Euryptericl Remains in Garhoniferous Shales of Scotland. 509 



hasso-relievo markings on adjoining part, exliibited in Museum 

 of Science and Art, Edinburgh. 



6. Shore West of Dunbar. — In red and green sliales a leg 

 of Eurypterid was found by the Survey collector. In collec- 

 tion of Geological Survey of Scotland. 



7. Several narrow body segments of an Eurypterid in 

 collection of E. Dunlop, Whiterigg, obtained from' the Coal- 

 measures of the neighbourhood. 



8. Hailes Quarry. — From the black bituminous shale above 

 the sandstone, obtained by Dr Macfarlane of the Botanic 

 Gardens during the last tirring of that shale in 1878, shown 

 to me by C. W. Peach, to whom it had been sent for deter- 

 mination. 



9. Left Bank of the Water of Leith, hetvjeen Reclhall Mill 

 and Colinton Tttnnel in the cutting of Balerno Eailway. — A 

 large piece of Eurypterid skin was found by the Survey 

 collector. It was remarkable from spine-like projections all 

 over the surface. Collection of the Survey of Scotland. 



10. Shore at Methil, Fife. — A small portion of Eurypterid 

 found by J. W. Kirkby, and determined by Dr Woodward. 

 Obtained from the red beds above the Coal-measures of Fife. 

 This is the highest position in which Eurypterid remains 

 have been found in Scotland. 



1 1. Fragments of Eurypterid described by Sir W. Dawson 

 as the skin of one of the reptiles whose bones and teeth were 

 found in a tree-stump — shown by Mr Peach to be Eurypterid 

 at page 443 of this volume. 



12. Calderwood Cement Stone, East Kilbride. — Piece of 

 Eurypterid skin well marked, with embossed crescents. 

 Collection of J. Coutts, now in Museum of Science and Art, 

 Edinburgh. 



13. Banks of the River Tweed at Lennel Braes. — Portion of 

 Eurypterid skin described and figured by Mr Peach in 

 Trans. Roy. Soc. Edinb., xxx., 523. 



14. Hunterian Museum College, Glasgow. — Several pieces 

 of Eurypterid skin from Kimmerghame Quarry, Berwickshire, 

 presented by Mr Stevenson of Duns; probably parts of 

 E. Stevcnsonii. 



