Q1. Describe the Important features of the Peninsular Plateau.
Ans: The Peninsular Plateau of India lies to the south of the Northern Plains and extends up to the tip of the Indian peninsula. It is a flat land with gentle hills and wide valleys.
The Peninsular Plateau is one of the oldest landmasses, formed by the breaking of the Gondwana land. It is a triangular-shaped landmass composed of ancient igneous and metamorphic rocks. It consists of two broad divisions — the Central Highlands and the Deccan Plateau.
1. Central Highlands (north of the Narmada River) – includes the Malwa Plateau, Bundelkhand, Baghelkhand, and the Vindhya Range. It extends eastward to the Chhota Nagpur Plateau. The Aravalli Hills, old and worn down, lie to the west and northwest.
2. Deccan Plateau (south of the Narmada River) – has a broad base in the north and narrows towards the south. It is formed from volcanic lava, mostly made of basalt rocks. The Satpura Range is to its north, while the Mahadev, Kaimur, and Maikal hills extend to the east. It is bordered by the Western Ghats (900-1600 meters high) and the Eastern Ghats (600 meters high). The plateau slopes from west to east. The black soil area here is called the Deccan Trap.
Q2. Write a note on the different parts of the Great Himalayan range.
Ans: The Himalayas are one of the highest and roughest mountain ranges in the world. They stretch from the Indus River in the west to the Brahmaputra River in the east, forming India’s northern border.
The Himalayan region has three main mountain ranges running parallel from west to east:
1. Greater or Inner Himalayas (Himadri):
2. Lesser Himalayas (Himachal):
3. Outer Himalayas (Shivaliks):
Q3. Explain about Barchans.
Ans: Barchans are crescent-shaped dunes that form in arid or desert regions with a predominant wind direction. They have the following characteristics:
Shape and Formation: Barchans have a curved or crescent shape, with the open side facing the direction of the prevailing wind. They form when the wind blows consistently from one direction, causing sand to accumulate on the leeward side of an obstacle or in a region where the wind’s speed decreases.
Movement: Barchans migrate slowly across the desert as the wind continually moves sand from the windward side to the leeward side. The movement is gradual and can lead to the shifting of these dunes over time.
Size and Scale: Barchans can vary in size from small hills to large dunes. Their size and shape are influenced by the availability of sand and the intensity of the wind.
Q4. Describe the causes of the Shiwalik Ranges’ vulnerability to earthquakes and landslides.
Ans: The Shiwalik Ranges are particularly prone to landslides and earthquakes due to several factors:
Tectonic Activity: The Shiwaliks lie where the Indian Plate and the Eurasian Plate meet. These plates keep pushing against each other, which makes the area shake and causes earthquakes.
Geological Composition: The mountains are made of soft soil, sand, and small stones. This loose material easily breaks or slips during heavy rain or earthquakes.
Steep Slopes: The steep slopes and rugged terrain increase landslide risk. Rainfall can cause the soil to become saturated, increasing its weight and reducing stability, leading to landslides.
Human Activities: Deforestation, construction, and other human activities in the region disturb the natural stability of the slopes. These activities can weaken the ground and trigger landslides, particularly in areas where the natural vegetation has been removed.
Q5. Which part of the Himalayas is known as Purvanchal? Write a short note on the Purvanchal Himalayas.
Ans: The eastern hills and mountains of the Himalayas running along the eastern boundary of India are known as Purvanchal.

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