Which spatial outcome results when desert vegetation stabilizes parabolic dune arms?

💡 Explanation

Deflation hollow formation decreases because vegetation anchoring increases surface cohesion, reducing wind erosion; therefore, hollow development slows noticeably, rather than intensifying ventifact abrasion or altering distant loess movements since surface deflation ceases within hollows.

• Which outcome is more likely when floodplain levees subside unevenly?
• Which mechanism accelerates weathering of andesitic volcanic ash deposits?
• Which risk increases when polar jet stream meandering amplifies?
• Which depositional pattern develops when a mountain stream abruptly enters a broad, dry valley?
• Which mechanism causes the formation of horst and graben structures within a continental rift zone?
• Which mechanism explains localized crustal uplift preceding major earthquakes near subduction zones?