 453
Granite Ridge

Geology and Landscape Development
The Granite Ridge along the Eastern Shore forms a prominent feature 80
km long and about 8-10 km wide. It rises sharply, sometimes with cliffs,
to a narrow plateau 100 m above the Atlantic Coast Region (see Figure 27).
The granite has been cut by faults in two places: along the valley
from Spider Lake through Lake Major, and along the Porters Lake valley.
The Musquodoboit River also cuts across it in a narrow gorge and
must have been superimposed by downcutting since the Cretaceous.
The surface of the granite has a thin veneer of coarse granite till
which, at the eastern end of the ridge, is overlain with a few drumlins of
red Lawrencetown Till (Wolfville soils). These have spilled over from the
area of the Eastern Shore Drumlins (sub-Unit 435a) to the north.
Fresh Water
The surface-water coverage in this Unit is very high,
 | Musquodobit River Click to enlarge |
with many irregularly
shaped lakes and long narrow lakes and rivers following fault lines. A few
small, scattered raised bogs and fens are found. Parts of the
Musquodoboit River are bordered by large wetlands. Conductivity
averages around 42 micromhos/cm, and pH ranges between 4.7 and
6.8.
Soils
Gibraltar soils (well-drained, gravelly, sandy loams derived from granite)
are dominant, with large areas of exposed bedrock and small areas of
imperfectly drained Danesville soil and peat bogs.
Plants
This Unit is somewhat cooler in summer than Unit 451 and has a climate
quite similar to Unit 452. Red Spruce, Balsam Fir, birch, Eastern Hemlock,
and White Spruce are common species on well-drained sites. Black
Spruce, Balsam Fir, and Larch occur in wetter areas. Parts of the Unit are
semi-barren. Scattered Red Oak occurs around the Lake Charlotte area.
Shade-intolerant birch and aspen colonize burnt areas.
The ruggedness and effects of repeated burns, which still continue,
were well described by C.D. Howe, writing in 1912: "The crests of the
granite hills east of Halifax harbour have been deeply eroded by glacial
action and have naturally very thin soils; and frequent fires have so
exposed the rocks, that from a distance most of the rounded domes
appear white. When not burned, they are sparsely covered by a black
forest, that is, coniferous, in striking contrast to the lighter green of the
hardwoods prevailing on the lower slopes. The higher slopes, especially
when facing southward are covered with spruce overtopped by scattered
white and red pine. The hardwoods go nearly to the top on the northerly
-facing slopes. The low ridges usually support pure hardwoods. Red
spruce prevails in the broader flats between the ridges, while hemlock
predominates in the ravines and gullies, and at the base of steep slopes
along the rivers and smaller lakes."
Animals
There is little recorded information about terrestrial animals in this Unit.
Fish species include White Sucker, Brook Trout, White Perch, Gaspereau,
Yellow Perch, Brown Bullhead, Banded Killifish, and shiners.
Cultural Environment
Forest management predominates in this area. However, farming has
also been important in the Musquodoboit Valley. Other resource-based
industries here include Christmas tree farms. The Waverley Game
Sanctuary spans part of the Granite Ridge. Seasonal hunting is common
in this area.

Sites of Special Interest
Provincial Parks and Park Reserves
Proposed Parks and Protected Areas System includes Natural Landscape
34 and Candidate Protected Areas 19 Tangier Grand Lake, 20 White
Lake, and 22 Waverley-Salmon River Long Lake.
| Associated
Topics |
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| T2.3
Granite in Nova Scotia |
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| T3-2
Ancient Drainage Patterns |
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| T12.11
Animals and Resources |
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| Associated Habitats |
| H4.1
Bog |
| H6.1
Hardwood Forest (Maple, Oak, Birch Association) |
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