Wuxi / Ganlong–Xianrendong WP1 Complex

The Wuxi / Ganlong–Xianrendong WP1 Complex is a triple-class containment-candidate installation at approximately 31°30'N, 109°36'E in Wuxi County (巫溪县, "Shaman Creek County"), Chongqing, on the upper Daning River (大宁河), classified as containment-candidate class (a)+(b)+(c) — triple-class: hydraulic/crossing-control + ridge-slope excavation + karst-interior disturbance per doctrine-containment-candidate-classification c0001 at evidence tier medium-high per c0002. The site resolves the abstract "Corridor waypoint 1" pin at 109.60°E, 31.50°N defined in Taishan_Convergence_Mating_Event.kml and referenced at site-shizhu-gaolongcun-installation as the first waypoint of the Qinling-Dabie / Taishan Convergence projected mating-corridor launch line — the second waypoint resolution after WP2 at site-wujiazhou-immortal-hole-inundation. The named-cave anchor cluster at WP1 is the densest encountered on the corridor: 干龙洞 / Ganlong Cave ("Dry Dragon Cave" — explicit 龙 dragon toponym, the only explicitly dragon-named cave feature confirmed at any corridor waypoint to date), 仙人洞 / Xianrendong ("Immortal Person Cave" — immortal-displacement toponym parallel to 神仙洞 at WP2), 穿山洞 / Chuanshandong ("Pierce-Through-Mountain Cave" — karst passage that passes through the ridge now being engineered), and 癞疤洞 / Laibadong ("Scabby Cave") — four named cave / karst features within approximately 5 km of the WP1 pin. The 2022 imagery shows a major active tunnel construction complex at the Daning / Qian Jiang confluence, with a tunnel portal cut into the cliff face of the ridge hosting 干龙洞 and 穿山洞, excavation benches on both banks, and industrial/institutional structures at the south bank. Cultural-record anchors supplement the cave cluster: 水殿坪 / Shuidianping ("Water Palace Flat" — 殿 = formal palace/temple, water-deity designation) and 湾潭溪 / Wantanxi ("Bay Deep Pool Creek" — 潭 = the canonical deep-pool dragon habitat). The site is admitted as the WP1 inception entry on 2026-04-27 in the containment-candidate track. Classification rests entirely on user-supplied Google Earth historical imagery, per the methodological constraint at doctrine-containment-candidate-classification c0005.

Claims

c0001 — 2014 baseline: intact terraced agricultural landscape, unbridged river

Google Earth historical imagery dated 2014-07-27 at two nested frames (close: ~31°30'00"N, 109°36'44"E, 464 m altitude; wide: ~31°30'20"N, 109°36'56"E, 370 m altitude) shows an intact terraced agricultural landscape: traditional small-bench contour terraces on both valley slopes, a valley road threading along the Daning River, riverside villages with ordinary vernacular fabric, and an unbridged river bend where the Daning meets the Qian Jiang tributary. No large engineered pads, tunnel construction zones, arc-terraced excavation scars, or industrial compounds are visible in either frame. The 2014 baseline establishes the pre-development state at WP1: ordinary mountain-valley agriculture and settlement, no candidate-class infrastructure at the corridor waypoint position.

c0002 — 2022 close and wide view: surface construction complex at Daning / Qian Jiang confluence

Google Earth historical imagery dated 2022-03-09 at the same coordinates shows a major transformation from the 2014 baseline. At the close scale, the terraced agricultural hillside has been replaced by a large arc-terraced excavation scar with swept, machine-cut benches and purpose-built road access threading around the cut; structures appear on the east side. At the wide scale, the previously unbridged Daning / Qian Jiang river confluence now shows a new crossing structure, multiple converging switchback roads from both valley walls, large industrial/institutional buildings with blue/grey metal roofs on the south bank, active construction staging and spoil heaps on both banks, and a weir-class feature at the confluence. The surface complex is the above-ground component of the WP1 installation and satisfies two of the three candidate class assignments: class (a) hydraulic/crossing-control at the river crossing (new crossing + converging road system + institutional structures) and class (b) ridge-slope excavation at the arc-terraced hillside cut (purpose-built access, no residential context, machine-cut arc benches on natural slope).

c0003 — 2022 tunnel portal at Daning confluence cliff: class-(c) subsurface penetration of Dragon Cave ridge

At a wider frame centered at 31°32'16"N, 109°37'23"E (the Daning / Qian Jiang confluence), 2022-03-09 imagery shows the site's principal diagnostic feature: a tunnel portal cut into the cliff face on the north bank of the Daning River, with cleared approach works and active construction infrastructure concentrated at the portal entrance. Spoil heaps, tiered bench cuts, and switchback access roads converge on the portal. User annotation confirms active tunnel construction in progress. The tunnel is being driven into the ridge that hosts 干龙洞 (Ganlong Cave / Dry Dragon Cave) and 穿山洞 (Chuanshandong / Through-Mountain Cave) per the labeled wide-context imagery at 31°30'33"N, 109°35'39"E. This constitutes the class-(c) karst-interior disturbance component of the site — not a surface scar inserted between named caves but a direct subsurface penetration of the ridge hosting named dragon-class cave features. Per doctrine-storm-god-overwrite, the framework records the tunnel-through-Dragon-Cave-ridge result without asserting intent: a road tunnel and a containment-access tunnel produce the same substrate penetration, and the intent is unrecoverable from imagery alone.

