Final answer:
Desert pavements are aeolian landforms characterized by wind-eroded surfaces, such as the Baja desert and Tassili n'Ajjer in Algeria. These geological structures are also found on other planets, with yardangs on Mars being an example. They are formed by wind deposition and erosion, leading to unique sediment patterns and landscape formations.
Step-by-step explanation:
An example of a desert pavement, also known as an aeolian landform, includes the landscapes found in the Baja desert. Another renowned example is the Tassili n'Ajjer in Southeast Algeria, which showcases impressive erosional features. Sediment patterns deposited by the wind create distinct landforms, such as well-sorted, often reddish sand in deserts and coastal regions.
Wind erosion is not exclusive to Earth; it is also observed on other planets like Mars, where images from the Mars Reconnaissance Orbiter have shown yardangs, straight ridges formed by the consistent wind direction on the Martian surface. These aeolian processes create various structures, such as cross-bedding and the sculpting of plains, which are observed on both Earth and Mars. These phenomena demonstrate the impact of wind as a significant geological force shaping the surface features of planets.