A Journey Through Time in the High Ridges of Armenia
The Armenian Highland stands as a testament to the Earth’s dynamic geological history. The high ridges of Armenia are the result of the most recent, Alpine stage of mountain building. This intensive uplift began approximately 25 million years ago, during a time when much of the highland was still submerged under water.
The Retreat of the Great Sea
The relentless growth of these mountains caused the once expansive Great Sea to gradually retreat. However, this does not imply that all the geological formations in the Armenian Highland are younger than 25 million years. In fact, the region is a geological treasure trove, preserving traces of much older eras.
Ancient Foundations
- The rocks forming the foundation of the Pambak Range date back a staggering one to two billion years.
- The Proterozoic layers in the region are over 570 million years old, offering a glimpse into the distant past.
Traces of Ancient Magmatism
- The Tsaghkunyat Range is home to gneisses, micas, amphibolites, and migmatites, with some samples dating back 2.7 billion years.
- These ancient rocks bear witness to the initial phase of the Earth’s crust formation.
The Picturesque Tsaghkunyat Range
- The Tsaghkunyat Range is renowned for its breathtaking scenery, featuring numerous waterfalls and lakes along its slopes.
- A cable car in Tsaghkadzor connects the base of the range to the peak of Tekhnisi, standing at 2,846 meters.
A Geological Storehouse
The Armenian Highland is not just a region of stunning natural beauty but also a geological storehouse, preserving the Earth’s history from its very beginnings. The ancient rocks and formations found here provide invaluable insights into the processes that shaped our planet.
The Armenian Highland offers a unique opportunity to explore the Earth’s geological past, with its ancient rocks and stunning landscapes. Whether you’re a geology enthusiast or simply a lover of nature, this region promises a journey through time like no other.
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