EGrisi Ime kwincam esemazantsi eBalkan Peninsula. Inommandla weekhilomitha ezili-131.957 zeekhilomitha, kwaye amanxweme ayo alinganisa malunga ne-15.000 km.
Ummandla wayo uquka iiyunithi ezintathu zejografi, ilizwekazi iGrisi, usingasiqithi we Peloponnesus, kunye neziqithi ezimele isihlanu somhlaba wonke. Unxweme lwamaGrike lunqumla ngasentshona kuLwandle i-Ionia nakwimpuma yi Mar I-Aegean, apho uninzi lweziqithi zaseGrisi zikhona. Iziqithi ezikwiAegean ezingezizo ezesiGrike yiImbros neTenedos. Inani leziqithi kwi EGrisi iyahluka ngokwenkcazo ekhethiweyo.
Kubalo luka-2001, iziqithi ezili-169 zazinabantu, kodwa isinye kwisithathu sazo sasinabemi abangaphantsi kwama-50. Ubungakanani bezi ziqithi ezinabantu zihlala ukusuka kwi-3 yeekhilomitha ukuya Ye, kwii-8.263, XNUMX zeekhilomitha zesikwere ze IKrete.
Akukho ndawo EGrisi Kukude elwandle, ePeloponnese nakumbindi weGrisi, ikwi-50 km kuphela kude. Ngapha koko, akukho zintaba eGrisi apho ulwandle lungenakubonwa khona.
EGrisi Ime kwintlanganiso yamacwecwe eteknoloji yaseAfrika kunye ne-Eurasia. Ngexesha le Mesozoic, yagutyungelwa lulwandle i-Tethys apho iMeditera yindawo yayo. Indlela phakathi kwamacwecwe yenza intshukumo yealpine apho iintaba zaseGrisi ziyinxalenye. Le ntshukumo ikhokelele ekuqhekekeni kwesitya se-Eurasia esenza ipleyiti yoLwandle iAegean.
Ikwadala iindawo ezinkulu ngokwenza intshona EGrisi Yenziwe nge-calcarium nakwimpuma ye-crystalline kunye ne-metamorphic massifs. Ukuhamba kwetectonic kuyaqhubeka kwaye ngenxa yesi sizathu kubakho iinyikima rhoqo. Isiqingatha seenyikima zonyaka ezenzeka kwi Europe kwenzeka eGrisi.
Ekuqaleni kwee-1830s, eyokuqala Lumente I-Greek ezimeleyo yexesha langoku izelwe, emva kwemfazwe yenkululeko ngokuchasene ne Imperio Ottoman.