Geography

Geography - Mountains

Mountains:
Mountains are of 3 types. They are volcanic mountains, fold mountains and block mountains. Volcanic mountains are formed when one plate is pushed below another plate or hotspot or mid-ocean ridge. Based on activity volcanic mountains can be classified as active, dormant or extinct. Based on structure, volcanic mountains can be classified as Shield, Cinder and Stratovolcano (Composite). Cinder cone is a conical hill formed from fragments of volcano that have fallen around the volcanic vent. It mostly has bowl-shaped crater at the summit. Example is Mount Etna, Italy. Shield is formed by low-viscosity lava. It can be very wide. It is most commonly found in Hawaii. Example is Mauna Loa in Hawaii. Stratovolcano is formed by ash, lava and other materials. Very dangerous. Example is Mount Vesuvius, Italy. Fold mountains are formed when two plates collide. Examples of fold mountains are the Himalayas, the Andes and the Alps. Block mountains are caused by faults. Block mountains are formed when rocks on one side of a fault rise relative to the other. Examples of block mountains are Sierra Nevada, USA and The Vosges, France.

ContinentMountain RangeMountainMountain typeHeight(meters) approxCountry
AsiaHimalayasMount EverestFold mountain8848China/Nepal
AsiaKarakoramK2Fold mountain8611China/Pakistan
AsiaHimalayasKanchenjungaFold mountain8586India/Nepal
EuropeCaucasusMount ElbrusVolcanic mountain5642Russia
EuropeCaucasusDykh-TauVolcanic mountain5205Russia
EuropeCaucasusShkharaVolcanic mountain5193Georgia/Russia
EuropeAlpsMont BlancFold mountain4809France/Italy
North AmericaAlaska rangeDenali (Mount Mckinley)Volcanic6190.5USA
North AmericaSaint Elias MountainsMount LoganVolcanic5959Canada
North AmericaCordillera NeovolcanicaPico de OrizabaVolcanic5636Mexico
South AmericaAndesAconcaguaFold mountain6961Argentina
South AmericaAndesOjos del SaladoFold mountain6893Argentina/Chile
South AmericaAndesMonte PissisFold mountain6793Argentina
AfricaKilimanjaroKiboVolcanic mountain5895Tanzania
AfricaMount KenyaMount Kenya (Batian)Volcanic mountain5199Kenya
AfricaMount KenyaMount Kenya (Nelion)Volcanic mountain5188Kenya

Plateaus:
Plateau is a flat terrain that raises above the surrounding area on at least one side. Plateaus can be formed by volcanic activity, tectonic plate movements or erosion by water or ice. One of the major landforms is Plateaus. Others are mountains, hills and plains. A dissected plateau forms from upward movement of earth’s crust, caused by collision of tectonic plateaus. A volcanic plateau is formed by volcanic eruptions. In some cases a plateau is eroded and forms small raised sections. Oceanic plateaus can be made up of continental crust or of igneous rock. They have steeply raised edges.

Plateau

Formed by

Location

Tibetan Plateau (largest)

Tectonic plate movements

Asia

Deccan Plateau

Volcanic activity

India

The Colorado Plateau

Tectonic plate movements

USA

The Mexican Plateau

Tectonic plate movements

Mexico

The Colombia Plateau

Volcanic activity

USA

Plains:
Plains are large, flat areas that does not change much in elevation. They are good for agriculture because they have fertile soils and have grassy lands for grazing animals. The plains near the ocean are called coastal plains. Different species of wildlife like squirrels, foxes etc. exist here. They cover about one-third of the land of the world. Alluvial plains are formed by rivers, Glacial plains are formed by movement of glaciers, Lava plains are formed by lava, Lacustrine plains are formed as the bed of a lake. Structural plains are mostly undisturbed horizontal surfaces. Erosional plains have been formed by agents of denudation as rivers, glacier, running water etc.