Albariza: The White Chalky Soil of Jerez

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Albariza is the soft white marl that forms the predominant soils of the Jerez-Xérès-Sherry vineyards: easy to work, with a great capacity to retain moisture. The DO's rulebook, the pliego de condiciones (consolidated by the Orden of 13 May 2026), sets out its make-up. Its silica comes from the shells of diatoms and radiolarians in the sea that covered the area in the Oligocene period. In a region of hot, dry summers, albariza is a natural ally for vine growing, because it stores winter rainfall and releases it gradually to the vines.

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Definition and Origin

Albariza is a soft white marl, the parent rock of the predominant vineyard soils in Jerez, and where it comes to the surface it gives the Jerez vineyard its traditional landscape. The name comes from the Latin alba, meaning white, and the soil takes on a dazzling whiteness during the dry months. The delimited zone lies in the northwest of Cádiz province, bounded to the north by the Guadalquivir River, to the west and south by the Atlantic Ocean and to the east by the foothills of the Sierra de Cádiz. Albariza's origin is marine. Its silica comes from the shells of diatoms and radiolarians in the sea that occupied the area in the Oligocene period, and the fossil remains of diatoms add to the soil's porosity, allowing it to absorb and retain water and then release it gradually.

  • Albariza is a soft white marl that is easy to work and holds moisture well
  • The name comes from the Latin alba, meaning white
  • Albariza is mainly found within the Sherry Triangle formed by Jerez de la Frontera, Sanlúcar de Barrameda and El Puerto de Santa María
  • The snow-white albariza soils are concentrated on the gentle slopes of Jerez Superior, a sub-region between Sanlúcar de Barrameda and the Guadalete River
Key Facts
  • Albariza's calcium carbonate is normally at least 25% and up to 40%, alongside clay and silica, under the consolidated 2026 pliego
  • Albariza's silica comes from the shells of diatoms and radiolarians present in the sea that occupied the area in the Oligocene period
  • Average annual rainfall is about 600 litres per square metre, falling mainly in November, December and March; albariza stores each winter's rain to nourish the vines through the dry months
  • Vineyard irrigation is allowed only in exceptional cases or where the vines' survival is at risk, and only with authorisation from the Consejo Regulador
  • Vine roots up to twelve metres long have been found at depths of up to six metres in albariza soil
  • Albariza comes in three recognised types: tosca de barajuelas (layered, like overlapping sheets), tosca cerrada (more compact) and lentejuelas (with small shiny inclusions)
  • Barros sit in hollows and on lower slopes, with more clay, sand and organic matter; arenas dominate the coastal vineyards, with less than 20% limestone

Water Retention and Viticulture

From a wine-growing point of view, albariza's main characteristic is its high moisture-retaining power. Its leafy structure opens up like a sponge during the rainy season and absorbs immense quantities of water; later the upper layers bake hard under the summer heat, which prevents the evapotranspiration caused by the region's high levels of sunlight. Average annual rainfall is about 600 litres per square metre, falling mainly in November, December and March, and that figure has to be read together with the capacity of albariza soils to retain moisture and avoid evapotranspiration. Irrigation is not a routine tool: the pliego allows it only in exceptional cases or where the vines' survival is at risk, with the Consejo Regulador granting authorisation on an exceptional basis under article 21.d of Ley 10/2007 on the protection of the origin and quality of the wines of Andalucía. Growers help the soil along with aserpia, a winter task that builds ridges of earth between the vine rows to form rectangular pits. These pits catch and store rainwater and stop it running off down the slopes.

