Rock 365 : Day 151 : Pseudotachylite

20100531

Day 151 : The dark, fine-grained rock in the centre of the image is
pseudotachylite. Literally a ‘false’ tachylite (basaltic glass), a
pseudotachylite is formed when frictional heat from earthquake
faulting melts the host rock which then chills instantly forming a
glass. The host rock here is a biotite acid gneiss from the quarry at
the west end of Lock Tollie, Gairlock, Scotland. Keele collection.

Leave a Reply

Your email address will not be published. Required fields are marked *

You may use these HTML tags and attributes: <a href="" title=""> <abbr title=""> <acronym title=""> <b> <blockquote cite=""> <cite> <code> <del datetime=""> <em> <i> <q cite=""> <strike> <strong>