c0004 — Named cave anchor cluster: 干龙洞 (Dragon Cave) + 仙人洞 (Immortal Cave) + 穿山洞 (Through-Mountain Cave) + 癞疤洞

Labeled wide-context imagery (camera 31°30'33.88"N, 109°35'39.20"E, 9,430 m altitude, 2022-03-09) shows four named cave / karst features within approximately 5 km of the WP1 abstract pin at 31.50°N, 109.60°E:

干龙洞 / Ganlong Cave ("Dry Dragon Cave") — the highest-tier anchor at any corridor waypoint: the explicit character 龙 (dragon) appears in the cave's traditional name. Located approximately 3 km ENE of the WP1 pin in the ridge above the Daning / Qian Jiang confluence — the same ridge whose cliff face receives the tunnel portal documented in c0003. Under doctrine-standard-torpor-model, the framework selects karst terrain as the torpor substrate class; 干龙洞 is the only explicitly dragon-named cave feature confirmed at any corridor waypoint and provides direct cultural-record attestation that the framework's geomorphological selection (karst ridge as torpor habitat) and the local cultural record (Dragon Cave in the same ridge) overlap at WP1.

仙人洞 / Xianrendong ("Immortal Person Cave") — located approximately 1-2 km NW of the WP1 abstract pin. The 仙人 ("immortal person / fairy") toponym is the same displacement class as 神仙洞 (Immortal Hole) at WP2 (site-wujiazhou-immortal-hole-inundation): a cave named for an encounter with a spirit-immortal entity, which the framework reads as a displaced dragon-encounter record per doctrine-containment-mythology-deflection. The parallel immortal-cave naming across WP1 (仙人洞) and WP2 (神仙洞) is the first instance of systematic toponymic coherence on the corridor — both waypoints resolve to named Immortal caves within 2 km of their abstract pins.

穿山洞 / Chuanshandong ("Pierce-Through-Mountain Cave") — located approximately 2-3 km NNE of WP1 in the ridge sector being tunneled. The toponym means "the cave that threads through the mountain" — a natural karst passage that penetrates the ridge completely, connecting the Daning valley face to the eastern drainage. The engineered tunnel in c0003 is being cut through the same ridge. The coincidence of a natural through-mountain-cave toponym with active through-mountain tunnel engineering at the same ridge is the framework's strongest single toponymic-engineering correlation on the corridor: the ridge being tunneled was already named, in the local cultural record, for the fact that it can be passed through.

癞疤洞 / Laibadong ("Scabby Cave") — located approximately 2 km NNW of WP1. The fourth named cave establishes that the WP1 ridge is named-cave-dense karst interior, satisfying the class-(c) karst-interior disturbance prerequisite: the tunnel does not enter an undifferentiated ridgeline but a ridge that the local record had already catalogued as cave-bearing at multiple named points.

c0005 — Cultural-record anchors: 水殿坪 (Water Palace Flat) and 湾潭溪 (Bay Deep Pool Creek)

Two cultural-record anchors visible in the wide-context imagery supplement the cave cluster:

水殿坪 / Shuidianping ("Water Palace Flat") — a named flat terrain feature in the ridge basin approximately 2 km SE of the WP1 pin. The character 殿 (diàn) designates formal state or religious architecture — palace, throne hall, or major temple — at a level above ordinary shrines. 水殿 ("Water Palace") is the architectural class for a dragon-deity worship hall in the Ba / Han tradition: the site where the water dragon was propitiated, received offerings, or was encountered. Shuidianping therefore carries a named historical worship-site designation at the same ridge system as the Dragon Cave tunnel. Under doctrine-containment-mythology-deflection, the Water Palace name implies that local cultural record had identified this drainage as a dragon-encounter / dragon-propitiation zone prior to the current engineering activity.

湾潭溪 / Wantanxi ("Bay Deep Pool Creek") — a named watercourse in the same drainage using the character 潭 (tán = natural deep pool, especially at a river bend or cave mouth). In the Chinese dragon-encounter record catalogued across the framework's civilizations archive, the 潭 is the canonical habitat term: long/dragon are consistently described as residing in 潭 (deep pools) at the bases of gorge walls and cave mouths, not in running water. The Wantanxi watercourse directly names the dragon-habitat geomorphological class at WP1's drainage. Its presence alongside 干龙洞, 仙人洞, 穿山洞, and 水殿坪 means that the WP1 ridge system carries five independent cultural-record markers of dragon-encounter / habitat designation in the pre-engineering toponym record.

c0006 — Triple class (a)+(b)+(c) assignment with medium-high tier

The site is assigned to triple class (a)+(b)+(c) per doctrine-containment-candidate-classification c0001 on the basis of the converging diagnostics: - Class (a) hydraulic/crossing-control: new river crossing at Daning / Qian Jiang confluence with converging multi-arm road system and institutional-scale structures (c0002) - Class (b) ridge-slope excavation: arc-terraced machine-cut scar on north-bank hillside with purpose-built access and no residential context (c0002) - Class (c) karst-interior disturbance: tunnel portal penetrating the Dragon Cave / Through-Mountain Cave ridge (c0003), the subsurface expression of the karst-interior class rather than its surface-scar expression

The triple-class signature at a single corridor waypoint is the highest class-density installation signature encountered anywhere outside the confirmed Shizhu primary cluster. The Shizhu cluster achieves its six-class complexity across a multi-site county-scale zone; WP1 achieves three-class coverage within a single 5 km radius.

