Most deserts have highly angular landscapes due to mechanical weathering dominating over deposition. Desert rainfall is infrequent, intense, and unreliable, causing flash flooding and erosion. The three main types of deserts are ergs, which are large seas of sand; regs with thin desert pavements of stones; and hamadas dominated by bedrock. In deserts, fluvial erosion carves steep canyons, while deposition forms alluvial fans. Aeolian processes cause erosion through deflation and abrasion, and deposition forms migrating dunes like barchans and transverse dunes. Desert terrain also includes basin and range topography with pediments and playas, and resistant rock landforms emerge like insel