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1930 Senigallia earthquake
The 1930 Senigallia earthquake struck the city of Senigallia in central Italy on October 30. It occurred just a few months after the destructive 1930 Irpinia earthquake, which had caused over 1400 casualties in the southern part of the country.
==Geology==
The coastline in the area around Senigallia is controlled by active thrust faulting at the leading edge of the North Apennines fold and thrust belt. Movement on a blind thrust, the Senigallia Fault, has caused folding in the area around the port forming an anticline that extends about parallel to the coast. The rupture area for the 1930 earthquake is thought to have measured about along strike and down dip.
抄文引用元・出典: フリー百科事典『 ウィキペディア（Wikipedia）』
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