| Ecosystem
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Slow and Sluggish:
Because their marine openings are so constricted,
the Lakes have an extremely low rate of
water circulation. It can take up to 2 years
for water to be flushed into the sea, and
in some inner bays and coves, far from the
marine interface, the flushing rate slows
to an astonishing 40 years! Although the
year-round population of the Bras d’Or
region is relatively small—less than
15,000 people – the Lake’s slow
flushing rate means that small amounts of
pollution can add up to big water quality
problems.
Bras d’Or
Basics
The highly irregular shoreline
of the Bras d’Or Lakes is 1,234 kilometres
long. About 13% is rock and about 27% lies
along the Lakes’ narrow channels.
The “main lake”
of the Bras d’Or, situated in the
south-central part of Cape Breton, is connected
to the Lakes’ channels by the small
Barra Strait.
The Great Bras d’Or
Channel to the northeast (only
320 metres wide in its narrowest stretch)
is the Lakes’ main source of seawater
inflow and lakewater outflow. There is a
net inflow of seawater in the subsurface
layers and a net outflow of fresher water
on the surface layer.
The salinity of
Bras d’Or surface waters varies from
29 parts per thousand at the entrance to
Great Bras d’Or to 20 -21 parts per
thousand at the east end of East Bay. Sheltered
bays connected to rivers that drain into
the western part of the Lakes have even
lower salinity levels.
There is no natural connection between
the Lakes and the Atlantic Ocean to the
southwest. A man-made connection
has existed since 1869, when the St.
Peter’s Canal was completed
through an isthmus at St. Peter’s
Bay.
Salinity levels
in the Lakes depend on rain run-off, depth,
stream drainage and proximity to the northern
sea connections.
The Lakes are underlain by
sedimentary rock, composed mainly
of shale, sandstone, gypsum and salt. Deeper
areas are floored by mud, with more exposed,
shallow areas covered in gravelly glacial
till.
Tides in the Lakes
range less than half a metre; tidal currents
in the entrance to Great Bras d’Or
average 4 -5 knots. Non-tidal currents are
weak.
Much of the Lakes are covered by
ice in winter.
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