Chablis
Oyster marl on the slopes, a limestone lid on top.
Chablis is one small river cutting through a table of limestone. The Serein runs north past the town, and its side valleys break the land into slopes. The slopes are Kimmeridgian, about 155 million years old: grey marl in beds with thin marly limestone, full of a fossil oyster the size of a fingernail, Exogyra virgula. The flat tops above are capped with Portlandian, a younger, harder limestone with little clay. The appellations follow the rock: grand cru, premier cru and Chablis on the Kimmeridgian slopes, Petit Chablis mostly on the Portlandian of the upper slopes and plateaux, at about 230 to 280 m. All seven grands crus share one hill on the right bank, looking south-west across the river at the town. Spring frost is the other constant; growers have lit heaters in the vines since 1959.
Our two growers work both sides of that line. The Dauvissats farm from Beine, in the cold side valley west of Chablis. Their Beauroy is one parcel at the eastern end of the climat, in the Côte de Savant, facing south-west above the lake at Beine; Florent says the lake “definitely has an impact on the microclimate”, with morning mists and slower ripening. Across the river, Les Brèches de Fyé faces south at Bréchain, below the plateau, carrying on from the grand cru Blanchot. Their Petit Chablis, Les Deux Terres, is named for its two grounds: clay on the plateau at Beine near Vau Ligneau, and hard Portlandian limestone on the plateau above Fyé. Yannick Cadiou’s Chablis and La Côte d’Or are on the left bank under Montmains, facing Vaillons; his Petit Chablis is the stony plateau at Lignorelles, the first vine he planted, in 1996.
Tap any two to compare them and cut a slice between them: Bréchain against the plateau above it shows the step from marl to hard limestone in under a kilometre. Lieux-dits are placed from the BIVB’s map of Burgundy’s lieux-dits; five pins are approximate, as the caption explains. Stéphanie Colinot’s Irancy, about 15 km to the south-west, has its own plate (XIV).
Curve shapes are illustrative; the size of each swing is from published figures.
Soils from the growers (Dauvissat and Cadiou, via our producer pages) and the BIVB. Soil depths are not published, so the pits are drawn to suggest the ground, not to scale.
Every producer on this plate
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How the ground is shown: there is no open soil map at the scale of a lieu-dit, so colours and pits follow what the growers and the BIVB describe. Heights and slopes come from the elevation data.
Heights marked as the grower's figure come from our producer notes; others are read off the elevation data at the pin. Soil notes come from the producers' technical sheets.
Sources: elevation from AWS Terrain Tiles (EU-DEM and other public data); geology, appellation heights and frost history from the BIVB (chablis-wines.com: Special soil, A unique climate, Petit Chablis, Chablis Grand Cru, the Climats of Chablis); parcels and soils from Agnès, Didier and Florent Dauvissat and from Yannick Cadiou, via our producer pages; lieux-dits from the BIVB’s Bourgogne Maps. Quotations as attributed.