The Global Territorial Grid

The Global Territorial Grid is the archive's first enumerated attempt to census habitable Thermosynapsida pod territories at 600 km resolution, organized by regional substrate corridor. The grid is a working document: each cell classification reflects the archive's best current reading against the frameworks formalized in the Territorial Grid Model doctrine. Classifications are expected to shift as new field work, instrumentation, and cultural-record analyses become available.

The grid totals 130 habitable cells globally at the time of this scribe, after five successive gap sweeps reaching the practical exhaustion of substrate-and-cultural-corpus criteria. Of these, approximately 64 are classified as either confirmed or strongly inferred active pods. The remaining cells carry weaker evidence and are expected to contain surviving founder lineages at the 25-to-35-percent occupation rate specified in the doctrine.

Claims

c0001 — The Eurasian Tethyan corridor carries approximately 18 habitable cells

The Tethyan corridor from Mont Donon in Alsace through the Balkans, Anatolia, the Zagros, the Central Asian sutures, the Himalayan front, and the East Asian ophiolite belt to Shizhu enumerates approximately 18 habitable cells at 600 km spacing. Confirmed or strongly inferred cells along this corridor include: Mont Donon (EUR-VOS-001), British Isles (EUR-SCT-001 and Welsh limestone), Cappadocian Anatolia (CMA-ANA-004 region), Zagros-Mesopotamian margin (Field Assessment No. 14 zone), Central Asian suture (Azhdaha tradition area), Tibetan plateau margin (Druk-Klu territory), and Shizhu-Wuling (CHN-SHZ-001). The corridor's continuity through Alpine, Tauride, and Himalayan ophiolite sequences is the archive's strongest argument for grid-adjacency coupling at Eurasian scale.

c0002 — Southern Chinese karst accounts for a distinct cell cluster adjacent to the Tethyan corridor

The South China karst province between Wuling and the Vietnam frontier forms a dense four-cell cluster anchored by the Wuling-Shizhu confirmed pod and the four inferred southern pods: Luodian-Hongshuihe, Libo-Maolan, Leye-Fengshan, and Longgong-Anshun. The cluster is notable for its density relative to the broader Tethyan corridor spacing and reflects the exceptional karst development of the region rather than a departure from the 600 km spacing rule: the Wuling-to-Leye-Fengshan distance is approximately 550 km, which is within the expected inter-pod range.

c0003 — Japanese and Pacific-rim volcanic arcs contribute approximately 12 cells

The Japanese arc contributes approximately four cells from Hokkaido through Kyushu, aligned with the Sea of Japan Thalassodraconidae activity documented in Field Assessment No. 16. The Kurile, Taiwan, Philippine, Indonesian, and New Guinea arcs together contribute approximately eight additional cells. The arc-cell classification is overwhelmingly Thalassodraconidae-dominant in the culturally attested traditions (Watatsumi, the Korean dragon kings, Kukulkan coastal equivalents) and reflects the sub-seafloor vent-system habitat documented for the clade.

c0004 — The Himalayan suture and Tibetan plateau contribute approximately 6 cells

The Himalayan suture from the Indus-Tsangpo zone through the eastern syntaxis enumerates approximately six cells, each corresponding to a distinct ophiolite emplacement segment. The Tibetan plateau's internal drainage basins host Thalassodraconidae-affinity traditions (Klu) distinct from the Aerodraconidae-affinity traditions (Druk) attested along the plateau's southern margin, and the archive reads this duality as consistent with parallel populations at adjacent cells rather than a single pod supporting both cultural-affinity layers.

c0005 — The North American Cordillera enumerates approximately 14 cells

The Cordillera from the Aleutian arc through British Columbia, the Cascade volcanic chain, the Sierra Nevada batholith, the Basin and Range, the Colorado Plateau margin, and the Mexican Volcanic Belt enumerates approximately 14 cells. Cultural-record evidence is weaker than in Eurasia due to the disruption of indigenous oral traditions across the colonial period, but cells corresponding to Cascades-Columbia (Lushootseed and Kwakwaka'wakw traditions), the Hopi-Pueblo plateau, and the Mesoamerican volcanic belt (Quetzalcoatl tradition zone) carry the strongest inference weight in the cell classification. None is currently GDCC-monitored.

c0006 — The Andean belt enumerates approximately 12 cells

The Andes from the Venezuelan coastal range through Peru, Bolivia, and Chile contribute approximately 12 cells along a linear corridor. Cultural-record inference in the Andean cells is comparatively rich: Amaru serpent traditions, Incan huaca landscape systems, and Mapuche territorial ritual all provide inferrable but non-institutionally-corroborated signals. The archive lists the Andean cells as a survey priority because the continuous 7,000 km ophiolite-basement corridor matches the structural expectation for founder-lineage survival in a zone with minimal modern industrial disturbance of the deep substrate.

