The grassland region of South Africa is known as

1. World Climatic Zones and Vegetation Biomes (basic)

Welcome to our journey through the world's natural landscapes! To understand why a specific plant grows in a specific place, we must first understand the concept of a Biome. A terrestrial biome is a large-scale, self-regulating association of plants and animals. Think of it as a massive community defined by its predominant vegetation—such as a forest, a grassland, or a desert. These biomes are not random; they are the biological expression of the underlying climate Environment and Ecology, Majid Hussain, MAJOR BIOMES, p.3.

What determines where one biome ends and another begins? The answer lies in climatic elements. The two most powerful architects of our natural world are Temperature and Precipitation. These are influenced by several factors, most notably Latitude (distance from the equator) and Altitude (height above sea level). For instance, as you move from the hot, humid equator toward the cold, dry poles, you will see a predictable shift in vegetation—from lush evergreen forests to sparse tundra Certificate Physical and Human Geography, GC Leong, Climate, p.131.

Geographers and ecologists categorize these into major zones to help us study them. These include:

• Equatorial and Tropical Zones: Home to Rainforests and Savannas.
• Arid Zones: Defined by low rainfall, leading to Deserts.
• Temperate Zones: Featuring Steppes (grasslands) and Deciduous forests.
• Cold/Polar Zones: Characterized by Coniferous forests (Taiga) and Tundra Environment and Ecology, Majid Hussain, MAJOR BIOMES, p.4.

Sources: Environment and Ecology, Majid Hussain, MAJOR BIOMES, p.3-4; Certificate Physical and Human Geography, GC Leong, Climate, p.131

2. Tropical Grasslands: The Savanna (Sudan Type) (basic)

Concept: Tropical Grasslands: The Savanna (Sudan Type)

3. Temperate Grasslands: The Steppe Type (basic)

The Temperate Grasslands, often referred to globally as the Steppe type, are found in the interior of continents within the mid-latitudes. Unlike the tropical Savannas which have scattered trees, these grasslands are practically treeless, and the grasses are much shorter and more nutrient-dense Certificate Physical and Human Geography, Chapter 20, p.191. Because they are located far from the moderating influence of the sea, they experience a continental climate with extreme temperature ranges — scorching summers and freezing winters. Interestingly, this extremity is more pronounced in the Northern Hemisphere; in the Southern Hemisphere, the tapering shape of the continents allows for more maritime influence, making the winters much milder Certificate Physical and Human Geography, Chapter 20, p.190.

While the term 'Steppe' originated in Eurasia, it is now used as a generic term for several regional grasslands that share similar characteristics. These regions are often called the 'bread-baskets' of the world because their fertile soils have been extensively converted for commercial grain cultivation, such as wheat and maize Environment and Ecology, MAJOR BIOMES, p.13. We can categorize these regional grasslands as follows:

Region	Local Name	Key Characteristic
Eurasia	Steppes	Extensive stretches from Central Asia to Russia.
North America	Prairies	Lies between the Rockies and the Appalachians.
South America	Pampas	Highly fertile plains in Argentina and Uruguay.
South Africa	Veld	Divided into High Veld (temperate) and Low Veld (tropical).
Australia	Downs	Found in the Murray-Darling basin.

In South Africa, the Veld (or Veldt) is a unique landscape. The High Veld consists of high-altitude temperate grasslands (4,000–6,000 feet) used primarily for livestock, while the Low Veld (or Bush-veld) transitions into more tropical, savanna-like conditions at lower elevations. This is a critical distinction to remember for your exams: not all 'Velds' are purely temperate Physical Geography by PMF IAS, Chapter 30, p.445.

Sources: Certificate Physical and Human Geography, Chapter 20: The Temperate Continental (Steppe) Climate, p.190-191; Environment and Ecology, MAJOR BIOMES, p.13; Physical Geography by PMF IAS, Chapter 30: Climatic Regions, p.445

4. Grasslands of the Americas: Selvas, Llanos, and Pampas (intermediate)

To master the geography of South America, we must distinguish between its three primary vegetation zones, which transition from the equator down to the temperate south. At the heart of the continent lies the Selvas. This term refers specifically to the dense, luxuriant tropical rainforests of the Amazon Basin. Unlike a grassland, the Selvas are defined by a multi-layered canopy so thick that it appears as a continuous carpet of green from above, broken only by massive rivers Physical Geography by PMF IAS, Climatic Regions, p.426. Here, the 'vegetational extravagance' is fueled by constant high temperatures (around 27°C) and heavy rainfall, allowing for a year-round growing season without a period of drought or cold Certificate Physical and Human Geography, The Hot, Wet Equatorial Climate, p.152. Moving into the drainage basin of the Orinoco River (primarily in Venezuela and Colombia), the landscape opens up into the Llanos. These are tropical savannas, characterized by tall grasses and scattered trees. Unlike the Selvas, the Llanos experience a distinct wet and dry season, which prevents the growth of dense forests and instead supports vast tracts of grazing land. Further south, in the mid-latitudes of Argentina and Uruguay, we find the Pampas. These are temperate grasslands, analogous to the Steppes of Eurasia or the Prairies of North America. The Pampas are famous for their incredibly fertile soils and moderate rainfall, making them one of the world's most productive regions for wheat and livestock.

