Wt. Ward et Ip. Little, Sea-rafted pumice on the Australian east coast: numerical classification and stratigraphy, AUST J EART, 47(1), 2000, pp. 95-109
Sixteen elements (Ca, K, Mg, Na, Al, Fe, Mn, P, Co, Cu, Li, Ni, Rb, Sr. Ti,
Zn, determined by atomic absorption) were identified in 453 pumice fragmen
ts recovered from Holocene strandplains in southeast Queensland and New Sou
th Wales. Eight pumice groups and 13 subgroups are recognised by numerical
analysis. Some pumices record known eruptions. Others come from known centr
es in Tonga and Vanuatu. Several pumice eruptions have occurred from some c
entres, but there are instances of single episodes. The numerical analyses,
combined with carbon dating and soil identification, identify marker horiz
ons in the development of the strandplans. These horizons provide a time-sc
ale for soil development. Pumice that occurs in middens has an archaeologic
al value. Coke was found with recent pumice. It conveniently identifies the
modern industrial age.