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THE GRECO-SYRIAC AND ARABIC SOURCES OF BARHEBRAEUS' MINERALOGY<br />
b) Abii'l-Barakat al-Baghdiidi, K. al-mu 'tabar (?)<br />
The following passage provides an illustration of how in looking for Barhebraeus'<br />
sources, we need to check the source at the level of single words and phrases.<br />
Cand. 120.7-121.4 (underline: agreement with Mab@ith; italic: agreement with Nic.):<br />
&*a 4 AG.~. 4uLL +& du+&a &d &a* -.+.~iir %<br />
&%%la am +*- ++dm. &- *b & . &+=,a l s a A<br />
d \ ~<br />
-<br />
+ . r ~ & . ~ ~ ~ u . r . r l c ~ c ~ ~ ~<br />
~ r ~ ~ a . o y a U . r ~ ~ d i W . r d . r ~<br />
+ ~ & ~ a a A % ~ . ~ r ~ + t d a + , + & ~<br />
--.+A&&.r&.*-Le+A*plrr.r&<br />
t-3- rr m a qtnj, A. -Ma &*fa tGua%m e-<br />
+.r&Apr~enw&r~oa.d&*d.r~~~<br />
.-.r+&a&+C;Lurd*ir-.*&<br />
[120.13 BakoS et Ci~ek: +& PBV et Nic. 11 121.1 Le+A: he+& Pet<br />
Nic.]<br />
(1) me@l d6qides awket lampide w-belsusyatii d-metwn b-laylawatii. (2a) dukkyatii<br />
hiinen d-it bhen kyiina kebritiinayiyl sdqin menhen 'ew kebritiinaye, (b) w-s&-n<br />
b-a'k haw detratpb b-qaniriitii lelyaytii, (c) w-h-a meshtwap hii haw %"fir la-kyfin5<br />
dahhina dadlil 1-metnabmhu. (d) metnabrash &n men zalliqay kawkak, (e) akmii<br />
d-gadshi ba-shgi d-men dalqa da-lcel ddeq ayni da-lmt meneh. (3) w-hiikanna<br />
nuk saggi'e ak 'ammiid5 mettpen d-n*tin w-I-arC2 wa-1-yamrna. (4a) w-niM Mb<br />
saggi'atii methen b-lelya d-qaymin w-msattetiin, yattira'it b-s&w& (b) Men d-pehtiitii<br />
metqryfin w-'ammuqe, w-haggage saggiJe d-madmiiniye wa-&6rit&x3ye w-argwmye,<br />
(c) b-hay d-gawna map@ d-niir& kad 'am heshsh6k bir methallas gawne d-ak hden<br />
'abed. (5) w-mi d-bdeq nuhra hi dukktii panwiya d-pehtii 'am. (6) w-b-im2m8 man<br />
15 metlyzyiin hden nabrshatii mettul d-shemsha.<br />
(1) On 'dokides' or 'lampAdesl and & [belsusyitii] which acsematnight (pl.).<br />
(2a) Sulphureous exhalations rise from those phxwhkhhmein&em [d-it b-hen] a<br />
sulphureous substance [kyfina kebrithiyii] (b) and adhere to that air which has been<br />
moistened by the nocturnal coldness; (c) and thus that air is transformed into an oily<br />
[dahhinf~] substance which is easily kindled, (d) and iskindled@ the rays of rhe stars,<br />
(e) m happens with a a that (the lamp below) catches fire from the light of (the<br />
lamp) above. (3) Thus are seen many lights, like columns, falling both to the earth and<br />
to the sea. (4a) Many fires are also seen at night which are stationary and fid,<br />
especially in clear weather, (b) those called chasms and depths, and many illusions<br />
[haggage], blood-red, scarlet and purple [in colour], (c) because when the radiant<br />
colour of fire is mixed a little with darkness, it produces such colours. (5) When the<br />
light comes [?, bdeqp that place produces a 'phantasia' of a chasm. (6) These blazes<br />
are not seen during the day because of the sun.<br />
The section here as a whole is evidently based, as often, mainly on Mabwth and<br />
55 . Perhaps representing Arist. Me@. 342b 17 mvdv (see n. 58 below).