Ishigedo - Towada

3.5/5 に基づく 4 レビュー

Contact Ishigedo

住所 :

石ケ戸(バス Okuse, Towada, Aomori 034-0301, Japan

Postal code : 034-0301
カテゴリ:

石ケ戸(バス Okuse, Towada, Aomori 034-0301, Japan
裕二広田 on Google

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yasuyuki oba on Google

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Shinichi Nakashima on Google

休憩所を出て、すぐ。標識に注意して歩かないと。紅葉に感動して歩くと見過ごしてしまうかも。石ヶ戸」とは、この地方の方言で、《石でできた小屋》という意味らしい。桂の木に支えられた大きな一枚岩は、その名のように小屋にも見えます。との事。
Immediately after leaving the rest area. You have to pay attention to the signs and walk. If you are impressed by the autumn leaves and walk, you may overlook it. "Ishigedo" is a dialect of this region and seems to mean "a hut made of stone". The large monolith supported by the katsura tree looks like a hut as its name suggests. That thing.
吉田博史 on Google

奥入瀬渓谷を歩くたびに思うことだが、東八甲田カルデラ火山の爆発はものすごいものであり、十和田市三本木原までが火砕流に吞まれ、火山灰はもっと広い範囲で堆積した。爆発後にやや南側で爆発した十和田カルデラ火山の原カルデラ湖は今より水位がずっと高かった。いまの休屋のあたりの湖底噴火で枕状溶岩ができるほど水圧があった。そして子ノ口のあたりで決壊すると、またたくまに流れ出した奔流が火砕流でできた溶結凝灰岩の大地を削り、奥入瀬峡谷ができたという事実。 その証拠物件が渓谷のあちこちに見られるのだが、石ケ戸の岩屋もその一つである。岩屋を形づくっている溶結凝灰岩の板状の一枚岩は板状節理によるものだ。方状節理の圧倒的に多い奥入瀬渓谷では板状節理を今の時点で確認できる場所はそんなに多くはない。火砕流の上部でできたものがほとんど粉砕され流されて大きなものを他で見ないのかもしれない。現在渓流沿いにある岩石は流されて角が削れた方状節理由来のものが圧倒的に多く、石ケ戸の岩屋の屋根岩を支えているのもそのような岩だ。とにかくあんな巨大で固い岩を押し流した流れがあったことを想像すると、自然の力の凄さを思い知らされる。 路線バスでも紹介される盗賊「鬼神のお松」のお話は全くの作り話であるのは明白なのでやめてほしいものだ。この道路は明治期に作られた道であり、江戸時代には三本木、三戸方面から十和田湖への道は月日山を越える山道しかなかった。その道は惣部牧野付近から寒沢の峡谷をを越えられず、寒沢に沿って下り、銚子大滝付近で現在の道路と同じルートとなり子ノ口に出ていて、石ヶ戸付近に道はなかったのだから。
Every time I walked in the Oirase Gorge, the explosion of the Higashi-Hakkoda caldera volcano was tremendous, and the pyroclastic flow up to Sanbongihara in Towada City caused volcanic ash to accumulate over a wider area. The water level of the original caldera lake of Towada caldera volcano, which exploded slightly to the south after the explosion, was much higher than it is now. The water pressure was so high that pillow lava was formed by the eruption of the lake bottom around the current closed house. And when it broke around Konoguchi, the torrent that flowed out suddenly scraped the ground of welded tuff formed by the pyroclastic flow, and the fact that the Oirase Gorge was created. Exhibits can be found all over the valley, including Iwaya in Ishigado. The plate-shaped monoliths of welded tuff that form the Iwaya are due to plate-like joints. In the Oirase Gorge, where square joints are overwhelmingly large, there are not many places where plate joints can be confirmed at this time. Most of what is made at the top of the pyroclastic flow is crushed and washed away, and you may not see anything else big. Currently, the rocks along the mountain stream are overwhelmingly the ones that have been washed away and the corners have been shaved, and it is such rocks that support the roof rocks of Iwaya in Ishigado. Imagine that there was a stream that swept away such a huge and hard rock, and I was reminded of the power of nature. It is clear that the story of the thief "Kijin Omatsu", which is also introduced on the route bus, is a complete myth, so I would like you to stop. This road was built in the Meiji period, and in the Edo period, the only road from Sannohe and Sannohe to Lake Towada was a mountain road that crossed Tsukihiyama. The road could not cross the canyon of Kanzawa from the vicinity of Sobe Makino, went down along Kanzawa, became the same route as the current road near Choshi Otaki, and went out to Konoguchi, and there was no road near Ishigedo. Because.

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