An unsually large ULVZ at the base of the mantle near Hawaii
Abstract Previous studies have documented the presence of ultra low velocity zones (ULVZs) at the base of the mantle, through observations of body wave complexities. Geometrically their heights are in the range of 5 30 km while little is known about their lateral extent beyond about 102 km, due to limitations in sampling. Here we show remarkable features in the waveforms of S/Sdiff phases of western Pacific events observed at stations in North America that indicate the presence of a very large ultra low velocity zone (ULVZ) at the base of the mantle, centered 11 deg to the southwest of Hawaii, within and near the northern border of the Pacific LLSVP. Waveform complexities include strongly delayed 30 s postcursors. Measurements of travel times, beamforming analysis of out of plane energy, and full waveform comparisons with 3D numerical simulations, constrain the location, lateral extent, height and velocity reduction of the ULVZ with some level of trade off. The simplified 3D model consists of a cylindrical ULVZ with a large aspect ratio of 20 km in height and 910 km in diameter at the CMB. The shear wave velocity reduction is 20 This is to our knowledge the largest ULVZ mapped to date and the first time the lateral extent of a ULVZ has been constrained with some precision. Its location suggests that it may be the root of a long lived, stable plume responsible for the Hawaiian volcanic chain, the hotspot track with the largest buoyancy flux.