By David Leather
Sand
Composition
Bay of Grobust after storm winds
have blown sand onto surrounding grassland, July 2006
Bay of Tafts, like Grobust, is
almost entirely shell sand, including a few micro shells of
foraminifera
Sand extraction and erosion has
reduced the dunes behind Mae Sand
The beaches of Westray and areas
of wind-blown sand deposits
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Sands of Westray

Sandy Beaches
There are seventeen wonderful almost white sandy beaches on Westray, plus a few
minor ones. Grobust sands, being near to Pierowall is a favourite and is
especially attractive when large green waves roll in one after the other from
the north. Mae Sand is wild and beautiful and faces south. Bay of Tafts and
Links of Garth form clean curves of white sand, while the white sands of Bay of
Skaill make a fine place to contemplate the beauty of the island with Papay on
the horizon. Sand o’ Gill, the Ouse and Bay of Tuquoy are quieter bays with huge
areas of sands uncovered at low tide. Local people know well the properties of
beach sands, whether good to sweeten the soil, or to make decent concrete or
mortar, and where to obtain it.

The composition of the
beach sand varies greatly between shell and quartz sands. There is no simple
explanation why one sort of sand should be restricted to one beach and not
another, though the quieter bays have quartz sand, and the beaches facing the
open sea tend to be shelly. However the Bay of Tuquoy and Mae Sand both face the
same direction and are only a mile or so apart yet the sands are very different.
The quartz sand is a medium to fine sharp sand, individual sand grains
showing slightly rounded corners. This reflects erosion of Westray flagstone
that originated from river sand, then in recent times has been worn to some
extent by the sea. Really sharp sand will squeak when you scuff it with your
foot. The graph will tell you which beaches have whistling sands. The sand
derived from shell material is slightly coarser but mixes readily with the
quartz sand. The dunes and most of the sand that has been blown inland is of the
shelly type.

Sand dunes and wind-blown sand
Several Westray beaches are backed by sand dunes and some have wind-blown sand
extending far inland. Behind Mae Sand there are thick beds of sand, now largely
covered with vegetation, that extend as far as Netherwood House, South Hamar and
Tuquoy. Immediately behind the beach, the high dunes have been exploited for
sand extraction and are now deeply eroded. Much of the area is now a nature
conservation site and lyme grass – a species similar to marram grass – is
helping to keep the sands in check. In the Grobust Bay area wind-blown sand
extends as far as Pierowall and northwards across the Links to Quoigrew. These
are the two most extensive deposits, though many of the other beaches are backed
by dunes or beds of sand, especially behind the Bay of Tafts where sand reaches
beyond the main road where the Old School is. Around the Bay of Skail there is a
200m belt and most of Westray’s airport is on this sand bed.

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