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                    NOTES :PHYSICAL FEATURES OF INDIA 
               OLDEST LANDMASS: GONDWANA LAND 
             PANGEAU 
    HIMALAYAN MOUNTAINS: 
? These are young and structurally fold mountains. These are the loftiest and one of the 
most rugged mountains barriers of the world. 
? DISTANCE : 2400 km (forms an arc) ; WIDTH-400km(in Kashmir)-150km(in Anu.Pra) 
? It is composed of Granite. It is perennial snow bound and glaciers desend. 
 
HIMALAYAN MOUNTAINS 
 
HIMADRI (GREATER OR INNER HIMALAYA) 
? It contains all the prominent peaks. 
? These are the most loftiest mountain ranges and are always snowbound. 
? AVARAGE HEIGHT =6000m -6100m 
HIMANCHAL ( LESSER HIMALAYA) 
? AVARAGE HEIGHT=3700m-4500m ; AVARAGE WIDTH=50km(rugged mount.) 
? It is well knowned for its  hill stations and beautiful valleys. 
            SHIWALIK( OUTER HIMALAYA OR SUB-HIMALAYA) 
? AVARAGE HEIGHT =900m-1100m;AVARGE WIDTH=10km-50km 
? It is made of unconsolidated sediments  and  are prone to earthquakes. 
? These valleys are covered with alluvium and thick gravels and are youngest. 
 
 
 
 
INDUS AND SATLUJ PUNJAB , KASHMIR, HIMANCHAL HIMALAYA 
SATLUJ AND KALI KUMAON HIMALAYA 
KALI AND TISTA NEPAL HIMALAYA 
TISTA AND DIHANG ASSAM HIMALAYA 
 
 
  
      ANGARA LAND 
   GONDWANA LAND 
    HIMADRI 
  HIMANCHAL 
     SHIVALIK 
The longitudinal valley which lies between Lesser Himalayas and Shiwalik is known 
as Duns. Ex. - Dehra Dun , Kotli Duns,Patli Dun etc. 
 
 
 
 
 
 
 
PURVACHAL(EASTERN HILLS ):BEYOND THE DIHANG GORGE , IT BEND SHARPLY TO THE 
SOUTH AND SPREAD ALONG THE EASTERN BOUNDARY.THESE ARE COMPOSED OF STRONG 
SANDSTONE AND ARE COVERED WITH DENCE FOREST.THEY ARE OF MEDIUM HEIGHT. 
Page 2


                    NOTES :PHYSICAL FEATURES OF INDIA 
               OLDEST LANDMASS: GONDWANA LAND 
             PANGEAU 
    HIMALAYAN MOUNTAINS: 
? These are young and structurally fold mountains. These are the loftiest and one of the 
most rugged mountains barriers of the world. 
? DISTANCE : 2400 km (forms an arc) ; WIDTH-400km(in Kashmir)-150km(in Anu.Pra) 
? It is composed of Granite. It is perennial snow bound and glaciers desend. 
 
HIMALAYAN MOUNTAINS 
 
HIMADRI (GREATER OR INNER HIMALAYA) 
? It contains all the prominent peaks. 
? These are the most loftiest mountain ranges and are always snowbound. 
? AVARAGE HEIGHT =6000m -6100m 
HIMANCHAL ( LESSER HIMALAYA) 
? AVARAGE HEIGHT=3700m-4500m ; AVARAGE WIDTH=50km(rugged mount.) 
? It is well knowned for its  hill stations and beautiful valleys. 
            SHIWALIK( OUTER HIMALAYA OR SUB-HIMALAYA) 
? AVARAGE HEIGHT =900m-1100m;AVARGE WIDTH=10km-50km 
? It is made of unconsolidated sediments  and  are prone to earthquakes. 
? These valleys are covered with alluvium and thick gravels and are youngest. 
 
 
 
 
INDUS AND SATLUJ PUNJAB , KASHMIR, HIMANCHAL HIMALAYA 
SATLUJ AND KALI KUMAON HIMALAYA 
KALI AND TISTA NEPAL HIMALAYA 
TISTA AND DIHANG ASSAM HIMALAYA 
 
 
  
      ANGARA LAND 
   GONDWANA LAND 
    HIMADRI 
  HIMANCHAL 
     SHIVALIK 
The longitudinal valley which lies between Lesser Himalayas and Shiwalik is known 
as Duns. Ex. - Dehra Dun , Kotli Duns,Patli Dun etc. 
 
 
 
 
 
 
 
PURVACHAL(EASTERN HILLS ):BEYOND THE DIHANG GORGE , IT BEND SHARPLY TO THE 
SOUTH AND SPREAD ALONG THE EASTERN BOUNDARY.THESE ARE COMPOSED OF STRONG 
SANDSTONE AND ARE COVERED WITH DENCE FOREST.THEY ARE OF MEDIUM HEIGHT. 
THE NORTHERN PLAIN : 
? This is made up of fertile silt called ALLUVIUM. This silt is brought by 
Himalayan Rivers. 
? LENGTH=2400km , WIDTH=240km-320 km, AREA=7 lakh sq. km 
FORMATION OF NORTHERN PLAINS: 
? Result of deposition of silt into the Tethys. 
? By erosion, large amount of silt is carried away by rivers and other agents of 
denudation. 
? DIVISION ON BASIS OF RELIEF : 
 
 
i) BHABAR 
Bhabar  is in form of a narrow belt. 
It is covered with pebbles. It lies 
parallel to slope of  SHIWALIKS. 
WIDTH=8 T0 16 km 
 
ii)TARAI 
It lies in the south of bhabar. It is wet 
and marshy. It has a thick forest and 
a variety of wildlife. 
 
iii)BHANGAR 
The older alluvium of the plain is 
called Bhangar. These lies above  the 
flood plain. Then present a Terrence 
like feature 
 
iv)KHADAR 
It is the younger alluvium of the flood 
plain. This region contains deposits 
of kankar. 
 
