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Category: nature and travel

Namib Desert’s northwest (#22 in series: sands, plural…rocks, ditto)

 

 

In this part of the Namib – its western edge, adjacent to the Atlantic’s “skeleton coast” – its dunes are often generally-lighter in colour than are those further inland and further south.

Here, also, variations in colour and texture are more readily-evident/common on the dunes’ surfaces.

Their “sands” are not all of the same kind, colour and density; accordingly, winds “sift”, “sort” and shift them, differentially.

The results are oft-exquisite: “sand mandalas”, sans any human role in their creation.

I especially love what happens when shifting sands meet rocks and/or riverbeds; they, too, are far from “uniform”.

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Namib Desert’s northwest (#21 in series: another win for the Springboks)

 

For Australian followers of Test Matches across two “major” sporting codes, this post’s subtitle will recall at least several decades of all-too-familiar, unwelcome headlines

The actual SpringbokAntidorcas marsupialis –  is South Africa’s heraldic beast.

However, this charismatic antelope is similarly abundant in Namibia and Botswana, and its range extends into the drier, southwest corner of Angola.

(Namibia’s emblematic mammal returns the compliment; gemsbok also thrive in South Africa and Botswana)

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Namib Desert’s northwest (#20 in series: maternity, on the rocks)

 

Baboons thrive in many different kinds of environment, across most of Namibia.

However, all of Namibia’s baboons belong to just one species: Papio cynocephalus ursinis, known as Chacma baboons, or Cape baboons.

Click here to discover more.

If you think that there are only two baboons in this post’s image, you are not looking closely enough!

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Namib Desert’s northwest (#19 in series: living it up)

 

 

This post’s heroes are superbly adapted to life in a very demanding, arid environment.

Oryx gazella – known locally as “gemsbok”, but labelled as “South African oryx” by many non-African English-speakers – is Namibia’s heraldic beast.

It is the largest oryx species.

Gemsbok are remarkably water-efficient.

Few, if any, other mammals can survive for so long, “between drinks”.

They can also reach/withstand amazingly high body temperatures – temperatures that would prove fatal to other mammals. (this ability reduces water needs and energy expenditure).

The pictured individuals are doing it “very easy”, in a place that offers green grass and mostly-moderate temperatures.

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Namib Desert’s northwest (#18 in series: not an irrigation project)

 

Absolutely nothing “artificial” is going on here, and you are indeed looking at one of the least-rainy places on our planet – a few kilometres in from the “Skeleton Coast”, on the Namib’s western edge.

Presumably/perhaps, there is a rock barrier below the dune on which I stood, at 10.24 am on 14 November 2022.

(dolerite “dikes” are a common landscape feature, above ground, in northern Namibia)

In any event, the “surprising” mini-forest in front of me could not survive on light and fog alone!

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Namib Desert’s northwest (#16 in series: sandfalls, on volcanic rock)

 

This post’s, the previous post’s, and the next post’s photos were all taken within the space of a very few minutes.

Their vantage points were not at all far apart.

This is a place where a very selective view can create a highly misleading impression.

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Namib Desert’s northwest (#15 in series: “pig’s ear” & rock, in hard place)

 

You are looking at a “succulent” which is highly prized by gardeners, worldwide.

Very probably, this wild, uncultivated one is an example of Cotyledon orbiculata, commonly known as “pig’s ear”.

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Namib Desert’s northwest (#11 in series: “castles”)

 

 

The Hoarusib is one of several ephemeral Namibian desert rivers that have generated  so-called “sand castles”, or “clay castles”.

These extraordinary landforms’ origins and age are shrouded in mystery, speculation, and competing theories.

I am quite unable to offer a definitive explanation, other than to quote some good sense from Roger Swart:

…there is abundant evidence that the silts were deposited by high-energy flows, separated by times of calm……The most likely explanation for the deposits is therefore flash floods during a wet period, which would have brought down a heavy sediment load that was dumped when the energy of the river waned.

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