— — the mountain the lake was made to hold.
“Mount Moran rises straight out of the west shore of Jackson Lake, a flat-topped twelve-thousand-foot block that reads almost like a wall. The Skillet Glacier sits high on its east face. The lake fills the foreground from any northern pullout, and on a still morning the whole mountain comes down into the water unbroken.
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Jackson Lake is the largest of the Teton glacial lakes, set against the northern half of the Teton Range in Grand Teton National Park. The lake covers about 25,540 acres at a surface elevation of 6,772 feet, with depths reaching 438 feet. Mount Moran, the dominant peak on the west shore, tops out at 12,605 feet. The pairing of lake and mountain is one of the most recognised compositions in the American West, photographed from Oxbow Bend, Signal Mountain, and the Mount Moran turnout along US 89.
Mount Moran is a granite block streaked across its east face by a dark vertical band of diabase, a 150-foot dike intruded into the older rock roughly 1.5 billion years ago. The summit is unusually flat for a Teton peak and carries a small remnant of the original sedimentary cover that once topped the range, a detail visible from the lakeshore. Five glaciers sit on the mountain; the Skillet Glacier on the east face, named for its long handle of ice running down a couloir, is the most visible from Jackson Lake.
Jackson Lake is a natural glacial lake whose surface was raised by Jackson Lake Dam, first completed in 1907 at the lake's outlet and rebuilt to modern standards in 1989. The dam raised the natural level about thirty-nine feet and stores water for downstream irrigation in Idaho. The lake holds lake trout, cutthroat, and brown trout. The cold, mineral-clear water reflects the west shore on calm mornings and breaks into hard chop when afternoon wind comes off the range.