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Shu (crater)

crater on Ganymede

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General referenceInterpretive dossier study · Crown Archives visual atlas
Record originEnglish Wikipedia
Text licenseCC BY-SA 4.0
Source revisionJul 22, 2026
Entity authorityQ25908171 ↗
Source-derived summary

Shu is a prominent bright ray impact crater in the northern hemisphere of Ganymede, the largest moon of Jupiter. The crater is approximately 44 kilometres (27 mi) in diameter, and its bright ray system extends for several hundred kilometers in all directions.

Naming

Shu is named after the Ancient Egyptian god of the air and wind, Shu. He is the firstborn son of Ra, the sun god and king of the Egyptian gods. The Ancient Egyptians believed that, as the god of the air and wind, Shu separated the earth (the god Geb) from the sky (the goddess Nut), and he fills the space in between the two.

The crater's name follows the International Astronomical Union's (IAU) naming convention, under which craters and other surface features on Ganymede are named after deities, heroes, and places from Ancient Near Eastern mythology, including Ancient Egyptian mythology.

The name for Shu was approved by the IAU in 1988.

Location

Shu is located in the mid-latitudes of Ganymede's northern hemisphere. It lies almost exactly on the eastern boundary of the dark region Perrine Regio. Its bright ray system extends across much of the surrounding dark terrain, making the crater stand out prominently.

Editorial summary

The public source identifies “Shu (crater)” as crater on Ganymede. This brief keeps that definition visible, then builds a research path around crater and Ganymede.

Editorial reviewA dependable orientation record for establishing vocabulary, names and a first evidence trail. The current lead gives the account dated anchors—1988—that can be checked directly. The selected authority fields contribute no independent date. Its value is orientation rather than verdict, with crater and Ganymede providing the first useful test.
Editorial analysis

Why this record matters

A short description can identify a subject without explaining its stakes. For “Shu (crater)”, the useful work is to connect “crater on Ganymede” to the records capable of establishing context and consequence.

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 22, 2026. The linked authority identifier is Q25908171. Authority coordinates are 43.160, -356.840. 1 of 1 selected statements include explicit references; 0 carry qualifiers and 0 use preferred rank. The first chronological checks are 1988.

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 Shu (crater) primary sources, Shu (crater) archive and crater 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.

Questions for further research

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Source & attribution

This entry incorporates text from “Shu (crater)” 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.