Cultivated
area: 35 acres (14 hectares)
Geomorphology : Altitude
of 125 to 130 meters. Sitting at the foot of the Appalachians,
on the east side of the Pike River which flows into the Yamaska
River west of the Callaghan Brook, the vineyard is situated
in the brook’s basin. This basin is a till plain (glacial
deposit) barely inclined which slowly rises toward a rocky
slope in the west with a gradient between 0 and 2 degrees.
The plain is lined with a silt-clay till derived from argillaceous
schist and slate reworked on the top 60 cm by the Champlain
Sea which incorporated littoral sand and gravel. The till is
only between 0,25 to 2 meters deep above bedrock. The rocky
slope is composed of thin alterites on rock, a deposit directly
derived from the breaking of the argillaceous schists.
Climate : The climate
in the wine region of Québec is continental, bringing
cold winters and hot and somewhat humid summers. Average rainfall
during growing season is 930 mm.
Spring
frosts :
They happen when the temperature on the buds goes down to 0° C. In
May 1987 a helicopter hovered above the vineyard for an hour at an altitude
of ten meters to stir the cold air. We gained two degrees and were able
to salvage the harvest. In the spring of 1989, we installed a French
Haltogel system (from the Champagne region) on part of the vineyard to
control the temperature with heaters. This protection system can raise
the temperature by 5° C and runs on fuel.

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