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ASEISMIC CREEP

  • Aseismic creep
  • Surface displacement along a geological fault without earthquakes occurring

    geology, aseismic creep or fault creep is measurable surface displacement along a fault in the absence of notable earthquakes. Aseismic creep may also

    Aseismic creep

    Aseismic creep

    Aseismic_creep

  • Creep
  • Topics referred to by the same term

    diffraction Aseismic creep, a slow, steady movement along an earthquake fault Chip creep, phenomenon of chips moving out of sockets Downhill creep, the slow

    Creep

    Creep

  • Fault (geology)
  • Fracture or discontinuity in displaced rock

    the cause of most earthquakes. Faults may also displace slowly, by aseismic creep. A fault plane is the plane that represents the fracture surface of

    Fault (geology)

    Fault (geology)

    Fault_(geology)

  • Asperity (faults)
  • the fault may become locked, rather than continuously slipping as in aseismic creep. Earthquake rupture generally begins with the failure of an asperity

    Asperity (faults)

    Asperity_(faults)

  • Parkfield, California
  • Unincorporated community in California, United States of America

    that have shifted more than five feet relative to one another due to aseismic creep since the bridge was constructed in 1936. Google satellite images show

    Parkfield, California

    Parkfield, California

    Parkfield,_California

  • 1692 Jamaica earthquake
  • Earthquake and tsunami in British Jamaica

    none of the motion on the Plantain Garden fault is accommodated by aseismic creep. Jamaica portal Earth sciences portal List of historical earthquakes

    1692 Jamaica earthquake

    1692 Jamaica earthquake

    1692_Jamaica_earthquake

  • Hollister, California
  • City in California, United States

    among geologists because it represents one of the best examples of aseismic creep anywhere in the world. The Calaveras Fault (a branch of the San Andreas

    Hollister, California

    Hollister, California

    Hollister,_California

  • Calaveras Fault
  • Geological fault in northern California

    segments of the fault includes moderate and large earthquakes as well as aseismic creep. The last large event was the magnitude 6.2 1984 Morgan Hill event.

    Calaveras Fault

    Calaveras Fault

    Calaveras_Fault

  • Xianshuihe fault system
  • Geological feature in Asia

    the Luhuo, Daofu, Qianning, Kangding and Moxi. There is evidence of aseismic creep along much of this segment. An overall slip rate of 12 mm per year has

    Xianshuihe fault system

    Xianshuihe fault system

    Xianshuihe_fault_system

  • Creepmeter
  • active geologic fault in the Earth. Its function is to record the slow, aseismic creep between earthquakes. Creepmeters are used in various countries in areas

    Creepmeter

    Creepmeter

    Creepmeter

  • Earthquake cycle
  • Natural phenomenon

    approaching the end of its interseismic stage. A significant amount of aseismic slow slip and creep during the interseismic period has also been discovered on both

    Earthquake cycle

    Earthquake cycle

    Earthquake_cycle

  • Echelon cracks
  • surface. Such cracks are typically found in asphalt roadways due to aseismic creep and in other planar structures such as walls and building facades due

    Echelon cracks

    Echelon cracks

    Echelon_cracks

  • San Andreas Fault
  • Geologic feature in California, United States

    rest of the central section of the fault exhibits a phenomenon called aseismic creep, where the fault slips continuously without causing earthquakes. It

    San Andreas Fault

    San Andreas Fault

    San_Andreas_Fault

  • List of earthquakes in California
  • Francisco, the central SAF segment near San Juan Bautista is where aseismic creep was first studied, and to the south is where the recurring Parkfield

    List of earthquakes in California

    List of earthquakes in California

    List_of_earthquakes_in_California

  • Meers Fault
  • Geological fault in Oklahoma, United States

    fault presently is largely aseismic, with no earthquakes recorded along its Holocene trace or any evidence of aseismic creep although minor seismicity

    Meers Fault

    Meers_Fault

  • La Palma
  • Canary island

    1999 concluded that the western flank is stable with no evidence of aseismic creep. Other experts agree that the fracture resulting from the 1949 eruption

    La Palma

    La Palma

    La_Palma

  • Oceanic trench
  • Long and narrow depressions of the sea floor

    headwalls and sidewalls. Subduction of seamounts and aseismic ridges into the trench may increase aseismic creep and reduce the severity of earthquakes. Contrariwise

    Oceanic trench

    Oceanic trench

    Oceanic_trench

  • Earthquake rupture
  • Extent of slip in the Earth's crust that occurs during an earthquake

    earthquake on another part of the fault or because the next segment moves by aseismic creep, such that the stress never builds sufficiently to support rupture propagation

    Earthquake rupture

    Earthquake_rupture

  • 1968 Borrego Mountain earthquake
  • Earthquake in California

    Angeles. After the earthquake, the fault displayed a phenomenon known as aseismic creep, observed only along the central and southernmost section of the rupture

