Which consequence results when accelerated pedogenesis exceeds stabilization limits?

💡 Explanation

Surface subsidence results from exceeding soil stabilization limits because rapid pedogenesis can dissolve subsurface geological strata via carbonic dissolution, thereby causing voids. This outcome is more likely through dissolution rather than the other options, which are connected to different processes.

• Which outcome is most likely when accumulated tectonic stress exceeds the friction along a transform fault boundary?
• Which weathering outcome significantly slows blanket bog pedogenesis?
• Which risk increases when a large coastal levee system experiences prolonged saltwater intrusion?
• Increased silt deposition into tidal inlets increases what risk to barrier islands?
• Which risk increases when a region's groundwater table declines significantly due to elevated evaporative loss during longer summers?
• Near strike-slip boundaries, what hazard increases given elevated pore water pressure?