By Ms Behjat Jami
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Transcript By Ms Behjat Jami
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By Ms Behjat Jami
Ms Behjat Jami
1
IMPORTANT TERMS - I
Avalanche : A huge mass of snow that moves down the slope.
Bar: Alluvial terrace an old flood plain fairly high to active flood plain.
Bet: Active flood plain.
Doab / Interfluves: Land between two rivers.
Dhand: Small salt lake.
Khaddar: Fresh Alluvium.
Karez : Irrigation Method used in Balochistan which consists of a watertunnel or a narrow under ground canal.
Landslide: landslide is the movement of rocks and soil down the
mountain slopes.
Mountain: A raised part of the earth with a peak ,steep slope attaining
over 1000 meters height than a hill.
Range : A group of mountains is called a range.
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IMPORTANT
TERMS - II
Plateau: An area of fairly level high ground.
Plain: A flat land with fertile soils used to grow
crops.
Topography: The arrangement of the natural
and artificial features of an area.
The synonyms of topography are land forms/
physical
features/
physiography
and
configuration of earth surface.
Relief: The specific forms of a physical feature.
Climate: the generalization of the all
atmospheric conditions prevailing in any area for
last 30 years.
Economic activities: All activities which are
carried out to produce something.
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NATURAL TOPOGRAPHY
&
DRAINAGE
(A multimedia presentation)
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Geographical Terms
Topography:
the study of surface of earth is
called topography (mountains,
rivers, deserts, forests etc.)
Drainage:
the natural flow of water on
earth surface is called drainage
(river, stream & waterfalls etc.)
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Geographical Terms
Relief features:
topographic features or shape of
the surface of a particular areas
or land e.g. Potwar plateau or
the Northern mountains
Alluvium:
the fine sand and minerals
which come with river water
due to soil erosion are called
alluvium
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Geographical Terms
Piedmont plain:
the foot hill area of a mountain
is called piedmont plain
Plateau:
the little high flat land above
the normal level of land is
called a plateau
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Geographical Terms
Delta:
a small ‘V’ shaped sediment
island on a river mouth is
called delta
Pass:
a passage or land route among
mountains is called a Pass
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Geographical Terms
Doab (Interfluves) :
the land b/w two rivers is called
Doab or interfluves
Bar upland:
the high land on a Doab is called
Bar upland
Alluvial terrace:
the Bar upland is also called as
Alluvial terrace
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PHYSICAL
REGIONS
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PHYSICAL REGIONS
Northern Mountains
Western Mountains
Indus Plains
Coastal Plain
Deserts
Plateaus
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Northern
Mountains
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Northern Mountains
Karakoram Range
(extreme North East)
Central Himalayas
(parallel to Karakoram range)
Outer Himalayas
(parallel to Central Himalayas)
Siwalik Range
(parallel to Outer Himalayas )
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Northern Mountains
Hindu Kush Range
(extreme North West)
Dir Range
(N-S. East of Safed Koh Range)
Swat Range
(N-S… parallel to Dir Range )
Kohistan Range
(N-S.. parallel to Swat Range )
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PEAKS
S. No
Peak
Range
Height
(m)
1
K-2
Karakoram
8611
2
Tirich
Mir
Nanga
Parbat
3
4
Hindu Kush 7690
Central
Himalayas
8126
Murkushi Karakoram
5833
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PASSES
S . No
Pass
Range Height
(m)
1
Khunjerab
K.K
4733
2
Babusar
C.H
4173
3
Dorah
H.K
4554
4
Karakoram
K.K
5575
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GLACIERS
S . No
GLACIER
Range Length
(Km)
1
Siachin
K.K
78
2
Biafo
K.K
62
3
4
Baltoro
Batura
K.K
K.K
58
59
5
Sakiz Jarab
H.K
32
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An Arial view of the Himalayas
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Ice
River
Glaciers in Karakoram Range
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KARAKORAM RANGE
Glacier Formation
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Godwin Austin
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K-2
22
Gasherbrum Peaks
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Left to right: Gasherbrum
IV, V, VI & VII 23
Rakaposhi
Height: Ms
7,788
m
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(Himalayas)
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Snow capped Range
