Which consequence results when bedrock compression reduces post-glacial rebound near fjords?

💡 Explanation

Enhanced salt water intrusion worsens where bedrock compression slows *isostatic rebound* near fjords, because formerly compressed bedrock rebounds slowly, therefore increasing coastal submergence and allowing prolonged intrusion, rather than creating uplift that would limit intrusion.

• Which risk increases when construction impends on an alluvial fan's active zone?
• Which outcome occurs when increased feldspar weathering affects pedogenesis?
• Which mechanism governs the formation of deep water masses critical for thermohaline circulation?
• Around braided rivers, which risk increases along alluvial fans due to avulsion events?
• Which outcome occurs when sustained unidirectional wind abrasion shapes desert pavement?
• Which risk increases when coastal engineers use impermeable groynes?