DJ, What makes deep earthquakes apart, interesting is those quakes are UNDER the continental plates. [url]https://en.wikipedia.org/wiki/Plate_tectonics[/url] or https://en.wikipedia.org/wiki/Plate_tectonics - https://en.wikipedia.org/wiki/Plate_tectonics ; The key principle of plate tectonics is that the lithosphere exists as separate and distinct https://en.wikipedia.org/wiki/List_of_tectonic_plates" style="text-decoration: none; color: rgb(6, 69, 173); background: none;" title="List of tectonic plates - tectonic plates , which ride on the fluid-like ( https://en.wikipedia.org/wiki/Visco-elastic" style="text-decoration: none; color: rgb(6, 69, 173); background: none;" title="Visco-elastic - visco-elastic solid) asthenosphere. Plate motions range up to a typical 10–40 mm/year ( https://en.wikipedia.org/wiki/Mid-Atlantic_Ridge" style="text-decoration: none; color: rgb(6, 69, 173); background: none;" title="Mid-Atlantic Ridge - Mid-Atlantic Ridge ; about as fast as https://en.wikipedia.org/wiki/Fingernail" style="text-decoration: none; color: rgb(6, 69, 173); background: none;" title="Fingernail - fingernails grow), to about 160 mm/year ( https://en.wikipedia.org/wiki/Nazca_Plate" style="text-decoration: none; color: rgb(6, 69, 173); background: none;" title="Nazca Plate - Nazca Plate ; about as fast as https://en.wikipedia.org/wiki/Hair" style="text-decoration: none; color: rgb(6, 69, 173); background: none;" title="Hair - hair grows). https://en.wikipedia.org/wiki/Plate_tectonics#cite_note-6" style="text-decoration: none; color: rgb(6, 69, 173); background: none; - [6] The driving mechanism behind this movement is described below. Tectonic lithosphere plates consist of lithospheric mantle overlain by one or two types of crustal material: https://en.wikipedia.org/wiki/Oceanic_crust" style="text-decoration: none; color: rgb(6, 69, 173); background: none;" title="Oceanic crust - oceanic crust (in older texts called https://en.wikipedia.org/wiki/Sima_(geology)" style="text-decoration: none; color: rgb(6, 69, 173); background: none;" title="Sima (geology) - sima from https://en.wikipedia.org/wiki/Silicon" style="text-decoration: none; color: rgb(6, 69, 173); background: none;" title="Silicon - silicon and https://en.wikipedia.org/wiki/Magnesium" style="text-decoration: none; color: rgb(6, 69, 173); background: none;" title="Magnesium - magnesium ) and https://en.wikipedia.org/wiki/Continental_crust" style="text-decoration: none; color: rgb(6, 69, 173); background: none;" title="Continental crust - continental crust ( https://en.wikipedia.org/wiki/Sial" style="text-decoration: none; color: rgb(6, 69, 173); background: none;" title="Sial - sial from silicon and https://en.wikipedia.org/wiki/Aluminium" style="text-decoration: none; color: rgb(6, 69, 173); background: none;" title="Aluminium - aluminium ). Average oceanic lithosphere is typically 100 km (62 mi) thick; https://en.wikipedia.org/wiki/Plate_tectonics#cite_note-FOOTNOTETurcotteSchubert20025-7" style="text-decoration: none; color: rgb(6, 69, 173); background: none; - [7] its thickness is a function of its age: as time passes, it conductively cools and subjacent cooling mantle is added to its base. Because it is formed at mid-ocean ridges and spreads outwards, its thickness is therefore a function of its distance from the mid-ocean ridge where it was formed. For a typical distance that oceanic lithosphere must travel before being subducted, the thickness varies from about 6 km (4 mi) thick at mid-ocean ridges to greater than 100 km (62 mi) at https://en.wikipedia.org/wiki/Subduction" style="text-decoration: none; color: rgb(6, 69, 173); background: none;" title="Subduction - subduction zones; for shorter or longer distances, the subduction zone (and therefore also the mean) thickness becomes smaller or larger, respectively. https://en.wikipedia.org/wiki/Plate_tectonics#cite_note-FOOTNOTETurcotteSchubert2002-8" style="text-decoration: none; color: rgb(6, 69, 173); background: none; - [8] Continental lithosphere is typically about 200 km thick, though this varies considerably between basins, mountain ranges, and stable https://en.wikipedia.org/wiki/Craton" style="text-decoration: none; color: rgb(6, 69, 173); background: none;" title="Craton - cratonic interiors of continents. What can explain those deep quakes ? I think horizontal movement-one part of the plate moving up-the opposite side moving down...Climate change will be a factor. Less ice and snow on Greenland, Antarctica, Himalaya's is pushing that landmass up-so there the "plate" can go up...the opposite side could be in a location with deep earthquakes...but-again-linking climate change to deep earthquakes is still in study...