Synoptic Table of the Inner Solar System Planets, with Cut-Away Views
General features | Differentiation | Atmosphere | Primary shaping processes | Erosion processes | |
---|---|---|---|---|---|
Mercury | similar to Moon, but higher density and mostly iron with few or no rocky crust | yes | none (in fact an extremely thin one) | heavy bombardment, lava floods | further smaller impacts produced a regolith layer |
a large core, about 75 percent the planet size, and a crust of about 62 miles (100 km) thick. Mercury's inner core was proved indeed solid. The solid, iron core is about 1,260 miles (about 2,000 kilometers) wide and makes up about half of Mercury's entire core (about 2,440 miles, or nearly 4,000 kilometers, wide). Hints of some molten area in Mercury's interior had been observed from Earth, through small shifts in the spin of Mercury, called librations | |||||
Venus | Earth-sized, warm, high density | yes. A molten iron core; a rock mantle | primitive atmosphere was modified by a runaway greenhouse effect. Water was lost | volcanism, few craters | no plate tectonics |
a crust of 16-25 miles (25-40 km), a core, a mantle | |||||
Earth | only known life-bearing planet in the solar system | yes. High density. Iron core, rock mantle | water evaporation and photosynthesis transformed primitive atmosphere (less carbon dioxide, oxygen). A moderate greenhouse effect | heavy bombardment, volcanism | plate tectonics, erosion |
a crust of 3-19 miles (5-30 km), a mantle, a dual-core | |||||
Moon | origin in debate (impactor at Earth?). Low density, all rock, few iron | yes. No molten core. It is unknown whether the Moon has a fully differentiated and melted structure with a metallic core or retains a partially primordial, unmelted interior | no primitive atmosphere | heavy bombardment period, lava floods | further bombardment produced a regolith layer |
a crust, mantle and core. note: recentest findings hint to a solid, iron-rich inner core with a radius of nearly 150 miles and a fluid, primarily liquid-iron outer core with a radius of roughly 205 miles as a partially molten boundary layer around the core estimated to have a radius of nearly 300 miles is then conceding to Moon's thick mantle | |||||
Mars | difference between northern (volcanoes and plains) and southern (ancient surface, craters) hemisphere | not entirely differentiated (melted core with solid rocks) as Mars features a liquid outer core of molten rock however. Medium density | a primitive atmosphere in lesser quantity than at Earth. Once water. A weak gravity rendered atmosphere thinner | heavy bombardment period, volcanism | water, wind |
a crust, a mantle and a core |