Which outcome increases when wind velocity increases near a source of loess?

💡 Explanation

Increased wind velocity leads to greater Aeolian transport capacity, enhancing loess deposition far from the source because increased shear stress entrains more particles, increasing downwind sedimentation, therefore long-range deposition increases, rather than changes limited to creep.

• Which outcome occurs when airborne tephra accumulates beyond capacity?
• Near subduction plate boundaries, which risk increases when fault locking intensifies?
• Which outcome results when earthworm limitations suppress bioturbation?
• Which risk increases when a large earthquake ruptures across a natural levee along a major river?
• Which outcome increases due to decreasing stream competence in alluvial fans?
• Which process shapes isolated sea stacks during high wave surges?