Examkin

Geography of Africa

145 questions

All types145Multiple choice75Numeric1Matching35Ordering34
Question 41Question →

The interior physiography of Africa is dominated by a characteristic basin-and-swell structure, forming vast inland depressions such as the Congo, Chad, and Kalahari Basins separated by intervening high plateaus. Which of the following geological processes responsible for this broad landscape architecture contrasts it structurally from the East African Rift System?

Show answer & explanation

Answer: Widespread epeirogenic warping of the stable Precambrian crystalline shield, resulting in broad crustal sagging and gentle uplift rather than localized rift faulting.

Answer

Widespread epeirogenic warping of the stable Precambrian crystalline shield, resulting in broad crustal sagging and gentle uplift rather than localized rift faulting.
The interior relief of Africa is famously described as a 'basin and swell' topography. Because the continent is anchored by an ancient, stable crystalline shield, continental forces express primarily through epeirogenesis—slow, large-scale vertical crustal warping. Downwarping forms immense inland basins (such as the Congo, Chad, and Kalahari Basins), while upwarping creates intervening swells and plateaus. This structural flexing contrasts directly with localized tensional rifting seen in the East African Rift System.

Step-by-Step Solution

1
Analyze the structural landform characteristic of interior Africa.
Interior Africa consists of ancient, rigid Precambrian basement rock (cratons) forming a vast plateau landscape.
Understanding the geological foundation of the continent is essential to determining its dominant deformation mechanisms.
2
Distinguish between structural mechanisms: epeirogeny, orogeny, and rifting.
Epeirogenic movements cause slow, broad vertical uplift (swells) and subsidence (basins) over vast areas without intense folding or localized faulting. Rifting involves tensional fracturing, and orogeny involves compressional folding.
Comparing these tectonic processes clarifies why features like the Congo and Chad Basins differ structurally from mountain belts or fault rifts.
3
Identify the correct geological process forming Africa's basin-and-swell relief.
Epeirogenic warping of the continental shield created broad internal drainage basins (e.g., Congo, Chad, Kalahari) surrounded by raised swells (e.g., Bié Plateau, Jos Plateau).
This tectonic flexure directly accounts for the unique macro-relief profile of interior Africa.

Key Concept

Basin and Swell Structure of Africa via Epeirogenic Warping
Question 42Question →

Which of the following major African landforms is an extensive high plateau formed primarily by basaltic volcanic activity?

Show answer & explanation

Answer: The Ethiopian Highlands

Answer

The Ethiopian Highlands
The Ethiopian Highlands were created by extensive fissure eruptions of basaltic lava during the Tertiary period, producing a vast, elevated volcanic plateau often called the 'Roof of Africa'.

Step-by-Step Solution

1
Analyze the landform description provided in the question stem.
The target landform must be an elevated plateau of volcanic origin.
The question specifies both the physical structure (high plateau) and the formation mechanism (volcanic activity).
2
Evaluate the relief features of Africa against this geological origin.
The Ethiopian Highlands were formed by massive flood basalt lava outpourings associated with rift system development.
This physical region is widely recognized as Africa's largest continuous high-altitude volcanic plateau structure.

Key Concept

Relief and Major Landforms of Africa - Volcanic Plateaus
Question 43Question →

A geographic research team is tracing political divisions across Southern Africa along the Tropic of Capricorn (23.5∘S23.5^\circ\text{S}) from the Atlantic coast eastward to the Indian Ocean. Which of the following lists represents the correct sequence of sovereign nations intersected by this line of latitude in order from west to east?

Show answer & explanation

Answer: Namibia, Botswana, South Africa, Mozambique, and Madagascar

Answer

The correct sequence of sovereign nations intersected by the Tropic of Capricorn (23.5∘S23.5^\circ\text{S}) from west to east is Namibia, Botswana, South Africa, Mozambique, and Madagascar.
The Tropic of Capricorn (23.5∘S23.5^\circ\text{S}) enters the African continent at Namibia's Atlantic coastline, travels eastward through central Botswana, passes through the northern region (Limpopo Province) of South Africa, continues across southern Mozambique, and crosses the Indian Ocean to cut through southern Madagascar. This yields the exact sequential order: Namibia, Botswana, South Africa, Mozambique, and Madagascar.

