Why is this a Desert World?Your planet is a hot (350K), bone-dry silicate rock that kept its atmosphere - with no water cycle to wash the air, wind lofts a permanent dust veil over endless dune seas.
Desert worlds are the Tatooine/Arrakis archetype: enough rock to build a solid surface, enough air to carry dust, and too little hydrogen for oceans or rain. Heat bakes out any trace moisture, so nothing interrupts the wind's work - dune seas, wind-carved rock, scorching days.
Classification Criteria:
✓ Hydrogen: 4.8% (<5% - bone dry, no water cycle)✓ Temperature: 350K (300-500K hot band)✓ Silicon + Iron + Magnesium: 33.3% (>=30% - a real rocky surface)✓ Holds an atmosphere to carry the dust haze
Habitability ScoreExtremely Harsh
30
Contributing Factors
water20
Very dry - minimal water
geology90
Active geology recycles nutrients and drives carbon cycle
rotation100
Optimal rotation period - balanced day/night cycle, moderate weather, and good heat distribution
Organic Chemistry20
Limited organic chemistry potential
atmosphere70
Nitrogen atmosphere provides protection but not breathable
temperature40
Extreme temperature - very difficult for life
magnetic Field100
Magnetic field provides radiation protection
Physical Properties
Mass
1.00x Earth (5.97e+24 kg)
Radius
1.00x Earth (6,371 km)
Surface Gravity
1.00x Earth (9.8 m/s²)
Surface Temperature
350 K (77 °C / 171 °F)
Rotation Period
24.0 hours/day
Orbital Environment
Star Type
G-type (Yellow (Sun-like))
Distance from Star
0.63 AU (94.2 million km)
Orbital Period
183 days
Atmosphere
Thin, dusty CO₂-nitrogen atmosphere - permanent haze of wind-borne sand
Elemental Composition
N - Nitrogen
23.8%
O - Oxygen
14.3%
Fe - Iron
14.3%
Surface Characteristics
Endless dune seas and wind-carved rock under a permanent dust haze - scorching days, freezing nights