Transient variations in the earth's magnetic field may be expected to induce electric current concentrations along the ocean‐land boundary. Depending upon the direction of the inducing field, magnetic effects in the vertical and horizontal component normal to the coast are predicted. The electric component will tend to be polarized perpendicular to the shore on land and parallel offshore. This paper presents the results of magnetic and telluric current measurements on both sides of the coast near Barrow, Alaska. Owing to the gradually shelving water depth, and the low (10 Ω m) resistivity of the land, no magnetic coast effect of greater than a few per cent was found. There is a polarization at nearly all sites in E nearly perpendicular to the coast including a site 3 km offshore. The frequency response of telluric current variations is relatively low to disturbances of the order of 10‐second period.