 
           
 
  
 
DIFFERENCE             FACTOR                        BHANGAR                               KHADAR 
         (i)                AGE IT IS OLD ALLUVIUM,OLDER IN AGE. IT IS NEW ALLUVIUM ,YOUNGER IN AGE. 
        (ii)      COMPOSITION IT OFTEN CONTAINS KANKAR OR 
MODULE OF CALCIM CARBONATE. 
IT IS FINER,MORE SANDY AND FREE FROM 
KANKAR MODULES. 
        (iiii)         FERTILITY IT IS NOT  RENEWED FREQUENTLY 
.HENCE IT IS LESS FERTILE. 
IT  IS RENEWED FREQUENTLY .HENCE IT IS 
MORE FERTILE. 
        (iv)       LOCATION IT IS FOUND AWAY FROM RIVER AT A 
HIGHER GROUND LEVEL. 
IT IS FOUND NEAR RIVERS ,DELTAS AND IN 
FLOOD PLAIN. 
DOAB: do + ad /(two) +(river) ,PUNJAB:(punj)+(ab)/(five)+(river) 
PUNJAB PLAINS:IT IS THE WESTERN PART OF NORTHERN PLAINS.IT IS FORMED BY 
INDUS AND ITS TRIBUTARIES.IT’S LARGER PART LIES IN PAKISTHAN. 
GANGA PLAIN:THE GANGA PLAIN EXTEND FROM GHAGGAR TO TISTA RIVER. 
BRAHMAPUTRA PLAINS:IT LIES IN THE EAST OF GANGA PLAIN. 
Page 3


                    NOTES :PHYSICAL FEATURES OF INDIA 
               OLDEST LANDMASS: GONDWANA LAND 
             PANGEAU 
    HIMALAYAN MOUNTAINS: 
? These are young and structurally fold mountains. These are the loftiest and one of the 
most rugged mountains barriers of the world. 
? DISTANCE : 2400 km (forms an arc) ; WIDTH-400km(in Kashmir)-150km(in Anu.Pra) 
? It is composed of Granite. It is perennial snow bound and glaciers desend. 
 
HIMALAYAN MOUNTAINS 
 
HIMADRI (GREATER OR INNER HIMALAYA) 
? It contains all the prominent peaks. 
? These are the most loftiest mountain ranges and are always snowbound. 
? AVARAGE HEIGHT =6000m -6100m 
HIMANCHAL ( LESSER HIMALAYA) 
? AVARAGE HEIGHT=3700m-4500m ; AVARAGE WIDTH=50km(rugged mount.) 
? It is well knowned for its  hill stations and beautiful valleys. 
            SHIWALIK( OUTER HIMALAYA OR SUB-HIMALAYA) 
? AVARAGE HEIGHT =900m-1100m;AVARGE WIDTH=10km-50km 
? It is made of unconsolidated sediments  and  are prone to earthquakes. 
? These valleys are covered with alluvium and thick gravels and are youngest. 
 
 
 
 
INDUS AND SATLUJ PUNJAB , KASHMIR, HIMANCHAL HIMALAYA 
SATLUJ AND KALI KUMAON HIMALAYA 
KALI AND TISTA NEPAL HIMALAYA 
TISTA AND DIHANG ASSAM HIMALAYA 
 
 
  
      ANGARA LAND 
   GONDWANA LAND 
    HIMADRI 
  HIMANCHAL 
     SHIVALIK 
The longitudinal valley which lies between Lesser Himalayas and Shiwalik is known 
as Duns. Ex. - Dehra Dun , Kotli Duns,Patli Dun etc. 
 
 
 
 
 
 
 
PURVACHAL(EASTERN HILLS ):BEYOND THE DIHANG GORGE , IT BEND SHARPLY TO THE 
SOUTH AND SPREAD ALONG THE EASTERN BOUNDARY.THESE ARE COMPOSED OF STRONG 
SANDSTONE AND ARE COVERED WITH DENCE FOREST.THEY ARE OF MEDIUM HEIGHT. 
THE NORTHERN PLAIN : 
? This is made up of fertile silt called ALLUVIUM. This silt is brought by 
Himalayan Rivers. 
? LENGTH=2400km , WIDTH=240km-320 km, AREA=7 lakh sq. km 
FORMATION OF NORTHERN PLAINS: 
? Result of deposition of silt into the Tethys. 
? By erosion, large amount of silt is carried away by rivers and other agents of 
denudation. 
? DIVISION ON BASIS OF RELIEF : 
 
 
i) BHABAR 
Bhabar  is in form of a narrow belt. 
It is covered with pebbles. It lies 
parallel to slope of  SHIWALIKS. 
WIDTH=8 T0 16 km 
 
ii)TARAI 
It lies in the south of bhabar. It is wet 
and marshy. It has a thick forest and 
a variety of wildlife. 
 
iii)BHANGAR 
The older alluvium of the plain is 
called Bhangar. These lies above  the 
flood plain. Then present a Terrence 
like feature 
 
iv)KHADAR 
It is the younger alluvium of the flood 
plain. This region contains deposits 
of kankar. 
 
