File:P001225.jpg: Revision history

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10 June 2014

  • curprev 15:0715:07, 10 June 2014Dbk talk contribs 3,496 bytes +3,496 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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