The mountains of Newfoundland, the Maritimes, and the Gaspe Peninsula in
Quebec are part of the main mountain system of eastern North America, the
Appalachian mountains. Appalachians are remnants of ancient mountains
that rose between 480 and 300 million years ago, when Africa first collided
with North America. It is hard to find jagged peaks in Estern Canada, so
characteristic for Rocky Mountains, the signature mountain range of North
America. The Appalachians were already well developed before the Rockies
started to form about 100 million years ago. Over a long period of time,
the eroding power of ice and water made the peaks of these eastern mountains
smooth and well rounded. Once buried under more than a kilometre of ice,
the mountains of the east coast are literally rising from the sea as they
rebound from the weight of their recent ice cap.
The Long Range Mountains are the central feature of the Western Newfoundland
Highlands, sloping gently toward the Atlantic to the east, and dropping
sharply toward the narrow coastal plain along the Gulf of St. Lawrence to
the west. The
highest elevation of the range, at 814 metres, is an unnamed peak in the
Lewis Hills located only 6 kilometres from the ocean coast.Tablelands, on
the west coast of Newfoundland, is a striking 600 metre high plateau of
molten rock that penetrated the Earth crust. The Table Mountain in
Gros Morne National Park is made of peridotite, rock that is found in the
mantle of the Earth. There are only a few places in the world where the
mantle rock can be found on the surface, an oddity on the landscape that
provide scientists with valuable information on the Earth's structure. Here
is where the geologists and hikers can enjoy an easy "journey towards
the centre of the Earth".
Peridotite rock contains largely iron and magnesium
silicates which are inhospitable to plant life - hence the barren landscapes
of the Table Mountain. Because of this and many other unique geological
features, Tablelands and surrounding area have been designated as a World
Heritage Site, and protected within the boundaries of the Gros Morne National
Park.
Cape Breton Highlands in Nova Scotia is a place "where the
mountains meet the sea". The Highlands are the most spectacular part
of the Maritime
Acadian Highlands, eastern extension of the Appalachian mountains. With
an elevation of 532 metres, the highest peak in the Highlands is White Hill,
located 17 kilometres west of Ingonish. Rising high above the nearby sea,
the Cape Breton Highlands provide spectacular views of the Gulf of St. Lawrence
and the Acadian forests of maple and birch, blazing in late fall colours.
Ancient fern forests led to formation of thick layers
of coal deposits, now harvested from the depths of Cape Breton. Modern lush
conifer (containing red and white spruce, and balsam fir) and hardwood forests
(white and yellow birch, American beech and sugar maple) along deep valleys
bear the impact of human habitation too, as they have been cut and stripped
more than once throughout history. Nevertheless, in spite of the long human
interference with these natural systems, Cape Breton Highlands can still
offer a true wilderness experience.
The steep, grey-white limestone cliffs of Cap Bon Ami and Cap Gaspe on
the tip of Gaspe Peninsula, lie at the tip of the northernmost continental
reaches of the Appalachian mountain chain.
Appalachians extends southward over 2000 km into Vermont and New Hempshire,
and reach as far south as Georgia.
Visiting Forillon National Park offers the best opportunity to experience
the ancient Appalachians being slowly eroded away by the relentless action
of ocean waves. The mountainous interior of the Park provides numerous hiking
trails through dense mixed forest of sugar maple, birch, white pine, and
eastern hemlock. On higher elevations mixed boreal forest is dominated by
conifers, such as white and black spruce, and balsam fir. The Park is well
known for its abundance of marine mammal and birds. Look for seals basking
in the sun along the coast.
A short drive away is the Bonaventure Island, one of many Migratory Bird
Sanctuaries found in the area, that supports a large colony of gannets,
common murres and an occasional puffin. Cliffs and narrow ledges provide
home to gulls, black guillemots, razorbills, double-crested cormorants and
black-legged kittiwakes.