Camperdown, Victoria is home to a variety of unique and fascinating volcanic features. One of the most notable of these is Lake Bullen Merri, a crater lake that was formed when a volcano erupted around 12,000 years ago.
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| Lake Bullen Merri - Click to read Wiki |
The lake is surrounded by a number of small cinder cones, which are formed when volcanic ash and lava are ejected from the volcano and then solidify into small, cone-shaped hills. These cinder cones are made up of a porous, lightweight rock called scoria, which is often reddish in colour due to its high iron content.
In addition to cinder cones, Camperdown is home to a number of other volcanic features. These include rock walls, built by settlers to keep sheep and cattle in and to make the land farmable, and lava tubes, which are underground tunnels that are created when the surface of a lava flow solidifies while the molten lava continues to flow beneath it.
Another interesting feature in the Camperdown area is the Camperdown Lava Flow, which is a large, flat plain that was formed when a lava flow covered the landscape around 10,000 years ago. The lava flow is composed of basalt, a type of rock that is created when lava cools quickly and solidifies.
Overall, Camperdown is a truly unique and fascinating destination for those interested in the natural history of volcanoes. Its diverse array of volcanic features provides a window into the processes that shaped the landscape over the past millions of years, and offers visitors the opportunity to experience the awe-inspiring power of these geological phenomena firsthand.
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