289 
Scotland^ near Cork and Dublin, Ireland ; and Silesia, Germany. This sea 
was still in existence at the time when the greater part of the Carboniferous 
rocks of America and Dussia, as well as those of the North of Ireland, and of 
the neighbourhood of Tournai, of Deluy, of Soignies, and of Comblain-au-pont 
of our country, had already emerged, and when the Fauna which they enclose 
had been for the greater part destroyed. 
