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Foehn winds are warm, dry winds that descend leeward slopes of mountains, caused by adiabatic heating as moist air rises and loses moisture.Foehn wind illustration.
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Tilers installing large format tiles on wall.
Dimmuborgir large area of unusually shaped lava fields east of Mývatn in Iceland.
Round formations of salt crystals. The Dead Sea in the Middle East. Picturesque result of salt crystallization. The famous sea on hot day. Israel.

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