Shaping of the Continental Rise by Deep Geostrophic Contour Currents

Bruce C. Heezen, Charles D. Hollister, William F Ruddiman

Science · 1966 · 518 citations · 18 references

Concepts

Abstract

Geostrophic contour-following bottom currents involved in the deep thermohaline circulation of the world ocean appear to be the principal agents which control the shape of the continental rise and other sediment bodies.

References

18