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The Aravalli Range is a mountain range located in Northern-Western India. The length of the range is approximately 670 km which runs in south-west direction. The range starts near Delhi and passes through Haryana, Rajasthan and finally ends in Gujarat. The Aravalli Range is a significant ecological hotspot due to its rich geological history, diverse flora and fauna. It provides significant fresh water to neighbouring states and act as a natural buffer from adjoining desert. The range faces concerns from unorganised urbanization, overexploitation of natural resources, mining, loss of forest cover and wildlife habitat. Centre and state governments along with the Supreme Court has stepped in to conserve it and the Aravalli Green Wall project is a welcome and holistic move.
Fold mountains are formed when two or more of the Earth’s tectonic plates collide and the sedimentary rocks are twisted and collapsed into rough slopes, mountains and entire mountain range. This process is also called as Orogeny.
The Aravali Range is one of the oldest mountain ranges in the world, extending approximately 800 kilometers across the northwestern part of India. It runs through the states of Gujarat, Rajasthan, Haryana, and Delhi.
Guru Shikhar (1722 metres) is the highest peak in the Aravali Range. It is located in the Mount Abu region of Rajasthan.
It is process of land degradation in which fertile land turns barren by losing its natural resources. Some of the causes of desertification are deforestation, over-cultivation, over-grazing, drought, or human actions.
Historically, the Aravalli Range has significantly determined the region's cultural and economic development. The range is one of the oldest mountain ranges of the world that was formed by orogenic process of folding and dates earlier than the formation of the Himalayan ranges. The approximate age of Aravallis is around 670 million years and belong to Pre-Cambrian era. The Aravalli were higher in ancient times but due to many years of weathering they have worn down considerably. The Aravallis and its geography have played a major role in shaping the region's history and will keep on shaping its future too.
The Aravalli Range has its own spiritual significance coupled with its natural beauty as it is adorned with sites which are sacred in nature such as Dilwara Jain Temples. Many wildlife sanctuaries, national parks and reserves such as Sariska tiger Reserve and Mount Abu Wildlife Sanctuary are located within the Aravalli Range. The Aravalli mountains are not just geological marvels; they are an integral part of India’s cultural and natural heritage. These majestic ranges are a recognized global biodiversity hotspot, showcasing India’s commitment to preserving its natural splendour.
A 1400 km long Green Wall of India from Porbandar to Panipat will help in restoring degraded land through afforestation along the Aravali hill range.
The Aravallis play a vital role in regional ecology. They act as a barrier against Thar Desert expansion, regulate climate, and provide water sources for millions. They are an ecological hotspot in northwest India. However, decades of deforestation, mining, and urbanization have degraded its natural resources and threatened biodiversity. Water scarcity, desertification, and human-wildlife conflict are major concerns.
Positive strides have been made towards conservation. The Supreme Court has recognized the Aravallis as a national asset and ordered demolition of illegal structures. The ambitious Aravalli Green Wall project aims to restore degraded lands through afforestation. By addressing the challenges and implementing effective conservation measures, we can ensure a healthy future for this vital ecosystem and its surrounding communities. This requires a concerted effort from all stakeholders - government, NGOs, and local communities - to work together for the long-term sustainability of the Aravalli Range.
List-I | List-II |
---|---|
A. Deccan Traps | 1. Late Cenozoic |
B. Western Ghats | 2. Pre-Cambrian |
C. Aravalli | 3. Cretaceous Eocene |
D. Narmada-Tapi alluvial Deposits | 4. Cambrian |
5. Pleistocene |
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