  • About 600 litres per square metre of rain a year on average, mainly in November, December and March
  • Roots up to twelve metres long have been found at depths of up to six metres in albariza soil
  • Albariza is easy to work and, being very moisture retentive, allows an excellent distribution of the root system
  • Irrigation only in exceptional cases or where the vines' survival is at risk, with authorisation from the Consejo Regulador on an exceptional basis
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Soil Composition and Subtypes

Albariza's defining components are calcium carbonate, normally at least 25% and up to 40%, together with clay and silica, so the soil is rich in calcium carbonate at up to forty percent. Within albariza there are several typologies that vary in structure and behaviour: tosca de barajuelas, with a layered formation resembling overlapping sheets; tosca cerrada, more compact in structure; and lentejuelas, with small shiny inclusions. Because of the high proportion of limestone in albariza, rootstocks used in Jerez must also be resistant to limestone. The soil is also extremely poor in organic matter: before planting, the land is ploughed to a depth of 60cm in summer, in the operation known as agostado, and then manured.

  • Calcium carbonate normally at least 25% and up to 40%
  • Tosca de barajuelas: a layered formation resembling overlapping sheets
  • Tosca cerrada: more compact in structure
  • Rootstocks must resist limestone, given the high proportion found in albariza

Why It Matters for Sherry Production

The Jerez rulebook links the region's predominant albariza soils with wines of clear calcareous expression: elegant, with body and sapidity, and with a great capacity to evolve over the long term. The same rulebook also credits the near absence of rain during most of the vine's active cycle, the dry levante winds and the moisture retention of albariza soils with healthy, high-quality harvests and very good ripening. The Consejo Regulador sees albariza as the most suitable environment for Palomino, the predominant variety in the region, and associates the soil with a restrained aromatic expression that lets winemaking and ageing take centre stage. The soil's white colour reflects solar radiation, moderating the immediate temperature around the vine. Wines destined for biological ageing are sourced from grapes grown in the finer albariza soils and produced from the primera yema, while those destined for the oxidative ageing path of Oloroso more often come from barros soils and the coarser segunda yema must. For the Consejo Regulador, to speak of Sherry wines and Manzanilla from Sanlúcar is inevitably to speak of their origin, a landscape marked by bright white tones.

  • Albariza soils are linked with wines of clear calcareous expression and a great capacity to evolve over the long term
  • Palomino, the predominant variety, is held to find its most suitable environment in albariza
  • The white surface reflects solar radiation, moderating the immediate temperature around the vine
  • Biological-ageing wines come from finer albariza and primera yema; Oloroso more often from barros and segunda yema

Producers and Pagos to Know

The delimited zone is divided into smaller geographical units traditionally called pagos, rural sites with their own soil and microclimate characteristics. The pliego's annex lists them by municipality, including Macharnudo Alto, Macharnudo Bajo, Carrascal, Montegil and Balbaína Alta in Jerez de la Frontera and Miraflores in Sanlúcar de Barrameda. The Consejo Regulador completed the official pago map in 2015, and wineries can put these historic names on labels when they show that at least 85% of the grapes come from the pago. Tradition speaks of the olorosos of Carrascal, the manzanillas of Miraflores, the chalk (the calcareous profile) of wines from Macharnudo and the finesse of those from Balbaína. Macharnudo also counts among the most renowned pagos, known for the brightness of its soil. González Byass presents Tío Pepe en Rama 2025 as a selection of casks from its soleras that reflects the strength of the Macharnudo and Carrascal vineyards. Lustau's Montegilillo vineyard, near pago Montegil north of Jerez, is planted entirely with Palomino Fino at 65 to 87 metres above sea level, with abundant tosca cerrada in its higher sections. Lustau's own Las Cruces vineyard near Chipiona mixes sandy soils, albariza zones and clay-rich barros.

