Show n 1 t wasfi yas fi BALANCED ROCKS V ir r 1 i ciomo imiri I 1 tiomi tion vior or tin 1911 alic tio cil 11 racks jiru are riot not very cry awl are in i ile ncncy ill all les of nf these are of glacial gl iccil origin liln lull la ii i acen left in ill their ti ilir poil lii i V the awit tile lich broll bt them elzic iii sn di ditalia 1 aile othen have ak ani ii can cirill vil il out on oil llie I 1 lie hv the lution of tile fit InC lits ly by llie 1110 brosi 0 effect of baim blown by tin the dilill i lill this au a binl d atlist li lia alinAn ini ol alie i cirell cr il lock formations of Colo colorado rodo and 4 lie I 1 locky 8 ric ale title to tins tills call while tin tile boine boi ue boi s anro more cognion in ill new ung land und sections ions of nf the iho cattily north of the be ceilio I 1 1 1 x i tilt rs r S i the ini tile cut A 3 k croen lit kat w wc ills ill tit baudil I 1 i ill bic i nov hinijos aliis th i kopul it ir science news sri ans s that tit alie e m most ot striking sinking peculiarity of this and other oilier ba lancel l stones i alic fact that they rin can readily ile be ninde made to move or oscillate ly by the of it comparatively abak forc arcu f the bonc of dandil tandil for instance oin call 1 lie C me ed by 63 pushing it ill it a single fang finser ger lint but tle of gravit so low that small anion iiii tit of cau can bo be produced and it would not dot be possible to overturn it by uny iny ordinary menus imam the ciuc of the bahin cing of these rocks is 14 not cry it is dimply A case of natural due to die shape of tho the rock and tile force of gra citation |