"“For a glacier to remain a constant size, snowfall at the top must equal melting at the bottom. More snowfall causes a glacier to advance, meaning to grow larger. Less snowfall results in retreat. At any size, to be called a glacier, snow fall compacted into ice must flow under the pull of gravity" - waymarking.com
"The majority of the glaciers in the Tetons have north or east aspect, with the exception of Falling Ice Glacier on Mount Moran, which faces southeast. All the glaciers are located on the east slope of the mountain range, and like the glaciers of the Wind River Range, this is most likely due to the decreased solar radiation and predominantly westerly winds (Fryxell, 1935)." - glaciers.us
" All of the existing glaciers in Grand Teton National Park were created during the Little Ice Age (1350–1850 A.D.) and have been in a general state of retreat since the mid-1800s" - wikipedia
"Schoolroom Glacier is a small glacier in Grand Teton National Park in the U.S. state of Wyoming.[2] This Teton Range glacier lies adjacent to the south Cascade Canyon trail at an altitude of 10,400 ft (3,200 m), approximately 12 mi (19 km) from the trailhead at Jenny Lake. " wikipedia
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