Title Buried Forest: Creation

  • Tottori
  • Shimane
Topic(s):
$SETTINGS_DB.genreMap.get($item) National Parks/Quasi-National Parks Public Works & Institutions (Museums, etc.)
Medium/Media of Use:
App, QR code, etc.
Text Length:
≤250 Words
FY Prepared:
2019
Associated Tourism Board:
Daisen-Oki National Park

埋没林の成因


埋没林を埋めている地層を分析することで、科学者たちは埋没と保存に至った事象を再構築することができる。約 4,000 年前に三瓶山の噴火が始まった。火山の圧力で山の北側が崩壊し、岩、土砂、泥が崩れて北側の谷へとなだれ込んだ。この泥と堆積物で、地下 20~12 メートルの谷を埋める下層ができた。

次に、噴火により生じたガス、火山灰、火山礫の火砕流が、厚い灰の層とともに下層を覆った。この火砕流が非常に熱かったことは、地下 15~10 メートルのこの層に混ざる炭化した幹や焦げた木片からわかる。

最初の土石流による堆積物が小豆原谷を流れていた川をせき止め、氾濫が起きた。そこへ火山灰や火山堆積物が上流からさらに谷へと流れ込み、行き場所を失ってそこで積み重なった。この火山灰の第二層は地下 10~2 メートルに広がっている。現在、地面の上部 2 メートルは土と近代の堆積物で構成されている。

噴火前は、森林の木々は現在まで保存されていた幹よりもずっと高く伸びていた。たとえば最も高いものは、残っている幹は高さ 12.5 メートルしかないが、噴火の威力で上部が壊される前は、一部の木は 50 メートルもあったのではないかと科学者は推測している。


Buried Forest: Creation


Analysis of the layers of soil surrounding the Buried Forest has helped scientists reconstruct the events that led to its burial and preservation. Approximately 4,000 years ago, Mt. Sanbe began to erupt. Pressure from within the volcano caused its northern side to collapse, sending an avalanche of rock, sand, and mud crashing down into the northern valleys below. This layer of mud and debris makes up the lowest layer filling the valley, between 20 and 12 meters below the surface.

Next, pyroclastic flow—a scorching wave of gas, ash, and stone particles called lapilli—burst from the mountain, covering the avalanche material with a thick layer of ash. The extreme heat of that flow is evident from charred bark and chips of burned wood mixed into this layer, which ranges from 15 to 10 meters below the surface.

Debris from the initial avalanche blocked the river that flowed through the Azukihara valley, causing it to flood. As more ash and volcanic sediment was carried to the valley by the current, it had nowhere to go, and it accumulated there. This secondary layer of accumulated ash stretches from 10 to 2 meters below the surface. Today, the top two meters of earth consist of soil and modern deposits of river sediment.

Before the eruption, the trees of the forest are thought to have reached much higher than their preserved trunks do now. The tallest remaining trunk segment, for instance, measures only 12.5 meters in height, but scientists estimate that some of the trees were as tall as 50 meters before their upper portions were broken off by the force of the eruption.


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