Calcite from the Viburnum Trend in Missouri is known for its unique geological characteristics and vibrant colors. The Viburnum Trend is part of the larger Missouri Lead Belt, a region renowned for its mineral deposits, primarily lead and zinc ores. The calcite found here occurs in association with these ores, often exhibiting distinct crystal formations, which can be clear, white, or even show striking hues of orange and yellow due to iron inclusions.

The formation of calcite in the Viburnum Trend is linked to the hydrothermal processes that impacted the region millions of years ago. This mineral typically appears in a variety of crystal shapes, including rhombohedra, which are characteristic of the calcite mineral family.

Collectors value Viburnum Trend calcite not only for its aesthetic appeal but also for its significance in understanding the geological history of the area. Specimens from this region often contain inclusions or are found in association with other minerals like sphalerite and galena, further enhancing their desirability.

In addition to its mineralogical importance, calcite from the Viburnum Trend is popular among lapidary enthusiasts. When polished, it can exhibit a beautiful luster and a pleasing finish, making it a favored material for decorative objects and jewelry.

Overall, calcite from the Viburnum Trend offers both mineral collectors and enthusiasts a glimpse into the rich geological past of Missouri, showcasing the intricate natural processes that have shaped this distinctive area.