Earth is a very old planet that was formed billions of years ago. Over this long time, many rocks were created, changed, and broken down. Some rocks from the early period of Earth still exist today. These ancient rocks are very special because they help scientists understand how our planet first began, what the early surface was like, and how the Earth slowly developed over time.
The Acasta Gneiss is one of the oldest known rocks on Earth. Studies show that it is around 4.0 to 4.03 billion years old. This means it was formed when the Earth was still very young and slowly changing from a hot, molten planet into a solid world.
Scientists used special dating methods, such as radiometric testing, to measure the age of the minerals inside the rock. These tests proved that the Acasta Gneiss formed during the early Archean Era, a time when the Earth’s crust had just begun to cool and harden. Because of this, it is considered one of the oldest exposed rocks ever found.
The rock is named after the Acasta River region in Canada, where it was discovered. The word “gneiss” describes the rock’s striped and layered look, which formed after billions of years of heat and pressure deep inside the Earth.
The Acasta Gneiss is found in the Canadian Shield, in Canada’s Northwest Territories. This region is famous for having very ancient rocks and is an important area for scientists who study the early history of the Earth.
While Acasta Gneiss is one of the oldest rocks, the oldest minerals ever found are zircon crystals from Jack Hills in Western Australia.
These tiny crystals are around 4.3–4.4 billion years old, making them older than any rock formation known today.
India also has very ancient rocks. Some of the oldest rocks are found in:
These belong to the Dharwar Craton, one of the earliest rock systems in the Indian subcontinent.
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