Step-by-Step Solution

1
Identify the latitude line and starting boundary
The Tropic of Capricorn is located at approximately 23.5∘S23.5^\circ\text{S} latitude and enters western Africa at the Atlantic Ocean coast.
Establishing the precise geographic coordinates defines the spatial corridor being analyzed.
2
Trace the latitude line eastward across mainland Southern Africa
The parallel 23.5∘S23.5^\circ\text{S} enters Namibia on the Atlantic coast, moves east through central Botswana, cuts across the northern Limpopo province of South Africa, and traverses southern Mozambique to reach the Indian Ocean.
Spatial evaluation of political boundaries confirms which mainland countries are traversed by 23.5∘S23.5^\circ\text{S} latitude.
3
Account for island nations in the Indian Ocean section
Crossing the Mozambique Channel, 23.5∘S23.5^\circ\text{S} intersects the southern region of the island nation of Madagascar.
Political divisions of Africa include offshore island states crossed by major lines of latitude.

Key Concept

Latitudinal Location and Political Boundaries of Southern Africa
Estimated Time:2m 0s
Question 44Question →

Which climatic zone in Africa is characterized by consistently high temperatures throughout the year and a bimodal (double peak) annual rainfall distribution?

Show answer & explanation

Answer: Tropical Equatorial Climate

Answer

Tropical Equatorial Climate
The Tropical Equatorial Climate zone in Africa, situated around the Equator in regions like the Congo Basin and coastal Gulf of Guinea, experiences high annual temperatures with minimal seasonal variation. Because the sun passes directly overhead twice a year during the equinoxes, atmospheric heating generates intense convective rainstorms resulting in two distinct precipitation peaks (a bimodal rainfall regime).

Step-by-Step Solution

1
Identify the key temperature and precipitation characteristics described in the stem.
The stem specifies constant high temperatures and two annual rainfall peaks (bimodal distribution).
Regions along the Equator receive direct overhead solar radiation twice a year during the equinoxes, triggering intense convective precipitation.
2
Match these characteristics to the corresponding African climate zone.
The Equatorial climate zone (found in the Congo Basin and coastal West Africa) uniquely exhibits this bimodal rainfall regime.
As the Inter-Tropical Convergence Zone (ITCZ) passes over the equatorial belt twice each year, it brings two periods of maximum rainfall.

Key Concept

Bimodal rainfall regime of the African Tropical Equatorial Climate
Question 45Question →

The physical landscape of Africa is characterized by diverse relief features ranging from vast interior basins to towering volcanic cones and folded mountain belts. Arrange the following prominent African highland peaks in sequential order based on their maximum elevation above sea level, starting from the HIGHEST peak to the LOWEST peak.

Drag items to arrange them in the correct order

Show answer & explanation

Answer

The correct sequential order from highest to lowest peak elevation is Mount Kilimanjaro (5,895 m), Ras Dashen (4,550 m), Mount Toubkal (4,167 m), Mount Cameroon (4,095 m), and Emi Koussi (3,415 m).
The peaks are arranged in strict order of descending maximum elevation: Mount Kilimanjaro (5,895 m) > Ras Dashen (4,550 m) > Mount Toubkal (4,167 m) > Mount Cameroon (4,095 m) > Emi Koussi (3,415 m).

Step-by-Step Solution

1
Identify the elevation of East African volcanic structures.
Mount Kilimanjaro in Tanzania is the highest peak in Africa at 5,895 m above sea level.
It is a massive stratovolcano formed along the East African Rift System.
2
Identify the elevation of the Ethiopian Massif landforms.
Ras Dashen in the Simien Mountains of Ethiopia rises to 4,550 m above sea level.
It is part of the extensively uplifted and dissected Ethiopian Plateau.
3
Identify the elevation of North African fold mountain systems.
Mount Toubkal in the High Atlas range of Morocco reaches 4,167 m above sea level.
It forms the highest point of the Alpine fold mountain belt in northwestern Africa.
4
Identify the elevation of the West/Central African volcanic line features.
Mount Cameroon stands at 4,095 m above sea level.
It is an active volcano along the Cameroon Volcanic Line.
5
Identify the elevation of Saharan basement uplift and volcanic massifs.
Emi Koussi in the Tibesti Mountains of Chad rises to 3,415 m above sea level.
It is a high pyroclastic shield volcano situated in the central Sahara.

Key Concept

Elevations and regional distribution of major African mountain peaks and highland massifs
Question 46Question →

Although Africa exhibits a notable symmetrical distribution of climate zones north and south of the equator, regional variations create distinct seasonal precipitation patterns. Which of the following temperature and rainfall characteristics specifically defines the Mediterranean climatic type found at the extreme northern and southwestern fringes of Africa?

Show answer & explanation

Answer: Mild, rainy winters and hot, dry summers resulting from the seasonal movement of wind belts.

