Article · Wikipedia archive · Last revised Jun 21, 2026

Knocklofty Formation

The Knocklofty Formation is an Early Triassic geologic formation from southern Tasmania, Australia, belonging to the Induan stage. It was deposited in a terrestrial, freshwater environment, and is primarily composed of shale and sandstone.

Last revised
Jun 21, 2026
Read time
≈ 1 min
Length
171 w
Citations
12
Source
Knocklofty Formation
Stratigraphic range: Early Triassic,
TypeGeological formation
Lithology
PrimaryMudstone, siltstone, sandstone
OtherConglomerate
Location
Coordinates42°54′S 147°18′E / 42.9°S 147.3°E / -42.9; 147.3
Approximate paleocoordinates82°24′S 61°18′E / 82.4°S 61.3°E / -82.4; 61.3
RegionTasmania
CountryAustralia
Type section
Year defined1966
Knocklofty Formation (Tasmania)

The Knocklofty Formation is an Early Triassic geologic formation from southern Tasmania, Australia, belonging to the Induan stage.1 It was deposited in a terrestrial, freshwater environment, and is primarily composed of shale and sandstone.2

List of known fossil taxa

Tetrapods

Fish

References

References

  1. "Australian Stratigraphic Units Database, Geoscience Australia". asud.ga.gov.au. Retrieved 16 January 2021.
  2. "PBDB". paleobiodb.org. Retrieved 17 May 2025.
  3. Cosgriff, J. (1 January 1974). Lower Triassic Temnospondyli of Tasmania. Geological Society of America Special Papers. Vol. 149. pp. 1–134. doi:10.1130/SPE149-p1. ISBN 0-8137-2149-0.
  4. Dziewa, Thamas. J. (1980). "Early Triassic Osteichythyans from the Knocklofty Formation of Tasmania" (PDF). Papers and Proceedings of the Royal Society of Tasmania. 114: 145–160. doi:10.26749/rstpp.114.145. Archived from the original (PDF) on 17 March 2016. Retrieved 18 January 2021.