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THE GRECO-SYRIAC AND ARABIC SOURCES OF BARHEBRAEUS' MINERALOGY 237<br />

&I y L w , ,y i& &> 2 bJk J,Al a&-3 &L ,y e2 d.&l lil &I &wl bl<br />

,y >A dl Jl a >I &Ul$b9 &I Jl G,i b @3 -dl dl; &i cl..l ,L GjJI ,y l+&<br />

dl 4 >> LS LA- .iil;JI @ bblj LA AL- jl ,+Ul &I<br />

--<br />

&Loll bl, .uL .I+II<br />

A, .&Ji k,y4Je2 LC> lp~~,>~YlJl&, lil&Jli3LJljl&<br />

.dl ,yAlJI d&~,~Lr;Yl JI iUJ1 i,j 4 Ld .&&Lw2d% ,yL-l<br />

The cause of the descending [whirlwind] is that (la) when amindxscapsfmacld<br />

& strives to descend, (b) then a piece of ~.meeki1~initspath of descent and<br />

knocks it, while other winds are pushing it from above, so that that part [of the wind] is<br />

caught between the downward propulsions of what is above it and [(d)] the upward<br />

propulsion of the cloud below it, (e) ihmm%sahaut [yacricju] fromlhebw mutually<br />

obstruct& pmpulsions that /the wind) moves in a circle; sometimes the<br />

++<br />

crookedness<br />

of the passages augments the contorsion, just as it happens to hair that it is made curly<br />

by the contorsion of its pores. (3) The ascending [whirlwind arises] when_thP3arindy<br />

matter reaches the earfh and strikes it hard, and then ~s M, thenantherxind<br />

meets it from its side so as to twist it; sometimes it also arises from the meeting of two<br />

severe winds. (4) S m . 5 the strength of the ~m reaches such a level that it<br />

uproots trees and snatches ships from thesea.<br />

Here again the similarities between the two passages is such that one can safely<br />

regard the passage of Mab3ith as the main source of the passage of Cand. and<br />

the comparison with the passage in Mabiikth helps us in various ways in our<br />

understanding of the passage of<br />

At the same time Barhebraeus is not quite so faithful here to his source as he<br />

usually is when using Nic. as his source. In parts (lc) and (Id), for example, he<br />

seems to have simplified the corresponding parts of Mabahith and in (2) he<br />

inserts a sentence which has no counterpart in Mab*ith, defining whirlwind in<br />

its ascent as "'a~'iili''.~~ This and the two terms qar~ and kiikitii are most<br />

probably taken from De mundo .46<br />

De mundo syr. 143.25-27 (corr. De mundo gr. 395a 5-8, cf. Ryssel [1880140):<br />

44 We see, for example, that the rather awkward construction of the sentence 'Thus from these<br />

two opposing propulsions it happens that ..." (men traykn d&-yt? ..., d- ... tekr6k ..., gcsdshci<br />

&ih) is due to an attempt to render faithfully the corresponding construction in the Arabic<br />

@z-yacri& min al-dq'ayni ... an ... ).<br />

45 The same definition in the passage of K. d-zalgd, which is evidently a summary of this one,<br />

ms. Bod. Or. 467 l 1r 14-16: A a ~ rrr- a . & M tcsu avar L eunm . . .<br />

-<br />

b3- 12); in Paris 3 1 1 (58v a 19-26) it reads more correctly (cf. tr. Schlirnme 625f.): +z<br />

ut- 1Q- aYLU L.l IdbYrlz e"d : 6 s * &. e.b 9 L -+a<br />

.d&L.lh&A.-&<br />

46 The passage of Bar Kepha quoted by BakoS (p. 125 n.1, from Hex. V.31) defines 'alC~la rather<br />

as the descending whirlwind. As noted by BakoS, the passage is conupt in ms. Paris 241 (191r<br />

.L.laYLUF&M'm&s+ze.b.A-F--**.-<br />

. +S et- * . A&I ut- - There is no corresponding<br />

passage in Bar Shakko, ms.. IV.24, where Bar Shakko otherwise closely follows Bar Kepha<br />

(at least not in ms. Brit. Lib. Add. 7193, the manuscript available to me [fol. 80r-v]; 6. Nau<br />

[IS%] 323 n.1).

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