145 
Hydrous Silicates. 
ya Tove A 
PS ES 
Oey crise ouinry 
epaiq ecg 5 (i) hg SaaS, ee a 
: * Iep 0} wood Ivo se weeees § OPTXOJOI 
is TA puv 4Jog Pe Naat A en [180d | 52-7 { SP) | anrmed 
9g'g  **optxojord uwolT 
6 Toe secces eos eo BUTOINTY 
yeppococ **BOTTTg 
or SB ]Og 
poctereeseessess Bpcg 
ystaMorq enbedo 0} ye ee he 
% %S : ueontsueiy, | 70t BIsousE 
$i is a “ystaoers Z vrron of ‘‘@prxombses meet oO 
ystféeiy Ost Vv | eguz *?- BUTUMTy 
esor c ean BOITIG 
Seg intrest IO}UAL 
"y Ystppos 
r e Io ystnyTq *ATIvOg rey Ries igh ged ey I0JB AA 
9°% e[qixey Teseq ‘OD ont US ‘USTUMOL *“ksvais STa0. “eg ccc ‘> BUTUN| 0 
epee. fet ae sajuog | kt )aUO “T BUA) “Spr b-ogtgtgeett: poe mater [oon vesnecmen Soriy | SrUHOey 
“OFT. 
at Bee egreg teas 10}B MA 
‘ju “SSB jueTna0Atn rs moonysuel PURGE nic eurluin pudo 
2 eae = yee ® | sgoors ‘ogre | 7 aeinta ee gteees naeeeS Dorne ouvydoyy 
“UsTnTy ele d 
paged ee pppoe vets FOqBAK 
ae aes snoa 04 s£ei3 % SSOTIOTOD 0} O74 JU918: Tf Phere | Sod A ouliry 
33-8 ie HI onan naueen ah | IO OFT M a uosLd-apade ~SUBIFQNG | gpg cette ttt purumnyy oN oId 
"STOOIZTA | grap rere seer see BOTTTG 
pus Ajre0g : 
; “aT "LSXG GOVAVATO : INGO uad 
H jp arsay "'SKUQ ALIOVNGG y ANALOVUG MVHULS H woToOO HaLsn'T NOLLISOAWOO STVUANIN 
(GaNNILNOD) GALVOITIS SNOUGAH 
Brush & Penfield’s ‘‘Determinative Mineralogy and Blowpipe Analysis.” 
Dana’s ‘‘System of Mineralogy.” 
