Ixxii NOTES. 



Herodotus, vi. 67, and Pausanias, ii. 34, 7 ; of those of J2depsos in Eubsea (of 

 which some have a temperature of 31 C. (87 0> 1 Fah.,) and others of 62 to 

 75 C. (or 143'6 to 167'0 F.,) in Strabo, p. 60, 447, and Athenams, ii. 

 3, 73 ; the hot springs of Thermopylae, at the foot of Mount Oeta, having 

 a temperature of 65 C. (149 Fah.,) are described by Pausanias, x. 21, 2. 

 These references are taken from manuscript notes of Professor Curtius, the 

 learned travelling companion of Otfried Miiller 



C 207 ) p. 210. Plin. ii. 106; Seneca, Epist. 79, 3, ed. Ruhkopf; Beau- 

 fort, Survey of the Coast of Karamania, 1820, art, Yanar, near Deliktash, the 

 ancient Phaselis, p. 24. Compare likewise Ctesias, Fragm. cap. x. p. 250, ed 

 Bahr; and Strabo, lib. xiv. p. 665, Casaub. 



f 08 ) p. 211. Arago, Annuaire, 1835, p. 234. 



f) p. 211. Acta S. Patricii, p. 555, ed. Ruinart, T. ii. p. 385, Mazochi. 

 Dureau de la Malle first called attention to this remarkable passage, in the 

 " Recherches sur la Topographic de Carthage," 1835, p. 276. (Compare 

 Seueca, Nat. Quaest. iii. 24.) 



O 210 ) p. 213. Humboldt, Rel. hist. T. iii. pp. 562567 ; Asie centrale, T. i, 

 p. 43, T.ii. pp. 505 516; Vues des Cordilleres, PI. xli. On the Macalubi (from 

 the Arabic Makhlub, overturned, from the root Khalaba,) and on "fluid 

 earth issuing from the Earth," see Solinus, cap. v. ; idem ager Agrigentinus 

 eructat limosas scaturigines, et ut vena3 fontium sufficiunt rivis subministrandis, 

 ita in hac Siciliae parte solo nunquam deficiente, ceterna rejectatione terrain 

 terra evomit. 



C 211 ) p. 214. See the excellent little map of the island of Nisyros, in Rosa, 

 Ecisen auf den griechischen Inseln, Bd. ii. 1843, S. 69. 



C 212 ) p. 215. Leopold von Buch, Phys. Beschreibung der Canarischsn 

 Inseln, S. 326 ; and the same author, tiber Erhebungscratere und Vulcane, in 

 Poggend. Ann. Bd. xxxvii. S. 169. Strabo distinguishes extremely well between 

 two modes of formation of islands, when he is speaking of the separation of Sicily 

 from Calabria, Lib. vi. p. 258. Casaub. He says, " Some islands are detached 

 parts of the main land ; others have been raised from the bottom of the sea, 

 as we still see. The islands of the open sea, i. e. those far from the shore, 

 have probably been raised from the bed of the sea ; and those situated near 

 promontories have been detached from the main land." 



( 213 ) p. 215. Ocre Fisove (Mons Vesuvius.) The word owe is true Urn- 

 brian, and, according to Festus himself, signifies " mountain" in the ancient 

 Umbriaii language (Lassen, Deutung der Eugubinischen Tafeln, im Rhein. 



