Geology of the Himalayas
Geology of the Himalayas
Origins and structure of the Himalayan Mountain range.
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First pulled by Siwaragee, Nov 1, 2026
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Readers' pathsAug 2026 – Oct 2026
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Pre-collisional Himalaya
11%
Himalayas
Mountain range in Asia.
8.6%
Nanga Parbat
9th-highest mountain on Earth.
7.3%
Geology of Nepal
6.1%
Namcha Barwa
Mountain in Tibet.
6%
Mount Everest
Earth's highest mountain.
5%
Cimmeria (continent)
Ancient string of microcontinents that rifted from Gondwana.
5%
Sedimentary budget
4.2%
Indian plate
Minor plate that separated from Gondwana.
4%
Main Himalayan Thrust
Geological feature.
3.9%
Readers come from
Share of the 2,321 readers arriving from another article
Himalayas
Mountain range in Asia.
16%
Zanskar Range
Mountain range in Ladakh.
11%
Karakoram
Mountain range spanning the borders between Pakistan, India and China.
8.3%
Pangaea
Supercontinent from the late Paleozoic to early Mesozoic eras.
6.2%
Tibetan Plateau
Plateau in Central, South and East Asia.
6.2%
Mount Everest
Earth's highest mountain.
5.3%
Indus-Yarlung suture zone
Tectonic suture in southern Tibet.
4.4%
Alpide belt
Belt of Eurasian mountain ranges.
3.9%
Miocene
First epoch of the Neogene Period.
3.5%
Nanga Parbat
9th-highest mountain on Earth.
3.2%