2019 Domaine Dujac - Morey St. Denis - 3 Garrafas (0,75 L)
N.º 85639807
![2019 Domaine Dujac - Morey St. Denis - 3 Garrafas (0,75 L) #1.1](https://assets.catawiki.com/image/cw_ldp_l/plain/assets/catawiki/assets/2024/6/24/b/2/8/b28900ba-6fc9-40d2-9355-6cfe48f9b269.jpg)
![2019 Domaine Dujac - Morey St. Denis - 3 Garrafas (0,75 L) #1.2](https://assets.catawiki.com/image/cw_ldp_l/plain/assets/catawiki/assets/2024/6/24/6/0/3/603f5c53-65e4-4393-84b0-f5c64bb6dbdf.jpg)
![2019 Domaine Dujac - Morey St. Denis - 3 Garrafas (0,75 L) #2.1](https://assets.catawiki.com/image/cw_ldp_l/plain/assets/catawiki/assets/2024/6/24/b/9/f/b9fbbe5e-dba0-40bc-83d5-05abc812a4d9.jpg)
The Morey-Saint-Denis white wine comes from 2 parcels located within the Porroux climate, east of the village of Morey-Saint-Denis, at the bottom of the slope where the slope is the least steep. The vineyards face north-east. The white Moreys are located just above the cellar plot of the red Morey-Saint-Denis. This particular location was chosen for the Chardonnay planting because the RD 974 blocks the cold air coming down from the hill and brings a natural acidity to the wine. The soil is rich in silt with fewer rocks on the hillside but Comblanchien limestone cobbles may be present. Two distinct substrates make up the subsoil of the Morey-Saint-Denis village cuvée. According to the plot, we can find fine deposits put in place when the collapse fissure closed over millions of years or the spreading of alluvial cones at the mouth of the Morey-Saint-Denis valley.
The Morey-Saint-Denis white wine comes from 2 parcels located within the Porroux climate, east of the village of Morey-Saint-Denis, at the bottom of the slope where the slope is the least steep. The vineyards face north-east. The white Moreys are located just above the cellar plot of the red Morey-Saint-Denis. This particular location was chosen for the Chardonnay planting because the RD 974 blocks the cold air coming down from the hill and brings a natural acidity to the wine. The soil is rich in silt with fewer rocks on the hillside but Comblanchien limestone cobbles may be present. Two distinct substrates make up the subsoil of the Morey-Saint-Denis village cuvée. According to the plot, we can find fine deposits put in place when the collapse fissure closed over millions of years or the spreading of alluvial cones at the mouth of the Morey-Saint-Denis valley.
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