Answer

The Mediterranean climate zone at the northern and southwestern extremities of Africa is defined by mild, rainy winters and hot, dry summers.
The Mediterranean climate region, situated at Africa's northern coast and southwestern tip (Cape region), is controlled by the seasonal migration of pressure belts and wind systems. During winter, prevailing westerly winds bring cyclonic rain, whereas in summer, subtropical high-pressure cells dominate, resulting in dry, warm conditions.

Step-by-Step Solution

1
Identify the geographical distribution of the Mediterranean climate zone in Africa.
The Mediterranean climate occurs at the northernmost coastal fringe (Maghreb region north of the Atlas Mountains) and the southwestern tip around Cape Town, South Africa.
Recognizing the spatial location helps determine the atmospheric controls governing those latitude belts (around 30°–35° N and S).
2
Analyze the prevailing wind systems and seasonal shifting affecting these latitudes.
In winter, mid-latitude rain-bearing westerly winds shift equatorward, bringing rainfall. In summer, subtropical high-pressure belts move poleward, bringing dry, warm conditions.
Understanding wind belt migration explains why precipitation occurs in winter rather than summer.
3
Select the option matching these unique seasonal temperature and precipitation traits.
Mild, rainy winters and hot, dry summers accurately characterizes this climatic zone.
This contrasts directly with tropical wet climates (year-round rain) and tropical continental climates (summer rain).

Key Concept

Characteristics of the Mediterranean Climate in Africa
Estimated Time:1m 0s
Question 47Question →

Arrange the following African mountain peaks in order of their elevation, starting from the HIGHEST peak to the LOWEST peak.

Drag items to arrange them in the correct order

Show answer & explanation

Answer

The correct sequence from highest to lowest peak elevation is Mount Kilimanjaro (5,895 m), Mount Kenya (5,199 m), Mount Cameroon (4,040 m), and Mount Tahat (2,908 m).
Mount Kilimanjaro is the highest point on the African continent at 5,895 meters above sea level. Mount Kenya follows as the second-highest peak at 5,199 meters. Mount Cameroon is the third-highest among these at 4,040 meters, while Mount Tahat in the Ahaggar Massif of Algeria is the lowest of the four at 2,908 meters.

Step-by-Step Solution

1
Identify the elevation of each listed African landform peak.
Mount Kilimanjaro (~5,895 m), Mount Kenya (~5,199 m), Mount Cameroon (~4,040 m), Mount Tahat (~2,908 m).
Determining the absolute or relative height of each peak establishes the baseline for comparison.
2
Sequence the peaks in descending order from maximum height to minimum height.
Mount Kilimanjaro > Mount Kenya > Mount Cameroon > Mount Tahat.
Comparing peak heights from highest to lowest yields the correct sequence.

Key Concept

Elevation Profiles of Major African Mountain Peaks
Question 48Question →

Arrange the following African climatic zones in correct latitudinal sequence, starting from the Equator (0∘0^\circ) and moving northwards toward the Mediterranean coast.

Drag items to arrange them in the correct order

Show answer & explanation

Answer

The correct latitudinal sequence from the Equator northwards to the coast is: Equatorial Climate Zone, Tropical Wet-and-Dry (Sudan Savanna) Climate Zone, Semi-Arid Steppe (Sahelian) Climate Zone, Tropical Continental Desert (Sahara) Climate Zone, and Mediterranean Climate Zone.
Africa exhibits a near-symmetrical latitudinal arrangement of climatic zones away from the Equator. Moving northwards from 0∘0^\circ, atmospheric pressure systems and solar radiation produce sequential climatic belts: Equatorial (0∘0^\circ), Savanna (5∘−15∘N5^\circ-15^\circ\text{N}), Sahelian Steppe (15∘−20∘N15^\circ-20^\circ\text{N}), Sahara Desert (20∘−30∘N20^\circ-30^\circ\text{N}), and Mediterranean (30∘−37∘N30^\circ-37^\circ\text{N}).

