51124 P1190312

180 JwBiCahtuuk

prodnccd Śijpifićant amount of resin. Thosc resins in typical condmoos «">» j fonrsj. \khere ta) len trees decompose in atmosphcre, ha\ing acces 10 fc* J tn\« chance to be preserv cd for too long. As for the Tematy forem of SBB one morę fictpr arose: laige river. which swept away fal len resoots |9 tbem and accutnulaied huge deposits of theni in its delta in tbe nrin—J ved of the air (Kasiński, Tbłkanowicz 1999: 42). Those condilions ledic ■]

mioon of resin into fossil resin. That process, from the physical-cheoscś ;e> I ń\« i scrapułousły described by the specialists (Kostno** ska-Cerancw et Ig;. I Fossil resin bas some qualińcs. which we may secm self-contradian i sobd stntcture and simultaneously Iow specific gravity (“light stoaaltia I transparent. usuallv of yellowish colour (a słone which is easy to beproctatc: I tłammable ("buming słone”, comp. German namc of it: Bernstein). WKkitej I itreteases intensivc odour (ground amber is one of the incense iaprifaii

.1. TEKTIARY DEPOSITS

l*$ discovered so far at least two hugc dcłtas wiifa i IHIKr    one occupied the area of the contemporaty Gulf of

^ ńver (Fig. 2), which ended its course there was called tbe Erida-

_<|f__ 1999). The other delta was dison-cred later and covef5ihe

Ukrainę (Kasiński. ToBcanowicz 1999). Lct us conccntrae here of the inentianed areas.

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