Early Earth's temperature is estimated to have been extremely high, exceeding 2000 degrees Celsius due to intense volcanic activity and impacts from asteroids and meteorites. Over time, as the planet cooled down and the atmosphere evolved, temperatures gradually decreased to levels that allowed for the formation of oceans and early life.
the temperature for early today is 87 degrees.
The temperature scale used to measure Earth's heat is called the Celsius scale.
Oxygen was the important element missing in Earth's early atmosphere. It was only produced later by photosynthetic organisms.
The average surface temperature of the Earth is approximately 288 Kelvin (K), which is equivalent to about 15 degrees Celsius or 59 degrees Fahrenheit.
The average temperature at sea level on Earth is around 15 degrees Celsius or 59 degrees Fahrenheit.
it depends on the deepth
it is 65
oxygen
29
Heats it up
1000
Mars
radioactive decay
temperature increases with depth
it depends on the deepth
it depends on the deepth
The earths crust varies. There is no temperature because it varies from cold to hot.