ScribbleLive

@RBeaner : we can only speculate, but i really assume they know how to construct a solid foundation. they constructed skyscrapers in tokyo and they all are still standing.

@Edano Another 4.6 warning

@fitter www.gloresis.info

it doesn't show anything past 6:30 or so

right church wrong pew

@fitter interesting video 3min of liquefaction in tokyo central park, reclaimed lan, but same idea. www.paleoseismicity.org

@dean I had a phone call yesterday, short cut the lady told her to take me off the list wasn't interested....blbla blab ( i have six lines and get about 20 calls a day from "sales") as i was hanging up and it was to late... heard her say that she was from the NRC .... I had been e-mailing them on various things... next time i guess i'll ask who is calling first ... I just went by the caller ID "unavalible"

@RBeaner : i still hope there is no soil under the reactors. under a highway, okay, but not under an npp.

@dean gremblims are back..... now its driving me crazy to know why she was calling..... I could hear her talking as I was puting the reciver on the hook, but i have sent so many e-mails i don't have a clue who might have responded

@dean do you have a link or larger pic of the mock ups

@dean Cool, we had a little snafu at first, but I think we have it now.

@Jim 700 central time

@dean gremblin!!!!!!!!!!!! read they have 16 relief vavles on the main steam lines, but could not trace now i see them

@dean surry has one i should take a ride over there, i don't read *** and couln't figure if they had six 4" lines or 6 4

'

gremblins11111111111

off to jim party, better leave early i guess i'm taking the gremblins with me tonight.... still no electrtions...

@Edano and RBean Not exactly granite, eh? From wikipedia: Mudstone (also called mudrock) is a fine grained sedimentary rock whose original constituents were clays or muds. Grain size is up to 0.0625 mm (0.0025 in) with individual grains too small to be distinguished without a microscope. With increased pressure over time the platey clay minerals may become aligned, with the appearance of fissility or parallel layering. This finely bedded material that splits readily into thin layers is called shale, as distinct from mudstone. The lack of fissility or layering in mudstone may be due either to original texture or to the disruption of layering by burrowing organisms in the sediment prior to lithification. Mud rocks, such as mudstone and shale comprise some 65% of all sedimentary rocks. Mudstone looks like hardened clay and, depending upon circumstances under which it was formed, it may show cracks or fissures, like a sun-baked clay deposit. They can be separated into these categories:
Siltstone - greater than half of the composition is silt-sized particles.
Claystone - greater than half of the composition is clay-sized particles.
Mudstone - hardened mud; a mix of silt and clay sized particles. Mudstone can include: Shale - exhibits lamination or fissility.
Argillite - has undergone low grade metamorphism.