[url]https://www.air-worldwide.com/blog/posts/2021/11/climate-change-may-influence-earthquakes/[/url] or https://www.air-worldwide.com/blog/posts/2021/11/climate-change-may-influence-earthquakes/ - https://www.air-worldwide.com/blog/posts/2021/11/climate-change-may-influence-earthquakes/ ; Glacial rebounding is a phenomenon where the crust rises due to melting of ice (unloading). The Canadian shield has been experiencing glacial rebounding since the last glacial retreat in the North America continent. As the climate continues to warm and reduce the amount of ice in some places and increase the mass of water (e.g., from oceans, precipitation), the stress on tectonic plates can change—sometimes abruptly. The topic of climate’s contribution to earthquakes, tsunamis, and even volcanic eruptions is not new and has been studied for the last few decades, with continued research interest. A https://agupubs.onlinelibrary.wiley.com/doi/full/10.1029/2020JB020411" rel="noopener" style="margin: 0px; padding: 0px; box-sizing: border-box; text-decoration: none; cursor: pointer; background-color: transparent; color: rgb(0, 78, 234); font-weight: bold; transition: all 0.25s ease 0s; word-break: break-word; - recent article , for example, discussed the contribution of glacial melt to a 1958 M7.8 earthquake in Alaska. That earthquake unleashed 30 million cubic meters of rock, causing a massive rockslide that slammed into the waters of the Gilbert Inlet and caused the https://geology.com/records/biggest-tsunami.shtml" rel="noopener" style="margin: 0px; padding: 0px; box-sizing: border-box; text-decoration: none; cursor: pointer; background-color: transparent; color: rgb(0, 78, 234); font-weight: bold; transition: all 0.25s ease 0s; word-break: break-word; - world’s largest tsunami runup ever recorded—1720 meters. The study noted that the event occurred in July, which is the warmest month of the year in Alaska, and that 1958 was the warmest year since 1944. The authors estimated that glacial melt increased the probability of the event occurring by 2%. While this may not be a big impact for that event, https://www.air-worldwide.com/blog/posts/2019/4/arctic-amplification-a-very-bad-positive-feedback-loop/" rel="noopener" style="margin: 0px; padding: 0px; box-sizing: border-box; text-decoration: none; cursor: pointer; background-color: transparent; color: rgb(0, 78, 234); font-weight: bold; transition: all 0.25s ease 0s; word-break: break-word; - Arctic amplification is causing rapid glacial melt in high latitudes, so the possibility exists for more activity like this to occur in the future. The reduction of glacial ice on and around volcanoes has also been https://pubs.geoscienceworld.org/gsa/geology/article/46/1/47/521232/Climatic-control-on-Icelandic-volcanic-activity" rel="noopener" style="margin: 0px; padding: 0px; box-sizing: border-box; text-decoration: none; cursor: pointer; background-color: transparent; color: rgb(0, 78, 234); font-weight: bold; transition: all 0.25s ease 0s; word-break: break-word; - shown to correlate with increased volcanic activity . This makes for a potentially interesting negative feedback mechanism between climate change and increased sulfate aerosols that would form from the activity and slightly reduce incoming solar radiation. [url]https://en.wikipedia.org/wiki/Deep-focus_earthquake[/url] or https://en.wikipedia.org/wiki/Deep-focus_earthquake - https://en.wikipedia.org/wiki/Deep-focus_earthquake other explanation...
------------- We cannot solve our problems with the same thinking we used when we created them. ~Albert Einstein
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