The measured physical properties of sediments recovered in a number of deep-sea drill holes in the North Atlantic have been used to derive expressions for the correction to basement depths required to account for loading by sediments. The average density and porosity over a given thickness of sediment show an approximate linear dependence on sediment thickness. This behavior can be explained as primarily the result of compaction. If the compaction of the sediments is neglected in correcting basement depths for sediment loading, errors of a few hundred meters in the corrected depths can be made. A sediment loading correction based on the observed variation of density with depth can give corrected depths to better than 100 m, with remaining uncertainties due to variablity in sediment properties and rebound effects on the measured densities. A relation between sediment thickness and vertical travel time was obtained from sonic velocity measurements on samples from drill holes, sonobuoy wide-angle reflection experiments, and direct correlation of seismic reflectors with downhole lithology. The sediment loading correction can then be expressed directly in terms of the vertical travel time measured along seismic reflection profiles. The loading correction obtained here for the North Atlantic may not be applicable in areas with different sedimentary enviroments. When direct measurements of physical properties in drill holes are not available in such areas, it is shown that it is preferable to assume a compaction curve for the appropriate lithology rather than to use observed seismic velocities together with a velocity-density relationship.