SI
SI
discoversearch

We've detected that you're using an ad content blocking browser plug-in or feature. Ads provide a critical source of revenue to the continued operation of Silicon Investor.  We ask that you disable ad blocking while on Silicon Investor in the best interests of our community.  If you are not using an ad blocker but are still receiving this message, make sure your browser's tracking protection is set to the 'standard' level.
Gold/Mining/Energy : BET YOUR ASSAY - Mining Terms Explained -- Ignore unavailable to you. Want to Upgrade?


To: Walt who wrote (386)4/2/1998 11:04:00 PM
From: Ed Pakstas  Respond to of 463
 
Thanks Walt... It came up in this NR:

Message 3937719

I wasn't sure what it was... Why the 'ell don't they just call it magnetite or pyrhotite... Those two I know... Learned all about it when I took that Gold Pannin' course up in Gr. Prairie back in '80... Found quite a bit of it (magnetite) in the Peace over south of Valleyview way... Unfortunately that's all I found...:-( ...ed



To: Walt who wrote (386)4/3/1998 11:51:00 AM
From: 1king  Read Replies (2) | Respond to of 463
 
Walt,

The difference between the two would be wavelength or frequency of the magnetic anomalies. The size and shape of the anomalies.

Magnetic sands have very short wavelengths which indicate a very shallow depth to source and very limited depth extent. In a survey they appear as spikes which may or may not form a coherent pattern. They almost always coincide with the local topography (a dead giveaway)

"True" geological features have varying wavelengths (always longer) indicating some depth to source and some measurable depth extent.

The two are very easily distinguished and separated.

1King