imide ORR RET

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Table V.—Analyses of Spring Waters.
1 2
Parts of solid matter per 100, 000— ee Fae

Sodium (Na)..... Gee em eae et pr ee ne Re ne a ee gee 102-25 | 39-49
Potassium (K)....... Se fe ee Oa Bete ee eee Eat Stee Se ree 9-95 2-49
Galeri 46 a ences rece ee ES ee a aE i SE 2-27 | None.
Magnesium (Mg)...... Peer Pee aied ens Seem eg eae at ae es 11-93 | 29-25
iron (Hey PRR POE ES EAA S eS Nt ER Rite Aenea es ere arey SA ee Re 0-25 0-22
MCarbonic-axeid (© Os\or ct oe Te as es ee ee BS 165-91 | 110-89
BicarboniG: acid Ch Og se ee eer a ene 34-32 | 75-86
Chilormet@ bs. re ee ee es ere eos 9-82 6-36
Silphiricg Abid (Owes fist eS a Oy ee Sie ae .«...| None. | 16-43
Phosphoric seid CPri).<:5 4 .2c. a eee ns ESS SS Ned ag Oe a ie ie a eae = None. | trace.
REEMCER: (ONO) 3) eee ate ee a ee ere Hess Sa Tie ie ee Les 4-99 2-21
Fluorine..... haere Soe Seren Were Cai es ena oe See Rae Pe Bir natn et a Bees et Te gees None. | None.
Berns) ses ae SS A Ee Sa ee es Ee BSS None. | None.

341-71 | 282-90
Total dissolved matter as found by drying at 180 degrees C................. 309-15 | 202-09

DRCCHIC Cltvabys ee Se a a ee ek ee ee ee ee eee 1-005) 1-004

“Reaction, as received, faintly alkaline; after evaporation to small
volume, strongly alkaline.” Analysed by A. Sadler, Mines Branch. The
temperature of the spring water No. 1 on August 29, 1919, was 55 degrees F.,
air temperature 66 degrees F., in the shade. eS tek

Two partial analyses are given below of cream-coloured, earthy mater-
ials occurring near the spring at 141 Mile House and whose waters are
represented by analysis No. l above. The earthy materials are very similar,
in general appearance, to the large deposits already described. Both
analyses are of samples taken close to a stream 7 inches wide and 1 inch
deep, issuing at the spring. Sample ‘‘a” was taken 20 feet downstream
and at the same level as the orifice of the spring. The material is coherent
and has formed in horizontal layers. Sample “‘b” was taken 100 feet down-
stream and 18 feet in elevation below the spring; the material is cream-
coloured, and granulated, like the impure earths underlying the hydro-
magnesite of the main deposits. s 3

Table VI.—Analyses of Earths Deposited by a M ineral Spring.

SSS a aa RE RSS eS Se ie te Ss eS

SiGsre si is a ea . . .

WOO se fe re eke ee : :

OO Se ie Ss a eae SE SEES :

CRORE Fee es ee . :

OES Ps ne eee . :

PN SEO) eee Sai ph es ee 0-10. :

PRR hittin ast feeh empty fo ee pets ce) Qt a a ee yee!) 53 Sars

SOia se See 2

CO: estimated............ Siete ; 10 2

H:20 loss below 105°C ; 30. : |

H:20 loss above 105°C F 0.

Carbonaceous matter x ei
WOtaleert- os. aii tot aiean cae Fe Pee ; -75 | 100-

Fe ee es x

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;
a ay eee