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Le Morne Brabant [lə mɔʁn bʁa.bɑ̃] is a peninsula at the extreme southwestern tip of the Indian Ocean island of Mauritius. On it is a basaltic monolith of the same name 556 metres (1,824 ft) high. Its summit covers an area of over 12 hectares (30 acres). There are many caves and overhangs on the steep slopes.
Trou aux Cerfs (also known as Murr's Volcano) is a dormant, crater lake, cinder cone volcano with a well-defined cone and crater. It is 605 m (1,985 ft) high and located in Curepipe , Mauritius . The crater has been alternately described as 300 [ 1 ] and 350 meters in diameter, [ 2 ] and is 80 meters deep.
Pages in category "Waterfalls of Mauritius" This category contains only the following page. This list may not reflect recent changes. T. Tamarind Falls
Ganga Talao (commonly known as Grand Bassin) is a crater lake situated in a secluded mountain area in the district of Savanne, deep in the heart of Mauritius. It is about 550 m (1,800 ft) above sea level. It is considered the most sacred Hindu place in Mauritius.
The chemical makeup of Clear Lake allows it to live up to its name, with over 100 feet of visibility underwater, said Powelson. About 3,000 years ago, lava from an eruption of Sand Mountain flowed ...
The highest point is 828 meters above sea level. Mauritius is the most populous of the Mascarene Islands, [1] with a population of 1,252,964. Réunion is located 150 km southwest of Mauritius. It is the largest of the islands, with an area of 2512 km 2. Piton des Neiges (3,069 m), an extinct volcano, is the highest peak on Réunion and in the ...
There are 3 national parks in Mauritius. [1] [2] Black River Gorges National Park, established in 1994, is the oldest and by far most visited. National parks
The geology of Mauritius and Rodrigues is comparatively recent. The oldest rocks on Mauritius are only 10 million years old and 1.54 million years old on Rodrigues Island. The mafic basalts of the two islands formed in relation to the hotspot that generated the Deccan Traps and coral reefs built on the volcanoes forming non-volcanic sediments. [1]
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