http://news.sciencemag.org/sciencenow/2011/05/another-look-beneath-hawaii-knoc.html?rss=1
The above two articles, probably, let us rethink current mantle plumes
and convection.concept. I tried to suggest another
heat transport mechanism:
Tectonics. Types Of Heat Transport To Develop Calderas, Volcanoes, And
Divergent Boundaries.
http://divergent-boundaries.blogspot.com/2011/06/tectonics-types-of-heat-transport-to.html
Sergey Sukhotinsky.
---
Slow Earthquake In Case A Divergent Boundary Is Close To Subduction Zone.
http://divergent-boundaries.blogspot.com/2011/06/slow-earthquakes.html
Formation Of Mountain Ridges by Broken Process Of Subduction Of A
Tectonic Plate.
http://divergent-boundaries.blogspot.com/2011/05/mountain-ridges-formation-keeping-it.html
On Mon, Jun 13, 2011 at 6:15 AM, Lin Kerns <linkerns@gmail.com> wrote:
>
>
>
> PRELIMINARY EARTHQUAKE REPORT
>
> GNS SCIENCE
> GeoNet Data Centre
> Lower Hutt, New Zealand
> http://www.geonet.org.nz
>
>
> The following earthquake has been recorded by GNS Science:
>
> Reference number: 3528839/G
> Universal Time: 13 June 2011 at 02:20
> NZ Standard Time: Monday, 13 June 2011 at 2:20 pm
> Latitude, Longitude: 43.58°S, 172.74°E
> Location: 10 km south-east of Christchurch
> Focal depth: 9 km
> Richter magnitude: 6.0
>
> Web page: http://www.geonet.org.nz/earthquake/quakes/3528839g.html
>
> Felt widely in Canterbury.
>
>
> The GeoNet project is core funded by the Earthquake Commission (EQC) and is
> being designed, installed and operated by GNS Science on behalf of EQC and all
> New Zealanders.
>
------------------------------------
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