This topic examines the variations in glacial processes, landforms, and landscapes over different time scales, focusing on short-term events, seasonal chan
Topic Synopsis
This topic examines the variations in glacial processes, landforms, and landscapes over different time scales, focusing on short-term events, seasonal changes, and long-term post-glacial modifications.
Key Concepts & Core Principles
- Glacial mass balance: the difference between accumulation (snowfall) and ablation (melting, calving) over a year, determining whether a glacier advances or retreats.
- Milankovitch cycles: orbital variations (eccentricity, obliquity, precession) that drive long-term climate changes, leading to glacial-interglacial cycles.
- Glacial erosion processes: abrasion and plucking, which create landforms like striations, roches moutonnées, and U-shaped valleys over thousands of years.
- Depositional landforms: moraines (terminal, lateral, medial), drumlins, and erratics, which form during glacial retreat and advance phases.
- Periglacial processes: freeze-thaw weathering and permafrost formation, which occur in areas adjacent to glaciers and vary with climate shifts.
Examiner Marking Points
- Process and landform changes in seconds: rapid mass movement processes causing changes in glacial valley profiles
- Seasonal process and landform changes: landform changes associated with seasonal variations in fluvioglacial transport and deposition
- Process and landform and landscape changes over millennia: post-glacial reworking of glacial deposits, infilling of glacial lakes, and creation of misfit streams by fluvial processes