Veliconda Hills, which is a part of Eastern Ghats, is situated in—

1. Physiographic Divisions of Peninsular India (basic)

To understand India's geography, we must start with its oldest and most stable geological block: the Peninsular Plateau. Unlike the young, folded Himalayas, this region is a massive tableland composed of ancient crystalline, igneous, and metamorphic rocks. It was formed due to the breaking and drifting of the Gondwanaland landmass, making it one of the oldest land surfaces on Earth NCERT Class IX, Physical Features of India, p.12. Geographically, it is divided into two broad regions by the Narmada River: the Central Highlands to the north and the Deccan Plateau to the south NCERT Class IX, Physical Features of India, p.15.

The Deccan Plateau is a triangular landmass that tilts gently from the west to the east. This eastward slope is the reason why most major peninsular rivers, like the Godavari and Krishna, flow into the Bay of Bengal. The plateau is flanked by two mountain ranges: the Western Ghats (Sahyadris), which are continuous and high, and the Eastern Ghats, which are lower and highly dissected by rivers NCERT Class IX, Physical Features of India, p.12. Interestingly, the plateau extends even further northeast into the Meghalaya and Karbi-Anglong regions, though it is separated from the main block by a geological fault Majid Husain, Geography of India, p.57.

Within the Eastern Ghats, the landscape is not a single wall but a series of broken hill ranges. In the south-eastern part of Andhra Pradesh, you will find ranges like the Nallamala, Palkonda, and the Veliconda Hills. The Veliconda Range, in particular, forms the eastern flank of the Ghats between the Krishna and Pennar rivers Majid Husain, Geography of India, p.62. Understanding these specific ranges is key to mastering the micro-physiography of the region.

Feature	Western Ghats	Eastern Ghats
Continuity	Continuous; can be crossed only through passes.	Discontinuous and irregular; dissected by rivers.
Elevation	Higher (Average 900–1600 m).	Lower (Average 600 m).

Sources: CONTEMPORARY INDIA-I ,Geography, Class IX . NCERT(Revised ed 2025), Physical Features of India, p.12; CONTEMPORARY INDIA-I ,Geography, Class IX . NCERT(Revised ed 2025), Physical Features of India, p.15; Geography of India ,Majid Husain, (McGrawHill 9th ed.), Physiography, p.57; Geography of India ,Majid Husain, (McGrawHill 9th ed.), Physiography, p.62

2. The Eastern Ghats: General Characteristics (basic)

The Eastern Ghats represent the eastern edge of the Peninsular Plateau, running almost parallel to the Bay of Bengal. Unlike the Western Ghats, which are a continuous wall-like structure, the Eastern Ghats are discontinuous, irregular, and heavily dissected by major rivers like the Mahanadi, Godavari, Krishna, and Kaveri, which flow into the Bay of Bengal NCERT Class IX, Physical Features of India, p.12. This fragmentation is a defining geological characteristic; they are essentially a series of detached hill ranges of heterogeneous composition rather than a single mountain chain.

Geographically, the Eastern Ghats stretch from the Mahanadi Valley in the north to the Nilgiri Hills in the south, where they finally converge with the Western Ghats Majid Husain, Geography of India, p.58. In terms of height, they are significantly lower than their western counterparts, with an average elevation of about 600 meters, though certain sections between the Mahanadi and Godavari rise to an average of 1100 meters Majid Husain, Geography of India, p.61. The highest peak of the Eastern Ghats is Arma Konda (also known as Sitamma Konda or Jindhagada) in Andhra Pradesh, reaching an elevation of 1,680 meters Majid Husain, Geography of India, p.62.

The range is known by various local names as it passes through different states. In the central section, particularly between the Krishna River and Chennai, you will find distinct ranges such as the Nallamala, Velikonda, Palkonda, and Erramala Hills. Further south in Tamil Nadu, the system continues as the Javadi, Shevaroy, and Panchaimalai Hills Majid Husain, Geography of India, p.62. Geologically, these hills are very ancient and primarily composed of rocks like khondalites and charnockites, which are types of metamorphosed and intrusive igneous rocks.

Feature	Eastern Ghats	Western Ghats
Continuity	Discontinuous; broken by river valleys.	Continuous; can be crossed only through passes.
Avg. Elevation	Lower (~600 meters).	Higher (~900–1600 meters).
Direction of Slope	Fades into the Coastal Plains.	Steep western slope, gentle eastern slope.