Step-by-Step Solution

1
Identify the climatic belt situated directly on the Equator (0∘0^\circ).
The Equatorial (Tropical Rainforest) Climate Zone sits at the center (0∘0^\circ).
High sun angles and continuous ITCZ influence create this wet equatorial core.
2
Determine the zone directly adjacent to the Equatorial belt moving northward (5∘N5^\circ\text{N} to 15∘N15^\circ\text{N}).
The Tropical Wet-and-Dry (Sudan Savanna) Climate Zone is next.
This region experiences distinct wet and dry seasons driven by the seasonal migration of the ITCZ.
3
Identify the narrow transitional zone lying between 15∘N15^\circ\text{N} and 20∘N20^\circ\text{N}.
The Semi-Arid Steppe (Sahelian) Climate Zone follows the Savanna.
It acts as a semi-arid buffer between the moist savanna and the hyper-arid desert.
4
Locate the major high-pressure arid zone between 20∘N20^\circ\text{N} and 30∘N30^\circ\text{N}.
The Tropical Continental Desert (Sahara) Climate Zone forms the fourth belt.
Subsiding air masses under the subtropical high-pressure cell maintain extreme aridity.
5
Identify the northern coastal margin zone beyond 30∘N30^\circ\text{N}.
The Mediterranean Climate Zone forms the final northern belt.
Influenced by winter mid-latitude westerlies, it brings mild rainy winters and dry summers to the northern coast.

Key Concept

Symmetrical Latitudinal Distribution of African Climate Belts
Question 49Question →

Arrange the following West African vegetation belts in correct sequential order, starting from the humid coastal region along the Gulf of Guinea in the south and moving northward toward the Sahara Desert.

Drag items to arrange them in the correct order

Show answer & explanation

Answer

The correct sequence from south to north is Tropical Rainforest, followed by Guinea Savanna, Sudan Savanna, and Sahel Savanna.
The vegetation zones in West Africa form parallel east-west belts corresponding directly to decreasing annual rainfall from south to north: Tropical Rainforest (southern coast), Guinea Savanna (sub-humid belt), Sudan Savanna (dry savanna), and Sahel Savanna (semi-arid desert margin).

Step-by-Step Solution

1
Identify the primary climatic driver of vegetation distribution in West Africa.
Mean annual precipitation decreases progressively along a latitudinal gradient from the Atlantic coast northward.
The moist maritime winds from the South-West Monsoon weaken as distance from the Gulf of Guinea increases.
2
Identify the coastal vegetation zone receiving maximum rainfall.
Tropical Rainforest occupies the southernmost position.
It thrives in high heat and abundant moisture (>2000 mm/year) near the equator and southern coastline.
3
Arrange the savannas in order of decreasing tree density and moisture availability.
The order inland is Guinea Savanna (1000-1500 mm), Sudan Savanna (500-1000 mm), and Sahel Savanna (200-500 mm).
Drier conditions further inland reduce tree height and grass density, leading directly into the desert margin.

Key Concept

Latitudinal Zonation of African Vegetation Belts
Estimated Time:1m 0s
Question 50Question →

The East African Rift System contains a prominent series of tectonic lakes formed along its eastern and western branches. Arrange the following major East African lakes in sequential order from north to south based on their latitudinal position.

Drag items to arrange them in the correct order

Show answer & explanation

Answer

The correct sequence from north to south is Lake Turkana, followed by Lake Albert, then Lake Tanganyika, and finally Lake Malawi.
The correct spatial ordering from north to south follows the latitudinal positions: Lake Turkana is the northernmost (approx. 4°30' N to 2°30' N), followed by Lake Albert in the Albertine Rift (approx. 2°20' N to 1°10' N), then Lake Tanganyika south of the equator (approx. 3°20' S to 8°48' S), and Lake Malawi as the southern terminus (approx. 9°30' S to 14°25' S).

Step-by-Step Solution

1
Identify the northernmost lake among the listed rift valley lakes.
Lake Turkana sits in northern Kenya, reaching up to 4°30' N latitude.
It is positioned highest in the Northern Hemisphere among all major East African Rift lakes.
2
Determine the position of Lake Albert relative to Lake Turkana and the Equator.
Lake Albert is located in the northern arm of the Western Rift between 1°10' N and 2°20' N.
It lies south of Lake Turkana but remains entirely in the Northern Hemisphere north of Lake Tanganyika.
3
Locate Lake Tanganyika along the latitudinal gradient.
Lake Tanganyika spans across the Southern Hemisphere from 3°20' S to 8°48' S.
It occupies the central section of the Western Rift Valley, south of Lake Albert and the Equator.
4
Identify the southernmost lake in the East African Rift System sequence.
Lake Malawi (Nyasa) lies between 9°30' S and 14°25' S latitude.
It forms the southern extremity of the Great Rift Valley lake system.

Key Concept

Latitudinal Distribution of East African Rift Valley Lakes
Estimated Time:1m 30s
Question 51Question →

An environmental researcher observes a distinct vegetation belt in West and Central Africa situated between the dense equatorial rainforest to the south and the dry Sudan Savanna to the north. This zone receives an annual rainfall of about 1,000 mm to 1,500 mm and is characterized by tall grasses and scattered deciduous, fire-resistant trees such as the baobab and locust bean. Which major African vegetation zone is being described?

