Glacial erratic

Skiing the trails of northeastern Lyme.

One of the cool things about skiing through the remote areas of northeastern Lyme, as I was early this morning after last night dusted the area with an inch or two of fresh powder, is the striking appearance of huge boulders in the middle of an otherwise uneventful patch of lowland forest. These boulders are likely glacial erratics, brought here long ago astride one of the slow-moving glaciers that flowed over this terrain during the last ice age.

A glacial erratic sits beside the ski trails in northeast Lyme.

Or maybe not; some of my readers have a geology background. Correct me if I’m wrong!

A bit further long the trail this morning was a more contemporary form of wildlife: a domestic dog, complete with matching winter coat, quietly and alertly watching me approach while he waited for his pet human to catch up from around the bend.

A dog waits for me on the trails.

Tunnel Brook

David skis across the ponds along the Tunnel Brook trail.
David skis across the ponds along the Tunnel Brook trail.

One of the classic ski tours on Mount Moosilauke is the Tunnel Brook trail, which climbs over a low north-south valley along the west flanks of Mount Moosilauke.  It follows Tunnel Brook upslope for several miles, continuing straight as the brook heads left up into the steep-walled Tunnel Brook Ravine.  (Last summer I completed that classic bushwhack route to the summit, discovering an incredible slide created by Tropical Storm Irene in 2011; see trip report.)  Today I had the good fortune to ski this route under a sunny sky and with fantastic ski conditions. Continue reading “Tunnel Brook”