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1968 Belice earthquake

Successive earthquakes occurred in Sicily between January 14 and 15, 1968.

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Record originEnglish Wikipedia
Text licenseCC BY-SA 4.0
Source revisionJul 26, 2026
Entity authorityQ1062315 ↗
Source-derived summary

The 1968 Belice earthquake (Italian: terremoto del Belice) sequence took place in Sicily between 14 and 15 January. The largest shock measured 6.4 on the moment magnitude scale, with five others of magnitude 5+. The maximum perceived intensity was X (Extreme) on the Mercalli intensity scale. The earthquake sequence, centred between the towns of Gibellina, Salaparuta and Poggioreale in the area of river Belice, killed at least 231 people, possibly more than 400, with between 632 and about 1,000 injured and left 100,000 homeless.

Tectonic setting

Sicily lies on the complex convergent plate boundary between the African plate and the Eurasian plate. The geology of the western part of the island is dominated by the Gela Nappe, a thin-skinned fold and thrust belt. The Gela Nappe consists of Pliocene-Quaternary age sedimentary rocks deposited in the earlier foredeep, thrust up onto the thick carbonate sequence of the Pelagian-Hyblean Platform of the African plate.

Earthquake

There was a sequence of six M 5+ earthquakes, making this western Sicily's largest historical seismic event, beginning with a M 5.2 shock at 12:28 on the 14 January, followed by a M 5.1 event at 13:15 on the same day and a M 5.2 event at 01:33 on 15 January, the mainshock at 02:01, and two M 5.2 events at 16:42 on 16 January and at 09:56 on 25 January.

The greatest perceived intensity on the Mercalli scale was X (Extreme) at Gibellina, Montevago and Salaparuta. Intensities at Poggioreale, Trapani|Poggioreale, Santa Margherita di Belice, Santa Ninfa, Partanna and Salemi reached IX (Violent) on the scale.

Editorial summary

Begin with the source’s own compact description: “1968 Belice earthquake” is successive earthquakes occurred in Sicily between January 14 and 15, 1968. The dossier treats that line as a proposition to test through Belice, earthquake and Successive, not as a finished interpretation.

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—1968—that can be checked directly. The selected authority fields contribute no independent date. For this dossier, Belice, earthquake and Successive is the immediate research focus.
Editorial analysis

Why this record matters

The phrase “successive earthquakes occurred in Sicily between January 14 and 15, 1968” 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

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 Q1062315. Authority coordinates are 37.919, 12.998. 1 of 1 selected statements include explicit references; 0 carry qualifiers and 0 use preferred rank. The first chronological checks are 1968.

Critical limits

A concise general-reference account can conceal disagreements about scope, terminology or the weight assigned to individual sources. The lead is largely declarative, so disagreement and counter-evidence require a deliberate search beyond the opening account. Authority statements aid reconciliation but still require their own references, qualifiers and ranks to be checked.

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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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Source & attribution

This entry incorporates text from “1968 Belice 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.