Londolozi is famed for its incredible wildlife, but the landscape itself tells an equally fascinating story. The koppies that run across the northern part of the reserve are a standout feature to anyone who passes by or climbs to the top. There’s an exhilaration I feel every time I reach the summit of Ximpalapala Koppie, with ancient rock beneath my feet and the vast wilderness stretching out before me. Whether it’s sharing stories with friends over sundowners at Southern Cross Koppies or just pausing for a quiet moment, these rocky outcrops invite us to reflect on the powerful forces that have shaped this land.
What exactly are koppies?
Koppie | ˈkɒpi |noun South African
A small hill in a generally flat area.
The word “koppie” comes from Afrikaans, meaning a small, usually rocky hill. It’s a term widely used in Southern Africa to describe these rugged formations. Rising above the landscape, they are formed when softer rock erodes away, leaving behind the harder, more resilient rock. Here at Londolozi, the koppies offer not just spectacular views but also serve as important landmarks for wildlife and explorers alike.
A Glimpse Beneath the Surface
As you stand on the top of Ximpalapala Koppie or Southern Cross Koppies, you might not realize there’s more to the story than what meets the eye. It turns out that these koppies share a deeper connection, lying along the same line—a dolerite dyke that runs through the reserve. This dyke stretches from the Northern Drakensberg Mountains to the Lebombo Mountains in the east, hinting at a fascinating geological history.
The Backbone of the Landscape
At Londolozi, these koppies are primarily composed of granite and dolerite—two very different types of rock with unique histories. Granite, found in places like Ximpalapala Koppie, formed around 3 billion years ago from slow-cooling molten rock deep beneath the Earth’s surface. This gave it a coarse, grainy texture made up of quartz, feldspar, and mica. Over time, natural forces such as wind and water eroded away the surrounding softer rock, leaving the harder granite standing proud. It’s why Ximpalapala, with its striking rounded boulders and rugged contours, remains a prominent feature on the landscape.
Ancient Origins
Dolerite, on the other hand, tells a different story. A dolerite dyke runs through the northern section of Londolozi, linking various koppies along a linear path. This rock was formed about 180 million years ago during a period of volcanic activity when molten magma intruded into existing cracks in the Earth’s crust. Unlike granite, dolerite cools relatively quickly, resulting in a finer-grained texture. It’s dark colour and mineral richness, with elements like iron and magnesium, give it a stark contrast against the paler granite.
The alignment of koppies along this dolerite dyke is no coincidence; the dyke’s presence created a natural line of resistance to erosion, allowing these koppies to persist while surrounding areas wore down over time. Essentially, what you’re seeing is a ridge of tougher rock standing the test of time, with the dolerite acting like a backbone running through Londolozi’s landscape.
Where Wildlife Finds Refuge
The contrast between the granite koppies and the dolerite ridges adds not only to the visual diversity but also to the variety of plant and animal life. The minerals released as these rocks weather enrich the soil, supporting unique vegetation and creating microhabitats that attract different wildlife. These koppies don’t just provide a backdrop for iconic wildlife sightings; they actively shape the environment and the living tapestry of Londolozi.
Connecting with the Past
The koppies at Londolozi are more than just scenic landmarks; they offer a window into the deep geological history that underpins this landscape. The dolerite dyke and granite outcrops tell a story of ancient processes that shaped the region, forming natural refuges and influencing the biodiversity that thrives here. From the shelter they provide for the Tsalala Pride to the unique vegetation that grows on their slopes, these rocky outcrops are woven into the very fabric of Londolozi’s wilderness.
Whether you’re climbing Ximpalapala Koppie, enjoying sundowners at Southern Cross Koppies, or simply gazing out at the horizon, you’re connecting not just with the present but with a timeline stretching back millions of years. These koppies remind us that this land has seen countless sunrises long before our time and will continue to do so long after. So next time you find yourself atop one, take a moment to pause and appreciate the incredible forces that have shaped the view before you. The story of Londolozi is etched into every rock and ridge; all you have to do is look a little closer. Stay tuned for a slightly deeper geological dive into Koppies.
So interesting and nice to read something we don’t think about when we think about Londolozi as we tend to focus on the fauna. Thanks Kels.
Thanks Ted, and it all is so interconnected! Hope to see you back here soon 🙂
Excellent article, Kelsey.
Thank you Ian
Hi Kelsey, how interesting to read your blog, it’s such a different and unique environment, with all the ecological implications. Every time I see luxurious vegetation I’m relieved! So moving to see the Tsalala family. The klipspringer is small, none the less it looks as the king of the koppies!
I’m glad you enjoyed it Francesca, the Klipspringer really is the true king of the koppies!
Very interesting story on the Koppel of Londolozi, with the dolerite Duke. Tsalala female and her cubs look so comfortable there in the Koppel.
Thank you Valmai, hopefully Tsalala will be using the koppie more in future.
Thanks for this interesting blog on the history of these Koppies. 3 billion years or also 180 million years are such an amazing amount of time, one cannot really imagine it. I have always found it totally fascinating how our planet earth has developed over those billions of years.
And apart from this fascinating history, the Koppies add so much beauty and diversity to the landscape of Londolozi and its neighbors.
Pleasure Christa, I’m glad you enjoyed it – it is so hard to imagine all those years ago and it really does add to the beauty of the landscape!
Kelsey, Thanks for in interesting info on Koppies! We have been to the top of Ximpalapala many times for sunsets and it holds a special place in out hearts! It is also the place where we first saw Mashaba when she was still Vomba Young female!
My pleasure Michael and Terri, I’m glad you have had the chance to go up Ximpalapala – it is a very special place! and what a special memory too 🙂
Thanks Kelsey for this fascinating report on the Koppies. I’ve seen them many times, although sadly never climbed to the top. Ximpalapala koppie area is where I saw Tsalala for the first time with her mother in ‘21. The grasses and the rocks were a perfect backdrop for the two of them. Geology is fascinating and I appreciate learning how the koppies came to be located here, knowing nothing about the dolerite dyke and how it i replays with the granite outcrops. I love that there is always something new to learn about the property that came to be Londolozi, not always associated with its animals.
Pleasure Denise! Perhaps you will have to climb up one of the koppies on your next visit as it sounds like you already have some special memories there. You never stop learning out here 🙂
Awesome Kelsey. Please take us to climb one of these majestic outcrops when we are back next month, we cannot wait.
Thanks Simon! We definitely will have to climb one of these koppies! Looking forward to welcoming you and the family back 🙂
I look forward to a future visit when I can get out and do a climb. The diversity of the land at Londolozi keeps revealing itself.
I’m glad to hear you are looking forward to the climb! So worth it 🙂