IMPACT PERIODICITY: 36 Myr FUNDAMENTAL MODE

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Holocene Sub-Cycle

FROM PERIODICITY TO THE DERIVATION CHAIN

The 36 Myr cycle is the temporal signature that first demanded a geometric explanation. Impacts don't just recur in time — they recur at the same geographic nodes (see Cycles). That spatial clustering led to the discovery of the lattice, and the lattice led to the derivation chain:

Φ = ∂_tΦ → Φ(t) = Ce^t → R = 1 + 1/R → R = φ → a_n = a_n−1 + a_n−2 → a_n ~ Aφⁿ → π = P₅·arccos(Φ/P₂) → d_m/d_n = φ^m−n → 1 axiom

The spatial quantisation d_m/d_n = φ^m−n explains why astronomical distances cluster on φ-shells. The geographic lattice — the 210-gon projected from Giza — explains why impacts cluster at specific nodes on Earth's surface. The temporal periodicity shown on this page is the third thread: the rhythm at which the lattice activates.