. Collected reprints / Atlantic Oceanographic and Meteorological Laboratories [and] Pacific Oceanographic Laboratories. Oceanography 284. 32 Fig. 1. Morphological fit of eastern North America and northwestern Africa at 2000-m isobath (from Dietz and Sproll, 1970, fig. 1). western Africa is largely unknown. The continental crust thins seaward from a thickness of about 30 km beneath the coastal plain to about 10 km beneath the continental slope off Cape Hatteras (Fig. 2; Worzel and Shurbet, 1955). The transition from oceanic to continental crust occurs in a distance of about 100-20
. Collected reprints / Atlantic Oceanographic and Meteorological Laboratories [and] Pacific Oceanographic Laboratories. Oceanography 284. 32 Fig. 1. Morphological fit of eastern North America and northwestern Africa at 2000-m isobath (from Dietz and Sproll, 1970, fig. 1). western Africa is largely unknown. The continental crust thins seaward from a thickness of about 30 km beneath the coastal plain to about 10 km beneath the continental slope off Cape Hatteras (Fig. 2; Worzel and Shurbet, 1955). The transition from oceanic to continental crust occurs in a distance of about 100-200 km centered beneath the 2000-m isobath (Worzel, 1968, 1057. Please note that these images are extracted from scanned page images that may have been digitally enhanced for readability - coloration and appearance of these illustrations may not perfectly resemble the original Atlantic Oceanographic and Meteorological Laboratories; Pacific Oceanographic Laboratories; United States. Environmental Science Services Administration. Research Laboratories; Environmental Research Laboratories (U. S. ). Washington, D. C. : U. S. Dept. of Commerce, Environmental Science Services Administration, Research Laboratories : For sale by Supt. of Docs. U. S. G. P. O.
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