Sources: CONTEMPORARY INDIA-I, Geography, Class IX. NCERT, Physical Features of India, p.12; Geography of India, Majid Husain, Physiography, p.58, 61, 62

3. Coastal Plains and their Relationship with Ghats (intermediate)

The Indian subcontinent is framed by two distinct coastal strips that offer a fascinating study in geographical contrast. These plains are not merely 'edges' of the land; they are the result of complex geological processes, specifically the faulting and subsidence of landmasses during the Eocene period Geography of India, Physiography, p.63. This tectonic history explains why the Western and Eastern coasts look so different today.

The Western Coastal Plain is a narrow strip 'sandwiched' between the towering, continuous Western Ghats and the Arabian Sea. Because the Western Ghats act as a steep wall close to the sea, the rivers flowing west are short and swift, forming estuaries rather than deltas. This coast is divided into three distinct zones: the Konkan (Mumbai to Goa) in the north, the Kannad Plain in the center, and the Malabar Coast in the south CONTEMPORARY INDIA-I, Physical Features of India, p.13.

In sharp contrast, the Eastern Coastal Plain is much wider and more level. This width is primarily due to the emergent nature of the coast and the massive alluvial deltas formed by great rivers like the Mahanadi, Godavari, Krishna, and Cauvery Geography of India, Physiography, p.65. Unlike the continuous Western Ghats, the Eastern Ghats are highly discontinuous and dissected by these east-flowing rivers. For instance, ranges like the Veliconda Hills in Andhra Pradesh form part of this broken eastern flank, allowing the coastal plains to stretch further inland. The northern part of this plain is known as the Northern Circar, while the southern part is the Coromandel Coast, famous for receiving rainfall during the retreating monsoon Geography of India, Climate of India, p.41.

Feature	Western Coastal Plain	Eastern Coastal Plain
Width	Narrow (Submerged coast)	Wide (Emergent coast)
River Features	Estuaries (short rivers)	Large Deltas (long rivers)
Ghat Relationship	Abrupt rise of continuous Ghats	Gently rising toward broken hills

Sources: Geography of India, Physiography, p.63; CONTEMPORARY INDIA-I, Physical Features of India, p.13; Geography of India, Physiography, p.65; Geography of India, Climate of India, p.41

4. Major East-Flowing Peninsular Rivers (intermediate)

To understand the major east-flowing peninsular rivers, we must first look at the tectonic tilt of the Indian subcontinent. While the Western Ghats form a continuous wall along the west coast, the entire Deccan Plateau tilts gently toward the east. This structural tilt forces most of the large peninsular rivers to originate near the Western Ghats and flow hundreds of kilometers across the plateau to reach the Bay of Bengal. Unlike the Himalayan rivers, these are non-perennial (seasonal), relying primarily on the monsoon for their volume. Exploring Society: India and Beyond, Social Science-Class VII, Geographical Diversity of India, p.16

The Godavari is the titan of this group, often called the Dakshina Ganga. It is the largest peninsular river, stretching approximately 1,465 km. It originates at Trimbakeshwar near Nasik and drains a massive basin covering Maharashtra, Telangana, and Andhra Pradesh. One of its most distinctive features is its tributary system: while it receives many left-bank tributaries like the Pranhita (the combined flow of the Wardha and Wainganga) and Indravati, it has only one major right-bank tributary, the Manjira. Geography of India, Majid Husain, The Drainage System of India, p.21

South of the Godavari lies the Krishna River, which originates near Mahabaleshwar. It is famous for its bird-foot delta (a Mississippi-type delta) and its significant tributaries like the Bhima (north) and Tungabhadra (south). Interestingly, the landscape between the Krishna and the smaller Pennar river is defined by the Veliconda Hills, a part of the Eastern Ghats that the Krishna has breached to reach the sea. Geography of India, Majid Husain, The Drainage System of India, p.21

Below is a quick ranking of these major basins by their drainage area size, which helps in understanding their geographical dominance. Geography of India, Majid Husain, The Drainage System of India, p.4

Rank	River Basin	Key Characteristic
1	Godavari	Largest Peninsular basin; 'Dakshina Ganga'.
2	Krishna	Second largest; forms a bird-foot delta.
3	Mahanadi	Drains the Chhattisgarh and Odisha plains.
4	Kaveri	Rises in Brahmagiri hills; perennial due to dual monsoons.

