Red Mountain (Skagit County, Washington) facts for kids
Quick facts for kids Red Mountain |
|
|---|---|
Red Mountain seen from Diablo Lake
|
|
| Highest point | |
| Elevation | 7,658 ft (2,334 m) |
| Prominence | 618 ft (188 m) |
| Geography | |
 Red Mountain
Location in Washington (state)
Red Mountain
Location in the United States
|
|
| Topo map | USGS Mount Logan |
| Climbing | |
| Easiest route | Scrambling |
Red Mountain is a 7,658 ft summit in the North Cascades Range of Washington, United States. It is located in Skagit County and within North Cascades National Park and the Stephen Mather Wilderness. It is situated on a smooth ridge of brick-red color at the western culmination of Ragged Ridge. Like many peaks of the North Cascades, Red Mountain is more notable for its large, steep rise above local terrain than for its absolute elevation. The nearest higher peak is Cosho Peak, 2.6 miles (4.2 km) to the east-southeast. Precipitation runoff from Red Mountain drains into the Skagit River via Panther and Fisher Creeks.
Climate
Red Mountain is located in the marine west coast climate zone of western North America. Most weather fronts originate in the Pacific Ocean, and travel east 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. 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.
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. These climate differences lead to vegetation variety defining the ecoregions in this area.
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. 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.