 
           
 
  
 
DIFFERENCE             FACTOR                        BHANGAR                               KHADAR 
         (i)                AGE IT IS OLD ALLUVIUM,OLDER IN AGE. IT IS NEW ALLUVIUM ,YOUNGER IN AGE. 
        (ii)      COMPOSITION IT OFTEN CONTAINS KANKAR OR 
MODULE OF CALCIM CARBONATE. 
IT IS FINER,MORE SANDY AND FREE FROM 
KANKAR MODULES. 
        (iiii)         FERTILITY IT IS NOT  RENEWED FREQUENTLY 
.HENCE IT IS LESS FERTILE. 
IT  IS RENEWED FREQUENTLY .HENCE IT IS 
MORE FERTILE. 
        (iv)       LOCATION IT IS FOUND AWAY FROM RIVER AT A 
HIGHER GROUND LEVEL. 
IT IS FOUND NEAR RIVERS ,DELTAS AND IN 
FLOOD PLAIN. 
DOAB: do + ad /(two) +(river) ,PUNJAB:(punj)+(ab)/(five)+(river) 
PUNJAB PLAINS:IT IS THE WESTERN PART OF NORTHERN PLAINS.IT IS FORMED BY 
INDUS AND ITS TRIBUTARIES.IT’S LARGER PART LIES IN PAKISTHAN. 
GANGA PLAIN:THE GANGA PLAIN EXTEND FROM GHAGGAR TO TISTA RIVER. 
BRAHMAPUTRA PLAINS:IT LIES IN THE EAST OF GANGA PLAIN. 
                                                                       THE INDIAN DESERT 
? IT IS A SANDY PLAIN COVERED WITH SAND DUNES. 
? IT RECEIVES VERY LOW RAINFALL, ALMOST BELOW IT 150mm per year. 
? IT HAS AN ARID CLIMATE WITH LOW VEGETATION. 
? DURING RAINY SEASON SOME STREAM APPEAR BUT THEY DISAPPEAR AFTER SOME TIME. 
? LUNI IS THE LARGEST RIVER. 
 
                                  THE  COASTAL  PLAINS 
WESTERN COASTAL PLAINS 
? WIDTH =40km, (FROM GUJARAT TO KANYAKUMARI)(BET. ARABIAN SEA AND WESTERN GHATS) 
? KONKAN-NORTHMOST PORTION,KANNAD-CENETRAL PORTION,MALABAR-SOUTHMOST PORTION 
? IT HAS SALT WATER LAKE CALLED LAGOON,SAND BARS,PLACID BACKWATER,NATURAL HARBOUR AND 
FAST FLOWING RIVERS. 
EASTERN COASTAL PLAIN 
? WIDTH=60 TO 100 km,(BET. BAY OF BENGAL AND EASTERN GHATS)(FROM W.BENGAL TO KANYAKUMARI) 
? NORTH CICARS-NORTHERN AREAS OF ANDHRA PRADESH,COROMANDEL COAST-SOUTHERN POTION(T.N.) 
? FOUR IMPORTANT DELTA-KRISHNA,GODAVARI,KAVERI AND MAHANADI. 
 
                        
                                                        THE ISLAND 
             LAKSHADWEEP           ANDMAN & NICOBAR ISLAND 
? THEY ARE SMALLER GROUP OF ISLAND. 
? EARLIER IIT WAS KNOWN AS 
LACCADIVE,MINICOY AND AMINDIVE. 
? AREA=32 sq. km 
? IT IS COMPOSED OF SMALL CORAL ISLAND. 
? HEADQUATER-KAVARATI ISLAND 
 
? THEY ARE BIGGER GROUP OF ISLAND. 
? SOME ISLANDS ARE LOCATED ON SUMERGED 
HILLS AND VOLCANIC ORIGINS. 
? IT HAS THE ONLY ACTIVE VOLCANO OF INDIA. 
? IT HAS EQUATORIAL CLIMATE AND THICK 
FOREST. 
 
 
                  
 
 
 
 
 
 
NOTE: BARCHAN ARE CRESCENT SHAPED DUNES 
CHILIKA LAKE IS THE LARGEST SALTWATER LAKE IN INDIA.IT IS IN ORRISSA. 
                                                                CORALS 
CORAL POLYPS ARE SHORT- LIVED MICROSCOPIC ORGANISM, WHICH LIVE 
IN COLONIES.THEY FLORISH IN SHALLOW,MUD FREE AND WARM 
WATER.THEY SECRETE CALCIUM CARBONATE.THEY ARE OF THREE TYPES-
BARRIER REEF,FRINGING REEF AND ATOLLS.ATOLLS ARE CIRCULAR OR 
HORSE SHOE  SHAPED CORAL REEF. 
Page 4


                    NOTES :PHYSICAL FEATURES OF INDIA 
               OLDEST LANDMASS: GONDWANA LAND 
             PANGEAU 
    HIMALAYAN MOUNTAINS: 
? These are young and structurally fold mountains. These are the loftiest and one of the 
most rugged mountains barriers of the world. 
? DISTANCE : 2400 km (forms an arc) ; WIDTH-400km(in Kashmir)-150km(in Anu.Pra) 
? It is composed of Granite. It is perennial snow bound and glaciers desend. 
 
