360 
PROCEEDINGS OF SECTION C. 
calcareous beds on the coast between Warrnambool and Cape Otway, 
and between Loutit Bay and Geelong (Spring Creek), Moorabool 
[River, Leigh River, Bairnsdale, Gippsland Lake’s entrance, Longford 
and Merri man’s Creek, near Sale, Curdie’s River, and other localities; 
lignites, McKirley’s Creek, north of Crossover and Tarwin River, near 
McDonald’s track ; calcareous beds underlying the Upper Tertiary of 
the plains bordering the Murray ; siliceous conglomerates and 
quartzites underlying older volcanic rocks, Gippsland. 
lower Tertiary (Oligocene). — Grey clays, with septaria, near 
Schnapper Point, and mouth of the Gellibrand River, also grey clays 
at Orphanage Hill or Eyansford, Geelong, Shelford (Ad. 14), referred 
to as Outer Geelong Harbour or parish of Moolap or Curlewis, and 
Muddy Creek near Hamilton. 
TABLE II.— PROFESSOR R. TATE AND MR. J. DENNANT, 1893. 
Cainozoic. 
Pleistocene. — Raised beaches. ^Eolian calciferous sandstones and 
limestones. 
Post-Pliocene . — The newer basalts and ash-beds of Victoria ; the 
ash-beds of the Mount Gambier area, South Australia, overlie deposits 
of the Diprotodon Period. 
Newer Pliocene. — Elevated shell beds — south-east from Mount 
Gambier and at Limestone Creek, West Victoria. Osseous breccias 
and mammaliferous drift of the Diprotodon Period. 
Older Pliocene. — Marine sands beneath mammaliferous drift of 
the Adelaide Plain. 
Miocene . — Upland Miocene plant beds, South Australia; low- 
level marine beds — Gippsland Lakes, upper beds of the Muddy Creek 
section, oyster banks of the River Murray Cliffs, and Aldinga Bay. 
Eocene.- — Clays and polyzoal limestone — Mount Gambier, Rivers 
Mitchell, Tambo, &c.; Sale, Gippsland ; Port Phillip Bay; around the 
carbonaceous area of Cape Otway ; Camperdown ; Muddy Creek, 
Hamilton. Polyzoal limestone — Mount Gambier, River Murray, St. 
Vincent Gulf, Great Australian Bight. Plant beds at Vegetable 
Creek, New South AVales — plant beds inferior to the older basalts of 
Victoria. 
Pre-Eocene. — The older basalts of Southern Victoria. 
TABLE III. — MESSRS. T. S. HALL AND G. B. PRITCHARD, 1895. 
Tertiary or Cainozoic. 
Pecent. — Raised beaches ; estuary beds ; alluvial deposits ; traver- 
tine deposits ; sand-dunes and Dune Limestones of the coast. 
Pliocene. — Limestone Creek beds, south-west Victoria, containing 
about SO per cent, of living mollusca. Volcanic ash-beds of Mount 
Gambier. Mammaliferous sandy clays containing Diprotodon, <fcc., of 
Adelaide Plain, and many other South Australian localities, Werribee 
Plains, Colac, Camperdown, &c., in Victoria, also in New South AVales 
and Queensland ; mammaliferous cave deposits of New South W ales 
and Victoria ; freshwater limestones of the Geelong district ; gold- 
drifts of Dunolly. Newer basalts at Werribee, Geelong, and Camper- 
down. 
