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  1. They concluded that the eruption unfolded in two phases, Vesuvian and Pelean, which alternated six times. [15] A first Plinian phase projected a column of volcanic debris and hot gases between 15 km (9 mi) and 30 km (19 mi) into the stratosphere.

  2. Historiography. The historical period of ancient Greece is unique in world history as the first period attested directly in comprehensive, narrative historiography, while earlier ancient history or protohistory is known from much more fragmentary documents such as annals, king lists, and pragmatic epigraphy.

  3. Historical earthquakes is a list of significant earthquakes known to have occurred prior to the early 20th century. As the events listed here occurred before routine instrumental recordings — later followed by seismotomography imaging technique, [1] observations using space satellites from outer space, [2] use of artificial intelligence (AI ...

  4. en.wikipedia.org › wiki › GreeceGreece - Wikipedia

    Greece features a vast number of islands —between 1,200 and 6,000, depending on the definition, [ 152 ] 227 of which are inhabited. Crete is the largest and most populous island; Euboea, separated from the mainland by the 60 m-wide Euripus Strait, is the second largest, followed by Lesbos and Rhodes.

  5. en.wikipedia.org › wiki › EarthquakeEarthquake - Wikipedia

    An earthquake is the shaking of the surface of Earth resulting from a sudden release of energy in the lithosphere that creates seismic waves. Earthquakes may also be referred to as quakes, tremors, or temblors. The word tremor is also used for non-earthquake seismic rumbling.

  6. Primitive Acropolis with the Pelargicon and the Old Temple of Athena. Elevation view of a proposed reconstruction of the Old Temple of Athena. Built around 525 BC, it stood between the Parthenon and the Erechtheum. Fragments of the sculptures in its pediments are in the Acropolis Museum.

  7. The earthquake occurred along the Chelungpu Fault in the western part of the island of Taiwan. The fault stretches along the foothills of the Central Mountains in Nantou County and Taichung County (now part of Taichung City). Some sections of land near the fault were raised as much as 7 m (23 ft).

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