The figure on the right compares Venus and Earth spacecraft images. The surface of Venus is shown in orange as
radar images while the atmosphere is reproduced on near true colors as it would be seen by the human eye.
The upper clouds are brightest in the blue and ultraviolet wavelengths making Venus a white-blue colour planet.
Both planets have almost the same size and density and Venus is only a 30% closer to the Sun than Earth. Both
share an interesting geological evolution with old volcanoes in Venus and some of them could still be active.
One of the biggest misteries of Venus is why its surface is so young
on geological time-scales. It is interesting to remark that there is almost no water on Venus' atmosphere.
The figure on the right illustrates the basics of the greenhouse effect on Venus.
Long-wave radiation from the Sun is mainly reflected
at the upper cloud deck and partially absorbed by the atmosphere but part of it reaches the surface and heats the lowest atmosphere.
The hot surface cools down emitting short-wave radiation that is absorbed and re-emitted by the green-house gases of the atmosphere
impeding cooling of the planet and originating the high temperatures at the surface. Figure extracted from
here.