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July 8, 2011 – How do we do this? The planet’s internal gradient is increasing and this means more chaotic conditions are in store for our planet. Among the most visible of these will include further deterioration of the planet’s magnetic field, the collapse of climate stability and the occurrence of more adverse weather extremes, hypervolcanism, and increased tectonic related earthquakes. Thermal energy is a driving force behind tectonic plate movements and so is magma plumes as I discussed in my book and as science has only recently concluded this week. If we look at the earthquakes occurring at Etna, the increased seismic and volcanic activity under Iceland’s divergent rift, the earthquakes in Southeast Australia, the rapid formation of storms in the Eastern Pacific north of Galapagos, and the 5.3 magnitude earthquake on the Central Mid-Atlantic Ridge- we find two important common denominators in all these events: They are all happening simultaneously and they are all occurring around magma plumes. Increased activity at the magma plume at Eritrea and the subsequent eruption of the Nabro volcano is another indication this process is accelerating. (See African hotspot below)

Increased activity at magma plumes: “If magma levels within the Earth’s crust are precipitously rising due to fluctuations in the thermal gradient- then pressures would be greatest at mantle plumes and the deepest fissures and faults in the earth will become more active. Technically, that’s what we’re beginning to see at agitated seismic fault zones across the planet…shallow plumes of magma are deep fissures in the earth’s surface which would be early flashpoint indicators of expanding uniform magma levels.” -The Extinction Protocol, page 564, 566

Plume activity and magnetic reversal: Some scientists, such as Richard A. Muller, believe that geomagnetic reversals are not spontaneous processes but rather are triggered by external events that directly disrupt the flow in the Earth’s core. Proposals include impact events or internal events such as the arrival of continental slabs carried down into the mantle by the action of plate tectonics at subduction zones or the initiation of new mantle plumes from the core-mantle boundary. –Wikipedia