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Carbonate Intraclasts, Mt. Yamnuska
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Carbonate Intraclasts, Mt. Yamnuska
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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
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Digitized Date
07/30/2016
Creator
Dolphin, Glenn
Digital Publisher
Calgary : University of Calgary
Country
Canada
Province
Alberta
Municipality
Kananaskis Improvement District
How can you use this image?
Permitted uses are outlined in License and Usage Rights. Usage Restrictions can only be waived by the copyright holder. Add to cart and make a request if you have any questions.
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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