Lubec, ME
The coastal area of Maine holds many secrets. Those
little out-of-the-way places where nature has shaped life in
strange and different ways. We found one of these while seeking
the easternmost point in the continental United Sates. Our search
brought us to the small community of Lubec. Driving for several
miles down a poorly marked road brought us to the West Quoddy
Head Lighthouse at the east end of the Quoddy Head State Park. This can be a pretty exciting
piece of real estate. The waters off West Quoddy Head peninsula
form part of the open end of Canada's Bay of Fundy, which lies
between New Brunswick and Nova Scotia. The shape of the Bay of
Fundy causes extremely high tides. At West Quoddy Head, tides
rise and fall an average of 15.8 feet in six hours. The cool
nutrient-rich waters host abundant marine life in the large intertidal zone. Northern types of
seaweed are found here, along with arctic clams and snails,
anemones and sea stars. Quoddy Head State Park, located on the
peninsula of West Quoddy Head is the easternmost point in the
United States. Steep rock cliffs, a peat bog and trees shaped by
harsh winds characterize the park's environment. West Quoddy Head
is wrapped in fog for an average of 59 days a year and has some of
Maine's coolest summer temperatures. Over time, these
temperatures, a moist climate and the area's topography created
conditions for the formation of a coastal peat bog. A park
feature typical of maritime eastern Maine and New Brunswick. The
park's cliffs are remnant of marine volcanoes that erupted 420
million years ago and now form the bedrock of much of coastal
Maine and New Brunswick. The horizontal volcano layers were
tilted almost vertical along the Pundean fault - a fracture in
the earth's crust that parallels the coast just off the park's
shores. Glacial scouring and the battering surf have carved the cliffs which
are 90 to 150 feet from the sea. The park has several hiking
trails, of varying degrees of difficulty, without climbing
anything more difficult than stairs. The terrain is thick with
trees and rocks and every turn greeted us with yet another
awesome sight. We took the trail that led to the only preserved
Peat bog on the Eastern Coast, and the only one we had ever seen.
West Quoddy Head
Bog has evolved through a slow process of plant growth and decay
over the past 8000 years. Conditions for the bog's formation
began when a glacier left a large submerged basin on West Quoddy
head peninsula. Most of the water eventually receded, leaving a
deposit of glacial and marine sediment. Fresh water from rain and
snow filled the basin to form a pond and gradually algae, pond
weeds and other aquatic plants grew. As these plants accumulated
and decayed, the pond area filled. Once the pond was filled,
sphagnum moss
and rooted plants began to grow. Drainage was impeded and the
retained water inhibited the complete decay of plant material
turning it into Peat. Peat in its natural state is about 90%
moisture and 10% organic matter and is the first stage in the
formation of coal. Peat has been valued by people for centuries.
It is used mainly for fuel especially in Europe, where it has
been widely harvested and processed. Because it is so absorbent,
peat is also used as a soil additive, surgical dressing , animal
bedding and a filtration material for septic systems. The Peat is
quite fragile and a footprint in it may last as long as two
years. Because of its unusual environmental condition of high water
and low quality nutrients, a strange assortment of plants have
adopted to its domain. They each have had to adapt to the
conditions and acquire the required nutrients in other ways or
suffer the effect by creating a dwarf version of themselves. The
Pitcher plants eat insects to obtain essential nitrogen and
proteins they cannot find any other way. Pitcher plant leaves
have nectar glands that attract insects. The cone shaped leaves,
lined with downward pointing hairs, also form a natural insect
trap. When an insect climbs inside the plant, the hairs prevent
its escape. Eventually it falls into water which has accumulated
in the base of the leaf and is digested by the plants secreted
enzymes. It took about an hour to walk to the bog, see it, and
return. I would put this one high on the nature lover's list.
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