He speculates that the presence of
our relatively large moon has stabilized the spin of the earth over billions of years, and this has made possible the evolution of life on the earth.
Not exact matches
The
large tan splotch just below and to the right of the South Pole is the two - hundred - mile - wide Schrodinger crater, one of the few areas on the
moon that shows signs of
relatively recent volcanic activity.
Although our own
moon is enticingly close, its gravity means that
relatively large rockets are needed to get astronauts to and from the surface.
The consensus is that several factors are important: atmospheric composition (the concentrations of carbon dioxide, methane); changes in the Earth's orbit around the Sun known as Milankovitch cycles (and possibly the Sun's orbit around the galaxy); the motion of tectonic plates resulting in changes in the relative location and amount of continental and oceanic crust on the Earth's surface, which could affect wind and ocean currents; variations in solar output; the orbital dynamics of the Earth -
Moon system; and the impact of
relatively large meteorites, and volcanism including eruptions of supervolcanoes.
Sophisticated computer modeling indicates Mars» two small
moons likely formed as the result of a
relatively modest - size impactor, not a much
larger body as previously theorized.
As a result, Vesta «differentiated» into a
relatively dense metallic core (of approximately 136 miles or 220 kilometers across), lighter mantle, and crust, like the rocky inner planets, many
large planetary satellite's like the Earth's
Moon, and probably most, if not all, of the newly named «dwarf planets» like Ceres.
For a
moon, Titan has a
relatively large diameter of about 5,100 km (or 3,200 miles).
I am not happy with the JEV theory (although I can't really judge), because even tidal effects on Earth caused by a
relatively large and close
Moon only have small, superficial effects.