Origin and Quality
Our deposits are of the rarest organic-origin mineral deposits of its type in the United States. This deposit began to form during the Lower Oligocene epoch and contains a rich abundance of mature fulvic micronutrients that are protected by a layer of iron ore.
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Our deposit was formed 23 to 33.9 million years ago*
It is comprised of freshwater layers and oceanic layers of sediment. Enormous prehistoric plants grew with roots that reached deep into the earth to take up an abundance of nutrients. The soil became a rich humus from countless undisturbed life cycles eventually producing a concentrated variety of organic acid molecules. The fulvic acid complex we extract from this material contains a mineral and organic acid profile that is different than fulvic extracted from lignite, leonardite and fermented peat. It is so complex that it cannot be synthesized or reverse engineered.