young fold mountains, northern border, Indus → Bramhaputra
2400km arc
width - 150km(arunanchal) to 400km(kashmir)
greater height variation in east
duns(valleys between himachal, shiwalik) - dehradun, kotli dun, patli dun
sharp southward turn from dihang gorge, spread along eastern border
continuous, 6000m, asymmetrical, granite, perennial snow
mt. everest - 8848m, kanchenjunga - 8598, makalu - 8481
rugged, compressed rocks
3700-4500m, 50km width
Pir Panjal(longest), Dhaula Dhar, Mahabharat
valley of Kashmir, Kangra and Kullu Valleyrugged, compressed rocks
3700-4500m, 50km width
Pir Panjal(longest), Dhaula Dhar, Mahabharat
valley of Kashmir, Kangra and Kullu Valleyrugged, compressed rocks
3700-4500m, 50km width
Pir Panjal(longest), Dhaula Dhar, Mahabharat
valley of Kashmir, Kangra and Kullu Valley
900-1100m, 10-50km width
unconsolidated sediments brought from rivers from main himalayas
covered with gravel, aluminium
strong sandstone, densely forested, parallel ranges
patkai hills, naga hills, manipur hills, mizo hills
slow down due to gentler course, form riverine islands
split into distributaries (due to silt)
pakistan, indus, doabs
ghaggar to teesta rivers
north india, haryana, delhi, up, bihar, jharkhand, wb
bhabar - width - 8 to 16km, parallel to shiwalik, rivers deposit pebbles, disappear
terai - streams reappear, swamp, thick forest cut for migrants after partition
bhangar - old alluvium, terrace-like, kankar
khadar - renewed every year, intensive agriculture
real old, tableland, rounded hills
crystalline / igneous / metamorphic rocks, formed from drifting of Gondwana land
full of minerals, boosted industrialisation
real old, tableland, rounded hills
crystalline / igneous / metamorphic rocks, formed from drifting of Gondwana land
full of minerals, boosted industrialisation
real old, tableland, rounded hills
crystalline / igneous / metamorphic rocks, formed from drifting of Gondwana land
full of minerals, boosted industrialisation
real old, tableland, rounded hills
crystalline / igneous / metamorphic rocks, formed from drifting of Gondwana land
full of minerals, boosted industrialisation
north of narmada
covers malwa plateau
vindhya bounded by satpura on south, aravali on northwest
western extension merges with rajasthan desert
rivers flow southwest to northeast- chambal, sind, betwa, ken
wider in west
eastward extension - bundelkhand, baghelkhan (even more east → chhotanagpur(drained by damodar))
parallel to western coast
continuous
thal, bhor, pal ghats
900-1600m, height increases north to south
orographic rain- moist winds rise along its slope
anai mudi(2,695m), doda betta(2,637m)
dissected by rivers draining into BoB (not continuous)
600m
mahanadi valley(north) to nilgiris(south)
highest peak - mahendragiri(1,501m)
southeastern extension - shevroy hills, javadi hills
ooty = kodaikanal = udagamandalam
inverted triangle, satpura as base
eastern extension - mahadev, kaimur hills, maikal range
higher in west
northeastern extension - meghalaya, karbi-anglong plateau, north cachar hills
separated from chhotanagpur by a fault
hill ranges(west to east) - Garo, Khasi, Jaintia
aravali hills - northern, northwestern boundary, ‘broken hills’, gujarat(southwest) to delhi(northeast)
western margin of aravali
sandy plain, sand dune, 150mm rainfall, arid, streams only in monsoon, luni river
barchans(crescent-shaped dunes), longitudinal dunes near indo-pak
konkan (mumbai-goa)
kannad plain
malabar coast
northern circar
coromandel coast
mahanadi, godavari, krishna, kaveri rivers form deltas
lake chilika(odisha) - largest saltwater lake in india
coral island, 32 km², kavaratti island(hq), pitti island(bird sanctuary)
laccaadive, minicoy and amindive- renamed in 1973
bigger, more scattered
andaman(north), nicobar(south)
elevated portion of submarine himalayas
densely forested
barren island - india’s only active volcano
