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Originally posted by kattraxx
Magnitude 4.1 - SAN FRANCISCO BAY AREA, CALIFORNIA
2010 January 07 18:09:35 UTC
Epicenter: Milpitas, CA near south bay on east side
Originally posted by kattraxx
reply to post by alysha.angel
Hi alysha. Can I ask how you determine your predictions? Is it via the Charlotte King geosensology method? Or another? Just curious. What type of precursors are you picking up right now?
I agree with you. I was just emailing a friend near Milpitas, CA who alerted me to the SF bay area EQ when it happened. I told her to be on guard because I'm still getting precursors for that area. Could be aftershocks, but I don't think so--- usually, the precursors pretty much go away after the main shock. Don't ask me how it works; I just know it does.
Hi JustMike, space cadet and soma!
Forgot to mention that Charlotte King informed me yesterday that some of the missing SF bay area sea lions have shown up off the coast of Oregon. Some of them were tagged, so that's how they can follow them.
[edit on 1/7/10 by kattraxx]
Originally posted by kattraxx
reply to post by alysha.angel
So true. And apparently, the sea lions went all the way to the Oregon coast, along with another group of sea lions from the Oregon coast. I believe Charlotte said they all, both groups, moved to another location on the Oregon coast.
Thanks for the response. I'm always interested to hear how others come to their predictions. Sometimes, it has more to do with a gut feeling than anything else.
The landslide reported is actually a reactivation of part of an older and larger landslide
The Derby 1:50 000 geological map area is located to the north of the city of Derby, incorporating the northern half of Derby itself, along with the western districts of the city of Nottingham (Figure 1). The southern margin of the Derby sheet is underlain by Triassic bedrock consisting of the Mercia Mudstone and Sherwood Sandstone Groups, which form relatively low relief and rolling agricultural land. To the west and north west of the map sheet, the underlying Namurian rocks of the Millstone Grit Group produce relatively steep-sided valleys and slopes and it is this terrain that contains the highest frequency of landslides. The central portion of the map area is underlain by the Pennine Lower and Middle Coal Measures Formations of Carboniferous (Westphalian) age, which form the southern limb of the East Pennine Coalfield. These produce a relatively undulating landscape, with locally oversteepened valley sides where mudstones outcrop between stronger sandstone beds. The eastern sector of the map is occupied by Permian dolostones, mudstones and sandstones of the Zechstein Group, which unconformably overlie the Pennine Middle Coal Measures Formation. These produce a relatively subdued topography, with gently sloping hillsides and valleys.
Originally posted by blujay
reply to post by alysha.angel
We felt that one here at work in Santa Cruz county.
I feel like something's really up.