The Egyptian Pyramids as the Geophysical Device-Properties and Opportunities

seismo- emissional fields were recorded at lateral sides of pyramids in Dakhshur (“Red” and “Broken”) and in Medume (“Wrong”), for the last one-in the internal chamber also. Registration of seismic noise or their envelopes was conducted with one channel, and the other channel-the electromagnetic signal from the ferrite antenna (electromagnetic emission). The induced seismic emission was investigated under simultaneous recording of envelopes of seismic noise in Dakhshur at top of the small pyramid (near the “Broken”) by two channels (it is anomalous high level). Research of other records have revealed more high-level seismic emission noise inside a pyramid in comparison with an external level, and also coincidence in time of changes of a signal from the ferrite antenna and seismic noise.

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