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1590 Neulengbach earthquake
The Neulengbach earthquake of 1590 occurred on September 15, 1590 shortly before midnight amidst a long series of much weaker seismic activity starting on June 29, 1590 and with aftershocks reported until November 12. It was the strongest historically documented earthquake in what today is Northeastern Austria.
==Epicenter and seismology==
The epicenter is believed to have been located southeast of Neulengbach, about 30–40 km west of Vienna, in a flat dipping and North-South striking thrust fault〔Hammerl C. and Lenhardt WA. A review of the 1590 earthquake in Lower Austria and its effects on Vienna. Geophysical Research Abstracts 2009; Vol. 11, EGU2009-13727. EGU General Assembly 2009 (Online abstract ). Accessed 2009-05-27. (Archived ) 2009-05-29.〕 that is part of the Vienna Transform fault zone. This moderately active fault system extends over a distance of some 300 km from the Northern Limestone Alps through the Vienna Basin into the West Carpathian Mountains. The temblor's energy release is estimated at 5.5-6.0 on the Richter magnitude scale and it had class VII intensity on the modified Mercalli intensity scale in most of Lower Austria.
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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