arrow back

icon hinting to the presence of a table Synoptic Table of the Inner Solar System Planets, with Cut-Away Views

The Inner Solar System Planets, with Cut-Away Views
 General featuresDifferentiationAtmospherePrimary shaping processesErosion processes
Mercurysimilar to Moon, but higher density and mostly iron with few or no rocky crustyesnone (in fact an extremely thin one)heavy bombardment, lava floodsfurther 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
VenusEarth-sized, warm, high densityyes. A molten iron core; a rock mantleprimitive atmosphere was modified by a runaway greenhouse effect. Water was lostvolcanism, few cratersno plate tectonics
a crust of 16-25 miles (25-40 km), a core, a mantle
Earthonly known life-bearing planet in the solar systemyes. High density. Iron core, rock mantlewater evaporation and photosynthesis transformed primitive atmosphere (less carbon dioxide, oxygen). A moderate greenhouse effectheavy bombardment, volcanismplate tectonics, erosion
a crust of 3-19 miles (5-30 km), a mantle, a dual-core
Moonorigin in debate (impactor at Earth?). Low density, all rock, few ironyes. 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 interiorno primitive atmosphereheavy bombardment period, lava floodsfurther 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
Marsdifference between northern (volcanoes and plains) and southern (ancient surface, craters) hemispherenot entirely differentiated (melted core with solid rocks) as Mars features a liquid outer core of molten rock however. Medium densitya primitive atmosphere in lesser quantity than at Earth. Once water. A weak gravity rendered atmosphere thinnerheavy bombardment period, volcanismwater, wind
a crust, a mantle and a core

Website Manager: G. Guichard, site 'Amateur Astronomy,' http://stars5.6te.net. Page Editor: G. Guichard. last edited: 5/6/2019. contact us at ggwebsites@outlook.com
Free Web Hosting