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Orbits. Orbital motion and types of orbits

Created by potrace 1.16, written by Peter Selinger 2001-2019
10/06/2026

The online orbit simulations on this page will help us to know in more detail how are the orbital motion, the orbital trajectories and some of the main types of orbits.

This Thematic Unit is part of our Earth Sciences collection

STEM OnLine mini dictionary

Apoapsis

Point in an orbit where the celestial body is at its maximum distance from its center.

Geostationary Orbit

Circular orbit above the Earth’s equator in which the satellite appears to be fixed in the sky.

Hohmann Transfer Orbit

Orbital maneuver that uses two engine pulses to move a spacecraft between two circular orbits.

Kepler’s Laws

Three scientific laws describing the motion of planets around the Sun.

Orbit

Curved path followed by a physical object around another under the influence of gravity.

Orbital Elements

Set of parameters required to uniquely identify a specific orbit.

Orbital Inclination

Angle between the orbital plane and a reference plane such as the equator.

Orbital Perturbation

Variation in a body’s orbit caused by external forces such as radiation pressure or the gravity of other bodies.

Orbital Velocity

Speed required to maintain a stable orbit around a celestial body.

Periapsis

Point in an orbit where the celestial body is at its minimum distance from its center.

What are orbits

Orbits are the trajectories (that is why the term orbital trajectory is also used) followed by objects in space as they move around another object due to the influence of gravity. In the context of the solar system, planets, asteroids and comets orbit the sun, while satellites orbit the planets. Understanding orbits is fundamental to astronomy and space exploration.

Orbital motion

We call orbital motion the continuous displacement of an object in space around another more massive object, guided by the influence of gravity. This motion is the result of a delicate balance between the gravitational force that pulls the object toward the central body and the tangential velocity of the object, which tends to push it away. This balance generates orbital trajectories that can vary in shape from perfect circles to ellipses and open trajectories such as parabolas and hyperbolas. It is a dynamic phenomenon observed in natural planets and satellites, asteroids and spacecraft, all following Kepler’s laws, which describe the relationship between the shape, velocity and position of the object in its orbit.

In addition to the gravity of the massive object around which the orbital path is established, the orbital motion can be influenced by by the gravity of other nearby objects. This is known as gravitational perturbation and can make orbits more complex. For example, the Moon is influenced by both Earth’s gravity and the Sun’s gravity, resulting in a slightly elliptical orbit around the Earth.

Types of orbits by geometric shape

The trajectory followed by an object in space is determined by its velocity and the gravitational pull of the central body. According to the laws of orbital mechanics, these paths always take the form of a conic section.

Elliptical orbits

An elliptical orbit is the most common trajectory in the universe and features an oval or ellipse shape. In this type of orbit, the distance between the orbiting object and the central body changes constantly throughout its path. This means there is a point of closest approach known as perigee (or periapsis) and a point of maximum distance called apogee (or apoapsis). The object’s speed is not uniform: it moves much faster when it is close to the central body and slows down as it moves away. Most planets, natural satellites, and spacecraft follow elliptical trajectories.

Circular orbits

A circular orbit is a special, theoretical case of an elliptical orbit where the eccentricity is exactly zero. In this type of trajectory, the object maintains a completely constant distance from the center of the celestial body at every single point along its path, which means its orbital speed also remains unchanging. Although finding a perfect circular orbit in nature is practically impossible due to the gravitational perturbations of other bodies, aerospace engineers aim to approximate this shape when launching certain satellites to ensure their instruments always operate at the same altitude.

Parabolic orbits

A parabolic orbit is an open trajectory that marks the exact boundary between objects that remain trapped by gravity and those that manage to escape. It occurs when a body travels at the exact escape velocity of the system. The object approaches the central body, makes a single sharp turn around it, and then moves away permanently into deep space, slowing down progressively but never coming to a complete stop. It is a single-pass trajectory.

