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Index
1. Introduction
2. Planet Classifications
3. Star Classifications
4. What are Planets?
5. What are Moons?
6. What are Stars?
1. INTRODUCTION
There are several planet classes that are commonly used within the scientific
community. Each class denotes what temperature the planet would be and
if it is able to sustain viable humanoid lifeforms. Stars also have classifications
and life cycles that they follow, which will be covered. There are also
several discoveries and terms that are helpful to know and will be covered
in this guide.
2.
PLANET CLASSIFICATION
|
| Class
A |
Geothermal |
| Age: |
0-2 Billion
years |
| Diameter: |
1,000-10,000
km |
| Location: |
Exosphere/Cold
Zone |
| Surface: |
Partially
Molten |
| Atmosphere: |
Primarily
Hydrogen Compounds |
| Evolution: |
Cools to
become Class C |
| Life-forms: |
None |
| Example: |
Gothos |
|
|
| Class
B |
Geomorteus |
| Age: |
0-10 Billion
Years |
| Diameter: |
1,000-10,000
km |
| Location: |
Hot Zone |
| Surface: |
Partially
molten, high surface temperature |
| Atmosphere: |
Extremely
tenuous, few chemically active gases |
| Evolution: |
N/A |
| Life-forms: |
None |
| Example: |
Mercury |
|
|
| Class
C |
Geoinactive |
| Age: |
2-10 Billion
years |
| Diameter: |
1,000-10,000
km |
| Location: |
Ecosphere/Cold
Zone |
| Surface: |
Low surface
temperature |
| Atmosphere: |
Frozen |
| Evolution: |
N/A |
| Life-forms: |
None |
| Example: |
Pluto,
Psi 2000 |
|
|
| Class
D |
Asteroid/Moon |
| Age: |
2-10 Billion
Years |
| Diameter: |
100-1,000
km |
| Location: |
Hot Zone/Ecosphere/Cold
Zone;
found primarily in orbit of larger planets or in asteroid
fields. |
| Surface: |
Barren
and cratered |
| Atmosphere: |
None or
very tenuous |
| Evolution: |
N/A |
| Life-forms: |
None |
| Example: |
Moon (Sol
llla), Lunar V (Bajor Vlle) |
|
|
| Class
E |
Geoplastic |
| Age: |
0-2 Billion
years |
| Diameter: |
10,000-15,000
km |
| Location: |
Ecosphere |
| Surface: |
Molten,
high surface temperature |
| Atmosphere: |
Hydrogen
compounds and reactive gases |
| Evolution: |
Cools to
become Class-F |
| Life-forms: |
Carbon-cycle
(Excalbian) |
| Example: |
Excalbia |
|
|
| Class
F |
Geometallic |
| Age: |
1-3 Billion
years |
| Diameter: |
10,000-15,000
km |
| Location: |
Ecosphere |
| Surface: |
Volcanic
eruptions due to molten core |
| Atmosphere: |
Hydrogen
compounds |
| Evolution: |
Cools to
become Class-G |
| Life-forms: |
Silicon-based
(Horta) |
| Example: |
Janus IV |
|
|
| Class
G |
Geocrystalline |
| Age: |
3-4 Billion
years |
| Diameter: |
10,000-15,000
km |
| Location: |
Ecosphere |
| Surface: |
Still Crystallizing |
| Atmosphere: |
Carbon
dioxide, some toxic gases |
| Evolution: |
Cools to
become Class-K, L, M, N, O or P |
| Life-forms: |
Primitive
single-celled organisms |
| Example: |
Delta Vega |
|
|
| Class
H |
Desert |
| Age: |
4-10 Billion
years |
| Diameter: |
8,000-15,000
km |
| Location: |
Hot Zone/Ecosphere/Cold
Zone |
| Surface: |
Hot and
Aric, little or no surface water. |
| Atmosphere: |
May contain
heavy gases and metal vapors |
| Evolution: |
N/A |
| Life-forms: |
Drought-
and radiation- resisteant plants, animal life |
| Example: |
Rigel Xll,
Tau Cygna V |
|
|
| Class
I |
Gas
Supergiant |
| Age: |
2-10 Billion
years |
| Diameter: |
140,000-10
million km |
| Location: |
Cold Zone |
| Surface: |
Tenuous,