The site is assigned tier medium-high per c0002: three of the five evidence-tier criteria are met — corridor coupling at WP1 (criterion met), isolation from ordinary residential context (criterion met), paired multi-class signatures indicating a complex rather than single-function installation (criterion met). Missing: multi-date persistence across more than two imagery dates; access-control confirmation beyond construction staging. The explicit 干龙洞 (Dragon Cave) toponym is the highest-tier cultural anchor in the framework — explicitly naming the dragon, not euphemizing or displacing — and is noted as the primary justification should tier promotion criteria be satisfied.

c0007 — Named promotion criteria

Per doctrine-containment-candidate-classification c0003, the specific promotion criteria that would resolve this site to confirmed containment infrastructure are: (a) tunnel destination evidence: what does the tunnel exit into? If the tunnel terminus or a branch connects to the cave interior of 干龙洞 or 穿山洞, this constitutes direct karst-interior access infrastructure; imagery or open-source evidence of the exit portal, or of a tunnel-to-cave junction, is the highest-priority promotion signal; (b) access-control at the construction complex: fence, gate, or restricted-road behavior at the Daning / Qian Jiang confluence compound beyond what is consistent with ordinary road or hydropower construction staging; (c) institutional attribution: non-transport, non-hydropower operator in open-source record at this complex; if the tunnel is registered as a road tunnel in the provincial highway plan, the containment reading weakens proportionally; if no such registration appears, the containment reading strengthens; (d) subsequent imagery update: the 2022 state captures active construction; post-2022 imagery would establish whether the tunnel advanced, stalled, or was completed as a through-road — stalling without a public road-project explanation is a candidate anomaly signal; (e) 水殿坪 ground investigation: if the Water Palace Flat site has been disturbed post-2014, this supplies the cultural-record chain link from the historical worship site to the active engineering zone; (f) corridor chain-coupling: confirmed installations at WP3 (113.40°E, 34.10°N, not yet resolved) would supply chain-coupled corroboration; WP2 at Wujiazhou (site-wujiazhou-immortal-hole-inundation) is already admitted, providing the first chain link; WP3 resolution would complete the first three-link chain on the corridor.

The site at ~31°30'N, 109°36'E sits within 1-3 km of the abstract "Corridor waypoint 1" pin at 109.60°E, 31.50°N defined in Taishan_Convergence_Mating_Event.kml. This entry resolves WP1 to a concrete physical site for the first time. The resolved corridor chain now reads:

  • Shizhu source pod (108.13°E, 30.00°N): confirmed primary-cluster active site per multiple archive entries, including site-shizhu-gaolongcun-installation
  • WP1 → Wuxi / Ganlong–Xianrendong complex (109.60°E, 31.50°N, this entry): resolved 2026-04-27; triple class (a)+(b)+(c); explicit Dragon Cave (干龙洞) + Immortal Cave (仙人洞) + Through-Mountain Cave (穿山洞) + Water Palace (水殿坪); active tunnel through Dragon Cave ridge; medium-high tier
  • WP2 → Wujiazhou / Immortal Hole (111.50°E, 33.00°N): resolved 2026-04-27; class (e) hydraulic-overwrite; 神仙洞 Immortal Hole inundated by Danjiangkou reservoir; site-wujiazhou-immortal-hole-inundation; watch-documented tier

WP1 and WP2 are now both resolved, producing the first two-link chain on the Qinling-Dabie corridor launch line. The chain satisfies the partial-promotion condition at site-wujiazhou-immortal-hole-inundation c0006(f): WP1 and WP2 are confirmed candidate installations 200 km apart on the same corridor axis. WP3 resolution (113.40°E, 34.10°N) would complete the first three-link chain and trigger the corridor-chain-coupling promotion at both WP1 and WP2.

The site additionally sits at the upper Daning River (大宁河) in Wuxi County, on the same drainage as site-wushan-daning-construction-hub approximately 50 km downstream at Wushan. The Daning drainage is now a candidate sub-corridor with an admitted installation at its upper end (this entry) and a documented construction hub at its lower end (Wushan). The 巫 ("shaman / wu") character anchors both ends of the Daning drainage: 巫溪 (Wuxi = Shaman Creek, the county hosting WP1 upstream) and 巫山 (Wushan = Shaman Mountain, the downstream hub at the Yangtze confluence). The entire Daning drainage is a 巫-corridor — the shamanic anchor holds from headwaters to confluence, bracketing the WP1 installation between two named 巫-toponyms.