Mailbox Peak
Northwest aspect, from Mt. Teneriffe
Highest point
Elevation	4,841 ft (1,476 m)[1][2]
Prominence	121 ft (37 m)[1]
Parent peak	Dirtybox Peak [3]
Isolation	0.42 mi (0.68 km)[4]
Coordinates	47°27′45″N 121°38′22″W / 47.462465°N 121.63942°W / 47.462465; -121.63942[1]
Geography
Mailbox Peak Location in Washington Show map of Washington (state) Mailbox Peak Mailbox Peak (the United States) Show map of the United States
Location	King County Washington state, U.S.
Parent range	Cascade Range
Topo map	USGS Chester Morse Lake
Climbing
Easiest route	class 1+ hiking trail

Mailbox Peak is a 4,841-foot-elevation (1,476 m) mountain located in King County of Washington state. It is set west of the crest of the Cascade Range, on land managed by Mount Baker-Snoqualmie National Forest. Mailbox Peak is situated seven miles east of North Bend, and one mile northeast above the Washington State Fire Training Academy. Precipitation runoff from the south side of the mountain drains into the South Fork Snoqualmie River, whereas the north side drains to the Middle Fork of the Snoqualmie. The summit lies along a ridge containing Dirtybox Peak, its topographical parent, and Dirty Harry's Peak. Topographic relief is significant as the northwest aspect rises nearly 4,100 feet (1,200 meters) above the Middle Fork in 1.25 mile. The popular Mailbox Peak Trail gains 4,100 feet of elevation over 5.5 miles.^[2] Prior to 2014 when the new trail was completed, climbing Mailbox Peak involved 4,000 feet gain in only 2.6 miles along an unmaintained route that was used for conditioning for major climbs,^[5] and recruits from the Fire Training Academy would celebrate graduation by carrying a fire hydrant to the summit.^[6] The peak is named for a mailbox at the top which functions as the summit register, but this toponym has not been officially adopted by the U.S. Board on Geographic Names.

Climate

Mailbox Peak is located in the marine west coast climate zone of western North America.^[7] 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, 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 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.^[7] 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.^[7] The months May through October offer the most favorable weather for viewing or climbing this peak.

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