Tsunamis
Introduction
A tsunami (“a wave in port” in Japanese) are the marine gravity waves that are extremely large in length and height, and are the result of the up or down shift of ocean bottom areas with strong underwater and coastal earthquakes, occasionally, though, are the result of volcanic eruptions and other tectonic processes. Tsunamis are among those few natural disasters that are capable of causing huge numbers. First chapter of this research is dedicated to the causes of tsunami, wave formation mechanism, and waves’ various characteristics. The topic of the conducted research is highly relevant to our area if ...