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ACM5p2_BeaufortFault.md

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Name ACM5p2_BeaufortFault
magnitude 5.2
latitude 49.330 degrees
longitude -124.840 degrees
maximum_peak_ground_acceleration 0.190 g
recurrence rate 41 years*
*For Cascadia, Leech River, and Devil's Mountain Faults these are characteristic earthquakes, else they are recurrence interval for an event of equal or greater magnitude in the scenario source region.
cost $295,697,765
redtag 77 buildings
displaced 14 people
deaths 1 people
critical_injuries_and_entrapments 1 people
all_hospitalizations 7 people
epicentre_map Epicentre
shakemap_file s_shakemap_ACM5p2_BeaufortFault_12.csv
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damage_baseline_file s_dmgbyasset_ACM5p2_BeaufortFault_b0_13_b.csv
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damage_retrofitted_file s_dmgbyasset_ACM5p2_BeaufortFault_r1_14_b.csv
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consequence_baseline_file s_consequences_ACM5p2_BeaufortFault_b0_13_b.csv
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consequence_retrofitted_file s_consequences_ACM5p2_BeaufortFault_r1_14_b.csv
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loss_baseline_file s_lossesbyasset_ACM5p2_BeaufortFault_b0_15_b.csv
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loss_retrofitted_file s_lossesbyasset_ACM5p2_BeaufortFault_r1_16_b.csv
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site_model_file openquake-inputs/earthquake/sites/regions/site-vgrid_BC.csv
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rupture_model_file ruptures/rupture_ACM5p2_BeaufortFault.xml
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rupture_mesh_spacing 4
gsim_logic_tree_file CanadaSHM6/OpenQuake_model_files/gmms/LogicTree/OQ_classes_NGASa0p3weights_activecrust.xml
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truncation_level_risk 3.0
maximum_distance 400
number_of_ground_motion_fields_risk 400
exposure_file openquake-inputs/exposure/general-building-stock/oqBldgExp_BC.xml
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taxonomy_mapping_baseline openquake-inputs/earthquake/vulnerability/CanSRM1_TaxMap_b0.csv
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structural_fragility_file openquake-inputs/earthquake/vulnerability/structural_fragility_CAN.xml
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structural_vulnerability_file openquake-inputs/earthquake/vulnerability/vulnerability_structural_CAN.xml
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nonstructural_vulnerability_file openquake-inputs/earthquake/vulnerability/vulnerability_nonstructural_CAN.xml
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contents_vulnerability_file openquake-inputs/earthquake/vulnerability/vulnerability_contents_CAN.xml
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description Scenario for a magnitude 5.2 shallow crustal earthquake along the Beaufort Range Fault based on a 10 percent in 50 years seismic hazard deaggregation and kinematics from a neotectonic study by Lynch et al. 2017 and focal mechanisms of the 1946 7p3 EQ associated with this fault by Rogers and Hasegawa 1978