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Karpathos Peak (Mount Olympus) facts for kids

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Karpathos Peak
Karpathos Peak (Mount Olympus).jpg
Karpathos Peak seen from Fryatt Valley
Highest point
Elevation 2,987 m (9,800 ft)
Prominence 367 m (1,204 ft)
Parent peak Mount Belanger (3120 m)
Listing Mountains of Alberta
Geography
Karpathos Peak is located in Alberta
Karpathos Peak
Karpathos Peak
Location in Alberta
Karpathos Peak is located in Canada
Karpathos Peak
Karpathos Peak
Location in Canada
Location Alberta, Canada
Parent range Canadian Rockies
Topo map NTS 83C/05
Type of rock Sedimentary
Climbing
First ascent 1926 by J.W.A. Hickson, Howard Palmer, Hans Fuhrer
Easiest route Mountaineering
Fryatt Valley IV
Karpathos Peak (Mount Olympus)

Karpathos Peak is a tall mountain in Jasper National Park, Alberta, Canada. It stands 2,987 metres (9,800 ft) high in the beautiful Canadian Rockies. This mountain was once called Mount Olympus.

It is found in the Athabasca River valley. Karpathos Peak is at the top of the Fryatt Creek Valley. It shares a high ridge with other peaks like Mount Christie and Brussels Peak. You can sometimes see Karpathos Peak from the Icefields Parkway if the weather is clear.

Mountain History and Naming

This mountain is named after Karpathos, a Greek island. On that island, there is a town called Olympos. The peak was first unofficially called Mount Olympus.

However, its name was changed to Karpathos Peak. This was done to avoid confusion with other mountains named Mount Olympus in the same mountain range. The name Karpathos Peak is still waiting to be officially adopted.

The first time people successfully climbed this mountain was in 1926. The climbers were J.W.A. Hickson and Howard Palmer. They were guided by Hans Fuhrer.

Understanding Karpathos Peak's Geology

Karpathos Peak is made of sedimentary rock. This type of rock forms from layers of sand, mud, and tiny bits of plants and animals. These layers built up over millions of years, from the Precambrian to the Jurassic periods.

Later, powerful forces pushed these rocks eastward. This movement happened during an event called the Laramide orogeny. This process caused the rocks to fold and lift, forming the mountains we see today.

Climate and Weather Around the Peak

Karpathos Peak is in a subarctic climate zone. This means it has very long, cold, and snowy winters. The summers are short and mild.

Temperatures can drop very low, sometimes below -20°C (which is -4°F). With the wind, it can feel even colder, below -30°C (-22°F). The snow and ice that melt from Karpathos Peak flow into Fryatt Creek and Lick Creek. These creeks then join the Athabasca River.

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