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Statements

Subject Item
dbr:1898_Mare_Island_earthquake
rdf:type
schema:Event geo:SpatialThing owl:Thing dbo:Earthquake wikidata:Q1656682 dbo:Event dbo:NaturalEvent n22:Event
rdfs:label
1898 Mare Island earthquake
rdfs:comment
The 1898 Mare Island earthquake occurred in Northern California on March 30 at 23:43 local time with a moment magnitude of 5.8–6.4 and a maximum Mercalli intensity of VIII–IX (Severe–Violent). Its area of perceptibility included much of northern and central California and western Nevada. Damage amounted to $350,000 (about $10,700,000 inflation adjusted to 2018) and was most pronounced on Mare Island, a peninsula in northern San Francisco Bay. While relatively strong effects there were attributed to vulnerable buildings, moderate effects elsewhere in the San Francisco Bay Area consisted of damaged or partially collapsed structures, and there were media reports of a small tsunami and mostly mild aftershocks that followed.
rdfs:seeAlso
dbr:Transform_fault dbr:Interplate_earthquake
geo:lat
38.20000076293945
geo:long
-122.4000015258789
foaf:depiction
n15:USGS_–_Green_Valley_Fault.gif n15:USGS_–_Hayward_Fault_Zone.gif n15:USGS_–_Rodgers_Creek_fault_zone.gif
dcterms:subject
dbc:Earthquakes_in_California dbc:1898_in_California dbc:History_of_the_San_Francisco_Bay_Area dbc:Mare_Island dbc:1898_earthquakes
dbo:wikiPageID
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dbo:wikiPageRevisionID
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dbo:wikiPageWikiLink
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owl:sameAs
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dbo:thumbnail
n15:USGS_–_Rodgers_Creek_fault_zone.gif?width=300
dbp:anssUrl
ushis341
dbp:countriesAffected
Northern California United States dbr:San_Francisco_Bay_Area
dbp:damage
350000.0
dbp:intensity
dbp:localDate
1898-03-30
dbp:localTime
1423.0
dbp:magnitude
5.8
dbp:pre
yes
dbp:timestamp
1898-03-31
dbp:title
1898
dbp:tsunami
Possible
dbp:type
Unknown
georss:point
38.2 -122.4
dbo:abstract
The 1898 Mare Island earthquake occurred in Northern California on March 30 at 23:43 local time with a moment magnitude of 5.8–6.4 and a maximum Mercalli intensity of VIII–IX (Severe–Violent). Its area of perceptibility included much of northern and central California and western Nevada. Damage amounted to $350,000 (about $10,700,000 inflation adjusted to 2018) and was most pronounced on Mare Island, a peninsula in northern San Francisco Bay. While relatively strong effects there were attributed to vulnerable buildings, moderate effects elsewhere in the San Francisco Bay Area consisted of damaged or partially collapsed structures, and there were media reports of a small tsunami and mostly mild aftershocks that followed. The mechanism of the shock is unknown, but several independent investigations focused on different aspects to gain a better understanding of the intensity, magnitude, source fault, and epicenter of this pre-instrumental event. Most investigators placed it under or to the north of San Pablo Bay, though two earthquake catalogs gave specific coordinates that place it within the confines of the San Pablo Bay National Wildlife Refuge. One of the numerous strike-slip faults of the San Andreas Fault System in the North Bay are most often named as the source fault, but one seismologist's paper detailed how an unnamed dip-slip fault may have been responsible. Several more recent studies gave alternate perspectives that named specific faults as the origin.
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