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The 1707 Eruption of Fuji Volcano and Its Tephra
Naomichi MIYAJI
Department of Geosystem Sciences, College of Humanities and Sciences, Nihon University
Sakurajyousui 3-25-40, Setagaya-ku, Tokyo, 156-8550 JapanAbstract
The 1707 eruption of Mt. Fuji with large amounts of pyroclastic fall was the most recent and oneof the most violent eruptions of this volcano. The magma discharge rate was the largest on the firstday and increased again after nine days. No victims of this eruption were reported, except those lostby starvation after the eruption because farmlands had been buried. Further eruptions are possible, so
it is important to prepare for them by drafting hazard maps and considering ways to cooperate with Mt.
Fuji because the volcano also provides great benefits.
Key words: Fuji volcano, historical document, magma discharge rate, tephra, 1707 eruption, volcanic
hazard

1. The Eruptions of the Fuji Volcano
Mt. Fuji has erupted repeatedly for the last 100,000years. The mountain is composed of two volcanoes,
Older Fuji (100,000 to 11,000 years ago), which
erupted on the ancient Komitake volcano (several
hundred thousands years old; Tsuya, 1968) andproduced basaltic pyroclastics, and Younger Fuji
(11,000 years ago to present), which produced basaltic
pyroclastics and lava. The 1707 eruption (called theHoei eruption) was the most recent and most violent
eruption of the Younger Fuji volcano. The Younger
Fuji built its edifice with many lava flows and pyroclastic deposits (tephra) from its summit and flankcraters. The craters of magmatic eruption shiftedfrom the summit to the flanks about 2,200 years ago(Miyaji, 1988). During the 1707 eruption, great volumes of scoria and small amounts of pumice dispersedto the east from the Hoei craters on the southeastern
flank of Mt. Fuji (Tsuya, 1955). In this paper, I summarized the sequence and hazards of the 1707
eruption and the characteristics of the tephra from thiseruption based on the results of recent studies.

2. The Sequence of the 1707 Eruption
The sequence of the 1707 eruption was reconstructed in detail based on many historical documents
and geological data (Koyama et al., 2002; Miyaji andKoyama, 2002). On October 28, 1707, a large earthquake (M8.4) occurred on the coast of middle Honshu,
the main island of Japan (the Hoei-Tokai-Nankaiearthquake). After the eruption, several smaller
earthquakes occurred on and around the Fuji volcano.

The eruption started at about 10 a.m., December 16,
on the southeastern flank of the volcano with a highcolumn making pumice fall deposits. The tephrachanged from pumice to scoria after about six hours
from the start of the first eruption. This violent eruption with scoria fall ceased early in the morning ofDecember 17. The eruption continued intermittently
until the evening of December 25 with eruptions ceasing for periods of nearly half a day. Violent eruptions occurred again from the evening of December 25
to the 27th. After that, the scale of the eruptions
decreased, with rumbling and emission of volcanic
bombs on December 31 to January 1. The activity
ceased completely on the morning of January 1, 1708.
This eruption produced no lava or pyroclastic flows.
During this eruption, three craters were formed,
named Hoei First to Third in order of descent from thesummit at elevations of 3,100 to 2,150 m. Judging
from the distribution of the tephra, the geomorphologyof the craters and descriptions in historical documents,
the Hoei Second and Third craters were formed on
December 16 to 17 or later, and the First crater wasformed from December 17 to January 1. Mt. Hoei,
which is composed of the tephra of the older Fuji
volcano, was formed close to the Hoei craters during
the early stages of forming the Hoei First crater.

3. Characteristics of the 1707 Tephra
The tephra of the 1707 eruption covers most of thesouth Kanto plain, including Tokyo, and is found indeep sea cores in the northwestern Pacific Ocean,
280 km distant from the crater (Machida and Arai,1988). Distribution of the tephra has been reconstructed based on data from historical documents and38