  • Pagos are smaller geographical units with their own soil and microclimate characteristics
  • The official pago map was completed in 2015; naming a pago on a label requires showing that at least 85% of the grapes come from it
  • González Byass presents Tío Pepe en Rama 2025 as reflecting the Macharnudo and Carrascal vineyards
  • Lustau's Montegilillo, near pago Montegil, is planted entirely with Palomino Fino at 65 to 87 metres, with abundant tosca cerrada higher up
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Terroir Context and Regional Classification

Albariza is not the only vineyard soil in the zone; vines also grow on barros and arenas. Barros, generally in the hollows and lower parts of the hills, contain a significant proportion of clay and sand besides the limestone, plus more organic matter, which gives them a darker colour and more fertility. Arenas predominate in coastal vineyards, with less than 20% limestone and mostly sand and clay, and the Moscatel grape is often grown on these coastal sandy soils. For quality ranking, the Consejo Regulador keeps a list of Jerez Superior vineyards, rated by a technical committee on their agro-geological and climatic characteristics. The vineyards traditionally designated Jerez Superior are those whose soil, the so-called tierras albarizas, and climate suit wines of superior quality. Over the three decades to 2016, the vineyard area fell from almost 23,000 ha to around 6,500 ha. Registered vineyard stood at 6,866.74 hectares on 1 August 2025, and the area has stabilised around 7,000 hectares in recent years. The process to recognise a new denomination of origin for white wines, Vinos de Albariza, began in 2025, with the Consejo Regulador's plenary approving the request at its 23 September session. Fernando Angulo and Alejandro Muchada, both of whom have worked in Champagne, are mindful of the similarities between Jerez's chalks and sands and those of Champagne.

  • Barros: hollows and lower slopes, with more clay, sand and organic matter, darker and more fertile
  • Arenas: coastal vineyards with less than 20% limestone, where Moscatel is often grown
  • Jerez Superior vineyards are listed by the Consejo Regulador on a technical committee's assessment
  • 6,866.74 hectares of registered vineyard on 1 August 2025

Sources and last verified

Primary sources: https://www.sherry.wine/documents/597/21052026_Pliego_Jerez_1wBQg8y.pdf, https://www.sherry.wine/sherry-wine/production/viticulture, https://www.sherry.wine/news/what-is-albariza-the-soil-that-defines-sherry, https://www.sherry.wine/es/vinos-de-jerez/pagos, https://www.sherry.wine/documents/593/Memoria_2025_compressed_1.pdf, https://lustau.es/en/blog/understanding-terroir-in-jerez/, https://www.gonzalezbyass.com/sites/www.gonzalezbyass.com/files/2026-03/EnRama2025_0.pdf. Secondary sources: https://www.guildsomm.com/webupload/webdocs/sherry.pdf, https://www.decanter.com/wine-news/opinion/jefford-on-monday/jefford-on-monday-the-jerez-terroir-challenge-293321/. Last verified 2026-10-04

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How to Say It
Jerezheh-RETH
Andalucíaahn-dah-loo-THEE-ah
Palomino Finopah-loh-MEE-noh FEE-noh
Guadalquivirgwah-dahl-kee-VEER
Manzanillamahn-thah-NEE-yah
primera yemapree-MEH-rah YEH-mah
Olorosooh-loh-ROH-soh
Exam Study NotesWSET / CMS
  • Albariza is the soft white marl behind the predominant vineyard soils of Jerez; calcium carbonate is normally at least 25% and up to 40%, with clay and silica from the shells of Oligocene-era diatoms and radiolarians.
  • Water: about 600 litres per square metre of rain a year, mainly in November, December and March; albariza absorbs winter rain like a sponge and its upper layers bake hard in summer, limiting evapotranspiration.
  • Irrigation is allowed only in exceptional cases or where vine survival is at risk, with Consejo Regulador authorisation; roots up to 12 metres long have been found at depths of up to 6 metres in albariza.
  • Albariza types: tosca de barajuelas (layered), tosca cerrada (compact) and lentejuelas (small shiny inclusions). The other two vineyard soils are barros (lower slopes, more fertile) and arenas (coastal, under 20% limestone, often Moscatel).
  • Wines for biological ageing come from finer albariza and primera yema must, Oloroso more often from barros and segunda yema. The official pago map (Macharnudo, Carrascal, Miraflores, Balbaína and others) was completed in 2015.

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