Mount Fuji | Facts, Height, Location, & Eruptions | Britannica

Ask the Chatbot Games & Quizzes History & Society Science & Tech Biographies Animals & Nature Geography & Travel Arts & Culture ProCon Money Videos Mount Fuji

• Introduction & Top Questions
• Cultural significance
• Origin
• Tourism and religious significance

References & Edit History Related Topics Images & Videos For Students Mount Fuji summary Quizzes Volcanoes Quiz All About Mountains Quiz Related Questions

• Why is Mount Fuji famous?
• How was Mount Fuji formed?
• Is Mount Fuji active?

Geography & Travel Physical Geography of Land Mountains & Volcanoes

Mount Fuji mountain, Japan Quick Summary Ask the Chatbot Print print Print Please select which sections you would like to print:

• Table Of Contents

Cite verifiedCite While every effort has been made to follow citation style rules, there may be some discrepancies. Please refer to the appropriate style manual or other sources if you have any questions. Select Citation Style MLA APA Chicago Manual of Style Copy Citation Share Share Share to social media Facebook X URL https://www.britannica.com/place/Mount-Fuji Feedback External Websites Feedback Corrections? Updates? Omissions? Let us know if you have suggestions to improve this article (requires login). Feedback Type Select a type (Required) Factual Correction Spelling/Grammar Correction Link Correction Additional Information Other Your Feedback Submit Feedback Thank you for your feedback

Our editors will review what you’ve submitted and determine whether to revise the article.

External Websites

• UNESCO World Heritage Convention - Fujisan, sacred place and source of artistic inspiration
• World History Encyclopedia - Mount Fuji
• Smithsonian Institution - National Museum of Natural History - Global Volcanism Program - Fujisan

Britannica Websites Articles from Britannica Encyclopedias for elementary and high school students.

• Mount Fuji - Children's Encyclopedia (Ages 8-11)
• Mount Fuji, or Fujiyama - Student Encyclopedia (Ages 11 and up)

Quick Summary Ask the Chatbot a Question Also known as: Fuji no Yama, Fuji-san, Fujisan, Fujiyama Written and fact-checked by Britannica Editors Encyclopaedia Britannica's editors oversee subject areas in which they have extensive knowledge, whether from years of experience gained by working on that content or via study for an advanced degree.... Britannica Editors Last updated Dec. 18, 2025 •History Table of Contents Table of Contents Quick Summary Ask the Chatbot a Question Top Questions

Why is Mount Fuji famous?

Rising to 12,388 feet (3,776 metres), Mount Fuji is the tallest mountain in Japan and is known for its graceful conical form. It is the country’s sacred symbol, and temples and shrines are located around and on the volcano. Climbing the mountain has long been a religious practice, and Fuji is one of Japan’s most popular tourist attractions.

Where is Mount Fuji located?

The mountain is located in Yamanashi and Shizuoka ken (prefectures) of central Honshu, Japan, about 60 miles (100 km) west of the Tokyo-Yokohama metropolitan area. It 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.

How was Mount Fuji formed?

While tradition holds that the volcano was created by an earthquake, the truth is more complex. Fuji seems to have formed during the past 2.6 million years. The present-day mountain is a composite of three successive volcanoes: at the bottom is Komitake, which was surmounted by Ko Fuji (“Old Fuji”) and, finally, by the most recent, Shin Fuji (“New Fuji”). Over the millennia the lava and other ejecta from Ko Fuji covered most of Komitake.

Is Mount Fuji active?

The volcano is considered active and has erupted more than 15 times since 781. However, Mount Fuji has been dormant since an eruption in 1707, and its last signs of volcanic activity occurred in the 1960s. Given concerns about the extensive damage that would be caused by an eruption, Fuji is monitored 24 hours a day.

News •

Village near Mount Fuji aims to draw more visitors with hot air balloon rides • Dec. 17, 2025, 5:58 PM ET (Straits Times) Show less

Mount Fuji, highest mountain in Japan. It rises to 12,388 feet (3,776 metres) near the Pacific Ocean coast in Yamanashi and Shizuoka ken (prefectures) of central Honshu, about 60 miles (100 km) west of the Tokyo-Yokohama metropolitan area. It is a volcano that has been dormant since its last eruption, in 1707, but is still generally classified as active by geologists. The mountain is the major feature of Fuji-Hakone-Izu National Park (1936), and it is at the centre of a UNESCO World Heritage site designated in 2013.

