
  • River Sewa (240km) in Sierra Leone flows through diamond-mining areas
  • River Cross (489km) forms part of Nigeria-Cameroon border
  • River Pra (240km) in Ghana empties near Shama

These rivers swell quickly during rainy season and shrink dramatically in dry season. Local communities use them for fishing and small-scale farming along their banks.

3. Inland Drainage Rivers

Inland drainage rivers flow into Lake Chad instead of the ocean. As water reaches Lake Chad, it either evaporates or soaks into the ground. There is no river flowing out of Lake Chad to the sea.

Key inland drainage rivers include:

  • River Yobe (1,200km) flows from northern Nigeria into Lake Chad
  • River Hadejia (combines with Jama’are to form Yobe)
  • Logone River (965km) flows from Cameroon through Chad
  • Chari River (1,400km) provides about 90% of Lake Chad’s water
  • Yedseram River flows from Nigeria’s Biu Plateau toward Lake Chad

Lake Chad has shrunk dramatically over the past 50 years. In the 1960s, it covered 25,000 square kilometres. Today it covers less than 2,000 square kilometres due to climate change, increased irrigation, and reduced rainfall. This affects millions who depend on the lake for fishing and farming.

Factors Influencing Drainage Patterns

Relief and Topography

The shape of the land determines where rivers flow. Water always flows from high ground to low ground. West Africa has several highland areas that act as water towers, feeding many rivers.

The Fouta Djallon highlands in Guinea (average elevation 900m) are called the “water tower of West Africa” because so many major rivers start there – the Niger, Senegal, and Gambia all begin in these mountains.

Other important highland sources include the Jos Plateau in Nigeria (1,200m), the Adamawa Highlands (2,000m), and the Guinea Highlands along the Guinea-Liberia border.

Climate and Rainfall

Rainfall patterns determine how much water flows in rivers. Coastal areas receive 2,000-4,000mm of rain per year, while Sahel areas receive only 200-600mm. Rivers in wetter areas carry more water year-round.

The seasonal pattern of rain means most West African rivers have high water from June to October (rainy season) and low water from November to May (dry season). Some small rivers completely dry up during harmattan.

Geological Structure

Rock types affect how water moves underground and on the surface. Hard crystalline rocks in highland areas don’t absorb much water, so rain quickly flows into rivers. Sandy areas absorb water, so fewer surface rivers form there.

Ancient rock formations created the basins that rivers flow through. The Niger River’s unusual boomerang shape exists because it flows through two different ancient valleys.

Comparison of West African Drainage Systems

Feature Long Rivers Short Rivers Inland Drainage
Length Over 1,000km Less than 500km Varies (200-1,400km)
Countries crossed 3-6 countries 1-2 countries 2-3 countries
Destination Atlantic Ocean Atlantic Ocean Lake Chad (no ocean outlet)
Flow speed Fast in upper course, slow in lower Slow throughout Slow, decreasing near lake
Examples Niger, Volta, Senegal, Gambia Ogun, Tano, Sewa, Cross Yobe, Hadejia, Logone, Chari
Seasonal variation Moderate (large volume) Extreme (may dry up) Extreme (depends on Sahel rains)
Navigation use Important for transport Limited (too shallow) Local fishing only
Economic importance Very high (regional trade) Moderate (local use) High (Lake Chad fisheries)

Economic Importance of West African Drainage

Rivers serve many purposes in West Africa. Farmers use river water for irrigation to grow rice, vegetables, and sugarcane. In Nigeria’s Fadama areas along river valleys, farmers produce tomatoes, peppers, and onions throughout the year.

Fishermen catch tilapia, catfish, and other species. Lake Chad alone supports fishing industries that feed millions of people in Nigeria, Niger, Chad, and Cameroon.

Rivers provide water for drinking and household use in cities like Lagos, Accra, Bamako, and Niamey. Treatment plants along rivers supply clean water to urban populations.

Hydroelectric dams on rivers generate electricity. The Kainji Dam on River Niger produces 760 megawatts. The Akosombo Dam in Ghana produces 1,020 megawatts. These dams power industries and homes.

Some rivers serve as transport routes. Boats carry goods and passengers along the Niger River between Mali, Niger, and Nigeria. During high water season, large boats can travel inland for hundreds of kilometres.

Common Exam Mistakes

WAEC examiners report these frequent errors:

  • Confusing river length with drainage area: Students write that River Niger is longest because it drains the largest area. Length and drainage area are different. Niger is longest (4,180km) but Volta drains a larger area relative to its length.
  • Listing rivers without classification: Questions ask you to “classify” or “group” West African rivers, but students just list river names. Always organize your answer by drainage type.
  • Wrong river destinations: Some students write that inland drainage rivers flow into the ocean. Remember: inland drainage means NO ocean outlet – water ends in Lake Chad.
  • Mentioning rivers outside West Africa: River Nile and Congo are NOT West African rivers. Stay within the West African region (16 countries from Mauritania to Nigeria).
  • Failing to explain factors: When asked to explain factors affecting drainage, don’t just write “relief” or “climate” – explain HOW these factors influence where and how rivers flow.

Practice Questions

Multiple Choice Questions

1. Which of these is an inland drainage river in West Africa?
a) River Volta
b) River Yobe ✓
c) River Senegal
d) River Tano

2. The longest river in West Africa is:
a) River Volta
b) River Senegal
c) River Niger ✓
d) River Gambia

3. Which highland area is called the “water tower of West Africa”?
a) Jos Plateau
b) Adamawa Highlands
c) Fouta Djallon ✓
d) Guinea Highlands

4. Short rivers in West Africa are characterized by:
a) Fast flow and deep valleys
b) Crossing multiple countries
c) Slow flow and shallow channels ✓
d) Year-round high water levels

Essay Questions

1. Explain the three main types of drainage systems in West Africa, giving two examples of each. (10 marks)

Examiner’s tip: Use clear headings for each drainage type. Define the type, mention its characteristics, then give specific river examples with their lengths or countries they cross. Don’t just list rivers – explain what makes each type different.

2. Describe four factors that influence drainage patterns in West Africa. (8 marks)

Examiner’s tip: Each factor needs explanation, not just naming. For example, don’t just write “relief” – explain that rivers flow from highlands to lowlands, and mention specific highlands like Fouta Djallon. Give 2 marks worth of detail per factor.

3. Discuss the economic importance of rivers in West Africa. (10 marks)

Examiner’s tip: Cover at least five different uses: irrigation, fishing, drinking water, hydroelectric power, transportation. Give specific examples like dam names, crops grown, or cities supplied. Each use should have 2 marks of detail.

Memory Aids

Three Drainage Types – “L.S.I.”

  • Long rivers (Niger, Volta, Senegal, Gambia)
  • Short rivers (Ogun, Tano, Sewa, Cross)
  • Inland drainage (Yobe, Hadejia, Logone, Chari)

Major Long Rivers – “Never Vote Silly Guys”

  • Niger (4,180km – longest)
  • Volta (1,600km)
  • Senegal (1,086km)
  • Gambia (1,130km)

Where Rivers Start – “Fouta Feeds Four”
Fouta Djallon highlands feed four major rivers: Niger, Senegal, Gambia, and tributaries of Volta.

Related Topics

  • Features and Characteristics of West African Rivers
  • Climate of West Africa
  • Relief and Physical Features of West Africa
  • Economic Activities in West Africa
  • Water Resources Management in West Africa

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