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Context
Recent geological studies using advanced 3-D seismic data analysis have confirmed that the Silverpit Crater in the North Sea was formed due to the impact of a large asteroid approximately 43–46 million years ago during the Middle Eocene epoch. The confirmation comes from new scientific evidence such as the presence of shocked quartz, which forms only under extreme pressure caused by meteorite impacts.
Location and Discovery
The Silverpit Crater lies beneath the North Sea, about 130 km east of the Yorkshire coast of the United Kingdom. It is buried 500–1000 meters below the seabed within sedimentary rock layers. The structure was discovered in 2002 by petroleum geologists Simon Stewart and Philip Allen while analysing 3-D seismic survey data during oil and gas exploration activities. Initially, scientists debated whether the formation resulted from meteorite impact or from geological processes such as salt dome collapse.
Formation and Structural Characteristics
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Silverpit Crater in the North Sea was formed by asteroid impact 43-46 million years ago. Recent 3-D seismic analysis and shocked quartz evidence confirm its extraterrestrial origin.
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