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Hills of Peninsular India
Page 2


Hills of Peninsular India
Aravali Range
• They are aligned in north-east to south-west direction.
• They run for about 800 km between Delhi and Palanpur in Gujarat.
• They are one of the oldest (very old) fold mountains of the world and the 
oldest in India. {Fold Mountains – Block Mountains}
• Now they are relict (remnants after severe weathering and erosion since 
millions of years) of the world’s oldest mountain formed as a result of 
folding (Archaean Era).
• At the south-west extremity the range rises to over 1,000 m. Here Mt. Abu 
(1,158 m), a small hilly block, is separated from the main range by 
the valley of the Banas. Guru Sikhar (1,722 m), the highest peak, is 
situated in Mt. Abu.
• Pipli Ghat, Dewair and Desuri passes allow movement by roads and 
railways.
Page 3


Hills of Peninsular India
Aravali Range
• They are aligned in north-east to south-west direction.
• They run for about 800 km between Delhi and Palanpur in Gujarat.
• They are one of the oldest (very old) fold mountains of the world and the 
oldest in India. {Fold Mountains – Block Mountains}
• Now they are relict (remnants after severe weathering and erosion since 
millions of years) of the world’s oldest mountain formed as a result of 
folding (Archaean Era).
• At the south-west extremity the range rises to over 1,000 m. Here Mt. Abu 
(1,158 m), a small hilly block, is separated from the main range by 
the valley of the Banas. Guru Sikhar (1,722 m), the highest peak, is 
situated in Mt. Abu.
• Pipli Ghat, Dewair and Desuri passes allow movement by roads and 
railways.
Vindhyan Range
• It runs more or less parallel to the Narmada Valley in an east-west 
direction from Jobat in Gujarat to Sasaram in Bihar for a distance of 
over 1,200 km.
• The Vindhyas are continued eastwards as the Bharner and Kaimur
hills.
• This range acts as a watershed between the Ganga system and the 
river systems of south India.
• The rivers Chambal, Betwa and Ken rise within 30 km of the 
Narmada.
Page 4


Hills of Peninsular India
Aravali Range
• They are aligned in north-east to south-west direction.
• They run for about 800 km between Delhi and Palanpur in Gujarat.
• They are one of the oldest (very old) fold mountains of the world and the 
oldest in India. {Fold Mountains – Block Mountains}
• Now they are relict (remnants after severe weathering and erosion since 
millions of years) of the world’s oldest mountain formed as a result of 
folding (Archaean Era).
• At the south-west extremity the range rises to over 1,000 m. Here Mt. Abu 
(1,158 m), a small hilly block, is separated from the main range by 
the valley of the Banas. Guru Sikhar (1,722 m), the highest peak, is 
situated in Mt. Abu.
• Pipli Ghat, Dewair and Desuri passes allow movement by roads and 
railways.
Vindhyan Range
• It runs more or less parallel to the Narmada Valley in an east-west 
direction from Jobat in Gujarat to Sasaram in Bihar for a distance of 
over 1,200 km.
• The Vindhyas are continued eastwards as the Bharner and Kaimur
hills.
• This range acts as a watershed between the Ganga system and the 
river systems of south India.
• The rivers Chambal, Betwa and Ken rise within 30 km of the 
Narmada.
Satpura Range
• Satpura range is a series of seven mountains (‘Sat’ = seven and ‘pura’ 
= mountains)
• It runs in an east-west direction south of the Vindhyas and in 
between the Narmada and the Tapi, roughly parallel to these rivers.
• It stretches for a distance of about 900 km.
• Parts of the Satpuras have been folded and upheaved. They are 
regarded as structural uplift or ‘hor s t ’.
• Dhupgarh (1,350 m) near Pachmarhi on Mahadev Hills is the highest 
peak.
• Amarkantak (1,127 m) is another important peak.
Page 5


