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.

• Over-extraction from urban aquifers in karst increases which risk?
• Which effect accompanies stratovolcano formation where subducting oceanic crust hydrates the mantle wedge?
• Which consequence results when extensive chemical weathering occurs in soils?
• Which mechanism causes the intertropical convergence zone (ITCZ) shift seasonally?
• Which atmospheric phenomenon is intensified near coastlines undergoing strong differential heating?
• Which environmental transformation results when groundwater saturation exceeds cave sediment's infiltration capacity?