AA&F: Bill Corner
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2017 - Ethiopia: Danakil Depression ·
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Danakil Desert Sunset Askoma Camels Erte Ale Erte Ale Erte Ale
Erte Ale Erte Ale Erte Ale Lava Lava Erte Ale Salt pan
Dragon trees Danakil Desert Sunset Salt canyons Salt canyons Halite Salt canyons
Dallol Dallol Dallol Dallol Dallol Dallol Dallol
Dallol Dallol Dallol Dallol Dallol Dallol Dallol
Dallol Dallol Dallol Dallol Dallol Dallol Dallol
Dallol Dallol Dallol Dallol Sulphur spring Camels Salt mining
Salt mining Salt mining Salt mining Salt mining Camel train Camel train Camel train
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February 2017
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© Bill Corner
Image 1: Danakil Desert ;Image 2: Sunset at Askoma The camp at the base of Erte Ale volcano;Image 3: Askoma ;Image 4: Camels carrying our bedding We walked up Erte Ale after sunset to avoid the heat of the day and camped at the summit - these camels transported our bedding;Image 5: Erte Ale A basaltic shield volcano (613m) which has had an active lava lake since 1906;Image 6: Erte Ale We were lucky to see the volcano in a much more agitated state than normal;Image 7: Erte Ale Two days after we were there the volcano had a major eruption which opened a new vent further down the flanks of the volcano which depleted the lava lake at the summit;Image 8: Erte Ale We spent the night on the edge of the summit crater sleeping under the stars and walked down in the morning;Image 9: Erte Ale In the light of the dawn;Image 10: Erte Ale When the volcano was less active you could climb down into the crater and actually peer over the lip of small central crater into the lava lake;Image 11: Fresh ropey lava Called pahoehoe in Hawaii - where they also have (much larger!) basaltic volcanoes;Image 12: Basaltic lava ;Image 13: Erte Ale ;Image 14: Salt pan at Lake Afrera Vast amounts of salt is extracted from the pans around Lake Afrera. The altitude of the lake is -102m;Image 15: Dragon trees ;Image 16: Danakil Desert ;Image 17: Sunset over Lake Asale AKA Lake Karum. Altitude: -115m;Image 18: Salt canyons at Dallol The banding is due to successive layers of halite and silt. The halite is an evaporite while the silt is carried into the depression during floods;Image 19: Salt canyons at Dallol The halite is then eroded to form these columns and canyons;Image 20: Halite ;Image 21: Salt formations ;Image 22: Sulphur springs at Dallol ;Image 23: Sulphur pools Apparently the water is at pH1 - you may be surprised to learn I actually didn't stick my finger into test that…;Image 24: Sulphur vents ;Image 25: ;Image 26: Crystalline sulphur ;Image 27: ;Image 28: Our party at Dallol And here's the proof, if you need it, that I haven't photoshopped the colours!;Image 29: ;Image 30: ;Image 31: ;Image 32: Dried out sulphur pools ;Image 33: ;Image 34: ;Image 35: ;Image 36: ;Image 37: ;Image 38: ;Image 39: ;Image 40: ;Image 41: Sulphur crystals ;Image 42: ;Image 43: ;Image 44: ;Image 45: ;Image 46: ;Image 47: Bubbling sulphur pool Locals use this (cold) water for treating skin conditions - the water feels oily due to the dissolved sulphur - and cleaning silver jewellery;Image 48: Salt mining: Lake Asale Camels waiting to be loaded with salt from Lake Asale;Image 49: The diggers first lever up the salt crust… ;Image 50: Then the blocks are shaped into 5kg slabs… ;Image 51: The salt is then bundled up… ;Image 52: And loaded onto camels (and donkeys) for transportation ;Image 53: Then the camel trains transport the salt to the nearest town where it is sold on ;Image 54: The camel trains seemingly appear out of nowhere ;Image 55: ;Image 56: