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[[Image:Subsaharan-africa.png|thumb|400px|Subsaharan Africa - Note location of Mosi-oa-Tunya]]
 
[[Image:Subsaharan-africa.png|thumb|400px|Subsaharan Africa - Note location of Mosi-oa-Tunya]]
  
Capital of the Tswana Kingdom. Mosi-oa-Tunya is Lothi for "''the Smoke that Thunders''," and is a large waterfall where the Zambezi River falls into a series of gorges. These gorges are pockmarked with carved archways, some more elaborate and decorated than others.  
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Capital of the Tswana Kingdom. Mosi-os-Tunya is Lothi for "''the Smoke that Thunders''," and is a large waterfall where the Zambezi River falls into a series of gorges. These gorges are pockmarked with carved archways, some more elaborate and decorated than others.  
  
 
==History==
 
==History==
The area, although celebrated for its beauty, could not be settled by humans, due to the nature of the gorges. Feral dragons were also unable to live there for lack of natural dwelling spots. The Sotho-Tswana people were the first to move into the region, and established it as their capital, which further established the tribal inter-connections. Once established, the dragon-ancestors desired to have more permanent shelters, and directed the first attempts at cave-drilling. This drilling, in addition to creating shelter, also allowed the discovery of both gold and precious jewels.
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The area, although celebrated for its beauty, was unable to be settled by men, due to the nature of the gorges. Feral dragons were also unable to live there for lack of natural dwelling spots. The Sotho-Tswana people were the first to move into the region, and established it as their capital, which further established the tribal inter-connections. Once established, the dragon-ancestors desired to have more permanent shelters, and directed the first attempts at cave-drilling. This drilling, in addition to creating shelter, also allowed the discovery of both gold and precious jewels.
  
 
==Physical Features==
 
==Physical Features==
 
For a considerable distance above the falls, the Zambezi flows over a level sheet of basalt, in a shallow valley bounded by low and distant sandstone hills. The river's course is dotted with numerous tree-covered islands, which increase in number as the river approaches the falls. There are no mountains, escarpments, or deep valleys which might be expected to create a waterfall, only flat plateau extending hundreds of kilometres in all directions.
 
For a considerable distance above the falls, the Zambezi flows over a level sheet of basalt, in a shallow valley bounded by low and distant sandstone hills. The river's course is dotted with numerous tree-covered islands, which increase in number as the river approaches the falls. There are no mountains, escarpments, or deep valleys which might be expected to create a waterfall, only flat plateau extending hundreds of kilometres in all directions.
  
The falls are formed as the full width of the river plummets in a single vertical drop into a chasm 60–120 metres (200–400 ft) wide, carved by its waters along a fracture zone in the basalt plateau. The depth of the chasm, called the First Gorge, varies from 80 metres (262 ft) at its western end to 108 metres (360 ft) in the centre. The only outlet to the First Gorge is a 110-metre-wide (360 ft) gap about two-thirds of the way across the width of the falls from the western end, through which the whole volume of the river pours into the Mosi-oa-Tunya gorges.
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The falls are formed as the full width of the river plummets in a single vertical drop into a chasm 60–120 metres (200–400 ft) wide, carved by its waters along a fracture zone in the basalt plateau. The depth of the chasm, called the First Gorge, varies from 80 metres (262 ft) at its western end to 108 metres (360 ft) in the centre. The only outlet to the First Gorge is a 110-metre-wide (360 ft) gap about two-thirds of the way across the width of the falls from the western end, through which the whole volume of the river pours into the Victoria Falls gorges.
  
 
There are two islands on the crest of the falls that are large enough to divide the curtain of water even at full flood. At less than full flood, additional islets divide the curtain of water into separate parallel streams.
 
There are two islands on the crest of the falls that are large enough to divide the curtain of water even at full flood. At less than full flood, additional islets divide the curtain of water into separate parallel streams.
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The principal gorges are:
 
The principal gorges are:
  
* '''First Gorge''': the one the river falls into at Mosi-oa-Tunya
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* '''First Gorge''': the one the river falls into at Victoria Falls
 
* '''Second Gorge''': 250 m south of falls, 2.15 km long (270 yd south, 2350 yd long)  
 
* '''Second Gorge''': 250 m south of falls, 2.15 km long (270 yd south, 2350 yd long)  
 
* '''Third Gorge''': 600 m south, 1.95 km long (650 yd south, 2100 yd long)  
 
* '''Third Gorge''': 600 m south, 1.95 km long (650 yd south, 2100 yd long)  

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