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In this article, we will discuss the formation of mountains.
1. Mountains
Mountains are land’s physical features protruding high beyond the hills and very high up the land surface with steep tops commonly shaped up to a peak. It is a feature that towers or rises above the level of the surrounding area more or less abruptly.
Mountain formation results from the forces of erosion, volcanism, or uplifts in the earth‘s crust. Usually, mountains occur in chains or ranges.
Have complex structures due to folding, faulting, volcanic activity, igneous intrusions, etc.
2. Formation of Mountains
The formation of mountains is done by the folding, faulting, or warping of the Earth’s surface due to the displacement of various plate tectonics or by the formation of volcanic rock onto the surface.
The formation of mountains can be by volcanoes spewing lava over and over again. The lava cools and gets solid and makes a mountain. The islands of Hawaii are made of volcanoes. The formation of mountains takes a million billion years.
3. Types of Mountain
Any landmass that is elevated above 1,000 feet in the surrounding area is taken as a mountain.
Different types of mountains have different methods of origin:
a. Fold mountains
b. Block mountains
c. Volcanic mountains and
d. Residual mountain
a. Fold Mountains
i. It results from the earth‘s crust being compressed from the sides
ii. The layers of rocks in the crust are pushed up to form a fold mountain.
iii. The Alps, Himalayas, and the Andes are examples.
b. Block Mountain
Mountains formed due to faulting.
i. A part of the land block is depressed so that the remaining block stands conspicuously above the
surroundings.
ii. The uplifted section is termed the block mountain (horst)
iii. When the middle section falls down instead of going up, it forms the rift valley (graben).
c. Volcanic Mountain
i. The outrushing magma forms the fissures in the crust of the earth at a place into a dome, mountains formed in such a way are called volcanic or laccolith mountains.
ii. Volcanoes emit gases, liquids, and solids as well. The gases are lost in the atmosphere, but the liquid and solid accumulate and heaps around the fissure or orifice.
iii. During continued activity for years, the accumulation grows into an enormous size justifying the name mountain.
d. Residual Mountain
i. When existing mountains or plateaus are in eroding state the resulting structures are called
residual mountains or relict mountains
ii. The eroding agents are snow, wind, rain
iii. They erode the softer materials from the existing mountains thus reshaping the lower hills and valleys.
4. How was Mt Everest formed?
Mount Everest was produced from a tectonic collision between the Indian and Eurasian tectonic plates tens of millions of years ago. The smashup crushed the landscape, elevating mountains along 1,5000 miles, a range that is known as the Himalayas range.
5. Which rock is found on Mt Everest?
The common rocks and minerals available on Mount Everest are granite, limestone, garnet, and schist. Granite is an igneous rock available on the lower slopes of Mount Everest and entire the Everest region.
6. Did Mt Everest grow after the earthquake?
Mt Everest has grown by 86 cm but not by the earthquake that came in 2015. The reason behind it is plate tectonics between Indian and Eurasian tectonic plates.
7. Is Mt Everest a volcano?
No, Mt Everest isn’t a volcano. It was produced from a tectonic collision between the Indian and Eurasian tectonic plates tens of millions of years ago. The smashup crushed the landscape, elevating mountains along 1,5000 miles, a range that is known as the Himalayas range.
8. Effect of Earthquake on Mountain
Larger earthquakes can be the reason behind the formation of mountains topography by making rock uplift more than 1,000 feet but also crumble mountains by causing landslides.
The formation of mountains can be by volcanoes spewing lava over and over again. The lava cools and gets solid and makes a mountain. The islands of Hawaii are made of volcanoes.
