| Chutla Peak | |
|---|---|
 | |
| Highest point | |
| Elevation | 6,007 ft (1,831 m)[1] |
| Prominence | 600 ft (180 m)[2] |
| Coordinates | 46°45′10″N 121°46′30″W / 46.752797°N 121.775063°W |
| Geography | |
  Chutla Peak Location in Washington  Chutla Peak Chutla Peak (the United States) | |
| Location | Mount Rainier National Park, Washington, U.S. |
| Parent range | Cascades |
| Topo map | USGS Mount Rainier West |
| Climbing | |
| Easiest route | Scrambling class 3 |
Chutla Peak is a summit on the crest of the Tatoosh Range which is a sub-range of the Cascade Range.[2] It's located south of Mount Rainier within Mount Rainier National Park. The mountain's name "Chutla" derives from Chinook Jargon which means "rock".[1] Precipitation runoff on the peak drains into the Nisqually River.
Climate
Chutla Peak is located in the marine west coast climate zone of western North America.[3] Most weather fronts originate in the Pacific Ocean, and travel northeast toward the Cascade Mountains. As fronts approach, 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.[3] 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).[3] 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.[3] Because of maritime influence, snow tends to be wet and heavy, resulting in high avalanche danger.[3]
References
External links
- National Park Service web site: Mount Rainier National Park
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