Deserts cover huge areas, mostly between 10-30 degrees N and S of the equator. Many of these deserts are sandy, at least partly. Good example is the Sahara – largest desert in the world. Ok, maybe it is second largest after Antarctica. To describe a desert sand, we first have to make clear what we are talking about. When we imagine desert sand, we probably think of sand dunes. That’s what I am writing about here although dune fields cover only about 20 percent of modern desert areas.
A dune sand is generally very well sorted. It means that all the sand grains are roughly the same size. There is almost no dust. It is blown away and deposited elsewhere, possibly as a loess deposit far away from the source area. There are also no gravel or boulders because wind is not capable of carrying such a heavy load. Another characteristic feature of a dune sand is the “frosted” or scratched surfaces of sand grains. This is the result of countless collisions between windblown sand grains.
There are approximately one square centimeter of sand on every photo.
Desert sand composed almost exclusively of rounded quartz grains. Sand sample is from the Sahara Desert (Erg Murzuk), Libya
Rounded quartz grains (covered with rust-colored hematitic pigment) plus biogenic and lithic fragments from the Dubai Desert, United Arab Emirates. Biogenic grains clearly indicate that the sea can't be very far away.
Dune sand from the Gobi Desert, Mongolia.
