Ja. Hanson et al., EARTHQUAKE ACTIVITY NEAR ASCENSION ISLAND, SOUTH-ATLANTIC OCEAN, AS SEEN BY A COMBINED SEISMIC HYDROPHONE ARRAY/, Geothermics, 25(4-5), 1996, pp. 507
Earthquake activity in the vicinity of Ascension Island is studied usi
ng data from a recently installed, very broadband seismographic statio
n and a network of ocean hydrophones deployed around the island. The s
eismic station ASCN recorded 121 local earthquakes over a 188-day peri
od. Distance from ASCN is computed for 41 of these events, most of whi
ch occurred at approximately 100 km-the distance to the Mid-Atlantic R
idge. A local magnitude scale is calibrated and applied to the same 41
events with magnitudes ranging from 0.4 to 4.2. Six earthquakes were
located using data from the hydrophones and ASCN. Two of the earthquak
es occur on the Ascension Fracture Zone 35 km northwest of the island
and the other four near the ridge-transform intersection. The location
s have errors less than 10 km and frequently less than 3 km. There is
no direct evidence for seismicity connected with geothermal activity o
n Ascension Island during the observation period. Copyright (C) 1996 C
NR. Published by Elsevier Science Ltd.