Kyrie

From Role Players Resource

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| main | = | talk = | user = | wikipedia = | file | image = | mediawiki = | template = | help = | category = | portal = | book = | other | #default =

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Name and etymology

Chronology

Formation

Evolution of life

Future

Composition and structure

Shape

Chemical composition of the crust<ref name=brown_mussett1981/>
Compound Formula Composition
Continental Oceanic
silica SiO 2 60.2% 48.6%
alumina Al 2O3 15.2% 16.5%
lime CaO 5.5% 12.3%
magnesia MgO 3.1% 6.8%
iron(II) oxide FeO 3.8% 6.2%
sodium oxide Na2O 3.0% 2.6%
potassium oxide K2O 2.8% 0.4%
iron(III) oxide]] Fe2O3 2.5% 2.3%
water H2O 1.4% 1.1%
carbon dioxide CO2 1.2% 1.4%
titanium dioxide TiO2 0.7% 1.4%
phosphorus pentoxide P2O5 0.2% 0.3%
Total 99.6% 99.9%

Chemical composition

Internal structure

Geologic layers of the Earth<ref name=pnas76_9_4192/>

Earth cutaway from core to exosphere. Not to scale.
Depth<ref name=robertson2001/>
km
Component Layer Density
g/cm3
0–60 Lithosphere<ref group="note">Locally varies between 5 and 200 km.</ref>
0–35 Crust<ref group="note">Locally varies between 5 and 70 km.</ref> 2.2–2.9
35–60 Upper mantle 3.4–4.4
  35–2890 Mantle 3.4–5.6
100–700 Asthenosphere
2890–5100 Outer core 9.9–12.2
5100–6378 Inner core 12.8–13.1

Heat

Present-day major heat-producing isotopes<ref name="T&S 137"/>
Isotope Heat release
W/kg isotope
Half-life

years
Mean mantle concentration
kg isotope/kg mantle
Heat release
W/kg mantle
238U Template:Nowrap Template:Nowrap Template:Nowrap Template:Nowrap
235U Template:Nowrap Template:Nowrap Template:Nowrap Template:Nowrap
232Th Template:Nowrap Template:Nowrap Template:Nowrap Template:Nowrap
40K Template:Nowrap Template:Nowrap Template:Nowrap Template:Nowrap

Tectonic plates

Earth's main plates<ref name=brown_wohletz2005/>
File:Tectonic plates (empty).svg
Plate name Area
106 km2
Pacific Plate 103.3
African Plate 78.0
North American Plate 75.9
Eurasian Plate 67.8
Antarctic Plate 60.9
Indo-Australian Plate 47.2
South American Plate 43.6

Surface

Hydrosphere

Atmosphere

Weather and climate

Upper atmosphere

Magnetic field

Orbit and rotation

Rotation

Orbit

Axial tilt and seasons

Moon

Characteristics
Diameter 3,474.8 km
Mass 7.349{{#if:22 ×10{{#switch:{{{2}}} #default={{#switch:Template:Valid #default={{#switch:{{{2}}} plus=+Template:Val/delimitnum #default=Template:Val/delimitnum
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Semi-major axis 384,400 km
Orbital period Template:Nowrap

Habitability

Biosphere

Natural resources and land use

Land use Arable land Permanent crops Permanent pastures Forests and woodland Urban areas Other
Percentage 13.13%<ref name=cia/> 4.71%<ref name=cia/> 26% 32% 1.5% 30%

Natural and environmental hazards

Human geography

Template:Multiple image

Cultural viewpoint

Template:Solar System Template:Earth Template:Earth's location Template:Earth science Template:Physical Earth Template:Nature nav Template:Featured article



