I wrote a post back in December entitled: “So what is slate anyway?”.
What’s really fascinating about geology is that it never stops its inherent onward progression! Slate, if subjected to further heat and pressure will change into other types of stone. With this additional metamorphism, slate turns to phyllite, then to schist or gneiss.
Check out the links – It makes for some very interesting reading.
There are loads of reclaimed wood stories out there, and some of them are downright incredible. One of the most attractive aspects of reclaimed... read more
In recent years, we’ve had troubles here in British Columbia with the pine beetle. Due to the warmer winter months thanks to global climate... read more
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