A desert pavement, also called reg (in the western Sahara), serir (eastern Sahara), Gibber (in Australia), or saï (central Asia) is a desert surface covered with closely packed, interlocking angular or rounded rock fragments of pebble and cobble size. They typically top alluvial fans. A vesicular, A soil horizon (Av) forms beneath the surface layer. Desert varnish collects on the exposed surface rocks over time.
Scholars debate the mechanics of pavement formation and their age.
Several theories have been proposed for the formation of desert pavements. A common theory suggests they form through the gradual removal of sand, dust and other fine grained material by the wind and intermittent rain leaving the larger fragments behind. The larger fragments are then shaken into place through rain beat, running water, wind, wind, gravity, creep, thermal expansion and contraction, wetting and drying, frost heaving, animal traffic, and the Earth's constant microseismic vibrations. The removal of small particles by wind does not continue indefinitely, because once the pavement forms it acts as a barrier to further erosion. The small particles collect underneath the pavement surface, forming an Av soil horizon.
A second theory supposes that desert pavements form from the shrink/swell properties of the clay underneath the pavement; when precipitation is absorbed by clay it causes it to expand ,and when it dries it cracks along planes of weakness. Over time, this geomorphic action transports small pebbles to the surface, where they stay through lack of precipitation that would otherwise destroy the pavement by transport of the clasts or excessive vegetative growth.
A newer theory of pavement formation comes from careful studies of places like Cima Dome, in the Mojave Desert of California, by Stephen Wells and his coworkers. Cima Dome is a place where geologically recent lava flows are covered by younger soil layers with desert pavement on top of them, made of rubble from the same lava. The soil has been built up, not blown away, yet the stones remain on top. There are no stones in the soil, not even gravel.
There are ways to tell how many years a stone has been exposed on the ground. Wells used a method based on cosmogenic helium-3, which forms by cosmic ray bombardment at the ground surface. Helium-3 is retained inside grains of olivine and pyroxene in the lava flows, building up with exposure time. The helium-3 dates show that the lava stones in the desert pavement at Cima Dome have all been at the surface the same amount of time as the solid lava flows right next to them. It's inescapable that in some places, as he put it in a July 1995 article in Geology, "stone pavements are born at the surface." While the stones remain on the surface due to heave, deposition of windblown dust must build up the soil beneath that pavement.
For the geologist, this discovery means that some desert pavements preserve a long history of dust deposition beneath them. The dust is a record of ancient climate, just as it is on the deep sea floor and in the world's ice caps.
Desert pavement surfaces are often coated with desert varnish which is a dark brown, sometimes shiny coating that contains clay minerals. In the USA a famous example can be found on Newspaper Rock in Canyonlands, Utah. Desert varnish is a thin coating (patina) of manganese, iron and clays on the surface of sun-baked boulders. It is formed by colonies of bacteria living on the rock surface for thousands of years. Desert varnish is also prevalent in the Mojave desert and Great Basin geomorphic province.
Stony deserts may be known by different names according to the region. A few examples are:
Covering extensive areas in Australia such as parts of the Tirari-Sturt stony desert ecoregion desert pavements are called Gibber Plains after the pebbles or gibbers, and so Gibber is also used in describing ecological communities such as Gibber Chenopod Shrublands or Gibber Transition Shrublands.
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