The continental shelf area immediately north of Seward Peninsula, Alaska, is characterized by medium-to coarse-grained clastic sediments and dominated by stronger than normal offshore currents. The pattern of current velocities is compared with the bathymetry, the distribution of sediment size and sorting characteristics, and the proximity of source areas.

This content is PDF only. Please click on the PDF icon to access.

First Page Preview

First page PDF preview
You do not currently have access to this article.