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Wentworth Valley

human settlement in Nova Scotia, Canada

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General referenceInterpretive dossier study · Crown Archives visual atlas
Record originEnglish Wikipedia
Text licenseCC BY-SA 4.0
Source revisionAug 31, 2026
Entity authorityQ7983039 ↗
Source-derived summary

The Wentworth Valley is a valley in the Cobequid Mountains of northwestern Nova Scotia, Canada. It comprises the lowest elevation pass through the Cobequids. It was named after the colonial governor John Wentworth (1792-1808).

Physical geography

The valley is oriented north–south and is located in a glacial trough named the "Folly Gap" (originally spelled "Folleigh"). The section framed by mountains measures approximately 8 km (5.0 mi) in length, from Folly Lake in the south to Wentworth Provincial Park in the north with the width of the valley floor varying from 0.5 km (0.31 mi) in the south to 1.5 km (0.93 mi) in the north.

The west wall of the valley is formed by Higgins Mountain (360 m (1,180 ft) elevation) and the east wall is formed by several unnamed peaks (290 m (950 ft)-330 m (1,080 ft) elevation). The south end and highest point of the trough is Folly Lake (190 m (620 ft) elevation) which drains south to the Bay of Fundy through the Folly River, therefore its waters do not enter the valley.

The Wallace River flows north through the valley to the Northumberland Strait from its source in Dicks Meadows on Higgins Mountain.

The trough descends abruptly north of Folly Lake where over a distance of approximately 2 km (1.2 mi) the valley floor levels out at approximately 120 m (390 ft) elevation. From there, the valley floor and the serpentine Wallace River gradually descends over the next 14 km (8.7 mi) to approximately 30 m (98 ft) elevation at the junction with the West Branch Wallace River.

Editorial summary

Begin with the source’s own compact description: “Wentworth Valley” is human settlement in Nova Scotia, Canada. The dossier treats that line as a proposition to test through Wentworth, Valley and human, not as a finished interpretation.

Editorial reviewA dependable orientation record for establishing vocabulary, names and a first evidence trail. The current lead gives the account dated anchors—1792, 1808—that can be checked directly. The selected authority fields contribute no independent date. For this dossier, Wentworth, Valley and human is the immediate research focus.
Editorial analysis

Why this record matters

The phrase “human settlement in Nova Scotia, Canada” 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 Aug 31, 2026. The linked authority identifier is Q7983039. Authority coordinates are 45.599, -63.562. 1 of 1 selected statements include explicit references; 0 carry qualifiers and 0 use preferred rank. The first chronological checks are 1792 and 1808.

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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Source & attribution

This entry incorporates text from “Wentworth Valley” 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.