Note fo p. J.J. 



With rufcffincB to Ulo viewi in Ihr leal it may bo laid thai no coB*,*fcaLion could ink* piece till the tempera Euro 

 of tbn whpla man wu hi that of fuiion , bacama nnlll tlion there would be 4 cenitani In! sellings of level between 

 the liiceeiaivn upper w dtuier iayora njid the lower. Wit bout reporting te I be itippoiiiion I bat gradual ex paction 

 H in WoEce- rniy hegJn prior fa congelation . it seemi nli-ar tint in inch d. dt#p.p» fluid ai inoflen flranite nuder ipreet 

 ■nrmure, Iba poiiige of en* parti* it Ibrcugh another mutt be effected with, difficult/ And very ilowly. Between 

 [fet IrTfrL ft! tolutb Lfae n3ba;ErD.Uiii liMEijirralHra Ceaaei p and ibe- re-ff frjeralijirj lUrfara , Ibirc DDll « ?U oUch a Elriid., 



in- in inajpiibln and Terj gruJupL diaii-nuLion of beat K and dicp mum wij be viewed it milling ef layer* of 



rMrafldejablP tkitLnetl it any uUB (if hicb tllft temporal Lire ii aLmeil uniform and \wlmfrn wpir|i ar>4 Ihi' ni!_aci'!i1 

 Jayen |ha IriPBfir of Jiflal Ja i-iEeediCgly *low. J| mey be J*Ffljf!Or Eo ei^ino Ihla furlhrr , lj*t*Uie wbflO tFt" (Pit 

 Vll wrilt-en 1 otei looked iba chapter in Air, LiaiV* Pi iiiejp5i:i £CJl.. \I.Y of fJook II) in wkicb he conErererta Ibe 

 doe-lrinn of I no internal fluidity of |ba globe bj an argument wb».ch im partially on-ncicd te a-ars* ef Iba above 

 Trswir BlLlinujflb ii de» net iultrfare wlln my general inference*. Jti object ii la prevo that an eou*oli.datiohi at Ifao 

 IlirfiCfl ef a fluid tntli like the globe Coukd" toko pUctt till t Kn whole. kn.it bern rprloced Er> a unLf«rnn Ki'aL or ftbcllt 



Ihut ar ineipiriiit ruiion^ Ft #pjpnn f n&bn p. 4-lfiJ Ibit II. Fr>iiwi li-n-d . irtdep<cidi'nitilj r r «d-optid lit* u&tt ftrgameflti 



a-nL khnl lit Jma|in«d Ibli if the gltiba «rar paai^d fnim a Jjnjuid lo a mliu ilnln frj-" radfalioji «f hr*t s L he <rr nt r-aL 

 niLdLrui ciiinL ]ia.Te bip^un l-p fisnj iod =PonnjliiPalp fint. rb* piiRfijinl /keIi en wbkn Mr. Lull ralifi arp » I bit 19 

 Ji>rig ai a fragment af j» naafni ia warrr Ehq- E^m-p^riii^ra of th-n m a Efir P ^nnjiuL hi* rai««d ab a va 32* , aid that 

 Pro feiiiji- EfjuKir, round (hjil whi\* a pife« of iron sic, rcrBni49il PHinpntd in a ruelren man of lbs im» anfe- 



lEance, 111 llfapcratura CHUld rj«t h>0 flUied above Llin nirlLin^ point. Th+- rein^tVi in tb« IriL rrlalin^ Id tJifl ori- 

 gin tiT ai'atiitl>D Ili'Uclllli'o io 11 »l fe^iiEre' to inLSTiie Hilt |ba temprraLurB of ■ [?ri|iiiLC mill Wif at pr nturb 



atiftvo itit of IE* milling point. « If njoormtnra s ll ilicm^l bri rf-co!llf etpi. bS^lwr frjt'XH than taatil wbieb buall rnn 

 rjrlit in lb? fluid alata ; and ai tlr. Ltell do^i nol teem to J*nr , « iLh H Poiairyi , t he neiiifaiLily of a tuiit 

 h-ri njif for mad wbtii too rjantral UmptralMro j| n^p.r (bat sf fmion. fail ifmarJi* uvr nn[ in^entll Elltl With tbo bjpo^ 

 lbp*ii tbal granila bu cryifnlliicd id lueceuiva liven. £ria if I bo igranita lluid apprnhrzlwd to Iba eon rli lion of 

 Vinliir, illilfiad of beirsg coraparatitfe^ Vfrj inm « Jflfl fangnlaEioa of Iba rir*L Jbjckt wonJd ii'nd |a maintain Lba 

 Cl-jiiitLr ef I fin nnxl fur fo-mr Mmi ■ nai reertlr bj arreiling I lie in t«rrbin^o of parEJoitJ br whlth it* brat fandj 

 lhvtfafrl« been trauifirrtJ lo lb« turface , hai «u,biLiLutin.| for il Iba pro-em r>f con due Lion / bnl hf adding lo H 

