WHAT IS HAPPENING AT WHITE ISLAND VOLCANO??? New Zealand/Kermadec & South Pacific QUAKE/VOLCANO WATCH

Whoa, I dreamed about all of this when i was napping around 11 pm est. Had no idea anything was actually going on over there. No proof to show anyone but I'm pretty weirded out right now.

Glad you are OK T !!!

John Seach@johnseach

18h
#Maroa volcano, New Zealand. Magnitude 6.3 earthquake hit 16 km north of Orakei Korako geothermal area on 8 Dec 2012.
[link to mobile.twitter.com (secure)]

Glad to see you are ok!
Been waiting to see you on!

Be safe sister!

love & light~~~~~~

Thank's Tauranga hang on, we nead you!!!

hi AC

there are lots of people all over the world having the same doom dreams as each other

including lots of children

there must be a reason for this

either it is collective unconscious awareness on a spiritual level of what is to come to pass soon

or it is some sort of collective programming that is being implemented by tptb, via our dreams..

i am unsure which it is, but i do think that tptb are very likely using the whole 2012 doom thing to their advantage, to herd up the sheeple into frightened submission

the 2012 thing is much bigger than just the mayan prophesy which i believe was prophesicing massive changes to our sun and therefore our solar system, etc

but it wasnt just the mayans who went to immense trouble to leave a message to humanity at this time, other cultures also tried to leave timeless warnings for us to recognise now

hiya OG xxxx

neat to see you, hope all is well with you and yours

i think of you very often

yep, i am great, sis

hiya luis

neat to hear from you, too

thanks for this, i am looking forward to reading what john seach has to say

volcanic developments are happening here very quickly now

thank you also for your constant support of this important thread, brother xxx

The way i see it is if ppl are having doom dreams it means they are ready when shtf and there seems to be a lot of people having them

My friend i want just to say i'm praying for you and all New Zealand people!

hiya ozark

and its neat to see you here too

sorry i have been a bit on and off here, but life gets busy for me sometimes and i have to do my own stuff

boy things are amping up here with our volcanoes...

i am as safe as one can be, given my proximity to the volcanoes, and i know that we are looked after from above

much love to you, sister xxx

thank you luis, your caring and prayers mean a lot to us here, you are a dear person xxx

and guess what, i need YOU here on this thread too!!!

hiya nibiflex

you have a good point there...

those of us who are mentally prepared for whatever is now close at hand, will cope with it with strength, and therefore be able to help others who are panicking when the time comes

I just try my best!

your job makes mine look small, brother..

i am watching/covering only one part of the world, you are keepng tabs on the whole worlds' volcanoes!

luis

i am concerned about rarotonga, that their volcano is awakening too:

4.7 01:26:31 Sun 09 Dec 2012 Depth: 15.8 km

Hehehe i even got a plane on standby so wether its now or 30 yrs from now im ready for anything ,

The island of Rarotonga in the southern Pacific is the emergent summit of a Pliocene - Pleistocene volcanic complex built by effusive and pyroclastic eruptions of mainly mafic magma. Petrographically the basaltic rock types are ankaramite and basalt, which range in chemical composition from alkali basalt to nephelinite. Phenocryst assemblages suggest two igneous series, one with a relatively simple equilibrium assemblage of olivine, titanian augite and magnetite, and one with olivine, diopside-augite and titanian augite in which the phenocrysts show disequilibrium textures. These variations reflect fractionation, assimilation, and recharge processes in the upper part of the magmatic system that produced the volcano. The final stages of volcanism at Rarotonga were pyroclastic eruptions of phonolites and effusive eruptions of foidal phonolites, both representing late stage fractionation products. Detailed mapping, together with geochemical work, has prompted a revision of the stratigraphy of the island based on the concept of a single cycle of magmatic activity rather than the Hawaiian style multi-phase evolution favoured by earlier workers. [link to researchspace.auckland.ac.nz (secure)]

lols

wow man, you really are prepared!!

good on you

what do you think we are seeing on the rarotonga graphs?

and what do you think about what looks like regular volcanic activity at kermadec (btw it looks steamy there again today, which it often does, this steaminess showing on the webcam seems to correlate to the volcanic episodes that show on the graphs very frequently)

are the quakes after that quake yesterday STILL deep?

Strong and deep earthquake M 6.3 struck North Island of New Zealand

[link to thewatchers.adorraeli.com]

A strong and deep 6.3 magnitude earthquake struck North Island of New Zealand on December 7, 2012 at 18:19 UTC. Epicenter was located 18 km (11 miles) SE of Tokoroa, New Zealand, 27 km (16 miles) SW of Rotorua, New Zealand and 39 km (24 miles) N of Taupo, New Zealand at coordinates 38.334°S, 176.044°E. Recorded depth by USGS was 167.2 km (103.9 miles). Both USGS and EMSC reported magnitude 6.3. EMSC reported depth of 146 km.

Geonet / GNS Science reports a Magnitude of 5.8 at a depth of 175 km.

