HomeGeographyCampbell Creek – Source to Confluence

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Campbell Creek – Source to Confluence — 1 Comment

  1. Of interest is a relatively new slide on the east shore of Trapp near the north end but south of the long point and behind the long beasc.New movement has taken place (Plus the rock slide on Cardew hill ).The slide at Trapp is 100,000 yds and is ready to come down into the lake this spring if waterlevels remain high.Trapp lake for the last 5 or 6 years has been successivly higher every year And I believe it is destabilizing the shore in several places.

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