Chapter 3: Planet Thexar

"She is not the largest, not the richest, not the oldest. But she is the only one who gave birth to us. And there is no other like her in all the galaxy." — From "Hymn to Thexar," classical work of the Flourishing Era
Related sections: see [Ch.01, "Cosmology"], see [Ch.02, "Star System"], see [Ch.04, "Biochemistry of Life"]
Introduction
Thexar (/ˈθɛk.sɑr/ — "earth-mother" in ancient Xha'Ruun) is the third planet of the Khar'Vex system and the only known body in the galaxy where life arose and developed. It is a world of astonishing geological diversity: from scorching equatorial deserts to polar ice caps; from the deepest ocean trenches to mountain peaks exceeding 9,500 sha.
From a planetological perspective, Thexar is distinguished by longer days, a more ancient and calm geological regime, a different atmospheric composition, and two small moons. These features shaped the unique evolutionary trajectory of local life — and, ultimately, intelligence.

Fig. 3.0. Sunset on Théxar: mountains, ocean, and both moons — Serrin and Thel.
3.1 Origin and Geological Evolution
3.1.1 Formation
Thexar formed ~6.5 billion cycles ago in the protoplanetary disk of Khar'Vex through accretion of planetesimals enriched with heavy elements (protoplanetary cloud metallicity: [Fe/H] = +0.12).
| Stage | Time (billion cycles ago) | Event |
|---|---|---|
| 1 | 6.50 ± 0.02 | Accretion of planetesimals, formation of proto-Thexar |
| 2 | 6.48 ± 0.01 | Core differentiation: Fe-Ni sinks to center |
| 3 | 6.47–6.40 | Period of intense bombardment, mass growth |
| 4 | 6.40–6.30 | Formation of primary crust, surface cooling |
| 5 | 6.30–6.00 | Outgassing of volatiles, formation of primary atmosphere and oceans |
| 6 | 6.00–5.50 | First tectonic cycle, emergence of proto-continents |
| 7 | 5.50 | Formation of the largest impact basin (Sea of Gharra) |
| 8 | 5.50–4.00 | Crust stabilization, tectonic regime transitions to modern |
| 9 | 4.00–3.80 | Oxygen catastrophe (beginning of photosynthesis) |
| 10 | 3.80–present | Modern tectonic regime |
3.1.2 Internal Structure

PROFILE: Internal Structure of Thexar
Layer Composition State T (°X) Continental crust Granite, basalt Solid 19…534 Oceanic crust Basalt, gabbro Solid 45…317 Upper mantle Peridotite (olivine+pyroxene) Solid 534…698 Asthenosphere Partially molten peridotite Viscous 698…806 Lower mantle Perovskite, ferropericlase Solid (plastic) 806…2,057 Outer core Fe (85%), Ni (10%), S, O (5%) Liquid 2,057…2,710 Inner core Fe (90%), Ni (8%), elements Solid 2,710…2,873
3.1.3 Plate Tectonics
Thexar has active plate tectonics — the movement of lithospheric plates across the asthenosphere surface. This process is a key factor in the carbon cycle and long-term climate stability.
TABLE 3.1: Lithospheric Plates of Thexar
Plate Type Direction Speed (sha/year) Thalas (oceanic) Oceanic NW 3.9 Kharrak (continental) Continental NE 3.4 Ruval (continental) Continental S 5.0 Gharra (oceanic) Oceanic SE 3.0 Vexar (continental) Continental W 2.3 Northern (oceanic) Oceanic E 6.5 Marginal (6 small) Mixed Various 0.6–8.5
Plate boundary types:
- Divergent (spreading): mid-ocean ridges — 4 main (Thalass, Southern, Western, Northern)
- Convergent (colliding): subduction zones — 6 active (along the edges of continent Kharak and Rhuval)
- Transform (sliding): 4 major faults (largest — Thash Fault, ~3,900 mo long)
KEY FACT
The average speed of tectonic movements on Thexar is 2.8 sha/year. This is due to the slow cooling of the mantle (lower mass but effective insulation). Slow tectonics means longer geological cycles — in particular, the carbon cycle takes ~120 million years.
