Thanks to Travellers!!

Thanks to Travellers!!

We wish all travellers who has travelled with Afrikaya in 2016, who made it possible for us and we hope a lot of dreams has come true for you!!

May you be blessed for 2017 and safe, may we find peace and happiness around the world and unite as a people’s nation.

Let your journey begin!!!

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Paarl History

 

OUR DIVERSE CULTURE
Paarl is the third oldest European Settlement in South Africa and is home to a culturally diverse community – the product of a unique history.

The people of Paarl are descendants of the Khoisan, slaves from African and Asia, Dutch settlers, French Huguenots, Jewish immigrants, Italian Prisoners of War, and Xhosa migrant labourers.

The Khoikhoi

The Khoikhoi and San were the first people to utilize the area and original San rock art can still be seen at nearby Wemmershoek and Bainskloof. Originally, Paarl Mountain was named “Tortoise Mountain” by the Khoikhoi.

The Berg River Valley formed the traditional border between the Peninsular Khoikhoi (the Gorachoqua and the Goringhaiqua) and the Cochoqua. The latter group moved their cattle around the various grazing areas of the Berg River and Drakenstein valleys.

The approximately 18 000-strong Cochoqua was one of the richest and strongest of the Khoi tribes, but they were eventually defeated during the second war between the colonists and Khoikhoi and most of their livestock looted.

On the death of their leaders, the tribe dispersed, with some trekking towards the Orange River, while others were in the service of colonists.

EUROPEAN SETTLERS

The Dutch

The original purpose of the Dutch settlement in the vicinity of latter day Cape Town, was to provide fresh food and water to the ships of the Dutch East India Company, on their way to the East. Founder of Cape Town, Jan van Riebeeck, built up fresh meat stock by bartering livestock from the local Khoikhoi.

In 1657, Abraham Gabbema led an expedition to find more Khoi groups to barter with and to search for the legendary treasures of Monomotapa. On the day that they arrived in the Berg River Valley, the granite boulders, towards the west side of our town, glistened in the sun and this inspired Gabbema to name this mountain “the Diamond and Pearl Mountain” from which the name Paarl was later derived.

In October 1687, thirty years after the Gabbema expedition, Governor Simon van der Stel granted the first farms to Free Burghers. Twenty-one of these farms were in Drakenstein (Paarl), and five were on the foothills of Paarl Mountain.

The French

When the French Huguenots arrived in the Cape in 1688, some were granted land in the Drakenstein area.

Their intimate knowledge of the wine industry would be instrumental in establishing the now internationally-renowned wine industry of South Africa.

The headquarters of the South African wine industry, the KWV, is situated in Paarl, on one of the earliest farms (La Concorde, as it is known today) to be granted by Governor Simon van der Stel.

Conflict

The traditional European practice of private land ownership soon clashed with  the communal land use of the Khoikhoi. Land was now granted to the French Huguenots and this meant that water was limited and the wild animals that were hunted by the Khoisan, systematically disappeared from the area.

European diseases, such as small pox, further decimated the indigenous peoples. Many of the Khoisan were forced to move to the interior or became labourers for the colonists.

The Slaves

Between 1658 and 1808, some 63 000 slaves were brought to South Africa from different parts of the world, to sow, harvest, and thresh the wheat and also to load wagons, weed the owner’s fields, and look after the livestock. On wine farms they harvested and pressed grapes. Women did housework and in some cases acted as wet nurses for their owner’s children.

Het Gesticht (a small unbaked brick church) was built in 1813 to provide slaves with a place of worship. From 1820, onwards it became known as the Zion Church and is the fourth oldest church building in South Africa.

After being emancipated in 1834, slaves in Paarl were awarded property in the vicinity of modern-day Berg Street and School Street.

Reason why I am a Tourist Guide?

Through all my experience and the way I love what I’m doing as Tourist Guide in South-Africa?

Old videos I wish to share with all!

Relax sit back and enjoy!

visit websites:

http://www.afrikayatours.nl

http://www.afrikayaleisuretravel.com

P.S. We do small group tours through Southern Africa max of 6-12 people.

https://www.youtube.com/watch?v=6Q7OX8RxmhY

Why visiting Southern Africa?

