I found this rock on the edges of a known Drumlin in North East England. It looks to be a fragment from a larger piece. It attracts a magnet strongly, it weighs 150 grams. It has vesicular holes (on what would have been the surface) with round beads of metal inside some of them. It looks crystalline in structure and has small shiny inclusions. It also looks like it has a layer section. All very confusing. Any idea what it could be?
closed as off-topic by Gimelist, trond hansen, user12525, Fred, Peter Jansson Aug 9 at 13:09
This question appears to be off-topic. The users who voted to close gave this specific reason:
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This texture is not Widmanstätten, which only becomes visible after polishing and etching. And it doesn't like like it anyway. Meteorites also don't have bubbles (at least not that big and rounded). Therefore, this is not a meteorite.
It also looks very much like a komatiite, but these rocks are not found in England. Komatiites form by fast crystallisation of very hot depolymerised silicate melt, which leads us to what it really is: Slag. Slag can sometimes be very hot depolymerised silicate artificial melt. Iron and steel production was very common in north east England, so this is the most likely explanation. Slag.
If the rock did not have the vesicles, I would say it is a komatiite as was suggested above. Because the vesicles are present, I agree with slag. The texture observed in the rock is called "spinifex" texture which is an irregular arrangement of tabular and acicular crystals, common in slag. https://www.researchgate.net/publication/279718297_Metallurgical_slags_with_spinifex_textures