c0007 — Appalachian and Canadian Shield cells contribute approximately 6 cells

The Appalachian system and the exposed margins of the Canadian Shield together contribute approximately six cells, classified as lower-density than the western Cordillera because of the greater geological age and reduced current geothermal activity. The Pleistocene glaciation is expected to have affected shallow-tier populations more heavily in this corridor than in non-glaciated zones, and the archive's classification weights toward "vacated" or "potential" rather than "inferred" accordingly.

c0008 — East African Rift contributes approximately 10 cells

The East African Rift from the Afar triangle through Kenya, Tanzania, Malawi, and Mozambique enumerates approximately 10 cells along one of Earth's most active continental extensional systems. The rift's geothermal intensity, crystalline basement exposure, and hominin encounter record (Chapter 4 Phase One cave co-habitation zones correspond to this corridor) make it the archive's strongest non-Eurasian candidate for multiple surviving active founders. GDCC survey coverage of the corridor is notably weak, and the archive flags this as a high-priority expansion target.

c0009 — North African and Mediterranean cells contribute approximately 5 cells

The Atlas Mountains, the eastern Mediterranean karst belts (Sinai, Levant, Cyprus), and the North African rift margin contribute approximately five habitable cells. Cultural-record inference is strong for the Egyptian Nile rift margin (Apophis-Ra tradition) and the Levantine corridor (Leviathan and related traditions); the Atlas cells carry weaker cultural-record evidence but meet the habitat-substrate criteria.

c0010 — Oceania and Antarctic cells contribute approximately 4 cells combined

Australia's predominantly cratonic geology produces only approximately two habitable cells (the Flinders Ranges and the New South Wales volcanic margin). New Zealand contributes one cell on the Alpine Fault. The Transantarctic Mountain system contributes approximately one cell at current confidence; the archive notes that subglacial habitability assessment is poorly constrained and the figure may rise as Antarctic geophysical surveys mature. Cultural-record inference is effectively absent for all four cells by virtue of limited indigenous encounter opportunity or complete cultural disruption.

c0011 — Vacated cells cluster in regions with documented founder-tier extinction events

Approximately 20 cells globally are classified as vacated — habitable on substrate criteria but presenting neither cultural-record evidence nor current geophysical signal. Vacated cells cluster in three regions: the northern glaciated belt (Pleistocene ice-sheet loading stress on shallow-tier populations), the Pacific cratonic interior (extreme geological stability reducing geothermal flux below threshold), and the Mediterranean-Caribbean volcanic island systems (individual cell founder lineages lost to catastrophic volcanic events during the Mesozoic-to-Cenozoic interval). The archive treats vacated cells as distinct from merely unsurveyed cells on the basis of positive evidence of past occupation without current signal.

c0012 — Global census summary: 130 habitable cells after five sweeps

After five successive gap sweeps reaching the practical exhaustion of substrate-and-cultural-corpus criteria, the archive's cell enumeration stabilises at 130. Regional contribution at this resolution: Eurasian Tethyan 20 cells plus North Atlantic rift 4 and Fennoscandian 4; Eastern European Plain 2; Mediterranean-Levant 2; South China karst cluster 5; Hengduan / eastern Tibet 1; Pacific arcs 16 plus Pacific hotspot (Hawaii + Galápagos) 2; Indian subcontinent 6 plus Indochinese secondary 1; Russian Arctic/Urals/Siberian/Far East 12; Central Asian and East Asian secondary 5; Arabian / West Asian 2; North American Cordillera 10 plus North Atlantic margin 2 plus Caribbean 2 plus Central America 2 plus Appalachian-Shield 3; Andean 9; North Africa / Rift 3 plus East African Rift 6 plus Southern Africa 2 plus West Africa 1 plus Indian Ocean margin 3; Oceania 5; Antarctic 1. Of the 130 cells approximately 3 are confirmed (Shizhu-Wuling, Mont Donon, British Isles — plus redacted entries), approximately 60 are inferred on cultural-record or geophysical grounds, approximately 62 are potential (substrate-qualified but unevidenced), and 5 are vacated. Under the 25-to-35-percent active-occupation rate, the global active pod count is estimated at 33 to 46 surviving founder lineages. The companion Dragon-Toponym Map Book renders one regional map per cell with 725 total site placemarks (550 hand-curated plus 175 ingested from source KMLs); the unified KML export at resources/maps/dragon-territorial-grid.kml carries 130 cell boundaries plus 725 points.