Which of the following are the oldest folded mountain in India?
Aravalli Range
The question asks to identify the oldest folded mountain range located in India from the given options. Understanding the geological age and formation process of different mountain ranges in India is key to answering this question.
Folded mountains are created when two or more of Earth's tectonic plates are pushed together. This immense pressure causes the layers of rock and sediment between them to buckle and fold, much like pushing the ends of a rug together.
Let's look at the characteristics of each mountain range listed:
Comparing the geological ages and formation types, the Aravalli Range stands out as the oldest among the options and is recognized as the oldest folded mountain range in India. While other ranges are also ancient, the Aravallis represent the highly eroded remnants of a very early mountain-building event involving intense folding.
| Mountain Range | Primary Type/Age | Location |
|---|---|---|
| Aravalli Range | Old Folded (Residual) / Proterozoic (Oldest) | Rajasthan, Haryana, Delhi, Gujarat |
| Vindhya Range | Escarpment / Ancient (Older than Himalayas) | Central India |
| Satpura Range | Block Mountain / Ancient (Older than Himalayas) | Central India |
| Himalayan Range | Young Folded / Cenozoic (Youngest) | Northern India |
Based on this analysis, the Aravalli Range is the oldest folded mountain in India.
| Mountain Range | Age Classification | Formation Type | Current Form |
|---|---|---|---|
| Aravalli Range | Oldest | Folded Mountains (formed during orogeny) | Residual Hills (due to erosion) |
| Vindhya Range | Ancient | Uplifted Block/Escarpment | Plateau Edge/Hills |
| Satpura Range | Ancient | Block Mountains (Fault-block) | Ridges and Plateaus |
| Himalayan Range | Youngest | Folded Mountains (collision of plates) | High Peaks (still rising) |
The Aravalli Range represents a very significant geological event in the history of the Indian subcontinent. Its formation is linked to an ancient collision event that occurred when continental masses came together during the Precambrian era, specifically the Proterozoic Eon (roughly 2.5 billion to 541 million years ago). This process, known as orogeny or mountain building, created a massive mountain belt. Over vast geological timescales, forces of erosion (wind, water) have worn down these mountains significantly, leaving behind the present-day Aravalli hills, which are considered residual mountains, meaning they are the remnants of much larger, older structures. Their rocks are some of the oldest on the planet, containing evidence of these early tectonic activities. Understanding the Aravallis helps geologists study the early stages of Earth's crustal development and continental formation.
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