Salt flat
Natural salt flats or salt pans are flat, open expanses of ground covered with salt and other minerals, usually shining white under the sun. They are found in deserts and are natural formations.
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Crystalline white like a salt flat after evaporation.
#eef3e5
Saltpan is a white.
It can be described as pale, delicate, faded and almost grey.
Set in black, because black reads best on it.
Saltpan
Sabkha
A sabkha is a predominantly coastal, supratidal mudflat or sandflat in which evaporite-saline minerals accumulate as the result of a semiarid to arid climate. Sabkhas are gradational between land and intertidal zone within restricted coastal plains just above normal high-tide level. Within a sabkha, evaporite-saline mineral sediments typically accumulate below the surface of mudflats or sandflats. Evaporite-saline minerals, tidal-flood, and aeolian deposits characterize many sabkhas found along modern coastlines. The accepted type locality for a sabkha is at the southern coast of the Persian Gulf, in the United Arab Emirates. Evidence of clastic sabkhas are found in the geological record of many areas, including the UK and Ireland. Sabkha is a phonetic transliteration of the Arabic root s b ḵ used when talking about any form of salt flat, including salt marshes and salt swamps. A sabkha is also known as a sabkhah, sebkha, or coastal sabkha.
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Noun
- Alternative spelling of salt pan.
Its neighbors.
Fresh Dew, #f0f4e5Hushed White, #f1f2e4Frostwork, #eff1e3Verde Pastel, #edf5e7Glacier Ivy, #eaf3e6Aspen Whisper, #edf1e3Storksbill White, #f2f2e2Quiet Whisper, #f1f3e8Belyi White, #f0f1e1Shattered White, #f1f1e5White Mecca, #ecf3e1Aloe Essence, #ecf1e2