Mars, the fourth planet from the Sun, is more than just a setting: it is a living character within La Seducción de Nadeah. Its deep valleys, titanic mountains, and rust-hued skies form the backdrop for a struggle for power, identity, and hope. Explore its geography, its emerging culture, and its pivotal role in the destiny of humanity.
Interactive Map
Navigate the highly detailed 3D map of Mars to discover key locations from La Seducción de Nadeah, each linked to crucial moments in the story.
Mapa interactivo de Marte
Explora Marte en 3D con sus lunas y rasgos geográficos destacados dentro del universo de Comet Surfer.
The Moons of Mars
Deimos and Phobos, silent witnesses to Mars’s past, orbit the planet along trajectories as unique as the history surrounding them. Here, you will discover their behavior as seen from the surface, their orbits, and their presence in the narrative.
Deimos
Modelo 3D de Deimos
Explora Deimos, una de las lunas de Marte, mediante un modelo tridimensional interactivo. Observa su forma irregular, superficie y características en detalle.
- Average diameter: ~12.4 km
- Average distance to Mars: ~23,460 km
- Orbital period: 30 hours and 18 minutes
- Apparent motion: Rises in the east and sets in the west
Deimos—”Terror”—is the smallest and most distant of the two. Unlike Phobos, its orbit is so slow that it barely outpaces Martian rotation; consequently, from the surface, it appears to drift calmly across the sky.
Its appearance is faint—even from Mars—and many colonists liken it to a wandering star. It takes over thirty hours to traverse the Martian sky, ushering in long, melancholic nights.
Martian poets have dubbed it the “lantern of the solitary,” and for some, it symbolizes introspection and emotional distance in times of conflict.
Fobos
Modelo 3D de Phobos
Explora Phobos, la mayor luna de Marte, mediante un modelo tridimensional interactivo. Analiza su superficie craterizada y su morfología irregular en detalle.
- Average diameter: ~22.2 km
- Average distance from Mars: ~6,000 km
- Orbital period: 7 hours and 39 minutes
- Apparent motion: Rises in the west and sets in the east
Phobos—whose name means “fear”—is the larger and closer of the two moons. Its orbit is so low and fast that it completes a full revolution around Mars in just seven and a half hours—faster than the rotation of the planet itself.
From the surface, Phobos appears as an irregular rock hurtling across the sky at high speed, rising above the western horizon and setting in the east—defying our terrestrial intuition.
Its proximity and velocity make it an object of study and speculation within the world of La Seducción de Nadeah. Some colonists regard it as a warning sign: ever-present, ever-vigilant.
Martian Calendar
Time on Mars flows differently than on Earth. Martian civilization within the Comet Surfer universe uses the Darian-Utopian calendar system, a scientifically inspired framework designed specifically around the orbital and seasonal rhythms of the Red Planet.
If you would like to fully understand how time is organized on Mars, explore the dedicated Darian-Utopian Martian Calendar page and discover the scientific and cultural foundations of Martian civilization.
Curious about your Martian birthday or the release date of your favorite movie on Mars? Use the simulator below to convert Earth dates into Martian sols, mirs, and seasons.
3D Martian Topographic Viewer
Modelo 3D de Marte
Explora Marte en tres dimensiones utilizando datos topográficos basados en imágenes del USGS.
In this interactive image, the major geographical features of Mars—ranging from the imposing Valles Marineris canyon to the Olympus Mons volcano—are displayed using a color scale that indicates relative elevation. Warm tones (reds and yellows) depict elevated regions, while cool tones (blues and greens) correspond to lower areas. Elevations are measured relative to the Martian datum—an equipotential reference surface analogous to sea level on Earth—which is used to standardize altitude measurements on a planet that lacks oceans. This tool allows for the exploration of Martian topography with both precision and depth.
For those wishing to explore this origin—the ultimate context for everything recounted here—the following external reference is recommended:
👉 The University of Mars — Encyclopedia