La Jaraba
Styles
Principal grape varieties
Accessory grape varieties
Terroir
Natural factors
- Quaternary fluvial depression (Guadiana River System) at 700 m elevation, completely flat, crossed by the Cañada de Valdelobos.
- Alfisol soils (red Mediterranean soils over calcareous parent material), pH 7–8.5, with a limestone hardpan at 60–90 cm depth and textures ranging from sandy loam to clay.
- Variable composition: quartzites, quartz, and Mesozoic and Miocene limestones; distinct from neighboring zones with higher calcareous content.
- 92 ha of holm oak and pine woodland shield the vineyards from the hot, dry Levante wind, creating a singular microclimate.
- Soil strontium levels of 110–160 mg/kg, up to 8 times higher than in surrounding plots; functions as a geochemical marker for the zone.
Human factors
- La Jaraba requires alcoholic fermentation using the grape's native microbiota and a maximum yield of 70 l per 100 kg.
- The practice of annual manuring exclusively with sheep manure from the estate's own flock distinguishes La Jaraba from the neighboring DOP La Mancha.
Product characteristics
- Deep cherry-red colour of medium-high intensity; on the palate broad and fleshy, with mineral and balsamic notes.
- The extended ripening period afforded by the microclimate delivers greater colour, tannins, and fruit aromas to the wine.
Terroir / wine link
- The strontium present in the soil (110–160 mg/kg) is transferred to the wine (≥2.2 mg/l) and is identified as a distinctive marker of minerality.
Facts drawn from the cahier's terroir-link section (Lien au terroir) by automatic interpretation — see the the specification.
Sources
- National pliego de condiciones (PDF) — +3 varieties added
- eAmbrosia register (EU) — File number PDO-ES-01895
- Official trade body site — Pago de La Jaraba