    1968 Borrego Mountain earthquake

    1968_Borrego_Mountain_earthquake

  • Slickenside
  • Smoothly polished surface in geology

    Calcite slickenfibres have recently been used to constrain the depth of aseismic creep in the Zagros Mountains as well as the orientation of stress acting

    Slickenside

    Slickenside

    Slickenside

  • 1978 Miyagi earthquake
  • Earthquake off Japan

    about 40 km, is interpreted to represent the depth of transition to aseismic creep on the plate interface. The maximum peak ground acceleration recorded

    1978 Miyagi earthquake

    1978 Miyagi earthquake

    1978_Miyagi_earthquake

  • Nadia Lapusta
  • Professor of mechanical engineering and geophysics

    interested in the mechanics and physics of seismic deformation and aseismic creep, and uses both analytical and numerical modelling to study friction

    Nadia Lapusta

    Nadia_Lapusta

  • Surface rupture
  • Offset at ground-level after earthquakes

    geotechnical, and structural or civil engineers. This can be quite expensive. Aseismic creep Ground fissure Vertical displacement "What is Surface Rupture". United

    Surface rupture

    Surface rupture

    Surface_rupture

  • Garlock Fault
  • Seismic fault in California, United States

    of the fault is locked, certain segments have been shown to move by aseismic creep, which is motion without resulting earthquakes. The Garlock is not considered

    Garlock Fault

    Garlock Fault

    Garlock_Fault

  • Seismogenic layer
  • processes (associated with brittle faulting) to a generally aseismic zone where ductile creep becomes the dominant process. The location of this change

    Seismogenic layer

    Seismogenic_layer

  • Slow earthquake
  • Discontinuous earthquake-like event

    a year each time, releasing as much energy as a magnitude 7 quake. Aseismic creep Long period ground motion Michael R. Forrest. "Slow Earthquakes". Southern

    Slow earthquake

    Slow_earthquake

  • UCERF3
  • 2015 US Geological Survey earthquake forecast for California

    California. This slippage is accommodated by ruptures (earthquakes) and aseismic creep on the various faults, with the frequency of ruptures dependent (in

    UCERF3

    UCERF3

    UCERF3

  • 2020 Kashgar earthquake
  • Earthquake affecting Xinjiang, China

    décollement is not due to the lack of friction. It instead displays aseismic creep at depth. According to the United States Geological Survey, the earthquake

    2020 Kashgar earthquake

    2020_Kashgar_earthquake

  • New Guinea Trench
  • Oceanic trench

    along the trench, it is thought to be accommodating strain through aseismic creep for most of its length. The 17 February 1996 earthquake near Biak was

    New Guinea Trench

    New Guinea Trench

    New_Guinea_Trench

  • 2021 Haiti earthquake
  • 7.2-magnitude earthquake in Tiburon Peninsula, Haiti

    R.; Vernon, A.; Vajedian, S. (2022). "Complex rupture and triggered aseismic creep during the August 14, 2021 Haiti earthquake from satellite geodesy"

    2021 Haiti earthquake

    2021 Haiti earthquake

    2021_Haiti_earthquake

  • Haiyuan Fault
  • Intracontinental strike-slip fault in Tibet

    (19–25 mi) section of the fault that displays a phenomenon known as an aseismic creep at shallow depths. The fault was the source of two very large and destructive

    Haiyuan Fault

    Haiyuan Fault

    Haiyuan_Fault

  • Hualca Hualca
  • Extinct volcano in Peru

    activity, and some have produced earthquakes in recent times or undergone aseismic creep. There are three clusters of shallow seismic activity at Hualca Hualca

    Hualca Hualca

    Hualca Hualca

    Hualca_Hualca

  • Echelon formation
  • Formation with units arranged diagonally

    commonly seen in asphalt roads subject to shear stress imposed by aseismic fault creep. In mathematics, the term row echelon form refers to a kind of matrix

    Echelon formation

    Echelon formation

    Echelon_formation

  • Fault mechanics
  • Field of study that investigates the behavior of geologic faults

    earthquake sometime in the future Orogeny – Formation of mountain ranges Aseismic creep Brune, J.N. (1970). "Tectonic stress and the spectra of seismic shear

    Fault mechanics

    Fault mechanics

    Fault_mechanics

  • Palu-Koro Fault
  • insufficient to account for the long-term slip-rate, suggesting that either aseismic creep is important in this fault zone or that other strands have been active

    Palu-Koro Fault

    Palu-Koro_Fault

  • 1981 Westmorland earthquake
  • 1981 earthquake in southern California, United States

    Lohman, R. B., and McGuire, J. J. (2007), Earthquake swarms driven by aseismic creep in the Salton Trough, California, J. Geophys. Res., 112, B04405, doi:10

    1981 Westmorland earthquake

    1981_Westmorland_earthquake

  • 1969 Alaşehir earthquake
  • Earthquake in Turkey

    However the measurement was recorded a week after the event hence aseismic creep may have occurred and contaminated actual coseismic offset measurements

