Near the shore, the water acquires an orange tint, because. The water in the lake has a red color, this feature is caused by the activity of microorganisms. So, he erupted in October 2008, and a couple of years later woke up again. Obvious manifestations of seismic activity relatively recently showed the nearby volcano Oldonyo Lengai. Natron is an integral part of today's most active volcanic system, the African Great Rift. Since the air temperature in this area often crosses the 50 ° C mark, the water in Natron also warms up to similar values. The area, on the contrary, is rather big - 1344 km2. The depth of Lake Natron is quite small, because in some places it does not even reach 3 meters. The water temperature in the wetlands can reach 50 degrees Celsius, and depending on the water level, the alkalinity can reach a pH of 9 to 10.5. A seasonal downpour passes over the lake in May-December and brings 800 mm of precipitation. The lake maximum reaches 57 km in length and 22 km in width. The lake has a depth of no more than three meters and changes the coastline depending on the season and water level.

Natron is mainly fed by the Ewaso Ngiro River, which originates in a mineral-rich area in Northern Kenya.

The basin of Lake Natron is protected by the international Ramsar Convention. The lake is located in the Gregory Rift, which is the eastern part of the East African Rift. Natron is a salty and alkaline lake located in the Arusha region in northern Tanzania, on the border with Kenya.

Lake Natron phenomenon - beauty and horror wildlife Tanzania

Lake natron mummies