270 MINERAL CENSUS OF AUSTRALASIA. 
EpsomiTe, or Epsom Sats !—Otago, as an efflorescence (Hector, 
1865). 
Faya.irE !—Nelson, in schist, contains 2°67/ copper (Skey). 
Freispar (Guassy) !—Taupo district, in rhyolites, &c. (Hector). 
Fiuor Spar ! ! !—Stewart’s Island and West Otago (McKay, 
1889); Batton Liver, associated with sulphate of 
baryta (Park, 1889) ; determined by Skey. 
Fuutier’s Eartu !—Great Barrier Island Hot Springs, in 
trachyte tuffs (Hutton). 
-GAHNITE !—Stewart Island, with tin stone (McKay) ; determined 
by Skey, 1888. 
GaLena !—Kaituna and Kaimauawa Range, associated with 
quartz, generally argentiferous ; Wangapeka, containing 
an average yield of about 91 ounces of silver per ton; 
Great Barrier Island (Skey). 
‘Garnet (Lron Lime)—West Otage, in gneiss (Hector). 
Black Garnet—Dunedin, in vesicular basalts (Hector). 
GLAUBER Sats !—Brancepeth, Whareama, Wellington, sample 
forwarded by Mr. W. H. Beetham in 1874 (determined 
by Skey). 
GLAUCONITE !—Otago, occurs in schist and green sands as rounded 
grains in several of the younger secondary beds (Hector). 
Gotp (Native) ! ! !—Auckland, Taranaki, Hawke’s Bay, Welling- 
ton, Nelson, Marlborough, Canterbury, Southland, 
Westland, occurs plentifully in reefs, alluvial deposits, 
sea sand, Wc., as crystals in the Ben Nevis Range and 
Mahakipawa. 
GRAPHITE ! ! !—Pakawau, occurs chiefly as thin flat veins inter- 
stratified with metamorphic schist, was largely worked 
prior to 1866; Wangapeka and Mount Potts, dissem- 
inated throughout the graphtolite or carbon slates 
(Silurian) and in the glossopteris beds (Permian), 
(collected by Hector); Waikoura Creek, a boulder of 
very pure graphite in a stream from Mount Egmont. 
Analysis of Pakawau sample (Skey) :— 
Carbon 2% ‘oe ice, DOuLO 
Water : has Joie +(e OS 
Ash a a Sate Oe 
100-00 
Green Eartsa !|—Malvern Hills, filling cavities in melaphyres 
(Haast). 
