▁which ▁the ▁Earth ' s ▁land mass es ▁and ▁bodies ▁of ▁water ▁are ▁sw apped , ▁with ▁land mass es ▁becoming ▁bodies ▁of ▁water ▁and ▁bodies ▁of ▁water ▁becoming ▁land mass es . ▁ ▁Top ography ▁and ▁climate ▁ ▁The ▁current ▁Earth ▁compr ises ▁ 2 9 % ▁land ▁and ▁ 7 1 % ▁water , ▁while ▁In vert ed ▁Earth ▁compr ises ▁ 7 1 % ▁land ▁and ▁ 2 9 % ▁water . ▁In vert ed ▁Earth ▁contains ▁one ▁large ▁land mass , ▁allowing ▁people ▁to ▁travel ▁to ▁any ▁" o cean " ▁on ▁foot . ▁ ▁When ▁in ver ting ▁the ▁Earth , ▁la kes ▁become ▁islands , ▁while ▁rivers ▁become ▁long , ▁narrow ▁stri ps ▁of ▁land . ▁The ▁mountains ▁on ▁the ▁real ▁Earth ▁would ▁be ▁under water ▁tren ches ▁on ▁In vert ed ▁Earth ▁and ▁vice ▁vers a . ▁One ▁of ▁the ▁prominent ▁ge ological ▁features ▁on ▁In vert ed ▁Earth ▁would ▁be ▁the ▁Marian as ▁mountain ▁range , ▁which ▁would ▁have ▁the ▁highest ▁peak ▁(" Ch allen ger ▁Pe ak " ▁or ▁" Mount ▁Ch allen ger ") ▁on ▁Earth , ▁even ▁higher ▁than ▁Mount ▁Ever est . ▁Like wise , ▁the ▁deep est ▁point ▁on ▁In vert ed ▁Earth ▁would ▁be ▁Ever est ▁Deep ▁in ▁the ▁H imal ay as ▁T rench . ▁ ▁The ▁climate ▁on ▁In vert ed ▁Earth ▁would ▁be ▁much ▁different ▁than ▁on ▁the ▁real ▁Earth . ▁Since ▁its ▁bodies ▁of ▁water ▁would ▁cover ▁much ▁less ▁area , ▁combined ▁with ▁trem end