Map and content courtesy of www.nzwine.com
In the southern area the soils are mainly alluvial silt loams over gravel subsoils while in Waipara they are chalky loams that are often rich in limestone. Long, dry summers, abundant sunshine and relatively cool growing conditions are a feature in both areas although Waipara, which is sheltered from the coast by a low range of hills, can be significantly warmer.
Chardonnay and Pinot Noir are the most widely planted grape varieties, together making up nearly 60% of the region's vineyard. Riesling is the third most popular variety with Sauvignon Blanc in fourth place. Canterbury is New Zealand's fourth largest wine region.
The Waipara Valley is snuggled in the lee of the Teviotdale hills that provide protection from cool easterly winds but leave it open to warming north west winds. The valley has three general sites - valley floor, hill slopes or river terraces. The soil types include gravely deposits on flats and terraces in the central and west of the valley, limestone derived clays on hillsides and valley floor to the eastern side and gravely loams over alluvial subsoil in the southern part of the region. The north facing moderately sloping terrain provides an ideal sun trap for fruiting vines.
This terroir gives each vineyard unique characters that contribute to a range of wine styles. It takes a visit to each winery to fully appreciate Waipara. The “terroir” combined with the long, hot autumn period helps produce unique richer, spicier Pinot Noirs and Rieslings – regional specialties. Other varieties of note include Pinot Gris, Chardonnay and Sauvignon Blanc.
Content and photo courtesy www.nzwine.com
Main city - Christchurch in Canterbury.
Other towns/villages - Amberley in Waipara; Akaroa in Canterbury
To find out more about the Canterbury wine region, click here
To view a map of Canterbury's wineries, click here
To find out more about the Waipara Valley wine region, click here
To view a map of Waipara's wineries, click here
For general (tourist) information, click here.
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