Chapter 2
The Solar System and Earth

Since the Big Bang, the Universe has been expanding, recycling itself through the birth and death of stars. Every supernova leaves behind the raw materials for something new.

Watch as Earth evolves from a violent, molten rock into a planet that somehow supports poetry, pizza, and primates. See how astronomers mapped our planet's place in the cosmic neighborhood. And explore Earth's surface, the cause of earthquakes, volcanic eruptions, and continental "surfing."

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Chapter at a Glance
35 Minutes
1 Threshold
4 Videos
2 Galleries

What Is the Solar System?

Is it daytime? Look up. That bright yellowish thing in the sky is your star. Your star is one of a septillion stars in our Universe. Your planet is one of over 100 billion planets in our galaxy. There are 2 trillion galaxies in our Universe.

You live on a speck of a rock careening around a mid-tier star with a bunch of other rocks and gas.

Don't let that make you feel small. Your home is extraordinary.

Threshold 4: Earth & Solar System

How tasty morsels of gas and rock created our home.
Blue and grey expanse of space with a vertical beam of light, centered is the Earth represented by a tiny white pixel.

Pale Blue Dot, a photo of Earth from 3.7 billion miles away.

What's in the Solar System?

Earth is part of a group of planets, moons, and smaller objects. All these objects orbit around one star, which we call the Sun. (No! Don't look directly at it... keep reading.) The Sun's gravity pulls all these objects into its orbit. Everything orbiting the Sun is part of the Solar System.

As of 2026, our Solar System contains:

Infographic displaying various compositions of the solar system including: a fiery star, planets, moons, asteroids, comets, dust, and gas.

How Big Is the Solar System?

Our Solar System is three light-years (18.6 trillion miles) across. Earth is 93 million miles from the Sun. Neptune is 2.8 billion miles out. The edge of the Oort cloud is about 1.5 light-years from the Sun.

If you jumped in NASA's best spaceship, it would take you tens of thousands of years to reach the edge of our Solar System. Don't try this at home.

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How Did the Sun Form?

Wait—"How did the Sun form?" Did you skip Threshold 2? It's a star.

Fine. One last time, for the people in the back:

Eons ago, an ancient supernova exploded across the Milky Way Galaxy, leaving behind a cloud of debris. About 4.6 billion years ago, some of that cloud collapsed under gravity. The center grew so hot and dense that hydrogen nuclei fused into helium. There you go. We got lucky. Our Sun is nice and mediocre. It's not so massive that it will burn through all its fuel in a few million years. And it's not one of those small stars that burns low and slow for trillions of years. It's just-right, allowing the time and heat for interesting stuff to develop around it. The Sun's been burning for 5 billion years, and its lifespan is about 10 billion. Humanity and all our nonsense is sorta like the Sun's midlife crisis. Look out, Universe! This star just turned 40 and bought a bright-red Lamborghini to avoid thoughts of its own mortality.

Activity

The Life Cycle of Our Sun

See how our Sun and stars will evolve

Age of star (billions)

How Did the Planets Form?

New elements, combined with the just-right Goldilocks Conditions came together and formed our Solar System.

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A Tour Across the Solar System

You live in an exceptionally weird neighborhood.


Earth: Third Rock from the Sun

Look down. That's Earth. Well, it's probably the floor or sidewalk or something... but under that, that's the Earth! It's a pretty OK place to live right now. But 4.5 billion years ago, no organism could survive where you're sitting. Radiation from a recent supernova kept the planet extremely hot, its surface was molten, and there was no oxygen. Massive meteorites and asteroids kept slamming into the planet, making it even hotter. Cosmic Yelp says: 3/10 stars. Not recommended.

What Did the Young Earth Look Like?

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History of Astronomy

Models of the Solar System

A historical map depicting the geocentric model of the universe, split into two circular diagrams on a decorative parchment background.

About 1,900 years ago, the Greek thinker Ptolemy standardized a model of the geocentric Universe, in which the Sun, Moon, and stars all orbit the Earth. Credit: Bartolomeu Velho's illustration of a Ptolemaic geocentric system, public domain.

Geocentric

For most of our history, humans believed the Universe revolved around us—like a whole species of TikTok influencers.

To be fair, if you wanted to study astronomy in the ancient world, you just kinda... looked up at the sky. From that vantage, it would have seemed like the Sun and stars revolved around you—around Earth.

A celestial map depicting the heliocentric system, framed by decorative engravings.

In 1543 CE, Nicolaus Copernicus developed a new model of a heliocentric Universe, in which the Sun sat at the center of everything. Credit: Andreas Cellarius's illustration of the Copernican system, public domain.

