After prolonged drought, which topographical consequence develops because of aeolian deflation?

💡 Explanation

Lag deposits form because wind deflation winnows away fine particles, leaving behind larger rocks and gravel; this forms desert pavement. The result is surface armouring, therefore protecting the underlying sediment rather than processes affecting shifting dunes, stabilization or yardang formation.

• Which effect results when seasonal shifts modify jet stream position relative to a mountain range?
• Which long-term outcome arises when intense chemical weathering of basalt releases soluble cations in tropical lateritic systems?
• Which consequence occurs due to increased tropical convection?
• Which condition causes the formation of lobate features in solifluction areas with coarse boulder obstructions?
• Which mechanism maintains relatively stable ocean surface temperatures globally due to latitudinal variations?
• Which increased risk follows loess deposit exposure to increased saturation?