The Incredible Hulk | |
Elevation Ft: | 11300. |
Elevation Ref: | [1] |
Prominence Ft: | 240 |
Prominence Ref: | [2] |
Isolation Mi: | 0.90 |
Parent Peak: | Eocene Peak (11,569 ft) |
Map: | California#USA |
Map Size: | 260 |
Label Position: | top |
Location: | Mono County, California, U.S. |
Range: | Sierra Nevada |
Coordinates: | 38.121°N -119.4144°W |
Coordinates Ref: | [3] |
Topo: | USGS Matterhorn Peak |
Rock: | Granodiorite |
Type: | Fault block |
Age: | Cretaceous |
First Ascent: | 1936 |
Easiest Route: | climbing Southwest Couloir |
The Incredible Hulk, or Incredible Hulk, is a granitic summit with an elevation of located in the Sierra Nevada mountain range, in Mono County of northern California, United States. The summit is set in Little Slide Canyon of the Hoover Wilderness, on land managed by Humboldt–Toiyabe National Forest, and is one mile outside the boundary of Yosemite National Park. The peak is situated approximately three miles southwest of Twin Lakes, three-quarters mile east of Kettle Peak, and 2.5 miles northwest of Matterhorn Peak. The nearest town is Bridgeport, 14 miles to the northeast. Topographic relief is significant as the summit rises 3700abbr=offNaNabbr=off above Robinson Creek in 1miles. Incredible Hulk is the unofficial name of this landform, and will remain unofficial as long as the USGS policy of not adopting new toponyms in designated wilderness areas remains in effect.
The first ascent of the summit was made September 6, 1936, by Bestor Robinson, Florence Robinson, Don Woods, and Carl Jensen.[4]
Established rock climbing routes on the 1,200-foot-high walls of Incredible Hulk:[4]
Red Dihedral (originally named "Yggdrasil") and Positive Vibrations are considered classic climbing routes in the Sierra Nevada.[7]
According to the Köppen climate classification system, The Incredible Hulk is located in an alpine climate zone.[8] Most weather fronts originate in the Pacific Ocean, and travel east toward the Sierra Nevada mountains. As fronts approach, they are forced upward by the peaks (orographic lift), causing moisture in the form of rain or snowfall to drop onto the range. Precipitation runoff from this rock feature drains to Robinson Creek which is a tributary of the Walker River.