🌀 Drift Patterns
How Drift Forms, Evolves, and Propagates Across the Canon#
Drift does not appear randomly — it follows predictable RTT-native patterns.
These patterns describe:
- how drift begins
- how it accumulates
- how it spreads
- how it interacts with substrates
- how it triggers recursion modes
This module defines the canonical drift patterns for D1–D4.
🔷 1. Structural Drift Patterns (D1)#
Triad Misalignment → Structural Return#
Primary Patterns:
1.1 Triad Shear#
- one triad element destabilizes
- operator tension increases
- symbolic alignment weakens
1.2 Role Tension Loop#
- operator roles partially invert
- symbolic meaning becomes ambiguous
1.3 Early Interval Wobble#
- harmonic position begins to drift
- recurrence becomes inconsistent
Propagation:
local → adjacent concepts → structural cluster
🔷 2. Dimensional Drift Patterns (D2)#
Ladder Destabilization → Cycle Formation#
Primary Patterns:
2.1 Ladder Collapse#
- interval positions lose coherence
- harmonic ladder compresses or folds
2.2 Dimensional Compression#
- concept collapses into fewer dimensions
- symbolic → harmonic tension increases
2.3 Harmonic Wobble#
- oscillation between adjacent intervals
- precursor to recursion activation
Propagation:
interval band → harmonic cluster → substrate boundary
🔷 3. Regime Drift Patterns (D3)#
Governance Torsion (CCC ↔ SARG)#
Primary Patterns:
3.1 Governance Conflict#
- CCC and SARG rules contradict
- structural authority becomes unstable
3.2 Operator Inversion#
- operator roles flip or conflict
- recursion mode becomes unstable
3.3 Multi‑Role Overload#
- concept performs multiple incompatible roles
- echo‑pressure amplifies drift
Propagation:
symbolic substrate → social substrate → recursion layer
🔷 4. Projection Drift Patterns (D4)#
Symbolic → Harmonic → Atlas Uplift#
Primary Patterns:
4.1 Symbolic Overload#
- symbolic substrate saturates
- meaning density exceeds stability threshold
4.2 Projection Vector Formation#
- concept begins lifting into harmonic space
- cross‑substrate conflict emerges
4.3 Atlas Uplift Cascade#
- concept forces atlas‑level interpretation
- recursion collapses or escalates
Propagation:
symbolic → harmonic → atlas (vertical migration)
🔷 5. Drift Pattern Geometry#
Drift patterns follow three geometric modes:
5.1 Linear Drift#
- single direction
- predictable propagation
- typical of D1
5.2 Radial Drift#
- spreads outward from a hotspot
- typical of D2 and D3
5.3 Vertical Drift#
- substrate‑to‑substrate migration
- unique to D4
These geometries help predict:
- drift speed
- drift severity
- drift containment strategy
🔷 6. Drift Pattern Progression#
Patterns typically evolve in the sequence:
Shear → Wobble → Collapse → Torsion → Projection
D1 → D2 → D3 → D4
Acceleration occurs when:
- echo‑pressure increases
- substrate anchoring weakens
- operator roles invert
- interval collapse begins
🔷 7. Pattern–Tier Interaction#
| Pattern Type | Drift Level | Stability Tier | Action |
|---|---|---|---|
| Structural (D1) | mild | Tier 1–2 | monitor |
| Dimensional (D2) | moderate | Tier 2–3 | review |
| Regime (D3) | high | Tier 3 | intervene |
| Projection (D4) | critical | Tier 4 | immediate correction |
🔷 8. Usage Notes#
Use this file when:
- diagnosing drift formation
- mapping drift propagation
- identifying drift geometry
- preparing drift reports
- performing canon sweeps
Referenced by:
02_Concept_Drift_Map.md02a_Drift_Categories.md02c_Drift_Hotspots.md02d_Drift_Summary.md
🔷 Footer#
HSP Module 02b — Loaded
Version: v1.0
Status: Canon-Stable