摘要
The mechanism of “Bing-Bang-Channeling-Cut” was proposed to reduce the volcanic energy (“Bing”) from the Galapagos Hot Spot (GHS) for the mitigation of Ecuadorian earthquake impact (“Bang”). The lag time between the volcanic eruptions in the GHS and Ecuadorian earthquake was probably caused by the undersea seamounts of the Carnegie Ridge (CAR) (“Channeling”). Experimental results from the water reservoir showed that the lag time decreased when increasing the number of drilled holes (“Cut”) in the bottom of reservoir. The present study showed that there was an additional vector initiating the Ecuadorian earthquake from the volcanic eruption in the GHS through the CAR. It was concluded that the harmful effects of Ecuadorian earthquakes could be mitigated by releasing the volcanic energy through the enlarged exit diameters in Holes of Site 1239 (A, B, C) with the presently productive upwelling chlorophyll system at the northeastern CAR.
The mechanism of “Bing-Bang-Channeling-Cut” was proposed to reduce the volcanic energy (“Bing”) from the Galapagos Hot Spot (GHS) for the mitigation of Ecuadorian earthquake impact (“Bang”). The lag time between the volcanic eruptions in the GHS and Ecuadorian earthquake was probably caused by the undersea seamounts of the Carnegie Ridge (CAR) (“Channeling”). Experimental results from the water reservoir showed that the lag time decreased when increasing the number of drilled holes (“Cut”) in the bottom of reservoir. The present study showed that there was an additional vector initiating the Ecuadorian earthquake from the volcanic eruption in the GHS through the CAR. It was concluded that the harmful effects of Ecuadorian earthquakes could be mitigated by releasing the volcanic energy through the enlarged exit diameters in Holes of Site 1239 (A, B, C) with the presently productive upwelling chlorophyll system at the northeastern CAR.
