🧪 Interactive Periodic Table of Elements

A periodic table explorer: search any element by name, symbol or atomic number for its atomic weight, group, period and electron configuration.

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6
C
Carbon
12.011
Category
Reactive nonmetal
Group / period
14 / 2
Block
p-block
Phase at room temp
Solid
Electron configuration
[He] 2s2 2p2
Shell occupancy
2, 4
Electronegativity
2.55 (Pauling)
First ionization energy
1086.5 kJ/mol
Melting point
Not known
Boiling point
Not known
Density
1.821 g/cm³
Discovered by
Ancient Egypt

All 118 confirmed elements. Atomic masses are the IUPAC standard atomic weights — for elements with no stable isotope, the value is the mass number of the most stable known isotope, which is why it is shown as a whole number. Blank fields are genuine gaps in the measured data rather than zeroes.

What Interactive Periodic Table of Elements Does

The periodic table is ordered by atomic number — the number of protons in the nucleus — and arranged so that elements with similar chemistry fall into the same column. That arrangement was worked out before anyone knew what an electron was, and it holds up because a column shares the same outer-shell electron count, which is what determines how an element reacts.

All 118 confirmed elements are here, with atomic mass, electron configuration, phase, melting and boiling points, density, electronegativity and first ionization energy. Masses are the IUPAC standard atomic weights, which are averages across the isotopes found in nature — that is why chlorine is 35.45 rather than a whole number, and why it is a range rather than a constant for some elements.

For elements with no stable isotope, there is no natural mixture to average, so the convention is to quote the mass number of the most stable known isotope. That is why the bottom of the table reads in whole numbers.

The last stretch of the table is largely predicted rather than measured. Elements past about 104 have been made a few atoms at a time with half-lives in milliseconds, so most of their properties come from extrapolating periodic trends. Where a value is genuinely unknown, this says so rather than showing a zero.

How to Use Interactive Periodic Table of Elements

  1. Type an element name or symbol in the search input
  2. Click any element box in the grid to spotlight its properties
  3. Review atomic mass, orbital electron configuration, and chemical family

Formula Used by Interactive Periodic Table of Elements

How the table is organized

period = the outermost occupied shell · group = the outer-shell electron count · block = the subshell being filled (s, p, d, f)

atomic number Z
protons in the nucleus — this defines the element, and the ordering
standard atomic weight
the isotope-abundance-weighted average mass, in unified atomic mass units
electron configuration
written from the previous noble gas, so iron is [Ar] 3d⁶ 4s²

Worked example

Chlorine, atomic number 17.

  1. Period 3, group 17 — seven outer electrons, one short of a full shell
  2. Configuration [Ne] 3s² 3p⁵
  3. Mass 35.45, because natural chlorine is roughly 76% chlorine-35 and 24% chlorine-37

Result: One electron short of stability, which is why the halogens are so reactive and why chlorine forms a −1 ion.

The categories, and what they share

CategoryWhereBehavior
Alkali metalsGroup 1One outer electron, given up eagerly — soft, and violently reactive with water
Alkaline earth metalsGroup 2Two outer electrons; reactive, though less so
Transition metalsGroups 3–12Filling a d subshell; multiple oxidation states, colored compounds
Post-transition metalsRight of the transition blockSofter, lower melting points than transition metals
MetalloidsThe staircaseIntermediate — the basis of semiconductors
Reactive nonmetalsUpper rightGain or share electrons; the elements of organic chemistry
HalogensGroup 17One electron short of a full shell, so highly reactive
Noble gasesGroup 18Full outer shell, so almost entirely unreactive
LanthanidesRow below, 57–71Filling 4f; chemically very similar to each other
ActinidesRow below, 89–103Filling 5f; all radioactive

Trends worth knowing

These are why the shape of the table is useful rather than decorative.

PropertyAcross a periodDown a group
Atomic radiusDecreases — more protons pull the same shell inIncreases — another shell is added
Ionization energyIncreasesDecreases
ElectronegativityIncreasesDecreases
Metallic characterDecreasesIncreases

How to Read Your Result

The column tells you the chemistry

Elements in a group share their outer-shell electron count, which is what reacts. Sodium and potassium behave alike because both have one outer electron to lose; fluorine and chlorine behave alike because both are one short of a full shell.

Atomic mass is an average, not a count

Standard atomic weights average over the isotopes found on Earth, weighted by abundance. That is why they are rarely whole numbers, and why IUPAC now publishes intervals rather than single values for a dozen elements whose isotopic composition varies measurably by source.

Missing values are honest gaps

Several superheavy elements have been produced only in single-atom quantities with half-lives too short to measure a melting point. Where a property has never been measured, it is shown as unknown rather than filled in with a prediction.

The f-block is drawn below to save width

The lanthanides and actinides belong between groups 3 and 4. Inserting them inline would make the table 32 columns wide, so convention pulls them out — they are part of periods 6 and 7, not a separate appendix.

Limitations & Accuracy Notes

  • Atomic weights are the abridged IUPAC standard values. For elements whose isotopic composition varies by source, IUPAC publishes an interval and this shows a representative value.
  • Melting points, boiling points and densities are measured at standard pressure and vary with allotrope — carbon as graphite and as diamond differ substantially.
  • Electronegativity is on the Pauling scale, which is not defined for the noble gases and several synthetic elements.
  • Properties for elements above roughly 104 are largely predicted rather than measured.
  • Isotopes, half-lives and decay chains are outside the scope of this table.

Frequently Asked Questions

What information is provided for each chemical element?
Each element card displays the atomic number, chemical symbol, standard atomic weight, chemical classification category, periodic table period/group, and electron configuration.
How do I search for a specific element?
Type any element name (e.g. Gold), atomic symbol (e.g. Fe), or atomic number (e.g. 79) into the instant search box.
How many elements are there?
118 are confirmed and named, running from hydrogen to oganesson. Everything beyond uranium at number 92 is synthetic, and the heaviest have been produced only in tiny quantities with half-lives measured in milliseconds.
Why is atomic mass not a whole number?
Because it is a weighted average across the naturally occurring isotopes of that element. Chlorine sits near 35.45 because it is a mixture of chlorine-35 and chlorine-37 in roughly a three-to-one ratio, not because any single atom has that mass.
What does the group and period tell me?
The period is the row and corresponds to the outermost occupied electron shell. The group is the column and elements within one share an outer electron configuration, which is why they behave similarly — the whole table is organized around that.
What is an electron configuration notation?
A shorthand for which orbitals the electrons occupy, such as 1s2 2s2 2p6. It explains chemical behavior better than any other single property, because bonding is almost entirely about the outermost electrons.
Can I cite this for coursework?
The page states the source of its atomic data. For formal work, cite that primary source rather than this page.
Is anything sent to a server?
No. The element data is bundled with the page.

References & Further Reading

By OnlineToolHubs Team • September 2026