Nova Scotia peninsula

The northern portion of the peninsula is dominated by the Avalon Uplands (the Cobequid Hills and Pictou-Antigonish Highlands) and the Carboniferous Lowlands, the latter of which straddles the fault zone.

The Cobequid Mountains contain the highest elevation points on the peninsula. This low, heavily eroded part of the Appalachian Mountains, along with the Pictou-Antigonish Highlands, comprises a highland across the northern portion of the peninsula with average elevations between 250–300 metres. It was heavily covered in sediment during glaciation; consequently it hosts an abundant forest as well as agricultural activities.

The Carboniferous Lowlands includes carboniferous sedimentary rocks south of the Minas Basin and along the north shore of the peninsula immediately south of the Northumberland Strait. The area south and east of the Minas Basin is dominated by karst topography lending to numerous gypsum deposits. Coal seams are found in the western and central areas of Cumberland County in the Joggins-River Hebert basin and the Springhill basin, along with the Debert basin and the Pictou basin.

Throughout the northern portion of the peninsula, the lowland plains, rolling uplands, and coastal fringe areas support numerous settlements, many of which developed around mineral extraction, particularly coal. When included with the Sydney and Inverness coal fields on Cape Breton Island, these regions were extremely prominent in the industrial and social development of Nova Scotia.

In addition to sharing the Carboniferous Lowlands, the southern portion of the peninsula is dominated by the Atlantic Interior (Sissiboo Lowlands, South Mountain, various slate ridges), followed by the comparatively small Triassic Lowlands (the Annapolis Valley), and the Fundy Coast (including Economy Mountain and North Mountain) and Atlantic Coast regions.

The Atlantic Interior is dominated by a glacial landscape of exposed granitic rock, thick forest, drumlins and numerous lakes. The Sissiboo Lowlands comprise many river valleys and lowland inland areas in the southwest and central portion of the peninsula. The South Mountain is a steadily rising slope that descends sharply at the Annapolis Valley but more gradually toward the Atlantic, resulting in a plateau across much of the southwest interior of the peninsula with average elevations of 150 m and maximum elevations of 275 m. Slate ridges are prominent in the Rawdon Hills and Wittenburg Ridge areas along the boundary with the Carboniferous Lowlands.

The Fundy Coast region includes the North Mountain ridge as well as the Digby Neck and the Economy Mountain areas along the north side of the Minas Basin. The Atlantic Coast region includes the barren and wind-swept regions from Yarmouth to Canso, extending several kilometres inland.

The Triassic Lowlands is an area of soft sandstone, much of which is covered by water resulting from sea level rise. The remnant is the open ended Annapolis Valley which is sheltered by the Fundy Coast and the Atlantic Interior, providing a micro-climate unique to the Atlantic provinces and conducive to fruit and vegetable farming.