Pocket Peak facts for kids
Quick facts for kids Pocket Peak |
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Pocket Peak, west aspect
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| Highest point | |
| Elevation | 7,056 ft (2,151 m) |
| Prominence | 1,136 ft (346 m) |
| Isolation | 2.25 mi (3.62 km) |
| Parent peak | Rapid Peak (7,259 ft) |
| Geography | |
 Pocket Peak
Location in Washington (state)
Pocket Peak
Location in the United States
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| Location |
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| Parent range | Cascade Range North Cascades Skagit Range |
| Topo map | USGS Mount Sefrit |
| Climbing | |
| First ascent | 1967 D. McKeever, R. Tabor |
| Easiest route | class 4 scrambling |
Pocket Peak is a 7,056-foot (2,151-metre) mountain summit located in the Skagit Range, which is a subset of the North Cascades in Whatcom County of Washington state. It is situated immediately west of Pocket Lake, and 4 mi (6.4 km) east of Mount Larrabee in the Mount Baker Wilderness, which is managed by Mount Baker-Snoqualmie National Forest. Pocket Peak is set on the Slesse Divide, 0.7 mile south of the Canada–United States border. Its nearest higher neighbor is Rapid Peak, 2.24 mi (3.60 km) to the southeast, and Slesse Mountain is set 3.24 mi (5.21 km) to the northwest. Other peaks which can be seen from the summit include Mount Baker, Mount Shuksan, American Border Peak, Mount Chardonnay, Mount Rexford, and many more. This unofficially named peak is named in association with officially named Pocket Lake. Precipitation runoff from this mountain drains into Silesia and Ensawkwatch Creeks, which are both tributaries of the Chilliwack River.
Climate
Pocket Peak is located in the marine west coast climate zone of western North America. This climate supports a pocket glacier on its north slope. Most weather fronts originate in the Pacific Ocean, and travel northeast toward the Cascade Mountains. As fronts approach the North Cascades, they are forced upward by the peaks of the Cascade Range (Orographic lift), causing them to drop their moisture in the form of rain or snowfall onto the Cascades. As a result, the west side of the North Cascades experiences high precipitation, especially during the winter months in the form of snowfall. Due to its temperate climate and proximity to the Pacific Ocean, areas west of the Cascade Crest very rarely experience temperatures below 0 °F (−18 °C) or above 80 °F (27 °C). During winter months, weather is usually cloudy, but, due to high pressure systems over the Pacific Ocean that intensify during summer months, there is often little or no cloud cover during the summer. Because of maritime influence, snow tends to be wet and heavy, resulting in high avalanche danger. The months July through September offer the most favorable weather for viewing or climbing this peak.
Geology
The North Cascades features some of the most rugged topography in the Cascade Range with craggy peaks, ridges, and deep glacial valleys. Geological events occurring many years ago created the diverse topography and drastic elevation changes over the Cascade Range leading to the various climate differences.
The history of the formation of the Cascade Mountains dates back millions of years ago to the late Eocene Epoch. With the North American Plate overriding the Pacific Plate, episodes of volcanic igneous activity persisted. Remnants of the Hannegan Caldera can be seen on the eroded southeast face of Hannegan Peak. The caldera erupted four million years ago during the Pliocene epoch, and was a precursor to the volcanism of Mt. Baker. In addition, small fragments of the oceanic and continental lithosphere called terranes created the North Cascades about 50 million years ago.
During the Pleistocene period dating back over two million years ago, glaciation advancing and retreating repeatedly scoured the landscape leaving deposits of rock debris. The U-shaped cross section of the river valleys are a result of recent glaciation. Uplift and faulting in combination with glaciation have been the dominant processes which have created the tall peaks and deep valleys of the North Cascades area.
