Geomorphology classifies the planet's surface into four primary landform types, each shaped by distinct tectonic, erosional, and depositional processes.
Definition: Elevated crustal blocks rising abruptly, high local relief.
Origins: Tectonic collision (Himalayas, Alps), volcanic arcs (Andes, Cascades), fault-block uplift (Sierra Nevada, Tetons), hotspot volcanism (Hawaii).
Key ranges: Himalayas (Everest 8,848 m), Andes (Aconcagua 6,961 m), Rockies, Alps, Urals, Atlas.
Definition: Elevated, relatively flat expanses with steep margins.
Origins: Crustal uplift (Tibetan Plateau), flood basalt accumulation (Deccan, Columbia Plateau), erosional dissection of uplifted plains (Colorado Plateau).
Notable: Tibetan ("Roof of World," 4,500 m avg), Colorado (Grand Canyon carved into it), Deccan (India), Altiplano (Andes).
Definition: Broad, low-relief areas, gentle slopes, low elevation.
Origins: Alluvial deposition (Indo-Gangetic, Mississippi, Amazon, North China Plain), glacial outwash (Great Plains), coastal emergence (Gulf Coastal Plain), lava plains (Snake River Plain).
Significance: Most agriculture, population, transport networks.
Definition: Elongate depressions between hills/mountains, drained by rivers/glaciers.
Origins: River erosion (V-shaped: Grand Canyon, Rhine, Nile), glacial erosion (U-shaped: Yosemite, Lauterbrunnen), rift tectonics (East African Rift, Death Valley).
Types: Canyons, gorges, glacial troughs, rift valleys, hanging valleys.
Each category fractures into subtypes by process, climate, lithosphere, and age. Real landscapes are mosaics—mountains dissected by valleys, plateaus ringed by plains. But the four-fold framework orders the first glance.