Which topographical outcome results when glacial isostatic rebound is slower than coastal sediment flow?

💡 Explanation

Net marine terrasse formation results because the rate of isostatic adjustment cannot keep up with the depositional rate of sediment flow; therefore, a new bench of land and sediment is deposited rather than an uplifting shoreline or deep-sea erosion patterns.

• Which risk increases when pyroclastic flows deposit substantial tephra?
• Which outcome occurs when a subducting plate becomes increasingly hydrated?
• Which geological change results when thermal convection weathers a subducting oceanic plate?
• Which atmospheric outcome is intensified because of Earth's rotation?
• Which condition causes the formation of lobate features in solifluction areas with coarse boulder obstructions?
• Which risk increases when sediment supply halts offshore breakwaters?