The Roost
The Roost seen from North Cascades Highway
Highest point
Elevation6,705 ft (2,044 m)[1]
Prominence865 ft (264 m)[1]
Parent peakGlee Peak (7,180 ft)[2]
Isolation1.76 mi (2.83 km)[2]
Coordinates48°43′44″N 121°15′11″W / 48.728939°N 121.253066°W / 48.728939; -121.253066[1]
Geography
The Roost is located in Washington (state)
The Roost
The Roost
Location in Washington
The Roost is located in the United States
The Roost
The Roost
The Roost (the United States)
LocationWhatcom County, Washington, U.S.
Parent rangeNorth Cascades
Topo mapUSGS Mount Triumph
Geology
Type of rockGranodiorite
Climbing
First ascentJuly 12, 1966 by John Roper, Taffy Roper[3]
Easiest routeScramble

The Roost is a 6,705 ft summit in the Picket Range[1] which is a sub-range of the North Cascades Range of Washington state, United States. It is located within North Cascades National Park and Stephen Mather Wilderness, and is situated one mile north of Mount Ross. Like many North Cascades peaks, The Roost is more notable for its large, steep rise above local terrain than for its absolute elevation. The Roost was first climbed on July 12, 1966 by John and Taffy Roper.[3] The nearest higher neighbor is Glee Peak, 1.76 miles (2.83 km) to the north.[1] Precipitation runoff from the mountain drains into the Skagit River.

Climate

The Roost is located in the marine west coast climate zone of western North America.[4] 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, causing them to drop their moisture in the form of rain or snowfall onto the Cascades (Orographic lift). As a result, the west side of the North Cascades experiences high precipitation, especially during the winter months in the form of snowfall.[4] 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.[4] Because of maritime influence, snow tends to be wet and heavy, resulting in high avalanche danger.[4]

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.[5] With the North American Plate overriding the Pacific Plate, episodes of volcanic igneous activity persisted.[5] In addition, small fragments of the oceanic and continental lithosphere called terranes created the North Cascades about 50 million years ago.[5]

During the Pleistocene period, glaciation advancing and retreating repeatedly scoured the landscape leaving deposits of rock debris.[5] The U-shaped cross section of the river valleys is 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.

See also

References

  1. 1 2 3 4 5 "The Roost, Washington". Peakbagger.com.
  2. 1 2 "The Roost - 6,705' WA". listsofjohn.com. Retrieved 2021-06-24.
  3. 1 2 Beckey, Fred W. (1996). Cascade Alpine Guide, Volume 3: Rainy Pass to Fraser River (2nd ed.).
  4. 1 2 3 4 Beckey, Fred W. (1996). Cascade Alpine Guide, Volume 2: Stevens Pass to Rainy Pass (2nd ed.). ISBN 978-0-89886-838-8.
  5. 1 2 3 4 Kruckeberg, Arthur (1991). The Natural History of Puget Sound Country. University of Washington Press.
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