HIMALAYAN MOUNTAINS 
 
HIMADRI (GREATER OR INNER HIMALAYA) 
? It contains all the prominent peaks. 
? These are the most loftiest mountain ranges and are always snowbound. 
? AVARAGE HEIGHT =6000m -6100m 
HIMANCHAL ( LESSER HIMALAYA) 
? AVARAGE HEIGHT=3700m-4500m ; AVARAGE WIDTH=50km(rugged mount.) 
? It is well knowned for its  hill stations and beautiful valleys. 
            SHIWALIK( OUTER HIMALAYA OR SUB-HIMALAYA) 
? AVARAGE HEIGHT =900m-1100m;AVARGE WIDTH=10km-50km 
? It is made of unconsolidated sediments  and  are prone to earthquakes. 
? These valleys are covered with alluvium and thick gravels and are youngest. 
 
 
 
 
INDUS AND SATLUJ PUNJAB , KASHMIR, HIMANCHAL HIMALAYA 
SATLUJ AND KALI KUMAON HIMALAYA 
KALI AND TISTA NEPAL HIMALAYA 
TISTA AND DIHANG ASSAM HIMALAYA 
 
 
  
      ANGARA LAND 
   GONDWANA LAND 
    HIMADRI 
  HIMANCHAL 
     SHIVALIK 
The longitudinal valley which lies between Lesser Himalayas and Shiwalik is known 
as Duns. Ex. - Dehra Dun , Kotli Duns,Patli Dun etc. 
 
 
 
 
 
 
 
PURVACHAL(EASTERN HILLS ):BEYOND THE DIHANG GORGE , IT BEND SHARPLY TO THE 
SOUTH AND SPREAD ALONG THE EASTERN BOUNDARY.THESE ARE COMPOSED OF STRONG 
SANDSTONE AND ARE COVERED WITH DENCE FOREST.THEY ARE OF MEDIUM HEIGHT. 
THE NORTHERN PLAIN : 
? This is made up of fertile silt called ALLUVIUM. This silt is brought by 
Himalayan Rivers. 
? LENGTH=2400km , WIDTH=240km-320 km, AREA=7 lakh sq. km 
FORMATION OF NORTHERN PLAINS: 
? Result of deposition of silt into the Tethys. 
? By erosion, large amount of silt is carried away by rivers and other agents of 
denudation. 
? DIVISION ON BASIS OF RELIEF : 
 
 
i) BHABAR 
Bhabar  is in form of a narrow belt. 
It is covered with pebbles. It lies 
parallel to slope of  SHIWALIKS. 
WIDTH=8 T0 16 km 
 
ii)TARAI 
It lies in the south of bhabar. It is wet 
and marshy. It has a thick forest and 
a variety of wildlife. 
 
iii)BHANGAR 
The older alluvium of the plain is 
called Bhangar. These lies above  the 
flood plain. Then present a Terrence 
like feature 
 
iv)KHADAR 
It is the younger alluvium of the flood 
plain. This region contains deposits 
of kankar. 
 
 
           
 
  
 
DIFFERENCE             FACTOR                        BHANGAR                               KHADAR 
         (i)                AGE IT IS OLD ALLUVIUM,OLDER IN AGE. IT IS NEW ALLUVIUM ,YOUNGER IN AGE. 
        (ii)      COMPOSITION IT OFTEN CONTAINS KANKAR OR 
MODULE OF CALCIM CARBONATE. 
IT IS FINER,MORE SANDY AND FREE FROM 
KANKAR MODULES. 
        (iiii)         FERTILITY IT IS NOT  RENEWED FREQUENTLY 
.HENCE IT IS LESS FERTILE. 
IT  IS RENEWED FREQUENTLY .HENCE IT IS 
MORE FERTILE. 
        (iv)       LOCATION IT IS FOUND AWAY FROM RIVER AT A 
HIGHER GROUND LEVEL. 
IT IS FOUND NEAR RIVERS ,DELTAS AND IN 
FLOOD PLAIN. 
DOAB: do + ad /(two) +(river) ,PUNJAB:(punj)+(ab)/(five)+(river) 
PUNJAB PLAINS:IT IS THE WESTERN PART OF NORTHERN PLAINS.IT IS FORMED BY 
INDUS AND ITS TRIBUTARIES.IT’S LARGER PART LIES IN PAKISTHAN. 
GANGA PLAIN:THE GANGA PLAIN EXTEND FROM GHAGGAR TO TISTA RIVER. 
BRAHMAPUTRA PLAINS:IT LIES IN THE EAST OF GANGA PLAIN. 
                                                                       THE INDIAN DESERT 
? IT IS A SANDY PLAIN COVERED WITH SAND DUNES. 
? IT RECEIVES VERY LOW RAINFALL, ALMOST BELOW IT 150mm per year. 
? IT HAS AN ARID CLIMATE WITH LOW VEGETATION. 
? DURING RAINY SEASON SOME STREAM APPEAR BUT THEY DISAPPEAR AFTER SOME TIME. 
? LUNI IS THE LARGEST RIVER. 
 
