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Luzonta

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This page contains the canonical information about the planet Luzonta, if you are looking for regional information look at Luzonta (Region).

Luzonta
Draft 1.png
A black and white map of Luzonta.
Designations
The World
Orbital characteristics
Epoch A2000
Aphelion152100000 km (94500000 mi)
Perihelion147095000 km (91401000 mi)
149598023 km (92955902 mi)
Eccentricity~0.0167086
365 d (12.0 months)
29.78 km/s (18.50 mi/s)
358.617°
Physical characteristics
Equatorial radius
6378.1 km (3963.2 mi)
Polar radius
6356.8 km (3949.9 mi)
Flattening0.0033528
Circumference40075.017 km (24901.461 mi) (equatorial)
40007.86 km (24859.73 mi) (meridional)
510,072,000km2
(316,944,000 mi2)
Volume1.08321 × 1012km3
Mass5.97237 x 1024 kg
Mean density
5.514 g/cm3
9.807 m/s2
0.3307
11.186 km/s (6.951 mi/s)
0.99726968 d (23.934472 h)
Equatorial rotation velocity
0.4651 km/s (0.2890 mi/s)
23.4392811°
Albedo0.367 geometric
0.306 Bond
Surface temp. min mean max
Celsius −89.2 °C 14.9 °C 56.9 °C
Fahrenheit −128 °F 58.7 °F 134.3 °F
Atmosphere
Surface pressure
101.325 kPa (at MSL)
Composition by volume78.08% nitrogen (N2) (dry air)
20.95% oxygen (O2)
0.930% argon
0.039% carbon dioxide (climate-variable)

Luzonta, or the Earth (Anglish) or Tierro (Spanish) is the fourth planet from the Son. It is the only known planet to accommodate life. There are around 8 million different plant and animal species around the World. Scientific analysis has concluded that Luzonta formed andd developed over 4 billion years ago. The Earth rotates around the Son in 365 and ¼ days, a period commonly accepted as an Earth year. The Earth's surface layer is formed of several slowly moving tectonic plates, interacting to produce mountain ranges, volcanoes, and earthquakes. The Earth's liquid outer core generates the magnetic field that shapes Earth's magnetosphere, deflecting destructive solar winds.

The atmosphere on the Earth is made up of mostly nitrogen and oxygen. More solar energy is received by tropical regions than polar regions and is redistributed by atmospheric and ocean circulation. Water vapor is widely present in the atmosphere and forms clouds that cover most of the planet.

The planet contains a variety of different nations and civilisations that inhabit the landmasses, which are home to many different vibrant cultures and languages. The planet is home to roughly 6 billion people, as of 2022.

Etymology

Geography

Continents

Parthenia

The Parthenian continent is located entirely within the northern hemisphere, located to the west of the Merillian Ocean and to the east of the Sarosan Ocean. It lies just north of continental Tarandra and the Aurean Sea, which a majority of the continents history and culture centres itself around. The continent is the home of a majority !Indo-European people, including the Anglish, Vermandan and the Sapherians. It is also home to other groups, such as the Uralic peoples of Rovanland and Sorkasia.The continent is rich in history, with humans settling around 46,000 years ago after passing across the Parthenian-Atusian landbridge. Parthenia is known for being a continent full of powerful empires and nations, that persist into modern day. Historic examples including the Sapherian Empire, the Anglish Empire and the Remillian Empire, all of which were the largest empire in the world at some point in time.

Parthenia makes up the northern part of the Parthrandran Landmass. The continent lies mainly within the temperate climate zones, being subjected to prevailing westerlies. The climate is milder in comparison to other areas of the same latitude around the globe due to the influence of the Gulf Stream, which is sometimes nicknamed "Parthenia's Central Heating".

Atusia

Atusia is a continent located within the northern hemisphere, located on the east side of the Merillian Ocean and to the west of the Sarosan Ocean. It lies just north of Muanbia and the Vareic Sea which seperates the two continents.

Muanbia

Barnesia

Tarandra

Oceans

Merillian Ocean

Sarosan Ocean

Siberic Ocean

Seas

Aurean Sea

Vareic Sea

Tectonics

Climate

History

Luzonta is home to humans, who over the last two million years of their existence have made history. The earliest humans appeared around 2 million years ago, and in their earliest migrations they spread through ancient landbridges from Muanbia to Atusia. It is likely that these early humans lived and survived on hunter-gatherer lifestyles. It was soon after that more of the early forms of humans migrated west into the Parthenian continent through the northern land bridge, and spread further south into the !Turkic regions of the continent.

Politics

Countries

Key: "*" = NPC Nation

Name Capital Population Continent Government type
 Angland Boroughsford 49,884,032 TBD Parliamentary constitutional monarchy
Moriora.jpg Moriora* Rawaki 418,440 TBD Parliamentary constitutional monarchy
Kaliban.jpg Kaliban* Subangjaya 17,900,000 TBD Presidential Republic
Savang.jpg Savang* Rakong 8,149,487 TBD One-party Marxist-Leninist unitary socialist republic
Hong Bang.jpg Hong Bang* Cao Lan 16,101,583 TBD Parliamentary unitary constitutional monarchy
Yerezh.jpg Yerezh* Tarshiha 3,329,309 TBD Parliamentary Republic

International Organisations

Sovereignty Disputes

References