Massifs

Massifs are large, cohesive blocks of the Earth's crust that form the cores of mountainous regions or stand as isolated high blocks. In geology and physical geography, a massif denotes a relatively intact block of rock that has resisted erosion longer than its surroundings, often composed of ancient, resistant rocks such as granites, gneisses, or other high-grade metamorphic rocks. As a result, massifs frequently retain rugged relief and can dominate the topography of a region.

Formation and boundaries: Massifs arise from tectonic processes that uplift and deform crust during continental collision or crustal thickening. Over geological time, differential erosion wears away surrounding rocks, exposing and isolating the massif. The edges are commonly defined by faults or other structural boundaries, which give massifs their characteristic blocklike outline within a larger mountain belt.

Geography and significance: Notable examples include the Mont Blanc massif in the Western Alps and the Massif Central in south-central France. Massifs host unique ecosystems and provide important water sources; their rocks often shelter endemic species and specialized habitats. They are important for human activity, including mining, quarrying, hydroelectric power, and outdoor recreation such as hiking and mountaineering. Because massifs are built from hard rocks at higher elevations, they can experience alpine climatic conditions and glaciation, leaving features such as cirques and horns.

See also: The term massif is a geological concept that describes a substantial, cohesive crustal block, distinct from but related to broader mountain ranges, as the massif can be the core block of a range or an isolated uplifted block within a region.