                                  THE  COASTAL  PLAINS 
WESTERN COASTAL PLAINS 
? WIDTH =40km, (FROM GUJARAT TO KANYAKUMARI)(BET. ARABIAN SEA AND WESTERN GHATS) 
? KONKAN-NORTHMOST PORTION,KANNAD-CENETRAL PORTION,MALABAR-SOUTHMOST PORTION 
? IT HAS SALT WATER LAKE CALLED LAGOON,SAND BARS,PLACID BACKWATER,NATURAL HARBOUR AND 
FAST FLOWING RIVERS. 
EASTERN COASTAL PLAIN 
? WIDTH=60 TO 100 km,(BET. BAY OF BENGAL AND EASTERN GHATS)(FROM W.BENGAL TO KANYAKUMARI) 
? NORTH CICARS-NORTHERN AREAS OF ANDHRA PRADESH,COROMANDEL COAST-SOUTHERN POTION(T.N.) 
? FOUR IMPORTANT DELTA-KRISHNA,GODAVARI,KAVERI AND MAHANADI. 
 
                        
                                                        THE ISLAND 
             LAKSHADWEEP           ANDMAN & NICOBAR ISLAND 
? THEY ARE SMALLER GROUP OF ISLAND. 
? EARLIER IIT WAS KNOWN AS 
LACCADIVE,MINICOY AND AMINDIVE. 
? AREA=32 sq. km 
? IT IS COMPOSED OF SMALL CORAL ISLAND. 
? HEADQUATER-KAVARATI ISLAND 
 
? THEY ARE BIGGER GROUP OF ISLAND. 
? SOME ISLANDS ARE LOCATED ON SUMERGED 
HILLS AND VOLCANIC ORIGINS. 
? IT HAS THE ONLY ACTIVE VOLCANO OF INDIA. 
? IT HAS EQUATORIAL CLIMATE AND THICK 
FOREST. 
 
 
                  
 
 
 
 
 
 
NOTE: BARCHAN ARE CRESCENT SHAPED DUNES 
CHILIKA LAKE IS THE LARGEST SALTWATER LAKE IN INDIA.IT IS IN ORRISSA. 
                                                                CORALS 
CORAL POLYPS ARE SHORT- LIVED MICROSCOPIC ORGANISM, WHICH LIVE 
IN COLONIES.THEY FLORISH IN SHALLOW,MUD FREE AND WARM 
WATER.THEY SECRETE CALCIUM CARBONATE.THEY ARE OF THREE TYPES-
BARRIER REEF,FRINGING REEF AND ATOLLS.ATOLLS ARE CIRCULAR OR 
HORSE SHOE  SHAPED CORAL REEF. 
Bonus Facts: 
a] In the last century, the east coast of the United States has moved about 8 ft. further away from Europe. 
b]The fossils of sea and coastal creatures can still be found in the Himalayas, as it was once two coast lines 
that merged together. These fossils not only provide evidence that the Himalayas once existed on a coastline, 
but also information about climate change and plate movement. 
c] The name for the Himalayas comes from the Sanskrit for snow and dwelling: “him” and “alaya” 
respectively.  Essentially, the home of the snow. 
d] Mount Everest is named after one of the Surveyor Generals of India, George Everest.  It was not, 
however, Everest who first survey the mountain, but Andrew Waugh who took over the role of Surveyor 
General after Everest.  Waugh thought it would be a good idea to name the mountain after his predecessor.  
Everest didn’t like the idea, but he was overruled and his name was eventually adopted for the mountain by 
the Royal Geographical Society in 1865. 
e] While Everest is generally considered the tallest mountain on Earth because it reaches the highest 
elevation, some argue that this should not be the measure used, but rather the tallest from the base to peak.  
In that case, Hawaii’s Mauna Kea would be the tallest at about 10,200 metres from its base on the ocean 
floor to peak at 4,205 metres above sea level. 
f] Sir Edmund Hillary and Tenzing Norgay, his Sherpa guide, became the first people to successfully climb 
to the peak of Mount Everest in 1953. Before Hillary, several dozen attempts had been undertaken to climb 
to the peak since 1921. Since then, nearly 3000 people have accomplished the same feat and around 200 
have died trying. 
g] The Himalayas serve as a “climatic divide” as well as a physical barrier between India and the rest of the 
continent. They prevent cold winter winds from entering into India in the winter, making India warmer than 
other regions along the same lines of latitude at that same time of the year. Similarly, they prevent the 
southern monsoon winds from taking moisture across the border to Tibet; the result is India gets far more 
precipitation than the relatively more arid Tibet. 
h] The Himalayas are home to some interesting creatures: clouded leopards, Asiatic black bears, tahrs, and 
langurs to name a few. Snow leopards and brown bears have adapted to live at higher elevations. 
Unfortunately, due to human interest and interference, many species that call the Himalayas home are dying 
out, such as the Indian rhinoceros and the Kashmir stag. 
i] While you might not think the icy mountain peaks of the Himalayas that you see in photos would be 
conducive to growing much of anything, the little hidden valleys of the Himalaya range are actually 
depended upon for food production. Farmers grow apples, cherries, grapes, oranges, pears, almonds, 
walnuts, tea, and a variety of herbs and spices in and around the range. 
j]The Himalayas are notable not only for their size, but for their structure. The Himalayas are considered 
fold mountains as they consist of a series of jagged peaks that are mostly parallel, as though they have been 
Page 5


