The Aravalli Hills are among the oldest fold mountain ranges in the world. Their formation dates back to the Precambrian era, roughly 1.5–2.5 billion years ago.
1. Ancient Geological Activity
The Aravalli range was formed due to tectonic plate movements in very ancient times.
Two crustal blocks—the Bundelkhand craton and the Marwar craton—collided.
This collision caused folding, faulting, and uplift of rocks, creating the early Aravalli mountains.
2. The Aravalli Orogeny
The mountain-building process is known as the Aravalli Orogeny.
During this event:
Sediments in an ancient sea were compressed and folded.
These sediments transformed into metamorphic rocks like schist, gneiss, and quartzite.
3. Erosion Over Billions of Years
After their formation, the Aravalli mountains were continuously eroded by wind, water, and weathering.
Because of this long erosion:
The range is now low and discontinuous compared with younger mountains like the Himalayas.
4. Present Structure
The range extends about 700–800 km from Delhi through Rajasthan to Gujarat.
The highest peak is Guru Shikhar in Mount Abu.
✅ In short:
The Aravalli Hills were formed by ancient tectonic collisions and folding during the Precambrian era, followed by billions of years of erosion, which reduced them to the worn-down hills seen today.
If you want, I can also explain:
Aravalli Hills formation in 5 easy points for exams, or
A labeled diagram of Aravalli formation (very useful for geography answers).
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