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Heezen, Tharp and Ewing: mapping North Atlantic seafloor structure

The1959 report explains how echo-sounding profiles were organized into a North Atlantic physiographic diagram and provinces, with detailed ridge and axial-valley descriptions.

What is recorded here?

The1959 report explains how echo-sounding profiles were organized into a North Atlantic physiographic diagram and provinces, with detailed ridge and axial-valley descriptions. Scattered ship tracks became an interpretable view of a largely inaccessible landscape. The authors distinguish recorded profiles from inferred relief between tracks, state the map's resolution and identify both striking morphology and unresolved geological interpretation.

Source-linked catalogue note. A detailed explanatory guide has not yet been prepared for this entry.

Scientific scope

The target is the selected physical mapping/morphology contribution in the 1959 report, whose first sheet covers 17–50 degrees north; it is not a complete world-ocean map or every earlier chart. Between-track relief is interpolated/extrapolated and explicitly speculative.40:1 exaggerated profiles and small map scale limit what features are represented; positional/data-quality limits remain. Plate 1 and the figures were not visually audited, and no raw sounding reconstruction was run. Ridge origin remains unresolved in the inspected text; this is not a complete plate-tectonics proof. The three source bylines do not absorb the named expedition, navigation, plotting and recorder-development teams, nor later maps or theories. No life-science observations are curated by this target.

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People and systems

Bruce C. Heezen; Marie Tharp; Maurice Ewing

Source-listed contributors to this scoped work. Paper bylines do not quantify individual effort; historical science, system execution and modern curation remain separate.

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English catalogue narrative

Heezen, Tharp and Ewing: mapping North Atlantic seafloor structure

The1959 report explains how echo-sounding profiles were organized into a North Atlantic physiographic diagram and provinces, with detailed ridge and axial-valley descriptions.

Scattered ship tracks became an interpretable view of a largely inaccessible landscape. The authors distinguish recorded profiles from inferred relief between tracks, state the map's resolution and identify both striking morphology and unresolved geological interpretation.

Scientific scope

The target is the selected physical mapping/morphology contribution in the 1959 report, whose first sheet covers 17–50 degrees north; it is not a complete world-ocean map or every earlier chart. Between-track relief is interpolated/extrapolated and explicitly speculative.40:1 exaggerated profiles and small map scale limit what features are represented; positional/data-quality limits remain. Plate 1 and the figures were not visually audited, and no raw sounding reconstruction was run. Ridge origin remains unresolved in the inspected text; this is not a complete plate-tectonics proof. The three source bylines do not absorb the named expedition, navigation, plotting and recorder-development teams, nor later maps or theories. No life-science observations are curated by this target.

People and systems

Bruce C. Heezen; Marie Tharp; Maurice Ewing

Original sources