Côtes de Bordeaux
How to read this
Capitals mark the stressed syllable. The French r comes from the back of the throat. The recording is the reference.
1 appellation on 5 stretches of hillside that never touch, from the Gironde to the eastern edge of the department: red on its own, or red and white under one of 5 place names, on more than 10,500 hectares.
The place
The Côtes are the hills of Bordeaux that face its rivers:
The rules
The reds are Cabernet Sauvignon, Cabernet Franc, Malbec, also called Cot, and Merlot, with Carmenère under 10% and Petit Verdot under 15% of the vines, and Malbec must always be blended with another principal variety. The whites are Sauvignon, Sauvignon Gris, Sémillon and Muscadelle, with Colombard and Ugni Blanc to 15%, and only
The names
No classification. The appellation grew out of older ones: Premières Côtes de
- Colors
- Red; dry white under
Blaye , Francs and Sainte-Foy; sweet white under Francs and Sainte-Foy - Place names
Blaye ,Cadillac , Castillon, Francs, Sainte-Foy- Vineyard
- More than 10,500 hectares, 1,000 growers, 9 cooperatives; 500,000 hectoliters, 97% red
- Grapes
- Red: Cabernet Sauvignon, Cabernet Franc, Malbec, Merlot; Carmenère and Petit Verdot. White: Sauvignon, Sauvignon Gris, Sémillon, Muscadelle; Colombard and Ugni Blanc
- Density
- 4,500 vines a hectare at least; 5,000 at Castillon
- Yield
- Red 55 hectoliters, 52 with a place name, ceiling 65; dry white 62, ceiling 72
- Alcohol
- Red 11% natural, 11.5% with a place name; dry white 10.5%
- Release
- Reds from March 31 of the year after the harvest
- Classified
- No classification
- AOC since
- October 29, 2009; Sainte-Foy from 2016; cahier of June 4, 2026
Sources: FGVB, cahier des charges
The stack
The same land in
It shares named communes with
The appellations of Bordeaux are stacked, not laid side by side. The map draws the whole stack. Open the map
The pyramid of names shows what each step promises: vines a hectare, bottles, ripeness, day of sale, grapes. Climb from here
Terroir
More than a third of the delimited area, 37.5%, is sands and clays of old rivers and lakes (molasse). Near Bordeaux these sands are dry and riddled with burrows, which earned them the local name of fox sand (Sable de Renards).
A thread runs through all 4: the starfish limestone (calcaire à astéries), laid by an Oligocene sea that on its second advance reached as far east as Castillon and Sainte-Foy-la-Grande. It covers 11.1% of the total, and on the hillsides above the Garonne it forms the foot of the slope, cut by many quarries. Lakes left limestone here twice, ages apart: the Eocene lakes of Plassac in the Blayais, the Oligocene lakes of Castillon. Add them up, and the answer comes out plural.
- Slope wash and cover11.4%
- River and estuary deposits of today0.8%
- Ice age river terraces: sand, gravel, pebbles10.6%
- Landes sand and the oldest river deposits7.7%
- Shell sands (faluns), limestones and marls of the Miocene0.1%
- Agenais molasses: clays and sands above the limestone4.2%
- Starfish limestone and marine marls11.1%
- Lake limestones and clays7.0%
- Molasses: sands and clays of old rivers and lakes37.5%
- Older sea limestones and marls9.6%
Shares of the delimited area, measured on BRGM’s geological map, in families by the age and rock its legend prints, youngest first.
Half its delimited soil lies above 52 m, and 9 tenths lies between 15 and 98 m. 19.3% of it is steeper than 10%.
Measured section:
The line runs 26.0 km, from 21 m to 39 m. Inside the delimited area it lies between 24 and 96 m.
Colors: Slope wash and coverRiver and estuary deposits of todayIce age river terraces: sand, gravel, pebblesLandes sand and the oldest river depositsStarfish limestone and marine marlsLake limestones and claysMolasses: sands and clays of old rivers and lakesOlder sea limestones and marls
Tap the marker on the section, or open the borehole below: a core slides out, layer by layer.
1Drill here: Saint-Girons-d’Aiguevives, borehole 779-3-3, 355 m from the line
| Depth | As printed | In English | Age (ICS) |
|---|---|---|---|
| 0.0 to 8.0 m | inconnu | not identified | not given |
| 8.0 to 33.4 m | Sannoisien et Éocène supérieur | Sannoisian and upper Eocene | Sannoisian is an old French name for the base of the Oligocene, which begins 33.9 million years ago; the upper Eocene lies below it |
| 33.4 to 63.5 m | Éocène supérieur | upper Eocene | late Eocene; no stage is named |
| 63.5 to 75.2 m | Calcaire grossier de | Lutetian, as the |
Log printed in BRGM notice 0779, p. 42, under the heading “Saint-Girons-de-
Measured section:
The line runs 6.9 km, from -1 m to 99 m. Inside the delimited area it lies between 47 and 107 m.
Colors: Slope wash and coverRiver and estuary deposits of todayIce age river terraces: sand, gravel, pebblesLandes sand and the oldest river depositsAgenais molasses: clays and sands above the limestoneStarfish limestone and marine marls
Measured section:
The line runs 10.4 km, from 46 m to 10 m. Inside the delimited area it lies between 25 and 101 m.
