Itinerary: Cape Town – Namib Desert – Cape Town
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The Sossusvlei, Namibia's famous highlight in the heart of the Namib Desert, is a huge clay pan, enclosed by giant sand dunes. Some of the spectacular hills of sand are, at a height of 300 metres, the highest in the world. Only after a heavy rainfall, which is a ra re event in this area, does the vlei fill with water. As the clay layers hardly allow any water infiltration, a turquoise lake will remain for quite some time. The dunes of the Namib desert have developed over a period of many millions of years. It is thought that the vast quantities of sand were deposited into the Alantic Ocean by the Orange river. This material was subsequently moved
northwards by the Benguela current to be dumped back onto the land by the surf. The coastal dunes developed as a result of this and were shifted further and further inland by the wind. Wind continuously reshapes the patterns of the huge dunes of the Namib desert. It timelessly forces the grains of sand on the flat windward slope upwards to the crest of the dune. Here they fall down in the wind shade. The leeward slope is therefore always considerably steeper than the windward side.
Day 7, Sesriem, visit Soussousvlei

The Namib-Naukluft Park is Namibia's largest nature reserve, about 50.000 sqkms
in size. It includes a 100 to150 km broad belt of land that stretches along the
coastline from the Swakop valley in the north, towards the road B4 to Luederitz
in the south. Most parts of this enormous area are not accessible to man. One
can only visit a small stretch north of the Kuiseb river: the Naukluft Mountains
and the Sossusvlei in the central dune fields.
Day 8, Sesriem – Marienthal, km 370, all Gravel

Mariental lies 260 kilometres south of Windhoek on the B1. The little town
provides for the surrounding farms and Nama communities. With the construction
of the Hardap Dam in 1962, irrigation farming on a considerable scale was introduced
to the area causing an upswing for the town of Mariental. Nowadays, mainly
melons, lucerne, wine and maize are being cultivated below the dam. The Hardap
Dam is the biggest of its kind in Namibia with a water surface area of about
25 sqkms and an 862 metre long dam wall. It dams up the waters of the Fish
River, the only river in the country's interior that flows just about all year
round, although carrying very low quantities of water during the dry season.
Day 9, Marienthal – Kalahari Desert - Koes, km 350, all Gravel.
The Kalahari in south-east Namibia is an area of ancient red dunes scattered
with grass and low bush and umbrella-shaped Camelthorn trees. It is the ancient
home of Bushmen, some of whom still live in this semi-desert. The Kalahari
has plentiful game with wandering Antelopes, especially the hardy Oryx, Wildebeest,
Ostrich, Cheetah, Wild Dog, Brown Hyena and Kalahari Lions. Smaller mammals
also do well here including Meerkat, who live in fascinating well ordered communities.
In the red sands of the Kalahari, some Bushman still roam in harmony with the
land, as their ancestors have done for thousands of years.)
Day 10, Koes – Kalagadi National Park, km 350, all Gravel

The Kgalagadi Transfrontier Park - the former Kalahari Gemsbok National Park
- in the northernmost corner of South Africa is still one of the best kept
secrets in South African tourism, attracting 50,000 visitors annually. From
any starting point, the journey to the remote nature reserve is a long drive
over dusty roads. The park provides an insight into the fascinating ecosystem
of the Kalahari with its orange-red sand dunes and a flora and fauna specially
adapted to the arid conditions in the Kalahari desert. The Kalahari park
was declared a National Park in 1931, mainly to put a stop to the destructive
game poaching. After the amalgamation with the bordering Gemsbok National
Park in Botswana in 1998 the reserve is now called Kgalagadi Transfrontier
Park and comprises an area of more than 36,000 sq km.
Access to the park (South African part) in the south leads through the restcamp
Twee Rivieren ("Two Rivers"). Excellent accommodation is available
here with a swimming pool, restaurant and other amenities. The two main routes
through the National Park start here and run along the - usually dry - riverbeds
of the Nossob and Auob rivers to the remote restcamps Mata-Mata and Nossob.
In distances of 5 to 20 kilometres, one can find waterholes along the riverbeds,
most of them fed by wind pumps. Here is where the game gathers, especially
in the early hours of the morning and late in the afternoon. The cooler winter
months from April to September are more suitable for a visit to the Kgalagadi
Transfrontier Park than are the very hot summer months, when temperatures might
rise above the 40° C mark. The most favourable time for game observation
is right after the rainy season, which usually ends in March or April. If you
don't mind the heat, January and February are good months to spot lions. The
border is marked only by whitewashed stones, so that the animals can roam freely
through both parks.
Day 11, Kalahari – Upington, km 260, Tar Road

