Mount Carleton Provincial Park

22. The Nepisiquit River valley is similar to the Tobique River, to the extent that they ar eboth in the same primitive state and are ideally suited to be established as Wild 'Rive rProvincial Parks .23. A long ridge of hills and mountains, enclosing the basin from the south, forms a buffe rfor the park, and provides for linear activities such as ski touring and hiking .24. In this area, there is gently sloping land, made up of glacial outwash, which has th ecapability of supporting intensive use .25. The eastern slope of the Mount Carleton monadnock, situated here, is visuall yprominent from the lake area .26. A narrow bowl, formed by a mountain stream is ideal for interpretive use, and offer slimited ski potential .27. A large bowl, with a vertical drop of over 1,600 feet is naturally condusive to ski are adevelopment .28. This unit is the exposed, forested slope of the Mount Carleton monadnock .29. The upland plateau of Mount Carleton is basically a barren, stunted, wind-sheare dforest .30. A wide valley floor, forested at the edges, divides the Mount Carleton monadnock fro mMount Bailey .31. This natural ponding area within the valley floor, is a favourite fawn-dropping area fo rthe white-tailed deer.32. A volcanic ridge, peaked by Mount Bailey is of scenic and interpretive value .33. The Mamozekel Valley is a second potential access corridor .29