The detailed study of the surface features of a region
Hills and Mountains
A Hill is generally considered to be an elevated piece of land less than 600-610meters high, and a Mountain is an elevation of land that is more than 610m high. Some hills are called mountains while some mountains are referred to as hills
Mountain Range
A succession of mountains which have the same direction, age, and same causes of formation. A snowfield is a huge permanent expanse of snow
Relief/Topography
The condition of the land related to the rocks, ups and downs, eroded and depositional features like valleys, rock type, passes, etc.
Drainage
Related to the eroded and depositional features of the rivers like ox-bow lake, meander, levees, etc. All types of river patterns including dendritic are part of drainage
Gorges
An irregular depression in a valley
Cirque
A regular depression made by the movement of glaciers
Valley
Plain land between two mountains
Passes
A natural path which connects two areas in a mountainous region
Snowfield
A plain field covered with snow usually above the snow line (4000m)
Ravine
A deep narrow gorge with steep sides
Gully
A ravine formed by water activity
Glaciers
Tongue-shaped mass of ice moving slowly down the valley
Streams/Springs
Channels of water from snow-capped mountains towards the valley
Cirque/Corrie
A steep-walled basin or a kind of lake. Example: Lake Saif ul Mulook
Serrated Landscape
Elevated mountain zone used for agriculture
Bare Rock
Rock without vegetation due to the accumulation of snow
Scree
Accumulation of loose rock debris
Abrasion
The scraping of rock surface frozen into the moving ice
Plucking
When ice freezes onto rock surface and pulls off pieces or blocks of moving ice
The Northern Mountains are divided into three main mountain ranges: the Karakoram, the Himalayas, and the Hindu Kush
Northern Mountains
Karakoram
Himalayas
Hindu Kush
Karakoram
Average Altitude: 6000m
Highest peak: K2 (8610m)
Lifestyle: Nomadic agriculture and livestock is practiced
Products: Apples, Barley, Millets
Valleys: Gilgit, Hunza, Baltistan
Himalayas
Average Altitude: 4000m lesser or lower Himalayas
Highest peak: Nanga Parbat (8126m)
Lifestyle: Nomadic
Economic activity: Tourism, agriculture, and livestock is practiced
Important locations: Murree, Nathya Gali, Ghora Gali
Valleys: Murri, Gullies, Naran, Kaghan
Hindu Kush
Average Altitude: 5000m
Highest peak: TirichMir (7690m)
Historical Importance: Alexander, Timurlane, Mughals, Ghazni, and Ghauris passed it to attack India
Important locations: Swat, Kohistan, Chitral, Dir
Products: Rice, Apples, Apricots, Tobacco
Valleys: Swat, Chitral, Dir
The Karakoram runs from South East to North-West with an average height of 6000m
They have an average height of 6000m
The Himalayas run from South-East to North-West with an average height of 4000m
They have an average height of 4000m
The Hindu Kush runs from North East to South West with an average height of 5000m
They have an average height of 5000m
Physical features of mountain ranges
Deep narrow valleys like Gilgit and Chitral
Snow-capped mountains with steep-sided slopes
Conically shaped peaks with altitude increasing from South towards the North
Fast-flowing rivers like River Gilgit forming alluvial fans and deep narrow gorges
Massive glaciers like Baltoro, Batura, and Siachen
Soil cover on slopes is extremely thin with bare rocks supporting little plant growth above snowline
Rocks undergo weathering by wind, water, and lichens breaking down into small soil particles over time
Drainage features
1. Indus starts from Manasarover lake in Karakoram range moving towards south joins river Kabul at Attock and enters the plain of Punjab at Kalabagh
2. Southern slopes of the Himalayas are drained by Eastern tributaries of the River Indus: Jhelum, Chenab, Ravi, Sutlej, and Beas
3. All these Rivers run in North-East to South West direction
4. Snowfields are found in areas above 4000m and feed the rivers in summers
Range is the only range, which has some existing snow capped peaks. Other ranges are quite dry.
These mountains generally have bare rocks due to low rainfall and in some cases very high temperatures (which leads to high rate of evaporation).
These mountain ranges have steep sided peaks along with deep narrow valleys and gorges
The Safed Koh range is drained by River Kabul, which runs in a West to East direction and eventually joins River Indus. The Waziristan hills are drained by small seasonal rivers like Kurram, Tochi, and Gomal.
These rivers run from West to East, and all are the Western tributaries of the River Indus. The Sulaiman range is drained by small hill torrents and small seasonal rivers such as the Bolan and Mula.
These rivers usually lead to small inland lakes, where the water collects and then dries up (for example the lake Damas). The rain falling on Eastern slopes of Sulaiman range runs down the slopes and falls into piedmont plains leading to the formation of alluvial fans.
The Kirthar range on the other hand is drained by the River Hab (seasonal river), which flows in a North to South direction and eventually joins the Arabian Sea.
Plateau: is an area of highland, which is usually flat although a heavily dissected plateau can also exist.
Features of Balochistan Plateau
Height varying from around 600m to around 3000m
Total covered area of 347190 sq km
Deep narrow valleys like Quetta
Bare rocks due to lack of rainfall
Steep slopes and none are snow capped
Parallel ranges running in an East to West direction like Chagai Hills, Raskoh Range, and Makran Coastal Range
Parallel ranges running North-South direction like Central Brahui and the Hala range
In the Southern part of the Balochistan Plateau, the River Dasht and River Porali flow from north to South, thus eventually draining into the Arabian Sea. Both are seasonal rivers; they flow only during the rainy season.