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Wednesday, 13 July 2011

Indian geography 8

MOUNTAINS

Overview
  • A mountain is a large landform that stretches above the surrounding land in a limited area
  • Mountains are sometimes referred to by the Greek name: montes or mons (singular)
  • The highest mountain on earth is Mount Everest (8848 m)
  • The highest mountain in the solar system is Olympus Mons on Mars (21,171 m)
  • Mountains cover 24% of earth’s land mass
  • The study of mountains is called Orology
Characteristics of mountains
  • Mountains are colder than lower ground because the Sun heats the Earth from the ground up.
  • When the Sun’s rays travel through the atmosphere and reach the ground, the earth absorbs the heat. In general air closest to the earth’s surface is warmest
  • Air temperature usually decreases 1-2 C for every 300 m of altitude
  • The flora and fauna in tall mountains tend to be isolated to one particular altitude zone. These isolated ecological systems are called sky islands.
  • The peak shape of mountains is produced by glaciation and erosion through frost action
  • As altitude increases, the atmospheric pressure decreases. Thus, although the percentage of oxygen remains constant (21%), the amount of oxygen decreases.
  • Altitude sickness (aka Acute Mountain Sickness) is caused by lack of oxygen at high altitudes. Altitude sickness can lead to High Altitude Pulmonary Edema (HAPE) or High Altitude Cerebral Edema (HACE)
  • Availability of oxygen decreases significantly over 3000 m (10,000 ft). for this reason, the cabin altitude in passenger aircraft is kept to 8000 ft
  • Higher altitudes also mean lesser protection to UV radiation
Formation of mountains
  • Mountains are usually produced by the movement of lithospheric plates
  • Major mountains tend to occur along long linear arcs, indicating tectonic plate boundaries
  • Compressional forces in continental collisions cause the compressed region to thicken and force the upper surface upwards
  • Meanwhile, in order to balance the weight, much of the compressed rock is forced downwards as well, forming deep “mountain roots”. As a result, mountains form upwards as well as downwards.
Types of mountains
  • Fold Mountains
    • Formed by the effects of folding on layers within the upper part of the earth’s crust
    • Fold mountains are generally formed on the less deformed areas adjacent to areas strongly affected by thrust tectonics
    • Most fold mountains are likely to relative young in geological terms since they will start to erode as soon as they are formed
    • Examples: Zagros mountains (Iran), Jura mountains (near the Alps i.e. France, Switzerland, Germany)
  • Fault-block mountains
    • Formed when large areas of bedrock are broken up by faults creating large vertical displacements of continental crust
    • These mountains are formed by the crust being stretched and extended by tensional forces
    • The uplifted blocks are called block mountains or horsts. The intervening dropped blocks are called graben, and can form extensive rift valleys
    • Examples: Vosges (northeast France), Basin and Range (western USA)
  • Volcanic mountains
    • Isolated mountains produced by volcanoes
    • Includes small islands that reach great heights beyond the ocean floor
    • Example: Mount Kilimanjaro (Tanzania)
  • Inselberg (or Monadnock)
    • They are isolated hills or small mountains that rise abruptly from a surrounding plain
    • They arise when a rock resistant to erosion is enclosed within a softer rock like limestone. When the limestone erodes away to form the nearby plains, the resistant rock is left behind as an island-mountain
    • Example: sugarloaf mountain (Brazil), Pilot Mountain (USA)
The Seven Summits
  • The Seven Summits are the highest mountain peaks of each of the seven continents
  • The Seven Summits are
    • Africa: Mount Kilimanjaro – Tanzania
    • Antarctica: Vinson Massif – British Antarctic Territory
    • Australia: Kosciuszko – Australia
    • Asia: Mount Everest – Nepal, Tibet
    • Europe: Elbrus – Russia
    • North America: Mount McKinley (Denali) – Alaska
    • South America: Aconcagua – Argentina
Important Mountain ranges in the world
Mountain Range
Location
Length
(km)
Notes
Mid ocean ridge
65,000
Underwater mountain range
Longest mountain range in the world
Demarcates boundary b/w tectonic plates
Consists of seven ridges connected together: Gakkel Ridge, Mid Atlantic, Southwest Indian, Central Indian, Southeast Indian, Pacific Antarctic, East Pacific Rise
Andes
South America
7000
Longest continental mountain range
Highest mountain range outside Asia
Rocky
North America
4800
Himalayas
Asia
3800
Highest mountain range on earth
Includes Karakoram, Hindu Kush
Separates Indian subcontinent from Tibetan plateau
Great Dividing Range
Australia
3700
Transantarctic Mountains
Antarctica
3500
Serve as division b/w East Antarctica from West Antarctica
Important Mountain peaks in the world
Mountain peak
Height
(m)
Mountain Range
Location
Notes
Mount Everest
8848
Himalayas
Nepal/ Tibet
Highest mountain on earth
K2
(Mt. Godwen-Austen)
8611
Karakoram
Pakistan/China
Second highest mountain
Second highest fatality rate (25%)
Kangchenjunga
8586
Himalayas
Nepal/India
Highest in India
Annapurna
8091
Himalayas
Nepal
Highest fatality rate (40%)
Aconcagua
6961
Andes
Argentina
Highest mountain outside Asia
Mt. Kilimanjaro
5895
Kilimanjaro
Tanzania
Highest volcanic mountain
Highest in Africa
Mt Erebus
3794
Antarctica
(Ross Island)
Southernmost active volcano
Mt Chimborazo
6268
Andes
Ecuador
Point on surface most distant from earth’s centre
Important Mountain ranges in India
Mountain range
Location
Notes
Himalayas

Aravalli
Rajasthan, Haryana, Gujarat
Were extremely tall in ancient times, now completely worn down due to weathering
Vindhyas
Gujarat, Madhya Pradesh
Earliest known fossil of eukaryotes discovered here (1.6 billion years)
Satpura
Gujarat, Maharashtra, Madhra Pradesh, Chattisgarh
Sivalik Hills
Sikkim, Nepal, Uttarakhand, Kashmir, Pakistan
Southernmost and geologically youngest of the Himalayan system
Eastern Ghats
West Bengal, Orissa, Andhra Pradesh, Tamil Nadu
Discontinuous range of mountains
Older than Western Ghats
Western Ghats
Gujarat, Maharashtra, Karnataka, Kerala, Tamil Nadu
60% of Western Ghats located in Karnataka
Rivers from Western Ghats drain 40% of India
One of world’s ten “Hottest Biodiversity Spots”
Nilgiri Hills
Tamil Nadu
UNESCO World Heritage Site
Anamalai Hills
(Western Ghats)
Kerala, Tamil Nadu
Under consideration for UNESCO World Heritage Site
Cardamom Hills
(Western Ghats)
Kerala, Tamil Nadu
Under consideration for UNESCO WHS
Southwest Indian Ridge
Indian Ocean
Separates African Plate from Antarctic Plate
Central Indian Ridge
Indian Ocean
Boundary between African Plate and Indo-Australian Plate
Southeast Indian Ridge
Indian Ocean
Separates Indo-Australian Plate from Antarctic Plate
Important Mountain peaks in India
Mountain peak
Mountain range
Location
Notes
Kangchenjunga
Himalayas
Sikkim
Highest peak in India
Third highest in the world
Nanda Devi
Himalayas
Uttarakhand
Highest peak entirely within India
Anamudi
Anaimalai Hills
(Western Ghats)
Kerala
Highest peak in India outside the Himalayas
Mount Abu
Aravalli Hills
Rajasthan
Highest peak in the Aravallis

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