Which geomorphic consequence primarily results when the depositional boundary moves downwind across landscapes?

💡 Explanation

Downwind movement leads to loess accumulation because aeolian **sediment transport** deposits silt far from the desert source, therefore widespread blankets develop, rather than increased lake evaporation due to localized inputs/outputs from ephemeral waterways.

• Which outcome occurs when earthquake rupture propagation reduces?
• Which outcome occurs when differential slip exceeds friction limits on strike-slip faults traversing sedimentary strata?
• Which process drives the formation of an arête between two cirques after glacial retreat?
• Which mineralogical change results when cave stalactites exposed to ventilation?
• Which mechanism causes the formation of freshwater lakes after glacial retreat?
• Which outcome is most likely when human barrier island development greatly impedes sediment transport?