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One coastal landform resulting
from both the constructive and destructive forces of the ocean
is a spit. Spits are elongate ridges of sand or gravel that project
from land and end in open water. The development of spits is
mainly related to a type of wave-induced current called a longshore current. A longshore
current is caused by waves that strike the beach diagonally,
and as a result, move sediment parallel to the shoreline. Such
wave action along the shore will erode and carry particles until
they reach the tranquil, deep waters of bays, estuaries or the
open ocean. The particles are then dropped and deposited due
to a decrease in velocity. Spits are essentially seaward continuations
of beaches and will
continuously expand in the direction of the longshore current
unless other water motions or human influences interfere with
the growth process.
Newfoundland has a number of spits like this one (ABOVE
and RIGHT) that formed along the province's western shore.
Flat Island is a 12-kilometre-long spit that is anchored to the
coast at Youngs Cove. It was formed as sand and gravel drifted
north from eroding coastal cliffs. The northeast end (RIGHT)
hosted one of the province's earliest settlements, known as Sandy
Point.
Toronto also has a well-known spit, the Leslie Street Spit
(now called Tommy Thompson Park), which was not formed by ocean
forces, but is an artificial landform that juts into Lake Ontario
at the southern end of Leslie Street. This five-kilometre-long,
471-hectare geographical feature (BELOW),
which was formed by the disposal of hundreds of thousands of
tonnes of construction waste, rubble and other waste sediment
into the lake, is the largest (and still expanding) lakefill
along the Toronto lakeshore. Natural forces have managed to transform
the spit into an urban plant and wildlife refuge. (For more on Tommy Thompson Park, visit www.trca.on.ca/ttp.html.)
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(Newfoundland
spit images provided courtesy of the Geological Survey of Newfoundland
and Labrador, Newfoundland Department of Mines and Energy. Their
website can be found at:
www.geosurv.gov.nf.ca/) |
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