Snow Line
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Muztagh Tower
Height: 7,273 m
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Hindu Kush
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PHYSICAL FEATURES
Snow capped; high rise peaks
Big glaciers among ranges
Source of rivers in subcontinent
Mountains passes & gorges
Foothill valleys (lakes & W. Falls)
Rain shadow area
Scarce vegetation
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CLIMATIC FEATURES
Temperature remains low
Harsh winter with heavy
snowfall
Short summer with moderate
rainfall
Sun shines everyday except
rainy days
Cool air moves slow
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Western
Mountains
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Western Mountains
All mountains in western, central
and south NWFP come under this
category
All mountains in Baluchistan
come under this category
Important mountain Ranges:
Safed Koh Range
(above Khyber pass)
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Western Mountains
Waziristan Hills
Sulaiman Range
Kirthar Range
(S-W… NWFP)
(border b/w P & NWFP)
(border b/w Sindh & Balochistan)
Toba Kakar Range
(N-W Balochistan)
Siahan Range
(Central Balochistan)
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Western Mountains
Central Makran Range
Coastal Makran Range
Central Bruhi Range
Pub Range
Hala Range
(Central Baluchistan)
(coastal Baluchistan)
(Central Baluchistan)
(S-E Baluchistan)
(S-E Balochistan)
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PEAKS (W.M)
S.No
Peak
Range
Height
(m)
1
Sikeram
Safed Koh
4760
2
Takht-eSulaiman
Sulaiman
3383
3
Kutto-joQabar
Kirthar
2097
4
Ras Koh
Ras Koh
3004
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PASSES
S.No
Pass
Range
Height
(m)
5
Khyber
Safed Koh
1067
6
Bolan
Sulaiman
989
7
Khojak Toba Kakar
8
Gomal
Waziristan
700
9
Tochi
Waziristan
580
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1312
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PHYSICAL FEATURES
Medium height mountains
Barren land and Badland
Water is scarce
Seasonal Rivers
Scattered vegetation
Natural passes
Parallel ranges
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BADLAND
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CLIMATIC FEATURES
Long summer with high
temperature
Weather extremes
Short and cold winter
Rainfall in Summer & winter
due to both Monsoon and
Western Depression
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INDUS
PLAINS
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INDUS PLAINS
The plain area which comes
under the effect of the river
Indus and its eastern tributaries
is called ‘Indus plain’ or ‘Indus
Basin’
The Indus plain starts from
South of ‘Himalayas’ and spread
over Punjab & Sindh down to
Arabian sea
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KEY
Sindh Sagar Doab
Chaj Doab
Rachna Doab
Bari Doab
Start
of
Lower
Indus
Plain
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Eastern Tributaries
Jhelum River
Chenab River
Ravi River
Sutlej River
Beas River
(India)
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THE INDUS PLAIN
Start of
Lower
Indus
Plain
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INTERFLUVES (DOAB)
Sind Sagar Doab
(b/w Indus & Jhelum)
Chaj Doab
(b/w Jhelum & Chenab)
Rachna Doab
(b/w Chenab & Ravi)
Bari Doab
(b/w Ravi & Sutluj)
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INTERFLUVES (DOAB)
CONFLUENCE
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Alluvial Terrace
( Bar Upland)
Kirana Bar in Chaj Doab
Sandal Bar in Rachna Doab
Ganji Bar in upper Bari Doab
Nili Bar in lower Bari Doab
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Physical Features
The length of the river Indus
in Pakistan is 2900Km
Lake Mansrowar is the origin
of the Indus in Tibet China
Indus passes through world
highest mountainous region
The Indus Enters in plain areas
at Kalabagh
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Physical Features
Indus plains are highly fertile
land with plenty of water
East of Slaiman-Kirthar range
is the piedmont plain
Sindh Sagar Doab (Thal desert)
is in the East of Indus
All Doabs have Bar uplands
Bari Doab have two Bar
uplands
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Drainage
River Jhelum joins river Chenab
near Jhang
River Ravi joins river Chenab
near Shorkot
River Sutluj joins river Ravi near
Alipur
Soan river in Potwar plateau
joins the river Indus at Attock
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Drainage
Water of all rivers come in one
river called Punjnad River at
Panjnad
Punjnad river joins Indus at
Mitthan Kot and enters in Sindh
In lower plain the Indus river
passes through wide plain area
up to the Arabian sea
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INDUS
DELTA
