Goldthwait Sea
prehistoric sea on the coast of eastern Canada

The Goldthwait Sea was a sea that emerged during the last deglaciation, starting around 13,000 years ago, covering what is now the Gulf of Saint Lawrence and surrounding areas.
At that time, the land had been depressed under the weight of the Laurentide Ice Sheet, which was up to 2 kilometres (1.2 mi) thick.
Areas on the Anticosti Island and low-lying regions of Quebec and the Maritimes bordering the Saint Lawrence were below sea level.
As the land rebounded over the next 3,000 years, despite rising sea levels the sea retreated to roughly the present boundaries of the Gulf.
Name
The term "Goldthwait Sea" was proposed by Elson in 1969 to distinguish the area from the Champlain Sea and the Laflamme Sea.
The sea is named after the geologist James Walter Goldthwait (1880–1947).
He did impressive work for the Geological Survey of Canada in the east of the country, and in Quebec in particular, despite handicaps such as lack of aerial photographs or detailed topographical maps.
The quality of his observations and his insights were remarkable.
Overall process
Formation of the Goldthwait Sea was part of a broader process in what is now eastern Canada towards the end of the Last Glacial Period.
The atmosphere was warmer near the oceans and towards the south, so melting of the Laurentide Ice Sheet progressed from east to west and from south to north.
The public source identifies “Goldthwait Sea” as prehistoric sea on the coast of eastern Canada. This brief keeps that definition visible, then builds a research path around Goldthwait, prehistoric and coast.
Why this record matters
A short description can identify a subject without explaining its stakes. For “Goldthwait Sea”, the useful work is to connect “prehistoric sea on the coast of eastern Canada” to the records capable of establishing context and consequence.
Maps, plans, fabric surveys and administrative records can establish how the site’s name, extent and function changed over time. The source revision retrieved here is dated Jul 25, 2026. The linked authority identifier is Q10461055. Authority coordinates are 48.000, -62.000. None of the 1 selected statements returned an explicit reference. The first chronological checks are 1969, 1880 and 1947.
A single description cannot reconcile every naming convention, rebuilding phase or administrative transfer associated with a place. 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
Treat names, boundaries and functions as historically changeable. Maps, plans, inventories and administrative records can clarify what the place meant at different dates.
- Historic place names
- Jurisdictional context
- Routes into maps and plans
Contemporary maps, plans, listed-building records, estate papers and the responsible local or national archive.
Three-step research path
- Establish the record: confirm the title “Goldthwait Sea”, its source revision and the description used here.
- Expand the search: follow Goldthwait Sea primary sources, Goldthwait Sea archive and Goldthwait research across catalogues and specialist indexes.
- Test the account: compare the strongest cited source with the responsible institution’s current record and note any disagreement.
Questions for further research
- Which source most directly establishes the central claim about “Goldthwait Sea”?
- What physical evidence or contemporary plan supports the description?
- Which earlier names or jurisdictions may reveal additional records?
Search terms from this dossier
This entry incorporates text from “Goldthwait Sea” 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.