PLUTONIC ROCKS.—CASE II. 11 
He 6 7 
102. Eurre. Map No. Rb 8. 
Section 13, Sutton Granae. 4 sheet 
13 NW. 
White 
Ite, granular felspathic rock, with 
very little mica, E f 
* P 
103. TERNARY GRANITE. 
Map No. Rb 75. 
Road between sections 48 and 49, 
„Parish of Langley. 4 sheet 5 
N.W. i A 
Brown, fine-grained, hard, granular 
8ranite, with very little mica. 
*104, FELSPATHIC, GRANULAR 
Rook, ° Map No. Ra 7. 
Wear allotment 2, section 24, Mal- 
don. sheet 14 S.W. 
‘Traverses Silurian rocks, and con- 
tains mica, Quartz is not visible, but 
forms, probably, a component part of 
the granular base, 
"105. Fersparuic Rock. 
Map No. Ra 33. 
Near Jackson’s Reef, Maldon. 
+ sheet 14 S.W. et 
Dense, white base, with quartz and 
black flakes, probably decomposed mica. 
*106. Fersparuic Rook. 
- Map No. Ra 34. 
West branch of German Gully, 
Maldon. 4 sheet 14 S.W. 
Similar to the last. 
*107. Fersparnio Rock. 
Map No. Ra 42. 
Near the Otago Reef, Sandy 
Creek, Maldon, }shect,148.W. 
Occurs in Silurian, and consists of a 
fine white, granular base, with white 
mica 
*108. FELsSPATHIC Rook. 
Map No. Ra 94. 
Victoria Reef. 4 sheet 14 N.W. 
„Similar to the last, with streaks of a 
pinkish tinge. 
*109. FeLsrarnic Rock. 
Map No. Ra 35. 
Near east corner of lot 7, section 
1B, Maldon. } sheet 14 S.W. 
White, rather soft, felspathic and 
micaceous rock, with crystals of ortho- 
clase, grains of quartz and plates of 
black mica. 
*110. FELSPATHIC Rock. 
Map No. Ra 37. 
Near S.W. corner of lot 3, section 
lo, Maldon. } sheet 14 S.W. 
Grey, close-grained rock, with a fel- 
spathic base, and grains of quartz, fel- 
spar and mica. 
*111, Freisparuic Rock. 
Map No. Ra 36. 
Near N.W. corner of lot 3, section 
1c, Maldon, 3} sheet 14 S.W. 
Grey, granular base of quartz, felspar 
and white mica, with blackish marks 
of (probably) mica. It has a slightly 
gneissose structure. 
*112. Fetspatuic Rock t. 
Map No. Ra 64. 
Kangaroo Creek, south of Kanga- 
roo township, 4 sheet 15 N.E. 
Brown base, with whitish spots of de- 
composed felspar, and apparently frag- 
ments of sandstone and quartz. Itoccurs 
between two beds of black slate, rich in 
graptolites, which have been faulted and 
greatly dislocated by the dyke, but only 
very slightly altered in character. 
*118. FELSPATHIC Rook. 
Yarra banks, near the Botanical 
Gardens. +4 sheet 1 S.E. 
Yellow, fine-grained, granular base, 
probably quartz and felspar, with quartz 
grains. The beds of slate in connection 
with it have a cherty character, 
*114, FELSPATHIO Rock. 
| Same locality as the last. 
White siliceous base, with quartz crys- 
tals. 
115*, FELSPATHIC Rock. 
Same locality as the two last. 
Brown and earthy, with small cavities 
from which some mineral has decom- 
posed. 
*116. FELSPATHIC Rock. 
Reservoir, Brisbane Ranges. 
-Argillaceous base, with embedded 
brown felspar crystals, and rounded par- 
ticles of an unknown mineral, giving the, 
rock an amygdaloidal appearance. 
Those marked with an * ocenr as dykes (Elvans). 
t This specimen comes from the same locality as specimens 67-70, Case I1I,, and is most probably 
“decomposed” diorite-porphyry. See Note, page 17. 
