Open main menu
Home
Random
Recent changes
Special pages
Community portal
Preferences
About Wikipedia
Disclaimers
Incubator escapee wiki
Search
User menu
Talk
Dark mode
Contributions
Create account
Log in
Editing
Explorer plate
(section)
Warning:
You are not logged in. Your IP address will be publicly visible if you make any edits. If you
log in
or
create an account
, your edits will be attributed to your username, along with other benefits.
Anti-spam check. Do
not
fill this in!
== Seismic activity == As a part of the Pacific [[Ring of Fire]], the Explorer plate has a high level of seismic activity. However, the activity consists of low-magnitude events; no earthquake above [[Seismic scale|magnitude]] 6.5 has been recorded in the region, though a swarm of several dozen magnitude 5β6 earthquakes occurred just north of the [[Seminole Seamount]] in 2008.<ref>{{Cite web|url=https://concord.org/stem-resources/seismic-explorer|title=Seismic Explorer|date=October 6, 2016|website=Concord Consortium|access-date=May 25, 2017}}</ref> The Explorer plate is the most seismically active area of Canada, but is anomalous as a subduction zone since most of the seismic activity occurs around the plate's perimeter rather than at the subduction interface.<ref name=":22" /> Events are generally centered around the southern and north-western areas where the borders of the plate are in contact with other plates; however, the newer ocean crust created at Explorer ridge and [[Juan de Fuca Ridge|Juan de Fuca ridge]] reduces the rigidity of the region and contributes to the low magnitude of events in the region.<ref>{{Cite journal|last=Fuis|first=Gary S.|title=West margin of North America β a synthesis of recent seismic transects|journal=Tectonophysics|volume=288|issue=1β4|pages=265β292|doi=10.1016/s0040-1951(97)00300-4|bibcode=1998Tectp.288..265F|year=1998|url=https://zenodo.org/record/1259709}}</ref>
Edit summary
(Briefly describe your changes)
By publishing changes, you agree to the
Terms of Use
, and you irrevocably agree to release your contribution under the
CC BY-SA 4.0 License
and the
GFDL
. You agree that a hyperlink or URL is sufficient attribution under the Creative Commons license.
Cancel
Editing help
(opens in new window)