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most common types of carbonates |
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Color of speleothems due to impurities: Iron |
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Color of speleothems due to impurities: Silt |
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Color of speleothems due to impurities: Manganese |
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Blue black and blueish greay |
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Color of speleothems due to impurities: Copper |
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Color of speleothems due to impurities: Nickel |
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small, crystal-lined cavities exposed during cave formation |
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mineral blades projecting from cave wall resembling a honeycomb; formed where veins in limestone were filled by a mineral |
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secondary deposit within the bedrock that became exposed during cave development |
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Describe crystalline forms of argonite |
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thin needle-like crsytals |
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Describe crystalline forms of calcite |
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short, stubby, dogtooth-like |
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formation formed by water flowing over floor, ledge or wall |
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globular forms composed of concentric layers of carbonate |
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thin-walled, round, hollow speleothems formed by calcite deposition around gas bubbles in water |
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free floating, thin crusts forming on the water’s surface in quiet cave pools; sunken rafts accumulate in heaps known as raft cones |
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protrudes from the wall like a shelf |
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is the 2nd most common mineral in caves after calcite; typically formed by evaporation of sulfate-containing waters; since water is usually not present in large amounts, sulfate speleothems tend to be deposited as coatings |
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hard rock erosional caves |
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ormed in granitoid rocks in some of the mountainous regions of the western United States. Sand particles borne by floodwaters have played a large role in creating this system.
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