Why is this a Desert World?Your planet is a hot (343K), 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: 1.0% (<5% - bone dry, no water cycle)✓ Temperature: 343K (300-500K hot band)✓ Silicon + Iron + Magnesium: 44.0% (>=30% - a real rocky surface)✓ Holds an atmosphere to carry the dust haze
Habitability ScoreMarginal
51
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 Chemistry100
All CHNOPS elements present - building blocks of life
atmosphere70
Nitrogen atmosphere provides protection but not breathable
temperature70
Challenging but potentially habitable temperature
magnetic Field100
Magnetic field provides radiation protection
Physical Properties
Mass
4.10x Earth (2.45e+25 kg)
Radius
1.60x Earth (10,197 km)
Surface Gravity
1.60x Earth (15.7 m/s²)
Surface Temperature
343 K (70 °C / 158 °F)
Rotation Period
32.0 hours/day (slower than Earth)
Orbital Environment
Star Type
F-type (White)
Distance from Star
1.68 AU (251 million km)
Orbital Period
1.91 years
Atmosphere
Thin, dusty CO₂-nitrogen atmosphere - permanent haze of wind-borne sand
Elemental Composition
Fe - Iron
25.0%
O - Oxygen
15.0%
Si - Silicon
15.0%
Surface Characteristics
Endless dune seas and wind-carved rock under a permanent dust haze - scorching days, freezing nights