Page 329 has a map showing the sabkha and the two settlements.

The climate variations lead to the very dynamic nature of a sabkha.

Other dry lake types include the sabkha and the mudflat.

There is an airport in Mécheria; and a big sabkha.

This is the beginning of sabkha development.

The halophytic sabkha type desert vegetation is predominant in Muscat.

At Taghaza there are ruins of two different settlements, one on either side of the ancient salt lake (or sabkha).

Much of the area is soft sand covered with "sabkha" - a brittle crust consisting mostly of salt.

Pisolitic grainstones are best developed in the upper part of the Hauptdolomit where sabkha environments predominated.

East of the city, the salt-crusted coastal plains, known as sabkha, give way to a north-south running line of dunes.

Finally, a drop in sea level (regression) exposed the entire platform, and became a broad, nearly featureless, hot, semi-arid sabkha.

Other outdoor habitats designed that are yet to be constructed include wadi, sabkha, central fog desert and sand desert.

Sabkha deposits are believed to form some of the major subsurface hydrocarbon reservoirs in the Middle East (and elsewhere).

Murshid Bazaar in Al Sabkha is well known in the area for textiles and electronics.

It is the closest station to the neighbourhood of Naif and the eastern section of Al Sabkha.

The origin and progression of sabkha development in the Persian Gulf is discussed by Al-Farraj (2005).

(A sabkha is a wide area of coastal flats bordering the sea, the name coming from certain coastal areas of Arabia).

Electrical goods at bargain prices are found on Baniyas Square on the Al Sabkha road.

The reason for this was probably that the sediments were deposited largely under sabkha conditions and therefore were particularly prone to exposure and freshwater flushing.

Next to Unaizah is the Al-Aushaziyah salt lake (or Sabkha), which is considered an official part of the city.

The reasons for this are that the sabkha surface is not a free-water surface, the high humidity during the night, and vertical stratification of the air column.

Factors enabling preservation include the progradation of the sabkha with sedimentation rates of 1 m/1000 years and the creation of Stokes surfaces.

These surfaces are created by the deflation of the sabkha surface that is related to the level of the groundwater table acting as a local base level.

In drier parts of the sabkha the gypsum can be altered to anhydrite and the aragonite can be dolomitized diagenetically.

In Arabic, an alkali flat is called a sabkha (also spelled sabkhah, subkha or sebkha) or shott (chott).