Sequence oe Rocks. 
83 
Recent. 
Quaternary. 
Miocene. 
Triassic. 
Permian, 
Carbonifcrou: 
Devonian. 
Silurian. 
Cambrian, 
Archaean. 
Pliocene 
Eocene. 
Cretaceous, 
Jurassic. 
Great alluvial plains of the interior. 
Alluvial deposits overlain by 
Basalt. 
Marine beds under the Pleistocene 
Arumpo.l 
Fresh-water heels with fossil plants, New 
England. 
No marine beds known east of the Great 
Dividing Range in New South Wales 
or Queensland. 
White Cliffs opal fields, and a 
largo area in the North-West 
of the colony. 
Sandstones with Fossil Fish, north 
of Gulgong. 
Hawkeabury Sandstone, NarrabeenShales, 
and the Shales around Sydney. Arte- 
sian water-bearing strata of the 
interior. 
The Coal-bearing beds at Newcastle, Lith- 
gow, and Bulli are classed as Permo- 
Carboniferous. 
The series of bedded sediments 
about Stroud. 
Mt. Lambie Sandstones, Wittagoona 
Sandstones, stretching west to Wil- 
cannia, Sandstones on North-West 
shoulder of the Canoblas. 
Limestones of Jenolan Caves, Mu- 
long, and Yass. Clay slates of 
Cobar district. 
Not known in New South Wales. Caroline 
Creek (Tas.), Yorke’s Peninsula (S. A.), 
and Kimberley (W.A.) 
Not known in Now South Wales. 
Fig. ‘22. — Succession of Stratified Rocks in New South Wales. 
t Geologists are not unanimous in deciding whether these beds are 
Eocene or Miocene. 
