Set five years after the 2nd Runner, Zero Wing is the story of multiple frames...
 
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» Nidhoggr
Zone of the Enders: Zero Wing Icon_minitimeThu Sep 23, 2010 11:38 pm by Tsubine

» Vic Viper Mass-Production Type
Zone of the Enders: Zero Wing Icon_minitimeThu Sep 23, 2010 11:37 pm by Tsubine

» Vic Viper Assault Type
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» Vic Viper II
Zone of the Enders: Zero Wing Icon_minitimeThu Sep 23, 2010 11:36 pm by Tsubine

» Vic Viper
Zone of the Enders: Zero Wing Icon_minitimeThu Sep 23, 2010 10:56 pm by Tsubine

» Clod
Zone of the Enders: Zero Wing Icon_minitimeThu Sep 23, 2010 10:56 pm by Tsubine

» Cyclops
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» Phantoma II
Zone of the Enders: Zero Wing Icon_minitimeThu Sep 23, 2010 10:55 pm by Tsubine

» Phantoma
Zone of the Enders: Zero Wing Icon_minitimeThu Sep 23, 2010 10:55 pm by Tsubine

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Rules and Information

This is where you will find all of the information on the site, as well as the rules. You MUST read these.
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This is where all of the templates will be located. You are NOT to post in here.
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Applications

This is where you will post your application for a character.
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Organizations & Mechanics

 
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Organizations

This is where you will learn of the groups here on ZOE: Zero Wing as well as apply for a position within it.
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Mechanics

This is where you will learn of the many Orbital Frames and space ships here on Zero Wing.
1414Thu Sep 23, 2010 11:38 pm
Tsubine Nidhoggr
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Earth

 
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Africa

Africa was relatively untouched during the first conflict on Earth in 2180. This resulted in the UNSF moving their main space base into Egypt.
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Antartica

A barren wasteland only filled with UNSF's research facilities. Well, those and a colony that fell at a low enough velocity that it only broke the ice. Lights have been seen within the powerless colony...
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Asia

With the fall of Communist China in 2045, Asia's power has grown substantially. The current capitol of China is in the recently-constructed city of Laoho. Laoho is in the direct center of China, and it is unreachable by any land-based artillery. Japan is rumored to have an AI construction system in Hokkaido. The UNSF also is rumored to have a top-secret base somewhere in the Taklamakan Desert...
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Australia

Australia has gone from vacation spot to an area only civilians can go to. In 2150, Australia closed its borders to all military personell and their families from the UNSF. Only political figures and civilians may enter Australia. In fact, the entire coastline is lined with large 200mm anti-warship cannons and 88mm anti-air cannons. It also has a metatron-powered shield surrounding the continent.
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Europe

The original capitol of the UNSF was Berlin, however the conflict years ago caused most of Europe to be a nuclear wasteland. In fact, Europe's total population is under 2,000,000 now. Currently, the entire UNEF is rebuilding the cities within the sky.
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North America

The United States has turned into a militaristic democracy. The military runs the police and most of the supplies are devoted to Orbital Frame and warship development. It is rumored that the USA is thinking of removing itself from the UNSF's roster of deployment.
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South America

Flooding due to environmental changes caused many cities to sink beneath the Amazon. Now, South America is split in half due to the river. An underground base in Brazil houses the UNSF's nuclear arsenal.
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Space

 
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Overwatch

Overwatch is the UNSF's main battle station in space. It is positioned on an asteroid brought to Earth's orbit. It houses most of the UNSF fleet and their computer networking hub. It is heavily defended so an attack would not be recommended.
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The Moon

While it is not massively colonized, there are a few scattered colonies on the moon. However, this does not include Line Ark, the moon's "ring" colony.
Line Ark
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Angel Halo

BAHRAM's main space base. Angel Halo is in Deimos's orbit. While it is much larger than Overwatch, Angel Halo is less defended by itself. However, the BAHRAM fleet is stationed around and inside of it. It was made after Aumaan's destruction.
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Hyperspeed Energy Transports

These are large tubes made of energy that propel matter at extremely high speeds to get from planet-to-planet in a matter of hours. If you touch the sides too long, your mecha will get caught in the flow and be ripped to shreds. It takes about 4 hours to get from Earth to Mars, and about 6 hours to get from Mars to Jupiter.
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Mars & Surrounding Space

 
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Mars

Mars is the fourth planet from the Sun in the Solar System. The planet is named after the Roman god of war, Mars. It is often described as the "Red Planet", as the iron oxide prevalent on its surface gives it a reddish appearance. Mars is a terrestrial planet with a thin atmosphere, having surface features reminiscent both of the impact craters of the Moon and the volcanoes, valleys, deserts, and polar ice caps of Earth. The rotational period and seasonal cycles of Mars are likewise similar to those of Earth. Mars is the site of Olympus Mons, the highest known mountain within the Solar System, and of Valles Marineris, the largest canyon. It is controlled by BAHRAM, and has been since the offensive there.
Borealis Basin, Valles Marineris, Vascilla City
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Deimos

