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The Himachal Range is an important hydrographic barrier crossed by relatively few rivers. Drainage systems have evolved candelabra configurations with numerous tributaries flowing south from the Himalaya through the Middle Hills, gathering immediately north of the Himachal Range and cutting through in major gorges as the Karnali in the west ...
The Himalayan range obstructs the path of the south west monsoon winds, causing heavy precipitation on the slopes and the plains below. [79] The effect of Himalayas on the hydroclimate impacts millions in the plains as the variability in monsoon rainfall is the main factor behind wet and dry years. [ 86 ]
Also called the Mahabharat Range, the Lesser Himalayas is a prominent range 2,000 to 3,000 meters (6,600 to 9,800 ft) high formed along the Main Boundary Thrust fault zone, with a steep southern face and gentler northern slopes. The range is nearly continuous except for river gorges, where groups of rivers from the north gather like candelabra ...
This range is made up of the "High Berg" basalt range, and the "Small Berg" sandstone range. Drakenstein: Dragons stone Mountains: Western Cape: 1,590 m (5,220 ft) Part of the Cape Fold Belt system Du Toitskloof: Du Toit's Canyon: Western Cape: 1,995 m (6,545 ft) Part of the Cape Fold Belt system Gatsrand: Hole Ridge: Gauteng: Groot Swartberge ...
Table Mountain. List of Mountains in South Africa, Lesotho and Eswatini is a general list of mountains in South Africa, Lesotho and Eswatini with elevation. This list includes mountains in two other sovereign states, in the Stormberg-Drakensberg range, where the highest elevations are to be found in Lesotho, as well as Emlembe, the highest mountain in Eswatini, located at the border with South ...
The Kali Gandaki Gorge (a graben), [13] transects the main Himalaya and Transhimalayan ranges. Kora La is the lowest pass through both ranges between K2 and Everest, but some 300 metres (980 ft) higher than Nathula and Jelepla passes further east between Sikkim and Tibet Arniko Rajmarg/Friendship Highway route 5,260 17,260
About 180 million years ago, a mantle plume under southern Gondwana caused bulging of the continental crust in the area that would later become southern Africa. [2] Within 10–20 million years, rift valleys formed on either side of the central bulge and flooded to become the proto-Atlantic Ocean and proto-Indian Ocean more or less along the present southern African coastline and separating ...
As a result, the Himalayan range is one of the most seismically active regions in the world. This region has experienced many high magnitude earthquakes in the last 100 years, including the 1905 Kangra Earthquake , 1975 Kinnaur Earthquake , 1991 Uttarkashi Earthquake , and the 1999 Chamoli Earthquake , all of which were recorded at magnitudes ...