When Oedipus knows that his end is near, he leads his
This text is part of:
If the scholiast is right as to the situation of the temple, Eupolis used πόλεως in the sense of "acropolis," as Athenians still used it in the time of Thucydides (2. 15).Μαρικᾶς of Eupolis,
2 It is beautifully and persuasively stated in Wordsworth's Athens and Attica, ch. XXX. (p. 203, 4th ed.). The author holds that the poet, embarrassed by the rival claims of the Areiopagus and Colonus, intended to suggest the former without definitely excluding the latter.
3 1. 28. 7 “ἔστι δὲ καὶ ἐντὸς τοῦ περιβόλου μνῆμα Οἰδίποδος. πολυπραγμονῶν δὲ εὕρισκον τὰ ὀστᾶ ἐκ Θηβῶν κομισθέντα: τὰ γὰρ ἐς τὸν θάνατον Σοφοκλεῖ πεποιημένα τὸν Οἰδίποδος Ὅμηρος οὐκ εἴα μοι δόξαι πιστά”, etc. He refers to Il. 23.679 f. See my Introd. to the O. T., p. xiv.
4 Prof. T. McK. Hughes, Woodwardian Professor of Geology in the University of Cambridge, kindly permits me to quote his answer to a question of mine on this point. His remarks refer to the general conditions of such phenomena in Greece at large, and must be taken as subject to the possibility that special conditions in the neighbourhood of Colonus may be adverse to the processes described; though I am not aware of any reason for thinking that such is the case. “"It is quite possible that a chasm, such as is common in the limestone rocks of Greece, might become first choked, so as no longer to allow the passage of the winter's flood, and then overgrown and levelled, so that there might be no trace of it visible on the surface. The water from the high ground during winter rains rushes down the slopes until it reaches the jointed limestone rock. It filters slowly at first into the fissures. But the water, especially when it contains (as most surface water does) a little acid, dissolves the sides of the fissure, and soon admits sand and pebbles, the mechanical action of which hurries on the work of opening out a great chasm, which swallows up the winter's torrent, and becomes a katavothron. But during the summer no water runs in, and, even without an earthquake shock, such a chasm may get choked. The waters which cannot find their way through then stand in holes, and deposit their mud. There would be for some time a pond above, but that would at last get filled, and all trace of the chasm be lost."”
This work is licensed under a Creative Commons Attribution-ShareAlike 3.0 United States License.