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Quiz
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The
Parks / Ontario
/ Bruce
Peninsula National Park
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During the Silurian Period
and the Paleozoic Era, 400 million years ago,
this area was covered by an inland sea where
the skeletons of underwater corals and other
sea creatures formed layers of calcium-based
sediments on the sea floor. As the water began
to recede, the dolomite bedrock of the peninsula
was formed by the compression of these calcium
layers to form limestone, which then combined
with magnesium from the sea. After thousands
of years of water erosion, the softer lower
rock beneath the caprock was undermined and
huge segments broke across straight fault lines
to create the topography of the Niagara Escarpment,
the backbone of the peninsula. Similarly, the
much smaller flowerpot and pillar formations
along the shoreline, and the coastline and karst
caves are molded by wave action. The largest
shoreline cave on the peninsula, the Grotto,
is accessible underwater. Over 7 kilometres
of karst caves have been mapped in the park.
Ontarios Great Wall is now
a World Biosphere Reserve - an international
designation that promotes a harmonious relationship
between people and their environment.
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