As Buechel Stone has grown, we have opened and operated additional quarries around the country, all of which are vastly different. Our original quarries contain dolomitic limestone. This is a very hard stone that starts as limestone and through time, heat, water, and compression, the calcium in the limestone was replaced with magnesium. This type of stone is what we knew and worked with for a little over 50 years. It’s quite simple to quarry: remove the overburden, drill and set off a light blast to loosen the stone layers, and quarry it out with a front-end loader. Not only is it fairly straightforward, the layers are also quite flat. The vertical and horizontal seams in the stone make for excellent quarrying and building stone functionality.
But the United States has more to offer than the dolomitic limestone found in Wisconsin. To become a natural stone company with the best domestic stone selection in the industry, we needed to expand our quarrying operations. This was not an easy task, and we are still learning how different the quarrying process is in other parts of the country.
When Buechel Stone opened operations in North Carolina’s Blue Ridge Mountains, we knew it was going to be different from what we were used to, and we were excited about it. Quarrying in the mountains really helps you appreciate how amazing the formation of the world is. As you could see in the pictures from Wisconsin, everything sat nice and flat. You probably learned in your Geography 101 class how mountains are formed in several ways. One formation happens when layered (aka sedimentary) stones are forced into each other at a fracture line. This force takes these horizontal layers and pushes them vertically. As you can see in the image above, extracting this stone takes a little more planning.