Cape Verde Rise
prominence on the Atlantic Ocean surface

The Cape Verde Rise is an oceanic feature that includes the Cape Verde Islands and the areas north and east of the islands and west of the African Continental Shelf as well as Mauritania and Senegal.
Geography
The rise are bounded by the Canary Basin to the north and the Cape Verde Basin to the south. Numerous seamounts are located in the rise including the Cape Verde (or Cabo Verde) (Latin: sometimes as Extracapitis being off the cape), Cadamosto, Boa Vista, Nola and Senghor. The third and fourth are named after explorers of Cape Verde, the other, the founding father of Senegal. The highest point is 2,220 meters below sea level and the deepest is in the range of over 3,000 meters deep. In the east end of the rise is the Dakar Canyon. It ranges between the 14 and the 22° parallels north and is 900 km long. Near the rise is the westernmost point in Africa, Cap-Vert, northwest of the rise is the Santo Antão Ridge.
In the waters above the Cape Verde Rise is the Canary (or Canarian) Current to the north and the Equatorial Atlantic Current around the south of the rise.
Nola Seamount may be the tallest seamount within Cape Verde with its elevation ranging from 60–70 meters deep, and probably the Cape Verde Rise.
Begin with the source’s own compact description: “Cape Verde Rise” is prominence on the Atlantic Ocean surface. The dossier treats that line as a proposition to test through Cape, Verde and Rise, not as a finished interpretation.
Why this record matters
The phrase “prominence on the Atlantic Ocean surface” 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.
Place names and jurisdictional language are key evidence: both can reveal earlier catalogue descriptions and overlooked record series. The source revision retrieved here is dated Nov 28, 2024. The linked authority identifier is Q1728835. None of the 0 selected statements returned an explicit reference.
A single description cannot reconcile every naming convention, rebuilding phase or administrative transfer associated with a place. 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
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 “Cape Verde Rise”, its source revision and the description used here.
- Expand the search: follow Cape Verde Rise primary sources, Cape Verde Rise archive and Cape 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 “Cape Verde Rise”?
- What physical evidence or contemporary plan supports the description?
- Which authority defined the place, boundary or structure at the relevant date?
Search terms from this dossier
This entry incorporates text from “Cape Verde Rise” 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.