N. MIYAJI

geological surveys (Fig. 1; Cabinet Office, 2002).
The 1707 tephra is composed of four groups, Ho-Ito -IV (Miyaji, 1984). The time of formation of eachgroup was estimated as follows by correlating thedescription from historical documents with the geological data (Miyaji and Koyama, 2002). Ho-I:
coarse pumice layers at the bottom of the 1707 tephra
which were formed from the mourning before noon on
December 16 to the late afternoon of that day. Ho-II:coarse scoria layers overlaying Ho-I which wereformed from the evening of December 16 to the morning of the 17th. Ho-III: an alternation of coarser tofiner scoria beds with coarse volcanic ash beds whichwere formed from the morning of December 17 to theevening of the 25th. The volcanic ash layers ofHo-III may have formed during periods of decliningeruptions. Ho-IV: two parts, the lower consisting ofcoarse scoria beds and the upper of fine scoria beds
which were formed from the evening of December 25
to the morning of January 1, 1708.
Magma discharge rates are estimated based on thetime of formation and volume of each group. The
volume of each group is estimated based on maps ofthickness of each group. The total volume is estimated to have been 0.68 km3 of dense rock equivalent
which formed over a period of 16 days. The averagemagma discharge rate during the formation of Ho-Iand II was 7×10–3 km3/hour, which was the maximum
for the 1707 eruption. While the average rate for theHo-III eruption declined to 1×10–3 km3/hour, the rateof the Ho-IV eruption increased to 4×10–3 km3/hour,
especially during the first half of the period.
The magma composition of the eruption varied
from the beginning to the end of the eruption. The
pumice of Ho-I changed from dacite to andesite, thescoria of Ho-II was andesite, and the scoria of Ho-III
and IV were basalt (Tsukui, 1985).

4. Volcanic Hazards of the 1707 Eruption
Many people lost their lives from starvation after
the eruption from the eastern foot of Mt. Fuji despite
no victims being recorded as a direct result of thetephra fall-out. In the village of Subashiri, at a 10 km
distance east of the Hoei craters, 72 houses and three
Buddhist temples, which were all part of the village,
were burned or crushed on the first day of the eruption.
After the eruption, many inhabitants could neither
obtain food from their farmland nor move easily toother places, so many died of starvation. The number of houses decreased by one thirds during fourteen
years after the eruption in a village where the tephra
was two meters thick (Kikuchi, 1990). The Sakawa
River, a large river flowing along the eastern foot ofMt. Fuji, flooded repeatedly for nearly 80 years after
the eruption. Flooding occurred even on small rivers
where the thickness of the tephra exceeded ten
centimeters (Cabinet Office, 2002). In these areas,Fig. 1 Thickness of the 1707 tephra, based on data from historical documents and geological data (in cm).
Modified Cabinet Office (2002)

The 1707 Eruption of Fuji Volcano and Its Tephra

the tephra was probably eroded easily by the rain anddeposited thickly on the river bottoms.

5. Readiness for the Next Eruption
The increase in low frequency earthquakes in 2000
- 2001 on the Fuji volcano reminds us that the volcano
is still active. The Cabinet Office of Japan created acommittee in July 2001 to draft a hazard map of theFuji volcano to minimize hazards during the nexteruption. An eruption like the Hoei eruption is theworst-case scenario on the map as the tephra disperses
widely in accordance with the wind speed anddirection at the time of eruption. We must prepare
for this kind of large eruption and also consider that
this type of eruption was the largest since 2,200 years
ago. Most of the eruptions that occurred during thisperiod were on the order of several tens of times
smaller than this eruption (Miyaji, 1992).
At the same time, Mt. Fuji provides us benefits
such as a beautiful landscape and flat land areas.
The 1707 tephra has been useful as a material forbuilding and gardening. Tephras of the Fuji volcano
have become the parent materials for volcanic soil thatoccupies most of the arable land of the southern Kanto
Plain. We must consider the enormous benefits ofthe Fuji volcano as well as the hazards resulting fromthe next eruption, and consider ways to cooperate withthe volcano.

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References
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and N. Anyoji (2002) Reconstruction of the 1707 Hoei
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Kikuchi, K. (1990) The Hoei eruption of Mt. Fuji. Annals of theGeography (The Chiri Shiso), Nihon Unv. Geographical
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Machida, H. and F. Arai (1988) A review of late Quaternary
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Tsukui, H. (1985) A magma reservoir and its evolution beneatha polygenetic volcano. Doctoral thesis of University ofTokyo, University of Tokyo, Tokyo.
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(Received 9 September 2002, Accepted 10 October 2002)