Hyperbolic orbits

A hyperbolic orbit is another open trajectory, but it differs from a parabolic one because the object travels at a speed clearly exceeding the escape velocity. The central celestial body deflects the object’s path due to gravity, but it lacks the necessary force to retain it. The object retains a considerable amount of speed even when it reaches an infinite distance from the central body. This is the type of orbit described by comets originating from outside the solar system or by spacecraft when performing a gravitational assist maneuver to gain speed and propel themselves toward other planets.

Types of orbits by space mission requirements

When artificial satellites are designed and launched, their orbit is meticulously selected based on altitude, inclination relative to the equator, and the specific needs of the mission on Earth.

Low Earth orbit

Known by its acronym LEO, this orbit is located at an altitude of between 160 and 2000 kilometers above the Earth’s surface. Being so close to Earth, satellites travel at high speeds (about 27,500 kilometers per hour) and complete a full loop around the planet in approximately ninety minutes. It is the ideal region for weather observation, mapping, and spy satellites, as it allows for very high-resolution imaging, and it is home to the International Space Station.

Medium Earth orbit

Known as MEO, this orbit encompasses the region of space located between 2000 and 35,786 kilometers in altitude. Satellites placed in this zone take anywhere from a few hours to a full day to complete a single orbit. Because it offers a perfect balance between data resolution and wide coverage of the Earth’s surface, it is used almost exclusively for global navigation and positioning satellite constellations, such as the American GPS system or the European Galileo system.

High Earth orbit

Known as HEO, this orbit comprises any orbit whose altitude sits above 35,786 kilometers from the Earth’s surface. At these immense distances, Earth’s gravitational pull is much weaker, causing satellites to move very slowly and take more than twenty-four hours to complete a single revolution. It is used for scientific satellites observing deep space and for globally monitoring our planet’s magnetic environment.

Polar orbits

A polar orbit is one that features an inclination close to ninety degrees relative to the Earth’s equator, meaning the satellite passes directly over or very close to the North and South Poles on every revolution. While the satellite moves vertically from pole to pole, the Earth rotates horizontally beneath it. This combination allows the satellite, after a set number of revolutions, to progressively scan and photograph every strip of the entire planet’s surface.

Sun-synchronous orbits

A sun-synchronous orbit is a special type of polar orbit whose altitude (usually between 600 and 800 kilometers) and mathematical inclination are calculated so that the orbital plane shifts subtly by about one degree per day. In this way, the orbit synchronizes with Earth’s annual journey around the Sun, ensuring that the satellite passes over a specific point on the surface at exactly the same local solar time every day. This is crucial for scientific and remote sensing missions, as all photos of a given area maintain the same light angle and shadows.

Geosynchronous orbits

A geosynchronous orbit is one that has an orbital period exactly equal to Earth’s rotation period on its own axis, which is twenty-four hours. This means the satellite takes the same time to circle the planet as the Earth takes to spin once. If the orbit has some inclination, the satellite will not look static from the ground; instead, it will appear to trace a geometric figure shaped like a figure-eight in the sky throughout the day, crossing the sky at the exact same times.

Geostationary orbit

The geostationary orbit (GEO) is a specific and highly important case within geosynchronous orbits. To achieve it, the satellite must be placed exactly at 35,786 kilometers in altitude with an inclination of zero degrees, meaning it is perfectly aligned over Earth’s equator. At this precise distance and position, the satellite moves identically to the Earth’s rotation, causing it to appear completely motionless at a fixed point in the sky when viewed from the ground. This allows fixed satellite dishes to point directly at it without needing tracking systems, serving as the foundation for satellite television and global telecommunications.

Molniya high-eccentricity orbits

The Molniya orbit is a markedly elliptical trajectory design with a sharp inclination of about 63.4 degrees, originally developed to bypass the issue that geostationary satellite signals do not reach northern polar regions effectively. In this orbit, the satellite passes very quickly at low altitude through the Southern Hemisphere (perigee) but travels extremely slowly at high altitude over the Northern Hemisphere (apogeo). Thanks to this, the satellite spends about eight hours of its twelve-hour orbit “hanging” almost motionless over the northern part of the Earth, providing stable communications to high-latitude zones.

