when was the last time mount fuji errupted
1707–1708
title: Mount Fuji text: between 7,000 and 3,500 years ago, and between 4,000 and 2,000 years ago. Flank eruptions, mostly in the form of parasitic cinder cones, ceased in 1707. The largest cone, Omuro-Yama, is one of more than 100 cones aligned NW-SE and NE-SW through the summit. Mt. Fuji also has more than 70 lava tunnels and extensive lava tree molds. Two large landslides are at the head of the Yoshida-Osawa and Osawa-Kuzure valleys. , the volcano is classified as active with a low risk of eruption. The last recorded eruption was the Hōei eruption which started on December 16, 1707 ("Hōei 4, title: Mount Fuji text: 23rd day of the 11th month"), and ended about January 1, 1708 ("Hōei 4, 9th day of the 12th month"), during the Edo period. The eruption formed a new crater and a second peak, named Mount Hōei (after the Hōei era), halfway down its southeastern side. Fuji spewed cinders and ash which fell like rain in Izu, Kai, Sagami, and Musashi. Since then, there have been no signs of an eruption. In the evening of March 15, 2011, there was a magnitude 6.2 earthquake at shallow depth a few kilometres from Mount Fuji on its southern side. But according to title: Mount Fuji text: Mount Fuji , located on Honshū, is the highest mountain in Japan at 3,776.24 m (12,389 ft), 2nd-highest peak of an island (volcanic) in Asia, and 7th-highest peak of an island in the world. It is a dormant stratovolcano that last erupted in 1707–1708. Mount Fuji lies about 100 kilometers (60 mi) south-west of Tokyo, and can be seen from there on a clear day. Mount Fuji's exceptionally symmetrical cone, which is snow-capped for about 5 months a year, is a well-known symbol of Japan and it is frequently depicted in art and photographs, as well as visited by sightseers title: Historic eruptions of Mount Fuji text: the period between 1083 and 1511, when no eruptions were recorded for over 400 years. At present, there have been no eruptions since the Hoei eruption in 1707–1708, around 300 years ago. Scientists study the activity of the magma rising by measuring CO emissions in the deeper parts of the volcano. Studies from before the Tohoku earthquake show the CO emissions below 5 gCO/m/day, which is the detection limit. If the emissions rise above 5 gCO/m/day then seismic activity is occurring and an eruption could possibly take place. According to a five-stage evolutionary model for the release of volcanic gas, title: Mount Haku text: Mount Haku , or Mount Hakusan (commonly referred to as simply Hakusan), is a dormant volcano. The stratovolcano is located on the borders of Gifu and Ishikawa (which are in Honshu) prefectures in Japan. It is thought to have first been active 300,000 to 400,000 years ago, with the most recent eruption occurring in 1659. Along with Mount Tate and Mount Fuji, it is one of Japan's . The mountain's tallest peak, Gozengamine (御前峰), is the one that gives the mountain its height of . Along with Kengamine (剣ヶ峰), which is , and Ōnanjimine (大汝峰), which is , the three