On 26th October 1707, another eruption show itself with an expansive 8.4 extent tremor destroying the Honshu island, trailed by a few littler tremors felt close Mt Fuji. The explosion began on sixteenth December 1707 from another vent on the South East flank of the spring of rushing lava emitting a sub-plinian segment of fiery remains, transforming into basaltic magma fountaining following 6 hours of ejection. On the principal day of the emission, 72 houses and 3 Buddhist sanctuaries were destroyed in Subassiri town 10 km from the spring of gushing lava. Cinder fell everywhere throughout the south Kanto area in Tokyo, and on territories of the North West Pacific sea 280 km from the fountain of liquid magma. The aggregate volume emitted more than 16 days was evaluated to 0.68 cubic km of magma. Fierce blasts were recorded until 25-27 December, before the emission quieted down and finished on first January 1708.
From 8000 to 4500 years prior, Fuji's action was for the most part touchy before another gushing cycle occurred between 4500 to 3000 years back. In the previous 3000 years, huge unstable ejections happened in the middle of periods of milder unreserved action. From 3000 to 2000 years back, most emissions occurred at the summit, while a substantial number of flank ejections happened amid the previous 2000 years, framing more than 100 flank cones.