Gry ony jpin sith _ealioas Uadepucsleally eo any pio toch chery GILICHTE STRUCTURE Trnbacdurcti | Al silicate mine als contain St on, fons. Since develops —4 arg a eng fe lama elds a evanities of scLical Aoepalyroe | Hghea the temp. ef fermabin Lo Cg tata 4 Silisatt_taiarnals x Lopurus toch displny oe pu painly pt pi allisabion et xu His pet nthe i ok canal “Tans te Labrtobaddan, + ean — Cepindin, seo palyeatnisation and enkent cf) intensbral ealions dike fer, mgt ate. hcp Gne she. ehtedig de pan. ef cations + ‘Wii Ateente packing: is dense hence have high spsynmity 6 honda. y SILO nablo. te) 12Y and net share. ey (4) fut ee SUiirranite, + Kiganite, Spine ©. 0. Hl ib os fatom ty give nse bo isi boy Mette ® sito nko & WFAN We cree) Ext figee grnuplDate Page No [Cy clost Leates P\|\Contasns aogs ol si0u! tetval Sig’ Sildéon ! Omgae vo 113 AGuoevl dtc in S'OSTe pn eek change in = On 2} foch—Sioy teherahedaa shares two of tlt eaygen ul stig tetsahedaa § sings todtnision S44 6.6 talathudaa ane eva! Tne _ctifdercont g 4 i Binge Slauclure’ are ' Sin O49 by Onl $1,204 ras t af, Ae t net charge (6) , ce) 6-12) Saoak, Ex~ Benctonite, Anincte, Beryl | Gl rastticates AiChacn silicates i by Sidy ted jot toa el toform Chan of. Slagle chant esi26612 5 Double chara Sit0e UI) onsish of forge oof Linked Sioy Groups each sh fwo oaygen © have tompocdhtonn(Sis0e)-) chicas iave chang 21>. bor ain Ca, Mo 24. iO-mabonis It & ine Goi Pyrat seb balanced iby cations. Chaink mans thes fell i 0 I i Doubles ¢| fog Known “as ena Gu3: sieglen hasd we . a Pe orredged: posniichi-t0 edit alkes/ ond : mt Haden st On-.atom at aeegjule tr intervals i. 5 sito cuh General Sts. CSipn)t = seats 1383 Ca? Amphibole Grows, tornblend&, Aothopyaite ete Phusllosi Shoei i - u i Oy tetsohedaa Unked by 3.6 thre ob tadefinibety 19 9-0 netunve of dict Cad fain Stro=4t! & met chose coy ) Sheet forms a plonas Ha ‘ ‘ Icha: ‘ > 7 : « . pSudebtvaganal habit nod petfeck basal elewage—poaaiel plane of +> Mott of munexal ane (-oH) Baar Bins oh Plakay Musto! abet, low Sp grevity , soft Flowih le. Oat Mica; ioleter tale eteDate Page No. Ceetnei Lente | Framwork, silicates: (2 i Leach ef 4 enygeassof gach telrahedana shared, bey mpc Letroahedrras. Gives'a 113-D:nelwork, to johich® SitO Pend ..& table sand stage end a tesueth a itlalie rectal (103) ‘ 20 erdes to produce a. net =vt sung an Prick Some silivon..tons “aeploceof py pert cre cations Wine Nat, cot Kt wGtaAce” ve» hacen seater : jetting Sipe Minesalo: 4 welt a 2 tard \ aotor'e Ainsdes 20 fpodaid opbednodsd 10 idle bJnJ minal feeudan O-¢ nt pied initeh al : De arent ioe 2 ttyso Sidenagiyn Arsdyt ccna nm recut + 7 F hy Nog ath to: Alnrenins be 20/4 atin Janes WAS q .Dan Page No. Rock fonming Minerals ey Rock Leming intemal, >for a A feclen— pl Ste *4 [yoke And ane” preduceds Cuming puocens » xy With So the three major ‘oleqiz of cocks, the di ffensnte socks tagpons Snkaastesx tl buy dd euan Aypisa mite ase Wy Silécales ano ta bas fi theses inpeatoal 9 reock= Poynting’: mirisuale | wy. Most of then Onda the cs ton asce ptt lpn Golo! qganuph’ ox Ee having sneinhers_of phipsical »— aaa ae : | OS vol! as f 7 fons Z Noo ~silicate minerals inxe much Jers. impovbaot ‘as mck } foaming: ‘erinewaly: Of the 2000 Known mineral Apuies leo ace “woek-fommers of which only about two lessens ave} most Commons + Rock sharing wtih lf e clawcfied) ad. Dang hws Io ehw