163 
15 feet, containing the following Corals, which have’ been 
kindly named for me by Mr Tomes :— 
Chorisastreea rugosa |  Thamnastrea Defranciana 
Latimzandra Davidsoni _ Oroseris concentrica 
Donacosmilia Wrighti Thecoseris polymorpha 
Thamnastrea Terquemi Dimorpharea, Lycetti 
and an undetermined Montlivaltia 
And above this is a Fissile Limestone of 14 feet. 
Section 4. 
This is a deep quarry of 60 feet of Limestone, with a clear 
division near the centre; and I have failed to find any fossils, 
and the beds dip 9 degrees to south-east. 
Srction 5 
Occurs in the plantation, and is not easy of access, and the 
top of the beds of the Freestone No. 4 are hard and smooth, 
presenting here a glazed appearance, resembling the action of 
ice, without, however, any grooving, and the dip is diminished 
to 2 degrees. 
The Coral bed of the Oolite Marl is a lenticular mass, 
assuming a dome-like form, and the lower part has the appear- 
ance of having been forced up, throwing off at the time a kind 
of bastard Freestone, which is unfossiliferous. 
In the numerous visits I have made to this Section, and 
also after many diligent searches by Messrs Hetpes and Foster, 
only one Terebratula fimbria has been found, and that was a 
very imperfect specimen. 
Now a most marked change takes place, as the next bed is 
a very hard stone, full of fossils, mostly much broken up. 
I was able to identify Terebratula globata, Rhynchonella spinosa, 
and inconstant, casts of Trigonias, Tancredia ; large Oysters, 
Gresslya, Fish palates, &e. 
Again is a great lithological difference, as the bed above 
is a hard coarse, yet fissile Limestone, destitute of organic 
remains. 
Then comes No. 20, the Clypeus plottii bed, with Terebratula 
globata, Pecten lens, &c., and it extends along the hill, and 
