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Trou au Natron

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City
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Trou au Natron (Chad)
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Practical info — Trou au Natron

🌤 Weather — 5 days

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Travelers embarking on deep Saharan expeditions visit the Trou au Natron for its otherworldly volcanic geology. This colossal caldera plunges nearly 1,000 meters down from its rim, spanning 8 kilometers in diameter. The crater floor is striking due to its thick crust of white natron salt, which starkly contrasts with the dark, jagged volcanic rock of the walls. The challenging descent into the crater is a focal point for extreme trekkers. The salt crust on the bottom provides essential minerals for wild animals and local camel herds that are occasionally guided down the steep paths by Toubou herdsmen. A few smaller volcanic cones rise dramatically from the white crater floor, indicating past explosive activity. Located near the Pic Toussidé volcano, getting here involves an arduous multi-day off-road journey from N'Djamena. Specialized expedition gear, ample water, and local Toubou guides are essential for survival and navigation. The expedition window is restricted to the winter months of November through February to avoid lethal summer temperatures.

Best time to visit & climate

The most pleasant time to visit is Feb, Mar, Nov.

JanFebMarAprMayJunJulAugSepOctNovDec
Avg °C151822262931313029252016
Rain mm0000222123000

Geography

Coordinates
20.97500, 16.56750

Facts

  • Measures 8 kilometers in diameter
  • Plunges almost 1,000 meters deep
  • Floor is covered in sodium carbonate
  • Located near the Pic Toussidé volcano
  • Part of the Tibesti volcanic group
  • Salt is utilized by local camel herds
  • Features small cinder cones inside
  • Formed by a massive volcanic collapse

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Frequently asked questions

Trou au Natron: where is it located?
Trou au Natron is located in Chad.
Trou au Natron: when is the best time to visit?
The most pleasant time to visit is Feb, Mar, Nov.
Trou au Natron: why is it worth visiting?
Travelers embarking on deep Saharan expeditions visit the Trou au Natron for its otherworldly volcanic geology.
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