Namibia is a state in southwestern corner of Africa. Bordered in the West by the Atlantic Ocean, in the North by Zambia and Angola, in the East by Botswana and South Africa to its South and East, Namibia has a small portion of the River Zambezi of close to 200 meters separating it from Botswana. It also got its Independence on the 21st of March 1990 from the South African state ensuing the Namibian War of Liberation.

Namibia is well-known for its Namib Desert that is alongside the Atlantic Ocean coastline. This republic is home to various numbers of wildlife among which the momentous cheetah populace is included. Its capital city is called Windhoek and littoral town known as Swakopmund which contains the German colonial-epoch structures like the Windhoek’s Christuskirche that was constructed in 1907.

namibia safari


The Etosha National Park:

Coveringover 20,000 sq. km, Etosha is one of the earth’s extraordinary wildlife exploration locations. Dissimilar from the other parks in Africa where you get to devote days searching for the animals, Etosha’s gems lie in its capability to bring the wildlife to you.The Etosha National Park’s essence is the gigantic Etosha Pan which becomes an enormous, leveled and salty desert for quite a number of days each year. It is transformed by the rain into a trivialinletswarming with pelicans and flamingos. In disparity, late in the arid season everything like the elephants and the one time golden savannas appears cast, spectra-like in the Etosha’s silvery, ashen dust.The Etosha National Park is home to the 114 animal kinds and also the 340 species of fowls, the 16 kinds of reptile amphibians, merely one typeof fish species and not overlooking the uncountable bugs. Another thing one gets the opportunity to see are the black rhinos. It is typically very challenging to spot them however as they gather at some of the watering holes around the camps in the night, it becomes very easy to see them. Dependent onthe time of year, one may perhaps spot the elephants, Burchell’s zebras, giraffes, the springboks, red hartebeests, blue wildebeest, gemsboks, kudus, elands, roans, ostriches, jackals, lions, hyenas and even the leopards and cheetahs. Amongst the threatened animal kinds are the black rhinoceros and the black-faced impalas. Etosha is Namibia’s most significant throttlehold for the lions with over a half of the nation’s wild lions – 450 to 500 lions.Birdlife is also prolific. The yellow-billed hornbills are a mutual sight and while on the ground you ought to look for the gigantic Kori bustard that weighs close to 15kg and it hardly ever flies – it’s the sphere’s weightiest flying fowl. You may also get to see the Korhaans, marabous, the ostriches, the white-backed vultures and many other minor kinds.


Twyfelfontein is a place of prehistoric rock engravings that are in the Area of the north-western part of Namibia, Kunene. It comprises of a spring in the vale flanked by the inclination of a granite table mountain that gets very diminutive rainfall and has a wide-ranging variety of diurnal temperatures. The forename Twyfelfontein refers to the waterbed itself then to the vale harboring the spring. The spot has been populated for over 6,000 years ago, first by the hunter-gatherers and then later by Khoikhoi herdsmen. Both tribal groups used it as an area for worship and a location to carry out shamanist rituals. In the course of these rituals close to 2,500 items of rock crafting had been shaped, as well as a small number of rock paintings. Showcasing one of the prevalent concentrations of the rock petroglyphs in the African continent, UNESCO accepted Twyfelfontein as Namibia’s foremost Global Heritage Site in the year of 2007. Twyfelfontein is positioned in the Huab vale of the Mount Etjo configuration in Kunene’s southern Region of Namibia in the vicinity previously identified as Damaraland. Sometime in August the 15thof 1952 the region was acknowledged as a Nationwide Monument by the South West African management. Despite its untimely identification the area was left unguarded until sometime in 1986 when the whole area was stated as a nature reserve. The center area was designated a state monument in 1948 and it is now cosseted by the National Heritage Act of 2004. A buffer precinct has been recognized and stated publicly. The overall state of maintenance of the land has enhanced over the precedent years principally in terms of the way guests are handled.


The area of Sossusvleigoes to an extensive section of the southern Namib with standardized geographies of almost 32.000 km²that spreads amid the Kuiseb and Koichab rivers. This region is branded by the extraordinary sand ridges of vibrant pink-to-orange pigment which is asign of the great concentration of iron in the sand and ensuing corrosion processes. The very old dunes are the ones with a more concentrated reddish shade. These dunes are amongst the chiefones in the biosphere; a number of them being above 200 meters, the main one also islabelled Big Daddy and is close to 325 metersin height. Still the uppermost dune in the Namib Desert is approximately 388 metersin height. Traces in sand that are and or were left by creepy-crawlies and other trifling animals can be seen.The utmost and more established dunes are to some extentconcealed with a moderatelyopulentplant lifethat is mostlydampened by anamount of subversive and transitory rivers that in season deluge the pans thusformingswamplands that are locally identified as vlei; when arid, these pans look more or less white in shadeowing to the great concentration of brackish. Another significant water source for Sossusvlei is the mugginess brought in by the day-to-daysunrisemists that cross the thresholdto the desert straight from the Atlantic Ocean.Wildlife in the area of Sossusvlei is somewhat rich. It commonly consists of trivial animals that can stay aliveeven with pint-size water. These include a number of small reptiles, arthropods and small mammalians such as jackals and or rodents; the much larger wildlife that includes the ostriches and antelopes (mainly springboks and oryxes). For the duration of the season of floods, quite a lot ofmigratory bird kindsshow up along the marshlands and rivers. A number of the Sossusvlei and Namib wildlife is prevalent and extremelymodifiedwith the explicitgeographies of the Namib. Particularly the fog beetles like the example of the Namib Desert Beetle which has developed a method for gathering water from the early morning mistsusing the bumps on their backbone.