3.2 Atmosphere
3.2.1 Composition and Structure
PROFILE: Atmosphere of Thexar
Parameter Value Surface pressure 1 tyazh Average surface temperature 51.6°X Temperature range 19°X … 75°X Average molecular mass 28.8 g/mol Scale height 10,000 sha Transparency (visible range) 0.72
Chemical composition (dry air, at surface):
| Gas | Formula | Fraction | Note |
|---|---|---|---|
| Nitrogen | N₂ | 71.8% | Main component |
| Oxygen | O₂ | 22.6% | High content |
| Argon | Ar | 2.9% | — |
| Carbon dioxide | CO₂ | 0.8% | Elevated |
| Water vapor | H₂O | 0.5–2.0% | Variable |
| Neon | Ne | 0.05% | — |
| Methane | CH₄ | 0.0003% | Biogenic |
| Hydrogen sulfide | H₂S | 0.0008% | Biogenic |
KEY FACT
At a stellar luminosity of 0.41 L☉ and a distance of 0.63209 AU, the flux at Théxar’s orbit is about 1.026 times Earth’s solar constant. Surface temperature also depends on reflection, atmosphere, clouds and ocean heat transport.
Vertical structure of the atmosphere:
| Layer | Height (sha) | Thexar Feature | T at boundary |
|---|---|---|---|
| Troposphere | 0–13,400 | ✅ | 19°X |
| Stratosphere | 13,400–54,900 | Ozone layer thinner (by 30%) | 17°X |
| Mesosphere | 54,900–103,700 | H₂S glow (twilight) | 6.6°X |
| Thermosphere | 103,700–426,800 | Strong variations | 208…589°X |
| Exosphere | >426,800 | — | — |
3.2.2 Sky Color
The color of Thexar's sky is one of its most striking visual features. Due to:
- Scattering by air molecules and suspended aerosols
- Presence of H₂S (scatters differently)
- Orange-yellow spectrum of Khar'Vex (peak ~570 nm)
— the sky of Thexar has a characteristic golden-bronze hue, transitioning to orange near the horizon and rose-purple closer to the zenith. Sunsets are deep orange with red flashes.
| Sky | Color | Reason |
|---|---|---|
| Noon | Golden-bronze | Molecular and aerosol scattering + stellar spectrum |
| Sunset | Deep red | Long path through H₂S layer |
| Twilight | Purple | Atmospheric glow |
3.2.3 Weather and Climate
Global atmospheric circulation is determined by:
- Slow planetary rotation (27.3 h)
- Active tectonics (CO₂ and SO₂ emissions)
- Ocean currents
- Axial tilt (14.2°)
Circulation cells:
Thexar has a 6-cell model of atmospheric circulation:
- Kharrak cell (equatorial): 0°–28° — ascending motion, abundant precipitation
- Tor cell (temperate): 28°–55° — descending motion, dry zones
- Thela cell (polar): 55°–90° — weak, cold
Due to slow rotation, the cells are wider and weaker — trade winds and monsoons are less pronounced, but winds are generally more predictable.
3.2.4 Hazardous Phenomena
| Phenomenon | Frequency | Region |
|---|---|---|
| Tropical cyclones | 20–35/year | Oceans, 8°–25° latitude |
| Tornadoes | ~500/year | Plains of Kharak |
| Dust storms | Frequent | Deserts of Kharak, Vexar |
| Volcanic winters | 1 per 5–20 thousand years | Global |
| Lightning | ~1.2 billion/year | Global |
3.3 Hydrosphere
3.3.1 Oceans
PROFILE: Oceans of Thexar
Parameter Thalas (Northern) Gharra (Southern) Average depth 4,488 sha 3,841 sha Maximum depth 10,268 sha (Khar-Tor Trench) 12,009 sha (Thash Deep) Average surface T 55°X (eq.) / 43°X (pol.) 53°X (eq.) / 43°X (pol.) Salinity 3.5% 3.3% pH 7.9–8.1 7.8–8.2
Current system:
Thexar possesses a complex system of ocean currents:
- Tor Warm Current — transports warm water from the equatorial zone along the continent of Kharak toward the polar region
- Thash Cold Current — return current along the continent of Rhuval
- Gharra Circumpolar Current — circles the southern continent of Vexar
3.3.2 Seas
| Name | Area | Average depth | Connection to ocean | Feature |
|---|---|---|---|---|
| Serrin Sea | 0.34 million mo² | 1,732 sha | Thalas | Inland, Kharak |
| Verksan Sea | 0.28 million mo² | 1,085 sha | Thalas | Shelf, Kharak |
| Gulf of Thash | 0.19 million mo² | 2,683 sha | Gharra | Deep water |
| Irkhen Sea | 0.13 million mo² | 780 sha | Gharra | Inter-island |
| Raal Sea | 0.12 million mo² | 463 sha | Thalas | Semi-enclosed |
3.3.3 Rivers and Lakes
The three continents of Thexar are crossed by an extensive river network. The largest river systems:
| River | Length (mo) | Continent | Flows into | Note |
|---|---|---|---|---|
| Khar-Tor | 870 | Kharak | Serrin Sea | Sacred river |
| Thash-Ven | 776 | Rhuval | Gulf of Thash | Hydroelectric power |
| Sharrus | 638 | Vexar | Gharra | Largest on Vexar |
| Moraat | 559 | Rhuval | Irkhen Sea | Navigable |
| Irkhen | 443 | Kharak | Irkhen Sea (via strait) | Provincial border |
The largest lake is the Khar Inland Sea (lake on Kharak, area 5,870 mo²), a remnant of an ancient inland sea.