 %\m Jar ja qiirxoLiLj of btfrot caloric t-ionlM m Ibf «cl of G«flfl*Mi<?nH Witt rafurenica. aoaroTtr^ lo tlr, Ltui/i nr- 

 puTr^r.t , H nrjiPij wB 1 romarkid Ibit lha candtlioait la wliicb a frigmtnl or it- >:\ » E njiDiorl *bch itnnariad in 



a llnid man of lba aama tnbifance, and. brnl <;omt»nltv a4drd from ■ murra clrj-w to U, ar* T^ry dilT^r^nl fiam 

 Ihoic of a rniit rriltna; on ihn lane fluid k in aenlack on eiis lida with a refrigerating iBTfarM . and on tbe otfaer 

 olth ane lo whieb eilorin i\&wlr aieeftdl from, a aobrrfo far Mntr. Tho iranmriflJ Ffapjinerit ■■ rorelo-prd in a ra- 



CbaatJr>p{ racrtrnni, Tb* dloaEing croit af btivean Iwa inodia . onf alou-lT pjirin-ff faeali tfaa otber abilracUn^ il- 

 .rerj'ud 1 Eberefaffh at vraieh a eruil etn ba formfrd ■■ not daldriaitied n'rnp]^ by Eba JTuiin^ point (tbal la, no- 

 e^tiiiiJy poat|vr>ned iLnEil Iba nrfaola maai baa rraolirHj ill InurtiiE field l^mnrraluraj (ml ji diiterntmed bj Iba reli-tsra 



■ Bin ai nli ink bcit moioJa Ibreupjb Iba ubif ance- in ita Fly id it ale * etid if roinfuclrd fi em it vthen in ill lelid 



■ Late- The laliir il an illdelerni-kiiale quanlilj , depindinpi , ai LL in ftomn rnpaiULrc- jLor-t. uonn th^ not nrr> of Ike fcfi i- 

 jremting fapdr- ffn|, laving lb*l of ritw k il ii »?idenl Lb^l ut tbt beat dirainiibri, lba rala of ilv pauaojo 

 from eiKt level te another will ilia deereaia + becaiJii* tbe tnation of the parUeletol thn fluid amnoijil Ibeiairhea will 

 tin impeiEfril ai I be deniiljr jnerraioi. Tfew l«n^ Uefora Ibe naif gp-nemllj ii reduceil to tbn teinpcralura of fuel on. 

 lb* dnffiiilv eT \\m higher pertian raav ree^h lba peiut a I -ubieb Ibe rale ef mdEion baa aiibiidnl te that at Nrfaieh 



llfll il given uJl' by a d e Ll J erUiL, fLBfj-r^rrafjori may eom'P la m lEairn al *wliic3i h while th-P upp^r tajeri ara at and 



rifvar thn noi.nl of foilon , |,ba lowtr maj be far removed fiom. it in pre pert inn to Ibe depth of tbe man. ftaeauie 

 171 a receptacle of wnler einoied to a eekl atnaoipHcro we iee a rapid iolefclianrjei of pm-tMri , and the forouEiotL 

 ef 3ce poilpqnail till all Ibe hwer ]ayfn buve reached Ibe temperafui a of eboet 40* , wo are net enU'lfed te eon- 

 rl udo I hat in the ineeenrro latere or a deep- tbrn of ilenia ipollen p<rn.niEe tbiro will be a armilar rapLdit^ and 

 i*it*nl of mutual melton of particle*. Hi™ in Ibp eftie irunpeiPii; by Ui- r Liett ef I ho fb&e eemiilFRJij: ef Witir 

 bifing it I hoi centre a ternneraloro ef 0JQ0 a ivJiicb pjradiiailv decrcaied tewardi the vtrwmttrmn *hero a era it 

 *f ice ftfly milei In thlekneii eaiited r da Jl neeefiarf tKit wo ib«uLd admit with tlr. Liiu H - ica woutd ioon 

 nmll inln an almoilphtrt of »te*m. P In a lajer a mite in thieknen the Umpire luro would not intreaie ene decree- 

 At S milei beneelb Ibe ice tbe ten|iiralu.re would ba onlj 4&*. BbIo* Ebal the <uiin|fr citrrint* would flnt be 

 eneeuntrri'd , hu| tna rala of Eknir nioliari in a lajef > Baile En Ibirkntii in wbi^'ri tlie lamruit only differed frera 

 tbe beie by I 4 weald be 10 extremely ilow ai to be FriinmihUi. Rul , lo render Iba eaiPi of ■ glnbo of water and 

 a globe of pfranile mnra Biiolo|oui 1 thn f^loba of walur abenlil bn nipnlird with a refrigefatinfl atDJOinbcre at a 

 fcrmnaralnrn more lhan 3QIH) 1 below uers i for ineb Ei Lba dJflarcnea ef lemperalure bclwran that of Ike almoipbere 

 feren tabEag thai of the equator) and lba fuiinrr paint ef finite- With ineb a medium n or even ene of wbicb 

 (b» Inrpnr j,iqrr' wai eelailited aeeereEnt" le the fining poinL of Irappean reehi , tbo beet rjirre eff en lba upper 

 ^irle of Iba Itv craat might exceed Lbal rflcisireJ ffom belew e^en wilh a central temperalere ef (ttflfl 1 . 



