208 
From N.E. corner of Allot. 48, go 356 deg. for 48 chains.—No. 4356. 
—Collected by Mr. W. H. Ferguson, 
Clonograptus rigidus var. tenellus. —4356(F). 
Rest indeterminate. 
Age.—Apparently Lancefieldian. 
b Report sent in 16.11.08.] 
WOODEND. 
From Woodend (Braemar golf-links).—(Nos. 2^2 5-253:;. Collected 
by Mr. D. J. Mahony, M.Sc.) 
Phyllograptus typus, J. Hall.—Nos. 2526, 2527 (counterparts), 2531, 
2 53 2 ( ])• 
Diplograptus sp.—Nos. 2526, 2527 (counterparts), 2529, 2530 
(counterparts), 2534. 
Climacograptus sp.—No. 2528(F). 
The remainder are indeterminate. The altered character of the rock 
renders identification difficult. The beds are Lower Ordovician, and are 
probably of the same age as those displayed a few miles to the westward 
and about four miles west of Gisborne. The exact horizon is doubtful, 
but I think it is near the middle of the Castlemaine series. 
[Report sent in ip-3 08.] 
Mansfield- 
From Flannery’s allotment, Mansfield. (Collected by Hon. D. Mel¬ 
ville, M.P.).— Nos. 2747 (765), 2748 (766), ^2749 (767), 2750 (771). 
Dictyonema sp. Nos. 2747 (765), 2748 (766), 2749 (767). Unidenti¬ 
fiable No. 2750 (771). 
The genus Dictyonema has a very wide range, and its species are too 
imperfectly known to allow of the identification of horizons bv their aid. 
Besides this, the present specimens are too imperfect for determination. 
The genus is said to range from Lower Devonian to Upper Cambrian. 
[Report sent in 23.3.08.] 
Kevington District. 
From Williams’ Cutting, Goulburn River. Collected by Mr. 0 . A. L. 
Whitelaw.—Nos. 6017-6023. 
The markings are not organic. 
From Boundary Hill, on spur between Edwards and Snake Creeks. 
Collected by Mr. 0 . A. L. Whitelaw.—Nos. 6024-6064. 
leptograptus sp.—No. 6024(F). 
Glossograpius sp.—Nos. 6024, 6025, 6028(F), 6032(F), 6034, 6039, 
6041, 6057, 6062. 
Diplograptidce. —Nos. 6024, 6026, 6032, 6042, 6051, 6054, 6062. 
Dicello graptus. —No. 6035(F). 
Rest indeterminate. 
It is very probable that the fragmentary stipes are those of Dicrano- 
graptidae. As regards the other genera, CAosso graptus and the Diplo- 
graptidae are both Upper and Lower Ordovician. If, however, Dicrano- 
graptidae occur, the beds are Upper Ordovician. 
From Star of the West Mine, Kevington.—No. 6074. 
The specimen is indeterminate, and may not be a graptolite. 
[Report sent in 16.12.og.] 
