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It is the remains of one of the seven Pleistocene epoch volcanoes that formed the prehistoric Maui Nui island, during the Quaternary Period of the Cenozoic Era. The islet has an area of 23 acres (9.3 ha), [ 2 ] a diameter of about 0.4 miles (0.6 km), is 161 feet (50 m) at its highest point, [ 3 ] and is located about 2.5 miles (2.2 nmi; 4.0 km ...
Koko Guyot is a 48.1-million-year-old guyot, [3] a type of underwater volcano with a flat top, which lies near the southern end of the Emperor seamounts, about 200 km (124 mi) north of the "bend" in the volcanic Hawaiian-Emperor seamount chain. [5]
Pages in category "Waterfalls of Mauritius" This category contains only the following page. This list may not reflect recent changes. T. Tamarind Falls
Interior while submerged. Atlantis Submarines is a Canadian passenger submarine company. The company currently has 12 submarines and operates undersea tours in Grand Cayman, Barbados, Aruba, St. Thomas, Cozumel and in Hawaii at Kona, Maui and Oahu to explore and observe the marine life and underwater landscapes without getting wet.
The Tamarind Falls or Tamarin Falls are a scenic attraction of southwest Mauritius. They are a series of seven cataracts located on the Rivière Tamarin , two kilometers northwest of the large lake Mare aux Vacoas .
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 ...
Haleakalā National Park is a national park of the United States located on the island of Maui, Hawaii.Named after Haleakalā, a dormant volcano within its boundaries, the park covers an area of 33,265 acres (52.0 sq mi; 134.6 km 2), [1] of which 24,719 acres (38.6 sq mi; 100.0 km 2) is a wilderness area. [3]
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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