What is the estimated age of the Kebira crater in Libya?

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In summary, the Kebira crater is estimated to be around 100 million years old and its age was determined through radiometric dating of the rocks found in and around it. The crater was formed by a meteorite impact and is not the only one of its age, as there are many others found on Earth and other planets in our solar system. Studying the Kebira crater can provide valuable information about the history of our planet, including the frequency and effects of meteorite impacts and the changes that have occurred over the past 100 million years.
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pixel01
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I have read some article about this crater in Lybia, but still have no idea the age of it. Anybody knows that?

Thanks you.
 
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Ohh, I found it myself : about tens of millions of years. The crater is also called glass desert.
 
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The age of the Kebira crater in Libya is estimated to be around 100 million years old. This estimate is based on the age of the rocks surrounding the crater and the geological processes that have occurred in the region over time. However, it is important to note that this is just an estimate and the exact age of the crater may vary. Further research and analysis may provide a more accurate age in the future.
 

1. What is the age of the Kebira crater?

The Kebira crater is estimated to be around 100 million years old.

2. How was the age of the Kebira crater determined?

The age of the Kebira crater was determined through radiometric dating of the rocks found in and around the crater.

3. What caused the formation of the Kebira crater?

The Kebira crater was formed by a meteorite impact, also known as an impact event.

4. Is the Kebira crater the only crater of its age?

No, there are many other craters of similar age found on Earth and other planets in our solar system.

5. What can studying the Kebira crater tell us about the history of our planet?

Studying the Kebira crater can provide insight into the frequency and effects of meteorite impacts on Earth, as well as the geological and environmental changes that have occurred over the past 100 million years.

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