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"extract": "Seismic magnitude scales are used to describe the overall strength or \"size\" of an earthquake. These are distinguished from seismic intensity scales that categorize the intensity or severity of ground shaking (quaking) caused by an earthquake at a given location. Magnitudes are usually determined from measurements of an earthquake\u0027s seismic waves as recorded on a seismogram. Magnitude scales vary based on what aspect of the seismic waves are measured and how they are measured. Different magnitude scales are necessary because of differences in earthquakes, the information available, and the purposes for which the magnitudes are used.",
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"extract": "Seismic magnitude scales are used to describe the overall strength or \"size\" of an earthquake. These are distinguished from seismic intensity scales that categorize the intensity or severity of ground shaking (quaking) caused by an earthquake at a given location. Magnitudes are usually determined from measurements of an earthquake\u0027s seismic waves as recorded on a seismogram. Magnitude scales vary based on what aspect of the seismic waves are measured and how they are measured. Different magnitude scales are necessary because of differences in earthquakes, the information available, and the purposes for which the magnitudes are used.",
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"extract": "The 2009 Dusky Sound earthquake was a Mw 7.8 earthquake that struck a remote region of Fiordland, New Zealand, on 15 July at 21:22 local time. It had an initially\u2013reported depth of 12\u00a0km (7.5\u00a0mi), and an epicentre near Dusky Sound in Fiordland National Park, which is 160\u00a0km (99\u00a0mi) north-west of Invercargill. It was the country\u0027s largest earthquake magnitude since the 1931 Hawke\u0027s Bay earthquake, but caused only minor damage and there were no casualties. A tsunami accompanied the event and had a maximum measured run-up of 230\u00a0cm (91\u00a0in).",
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"extract": "Fiordland is a non-administrative geographical region of New Zealand in the south-western corner of the South Island, comprising the western third of Southland. Most of Fiordland is dominated by the steep sides of the snow-capped Southern Alps, deep lakes, and its steep, glacier-carved and now ocean-flooded western valleys. The name \"Fiordland\" derives from the New Zealand English spelling of the Scandinavian word for steep glacial valleys, \"fjord\". The geographic area of Fiordland is dominated by, and roughly coterminous with, Fiordland National Park, New Zealand\u0027s largest national park.",
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"text": "A .mw-parser-output .tooltip-dotted{border-bottom:1px dotted;cursor:help}Mw 7.8 earthquake struck a remote region of Fiordland, New Zealand, the country\u0027s largest earthquake magnitude since the 1931 Hawke\u0027s Bay earthquake.",
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