It looks like you're using an Ad Blocker.
Please white-list or disable AboveTopSecret.com in your ad-blocking tool.
Thank you.
Some features of ATS will be disabled while you continue to use an ad-blocker.
just checked usgs they got 5.8, no phase data yet
2011 January 23, St. George, QLD ML 3.8 (Google map)
1940 UTC, 148.5°E, 28.4°S, normal depth
(Monday, January 24, 06:40 am AEDT)
This earthquake occurred approximately 45 kilometres south of St. George, 200 kilometres south of Roma, QLD.
Originally posted by bkaust
Earthquake in St George, QLD today - due to the amount of floodwater they have received lately?
2011 January 23, St. George, QLD ML 3.8 (Google map)
1940 UTC, 148.5°E, 28.4°S, normal depth
(Monday, January 24, 06:40 am AEDT)
This earthquake occurred approximately 45 kilometres south of St. George, 200 kilometres south of Roma, QLD.
Source
Monday morning's quake was not related to an earthquake that hit Pakistan's Baluchistan province on Wednesday, Mehmood said.
The Indian Plate is moving northward lubricated by the heavy flooding in Pakistan.
Melt produced by friction during earthquakes may act either as a coseismic fault lubricant or as a viscous brake. ................... We conclude that friction-induced melts can lubricate faults at intermediate crustal depths.
Increases in heat flow have not been found near active faults (6). These observations can be explained by low tf (4, 7). Melt lubrication is a possible cause of low tf, because solidified, clast-laden, friction-induced melts (pseudotachylytes) decorate some exhumed ancient faults (12). However, evidence of melt is not ubiquitous on faults, indicating that other weakening mechanisms may be important, especially in the presence of fluids.
Here we present evidence for dynamic weakening of experimental faults that are sheared at velocities approaching earthquake slip rates. The experimental faults, which were made of room-dry, solid granite blocks, quickly wore to form a fine-grain rock powder known as gouge. At modest slip velocities of 10-60mms-1, this newly formed gouge organized itself into a thin deforming layer that reduced the fault’s strength by a factor of 2-3.
£566K to Nicola de Paola for a project 'Fault lubrication during earthquake propagation in thermally unstable rocks'
The estimation of this parameter is out of the range of seismological studies, although it controls the magnitude of the stress drop, the seismic fault heat flow and the relative partitioning of the earthquake energy budget, which are all controversial and still debated issues in the scientific community
Geologists say they have discovered that an ultra-thin layer of smectitic clay on rocks along deep, older fault lines in the San Andreas fault region provide important lubrication that permits gradual movement rather than earthquake-producing jumps.
It’s been raining a lot, or very hot--it must be earthquake weather!
FICTION: Many people believe that earthquakes are more common in certain kinds of weather. In fact, no correlation with weather has been found. Earthquakes begin many kilometers (miles) below the region affected by surface weather. People tend to notice earthquakes that fit the pattern and forget the ones that don't. Also, every region of the world has a story about earthquake weather, but the type of weather is whatever they had for their most memorable earthquake.
You can prevent large earthquakes by making lots of small ones, or by "lubricating" the fault with water
FICTION: Seismologists have observed that for every magnitude 6 earthquake there are about 10 of magnitude 5, 100 of magnitude 4, 1,000 of magnitude 3, and so forth as the events get smaller and smaller. This sounds like a lot of small earthquakes, but there are never enough small ones to eliminate the occasional large event. It would take 32 magnitude 5's, 1000 magnitude 4's, and 32,000 magnitude 3's to equal the energy of one magnitude 6 event. So, even though we always record many more small events than large ones, there are far too few to eliminate the need for the occasional large earthquake. As for "lubricating" faults with water or some other substance, if anything, this would have the opposite effect. Injecting high- pressure fluids deep into the ground is known to be able to trigger earthquakes-to cause them to occur sooner than would have been the case without the injection. This would be a dangerous pursuit in any populated area, as one might trigger a damaging earthquake.
The Indian Plate is moving northward lubricated by the heavy flooding in Pakistan.