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Massif |
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This article does not cite any references or sources. Please help improve this article by adding citations to reliable sources. Unverifiable material may be challenged and removed. (December 2007) |
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. The massif is a smaller structural unit of the crust than a tectonic plate.
The word is taken from French (in which the word also means "massive"), where it is used to refer to a large mountain mass or compact group of connected mountains forming an independent portion of a range. One of the most notable European examples of a massif is the Massif Central of the Auvergne region of France.
In computing, massif is a plugin for the Valgrind memory analyzer.
In mountaineering and climbing literature, a massif is frequently used to denote the main mass of an individual mountain.
The Face on Mars is also called a massif, or alternatively, an albedo feature.[1]
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