Which mechanism limits sediment deposition rate within a fjord undergoing isostatic rebound post-glaciation?

💡 Explanation

When isostatic rebound occurs, a fjord's bathymetry shallows, which increases tidal current velocities due to a reduction in cross-sectional area and thus channelization; this intensification of bottom currents scours the seabed, preventing substantial deposition on specific areas. Therefore, increased tidal current scouring limits sediment deposit, rather than alterations from sediment, plant systems, or landslides, each requiring different conditions.

• Which topographic consequence results from the subduction of an oceanic plate beneath a continental plate lacking sufficient sediment?
• Which phenomenon causes the formation of patterned ground in Arctic regions underlain by permafrost?
• Which mechanism amplifies temperature gradients at mid-latitudes when polar Hadley cell boundaries shift equatorward?
• Which risk increases when thawing permafrost destabilizes coastal cliffs near settlements?
• Which mechanism explains why major river systems in the Northern Hemisphere deflect to the right?
• Which risk increases as floodplain development restricts space allowing for proper river levee maintenance and inspection?