Sources: Exploring Society: India and Beyond, Social Science-Class VII, Geographical Diversity of India, p.16; Geography of India, Majid Husain, The Drainage System of India, p.21; Geography of India, Majid Husain, The Drainage System of India, p.4

5. Protected Areas and Biodiversity of the Region (intermediate)

In our journey through Indian physical geography, it is crucial to understand that biodiversity is not randomly distributed; it is a direct product of the landscape. The Peninsular India region, characterized by its ancient plateau and broken hill ranges like the Eastern Ghats, hosts a variety of ecosystems ranging from tropical moist deciduous forests to dry scrub vegetation Environment (Shankar IAS Academy), Indian Biodiversity Diverse Landscape, p.159. These variations are driven by rainfall gradients: while Sal trees dominate the moister north and east, Teak is the king of the southern plateau, with the dry areas of the Aravallis and Rajasthan transitioning into thorny scrub and savannah habitats.

Focusing on the Eastern Ghats, we see a series of discontinuous ranges such as the Nallamala, Erramala, Palkonda, and the Veliconda Hills. The Veliconda range, specifically, forms the eastern flank of the Ghats in Andhra Pradesh, trending north-south between the Krishna and Pennar rivers. This rugged terrain is not just a geological feature but a sanctuary for wildlife. For instance, the Nagarjuna Sagar-Srisailam Tiger Reserve, which spans across Andhra Pradesh and Telangana, stands as the largest tiger reserve in India by area, covering over 3,296 km² Geography of India (Majid Husain), Natural Vegetation and National Parks, p.45. Such protected areas are established to preserve biological heritage for its scientific, ecological, and aesthetic values Geography of India (Majid Husain), Natural Vegetation and National Parks, p.46.

Beyond Tiger Reserves, India utilizes the Biosphere Reserve model to protect larger ecosystems. A biosphere reserve is a unique category of protected area where the goal is to conserve biodiversity while also fostering sustainable development for local communities Contemporary India-I (NCERT Class IX), Natural Vegetation and Wildlife, p.47. Notable examples include the Nilgiri (the first to be established in 1986), Simlipal in Odisha (known for the Royal Bengal tiger and wild elephants), and the Gulf of Mannar (famed for the Dugong or sea cow) Geography of India (Majid Husain), Natural Vegetation and National Parks, p.49.

Feature	National Park	Biosphere Reserve
Primary Goal	Strict protection of wildlife and habitat.	Conservation, research, and sustainable development.
Zonation	Usually a single core area.	Divided into Core, Buffer, and Transition zones.

Sources: Environment (Shankar IAS Academy), Indian Biodiversity Diverse Landscape, p.159; Geography of India (Majid Husain), Natural Vegetation and National Parks, p.45; Geography of India (Majid Husain), Natural Vegetation and National Parks, p.46; Geography of India (Majid Husain), Natural Vegetation and National Parks, p.49; Contemporary India-I (NCERT Class IX), Natural Vegetation and Wildlife, p.47

6. Regional Hill Ranges of the Eastern Ghats (exam-level)

Unlike the Western Ghats, which stand as a continuous wall of mountains, the Eastern Ghats are a series of detached, discontinuous hill ranges. These hills have been heavily eroded and bisected by the great peninsular rivers like the Mahanadi, Godavari, Krishna, and Cauvery, which flow eastwards into the Bay of Bengal CONTEMPORARY INDIA-I NCERT Class IX, Physical Features of India, p.12. To master this geography, we must view these hills as regional clusters that change character as we move from Odisha down to Tamil Nadu.

In the northern stretch (between the Mahanadi and Godavari), the elevation is higher, averaging around 1100 meters. Here, you will find prominent peaks like Aroya-Konda (the highest at 1680 m) and Mahendragiri in Odisha Geography of India Majid Husain, Physiography, p.61. Geologically, these hills are composed of ancient rocks like khondalites and charnockites, which are metamorphic and intrusive in nature.

The central part of the Eastern Ghats, primarily in Andhra Pradesh, consists of several distinct parallel ranges located between the Krishna river and Chennai. These include:

• Nallamala Hills: Located in the Rayalaseema region, known for their rugged terrain.
• Erramala Hills: Situated to the west of the Nallamala range.
• Veliconda Hills: These trend in a north-south direction and form the eastern flank of the system in the Nellore and Prakasam districts. They are relatively low but include peaks like Bhairani Konda (approx. 1100 m).
• Palkonda Hills: Located further south, primarily in the Anantapur and Chittoor districts.

