A **mountain** is a **natural elevation of the Earth's surface** rising **abruptly from surrounding terrain** to a **summit**, typically defined as **≥600 meters (2,000 feet) above sea level** (or ≥300m/1,000ft above surrounding base). There is no single universal standard; prominence, isolation, and cultural perception also factor.
| Type | Mechanism | Key Features | Examples |
|---|---|---|---|
| 1. Fold Mountains | Compression of sedimentary layers at convergent boundaries → folding, thrust faulting, crustal thickening. | Long, linear belts; parallel ridges (anticlines) & valleys (synclines); thick sedimentary sequences; high seismicity. | Himalayas, Alps, Andes, Rockies, Appalachians, Urals, Atlas, Zagros. |
| 2. Fault-Block Mountains (Block Mountains) | Tensional forces → normal faults → crustal blocks tilt/uplift (horsts) & drop (grabens). | Steep fault scarp on one side, gentle dip slope on other; linear ranges separated by basins (Basin & Range). | Sierra Nevada (CA), Teton Range (WY), Wasatch Range (UT), Vosges/Black Forest (Europe), Rwenzori (Africa), Basin & Range Province (US West). |
| 3. Dome Mountains | Magma intrusion (laccolith/batholith) uplifts overlying strata into dome; erosion exposes core. | Rounded, symmetrical uplift; concentric drainage; exposed igneous/metamorphic core. | Adirondacks (NY), Black Hills (SD/WY), Henry Mountains (UT), Erongo (Namibia), Pilanesberg (SA), Ozarks (broad dome). |
| 4. Volcanic Mountains | Accumulation of erupted lava, pyroclastics, tephra at vent. | Conical (strato), broad gentle (shield), steep loose (cinder), dome. Craters, calderas, lava flows. | Mt. Fuji (JP), Mt. Rainier (US), Mt. Etna (IT), Kilimanjaro (TZ), Mauna Loa/Kea (HI), Popocatépetl (MX), Cotopaxi (EC). |