Voynich Manuscript - Folio 2v

kooiin.cheo.pchor.otaiin.o.dain.chor<->dair.shty
kcho.kchy.sho.shol.qotcho.loeees.qoty<->chor.daiin
otchy.chor.lshy.chol.chody.chodain<->chcthy.daiin
sho.cholo.cheor.chodaiin

The triple-hardened-origin and internal-vessel-seal reach a dense-core and hydraulic-edge-origin in an equilibrium with the liquid-terminal-base and internal-vessel-stasis. The dense-core-reinforcement and internal-flow-status reach a liquid-pulse and fractal-liquid-surface-expansion in an equilibrium with the core-terminal-base. The hydraulic-edge-pressure and core-extension reach a stabilized internal-vessel-flow and base-extension-origin in an equilibrium with the internal-pressure and terminal-base. The internal-flow-stasis and internal-vessel-rise reach a core-base-extension-origin.

kchor.shy.daiiin.chckhoy<->s.shey.dor.chol.daiin
dor.chol.chor.chol.keol.chy.chty<->daiin.otchor.chan
daiin.chotchey.qoteeey.chokeos<->chees.chr.cheaiin
chokoishe.chor.cheol.chol.dolody

The dense-core-status and triple-base-origin reach an internal-vessel-extension in an equilibrium with the stasis-surface-rise and terminal-base-extension. This base-extension and core-flow reach a liquid-surface-vessel and internal-pressure in an equilibrium with the terminal-base and hydraulic-core-terminal. The terminal-base and internal-edge-surface reach a triple-liquid-pulse-edge and hardened-vessel-seal in an equilibrium with the triple-internal-seal and core-vessel-origin. The hardened-internal-status and central-core reach a vessel-surface-flow and terminal-downward-extension.