Carbonate Intraclasts, Mt. Yamnuska

Carbonate intraclasts are carbonate fragments that have been transported by tides, waves and storms. The internal structure of each clasts can still be seen but they have been rearranged and deposited together. The allochems in this sample are composed of micrite (carbonate mud) and deposited in spary calcite. Allochems are the recognizable grains present in carbonate rocks

Digitized Date 07/30/2016

Creator Dolphin, Glenn

Digital Publisher Calgary : University of Calgary

Country Canada

Province Alberta

Municipality Kananaskis Improvement District

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Copyright Status In copyright

License URL https://creativecommons.org/licenses/by/4.0/

Attribution "Carbonate Intraclasts, Mt. Yamnuska", 2016, (CU123293) by , is used under . Courtesy of Collection, Libraries and Cultural Resources Digital Collections, University of Calgary.

Unique identifier: CU123293

Legacy Identifier: 20190213_geoimage_Dolphin_e_0136

Type: Geoscience Image

Size: 5184px × 3456px 18MB