Show answer & explanation

Answer: Guinea Savanna

Answer

Guinea Savanna
The Guinea Savanna (also known as the Moist Savanna) forms a broad transitional belt directly north of the tropical rainforest. It receives between 1,000 mm and 1,500 mm of annual rainfall and features continuous tall grass cover interspersed with fire-resistant, drought-deciduous trees such as the baobab, locust bean, and shea butter tree.

Step-by-Step Solution

1
Analyze the spatial location given in the stem.
The zone lies between the equatorial rainforest to the south and the drier savanna/Sahel to the north.
Vegetation belts in West and Central Africa follow a latitudinal zonation aligned with decreasing rainfall northward from the Equator.
2
Evaluate the vegetation characteristics described.
Tall grasses combined with fire-resistant deciduous trees (baobab, shea butter, locust bean) indicate a moist savanna environment.
Annual rainfall of 1,000–1,500 mm produces a longer dry season than the rainforest but far more moisture than the Sahel or desert zones.
3
Match the location and vegetation characteristics to the correct African vegetation zone.
The zone is identified as the Guinea Savanna.
The Guinea Savanna (Moist Savanna) is the broadest vegetation belt immediately north of the rainforest zone.

Key Concept

Major Vegetation Zones of Africa
Question 52Question →

The River Niger exhibits a unique hydrological regime featuring a vast inland delta (the Macina) in Mali, where severe transmission losses occur due to high evapotranspiration and seepage in the semi-arid Sahel. Which of the following hydrological factors is primarily responsible for sustaining its downstream volume as it flows through Niger Republic and into Nigeria?

Show answer & explanation

Answer: The seasonal flood surge generated by heavy summer monsoon rains in its humid headwaters in the Fouta Djallon highlands, augmented by the influx of the Bani River.

Answer

The River Niger's flow into its middle and lower courses is sustained by the seasonal flood surge originating from heavy summer monsoon rainfall in the Fouta Djallon highlands of Guinea, combined with significant tributary inflow from the Bani River.
The upper River Niger originates in the high-rainfall Fouta Djallon plateau of Guinea, receiving heavy monsoonal precipitation. This generates a massive seasonal flood wave. As the river enters Mali, the Bani River contributes critical additional volume before the main flow enters the Macina inland delta, allowing sufficient water to survive extreme evaporative losses and sustain the middle and lower river courses.

Step-by-Step Solution

1
Analyze the hydrological behavior of the River Niger across its distinct course sections.
Identified that the upper course receives tropical monsoonal rainfall in the humid Fouta Djallon highlands, initiating a major annual flood wave.
Understanding headwater climatic controls explains how large volumes of water enter the system before reaching arid zones.
2
Examine the effect of the Macina inland delta on river discharge.
Recognized that while the Macina causes substantial water loss via evaporation and infiltration, the primary flood wave takes months to navigate the wetland.
Explains why a delayed secondary high-water peak (the 'black flood') emerges downstream in Niger and Nigeria during the dry season.
3
Evaluate the role of major tributaries in maintaining flow south of the inland delta.
Determined that the Bani River joins the Niger at Mopti, adding substantial volume drained from the humid southern savanna zone.
Confirms the primary hydrological mechanism sustaining downstream discharge into its middle course.

Key Concept

Hydrological regimes and discharge characteristics of major African rivers
Question 53Question →

Match each African political entity in Column A with its corresponding unique political-geographical boundary or territorial characteristic in Column B.

Click a left item, then click its matching right item

Items

Lesotho
Cabinda
Equatorial Guinea
The Gambia

Matches

Show answer & explanation

Answer

Lesotho matches with being an enclave completely surrounded by South Africa; Cabinda matches with being an angolan exclave separated by DRC territory; Equatorial Guinea matches with having its capital Malabo on Bioko Island separate from mainland Río Muni; The Gambia matches with being a riverine nation almost entirely surrounded by Senegal.
Each matching pair accurately reflects established geopolitical terminology and territorial features in African geography: Lesotho is an enclave within South Africa; Cabinda is an Angolan exclave across DRC territory; Equatorial Guinea places its capital on Bioko Island off mainland Río Muni; and The Gambia is virtually surrounded by Senegal along the Gambia River.

