In 1963In , 1964 geomagnetic variations in 3 components were measured at 14 sites in the Western Arctic Islands of the Canadian Archipelago. The suppression of Z amplitudes, first observed at Mould Bay, is now confirmed to extend from Mould Bay south to Holman Island, a distance of 620km, and from McCormick Inlet to Houghton Head, an east-west distance of 292km.
Spectral decomposition of many component time series gave mean Z/X energy density ratios which fall into two groups.