Geology and Landforms: Key Concepts for Earth Science

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27 Terms

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Dynamic equilibrium

Balance between tectonic uplift and reduction by weathering/erosion.

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Angle of repose

The steepest stable slope angle for loose material (~35° for sand, ~45° for gravel).

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Regolith

Weathered rock material covering bedrock.

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Mudflows

Mass movement with moisture.

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Rockfalls

Mass movement without moisture.

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Karst topography

Landscape from dissolution of limestone (≥80% CaCO₃), forming sinkholes, caves, disappearing streams.

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Continental divides

High terrain separating drainage to different oceans.

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Erosion vs. deposition

Erosion removes material; deposition drops it.

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Water velocity significance

Higher velocity increases transport capacity and particle size moved.

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Point bar

Depositional feature on inside bend of meander.

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Cut bank

Erosional feature on outside bend of meander.

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Oxbow lake

U-shaped lake from cutoff meander.

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Base level

Lowest erosion level (usually sea level).

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Eolian landscape

Shaped by wind (erosion, transport, deposition).

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Abrasion vs. deflation

Abrasion = sandblasting; deflation = lifting/removing loose particles.

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Loess

Wind-blown silt deposits from glacial outwash (e.g., Midwest, China).

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Desertification

Fertile land becomes desert due to drought, deforestation, poor agriculture.

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Sand dune types

Crescent (1 wind direction), linear (2 directions), star (>2 directions).

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Glacier

Persistent ice mass moving under its own weight.

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Alpine vs. continental glaciers

Alpine in mountains; continental cover large areas (Greenland = continental).

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Depositional landforms

Lateral moraine (sides), medial moraine (middle), terminal moraine (end).

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Permafrost

Ground frozen ≥2 years.

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Weathering

Breaks down rock in place.

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Physical weathering

Breaks rock without chemical change.

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Chemical weathering

Alters rock composition.

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Drainage patterns

Dendritic: tree-like; Trellis: parallel with right-angle tributaries; Radial: outward from central high point.

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How glaciers form

Glaciers form where snow accumulation exceeds ablation (melting/evaporation) over years.