The provided image shows a close-up view of an expanse of reddish-brown desert sand, with numerous white-to-gray-colored crystalline features scattered across its surface.
A closer inspection reveals that these crystalline features are formed by gypsum crystals (selenite) that have been deposited on the desert floor. The selenite is arranged in a series of small, jagged formations resembling pavement blocks and appears to be growing out from within the sand.
The image does not appear to show any signs of erosion or damage to these crystalline features. It seems likely that this area has been undisturbed for an extended period of time and therefore offers a unique opportunity for scientists to study the formation process of selenite in its natural state. – AI vision
Similar(1): Gypsum crystals pavement (selenite) in area of Jebel Al-Nakhsh in south-western Qatar, April 2, 2016
Similar(2): Polycarpaea repens on gypsum pavement (selenite) in area of Jebel Al-Nakhsh in south-western Qatar, February 7, 2014
Similar(3): Slabs of gypsum crystals (selenite) in area of Jebel Al-Nakhsh in south-western Qatar, February 7, 2014
Similar(4): Layers of gypsum crystals (selenite) in area of Jebel Al-Nakhsh in south-western Qatar, February 7, 2014
Similar(5): White gypsum crystals (selenite) in area of Jebel Al-Nakhsh in south-western Qatar, February 7, 2014
Similar(6): Slab of gypsum crystals (selenite) in area of Jebel Al-Nakhsh in south-western Qatar, February 7, 2014
Similar(7): Patterns of gypsum crystals (selenite) in area of Jebel Al-Nakhsh in south-western Qatar, February 7, 2014
Similar(8): Slabs of gypsum crystals (selenite) with sand in area of Jebel Al-Nakhsh in south-western Qatar, February 7, 2014