▁which ▁is ▁between ▁N es cope ck ▁Mountain ▁and ▁Buck ▁Mountain . ▁N es cope ck ▁Creek ▁flows ▁through ▁this ▁valley . ▁The ▁valley ▁is ▁ ▁long ▁and ▁ ▁wide . ▁Some ▁streams ▁on ▁the ▁r idge ▁are ▁part ▁of ▁the ▁Le high ▁River ▁waters hed . ▁ ▁A ▁stream ▁known ▁as ▁Scot ch ▁Run ▁flows ▁through ▁a ▁valley ▁with ▁N es cope ck ▁Mountain ▁on ▁its ▁northern ▁edge . ▁ ▁N es cope ck ▁Mountain ▁forms ▁a ▁water ▁gap ▁with ▁C ata w issa ▁Mountain . ▁C ata w issa ▁Creek ▁cut s ▁through ▁this ▁water ▁gap . ▁There ▁is ▁also ▁a ▁water ▁gap ▁car ved ▁by ▁N es cope ck ▁Creek ▁through ▁N es cope ck ▁Mountain . ▁Both ▁of ▁these ▁water ▁g aps ▁are ▁relatively ▁narrow . ▁The ▁mountain ▁serves ▁as ▁part ▁of ▁the ▁div iding ▁line ▁between ▁the ▁Sus que h anna ▁River ▁and ▁the ▁Le high ▁River ▁waters h eds . ▁For ▁some ▁distance , ▁the ▁r idge ▁runs ▁parallel ▁to ▁the ▁Sus que h anna ▁River ▁at ▁a ▁distance ▁of ▁. ▁ ▁Ge ology ▁ ▁N es cope ck ▁Mountain ▁is ▁mainly ▁formed ▁by ▁hard , ▁u pt urn ed ▁con gl omer ates ▁belonging ▁to ▁the ▁Po cono ▁Form ation . ▁There ▁are ▁a ▁total ▁of ▁three ▁rock ▁form ations ▁on ▁N es cope ck ▁Mountain ▁in ▁the ▁Ber wick ▁Qu ad rangle , ▁which ▁is ▁in ▁Columbia ▁County ▁and ▁Lu zer ne ▁County . ▁From ▁north ▁to ▁south , ▁these ▁rock ▁form ations ▁are ▁the