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

522 Judique Coastal Lowland

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

500 region map - click to enlarge

Geology and Landscape Development
The Judique Coastal Lowland forms a very narrow band along the eastern side of St. Georges Bay and is the geological continuation of sub-Unit 521b. It appears likely that the entire bay area was once composed of the same strata as is now exposed around its rim. The bay may have been carved out by an ancestral river flowing from the Scotian Shelf through the Strait of Canso.

At Port Hood a small area of grey Riversdale sandstone and shale contains thin coal seams. These dip under the waters of the bay at an angle of 20°.

upFresh Water
Several small, isolated tertiary watersheds run parallel to each other and drain first-order streams into the east side of St. Georges Bay. A few small bogs are scattered further inland.

upSoils
The soils in the Unit are predominantly imperfectly drained Queens clay
Port Hood Island, Marble Hill, Inverness County
Port Hood Island, Marble Hill, Inverness County
Click to enlarge
loams, with their poorly drained associate, the Kingsville series, occurring frequently and over substantial acreages. Better-drained soils of the Woodbourne and Shulie series are developed on tills derived from sandstone in small areas throughout the Unit. Around Port Hood, Springhill soils occur. These sandy loams, related to Shulie soils, occupy imperfectly drained sites where water movement is restricted by the topography. Small areas of peat, coarse Hebert soils, and Falmouth and Cumberland soils occur throughout.

upPlants
Loucks places this unit in the Sugar Maple-Hemlock, Pine Zone. The main influences on the vegetation are the wet clay soils, the late spring, and the effects of agricultural clearing. Conifers are dominant. Many of the oldfields are regenerating in White Spruce and Balsam Fir. Black Spruce and Larch are found in the wetter areas. Shade-tolerant deciduous trees grow on some slopes, while a mixed forest of spruce and fir with some shade-intolerant hardwoods covers much of the area.

upCultural Environment
Small-scale farming, fishing, and woodlot exploitation form the economic basis of communities in this area. In former times, coal was mined at Port Hood.

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up Sites of Special Interest

  • Port Hood - coal seams in Riversdale strata

Provincial Parks and Park Reserves

  • Craigmore

Proposed Parks and Protected Areas System includes Natural Landscape 59.


Associated Topics
T2.4 The Carboniferous Basin
T3.2 Ancient Drainage Patterns

Associated Habitats
H3.1 Freshwater Open-Water Lotic
H3.5 Freshwater Water's Edge Lotic
H5.2 Oldfield
H6.2 Softwood Forest (White Spruce Association; Black Spruce, Larch Association)
H6.3 Mixedwood Forest (Spruce, Fir, Pine-Maple, Birch Association)
up