Description

Padigan Malbec 2020

Vineyard

Although part of the Rogue Valley, the Padigan Estate Vineyard lies in the area known locally as the Bear Creek sub-basin, which is the Rogue’s largest tributary. Beneath our vineyard soils lies a two-layered bedrock consisting of a volcanic layer, known as the Roxy Formation, and a deeper, softer layer of alluvial sandstone known as The Payne Cliffs Formation. As the Klamath Mountains began to uplift roughly 20 million years ago our bedrocks began a long erosion process that resulted in the predominately volcanic soils we find in our estate vineyard, which are unique to the Rogue Valley AVA. Padigan is also distinguished by a large amount of cobbled river rock, especially in our eastern section, and a somewhat sandy streak of significantly younger colluvial deposit that runs through the center of our site. Overall, we have some of the oldest soils in the valley. They are generally characterized as relatively shallow silty- to clayey-loams that are moderately well drained with moderate to rapid runoff.

Tasting Notes