Little Tahoma
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Little Tahoma
Little Tahoma Peak, also called Little Tahoma, is a satellite peak of Mount Rainier in Pierce County, Washington and in Mount Rainier National Park. It is quite noticeable from Seattle over away. Little Tahoma Peak is a volcanic remnant. It was part of a larger Mount Rainier which has eroded. The rock is quite unstable and in 1963 a large avalanche originating below it covered the lower section of Emmons Glacier with rock debris. The Fryingpan Glacier and Whitman Glacier are located just to the east of the peak. Little Tahoma Peak can most easily be accessed from Summerland, an alpine meadow area in Mount Rainier National Park Mount Rainier National Park is an American national park located in southeast Pierce County and northeast Lewis County in Washington state. The park was established on March 2, 1899, as the fourth national park in the United States, preservi .... The first recorded ascent was on August 29, 1894, by JB Flett and Henry H. Garrison who climbed f ...
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Fryingpan Glacier
Fryingpan Glacier is on the eastern face of the Little Tahoma Peak, just to the east of Mount Rainier in the U.S. state of Washington. The glacier is located on top of a cliff from the Emmons Glacier to the north and a small ridge separates this glacier from the Whitman Glacier to the south, except for a small snowfield in which these two glaciers are connected. Most of the ice is located on a broad plateau at an elevation of . The head of the Fryingpan Glacier is located to the northeast of the ridge and at the foothill of Little Tahoma Peak at around . The glacier flows downhill eastward and the uneven topography causes the glacier surface to be crevassed The glacier ends on shallow to steep slopes at about . Numerous snowfields and alpine meadows are located near the bottom and east of the glacier. Meltwater from the glacier drains into the White River. See also *List of glaciers in the United States This is a list of glaciers existing in the United States, currently or ...
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