TERROIR
HEMEL-EN-AARDE REGION
The HEMEL-EN-AARDE VALLEY
The overwhelming majority of the vineyards in this appellation are planted on northeast, north and northwest facing slopes of Bokkeveld Shale-derived soil on the southern side of the Onrus River. This soil has an unusually high clay content. The clay content of these soils approximate that of the Cote D’Or in Burgundy, although they tend to be shallower and far stonier. In addition, they do not have the limestone content or limestone bedrock, but have pure clay subsoil and solid shale bedrock. For the South African winelands, these soils would be classified as low-vigour and more
marginal.
Higher up the northern slopes and on the south-facing slopes of the valley, the soils are Table Mountain Sandstone-derived. These quartzitic, sandy soils have a very low to non-existent clay content, and are light structured, generally far deeper and have the potential for greater vigour.
UPPER HEMEL-EN-AARDE VALLEY
HEMEL-EN-AARDE RIDGE
Bokkeveld Shale-derived soils re-occur in the Hemel-en-Aarde Ridge and the overwhelming majority of the vineyards are on these stony, clay-rich soils. The vineyards are planted with many different aspects from southerly to northerly, and the average altitudes of these vineyards are the highest of the three Hemel-en-Aarde Region appellations. The highest mountain slopes of this appellation have lighter structured Table Mountain Sandstone-derived soils.