Step-by-Step Solution

1
Analyze the geographical position of Lesotho relative to its surrounding borders.
Lesotho is entirely surrounded by South Africa, establishing it as an enclave state.
An enclave is a territory completely surrounded by another single foreign state.
2
Examine the political division of Angola's northern territory of Cabinda.
Cabinda is separated from mainland Angola by the Democratic Republic of the Congo's narrow coastal corridor along the Congo River.
This spatial separation defines Cabinda as a political exclave.
3
Identify the multi-part territory of Equatorial Guinea.
Equatorial Guinea consists of mainland Río Muni and offshore islands, with its capital Malabo located on Bioko Island.
This creates a unique arrangement where the national capital is geographically isolated from the country's mainland region.
4
Evaluate the political geography of West Africa regarding The Gambia.
The Gambia forms a narrow ribbon state centered on the Gambia River and is surrounded on three sides by Senegal.
Its boundary shape makes it a semi-enclave within Senegal.

Key Concept

Political-Geographical Terminology and Territorial Patterns in Africa
Estimated Time:2m 0s
Question 54Question →

Rank the following African climatic zones in ascending order based on their average annual precipitation totals, starting from the driest zone with the lowest annual rainfall to the wettest zone with the highest annual rainfall:

Drag items to arrange them in the correct order

Show answer & explanation

Answer

The correct sequence from driest to wettest is: Tropical Arid (Desert) Zone, Tropical Semi-Arid (Sahelian) Zone, Tropical Savanna (Sudan) Zone, and Equatorial Rainforest Zone.
The correct order follows the latitudinal moisture gradient created by atmospheric circulation over Africa. The Tropical Arid Zone receives less than 250 mm250\text{ mm} annually due to dry Continental Tropical (cTcT) winds and oceanic high-pressure cells. The Semi-Arid Sahel transitional zone receives 250 mm−600 mm250\text{ mm} - 600\text{ mm}. Further equatorial, the Tropical Savanna zone receives 600 mm−1,500 mm600\text{ mm} - 1,500\text{ mm} during its prolonged summer wet season. Finally, the Equatorial Rainforest Zone centered on the Congo Basin and Gulf of Guinea receives the highest rainfall (1,500 mm−3,000+ mm1,500\text{ mm} - 3,000+\text{ mm}) due to perpetual low-pressure convective activity.

Step-by-Step Solution

1
Identify the climatic mechanism controlling moisture availability across major African climate zones.
Precipitation in tropical and sub-tropical Africa is governed primarily by proximity to the Equator and the seasonal migration of the Inter-Tropical Convergence Zone (ITCZ), creating a gradient from continuous low-pressure convergence at the Equator to permanent high-pressure subsidence at the tropics.
Understanding the driver of atmospheric convergence explains the spatial variation in annual rainfall totals.
2
Determine the annual rainfall amounts for each zone.
Tropical Arid (Sahara/Namib/Kalahari) receives <250 mm< 250\text{ mm}; Tropical Semi-Arid (Sahel) receives 250 mm−600 mm250\text{ mm} - 600\text{ mm}; Tropical Savanna receives 600 mm−1,500 mm600\text{ mm} - 1,500\text{ mm}; Equatorial Rainforest receives >1,500 mm> 1,500\text{ mm} (up to 3,000+ mm3,000+\text{ mm}).
Comparing quantitative mean annual precipitation ranges allows exact ascending rank ordering.
3
Arrange the zones in strict ascending order of precipitation.
Tropical Arid Zone →\rightarrow Tropical Semi-Arid Zone →\rightarrow Tropical Savanna Zone →\rightarrow Equatorial Rainforest Zone.
This establishes the progression from hyper-arid moisture deficits to humid surplus conditions.

Key Concept

Precipitation Gradients and Climatic Zoning of Africa
Question 55Question →

Which of the following major African rivers flows eastward across southern Africa to empty its waters into the Indian Ocean?

Show answer & explanation

Answer: The Zambezi River

Answer

The Zambezi River flows eastward across southern Africa and empties into the Indian Ocean.
The Zambezi River is the fourth-largest river in Africa and the largest African river flowing into the Indian Ocean. Its course runs eastward from central Africa through the Zambezi delta into the Mozambique Channel.

Step-by-Step Solution

1
Identify the primary flow direction and oceanic discharge body for major southern African rivers.
The Zambezi River originates in Zambia, flows east through Mozambique, and empties into the Mozambique Channel of the Indian Ocean.
Topographic gradient across southern Africa directs the Zambezi Eastward toward the Indian Ocean coastline.
2
Compare against the outlets of other major rivers listed.
The Orange River drains west to the Atlantic Ocean, while the Congo and Niger rivers also empty into Atlantic waters.
Distinguishing Atlantic drainage basins from Indian Ocean drainage basins is essential for identifying river outlets in Africa.

