Fisheries and Land Resources

Forestry and Agrifoods

Western Newfoundland Subregions

Western Newfoundland Subregions Map

This ecoregion is characterized by a humid climate with a relatively longer frost-free period. It contains some of the most favourable sites for forest growth although there is considerable variation due to altitude and proximity to the coast.

The Dryopteris-Hylocomium-Balsam Fir forest type is the zonal forest for this region. The zonal soils are nutrient rich humic podzols with a very dark podzolic B horizon due to humus enrichment. The absence of prolonged dry periods appears to have excluded fires from all but the most coarse textured soils. Consequently, Balsam Fir rather than Black Spruce is the dominant forest cover. Yellow Birch is common in protected valleys below 200m elevation. This species (Yellow Birch) also occurs in less vigorous forms in the Maritime Barrens and Avalon Forest Ecoregions, but it is absent at higher elevations and north of Deer Lake. Red Maple is also most common and robust in this ecoregion.

As a general rule overstocking is a more common silvicultural problem than understocking in Western Newfoundland. Localized regeneration failures can occur in forests with a very dense fern and herb stratum such as the Rubus-Balsam Fir and the Dryopteris-Balsam Fir forest types. On these types, hardwoods, particularly Mountain Maple on seepage slopes, can form semistable thickets. These thickets may eventually develop into hardwood forest types. The development of ericaceous heath after logging or fire is only observed on very small areas of coarse textured till. This is in stark contrast to Central Newfoundland where succession to Kalmia Heath is a common occurrence. The Western Newfoundland Ecoregion is subdivided into five subregions.

A. Serpentine Range Subregion

This subregion extends from Blow-Me-Down on the south shore of the Bay of Islands to include the Lewis Hills. The area is mountainous with elevations in excess of 800 m and the vegetation is dominated by rock barrens. The serpentine and ultra basic rock types support numerous rare and endemic species of plants.

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B. Corner Brook Subregion

This subregion includes the coastal plain and mountain slopes and river valleys from the southern end of Grand Lake to Robinsons River. Areas of deep undulating till occur locally. These are characterized by orthic podzols on sandy loams with the Dryopteris-Hylocomium-Balsam Fir type occurring in the mid-slope position.

On the steep mountainous slopes, gneiss, granite, sandstone and quartz are the most frequently encountered rock types and the parent material is a shallow, often stony, sandy loam till. The Hylocomium-Balsam Fir forest type occupies the midslope position underlain by orthic or gleyed podzols with seepage over bedrock. The occurrence of seepage waters ensures good forest growth and profuse regeneration after cutting. This landtype is also prevalent in the Corner Brook subregion.

The coastal plain is dominated by numerous coarse textured deposits, such as glacio-fluvial deposits, eskers, drumlins and kames. The generally, low productivity of these site is in stark contrast to most of Western Newfoundland. The Pleurozium-Balsam Fir and Gaulteria-Balsam Fir forest types are the most common in undisturbed landscapes, but these may be replaced by corresponding Black Spruce-Feathermoss types, Kalmia-Black spruce or Kalmia Heath after fire. Orthic podzols dominate these landscapes with gleyed humic podzols in transition to large peatland deposits. This is one of the few landtypes in the Western Newfoundland Ecoregion where serious growth and regeneration problems may be encountered.

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C. Port aux Port Subregion

Hilly to undulating terrain from Bonne Bay to Stephenville and east to Grand Lake. The parent materials in this subregion are dominated by slates and limestone till. Areas with calcareous till are distinguished by the occurrence of light coloured marl deposits around ponds and in valleys. The parent material consists of shallow, stony silt loam underlain by limestone bedrock or calcareous basal till. The rugged topography is dominated by the Taxus-Balsam Fir and Dryopteris-Rhytidiadelphus-Balsam Fir forest types.

The hilly, non-calcareous terrain in this subregion is dominated by shallow loamy soils over shale bedrock. However, the shallowness of the till does not adversely affect forest growth since nutrient rich seepage waters are held in the rooting zone by bedrock or a fragipan layer. The steep topography is dominated by the Dryopteris-Balsam Fir forest and supports some of the most productive stands in Newfoundland.

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D. St. George's Bay Subregion

The Codroy Subregion extends from Robinsons River to the Cape Anguille Mountains. Climatically, this area has some of the most favourable conditions for growth in Newfoundland and a large portion of the area has been cleared for agriculture. The forested landscape is dominated by steep slopes.

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E. Codroy Subregion

This subregion includes the Port au Port Peninsula. Again the landscape is dominated by rock barren, however, the rock type is dominated by limestone. The Limestone Heaths of the area also support numerous species of rare and endangered plants. Forests are generally unproductive or totally lacking.

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F. Bay d'Espoir Subregion

This small outlier of the Western Newfoundland Ecoregion is in a sheltered valley system on the southeast coast. Excellent stands of the Dryopteris Balsam Fir forest type dominate the valley slopes. However, Mountain Maple Thickets and Trembling Aspen are generally lacking in these stands.

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