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The rate depends on the amount of carbon dioxide held in solution, on temperature, and on other factors.
When the solution reaches an air-filled cave, a discharge of carbon dioxide may alter the water's ability to hold these minerals in solution, causing its solutes to precipitate.
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Note: Many of our articles have direct quotes from sources you can cite, within the Wikipedia article! Speleothems are typically formed in limestone or dolostone solutional caves.
A speleothem (from the Greek for "cave deposit"), commonly known as a cave formation, is a secondary mineral deposit formed in a cave.
Water seeping through cracks in a cave's surrounding bedrock may dissolve certain compounds, usually calcite and aragonite (both calcium carbonate), or gypsum (calcium sulfate).Speleothems made of pure calcium carbonate are a translucent white color, but often speleothems are colored by minerals such as iron, copper or manganese, or may be brown because of mud and silt particulate inclusions.Many factors impact the shape and color of speleothem formations including the rate and direction of water seepage, the amount of acid in the water, the temperature and humidity content of a cave, air currents, the above ground climate, the amount of annual rainfall and the density of the plant cover.An ongoing debate within paleoanthropology is whether to place Ngandong hominids as Homo sapiens.Replacement theory predicts that Late Pleistocene Africans and Levantines are direct ancestors of WHL-50 and that Ngandong hominids are not direct ancestors of WHL-50.These phases cause displacements in the surrounding sediment and stratigraphy, thus making it difficult to properly date the fossil.