2021 FX Pichler Gruner Veltliner Klostersatz Federspiel

The Ried Klostersatz is, as the name suggests, one of the oldest vineyards in the Wachau to be cultivated by the monks of Bavarian and Salzburg monasteries.The Ried Klostersatz is, as the name suggests, one of the oldest vineyards in the Wachau to be cultivated by the monks of Bavarian and Salzburg monasteries.

It is a vineyard with a remarkably deep soil composition situated in the Loibner basin, within the majestic curve of the Danube river between Dürnstein and Oberloiben. The topsoil is characterized by fine sand particles, which indicate a slow flow rate during the deposition. The underlying gravel, on the other hand, was deposited at a high flow rate. The high degree of rounding of the pebbles is evidence of a long transport route from the Alps.The Ried Klostersatz is, as the name suggests, one of the oldest vineyards in the Wachau to be cultivated by the monks of Bavarian and Salzburg monasteries. It is a vineyard with a remarkably deep soil composition situated in the Loibner basin, within the majestic curve of the Danube river between Dürnstein and Oberloiben. The topsoil is characterized by fine sand particles, which indicate a slow flow rate during the deposition. The underlying gravel, on the other hand, was deposited at a high flow rate. The high degree of rounding of the pebbles is evidence of a long transport route from the Alps.It is a vineyard with a remarkably deep soil composition situated in the Loibner basin, within the majestic curve of the Danube river between Dürnstein and Oberloiben. The topsoil is characterized by fine sand particles, which indicate a slow flow rate during the deposition. The underlying gravel, on the other hand, was deposited at a high flow rate. The high degree of rounding of the pebbles is evidence of a long transport route from the Alps.The Ried Klostersatz is, as the name suggests, one of the oldest vineyards in the Wachau to be cultivated by the monks of Bavarian and Salzburg monasteries.

It is a vineyard with a remarkably deep soil composition situated in the Loibner basin, within the majestic curve of the Danube river between Dürnstein and Oberloiben. The topsoil is characterized by fine sand particles, which indicate a slow flow rate during the deposition. The underlying gravel, on the other hand, was deposited at a high flow rate. The high degree of rounding of the pebbles is evidence of a long transport route from the Alps.