Marchesi di Barolo Barolo Sarmassa 2008

The southeast-facing Sarmassa vineyard is located on a hill with good slope. Despite the fact that the area is of Tortonian origin, there has been a significant amount of soil erosion, probably due to the steep slope of the hill. The soil is composed mainly of clay and limestone and has a very substantial percentage of stones. The high percentage of stones, combined with clay, limit the growth of Nebbiolo grape and allow the vines to react quickly to climactic variations, enabling clusters to achieve a perfect ripening. (On the sheet N.9 of the community of Barolo, lots 104, 149, 157, 303). [+]