We are going to revisit the creek at Adels Grove, this time in daylight.
As you can see, on a sunny day it’s a gorgeous place to be.
From the top of Lookout Hill, I could see the slag heaps of Century Mine on the horizon.
The mine is one of the biggest open-cut mines in Australia (perhaps the biggest), meaning it is a very, very big hole in the ground. They mine zinc and lead ore here, and it’s been going for 20 years.
Because it is an isolated place, and prone to flooding in the Wet, they had to build a lot of very clever infrastructure. They crush the ore and then dilute it with water. Then they pump it through 300km of pipes to Karumba in the Gulf of Carpentaria, where they ‘dewater’ the ore, put it on barges, and haul it 50km out to sea and on to the big export ships.
Hubby and a few of his colleagues got to go on a short visit, and he said the scale of everything, from the ‘tonka trucks’ to the big hole, was impressive. This is one of those operations where workers are flown in and out via their private airport, and where everything is self-contained.
The thing that got me about a mining operation like this is how efficient it was compared to, say, public transport in Sydney. I guess people in this country can make the effort to be efficient when there’s big money about. Public infrastructure however, makes no money, and so we’re left in the dark ages.
This mine is actually wrapping up operations pretty soon. But I doubt mining will disappear completely from the Lawn Hill area – there are plenty of other minerals about.
I wasn’t out in the field everyday (I was on holidays after all), but I liked to see what people brought in at the end of the day. One afternoon, Hubby returned with slabs of Cambrian trilobites and brachiopods. I was very happy because trilobites are my favourite fossils.
I like their other-worldliness, these fossils being representatives from another time – when the Gulf Country and most of Eastern Australia was still under water, and when the only creatures on land were insects and spiders. Hubby suspected that there may be a new species in those slabs – he was only partially right.
This trilobite is a known species in the Gulf.
We’re yet to find out what species this is.
The ridged brachiopod (shell) is a known species, but those specimens came from western NSW. We’re yet to find out what species the smooth brachiopod is.
These are giant burrows of some kind. So far no one has any idea of what could have made them. It must have been big, scary thing, whatever it was.
And lastly, these are fossilised mud cracks! Surprising the things that survive.
The landscape at the last water bore we visited was flat.
Very flat.
I was later told that we were inside an impact crater from a meteorite which fell to earth hundreds of millions of years ago. Later I looked the area up on Google Maps, and what do you know, it did look like a crater. Whereas the surrounding hills were all in lines and curves, the hills around the crater was definitely a circle.
The week however wasn’t all about palaeontology. I also joined the geologists on a few of their water and rock collecting trips. They sampled water from the local creeks, took rocks from the surrounding area, and attempted to collect data from the monitoring devices they had left in various water bores the previous year. These monitors tracked water levels and pressure and temperature.
It was the last activity that took the most time – the monitoring devices were frustratingly difficult to retrieve. These devices were basically suspended into the bores with a length of rope and then taped into place. To retrieve them involved a lot of fishing about.
Unfortunately, their survival rate was low. If they hadn’t detached from the rope, chances were that the bore they were in had been trampled by a herd of cattle. Even if you retrieved the monitor, you might not be able to extract the data from it.
In the end, only one device out of five came up with the goods. I guess it’s pot luck out in the Outback.