bergmassers
Bergmassers are large, cohesive rock masses that form the structural core or stand as prominent blocks within mountainous terrain. The term is used in geology to describe monolithic rock bodies, typically resistant to erosion, that protrude above the surrounding topography. In English-language literature they are closely related to the concept of a massif or bedrock core of a mountain range, though bergmassers emphasizes their monolithic, massive character.
Etymology: The word combines German roots berg, meaning mountain, and masse or masse, meaning mass. The term
Formation and composition: Bergmassers originate when deep crustal rocks are uplifted and exposed through tectonic collision,
Geomorphology and distribution: Bergmassers commonly form the high-standing cores of mountain belts and can persist as
See also: Massif, Craton, Batholith, Igneous rock, Metamorphic rock.