comprised of gaseous hydrogen and hydrogen compounds; radiates
heat |
| Atmosphere: |
Zones vary
in temperature, pressure and composition; water vapor may
be present |
| Evolution: |
N/A |
| Life-forms: |
Unknown |
| Example: |
Q'TahL |
|
|
| Class
J |
Gas
Giant |
| Age: |
2-10 Billion
years |
| Diameter: |
50,000-140,000
km |
| Location: |
Cold Zone |
| Surface: |
Tenuous,
comprised of gaseous hydrogen and hydrogen compounds; radiates
some heat |
| Atmosphere: |
Zones vary
in temperature, pressure and composition |
| Evolution: |
N/A |
| Life-forms: |
Hydrocarbon-based
(Jovian) |
| Example: |
Jupiter,
Saturn |
|
|
| Class
K |
Adaptable |
| Age: |
4-10 Billion
years |
| Diameter: |
5,000-10,000
km |
| Location: |
Ecosphere |
| Surface: |
Barren,
little or no surface water |
| Atmosphere: |
Thin, mostly
carbon dioxide |
| Evolution: |
N/A |
| Life-forms: |
Primitive
single-celled organisms; adaptable for humanoid colonization
through the use of pressure domes |
| Example: |
Mars, Mudd |
|
|
| Class
L |
Marginal |
| Age: |
4-10 Billion
years |
| Diameter: |
10,000-15,000
km |
| Location: |
Ecosphere |
| Surface: |
Rocky and
barren, little surface water |
| Atmosphere: |
Oxygen/argon,
high concentration of carbon dioxide |
| Evolution: |
N/A |
| Life-forms: |
Limited
to plant life; suitable for humanoid colonization |
| Example: |
Indri Vlll |
|
|
| Class
M |
Terrestrial |
| Age: |
3-10 Billion
years |
| Diameter: |
10,000-15,000
km |
| Location: |
Ecosphere |
| Surface: |
Surface
water abundant; if water or ice covers more than 80% of surface,
planet is considered Class-O or Class-P |
| Atmosphere: |
Nitrogen,
oxygen, trace elements |
| Evolution: |
N/A |
| Life-forms: |
Extensive
vegetation, animal life, humanoids |
| Example: |
Earth,
Vulcan, Cardassia Prime |
|
|
| Class
N |
Reducing |
| Age: |
3-10 Billion
Years |
| Diameter: |
10,000-15,000
km |
| Location: |
Ecosphere |
| Surface: |
High surface
temperature due to greenhouse effect; water exists only as
vapor |
| Atmosphere: |
Extremely
dense, carbon dioxide and sulfides |
| Evolution: |
N/A |
| Life-forms: |
Unknown |
| Example: |
Venus |
|
|
| Class
O |
Pelagic |
| Age: |
3-10 Billion
years |
| Diameter: |
10,000-15,000
km |
| Location: |
Ecosphere |
| Surface: |
Liquid
water covers 80% or more of surface area |
| Atmosphere: |
Nitrogen,
oxygen, trace elements |
| Evolution: |
N/A |
| Life-forms: |
Aquatic
vegetations, animal life, humanoids |
| Example: |
Argo |
|
|
| Class
P |
Glaciated |
| Age: |
3-10 Billion
years |
| Diameter: |
10,000-15,000
km |
| Location: |
Ecosphere |
| Surface: |
Water ice
covers 80% or more of the surface area |
| Atmosphere: |
Nitrogen,
oxygen, trace elements |
| Evolution: |
N/A |
| Life-forms: |
Hardy vegetation,
animal life, humanoids |
| Example: |
Exo lll |
|
 |
| Class
Q |
Variable |
| Age: |
2-10 Billion |
| Diameter: |
4,000-15,000
km |
| Location: |
Hot Zone/Ecosphere/Cold
Zone |
| Surface: |
Ranges
from molten to water and/or carbon dioxide ice, due to eccentric
orbit or variable output of star |
| Atmosphere: |
Ranges
from tenuous to very dense |
| Evolution: |
N/A |
| Life-forms: |
N/A |
| Example: |
Genesis
Planet |
|
 |
| Class
R |
Rogue |
| Age: |
2-10 Billion
years |
| Diameter: |
4,000-15,000
km |
| Location: |
Interstellar
space, cometary halos |
| Surface: |
May be
temperate due to geothermal venting |
