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‹IˆÉ‘哇‚É•ª•z‚·‚é—¬–äŠâŽ¿‰ÎÓŠâ’†‚ɋ󂢂½‘å‚«‚ÈŒŠ‚Å‚·B‰Î¬Šâ‚©‚ç‚È‚éŠCH“´ŒA‚Ì“Vˆä‚ª•ö—Ž‚µ‚½‚à‚Ì‚Æl‚¦‚ç‚ê‚Ü‚·B’ê‚ÍŠC‚ÆŒq‚ª‚Á‚Ä‚¢‚Ü‚·B‚©‚‚ÄA˜Z•”i˜Z\˜ZƒJ‘‚Ì—ìê‚É‚¨Œo‚ð”[‚߂ĉô‚ésŽÒj‚ª‚Ql‚Ì•Žm‚É’Ç‚¢‚©‚¯‚ç‚êA‚±‚ÌŒŠ‚Ì•£‚܂Œǂ¢‚‚߂ç‚êŽa‚èŽE‚³‚ê’ê‚É“]—Ž‚µ‚½‚Æ‚¢‚¤“`à‚ª‚ ‚è‚Ü‚·B


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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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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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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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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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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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.

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‚¤ 2022/11/10(Thu) 00:07 No.357
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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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ivoedfgxl 2024/10/02(Wed) 11:16 Home No.429
”’•l’¬Eƒ}ƒbƒv‚R‚QFW13@•Û˜C‚Ì’Ž‹òŠâ

‚±‚ÌŠâ•ǂ͓c•Ó‘wŒQã•”‘w‚ÌŒú‚¢»Šâ‚ÆâIŠâ‚Ì’n‘w‚©‚ç‚È‚èAâIŠâ‚Ì•”•ª‚Éu’Ž‹ò‚¢v•—‰»‚ª‚æ‚­Œ©‚ç‚ê‚Ü‚·BŠâ•ǂɂ͑½”‚̉š‚Ý‚ª–I‚Ì‘ƒó‚É–§W‚µ‚Ä‚¢‚Ü‚·B‚±‚Ì–I‚Ì‘ƒó‚Ì•—‰»‚̓^ƒtƒHƒj‚ƌĂ΂êA’n‘w’†‚̉–—Þ‚Ì—n‰ð‚ÆÍo‚É‚æ‚Á‚Ăł«‚½‚Æl‚¦‚ç‚ê‚Ä‚¢‚Ü‚·B

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.

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‚¤‚¦‚à‚è@‚¤ 2022/01/20(Thu) 22:26 No.206
Re: ”’•l’¬Eƒ}ƒbƒv‚R‚QFW13@•Û˜C‚Ì’Ž‹òŠâ
fjvvdstfsm 2024/09/23(Mon) 03:36 Home No.428
ã•x“c’¬Eƒ}ƒbƒv‚S‚TFW16@•FŒÜ˜Y’ç–h

•FŒÜ˜Y’ç–h‚Í•x“cì‚̉EŠÝ‚Ɉʒu‚µA–ñ‚P‚‹‚‚É‚¨‚æ‚Ô’·‘å‚È’ç–h‚Å‚·B”×”‚ðŒJ‚è•Ô‚µ‚½•x“cì‚ÌŽ¡…‚Ì‚½‚ß‚Él’Œ‚ɂȂÁ‚½‚Æ‚¢‚¤•FŒÜ˜Y‚Ì“`à‚ª‚ ‚é’ç–h‚Å‚·B’ç–hã‚É4Šî‚ÌΓƒ‚ªŒš‚¿A‚PŠî‚Íl’Œ•FŒÜ˜YŒ°²”èA‚PŠî‚Í–¾Ž¡^…µ°”è‚Å‚·B


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

‚¤‚¦‚à‚è@‚¤ 2022/01/20(Thu) 14:35 No.108
Re: ã•x“c’¬Eƒ}ƒbƒv‚S‚TFW16@•FŒÜ˜Y’ç–h
mlffdxfnd 2024/09/23(Mon) 03:34 Home No.427
ykvnwnfx

