A massif (/mæˈsf, ˈmæsɪf/) is a principal mountain mass,[1] such as a compact portion of a mountain range, containing one or more summits (e.g. France's Massif Central). In mountaineering literature, a massif is frequently used to denote the main mass of an individual mountain.

A massif in Ukraine

As a purely scientific term in geology, however, a "massif" is separately and more specifically defined as 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. A massif is a smaller structural unit than a tectonic plate and is considered the fourth-largest driving force in geomorphology.[2]

The word "massif" originates 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. The Face on Mars is an example of an extraterrestrial massif.[3] Massifs may also form underwater, as with the Atlantis Massif.[4]

List

edit

Africa

edit

Algeria

edit

Antarctica

edit

Asia

edit

India

edit

Iran

edit

Kazakhstan

edit

Europe

edit
 
Aerial view of Mont Blanc massif, an example of a massif and also the highest summit in the Alps.[5]
 
Panorama of Pirin Mountain massif, Bulgaria
 
Gran Sasso d'Italia massif seen from an airplane. Part of the Apennine Mountains, it is located in the Abruzzo region of Italy.

France

edit

Italy

edit

United Kingdom

edit

North America

edit

Canada

edit

United States

edit

Oceania

edit

Caribbean

edit

South America

edit

Submerged

edit

References

edit
  1. ^ "massif". Merriam-Webster.com Dictionary. Retrieved 2023-06-21.
  2. ^ Allen, 2008, Time scales of tectonic landscapes and their sediment routing systems, Geol. Soc. Lon. Sp. Pub., v. 296, p. 7–28.
  3. ^ Britt, Robert Roy (2006-09-21). "Mars Face Makeover: Controversial Formation Observed from New Angles". Space.com. Retrieved 2009-05-04.
  4. ^ 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.
  5. ^ "The Sydney Morning Herald, November 6, 2009". 2009-11-06.
  6. ^ Tollo, Richard (June 16, 2023). "Mesoproterozoic Geology of the Blue Ridge Province in North-Central Virginia: Petrologic and Structural Perspectives on Grenvillian Orogenesis and Paleozoic Tectonic Processes". USGS. Retrieved June 15, 2023.
  7. ^ Tollo, Richard (June 16, 2023). "Mesoproterozoic Geology of the Blue Ridge Province in North-Central Virginia: Petrologic and Structural Perspectives on Grenvillian Orogenesis and Paleozoic Tectonic Processes". USGS. Retrieved June 15, 2023.