Sand calcites are a fascinating mineral oddity formed as calcite crystallizes in sandy soil, capturing sand particles during crystal growth. These crystals typically consist of approximately 40% calcite and 60% sand inclusions. They naturally occur as double-terminated, hexagonal scalenohedrons. The crystals are found within beds of coarse sandstone. This is a notable and very sculptural example of this phenomenon from South Dakota, USA. Other calcite sand concretions are known from only a few localities worldwide, including the Imperial Valley-Salton Sea area of California. This unique formation process and the resulting distinctive crystal morphology make sand calcites an intriguing subject of study in mineralogy.
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