‘ÛƒT[ƒNƒ‹—pî•ñŽºEDB
[url=http://www.gfw330815jbk4urf4ul4m96cb0o3589ts.org/]uykvnwnfx[/url]
ykvnwnfx http://www.gfw330815jbk4urf4ul4m96cb0o3589ts.org/
<a href="http://www.gfw330815jbk4urf4ul4m96cb0o3589ts.org/">aykvnwnfx</a>

ykvnwnfx 2024/09/22(Sun) 23:25 Home No.426
ƒWƒIƒp[ƒNƒZƒ“ƒ^[@“ü‚èŒûƒpƒlƒ‹

Žñ‹L@“Y•t‚Ípdf ‚Å‚·B

‚¤‚¦‚à‚è@‚¤ 2022/01/21(Fri) 21:47 No.223
Re: ƒWƒIƒp[ƒNƒZƒ“ƒ^[@“ü‚èŒûƒpƒlƒ‹
Three Landmasses Formed by the Convergence of Tectonic Plates: Nanki Kumano Geopark

The accretionary prism, the forearc basin sediment, and the igneous rock body are three geological formations created by the convergence of oceanic and continental plates. In the Nanki Kumano area, these formations are the stage for stunning natural wonders and diverse ecosystems. It was also the birthplace of the Kumano faith and its unique culture.

Experiencing the Nature and Culture of Kumano

A geopark is a place where researchers and local communities work together to conserve and utilize the precious things from the earth.
You will be able to experience the relationship between humanity and the land`s resources while learning about the history of the Earth.

Plate Subduction Forms 3 Landmasses

More than a dozen tectonic plates cover the surface of the Earth. At the western edge of the Pacific Ocean, oceanic plates (tectonic plates in the ocean) were subducted under continental plates(tectonic plates that contain continents). The subduction of these plates created the geological formations that created this region.

70 Million - 20 Million Years Ago

The Accretionary Prism
As the oceanic plate was subducted under the continental plate, sediment accumulated in the ocean trench, and was pushed into the continent. This process created the accretionary prism upon which all of the Nanki Kumano area rests.

18 Million - 15 Million Years Ago

Forearc Basin Sediment
The ocean side of the accretionary prism was pushed upward, creating a tray-like depression where mud, sand, and other material that flowed from the continent collected. That buildup of sedimentation created the landmass that has come to be known as a forearc basin.

15 Million - 14 Million Years Ago

Igneous Body
A large amount of magma from deep within the Earth rose up through the accretionary prism and forearc basin. The lava that made it to the surface, as well as the magma still underground cooled off and hardened to create an igneous body, or a pluton.
Joshua 2022/10/14(Fri) 13:39 No.342
Re: ƒWƒIƒp[ƒNƒZƒ“ƒ^[@“ü‚èŒûƒpƒlƒ‹
yfcrlbih 2024/09/19(Thu) 03:19 Home No.425
ã•x“c’¬Eƒ}ƒbƒv‚S‚SFW5@‹~”nŒk

–´˜K•t‰Á‘Ì‚ÆA‚»‚ê‚𕢂¤‘OŒÊŠC–~‚É‘ÍÏ‚µ‚½“c•Ó‘wŒQ‚Ì•s®‡‚ªŠÏŽ@‚Å‚«‚Ü‚·B•s®‡’¼ã‚ÌŒú‚¢»ŠââIŠâ‘wiŠî’êâIŠâ‘wj‚Í•—‰»‚âNH‚É‹­‚­A‹~”nŒk‚Ì’fŠR‚ðŒ`¬‚µA‚»‚Ìã‚É‹~”nŒkŠÏ‰¹‚ªŒš‚Ä‚ç‚ê‚Ä‚¢‚Ü‚·B‹~”nŒk‚É‚ÍA–ðsŽÒ‚ªŠJ‚¢‚½‚Æ‚³‚ê‚éCsꂪ‚ ‚èA¬ŒI”»Š¯‚Ì“`à‚àŽc‚³‚ê‚Ä‚¢‚Ü‚·B

Inconsistencies can be observed between the Muro accretionary prism and the Tanabe Group deposited in the forearc basin that covers it. The thick sandstone gravel layer (basic gravel layer) directly above the inconsistency is resistant to weathering and erosion, forming the cliffs of Sukumadani, and Sukumadani Kannon is built on it. In Sukumadani, there is a training ground that is said to have been opened by the officials, and the legend of Judge Oguri remains.

