Stanley Glacier - July 25, 2020
Read MoreMy lunch-seating spot is amongst the trees sitting atop the hump on the left-hand side.
My first time up in this basin was August 1997 and again in 2007. Both times before I made the steep trek up to the tip of the glacier. Today, it's "been there done that."
On my way down I'll emerge from the trees on the right side of the plateau and continue along the trail on the other side of the basin.Heading back down.
This time I'll follow the faint path you see on the left-hand side and across the talus slope.
The large rock to the left of centre in the distance is called an erratic, leading the way down and connecting with the trail directly ahead and into the trees.
"Glacial erratics are stones and rocks that were transported by a glacier, and then left behind after the glacier melted. Erratics can be carried for hundreds of kilometres, and can range in size from pebbles to large boulders. Scientists sometimes use erratics to help determine ancient glacier movement."