Upon sea stack collapse, which factor most retards longshore sediment redistribution?

💡 Explanation

High sediment cohesion inhibits redistribution because internal friction resists dispersal by waves and currents, rather than wind or waves slowing erosion. Strong cohesion maintains stack-derived sediment close to the source, therefore preserving localized deposits rather than causing widespread distribution.

• Which outcome occurs when a warming climate thaws discontinuous permafrost beneath an Arctic oil pipeline?
• Which risk dramatically increases when diverting surface runoff toward karst regions?
• Which process regulates salinity in closed-basin lakes under high evaporation rates when inflow halts?
• Which consequence results when persistent high-pressure systems strengthen subtropical gyres?
• Which outcome is promoted at strike-slip faults crossing shallow geothermal reservoirs?
• Which landform develops extensively because seasonal thawing destabilizes slopes?