| Atmosphere: |
Primarily
volcanic outgassing |
| Evolution: |
N/A |
| Life-forms: |
Non-photosynthetic
plants, animal life |
| Example: |
Dakala |
|
 |
| Class
S |
Ultragiant |
| Age: |
2-10 Billion
years |
| Diameter: |
10,000-50,000
km |
| Location: |
Cold Zone |
| Surface: |
Tenuous,
Composed of gaseous hydrogen and hydrogen compounds; radiates
considerable heat |
| Atmosphere: |
Zones vary
in temperature, pressure and composition; water vapor may
be present |
| Evolution: |
N/A |
| Life-forms: |
Unknown |
| Example: |
N/A |
|
 |
| Class
T |
Ultragiant |
| Age: |
2-10 Billion
years |
| Diameter: |
50,000-120,000
km |
| Location: |
Cold Zone |
| Surface: |
Tenuous,
composed of gaseous hydrogen and hydrogen compounds; radiates
considerable heat |
| Atmosphere: |
Zones vary
in temperature, pressure and composition; water vapor may
be present |
| Evolution: |
N/A |
| Life-forms: |
Unknown |
| Example: |
N/A |
|
|
| Class
Y |
Demon |
| Age: |
2-10 Billion
years |
| Diamater: |
10,000-50,000
km |
| Location: |
Hot Zone/Ecosphere/Cold
Zone |
| Surface: |
Temperature
can exceed 500* K |
| Atmosphere: |
Turbulent,
saturated with toxic chemicals and termionic radiation |
| Evolution: |
N/A |
| Life-forms: |
Mimetic
(Delta Quadrant) |
| Example: |
N/A |
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3. STAR CLASSIFICATIONS
Picture provided by Star Trek Star Charts- Paramount
4. What are Planets?
A
planet is a body of considerable mass that orbits a star and that produces
no energy through nuclear fusion. Prior to the 1990s only nine planets
were known (all of them in our solar system). As of 3 November 2004, 133
are known, with all of the new discoveries being extrasolar planets, sometimes
known as exoplanets; that is, planets outside of our solar system and
orbiting other stars.
Planets
are believed to form from a collapsing nebula that a star formed from,
aggregating from gas and dust that orbited the protostar in a dense protostellar
disk before the star's core ignited and its solar wind blew remaining
material away.
An extrasolar planet
(or exoplanet) is a planet which orbits a star other than the Sun, and
therefore belongs to a planetary system other than our solar system.
5. What are Moons?
Chunks or balls of rocks that travel around planets. They are held in
place by the gravity of the planet. All the planets in our solar system,
except Mercury and Venus, have moons. The Earth has one moon. Jupiter
has the most moons of all the planets - with more than 60.
6. What are Stars?
A star is any massive gaseous body in outer space, just like the Sun.
Unlike a planet, a star generates energy through nuclear fusion and therefore
emits light. All stars except the Sun appear as shining points in the
nighttime sky that twinkle because of the effect of the Earth's atmosphere
and their distance from us. The Sun is also a star, but it is close enough
to Earth to appear as a disk instead, and to provide daylight.
The nearest star to
the Earth, apart from the Sun, is Proxima Centauri, which is 39.9 trillion
kilometres, or 4.2 light years away (light from Proxima Centauri takes
4.2 years to reach Earth). Travelling at the orbit speed of the Space
Shuttle (5 miles per second -- almost 30 thousand kilometers per hour),
it would take about 150 thousand years to get there.
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