Monday, January 28, 2008
Earth
Sunday, January 20, 2008
Venus and Earth
* Venus is only a bit of smaller than Earth (95% of Earth's diameter, 80% of Earth's mass).
* Both have a small number of craters representing relatively young surfaces.
* Their densities and chemical compositions are in a similar way.
Because of these similarities, it was measured that below its dense clouds Venus might be very earthlike and power even have life. However, unfortunately, more detailed study of Venus reveals that in plenty of important ways it is radically different from Earth. It may be the smallest amount hospitable place for life in the solar system.
The strength of Venus' atmosphere at the surface is 90 atmospheres (about the same as the pressure at a deepness of 1 km in Earth's oceans). It is collected generally of carbon dioxide. There are numerous layers of clouds many kilometers bulky composed of sulfuric acid. These clouds entirely incomprehensible our view of the surface. This thick atmosphere creates a run-away greenhouse effect that raises Venus' face temperature by about 400 degrees to over 740 K (hot enough to melt lead). Venus' surface is truly hotter than Mercury's in spite of creature nearly twice as far from the Sun. The oldest terrains on Venus appear to be regarding 800 million years old. Extensive volcanism at that time wiped out the in move ahead surface counting any large craters from early in Venus' history.
Monday, January 7, 2008
The facts about Venus
Venus' rotary motion is rather unusual in that it is both very slow (243 Earth days per Venus day, somewhat longer than Venus' year) and retrograde. Moreover, the periods of Venus' rotary movement and of its orbit are synchronized such that it for all time presents the same face in the direction of Earth when the two planets are at their neighboring approach.
Tuesday, January 1, 2008
Mercury's dense iron core
Mercury's inner is under enemy control by a big iron core whose radius is 1800 to 1900 km. The silicate on the outside shell (analogous to Earth's mantle and crust) is just 500 to 600 km thick. At least several of the core is perhaps molten. Mercury truly has an enormously thin atmosphere consisting of atoms blasted off its surface by the solar wind. Because Mercury is so hot, these atoms speedily flee into space.