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ACM7p7_QueenCharlotteFault.md

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Name ACM7p7_QueenCharlotteFault
magnitude 7.7
latitude 53.000 degrees
longitude -132.620 degrees
maximum_peak_ground_acceleration 0.382 g
recurrence rate -21 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 $36,949,541
redtag 20 buildings
displaced 121 people
deaths 2 people
critical_injuries_and_entrapments 1 people
all_hospitalizations 8 people
epicentre_map Epicentre
shakemap_file s_shakemap_ACM7p7_QueenCharlotteFault_1.csv
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damage_baseline_file s_dmgbyasset_ACM7p7_QueenCharlotteFault_b0_2_b.csv
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damage_retrofitted_file s_dmgbyasset_ACM7p7_QueenCharlotteFault_r1_3_b.csv
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consequence_baseline_file s_consequences_ACM7p7_QueenCharlotteFault_b0_2_b.csv
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consequence_retrofitted_file s_consequences_ACM7p7_QueenCharlotteFault_r1_3_b.csv
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loss_baseline_file s_lossesbyasset_ACM7p7_QueenCharlotteFault_b0_4_b.csv
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loss_retrofitted_file s_lossesbyasset_ACM7p7_QueenCharlotteFault_r1_5_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_ACM7p7_QueenCharlotteFault.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 Magnitude 7.7 rupture along the Queen Charlotte Fault based on 10 percent in 50 years deaggregation and based on kinematics documented by Bostwick 1984 in their paper titled A re-examination of the August 22, 1949 Queen Charlotte earthquake and depth constraints based on paper by Wang et al 2015 titled Thermal Condition of the 27 October 2012 Mw 7.8 Haida Gwaii Subduction Earthquake at the Obliquely Convergent Queen Charlotte Margin