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I gathered these downstream from the Oldman River dam in southern Alberta, it exits the Rocky Mountains nearby. I want to paint on underglazes, clear glaze over them and fire to cone 4-6. Upper right: The rocks as I gathered them. Lower left: After firing to cone 04 (about 1900F). Lower right: After I poured water on them! Seven disintegrated in front of my eyes. With sound effects, high heat, even steam! That means they are all limestone or dolostone. The firing drove off the carbonate (they lost considerable weight and converted to calcium oxide, or Quicklime). When the water is added hydrated lime (calcium hydroxide) is produced. #5 and #10 cracked badly. The unfractured ones appear to be iron-bearing silt and sand stones, they can withstand considerably higher temperatures.
Things to note. The orange is not developing well, it is flaking off #2 and #6. The black is flaking off #2. The yellow works on everything. The degree of flaking on #6 indicates it is likely quartz.
URLs |
https://miningmatters.ca/school-programs/students/rock-and-mineral-identification-guides/rock-identification-guide
Identify a Rock Complete with photos and information about each rock’s distinguishing characteristics. |
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Minerals |
Limestone
Limestone forms by sedimentation, of coral and shells (biological limestone) or by the precipitation |
Minerals |
Dolomite
Dolomite, as a rock, is called "dolomitic limestone". It is a carbonate, similar to limestone, but h |
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