Hiking the Lower Rose Trails
At the end of summer I hiked a loop route on grasslands benchlands near Rose Hill. This area was once under a glacial lake. The silts, sands, and clay deposits were laid down over several ice ages. Then as the ice retreated, gullies were cut by continuous meltwaters creating drainage channels for the melting snow and ice higher in the hills. the gullies have continued to be eroded by spring melt each year. Hiking in the Lower Rose area requires going down and back up some of the gullies and trails have developed following some of the easier routes. Double tracks connected power lines and access for ranchers. Single tracks were added by … Continue reading →










