The Earth is geoid THE EARTH IS SPHERICAL
the shape of the earth is not flat. it has a spherical shape. its slightly flattened at the poles to give a nearly spherical shape hence; the earth's shape is better described as a geoid which means the earth's shape
the first person to discover earth was round was god he made the earth in a spherical shape b00m theres ur answer
Because it has to do with science and its axis
they are both spherical in shape
the earth and the globe are both spherical[round shape]
The geoid is an equipotential surface that represents mean sea level around the Earth, taking into account the planet's gravitational field and rotation. It serves as a reference for measuring elevation and is used in creating precise global height models for applications like GPS systems and geodesy.
the shape of the earth is not flat. it has a spherical shape. its slightly flattened at the poles to give a nearly spherical shape hence; the earth's shape is better described as a geoid which means the earth's shape
The geoid has an equipotential surface where the force of gravity is perpendicular everywhere. But the earth has an irregular mass distribution and the resultant anomalies, makes the term geoid not a suitable reference.
The technical name for the shape of the Earth is geoid. This is studied in the science of geodesy.
an eclipse is a evidence of the earth being in spherical shape is that it can figure it self...
Spherical
Earth's shape is oblate spheroid.
the first person to discover earth was round was god he made the earth in a spherical shape b00m theres ur answer
the first person to discover earth was round was god he made the earth in a spherical shape b00m theres ur answer
"Roundish" is the clear winner so far as I know.(The actual shape of Earth is not a sphere; it's a "geoid", but saying "Earth is a geoid" is pretty much a tautology, since it amounts to saying "Earth is Earth-shaped.")
Spherical
Approximately spherical, but because of the speed of their rotation, there is certain 'oblateness' - a little flattening of the shape on the poles. The shape that results is often called a 'geoid'.