Ngorongoro crater lies within the Tanzania highlands. The Ngoronngoro Conservation forms an environment often known as the Serengeti-Ngorongoro-Maasai Mara, interlocked on the east by the famous Rift Valley and to the west by Serengeti National Park. Although the terrain of Ngorongoro Conservation Zone was formed several million years ago, it continually undergoes modern day geological processes.

The gneiss, granite outcrops as well as the Ol Doinyo Mountains dotted Serengeti plains several hundred years ago. 20 million years back, the eastern side of Africa started to rift or fault allowing the area around the fault lines to subside. The land around this zone eventually became weak due to the slow thinning and softening of the earth's covering. The molten substances inside the earth were easily thrust to the surface to create lava plateaus as well as volcanoes. Some of the most ancient volcanoes formed are Lemagrut, Oldeani, Ngorongoro, Olmoti, Sirua, Lolmasin, Sadiman, and Empakaai. Each of these volcanoes now form the high cliffs at lake Eyasi. Ngorongoro is considered to have been higher compared to Kilimanjaro, the highest mountain in Africa. It can be noted that, its altitude was reduced due to block subsidence where the lava that formed a rigid lid slowly and gradually collapsed leaving behind an enlarged crater, the caldera we see today. Volcanoes that underwent common processes as Ngorongoro consist of Emrpakaai and Olmati but the calderas did not actually form as immensely as that of Ngorongoro. The two newly born volcanoes in the region, Ol Doinyo Lanai and Kerimasi. They 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, remains to be active and most recently erupted in 1983. The molten rock derived from volcanoes has two core advantages: improving fertility of soils for crop production outside Ngorongoro Conservation Area as well as sustenance of savanna grasslands which support the largest herds in the world. It does possess an additional benefit,- though invaluable - the retention of fossils that archaeologists and paleontologists cultivate a much better comprehension of the origin of mankind and other creatures that inhabited the part of the globe primarily around Olduvai Gorge and Aetolia. Through erosion and deposition the landscape of Ngorongoro Conservation area continues to be gradually modified despite the fact that a great deal of of it was formed about two million years in past.

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

A full day Ngorongoro crater tour starts off as early as six in the morning and will last the entire day with picnic lunch break taken on the base of the crater.

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