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Ngorongoro crater lies within the Tanzania highlands. The Ngoronngoro Conservation forms an ecosystem often known as the Serengeti-Ngorongoro-Maasai Mara, interlocked on the east by the well known Rift Valley and to the west by Serengeti National Park. Though the scenery of Ngorongoro Conservation Area was formed several million years ago, it up till now undergoes modern geological processes.

The gneiss, granite outcrops as well as the Ol Doinyo Mountains dotted Serengeti plains a couple of years ago. 20 million years ago, the eastern side of Africa started to rift or fault resulting in the terrain around the fault lines to disappear. The land around this region became weak because of the slow thinning as well as softening of the earth's crust. The molten substances inside the earth were effortlessly thrust to the surface to create lava plateaus and volcanoes. Some of the most ancient volcanoes formed are Lemagrut, Oldeani, Ngorongoro, Olmoti, Sirua, Lolmasin, Sadiman, and Empakaai. All these volcanoes now form the high cliffs at lake Eyasi. Ngorongoro is considered to have been higher compared with Kilimanjaro, the highest mountain in Africa. It can be noted that, its height was reduced as a consequence of block subsidence where the lava that formed a strong lid eventually collapsed leaving behind an extensive crater, the caldera we see today. Volcanoes that underwent like processes as Ngorongoro include Emrpakaai and Olmati but the calderas failed to form as immensely as that of Ngorongoro. There are two fairly recent volcanoes in the region, Ol Doinyo Lanai and Kerimasi. The pair were formed along the Gregory Rift and lie to the northeast of Empakaai caldera. The Ol Doinyo Lengai Mountain, that is Maasai for Mountain of God, is still active and most recently erupted in 1983. The molten rock derived from volcanoes has two primary advantages: increasing fertility of soils for crop production outside Ngorongoro Conservation Area as well as sustenance of savanna grasslands which support the largest sized herds in the world. It does possess another benefit,- though invaluable - the retention of fossils that archaeologists and paleontologists cultivate a better comprehension of the origin of mankind as well as other creatures that inhabited the part of the earth especially around Olduvai Gorge and Aetolia. Through erosion and deposition the terrain of Ngorongoro Conservation area continues to be gradually modified although a great deal of of it was formed about two million years in past.

A Ngorongoro safari offers guests an exceptional glimpse into this natural spectacle which has maintained its origins for a million plus years.

A full day Ngorongoro crater tour begins as early as six in the morning and normally lasts the entire day with picnic lunch taken on the bottom of the crater.


Taking a tour or safari in the caldera which is known as Ngorongoro crater is an experience to behold for a visitor on a Tanzanian safari. Ngorongoro has remained a world class attraction in this part of the world teeming with abundant wildlife and scenery to behold.


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