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It is a large hole in the rhyolite pyroclastic rocks distributed on Kii Oshima. It is probable that the ceiling of the seafood cave made of igneous rock collapsed. The bottom is connected to the sea. There is a legend that Rikubu (a person who pays sutras to the sacred sites of 66 countries) was chased by two samurais, chased to the edge of this hole, slaughtered, and fell to the bottom.

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The Tonda River in Kamitonda Town does not meander very much and flows through the lowlands of the active fault zone. The Shimoayukawa on the right bank has a small but typical river terrace. This river terrace has three steps, and on the second terrace surface, which is the most widely developed terrace at an altitude of about 65 m, there are many place names that are used as cultivated land and have the characters "hira" and "field".

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It is a heart-shaped lagoon, a brackish lake where seawater flows in at high tide. The Yukawa River was created in addition to the rise in sea level due to warming from the cold glacial period 20,000 years ago when the sea level had dropped to a position exceeding -100 m. This is because it was blocked by the earth and sand supplied from the two rivers on the downstream side of the confluence of the Yukawa River. The name Yukashigata was named by the local poet Haruo Sato. "Yukashigata and Otagawa estuary" is registered as an important wetland by the Ministry of the Environment.

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Re: “ß’qŸ‰Y’¬Eƒ}ƒbƒv‚U‚QFE13@‚ä‚©‚µŠƒ
It is a heart-shaped, brackish lagoon where seawater flows in at high tide. The Yukashigata was created due to the rise in sea level caused by warming from the cold glacial period 20,000 years ago when the sea level had dropped to a position exceeding -100 m. This is because it was blocked by the earth and sand supplied from the two rivers on the downstream side of the confluence of the Yukawa River and the Hashinokawa. The name Yukashigata was named by the local poet Haruo Sato. "Yukashigata and Otagawa estuary" is registered as an important wetland by the Ministry of the Environment.

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It is a heart-shaped, brackish lagoon where seawater flows in at high tide. The Yukashigata was created due to the rise in sea level caused by warming from the cold glacial period 20,000 years ago when the sea level had dropped to a position exceeding -100 m. This is because it was blocked by the earth and sand supplied from the two rivers on the downstream side of the confluence of the Yukawa River and the Hashinokawa. Downstream from that confluence is the Niko River, which leads to the opening in the river leading to the ocean. The name Yukashigata was named by the famous poet Haruo Sato, who was born in the region surrounding the lagoon. The "Yukashigata and Otagawa estuary" is registered as an important wetland by the Ministry of the Environment.

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Re: “ß’qŸ‰Y’¬Eƒ}ƒbƒv‚U‚QFE13@‚ä‚©‚µŠƒ
It is a heart-shaped, brackish lagoon where seawater flows in at high tide. The Yukashigata was created due to the rise in sea level caused by warming from the cold glacial period 20,000 years ago when the sea level had dropped to a position exceeding -100 m. This is because it was blocked by the earth and sand supplied on the downstream side of the confluence of the Yukawa River and the Hashinokawa. Downstream from that confluence is the Niko River, which leads to the opening in the river leading to the ocean. The name Yukashigata was named by the famous poet Haruo Sato, who was born in the region surrounding the lagoon. The "Yukashigata and Otagawa estuary" is registered as an important wetland by the Ministry of the Environment.

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Re: “ß’qŸ‰Y’¬Eƒ}ƒbƒv‚U‚QFE13@‚ä‚©‚µŠƒ
It is a heart-shaped, brackish lagoon where seawater flows in at high tide. The Yukashigata was created due to the rise in sea level caused by warming from the cold glacial period 20,000 years ago when the sea level had dropped to a position exceeding -100 m. This is because it was blocked by the earth and sand supplied by the Niko RIver on the downstream side of the confluence of the Yukawa River and the Hashinokawa. Downstream from that confluence is the Niko River, which leads to the opening in the river leading to the ocean. The name Yukashigata was named by the famous poet Haruo Sato, who was born in the region surrounding the lagoon. The "Yukashigata and Otagawa estuary" is registered as an important wetland by the Ministry of the Environment.

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Re: “ß’qŸ‰Y’¬Eƒ}ƒbƒv‚U‚QFE13@‚ä‚©‚µŠƒ
It is a heart-shaped, brackish lagoon where seawater flows in at high tide. The Yukashigata was created due to the rise in sea level caused by warming from the cold glacial period 20,000 years ago when the sea level had dropped to a position exceeding -100 m. This is because it was blocked by the earth and sand supplied by the Niko River on the downstream side of the confluence of the Yukawa River and the Hashinokawa. Downstream from that confluence is the Niko River, which leads to the opening in the river leading to the ocean. The name Yukashigata was named by the famous poet Haruo Sato, who was born in this region. The "Yukashigata and Otagawa estuary" is registered as an important wetland by the Ministry of the Environment.
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ƒWƒ‡ƒVƒ…ƒA 2022/09/09(Fri) 20:58 No.337
Re: “ß’qŸ‰Y’¬Eƒ}ƒbƒv‚U‚QFE13@‚ä‚©‚µŠƒ
It is a heart-shaped lagoon and a brackish water lake where sea water flows in during the high tide. Yukashi Lagoon was formed when the sea level rose with global warming after a cold glacial period 20,000 years ago, when the sea level dropped to over minus 100 meters, and was dammed by sediment supplied from two rivers downstream of the confluence of the Yugawa River and the Hashino River. The name "Yukashi Lagoon" was given by local poet Haruo Sato. Yukashi Lagoon and the mouth of the Ota River" is registered as an important wetland by the Ministry of the Environment.

Translated with www.DeepL.com/Translator (free version)
‚¤ 2022/11/10(Thu) 00:07 No.357
Re: “ß’qŸ‰Y’¬Eƒ}ƒbƒv‚U‚QFE13@‚ä‚©‚µŠƒ
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"Bentenjima, a scenic spot, can be walked to the low tide of the spring tide. There is a gently sloping Kumano Group on the coast of Bentenjima and the southern tip of Hebiura, with small faults and folds. In addition, trace fossils can be found. A large-scale liquefaction and fluidization occurs inside the stratum near the entrance of the Ojaura promenade, and the mud diapill that rises while taking in the surrounding rocks from the underground. There are also traces of hydrothermal activity in this area.

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"Bentenjima, a scenic spot, can be walked to during low tide. There is a gently sloping rock formation of the Kumano Group on the coast of Bentenjima and the southern tip of Ojaura, with small faults and folds. In addition, trace fossils can be found. A large-scale liquefaction and fluidization occurs inside the stratum near the entrance of the Ojaura promenade, and the mud diapir that rises while taking in the surrounding rocks from the underground. There are also traces of hydrothermal activity in this area.
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