Once upon a time, this Glacier was a tributary to Dawes Glacier in Endicott Arm. Now it’s a peek-a-boo reminder of a cooler time when glaciers filled Endicott Arm. One thing I like to think about as we pass this particular glacier is how you can see in the vegetation that the glacier had been in its valley as recently as 50 years ago. That’s because the low shrubby willow and alder are considered pioneer plants that are slowly helping to make soils. As time passes trees like cottonwood will begin to grow and eventually those trees will be replaced with a spruce and hemlock forest.
This photo was taken our Southeast Alaska Fjords Photography Workshop. To learn more about this trip click here.