PLUTONIC ROCKS.—CASE II. 11 
*102. EURITE. Map No. Rb 8. 
Section 13, Sutton Grange, 3 sheet 
13 N.W. : 
White, granular felspathic rock, with 
very little mica. 
*108. TERNARY GRANITE, 
Map No, Rb 75. 
Road between sections 48 and 49, 
parish of Langley, 4 sheet 5 
N.W. ih ae 
Brown, fine-grained, hard, granular 
granite, with very little mica, 
*104. FELSPATHIC, GRANULAR 
Rock. i Map No. Ra 7. 
Near allotment 2, section 24, Mal- 
don. } sheet 14 S.W. 
Trayerses Silurian rocks, and con- 
tains mica. Quartz is not visible, but 
forms, probably, a component part of 
the granular base, 
*105. FELSPATHIC Rock. 
Map No. Ra 33. 
Near Jackson’s Reef, Maldon. 
4 sheet 14 S.W. 
Dense, white base, with quartz and 
black flakes, probably decomposed mica, 
*106. FELSPATHIC Rock. 
p ‘ Map No. Ra 34, 
West branch of German G 
Maldon. +4 sheet 14 SA É “lly 
Similar to the last. 
*107. Frtsparuro Rock. 
at een Map No. Ra 4g, 
ar the gyp í 
Creek, Maldon, ł ieee ay SW 
Occurs in Silurian, and consists of a 
fine white, granular base, with white 
mica. 
#]08. FELSPATHIC Rook, 
t Map No. Ra 94. 
Victoria Reef. 4 sheet 14 N.W. 
Similar to the last, with streaks of a 
pinkish tinge. 
*{Q9. FeLseaTHIc Rock. 
Map No. Ra 35. 
Near east corner of lot 7, A 
Ip, Maldon. } sheet 14 sw 
White, rather soft, felspathic fon 
micaccous rock, with crystals of ortho- 
clase, grins of quartz and plates of 
plack mica. 
Those marked 
*110. Ferspatuic 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. Ferspatuic Rock. 
Map No. Ra 36. 
Near N.W. corner of lot 3, section 
lo, Maldon, } 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. 
*]12, Fetsparuic Rock f. 
i Map No. Ra 64, 
Kangaroo Creek, south of Kanga- 
roo township, } 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. 
*113. Feisparnic Rock. 
Yarra banks, near the Botanical 
Gardens. 4 sheet 1 X.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, Fersparuio Rook. 
Same locality as the last. 
White siliceous base, with quartz crys- 
als, 
115*, FELSPATHIC ROCK. 
Same locality as the two last. 
Brown and earthy, with small cavities 
from which some mineral has decom- 
posed. 
*116. FeLsraTHIC 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. 
@ 
+ This specimen comes from the Sah an * occur as dykes (Elvans). 
«qecourPesed” diorite-porphyry, See eer ee a specimens 67-70, Case IIL., and is most probably 
