Tuesday 28 October 2014

Smart Notes on Indian (Physical) Geography Part - 2



PHYSIOGRAPHIC DIVISION OF INDIA

India can be divided into six physio-graphic regions. 

1)  The Northern Mountains   (The North and North-eastern Mountains)                           
 2) The Peninsular Plateau
 3) Indo Gangetic Plains
4 Indian Deserts 
5) The Coastal Plains (East & West)
6) Island









































1)  The Northern Mountains (The North and North-eastern Mountains)

1.       The Himalayas consist of a series of parallel mountain ranges.
2.       The general orientation of these ranges is from northwest to the southeast direction in the north-western part of India
3.       Himalayas in the Darjeeling and Sikkim regions lie in an east west direction
4.       While in Arunachal Pradesh they are from southwest to the northwest direction
5.       In Nagaland, Manipur and Mizoram, they are in the north south direction
6.       The approximate length of the Great Himalayan range, also known as the central axial range, is 2,500 km from east to west
7.        Their width varies between 160-400 km from north to south.
8.       Himalayas are not only the physical barrier; they are also a climatic, drainage and cultural divide.

 On the basis of relief, alignment of ranges and other geomorphologic features the Himalayas can be divided into the following sub-divisions

(i) Kashmir or North-western Himalayas
(ii) Himachal and Uttaranchal Himalayas
(iii) Darjeeling and Sikkim Himalayas
(iv) Arunachal Himalayas
(v) Eastern Hills and Mountains

(i)Kashmir or North-western Himalayas

 Comprise a series of ranges such as
1.       Karakoram
2.       Ladakh
3.       Zaskar
4.       Pir Panjal


Figure (1) - Western Himalaya

1.       The north-eastern part of the Kashmir Himalayas is a cold desert, which lies between the Greater Himalayas and the Karakoram ranges
2.       Great Himalayas and the Pir Panjal range, lies the world famous valley of Kashmir and the famous Dal Lake.
3.       The Kashmir Himalayas are also famous for Karewa formations, which are useful for the cultivation of Zafran, a local variety of saffron.
4.       This region is drained by the river Indus, and its tributaries such as the Jhelum and the Chenab.
5.       The Kashmir and north-western Himalayas are well-known for their scenic beauty and picturesque landscape
6.        Famous places of pilgrimage such as Vaishno Devi, Amarnath Cave, Charar -e-Sharif, etc. are also located here and large number of pilgrims visit these places every year
7.       Srinagar, capital city of the state of Jammu and Kashmir is located on the banks of Jhelum River.
8.       Srinagar, capital city of the state of Jammu and Kashmir is located on the banks of Jhelum River.
9.       An Interesting Fact
10.   In Kashmir Valley, the meanders in Jhelum River are caused by the local base level provided by the erstwhile larger lake of which the present Dal Lake is a small part.
11.   The Himachal and Uttaranchal Himalayas
12.   This part lies approximately between the Ravi in the west and the Kali (a tributary of Ghaghara) in the east
13.   It is drained by two major river systems of India, i.e. the Indus and the Ganga.
14.   Tributaries of the Indus include the river Ravi, the Beas and the Satluj
15.   The tributaries of Ganga flowing through this region include the Yamuna and the Ghaghara.
16.   The northernmost part of the Himachal Himalayas is an extension of the Ladakh cold
Some Important facts of this region
Karewas
Karewas are the thick deposits of glacial clay and other materials embedded with moraines.
 Important passes of the region are
1.       Zoji La on the Great Himalayas
2.       Banihal on the Pir Panjal
3.       Photu La on the Zaskar
4.       Khardung La on the Ladakh range.
Important fresh lakes
1.       Dal
2.       Wular
Salt water lakes such as
1.       Pangong Tso
2.       Tso Moriri
‘Valley of flowers’
1.       The famous ‘Valley of flowers’ is also situated in this region.
2.       The places of pilgrimage such as the Gangotri, Yamunotri, Kedarnath, Badrinath and Hemkund Sahib are also situated in this part.
3.       The region is also known to have five famous Prayags (river confluences)

(ii) Himachal and Uttaranchal Himalayas


Figure (2)-  Himalayan Mountain Complex : Cross Sectional View from South to North

Great Himalaya or Himadri

1.       Northern most range is known as the Great or Inner Himalayas or the ‘Himadri’.
2.       ‘Himadri’. It is the most continuous range consisting of the loftiest peaks with an average height of 6,000 metres.
3.       The folds of Great Himalayas are asymmetrical in nature.
4.       The core of this part of Himalayas is composed of granite.
It is perennially snow bound, and a number of glaciers descend from this range. The Himalayan Mountains are divided into three main parallel ranges.

Bhotia’s

1.       In the Great Himalayan range, the valleys are mostly inhabited by the Bhotia’s.
2.       These are nomadic groups who migrate to ‘Bugyals’ (the summer glasslands in the higher reaches) during summer months and return to the valleys during winters.

