▁is ▁a ▁branch , ▁the ▁Bow do in ▁F j ord , ▁and ▁on ▁the ▁southern ▁there ▁are ▁two , ▁the ▁Academy ▁Bay ▁in ▁the ▁inner ▁f j ord ▁with ▁the ▁Le id y ▁Gla cier ▁at ▁its ▁head ▁and ▁the ▁narrow ▁Ol rik ▁F j ord ▁running ▁roughly ▁from ▁east ▁to ▁west . ▁ ▁The ▁Heil pr in ▁Gla cier , ▁flow ing ▁from ▁the ▁Green land ▁Ice ▁She et ▁in ▁the ▁east , ▁is ▁the ▁largest ▁gla cier ▁that ▁has ▁its ▁termin us ▁in ▁the ▁f j ord . ▁The ▁T racy ▁Gla cier ▁has ▁its ▁termin us ▁further ▁north ▁near ▁Joseph ine ▁Pe ary ▁Island ▁in ▁a ▁bay ▁at ▁the ▁northern ▁side ▁of ▁the ▁head ▁of ▁the ▁f j ord ▁where ▁the ▁smaller ▁Hart ▁Gla cier , ▁Sh arp ▁Gla cier , ▁Mel ville ▁Gla cier , ▁and ▁Far qu har ▁Gla cier ▁have ▁their ▁termin us . ▁As ▁they ▁dis charge ▁into ▁the ▁f j ord ▁all ▁these ▁gla ci ers ▁are ▁separated ▁by ▁nun ata ks , ▁the ▁largest ▁of ▁which ▁is ▁the ▁Smith son ▁Range . ▁In ▁the ▁central ▁area ▁of ▁the ▁f j ord ▁the ▁Hub b ard ▁Gla cier ▁dis charg es ▁on ▁the ▁northern ▁shore ▁and ▁the ▁H url but ▁Gla cier ▁on ▁the ▁southern ▁shore . ▁ ▁The ▁islands ▁of ▁Q eq ert ars ua q ▁( Her bert ▁Island ) ▁and ▁Ki ata k ▁( N orth umber land ▁Island ) ▁lie ▁off ▁the ▁f j ord ' s ▁mouth . ▁They