We have decided to make use of National Geographic’s video.

Our 17 & 25 day tours go through South-Africa, Swaziland and Lesotho (4X4).

Our 29 day tour go through Namibia, Botswana and visiting Victoria waterfalls (Zimbabwe side).

Mozambique is great place to visit for snorkelling and scuba diving.

Visit: http://www.afrikayatours.com

http://www.afrikayaleisuretravel.com

Watch the movie!

http://video.nationalgeographic.com/video/destinations/africa-south-dest?source=searchvideo

Memory lane!!!

For the past few years we have travelled through Southern Africa.

As a tourist guide and tour operator in Southern Africa I’m proud to show some of our photos.

Enjoy and hope to see you on our next tour with:

Afrikaya Tours and Afrikaya Leisure Travel!!!!!

From Margreet van Belle and Wynand Meyer.

We wish to thank you all for making this tours all possible!!!

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IMG_7012 IMG_7055 IMG_7081 Wynand playing soccer Makgadigadi pans Fish catcher 2255 IMG_5050 IMG_5065 IMG_5071 IMG_5108 IMG_5118 IMG_5133 IMG_5177 IMG_5205 IMG_5307 IMG_5317 IMG_5068 IMG_5336 IMG_5351 IMG_5372 IMG_5445 IMG_4417 IMG_4437 IMG_4453 IMG_4465 IMG_4486 IMG_4521 IMG_4540 IMG_4579 IMG_4598 IMG_4603 IMG_4744 IMG_4747 IMG_4796 IMG_4906 IMG_4926 IMG_4947 IMG_4988 IMG_4999 IMG_5021 IMG_5476 IMG_5532 IMG_5536 IMG_5441 IMG_5487 IMG_5627 IMG_5630 IMG_5661 IMG_5689 IMG_5731 IMG_5739 IMG_5749 IMG_5516 IMG_5581 IMG_5778 IMG_5846 IMG_0065 IMG_0070 IMG_6006 IMG_6106 IMG_6107 IMG_6166 IMG_6279 IMG_6318 IMG_6350 IMG_6367 IMG_6362 IMG_6472 IMG_6473 IMG_6641 IMG_6650 IMG_6698 IMG_6711 IMG_6718 IMG_6820 IMG_6836 IMG_6863 IMG_6925 IMG_0129 IMG_6961 IMG_6968 IMG_7033 IMG_7055 IMG_0371 IMG_0049

Makgadikgadi Pan

Botswana

Botswana

IMG_6725

The Makgadikgadi Pan, a salt pan situated in the middle of the dry savanna of north-eastern Botswana, is one of the largest salt flats in the world. The pan is all that remains of the formerly enormous Lake Makgadikgadi, which once covered an area larger than Switzerland, but dried up several thousand years ago.

Location and description

Lying southeast of the Okavango Delta and surrounded by the Kalahari Desert, Makgadikgadi is technically not a single pan but many pans with sandy desert in between, the largest being the Sua (Sowa), Nwetwe and Nxai Pans. The largest individual pan is about 1,900 sq mi (4,921.0 km2). In comparison, Salar de Uyuni in Bolivia is a single salt flat of 4,100 sq mi (10,619.0 km2), rarely has much water, and is generally claimed to be the world’s largest salt pan. A dry salty clay crust most of the year, the pans are seasonally covered with water and grass, and are then a refuge for birds and animals in this very arid part of the world. The climate is hot and dry but with regular annual rains.

The main water source is the Nata River, called Amanzanyama in Zimbabwe, where it rises at Sandown about 37 mi (59.5 km) from Bulawayo. A smaller amount of water is supplied by the Boteti River from the Okavango delta.

These salt pans cover 6,200 sq mi (16,057.9 km2) in the Kalahari Basin and form the bed of the ancient Lake Makgadikgadi, which evaporated many millennia ago.Archaeological recovery in the Makgadikgadi has revealed the presence of prehistoric man through abundant finds of stone tools; some of these tools have been dated sufficiently early to establish their origin as earlier than the era of Homo sapiens. Pastoralists herded grazing livestock here when water was more plentiful earlier in theHolocene.

The lowest place in the basin is Sua Pan with an elevation of 2,920 feet.

