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Originally posted by PuterMan
reply to post by muzzy
HALT is a CERI seismometer.
folkworm.ceri.memphis.edu...
Fecha, Tiempo, Latitud S , Longitud W, Prof.km, Mag ML, Intensi.MM, Localidades
2011-08-24 17:46:11, 07.67, 74.77, 149, 7.0, V-VI Contamana; V Pucallpa;IV Tingo Maria, Tarapoto; III-IV
Originally posted by Robin Marks
Water does lubricate faults. But it's not the same thing as lubricating an engine with oil. The water travels through the fault and causes erosion. It's superheated because of the pressures and heat underground. It carves channels and removes material. It's kinda like glaciers.Glaciers have supercooled water that flows down through the glacier until it hits the crust. It then slices along the bottom like a large waterfall. The glacier is actually moving on a superthin-cooled layer of water. You can think of water in a fault in reserve. It moves through the fault and destabilzed the fault until enough resistence is removed. It technically doesn't slide along on the water making it more slippery,
Damn, I forget the name of this type of sand, that contains water, and they find it in California and scientists think this material lets those particalur quakes slide.
If you throw cold water on a rock you will crack it. A sudden rush of cold water that runs into a fault can cause it to crack. That's what can happen at Yellowstone. When water can breach one part of the geyers plumbing and migrates and hits hot rock, there is an hydrothermal exposion underground causing an earthquake. Or more likely a swarm.
Water does all kinds of weird and whacking things depending on its state.
Magnitude
4.5
Date-Time
Thursday, August 25, 2011 at 05:07:50 UTC
Thursday, August 25, 2011 at 01:07:50 AM at epicenter
Time of Earthquake in other Time Zones
Location
37.940°N, 77.896°W
Depth
5 km (3.1 miles)
Region
VIRGINIA
Distances
51 km (31 miles) E of Charlottesville, Virginia
53 km (32 miles) SW of Fredericksburg, Virginia
58 km (36 miles) NW of RICHMOND, Virginia
83 km (51 miles) NNE of Farmville, Virginia
Location Uncertainty
horizontal +/- 11.3 km (7.0 miles); depth +/- 3 km (1.9 miles)
Parameters
NST= 94, Nph=109, Dmin=52.3 km, Rmss=1.41 sec, Gp= 86°,
M-type="Nuttli" surface wave magnitude (mbLg), Version=5
Source
Magnitude: USGS NEIC (WDCS-D)
Location: USGS NEIC (WDCS-D)
Event ID
usc0005jg1
Originally posted by sylvrshadow
Just felt that one. In in southern va, 20 min from the epicenter of the last one. Definitely felt that, but not as bad as before. Nothing on USGS yet though.
edit to add that it is now reported on USGS as a 4.5edit on 8/25/2011 by sylvrshadow because: (no reason given)
Yeah, I was expecting aftershocks, but certainly not ones I could feel. This is all quite a new experience for me!edit on 8/25/2011 by sylvrshadow because: (no reason given)
Originally posted by sylvrshadow
reply to post by TrueAmerican
"And just for the record, that measured about 800 microns/sec at US.CBN- with the quake very close to the 5.8."
Could you please explain the significance of that for me? Thankx!
edit on 8/25/2011 by sylvrshadow because: (no reason given)
Originally posted by CodyOutlaw
reply to post by summer5
I just read on glp that they are smelling rotten eggs in tennessee right now, too.
Strongly.
Originally posted by sylvrshadow
reply to post by TrueAmerican
Thanks for the reply. So how many more aftershocks do you think we will get? (At least ones we can feel) And do you think there is a possibility of an aftershock that is stronger than the original quake?