Ngorongoro Crater is what geologists call an unbroken, inactive volcanic caldera — meaning that unlike
most large craters, it was never breached or filled by a lake, and the bowl shape remains essentially
complete. It formed approximately 2 to 3 million years ago when a large volcano, estimated to have once
stood as tall as Kilimanjaro, erupted and then collapsed in on itself, leaving behind the vast natural
amphitheater visible today.
The numbers alone explain why the crater feels so unlike anywhere else in Tanzania. The caldera measures
roughly 19 kilometres across and encloses 260 km² of crater floor,
walled in by slopes rising 400 to 610 metres from floor to rim. The rim itself sits at
2,200 to 2,400 metres above sea level — high enough that mornings on the crater edge are
genuinely cold, while the floor below warms quickly once the sun clears the walls.
The same eruption that created Ngorongoro also formed several smaller volcanic features nearby, including
the Olmoti and Empakaai craters, and contributed to the fertile plains of Ndutu and the
southern Serengeti — the same ground where the wildebeest migration's calving season takes place each
year. The Ngorongoro Crater itself was originally part of Serengeti National Park when the park was first
established by the British in 1951; it was separated into its own protected area, the Ngorongoro
Conservation Area, in 1959, specifically to secure land rights for the Maasai pastoralist communities who
live within its boundaries.
Today the Ngorongoro
Conservation Area is unique among Tanzania's protected areas for one further reason: it is the only place in
the country where wildlife, livestock, and human communities coexist within the same protected boundary. The
Maasai retain grazing rights across much of the 8,300 km² conservation area — though grazing inside the
crater itself was restricted in 2015 — making this one of the only landscapes on earth where pastoralist
cattle and wild lion prides share the same open ground.