3.4 Climate Zones
TABLE 3.4: Climate Zones of Thexar
Zone Latitudes Average T (°X) Precipitation Characteristic biome Equatorial 0°–12° 60…68 2,000–4,500 mm/year Humid jungles Tropical 12°–28° 55…66 800–2,000 mm/year Savannas, monsoon forests Subtropical 28°–38° 49…58 400–900 mm/year Mediterranean type Temperate 38°–54° 44…55 500–1,500 mm/year Broadleaf and mixed forests Subpolar 54°–66° 39…49 200–600 mm/year Coniferous forests, tundra Polar 66°–90° 19…42 50–200 mm/year Ice caps, desert
3.4.1 Equatorial Zone
Hot and humid belt encompassing the central regions of Thexar. Characterized by:
- Average annual temperature +63.6°X (daily range: 8–12°C → 4–7°X)
- Two rainy seasons (after equinoxes)
- Dense multi-tiered jungles with high biomass
- Red soils (iron oxides — "ferralite")
- Biodiversity: ~70% of all species on the planet
3.4.2 Polar Regions
Due to the axial tilt (14.2°), the polar regions of Thexar are covered by a permanent ice sheet.
| Region | Ice area | Thickness | Temperature (average) |
|---|---|---|---|
| Northern polar cap | 0.46 million mo² | 976–2,927 sha | 45°X |
| Southern polar cap | 0.53 million mo² | 1,463–3,780 sha | 30°X |
3.5 Geography
3.5.1 Overview

3.5.2 Continent Kharak
Kharak (from the root khar- — "light," "star") is the largest continent, located in the Northern Hemisphere.
PROFILE: Kharak
Parameter Value Area 65.721 million km² Population ~1.1 billion (39% of planet) Largest city Khar-Vexar (18.6 million) Highest point Mt. Verksan (9,537 sha) Largest river Khar-Tor (870 mo) Climate zones Equatorial — Polar Natural resources Fe, Cu, U, Pt, P, H₂S sources
Regions of Kharak:
| Region | Area | Type | Characteristic |
|---|---|---|---|
| Central Plain | 0.34 million mo² | Plain | Fertile, "breadbasket" of Kharak |
| Khar-Tor Range | 0.12 million mo² | Mountain chain | Highest peaks on the planet |
| Shan Desert | 0.14 million mo² | Desert | Rocky, rich in metals |
| Serrin Plateau | 0.07 million mo² | Plateau | Basaltic, ancient |
| Northern Taiga | 0.17 million mo² | Forest zone | Coniferous forests |
| Khar-Tor Delta | 0.03 million mo² | Delta | Oldest settlements |
3.5.3 Continent Rhuval
Rhuval (from the root rhuun — "great," "people") is the second largest continent, mostly in the Southern Hemisphere.
PROFILE: Rhuval
Parameter Value Area 42.249 million km² Population ~0.9 billion (32% of planet) Largest city Ven-Khal (12.4 million) Highest point Mt. Moraat (7,915 sha) Largest river Thash-Ven (776 mo) Climate Tropical — Subpolar Natural resources Au, Ag, Zn, oil, gas
Regions of Rhuval:
- Raal Plateau — highland plateau, mining center
- Thash-Ven Valley — densely populated agricultural area
- Irkhen Coast — resort zone, ancient ports
3.5.4 Continent Vexar
Vexar (from the root vex- — "to give," "to create") is the smallest of the three continents, the most isolated.
