176 Mr. WiTHAM on the Red Sandstones of Berwickshire. 



TABLE. 



Succession of the Strata of the Coast of Northumberland, from the Red Sandstone Rock' 

 of Scremerston Mill-house, to the great Formation of Red Sandstone between Scremerston 

 and Berwick. 



Sandstone (Red), dip 26 degrees. 



Shale, dip 34 degrees. 



Limestone. 



Shale. 



Limestone, dip 30 degrees. 



Shale. 



Sandstone, dip 24 degrees. 



Shale. 



Limestone. 



Shale, dip 32 degrees. 



Sandstone, dip 36 degrees. 



Shale, with Girdle Beds, and Iron Stone. 



Limestone, dip 36 degrees. 



Shale. 



Limestone, dip 38 degrees. 



Girdle Beds. 



Limestone. 



Shale. 



Sandstone, with Variolaria. 



Shale. 



Sandstone. 



Shale. 



Sandstone. 



Shale. 



Sandstone, and Girdle Bed. 



Shale. 



Limestone. 



Sandstone (Red). 



Shale. 



Sandstone (Red). 



Shale. 



Sandstone, dip 36 degrees. 



Sandstone of a deep red colour, of great thiclmess, dip in one situation 46 degrees, 

 direction north and south. This stratum appears to continue all the way to 

 Berwick. A Red Sandstone, apparently one of the beds of this rock, is seen 

 cropping out under Tweedmouth Church, its direction nearly north and south, 

 and dip 30 degrees east, this appears to be the same rock upon which Berwick 

 Castle stands. The dip of the beds below Berwick Castle, is 48 to 50 degrees 

 east, and the direction north and south. 



By this digression, the various alternations of the Red Rock with the 

 Shales and Limestones from Fenwick, nine and a half miles south of 



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