
 
This earthquake, which caused the deaths of seventeen
 people and injury to upwards of 135 others, besides doing damage to 
buildings to the extent of hundreds of thousands of pounds in Accra, the
 capital of the Gold Coast and the surrounding country (NATURE, 144, 18;
 1939), has recently been the subject of comprehensive research. The 
Gold Coast as a whole is a relatively stable region and earthquakes are 
rare, though the Accra district and the coastal area to the east and 
west are subject to earthquakes. Major shocks occurred in 1862, when 
every stone building in Accra was razed to the ground and Christiansborg
 Castle and the forts at Accra taken over by the British from the Danes 
twelve years before, were rendered uninhabitable; in 1906 when on 
November 20 Government buildings in Accra were damaged though no 
casualties were reported; and in the present instance. Recorded minor 
shocks occurred in 1636, 1858, 1863, 1883, 1907, 1911, 1918-19, 1923, 
1925, 1930 and 1933-35. There are no records of any minor precursor 
shocks to the 1939 earthquake since the operation of the seismograph at 
Accra had been discontinued a few years previously on the grounds of 
economy; but between 1932 and 1935 cracks began to appear in substantial
 Government buildings in Accra and in the ground near the buildings. At 
the time Dr. Junner directed attention to the possibility of earthquakes
 occurring within the next 10-15 years. The earthquake of June 22, 1939,
 occurred at approximately 7.20 p.m. (G.M.T.) and was felt for about 
20-30 seconds at Accra. There is no doubt that casualties were fewer 
than might have been expected from the severity of the shock since at 
the time many people were out of doors and there were no subsequent 
outbreaks of fire. The earthquake was felt by persons over an area of 
approximately 300,000 square miles and at places more than five hundred 
miles from Accra. As the epicentre was probably out to sea some 
twenty-five miles from Accra it is likely that it would have been felt 
over an area of 600,000 square niiles if the whole of the area had been 
populated land.
 
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