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Key Facts about Mount Fuji

29-10-2024

08:34 AM

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1 min read
Key Facts about Mount Fuji Blog Image

Overview:

Japan's Mount Fuji remained snow-less recently, the latest date that its majestic slopes have been bare since records began 130 years ago.

About Mount Fuji:

  • Mount Fuji, also known as Fuji-san, is the highest mountain in Japan, standing at 3,776 meters.
  • It is situated close to the Pacific coast in the Yamanashi and Shizuoka prefectures in the heart of the large island of Honshu, about 100km to the southwest of the Tokyo-Yokohama metropolitan area. 
  • Unlike other famous high-elevation mountains in the world, Mt. Fuji is not part of a large mountain range. 
  • It is a stratovolcano that has been dormant since its last eruption in 1707 but is still generally classified as active by geologists.
    • It has a prominent summit crater and is constructed from innumerable basaltic lava flows, each a few meters thick.
    • It has a smooth slope and a wide, spreading base, creating a beautiful skyline as it narrows to a magnificent peak.
    • It is said that the main cause of Mt. Fuji's volcanic activity is the Pacific Plate sinking under the bottom of the Philippine Plate.
  • On the northern slopes of Mount Fuji lie the Fuji Five Lakes (Fuji Goko), comprising, east to west, Lake Yamanaka, Lake Kawaguchi, Lake Sai, Lake Shōji, and Lake Motosu, all formed by the damming effects of lava flows.
  • Despite its active volcanic nature, Fuji’s summit is covered in snow most times of the year. 
  • The mountain is the major feature of Fuji-Hakone-Izu National Park, and it is at the centre of a UNESCO World Heritage site designated in 2013.

Q1: What is a stratovolcano?

It is a tall, steep, and cone-shaped type of volcano. Unlike flat shield volcanoes, they have higher peaks. They are typically found above subduction zones, and they are often part of large volcanically active regions, such as the Ring of Fire that frames much of the Pacific Ocean. Strato Volcanoes comprise the largest percentage (~60%) of the Earth's individual volcanoes, and most are characterized by eruptions of andesite and dacite, lavas that are cooler and more viscous than basalt. These more viscous lavas allow gas pressures to build up to high levels. Therefore, these volcanoes often suffer explosive eruptions. 

News: Still No Snow On Japan's Mount Fuji, Breaking Record