About Calcified Forest
The Calcified Forest is a natural limestone formation on the west coast of King Island, Tasmania, within the King Island local government area. It preserves the stumps and root structures of an ancient forest encased in calcium carbonate after being buried by calcareous sand dunes thousands of years ago. The exposed fossilised remains, set among coastal dunes and heathland, are notable for their geological rarity and scientific interest, offering visitors a distinctive landscape unlike elsewhere in Tasmania.
Visitors guide
Visitors can expect an open coastal dune landscape with numerous hollow, calcified tree stumps and root casts protruding from limestone. A short boardwalk and interpretive shelter lead through the site with views over the rugged west coast, heathland and ocean. The area is exposed and windswept with no tree cover, focused on sightseeing, photography and understanding the geological formation.
Key highlights
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Fossilised calcified tree stumps and root formations encased in limestone
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Interpretive boardwalk through the dune and forest remains
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Coastal dune and heathland landscape on King Island's west coast
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Information shelter explaining formation process
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Photographic views of rugged coastline and geological features
History of Calcified Forest
The site preserves an ancient forest buried by calcareous sand dunes and subsequently calcified by calcium carbonate-rich water percolating through the dunes. Over thousands of years the wood decayed leaving hollow limestone casts of trunks and roots, later exposed by wind erosion. It is considered a significant geological example of calcification and dune formation in Tasmania.
Route
| By air | Fly to King Island Airport (KNS) from Melbourne or Burnie, then drive to the site |
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| By road |