Surface rupture

 

Not every earthquake results in surface rupture, particularly for smaller and deeper earthquakes.^[1] In some cases, however, the lack of surface effects is because the fault that moved does not reach the surface. For example, the 1994 Northridge earthquake had a moment magnitude of 6.7, caused major damage in the Los Angeles area, occurred at 18.2 km (11 mi) below the Earth's surface, but did not cause surface rupture, because it was a blind thrust earthquake.^[3]

Surface ruptures commonly occur on pre-existing faults. Only rarely are earthquakes (and surface ruptures) associated with faulting on entirely new fault structures.^[4] There is shallow hypocenter, and large fracture energy on the asperities,^[5] the asperity shallower than 5 kilometres (3.1 mi). Examples of such earthquakes are San Fernando earthquake, Tabas earthquake, and Chi-Chi earthquake.^[6]

In surface rupture earthquakes, the large slips of land are concentrated in the shallow parts of the fault.^[7] And, notably, permanent ground displacements which are measureable can be produced by shallow earthquakes, of magnitude M5 and greater.^[8]

The form that surface rupturing takes depends on two things: the nature of the material at the surface and the type of fault movement.

 

Where there are thick superficial deposits overlying the trace of the faults, the resulting surface effects are typically more discontinuous. Where there is little or no superficial deposits, the surface rupture is generally continuous, except where the earthquake rupture affects more than one fault, which can lead to complex patterns of surface faulting, such as in the 1992 Landers earthquake.^[9]

Surface ruptures associated with normal faults are typically simple fault scarps. Where there are significant superficial deposits, sections with more oblique faulting may form sets of en-echelon scarp segments. Antithetic faults may also develop, giving rise to surface grabens.

Reverse faulting (particularly thrust faulting) is associated with more complex surface rupture patterns since the protruding unsupported part of the hanging-wall of the fault is liable to collapse. In addition there may be surface folding and back-thrust development.

 

Strike-slip faults are associated with dominantly horizontal movement, leading to relatively simple linear zones of surface rupture where the fault is a simple planar structure. However, many strike-slip faults are formed of overlapping segments, leading to complex zones of normal or reverse faulting depending on the nature of the overlap. Additionally, where there are thick superficial deposits, the rupture typically appears as a set of en-echelon faults.^[10]

To retrofit a house to survive surface rupture requires engineered design by geotechnical, and structural or civil engineers. This can be quite expensive.^[4]

• 1983 Borah Peak earthquake M6.9 in Idaho, normal faulting – 34 km (21 mi)
• 1992 Landers earthquake M7.3 in San Bernardino County, California, strike-slip faulting – 80 km (50 mi),^[4]
• 1999 İzmit earthquake M7.6 in Turkey, strike-slip faulting – 150 km (93 mi),^[11]
• 1999 Jiji earthquake M7.6 in Taiwan, thrust faulting – 100 km (62 mi)
• 2001 Kunlun earthquake M7.8 in Tibet, strike-slip faulting – 400 km (249 mi)
• 2002 Denali earthquake M7.9 in Alaska, strike-slip faulting – 340 km (211 mi)
• 2008 Sichuan earthquake M7.9 in Sichuan, thrust faulting – 300 km (186 mi)
• 2023 Turkey–Syria earthquakes M7.8 in Turkey, strike-slip faulting – 400 km (250 mi)^[12]

• Aseismic creep
• Ground fissure
• Vertical displacement

• A large article about surface rupture