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The Solar System. Characteristics and structure

09/04/2026

The online solar system simulations on this page will help us to discover the structure and some of the most interesting characteristics of the space of the universe where we are.

What is the Solar System

The solar system is a fascinating planetary system found in the Milky Way, our galaxy. It is composed of the Sun, a G-type star that radiates light and heat, and all the celestial bodies orbiting around it, including planets, dwarf planets, asteroids, comets and other smaller objects.

Characteristics of the Solar System

The solar system is distinguished by its organization and dynamics, being a harmonic set where various celestial bodies interact under the influence of the Sun’s gravity, which acts as its energetic and gravitational core. The orbits of the planets and other objects follow elliptical trajectories, showing the complexity of the forces that govern them. It is also remarkable for its enormous scale, with distances between planets spanning millions of kilometers, underscoring the vastness of space. The diversity of materials and phenomena present in the solar system, from the intense heat near the Sun to the icy regions beyond Neptune, reinforce its role as a microcosm of the universe, full of contrasts and wonders.

Structure of the Solar System

The solar system is composed of a diversity of elements orbiting the Sun. Among these, the eight main planets stand out, each with unique characteristics. In addition, we find dwarf planets, asteroids, comets and other formations that enrich the complexity of this vast system.

The Sun

The Sun, located at the center of the solar system, accounts for more than 99% of the total mass of the system. It is a hot plasma sphere composed mainly of hydrogen and helium, which generates energy through nuclear fusion in its core. This energy is radiated into space in the form of light and heat, and is essential for sustaining life on Earth.

Planets of the Solar System

There are eight recognized planets in the solar system: Mercury, Venus, Earth, Mars, Jupiter, Saturn, Uranus and Neptune. These planets vary in size, composition, and characteristics. The four inner planets, known as terrestrial planets (Mercury, Venus, Earth, and Mars), are rocky and relatively small. The four outer planets, known as giant gas planets (Jupiter, Saturn, Uranus, and Neptune), are much larger and are composed primarily of gases and liquids.

Other Solar System objects

In addition to the planets, the solar system is home to numerous smaller objects. Dwarf planets, such as Pluto and Eris, are smaller, planet-like bodies. Asteroids are irregular rocks that orbit the Sun, mainly in the asteroid belt between Mars and Jupiter. Comets are icy bodies that follow elliptical orbits around the Sun and, as they approach, may develop a bright coma and tail due to solar heating.

Beyond Neptune’s orbit extends the region called the Kuiper belt, which is home to a large number of icy bodies, including Pluto. Even further out lies the Oort cloud, a spherical region of comets in very distant orbits.

The online solar system simulations on this page are a very useful tool to improve our knowledge of our corner of the universe, so be sure to try them out!

Explore the exciting STEM world with our free, online, simulations and accompanying companion courses! With them you’ll be able to experience and learn hands-on. Take this opportunity to immerse yourself in virtual experiences while advancing your education – awaken your scientific curiosity and discover all that the STEM world has to offer!

Solar System Simulations

Solar System representation


This simulation is a generic representation of the Solar System that serves as an introduction to get to know it better. Try zooming in or out.






Solar System Scale


This simulation represents to scale what are the distances in the Solar System.






Solar system simulation


This complete solar system simulation allows you to predict how the position, mass, velocity and distance between planetary bodies affect their motion and orbits. It also illustrates how the gravitational force controls the motions of the planets and facilitates the exploration of the different motions that a group of planetary bodies can have.
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The solar system is a collection of astronomical bodies that orbit the Sun due to the gravitational force it exerts. It includes eight planets, their moons, dwarf planets, asteroids, comets and smaller objects distributed in regions such as the asteroid belt and the Kuiper belt. It is considered an organized system because each body follows a defined and stable orbit determined by its mass and distance from the Sun. The inner planets are rocky and located close to the Sun, while the outer planets are gas or ice giants found in colder, more distant regions. This structured arrangement allows scientists to study how the solar system formed, how its components evolve and how they interact, making it a fundamental model for understanding planetary systems throughout the universe.
The inner planets—Mercury, Venus, Earth and Mars—are small, rocky and dense, formed in the hotter region close to the Sun where light gases could not accumulate. In contrast, the outer planets—Jupiter, Saturn, Uranus and Neptune—are much larger and composed mainly of gases or ices, having formed in colder regions where these materials could condense and gather in great quantities. This division reveals that the solar system developed according to distance from the Sun and the physical conditions of each region of the protoplanetary disk. The contrast between rocky planets and gas or ice giants reflects different formation processes and explains why the bodies in the solar system vary so much in size and composition.
Because the Sun has far more mass than any planet, and its gravity keeps all the bodies in the solar system bound in stable orbits. Without that force, the planets would move in straight lines and drift away. They orbit because they move fast enough not to fall into the Sun, but not fast enough to escape its gravity. It’s a constant balance.
It depends on where they formed. Near the Sun, temperatures were too high for gases to accumulate, so only small rocky planets could form. Farther away, the environment was cold enough for light materials to condense, allowing planets to grow enormously and become gas or ice giants. It’s not luck—it’s physics.
Pluto still exists, but it doesn’t meet all the current criteria for being a planet. Although it orbits the Sun and is spherical, it hasn’t “cleared” its orbit, meaning it shares its region with many other Kuiper belt objects. For that reason, it’s classified as a dwarf planet. It’s not a downgrade—just a more precise definition..

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