Istočna kontinentalna Hrvatska
Styles
Principal grape varieties
ChardonnayGraševina (Welschriesling)Kerner Bijeli (Kerner)Manzoni Bijeli (Manzoni Bianco)Moslavac (Furmint)Muškat Bijeli (Muscat A Petits Grains Blancs)Muškat Ottonel (Muscat Ottonel)Muškat Žuti (Moscato Giallo)NeuburgerPinot Bijeli (Pinot Blanc)Pinot Sivi (Pinot Gris)Radgonska Ranina (Bouvier)Rajnski Rizling (Riesling Weiss)Ranfol (Ranfol Beli)Rizvanac (Mueller Thurgau Weiss)Ružica CrvenaSauvignonSemillonSilvanac Zeleni (Silvaner Gruen)Traminac Bijeli (Savagnin Blanc)Traminac Crveni (Gewuerztraminer)Verduzzo (Verduzzo Friulano)Viognier Bijeli (Viognier)Zelenac Slatki (Rotgipfler)Alicante Bouschet (Alicante Henri Bouschet)BlauburgerCabernet FrancCabernet SauvignonFrankovka (Blaufraenkisch)Gamay Bojadiser (Gamay Teinturier Freaux)Gamay Crni (Gamay Noir)KadarkaMalbec Crni (Cot)MerlotMuškat Crveni (Tamjanika Crna)Nebiolo (Nebbiolo)Pinot Crni (Pinot Noir)Portugizac (Portugieser Blau)SyrahTribidrag (Primitivo)Zweigelt (Zweigeltrebe Blau)
Terroir
Natural factors
- The western part of the region is formed by the Slavonian hills, with peaks at Psunj (984 m a.s.l.), Papuk (953 m a.s.l.), Krndija (752 m a.s.l.) and Dilj (471 m a.s.l.), while the plains of Podravina and Posavina extend to the north and south.
- The core of these hills consists of Palaeozoic igneous and metamorphic rocks, partly overlain by carbonate non-clastic sediments such as limestones and dolomites from the Mesozoic era.
- Terraces and plateaux at elevations of 95 to 230 m above sea level are covered by a thick aeolian loess mantle ranging from 17 to 24 m in depth, and in some locations such as Baranjska planina and Erdutsko brdo exceeding 100 m.
- In the eastern part of the region, terrace and plateau sediments occur as carbonate loess, while towards the west the CaCO₃ content decreases, transitioning into non-calcareous, pseudogley and marbled sediment.
- The climate of this area is moderately continental, with a mean annual temperature of 10.9 to 11.2 °C, a sum of effective temperatures of 1,450 to 1,650 °C, and annual precipitation of 650 to 890 mm distributed evenly throughout the year.
Human factors
- Historical records of viticulture and winemaking in this area are linked to Emperor Probus (232–282 AD), and it is assumed that the vine was cultivated even earlier, in the pre-Roman Celtic and Illyrian-Japodian periods.
- With the appearance of phylloxera in 1890 in the Istočna kontinentalna Hrvatska area, a new era of vineyard restoration began, involving the planting of American rootstocks, field grafting, and the replacement of the existing assortment with higher-quality cultivars.
Product characteristics
- The white wines of this region are crystal clear, ranging from yellow-green to golden yellow in colour, of medium to high alcoholic strength, with balanced and moderate acidity, good extract, and discrete to pronounced fruity, floral and spicy aromas.
- The red wines, among which Frankovka, Cabernet Sauvignon, Merlot and Pinot noir predominate, are clear, ruby red of varying intensity, medium to high in alcoholic strength, with moderate acidity, moderately ripe tannins, and pronounced fruity aromas.
Terroir / wine link
- The continental climate produces greater diurnal temperature variation, which favours the preservation of acidity during grape ripening, while high daytime temperatures promote sugar accumulation in the grapes.
Facts drawn from the specification's terroir-link section by automatic interpretation — see the source.
About this boundary · approximate area
Approximate area — the Bétard 2022 dataset polygon (EU PDOs), at municipality resolution.
Sources
- eAmbrosia register (EU) — File number PDO-HR-A1651
- Official trade body site — Graševina Croatica – Udruga vinara Slavonije i hrvatskog Podunavlja