Geography and climate

[taixyz1992]

Carved out of an ancient floodplain, the small terrace upon which Chetwynd is situated lies in the northern foothills of the Rocky Mountains. Once used as a grazing spot by nomadic Aboriginals, the terrace was farmed by settlers until it was developed into a town. Two types of soil—namely, the Widmark and Centurion Series—comprise the terrace's surface. The Widmark Series—a moderately well-drained degraded loamy, woody, silty, and clay-like soil—lies north of Highway 97. Meanwhile, the Centurion Series—which lies south of the highway—is a poorly drained soil with a dark-brown peaty surface material consisting of decomposed leaves and mosses. These soils, also limited by topography and stoniness, are generally used for forage and pasture.[12][13]
The town is surrounded by forested hills but the prairies of the Peace River Country begin here and continue eastward into Alberta. It lies in a transition area dividing two biogeoclimatic regions: the Boreal White and Black Spruce zone and the Engelmann Spruce-Subalpine Fir zone.[14][15] The area's native tree species include deciduous balsam poplar and coniferous spruce and pine. Many fur-bearing animals—deer, moose, elk, beaver, and bear—comprise the region's mammalian wildlife. Three creeks run south through town. Windrem Creek—which flows down from Ol' Baldy Mountain—and Widmark Creek both flow into Centurion Creek, which itself drains south into the Pine River.



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