A Terroir Unlike Any Other
Since 2018, Springfontein has held what is reverently known in Burgundy as a “monopole”: an appellation of its own, registered as Springfontein Rim. It recognises what our vines have been telling us from the beginning — that this small piece of land in Walker Bay is markedly different, not only from the better-known Cape Winelands, but even from our immediate Kleinrivier neighbours.
When we began developing the farm nearly thirty years ago, established figures in the South African wine industry warned us, half in jest, that we might manage nothing better than good vinegar here. They had reason to be sceptical. Springfontein sits on a sparse, alkaline limestone terroir, shaped by a cool coastal microclimate and a hydrological and biological system of its own.
It took years to understand how these elements work together. Today, they are at the heart of what makes Springfontein what it is.
The Microclimate
Springfontein lies between the Atlantic Ocean and the Kleinrivier Mountains, which rise to almost 1,000 metres immediately to our north. The mountains form a natural barrier for weather systems moving up from the south, while the cold Benguela Current keeps the surrounding waters cool.
The result is a remarkably moderate growing environment. Summer temperatures rarely climb far above 26°C, nights remain cool, and a steady breeze moves through the vineyards. Overcast conditions are common, and rainfall is spread relatively evenly across the year.
These conditions slow down ripening and give the grapes more time to develop. Sugar accumulation can progress alongside the physiological ripeness of skins, seeds and stems, while the difference between day and night temperatures helps retain freshness and build aromatic complexity.
The constant movement of air is equally important. It keeps the canopy dry and reduces pressure from fungal disease, allowing us to work with a very restrictive spraying regime.
The Soil
At the heart of Springfontein lies a small, lentil-shaped parcel of limestone. Geologically, it belongs to the Waenhuiskrans and Klein Brak formations of the chalk-dominated Bredasdorp Group.
It is a remarkably limited resource. The limestone runs out at the northern edge of the farm, where the Klein River passes through, and extends only a few metres beyond our southern boundary. Around it lie very different, generally more fertile and acidic soils — weathered granite and clay slate — that dominate much of the surrounding wine-growing landscape.
For vines, limestone creates a particular set of conditions. Its alkalinity naturally limits vigour and yield, meaning that we do not need to impose the same degree of artificial crop restriction. The soil also contributes to a naturally fresh acidity in the grapes, while its relatively low heat storage helps keep ripening gradual.
But perhaps more important than any individual characteristic is the fact that this is not a typical Cape vineyard soil. The vines have to work differently here, and the wines reflect that.
The Hydrology
The story continues below the limestone. Our limestone formation sits above a relatively impermeable section of the Bokkeveld Group, within a geological depression that narrows towards Stanford. The area is bounded by the Kleinrivier Fault to the north and the Akkedisberg–De Kelders Fault to the south.
Water moving through the surrounding geological formations collects beneath the limestone, forming a substantial groundwater system fed primarily by the Stanford Aquifer, with additional contribution from the Nardouw Aquifer to the southwest.
At the edges of the limestone, the underlying bedrock can still be seen in places, including around the entrance to the farm.
Springfontein’s own spring provides the water we use for irrigation. It is one of the reasons we can farm this relatively dry piece of land without forcing the vines into unnecessary stress, while remaining mindful of the resource beneath our feet. Water here is not simply something we add to the vineyard. It is part of the geological system that makes the place what it is.
The Biotope
The limestone shapes more than the vines. Springfontein forms part of the Cape Floristic Region, but unlike most vineyards in the Western Cape, which grow predominantly on acidic Table Mountain Sandstone, our land supports a regionally rare form of Limestone Proteroid Fynbos.
More than a hundred unusual plant species are associated with this vegetation. Together they create a dense and highly diverse biological environment that extends far beyond the vineyard rows. That matters to us not only because the fynbos is part of the landscape, but because the vineyard exists within it.
The plants attract insects, bees and birds. Their aromas and organic matter contribute to the environment around the vines. And the microorganisms living in this landscape — together with those in the vineyard and cellar — form part of the biological world from which our spontaneous fermentations begin.
The ecosystem is not always convenient. The dense vegetation, together with invasive species such as Rooikrans and Port Jackson, makes fire an ever-present risk. We have experienced several serious fires over the years, including the 2013 fire that destroyed more than three hectares of vineyard. Cape starlings create a different kind of pressure during harvest, sometimes pecking whole bunches rather than individual berries and leaving exposed juice to ferment in the vineyard. These are simply part of farming here. The same landscape that creates challenges also gives Springfontein much of its character.
The Vines
Everything we plant here has to make sense within this environment. Springfontein increasingly concentrates on two South African varieties: Pinotage and Chenel.
Pinotage was created in 1925 by Abraham Perold, the first professor of viticulture at Stellenbosch University, by crossing Pinot Noir and Cinsault.
Chenel followed almost fifty years later, bred by Christiaan Orffer, who succeeded Perold in the same chair and played a major role in the development of South African wine science.
Neither variety is a mainstream international grape. Both, however, are part of South Africa’s own viticultural history — and both have proved capable of finding an individual expression on our limestone. Alongside them, we grow smaller quantities of established European varieties, mainly as blending partners. Depending on the site, our vines are trained as single stakes, bush vines or on classic trellises.
Within Springfontein Rim, several individual parcels stand out even from the rest of the farm. Jonathan’s Ridge and Jil’s Dune are two such sites. We vinify their grapes separately, allowing the differences between individual pieces of ground to remain visible in the wines.
Farming With the Place
For us, terroir is not something that begins with a bottle label. It starts with how the land is farmed.
Springfontein has followed organic principles since the beginning, and the estate has been Ecocert-certified since 2019. We use no chemical fertilisers and work with an extremely restrictive spraying regime. The cool climate, limestone soils, wind and surrounding vegetation all contribute to making this possible.
We also grow and select an increasing number of young vines ourselves, alongside certified nursery material, including ungrafted vines where conditions allow.
The aim is not to make the vineyard independent of its surroundings. Quite the opposite. We want to keep the relationship between soil, vines, microorganisms, climate and wider landscape as intact as possible.
From Land to Wine
The limestone, the climate, the groundwater, the fynbos and the vines are not separate stories. They are parts of one place. Our job is to understand that place, farm it carefully and then interfere as little as possible in the cellar.
Everything we do ultimately has the same purpose: to let the character of this particular piece of land arrive, unforced, in the glass.