Planets are large celestial objects which revolved around a particular star and are usually spheroid in shape. The most commonly known planets are the eight that make up our solar system: Jupiter, Saturn, Uranus, Neptune, Earth, Venus, Mars, and Mercury. However, there are many more planets that exist outside of our solar system. Astronomers have come up with many criteria they use to classify these planets, one criterion is classifying the planets based on their composition. There are 17 different types of planets on the basis of composition.
Chthonian planets are celestial objects revolving close to a star which was originally gas giants but had their helium and hydrogen atmospheres stripped away by high temperatures emanating from their respective nearby stars leaving behind a metallic and rocky core. There are no chthonian planets in our solar system, but there are several such planets that have been observed including Kepler-57b and Kepler-52b.
A carbon planet is a theoretical planet that is believed to have a higher concentration of carbon than oxygen in its composition. Such planets are also thought to have cores made of iron or steel, characteristic to terrestrial planets. The surface of these planets is believed to be covered by liquid or frozen hydrocarbons with a layer of graphite or diamonds several miles thick beneath the surface. A suitable candidate of a carbon planet is the 55 Cancri e planet.
A city planet is a hypothetical planet, also known as an ecumenopolis, which is a planet-sized city. Proponents of the city planet concept believe that in the future global cities will grow and cover the entire globe and form a city planet. The concept was popularized after city planets were portrayed in several works of fiction including the famous Star Wars franchise. City planets are purely hypothetical as there is no known city planet.
As its name suggests, a coreless planet is a planet without a core. This hypothetical type of planet is exclusively made up of a mantle.
Desert planets are terrestrial planets whose surfaces have desert-like conditions. Such planets are believed to have a bigger habitable zone than Earth-like watery planets. The concept of desert planets has been portrayed in modern works of fiction such as the 1965 novel “Dune.” Some astronomers believe that the Earth will eventually become a desert planet as the Sun increases in luminosity. Venus is also believed to have been a desert planet in the past.
A gas dwarf is a celestial body with a solid core but covered by a thick atmosphere made up of helium, hydrogen and other volatile gases. The gas dwarf is similar in composition to the gas giant planets and only differs in size. One example of a gas dwarf is Kepler-138d which is an extrasolar planet.
Gas giants are planets which are mainly made up of helium and hydrogen and other volatile compounds. These planets which exist in immense sizes are some of the largest known planets. Our solar system has two planets that are classified as gas giants, and these are Saturn and Jupiter. These planets are believed to have a molten rocky core. However, the properties of the compounds that exist in the cores of these gas giants are poorly understood due to the great temperatures and pressure.
A helium planet has an atmosphere that is predominantly made up of helium. Scientists believe such planets are formed after high temperatures of a nearby star cause the evaporation and disappearance of lighter gases including hydrogen and leave behind an atmosphere made up of helium. Due to the high concentration of helium in the atmosphere, helium planets are believed to be white and light-gray in appearance.
Ice giants are planets which are mainly composed of dense gases which are heavier than those found in gas giants. These planets which were initially categorized as gas giants were established to be distinct in composition as they are primarily made up of carbon, sulfur, oxygen, and nitrogen instead of the hydrogen and helium found in gas giants. Neptune and Uranus are the two ice giants of our solar system.
An ice planet is is predominantly made up of volatile compounds such as water, methane, and ammonia in their frozen states. These planets experience extremely low temperatures (below negative (-) 13 degrees Celsius). Our solar system does not have any ice planets, as the only icy objects which have these characteristics are too small to be classified as planets. Ice planets are key candidates of the presence of extraterrestrial life as scientists believe these planets have sub surface oceans which have conditions suitable to accommodate life.
An iron planet is a type of planet which is mainly made up of its iron-rich core. Such planets are also recognized for the limited presence or complete absence of a mantle. Scientists believe that these types of planets were initially terrestrial planets but had their mantles stripped away as a result of giant impacts. Mercury is the only iron planet in our solar system.
Lava planet is a theoretical type of planet which is characterized by the presence of molten lava covering its surface. These planets are believed to have intense volcanic activity as a result of a recent large collision event or a planet in its infancy. These planets are also believed to exist within proximity of their respective stars.
An ocean planet is a hypothetical type of planet which is thought to be wholly or predominantly covered by water. These planets have 10% of their mass being water (water accounts for only 0.05% of the Earth’s mass). Ocean planets have oceans hundreds of miles in depth.
A protoplanet are large celestial bodies which were formed as a result of the collision of planetesimals and are also known are planet embryos. There are no established protoplanets in our solar system with the closest equivalent being asteroids such as Pallas and Vesta.
Puffy planets are gas giants which exist close to their stars and temperatures from the stars cause their atmospheres to expand and result in such planets having a large equatorial radius but relatively low densities. There are no such planets in the solar system, but few have been discovered beyond our solar system including WASP-12b and WASP 17b.
A silicate planet is primarily made up of silicate compounds. These planets are characterized by a solid crust, a silicate mantle, and an iron-based core. Depending on the presence of tectonic and volcanic activity, these planets can also have mountains, canyons, and valleys. All the four planets closest to the Sun (Mercury, Venus, Earth, and Mars) are categorized as silicate planets.
A terrestrial planet is the broader classification of silicate planets as they have solid surfaces. The composition of the core of terrestrial planets is also diverse with some being made of iron while others are made of carbon-based compounds. However, there are terrestrial planets which do not have a core which is known as coreless planets.
How Many Types Of Planets Are There On The Basis Of Composition?
There are 17 different types of planets on the basis of composition. These are chthonian planets, carbon planets, city planets, coreless planets, desert planets, gas dwarfs, gas giants, helium planets, ice giants, ice planets, iron planets, lava planets, ocean planets, protoplanets, puffy planets, silicate planets, and terrestrial planets.
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