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| | IngentaConnect Relict tufa at Miette Hot Springs, Jasper National Park, Alberta,... |
 | | The tufa, composed of low-Mg calcite, precipitated from waters discharged from a line of perched springs. |
 | | The relict tufa is divided into six morphotypes that reflect variations in water flow down the steep and rugged flow path. |
 | | The tufa contains stromatolitic facies (including streamer, porous laminar, dense laminar) and nonstromatolitic facies (bedded, crenulated) that reflect variations in the biology, water temperature, and style of flow of different parts of the spring flow path. |
| www.ingentaconnect.com /content/nrc/cjes/2003/00000040/00000011/art00004 (524 words) |
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