词条 | Tunguska event |
释义 | Tunguska event astronomy and geology ![]() The remote site of the explosion was first investigated from 1927 to 1930 in expeditions led by Russian scientist Leonid Alekseyevich Kulik. Around the epicentre (the location on the ground directly below the explosion) Kulik found felled, splintered trees lying radially for some 15–30 km (10–20 miles); everything had been devastated and scorched, and very little was growing two decades after the event. The epicentre was easy to pinpoint because the felled trees all pointed away from it; at that spot investigators observed a marshy bog but no crater. Eyewitnesses who had observed the event from a distance spoke of a fireball lighting the horizon, followed by trembling ground and hot winds strong enough to throw people down and shake buildings as in an earthquake. (At the time, seismographs in western Europe recorded seismic waves from the blast.) The blast had been initially visible from about 800 km away, and, because the object vaporized, gases were dispersed into the atmosphere, thus causing the abnormally bright nighttime skies in Siberia and Europe for some time after the event. Additional on-site investigations were performed by Soviet scientists in 1958 through 1961 and by an Italian-Russian expedition in 1999. |
随便看 |
百科全书收录100133条中英文百科知识,基本涵盖了大多数领域的百科知识,是一部内容开放、自由的电子版百科全书。