Reynard (Cornas Lieu-Dit)

Reynard occupies the central part of the Cornas hill, a steep south-facing slope on the right (west) bank of the Rhône River near the town of Cornas, between the villages of Saint-Péray to the north and Saint-Joseph to the south. The lieu-dit sits at moderate elevation (approximately 200 to 300 metres), with terraces climbing the granite hillside on aspect that captures maximum afternoon and evening sun. Slope gradients reach 50 to 60 degrees on the steepest sections, requiring traditional stone-walled terraces (called murets locally) and hand or horse cultivation throughout. The lieu-dit is bounded by other prestigious Cornas sectors including La Côte to one side and the broader Reynard sector extending to nearby parcels. The granite tail of the Cornas hill forms a distinctive crystalline outcrop visible from the riverside road, with the named lieux-dits including Reynard arrayed across the south-facing terraces.

• Central section of the Cornas hill on the right (west) bank of the Rhône, between Saint-Péray and Saint-Joseph
• South to south-southwest aspect with terraces climbing from approximately 200 to 300 metres elevation
• Slope gradients of 50 to 60 degrees on the steepest sections, requiring traditional stone-walled terraces (murets)
• The granite tail of the Cornas hill forms a distinctive crystalline outcrop visible from the riverside road

Reynard sits on Hercynian (Variscan) granite bedrock approximately 300 to 350 million years old, the same age class as the Hermitage hill, the Côte Blonde of Côte-Rôtie, and the granite Grand Crus of Alsace. The granite here is exposed near the surface in many parcels, with thin, sandy, decomposed-granite topsoils called arzelle (or arène in standard French granite-terroir vocabulary), derived from millennia of weathering of the parent crystalline rock. The soils are nutritionally poor, slightly acidic, well-drained, and force vine roots to penetrate deeply through fissures in the bedrock to reach water and minerals. Drainage is rapid through the granite-fissure system, but the steep south-facing slope and Mediterranean climate of the Cornas valley produce some of the warmest growing conditions in the Northern Rhône. The mineralogy contributes a bright, vertical mineral signature to wines, with iron, graphite, and savory mineral lift layered onto the dark Syrah fruit core. The combination produces the most uncompromising granite-driven Syrah expression in the Northern Rhône.

• Hercynian (Variscan) granite bedrock approximately 300 to 350 million years old, exposed near the surface in many parcels
• Surface soils: thin, sandy, decomposed-granite (called arzelle locally) with rapid drainage and minimal organic matter
• Nutritionally poor, slightly acidic, well-drained soils force deep root penetration through granite fissures
• Mineralogy contributes bright vertical mineral signature; iron, graphite, savory mineral lift in finished wines

Reynard produces some of the most powerful, structural, mineral-driven Syrahs in the Northern Rhône. The combination of decomposed-granite soils, steep south-facing aspect, old-vine plantings (some dating to the early twentieth century from Noël Verset and other historical Cornas vignerons), and traditional whole-cluster fermentation by the leading producers creates wines of deep purple-black color, intense tannin grip, savory mineral-driven aromatic register, and long aging trajectories. Aromatically the lieu-dit shows blackberry, blueberry, black olive, iron, graphite, smoked meat, leather, garrigue, and savory mineral lift; the palate carries firm structural tannin, bright natural acidity (granite signature), and a long savory mineral finish. With bottle age (15-plus years) the wines develop tertiary leather, dried game, tobacco, and forest floor while retaining the granite-driven mineral grip. Aging trajectories at the highest level (Allemand Cornas Reynard, Clape Cornas) run two to four decades, with some celebrated bottles aging well beyond. The lieu-dit's stylistic signature is the heart of Cornas's identity as the most uncompromising pure-granite Syrah expression in France.

• Most powerful, structural, mineral-driven Syrahs in the Northern Rhône; deep purple-black color and intense tannin grip
• Aromatic register: blackberry, blueberry, black olive, iron, graphite, smoked meat, leather, garrigue, savory mineral lift
• Granite-driven bright natural acidity and long savory mineral finish; tertiary leather and dried game develop with bottle age
• Aging trajectory: two to four decades at the highest level; the heart of Cornas's identity as pure-granite Syrah

Thierry Allemand is the most celebrated current producer working Reynard. His Cornas Reynard cuvée draws fruit from the oldest and best parcels in his roughly 5-hectare estate, including the legendary old-vine plot purchased from Noël Verset (whose plantings dated to the early twentieth century and represent some of the most pre-phylloxera-style genetic material remaining in Cornas). Allemand's Reynard is fermented with whole clusters, raised in seasoned oak with minimal new wood, and bottled without fining or filtration, producing one of the most uncompromising traditional Cornas wines made. Domaine Auguste Clape (founded by Auguste in the 1950s, now run by his great-grandson Pierre-Marie Clape, fourth generation) farms parcels adjacent to Allemand's Reynard holdings. The Clape estate Cornas blend draws heavily from this sector and is among the most age-worthy wines in the appellation, with vintages from the 1980s and 1990s still showing structural integrity today. Vincent Paris, Thierry Allemand's nephew and a close protégé, produces his own single-vineyard Cornas Reynard cuvée from old-vine plantings. Other producers with parcels in or adjacent to Reynard include Domaine du Tunnel (Stéphane Robert), Eric and Joël Durand, Alain Voge (now run by Albéric Mazoyer), Domaine Courbis, and Jean-Luc Colombo, though the dominant Reynard reputation rests primarily on Allemand, Clape, and Paris.