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Babinda Boulders, officially called the Boulders Scenic Reserve [1] but known locally as Babinda Boulders or simply the Boulders, is a public recreation reserve alongside Babinda Creek, managed by the Cairns Regional Council and adjacent to the Wooroonooran National Park in far north Queensland, Australia.
This list includes all gazetted rocks, boulders, pinnacles, crags, needles, pillars, rock formations, and tors in Western Australia, both inland and offshore. It does not include monoliths gazetted as mounts or hills, such as Mount Augustus. It is complete with respect to the 1996 Gazetteer of Australia. [1]
This list includes all gazetted rocks, boulders, pinnacles, crags, needles, pillars, rock formations, and tors in Western Australia, both inland and offshore. It does not include monoliths gazetted as mounts or hills, such as Mount Augustus. It is complete with respect to the 1996 Gazetteer of Australia. Dubious names have been checked against the online 2004 data, and in all cases confirmed ...
This list includes all gazetted rocks, boulders, pinnacles, crags, needles, pillars, rock formations, and tors in Western Australia, both inland and offshore. It does not include monoliths gazetted as mounts or hills, such as Mount Augustus. It is complete with respect to the 1996 Gazetteer of Australia. [1]
Devil's Pool is a natural pool in a treacherous stretch of Babinda Creek where large granite boulders fill the creek bed. It is one of the main attractions of the Babinda Boulders scenic reserve, near Babinda, Queensland, Australia. Between 1959 and July 2023, 21 people have drowned at or near the pools.
The park is 25 km south west of Cooktown.It is managed and protected as a national park under the Nature Conservation Act 1992.. The main feature of the park is the mass of granite boulders, some the size of houses.
These were the Cape Melville leaf-tailed gecko, Cape Melville shade skink and the Blotched boulder-frog. [5] The park is home to a wide variety of plant communities, including mangroves, rainforests, heathlands, woodlands and grasslands. [6] [7] The average elevation of the terrain is 43 metres. [8]
The distinctive beehive-shaped towers are made up of sandstones and conglomerates (rocks composed mainly of pebbles and boulders and cemented together by finer material). ). These sedimentary formations were deposited into the Red Basin 375 to 350 million years ago, when active faults altered the lands