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I’ve been meaning to do a bit of skin diving and I thought I’d share my favourite places to dive.
You don’t have to be an expert in skin diving to dive, there are plenty of places to get lost in the Australian outback.
I found myself diving into one of the oldest and most famous Australian cairns, The Stag Lane, in the early 1900s.
Stag Lane in the north-west of the state of Victoria, is one of only two cairn-protected areas in the world, the other being the Great Barrier Reef in Australia.
It’s located in the small town of Sandringham and is a part of the Great Sandstone National Park.
The cairners are made up of a series of deep holes which are made of sandstone and limestone.
There are several different caves in the area and some of them have been used for medical purposes, though it’s not known if they are safe.
As you’ll see in the pictures, it’s very different from most of the other caves around the Great Australian Outback.
The sandstone caves in this area have been well cared for and the rocks are very hard.
I was surprised to find one of my favourite caves, The Beryl Hole, when I arrived in town a few weeks ago.
Beryl Hole is one cave in the Sandstone Cave System, which is a group of caves that have been around for thousands of years.
The caves are located in an area known as the Beryl Basin.
The area is known for being a great source of wildlife and it’s also one of those rare places that has been protected by the National Parks and Wildlife Service (NPWS).
Biggs Hole is also in the Banges Basin, and has been listed as one of Australia’s “best protected sites” for hundreds of years by the NPWS.
It has the longest rock formation in the park, and is the site of one of its best recorded waterfalls, the Biggs.
The caves at Beryl and Biggs are very different to the rest of the cairner sites.
Beryl is the longest, and most impressive, of the caves in The Stags Lane.
It is the largest cave in Australia and is thought to have been formed when the Stag was about a metre deep.
Biggs is the smallest and is only a small patch of rock on the rock face.
A typical day at Biggs Cave involves visiting several of the cave entrances.
The first few days were pretty much the same as any other day.
I’d head out to visit the entrances to Beryl, Biggs and the other two caves.
I usually would just stop by the cave entrance to make sure I was safe.
On the third day, I would go back in and make sure there was no one nearby.
After a few more days of waiting, I’d go back out to the cave and do a couple of more trips.
I would try to make it to the entrance to the Bandshell Cave and make it there as soon as possible.
On most days, I made it to Bandsheim, but if I had to go back for a day or two, I might just make it in another direction.
During my travels around the Stags and Bandshelmes, I was often walking in the sand to get to the caves and to see the waterfalls.
This was one of these times.
I started my trip at the entrance of Bandsham and walked around for about 30 minutes or so.
The cave was a great place to take pictures of the water in the caves.
My main activity at this time was to explore the caves around.
I visited a number of other caves and spent a lot of time exploring the Backshell.
Once I was done exploring, I headed back to the main cave entrance.
This cave is called The Stagh Lane and is probably the most famous in the cave system.
The Strag is a very old rock formation, and it is said to be about 30 metres tall and over 50 metres wide.
It is a large and beautiful rock formation and was formed when a river flowed through the caves during the wet years of the 1800s.
It sits in the middle of a large creek which flows through the Stagh.
In the early days of the National Park, there was a large waterway flowing through the cave, which the river used to bring in water.
For many years, there were also large cairned caves which were dug out of the rock and used for fishing.
At the time of the early opening of the Stages, there weren’t any fish to be caught on the Stang Lane.
There are a number places in the Stats that have survived the floodwaters and are used by locals for their fishing.
They include: The Stats Cave, which was formed in