Which mechanism creates mid-latitude stream meanders in glacial landscapes?

💡 Explanation

When glaciers recede, isostatic rebound occurs because the land adjusts upward due to reduced ice weight, changing the stream gradient and altering flow patterns, initiating meandering. Therefore isostatic rebound causes meanders, rather than freeze-thaw, cryoturbation, or orographic precipitation which have different geological preconditions.

• Which mechanism influences stream course alignment in areas bisected by a transform fault?
• Which effect causes increased coastal erosion when vegetation is removed by storms or development?
• Which outcome results when a meander erodes through its neck during enhanced streamflow?
• Which topographic outcome results when aeolian deflation dominates?
• Which outcome occurs when freshwater influx disrupts circulation?
• Which erosion outcome primarily results when exposed granite undergoes chemical alteration?