Voynich Manuscript - Folio 1r

fachys.ykal.ar.ataiin.shol.shory.cthres.y.kor.sholdy
sory.ckhar.or.y.kair.chtaiin.shar.are.cthar.cthar.dan
syaiir.sheky.or.ykaiin.shod.cthoary.cthes.daraiin.sa
ooiin.oteey.oteos.roloty.cth?ar.daiin.otaiin.or.okan
dair.y.chear.cthaiin.cphar.cfhaiin ydaraishy

The hardening process initiates at the rising origin as the internal flow stabilizes and extends through the central core. This hydraulic state ascends via the core-origin where internal pressure rises and repeats toward the terminal point. Triple-fractal expansion at the core-origin creates rising liquid pressure, initiating an equilibrium between the outward extension and the stabilized state. This triple-fluid movement reaches the surface edges where new liquid origins solidify into a hardened equilibrium state. The active internal rise completes the flow circuit at the origin point to reach a finalized state of extended stability.

?.odar.o.y.shol.cphoy.oydar.sh.s.cfhoaiin.shodary
yshey.shody.okchoy.otchol.chocthy.oschy.dain.chor.kos
daiin.shos.cfhol.shody dain.os.teody

The hydraulic-origin initiates an active internal flow as the liquid-seal expands into a state of stabilized downward extension. Active surface-stretching triggers a liquid-core-pulse through the internal pressure-channels, transitioning into a dense-core terminal point. This stabilized flow-origin maintains a steady internal-liquid-extension, concluding where the terminal-grounding meets the hydraulic-surface-boundary.

?.ydain.cphesaiin.ol.s.cphey.ytain.shoshy.cphodales
oksho.kshoy.otairin.oteol.okan.shodain.sckhey.daiin
shoy.ckhey.kodaiin.cphy.cphodaiils.cthey.she.oldain.d
dain.oiin.chol.odaiin.chodain.chdy.okain.dan.cthy.kod
daiin.shckhey.ckeor.chor.shey.kol.chol.chol.kor.chal
sho.chol.shodan.kshy.kchy.dor.chodaiin.sho.kchom
ycho.tchey.chokain.sheo.pshol.dydyd.cthy.daicthy
yto.shol.she.kodshey.cphealy.dasain.dain.ckhyds
dchar.shcthaiin.okaiir.chey.rchy.potol.cthols.dlocta
shok.chor.chey.dain.ckhey otol.daiiin

The terminal-base action initiates at the internal-pressure origin as the hydraulic-stasis-seal activates a triple-surface extension through the internal-vessel boundaries. Reinforced hardening in the core-vessel triggers a hydraulic-rise-origin at the surface-liquid boundary, reaching a hardened state where the flow-base meets the stabilized internal-pressure origin. The rising flow and internal-stasis reach a hardened-base origin as the internal-pressure vessel-seal stabilizes the internal-liquid-origin to maintain a steady-state. The terminal-base then reaches a liquid-origin as the internal-flow-origin and internal-flow-extension stabilize the hardened-liquid-origin at the terminal-point. Internal-pressure and reinforced-base origins stabilize the internal-surface-hardening of the core-vessel, where the core-action and reinforced-liquid flow through the central-core-system. Internal-flow and flow-grounding establish a dense-structural-stasis as the base-extension-origin concludes at the internal-hardened-seal. The internal-action and surface-pressure-seal reach a hardened-liquid-origin as the internal-action-pulse expands through a triple-downward-extension. The surface-action and internal-flow reach a reinforced-stasis-state, extending the internal-vessel-boundary toward the base-origin and stabilized-grounding-system. The core-rise at the internal-pressure-origin creates a hydraulic-core-rise where the internal-action and internal-vessel-pulse reach the internal-flow-stasis. Flow-stasis through the core-vessel and terminal-base reaches a stabilized-internal-stasis. The surface-liquid-flow then completes the triple-base-origin.

cpho.shaiin.shokcheey.chol.tshodeesy.shey.pydeey.chy.ro.d?
?doin.chol.dain.cthal.dar.shear.kaiin.dar.shey.cthar
cho?o.kaiin.shoaiin.okol.daiin.far.cthol.daiin.ctholdar
ycheey.okay.oky.daiin.okchey.kokaiin.??chol.k??chy.dal
d?eeo.shody.koshey.cthy.okchey.keey.keey.dal.chtor
?eo.chol.chok.choty.chotey dchaiin

The internal-pressure-seal initiates a surface-origin through a reinforced-triple-action, as the core-flow reaches an edge-surface-extension. This active-state moves through a triple-downward-extension where the internal-vessel-boundary completes the current-flow. The terminal-liquid-origin then moves from the core-flow into the terminal-base, as the internal-pressure-rise and extension-base reach an internal-active-rise. This origin-point extends the base-action toward an internal-pressure-rise. The internal-fractal-liquid reaches the core-origin and surface-origin, where the hardened-liquid and terminal-base reach the edge-limit of the internal-flow. The terminal-base then stabilizes the internal-flow-extension. The active-triple-surface-extension reaches a hardened-action and liquid-state, as the terminal-base and hardened-internal-action reach a reinforced-core-origin. The internal-flow and reinforced-internal-vessel-boundary conclude the base-extension. A triple-fractal-completion reaches the flow-extension and reinforced-stasis, as the internal-pressure and hardened-internal-action reach a triple-surface-reinforcement. This triple-reinforcement at the base-extension reaches the internal-edge-boundary. The fractal-completion then moves through the core-flow and reinforced-core toward the flow-extension and surface-extension-status. The internal-base-origin then completes the circuit.