Ask a geologist what's special about Yellow Beach and they'll tell you ...
Walking along the beach to the west it's a lovely sheltered bay and because it is sheltered some of the older Pleistocene rock types have been preserved. Pleistocene is roughly 2m to 12,000 years ago.
The sedimentary rocks here are not like the calcareous sandstones we find elsewhere - they are almost peaty.
They have very high organic content - you see cross bedding - very gritty - there very unusual.
There are other places on peoples' properties on the island where they are found - this kind of stuff - this peaty stuff. Way back when there are reports where people had it on their land and they got that methane smell and they were thinking they had oil and all those kinds of things.
Looking at the peaty sedimentary rock and you can clearly see the bedding and some of the sedimentary structure in the rock.
Compared to the limestones you can see on the island which are predominantly fragments of shell cemented together – here you’ve got a lot of quartz and probably some feldspar grains. There’s still a little bit of shell cemented in there – so compositionally its a little bit different.
The rocks here are partly marine deposition. As the sea level has retreated you’ve developed lagoon shallow marine environments – a bit like those lagoons you go past after Camerons Lagoon. It’s that in between place and that’s why it looks like it got soil as well as just the pebbles. It’s a mixed environment - there’s a lot of organic matter mixed in. If you did pollen studies you’d probably find plant stuff mixed in there. Again – it’s not that old – you can see how friable it is. It easily erodes under the action of wind and water.
So while the Mathinna beds were deposited in deep water probably 1km offshore this is shallow water deposits probably no more than 5m deep at the most – very near shore.
The Mathinna Beds are very fine grained – deposited in quiet deeper water.
This rock is in water with a bit of wave action and you can see the dune forms that kind of tell you there were waves.
And you can see how all the erosion is still going on - basically it’s creating more sand - you can see how the rocks have fallen down because they have been undercut so it’s an ongoing process.
So if you’re talking about erosion on a seashore and how it happens this is a great example.
Also on this beach you can see a fine black mud which is really interesting - that’s like peat - you wouldn’t call this peat - it’s just sandstone which does however have a high organic content as well.
With sandstones we usually think of nice consistent clear crystals like the Hawkesbury sandstone – this is different. You can see it – it looks so dark. Its got a fair bit of grit in it.
There’s a good profile through here. Right at the top you’ve got recent soil layer – the dark stuff. Then below that you’ve got the white sands – these are the recent wind blown sands.
Then below that you’ve got the gritty layer - but if you look at the top 2-3 feet of the gritty layer its yellow in colour and that’s due to the superficial weathering - we call this a soil profile.