Show A AMONG IONG THE GLACIUS GLACIERS grand paid Romark ablo traces ot of natures powerful Ea ginory I 1 at the iho american institute 0 cf I 1 at nowton to M ilio I 1 a lecture ans given by lion jarras W patterson state resident of bublic alic instruction of now new mattall shire upon A trip amons among tile tho Ula clors mr soo baia if wo iva co cc forth into our fields and anil reso ho he begun boffi in iva sea 00 oo rocks and scat lorod load la in countless num bart her have boost been fro from their original beds bed by somo giant force orco which the world ili a primitive age but iown ioco the lasion period it if lu in our northern latitudes wo we lay bare baio the banks of ilia wo we find tile under lycoff ledges nil ground find and toy b some powerful of biltl lil tl has massoll down delve 1 li t v plow ing at intervals pari Uil furrow ja 11 their tough and tan unyielding yielding surface everywhere I 1 very where over our northern no atio lit aul workers of ct the iho olden oldia chuo lic hane dumped duniC tl their weighty burdens of drift n bovo the iltis of abet A yet air iq r period find anti the iho us maiac of p mingled dirt gravel and idall 9 found among our moun tallas and stretching cast cal end and west along our temperate zono ell 11 point to a time when glaciers title lilio tile tholo of greenland moved over our continent nent and soul out their mighty borgs into the iho see but nihon cc conic came this power and whither iva lias at 16 gone it Is tho the question which naturally cornea lc ic every lip thera tiro are abundant tc lc ielo believe flint this glagla force 14 liko like so no many other of tho the operations of nut uro 1 ro several aci stcl it voas here natal propounded ul at different times to account for the periodicity of glacius action that of call vi luch PC ftc counts forthe for tho varting mean temperature of the carth by the revolutions of the seasons around fact earths bartha orbit and tho the changing lily of the orbit itself seems to ili bv the iho moa mo rational winter tit fit aphelion must bo be loncer and colder than abi io winter v bulor tit nt per peri italian and the iho variation va rution must increase nich ilia I 1 bereave of the eccentricity of tho ilia orbit nod and with tho the increase of tho the inclination of at I 1 tho the axis of c tho the earth to tuo tile plino piano of its burm our modern glaciona gla ciora are arc produced liko LUC ancient anc kit by iliyn AN low temperature acting upon the iho ra ia tire of the atmosphere tile i ater reaching t tho b 0 valley throe of us MS A an I 1 u i to a wio no ito the m coni cent I 1 11 munt blanc having so s ared five sann r f kle ms u 0 vero ld lag in 1 lo 10 with heaby har harp 1 1 I 1 a lu in tho the rates boles and heels aud and vi eiith till busk brakina ints around our oui lower limbs L ch man was ivaa armed with ith fi a loll 1011 long alpen adock having a steel spoke in one else CIA tro tae guldon look ionic with them au an nillon nice binl 1 1 I a coil call if f strong rope with leathern alhorn lo bo il at at luto rols of foot thus ad me started on oa our li at 11 ip up oil the eleezer el g eeler rep 1 n I luna ibo coolant was easy m anil iv lial laid trouble lo ba hut after face santa distance wo ire began to luiis crocks cracks or fissures in the iho fee which 0 ito o ceru obliged to loop As yea wo advanced the opening sor crevasses cre wider and more moio to p iss at length vo a cometo came to one me it ali a 0 foci v ido iod to an ail unknown depth our loader leader start slopped and bullied one ut of the heavy traits about his waist mid anti lm ol l I 1 be act no to ino I 1 listened ahia about ild end the iho third to tho the second iredo faud it to lo tho the till I 1 a 0 were vero nil all barcz sl or raised together thu lams r pared tile tho rom fore most moat guide plind f copon upon tho the edge of tho the crevasse end giving ft a sarus oval wo WAR followed him in order till a all it were b r over uno ono of at our number it a short inan nano failed ofa ot a secure decuio landing oak tuo i ii z r bill ropo wai nid we 0 I 1 still him up bund over he bubil ul we lo 10 repeat 1113 operation caf ration till bosti hostiuck wk a crevasse some tweety feet feel vida mida lloro lie re vo tonal a ladder wadi kiili heave in tile lower cal which ono of the guides drove into so tho the ico ice bolow below tile surface anti anil then dropping it onto the iho other side let dowa dou i I 1 no lie ladder anti anil to ti lite na it a above we ve all followed suit nud anti barely airel r landed ou on tho the other side ado so we continued to lid ancas till dilvo iva reacted the retail able four our Welock lathe in alio afternoon here more t ban ten tali thousand foot above lie sea ca wo we spent eik nl tho the night ni flit intending to complete t tho lie ascent tho the following morning lilt but a thunderstorm abona us no up ilia ilio to mount meant EI a covered the rt I cri cei vatha v ih BIC m cr ing of glenro lea ico wit 1 I i ronde rul I 1 I 1 furl u art lie il dir aroas so that ilia gl too ico i fused to call us up to the au W ic c wo we turned back rut crept call down ilia iho mountain moui tain or 11 taurel ire fee alone at ono W ontjo on nt two we reached rea Aed a arv sofilio of live ilvo wi with I 1 is a darrow n arow loue a or diw co hey and und bud ft ct oril tant tim t was a pe pc ous glint and wo iva our tender lender will anxiety up lit to like cilc cde cautiously ho he cut a lur lot his foot fool hl hij apan abo 11 air hini Acir it in a apoi N uon ron cava a stirring anga mn ga m 1 I 1 I 1 alny flat upon tho iha