Major Landform on Earth
Major Landforms
- First order – Continents/Ocean Basins
- Second order – Relief Structure (Mountain, Plateaus, Plains)
- Third order – Form due to Action of Climatic agents (Running water, wind, Glacial, Waves/Currents, Ground Water).
Orogeny (Mt Formation)
- Pre-Cambrian – Aravalli’s
- Caledonian orogeny about 360 million ago (Candenary country: Norway, Finland, Sweden)
- Heregonian – about 240 Million years (Ural: Asiatic Russia from Europe Russia & Appalachian: North western part of USA).
- Alpline – About 30 Million years. They are young fold Mountain (Rockies, Andes, Alps, Atlas, Himalayas).
Types of Mountain
- Fold Mountain – Structural Mt
- Block Mountain – Structural Mt
- Volcanic Mountain – Mt of Accumulation
- Residual Mountain – Mt of Denudation
Fold Mountain & Types
- Anticline Simple fold
- Asymmetric fold
- Over fold
- Recumbent fold
- Over thrust Fold (Nappe)
Block Mountain
- Due to tensional force – Crustal faulting
- Ex: African Rift Valley
- Due to Compressional force – thrust of Reverse fault
- Ex: Sierra Nevada (USA)
Volcanic Mountain
- Layer of Solidified magma
- Ex: Mt. Fuji (Japan), Mt. Mayon (Phillippines), Mt. Merapi (Sumatra), Mt. Agung (Bali), Mt. Catopaxi (Ecuador)
Residual Mountain
- Evolved by Continuous denudation (Weathering + Eroding + Transportation)
- Denudation process called Relict Mt – Ex: Aravalli
- Ex: Mt. Manodnock (USA),
Facts
- Deepest mine – South Africa (4 km).
- Radius of Earth - 6371km - Crust – 1% Mantle – 84%, Core -15%.
- Tsunamis are waves generated by the tremors and not an earthquake in itself.
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