Geology

As the ancestral Lake Makgadikgadi shrank, it left relict shorelines, which are most evident in the southwestern part of the basin. As the lake shrank numerous smaller lakes formed with progressively smaller shorelines. The relict shorelines at elevations of 3100 feet and 3018 feet can be seen mostly easily on Gidikwe Ridge, west of the Boteti River.

The geologic processes behind the formation of the basin are not well understood. It is conjectured that a there was a gentle down-warping of the crust, with accompanying mild tectonics and associated faulting; however, no significant plate boundary faults have been identified. The main axis of the developing graben runs northeast-southwest.

Kubu Island and Kukome Island are igneous rock “islands” in the salt flat of Sua pan. Kubu Island lies in the southwestern quadrant of Sua Pan, contains a number of baobab trees, and is protected as a national monument.

Flora

The pans themselves are salty desert whose only plant life is a thin layer of blue-green algae. However the fringes of the pan are salt marshes and further out these are circled by grassland and then shrubby savanna. The prominent baobab trees found in the area function as local landmarks. One of them, named after James Chapman, served as an unofficial post office for 19th-century explorers.

Fauna

Very little wildlife can exist here during the harsh dry season of strong hot winds and only salt water, but following a rain the pan becomes an important habitat for migrating animals including wildebeest and one of Africa’s biggest zebra populations, and the large predators that prey on them. The wet season also brings migratory birds such as ducks, geese and Great White Pelicans. The pan is home of one of only two breeding populations of Greater Flamingos in southern Africa, and only on the Soa pan, which is part of the Makgadikgadi pans. The other breeding population is at Etosha, in the Northern part of Namibia. The only birds here in the dry season areostriches, Chestnut-banded Plover (Charadrius pallidus) and Kittlitz’s Plover (Charadrius pecuarius). The grasslands on the fringes of the pan are home to reptiles such astortoises, rock monitor (Varanus albigularis), snakes and lizards including the endemic Makgadikgadi spiny agama (Agama hispida makgadikgadiensis).

Threats and preservation

The salt pans are very inhospitable and human intervention has been minimal so they remain fairly undisturbed, although land surrounding the pans is used for grazing and some areas have been fenced off, preventing the migration of wildlife. Modern commercial operations to extract salt and soda ash began on Sua Pan in 1991, and there are also plans to divert water from the Nata River for irrigation, which would cause severe damage to the salt pan ecosystem. Another threat is the use of quad bikes and off-road vehicles by tourists, which disturbs breeding colonies of flamingos. Illegal hunting in the national parks is a persistent problem.

There are some protected areas within the Makgadikgadi and Nxai Pan National Park. The Makgadikgadi Pans Game Reserve is the scene of large migrations of zebra and wildebeest from the Boteti River across to Nwetwe Pan, while the Nata Sanctuary in Sua Pan is a place to see birdlife and antelopes. In Nxai Pan you can still see thebaobabs painted by 19th century British artist Thomas Baines. The area can be accessed between the towns of Nata and Maun or from the town of Gweta.

Etosha National Park

Etsosha

Etosha National Park is a national park in northwestern Namibia. The park was proclaimed a game reserve on March 22, 1907 in Ordinance 88 by the Governor of German South West Africa, Dr. Friedrich von Lindequist. It was designated as Wildschutzgebiet Nr. 2 which means Game Reserve Number 2, in numerical order after West Caprivi (Game Reserve No. 1) and preceding Namib Game Reserve (No. 3). In 1958, Game Reserve No. 2 became Etosha Game Park and was elevated to status of National Park in 1967 by an act of parliament of the Republic of South Africa which administered South-West Africa during that time.

Etosha National Park spans an area of 22,270 square kilometres (8,600 sq mi) and gets its name from the large Etosha pan which is almost entirely within the park. The Etosha pan (4,760 square kilometres (1,840 sq mi)) covers 23% of the area of the total area of the Etosha National Park.[2] The park is home to hundreds of species of mammals, birds and reptiles, including several threatened and endangered species such as the black rhinoceros.

The park is located in the Kunene region and shares boundaries with the regions of Oshana, Oshikoto and Otjozondjupa.