                    NOTES :PHYSICAL FEATURES OF INDIA 
               OLDEST LANDMASS: GONDWANA LAND 
             PANGEAU 
    HIMALAYAN MOUNTAINS: 
? These are young and structurally fold mountains. These are the loftiest and one of the 
most rugged mountains barriers of the world. 
? DISTANCE : 2400 km (forms an arc) ; WIDTH-400km(in Kashmir)-150km(in Anu.Pra) 
? It is composed of Granite. It is perennial snow bound and glaciers desend. 
 
HIMALAYAN MOUNTAINS 
 
HIMADRI (GREATER OR INNER HIMALAYA) 
? It contains all the prominent peaks. 
? These are the most loftiest mountain ranges and are always snowbound. 
? AVARAGE HEIGHT =6000m -6100m 
HIMANCHAL ( LESSER HIMALAYA) 
? AVARAGE HEIGHT=3700m-4500m ; AVARAGE WIDTH=50km(rugged mount.) 
? It is well knowned for its  hill stations and beautiful valleys. 
            SHIWALIK( OUTER HIMALAYA OR SUB-HIMALAYA) 
? AVARAGE HEIGHT =900m-1100m;AVARGE WIDTH=10km-50km 
? It is made of unconsolidated sediments  and  are prone to earthquakes. 
? These valleys are covered with alluvium and thick gravels and are youngest. 
 
 
 
 
INDUS AND SATLUJ PUNJAB , KASHMIR, HIMANCHAL HIMALAYA 
SATLUJ AND KALI KUMAON HIMALAYA 
KALI AND TISTA NEPAL HIMALAYA 
TISTA AND DIHANG ASSAM HIMALAYA 
 
 
  
      ANGARA LAND 
   GONDWANA LAND 
    HIMADRI 
  HIMANCHAL 
     SHIVALIK 
The longitudinal valley which lies between Lesser Himalayas and Shiwalik is known 
as Duns. Ex. - Dehra Dun , Kotli Duns,Patli Dun etc. 
 
 
 
 
 
 
 
PURVACHAL(EASTERN HILLS ):BEYOND THE DIHANG GORGE , IT BEND SHARPLY TO THE 
SOUTH AND SPREAD ALONG THE EASTERN BOUNDARY.THESE ARE COMPOSED OF STRONG 
SANDSTONE AND ARE COVERED WITH DENCE FOREST.THEY ARE OF MEDIUM HEIGHT. 
THE NORTHERN PLAIN : 
? This is made up of fertile silt called ALLUVIUM. This silt is brought by 
Himalayan Rivers. 
? LENGTH=2400km , WIDTH=240km-320 km, AREA=7 lakh sq. km 
FORMATION OF NORTHERN PLAINS: 
? Result of deposition of silt into the Tethys. 
? By erosion, large amount of silt is carried away by rivers and other agents of 
denudation. 
? DIVISION ON BASIS OF RELIEF : 
 
 
i) BHABAR 
Bhabar  is in form of a narrow belt. 
It is covered with pebbles. It lies 
parallel to slope of  SHIWALIKS. 
WIDTH=8 T0 16 km 
 
ii)TARAI 
It lies in the south of bhabar. It is wet 
and marshy. It has a thick forest and 
a variety of wildlife. 
 
iii)BHANGAR 
The older alluvium of the plain is 
called Bhangar. These lies above  the 
flood plain. Then present a Terrence 
like feature 
 
iv)KHADAR 
It is the younger alluvium of the flood 
plain. This region contains deposits 
of kankar. 
 
 
           
 
  
 
DIFFERENCE             FACTOR                        BHANGAR                               KHADAR 
         (i)                AGE IT IS OLD ALLUVIUM,OLDER IN AGE. IT IS NEW ALLUVIUM ,YOUNGER IN AGE. 
        (ii)      COMPOSITION IT OFTEN CONTAINS KANKAR OR 
MODULE OF CALCIM CARBONATE. 
IT IS FINER,MORE SANDY AND FREE FROM 
KANKAR MODULES. 
        (iiii)         FERTILITY IT IS NOT  RENEWED FREQUENTLY 
.HENCE IT IS LESS FERTILE. 
IT  IS RENEWED FREQUENTLY .HENCE IT IS 
MORE FERTILE. 
        (iv)       LOCATION IT IS FOUND AWAY FROM RIVER AT A 
HIGHER GROUND LEVEL. 
IT IS FOUND NEAR RIVERS ,DELTAS AND IN 
FLOOD PLAIN. 
DOAB: do + ad /(two) +(river) ,PUNJAB:(punj)+(ab)/(five)+(river) 
PUNJAB PLAINS:IT IS THE WESTERN PART OF NORTHERN PLAINS.IT IS FORMED BY 
INDUS AND ITS TRIBUTARIES.IT’S LARGER PART LIES IN PAKISTHAN. 
GANGA PLAIN:THE GANGA PLAIN EXTEND FROM GHAGGAR TO TISTA RIVER. 
BRAHMAPUTRA PLAINS:IT LIES IN THE EAST OF GANGA PLAIN. 
                                                                       THE INDIAN DESERT 
? IT IS A SANDY PLAIN COVERED WITH SAND DUNES. 
? IT RECEIVES VERY LOW RAINFALL, ALMOST BELOW IT 150mm per year. 
? IT HAS AN ARID CLIMATE WITH LOW VEGETATION. 
? DURING RAINY SEASON SOME STREAM APPEAR BUT THEY DISAPPEAR AFTER SOME TIME. 
? LUNI IS THE LARGEST RIVER. 
 
