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Municipality Climate Adaptation Case Study Report

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Table 6<br />

West Hants Natural Landscapes<br />

7-South Mountain Rolling Plain<br />

Location<br />

Southern portion of the municipality<br />

Character<br />

Southwardly inclined and resistant upland plain characterized by a variety of<br />

glacial deposits and dominated by Acadian coniferous forest.<br />

Bedrock Geology<br />

Devonian Carboniferous granites (90%), and Cambrian/Ordovician slate and<br />

grey wacke (10%)<br />

Surficial Materials<br />

Stony till (50%), silty till (20%), ground moraine (20%), glacially scoured<br />

bedrock (10%)<br />

Soils Gibraltar (90%)<br />

Coastal Environment None<br />

(1) Well-drained coniferous (red spruce-white pine-eastern hemlock and red<br />

Dominant Ecosystems oak) undulating terrain;<br />

(2) Poorly-drained coniferous (black spruce-larch) flats<br />

28-Shubenacadie River Rolling Hills<br />

Location<br />

Northern and central portion of municipality surrounding Minas Basin<br />

A series of hills and undulating terrain with Acadian coniferous-dominated<br />

forest types, and drainage defined by portions of several large rivers (e.g.,<br />

Character<br />

Avon, St. Croix, Kennetcook); coastal sections consist of eroding, low cliffs,<br />

wide intertidal flats and several large estuaries.<br />

Early-late Carboniferous sandstones, other clastic sedimentary rocks and<br />

Bedrock Geology<br />

carbonates (95%), and Cambrian/Ordovician slates (5%)<br />

Surficial Materials Silty till (90%), alluvial deposits (5%), glaciofluvial deposits (5%)<br />

Soils Queens (60%), Wolfville (20%), Tormentine (15%), Stewiacke (5%)<br />

Eroding, non-resistant, low cliffs; wide intertidal mud or sand flats; saltmarshes<br />

Coastal Environment<br />

in estuaries.<br />

(1) Well-drained mixwood and mixed forest (red spruce-sugar maple-<br />

American beech (eastern hemlock) hills;<br />

Dominant Ecosystems<br />

(2) Imperfectly-drained coniferous (red spruce-black spruce+white pineeastern<br />

hemlock) undulating terrain<br />

27- Walton River Clay Plain<br />

A large area roughly centering around Cogmagun in the northeastern portion<br />

Location<br />

of municipality, north of the Kennetcook River<br />

A predominantly flat plain characterized by Acadian coniferous forest types<br />

and many wetlands on flat to hummocky terrain. Dendritic drainage defined by<br />

Character<br />

headwaters and upper reaches of a few moderate-sized rivers (Walton,<br />

Cogmagun and Tomcod).<br />

Bedrock Geology Early-late Carboniferous sandstones and carbonates (100%)<br />

Surficial Materials Silty till (90%), organic deposits (10%)<br />

Soils Kingsville (75%), Queens (15%), organic soils (10%)<br />

Coastal Environment None<br />

(1) Poorly-drained black spruce-larch flats;<br />

Dominant Ecosystems (2) Imperfectly-drained black spruce-red spruce (white pine, red pine)<br />

undulating terrain<br />

Source: N.S. Environment and Labour, Natural Landscapes of Nova Scotia: Summary Descriptions, January 2002.<br />

Parks, Protected Areas and Sites of Ecological Interest<br />

<br />

Panuke Lake Nature Reserve: 150.9 ha (373 ac) including 47 ha (116 ac) of old growth<br />

eastern hemlock-red spruce forest.<br />

13

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