Skip to main content

India Physiographic UPSC

 PHYSIOGRAPHY OF INDIA

Physiographically, India can be divided into 5 units:
1. Northern Mountains
2. Northern Plains
3. Plateau region of the South
4. Coastal plains
5. Islands

Areas with different altitudes

The northern mountains consist of
1. Himalayan mountains
2. Trans-Himalayas
3. Eastern-Himalayas or Purvanchal

The Himalayas
1. Means ‘Abode of Snow’.
2. They are one of the youngest fold mountain ranges in the world and comprise mainly sedimentary rocks.
3. They stretch from the Indus River in the west to the Brahmaputra River in the east.
4. Total length is about 5000 km.
5. The width of the Himalayas varies from 500 km in Kashmir to 200 km in Arunachal Pradesh.
6. Their average height is 2000 m.
7. The Pamir, popularly known as the Roof of the World, is the connecting link between the Himalayas and the high ranges of Central Asia.

Himalayas can be divided into 3 parallel or latitudinal ranges:
1. Great Himalayas or Himadari
2. Lesser Himalayas or Himachal
3. Outer Himalayas or Shivalik

Greater/ Outer Himalayas/ Himadari
(i) The average height is 6000 m.
(ii) The average width is 120 to 190 kms.
(iii) These ranges are composed of archean rocks like granite, gneisses, and schists.

Mt. Annapurna

(iv) There are few passes and almost all of them have a height above 4,500 m.

(v) They include
a. Shipki La and Bara Lapcha La in Himachal Pradesh,
b. Burzil and Zozi La in Kashmir,
c. Niti, Lipulekh and Thag La in Uttarankhand,
d. Jelep La and Nathu La in Sikkim.

Lesser Himalayas/Himachal
(i) These ranges have an average height of 3500-5000m and have a width of 50-80 km.
(ii) These ranges are composed of metamorphic rocks.
(iii) This range has the famous and beautiful hill stations which include Shimla, Mussoorie, Nainital, Ranikhet etc.

Lesser Himalayas(iv) Important ranges include Pir Panjal, Dhaula Dar, and Nag Tiba.
(v) In Uttarakhand, the Middle Himalayas are marked by the Mussoorie and the Nag Tibba ranges.

Sub Himalayas or Shivaliks
(i) These ranges have an average height of 1000 to 1500 m. and have an average width of 15 to 50 kms.
(ii) These ranges are made of clay, sand, gravel, slate, boulders etc.
(iii) The Doon valleys are situated in the ranges which include Dehradoon, Patlidoon, and Kothridoon.

Shivalik rangeLongitudinally Himalayas can be divided into the following 4 sections.
1. Punjab Himalayas; between Indus & Satluj
2. Kumaon Himalayas; between Sutlej & Kali
3. Nepal Himalayas; between kali & Tista
4. Assam Himalayas; between Tista & Dihang

TRANS – HIMALAYAS
1. This range lies to the north of the Great Himalayas.
2. It has some important ranges like Karakoram, Laddakh, Zanskar, etc.
3. the highest peak in this region is K2 or Godwin Austin (8611m, in Pak occupied Kashmir).
4. Other high peaks are Hidden Peak (8068 m), Broad Peak (8047 m) and Gasherbrum II (8035 m).
5. The longest glacier is Siachin in the Nubra valley, which is more than 72 km long (biggest glacier in the world).
6. Biafo, Baltaro, Batura, Hispar are the other important glaciers in this region.
7. This area is the largest snow-field outside the Polar Regions.
8. The Eastern Himalayas-made up of Patkai Hills, Naga Hills, Mizo Hills and the Garo, Khasi and Jaintia Hills-are also known as Purvanchal.


NORTH INDIAN PLAINS

North Indian plains(i) Formed by the alluvial deposits brought down by the rivers- Indus, Ganga & Brahmaputra.
(ii) The westernmost portion is occupied by the Thar Desert.
(iii) Approx. 3200 km long & 150-300 km wide.
(iv) Can be divided into following zones:
a. Bhabar
b. Terai
c. Bangar
d. khadar
e. Bhabar Belt

Comments

Popular posts from this blog

Climate

  CLIMATIC DIVERSITY FACTORS AFFECTING INDIAN CLIMATE LATITUDE   THE HIMALAYAS  WEATHER MECHANISMS The variations in local climates of India arise due to a number of factors including : (i) Surface distribution of pressure and winds, (ii) Upper air circulation caused by factors controlling global weather and the inflow of different air masses and jet streams and (iii) Inflow of western disturbances during the winter months and the tropical depressions during the South-West monsoon period into India creating weather phenomena conditions for rainfall. Pressure and surface winds These mechanisms can be described with reference to the two main seasons of the year i.e,  winter  and  summer  when striking changes in weather occur.  The distribution pattern of pressure in Central and West Asia generally influences the weather conditions of India during the winter months. A high pressure centre in the region lying to the north of the Himalaya gives rise to the flow of air at the low level from

Laxmikanth Polity Summary Chapter 1

  Table Of Contents Historical Development of constitution of India Timeline of British rule in India Important Acts Passed during British India and their Provinces Rule in India (1773-1858) Rule in India (1858-1947) Historical Development of Constitution of India During 200 years of British rule in India various acts were passed in order to have a better control over the administration of this diversified large land under both Company and the Crown rules. These acts have a great influence on country’s present political structure and various constitutional provisions. Timeline of British Rule in India 1. The Company Rule(1773-1857): 2. The Crown Rule (1858-1947) Question: When did the "Crown/Queen Rule" started in India?  a. 1833 b. 1858 c. 1919 d. 1773 ➢  Important Acts passed during British India and their Provisions: 1.  Rule in India (1773-1858) (i)  Regulating Act, 1773 Features of the Act: The act was the first attempt to regularize company affairs in India. It laid the