                                  THE  COASTAL  PLAINS 
WESTERN COASTAL PLAINS 
? WIDTH =40km, (FROM GUJARAT TO KANYAKUMARI)(BET. ARABIAN SEA AND WESTERN GHATS) 
? KONKAN-NORTHMOST PORTION,KANNAD-CENETRAL PORTION,MALABAR-SOUTHMOST PORTION 
? IT HAS SALT WATER LAKE CALLED LAGOON,SAND BARS,PLACID BACKWATER,NATURAL HARBOUR AND 
FAST FLOWING RIVERS. 
EASTERN COASTAL PLAIN 
? WIDTH=60 TO 100 km,(BET. BAY OF BENGAL AND EASTERN GHATS)(FROM W.BENGAL TO KANYAKUMARI) 
? NORTH CICARS-NORTHERN AREAS OF ANDHRA PRADESH,COROMANDEL COAST-SOUTHERN POTION(T.N.) 
? FOUR IMPORTANT DELTA-KRISHNA,GODAVARI,KAVERI AND MAHANADI. 
 
                        
                                                        THE ISLAND 
             LAKSHADWEEP           ANDMAN & NICOBAR ISLAND 
? THEY ARE SMALLER GROUP OF ISLAND. 
? EARLIER IIT WAS KNOWN AS 
LACCADIVE,MINICOY AND AMINDIVE. 
? AREA=32 sq. km 
? IT IS COMPOSED OF SMALL CORAL ISLAND. 
? HEADQUATER-KAVARATI ISLAND 
 
? THEY ARE BIGGER GROUP OF ISLAND. 
? SOME ISLANDS ARE LOCATED ON SUMERGED 
HILLS AND VOLCANIC ORIGINS. 
? IT HAS THE ONLY ACTIVE VOLCANO OF INDIA. 
? IT HAS EQUATORIAL CLIMATE AND THICK 
FOREST. 
 
 
                  
 
 
 
 
 
 
