Why is this a Desert World?Your planet is a hot (461K), 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: 0.0% (<5% - bone dry, no water cycle)✓ Temperature: 461K (300-500K hot band)✓ Silicon + Iron + Magnesium: 63.9% (>=30% - a real rocky surface)✓ Holds an atmosphere to carry the dust haze
Habitability ScoreUninhabitable
0
Contributing Factors
water0
No water - the recipe has no hydrogen and oxygen to form it
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
temperature15
Extremely hot - hostile to known life forms
magnetic Field100
Magnetic field provides radiation protection
Physical Properties
Mass
0.90x Earth (5.37e+24 kg)
Radius
0.97x Earth (6,151 km)
Surface Gravity
0.97x Earth (9.5 m/s²)
Surface Temperature
461 K (188 °C / 370 °F)
Rotation Period
28.0 hours/day (slower than Earth)
Orbital Environment
Star Type
K-type (Orange)
Distance from Star
0.23 AU (34.4 million km)
Orbital Period
48 days
Atmosphere
Thin, dusty CO₂-nitrogen atmosphere - permanent haze of wind-borne sand
Elemental Composition
Si - Silicon
41.7%
S - Sulfur
12.5%
O - Oxygen
11.1%
Surface Characteristics
Endless dune seas and wind-carved rock under a permanent dust haze - scorching days, freezing nights