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Physical Process

Playa Formation

Geomorphology

The development of a flat, sediment-floored basin at the lowest point of an arid, closed drainage system, formed as intermittent runoff collects in the basin and evaporates entirely, leaving behind a smooth surface of fine mud and, where groundwater has carried them in, evaporite salts. A playa can remain dry for years between rare flooding events, and where salt content is high enough it can form a hard, crusted salt flat such as Bolivia's Salar de Uyuni.

Facts
Process Type
Geomorphological 1
Connections

Associated With

Playa, Landforms

Caused By

Sources
1. Playa Formation (Wikipedia)
Wikimedia FoundationIntroduction
Quote, Introduction
A dry lake bed, also called a playa, is a basin or depression that formerly contained a standing surface water body, which disappears when evaporation processes exceed recharge.
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