Lanner Gorge

Infobox_protected_area | name = Lanner Gorge, Makuleke Area, Kruger National Park
iucn_category = II


caption = Map of South Africa
locator_x = 255
locator_y = 32
location = Limpopo, South Africa
nearest_city = Tshipise, South Africa
lat_degrees = 22
lat_minutes = 25
lat_seconds = 22
lat_direction = S
long_degrees = 31
long_minutes = 2
long_seconds = 8
long_direction = E
length = about 11 kilometres
established = Incorporated into Kruger Park 1969 returned to Makuleke people 1998
visitation_num =
visitation_year =
governing_body = National Park Service and Makuleke People

The Lanner Gorge is located in the far North of the Kruger National Park. It forms the boundary between the Kruger National Park to the South and the Makuleke Concession to the North. It was carved by the Luvuvhu River and is at some points more than 150m deep.

Description

Lanner Gorge is approximately 11km long and is carved into sandstones and shales.cite web|url=http://www.profleeberger.com/files/Into_the_Heart_of_Eden_for_web.pdf|title=Into the Heart of Eden|accessdate=|author=Berger, L.R.|authorlink= |coauthors= |year=2004 |format= |work= |publisher=Prime Origins|pages=97|language= |archiveurl= |archivedate= |quote= ]

Geology

The uppermost rocks are gravels which are thought to be Cretaceous in age while the basal shales are thought to be Permian in agecite web|url=http://www.profleeberger.com/files/A_History_of_the_Makuleke_licensed_copy.pdf|title=the History of the Makuleke Concession|accessdate=|author=Berger, L.R.|authorlink= |coauthors= |year=2005 |format= |work= |publisher=Wilderness Safaris|pages= |language= |archiveurl= |archivedate= |quote= ] . The majority of the walls appear to be comprised of Triassic and Jurassic aged sandstones formed under arid conditions.

The Luvuvhu river has eroded through the sandstones and shales and formation is still active as is evidenced by the many collapsed boulders in the river bed.

Fossils

Geological Age

The precise age of the gorge is unknown, however, the absence of Early Stone Age occupation in the many caves and shelters in the gorge suggests that the gorge may be relatively young and have formed in the last 2 million years.

Flooding

As the Luvuvhu River is still a young, active river, flooding is common and the gorge is often cluttered with debris such as fallen trees.

Accessability

There is extremely limited access to the gorge due to its steepness and its status as a wilderness area of Kruger. Nevertheless, some walking trails approach and enter the gorge from both the Makuleke areacite web|url=http://www.wilderness-safaris.com/news/detail.jsp?newsitem_id=348919|title=Wilderness News|accessdate=|author=Wilderness Safaris|authorlink= |coauthors= |year=2006 |format= |work= |publisher=Kruger National Park Safaris|pages= |language= |archiveurl= |archivedate= |quote= ] as well as from the Kruger sidecite web|url=http://krugerpark.safari.co.za/Game_Walking_Trails-travel/kruger-park-hiking-trails.html|title=Kruger Park trails|accessdate=|author=SANP|authorlink= |coauthors= |year=2007 |format= |work= |publisher=Kruger National Park Safaris|pages= |language= |archiveurl= |archivedate= |quote= ] .

Wildlife

The gorge holds a variety of wildlife including abundant crocodiles, hippos, hyraxes, baboons, leopards and other small game. Elephants and buffalo and other larger game are common at both ends of the gorge, but have difficulty in accessing the central region due to the steep walls.

Their is an abundance of birds including raptors such as the Black Eagle and Lanner Falcon - after which the gorge is named.

Other interesting facts

*The archeological site of Thulamela is located just outside the eastern end of the gorge.
*Legend has it that a former chief used to throw criminals and enemies to their death from the highest points of the gorge.

References

External links

* [http://www.krugerpark.co.za Kruger National Park]
* [http://www.wilderness-safaris.com/camps/camps.jsp?map_id=2590 Wilderness Safaris]