Key Concept

Major African river drainage basins and ocean discharge outlets
Estimated Time:1m 0s
Question 56Question →

During the Northern Hemisphere winter (January), the northern coastal fringe of Africa experiences mild, rainy conditions, whereas the Sudan Savanna belt lying between 10∘N10^\circ\text{N} and 15∘N15^\circ\text{N} experiences an intense dry season. Which atmospheric mechanism primarily accounts for the dry season in the Sudan Savanna belt during this period?

Show answer & explanation

Answer: The southward movement of the Inter-Tropical Convergence Zone (ITCZ), allowing the dry Continental Tropical (cT) air mass to dominate the region.

Answer

The dry season in the Sudan Savanna during January is caused by the southward movement of the Inter-Tropical Convergence Zone (ITCZ), allowing the dry Continental Tropical (cT) air mass (Harmattan) to dominate the region.
In January, during the Northern Hemisphere winter, solar insolation is concentrated in the Southern Hemisphere. Consequently, the Inter-Tropical Convergence Zone (ITCZ) retreats southward. This allows the dry, warm, and dusty Continental Tropical (cT) air mass, commonly known as the Harmattan, to blow from the Sahara Desert southward across the Sudan Savanna, bringing clear skies and dry conditions.

Step-by-Step Solution

1
Identify the seasonal position of the overhead sun in January.
In January (Northern Hemisphere winter), the sun is overhead in the Southern Hemisphere near the Tropic of Capricorn (23.5∘S23.5^\circ\text{S}).
Apparent movement of the sun dictates the thermal equator and low-pressure belt position.
2
Determine the resulting shift of the Inter-Tropical Convergence Zone (ITCZ).
The ITCZ shifts southward toward the Equator and Southern Africa.
The low-pressure zone follows the zone of maximum solar heating.
3
Analyze the prevailing air mass brought by this ITCZ position over West/Central Africa north of the Equator.
The dry Continental Tropical (cTcT) air mass (Harmattan wind blowing from the Sahara Desert) prevails over the Sudan Savanna belt.
With the ITCZ located further south, offshore continental winds blow from high-pressure desert regions toward the low-pressure equatorial belt.

Key Concept

Seasonal movement of the ITCZ and air mass movement in West and Central Africa
Question 57Question →

Arrange the following major African landforms in order of their geographical position, from the northernmost feature to the southernmost feature.

Drag items to arrange them in the correct order

Show answer & explanation

Answer

Atlas Mountains → Tibesti Massif → Ethiopian Highlands → Drakensberg Range
The correct sequence places the Atlas Mountains first as they form the northern rim of Africa in the Maghreb. The Tibesti Massif comes next in the central Sahara. The Ethiopian Highlands follow further south in the Horn of Africa, and the Drakensberg Range is last as it forms the high escarpment of Southern Africa.

Step-by-Step Solution

1
Identify the geographical region and latitude of each landform
Atlas Mountains lie in North-Western Africa (approx. 32°N); Tibesti Massif lies in the Sahara of Chad (approx. 20°N); Ethiopian Highlands lie in East Africa (approx. 9°N); Drakensberg Range lies in Southern Africa (approx. 29°S).
Establishing absolute latitudinal positions allows for accurate north-to-south sequencing.
2
Sequence the features from north to south
1st: Atlas Mountains (North Africa), 2nd: Tibesti Massif (Sahara/Central-North), 3rd: Ethiopian Highlands (East Africa), 4th: Drakensberg Range (Southern Africa).
This places the landforms in correct descending latitudinal order across the African continent.

Key Concept

Latitudinal and spatial distribution of major African relief features
Question 58Question →

Match each of the following major African physical landforms with its primary tectonic origin and structural formation process.

Click a left item, then click its matching right item

Items

Atlas Mountains
Ruwenzori Mountains
Ethiopian Plateau
Ahaggar Massif

Matches

Show answer & explanation

Answer

Atlas Mountains pair with orogenic folding from African-Eurasian plate collision; Ruwenzori Mountains pair with horst block uplift along the rift valley; Ethiopian Plateau pairs with flood basalt accumulation over a mantle swell; Ahaggar Massif pairs with intraplate volcanism on an uplifted cratonic dome.
Each major African landform corresponds to a distinct tectonic origin: the Atlas Mountains were formed by compressional folding during the collision of the African and Eurasian plates; the Ruwenzori Mountains represent a non-volcanic horst block uplifted along rift faults; the Ethiopian Plateau was formed by extensive flood basalt volcanism over a mantle plume swell; and the Ahaggar Massif is an intraplate volcanic capping on an epeirogenically uplifted Saharan basement dome.