Physical Features of India - GEO CLASS 9
young fold mountains, northern border, Indus → Bramhaputra
2400km arc
width - 150km(arunanchal) to 400km(kashmir)
greater height variation in east
duns(valleys between himachal, shiwalik) - dehradun, kotli dun, patli dun
sharp southward turn from dihang gorge, spread along eastern border
continuous, 6000m, asymmetrical, granite, perennial snow
mt. everest - 8848m, kanchenjunga - 8598, makalu - 8481
rugged, compressed rocks
3700-4500m, 50km width
Pir Panjal(longest), Dhaula Dhar, Mahabharat
valley of Kashmir, Kangra and Kullu Valleyrugged, compressed rocks
3700-4500m, 50km width
Pir Panjal(longest), Dhaula Dhar, Mahabharat
valley of Kashmir, Kangra and Kullu Valleyrugged, compressed rocks
3700-4500m, 50km width
Pir Panjal(longest), Dhaula Dhar, Mahabharat
valley of Kashmir, Kangra and Kullu Valley
900-1100m, 10-50km width
unconsolidated sediments brought from rivers from main himalayas
covered with gravel, aluminium
strong sandstone, densely forested, parallel ranges
patkai hills, naga hills, manipur hills, mizo hills
slow down due to gentler course, form riverine islands
split into distributaries (due to silt)
pakistan, indus, doabs
ghaggar to teesta rivers
north india, haryana, delhi, up, bihar, jharkhand, wb
bhabar - width - 8 to 16km, parallel to shiwalik, rivers deposit pebbles, disappear
terai - streams reappear, swamp, thick forest cut for migrants after partition
bhangar - old alluvium, terrace-like, kankar
khadar - renewed every year, intensive agriculture
real old, tableland, rounded hills
crystalline / igneous / metamorphic rocks, formed from drifting of Gondwana land
full of minerals, boosted industrialisation
real old, tableland, rounded hills
crystalline / igneous / metamorphic rocks, formed from drifting of Gondwana land
full of minerals, boosted industrialisation
real old, tableland, rounded hills
crystalline / igneous / metamorphic rocks, formed from drifting of Gondwana land
full of minerals, boosted industrialisation
real old, tableland, rounded hills
crystalline / igneous / metamorphic rocks, formed from drifting of Gondwana land
full of minerals, boosted industrialisation
north of narmada
covers malwa plateau
vindhya bounded by satpura on south, aravali on northwest
western extension merges with rajasthan desert
rivers flow southwest to northeast- chambal, sind, betwa, ken
wider in west
eastward extension - bundelkhand, baghelkhan (even more east → chhotanagpur(drained by damodar))
parallel to western coast
continuous
thal, bhor, pal ghats
900-1600m, height increases north to south
orographic rain- moist winds rise along its slope
anai mudi(2,695m), doda betta(2,637m)
dissected by rivers draining into BoB (not continuous)
600m
mahanadi valley(north) to nilgiris(south)
highest peak - mahendragiri(1,501m)
southeastern extension - shevroy hills, javadi hills
ooty = kodaikanal = udagamandalam
inverted triangle, satpura as base
eastern extension - mahadev, kaimur hills, maikal range
higher in west
northeastern extension - meghalaya, karbi-anglong plateau, north cachar hills
separated from chhotanagpur by a fault
hill ranges(west to east) - Garo, Khasi, Jaintia
aravali hills - northern, northwestern boundary, ‘broken hills’, gujarat(southwest) to delhi(northeast)
western margin of aravali
sandy plain, sand dune, 150mm rainfall, arid, streams only in monsoon, luni river
barchans(crescent-shaped dunes), longitudinal dunes near indo-pak
konkan (mumbai-goa)
kannad plain
malabar coast
northern circar
coromandel coast
mahanadi, godavari, krishna, kaveri rivers form deltas
lake chilika(odisha) - largest saltwater lake in india
coral island, 32 km², kavaratti island(hq), pitti island(bird sanctuary)
laccaadive, minicoy and amindive- renamed in 1973
bigger, more scattered
andaman(north), nicobar(south)
elevated portion of submarine himalayas
densely forested
barren island - india’s only active volcano