Cart 0 items: $0.00
Selection will refresh the page with new results
AVA
Chehalem Mountains
Cases
323

The soil in the polygon consists of sedimentary and alluvial soil that contains some silt and clay layering as well as volcanic red basalt.

Add To Cart
$100.00
 
SKU: 19CHEHALEMHIGH
AVA
Chehalem Mountains
Cases
323

The soil in the polygon consists of sedimentary and alluvial soil that contains some silt and clay layering as well as volcanic red basalt.

AVA
Eola-Amity Hills
Cases
328

The soil within this polygon is clever combination of red and black basalt, consisting of vertical and horizontal fractures. These soils also have a distinct marbling of slow cooling, irregularly shaped, vesicular basalt.

Add To Cart
$100.00
 
SKU: 19RAAMITY
AVA
Eola-Amity Hills
Cases
328

The soil within this polygon is clever combination of red and black basalt, consisting of vertical and horizontal fractures. These soils also have a distinct marbling of slow cooling, irregularly shaped, vesicular basalt.

AVA
Eola Amity Hills
Cases
240

This soil is full of rocks. It contains black basalt with vertical fractures as well as the occasional occurrence of slow cooling irregularly vesicular basalt.

Add To Cart
$125.00
 
SKU: 19RAHOPEWELL
AVA
Eola Amity Hills
Cases
240

This soil is full of rocks. It contains black basalt with vertical fractures as well as the occasional occurrence of slow cooling irregularly vesicular basalt.

AVA
Dundee Hills
Cases
100

A thin layer of topsoil followed by a medium fractured alteritic iron rich basalt and then fractured unalterated basalt.

Please inquire.
AVA
Dundee Hills
Cases
100

A thin layer of topsoil followed by a medium fractured alteritic iron rich basalt and then fractured unalterated basalt.

AVA
Eola-Amity Hills
Cases
137

The soil here is riddled with a thick layer of black and grey irregular basalt rocks that are slow cooling vesicular igneous rocks. These rocks sit upon a larger layer of bedrock consisting of vertically fractured basalt.

Please inquire.
AVA
Eola-Amity Hills
Cases
137

The soil here is riddled with a thick layer of black and grey irregular basalt rocks that are slow cooling vesicular igneous rocks. These rocks sit upon a larger layer of bedrock consisting of vertically fractured basalt.

AVA
Chehalem Mountains
Cases
139

The rocky soil in Chehalem has a distinctive moderately fractured basalt composition and contains three types of basalt; black, red, and white. The white basalt takes its color from volcanic ash while the red shows its pronounced color from oxidation.

Please inquire.
AVA
Chehalem Mountains
Cases
139

The rocky soil in Chehalem has a distinctive moderately fractured basalt composition and contains three types of basalt; black, red, and white. The white basalt takes its color from volcanic ash while the red shows its pronounced color from oxidation.

AVA
Chehalem Mountains
Cases
99

This soil has a distinctive constitution of pure alteritic basalt, which sits upon a layer of older vesiculated alterite.

Please inquire.
AVA
Chehalem Mountains
Cases
99

This soil has a distinctive constitution of pure alteritic basalt, which sits upon a layer of older vesiculated alterite.

AVA
Chehalem Mountains
Cases
136

The rocky soil in Chehalem has a distinctive moderately fractured basalt composition and contains three types of basalt; black, red, and white. The white basalt takes its color from volcanic ash while the red shows its pronounced color from oxidation. In addition, the basalts are shot through with weathered black basalt pebbles.

Please inquire.
AVA
Chehalem Mountains
Cases
136

The rocky soil in Chehalem has a distinctive moderately fractured basalt composition and contains three types of basalt; black, red, and white. The white basalt takes its color from volcanic ash while the red shows its pronounced color from oxidation. In addition, the basalts are shot through with weathered black basalt pebbles.

AVA
Eola-Amity Hills
Cases
100

The polygon within our vineyard in Eola-Amity is incredibly special due to its high amount of medium-weathered red and black basalt within its structure. This layer is surrounded by topsoil and thin alterite above and vertically fractured vesicular basalt bedrock below.

Please inquire.
AVA
Eola-Amity Hills
Cases
100

The polygon within our vineyard in Eola-Amity is incredibly special due to its high amount of medium-weathered red and black basalt within its structure. This layer is surrounded by topsoil and thin alterite above and vertically fractured vesicular basalt bedrock below.