9. List of World’s Highest Peaks
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Position | Mountain name(s) | Height (rounded) | Prominence (rounded) | Range |
---|---|---|---|---|
1 | Mount Everest Sagarmatha Chomolungma | 8,848.86 | 29,029 | Mahalangur Himalaya |
2 | K2 | 8,611 | 4,020 | Baltoro Karakoram |
3 | Kangchenjunga | 8,586 | 3,922 | Kangchenjunga Himalaya |
4 | Lhotse | 8,516 | 610 | Mahalangur Himalaya |
5 | Makalu | 8,485 | 2,378 | Mahalangur Himalaya |
6 | Cho Oyu | 8,188 | 2,340 | Mahalangur Himalaya |
7 | Dhaulagiri I | 8,167 | 3,357 | Dhaulagiri Himalaya |
8 | Manaslu | 8,163 | 3,092 | Manaslu Himalaya |
9 | Nanga Parbat | 8,126 | 4,608 | Nanga Parbat Himalaya |
10 | Annapurna I | 8,091 | 2,984 | Annapurna Himalaya |
11 | Gasherbrum I Hidden Peak K5 | 8,080 | 2,155 | Baltoro Karakoram |
12 | Broad Peak | 8,051 | 1,701 | Baltoro Karakoram |
13 | Gasherbrum II K4 | 8,035 | 1,524 | Baltoro Karakoram |
14 | Shishapangma Gosainthan | 8,027 | 2,897 | Jugal Himalaya |
15 | Gyachung Kang | 7,952 | 672 | Mahalangur Himalaya |
S | Gasherbrum III K3a | 7,946 | 355 | Baltoro Karakoram |
16 | Annapurna II | 7,937 | 2,437 | Annapurna Himalaya |
17 | Gasherbrum IV K3 | 7,932 | 712 | Baltoro Karakoram |
18 | Himalchuli | 7,893 | 1,633 | Manaslu Himalaya |
19 | Distaghil Sar | 7,884 | 2,525 | Hispar Karakoram |
20 | Ngadi Chuli | 7,871 | 1,011 | Manaslu Himalaya |
S | Nuptse | 7,864 | 305 | Mahalangur Himalaya |
21 | Khunyang Chhish | 7,823 | 1,765 | Hispar Karakoram |
22 | Masherbrum K1 | 7,821 | 2,457 | Masherbrum Karakoram |
23 | Nanda Devi | 7,816 | 3,139 | Garhwal Himalaya |
24 | Chomo Lonzo | 7,804 | 590 | Mahalangur Himalaya |
25 | Batura Sar | 7,795 | 3,118 | Batura Karakoram |
26 | Rakaposhi | 7,788 | 2,818 | Rakaposhi-Haramosh Karakoram |
27 | Namcha Barwa | 7,782 | 4,106 | Assam Himalaya |
28 | Kanjut Sar | 7,760 | 1,660 | Hispar Karakoram |
29 | Kamet | 7,756 | 2,825 | Garhwal Himalaya |
30 | Dhaulagiri II | 7,751 | 2,397 | Dhaulagiri Himalaya |
31 | Saltoro Kangri K10 | 7,742 | 2,160 | Saltoro Karakoram |
32 | Kumbhakarna Jannu | 7,711 | 1,036 | Kangchenjunga Himalaya |
33 | Tirich Mir | 7,708 | 3,910 | Hindu Kush |
S | Molamenqing | 7,703 | 433 | Langtang Himalaya |
34 | Gurla Mandhata | 7,694 | 2,788 | Nalakankar Himalaya |
35 | Saser Kangri I K22 | 7,672 | 2,304 | Saser Karakoram |
36 | Chogolisa | 7,665 | 1,624 | Masherbrum Karakoram |
S | Dhaulagiri IV | 7,661 | 469 | Dhaulagiri Himalaya |
37 | Kongur Tagh | 7,649 | 3,585 | Kongur Shan (Eastern Pamirs) |
S | Dhaulagiri V | 7,618 | 340 | Dhaulagiri Himalaya |
38 | Shispare | 7,611 | 1,240 | Batura Karakoram |
39 | Trivor | 7,577 | 997 | Hispar Karakoram |
40 | Gangkhar Puensum | 7,570 | 2,995 | Kula Kangri Himalaya |
41 |
| 7,556 | 3,642 | Daxue Mountains (Hengduan Shan) |
42 | Annapurna III | 7,555 | 703 | Annapurna Himalaya |
43 | Skyang Kangri | 7,545 | 1,085 | Baltoro Karakoram |
44 | Changtse | 7,543 | 514 | Mahalangur Himalaya |
45 | Kula Kangri | 7,538 | 1,654 | Kula Kangri Himalaya |
46 | Kongur Tiube | 7,530 | 840 | Kongur Shan (Eastern Pamirs) |
S | Annapurna IV | 7,525 | 255 | Annapurna Himalaya |
47 | Mamostong Kangri | 7,516 | 1,803 | Rimo Karakoram |
48 | Saser Kangri II E | 7,513 | 1,458 | Saser Karakoram |
49 | Muztagh Ata | 7,509 | 2,698 | Muztagata (Eastern Pamirs) |
50 | Ismoil Somoni Peak | 7,495 | 3,402 | Pamir (Academy of Sciences Range) |
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