[EHPweb] Recenteqs Monitoring messages

Jeremy M Fee jmfee at usgs.gov
Thu Feb 11 16:14:42 UTC 2010


FYI, this difference is planned and is due to a lower magnitude  
threshold for REQS_US on ehpmaster and ehpbackup.  This is in  
preparation for the CA/NV fault maps move from quake to earthquake.


Thanks,

Jeremy


Begin forwarded message:

> From: quake at ehpbackup.cr.usgs.gov
> Date: February 11, 2010 6:47:32 AM MST
> To: jmfee at usgs.gov
> Subject: Difference in numeqs >= 10 for 72 times in a row at Thu Feb  
> 11 05:47:28 PST 2010: WW 177 177 177 177 177 177 US 726 726 726 726  
> 1082 1082
>
> Difference in numeqs >= 10 for 72 times in a row at Thu Feb 11  
> 05:47:28 PST 2010: WW 177 177 177 177 177 177 US 726 726 726 726  
> 1082 1082
> Thu Feb 11 05:47:28 PST 2010
> Number_eqs  Time_elapsed_since_last_update  Last_event  Version   
> Server
> 177   44:08 us2010spa2 7  :earthquake on Akamai = ehp?
> 177   44:09 us2010spa2 7  :ehp1-earthquake on ehp1
> 177   44:08 us2010spa2 7  :ehp2-earthquake on ehp2
> 177   44:08 us2010spa2 7  :ehp3-earthquake on ehp3
> 177   44:02 us2010spa2 7  :ehpm-earthquake on ehpmaster
> 177   44:07 us2010spa2 7  :ehpb-earthquake on ehpbackup
> 726   14:59 ci10541197 1  :earthquake on Akamai = ehp?
> 726   14:59 ci10541197 1  :ehp1-earthquake on ehp1
> 726   14:58 ci10541197 1  :ehp2-earthquake on ehp2
> 726   14:57 ci10541197 1  :ehp3-earthquake on ehp3
> 1082    7:59 ci10541197 1  :ehpm-earthquake on ehpmaster
> 1082    7:56 ci10541197 1  :ehpb-earthquake on ehpbackup
> 701    7:03 ci10541197 1  :quake on Akamai =<BR> ehznorth-ehzeast- 
> ehzden
> 701    7:04 ci10541197 1  :ncweb-north on ehznorth
> 701    7:03 ci10541197 1  :ncweb-east on ehzeast
> 701    7:01 ci10541197 1  :ncweb-den on ehzden
> 701    7:04 ci10541197 1  :ncweb-menlo on ehzmenlo
> 701    6:42 ci10541197 1  :scec on scec
> 701    7:03 ci10541197 1  :berkeley on berkeley
>
>
>  Message from REQS_monitor on ehpbackup.
>   Check  http://ehpb-earthquake.cr.usgs.gov/earthquakes/recenteqsww/mostrecent_summary.html
>



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