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1038 Dingxiang earthquake

earthquake in China

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General referenceInterpretive dossier study · Crown Archives visual atlas
Record originEnglish Wikipedia
Text licenseCC BY-SA 4.0
Source revisionJul 26, 2026
Entity authorityQ124381819 ↗
Source-derived summary

The 1038 Dingxiang earthquake devastated present-day Shanxi Province, northern China on 9 January. At least 32,300 people died across the province when the Ms 7.25 earthquake struck Dingxiang and Xinxian counties. In Xinzhou, about 19,742 people died and 5,655 were injured. More than 50,000 livestock also perished. About 759 were killed in Guoxian County and in present-day Taiyuan, 1,890 people died.

Geology

The Xizhoushan Fault Zone, a strike-slip fault system within the Shanxi Rift System, may have been responsible for the earthquake. Field studies indicate at least three earthquakes occurred along the fault during the Holocene with the most recent event possibly being the 1038 earthquake. This fault delineates the Xizhoushan Mountains and Xinding basin within the rift system. Estimates of the right-lateral slip rate range from 5.86–5.22 mm (0.231–0.206 in) per year to as low as 2 mm (0.079 in) per year during the Holocene. At least 60 km (37 mi) of surface rupture along the fault was associated with the earthquake.

Editorial summary

Begin with the source’s own compact description: “1038 Dingxiang earthquake” is earthquake in China. The dossier treats that line as a proposition to test through Dingxiang, earthquake and China, not as a finished interpretation.

Editorial reviewA practical starting point whose main value is the path it opens into stronger specialist and primary sources. The current lead gives the account dated anchors—1038—that can be checked directly. The selected authority fields contribute no independent date. For this dossier, Dingxiang, earthquake and China is the immediate research focus.
Editorial analysis

Why this record matters

The phrase “earthquake in China” supplies a clear boundary for inquiry. It also exposes the unanswered questions: who defined that boundary, when it became stable and which sources sit outside it.

Evidence profile

The citation trail is more important than the brevity of the summary: it shows where individual claims can be examined in context. The source revision retrieved here is dated Jul 26, 2026. The linked authority identifier is Q124381819. Authority coordinates are 38.400, 112.920. None of the 1 selected statements returned an explicit reference. The first chronological checks are 1038.

Critical limits

Overview language is designed for orientation and should not be treated as a substitute for the evidence cited beneath it. 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 1038 Dingxiang earthquake primary sources, 1038 Dingxiang earthquake archive and Dingxiang 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 “1038 Dingxiang earthquake” 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.