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

580 Hills and Valleys

Geology & Landscape | Scenic Quality

500 region map - click to enlarge

The Units within this District are:
581 Cumberland Hills
582 Pictou Valleys
583 Antigonish Uplands
584 Ainslie Uplands
585 Iona Uplands

Geology and Landscape Development
This District includes two areas of Carboniferous strata that have the characteristics of foothills. They are adjacent to faulted upland blocks which have moved vertically upwards in the landscape. The close interrelationship of resistant
Nova Scotia Highland Village, Iona
Nova Scotia Highland Village, Iona
Click to enlarge
Horton Group strata and the overlying, less-resistant Windsor Group limestone, salts, and shales is strongly reflected in the eastern sections of this District (Units 583, 584, and 585).

Some areas are lowland, others are upland, reflecting both the position of these strata on the tilted planation surface and the relative proportions of Horton and Windsor deposits. Except in the Pictou Valleys Unit, these strata have been compressed into folds which lie parallel to the axis of the province. Typically, erosion has removed Horton strata in the centre of anticlines (upfolds) and left the Windsor strata in the synclinal hollows in between. In some locations Windsor strata have also been protected from erosion by downfaulting, as in the Pictou Valleys. Where resistant Horton grits are exposed, they stand as ridges and as shoulders on the flanks of highland blocks. The Windsor deposits form low areas and valleys in which salt springs and brackish lakes are common.

upScenic Quality
These landscapes generally lie below 200 m but, owing to river erosion, exhibit varied relief. The exception is the southern portion of the Ainslie Uplands (Unit 584), which tends to be both higher and less dissected. The latter area also possesses less settlement than the norm; elsewhere there are lines of sparse settlement along the valley floors. The dendritic drainage patterns preclude lakes, so water features are seldom present. Lake Ainslie and the shorelines of the Grand Narrows (Unit 585a) are the major exceptions. Scenic value is high to very high around the lakes, on the edge of the Mabou highland, and at Mabou Harbour. Elsewhere it is typically in the medium range. The Pictou and Springhill coalfields possess urban-industrial landscapes which, though hardly attractive, have much of human interest.