Cultural significance

The origin of the mountain’s name is uncertain. It first appears as Fuji no Yama in Hitachi no kuni fudoki (713 ce), an early government record. Among the several theories about the source of the name is that it is derived from an Ainu term meaning “fire,” coupled with san, the Japanese word for “mountain.” The Chinese ideograms (kanji) now used to write Fuji connote more of a sense of good fortune or well-being. In the present day the Japanese typically refer to the mountain as Fujisan, whereas foreign visitors tend to refer to the mountain somewhat incorrectly as Mount Fujiyama, which translates to “Mount Fuji mountain” in the Japanese language.

Mount Fuji, with its graceful conical form, has become famous throughout the world and is considered the sacred symbol of Japan. Among Japanese there is a sense of personal identification with the mountain, and each summer thousands of Japanese climb to the shrine on its peak. Its image has been reproduced countless times in Japanese art, perhaps no more famously than in the series of woodblock prints Thirty-six Views of Mount Fuji by Hokusai, which were originally published between 1826 and 1833.

Origin

1 of 2

2 of 2

According to tradition, the volcano was formed in 286 bce by an earthquake. The truth is somewhat more complex. The age of Fuji is disputed, but it seems to have formed during the past 2.6 million years on a base dating from up to 65 million years ago; the first eruptions and the first peaks probably occurred sometime after 700,000 years ago. The earliest precursors to Mount Fuji were Komitake (which forms the mountain’s north slope) and Ashitaka-yama (which sits southeast of the mountain). Mount Fuji is a stratovolcano that rose sometime after 400,000 years ago between the peaks of Komitake and Ashitaka-yama. The present-day mountain is a composite of three successive volcanoes: at the bottom is Komitake, which was surmounted by Ko Fuji (“Old Fuji”) about 100,000 years ago and, finally, by the most recent, Shin Fuji (“New Fuji”). Over the millennia, the lava and other ejecta from Ko Fuji covered most of Komitake, although the top of the latter’s cone continued to protrude from the slope of Ko Fuji. Shin Fuji probably first became active about 10,000 years ago and has continued ever since to smolder or erupt occasionally. In the process it has filled in the slopes of its predecessors and added the summit zone, producing the mountain’s now nearly perfect tapered form.

The base of the volcano is about 78 miles (125 km) in circumference and has a diameter of some 25 to 30 miles (40 to 50 km). At the summit of Mount Fuji the crater spans about 1,600 feet (500 metres) in surface diameter and sinks to a depth of about 820 feet (250 metres). Around the jagged edges of the crater are eight peaks—Oshaidake, Izudake, Jojudake, Komagatake, Mushimatake, Kengamine, Hukusandake, and Kusushidake.

Japanese: Fuji-san (Show more) Also spelled: Fujisan (Show more) Also called: Fujiyama or Fuji no Yama (Show more) See all related content Britannica Quiz All About Mountains Quiz

Mount Fuji is part of the Fuji Volcanic Zone, a volcanic chain that extends northward from the Mariana Islands and the Izu Islands through the Izu Peninsula to northern Honshu. Geologists note that the subduction of the Pacific Plate beneath the Philippine Plate at the Nankai Trough, which extends along Japan’s southern coast, likely drives Mount Fuji’s volcanic activity. Large eruptions occur about every 500 years. Accounts of the most recent major eruption, in December 1707, note that ash darkened the midday sky as far as Edo (present-day Tokyo) and buried temples and dwellings near the mountain. Geologists report that the eruption was triggered by a magnitude-8.4 earthquake, which struck the region 49 days earlier. Mount Fuji’s volcanic activity since 1707 has been limited mostly to small earthquakes; however, a magnitude-6.4 aftershock struck the mountain’s southern flank in the days following the Great Sendai Earthquake of 2011.