ico ice arrested ilia hi find and a ailed our corning ono by onu ono in ail the same manner on 01 ra our clotel wo iva found the nervous strain tied been AN novel 0 ono one but were ready cready tho the next morning forth met do glam wo we went on art foot unit I 1 ilia out ont niilo tu to tile vert land in ilia iho huici which wo iva crossed and a nl rec rosted and studied with go kiivit call liiro am too ori orisan in 0 of glac tarK is cagily under stood but it is difficult to ta account tu sati balisano tordy fur for anousis of their no on the OULU side of the alps w wo 11 and the iho snow know line about eight thou Mind AN it 1 feet 0 t above tho sea all ali moisture tho ilia I 1 line nic it in JH evident must bo be condensed all end d coach tit tho surface as or grants fated bonow or an 04 half when the iho aides cf c these lofty heights become overloaded with wilh abow it pushes down of its own weight find and sometimes somo limo diblee thousand feet below tho the frost li it to 10 into inlo ilia deep valloy valleys below tho the doplh depth pi of the iho snow and ILU ice wall wi il be cil by tin tile 11 i of 01 the flat llcy illey and anly bo be front from 0 01 I 1 madred to lu i 1 u hundred feet tho the to 11 r lor for Is air ej ca where tho the mollo mol lo r r i 1 ilio lie cicat below Is in bulimic balino eJ by b I 1 hiir MI 1 i iv 17 0 I 1 airow and ire train froin tho he artia ini r i i 11 ir 1 fiut at I 1 of course this in I 1 i i 1 na na alj 1 advance and remiss willi it i i I 1 i c of tile iho meau ille X h i bait already been abua anua assim I 1 i 1 glacier is ia in an motion tile of 1 1 it Is the iho moMin nl ur of 0 ing on tho the surface of i tal I 1 fin eliut object acor tho contor airo cu ki 11 ll il more rapidly than those neo i it ls ides aro are retarded by ill feitl littion oi witt vil its banks bank liessen li essee MO iva later that ilio move move intent Is not in ili mass lili issi but bul molecular various theories havo have been becu started to tic oc count for lino motion olion iu it has bab been oaid that mot tho the wati Stat of the altow above nuovo und bold I 1 to 9 blood the ibo khi for pubs it donn the iho in plane piano on DU which it rett rests undoubted ly AN foreso of title abl kind must musi c culat but bul it if that wei 0 all li it woula advance us un a u wild block balch v la is not tile ft foci A ailiin it liaa 1143 been that ruins cairl I unit molting bolting allows r e r 01 1 11 ul I 1 U 1 t 11 tv 0 nuat LA list ancla yf of tho the and 1 ahon fiu jin I 1 I 1 PuRit six it 1 l forward by the force orco of 0 P massilon hut the glacier moves in wt J 1 lea fco does not inel t slad and in in too ici when it does docs not from another has a ginned affirmed uial ice I 1 I 1 iongi r 1 britti cand unwittingly u 01 1 and gelatinous bud and move leaves andor fr PI I 1 a 1 like t v lyndall anti and huxley Y text n a later upon ran an extended serf rl 11 bopa im lutta will lea ico cru 1 led iod 1 into ft a ff grana lite litel l stale mate if aubut tt 11 I 1 to great peas suro will readily take auy any it I liina 0 inca ir awl to re turn blumlo to a olad solid and tea 1 A wi dill aull yo ko tho the el 01 creaso a I 1 I 1 y yi 4 A own I 1 J bulc ol 01 table weight of amaitis t tell at A I 1 arf is ia ground up mid anti made inide to asi ina lilt did I 1 uro tire ot of its il channel cha and d to a nova like a vicious substance aud ud alho he very forb ethic grinds la it up last J so A it again to its I 1 I 1 vo found the iho comil ive of tile 31 r lie aliett changed contenul COnti nUl A n tile lic ra to tile tho chapeau the brie banow v a nl I 1 lion source took on agran ft od I 1 arni 6 I 1 nakli kit the call us aud and al 15 it ivaa A don donawald award to it mate ill 1 and froze ib at wall VIM use I 1 I 1 into bauo I 1 I 1 ice I 1 1 Who whenever never tho the glacier gln cir loops ilou doum nard iq ian annit it in brokon up bv in ou civil the lateral crovi cro viLma foit aro at caused by the iho strain put iut upon rho too lo 10 ly by tuu the un equal movement inoc mont of the andea und the benter of tile gl alor arlor and allots it at a ight angles ft to tile alno no of greatest ten tell spin myo they curve upward tile cout cou edity being up tho during tile beat of bf alio llio ummer it is a costion courmon sin thing to see ice ono one or moro more brooks etAu along tho the star ir fare of the abo glacier into fissures they tile form of deep wells melts this water passes denva to tile bottom of tile a uric r ond iho rock ties been ground up lip by tho the friction tums between ilia ivand its ita bed issues at the lower ond and in A a 1 I turbid stream which being bolo drunk by the iho people produces pro ducoit the iho strong tendency lon doocy to I 1 iho lie boktor so 60 common co Dicion JQ in somo some of the a M 0 i are prod wool tile aluff of durt dirl and ud train be by LIMA triou tho the sides of the glacier these aro ro called moraines mo mor raines nines but two five glaciers glacier ustate to forni form a third os as la IQ tile LUBO come of tile mer do lacea lace 1 two twit lateral Mo moraines mora raines inca combine anti anil form forin a larro largo medial is ia all borno on together top olLor rim nn the iho glacier nd ad rances and is dropped oft off at ilia lower and a forming tile iho terminal roo raino irso these DIO a raines scattered over new angland bre aro st tho h 0 former glacial allion in iglo this s part of tho the country sometimes a large oat boulder bowlder falling lioa tile tho ico ica it bolting molting beneath anti and wo havo have the of 0 an aa lea ivo pillar |