The Martian atmosphere consists of approximately 96% carbon dioxide, 1.9% argon, 1.9% nitrogen, and traces of free oxygen, carbon monoxide, water and methane.
The strength of chemical bonds varies considerably; there are "strong bonds" such as covalent or ionic bonds and "weak bonds" such as Dipole-dipole interaction, the London dispersion force and hydrogen bonding.
The most abundant elements in the Earth's crust are oxygen (46.6%) and silicon (27.7%). Minerals which combine these two elements are called silicates.
The Earth's inner core is believed to be primarily a solid ball with a radius of about 1220 kilometers. It is composed of an iron-nickel alloy and some light elements.
Fossil fuels are hydrocarbons, primarily coal, fuel oil or natural gas, formed from the remains of dead plants and animals. Solar power is obtained by harnessing the energy of the sun's rays.
Igneous rock is formed through the cooling and solidification of magma or lava.
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