Natural History of Nova Scotia, Theme Regions
400 Atlantic Interior
 
         
410 Quartzite Plains
 
411 Southwest Schists
412 Mersey Meadows  
413 Quartzite Barrens  
420 Slopes and Ridges
 
421 Sissiboo Lowlands
422 South Mountain Slope  
423 Slate Ridges  
 
430 Drumlins  
431 Annapolis Drumlins
432 Ponhook Drumlins  
433 Kejimkujik Drumlins  
434 Lunenburg Drumlins
435 Eastern Shore Drumlins  
436 Headwater Lakes  
 
440 Granite Barrens  
 
450 Granite  
451 Granite Uplands
452 Shelburne Granite Plain  
453 Granite Ridge  
 
460 Bays  

 

Museum of Natural History

452 Shelburne Granite Plain

Geology | Fresh Water | Soils | Plants | Animals
Cultural Environment | Sites of Interest | Topics & Habitats

400 region map - click to enlarge

Geology and Landscape Development
This Unit presents a typical granite terrain, hummocky and covered with large boulders. The elevations are low, in keeping both with its position on the planation surface and with the fact that the granite body is probably not fully exposed.

The surface has a mantle of thin, stony till with no drumlins.

upFresh Water
Great Pubnico Lake, the largest body of water in this Unit, is the
Shelburne Barrens
Shelburne Barrens
Click to enlarge
headwater for the Barrington River. Smaller lakes are dispersed throughout and connected by a network of streams and rivers. Scattered medium to large wetlands tend to be associated with the larger watercourses. There are concentrations of sloped and raised bogs. Conductivity averages 35 micromhos/cm, and pH ranges from 4.7 in the Clyde River and Great Pubnico Lake to 6.5 in Alvin Lake.

upSoils
Soils in this Unit have developed from various parent materials - granite, quartzite, and schist. Large areas are poorly drained, either because of topography, shallow depth to bedrock, or the presence of a cemented ortstein layer. Sand plains are common. In the Yarmouth County corner of the Unit, Gibraltar, Bayswater, and Aspotogan soils - all derived from granite - occur with patches of peat. In the rest of the Unit, poorly drained Bayswater and Aspotogan soils, and imperfectly drained Liverpool and Danesville soils, each often gleyed and mottled, are dominant on the largely level topography towards the coast, with some areas of better-drained Medway, Mersey, and Port Hebert soils where the relief is more pronounced.

upPlants
This Unit is the most southerly portion of Nova Scotia not directly affected by the cold and fog associated with the Atlantic Coast. The growing season is hot and subject to drought on shallow soils. The natural vegetation appears to have been White Pine and Red Oak, but repeated burning has reduced many of the pine sites to a shrub cover of cinquefoil, Bearberry, and Broom-crowberry, with scattered Black Spruce. Black Spruce predominates on ill-drained lands, while Red Oak covers the ridges. Eastern Hemlock and Red Spruce are found in the few unburned areas. The warm climate is indicated by the presence of plants which otherwise occur no further north than southern Maine, for example, Inkberry.

upAnimals
The barrens do not provide productive wildlife habitat, and this Unit has the lowest small-mammal diversity in the Region, with no more than four species commonly occurring. It does, however, support one of the best moose populations in western Nova Scotia. Typical freshwater fishes include Brook Trout, Yellow Perch, Brown Bullhead, and Golden Shiner.

upCultural Environment
Much of this area is barren as a result of repeated fires. Around the turn of the century, meadows in southwestern Nova Scotia were burned annually to promote hay growth, and barrens were burned periodically for production of blueberries. Although there were fewer forest fires than today, they were often unattended unless they threatened settlements and therefore burned much larger areas. From 1900 to 1914, more timber was lost to fire, disease, storms, and old age than was harvested. Barren lands of the Shelburne Granite Plain feature significant moose populations that attract seasonal hunters.

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upSites of Special Interest

  • Many eskers along the shoreline, along Clyde River and north of Clements Pond

Provincial Parks and Park Reserves
Proposed Parks and Protected Areas System includes Natural Landscape 8c.

Associated Topics
T2.3 Granite in Nova Scotia
T3-4 Terrestrial Glacial Deposits and Landscape Features
T9.1 Soil-forming Factors
T10.1 Vegetation Change
T11.10 Ungulates
T12.10 Plants and Resources

Associated Habitats
H4.1 Bog
H5.1 Barren
H6.2 Softwood Forest (Black Spruce, Larch Association; Spruce, Hemlock, Pine Association)
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