Heliocentric

This geocentric view endured for more than 1,400 years until it was toppled by Nicolaus Copernicus, whose work was confirmed by Galileo Galilei.

Through observational evidence, and by using the newly invented telescope, they produced data and logic supporting a heliocentric (Sun-centered) model of the Solar System.

The Atmosphere

How Did Earth's Atmosphere Form?

Early Earth was chaos. See how things settled down enough for the oceans and atmosphere to take shape.


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5:32

Activity

Goldilocks Conditions

Not too hot... Not too cold... Where in our Solar System are the conditions just right to support life?

  • Sun

    Even the coolest sunspots on the surface of the Sun are 5,500 °C. So, yes, way too hot.

  • Mercury

    With no real atmosphere to retain heat, the temperature is a freezing -180 °C at night to a scorching oven of 430 °C during the day.

  • Venus

    Because of a dense atmosphere (over 96% carbon dioxide) it's a runaway greenhouse effect. At 480 °C, it's the hottest planet in the Solar System.

  • Earth

    Our planet contains just the right amount of energy and water to support a diverse variety of life.

  • Mars

    Even though Mars reaches a temperate 20 °C at noon at the equator in summer, it's usually a frozen, arid world. The poles are way too cold to support humans—around -153 °C.

  • Jupiter

    This is a "gas giant"—nothing more than a giant ball of hydrogen, helium, and other gases with little solid surface, with an average temperature of -148 °C.

  • Saturn

    Saturn is too cold and gassy. Life-supporting planets usually posses a heavy-metal core surrounded by a rocky mantle.

  • Uranus

    The surface of Uranus is mostly composed of ices: methane, water, and ammonia. This -216 °C hydrogen and helium atmosphere isn't hospitable.

  • Neptune

    The only energy is lightning, ultraviolet light, and charged particles. Although it's the kind of environment in which scientists believe life began, it's not viable today.

  • Pluto

    Not only does liquid freeze solid on this dwarf planet, but even gases, like methane, will harden when Pluto is at its most distant, 5.9 billion kilometers from the Sun.

Is There Life Beyond Earth?

The textbook version of the Goldilocks Zone says that anything outside a thin band around a star is either too hot or too cold to support the development of life. We're just lucky that Earth sits in that just-right band. That's the textbook version.

But the truth might be...out there.

If you want to find other life in our Solar System, forget Mars. Look to the moons. Jupiter has 95, and Saturn has 274. Some moons, like Europa, Ganymede, and Enceladus hide huge, salty oceans beneath ice. Down there, chemistry and heat might have produced life. Those moons are way outside the "Goldilocks Zone" of our Sun.

Tectonic Plates

A Restless Planet: Plate Tectonics Explained

The Earth's tectonic plates

The Earth's crust creeps along at about two centimeters a year, sliding over a layer of molten rock. Where those massive plates meet, things get dramatic—they grind, collide, and occasionally lock up until the tension snaps. When that happens, the planet moves a lot faster than two centimeters a year. The idea that Earth's surface moves wasn't always obvious. Early mapmakers noticed that West Africa looks like it could plug neatly into Brazil. Then, in the early 1900s, German meteorologist Alfred Wegener argued that all the continents had once been part of a supercontinent he called Pangaea.

Why we're all Lava Surfers

Why we're all lava surfers

Journey with our team of Big Historians to Iceland, where the North American and Eurasian plates collide.

How Do We Know About Continental Drift?

Alfred Wegener

Alfred Wegener (1880–1930)

Alfred Wegener was the first to gather extensive evidence to support continental drift. He found tropical fossils on Arctic islands and matching mountain ranges on continents now oceans apart. This convinced him that the continents were moving. What he couldn't explain was how whole continents could bulldoze through Earth's crust. That missing piece left his theory adrift and most scientists unconvinced. Wegener died chasing the idea everyone thought was ridiculous... until it wasn't.

Harry Hess

Harry Hess (1906–1969)

During World War II, Harry Hess was hunting enemy submarines in the Pacific using the Navy's new sonar system. But Hess kept the sonar running between battles—mapping the seafloor instead of just scanning for enemies. After the war, he pieced together his data with findings from the Atlantic. The pattern was unmistakable: the ocean floor was growing. By the 1960s, studies of the Mid-Atlantic Ridge confirmed it: the Earth is constantly remaking itself.

Threshold 4

Earth & Solar System

  • Ingredients
  • Goldilocks Conditions
  • New Complexity
  • Which of the following is not a necessary ingredient in planetary formation?

  • Which process best describes how new planets are planets?

  • Why are planets considered to be more complex than stars?

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