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"Lowest" level position/"jobs".
E.T
Quote-o-matic
in Zocalo v2.0
There was interesting article in one magazine about certain position.
And I mean literally low level.
So does anyone want to guess or do I have to tell more?
And I mean literally low level.
So does anyone want to guess or do I have to tell more?
Comments
Atleast so people seem to think.
I'd say customer though. Because even cashiers despise most customers.
[B]I'd say customer though. Because even cashiers despise most customers. [/B][/QUOTE]
The man tells the truth.
For the most part, I treat customers with neutrality until they do something to make me think favourably/unfavourably of them. More often than not, it's the latter.
If you guys want an entertaining thread pertaining to the trials and tribulations of working in retail, check out this thread I created on UKAN. ;)
[URL=http://forums.ukairsoft.net/showthread.php?s=&threadid=62713]The Retail Rant[/URL]
Regards,
Morden
Is that "low" enough? :D
So like you might guess it's mine... although there's also other things going on there.
[url]http://www.gl.rhbnc.ac.uk/geode/Fennoscandia/Pyhasalmi.html[/url]
[url]http://cupp.oulu.fi/pdf/cupp_infra_012003www.pdf[/url]
[url]http://geothermal.stanford.edu/pdf/SGW/2005/Oye.pdf[/url]
[B]The man tells the truth.
For the most part, I treat customers with neutrality until they do something to make me think favourably/unfavourably of them. More often than not, it's the latter.
If you guys want an entertaining thread pertaining to the trials and tribulations of working in retail, check out this thread I created on UKAN. ;)
[URL=http://forums.ukairsoft.net/showthread.php?s=&threadid=62713]The Retail Rant[/URL]
Regards,
Morden [/B][/QUOTE]
I'm gonna give that url to other cashiers at work... :)
Regards,
Morden
[QUOTE]
Zn (Zinc)
Cu (Copper)
Ore Age: Palaeoproterozoic 1900 Ma
Host Rock Age: Palaeoproterozoic 1930 Ma
[/QUOTE]
Damn that's old! Whew!
:)
[B]I love that Axonometric view... :p
Damn that's old! Whew!:) [/B][/QUOTE]I thought so... because it's same here.
Here's quite nice bedrock map of area:
[url]http://www.gtk.fi/explor/zinc/kettupera.htm[/url]
But before we continue this very interesting conversation...
So here's warning for others... You might want to ignore rest before you get bored to death.;)
And that's not even "old" part.
Only small part of bedrock is younger than 1500 Ma and oldest parts are 3200 Ma old. (although original age of many youngest metamorphic rocks is propably much bigger)
There has been at least two mountain ranges going through Finland's area but those have been eroded away.
In that time old bedrock has been many times crushed, folded, compressed, tilted, weathered.
Also there's only base of those mountain ranges visible now so time has taken quite many kilometers thick layer as toll and only hardest rocks and minerals are left as higher places...
This is what your Rocky Mountains will look two billion years later:
[url]http://koti.mbnet.fi/~tuunaes/temp/PICT3877.JPG[/url]
[url]http://koti.mbnet.fi/~tuunaes/temp/PICT3894.JPG[/url]
Here's more stuff:
[url]http://www.gtk.fi/explor/[/url]
[url]http://www.gsf.fi/info/maps/suomenkp5m300.jpg[/url]
Black lines are BIG faults (if map would have all smaller faults and cracks it would be full of them) and subduction zones.
[B]Here's more stuff:
[url]http://www.gtk.fi/explor/[/url]
[url]http://www.gsf.fi/info/maps/suomenkp5m300.jpg[/url]
Black lines are BIG faults (if map would have all smaller faults and cracks it would be full of them) and subduction zones. [/B][/QUOTE]
This map is interesting, although I don't know the language I can pick out meteorite, kimberlite (diamond bearing zones), gneiss, granite, etc, and other references by the similarities in the words.
I am curious, is KAMBRIKAUDEN a reference to the Cambrian Era or Pre-Cambrian era?
Another thing I'd be really interested in is the Meteor Strike locations indicated by the stars.
