Mineral King - Geography

Geography

Mineral King is a 7.5-mile (12.1 km)-long, 1-mile (1.6 km)-wide glacial valley in the southern Sierra Nevada. The valley floor lies at an elevation of 7,400 feet (2,300 m), while the granite peaks rising above the head of the valley reach heights of 11,000 feet (3,400 m) or more. As the crow flies, it is located about 20 miles (32 km) southeast of Three Rivers, which is near the confluence of the East Fork Kaweah River and Middle Fork Kaweah River.

The valley floor is an expanse of open meadows with a narrow strip of riparian vegetation, including short trees and bushes, along the East Fork Kaweah River. As the flat meadows give way to rocky slopes, there are many congregations of conifers that climb the slopes to the tree line. Above the tree line, there are sheer or almost sheer granite walls that slope up to form Sawtooth Peak, Empire Mountain, Mineral Peak, Hengst Peak and others. There are two prominent mountain passes leading out of Mineral King: Timber Gap, which leads into the Middle Fork Kaweah River drainage' and Farewell Gap at the valley head, which leads into the Kern River drainage. The first half of the valley runs from south to north and the second half runs from east to west.

Fed by snowmelt, springs and abundant lakes in granite bowls at the upstream-most section of the valley, creeks plunge down the steep valley walls as long and twisting waterfalls. These include Tufa Falls, Crystal Creek Falls, and Franklin Falls, in upstream order. This section of the valley is dotted with tributary gorges that fan out from the main canyon. Lakes in this section of the valley include the Mosquito Lakes, Eagle Lake, the Franklin Lakes, and the Crystal Lakes. From the end of the valley, the East Fork Kaweah River drops over Mineral King Falls and East Fork Falls, before continuing down a steep and narrow gorge, following Mineral King Road.

Mineral King is one of the oldest communities in the High Sierra, with many families owning cabins for six or seven generations. Many of the communities date from the 1870s silver boom and have been inhabited since.