Telluric Current - Revision history

Lisa at 05:04, 29 December 2018

2018-12-29T05:04:35Z

← Older revision		Revision as of 01:04, 29 December 2018
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	In industrial prospecting activity that uses the telluric current method, electrodes are properly located on the ground to sense the voltage difference between locations caused by the oscillatory telluric currents.It is recognized that a low frequency window (LFW) exists when telluric currents pass through the earth's substrata. In the frequencies of the LFW, the earth acts as a conductor.<ref>[http://en.wikipedia.org/wiki/Telluric_current Telluric Current]</ref>		In industrial prospecting activity that uses the telluric current method, electrodes are properly located on the ground to sense the voltage difference between locations caused by the oscillatory telluric currents.It is recognized that a low frequency window (LFW) exists when telluric currents pass through the earth's substrata. In the frequencies of the LFW, the earth acts as a conductor.<ref>[http://en.wikipedia.org/wiki/Telluric_current Telluric Current]</ref>

			==Daytime vs Nighttime==
			These currents have daytime characteristics wherein the general direction of flow is towards the sun. [[Telluric Current]]s continuously move between the sunlit and shadowed sides of the earth, toward the equator on the side of the earth facing the sun (during the day), and toward the poles on the night side of the planet. When the Telluric current passes through the earth substrata, it generates a low frequency window that acts as conductor for carrier wave frequencies. This is more amplified in strong daylight hours with bright sunshine and no clouds. Sunlight can be directed to power [[AI]] technology which moves in frequency carrier waves with the telluric current towards the equator line. The equator is the area of the planet where the [[NAA]] base themselves in order to harvest vast amounts of energy gathered there in daylight hours. We will notice the artificial frequencies are much stronger during the day when there is strong sunshine (bright light and radiant heat), rather than at night.

			During this phase, [[AI]] technology is being used to take over the lower three dimensions and their spectrums of frequency that exist as telluric (Earth) current. This means that in the lowest frequency dimension, the things that are manifesting in matter, whether realities or bodies, will be synthetic and created from an AI mind. Anything that is manifested from artificial intelligence technology, such as synthetic bodies, are dead energy. This type of body cannot hold God spirit in its cells.

			At this time, as an awakened spiritual being, it is more important than ever to command your personal space, and to dedicate your life force completely to your spiritual development and to serve organic living consciousness. To do so is to maintain sovereignty by taking personal responsibility to play by your own rules in the consciousness structure that is governed by your highest power in [[God]] Spirit.<ref>[https://energeticsynthesis.com/index.php/resource-tools/news-shift-timelines/2705-separation-of-worlds Separation of worlds]</ref>


	==References==		==References==

Charlotte at 14:15, 11 September 2015

2015-09-11T14:15:22Z

← Older revision		Revision as of 10:15, 11 September 2015
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	Both telluric and magnetotelluric methods are used for exploring the structure beneath the Earth's surface (such as in industrial prospecting). For mineral exploration the targets are any subsurface structure with a distinguishable resistance in comparison to its surroundings. Uses include geothermal exploration, mining exploration,petroleum exploration, mapping of fault zones, ground water exploration and monitoring, investigation of magma chambers, and investigation of boundaries of tectonic plates. earth batteries tap a useful low voltage current from Telluric currents, and were used for telegraph systems as far back as the 1840s.		Both telluric and magnetotelluric methods are used for exploring the structure beneath the Earth's surface (such as in industrial prospecting). For mineral exploration the targets are any subsurface structure with a distinguishable resistance in comparison to its surroundings. Uses include geothermal exploration, mining exploration,petroleum exploration, mapping of fault zones, ground water exploration and monitoring, investigation of magma chambers, and investigation of boundaries of tectonic plates. earth batteries tap a useful low voltage current from Telluric currents, and were used for telegraph systems as far back as the 1840s.

	In industrial prospecting activity that uses the telluric current method, electrodes are properly located on the ground to sense the voltage difference between locations caused by the oscillatory telluric currents.It is recognized that a low frequency window (LFW) exists when telluric currents pass through the earth's substrata. In the frequencies of the LFW, the earth acts as a conductor.<ref>[http://en.wikipedia.org/wiki/Telluric_current]</ref>		In industrial prospecting activity that uses the telluric current method, electrodes are properly located on the ground to sense the voltage difference between locations caused by the oscillatory telluric currents.It is recognized that a low frequency window (LFW) exists when telluric currents pass through the earth's substrata. In the frequencies of the LFW, the earth acts as a conductor.<ref>[http://en.wikipedia.org/wiki/Telluric_current Telluric Current]</ref>

