The estate soils have been formed from sediments from the Garraf Massis, deposited thousands of years ago. One of the most characteristic features of the estate’s soils is the presence of accumulations of calcium carbonate. The movement of water through the soil dissolves the carbonates and takes them to a certain depth. The continuous repetition of this process has ended up producing the accumulation of these deposits. When these become massive, after thousands of years, they bind together and form a hard stratum called a petrocalcic horizon. This hard stratum limits the availbility of water to the vine and the production, but is a factor that gives the grape quality
The wine offers a straw yellow color, clean, transparent, fine, and persistent bubbles with a rosary formation. In the nose fresh pear aromas stand out along with delicious notes of pastry cream, white flowers, and candied fruits. On the palate, good balance and acidity. Powerful and flavorful with white flowers and notes of brioche, almond and great length.