 |
 |
|
 |
 |
 |
|
|
|
 |
 |
|
|
Our soils are derived from Cambrian age basaltic rock (500 million years).
Quite rare in the world and particularly in Australia, here they are unusually deep (4metre), red coloured, well drained, gravelly loams on undulating hillsides, but with good moisture retention.
They occur in a narrow, non-contiguous strip between two naturally occurring North/South faults which gives them a complex mineralogy. |
|
|
|
|
 |
 |
|
 |
|
 |
|
|
 |
|
| |
|
|
|
|
|
|
|