Voynich Manuscript - Folio 4r

kodalchy.chpady.sheol.ol.sheey.qotey<->doiin.chor.ytoy
dchor.chol.shol.cthol.shtchy.chaiin<->s<->choraiin.chom
otchol.chol.chy.chaiin.qotaiin<->daiin.shain
qotchol.chy.yty.daiin.okaiin.cthy

The internal-vessel-extension and internal-liquid-seal reach a stabilized surface-flow and triple-surface-extension in an equilibrium with the liquid-pulse-terminal-base. This terminal-origin and core-flow reach a rising-surface-extension. The central-core-status and core-flow-stasis reach an internal-vessel-rise and hydraulic-extension-origin in an equilibrium with the stasis-point, reaching a further equilibrium with the core-flow-origin and internal-completion-seal. The hydraulic-vessel-rise and core-flow reach a rising-liquid-origin and liquid-pulse-base-origin in an equilibrium with the terminal-base and internal-surface-origin. The liquid-pulse-vessel-rise and internal-vessel-status reach a terminal-base and internal-hardened-origin-status.

pydaiin.qotchy.dy.tydy<->
chor.shytchy.dy.tcheay<->
qotaiin.cthol.daiin.cthom<->
shor.shol.shol.cthy.cpholdy<->
daiin.ckhochy.tchy.koraiin<->
odal.shor.shyshol.cphaiin<->
qotchoiin.sheyr.qoty<->
soiin.chaiin.chaiin<->
daiin.cthey

The active-internal-extension and liquid-pulse-vessel-status reach a downward-extension and terminal-flow-status in an equilibrium with the core-flow and reinforced-vessel-status. This reaches a triple-fractal-surface-rise. The liquid-pulse-origin and internal-vessel-rise reach a terminal-base and internal-completion-seal in an equilibrium with the core-flow and steady-flow-stasis. This stabilized-flow-stasis and internal-pressure reach a reinforced-vessel-status. The terminal-base and dense-internal-vessel reach an internal-vessel-status and core-internal-origin in an equilibrium with the hydraulic-base-extension and core-flow. This reinforced-stasis and internal-pressure-origin reach an equilibrium with the liquid-pulse-triple-origin and surface-stasis-rise. The liquid-pulse-status and triple-stabilized-origin reach a triple-internal-surface-origin in an equilibrium with the terminal-base and internal-pressure.