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Past Club Activities
Only summaries of some of our excursion activities will be posted to the website. You will have to consult the Bulletin for the detailed geological information. At least here we can have a few colour photos! This year's activities will be reported as they occur.
EXCURSION: MASLIN BAY AND PORT WILLUNGA
Sunday 25th March 2012
Leader Dr Brian McGowran
The first stop was at a road cutting near Chapel Hill Winery, which showed deeply weathered Neoproterozoic/ Eocene contact - with an unconformity of some 700 my!
Down to Maslin Beach, with its stunning views to Blanche Point, and clearly defined sedimentary strata of South Maslin Sands, Tortachilla Limestone and Blanche Point Formation rocks with profuse examples of marine fossils. The reasons for variety and density were explained by Brian.
We walked on to Perkana Point, then Chinaman Gully and finally the old Port Willunga Jetty, with further discussion and fossicking, to meet the bus at the Star of Greece Cafe.

| Roadside cutting, Eocene (40my) above Precambrian (700my) rocks |
Clambering over beach rocks, Blanche Point |

| Gastropod cast, Tortachilla Limestone |
Platform of Tortachilla Limestone beneath Blanche Point |

Excursion to Marino Rocks
Sunday 30th October 2011:
Excursion Leaders: Cynthia Pyle, Frances Williams, Steve Elsby
An excellent day for scrambling along the rocks and cliffs of the coastline between Marino Rocks and Hallett Cove.
We were able to examine the classic sequence of Marinoan age rocks (about 650my), including the Wilmington Formation, interbedded with Marino Arkose and lastly, the Reynella Sitstone.
Our guides pointed out the nose of the plunging anticline from the top of the cliffs, and we walked to the contact point between the Wilmington Formation, with its various layers, and the lighter coloured Marino Arkose.
Further along we came to the reddish Reynella Siltstone, still in the Neoproterozoic and then the sudden contact, along the Eden Fault, with the recent Pleistocene Hindmarsh Clay - an unconformity of some 650my!
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Bob Major looks at ripple marks in Wilmington Fm rocks |
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Anticlinal fold - note horizontal layers at top of fold |
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Note clear faultline in cliff face |
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Stephanie astride Eden Fault -right foot in Reynella Siltstone, left foot in Hindmarsh Mud - a gap of 650my! |
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Excursion to Ochre Cove
Sunday 27th March 2011
Excursion Leaders: Prof Bob Bourman and Dr Wolfgang Preiss
The excursion descended from the cliff top south of Moana, through a succession of Pleistocene sediments, across a major unconformity, to the folded and faulted Neoproterozoic rocks near the base of the cliffs and along the shoreline.
Bob provided expert commentary of the younger Pleistocene (<2.6 my) and Pliocene (2.6my - 5my)sediments, while Wolfgang discussed stratigraphy of the older rocks, including the ABC Range Quartzite, around 600my, similar to those seen in the Flinders Ranges. An enjoyable, and informative day was had by all, scrambling down the cliffs and along the shoreline.
Photos by Bill Kelly
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James looking at contact between Bunyeroo Mudstone & ABC Quartzite |
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Dr Wolfgang Preiss on beach mudstones |
