Since 1797, on the prestigious terroirs of Vosne-Romanée and Vougeot, our vineyards have offered the Estate their precious fruit. From these terroirs , we produce fourteen different wines, including la Grande Rue, a monopole of the Estate, one of the rare grands crus of Vosne-Romanée.
The Lamarche Estate, which now boasts a total surface area of nearly 28 acres, is a family firm, whose origin goes back several generations. We have adopted integrated viticulture for all our vineyards, and we try to express both our terroir and our history in our wines. They all have in common that elegance which combines exceptional balance and a delicate nose.
The Clos de Vougeot in the heart of the Côte de Nuits occupies most of the vineyard area belonging to the commune of Vougeot. Vougeot's neighbours are Chambolle-Musigny, Flagey-Échezeaux and Vosne-Romanée. On the slopes at the upper end of the Clos, it abuts on the vineyards of Musigny and Grands-Échezeaux.
Founded around 1110 AD by the monks of nearby Cîteaux, who remained its owners until the Revolution of 1789, the Clos de Vougeot is a Burgundian icon. Its 50.59 hectares have never been broken up and it retains its identity intact within the walls which were built to enclose it 5 centuries ago. Its wines are among the finest of the Grand Cru reds and it has held Grand Cru status since 31 July 1937.
The château, (which adjoins the cellars and the winery with its giant presses dating back to the 12th and 14th centuries), is built in the Burgundian Renaissance style and is open to visitors. The Confrérie des Chevaliers du Tastevin holds its meetings or "chapters" here and therefore it is no surprise that the finest food and wine in France is found here.
The diversity of soils within the Clos de Vougeot makes up a sort of needle-point tapestry. At about 255 metres above sea-level, its upper end is gently sloping, with soil only some 40 cm deep, coarse-grained and gravelly over a limestone base. In the centre, at about 250 metres of altitude, the soil is still shallow (45 cm), brown, more clayey, overlying broken limestone. The lower portion (around 240 metres) has a brown soil which is deeper (90 cm) and lies on a layer of marl, rich in clay and alluvium. The rocks belong to the Jurassic period (175 million years BC).