	==References==		==References==

Lisa at 03:30, 27 April 2015

2015-04-27T03:30:29Z

← Older revision		Revision as of 23:30, 26 April 2015
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	A telluric current or Earth current, is an electric current which moves underground or through the sea. Telluric currents result from both natural causes and human activity, and the discrete currents interact in a complex pattern. The currents are extremely low frequency and travel over large areas at or near the surface of the Earth.		A telluric current or Earth current, is an electric current which moves underground or through the sea. Telluric currents result from both natural causes and human activity, and the discrete currents interact in a complex pattern. The currents are extremely low frequency and travel over large areas at or near the surface of the Earth. Telluric current runs in 1D-2D-3D.

	==Description==		==Description==

Lisa: /* Description */

2015-04-27T03:27:03Z

Description

← Older revision		Revision as of 23:27, 26 April 2015
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	==Description==		==Description==
	Telluric currents are phenomena observed in the Earth's crust and mantle. In September 1862, an experiment to specifically address Earth currents was carried out in the Munich Alps (Lamont, 1862). The currents are primarily geomagnetically induced currents, which are induced by changes in the outer part of the Earth's magnetic field, which are usually caused by interactions between the solar wind and the magnetosphere or solar radiation effects on the ionosphere. Telluric currents flow in the surface layers of the earth. The electric potential on the Earth's surface can be measured at different points, enabling the calculation of the magnitudes and directions of the telluric currents and hence the Earth's conductance. '''These currents are known to have diurnal characteristics wherein the general direction of flow is towards the sun. Telluric currents continuously move between the sunlit and shadowed sides of the earth, toward the equator on the side of the earth facing the sun (that is, during the day), and toward the poles on the night side of the planet.'''		Telluric currents are phenomena observed in the Earth's crust and mantle. In September 1862, an experiment to specifically address Earth currents was carried out in the Munich Alps (Lamont, 1862). The currents are primarily geomagnetically induced currents, which are induced by changes in the outer part of the Earth's magnetic field, which are usually caused by interactions between the solar wind and the magnetosphere or solar radiation effects on the ionosphere. Telluric currents flow in the surface layers of the earth. The electric potential on the Earth's surface can be measured at different points, enabling the calculation of the magnitudes and directions of the telluric currents and hence the Earth's conductance.

			'''These currents are known to have diurnal characteristics wherein the general direction of flow is towards the sun. Telluric currents continuously move between the sunlit and shadowed sides of the earth, toward the equator on the side of the earth facing the sun (that is, during the day), and toward the poles on the night side of the planet.'''

	Both telluric and magnetotelluric methods are used for exploring the structure beneath the Earth's surface (such as in industrial prospecting). For mineral exploration the targets are any subsurface structure with a distinguishable resistance in comparison to its surroundings. Uses include geothermal exploration, mining exploration,petroleum exploration, mapping of fault zones, ground water exploration and monitoring, investigation of magma chambers, and investigation of boundaries of tectonic plates. earth batteries tap a useful low voltage current from Telluric currents, and were used for telegraph systems as far back as the 1840s.		Both telluric and magnetotelluric methods are used for exploring the structure beneath the Earth's surface (such as in industrial prospecting). For mineral exploration the targets are any subsurface structure with a distinguishable resistance in comparison to its surroundings. Uses include geothermal exploration, mining exploration,petroleum exploration, mapping of fault zones, ground water exploration and monitoring, investigation of magma chambers, and investigation of boundaries of tectonic plates. earth batteries tap a useful low voltage current from Telluric currents, and were used for telegraph systems as far back as the 1840s.

Lisa: /* Description */

2015-04-27T03:26:46Z

Description

← Older revision		Revision as of 23:26, 26 April 2015
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	==Description==		==Description==
	Telluric currents are phenomena observed in the Earth's crust and mantle. In September 1862, an experiment to specifically address Earth currents was carried out in the Munich Alps (Lamont, 1862).~~[2]~~ The currents are primarily geomagnetically induced currents, which are induced by changes in the outer part of the Earth's magnetic field, which are usually caused by interactions between the solar wind and the magnetosphere or solar radiation effects on the ionosphere. Telluric currents flow in the surface layers of the earth. The electric potential on the Earth's surface can be measured at different points, enabling the calculation of the magnitudes and directions of the telluric currents and hence the Earth's conductance. T'''~~hese~~ currents are known to have diurnal characteristics wherein the general direction of flow is towards the sun.~~[3][4]~~ Telluric currents continuously move between the sunlit and shadowed sides of the earth, toward the equator on the side of the earth facing the sun (that is, during the day), and toward the poles on the night side of the planet.'''		Telluric currents are phenomena observed in the Earth's crust and mantle. In September 1862, an experiment to specifically address Earth currents was carried out in the Munich Alps (Lamont, 1862). The currents are primarily geomagnetically induced currents, which are induced by changes in the outer part of the Earth's magnetic field, which are usually caused by interactions between the solar wind and the magnetosphere or solar radiation effects on the ionosphere. Telluric currents flow in the surface layers of the earth. The electric potential on the Earth's surface can be measured at different points, enabling the calculation of the magnitudes and directions of the telluric currents and hence the Earth's conductance. '''These currents are known to have diurnal characteristics wherein the general direction of flow is towards the sun. Telluric currents continuously move between the sunlit and shadowed sides of the earth, toward the equator on the side of the earth facing the sun (that is, during the day), and toward the poles on the night side of the planet.'''

