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| Date/Time | Thumbnail | Dimensions | User | Comment | |
|---|---|---|---|---|---|
| current | 15:07, 10 June 2014 |  | 1,000 × 769 (257 KB) | Dbk (talk | contribs) | The dry valley to the north-west (right) contains the Gualann Fault with the subsidiary grassy ridge consisting mainly of serpentinite - now largely brecciated and altered to dolomite. Its derived clastic origin is seen in parts. The low relief areas t... |
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