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1026 Manju tsunami

Tsunami affecting Japan

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Record originEnglish Wikipedia
Text licenseCC BY-SA 4.0
Source revisionJul 26, 2026
Entity authorityQ11353814 ↗
Source-derived summary

The 1026 Manju tsunami affected the Sea of Japan coast of the then Iwami Province on June 16. Considered one of the largest tsunamis in the Sea of Japan, it generated a tsunami with waves of 10 m (33 ft) at present-day Masuda, Shimane. Off the coast, an island reportedly sank because of the waves. More than 1,000 people were killed, and 3,000 homes were destroyed. The source of the tsunami has been debated between an earthquake or undersea landslide.

Description

In historical records, locals claimed that a large stone called Kuroiwa was carried by the tsunami to its present location in Tonda, along Japan National Route 9 about 3.5 km (2.2 mi) from Masuda Station. The 5 m (16 ft) tall stone was allegedly carried 2 km (1.2 mi) from the coast at an elevation of 25 m (82 ft). A subsequent investigation revealed the stone, comprising basalt, originated from the inland mountains, as basalts do not occur at the coast, and was transported downhill by a landslide rather than the reported tsunami.

The tsunami reportedly sank the islands of Kamo, Nabeshima, and Kashiwajima, which were then busy settlements. Oral records suggest these features were solid outcrops rather than sandbars.

Editorial summary

This brief starts where responsible research should: with the source description of “1026 Manju tsunami” as tsunami affecting Japan. Everything that follows is an evidence route, not borrowed authority.

Editorial reviewA concise reference frame for defining the subject, testing terminology and identifying the institution closest to the evidence. The current lead gives the account dated anchors—1026—that can be checked directly. The selected authority fields contribute no independent date. The account is most persuasive where Manju, tsunami and Tsunami can be independently traced.
Editorial analysis

Why this record matters

The subject matters to the general reference register because the source frames it as tsunami affecting Japan. Its deeper value depends on whether names, dates, institutions and citations support that framing.

Evidence profile

Vocabulary and entity names are the principal evidence signals here, because they determine the precision of every later search. The source revision retrieved here is dated Jul 26, 2026. The linked authority identifier is Q11353814. Authority coordinates are 34.800, 131.800. None of the 1 selected statements returned an explicit reference. The first chronological checks are 1026.

Critical limits

The absence of detail may reflect summary conventions rather than a lack of surviving documentation. The source lead contains qualifying language; that uncertainty should survive quotation, summary and reuse. Authority statements aid reconciliation but still require their own references, qualifiers and ranks to be checked.

How to read it

Use the entry as an orientation point, then follow its citations and revision history. Names, dates and institutional relationships should be checked against the original record.

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  2. Expand the search: follow 1026 Manju tsunami primary sources, 1026 Manju tsunami archive and Manju research across catalogues and specialist indexes.
  3. Test the account: compare the strongest cited source with the responsible institution’s current record and note any disagreement.

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Source & attribution

This entry incorporates text from “1026 Manju tsunami” on English Wikipedia. Contributors are listed in the page history. Text is available under the Creative Commons Attribution-ShareAlike 4.0 License. Selected authority identifiers and statements are retrieved from Wikidata under CC0; their references and qualifiers remain part of the verification path.