	Both telluric and magnetotelluric methods are used for exploring the structure beneath the Earth's surface (such as in industrial prospecting). For mineral exploration the targets are any subsurface structure with a distinguishable resistance in comparison to its surroundings. Uses include geothermal exploration, mining exploration,petroleum exploration, mapping of fault zones, ground water exploration and monitoring, investigation of magma chambers, and investigation of boundaries of tectonic plates. earth batteries tap a useful low voltage current from Telluric currents, and were used for telegraph systems as far back as the 1840s.		Both telluric and magnetotelluric methods are used for exploring the structure beneath the Earth's surface (such as in industrial prospecting). For mineral exploration the targets are any subsurface structure with a distinguishable resistance in comparison to its surroundings. Uses include geothermal exploration, mining exploration,petroleum exploration, mapping of fault zones, ground water exploration and monitoring, investigation of magma chambers, and investigation of boundaries of tectonic plates. earth batteries tap a useful low voltage current from Telluric currents, and were used for telegraph systems as far back as the 1840s.

Lisa: /* See Also */

2015-04-27T03:26:11Z

Lisa: /* Description */

2015-04-27T03:25:57Z

Description

← Older revision		Revision as of 23:25, 26 April 2015
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	==Description==		==Description==
	Telluric currents are phenomena observed in the Earth's crust and mantle. In September 1862, an experiment to specifically address Earth currents was carried out in the Munich Alps (Lamont, 1862).[2] The currents are primarily geomagnetically induced currents, which are induced by changes in the outer part of the Earth's magnetic field, which are usually caused by interactions between the solar wind and the magnetosphere or solar radiation effects on the ionosphere. Telluric currents flow in the surface layers of the earth. The electric potential on the Earth's surface can be measured at different points, enabling the calculation of the magnitudes and directions of the telluric currents and hence the Earth's conductance. T'''hese currents are known to have diurnal characteristics wherein the general direction of flow is towards the sun.[3][4] Telluric currents continuously move between the sunlit and shadowed sides of the earth, toward the equator on the side of the earth facing the sun (that is, during the day), and toward the poles on the night side of the planet.'''		Telluric currents are phenomena observed in the Earth's crust and mantle. In September 1862, an experiment to specifically address Earth currents was carried out in the Munich Alps (Lamont, 1862).[2] The currents are primarily geomagnetically induced currents, which are induced by changes in the outer part of the Earth's magnetic field, which are usually caused by interactions between the solar wind and the magnetosphere or solar radiation effects on the ionosphere. Telluric currents flow in the surface layers of the earth. The electric potential on the Earth's surface can be measured at different points, enabling the calculation of the magnitudes and directions of the telluric currents and hence the Earth's conductance. T'''hese currents are known to have diurnal characteristics wherein the general direction of flow is towards the sun.[3][4] Telluric currents continuously move between the sunlit and shadowed sides of the earth, toward the equator on the side of the earth facing the sun (that is, during the day), and toward the poles on the night side of the planet.'''

	Both telluric and magnetotelluric methods are used for exploring the structure beneath the Earth's surface (such as in industrial prospecting). For mineral exploration the targets are any subsurface structure with a distinguishable resistance in comparison to its surroundings. Uses include geothermal exploration, mining exploration,petroleum exploration, mapping of fault zones, ground water exploration and monitoring, investigation of magma chambers, and investigation of boundaries of tectonic plates. earth batteries tap a useful low voltage current from Telluric currents, and were used for telegraph systems as far back as the 1840s.		Both telluric and magnetotelluric methods are used for exploring the structure beneath the Earth's surface (such as in industrial prospecting). For mineral exploration the targets are any subsurface structure with a distinguishable resistance in comparison to its surroundings. Uses include geothermal exploration, mining exploration,petroleum exploration, mapping of fault zones, ground water exploration and monitoring, investigation of magma chambers, and investigation of boundaries of tectonic plates. earth batteries tap a useful low voltage current from Telluric currents, and were used for telegraph systems as far back as the 1840s.