Fish River Canyon:

The Fish River canyon comprises of an uppermost gorge where river corrosion was inhibited by the hard gneiss rock layers and also a minor gorge created after the corrosion had finally dilapidated through the gneisses. Upstream the waterway runs through parallel dolomite layers; these metamorphic pillars made part of the gorge. Approximately 650 million ages ago, Mya platter movement molded a northern-southern graben and or depressed area along which the olden Fish River could flow and sooner or later erode a leveled plain that is the present day’s uppermost canyon. Glaciation at about 300 Mya, a portion of the Dyka glaciation throughout the Karoo Ice Age additionally deepened the gorge. Approximately 60 Mya, Southern America and Africa detached (owing to the continental drift) and Africa jetted ominously; the inevitably enlarged gradient of the Fish River permitted it to corrode the lower gorge into the solid gneisses establishing the current deeply winding, snaky system of the lower gorge. The Fish River Canyon climbing trail is one of the more prevalent climbing trails in the Southern Africa. The vast scale and rocky terrain has drawn many tourists from all over the biosphere to experience what climbing or track running the gorge can offer. Putting aside the 2 kilometer slope that is west of Hobas and some non-compulsory short cuts, the trail in general follows an 88 kilometer of the Fish River over to Ai Ais and is regularly completed in 5 days. Even though there are a number of trails through the gorge, the tracks are not fixed thus leaving the trekker to choose where to and how long the hike will take. There aren’t any facilities along the trail and trekkers have to carry along all their essentials with them. Exposed fires are not accepted on the track. Because of overflowing floods and the tremendously summer hotness that reaches 48 °C during the day and 30 °C in the night, licenses are only given out between 1st May and 15th September. Prior to your arrival at Hobas, a climbing license must be got from the Namibia Wildlife Resorts for the crowds not lesser than 3 and not greater than 30. All trekkers must be adults of not lesser than 12 years and a credential of fitness filled in by a medical specialist must be provided at the headquarters of the Ministry of Environment and Tourism in Hobas. In the current years, the track has become common mainly all through the school breaks and extended weekends and licenses should be booked for well in advance. Reservations for the next year’s season are available come 1 May. The river drifts tougher early in the time of year and by September it habitually becomes dry to form a chain of motionless pools. The water is safe for drinking though the use of water cleansing tablets are suggested. River crossings are a prominent feature with over 20 crossings in the course of the trail and these crossings may turn out to be a major concern when water levels rise.

Namib Dessert:

The Namib is a littoral desert in southern part of Africa. The forename Namib is of the Nama derivation and this means a “vast place”. In reference to the extensive definition, the Namib springs for more than 2,000 kilometers (1,200 mi) lengthways the Atlantic shores of Angola, South Africa and Namibia outspreading southward from the River Carunjamba in Angola through Namibia and then to the River Olifants in the Western Cape, South Africa. The Namib’s northernmost ration thatspreads 450 kilometers (280 mi) from the Angola-Namibia boundary is identified as the Moçâmedes Desert, whereasthe southern ration comes close to the adjacent Kalahari Desert. From the Atlantic shoreline eastward, the Namib increasinglyrises in heightattaining up to 200 kilometers (120 mi) in the interior to the foot of the Great Ridge.Yearlyrainfall ranges from 2 millimeters (0.079 in) in the utmostdryareas to 200 millimeters (7.9 in) at the ridge, making Namib the only spot-on desert in the southern Africa.Having endured dry and or semi-waterless situations for approximately 55–80 million ages, the Namib might be the most ancient desert in the biosphere and also it comprises some of the biosphere’sdried outareas.The Namib is nearlywhollyunpopulated by human beings save for numerousminor settlements and nativerural groups that include the Obatjimba Herero and Ovahimba in the northern part and then the Topnaar Nama in the middlepart. Because of its olden times, the Namib might be household to more common species than any other desert in the biosphere. Most of the desert wildlife are the arthropods and other little animals that stay on miniature watereven though larger animals inhabit the northern regions. Close the coast, the icy ocean water is rich in fishery capitals and helpspopulaces of shorebirds and brown fur seals, which serve as game for the Skeleton Coast’s lions. Deeperin the interior, the Namib-Naukluft National Park which is the biggest game park in Africa, accommodatespopulaces of the Mountain Zebras, African Bush Elephants and other huge mammals. Even though the external Namib is essentially barren of undergrowth, succulents and lichens are seen in the littoral areas, while grasses, shrubs, and ephemeral floraeflourish near the ridge. Some uncommoncategories of trees can also be able to endure the particularly arid climate.The Namib-Naukluft National Park that spreads over a greater part of the Namib Desert is the biggest game reserve in the African continent and one of the prevalent of the biosphere. Even when most of the park is barely accessible, quite a lot of well-known touristfascinationscan be found in the desert. The noticeable attraction is the prominent Sossusvlei area where the high orange sand ridgesborder vivid white salt pans thusforming a captivatingscenery.Entréeinto the park is by pebbleand or dust roads (save for the 60 km of concrete path from the Sesriem entranceinto Sossusvlei) or by the light airplane from Windhoek (which is the capital city of Namibia that is about 480 km (300 mi) north-east of the epicenter of the desert). Lastly Walvis Bay and Swakopmund at the north end of the desert.

Namibia Safari  Accommodation

Namibia entails a number of places where tourists can take a nap, dine, enjoy a number of fun activities and do so much more. These range from the luxurious high end class hotels, down to the low budget accommodations that are still worth your stay. Some of the places you can check out include; the Hilton Windhoek, the Klein Windhoek Guest House, the Rivendell Guest House, the Elegant B&B, the, Safari Hotels Namibia and the Vondelhof Guest House among the many others. You can also get to visit their various websites for more information and bookings and or reservations.

Add a Comment

Your email address will not be published. Required fields are marked *