Upington, on the banks of the Orange River, is the economic and traffic centre
of the Northern Cape and the gateway to the Kalahari desert. For travellers
to the Kgalagadi Transfrontier Park, this is the last stop to do the shopping
in well stocked supermarkets and replenish the provisions. Those coming from
the Kalahari can enjoy the green lawns and the luxury of a swimming pool after
a dusty desert ride. The town developed from a missionary station, founded
here in 1871. Today, it houses a little museum (Kalahari Oranje Museum).
In the middle of a dry semi-desert area an oasis has been created using the
waters of the Orange River for irrigation. A narrow ribbon of fertile land
runs for over 280 kilometres on both sides of the river. The main crops are
wine grapes, as well as citrus, wheat and vegetables. The grapes are exported
to Europe as table fruits or used in the local wine production.Upington is
the hottest town in South Africa. In summer temperatures often rise to over
40 degrees.
Day 12, Upington – Augrabies Falls National Park, km 160, Tar
Road
The Orange River drops 191 metres at the Augrabies Falls. The thundering cascade
of water led the original Hottentot residents to believe that evil spirits were
active here, and so they named the waterfall Ankoerebis, "place of big noises",
from which the Trek Boers, who settled here later on, derived the name Augrabies.
Especially in late summer, when the river carries a lot of water, the roaring
waters fully justify that name. New waterfalls then form at the sidewalls, and
the air is filled with dense spraying fog. The gorge at the Augrabies Falls is
240 m deep and 18 km long. It is a most impressive example of granite erosion.
When the whole landmass of the area lifted about 500 million years ago, the Orange
River slowly started to dig its bed into the ground. The Augrabies Falls National
Park, an hour from Upington, comprises an area of 820 sq km and stretches along
the Orange River. The vegetation is suited to the arid desert climate. The Kokerboom,
or Quiver Tree grow here. They are succulents and can store huge amounts of water
in their stems and so survive long periods of drought. The park contains a game
reserve with rhinos as the main attraction.
Day 13, Augrabies – Calvinia, km 470, Tar and Gravel Road

Calvinia lies off the beaten tourist tracks, some 120 km east of Vanrhynsdorp.
Time seems to stand still in the little rural town which is why nostalgic Calvinia
is worth a visit. The town at the Oorlogskloof River was founded in the year
1847, first under the name "Hantam", a Khoi-Khoi word meaning "Mountain
where the red edible flowers bloom". After the building of the first Dutch-Reformed
church the minister insisted in changing the name to Calvinia in honour of
the Swiss reformer Johannes Calvin. Calvinia lies at the foot of the Hantam
mountain range at a height of about 1000 metres above sea level. The vegetation
mainly equals Karoo Flora, but some fynbos plants can also be found in here.
Calvinia is the trading and service centre for the merino and dorper sheepbreeders
in the vivinity. Over the last years this agricultural sector was badly hit
by the falling of the wool prices. Lately, though, the prices start to recover.
Day 14, Calvinia – Cape Town. km 400, Tar and Gravel Road

Cape Town is a city like no other. Its a contrast of vibrant activity and meditative
relaxation. She often compared to Rio de Janeiro, Sydney and San Francisco. Many
travellers, however, find her the most beautiful city in the world. The position
of South Africa's "Mother City" is at the foot of the mighty Table
Mountain massif, amidst a National Park of extraordinary beauty and surrounded
by two oceans, with stunning expansive beaches that enchant innumerable visitors
every year.
Final routing depending on availability of accommodation at time of booking and might change slightly



A trip to Cape Point is a must for any Cape Town visitor. The southern end of
the Cape Peninsula boasts two points of interest really, the Cape of Good Hope
and the more southernly and a bit higher situated Cape Point. However, the most
southern point of Africa is to be found 150 kilometres towards the southeast.
There, at Cape Agulhas, the two oceans, the Indian and the Atlantic 'meet'. For
the early se afarers the Cape of Good Hope marked the turning point in their
luck because once the " Cape of Storms", as Bartholomeus Diaz called
it in 1488, had been passed, the battle against the sea was basically won.
The Fish River canyon, situated along the lower reaches of the Fish River,
is one of the most impressive natural beauties in the southern part of Namibia.
It developed predominantly during the pluvial times - a rainy climatic epoch
- many millions of years ago. With a depth of up to 550 metres, the Fish River
Canyon is the second largest canyon in the world, before the Grand Canyon in
America. The enormous gorge meanders along a distance of approx. 160 kilometres
through the fissured Koubis massif all the way down to Ai-Ais. The canyon starts
near Seeheim, is 161 kilometres long and ends at Ai-Ais. The Fish River Canyon
probably formed about 500 million years ago. However, the gorge was not only
created by water erosion, but also through the collapse of the valley bottom
due to movements in the earth's crust.


