Bucks Earth Heritage GroupMilton Keynes Shopping CentreGrid reference: SP 857 390 (information office) Location: Central Milton Keynes shopping centre The shopping centre includes
building stones from all round the world in a setting that is safe and
accessible. The building stones have been cut and polished and therefore present
their geological information in its best light. Marks
and Spencer (floor area) There are floor inlays outside Marks and Spencer and along Sunset Walk (below). The red squares are a red granite (source currently not known), the white squares are a shelly limestone (the shell cross-sections are clearly seen), pink tiles of Peterhead Granite from Scotland and the dark blue rock in the outer ring is called Larvikite (an igneous rock known as syenite from Larvik in Norway). The shimmering of the blue crystals in this rock is due schillerisation of the feldspars (a kind of ‘un-mixing’ of the partially formed melt). A notable open textured travertine, full of holes (or vugs as geologists call them). The 'vugs' have occurred due to escaping gases. Travertine is a limestone formed in shallow, thermal waters with algal or bacterial mats forming.
Flooring
and garden containment of central walkway All the flooring of the
centre, the seating and the boxed areas around flower beds are formed of a
particularly good quality travertine (above). These areas show the layers of
algae and mud very clearly. The intricate form of the mats and also de-watering
structures and brecciation can be found in different sections. This is probably
the Italian source of travertine (about 40 million years old). Goldsmith’s A particularly deep blue form of Larvikite (similar to Marks and Spencer above, but slightly different mineralogy). MacDonald’s Without doubt the best quality
travertine in the centre. The layers of mud and algae are well defined as well
as the brecciated horizons where the sediment was ripped up by storms or
influxes of water. House
of Fraser Good quality travertine again
at this second store location. BHS A pink marble which is highly fractured (below).
Several shops show this
brecciated limestone - the rock is made up from an earlier limestone (grey
pebbles) which has been cut through with veins and then this was broken up and
re-cemented into this rock, presumably as part of a sea-floor mass movement -
source unknown.
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