also in the contact aureole of the Land’s End granite. There, it is part of the retrograde skarn assemblage including stanniferous epidote, cassiterite, amphibole, titanite/malayaite and chlorite and overprinting earlier grossular/andradite-rich skarn (van Marcke de Lummen1986). ...
When bend- ing small tin bars (Fig. 2), one notices a peculiar sound which is known as the tin cry. The latter results from the friction of small crystallites in the β -modification. A sound reception of the tin cry can be obtained from the internet [4]. The bending of a tin ...