IPA: /ˈdʒiːɔɪd/
KK: /ˈdʒiːɔɪd/
A theoretical shape of the Earth that represents the average sea level across the globe, extending under land areas as well.
Scientists use the geoid to understand sea level changes and the Earth's gravitational field.
Geoid is formed from "geo-" (from Greek "gē", meaning earth) and "-oid" (from Greek "eidos", meaning form or shape). The term geoid refers to the shape of the Earth as determined by its gravitational field, resembling an equipotential surface of the Earth's gravity.
Think of 'geo-' meaning earth and '-oid' meaning shape — the geoid is the shape of the Earth.