Importance of orbits

Understanding orbits is crucial for space navigation and space mission planning. Scientists and space engineers use calculations and mathematical models to predict and control spacecraft orbits, ensuring that they stay on safe and efficient trajectories.

In addition to natural orbits, humans have succeeded in placing satellites in orbit around the Earth, which are used for various applications, such as communication, Earth observation, navigation, and scientific research.

The online orbit simulations on this page are an excellent way to delve deeper into orbital motion and the most important types of orbits. Give them a try!

STEM OnLine mini dictionary

Apoapsis

Point in an orbit where the celestial body is at its maximum distance from its center.

Geostationary Orbit

Circular orbit above the Earth’s equator in which the satellite appears to be fixed in the sky.

Hohmann Transfer Orbit

Orbital maneuver that uses two engine pulses to move a spacecraft between two circular orbits.

Kepler’s Laws

Three scientific laws describing the motion of planets around the Sun.

Orbit

Curved path followed by a physical object around another under the influence of gravity.

Orbital Elements

Set of parameters required to uniquely identify a specific orbit.

Orbital Inclination

Angle between the orbital plane and a reference plane such as the equator.

Orbital Perturbation

Variation in a body’s orbit caused by external forces such as radiation pressure or the gravity of other bodies.

Orbital Velocity

Speed required to maintain a stable orbit around a celestial body.

Periapsis

Point in an orbit where the celestial body is at its minimum distance from its center.

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!

Orbit simulations

Gravity and orbits


In the first of our online orbit simulations, you can move the sun, earth, moon and space station to see how it affects their gravitational forces and orbital paths. Visualize the sizes and distances between the different celestial bodies and turn off gravity to see what would happen without gravity!
Licencia de Creative Commons

Trajectory of a satellite


The last of our online orbit simulations, allows us to observe how the trajectory of an artificial satellite over the Earth’s surface changes as its period and the inclination of its orbit change.






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An orbit is the curved path that one object follows around another due to gravity. It is fundamental because it explains why planets, moons and satellites neither drift away into space nor fall directly toward the body that attracts them. In the solar system, for example, Earth orbits the Sun and the Moon orbits Earth in stable, repeating paths. Orbits can be nearly circular or slightly elongated, depending on the object’s speed and the strength of the gravitational pull. Understanding orbits helps explain everyday astronomical phenomena such as the movement of planets, the length of the year, the repetition of the seasons and the behavior of artificial satellites, which also remain in orbit because Earth’s gravity keeps them on a curved trajectory. For this reason, the concept of an orbit is essential for understanding how the nearby universe is structured and how celestial bodies move.
Gravity pulls objects toward the most massive body, but at the same time those objects move forward with a certain speed. The combination of both effects creates a curved path: gravity constantly “pulls,” while the object’s motion prevents it from falling straight in. If a planet or satellite moved too slowly, it would fall toward the central body; if it moved too fast, it would escape into space. When the speed is just right, gravity keeps it following a stable orbit. This balance explains why Earth continues orbiting the Sun and why the Moon remains around Earth. It also allows artificial satellites to function: they are launched with the exact speed needed so that Earth’s gravity keeps them in a steady path. Thus, the interaction between motion and gravity is the key mechanism behind all orbital movement in the solar system.
Because Earth is moving forward very fast at the same time the Sun pulls it inward. That combination creates a curved path instead of a fall. It’s like throwing a ball: if you throw it hard enough, it travels forward while gravity pulls it down. Earth moves so fast that it never reaches the Sun, and that’s why it stays in orbit.
Natural satellites, like the Moon, are objects that already existed and were captured by a planet’s gravity. Artificial satellites are built by humans and placed in orbit to do things like communication, observation or navigation. Both stay in orbit for the same reason: gravity keeps them following a curved path around the planet.
Because the object’s speed and the strength of gravity don’t always match perfectly to form a circle. Most of the time, the path is slightly stretched, forming an ellipse. Many orbits look almost circular, but technically they are a bit elongated.

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