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The Ngorongoro volcano was active from about 2.45 to 2 million years ago. [12] Volcanic eruptions like that of Ngorongoro, which resulted in the formation of Ngorongoro Crater in Tanzania, were very common. Similar collapses occurred in the case of Olmoti and Empakaai, but they were much smaller in magnitude and impact. [citation needed]
The district is home to the Ngorongoro Conservation Area which is a UNESCO World Heritage Site. The district is also home to the third tallest mountain in the country, Mount Loolmalasin. According to the 2002 Tanzania National Census, the population of the Ngorongoro Region was 129,776. [3] By 2012, the population of the district was 174,278. [4]
Topographical map of the Crater Highlands, looking from the north to the southwest. The Crater Highlands or Ngorongoro Volcanic Highlands (Milima kasoko ya Ngorongoro , in Swahili) are a geological region along the East African Rift in the Arusha Region and parts of northern Manyara Region in north Tanzania.
Below is an alphabetical list of plants occurring in the Ngorongoro Crater in Tanzania. Ngorongoro Crater covers an area of 265 square kilometres and is thought to have been formed from the collapse of a volcanic mountain which had become inactive. Its rim lies some 2280 meters above sea level, while the floor is at 1800 meters.
The monument project was funded by the Stone Age Institute and the John Templeton Foundation, in partnership with the Ngorongoro Conservation Area Authority (NCAA). [ 16 ] The Olduvai Gorge Museum , located 5 km beyond the monument, is situated on the rim of the gorge at the junction of the main gorge and the side gorge.
The Empakaai Crater or Embagai (Kasoko la Empakai in Swahili, also Ela Nairobi) is a collapsed volcanic caldera located in Naiyobi ward of Ngorongoro District in Arusha Region of Tanzania. It is 300 meters high and 6 kilometers wide.
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