Tamanos Mountain
Climate
Tamanos Mountain is located in the marine west coast climate zone of western North America. Most weather fronts originating in the Pacific Ocean 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 snow onto the Cascades. As a result, the west side of the Cascades experiences high precipitation, especially during the winter months in the form of snowfall. Because of maritime influence, snow tends to be wet and heavy, resulting in high avalanche danger. 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. Precipitation runoff from Tamanos Mountain drains into the White River.
See also
- Geography of Washington (state)
- Geology of the Pacific Northwest
- List of mountain peaks of Washington (state)
Gallery
References
- ^ "Tamanos Mountain, Washington". Peakbagger.com.
- ^ "Tamanos Mountain - 6,790' CA". listsofjohn.com. Retrieved 2022-05-17.
- ^ "Tamanos Mountain". Geographic Names Information System. United States Geological Survey, United States Department of the Interior. Retrieved 2022-05-17.
- ^ Gibbs, George Dictionary of Nisqually Indian Language of Western Washington. Shorey's Bookstore publisher, 1970.
- ^ Beckey, Fred W. Cascade Alpine Guide, Climbing and High Routes. Seattle, WA: Mountaineers Books, 2008.
External links
- Weather forecast: Tamanos Mountain
- National Park Service web site: Mount Rainier National Park