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‚¤‚¦‚à‚è@‚¤ 2022/01/19(Wed) 21:24 No.106
Re: ã•x“c’¬Eƒ}ƒbƒv‚S‚SFW5@‹~”nŒk
kcblmzmop 2024/09/18(Wed) 21:08 Home No.424
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MariyaUncell3037 2024/09/15(Sun) 19:27 Home No.423
XEvil 5: ReCaptcha‚ÆhCaptcha‰ðŒˆ‚Ì‚½‚ß‚Ìŗǂ̃vƒƒOƒ‰ƒ€‚ª—˜—p‰Â”\‚Å‚· !!!

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MariyaUncell2614 2024/09/15(Sun) 10:24 Home No.422
ƒoƒCƒpƒXReCaptcha captcha‚Ì‚½‚߂̃vƒƒOƒ‰ƒ€

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ŒxF–³—¿‚ÌXEvilƒfƒ‚‚ÍReCaptchaAhCaptcha‚Æcaptcha‚Ì‘¼‚̂قƂñ‚ǂ̃^ƒCƒv‚ðƒTƒ|[ƒg‚µ‚Ä‚¢‚Ü‚¹‚ñI

http://XEvil.Net/

MariyaUncell8968 2024/09/15(Sun) 02:18 Home No.421
‚Ù‚Æ‚ñ‚Ç‚Ìcaptcha‚ðŽE‚·‚½‚߂̃vƒƒOƒ‰ƒ€

XEvil6.0‚ÍA‚Ù‚Æ‚ñ‚ǂ̎í—Þ‚Ìcaptcha‚ðŽ©“®“I‚É‰ðŒˆ‚µ‚Ü‚·,
‚»‚̂悤‚ȃ^ƒCƒv‚Ìcaptcha‚ðŠÜ‚Þ: ReCaptcha-2, ReCaptcha-3, Hotmail (Microsoft), Google captcha, Solve Media, BitcoinFaucet, Steam, Amazon, Twitter, Microsoft, Twitch, Outlook, +12000
+ hCaptcha, ArkoseLabs FunCaptcha, ReCaptcha Enterprize V‚µ‚¢XEvil6.0‚ŃTƒ|[ƒg‚³‚ê‚Ä‚¢‚Ü‚·I

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- Google‚ÅŒŸõ‚µ‚Ă݂é "Home of XEvil"
- XEvilƒ†[ƒU[‚̃|[ƒg80‚ªŠJ‚¢‚Ä‚¢‚éIp‚ðŒ©‚Â‚¯‚邱‚Æ‚ª‚Å‚«‚Ü‚·iŠmŽÀ‚É‚·‚邽‚߂ɔCˆÓ‚ÌIP‚ðƒNƒŠƒbƒN‚µ‚Ä‚­‚¾‚³‚¢j
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- ‚¨Šy‚µ‚Ý‚­‚¾‚³‚¢I :)
- i‚»‚ÌhCaptcha‚Ì‚½‚߂̎dŽ–‚ł͂ ‚è‚Ü‚¹‚ñI)

ŒxF–³—¿‚ÌXEvilƒfƒ‚‚ÍReCaptchaAhCaptcha‚Æcaptcha‚Ì‘¼‚̂قƂñ‚ǂ̃^ƒCƒv‚ðƒTƒ|[ƒg‚µ‚Ä‚¢‚Ü‚¹‚ñI

http://XEvil.Net/

MariyaUncell0849 2024/09/14(Sat) 20:30 Home No.420
Ai Trading Bot For Beginners

<a href="https://bestcryptotradingbots.com/trade-eurex.php">How Does Futures Trading Work Crypto</a>

EddBfOblids 2024/09/10(Tue) 17:29 No.418
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