▁stands ▁between ▁it ▁and ▁L ing ▁F ell . ▁Jo ining ▁the ▁Dub w ath ▁Beck ▁it ▁then ▁flows ▁east ward ▁along ▁the ▁V ale ▁of ▁Em ble ton ▁and ▁into ▁the ▁northern ▁end ▁of ▁Bass enth wa ite . ▁Beck ▁W yth op ▁by ▁contrast ▁cut s ▁through ▁the ▁r idge ▁of ▁high ▁ground ▁running ▁alongside ▁Bass enth wa ite , ▁and ▁dro ps ▁directly ▁into ▁the ▁lake . ▁ ▁S ale ▁F ell ▁itself ▁is ▁an ▁east - west ▁r idge ▁about ▁a ▁mile ▁long , ▁cl ad ▁primarily ▁in ▁fell ▁grass ▁and ▁bra cken ▁The ▁eastern ▁end ▁is ▁heavily ▁for ested ▁as ▁part ▁of ▁W yth op ▁Wood . ▁These ▁are ▁mostly ▁con if ers , ▁although ▁the ▁mix ▁of ▁trees ▁is ▁gradually ▁changing . ▁There ▁are ▁Forest ry ▁Commission ▁offices ▁hidden ▁in ▁the ▁trees ▁at ▁the ▁base ▁of ▁the ▁fell . ▁The ▁sum mit ▁of ▁the ▁fell ▁is ▁toward ▁the ▁west ▁of ▁the ▁r idge ▁and ▁there ▁are ▁two ▁other ▁to ps ▁to ▁the ▁east . ▁Riv ings ▁( 1 , 0 9 9   ft ) ▁and ▁L oth wa ite ▁( 1 , 1 3 2   ft ) ▁are ▁included ▁in ▁some ▁guide books ▁ ▁Ge ology ▁The ▁fell ▁is ▁pre domin antly ▁composed ▁of ▁Ord ov ician ▁rocks ▁of ▁the ▁Low es water ▁Form ation . ▁This ▁consists ▁of ▁gre yw ack e ▁sand stone ▁tur bid ities . ▁The ▁southern ▁fl anks ▁are ▁of ▁the ▁l amin ated ▁mud stone ▁and ▁s ilt stone