CYNGOR
CEFN GWLAD
CYMRU COUNTRYSIDE COUNCIL FOR WALES
SITE OF SPECIAL SCIENTIFIC
INTEREST: EXPLANATORY GEOLOGICAL NOTE
SITE NAME: SGISTIAU GLAS YNYS MÔN
UNITARY AUTHORITY: ISLE OF ANGLESEY
The purpose of this note is to
describe the nature and importance of a site, avoiding specialist
terms, for
the site owner and/or occupier. This note does not form part of the
formal
notification documents.
Sgistiau Glas Ynys Môn, Anglesey
This site consists of three
individual localities which have been selected to illustrate key
features
associated with a rare type of rock called a blueschist. The
blueschists on Anglesey
are Precambrian in age and are amongst the
oldest such rocks known in the world. They form a narrow NE-SW-trending
belt
across southern Anglesey,
with the main area
of blueschist centred around Llanfair P.G. and extending towards
Llansadwrn.
These rocks are of international importance and have been of interest
to
geologists since Reverend Blake first described them in 1888.
Blueschist is a
type of metamorphic rock, which means that it has been changed or
altered in
some way. Minerals crystallize at specific temperatures and pressures
which
provides geologists with important clues about how the rocks were
formed. In
this case, the sediments and basalts on an ancient ocean floor were
buried
quickly and subjected to high pressures, whilst remaining at relatively
low
temperatures. If the original sequence of rocks (protolith) was buried
further
the
temperature and pressure would
increase, changing the mineralogy. This type of relatively rapid burial
occurs
at plate margins when oceanic crust slips underneath continental crust.
On
Anglesey this process occurred some 590-580 million years ago and can
be
compared to processes that are currently operating along active plate
margins
such as those along western North
America.
Other examples of ancient blueschists from around the world can found
in California, Japan
and Corsica and, as in the case of the blueschist on Anglesey,
normally occur in long linear zones that define ancient plate
subduction
boundaries. The preservation of such ancient blueschists is a rare
occurrence
and the Sgistiau Glas Ynys Môn SSSI is an internationally
important site
providing an excellent opportunity for geological research. The rock
exposures
allow geologists to study the mineralogy of the blueschists, in
addition to
contributing to the understanding of the tectonic evolution of Anglesey
and Northwest Wales.