Hills of Peninsular India
Aravali Range
• They are aligned in north-east to south-west direction.
• They run for about 800 km between Delhi and Palanpur in Gujarat.
• They are one of the oldest (very old) fold mountains of the world and the 
oldest in India. {Fold Mountains – Block Mountains}
• Now they are relict (remnants after severe weathering and erosion since 
millions of years) of the world’s oldest mountain formed as a result of 
folding (Archaean Era).
• At the south-west extremity the range rises to over 1,000 m. Here Mt. Abu 
(1,158 m), a small hilly block, is separated from the main range by 
the valley of the Banas. Guru Sikhar (1,722 m), the highest peak, is 
situated in Mt. Abu.
• Pipli Ghat, Dewair and Desuri passes allow movement by roads and 
railways.
Vindhyan Range
• It runs more or less parallel to the Narmada Valley in an east-west 
direction from Jobat in Gujarat to Sasaram in Bihar for a distance of 
over 1,200 km.
• The Vindhyas are continued eastwards as the Bharner and Kaimur
hills.
• This range acts as a watershed between the Ganga system and the 
river systems of south India.
• The rivers Chambal, Betwa and Ken rise within 30 km of the 
Narmada.
Satpura Range
• Satpura range is a series of seven mountains (‘Sat’ = seven and ‘pura’ 
= mountains)
• It runs in an east-west direction south of the Vindhyas and in 
between the Narmada and the Tapi, roughly parallel to these rivers.
• It stretches for a distance of about 900 km.
• Parts of the Satpuras have been folded and upheaved. They are 
regarded as structural uplift or ‘hor s t ’.
• Dhupgarh (1,350 m) near Pachmarhi on Mahadev Hills is the highest 
peak.
• Amarkantak (1,127 m) is another important peak.
Western Ghats (or The Sahyadris)
• They form the western edge of 
the Deccan tableland.
• Run from the Tapi valley (21° N 
latitude) to a little north of 
Kanniyakumari (11° N latitude) 
for a distance of 1,600 km.
• The Western Ghats are steep-
sided, terraced, flat-topped hills 
presenting a stepped 
topography facing the Arabian 
Sea coast.
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FAQs on PPT: Peninsular India- 2 - Geography for UPSC CSE

1. What are the major geographical features of peninsular India?
Ans. Peninsular India is characterized by several major geographical features including the Deccan Plateau, the Western Ghats, the Eastern Ghats, and the coastal plains. The Deccan Plateau occupies a large portion of peninsular India and is composed of rugged terrain with several rivers flowing through it. The Western Ghats and the Eastern Ghats are mountain ranges that run parallel to the coastline, while the coastal plains lie along the Arabian Sea and the Bay of Bengal.
2. Which states are part of peninsular India?
Ans. Several states in India are part of peninsular India. These include Maharashtra, Goa, Karnataka, Kerala, Tamil Nadu, Andhra Pradesh, and Telangana. Additionally, parts of Odisha and Gujarat are also considered to be part of the peninsular region.
3. What is the significance of the Western Ghats in peninsular India?
Ans. The Western Ghats in peninsular India are of great significance due to their ecological and biological importance. They are recognized as a UNESCO World Heritage Site and are known for their rich biodiversity. The Western Ghats are home to numerous endemic species of plants and animals, making them a hotspot for conservation efforts. They also act as a barrier to the monsoon winds, causing heavy rainfall on the windward side and creating a rain shadow on the leeward side.
4. How do the coastal plains contribute to the economy of peninsular India?
Ans. The coastal plains in peninsular India play a significant role in the economy of the region. They are ideal for agriculture, particularly for the cultivation of crops like rice, coconut, and spices. The coastal plains also support industries such as fishing, salt production, and tourism. The ports located along the coast facilitate trade and commerce, further contributing to the economic development of the region.
5. What is the climate like in peninsular India?
Ans. The climate in peninsular India varies across different regions. The coastal areas experience a tropical monsoon climate, characterized by high temperatures, heavy rainfall, and high humidity. The interior parts of the region, including the Deccan Plateau, have a semi-arid climate with hot summers and moderate rainfall. The Western Ghats influence the climate by causing heavy rainfall on the windward side and creating a rain shadow on the leeward side, resulting in drier conditions.
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