PROFILE: Vexar
Parameter Value Area 37.555 million km² Population ~0.5 billion (18% of planet) Largest city Shan-En (7.8 million) Highest point Mt. Sharrus (7,451 sha) Largest river Sharrus (638 mo) Climate Subtropical — Subpolar Natural resources Ti, Mn, Cr, Co, rare earths
3.5.5 Island Territories
| Archipelago / Island | Area | Belongs to | Feature |
|---|---|---|---|
| Khal-Tor | 49,586 mo² | Kharak | Volcanic |
| Sha-enn | 37,190 mo² | Rhuval | Largest island of Rhuval |
| Serrin-Ur | 24,793 mo² | Vexar | Nature reserve |
| Irkhen (archipelago) | 16,529 mo² (total) | Between Kharak/Rhuval | Disputed territories (historically) |
3.6 Magnetosphere and Radiation Belt
3.6.1 Magnetic Field
Thexar possesses an active magnetic field, generated by the dynamo effect in the liquid outer core.
| Parameter | Value |
|---|---|
| Surface strength | 42 µT |
| Magnetic dipole moment | 5.8 × 10²² A·m² |
| Tilt relative to rotation axis | 9.8° |
| Reversal period (average) | ~350,000 years |

3.6.2 Radiation Belt
Thexar has two radiation belts:
- Inner belt: altitude 1,463–5,488 sha, consists of high-energy protons
- Outer belt: altitude 9,756–21,951 sha, consists of electrons
KEY FACT
The magnetosphere is one of the reasons the Xha'Ruun developed increased radiation resistance (see [Ch.05, "Physiology"]). Evolution "got used" to a somewhat higher level of cosmic radiation penetrating through the weakened magnetosphere.
3.7 Biomes and Key Ecosystems
3.7.1 Biome Map
| Biome | Area | Characteristic vegetation | Characteristic fauna |
|---|---|---|---|
| Humid equatorial jungles | 14% | Six-tier forests (height up to 98 sha) | Arboreal hexapods, flying predators |
| Savannas and woodlands | 12% | Grass (height up to 3.7 sha), umbrella trees | Herding herbivores, burrowing predators |
| Deserts (rocky and sandy) | 8% | Cactus-like, lichens | Nocturnal hexapods, reptiloids |
| Broadleaf forests | 16% | Silicon-carbon trees | Species diversity |
| Coniferous/boreal forests | 14% | Needle-leaf, scale-leaf | Large herbivores |
| Tundra | 6% | Mosses, lichens, dwarf shrubs | Migrating herds |
| Ice sheets | 8% | None (algae on ice) | Marine, sub-ice |
| Aquatic ecosystems | 22% | Phytoplankton, algae | Fish-like, giant filter feeders |
3.7.2 Unique Ecosystems
Deep-sea hydrothermal vents — in the Gharra Ocean, at depths of 4,268–9,146 sha, ecosystems based on H₂S chemosynthesis have formed around 6 hydrothermal vent fields (see [Ch.04, "Biochemistry"]). These "oases" of life contain endemic species found nowhere else on the planet.
Cave ecosystems — in the limestone massifs of Kharak and Vexar, large subterranean ecosystems have been discovered (total area ~9,917 mo²), isolated from the surface for millions of years. Many species are blind, depigmented.
RELATION
The biodiversity of Thexar and key evolutionary adaptations are described in detail in see [Ch.04, "Biochemistry"] and see [Ch.05, "Xha'Ruun Species"].
