The Inner Planets

The Inner Planets — page 5
The Inner PlaneTs produced by infrequent later impacts Volcanic activity has been an important force in the shaping of the surfaces of the Moon and the terrestrial planets We can learn a lot about Earth from our inner-planet neighbors Mercury is too hot to retain an atmosphere but Venus’s brilliant white appearance is the result of it being completely enveloped in thick clouds of carbon dioxide impenetrable at visible wavelengths Below the upper clouds Venus has a hostile atmosphere containing clouds of sulfuric acid droplets The cloud cover shields the planet’s planet’s surface from direct sunlight but the energy that does filter through warms the surface which then radiates at infrared wavelengths The long-wavelength infrared radiation radiation is trapped by the dense clouds such that an efficient greenhouse effect keeps the surface temperature near 465 C 870 F 740 K Radar which can penetrate the thick Venusian clouds has been used to map the planet’s surface In contrast the atmosphere of Mars is very thin and is composed mostly of carbon dioxide 95 percent with very little water vapour the planet’s surface pressure is only about 0 006 that of Earth The outer planets have atmospheres atmospheres composed largely of light gases mainly hydrogen and helium The inner planets are similar to Earth in many ways and in other ways very different This gives scientists great opportunities to study the nature and origin of Earth 8