Campo del Cielo

Long ago, rocks fell from the sky.

These rocks hit the ground in Argentina. They made many big holes in the land.

People call this place the Field of Heaven. The rocks are made of heavy metal. They broke into many pieces.

One big piece is called Gancedo. It is very heavy.

People found many pieces there.

This is the most metal found in one spot. It is a very special place.

The rocks are very old.

In Argentina, there is a place called Campo del Cielo. This name means "Field of Heaven."

This place has many craters. A crater is a large hole in the ground. There are at least 26 craters there. These holes were made by rocks from space. We call these rocks meteorites.

Scientists think these rocks fell 4,200 to 4,700 years ago. The rocks themselves are very old. They are about 4.5 billion years old.

A large object likely entered our air. It broke into many pieces. These pieces fell to the ground. This left behind many iron fragments. Most of these pieces are made of iron and nickel. People have found 100 tonnes of these pieces. This is the most metal found in one spot. One huge piece is named Gancedo. It was found in 2016. It weighs 30.8 tonnes.

Other big pieces include El Chaco. El Chaco weighs 28.8 tonnes. These pieces are very special to study.

In Argentina, there is a special place called Campo del Cielo. This name means "Field of Heaven" in English.

It is a large area near the provinces of Chaco and Santiago del Estero. This place contains at least 26 craters in the ground. The largest crater is 300 meters wide. These craters were made by rocks from space. Scientists think the impact happened 4,200 to 4,700 years ago. These space rocks are called meteorites.

The meteorites themselves are very old. They are about 4.5 billion years old.

How did these many pieces get there? A huge object likely entered the Earth's atmosphere. It broke into many pieces while it fell. These pieces then landed across a large area. This created a strewn field of smaller meteorites. The main body was likely larger than 10 meters wide. The fragments are mostly made of iron and nickel. They also contain small amounts of other things like cobalt and germanium.

The metal is very pure. This is why so many pieces were found.

People have known about these rocks for a long time. Aboriginal peoples knew about them long before others did. In 1576, a Spanish governor sent soldiers to find the metal. They heard native people used it for weapons. Later, in 1774, Don Bartolomé Francisco de Maguna found a mass. He called it "the Table of Iron." In 1783, Rubin de Celis led another expedition. He used explosives to clear the ground. He thought the metal came from a volcano. He sent samples to the Royal Society in London. Scientists there found the metal was actually from space.

Many huge pieces have been found over the years. In 1803, people found a mass called Otumpa. It weighed about 1 tonne. In 1969, a metal detector found El Chaco below the ground. It was taken out in 1980. It weighed 28.8 tonnes. In 2016, the largest piece was found. It is named Gancedo after a nearby town. Gancedo weighs 30.8 tonnes.

Altogether, people have found 100 tonnes of fragments. This is the most meteorite metal found in one spot on Earth.

These heavy rocks are very important to study. They help us learn about the Solar System. The metal pieces are part of how our world began. Some pieces are very small. They can weigh only a few milligrams. Other pieces are huge like the Gancedo meteorite. These large rocks are now protected by law. This helps keep them safe from people who might try to steal them. Finding them is like finding a piece of history from the sky.

Campo del Cielo is a famous site located in Argentina. The name means "Field of Heaven" or "Field of the Sky" in English.

This area straddles the provinces of Chaco and Santiago del Estero. It contains at least 26 impact craters. The largest of these craters is 300 meters wide. This site is significant because it holds the largest collection of meteorite fragments ever found. In total, researchers have recovered approximately 100 tonnes of material. This makes it the heaviest set of meteorite finds on Earth.

The craters were created by a massive cosmic event. Scientists believe a large body entered the Earth's atmosphere. This object was likely larger than 10 meters in diameter. As it fell, it broke into many different pieces. These pieces landed across a wide area called a strewn field. This field includes an additional 10 kilometers of smaller meteorites. This process explains why there are so many fragments scattered around the main craters. At least two of the craters contain thousands of small iron pieces.

The meteorites themselves are incredibly old. They are estimated to be 4.5 billion years old. This means they formed during the development of our Solar System. We know when they landed on Earth by studying charred wood found beneath the fragments. Using carbon-14 analysis, scientists determined the impact happened between 4,200 and 4,700 years ago.

This places the event roughly between 2,200 and 2,700 BC. The metal in these rocks is mostly iron and nickel. The average composition is 92.6% iron and 6.67% nickel. They also contain small amounts of gallium, germanium, phosphorus, and cobalt. The fragments have a high density of inclusions. These tiny particles may have caused the original body to break apart during its fall.

People have known about these rocks for centuries. Aboriginal peoples were aware of the site long before Europeans arrived. In 1576, a provincial governor sent the military to find iron for weapons. They followed native reports of a mass that fell from the sky. The Spanish called the area Piguem Nonralta. Later, in 1774, Don Bartolomé Francisco de Maguna rediscovered a mass called el Mesón de Fierro. He thought it was part of an iron vein in the ground. In 1783, Rubin de Celis led an expedition using explosives to find the source. He incorrectly believed the metal came from a volcanic eruption. However, he sent samples to the Royal Society in London. Scientists there analyzed the samples and confirmed they were meteoritic.

Many different sized fragments have been discovered over time. Some pieces are tiny, weighing only a few milligrams. Others are massive. In 1803, a 1-tonne mass called Otumpa was found. In 1969, a metal detector helped find El Chaco below the surface. It was extracted in 1980 and weighed 28.8 tonnes.

The largest fragment was discovered more recently in 2016. It is named the Gancedo meteorite after the nearby town. The Gancedo weighs 30.8 tonnes. This makes it the largest piece from Campo del Cielo. It is one of the heaviest single-piece meteorite masses on Earth. It follows the 60-tonne Hoba meteorite from Namibia and a 31-tonne fragment from Cape York.

Protecting these treasures is a major concern. In 1990, police stopped a plot to steal the El Chaco meteorite. In 2015, authorities arrested four people for attempting to smuggle more than 100 kilograms of protected meteorites. Because of these threats, the meteorites are now protected by provincial law. This ensures that these scientific wonders remain in Argentina for study. The fragments are not just heavy rocks; they are protected pieces of history.

Studying Campo del Cielo helps scientists understand the early Solar System. The specific chemical makeup of the iron and nickel provides clues about how planets formed. The distribution of the strewn field shows how large objects behave when they hit our atmosphere. By looking at these fragments, we can see the materials that built our world billions of years ago. The site remains one of the most important locations for studying the history of space and Earth.