[QUOTE]
GENETIC MODEL
Evolution of the area started(?) with felsic magmatism (Na rhyolites) in an extensional continental-margin island-arc setting at about 1930-1920 Ma, and was followed by mafic volcanism (low-K tholeiites of primitive island arc type) and sulphide mineralisation in a rifted marine setting and, soon after, by intermediate(?) calc-alkaline volcanism related to accretion(?) [2,9,13,14], or the mineralisation took place during the early stages of the evulution, possibly related to the felsic volcanism at 1930-1920 Ma [4]. As a whole, the setting is an island-arc environment along the margin of the Archaean Karelian craton [4,13,15].
[/QUOTE]
This of course gives a very nice picture of how things looked in the past... :)
I used to do stock/grocery for a supermarket, and while it wasn't as bad as what the cashiers had to put up with, it could get pretty disgusting at times.
My favorite supermarket find was a chewed up apple (not swallowed...just mechanically digested) mixed with ice cream and some other unknown substance, possibly pure liquid evil, placed neatly behind a box of crackers on the next-to-top shelf and dripping all the way to the floor. I'm assuimg that it was there earlier and that a fellow employee had topped off the aisle with that in plain sight and didn't even bother to clean it up as that was clearly not worth the effort (such things had happened before...).
And then there's my favorite product/packaging method...Condensed juices! Yes, condensed juice...it comes in 12 oz soda-like cans and has an incredibly high sugar content. However, they're typically packaged in a very thin heat-shrink or such plastic which many of the employees repeatedly used their boxcutters to open.
Bad idea. The cans are slightly more thin than those typically found holding soda and upon even remotely grazing the surface, a pinhole leak is formed. what then happens is that if this can is stil in its packaging after being cut, sometimes the plastic would cover the leak and will go unnoticed (which was quote often) right until it was time to take the U-boat of drinks out and put them on the shelves. take the plastic off and all of a sudden you find that the floor--as well as everything else within 15 feet (Especially hard-to-clean products and boxes)--has become incredibly sticky. a closer inspection leads one to find a trail of goo so small that it can be interrupted by your finger without even noticing it was there. end result? A regular sugar coating on the entire juice aisle because on occasion, someone would roll the U-Boat around the aisle with a squirting can...
Gah. Just one story among many. :D (And I only worked there for less than ten weeks!)
[B]This map is interesting, although I don't know the language I can pick out meteorite, kimberlite (diamond bearing zones), gneiss, granite, etc, and other references by the similarities in the words.
I am curious, is KAMBRIKAUDEN a reference to the Cambrian Era or Pre-Cambrian era?[/b][/QUOTE]
Quite many names are almost same as in english, there's just small change in word like granite=graniitti, migmatite=migmatiitti... exept rapakivi which is also its english name.
(vihreäkivi=greenstone seems to be one of the few fully translated names)
Good example how words differ generally is quartzite
[url]http://www.websters-dictionary-online.org/translation/kvartsiitti[/url]
Kauden/kausi in the end of word means era, if there's "esi" in the beginning of word it means same as "pre".
Varhais(/varhainen)=early=paleo, keski=middle=meso, myöhäis(/myöhäinen)=late=neo.
([url=http://www.fossilmall.com/Science/GeologicalTime.htm]this[/url] looks usefull page)
Otherwise words are again quite close to english words.
[url]http://www2.nrm.se/lig/fennmap.html.en[/url]
[url]http://www.igem.ru/igem/petr/int4.htm[/url]
[url]http://www.posiva.fi/raportit/POSIVA-2002-04.pdf[/url]
[QUOTE]Another thing I'd be really interested in is the Meteor Strike locations indicated by the stars.[/QUOTE]Here's good site, author of site is other founder of Keurusselkä crater, or actually it's just highly eroded "root" of crater (or central peak).
[url]http://www.somerikko.net/impacts/fincrat.html[/url]
[url]http://www.geophysics.helsinki.fi/tutkimus/impacts/impacts_finland.shtml[/url] (requires allowing popups in Opera and Firefox, otherwise infopages of craters won't open)
[url]http://www.geophysics.helsinki.fi/tutkimus/impacts/maps.html[/url]
[url]http://www.student.oulu.fi/~jkorteni/space/craters/[/url]
[url]http://www.lpi.usra.edu/meetings/lpsc2004/pdf/1619.pdf[/url]
[url]http://www.lpi.usra.edu/meetings/LPSC98/pdf/1171.pdf[/url]
[url]http://www.lpi.usra.edu/meetings/lpsc2003/pdf/1571.pdf[/url]
[url]http://www.lpi.usra.edu/meetings/largeimpacts2003/pdf/4074.pdf[/url]