Brisbane tuff
Brisbane tuff is a type of rock, formed as a result of a volcanic eruption. As the name suggests, it is a type of tuff found in Brisbane, Queensland, Australia. It is a form of welded ignimbrite. Brisbane tuff comes in a variety of colours: pink, green, blue-grey, yellow and purple. The different colours are due to the extent of oxidation of iron and manganese.
It is often incorrectly described as porphyry.
History
Brisbane tuff began to be used during the period when Captain Patrick Logan was the commandant of the Moreton Bay penal colony.Brisbane tuff is found in various parts of Brisbane and was quarried extensively in the early history of Brisbane at the Kangaroo Point Cliffs and the Windsor Town Quarry Park for use in construction of Brisbane's earliest buildings.
Geology
Brisbane tuff was formed by the welding and compaction of volcanic ash more than 226 million years ago. It displays pyroclastic flows of rock fragments deposited as the volcanic ash was forming. Layers of Brisbane tuff can be over thick.It is a form of welded ignimbrite. Brisbane tuff comes in a variety of colours: pink, green, blue and purple. The different colours are due to the extent of oxidation of iron and manganese.
Construction
Brisbane tuff has been used in the construction of the following Brisbane buildings, many of them now heritage-listed:- Commissariat Store, William Street
- Cathedral of St Stephen, Elizabeth Street
- Old Bishopsbourne Chapel, Milton Road
- St Martin's House, Ann Street
- St Mary's Anglican Church, Kangaroo Point
- Manor Apartment Hotel, Queen Street using Benedict stone
- Shell House, Ann Street
Benedict stone