Abundances

We all know that some chemical elements like iron are more abundant than others like gold.
Here you can find more information.

Abundances in Earth's crust
Cosmic Abundances

The Chemical Elements

Here you can find information on all the known chemical elements.
Information on different isotopes of chemical elements can be found here .

Periodic table of the chemical elements

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The Periodic Table Songs

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http://www.youtube.com/watch?v=zUDDiWtFtEM
and a slower version:
http://www.youtube.com/watch?v=-I7l8TgtuLQ

Elements listed by name and by atomic number

Name Symbol number Name Symbol number
Actinium Ac 89 Hydrogen H 1
Aluminum Al 13 Helium He 2
Americium Am 95 Lithium Li 3
Antimony Sb 51 Beryllium Be 4
Argon Ar 18 Boron B 5
Arsenic As 33 Carbon C 6
Astatine At 85 Nitrogen N 7
Barium Ba 56 Oxygen O 8
Berkelium Bk 97 Fluorine F 9
Beryllium Be 4 Neon Ne 10
Bismuth Bi 83 Sodium Na 11
Boron B 5 Magnesium Mg 12
Bromine Br 35 Aluminum Al 13
Cadmium Cd 48 Silicon Si 14
Calcium Ca 20 Phosphorus P 15
Californium Cf 98 Sulfur S 16
Carbon C 6 Chlorine Cl 17
Cerium Ce 58 Argon Ar 18
Cesium Cs 55 Potassium K 19
Chlorine Cl 17 Calcium Ca 20
Chromium Cr 24 Scandium Sc 21
Cobalt Co 27 Titanium Ti 22
Copper (Cuprum) Cu 29 Vanadium V 23
Curium Cm 96 Chromium Cr 24
Dysprosium Dy 66 Manganese Mn 25
Einsteinium Es 99 Iron (Ferrum) Fe 26
Erbium Er 68 Cobalt Co 27
Europium Eu 63 Nickel Ni 28
Fermium Fm 100 Copper (Cuprum) Cu 29
Fluorine F 9 Zinc Zn 30
Francium Fr 87 Gallium Ga 31
Gadolinium Gd 64 Germanium Ge 32
Gallium Ga 31 Arsenic As 33
Germanium Ge 32 Selenium Se 34
Gold (Aurum) Au 79 Bromine Br 35
Hafnium Hf 72 Krypton Kr 36
Helium He 2 Rubidium Rb 37
Holmium Ho 67 Strontium Sr 38
Hydrogen H 1 Yttrium Y 39
Indium In 49 Zirconium Zr 40
lodine I 53 Niobium Nb 41
Iridium Ir 77 Molybdenum Mo 42
Iron (Ferrum) Fe 26 Technetium Tc 43
Krypton Kr 36 Ruthenium Ru 44
Lanthanum La 57 Rhodium Rh 45
Lead (Plumbum) Pb 82 Palladium Pd 46
Lithium Li 3 Silver (Argentum) Ag 47
Lutetium Lu 71 Cadmium Cd 48
Magnesium Mg 12 Indium In 49
Manganese Mn 25 Tin (Stannum) Sn 50
Mendelevium Md 101 Antimony Sb 51
Mercury Hg 80 Tellurium Te 52
Molybdenum Mo 42 lodine I 53
Neodymium Nd 60 Xenon Xe 54
Neon Ne 10 Cesium Cs 55
Neptunium Np 93 Barium Ba 56
Nickel Ni 28 Lanthanum La 57
Niobium Nb 41 Cerium Ce 58
Nitrogen N 7 Praseodymium Pr 59
Nobelium No 102 Neodymium Nd 60
Osmium Os 76 Promethium Pm 61
Oxygen O 8 Samarium Sm 62
Palladium Pd 46 Europium Eu 63
Phosphorus P 15 Gadolinium Gd 64
Platinum Pt 78 Terbium Tb 65
Plutonium Pu 94 Dysprosium Dy 66
Polonium Po 84 Holmium Ho 67
Potassium K 19 Erbium Er 68
Praseodymium Pr 59 Thulium Tm 69
Promethium Pm 61 Ytterbium Yb 70
Protactinium Pa 91 Lutetium Lu 71
Radium Ra 88 Hafnium Hf 72
Radon Rn 86 Tantalum Ta 73
Rhenium Re 75 Tungsten (Wolfram) W 74
Rhodium Rh 45 Rhenium Re 75
Rubidium Rb 37 Osmium Os 76
Ruthenium Ru 44 Iridium Ir 77
Samarium Sm 62 Platinum Pt 78
Scandium Sc 21 Gold (Aurum) Au 79
Selenium Se 34 Mercury Hg 80
Silicon Si 14 Thallium Tl 81
Silver (Argentum) Ag 47 Lead (Plumbum) Pb 82
Sodium Na 11 Bismuth Bi 83
Strontium Sr 38 Polonium Po 84
Sulfur S 16 Astatine At 85
Tantalum Ta 73 Radon Rn 86
Technetium Tc 43 Francium Fr 87
Tellurium Te 52 Radium Ra 88
Terbium Tb 65 Actinium Ac 89
Thallium Tl 81 Thorium Th 90
Thorium Th 90 Protactinium Pa 91
Thulium Tm 69 Uranium U 92
Tin (Stannum) Sn 50 Neptunium Np 93
Titanium Ti 22 Plutonium Pu 94
Tungsten (Wolfram) W 74 Americium Am 95
Uranium U 92 Curium Cm 96
Vanadium V 23 Berkelium Bk 97
Xenon Xe 54 Californium Cf 98
Ytterbium Yb 70 Einsteinium Es 99
Yttrium Y 39 Fermium Fm 100
Zinc Zn 30 Mendelevium Md 101
Zirconium Zr 40 Nobelium No 102
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Abundances in Earth's crust

Abundance (atom fraction) of the chemical elements in Earth's upper continental crust as a function of atomic number. The rarest elements in the crust (shown in yellow) are the most dense. They were further rarefied in the crust by being siderophile (iron-loving) elements, in the Goldschmidt classification of elements.
Siderophiles were depleted by being relocated into the Earth's core. Their abundance in meteoroid materials is relatively higher. Additionally, tellurium and selenium have been depleted from the crust due to formation of volatile hydrides.

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Cosmic Abundances

From the human perspective only the abundances of the chemical elements in the Earth's crust and atmosphere is relevant, but it is not typical for the Earth as a whole or for the Solar system.

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Moreover the cosmic abundances evolved during the history of the universe by nuclear reactions mainly in the cores of heavy stars and during supernova explosions.

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Read the complete article by H. Schatz in Physics Today here (PDF) .

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