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上富田町・マップ39:W12 下鮎川の河岸段丘

上富田町の富田川はあまり蛇行せず活断層帯の低地を流れます。右岸にある下鮎川には、小規模ながら典型的な河岸段丘が見られます。この河岸段丘は3段あり、もっとも広く発達する標高約65mにある2段目の段丘面には、耕地として利用され「平」や「畑」の字をもつ地名が多いです。

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".

google翻訳

うえもり う 2022/01/19(Wed) 20:57 No.101 [返信・追加]
Re: 上富田町・マップ39:W12 下鮎川の河岸段丘
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那智勝浦町・マップ62:E13 ゆかし潟

ハートの形をした潟湖で、満ち潮の時には海水が流入する汽水湖です。ゆかし潟ができたのは、海水面がマイナス100mを超える位置まで低下していた2万年前の寒冷な氷期から、温暖化に伴って海水面が上昇してきたことに加えて、湯川川と橋ノ川の合流部の下流側で、二河川から供給された土砂によって堰き止められたことによります。ゆかし潟という名称は、郷土の詩人・佐藤春夫により名づけられました。「ゆかし潟および太田川河口」が環境省重要湿地に登録されています。

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.

google t.

うえもり う 2022/01/20(Thu) 15:30 No.125 [返信・追加]
Re: 那智勝浦町・マップ62:E13 ゆかし潟
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.

ジョシュアの編集
ジョシュア 2022/09/09(Fri) 18:32 No.322
Re: 那智勝浦町・マップ62:E13 ゆかし潟
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.

ジョシュアの編集2
ジョシュア 2022/09/09(Fri) 20:42 No.332
Re: 那智勝浦町・マップ62:E13 ゆかし潟
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.

ジョシュアの編集3
ジョシュア 2022/09/09(Fri) 20:46 No.333
Re: 那智勝浦町・マップ62:E13 ゆかし潟
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.

ジョシュアの編集6
ジョシュア 2022/09/09(Fri) 20:54 No.336
Re: 那智勝浦町・マップ62:E13 ゆかし潟
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.
ジョシュアの編集7
ジョシュア 2022/09/09(Fri) 20:58 No.337
Re: 那智勝浦町・マップ62:E13 ゆかし潟
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: 那智勝浦町・マップ62:E13 ゆかし潟
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Re: 那智勝浦町・マップ62:E13 ゆかし潟
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那智勝浦町・マップ57:E9 弁天島とお蛇浦

"景勝地である弁天島には、大潮の干潮には歩いて渡ることができます。弁天島とお蛇浦南端の海岸には緩く傾いた熊野層群の地層があり、小規模な断層や褶曲のほか、生痕化石などが見つかります。お蛇浦遊歩道の入口付近には、地層内部で大規模な液状化・流動化が起り、地下から周囲の岩石を取り込みながら上昇してできた泥ダイアピルがあります。この場所では熱水活動の痕跡も観察されます。

"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.

google t.

うえもり う 2022/01/20(Thu) 15:13 No.120 [返信・追加]
Re: 那智勝浦町・マップ57:E9 弁天島とお蛇浦
"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.
ジョシュアの編集
ジョシュア 2022/09/09(Fri) 18:54 No.324
Re: 那智勝浦町・マップ57:E9 弁天島とお蛇浦
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白浜町・マップ32:W13 保呂の虫喰岩

この岩壁は田辺層群上部層の厚い砂岩と礫岩の地層からなり、礫岩の部分に「虫喰い」風化がよく見られます。岩壁には多数の凹みが蜂の巣状に密集しています。この蜂の巣状の風化はタフォニと呼ばれ、地層中の塩類の溶解と析出によってできたと考えられています。

This rock wall consists of thick sandstone and conglomerate formations in the upper part of the Tanabe Group, and "insect-eating" weathering is often seen in the conglomerate part. Many dents are densely packed in the rock wall like a honeycomb. This honeycomb-like weathering is called tafoni and is thought to have been caused by the dissolution and precipitation of salts in the formation.

google t

うえもり う 2022/01/20(Thu) 22:26 No.206 [返信・追加]
Re: 白浜町・マップ32:W13 保呂の虫喰岩
fjvvdstfsm 2024/09/23(Mon) 03:36 Home No.428
上富田町・マップ45:W16 彦五郎堤防

彦五郎堤防は富田川の右岸に位置し、約1kmにおよぶ長大な堤防です。氾濫を繰り返した富田川の治水のために人柱になったという彦五郎の伝説がある堤防です。堤防上に4基の石塔が建ち、1基は人柱彦五郎顕彰碑、1基は明治洪水招魂碑です。


The Hikogoro embankment is located on the right bank of the Tonda River and is a long embankment that stretches for about 1 km. It is a dike with the legend of Hikogoro, who became a pillar for the flood control of the Tonda River, which was repeatedly flooded. Four stone towers are built on the embankment, one is the Hitobashira Hikogoro Honoring Monument and one is the Meiji Flood Invitation Monument.

google translation

うえもり う 2022/01/20(Thu) 14:35 No.108 [返信・追加]
Re: 上富田町・マップ45:W16 彦五郎堤防
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