Templeton Gap District

Climate

The gap in the Santa Lucia Range creates a natural wind tunnel that channels cool Pacific marine air directly into the vineyards, creating a significantly cooler microclimate than inland Paso Robles areas. This consistent afternoon cooling effect extends the growing season and preserves natural acidity in the grapes.

Terroir

The Templeton Gap District sits atop Monterey Formation marine sedimentary rocks, rich in calcareous deposits from ancient sea beds that create the signature limestone and clay loam soils. The underlying bedrock contains fossilized marine shells and organisms, contributing to the high calcium carbonate content that provides excellent drainage while allowing deep root penetration. The porous limestone substrate maintains a moderate water table that supports vines during dry periods without waterlogging.

Typical Aromas