Which process explains differences in fjord sill depth and isostatic rebound rates?

💡 Explanation

When glaciers advance, differential glacial erosion occurs, deepening fjord basins based on varying rock resistance and fault structures; areas with softer rocks erode faster affecting isostatic rebound. Therefore, erosion causes differences in fjord sill features, rather than tectonic shifts sediment budget or varying heat flux , which are secondary geological processes.

• Which process drives the formation of layered sedimentation within an alluvial terrace?
• Which mechanism primarily controls orientation, asymmetry, and shape of cirques on a mountain range?
• Which mechanism initiates the formation of rift valleys along divergent continental plate boundaries?
• Which mechanism sustains high sinuosity in meandering streams within humid continental regions?
• Which risk increases when degassing pathways become blocked within a volcanic dome?
• Which mechanism causes surface-level convergence of water in the center of ocean gyres?