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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.
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.
The place has become one of Mauritius' main tourist attractions since the 1960s. Nowadays, the dunes are protected by a wooden fence and visitors are not allowed to climb on them, although they can look at the scenery from observation outposts placed along the fence. Curio shops in the area sell small test-tubes filled up with the coloured earths.
Pages in category "Volcanoes of Mauritius" The following 2 pages are in this category, out of 2 total. This list may not reflect recent changes. R. Rodrigues; T.
The Mascarene Islands, the island chain that Mauritius lies in, is a volcanic belt. [4] Le Pouce is the second highest peak in the Moka Range, which was formed ten million years ago from volcano eruptions. [5] The range is a basalt lava dome and is no longer volcanically active. [5]
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.
If you’re stuck on today’s Wordle answer, we’re here to help—but beware of spoilers for Wordle 1252 ahead. Let's start with a few hints.
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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