<p>I suspect you are referring to the mesas and buttes dotted around the Karoo - the large semi-arid plateau that makes up much of South Africa's interior. These are a product of the glacial and geological history of the region. The flat hills are capped by hard, resistant dolerite. This is solidified lava that was forced between the horizontal strata of the sedimentary rocks (which make up most of the Karoos geology) through high pressure. The dolerite erodes much slower than the surrounding rock and forms a flat cap above the underlying rock.</p>

<p>Most South African mountains are actually not like this - Google "Drakensberg" and you will see that the country's most prominent and highest mountain range is far from flat and short!</p>

CC BY-SA 4.0
2019-01-23T11:59:42.337Z
Pretty sure this identifies the intent of the question in the second paragraph. I recommend making this the focus of the answer.
Semidiurnal Simon
CC BY-SA 4.0
2020-03-07T08:16:21.107Z
I've voted for this, as it contains the main points. You could add that mountain regions such as Drakensburg in S. Africa, the European Alps or N. American Rockies result from tectonic activity. The flat top mountains you refer to occur through differential erosion in regions that have no or little tectonic activity (other than large scale up-lift).
M Juckes
CC BY-SA 4.0
2021-06-24T23:43:22.830Z
I think the word '[kopje](https://www.britannica.com/science/veld#ref417808)' needs to appear in this answer somewhere.
Spencer
CC BY-SA 4.0
2019-01-23T11:12:47.983Z
2019-01-24T14:13:13.133Z
2019-01-24T14:13:13.133Z
Wooshness
<p>At least speaking for Table Mountain, from when I was at the top, it is actually not as flat as it appears from the surrounding landscape.</p>

<p>Table Mountain was formed from horizontal layers of sedimentary deposits. One hypothesis is that a collision between Africa and another oceanic plate occurred around 250 million years ago. The collision upheaved these layers. The apparent flat appearance of the top of the mountain probably reflects the original sedimentary layers. We see further evidence of this same collision, in the form of the Cape Fold Belt system, which stretches deep into the interior, for 700 km east and 200 km north of Cape Town.</p>

<p>Today, the mountain is composed of sandstone, which eroded into the shape we see today. This is similar to the shape of a flat clay river bank, without any plant growth, that is eroded by water. </p>

<p><a href="https://i.sstatic.net/OpovN.jpg" rel="nofollow noreferrer"><img src="https://i.sstatic.net/OpovN.jpg" alt="River bank erosion in Bangladesh"></a></p>

<p>The same phenomenon is probably responsible for the geological features, that make the entire Cape region so spectacular.</p>

<p>I'm not sure how related this is to what you saw in Mozambique.</p>

CC BY-SA 3.0
2017-01-20T04:41:28.067Z
I don't see how this answers the question
f.thorpe
CC BY-SA 3.0
2017-01-19T14:56:04.983Z
2017-01-19T14:56:04.983Z
Jacques Nel
<p>I drove through South Africa from Cape Town to Mozambique and noticed that almost all heights and mountains were no higher than approx 200-400 meters and had a flat top, just like the iconic Table Mountain. Why is this the case? 
Thanks. </p>

CC BY-SA 3.0
2017-01-18T23:50:20.777Z
Anything in this Wikipedia article: [Cape Fold Belt](https://en.wikipedia.org/wiki/Cape_Fold_Belt) ?
mkennedy
CC BY-SA 3.0
2017-01-21T02:07:23.273Z
Or for more help, saddly most of the chapter is behind a paywall. https://www.eolss.net/Sample-Chapters/C01/E6-15-07-02.pdf
John
CC BY-SA 3.0
2017-01-23T08:30:30.863Z
Could it be that the engineers that built the road put it through relatively flat county?
nmtoken
<geology><mountains><regional-geology>
Why are South African mountains short and flat?
metazoa
# Why are South African mountains short and flat?

(Asked by: username_0 on 2017-01-18)

I drove through South Africa from Cape Town to Mozambique and noticed that almost all heights and mountains were no higher than approx 200-400 meters and had a flat top, just like the iconic Table Mountain. Why is this the case?
Thanks.

**Tags:** geology, mountains, regional-geology

> **Comments:**
> **username_1**: Anything in this Wikipedia article: [Cape Fold Belt](https://en.wikipedia.org/wiki/Cape_Fold_Belt) ?  
> **username_2**: Or for more help, saddly most of the chapter is behind a paywall. https://www.eolss.net/Sample-Chapters/C01/E6-15-07-02.pdf  
> **username_3**: Could it be that the engineers that built the road put it through relatively flat county?  

---

## 2 answers

### Answer by username_4 on 2019-01-23. Score: 9

I suspect you are referring to the mesas and buttes dotted around the Karoo - the large semi-arid plateau that makes up much of South Africa's interior. These are a product of the glacial and geological history of the region. The flat hills are capped by hard, resistant dolerite. This is solidified lava that was forced between the horizontal strata of the sedimentary rocks (which make up most of the Karoos geology) through high pressure. The dolerite erodes much slower than the surrounding rock and forms a flat cap above the underlying rock.

Most South African mountains are actually not like this - Google "Drakensberg" and you will see that the country's most prominent and highest mountain range is far from flat and short!

> **Comments:**
> **username_5**: Pretty sure this identifies the intent of the question in the second paragraph. I recommend making this the focus of the answer.  
> **username_6**: I've voted for this, as it contains the main points. You could add that mountain regions such as Drakensburg in S. Africa, the European Alps or N. American Rockies result from tectonic activity. The flat top mountains you refer to occur through differential erosion in regions that have no or little tectonic activity (other than large scale up-lift).  
> **username_7**: I think the word '[kopje](https://www.britannica.com/science/veld#ref417808)' needs to appear in this answer somewhere.  

---

### Answer by username_8 on 2017-01-19. Score: 3

At least speaking for Table Mountain, from when I was at the top, it is actually not as flat as it appears from the surrounding landscape.

Table Mountain was formed from horizontal layers of sedimentary deposits. One hypothesis is that a collision between Africa and another oceanic plate occurred around 250 million years ago. The collision upheaved these layers. The apparent flat appearance of the top of the mountain probably reflects the original sedimentary layers. We see further evidence of this same collision, in the form of the Cape Fold Belt system, which stretches deep into the interior, for 700 km east and 200 km north of Cape Town.

Today, the mountain is composed of sandstone, which eroded into the shape we see today. This is similar to the shape of a flat clay river bank, without any plant growth, that is eroded by water.

[![River bank erosion in Bangladesh](https://i.sstatic.net/OpovN.jpg)](https://i.sstatic.net/OpovN.jpg)

The same phenomenon is probably responsible for the geological features, that make the entire Cape region so spectacular.

I'm not sure how related this is to what you saw in Mozambique.

> **Comments:**
> **username_9**: I don't see how this answers the question  

---