Himachal or lesser Himalaya

1.       The range lying to the south of the Himadri forms the most rugged mountain system and is known as Himachal or lesser Himalaya.
2.       The altitude varies between 3,700 and 4,500 metres and the average width is of 50 Km.
3.       The Pir Panjal range forms the longest and the most important range
4.       The Dhaula Dharand the Mahabharat ranges are also prominent ones.
5.       This range consists of the famous valley of Kashmir, the Kangra and Kullu Valley in Himachal Pradesh.
6.       This region is well known for its hill stations

Shiwaliks

1.       The outer most range of the Himalayas is called the Shiwaliks.
2.       They extend over a width of 10-50 Km and have an altitude varying between 900 and 1100 metres.
3.       These ranges are composed of unconsolidated sediments brought down by rivers from the main Himalayan ranges located farther north.
4.       Covered with thick gravel called Alluvium.
5.       The longitudinal valley lying between lesser Himalaya and the Shiwaliks are known as Duns.
6.       Dehra Dun, Kotli Dun and Patli Dun are some of the well-known Duns.
7.       The word shiwalik has its origin in the geological formation found in and around a place called Sivawala near Dehra Dun
8.       Which was once a headquarter of the Imperial Survey and which subsequently established its permanent headquarters at Dehra Dun.
9.       Dehra Dun is the largest of all the duns with an approximate length of 35-45 km and a width of 22-25 km.

Some of the important hill stations

1. Dharamshala
2. Mussoorie
3. Shimla
4. Kaosani

The cantonment towns and health resorts

1. Shimla
2. Mussoorie
3. Kasauli
4. Almora
5. Lansdowne
 6. Ranikhet

The two distinguishing features of this region

1. The ‘Shiwalik
2. ‘Dun formations’

Some important duns

1. Chandigarh-Kalka dun
2. Nalagarh dun
3. Dehra Dun
4. Harike dun
5. The Kota dun

(iii)The Darjeeling and Sikkim Himalayas

1.       They are flanked by Nepal Himalayas in the west and Bhutan Himalayas in the east.
2.       It is relatively small but is a most significant part
3.       Known for its fast-flowing Rivers such as Tista
4.       It is a region of high mountain peaks like Kanchenjunga (Kanchengiri), and deep valleys.
5.       The higher reaches of this region are inhabited by Lepcha tribes while the southern part, particularly the Darjiling Himalayas, has a mixed population of Nepalis, Bengalis and tribals from Central India.
6.       The British, taking advantage of the physical conditions such as
·         Moderate slope
·         Thick soil cover
·         High organic content
·         Well distributed rainfall throughout the year
·         And mild winters,
7.       Introduced tea plantations
8.       In place of the Shiwaliks here, the ‘duar formations’ are important
9.       Which have also been used for the development of tea gardens

(iv) The Arunachal Himalayas

1.       These extend from the east of the Bhutan Himalayas up to the Diphu pass in the east.
2.       The general direction of the mountain range is from southwest to northeast.
3.       Some of the important mountain peaks of the region are Kangtu and Namcha Barwa.
4.       These ranges are dissected by fast-flowing rivers from the north to the south, forming deep gorges.
5.       Bhramaputra flows through a deep gorge after crossing Namcha Barwa.
6.       Some of the important rivers are
·         The Kameng
·         Subansiri
·         The Dihang
·         The Dibang
·         The Lohit.
7.       An important aspect of the Arunachal Himalayas is the numerous ethnic tribal community inhabiting in these areas.
8.       Some of the prominent ones from west to east are
·         The Monpa
·         Daffla
·         Abor
·         Mishmi
·         Nishi
·         The Nagas
9.       Most of these communities practise Jhumming.

(v) The Eastern Hills and Mountains

1.       These are part of the Himalayan mountain system having their general alignment from the north to the south direction
2.       They are known by different local names
3.       In the north, they are known as Pataki Bum, Naga Hills,
4.       In the south as Mizo or Lushai hills.
5.       Most of these ranges are separated from each other by numerous small rivers.
6.       The Barak is an important river in Manipur and Mizoram.
7.       The physiography of Manipur is unique by the presence of a large lake known as ‘Loktak’ lake at the centre, surrounded by mountains from all sides.
8.       Mizoram which is also known as the ‘Molassis basin’ which is made up of soft unconsolidated deposits.
9.       Most of the rivers in Nagaland form the tributary of the Brahmaputra.
10.   While two rivers of Mizoram and Manipur are the tributaries of the Barak River, which in turn is the tributary of Meghna;


Figure (3) - Eastern Himalaya

Some Highest Peaks of the Himalayas
Peak                         Country                  Height in metres
Mt. Everest               Nepal                        8848
Kanchenjunga            India                        8598
Makalu                       Nepal                       848
Dhaulagiri                  Nepal                       8172
Nanga Parbat             India                       8126
Annapurna                 Nepal                     8078
Nanda Devi                  India                     7817
Kamet                          India                      7756
Namcha Barwa             India                    775
Gurla Mandhata          Nepal                   7728

THE HIMALAYAS AND OTHER PENINSULAR MOUNTAINS

1.       The Himalayas along with other peninsular mountains are young, weak and flexible in their geological structure
2.       They are still subjected to the interplay of exogenic and endogenic forces,
3.       Resulting in the development of faults, folds and thrust plains.
4.       These mountains are tectonic in origin, dissected by fast-flowing rivers which are in their youthful stage.
5.       Various landforms like (are indicative of these stages)
a)      Gorges
b)      V-shaped valleys
c)       Rapids
d)      Waterfalls

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