Fig 2 - uploaded by Yuriy Bogdanov
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The geopolariton radiation intensity map on Galindez Island glacier. The contours show glacier borders. The white lines on the left -arc-like failures. On the left there is a fragment of watered part of rock surface on depth of 22m from the glacier surface (shown in white).
Source publication
This paper discusses the problems of the natural Earth pulse electromagnetic radiation occurrence and it's usage for the Earth interior exploration. The main attention is paid to radiation of the radiowave diapason (from ~1 kHz to ~1 MHz) which sources is located inside the Earth lithosphere. The nonlinear aspect of mechanic-electromagnetic interac...
Contexts in source publication
Context 1
... results are given as geopolariton radiation intensity maps ( fig.2) and geological section by A'-A line ( fig.3, 4). ...
Context 2
... results are given as geopolariton radiation intensity maps ( fig.2) and geological section by A'-A line ( fig.3, 4). The map ( fig.2) shows structure failures of submeredional extent and sublatitude arc-like failures that may be caused by glacier movement. ...
Context 3
... most probable water source is the ice melting. From the glacier bed it flows to the sea. But it is also possible that the water weeps from the sea along crumbly border of geological layers. The water saturated soil and correspondingly lowered stress areas are shown as dark spots on the map ( fig.2. right). Here: 1-glacier cover, 2,3,4-lithologic borders, 5-tectonic faults, 6 -glacier faults, 7,8-firn, 9-watersaturated ...
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This paper discusses the problems of the natural Earth pulse electromagnetic radiation occurrence and it's usage for the Earth interior exploration. The main attention is paid to radiation of the radiowave diapason (from ~1 kHz to ~1 MHz) which sources is located inside the Earth lithosphere. The nonlinear aspect of mechanic – electromagnetic inter...