Colors: Slope wash and coverRiver and estuary deposits of todayLandes sand and the oldest river depositsStarfish limestone and marine marlsLake limestones and claysMolasses: sands and clays of old rivers and lakes
Measured section:
The line runs 5.0 km, from 42 m to 43 m. Inside the delimited area it lies between 43 and 84 m.
Colors: Slope wash and coverRiver and estuary deposits of todayMolasses: sands and clays of old rivers and lakes
The units, as BRGM prints them
| Code | Name and age, as printed | Share |
|---|---|---|
| Slope wash and cover | 11.4% | |
| CFp | Formations superficielles | 10.2% |
| and 2 more units under 1% each, 1.2% in all | ||
| River and estuary deposits of today | 0.8% | |
| and 3 more units under 1% each, 0.8% in all | ||
| Ice age river terraces: sand, gravel, pebbles | 10.6% | |
| Fxb2 | Basses terrasses (RD Garonne) - Terrasse d'Izon (type 6), Saalien - "Riss" | 1.0% |
| Fxb1 | Basses terrasses (RD Garonne) - Terrasse d'Izon (type 6), Saalien - "Riss" | 1.4% |
| Fva(D) | Très hautes terrasses (RD Garonne) - Terrasse d'Artigues (type 1) indiférenciée, Waal - "Donau-Gunz" | 1.8% |
| Fu | Très hautes terrasses (RD Garonne) - Terrasse de Cénac, Eburonien - Donau | 5.3% |
| and 4 more units under 1% each, 1.0% in all | ||
| Landes sand and the oldest river deposits | 7.7% | |
| Ft(Sa) | Fmt de Sadirac, Tiglien - "Biber-Donau" | 6.4% |
| Ft(Bn) | Formation de Belin, Tiglien - "Biber-Donau" | 1.3% |
| and 2 more units under 1% each, 0.1% in all | ||
| Shell sands (faluns), limestones and marls of the Miocene | 0.1% | |
| and 2 more units under 1% each, 0.1% in all | ||
| Agenais molasses: clays and sands above the limestone | 4.2% | |
| g1-A | Molasse de l'Agenais inf. à facies argileux dominant, Rupélien continental | 3.2% |
| and 1 more unit under 1% each, 1.0% in all | ||
| Starfish limestone and marine marls | 11.1% | |
| g1-As | Calcaire à Astéries, Rupélien marin | 11.1% |
| Lake limestones and clays | 7.0% | |
| e7a-P | Groupe de Plassac - Calcaire de Plassac, Priabonien inf. continental interstratifié dans le groupe de Plassac | 6.0% |
| and 3 more units under 1% each, 1.0% in all | ||
| Molasses: sands and clays of old rivers and lakes | 37.5% | |
| g1a | Formation de Boisbreteau moy. et formation de la Garde, Rupélien inf. continental | 1.9% |
| e7-g1 | Molasses du Fronsadais indifférenciées, Priabonien sup. à Rupélien basal continental | 10.4% |
| e7-g1-A | Molasse du Fronsadais sup. à facies argileux dominant, Priabonien sup. à Rupélien basal continental | 1.1% |
| e7-g1-S | Molasse du Fronsadais sup. à facies sableux dominant, Priabonien sup. à Rupélien basal continental | 4.2% |
| e7c-A | Molasses du Fronsadais inf. à moy. (facies argileux dominant), Priabonien sup. continental | 2.2% |
| e7a-Mp | Groupe de Plassac - Molasse de Plassac, Priabonien inf. continental interstratifié dans le groupe de Plassac | 2.0% |
| e6-7 | Argiles à Paléotherium, Bartonien sup. à Priabonien inf. continental | 2.8% |
| e5-6 | Formation de Guizengard sup., Lutétien sup. à Bartonien sup. continental | 8.0% |
| e4b(1) | Formation de Guizengard inf., Yprésien sup. continental | 3.9% |
| and 4 more units under 1% each, 1.1% in all | ||
| Older sea limestones and marls | 9.6% | |
| e7b-Ms | Groupe de Plassac - Marnes à sismondia occitana et ostrea bernonensis (supérieures), Priabonien moy. marin | 2.1% |
| e7a-Ce | Groupe de Plassac - Calcaires de St Estephe, Priabonien inf. marin | 1.6% |
| e6b-Ac | Groupe de Plassac - Argiles à ostrea cucullaris, Bartonien sup. marin | 2.4% |
| e5-6(Bly3) | Formation du calcaire de | 2.9% |
| and 5 more units under 1% each, 0.6% in all | ||
Informative figures, computed from INAO’s digitized parcel delimitation of October 12, 2026 and BRGM’s harmonized geological map (BD Charm-50); heights from IGN’s RGE ALTI 5 m. The plans held at the town hall are the legal reference. The delimited area is always somewhat larger than what is planted.
Sources: BRGM, Notice explicative de la feuille Bordeaux à 1/50 000, 1977; BRGM, Notice explicative de la feuille
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