Which long-term outcome occurs when freeze-thaw cycles affect dolostone formations?

💡 Explanation

Freeze-thaw cycles promote mechanical weathering via ice wedging, which widens fractures; this enhances the dissolution of dolostone because water has increased surface area, thus accelerating karst development, rather than the other options which are less directly impacted.

• Which outcome develops when increased wave refraction focuses on islands?
• Which limit constrains the formation of extensive alluvial terraces in a rapidly uplifting mountain range?
• Which risk increases as coalescing alluvial fans block canyon outlets?
• Which mechanism promotes increased wave energy concentration as headlands erode into isolated stacks?
• Which seismic consequence results when repeating stress exceeds friction along an existing fault line?
• Which mechanism increases the lifespan of resilient sea stacks?