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Xha’Ruun

Chapter 3: Planet Thexar

Théxar with clouds, oceans, mountain ranges and two moons
Théxar from orbit: oceans, three continents and two moons.

"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.

Landscape of Théxar

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

Deep rocks in a laboratory: core samples and instruments for studying the interior.
Deep rocks in a laboratory: core samples and instruments for studying the interior.

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:

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:

  1. Scattering by air molecules and suspended aerosols
  2. Presence of H₂S (scatters differently)
  3. 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:

  1. Slow planetary rotation (27.3 h)
  2. Active tectonics (CO₂ and SO₂ emissions)
  3. Ocean currents
  4. Axial tilt (14.2°)

Circulation cells:

Thexar has a 6-cell model of atmospheric circulation:

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:

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:

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

Théxar from orbit: oceans, continents and cloud systems.
Théxar from orbit: oceans, continents and cloud systems.

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:

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
Aurora over the nightside of Théxar.
Aurora over the nightside of Théxar.

3.6.2 Radiation Belt

Thexar has two radiation belts:

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

  1. Thexar is a geologically active planet with a fully differentiated core, plate tectonics (7 main plates), and volcanism
  2. Atmosphere is rich in CO₂ (0.8%) — this is compensation for low insolation, not a greenhouse catastrophe
  3. The sky is golden-orange due to atmospheric composition and stellar spectrum
  4. Hydrosphere: 2 oceans, 5 seas, 67% of surface covered by water
  5. 3 continents: Kharak (65.721 million km²), Rhuval (42.249 million km²), Vexar (37.555 million km²)
  6. Magnetosphere is moderate (42 µT), atmosphere compensates for its weakening
  7. Rich mineral resources — especially Fe, Cu, Th, Pt on Kharak
  8. Energy: 62% — thermonuclear, solar and hydroelectric power

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