Natural History of Nova Scotia, Theme Regions
500: Carboniferous Lowlands
         
510 Till Plain
 
511 Windsor Lowlands
512 Salmon River Lowland  
520 Coastal Plain
 
521 Northumberland Plain
522 Judique Coastal Lowland  
523 Tantramar Marshes  
530 Stony and Wet Plain
 
531 Sydney Coalfield
532 Chignecto Plains  
540 Clay Plain
 
550 Coastal Fringe
 
551 Inverness Coastal Plain
552 Victoria Coastal Plain  
560 Submerged Lowland
 
570 Rolling Upland
 
571 Mulgrave Plateau
572 St. Marys Fault Block  
580 Hills and Valleys
 
581 Cumberland Hills
582 Pictou Valleys  
583 Antigonish Uplands
584 Ainslie Uplands  
585 Iona Uplands  
590 Dissected Plateau
 
591 Margaree Plateau  
592 St. Lawrence Slopes  

 

Museum of Natural History

540 Clay Plain

Geology & Landscape | Fresh Water | Soils | Plants
Scenic Quality | Cultural Environment | Sites of Interest
Topics & Habitats

500 region map - click to enlarge

District 540 is divided into two sub-Districts:
(a) Cogmagun River
(b) Stewiake Barrens

Geology and Landscape Development
In the two sub-Units within the Clay Plain (District 540) are found Middle to Late Carboniferous deposits of Canso and Pictou strata (see Figure 11). These strata are predominantly fine red or grey-brown sandstones and siltstones, known as the Scotch Village Formation, which lie horizontally on top of the Windsor deposits.

upFresh Water

Cogmagun River (sub-District 540a)
This area contains the headwaters of the Tomcod, Walton, and Cogmagun rivers. It falls within three tertiary drainage areas, including a portion of the Kennetcook River watershed, and drains into the Minas Basin. The several extensive wetland systems include Collins Bog and McDonald Bog, both of which are larger than 400 hectares.

Stewiacke Barrens (sub-District 540b)
This landscape is within the Shubenacadie River watershed and contains numerous tributaries that feed into the Stewiacke and Shubenacadie systems.

upSoils
The soils in this Unit are mainly of the Kingsville series - poorly drained clay loams, usually strongly mottled, that have formed from till deposits derived from grey sand and siltstones. Large areas of peat have developed in level and depressed areas.

upPlants
This clay till plain with scattered mounds supports mostly Black Spruce, with some Red Oak and Balsam Fir. On the better-drained gravelly ridges, Red Pine (on burnt sites) and the shade-intolerant Red Maple and White Birch occur.

upScenic Quality
These featureless plains have some of the lowest scenic ratings in the province. With little relief, few lakes, and no human settlement, the only variation is provided by bogs and extensive cutover areas (in District 540a). There is little public access to these areas; the only paved road is south of Middle Stewiacke (District 540b).

upCultural Environment
These sub-Districts have a history of forestry. At present, recreational use of the land includes an airfield that was a Commonwealth training field during the Second World War. Peat harvesting potential exists on the Clay Plain.

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upSites of Special Interest

  • Scotch Village Barrens - extensive peat deposits

Provincial Parks and Park Reserves

Proposed Parks and Protected Areas System includes Natural Landscapes 27a and 27b.

Scenic Viewpoints

  • River Hebert, both sides - dyked farmland


Associated Topics
T2.4 The Carboniferous Basin
T8.1 Freshwater Hydrology
T12.10 Plants and Resources

Associated Habitats
H4.1 Bog
H3.1 Freshwater Open-Water Lotic
H3.3 Freshwater Bottom Lotic
H5.1 Barren
H6.2 Softwood Forest (Pine Association; Spruce, Larch upAssociation)