Mary River, Perry Creek cuts through the foot hills of the Purcell Range. Where tributary streams cut through the accumulation of glacial debris, steep banks or cliffs are evident.Īt 12.5 km from its mouth to its junction with the St. Glacial till, as thick accumulations masking bed rock and consisting of silt, clay sand and boulders forming remnant shelves, is confined to the steep, lower portion of the slopes. The valley slopes are steep to about 300 meters above the floor. From its head waters to about 12.5 km from its mouth it occupies a distinctly trough shaped valley. The search for gold bearing quartz veins followed shortly. The main area of interest reportedly was located between Old Town and Perry Creek Falls and two miles above the falls. During this time period extensive placer mining took place above Old Town. The first recorded mining activities along Perry Creek date back to the mid 1850’s.
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