User:Rouve Pofadder (211003417)

Burnt Mountains: Namibia

The area where the valleys of the Burnt Mountains cover, lies in the Kunene Region (22°35'S - 14°22'E). It is commonly mistaken for "Brandberg Mountain". It is formerly known for the way it looks like. The exposed layers of rock are in such a manner because it were burnt.

Formation

Due to scientific research and expedition, it is estimated that this mountain has been around for millions of years since its formation. It was formed when part of Namibia was engulfed with ocean water. Due to the dead organisms that drifted to the ocean floor and the drying up of the ocean floor, the land became vulnerable to soil erosion with drought. The exerted pressure of sand created stress and formed variable sedimented layers of shale. Soon the tectonic plates started to move the magma from below the crust exerted great amounts of heat against the crust and resulted in the contact of magma with the solid shale mixture of organic material and silt. The great amounts of heat ensured that the resultant shale was a blackish color but it remained compacted (compressed).

Natural habitat

There are various types of species that live along the mountain. Some close up animals that come too this extraordinary place would be monkeys, where they bask under the sun and enjoy a relaxing moment. This location is found at the grasslands and savanna. It is characterized by predominant grass and bush (shrubs). There are not fairly so many trees as in a forest, since there is not enough rainfall that can support that much. Rainfall usually occur during summer, but during winter it is usually dry. The temperature is average, not too high nor too low, which makes it a suitable area for most animal and plant species.

Nearby attractions

• Twyfelfontein
• Organ Pipes (Twyfelfontein)
• Damaraland
• Dessert elephants

Recreational activities

• Elephant nature drive
• Bird watching
• Excursion
• Hiking