Native metal

Some metals are found pure in nature.

They are not mixed with other things.

Gold is one of these metals.

You can find gold in rocks. You can even find it in river sand.

Silver and copper are also found this way.

Silver can look like tiny wires. Copper can be found in very large pieces.

Most metals change when they touch the air. But gold and platinum stay pure. This is because they do not react easily.

Finding these pure metals is very exciting!

Some metals are found in nature in a pure form. We call these native metals.

Most metals change when they touch the air or water. This is called oxidation. Gold and platinum do not change easily. This is why they are often found as pure metals.

Gold is often found in nuggets or wires. It can also be in fine grains in river sand. People use gold panning to find it. This method works because gold is very heavy.

Silver is also a native metal. It can look like tiny wires or crystals. It can even mix with gold to make electrum.

Copper is another common native metal.

It is stronger than gold. Ancient people used it to make tools and fishhooks. Some copper pieces weigh hundreds of tons. Most iron on Earth is not native. It comes from meteorites that fell from space. These meteorites are made of iron and nickel.

Other metals like aluminum and zinc are found in very small amounts.

Some metals are found in nature in a pure form. We call these native metals.

Most metals change when they touch air or water. This change is called oxidation. Very few metals can resist this weathering over a long time. Gold and platinum are less reactive, so they stay pure.

Other metals appear as small flakes. This happens when a natural process reduces a common ore. The metal is left behind as tiny bits. Some non-metals like carbon and sulfur also exist in this state.

Gold is a very common native metal.

It can appear as nuggets, wires, or veins in rock. You might also find fine grains in river sediments. People use gold panning to find these pieces. This works because gold has a great density. It is very heavy compared to the sand around it. Gold is often found mixed with silver to make electrum.

Silver is another important native metal.

It can look like irregular masses or long coatings. Sometimes silver forms beautiful crystals like cubes or octahedrons. It can also mix with mercury to form amalgams. One rare example is a mineral called eugenite. Silver is more reactive than gold. This means there are many more silver compound minerals in the world. Silver nuggets and wires are still relatively common to find.

Copper is a very useful native metal.

An ancient group called the Old Copper Complex lived near Lake Superior. They lived between 6000 and 3000 BC. They used native copper for tools and fishhooks. Copper is stronger than gold but still easy to shape. In Michigan, some copper masses weighed hundreds of tons. From 1845 to 1887, this area was a top producer. This helped people make many useful objects.

Most iron found on Earth is not actually native.

It mostly comes from iron-nickel meteorites from space. These fell to Earth after being kept safe in a vacuum. Truly native iron is very rare on our planet. One major deposit is near Disko Island in Greenland. Other metals like aluminum and zinc are also found. For example, tiny aluminum specks were found in Azerbaijan. Native molybdenum has even been found on the moon.

A native metal is any metal found in its pure, metallic form within nature. Most metals do not stay pure because they react with their environment. However, some elements can exist alone as single metals or as alloys. An alloy is a mixture of two or more metals.

This group includes many elements like iron, copper, and zinc. It also includes the gold and platinum groups. Understanding native metals helps us see how different elements resist or succumb to natural changes.

Most metals undergo a process called oxidation when they are exposed to the environment. Over geological time scales, natural weathering processes usually change metals into different compounds. Only a few metals are less reactive, meaning they do not change easily. Gold and platinum are primary examples of these stable metals. Other metals, such as nickel or chromium, appear in much smaller amounts. They often occur in isolated pockets. This happens when a natural chemical process reduces a common ore. This reduction leaves the pure metal behind as small flakes or tiny inclusions.

Gold is the most well-known native metal. It is the predominant gold mineral on Earth. Gold can be found as nuggets, wires, or veins within a rock matrix. It can also appear as fine grains mixed in river sediments. Because gold has a great density, it is very heavy. This allows people to use gold panning to separate gold from lighter sediments.

Gold is sometimes alloyed with silver to form electrum. While gold compounds are rare, gold can occasionally be found as selenides or tellurides.

Silver is another common native metal, though it is more reactive than gold. Silver can appear as irregular masses or elongated dendritic coatings. It also forms distinct crystals, such as cubes, octahedrons, or dodecahedrons.

Silver often occurs alongside silver sulfide or sulfosalt minerals. It can also form alloys with gold, known as electrum. In rare cases, silver and mercury form amalgams. One specific mineral example is eugenite, which is an Ag11Hg2 compound. Because silver reacts more easily, there are many more silver compound minerals than pure native silver.

Copper is a highly significant native metal for human history. An ancient North American civilization called the Old Copper Complex used it. They lived near Lake Superior between 6000 and 3000 BC. They mined native copper to make weapons, tools, and decorative objects.

Copper was more useful than gold because it is stronger. It was hard enough to make fishhooks and woodworking tools. Yet, it remained soft enough to be easily shaped. In the Michigan Copper Country, some native copper masses weighed hundreds of tons. This region was a leading U.S. producer from 1845 until 1887.

Iron is a metal that is rarely truly native to Earth. Most iron found on our planet actually comes from iron-nickel meteorites. These meteorites formed millions of years ago in the vacuum of space. The vacuum protected the metal from chemical attack. When they fell to Earth, they brought alloys like taenite and kamacite.

True telluric iron, which is born on Earth, is extremely rare. There is only one major deposit known near Disko Island in Greenland. Native nickel has also been found through hydrothermal alteration in places like New Caledonia.

Many other metals exist in the native state in very small quantities. For example, metallic cadmium has been found at only two locations, including the Vilyuy River basin in Siberia.

Native molybdenum has even been discovered in lunar regolith on the moon. Other elements like antimony, bismuth, and arsenic also occur this way. While metals are the most famous, non-metals can also be native. Carbon, sulfur, and selenium are examples of non-metallic elements found in this pure state. Even the semi-metal silicon has been found as tiny inclusions in gold.