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Bassett and Grylls exotic semiconductor field trip: Difference between revisions

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Created page with "A morning trip to Bassett and Grylls mine in Wendron. This is a very different location to the copper mines I visited near Porthtowan on the first trip as it was a tin mine. It's actually one of the mines that apparently wasn't completely exhausted and was shut due to financial mismanagement. Now it is well overgrown but still with quite of a lot of visible infrastructure. This was trip was initiated by a discovery..."
 
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A morning trip to Bassett and Grylls mine in Wendron. This is a very different location to the [[Porthtowan/Nangiles exotic semiconductor field trip|copper mines I visited near Porthtowan on the first trip]] as it was a tin mine. It's actually one of the mines that apparently wasn't completely exhausted and was shut due to financial mismanagement. Now it is well overgrown but still with quite of a lot of visible infrastructure.
[[File:Bassett_Grylls_main.jpg]]


This was trip was initiated by a discovery that specularite [[hematite]] seemed to conduct electricity indicating that it may be a semiconductor.
The second search for exotic semiconductors was at [https://www.mindat.org/loc-224573.html Bassett and Grylls mine in Wendron]. This is a very different location to the [[Porthtowan/Nangiles exotic semiconductor field trip|Porthtowan trip]] as it was a tin, rather than copper mine. It is well overgrown but still with quite of a lot of visible infrastructure from ore processing activities that went on here.
 
This location was initiated by a discovery that [[hematite]] I'd found from here previously seemed to have a low resistance in contrast to hematite from elsewhere, so I wanted to see if I could find some more usable quantities for sound making. It's also a site rich in pale brown [[cassiterite]].

Revision as of 07:35, 22 July 2026

The second search for exotic semiconductors was at Bassett and Grylls mine in Wendron. This is a very different location to the Porthtowan trip as it was a tin, rather than copper mine. It is well overgrown but still with quite of a lot of visible infrastructure from ore processing activities that went on here.

This location was initiated by a discovery that hematite I'd found from here previously seemed to have a low resistance in contrast to hematite from elsewhere, so I wanted to see if I could find some more usable quantities for sound making. It's also a site rich in pale brown cassiterite.