Sxry.—On the Mineral Waters of New Zealand. 485 
Analysis.—continued. 
Chl 25 2 
d s s s is :. + 08:55 
Sulphate of lime dis e x vx 2 10:06 
soda Ae še = s 1:01 
ihr as phosphate .. s4 $. ve v. "54 
Silica, free ig x $1 es Us oe 49:95 
Iron oxides $t E. eis ʻi Ei traces 
154313 
. (7.) Manupirua, on the S.E. shore of Rotoiti, a beautifully clear 
pool 20 feet in diameter, having a temperature of 107? to 110°, at the foot of 
a high pumice cliff on the shore of the lake. The water is clear, with a 
bluish tinge, harsh to the touch, and deposits sulphur. This pool has a 
strong outflow of 40 to 50 gallons per minute, and is reported to have great 
curative properties. | 
Analysis. 
Mono-silieate of lime 2 zs e. Ae > oe 
> magnesia jx ee ae es "FT 
Y. iron is m e. x v 99 
Sulphate of soda  .. y x ys 4s + H00 
lime s Ss x ; Ac 248 
Chloride of TPES € ve d es 2 “47 
sodium m Vs ks i. 1j; 035 
Silica, Sub s J e s < -8:53 
32:45 
No. (8.)—From Te Kauwhanga, 1} miles from Ohinemutu, a powerful 
sulphur bath, having a temperature of 204°. The water as received was 
clear and colourless, with a distinct acid reaction, and evolving an offensive 
odour; it deposited a brownish sediment on being boiled. This bath is 
reputed to have great curative properties, and is known to tourists as the 
** Pain-killer.”’ 
Analysis. 
Sulphate of potash ex pe zu A x. — 2:96 
i soda . s ws as zw 34:37 
Chloride of sodium ie = ex =b s+ 69°16 
r calcium oe 2s vs e i 
» — AP ss ia X = br ri 
rs vs č: žė ms "25 
Phasphais of pii iia e "ovi ur ua 
ilica i us 2s es ss 1609 
ioiii ai E. se $s $e i 40 
Sulphuretted hydrogen  .. oe se vx uc Sgi 
