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order that he might regain Sicily, brought about a conclave. As the election of any cardinal seemed impossible, on the 5th of July 1294 the Sacred College united on Pietro di Morrone; the cardinals expected to rule in the name of the celebrated but incapable ascetic. Apocalyptic notions then current doubtless aided his election, for Joachim of Floris and his school looked to monasticism to furnish deliverance to the church and to the world. Multitudes came to Celestine's coronation at Aquila, and he began his reign the idol of visionaries, of extremists and of the populace. But the pope was in the power of Charles II. of Naples, and became his tool against Aragon. The king's son Louis, a layman of twenty-one, was made archbishop of Lyons. The cardinals, scarcely consulted at all, were discontented. The pope, who wanted more time for his devotions, offered to leave three cardinals in charge of affairs; but his proposition was rejected. He then wished to abdicate, and at length Benedetto Gaetano, destined to succeed him as Boniface VIII., removed all scruples against this unheard-of procedure by finding a precedent in the case of Clement I. Celestine abdicated on the 13th of December 1294. There is no sufficient ground for finding an allusion to this act in the noted line of Dante, "Che fece per viltate il gran rifiuto" ("who made from cowardice the great refusal," _Inferno_, 3, 60). Boniface at length put him in prison for safe keeping; he died in a monastic cell in the castle of Fumone near Anagni on the 19th of May 1296. He was canonized by Clement V. in 1313. See Wetzer und Welte and Herzog-Hauck (with excellent bibliography) as above; Jean Aurelien, Superieur de la Congregation des Celestins, _La Vie admirable de ... Saint Pierre Celestin_ (Bar-le-Duc, 1873); H. Finke, _Aus den Tagen Bonifaz VIII._ (Munster, 1902), pp. 24-43. (W. W. R.*) CELESTINE, or CELESTITE, a name applied to native strontium sulphate (SrSO4), having been suggested by the celestial blue colour which it occasionally presents. This colour has been referred to a trace of iron phosphate, but in some cases such an explanation appears doubtful. The mineral is usually colourless, or has only a delicate shade of blue. Celestine crystallizes in the orthorhombic system, being isomorphous with barytes (q.v.). The angle between the prism faces is 76 deg. 17'. The cleavage is perfect parallel to the basal pinacoid, and less marked par
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