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INDUS DELTA
A delta is formed at river mouth
due to sedimentation process
done by the river
Sand and silt which come with
the river water settle in the sea
bed; slowly a small island
comes out of the surface of the
sea is called Delta
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INDUS DELTA
ARABIAN
SEA
The
Indus
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INDUS DELTA
Physical Features
It is a marsh land or wetland
It has great mangrove forest
on the whole length of the
Sindh coast
It has many fish harbors and
small ports like Keti Bandar &
Shah Bandar
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DESERTS
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DESERTS IN PAKISTAN
Pakistan has 41% desert area on
its land
Pakistan has three deserts
Thal
Desert
Thar
Desert
(Sindh Sagar Doab; western Punjab)
(South East Punjab & Eastern Sindh)
Kharan
Desert
(Central to south Balochistan)
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THAR DESERT
The Thar Desert in Pakistan is the
part of great Thar Desert in
Rajhistan India
The Thar Desert in Pakistan is further
divided into three deserts :
Cholistan Desert
(South East Punjab )
Nara Desert (North Eastern Sindh)
Tharparkar Desert (Eastern Sindh)
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PUNJAB
THAL
DESERT
CHOLISTAN
DESERT
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NARA
DESERT
SINDH
THARPARKAR
DESERT
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Sand Dunes
A result of high wind
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Sand Dunes
Pyramidal Sand Dunes
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Star Sand Dunes
indicate that winds blew in
many directions
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Stony Part of a desert
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Desert
Physical Features
Sandy, stony & rocky
Water is scarce
Land is fertile but needs water
to show its strength
Natural vegetation is scattered
with bushes, small trees &
thorny plants
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Desert
Physical Features
Sand dunes are special feature
of a desert
Sand dunes are formed due to
high wind activities
Air takes layers of sand from
one place to another place
Most of the dunes in Thar
desert are longitudinal
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Desert Vegetation
CACTUS & OTHER THORNY PLANTS
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DESERT VEGETATION
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Desert
Desertification:
Desertification is a natural
process in which a desert
covers more area due to
climatic changes
Reclamation:
Reclamation is to turn
deserted area into arable
land by human efforts
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PLATEAUS
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PLATEAUS
a plateau is a high flat land
little higher than normal level
of land
Pakistan has two plateaus:
Potwar Plateau
(North West Punjab)
Balochistan Plateau
(central Balochistan)
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POTWAR PLATEAU
Boundaries:
Jhelum River (East)
Indus River (West)
Kala Chitta Range and the
Margalla Hills (North)
Salt Range (South)
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POTWAR
PLATEAU
PUNJAB
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POTWAR PLATEAU
Physical Features
Mostly mountainous
Rugged, rocky & bare land
Scattered vegetation
Mineral deposits are large but
difficult to mine
Water is scanty
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POTWAR PLATEAU
The Soan River flows through
POTWAR PLATEAU
It starts as a branch of Jhelum
river near Muree
It joins the Indus river near
Kalabagh; Northern part of the
plateau is arable due to this
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Climatic Issues
Low rain fall
Extensive deforestation
Coal mining and
Oil and Gas exploration
Due to these activities the
plateau is facing serious
environmental problems
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BALOCHISTAN
PLATEAU
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BALOCHISTAN PLATEAU
Physical Features
Completely mountainous
Rugged, rocky & bare land
Scattered vegetation
Seasonal rivers
Water is scanty
Mineral deposits are large but
difficult to mine
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COASTAL
PLAINS
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COASTAL PLAINS
Pakistan has
1000Km long
coastal line
Sindh Coast
200 Km
Balochistan
coast 800Km
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COASTAL PLAINS
Coastal belt in Pakistan
stretches from Indian border
in the east up to Iranian
border in the west
Pakistan Coastal belt has:
commercial ports
fish harbours
Naval bases
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