Lily Still Waters

Title

Lily Still Waters

Artist

LeeAnn McLaneGoetz McLaneGoetzStudioLLCcom

Medium

Photograph - Photography

Description

Lily Still Waters, Lily Lake Lake Tahoe
Fallen Leaf Lake is about one mile south of the much larger Lake Tahoe, near the California-Nevada state border. It is approximately aligned north-to-south and oval in shape, measuring approximately 2.9 miles (4.6 km) on the long axis and 0.9 miles (1.4 km) on the short axis. The lake was created by at least two glaciers which traveled northward down the Glen Alpine Valley. If the glacier had continued instead of stopping, Fallen Leaf Lake would be a bay similar to nearby Emerald Bay. Fallen Leaf Lake is fed almost entirely by Glen Alpine Creek at the south end, which is in turn fed by several lakes in the Desolation Wilderness area including Gilmore Lake, Susie Lake, Heather Lake, and Grass Lake. In the spring, melting snow causes a vigorous flow of cold water into the lake which gradually tapers off during the summer months until the creek flow is greatly reduced in late summer and the fall. Other much smaller creeks and streams feed the lake, including Cathedral Creek, but they are not nearly as important as Glen Alpine Creek.

Fallen Leaf is approximately 415 feet (125 m) deep at its deepest point, which is east of the sheer face of Cathedral Peak and north of Stanford Sierra Camp. The average depth of the lake is around 240 feet (72 m), and the bottom falls away rapidly as one moves away from the shorelines. Due to the action of the glaciers that carved the lake, the northern end of the lake has a much more gradual depth change, and the bottom can be seen from the surface for a quarter-mile (400 m) offshore. Along other shores, the bottom may be hidden in as little as 100 feet (30 m) offshore.

Uploaded

August 17th, 2011

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