    1969 Alaşehir earthquake

    1969_Alaşehir_earthquake

  • Buried rupture earthquake
  • Earthquake which does not produce a visible offset in the ground along the fault

    plane in buried rupture earthquakes makes for large tsunami waves. Aseismic creep "Observed differences in ground motions" (PDF). IJR. Retrieved 30 October

    Buried rupture earthquake

    Buried rupture earthquake

    Buried_rupture_earthquake

  • Brittle–ductile transition zone
  • Strongest part of the Earth's crust

    F.; Bürgmann, R.; Nadeau, R. M. (2004), "The evolution of the seismic-aseismic transition during the earthquake cycle: Constraints from the time-dependent

    Brittle–ductile transition zone

    Brittle–ductile transition zone

    Brittle–ductile_transition_zone

  • Alex Giuliani Plaza
  • City Hall (1930-1969) in Hayward, CA

    building. The building was abandoned due to structural damage caused by aseismic creep. The Hayward 9/11 Memorial, located adjacent to the city hall building

    Alex Giuliani Plaza

    Alex_Giuliani_Plaza

  • Coast Range Geomorphic Province
  • majority of motion occurring during large earthquakes, with some aseismic fault creep. The overlap of the plates is about 100 km wide and contains all

    Coast Range Geomorphic Province

    Coast_Range_Geomorphic_Province

  • Chixoy-Polochic Fault
  • Fault zone in Guatemala and Mexico

    activity includes at least for slip events between 17 ka and 13 ka BP, and aseismic surface rupture over some of the past 5 centuries. One or several intermediate

    Chixoy-Polochic Fault

    Chixoy-Polochic_Fault

  • Episodic tremor and slip
  • Seismological phenomenon observed in some subduction zones

    by about two weeks of 1 to 10 Hz seismic trembling and non-earthquake ("aseismic") slip on the plate boundary equivalent to a magnitude 7 earthquake. (Tremor

    Episodic tremor and slip

    Episodic_tremor_and_slip

  • El Pilar Fault System
  • Geological faults in Venezuela

    as a whole is seismically active, although some sections appear to creep aseismically, which may explain the relatively small number of major historical

    El Pilar Fault System

    El Pilar Fault System

    El_Pilar_Fault_System

  • List of Greek and Latin roots in English/P–Z
  • sei- shake Greek σείειν (seíein), σεισμός (seismós), σεῖστρον (seîstron) aseismic, microseism, microseismic, paleoseismology, seism, seismic, seismogram

    List of Greek and Latin roots in English/P–Z

    List_of_Greek_and_Latin_roots_in_English/P–Z

  • Michele Cooke
  • American geoscientist

    tectonically active regions in the crust. This phenomenon involves the aseismic slip of fault segments that can pass shear stress to relieve tectonic stress

    Michele Cooke

    Michele_Cooke

  • Mayon
  • Stratovolcano in Luzon, Philippines

    the volcano's summit lava dome since the last week of April, indicating aseismic growth. Rockfall increased in frequency from an average of five events

    Mayon

    Mayon

    Mayon

  • List of Greek and Latin roots in English/S
  • sei- shake Greek σείειν (seíein), σεισμός (seismós), σεῖστρον (seîstron) aseismic, microseism, microseismic, paleoseismology, seism, seismic, seismogram

    List of Greek and Latin roots in English/S

    List_of_Greek_and_Latin_roots_in_English/S

  • Outline of plate tectonics
  • Hierarchical outline list of articles related to plate tectonics

    Eurasian Plates Aden Ridge – Rift portion in Gulf of Aden Cocos Ridge – Aseismic ridge within the Cocos plate Explorer Ridge – Mid-ocean ridge west of British

    Outline of plate tectonics

    Outline_of_plate_tectonics

  • Timeline of the development of tectonophysics (after 1952)
  • Chronological listing of significant events in the history of tectonophysics

    a solid and crystalline body, is one school of thought. A lithosphere creeping over the asthenosphere is a logical consequence of an Earth with internal

    Timeline of the development of tectonophysics (after 1952)

    Timeline_of_the_development_of_tectonophysics_(after_1952)

  • Cerro Blanco (volcano)
  • Caldera in Catamarca Province, Argentina

    V.; Folguera, A. (September 2023). "Reviewing the geodynamic impact of aseismic ridges subduction on the tectonic-magmatic evolution of the Southern Puna

    Cerro Blanco (volcano)

    Cerro Blanco (volcano)

    Cerro_Blanco_(volcano)

  • 1852 Banda Sea earthquake
  • Earthquake and tsunami in Indonesia

    on this fault, therefore, it is suggested that the structure is creeping aseismically, or that earthquakes on this fault have occurred before the birth

    1852 Banda Sea earthquake

    1852_Banda_Sea_earthquake

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