Tasks and Days

 

The full range of vines can only be demonstrated and appreciated by exploring the soil as a whole!

 

So here is a brief account of the long saga of Alsatian vintages, genuine relations that tell all the secrets of the local soil and its complex geology.

Beblenheim: soils in the heart of the Ribeauvillé group of faults

"Native soil tang is the result of a combination of climatic characteristics (pluviometry, temperatures, exposure) the location (slope, stoniness and rockiness, planning (parcelling) and the type of ground (pedology)."

 

 

 

 

The Alsatian vineyards stretch from the faults of the Vosges to those of the Rhine, which have been there for 50 million years. These groups of faults are at their most complex in Beblenheim, where their mosaic-like structure leaves its mark on the landscape. The soils here are divided to the extreme, and a single geological stage is sometimes represented by just a few hectares. Vine formation on the surface is even more complex as a result of deposits of tertiary conglomerates followed by the contents of the rivers of the Vosges in the quaternary period and lastly the modern phenomenon of erosion.
Various different soils exist in the estate. On the uppermost slopes, brown chalky argillaceous soils on Oligocene calcareous clay can be found alongside compact Lias soils.

 

The ground on the intermediary slopes is often made up of brown calcic soils on Lias clay covered with pebbles. There are also some brown calcic soils on Oligocenous conglomerates, loamy- argillaceous-sandy soils, generally towards the bottom of the slopes.