A massive topographic and structural feature, especially in an orogenic belt, commonly formed of rocks that are more rigid than those of its surroundings.
A compact mountain group consisting of several summits.
A block of the earth's crust bounded by faults or folds; a group of mountains formed by such a structure.
In geology, a massif is a section of a planet's crust that is demarcated by faults or flexures. In the movement of the crust, a massif tends to retain its internal structure while being displaced as a whole. The term is also used to refer to a group of mountains formed by such a structure.