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kyriet.png

Kyrie

Designations
Name
Galactic Location
Quadrant
Sector
Coordinates
System Name
Star Name
Star Type
Star Diameter
Interstellar Neighbors
Total Planets  
Physical characteristics
Planetary Class  
Equatorial Diameter
Polar Diameter
Equatorial Circumference
Land Surface (%)
Water Surface (%)
Gravity (Relative to Earth)
Escape velocity
Length of Year (solar days)
Length of Day  
Axial tilt
Surface temp. min mean max
Kelvin ? K ? K ? K
Celsius ? °C ? °C ? °C
Capitol City
Major Starport
Minor Starport
Major Export
Minor Export  
Race Name
Population Count  
Technology Level  
Atmosphere
Surface pressure  
Composition nitrogen (N2)  
oxygen (O2)  
argon  
carbon dioxide (CO2)  
water vapor  

Chronology

 

Evolution of life

 

Future

 

Composition and structure

 

Shape

 

Chemical composition

Chemical composition of the crust
Compound Formula Composition
Continental Oceanic
silica SiO2 60.2% 48.6%
alumina Al2O3 15.2% 16.5%
lime CaO 5.5% 12.3%
magnesia MgO 3.1% 6.8%
iron(II) oxide FeO 3.8% 6.2%
sodium oxide Na2O 3.0% 2.6%
potassium oxide K2O 2.8% 0.4%
iron(III) oxide Fe2O3 2.5% 2.3%
water H2O 1.4% 1.1%
carbon dioxide CO2 1.2% 1.4%
titanium dioxide TiO2 0.7% 1.4%
phosphorus pentoxide P2O5 0.2% 0.3%
Total 99.6% 99.9%

 

Internal structure

 

Heat

 

Tectonic plates

 

Surface

 

Hydrosphere

 

Atmosphere

 

Weather and climate

 

Upper Atmosphere

 

Magnetic field

 

Orbit and rotation

 

Rotation

 

Orbit

 

Axial tilt and seasons

 

Moon

 

Habitability

 

Biosphere

 

Natural resources and land use

 

Natural and environmental hazards

 

Human geography

 

Cultural viewpoint

 

Cultural History

The Kyrian civilization is roughly one hundred thousand years old. In it's early history, the planet, was a group of nations that were continually at war with one another. The internecine war period lasted roughly thirty-five hundred years. Oddly enough, it took a nuclear war to stop the warfare between these nations. This war killed seventy-five percent of the population, but due to government preparations, there were enough members of the various governments left to start negotiations between them so that there would be no more warfare anywhere on the planet.

This was the beginning of the Restoration Period that eventually led to a planetary democratic government. The Restoration period lasted roughly two hundred years and resulted in the Kyrians living under a planetary democracy where everyone was guaranteed that they could live free.

It was like this for another fifty years before their space program was begun. The first six colonies that were constructed in geostationary orbit at twenty-two thousand miles. They were spaced out so that they were sixty degrees apart around the orbit. These colonies were six mektons long and one point two mektons in diameter. A mekton is a Kyrian length of measure that is 0.81 miles in length. As time went on the colonial populations increased as more people came to live there and others were born. Eventually, the ability to supply the colonies with materials and food outgrew the ability to supply it from the ground. They started to build orbital reclamation factories in order to have more useable materials, lessening the need for materials brought up from the surface.

It was at this time that a large ferrous nickel asteroid, roughly twelve mektons in volume came into the area. It missed the colonies by a thousand miles. In astronomical distances this was a bullet burn and got their attention. This asteroid was moving slowly enough so that it was trapped in an unstable orbit. The governors of the colonies decided to build a ship that could go out to the asteroid and start taking it apart for useable material. The amount of metal gained from this allowed them to construct several more mining ships, allowing them to go mine the asteroids in both asteroid belts. As time went on they were able to hollow out the inside of the two moonlets in orbit around the planet, and colonize them.

The internal volume of the two moonlets was roughly fifteen time the volume of all of the orbital colonies together. As this was the case, the colonists started moving into the moon colonies abandoning the previous generation of colonies. This gave enough materials to start construction of an orbital spacedock. After a couple of centuries a breakthrough in energy technology was made followed by a propulsion breakthrough. It was discovered that when these two technologies were merged together that they allowed faster than light travel. This was more than ninety thousand years ago.

Locations of Interest

 

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