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Mount Judge Howay facts for kids

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Mount Judge Howay
Mt. Judge Howay.jpg
Highest point
Elevation 2,262 m (7,421 ft)
Prominence 1,627 m (5,338 ft)
Listing
Geography
Mount Judge Howay is located in British Columbia
Mount Judge Howay
Mount Judge Howay
Location in British Columbia
Mount Judge Howay is located in Canada
Mount Judge Howay
Mount Judge Howay
Location in Canada
Location Lower Mainland, British Columbia, Canada
Parent range Garibaldi Ranges
Topo map NTS 92G/09
Climbing
First ascent 1921 Tom Fyles; E. Fuller; H. O'Conner
Easiest route navigation, technical rock climbing

Mount Judge Howay is a tall mountain with two main peaks. It was first called the Snow Peaks, a name that also included Mount Robie Reid. This mountain is found about 10 kilometers (6 miles) from the Central Fraser Valley. It is also very close to the north end of Stave Lake.

Mount Judge Howay is one of the highest mountains in its area. You can often see it from other peaks around Vancouver, British Columbia. It sits inside the eastern part of Golden Ears Provincial Park. Another mountain, Mount Robie Reid, is just to its south.

Naming the Mountain

Mount Judge Howay got its name from Frederic W. Howay. He was a famous judge and an expert on the history of British Columbia.

Just southwest of Mount Judge Howay is Mount Robie Reid. This mountain is named after Robie Lewis Reid. He was a lawyer and historian who worked with Frederic W. Howay for many years.

Getting to the Peak

Mount Judge Howay is a very challenging mountain to climb. This is because it is far away and has difficult terrain.

To reach it from the southeast, climbers must first use a canoe to get to the end of Stave Lake. Then, they walk along old logging roads. After that, they need to cross the Stave River. Finally, they climb through a very steep Pacific Coast rainforest. They also have to find their way through areas with many cliffs.

Mountain Weather

Mount Judge Howay is in a marine west coast climate zone. This type of climate is common in western North America.

Most weather systems start over the Pacific Ocean. They then move east towards the Coast Mountains. When these weather systems hit the mountains, they are forced to rise. This causes them to drop their moisture as rain or snow.

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