	In industrial prospecting activity that uses the telluric current method, electrodes are properly located on the ground to sense the voltage difference between locations caused by the oscillatory telluric currents.It is recognized that a low frequency window (LFW) exists when telluric currents pass through the earth's substrata. In the frequencies of the LFW, the earth acts as a conductor.<ref>[http://en.wikipedia.org/wiki/Telluric_current]</ref>		In industrial prospecting activity that uses the telluric current method, electrodes are properly located on the ground to sense the voltage difference between locations caused by the oscillatory telluric currents.It is recognized that a low frequency window (LFW) exists when telluric currents pass through the earth's substrata. In the frequencies of the LFW, the earth acts as a conductor.<ref>[http://en.wikipedia.org/wiki/Telluric_current]</ref>


	==References==		==References==

Lisa at 03:25, 27 April 2015

2015-04-27T03:25:47Z

← Older revision		Revision as of 23:25, 26 April 2015
Line 1:		Line 1:
	A telluric current or Earth current, is an electric current which moves underground or through the sea. Telluric currents result from both natural causes and human activity, and the discrete currents interact in a complex pattern. The currents are extremely low frequency and travel over large areas at or near the surface of the Earth.		A telluric current or Earth current, is an electric current which moves underground or through the sea. Telluric currents result from both natural causes and human activity, and the discrete currents interact in a complex pattern. The currents are extremely low frequency and travel over large areas at or near the surface of the Earth.


	==Description==		==Description==

Lisa: Created page with "A telluric current or Earth current, is an electric current which moves underground or through the sea. Telluric currents result from both natural causes and human activity, a..."

2015-04-27T03:25:37Z

Created page with "A telluric current or Earth current, is an electric current which moves underground or through the sea. Telluric currents result from both natural causes and human activity, a..."

New page

A telluric current or Earth current, is an electric current which moves underground or through the sea. Telluric currents result from both natural causes and human activity, and the discrete currents interact in a complex pattern. The currents are extremely low frequency and travel over large areas at or near the surface of the Earth.

==Description==
Telluric currents are phenomena observed in the Earth's crust and mantle. In September 1862, an experiment to specifically address Earth currents was carried out in the Munich Alps (Lamont, 1862).[2] The currents are primarily geomagnetically induced currents, which are induced by changes in the outer part of the Earth's magnetic field, which are usually caused by interactions between the solar wind and the magnetosphere or solar radiation effects on the ionosphere. Telluric currents flow in the surface layers of the earth. The electric potential on the Earth's surface can be measured at different points, enabling the calculation of the magnitudes and directions of the telluric currents and hence the Earth's conductance. T'''hese currents are known to have diurnal characteristics wherein the general direction of flow is towards the sun.[3][4] Telluric currents continuously move between the sunlit and shadowed sides of the earth, toward the equator on the side of the earth facing the sun (that is, during the day), and toward the poles on the night side of the planet.'''
Both telluric and magnetotelluric methods are used for exploring the structure beneath the Earth's surface (such as in industrial prospecting). For mineral exploration the targets are any subsurface structure with a distinguishable resistance in comparison to its surroundings. Uses include geothermal exploration, mining exploration,petroleum exploration, mapping of fault zones, ground water exploration and monitoring, investigation of magma chambers, and investigation of boundaries of tectonic plates. earth batteries tap a useful low voltage current from Telluric currents, and were used for telegraph systems as far back as the 1840s.

In industrial prospecting activity that uses the telluric current method, electrodes are properly located on the ground to sense the voltage difference between locations caused by the oscillatory telluric currents.It is recognized that a low frequency window (LFW) exists when telluric currents pass through the earth's substrata. In the frequencies of the LFW, the earth acts as a conductor.<ref>[http://en.wikipedia.org/wiki/Telluric_current]</ref>

==References==

<references/>

==See Also==

[[Ley Lines]]

[[Doradic Current]]

[[Category: Ascension]]

[[Category: Newsletter]]

← Older revision		Revision as of 23:26, 26 April 2015
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	==See Also==		==See Also==


	[[Ley Lines]]		[[Ley Lines]]


	[[Doradic Current]]		[[Doradic Current]]





	[[Category: Ascension]]		[[Category: Ascension]]


	~~[[Category: Newsletter]]~~