The Thermenregion or ‘spa region’ in Austria commemorates the spa (‘thermen’) towns of Baden, Bad Vöslau and Bad Fischau (‘Bad means ‘Bath’ in the German language and is often added to a spa town′s name). These spa towns lie along the Südbahn or Southern Railway from Vienna, used in the 19th-century by the Viennese to make Thermenregion ‘Vienna’s back yard’, with its Biedemeyer villas, casinos and horse racing (Giles MacDonogh (1997, p.23).
Grapevines were already being cultivated more than 2000 years ago in this climatically favoured region south of Vienna. Roman legionnaires stationed in Carnuntum and Vindobona introduced vines from their homeland and brought the technical expertise of wine production to Pannonia. The name Thermenregion refers to the sulphurous hot springs of Aquae (Baden). In the Middle Ages, viticulture experienced a veritable heyday here under the guidance of the Cistercian monks. The arrangement of the vineyards clearly shows the influence of their Burgundian mother-monastery Citeaux, as does the character of the villages themselves.
Cistercian winegrowing immediately recognised the value of this terroir . The vines benefit here from the Pannonianclimatewith hot summers and dry autumns as well as the1800 annual hours of sunshine. Constant air currents enable the grapes to dry quickly after dew or rainfall in autumn.
Main wine towns: Mainly red wines (r) or white wines (w). (Bad Vöslau (r), Baden (w), Gumpoldskirchen (w), Guntramsdorf (w), Perchtoldsdorf (w), Pfaffstätten (w), Tattendorf (r). Teesdorf (r). Traiskirchen (w). | Sooss (r).
Vineyard area: 2.181 ha.
Grape varieties: Regionally typical, but otherwise seldom encountered white grape varieties include Zierfandler (Spätrot) and Rotgipfler, often monovarietal wines, but also happy as a cuvée, the legendary Spätrot- Rotgipfler. Traditional varieties also include the Blauer Portugieser (formerly called Vöslauer) or Neuburger, as well as other wines from the Pinot family, Pinot noir, Sankt Laurent, and Zweigelt, but also Merlot and Cabernet
Terroir: The region extends on the eastern edge of the Limestone Alps to the Vienna Basin. Only a small part of the vineyards lies directly on consolidated limestone and dolomite rock or on the sandstones and conglomerates of the Gosau Group. Most of the vines are planted upon deposits from the primordial sea and Lake Pannon in the Vienna Basin or on alluvial gravel from the glacial periods in the Steinfeld plain.
At the edge of the basin one finds mostly sand, gravel, sandstones, conglomerates and breccias, which are composed of rock material from the Limestone Alps and flysch, brought here by rivers from the nascent Alpine Range. They house famous sites of fossils, such as the Gainfarner sands. There, along with shells, snails and corals, an entire manatee skeleton some 14 million years old was found. Toward the basin, vineyards often stand on fine-grained clays, marls, debris or colluvium, upon which loamy soils, quite often with high limestone content develop.
Loamy soils of finely grained deposits predominate. A high coarse fraction is common, stemming from solidified or loose gravel and sands with high limestone content and substantial remains of shells, snails and other marine life. Rubble-laden hillside deposits help in matters of drainage and warming. In the Steinfeld, barren gravel soils provide excellent conditions for growing red wines.
In the far southeast, some vineyards on the other side of the Vienna Basin grow on crystalline slates and carbonates of the Eastern Alpine unit, which rises here in the Rosalia Range.
Climate: Warm climate due to the protection against cold, northerly winds from the Vienna woods and the last hills of the Alps.
Giles MacDonogh, Austria, New Wines from the Old World (Osterreichischer Agrarverlag, 1997).
Wines of Austria