Step-by-Step Solution

1
Determine the formation process of the Atlas Mountains system
Identify the Atlas Range as a young fold mountain belt produced at a convergent plate boundary.
Compressional tectonic stresses during the Alpine orogeny folded thick sedimentary strata along Africa's northern margin.
2
Analyze the structural mechanism of the Ruwenzori Range
Classify Ruwenzori as a crystalline horst block rather than a volcanic edifice.
Tensional stresses along the Albertine Rift caused vertical block-faulting, lifting ancient Precambrian metamorphic rock above the surrounding grabens.
3
Evaluate the geological composition of the Ethiopian Plateau
Link the high plateau to massive trap basalt volcanism.
Mantle plume upwelling elevated the Horn of Africa and triggered continental flood basalt eruptions that built up thick lava sheets.
4
Identify the origin of Saharan interior massifs such as the Ahaggar
Recognize the combination of epeirogenic doming and secondary intraplate volcanic activity.
Slow upward warping of the African continental shield exposed basement rocks, which were subsequently modified by volcanic extrusions.

Key Concept

Geological Origins and Tectonic Classification of African Landforms
Question 59Question →

Place the following operational stages of timber export logistics from inland forest concessions in Central Africa to overseas markets in the correct chronological sequence from first to last.

Drag items to arrange them in the correct order

Show answer & explanation

Answer

The correct sequence from first to last is: Felling timber trees and clearing branches at the forest concession site → Transporting heavy logs via river floating or rail lines toward coastal ports → Inspecting, grading, and sorting logs at coastal port timber yards → Loading sorted logs onto ocean cargo vessels for overseas shipment.
The sequence follows the physical flow of commercial lumbering in Equatorial Africa: tree harvesting occurs first in interior forest concessions, followed by long-distance transport down river systems or railways to coastal ports, then quality sorting and inspection at port yards, ending with ocean freighter loading for international trade.

Step-by-Step Solution

1
Identify the primary extraction phase in the forest.
Standing trees are felled and trimmed into manageable log lengths in interior forest concessions.
Physical harvest is the essential starting point of all forestry operations.
2
Determine the transport phase from interior concessions to the coast.
Logs are moved along waterways (river floating/rafting) or heavy logging rail routes towards maritime outlets.
Inland transport bridges the distance between remote rainforests and coastal industrial ports.
3
Identify the port handling and evaluation phase.
Logs reaching port yards undergo official inspection, volume measurement, and quality classification.
Customs clearance and quality grading are required before commercial international shipping.
4
Determine the final export loading phase.
Graded logs are loaded onto ocean freighter ships bound for international buyer destinations.
Ocean vessel loading concludes the export logistics workflow.

Key Concept

Timber Export Logistics and Transport Stages in Central Africa
Question 60Question →

In Africa's Sudan Savanna climate zone, rainfall is strictly seasonal and concentrated within a single wet season. Which atmospheric mechanism primarily controls the seasonal movement of rainfall across this zone?

Show answer & explanation

Answer: The seasonal apparent movement of the Inter-Tropical Convergence Zone (ITCZ)

Answer

The seasonal apparent movement of the Inter-Tropical Convergence Zone (ITCZ)
The correct answer identifies the seasonal apparent movement of the Inter-Tropical Convergence Zone (ITCZ). The ITCZ is a low-pressure belt where trade winds converge. Its movement northwards following the sun during the Northern Hemisphere summer draws moisture-laden Tropical Maritime air into interior West and Central Africa, producing the characteristic single rainy season of the Sudan Savanna climate zone.

Step-by-Step Solution

1
Identify the climatic characteristics of the Sudan Savanna zone in Africa.
The Sudan Savanna experiences a tropical continental climate marked by distinct wet and dry seasons.
Rainfall in this zone occurs primarily when warm, humid air masses drawn by low-pressure systems sweep over the continent.
2
Analyze the primary atmospheric driver responsible for shifting rain-bearing air masses across sub-Saharan Africa.
The Inter-Tropical Convergence Zone (ITCZ) follows the apparent movement of the sun, shifting northwards toward the Tropic of Cancer in July and southwards toward the Tropic of Capricorn in January.
As the ITCZ moves north in northern summer, it pulls the rain-bearing Tropical Maritime (mT) air mass deep into the Sudan Savanna zone.

Key Concept

Inter-Tropical Convergence Zone (ITCZ) and Seasonal Rainfall in Africa
PreviousPage 3 / 8Next
Geography of Africa Practice Questions — JAMB UTME — Page 3 | Examkin