Jump to content

The Castle (Washington)

Coordinates: 46°45′28″N 121°43′42″W / 46.757752°N 121.728328°W / 46.757752; -121.728328
From Wikipedia, the free encyclopedia

This is an old revision of this page, as edited by Ron Clausen (talk | contribs) at 05:21, 12 August 2018 (Created page with '{{Infobox mountain | name = The Castle | photo = The Castle at MRNP.jpg | photo_caption = The Castle, south side | elevation_ft = 6440 | elevation_ref = <ref n...'). The present address (URL) is a permanent link to this revision, which may differ significantly from the current revision.

(diff) ← Previous revision | Latest revision (diff) | Newer revision → (diff)
The Castle
The Castle, south side
Highest point
Elevation6,440 ft (1,960 m)[1]
Prominence200 ft (61 m)[1]
Coordinates46°45′28″N 121°43′42″W / 46.757752°N 121.728328°W / 46.757752; -121.728328
Geography
The Castle is located in Washington (state)
The Castle
The Castle
Location of The Castle in Washington
The Castle is located in the United States
The Castle
The Castle
The Castle (the United States)
LocationMount Rainier National Park, Washington, U.S.
Parent rangeCascades
Topo mapUSGS Mount Rainier East
Climbing
Easiest routeClimbing class 5

The Castle[2] is the descriptive name for a summit in the Tatoosh Range which is a sub-range of the Cascade Range. It is located in Lewis County of Washington state. Situated in Mount Rainier National Park, The Castle is 0.2 mile immediately east of Pinnacle Peak. Precipitation runoff from The Castle drains into tributaries of the Cowlitz River.[1]

Climbing

The Pinnacle Saddle Trailhead is located at Reflection Lakes and the trail to the saddle is over a mile in length. From the saddle, a climber's path traverses the south slope of Pinnacle Peak. Reaching the summit of The Castle is minimum class 4 scrambling, with class 5 climbing options.[3]

Climate

The Castle 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 Cascades experiences high precipitation, especially during the winter months in the form of snowfall.[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

  1. ^ a b c "The Castle, Washington". Peakbagger.com.
  2. ^ "The Castle". Geographic Names Information System. United States Geological Survey, United States Department of the Interior. Retrieved 2018-08-11.
  3. ^ a b c d e Beckey, Fred W. Cascade Alpine Guide, Climbing and High Routes. Seattle, WA: Mountaineers Books, 2008.