Earth molecule

OE50FeE49SiE49MgE49SE48AlE48NiE48CaE48CrE47NaE46KE46HE46TiE46FE45 CE45PE45MnE44SrE44BaE44ClE44VE44LiE44ZrE43RbE43ZnE44CuE43NE43BE43 CeE43CoE43ScE43NdE43GaE43BeE43LaE42NbE42PbE42PrE42SmE42ThE42 GdE42DyE42YE42GeE42ArE42ErE41CsE41UrE41HfE41YbE41SnE41EuE41TaE41 AsE41MoE41HoE41WE41TbE41BrE41TlE40LuE40TmE40HeE40SbE40IE40CdE40 InE40AgE40SeE40HgE39BiE39TeE39RuE38PdE38AuE38PtE38NeE38ReE38RhE37 OsE37KrE36IrE35XeE35RaE35PaE32AcE30AtE30PoE30RnE28TcE23PmE23FrE23

In science, earth molecule is the definition of the planet Earth from a chemical perspective, a view in which all motile structures are characterized as "molecules" defined by their atomic structure, formula, dynamics, and reactions with other like-sized structures. [1]

The approximate molecular formula for the earth was first calculated by American chemical engineer Libb Thims in circa 2005, as shown adjacent. [2] The "molecular" view of the earth shows, according to the mass composition of the 92 naturally-occurring elements in the structure of the earth, that the earth can be viewed as a type of reactive molecule, active in the solar system, attached to the sun via a type of yet undefined chemical-gravitation, composed primarily of the elements oxygen O, iron Fe, silicon Si, and magnesium Mg, among other elements in decreasing percentages.

See also
● Sun molecule
● Human molecule
● Bacterial molecule
● Walking molecule
● Molecular evolution table

References
1. Thims, Libb. (2008). The Human Molecule (ch. 8: Modern Views, section: “Planetary-sized molecules”, pgs. 57-59) (preview). Morrisville, NC: LuLu.
2. Thims, Libb. (2007). Human Chemistry (Volume One) (pgs. 20-21) (preview), (Google books). Morrisville, NC: LuLu.

External links
● Earth molecule – IoHT Glossary.