NOTE: BARCHAN ARE CRESCENT SHAPED DUNES 
CHILIKA LAKE IS THE LARGEST SALTWATER LAKE IN INDIA.IT IS IN ORRISSA. 
                                                                CORALS 
CORAL POLYPS ARE SHORT- LIVED MICROSCOPIC ORGANISM, WHICH LIVE 
IN COLONIES.THEY FLORISH IN SHALLOW,MUD FREE AND WARM 
WATER.THEY SECRETE CALCIUM CARBONATE.THEY ARE OF THREE TYPES-
BARRIER REEF,FRINGING REEF AND ATOLLS.ATOLLS ARE CIRCULAR OR 
HORSE SHOE  SHAPED CORAL REEF. 
Bonus Facts: 
a] In the last century, the east coast of the United States has moved about 8 ft. further away from Europe. 
b]The fossils of sea and coastal creatures can still be found in the Himalayas, as it was once two coast lines 
that merged together. These fossils not only provide evidence that the Himalayas once existed on a coastline, 
but also information about climate change and plate movement. 
c] The name for the Himalayas comes from the Sanskrit for snow and dwelling: “him” and “alaya” 
respectively.  Essentially, the home of the snow. 
d] Mount Everest is named after one of the Surveyor Generals of India, George Everest.  It was not, 
however, Everest who first survey the mountain, but Andrew Waugh who took over the role of Surveyor 
General after Everest.  Waugh thought it would be a good idea to name the mountain after his predecessor.  
Everest didn’t like the idea, but he was overruled and his name was eventually adopted for the mountain by 
the Royal Geographical Society in 1865. 
e] While Everest is generally considered the tallest mountain on Earth because it reaches the highest 
elevation, some argue that this should not be the measure used, but rather the tallest from the base to peak.  
In that case, Hawaii’s Mauna Kea would be the tallest at about 10,200 metres from its base on the ocean 
floor to peak at 4,205 metres above sea level. 
f] Sir Edmund Hillary and Tenzing Norgay, his Sherpa guide, became the first people to successfully climb 
to the peak of Mount Everest in 1953. Before Hillary, several dozen attempts had been undertaken to climb 
to the peak since 1921. Since then, nearly 3000 people have accomplished the same feat and around 200 
have died trying. 
g] The Himalayas serve as a “climatic divide” as well as a physical barrier between India and the rest of the 
continent. They prevent cold winter winds from entering into India in the winter, making India warmer than 
other regions along the same lines of latitude at that same time of the year. Similarly, they prevent the 
southern monsoon winds from taking moisture across the border to Tibet; the result is India gets far more 
precipitation than the relatively more arid Tibet. 
h] The Himalayas are home to some interesting creatures: clouded leopards, Asiatic black bears, tahrs, and 
langurs to name a few. Snow leopards and brown bears have adapted to live at higher elevations. 
Unfortunately, due to human interest and interference, many species that call the Himalayas home are dying 
out, such as the Indian rhinoceros and the Kashmir stag. 
i] While you might not think the icy mountain peaks of the Himalayas that you see in photos would be 
conducive to growing much of anything, the little hidden valleys of the Himalaya range are actually 
depended upon for food production. Farmers grow apples, cherries, grapes, oranges, pears, almonds, 
walnuts, tea, and a variety of herbs and spices in and around the range. 
j]The Himalayas are notable not only for their size, but for their structure. The Himalayas are considered 
fold mountains as they consist of a series of jagged peaks that are mostly parallel, as though they have been 
folded over and over again. They are also home to deep ravines, glaciers, and rivers, forming a complex and 
treacherous range. 
1.  Importance of Himalayas: -  
a] Provides water to a large part of the country as many rivers originate from the glaciers present here. 
b] It contains varied flora and is also the habitat to various fauna. 
c] They are an important climatic divide – they check the cold polar winds coming from the north from 
entering India thus making its climate moderate. Also they do not allow the monsoon winds to cross over to 
the north which helps in providing the much needed rainfall to the country. 
d] The rivers bring with them the much needed fertile soil from the mountains and deposit it in the plains 
making them fertile for growing crops. 
e] The Himalayan mountain system offers numerous sites suitable for generation of hydel power. 
f] Throughout history, foreign invaders have never entered India from the northern side due to their height 
thus making the Himalayas important from the defence point of view. 
g] Himalayas are known for their scenic and aesthetic beauty all over the world and offer cool and 
invigorating climate from the scorching summer heat in the rest of the country. 
sanctified shrines which are considered to be the abodes of the Gods. Large number of pilgrims trek through 
difficult terrain to pay their reverence to these sacred shrines. Kailas, Amarnath, Badrinath, Kedarnath, 
Vaishno Devi, Jwalaji, Uttarkashi, Gangotri, Yamunotri, etc. are important places of pilgrimage. 
l] The Himalayan region contains many valuable minerals. There are vast potentialities of mineral oil in the 
tertiary rocks. Coal is found in Kashmir. Copper, lead, zinc, nickel, cobalt, antimony, tungsten, gold, silver, 
limestone, semi-precious and precious stones, gypsum and magnetite are known to occur at more than 100 
localities in the Himalayas. 
FORMATION OF HIMALAYA: 
? DUE TO THE SANWICHED OF TETHYS BY ANGARA LAND AND GONDWANA LAND. 
? THE MOVEMENT OF ANGARA LAND AND GONDWNA LAND BUCKLED UP THE SEDIMENTS INTO MIGHTY 
FOLD MOUNTAINS. 
? THESE GIANT LAND MASSES MOVE OVER EACH OTHER AND FORM A FOLD MOUNTAIN. 
       
 
                       
  
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FAQs on NOTES : PHYSICAL FEATURES OF INDIA - Class 9

1. What are the major physical features of India?
Ans. The major physical features of India include the Himalayan mountain range in the north, the Indo-Gangetic Plain, the Thar Desert in the northwest, the Western Ghats in the west, and the Eastern Ghats in the east. It also has major rivers like the Ganges, Brahmaputra, and Yamuna.
2. What is the significance of the Himalayan mountain range in India?
Ans. The Himalayan mountain range plays a significant role in India. It acts as a natural barrier, protecting the country from the cold winds of Central Asia. It is also the source of several major rivers, providing water resources for agriculture and hydropower generation. Additionally, the Himalayas attract tourists from around the world, contributing to India's tourism industry.
3. How does the Thar Desert impact the region?
Ans. The Thar Desert, located in the northwest of India, has a significant impact on the region. It is one of the hottest and driest regions in the country, with limited vegetation. The desert experiences extreme temperatures and is characterized by sand dunes. The Thar Desert influences the climate of surrounding areas, causing hot and dry conditions. It also poses challenges for agriculture and water availability in the region.
4. What role do the Western Ghats and Eastern Ghats play in India's geography?
Ans. The Western Ghats and Eastern Ghats are two major mountain ranges in India. The Western Ghats run parallel to the western coast of India, while the Eastern Ghats run parallel to the eastern coast. These mountain ranges act as barriers, influencing the climate patterns and causing variations in rainfall. They are also home to diverse flora and fauna, including several endangered species. The Western Ghats are known for their scenic beauty and contribute to the tourism industry.
5. How do the major rivers of India contribute to the country's development?
Ans. The major rivers of India, such as the Ganges, Brahmaputra, and Yamuna, play a crucial role in the country's development. They provide a source of water for irrigation, facilitating agriculture and ensuring food security. These rivers also support hydropower generation, contributing to the country's energy needs. Additionally, they serve as transportation routes, enabling the movement of goods and people. However, pollution and over-extraction of water pose challenges to their sustainable management.
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