The Granite Belt was formed by an ancient tectonic uplift that forced a significant Granite Mass 820m above sea level. Over time, softer rocks and soils have eroded, leaving a clearly identifiable Granite Plateau. Due to its elevation, this plateau experiences some of Australia’s coldest winters. The sub-zero temperatures cause water that has been absorbed in exposed granite boulders and rocks to freeze and expand, forcing mineral particles into the soil. This annual soil enrichment allows local vineyards and orchards to grow the highest quality produce with unique, rich flavours.