The main shock of the Northridge Earthquake ruptured on a hidden fault approximately 18 Kilometers beneath the surface for roughly 8 seconds. The rupture proliferated upward and northwestward alongside the fault at around 3 kilometers per second. The resulting size of the rupture was between 15 and 20 kilometers and concluded at a depth of 5 to 6 kilometers. Unfortunately, the greatest seismic energy was directed toward the most populated areas in the northern regions of the San Fernando Valley. The Earthquake caused significant damage to surrounding areas within approximately 4,000 square kilometers, forcing the land surface upward in the shape of an asymmetric dome, primarily due to uplifting of the valley and surround mountainous areas. According to USGS, the Santa Susana Mountains were moved by as much as 52 centimeters. The northern part of the valley was uplifted as much as 20 to 40
The main shock of the Northridge Earthquake ruptured on a hidden fault approximately 18 Kilometers beneath the surface for roughly 8 seconds. The rupture proliferated upward and northwestward alongside the fault at around 3 kilometers per second. The resulting size of the rupture was between 15 and 20 kilometers and concluded at a depth of 5 to 6 kilometers. Unfortunately, the greatest seismic energy was directed toward the most populated areas in the northern regions of the San Fernando Valley. The Earthquake caused significant damage to surrounding areas within approximately 4,000 square kilometers, forcing the land surface upward in the shape of an asymmetric dome, primarily due to uplifting of the valley and surround mountainous areas. According to USGS, the Santa Susana Mountains were moved by as much as 52 centimeters. The northern part of the valley was uplifted as much as 20 to 40