Voynich Manuscript - Folio 2r

kydainy.ypchol.daiin.otchal<->ypchaiin.ckholsy<->
dorchory<->chkar.s<->shor.cthy.cth
qotaiin<->cthey.y<->chor.chy.ydy<->chaiin
chaindy<->chtod.dy<->cphy.dals<->chokaiin.d
otochor.al<->shodaiin<->chol.dan<->ytchaiin.dan
saiin.daind<->dkol.sor<->ytoldy<->dchol.dchy.cthy
shor.ckhy.daiiny<->chol.dan

The hardened-base-extension and active-internal-pulse-flow reach a terminal-base and hydraulic-edge-rise in an equilibrium with the active-internal-pressure-origin and dense-internal-status, reaching a further equilibrium with the extension-core-rise. This dense-core and stasis-point reach an equilibrium with the rising-flow and internal-pressure. The liquid-edge-origin reaches an equilibrium with the internal-pressure and action-point, which reaches an equilibrium with the core-vessel and active-downward-extension, finally reaching the internal-pressure-origin. The internal-flow-extension reaches an equilibrium with the internal-surface-base and downward-extension, which reaches an equilibrium with the internal-pressure and terminal-base-status, concluding at the internal-core-origin. The hydraulic-edge-core and liquid-seal reach an equilibrium with the flow-base-origin, which reaches an equilibrium with the core-flow-terminal, finally reaching the active-internal-surface-origin and terminal-point. The internal-origin and terminal-base reach an equilibrium with the dense-core-extension and status-rise, which reaches an equilibrium with the active-internal-surface-extension, finally reaching the internal-core-flow and internal-vessel-extension. The rising-flow and internal-dense-vessel reach a terminal-base-extension in an equilibrium with the core-flow-terminal.

kydain.shaiin.qoy.s.shol.fodan<->yksh.olsheey.daiildy
dlssho.kol.sheey.qokey.ykody.so<->chol.yky.dain.daiirol
qoky.cholaiin.shol.sheky.daiin<->cthey.keol.saiin.saiin
ychain.dal.chy.dalor.shan.dan<->olsaiin.sheey.ckhor
okol.chy.chor.cthor.yor.an.chan<->saiin.chety.chyky.sal
sho.ykeey.chey.daiin.chcthy

The hardened-base-origin and internal-surface-origin reach a liquid-stasis and internal-flow terminal-grounding in an equilibrium with the active-core-hardening and triple-liquid-surface-extension. This terminal-base-extension and internal-stasis-flow reach a reinforced-core and triple-surface-extension in an equilibrium with the core-flow and active-core-base-extension. The liquid-edge-pulse and core-internal-origin reach a stabilized internal-flow-status in an equilibrium with the internal-pressure and active-core-surface-origin. The active-internal-origin-extension and terminal-base reach a internal-vessel-rise and terminal-grounding in an equilibrium with the liquid-surface-origin and triple-surface-extension of the dense-core. The hydraulic-hardened-liquid and internal-vessel-rise reach a core-rise and active-edge-rise in an equilibrium with the surface-origin and internal-vessel-extension. The internal-flow and active-triple-surface-extension reach a terminal-base and internal-pressure-rise.