Haut-Benauge
How to read this
Capitals mark the stressed syllable. “zh” is the s in “measure”. “eu” is “ay” said with rounded lips. “ahn” is a nasal vowel: say it through the nose, with no n. The French r comes from the back of the throat. The recording is the reference.
1 place name that 2 appellations may add, in the hills of the
The place
The Haut-Benauge is hill country in the middle of the
The rules
Neither of the 2 is an appellation on its own. Haut-Benauge is a place name added after
The names
No classification. Bordeaux was recognized on November 14, 1936 and the
- Colors
- White: dry as
Entre-deux-Mers Haut-Benauge ; dry or sweet asBordeaux Haut-Benauge - Communes
- Escoussans, Gornac, Ladaux, Mourens, Porte-de-Benauge, Saint-Pierre-de-Bat, Soulignac, Targon
- Vineyard
- 45 hectares and no more than 10 growers for
Entre-deux-Mers Haut-Benauge - Soil
- Molasse of clay and sand on 67%; starfish limestone and old river gravel
- Grapes
- Sémillon, Sauvignon, Sauvignon Gris, Muscadelle; Colombard and Ugni Blanc also for
Entre-deux-Mers Haut-Benauge - Density
- 4,500 vines a hectare for
Entre-deux-Mers Haut-Benauge - Yield
Entre-deux-Mers Haut-Benauge 65 hectoliters, ceiling 75;Bordeaux Haut-Benauge 55, ceiling 60- Alcohol
Entre-deux-Mers Haut-Benauge 10.5% natural;Bordeaux Haut-Benauge 11.5%- Classified
- No classification
- AOC since
Entre-deux-Mers 1937, Bordeaux 1936; the name Haut-Benauge since 1955
Sources: FGVB, cahier des charges
The stack
The same land in Haut-Benauge may also be labeled Bordeaux,
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
Around Gornac, a plow or a new ditch can turn up oyster shells more than 10 centimeters across. They come as a surprise, because most of this soil was laid down by rivers and lakes. Their clays and sands, the Agenais molasse, cover 67.0% of the delimited area, and the upper layers show those rivers losing strength, their channels giving way to an ever quieter floodplain.
Then the sea slipped back in, briefly. At Laurès, east of Gornac, it left a layer too thin to show on the map. Around Mourens and Gornac it made its last arrival recorded on the map sheet, a bed of sandy limestone.
At Meyssan, near Cantois, a clay pit laid bare what lies beneath the molasse: the starfish limestone (calcaire à astéries), sometimes with oyster and sand dollar debris at the contact, from another brief visit of the sea. The pit's clay went to a tile and brick works near Gironde-sur-Dropt. Small quarries at Escoussans and Arbis cut the limestone itself for ornamental stone, ballast and lime, and most of them closed. In the old quarry faces at Arbis, sea urchins and corals survive as molds. The sea came back to these hills as a guest.
- Slope wash and cover9.2%
- River and estuary deposits of today0.4%
- Landes sand and the oldest river deposits9.1%
- Shell sands (faluns), limestones and marls of the Miocene3.1%
- Agenais molasses: clays and sands above the limestone67.0%
- Starfish limestone and marine marls10.4%
- Lake limestones and clays0.8%
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 74 m, and 9 tenths lies between 50 and 106 m. 18.1% of it is steeper than 10%.
Measured section
The line runs 11.2 km, from 64 m to 50 m. Inside the delimited area it lies between 40 and 106 m.
Colors: Slope wash and coverRiver and estuary deposits of todayLandes sand and the oldest river depositsShell sands (faluns), limestones and marls of the MioceneAgenais molasses: clays and sands above the limestoneStarfish limestone and marine marlsLake limestones and clays
The units, as BRGM prints them
| Code | Name and age, as printed | Share |
|---|---|---|
| Slope wash and cover | 9.2% | |
| CFp | Formations superficielles | 9.2% |
| River and estuary deposits of today | 0.4% | |
| and 1 more unit under 1% each, 0.4% in all | ||
| Landes sand and the oldest river deposits | 9.1% | |
| Ft(Sa) | Fmt de Sadirac, Tiglien - "Biber-Donau" | 9.1% |
| Shell sands (faluns), limestones and marls of the Miocene | 3.1% | |
| m2-G | Grès à Miogypsines, Burdigalien marin | 2.0% |
| m1-Ma | Marnes à Ostrea aginensis, Aquitanien inf. marin | 1.1% |
| and 1 more unit under 1% each, 0.0% in all | ||
| Agenais molasses: clays and sands above the limestone | 67.0% | |
| g2-A | Molasse de l'Agenais sup. à faciès argileux dominant, Chattien continental | 31.0% |
| g1-A | Molasse de l'Agenais inf. à facies argileux dominant, Rupélien continental | 36.0% |
| Starfish limestone and marine marls | 10.4% | |
| g1-As | Calcaire à Astéries, Rupélien marin | 10.4% |
| Lake limestones and clays | 0.8% | |
| and 1 more unit under 1% each, 0.8% 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 Podensac à 1/50 000, 1996; INAO parcel delimitation (file of 2026-10-12) laid over BRGM BD Charm-50 Gironde, harmonized geological map.
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