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 mechanism generates tsunamis after significant seafloor displacement?
• Which mechanism amplifies the Coriolis effect experienced by air masses moving toward high-latitude regions?
• Which outcome occurs when persistent abrasive winds sculpt desert rocks?
• Which outcome occurs when intense tropical weathering increases soil acidity?
• Which ionic depletion slows stalactite formation in caves?
• Which formation process dominates when wave-cut platforms erode isolated headlands?