Natural history -- Scotland -- Orkney; Orkney (Scotland) -- Description and travel; Orkney (Scotland) -- History
As we resume our way along an undulating road, we pass through a district
which, despite its northerly exposure, seems able to support a large
population, and numerous tidy cottages cluster here and there along the
roadside. By-and-by the cultivated strip becomes narrower, the sandy
beach of Aikerness gives place to the rocky shores of Burgar, and the
road turns inland with a steep incline to dip down on the other side of
the ridge towards the Loch of Swannay.
Here we shall find it well worth our while to make a somewhat longer halt
than before, and, leaving our bicycles, we turn to climb Costa Hill, and
to view the wild cliffs at Costa Head. From the hill we look down upon
the mysterious green islet of Eynhallow, the “Holy Island,” where the
ruins of an ancient monastery have been traced, and round which more than
the usual crop of legends has sprung up. A fair contrast it offers to the
bold, rocky cliffs of Rousay just beyond.
If it happens to be the time of spring tides, and the ebb is running
out, we shall see at this place one of the most impressive sights which
our coasts present. However calm be the sea, as soon as the tide begins
to gather strength, the channels on either side of Eynhallow for some
distance out to sea become a mass of heaving, foaming billows, reminding
one of the long stretch of boiling rapids below the Falls of Niagara.
And that is just what this “roost” is—rapids on the course of the tidal
river which is now sweeping westward through Eynhallow Sound. When we
look at our pocket map, we see that on each side of the islet the depth
of water is only about five fathoms. In about a quarter of a mile it
becomes ten fathoms, and within a mile of the west end of the island
twenty fathoms. Thus the tidal river first passes over a ridge on each
side of Eynhallow, where it is less than thirty feet deep, and then
plunges down a slope which dips nearly one hundred feet in a mile.
If there is a long swell rolling in from the Atlantic, as there often is
on our western shores, the turmoil is increased, and the boiling fury of
Burgar Roost, as it is called, is a sight which it is worth going far to
see. The roost which is formed in Hoy Sound with a strong ebb-tide is due
to similar causes but there the dip in the sea-bottom is not so steep.
When the tide turns, the change seems almost magical, and in a short time
there may be not a ripple on the water to mark the scene of this mad
dance of the billows.
[Illustration: _Birsay, the Barony._]
The cliffs at Costa Head are the highest on the Mainland, but we can only
see them from above, and thus we lose much of their wild grandeur. We
enjoy, however, an impressive view of the cave-pierced shores of Rousay,
and of the stern ramparts of Noup Head, in Westray, with its sentinel
lighthouse.
Public-domain text, read in full here on John Shaqi.
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