LANDSCAPE EVOLUTION
Nova Scotia has a rich diversity of landscapes not found in many
areas of comparable size in Canada.
The landscape surrounding Uisge Ban Falls is a product of
incredibly powerful forces which have shaped and reshaped the area
over 5 billion years. Formation of the earth's landmasses,
tremendous volcanic activity, collision of continents,
mountain-building, massive erosion and glaciation, have all played
a role in shaping Nova Scotia's landscapes.
Traditionally, the term "landscape" has been viewed as an artistic
or aesthetic concept, being an expansive area of scenery observed
from a single vantage point. Today, "landscape" is also used to
describe areas which have common patterns of topography (or
landforms) and vegetation. Individual landscapes may contain many
different landforms, each having its own characteristic or
particular mix of vegetation. The combination of a specific
landform and its associated vegetation is known as a "landscape
ecosystem". Thus, each landscape is composed of a recurring pattern
of landscape ecosystems.
Within the immediate vicinity of Uisge Ban Falls, you will
encounter three distinct landscapes: (1) The Cape Breton Boreal
Plateau, (2) The Interior Steep Slopes, and (3) The Central Cape
Breton Hills.
1. THE CAPE BRETON BOREAL PLATEAU
The Cape Breton Boreal Plateau is an extensive, elevated,
relatively level surface, which is bounded by steep, sometimes
cliff-like slopes and is surrounded by much lower lowlands. This
landscape has few lakes and is moderately dissected by slow-moving
rivers. Its generally well drained, shallow, sandy loam soils are
derived from very old granite, gneiss, and schist rock types.
As a result of its high elevation (300 to 450 meters above sea
level) and its being surrounded by major water bodies, the climate
of the Cape Breton Boreal Plateau Landscape is cool, moist, and
windy year round. This type of climate produces a "maritime boreal
forest". Unlike the continental boreal landscape of central Canada,
with its white and black spruce and jack pine forests, the Cappe
Breton Boreal Plateau Landscape is dominated by balsam fir. White
spruce, white birch, and mountain ash are minor but consistent
components of this landscape.
The two major landscape ecosystems of this landscape are the
well-drained gently undulating coniferous (balsam fir
forests)terrain; and the poorly drained flat coniferous(balsam fir,
black spruce forests) terrain.
2. THE INTERIOR STEEP SLOPES
The Interior Steep Slopes Landscape is a complex of steep canyons.
It forms the interface between the elevated Cape Breton Boreal
Plateau and the lower Central Cape Breton Hills landscapes. Major
river systems, such as the Baddeck River, originate in the boreal
plateau, plunge down the steep slopes (approximately 300 meters in
height), to eventually empty into the Bras d'Or Lakes. Soil and
rock types of this landscape are simliar to those found in the
boreal plateau - well drained shallow sandy loams derived ancient
granites, gneiss, and schists.
Major landscape ecosystems found in the Interior Steep Slopes
Landscape are steep-sided canyons with deciduous, coniferous, and
mixed forests. Dominant tree species include sugar maple, yellow
birch, beech, white spruce and balsam fir. Pockets of pure eastern
hemlock forests can be found along the lowers slopes of many of the
major canyons. Provincially rare and uncommon plants occur in the
canyons.
3. THE CENTRAL CAPE BRETON HILLS
The Central Cape Breton Hills Landscape, bounded to the north by
the steep slopes associated with the Boreal Plateau and to the
south by the waters of the Bras d'Or Lakes, is characterized by
rolling hills and large river valleys. The northern portion of this
landscape is dissected by the lower valleys of the Baddeck River
and the North River. Soils consist of deep, well drained sandy
loams developed from conglomerates and sandstones and of poorer
drained clay loams developed from shales.
Follow the trail through the canyon to arrive at the earth cache
site.
In order to log this earthcache, complete
the following and email me your answers:
1. Upload a picture of you and/or your GPSr at the upper plunge
pool (the top of the lower falls)
2. Estimate the total height of the falls
3. Describe the vegetation in the canyon near the falls.
(if you can't do the climb to the upper plunge pool, don't worry
about it...just a pic of the falls from the trail will do)