— — the ice the mountain is still letting go of.
“A short spur off the Highline Trail in Glacier National Park climbs to a railing-less ledge above the Grinnell basin. From it the glacier and its meltwater lake sit a thousand feet below, the same milky green every year, smaller every year. Marmots whistle from the talus. The wind off the ice carries the cold up the wall. from the studio
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The Grinnell Glacier Overlook is a half-mile spur off the Highline Trail in Glacier National Park, climbing roughly a thousand vertical feet from the main trail near Granite Park Chalet to a ledge on the Garden Wall. From the overlook the route looks straight down on Grinnell Glacier, Upper Grinnell Lake, and the Salamander Glacier above. The Highline itself runs along the Continental Divide between Logan Pass and Granite Park, in the heart of the park's namesake glaciated terrain.
The overlook sits near 7,300 feet on the spine of the divide, where weather from the Pacific side meets the prairie air rising from the east. Afternoon thunderstorms build fast in July and August, and the spur trail is exposed the whole way. Hikers often turn back when the first cumulus stacks over Mount Gould. Mountain goats and bighorn sheep move along the cliffs below; the descent rejoins the Highline before any storm reaches the wall.
The lake at the foot of the glacier is meltwater, fed each summer as the ice gives back another season's accumulation. Grinnell Glacier has lost more than three-quarters of its 1850 area, according to U.S. Geological Survey monitoring, and the visible bare rock around the lake marks the recent retreat. The water carries rock flour from the grinding ice, which scatters light and gives the lake its pale opaque green. The same silt colours Iceberg Lake one valley north.