A sample of galena (lead sulfide), the most important lead ore.


by Chris Woodford. Last updated: December 28, 2019.

As heavy as lead—it's probably something you say all the time and, if you've ever tried to lift a car battery, you'll know it's true. But have you ever stopped to think what makes this famously "heavy metal" weigh so much? Lead was one of the very first metals people discovered; in ancient times, the Romans used it for making elaborate networks of water pipes, and their word for lead—plumbum—gives us both our modern word for "plumbing" and the chemical symbol for lead (Pb). But this dull gray metal has an ambivalent history. Known to cause serious health problems, it's been slowly and systematically removed from everyday things such as gasoline and paint for a number of years; on the plus side, it's still just about the most effective substance for protecting us from radiation. More to lead than you thought? Let's take a closer look!

Photo: A sample of galena (lead sulfide), by far the most important lead ore. Photo by courtesy of US Geological Survey.

Where does lead come from?

Lead poisoning is a classic example of what happens when we take a material that was once buried deep underground and with which humans rarely had contact and introduce it widely into humans' ecology.

Gerald Markowitz and David Rosner, Lead Wars, 2014.

Lead is reasonably widespread (about the 36th most common element in Earth's rocky crust) but, like most other metals, hardly ever found in its pure form. Most of it comes from an ore (raw mineral) called galena (lead sulfide, PbS), though smaller amounts are present in other ores such as cerussite (lead carbonate, PbCO3, also called white lead ore) and anglesite (lead sulfate, PbSO4).

Black and white photo of disused lead mine.

Photo: The Old Wheatly lead mine, near Phoenixville. Chester County, Pennsylvania. Photo by Geological Society of America courtesy of US Geological Survey.

Galena is turned into pure lead metal through a multi-stage process. First it is crushed and washed to remove dirt and impurities. Then the lead is extracted either by smelting (heating in a furnace with coke) or in a two-stage process involving first roasting to convert lead sulfide into lead oxide, then smelting to remove the oxygen. Other precious metals are usually mixed in with the galena ore (including gold, silver, copper, and zinc) and are extracted during the process. Roughly half of all the lead now consumed is produced by recycling unwanted waste materials such as old car batteries.

Many countries mine lead, with leading producers including China (responsible for half of all mining), Australia, Peru, Mexico, and India. Although the United States once mined about a third of all the world's lead, by 2018 it was mining only around 7 percent. Most US mined lead comes from Alaska and Missouri, with the rest coming from Idaho and Washington. About 60 percent of lead used in the US is produced from "secondary" (recycled) sources.

Pie chart showing which countries mine most lead.

Chart: Who produces the world's lead? About half of it comes from China. Chart shows world mine production for 2018. Source: US Geological Survey, Mineral Commodity Summaries, February 2019.

What is lead like?

Lead is a soft, heavy, blueish gray metal that lives in group 14 (formerly IVa) of the Periodic Table of chemical elements.

Physical properties

On the face of it, when it comes to metallic properties, lead doesn't put up much of a showing. It's soft, weak, a poor conductor of electricity, heavy, dense, and has a low melting point. On the positive side, its softness means it's very malleable (easy to shape and work) and ductile (easy to pull into wires). Pure lead metal oxidizes rapidly in air to form a protective coating of lead oxide, and is resistant to corrosion by both acids (sulfuric and hydrochloric) and water.

Chemical properties

Gloss paint being applied to a door

Photo: Health and safety concerns mean lead is no longer so widely used in paints. Photo by Brian M. Brooks courtesy of US Navy.

Lead has a valency (combining power) of either +2 or +4, joining with a variety of other elements to make useful lead (II) and lead (IV) compounds, including oxides, sulfates, and carbonates. Industrially, the most important lead compound is a yellow powder called litharge (lead (II) oxide or lead monoxide), which is a vital ingredient in all kinds of glass, as well as oils and insecticides. Another useful oxide, trilead tetroxide (Pb3O4), makes up the familiar pigment "red lead"—once widely used in rust-resistant paints to protect iron structures such as the famous Forth railway bridge. Lead carbonate, (PbCO3)2·Pb(OH)2, is also a pigment (better known as "white lead"), used for at least 2000 years, while lead chromate ("chrome yellow") is used both by itself as a yellow pigment and to make various other lead-based pigments. Until the 1980s, one of the most important lead compounds was tetraethyl lead (lead with four C2H5 ethyl groups bonded to it, with the formula (CH3CH2)4Pb), an additive that improved performance in internal combustion engines. Following widespread concerns about air pollution and lead poisoning, most cars are now built to run on "unleaded" gasoline (petrol) that doesn't contain this substance. Other important lead compounds include lead (II) acetate or "sugar of lead" (used in making paints, varnishes, and dyes) and lead azide (an explosive used in such things as airbags).

What do we use lead for?

A typical car battery

Photo: Much of the world's lead finds its way into vehicle (car and truck) batteries. In the United States, some 85 percent of all lead ends up in batteries like this. Around 116 million batteries like this were shipped in the United States during the first ten months of 2018 alone (a slight increase on the year before). [Source: US Geological Survey, Mineral Commodity Summaries, February 2019.]

Consider lead's useful properties and you can more or less predict what people will use it for:

Key data: Lead

Periodic table thumbnail with the position of lead indicated.

Artwork: The periodic table of the chemical elements showing the position of lead (Pb). It's quite low down in the table because atoms of lead contain lots of protons and neutrons; that explains why lead is so dense and heavy.

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