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Dynamic equilibrium
Balance between tectonic uplift and reduction by weathering/erosion.
Angle of repose
The steepest stable slope angle for loose material (~35° for sand, ~45° for gravel).
Regolith
Weathered rock material covering bedrock.
Mudflows
Mass movement with moisture.
Rockfalls
Mass movement without moisture.
Karst topography
Landscape from dissolution of limestone (≥80% CaCO₃), forming sinkholes, caves, disappearing streams.
Continental divides
High terrain separating drainage to different oceans.
Erosion vs. deposition
Erosion removes material; deposition drops it.
Water velocity significance
Higher velocity increases transport capacity and particle size moved.
Point bar
Depositional feature on inside bend of meander.
Cut bank
Erosional feature on outside bend of meander.
Oxbow lake
U-shaped lake from cutoff meander.
Base level
Lowest erosion level (usually sea level).
Eolian landscape
Shaped by wind (erosion, transport, deposition).
Abrasion vs. deflation
Abrasion = sandblasting; deflation = lifting/removing loose particles.
Loess
Wind-blown silt deposits from glacial outwash (e.g., Midwest, China).
Desertification
Fertile land becomes desert due to drought, deforestation, poor agriculture.
Sand dune types
Crescent (1 wind direction), linear (2 directions), star (>2 directions).
Glacier
Persistent ice mass moving under its own weight.
Alpine vs. continental glaciers
Alpine in mountains; continental cover large areas (Greenland = continental).
Depositional landforms
Lateral moraine (sides), medial moraine (middle), terminal moraine (end).
Permafrost
Ground frozen ≥2 years.
Weathering
Breaks down rock in place.
Physical weathering
Breaks rock without chemical change.
Chemical weathering
Alters rock composition.
Drainage patterns
Dendritic: tree-like; Trellis: parallel with right-angle tributaries; Radial: outward from central high point.
How glaciers form
Glaciers form where snow accumulation exceeds ablation (melting/evaporation) over years.