Leaving Wilpena we headed north to the gorges. Some of them
were quite ordinary, but one in particular was interesting in that the geology
gives an insight into how the Flinders
Ranges were formed.
650 million years ago, prior to life on earth, most of this
region was undersea, and the rock that was formed is quartzite and sandstone,
and other harder rocks. There are no fossils in these rocks, as it was later,
after lifeforms evolved, that softer mudstone and limestone were formed and the
rocks started to contain them. Then, as the continent was pushed up from
beneath the waters many weird shapes evolved, with the softer siltstone and
shale eroding and the harder standing out.
Brachina Gorge shows much of this, and as we drove through
the valley there were many signs giving us information about the formations,
and it also told us that a large meteorite about 4 kms in diameter fell to earth
close by around 600 million years ago, leaving a large crater and huge lumps of
rock in the area. Such an impact today would wipe out much of life on earth.
Later we camped in the last true town before the Oodnadata
track, Leigh Creek . There was no town here before 1948,
when it was decided to mine the coal that was there for the power Station in
Port Augusta. They still do, and as a result there is a thriving small town
there with a lovely clean caravan site.
Moving on we passed through a 'significant city' called Lyndhurst, I'm sure you can see why I call it that....
But there are a couple of railway engines, we have followed
the Old Ghan track up from Leigh
Creek , and here in Marree
they have preserved the Station and the diesel engines. We also came across a
wartime truck that had been used to deliver mail in the area at one time, as
well as an old bullock wagon. This is Maree....
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