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Xha’Ruun

Thexar-VIII: The-Xar-Ak — Sha-El 08: Thar-Vokh Ak-El — Geological Map

"Stones remember what water has forgotten. The layers are the pages of a book written long before us. To read them is to know where we came from." — Guild of Geologists, +2,500 Y.E.


Ruun-ak rass: → rhu [Thexar-I, Ruun 12, "Geological Evolution"]; → rhu [Thexar-I, Ruun 13, "Continents"]; → rhu [Thexar-VIII, Sha-El 10, "Resource Map"]; → rhu [Thexar-I, Ruun 27, "Geodesy"]. Mor-ven: The geological map of Théxar records the long geological history across 10 lithospheric plates (four continental, five oceanic and one mixed). Kharak preserves the ancient craton, Rhuval hosts active volcanism, Vexar bears alkaline REE massifs, while the Thalas ridge spreads and the Thash Trench reaches 9,847 m.


Veins in dark rock
Veins in dark rock

08.1 Tectonic Plates

Théxar has 10 lithospheric plates, of which four are continental, five oceanic and one mixed.

Plate Area (million mo²) Speed (pa/cycle)
Kharak 1.8 2.4
Rhuval 1.1 2.1
Vexar 0.9 1.7
Thalas 2.0 3.7
Gharra 1.9 3.3
Koss 0.7 1.4
Irkhen 0.5 2.2
Serrin 0.3 0.9
Thel 0.2 0.6
Polar 0.3 1.2

Plate boundaries:

08.2 Geological Provinces of Kharak

08.2.1 Kharak Craton

Ancient continental core, 5.5 billion cycles old.

Parameter Value
Composition Granites, gneisses, greenstone belts
Tectonic activity Low

08.2.2 Khar-Tor Ridge

Mountain chain along the western coast, formed by Thalas plate subduction.

Parameter Value
Length 976 mo
Width 122–244 mo
Highest point Mt. Verksan (9,537 sha)
Age 2.5 billion cycles

08.2.3 Central Plain

Sedimentary basin filled with alluvial deposits.

Parameter Value
Sediment thickness Up to 4.9 mo
Age 500 million cycles

08.2.4 Shan Desert

Southeast plateau in the rain shadow of Khar-Tor.

Parameter Value
Height 610–1,220 sha
Type Stony desert (hamada)

08.3 Geological Provinces of Rhuval

08.3.1 Raal Plateau

Central highlands formed by mafic intrusions.

Parameter Value
Height 1,463–3,415 sha
Composition Layered mafic intrusions
Resources Pt, Cr, Mn

08.3.2 Irkhen Chain

Volcanic ridge along the northern coast.

Parameter Value
Length 488 mo
Number of volcanoes 48 (12 active)
Highest point Mt. Moraat (7,915 sha)
Last eruption +3,890 Y.E.

08.4 Geological Provinces of Vexar

08.4.1 Sharrus Chain

Central fold belt massif.

Parameter Value
Length 366 mo
Highest point Mt. Sharrus (7,451 sha)
Type Fold belt

08.4.2 Alkaline Massifs

Unique REE-bearing formations.

Parameter Value
Age 1.8 billion cycles
Resources La, Ce, Nd, Eu

08.5 Oceanic Geology

08.5.1 Thalas Mid-Ocean Ridge

Spreading zone in the center of the Thalas Ocean.

Parameter Value
Length 2,439 mo
Width 122 mo
Spreading rate 3.7 pa/cycle
Ridge-crest depth 2,439 sha

08.5.2 Thash Trench

Deepest point of Théxar, in the Gharra Ocean.

Parameter Value
Depth 9,847 m
Length 366 mo
Width 61 mo
Water temperature 2.0°X

08.6 Seismic Map

Average annual earthquake counts by region:

Region M > 5.0 M > 6.0 M > 7.0
Khar-Tor Ridge 12 2 0.2
Irkhen Chain (Rhuval) 18 4 0.5
Thalas Rift 25 8 1.0
Kharak Craton 2 0.1 <0.01
Vexar 6 1 0.1

08.7 Geochronological Map

Era Age (billion cycles) Rocks Distribution
Chaotic 6.50–6.00 Primary basalts Ubiquitous (deep)
Archean 6.00–5.00 Gneisses, granites Continental cores
Prototectonic 5.00–3.50 Greenstone belts Kharak, Rhuval
Rift 3.50–2.00 Sedimentary basins All continents
Biogeological 2.00–0.58 Limestones, coals Coasts
Modern 0.58–present Alluvium, glacial Plains, poles

Ruun Ven

  1. Théxar comprises 10 lithospheric plates — 3 continental (Kharak, Rhuval, Vexar) and 7 oceanic/mixed/polar.
  2. Kharak preserves the oldest craton at 5.5 billion cycles; Rhuval remains volcanically active with 48 Irkhen volcanoes (12 active).
  3. Khar-Tor subduction lifts Mt. Verksan to 9,537 sha; Sharrus and Moraat mark Vexar and Rhuval highs.
  4. The Thash Trench in the Gharra Ocean plunges to 9,847 m — the planet's deepest point.
  5. Seismicity concentrates on plate boundaries: Thalas Rift leads with 25 M>5 events/cycle; Kharak Craton is quietest.
  6. Six geochronological eras describe the sequence, from Chaotic basalts to Modern alluvium.