Deimos is the smaller and outer of Mars's two moons (the other being Phobos). It is named after Deimos, a figure representing dread in Greek Mythology. Its systematic designation is Mars II. Deimos, like Mars' other moon Phobos, has spectra, albedos and densities similar to those of a C- or D-type asteroid. Deimos is composed of rock rich in carbonaceous material, much like C-type asteroids and carbonaceous chondrite meteorites. It is cratered, but the surface is noticeably smoother than that of Phobos. The two largest craters, Swift and Voltaire, each measure about 3 kilometres across.
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Phobos

Phobos is the larger and closer of the two moons of Mars, the other being Deimos. Both moons were discovered in 1877. With a mean radius of 11.1 km (6.9 mi), Phobos is 7.24 times as massive as Deimos. It is named after the Greek god Phobos (which means "fear"), a son of Ares (Mars). Phobos is one of the least-reflective bodies in the solar system, and features a large impact crater, Stickney crater. It orbits so close to the planet that it moves around Mars faster than Mars itself rotates. As a result, from the surface of Mars it appears to rise in the west, move rapidly across the sky (in 4 h 15 min or less) and set in the east. Phobos's orbital radius is decreasing, and it will eventually either impact the surface of Mars or break up into a planetary ring. It was originally the site of BAHRAM's headquarters, but now it is on Deimos.
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Jupiter & Surrounding Space

 
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Antilla Colony

A large torus-like colony, Antilla is where Jehuty and Anubis were constructed. It is quite well protected nowadays as it is the Jupiter Alliance's main Orbital Frame construction base.
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Callisto

Callisto is a moon of the planet Jupiter, and it is the third-largest moon in the Solar System and second largest in the Jovian system after Ganymede. Callisto has about 99% the diameter of the planet Mercury but only about a third of its mass. Callisto is composed of approximately equal amounts of rock and ices. The surface of Callisto is heavily cratered and extremely old. It does not show any signatures of subsurface processes such as plate tectonics or volcanism, and is thought to have evolved predominantly under the influence of impacts. It is also very rich in metatron ore.
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Europa

Europa is the sixth moon of the planet Jupiter, and the smallest of its four Galilean satellites. Slightly smaller than Earth's Moon, Europa is primarily made of silicate rock and probably has an iron core. It has a tenuous atmosphere composed primarily of oxygen. Its surface is composed of ice and is one of the smoothest in the Solar System. This surface is striated by cracks and streaks, while craters are relatively infrequent. The apparent youth and smoothness of the surface have led to the hypothesis that a water ocean exists beneath it.
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Ganymede

Ganymede is a satellite of Jupiter and the largest satellite in the Solar System. It is the seventh moon and third Galilean satellite outward from Jupiter. Ganymede is composed of approximately equal amounts of silicate rock and water ice. It is a fully differentiated body with an iron-rich, liquid core. A saltwater ocean is believed to exist nearly 200 km below Ganymede's surface, sandwiched between layers of ice. Its surface is composed of two main types of terrain. Dark regions, saturated with impact craters and dated to four billion years ago, cover about a third of the satellite. Lighter regions, crosscut by extensive grooves and ridges and only slightly less ancient, cover the remainder. The cause of the light terrain's disrupted geology is not fully known, but was likely the result of tectonic activity brought about by tidal heating.
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Io

Io is the innermost of the four Galilean moons of the planet Jupiter and, with a diameter of 3,642 kilometres (2,263 mi), the fourth-largest moon in the Solar System. With over 400 active volcanoes, Io is the most geologically active object in the Solar System. This extreme geologic activity is the result of tidal heating from friction generated within Io's interior as it is pulled between Jupiter and the other Galilean satellites—Europa, Ganymede and Callisto. Several volcanoes produce plumes of sulfur and sulfur dioxide that climb as high as 500 km (310 mi) above the surface. Io's surface is also dotted with more than 100 mountains that have been uplifted by extensive compression at the base of the moon's silicate crust. Some of these peaks are taller than Earth's Mount Everest. Unlike most satellites in the outer Solar System, which are mostly composed of water ice, Io is primarily composed of silicate rock surrounding a molten iron or iron sulfide core. Most of Io's surface is characterized by extensive plains coated with sulfur and sulfur dioxide frost. Io's volcanism is responsible for many of that satellite's unique features. Its volcanic plumes and lava flows produce large surface changes and paint the surface in various shades of yellow, red, white, black, and green, largely due to allotropes and compounds of sulfur. Numerous extensive lava flows, several longer than 500 kilometres (311 mi) in length, also mark the surface. These volcanic processes have given rise to a comparison of the visual appearance of Io's surface to a pizza. The materials produced by this volcanism provide material for Io's thin, patchy atmosphere and Jupiter's extensive magnetosphere.
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