I recently finished doing two mag grids with a lot of remanent magnetic
responses.  Both of these grids were located on mountain peaks with highly
magnetic Precambrian rocks.  There wasn�t any real pattern to the remanent
responses and they were of various sizes (ranging from 5 to 50 meter
diameters).  The overall magnetic field varied from about 30,000 to 70,000
gammas with the background at about 56,000.

At first, I thought the remanence was probably induced by lightning strikes.
After finishing the survey, I compared the local grid responses and
locations to a high resolution helicopter magnetic survey that was flown
earlier over the same area.  Both of the grids are located near a major
contact and there did seem to be an overall motley appearance (lots of small
bull�s eye highs and lows) in the helicopter magnetic data near the contact
regardless of terrain elevation.  Therefore I concluded the remanent
responses in the ground mag were probably caused by hydrothermal alternation
from metamorphic activity near the contact rather than by lightning strikes.

This project forced me to realize how little I know about lightning strikes
and remanent magnetism.  How strong are the responses (both in changes to
the magnetic field and aerial extent) likely to be?  I am curious to know if
there is anyone on this list who has had experience with this or knows of
any published works regarding lightning strikes and magnetism.

Sincerely,

Clark Jorgensen

Big Sky Geophysics
P.O. Box 353
Bozeman, MT 59771
USA
(406) 587-6330 phone
(406) 587-6394 fax
[EMAIL PROTECTED]

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