Zagorje – Međimurje
Styles
Principal grape varieties
Belina HižakovoChardonnayDišeća Belina BijelaGraševina (Welschriesling)JohanniterKerner Bijeli (Kerner)KraljevinaLipovina (Harslevelue)Manzoni Bijeli (Manzoni Bianco)MerzlingMirkovača (Galbena Uriasa)Moslavac (Furmint)Muškat Bijeli (Muscat A Petits Grains Blancs)Muškat Ottonel (Muscat Ottonel)Muškat Žuti (Moscato Giallo)PhoenixPinot Bijeli (Pinot Blanc)Pinot Sivi (Pinot Gris)Radgonska Ranina (Bouvier)Rajnski Rizling (Riesling Weiss)Ranfol (Ranfol Beli)Rizvanac (Mueller Thurgau Weiss)SauvignonSemillonSilvanac Zeleni (Silvaner Gruen)Smudna BelinaSokol (Luglienga Bianca)SolarisStara Hrvatska Belina (Heunisch Weiss)StauferSvetokriška Belina (Zacretska Belina)Traminac Bijeli (Savagnin Blanc)Traminac Crveni (Gewuerztraminer)Veltlinac Crveni (Veltliner Rot)Veltlinac Zeleni (Veltliner Gruen)Zelenac Slatki (Rotgipfler)Alicante Bouschet (Alicante Henri Bouschet)BlauburgerCabernet CortisCabernet FrancCabernet SauvignonFrankovka (Blaufraenkisch)Gamay Bojadiser (Gamay Teinturier Freaux)Kavčina CrnaLovrijenac (Saint Laurent)MerlotModra Kosovina (Zimmettraube Blau)Muškat Crveni (Tamjanika Crna)Pinot Crni (Pinot Noir)Portugizac (Portugieser Blau)RegentSyrahTrollinger Blau (Schiava Grossa)Zweigelt (Zweigeltrebe Blau)
Terroir
Natural factors
- The highest parts of Hrvatsko zagorje, at elevations of 500 to 1,000 m above sea level, are ridges whose basement or surface consists of Mesozoic carbonates or Palaeozoic metamorphic and igneous rocks.
- The greater part of Hrvatsko zagorje is built from Tertiary sediments such as conglomerates, sandstones, and marls, deposited mainly in a lacustrine environment and extensively dissected by watercourses.
- The weathering of Palaeozoic crystalline rocks, Mesozoic argillaceous limestones, and various clastic deposits gave rise to diverse clays and fine-grained sands, which favoured the development of arable soils on the so-called 'gorice' (hillside vineyard ridges).
- The Međimurje area is predominantly lowland, dominated by younger Neogene clay–sandy sediments, with vines cultivated at elevations of 240 to 330 m above sea level.
- The climate of this area is classified as humid, moderately continental, with moderately warm summers and fairly rainy, cold winters, a mean annual temperature of approximately 11.1 °C, and annual precipitation of approximately 890 mm, of which more than 55% falls during the growing season.
Human factors
- Viticulture in this area dates back to Roman times, when the Romans introduced the vine and established vineyards on mountain slopes during the rule of the Roman Empire.
- In the 13th and 14th centuries, viticulture and winemaking stagnated as a result of the Turkish invasions, during which vineyards were cut down and destroyed, with recovery beginning only after their withdrawal.
Product characteristics
- White wines from this area are crystal clear, ranging in colour from yellow-green to yellow, medium in alcohol, with moderate to high acidity, good extract, and discreet to pronounced fruity, floral, and spicy aromas.
- Red wines from Pinot noir, Cabernet Sauvignon, and Frankovka are clear, with varying intensities of ruby-red colour, medium alcohol, moderate to high acidity, moderate tannin ripeness, and pronounced fruity aromas.
Terroir / wine link
- The collision of continental and Alpine climates produces greater diurnal temperature variation, which is conducive to the production of fresh, approachable wines with good acidity and expressive primary fruity and floral aromas.
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-A1662
- Official trade body site — Društvo vinogradara i vinara Međimurja “Hortus Croatiae” Štrigova