345 
Details of Bores Nos. 1 to 11, etc.— continued . 
Bore No. 6— continued. 
Depth (feet). 
Nature of Rock. 
Details and F email Contents. 
158-161— 
continued. 
Fossils— continued. 
Peleoypoda. —Nucula semistriata, Tate ; 
Glycimeris halli , and var. intermedia, Pritch. 
G. maccoyi, Johnst. sp. ; Limopsis beaumari- 
ensis, Chapm., and var. depressa, Ch. ; Tri- 
gonia margaritacea, var. acuticostata, McCoy; 
Pecten anliaustralis, Tate ; Cardita calva, Tate ; 
C. spinulosa , Tate ; Corbula ephamilla, Tate ; 
C. pyzidata, Tate ; Venus (Chione) propinqua, 
T. W. sp.; V. (Ch.) subroboraia, Tate sp. ; 
V. (Ch.) hormophora, Tate sp. ; Barnea tiara , 
Tate (dorsal valve). 
Gasteropoda. —Liopyrga quadricingulata, 
Tate; Bissoa (Onoba) bassiana, Hedley ; 
Calyptrcea corrugata,T&bQ; C.kalimnce, Chapm. 
and Gabr. ; Natica cunninghamensis, Harr. ; 
N. perspectiva, Tate ; N. (?) substolida, Tate ; 
Turritella tristira, Tate ; Tyiospira coronata, 
Tate sp. ; Marginella prcejormicula, Chapm. 
and Gabr.; Ancilla papillata, Tate; Pleurotoma 
(Drillia) dilectoides, Chapm. and Gabr. 
Crustacea. —Balanus varians, Sow. ; claw 
of crab, indet. 
Pisces.—O toliths of teleosteans. 
Notes on Bore No. 6. 
The first 104 feet are composed of subaerial accumulations. At 104 to 
114 feet there is an extremely interesting occurrence of consolidated dune-sand 
material, with shallow-water foraminifera. From 114 to 154 feet the deposits 
represent the Kalimnan stage, in which Turritella pagodula (a species from 
the Jemmy’s Point beds) again occurs, as in Bore No. 5. From 154 to 161 
feet the fauna represented i3 an admixture of Kalimnan and Janjukian 
species. 
BORE No. 7. 
Depth (feet). 
Nature of Rock. 
Details and Fossil Contents. 
Surface-4 
4-8 . 
Reddish sandy loam 
Boulders of hard lime¬ 
stone 
Quartz grains, sub-angular to well-rounded. 
Residue, after dissolving in acid, a little quartz 
sand. In thin sections this limestone shows 
spheroidal aggregates surrounded by a white 
calcareous border, and scattered through the 
matrix are numerous vestiges of (?) organic 
reticulate structure. Alternations of moist and 
dry conditions would account for the forma¬ 
tion of the nodules. (See Tate, Trans. Roy. Soo. 
S, Aust., vol. XXII., p. 236.) 
