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Ol Doinyo Lengai, in northern Tanzania, erupts the coldest and runniest lava on Earth. It comes out black, and within hours or days it turns white as snow.

The short answer
Almost every volcano erupts molten silicate rock. Ol Doinyo Lengai erupts a carbonate melt called natrocarbonatite, and no other volcano is known to have done so in historical times.
Black, then white

During the eruption
The lava pours out dark and glistening. It glows only faintly, dull orange or red, and only at night.
Hours to days later
Its minerals absorb water from the air and react, turning the surface white. In rain, this can happen before the flow has even cooled.
Within a few months
The white crust keeps weathering and breaks down into a soft brownish powder.
The coldest lava on Earth
Ordinary lava is so hot it shines yellow and orange in daylight. Lengai's lava is roughly 600 °C cooler, so it looks like flowing mud. It is also the least viscous lava known, and can run at 1 to 5 metres per second.
Eruption temperatures, from the U.S. Geological Survey.

What it is made of
Natrocarbonatite is a carbonate lava rich in sodium and potassium. Those carbonates melt at far lower temperatures than silicate rock, which is why the lava is so cool and so runny, and why it reacts so quickly with water.
Molten silicate rock, around 1,000 °C or more. Cools into dark basalt or andesite that stays dark.
Molten sodium and potassium carbonates, around 550 °C. Erupts black and weathers to white.

From the air
The volcano sits less than 3° south of the Equator, where it never snows at this height. The white crater floor and the streaks running down its slopes are old lava flows that have changed colour.
Where on Earth
Ol Doinyo Lengai rises from the Gregory Rift, the eastern branch of the great crack where Africa is slowly pulling apart. Lake Natron lies 16 km to the north.


Its neighbour
Lake Natron is shallow, hot and so alkaline that few animals can live in it. Salt-loving microorganisms colour its water red, and its salt flats are the nursery of East Africa's flamingos.
An active volcano
The first recorded eruptions. Activity is noted many times through the twentieth century.
A long phase of activity begins, with lava flows filling the summit crater on and off for decades.
A lava flow spills onto the western flank.
A large explosive eruption begins. Its ash column rises about 3 km, a new crater forms and three villages are evacuated.
Lava begins to flow again in the new crater.
Seismometers and GPS stations monitor the volcano.
Quick answers
Its lava is natrocarbonatite, made of sodium and potassium carbonates. It erupts black or dark brown, then absorbs water from the air and reacts chemically, turning white within hours to days.
The natrocarbonatite of Ol Doinyo Lengai in Tanzania, which erupts at about 540–593 °C. Typical basalt lava, like Kīlauea's, erupts at around 1,160 °C.
No. The volcano lies less than 3° south of the Equator. The white on its summit and slopes is weathered lava.
In the Arusha Region of northern Tanzania, in the East African Rift, about 16 km south of Lake Natron and 120 km northwest of Arusha.
The short version