Massif
In geology, a massif ( /mæˈsiːf/ or /ˈmæsɪf/) 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 also refers to a group of mountains formed by such a structure.
In mountaineering and climbing literature, a massif is frequently used to denote the main mass of an individual mountain. The massif is a smaller structural unit of the crust than a tectonic plate, and is considered the fourth-largest driving force in geomorphology.[1]
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.
The Face on Mars is an example of an extraterrestrial massif.[2]
Massifs may also form underwater, as with the Atlantis Massif.[3]
List of massifs
Africa
- Adrar des Ifoghas – Mali
- Aïr Massif – Niger
- Benna Massif – Guinea
- Bongo Massif – Central African Republic
- Ennedi Plateau – Chad
- Kilimanjaro Massif – border of Kenya and Tanzania
- Oban Massif – Nigeria
- Marojejy Massif – Madagascar
- Mulanje Massif – Malawi
- Virunga Massif – border shared by Uganda, Rwanda and DR Congo
- Waterberg Biosphere – South Africa
Algeria
- Collo Massif – Algeria
- Edough Massif
- Khachna Massif
Antarctica
- Borg Massif
- Craddock Massif
- Cumpston Massif
- Vinson Massif
- Otway Massif
Asia
- Annapurna – Nepal
- Chu Pong Massif – Vietnam
- Dhaulagiri – Nepal
- Gasherbrum – China-Pakistan
- Kangchenjunga – Nepal–India
- Knuckles Massif – Sri Lanka
- Kondyor Massif – Russia
- Kugitangtau Ridge – Turkmenistan
- Kumgangsan – North Korea
- Logar ultrabasite massif – Afghanistan
- Mount Ararat – Turkey
- Mount Everest massif (including Lhotse) – border of Nepal and Tibet (China)
- Mount Kinabalu – Malaysia
- Mount Tomuraushi – Japan
- Nanga Parbat – Pakistan
Iran
- Dena – Iran
- Hazaran – Iran
- Kheru-Naru (Chekel) – Iran
- Kholeno – Iran
- Mount Damavand – Iran
- Sabalan – Iran
- Takht-e Suleyman Massif – Iran
- Zard-Kuh – Iran
Europe


- Aarmassif - Switzerland
- Ardennes Massif – France/Belgium/Luxembourg
- Åreskutan – Sweden
- Arlberg – Austria
- Bohemian Massif – Czech Republic
- Ceahlău Massif – Romania
- Gotthard Massif – Switzerland
- Hesperian Massif - Iberian Peninsula
- Jungfrau Massif – Switzerland
- Mangerton Mountain – Ireland
- Montgris – Spain
- Montserrat – Spain
- Mont Blanc massif – Italy/France/Switzerland
- Rhenish Massif - Germany, Belgium, Luxembourg and France
- Rila - Rhodope Massif – Bulgaria/Greece
- Troodos – Cyprus
- Untersberg – Germany/Austria
- Vitosha Massif – Bulgaria
France
- Alpilles
- Aravis Range
- Armorican Massif
- Bauges Massif
- Beaufortain Massif
- Belledonne massif
- Bornes Massif
- Calanques Massif
- Cerces Massif
- Chablais Massif
- Chartreuse Massif
- Dévoluy Massif
- Massif des Écrins
- Jura Mountains
- Lauzière massif
- Luberon
- Massif Central
- Massif de l'Esterel
- Mercantour
- Monte Cinto massif
- Taillefer Massif
- Queyras Massif
- Vanoise Massif
- Vercors Plateau
- Vosges Mountains
Italy
- Gran Sasso d'Italia
- Grappa Massif
- Massiccio del Matese
- Massiccio del Pollino
- Monte Ermada
- Sila Massif
- Speikboden (South Tyrol)
Kazakhstan
- Degelen
- Kokshetau Massif
- Mount Ku
- Myrzhyk
- Semizbughy
United Kingdom
- Ben Nevis massif
- Cornubian Massif
- Long Mynd
- Snowdon Massif
Canada
- Laurentian Massif – Quebec
- Le Massif de Charlevoix – Quebec
- Mount Logan – Yukon
British Columbia
- Mount Cayley – British Columbia
- Level Mountain
- Mount Edziza
- Mount Meager massif
- Mount Septimus
United States
- Adirondack Massif – New York
- Denali – Alaska
- Mount Juneau – Alaska
- Mount Katahdin - Maine
- Mount Le Conte – Tennessee
- Mount Shuksan – Washington
- Mount Timpanogos - Utah
- Teton Range – Wyoming
Oceania
- Big Ben – Heard Island
- Ahipara Gumfields – New Zealand
Caribbean
- Massif de la Hotte – Haiti
- Valle Nuevo Massif – Dominican Republic
South America
Submerged
- Atlantis Massif – part of the Mid-Atlantic Ridge in the North Atlantic Ocean
- Tamu Massif — the largest volcano on Earth
References
- Allen, 2008, Time scales of tectonic landscapes and their sediment routing systems, Geol. Soc. Lon. Sp. Pub., v. 296, p. 7–28.
- Britt, Robert Roy (2006-09-21). "Mars Face Makeover: Controversial Formation Observed from New Angles". Space.com. Retrieved 2009-05-04.
- Blackman, Donna (2002). "Geology of the Atlantis Massif (Mid-Atlantic Ridge, 30°N): Implications for the evolution of an ultramafic oceanic core complex". Marine Geophysical Researches. 23 (5): 443–469. Bibcode:2002MarGR..23..443B. doi:10.1023/b:mari.0000018232.14085.75. S2CID 96459991.
- "The Sydney Morning Herald, November 6, 2009". 2009-11-06.