Ouarkziz
Ouarkziz Crater is an impact structure located in northwestern Algeria, near the Moroccan border. This 3.5-kilometer diameter crater was formed by a meteor impact less than 70 million years ago, during the late Cretaceous Period. Despite significant erosion, its circular shape is still discernible, highlighting older sedimentary rock layers.
Key Facts
- ›Diameter: 3.5 kilometers
- ›Age: less than 70 million years old (Cretaceous or younger)
- ›Location: Tindouf, Algeria
- ›Morphology: Circular, with exposed sedimentary rock layers forming ridgelines
- ›Visibility: Clearly visible from the International Space Station with magnification
- ›Discovery: Identified through geological interpretation of images
About Ouarkziz
Ouarkziz Crater
Ouarkziz Crater is an impact structure located in Tindouf, Algeria, in the northwestern part of the country near the border with Morocco. This crater, measuring approximately 3.5 kilometers in diameter, resulted from a meteor impact that occurred less than 70 million years ago, during the late Cretaceous Period of the Mesozoic Era.
Geological Features and Visibility
Despite considerable erosion since its formation, the Ouarkziz Crater retains a discernible circular morphology. This shape is accentuated by the exposure of older sedimentary rock layers, which form ridgelines trending roughly northwest to southeast. Geologists can interpret the crater's formation by observing the relationship between the crater and these rock layers; the fact that the crater is superimposed on the existing rock layers indicates that the impact event occurred after the rocks were in place. Furthermore, a stream channel cutting across the center of the structure demonstrates that the channel formed subsequent to the impact.
The Ouarkziz Crater is notable for its visibility from space. From the vantage point of an astronaut aboard the International Space Station, the impact crater is clearly discernible when viewed with a magnifying camera lens. This feature underscores its significance as a visible testament to extraterrestrial impacts on Earth's surface.
Age and Geological Context
The age of the Ouarkziz Crater is estimated to be less than 70 million years, placing its formation within the Cretaceous Period or younger. This geological timeframe is significant as it aligns with periods of notable geological activity and potential extraterrestrial events. The crater is exposed at the surface, allowing for direct study of its features and the surrounding geological context. Its identification and study contribute to the broader understanding of impact cratering on Earth and the geological history of the African continent.
Source: Wikipedia ↗
Frequently Asked Questions
Where is the Ouarkziz Crater located?
The Ouarkziz Crater is situated in Tindouf, Algeria, in the northwestern part of the country, close to the border with Morocco.
How large is the Ouarkziz Crater?
The Ouarkziz Crater has a diameter of approximately 3.5 kilometers.
When did the impact event that formed Ouarkziz Crater occur?
The impact event is estimated to have occurred less than 70 million years ago, during the late Cretaceous Period of the Mesozoic Era.
Can the Ouarkziz Crater be seen from space?
Yes, the Ouarkziz Crater is clearly visible from the International Space Station when viewed with a magnifying camera lens.
What is the current state of the Ouarkziz Crater?
The Ouarkziz Crater has been heavily eroded since its formation. However, its circular morphology remains, with exposed sedimentary rock layers forming ridgelines.
Related Impact Craters
Decorah
The Decorah crater, located near Decorah, Iowa, is a potential impact structure estimated to be 5.6 km in diameter. It is believed to have formed approximately 470 million years ago during the Middle Ordovician period when a meteor around 200 meters wide struck the Earth, pushing down the underlying bedrock. Despite its significant size, no surface evidence of the impact remains due to burial by the Winneshiek Shale.
Jänisjärvi
Jänisjärvi is a lake in the Republic of Karelia, Russia, whose basin was formed by a meteorite impact approximately 700 million years ago. The impact created a circular crater with a diameter of 14 kilometers. It was once mistakenly identified as a volcanic caldera before its true impact origin was recognized.

Tvaren
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