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EARTHQUAKEs IN POLAN D. An earthquake – a sudden release of energy strains stored in the Earth's crust. About 20-30% released energy creates seismic waves that reach the surface of the Earth. epicenter picenter. Seismic waves waves. hypocenter hypocenter.
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An earthquake – a sudden release of energy strains stored in the Earth's crust. About 20-30% released energy creates seismic waves that reach the surface of the Earth.
epicenterpicenter Seismic waveswaves hypocenterhypocenter
An earthquake's point of initial reputure is located in the depth of the earth and is called its focus or hypocenter. The epicenter is the point at ground level directly above the hypocenter.
EARTHQUAKES IN POLAND Zbigniew Zwoliński Instytut Paleogeografii i Geoekologii, Uniwersytet im. Adama Mickiewicza, Poznań Earthquakes rarely happen in Poland. The most frequently places that earthquakes appear: • coal mines • mountain caves (Sudety Mountains, Krakowsko-Częstochowska Upland) Large earthquakes in the area of Poland occured about 150-200 mln years ago.
The last earthquake took place in 2001 in Bełchatów. It was of magnitude 4,7 on Richter scale. This earthquake didn't cause any serious damage, furniture and floors were shaking, walls cracked in several buildings. Silesia is the place in Poland where earthquakes occur most frequently and some of them are almost magnitude 4.
In Poland there are two main areas where the earthquakes occur: • Góry Kaczawskie, Przedgórze Sudeckie, Nizina Śląska, • Wał Trzebnicki i Nizina Wielkopolska wzdłuż linii Jelenia Góra-Leszno - Kotlina Oświęcimska, Wyżyna Śląska i Wyżyna Krakowsko-Częstochowska wzdłuż linii Oświęcim-Herb
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