Eisenberg

Styles

Principal grape varieties

Terroir

• Subsoil of heavy, iron-rich loam and basalt soils with a high iron content
• High mineral content in the soil: potassium, calcium, sodium, and phosphorus
• The pannonisches Klima–illyrisches Klima with large diurnal temperature swings shapes the wines
• The influence of the crystalline bedrock yields fruitiness, a lean extract structure, and minerality
• The hilly topography of the Eisenberg region forms its defining landscape relief

• The cross-generational transmission of traditional winemaking styles by family estates shapes the character of Eisenberg wines.
• Vines are trained exclusively in high-trellis Drahtrahmen culture; direct sales from the estate are widespread.

• Eisenberg wines display pronounced fruitiness, a lean extract structure, and dominant minerality.

• Iron-rich loam/basalt soils combined with pannonisches Klima–illyrisches Klima yield pronounced fruitiness, a lean extract structure, and dominant minerality.

Facts drawn from the cahier's terroir-link section (Lien au terroir) by automatic interpretation — see the source.

Sources

• Specification (EUR-Lex, single document)
• eAmbrosia register (EU) — File number PDO-AT-A0215
• Official trade body site — Verein EisenbergDAC