As the Eastern Ghats move into Tamil Nadu, they continue as the Javadi, Shevaroy, Panchaimalai, and Sirumalai Hills Geography of India Majid Husain, Physiography, p.62. Eventually, the Eastern Ghats lose their identity as they meet the Western Ghats at the Nilgiri Hills. Understanding this sequence is vital because it explains the drainage patterns and the climatic variations of the eastern coast.

Region	Key Hill Ranges	Notable Peaks
Northern (Odisha/North AP)	Maliya, Madugula Konda	Aroya-Konda, Mahendragiri
Central (Andhra Pradesh)	Nallamala, Erramala, Veliconda, Palkonda	Bhairani Konda
Southern (Tamil Nadu)	Javadi, Shevaroy, Panchaimalai, Sirumalai	Solaipallam

Sources: CONTEMPORARY INDIA-I NCERT Class IX, Physical Features of India, p.12; Geography of India Majid Husain, Physiography, p.61; Geography of India Majid Husain, Physiography, p.62

7. Hills of the Cuddapah and Kurnool Systems (exam-level)

When we study the Eastern Ghats, we aren't looking at a continuous mountain wall like the Western Ghats. Instead, we see a series of broken, weathered, and ancient hill ranges. In the heart of Andhra Pradesh, these hills are geologically linked to the Cuddapah and Kurnool sedimentary systems—ancient basins filled with rocks like quartzites, shales, and limestones that have been folded and uplifted over eons.

The central portion of the Eastern Ghats is characterized by a group of parallel ranges located between the Krishna and Pennar rivers. These include the Nallamala, Erramala, Veliconda, and Palkonda ranges Majid Husain, Geography of India, Chapter 2, p.62. While they might appear as a jumble on a map, they follow a distinct structural pattern. The Veliconda Hills (meaning 'outside hills' in Telugu) form the easternmost flank of this system, trending north-south through the Nellore and Prakasam districts. They are relatively low in elevation, though peaks like Bhairani Konda reach about 1100 meters.

Range Name	Key Characteristics	Notable Features
Nallamala Hills	Located to the west of the Veliconda range.	Famous for dense forests and the Krishna river gorge.
Veliconda Range	Forms the eastern edge of the Ghats in this region.	Discontinuous nature; acts as a flank to the Cuddapah basin.
Palkonda/Seshachalam	Located further south-west towards Tirupati.	Known for rich mineral deposits and ancient rock formations.

Geologically, these hills are composed of Khondalites (metamorphosed sedimentary rocks) and Charnockites Majid Husain, Geography of India, Chapter 2, p.62. Unlike the Himalayas, these are relict mountains, meaning they are the remains of much larger structures that have been worn down by millions of years of erosion. This explains why the Eastern Ghats are lower and more fragmented compared to the western edge of the Deccan Plateau NCERT Class IX, Contemporary India-I, Chapter 2, p.12.

Sources: Geography of India, Physiography, p.62; Contemporary India-I, Geography, Class IX, Physical Features of India, p.12

8. Solving the Original PYQ (exam-level)

Now that you have mastered the Physiography of India, you can see how individual building blocks like drainage basins and tectonic trends converge in this question. You previously learned that the Eastern Ghats are not a continuous chain but a series of broken hill ranges fragmented by major rivers. By identifying the Veliconda Hills as being situated between the Krishna and Pennar rivers, you are applying your knowledge of regional drainage to pinpoint geographical locations. This specific range follows the classic North-South trend characteristic of the central Eastern Ghats, a concept detailed in Geography of India by Majid Husain.

To arrive at the correct answer, (D) Andhra Pradesh, think like a cartographer. Visualize the "Konda" suffix, which is a common linguistic marker in the region for "hill." In your learning path, we grouped the Nallamala, Palkonda, and Erramala ranges together; the Veliconda Hills form the easternmost flank of this same structural group. Since these companion ranges are centrally located within the Nellore and Prakasam districts, it becomes logically consistent to place Veliconda within the same state boundary. This spatial association is a key mental shortcut for solving UPSC map-based questions when you cannot recall the exact coordinate.

UPSC often uses neighboring states as distractors to test your precision. While Odisha (A) is home to the northern Eastern Ghats like Mahendragiri, it lacks the specific structural cluster of the "Konda" group. Tamil Nadu (B) is a common trap because it also hosts significant Eastern Ghats sections, but these are typically the "Malai" ranges, such as the Javadi or Shevaroy Hills. Karnataka (C) is primarily territory of the Western Ghats, and its few Eastern Ghats extensions are situated much further west. By recognizing the linguistic patterns and the inter-riverine positioning, you can confidently eliminate the traps and select Andhra Pradesh.