To keep these distinct in your mind, compare their core characteristics:

Region	Biome Type	Primary Location	Climate Highlight
Selvas	Tropical Rainforest	Amazon Basin	Equatorial (Hot & Wet year-round)
Llanos	Tropical Savanna	Orinoco Basin	Tropical Wet-and-Dry
Pampas	Temperate Grassland	Argentina/Uruguay	Warm Temperate (Continental)

Sources: Certificate Physical and Human Geography, The Hot, Wet Equatorial Climate, p.152; Physical Geography by PMF IAS, Climatic Regions, p.426

5. Grasslands of Oceania and Eurasia (intermediate)

In our journey through global biomes, we now move to the mid-latitudes to explore the Temperate Grasslands of Eurasia and Oceania. Unlike the tropical savannas, these regions experience distinct seasonal temperature variations. In Eurasia, these vast, treeless plains are known as the Steppes. They stretch impressively from the shores of the Caspian Sea eastward to the mountains of China. Because they are located deep within the interior of the giant Eurasian landmass, they exhibit a 'continental climate'—characterized by very hot summers and bitterly cold winters. The soil here, often called Chernozem (black earth), is incredibly fertile, making the western Steppes the 'granary of the world' for wheat production. Moving to Oceania, we find a different character of temperate grassland. In Australia, these grasslands are famously known as the Downs, located primarily in the Murray-Darling Basin of New South Wales and Victoria GC Leong, Chapter 20, p.190. A unique geographical feature of the Australian grasslands is their dependence on the Great Artesian Basin. Since the interior of Australia is prone to acute water shortages, farmers bore deep wells into these artesian basins to provide water for their massive flocks of sheep and herds of cattle GC Leong, Chapter 4, p.45. In New Zealand, the temperate grasslands are concentrated in the Canterbury Plains of the South Island, where sheep rearing is the dominant economic activity, supported by a mild climate and well-drained level ground GC Leong, Chapter 22, p.213.

Region	Local Name	Key Feature
Central Eurasia	Steppes	Extreme continental climate; Wheat 'granary'.
Australia	Downs	Murray-Darling Basin; Merino sheep.
New Zealand	Canterbury Plains	Intensive sheep farming; 20 sheep per person.

Sources: Certificate Physical and Human Geography, GC Leong, Chapter 20: The Temperate Continental (Steppe) Climate, p.190; Certificate Physical and Human Geography, GC Leong, Chapter 4: Weathering, Mass Movement and Groundwater, p.45; Certificate Physical and Human Geography, GC Leong, Chapter 22: The Cool Temperate Western Margin (British Type) Climate, p.213

6. The Veldts of South Africa: High, Middle, and Low Veld (exam-level)

The Veld (or Veldt) represents the vast temperate grasslands of the interior plateau of Southern Africa. Unlike the flat, sea-level grasslands of the Pampas, the Veld is characterized by its varying altitudes, which create distinct climatic zones. These grasslands are largely a result of continentality—being deep within the interior where rain-bearing winds from the Indian Ocean lose their moisture—and the rain-shadow effect of the Drakensberg Mountains Physical Geography by PMF IAS, Climatic Regions, p.445. While naturally treeless in most parts, the Veld is a critical 'bread-basket' region, heavily modified by human activity for grain and livestock production Environment and Ecology, Majid Hussain, MAJOR BIOMES, p.13.

The Veld is traditionally divided into three distinct sub-regions based on elevation, which significantly influences the local flora and temperature gradients:

Region	Elevation (Approx.)	Characteristics
High Veld	4,000 – 6,000 feet	The true temperate grassland. Located in the south/central plateau, it has cold winters with frequent frost and is dominated by tall grasses.
Middle Veld	2,000 – 4,000 feet	An intermediate zone with a mix of grasses and scattered shrubs, bridging the gap between the high plateau and the lowlands.
Low Veld (Bush-veld)	Below 2,000 feet	More tropical and savanna-like. Located in the north/northeast, it features warmer temperatures and iconic acacia trees/thorny bushes Physical Geography by PMF IAS, Climatic Regions, p.436.

The Bush-veld (Low Veld) is particularly famous for its biodiversity, hosting iconic African megafauna. In contrast, the High Veld is the industrial and agricultural heartland of South Africa. It is important to distinguish these from other Southern Hemisphere grasslands, such as the Downs of Australia's Murray-Darling basin or the Pampas of South America, which operate under different moisture and soil regimes Physical Geography by PMF IAS, Climatic Regions, p.445.

Sources: Physical Geography by PMF IAS, Climatic Regions, p.445; Environment and Ecology, Majid Hussain, MAJOR BIOMES, p.13; Physical Geography by PMF IAS, Climatic Regions, p.436

7. Solving the Original PYQ (exam-level)

Now that you have mastered the classification of global vegetation, this question tests your ability to map those conceptual building blocks to specific regional names. You have learned that Temperate Grasslands occur in mid-latitudes and are known by distinct local names across different continents. In the context of the interior plateau of Southern Africa, these grasslands are shaped by both elevation and a semi-arid climate, forming a vital part of the region's physical geography as detailed in Physical Geography by PMF IAS.

To arrive at the correct answer, visualize the world map of grasslands. When you think of South Africa, you should immediately recall the 'Veld'—a term derived from the Dutch word for 'field.' These are categorized by altitude into the High Veld (cooler, higher altitude) and the Low Veld (warmer, savanna-like). Therefore, (C) Veldt is the correct designation. As explained in Certificate Physical and Human Geography, GC Leong, these grasslands are a classic example of the temperate continental climate found in the Southern Hemisphere.

UPSC frequently uses geographic distractors from different continents to test the precision of your memory. Options (A) Selvas and (D) Llanos are common traps located in South America—the former being the dense Amazonian rainforests and the latter being the tropical savannas of the Orinoco basin. Similarly, (B) Downs refers to the temperate grasslands found in Australia. By systematically eliminating names associated with South America and Australia, you can confidently identify the Veldt as the unique landscape of South Africa.