3.8 Natural Resources
TABLE 3.8: Mineral Resources of Thexar
Resource Reserves Main region Use Iron 1.27 × 10¹¹ ru Kharak (Khar-Tor Range) Industry Copper 1.94 × 10⁹ ru Rhuval (Raal Plateau) Electrical, alloys Uranium 5.09 × 10⁶ ru Kharak (Shan Desert) Energy (historically) Thorium 2.48 × 10⁷ ru Vexar (coast) Thermonuclear energy Platinum group 1.70 × 10⁵ ru Kharak (Khar-Tor) Catalysts, electronics Rare earths 5.58 × 10⁷ ru Vexar Electronics, superconductors Gold 9.09 × 10⁴ ru Rhuval (Thash-Ven) Electronics, jewelry Phosphates 5.15 × 10¹⁰ ru Kharak (sedimentary) Fertilizers
Energy resources:
| Type | Potential | Developed | Share in energy balance |
|---|---|---|---|
| Thermonuclear | Unlimited | ~2.4 × 10¹⁶ sv/year | 62% |
| Solar | ~1.1 × 10¹⁷ sv/year | ~7.9 × 10¹⁵ sv/year | 20% |
| Hydroelectric | ~1.5 × 10¹⁶ sv/year | ~3.4 × 10¹⁵ sv/year | 9% |
| Geothermal | ~5.1 × 10¹⁵ sv/year | ~1.8 × 10¹⁵ sv/year | 5% |
| Wind | ~1.2 × 10¹⁶ sv/year | ~1.6 × 10¹⁵ sv/year | 4% |
3.9 Natural Threats
3.9.1 Earthquakes
Due to active tectonics, Thexar experiences ~15,000 earthquakes of magnitude > 2.0 annually.
| Zone | Activity | Max. magnitude | Risk to population |
|---|---|---|---|
| Khar-Tor subduction zone (Kharak) | High | 8.7 | High |
| Thash Fault (Rhuval) | Moderate | 7.4 | Moderate |
| Vexar deep fault | Low | 5.8 | Low |
| Serrin transform fault | Moderate | 6.9 | Moderate |
3.9.2 Volcanism
Thexar has ~180 active volcanoes, of which ~30 are supervolcanoes (capable of VEI-8 eruptions).
| Volcano | Height | Last eruption | Type |
|---|---|---|---|
| Khar-Tor (Kharak) | 9,537 sha | 1,280 y.E.U. | Stratovolcano |
| Moraat (Rhuval) | 7,915 sha | 230 y.E.U. | Shield |
| Tor-Ven (Kharak) | 6,354 sha | ~8,000 years ago | Supervolcano (caldera) |
3.9.3 Impact Events
Thexar is subjected to asteroid and comet impacts with a frequency of ~1 major event (crater >10 km) every 500,000 years. Planetary defense system — see [Ch.09, "Planetary Defense"].
3.10 Thexar in Culture
QUOTE
"Three continents — three characters. Kharak — old, wealthy, wise. Rhuval — young, passionate, warlike. Vexar — detached, mysterious, proud. So say the geographers. But the inhabitants of each are certain that their continent is the best. And each is right in their own way."
— "Geography for Travelers," popular edition, +2,500 y.E.U.
In Xha'Ruun culture, Thexar is perceived as a living entity — the "Great Mother." The oceans are associated with the circulatory system, the mountains with the skeleton, the winds with breath. This metaphor is deeply rooted in the language: the verb "to breathe" (shal-ven) and "to blow (of wind)" (shal-thar) share a common root.
RELATION
The attitude toward the planet as a living being is not only a poetic metaphor but also the foundation of Xha'Ruun ecological ethics (see [Ch.08, "Culture"]), as well as an element of religious worldview (see [Ch.10, "Mythology"]).
Chapter 3 Summary
Key Takeaways
- Thexar is a geologically active planet with a fully differentiated core, plate tectonics (7 main plates), and volcanism
- Atmosphere is rich in CO₂ (0.8%) — this is compensation for low insolation, not a greenhouse catastrophe
- The sky is golden-orange due to atmospheric composition and stellar spectrum
- Hydrosphere: 2 oceans, 5 seas, 67% of surface covered by water
- 3 continents: Kharak (65.721 million km²), Rhuval (42.249 million km²), Vexar (37.555 million km²)
- Magnetosphere is moderate (42 µT), atmosphere compensates for its weakening
- Rich mineral resources — especially Fe, Cu, Th, Pt on Kharak
- Energy: 62% — thermonuclear, solar and hydroelectric power
Links to Other Chapters
- see [Ch.02, "Star System"] — position of Thexar in the system and habitable zone
- see [Ch.04, "Biochemistry"] — how Thexar's geochemistry shaped the biochemistry of life
- see [Ch.05, "Xha'Ruun Species"] — evolutionary adaptations to the environment
- see [Ch.09, "Technologies"] — use of geothermal energy and resources
- see [APP:physical-ref] — complete planet profile