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Kemp Peninsula

ice-covered peninsula in Antarctica

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General referenceInterpretive dossier study · Crown Archives visual atlas
Record originEnglish Wikipedia
Text licenseCC BY-SA 4.0
Source revisionJul 14, 2026
Entity authorityQ2680567
Source-derived summary

Kemp Peninsula (73°8′S 60°15′W) is an irregular ice-covered peninsula 26 nautical miles (48 km; 30 mi) long in a north–south direction and 5 to 12 nautical miles (9.3 to 22.2 km; 5.8 to 13.8 mi) wide.

The peninsula rises gently to 305 metres (1,001 ft) and projects east between the heads of Mason Inlet and Mossman Inlet, on the east coast of Palmer Land, Antarctica.

Location

The Kemp Peninsula is on the Lassiter Coast of southern Palmer Land, beside the Weddell Sea to the east.

Mason Inlet is to the north, fed by Clowes Glacier.

The coastal ice sheet extends north from Mason Inlet to Cape Herdman, at the south of the mouth of Violante Inlet.

The northern point of the peninsula is Cape Mackintosh.

The Wegener Range is to the east.

Cape Deacon is near the southern point.

Mossman Inlet is to the south, just north of New Bedford Inlet and east of Mount Pawson and Mohn Peaks on the mainland.

Discovery and name

Kemp Peninsula was first seen from the air in December 1940 by members of the United States Antarctic Service (USAS), who at that time photographed all but its northern extremity.

Editorial summary

The public source identifies “Kemp Peninsula” as ice-covered peninsula in Antarctica. This brief keeps that definition visible, then builds a research path around Kemp, Peninsula and ice-covered.

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—1940—that can be checked directly. The selected authority fields contribute no independent date. Its value is orientation rather than verdict, with Kemp, Peninsula and ice-covered providing the first useful test.
Editorial analysis

Why this record matters

A short description can identify a subject without explaining its stakes. For “Kemp Peninsula”, the useful work is to connect “ice-covered peninsula in Antarctica” 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 14, 2026. The linked authority identifier is Q2680567. Authority coordinates are -73.133, -60.250. 1 of 1 selected statements include explicit references; 0 carry qualifiers and 0 use preferred rank. The first chronological checks are 1940.

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.

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 Kemp Peninsula primary sources, Kemp Peninsula archive and Kemp 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 Kemp Peninsula” 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.