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What causes earthquakes? Earthquakes occur when the plates that make up the Earth's crust move around. These plates, called tectonic plates, can push against each other.
A 3.8-magnitude earthquake struck Monday morning near Buffalo, New York, the strongest recorded in the area in 40 years.
A damaging earthquake affecting New York City in 1884 was incorrectly argued to be caused by the Ramapo fault, likely because it is the most prominent mapped fault in the greater New York City area. At the present, the relationship between faults and earthquakes in the New York City area is understood to be more complex than any simple ...
This is a list of accidents and disasters by death toll.It shows the number of fatalities associated with various explosions, structural fires, flood disasters, coal mine disasters, and other notable accidents caused by negligence connected to improper architecture, planning, construction, design, and more.
The Angola Horror [note 1] train wreck occurred on December 18, 1867, just after 3 p.m. when the last coach of the Buffalo-bound New York Express of the Lake Shore Railway derailed at a bridge in Angola, New York, United States, slid down into a gorge, and caught fire, killing some 49 people. At the time, it was one of the deadliest train ...
The reservoir emptying through the failed Teton Dam on June 5, 1976 Ruins of the dam of Vega de Tera (Spain) after breaking in 1959. A dam failure or dam burst is a catastrophic type of structural failure characterized by the sudden, rapid, and uncontrolled release of impounded water or the likelihood of such an uncontrolled release. [1]
The study indicated that some of 121 earthquake swarms documented over a 24-year period in a section of the Czech Republic were caused by hydroseismicity. Scientific debate
Earthquake environmental effects are divided into two main types: Coseismic surface faulting induced by the 1915 Fucino, Central Italy, earthquake. Primary effects: which are the surface expression of the seismogenic source (e.g., surface faulting), normally observed for crustal earthquakes above a given magnitude threshold (typically M w =5.5 ...