Extending Milankovitch - Celestial Cycles and Magnetism: 05/27/17

5/27/2017

M 2.5 - WESTERN AUSTRALIA

By: Gordon Rutherford

M 2.5 - WESTERN AUSTRALIA
Magnitude M 2.5
Region WESTERN AUSTRALIA
Date time 2017-05-27 11:33:31.0 UTC
Location 30.72 S ; 121.51 E

Depth 2 km

Drivers:
Jupiter at Geocentric Opposition to Neptune at Median
- NEPTUNE AT 120 DEGREES FROM THE MOON

NOAA Geomagnetic Polarity

NASA JPL Data

Epicenter Skyview

Antipodes

Antipodal Skyview

M 4.2 - 121km S of Akureyri, Iceland

By: Gordon Rutherford
M 4.2 - 121km S of Akureyri, Iceland
UTC Time = 2017-05-27 09:36:23
Magnitude = 4.2m
Location = 64.597°N 17.871°W
Depth = 10.0 km.

Drivers:
Neptune at 120 degrees from the Moon (Para-Magnetic)- during Lunar Conjunction w/ Mars.

NOTE:
Mars in the Negative Rotating Solar Magnetic Field(Para-Magnetic)

Epicenter SKYVIEW

NASA JPL Data

NOAA Geomagnetic Polarity

ICELAND Recorded this quake

Epicenter DISTANCE from the Volcano

About the Volcano:Bárðarbunga is an Icelandic stratovolcano located under the ice cap of Vatnajökull glacier, rising to 2,009 metres above sea level, making it the second highest mountain in Iceland, just about 101 metres lower than Hvannadalshnjúkur..Bárðarbunga is a large and powerful stratovolcano, it is also Iceland's largest volcanic system, considered to be close to 200 kilometres long and up to 25 kilometres wide.The Bárðarbunga caldera is about 70 square kilometres, up to 10 kilometres wide and about 700 metres deep. The surrounding edges rise up to 1850 metres but the base is on average close to 1100 metres. The volcano is covered in ice, hiding the glacier-filled crater..Bárðarbunga was a little known volcano in Iceland because of its remote location, far away from settlement, and infrequent eruptions. Bárðarbunga's highest point is 2,009 metres high and is the second highest mountain in Iceland..Many tephra layers originally thought to belong to other volcanoes have in the recent studies proved to be from Bárðarbunga. The Gjálp fissure eruption in 1996 revealed that an interaction may exist between Bárðarbunga and Grímsvötn. A strong earthquake in Bárðarbunga, about 5 on the Richter scale, is believed to have started the eruption in Gjálp.