Rutherford Star System

Rutherford Star System

Level 45

Rutherford is a level 45 star system in Starfield.

All star systems in Starfield have a recommended player level. For Rutherford, this level is 45. It is recommended that your character is at level 45 or higher if you would like to visit any of the planets in the Rutherford system.

Resources

Rutherford contains 24 resources.

NameRaritySymbolWeightValueID
Aluminum0Al0.570000557D
Antimony3Sb0.8300000557B
Argon0Ar0.5500005588
Benzene1C6Hn0.61900005585
Beryllium1Be0.512000057D9
Caesium3Cs0.825000057DF
Carboxylic Acids2R-COOH0.81200005586
Chlorine0Cl0.560000557C
Chlorosilanes1SiH3Cl0.6140000557E
Copper0Cu0.61000005576
Helium-30He-30.550000558E
Iridium1Ir0.7140000558A
Iron0Fe0.680000556E
Lead0Pb0.71000005568
Lithium2Li0.5140000557F
Mercury2Hg0.8220027C4A1
Neodymium2Nd0.82000005580
Neon3Ne0.51600005587
Nickel0Ni0.61000005572
Platinum2Pt0.82400005573
Titanium2Ti0.5120000556D
Uranium0U0.71400005589
Vanadium2V0.7240000558B
Water0H2O0.5400005591

Planetary Bodies

Rutherford has 21 planetary bodies: 6 planets and 15 moons.

Rock
0.71
Temperate
Std O2
Very strong
Heavy metal
7
7
Type
Gravity
Temperature
Atmosphere
Magnetosphere
Water
Fauna
Flora
Barren
Inferno
Std CO2
None
None
Type
Temperature
Atmosphere
Magnetosphere
Water
Biomes
Craters
Barren
Inferno
None
None
None
0
0
Type
Temperature
Atmosphere
Magnetosphere
Water
Fauna
Flora
Biomes
Craters
Barren
Inferno
None
None
None
Type
Temperature
Atmosphere
Magnetosphere
Water
Biomes
Craters
Rock
Inferno
Extr CO2
Very strong
None
Type
Temperature
Atmosphere
Magnetosphere
Water
Biomes
DesertHills
Barren
Scorched
None
None
None
Type
Temperature
Atmosphere
Magnetosphere
Water
Biomes
Craters
Barren
Temperate
None
None
None
Type
Temperature
Atmosphere
Magnetosphere
Water
Biomes
Craters
Gas giant
Frozen
H2
Extreme
None
Type
Temperature
Atmosphere
Magnetosphere
Water
Biomes
Ocean
Ice
Frozen
None
None
Chemical
Type
Temperature
Atmosphere
Magnetosphere
Water
Resources
Biomes
Ice
Ice
Frozen
None
None
Safe
Type
Temperature
Atmosphere
Magnetosphere
Water
Resources
Biomes
Ice
Ice
Frozen
None
None
Chemical
Type
Temperature
Atmosphere
Magnetosphere
Water
Resources
Biomes
Ice
Rock
Frozen
Thin M
None
Heavy metal
Type
Temperature
Atmosphere
Magnetosphere
Water
Biomes
CratersDesertIceMountains
Ice
Frozen
None
None
Safe
Type
Temperature
Atmosphere
Magnetosphere
Water
Ice giant
Frozen
H2
Weak
None
Type
Temperature
Atmosphere
Magnetosphere
Water
Biomes
Ocean
Rock
Deep freeze
Thin O2
None
Safe
Type
Temperature
Atmosphere
Magnetosphere
Water
Biomes
IceOceanTablelandsWetlands
Rock
Frozen
Thin M
None
Chemical
Type
Temperature
Atmosphere
Magnetosphere
Water
Biomes
CratersDesertIceMountains
Gas giant
Deep freeze
H2
Extreme
None
Type
Temperature
Atmosphere
Magnetosphere
Water
Biomes
Ocean
Rock
Deep freeze
Thin N2
None
Chemical
Type
Temperature
Atmosphere
Magnetosphere
Water
Ice
Deep freeze
None
None
Heavy metal
Type
Temperature
Atmosphere
Magnetosphere
Water
Biomes
Ice
Ice
Deep freeze
None
None
Safe
Type
Temperature
Atmosphere
Magnetosphere
Water
Resources
Biomes
Ice
Ice
Deep freeze
None
None
Chemical
Type
Temperature
Atmosphere
Magnetosphere
Water
Resources
Biomes
Ice
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Information

Level45
Catalogue IDGl 504
Planetary Bodies21
Planets6
Moons15
Star Spectral ClassG0
Star Temperature (Kelvin)6000
Star Solar Mass1.1
Star Radius731115
Star Magnitude3.97

Origin

Ernest Rutherford (1871-1937) is a towering figure in the annals of science, often referred to as the "father of nuclear physics." Born in New Zealand, Rutherford's pioneering research in atomic physics and radioactivity led to several foundational discoveries and has cemented his legacy as one of the most influential scientists in history.

One of Rutherford's initial significant contributions was his work on radioactivity. While collaborating with Frederick Soddy at McGill University in Canada, Rutherford categorized two distinct types of radioactive decay, which they termed as alpha and beta radiation. This groundbreaking work unveiled the spontaneous disintegration of atoms and won him the Nobel Prize in Chemistry in 1908, albeit for investigations in the "disintegration of the elements," which is now more associated with physics than chemistry.

In 1911, Rutherford made another revolutionary discovery related to the structure of the atom. Through a series of experiments, often referred to as the "gold foil experiments," he deduced the existence of a concentrated, positively charged nucleus at the center of the atom. This challenged the prevailing "plum pudding" model proposed by J.J. Thomson and marked the inception of the Rutherford or planetary model of the atom. This model conceptualized the atom as having a tiny, dense nucleus surrounded by electrons orbiting in empty space, much like planets orbiting the sun.

Later in his career, at the University of Manchester, Rutherford continued his work on nuclear physics. In 1919, he achieved the artificial disintegration of atomic nuclei, essentially transmutating one element into another, a significant milestone in the realm of atomic research.

Rutherford's numerous contributions extended beyond just his experiments. He mentored and collaborated with other notable scientists, such as Niels Bohr, James Chadwick, and Henry Moseley, facilitating crucial discoveries like the concept of atomic number and the existence of the neutron.

In recognition of his profound impact on science, the element with atomic number 104 was named "rutherfordium" in his honor. Rutherford's work laid the groundwork for modern atomic and nuclear physics, and his discoveries have had lasting implications, from the conceptual understanding of the atom to the practical applications of nuclear energy.

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