GDACS reported that this earthquake can have a low humanitarian impact based on the Magnitude and the affected population and their vulnerability. 550 000 people are living within 100 km.

Magnitude 6.3
Date-Time
Friday, December 07, 2012 at 18:19:08 UTC
Saturday, December 08, 2012 at 07:19:08 AM at epicenter
Location 38.334°S, 176.044°E
Depth 167.2 km (103.9 miles)
Region NORTH ISLAND OF NEW ZEALAND
Distances 18 km (11 miles) SE of Tokoroa, New Zealand
27 km (16 miles) SW of Rotorua, New Zealand
39 km (24 miles) N of Taupo, New Zealand
72 km (44 miles) S of Tauranga, New Zealand
Location Uncertainty horizontal +/- 13.2 km (8.2 miles); depth +/- 8 km (5.0 miles)
Parameters NST=173, Nph=181, Dmin=93.5 km, Rmss=1.71 sec, Gp= 47°,
M-type=teleseismic moment magnitude (Mw), Version=8
Source
Magnitude: USGS NEIC (WDCS-D)
Location: USGS NEIC (WDCS-D)
Event ID usc000e5z5

Tectonic summary by USGS

Seismotectonics of the Eastern Margin of the Australia Plate

The eastern margin of the Australia plate is one of the most seismically active areas of the world due to high rates of convergence between the Australia and Pacific plates. In the region of New Zealand, the 3000 km long Australia-Pacific plate boundary extends from south of Macquarie Island to the southern Kermadec Island chain. It includes an oceanic transform (the Macquarie Ridge), two oppositely verging subduction zones (Puysegur and Hikurangi), and a transpressive continental transform, the Alpine Fault through South Island, New Zealand.

Since 1900 there have been 15 M7.5+ earthquakes recorded near New Zealand. Nine of these, and the four largest, occurred along or near the Macquarie Ridge, including the 1989 M8.2 event on the ridge itself, and the 2004 M8.1 event 200 km to the west of the plate boundary, reflecting intraplate deformation. The largest recorded earthquake in New Zealand itself was the 1931 M7.8 Hawke’s Bay earthquake, which killed 256 people. The last M7.5+ earthquake along the Alpine Fault was 170 years ago; studies of the faults’ strain accumulation suggest that similar events are likely to occur again.

North of New Zealand, the Australia-Pacific boundary stretches east of Tonga and Fiji to 250 km south of Samoa. For 2,200 km the trench is approximately linear, and includes two segments where old (>120 Myr) Pacific oceanic lithosphere rapidly subducts westward (Kermadec and Tonga). At the northern end of the Tonga trench, the boundary curves sharply westward and changes along a 700 km-long segment from trench-normal subduction, to oblique subduction, to a left lateral transform-like structure. More information on regional seismicity and tectonics

Featured image: EMSC + Google Earth
[link to thewatchers.adorraeli.com]

map:December 7, 2012 – M 6.3 North Island of New Zealand
[link to thewatchers.adorraeli.com]

that is a good question, AC

and yes the current quakes are mostly deep, which is not quite normal, normally most of our quakes are very shallow, hmmm...

here is where you can see our quakes as they are happening
[link to www.geonet.org.nz]

thank you for bringing this to our attention

IMO we see clear rise of activity in all Pacific "fire ring" region, but I'm proposing the main events we can expect more likely again in Japan's, Kamchatka and Aleutian-Alaska neighborhoods

That's where I'm expecting to see them too we are having a blizzard I just got home snowing so hard it was like driving in an asteroid game game high beams make it worse. Woke up the other night dreaming about Yellowstone going off it was bizarre. to all. You are doing an amazing job with this thread it's awesome

Something's going on around Mt. Redoubt
3.2 32km NW of Anchor Point, Alaska 2012-12-09 07:28:56 60.006°N 152.182°W 46.1
3.4 62km SSW of Old Iliamna, Alaska 2012-12-09 02:28:28 59.205°N 155.151°W 199.6
[link to earthquake.usgs.gov]
Felt this heard rumbling
3.0 33km WSW of Big Lake, Alaska 2012-12-09 08:15:52 61.402°N 150.524°W 33.9
Here's 4 more all around Mt Redoubt
11:27 PM AKST Saturday December 8th, 2012 1.91 ML in the Cook Inlet region of Alaska
11:15 PM AKST Saturday December 8th, 2012 2.96 ML in the Cook Inlet region of Alaska
10:50 PM AKST Saturday December 8th, 2012 3.00 ML in the Unimak Island region of Alaska
10:28 PM AKST Saturday December 8th, 2012 3.20 ML in the Cook Inlet region of Alaska
[link to www.aeic.alaska.edu]
Look at the webicorder!

[link to www.avo.alaska.edu]

Last Edited by AKObserver on 12/09/2012 03:41 AM

Weak seismic unrest continued at Ruapehu volcano in New Zealand, but has been lower compared to earlier in November. [link to www.volcanodiscovery.com]

hiya sis

im glad you found the russian AC's post, i was going to refer them to your research

thank you for your support, AK it means a lot to me xxx