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]
Contents
1 List of massifs
1.1 Africa
1.2 Antarctica
1.3 Asia
1.4 Europe
1.5 North America
1.6 Oceania
1.7 Caribbean
1.8 South America
1.9 Submerged
2 References
List of massifs
Africa
Adrar des Ifoghas – Mali
Aïr Massif – Niger
Bongo Massif – Central African Republic
Marojejy Massif – Madagascar
Mulanje Massif – Malawi
Waterberg Biosphere – South Africa
Virunga Massif – border shared by Uganda, Rwanda and DR Congo
Kilimanjaro Massif – border of Kenya and Tanzania
Oban Massif – Nigeria
Antarctica
- Borg Massif
- Craddock Massif
- Cumpston Massif
- Vinson Massif
- Otway Massif
Asia
Annapurna – Nepal
Chu Pong Massif – Vietnam
Dhaulagiri – Nepal
Gasherbrum – Pakistan
Hazaran – Iran
Kholeno – Iran
Kangchenjunga – Nepal
Knuckles Massif – Sri Lanka
Kondyor Massif – Russia
Kugitangtau Ridge – Turkmenistan
Logar ultrabasite massif – Logar Province, Afghanistan
Mount Ararat – Turkey
Mount Everest massif (including Lhotse) – border of Nepal and Tibet (China)
Mount Kinabalu – Malaysia
Mount Tomuraushi – Japan
Nanga Parbat – Pakistan
Nun Kun – India
Panchchuli – India
Shillong – Meghalaya, India
Europe
Alpilles – France
Aravis Range – France
Ardennes Massif – France/Belgium/Luxembourg
Areskutan – Sweden
Armorican Massif – Brittany, France
Bauges Massif – France
Beaufortain Massif – France
Ben Nevis massif – Scotland, United Kingdom
Bohemian Massif – Czech Republic
Bornes Massif – France
- Calanques Massif
Ceahlău Massif – Romania
- Cerces Massif
Chablais Massif – France
Chartreuse Massif – France
Cornubian Massif – United Kingdom
Dévoluy Massif – France
Massif des Écrins – France
Gotthard Massif – Switzerland
Jungfrau Massif – Switzerland
Jura Mountains – France
- Lauzière massif
- L'Esterel Massif
Long Mynd – England, United Kingdom
Lubéron – France
Massif Central – France
Massiccio del Matese - Italy
Mangerton Mountain – Ireland
Mercantour – France
Montgris – Spain
Montserrat – Spain
Mont Blanc massif – Italy/France/Switzerland
Massiccio del Pollino - Italy
Rila - Rhodope Massif – Bulgaria/Greece
Sila Massif – Italy
Snowdon Massif – Wales, United Kingdom
Taillefer Massif – France
Troodos – Cyprus
Untersberg – Germany/Austria
Queyras Massif – France
Vanoise Massif – France
Vercors Plateau – France
Vitosha Massif – Bulgaria
Vosges Mountains – France
West Staines Massif – Staines-upon-Thames, United Kingdom
North America
Adirondack Massif – New York, USA
Mount Cayley massif – British Columbia, Canada
Laurentian Massif – Quebec, Canada
Le Massif – Canada
Denali – Alaska, USA
Level Mountain – Canada
Mount Edziza – Canada
Mount Juneau – Alaska, USA
Mount Le Conte – Tennessee, USA
Mount Logan – Yukon, Canada
Mount Meager massif – Canada
Mount Septimus – Canada
Mount Shuksan – Washington, USA
Teton Range – Wyoming, USA
Oceania
Big Ben – Heard Island
Ahipara Gumfields – New Zealand
Caribbean
Massif de la Hotte – Haiti
Valle Nuevo Massif – Dominican Republic
South America
Brasilia Massif – Brazil, Argentina, Paraguay, Uruguay.
Neblina massif – Venezuela–Brazil border
Colombian Massif – Colombia
North Patagonian Massif – Argentina
Deseado Massif – Argentina
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..mw-parser-output cite.citation{font-style:inherit}.mw-parser-output .citation q{quotes:"""""""'""'"}.mw-parser-output .citation .cs1-lock-free a{background:url("//upload.wikimedia.org/wikipedia/commons/thumb/6/65/Lock-green.svg/9px-Lock-green.svg.png")no-repeat;background-position:right .1em center}.mw-parser-output .citation .cs1-lock-limited a,.mw-parser-output .citation .cs1-lock-registration a{background:url("//upload.wikimedia.org/wikipedia/commons/thumb/d/d6/Lock-gray-alt-2.svg/9px-Lock-gray-alt-2.svg.png")no-repeat;background-position:right .1em center}.mw-parser-output .citation .cs1-lock-subscription a{background:url("//upload.wikimedia.org/wikipedia/commons/thumb/a/aa/Lock-red-alt-2.svg/9px-Lock-red-alt-2.svg.png")no-repeat;background-position:right .1em center}.mw-parser-output .cs1-subscription,.mw-parser-output .cs1-registration{color:#555}.mw-parser-output .cs1-subscription span,.mw-parser-output .cs1-registration span{border-bottom:1px dotted;cursor:help}.mw-parser-output .cs1-ws-icon a{background:url("//upload.wikimedia.org/wikipedia/commons/thumb/4/4c/Wikisource-logo.svg/12px-Wikisource-logo.svg.png")no-repeat;background-position:right .1em center}.mw-parser-output code.cs1-code{color:inherit;background:inherit;border:inherit;padding:inherit}.mw-parser-output .cs1-hidden-error{display:none;font-size:100%}.mw-parser-output .cs1-visible-error{font-size:100%}.mw-parser-output .cs1-maint{display:none;color:#33aa33;margin-left:0.3em}.mw-parser-output .cs1-subscription,.mw-parser-output .cs1-registration,.mw-parser-output .cs1-format{font-size:95%}.mw-parser-output .cs1-kern-left,.mw-parser-output .cs1-kern-wl-left{padding-left:0.2em}.mw-parser-output .cs1-kern-right,.mw-parser-output .cs1-kern-wl-right{padding-right:0.2em}
^ 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.
^ "The Sydney Morning Herald, November 6, 2009". 2009-11-06.